RPT ON JOSEPHINE MINE - Geology Ontario

Kp""-*'

eeis CORBIERE 0107ort Arthur, Ontario,

September 2 r 1916,

The Alcona Steel Corpora t i or., Ltd.,

Ssiult Ste. !'u-ie,

Ontario.

r.vjfje :!cJ!aj? , "'ho is ons of tlife orders of the Jcs-

etV.ns Tro* i'i^s su,'.-:es;ted t'.at I should v/rite to you4b J OW **

re^ai-aiT this nropertv.' I have a** eotimte, made by anC-* tx jL * v FI/-

experienced ri~i*-r onrir.eer, and. ho estimtes that there .

?.re 1,431,252 ^ros's tons of ore proven uo in the'Josephine

Iron !!ine, as appears by the drill records; and the re

port i c confir.red by c.^ experienced nine *.!ancxer,

" " isriv.1 ^ t.j' e r'clos*; a cc1 ^*' of a report !ii?d.e b*' **".

Alois Costs, v/'.o is irtoroste-I i", t' is :::ine, and f i* on

this ;'cv; v:ill see that the o'.vr-ers arc co^fide^t that r;ith

the fye?.t depth of the oro body, there is a very lar^e

ton^r/e in i.'iri"; ''lai:.! "-."1, or v.\ .!c!i .-.l-^'nt all of the

dia::','-.'i c'.rillipf has be?r done, -- th;;-!! ^r-:: t;o i:.-;.'crt-

i-rt c-r5 V.v.aar. -r* the '..ftfitw*? bou v.rj-r, ab:-ut 1500 fact

l/V

,...; .e o""-crs '

ti.rc"- h t" t1 of c j" i ', o c"';'i"f;.

:^;':vX:V 'to lease or coll the property

(:

it* (2)

'filling to lease the three wiring- claims to you for 25

years, subject to the payrcert of a royalty,of 20 cents

per ton on all merchantable ore; and also give you an

option for two years to purchase Y451 for $300,000; pay-t

able i^ four equal arrual irstiillmeHs of v75,000 each;

v.'ith interest at six (6) per cert, pc-r a^m, so that

you could pay ths ûrcluv. : -i-j- -raol:-3illy out .of the

ore ?:;ir.3a each ye^r; ar/i they -vovild probably give you a

further option to purchase the other t',?o claims for

9200;000 additioral. -

I have beer, corresponding' r/ith some prospective

purchasers in the United States; but ouoted :to then 25

cents per ton royalty, a^d ^500,000 as the piirchase

price; but I thought it might be advisable to let you

!:no'.r the best ;:.'o'j..ole terr-s r.:S ov.-êrs v;oalu be dis

pose f to offer t) .you, as tl.sre seems to be a disposition

or the part of rii^'ir.^ capitr.listc ir. the United Sta'josûrch'''co

to rive a nore fuvcrable consi-rievutior. to rrxxrs'-rnf -ro-*

rerties ir Crtnrio than i v former years.

If you are disposed to coâider the proposition, I

vrov.ld be jleasei to jiear f rain you at .^ ei'.rly cbte.* *lC" f 'i*'* l "(

^ l J. -I.J~

Oct.

baa forvarded lluo prints tind reports on th0 Jocopbiw Mine, and aoliod roe to look then owr end let you hnva ny opinion on tbeof nleo tbo probftble cost of sinking ehaf t 400 foot nnd equip-* ping Mine for 603 tons per cfcgr. I trust therefore thoso suggsstiono will be of interest to y(w.

The cost of sinking, dc5telopinc tmd equipping I bairo placed at tho follotfinff approximate figures*

Sinking Shaft 55D,(XX).

ItevelopDent 25, (XX),

Hoist and Gklp3 0,CX)0.

Conpressor . 7^000.Blaokeaith Shop . 2,000.

Sfichine Drills 2,000.

Cweber Plant 5,000,

Building fi Bins * 10,000.

CaoJ and Hquipaent 5,000. '

Flectrio Installnenta 15,000.?

Pjwps 2,000.?Pipes Rails Etc. 3,000.

Boilor 5 Eoiet (for preliminary devrl^ont sork) 3,000.

Foundations 20,000.

cost of sinking I have placed at 250,000 for a three-

conperfccent shaft. This figure for nonnnl c?nditicins, if fc lot of

water is encountered and surrounding conditirpc naturally warrant it,

it soing undor the lake, even if tho laVo lo dr&inod and local otri

diverted, the Ronoral fwr round ln#a will naturally drain a good daul

of surface, I irsagine J&SL tbwreforo you trill tato considerable water* to contend with, if eo It will cost KOTO than fi^uro su'boitted, and

my estimate for punping outfit is too lou; it oill Ixs herd to eetiia*

ate this until property ia Oavelopod end quantity of t?ater to fce

bandied dstcrrained; but under norcjnl conditions this ehould install

o very satisfactory oi\tfit.

ft * The drifting, raising, and opening ap etopoe, 10 aaIwportant feature to in&tre a ctoady oufput, ond ohould always kept well in advance. For this, you will tjot*i I hava made nn ea-

tinate of #53,000* S'hio diould pat tVid Jline in gpbd wcrkiug condition*It will be n^cessaxv to eroot Q tesporary Honil-frajae for pre-

lirainerjr work, or until ehaf t is doep enough frooi luosting daiger,

tsid shaft collar permanently f bed, before IjeaJ ifrarse can ', ,- ercc- tod* win leave this for on after consideration tn cocte under the head of contingsnoies*

Tho tesnorary head tfrgsje ie included in the 53,000 for boiler* i *

and hoist in prslisinory developarat wort*t- After the different levels and raises b aye beoa put

in sbape end slopes opened upt l would figure tfie tX)st ofot 01.75 per ton jrad on oars at dine* This nny seoi hiî, lw t youmat bftfcr in mind labor conditions nnd prosoni ooet of nateriiU.* -

*

* The hnarl fratio to be oonsidorod, tho olootric in-and pumping, end water conditions, in Killing doubtful,

I would plsê figure f o." CbntU^nclRa at ^42,000, imkin^ tus total

nam of 3200,000 fbr sinking developing and cîppir^ aino for 600

Ions p r clay. Figure usj coe* higi for Contin^nciosj bii 'sr

thin hcs5 will cczc Jis v?cll iis hsao-iranie, iroa of different diaen-

necessary for equipping, stoel for drills, ond extra repsir

for drills end îcHncry; also Bail*ay Rea lee to bo oonsidnrod

estimated Crash or Building and Oro Bins for about 1,030 tons

cnpncity, which iu iuudoquato for a 600-ton output, unless you have!

c^trenely ôod Hail esryico, and s^ne portiui of this eetioate for

Contingeticioa tiny bs needed to increase capacity fo? otorage; BO,

tnkon on t!io u'-nlc, l thinS: it ie a very conservative estimate*

^.^ Ha P'ill Holes, and the advisability rt d rilling

nest of Holsa lo and 18. I ttould not advise doing this at present

You have on cstiaitrte of one cullicn lona or thereabouts, elrondy

proved by ditônd drill \wrkj chy not unit until you net under

inn; conditicas end ttork îs ors todies ulreauy pwsveC in that directio

to their Ifcclt, sny fit the 403-foot level. 7hen, if it is tteu/Tbtj

fldvitfttle, sot up the drill underground, and rusko o test. By that

tiso yo:2 will heve a better idea of tiê trcno of tho oro bodies ond

rrivs .-50 re definite qata on the boundnry of the iron ibrnation.

. .flit ' ^This.canbe toa* without interfering in any nay with the

ot a good deal less cost, and 09 far 89 J can as*, without anyV; . ";-i; f. -.'-' ' i -, -.''- - v . -. " '

!!S- VKVto the settling location for shaft nt nny time. Wonl4

locating it BB near central point as poscibla of ore bodies proved by dianond drill wor!c,(eurfnce coaditlone fevorablo).

These nre only a few suggest inns based on practical ootperience and ^ile you have had reports froa experts asd their ndvioe, and thew parties having been on the location, will *mve o bottsr idoa of conditions and should bo in a better condition to report on it*

Kill be pleased to let you have ay opinion on CD y thin^ I can assist you with at any titse.

lours very tmly,

33POBT O? 7m J033PHIJ3 IHON I.M III TH2 HIOHIPICOTSN DI3JHICT

Iff THE PROVINCE OP OKTASIO AND DOMINION OF CANADA.

The Josephine Hine is situated on a short spur of the Algoma

Central b Hudson Bajt Railway, twenty miles from the Harbor of

Michipicoten on Lake Superior;1 where there is a modern ore dock

for the handling of iron ore, and consists of one patented min

ing claim containing 75 acres, extending along the iron range for

nearly Half a mile. It is about 170 miles north of the City of

Sault Ste. 1,'ario. The timber consists of spruce, balsam,1 and

white birch. Electric power for all purposes may be obtained

from the Algoiaa Power Company of Berlin, Ontario, which has de- 'j

veloped a large water pow^r on the L'ichipicoten Biver, about

twelve miles to the southwest.

The greater part of the claim is covered by the waters of

Hed Lake, which contains about 100 acres, and having a very ir

regular bottom. The deepest parts are two small areas, one of

which is close to the northeastern shore, and the other is near

the outlet of the lakeiSjBoth depressions .attain a depth of 66

feet. The depth of the pther parts of the lake veries sar-rrdrdssai

K*n2ygreatly, and would probably average about 30 feet. It em

pties by a short creel: wfth a gradual and stoop fall of 0*39 hun

dred feet into Goetz Ls.1:^ to the west, and should be drained be

fore mining operations are begun in order to nine the pre bodies

safely and also to give qccss.-; to the lake bottom for inspection

whether any of the ore still crovs out. I.'any large and s.'^ll

r.icoes of ore lie DCS! t :To3 o?i t\? s ? :ore a-d a o;'a c e:, l 1^0.,* * *,, l* .A,' ^11** "11:)-:.;-:-.i :i a^:.: -v.'t 1:^0.^1 ov.; ".-. ..is i - '? '•...•',\r -Jv j;l^e;..

' ti;r. v,\;ich .;i{::t r.ot :..:vo s'/opt t'.ie lake Tloor clean of or a

./hi eh

•;T'V nik ', l -, , /.., (

(2)

close to this shore are a string of small rocky,islands of green

stone, running north-easterly. Those; together with the buckling

movement of the southern rocks, evidently contributed to the

Mattering of the iron formation, thereby aiding in their des

truction by weathering ancl so forming the lake basin and also en

riching the iron rocks below.It is a difficult matter to definitely estimate the number

of tons shown up between holes 53 and 18, a distance of about

850 feet; as two of the holes were stopjed in ore, and several

others^ did not entirely pass through the iron formation, leaving

portions of the areas in tauby as to what they contain.

Taking the Iqiown width of the ore bodies and figuring from

the 300 foot level (about 50 feet of which is lake water) to the

900 foot level will give on a conservative estimate about 1,000,-

000 tons of 59;* ore of bessemer quality and about the sarae number

of tons of a 40;? ore, also of good quality, p-'?d a large tonnage*

more or less mixed with silica and so..ie solid ore high in sulphur;

but low in phosphorus, both of which would reqv.ire some sort of

treatment before becoming available for smelting purposes. Prob

ably in mining the ore a .much higher tonnage might be developed

in the areas under consideration and in addition thereto probably

a very large tonnage belo'7 the 900 foot lev-d,and my reasons for

thr'-cing so are given, as well as a few notes applying to other

parts of the range on this, property. Hear the western boundary,

which is about 1700 feet 'vest of the said eoti'^ted deposit, the

di.-. :^d Srill cut through |25 and L j foot of ^o.'d hartite ore, at

L .'U/'th of Jvx/t 330 f:;ct f ' anil t.";c irtsrvenir.^ territory fer the

distance of 1700 foot is very pro.nisin^, .vi :;;.y contain many :-*".V -r*. -,f ! ' v- cf r'" . i - - -- -' - -"- - -; ; . . . ; . .

.y

(3)

which has only boon ponetrated to o width of ten feet iHole 51 driven directly below hole 52, at a higher angle;

oufefc the sane width of iron formation at a vertical depth of 1615

feet, including therein about the sa;ne kind of jnaterial as in hole

52, and stops in less than ten feet width of schists. Hole 17,

at a vertical depth of 740 feet, shows a width of iron rocks of

S?5n rocks or 270 feet, including therein in the lower 110 feet

foedskof solid ore aggregating a width of about 50 ieet with no

schist inside the formation. Though hole 53, about 360 feet high

er up; shows towards the bottom of the hole about 13 foot bed of

schist followed by a 35 foot bed of ore resting on the underlying

schists. Hole 16 to the east; shows a width of 330 feet of iron

formation with no schists included. Included in the lower 140

feet are solid beds of ccre^ aggregating a width of about 50 feet,

and a solid bed of ore 45 feet wide, resting on the schists. It

is hardly probable that the.iron formation pinches to such nar

row limits as shown in hdlbs No* 51 and No.52 in so short a space,

and in view of the fact thiit it includes layers of schist (less- ,

oning still more the width of the iron fo'fnation) while none are

chowr on the deeper parts of adjacent holes. It seerns reasonable

to think that beyond the lower shMsts of v/h i eh only a width of

less than ter. feet has been penetrated, more iron formation ex

ists, holding similar ore bodies as shown in the neighboring holes.

Holes 11 and 50, farther to the '.vest, which are not inolad^I in

the C3ti?'i-te of" available ores, ;jr; v.i urob^bl^ do indicate a

0".li t ' .':j:', that

'.-s. Still, t", ere is roora for a

.vi it -.".ay b;; icivisiblo to sir.k

hole 5D Hole ;3-.- reaches :-. ve// tic;.; l of 245 feet to

(4)

feet of iron rocks, apparently stopping at a point ^7here hole No*

54 indicates as entering schists, according to the scale of the

plan furnished to me. If the measurements thereon are correct;1

then hole 6 has not gone far enough to reach the ore beds out

lined in hole 54 in their extension dovmwards. At any rate, the

bore hole has not gone through the entire formation, thereby

leaving a doubt as to what might be there.Hote- To make things

clear I may say that I had access to the firill bores from holes

Nos. 50 to 54 inclusive, and for all of the other holes I have

drill hole plans only for my information. Hole no 7 attains a

vertical depth of 325 feet anid a horizontal distance of 345 feet;

penetrating only 90 feet of iron formation, ircludir.g therein a

6 foot bed of ore, and the last few feet of the drill entered an

other bed of ore, and stops therein. The iron formation appears

to sv;ing a little ir the direction the drill hole takes; therefore

one would have to cut nore of the iron rocks than in hole 15 to

reach the same point where ore is entered. So there is but littlej

room for doubt that there might be as much oro hore as ir hole 15.

"ole ?*o. 15 reaches a vertical depth of 590 feet and a horizontal

distance of about 300 feet, jjer.etratirig orly ICO feet of iron for-j

nation, 94iV feet of which is ore. 1-earr.:^ i"! rind that the iron

formation varies between 20C1 jurcl SCC feot ara that drill holes in

ore, it ie. clear that at lessjt sorr.e ore m&ht lie beyond. Hole Fo.

16 att^Jr.s a vertical depth of 660 feet ar.d a horizontal distancej

of i: l'O Teet, voretntir?. 4". feet width:::: o f ore, followed by 59

'oot v.'.rih of roc1.: ( !;i"u ^oi i.ie^tiov.ed O" drill hole cltr ) thor.i

oc':.'C;?j i. Y/idth of 131- ftet of lore, ic'llo'.veu by a v;ic.th of 16 fee.ti** * * ^ * . . . j * *t n B,|*M m * t J l "( l *, l ^ A.*. 90p r -* - ^ ft t O. l ** "" 't tV^ IMP f l Y) J ' i^O'f: ~^' ' CJ v s " " ^ *''' L'J --I " " f-- \ - *

•-.•. * .•••."•A ^ . . ... V./,' V t ' W- -,- ± J -*f. ~. B * W M. V ^ ~" v J , . t- . . * , . U-.'W^v .i. - i ^. * f i **t , -' \t

(5)

ought to bo sought for at a much doepor level. Intermediate drill

holes should be put down at angles to cut the iron rocks at deep

levels as the appearance of this area warrants the expectation of

finding large ore bodies therein. The flrillind done on this claim

east of Hole Ho. 11 apparently does not cut the iron formation in

such manner as to indicate that it is unpromising or holds no ore.

A few well placed drill hoj.es north of the iron formation, driven

southward at an angle to reach a vertical depth of 800 feet or 900

feet or even much deeper probably would show more encouraging re

sults, as for a distance of about 1700 feet, between holes 12 and

17 is equally favorable for ore concentration. The ore bodies

shown it holes 12 and 17 may extend through the claim and contain

large quantities of good ore.

Ore possibilities in depth.

C.3. Van Hise in the twenty-first Report of the United States

Geological Survey, 1900, Part 3, Pages 410-411 refers to the Michi

picoten Iron Range as reselling the Vermilion so elosely that

there is little doubt in his mind that the two districts are in

most essential points alike. In The Geology of The Lake Superior

Region, by C.3. Van Hise and O.K. Leith, 1911, rage 1Q, they say

that the geology of the ""ic::ij,icoterj District is remarkably sim

ilar to that of the Vermilion District of Minnesota in regard to

lithology, succession a-:J structure. A.?. Solemn and ...3. '.7il-

uott, two Car.&diar. Government Geologists in the Ontario Bureau of

I.'ines Beport, page 175, also speak of the conditions obts.ir.ing at

~ec Ii.ke ( :"::rks 1^:6} ns cpi^^ s irr.ilsr to those at lily on the

Vermilion .".:."?e 2 :: a t".i-l; pr.it a-y o;-s body f our. t! Y; ill be at the

bottcL'i of t::':.:-:,:iTS3c:-pi ircr. ifcrroatio**- in the trouch made by the

/

i (6)

T they may lie deeper down than at others* -

: The narrow bed of ore and the larger bed ofppyrit&o ore cut

. at a vertical depth of 161(5 feet in.hole 51; and also at a higher

level in Hole Noi 52 indicates that the ore bodies shown in the

other bore holes probably ^Iso attain great depth and may event- .

rally dip into the lower basins.

Hote./ The Soudan Lline) on the Vermilion Hange is being mined

at a vertical depth of 1250 feet. Ore occurs in lenses from 150

feet to 1000 feet long, fiVe to eight feet wide, and has produced

over 8,'500,000 tons of ore see Iron 1-ining In Kirr.esota; by C.B,

Van Barneveld in 1918.

Therefore, taking all things into consideration, it seems

that the Josephine should be a very attractive property, -

I)rill Hole Record.

Drill Hole Mo. 19 is located on the north shore of Hed Lake, about

200 feet west of Post Fo. 4 on the claim, sunk at an angle of 624

degress S 40 degrees E to a depth of 892 feet. It reaches a vert

ical depth of ?50 feet to bottom of ore resting on schist.

Schist L'ixed ore Solid ore

to 614

to 853 lying at an ar^le of about 54 degrees 25 feet bed of ore (ho assay riven.)

Schist to 692

Drill Hole Mo. 12 is -locatefl about SO feet east of Hole 19, sunk

at an a^gle of 55 deirees 3 35 degrees 3 to a depth of 715 feet.

It reaches a vertical depth of 570 feet to bottom of iron, lying

about 60 feet uest of the -.Test boundary lino of the claim. Hole# l

IS i-cUcates a 250 foot v;:dth of irov- rocks a-d as hole I'o 12 per- ctri'cs or:J..7 ]35 feet ore :;*y e::ist brlotv tl.fi bott^i of the hole.

574~

..

(V... •' ;' J^.^'/v

. . . AJ

/

/,

(7)

mffi.*:-:-- ^Schist

^ Schist

to 150jasper to 355 J to512 .

- -Drill Hole No. W l located near the middle of Jasper Island

(wL.'ch name is misleading, as it is composed of softish red hema

tite and quartzite, and the word "banded jasper" use.d to designate

iron rocks in the drill hoj.es probably means the same sort of mat

erial) and about 900 feet east of the western boundary line of; l

the claim; is sunk at an angle of 45 deg. S 10 deg. E ( in a dir

ection away from the main "body of theiron rocks ) to a depth of

460 feet. As the iron formation dips northv/ard, a clrill hole lo

cated on the little greenstone island driven southward at an angle

to reach a vertical depth towards Jasper Island of about 800 feet

probably would show better results,

Drill hole No. l, loc&ted on the eastern end of Jasper Is

land about 250 east of Hole '.7-1 is sunk at an angle of 50 'degrees

3 to a depth of 416 feet reaching a vertical depth of about 315

feet banded jasper including three narrow beds of ore to 255

feet, each bed is about 5 feet wide but no assay given.

Brill Hole No. 4 located about 300 feet N.3. of No. l is sunk

to E vertical depth of 296 feet; banded jasper. Drill hole No. 11

located about 400 feet northward of Hole I'o. l on a smll island

of massive green.. i.,, 10 is sunk at an angle of 50 deg. S 46 deg. 2.

to a depth of 717-j feet, reaching a vertical depth of 385 feet

to bottom of iror rocks, cutting a width of iron rocks of or*lyi r-? r: r r. -i JLOv A GGl.

Schist to 363tesr to

ecu- it:- -X

j (f j c.-. 5 //('' ' k^t. i - i - ..\^t. j

A -j \'j 7 { * --..i'

(8)

'Schist to 536 Banded iasper to 597

v Ore to 603 allowing for angle ofFe S Si02 Pore bJds.-5 ft. ore 60 .05210 P

lean ore to 631 18 ft 21.90.025 60 Ore to 642 ' 7 ft 35.70.070 46 Banded jasper to 652 ^rt nen Ore to 661 6 ft 39.80.850 40 Quartzite lean in

6 ' 5

Pyritic Ore 712 5 -' . 52. 3.29 21.

' Drill Hole No 17 is located about ftOO feet northerly of Hole

ITo. 11 on the western end of Greenstone Island and is sunk at an

angle of 68 degrees S 50 degrees E to a depth of 935 feet; readgihg

a vertical depth of 740 feet and the iron formation here has a wid

th of 270 feet.

Greenstone to 450 xxzclexait'istrataxs Banded jasper to 480 feftxxj-Ore to 485 Angle of strata about C5?e S P Si02

deg. 4V [et. bed of ore 51.50 .030 .067 24.25 Banded jasper to 645Ore to 655 Bs if t. assay not given. Banded jasper to 689Ore to 698 8V ft. 50.66 .050 .067 Banded jasper to 735Ore to 760 18 if t. 52. .035 .064 Banded jasper to 778Ore to 803 18ft. 63.50 .045 .061

935

Drill Hole No. 53 is located along side hole Ho 171 and is sunk

p.t ar angle of 38 deg.S 50 deg.3 to a depth of 613 feet, reaching a

vertical depth of 355 foet to bottom of ore and the iron rocks show

a r.idth of 230 feet.

Schist toQuartzite leanin irorL- .n ore 453 angle of about 65 dec.

about 13 ft. bed 2e 26.70 3 .050 3i02 55. P Black slate 457 fritr Slxsft .fifiSbc ^fixx Lean Ore 463 6ft. 31.50 .009 46. Quartzite lean in iron 500Ore 515 JL5 ft. 59.90 .097 43.00 Schist iron stained 522Ore 534 12 ft. 33:10 .007 43.20 Schist 546VOre 567 20V ft. 33.60 .010 44.00 .™. Ore 582 JL5 ft. 50.80 .961 22.45 .010

Drill Hole Ho. 51 is located north of Hole 53 on the north

shore of the Island, su^.k p.t an ar.gV of 80 deg.. S 50 deg. 2 to a

.•;*. 1 v-

^

(9) i,

1695 feet; reaching a vertical deuth of 1615 foot to bot-f/ ' ^f ;ton of ore; penetrating only 80 feet of iron formation and 8k feet

' of schist at the bottom-of hole; not far enough to determine whether

1 this is all of the iron rocks at this point; as hole Jfo.17 on the

west shows the iron formation to have a width of 270 feet.

Greenstone to Ore to

11671174 in about vertical

plane about 22 Pe S SiOE P inchos of ore 47.02 ;OE5 24735.019

Quart ait e and narrow beds of low grade ore and schist to 1575Ore to 1585 fc* ft oro aver.33.50 .318 38.00; Schist aid a little uartzite 1602

itic ore 1640 7 ft. - 50.14 9.345 19.41 .010chist to 1696 ft.

Drill Hole No i 52 is located about 150 feet N 50 deg.S from

Hole 51; on the north shore of 3ed Lake, sunk at an angle of 66i

degi S 50 deg. S to a depth of 1114 feet; reaching a vertical dep

th of 985 feet to bottom of ore; also penetrating only 80 feet of

iron rocks and about 10 feet of schist at bottom of hole; not far

enough to determine whether there are no iron rocks; and ore be

yond the schist, as hole 16 to the east sho\?s ar. iron formation

330 wide with a 45 foot body of ora resting on the schist.

865a

687 at

t.uartsite lean ir. iror901

Greenstone toOre (Schist turnedinto ore) vert.ulane P e

9 ft. bed*aver. 47.

Lcw-nrade ore "uartsite ard iron low-grade ore Schist?.u2rt:;ite a^d iron lc'?r' ;"d{le ore

Ci'eci'sior.e to C: e to"witlo ore

ls f t. 927954 111 ft. 962 1010

OQ f t^J * .

30.

S Si02 .012 26.00

.008 52.60

.012 51;

101-19 Li ft

...,. f-\ "iOtr i" ]fe ft.10?0 3 1/S ft. ?.114 about 10 r'.

31.50 .008 50.20

3-3.90 .026 40.CO.41 .083 4.64 '"..C5 S.50 20.

.028

.003

l

t*frv&ii^H5'v-

0

W1.

Drill Hole To.13 is located 200 foot N.3. from Holo 51 on

Greenstone Island and is sunk at an angle of 55 deg. S 45 deg. S

to a depth of 740 feet; reaching a vertical depth '" 560 feet to

bottoia of iron ore. Hole 16, about E40 feet below hole 13 shows iron

rocks to a width of 330 feet with ore resting on the schist; while

hole 13 penetrated only 315 feet and is bottomed in iron rocks;

.do)-.v . . , .

pi therefore ore may exist belojy the hole.i|-i :-., - j . ^i-'.iSchist to 422

J'asper to S49 ' Pe S P sioaor ore.55.78 ;103 .028 19.17

mpj:1 : Drill Hole Ho.16 is located along side of Hole 13; and is sunk atd/*;"'.' ' - b !

f; an angle of 68 deg;'S 50 deg. S to a depth of 1001 feet; reaching^ --- a vortical depth of 820 foet to bottom of hole.*.; ' .i

Greenstones to 512Banded including 2narrow beds of ore 725

; Ore low grade 735 at an angle of 50de^;- 9 ft. bed of ?e S P Si02 ore 30 15

Ore to , 740 4| ft. 62ll7 .044 .024 9.45Banded tp 745Ore to ' 750 41 ' 58.82 .049 .028 11;15

38.820?edto t0 810 27 . 33.30 .067 .029 40.20 Banded to aiOOre to 890 45 ft aver. 52. .015 .020 26.Ore and schist 910 assiW not given,Schist to 1001

Drill Hole !Io.54 is located about 50 feet north from Hole 13

and is sunk at an angle of 30 deg. S 68 deg. E to a depth of 536

feet, reaching a vertical depth of 845 feet to bottora of iron, *r.d

a horisor.tsl distance of 435 foet, and the iron formation has a

width of about 230 feet. The drill coro cleavage shows a vertical dip.

Schist toQuartzite lean in iron330, ' Po 3 Si02 Ore low grade) 346} 30.30 .010 54. Ore low grade) 354) dip vert. 21 ft. 31.24 .010 52.20

SiJj0 -f A * ^95 ^ f? ' Or0 ' 37 ' 80 ^ 42-20 Quartzite and ore insraall pieces only 15in. of core to 406 VOre to . 457 17ft. 33.10.010 47.80 Quartsite and black slato 464

SLt.it. and iron 8 U "' 35 ' 10 ' 070nOre (schist tinned anto iron - - 7 ft,'

jl

Prill Hole No. 6 located on the eastern shore of 3ed Lake, abouti

i (11)i

-, 800 foot S 55 dog, E from Hole 54 is sunk at an angle of 45 dog.

N 45 deg. TT to a depth of 423 C00 ** reaching a vortical depth of. i

325 feet to bottom of hole atjd a horizontal distance of 340 feet

penetrating about 90 feet of iron rocks.

l

Schist to Banded to

345473

Drill Hole Fo,7 is located beside hole 6 and is sunk at amj

ang;e pf 45 degrees H 10 degrees T/ to a depth of 491 feet,' havingl

a vertical depth of 335 feet to botton of 'ore and a horizontal dis

tance of 345 feet, The Hole penetrates only 3-10 feet of iron for-

Viation, which is here also in a vertical position,1 and is bottomed

in ore, so there is good reaspn for thinking that the ore body

probably is as large and of sjarje quality as in hole 15.

Schist to Banded to Ore to

Banded to Ore to

340 - k 461468 allowing for angle- 6 ft bod of ore

assay rot given.491

Drill Hhle No.15 is'located about 300 feet N 30 deg. S from

hole TIo.7 and is sun]: at an a^gle of 64 dog; H 80 deg T/ to a depth

of 670 feet, reaching a vertical depth of 590 feet to bottom of ore

and a horizontal distance of 300 feet. As or?ly 100 f601 of iron

rocks have beer, penetrated a*:d the hole is bottoue-l in ore, the

chances are that there is protjably very r.rjch wore ore than shown;!

A large arjount of the ore rur.g about c3;* ir. iron. By nir.ir.g the

er.tire b o ci;; it v:ill aver--::e Lom;t z s E 'IO'.T.I hsreon.

Schist to Ore to

Ore to Schist to Ore

455490 allowing for angle t

16 ft ore aver. 353 ,in iron. 505 8* ft. of ore 54' f in iron, 525 670 70 ft. Fe 51 3.009 P.045

l

Kg y

Drill Hole No. Ip is located beside hole 15 and is sunk at an

angle'of 67 de, N 41 {f to a depth of 751 feet; having a vertical

depth of 680 foot to bottom of hole ar.d a horizontal distance of

290 feet. Allowing for the angle of the strata, the hole penetrates

only 95 feot of iron rocks, being bottomed therein.

, Schist tog Oro to

lil Kind of material not

reImBanded to

\fa

5B5535 fit a yertiposition

f? ft, ore no assay given.680710 SOifUono no assay given751

Drill Hole lfo.9 is located 450'feot li 10 deg. E from Hole 18

is'-sunk at an angle of 45 de#. N 12 deg. 17 to a depth of 600

in schist all the way. Apparently having been sunk north ofj

iron form:ition,

Drill Hole No.8 is located 450 feet northerly frora Hole 9 and

is sunk at an angle of 44 deg.S 45 deg.S t-o a depth of 785 feet

reacftcng a vertical depth of 540 feet and a horizontal distance ofi i

579, penetrating and being b^ttoiaed in 450 feet of iron formation:

KSPOHT OP TIH3 JOS3PHIIE IR03

Tho Jooophine mine le located bn a xprcc ohort opur ?f the Algona centra* and Hudoon Railroad ( the railo fron thio opur were removed aurlng the vrar)

i

about *70 ml le D north from Sault Ste arie ,and about 20 niloo JTroa Michi

picoten harbor ,Lako Superior, in the District of Algoma , Canada and oon-

oieto of thro o patontod claina containing *03 aorea , extending along tho

iron range for over one nile * fcitlo io guaranteed by the Province of Efctfco:

Ontario *——————— .. OKIZ&RAL HIFCRl^TIOU ——————————

Hoatly all of tho diamond drilling hao been done on Y45I , \vhich contains 75l

acroa ,the greater port io covered v/ith tho -water of Red (or 2?arkD ) Lake

which contains about 100 acron. It empties by a omall creek .having a fall

of about 100 foot , into Goetz fLalco , about 1300 foot ,to the troottfard *

The depth of the lako vorioo but all along tho northern oide ,the dopth io

froa 45 feet to 66 feet , except a chort otrotoh in tho niddlo near a onrxll

ioland * The sounding -iao a hurried one ^perhaps a nore careful night revoa

-l a contintras deep channel through tho lalro *

On tho Bouthweutern chore of So^l ^tUce on S45I , largo and onnll bouldcro of

rod hcinatite trore otrewn along ^ho choro , nono of them are oocn no;r , pro

bably having boon removed by thb Clergue people for onoltlng purpooen *!

There lo but little doubt that ^hio boulder ore v/as oc6opod O' 1 *- vv glacial

action fron the baoin ncr^ occup|led by ^ed Id:e *j

Tho Clcguo people had ctratecl a ohaf t on tho oouthvreotorn end of . , ±n±

o" tbcdbintending to nine tho oro under tho lake, but it night bc r.oafer

drain the lake. It v/ould bc jkzzfeex. t o nine the ore, the loko baoin oould

also To inopectoc! for aitlcrito, soft r.nd luird rod hoiar.titc of tho boulderi

cl:i;K' f It './oul'A not ta?:o a lar^c buuy of nucj). ore to pay for draining the

Ir^c .TVo •.•.'••••f?v.:rn cho-.r- i-j lov:0. f ;-r rv c.ut 100 feet , inlr.j-.:1. -..O i.cr ; r.lr.r-

-t Vv.r^ic:.l Il'.jIVr, anil ci.': .; 5iillrj r.'.;.;, tj iJv.i;:'ii of TO fe-.t , ur r: v ro

cJ : - i- ;. .'ill'-::*r. ' l- ' -' U:'

.^ c; :,l'-.rly n:::. -:... : v -.llcv j.-. ntior.C'

t Theoa together with the buckling raoYcraent of tho oouthorn rooks evidentlyircoirw'ibuted to tho nhattoring of tho iron pooka f thereby aiding thoir don- '

i

traction by -weathering and no forming the lake baoin and ala o enriching tho

iron rocks below*; A diabase dyke strikes nortbareeterly through tho cast

ehoro of Goots lake intoraectlrig another dyke running northeaoterly close

to tho north chore of êd Lake , which jaakea it clear froia vrhcnce the cruohi*-ing force cane which in all probability chattered tho pinched in iron rocl:

-o to a groat depth ,oonoequen^ly it nay reasonably be asBunod that thej

iron ore bodo aro apt to be foiind ao far down ao the iron formation goeai'i

Tho dip of the strata on the surface io generally otoep to northward ,but

in drill hole SI, it O'.vingo elijghtly southward *(

Y452 , adjoins on tho east , and contains 57 acres , and enbracoo a onalll

part of Eed *ol:e, 77iostrilro^pjt,^jae-^.ron range heada^f or tho, wide clrift^

cororod valley extending eaotwdrdo from tho lake ,and not naich of the irony. - — ^ ___ — ^ —..—..—™— .^— __ ri, . _____ * __ -^—-— - , — - —— - — — ------^....^^.... _ .. ....rocks are oeen for come diotante Inland t but hole JTo.4 8 ohcnro that

lio buried tinder the drift from XThich they rise ijnto a otecp hlcih hill ,' and at the line between Y4D2-4^3 , they are over 600 feet \7ide, continuing

^— r- ———— ~~— ——— - —— ————— - —— "^^~- — ——— ———— —— — ~ * ————— " —— — .. . . '

that width through Y453, \tifti an alnont vertical dip.

va3J.ey opoken of , extends borthoaotorly rJ.ong the range on tho north oidc, bounded by steep ridden 0f olnty ochiot trending in tl:o sri-a direct ion * Along the oouthern oide bf t2io iron roc!;o ,on top of t:in hiî hill

boiildcro of oidcrito r/ero cocn v/hcn otalcing tho claiiao * Ciit-cropo of side- erite v/ore aloo ooon on the ohoro of ^cd IcJic rj;d on tho e an tern boundary of Y453 * Hecent exploration hR9LjUnclo3cd a body of ôldo.rito Sieving an rees

v;ldth of DO foet ,ixnd bnuos frou tho eastern boundary of Y453 ^to *!ithe chore of Ked Lake into vrhi;ch it dips , a dlotance of about 3000

v;ith rji average hlcht of about 1^00 font to la?cc level . Probr.bly nr-iy

can I;D quarried . Drciinin:; the| Ir.hc ,:,hich ic here 6G feet coop night civo

iii^ . At the laJio ocliirjt intcrvoncc

en r.t -"'.i c point lio l r. vied beneath

::: cff;/ ' . i c " l v.r.'i ' " r;:'.: : •••?3v" c ::t-::-- T ,. V -..l ' ^. , rf r- \ f'..,- . .J f , .,..

' l , ^ * . ' . - , . vj.: .- .'A. J . \ ,: * ..

an r.duitionnl Inrjc tcn.ir,^c: for

Vc.t-.73-n tho cidcrito r,nd iron roc!:j

r f- O-

i i' c*. i ...; .

.t iv.;\;: .'.r.vtlr.ro::U:rl;; -M ., ,,..^. :., v,,.,..

eastern oro under tho lake,'Y453, adjoins on tho cant , containing 51 acres ,

On tho northeaotom sido lo a broken baoin acrooo a part of tho range bu*

tho ohattorins and erosion along the oaotorn port of tho rango on tho two

claina has been lean oevore t j an to westward ,but tho iron rocks api*ircntly

are mioh wider from which to draw ferruginous raaterial , so that rod hema

tite nay exiot in tho raney running along on the north oido of tho iron .

,'; Several placea t)n thio clc-in ,in tho volley Dhow

^bandod hematite^ and hcmtito pebbles cemented i"ith hecatito , ao chown

ft plan T7hich should accompany thio report ,

Tho drill plans furnished to us by Algona Steel Corporation in 1914 ,shows

that nil mtorial below 4D/5 i^on was classed as banded so ono night ascura

that only tho oro running about 50# iron was included in their ostixaato oft '

1,250,000, tons of oro * Y3ien M,A, Gootz assembled the two drill plans into

one conploto plan , in Aug,0tfc 1921 1' ho olicvded tho parto mrkod as banded in holes IC-I7 , along r/ith the parto rr.rlrod ao oro , thinking that the

i k j

whole night novr bo taken ao all oro. The undersigned had an opportunity to

oxanino the drillers' 1901 .original drill record books for holeo 17o,I to

10 and at tho sane tine examined all of the drill cores fron No, I to 21,

holeo , in their undisturbed core "boxes , v;hioh had boon left in buildings

at tho Josephine nine, v/hen the Clerguo interests abruptly quit drilling

and shaft sinking , and deserted tho prcnicec v/hich they wore tiying to

vrrongfully acquire under tho Algona Central i: Iludoon Buy railway land gran.i

, md loft things open for anyone that cared to loofc around f * Core boxes

for holes TTo.o. 4-6-7-and 13

.,-*l3O,j3ho\7ecl

it

of oidcrito

I:.".D'' r "/.7 il-.r

::-"in r/-, c',t v/ort ,oi"

ao \7cll ao oone other boxes contained nuch

r. .licrial rated on tlio drill plrji furnished to uo ,ao banded ,v;hich night

j : bo clac: cul ;;a oro .'Die drill rccordo for C-0 rjid 9 Lv ruch and Peternc::, ^....t5\c drill plr-n furniohod uo, do not

'.i ? ". - O '.;i into Hod 7f.\:c ."rid cro^r:

n lino of ,on

- . .L,.*... . .^ wv i .. ^ . , ,

hr... i :.\ o \- -wic;i t...

4.

zaontlon la mds on tho drill plans of thlo o of t material , or choirA l

al holes In the place o aa ohomi on Wiley 'o plan . Probably tho Algona* *Steel Corporation did not got Sattt nn of tho data , prior to 1913, obtain*-od by the Clergue Interests ;;

Holos 12-19 fjuot across tho woijt bodr'bf 7451 , at a depth of about 600 to.

feet ohorrs good hemtite 20 foot -45 foot In width indicating that oro exio**

at tho western end of tho lake. Holo T/2 . angle 45 degroea , depth Illfoet ,'i * * *

fiolo T/3 *anglo 45 degrees depth 41 feet , hole Ifo. 4 Vortical 294 feet , Hole

Ho. 5 angle 50 degrees depth J33 feet , Hole J4 , angle 55 degrees , truo verti! *

-cal depth to Lot tom of banded about 200 f&et ,cutting 3 narrow beds of oro*'

Hole "El. angle 45 degrees starts on southern oldo of iron range ,ooon enterin

-gtfeat the drill plan ahcvnj ochlot * Judging frou tlie carolo33 laannor things!

were done at that tino ,thio ochiot might have boon oiderite * Aloo the niat-

e rial la hole Ho*1 21 closed as jpyritea chert nay have been pyritio siderite

ao hole Uo. 21 , lo about 400 febt tract of the oiderito outcrop on tho oouth-

VDstorn shore of Red I^ko * In vjow of the oro shown in holes Uos,1 12-19 this

drilling cannot bo accepted that no hcoatito exioto in tho trenton* area of

tjje lalro on Y451 * ôrejoarafttl and docpoi^drillin^ngy glvo Cood^roBults *

The lake area cact coot oC hole ilo. I O holds out fairly good proopects of

finding oro JJ}cre as well as in ^ho eactcrn valley * !Eho

north of and.îc4âlo o -Inside .Jtt""- iron fprâtion^ , indicating that they wore

not derived froa the oideritea on tJio ocuth 9 "v/hich my still cxiot in tho

baoin . w. ^" î f f \

Algoma Steel Corporation , tro drilled tho ârca l^trrecn holoo "^0 and 53

in years I9I3-I9I4 , figured that; tliero r;ero 1,250,000 ,toii3 og a liigh grade oro ch07,7i * They took a lease on -the property and paid C'2000* mlvanco royal ties thereon * A fei? \rse!o3 later [V7ar cane and the leano VTH.O canoellod o\?ing

to finr.ncial otrli^cncy. In iilniir; thlo cnallcarea of about 000 feet along the!,:-.d; itio:r..1 ionnaGeu are npt to bo found deeper dovm tlian tho tonnage

totl . rc:.i(:.cr: the lii^h grrxlc oro flora i'; o. l- \rtfo tcrrtv;o r.Vvî'nginc

' i I'C.. t

,. ^ . r- -rL. ^ t - . . . t i. * J

tho general goologioal foaturoo can' •m^rM^- :

tut little room for doubt thati'; property taorlia a jnoro careful exploration * which in all probability

wry rich reiralta in heraatito and oidorite 6roo , oror andat liand *

Sto *Vxrio "ilidhigan rotruary 4th 2931 *!

Youro truly!

( Dinned )

ALOIS"

'V. \ ".

•'••'^t - V REPORT ON THfr JOSEPHINE IRON HJNR.'•;, " - - -' --' - -. -^ p.- -. :- - -j, " .

LOCATION. ' *.;.,i ,

The Jospehine Iron ine is located on a.abort spur of Vhe Algona Central and Hudson rJay Railway, about 170 Hiles north from Sault Ste.Kario, and about 20 miles north-east from tho ore docks and harbor at Michipicoten on Lake Superior, in the District of Algona, in the Province of Ontario, in the Domin ion of Canada, and consists of three claims, 'containing 1#3 acres, ex; t end in F. along the ranp,e for over one mile.

The owners are Lady Hearst, Toronto, His Honor Judge John McKay. Port Arthur, Ontario; and Alois Qoot2, Sault Ste. ,'iarie, Michigan, U.S.A. Patents were obtained from the Crown for the said lands in 1907, and are registered in the Office of Land Titlo^ at Sault Ste. Karie, Ontario.

GENERAL INFORMATION

Nearly all the diamond drilling has been done on Y-^51, which c mtainj? 75 acres. The great v r nart is covered by the waters of Red Lake (Parks Lake) which contains 100 acres. It empties by a small e*"eek, having a fall of about 100 feet, into Goetz Lake, abou* 13-X) feet to the west. The depth of the Lake varies greatly, but would average probably about 30 foot. The northern side is the deepest, and two areas attain a cleptn of 66 feet. One area is close to the

O f* eastern shore; the o^her is near the western boundary line 2: --j bf Y-451. Widr aretfs have not been counoed and a closer

^5 survey might reveal a continuous deep channel through the iTj L:; lake. There is little doubt that the boulder ore, discovered ci! w on the shore of the lake, was scooped out of the la K-e by a y ^ . glacial action.\JJ *t

^ Q Before minirig operations areundertakcn, it would V? seen advisable to drain the Lake. It would be safer to Zt mine th* ore; also the lake bottom could be inspected for

soft and hard ores. It would not take a very large body of ore of the boulder class, or of soft ore to pay for

en draining the lake.tog -j Jasper Island in Red Lake, is about 600 foet long, ra 2Ly over 200 feet wide, and is composed of banded material; [J j surface samples run about 30# iron; and as there ie a large^aaount of this banded material in the island and elsewhere

^ as shown by the boreholes, this class of ore way become of uj a considerable value by concentration. ..j-.- -. o r r ^O < NQT TO BE REMOVED FROM—.LO

UU . THE OFFICE OF THE RESIDENT

GEOLOGIST, ONT. DEPT. OF* MINES

SAULT STE. MARIE.

The southern shore of the lake is level for about 100 feet inland, vnere almost vertical bluffs and steep hills rise to a height of 80 feet, or more, consisting of ferrugin ous limestone, snail patches of iron rocks, and greenstone. The bluffy hill of sideHtic limestone fronting on this level roadway, is of l&n-e size, and the shattered, eroded part thereof apparently extends into the lake basin. Owing to its favourable location and quarrying facilities of oany tons, this rock nay have s owe value. Surface samples run: Fe,12.50^;Si02 5.00^; Lirae, 21.10*; KgO, .6kty, S , 0.035*. The north shore consists nainly of slaty schists, but close to this shore are a string of staal l rocky Islands of greenstone. These, together with the buckling movement of the southern rocks, evidently contributed to the shattering of the iron rocks, thereby siding tfrler destruction by weathering and so forming the Lake basin; and also enriTshing the iron rocks below.

W. I!. Collins, Government Geologist, as shown on his Geological .Map of that region, 196, has traced out the two north-west-running diabase dykes which cross tnu iron range on the Ruth property, a mile to the southward. The eastern one of these dykes striken through the west shore of Goetz Lake, where it intersects another Dyke running north-easterly clooe to the shor*: of lied Lake, which makos it clear from whence the crushing force cane, which in all probability shattered the pinced-in iron rocks to great ;iepth. Consequently, it nay be reasonable to assume that ore beds are to be found as far down as the iron formation goes.

The dip of t.'ie strain on the mi rf ti c e is generally steep to the northward, but in depth as shown on the deep oore holes of No. 51, it s ings about 80 degrees southward, indicating that the oro taakes u&ck into the property, inst*4id of leaving it.

The other drill holes out the range — at a much hifcht.-r li-vel, so tnat the corsh-sections thereof would not indicate the everburning of the strata deeper down.

adjoins fr-451 on the east; it contains 57 acres, and embracey a small part of Red Lake. Six drill holes were sunk on shore, on this claim. The strike of the im range heads for the wide drift-covered valley, extending eastward from the Lak' , and not ouch of ferruginous rocks are seen for sonedistutico inaland; but hole No. 3 shows that they lie buried under the drift, from which they rise into a high hill, ana at the- line uetween Y-4^2 and Y^53* they are 600 feet wide, containing about that width through Y-453, with an alraost vertical dip. The valley spoken of extends northeasterly along the range on the north side, bounded by high ridges of slate and green schists, trending in the same

SSM-949-

direction. Boulders of .siderite are strewn along the south side of the iron range and,, near the east boundary of Y-453 is . a low outcropping of siderite, about 50 feet wide. Ko stripping has been done on these two claims (Y-452 and Y-453) to ascertain the extent of this class of oro. Near the north east corner of Y-453, which contains 51 acres, is * broken basin across the fcange. Toe shattering and erosion along the eastern part of the range has been less severe than to the westward; but the iron rocks aremuch wider, from which to draw ferruginous Material.

The drill plajno for Holes 50 to 54, drilled by Algoma Steel Corporation in 1913-1914, shows that all material below 405& iron was classed as banded by the drillers; and the drill plans for Holes from l to 21, drilled prior to 1903, classes all material below 50?* lro" as banded. The under signed has an opportun ty of examining the driller's original note book, and the cores from Holes 4,6,7, and 13; and much of the material marked as banded on the drill plans would now be rated as commercial ore; so that it would seen reasonable fair to inf ' r that some of the other holes contai n material marked as banded, which would now also bo rated ae a good grade of ore. The cores for Holes 50 to 5k were delivered to Mr. Alois Goeta; check assays were made of the cores; and several errors corrected. The banded material was also assayed, and the results marked on the assembled plan, marked August 6th, 1921, M. A. G. and this is the supplementary analysis recorded thereon,. A plan of which should accompany the report.

Figuring the area between holes 53 and IB from the 300 foot level to the 900- foot level, it will give about 1,000,000 tons ol high gradr ore, and about the same number of tons of a 4C?o ore; and a large tonnage mor or less mixed with silica and quite a large tonnage of ore which runs high in sulphur tbut low in phosphorus. The two last-mentioned ores would require benefication before being salable for

purposes,

.. V•f:

In mining thb ore, a much larger tonnage might bc developed in the area under consideration, and in addtion thereto, probably oome ore above the 300-foot level, and a very large tonnage bejLow the 900- foot level, as well aa a great tonnage in the adjacent promising areas to the east and west. In the early history of the mine, the Clergue people intended to aihk the shafts they had started about 400 feet deep and mine there, without draining the lake.

At the expiration in 1941, of the option given to the Algoma Steel Company, a l oar. t wan taken in June 191A . A few. weeks later, war came, and the least was relinquished. The Company had made preparation to drain the lake, sink a shaft at the eastern bf the lake to a depth of 1,200 feet, mine and follow the ore in every direction until such time that futther drilling seemed advisable, b. aring in aind

s

that this ore la, figured only .to the- ^QO-JToot level, this deeper'.shaft' In4icates j that ;thsj Company exacted to reap a : J;- ^'':1 .richer -harvest than 1,250,000 -tons, which; according -to theirv ^, own-estimate, is the tonna-g* of high-grade ore proven upland the expense involved in the 4 eepei^'shaft have1.to be figuredr f i on a basis of t,hia',additional probable tonnage. - Judging' ^ - ' from Hole No.51* and from the great crudlng of the iron rocks, it seems, fairly reason^bê to expect^ that the ore goes very ' much deeper than shown in Hole Np*61". .The timber consist a,, of spruce,"balsam, white birch,., and a little pedar. '-"- ;

'i ' ,, - f ' * . . - . -v ' .. - -.

COUNTS ON YriE DRILL HOLES n

Holes No.2 and Ho.3 on Jasper, Island, Holes 2-5 and 10, areall shallow; and Hole 21,'the. lovar part of whiho . is not in ^f-451, need ô further mention herein. Holes 13-19 ' are about 60 ff; et west of Y-451J penetrate ore close to this property, and show that ore beds 45 and 20 feet wide at vertr ical depthr- of 565 and 7^3 feet, respect ively, exist in the - western end of the Lake, as well as an iron formation of uver 200 feet in width.

!

Hole 14 reaches a vertical depth of about 20 feet to bottom of banded. This is put probably deep enough to strike the ore shown in No.l2| Hole l, on Jasper Island, starts on the southern side of tê iron formation and la driven away therefrom, onterin .*. t h(J} schists at a vertical depth of about 105 feet, to bottom of banded, cutting a width of about 170 feet iron formation, irtcludin/ three beds of ore. This of course does not cut th6 whole width of the iron rocks here. Hole No.4 sunk vertically, all in banded, except 42 feet surcaoe, including Lak^-water (the drillers note back recorded many vertical feet cis ore).

Hole 11 re&ches a vertical depth to bottom of banded of about 265 foot showing a width of about 120 feet of iron rocks. Hole No.50 sunk below Hole No.11 at a vertical depth of about 650 feet, shows a width of about 105 feet iron form ation, including therein large beds of mixed ore and tvo beds of solid ore. The iron rocks cut in these two holes are much less than shown in other parts of the range. This may indicate a sudden contraction of the iron rocks. Still, there is roon f6r a JLii-tle doubt upon that question, as just below the lower of the two ore bodies comes a bed of," about 9 feet width of quartz porphyry, which might represent an infolded part which the two holes have followed*

"Hole 53 reaches a vertical depth of about 3#5 feet -^ to bottom of, iron rocks, having a width of about 230 feet f including therein 3 be48 ^f schists and the following are ore beds. t ' At footago 440 id a 22-foot bed of mixed ore, eraging 30J* iron; at flotage 511, is a 11-foov bed of mixed ,

* ! n ,.

ore, carrying; 39-90^ ijron, resting on ferruginous schists. At footage 534 is a 12*foot bed of material running 33.1O5* ifcon, below which-comes a 13-foot bed of ferruginous schlnt, beneath which lies a 20-foot bed of riixed ore with 33.60# iron, followed by a 15t-foot bed of mixed ore running 50. in iron,;resting on schist.,.

Hole 17, lying below Hole 53, reaches a vertical depth of about 144 feet, to bottom of iron resting on echlat. The iron formation has a width of nearly 100 feet, Including 4- befl* of ore aggregating a width of nearly 50 feet;

J5EMO- Some of the nL&erial narked on the drill plan as banded, but shoving such a high iron content that it waa colored as ore in the assembled plan of August 5th, 1921.'i '

l ' V

H61e 52. reaches a vertical depth of about 800 fett to top and 995 feet to botton of iron rocks, showing a width of about BO feet of iron formation, including therein theree beda of schist, ueds of mixed ore, and a larger bed of solid ore, the lower throe feet of which are high in sulphur resting on schist which has been cut to width of less than 10 feet.

Hole 51 reaches a vertjic&l ctepth of 1144 feet to top and 1615 feet to btttom of iron formation cutting about the same width of ore and material as shown in Hole 52 iind^r which lies. It also stops in ler,p than a 10-foot width of schirt. Sone of the holes show ochlot in different horizons while others show no Rchint inside thn iron formation. Had the drill stopped in less than 10 feet of schist in Hole 53, no one would have fcnpwn of the 35-foot bed of ore lying thereunder. Hole 50, also shows a bed of oro under a 9 foot bed of schist. As only a small proportion of the usual iron rocks have been cut in Holes 51 and 52 some iron rocks or ore night exist beyond the schist.

Hole 13 reaches a vertical depth o, 345 feet, to top and 537 feet to bottom of hole stopped in banded, showing a width of over 300 fe^t of iron formation, including therein a 40-foot wide bed of 0re. Hole 16, drill*d Just below Hole 13, reaches a vertical depth of 474 feot to top and #25 feot to bottom of iron rocks, which have a width of about 300 feet, showing 4 narrow beds of ore, and a large bed of ore resting on schist,

f \ - *

Hole 54 reaches a vertical depth of 243 feet.to bottom of iron rocks, which have a width of about230 f-ot* including therein large beds of mixed ore, and two beds of solid ore, which are schist turned into ore. The Drill cores are broken into snail pieces, interningleo with fine

6.

ferruginous material, and especially so in places where little ore was obtained* Therefore the results of the assays of the cores is probably a little low in iron. The shattered condi tion of the iron rocks Suggests the probable enrichment of the or3s in depth. The schists show no shattering.

Hole 6 reaches a vertical depth of 243 feet to top and 334 feet to bottom of banded, penetrating only 90 feet of iron formation; the drill stepping therein at a point where hole 54 indicates schist. Apparently the drill has not gone far enough to reach the ores outlines in Hole 54 t *t * ny rate the entire iron formation has not been cut, thereby leaving a doubt as to what night ue there.

Hole 7 attains a vertical depth of 240 feet to top of banded and 347 feet to bottom of ore cutting about 68 feet of iron rocks, including therein 2 beds of ore, in the lowor one of which the drill is stopped. The iron formation appears to swing a little in the direction the drill holes takes; therefore, more of the iron rocks would have to be cut, th; n in Hole 15, to reach the same point where ore is entered; so that there jls little doubt that there is as much ore here as in Holfe 15. It seems that Holes :4, 6 ard 7 should strike the same strata at depths 2 1*8, 243, and ?^0 respectively., which however (seems) not to oe the case.

Hole 15 reached a vertical depth of 466 feet to top and 601 feet to bottom jjf iron ore wherein the drill stops, cutting; a width of about 94 feet of ore with a 9-foot bed of schist in the upper part thereof. Much of the ore is shown on tho drill plan as banded: the analysis is given and while this material is markedbanded, on the assembled plan it is classed thereon as ore. Other holes in thio part of the range about the same dejsth show an iron formation from 230 to 300 feet wide; so it seeus reasonable to think that much ore lies beyond the botton of this holes.

Hole 18 reaches the vertical depth of 483 feet to top of banded and 690 f Bet to bottom of the whole, cutting a- bout 92 f'ot of what I ftssune to be iron rocks, including therein a width of about 4 feet of ore, followed by a width of 58 feet shown blank on drill plan; then comes a width of 18 feet of banded in which the drill, stops. This is not conclusive evidence that no ore exists beyond the bottom of the hole. If one were to apply the method of deduction it would seem that the cor^ marked in blank is ore. Hole 9 is sunk north of the iron formation, and Hole No.10 is sun k vertically in schist alongside of Hole 9.

Hole 6 reaches a vertical depth *f 243 feet to top of banded, and 542 feet tobottora of banded, wherein the drill stops, cuttinc about 250 feet of iron rocks; BO it is not

certain whether*'any ore might exist beyond .the whole, roasting Ort schist, though I think one wight be here at a much lower .depth.'- ,.. r .•'."•'.". :\ " '*;'""-- v's," V-' ;' " L '

The drilling done on Y-451 west of HoliB 11, does not cut the iron formation in such a wanner ae to indicate that it is un-proniaiHg or holds' no ore,. Holes dr i vert- southward to cut the iron roc k o at deeper levels "^would , - probably show better result d., Tie area eastward from Hole 11 i and eastward from Hole 10 also warrants taoro careful exploration, but this [would not be necessary at present , - if the plan of 'he Algotaa Steel Corporation were followed - that is, sink a shaft on the eastern end of the L*ke, mine, and follow the ore beds until such time that more drilling wore advisable, which would then be done to better advantage with the data obtained from the underground work.

ALOIS QOKTii.

Sault Ste.Mario. Kich* April 11

SAI^ co^

ALLOUIKO FOR LOU TAXATION, EXISTING G01rJ2?.N}*ENT DOUITTIJ3S?LC7 PRICED ELECTRIC POV/EJl,' A!ID SHOr.? CAXL HAUL C? 21 KILIiS TOLAKE SUPERIOR, EXCELLENT !;p:ATIT2 I^CK (T.E CAI! B^ SSCtttDD?OR THE ALGOMA STELL PLAIiT; AT SAUL2 SSS.MASIE, 03TAIUO, 2'fcOMTHE JOSEPHINE IRON MINE (O^TAHIC) I-'CP-H Ci:2A?LY THAN FilGM AMSHZCASIRON MINKS, AFTER PAYIKC ApOUT 50;" KIGIJS.l FI.CIGHT RATIIS TO THSALGOMA CENTRAL RAILWAY COMPANY, THAN SIIOSE PAID CM AMEP.ICANIRON ORE.

1. The Josephine Iron Miiio ie located on a epur about one-third of a uilo lon~, pstcndin2 froiu I-Iile 20 oa the Central and Hudson Bay Railway, ar:d i s about 21 nilcc fr Railway's dock at Michipicoten IJc.ro o i: r; c.': tho Lahc Sup It i o about 120 îlco by boat fro:a l:ichi':ic;oi;o;; harbour Sault Stc.Mariot anO about 200 nilc- l- l :-;.t t^ Port Art The distance v:; i'-.-.ult Stc.Jlaric fro;: ti.^ uii:^ by t!:^ ; routo i.a abou^ 170 nilee. i The i ..^~. : 'lc.;t at cai.!--: . could snclt abo;st 1,000.00^) tc:-.3 of ir..-.; oro ;~ :.., ly,

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. ..^ \ .-.C C,.'.'~-j o OVvJ l'...'.wli C .'..^^ .'^'0 O- --'~ JJ. t;OU^.C iriU— CC.'Jo "J.-•J •; s.^:*i:Vv0. ii;I',.-.::^ of the dit.r.o::u Crillii-:^ ci5c-*ttwior.y vas c^ o.....;io:-. v.'.r/^ the ore .body k.vorc^cl ;;bo;iU CO ^cot i^ uiclvh, r-:.J. c::tc.:v-Ot! r. o,.i c t an c o oi' r.lou^ ",CCO feat. ;;r.A*rk . Willmott Cc..:sult:l::c I.'r.îr.uor Mining Coc.lo;ji^t for .'ciio L.^!:o cuporior Coôravjio:: c.Ttor the first 21 cirill/!:oloi; voro put clo-.;n, c..:ti;io.':ccl that euoh dianonci clrillir.r; had proven up a':out 500,000 tor.c of iron ore, 4vc'-^-C—r: about 50 per cor.t irca^ and ,C-'.- ôr ccr.t *;l:oc;xhoru3 ar.4 interacted the LrJrc ^'ipcrior^ '- --*- - ". ** r- "' "' *\ "^ *" v* ^" "^ " * *-t t* r* f*1 tA ^*S*"* *i r1 ''* j ^* ' ^* ** '^ r ' ' * ** /' V- ri/-, t\/ . *^ v- ^ r ** *i ^ f*'1 T C\ WV-H^ t'\^^ C- *. — O.. u.;4 \-k.*- —1.^ i-H vj* v-1. C*-i w*i w-..'.- w w*-.U !/- O^w i.wj u..I ^-w/^-VJ,' ' *. y -. f'^s'î** r-'1 "*'" l *' *'n"' r* ^ ' *"* *"*r* '^ ?'*r '"* "* t *" t *\^ " ~ li T*'* ' * ^'** ^^ f* v " f* " rt t* .^ l~ -. * W ...*v/ ^ V* ^ — —— J- . ^ sW ——^ *V *-* V*- -t IM* \o*,V*. ^'w*V V* W *J -. ^ Oiwwi^^——*.^ i***W V^W .^.

i"oot::^;c .up to lO^^CG feet, jr.r.d nroviiv; r:;; c. total ôiina^c of : 0 2JD,000 tons of hcrcatite |iron oro; c.r, if all ore bclov o.v'J ;;oro excluded, a tonnaô o^ 1,300,0.0 to^.3 of ire.. oro 9 :.^^;.yir.j fro::: 50^ to 63/5 ii|cn, in the cl.^rt Jliata..wO of about lÔO'b feat of an iron rance vliich c:-:tcr.f.^ , ..wr a v'.iatance of

:-ij r..ilc or. tho caid proporjty. The cirilliaj aluc proves t-a-i the iron oro body extends dovayard to a dcptl. of at loist J.,350 foot* .

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' ' 11. It io octir.atcd th&t tho iroh ore reserved in tho Stateof Michigan vill only laat 13 yo&r;:. 7ho iron oro should bo mined fi-on the Jc;i;cpliinc at a subotr.r.ti.'il profit of 51.00 per ton, ovo*i without: any aciditiontil iioiuition, B-scidcs this., tho operation of tho Jor.cphir.c Iron Mir.o x.ould i-can that i-;a oro vould bc chi;-^2d over the Al^o.na Ccntr-al Hailvey, cad tho prico p:iicL for thivr.iut \:ould cdd to tho receipts of that; i'ailvay,

ia I'oaJlly a eubsiditi-y of tho LcJ:o Superior Corporation;Michirj^n o;s ro, which is in come caseo shipped to

Sault S'coJ.'ario ovor an all-rail route, contributes nothing to the rcvoiiuo of tho Algona Control I'ailvay.

thio 12th day of Aufeist, A.D.1D2D.

s SAf-9

l'': -\ - REPORT OS ( 'THE J03EPHIHE IROIf MIgE.

LOOATIOH

The Josephine Mine consists of three patented mining claims,. ! 9

BOB. Y451, Y452 and Y45J, located at a. point one half mile oast of mile* . :

6 oa the Uiohipiooten Branoh of the Algoma Central and Hudson Bay

Railway. The distance to Michipicoten Harbor is 20 miles and to tho

Sault by rail 171 miles. The property is situated in Township 28, Range

25 in the Sault Ste. Jiario HinJLng Division*

TOPOGRAPHY

The topography for the most part is rugged, consisting of

relatively high, steep sided hills with, low and generally swampy ground

between. Searly all of claim Y451 and part of claim Y452 la covered by

Parks Lake. There is a railway grade from the Michipicoten Branoh around

the" south shore of Parks Lake. The ground .is fairly level along a strip

about one hundred feet wide on the south side of the lake and then the

hills rise abruptly to a height of from 75 t o 100 feet. Parks Lake has a maximum depth of seventy feet and an average depth of at least forty

feet. The outlet is at the west end \7here a small stream flows into

Goetz Lake one half mile distant and at an elevation about one hundred

feet lower than parks Lake.

QKOLOGY

The general forcnatibn is made up of various phases of tho

Keewatin rocks. Part of a range of iron formation several wilos in

length striken through the claims from south went to north east. The

part of this range included in these claims has a width of from 75 to

500 feet and consists, in descending ordor, of banded silica, pyrite,

and siderite. In places the pyrite member lo very thin or missing and in

places principally under Parkfe Lake part of the siderite and pyrite

Josephine Wine'

n altered to a brown hematite. The Iron Formation dips steeply

to the north at from 60 to 85 degrees although one diamond drill holo

showed a steep dip to the south at a vertical depth of 1550 feet. Thei **

siderite and hematite members are looated on the south side of the iron .' '. * * * i

formation* . '' * ' ' ' ' ' '

The iron formation can be seen outcropping on the two easterly

claims and also south west of Parks lake. Where visible it consists almost

enti-ely of the banded silica member together with some pyrite and siderite.i

The banded silica oan also bo seen on Jasper Island in Parks Lake. Ho

hematite in plaoe was seen but a few small fragments were picked up east

of the lake*

aXPLORATIOH

Twenty-nine diamond drill holes have been bored on this property.

Practically all of the drilling has been done under Parks Lake. The first

three holes were put down by . A. Wiley of Port Arthur in 1899. Twenty-

one holes were put down by thb Clergue Interests between 1900 and 1906.

Five holes were put down by the Algoma Steel Corporation during 1913 and

1914* Two shafts were aunk between 1901 and 1903, one on the south side

of Parks Lake opposite Schist Island, to a depth of 150 feet and the other

at the east end of the lake, to a depth of fifty feet.

ORE BODIES

The record of the oarly drilling is not very complete and the

wori was not very informative, later drilling however disclosed a fairly

large body of hematite. The enclosed map shows the location of the drill

holes and other features mentioned in this report.

Uost of the holes explored un area between a vertical range of

200 and 900 feet and the deepest hole reached a vertical depth of 1550

feet. The drilling showed a band of iron formation consisting of banded

Mine*f' /-

ei Aa from 50 to 350 feet in 'thickness. On tho oouth side of the

silica member there -was a sheet of brown hematite* The hematite band

is not continuous and is partly trade tip of alternate bands of oilioa and

hematite* The thickness of the hematite, both massive and banded varies

from O to 135 foot. . L "All the early holes were of neoessity of an exploratory nature.

?airly systematic drilling was done in a promising area starting at a

point 200 feet oast of Jasper Island and extending in a north easterly

direction for about 1000 feet. Thirteen holes drilled in this section

disclosed a sheet of hematite of rather irregular, oval outline, 1000

feet long, -1350 feet in maximum depth and from 5 to 50 feet in thickness.

Banded hematite was found over a greater thickness than the above figures

and it la possible that part of this material could be mined, the rook

portion being eliminated by m^ana of a picking belt. Part of this ore .

contains a o&nsiderable ataouni of sulphur but there is ovor 800,000 tons

of recoverable ore of a good grade, averaging over 5^ iron in this one!

lease. It is quite possible that further drilling would extend the size

of the lense "both laterally ahd at depth. Hole Bo, 5* out ore at a

vertical depth of 1550 feet and no other holes wore drilled in this

vicinity at this horieon. It would Stiero quite possible that oro i?ould

bd found at oven greater depths. In my opinion the size of this lense

could be considerably extended by further drilling.

About 1400 feet south west of this lense holes 12 and 19 out

good ore from 20 to 40 foot in thickness at vertical depths of 500 and

700 feet respectively. Do other holes at thie horieon were drilled in

this vicinity that would short the extent of this lense but it is quite

possible that it might be of oonniderable size. Further exploration

right also disclose other lenses z'ot only laterally but also at greater

depths.

JOBOphlnt Mine /- ' 4*... v -* - - ! " ' '' , '

1 - ' ' ! *.

^ JL small amount of surface work done during the summer has

Bhown up a band of siderite northeast of Parks Lake* This in all *

probability is tho westward extension of the siderite found on tho . Bartlett property of the Algbma Steel Corporation, . This property lo

' . . .j Vi i - .

" itnaediateiy adjacent to the Josephine and both properties are located,*. - .* ' ^ .

on the same iron range. Drilling on the Bartlett property indicated ,,, f 't

a body of siderite 2000 feet long and 50 feet in thickness. The grade

of iron is good but the sulphur content is higher that either that of

the ttagple or Helen* The amount of work done 'on this portion of theiJosephine is very limited and aside from showing the presence of1

siderite, which was to be expected, no estimate could be made as to

possible sise. In places the siderite appeared to be of good grade buti ' in most instances contained considerable pyrite. This might be accounted

k i

for by the places exposed boring the top of the siderite band although

the pyrite might have been general at the points exposed throughout the

band. There is probably a t|iore or less continuous band of sideritej

extending from the Bartlett property to Parks Lake and there may be

places where the band reaches thicknesses equal to those on tho Bartlett.

I do not believe however that the merit of this property depends on the

Siderite possibilities. It is possible that siderite will be found undor

Parks Lake as portions of the original band from which in part the

hematite was formed. The early drilling makes no mention of siderite

but it is likely that some kas encountered* Siderite was not generally

recognized in those days and would not have been noted even though it

existed. In my opinion the chief r.erit of this property lies in the

possibility of proving a larger tonnage of hematite than has boon proven

to date.

(

0030LUSIOH9

There has been proven nearly 1,000,000 tons of good grade hematite ta one lense east of Jasper Joland. There are further amount*

of hematite whloh taight be recovered by some system of beneficiation

f ; whloh would have .to be worked out when the lower grade taaterial was

v. .better known. In my opinion this lonse oan be extended both laterally

and at depth by further systematic drilling beyond the limitB already

drilled. There appears to be a reasonable chance of proving another

lense in the vicinity of h^oles flos. 12 and 19 by systematically

drilling the area around the points of intersection of these two holes,l

There is also a possibility of locating further lenses of hematite

both laterally and at depth.

There has not been enough ore proven to date to warrant a

mining operation. In addition to the ordinary expenses in connection

with such an operation it appears probable that Parks Lake would havep 'to be drained and the proven ore is not sufficient to justify the cost

Involved. I believe howetor that the indications of tfurther ore are

sufficient to Justify an extensive drilling campaign. In event of

finding sufficient oro to make the mining of it a commercial operation

there are several factors which make the location of this property

very favorable.

It is only n foW hundred yards from a railway. It is only

twenty olios from Michipicoten Harbor on Lake Superior. This harbor

is only a little over one hundred miles by water from Sault Ste. Iforie

where the largest steel company in Canada is located. The property

is only 171 miles by rail from tho same plant in oaae winter shipments

were necessary. A large supply of cheap electric power is available

only a few miles distant; A good class of mine labor la available

from the various mining districts of northern Ontario.

Josephine Mine

I have already indicated that in oy opinion the onlyi- t

work justified at the present time la in oonneotion with tho. ' ' - ' ' . , '

exploration for nore hematite* I -do not mean that tho siderite

possibilities should be altogether ignored. If sufficient hematite

to Justify a mining operation were located it would be woll worth

while to investigate tho siderite* This might be mined in con

junction with some of the high sulphur hematite and sintered in the

same operation* If sufficient siderite was located to Justify a

sintering plant, this fact would immediately make available a con

siderable tonnage of hematite that owing to its high sulphur content

is not suitable in its raw state for the blast furnace. Another

fact in oonneotion with the siderite la that in addition to it

containing sufficient litfle to flux the silica content, it actually

contains an excess of lime* This makes it a very desirable ore to

mix with hematite as it materially reduces the amount of lime that

would otherwise have to be added to the hematite when charged to the blast furnace. Tho siderite also uaxtally contains about two and one

i

half percent manganese whioh in some instances is an added feature*

Aside from the siderite possibilities there is a zone

nearly 5000 foot In lengih, extending to a depth greater than any

of the drill holes have penetrated in v?hloh one largo lonse of

hematite has been located and another lense indicated. There would

appear to be a reasonable chance of locating other lenses within

this zone and also of extending the size of those already found

or indicated. If other lenses comparable in size and grade to the

one already proven were found, a successful mining operation would

bo the result.

'•- r.''•'.••y.V'*'-'.. - J -'-. ' -"

oy opinion, tafelng Into'oonaidoratlon the known faota'- . ' 'the geographical location, the JOBOphlne is the most

, * - C - ' :high grade hematite property that le knovm In Canada*. .

- .. Q our o ea of Information.Personal Examination.W* H. Collins, {Hiohipiooten Iron Ganges,

0.3.0.1926.)Drill Beoords, Algoma Steel Corporation. Early Drill Heaults furnished "by Alois Goets and- Judge John UaoKay.

**6 G

Mining Engineer

Sault Ste. llarie, Ont. August 22,

MEMORASDUM HEOA^i)ITI3 TiTS POSSIBLE TOJJHAOB W HEMATITE IBOH OB3 IS THK JOSEPHS IHOfl MINB, IN THK MICHIPIOOTJ5H DISTRICT, 15 THS 3?ROYII?OJ5 OP OflgARIO, IK THS DOMIHICM. 07' OAKAPA,

l* In 1937,' the'Ontorio Legislature enacted Legislation, uhloh v' ' - '* ~ - ' * , .

authorises the paynebt bf a bounty of two cents per unit on all ,/: siderite and'ather low-grade iron ores when mined and bonefioiatod

, within, the Province of Ontario and i* rkoted in Canada or tho TJnit-1 ' - t -~ ed States; and also a similar bounty on hematite and other iron ose,

mined and smelted in Ontario. These bounties shall apply for ai

period of ten years, commencing on the tfirst day of January,A.D.

2* The Blast Farnaoeo at Suult Ste.llarie, Ontario, have a totals* oapaoity of 1,600 tona of pig i&xm per day; and those at Hamilton,

Ontario, of 82^ tons per day. Theso fumaoes, When operating at

toaximum capooity, viould require about 1,800,000 tons of iron ore,

annually. . '

3* The Josephine Iron Mine Is located within a few hundred yards

of the Algoma Oentral A Hudson Bay Railway line. The rail haulj

from thio Mine to Hiohipiooten Harbor, on I&ke Superior, is about

J& 20 miles* The dictanoe by boat from liiohipiooten Harbor to thet *

Sault ste.l!urie Bl&st Furnaoos is about 120 ail e B*

4. In 1914, the Lake Superior Corporation Limited, after first

diamond drilling the property, paid the Owners ^2,000, and took a

Lease on the Josephine Iron Hine for tuenty-five (25) yoaro, sub

ject to tho payment of a royalty of twenty-five (25) cents per ton

on the hematite ore ninod, with an Option to purchase the property

outright for J400, 000 or ^00,000. Ovilng to the outbreak of the

Great War, they cancelled the Lease in 1915* In 1914, there was

no bounty at all; and the Jirioe of iron ore was only 53*75 per ton

instead of ^5*25 per ton as in 1937* In 1936, thero r.oro more thanK

4,400,000 tons of hematite ore, averaging apparent l? about 52 per

cent, iron, shipped from the shuft Mines on the Unrquette Kaiige

*.n theSta-s of "'chipan. 3r-:-;d en the fixed 1736 price o .f about

H. 8063 et Lulre Krio ?or|tn, f: oro \rcn a profit of ?1.OO por ton,

I". i •/.ir..'; snu uvcrhsud c^; :: por tc.: ;. l.i-oi)7 'A r.:: 6 c' ' i l'. r"' 7^0 i "' -*:

• •.. .if?!- - - - -cent* iron voro nlnod from the Josephine Iron Hino, about 850,000

1 tonp of honatlt* ore, averaging from 55 to 5? per oent. Iron, ooaid be mined and sold* This ore ahonld oell for abont f 5.25 per ton, pitts 30 cents for extra high-* grade, or about f5.55 per't on. Thia might indicate a possible net profit of about fl.?3 per ton, *hon ooid to'American fttrriaoea, lesa 25 oent a per ton for increased mining ooata..' If the Ontario Bounty of Jl.10 per ton were oredated to the' Mining Company, Inhere might be a possible maximum profit of fc2*93 per ton, loas ^5 cents for increased mining costa in 1?37

5. Tho Josephine Iro^n Mine comprises about 183 gores, and con sists of en iron range rib out 5,000 feet in longth. The westerly 2,200 feot of this 5 r on range la largely covered by Bod or Parka

Lake. Diamond drilling qn the easterly 1,000 feet of thia westerly

2,200 foet has proven uj about 2,2^0,000 tons of hematite ore, of vjhioh 1,300,000 tons carry 50 pur oent. iron and over, IJr.George

, Mining Engineer, of Ssolt Ste.Marie. Ontario, states inhis written report aa follogs; '"Aside from sidorite pbBBJbilitieB,

thore la a zone nearly 5,000 feet in length, extending to a depth

greetor than any of the l drill holes have penetrated, in vihioh one l,.————————————— ——————————————————————— s —————————————————————

lor go lenao of hem&tito hao boen Iboated, and anothor lense indl*

ea ted* Thoro \\ould to bo a rpunonable ohanoo of looating

other lensop ' viithin this gone and oleo cf oxtenaing the pize of Jt——————————————————————————————————————————————those air on Ay ; found or jLndicatod. If qthur lonaeB ooiaprqable in sJt-

oize and grado to the ofro already proven ve re found, a suooeaafgl

mining cporation would bo tho rostxlt. In my opinion, taking into

consideration tho toioun facts, together with the geographical

loctition, the JoBephipe; is the mobt attr&otlYe high-gr&de hematite

property that ia kncvin in Canada *J*j

6. In 19P6, the Depcrtinent of J'inea at Ottawa published an ex-j

l^c^ort on the t'.ichipiuo-,on Iron .-.cr.~es, r.r-.uo by tho lute

?.lcvi: -." r -.c -en Tier.:- :.ro

.- c-uiu iron runno: "' "i s

r.: ."/,f-; ; 1C", c^ thu ct-ic rxj-.'O^,

o." rV vi-- t: .'l" ^,rOO ^-.v.-t of

v.l c'r.out of orov.n oro ap;of,ra

r i . i

(J) '. , . . " ' - '-i-l ( f

"and appbrontly' tho larger one, bogins about 200 feut oust of

Joppt'r lnlundVond extendo north-oastwurd for at lount'l,000 fo&t, ,.

bo ing'crossed farthereot in thio dirootion by Jbrill Holo No* 18*' It - * ia intersected by thirteen holes;1 nhioh ehov iron oro at doptho -' '

ranging from 200 to 900 feet, and in thd eoat of Holo 51, 1,550 fo*t

bolow thy surface of Par^o 8X& Lake. Tho drill holes dofino a

vortical sheet of ore of k±g kito-shaped outline, 1,000 feet In * '

maximun length and 5 to 125 feet thick. M . *

"It seems likely, however, that the loisor linita could be ex- :-;l - .- . . ". ;' V. ' ..

tended considerably if deep hoios like Ho,51 *eru drilled on either,

side of it...If all ore currying 301 metallic iron bo taken intooonsideration, tho oval sheet defined by the thirteen drill-holes

lo estimated to contain 2,2^0,000 tons. If ore carrying loos than

50 per oent. iron IB excluded, the tonn&ge woald be reduced to 1,200,000 tons.**In all probability it is o aeoondory ore deposit

derived from a print*ryaiaerito and pyrite ore in the Butna raanner

fap the Helen deposit. ..'.'gor 1,200 feet southwest of thio sheet or

ler,ae of ore, no bro\;n ors, sas enuountorod by the drill; but Just beyond that distance Holos Uoo.l? and 12 out across a oooond sheet

of fairly high-grade oro 20 to 40 foot thick at depths of 700 and

800 feet, respectively.. .Parks Lake, under tsjjihh the ore deposits

lie, io about 70 foet in greatest depth. There is a doaotint of

nearly 100 feet to Goeta lake. H

7* THE HELEN UII72.- The following quotations are taken from Page

115 of Hr.Oollinst Report: "This deposit had yielded more iron ore

than any othor deposit in Canada, its total output from 1900 to

1910 being 2,825,36? tons of brovm Uron oro of good quality andi

^1,000 tono of pyrito..*.""Thu ore body .is no* known to have been

a pocket of oxidation products in tho siderite a-.id pyrito nctibors

no.-jr tno '..oat end oi uhw Holon IrO:i::i'C.:5jD alriJdy u&scribcil in

lit 'tt, "••"•'-,n j 1 ; p,;- ot'.r r r c- ci o;-i f; -., v.ho

-.-'.no run

i i \t- -i.' , lj. L ' ' ' '

• . . Pago H8s ltH Th* brown iron ore forma a pocket In the eiderJ.to andpjo-it* member of the Helen range 700 foot depp, 700 fost in di o me t tt along tho o oa re e of the nmgo, and the full width (200 feet) of the

ft t ' ' ' ' i' * p ( ' * , k . t ' - ! - t

siderite and pyrite, being bounded on the North by tho banded Bill-

ioa of tho iron rangr and on the eoutU by tho voloonio sohieto that

form the base of tho ir6n formation, ill the contents of thie poo-. ! ' .

kot — brown iron ore, pyrite and quartz sand,— are contained In

the Bidarite-pyrite member of the iron, formation or oan be detiyed

from it by oxidation. Geologists and mine officials ogroe that at

the eastern and western margins of the ore-body there was a grad

ation from brown iron ojre into unaltered siderite* {Endeed, BUG h K

approximate data aa are available soera to indicate thut the Bid* erite and pyrite which briginally must have oooupied the popket,

if converted into iron oxide and pyrite, would yield Just a little

more of t base products than actually appeared to have existed* ** Page 119: "The fact of the deposits formed only at a place on the

iron TB-L-za w here sulphate waters could collect in a natural depres sion seems to point to those waters aa the ohemioal agents whioh gradually digested its way downward intoa the siderite members of

the iron formation."8* While Boyer Lake, in which tho Helen Iron Hine wus largely

located, was about 1,090 feet long, and about 400 foot wide, Parks

(or Rod) Lake, in which the Josephine Iron Hine is located, io

about 4,000 feet long and about 800 feet wide. j^Soe Pugo 11J? of

Collins' Report.) While! the hematite iron ore only went down to

the depth of about 700 feet in the Helen Iron Mine, the hematite

iron ore has been alro&dy proven by diamond drilling to go dov;n to

a dopth of at lcaot 1,^30 feet in tho JQBOphino Iron Hino. Tho

extent of Pur':3 L&ko, and the much groator Isngth and dopth of

•;h*3 hc.-'-r'.tc c:?o ir. th'i Jo-cnMro Iron : f:'--:o nipht in-Uci-.to thit

, to he-'T^.t^ tr'r.oro rirht bo at loutt eovorul tir.eL greater r,c.',

. ., MEMORANDUM REGARDING THE POSSIBLE TONIJAOB OP SIDERITE ORB IK THB

IROH MIHB, ID THfi MICHIPICOTKfl DISTRICT , II? THE PROV- Qg ONTARIO. , UT THK DOMINION O? CANADA, ___________

, l* In hie Report, Mr.DuVi* estimates that olntered oro,* * :

carrying 64 per oent. iron and 10 por oont. sillioa, tfould cost

about 1^50 P or ton, if rn&do from magnetite oro carrying about 33

per oent. iron, and ground to 200 mesh, as follows:

Taxes . 50,25 Royalty 0.25 Mining 3 tons 0.90 Transportation of 3 tons 0.15 Crashing and fine grinding 3 tons 1.05 Concentrating 3 tons 00.25 Devjaterlng - l ton 0. 05 Interest, Overhead oijid other fixed charges 00.60 CBatxof Agglomerating ut the Mine __________ 1*00 "Total Coat Per Ton f ' —————————————— 5*^P

It is confidently Bubmitt^d that the Siderite ore in the Josephine

Iron Mine can be quarried and crushed to a suitaole Bize foy sinterj

ing at e coat of 46 cents per ton* It requires three tons of

siderite ore to produce tvto tons oj sintered product. Accord

ingly, the cost per ton oi sintered product, xor

quarrying and crushing, wbulu be ^0.6QA !

Mr. K. W.Davis, Superintendent oi Minos Expiremental

Station, University ox Minnesota, presented o Reportj

at the Annual Metal Mining convent ion, Wes tem i*ivia-

ion of tho American Mining Congress, Sop. 23-27*1935*

in i;hich he estimated tho coot of sintering or agglom

erating oi fine iron concentrate at the mino per ton 1,00

IK the dibtant future thit* may be reduced to j?0 uents.

He allous ior interest,ove'rheod ft fixed charges per ton .60

Koyalty Per ton - 1 5

Taxes per ton * 2^

Total Cocit ut the Mine ;?2.69

Tronaportatlon to Laku Krie Ports per ton _____ 1.50

^orol 00,a y 0 r ton ^ ! .^fo Kriu rrrt* :;4.19. iron or,, io no^ ac;u {or ^ .i** - br vono the proxix- por ton

ouotuu l,W,j*0 ton. o^ oiuoiitc Oro. ^rin: iht- y B ric s

no Govern:----^! ooi-,r.ty -t -He•, . -- -- --- 1 - r" ^ -.i^ oi ttui Joouvhinw Iron

•/•V

( l (O

(or Bed) Lake easterly to tbo eastern boundary of this property*

about 150 or 200 feet of thie ore-body la above the l&ko-lovol lor a distance of about 2,800 feot, and oan be quarried very ohoaply*

If ParJtB lake is drained, another 60 foot oould probably be added

to that section. Siderite oxe hau also been located on the western

shore of Parka Lake, a short distance nest of the western boundary

of Claim Y-451, or about 2,200 feet *ost of the siderite deposit on

Y-452* It is said that the Drill Keoorda shos siderite in the drill cores from Holes Numbers 6, 8, and 9, where the drill plan indicates

banded* This vsonld probably indicate that there is, poosibly, an

oro bodt of siderite, extending vieaterly from Y-452 underneath Parks

take, for a distance of about 2,200 feet*J. Diamond drilling has proven that the siderite deposit on the

Bartlett, lying immediately to the Kast pf the Josephine, and on the

same range, has q viidth of over 50 feet, and goes uovin to a d^pth of

at least 900 feet; and indicated b tonnuge of almost 6,000,000 tons

of siderite ore. The diamond drilling on the Uev* Helen, and other

.•ork, bhowo that the siaerite deposit goes dOnn to a uopth of ap-*

parently over 2,000 foet; -nd inuicai;es a siderite dopoait contain

ing frcm 70,000,000 to 100,000,000 tons, apparently above 1,700 foot

in depth. The Hematite on the Joouphine Iron Mine good dovin at least

1,350 feet. It Viould sybm poaaible that diamond drilling on the Jo B-

ephine might prove up ~ oiuerito ore deposit, avorwging about fifty

feet in width, for a dibtanco OJL ubout 5,000 feet, v.ith ^ depth of

over 1,500 feet. In September, 1930, Mr. John E,Groenv,ult nroto that

"Tho coot oi sintering depends bomywhat upon local conditiono, ^50 oonts to 75

is all th\i v,ay iron îx&rx?^ ~s cents, depending op the cost oi

fuel, c i/o.; also the oiê of iho pl^nt* 114. So,r,plwo OA tne oiaerite oro v.ere taken by J.tr.^loia Gooti, unu

ônt uo i: o Bouhlono::, ritool U'or.;^ny; r.Jiu the fsr:.^ ,.wre owcu;:ui li;

; :.:ir /^-'.^-cory j. r r l^.C.^.?"^:^ vr-. aOllo..inF T olo rivoo t h;

s^',; fa:t.

As,Loss "by

CaO. MgO Ignition*2. 3*

, 5*12*13* 14.

56,96 2,12 39*2? 2,31 37*0] 1.84 29.26 1,68

,OU .01?*016*024

3.913.182.481.28

54 1.57 1,84 5.41 20.28"~ " " 2.48 4.1? 27*10

7*01 5.08 27.* 0'03 7.70 i.n.01 13.93 0.67.T. 13.89 2.64ta-. — f - — - -— ''"'^ v — ^ "™X^ ^ ** r ft** ** ^

32*56 2.44 ,019 0.96 T. 9,89 5,1744,11 2,41 .016 8.8J *57 2*57 8*84

7.01 4*67 29*82*61 5,36 30*161.10 2.56 22*75

AverageAnalysis 36.54 2.13 .017 3,44 .11 9*8? a.31 2.72 27.73

AVERAGE ANALYSIS AFTER IGNITION.

50.56 2.94 .023 .15 T, 12,83 3*20 3.77 6,73

Y-453*Sample No. 2 was taken 570 feet viest oi the east boundary ofeast

Sample No, 3 v.as taken 700 ieet west oi the sai boundary of Y-453o

Sample No. 5 was taken 500 feet west of Sample No. 3,

Sample No. 12 isao taken 300 feet east of the Lake shore,p

Sample No. 13 v.as taken irom ore near the lake shore.

Sample No. 14 v;as taken irom liear the ea at "boundary oi Y-453.

All samples were taken irom natural outcrops; not irom trenches;

and were taken during t'he sunnier oi 1930, and assayed on November

12th, 1930, Apparently, it is customary to add one percentage oi

Mnnganese tp the trpn content, vhioh viould "bring the iron and

Manganebe content up to 53* 50 Per cont.

5. Owing to the pooaibly large tonnage oixaiderite, the Josephine

Iron Uine, should be oi considerable value. The Bartlett Iron Pro

perty ia on the uaice iron range, and lies to the east oi the Joseph

ine Iron Mine. Particulars oi the resMlts obtained on the Bartlett

Vi ill indicate the claaa oi ore that Kill likely be encountered oni

ths Joatjphine tidalite ore body. The following ^uotutionb ore token

ixom tne tjaia report nitiue by n. H. Colline, on Pgge 915

RSNGS.- At i he eoot end oi long Lake Range, the iron

is faulted nbrthvit,ot*uru 5,000 feet, a-nd j.rom tfcore

in - gentle curvo AOr -j o.^ L!;3 milus vo vbo

...•.--I" rj:.1. ci !i,r.it. ;.-r-u i~ i:v..n ~ * t he JnsepLlnj pro-pert;:,

.ill ut, Ciot.oriocJ. ^J-TC^ -^ or y o j tn c t,e.oorjuury iron oro uc-

v^* xr.e rtjr.oir.uar; ^^ - "inir.r 01 1: i:.: Y- ^3, I:n7*,n

Portl- -T. ?ur.f^* * -The lurtlott u loirly uontinuouo

(4)

Oouupieu the second raining claim ee,st of Y-452* The iron formation

stands on edge with its top facing north* The dip varies from o fe*

degrees lees than vertical towards the to at h to a similar amount

northward. In the two easterly claims t he iron formation IB only 80

to 150 feet thick; but the remainder IB from 250 feet to 550 feet

thick* A siderite member appears to be fairly continuous along

the o oath of the range, and in the upper port of the eider! to, next to the banded eillioa there is u concentration of pyrite, ^uite

distinct, but not rich enough to form pyrite ore. The siderite

appears to marge southward into KeeviDtin schists*

"In 1912 the Algoma Steel Corporation stripped and diamond drilled

o part of theBartlett Bango in the fourth and fifth olaima from

the east end, revealing a bond o± siderite 2,000 feet long*"

At Page 92: "All three holes, after traversing the volcanic schists

in which they started, phased through a band oi high-grade siderite*,

42 to 6s4 64 feet true thickness, anu then through 24 to 200 feet

(true thickness) of lesser pyritio siderite beiore entering tho

banded sillioa member.

"Systematic analysis of each ten feet of drill-core by the owners

indicates the high^-grade sheet of siderite to contain as large o^

percentage of iron as the Helen '.flange siderite, but considerably

more sulphur. The lean pyrite part, similarly analyzed, shows

from 7.17 to Jb par cent, sulphur, or not suififcient to consti

tute a pyrite ora."

6. THE IMW HKLitf RANGE SERIES,- The fo3.lov.ing quototiona are

token irom PagexbA of the saiu Collino Report: "Between 1913 and

1917 the ourfoCb of the (Helen) range nob thoroughly explored by

trenches dug through the driit, o mi. the inon iornu*tion nus system

atically bored, the urill holo^ ranging in uepth irom i?00 feet to

'd 4 44 iubt (Figaro 10.) : 3ctu 0 on Cctoboi- 1917 ""u Ootooor 4,1911),

trie n^rth OJL

ho

' *'i if*'i T- i Y"* T ' ' ^ \ *~ l r' T "'-t i *- H " f l "TV "i.Jo .1 * A j.. JL j. J. .:' \.cj-c . .*. viu u,. U-O.IA

till! i'tJlVTo : 'itO t;-;u t-iUG/ite, olIQ

r ~ i hw' or i/- r "*u.v, t*t k-or-ui uO'J lutii t)wlo.. t no

•o (Figure 1C ,) 0

.-?."1 vr.i..-i i. ! r r,. li CM i-r.v; r. y mn iron ^.01. ..^ioii

r.. .••Mi

(5)W "Prom North to south thbre appear (l) a very thick banded sillioa

member oojjistitnting froin tfto-thirds to seven eighths ox the total thickness of the iron formation; (a) o Jointly marked pyrite mem

ber aot over sixty feet thick and consisting of siderite with more

then 50 per tent* of pyrite; (3) a siderite member of variable

thickness up to gAC fêt. The country rook on either side consists

of volcanic ouhiots. Th^se holes indicate thut the iron formation

dips toward the south ffom 70 to 80 degrees; in other words, it

is overturned from 10 t^ EO degrees."

Page 8?: "It has been estimated iron data obtained by diamondj

drilling and surface exploration that the ore body contains be*

tween 69,000,000 and 100,000,000 tono oi ore in o depth of 1,700

feet; 11,000,000 tone ojc which lie above the adit, and ita drifts."

7* While the siderite from tha Magpie Iron Mine averaged about

35 per cent, to 37 per bent, iron, and theroasted product 50.60 per

cent, iron and 2.74 per cent Manganese, the Nev* Helen Siderite is

estimated us carrying 3-5* ?7 per cont. iron on the surface; 57.97

per cent, from drill boyes, and the roabted (oaloul. tod) 53*37 P^r

eent. iron, respective!^* The average of the analyses of over 40

samples from trenches oh the Bartlett Mine, were! for ravi ore, 40.72

per cent, iron, and th6 roasted product (calculated) 5*7*02 per cent.

iron. Iiouving out the samples numbers 12 and 13 taken v.itbAn 300

feet of Bhuks Lake, the 66mplo8 taken xron thy eaotern 2,600 feetj

on the Josephine Irofa Mine Mould average apparently about 39*32

per cent, iron, anu the Billicato ubout 7 P^ 1" cent.; and the roasted

product might toe vory clobe to thbt oi t ha Bartlett Mine, or ooout

57.02 per cent, iron, especially li the I'nnganodo io uruuited as

iron oro; (See Report oi Iron 0*e Com::itt6e,1923iPP.li)9,191,andl93. )

8. Thu bain Colling Report, ^^nPige 99, states "B iollov,s:

"He A o j. r i r. i vo tho îuurliXu oru i r tay I.'i-cpiy Iron *.,'inu, tnib oro a^ f.

ontînt. 0%-r t. :-v? i cy r.-, r.ur. ^nuoo . m :~ t,non ^:n li; . *.nu r^cn^-i

^r.r.r j x . Irr.o.-' ô'lx-xlu.-.'.r-.-. Tt c T*. n in.v r.? . .ntor. T'oo-u icv.t-

t3'^ l ikoly to no pObi-oo.ww in inner, the biiro uofrrwo oy 1. 11 oro

.i-r, ,r , '/^ L ; N., -; ^,.,( ;,;y,l.^.r: 0.' ' X

(6)

oat tho siderite ore at k vertical depth of over 2*000 feat* The

drill holes on the Bartlett property apparently go to a depth of

900 feet, .Drill Hole leader ^1 on tho Josephine Mine was pat down

to a depth of 1,^90 feet, at an tangle of 80 degrees, and apparently

oats commeroial hematite iron or© at a vertioul depth of aboat

1,5^0 feet* It would seejn very probable that both tho hematite and

siderite on the Josephin^ Iron Mine go down to very great depths;

and thy t additional drilling might indioato millions of tons of

hematite ore*

9. The Brief presented by the Algoma Steel Corporation Limited

to the Advisor^ 3oard on Tariff and Taxation on November 27th,

1928, contains the following statements: "Page 12. To develop this

mine (the No* Helen eidejrite iron mine) to each a producing stage,i *"

and. to install the necessary buildings and roasting plant, would

take about two yearb, and involve a cppital expenditure of 52,000,000*

The oost of producing R ton of finished ore is estimated as follows:

Mining (3 tons for 2) ' #1. 20 Boosting 1.25 Depreoiu ti on a nd deple t i bn _____________________ *59 Oost at Mine f277p Pelivegy Costs f rorn mine to Lake Erie Ports ________ l,6l

^4, b!An ore of similar grtlio M prebent sells at Lake Erie Ports at 4*2?'operating 16bs per ton o 4

Interest charges on the investmunt viould add almost 50 cents, per

ton to thi.6 5-OSB, so that until increased mining costs in The Am

erican iron ore fields force tho price oi ore well beyond present

levels, ue will Da unnbl^j to proceed v,ith the development of this

important xuture aouruw bf supply.

"For your jLurthor inx'or ration ..e append (p. 40) a memorandum oet-

ting iorth in detail the! poat,ioilitiob lying in tho development

ur.c*. Ueo Oi C::nydi-n ooneiiciateu oro^o "

The lollo.-ing e^truotb ore tokon azom " ho ot.iu .brial (Pugeo 40-41);

;- 1 -. \ ' , . r , ' L:.*" ' : , ui.i. l i; . .*."i\:~ i. r... Vi v.-j; rt- y j-^u^ctu rrius.-! 1:

rr. ^vi;'- Xi;::ctiu. ..l^r. i.: r i^^n I.-.":t: : ' •;":-."l: ± r x- 1, o. ?'r.i^ tncj.-c~

j. . ^ ru-''.^'-^ our ju'CL'iuiii uo "cr.u tiluriciVw o... r..c*:ipciiieou , ..iJ.ua t-ouu*,

'•"At? t'Ow-n over io civur. ic!0nciiut..-ru'cion in vr.w nunuioc'curc ol

a

( (7) (

of those two ores is reduced to the simple expedient of varying

nix to salt tho grade of oro required. Briefly, a mix of 60^ sider ite and 40f. magnetite sill give c manganese content of 2^, making an excellent Bessemer iron of •'Hf, Manganese*

"Insofar uo the adoptability of these oroa to present-day blast furnace design Is conaenned, they oan readilfr replace the ores not; in use, with a tendeney to increased production.""fflth Manganese assuming its proper place in the manufacture and

use of steel, the Gdnadian aide rite deposits will become oi. inoreasa{l

importance, not only for home consumption, , but also for export, on

account of the ooinparatively small tonnage of manganese ores avail"

able in the ^•on-bearing district of Lake Superior, and the faot

that nearly all of the manganese ores are of a low grade, and re

quire beneficiation, ae do the siderite ores*

"The cost of mining th0 knov.n uepfcsits of Canadian siderite and

magnetites offers, no problem, and mining costs might bo placed ox\

the sumo bctais WB oiher underground viorkings.t i

"If theAlgoma Steel Corporation was operated continuously, itsits

four blest furnoces.xitek ore requirements ior a year viould be fip-

proxinutely 1,200,000 tons of which 640,000 tons vt ould be magnet-ores*

ite, ond 3?b,000 siderite tana: It is reasonable to suppose that, in

addition to our o,.n reqbiremunts, other Canadian lurnt-oos v.ould

take considerable tonnage, and that a iurther tonnage v.ould be oxporttV

The xoregoing iitateioents are, upvarontly, reasonable correct;

but prospective optionees are expected to have the property examined

by their ov.n Mining Sxp^rts, ^na rely entirely on their reports

UAT3D thib iibtn day ox July, ^. P.

i:,- - i . - .l* Tho J OB op hine Iron Miho le situated in the Mlohipioogen

District, a few hundred yardo from the Una of the Algoma Central

Railway, and io diotant from Michftpiooten Harbor by tho oaid

line of railway about 21 mile o* Extensive diamond drining on the

property haa proven up abour 2,2^0,000 tons of iron ore, If 30^

or* la included. If ore carrying IOBB than JjO per cent* iron le

excluded, the tonnage wbuld be reduced to 1,300,000 tons, of which.

it is estimated that over 8^0,000 tona of ore can be mined and

ohipped, averaging from 55 to 5? per oent. iron. The opinions of the Mining Geologists appear to bo unanimous that the formation

of Red or Parka Lake was caused by the ohenioal eroding of th*

aiderite ore into hematite in the Josephine Iron Mine. The hema

tite ore in the central lens ia at least 1,000 feet in length,

and goes down to a depth of at least 1,500 feet; vgereas the hem-*atlte in the Old Helen Mine wfiafe doisn to a depth of only about

700 feet, and had a length of about 700 feet. The Old Helen Minehaa produced about 2,800,000 tona of hematite ore, and it eoems

t probable that further diamond drilling or mining would prove up

orpossibly 3,000,000 isnt 4,000,000 tons of high-grade banatite o'jpe

also many millions of tons of, \ fcn the JoBophino Iron Ulna, ohd akoijQMdtiaaiaJckiiikKxkf \\3lderito ore. v

\2* There IB aleo a largo body of oiderite ore on the property, \

about fifty feet v?ide, extending from the eastern boundary -nester-V

ly to Porks or Hod Lake, a diBtanoe of over 2,800 foet, shioji ra'y

also extend westerly ojidorneath the aaid Lake a further diBtanoe .l ' of about 2,200 foot. The Bidorite in the eastern 2,600 feet may

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average otout 39.52 per oent iron, and about 2.13 per oent Ltenganese.

3, When operating at 100 per oent. capacity, the four blast

furnaces nt Gault sto.Uarie, Ontario, v.ould require about 1,200,000

tons of iron ore, annually.

4. '/he Aljjoi.-.a Btcol Oorporauloi: Lir:i-;ea, plans to oper.d c.'uout

" . ''TJO.CC;.1 r/*, rn ovc i. ~ G':' * t. r. C -.C- A : fi ci r. vi". " v.-lf:-.-.^ , i. o bc-. •.•:ricl ". ;

ricicriir- oro ir. w '!rv. H; l c:: I.'.ir^ , c? :u:ble of rr o,".'.:oi::'- fi ft D/. '..'

D, 000 TsnB of hG::..uiio oro, cr.iiually, if it operutod at naxitaun

(2)

twenty-five cents per ton on the hematite oro. This Lease contained

an option to purchase the property for #490,000 or ^00,000. Owing to the outbreak of the Great ttur, the Company oanoolled the Lease

In 1915*

5* In 1936, over 4,400,000 tons of iron ore, probably averaging about 52^ iron, were shipped from the shaft mines on the Marquette

Range in the State of Michigan, at a profit of ^1*48?0 per ton, less a royalty of JO* 2636, or Jl. 2234 per ton, made ap as follows:

Mining A Overhead Costs per ton Jl.6667Taxes .1683Railway Freight ..?033Boat Freight and Insurance * . 7846Total ' 'j 2

This estim&to is based on t\ prioe of about J4.8063 at Luke Erie

Ports.

6* It has been estimated that if GO ore carrying lens than jjO

per oent. iron were mined from tho property, about 8^0,000 tons of

hematite ore, averaging from 55 t o y) p er oent. iron ooald be mined

and sold* This oro should sell in 1937 for about Sjj.2J? per ton,

plus 30 oonts for extra high grade, or about 5^*55 per ton* This

might indicate a possible maximum net profit of aboutx^J&d&xjoox-ttrvt

±Q3Dtax ?1.93 per ton, loss 25 cents per tbii for increased raining

costs in 1937. *hen sold to American furnaoos. If tho Ontario

bounty of Jl.10 pos?xton were credited to the Mining Company, the

possible maximum profit might be #2. 93 per ton, leas 25 oonts for

increased mining costs daring 1937- In 19J.4* the price of iron ore

v;as only |3*75 periton; 1916, ^5*95; 1918, 56.40; and In 1919,

The price for 1937 is |5. 2Jj. Tho American Iron Minos in the Lakei

Superior region oxpoct to ship over 60,000,000 tons during 1937.

There should bo a profitable tn&rkot in tho United States for 300,000

tons of iron ora from t ha ?.!iohi:uooten ranges, annually, UB Araorics&n

ctoarjboata brine -about 1,000,000 tons of Ar.crioun coal to ,'-ault ste.

:'ic r.:'/": !!'lci\ ;^ir:o';' " '.'-yjc:* c"C". "c..:1 ; L '.-"-. : .i~:: -; :.; :"::io.- i. o {;:'i

..i::.-.") c '.-.r "o r- p o:" i.-n": ^ro to .' - ri-jnr. C". i'" c c". :: t t;-: ..-.'.t: c."

' ci. 't r T '-'-' t, c:;. :.'^:.::i 4 3 ve;' cc::tH O- t:.- ire:; oro ;. '.'.K. i", ir. t c.;.

'con Dictrict; \.:io ap..faror.tly exported to A nor i e.' vi iur

V\

(3)* . *

8* ThefcOanera would favorably consider the givin, of an Option

for twelve months, to a reliable Mining Company, cho "would agree

to ospend at least 312,000 on farther diamond drilling, at the rate

of at l ea at jl,000 per month* This Option viould give the said Compaiy" ' ' V

the right to enquire a thirty-year lease of the property, subject

to the payment of a royalty of twenty-five oents per ton on tha

hematite iron ore, and fifteen oonts per ton on the siderite ore

or its sintered product, with a minimus* tonnage of ono hundred

thousand dumtjadatfasudaaxkai (100,000) tons of ore to be mined eaoh

year. There would also be the further option or right to purchase

the Josephine Mine f or the sum of Three Hundred and Fifty Thousand

Dollars C$350,000.), payable, {2^,000 in oash; and the balanoe in

13 yearly installments of ^2^,000 eaoh, Kith interest at the rate

of fiva (5) per cent. per anrmm on the unpaid purchase money, pay

able with eaoh installment. The Purchasers would be entitled to

ship one ton of ore annually for every twenty- five cents paid by

thorn on account of principal and interest payable by them.

9* Tho foregoing statements are, apparently, reasonably correct;

but prospective Optionees ara expected to hove the property exam

ined by their own Mining Engineers and Geologists, and to rely

entirely on their Hoports and investigations,

DATED this 28th day of July, A. D. 1937*

42C02SEe779 eel 9 CORBIERE O2O

The Michipicoten Iron Mines, Limited have been exploring and

developing the Josephine Property for the past two years,

Previous diamond drilling had indicated about 800,000 tons of'good grade hematite and further drilling by the Michipicoten Company,

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in the same area, approximately checked this tonnage* In addition.

they indicated some 2^ million *;ons of lower grade ore. They estimate

a total, (high and low grade) of about 32 million tons to the. 1000*

level, which would average 5lfr iron and 20J* to 25# silica. Some

sections of the ore body contain massive high grade ore while", at

other points, the ore body consists of soft ore. They have estimated

that l^/* of the total tonnage would be recoverable, high grade lump .

ore and the remainder would have to be crushed, concentrated and

sintered. The resultant sinter would be high grade material. The

ratio of concentration would be nbout 3 to 2.

The diamond drilling, both old and recent, indicates that the

ore does not corao to surface although the fact that boulders of high

grade hematite foxind on surface in the vicinity, would tend to show* i

that, in places at least, the ore must have come to surface. The ore

body lies under Parkes Lake, v/hich has been pumped out. Unfortunately

the mud in the botton of the lake lias so far prevented nn examination

of the top of the ore zone,*

It had been expected from the drilling results that the ore body v

\7ithin the area drilled, was continuous ore. It was also concluded

that when holes, drilled outside this section, showed little c.r no

ore that the outside limits of the body had been reached. Therefore,

v/h on tv;o dr.Vll holes near the \Vest end of the lake and 2000' V/est

of the lunt ore indicated in the rmin lense, cut COO(3 grade hematite,

C 2.

4he conclusion -was that this was an entirely seperate body. Little

further attention was paid to it.

The present information, however, obtained from underground

mining has shown that the ore, even in the main ore section, consistsV

. of a series of lenses. The ore body in a short distance, would vary

- from a width of fifty feet to less than five feet. .

This would suggest that holes drilled outside of the ore section,

that cut little or no ore, might have cut the narrow or barren

points between recurring lenses.i

The ore is found on the South side of a band of quartz and

iron formation that extends the -whole length of the Lake and for

a considerable distance beyond in both directions. The map which

accompanies this report shows thl. *? situation.

The Algoma Ore Properties, Limited owns the property, shown

on this map, at both ends of the Josephine property.

To the Northeast the claims, known as the Bartlett, have

been drilled and several million tons of siderite ore have been\ \

indicated. This body is not immediately contiguous to the Josephine

claims but the same range of iron formation, of which this body

is a p?irt, extends to and appears to be a part of the Josepnine iron

formation. Si/nilarily to the West, the iron formation extends into

the claims of the Algor.a Ore Properties, Limited.

Nearly forty years ago three drill holes were drilled on this

Westerly property and no ore was encountered. It was, therefore,

decided that the claims had no value. Unfortunately there is no

accurate record of the location of these holes and it is doubtful

if they \vere drilled with a full knowledge of t Vi e most likely place

to rind ore, if such existed i*

Ore has been cut by two drill holes only 100' from .the

Algoma property* It is a possibility that ore exists on the Southerly

contact of the large quartz band on claim No. 7*3*

Nothing in the way of ore Is Indicated on surface and any

drilling planned would have to cut the contact at considerable depth.

The Michipicoten Company will eventually carry their explor

ation work both East and West from the present operations. Tills

work will give the answer to the question of whether or not lenses

of ore continued to the Algoma ground.

A situation might arise where ore bodies would be found on -

Algoma property which might be of such size or at such depth as to

preclude a commercial operation on them alone. They, hov/ever, might

be profitable, if mined and treated by the Michipicoten company.

Should the Federal Government grant aid to the Michipicoten

Iron Mines Limited for the construction of a concentrating andf

sintering plant, a provision should be made that, if requested,

they would act as a custom plant for any ore from adjacent bodies

on Algoma Ore Properties claims.

Sault Ste. Marie, Ontario. May 22nd, 1943.

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.AX.GOMA ORE PROPERTIES, LIMITED

IN you* nrvt rtrui wortATTtNTIOM Of

STE. MARIE ONTARIO

-October 18, 1?46.

Sir James Dunn, Bart.,President,Algoos. Steel Corporation, Limited,Seigniory Club,Quebec.

Dear Sir James,

On Monday, the 14th October, I received a cellfrom X'j. Eldon Brown, President of I'.ichipicoten Iron Mines, that they were having trouble at the Josephine IT.ine with material from the bed of the lake on surface finding access to the nine workings. I immed iately contacted V.r. Beck, k'onager of the Helen I'ine, instructing him to proceed immediately to tfrie Josephine with the idea of offering any assistance in our power to help them in this emergency, l reached the mine myself en the morning of October 15th,

At the tifr'- of my arrival the situation was that eslight depression had teen hoted in the bottom of the lake beneath which their mine workings lie and that some v/ater, together with blr.ck muck apparently from the lake bed, was finding its way into the mine on the 4th level. The mine pumps k^ere still handling the v;ater in the nine \vhich wes not excessive end the amount of muck from the lake bed that had entered the mine v/as not of serious proportions. There yes, how ever, a potential threat to the safety of the men, as no one knev/ exactly what had occurred. The Ontario Inspector of Mines, from Sudbury, had arrived at the mine and considered the situation too dangerous to el low men to work in the stopes until more information was available. V.r. Brown's ide.u at this time was to remove all the material and equipment thet could b?' Fclvtired from the umU-rrround workings, including the primary crusher, wid then pump water dov.-n the mine until it vas filled. Tin i c would hv. ve the effect of equalizing the pressure from outside andminimize the danger of inny serious cave-in. The. vork of salvaging

natorial hso cczjoienced but shortly after the noon-hour lunch p. further flc-v of mete-rial into the mine WP.F noted and all ir. en were withdrawn from underground. Tht cuvinc of the bottom of the Hke became clf-arly tpptrrnt tbout thit time in the area immedistely over the r.oet easterly pt-rt of the n:ine workings. This movement increased in i ntonr.it y end it became apparent that un opening of conBiderable dimensions existed in t h*: bottom of the Itke i.nri the material in the bed of the lake v/as

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Sir Janes Dunn, Bart. October 18,

funnelling down this opening. At one stage it was estimated that a thousand cubic yards a minute were pouring down into this cavity. As no men lere under ground it was not possible to $tate whether this material was actually going into the mine workings or into a natural subterranean cavern not directly conn ected with the mine workings. The flow of material dern this opening in the bed of the lake continued on a diminishing scale until about eight o'clock in the evening of the 15th when apparently the cavity was filled. No movement in the bed of the lake hae been noted since that time.

It was at first thought thst tne amount of material flowing from the bed of the lake was greater than the amount of ore and rock extracted from the mine during their three years of operation. However, last evening l was informed by the mine superintendent that surveys of the amount of material which had dropped through the bottom of the lake bed almost exactly equalled the open ings in the mine caused by raining operations. This amounted to approximately 85jOOO cubic yards. From this it would appear that the materiel from the bed of the lake flov/ed directly into the mine workings and has completely filled then up to a point close to the 5th level (practically all the ore has been extracted froir. the area belox the 5th level and the only openings above the 5th level are development drifts r.r.d raises).

I The only pt oping above the 5th level had been done at the extreme easterly end of the mine where the stoping had been curried practically to the 4th level. I t was directly over this point that the opening in the bed of the

(m l ake existed.

The \vater in this part of the lake had been pumped out but an. unknown amount of silt still remained covering the leke bed. The depth to the l actual rock bottom of the lake at thic point is not kno\vn but from observation * at the point of the cave-in it in at least from 3^ "to * p feet. The distance

from the uppermost working in-the mine, nrjnely, the 4th level, to the supposed

I bet tom of the lake, is over 5^6 feet, therefore an opening must have existed between the bottom of the like and e point very close to the uppermost part of the stone at the 4th level.

It is indeed fcrtvnate that sufficient warning was given to allo'i iT:"n to be vi ihdr.".wn fron there : workings because it apvf-ars quite probable thst hid stoping continued uj'V.-ar:! from th s noft easterly stope they v/culd have broken directly into the cavity to t)." lake bed, in which case few, if any, man working underground would haw 'been able *~ escape.

I !'.r enclosing a sketch t h 2. t thors the location of the cave-in to the mine

•Ir. fcldon Brown ir at present in Toronto but he has not ststed what th r: policy of thfir company will be. It is evident, however, that they Eire preparing the .7,ine for a prolonged shutdown or abnndrwior.t . The cables- are V-in~ rcrc'V"'' fro~ th'- skip? and the collar of the sh^ft ir beir.^ rfjtl?d over.

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Sir James Dunn, Bert. - October 18, 1?46.

I Some of the material from underground has been sal vaged but many thousands of dollars' worth of material, including the under- nround crusher, has been left in the mine.

I am enclosing e copy of a letter written to ne byI'r. Brown on October 13th and, as he refers in this letter to blasting at the Helen, I am also enclosing a letter from llr. Beck describing the blasting at the Helen during the time of the accident.

Yours very truly,

G'-ft/rSW

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COPY

MCH1PICOTEN IRON I'lNES. LIMITED\

Josephine ACR, Ontario.

1 October 13, 1?46.* * . : '-'

l!r. George W. VacLcod, General Vanager, —Algoiaa Ore Properties Limited,Sault Ste. Karie, Ontario. . -

Dear George, -

3 an writing to advise you of a rather extraordinary happening here, which will prevent us from shipping you any more lump ore thit year, and which will also stop our shipments of concentrate once our stock pile has been chipped out. i

Our number 3^ stope, which is the stope at the extreme east end of the orebody up against the Vorricon Fault, has caved right through to the surface. This stope st.arted caving right after we got it undercut above the 6th leyel, juet ebout a year ago. It caved up to e short distance above the ^th level end then practically stopped. About th'e middle of September it started caving again and in two days it caved up a distance of over 100'. When it passed the 4th level there was an open cpace approximately 30' in height between the top of the broken ore and the bsck of the stope. 7/e have no df if ting completed on any of the lev?] s above the 4th t.nd consequently once the stope passed that level we had no way of keeping truck of it. Assuming the normal increase in volume of rock or ore when broken, we calculated that this opening would be completely filled ?.rd the back would be supported by the broken ore before the stope rer.ched the 2nd level horizon.

On Wednesday, October 9th, we noticed that a slightdepression had appeared in the bottom of the mott easterly ba?in of the old It'V" bed. The location of this depression -vaf plotted end found to be directly above the location of number 3^ stope. This indicated the possibility of there being r. connection between this depression md the stope he l or, but no i r,cret se in the mine pumping load had been noted. Jn an endeavour to rr.uk*- certain as to whether or not there actually was some such connection a ntl l tonni.g'j of ore was drawn off from thisctope through the chut e r, on the 6th level.

Kithrr as t result of this drawing, or as a result of the heavy blui-ting which has ber-n poing on at the Helen for the past two days ar.'i which h r s been rh:;V. ing the whole countryside, or ac t combination of both, l:,ft nij.ht we h r. d e .definite tubsidenc? of a considerable are e of the old l?Ve tiottom. T r. i t '.vu^ tcccirr.Pi.nied by e flood of v/ater in the mine snd the (ii" : .-"nee of un K r pr^cicsble ti.-'Ount of Ptlatinous ooze in the 4th r.ndf t l *-'

5th 1-vcl driftr i ri the e a r. t end of the mine. Thi c oo:e ip typicnl rruterial fron-. th-i- i. f d of thr 1 :\:*j f;iid it ir coking out v.ith the water through the broken '.r* i n nurr.l-r }6 L-ioj'f. Trie provide positive rroof thf-.t thiv'tope Y,1.9 c.':-;-.'. r ij.'ht tVr:-iJC:- t^ the \ '-('. o f the o! d lv. k c, L vertical distance of ,..,11 r-- r -".00* ubov- the 4th lev.-].

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Under the circumstances I have no alternative but to suspendall mining operations until such time as the accumulation of mud and debris can be cleaned out of that portion of the old lake bed overlying the east end of the orebody. I consider that raining under existing conditions would be altogether too hazardous. Once this area wafi stripped off to the rock surface however, I can pee no reason why mining operations could not be resumed in safety.

I regret very much the necessity for such a sudden shutdown,but it is caused by circumstances which are certainly beyond our control. I hope to have an opportunity of discussing this situation with you in Toronto in the immediate future. '

Vi'ith kindest regards,

Yours sincerely,

{Signed) "Eldon L. Brown"

President ft Managing Director Ifichipicoten Iron Mines Limited.

. . COPYALGOVA ORE PROPERTIES.' LIIHTED

Helen k'ine,Ontario.

October l?, 1?46.

Mr. Geo. W. YacLeod, General Vcntger, Algona Ore Propertieo, Limited,

Sault Ste. ytrie, Ontario.

De w Georgei* *

Ir. Eldon Brown 1 c letter to you, dated October 13th, in which he describee the flooding of the Joceyhine Mine, he mention* the fact that they hed noticed heavy blasting at the Helen k'in* during t h i c period.

On October ?th, we blnoted three churn drill holes. The next churn drill hole WIB o ningle hole on October Ipth at 7*00 P.I!. The firrt blemt wae before tny ei^n of subsidence rao noted end the second blant was after thp muck was'flowing stcudily. In the intervr.l only routine block holing and Band blasting htid been carried on.

One of the peculiarities of the bltcting here is that a relatively tcntill fcand blent will auk e u.cre noiee and will be noted at a greater distance than a churn drill hole containing 200 or 300 tiroen ee much polder. Atmospheric cond.Hionc also have- an effect on th.e noticoability of the blasting.

l woulri BS;* thore w*iB li '.le chance of the blasting at Helen k'ine huvinc tnythinf: to do witn tny eubsidence which occurred at the JcB^phine I'ino.

Yours truly f

(Signed) "C. V.. Peck"

)

)

REPORT ON THS DIAMOND DRIU^NG OF THS JOSEPimG SIDSRITB DEPOSIT

JQSBPHPg PROPERTY

IRON MINES HUTTED

, ONTARIO.

MARCH,

)E. |r. V.'onQoborn.

ON'THg DlAIfflKD DRILLIHO O? THB J03SKHK5 SIDSRITB DEPOSIT

IMTRODTJCTIONi During the period Soptoiaber 25, 1950, to February 25,

Q eystenatlc dlaraond drill exaialnation ras Bade of the Josephine Siderite

Deposit for the purpose of determining Its economic extent. The deposit

lioa to the east of Parks Lake on Mining Claims Y452 and Y453 of the Jose

phine Property, which lo situated some 170 miles north froa Sault Ste. Karl*

and about 20 miles north-east fron Kichlpicoten Harbour on Lake Superior,

In the District of Algona, Province of Ontario. The Josephine Csnp 10

reached by an all-weather road, approximately l nile in length, froia llilo

6.5 of the Michipicoten Branch *if the Algcjaa Central A Hudaon Bay, Railway.

Previous to this drilling progran only a relatively ma*}!

aaount of ourfaco work \vas done on the deposit In the summer of 1931, at

which tiuo the existence of the siderite was established. It was aloo ob-

eorved at that tins to bo the eJrtonsion of the Iron Range of the Algoma

Stoel Corporation, B&rtlott Eropo^^.y, ircnodlataly adjacent to the oast*

GHNSRAL G':OIX)GYt The fjoa le osaenvifilly coHprlced of vorious phases of

Hbov/atln rocks, which Include volcanic flows and fi^afiiaentals Interstratified

with oedirasato. They have all buffered intense folding and faulting with

resultant cchiGtlficatlon, Dykos of diabase and granodiorite have Invadod

the Koc.".yatin oorlos, quite Piston oloiic crosp-fault pianos which intorfor to

n varying ticycQQ with the continuity of tho rance*

In gonernl tho eerioa is a oinglo band, with an opproxinato

vorticnl dip, having pro^resDivoly dovmrrard tho follov/ing fonintiono:

(1) Intermediate to bacic flows incltuUne eona tuffs, (2) A bandod cherty

quart -j or r.ilica sedinont, (3) Intomoaiato to acid pyroclDatics vdth con-

ciclcrablo rcplacciacinfc by cideritb tuicl pyrlto, orul (A) An ocld volcanici

cellist. I '.o o if/ic of contact jaodjicorphisa oro evident in tho band. Concc-

quontly tlio volcnnica nnd sodlraoht ara connidorod to bo in tho propor oso

relationship with the tops of the bods and flows facing toward the north.

ECONOMIC CEOIOGT; The naln goological feature in the vicinity of the Josephine * ' Siderite Deposit is the banded silica formation, which appears to have local-

llzed the ore. Characteristically it consists of laninae of nearly pure,

gray-white to gray-blue, cherty eilica, alternating with other laminae of

clliea Eixod with siderite ond/Or pyrite. The layers appear to taper and

overlap, showing considerable variation in thickness oven in short distances.

Local brecciation is cornon throughout. On Soction Ko. l, the drilling shoved

the silica aeribor to be very narrow and also intercalated with volcanic tuffo

in sharp definition suggesting deposition of tho volcanics during the fora-•s

at ion of tho banded silica sediment.

The pyrite replacement member, which occurs within the

Siderite Deposit lies boneath the silica and is composed of heavily dlnsen-

inatod to nassive, dendritic pyrito with losser pyrrhotite in a ground naoa

or dark-coloured siderite. It shcnvD a narked variation in thickness and do-

groe of concentration, In all cases being most highly concentrated immediately

benoath tho banded silica end tondlns to bocono leaner Trtth fiopth. Tho pyrite

contact with the silica \vna found to be fairly sharp, but alternations of

pyrito end banded cherty silica, nloo local interbedded areas of slaty and

silica bands, xvero oncountorod beneath the naln nilica rjion. Tho dark olaty

bands in rioot cases \\t)re ninerailzod \\lth considsroblo blobs and bands of

nasslvo pjTrhotito. The lower boundary of tho pyrite naiabor tvas found to be

Mchly indofinlto, uith nn oooy c^rndlatlon fron heavy sulphido r^atorlnl to

sidorlto v/lth cpnrsoly ccnttorod sulphide grolno. Occasional vague patches

of nnsnivo nldcrlto or oven volcanic echist wcro oncountorod within tho pyrite

r.arjbor, tho Ir.ttor oviclcr.tly vcEtif,O3 of unreplaceJl country rock. A ft/v?

volnloto o l* fresher pyrito, apparently of cecor.dary derivation {fracturo-

alco occxirrod v;ithin tho nenber. Cioos-cuitinr; roLritionship chO77od

3.

the pyrite to bo younger than the siderite ineaber within which it lies. In

come cases tho pyrite nonbor was found to be locally absent In the siderite.

The siderite Jfoplaceasnt nesiber is composed of a xnixttiro of

carbonates of iron, llrie, magnesia and .manganese, with scattered graino of

pyrite and raror magnetite and arsenopyrite {the latter partlctCJxirly noted

noar tho contact with the footwall ochlot). Tiny threadloto and blebs of

quarts are found throughout. Yostigos of fragmental and lava ochists are

fairly common, but on tho vholo fora a very minor part of tho neoabor. Tho

bottom of the siderite grades doumvrard, through alternations of Inpure and

poorly dofinod siderite areas and volcanic schist, into continuous acid

DChiot. Occasionally in the ore, the siderite exhibits a schistosity with

acconpacying chlorite, soricito and calcite. This appears in nost cases to

be representative of zones of Incomplete replacement. Frequent local zones

of ottrelite schist *aro intersected in tho siderite and qulto often forned

the footwall of the ore-grade ipatoriol. The ottrelite ninoral occurrod in

tho croara-gray, somewhat-sidoritle,schist ao tiny, tabular cryotalo r/hich at

first uppoar to bo nlnuto flocks of pyrite and pyirhotito. Tlius in many cases

those cchlotn are vory coolly iklotakon for the siderite. Thoy do not, how

ever, po03OB3 the woicht of tho latter.

Tho siderite jnoaber was shown by tho drilling ond ourfoco

exploration to bo lenticular in ohapo end occurrence, often having wide

variations In thickness. Accordingly it was found to be locally absent,

although Ito provnlcnco ond otratifiraphlc pooition Is urcaintakcablo. Tno

preoonco of tho oro cpj/jorod to depend upon tho character of tho volcanic

.formation underlying tho r.ilic^jnass. The intense folding of tho silica

::-jdl-".ont r.r.r! urjnrlyiji/; r.yroclonticn undoubtedly f^vo rico to tho forr.ntion

of tho ch.-'.T!p.ol-..:jy for thj roluilono or vcpoia-3 v.'.lcli t;ould rc:.dlly pnr.-.

4,

and alter tho latter. It lo significant that In the aroa of greatest sidorito

thickness tho volcanic footwall Is predominantly a course agglomerate, well

sheared and ochloted throughout, whereas la the sectors where the siderite

was found io bo 7or7 Jiarrow, or locally, absent, the footwall formation la a

falrly-nassivo, acid lava*

EXPLORATION: Eighteen holes in all were drilled during the program, con-

prislng a total, of 8,822 feet. The holes ranged from 104 to 905 foot In

length* The drilling was dono on sections at approxlnately 500-foot Intervals,

giving Intersections through the orebody at approximate vortical depths of

100, 300 and 500 feet. Tho deepest hole (J-3) reached a vortical depth of

700 foot.

A total of 4*917,950 tons of oidorlte ore, grading 35.90/&

Y-* 11.845& S102 and 12.33# S, wore outlined. This orebody extended from the

oant ooxmdary of tha Josophtno Property westward for o dlotonco of 1,930 foot,

Drilling to tho west of this body ohcwod tho continuation oi* tho Iron range,

but no oro of economic importance woe .encountered to the depths drilled

(Soctiono i:o. l i Ko. 2).

The occonpauying ecological plan ehov/a the location of tho

holos and various othor features laonMoned in this report.

Section. Hole. Foota.^o

Surnraary of i.ho Drilling;

Lop.

To. 5 (32.G67E)

J-l 0.0- 65.065.0- 75.375.3-173.0

173.0-ieo.o1CO.O-1S5.0 185.0-1C6.0

Tuffs Cttrolito Schist Sidorito Oro Slftty-Chorty Sodinant Grinodiorlto Intruaivo 'ilcty-Chci-ty

True

35.07

^-' - ' i'.-. l ~-

42ceaseei779 0019 CORBIERE 300

Helen Hine, Ontario August 14, 1951

Kr. George W. KacLeod Vice-President It General Algona Ore Properties, Ltd. Sault Ste. Harit, Ontario*

Dear Sir: -

In accordance vdth your recent request, I suboit

herewith an interin and summary roport dealing vith a prelijsinary

study of the economics of re-opening the Josephine hooatito Mino.

A detailed report vill follow later.

Yours vory truly,

Hichard E. Barrett ]-Iining Engineer.

m

INTERIM REPORT ft? PKoLlHlNAIft IKVESHGATICH RK OPSJIKG JOSEPHINE MINE

The most inportant consideration in a dtudy of tha economics of re-oponing tho Josephinb Hine is whether the s tope a on the 6th Level have cavod to any great extent since the aine closed.

If they did cave, as much as half a million tons of ore could be involved and the cost of recovering this would exclude any chance of ft profitable operation under present day markets, methods and costs.

The condition of these s tope s could be pre-deterained by diaaond drilling or by churn drilling. Such drilling night involve an expenditure of C-15,000 to $20,000 but Would be Justified in view of the conmitcent involved.

If th '' ?pea d^d not c^ve it is technically feasible to re-open the mine tûjr draining the overlying lake, and renoving the accuisulstion of mid froa its bottom.

COST W ORE

A preliminary ebtir^xte places the overall cost of winning the ore above the ?th Level, rt torfnys vages and prices, at tB.30 ter ton shiprod (f.o.b. Josephine îine) plus or rJnus M.00 por ton depending upon factors inporsible to assess accurately at this tine.

VJorking frou the shaft and to its present depth, it is estimated that the following ore could bs shipped: -

Lucp Ore 322,500 tons (152 of hoisted tons)

Jig Concentrates 1,182,500 (55*1,504,000

This would be Won froia the mining, corting and milling of2,150,000 tons of ore recoverable frm reserves calculated at 2,41*5,550 tons of average assay: - Fe - 51*9?

M 02- 1B.O?S ~ 1.6?

Thin production estimate excludes /,00,000 tonr. of 8.6/. sulphur, bearing icatcrinl, which conceivably could be rdned if sufficient sintering caj-ccity uere avîlrblc.

.- ^.^^vf^f-'v^jltJlf^if?x-v V; :,

ffV^;.1 ' -.i*;. - 2 -

TIKE SCHEDULE

••(•S '

From date of decision, tiae required toplan, organize, acquire and erect equipmentfor draining and dredging Parks lake (oinimua) 6 nonths

Pumping and dredging Lake ......................... 18 "

Develop one Level of the mine ...........*............12^ "

PRE-PRODUCTION PERIOD ...................... 36 "

This schedule is based upon using a 15" dredge pump and the removal of 1*7 million cu.yds. of mud.

CAPITAL REQUIREMENTS

PC f ore production can begin, an allocation of 1*9 million dollars vill be required. Details are as follows: -

Drain and dredge Lake .................. S 600,OCO

Divert natural drainagefrom mining area ......,................. 200,000

Rehabilitate plant and camps ............ 250,000

Mining isachiiiary ........................ 100,000

Stores ................................i.. 25,000

Mine General Expense30 loonths fe S 6,000 por eonth ............ 160,OCO 1,355,000

Mine primary development of2nd Level ........................ e 52,000

Special devolopaent re nudremovnl - 2nd Level .............. 108,000

Stope Development, 2nd Level ............ 25ft.000 /O4,000

VbrJdng capital ......................... t 100.010 100,000

5 1,069,000

PRODUCTIOK RATE

The production rate vill depend upon the tine required to clear a level of mud and make it available for nining. The assumptions used in this report allow a hoist of i -

First year - 300 tons green ore por day

Subsequently - UOQ " * * u m

After milling and rejection of 30? of the hoisted tonnage as tailings, the daily chipaents vould average:

First year

Subsequently

Ljrop

A5 tons

60 "

Concentrates

165 tons

220 "

TotalViHI^HMKV^

210 tons

230 "

CRAPE OF SHIPrSMTS.

It can be assured ihe erode of tho Ehippcd products will be as formerly produced: -

LUMPFo

Si02

S

59.52

8.5*

0.06^

JIG CCflCSNTT*ATES

Fe

Si02

58.5*

9.5?

CEKSFwM PiOCRAK FCR IIHIIKO

No horizontal pillars con be oDtabliched vdth security in ores ao soft as heantito. It is therefore nacensary to nine the level nearest surface before nining the ore on tho next lower, and eo on progressively downv/Hrd.

In the case of the Jose]phine, it is expedient to nine in this r.anr.or in nny case, cince the recovery of t):a mud filled yxsrtions of the nine i:;;:st proceed fro?: the top down and in increrisnts of err-ill vertical nxtcnt r.o that the ron /ire riot subjected to the hazard of i';ud flo-.jr. under hirh iicc-dr..

l l l l ll

Recovery work will be slow. The mining rate vi 11 depend upon the B peed with which a level can be cleared and stade saXe for mining*

Ibe first level underground will not be opened owing to its proximity to surface* AB coon as the second level has been developed, recovery of the colunn of caved ore over the east stope plus ooae mining of Bolid ore can begin,

No previous lateral development was done on the first, second or third levels, which is an advantage, since the caved cone can be approached through solid rock without danger of rsud flow*

The technique of cave recovery is to drive A raise near the "pipe" and then extract the caved ore and i&ud through s cram-drift sub- levels, driven from the raise *

retails of this and the emtying of the large 6th level s tope B will bo covered in the f till report to be submitted later*

DILUTION

Vihen raining has reached the ?th level, soae 10 to 14 years after the start of production, there will be an open unsupported vortical pit over the workings 1000 feet deep from TOO to 1200 feet long. It is obviouo that dilution will be a major factor.

J'dning will hav0 to be of the caving typo BO that the we ste froa the walls nay fall on top of the ore and not into it as would occur were ope?n stoping methods applied.

It is believed that the ore of greater than 30' width(i.e. - 1,3 million tons) can be made to block cave if cut sufficiently freo from the walls* "Ihe nairower sections can be rdnod by a combination of long hole blasting nnd caving techniques.

Tinco all the Josephine ore is ndlled, dilution will effect costs hut not the quality (j)f the chipped oro.

FAKKS LAKE

lias a length of JljOOO feet and an average width of - 1000 feet. Ihe r.rea at normal water level is ^30,000 sq. yards

The lake is underlain by a deposit of black gelatinous nuck resting upon soft gray cili which in turn overlieo a thin layer of fine gravel. There do not Been to bo boulders present except perhaps on the very bottom.

In July 1951 /Ipomn Ore J'rojerlics r^.do i? soundings to bodroc):.

(

of theM indicated the following averagos: -

Soft black Buck Soft silt Hard idlt Gravel

This average applied to the lake area gives a volume of mud and gravel equal to 1,670,000 cu. ydn.

A previous estimate based upon a geography si cal survey of the rock surface gave a voluae of 1,869,000 cu. yds. Host soundings in the above referred to work showed the goophyaical survey exaggerated the depth of laud*

Apparently an area of very deep oud overlies the ore body.

DRKIX5IKG PARKS LAKE

General

Eofore roclaration can begin in the Josephine nine, Parks Lake must be drained and the mud in the lake bottom removed. This is necessary because the ore body outcrops under the siud and experience at the Josephine and other hematite uines indicates that the toft ore will cave under average conditions. Iherofore it is not practical to leave a surface pillar to restrain the aud p.nd water fron entering the mine.

Widths are too great to allow the artificial support of such a cur f ace pillar.

Prod ring

In 1947 tho Canadian Dredge and Dock Co. proposed the dredging Parke Lake vdth a 15" floating cutter dredge, the spoil being pumped to Gootz Lako. Tho rate of dredging was esticated at 100,000 to 130,000 cu. yds. per month. This would require from 16 to 20 months to conplete depending upon tho actual volume of mud and the ease vdth which it can be cut and pumped. A revision by the writer of their cost data to bring it in lino with 1951 prices indicates a cost of about ?1, 150, 000. This figure is possibly high and the Dredge Company should bs asked for a new estinate.

Alternative Method

A rough estimate of tho cost of enid reraoval by renns of hydraulic conitors sluicing to seni-stationary punpa indicates a total cost of about C600,000. end a tino requirement of 18 months. This figure is nade up as follov/s: -

Efuipr.ent and ICroction - v 250, ODD Cj.orr.tins coot J 15 f cu. yd. 250,000 Contingencies - 100 t OCO

t 600,000

- 6 -The writer feels [that a detailed engineering estimate of thia

Beans of mid removal might ehow it feasible to double the rate of pumping without undue extra plant cost. Steep Rock Mines are sluicing and pumping mud with a 15" puap for about 12 cents per cu, yd* and a normal monthly output of 100,000 yds. One month recently a volua* of 160,000 cu. yds. was handled by this pump.

Venter

Canadian Dredge nnd Dock Company state that it would not be economic to dredge during the winter months* This is because the large dredge barge as well as the pipe line pontons oust be free to nore continually| However, we understand that Steep Rock Hi ne e successfully hydraulic and puap mud during the winter months.

This phase of the problem oust be thoroughly investigated.

vator.

Draining

The previous operatoro pumped Parks Lake empty of the clear This required 8 months punping S 6000 Imperial Gallons por minute.

The lake would have to be at least partially drained before hydraulicing aud could begin, On the other hand dredging would loi;er the lake level as it renoved the fo

DETAILED RKPCR7

A detailed report covering this investigation vill be submitted vihen prepared.

CYours very truly

Helen Xino, Ontario August 14, 1951

Kichard E. Barrett Professional Engineer.

.ri

ALGOMA ORE PROPERTIES DIVISION

THE ALGOMA STEEL CORPORATION, LIMITED

EXPLORATION DEPARTMENT

JOSEPHINE EXTENSION PROPERTY

Subject! Geological Mapping of Josephine Extension Property, May 13 - 17, 1966

General Geology

The area napped le Bituated on the vest end of the Bortlett-Josephine iron range. An assemblage of rocks typical of the Michipicoten group is exposed on the property. Along the southern portion of the grid, from 2-K)OW to 15-KX)E, lie a series of silicic volcanics, these being the oldest rocks in the section. The iron formation rests upon these volcanics. No contact was observed, but from the proximity of outcrops it appears to be abrupt, or, at most, gradational over a very few feet. A series of mafic volcanics overlies the iron formation. A sharp contact was noted in two locations; in each instance the base of the volcanics shoved shearing roughly parallel to the contact. Mafic volcanics comprise the section from 0+00 to 8+OOS on the western end of the grid. A band of grayvackes and minor shales lies above the mafics in the north east portion of the grid. This contact appears to be interbar.ded over an indefinite width. Diabase dykes are observed in contact with all older formations; they represent the only noted intrusive activity within the grid area.

The volcanic-sedimentary sequence strikes slightly north ofeast and dips steeply north-vest. It represents a portion of the south limb of the South Range syncline.

A major fault abruptly terminates the iron formation on thewestern end of the map area. It ha.^ been noted by Goodwin (G.S.A. Dull, Vol. 73, p. 561-586 Plate l, May 1962) and designated the Josephine fault.

Local topography is quite uneven. The central portion of the grid from west to east is aoniinated by a steep sided hill which rises 75-100' above Parks Lake.

Glacial striae tr0nd north-easterly.

Silicic Volcanics

The lover volcanic member grades between massive rhyolitic,banded and pyroclastic phases, the pyroclastics being predominant. Much of the sequence ha:; been sheared and altered; in places i t appears schistose. Alteration precise t n arc chiefly carbonates. Chlorite may impart the light-^yreen

Cont'd.

•'V-ii-V.

- 2 -

'Silicic Volcanics (Cont'd.)

colour. Flow lines may be seen to bend around small (^" -3") volcanic bombs In the pyroclastic phase. Quartz and quartz-carbonate stringers are present throughout, but are -B&W*frequent in the eastern portion in the vicinity of 8-KX)3 to 9-KX)S, i.e. deeper in the stratigraphic section.

Iron Formation

The iron formation consists of interbanded chert and siderite. The chert is fine grained becoming finer towards the base of the member. Siderite is associated with chert or quartz within narrow brcwn bands. Nearthe lower contact the siderite bands become slightly wider, but chert is still greatly predominant. Some sulphides are present close to the south-easterly margin.

A maximum width in plan view of about 500' is attained between 1+OOE and 2+OOE and again between 7-tOOE and 8+OOE. To the west it is cut off between 1-KXJW and 2+OOW by the Josephine fault. From 8-*OOE it narrows rapidly to a few tens of feet at 13+80E and jnay pinch out entirely by 14-KX) or 15-*OOE. Thus there is an approximate strike JLength of 1,500 - 1,600*.

Iron staining is widespread and presents a deceiving picturewith respect to iron content. At no location does the formation seem to be ore bearing.

Mafic Volcanics

The cherty iron formation is overlain by a series of maficvolcanics. A gradation between massive and banded phases is present. In the north-west portion, east of the Josephine fault they are gray and massive, while towards the east they become chloritized and banded in part. On a small point in Parks Lake (15+OOE, 3^08) a porphyritic phase is present.

around 8-*OOE.Thickness varies greatly; the member may pinch out altogether

Where observed in direct contact with the iron formation the mafics showed shearing parallel to the contact. In gradational contact with overlying sediments they are schistose and chloritized. Otherwise they are generally fine grained and relatively undisturbed.

West of the Josephine fault they exhibit a coarser texture.Chlorite schists are interbanded with massive andesites. In places they grade from a medium grained to near diabasic texture.

Sediments

Gr^yvncke with minor slate is exposed in th^ north-eastern corner. These are fine grained and grey to black in appearance.

Two slaty cleavages are present. The latter and more pronounced strikes slightly north of east and dips steeply north; it is likely

Cont'd...

- 3 -

(Cont' d.

; related to the folding of the South Range syncline. The earlier, poorly ' developed cleavage makes a small angle vith the veil developed cleavage. It may "be related to a previous movement,

Diabase tykes

The diabase displays the typical texture, fresh in' appearance. Contacts are sharp vith narrow- chill zones. One dyke appears to be associated vith the Josephine fault. All are discontinuous across the surface of the map area, TopographVand their manner of disappearance mpy suggest a northern feeder source at depth.

Stratigraphy and Structure

Stratigraphy and regional structures are discussed at length by Goodvin (see previous reference) and vill not be mentioned further herein.

The major linear structure on the property is the north trending Josephine fault. It is exhibited in ^hear zones betveen 1-HDOW and 2+OOW. In the vicinity of 2-*OOW, 8+OOS to 10-KXDS the shear zones f ollov a narrov steep sided gorge vhich provides drainage for Noname Lake. Iron formation is exposed on the east face, vith diabase on the vest. . -

Disappearance of the iron formation to the east may be due to an easterly plunge of the fold axis.

Academically some interesting problems are posed by the diabasedykes. When ?earing or crossing contacts the dykes change direction or disappear. Several possibilities u^iy be examined.

(1) Tppograp); y

If the attitude of the dyke vails is other than verticala difference in elevation will create an apparent offset. However, the contacts are very nearly vertical; within the restricted areas in question topography could not produce apparent offsets in the range of 100' .

(2) tedia Changes

In passing from one rock type Into another fluid drag and surface tension may cause a deviation in direction.

(3) Vertical Movements

Subsequent to dyke emplacement, adjustments mainly of avertical nature with a horizontal component may have occured. These could conceiveably be related to areal folding in the major syncline.

00 Strike -Slip

The east-west trending contacts between the host rocks mayprovide planes of weakness for strike-slip faulting to follow. A longitudinal movement of 100' would be difficult to observe In mapping these contacts without tt transverse market" horizon.

Cont 'd.,...

.. k -

l

l

shearing.

Strike-Slip (Cont'd.)

Whether (3) or (U) may apply, the rocks near the contacts

(5) Top Contacts

Some of the diabase-hos^ rock contacts may be those ofthe upper surface of the diabase. This may be true particularly in the area around 1-KX)W, 2+50S. The dyke top may undulate or rake beneath the older formations. On the other hand, the lower contact of the overlying strata may act as a barrier to the intrusive mass. Drilling in DDH 5 indicates a mass of diabase "between a vertical depth of 350' to 600' with a horizontal extent "between l-*JfOS to 2-KJOS along X-Sec 6+65E. This would place the intersection in the path of the large north-easterly trending dyke.

Conclusions

The iron formatioi^ as exposed on surface does not appear to "be of economic value. Systematic trenching and channel sampling across the formation near its base might reveal the upper configuration of the ore zone as outlined in diamond drilling.

The magnetic high at 1+OOW, 8+50S may be caused by the diabase dyke. Less conspicuous highs occur above the dykes at other locations, notably 15-JOOE - 16+OOE, O-HJOS and 9-KX)E - lCHOOE, 0-KX) S.L.

May 20, 1966. L. B. Goldsmith, Exploration Department,

Algoma Ore Properties Division.

i|Jf The Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

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Day runner,

Night runner.

Foreman,

i The Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT,

..At

tNa. WEEK ENDING.-.-- ..-^^^...^ff.. 1...,.,.. .. .,,J90 1

Ft I.

Kramrd f^rCaning. .

FL I..

Cor* dpverv

FL 1*.

Tout PL In. lire, Mbk

B*

•t

11..

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i-*v- rPrl.rL

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D.y.

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M-

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n jl^L.

^-^

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fturfat*.Kind of K tvk. Dale. C*uw of JMavv

IS

l

t l,

lfc-

Day runner,

Nigh, runner

Fo^an,

He*

liie Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

, t

^....(tyiiMJLt......

.y

-; . ' t tThe Algoma Commercial Company, Limited,


.....jL..~ . ... ......... ..490 7 .

w*- v•f#........490/J

MINING EXPLORATION DEPARTMENT

H..-

IfHie "Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

9

Commercial Cpmpany, Limited,10


*^

fn.r.Kiffcl.

/Q

r Kifbl. z: 2*-/e.

Y- Xighl..... -4~.

.A.JA-'lCL, J~

from

/f

Kind of Ki.V MM rf Delay*.

i//

Day

Nigh! runner.

Foreman.

^^5i^'^^:r^:v ;?";y:v \'^'-:'.;;. '"v;'- : ."v^ ' ' :; "' v'- ;:\v;' '^^'^•• :z^"X.y - : ,' : v ;

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Algoma Commercial Company, Limited,

.J90/ .

wi,u.

[FKe: Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

12

...At

WEEK ENDING.....

D.U.

ft

Shift.

und TIP* Jnwrrlco.

FL

Rurned forC**in(. '

Fi, In.PriUMi

Pt. In.

y//

Con Retovrxd.

PL J*.

Total D.ptV

Ft In.UnuuJIhhyt. Hrm. MU.

Carko* Wut*.

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tri. .

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.

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from' *rvnptio*i **f

. . —,___ -. -J^~~';-~ [-- ^ -

l

lt

l

l

li!4

l l

l

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Kind of Kocb Cauw of IVIiy

i ' i

*^e/'

Day .unncr,

Nigh, runner,

/

l The Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

xWEEK ENDING. r...*Z?.

D.U. Shift.

Suivd Pin* Inwrteo.

Fi. 1*.

Keamcd for Cwin,. '

Ft. U.

Dnlled.

Ft. In

Cm Rrcovrrni

Fi. In.Tot*) DrpU.

Fi. IB.limnal DrUy^ lire. Ma.

BitNo.

Carfco* WMU.

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from•u rf ACT.

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**^~?L

--.^?^:^

Algoma Commercial Company, Limited,. ' ^^ * ' -

14


WEEK ,-.190./-.

iti t

n.u.

S

suit"IHy.

NI.M.

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zzr;

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S//1?

l

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/

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4tt

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C.AO.WMU.

Xu.

X

^,

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foe. Day runner, ,

Nighl runner,

Foreman,

ill|ie Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

elQfcM, . ...,

' -

15

WEEK .490

l D.U.

t l

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Shift.JHy.

Ni.1.1.

D.y.

Nifkl.

D.jr.

D.y.

^Xifht.

!l ll

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Depth from

Sund Pin* Invrud

PL l*.

.1.—i.

for

Ft.

T

Dntkd.

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-^~~3

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' CmRtcovmd.

PL In.

Z

TdUl Drpth.

PL l*.

AJ1L

Vnuial tMjiym.

lin. Mi*.

BH No.

WMI*.

x

CAUM' of

Day ninner,

Nighl runner

Foreman.

Hlgoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

WEEK ENDING..

Suml P,D* Imerua.

t. in.

"T"

Rramtd fer CkHH(.

Ft. I ..DrUWd.

Pt. la.

X

\w

Ktiui

9-

/tUnJ

^

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Pt. In.Tout Depth. Fu 1^

22Vnuui Dcl*r^ Hra. Mi*.

BUNo.

C.rbo*

Kto.

UMT of IX-Uy*.

Day runner.

Night rum.cr.

Foreman,

\\-:..\tia.

e Algoma Commercial Company, Limited/MINING EXPLORATION DEPARTMENT,

16

n.y.

FI. i*. Fi. IB.

. .... .

/o

y ^

Day

Foreman,

^t^/^/e^--^

J st

;|i^53J;/; vv^f1 x"- r :' ~'^.'-^:;"'

v45i^i^'i'I'J'"'-/--" ' 1^!:-:^-

Algoma Commercial Company, Limited,' MINING EXPLORATION DEPARTMENT.

Steffe,.

WEEK ENDING

Dal*.

M.

Shift.

Day.

Day.

Xi^rt.

Rljuvd Pip* InMerUd.

Ft. U.

Return) f"r CaMnf.

Pt. In.Drilled.

Ft. I..

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Ft. 1*.ToUl Depth.

PL 1*.

Vnunl Dcby*.

lin. Ml*.

K* Ne.

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lUy.J

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7- 21 SZ

ptitw ofl surface,

lti

a/'

i X/

K.nJ .J Mock D.lr. C*uwr of

D,iy ninner,

Night runner.

Foreman.

Algoma Gommercial Company, Limited,MINING EXPLORATION DEPARTMENT.

19

WEEK ENDING..

DrUJwL

FL In

Con Recovered.

FL l*.Total IVpO..

Ft. In. Hra. M

Bil No.

Wuta.

Ku.

s.

t

Xx

/fi.J&.

//o

Jg-*.~4:qrz~r-Tr"^l IT "v—f———

usf of IVUy*.

Day runner,

Nigh, runner,

Foreman,

In-*.

wiiisigj^[omaCommercial Company, Limited,


WEEK ENDING.. .190 /.' Cor, Rccov(ced.

FL la.ToUl Depth. Ft 1*.

Unuul Delay*. Hn. Min.

Carto, Wuu.

K*.

/^:3 s

.•le. frotn surface.

K.nJ of K.vh C* us* **f

T

SS®5iU^p*-^ : ."v"^-V^/ - . :. :- -' . ' - -. ' " - : ^.VBp^B^^yr;;V---\--.^;.- :; , --' - . : ;- ;; . , - , - -' 23iT^^lflie:! Algoma Commercial Company, Limited,*3fcl' ^, r . MINING EXPLORATION DEPARTMENT.

'^vC'fck ;! ' :

tli^-. '•."- ' '. ' "' "' ' '

#^- —— : ———

1 D.U.

1*4f fI-/,i 1\ 1jLr"•on of

tirr

11 1 .i^f ' M^Ct

SMft.

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Ki^fcU

Ray.

XirfciHay.

Ni^.1.

Day.

NilfKt.

Itay.

\i,Ki.

Day.

Niyht.

Pa,.

N,M.

IX:p(h frooi

t&v^D

'

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Pt In. Ft. In.

1

1

.

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l/' A

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i

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t/ ff /^/?J n f ' 3

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l/tî^jSHJ^PT^&t, tt——t' C/

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i

^

fi ' '

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Algoma Commercial Company, Limited, 25


WEEK 190/..

t••••di

"-d

id

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Niclit.

Niyfct.

JLteL-

Day.

Nirtil.

, i of

l1

l

z

Hay

NljhL

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(J O

PL 1*. PL

forf.

U.DnBci

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Pt. lo

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fu:.-2

ToUlDcjxli. Pi. li.

J&L

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t'niMal Dekya lin. MM.

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Xu.

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Foreman,

J J^ :^ ; :^ ^

.- :'-i- - - - - ,- , . -Algorna Commercial Company, Limited,' '


|p:fc': *Knf-'--.;\ riirt^Jj-'-J'-, -- .'4H

( n.u.

J^/

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pt ion of"k.

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^ [^ X/ -^ J^^^ÛÛ^

Shift.

l).y.

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O.y.

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Day.

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N^.

IVjrth Trom

Suni) Pin* Inirrwd.

Ft. li.

|'

1.i

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;

:

ommercicu vôniEXPLORATION DEPARTS

tif (tyltsrLZ,

WEEK END]

XeanwJ for

Ft. In.J"

t/-

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ft

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t

1

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^

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/

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The Algoma Commercial Company, Limited,MINING EXPLORATION

[f IfFhe Algoma Commercial Company, Limited,/..t**) *". '•-••\ v.-'-.'.' . ^^ ** ** ''." ; *' : ' "'.' '\'.' . *

T! MINING EXPLORATION DEPARTMENT.

26

•


l WEEK ENDING-.f/^^!^:..^.^.'0. ,.... 190 A.

tDuU.

/IM

i'•*,i i i

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nurfjtrc.

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aro

1

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0t -^ *45^FTZ

Un lira. Mi*.

l/

Bil No.

C.rhoo \V*.U.

Ku.

CaiiMT of

Day runner.

Nigh, runner.

Foreman. (I

mm

Algoma Commercial Company, Limited(MINING EXPLORATION DEPARTMENT.

.Commercial Company, Limited,


Commercial Company, Limited,:


31

^itt?F

if1 i ,

* ; :~-/..'.-, : ' -r^^./. LV'V'^''';~-r ;r ; ' -.- -' :. ' ' -. ' :-' ' ' , . - ' ' "'

pThe Algoma Commercial Company, Limited,v- - MINING EXPLORATION DEPARTMENT.

# . At Jfa^jU^JutrtJL. (ftlt/YU*M. *^ , ,.^ ^, .

f -

If DI.W. Shift.

If i.

i 7^

f \ n**-ff C' N i"fct-' 7| Hay.

j/ ^ Night

' ! i*r.l ^//! Night

1 Day.

1/3/1 Ki^

r

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ty/a N^tj Day.

flit *^(i n.y.

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l1

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1 1 1f

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ij

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i . . ..... . ..... — ..[ - "' - ~~~

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ff lJ~

y/O '/D *y */Z *ts ^/0 i ' 4#6 //^ '

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WEEK ENDING . Jtlt^^M* riP-Rnvfcred. Tout DcplK UmwaJ Delay*. Ft In. Ft l*. Hn. Mim.

g ' d'&f' .\S~ " *J~o6fy 2. J'fy ./P r n Syjr 'ff ir *rfy 'd 6 J~04 '

4 , " //f^ f WJ r 6/4 '

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f

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f

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/0

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3\

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uj li^-^^^. —i . ....

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Night runner, c^t^C- (

Foreman, CsL^ff'^&C*!

——

'P /(tis&Lsf)^

i

i

l 1

p^W^'^-v' -^y\v; •"'."' ' -- - .'" ;/," ' . ' -- v

Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

WEEK ENDING-

Shift.

Stand Pip* Iiurrted.

ft. In.

Rmned for Ciautf.

PL In.

DnTUA

PL In

" Cwt Recovered.

Ft. 1*.Tout

PL In.

U*UM

Hn. Mn.

Bit No.

Carbo* Wuu.

K to.

l

Day. AJJLJ*

/oI/Z /O

/X /o

l ^/.

x/ -2-.

NiKlil. 6

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l

l

l

l

l

l

l

l

l

l

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C^a j. /tx4-^x?Mxi^M ^X/

.

Day

Nigh, runner.

Foreran.

./,A

Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

WEEK ENDING.

Shift.

Day.

-PVl-Night.

Ray.

Night.

1

1

i i ii

-?±?-.Niirht.

Depth from

i *nd 1NM Inserted.

Pi.

..J.,- —

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PL In

•4^-

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y

\1Z-i it

Kind of Knck. Datr.

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Uninid IlcUy*. Hn. MU.

SO

Bil

/oJD-

l*

C*ttx* of I Way*.

V

Day runner.

Night

Foreman,

|li^H it v,. '

\^

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L

^^Jgdriia C• ;'- v'V ,; ',- ' - ' ' '. -' ' " ^^ '. ' '•••* " ' :

; MINING. . f

surtRiy.

Ki*lit

Day.

| NicfcL

Day.

j NJ(hL

Pay.

Ki.KL

1 Dtty.

j Night.

Day.

j N^

M&jf ^ li. .'^.

Stand Pip* Inurted.

Pt. In.

1

l

iiil;

RramcJCaw.

Ft

" ' - . ' , ' ' '" : . ' - . f ' .' . - ^ . '.

ommercial ComEXPLORATION DEPART!

i*c f/PLC'MJz, . ..........WEEK END

fw

1*.1

..j ,. ,

Kind of K nek

.-.,-.---

Ft. In.

/0

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,

,

,

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,

,

.

,

,

t m ,r

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Ft. 1*.

-Z*^

^^

Af/f

s/•S—y

.

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,,

pany, Limited,^ENT.

* *

IMG jfeteHt#6cS ^~f

ToUlIVptk. PL I*.

3 y z3trj~S&J'//P7\tJLft?J/-6L-4J&4J3/{//J/S/J3"4&T.'

.

Unuvi] Dvtayft. lira. Mm.^/"

^

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li

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vfliu!Kta.

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/^. !

IIPIpHii"i,tlr1-

i/t••OH *vf

jrii ii i. ii i

r'07tt,tt

~r

^'.^^-•';;l; , ;.v; ." :r '\v-'\v "- . -p :l^Vi/'^^' " ' '"•. V^-" '" "V*.? • ;; -'--IV ' ':* ' ."' -

J;ti^AJgoma Com? ^ MINING EX!

! i Stand Pi.* J Inxrted

Fu In.

i

D,, j

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Day.

Nifht

D.y.

Niyhl.

n.y.Niyht.

K.y.

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i

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ii— .— .— - .--.

Reamed forc*™*. iFt In. j

^•'.•'**: '''-''^ '•\'",'-'' 34 imercial Company, Limited,JLORATION DEPARTMENT.

WEEK ENDING, vtl^^nc^*^.//'^. .J90/.-

. OrilUL Ft. K

; !j /y ,'

1

1

1

//9 - ..lo -A.P ,

/2^ ,/Z/O '

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g ^ JfUtf j . fa

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j .... -. ...- ... ——— ...... ^ . . . ... . - . - -

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!; - . - ../y

j

i ,. . ————————— . ———— . —— . —— . — —————

i

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Night runners W#^L (/^l^yl^^^^

Foreman. CL^r*sfat^L-^t ,

\

i,J

i

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5il

l),X

^ :'' - - ,-' ' ' tAlgoma Commercial Company, Limited,

*"^. ' . - ^ * - ,

33


WEEK ENDING . . /-

Stand Pine lawrtnl

PL In.

Reamed for C**inf.

Pt. In.

IMUnL

Pt. la.

' Cor. Recovered.

PL la.

Tola) Drptk.

PL In.

VnuultWUjn.

lin. MM.

Bit No.

WMU. Kta.

Nijhu AT

Nifht.

D.y. ____l____

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Xight.

NitfhL

IVplh t f twn

i

lit h

Kind of Kixk D- le CAUM; i^f 1VU)*.

'l'

Day

Nighl runner,

Foreman,

H**

{Hie Algoma Commercial Company, Limited,^ MINING EXPLORATION DEPARTMENT.

e WEEK ENDING., l

"au. Shift.

Sund rip* InftrrtML

Ft. I..

Keamnl for Ca

Ft.

PrilUL

Fi.

,

Ft.

CorfTr-al IVptK

Ft la-

UnuulDcUya.

lin. MU.BH Wuu.

wDay.

Night.

IHy.

Day^

2L'*^-

Night.

Day.

Night.

.urfi.rc.

1

s:

Kind of Kivk. Dalr Cam* of IVUy*.

/lee y*-

runntr,

Night runner.

Foreman,

Algoma Commercial Company, Limited,''*' "' ' '•' "

38

|^p,y MINING EXPLORATION DEPARTMENT.

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i^

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i: Y' -T 0 - J

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^teTKe? Algoma Commercial Company, Limited S:7NKR-3x* - v- - A--,:* *-* ' ; i ' -- . * * -.:.-

•fe^ :r -^ : " ; .' ' - ;! " ' " - 'Ifta^i -f MINING EXPLORATION DEPARTMENT.OT* ;r s " •.-•" . ' -: - - . |R^^ 4L-**JLLL~ PlttA^L5|lf^^xv'" '"{•Noi^' : V #*t^* '

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Bil No.

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—————— ...

!l ^v j^Day runner, ^~f /f/f*

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l Foreman,l l

li

3 f

Kllie Algoma Commercial Company, Limited,ftffg^v.;; "' " " :

40


WEEK ENDING...

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1

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MINING EXPLORTION DEPARTMENT.

WEEK ENDlNG...~ife^*iSisS.......'LC...,,..,..-.. .490 3

Day runner, . ^0***?.

Night runner. V^ C

Foreman, . l '

Algoma Commercial Company, Limited,.


vwIfatA-

WEEK ENDING........ ..^4r^?......^....,....... .........190.*

SUft.

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Ft. U.

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......i

l-'f l

•-..-^ -v- -. .-v.--- . - -Gornniercial Coinpany, Limited,

43'


* *

WEEK ENDING-... . tty'^....A6'**: . .....1903..

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ie Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

WEEK ENDING.......... .-.f. .....190

ilrir] fi

.DaU.

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if." *^-'**'-:*-.'' "' . "''"

Commeraal Company, Limited,I^^v.vr^'-'-.'T •••- - ' : ,-

S^'^ ' MINING EXPLORATION DEPARTMENT.

45;

WI j^jf i

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Pi. I..

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^^^'^f^|*^)v'''-^J;VrS^,7,'f ;' 1 '": 'X ! ''' ; :.,vV'! " *}:^:~ : -- ".. . '

. oina Comnier dal Company, Lkoited,

MINING EXPLORATION DEPARTMENT.-

46

iBn^NotV.. P "Jtft* ..{fcdb. . ... WEEK ENDING ........,.!^2f^........//......*,.. . .... . .,,.J90 *...• : • '•'••: -' ' ' 17

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l f S

-.... - - .Algoma Commercial Company, Lirnited,


WEEK ENDING-.-.-..^/.*-**:.....*?.

47

490 SjBwv ^ /X^.f'^

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c /"

li The Algoma Comniercial Company, Limited,MINING EXPLORATION DEPARTMENT.

E,//l No^.j -v?'- :-hw,;;.,

WEEK ENDING...... .......f..**^........... 1?...?....... ,. ,-. .......190-S...

ll

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i

||TThe Algoma Commercial Company, Limited,49


WEEK ENDING...-.-.jife-ot. . ....A.?^....m 3 .

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1

. . .. .-.. — - .. . .!l - -.-.-..— ...

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•- - "'

1al

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Foreman,

t/ , S P ^*

(t)\ 4

8i*p*rir*tondont

^WEEKLY DRILL REPORMINES DEPARTMENT

V

m" No.^X-451

goma Coi^nercial Company, Limited,'s f^-MINING EXPLORATION~—"**™ - —*- ^

WEEK ENDING

l

l iSal.

l

f

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Day.

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Ft. In.Drilled.

Fi. In

is-U

f notion of niw.

1

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e-RtcincrcJ. U Total Depth. Ft. In. i Fi. In.

,Aoajj? iffm

UituMl DeUyi. H rv. Mill.

Bil

Cau^ pf DcUy*.

C.fbo.

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Algoma er cial Company, Limited,MINING EXPLORATION DEPARTMENT.

M^f-i . V , , ' :f^CJJ^^

imsrn?^. ne algoma ^onidpcierciai company, juimuecif f ^ S^.s#:i^:X-.,-;':-"' ••..\; 1 . : :'.'.'. -. . . - - . " ••''?/ •1 ry^^yNi/-:-'-'-' --•.•'•- "V ' - '' ' ~''i,\W^Ji^^^^^f-.'-' MINING EXPLORATION DEPARTMENT.

1 ' j [j p.*.f'rf"Wu**. j /^

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Pt. In.

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l i i i i i i. '\i

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b 4

e;Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

WEEK ENDING......../*t^H5A.....~.*.L... ...,.... 490 3

r~~ \f-

^Rfe

m^:

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1-

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IXiy.

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NiKM.

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Foreman.

l.,.

**. ..llel^Algonia Gommercial Company, Limited, ^


.&W.H-"-1 *

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jt-rl j

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tt

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surface.

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Sitt J A'S Wf f"

J76

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Hrm. MM.

Bil No.

1 ' ' .Carfco* Wawa.

Kta.

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fr(Lf/ s/9-A^

i

V

i*?g!-~O \*i j .''J

•w? te ;. 4; i-™ "* - '-. jrfpf v; :.• n8.'',^•v^v":-j)ip,

-; : - - . ' • •• Jl t' . - - - -- ;. '•' ' - V ' "'' "' r *?',' . '

. . . " "' ' ' -•"•••-•'- : .'^•'. ' ' .'*' ""

- , ' " ' '64 degrees

•j . '

.j -^ . . -' ; . ..' . ' , : l-.

HOLS WO. 15.equals v . ^

. 1* length .438' horizontally

triVv--,- -;' ; ;. l f length equals .898' vertically^,::'-'iiUr

|0

1t11111iiiii\ii

* - ' '- - f -1 — 16*

16 -455455 - 460460 - 470470 - 480480 - 485485 - 490490 - 495495 - 500 500 - 50550S - 510510 - 515515 - 520 520 - 525525 ~ 530 530 - 535555 ~ 540540 - 545545 - 550 550 - 555555 - 560560 - 565565 - 570570 - 575575 - 580580 - 585585 - 590590 - 595595 - 600 600 - 605605 - 610610 - 615615 - 620620 - 625625 - 630630 - 635635 - 640649 - 645645 - 650 650 - 655655 - 660669 - 665665 -r^670

surface .SchistJasper Sen

Mttnn

.'i tttt

.-'intt

frre"n

Jr,npor wHnif

Oronnitttit it

Jasper wit"•t""11tttt ttHtt

Analysis of Sludge *. Iron In'sol. Sul.J

Ore 12.535*27.4046.3045.8646.3061.2JL53.03 54,8117.65:- 15.45 T.- ' -.- ' ' ' - . -9.20 l v: ' -.

21.7056.70 48.1758.40 10.01 .00658.02

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fa*S'Sfa, r ,^/^^ '

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DrilW. Pt. l*.

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WEEK ENDING....™^"^. .. .X.^-.-..... .. ..........1903..X" ^ i

. ' Cor* l ' C*rlw* Rmn-cnJ. T rt.! Drpik. UnuMl DrUyt Bil Wul*.Pi. In. Ft Ift. llr* Mi*. N* Xte.

/ Z~w x/^ x

xf //)^...x...., ,,. ^^7 . ,/ i^— y/^ ^7 •J'jtX

X /™" X /*/ XJ ^â X.y 5"// X^ t?J-/ X Is ' 7sr xA '91* - - l x

Cauk*' c*/ IX' la y*.

'

1t . - - i-- - iii i1 -. i\

Day runner, /X /V0-**-?**y

Night n.nner, (7VJ*-/ ^'* ^"?

Foreman. /X X fy^f'c

7 (

Algoma Commercial Company, Limited,ITfe-;-?'^ -"'- i ' - '

M-?3f'*'...-: -

,te , ^ - MINING EXPLORATION DEPARTMENT.,*i4.'- -*/? ''i ' " ' . '

Sif:*":.:-; -. x. •fc^'-v. ;.'l^:,.,/^- - ...At.........

c^fo*

20

m?,-lev WEEK .190-3.

Shift.

Stand Pin* liu*rt*d.

PL ' 1*.

' Rnaml for Cuinf.

PL In.DnlML

PL

'* ConRofnvtffMi.

PL UTeUlDcfKlk

Pi. U

Untiut Ddiy*. Hra. Ml*.

M Ko.

J -

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fi If hi.

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i"* . '; !

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J.

UM- f*f IVIayt.

Day runner,

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Foreman.

@ fi?

/l ^

lsev--:-13^: -8®.'jy&ttf

. . . . , . . . . .

Algoma Commercial Company, Limited,2i

y'i?'~. "' t

JP.V--Mm- MINING EXPLORATION DEPARTMENT.

SJ

Ol

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Analysis of Core.*

vertical v- horizontally

•PW?'''

I V^X-V'-'^V'/- . te^--'^fwfyrt-V'Vffrt*'-'.'P:'*V- : -i ''

Pi;iiiiiiii

• ; '^y';"--' 302 -390

390 - 450

450 - 480

480 - 485

485 ~ 495

495 - 516

516 - 530

, .530 - 5-14

Green Schist . - :- -' .^ f- r..v" .'l : ' " - "- -. ** - -

PocoJnposed Green Schist ' . 'Mixed Ore and Jasper .

Ore Iron 51.50; Insol.24.25; S.030; P. .024.

Jasper ' '" -.

Uipced Ore and Jasper

Jasper - -

Mipced Ore Se Jasper.

1! p'WS

J4.n .-f-

J

|)uU*^.

i t

Ill nrt*e Algoma Commercial CompaniipiS"';^. ' .; - -* .v TV-'"'-.-.- '- . -

i^'W ! ' ; MINING EXPLORATION DEPARTMENT.||?| : - v; ' : - : v . ' -. ;-. -., - - -- .

piM^^Z^L-'

Dal*.

-J

— f

f

i

t

Wttwn'\L.

'^WF ————— -

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Skill.

Day.

Nift"-

Day.

Kifiit.

D.,.

Kifkt.

Day.

Xiffht. -

Day.

Nijhi.Day.

Nl'fhl.

Xighl.

IVpth from

Hurfacc.

l

1

|

i

1 .1

i

Stand Pipe Invrtol.

Fi. In.

/t5

j

\

WEEK END]

Reamed for Ca*int;.

Fi. In.

i

1

Kind of Kt-V.

o /^ ' ;-^) p i^is-f

DnOcd.

Pt. la.

/A

/f

/f

-t2-frsJLJUTj o\f

lUlr.

R^U Pt. la.

M,rsog33/f

—— -

ING......^s^?

y, Limited,

Total Drplli.

Ft. la.

/A' l

/js

3d_^/^•^t??3SJtJL/3a/*rz*SJ'f

-.- ----Cau

lin. Mi*.

v of IX

-^-.

-....—..-.. -. — — . — -— —

-- --- - -- - - --

- — —.

-- —— .. ——— ————

Bil Nix.

s

/

fss

ST———

Cartwa

Kta.

-

Trrrrrr:-: ^r-.-

— — — —— - — - .

— . — .-- — . —— .

--- ---- - - --- - ..— — - — .-. — .. ———————

--- -- - - - - - ---......-.— —

—————————— .

j&P 6?) PS Day runner, --Z^T*-*^' L/ fx^x^j,

Night runner, y /y3"~l-fvr'i':-'*' S s /^\

ll'-W "

Foreman,' A *

Commercial Company, Limited,51

MINING EXPLORATION DEPARTMENT,

V^-^ft^-^mmtJiti i

:"/^

'Dal*.

Sf 0l

~~iL-

3

"-*CriptIo*l of'Jit .-..

Shift.

Day.

Ni,hu

Day.

Nifc-hL

Day.

Nil**-

Day.

Nifht.

Day.

Xurki.

Day.

Nilht.

Hay.

Night.

Depth from

-

n/' nW . (ft*Jb±. . ,.

Stand Pip* 1 lurried.

FL la.

*

J

" "

WEEK ENDING......'^- S"s

Reamed for

Ft. la.

. Kind of Knck.

DriUed.

Pu In.

x^X^

X^

t^X

tf--7- ——

J?3if"If - --

Hair.

*

Cm ReoovrreJ.

Fi. la.c/"

ti~

/X

f/

t

flf

S

/yAJx

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rt i*.

/j?7//P?2AJLt y?Z?7j[ggj//335jj-f

*fc

^/V-L

4.,^.^!.,.. .490/5X

UAtnal Delay*.

Hre. Ma.

Kl Now

x/

xxx

xxxx

Carbo* Waata.

Kta.

— . ———

—————

Cause of Delay*.

'---•- ——— ——

..-- ——

- ———

-.— --— .— —

—— ---- — —

,

ll

iDay runner, P rO4

CNight runner,

Foreman. /Y *

l

Algoma Commercial Company, Limited,52


WEEK ENDING. .. .,..#*-*Z .....~4L .Z,,. .....190 ft...

i SMfi.

Tip

PL In, PL

tot

1*.

DrilWd. PL I.. Pt. lo.

Tout tVptk.

PL U

BH No.

Kta.

li*.

t

t l

1

D.,.

. f

——__-- -i-vl—-J l.. . .. — ^ . -. - j*—,— ———

j:-ji

JL

|EL-'jif-

t11

-

IVpili from Kind c-f Kock. C*UM* rf i VI* y*.

9 ^'.

i fi'u ^ y-t ?f t*

Day runner,

Night runner,

Foreman,

'fit*

's/

Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

'fei^f-p)1^

1i'Jfrc*.

B-

f

t lf^H

1

1

i i i4

1

1

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- —

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.

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NlrfcL

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Kl^t

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Ni,fcL

D.y.

NfrM

Day.

NijfliL

Day.

Ni*M.

Day.

Night.

DcpOi fromr" '-~- "-~~

!

1

1 1

1 1

i

Surwl Pin* IrM*rW.

PL I..

WEEK ENDINO..-.-.^*.^^7

Rumtd for Citing.

PL la.

— ~l ----

i

. - .

Kind o/ K o*" k.

i

. 1

•- ••-~

DrOUd.

PL l*.

*

Ci*. -RccpWTwL

PL la.

,,,,

il

1

ToUl Drplk.

PL la.

——— ^ —

—

d^....S..f-....-. ~.. . 190 5.

VnuuJ rVUy*.

Mr*. Mk.

BHCarbo* WaM*

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-, ——— . — -.-

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J/*-— ——

^/7

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^ yv"-" "- V2-*

f'-"

•- —-

-- — -

———————— —

, . .— . — . - --- - - - -- - - - -- ——

———————— -- —

Day runner,

Night runner,

Foreman, . . .. . ,

' .. . .a. Commercial Company, Limited,

541


WEEK ENDING.....^**^.......ff..C. 490 J

Day runner, ^tK'W-^ t^-^W

. . , , - - - , ,Algoma Commercial Company, Limited' '

55


s*-/'

lri

wmSif

,-: - ,-; ft.

'tyPj,

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fm,.

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fej^tot*

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—

f*

, jLjit; u xi^waiAd VÛAXXJLJIJI^JL \jiax vûiiiâxiy,


. (yWtfc^Ko^(fifcr-^L# WEEK ENDING ..... ....^^

1 Stand Pip. InwrtcJ.

Ft. In.

Pay.

Nirht.

O.y.

Kiirtit.

n,y.Nifht.

Pay.

XigM.

Pay.

1 "KM.

! Night.

\ .SE1

— —————

. - .

i

j

Rumed lor Cuuf.

Ft. In.

——————

1

i

'

Kind of Kock.

*-5"t. . i j Jt f

ir c~DrObd. Recover**,

Ft. In. |J rt. In.

——

l?

tf

—

\ —

r33^^t

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— fl-.- - .

1!—..

IUI*.

w.

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. —

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*

1

X Js&is

> J^.Q t wo !^

Bit

p.

s

ftii

^—HWe..?

ic^ ;:\

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xa-/

iii i i i i il

P^^^^-C

X 7tx

f ^ '

Nijh runner.

Foreman,

'-: ^" -'

te^TK* Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT,

- .

57

liJS;

—— ; ; ' '

t

*

1

1

!i i i i i iti i

^m

riK afe

.

f

'H-^':-' . ;^'^ ;7 ' ' . •" :jl.-:. V .' ' " -' ' '••'.•'•'" - ; .-,': -: '"' ' .' "'•••' ~-".; j'wfiiVv-'.""' " : "-.--:. •'•.'••,:.--':;-,- '' ' . ' ' ' : ; -" .' ' - ' -' rrOV;^Kxi:V.''-':''~ :' . . .- - -' ' - ' - - ' ' " - ; ' " - ;- - ,/ ; OorTlie Algoma Commerdal Company, Limited, "

MINING EXPLOITATION DEPARTMENT.

•; ./o A i V^^-e^-^Ti-T^ x^*ix*-o~i/

DaU.; i j

V7,y/1

x?^.2

?

vi of

LS1^-'

0

1 1

,

\

p (75*^

\' SUft.

i Pay.

n,y.i Nijht,

Day.

' Ntf KLPar.

' Niffbl.

Uay.

! Nitlkt.

Day.

Ni|(ht.

| Day.

, Niichl.

1 1 from 1 Kurfacr.

i:

iii 1

I

'

;

- '

Stand PIP. ' Intcnot

Ft. I*.

i

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^

C/5

,

- Reamtd for

Fi. la.

|

1

i

.

iiiii

f

———— J ———

WEEK END

DriOmL

PL In.

V

2XX

J

*yV

^ij

!

. -. . Kind of Kock

1L

1 f sf'

i ; j h--

/7

i

Cor* Recovered.

PL la.

——————— j —————

X7

xx- ,J

f

4*XING......... (Zu^fr. . ,.-?.A......... .. . . .J90*

Total Depth. Vnu*al Dday*. Bit

Ft. la. Hr* Mi^ NlK

7// /\ \

7/V ty/ C- ! i7/7

7^-V /7 p.f x7^/ y73* 17.37 ! X

^T

Carbo. Wart*

Kta.

C*om: of Dclayik. t

foa^-^^^f *-t*J —— -I^r-Sf^1

tt/ As^~f-1***-~4 f-t*-sT -^T—^f.

irsi -' -4 - -.'

i; ^Day runner, s / *-\ ^^L~^ — -* — ^

Night runner, S/ ^'^* f/ff/i^-^' ~''i-^Cf

Foreman, ^^^~~ '

Algoma Commercial Company, Limited,\ ;v ' - .MINING EXPLORATION DEPARTMENT.

59

^?®;-/i|p,r.L

|•'^-

*.

4llJ

D.U.

^^

^'

X

^ 7

rf

rf

. , -, ....yi|........^-7-*v-^T*—''-*^-c— *v- ••••" *

7 ^J J,:

Shift.

IHy.

N-ieM.

D.y.

XltchL

IHy.

Nirtt.

D.y.

Nirtt.

D.y.

l "'y.! Night.

l n.y.NfcM

. . . | i IVpOi

IB*- ^i 'j?"1

ii i

1i 1

\

i ir

1t

j/V-

1

1

Sun4 FIM Rc*mrd for Inverted. Cfc*lnj.

Fi. In. Pt. In.

t

i

l

1 '"~1 " " ' *

" i - i-i i

Kind of Hot It.

i

i

l

WEEK ENDING.. .. jZ2**

Mttel

Fi In.

fyJ

3

fy

'

n,.

1 :

l

i

Cora RccovcfgJ.

Pi 1*.

t

0

ToU) DcpOk

' FL l*.

7tff/f*/

Z/7-Af

Jf/'^?\

'li

*^ r*

-rfd^

Vnuu) Dday..

Hra. MM.

f **~*

Brt '

Ka

yx,

X

™H

Kb.

————— ———

r-—————

i

1ii*t——— 1i

*~""* ,1

— -- ———

Day runner, . /^^ ^^^^-^

Night' ru4^x)W ^ ^^a-^*^

Foreman, c-SI.™*-^?^*'

li^fî^-f-:^^' '--.':

^fFtie Algoma Commercial Company, Limited,' i; -'' ' -,; : MINING EXPLORATION DEPARTMENT.

.........At,,...,.190mvmj^,..;....^./...-^^.**:!:........-...?..^...... - *~ . — ,VM ,V .-^,.—...,. ..^ ..- . ——— ..-. ........,,, ..^ ,

îi ri

t::' .' ''

Date.

fl

ti

^ /'

^

Sj

ShtfL

D.y.

Xiirtit.

n,r.Nichl.

I*,r.

Xilkt.

D,y.

Nirhi.

D.y.

Nighi.

Hay.

Nirku

l).y

Nigkl.

i-" II IS?j**' J l .urfAW.

i

f1

i

ii i

^

r* : 'i

i

; 1

j:

i

Sund Pip* . InwrudT

FL 1*.

^

^T-

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iii

Re*n*4C.w.1

FL

fo,r-

In.

1

j^. i 11 1

4—i-

Kind 0* Xnck.

xKkV'Cxx^'

| / r^4i

1

DnlM.

Fi. In.

/^7/^?/a/o

-^3U^'^•^L CuA

D*IC

tt 1

•- Co~ RecovrmL

FL U.

,^

9^'

^ -^ ^rr^ff

Teul Depth. PL lo.

. S.?3030(/OS'O*y

Unuul Delays

lin. - M-.

Bk N*

X

C*rt*M Wwu.

Kta.

- S *

CatiM. of IMajn.

.yI-et-^v

rV â ^ ^ ' ^

s ,

i

1

l1

{ tffr -r jtf~ 'Day runner, LS&^t^f XV/-P-V-C-O

Night runner,

Foreman,

1,"^1. U.B

W Tne Algoma Commercial Company, Limited,11^.'-"--'"--'--;"" - . ' -

fei"'. ~ MINING EXPLORATION DEPARTMENT.

:- tf^^Jb.. WEEK ENDING..

•7"•,c

f

1

1ur*.

1

1

1•^'Ti'Si

r i i i i i im

Date.

fO

ti

irii'b

yrf

on of.

SMft.

Day.

NifhL

Day.

NithL

Day.

N'iftiL

Day.

Nifht.

Day,

NiifKt.

Day.

NiKkL

Hay.

K*L

IVpln

I " J ' ^

1

1

i

li li i

Stand rip* IntrrUd.

Ft. lv.

t

Rt.med for Ca*inf.

FL I*.

.

j

i

Kind of Knelt.

^

UsL*^s

DriOcd.

FL ID.

B

H,/2*

X3/(f/f/y/*ji

/j*

J*j

IlaU.

Cora Kecovrrad.

Fi. I*,

2^?s

qt?

93^t/xx't-

Total IVjrt..

FL I*.

^"S

79

/oyf 2- o/2//t/ i./Co/C#JJ^L.

/W303

Hn. MM.

Bit No.

f

s

fxx

xz.1

^T 1

Cau*r of Drlay*.

—————————

'

—— ——— . ———

————

Day runner, 6-^v r 2 (*-~~Z*^*--iZsf

Night runner. ^ 'O f-^f/O A -^*-C-

"3/ X*

1^*

Foreman.

(7l

l -'-"

iBI^P^^^rL^'^C 1 -. ''""' :'; '.'-' ' '•"•s,-v - -' Algoma Commercial Company, Limited,


25

il?"^-.?;.' 1/'.. - V .-'

;,--t**i ;V*'-'.. '

*w^ M--- ^it-^:.

Na.V. ff

WEEK

1-on.

I

rrL l

IHi*.

/7

x//^^0

?*31

SKA.

D.y.

Nigta-

Day.

NickL

n.y.Nfcfct.

D.y.

Nirta.

tiny.

Night.

Pay.

Night.

NiKhl.

"" li IVpth' ^U"*C*-

f j

Sand Pipe Inwrud

FL In.

.

:

KeiRud lor

PL In.

Kind of KixV

DnTUd. FL In.

rsi

—liJ*

9/3

^ML't—~

Date.

Core

FL U.

^

2,),

7Is

Jist'

C6'^j.

ToUl Dcptk. FL I*.

jLft

L?33Z VJ2 j- 5^/3

^.21-

^J'

3/tf3^^'

^

lin. Mi*.

-

BkNo.

xx

xx^t

1

wr

—

Cauv of Dclayt.

——— -- — — - ——— - — -

-

l l

J

l lr

Day runner

Night runner,

Foreman.

-

, \JJjtstS \S



m&.'^.ffa+'te* A^A*. , ., L. WEEK ENDING....... -Cd* JV ' j

i1l•^-li- i*-*a*-—

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}

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^v^J'

e^V

^7

P

f

oaoT

Shift.

n.y.Nilfnt*

I'By.

Niyhl.

Day.

Nijbt

Day.

NiyhU^

Day.

Night.

Day.

Night.

J*ay.

NigKl

l)cpth fromf™;

j

!

Slam) Pine InwttnL

Pt. I*.

*

1

t

Rramed (or

Pi. la. PL IA.

XI-

23

/^

Jo

^0If

\r i /y M^

"kind of Knrk.

j..... ,,

r ii-i!

|

Cora Rvoovrrvd.

Fi. lo.

6'

X>

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#

^

f

^

^

V

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Total DrptV

Pi. I*.

fy fa (fjf tf Q

S/ 4 6'Wf.

*jk3'f?76'0 2-rxrJV5/3'ljj'

i y6 1)

*

^0f^

^....•2. /T ,.,...,......490^y

Uflutal IMayt,

Hra. MM.

Bk No.

X

x

^xx

x

r.

Cart.*

Xta.

i

Cau** of i^U)-ft.

-

-- - - --

li

l i i

Day runner,

Night runner

f3/. fForeman, c- r ^ u

.- , . - t . tAlgoma Commercial Company, Limited, 27


, ^/-/'•--^-- ifer-

1—^ **j^ f-1*" WEEK ENDING....... ..S^^f^L...^....™......^... .490 3fc•H*-™ ' •••••"' f ——

1

1

1

t

1

1jjSrl

11

1

1

1

DM*

J/

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.

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M Of

Shift.

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N.Ehc

D.y.

^lf nt.

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Hh fn

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f y ' ~

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i!

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Ft- I..

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Ft. In. l! Ft. IB.

| . /f)1

i. , rii iiii

ii

/ b' /Kg"2"

ZPA'4-5'6'

- 4 -6 '~ r 4" — ;-"1-

Kind o( K.vk. l! W*.1

~^ty JPPjf't ^f-*^'f*^fu•-•l ., f tl . 'S~:/ /'" ' ' / ' " '

' ; m

V1;

- Cor. Rccovcnd.

Fl 1*.

3

3

/ysfs

/t1'3

3^

ToUl Drptk

FL la.

*i?0•yj*(,6 j CL6,/fbs*-/(r/ ^t*/6?lZ69 'fzlfCi/'(tJSdf

Unuul DcUyv

Hn. MU.

f/

f

t

f

Bk No.

Wwu.

*

C*u*c of IVtayh.

—, — .

' -

- - — — —

...... ——— ...—— . - .

- — -"" — -.---

———————————

—— -

.. ..- —

Day runner. C/^-f^^ ^ O^rt^-

... . S~} Sisr -^^fj f JT J f SS

l lt

Foreman.0

li

; x ^, {.''j l'

. ( . Algoma Commercial Company, Limited,


WEEK ENDING.-.-...-^.V5^-^--—-—". -490 JC

^

1

1

1

1

l

1npi lolt

I

D.I*

7,^fX//x -

/^

.vi of,

SWft.

IHy.

.••iltfct.

D.,.

Ni,kt.

lUy.

N.^,1.

D.y.

NifSt.

D.,.

Ni,M.

Day.

Xifhl.

Day.

Night.

IVplh

1

i1

Stand rip*

Pt. la.

t

l

"I "

....—..

Reamed for Cuin(.

Pt. IB.

I

|1

!'

Kind of Knck.

^'tt^^fjf '

DrDUA

Pt. U

~f'

VVy/y^

V3t/j3

Date.

t

Cora Recovered.

Ft. IB.

f

2,

^

//

0

0

fiV0

ToUl Drptk.

Fi. l.,'

li-o

C boUtiff6?}"C 7 V^7/fjj/fx6^JCMf, g/

.

Unuul Delay*. Mn. Mi*.

Bil No.

X

xxX

X/

Xx7

Cartn WM*.

Kta. j

i———— ———

Cautc of IVlay..

-

——————————— ...- ———— .— . ———— , . —— .— ———————————— ——————————

. , . . ....

l

i i i i

Day runnrr, .

Foieman.

. - - , , Algoma Commercial Company, Limited

' ^^

29

MINING EXPLORATION DEPARTMENT

Day runner.

Night runner

lillie Algoma Commercial Company, Limited, 30


.At

WEEK ENDING-..

DM* Shift.

Sum] Pipe InwrlaL

r1 1. IB.

Ke*nx4 for C*iin(.

PL 1".

Drilfed.

PL lo

•- Cor* Recovered.

PL l*.Total Depth. PL la.

Unuul Delay* Hr^ Mi*.

M *"

Carbon Wawa.

Kto.

D.y.

Day.

iOay.

JLDay.

..J-

-SU "i'o

Niyht.l*Kind of Knck. Dale. nf IVeby*.

Day runner.

Night runner,

Foreman, V' 0 c

l lice.

Ir The Algoma Commercial Company, Limited, 31


gm ....A.........



'.•vc./v-.A^***exA

WEEK ENDING.... .-....^:^!:.f^V.....^.L...™.- . ..190 *~

Shift

Stud Pitud ip* Uterud

FL

Reuncd for C*Mf.

Ft 1*.

DrflfcJ.

Ft 1*

Cm lUcowrad.

1*.

Total DrpOk

Ft In

VKUM! Delay*. Hm. Mm.

KtCarWM Waau.

K*.

Day.

NifkU

73*?

Day.

li.Day.

(fL-L 5isht-75-7

Day. JL.-5^

l)ay.

Hay.

...|..^a,-J7-S3L

Ji-

h;Caui* of

Day runner,

Night runner.

Foreman.

S >xOxO o

O y^ no.

I'tii

Commercial Company, Limited,33


Day runner,

Night runner,

Foreman,

i 1jP *|

'

J1 11 l

~I?oif

j1

1

1

1

1

j

ipi^V^r-^ . • v . r .:; ; ..-. ; . . - o/f •?jv*;c • •-•-.t - '•••'•' •••- - ••.- -. . " ' OTC||;The; Algoma Commercial Company, Limited,*. MINING EXPLORATION DEPARTMENT.

^ \ a . o IP- 'ite.^~li . .../.'-At **- O-'ir^K \As*\t^ . .. ... ...... :,T-V;'".'." . - .

n.ta.^

30

——J

m i a

1

7 ,

3

^

0. ...,....... ...... ^y . .. . ........,

Sluft.

Day.

Nvht

Djy.

Kijcbl.

0*y.

Nnrfci.IHy.

Nifht.

D,y .

Kicht.

I).X.

NU*.

ij .S.— >

— *

—

—

I

| (

i

i o '^ ' -

** C) ' -vv

Sund Pir* Rc*mtd for InMrrtoo. Cavuif.

Ft. 1* Fu In.

i

~" tI '

Kind uf Knrk.

s p Q -JKK'\I fV J\t fÂf **^tAA^ ' ^*O lT J

t/ f f\ f\.t * "7 O A * i

0,^t *?CVP^5/! '7 'C -, T1 'V 7QC' \ J'/xrr-*/^^**^ rio J ; x

; /

/-^ r S'-"^ i. v^;"*-*—— ^-'

j i

DrOW. Pt. 1*.

3,

a.r c.a.4

1; t.•i 4-J.3JL (^

,v,t.

i!

WEEK ENDING...... .......^^^.^r^.ûA/...,/*-..:. .. ...i?0 A..

Core Ctrto* ^ Kccnvtrad. ToUl Depth. Uiiuul DrUjr^. Bit WMW.Ft. la. Pt. lo. Hn. Mw. * Ku.

1 y l TP-7 X 7 l, I ft f (e

10 la 18*1 l.t Til a si

A 7 *75' 79^ i' 7*?t 1

4 7*77 4 l5. geo I

L Sol ' f; JT03 i1 Sou l*.

e—— ,M^

:

ij)LV^î'/ OtxjL lUC/OvjG'xvm/^tlir^•T*wTc !±^:fc" w^T/'"^^,y

------

i

titThe Algoma Commercial Company, Limited,


35

••*. !"Vi',* • ~'.:

WEEK

l

r i

Date.

J3.lo.M.

Shift.

Day.

D.y.

Kifhu

Xight.

Sun] Tip* InKrtol

Ft U.

lob.IVpth from

l

l

l

l

l

l

l

i

ReamnI forCa*inf.

Ft. U.

-l-

DritlnL Pi. In.

Kind fi K ncV.

Con

Ft. l*Tool Ft In.

UnuMl Dcby*.

lin. Mil.

JLtL

toJJDL

J.O.O.

'O

BilNo.

Carto. Wu

Kb

C*uv of

"Vpu. "7. .

l O11

-OnZl^oiiic^ l

Day runner,

Night runner,

Foreman,

n

Algoma Commercial Company, Limited,- ^ F 's,;

Ip^v

I wSJ* *5l

Jyi^"

fit11tr1 1,

ii

l ii r i i i i

S MINING EXI•-.'•.'.•'•fi 1---- ' -il^:l ef

X-.-' 1 ' -'

Date.

/^'/f-

.—

/4

^

Shift.

l).y.

Nifht.

Day.

Ni,J,L

lUy.

Ni,kL

Day.

Nlfku

Day.

NirHt.Day.

Nirhu

j l ja)

Kl^

"" i H.**—

i

,

.

**.- t

f

t 1

J 1

li

S .T a1

Stand flat R ramn) for Innrrtod. Caunr-

FL 1*. FL In.

••""t~ - —————

- - j- T"

|l i

i ~;Kind of Knck

A. J C iv*.* U f^ KV*lC.

C (l C

*7 t/ ^

c (K*m/ 6 AC

V5 U 'i^vctf , . .

fi-4. i f^i^J

t ^

1 C '/f ^- * v t".

C /c.,,./,

T. '.RATION DEPARTMENT. : , H

TETCCV cwniMr- f\.Gw*n*MtJi/ i S i on i" ^.1

IMDed.

Ft. lo.

d

/^La.^^,

to/o

'/r-

?O

-4-4

^4

Date.

^1 5

Oo ^^v o•! ^ v~"

Cora Carbo. |H Rccovmd. Total Drftk. UmuaJ Delay*. Bit WaM*. ^H

No. ^H Ft. la. Ft. In. Hn. MM. Ku. H

; ^/s d, 1t Sa.^ Q

' 5-^9 ' 1^^6" l

L, 8kS \15" S56T 13 4^ ,S"fc7 ;1" 55/ t 1A 57^. ]

*

i- -- - - ~ - ~ - - J L

C*ux of IVUy*.

..JL^^^f^t^A^^.^^^^^ j~- ' j

.

11 .. . . .. . li ~ j - ^ jDay runner, 7 . 0/o.A/vt'n^ C^tc l

nr"' ^ ^-, vr c



t sn....Ai........

WEEK ENDING....... ....^T^fL /..^........ ....... . .490^",'

suh-SUnd Pip*

lnwrtcdlPi. la.

Runwd for Cauny.

Ft. I..prided.

Pt. In.

Con Rcoovmd.

Pt U.

/X

Tout Dcptk. Ft. t*.

Unuul DrUya. Mn. Mte.

Bil NIK

Wuu. Ku.

I H

3j&ri Nighl. JJ1L.

li ); NifM. /f

iDay. /j'

Nieht.

-f-w —i from

l

Ii i\ii

Kind of Kock.

IfDate uw of Delay*.

Day runner.

Nighl runner.

Foreman.

f

-( J?

/J-/.'7

••Algoma Commercial Company, Limited, :^H|S i MINING EXPLORATION DEPARTMENT.

I is •nr,^'- 1^ .' . ^ ' ^•''*f ' ' " ' "- i ' - ^^f~. *\ *

l- 1i"t,;:f1

-

ri• Holi('

jl

1

1

rr--:-v - .......,... .... ^ ..- y

Ma f/flExt^-* j\f~^f

Dale-

/v/r

yy C2.7"'i

KM* Of

Shft.

Day.

Ni(ht.

Day.

Kitnt.

Pay.

Ni(t,L

Day.

N'itM.

Day.

NiehuJ)ay.

Ki,ht

Day.

X^.

from vurfjicr.

1

i

i

1 ii i

Stand Tip* Reamed fer InwrUA. Cating.

PL In, Ft. la.

. . j . .

1

Kind of Knk.

k

1

1 c fl

i!

IMUnL Pu In.

/fi. '

?L0X Vy 6/^S 6J-03 (j^ ../yJ?y /

//^

i;

ii

WEEK ENDING _ C^*^^!! ../..jt.~... ... . . .. .. 190 8*" .''

Con Carton Recovrred. Total DcjKk Unuul DeUyv Bk WaaM.Pu In Pt. In. lira. Mill. "" Kla.

/ /SZ

/ /St XS X00\ X

•3 A/k /yy ^?^i /J X '/^ 2#t/ f

(* \3tt/- f/f \j.rt//7 2 0{/ fl/ 3/ *?J' 2^ '

*y

Cauw of Delays

.

Day runner, /f ^^ ^^ \-A.-\J ^~

VQ, y a i ^Night runner. A' y ifS sl''r~ * sL-^l? .

Foreman, v " ' '.* ''- -* - (- - -i :- ,

L

Algoma Commercial Company, Limited,

- -

62.


RiftNf.r."

•"f^ 0"

RS* -T'^'-'t

l1-

- *M*.INn.ri'"T?,ii ii ii t

-

ST

/l '

Date. j Shift.H

——————

Ml of

——— "

'

j "*y.J Kickt

Day.

KickL

D.y.

Nigt.1

t D*y.1

Ki^hU

| i*y.Ni(ht.

l D*y.

i NiKht.

—————————— |T- —— - ————— — ———

[A.

iiiiii!ii

Sund Tip* Rnuncd for InnertM. C*un(.

FL lit. Fi. 1*.

* i

1 J

j1 l

lil,

Kind of Krck.

i

j.

...... J,.......- ,,sQjCJi. . sl^n-tfc.

WEEK END

DiilUL

Fi. la.

lute.

lil

1

Corrp -fa, u- - ,.ilKOTPTCnM.

Ft. U

(e!4tNG................. .... .........,.............. -.....^...-.. -. -190 --

Toul Drptk. Ft. 1*.

~'

U.i-jJ DtJjiym. Hra. Mm.

- — ———

Kt No.

Cirtua

Kte.

Cautr of PeUym.

-- -

— — ... ———

Day runner,

Night runner,

Foreman, - .

SiS^-:'"" .: - r; ' ' ' , - ' ' : " " , , 65gjTtie Algoma Commercial Company, Limited,


WEEK ENDING..... ^Dxu.

&Z.

Shift

P*y.Night.

SUM! Pip* Inwrtol

PL U.

Rrunnl for Cai'uif. '

Ft. IB.

DfOlnL

PL U

Con Ruxnrmd.

Pi 1

Tout Dcyik.

PL In.

Umuwl May*. Hn. Ma.

Kt No.

Kta.

NifkL

D.y.

ri.

i

1

J^L-J^ithl.

U.y.

Night./O

Pay.

Kiyhi.

|^5Piton of *.

i i

IVpth from Kind of K.x-k. Hitc. of IVUyt.

O

-55^J

35.74,

/pV. .*

JixiziXSZ.

l

i- ' 4

VlIT

Day runner,

Nighi runner,

Foreman,

Algoma Gommer dial Company, Limited,MINING EXPLORATION DEPARTMENT.

66

^ 36 Q ^tdLfa^tfcp^.... ......At,^*^

ife C/B ~~

l1 1i iijjiii ii il

iti \\ \

D.U.

". - *-JE

*0

^

ISâoai

,..A

;"'onpf

;

1

1

1\

1

1r

i i

1

•——T-*

Shift.

Itajr.

Nicht

D.,.

NlMfct

U.r.

NitkLD.Y.

Da}-.

Night.

Ni([ht.

Depth from

ii

l,

i

'i 1.5 S

Sum) Pipe IfMcrtnl.

Pi. U.

^

I

-— --

Reamed for doing.

PL In.DiHknL

Ft. la.

'A,

/(,

^0

so50

.20

i!Kind of Ktx-k.

t

/o * ' ^

i

,,t.

i

' Cor.R *,-,n,,~m*A oCOVCfPO.

Pi. la.

7

^*?

-Jî,V1

^

J

^

^

ToUl Drpth. FL la.

^4^2-

-a.75.355

u\S

it- A S

h SG

Uninal DrUy*. Hra. Mn.

Bk No.

Cut** WMU.

Ku.

Cauv of DrLiyn.

— --

. ——— -

-

- ————

-...

.... .

— ————— —

i j

Day runner, l'CCiJ'*v'tC **y

Night runner, ^ (T^Foreman, - Ô/M t-(C .

Htejinie^

||p:., -. ......

ir'ir ii••uripti

)loW

)j

1

i

D.U. Shift.

i I**y-/4- Night.

l Day-

- 5" j NifM.

Day.

^ NiltnU

Day.

*7 Niifht

Hay.

ft Night.

Hay.

fl Ij Nixht.

ll.y.

Night.

" rf i Si

li

i 1'

t

---? sni 1:

!

*;.iu.'

'-; -.r:'- . i -- . . - . - - V'BB6?m

AJgoma Gommercial Company, Limited, B~ ' - ^B

MINING EXPLORATION DEPARTMENT. ^B

Q*a*jt#M ^BAl~" ' j ^ B" WEEK PNniNR /erfLAAC^v^*^ *3 ' 1QO& ^^B

Stand Pip* Rfjimtd 1*9 InvnnL fi. i. ig.

Pt. U. Tt. I n.

! 1

L J

t "-!! i' 1

ir~

Kind of Kivk.

fi *~—

i

DrObd.

Ft In.

/ft

'P,

Q

/.O

tl

/5

(J

#

^

D.lr

CP

;

Con ' * Carbo* ^^Hi Recovered. ToUl DcpUk Vnual Delay*. Bit Wuw. ^^^B

Ft. l*. Ft. In. Mn. MM. ^ Ku. ^^H

K t, 1+-IO ^B

i /,^l Ô a^B

/f- 4 ^TOf ^B

;,. s ix, 1 ^Bt, d f3^* ^^B———— V. ———— ——————— ———— ——————— ———— ———— ——————— ———— ^M

^ ^6, ^B^ 5*//.^ ^^B; 5/^s ^HA ^ .55*3- i ^H

E B—.-.—J- ^ JCJIUMC of 3)cU)i*. ^^^^H

*Oi-T 4) CA-MT ^- ^ *v*v x-^Vw/v/ ^^^^BHW'C^CtA C^V^r ClA^tx/ rv^. 3 tP^ a^B

. 0 ô .c.0. .. . . * —— -^HJfJJf/^^r^ tAî CX-ttJt ^J/ •^•^•^•^

' ; d/^^.j./A. ^jL^*,^ -o/-,/ vL',/- ^H! "' ^ ' H

i/C^-f/0 /S.V^r^^ n J" 3 1^'^ *j*-f?..f* ^H

ôtx^^x^^Q^ J&a^yd^^^f-s^**. —— B

^BDay lunncr, ' (\ff.t\l *-xCL ^^^H

) ^HNight runner, ^ { Cf\J ^••fCto.y ^^H

Foreman. 6. ^ -^ r ' -.; H! . ^B

" ' ^^B

Wkw

ii?-"x;*-';The Algoma Commercial Company, Limited,


69

... .At•^Hv'-1*' .' '*(•kn No.^••'" -- -

±~

t .

Tut*,

*i

TPrl.i i

^ ^ 7Pal*.

^

t

^w

/A;

— iiSt'T"*'

1ii ii iiife

-

i t

tt^

Shift.D*y.Nirht-Day.

Night

l).y.

Night.

D.y.

" NilfKl.

Day.

Night.

l).,.

1 NiKhL

H2r

Sund Pip* Inwrud

Ft. In.

——

Ke*nud for

Ft. U.

---!

II " '' jl from , K iftd ^f H nclt

1 1,- *

i 5T^l

j

i i ii

i

P r

ii

ii li

it i

L

DriOnL

Ft. In.^~

tg-

^- -4..^(5/;s

.5- — |/o7 j

u*.

i^y 33,

i

!

WEEKENDING *K dfc****, *** m*-I

Recovered. Toul Depth. Ft. In. j! FL I..

li 1 ^GPfi IT **2V5S Sf^4-** (o ^ 02, ja LO-] L5 LI S L

** 1 fr-25 6

'7 t.V, LA i /fci. 4/ L SD L

2. L S H t.3 t/.^ t' L I! ^

UnuuJ DrUyv

Hra. MM.

5"

Ki No.

Ccrln* Wwu.

Xta.

Cau-* of IJeUyi.

———————— .

ifc**! o/tiT" 3 tf^v tot*\t-^vxA*^g \*sc(?'ayCCtA^^v V/9 ^y 7

—XXAAX^

- —— -—

^

f )

wV?e^--"

: /-i /^ jDay luiincr, l A. ^p7" J o-t^.C CVA.

^ ,. i/ M^ r"* y *k /? —Nighl runner, 7 ^ ' **^ v l l/^-vv ttx*.

Foreman, ^-' rt "7 l* r ' -'

IfIfHie Algoma Commercial Company, Limited,7C

fSvl'Sv'-


^ oVi Q PP- s No,., .5 O ....At . ^ ^o^l Ax/vv*:.

WEEK ENDING... •49CN

Pat*. SMfL

Con Ricovtrad.

FL In.ToUl Drpth. Fi. lo.

Umiul tWfay*.

Hn. Mi*.

Cvtm Wwta.

Kb.

rl**/-- ' 1

u-j^a

•705

Day.

Ji

f Tt. .Jk 730

' Ni^fcl.

IVvnptkxi of Hole. from

t !

Kind ft Rock

ut X^

D.lc auv of Dclaym.

- /d -^*y . .Day lunncr. y" t.'J r^/i/x trcryry 7

Nighl runner, ' M..^"' J O-M. (o*y

Foreman. ? ^ ,-t

' ;- - - ,Algoma Commercial Company, Limited,

71


iII -^ * -|

jiIFne*. -

1

ri.

1

l

Daw.

~

E^nôr

1

i ii i i1 i

r

. —

3JL-

6"

(o

-*

! Stand Pipe

Shift. 1 Pi. U

i "*"

i Day.

îfnC

n,,11 Hay.

j Kiffct.

! Day.

i Day.

i XiKbl.

Nifht.

;| ivprt.' fnon .j ikiirfArr.

î i!

\

''

—-—•— —

PI 1.

;1

ii

i

Drilled.

Fi. 1"

g

Sy

V*

g4

i ft•j—- j -

i,~- - - p-~Kind ..f Kock

j

t

"~-

!-

Core Recovered.

Fu I..

^

If.

/fei

f?J

^Tr

-—— -

Total Depth.

PL IK

752,

J?**^7*7'779

L2.9^SCD

Unuial Drlay*. lin. ;. M-u

"*i.4rj|d-. ^

"~#,;-~— - - *

-I-1Z

1

y,.,,A- -

fi wLw.

CaiiMf of IVlayfc.

—————— ,

^v^^T?C**

—— -

id* n ^tr ft

— — .....

G w1

J

Day lunner, ^ ^ Cr-' ^vi^cuy

Nighi runner, Y" ^ xA/i. tûc; ^^k p-n L-Foreman, ^ •--••yiAC Vv^.,

The Algoma Commercial Company, LimitedMINING EXPLORATION DEPARTMENT.

37

INcv -

..190 *T

ft.ilfrt.

1

l

1

: '. ;"mtfc

30

51**Jteri

4 f

5. r/:

}6~

Stull.

n*ir.Ni,ht

i D.y.

l D*jf.

j Xirlrt.

i l*y.KirSu

IUy.

l Xi^ht.

i—.'-^JL.-.

Djiy.

' Sif hi.

5s-- ;! S.J

H

1 1

t

ii i

s

1

ii

i

|i

r

i

1

Fi.

—x. ——

2rIn.

—— ——

j..-..

KcanrJ for Cuin(.

Ft t*.

-

1

1

Kind of K nek.

jii 1

)

!

,FL la-

Pate.

l

l!|i

j

Cw.

FL I..Tout Drp*. Ft U Hn. Mk.

Kt No.

Corbo* Wuu.

V*A 1J•-

C^oT.VUy.

*i**

T-VV*JLtki-.

--- —

- "7-r^W f.

(TOJLV

i.*. .te

- - -- — -

ctAx^jC

^rt? J/^Cc. ^Q

— - . ——— - ——— .

———

—— .... — .... —— ..

Day runner,

Night runner, . . .

s OForeman, -J - " ^J/'*- 1 ^ . ,.

J|ll,'-i-Jwr.;-'.- ~

I^The Algoma Commercial Company, Limited,MINING EXPLORATION DEPARTMENT.

38

•^T::imNa

il;1f^r*.ii

t

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from *urf*cr.

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1/oy

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Ft. I..

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d^~.

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KtK.

C*u^ of IVUyv

———— — — -— :1

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Night runner.,

Foreman, O. (/

j||;OTe Algoma Commercial Company, Limited, .I ^s-^s- ' ;*'' ^ "'' ' ' - f '

40

*^uy,---** - , ;^r--'-^•Si'^^/...,::.At... 1^^


^WEEK ENDING...- ../*^*^T^.?^/.../^ ' . -J90

Shift.

Suni Pinr InxrUd

PL I..

Rumrd for C.~f.

Ft. 1*.

Drilled. PL I*

Cot.Total Dcptk.

Ft IA.

Uniiul Delays

Hn. Mk.

Brt N*.

WMM. Xto.

lNichl.

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V Qdtr^O

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l,. .......S

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l *

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Foreman,

'

^ vt.

THe Algoma Commercial Company, Limited ,I"f5W :V'.'-' - - - ^ MINING EXPLORATION DEPARTMENT.

......At..... ...Q V*vdL

41

1

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Stand rip* Inwited,

Pt. I..

r -

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Fu IB.

•- ——————

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:------

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Ft. IB.

lo10

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U9

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J

•- Co™ Recovered.

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Total Dcptk

Ft. t*.

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i

.— ——— — — - — - —1

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id cDay runner,

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Foreman,

d/ l

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^ - . v,' *" '." - ' r '-. ^^ -'... f-''

MINING EXPLORATION DEPARTMENT.s.Vtr^v-:".-'.v-.: . 'i/.''-'-' - i^,V: ;v? ' -.^Vt 1-:.,-/..'-' '

^5^--:- : ;.-- ;s^XS- : v-- . .

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PL In. Hn. MU.

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JLL.

jj1

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from Kind of Kork.

*?CO^ /X^x

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f

x/

Caux

Day runner,

Night runner,

Foreman,

l*, i:


,^'vt

llftte MINING EXPLORATION DEPARTMENT.

WEEK ENDING.

Dm*. SUA.

Sum) f if* InvrUd

Ft. IB. Pt. IB. lira. Mk.

Cmrbo,

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Jfc.

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r*

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SOI

SIS.

,i fcurffccf.Kind of K ink. Date C*u*e *-*f I Via y*,

w^

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Night runner,

Foreman,

Algoma Commercial Company, Limited,44.


p -•:AfKC ,. ...F^-.

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WEEK END!

Reamed for Caaing.

PL la.

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Kirvd of Ki^k

c' A.C>l>

Drilled.

PL la.

3

5

5

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Cow Recovered.

Pt. la.

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53

(,4.4

ti

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4

ING......... ^ M^ x...!T.CV*WU.*WV*/...../..?'. .. .......490 Co..V ^7i/

Total Deotfc.

PL la.

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5"eiO^

553..1

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t

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Bit No.

Wa.1*.

Kta.

Cauw of PeUyi.

——— ..

i

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Night runner,/ G^l/^^v C C-*?.

A ,P Foreman, ^ " "i^/tiC * ^. . .



Ijfe^.J1lt 1.•IK

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Stand Pip* InxnoL

Ft. 1*.

. -— -

——

Re*mc4CAMP

Fi.

WEEK END

(or

1*.

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Kind of K nek.

...... ,

Drilled.

Pt. lo.

77

/5T

95"

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f,~

^

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—

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Ft U.

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ING -..- ...y.aoMA!SA y., ,S**! . ... . .J90. b.. 1U- /l 1(7

Total Drpih.

Fi. In.

5?,L*7S

.5^5 4^0^(fi h

JeSLO

i&o

i/Unuul Delay*.

lin. Mia.

Bil No.

CarKoo 1 Wwu. H

""l——— 1

F1"1 I

ii

r- •••-•i

Caux- of Delays. I

—— —

]

.!j--•--•--

1i -— ---

i

i , _ ,,,. ..........—..- ... --- ... _ ..^ ....... _ |Day runner, C-C . "^ *A/ e~nxt'.*L t

Or//,.; ' f- l Night runner, ^ ^ rc Vt/^ '"Jftc ...........i

Foreman, ' ^^y^.A^f ^t^ j

i

,-v.ov-v:-:,"- •••••••: ' ' - - . - ^—-. ' ^ \fty'V: -'. , "- '- V ' .' - - " : . - ' *-v ; i . V '•Log of drill holes in' possesion of A. Goetz(Drilled by Clergue]

logged by ??50 deg

grovel ;'banded ore

liB^banded quartz and ore ?l83'banded quartz and ore j185 soapstone and shale |l'306 quartz and ore 1214 shale and soapstone 1^223 banded quartz ^285 good ore {241 quartz '248 quartz and ore

schist(depth 416)

1901. 45 d eg .

16 surface 55 siderite 70 schist 84 siderite 90 schist 95 siderite 98 schist 106 siderite •120 schist 122 siderite 165 schist 173 siderite 307 schist 337 siderite '355 schist, paint rock356 ore357 banded ore 363 ore and banded ore 395 ore 383 jasper 409 hard jasper 415 banded ore, jasper 417 good ore 420 banded ore 423 abnded ore jasper 427 quartz and pyrhotite 445 banded ore 448 ore and jasper 453 banded ore

IV462 ore 470 banded ore 473 quartz

#2. 1901. vert.•37- gravel, sand, schist. 149 w w "

#4." 1901. vert.21 water25 mud36 gravel, sand.42 ledge45 banded46 gravel47 banded49 ore54 mixed ore70 ore.no core77 soft ore84 mixed ore and pyrites88 igneous rock101 banded ore126 ore134 banded ore136 igneous rock178 ore182 banded ore195- ore'198 banded quartz206 mixed ore233 banded rock237 ore240 banded rock257 mixed ore267 quartz282 mixed ore{^ ore)296 banded(depth)

#7.1901. 45 d eg. 341 schist 343 paint rock ^77 banded ore 408 hard quartz

banded ore, quartzbanded oreorebanded oreschist

447 banded quartz 461 banded ore 468 ore476 paint rock 485 ore and paint rock 491 ore(depth 491)

1901'. vert.. 37 banded'

410421425443444

\67 banded and quartz.)

#5.1901. 45 deg. \

16 surface19 hardpan341 schist343 paint rock353 schist,paint rock371 paint rock373 schist banded397 banded ore405 banded ore408 hard quartz . .,410 quartz,ore443 banded ore446 banded quartz -457 banded ore476 rusty silica485 ore,paint rock491 ore,paint rock ^i n t#8. J 1901. 44 des.

36 gravel . . 38 gravel,schist 91 schist f 104 schist,pyrite 164 schist l 200 siderite ( J 213 schist,pyrite 240 schist,pyrite,quartz 346 " n j s iderite350 pyrite,ore351 schist l 359 flint,pyrite " 379 pyrites,Quartz 386 sideritejquartz 398 quartz J , ' 480 white quartz. - 484 green quartz ' 'm 552 white quartz^ 785 white quartz! 797 not logged (deptji

#1Q. ,9 boulders23 schist28 schist,pyrit^38 schist . -? ^ .66 pyrite, quartz .74 schist.

1901.

w^M^i^^^^.^j^Si'^/f'^V-*''.' - ;. ''':.'"- "•'•; i '- ' -'-' ' ' ,

•:^-- :'if"- . 'V'i/^V:1 ;:^-;-;^^ ";.^';;:-:' PV' : - -, Vv. i-'.'' -*'^-''C^,

A^:

schist;97 : schist, pyrite 109 schist,siderite 117 schist •137 schist,siderite '158' pyrite .mixed ore "162 schist,pyrite198 siderite199 schist,siderite 202 schist 215 schist,pyrite 241 schist,siderite 246 slate .355 schist 363 siderite 564 schist 566 schist,quartz 600 schist(depth)

#19.

726 jasper815 jasper835 ore867 ore and schist

7' of ore 892 not logged

#81.1905, 45 deg.

5 schist , quartz 321 schist,quartz 444 gneiss,quartz 485 Jasper 563 quaj-tz 630 schist

#20. 1905

470 green rock 574 greenstone 623 jasper 634 schist 679 quartzite 752 quartz,schist 890 quartzite

\ '.

'i'1i r

l i

1i J

l l l l l l l l l l l l l l l

Vhis property consists of S patented mining claims containing 183 ac re B.

JjQOAglOS* The property IB locctod 20 milos north of Hicshlpieotoxr

Harbour on the north shore of Lske 'Superior, in the District of

Alcona. A "branch ona mile in length connects with tho main lin*

of the; Algoma Central Iteilwfry. ?rora the rains to the hrirhour

\vhoro the oro docks of tho ri-ilrKy ore situated is a distance of

20 milos.

G vÛivg. Sunning through the cli'iras cro "btnds of Jasper ond

hentitito Birailar to tho various iron ranges oouth of L&ka Supsrior.

The ra joining rocks arc vr.rious c^cca eehinte of tha Keev/atin Ego,

ths v.hol,-. "bains clorely rn&li.ô^s to tho Vorr-ilion iaon rcnrre in

:. 1*1x0 cot r-.. The iroi: f or r. F t i on pt seen throuo^- "ciks I^:l:e e.

{:r.;llov. "boay of v?!:tcr -apv/erdr: ci" ht-lf a mile in length. "cvoral* *

nn'-ll irlr.nac BE well ; s tho rhorc ct "both eniln rhovv the ii-on

iTcrmrtion. ôme excellent 'oouldern of hetuc-.tito en tho rhoro firat

di j o ct e fi r. 1 1 onti on tc th e . pr ope il y .

Iln-ler ROT- rnl ov.Tiori; P.Z ftirr.onA r. 2! 11 holes

ir. '11 he ve "bum ?nit clo*.7i untie. -r tho v.-r.tcrs of l?crl:n ^rl:o. ' Those

tt tho erjrt vrA hsve iin:rly fill b^cr. rueccr.cful in locrtinj; oro.

?h" rocoaxln o^ tho: e orill V-oloK :a-e rr. follov:s:-o

Srill Hole To 7. 11^ 45O - 541 f.-.- 9 t tcv.iP-t.

"^1 - 461 " ^rr:-- 4 CI - 4C8 " Cre 'U: 9 - 4 !.'C. n ^-i.'M 40'c - 401 " fra.

c "rill Vole '/.o 12. Vi j, CD

o - f)7^ f -..-rt 574 - 665 1 : 6ST, -710 ' : Vl^ - 715 ;'

. -.r rnfl Ore

ms Drill Eolo Eo. 13. Dip 55

422 ~ 649 649 - 700700 "- 740- ' ---' . "

Drill Holo Bo 15.

f:ohiBt Banded Jasper.

' Oro. Bended.

o . Dip 64

O -455 foot Schist. 455 - - 490 "

. '-W- ..•t. M* ',".-'.\V-^ ,'*\":.N"

1ij1 "

iiiiiiiiiiiii

490 - 505D05 - 525 525 - 550550 - 570570 - 605 605 - 670

Drill Holo Ho 16.

0 - 512512 - 040G40 - 890 090 -1001

Lrill Holo lo 17.

0 - 450 45C - 77B 778 - 005003 - 935

Drill Tolo Eo 10.

0 - !i2 D525 - 600630 - 710710 - 757

Drill "olQ Jio 19.

0 - 614614 - 820828 - 8558f)3 - 892

" Oro" Schist " Cron Bended" Oro.

0Dip 60

foot Schist" Bonded" Oro . " .Schist.

0Dip 68

feet Groen Schist

" Cre. ." Schist,

0Dip 67

fcfot SciiiBt11 BrnOod. " Cro ." Bonded.

oDip 62

foot G r. en .".chiat" 3:n:iiju.11 Oro." .'•O'fiiF.'t .

' . . *TO,r l.'-.^ A vory consorv- livo efrticKto of the mount

cr^ rhov;n -JP : t tha os-:

."•'3,000 tr:-. ". -'.or^ 'l

' --:: y -- ;-\ ' ; -- ' . ;.

t onu of Ir.e liO:o "uy dirr.oiia i' rilling

: i. n J-/! :Y . :- t i!u--r. "i*!, i f; "•.jcuri j- o n V.? rv.:

•:.'- ?. ^i "-Y '.-- TO - ': -lv.', i : -, ' - :"bj.lovi

of

i i i i i i

i i i i i i i i i

f—-.. " -- -- ---- --- *;Thickness. In holo 17 the ore proved to be 25 feet in thioinaBB,

this holo wes bored at en eagle of 68 degrees, and It is bellevod, -^4'!

that the formation Is dipping at en angle of 75 degrees 4tx thoi.

opposite dirootion. Prozo this it is calculated that the thickness

of this 1)9d is only 15 foot. Similarly at hole 16 -whore 50 feet

of ore is shown up by tho drill, the thickness of tho bod la

o&loulated to be 28.6 feet. ' In holo 13, the 51 foot of ore shown

up by the drill is calculated to represent 57.9 foot. In hole 15, '

thirtyfivo foet of oro vrns pcssed through by tho drill; apparently tho ore bod is hore dipping at en yaglo of 82 dogroaa, md in the

Dane direction as the drill holo, r. thickness of 10.8 foot is

assumed. In holo 18, tho 30 feat of oro pasood through is assumed

to represent a bad 7.7 feot thick* Jlolo 16 is undor holo IS,

and averaging the tr/o TTO gdt a thickness of the bad at this point

of 53.25 feet. Eole 18 is tinder hole 15, nad BVorbing tho tv/o

v.o trot aa cvorE-go thiclrnocs at this point of 9.25 foot. Averaging

throe ihicknonsGa tho'.Tn by holes 17, 13016, md 15-18, end

g tv~ico tho valuo to IE-16 because of its middle position,t

tho rverrs3 thicknens of the v.hple "bed v;orlrs out at 22.7 feist.

Hoi^ht. , B9tr;sen tho top of tho ore in hole 13, r:nd tho bottom

of ths oro in hole 16 vhich liop ira-noclittrdy below thoro is a

vertical dirtr-nco of T91 foot, end botv;oen the top of the oro in

holo 7, md tho botton of tho ore in 18, a clirtrncs of 315 foot,

"rorr. tho r o vo hrr/c ft\ L Tore go viyovc^ hoirrht of ?00 fe'it.

?:yov:oon Iho top of tho oro in V.nlo 6, (5S4) r.nd tho bottor.i of tho

oro in holo 16, (825) there ID r v rt i cal dintmce of 491 foot.

:t ir er.-l'rcr.v.^ y rcf.ror.ru3 o to :-.i ..ODO tr..-:t tho oro r;o?r. rt le-r st

' -t \ A o:. t:.o •.i:;-' J..m of v 'loi to:.: 'rr.!! holo, ; :id 100 f-ot

l

l

l

l

l

l

l

l

l

l

l

l

l

l

l

a.th*-top on* tihioh to-ulA rwfco a vortical hoitfit of 700 feet.

tho oro rorchoo tho bottoa of tho It&o* BO only in thin troy oen tho float boulder a bo acooixntod for* It io thus eafa to count on a hoig-ht of SOO foet, tad a probable height of 700 foot* - . ' - . Txmgth,* Prom holo 17 to holo 10 io a dietcnca of slightly over 000 foot, rnd holoc 6, 15-16, pif?roed it r.bout hrlf my, and withgood oro ct "both onds, it is v.lthln tho boundo of probability thofc the oro czrtcndo ot loact mother hundrod foot each woy, o longth of lOOOfeet quito probuble.Vhie oro in hr.rd, fcirly cocrpcot, rnd nay bo trJion an n

10 cubic feet to tho ton.

GOO foot 1'JcCt by ECO f o at hi^h, by 22 feet v;lfio v•o^lld yiold

520,000 tono.

1000 foot lon^, by 7CO f . ct V.ir;h t by 22 vide, v.-ould yiold 1,D40 ( OOP

•fccnc.In nollhcr or tJiaro ontir^ton in i'ny t^jcownt taken of the 'indication

of pt-rr.llcl IcncoD or. :iQv*n in the records of drill holo 15 rnd

to i: lo .".ter orrlent in 16 rjid 17.

K OF ORH. 71w corcn

irill Hole J.'o ir;.

Drill Kolo *:o 13.

j)rill "'Tolo Ko 15.

•l h o drill holo:j i Iron.

OGO to V10 iVot. :V*.S5

- 7C-0

i n i'ollovvo:-Ihon.

.019 .031

.10S .op.a

; oio ;:o 10.

;rill I'olo r.o 1 7.

430 - n05 "5?Jii - J;''0 "570 - COS "

rj'io - QUO7HD - 7.5V70 - ".-;;r "•"': - ' -

, - .,-

to ', ; o -? .'i' i; -ir.

B6.XGr-a.r.4r.s.is!i:-.-JC

or.'./.oo r.. -G". .T'"'

* t *"i:-: f- U- ?

.009 .OcO

.000 .049

.01G .OSO

,0'iD .065.o-; r. .063.OL-0

, :rt , : iv- ?'- t :n-l

o? iV.cir c- nlr::l

*i . .. -., - , ;-., we have an'avergge of 59# In iron, and .040 in phosphorus^

JBL^&.thisi probably.represents very fairly the grade rf the Josephine

of the boulders of ore.found on the lake v'/

shore when,the.property was first discovered, were about this . .. -"

character, but averaged.a.littie lower in phosphorus. , . , . ,^

l

l

l

l

l

l

l

l

l

l

l

l-'ft.'

l

"•- :i

- - " : 3 JOF.SPHI1B PHI II HOL3S

l

i i i

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' . . Drill Hole Ho. 5, Course South 50 degrees Sast, dip .;v. 45 dogreoD, length 122 feet ' ' . ^

0-96 feet, Eassive Greenstone* -. - . " . - V 96 l 128 feet, Gravel '^ '

Drill Hole Ho.- 5A, course South 50 degrees East, dip -: /""" 50 degrees, length 133 feet. . -.. -,-- .

O ~ 103 feet, Kassive Greenstone : .* ' 103 - 133 feet. Gravel

Drill Hole Ko. 6, Course North 50 degrees '.Test, dip 45 degrees, length 473 feet.

O - 15 feet, Clay and Gravel. , 15 - 345 feet. Schist carrying small anounts of Carbonate

of iron. 345 ~ 473 feet, Banded Silica and Iron. ' . '

Drill Hole oJo. 7, course Horth 10. degrees West, dip 45 degrees, length 491 feet.

0-19 feet, llud find Gravel 19 ~ 341 foet, Schist carrying Carbonate 341 - 461 feet, Banded Silica. . 461 - 468 foet, Hematite Ore 469 - 483 feet, Banded Silica 483 ~ 491 feet, Heraatite OreAccording to reports the ore is very soft and'the coving at

the bottom caused the stopping of the drilling.

55

in C! a

Drill Kolo No. 12, course South 35 degrees East, dip degrees, length 715 feet. .

O - 574 feet, Green Schist574 ~ 660 feet, ^^nded Silica660 - 710 feet , Ore710 - 715 feet, Banded silica.Regarding ';ho ore exit in thio hole I ouote as follov/s from

report by "r. Bradt;"At a depth frora 660 to 710 feet v/e cut oro of profiling

-iality. The e.:aount of core we obtained fron this 50 feet of Grill- j is about 16 foet. '.'he core v;ao mixed soraewhut \vith pieces of C:T qui'.rtr, or jr.aper. Reprcsenu^tive pitncs pieces of the ore sayed bet-.vccrf 56 and 57f metnllic iron, and were lo-,v in Phosphorous. e sludge v/e obtained from this 50 foot of drilling, that is ^rora 0 to 710 feet, a .•••saved as follov/s;

Froa 663-608 608-673 673-670 678-683' 683-008 686-0936113-'* 01:'

705-71^ 713-718

Iron 2H. 1525. HO16.7416.67^0.^013. SI1 -.' . \ - "'1'; ' ly

li-'' ' w I-

'•r- r- r?!'\J . \JO

19 . C3

Sul-ohur .130.;:97.191.130.130.lv 6.1GC. 'i- 36

.115

.130

F.:os. .019.023. O':0. O.'^O. 01-' 1.031. 0017.01' 6. C J i. L. GO-0.0011

l lli i i i i (i i i i i i i i ii

The iron in the above le somewhat lower than I expected it rould "bebut I believe it .to be accounted for by the fact that above the oro .formation, and Just'before entering it, we passed through severalfeet of very soft rock vfoich would not make a core and was easily

r washed but of the.hole, and it is my belief that a great deal of 'this soft rook was washed out along with the sludge abovo mentioned,as the chemist said he.could detect particles of rock in the

•samples. While the-percentage of iron obtained from the sludge andthe core is not high, it is quite probable that we passed through ,the leaner portion of the large ore-body."

Drill Hole Ho. 13, course South 45 degrees 2ast, dip 55 degrees, length 740 feet.

O - 422 feet, Greenstone and Green Schist 422 - 649 feet. Banded silica ' 649 ~ 700 feet, Ore 700 - 740 feet. Banded Silica.The core from this hole, 649 - 700 feet, averaged as follows;

Insol. 19.17 Iron 55.78 Culph. . .103

' Phos. .028

Drill Hole Uo. 14, course llorth 34 degrees West, dip 35 degrees, length 512 foot.

O ~ 132 feet, Schist ( 132 - 159 feet, Br.nded Silica 150 - 155 feet. Schist155 - 355 feet, Bunded Silica * 355 feet to 512 feet. Schist

2he torn "Banded Silicr." on the map is short for Banded Silica and Iron Ore.

li'

WEEKLY DRILL REPOr ' . MINES. DEPARTMENT

*rrf\T-g51 WEEK END1NQ S6pt. 27th

1K

l

1U*M

iB

B

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24

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27

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. Total

17..35™.

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DRILL REPORT-' : M INES DEPARTMENT V : :

! i1il'9;JP-?'':?-; i 8-4-6,6 o.^.YJbr - - - - -™ WEEK ENDINQ__Oftt- -7

IPiV

flalm No...

1HaIon.

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1un.

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u5^jji:^'.:.;*t-..^.^,.4,^SBPHI!IE. ______ .. __ . ' . - - ^**jl*ST 45i. WEEKENDING .Oct.16.tb*. l*-!!

•Mirr

PSI....NlffHt

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DAWMiflfn*

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390

460

475

526

536

506

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LKind of Kocfc

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soft grey schist

Graphitic ochiot

{f Grey 8 eh let

Grtphitic s c^ i st

J* ape r with p ênatite ondT.i!nonite

•^T;-7'-.r':; :.7r-

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Date

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H

M*k ** -' '••V * P^Vt r MV F^4V UFA Mlfb - . - tttt

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,. . .^..7...... , l4f.,, 542 ^6 2-8" 5486 7^ 554

............. ......7 . , .5-8" 561 ...:5 5^ 566 ,8 6 .574 " *~" ~ " ~: —| L- 111-

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WEEKLY DRILL REPORTi'PPijv- M INES RE

" ''' ' ' ''

WEEK ENDINQ__Q.C.t.*

Day Runner, ...,....]K....lTr.ley

Runner, .A il

. " C C1 ?recV.7E".........,.......,.....,..Superintendent

WEEKLY DRILL REPORT:^: "' : MINES DEPARTMENT

l HOI* Ntv -Ati Olalm No.. 451 WEEK ENDINQm-

lT.20...-V-

nun

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.P-r.™.HI**!

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1

Iron formation

U'X

•1630

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WEEKLY DRILL REPORTDEPARTMENT

:PQR't^ ;^l0Srv, KCV 2V: ••'- '"-' '"•''•^•i'- t'--- --i- r, . * ] - . T '-v?.-* into l - . . - i

m No.

1913N * ^

WEEK ENDINC^.cifx^C.tju-SLat.i 19 l!

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663

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•n Depth Inn 14KlmJ *f Hock

12Dot*

634

685

692

Iron formation

witH spots of henattit/e

{Depth a.t. 11

^...JUxdt-.

HOTIO'

B

702

707

778

altHera.joa

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DEPTH

DIP ...

BEARF

IINE MINE.1 HOI F No fiO

... HATE .......LOO. .......................

NG ....^..............................................,...............,......................,.....................................................

FOOTAGEFrom

K1 R

-5E5L-

-537

KA Q

C |* ^— ot^l —

596

-603^

609

—615—

6?.7

e *X ft —— O^O ——

642-

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— 660-

R71-

672

To

527

537

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^J5.Q1-

-609

615

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-63.6

- 642—

652—

asi.

660

-67X-

672

-fiQS-

Length

f*ft

.

^tl——

1v

t f

ASSAY OZ.

#23

#22

Jia.#20

#21

-dt&t:-Tff-**~

-^•—'- —

#16

#17

JLL

Ave.

A1&

3?#

j&f*

IZji-

Utt

4*h-

3 M

1A&

16&i

GEOLCX1Y BY p.A . Chubb

Schist, liRht ccrey to dark Krey, talcose.

Graphitic schist, black.

Q.uartzite. slightly fractured , Sfr hematite

Cherty quartzite tc. Jasper, 15^ hematite.

Charty quartzite fe jasper, S& hematite instreaks and bands*

Hematite , c6mpact , soft , reddish-brown ,805& hematite.

Cherty quartzite. 30# soft, compact hemaitte

Cherty quartzite, brecciated, 50# softcompact hematite.

Cherty quartzite and ftasper. 10# hematite.

Cherty qunrtzite and jasper, brecciated,50^ Bof t , compact hematite.

Cherty q\mrt7,ite and .lasoer. brecciated. 120^ hematite. 1

Cherty quartzite, jasper, banded, slightly 1fractured, 10# hematite.

Hematite, compact, soft, reddish-brown, 80^ |

Cherty quartzite, brecciated, 60# soft icompact hematite.

Cherty quartz i te f^trfisiured, 5^ hematite.

Hematite, ground core or sludgo.

Quartzite, brecciated, 50vo soft, compacthematite

DRILL HOLE No.JSQ.

•r '

LAT. ,............. DEP. ........ ........ ELEV. ...,.,.,,... DATE . .... . . . LOC. ..,.,..,'................ .... . .. .

DEPTH

DD? ,,

BEARI1VQ ,,,,,,,.,,,,,,,.,,,,,,,,,,,,,,,,,,,,,.,,,,,,,,.,,,.,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,..,.

FOOTAGEFrom6R2

692

^7^15"

712

. ————

To

692

.705

712

917

Length

to—

^^^

-ff-

ASSAY OZ.

#24

j^25

^

Ave.

^f"^o

——— rtt&y*--' r 9

^^^^

GEOLOGY BY

Hsmn tl t fl , nof t , comoac-trred,— 905i-4;ematite-r

Schist t light gray— gfssp^ — sligh-t-lry— taioos0. —

Hematite, 9oft,Tftd ( o.nmpnp.t. Rn^ hematite*'

Schist, slightly talcose onfl chloritic-

^' ' tr* rt~/ ? -C- 'yJ^yfe (n*J-*r**-~(

"" ^V*^ **WV/ *- /Z* "/'/'r*

\

"3SK?-^Sî

fiklii

J

f*!-

••c*.

fc

tsjws/^ y-w, f- r. ' : ^ - ^ - .' " v*•i K-V: *î''- ,( •rjj.' ^^vi\^: • '^•;- ' '' -••

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r- ; ... - •."•- - - - : ••..•- - . - •.••.'•".'.••^•p

LY DRILL REPORT ;^,îl|MINES DEPARTMENT ; .'. ' , A^.;vy;'^^

WEEKENDING TTov. ISfh- toft, ^ ........,,.^. -I.

1-;;'J \ "

-JLll...

.IE—

13

,14.,,,

15

,

1 ~'* "'i' . '

,: fl5'"')i*i-' ri.'. - f* -f* H

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NlrMtôT ^H*J^[, —— ~ 1

r i i i i i i i1 i.B** O r\

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175

i

Nfc*f

.

*

'

-

•tanrirlp*

r**t

.

Und ef Rod)

.Greenstone

"3-

-

Hat*

,

Cutnv ter*'-. ' T*UI . •mitMl '-. " ' ' car tnurt*4 BrttM H*c***r*d D*ptli ••tay* Mt ' ; l*

f . - ^^ ; . - - , , M*. /V-*-

'" 5 - Onq^n ' -' - -, '••*' ;--*'-15 15 20 " -i -A

., ..XT. 17.' : 37 . J- . l' - - ;-"s...........,™.. ...17...... , . 17..,. ..M,,. ..:...,: ' "

18 17 72..,.,,,,,,|,,,iv,,, 17,.. P.?,-..

16 15 105 ',,,..,,..,,,. ,,.17..^,,. ........16...... .1.22,,.. .... .....

15 15 13714 14 15115 14 166

9 9 175 -'

175 166 175

••mull* ' -. - '"- ' ."" ". ,

- . : - .v

S, . *

.

^^rr-r -./•'iP "*r"' . \

Day Runner, . . .....^...3,,jr:,l.Q.y,A^f,,..,..:,,OfC--""--c

NiBht Runner, . A '"'i 1 S On \ ISly... - . , !""

\A, , ^

Vup*rln^6nd*n1

'' '" ' ' ''";

WEEKLY bRlLL'REPORT'^i'sS '. -- MINES DEPARTMENT ., . , ;

(Reg.'

^."•''- ' *lm " WEEK

'#;

Greenstone

Day Runner, ...............A.,

Night Runner, .....,....J/...E,,J!

^^irnrn^' -^ ^:^ipi^p/VyEEKLY; DRILLteM^P^V^YC{M; - .MINES DEPARTMENT^*:.xV ,' : '"^^.^'y'^' ; r.'.:'-^-^.'.'.'.'-''- -/W--.; . ." ""-v-:..- .'

OliUm No.L -1*^.

•MJFTImw!** RMiiMtf Tvtal

Dec

-llS-..15,

1Q.

..li,.,

^JB33.. .-,..p^5., .J.63.Iil8. .....853, .....5,0.8, ,,,9.23,

8

Ib8 Ib8Depth frw

turf MM Kind or RM*

833

076

l*g1*.Ty..Br*.i;

j:otone

Day Runrmr,

Night Runner,..............A-

WEEKLY DRILL REPORTi ; :: S V .MINES DEPARTMENT

., . . ' ' t -,1 ' -

'OKI- .- ;:i*x*S8m,:-\'.:t -, : r-l3*l*?QM

lfli| vWEEKLY DRILL REPORTK^.*J^Xivf: iWi:C: : .MINES DEPARTMENT ',- -V ;,;.

;-; -WEEK®^^fe^S^A;vU^'--v; . M' ' '"

WEEKLY DRILL REPORTMINES DEPARTMENT

WEEK ENDING JeO.: 5

Trial

JEQ.33P.PTTW T fTTTP.

Day Runner, ......,Ar...~.V-.l?...s. o.?!L.......

NiKht Runner, . .T".r ..J-.V.J^lcy.

;1v^^f-'--: WEEl*^ fclS^&v : " - -v f*WEEKLY DRILL REPORTMINES DEPARTMENT

. .?; : WEEK eNDIHCLM.-*L?B.

^^ K^!f.liw

Mirr

Day

HI***

Day v.

P-*-:,

H*.**•ten* rip*

*Mun*4lTohri0*pth

.1227..1253

1252

72 67 1277Depth from

Iron Ponnation

Day Runner, ..... . A *. ..Vfl IsjQA ....

Nteht Runner, " . S .UUrlejr.

^uporlnt•n<l•nt

•ffe•Ut'

*Hoii.1-i~ 1

*4-

*- i'"1-' " ' " i - *"* '* - "* ' ' o ' -' ' ' ^^^— ' " ^^^^ * *"*- i- fttfff.

ft W WEEKLY DRILL R^TO&x - -'^r^mf^fe^Vi'V " .v v -V* MINES DEPARTMENT r J\ ^V. ; '{ ..i'v^'^i^^

* NO. - -. - WE^K ENniN^V/ Jan t 'Mt^ t , i:; ii ,.,ia?.4ir:j /^ . .'

10

11IE

....13...14

" •wrr

D^

Hl^ht**r'"'

Nir*rt.D.y

NIFHt

jp.-y....-W Jirt**

O Ay

NirMDayNl.St

DAV

Nirht•i Tctal fer W***

PpllMI** H**

1

1

1

1

1

1

1

1

1

1f*J-1

S.pth frtm •urfae*

1*11

•tt*

. ' ..-i-..

' .

*SSiSr

nnd *f Hw*

Iron Jrorrnation

WJt*/^ Mfvfc*^*****^

FM*

* . .

Bate

,

————— -—

————————

Cartnff ' ' e*r* ' THal Hull la ri ' "* Bark fo**rtetf BrUM **c*v*r** Durt* - **tav* Mt .* x U*

. -^ - . -,* — r*. .. - IN. ,*:'- :'ato. *-' --' . - - . .''''' i*T*.-" 1".*.'-?*!*" *~'' -.-^c- J — .- *-. ' ' ' .' . * ^; -, - . J - '•s.. _ :..ir— . . G |i-" 1?8S x * '" "* " ' ^

... .....:........ :.™.6..... .:.u.l.fiJ' 1288' '-'A " ' *.:::' -^i-" '-T^y-4 B 1298 "' ; ' "^ "f*.". . . -^ '

.1............. .......4...... l:.:...4-*... 1296 ' -v.' -:- "-V- -. : 'L5 5 12014 -4 1305 " : s -' '

' " •••- ' . - ' . •.- 1;..'•' - '' 'i •*-

o - 5 ialo - -D 5 1315 *- "•••'••'•b D 1320 --. ^ * .K\

.......,.,....™, ...,..,..5...... ,.,......C...,, 1325.. .. ....' . '-*'- :'*'6 D 1330 - l r'

' ' o 5 133558 BS 1335

••martx ^ ' , '...'-j ,-'

' ''..' - ••

.

' .- ' ' '''

' ' -.

. ' -'•- x -

.

B

.

Day Runner, it t Jlmiey ................... .... ............................

Night Runner, . A. ...W.l la On......................... ...:................

Bupvrlntonden

lilt! 'Sill i' ' : ' W E E K LY D R l LL R EP ORT\ ^H^M9iî.9-^^sW:-':''!--^î^ MINES DEPARTMENT. '^''-Vi* ' - - \A"i: ••vAivi'&iSi38k. 'Tr^**-''* * ' * "**"*?-*** v1 v.,'- ** - * m*.-,V- J\r' **. ,. '•-, - ' ~. . . ' ; -*- * - ; *^ *îXY1^ "^ ^~* '-- * " *'j ~ ' -**"* - 1 " *"'"*- ; *' VSPP^'- " :îSl^v-'-'*^^l ' : -' ' "•*- .' - ' T'- : \A :: ^^ v î^ '.''. :...^!^ itawo^!——5X-^—~.A*___..J.OSSPHIilS.JAIH3...___._i-'- v# - t?/ '".'^ -' ' " v-*Vftf-- - .- -* . ;. vJ.'---- - ' ' V^" ' X'X : - ; - - '. : - .I^No. -' '. ••^•^•J.g-.-V. - /: ' . ••: - - -..., V-. WEElO^NDlNO. ,iJaft*-JljtiiJ;—————19J14

18

20

^1

jPay^g

-l1***!;Day -V V

.??.!ff*!l.

Nlytot

P-.X..Night

tatng

....P..

....5..

2...a.3

..3..

..3. ^

..fi.î

...5... ,3..,

...o...

...3..

...3...

1345.1350.1365.1358.

13601363.1366.136913721375

Mt

•-?

l 1

l

l

l

l

lm

40__ MO 111375.jrtS troi •urfM* Date

Iron fornation

AiKto.d.O.Ctf.

Day Runner, ..................4*.....?.!l-.A?On

Night Runner,................"* ....^*.!,

frHp5?t^^^v:^^:-.,-. : .-v- v ' ;-\/::-:-., . : :- : ^HS^C^^v^-'V^^.---^ .'i-r ^-.;- " , - -'- •':- ;.v.-'-v,,r 1 -.;..v; ; .-.v^,i:iiiiiiP^-tM^'. 'WEEKLY; DRILL REPORT^:v^^^f^fe;^p^^v^^V-'' r ' ^:^ MINES DEPARTMENT \ '. • "••; V;-:;U "v^- .^4^1*^ Noiw.^51 ;,'?i'',',''At' .TftSRpTTrra , . - ,-. v .- - - - - -. - - ^.v.,-7..- -i.'.- .'vV- ^,^V

*- v. ' ' , ,- -^ " ' - ^ v " ..

P•H— — .-- -

1PI

1K"

****\*v*

^23

26

or*

.'...28,..

29

SHIFT" i v * "

D.y ;

•2f~

NI*Ht

D*r

^Nl|(titD.yNlffHt

NlyhtR*r.NlRht

^^-7 ——————

f

Dtpth trow gurffto*

|

i

M*, tt lMMTto4Uta

--lv., . ' .•f '.-' - . " . -

- .

"-'.

Kin* of Heck

Jasper rith specks of Eeraatite and limonite

r**t.

,. ".

- '

t

. O.u'

% --

- -- - —

i

r WEEK ENPiNQ,:-.:...,..;,:, Ja]tt,^lat*^— tft-14-

"l. w 1 " - * *^ .' 1Mb ^ ' , ^

" : '^y.-S' R '' T37fl ^-X-:L: ^"3 3'" 1ZR1 .-^:- V- ••J .

.•","5 ' 6^ 1386 '- *: '- V- v- .-:...--, 5 - 5; . 1391 .

3 3 1394. ............ ,....,..3...... ........3.;...- 139.7.. '. . . '

2 2 1399 .j /..2 2 1401

.....^....., . 2 2.... 1403 .3 2 14062 2 14082 2 1410

.....:............. ,,......3...... .......3...... 1413. ...J.,, .., ..3 3 1416

Rtmark* - ' ** ' . --. x

. '. .(J

^~~—^ -/^. "'''^^s.~fa "* ^Q\[to ^, s(fb \Ife "' ^\tc j- - \V ^' ^7 -

v - -s*yX^^j^t^X-

f

Day Runner, ..............^....wilaon—-—------—-— —"-- —— -

Night Runner, W E Hurley........................................ .. .

..NO. WEEK ENDINQ, : yJjMl* 3l8t. "1*14

si •Nirrr**t

ut

Day *-"

Day *- - : -3Night

1422.1425..1426

fisti

P""'

f '*i -1'

Depth from turfaM KlnJ rt *Mfc Date Rtmartt*

Day Runner, ^. ffilsOU

Night Runner.W E .Jfaley.

?|^f':'j:;C*:;" v i.; " "i""

v ; v" '

- . - - ' '-- .. - - -

WEEKLY. DRILL REPORT-.. MINES DEPARTMENT .,; V .

WEEK ENDINCL.-JE&'b *.JLth.

WEEKLY'DRILL REPORT

Iw ST--Ho1*•fi*}*

I•v'V t-

.f-Tu**.rtFrt

I

wo.!.-™rt No.,•s :

Bat*

10

1112

13

14

Bl'-X*-*''*;-

'. - ; '* ' ; -l^Pîln,

•MOT"

D.yV

Wl^fit"

Dwy^

Nlfftit

Day

HlKM

DayNlfftlt

Day .

NlrM

OayNlfht

Day'NifcHtt -

tot*) f*r W***i4

f^

1

1

i i i i i i i. i

-

Depth fron turf ax

t

1476

1520

i

H*.**Ht*

'H-— v

-1 '

^ '

-, ; -

^.t - -i :'.

'

(tentfHp*

- ' . . ;' ' **' T

*.*---

: '.'- •k.''"'-

- . "" t

Kind tt Hoc*

Iron form with smallbands of hematite ond Dchlat

i

"Z"S-v .

-

••.•-•--. ','-

'

Pat*

lasi.-Jro>

l ST'T^,

*

UC.r-MM 1 IVIC.IN 1 ' . .' -, ' ' ~. .- *-.-.' ..i^^Ji^V

, . ..-... -..^ , ,. v.., ..^.. J : WEEK ENDINq...: ——— H.eOjt-JLi.tll.^.^.lB.J

- ' sssssss^: ssssf sssssss:Boh* ' C*!!^^ T*tal Vwwid "' Owl

•'w^rt^w Onn^v ••••wwrpw pvpn .^ vw^yv Bit fc VMFMt - ', '.': r*H v FM*: H* Mr*'. Ml^ -.. - . ''J.'""*

''•J.i.t - ---. -- ' ' - si.-fr " . . ^.^ .

:.- '•' ' ^ __ - ' 4 -' lABQ V; . . : ' -: ;.W' .

.,,^: -'- "4 '- 4 :-:.' 1AB4"' -^"' ' -"'• : J 3 . M,3L.l. 1487... v' . - . ..". --v:

,,,..:,,. ,. .. ...3, ...3.,....,, 14.90, ... ..3 3 14935 5 1498

....... 4 4 . 15 OB

.,.,,,.:,..,- ,5., '. ,. .5,,,..,. 1507, .i,..4 4 15115, 5 1516 - :

-,-.l-™ , ...4j-™.- ..1. 4.......... 1520.. .. ~ . —.. ™... :-^ '-..J......... ,,,0.,,,, ........O........ 1520, ...,.., ..L. -' '-"

. - .

' ' -, - . . - . ,tHat*. - - - ' - '; -- -v;.".', .

V-W- ,i^#t ^â tt^LJi. -rt**- : :4- -^JClIcSZ {^W-l-^vvw^^!^^t^jL pî,/. "X ^c/fl, '

; '

* r .^ a^^ A^t~ v^^* ^^x^^-CZ*.

^^f'^LÛ-Y'

'" /o^' r^ ^\/•'D ••'^'^ \lî ' Ô . JVî . \^'v *.7\ 't^f\^ iio^x

i(g)v^ .Day Runner, -A^JI^SOn

Nf^Ht Runner, W E Haley ^ ^

i*VV*fc'i* -KVÛ'' : ~s'^y^: :-Vv!.^.S'

WEEKLY DRILL REPORT-A. v. MINES DEPARTMENT - .-A.*':.;

. JOSEPHINE— _WEEK ENDINCU^^..Pfllu.2l8t*.

te p••^,-1?ifTUtt*..|i"?

i - t•7

PH.

V

Kn,

••'-'M ' X""* '

* VJ J " ' '

SUB-- V ", ,

1.17.

...18...

...19

20

.21

^ - ' ~'v ' r -.

•Mirr••"-T.'

JDjjX*-

Hfrht.1

Day ..V .

Nlfht

P*y-

NlfM

*-*L....Nlcrhi

JP*Jf.......NIKM

5*y. .-Nlrht

S-R™.NI KM

T*tet f*r W***

BMOrtptl*ii*f •f Not*f^-J

1

1i' i i i is.

1

ji..80 M..

Depth frwr •urtko*

1520

1581

'i

Nfc.1 •tt*

. * ?. "

V .1 .'-

'

'

- tUfi*Mp*

rMi

z::::-I.::::::1

.

Km* true** '

Iron form containing numerous bands of hematite

J

***m*4

FMt

-

Cat*

ir*.;*.....

...liQO....

.\fJZ\%

- ————

tulnff tn**rt*d

KM!

:-~

-

DrW^ "h**

.6 1,65 '

5..e.......5..........

.-*.5i

.. 6......6.................6...............4

2

61

0*r* ft*t*mr*4., **H ;-

. e.ii.- 6 "r-5 "55

......B.........5..

.......6.........

.......6................6.......

4Z

61

TctaJ O^tk

fMl ;

152&.1532.153.7., 1542. 15471552. 15571563 1569,. 1575.. 15.7.9,1581.

15.81.

VfWM*lMqn

•r* Mhv

f. i "-.'" -** i. **

Wf"* . '. . "^

. ; * -t * i,-*-***;*- ' -^*^*- "

-^ -..

i* *

. — -^ — u..

MtN*.

'. '

. . .'V--

iz———

*. t

— —

'•. c* . it•• ;'M.

' **""'~i ,.

^•. . v

-J: — .

.-i—.

—r—

*^*-.:'

"/*

. . '; , " , - ••mark* ' ' V . " -;

'

^^^x^Xjt^v^ >>VA^C'

~tjt V*tU ..brCfcc oLx~~C*3cn

1^0 ^

-v---- :---f P ' " '..................™.......-^...........,............- ......—...™. . ™

fe^î^JtJiÂL^ JCxwolittX /Ojuxtfe^^^-^t^'" J(T \ .

J . '

i A *-X," "•.

-.—.. — ..*.

-— ——— -

---••••--•— •-•-•-------— --— "^

Day Runni

Night Run

9r, t?. E. Ha ley.......... ...,.......... ......ner, . A. WllS on.......,....,................'......,....

•up*rlntond*n

DRILL REB. MINES DEPARTMENT

[Hot*LfX*-*"

•laln

SiypsP-l-s^

iKri.

1

NOb.......f '-

n No..^ssssssss

Date

23

.'.2.4...,

25

26

...27....

,28

51 ;*T At iluIOSKPH ITIR..MIHS--•.-'.-' '- ' - '-'- ; ,-

.'.i*-' V •Hirr

•'S-*?

bmjr W

Might

D.X

Night

D"J' -

Night

0*y.^^. .^.^.....

Night

D*y

Night

D*y '

Night

S-*.....Night

fetalfwWMh

D**erlpU4H rf ^ *fHoH

1

1

f

1:1 1 1

! 'A11n*l

\

• ..../tt*-

Xpthfmt turf UK

1581

j

1602

1632

i

N*.*f •rt*

f. .

•-": :'-

-- ———

-

'..•,'.'.-

- —

•tMtfMp*InMTtW

r*M

. —— .,... — .

Kind of UK*

^.*

Iron Form . v?ith "bands of Hernattte

t \

Ilenatito very hi^h in sulphur

/A

itamtJ ' Tut ,:

^ ' ~' ' •

'

~~—~ —

DaU

...mo..,..o-V-J—----j-

.liio/*

..,, ^;...

. viofb)., r v

- .' . . i -;.... f l ? r-, ' -,- - '-i . _ . - . . - - ; i-/. k ' 1. , - - .. . . s.,i :,

. i ' ' * -

. ; . r WEEK END1NQ _____ ...E01l..mE8±h.---19,4

t**iT*lnMrt*4-

'•** ,

--Udl

———

DrflMr**f

5 -. ;:.1...5......:v 5

s. .... 4

4—..a _ .

..4. ....-...4. .......4 .™...5.......

2

fi!

t*r. tx*nn4

tut

" : 5'..:..6..::..,

5. :. .5......

44

.......4...,. 4

1 4..,,,..4..................5,..,.

2

61

Tvtal P*(rt*FMI'

JLS86-15911596. .16011605

..1609.. ..16131 AT T • J. OX l-

,16211625.1630 1632

Jlfiâ

Bimiyi"-r Kl"r* Mm. . -*v *

•' . . . . : -*'^.'.'. '- -'*

"\~" " ~ -.

™- —; —— - ————

.— —— . — ... .. ———

- ———— ——— ——— -

Cvt IM

-'f.**

' ' C '

-V.

i.mfcrV* - - . : " *. - ; - .;.* ;.

- - . ^ * " . ;- *'*

.. i^!tivqJt^ ,. V^ MM ' .. ............................ ...... ........... ......~... — —— , —— .

.:......-J6Û(M**#nM;.....,,....,,^ ....-.....'..j.. .

x t :

oWiuJ,^r :.^r . ; . -

jdi,.^ i>^vÊ*.....1tÂ^^ :. .

.

*

A (O/^,L^JÎx'""" ~~-^^~~~~ —T' —

Day Runnc

Night Rum

l

A J71 Ispn..... ... ......,... ...... ......,.. ...........ner, . W E Hcl(

^^^

iy . ... ........ ...... ... . ..

Sup*rln

1 ****r2tvi/dknt

JOSEPHINE 15INB.DRILL HOLE No 51

LAT. DEP. ................ ELEV. ................ DATE .......,................... LOG.

DEPTH

DIP ..........

BEARING

FOOTAGEFrom

-1120-

-112&-

-^1146^

-O1&5-

-11&7-

1174

lies

-1186-

JL19IL

.1204,.

.12(35

JL211-

.1271,

JLSSQ-

-1536, -4S5S-

To

-1126-

-1146-*

^ ^ ft e*—1-165-

-1162-

-117A-

nna

-1186-

1190

.1204.

-1205

^laii-i2?r.

.JL330

-1336.

-1552,-1S60-

Length

. ————— ,

3--

6

ASSAY OZ.

'J.X4& -rtpp,

#13-

r^l^-

ttl^ -^j-o—

#12

#30

Hrrl-#51-

Ave.

——— —~

JZ2J&

?( 5^ /c./^-

9 ffi3 t /t

, t "0? •^ s-âfV

———— -

lift./X ^^J

-^

GEOLOGY BY P, A. Chubb

— Aoid-ûff-r-^^ht^rey-brov/n-r-eof-fri — — —— ——

Artld flow(rhyolitpjf hord, .^wlnfirt Hnrt.. atrenfcOf hfimnt.it.Fu

Rhyolite* slightly fractured - o f ew stroaks^-a of hematite. ———————

- Jnaper, frnctured. ......

Hematita.—ixeddi3h-brown.— 9 Oji-softr compact ——F f * * *— hamat-iêT—soma-Dick^l— stain, ————

qiinrt^Jte, hrfio.nintftd nnrt fractured50^ hemfttita.

nhp-Tt-y qunrtzltft, nilght-ly br^cciat-ed.10^ hninntite.

-.Cherty-Quart2ltet— br-ecciatedy— 35^-heaatite^-

Chorty qimrt7.it.ft, slightly hrftnnlftt.ftrt ,?-OjJ hematite r

Quartzite breccia, 40^ hemfitite.

Hematite, 80^, reddish-bro\vn,compact,spft.

.. Ja a pj2n..and-Quar tzit e .banded —lO^hematiit Q_In atreaka nnd hands.

Cherty white quartzite, some jasper^ a littlbanded ore, 5# hematite.

\

Quertrite and, jasper, slightly hrfinolfitfid.2S'^ hematita^.

Banded quartzite and Jasper, 10* hematite.-Bandod-Hjuartzi-t-e-^ndâspts^—l^Ty-hemfrtlt© s —

-

DRILL HOLE

DEP. ................ ELEV. ................ DATE.., .LOO.

DEPTH

DIP ..........

BEARING

FOOTAGEFrom

1360

1367

1370

JL3Q5-

1393

J 4 1 1.

1416^

1451,

144fiL-

1469

1474

1505

1567

1575

1583

1587

1598

leoo

To

1367

•JK70

1385

-1293.

1-411

-1416.

^JL431.

1446

.JL4.6SL

1474

1505

1567

1575

1583"

1687

..X5S8

1600

.IfiOJL

LengthASSAY OZ.

-#27

#28

#29

#26

#53

144

Ave.

t* KJ&JL-

ixfr

"l/ ft —5^/5

J^j^JJ&L

GEOLOGY BY 1

Jtended quartzite and jasper, 10^ hfinv*t.it.R. 1

tymrt.7.1t.n,n1lght,ly brecciated, -40#-hemat4^r-|

Quartzite and jasper, 15^ b,pnrmt.1t-,ft t 1

Quartzite and jasper, nllghtly brecciated,35^ hftpwtite. 1

-Quartzlte-^and--ja3ft3rLT-soao--horaat4rte-s^reako,

Miaaing, 1

Cherty,.ciuar.tzite and. jasper, . banded, 5;* heoatij

'Jasper and qunrtr.ttfi.hnndnd, .bmcciated,30& hpmat.lto 5M hnlfVna hfvr4 ^vrittlA hAtnn

Quartzite and ,Jnnpp.r,n. littlft .schist, afew minor streaks .of -hematite-.. - ...... .

Acid tuff, lifl;ht Rrey-^reen. hard. l

Quartzite p.nd ,1asner t -5* hematite

Bonded Quartzite, Jasper, slightly brftonlnt-ort5^ hematite^ 1

Tapper and ojiartzire, brecpintort , 5tV* bnmnt-ltJ

Quartzite and jasper, 40^ hematite, a littlehard hematite, lOvi ovrite. j

Brecciated quartzite, jasper, 5/i hematite.

Chlorite schist.

jTas&er and quartzite t Sf, h pwAt.it.n.

Chlorite nohlnt.

((

DRILL HOLE No.J51

LAT. DEP. ................ ELEV. ................ DATE............................. LOO.

DEPTH

DIP ..........

BEARING

(

FOOTAGEFrom | To

-160^.

.1612-

1622

1640

-4.612-

.1622.

1640

JL695

^,... ...^.

~

I1~ ~

Length

*r^Î..i -/3'h*

ASSAY OZ.

-#4S

-*46.

~?47

>-

Ave.

-*a^J-

^-Tl

^"J^

^

GEOLOGY BY

-Hea^tite,— ccmpaat^—sêd-r-floftn— extdiBed — —— pyrite nfttfit-ifts. 50i pyrite. - - '- -—

-Hematite, _ a-fBW-brêccia-tra*9nentar-nuraepoua- -..80j.ulLi.QnLJ?lL5fJL1ilfi.3^—lO^ .frftflh pyrlfn.

H-emaiJLts,__hard^_i)lackf_b^^t^^ft, P.O^n pyrite.

—Chlorit^Sfibist, _ light- grên^ slightly talet

/L^. —— j ——— —— ^^-^L^^f^L —————^ s J .^- j.t~* /~~y^- — ' —— rl^sfyf** ^ V ^

'

WEEKLY DRILL REPORT "^: MINES DEPARTMENT

•^'''^K''?v Otcg.1wH\:^w^m^-' - v^. ^\ ' - •Z-*--*.V;.-i1:s-..- #v^ "*i -: '^:;.svr.ir,?c ,. . *" * 7 '/KVV -';Hse ' V "' ; '"'" : -"-'

WEEK ENDINQ_ v^Jarch 7th. -IB 4|

ISp^r/-KJ* X'*'.'"; " '^•'.'•'•" ' '

DRILL MINE8 DEPARTMENT

fei-yiWjf.;., .Y- , :,^^f 4*^41'P*' . ' , ' !•laJm HO. WEEK ENDINQ..

17

19

21

•Nirr

Dny

NljCfet..

Nljprht

.5**-™,.Nilcht

Nlc+lt

BM*InurtMl

fMt r**t r**tDrttlwl

r**t

.J8Q...

.25,-22,,,. JB&.......JL9.........21-6

ter*ttvn

PMt

,25,.^.,E5i.l25™.

,EQ.,.,.

2S...12,.15, .15.

Tvlal

..533.,.E64.. ,,5.89,

...652...673s ..6.33s ..704. ...7.EO ..72E

L.

NlffM

tiMt rf tpUi fm* •urfM* Kind ef Dock '

499

Greenstone

722

F. ynr.Day Runner,.

Night Runner, A. J?.?.A?A6,

.*rgri*.

i•I•ol*

Stall.-l* ;- *'il

li?fcon^

C1

'-.

• un.

Ifll^^^fe:^f^^; ' -;:4^?yjg^?--; MINES DEPARTMENT - ; ,. ";./; '.~"''; ' [ ffi-'

,-Nft. ' -: : WEEK ENDING* Har eh 28th. X|v

#r-;-

'..•-'.'*'-'- ".-

? 24

i

25

26

...27,...

...28...,

*lf*rWMk

ptlMWcrfH***

1

1

J

1

1

1

1

1

1 *"

*

(1*. 4 Ci o,i

titirr ||o*/*

NlcHt'

Day 'V

. * .Hfc*f

Tfc*"-•/: r,;

' :: V

•••-

;;;-|•sTi———— -

— irNirnt IID*y 1NI*M |Day -. liWirht IIDay 1NlKht If

. ' . \

'••.'

-— '-~

iHMTted li IIMIMtf

Vr-'- 1r ".' x v II -

' '. ' II - "

11 i

.....j '.-..I '. . | "

———————VurtaMn Kind *f Mock

7Z.2

005

007

(9 T *JLJ 1 1 fiC-s^onotom? Sch i st

//*-*77*^C

Iron form

(5 '

D.U

*

-

.,................

1

tmttng ' Cw* . Tctal Brim ml Inwrtetf Dritt^ llMM*r*4 Ptptlt . •Aq*

..........:' 10 8 732- - ±':-........ '4 2 736 v. '

11 18. ' 747 ":.'-......,........ .....19 18 766 ,": ;'-

..................- ....19....... .....l.?,.,.... ,785.. ,. . ^............ 19 15 804.............— ^..1S.. ... ., 21..,:. PB23....

18 17 841.........,..., .....13 13 854...,,,...,. 16 14 870.........,.,, . 15 5 885-. ..........:. 2 4-6 807

"

165 154-6 R07

•tt

-

~—

~ ——

•T '* "

^4S3ButlM

.:'i .

..~—-

~—..

' Mn,^, . V-.-V.-.

f - ' ~ '

. ••!'-

•'— -; ——————— ...

. ^'

' ", -,—— _-._

——— -.

'

Night Runner, . ,. ..,............................. .

ntin-..

WEEKLY DRILL REPORT., . MINES DEPARTMENT

WEEK EN DI NO.. _ U.erch.JHLat,

Bupvrlntvnde

WEEKLY DRILL REPORT; ^ -:;: .. MINES DEPARTMENT ^ V

Jm No., WEEK

Bat* tmn •tt. r***KMunMl tn**rt*tf

r**t

Trtal- li.pt*

Nr*

•tt ttt*, l

Nljfht

.9Q5.-6

...3-6..9.08......

,5-6,.4-6

,3......4 .

..3-6, ,3....*..

917.923.,927-6

Nl^ht

NI^Kt

932.., 935.,

IttalfcrWMk 33-6 23 935Ui fromtpUi

turf Rtmvtu

ooi-eIron Porta

935

Day Runner,......,.?,*.....?.r,f""R.^..

Night Runner, ......A*...", f

WEEKLY DRILL REPORT. MINES DEPARTMENT •t•f-

WEEK ENDiNq.^,Aprn "lith.*.

1sy.%

f

ii.i

a , : -:^' '. ,

7

-JL-9

..10.....

...11.....

i i , ' " i •"

twrr'

o*x f-WI^M

D*;--NI(Mt

Da?

..••.'.iSSt..

Mlfint

OAV

D.yNlftit

OiiyNil h*———

•t*l Iff W**k

pD1 1i i

lii i ir

-

•urfk**

085

934

953

962

982

•ii.

Mtl

;,.

, '.

—— ....

-

-

•— :-

tun* HP*

. '

(

KlfMlvf RMk

Jeor*er nith Q little hematil

Hematite le Jasper-12' coi

Creenotor1.© "badly altered

Jasper ri t*' a little henrtH

r*M

-

bat* '

a--------

g. .......,.......

3.,...

,v

-

. '

3 -fi54

. 56-652-63-6

.....4-6......

......3-6...... 2

2

"fir2

.. .....3........- .....4..........

4..............7.,...

52-62

.........3......3-67

........ 2.,..,.

isa938=5943-6

5SE.-6 3.5.9........964366-6J.7.Q..,.,174-6.

)82 .

?82

Mhtf* Mr* . MM.

. ——— .

.....J™.

..... —— ..

...~.~

— .

— .

— .

MlH*.

——— ,.

—— ..:

1 S

UM

'. fi'--f .

..-:——

. —— .^'. -.

•— —

vlu V '

——— -'

.

—— ~~ —— .———

' v

Day Runner, ~ ....'T.O.p.? p

Nlehi Runner.P '"nfcrH'.r

^^c^

^-—— --

i•jH

Prft***-b

i

^:;--'-.'v ••'/•i-,/.' ' '.. . ••-;':-- - . : - : - ' - " ."•.'•' ' ' :' ; . ' .- '- - ; v tncit.K. : •'l v: WEEKLY DRILL REPORT ; v^^|*V".^ v"!-'' ' ' ; '' ' MINES -DEPARTMENT • ••• :'.'^;: ': . f /..:; ;j'sH,'^;.

V *W-'-'*'. . . - ' -. -- ' - . ' 9 -' - ' . - . ': * " ' v . . *". . .* ," , '* 1*--;' '-' ,- ." ' ' . - ' . ..- . ' \ : , . *, -- ', . " . - -*'. , ' :'t m.t' _ - K O ' A^ *t \ Q T?T5^T Y iT f ^T Til W * *- ' * - r/ , -. ~ , * * * , -, * ^*VO* \jf-A t -itm --n^nnuiJ -Tt--" *aj..i.. A/ 1^ tJ^/JL jLt*^ * JV i-ifftaL 1 1 ifj * ' * 4 ' * " '. ' ' ' *-

^ "' - ' ' ' , ' ' ' * " ."'s

n Ma. ' ' . WEEK ENDiNO JLnr -P TRtVi. inl^1 "', -.

il' *.' ' -113..

.14

15

™,16....

. 17

.1.18.,

imn

D*JL.'WfM~

Day

Nipt,*

DayNight

D*;rNlft.*

***xMl x to t

DAV

NlgXt

bjhvN: KM

P| TtUI ttr W Mh

pr^j

1

1

1*

1

1

1

1

1

i0(1

-'

DtpUi trwt turf M*

902.

1037

i-

M*.*r*tt* '"' '*

:'*'-^ - '

*

•UntfMp*tftMTU*

'" -.•' '. -'

- -- '

.— ~

Iron*

V* CLQP If fL*^*"^* ^-

P rt^JJL y Vr 1 ir^ni i. T*-*^^-

'3-

. . ; r..' .' ' :J

tot*

.

1

• 1

tetlnv ttr*' Tvtal *mtMu4 Urfc litMrtotf Brttli* *K9v*r** Diptli ttljy* Ml , U*

, ^ '.. . N* '••1 . r**t " rtn 4 - rMt ' , Wrt, ' Ml** . Xll. -. ' - .' - . ' *

: ' ;-- !" 4 4 ^SS •""'•"- " ' "' :V- * ' ' - - * * A A n on " v * i *. . . - s - -J ^f ** *? y* ^

'. 5-6 5 995-6 ^ "' - '

5 '4 1006- i3.5 g.g 1010- ^.

, 5 4: 1 1015...™...,..l... .3.... .......3........ .1018.. :... . ... .. ,. - j

.4 - 3-6 10223 3 1025. L

^. 3 V2-6 102a ....... ...... -3 2-6 1031 .. ........ ' '

r

1031

••mark* ' . , '.

^*

i-.

X^^UlAN.X^ ^v\

fa '\^. O 0\'jfj ' o^S 15 ^)

vi ** ^9 ^7\ \*y^sTi'525^

^^s*d^

.

Day Runner, ... ,. ,|'..'.....?.vP"'r'. c'T..... ........... ,. . . ............. ...... ,. . .

Nle^t Runner, A. *"lloie

. . . .. ,. . .. .........

1^w^^?^''^?--; -"•''"' L -'''•''•' - -' ' -'"' : ' - ; - ''••' '' '

^pwv-:; WEEVsMrit^/;--^'*-''—-- -•- .-••-•^ ' ' -S.*v r:^"K-fV;-.* . ;..:''-'--.C"-j- ' - ••'.- .' '.' 3,1.'"

KEmH 1Ir-

rF^A ' '(4. No*'^^.l.'l).' '". 'i

1*^*

^pIPX.

..23.,,

^4

25-

x*?*•Nirr

0*;'.*:.-

NI^M0^-'-','

MtfM

D*r!M±.

NI^HtP.yNl.**t*D*yNI^M

s-r.......lr.Ulf.rWMl.

toMrtpUm**:i i i i i il"**

0.1} S OCX-

turfct*

1041

1051

1054

1063

1081

1003

1000 i

lOfl-3-

1007-

IM.H.Ut.

x:y..* ' *

,.'--

—— -~

'•

.-.. -

*{^2r

. — ...;.™.,

*

Kin* of II Mk

Groen st ono 'Jrspcr and ^G./ hematiteGrccnotoneJiQper md HeTrtl toHo iriEti te

no c or e Tlo'trtlte r r.3.pJftHfcB Cherty PolBito ochlst

(b

A•MMM*

r**i

———— --

Cat*

7'vHena

,•-•' - ---

- .--•-- r-

" ^ ^ '^EEK ENDINO^PrU

"^

— — -~---.

-

-

-

NM

-fi-L ...-6 , - ; .

2-6.....5...........

5.....S.................3.............fi ......4......

.......3,,......,

.

tor*

rwt2 '7

....2, ..5

.....3.. ....

......3,....,.........,2-.6,.......4 ,............3.............2...........

Tctal

JLQ26..JP.4..2.

..1Q5.0 105510601063.10S6 1071 10751079loon

1002

Bonual ••kor*

Mr* Mta.

6. —— .. .. —

. —— . —

- — - - — -

- — - -~

MtM*.

——— ..

E— .

"' Cwh

UM

~~—— .

————

.-- ———

— - —— -

M^H. ' ' .

,-— — --

i

i b U 1

-^

-

. -- -'

" ' "" " -r '~" "s.""' "" " ' " "' ""'" "' ' " " ——— "'

(

Day Runnc

Night Rum

r, , ....A... v?ilo le... . . ... . .. .l. ......... ,. ...........,.ior, . . ^.r..^^ 0?;,.................,. ....,........... .....

/•V.^'

WEEKLY: DRILL REPORTMINES DEPARTMENT ''- *-.

JOSEPHINE MINE. DRILL HOLE NO..52.

Ci.;LAT. .....

DEPTH

DEP. ................ ELEV. ................ D/VTE............................. LOO. .....

•^;-i ;-W DIP ..........

- 'f{-:. :^ nEAUINQ

FOOTAGEFrom

-851—

.865

-866—-07-7—

' QOQ

ocjr?

-9.00-.

-9^0

930

953

961

-9.68

9R4

-1002.

1013

1033

-JLQAfL

104Q

1055

1075-1091

To

OR*^

-866—

-&7-T—

-879—

887

900—

J920—

93IL.

-.253

-fifii-

968

2B4^

10D2.

-1013.

-1032-

JLQ4JO

-1049

-1055-

1075

1091-1114

Length

T*-f

\'s'ft

,-~-~\UlJl^.^

) ;\^b^

;

ASSAY OZ.

-#38-

J/3Q

w j ^ -#40~

.#41..

#43

#43

-jB8

J49-

#50

#51

#52

Ave.

f

V?^?^J&zV-— \, —^xJS^Sf?fo -

^f*-

2&L

Â

.*ji--^

^

Wtf**ti

CEOLCXJY BY p. A. Chubb

TAV- snhint, itftln^d potre ?trft^k?-Qf frftre.i±4-t

Hemat It e, compact, reddiah-brovm,3OXJiematlta —r

Talc schist friif./itfj

-Talc-s ohis tt br ecclate3^40^-heraat-tto-e0— aem^nt

Hematite, 90jh . .

Jasper^-end-hemot it e-(SO^)— banded, —————————

Jasper and hemntitfi (40y,) bflnd^d.

Jasper and hematite (5#) banded.

Jasper and hematite (50#) banded.

Ferrucinoua talc schist.

Quartzite and .1asper f 10# hematite.

Quartzite and Jasper, 155S. hematite, .compaat.soft, a little nichol stain.

Qim* 'to nnd ja-Spor- 10^ hftrn*t.tf.a

îiu *JJtjO—eLnd^4asp^r^-brQCJ3ia±^dâ5îiQiaatltJaw. ax— aad- liema.tltai35^LôrcLJiadJx-}u^keji—

hematite content^ probably greater.

Greenstone,

JrscjBia^^spi^ and-auaru?^^

Talo achiat.

HeinatitQ t a little jasper and quartzite85# hematite, a little hard hematite.

Hematite (95-#) a little hard hematite.Chlorite soh 1st Riroy-groon, slightly talcose

v~ ' ho- ^-Ito 'n r- ^-n .MvL ^tTvn^rrj.

WEEKLY REPORT

1i irut*.

i

ir

n.

1t-B T*U

'm^^m^-j ^^- '.•"'••• : . •v'': "- •••' ;- ••••.-. ••. - ; -. - •'••- - . ; -.^'.,;--,,^,. . : . . . . : . ,.,. : . ., .^,^,,..,™*5Tji'vV'-,' 1v;i;'"S .'.' '- '..'i'- ' . ,'-'--' ". . ,. v.- - -. - : - -.-' ' * ' , - . , - ' ' . . -. -. • '.•'•'. •'•- S-*fJf-iib fc-V r *-'""-; '''v .- Y. - '.. . ' ' ' . ' -" - ' . ' ~ '' -' - -- -f r. :

R^^^: ;-\ ;VÎEEkLY.:-DRlLL--'REiib^T'-1 ' :' :^;l^^5SSwiW;f^^ ".î Mi -.MINES DEPARTMENT : ' -: ;. -;. ,-.V tv^gî

i 1 '* .'.'J-'' ^ :- . - ' \' - V~ t '•'^•' -i; - "-' ' ' 'j

-!\ ^ S

' . Batt-v---- -V '.i :

17.

18

19

20

211

O Jiy .1

Nl^t.V

0^

D.y

NI^M

Nlctit

D.y

NlgM '

D.r

Nir^tD.y

Nl*ht

HW****

I &f M*te - —— '

1 1i \ i i i i i•,.*i

:

AiV t***.

D*pth Iran

60

\9"\

347

360

i i 1

' ' '.. WEEK ENDINQ llnr.fib.-Zlfit^-il- *." 1*4

M*.*r InwrtMI

^-":; .~

"^ .

'>.'"••'•

-

.

*

.

Kind of MM*

1 s-v r

Greenstone

Iron l VV" Formation fixWS

c-

"3-'

' . \ '

- but*

, —————— ,

.-iJJU^WAA'

-•^)-

Pîlny ' 6*m Tfftrt VMMM^ ' * A ' tfaH IBBWI^B Orttwv llvoovvcvv Dvptfi vvtajw ^ * ft^t ^ IM

r*M -. KM r**i . r*rt ** \ ' *w* -I** ' 7 'ut

,....:,-L,. , 29 29 09 :;.- -.-. - -^

P Q .'H PQ ' T AV * "- " ' * . *-*'

OQ O Q T 7 fi " " * * "

,..,..,,-.— —..29.... ..,..,29,.,.. ....205, ™. . . -. j,.. .. 29 29 234

29 25 263OQ CO ^QP

1.,,,,,,,.,, ...,..29.,., .:....,.24,,,.| ,..321. , . . .. '29 29 350 ' '

.———. .... ,.,.6,.., .,.,,.,...4,.., .....356.. . - ,. ;.j-v ••'•'4 3 l 360 "

.36D.

••mark* ' :' , " . ,. ,,

.

'

~~ - J . ' ' . ' : '-

•;.- .^~ —— ^^

-. .;\V'^ "^N. ;*r " Â

...,.......,,..,,.,,..,.....,........,.,,,.,,,,,,,..,,,^

\ ^ -*" y\^ ôraV^X/''"^ — -—

Day Runner, ^ 13 *Tr. Icy , .... .. ., . . . ...,,,. .

Night Runner, A VTIlson . ...,,..,.,.,, ........

OBup*rlnt*nd*n

0

WEEKLY DRILL REPORT, * .. MINES DEPARTMENT

lot*

No. WEEK ENDIN "-

IlMn•b?

•'' Vat*

V23

24

25

26

.-JMT....

,,.29,30

*'~33*

jpw

i i i i i i i i i

*B

1

0*.3. Pur.

•Mirr

DJ^ -.;.Mliht''

D^y'i

NI^Ht

0*;

Hl^ht'

D*r

NirMOay

NirhtD*y

Nlcht

p*?r,,,.Nlcht

)*pth f rw*

360

"~s

-^ ..

InMTtMl

Kind of Koch

Iron forra

\ ^ ** C-l^s ^^J

i;

H*t -

- - ;

P.U

,

- ——— -

-- —————

In**rto4

* .IT

BrtlMI

6...fi. .1,..

6

.....6,.,...,,,,6. .™fi........

6,,,6,..,,,,.-.B...............B.............,,4,.,,. ..,..,5.,.,,.

55

t*r* ^

r**t '

55" '.4,

,,,,5.,...,.•44

. 4.........4...™...

3..........5.........

2232

Yvtal

FM*

366

384..3.9.Q....3.56..,,402.408,,414,,.420,. 426430435440445 lu*-t;n — l

=====

Mr* MM.

- •••.y" ;.. ', J .

Jv

.. ——— . ——

-— -- --—

Ml

-

•"•••--

————

.—^,

e*r*u*' Kh

-

"V *

E- — ,

-iOO 59 ...t^ii

— — - —— — --

-'-

.*

.w.,.-..,,....

Day Runner, ,....... ..... . . .

Night Runner, . -

1

...- . ..

^--^.

WEEKLY DRILL REPORT' .MINES DEPARTMENT - ; :

(Ilrjj. 71)

WEEK ENDINQ__AprtX-4±U*-12I4—19.

tMrlptfenW

Iron form

K n r*f T* w^ i *"*^Day Runnbr, .......*!.....if....-.^.'i:..T:.r.*

Night Runner, ,...A....:7.1?:.??..9.?..

Bup*rint*nd*nt

lll^ WEEKLY D RILL REPORT^.-•'y^-

•••••^\v'4î-- Â T ^16* -l- r* \ ' •J* -.iv*' *

t_,..J.D3EP.EI1I2

k I— I l—' l l l l— t-. l l L. l \^ || l l. * -' ^ r : ; . '-*X ' V ;"Jvy

MINES DEPARTMENT. /j:; V*^ V? tj^lP

;_MUTE.___..™...^ ' - \ '.-V..-V •••"' •.v//;^^.

B

1Fi v**cr

i ii i i i i1i i

ssss^z

^.6.-,..

7

9

10

11

13 .

•Birr

o./ -HirHiD.;-:NlyM

D.f

NI^M

o*yNlfffct0.x

NtffM

S**...-....

DayNl*M

.15*3*.*IptlMIOt HVM

-

B.pth fran Curt M*

500

515

522

S46-5

j67

302

•i

wu iîsr

* -

K1A4 *r Cock

Jr.sper with o little hentite

Greenstone ' [badly altered)

Jpsper with u little henotit*

Greenstone N ibndly c.lterecU

patches of Menotite

Tenrtite chertj 11 ' core

?f; i.a i to Schist

NM

-

————— - ——

t

BM*

,

. —— -. ——— .-

tntwt*d

;-p"

'

"T...-10,-,.— ™7.

7........ -.0........

n

........7..................7.,.....:755

...........S............22.......

9

"Ir..7... .

. 5..

t?

6,7g7553

1214

9

Tvtal

fMl

510...51-7-..^24531.

..537....

...5.44.....551..558

.565...570.

..575.,578590fir*4

^JL3

W?

•;-

•i-.. -- -' - :

•ttH*.

———— ..

'

.— —— .

Cwt U.

••-

'

H.mmrfc*

,;

Hole finfehofl at 613— ^'," "" -:~ ' ' """" " " ~"' 1

- .. ——J

.... ..... .... ....... ........ - ^ """::i... ~ -i............... .... .y........ : .:-:"*\" . ^ . J,

— ——

"" : ' ------ — ----— -— - :— — ---|

Day Runnc/"' t O Ntf^ht Run

...^......--.--..^r*ert .,. ^ .. 1

êpx/,.J

c

c

•i ; -- ; "—" *: ' JOSE

DRIL

LAT DEP. ..... . KT.V.V

DEPTH

DIP ....

JJEARI3

PHINB MINK1 HOI F No. 53

HATF. LOO. ....................................................

v?G ...................o................................................................^

FOOTAGEProm

331

267

269'276'

296

33 6~

34V

389

408

4~T6~

421

422

T|;45 —

453

470

490

To

260

269

276295'

336

3S7 —• -

389

408

Length

1416

421-

T32~

443

"453

470

490

W5

x— /^ ——— O

tisr

ASSAY OZ.

#1F2~

#3——

ij .#4

jflO—

//li

#6

Ave.

s-J77 Y*

/^y'r*/ /o

-flrfr

-Wft

rt-/tffe

rtV//

GEOLOGY BY p.A . Chubb

Acid rock, felsitic, very talcose, slightlyspotted with pyrite, rare hematite streaks.

80J& reddish soft hematite

Black, carbonaceous schist

Acid rook, light grey, medium grained, talcose

Rhyolite* light grey, medium grained, talcosemedium-grained

Chloritic schist, grey, a few seams of redhematite.

Cherty quartzite, 10^ hematite in streaksand narr6W bands.

Chert and Quartaite, brecciated, interbandedwith 25# reddish Soft hematite

Chert, Quartzite, brecciated, 40# reddishinterbanded soft hematite

Hematite, brick red, compact "but aof t

Schist, light green, very talcose.

Quartzite and chert, banded and brecciated —30^ reddish brown aoft hematite. - 1 ---

-SOJb hematlbuvreddlsh brown, compact, chert —and quartzite,

Brecciated Quartzite, fc schist, 2u^ hematite™Bome graphite seaas, - -

-Brecciated quartzite and schist, patchy

5# henatite.

Cherty quartzite, '65^ rod 9dft lT5matlte•"

,f;-- ~

*"' LAT. ......,...' *- *

v ' DEPTH ....

DIP ........,.

BEARING

DRILL HOLE No..S3.

DEP. .........,...... ELEV. . ............... DATE........,.................... LOO.

FOOTAGEProm

515

522

-534-

-^6-

567

"5T5

562

To522

534

546 .

567

574

~~583

617

**

Length

•?*

—7 —

^*'

---*2*7

—— -

ASSAY OZ.

#9

#6

//7

#5

^~-

^*x

Ave.

26/ti

Mftfi *

^r^yfty

^-

inL7j

GEOLOGY BY B

Schist. bro\vnish-Krev f sliahtly carbonated. ... K

Quartzite and chert, brecciated cemented 1y soft compact red hematite 140^ hftmftt-Mt.o R

JBhy-Olit-Q^-med 1 iim-grn inedylight^gre-y, taloos^^-B

Chert and .quartzite j. .brecciatedr cemented by-red soft hematite .with a few inr.hef? ofscattered black hard brittle hematite Hhematite 50#

Chert., auartzite, hracoifttRd, cemented by ..red-]soft hematite, hematite 80^ .

" " ' "jHematite, compact, red, soft, Q^ Quartz. _ l

1 foot of black hard brittle hfimntlt.*Jo^ pyrite.

Schist, liKht-.Rrey to gre-nish.sMght.lytalcose, slightly patohy, . aono ..atrfinka ofhematite at 587'

^^^^ /a ^/^y^

c

JIÂEÔR^— ri - ;^-^.^f^

; '.i,'-'-' " je";' - :vv. :'

.i*.!

MINESNES OBPA-RTIWEf ' "-'i . O

' /- x ^^ 1(.*...—....J.â(-.-..,.^rt.,t^.'* w

1.1Q 13.6.

.5.Q X6.fi .173.

Coslrtg

Greenstone

' Grey ochist

Day Runner,

Runner,... ,.V?.....^.ÎTf Icy

•upvrlntondoJ

i;^ WEEKLY DRILL REPORT|!MK:?-, l^^lf-' ^ -f;-. MINES DEPARTMENT i-."^jV^b**^'-'':'- V.V-'" '' ''- V'-;'' ' "..-.j'^i^ cji - .- ' .. •mntfnrfrrmt i *TYTo - : .

WEEK ENDiNa....,Apr..il-3,CM;h..-JL4

37~

tmn"i .W

M\fM^

Nl|fhl

NI^M

p*y.......Nlgnt

K*.** •K*

,.f...

IHMTtMl

FM*.ln**rt*tf **c*ir*rMl

T*tal P*pt*

20 23?-. .ii?!.25.6,, .262,, 26a..

T*Ulf*rW**h

DtpOi turf

Oi trmKind *f *Mfc r-*u Rcmarli*

Day Runner,.. J7. .E...5.rl.Cy.

Night Runner, .A Av|"lf3pn

Superintenden

WEEKLY. DRILL REPORT-DEPAffcBMENT

••to

JJU

.12.

JL3

.14,

16

*Hirr

NlgM

Hi/Pi*..

Nlfht

5S*..

K*. *f

EEK ENDINO HC? 16th .1914.,^ .. 1ft

.-.5.

..4... -.3-..i:...S....fi.. ...5,...s:

tort

.3, ..3,

.3..

.3..4.:

..i..

Depth r**t

369.,.. 37.3.....

.3.00..363.3.BB3.23.398.403.

403

Mr* MMb

a-

Depth frw •urtaa*

H O"*-r- 03

T r o j Y- r

.Jr.sper. .-.."badl?; ''roJron...up*.......r.locfis....of.....core.....,. .,,,,,...Kenera 1.?x...un.cl.e.r...2..7....in..

Hole cc y 1 ng - n q.. r e t. rir n ...v?..Holei cemented.,.SPttir.day.,.tp.,.be.. ..ste r*el ."'edinendr;;, n.orni.. ..M . M . .^.,

Day Runner, . ' ..'.....rr*.*....

Night Runner, A. "1?3On

Bup*rlnt*nd*nt

DRILL REPORT, : . MINES DEPARTMENT

. ' 4 " 4 - . ' *r - "•/yT* ""ffT? l*. ' -*-*-~- i— .*"*~.-~.. .^ —......-I-" 6'

l -B V-?'

iif

-— J1^,....'..L..

p;"v** '" '* '

2

3

?,

i*r . . li . fi . .fi 6 ,

. - - - - \ . *v' ' f l ™

•Mirr

BsLl.NlffHtDay".'.-'*

Nlffttt'

SSX-...Mljftvv

OAV

HirntDAV

Hl^ht

D Ay

Nl/x^t

.P-r......NlRht

|B^*UI f *r W**lc

Jl^car-

l l l i l l l

•"

-

)epUi Inn •urfae*

442

^74r

485

409

501

i

•f

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JOSEPHINE MINE DRILL HOLE No.54:

ELEV. DATE........,.................... LOO.

DEPTH

DIP ..........

JJEAKING

FOOTAGEFrom

ZSZ——

244306 ——

3JiO

346,—

37CL-

406

426^if

464

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490

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1

GEOLOGY BY P. A. Chubb

Greenstone... ——— . —— —————————————

Handed quartzJtO nnrt Jr\npor^ X^'/ ^ hPTTint.t t.p—Bandfld^QuarJizito nnd . Jnapp.r., hrfiflr.1ate.rt7 ' 15* hematite;- -^'Banded quartzite, brecciated, 25# hematite.

Brecciated Quartzite and jasper. solutioncavities, 65# hematite f core badly broken.

Brecciated mitrtzitft and jasper 50^ hemntit-^broken coro.

Hematite, (905J) compact noft.

. Quartzite and jasper, streaks of -hematite.r*

Quartzite, 50# Jiematite, 5* of^core misalnw.

Tftlc^Qfihist . •-

.Hematite, 80#, soft, compact t

Talc schist.

Tuff, li^ht c;rey-^tsan, slightly spottedand slightly streaky.

i

- \1

f

C

Hole Ho*

11

12

Drift

Vr-'VV \'*- ;V"v'

;' ' '

AHAIYSIS OF' ^ tf*" 4 '

1 . - - f ** '-'*, - '-

j; . - .- : ;'j,V';V;fi' -

- Depth'"-;-,-' - . .*-'.--.; .j? *

y.']- ^ ': ' '.356'"'-. ' .* -' ' r - '."'•'. -

363

369

476476 ~ 485485 - 490490 - 495495 - 500500 - 505505 - 510510 ~ 515515 - 520520 - 525525 - 530539 - 540648 - 653653 ~ 658658 - 663663 - 668668 - 673673 - 678678 - 683683 - 688688 - 693693 - 698698 - 703703 - 708708 - 713713 - 718718 - 723723 - 728728 - 733733 - 738738 -743743 - 748748 - 753753 - 758758 - 763

0 - 44 - 88-12

1:1 - 16i:. - ;;o;:o - ?A:X- - Z BS5 - 37

)rift

* t " * "- —'- . ' '. -. '' '- - 1"':-' - '.:

' : , ' V ' "' . - - ' -

DLAKOND DRILL- ' , .. - -* i•- ' '-- ~ ' •-••- - •••' -/;V- :v i:;*V'-; -:" i, . - - . t -\.. . . -j Material'.- ' ' ^.~"A..v".. -'

Sil .^Hematite; ' '. *V ''',- '; ' ,' . . '.' ; . ir' 'n' ^ ]

11

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CORES FOR*

.Fe.

18.44

18.51

15.62

24.3515.6516,5815,7214.4032.0317.69

- 14,8317.0415.3516.5217.1917.9114.4715. 8622.1523.2016.7416.6720.2013.8114.1216.9716.5920.0319.0815.1313.6017.9114.8415.7220.2014. "G16.821 C. ^^ o . Vvu

46.6527.0715.5911. -1111. -;?IS. 2324 . 83SI. 6131.61

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Angle Depth

tRITT GORDON MINE• x - . '•V -' '.'-' ' - . -' ' "' '.

DIAMOND DRILL REPORT

Started Finished J

Plan No. Section No. Lat. M204- Elevation

Dept.

No; .SHEET No. 2DEPTH

TO

i7S'0

'00-0

&0-0

DESCRIPTION ANALYSISKO. Vi. a? 1NSOL

o

':

•SVCe/fv rye

•f 233-f

SHEET No. y.

^ HOLE No. SHEET No. *.

DEPTHTO

DESCRIPTION ^ ANALYSISNO. ,

55v—

fft/'S

2W-S 29*7

Z9Z-7

or a*4t*s.feu3 *f*r-rjin PX.o646tY GAIPWr/c., 4rf9t-3 ^AssfS strt* wwrr foiotfa s9f'0#of*s.

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3 fo -35/-0 3SJ-Q

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49-0Z

3t9'o 770-1

vsre-o ^ w ' AB OUT/O" f t*

72- JS

' HOLE No. S.l. SHEET No. .5

f 1 3-0

S7S-S mi.ro

9f*X,.A*'f*ssjv*HfS *pvs)t}rz. s/fT-ir/vf t f s*?fOHr"7 tftfD,

rue*

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-92-00 21- f Z

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ir i- HOLE No. S.l.

..;;"li^.-Z.J.

i f *'

.*.**. UTO. WU* '

SHERRITT GORDON MINE


Hole No. ,S.*2. Strike ^. 35***,'C.

. , f-o' j***AngleS:::^: Depth 724*0*

Started Finished

Plan No. Section No. Lat. //5-7/-0 Elevation

n . Uept.

C)

o

C r

(i

C:

C'J

DEPTHFKO.MI TO

49-0

6-0

DESCRIPTION

QUARTZ.

7/-OKS3

r/'op^-jro

, o t. stss y

ANALYSISNO.

s? 7-

x.r

ro

cu. 7.V. AU. AO. 1NSOL.

t V.M.LTD.M1** v

SHEET No. Z.DEPTH DESCRIPTION ANALYSIS

NO. CO. ZN. AU. AG. INSOL.

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SLIG-HTt-Y

C O/)/? 3 A

/Ir 9 f -s /^ -v?"

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No. S.Z- SHEET No. 3.

if C)

C

o

c

c178-S 20*c

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c.it>

DESCRIPTION NO.

cvr ayf '/tt. * o

TO t: 0*9*? j f.

0tfff M/Gf/J. X

70* mor f,- //•9S

l ?J CO |i.

l

fi^-'^HOLE'No..**-•i-f ' ' — A'.';.; . SHEET No.x';x,.; DEPTH

iPKOM TO

C r

DESCRIPTION

TtJffA t 'f 'OO 'J. Afteror

NO.y ANALVg -/^J^r

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P2S02. 1*92 7/4?

Jt/J'J

313-S J/7-0 iki.; jo/ry 4T3,3.s'*o*,Sj~V*rirx. B4-70

3/7-0• ? IS- So 7Z-49

3203 323-C

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JASPfffY HftrtJ

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NO. ^5;.ANALYSISweet..

O

mP

49*-* 497-0im.*A5

497-05*0-0

lS5&

i

H

ffjMSfJt-o

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DESCRIPTIONNO.

5T7-S S9I-0

iSo'S* TTTTlaH im

to-7-Z•4Q.OS

T&T& ana607-0 6/0-o6/0-0 6/Z-

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^j JPf*7**tSr'0JF# -rsA/ei Bf. '*CC'A^93- 33-A-? •OIO Of

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6'0-t* 627-3

pfe S/fSVArtrf,

t&rtffao-sj

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, Sf*' f* S' f 40 X r A ft ft fUOT'Tfi

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Z-46Z • oe.o

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^*34 -Off

s? f 4* 6s3-6s9. f,*3S3. t f-48 77-25 •074 • 04

(,1,3- PZ3S+ 07 4 3- 5-2 •Oft •o/Z • 04

ssv e? J? f c s*S^'Q Y/Z'X .

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FOAM** K.AC.L.TO.MIM

tl^XHOlJvNo. .SHEET No. 8

699-0 7X4-0

4*3

DESCRIPTIONNO.

/7 {/j? f* f? G e

y T1//

W66

'O/ ft

•073

No. &.Z - SHEET No. Agfcl-DEPTH

0

O

C)

o

c

4B5

5oo SOS

585

590 J&5

5&S

(.rt

Q

6,5

620

6zs

fos

6*y

DESCRIPTION

J-JL isx* G.

KO.~ ANALYSIS ^ ^^..5-oj-^i?——jo——*c2L

^323

P2325

PS32?

9-85

27-62

24-39

4&-OS

- SI

45-74,

4/-2S

47-70

69-02

S0-4&

(,0-ei

27-29

2B-33

Z9-OS

2 S- 7 4

21-53

47-21 Z43Z

•096

•or s

•070

•07/

•063

•/0 +

•007

•97 f

'8/0

3-344

'017

0/6

• 0/9

• 0/7

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•2*

•20

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2o

•2o

-/a

/X

• 09

•07

.09

- * AC. LTD. M1M

'

..

SHERRITT GORDON MINEDIAMOND DRILL REPORT

-Tx?oxy-e.

Hole No.Strike *5!A i o.o'- 75 LAngle ZJDO-O' -yo*

400-0 - -"Depth *x*o * 76*4-'

Started Finished vt,y 9

Plan No. Section No. MD. Lat. x/^56-6 Elevation

D

0 DEPTHFMO.M TO

DESCRIPTION ANALYSISNO. CU. 5".N. AU. AO. INSOL.

/•J

c 1-5

tl-7

ZZ-o 27- /

o

C)27- / 995

o

ssv

ft/

/•S ' To /J- 7. SOT-S/

#rf*f-9JeAf*cc.

.SHEET No.*P? v DEPTH

IFHOM

'^\~\^.•''''-: -*: i"''j'

TO.

Zoi-5

DESCRIPTION ANALYSISNO,

l*

//v

cu. ZN. AU. INSOL.

•SHEET No.3.

PttOLE No. SHEET No..*.DEPTH

FROM TODESCRIPTION

(see •;

ANALYSISNO. CD. ZN. AU. AO. INSOL.

.SHEET No. 5".

c

C)

HOLE No. 5-.S SHEET No. T:

6***

DESCRIPTION

to s r

641-5^4*0

6*py &S3S

tf+t I'-Hi

664-0 602-0

~ZTftfr

4* H/tT*/ S3?4e-y-

ANALYSISNO. CU. XV. At". AO. INSOL

Hole No. Strike

0.0 '

Depth

SHERRITT GORDON MINE;-.i-S ^/••x.-vv-V; •-•. " - - ,. DIAMOND DRILL REPORT

Started *xi*v*f 20 Finished S

Plan No. Section No. Lat. //f72-- Elevation

9770-/

c

o

DEPTHFMOMI TO

O-O

/•f

3/-Z

ff-Z

DESCRIPTION

ssr

NO,

ANALYSIS nm.

SHEET No.

C.

o

o

f/Z

DESCRIPTIONKO.

i

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o

TODESCRIPTION

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KO.ANALYSIS ^

JSP^^V'-^-'-" . . No. *.*. SHEET No.-

iSfr - LP-EPTH:

G.

o

o

301 1,o

DESCRIPTION

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TffAct/yrf, yfey

Cf r- fi y SW* *

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SHEET No.DEPTH

O

o

c

464,-

TODESCRIPTION

ro-060-3 -

NO.

f&rotsst *. t f) o ft r s c s*rs*-rrf4,

/o J r-

ANALYSIS

SHEET No. 6.

S.A*. LTD. HIM

HOLE No. SHEET No. 7

l j-TO

507-5

DESCRIPTION

COS? f..

NO. W.V*#Vrt r*9Otf*

,WI5 *9^0 20-49 f 7-94

EZZ

r ft f rt A -r/-re. Jf *M* MSI rtf f f-id

//e*rt T/rf ju* 36 w/ r// n/ffy or x", J9-+0

G-fCY QlSjffTZ.

6*7-5 Gffey

'62 7^^6*03 j f* f f ut /)ff 30-79

t: Off E.

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l) 4lg*

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f r- t: o*? f.

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39-07

67*-)G-#fY ro Krss/rf ftr z. /0& M f MAT/ rf .

Oft!* M •.•B. LTD. MIX

HOLE No.*5.-5t. SHEET No. to.

880-0 092*

DEPTHFROM TO

DESCRIPTION

/o s r cox*.

ANALYSISNO. et). ^2 -ff-

t&frt INSOt**

093-Sff*S-C ffffy t /*f f o* iff* f/jxa /004- /y -/s

O/o

P^/vP ?oo o xxvr e w** W t* 05AV of nSfti f?/ J r*! A J* t*.

9oo-^ Pw/'j' - 900' /f -f -t9o* s 9oS-0

c: 9o5-o 9*9-of/ 007 69-04

9/0-0 9/3-0 r /o i 6 12-16 79-70

9'3-o f/ 1 1- f e f f t o s 7*0 Go-//

9/g-o7-0 9/7'- 9/a'avr 7*'^ Mrs** r* rf . f/oto 31-97 y 9 -

t*/ 1 1/ f- f Z 70 of

o9Jt-o 36 06 44-fto

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979-6 903-2

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lo f -r f****.

rOWM M *.fct, LTD. MIM

i^y^ HOLE No.- r "-" SHEET No. /XDEPTH

FROM TODESCRIPTION

NO. CtJ.ANALYSIS

IWf.

107* - 903-2 43-30 •007

990-0 994*

to t -r ce*#*i.

fj*4n-jur TP 97*0'- P&tt OfO-

f^ 'JAJL.t

996-9

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: J3-9* 38-00

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60 .r?

60-43

'OS

HOLE No- s- SHEET No. A?.

FROM TO

O

DEPTH DESCRIPTION

S/rttJ.41? •r*)(,

si BOY x. t -r e.

A ess r***/*

NO.rtr *.

7- ea

ANALYSISAA.

S&+IN9OL*

t/OZ-Z 32-&S •t37 • o/ y

loZ-2 60-6 Z009-0 rt tt f

Z222/ot-' /JtO-e

II to -f-fo

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S. 3 . Kidder

O. C. MoCartney

November 15, 1944*

Cojamants end Rnconaendatlons In regard" to investigationof A.O.P. ilairaa adjacent on West Side of the Josephine Property,

1. The extension westward of the Josephine iron formation cuts across the north' side, adjacent to the north A. O. P. property line, of the nore easterly of two claims and across diagonally froa northeast -to south west the raore westerly of the two claims. . ,. .

2. The iron formation is not exposed on surface across xhe more easterly claims. The extension westward of the Josephine iron formation across tho noro easterly claim is limited to an area which does not exceed o. width of 100 feet. Across the metre westerly claim, tho iron f creation is .exposed over a width of about 400 feet. The exposed iron Tornation consists essentially of banded silica. A trace of siderite can be seen but no honatite is apparent on ourface.

3. In the area about 100 ft. east of tho northeast corner of the property i.e. on Josephine property, information is available from threo old i diaiaond drill holes.' Holes Nos. 12 and ID drilled southeastward frora the north Bide of Parks Lako intersected banded silica and hematite . The entire zone is about 100 ft. in width and along the eouth side of tho zone- there is- a tand of hematite 20 feet in width.- The log of Hole No. 12 shows tho grade of the horatite to be ?e - -56.3jt; SjOg - 19. 6^

Role No. 12 cuts the hematite approximately 560 ft. vertically bulow Gurfhco and Hole No. 19 cuts tho hematite e.pproxi;..ately 740 ft. belov; surface. Hole No. 21 drilled, northward from the south shore of the lake intersected iron formation over a ritl'th of 100 ft., but no hematite is noted. This intersection is at a vortical depthof 350 ft. and thus, is considerably atove the t'.vo which contain hematite. '

Those intersections also Indicate that tho hematite obtained r.oy be De much ti3 100 feet north of the northeast corner post of the property.

4. Mr. y.orrlcon, Geologist for Josephine, htis definitely established th-3 presence of ea ir.portr;nt cross fault wiiici; tronds e few dogroes uost of north across tho oast end of their developed hen^tito orebody. This fuult is VBrj' fcizilur in rotative position ar.c bohfrviour to Fxiny of thooe roco-;nized ut the Flt-len .iino. The vlriter rcco-ni?.os certtin f-,!at\:roD tj'.-.ich sur—uot- t'-.o possitilit. 1 trnt tinot:.far cross fc'-lt ir pro ra r t in tt. c t.re.. roar the -.:at end of i-r.rks L-.i-.u, ?ir.d thus tie or.s t .u ...0.. . oJei^s, :-.f.d t is fduti:r-3 :-.." ..olp

l-^ : : o." -^ ::-itu or, t\ - s.-.:-r. :e -id in "o] o o. ^1.

I

l

lx

l l l l l l l lll l l l l l

- B -

5. Ta the writer*s opinion, all evidence available leads to the conclusion that the cost attractive possibility for the location and development of a banatite orebody on A.O,P. ground lies in the Investigation of the extension of the Josephine zona at considerable depth. ' ". .

6. A preliminary progrtn of investigation will involve two, and possibly throe drill holos. It -is reaor^omled that one hole be placed about jdLdway across the noro easterly clain No. AS 743, and drilled northwestward at an angle of -65O , This hole v.lll bo a ainir.ua of 1,000 feet in length nad posslLly of greater loagth because it is known that in drilling frcn south to north the holos flatten rapidly. A second hole will bs placed in the southeast part of the s;ore westerly clain Ko. AC 743, and drilled north westward at a similar angle and footage. Those two holes should serve to show the extent of possible inprovtinant at depth and also, if spaced as suggested, should serve to test the quality of the zone on both aides of a possible cross fault. A third holo may be necessary supposing either of the above hcloe ore lost throurh too nuch flattening or through intersection of diabase r onunbor of s ra 11 dikus are Known to be present in the eroa.

It raay be necessary to follow the preliminary drilling progress outlined above ?.lth doupor drilling jrovidsd it con be shown that an important improvement in structure end grudo takes place at dopth.

GCL:cC:I3

S. J. Kiddor Hovenber 15, 1944*

l

l

l

l

l

l

l

l

i i i i i i i

O. C. KcCartney ' :* - . *

Coniasnta tmd Reooeaendations in regard to investigationof A.O.P. bin. ins adjacent on Tfest Side of the Josephine Proporty.

l* Tfeo extension westward of the Josephine iron fori"**lon cuts across the north side, adjacent to the north A. Q. P, property line, of the nore easterly of two claina and across diagonally fros northeast to couth- wo D t the noro westerly of the two claims.

*

2. The iron formation is not expo so d on surface across the more oastorly claims. The extension westward of the Josephine iron formation across the nore easterly claim is limited to an area which does not exceed a width of 100 feet. Across tho roare wostorly claiR, the Iron formation la ' exposed over. a width of rsbout 400 feet. The exposed Iron fornation consists essentially of baodod silica. A truce of si dor l to can bo soon but no henatlte is apparent on surf tee.

3. In the area about 100 ft. east of tho northeast corner of the property i.e. on Josephinu property, information lo t.vnilablo froia throe old' k dlcusond drill holes. Holed Nos. IE and 13 drilled southoastv/ard fron tho north eido of Parks Lake Intorauctod banded silica und hor.ntito. The ontiro zono is about 100 ft. in width und aloag the south side of tho zone thoru is a hand of hematite 20 foot in width.'- The log of Ilolo No. 12 uhows tho jrude of the horatite to bo Fe -.56.3J&; 8^02 - 19.65*

Hole Ho. 12 cuts tho banatite approxinatoly 560^ ft. vortlc&lly bulow surface and Holo Ko. 19 cuts tho hematite tpproxi(*toly 7^0 ft. bolo-s surface. Hole No. 21 drilled northvîrd Iron; tho south shore of tho lako Intorsoctod iron forrîtion ovor a wi.ith of 100 ft., but no hor^ntlto Is notod. This intersection la nt a vortical depth of 350 ft. and thus is conoidornbly QI ove tho two which contain htmatltu.

4

Those interr.octioas nlix) indicate Uiat tho hdr-ati to oi'tnlnod soy be os much 03 100 foot north of tho no-theaut cornor post of tê property.

4. !!r. t'orrisori, G-JolDîst for Josophino, hiifl definitely estnbllnhud tho nrostnco of an Ir.: ortf;nt uroso fault v/l'.ic}; tror.do a fo-.v d o?; roe s 6t;st of north across Lho oact ond of Lhelr dyvjloue-d hs:^tito orobody. Tnis fault is - vory si.T.ilur in rolutivo position anc hohr-.-iour to rony of vhooo roco-ni-.-.ud ut the Helen 'iir..;. ~hc .-.riter rocornir.os cart',in features nhich su~~ost t'r-o pOEslbilit- tr.at anot-ior crons ff-lt ir r-ror, irt ir. tr.c uro-.. r.cur tho v.'.-st und of 'r'-rrts I.r.Ko , and i-::uc uo.-^r.n t. -o .'..0.. . ujni'.s, ::'d tiia fduturc; .fly :ic-lp --o ox:.Jfiir t-. d i: ' :r-.;:it l,.::, o." -u.r.titu or. tv . j r.urfi oo -.'.d ir. ' r olc "o. .''1.

Vll' "l

l l l l l l l l i i i i i i i

- 8 -

5. In the writer*a opinion, oil evidence available leads to the conclusion that the cost attractive possibility for the location and development of a hematite orebody on A.O.P. ground lies in the investigation of the extension of the Josephine zone at considerable depth.

- 6. A preliminary progrta of investigation will involve two, and possibly throe drill holos. It is reco:mr.onded that one holo be placed ubout nidway across the aoro easterly claim Ko. AC 743, und drilled northwestward at an angle of -650 . Thia hole Till bo a minimum of 1,000 foot in length and posaiuly of greater length because It is known that in drilling froa south to north the holes flatten rapidly. A second hole will ba placed in the southeast part of the core westerly ciaIn No. AO 742, and drilled north westward at a similar angle and footage. These two holes should serve to show the extent of possible improvement at depth and also, if spaced as BuggQsted, should servo to test the quality of the zone on both sides of a possible cross fault. A third holo nay. be necessary supposing either of tha above coles tire lost through too isuch flattening or through intersection of diabase r abunber of small dikes are known to be presont in the troa.

It may be necessary to follow the prolindnary drilling program outlinod above with deupar drilling jrovicusd it oiin be nhovrn thut an important inprovonont in structure and grude iakos ploce at dopth.

^ .-' 'f o h t (l (f

\f J fVWA/O-/ MO H f .'() A/C'//".!',/

'j /v/ / ,-

/v o x *.- A/-:/ j x y

L/'/J. M^JdQUd -J V O V/ W O O 7 V

l

March 8 , 1945,

JOSXFHIN2 KTTSNSION

Summary Results - P.P.H. No* l

Hole Started ~ January 7, 1945 Hole Conpleted ~ February 19, 1945.

Bearing Dip

- Northwest. - Surface - 64O 1000' - S36 1400* - 330

Aver. Decrease Dip O - 1000* - 3 - 18* per 100* Vertical depth ore Intersection below Porks Lake 780' i ,Excellent quality siderite oro obtained between footages1083.5' - 1192.5' n 109' . 88' horizontal width.Good quality siderite ore obtained between footage 1033.5* -1239' - 155.5' - 125' horizontal width, (except for presenceof one greenstone dike 14* in width.).Apparent dip of formation 83O Northwest. Total depth Hole 8 1503'

1^f^'life--:--::- ALGOMA ORE PROPERTIES, LIMITED

EZSSNSIpN

A.O.3O

Diamond Drill Report?^v*'-r''HOIJe No. l '' '

STRIKE N 30* 39 W

] -.^Kr.' ANGUS ,. -644 .

1503*

STARTED Jan. 7/45 FINISHED Feb. 19/45

PLAN No.

SECTION No

UAT. DEFT.

ELEVATION 1170* 4- 40*

Iri11J1111111bI1i

DEPTH

rwonj TO

0

28

65

. -

105

145*

185

204

225

265

310

345

SfyS

28

65

105

145

1B5

204

225

265

310

345

365

3^

-

DESCRIPTION

Casing

Tuffs, agglomerates, bedded fc sheared,chloritic.

Bedded fragmental, probably broken agglora,Rock - gradually be coaling lighter incolour owing to development of sericite.

As above except more chloritic againqtz frags, fc silic. rhyolitic lens-shapedfrags are numerous in certain sections.Trace of qtz. "eyes" TO present.

Vol. fragmental, ma . large angular milkyqtz. frags in chloritic schist, grdniass.

As above

Finely banded sericitized rhyolitic rockTiny parallel lens-shaped frags 'ofsiliceous material are abundant.

As above except passes into brecc. phaseof above rock type with one 4' sect. note(of distinctly fragmental material.

As above, fine banding continues fc alsothere are short sections of fine frags.

Chloritic phase of tuffaceous fragmentalfine banding present as above but rock i odark and contains small wisps k lensesof very dark chlorite in t l istercoloured grdmass.

Chloritic os above. Eere the frars. are H coloured K. cherty in a chloritic rjrdinass.The fra~s. are lens-shaped u are parallelto the schistosity.

5oricitir.od rhyolitic phase.

ANALYSIS

NO.

V

10*

r*. m I NSOL. j

.~r --

i

.*

ALGOMA ORE PROPERTIES

HOLE NO. l SHEET NO. 2

ji

fci i

- DEPTH

ritoM

395

425

465

516

524.

545

572

593

605

619

619.

621

623

TO

425

465

516

524

545

572

593

605

619

619.

621

628

640

i

i

* DESCRIPTION

Chloritic tuffs, finely banded or beddot numerous email lens-shaped light coloured frags, is 1st. 10'.

(juXv/fvU. section of sericitized tuffs, very fine banding, suggestion here k the: of cherty frags, are present

As above - qtz. sericite schist.

Chloritic tuffs iTith scattered metacryst of black mica - ottrelite

Chloritic tuffs with very fine banding

Chloritic tuffs as above

Chloritic fragmental with numerous tiny frags of light cherty material and few qtz eyes are present between 580 - 593 qtz eyes are round - are they frags? Probably introduced type fc rock can bc a chloritized phase of qtz porphyry.

Finely sheared fc schisted "qtz. eye" rhyolitic qtz porphyry

Chloritized section of sheared fi: schiste qtz. porphyry.

.2 Siderite and W/^ qtz. , the qtz. may be filling fractures in the siderite

Finely banded fc. very fine qtz eyes, seri porphyry.

V.'oll defined wavy contact of fine raassiv siderite v/ith finely banded qtz. eye roc Siderite, good quality, light in colour fc, does contain a lot of ;.ilky qtz strgs. The other contact is similar to abovebut in this instance it seoms very appar that tte siderite contact cuts across thschistosity in the fine qtz eye rock.

Finely banded qtz. eye pyroclastic, 3i.^ht in colour, v/ith sons carbonate

ANALYSISNO.

e

:itic

•*

jnt

r*.. m

\

• lOl

-

'

Hw



•Lj -ff- -itllill1*l11*ili

. , 5=5DEPTH

FROM

640

647. J

653

665

675

712

731

742.

765

805

845

TO

647

653

665

675

712

731

742.

. 765

805

845

r* f: '

1

JT^-

5

1

DESCRIPTION

t

Chloritic and sericitic schist with.numerous very large "qtz* eyes"

Siderized fine qtz eye pyroclastic

Siderized fine qtz. eye pyroclasticwith 3 -or 4 - 1' sections well siderizedand one has the impression of sidori-tebeing introduced and replacingfavourable bands. .'

Finely banded and fine qtz. eyecarbonatized pyroclastic - sideritesections are not defined

Sericitic and chloritic schistsintorbanded with siderite bands 1/4"wido parallel to schistosity and other ostringer type which definitely cut across schistosity. No abosiPqtz'. eyeslast 5.0' seems more siderized.

Chloritic schist section with numeroustiny parallel light coloured rhyoliticbands and tuffaceous bands and at timesrock almost suggests a platy chloritetypo of horizon.

Well defined light coloured sideritewith milky qtz. strgs. mixed wi*hnumerous tiny irregular black schistsections.

Chloritic tuffs with few narrow sericitibands 1" - 2" wido "Bill Uorrison""Intermediate Tuffs".

Ihloritic and sericitic tuffs interbandedis above av. about 2" wido.

Chloritic and sericitic sectionsintorbandod as above. The sericitic sections often contain qtz. end look as ifmaterial has be^n introduced. I-'orriconsu~j;ests a rhyolitic origin.

Chloritic tuffs with only fow sectionswhich arc partially sericitizod.-

ANALYSISNO.

*

.

rx.

.

'

mss

t ,

BlOl

-

MN

-

-

-

! 1*0,11* KIM*


HOLE NO. SHEET NO. 4

•ft"'.

lg* .1i11 1

1s111Jv^1JI1

V11

, , DEPTH

raoM

885

925

986

1015

o?*vV

1036

071^

.03 Zli

1095

1105

IID

TO

925

986

1015

1023J

1036

1071

1083;

1095

1105

1115

ii i

r 12

li.

10'

10'

10'

DESCRIPTIONX

Chloritic tuffs as above except there ar*fragmental sections in which 1/3* - 1/4" frags of qtz. are present and alsosome cherty frags are present;-

Chloritic fragmental with at least twotypes of. frags, one cherty and lightcoloured and the other black and cherty.

Sericitic fragmental phase of tuffs.

Chloritic and banded with some bandssiliceous.

Sericitic and fissile schist, veryfine grained.

Chloritic and fissile schist, very darkrock with suggestion of light colouredfragments oriented to give a poorlydefined banding - morrison 1 s basictuffs. Occasionally there is a lighter coloured section which appear brecciated with the lighter coloured materialpossibly introduced*

Siderite stringers and bands parallelto schistosity of very dark (black)chloritic schist. l*he siderite seems toinclude1 and surround frags of the black

(1082 - 10d3^)Contact of balck schist and sideriteThere is only a trace of black schistparallel bands in the siderite in thissection

i Siderite, f.ood quality light incolour with^abundant strgs.. and seamsof pyx boTfc D M at c mixed i^ 4/nte^chalco.and both very fine grained. Here andthere are scattered tiny bluish qtz. "eyes" 1/10" - 1/8" in diameter.

Siderite ay above

Siderite as above

Siderite as above

ANALYSISNO.

*

19116

19117

19118

19119

1912C

rt.

28.10

34.49

36.1?

37.99

33.0"

*

-

1.43

4.14

5.37

4.06

9.52

• lOl

'

16.84

6.54

5.60

4.63

6.92

MM——————

1

-

1.86

2.36

2.32

2.43

2.17


lil l ii i

l

HOLE NO. l SHEET NO. Si,

DEPTHmoM—

1125

1135

1145

1155

1165

1175

1185

192.5

'

stoke.*

1215

TO

1135

1145

1155

1165

1175

1185

L192

120*

} 12

L225

" .

10*

10*

10*

10*

10*

10*

57.5

.814.:

58.2

10'

DESCRIPTION

Siderite good quality light in colour

Siderite good quality light in colour

Siderite good quality light in colourand heavily mineraled with very finepyrr. chalco and magnetite

Siderite as above

Siderite as above

Siderite as above

Siderite as above with one 1' strg. ofqtz. x

- -

1192.5 - 1193.8 Hetadiorito withfuchsite in evidence.1193.8 - 1194.7 - Siderite1194.7 - 1195.1 - Metadiorite1195.1 - 1195.6 - Siderite1195.6 - 1206.8 - UotadioriteContacts between siderite and metadiorit*are difficult to interpret. There is awavy line contact with suggestion ofadvancing fronts. by the siderite in one jinstance but nov&i of the /time it is impcto say which is the later mineral andagain it appears they are simultaneousThere are numerous tqz car. strgs. cuttithe meta. but they are all very much qtz\7ith only a border of carb, xtals. The1E06.8 contact of the siderite is wellbrecc. for a length of 2.0' and thespaces between the brocc. lightcoloured siderite is filled with a deepgroen rather fresh appearing, chlorite.

2.0' brecc. sideriteHcnainder vary heavily pyrrhotizedsiderite.

Siderite heavily mineralized withpyrrhotite as above and also there are afev; 1/4" round areas of qtz.present.

ANALYSISNO.

19121

19122

19123

19124

19125

19126

19127

19129

nessibl

B

19129

19130

rt.

37.00

33.56

38.80

40.94

35.99

34.37

33.58

9.70

36.43

39.00

B

8.0:4.51

8.65

5.60

6.05

2.49

2.29

0.06

8.92

10.21

• lO*

6.36

7.52

5.44

4.70

7.50

5.56

7.28

36.92

12.74

6.8

MM4ST. 'i aa

2.21

2.13

2.31

2.56

2.27

2.50

2.42

0.49

,

2.07

2.1

ass

i *

0n.

r*)^*v

'


HOLE NO. l SHEET NO.

^1 J j :; -

J^wSf- " -m~ ,qVW V'•l:' -

1l11111i1

i1)**r

b|)

11

~r"Vi 1.i . t — J-i— - DEPTH

rnoM | TO

1225

1239

'

1245

1253

1265

1285

1305

1325

1345

1355

13G9

137-3

123

-

1245

12^8

1265

1285

1305

1325

1345

1355

1369

1378

1537

) 14

6*

13'

7'

— -"- — DESCRIPTION

Siderite fairly light in colour andwith tiny mag. xtals. scattered throughothe 1st. 6.0* and the remainder is veryheavily miner aled with pyrr. ! -and finechalco.

l.F. Siderite and qtz. The qtz. ispresent in strgs. or bands ^" wide andsome of them seem to be cutting the. siderite. There is carb, assoc. with this qtz. and probably introducedtogether. This material may be the sameage as the qtz. carb, strgs. in the meta

l.F. Siderite and pyrr. with fewscattered bands cherty qtz. and fairamount of chloritic schist alsoconsiderable mag. throughout. - -

l.F. - Abundant bands of cherty qtz..ittle siderite and trace of pyrr.Jhloritic schist scattered throughout.

l.F. well defined banded silica about3:1 qtz. and siderite - specs, at1267' and 1234'.

l.F. as above except ratio of qtz. tosiderite almost 50:50. Banding is fairldefined but upon close exanination thereis seen a fclzzy contact with tiny xtalsof siderite qtz. in*the qtz. in form ofislands adjacent to main sideritecontact.

l.F. as above

l.F. as above

l.F. as above

l.F. interbanded qtz. and black cherty i.iate^ial with abundant rous, andsome pyrr.

Platy chl. or fuchsite dike.

l.F. - qtz. and nag. as above.

-

i

ANALYSISNO.

19131

19132

191K

19134

r well

0

re.

40.01

28.71

23.65

22.75

s

16.42

'

3.08

'

10.01

3.13

BlO*

4.36.

-

25.32

17.06-

40.62

,.

MMisa

1.83i" H ^•••^i.

.

1.58

-

1.41-

I.**

I'

l ALGOMA ORE PROPERTIES


P0x-' i'.

P '". .;:.y '

f"'?;' ;

. ;''*

11

1

1

l1

1

1

Q

™

b

bf)

11

DEPTHFROM

1387

392.1

1402

.423. 1

1445

1483

TO

1392

140

1423

144-1483

1503

'

5

.

7

i

DESCRIPTION

Fuchsite dike, fairly well schlsted last1.0* is black and contains numerous tinygrains or frags, light colouredmaterial. :*

I.F. - Interbandod black cherty mag. andpyrr. bearing material and light coloureicherty qtz.

Diabase dike, fine to med. grained, freslin appearance and contains few tiny qtz.carb, strgo.

I.F. - Interbanded Black cherty mag. andlight coloured "qtz.

Fucnsite dike, wisps of fuchsite fairlywell defined and occasionally anattempt at forming an 8 sided green clusis seen. (Metadiorite) - Well definedpatchy, green chlorite clusters in acarbonatized quartzose probably ;uffaceous rock. A number of the chlorit clusters are distorted octagnal-shapedareas. Spec, taken at 1451' which shows

i well formed 8 sided chloritic area andcentral part of the area appears to bejarb. quartz rock same as that injurrounding area. These areas definitely:ut across the schistosity of the rock.

[.F. ~ Banded nilky qtz. a trace of sidorLn stringers and seams is scatteredthroughout and often shows a feathery:dge effect where it replaces qtz. i few black cherty frags, are present in tho milky qtz. (

DIP TESTS

Collar - 64" 500' ~ 47 0 100' - 62" 600' - 4E0 200' - 13" 800' - 38 C300' - 5-4" 1,000' - 33" 400' - 50" 1,200' - 33*

2 .D OF HOLE

ANALYSISNO.

*

;or is

,he

to

re. m SlOissc

-*

'

JOS3PHINS EXTENSION) ; ^v

Karch 29, 1945.

SIMiftRY R550I/TS ~ D. D. H. NO.2.

Hole Started - February 23, 1945

Hole Completed - March 15, 1945.

Bearing Southeast

Dip - Surface - 70ODip - 1400' - 380 30' '

Aver. Decrease Dip O - 1400' B 2O 15' per 100'

Vertical Depth. Intersection below Parks Lake s 778'

No ore present in core but in section 918.8' to 940', there is a mixture of siderite and schist with trace of the iron formation quartz member. Trace of siderite is present within schist to 957.2'

Apparent dip of formation 72O30' northwest

*

Total depth of hole - 1445'.

li l

ALGOMA ORE PROPERTIES, LIMITED A.O.90

- . jifo JOSSFHIN^ EXTENSION' Diamond Drill Report

HOLE NO.

STRIKE

ANGLE

DEPTH

S SO0 E 39-?00

1445*

PLAN NO.

STARTED Feb. 22, 1945. SECTION NO FINISHED March 15, 1945. LAT

ELEVATION 1170*

DEFT

11111111iiiib1im

OBTTH

F*OM| TO

0

n

60

80

125

160

250

262

280

320

11

40

80

125

160

250

262

280

320

263

DESCRIPTION

Casing.

Greenstone, fine to med. grained with in numerable tiny carb, itals scattered throuout.

Greenstone - {3.0* lost corej - as above,considerably broken.

Greenstone - fine grained, dark green fcschistose not carbonatized as in sectionsabove ,-

Sediments - Interbedded gwkes. some slateybeds Bc chloritic beds. Section is very fingrained and exhibits very fine parallelbanding.

Sediments as above. Possibly the seds. arvolcanic nmds and niay even have some interbedded volcanic flow material also.

3JLaty chlorite section - may be metadiorit type and def. does cut across banding in tjeds.

Jreenstone, fine grained with few shortbanded or bedded sections in evidence.

[nterbanded greenstone fc seds. , fine grainschistose. Two or three .3' bands of qtz.iye rock are present, may be porph. rhyoliir qtz. porph. dikes possibly. At 266' thLs a contact in which the qtz. eye rock cuacross the schistose structure and at sametike t r. ere seen to be a few tiny "qtz.eyos within the schistose rock.

[nterbur.dod greenstone l;- seds. , fine gr?iir;r.d r.c istose. Li^ht rrey in colour v:ith

ANALY0I*

KO.

3h-

)

i

ie

:d

-e,:re-S

t

:fl

fE. j m INVOU

,

•'SH.HfclM(J^'W;. v^.'.


'^ HOLE NO. 3 SHEET No. 2

faH

it"™ ;

f'/'

— -1WM^

1

gO

1

I

f

1

|BLmL|*^f

1jl

DEPTHrnoM

320

340

493

524

529

533?;

558

562^

585

500

562

TO

3^0 {

493

524

529

533J!

558

552;?

535

600

662

732

i

cont

7

DESCRIPTION

,) trace here and there of fine banding.331 - 333 band of qtz. porph. similar toshort sections described above and at 32?bhero'ia a ..4* section of qtz. porph. whi definitely cuts across the schistose struin the grn. Also 321-322^ there is a secof fairly coarse quartz frags, in sharpcontact with grn. schist.

Sediments, slatey rocks in which schistosseems parallel to banding, ^tz. eye bandsfew inches wide are common and one of theat 449' contains ^n frag, of cherty qtz.

Seds. as above, except have been ratherthoroughly sericitized into light te. darksericitic bands. Last 4.0' of section iscoarse gra'ined, contains pyrite seams andis not so thoroughly sericitized as sectiabove.

Tuffs - coarse tuff or aggloro, coarse qt!frags, and frags, of shist ^" -' fj" indiaiaeter.

Uetadiorite with scattered wisps of fuchsand abundant vein qtz. ffi qtz. carb, strgsasaoc. with some of original rock remnant

Seds. - partially sori citized as above.

Metadbrits - fuchsite dike. Platy chlo.schistose type.

Seds. - dark fine grained givke type, butbedding rather indistinct.

Greenstone, fine grained with -distinctgrey colour.

Grn. as above v:it.h few tiny flakss whitemica and nany srall irregular milky qtz.and qtz. carb, strgs.

Grn. nore typical fine grained and dis tinctly groen in colour.

ANALYSISNO.

-t

3h jturetion

ity

Q

OD.

i

ite.s.

rt..

•-

i

* • lOl

-

MM

.

l M*.

ALGOMA ORE PROPERTIESHOLE NO. 2, SHEET NO. 3.

g.pi1J

l11115Hii11D

WL?

1fm

1

DEPTHpiton

732.7

783

859

J13.5

518.8

930

940

950

TO

783

859

913.

818.

930

940

950

957.

957 .'^ '.)35

j

S

—

)

LI. 2

10'

10'

' 7.

- —

DESCRIPTION

Grn. in fairly woll defined contact withcoarse mottled chloritic typa,' alraost a*isetadiabasic type. 709-710 i a. a sectiongrey lava caught in the Coarse, possibly trusive type. Both contacts are well de fined in this instance. Can the not tiedtype represent an old dike, or sill betwflows?

Grn. typical fine grained as in sectionabove, jneta. type. Last 5.0' of sectionlighter green in celour and appears to hbeen altered by the diabase diko v/hich ipresent in next section.

Diabase dike, contact is well defined buhole cuts flike at an acute angle for adistance of 1.0' from 859-860, shows conalong core. Last 3.5' of coro seeras alsoto represent a contact section. The diabdike is wed. to fairly coarse grained anexhibits typical diabase texture of the"younger" type of dikes in the area.

Sericitized schist talcy and light brownor buff in colour.

*Iron fortcation - poorly defined and

seems *,o represent a siderized sectionwith o.uly scattered* frogs, and tiny bandof cherty quartz mixed with the siderite927-928 contains few seams pyrite

Siderite and dork schist mixed. Sectionfrom ^31' -^32' appears to be fair sideribut remainder seems more like siderizedschist with only a trace of quartz.

Schist with interbanded sections ofsiderized material. The bands consist ofvery dark schist and of sideri ze^ buffmaterial and are ^~ to J-" in v.-jdth andalternate with ons another.

l Chloritic ar.d sericitic schists withinterbanded mottled areas of siderizedrock.

Sericitized pyroc)ustics v.ith nu .ber offre.^s. scattered t,hrov.~hout.

ANALYSISNO.

a

ifn-

sen-

.3ivei

,

•act

isei

*

Samp]19137

i

19138-e

19139

1914C

r*.

a24.69

20.08

10.74

.

13.75

m

4.17

0.57

0.53

0.67

iL

1

•tO*

29.40

*

36.40

46.24

43.63

-™^-——— *.™—

MN

1.37Fe .

S .SiOgsKn .

1.07

.5S

.7

-

ri~m

' H

l

•j

22. 5|2.4|

32. 7 11.2J

H

l

* Nft, tt*.—•t***


HOLE NO. 2. SHEET NO. 4.

*#':.'••'-

1

1

i

lh

DEPTHPROM

985

1000

058fc

,

.067&

1120

11V9

1203

.295. *

.316.6

TO

1000

-

105&

1067

1120

1179

1203

1296

331

133

2

..6

i.B

DESCRIPTION

4

Sericitic and chloritic pyroclastics int*banded. Numerous cherty frags', in sectioi993' -999'.

Chloritic pyroclastics with few sericitiband .l 1 -. 2' wide. Number of very small icarb, strgs. are present. Frags, of milk;qtz. are scattered through the chloriticrocks.

JJetadiorite dike - both contacts are welldefined and in the upper contact one off!or branch of the chloritic material trencinto the pyroclastics. One or two faintlji sided chloritic crystals noted, and al;suggestion of chilled margin .1* side. L!cof section is the patchy chloritic type !to the Helen Ifetadiorite.

Chloritic pyroclastics tendency toward '"basic type". Suggestion hore and there cpossible bedding and number of qtz. carbFew strgs. and g" sections of carbonatiz*magerial practically a siderite.

Chloritic pyroclastics with few strgs. o:silexite type of material. Also some qtzcarb. strg. material present.-

Chloritic pyro. above gradea into a ligdolorod phase of pyroclastics with scatttiny xtals of ottrelite present and alsofew tiny crystals of pyrite in cluster.

Chloritic pyroclastics similar to sectioabove last one. Qtz. carb, strgs. are nuSection 1239.6 - 1242. 6 and again from1257-1262 appear to be intrusive rhyolior silexites.

::etadiorite with very many qtz. carb, stand one 1^,' saction of milky qtz.

3 t z. eye tuff, eyes of qtz. are large l/1/4" in a ir^trix of sericitized pyroclasThere ore strgs. of silextie f:nd theoccasional frag.- li KG type which may represent roplaco.-ent of a l'ra~. by silexi

ANALYSISNO.

r-

edtz.

.

hoots

ostimila

i

fstrg

d

terred

ierous

os

•gs.

:" -•ic.

e .

rg.

. .

s • lO* MN -,gs

.

|||^ ALGOMA ORE PROPERTIES .*M HOLE NO. 2. " SHEET No. 5.^^h '3y 'P'

1*

1

1' -,.'

1

1

1

1

1

1

,

1

i1

.DEPTHFROM

L339.J

1360i

1380

TO

136

1380

1445

)

DESCRIPTION

Serlcitieed and carbonatized pyroclastic interbanded within tiny chloritic sectioQtut. eyes are present, but are , very fine grained. Most of the light banding seems be due to introduction of rhyolitio.orsilexitlc material.

Chloritic phase of relatively fine grainpyroclastic.

Sericitic pyroclastics with trace of bedibut no obvious fromgonts or quartz eyes.

- END OF HOLS -

Dip Tests

Angle Tube Connected Angle

Surface 70O 70O 100' 72 0 690

' 200' 690 660 300' 630 590 400' 600 560500' 570 540600' 540 500700* 52O . 48O 800' 540 ' 500900' 5ii0 510

1000 ' 530 490 1100' 500 450 30'1200' 47030' 4301300' 45030' 41 01400' 42030' 380 30'

-

ANALYSISNO.

8.

to

td

ing

t

r*. m • lO(

s

.

f

-

MM

'

'

,

r

-

-'

\'\ ' V 7^%'r \:\^^^ \ S*W3***te \ ^^ v, ^^,? r(\V'^+^W"''

i.'*'

?. -^^AC 743

/' V'X\f\\'X1C 7^/\ -. (V) o /MV: N

'a

V \

f, C' O* c t

r t :.

.J *.)±,

'l. .-

COMA ORE PROPERTIES

Diamond Drill Report

STARTED

FINISHED

" DEPTH j

ntOMJ11 ' —

TO I

l

———

V DECOR

x. n.\sX /O -

)l'1 * J 51 f' 3-*

,.o? X /O

PLAN No.

SECTION No

LAr V', - . ":".

ELEVATION . ,' .

DEPT* - v- -r

ANALYkl* ;:--

NO. re. IN90L.

X9/3?

BB

39 V6 o.t7 V/-67

"l

ppas

.-••*

"t':-

;- .

••'-••

'••-•;

-i-,-"

o. -.2

^-:-'

" ni

^x^

^^-

-c 2

--:

ODTh

--"

'-

"T

:^^

*

lir-3^

-i ,* O

- f

^w

: tj

,-^

^-^

;;^

-'•-.

'.'

- -.

-

-:-.

^"i

^

CN

JTN

fY

,

^O

l ^

^^

: .:-

^-,::

. ^

•---^

in-. .

-.^--

-".

-" 2i?^

J*30

n

•^ -^ '^

*ON

-

•-N"

*^ V

!:

l^fe-

- .'•-'"

^

•i'*

*-

GO/v)/)

.'* ' ' ' ' * ' *"' -' \etopfrRTiGS: -:.

' :.

. * ? \^^

50^0

^ X

. vi

(^

l^^^S •S5l

;?^

c- ^ *

(B

TV

>S

J0

^.-^ n* -v ^

.^Ift

\0 ^

-n

•^r^ n

^^

N^

tt;

O.rj

,,

^

0 •^

1^1

t^l

^1

^H

ll ^|

3

^^

i':

.-..v.

-to

171:' Q

--

^

;-4T

^--

- l^

] |^

J' -

'-; -

. '

,-:

- - ,

;^

(f)

O

Lo ;

tD

"^

O

i 5

i I-

-I f

ei;-l

i! m

w?--

.

v

w)

v-

v ty

M

^ n

^ ^'

-- 'i

* 2

- -- -.

- -.

v;

- fV

. -. Q

v.

.~^ i

^1 ^^

--'"r

h*

r* f

r T1

'; r

^ ^*

' ^

- -

Oi ^

Oi-r

v

^ ^

O)

o h,

0 *

5: i--

.C

lA

lA

^: -

CL

- - ; .

' - -':'

0 ^

-*

V

*.

- *

*-

'--'

-

. - ^ —

——

——

'

..'-

r

- -^

X

- .-

*

- .

-.-

"—

,

- -

^.' *

'

* ,-

V;"^5

-0 ;;

••::

4- .

r .

:-.'

^ ^

.-':

l o

5, ^

. .

r*'

; -

^

- -

V^

Inl

C?

^^

^ -

fi w

*

*

- .

'

.-

-'

*

-

:" -

' .

"N- :

;;..-..

v.v ^

"

' '..-

.- ~

-'~

'-'

,- .

- . '

-- '

— -

i'T'"-;

': :^/

"' "'

-' '"'

v.'-:1-

^. -

'•••".-

•••"s-

^—

'

CJ/

^

^ Z

-*•; t:

* iS

0*4^

* *

l

l

l

JOSEPHINE EXTENSION

April 11, 1945.

Summary Results ~ D.D,H..No* 5

Hole Started - March 18, 1945 Hole Completed - April 6, 1945.

Bearing Southeast

Dip - Surface - 68O Dip - 1000' - 610

Aver. Decrease Dip O - 1000' s ^O per 100'.

Vortical Depth Intersection below Porks Lake a 673'

One important oro intersection obtained between footages 673.5' - 825.8'. A second ore intersection was obtained between footajes 972.5' - 1037.0'. The intervening area between the two ore intersections is nade up of banded siliea, siderite end greenstone dike material.

Diabase dikes were intersected both above and below the ore intersections and then interfere with ore continuity.

Total depth of Hole - 1216'.

ALGOMA ORE PROPERTIES, LIMITED A.O.30 l

^^ ECT3NSION Diamond Drill Report"HOLE No. . 3 ' : - .

STRIKE S SO0 39* S

ANCLE -68O

DEPTH 1216*

STARTED ilarcb IB, 1945. FINISHED April 6, 1945.

PLAN No.

SECTION NO LATELEVATION 1170*

DEPT*

Wt^^M ' r

i

iiiiif1 -

liilol(ii

DEPTH

FROM

0

12

40

L15

L66.E

221. E

J40

260

32C

TO

12

40

115

168.

221

240

360

320

596

3

.5

B

DESCRIPTION

Casing

Greenstone, grey lava type, roed, grained icontains abundant tiny carb, xtals. throuf

Greenstone, med. to fairly coarse grey la-vwell carbonatized in many .sections and hejfc there few tiny qtz. s^rgs. The developraeof xtals of carbonate If continued much ftTould give an ankerite rock.

Greenstone med. to fine grained and characby develop, of scattered xtals of green otTVTf frfoffg TitTf^ "T'nT'Tft'Y*"' fm f\ ' "T*Y^ Tfl rm'TTlT'All F\ ~f*rtf\ t

association suggests netadiorite. Upper ccis not as well defined as lower, but againare strgs. of qtz. carb.

V

Greenstone, grey lava type r.ed. to fine giand does contain some tiny carb.-, xtals seethroughout.

Iron Formation - bonded silica necber. Blabanded qtz is partially replaced by milkyThere is a truce of siderite present and tara numerous bands and strgs. of both pyriand pyrr. The actual contact with the lavaIs obscured by a 6" band of nassive pyrite

I. F. - i'anded sil. as above withanunber obands of pyrr. and a few 1" bands of sider

[.F. - Banded sil. as above. Ti.ero are onlfew s"-l" bands of siderite . l.'ost of thebands in the qtz. consist of pyrr.

D. F. - os abovo plus tendency for re.raantjf rroy schist to bo present. Pr.sss bands:ot readily recognized because they are ci)urtially to ."Ji^nttite. Lost O' of sectio•.vir.ly Lundod -:ilscy qtz. fs i r. 3 O..3 sectio.i -her in hoi o.

ANALYBI*

NO.

ndhout.

iQtr the rt

.erizerelitt*.\S

ntectthere

ainedbterec

Jk]tz.leret,e

'.te.

' a)lack

landsire.nc-edi is:s

FK.

C Ai*fu

m

J}

IN*OL.

-


HOLE NO. SHEET NO. 2.

i l l

l

l

il ib br- ii

-

1

-

r

)1*

I Z - - ; ~- ' ' ' — - ~

DEPTHritoM

396.8

417

513.5

673.5

680

690

700

710

720

730

740

7-0

7 c:

TO

417,

512

673

680

690

700

710

720

730

740

750

750

770

~

5

5

6.5'

10.0'

0.0'

.0.0'

10 JD

10 JO

10.0

i

10 JO

100

Ij.C

Basic igneous material, probably a basic dike and appears to have the patchy chare usually present in the metadiorites.

Iron Formation - banded silica member. Ft sections are very dark in colour and are* cherty in appearance, but do retain a schistose structure. Apparently the qtz. has replaced an old schist. Some sections the qtz. are thoroughly brecciated and ai present in a matrix of pyrr. and magnetit bearing schist.

Diabase dike - 1st. 12.5' of.section is e somewhat schistose basic rock not recogni as diabase. Last 50.0' of section is age schistose phase not readily recognizable diabase. However, central protibn is med. grained granular diabasic rock relatively fresh in appearance. It is apparent that cuts diagonally across dike to give the v sections of contact material obtained.

DESCRIPTION

e with considerable pyrr. and trt of fine siliceous'material.

Magnetite, fine grained.massive as above. Strgs. and seams of pyrr. are. present.

Magnetite as above*

Magnetite as above except is dull in appearance and is softer and thus nay contain more siderite than sections above v;hich are closer to the diabase dike.

Magnetite as in last section

L'a^netite as above

:,'.a?yiotite as'above- except seor.is to bo :.'.oi siderite developing or at least more in afidenco. Pyrr. continues to bo scattered throughout.

Mnctnetite os in Itst section

ilivnetite cs ir.- Iri.oL sectio::

. .i ts ir. l:.;-,t section :r.u in addition list ij o:" nappies is :,c.ir.ly siderite. .

ANALYSIS |NO.

cter

W

ofee-

zablein as

t

i core

'ide

;C619141

t

19142

L9143

: 19144

19145

1?146

C 3

19147

19142

19149

19150

r*..1,

'

44.87

42.08

40.64

43.49

38.64

37.61

35.73

36.62

37.23

24.99

* 1

\

9.04

4.34

4.83

5.69

2.99

2.30

1.65

1.70

1.65

1.60

•to*fe

\

7.62

10.24

13.76

6.54

9.68

7.74

14.72

9.24

7.20

7. iS

MM————— SSE

-

1.68

2.87

2.74' Ye

2.72lin

2.54

2.45

2.^8

2.44

2.5S

2.43

-37

* O

ALGOMA ORE PROPERTIESQ3 -

feif" i t-.:

—33*Jti!fr"mirtiii•^fiiiriife

\ji_c. INI* - . &I-IC.G.53- DEPTHntOM

770

780

790

800

810

820

825.8

833 .S

850

861.2

870

eeo

692 .2

307.7

TO

780

790

800

810

820

325. f

333.8

850

361.2

870

880

2922

307.7

915

10.0

10.0

10 JD

10 JD

10.0

5.6

13 .(

\\--i-

11.2,

M

|0,0

12.1

15.?

7. S

DESCRIPTION

Siderite with numerous seams le. clustersof pyrr. and also contains numerous seamslo feathered streakB of fine magnetitecutting through the siderite. ''It seeas veapparent the mag. is caused by ths diabatdike.

Siderite, oxcell. quality, light incolour but does contain many tiny seamsand clusters of :nag. and trace of pyrr.

Siderite as above

n rt it

n tt tt

tt n n . -

Iron Fornation1.0' schist, soft grey2.5' banded sil. and siderite2.0' schist, soft grey7.5' banded silica" and siderite.Uuch of the banded sil. is brecciated

and has pyrr. and siderite in the matrix.

!.'etadiorite with trace of fuchsite atupper contact.

lietadiorite as above.

Siderite, fair quality light in colourwith two sections of bonded sil. .2' &.4 1long.

Siderite, light in colour and fair qualitFew very siml! frt.gs. of qtz. in evidenc

Siderite good quality, light in colourexcept for last 2.0' which containsabundant ir^gnotite. Tnere are seains ofKicg. with feathered edges present throu.~!out sections above.

Lamprophyre dike, contains abundant tir.jplhtes v:hitD r.iea or.d considerable cerb.

siderite1.0' i.-.ernctite

.5' chloritic schistg. Q' Man. and sideriteo.cv siderite fair quality

NO.

19151

rye

19152

19153

19154

19155

19156

19157

19158

19159

19160

19161y.3.

19162

-

19165

191C4

r*.

36.80

35.59

34.96

35.57

34.58

34.80

25.06

7.00

31.60

34.70

-

35.60

35.50

6.60

34 .k)

1 MO. " -""-' ' " "i"!— L/, . .li-.ii li in* • L.MI . im^m^

ANALYSISm

r;

3.89

-

2.^1

t

1.37

1.24

1.96

2.82

1.20

\

0.15

0.16

1.52

1.86

2.03

0.10

1.86

••o*— — 5.56

6.28

5.36

9.26

7.60

5.18

46.00

48.96

25.03

11.34

6.40

6.00

49.10

9.40

MM— 2.42*

,

2.38

2.44

2.19

2.25

2.30

1.76

0.19

0.32

2.16

2.25

2.33

0.25

2.33

ALGOMA ORE PROPERTIESHOLE NO. 3 SHEET NO. 4.

DEPTHPROM

915

922

932

942

956.4

963

972.5

980

^990

1000

1010

-

1020

1030

1037

1045

1054.

TO

922

932

942

956.4- V

963i

972.1

980

990

1000

1010

1020

103C

1037

L045

LO 54

t 106

*

7.0

10'

10*

14

6.(

9.5

7.5

10. C

10. (

10. C

10. C

10

7.0

8.0'

1 9.

0 5.

r"*r**zf*pip*TirtKi * Ufe9v*nlrTI(sn ***-*

Siderite' goodquality, light in colour.

Iron Formation, banded sil. and pyrr. \ :with few bands siderite.

Iron Formation, banded silica with pyrr,as above. Last 2.0' is heavily miner alized with nag.

4 Chloritic stalcy schist probably anoriginal tuffaceous rock.

I.y. .- mainly cagnetite with littlesiderite and few pieces of brecc. milkyqtz.

LSetadiorite dike. . .

Magnetite and siderite with few carb.qtz. strgs.

Kagnetito,fine grained dull lustre.

Magnetite as above.

Magnetite as above.

Magnetite as above except in additioncontains two sections:1012 -1013.5 of a peculiar feldspar1015-1017 porphyry with black grdmas

and with some magnetite in evidence;

0 llagnotite as in sections above last one

Llagnotite as above. Hock is covered wit]a bl^.ck sooty material which rubs offreadily. Possibly t prolably, c nanganeimineral such e.s pyrolusite.

Chloritic schist, probably an old sm.restnent.

4" Chloritic schist as above.

6 t'agnetite v.ith tre^e of sil. fra^s. Zcrock is coated v.ith fine black softpowder. Possibly a r-.t~e Mineral

•Hx^.

ANALYSISNO.

19165

19166

19167

19168

19169

19170

19171

19172

1-J173

19174

19175

s

19171

19177

o

19178

19179

191BO

r*.

34.62

24.22

28.47

n.8i

34.22

9.01

38.93

*o.*8A~t "A.

41.74

42.34

29.83

42. 6^

45.70

7. -20

11.40

45.04

m

1.22

2.16*

3.12

0.58

1.48

0.66

1.78

MtIv99

1.98

1.43

1.22

4.92

4.25

0.16

0.38

1.00

••o*

4.72

47.34

37.56

24.30

t

9.86

37.94

8.36

C.**•4-rfS-

4.76

5.32

30.92

5.70

5.62

4'',. 48

50.94

9.22

MM

2.33

1.29

1.55

0.86

2.52

0.35

2.74

a.1?rr r\T O.vll?

3.03

3.00

1.75

FeS

Si02 lin

2.67

2.16

0.39

0.71

2.28

401

8

p ALGOMA ORE PROPERTIES


m\Hk— -L

W1 1 ' 'H ~^'-;l'

S1iiuK.-J

l1i

®

fi.

•- V. DEPTHrnoM

1060

1062

-

TO

1062

1216

-

-

DESCRIPTION

Chloritic Ehhist and nagnstitic material about 50:50.

Di abase' dike:Beacuse of fairl7 coarse grained chara

of dike, it is apparent that hole is folcentral portion of a dike which is trendapproximately parallel to the hole.

2ND OF HOIS

Dip Tests

Surface - 68O ' * 100' - 700 660 200' - 69OC 630300' - 66030' 630400' - 65OC 610500' - 650 610600' - 650 610800' - 64030' 60030*

1000' - 650 610—

-

ANALYSISNO.

t

terowing

ing

re. ~-

-

9as

-

SlO*

-

-

MN

f

'

t

:

:

to

oo

o o

\p M

)

Uj

;^.'--;V-V

---1;'";" •;-V--

- .'••-•',.-: - •'•'*~-

-. :-

v ^ :; - -

VJ

N

krr Q:

o

o

s

o: k

CQCi tl;

1

OK

^QC o

V)

S^^S

^Jvy--^'-,'"f

Ol!

y**iO

l .i t

' ' ' *;7./ x y •••'/v///,

f; wo

E-FV "^ -

wv"-i'-*p:-v**fy':'fc-\ . .

JOSSFHINE KXTERSICN

April 20, 1945.

Summary Results D. D. H. No._4.

Hole Started Hole Finished

April 8, 1945. April 12, 1945.

The hole was stopped at depth o*f 431* because

j continuous section of diabase dike was obtained fron 2&8.5 1

to 421' and it seemed likely that hole was folia?ing strike

of the dike.

r ALGOMA ORE PROPERTIES, LIMITED

'•^jossanm EXTENSION

A.O.3O

Diamond Drill ReportHOLE No. *

STRIKE S SO0 39* Tt.

ANGUS -65O

DEPTH 421*

STARTED April 8, 1945, FINISHED April 12,1945.

PLAN No.

SECTION No

LAT*

ELEVATION 1170* -

DEPTT

1

I

ri1

iiiiiii

(ii

BIT

FHOM j

0

10

182

J48.7

261

288.

TH

TO

10

182

348.

261

288.

3 42

)

DESCRIPTION

Casing

Grey lavas

Rhyolitio schistose lava

Iron Formation, inter banded silica andpyrite similar to D.D.H. No. 5.

Iron formation, interbanded silica andirregular siliceous siderite stringers.Actually there is very little real si der!present. (267* - 273.5' consists of brownschist of metadiorite type.)

Diabase dike.

- - -

Hole stopped at this point because thorseemed considerable likelihood that hole following strike of dike.

HO. |

be

)vas

rt..

-

ANA

- 1

LYSIS

INSOL.

Isr^;.-.' M:

JOSEFH3NB EXTENSION

May 14, 1945.

Summary Results - D.D.H. No. 5,

Hole Started Bole Completed

Bearing Southeast

April 13, 1945 May 3, 1945.

Dip Surface Dip 1000'

- 650 .- 580 30*

Vertical Depth Intersection Below Parka Lake 1010*

The main siderite ore section occurs at the contact

of the Iron Formation with the "Wawa Tuff" similar to section ob

tained in D.D. Hole No.l and suggested in D.D. Hole No.3, except

in thet instance a diabase dike interfered with obtaining a complete

section.

Two sections of diabase dike were intersected above

the ore section.

Total Depth of Hole -

ALGOMA ORE PROPERTIES, LIMITED


A.0.30

STRIKE B SO0 39'BANGLE -G5

PEPTH aOOO 1 t

PLAN NO.

STARTED April 13, 1945 SECTION NOFINISHED May 3, 1945 LAT DEPT

ELEVATION 1170* -•1 s /Z"i-tf-

itiiiiiiiii1i

DEPTH

PHOM | TO

0

11

65

138

148

L89

L91

260

S25.5

537.4

355

361

n65

138

148

189

191

260

325.

337.

355

361

380

1

380

04.6

64.6

cii -

J04.

664

70^

L

6

r

DCAcnirrioN

Casing

Grey Carbonatized lava.

Grey lava, finer grained and darker thanabove. Contains many qtz. carb, strgs.

Grey lava, crystals of carb, are veryprominent. Also few xtala of feldspar prei

Grey, lava, fine grained and schistose.

Grey lava with trace of green micaceous rawhich nay be a poorly developed fuchsitic

Grey lava with numerous tiny qtz. carb, st

Rhyolitie schistose lava. Contact wi th lavabove is gradational.

.Iron Formation- Banded silica and massive;::ained pyrite interbandod in proportion 5

[ron Formation - mixture of brecciated bansilica material in matrix of siderite. ConJiderably more qtz. than siderite present.

Siderite, fair quality light in colour.

Cron formation. - Qtz. frags, with sideritis in section above.

iron formation - Intimate mixture of qtz.md siderite. Definitely too much qtz. pre-o give section any value.

)iabase dike- Both contacts are fine grain md lower contact is schistose.

:.F. - well defined banded silica. There aluroerous dark coloured siliceous bands whiire dark because of presence of mgnetite.

ANALYSIS

NO.

ant.

terlalhorizc

rgs.

as

Tine):50.

led.

i

'rass.sent

id

•oh

r*.

.

* INCOL.

BBBB

' 1IiEBBBBBB

imm1iERRIE

1li:\."

fii':"1

f1111\11iiiiPJitii

y HOLEDEPTH

FROM

700

132.3

142.5

J47.5

*60.7

975

986

1000

1011

1020

1030

1040

1050

TO

832.1

942.

947.

960.

975

986

1000

1011

1020

1030

1040

1050

1062,

ALUUiyiA UKfc fKUPEKTIES

NO. 5. SHEET NO. 2.

t

i

l

14.:.1.0

9'

10'

ft

10'

10'

3-1

DESCRIPTION "

I. P. well defined banded silica intorbanwith black te. dark green schists. There imagnetite scattered throughout- the schisand some contacts appear to indicate thathe magnetite-bearing material is laterthan the silica and partially replaces i

Diabase dike.

I.r. - fine grained massive mag. with trjof siderite. It is apparei i. v le is foil*contact of dike.

Diabase Dike - contact is well defined apartially schistose.

Magnetite and siderite - excell.. quality

it n n rt it

Dike Rock - contact again slightly schlsand distinct possibility exists that entsection from 986-1011 should be classifias metadiorite.

oJike rock but not exactly seme as above-this type seems to contain chloritic duand near contact contains 1/8 -in. pheno.of carb. This may. be the'metadtorite rocktype.

Magnetite and siderite, very fine graineand excell. quality.

I. F. -Fine grained mag. fc siderite blackin colour. Section 1028-1029 composed ofmilky vein qtz.

I. F. -1030-1035. 5 sid. tt mag. as above.1035.5-1040 chloritic schist with traceof siderite and noa. of tiny qtz. carb.strgs.

'Chloritic schist with numerous tinyinetadlorite, irregular qtz. carb, strgs.,sono pyrr. fc. some siderite replaces theschist.

J '.3- Chloritic schist with suggestion herand there of the patchy or mottledappefirance of metadiorito.

ANALYSISNO.

od

' *

icewing

d

19181

19182

.osereid

ters

1918?

19184

1918E

19186

)1918?

r*.

-

39.80

41.12

38.19

33.79

23.74

30.23

6.35

i

1.32

1.17

1.98

2.87

9.43

7.74

0.13

fliO* -

8.46

7.52

15.56

19.86

24.00

27.26

48. 5C

MMi

2.79

2.75

2.67

2.3C

1.6E

1.19

0.2?

f

*

-

ALGOMA ORE PROPERTIESHOLE NO. 5. SHEET NO. g.

•^•:f

i1111

f11iiliiii

DEPTHmoM

062.3

1070

1080

1090

r

1100

1110

.. ,1120

1130

1140

1150

1160

1170

1180

1190

TO

107(

icec

1090

1100

LI 10

L 120

1130

L140

1150

1160

1170

1180

1190

1200

7.V

10.(

10jD

10'

10'

10'

10'

10'

10*

10'

10'

10'

10'

t

10'

DESCRIPTION

'-Magnetite and siderite - trace ofquartz in tiny bands.

'-Siderite and magnetite - sections of siderite are partially banded.

Siderite, fine grained dull grey incolour with trace here and there ofbanded structure.

Siderite as above, grade is only fairsince some portions of core seem to barelatively light in weight.

Siderite fine grained black in colourbut not particularly high grade.

Siderite fine grained and very dark asabove with fine mag. scattered throughoit

Siderite fine grained and very dark asabove with fine mag. scattered throughout

Siderite fine grained and very dark asabove with fine mag. scattered' throughout

Siderite and magnetite, good quality fitgrained and dark grey in colour.

Siderite and magnetite, good quality firgrained and dark grey in colour.

Siderite and mag. as above1160-1166.3 -dark in colour It, contains

abundant magnetite.1166.3-1170 - light coloured siderite

contact between dark tt. lightis gradational over .9* lengof core.

Siderite, light yellowish buff in colouand good quality.

Siderite, fair quality, some streakschloritic schist present.

-Siderite as in last section.

ANALYSISNO.

19188

19189

19190

19191

19192

19193

19194

'

19195

e19196

e19197

19198

\

h

19199

19200

19090

re.

37. V

34.8;

32.03

37.39

38.39

37.68

37.59

35.03

35.85

40.38

36.94

33.14

33.55

34.13

s

2.2(

0.28

0.21

0.31

0.93

0.90

1.86

1.25

1.28

l.*P

0.87

0.71

1.08

1.28

8.0.

13.70

21.14

•^8.72

12.82

4.54

6.94

7.58

21.48

8.26

5.76

5.24

6.00

5.82

5.32

MN

2.47

2.06

1.96

2.41

2.44

2.56

2.54

2.43

2.56

2.52

2.51

FeS

Si02Mn

2.23

2.14Fe

SSiOo

Mn2.11

M

•1

j 1i l

•36. t- 1.2- 7.?. 2 . k

•Z

i

I.]k. t-18.1- 2. i

^

'

Ir** w*, it*



mf -

lmm1iFiiiii

DEPTHFROM

1200

1210.

1220

1230

1240

1251.5

1B60

1273

TO

1210

1220

1230

1240

1251

1260

1273

12S©J32^J

10'

10'

10'

10'

.5 -

8.5

* DESCRIPTION

-

Siderite with numerous streaks ofchloritic and schist present.

Siderite, excell. quality - light incolour*

Siderite, 1st 5.0' excell. quality -2nd 5.0' contains number of

chloritic seams.

Siderite, good quality. There are a numbof dark areas but not much magnetite.

LI. 5 - Siderite, fair quality light incolour with one .5' qtz. band.

Agglomerate vi th fair amount of sideritein grdmass. Frags, of rock are ^"-1" indiameter and appear to ba grey pyroclastwith track of ottrelite. There is littleif any, siderite in the fragments.

Agglomerate as above with only a trace osiderite in grdmass. A number of quartzand cherty frags, noted.

Agglomerate as above, passes into "qtz.pyroclastics "Wawa Jfuffs"

- Hfl) OF HOLS -

Dip Tests

Surface 65O100' 650 200' 610300' 600 30'400' '600 500' 600 600' 600800' 590

1000' 580 30'

ANALYSISNO.

19091

1909Z

L9093

srL9094

.9095

1909f

C3.

-

jye"

rt.

30.15

24.26

31.57

31.75

31.43

16.31

,

m.

2.92

6.66

1.91-

1.85

1.99

1.66

• lOi

15.28

31.48.

12.26

11.42

8.72

34.96

.

-

MM

j

1.72

1.42

2.08

2.27

2.49

2.00

^W^'"',-^^ . 'i.-. .-•;- : -ZMJAf^±'-..'~Z*.? ;* ' ' •'•- '- " ; ; ; - S^fAt^.-'.^l1 s- 1 •-••. -- -'••-. : ,' ,^n^;l^;;.':y ;v' ; ---- '

II

I^'J - ,;m-*i^-\m.

JOSEPHINE EXTaiSICN

May 21, 1945.

Summary Results - D. D. H. No. 6.

May 5, 1945. Kay 17, 1945.

Hole Started Hole Completed '

Bearing Southeast . .Dip Surface - 55ODip 900' - 520

Vertical Depth Intersection below Parks Lake 590*

A continuous section of siderite ore was obtained along

the contact between the Iron Formation and the lt Wawa"Tuflf8H ,

Total depth of Hole -'. 899'

S^O'^K'V-- 4-'':' '\ " 'V ' ' "

I^MfSv ALGOMA ORE PROPERTIES, LIMITED A OSO^Sr ' - "

., ..V^'-i -:- . '- - -^fe--jrftePTT.:- ———————————————————————— -

,:.; .-' '.'

5JSHUN3 EJ

,FUSION Diamond Drill Report

B J 3;, r- HOLfi NO. 6 . PLAN No.•™.i*':; , -' - ' *-sWv ; STRIKE S 300 39'X . STARTED May S, 1945 SECTION NO•f*-"'- - '- .- - " - ' - -•P ' ANGUS -550 - FINISHED May 17, 1945 LAT- DEPTml . , : ' -- .

"4?C DEPTH 899* , ' ELEVATION 1170'-

t

1

1

1

1

1

|i

1liii .iJl 1i

DETTM

F MOM j

0

5.0

31. f

LOOJO

.22.3

160

215

; 17,5

122.5

124.4

.34.6

33.5

440

H ,.

TO

5.0

31.5

100

122.

160

215

417.E

422.5

124.4

134.6

133.

440

560

.0,

5

j

DESCRIPTION

Casing

Sediments, well defined banding IB e vi d en cThere are rather nuraerous tiny parallelquartz carb, sections which appear to re present introduction of material.

Greenstone, fine grained fc from 60*-100'schistose broken with 3 sections of lastcore (76.5'-79){86.5'-87.5){96-97*).

Greenstone as above, schistose and brokenwith two .6' sections of last. core.

Iron formation, massive dark blue fc grey qwith scattered strgs. and seams of slderitrhere numerous short sections and seams anstringers of massive pyrite present.

Iron Formation as above- the pyritlc seamsbands diminish in quantity until at 215' tis relatively little py. present. Pyrrbotlseems to increase in amount gradually.

[ron formation as above. Rock is about 80-jtz. and remainder consists of seams and sif pyrr. and siderite and few block bandscontain little mag.

ietadiorite with trace of fuflcliite present

[ron Formation.

•letadbrite, porphyritic phase caused by de/olopraent of 1/8"-^" areas of qtz. carb.aatorial {l.O 1 lest core).

[ron Formation.

letadiorito with fuchsite {1.0' lost core)

[ron formation, interbanded quartz andsiderite. Seems to bo a definite but graduincrease in amount of siderite.

ANALYSIS

NO. |

e.

lartzS.1

mdlere,6

55^• rgs./h i eh

il

re. j m j INVOL. |

*

1

.

ri"i~PtpiiiiiiiFili)i

V

lm

HOLEs

DEPTHmo**

sea

600.15

6375

57.5

674

688

700

710

720

730

740

750

760

770

780

TO

600.!

537.!

557.5

574

683

700'

710

720

730

740

750

760

770

780

790


NO. 6. SHEET NO. Z .*

12'

10'

10'

10'

10'

10*

10'

10'

10'

10'

DESCRIPTION

Iron formation inter banded silica andsiderite.

Iron formation interbanded silica and bit banded magnetite-bearing schist plus fewnarrow bands of siderite.

Iron formation heavily mineralized with 1fine pyrite and pyrrhotite.

Basic'dikefmedlua grained sort of "saltpepper" rock.

Laetadiorite with patchy chloritic clusterprominently developed. Last 1^' of secticappears bleached and fuchsite plates areprominent. One gains the impression hereagain that the siderite is something lat{than the metadiorite and has not only beeintroduced into the metadiorite but has tbleached it. ?

Siderite, dork in colour with numerousstrgs. of light coloured carb, and a fewfrags. ' i" in dia. of silica. Pyrite is abundantly developed fc some pyrr.Siderite as above, possibly not so manyqtz. frags.

Siderite as above.

Siderite as above except possibly littlebetter quality.

Siderite good quality, fairly light incolor

it n n tt it tt

n it M tt tt it

n n it n n n

tt n n n n n

Siderite, fair quality, dark in colourwith few chloritic schists seams present.

ANALYSISNO.

ck

oth

fc.

sn

nIso

** i

21801

21802

21803

21804

21805

21806

21807

21808

21809

21810

rm.

-

33***

39. n

38.71

37.98

36.30

35.33

35.89

36.16

34.61

34.52

33.05

*

-

7.14

8.96

10.52

8.54

7.61

3.61

5.72

2.23

1.94

2.01

•.o*—

-

*

5.26

4.46

4.52

6.42

5.46

5.30

5.06

4.78

6.98

9.82

MNsst

*

2.45

2.22

2.00

2.12

2.20

2.52

2.12

2.35

2.27

2.21

?e - 3 —

'It Og^Ln -

- 1

1

~

6.2 5.85.82.2

ALGOMA ORE PROPERTIESHOLE NO. 6 SHEET NO. 3.

p*"V ' :- ~/*' "

0niiii\iiiiii iji i

DEPTHFROM

. , 'l

790

803

810

845

TO

803

810

845

899

7*

DESCRIPTION

-

Siderite as in last section above.

Pyroclastics, brecciated phase 'with, siderite present in grdmass of rock fragt for 1st. 6" of section.

Pyroclastics, brecciated phase of tufacecrocks.

Pyroclastics med. grained and fairly darkin colour owing to presence of chloriticmaterial. The^ brecciated phase noted abovdoes not seem to continue. There is a tiof sideritic material in form of tiny see present especially in section fro^ 894 -it is of no commercial importance.

END OF HOLE

Dip Tests

CorrecAngle on Tube Angle

-Surface . - 540 30

100 580 540200 580 540300 580 540400 570 30* 530 30500 570 530600 570 530 700 560 30' 520 30800 550 30' 520 30900 560 520

ANALYSISNO.

21811

21812

as

9aceins 897 bx

-od

t

rt.

24.74

6.09

t

s

1.9-!

5.1E

• •O*

19.96

54.50

MM

i

1.69

0.37

-.OALGOMA ORE PROPERTIES, LIMITED A.OJO

R*^J^?*i-?"J*;i .^vv ;.";' ;. "' - V-. "' *-vV -" "' ' 1 TV *H T* t ' ' ~" ' ''fti^fgj a Diamond Drill ReportIBi^S^LK'r-i'J.'VsV' '.'.'•-i;-', V-'''-! '- "' . . '- ' - ' ' '''t - 1 - '" ' "•J^?- jHOLE No...- ; " ;' . : ' -.- . . ' PLAN No.

Rftlr " ^ STRIKE - STARTED - SECTION Noy\fcv: : v '.:- ! '*-. •••' "- -. ". . - - *• S;:. ANGLE ' FINISHED UCT DEPT• r-;.;^::- ,, '.\;. ,. , ' *RJ^KDEPTH ' ELEVATION1 • JA J '- .•..-V- 1 ': : , .' ' ' .

• \DtrTM

ffrioiij

1 '-'- l ' : '

l \ ''m"

m

M

iM

j

i

TODESCRIPTION

-

ANALYBI*

NO. re. s INSOU | f-) n .

3116)

0

03

O/

05

6k

rf

01

10

II

j CV t f

*4 o r) f

37.9?

34-30

3i--33

3^f^

.3CY4

3V*/

3 i. 05

jy.7y4-09

7/v

f-9fe

/^.^l

/^v

7-4^

3.6/

^•7i

3.33

•3.01

/•9V

3V/

jracV-V6

^y*C-Vii-.^t

6" 30

^.04

v../

y. /i(9^9 L

s-yr

a. D a.

J?.00

^./a.J.AO

J.^

^./a,

5. j y

^.a;

/.(*1

0-37

, x-—.xl//*,

i/

S,f

iff - Solif-

.rot' - l '

t * 7 c' v. V. A' -W X -y .X A/ X X A y -y \ o

.t / -J o O i;c/ 5 b' V/y 7V

,.., \\ •"" \\

v :- - 'v'. :7i':^i v - - -. '"- ' \'"- :''\'-f\

r ' *~".1 r

JOSKPHIH3 EXTENSION

May 30, 1945.

D. D. H. No. 7.

Hole Started: Hole Con5)leted:

Kay 19, 1945 llay E9, 1945.

l

l

l

l

l

l

hl

Bearing Southeast- - Dip Surface - 60O Dip 780' - 370

Vertical Depth Intersection below Parks Lake 410*.

A 20* width of Iron Formation was intersected. The

projected position of the Iron Formation fron the surface to the

drill hole indicates a dip N. of. 71 O .

There is'only a trace of siderite in the banded si?.ica.

The main iron minaral present is pyrite.

Total depth of Hole - 787'.



A.O.3O

HOLE No. 7 ; i

STRIKE S 300 39* B

ANGLE -60O

DEPTH 787*

STARTED May 19, 1945 FINISHED May 29, 1945.

PLAN NO. "-

SECTION No

LAT. 29964.98 DEPr 27423.57

ELEVATION 1175.47

l l llil l ll ll

— - ———— —

r ROM—

0

6

54

J0.3

160

200

534. i

239

277

281

282

!9i.e

HI. 5

p.

-

TO:

6

54

60.3

160

200

334.

239

277

281

282

291.

311

315

316

)

i

5

5

5

DESCRIPTION

Casing

Sediments, finely bedded and well defined greywacke.

Ketadiorite type of basic intrusive .Ra thor poorly defined.

Greywacke interbedded with few narrow' arko layers. There are a few a.tz. carb, strgs. (82'-90* open ground) cemented.

Greywacke interbedded with dark arkosic la

Greywacke as above.

kletadiorite type of basic intrusive.

fragmental rock with very indistinct beddi rhere are few scattered frags, of '-quartz o milky variety. Sections- gradually becomes silicified and bleached.

Basic very fine grained dike rock, possibly poorly defined diabase- contacts seem to b ;radational than is usual for diabase.

Silicified seds. as above basic rock.

letadiorite, schistose but rather well def with usual associated qtz. carb, strgs.

Sediment, very coarse as above or congloce .vlth very abundant frags, ft, rounded areas jranular qtz. and rhyolitic icaterial. "atr frags, is sericitized ^ schistose.. Pebbles irory well rounded k the sericitized schist around then.

Greywacke.

lotadiorite with trace of fuchsite.

ANALYSIS

NO. | PC.

sicpreser

f era.

ng.m

nore

a3 more

Lned

-ate )fLx of are bends

* *

* INBOL.

1

t M*. It*

; * *-


l l l

l i i

olV

HOLE NO. 7 SHEET NO. 2z:^^

f

DEPTHFROM

16.5

340

359.5

379.5

381

420

460

500

539

550

561

611

615.5

619

636.5

G4D

TO

340

559.1

379.

381

420.

460

500

539

550

561

611

S13.J

619

336. L

640

o'X .E

5

11'

11'

DESCRIPTION

Greywacke with few interbedded layers ofarkosic material.

Sreywacke as above, numerous tiny qtz. costrgs. are present.

Diabase, well defined.

Sreywacke with few rhyolitic pebbles in e

Greenstone with both slightly granular acschistose phases k with a number of tinybarren qtz. carb, strgs. present.

Sreenstone with numerous qtz. carb, strgsSection from 448 - 455 is considernbly brSt does contain a lot of barron carb, mate

Jreonstone, fine griinad typical, qtz. costrgs. are abundantly developed.

Greenstone as above except last 20* ispartially bleached.

Iron formation, sect ion consists almost ertiroly of banded silica and massive pyriteabout 40:60- Few tiny siderite atrs. arepresent.

Iron formation 40:60 silica !t massivepyrite as above .Trace of siderite presentin form of very tiny strgs. There is a lipyrr. with the py.

Pyroclastics with very well defined rhyoior felsitic frags, in a matrix of green E

Pyroclastic bleached and with a trace offuchsite present.

I'.otRdiorite prase partially developed inpyroclastics.

Pyroclastics, dark in colour.

Pyroclastics which are in part silicifiedpart siderizod with development of 1.0' cquality light coloured siderite betv;een653.5 - 639.5' .

i-yroclastics with few qt?.. fra^s - .sectio:is bleached and silicified.

ANALYSISNO.

lark

rb.

videnc

i

*

ok enrial.

rb.

21813

31814

t tie

iticchist

the

k inf fai

re.

.

e.

34. 1C

28.6C

*

9

-

28.04

22. 2(

• iO*

22.24

36.96

MM

0.21

0.35


SHEET NO. 3.. ass

DEPTH

rnoM" —644. f

653

668

700

\*

740

t

TO:

653

668

700

740

787

t

DESCRIPTION

Ketadiorito with number of barren qtz.ca:strga. ' .

x '

Pyroclastics, frags, of qtz. So- in a darkgreen schist matrix.

Pyroclastics, rather well defined conglomhorizon in which there are 1" -f rags, ofsiliceous rock, in a chloritic matrix.

Pyroclastics, chloritic schist with trac*fc there of well defined frags. There areshort sections either carbonatized orsericitized or both.

Pyroclastics, chloritic as above.

-END OF HOLE- - -

Dip Tests

Angle on Tube Correct!

Surface 60 o - 60O

100' 590 - 530200 ' 540 - 500300' 500 -. - 450400' . 480 - 430500' 460 30' - 430600' 450 - 410780' 410 - 370

1

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MICHJPICOTEN IRON MINES LTD. DIAMOND DRILL REPORT

PLAN No.STARTED October 8,1950 SECTION NO. 5 FINISHED October 9, 1950 LAT- 32,163.9 H

ELEVATION 5223*DEPT. 32,867.7 S

li . .'it#-*-:-. fe

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DESCRIPTION

Casing.

Aoid Agglomerate, medium gray, fine gr.,rhyolitio with cherty and felsitic frag -mont s, elongated along the shear direct -ion of 30 - 35O to core. Minor f iuie pyriteand few large blebs after 20.0*.

Intermediate Staffs, gray green, distinctlybanded at 45-500 to oore. Frequent coarsepyrite Teinlets. Pew narrow siderite bandsafter 60'

Acid Agglotn. PlecJced throughout with a tin,black hard mineral{ ottrelite ) . Pew .siderite bands and traces of pyrrhotite.

Similar, considerable banded siderite. .

Similar, decreasing siderite. t

Siderite, fine grained, gray buff. Minor tpyrite and pyrrhotite blebs.

Similar, sparse pyrite and arseno.At 80* i3 - inch quart* stringer st 400 to oore.

Similar.At 87.0 ^-Inoh white quart* string*

Similar.

Similar. At 98' 1-inch Agglon. inclusionshowing strong brecciation.

Similar, Increasing sulphides.

Similar, few tiny irreg. pyrite veinlets.

Similar, fevr quartz stringers at 45O -i

Similar, sparoe fine pyrite, soatt. arsono. *

Similar, inoreaeltis aulphldeo.Pew quart* atj*

ANALYSISNO.

2501

2502

2503

2504

2505

r25062507

2508

2509

2510

2511

12512

J2513Similar, darker gray buff, decreasing sulphJ

J2514Similar. J2515

\

ri. •l 0* *- *- 1

'

*

i

MN.

l

A*. tV

i

t

i

i

i

i

ili1•K||11?r1

p^?t:^pqm^^sQ^zki^ •M/rvkM-t*.*.-:

y DEPTHSriioM

31^5ffi*.m-3S.5

l -^ f 1 '. : 1 . i•",; -.':.,V';,

41.0,-f J -

46.0

51.0

S6.0

J il.Oi! 'l 1

l|

i

li.1r

56.0

70.5

73.0

75.0

(0.0

ii

1iPP1

J5.0

:c.o

i•-*-.i

! ;- ''

i. ,. '

'i-iroi

136,wy?,-Vv .-141,;';-;,,146,

151,

156,

161,

166,

170,

173,

175C

180.

185.

1863

v-3?'Vf'-'**

NC'".'

5

0

0

0

0

0

0

5

0

0

0

0

0

1jii! i-

'•".iy ' 'V-V.* \'* . ' ." '. . . --- . ";. .: 1 , ;. ': . 'W'?K '.- • ;.'' ' ' '-•'•'- ' '."-'-- ".'-"' " "- '^.'V;- :'v'-; ' - . . . ; : - -' ' "- :).yJ -;l.:-'.,.,;.. . ' • /••.[,.- '

•V; ' DESCRIPTION

Siderite, light gray buff, frequent tinypyrite blebs and irregular velnlots.

- 'yritiferoa* Siderite, dark gray, fine gr.

with approx. 30jJ dendritio pyrite.t~

Similar, approx. 20/S pyrite.

Stellar, 35-40J? pyrite.'

3imilar, 25-30^ pyrite.

Similar, 30-40J& pyrite.

ilmilar, 35-45^ pyrite, scattered pyrrh.Strong directional texture at 450 to core.

Similar.

Similar, Increasing sulphides Jit 172. 5 -toL73 1 very diorito-like,mlnor sulphides.

Slaty Iron Formation, dark gray-blaok,-with ii few dark quartz and pyrite bands at 56O.

.,,,..SHEET NO. B ^ v

ANALYSISNO.

2516

21,17

2518

72619

72520

2521

72622

72523

72524

2526

r*.

:ron Formation, quite similar to preceding , . ]Jith frequent dark gray-blue sjid cherty qtzjands to 1^ inches 60-650 to core. Minor)yrite ve Inlet o.

Granodiorite, medium grained gray-green ipeckled Iporphyritio) intrusive. Veryoassive but shows evidences of being re -jrystallized. Contact at 185' very sharp it 800 to oore. At 176.6' inclusion ofilaty iron formation over ^ inch.

iron Formation as preceding, intrusive.

2nd of hole.

DIP TESTSDeptfr Etohe4 Correpted,

Collar - - . 240 ( on rods )100' 22^ 180

1

!

i

i

•l O*

i!

i

9.

j

r. MN.

i 1

AS.! ' , .1

tat- LOS

iiiiii\

: HOLE HO. J - SHE2T HO. 3

ANALYSIS MID GRADE

Sample Bo. Footage

JJJJJJJJJJJJJJJJJJJJJ

250425052505250725082509251025112512251325142515251625172518251925202521252225232524

Totals

75.78.83.86.93.98.

103.

3- 78.5- 83.5- 88.5- 93.5- 98.5-103.5-108.

108.0-112,112.117.122.127.131.136.141.146.151.156.161.166.170.

5-117.0-122.0-127.0-131.5-136.5-141.0-146.0-151.0-156.0-161.0-166.0-170.

55555505000550000005

5-173.0

75.3-173.0

Width3.2*5.05.05.05.05.04.54.54.55.05.04.55.04.55.05.05.05.05.04.52,5

97.7'

P*32.2929.3232.1433.1033.3032.9434.1533.6031.9432.0932.7934.6033.2036.9736.8737.9241.5540.4440.4940.0436.31

Pt.**.103.33146.60160.70165.50166.50164.70153.68152.10143.73160.45163.95155.70166,00166.37104.35109.60207.75202.20202.45160.1890.78

3426.62

5&102

7.9615.069.28

"7.625.926.126.946.708.84

11.669.967.708.886.42

10.2210.124,905.744,045,50

11.46

Pt.x^SiO

25.4775.304S.403P.1029.6040.6031.2330.1539.785S.3049.8034.6544.4028.8951.1050.6024.5028.7024.2025.1128.70

805,58

Z 5*0.823.823.054.022.182.571.562.722.414.814.924.003.46

15,7517.6218.4217.8318.1619.0720,3719.34

Ft.X/oS Grade

2.6219.1015,2520.1010.9012.65 35.07.11 ,o Fe s, 3*

12.2410.85 ifei02* *24.05 9^24.60 # S m /t16.00 O jfo17,30 670.0836,1092.1009.1590.0099.3591.6646,35

065.36l

l l lr i

Intersection 83,5-173,0 (89.5'}

a 35.49^ - 7,87

S s 9 .42

KBgR^pW^^ ;m-;;. " ' '" " "- ••-:^ ;:^-:Bmif^^^^&^f-. : ^MICHIPICOTEN IRON MINES LTD. ' ' " ' ,- M - 1W*W**MII;* 'V*-;l|?^5^,-'-s: '-:. ; V' v : --' ' ' .' -- - ' ' : •"" ' -"v -'.- BESSîSS^vvSS1-' 1 -- '' ;- : '"' DIAMOND DRILL REPORT ' " ' -- '^ I•^^W^'^v.?;-r''- . " : : IIBliôii^ J-2 '. '' ; ^ ": .-'' : "~ : : PLANNO. . ."-•'•".•-lmf^^-^'--'-'----^:-'-" t '"''!-'- ' ' ' ' -'-- - ' ' ' 1 |J^^ STRIKE ThieHorth STARTED October 10, 1950 SECTION NO. 6 Bl^^lS ANGLE ;34^ FlNISHEDOcVober 13, 1950 UT. 32 .000 S DEPT-32,867 X B

I^^y DEPTH 416* : ELEVATION 5202* |^ j -' B*-^:-|||

li- •"•:-

fi•.i;

liii** 1

l 11

1ri, ii5i1:t'f*jj;.,'.

DEPTHrnoM

0.0

L2.0

50.0

55.0

59.5

14.0

19.0

53.5

)8.0

i3.0

)8.0

)7,0

.1.5

.6.0

!1.0

!6.0

51.0

S6.0

11.0

15.5

)0.0

TO

12,

30,

-

35,

39.

44,

49.

53.

58.

63.

68.

107.

Ill

116

121

126

131

136

141

145

150.

155.1

0

0

0

5

0

0

5

0

0

0

0

5

0

0

0

0

0

0

5

0

0

i^

DESCRIPTION

Casing; 0-5 overburden* 5-12 boulders.

Aoid Agglomerate, fine grained with fairlylarge fragments of moro basic composition.Fairly well sheared at 40-500 to core.Scattered narrow bands of ankerite-siderit aî sparse pyrite blebs throughout.

Similar, increasing siderite.

Similar.

Similar.

Similar, considerable siderite and sparsefine pyrite.

Similar.

Similar.

Similar, shearing at 50 O to core.

Similar, decreasing siderite.

Agglomerate with irregular, narrow areas of siderite throughout.

Sim. increasing siderite. Few qtz. blebs.

Similar. "

Similar, considerable siderite. .

Similar. '

Similar.

Similar, increasing siderite. At 132.5 to133* considerable pyrite.

Similar. Shearing at 40O to core.

Sim. At 141-142.5' consid. pyrite.

Similar, decreasing siderite.

ANALYSIS |NO.

|

2526

2527

r2528

2529

2530

2531

12532

2533

2534

2535

2536

253

'2538'253

254

2541

2542

Sin. Consid. pyrite at 154-155', ^254C

rx.

'

•l Ot

l

*. f. MN.

li

AS.1

i i

to B^B

P*'M^:;:-:r"v.:''. l^^fe^-'i-v.v?ISoL^fe-^:^ 2 SHEET NO. z

Ml—— r1ll^jT

Iflppt v

P• r

Pl

^ DEPTH :riPtoM

* 0mr** r ,-^-.•v 0.0HeW'9-5••',; : "'V

4.0

r9.o4.0IT-

l1?3* 5

MMH H2(

li2'

k 2:[•2'

Z'.

8.0

2.0

6.5

1.0

5.5

0.5

•225.5

f21iiitt!

7.0

1.0

1.0

3.5

5.0

0.0

5.0

6.0

t

'#**::;

160.sir 'V:-

165,

1169.

174.

179.

104.

189.

193.

198.

202.

206.

211.

215.

220.

225.

227.

231.

241.

343.

245.

250.

^;;;'.

^

S '

1 .'

1

)1

ml

1

1

t

1

)

J

)

)

)

)

)

)

0i

256.6

318.6ti

i. .': v.

18. 0 520. 6ii

-v . DESCRIPTION

Agglomerate, considerable scattered isiderite.

Similar. . .

Similar, sparse pyrite. " t

Similar. *

Similar, increasing siderite. *

Similar, somewhat decreasing siderite. *

Similar. Shearing at 500 . i

Similar. .

Similar, i

Similar. - - i

Siderite, some(unreplaoed) agglomerate. *

Similar, scattered fine pyrite. **

Similar, J

Similar. *

Similar. J

Similar,

Agglomerate, scattered siderite bands.

Tuff, medium gray, fine grained. Shearingat 40-500 to core.

Agglomerate, scattered siderite and pyritebands (largely irregular) throughout.

Siderite, minor agglomerate. Sparse fine Jpyrite.

Similar. ^

ANALYSISNO.

2544

2545

2546

2547

2548

2549

2550

2551

2552

2553

2554

2555

2556

2557

2558

2559

2560

2561

2562

12563

Similar. J 2 564

Tuff, occas. siderite bands. Sparse py. J2565

Tuff, as above^ only minor siderite. After 280* scattered agglomerate fragments.

iSimilar, increasing siderite. Shearing at * 40 degrees to core.

12566

re. •l Oi

i

9.

1

f. MN. A*.

. ' i

10 LO

1

1i *

jsmm

•(FROM j .TO/,

IP•Ip||3.08^0-

If^•1 f-,% -' --

Ep.ottd.o•^•i''.of'/'firfaka.o• 353.0

lip8*0lap. 5

[l

3

• •3

13

•4,Ir

. 4

-A".

s , 1i*

J7.0

72*0

77.0

52.0

J7.0

a* 5)5.0

)6.0

)1.0

)7.5

L3.0

l

^MMW—

323.•i" i - !'- -'

328.^•i'i333.

338.

343.

348.

353.

358.

362.

367.

372.

377,

382

387

V?^ ; v;5^

^NC

0'i; ;

0

0

0

0

0

0

0

5

0

0

0

0

0

391J5

395JO

396,

401,

0

•JO

407 J5

413.0

416*0

i i1

l

^'^v i t'' - ' v. ? --" - '' ' - - -- ^^^^^^^^^^^^^^

^y - -2 SHEET NO. 5

1 V ; DESCRIPTION

Igglomerate, with oonsiderahle "banded and 'brecciated siderite. Oooas.qtx. stringer*.

Sira.banding distinct at 40O to core. . i, . ' *

Ottrelite schist, light gray with frequentflecks of ottrelite.Bands of siderite.

Similar. i

Siderite, gray "buff with darker mottling .of cream buff. Scattered fine and blebularpyrite throughout*

Similar, occas. calcite stringers. *

Similar.

Similar. '

Similar, increasing pyrite. i

Sim. some unreplaced rock throughout. i

Pyritiferous siderite, dark gray, 55-65/S ipyrite.

Sim.oonaid.olaty-lftice material. i

Pyritiferoas siderite, 20-25^ pyrite. .

Sim. 25-35^ pyrite, Scattered qtz.blebs.

Similar.

Similar, 20jJ pyrite.

Interbanded siderite and cherty Iron Pom-ation. Banding at 45-500 to core. Consid-)rable scattered pyrite and pyrrhotite.

Similar, decreasing siderite*

Slaty Iron Formation.well banded with oooacherty qtz. band s. Scattered pyrite and pyr

Granodiorite, mod. gr. gray-greon.

Cherty Iron Formation.End of Hole.

DIP TESTS"DftTvth E t oh cd Cojir^pted.Collar - - 34P Ion rods)

200' 34^0 27^*390' 290 230

ANALYSISNO.

2567

2568

2569

2570

2571

2572

2573

2574

2575

2576

2577

2578

2579

2580

2581

2582

2583

2584

i.•*

re. •l Ol

*

s. r.

t

MN.

1

A*. ION. LOS*

3

i 1

l 1

V

ip ®mI,4V •f*-'-W

||te2572*r 343.0-348.0, m.J^*519tf: 340.0-353.0 P 2574:;^ 353.0-358.0 1^2575^:358*0-362.5; m*t*Vt*'f. 362.5-367.0 P J, 2577 •367.0-372.0 |^j;2578 v s 372.0-377.0 ||J 2579 377,0-382.0 'fi* 3 2580 382,0-387.0 'I,; J 2581 387.0-391.5 H S 2582 391.5-395.0

Total* 343•0-395.0

•5.0';M.o: 5.0•^.*.B;

4.5 5.0 5.0 5.0 5.0 4.5 3.5*

52.0*

30,88 32.70. 33.00 34.80 19.80 37.20 40.44 39.83 40.64 41.44 40.94

154.40 ; 163.50

165.00 156,00. 99,10. 186.00"

202.25 199.15 204.20 186.48 143.29

1849.92

13,84 8.12

11.0ft 8.10

42.24 15.32 5.80 5.14 6.34 4.60

11.04

•™ 'in ™— M

,* VAJL^WJII

69.20 40.60 55.30 36.45

190.08 76.60 29.00 25.70 26.70 20.70 38.64

608.97

** /**

3.23 3.67 3,46 9,29

13.56 25.84 20.30 17.68 25.26 25.73 14.33

'I.X/K)

16.15 18.35 17.30. 41.80} , 61.02 j '

129.20; - . 101.60} '

68,40} , 126.30 J ' 115.79 50.15

1 —

765.96

v*r*d*

- ' - j •.-" "

^ 'e w 35.5

fciOjj. 11.7

^ S - 14.7

~— — ~— — ^.

Interaeotion 367.0-395.0

( 28.0 ?t.)

40.057.76

21.83

•• . No. J - 3

if;* STRIKE ; Due Horth|^f ANGLE ' 540 ; -P DEPTH 905*

MICHIPICOTEN IRON MINES LTD. DIAMOND DRILL REPORT

. PLAN No. STARTED October 14, 1950 SECTION No. 5FINISHED October 24, 1950 LAT. 51,917 H

ELEVATION 5195*5*DEPT. 32,867.1 E

Ipm-

m"''*''''' '

^^B*-*V '^B'' :

[iM

[l

1 -

iii;iii'•V-

1;If-

: DEPTH

- i W

o.t4. C

79. C

99.0

01.5

12.0

29.0

43.0

51.0

59.0

63.0

TO

4

79

99

101

212

229

243

251

259

263

300i

i

0

0

0

5

0

0

0

0

0

0 '

0

DESCRIPTION

Casing.

Seriolte-carbonate schist, fine grained.gray-green to gray with white mottling (duto the heavy carbonatization). Stronglysohlsted at 350 to core.At 36-41 wellfractured as evidenced by criss-crosscarbonate (ankerite Se calcite) volnlets.

Similar but lighter gray end fairly talco3(with occasional sorpentine-chlorite slipsparalleling the intense schistosity 'at 20-250 to core, changing abruptly after 79*.The schist is very likely derived from anacid flow.

Intermediate to basic schist (presumablyderived from a flow) f dark gray-green andvery andesite-like in appearance and comp osition. Schistosity at 30O to core.

Sericite-carbonate schist as before. Strongschistosity at 25-300 , Frequent carbonate"eyes'* to 1/10 inch diameter (possiblyamygdules) .Sanewhat talcose throughout.

Intermediate flow.TCell sohisted at 30O ,

Sericite-carbonate schist as before.

Intermediate to basic schist, andesitio.

Agglomerate, medium gray mottled with lighgray and cream-gray fragments to lg- inchesacross and somewhat elongated along theschistosity at 300 to core.

Sericite-carbonate schist speckled withfrequent carbonate "eyys".

Agglomerate, nedium-fine grained, gr ay-gree.with scattered lighter gray fragments. Fewscattered pyrite and pyrrhotite blebs andtraces of siderite. After 2S4 occasionalirregular cutting voinlots of siderite.

ANALYSIS

NO.

*

er

t

ri.

t

• l O* •-

i

f. MN. AS. toLO'

1

1

i

SHEET NO. 2

I•r

1P;LBIH?n\m\f.I A *

W4

m

,ii!i r,-" "•m~~^*!?sm ^ DEPTH

ffl9M.-'fti-77

^s?o&p0?i'5?Si:1 '(.''64.0

67.0

71.5

'6.0

S3.0

S6.0

73.0

rsbe.oISJLI.O

5

5

i,Oi

i!• 5

5

1r

i . i

L6.0

11. 0

*.o5.UO

56.0

11.0

L5.0

50.0

55.0

50.0

54.5

:.TO,'•i' -''305

309

364,-V.367,

371,

376,

463,

460,

473,

506

511

516

521

526

531

536

541

545

550

555

560

: ';'

*T5.'.'0

0

5

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0i

5G4 J5569 JO

m -69.0 i 574 JO(

B 574. 0:579 JO

i. "579.0 '504 JOm - ]

i DESCRIPTION

Lgglonerate^aediun gray. Soatt. siderite.

Similar.

Agglomerate, scattered veinlots and .bleba olsiderite generally with assooiated 'minor py

Similar with increasing siderite veinlets.

Similar. Pew carbonate stringers.

Similar.

Lgglbmerate with scattered siderite-ankeritareas giving core a very mottled appearance

iggloraerate, gray-buff mottled.Oonsiderablesiderite throughout. Very minor fine pyrite

Similar.

tgglomorate, gray-green, mottled with Irreg.Lens-like areas of siderite and blobs of py

Similar with increasing siderite.

Lgglcttorato-siderite,raottlod gray-buff.

Similar, few scattered py, tc pyrrhotite

Similar, scraewhat decreasing siderite*

Similar, somewhat banded at 300 to core.

Similar, Minor pyrrhotite blobs.

Similar,

Similar with scattered fine pyrite.

iggloraerate, medium gray, scatt, s!4erite.

Similar, increasing siderite and pyrite.

Similar with decreasing siderite 4 pyrite.

Similar, increasing pyrite (largely blebs).

Stellar. ,

Similar. Scattered fine pyfrite throughout.

Similar with gomer.vhat decreasing siderite.

Similar, decreasing siderite and pyrite.i

ANALYSIS ^i

NO.

r258!

'258*

i

f258^

F258(

f258S

259C

2593

12592

T2593

12594

f259E

r 259 6

r 2 597

T259G

T2599

[260C

260 J

F 2 60 J

T260;

2604

I260J

12601

1 260' i

ri-

3t

t

•l Ol ** f.

1

M H.— ———

AB. ION. Mft-OB.H

I

I1i

1I111

l

•;1

: s SHEET NO. 3

pHI*wi'11LeP*

heIle

r1lir E

ir

G

tll(1

' v DEPTHFROM

Wo'•Q&y -80.0?|' :v ;-.-^fTS .'

93.0

96.6

01.0

06.0

U.O

16.0

20.0

25.0

30.0

35.0

40.0

45.0

49.0

54.0

59.0

64.0

69.0

73.0

77.5

82.0

87.0

92.0iV* ' '

TO

588,r ^

593,

596

601

606

611

616,

620

625,

630

635

640

645

649

654

659

664

669

673

.1,.- -

0

0 .

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

677J5

68210

687*0

692 ;0

697.0

'v DESCRIPTION

A.gglcraerate-8lderite .mottled gray-buff.

Similar .Considerable pyrite associatedwith the siderite* Few qtz-carbonate blebs.

Similar* Considerable broken core.

Similar. Scattered fin^ ft blebular pyrite.

Similar, fairly distinot banding at 30O.

Similar, considerable pyrrhotite at 610* .

Similar, banding at 35-400 to core.

Similar, Increasing siderite 4 sulphides*

To t tied agglom. -siderite with scatt. pyrite

Similar but decreasing siderite, minor py.

Mottled agglomerate and siderite. Soatt'.py*

Similar with increasing siderite i pyrite*

Similar*

Similar.

Similar. Scattered large blobs of pyrite.

Similar* Iron-oxide stain* between 657-658'.

Similar, minor iron-oxide stain at 659.5.


Similar, considerable siderite.

Similar. At 672 agglomerate frapnent with J- inch pyrite border.

Similar, considerable pyrite blebs.

5.gglonerate,gray with bluish cast. Widelyscattered siderite areas. Scatt. py. blebs.

Similar.

Similar, considerable tncrerisa in sideritekvith scattered fine pyrite throughout.j

(97.oi 701,5vv i

,. 61.5* 706iOm--. -. 'Similar, decreasing siderite and pyrite.

Slnllar but only very ninor pyrite.

ANALYSISNO.

T260C

J260S

I26K

J2S13

J261J

J261I

T26K

J26U

J26K

J261 1:

J26K

il2615

F262C

F262]

J262J

1262!

J 2624

1262

1262

J262

3262

3262

3263

3263

rt.

1

9t O*

i

32632 - |

J2633

•- f. MN.

1 ..•^M..^^

AS.

' ' i

ION! Lo* f

f

liEit•VkBII11k1i ih1lii iiI r

^f^i'NCXJrS SHEET NO. 4T-5PCPTH j 'rnoM

c&S^':

li;016.0

20.0

25.0

30,0

5,0

37,0

40.0*

45.0

47.5

49.0

54.0

59.0

64.0

69.0

74.0

79.0

84.0

69.0

93.0

9G.O'.

iT*v|711

'.V*'L t' .

716

720

725

730

735

737

740

745

747

749

75-1

759

764

769

0

0

0

0

0

0

0

0

0

5

0

0

0

0

,0

754*0

779,0

764JO1

709*0

793*0

796iO

DESCRIPTION

igglanerate, gray-blue with scattered Jsiderite areas and very minor pyrite.

Similar, decreasing siderite. , S

Similar* somewhat increasing siderite. J

Agglomerate with scattered siderite areas. J

Similar. 3

Similar, faint banding at 300 to core. J

Similar, more distinct banding with a few 3pyrite veinlets ]j banding.

igglonerate-siderite, sonewhat mottled Jlight gray and gray -blue, with fine pyrite.

Similar, only minor pyrite. ' ' J

Similar, considerable siderite. J

Banded cherty quartz (Iron Formation) Jwith interbands of dark slaty material*and occasional bonds of siderite at 20-22 .

Agglomerate, light gray with scattered Jto minor siderite. Pew cherty qtz. blebs.

Similar, very rhyolitic with few dark gray Jbands at 25 to core. Very minor pyrite.

Similar. J

Similar, Occasional voinlots of serpentineJ

Stellar, somev/hat increasing siderite. J

Similar. Pew pyrrhotite blebs. J

Similar, increasing pyrrhotite blebs. J

Similar, darker uray. Schistosity at 25? J

Similar. Occasional cherry qus.rtz blebs, J

Similar but considerable cherty c^tz.bands.J

B00,0 (Similar, decreasing quartz bands, Ci

,,00.0' W ~* 0 lAsslorierate.lijht ^ray, rhyolitic v/Uh t

j002. D! B07.0

[scattered to niuor siderite.

ANALYSISNO.

2634

2635

2636

2637

2636

263*

2640

2641

2642

2643

2644

2645

2646

2647

2640

2649

2650

2661

2652

F2653

2654

f2655

7L'65o

Sir.llar, fe\v scattered pyrrhotite blebs, J"~Grv

f

ri. •i O*

i1

s.

i

i

f.1

1

t 1

MN.

j

A*. ION. LO* B

i

i

1

i 1111111

fj-r^ ' HOLE NO. J - 3 SHEET NO. 5

P^.r. e? ;'v' 0

8

^-- 8

0

8

6

D

-j *i' " 8

1 0

6

1 o

1 e

DEPTHrnoM

)7.0

.1.0

.5.5

!0.0

J5.0

(0.0

S5.0

18.0

10. 0

.5.0

iO.O

:5.0

iO.O

i5,0

S9.011 - Dt'4.0

1 80

6

1

r9.o54.0

56.0

17. 5

l.o1

)1

TO

811.

815.

820.

S25.

830.

835.

838.

640.

845.

850.

855.

060.

865.

869.

674.

879.

684.

086.

887.

906.

0

5

0

)

D

3

3

)

0

D

0

0

0

0

0

0

0

0

5

01

DESCRIPTION

SidoriteJ-'edium gray-buff , fairly massive t with occasional white calolte (minor quart stringers. Scattered finely dlssem, pyrite

Similar. Scmo lOJw pyrite and minor arseno.^

Similar but decreasing sulphides. i

Similar with lOjS pyrite. Few calcite ; stringers at 50-550 to core*

Similar, lighter gray-buff. 5-BJ& pyrite, i

Similar with somewhat increasing pyrite, .

Similar, scno 10-15^ finely dissent, py, i

Pyritiferous siderite) some 35Jo pyrite i and scattered pyrrhotite in siderite matri:

Interbanded pyrrhotite, siderite and ala t ci

Banded slaty schists (very likely a phaoe i of the slaty Iron formation) with some 10- 15/S interbanded pyrrhotite at 55O to core.

Similar with increasing pyrr.fc scatt. py. *

Similar. Seme 25-30/S pyrrhotite, .

Interbandod slaty schist, pyrrhotite and . occasional siderite bands.

Similar. Some 40-4 5/J pyrrh. ft scatt. py.

Similar with 60jo pyrrhotite and pyrite.

Pyritiferoua siderite. Some 60/J sulphides.

Similar. Some 35j? pyrite 4 scatt. pyrrh.

Similar. Scattered blue— gray qtz. blobs.

Interbandod siderite and cborty quartz. Scattered finely disaeminatod pyrite.

Cherty Iron Formation. Blue-gray quartz with scattered bands of pyrrhotite ?nd py.

End of Hole.DTP 1'ZSTS

Djbjith, Etched CorrectedAt collar - - 54 0 Ion rods)

200' 600 530400* 59'-o PS-.-0 600' 57",, HO5 . 000' 54 , 0 47

ANALYSIS

NO.

2658

2659

2660

2661

2662

2663

2664

2665

2666

2667

2666

2669

2670

2671

2672

2673

2674

2675

'2676

l

re. j st o* •. f. MN.

'^i'-^'yt'fMyff^f Wi*. r-'.'" -

^'-'••t'.-1 *'•li^Oi^BOV^^S^H^^ . ' - -. . ;- :' ;- 2HEKJ HOf ; •'•-.•"--.. V- . - :K ^ ••to^^^.^^^v^ fe^,?* . ' - . -V:--.-, ••.-•••.-•- -,v-,.-,v.. •-,:-..,. --- - •,:--:.-.'^.

n^m•26^,i;J|jt659p;

•f2661!K'B^ftiRi5'2'S?;BjftRkS :'*.'•2S&44 'y 2665L^B

807.0-8H.O8ii;6-815.5815.5-820.0820.0-825.0825.0-630*0830*(M)35.0835.0-838.0838.0^840.0607*0-840.0

Width

r 4.0*4.5

; 6.05.05.05.03.02.0

33.0*

•ritn31.2334.0031.7033.9034.2032.3082.6037.20

Tt.xjfr.

124.92153.00142.65169.50171.00161.5097.5074.40

1094.47

Jfei02

12.407.08

13.946.32 '7.08,,

11.5812.448.66

yt.xj&io,49.6031.8662.7341.6035.4067.9087.3217.12

338.63

2 ^ 8

8.796.722.866.023.144.016.64

13.24

Ft.x Jfe

15.1630.24 j12.87 j30.10 |15.70 J20.06 l19.92 -26.4B

170.52

1. J* m 88.17jteiOg* 10.11jt 8 a 5.17

Intersection 811.0-840.0

(29.0 Ft)

s 33.48. 9.79x 5.36

l l l i i i i i

-',l

. .

|pvl:A ; HbLENa. J -4 : STRIKE: Dad jforth

I- ^ ANGLE 2B0 It:-." DEPTH

MICHIPJCOTEN IRON MINES LTD. DIAMOND DRILL REPORT

PUN NO. STARTED October 25,1950 SECTION NO. 6

. FINISHED October 26,1950 UT. 32,452 H; : ELEVATION

DEPT. 33,382 x

••".I fST•yi

iiiSI

1Z

ii:1kii

DEPTHrwoMa- i" i

0.0i

12*0

56*0

58*5

61.0

66*0

70*0

74.5

79.0

34*0

38.0

33.0

)7.51

)2.5

)7.0

TO

12

56

58

61

66

70

74,

79

84

88

93

97

102

107

111

t

-— -'liJS

0

0

5

0

0

0

5

0

0

0

0

5

5

0

5

•f^ ,il.5|115 0

1I1

i L5.0J120, 0

JO.O 125,0f

DESCRIPTION

Oaalng*

Agglomerate, medium gray frith bluish oast.fine grained daoitio groundinass withscattered felsitic to andesitic fragments of varying sizes.Oooasional Iron-oxide stained slips at 70-80 to oore*3troag 'sohistoslty at 60-65o*8oatt.pyrite blebs*

At 45* 4-lnoh f airly .massive siderite*

Similar, scattered siderite areas at 70 . J

Siderite, gray-tjuff, fine grained and Jfairly massive, small areas of agglomerate*

Similar, occasional large blebs of pyrite.J

Darker pray-bnf f and someTrhat decreasing Jsiderite* At 68*5-69 oaloite-ankeritestringer irlth conoid, fine arsenopyrite*

Similar, scattered areas of tinreplaoed Jmaterial. Sparse blebular and dissem* p/rit

Similar. J

Similar, increasing pyrite. J

Similar. At 86 oalolte-ankerite string. J

Similar, decreasing pyrite. J

Similar. J

Similar, At 103-104 coneid. dendritic Jpyrite.

Similar. 15jS dentritlo and blebolnr py. J

Light gray-buff siderite with scattered Jcjreas of unreplaced material. 5/S pyrite.

Similar, increasing siderite. Sparoe py. J

Similar. J

ANALYSISNO.

2677

2678

2679

2680

26819*

2682

2683

3684

2685

2686

2687

2688

2689

J690

2691

r*. • l 0.

Similar. J2692 '

•- c. YIN. A*. 10 LO

i

; i

; f ; 4

SHEET m

F^iP1rk•si

tlrISfll'

riiiiiii1ii

IIIM-nai m m - J )r ™

# DEPTH y

. , - ".J1 - '

If^if'^f!'^jd*p-..*'" IL ' -'S*

(3.7*v;'v

5*0

7.0

0.0

6*0

-

;TO

; -- t

130.;,H ;,.,'." *:.*'

133.

135.

137*

140.

145.

160.

1i;;,.'\'.*

i

i

)

)\

i

. . ' ( J , 1*,. 1; .

A'^;'.-': : -- : ; ''••••-. DESCRIPTION . ' "' -v- :.:-;'-' v . ' ' . . . ' J , :. . : . . , . .- , . .. . - ' .

Slderitefoream-buff fgood auboonchoidal Jfracture, Sparse fine and blebular pyriteand traces of pyrrhotite.

Similar. ^. ;

?yrltiferous siderite. Some 25-30^ .banded pyrite at 65~70O to core*

Cherty Iron Formation. Dark grayish blue ibanded silica with occasional sideriteband. Banding Tery distinct at 680.

Slaty Iron Forma t Ion, dark gray to black *with occasional cherty quaits bands. Teryminor cream-buff siderite.

Similar, considerable blue quartz bands* *

Slaty Iron Formation, Scattered pyrrhotite bands at 70 to core. Massive pyrrhotite at 151.5-153.5 and 156-158. Few narrowgray-blue cherty quart* stringers or bands.

r.nd of Bole

PIP TESTSPepth, Etched CorrectedCollar - - 250 (Brunton on rodi100* 260 20 0

-

ANALYSISNO.

2693

2694

2695

2696

2697

269B

J

re. •l O*

4

\

9. f. MN.

'

AS.sssssss

\

SBXEX 3 l^m&rf-'i"-*'.*'".''. •./^Hsss'ijii-i;'.^; ^ , .-l^ba^loHo.^•^'u8"*:' :" io'i;'?Ji*,

^J if 2673 ?:.'-^\1^2680^ -;v 'j:.^HT'f* 2681'' ' " "

1^5^2682^;: ' .;^Jjp.' ;t v

B 26Q51 J 2886 Li 2687•r 2688 Hf 2689Lr 2690H 2691Rf 2692l/ 2G93Bf 2594•f 2G95

F~~ otala,,

1

l

1

1

1

1

1

1

ite-:

1 -^i1 .;.-' ,! ii',;:

58.5-61.061.0-66.0

'66*0- 70.070.0- 74.574.5- 79.079.0- 84.084.0- 88.088.0- 93.093.0- 97.5 97.5-102,5

102.5-107*0 107.0-111.5111.5-115,0115.0-120.0120.0-125.0125,0-130.0130.0-133.7133.7-135.0

58.5-133.0

.Width2.1*5.04.04.54.55.04.05.04.55.04.5 4.53.55.05.05.03.71.3

76.5*

J8I."37.1036.3037.0237.6036.4039.2239.0339.8239.43 40.7441.04 39.6040.2429.1739.2340.0240.2440.64

*t.x*.

92.75181.50143.08169.20163.60196.10156.12199.10177.44203.70134.68 178.20140.84145.65196.15200.10148,8952,83

2935.33

*3i02

8.823.663.862.5S3.904.563.864.965.10 3.502.96 6.805.107.847,026.724.624.94

lt*010,

22.0519.3015.4411.5217,5522.8015.4424.6022.95 17.5013.32 30.6017.8539.2035.1033.6017.096.42

382.53

5^3

2.782.583.542.953.244.752.622.682.52 3.99

12.40 12.517.252.653.14**OB

•S3J7

Tt.x^3 ax

6.9512.9014.1613.2714.5823.7510.48)13.40)j6?o m11.34) . 19.95)^02-65.80) . 56.29)? 3 "25.38)13.25)15.7010.404.92

22.06

344.58

-

•aft*

-

38*97

5.00

4.50

HOLE No. j u s , STRIKE Due Worth

'i' '-

. vr&'v:- .:~" : - ANGLE'•W'^y -' - ' "•K DEPTH 594*

MICHIPICOTEN IRON MINES LTD.DIAMOND DRILL REPORT

PLAN No..STARTED October 27,1950 SECTION No. 6 FINISHED OotoVer 31,1950 LAT. 32,462 X

ELEVATION 5236*DEPT. 35,388 X

fmsszzmRf

BrPli[l

1ii,ilif

^^DEPTH

FROM—

0.0

13.0

23^0

25.0

28.0

33.0

57.0

10.5

12.0

J2.0

56.0

J9.5

14.5

19.5

^ 9.0

1i

TO

13

23

25,

28,

33,

37,

40,

42,

122,

136

139

144,

149

159

163,

-,--— -

0

0

0

0

0

0

5

0

0

0

5

5

5

0

5t

J3.5 168, 5i

l

DESCRIPTION

Oasingv

Agglomerate, fine grained ,medtum gray, verystrongly sohlsted at 50O to core. Sparsescattered siderite and finely dissera. py.

Similar .Increasing slderlte.Traoes ofarsenopyrite.

Siderite, fine grained massive with vagaebanding at 48-50 . Minor pyrite 4 areetfo^

Siderlto-agglomerats. Some 60jJ siderite.

Similar .decreasing siderite .Spar s e pyrite.

Siderite, somewhat banded at 50O.

Agglomerate, scattered Irregular sideritegiving core a very mottled buff and grayappea* "mce. Minor fine pyrite.

Agglomerate heavily mottled with sideriteand associated sparse disseminated pyrite.

S?aff t fine grained, gra# with bluish gas t.rhyolitlo.Directional texture at 40 to corOccasional siderito-pyrite veinlets.

Siderite-agglcrnerate, Considerable some what banded siderite.At 136-137.5 oonsld.pyrite. Banding or schistosity at 30-35; at 139.0 oross-Bohisted at 18-200 to oo*e.

" C^V*. ^ *s" f •f^-^^'^- '

Similar. Sohistooity at 24-280 to core.

Similar. Schistosity at 30-330 . MasBlvesiderite at 145-1(17 and 148.5-149,5,

Agglomerate nottlod with siderite.

Similar, increasing siderite. Sparse pyriteblobs. At 161.5-162 considerable pyrite.

Similar.

ANALYSIS ~|NO.

T269S

I270C

I270J

J270J

F270!

T2704

9.

T270E

T2706

T2707

f270E

f270Si

ri.

i

i

•l O*

'

c. f.

1

MN. A*. to mLO J

1

1

n

; i1 i

Pilpci^^ .SHEET NO. 8 -r-'''..?•pODEWTHT" ;#.Bjg*"*

Kipp??5BjpPfoS• : '-- r|v3.S^^H ", -

Lli.olT 'FiIRs.oH|4*0B9*0E&4.0••9.0

•293*5

It'5

li '5

308.0

1.2.2

•6.2B

JK2.0

i.o1

(o rt & + V

fi'- K

,*fO".

173*G:vV T- . .

F*

180.^182.

211.

226.

269.

274.

279.

284.

289.

293.

298.

303.

308.

812.

316.

322.

327.

332.

i y

()V

,\;,'

i

a

)

)

)

)

)

)

)

3

S

3

)

J

2

)

)

D

336.5

'^tf*'\^. i; •••- - ' : . . ' -' - '"•• : . '

Siderlte-agglcmerate. Scattered pyrite* i

Similar decreasing alderite Jilnor pyrite* i

Siderite.f ine grained and somvMbat banded *at 55-58 to oore. Spar a e pyrite veinleta*

Agglcaaerate-siderite, Scat t. pyrite blebs,;

Agglomerate. Scattered areaa of sideriteand oooas. bleba of pyrite and pyrrhotite*

9aff,gray,8omevhat dacitio.Schiatoalty nt550. Few narrow alderite banda .Minor py*

Agglomerate a* before.

Similar. Scattered aiderite areaa. J

Siderite, fine grained, gray-buff. Pew ' ' *small areas of unreplaoed material.

Similar tquite maaaive, *

Similar, spar ae disaerainated pyrite* *

Similar, good ffuboonchoidal fracture. J

Similar. *

Similar. ' J

Simllar.inoreaaing pyiite. J

Similar, oonaiderable blebular and fine py*J

Siderite-oherty iron fonnation.Well banded at 55 to oore. Scattered pyrite.

Iron Formation . Interbanded dark gray-blue quartz and black slaty bunda at 50-55Oocaa* pyrrhotite banda and aoatt. aiderlt

Similar. Minor folding at 324.

Pyrltiferoua aidorite. ^.0^ blebular tointerstitial pyrite.Occaaional quartz bleb

Banded siderite and pyrite with fow aoatt.* j quartz banda. Some 30-40J2 pyrite.!

341,0 Similar. At 33G.C-340 coneiderable pyrite.l'5ftl.O 1346.0

|.oU 0

Pyritif eroua aiderito.Scme 25-30J5 pyrite.

ANALYSISNO.

2710

2711

2712

2715

2714

2715

2716

2717

2718

2719

2720

2721

2722

2723

2724.*

2725

2726'

2727

2728

2729

r r. •l 0*

~-

! i

Sinilar,Bcmo 65;J pyrite, Pe-,7 quartz blebs^32730

*- f.

'

MN.

t

AB. ION. LOS*

.

-

ii

t t

E•iinnli

JLi~r '-- ' -T-L— :

fe DEPTHPMOMY^n'

fs^;-Ni^v'"6.0W^.iyH? '

0*0-' 'l'"''""

3.0

5.6ritbphhiiiiii

0.5

1*5

jti\*( "

t

ITO;

56*V.^-'-'/i ; V60*

63*

65.

70.

71*

394*

V- .

i; :.

i

i

i)

i

i

K'J-S.":' ".'- "'- ^ DESCRIPTION

Pyrltiferotta siderite. 40-50J& pyrite*Occasional gray-blue quartz blebs*

Similar* JLt 356.5-357 interbanded sideriteand cherty quarts.

: ' ' . . - "'Iron Potnation. Interbanded blue quart*,and dark slaty bands at 55O to core. PC*'scattered pyrrhotite bands*

Interbanded siderite and cherty blue qtz*

Similar* Considerable ble'balar pyrite*

Similar; largely pyrite and cherty qu&rtz*

Cherty Iron Formation, Gray-blue to blue banded silica with considerable scatteredpyrite and pyrrhotite bands after 380.Banding very distinct at 58-600 to core.

End of Hole*

PIP TBST^Peijth, B^oh.ed. OoryeQtod

# Collar - - ' 37i-0 iBrunton on rodfl^ 20* 400 34g

200? 350 28394' 340 270

^ Bole uas started at 40O but was f la t t en ewhen the casing vas drilled into leftge.Drillers report that this was due to drilthrough loose slabs before aotu&l ledge vencountered.

SHEET NO. s

NO.

T27S:

T273J

12735

1273^

1273!

L

lingaa

1

rt. 1 Oi *. * MN.

\

A*.r?

ION. LOS*

i

t1

,

|

[ At 312.2-341.0 interbanded cherty and slaty Iron Formation ___________with sidorltc and pyrrhotite bands).^^^^ 341.0-346.0 5.0' 40.12 200.60 6.66 43.30 19.10 346.0-351.0 5.0 45.14 225.70 6.82 54.10 35.16

J 2731 351.0-356.0 5.0 46.94 234.70 5.60 28*00 24.49 J 2732 356.0-360.0 4.0 46.83 187.32 11.02 44.08 20.45

35.50) 175.75) 122.45)31.801

j* 7.8t•as.oi

i.•A'i

l

w**;* - 1; HOLE NO.'•if?;','': - 1 '.

l'.fft\i -STrtIKEfev, . ANGLE'

DEPTH

J - 6H 1030* 580 - 650*

MICHIPJCOTEN IRON MINES LTD. DIAMOND DRILL REPORT ,

.' x. - .

PLAN No.STARTED Havener l, 1950 SECTION NO. 5 FINISHED November 10, 1950 UT. 33,194 S DEPT- 33 * 382

ELEVATION 5206*. '. '. —

i*"

iiiI ig iijl f'i '

21'.

1 2*\ f*

1 2

1 21

l 2

h.'A 2

1;i i' 2i ""1

DEPTHritoM

0.0

L2.0

98.0

46.2

57.0

)8.0

L3.0

16. 0

53.0

S8.0

33.0

58.0

13.0

18.0

53.0

58.0

S3.0

TO

12,

98,

146,

167,

208,

213,

218,

223,

228,

233,

238,

243,

248,

253,i

258,

263,

267

0

0

2

0

0

0

0

0

0

0

0

0

0

0

0

0

5

DESCRIPTION

Casing.

Agglomerate, fine grained light grayishdaoitlo groundmass with frequent darkergray felsitic fragments. Very stronglysohlsted at 28-32 to oore.

Toff, medium {pray with greenish oast* At 98* contact sharp at 37 to core. After 99'"schistosity at 39-420. At 117-135 massive.

Agglomerate, as before except darker gray.Scatt. siderite and pyrite. Schistosity 43

Similar but mottled with saaewhat Irregula.cream-gray siderite averaging at 45?o coreScattered fine pyrite throughout.

Siderite-agglonerate, Fairly schistose at42~45O to oore. Sparse finely disscra. py.


Siderite, fairly massive. Oooas.py. blebs.

Agglomerate with sparse s ea t t. siderite. .

Similar; Increasing siderite. Few pyriteveinlets throughout.

Sidorito-agglomerate* Some 60# siderite.

Similar but' decreasing siderite. Scatt.py.

Similar. At 246.5-247.5 considerableoalcite and pyrrhotite.

Similar but sli^tit banding at ^.Abund ant tiny pyrite flecks giving a speckledappearance to side of oore.

Siderlte-agglonerate with soatt.py.&arseno

Slmilftr.Pre^aeut pyrite blebs. Scatteredfin* arsenopyrite. Somewhat decreasingsiderite*Similar, slight banding at 500 . Only

ANALYSISNO.

yi

i"

2736

F2737

r2736

T2739

T274C

F2741

T2742

T2743

f 2744

1274

f 274

f 2741sp.mrse sulphideo. |

re.

1

• l O) •- f. MN. A*.

; J ~ 6 SHEET NO. 2•ifcf?^'LpL-P;Hy

fi11 :j :

Fi*i•a

1 *-,iz13

1•;i;

•3

3r

j DEPTHr MOM

67.*•,'iVii.' "i"#;-;t ^••v72.C^••V

77,C•^ *'

82.C

91.f

96.E

01.:

06.0

11.0

15.5

20.0

39.0

43.5

48.0X

53.0

58.0

63.0

77.0

81.5

86.0

91.0

96.0l

-400.5

•; 'TO.:,

'278.'•..,";r

277

282

291

296

301

306

311

315

320

339

343

348

353

358

363

377

381

;,'

6

.0

,o5

5

5

0

0

5

0

0

5

0

0

0

0

0

5l

386JO!

391,0

396

400f,5

405JO

™4!05.0' 410iO

DESCRIPTION

Siderite-agglonerate, Seme 10-15^5 pyrite iblebs and traces of arsenopyrite.

Similar, somewhat increasing siderite 6 pyi

Similar. {' J

Mottled agglcmerate-aiderite with sparsescattered pyrite blobs*

Similar, increasing siderite. J

ANALYSIS .NO.

2748

2749

2750

2751

Similar. J 2752

Similar. Deaoreasing siderite. After J 2753304* schistose and sericitio at 40oto core

Banded slderite-agglomerate. Scat t. pyrite J

Siderite. Fairly massive. Scatt. pyrite. J

Agglom-siderite. Seme 35-40Jo siderite Jand scattered blebs of pyrite and pyrrh.

Agglcfnerate,8cmewhat no 1 1 led with scatt.areas of siderite and blebs of pyrite*

Similar with increasing siderite k py* J

Similar. . J

Similar, considerable siderite* J

Similar. Paint schistosity at 45-480. J

Similar. Considerable decreasing siderideJand only minor pyrite blebs.

Agglomerate. Minor siderite and pyrite.

Aggloraerate-siderlto. Scatt. pyrite blebs. S

Similar. J

Similar. J

Sidorito-agglctn. Slight banding at 50O. J

.

2754

2755

2766

2757

2758

2759

2760

2761

2762

2763

2764

2765

Siderite. Cream-buff ,taaa8ive.At 396* J2766sharp contact at 580 (chlorite slip). jMinor flocks of pyrite.

Similar, minor agglomerate areas, J2767

S id er i t o, gray-buff aod very massive. J2768

"1

1

1

•i Oa

l

*.

i••-.i ' -' ' ' ' ' . fi)

f. MN.

1i

m ' ' ' '

A*. IQriLC.3

^fey&OLE NO. J -6 SHEET NO. 3

l•7nHrli(lBf 4

li11 i

1i

1f

t

tii iiii

-i"1-— "-~ : " — - -^ V DEPTH |

mow

10.0f;Y

•s-"*'' '

15.0

19.5

24*0

29.0

34.0

39.0

44.0

49.0

54.0

59.0

64. C

19. C

74. C

79.C

04. (

89.C

94. (

98. J

*D3.(

TO

415

419

424

429

434

439

444

449

454

459

464

469

474

479

484

489

49'

498

503

0

5

0

0

0

6

0

0

0

,0

,0

,0

,0

,0

,o

.0

,0

.5

..0

3 507.5*

1*507.9 512.0s :. t 513.0 517.0

1

DESCRIPTION

Siderite. At 410.0-414,2 veil banded at530 to oore. At 414.2 drag fold out off bygraph! t io slip at 60oto oore (Fault)* Hobanding follow* the slip and the sideriteis a darker gray. At 415* graphitic slip.

Siderite, very massive gray-buff.Oooat*fine pyrite threadlets. Oaloite stringerat 417.5.

Similar.

Similar, increasing pyrite after 437* .A,t426.0 two graphite slips at '65 and 80respectively and crossing each other,

Siderite, gray-buf f. Scatt.pyrite blebs.

Similar.

Similar, sparse finely disseminated pyrite.

Similar.

Similar, occasional tiny pyrite veinlets.

Similar. At 456-457' calcite stringer*

Siderite, medium gray-buff .massive.

Similar, occasional pyrite blebs.

Similar, increasing pyrite.

Siderite, gray-buff with oream-buff mott ling. Massive with a few pyrite velnletsand scattered fine pyrite.

Similar .Oooas. calcite stringers at 60O.

Siderite. Graypbuff rma,Bsive. Scat t. pyrite.

Slmilar.Very masoive -with decreasing py.

Similar.

Siderite, medium gray-buff with scatt.pyrito voinlets, irregular in thoir cutto core.

Similar.

Similar.

Similar.

-J1 r.-""" - " l n - ~ - -^—— J..-- -•.•—.. - " - -' i-, i—--;

ANALYSISNO.

2765

277(

277:

277J

277i

2774

2771

277(

277'

3277J

J2775

J23B

3278

J276

J278

J278

J 278

J278

J 278

KE.

1

)

-t

J l1

J27E

J 27?

m

)n

•lO* •- f. MN.

,

i

A*.™| r ^——— M.

t

os*

SHEET NO. 4

PIm ?y

i5

1ii5

1

15

1

f5'

~*-. '.DEPTH:

FROMsssss

?McitoJ^5

29.0

51.0

56.0

rl.O

5.5

;o.o54.5

59.5

4.0

9.0

4.0

8.5

If3* 5

j5'

1

j~

1-S

18.0

2.0

5.0

8.0

'3.0

&8.011r*.. 5

TO

522,: •'•-.•'

526.

929.

531.

536.

541.

545.

550.

554.

559.

564.

569.

574.

578.

533.

588.

593.

595.

598.

603.

——

0

5

0

0

0

0

}

3

5

'

)

)

5

5

)

)

)

)

)

608. D

612.5

617. D'.i * i

1 :, ; 7.0 622.0

i '

DESCRIPTION

Siderite with sane 15J& diaseminated pyriteand occasional pyrrhotite blebs.

Similar. . i

Similar, " ;

Pyritiferoaa siderite* Some 75-80J& dendritlo pyrite with occasional pyrrhotite blebs'

Similar but only 45-55/6 pyrite. ,

Slderite-pyrite. 20-30^ pyrite in dark igray siderite.

Similar. About 20# dendri tic-like pyrite, i

Similar. Increasing pyritei 25-30J&. *

Similar. Pevf qtiartz blebs at 554~554,'5. ;

Pyritiferou* siderite. Sane 45/5 pyrite. *

Similar. *

Similar. 65-70/c pyrite. Minor qts. blebs. *

Similar but only 50# py.Siderite 571-573* ^

Pyritlferous siderite. 65-70^ pyrite, *

Similar. * *

Similar. *

Similar. At 690.5 inclusion of grano diorite.

Granodiorite IntrusiTe^mediura graygroundmass with abundant feldsjiar phenc—crysts. Contacts sharp at 35o vo core.

Pyritiferous sidorito.Soatt. quartz blebs.

Similar.

Massive pyrite. Occasional qtz. blobs,.

Similar, Increasing bluo-gray qts, blobs.

Pyritiferous siderite. 35-40^ pyrite ingray-buff siderite groundmasa^'tuor qtz.

Similar, increasing qtz. blobs and stringer

"^T'n "r ""J- ' •'n'"~-' ™ - ~ '-'.'??^'?-Z.~^-! ' ^'* -L^ " -ii -, , HI i . ^.

ANALYSISNO.

2791

2792

2793

2795

2796

2797

2798

2799

2800

2801

2802

2803

2804

2805

2806

2807

2808

2809

2810

2811

2812

2813

32814

r*.

-

•l O* s.

—— '

f.

——

'

MN. AB.

ssssssz

" H^.MI^

ION.tossss

f

it 1

i'

1 ' " -.' , '' . '" ' ' ' - ' L ". r'-l l ' :" \l ""•-, 1 -- : "' - . '-

SHEET No. 5

j^

j ,

In

S

II

l

1

1

1

1

1

iiiiii

*im

t- DEPTHrnoM

!2*0:;5v.-'.

!7.0• ;/:,'-'

(2.0*

.

x

-'TO

627.

632.

650.

- f D '

D

3

.

i

iiii

DESCRIPTION

Massive pyrite with scattered gray-bine * quart* blebs and stringers.

Cherty Iron Poroatlcc. Median gray with isky blue oast ( especially pronouncedwhen core is we t) .banded pyrite andsilica. Banding at 55oto core.

Cherty Iron Pormation. Oray-blue as above,well banded at 55O with occasional bandsof pyrite and pyrrhotite decreasing after 640*.

2nd of Hole..

PIP (CE3T3Deoth Xtohed Oor^eoeted

At collar - - 58* (on rods)200' 580 520400* 52J-0 450 600* 4?P -400

-

•-

.

ANALYSISNO.

2815

2816

rt. •l O* •.

i

f.

i

MM.

•'

AS. ION. LO* l

HOLE No. j - v STRIKE dueXorft ANGLE 400 DEPTH 189*


PLAN NO.STARTED tfoveober 12,1950 SECTION No. 4 FINISHED Hovmber 14,1950 LAT. si,85o s

ELEVATION 5230*DEPT. 32,380 B

p

yHrri.iP,1"i

riP18

—1

, . DEPTH

ritoMt i - -

b.oll.O

J5.0

J8.7

12.0

15.0

50.0'5.0

JO.O

51.5

15.0

)2.8

B '^vY

1™

1

56.5

TO

11,

135,

138,

142,

145.

150.

155.

160.

161.

16o.

182.

0

0

7

0

0

0

0

0

5

0

8

l186. '5

i,

,

189.'0

'••.

DESCRIPTION

Casing.

Serioite-oarbonate schist, fine grained.light to medina gray, strongly echlsted at40 to oore. Frequent carbonate blebaelongated along the direction of schist ing (possibly amygdules). Occasional ankeritestringers stained with Iron-oxide. After51*; schistosity at 45-500.

Felsite intrusive, light gray,very hard andmassive. Contacts very sharp at 52oto oore

Slaty Iron Forma t i on, dark gray to blaok, ,with occasional dark gray cherty quarts,and pyrite bands at 50oto oore.

Massive pyrite. Oocag. slaty and quartz .bands. Some 65-75/2 pyrite throughout.

Similar. 75-80J& pyrlte;only minor quartz. ,

Similar. At 154-155* oonsid.cherty qtat. ,

Similar. .

Similar, decreasing pyrite. .

Slaty Iron Formation with considerable ,qtz. Scattered pyrite and pyrrhotite.Graphite slip at 162.3*.

Cherty Iron Formation, Intortanded chertyquartz and lesser slaty and pyrite bandsat 55-500*At 169-180.5 massive blue-grayquartz and pyrite; in places scatteredsiderite which appears to be replacedpartially by the pyritejdlnof folding andbrecciation at 180.5-182.8*.

Granodiorite intrusive, med, grained ,porphyritic. Considerable chlorite developmenttowards end of section. Contacts at 40O .

Cherty Iron Formation. Similar to thatpreceding the intrusive,

End of Hole.

^-^ ' - - - -ANALYSIS

NO.

2817

2818

2819

2820

2821

2822

2823

t

rt. • l Ot

V}V1 }PeptH St

m.

T??hed

Collar75* 4J* 0

150' 390

r.

\Q

Cor

•^--—— 1 -

MN.

1i

neat e100J503**vo

sssas— — 1 1 IJ

A*.

(J

i J

sliRi i i ij Si

C 92*6*1 99'6fll

48*62oz'on n-ll TO.;jt S'S *.'1 stt"^'oif n..rn, —.r w "l OB'ce o's o'091-o'sai 0*B 'l

s^^,,-;;^.s?^^w2iM5sa::Mu^iK,';

i'&i--?: HOLE N . STRIKE

J - 8 H 0030*


PUN NO. STARTED Bovereber 15,1950 SECTION NO. 4

U^- ANGLE 450 - - FINISHED Hoveaber 18 1 1950 UT. 31,650 S utPT' ^t380 *||;Jv DEPTH 511* ELEVATION 5210*

11l11111i

•i1i;1

1Ir1'1

DEPTHrnoM

0.0

13. E

94.0

07.0

12.C

17.0

21.0

24.5

26.5

30.0

35.0

40. C

44. E

. .

TO

13

394

407

412

417

421

424

426

430

435

440

444

449

s

5

0

0

,0

0

0

,5

,5

,0

,0

,0

,5

,0

r

DESCRIPTION

Casing*

Serioite-carbonate schist. Light to mod.gray-green,daoltio -with angular andesltlofragments throughout (flow breccia). Powiron-oxide slips at right angles to theschistoslty^whlch averages at 43oto core.

At 121 rusty carbonate seam. (Drillersreported considerable sand in the coreand loss of water- return at this depth).

At 392.5-394 heavily brecciated and .shot through with quartz-carbonate stringbecoming very sericitic anft gauge-like(soft and mud-like) towards end of seotic

Agglomerate. Light gray and fairly heaviljmottled with cream-buff carbonate, largelysiderite. In places the agglomerate ha* agreenish-blue cast. Sparse scattered fineljdisseminated pyrite, often seeminglyassociated with the siderite.

Similar with increasing siderite. J

Similar f soraewhat increasing pyrite. J

Agglomerate-siderite.Few cherty qtz.blebsJ

Similar, increasing quartz blebs. J

Similar. J

Siderite. Gray-buff, f airly massive with Ja f e-* scattered q^lartz veinlets (fracturefillings). Minor pyrite blobs.

Similar. V/ell fractured as evidenced by Jtiny criss-cross qtz-carbonate threadlets

fSimilar. Only minor quartz. Scattered *

ANALYSIS

NO.

era,

n*

2824

2825

2826

2827

2828

2029

2830

2831bleba and tiny f looks of py. and pyrrhotine.

Siderite. Cream-buff , with occasional *mall areas of gray-blue agglomerate.

Similar, Scattered pyrite le pyrrhotite, ,

2832

28331

r*.

-

•i Oi 0.

-

f.

,

MN.

— -

A*.

-- - . —

ION 1.0*1

'

SHEET NO. Z

ifHfecssxsppw?:

1'"' ^4

VT:l 4j 4^~r~9i —

4

14

1—

|Vliiiiii

; DEPTHPROM

19.0•l*-: v

53.0..T'- '

55.0

58.0

53.0

68.0

73.0

78~.b

03.0

10.2

1

TO

453,

455,

458,

463,

468,

473,

478,

503,

0

0

0

0

0

0

0

0

510,

511,

( i

2

0

'•i : 1

1

1

i

DESCRIPTION

Siderite.Cream-buffjinasslve tilth oooaa.criss-cross quartz-carbonate velnlets.

In ter banded siderite and gray-blue chertyquartz In appro*. 6-inch bands at 450to co

Siderite tfairly massive.acatt.qtz.velnlets

Sitnilar.Sparse scattered cubic pyrite.

Similar, increasing pyrite.

Pyritlferous slderite.Gray-buff withsane 15/C finely dlssem. pyrite Si pyrrhotit

In t or banded cherty quartz and siderite.Occasional pyrite bands throughout.

Iron Formation. In ter banded slaty and'cherty quartz bands at 45 to coro,'withfrequent, largely Irregular, areas of pyriteand pyrrhotite.

At 478-484 massive gray-blue quartz andpyrite.

Granodiorite. Medium gray speckled withabundant feldspar phenocrysts of lightsmoky gray colour. Contacts sharp at 45 .

Cherty Iron Formation. Largely banded gray-blue to light blue cherty quartz.'

End of Hole.

DTP TESTS:Depth. gtohod. Corrected.

Collar - - 45 {Brunton on rods]150* 47i0 400300* 4l5 340450' 33e 27^0

^^ ANALYSIS

NO.

T2834

T283Ere.

T2836

12837

I283E

12839B.

J284C

re. •l O*

i

•.

i

f.

:: ss:•^^•••^i.MMH

M H.

\

-' '

~VI*MM^

AS.

:ssz

IO LO'

i

4

f i

06*12 82*9 02*02 01*6 29*1 OO'WI

HOLE NO. J - 9A* STRIKE du* Forth

MJCHIPJCOTEN IRON MINES LTD. DIAMOND PRILL REPORT

\PLAN No.

STARTED November 18,1950 SECTION No. 4^.: ANGLE 650 FINISHED November 19,1950 UT. 31,650 H Ut"' ^•oou J|^ DEPTH 109* ELEVATION 5210*

J-,• ~l1iir

-

1ii

!

DEPTHr motu

o.c10* C

TO

10

109

0

0

i;

i

DESCRIPTION

Casing.

Sericite-oarbonate sohist. Fine grained,medium gray-greentdaoitio with scatteredto abundant breccia fragments of darkgray-green colour and andesitlo ocrapositiiOccasional rust slips at 60-670to oore|and a few chlorite-talo slips at 10-200.

At 10-30 schistosity at 28-340.At 30-63 schistosity at 24-280At 63 abrupt change in schistosity to

16-180to core (large fold or roll)*At 99-109 schistosity at 8-12oto core,

xEnd of Hole,

T\l L) flVJJ*OfltQ mUjjt ^-JVvX^)2

Depth J5tohoi CorrcokiAcollar - - 65O (Brunton on rods)

100* 740 690

* Hole was abandoned at 109 feet.Anticipating a flattening of the hole aaa general rule J-9A was drilled fairlysteep in an attempt to obtain a deepintersection of the siderite zone indloattin J -8, drilled from the saroe set-up at anang^e of 45? at an approximate verticaldepth of 300 feet. However, as the holesteepened 40 in the first 100 feet andbecame very acute in the relationship tothe schistosity further drilling wasImpraotib&l.

ANALYSISNO.

n.

d

ri.

i

•l O* *.

i i *

f. MM.-" MI.

At.

K

"TL

li

i1 t' i1

lHOLE No. STRIKE ANGLE DEPTH

MICHIPICOTEN IRON MINES LTD.


j - 9 PLAN No.Due North STARTED November 19, 1950 SECTION NO. 4600 FINISHED November 29, 1950 LAT. 31,650 H DEPT' 32 *3BO796* ELEVATION 5210*

:rrr

4

t

i

i

i

\

ti*

f•t

is

DEPTH

r*OM

0.0

12.0

53.0

12.0

14.0

19.0

32.0

37.0

42.0

47.0

51.5

55.5

TO

12,

433,

442,

444,

449

532

537

542

547

551

0

0

0

0

0

0

0

0

0

5

555*5

560 ;oi

60.0 564; 5

DESCmPTION

Casing.

Serieite-carbonats schist. Light graydacitio groundmass with gray-green angularfragments of andesitio composition to ^-inin length (Plow Breooia) . Occasional narrolocally feldspathized sections. Schistositat 28-340 to core.At 60-63.5 heavily feldspathized withsome introduced quart and frequent eer -pentine (slickenside) slips. At 61 dis -placement indicated by difference In com position on either side of slip at 30O .At 123.5-143.2 andesitic, gray-greenmassive to schistose with scattered qtz-carbonate veinlots at 30O and eo^to core.

Acid Agglomerate. Medium gray with bluishcast, fairly schistose throughout althoughvery masaive-like in appearance.

Similar but src*ky gray in color and wellfractured with darlc (chlorite) criss-crossveinlets. Soxe scattered sidorite-ankerite

Similar.

Agglomerate. Kodium gray with scatteredlighter gray fragments. Schistosity at 2So

Similar, sorae scattered siderite.

Siderite. Dark gray, fractured and scene -what brecciated with few blebs of quartzand scattered agglomerate.

Similar. After 545 few blebfl of pyrite.

Mottled siderite and agglomerate.

Siderite. J!lnor pyrite; scattered agglom.

ANALYSIS

NO.

1

fr

T2841

72842

V

J284v

J2844

J 204

J284

J204

Siderite and agjlonerate with scattered [J2G4fine and blebular pyrite. Faw chlorite si

Similar, increasing siderite and pyrite.

i

lj*s.

J 2 84

rt.

3

r

Ei

e

•i Oa

1

i

i

s

•- r.

1

MN.

i

t

;

AS. |

\

1

No., J - 9 SHEET NO. zW&'S1R''"' * i.teSbV&mr"b 'r'P {tm

1 !

rijii iii

6

1 6

i:iiii

S5S SSSDEPTH

rnoM^ i i -'B

68. E;-'" :

72.5

74.5

76.5

81.0

85.5

90.5

95.0

96. B

00.0

05.0

10.0

15.0

20.0

24.5

28.5

33.0

47.0

55.0

70.0

J73.0

TO

568

572

574

576

581

585

590

595

596

600

605

610

615

620

624

628

633

647

655

670

673

674

i

^zzz

5

5

5

S

0

5

5

0

5

0

0

0

0

0

5

5

0

0

0

0

i"

.5

^^ - ' ' — " - " — -

DESCRIPTION

Agglomerate with 25-30J& siderite and py.

Siderite* Cream gray, fairly massive,scattered fine pyrite and quartz blebs.

Similar but some 15-20^ pyrite. :-

Aoid Agglomerate Bottled with scatteredsiderite and pyrite*

Siderite* Cream buff, well fractured withsparse pyrite and minor agglomerate*

Similar. Some 10-12^ pyrite (blebular).

Similar, decreasing pyrite. Scatteredagglomerate and a few quartz blebs.

Similar.

Granodiorite dyke. Gray-blue porphyritic*Contacts sharp at 370 to oore. Sideriteinclusion at 595.0-595.5.

Siderite with minor agglomerate and occas ional blebs of pyrite and cherty quarts*

Similar, increasing agglomerate.

Siderite and agglomerate. Minor pyrite.

Similar, occasional quartz blebs.

Similar, somewhat increasing siderite.

Siderite with 20-25/S pyrite. Scatt.agglora

Agglomerate with scattered siderite.

Similar, somewhat increasing siderite.

Agglomerate with widely scattered siderit

Ottrelite schist. Medium gray with darkflecks. Schistosity 30-330 to core.

Acid Agglomerate with local narrow eeotiorof ottrelite schist. V/idely scattered areaof siderite {largely irregular to oore).

Siderite with scattered agglomerate. Few vugs lined with calcite and coarse cubic i

Siderite. Croa-n gra7. massive '.rith a few tiny criss-cross quartz thrcadlets.

ANALYSIS

NO.

2851

285:

285;

265:

2854

2851

285(

J285'

J285f

7285!

T286C

7286

7286

7286

7286

7286

7286

*

9

13

J286 )7-

1286

re.

i

1,

E

• l 0* i

i

f.

*

MN.

•i' - - - ; :

sass

•WMMM

AS.aJ —

1

fix; HOLE NO. J - 9 SHEET NO. 3

PB*P'prVfa6

SL•?(Pf 7:

7 " *

1ft

l•7;

r7-

11'

75

1

i ——• DEPTH

FROM

rf.s/i: : . '.

•9.6

34.0

J7.0

a.o5.0

0.0

5.0

9.5

4.0

9.0

4.0

9.0

4.0

9.0

4.0

9.0

4.0

9.0

4.0

• 749.0

TO

679.

684.

687.

691,

695.

700.

705.

709.

714.

719.

724.

729.

734.

739.

744.

749.

754.

759.

764.

769.

1773.

0

)

)

)

)

)

)

5

)

)

)

)

)

)

'

)

)

1 l

)

)

b/3.5 778.0

1 ! 778.0 |703.

iD

1

DESCRIPTION

Siderite. Cream gray, fractured with tiny ;quartz threadlets. Minor unreplaoed ma ter li

Similar, very heavily fractured (largely ibroken core).

tv

Similar with frequent graphite-chlorite ^slips.

Similar; some scattered agglomerate. i

Similar. Heavily fractured and brecciated.*

Similar, fair amount of agglomerate. i

Similar, decreasing agglomerate. At 704- i705 well banded siderite at 350 to core.

Banded siderite, minor folding. i

Siderite. Cream gray, massive with few iblebs and vei&lets of quartz. :

Similar, darker gray. S cat t. py. 4 pyrr. J

Interbanded siderite and slates with Jsoatt. pyrite and quartz bands at 25oto ooj

Largely massive pyrite with some gray qtz.*and minor slates. Considerable folding.

Interbanded slates and -pyrite with oooas. Jgray quartz bands* Considerable folding.

Similar, banding at 30-350 to core. ;

Massive pyrite and quartz; scatt.siderite.J

Banded siderite with scattered pyrite, J

Pyritiferous siderite. Some 40^ dendritic Jpyrite and occasional gray quartz blebs.

Similar. J

Similar but only 15-20^ pyrite. J

Similar. t

Similar, 35-45)o pyrite. Scatt.qts. blobs, *

Similar.

Similar, 15^ pyrite and scattered blebs ^of pyrrhotite throughout.

ANALYSIS

NO.

2669I.

2870

2871

2872

2873

2874

2875

2876

2877

2878

28790*

2880

2881

2882

2883

2864

2885

2886

2887

2888

2689

2890

2891

re. •l Oi

i

m. f-SS

pHm^^mm

MN,

•B

MMVMHm

AS. ION (.0*i,

ii

^^mm

M*#fJ^•*'-*-- *HOLE NO. J-9 SHEET NO. 4

DEPTHrnoM

35.0. \

4-".'*" '-'"

87.5

92.0

i

i 1

TO

787

792

796

* '

ii i

5

0

0

1:

DESCRIPTION

Pyritiferous siderite. Some 25# pyrite •with occasional blebs of pyrrhotite.

Massive pyrite and pyrrhotite with scatt ered siderite and quartz. t"Cherty Iron Formation. Banded gray-blue cherty quartz -with scattered interbanded slates and minor pyrite. At 792.0-792.5 acid intrusive (granodiorite) with abunda bright green chloritic {fuchsite) pheno - orysts.

BID OF HOLE.

PJTP TESTS

Deptfc Btofcojk Corrected, Collar — 600 (on rods)

100* 6l20 550 , . 250* 580 510 450' 540 470 650* 52p 450

*

l

ANALYSISNO.

289!

2892

J2894

at

l

re.*

i

•i O*

i

•. "- 1

-

MN. A*. 10 LO

1t i

t

[

IP pt^Sample;|^28te. |^2884:* 4f2885J: |^|2886i l^2887; ^12888^ I'j/2889 j -2890

j; J 2891 a J 2892 | J 2893.Totalsli

Zsg:s8f*\: ^:':'-~i -\*-"-'^^?:r-. Vvy^vSf^v/r-;,: ,

jf 5'abii :uo.

Footage; '739^0^744.0 744.0-749.0 749.0-754.0 754.0-759.0 759.0-764.0 764.0-769.0769.0-773.5 773.5-778.0 778.0-783.0783.0-787.5 787.5-792.0739.0-792.0

J -9

Width5*0* 5.0 5.0 5.0 5.0 5.0 4.5 4.5 5.04.5 4.5

53.0'

•/•\ ' :''

*Fo26.28 36.10 40.32 39.52 43.53 39.12 40.62 41.12 39.32 37.91 46.93

- . , v.., v -, . ,, ,.- , . .- - . -. -. . - .-.-'.-^.rT''-^.; -.'v-' - : ' '" . -'.- v-'.--* '-"- - - ' - .'.' : :,:'*- . . - - '- ' - '^.'•'••"•.•'•.•.•\^.

SHEET 5

Ft*3#Fe131.40 180.50 201.60 197.60 217.65 195.60182279 185.04 196.60 170.60 211.18

2070.56

*Si.)213.' 52 8.: .6 4*50 5.24: 3.U 5.24" 5.88 5.44 7.54

n.46 7.20

Ft^SSi69.10 40.80 22.50 26.20 15.70 26.20 26.46 24.48 37.70 51.57 32.40

373.n

02 JfS Ft.2#18.71 93.55 8.01 40.05

23.12 n5.60 19.10 95.50 16.01 80.05 n.46 57.30 23.59 106.15 28.27 127.22 19,30 96.50 TJ.09 103.90 25.66 n5.47

1031.29

5 Grade

) *Fe - 39.07 j&iQz - 7.041.S m 19.46

lll l/'

l l l l lll

HOLE No. j - 10 STRIKE Doe North ANGLE SO0 DEPTH 287*


PLAN NO.STARTED December l, 1950 SECTION No. 3 FINISHED December 3, 1950 LAT 31,950 IT

ELEVATION 5296*DEPT. 31,880 Z

ss:

1

1C

,l

111

11111Ig *

111fi•i

DEPTHFROM

0.0

6.0

26.0

30.0

46.5

59.0

74.0

79.0

S4.0

89.0

93.5

OQ.O

00.5

TO

6

26

30

146

169,

174,

179

184

1G9,

193

1SS

0

0

0

5

0

0

0

0

0

5

0

200,, 5i

203 JO

03.0 2071 5

DESCRIPTION

Casing.

Sericite-carbonate schist. Light gray-green /very hard and rhyolitic with a fal*amount of serpentine throughout. Scatteredlimonite slips at 40-60o to core.

Similar with abundant rusty slips andconsiderable introduced quartz v/ith soatt.fine arsenopyrite and pyrite. (Sample cutfor Au and Ag assay).

Similar with only a fey; xvsty slips. Schistoslty becoming more pronouncea o. t 30-38 0,At 144-146.5 largely broken core witha few rusty pieces (somewhat pebble-like);considerable introduced quartz evident.

Acid Intrusive (Fuchsite). Medium gray-green with abundant bright green flecksor ph enocry s ts, presumably fuchsite, some what elongated along the schistosity at25~300to core^-t 146.5-148.5 stronglysheared at 20-220 with considerable qtz.

Mottled agglomerate and siderite with afew bands of dark slaty-like material.Schistosity 28-30o ^inor arseno at 169-170

Siderite. Cream-gray and fairly massive.Minor fine pyrite and few quarts blobs.

Similar, scene agglomerate.

Similar, Scattered pyrite 4 pyrrh. blebs*

Similar. Fuchsite tongue at 193.2-193.5

Granodioritio Intrusive. V.odiun to darkgray v/ith fairly abundant darker grayphenooryBts.PosslMy a phase of the Fuohs:

Similar. At 2UO-;. - ^.i- ^ r:.;,— jrc-j.i fuchsitegr&dational from the dark g;*ty material.

Siderite. Fairly jnassivo;minor qtz.

Similar with sparso scatt. pyrrh. t py.'

-—— .^M^.. __ ___ _ ___-- ,- -..,,-,n-..n.-t ...— -r-,., r--^,^-,.^ , ,.- ^ - — - ————.——-—^^.

A'NAUYsis "~~NO.

1289!

F289*

ft

r289'

F289E

I209S

I290C

J2903

to,

r*.

,

J2903

J290:

J290-

•l Ot m.

t

r.

*

MN.

i i

A*.' ' -J-

ION. LO**

1

HOLE No.'J - SHEET NO. 2lB 3?# ~B S 2•i?pp|:;'!2

^c2

• 2i 2ir

' 2

1*j^

121

f 2(

•W 9 HI M

I p

1 2" 2

1 ^

2

11

DEPTHFROM

;'vvj™ -*'

-'3 y J -M'V.' -•A . J ' -

12.0

L5,0

L7.0

22.0

24.0

53.0

55.5

10. 0

15.0

50.0

55.0

59.0

i4.5

i7.5

:TO

212.

215.

217.

222.

224.

233.

235.

240.

245.

250.

255.

259.

264.

267.

271.

i71.0

73.5

78.0

52.5

'

273.

276.

0 '

0

0

0

0

0

5

0

0

0

0

0

5

5

0

5

0

262 .'S

20 7 JO

DESCRIPTION

Siderite, Dark crera-gray. At 209-209,6 ;aoid schist (schistosity at 35O ) followedby considerable Increase in pyrite andminor fine arsenopyrite.

Similar tdecreasing pyrite, Few quarts blebs,

Fuchsite, Contacts sharp at 35oto core, ,

Siderite. Klnor pyrite and qtz. blebs.

Similar, Scattered quartz blebs A string, i

Granodioritio IntrusiveU.t 224.0-224,5 , fuchsite (gradational). At 230.5-233fuchsite, somewhat sheared at 32oto core.

Siderite with scat tared {fairly large)pyrite blebs. Acid schist at 234-234.7.

Siderite. Dark gray traassive. Minor pyrite..

S 1m i larkin or unrenlaced material. i

Similar, Increasing py. Schist at 247.5- .248,2, Scattered blebs of pyrrhotite.

Similar. Scattered schist at 251.5-253. i

Similar^ somewhat increasing sulphides.

Intermixed siderite and gray cherty qtz. *Scattered pyrrhotite blebs.

Similar.

Granodiorite. Dark gray-green, porphyritic..7/ell sheared with scat t. introduced quartz.

Intermixed cherty quartz and siderite. .

Similar. Scattered pyrrhotite blebs. .

Similar, increasing quarts.

Bonded light gray cherty quartz. Banding .very distinct at 300 ,Very minor sideriteat beginning of section.

End of Hole.

DIP T^STS^^ i ———— — — - i ! Depth Etqbct?, Corroqt'si

I t Oollar - - 500100 520 44k0250 510 43j0

K O.

2905

2906

2907

2906

2909

2910

2911

2912

2913

2914

2915

2916

2917

2918

2919

2920

2921

2922

2923

rt.

k

,

•l O*

A M At

B.

i

,YSI9

-

. - ,!ss;

MN.

t

iti . ! i j

AB.

l

i^^'^jttuusjiD,

67.16111.91110.7163.04

2.12 J 20.34 42.39 J 15.45

24.58 27.S8

.#2903200.8-203.0 2.5* 26.87^2904 203.0-S07.3 4.5 24.87gj? 2905:207.6-312.0 4.5fo 2906*212.0-315.0 3.0lotal* 200.5-215,0 14.5*

R^T^

X

l

i| l l ll ll l l l l l

sfp-'^'-Y^ -^,, n P* - - . - .. .-sfev::'.vv '" "v ' ' ••-- p-

WW&'Z '•••'-'"' ' ' ' ' ' -UT^-D;/v,'.- . . . ;

HOLE NO. STRIKE ANGLE DEPTH

J - 11

H l0 E 500 470*


PLAN No.STARTED December 3, i960 SECTION NO. s FINISHED December 7, 1950 UT. 31,800 H

ELEVATION 5280*DEPT. 31,880 X

•I

C

DEPTH

rflOM

0.0

6.0

m11

ffi1 *

1•x14

1l 4

i;1;k -jm om

43.3

50.5

39.0

34.0

98.0

)2,0

)7.0

12,0

17. 0

21.5

TO

6

143

150,

389,

394,

398,

402

407

412

417

421

426

ae.oUsi31.0 43ft

0

3

5

0

0

0

0

0

0

0

5

0

0

0

DESCRIPTION

Casing*

Seriolte-carbonate schist* Light gray-greefairly rhyolltio with considerable serpen tinization throughout* Schistosity at 23-2to core. Very minor cubic pyrite.

At 38-41 largely blue-gray quartz.At 141-142 heavily feldspathized.At 142-142.3 fuchsite tongue.At 142.3-143.3 heavily sheared with oktz

Acid Intrusive. Light green with abundantbrighter green phenoorysts.Oontacts at 45?

Serioite-carbonate schist as before.At 162.4-163 intrusive tongue (fuchsite At 193-198 fairly well brecciated.

After 347 few scattered carbonate (oaloi ankerite) veinlots t largely irregular intheir out, often being criss-crossed.

Similar but heavily fractured and brecc iated becoming dark green to ond of seotio

Siderite. Dark creaa-gray with a few gray quartz vsinlets and some 5-lOj? dissem. py.

Pyritiferous siderite. Dark gray ground mass with 30J* dendr i tic-like pyrite.

Similar. At 402-404.5 only minor pyrite ;v/ith considerable calcite and massive py.and occasional vu^rs at 404, 5-404, 8, (Fault?

Pyritiferous siderite. Some 65;"o heavilydisseminated pyrite, Occas.' quartz blebs.

Similar,

Similar. Occasional pyrrhotite flecks.

Similar, so-newliat decreasing sulphides.

Similar. Faint banding ut 45-500 to core.

Similar.

ANALYSISNO.

O

e-

F2924**

T292I

1292

f292

)-

r 292

(292

1293

F293:

12932

1293;

r*..

j

\

•i O*

i

•- f. MN. A*. ION LO*

IfftOMsa

AV&••Qi.^mW; -:

•B-P

G.O

j-TO

44S

451.0

SHEET NO.* 2

o-;

I.- 470.b

i'^';:- :;'''" ; '''':;;"'--' .-DESCRIPTION- -\' : ' " ;;^-.-;' . -\ /\-:- . --' r,;. . - :-. -,. ; - -

Pyrltlferoas siderite. Some 45-50^ heavily, disseminated pyrite with traces of pyrrhot Occasional small gray quartz "blebs.

•r* " - . ' ' '

Cherty gray quartz Iron Pornation .with "v i interbanded siderite and pyrite* :'

* *~ Similar. Considerable breooiation at 44 S- i 448. Occasional pyrrhotite blebs.

ANALYSISNO.

2934 te.

2935

2936

rt. •l Ot *.

-

f.

Cherty Iron Formation. Medium gray quartz •with scattered interbands of siderite, pyrite and pyrrhotite.

End of Hole,

PIP TE3J3*Depth Etched

Collar - - 500200* 550 47j400' 54^0 470

'feVx-}\ *-"';" •• 14v,^'.',:i ' .' : .-'-' -'ttiKKT HO. S

C^f*™ . 1 "'

1^925^-v|2926P^y^T-^'2928''^

f ^929 293*

J' 2931A 29321 2933T 2934•Mals^Totals

l1

111

T; ;vyo394.398.402.407.

otage -0-398.00-402.00-407.00-412.0

412.0-417*0 417.0-421.5421.428.431.436.394.402.

5-426.00-431.00-436.00-442.00-442.00-442.0

Width4.0*.4.05.05.06.0 4.54.55.05.06.0

48. O 140.0'

P*28.7929.4936.9040.9240.72 38.2238.9241.1238.3235.90

y* 4x#.115.16117.95184.50204.60203.60 171.99175.14205.60191.60215.40

1785.651552.4S

Xntarttotion(40

J&iOjj21.9026.308.864.926.499.547.846.06

10.5416.44

7t.x#K*87.60

105.2044.00

'24.6032.45 42.9935.2825.3052.7092,64

543.09350.20

312

fr.83

14.7610.1029.1729 2819

.63

.70

.7028. IS2319

.06

.71

It*

515950

145148 129

88140115

xjte Qr*d*.32.04.50.85 T&9 m 37.20•15 jfaiOj . 11.81.13 tt a - 91 Al• OD.60.30

118.26 )1046.82

402.0-442.0 } P* ".0*) 1

;

ysi**2"

936

38.e.

23.

.46 (Sae ~b*lo*)

8176 41

i i i i i i

V.'

li

'S;-sC'-^ i.-;-'-"'^ '':i -"'; 'fa#'tfS^..;.'- .;:.,.

ANGLE DEPTH

J. -12 Due North

730*

MICHIPICOTEN [RON MINES LTD.


PLAN No.STARTED December 9, 1950 SECTION NO. 3 FINISHED December 16, 1950 LAT. 31,650 N

ELEVATION 5253*DEPT. 31,880 E

Lri

^^H*r•^M

iiii1iii

; DEPTHritOM• H ' '

O.C

5.1

40.5

44.0

31.0

34.5

35.0

51.0

)3.5

)6.5

18.5i *

ii

i

S4.0

TO

5

240

244

331

334

535

551

603

60D

640

5

5

0

0

5

0

0

5

5

5

t

6 50 JO

654.0

l659JO

.

DESCRIPTION

Casing.

Sericite-carbonate schist, light gray-greirhyolltlo schist with occasional sectionslocally feldspathized. Schistosity faintljdlsoernable at 22-260 to core. At 86-109darker green, fractured and brecciated wHscattered quartz blebs* Schistosity at 28(

Acid Intrusive (Fuchsite). Modlvra gray witabundant phenocrysts of chromium mica(orfuchsite) of bright green col our. Somewhatsheared at 40-43 to core.

Sorlcite-carbonate schist as before. At269 1-inch banded cherty quartz at 20O.

Quartz Vein, Smoky-gray, minor inclusions Zof schist, Ko apparent mineralization.(Sampled for Au and Ag).

Serioite-carbonate schist. Occasional grayquartz blebs and stringers. At 448.0-472strongly fractured with. heavy brecciationat 463-467.

Acid Intrusive. Fuchsite phenocrysts.Contact at 535 exceedingly sharp at 48otocore. Fairly schistose at 30-350.

Sericite-carbonate schist. Booming verymuch harder and rtyolltio after 570.

Acid Intrusive (Fuchsite) .Contacts at 20O

Sericite carbonate echist. At 610-612largely quartz (injected). At 619.5-621.3considerable gray quartz. After 636 fairlywell fractured becoming darker groen toend of section.

Intrusive (PuchBito) .Fo-s ohloritic slips.

Sideritized schist, RhyolitJc schist withv/Ith scattered siderite and fine pyrite.

Sidcrite-agglomerato. Eoavily mottled

ANALYSISNO.

n

1*1

2937

F293f

rt.

1

f293c

J 294

3

3

•l O* s. f. MN. A*.

-

ION. LO**-

*

i

creon-'jrcy and dnrX rrrey with bluish cs.st. ; j ' 1 i

mi: HOLE NO." J - 12 SHEET NO. 2

KmI^'K*'*"* l^j*t'

|1

Pl™51

li A

P1 j

|1l6

1

W"

((3

i7]

1li

\

l

1

1

isa-s^-:.: i ni -rDEPTH

rnoM•LS — -9.P

4.0

9.0

3.5

6.0

2.5

7.0

1.5

5,5

0.0

4.5

2.0

8.0

3.0

f. TO,

564.

369.

573.

578.

682.

587.

591.

595.

700.1

704,1

712.

718.

723.

730.

-/;

i

i

i

i

i

))

)

i

j

*

i1

l . i

11

: ' '

1

t

' '. -

, DESCRIPTION

Aggloraerate.Dark gray-green with scatteredJcream-gray siderite and few quarts blebs*

Similar; only sparse siderite and pyrite Jblebs Jit 666-666.3 granodioritio.

Similar. Brecciated at 669-671.5. J

Aggloraerate-siderlte. Breccia at 674-677. J

Siderite-agglomerate. Considerable sider- Jite with scattered angular (breccia)fragments of agglomerate*

Siderite. Minor agglomerate fragnents. JSparse finely disseminated pyrite.

Siderite-agglomerate. Considerable breoc- Jiation at 689-691. Scattered quartz blebs.

Similar .increasing siderite. At 691,5- J692,8 considerable dendritic-like pyrite.

Agglomerate with scattered sider It o, A t J697.5-700 light greenish schist withscattered tiny flecks of pyrrhotite tt py.

Similar, only minor siderite, J

Similar, Occasional cherty quartz blebs. J

Intorbandod slates and cherty quartz (I. JFormation) with frequent bands of pyrrhotltand e ea 1 1 or Ad coarse cubic pyrite.

Iron Formation, similar to above butbecoming more sllioious to end of section.

Banded cherty quartz with scattered bandsof pyrrhotite.

End of Hole.

PIP TESTS:Depth Etched, Correoted Collar - - 5?k0

200* 600 53|-0400* h 4Y 0600' 52j0 450

i

-- ' ' i ANALYSIS

NO.

2941

2942

2943

2944

2945

2946

2947

2948

2949

2950

2951

2952e

rt. •l O*

i

t

•- *-

i

i

MN. A*.KSS

^^^—-^^— — —————— -

I^^^^M?*^.^ '^^••;'^;'^';O'; -''V:v -Y" : V'O.' '";. ; IJ^P^^^^-Wr ^i'f.^-:-:'-. •'•'•-'.•'V.:'. ' - L 'v-- :--' -' -'"!^V^^^-:-^-'- v^;^^g^-^,,,.-.,:,.f*P EHSEZ SO* 8

Width JS3102 yt.xSZ3i02^1682.5-687.0 4.5* 26.08 U7.S6 19.96 89.82

sL*f 682.5-687.0 4.5* 117.86 89.83 16.29

l\v.t•j-',

i i i i

HOLE NO. J -13vj^ffv^ STRIKE Due north

ANGLE 550DEPTH 488*

DEPTH

IrftOMI TO

0.0

7.0

7

429


PLAN No.STARTED January 3rd, 1951 SECTION NO. 2FlNISHEDJanuary 10^ 1951 UT. 31,800 H DEPT- 31 * 380 E

ELEVATION 5255'j———————————ANAUYSIS

DESCRIPTION l————:————'———:——————

29.7

i2.0

, o•152.0

459.0 51.0

4 55.O 1.0

437

442J

447

452

459

461

466

471

475

fre.o 468

O

l

i

Casing.

Serlcite-carbonate schist. Fine-grained, light greenish-gray, rhyolitio and very massive lookirj but schistosity discernable at 300 to cor". Pew iron-oxide slips and fractures, largely at 70-850 to oorejtare quartz veinlets at 25-350 to core.

At 164-174' dark gray-green and eotaewhatbrecciated.?-!inor cubic pyrite flecks. After 365* fairly frequent saioky guartz

veinlets and stringers.

Agglonerate.Dark gray with bluish cast. V/ell fractured \7ith criss-cross carbonate veinlots (ankerite-siderlte).

Fuchsite intrusive.Light gray-green with abundant bright green phenocrysts. At 440, 441.3 locally feldspathizod with conside fine cubic pyrite.

Cherty quarts with siderite and fracture- filling to dendri tic-like pyrite.

Slailar. At 449.5-450 fuchsite tongue. Fuchsite intrusive.

Cherty quartz mottled with siderite 4 py. Similar.

Similar.

Cherty quartz -with scattered siderite. Sonewhat banded at 35-400 to core.

Banded cherty quartz (Iron FormationJ. anoky gray to blue-gray quartz scmowhat mottled with crea-a-gray siderite areas v/idely scattered.

End of Hole.

• l O*

DIP

(on rods).

l-HOLE No. J -14 STRIKE Due Korth

863*DEPTH


PUN NO.STARTED January li, 1951 SECTION No. 2 FINISHED January 22, 1951 UT. 31,630 K

ELEVATION 5243*DEPT. 31,380 S

j J DEPTHjlritoM

(l

1t

1

1p

J1

1

1

1

1

1

1

!l

0.0

9.0

2.0

7.0

1.0

2.0

i6.0

TO

9

52

837

841,

842,

346,

383

i

i

i

i

0

0

0

0

DESCRIPTION

aslng.

"\aohsite intrusive. Kedivoa gray with abundsrij^it ijreen phenocrysts. Occasional iron-

wcide stained sllpsJU 31-36 feldspathised.

erlcite-oarbonate schist (Hhyolite flow).igit green gray, fairly massive and hard ith very faint schistosity at 20oto core.At 130-140 slip at 2-5oto core.After 370 scattered quartz veinlets.After 560 becoming somewhat fractured.

gtjlomerate. Medium gray. Sparse dissem.yrite and minor siderite,

yritiferous siderite. Sane 35jo dendritic-ike pyrite in oream-fjray sidoritic matrix,

?ev; scattered cherty quartz blebs.

Jherty banded quartz (Iron Formation) .Grayto gray-blue, fairly well banded at 400 tolore. Few scattered siderite bands,

Jherty Iron Formation as above. At 652-860joroewhat brecciated.

3nd of Hole.

DIP TESTS'pepth E t eh ejl. porject^iCollar - - 620

100' 65^-0 590300' 67 0 61fc-0500' 67^0 620700' 7 O0 63J,;0

:

ANALYSIS

NO.

t

296C

2961

\ 29 62

re. l Oi m. r. MN. A*. ION. LO* M

^^H

1

lll

HOLE NO. J ~ 15

STRIKE Due South5^; ANGLE - 450fe DEPTH 563*


PLAN No. STARTED January 26, 1951 SECTION NO. iFINISHED January 31, 1951 UT. 32,350 H

ELEVATION 5060'DEPT. 30,890 E

l . '\

rlli1lriii,1

ortit-

DEPTHrnoM—— —

0.0

6.0

J7.0

54.5

53.0

'6.0

?e.3

)1.0

.4.5

'•o.O

TO

6,

67.

84.

153.

176.

1G8,

201

.04

263

;

0

0

5

0

0

3

0

5

0

~7f .0

•- ' — ',, y - ^^

DESCRIPTION

Casing.

Aoid Tuffs. Gray-green ,daci tic, fine tomediua-fine grained, well banded at 45-480to coire. Scattered Iron-oxide stained slipat 60-65 jminor pyrite flocks throughout.

Granodioritic Intrusive. Greenish-gray andspeckled with v/hite-sray phenocrysts offeldspar somewhat altered to carbonate.Fairly well fractured throu^iout '.vith -sone scattered brecciation.Considerablecarbonatization throughout.

Acid Tuffs as "before with sane development of sericite alonj the banding (\vhich is likely coincident schistosity). At 130-134frequent slips lined with iron-oxide stain(Drillers report voter lost at this depth)

Sericitic Tuffs, Similar to p^cedins butnumerous talc-sericite bonds parallelingthe banding (and very likely resultingfrom shearing coincident with the primary banding). After 166 frequent bands of lifjhcolored carbonate. Bonding at 40-43o to cor

Intercalated sericitic Tuffs and chertyquarts bauds (the latter resenbling theIron Fomation). Sparse scattered pyrite,largely fracture-fillinjs.

Sericitic Tuffs, "/ell banded at 30-350 .

Intercalated cherty quarts and tuff.Scatt

Sericitic Tuffs. After 226 very highlysericitised ..nd v.'.uch lister colour thanprecodj.n^ seo'.iors. Boiidinj at 30O . At230-232 scattered frajnents of jray quartAfter 25C beco:'inj darker jriy and morec*'ilo*'i tic.

•"iiv.rioAiorit.ic Intrasivft. jrennish-^ray,i'oiv'xyritic. '.Veil alt^rr-d c.:id -Jractured•:ii l i scuttered .;i'^.rtn-carbo:v-te strinjcrsContacts sViar^t at 32 D to GOTO.

ANALYSISNO.

2.

tf.

M. •l O* S. f.

t

MN. A*." "

1t

KfDEF ^ ImoM

|i*

1ii'••~('!i

~ —— :

re^of':v !j.:j' ( -, -'"

U2.0

iif.i

4

1i;i4

1l 5

fl

1

1(

l

J4.5

72.0

n. 5

J2.0

55.0

iP.O

11.0

17.0

)1.0

)5.G

i

OLEis. -.' TH |

T0 1

312,

434.

472.

477.

402.

485

486

491

497

501

505,

563.

1l

li-.

NO

)

5

0

5

0

0

0

0

D

0

D

D

.Jv- 15

DESCRIPTION r

Sericitic SMffs. Medlun ipray-green , bandedat 34-360to core. Kumeroas thin fllny bandof sericite and chlorite throughout. At305 9-inch tongue of Fuchsite at 45oto oor

Grtnodioritic Intrusive. Kediutn grained,Sray-ijreen speckled with white carbonatef leeks, fairly hard and acidic but in placeheavily fractured with considerable chloriand some talc developed. Fev? scatterednarrovj sections of feldspathization withcoarse cubic pyrite. After 359 darker greeand very dioritic scroev/hat mottled withcream colored carbonate. At 423-425 wellsheared at 55oto core.

Ottrelite Schist. Sray-green to ara7tstrongly schistfy" at 50-54oto core.Locally abundant to scattered crystals ofottrelite. At 438— i46 somewhat dioritic.Considerable sericite throughout.

i

Similar with minor siderite. *

Acid Agglomerate. l.Tedium crar-green andsomewhat mottled with sparse scatteredsiderite and 10/b coarse cubic pyrite.

Similar but lighter colored and only few i

SHEET No. 2 • ~

ANALYSISNO.

.

1

.6

L

1 .

-1L

. " :- 'i

2963

2964

2965scattered pyrite cubes.

Similar with soraev/hat increasing siderite.*

Impure Siderite, IH\11 oroan-gray,fairlymassive looking but very poor fracture.ITinor pyrite flecks.

Similar. Occasional cherty quartz blobs.

Acid Agylor?. orate. Very ninor siderite andfew pyrite flecks. At* 497-496 dioritio ton

Ottrelite Schist. ITinor siderite.

RVyolitic Schist. Li^t greenish ^ray,vory hard and massive-liko with scattereddark ^ray cjuartr fracture-fillings. After;-12 lijht [preen and vory rhyolitie.(3',-ction resa-ibles the Serlcito-oarbonateschist encountered in holes J-13 c-nd J-142nd of Hole.

DIP TESTS:Depth Etched 5.9-rJL.leeJ;.0'jL

Jollar - - 4 G0i i :~ r C" -it ~: -;I 0 : f, " ~ ' -: r

2966

2967

2966

2969;uo.

2970

*

i

•lO. I

t1 i

B.

l

f. MN.

i

Am.

*

.

1 t

ION.LOSS1 L.

1

r :MICHIPICOTEN IRON MINES LTD.


'

HOLE NO. 3 - 16A* STRIKE Due South

! ANGLE 580:. DEPTH 300*

STARTED February 1, 1951 FINISHED February 5, 1951

PUN NO. SECTION NO. 1 LAT. 32,420 H ELEVATION 5048*

DEPT' 30 *890 B

U DEPTH{•FNOM -^TJ; 0.0ill.O

iT1111l}

11111

65.3

81.3

92.0

•i.o

D1.5

52.0

11

TO

11

65

ei;

92

171

191,

262,

300

0

3

3

0

0

0

0

DESCRIPTION

basing.

A.old Tuffs, Gray-green, dacitlc, fine tonediuro-fine grained, -well banded at 55-600to core; in places tending to be smerAiatfragmental. Rare iron-oxide slips. After 53fairly well sheared with minor folding andfair development of sericite. Scattered grajquartz (introduced).

Orano''1 i critic Intrusive. Medium greenish-S**ay, speckled with white-coloured pheno-crysts (feldspar, altered to carbonate).Contacts very distinct and sharp at 45O.

Interbandod Acid Tuffs and Granodiorite*

icld Tuffs. Few scattered rusty slips at •15-75 to core. At 114-134 very hard and'lassive-like. After 134 locally fractured'j.s evidenced by tiny criss-cross quarts-carbonate veinlets.

Jranodioritic Intrusive, *0ontaotn at 36 .

icid 'Tuffs, Bandinj at 40-450 . Few scattsrcpyrite flebks. At 203-204 i^ranodiorito.

Sericitic Tuffs. Similar to preceding butfrequent sericite-chlorite-talc bandsparalleling the banding at SS-oS0 to core.It 297-300 ground core.

End of Role.

x H ole was abandoned due to excessiveflattening.

7) IP ?SST3:

Depth Et^ched^ C or r eQ ted.Collar - - 5B0 (Bninton on rods)100' 59 i-0 5C 0200' 550 -17,,,-0300' 54 c 46a-0

i

ANALYSISNO.

L

re. •i O, •- f. MM.

'

AS.

'

1

ION. UOiB

.1


HOLE NO. STRIKE

DEPTH

j ~ Due 650 785*

16 South STARTED

FINISHEDFebruary 5, February 14,

1951 1951

PLAN no. SECTION No. iLAT. 32;, 4 20 SELEVATION 5048*

DEPT. 30,890

l

F(lM

j|

1I

1l

1i;iiiriii

DEPTHFROM

0,0

10.0

7.5

2.5

0.0

)9.0

)9.5

J2.0

)0.0

i6.0

i7.0

7L.5

36.0

TO

10,

77,

92.

100.

109.

199.

222

290

366

367

372

390

397

0

)

J

0

0

5

0

0

0

0

5

0

0

DESCRIPTION

Casins*

Acid Tuffs* Gray-green, daoitio, medium-fine grained, well banded at 40-45oto coreLocal minor folding; rare pyrite flecks. After 30* banding at 32-38 .

Granodioritio Intrusive. Porphyritic andsomewhat schistose at 38-400 to core.Contacts sharp at 400.

Acid Tuffs. Banding at 45-500.

Granodioritio Intrusive. At 108 tuff inclus

Acid Tuffs. At 125-139 fairly well fraoturAlter 170 becoming lighter sray in colourduo to sericitization.

Granodioritio Intusive. Faint schistosityat 35—100 . Carbonatized throughout.

Acid to Intermediate Tu.ffs. Banding at 40?Few scattered pyrite flecks throughout.

Sericitic Tuffs, oinilar to preceding butfrequent bunds of sericite-talc-carbonatealteration, paralleling the banding of theformation at 35-3G0 to core. Becoming verystrongly serioiti7.ed, and sheared, to endof section.

Banded Oherty Quartz. Gray-blue, banded at 36-40 to core. Few pyrite bands, (IronFormation) ,

Acid to Intermediate Agglomerate, Light tomedium Cray with highly abundant light^ray-white felsitic fragments elonjatedalont; the schistosity at 30-353 to core.Fo\v pyrite bauds at 367-36C. At 372-372,5;ray-bluo cherty ^uc.rta v/ith T'.inor pyrite.

Sericitic Tuf fs.Bondius at 30-350 .

Lnrjely gray-blue Cherty -Quartz, Soatteredocrite and intercalatod sericitic tuffs•i.i:l ^ ' ' le- '-';r-tc.

ANALYSIS

MO,

on.

d.

ri. •i O*

t* . , ' ' i

•- f. M K, A*. ION. LO**

.1 1 .li

^H

i H

i ^

SHEET NO. 2

1 Vki•Sirt5

11J[j?

1

1

i7.

1

1

1

1

1

1

l —— r DEPTH

raoM'

J7.0' ' -1 .

)3.0

-.

)0.0

3.5.

7.5

8.0

,

1.0

i5.5

TO

401.

403.

500.

1

513.

517..

718.

741.

755.

765.

t

I^VJ ~

5

l

5

5

i

i

i

)

i i

- -

DESCRIPTION

Agglomerate. Kedixm gray, dacitic.

Banded Cherty Qiarta anl Pyrite.

Sericitic Tuffs. Scattered agjlccieratft atbeginning of section. After 409 dar'ier'gray and more chloritic. Banding at 30otocore. At 459-460 brecciated with quartz.At 496.5-500.0 heavily altered with oonsid^serpentine development. Shearing at 35-40

Granodioritlo Intrusive. Contacts et 35otocore. Heavily carbonatized, . -

Acid Tuffs. Light' gray, rhyolitio, bandfcdat 35-400 .'

' ' ' * iGraaodioritio Intrusj.ve. Medium gray withbluish green cast, porphyritic. Heavilycarbonatized with scattered serpentine—chlorite areas. At 523-524 brecciated withijuartz. After 531 becoming darker grayand very dioritic, with local feldspathic

Acid Agglomerate. Medium to darker grayscnewhat mottled with light gray felsitic :Fer? scattered areas of cream-white carbona'Minor pyrite flefeks and few veinlets. A\

722.0-730.5 modiuta fine grained and verydioritioj resembling preceding intrusive.

Ottrelitio Schist. Light buff-gray with scattered crystals of ottrelite throughout,

Rhyolitlo Schist. Light gray, very hard andraassivej'inor sericSte-carboaate alteratlor

Snd of Hole.

DIP TESTS:Depth Etched Cj.orreQje4Collar — G50 (On rods)200' 650 58'-0400' 62^0 560600 ' 59^ o 52. 0765* 550 47fc-0

ANALYSISNO.

rabl

t ion

ragme*

rm.

mts.

1

•l O* ..

^

ssss^

l

MN.

i

AB.

;

l

r

ION. LOS*


J 17J-og of Diamond Drill Hole No/ 17 at^EVATION W6.7 STRIKE North ANGLE 60O

^SECTION Z ero PUVN "Location: 2 4. 82.4'

UAT.N. of baseline

JOSEPHINE EAST EXTENSION. Claim A.C. 289

DEPTH 1019 STARTED JUaC 17/51

FINISHED June 27/51DEPT.

ANALYSIS

rOOTAO.

o* - 4'4* - 43'

43' - 75'

75' -100'

100* -144'

144 '-145.

H5.2'-22

225 '-250*

250 '-495'

495 '-600'

j i

: DESCRIPTION i '

Casing.

Tuff, -acid, coarse grained, 1 some sections completely alte schist. Contact with next se slickensiding throughout last thin rusty films. Schistosity at 30O to core.

Tuff- acid, fine and medium g begins as dark gray colour, b at end of section. Schlstosi

Tuff- acid, medium grained, f pale yellow gray colour, many and flecks of chocolate brown

Tuff- acid medium to coarse g 1" in diameter - mainly pale sericitization.

Dioritic dyke - medium graine enclosed by light gray felsic some yellow carbonate-, and gre gradational over |".

Tuff- acid, fine grained schi pale to dark gray with minor sections. Most of section co developed v/hite f eld spars.

Tuff- acid, dark gray colour, of chocolate brown material t a speckled appearance.

Tuff- gray colour, mostly alt schist. Much brecciation and siderite and pyrite increasin

Siderite - good grade, brown

j

NO.

ght ed t tion foot

aine com! ty 30

agme pate carb

'aine jray

1 whi mate m f u

;tose fello itain

many iroug

jred c erne

; to;ray

rt.

ello ser

poss of c

secg Pa to

ts J es s Dna t e

, f r olou

e f e rial hite

, var 7ish j sma

smallOUt

to a itati ;ider

:olou

a

col cite ble re,

.e gr ore.

in ring

gmen , mi

d sp- con- CO

''ing ;eric LI pa

L ''f le )rodu

:alcy ?n w: Lte c

*, mi

i

UT,

ault ith

y

lame rs

s up or

irs tains itact

from Ltic rtlal

:ks ;ing

th )ntac

lof

ter,

to

i

iy

.

' 'ALGOMA ORE PROPERTIES, LIMITED

Diamond Drill Hole No. J 17 at JOSEPHINE EAST EXTENSION(CONTINUED) ANALYSIS

,V'-''- rOOTAOB .

600* -625*

625* -632*

632* -662*

662* -685*

685* -855*

855 '-950*

950'-974*

974 '-995*

995 '-1000

1000 '-101

i

) t

DESCRIPTION

siliceous material, 5 to 1Q# pyrrhotite. South contact gr section. North contact conta stringer zone with many small fault.

Tuff - As section 250'* - 495* cemented with (50#) siderite.

Siderite - Pale brown colour,

Tuff - Brecciated - 50# sider 250* - 495*.

Siderite - As 625* - 632*.

Tuff - brecciated - 50# sider section 250* - 495*.

Siderite - brown gray colour stringers \ n to 3" wide - 3 t section 915.5* - 916* - diori green fuchite.

Siderite - brown gray colour, material - 20 to 30^ massive

Dioritic dyke - light gray co! 5/6 small white carbonate strii some green fuchite.

Siderite -.as section 950 *-97^

Silica - granular - 50^ narro; pyritic siderite.

Bottom of hole - '.

DIP TESTS - C(

100' 20C 1 -300' 400 * 500' 600' 700' 800' 900'

1000'

i

NO.

ayrit idatl Lns 3 seri

- br

sill

Lte -

Lte f

Oft -t

;ic d

mino )yrlt

.our, igers

,* - ;' bane

.019*

5RREC

600 60o

ra

5 and Dnal11 qua 3itic

jccia

;eous

as s

.llin

illky )yrit ^ke c

- sil t.

medJ- COl

.5' '

s of

'ED AJ

10' [)0'

580QOt 580d)0'58000' 57000'

550|0'i

9

vith i rtz slip:

ted a

-

ictio

; - a

quarJ —

mtaii

.ceou:

im grc itact,

ore r

sili(

IGLE

i!

i

-

)revi

3. I

id

x

i

ling

i

ined ; con

lissi

eous

us

ssil

;aln

Lg.

e

ALGO,ALGOMA ORE PROPERTIES, LIMITEDDrill Hole No. J 17at JOSEPHINE EAST EXTENSION , , '' ' . ANALYSIS

^rooTAo. ;: -*^-~ v." *' ;.- i - " ~ -' ^ i- j ?. -* ^ v. . - ' ' . * . '

DESCRIPTION

TRO - PARI COMPASS TESTS

FOOTAGE - i COR3

200* - N406* " - N:395 ' - N: 600* - N800* - N:

SAMPLES

SMAPLE NO'S.

62001-62051 - 45 62084 - 7" 62052-62083 - ' ' 7^ 62085-62098 - 9C 62099 - 91 62100-62103 - 9S62104 - ic

Hole Size - Ex.

Logged by - W. A. J.

NO.

ECTE!

2^30 1000 1000 9030 3000

F0(

0-735 5-74C

0-97C 0-97^ 5-10] 15-1C

t

ii

rx

BEAI

E WW E E

TAGE

~:5 - i 19- i

.

ING

Ft. ttn

.1Rn

|'

Samp! nn n n n n

es

-: ''-t

-

; t . ; ALGOMA ORE PROPERTIES, LIMITED

Log of Diamond Drill Hole No. J 13 at JOSEPHINE EAST EXTENSIONrt Claim A.C.289 , nfk 5Q7 - n

ELEVATION 1401.1 STRIKE North ANGLE 60 DEPTH 842* STARTED U™ **f?t

'•- FINISHED July 7/51SECTION One PLAN - LAT. DEPT.

Location; 4 .f IQ.yi u. of baseline - ANALYSIS

; r

COOTAOK

0' — 9'

9 1 -149*

149 '-333'

333 '-346'

346 '-376'

37 6 '-3 83'

383 '-391'

391 '-450'

450 '-459'

459 '-689'

689 '-713'

i

. -.

: DESCRIPTION !^

JCasing.

Tuff - gray colour with 50# c a very light gray talcy schis sideritic material in last 3C

Tuff - brecciated fine graine cemented with 30/5 sil. siderJ from 1/16" to one foot in dia intense throughout excepting 275' which is sideritic but d 45 to core. . . -

Silica - Brecciated and recera siderite Section 335' -337' - Massive inclusions of silica and sil.

Pyrite - (60#) - Massive but brecciated siderite and 30# b bands of silica and some seco

Talc schist - light gray colo brecciated and recemented wit

Brecciated silica (50/6) recem

Pyrite (70^) - some massive s cementing brecciated siderite silica (10#) .

Siderite - 25/S patches and st some brecciated silica.

Silica - brecciated and cemen (25#) - brecciation less into

Dioritic dyke - medium to coa |n of contacts. Light colour minerals in well rounded grai brown fine mafic mineral. Ma porphyritic texture.

NO.

f sec t. Ei of

i* grte. meter a sec ispla

ented

pyri side

Ln pi md * id .-y

ir - a sid

*nted

jctio

'inge

;ed b ise a

•se g ?d f e is en 'ics

i

r*.

ion me 1 ectJI

y cc Brecc and ion

ys ba

(50^

e wi ite.

ces of si quar

Last jrite

with

is bu ant

•s of

' sil ; cen

•aine .d sp :lose )ccas

m

bleac andec on.

.our,

.a Ti

.s ec from tiding

by

th f e

receir deritt2 St

and

sil.

t mos brec

pyri

sid tre o

l to ithic 1 in lonal

-

led 1

talc ages aallj 265 ' at

sil.

w sma

ntin

ringe

chlor

side

tly liate

;e an

jriteT sec

/ithi

lark Ly sh

3

y, re

to

11

PUrs.

.te.

-ite.

1

l

;ion.

i

)V/

-

•B

'

, l ^ v P^ "ALGOMA ORE PROPERTIES, LIMITEDJofJDiamond Drill Hole No. J 18 at JOSEPHINE EAST EXTENSION

: - v ; ! - ; ; - (CONTINUED) ANALYSIS

'.':'. .'-." "W,

^ro^o.'v-:;ji-; •'•ft* -.'i.. - ..- .•^.. *f'-t;";:; ". V.' ;. : '''"-

T^t-749,

749 ' -772.

772. 5 '-77

774 '-779.

779. 5 '-84

5'

PJ'

ji

v" DESCRIPTION

- .- .' -' ". V ' -' - - ~. ' - ' . ' ' ' ' ' '

Banded siderite (60#) and sil pyrrhotite and few bands of m Minor brecciation.

picritic dyke - as section 68 grained throughout. Contacts chilled edges for 6" to 8".

Silica - with 20# bands of ma

Dioritic dyke - as section 74 chilled edges.

Banded silica 80# with 20# baj magnetite and pyrrhotite. Minor brecciation.

Bottom of hole - 84 Hole Size - Ex

DIP TESTS / COR

100'- 55030' - 500 200 '-536 00' - 600 300'- 52000' - - 700 400'- 50000' - 800

SAMPLES

#62105-62135 - - 325

in consecutive 5' samples.

Logged by: W. A. J.

NO.

Lea (3 agnet

)i -have

jneti

^-77

ids o.

) t

IECTE

'-l- 4- 4

' to

i

ra

.te*

fine

be.i.5 1

- sil

'

l))000'

J030 f) ^ f

480

i

m -

Lth 1

- but grai

t

- but

sid

i

X

fine led

no

irite

-


jLog of Diamond Drill Hole No. J iq at JOSEPHINE EAST EXTENSION- . Claim A. C. 289

E^EVAYION H28.0 STRIKE North ANGUS 6QO

-SECTION PLAN LAT.t:;Location: 3 -J- 83-3' N. of baseline.

DEPTH 614*

DEPT.

STARTED .

FINISHED July 15/51

ANALYSIS

rOOTACX

Ot - 31

3* -135*

135 ' -224 '

224 '-405*

405 '-426 t

42 6 '-470*

470 '-482'

482 '-490'

490 '-526'

526'-591'

591 '-614'

DESCRIPTION :-

Casing.

Tuff - acid, fine grained, pa colour - somewhat sericitic, scattered coarse fragmentals.

Tuff - acid, medium grained, contains few small quartz "ey fine grained with banded appe

Tuff - Brecciated, fine grain* recemented with 30^ siliceous 5# pyrite.

Siderite - siliceous, pale ye'. 15# tuff remnants.

Siderite - medium grade with : tuff and silica, minor pyrite,

Pyrite (50;?) and siderite (50}

Pyrite (50#) siliceous sideril bands of black slatey material

Black slatey material with 25? Few brecciated zones.

Brecciated silica - recemented pyrite.

Brecciated silica - recemented (20^) and pyrite (5?5) .

Bottom of Hole - 614'

NO. me

.e } 'lowCo. ru ns

*

)cle

iranc

d, g: side

low-

ew si

;)e (3(

bant

Vfitl

wit}"

;ray Beco

j in

•ay c •ite

)rown

all

#) ai

s of

(50?

sil.

m

- gra

jolou oes v Last

)lour md

coloi

jatch(

id 20;

sili(

) vug

side

i

———— .

f

.**x*yi* oftal

ir wi

s of

d *

gy

rite

-

coret

-y,

;h

^g^bfsDiamcmdtDriU Hole Noi J 19: at JOSEPHINE EAST EXTENSION. ' " ^fQ^^^^^^;V^^:^^: :: : ;.V;----;: :' ; ,^ "' . ""v COONTINTOD* J& ; - v ; "••- '.'. - ". •^.• : --' '. ; :..' ANALYSIS ' ' ^'^

^mw*w^J.v

i' '- - : ' .'' -"-' " ,'.- f'f;-. ; ; -. .' ; f -. -' - , :

••f;'."'" -

f

i i

^

*i :-fy.^?'"';'*: • •' i :-'-': DESCRIPTION'^'^ ,.'\. .- -'.v:S,'V^V^... ./...:;.'V,:,?: :":- ,\.V v . \.' P ..' '' . ' -

PIP TESTS : -

100' - 60000' 200' - 55O30'300' - 53000' t ' 400' - 51000' 500' — 4SO00' . - 600' - 48O00*

SAMPLES

"62136 - 62153 - 400' to

in consecutive. 5 Ft. s

Hole Sise - Ex

Logged by - W.A.J. ' '

*

NO.

COR

-

490'imple

rt

RECTE

* i *

'

*

D

"

*


of Diamond Drill Hole No. j 20 at JOSEPHINE EAST EXTENSION"' " ' O ClalD1 A- C * 2|?ARTEDELEVATION 1419*0 STRIKE North ANGLE 60 DEPTH

.; SECTION.'-'-

v Location:PLAN LAT. DEPT.

3 4. 56.3* H of base line.

July 16/51 FIN.SHSD July 20^

ANALYSIS

rooTAOx

0' - 10*

10* - 35*

35 f -182*

182* -192*

192 '-256*

256 '-336.

336. 5 '-34

346. 5 '-51

515 '-W

547 '-560*

560'-566*

566'-590'

590 '-612*

5*

j. 5

5'

: DESCRIPTION t-

Casing. *

Tuff - coarse Gr. grayish-greacid, pale colour 1/8" to 1"a green chloritic ground mass

Tuff - coarse Gr., pale grayfragmental J" "but up to 1" disericitic.

Acid schist - very fine gr.,appearance at 50O to core.

Tuff - medium grain, Interbedand dark gray intermediate.stringers.

Tuff - Brecciated, fine gr.,recemented with 20# siliceous

' Siderite - yellowish brown coFew inclusions of talcy tuff.

Tuff - Brecciated - as sectioSection 377 '-394* not breccia'Last 10' contains 75/c siliceoi

Siliceous siderite - containstuff. Minor pyrite.

Banded black slatey materialand 20# sil. siderite and pyr

Siliceous siderite, yellowishmany silica fragments.

Pyrite (60#), sil. siderite (brecciated silica.

Silica, brecciated (70/5) rece siderite and pyrite.

Hole Siae - Ex.Bottom of Hole - 612'

Logged by: - V/.A.J

NO.

sn coilame*

jolouamete

pale

led p?ew q

larkside

Lour,

i 256;ed.is si

much

:60#)te.

brow]

'0^)

lente

FK

Lour.ter.

r, acp. SI

jray

ale gnartz

gray,*ite

5^ P

f -336

ierit

fine

sili

i col

md (

l wit

m

FraEnclo

Id.Ightl

20lOU

[•ay a-carb

talcand p

rrite

5*.

j.

talc

:a (2

)ur -

o^)

i sil

jmentsed 1

Iverar

r - TD

2 id*

y./rite

i

r

)^)

cont

ceou

rilsi

^e

anded

*

i ins.

W^^^KK^-^' 0^ '. C&E p^bPERtiEs, LIMITED; . : , -fof|t)I^oxid^][3rm Hole No. J 20 at JOSEPHINE EAST EXTENSION.^^v;^^^-,^;,^^;^.^^-;; ;: , , * . . (CONTOTOKD) '. - a ISA&T EXTENg^SJ8

HiHOTS*IRw

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•p", ' ; J//.''- '"r"-'-. : V DESCRIPTION ' ; : '

PIP TESTS - .1 : -' " ' i.. ' . ' - ' ' - : ; " ' ' '

100*200* .300* - ' ~

\ 400*' 500* .

600*. .

SAMPLES

#62154 - '336.5* -346.5*62155 - 62163 - 500* -545*62164 - 62171 - 560*-600*

-

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NO.

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J03EPHISB SIEERXTJS l OSE RESSK7B3 1950

Section Tonnage /S ?e Length

430500500500

1^30

ft. 2,388ft. 1,523ft. 461ft. 655

ft. 5,027

GRABS}

,700.000,000,000

,700

1i

38.2334.8736.6234.09

\ ?e m

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TCfflTVlgO 5b3l05 X foffft

91,32053,10716,88122,328

183,637

36JS3 10.6312.66

,001,010,820.950

,781

10.019.57

12.7813.82

TCHBAOXi

tonnage

23,910,88714,575,1105,891,5809,052,100

53,429,677

5,027,700 per 1^30

rf Q Tonnage

11.769.85

20.3217.07

ton* Lineal

28,09115,0019,367

11,180

63,641

Feet.

.112,550,520,850

,032

1

^otifi llAutal

on Section Length

430 ft.500 ft. 500 ft. 500 ft.

s 1,930 ft.

Tonnage

2,034,700 1,190,000

262,000 256,250

3,742,950

jj Po

39.75 35.96 38.07 38.81

Tonnage x Jo Pe

80,879,325 42,792,400 9,974,340 9,945,063

143,591,128

fr6 8

•8 8

102

.64

.23

.05

.76

Tonnage

13.510, 9,793, 2,109, 2,244,

27,657,

408 700 100 750

958

*3

12. 10. 17, 23.

29 99 0241

Tonnage

25,005,463 13,078,100 4,459,240 5,998,812

48,542,615

l

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GRADEj Fe - 38.36- 7.39. 12.97

TOMAOKi 3,742,950 tomper 1,930 Lineal ?eet

;v: c^; .;-W

3 ( 31.880 E )

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3.62 16.C9

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J-10 14,5*J-U 4G.OJ-12 4,5Totals 67,0*

3C-C.64 17G.0.55 117.36

2203.75

293.43 543,00 09,02

926.25

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1046,52 j 16,29 )

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ir.rc.43 3.-0.20

655,000

J 936.45 J

256,2?0

30,0 Pt. 28.0 Pt.

3.0 Pt.

- 34.09- 13.02- 17.07

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•* Jootag* Width ^fc Jt.xj{Fi200.5-215.0 U.5* 26.26 580.64

594.6-442.0 48.0' 57.20 1785.55402.0-442.0 40.0* 38.81 1552.45

682.5-687.0 4.5* 26.08 117.5ft'

Orado Determination*!(1) .Pol*. W^d.ta F.U.^t

J-10 14.5* 380.84 J-ll 48.0 1786.55J-12 4.5 117.36Total* 67.0' 2283.75

TONN10S PER 500

^ 2)J-11 40.0* 1552.43

TQNHAOB PER 500

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20.24 295.45 5.54 80.50 12.0 71.

11,51 545.00 21.81 1044.62 30.0 ft.8.76 350

19.96 89

yt.xjbio?293.43 543.0089.82

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350.20

LINSAJ, PEET

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97.7' 28.0

JSUP,158.7

09.5' 2G.O 39.0

146.5

3426.62 . 1121,32

109.4*47.5642,41

3176.69 1121.32 J.69.555267,56

TONNAGE PER97.7' 23.0 29^0

149.7

mi. F, 23.0

...29^01 Al r:

3426,62 935.32

.969.. -355331,49

3175.69 935.32

-2.Q9.fc55

005,58 217, 3-i

-J*22iH21356.45

704,01 217.34

-^02x9-2•1206.08

500 LINEAL005,56 140.74

-3fi2*23.1230.25

704.01 140.74

-Sfia*22 .

065,36 611.34

070*551647,22

043.59 .611.34

.155,36^1610.29FEET r.065,36402.14 1 r^fj gc

1502.06

043.59 4S2.14

JL55.36

) ) ffo s 35,54

J

) ) ,i'e s 35,96

)1,482,000

) * ,*?H m 35,61

)

J J ..i'e a 35,91

9.57 ;4S w 9.8

0.55 ,^ a 10.

s 0 .23 ,.ij ~ 10,9*

o~ e.22

1189.40 1401,09 j^s 7.90 .^5 ~ ic.47

I.

*',:;'-*.-' : ' , ' .'

V. * ; -' '^j*''.' " '." . '

x, r

1)992

v !s*o V'J.^r **~~"V~'

-'.- '.*

.-"y".

/j 3

. ,.-'..•-.-• r .-l '

LOOKING WEST

MICHIPICOTEN IRON MINES LTDJOSEPHINE PROPERTY

SECTION NO.5 - 32.867E SHOWING

ORE OUTLINED BY D.D. H! S J-l, J-2 8 J-3

SCALE l" * 100'OCTOBER. 1950

1,190,000BROKENa FULL LINE1,523,000

;tora ri'V;V •'.••". ft-/.-:-- .v./ - '^,-- ,:fei^^-ft^L-i?.--- av,v ;;--^^H-^

^/? : ' ;r; ' •;-: .'kf^'''1^-

i

HRC

/*1kIIr4-!*

2677

2670

JS679

26BO

2681

2C82

26B3

2004

26H5

26U6

fc687

2f.BB

26ftV

S; 690

26yifc69S

kGv3

SiOt'4

2695

Lcyo2GV7

26yo

Hole J-4 complete (COPY)

'

-

3 FaLI. b '6

.^7. 10

36.30

37, 02

37. 60

36. 40

39. 22

3V. 03

39.82

3tf. 43

40. 74

41. 04

3V. 60

40. i t.

M. 1 7

3V. 23

40. G i

40. t.4

40. 64

17. 10

27, 36

13. 4h

S30.33

L. 7B

2. 58

3.54

2.95

3,24

4.75*, R.**U DA*

2. 6f*

t. 62

3. 9S/

12.40

12.51

7. i5

k. 6ti

3.14

i.. UB

1.33

16. y?0. b b

0. 8P.

0.7k

&10?28.54

8.82

3.86

3.86

2.56

3.90

4.56

3.86

4.96

5.10

3.50

2.96

6.00 '

5.10

7.84

7.02

6.72

4.62

4.94

55.72

27.08

GC. 36

Hw— •••^MMd

P

Ch ens l st

COPYSECTION 3 Results of

.'j " p

iA

1

1

I

l

l

l

l

li

l

J 2096 J 2097 J 2898 J 2699

ifS5

1 i

17.24 23.17 22.; 19.96 27.( 20.06 20. i

6 '61 35.20 26.87 19.74 24.87 21.50 26.38 27.68

.S

sj 39172917

SsS

I

j in f'" J-07

* -.ft

l"S49ao20.66 *

H"-50

1 J - 11

1i

J 2924J 2925J 2926J 2927J 2926 J 2929 J 2930

5.2128.7929.4936.9040.92 40.72 38.22

l' 1-'. DO

65.0021.9026.306.064.92 6.49 9.54

u.2f

0.1612.0314.76 10.1029.17 29.63 28. 7 f)

J -93B J 2936

41.12 5.06 20.l?30.32 10.54 23.063H.90 J r..14 1 9 . 7124.17 40.40 f. i.

J 2939

S

•s*J 2948

5.61 41 9f) 2l . 6J -JJ-JJ

is 15 '0 .03

S

-S IS -S21.66 ayes I' J?i- re *'* 05 4.. 16

J 2952 n S J* 07

Note:

I will fool around a bit with

Got. 24/50 19

B

[|t1riiri-Krk

Sample ^ No.

2501

0902

2503

2504

2505

2506

2507

2503

2509

2510

2511

2512

2513

2514

2515

2516

2517

2618

2519 .-

2520

252*

2528 v

2523

2524

^2525

- i. '

^

, *

•k w -*.

\

•J Cu, Insol.

l

* ye10. y e17.60

16.99

32.29

29.32

32.14

33.10

33.30

32.94

34. 1C

33. BC

31*94

32*08

32. 7t

34. 6(

33, 20

36.9

36.8

37.9

41,5

40. 4^

40.41

40. 0.

56. S

16.7

**

0.25

0.30

0.50

0.62

3,82

3.05

4.02

2.18

fi, 57

1* 58

2.72

2,41

4,61

4.92

4.00

3.46

16.7

17,62

18.4k

17.65

16. 16

19.67

20.57

19.34

4.54

*31O2

47.48

36.60

38.58

7.96

15.06

9.28

7.62

5.92

C. 12

6.94

6.70

a. 8411.66

9.96

7.70

C. 88

S 6.42

10.2

10.1

4.90

b. 74

4.84

5. 58

13.4

63.2

l

•i ' tire j c

Pot. Sl/OQ 19

PEP

fiHiiiiiiiti

Sample No.

2326

8327

2520

2529t

2530

2531

2532

2533

2534

2535

2536

2537

2538

2539

2540

2541

2542

2543

2544

2545

2546

2547

254B

2549

2550

2551

'55i-

2fcb3

-

i*"*

k

2 Ni.

• '

-

Z Cu,

i

Insol. * Ta

14.3*

IP op

ie. 90JSXJLL

-21*JUQ

19.90

l^&OIB. 70

3ft, 60

15*90

20,70

20.50

ki7. 39

24.94

25.94

27. 70

25.95

23. 74

17,90

16.50

23.92

22. 02

21*32

19.11

25. 75

22. 50

20. 62

17. 00

* 8

0.75

0.67

0.29

0.62

0.43

0.24

0.60

0.72

1.46

0.49

0.61

0.68

1.63

34 71

3a,GI.

10.86

8.90

10.66

3.69

4. 18

10. 14

1SjJSf&viJi2.35

3. 16

2. 48

1.77

2.68

"*———— -"————— -W MB,

j&aifl.—————— -Tg

37.32

33.72

S&&26,96

29.^0

31.30

30.08

35.36

31.72

32.86

27.80

29.68

16.80

20.92

19.68

17.64

21.28

24.06

30.56

29.28

25.00

26.64

33. 14

30,04

19.30

22.76

24.80

56. 28

J—\ZJ,

;

.

a PT. 13/&0 19

li

i

;

m-. p-i*1|-

i-14-1J

4^1t1-1ri-thi

Sample No.

26u9

2610

2611

261226 ia2614

2615

2616

2617

2618

2019

2620

2621

2622

S 623

2624

S,6i-5

i.'CJ;6

2 W 7

2fi28

fc629

2630

iS33

^63^

* . n. t **^ Oo t'

^C-54

1635

L G 7. 6

LG37

- i - r-

-

t Ni.

• '

- -

'l Cut Insol. 5^ X*

20.G

1:0,72

20.72

16*11

19.71

io, 7ti04 46

21.72

15.29

21.62

25.14

23. 42

23,21

2i, 60

20.72

23.32

26. b5

27. 06

2G. 15

i 5, 43

1&. 10

14. 60

20. V3

1 6. 1 3

13. 82

13. 48

V. tf6

1J. VU

6, 43

C). o ;\

4 B

6. 60

6.10

4.56

2.41

4.32

3. M

6.45

4. 15

1.14

3.66

5.35

4.23

3. 23

4. 69

3. Jo6

3.31

2.50

3.67

2. 70

7. fil

3. 72

3. y 6

7, 06

2. 05

0. 77

0. fj

0. '.b

0, 63

0. 41:

C . - h

*SiOfS3.10 yjfcsJb

29.76

31.70

3R06

35. 16

34. e;.•L 6. 6 i.

c7. 0^

36. Ci:

26. 76

21. 12

24. 64

i-4. If

26. 00

i.?, a24. k;6

IV. OG;

17. 34

' 0 , oO

i:V. 04

41. 34

40. 5L

31. 41-

33. 1C

3v, OL

40. IJL

46. i A

43. ot

54. W

b... if

q"1nHn

lv?

Iii

f&anpie^**tf r Vft- -.".••''"'• v ''^f-^0 * :.-''"-^••^fv-;ik : 2699V -

^fejfev?-. #700 tfv-.#V^::yV^:; ' 2701' i-'i5^-'-, ••:V'; -'V.-;-'27oai:'^" ; '-•V^V' i. :

2703. f - "' * '

2704-.V :,\ -'i '

2705

S706

2707

2708

2709

2710

2711

2712

12713

2714

2715

L-Z^ —— '• •/7*7 l 7• H ' "*

M27 -18l lOO 1 Qf |c f J .

jfc.720

•J2723

1^722

• •279^ UE!2 ————IJ2724

11 r925^imo

W1727-

ll&V.::

V-fl-ft'-',,;.' ', •••- ~../ . ' - ' .itftt-^: : - '-"V "'- v . . - - - :

'^•^•: ' : ; . ' .

V.-VV-.;: - ' . . ' '. . - -

^

t, Ni.

.

•~

•J5 Cu, Insol. Jf Fo[7, 86 Ifid^

97, ftfl

JLaJiS.Ifi fl!S

9:5, 6716. 45^0, 5-.Q

20.26

20. 66

fc3. 46

21. 27

fcfc. 66

Ifi-JBii.

29. W

19. 06

11. 83

IR. 76

10. 65

2 B. 69

36. 83

38. 31

40. 22

39. 9 ?.

3P t 00

•;.h, i ?

V',. C, 7

U..07.

4flt ."S 4

*4..,20

v'. yi

^ Bp

l t 7B

O 1-!)

0. 48

1 5 fi

0 43

3. PIi

1 1 t'-'

3. O 4

fcr 38

8. 13

3. R4

4. 6i)

3. 93

S* 7.7.

4.30

3, 76

0. 69

0. 53

i . SI

3. Ut

b. ?b0. 33

.?.. 3. e.33. 60

3. HO

4. /if,

11, 76

if). 7

3 3, H

U. 4

2 810— '

37 #54

19. 8. H

33.96

•^S, 1 n

IR. OS-

J;R. 7fi

JL6^JL6.

29,02

31.20

16.24

33.96

25. 12

25. 64

fc3. 54

27, 84

42. 68

30. 46

31. 78

18. 44

10.62

8.20

4, 88

5.26

9. ifc

3V. 36

45.98

65. 68

8.84

i:3. 4

33. C

.1.1*.-!^^ M,l.^

n

i

1

i

i

~!

l

1

-

HOV. L ^f.r* tt A f ."nl1 iSf

KLM- HkP^l

H ' k

IIri-ii-i-ii-i-ii-li; 2

fSaaple^-MO^-V,,'.i"-, j :- -v-i-iS'639 ""''-^

'2640 V: :::: 'i^ji-: ..y. -V... . ' ;8'6"41^^'SV-f: . '- i . .

2642

2643

2644

2645

2646

2647

2648

2649

2650

2651

26 5 2

2653

2654

2655

1J656

2657

id65R

2659

2660

266]

2662

2663

26C4

2665

i656

26A7

-1*6 '

' '^ '".V ' ' '•.•' ' , ^ : ' ' - '"'•'••"' ' . '

' - . '...., ' ' - .

#Ni.

:

•B

i

•^Cu,

\

Insol. ^Pe

8. 54

P, 7O

20.1!

ftS, P,

t'.R, fi!

12t 9

10. CK

7.84

8. 45

0.90

12.68

lii. 45

13.39

13. 23

16, 50

1.11

14, 38

13. 83

16.0.

31. 2?

34. OC

31.7

33. 9C

34. 2C

32. 3C

32.50

37. 2C

26. 15

9. 10

1 3. 3i

*s

0.65S* **j

2.36

0..710.48

1.02

0.25

0.34

0.32

0.49

0,37

0.46

1.17 ,

0.25 S

0. 23 {

0.31 e

0.27 t

0.31 t

1.12^

3.79i

6. 7i.-

2.86

6. 020

3.147

4.011

6. 641

13. 1 4

4. fc3^

7. 6?b

14.1?

kVHMMOMMHM-.

f SK

SI *,e

6 ftft

"x fm •* J r ro

^4iOO-

3. cq4 5f)

6. 3 Si

B. 06

9.24

0.60

4*04

15.54

1.08

1. 5ft

fj.30

B, IB

3.74

5. 66

0. 82

L. 40

.06

5. V4

32

OB

U5fi

-.44

56

.. 53'.40

. ?4

^™*^™——™.a

/''f" 1

U-JJUStE)

'*-nV V'^V'''" -' **'~ '*"-'" " - 1

lPkJ"

WIIIyckli11

p-•-li1

'

.f~I

f1 Sample e'lto. , : -

irtff' " li JTj'jr.' ' aii-is

|fe789' - .

1 2790n ' -1"

2791

J2792

.2793

2794

2795

2796

2797

2798

2709

2800

2B01

2802

2 P 03

2804

fcRCfc

&R06

li R 07

knuoi;R09

I:ftlO

2f-ll

J'.Blfc

2B33

k 0 34

i "3 b

l P3 6

: r3?

.

-

1 ,..,.. 1

t Hi.

ti

*Cu. Insol. * y*40. s:

se. vi39.71

A2*JilISB, 11

44.5343. BS

45.33

40. 7 Z

45.12

43. li

44.13

44.53

43.92

41.. 9?

43.38

43.63

4S. 92

4C. 92

21, 36

41,95

42. 5?

45:. 71

41.72

43.33

42, 12

41*. 3V

:-.fl, 09

1 b. ',b

ISO. F?

* B-

)3.74

1.93

3. OS

14..1R

8.63

1:1. 33

3K. 11

feO. ?.t

7t t4

i 4. 3B

1 4. 7 3

8 i. 67

5:6. 35

Jf7. 1.6

26. 30

3P. )P

?.7, 74

i.7. 56

S3. 70

31. Ib

3k. b!i

M. 15

XV. 75

3V1 . r:5

37. is

l -. . H?

t ' . * * * * * *. fc

1 4. t P

7, brs: '-. rv

^sio,'-.d

5. r,^*. r.a7.44

S. t*

7. It

'f. I f^

3. PO

2.90

b. i 4

4. 4U

4. 75:

a. 74^.H6

3.14

7. 36

5.3S

4. 6i

4. 36

6. S6

V:5. t

a. 446. OU

G. Vfi

y. 743.64

A. ?.r.1V-. bL

; c. ?.-v4.".. 6v

t.n t, * **v* *ii " —

- 0*

^

""" .

.

——— kMMMNM.

m

HR

Hffl

luB-^B

30/50

fc*lIpfeEHpiUlilE• 5-:-^i-:,.m-K.fern.P" '

B,--

^i ' '

Df-|l

li—f—i—it—l—

-f Sample ?'^KO.-Cr: :.

fcBie

^820

5:821

fcp&a

LP23

!tP:'.4

2B25

2826

2827

2028

2P29

2K50

2831

2832

2833

2834

2835

2P.36

2P37

2F38

1P39

J P40

'/FM]

J-P'tS:

J- Hi S

i. p ^4I.^'-.fj

i.P4G

: c^.7JK

: . -' -V j --- "' ' - - -

'

*--

*^

*

*

^ Ni.

-'

i

^5Cu. Insol. ^ Pe

32.70

30. 49

33.30

31.69

52.83

14.25

33.04

I;3. f.fi

19.26

23.07

30,09

22. 06

22. F&

23. 47

24. C7

25. 58

11.03

23. 27

26. ey2 P. 49

37.13

LO. 1-6

2. 40

3. CO

3. /-O

37, /.l.

3 . . C

3V. /.b

11. P?

^ sas

31. ST

29.87

32.52

31.11

6. 60

2. 37

3.07

b. 97

3.01

3.75

0.78

0. 48

0. 60

0.73

0. 80

0. i- 7

0.30

1. 30

1. 4C

3, S2

6. 38

3. i i

0. L7

0. 03

0. 34

C. * 1

:. O H3. 37

J. V9

**'" i — .

foio,.

- 26. 4J

30.34

25.64

27. fi^

66. BQ

41. 3.Q42. 28

26. 72

32.30

26.40-— —— *— *™.^.

12.08

28.46

23.36

22.84

21. 48

39.62

65. 46

39.84

23. 86

20. 80

6.06

45.72

63. 7L

64. k8

60. 64

3o. f,C

..o. 4 P

3U. bO

1.4. :.c

•*—wl

SK

^••"B

^•^•1

——— B.

*^-H

mw^

. . A 1 DIAMOND Exploration Started ^u**. xo,/pfosFinished J. Bill 4 Logged By A. Clark Core Size Safety Plate

COREPlan No. JosephineSection No, 2.t-ooaLLat, "7-t-jifc 3Dept,Elevation t z.4.G. Ct/

ACID TESTSDeptho ' :- o '

Read Corr. Depths. i r.

Read Cc

4-a'

DEPTH

J*vCr .— — — —— t1

'v/4

50(

5' ,-

gof —4

50

uo

\N

-" * ' i ' ^"^^t"v" ••" ' 1

CORE LOSS

9*

18*

DESCRIPTION

Casing and, Overburden.

luff.fine grained.•tedium grey colour.Agglcmoritio portions.Sericitic.Evidence of shearing.Felsite at 16*.Numerous narrow Quartz-Calcite veins up to 1*width.Ottrelite.Banding from 20* to 45* to core.

ruff.Ine grained. Sericitic.Medium grey colour with portiona of light grey -buff felsite at 83' fi 91*.Shearing.3ore still contains narrow Quartz-calcite veins.Jigh carbonate content. A few scattered pyritex's. Agglcoeritio portiona* Higher chloritecontent last 5 feet.

j^

SAMPLE NO.

ANALYSISAs S*

t

Fe

r

S Si 02 CaO M?0 A1203 Mn

' — *

f'.

PfSjBOlE MO J/ M

ft 0KPJH

?THQK-

v 110•v.

f.V

12S

tXf

ISO

:" V

MMMM •••B

TO

125

ii

150

175

-

•MM ^^B

OCRS. LOGS

2*

8*

0

mmm ^^^m

•y '-i-:': , ;v;"v ' - : '.. v , " -

•^T'-'-^" ' " ' . DIAMOND DRI

MHH jojr~/.^

DESCRIPTION

Siderite.Buff.Jointed with chlorite filled fracture planoa.Pyrite flocks throughout. Evidence of leachingScow Quartz-caloite bloba and veins to ^.Magnetite portions up to one foot in length.Portirna of broken core throughout box. Nonamenable.

110*115115-125

vSiderite.Buff.Highly jointed with Chlorite and loaf pyrite inthe fracture planes. Some magnetite at end ofbox. Several narrow QuartB-Caloite veins toi*. Scattering of pyrite x'a throughout.Non amenable.

Core loas 126 to 130 125-135* 132 to 133 135*145

* * 134 to 135 145-.15S

Siderite. -Buff to grey-blue.Core atill highly Jointed.Portions of core magnetic throughout box due tomagnotrte (dark grey-blue colour). A fewQuartz-calcite veins to jf width.Pyrite and pyrrhotite flecks throughout.Non amenable. -*

155-165165-175

**~s

•iB^HVBlMMHMBVB^B^HB^HMB^RlHHHVHHHHMHHBHIB^HHHHBI^^^^^^^^^^^^v^^^^v^^M^^M^^HiBBB.1 ''""^^^^^^^^^^^^^^^^*"**M|Elir*B^BBI^ —————————————— ------ ^^

m *mm mm ^a mm m* mm wm -cmm amLI CORE REPORT

SHEET NO. 2

SAMPLE NO.

127001.02

V

030405

J

0607

V

MMHmi

ANALYSISAs *fe

.300

.063

t

.095

.171

.028

.042

.052

M^^B^^fn

Fe

31.631.9

15,031.633.0

34.734.8

S

2.723.38

.994.292.44

i

2.684.23

S102 CaO

1

1

6.88 ' 6.098.07] 5.59

i

,

34.609.084.68

4.003.80

4.465.365.36

M?0

,

5.375.38

5.475.22S. IS

A 1203 Mn

t

,

.44

.462.102.17

9.30 1.06.99; 2.07

1.03 j 2.23l

i1 i , 1 1

4.835.17

5.2C5.37

\J

j1

.KB

.34" 11*- t O O

?.24

mmmm

DIAMOND DRILL CORE REPORTHOLS HO. -Gt-i- Jo-j w- SHELT NO. 3

•DEPTH

FROM175

200

225

TO200

225

240

'

CORE LOSS

2

1*

9*

DESCRIPTION

Siderite and Magnetite.Buff to dark grey-blue.Jointed vith chlorite filled fracture planes.75t, of core is magnetite. -A few narrow quartz veins. Core has high car bonate content.Non wnenablo. ~

175-185185-195195-205

Siderite and-Hagnotito.Buff to Blue-grey colour.50^ of core is magnetite.Core still highly jointed with chlorite & leafpyrite in joint planes.Still a few Quartz veins fi blebs.Increase in pyrrhotite in the form of blobs andveins.Massive pyrrhotite at 213*. High carbonatecontent. Hon amenable.

~205-215215-225 ^

Siderite andhMagnotito .Euff to Groy-Blue colour.Fine grained. - -Highly jointed d brecciated. A few quartfc-cal-cito veins.High core loss.?lecks of pyrite and pyrrhotite throughout.lion anenable. ~

225-235235-240

End of Hole 240 i^,:. V

SAMPLE NO.

1270080910

**

t

1112

V.

1314

*^

ANALYSISAsBoc

.151

.069

.190

.300

.310

.153

.064

Fe

32.832.533.1

33.634.0

33.929.5

S

2.723.083.25

5.804.37

4.361.96

S102 CaO M?0

6.39' S. 836.24 6.237.20 6.07i

i

i

.

8.225.95

7.9822.20

1

5.475.24

4.853.68

5.775.665.62

A 1203

.15

.06

.12

i

4.91:5.02

Mn

2. M2.222.24

1

;

1l

.24;

.30l

l

2.UU2. M

l

j

S.02i .264.4H .37

1-j l v. '

L

2 . l -: :l! 97

I^H^^^^^H^^MH

f

r* 7 * 7 '.7*7'.7 t 7

rr * 7r ? * 7

OC *~

Of **7?*

7 T *

C 0 *i T *

AA

?A . f;

70*67A "7

70 * c rso * c

/. y. * ei? ' S

07 ' C,CT . s7 7 o r; y.*,'*0 f * C,

^ C ' C

ff'f,

) Q * f

or * ^

n*.-r,

(JO**,

f 7 ' Q

/.T'?

' * *7

r: -c0 '0

0?'?7

^y 'P96* i

T 'R

p f. 'f

r*?* r

OP'S

BO**:

O* O, PT 0*T*,2 f, * ? T T

fi? "7*6'0p*:*?

o**??: 9*?t:T'CC ?*?Kp '2*; R**7jf

i**7t; "•?.e s** tC'ST fi'K 9* T?

•i -'' mm' HH rnn ' mm mm, mm*

OAT'0 6on*o IST'Oz*;p*o2 bn * n9e^'.TUT*n

OTTt

•TOT

0*0: O:^A: o*5stO'OT 0*581 C*?i.TO'OT 0*5it C*?9T

0 * C t0*01ei c*5?T

Exploration StartedFinished 1968 -Jdt-r Logged By A. Clark Core Size Safety Plate

DIAMOND DRILL CORE REPORTPlan No. Josephine *~

/a Section No. Lat. 6-*-xo Dept. Elevation

^^^^^^ J0g~.—^ -^u^^ll -t ^ ^^^a ^^^^^

B V BOB, -mm

ACID TESTS Depth Read Corr. Depth Road Corr.

i DEPTH

T!- 0

50

gil^y

100

131; v' (

i TO

so

100

131

132

IfeSj'-"

CORE LOSS

5*,

2*

0

\•i'", --

DESCRIPTION

Tuff.Medium grey colour.Sericitic. *Few portions of Felsite.Agglotaeritio portion 41 to 44 feet.Shearing evident 40* to 50* to core.Core badly broken up.

JTuff.Light grey to buff-yellow.Sericitic.Sheared fracture planes 45* to core.Scattering of Ottrelite crystals.Moet of last box agglomeritio. (i.e.) 75 - 100).Increase in felsitic portions* Core not sobroken as previous boxes.Setae carbonate content observed.

Tuff. . VMedina to dark grey colour.Fine grained.Not touch sericite. - :Increase in chlorite last fr*.Good carbonate content*Core has been split 110' 'to 120'^

Massive pyrite.Core has been split 130* to 145*.

-^ \s

SAMPLE NO.

'

ANALYSIS

Fa

t

Fe

1

S Si 02 CaO hfcO A 12CQ Mn

.r

•?! (in'^^^^^^i^f^f^'J'---''''' DIAMOND DRILL CORE REPORT ' " • ^^|?S: MOUB :MO;'-^|rj.yft ,. a.. 68 --- ' SHEET NO. 2

f life" ''DEPTH • ifit'-*ROMj,'--'.-' :, - " ' ';''*-\?~. :'.' '"V.Vr-132-•-..'••.'. : .

1 ' J'A F

4fe^g7

150

TO

150

177

i177

, 183

1&9

V

'V-*',::; ':G'.f. ',

183

189

-

195

CORE LOSS

4

V

1

0

0

0

DESCRIPTION

Siderite.Buff to grey.Highly Jointed vith chlorite filled fractureplanes.Scattered pyrite x's throughout.Some leaf pyrite.Fox narrow Qta-calcite veins ,-Non amenable. ^

Siderite. sBuff to grey colour. .Some magnetite 163 to 167*. 'Considerable pyrite content.Jointing still evident but not ao uaich chloriteas previous box*Non amenable.Cor* split 150 -175. ^Silica Rib. iSiderite with blebo and veins of grey chert andvhite granular silica.Sane pyrite veins. 'About 6* of removable naterial.This section aramable to treatment.-Cor* split 175 - 200.

Siderite.Buff to grey.High pyrite content.Numerous chlorite filled fracture planes.Non amenable.

Foot Wall Zone.Buff siderite.High sulphides.Blobs and some rv TOW veins of silica.Non amenable. ^ ^

SAMPLE NO.

t

^,

ANALYSISAsfee

-

Fe S S102 CaO

i

1

ii

M?0

i

i

A 1203 Mn

t

i

i

i

ii

DIAMOND DRILL CORE REPORT

SHEET NO. 3

fe^rv^ ..DEPTH-.PS'FROM

f^'yf- ^ 195

-

i

®

H *. '- '^^^^ ' '•y*' "' , . ' "I"- ~ ' ' "'

TO

117

*

CORE LOGS

- -

:'.' '' : DESCRIPTION

Iron Ponoation, Grey to Black chert,. Veitui of pyrrhotite. . Some siderite enrichment. A few large veins of -white granular eilioa Core brecoiated throughout. Some chlorite filled jointing lant few foot in box. Cor* split 200* to 217*.

End of hole 217*. '

t

^

SAMPLE NO.

t

^

ANALYSIS

Fa Fe 8 S102 CaO

i

i

i

i

M?0

f

A 1203 Mn

MPLAlTMN 4MAYHIEQMD MB

^r:-,\; O.O.H. NO.t'""- Jc,r* - ^-6s

PROPERTY

LOCATION

SAMPLE NO.

, s.Si ^

•*ff*^fc.

^^54

ISSS*4-

i s ss/ISSS3/55SS

^

FOOTAGE

FROM

/os/rs/io/34/^•o/fcS

/SOy 9^

-

TO

US

/VOJ3&/^•o

/6S/ao/9J-

^/7

LENGTH FEET

/O

S

-Z6—

/5-/5/.Si^

, FeO

•m

Fa

r.

i

.

1

Fe V- Si 02•y

.

Ca 0

"-^'

bij 0' - J --^

DATE

ste,pr. 2.6. /^6..GRIND

DATE

•AL2 03^

: K,i

. -*-

^?

-— -

fWTIO

, ' t A .O.^••Ife^r^;^.^^.' -.jsMfrj^M-i.^r ,i.*tf'-'VV - .lv.--.|8|||!f^'-^ ; -' '

-Jofi.-j.r6A

a Depth ' V79o''

DIAMOND DRILL CORE REPORTStarted •'"•f ac. Plan No, JosephineFinished "68 -*"*-r a-* Section No. e *-coa. x DepthLogged By A . Clark/ Lat, ff-t-s*. l/Core Size XPP Dept.Safety Plate Elevation

ACID TESTS Read Corr. Depth Read Corr,

^. .

DEPTH

FfiCK

0

4

^

25

50

A

1TO

4

25

SO

60

*W^'"'"'

CORE LOSS

1*

.2*

4*

^\

DESCRIPTION

Casing.

Tuff. ,Hodium grey colour.Fine grainod.Sericitic.Sheared 45* to coro.Felsitic froa 7* to 19' and Yellow to Buff Mncolour*Agglomaritic last 6 feet.Hodium grey colour. -Serioitio - Fine grainod. S

Tuff.Hodium grey colour.Fino grainod.AggloxMrritio.Yellow - buff felsite from 38* to 45'. XFino grained, grey tuff frau 45. to .end of box.Sana narrow reins of felsite..

JTuff..Hodium Grey Colour.Fine grainod.Sericitic.High chlorite content.

\^/^

SAMPLE NO.

i

ANALYSISFa

t

Fo

1

S Si 02 CaO MjO A1200 Mn

'

^•P" 1f^am ^* " ^B^Et

ppf'v'HOLE'HO.^'fi'ip'!*' DEPTH—""FROM

-''v : ,r. j . , ; -- . , ~ './.* : - '- 60

,'v, ; ,-. .

65

66

,

100

ISO

-,.

TO

65

66.

100fc

i

ISO

190

'-

CORE LOSS

4

0

4*

V '"

.3'.

. -

. .0

DIAMOND DRILL CORE REPORT UT-*-* J GS-3-&& SHELT NO. 2

DESCRIPnON

Chlorite Dike*Dark Groen.Fine grained.Sericitic,Numerous narrow calcite veinlotts. High coreloos. v ,

Agglomerate.Calcite and pyrite crystals in chlorite natrix.

Iron Formation.Grey granular silica.Groy and bluo chert.Pyrito and pyrrhotite voins and blebs.High staphldoa 76 to 77'. Distorted bandingand blebs.Core brecciated throughout. 'Good siderite enrichment throughout. 'Jointing nootly in the siderite with chloritefilled Joint pianos. y

Iron Formation.Grey to blue chert.Some bands 30* to core.A fow vhite granular quarts voins.Soatterod pyrite and pyrrhotite voins.High poroont of siderite enrichment (about JCft)Core still Jointod vith chlorite in the jointplanes* Most of core brecciated. , -

V

Iron Formation.Grey to bluo chert.SCEO \ddte granular quartz voina.Not tuoh milphid&J.

SAMPLE NO,

1 '

t

\

^

ANALYSIS

Fa

..'

x

Fe S Si02 CaO

t

i

MjO A 1203 Mn

1

i

i

~-

.

mm mmi ^^m mm mm mmDIAMOND DRILL CORE REPORT

-'o* - J - 8 SHEET HO. 3

pfe? DEPTH/

,'

.

m, j

TO

190

i

*

CORE LOSS

0

DESCRIPTION

Cont'd,

Magnetite portiona and voins throughout* Siderite enrichment about 1511. , Moat of core brecciated. Some banding 45* to core. Siderito portions are jointed with chlorite filied fracture pianos.

End of Hole 190*. l/ .i

-,

SAMPLE NO.

, i

t

-

ANALYSIS

Fa Pe S S102 CaO

i

i

.

M*0 A 1203

f

~-

Kn

1

j

1

i

i

i

COP .

B^SS^;'-,;-- -P'^-^jcr y. f a

PROPERTY

LOCATION

W-.----[A,.;-..-- i ''•h-.V-." -

i,'.-; r. -SAMPLE w.

. 'JLff-'t 5

T?I^7M**?..

—— - — -

•o

FOOTAGE

FRCM

5jr.70 ———

TO

±5, 7 5,

LENGTH FEET

J.O

S

DAVIS TUBE MAGNETIC ANALYSES

.FoO^

———— .

Ffi .1

V--

.0 /v4. /O J

-

?e,.^

a. 22^-, 1

——— -

J S-*

.y^g•2, TS"

^ Si 02 j Ca 0 ^

7/, 2^^J. J

^

^-.47j 9^

VQ O/

J2.^d^../.fl

DATE

GRIND

DATE

tAL2/ 03 j . j Mr*

7^.5

1 * - -

• 07

/.r?

^ 02

^,

RATIO

'"'

t

yrgr-yniB1

^^J^Wa*-'v'-.^J ; ' :"- Exploration ^MoI'-OIri-Jos~^.-^A Started ^0AX

^Strikft^360 ."^. -,,, . , ' Finiahed i™ . , /Xngle^l4.j? e V- ' Logged By A. Clark ?DepthVi^;216* ' Cora Size A

r ' v Safety Plate

DIAMOND DRILL CORE REPORT Plan No. JosephineSection No. u-^

Dept. Elevation

s.

ACID TESTSDepth Read Corr. Depth Read Corr.

So' s/* 4.3 1 50 j. /o' 4-j .j"*J. 3 "

H -'

VDBPffi

•V;:p

115

IB

20

27

; --

\ '-

44

63

t ,; : - 1 ';

•••B

feiay—'

15

16

20

27

44

563

74

^.

•••B

CORE LOSS

MMBMBMMMm

4

5

0

.

2*

0

"r"-'

———-——

DESCRIPTION

Casing,

Overburden.

Core Loss.

Tuff.Medium grey-yellov colour.Fine grained.Sericitic.

Siderite.Grey to Buff.Pyrite content high.A few blobs of grey chert.Non amenable.

Footwall Silica.Grey chert with portions of aidorito and pyrito.Soao magnetite.Ground core at 63'.

Magnetite?Dark grey-blue.Fine grained.Highly magnetic*Pyrite veins and blebs throughout.if calcite vei:, at 65'. Sane siderite last 3 or4 feet with some chert ble* ,

i ^

SAMPLE NO.

^——^^^——-^^^^^^B

ANALYSISAs

'

Fe S Si 02 CaO

'

^0 A12CG Mn

V^mm^mmimt''-'mm mm 'mm mm mm mm tt mm mm mm mm mm mm mm'-'mm mmiimwl^^'^^^W^v- : ' : ' ' DIAMOND DRILL CORE REPORT

^MHblEBO.^4- Jd^-4-^fl SHEET NO. 2typrVVs^'' - ' - ' -^ DEPTH

||rBbk

ffiWy,-'**-

; , :

V '

#'74'j*~.'-".~ '-~ ' ,'^•'-'.:.-' :

\v-

iTO

103

l(ffl 121

121 216

!

®

. -

-

*

CORE I/3SS

3

2

4

*-

DESCRIPTION

Iron Formation.Grey to black chert.A few pyrite veins and blebs.Setae magnetite veins.Siliceous siderite enrichment.

Quartz porphyry.Kediun grained.Light grey.Agglomoritio.Epidotisation at 103' and 121*. i

Iron Formation.Grey to black chert.Some veins of xhite granular quartz.Siderite enrichment SIL. A few magnetite veins.Massive magnetite 164 to 165. Occasional pyriteand pyrrhotite veins and blebe.

-

End of Hole 216*.

\./

t L

SAMPLE NO.

-

ANALYSISAS

1

Fe

**

S S102 CaO K?0

l

t

t

'

A 120 3 Mn

i

1

i

—

-^^^.,~^JJ^^ysN 3ND COPY

A.O. -leak:*:--.^:-. ' - -

D.D.N. NO.- , -^ os — -^- — fj) Q

PROPERTY

LOCATION

;, p-LJ"" " ll " I""- IL '

DATE

GRIND

DATE

SAMPLE NO.FOOTAGE

FROM TO

LENOTM FEET ..Si 02 Ca

^AL2 03-f ,, Ki\ — RATIO

2.0 J

15 S3 9GS . /.S 7 23.5/o S •2.0 . 9

1 lo1 1.0 . S

C4-9 l&.l/e o . O.S5 .9

lo i(eS '6 3./.0

11.4.

I.&Q, 59

2-.04-

. a51,. 4-

4-9.0

2.5 . 4-9l.ad

J.1,4.1 4.

3. Jo J4.

I.6&

/.MA

A 5.5

g^^^fe^.-;4 '.vV-'^/'' - '^^^fev^;;'.,i^:.v-'' ; 'ml* ^ JfiM&in. ':--''.V'' -:'''' .ExtJosejhttit

le 'No.---Gir6* Strike - Vao*.Angle '•• ?'^- " :-' -'-•'••*- t '

. ,. -j - DIAMOND DRILL CORE REPORTExploration . .j ACID TESTSStarted /*ue Plan No. Josephine ——————

Finished Section No. i t*rc*xz. Depth Road Corr. Depth Road Corr. Logged By A. Clark ^ Let.Core Size Dept.Safety Plate Elevation

f f i t . '> ^ < . .^ . ^,,. x'

;. DEPTH

SH^fL""'- ~ j ' -

^ ; 15

28

IS

28

29

^25

48

. ; \ .V ^: '

lw

^48

107

. 'j•r i

^

CORE LOSS

8

0

-

0

3*

-V,

DESCRIPTION

Casing. -Tuff.- 'Green-yellow colour.Fine grained.Sericitic.1 -High chlorite content. .Host of core broken up. High core loss'.Agglonoritio portions. i

Iron Fonn&tion.Grey chert with siderite enrichment.Massive pyrite at 29'.This section possibly Hanging Wall Typo, y

Footwall Silica Type.Portions of aiderite with bleba .and distortedbands of grey to blue chert throughout.Bleba and bands of massive pyrite in moat of thiasection.

S/

Iron Formation. 'Bands of Grey aad Blue chott throughout about 45*to cor*.Moat of core brecciated. Bands of nagnetite.black slate and black siderite'.

SAMPLE NO.

Portions of siliceous buff siderite up to one fool!in length. l

M ^

ANALYSISAa 2s

*

Fe

^^

S Si 02 CaO MgO A12Q3 Mn

" —

• O.

m i

B^PiP^^^^-SVv;,:- ,' ••,, v UIAMOND DRILL CORE REPORTIBJmiffi&StJ-W;^*-'"'.'''.' . ' "' . '.' -^BblEHO.^efc-^'yes-^^g ~ SHEET NO, 2

DEPIH^FROH^ TV. 1

S;'*."'".

- ; ;i

v

IIMMBH

11"

]?': ".

iTO

107

.

i ^^^1•* 1

e

mmmmi

COGE LOSS

3*

•••••••••i

; - DESCRIPTION* ' r

Cont'd.

Veinc of pyrite and pyrrhotite.Not much jointing.Core has boon split 80 to 85',

'

End of hole 107*.y?

SAMPLE NO.

'

ANALYSISAaSac

'

1

Fe

^

S Si02 CaO M30

ii

jj

ii

A 1203 Mn

l

ji1

i

1

l

K. f '

ft.;

ftw&^'i l '''. f V; ! ' '' -* •••' . ' ' ": :' ?*'? X1'-'-' '- --''' ' " ' '' ' "

/y DiOiH* NO*m-.-: 'i?-. J ojS— 5"- fog

PROPERTY

LOCATION

'^•''•• ; ' :---

-SAMPLE NO.

'. .

/55^,a

. . — ..-.-.

^

FOOTAGE

FROM

^0

- ———

TO

3s

LENGTH FEET

5-

j FCO

rti^P^J/KJtt- ( — t4i.5T ta-X7fc5.*uJ( flv

Fa j - -

Y

• 0SJ

.

1

ANALYSES

Fe

2.2 .J

Sbfc

J. d 3

————

1~rlrrr^~~ Ca 0

4-^.9

•—'

^ ,J?A

Mj 0— -—j —

J.4/;

DATE

GRIND

DATE

AL2 03":f -~— r

. /f

.: Mn ^

^

A/8

~-

RATIO

.• Josephin*

Hole KorOirfr

^^*y,:Afflt:.-!)..v^^-.,.- ^- ^^m ' mm-~ ' ——— ^^^ . - . ^ . ^^ . C ~} ' •• 1 ''

Exploration 'StartedFinishedLowed By A. ClarkCore SizeSafety Plate

DIAMOND DRILL CORE REPORTPlan No, Josephine Section No, 9^.00 es. Lat, s-*?0 s Dept. Elevation

ACID TESTS

Depth Read Corr. Depth Road Corr. -So 1 ~ 5/ 0

"J DEPTH- "

jffi^

0

3

46

/fo^?S

~-

*

A ;:. "

i TO

3

46

55

LOO

4^K|-;'

coeLOSS

3.5'

3*"

7*

^^^^^•^IM

DESCRIPTION

Casing. "

Iron Formation.Grey to black chert vith bands, of Whitegranular silica.Some Siderite enrichment.A fev narrow pyrito and pyrrhotite veins.Distorted banding and breccia throughout,Core split 25 to 30*.

Quartz porphyry Dike.Medium grey colour.Fine grained.Agglctaoritic.

footwall Silica Type.Portions of Silica, Siderite and Magnetite upto one fx)t in length. Most of core brecciated.Siderite oakes up about 4 Cft of core.Core is Jointed vith chlorite filled fractureplanes. ~Minor pyrite fi pyrrhotite ~ veina throughoutcore. -Pyrite-^rgillite at 58*.

58-68

End of Hole 100*.

f

SAMPLE NO.

,

127016

ANALYSIS i

Fa

.099

Fe

23.3

^\

S

2.16

Si 02

41.2

CaO

1.93

l

M?0

3.75

,

A1203

.21

Mn

.91

-

.\

1i1ii

iil1

l

i

ii!

1

i

1

1ST COPY

RD COPY FIELD

WZ

'-

XC.D.H, w.f^H}*~v'"\" J ft

.fV;. V; ;\ , .. -

is - fi, ~ t,a

PROPERTY

LOCATIONJ O

*

DAVIS

ria-7'HifjG.

TUBE MAGNETIC

^-a

ANALYSES

-,.XTti^wi"/ er^

DATE

GRIND

DATE

•:; v SAMPLE W.

::-;.;-..v ., .

^L5^

••---

. - j -,

FOOTAGEFROM

a^

TO

JO

LENGTH FEET

S

|r.o Fa i

r,

.Offl.

t

'...^ ,S——— j j ,..... t —

/C, 2 l,\~)

-

Si 02

.

,-

———

t — ~Ca^O

?o. 9

-

v~^

J^JT?

Mj ( 0

A? 3

;AL2 03—t ———

.09

'

•,' 1-

In i - *V

* 4- ^

RATIO

Exploration StartedFinished J. Bill fi logged By A, Clark Core Size x i*. T* Safety Plate

DIAMOND DRILL CORE REPORT Plan No. Josephine ACID TESTSSection No. 6-*-oo c. Depth Read Corr.t. A iDept. /oo 1 — se * Elevation ~"

•j'/*' 'i^ * -.*' -" - '

Depth Rood Corr.

DEPTH

0

3x -

34

3

34

73

(LT73

J:^ l

82

-

W

CORE LOSS

0

JS*

2

DESCRIPTION

Casing*

Iron Formation.Grey to Blue Chert.Some pyrite 6 pyrrhotite veins.Good siderite enrichment.Bandings distorted due to brecciation.Scene chlorite filled joint planes.Signs of oxidation.Core split 20 - 25*.

Footwall Zone 12A.Blebs and bands of grey chert.Low sulphides*Siderite content high.Portions of siderite up to one foot in length.Parts of core broken and brecciated.Jointing taoatly in siderite sections.

Siderite. ^Buff.High pyrite content. ,A few quartz~calcito veins.Broken core at 74, 77 A 82'.Non amenable.

^ 73-82

t

SAMPLE NO.

127015

Fa ANALYSIS

to

. -

*

.102

Fe

34.6

^

S

11.6

Si 02

5.57

CaO

4.34

M?0

4.21

A12Q3

.19

Mn

1.77

—

1.t :*\-

f'

- ;

: r. '

r; -.

frS

fSPfPl^sPCTll&i? v-;'*?^ *jt H.V&* -' r'''^ y-*4Vv ?S"..'' . ' ' . J TiTAMnwn ftPTti mov ppcnp?S^^SBM^'^wif ^'.^ T,'. ?,!' ?- - , i.Vj j...;', -- . fiAflUHy i^AJLLLi LAJKfi Ktst\JKL

Syn^.-'f-' - v --. H .. -' v* ' "" .^'OEHH".K

FEGH

jfVx* c 2 'V/^v". - "v

r -

©

ib

'

^•'v.ml A- :

COBS LCB3

2

,j.^V, ; ,;^ V ; "' DESCRIPTION . .

Light gray colour* . Uediun grained.

Agglcaeritio. Siderite enrichment. Fracture pianos 45" to core.

End of hole SO feet.V

l

*

SAMPLE NO.

ANALYSISAa

*

Fe

T

S S102 CaO

i

i

MgO

i

A 1203 Mn

j

•v™^-

i

j

t

'

^^COPY HtlD

ipl|ll^}'' A.oV- 188

#tJ4" O.O.M, NO.^V^.--'.-: "' J"oS-;?..k8

PROPERTYJort

LOCATION

:?'-V*''. SAMPLE NO.

:- } '.; ' -

(JSS70

———————

tty..'~

FOOTAGE

FROM

•Lo

TO

i. r

LENGTH FEET

-5

DAVIS

.| FoO

.PW^c*. u^wV

TUBE KAGNETIC ANALYSES

Fa | Te

r

^

.031

t

20. 9

s—— —

).4.L

Tte-^SI G.

Si 02

.

*

V

^

Ca.O

53.^

^^ '

\f

3.0J

^4^-

^.06

\

-DATE

44, /96SGRIND

DATE

as, 03B- /'t "* ^ -V

1 i J

l

'.' l•In , - -T-1 '*'

t. II

~l~~'

RATIO

r*Jytfi:-,s;' .- :'4 -**fytomBole Mo.

l ' Depth ' 77*

Exploration r StartedFinished 1958 Logged By A. Clark Core Sizo EX u Safety Plate

DIAMOND DRILL CORE REPORTPlan No. Josephine ^Section No,Lat.Dept.Elevation

ACjDCorr. Depth Read Corr.

S'o* -

"v/.i-'n ifJ

,^ fie J2

BKPJH

J®*

0

7

50

TO•M^BM

7

50

77

••••••^

CORE LOSS

2*

3 ,

DESCRIPTION

Casing. J

Iron Ponoation.Grey to black chert.Vhite granular silica veins.Pyrite A pyrrhotite veins throughout.Siderite enrichment in portions up to 3 A 4*wide. Soae black slate. Core brecciated.Cone has been split 25' to 30'. -y

Iron Formation.Grey to Black chert.Some white granular silica.Portiona of massive pyrrhotite.Scene black slate.'Spa ree siderite enrichment.

^End of hole 77*.

SAMPLE NO,

ANALYSIS i

Fa

,

t

1

Fe S Si 02 CaO MjO A12CQ Mni

li iil

ii

i

i

j

'

COP COPl

JftO COPY FIELD

^•v;;/- ; - ' '; vr;ciu'.

J;'0,D.H, NO.

PROPERTY•3 o j" ts-*?* H //vi*- w-es^fT tssj(7*s^JS (GAS

LOCATION

V.-y . . loAVIS TUBE HACNETIC ANALYSES' '*'.' '.' ' 1- ' s l * ' . * . - .*

DATE

GRIND '

DATE

': : -'": SAMPLE NO. FOOTAGE

FROM TO

LENGTH FEET :U±4 Fa Fe

-4—

. . . - - , S . Si 02 Ca ,0 ,Mj Or-1 . |.J ...iJfe AL2 03 i Mn -

^

RATIO

l^^/ lo n.i ^. 70,2 3. O R ..ei • 97

ACID TESTS

iliil&v^ - 'jSm^;!4-'• ;;-;YV "V. :':vVt'"'- J : . , xj DIAMOND DRILL CORE REPORT;W'*VJ ^; .-'•'*''-'^--- v '- ; "' - '' ' Exploration litele Ho. JoatphlM-et-t-^oA.^fcStartod 1S68 Plan No. Josephine fr

' * /AO" ' ,' Finished * , . Section No, i^-ocxa. Depth Read Corr. Depth Read: - 'm '4.5* '."'"-. . : * V. Logged By A, Clark Lat, s -f,

100* ^ . Core Size Dept... 7;;/ ' Safety Plate Elevation

Corr.

'J t A'.- ' -....-.'; DEPTH

0M

, 0

12

, 25

45

,v ': O

••^•^•^

1

TO

12

25

,45

100

^^•^^^

CORE LOSS

3

0

2* .

l^^^^l^^HM

DESCRIPTION

Casirg. v

Iron Formation.Grey to blue chert.Black slate. -Pyrrhotite bands.\Jhlto granular silica.Some siliceous siderite.Core brecciated throughout.Fractures highly oxidised vlth limonite.Leaching evident. Broken core at 17 and 20feet. Chlorite A pyrite in joint planes, y

Iron Formation.Grey to Black chert.Granular texture.Spares siderite enrichnent.Humorous pyrrhotite bandsChlorite 6 pyrite in fracture planes.Predominantly black chert last 8 feet.Scene toognetlto 43 to 45'.Core split 35 to 40*. .

Diabase.Dark grey colour.Medium grain size.Ophitic texture.Hufflorous fault planes.Chlorite filled joint p3' -os.Much of core broken up c*~* to jointing.Numerous calcite filled volnlotta, .

— m* —— ~* ——— — * — * ——— ———— m~i^^-M _______________ , __________________ \^f .... .. . . ..^ ^ ^^

SAMPLE NO.

,

ANALYSIS

Fa

t

Fe

1 1

S Si 02 CaO HjO A1203 Mn

1i 1

j'

iiii

Exploration Started sru^r, i Finished 1968 Logged By A, Clark Core Size Safety Plate

DIAMOND DRILL CORE REPORTPlan No. Josephine

j Section No. La t. 3+st s Dept. Elevation

Depthi o'

t oo'

ACID TESTS Read Corr. Depth Read Corr,

l>^

: DEPTH

nfj0

s

25

4fAv^

50

fc^l

t TO

5

25

SO

75

CORE LOSS

7-

10*

6*,

DESCRIPTION

Casing. -

Iron Formation.Grey to Blue chert.Bands and blebs of pyrite.Massive pyrite at 24*.Core highly fractured with chlorite filledjoint planes,, 'Leaching 6 Oxidation evident.Spa ree siderite enrichment.Brecciated throughout. l

Iron Formation.Grey to blue chert.Pyrite and pyrrhotite veins throughout.Increase in siderite enrichment.Core still highly Jointod with chlorite infracture pianos.Massive pyrite from 28* to 27,5*.Most of core brecciated.High core loss.

Iron Formation.Grey to blue chert.Pyrite 4 pyrrhotite veins A blebs throughout.Massive pyrite- at 65*. .Good siderite enrichment (about 15*).Coro otill Jointod with chlorite filled fractureplanes (about 45* to core). Most of corebrecciated. , ,

SAMPLE NO.

.

ANALYSISAa 2ft

t

. 1

Fe S Si 02 CaO MgO A1203 Mn

-

j

t

i


NO. k — IO' SHEET NO. 2

fe;.:DEPTH.:*

fS;FKOMlip'75•i.(".; :.' ; /-' : .pf^'".

v

J'/:^

T0 :

100

CORE LOSS

.

'•:,- ; ; ." ' DESCRIPTION

Iron Formation.Grey chert*Some white granular silica. (.Lesser amount of pyrite A pyrrhotite veins. High siderite enrichment (Approx. 25t).Some magnetite veins. Core still fracturedwith ohlorito fillod joint planes, Brecciatedthroughout most of box.Core split 85 - 90. -

End of Hole 100'. \s -\

i

SAMPLE NO.

t

^

ANALYSIS

ib Fe 3 Si02 CaO M,0

1if

j.

'1

i

A 1203 Mn

'

i

t

i

— •"••-^-^—-"-

cop?RD COPY FIELD

l^lu'-''1 "'-'. - ' •"••' :^O.O.M. NO.3.!fj.''y-:'-' , ' -J of— /c? — 6fl

PROPERTY

LOCATION ,* ^ ^ ^ 'h 0 r , v "S M -j l S

4-',?- , JOAVIS TUBE MAGNETIC ANALYSES** ' ^ - " ' h*'' ' ' 1

DATE

GRIND

DATE

, SAMPLE NO. FOOTACE

FROM TO

LENGTH FEET FeO Fa i 02 Ga 0 tt*^AL2 03 -h-g . -RATIO

i

A^JL

ksW

C-^&

i^en

enen

en 3

enen

•Jl JJ(D

l 3 9

O 0

O H-J en

cp

eno

coo 00

o CO eno CO 00

o

eoo

en

oo CO

o

en

eno CD

o en

eno J"

.en

•rj

B

to COen o

to

oen

NS l oo l en

to

o CO

co.

o* eno

en -Jen ID

enCO en

en

to -

en oto

COen CO

CD i CO

toCO

A

oCO

-o oen OO en

o l co

i. en ID

oo

o oo

.N

(Oto l o

en

oen C

Oen

s*

CO en

co i O

OJ O

to

to oCD

OO

N5 OCO

en

CD enen

o

oo

to

toto

oo

N5 O

CO

l -J COCO o

o O)

en

oo oo

to

-s.o 00

00 O

ji enen O

so o :o

oo

i CI

M CO

00 o•J)

en •sj

00 en

O COen

S3to 00

oo en

co en o.

^ CO

s O

Co

ra CO 09 O

CO

'V (ft V* t '* * '- . ' ^

rwf'X';.'.. VV. ^ . i . T! * M T '*\ 1 \ t C Ti'ft-V^:,; ' . ^ - * ' o U i o I

W.i;;-V V .... . ilb.O ij.O^p-;: ' 1.:.. 125. -0 l u.o- ft.:.'--'' - - l.i.; 135. u lu.o'-r,-' 1;:.; l'45.u 10. o# :- l- .. 155.0 lu.u

L : . . 1 6 1) . 0 lu.O, . ; . ' 1 : . -' 175.0 10.0

-. . " .. 135.0 iO.O '. : . : 1V5.0 10. C • * ' . 2 J P . J lu.O 2... 215. U lu.U1. . 225.0 1U.U

: i . : . , i 3 5 . u lu.U

it::,. .2uc.y 5.0

1 ** ;:-;.. 2*. o.o i.o

1 - - - .

• *

A\U LOCATIO.,-

*ASTE

FEET •.VAbTE AS

0.300O.U63

1U. O.U950.171 0.028

0.052 * 0.151 0.069 0.190 0.3000.310 0.153

O.U1

0.06,

J.Ub3

0.139

•i

t

'' A igOTuO•H Hi iH Mi JBli"^; j JEB ....yj/..

Jiff

^Ldfr* * * ** * * *" *

WAJ...........•s

Ft s s J02 TAUU""

Jl31 1531

' 3^

32 3233 33

..3*4, .J3

31

2V

2V

• 6 *: . 72 b. db 0. UV• V 3.3ti a. J 7 5.yV .0 0.9V i*4,6J **.'*o•6 *t.29 9. Ob 5.3o

7 ^ A M "* i* ' *J

•B ^.23 3.tiO 5,17 •.b ^.72 b, 3V 5.b3 •5 3.08 b. 2** 6.2J * 1 3.25 7.20 6.07 •6 5.bO b.22 5.47•0 *i.;7 i.ViJ 5.^ •V **. ib 7.9B t* , a5

•-7 i. 43 8.77 - t) . **0

.5 l.Vb ^2.20 3.bO

•^ i. 95 ^.20 3.0 ^

31 .b i . 3 b V.2V 5.33

. * J^^^*W*4 ^^^^ ^^^^ ^^^^ ' ^ ^^m ^^^M

VRV ............

PL .............

DT......... M ..

JO............^f "l^ f^Pf('

}R nUNQ

-'.Uw AL2U3 ,',.,

5. J/5.3d 0.46 *s. 17 S.**? V. ^0 l.^o5 t tic. u , W c .y ^ 5. 13 1.U3 *i.^3 5, *:o o.2d 2.33 5o7 0.34 2,2^ 5.77 0.15 2.2* 5.o6 0.05 ^.22 5.02 0.12 ii.^4

5.U2 w, 30 2. IM . 5.u2 u.^y C.IH

5.3.i 1.10 *i.v,V

4.'*6 o. j 7 i . -y 1

**.^U u.Jo l . v o

5.*v i.v;7 i.wv

i- mn

H a-i-

: ^

ri f

-l-4-

1 j.

(

hese lojs from Wine office in Wawa, first flet from AOP office in Sault

' ..- i-

iiiiiiii9 l l l l l l l l l

,.., . N6s Josephine, GL l"1 •••'. '

Exploration StartedFinished j. Bill & Logged By A. Clark Coro Size Safety Plate

DIAMOND DRILL CORE REPORTPlan No. JosephineSection No.Lot.Dept.Elevation

ACID TESTS Depth Read Corr, Depth Read Horr,

i|^ DEPTH

li FROM

SM fl^v-;i-^/'- *p|'"y': v,'

f "o* ^-'' -'

j?: r-j-Y v ,, V-.fjjV;-;';'''

K-V. ' '

f. .'ft*' ' ;". - i "

'i\ *

K.V.-scl' ' ' .\ ' ' -VV ' ''( : '~?~'f'"

,

i^:-: li^Mft^tM

TO

4

50

110

CORE LOSS

9'

18'

-

mm

DESCRIPTION

Casing and Overburden,

Tuff.Fine grained.Medium grey colour.Agglomeritic portions.Sericitic.Evidence of shearing.Felsite at 16'.Numerous narrow Quartz-Calcite veins up to 1"width.Ottrelite.Banding from 200 to 45* to core.

Tuff.Fine grained. Sericitic.Medium grey colour with portions of light grey ~ -buff felsite at 83' Z 91'.Shearing.Core still contains narrow O^iartz-calcito veins.High carbonate content, A few scattered pyritex 's. Agglomeritic portions. Higher chloritecontent last 5 feet.

mmmmmmmmmmmmwmmm

SAMPLE NO.

M

ANALYSISAs

•l

i

Fe

mm

3

-

Si 02

'

-

CaO

•-

VgO

"

A12Q3) Mn

•j-imm m

^^^^^^y^vX;;;,, .-: . - ^ DIAMOND DRILL . CORE REPORT^' - ^

ft^0aS:li;6. di. i ' '' : SHEET NO. 2*fesfc DEPTH ' :

PTRCK ;l^iiOLW^*-* ;

j;??:^'. '^'-- 1 - ! '

:' . t. -

125

150

-

^

TO"

125

150

175

-

.

—

Lee?2'

'- -

8'

DESCRIPTION

Siderite.Buff.Jointed with chlorite filled fracture planes.Pyrite flecks throughout. Evidence of leaching.Some O^iartz-calcito blebs and veins to ^".Magnetite portions up to one foot in length.Portions of broken cora throughout box. Nonamenable.

110-115115-125

Siderite.Buff.Highly jointed with Chlorite and leaf pyrite inthe fracture planes. Some magnetite at end ofbox. Several narrow Quartz-Calcite veins to^". Scattering of pyrite x's throughout.Non amenable.

Core loss 126 to 130 125-135" 132 to 133 135-145" 134 to 135 145-155 v

t0

•H

Siderite.Buff to grey-blue.Core still highly jointed.Portions of core magnetic throughout box due tomagnetite (dark grey-blue colour), A fewQuartz-calcite veins to j? width.Pyrite and pyrrhotite flecks throughout.Non amenable.

155-165165-175

SAMPLE NO,

12700102

030405

t

0607

--

As

.300

.003

.095

.171

.028

.042

.052

.

Fe'

31.631.9

15.031.633.0

34.734.8

.'.

S

2.723.38

,?94 fc 292.44

2.584.23

-,

Si02

ANALYSIS

CaO I'gQ

ii

6.88 6.098.07 i 5.59

;i

34.609.084.68

4.465.365.35

4.003.80

.4.835.17

mm

5.375.38

5.475.225.13

5.285.37

^

Al203

.44

.46

9.30.99

1.03

Mn

2.102.17

1.062.072.23

i

ti

.28

.342.332.24


yv.-;.'-V; NO. GL l SHEET NO, J

v .DEPTH '

?.' 175

200

225

-,

TO200

225

240

'

.

CORE LOSS

2

1'

9'

•LJ

DESCRIFIION

Siderite and Magnetite.Buff to dark grey-blue.Jointed with chlorite filled fracture planes.757. of core is magnetite.A few narrow quartz veins. Core has high car bonate content.Non amenable.

175-185: 185-195

195-205

Siderite and Magnetite.Buff to Blue-grey colour.50% of core is magnetite.Core still highly jointed with chlorite S leafpyrite in joint planes.Still a few Quartz veins St blebs.Increase in pyrrhotite in the forrr. of blebs andveins.Massive pyrrhotite at 213'. High carbonatecontent. Non amenable.

205-215215-225

Siderite and Magnetite.Buff to Grey-Blue colour.Fine grained.Highly jointed St brecciated, A few quartz-cal-cite veins.High core loss.Flecks of pyrite and pyrrhotite throughout.Non amenable.

225-235235-240

End of Hole 240 feet.

m^wm^iwmmmmmwm

SAMPLE NO.

1270080910

'

-'

1112

- ' -

1 i; 13' 14

ANALYSIS

Rs

.151

.069

.190

.300

.310

.153

.064

t

- -

Fe

32.832.533.1

33.634.0

33.929,5

m

s

2.723.083.25

5.804.37

4.361.96

•H

Si02 CaO

1

6.39 5.836.24 6.237.20 j 6.07

K?0

5.775.665.62-

l

i;

,

8.225.95

7.9822,20

M

5.475,24

4.853.68

.

4.925.02

5.024.48

A 1203

.15

.05

.12

.24

.30

.28

.37

Mn

2.242.222.24

2.002.14

2.141.97

i

J|'~'

V

i

V

l-.V

1j -

•4

\\

'

\ i1

1

i!

j ;; '

"ii i

V . '''

-, - -

•t'*t.

DIAMOND DRILLA.O. 6(2

ALGOMA ORE DIVISION

:ALG;)' ; A ORE DIVISION UIA''',Cx ,D DRILL ASSAYS

LOCATION-

*- 4IXED ORE AND .vASTE **-S'JB TOTAL

**#-TOTAL

FROM TOFEET

DIST .VAST E AS

CJL l

SI02 GAO AL203

# *

110.0115.0125. 0i 3 i1 . C1^5.0155.0165.0175.01 S 5 . 0195.0205.0215.0225.0

1 1 y . G

235.0

235.0

110.0

115.0125.0135.0145.0155. U165.0175.0135.0195.02 J 5 . 0215. U225.0235.0

235. ~

2*40. 0

240.0

2 '* 0 . 0

5.lo.lo.lo.lo.lo.10,10,1U,lw.lo.10.10.

125.

5.

5.

130.

00o lo.0000 '

0c0000

0

0

0

0

0.3000.0630 . u9 50.171O.o28O.U420.0520.1510.0690.1900.3000.3100.153

0.141

0 .u64

0.063

0.139

313115313334#4323233333433

31

29

29

31

.6

.9

.0

.6

.0

.7

.8

.b

.5

. 1

.6

.0

.9

.7

.5

.5

.6

2.723.380.99*t. *i92.442.664,232.723. Ob3.25s. bO*4. 374.36

.3.43

1.96

1.95

3.36

6.d8H. 07

54,609.UB4.684.003. dO6.39b. 247.20d.225.957.98

8.77

22.20

•i2.20

9.29

6,095.594.465. 365.3b4.a35.175.636.236.075.475.2*44. d5

5.40

3.66

3.67

5.33

5.375.365.475 . ^25.135.265.375.775 . oo5.624.925.025.02

5.32

4.46

4.4U

5.^9

00Vu1u0000000

1

0

0

1

.44

.46. ^0.99.03. 2a.34.15.05.12.24.30.23

.10

.37

.36

.0?

2. 102.171 . 00*L . 0 12,232,332,242 , 2*tt , tt2.^4*i. 002. 142. 14

..U9

1.97

1 . 96

2.09

Josephine GL 2

217'

Exploration Started Finished 1968 Logged By A, Clark Core Size Safety Plate


Plan No. JosephineSection No.Lat,Dept.Elevation

ACID TESTS Depth Read Corr. Depth Read Corr.

Twy r/'***' - ' K ' -fS , ///e* i 7, rv/Cs .

DEPTH

FROM

0

50

100

131,

TO

50

100

131

-

132

CORE LOGS

5'

2'

0

0

DESCRIPTION

Tuff.Medium grey colour.Sericitic.Few portions of Felsite.Agglomeritic portion 41 to 44 feet.Shearing evident 40* to 50* to core.Core badly broken up.

Tuff.Light grey to buff~yellow.Sericitic.Sheared fracture planes 45* to core.Scattering of Ottrelite crystals.Most of' last box agglomeritic, (i.e.) 75 - 100).Increa^w in felsitic portions. Core not sobroken as previous boxes.Some carbonate content observed.

Tuff,Medium to dark grey colour.Fine grained.Kot nich sericite.Increase in chlorite last 8',Good carbonate content.Core has been split 110' to 120'.

Massive pyrite.Core has been split 130' to 145'.

SAMPLENO.

r i

ANALYSIS

Fa Fe

i

S Si 02 CaO MgO

X

A12CC Mn

.

"DIAMOND DRILL CORE REPORT

v-- HOLE NO. G L 2.'-*"',f-. -l ' '' '" *" ' ______

SHEET NO. 2

i,,^: DEPTH'

' ; FROM

C ' 132

150

177

183

-

189

t f—- mmmmmm

TO

150

177

183

189

195

•1MIMHH

CORE LOSS

4

1

0

0

0

••iMMIBMri

DESCRIPTION

Siderite.Buff to grey.Highly jointed with chlorite filled fractureplanes.Scattered pyrite x's throughout.Some leaf pyrite.Few narrow Qtz-calcite veins.Non amenable.

Siderite.Buff to grey colour.Some magnetite 163 to 167'.Considerable pyrite content.Jointing still evident but not as much chloriteas previous box.Non amenable.Core split 150 - 175.

Silica Rib.Siderite with blebs and veins of grey chert andwhite granular silica.Some pyrite veins.About 6" of removable material.This section amenable to treatment.Core split 175 - 200.

Siderite.Buff to grey.High pyrite content.Numerous chlorite filled fracture planes.Non amenable.

Foot Wall Zone.Buff siderite.High sulphides.Blebs and some narrow veins of silica,Non amenable.

SAMPLE NO.

.

ANALYSISAs Sac

*

Fe S Si02 CaO

1

M?0 A 1203

i

Mn

DIAMOND DRILL CORE REPORTNO. GL 2' SH3ETN0.3

St DEPTH "

FROM

195

TO

217

CORE LOSS

1

DESCRIPTION

Iron Formation,Grey to Black chert,Veins of pyrrhotite.Some siderite enrichment.A few large veins of white granular silicaCore brecciated throughout.Some chlorite filled jointing lost few feet inbox.Core split 200' to 217',

End of hole 217'.

\

1

SAMPLE NO.

-

ANALYSIS

Fa

t

Fo S Si02 CaO

1

I

l

j

*o A. 1 203 Mn

Josephine GL 3 StartedFinished 1968

Lowed By A. Clark Core Size Safety Plate

DIAMOND DRILL CORE REPORTPlan No. Josephine Section No,

- Lat. Dept, Elevation

ACID TESTS Depth Read Corr, Depth Read Corr.

DEPTH

FROM

0

4

25

50

J* —

TO

4

25

50

60

(

————

CORE LOSS

l'

2'

4'

DESCRIPTION

Cosing.

Tuff.Medium grey colour.Fine grained.Sericitic.Sheared 450 to core.Felsitic from 7 ' to 19' and Yellow to Buff incolour.Agglomeritic last 6 feet.Medium grey colour. .Sericitic - Fine grained.

Tuff.Medium grey colour.Fine grained.Agglomeritic.Yellow ~ haff felsite from 38 f to 45'.Fine grained, grey tuff from 45 to end of box.Scne narrow veins of felsite.

Tuff.Medium Grey Colour,Fine grained.Sericitic.High chlorite content.

t

SAMPLE NO.

i

'

!

ANALYSIS

Fa Fe

* t

S Si 02

-

CaO MgO A1203 Mn

.^ : . DIAMOND DRILL CORE REPORT HOLE NO. GL 3 SHEET NO. 2

DEPTH

FROM

GO

65

66

TO

05

66

100

100

•150

150

190

CORE LOSS

4

0

4'

3*

0

DESCRIPTION

Chlorite Dike.Dark Green.Fine grained.Sericitic.Numerous narrow calcite veinletts. High coreloss.

Agglomerate.Calcite and pyrite crystals in chlorite matrix.

t

Iron Formation.Grey granular silica.Grey and blue chert.Pyrite and pyrrhotite veins and blobs.High' sulphides 76 to 77'. Distorted bandingand blebs.Core brecciated throughout.Good siderite enrichment throughout.Jointing mostly in the siderite with chloritefilled joint planes.

Iron Formation.Grey to blue chert.Scene bands 300 to core.A few white granular quartz veins.Scattered pyrite and pyrrhotite veins.High percent of siderite enrichment (about 30ft)Core still jointed with chlorite in the jointplanes. Host of core brecciated.

Iron Formation.Grey to blue chert.Some white granular quartz veins.Not rcuch sulphides.

SAMPLE NO.

•••••••B

ANALYSIS 1

Fa

f t

•MH

Fe

•IMHI

S

mmmmm

Si02 CaO

1

KcrO

i

'ij

iiiiii ii

j

•^••i^•••i•••B

A 1203

ii

Mn

H1

i1

•M^l••••B

iSir,-'DIAMOND DRILL CORE REPORT

HOLE NO. G L 3 SHEET NO. 3

- DEPTH

FROM

150

•••••••M

TO

190

^^^^mm

CORE LOSS

0

•^••i^Mi

DESCRIFTION

Cent 'd.

Magnetite portions and veins throughout.Siderite enrichment about 157e.Most of core brecciated.Some banding 450 to core.Siderite portions are jointed with chloritefilled fracture planes.

End of Hole 190'.

M^^|aHH^|HB^^^BHB|^^^HaHBaBHHMHM||MMBBHMHMBMMBM.-MMBlB^——^^B^HaHBBlMMHMMMMBM^MM|

SAMPLE NO.

-

•MMMftaattMOMM

ANALYSIS

Fa

*

•MMHAA^

Fo

^taMMMMB^H.

S

.^dl^IMM^

Si02 CaO

liii

.. i - m ^ . tjL L--

M?0

1

Al203 Kn

;

j

Exploration Started l tJfiR Finished 1 968 Logged By A. Clark Core Size Safety Plate

Plan No, JosephineSection No.Lat.Dept.Elevation


BlKcr v ' ~'ff"'"f '^^^'IfracMl!0S !'-'-' " ' 'pMi'i1-''fee i*I&. -' .

1 - 20ft' '-.|- u -l" :

r 27jrt 'li/';l-:; ' v . 44K" :l" '

i.'. ,i'-'

^ ' 0 3t . .

b.ki'

fc- '-.' i-' X

K

TO

15

3.6

20

27

44

63

74

CORE IflSS

4

5

0

2'

0

DESCRIPTION

Cosing.

Overburden.

Core Loss.

Tuff.Medium grey-yellow colour.Fine grained.Sericitic.

Siderite.Grey to Buff.Pyrite content high.A few blebs of grey chert. ^Non amenable.

Footwall Silica.Grey chert vdth portions of siderite and pyrite.Scrr.c magnetite.Ground core at 63'.

Magr.otitc.Dork grey-blue.Fine grained.Highly r&gnetic.Pyrite veins and blebs throughout.•fr" calcite vein at 65'. Sone siderite last 3 or4 feet with sor.e chert blebs.

SAMPLE NO.

.

ANALYSISAs

-

i

Fe

4

S

-

Si 02 CaO M70 A12CC Mn

" DIAMOND DRILL CORE REPORT

'X, C L 4 SHEET NO. 2

[lg- - . DEPTH

jly-rpox^f- r*- v '- p '

3i*--'?-A - . - ''

'"{•'"' ' . m . . "

,' '

\ - ** .

••-t -''••• : "" 103',: r -.''•. '';

. 1 .. '.K'/',

121

'

TO

ion

121

216

CCR* LOSS

3

2

4

DESCRIPTION

Iron Formation,Grey to black chert.A few pyiite veins and blebs.Some magnetite veins.Siliceous siderite enrichment.

Quartz porphyry.Medium grained.Light grey.Agglomeritic,Epidotization at 103' and 121'.

Iron Formation,Grey to black chert.Some veins of white granular o^iartz.Siderite enrichment Sic. A few magnetite veins.Massive magnetite 164 to 165. Occasional pyriteand pyrrhotite veins and blebs.

End of Hole 216',

'

SAMPLE , NO.

•••^^•^••i

ANALYSISAs

jBa

.

•IBBBH

Fe

i

mmmmmmm

S

•^•••i

Si02 CaO

i

ri

1

i^'

^^••HIBH^BH

MjO

l

•^••i

A 1203 Mn

ii

••••Mmmmm mm

|vV DEPTHi '.'r ' -

^: FROM|;:;., o

f' : '-- i*fc-;1 ;-'-f;'.;..*'/

r '-

t: : 28- ^ - . "

V* -

'•'* - 'l ' : .- J"-" '?.9l \

h-.'/"i r ' 48~v

;

i"4": -

if

TO

15

28

29

48

107

, .

CORE LOSS

8

0

0

3'

j

DESCRIPTION

Casing,

Tuff.Green-yellow colour.Fine grained.Sericitic,High chlorite content.Most of core broken up. High core loss.Agglomeritic portions.

Iron Formation.Grey chert with siderite enrichment.Massive pyrite at 29'. y'This section possibly Hanging Wall Type.

Footwall Silica Type,Portions of inderite with blebs and distortedbands of grey to blue chert throughout.Blebs end bands of massive pyrite in most of thissection.

Iron Formation,Bands of Grey and Blue chert throughout about 4 S0to core.Most of core brecciated, Bands of magnetite,black slate and black siderite.Portions of siliceous' buff siderite up to one' foolin length,

SAMPLE NO.

ANALYSISAs fa

'

Fe

i

S Si 02

,

CaO MgO A 1203 Mn


SHEET NO. 2PC1 ''. ' ' ''" r —— 1 Jg^fcDEPTH'?.;-'Pjj^roOM'''

^t- W'

vJV^' "C;;X ; - ,/b^''"-'. ;If:: .f!'",: '

K?-^\ - ' ' '•-': )V' V "' Y

l'.'" ''

' i '

i""1 r * ,

r--,;'.:^ '

^^•'.'••:l

TO

107

cow,LOSS

3'

DESCRIPTION

Cont'd.

Veins of pyrite and pyrrhotite.Not much jointing.Core has been split 80 to 85'.

End of hole 107'.

t

SAMPLE NO.

ANALYSISAs

-

Fe

*

8 Si02 CaO

1

t

!

i1

:

ITjO

i

A1 2031

Mn

Explc tion Started FinishedLogged By A, Clark Core Size Safety Plate

DlBMD MILLPlan No. JosephineSection No,Lat.Dept.Elevation


fJt.f \^. r/". ,v^v;-

DEPTH

FROM

0

3

46

55

TO

3

46

55

100

CORE LOSS

3.5'

3*

7'

DESCRIPTION

Casing,

Iron Formation,Grey to black chert with bands of whitegranular silica.Some Siderite enrichment.A few narrow pyrite and pyrrhotite veins.Distorted banding and breccia throughout.Core split 25 to 30'.

Quartz porphyry Dike.Medium grey colour.Fine grained.Agglomeritic.

Footwall Silica Type. vPortions of Silica, Siderite and Magnetite upto one loot in length. Most of core brecciated.Siderite make j up about 40*X, of core.Core is jointed with chlorite filled fractureplanes.Minor pyrite 6 pyrrhotite ~ veins throughoutcore.Pyrite-Argillite at 58'.

58-68

End of Hele 100'.

SAMPLE NO,

i

i

127016:

ANALYSIS

Fa

.099

Fe

23,3

4

S

2.16

Si 02

41.2

CaO

1.93

M?0

1

3.75

A12CC

.21

Mn

.91

Josephine No. G L 7

90'

Exploration StartedFinished J. Bill S Logged By A. Clark Core Size Safety Plate

DIAMOND DRILL CORE REPORTPlan No. JosephineSection No,Lat,Dept,Elevation

Depth ReadACID TESTS

Corr, Depth Read Corr.

DEPTH

FROM

0

3

3',

7;

.

y . " - . :••••M

TO

3

34

73

82

•••B

CORE LOGS

0

5*

2

••••I^Hi

————————————— " ————— ~— ————————————————————————————————————————————————————————

DESCRIPTION

Casing.

Iron Formation.Grey to Blue Chert.Some pyrite St pyrrhotite veins.Good siderite enrichment.Bandings distorted due to brecciation.Sone chlorite filled joint planes.Signs of oxidation.Core split 20 ~ 25'.

Footwall Zone 12A.Blebs and bands of grey chert.Low sulphides.Siderite content high.Portions of siderite up to one foot in length.Parts of core broken and brecciated.Jointing mostly in siderite sections.

Siderite.Buff.High pyrite content.A few cjuartz~calcite veins.Broken core at 74, 77 & 82'.Non amenable,

' 73-82

——i———————.—.———.—————-—.—————-—^——^—^^^.—^^—.————-—

SAMPLENO.

127015

••••••^•^H

Ta ANALYSISJttSFa

'

.102

^^•^^•H

Fe

34.6 *

^••••.^

S

11.6

^^^^^^•B

Si 02

5.57

^•^•MMMI

CaO

4,34

^^•^•••Mi

MjO

4.21

•••^•^^^H

A1203

.19

^^^••^••••B

Mn

1.77

••^^^^^•^ ^m mmtm-li^ m m —

DIAHOND DRILL CORE REPORTIJC. GL7 SHEET NO. 2

ffclEKH vl&okK?B2'-1 f-."1 - . 'j/:'.-'--,

* '

^.^^^^^^^^——a,

TO

90

t t

L^^^———mmf

cos:LOS?

2

i^^^^-^^^^—

DESCRIPTION

Tuff. Li?ht grey colour* Medium grained. Aggloroeriti'o* Siderite enrichment. Fracture planes 45* to core.

End of hole 90 foot.

\

t

SAMPLE NO,

-

AM LYSISAS9V Ft

t t

8 8102 CaO

r

i

M?0 A 1203

i i

i1

Kh

IHHHh M HIfr^te'.-.;'-: -JosephinG ^**tolo No. G L 8

77'

Expiora^^n ^^ StartedFinished 1968 Logged By A. Clark Core Size EX Safety Plate

No. JosephineSection No, Depth Read Corr. Depth Read Corr. Lat. Dept. Elevation

. DEPTH

FROM

0

7

50

TO

7

50

77

-

CORE LOSS

2'

3

DESCRIPTION

Casing.

Iron Formation.Grey to block chert.White granular silica veins.Pyrite & pyrrhotite veins throughout.Siderite enrichment in portions up to 3 fi 4"wide. Some black slate. Core brecciated.Core has been split 25' to 30',

Iron Formation,Grey to Black chert.Some white granular silica.Portions of massive pyrrhotite.Some black slate.Spa ree siderite enrichment.

End of hole 77'.

SAMPLE NO.

1i

ANALYSIS

Fa

.

Fe S Si 02 CaO i A120" Mn

WMY-'-fr'''--*'-''."--- •• H61e\K6';v Josephine G L 9

O.--:- ' - ..''•100'

-..-. jtion Started 195 e Finished " Logged By A, Clark Core Size Safety Plate

Plan No, JosephineSection No.Lat.Dept.Elevation


1-.- DEPTH'•. ' . L' FROM

0;- - 12

y : '.

25't

,- '

45

li - ' ' :

TO

12

25

45

100

-

CORE LOSS

3

0

2'

DESCRIPTION

Casing,

Iron Formation.Grey to blue chert.Black slate.Pyrrhotite bands.White granular silica.Some siliceous siderite.Core brecciated throughout.Fractures highly oxidized with limonite.Leaching evident. Broken core at 17 and 20feet. Chlorite 6 pyrite in joint planes.

Iron Formation,Grey to Black chert.Granular texture. \Sparce siderite enrichment.Numerous pyrrhotite bandsChlorite fi pyrite in fracture planes.Predominantly black chert last 8 feet.Some magnetite 43 to 45',Core split 35 to 40'. '

Diabase,Dark grey colour.Medium grain size.Ophitic texture.Numerous fault planes.Chlorite filled joint planes.Much of core broken up due to jointing.Numerous calcite filled veinletts.End of hole 100'.

SAMPLE NO.

*

ANALYSISFa

-

j

Fe

t*

S

.

Si 02 CaO KgO A120; Mn

Hole No.StrikeAngleDepth 100'

Josephine GL 10

Exploration Started Finished 1968 Lowed By A. Clark Core Size Safety Plate

DIAMOND DRILL CORE REPORTPlan No. JosephineSection No.•La t.Dopt.Elevation

ACID TESTS Depth Read Corr. Depth Read Corr,

DEPTH

FROM

0

5

25

50

TO

5

J. 5

50

75

CORE LOGS

7

10*

S'

DESCRIPTION

Casing,

Iron Formation,Grey to Blue chert.Bands and blebs of pyrite.Massive pyrite at 24'.Core highly fractured with chlorite filledjoint plains. Leaching & Oxidation evident.Sparce siderite enrichment.Brecciated throughout.

Iron Formation.Grey to blue chert.Pyrite and pyrrhotite veins throughout iIncrease in siderite enrichment.Core still highly jointed with chlorite infracture planes.Massive pyrite from 26' to 27.5'.Host of core brecciated.High core loss.

Iron Fomation.Grey to blue chert.Pyrite fi pyrrhotite veins & blebs throughout.Massive pyrite at 65',Good siderite enrichment (about 15ft),Core still jointed vith chlorite filled fractureplanes (about 45" to core). Most of corebrecciated.

SAMPLE NO,

1 '

t

ANALYSISAs 'Sft

Fe

t

S Si 02 CaO MgO A120C Mn

MDi OND DRILL CORE .PORT

l?®'HOLE'NO.. G L 10 SHEET NO. 2

m 'DEPTHr.

1FROM

75

TO

100

CORE LOSS

2'

DESCRIPTION

Iron Formation.Grey chert.Some white granular silica.Lesser amount of pyrite A pyrrhotite veins,High siderite enrichment (Approx. 25%).Some magnetite veins. Core still fracturedwith chlorite filled joint planes. Brecciatedthroughout most of box.Core split 85 - 90.

End of Hole 100'.

.

SAMPLE NO.

ANALYSISAs jfia Fe S Si02 CaO

1

i;

1

j

MjO

'

A1203 Mn

i

i

3*X;t-*".M., tt*


HOLE NO. 3500 SHEET NO.

l

l

i i ii i

" . — DEPTH

r MOM

1405

1705

1858

2030

2141

21S4

2300

2652

2350

12920

TO

1705

1858

2030

2141

2154

2300

2652

2858

3920

2973

DESCRIPTION

Toff a - intermediate to basic, dark grey colour. Alternating beds of fine, meditn and coarse Kith coarse predominating. Minor sericitization. Slight carbonatizi

Tuffs - acid, medium and coarse grained, pale yellow color, well sericitized and carbonated.

Tuffs - basic, fine and medium grained, dark grey colour, very minor carbonate.

Tuffs - acid and intermediate, fine grained, light yellcwish grey colour, well carbonated.

Tuff - acid, pale grey colour, coarse grained fragments up to 2" in diameter. Soricitized and carbonatized. Last 30* of section contains 20# flecks of green mafics producing a speckled appearance.

Tuff - acid, fine grained, yellowish grey colour, well sericitizod and carbonated. Contains 5 to 10jS saall specka of dark nafics producing a poppored appearance.

Tuff - intermediate d ark grey coloured and acid-— Pale grey, fine grained interbedded. Small flecks of dark mafici throughout , in places producing a banded appoarance, probably due to schisting. FO-.T inclusions of groen chloritic tuff in last 20*

Tuff - basic, dark green colour, chloritized. Some sections contain much fine light coloured carbonate. ^ irregular quartz-carbonate stringers.

Tuff - Intermediate and acid, Tine grain Section begins as dark Grey, becomes pal grey at centre end grades back to dark grey.

Tuff - bnoic, dark creon colour, o.hlorit Sor.e sections containing much lipht coloured crystalline carbonate.

i

NO.

tion.

d.

c.

rt.

i

'SSS

ANA™ in i i

•- LYSIS' "" i . i^

• lO.

"- MN

.

:- js

l He. 1" VT*'***

'w-f ALGOMA ORE PROPERTIESii rC;'' "'t v. \Vr'--

lllll liil l lll

HOLE NO. 1200 SHEET No.—— --m "i'--- 'i —— •f--'

DEPTHFROM

—

2973

3121

3336

37C6

3800

TOsszss:^

3265

3396

3706

39 OC

3913

1 ' l :

DESCRIPTION

Puff- intermediate and acid. Interbeddedlark grey intermediate and light greyicid, fine grained tuffs in approximatelyjqual amount. Sone carbonate, -mostly inicid sections. Last 30' containa 30J&lark green chloritic tuff.Cnoluded section 3028-3030 - lamprophyre,)lack colour, fine grained, sugary texturContains few blobs and stringers of whitefeldspar.

Hole wedged back to 5118*Core beginning at 3126'3126-3204 - tuffs, as section2973 - 3265.Re-entered original hole at 3204.Resumed drilling at 3265'.3265-3304 - tuff, intermediate,dark grey colour, fine grained,minor carbonate.

M out xJE.C? 6t5' fc/^CK /ST S\*O

C-e *-i ft,E6-i'Jt0 l' 1 6- AT 3 * i- 1Puff - int. and acia. InterbeddedIntermediate dark grey and acid, light5roy, fine grained tuffs.last 50' of section 'partially chloritizedpossibly alteration material derived fromnetadiorite.

.letadiorito - dark groen colour, basic.Patches of dark groen mafics surroundedby light coloured feldspars producinga mottled texture. Some sections incentre of section are coarser and displaya distinct phitic texture. Contact zonesfine groined. South contact con tains '15ffine crystalline carbonate for 15*; Northcontact contains few inclusions of tufffor 10'.2*3 quartz-carbonate stringers up to 12"'.ri.de, occasional patches and crystalsof coarse pyrite.

ruffs - intermediate, dark grey colour,fine grained, minor carbonate.

?uff - inter odiato and aci.1 , interbeddedintermediate dark proy and acid, lightf.rey, fine grained tuffs.\cid sections carbonated last 10' ofsection contains 25^ milky quartz striateand 25?o yello'.vish coloured quart s-carbonalo matallicD.

ANALYSIS —— "NO.

.

9.

i

i

rsto.

rt. ms

.

- SiOj

sag:

-

"*- i m.m~

MNszjszrs::

*

•" i^

l

" , ,

l**;v;.**W M*. Ut.J-v.V-M***

ALGOMA ORE PROPERTIESHOLE NO. 1200 SHEET NO.\tIs-i; r ;

tlJlii1iii1iii ii\

^t'f m

DEPTHFROM

3913

3975

3995

4160

4660

4788

4795

4820

4843

4880

4965

i

TO

30 75

3995

1160

1660

1788

1794

4820

1843

1880

4965

5006

t

DESCRIPTION

Tuff - intermediate, dark grey colour,fine grained, moderately carbonated*

Tuff - intermediate, dark grey coxour,coarse grained. Contains many "eyes" offeldspathic Tutorial, many of which havebeen replaced by yellowish carbonateproducing and augen appearance*

Tuffs - acid, light grey colour, mediumgrained, somewhat carbonatized and oeric:50# of section contains some small blackottrelite crystals, some narrow sectionscontaining as much as lOjS.

Tuff - acid - "quartz eye" type, lighti'ey colour, medium grained. 1 to 2J& bluiscoloured "Quartz eyes" increasing toSfc towards end of section.3 to 5^ ottrelite cyrstals throughout,minor carbonatization and sericitization

Tuff - acid, mr.inly light groy colour,alternating fine schistose and mediumgrained. 10 to ISJo streaks of yellowishcarbonate.

Tuff - basic, dark groen colour, chlorit:very fine grained, minor onoll bluishcoloured quartz "eyes".

Tuff - as. section 4660 - 4788.

Tuff-- acid - pale greenish colour, finegrained, contains few streaks of groenchloritic material and streaks of pyrrhol2tfo small dark ottrelite cyratals.

Tuff - acid, as section 4660 - 4788.

Rhyolite - acid, light yellow colour,felsitic texture, sericitic, very uniforzthroughout. Last 17' very pale greycolour, felsitic, with scattered patchesand streaks of pyrite and 5f, milkyquartz stringers.

Tuff - acid, fine grninod, light yollov;ii^roy colour, aericitizod nnd carbonatizei

ANALYSISHO.

tized

h

c,

ite.

,

•h. *

t

re*

i

m

t

• lOa MM

•e

II***ALGOMA ORE PROPERTIES

1 ;'.- - HOLE NO. 1200 SHEET No. 5

\~t.*j*

l1

i1 52

!'

!ii

] r.

*

DEPTHFROM

5006

5130

5305

5318

36.5

5453

4.54.3

5458

TO

513C

5305

5318

5336

5451

54 S'

5456

546C

5460 54 C2,

.5'

.3

5

DESCRIPTION

Tuff - intermediate, alternating nndiumand coarse grained, gyeyish green colourlAst 25* contains much green chloriticmaterial, contact gradational-vilth^metadiorite. At 50iT9* a 6" lamprophyredyke, blaci- colour, sugary tortured,micacouo type.

Metadlorito - first 18' fine, shistoss,dark green colour. Remainder mediumgrained cyrstalline, generally with anophitic texture but contains many finegrained schistose sections*Section 5256-5257 lamprophyre dyke,black colour, fine grained, micacious t y

Metadiorite - grey green colour, finegrained, schistose. lOJf pale colouredcrystalline carbonate In last 5* of sect

Tuffs? - grey-green colour, schistose,indistinct fragmental.* but mainlyaltered to grey green coloured schist.10^ quai'tz-carbonate stringers up to8" wide.

llotadiorite - grey groen colour, finegrained, schistose. 15^ crystallinecarbonate. Fow tuffaceous remnantsthroughout- last 2' of sect ion*- Dark^reon chlorite schist containing a fowciystals of magnetite.

Fi) o grained siliceous magnetite withfew streaks of carbonate. First 6nof section a mixture oi carbonate andgreen schist containing 15^ coarsemagnetite and 10^4 coarse arnonopyrite.

Banded siliceous siderite and finegrained magnetite with for/ stroe-Jcs ofpyrrhotite, banding averages 50 0 to core.

Banded fine grained mafjiotito.80^, and siliceous siderite, minorstroaks of pyrrhotite. La3t 3" containt50-^ green schist and 50-^ pyi-rhotite.

Biindod green schist, silica, siliceoussiderite in tib out. oqupj proportion.Last 6" cor.tftir.c 50,"S pyrrhotite. Minorcrystals of magnetite.

ANALYSISNO.

.

pe.

ion.

69910

11

12

G9901

re.

43.4

26.3

39.7

i

34.9- L ^ f.- C

S

7.8•- - s

SlOa

14.1

44.0

23.3

18.52•t- -s- - s-

MN

*-\

Tft.

i

l

f

15.i -^


HOLE NO. 1200 SHEET NO. 6

541 S .

!

y.,1f . .

,

5

5

DEPTHFROM

32.5

5465

5470

5475

5480

5485

5490

5495

197.3

i93.5

5500

3505

S509

j

551 R . T)

TO

465

5470

5475

5480

5485

5490

5495

5497

5498

5500

5505

5509

5512

552-1

.2

.5

DESCRIPTION

siderite - pale "brown colour.35S disseminated magnetite, minor patchesDf coarse pyrite and few crystals ofarsenopyrite. Some crystalline- calciteand secondary quart/, stringers.

Siderite - pila brown colour.5# disseminated magnetite. Somecrystalline calcite and secondary quartz.Few crystals of arsenopyrite and minorpyrite and pyrrhotite.

Siderite - as prevous section .10J& secondary quartz stringers.

Siderite - as 5465-5470

Siderite - grey brown colour, llinorlissoninated magnetite but contains fewstringers of magnetite near centre ofsection. )Cinor calcite or secondary qtz.

Siderite - as previous section.3^s quartz stringers.

Siderite - Pale brown colour.yZ d isseminated magnetite. 8j5 finelisseminatod" pyrrhotite and coarse pyrite~fp secondary quartz stringers and 5ySjrystallinB calcite.

Siderite - as previous section

Passive pyrite and pyrrhotite with minorsiliceous siderite..

Siderite - rilicoous, 15/J pyrite.

,5

f quartz stringer paralleling last 6*3f core.

landed siliceous siderite and silica.20J: pyrite, banding irregular, in places)p.ralloling core but mainly at 45' to cor

U-jided silica, OOjS and siderite, 20f3 .binding at GO 0 to coi-e.

'ct'idiorito? Fine ;-.rainod pi-ay green3;;lour, silicified. 15^ bands of silica:\:id loan siderite at 60* to core.

Silica, dense, bluish colour, llinor;-)ptchos and irregular stringers of silic'ivorite. Indistinct banding at 50" to

NO.

69901

o:

04

05

06

07

OBA

08

08C

09

).

3U3ire.

ANALYSISrf.

1 ^ 1 —

39.4

57.2

36.9

36.5

36.2

37.2

39.1

49.1

38.9

30.7

w

- — ——

3.74

4.55

2.32

2.08

'3.56

4.44

3.80

25.5.

16.0

11.6

BlO.

- ——— ———

5.34

13.40

U.24

7.46

14. 18

9.20

7.04

4.96

L8.06—— -— -~*~ ~~

J4.64

:rr1MN

— -*

— —— '"

O3fi|

2.e

18. S

ort 7t, O K-

27.2

21. E

01 rjijJL.*.

l

22. i

18. S

18. J

16. J

1

iwr.n-.--"--:*r*( w*, tt*m^.-*****V^Jv-^* . ALGOMA ORE PROPERTIES

HOLE NO. 1200 SHEET NO.

I2SL7?'.

~-\ 'l111

5

1

I 5y

j1

1

1

i

1

i

1

j

DEPTHrnoM

5524

5528

5531

5540

#3.5

5559

2*-)53.5

5579

5606

5616

5642

5663

5678

5707

TO

5528

5531

5540

5543

5559

r 5*2.-5553

5579

5606

5616

5642

5662

5678

5707

5732

5

s5

DESCRIPTION

Banded silica, 70# and siliceous siderit30#. Banding at 45* to core.

Siderite, dark "brown colour, 30*5 patchesand stringers of massive pyrite.

Silica, light bluish colour. 30# patcheand stringers of siliceous siderite. Nodistinct banding.

Siderite -. light brown colour, siliceouslast foot black siderite. 30J& Inclusionof silica.

t

Banded silica, 50J5 and siliceous siderit*banding at 60J& to core.

Black slatey material, brecciated, with50j5 pyrite matrix.

Banded silica, 50^ and siliceous 'sldorit50J&, banding at 60* to core.

Banded silica, 70^5, and siliceous siderite30#. Banding at 60* to core.

Silica, dark bluish colour with 1055 bandof siliceous siderite. Banding at 60*to core*

Silica, light coioui- with 5J& narrow bandof siliceous siderite and 5# patches andstringers of pyrite. Banding at 70* to (

Silica, dark colour, 5# bands of silicooisiderite and 3# stringers and patches ofpyrite. Banding at 70e to core.

Banded light and dark silica and 5^siliceous siderite, most of which centalmany patches of fine jiagnotito and somechlorite. 9f) pyrite and pyrrhotite.Banding at 70* To core.

Banded silica, dark colour and 30#mirtura of siderite, pyrite and pyrrhotiFew small brecciations. Banding at 70*to core.

Banded light and dark coloured silica wi2C,! bands of pyrite and pyrrhotite.Silica brecciated near pyrite zones. Ba

ANALYSISNO.

J

'l

'*

t

i

ore.

is

ts

;e.

;h

idingat 70* to core.

re*

-

,

.

9

'

BtOt

f

.

*

MM

'

r

-

.

-

U*jV*.it*

IS! f; " ALGOMA ORE PROPERTIES t ,HOLE NO. 1200 SHEET NO. 8

'

"*

5',

5

5

.

DEPTHFROM

5732

5737

40.5

5743

5747

5756

'73.5

'76.5

5796

58E6

5327

TO

5737

5740

5743

5747

5756

5773

5776

5796

5826

5827

5840

1i 1

5

5

5

DESCRIPTION

Banded silica, light green coloured with few bands of light green schist, minor silica, siderite and pyrite.

Massive pyrite and pyrrhotite, 70#; remainder "bands of green schist", banding at 70* 'to core.

Banded light coloured silica, 50J&; very siliceous siderite, 30J&; bands of pyrrhotite, 20J&.

Banded light and dark coloured silica, minor brecciation, few patches of very siliceous siderite.

Brecciated silica, brecciated light and dark coloured silica with 20^ siliceous i

Banded light and dirk coloured silica, 60 very siliceous siderite, 40#; banding irregular, varies from 65* to 80* to cor Minor brecciated zones.

Lias s i ve pyrite and pyrrhotite.

Banded dark coloured silica with 20JS ban of pyrrhotite and 5jJ bands of siliceous siderite. Banding at 708 to core.

*

Banded light and dark coloured silica wi 10^5 bands and irregular stringers of siliceous siderite and 10^ irregular bands and patches of fine grained magnet Banding averages 50* to core. Uinor brecciated zones.

Pale green felsitic material with 15^5 lath shaped crystals of dark green mafic mineral.

Banded silica with minor bands of siliceous siderite and 5jS bands end pate of magnetite. Banding averages 60* to core. Few narrow 'stringers of metadiori

Bottcra of hole, 5840'

Core size: 0-2518 BX 2-318-1)340 AX

ANALYSISNO.

ideri

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t

Is

;h

.te.

103

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- rt.

-

te.

m SiO*

-

MN '-:

x

W:";-,

XV

'..-'-:A " JA

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r

mcrtCOffiHOKgoP*--i.v-

totnatCOCMO

•HCO

• - o.fr0to a4Joofetg;0)

Ht'

. 't *'."

BJM

*'*

* A

XfV CM

rt CM

O

J"

, o5

tt.l

* *

Cs. f)

8 A

* *

co lr\

rt

,

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N J-

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^-

CN7n

co

is R

* *

i t

o

xr\vO

vO

* A

rt CM

O

O

ON ON

O

ON

SO vO

e*. O

* CO rt

lr\\A*

StfirtCM4

fefi

-\r\

tlP^rn0ON

ONN

O

CO O

O

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CM CO

t *

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CS. rt

CM CM

CM

CM CO

vO

m

o

t^*

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CM CM

fi

3-

NO

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J?

rt*

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rt Cs,

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rt

ON \T

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vO

vOfi

fi

fi

tlr\

o

co CN

CN v\

1 t

1

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co\r\

v\

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vO^)

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0

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CN ON

vO

sO

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CM fi*

rt CM

4f-iA

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c*

ONCMa Cs.fi

U\

Sfg*Cs

O

ONON

NO

8*

CM CM* fi

**

C^

rt* ONfi

CMtC

s ON

^

t

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^Ctf 1 COoO

NO

N

NO

g'* CO rt0\r\* X

r\CMvO

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N*J"

rt

S\f\4C

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11CM* Cs.

2.0cA0CN

CNvO

O

ON*CO rtOO*N

Ort

CO Ot

cort•"s

ON*

COfi

g\r\1Xr\*CO

O

N

Ac?oCN

ONN

O

OCM*N

Ort9\O* Hrnj. vO^Cs.* 0r^

\i\

RITN1

8xr\ \r\

ON

OCNON \0

N

w

\v,. v,

\•s

•jxS#,m l

-A no*, l* Jco

)oo* 7

ii i

poor ADSt.14 O

.20 409,89 1140

or* fi

0510 BD33

209130045004303330633143

31483200

too,23 [Jan. l•an. 3• an* Ori -- 7

an. 13

an * 10

Ian* 10 an. CO

an. 30 ôb. l lob. H Pub. G .ob. C•ar.10•or.11

f*';r* 4.r. O

..r. 7

r,ii

r.y l y 11

3136

3120320732045304

3117320332414400 4501 1501 45 D3 4041 5030 5203 5241

53-30 53'JO

55045700

' .'l f )

tortad drilling with *B* Bquljnonti * put* down O' Coaina Cecjontod5

troutola - round olutah rivota otripjxxU Placod "D" Y?odoa (tfl) at C83* fi: ccatmtod hold liolot otuclc ~ Vfaitin/j rpr pnrtj* b j*opairin# holaS until Doo* lot*Stortod to drill with AX2 oqulpaont* Jrlaood *An Hodga (#3)Placed "A" Wadge* (03) Ho Kurtboy Drillinfj until Jan* lot. Jtoaaod by oodno* Lost bit in hola* Plaood Hodô Ti;d) ft roonad by vod(^ Svjivol boad Jamod. llopalrod Jjoad. Plaood t/edâ (^5) !t repaired iwnd. Plaood tfod&o (^0) ft rottcod by wod&a

Draka lovor*lino fro son. Two chifta doloy thowin/t hooa lino*

' " ' (tf?) -Trlod to place uodoa (^0). Plaood pilot wodf.o at 32C4* Lôriootlnfj t?odgo oaitfjht on tfodgo i?0 at 3143* and oho oro d plno.i'lohin^j for wodga* li o OUOOODO* Thauing rroson hoiio lind* Plaood Efoil^g (^9) abovo looos wodô ( i)Q) Han back into old halo. ilocod uo-Jro (^10) at yri^jinal bottoa, riccio a tuck In v/odô Ov at 31BOJarrod on ro-Jo, PulloU rodo tt ooro barrel oiV bit i: S-:oll. i'lacod uod[;o (c!ll) to dofloot nolo aide linn Gonvox iôlo riattonor - liolo j'laood woilr^d (t'li2) i'at naif botiriria in Isoad lirako band broko-VJoldod it at woldod bralco band broUo •Jrolio bond broke Oijain* Uoiat boai'Ins railed.i,roko countcraluil't * 3 days repairing hoad. C:aijôd hond bourlrigbur:;t bit -* I'lnl.od for coi'o ii bit. ?io auocoao. 5 ri Hod out burnt bit. Lro3:o ohouvo w..ool o..iil't.Jto.io atucl: on xiotij-o ot 1)2^1 (i;13) Ai^rll 15*Aj^ril lil. Viorkina on otucU roda (Dit fc o;.oil otucii In cavo alo.-ir; oldo of

ll'ji u lrod ti*a::ii:jlooion : ilrlllod out b*t ^ ol.oll*epitract dopth roachod.C:..a:ij*od clutch - Ccpcpnoo tooting..";;y 14 - !'ny KO Cor.ipa^J

.Or*

i yootac*

!

Iron Silica sulphur Los* ea

'f 71* - 2715•715 - 2717.5W7.5 - 2720

1720 - 2722.5 722.5 - 2725725 - 2727.5

2727.5 - 2730

1742 - 2745755 - 2757.5

2757.5 - 2760

(760 - 2762.5 i2.5 - 2765

765 - 2767.5

J 767.5 - 2770.3775.7 - 2777.5777.5 - 2780.0

2780.0 - 2782.5

1 782.5 - 2785785 - 2787.5

2787.5 - 2790

(790 - 2792.5792.5 - 2795795 - 2797.5

2797-5 - 2300•600 - 2802.51802.5 - 28052805 - 2807.5JC07.5 - 2810

39.1142.32,38.1122.38 33.7034.3040.5142.3044.5345.7445.4441.18 43.4146.1441.1845.3345.5442.6239.7842.6040.7843.3042.8040.5840.3842.3040.8839.48

, 5.608.6.8 -4.909.10

32.7018.6416.603.262.721.661.94 9.98 9.723.64

' 7.503.102.484.809.105.506.405.602.405.107.106.608.008.80

16.8222.4514.605.11 8.324.59

14.0919.8028.9526.0521.34 16.38 23.4416.09-19.4121.1624.2322.2021.3618.6913.4217.0115.5815.7818.8115.7614.5510.03

1 — . , Jl^

1.701.601.761.141.992.202.021.941.341.571.79 1.831.501.861.441.531.781.531.361.781.861.852.011.501.692.052.072.15

25.8027.6725.4615.56 23.5623.5328.2729.6328.9028.77.27.30 23.3721.0524.2525.6527.5623.2029.7628.1027.1029.23'27.0128.8529.9028.4527.7728.0027.95

Pyk

22.1622.5610.625-36

16.608.80

32.2031. b238.0438.303?. 7034.60

3.845.283.48

.105.17

.46

1.371.311.19

.42

.71

.35

14.1314.3612.869.17

12.1419.39

730- 2732.5

(732.5 - 2735 /35 - 2742 745 - 2750 '

2750 - 2755.4 1770.3 - 2775-7

Averogo valves for Deop Hole - Exclusiya of ^yka UatcripJ

41.02 7.55 17.48 1.75 26.72

Avcrtire Vrlues (All Ore Bodies)

Surfac*

Il30o*

40.4?

39.96

40.19

5.92

6.94

5.93I i :.- 1 ..c J r!.

11.63

8.66

9.66t c :; ..\ 'r ; e

2.11

2.03

2.14

Gr:.df

24.59

24.22

25.91

Our Sinter (Iron plus

(TotLl Crft FodioB - L.rface To 2400')

60.6*

27^8* 46.6*47-7* 59.4* 62.8* 64.4* 66.4* 64.9* 56.2* 56.8* 63.4* 57.2* 64.6*

62)2* 57.2* 60.8* 60.2* 61.8* 63.0* 60.0* 59.8*61.4*

57*8*

27.4* 27.8*22.7* 6.4*

19.7* 11.3*

58.36

53.67

52.73

54.24

.- .1 p

. .

. (,J

.;' .

' -'; e

r '-

l.."

'^

pi r

T-1

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k.1

r '

' "( \

f .\

O*

r' '

A

—.

'?

., "

l ,

t S' y

•--X

'A

\x-

X

x^x

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v..., --

Nrt fa 01

'

^

li. v

^- •

-•lZJ

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**-

^^

^

DIAMOND DRILL RECC01*108 8.S.U. 15596, 15597 A 15598

*** .o--••••t'**** v*Departure on DrinVC^aUlUC.,.-——

Bearing.....^

0' 100'-

500'- 6oor"700'-Total Foo

570 oo* D•520-30'""-

-52P-00'""--460-30'""-...37o--30 ,.---32 "00*"

taec ^9'

ip 900' -

—1300'-- —1500'---

27 "23 24'24

FootaFrom

u*r350'— &T-

6^6*— 75T~

7b6'—— 785*-10^'

1172 1

li/y1201*

—1220*-izyu.^ 1i27i;H1287.5*— 1*9**-

P,eTO

f356'3W6^6^

?fKjTOO 1905'

lloj'11 72'117^'1Z01*122U'127075'"

12-/1.5 11287.5*

1491*-as*?*-

FormationCaoing.Hotadiorite.Lamprophyre.itetadiorite.Tuffs intermediate.uotadiorite.Tuff B intonnudiftto to acid*Tuffo tafiio.Tuff 8 acid.Fault tone* Breooiated tuffo cemented with dork groan•chloritic "material.Tuff a fine grained dart gray - Baolc, carbonated.Siderite low grade 2^ pyrite. Tul'f incluoiono. )Siderite, dark gray good grade )Bdeio",dyy.e, fine grained, greenish tlack color. )Siderite, dark gray good grade. )Banded iron formation.Greenstone.

Sample Number

.JJU~34.'43 —

o

6

F/UVlck (9/0

/oc i

TDfy-f

i"v

ALLOWING FOR LOW TAXATION, EXISTING GOVERNMENT10W PRICED ELECTRIC POWER, AND SHORT BAIL HAUL OF 21 MILES TOLAKE 30PWIOR, EXCELLENT HEMATITE IRON ORE CAN BE SICtfJlEDFC'R THE ALGOMA STEEL PLANT AT SAULT ST E. MARIE, ONTARIO, FROMTHE JOSEPHINE IRON MINE (ONTAXIO) KORE CHEAPLY THAN FROM AMERICANIRON MINES, APTKg PAYING ABOUT SO* HIGHER FREIGHT RATES TO TRXALGONA CENTRAL RAXLVAT COMPANY, THAN THOSE PAID ON AMERICANXfcON ORE. .

1. Th* Josephine Iron Mine is located on a spur about one-third of a mile long, extending from Mile 20 on the Algoma Central and Hudson Bay Railway* and is about 21 miles from the Railway's dock at Michipicoten Harbour, on the Lake Superior. It is about 120 miles by boat froa Michipicoten Harbour to Sault Ste.Marie i and about 200 miles by boat to Port Arthur. The distance to Sault Ste.Marie from the mine by the all-rail route is about 170 miles. The Steel Plant at Sault Ste.Marie could smelt about 1,000.000 tons of iron ore annually.

2* The Josephine property comprises three mining claims containing about 183 acres and includes over one mile of the iron range.

3. Prior to the Diamond Drilling shown on the blue print, Mr. F.S.Wiley of Port Arthur, drilled four holes] and his report to Mr. Alois Goets, one of the owners, was that drill hole No.l struck soft red ore at a .depthof 42 feet, and contin ued in soft ore for 45 feet} and froa the 85-foot level to the 123-foot level, it passed through 30 feet of hard and soft ore, partly mixed with quarts. Drill hole No.2 passed through chiefly ore ar.d quarts and some mixed ore a distance of appArantly one hundred and eleven feet to the bottom of the hole. Another drill hole was put down apparently in the vicinity of Northern Island, where considerable rich float ore was dix covered and about 73 feet of soft ore was cut through* The hard oro assayed about 60JC and the soft ore 40JC to 4SJC iron. The tonnage proven up bv, tffri* diaaopd,

not included in the estimate*^ tonnage hereinafter.t.he not en trc(

LB 2Ajia^t^ blue print.______ __ _.__________itej-^—^————-^-—^-^.

the Ontario Government ?Report of 1901 would indicate that the Superintendent of the diamond drilling operations was of the opinion that the ore .body averaged about 50 feet in width, *nd extended a distance of about 3/000 feet. Mr.A.R.Willmott Consulting Engineer Mining Geologist for the Lake superior Corporation after the first 21 drill /holes were put down, estimated that such diamond drilling had proven up about 500,000 tons of iron ore, averaging about 50 per cent iron, and .04 per cent phosphorus and interested the Lake Sapwrior Corporation in taking an option on the said property in 1910. Five more drill .holes were then put down, bringing tho total footage up to 10,406 feet, and proving jip a total tonnage of 2,250,000 tons of hematite iron ore} or, if all ore below 50* were excluded, a tonnage of 1,300,000 tons of iron ore, assaying from 509T to 63jf iron, in the short distance df about 1,000 feet of an iron range which extends over a distance of one mile on the said property. The drilling also proves that the iron ore bady extends downward to a depth of at leaat 1,350 feet.

- /-. .4. In 1914* the sivid Lake Superior Corporation took a twenty fly* year lease en the t aid property and planned to a ink a sh*ft 900 feet in depth mad drift a distance of 1200 ftat and nine the ore f or use at the furnaces of the algona Steel Comp any Limited, at Sault Ste.Marie Ontario* In 1914* the price of iron ore F*O.B* at Lake Xrie ports vas only l.88 per ton add there was no Government bounty at all. The present price is fro* 14.40 to 14*80 per ton; and there would be a

^Provincial Government bounty of about 25 cents per ton. The Oreat Vat broke out in August 19m i and the Lake Superior corporation cancelled its lease on the 10th May* 1915.

5. The Oeological Surrey of the Dominion Depf-tment of Mines in 1926 published a very comprehensive report ta the Michipi coten Iron Ranges. The following quotations are taken from Page 122 thereof* regarding the Josephine Iron Mine.

•The drill holes define a vertical sheet of ore ci oval or kite-shaped outline. 1*000 feet in maximum length) 1*350 feet in maximum depth* and 5 to 125 feet thick*. Of the total thickness only 5 to 50 feet is ore. It seems.however, that the lover liaites could be extended considerably, if deep holes like number 51 were drilled on either side of it.

n lf all ore carrying 30 per cent metallic ironbe taken into consideration* the oval sheet defined by the drill-holes is estimated to contain 2*250*000 tons. If ore carrying less than 50JC is excluded* the tonnage vould be reduced dewn to 1*300*000 tons'*.

6. In 1916* the Algoma Power Company Limited supplied power to the Helen Ir^:*. Mine at 132.00 por R.P. net at the mine. The Power Line is about three miles west of the Josephine* and ample power is available for a 24-hour service at about 140 or ISO per H.P. or less.

7. In 1918* Captain Fred Rodds* who opened up and operated the Atikokan Iron Mine* estimated that the cant of sinking a 400-foot working shaft* and equpping the same to mine 600 tons per day to be 1200.OOOi and the cost of mining the ore to be 11.75 per ton 7,0.B, the railway cars at the mine. During the last five years tha cost of mining iron ore in the shaft mines of Michigan has teen reduced by 50n cents per ton. Iron ore from the Josephine Mine should be mined at a profit of about 11.50 per ton and 11.90 per ton cheaper than sinterad ore produced from the (Hew) Helena eee Report of Ixn Ove Committee Page 7* In 1914* it cost 11.90 per ton to plrce Helen iron ore P.O.B. cars at the Helen Iron Mine (excluding 30 cents per ton for sinking f tied) i see Report of Iron Ore Committee* 1923* pag* 156. The cost of Josephine iroa ore F.O.6. cars at the Josephine Iron Mine should not exceed 31.75 per ton* taking as a basis the estimated costs by Captain Fred Rodds and actual costs in the

aihaft mines.

e.8. During the l** t five years, including 1927, the priceof iron ore has been 14.25 at take Sri* port*. During that periodthe average profit per ton to the Michigan operator* was only27 tents per ton, according to Skill ingi( Mining Review of June2nd, me pat* 3. ;;

Cast Of mining, including depreciation t/ overhead per ton 12,2564

Royalties and taxes per ton .4351Marketing and transportation to Lake Brie ports 1,4582Profit par ton ' *27el

Price of *3* iron ore per ton at take Erie ports 14.4398

In the State of Minnesota, as per the Report of the Minnesota Tax Commission, at pages 14 and 15, the costs and profits are set forth as follows t

Mining including depreciation b oY*rhead per ton 11.071Royalties and Taxes per ton 1.146Total cost F.O.B. the Mines per ton $2.217Transportation (f Marketing to Lake Erie ports per ten 1.888Profit per ton for iron ore averaging aboaut 51JC .241

Price of 51* iron ore, per ton at Lake Erie Ports 14.346

For the purposes of State and Miniopaltaxation, the iron ore is valued as being vorth in the 'round 50 cents per ton in the State of Michigan j and at 11.00 per ton in the State of Minnesota.U.S.A. The Report of the Bureau of Mines (U.S.A.) shovs that the total underground expense of mining iron oro from an iron nine at {shpeaing, 16 Miles Vest of Marquotte, is only 11.412 per ton in 1928. See Skillings Mining Review, June 22, 1929, page 3.

9. Vith cheap hvro-electric power, and short rail haul, the iron ore from the Josephine should be ained feoro cheaply than the iron ore from tb shaft nines of the State of Michigan, at a profit of about $1.00 per ton as follows t There would be a saving of about 25 cents per ton in srespect of royalties and taxes which with the Ontario bounty of about 27 cents per ton, and the American profit of 27 cents per tOn, plus 25 cents increaoe in price, would aggregate about 11.00 ' per ton.

10. between 1897 and 1911, the Dominion Government paid bountiee on pig iron and steel products equivalent to e fcmmty of about 11.59 per ton, on iron ore smelted in Canada* The Duncan Commission that enquired into the claims of the - Maritime Provinces, srecommended the renewal of the iron siU steel bountiee. The Dominion Government may renew these bounties, or grant bounties on coal and iron ore used in producing pig iron and steel products i and it is possible that the Province of Ontario may increase the Ontario Bounty* Even now, the Dominion Oivernment has authority to enter into contracts with coking companies to pay the equivalent of 11.00

ton on Canadian .coal coked in Canada for domettle purpose**i,* ' ' .

11* It l* ettlaated that tho iron oro referred in the Jtatt Of Michigan will only last 13 yaara. The iron or* ahoold be mined froa the Joatphin* at a aubatantial profit of 11*00 per ton. •TO** without any additional Vountie*. Boaidoa thia. the operation of the Josephine Iron Mint vould nean that ita oro would bo shipped over the Algoma Central Railway, and the price paid for shipment would add to the receipts of that railway, which is really a subsidiary of the Laka Superior Corporation i whereas Michigan o?re. which is in some cases shipped to Sault Sto.Maria over an all-rail route, contributes nothing to tha revenue of the Algoma Central Railway.

DATED this 12th day of Augast, A.D.1929.

x.t

lr

ON THE JOSEHm-TE IRON MIKE .J

'— Location and Extent——

The Josephine Mine is located on a short spur of the Algoma Central and Hudson

Bay Railway (The rails fron this spur were renovod during the war) about 170 miles north

from Sault St**. Kario, and abo\i\ 10 miles from Michipicoten harbor, Lake Superior,

in the District of Algoma, Canada, and consists of three patented claims contain

ing 183 acres extending along the iron range for over onemile.

Title is guaranteed by the province of Ontario.

———— GENERAL DfFORI/ATIOH ———

Mostly all of the diamond drilling has been done on Y451, which contains 75 acres,

the greater part is covered with the water of Red or Parks Lake which contains

about 100 acres. It empties by a small areek having a fall of about 100 ft. into

Goetz Lake, about 1300 ft. to westward. The depth is fron 45 ft. to 66 ft. except

a short stretch in the middle near a small island. The sounding was a hurried

one, perhaps a more careful survey might reveal a continuous deep channel thru

the lake. On the southwestern shore of red lake on Y451, large and small boulders

of red hematite were strewn along the shore, none of them are seen now probably

having been removed by the Clergue people for smelting purposes. There is but

little doubt that this boulder ore was scooped out by glacial action from the

basin now occupied by Red Lake.

The Clergue people had started a shaft on the southwestern end of Y451. intending to

mine the ore under the lake, but it might be advisable to drain the lake. It would

be safer to mine the ore, the lake basin could also be inspected for siderite, ioft

and hard red hematite of the boulder class. It would not take a large body of such

ore to pay for draining the lake.

The Southern shore is level for about 100 ft. inland where almost vertical bluffs and

steep hill* riae to a height of 80 ft. or nore, consisting of ferruginious lime

stone, small patches of iron rocks and schist. A graded road bed for a railway ex

tends around Red Lake to the southeast end, and from this point a good trail leads

northerly around the east shore to the easterly running rxiijni valley mentioned herein.

The north shore consists mainly of itery steep hills of slaty schist, but close to

the north shore and running parallel to it, is a string of small rocky islands of

greenschist* The0e, together with the buckling of the southern rocks evidently

contributed to the shattering of the iron rocks, thereby aiding their destruction by

weathering and so forming the lake basin ttnd also enriching the iron rocks below.

A diabase dyke strikes northwesterly thru the east shore of Goetz Lake, intersecting

another dyke running northeasterly close to the north shore of Red Lake, which makes

it clear from whence the cruching force came which in all probability shattered tho

pinched in iron rocks to a great depth, consequently it may reasonably be assumed that

the iron formation goes. The dip of the strata on the surface is generally steep

to northward, but in drill hole 51, it swings slightly southward.

Y452, adjoins on the east, and contains 5? acres, and embraces a small part of Red

Lake. Tho strike of the iron formation heads for the wide drift covered valley ex

tending eastward from the lake and not much of the iron rocks are seen for some dis

tance inland, but hole No.8 shows that they lie buried under the *rift, from which

they rise into a steep high hill, and at the line between Y452-53, they are over

600 ft. wide, continuing that width thru Y453 with an almost vertical dip. The

valley spoken of extends northeasterly along the range on the north side, bounded

by high steep rldgee of slaty schist trending in the same direction. Along the

touthern side of the iron rocks, on top of the high hill boulders of siderite were

seen when staking the claims outcrops of siderite were also seen on the shore of Red

Lake, and on the eastern boundary of Y453. Recent exploration has disclosed a body

of siderite having an average width of 50 ft. and runs from the eastern boundary of

Y453 to the shore of Red Lake, into which it dips, a distance of about 2900 ft, with

an average height of about 200 ft. to lake level. Probably many tons can be quarried.

Draining the lake, which near here has a depth of 66 ft. might give an additional

large tonnage for quarring* At the lake schist intervenes between the siderite and-f-

iron rocks which at this point lie buried beneath the drift covered valley. Apparently

an offshoot of buried siderite extends eastward in the valley, as indicated by boulders

of siderite and hematite lying scattered in low ground about 600 ft. east from the lake

and at this point about 200 ft. north from the iron rocks and main body of siderite.

On the eastern end of the siderite on T[453, a 10 ft wide off-shoot runs southwesterly

for about 800 ft, where it sinks into low ground. This part is very pyritic. Schist-f-

intervenes between this offshoot and the main body of siderite.-f- Reported by George Me Cullough who did some work on the property in 1930,

A shaft had beenstarted by the Clergue people, on this claim near the eastern shore

of Red Lake, which no doubt was to be ased in mining the eastern ore under the lake.

Y453, adjoins on the east, containing 51 acres, on the northeastern side is a broken

basin across a part of the range, but the shattering and erosion along the eastern part

of the range on the two claims has been less severe then to westward but the iron rocks

apparantly are much wider from which to draw ferruginous material, so that red hematite

may exist in the valley running along on the north side of the iron rocks.

l- Several places on this claim, in the valley show some outcrops of bonded hematite and

hematite pebbles cemented with hematite.-f- AB shown on a plan which fihould accompany

this report.

The drill plane furnished to us by the Algoma Steel Corporation in 1914 shows that

all material below 45# iron was classed as banded, so one might assume that only ore

running about 50# iron was included in their estimate of 1.250.000 tons of ore. KTien

M. A. Goetz assembled the two drill plans into one complete plan in Aug. 8, 1921, he

shaded the parts marked as banded in holes 15, 17 along with the part marked as ore,

thinking that the whold might now be taken as all ore. The undersigned had an

opportunity to examine the frillers 1901, original drill record book for holes No. l

to 10 and at the same time examined.all of the drill cores from holes No. l to 21 in

their undisturbed core boxes, which had been left in buildings at the Joephine Mine,

when the Clergue in erests abruptly quit drilling, and shaft sinking, deserted the premises

which they were trying to wrongfully acquire under the Algona Central and Hudson Bay

Railway land grant, and left things open for anyone that cared to look around. Core

boxes for hole No. 2-4-6-7- as well as some other core boxes contained much material

rated on the drill plans furnished tc us, as banded, which might now be classed as

ore. The drill records for holes 6-8-9 by Bush and Peterson, also showed beds of siderite,

the drill plans furnished us do not show it. We now know that the siderite lens dips into

Red Lake,-j|- and crops out agin about 60 ft. west of boundary line on Y451, on the

southern shore of Red Lalce*^- Some credence might be given as to the correctiess of the

drill records of 1901, by J. T. Bush and Adolph Peterson, drill crew foremen. At

an earlier date H. A. Wiley had an option on the property and while drilling on, and

in the lake near Jasper Island, on Y451, the writer saw a core box containing many contin-

ious feet of a red powdery material assaying 40 and 45# iron. lir. ^iley also fur

nished a email plan showing the location of the holes drilled, but no information

was given from which hole the soft ore came from. No mention is made on the drill plani

of this soft ore, or show two vertical holes in the places ae shown on Wiley's plan.

Probably the Algoma Steel Corporation did not get all the data prior to 1913,

obtained by the Clergue interests.

Holes 12-19, Just across the west boundary of Y451, at a depth of about 600 ft shows

good hematite, 20 ft. 45 ft. in width, indicating that ore exists at the western end of

the lake. Hole W. 2 angle 45 degrees, depth 111 ft. Hole W.3 angle 45 degrees, depth

41 ft. Hole No. 4 vert. 294 ft. Hole No. 5 angle 50 degrees depth t* 133 ft. Hole No.14

angle 55 degrees, true vert, depth to bottom of banded about 200 ft. cutting 3 narrow

-f- Sported by George Me Cullough who did some work on the property in 1930.-f-

beds of ore. Bole W. 1. angle 45 degrees starts on Southern Bide of iron rocks, soon

entering what the drill plans show schist. Judging from the oroless manner things were

done at that time this echist might hare been aiderite, also the material in drill hole

21 classed as pyrites chert, may have been pyritic siderite as hole 21 le about 400 ft.

east of the siderite outcrop on the southwestern shore of ^ed Lake. In view of the

ore shrwn in holes 12-19, this drilling caanot be accepted that no hematite exists in

the western area of the lake, on Y451. More careful and deeper drilling may give good

results. The lake area east of hole 18 holds out fairly good prospects of finding ore

there, as well as in the eastern Talley. The hematite ore apparently lie* south of and

also inside the iron rocks, indicating that they were not all derived from the siderites

on the south, some of which may still exist in the lake basin.

The Algoma Steel Corporation, who drilled the area between holes 18-53, in years 191314

figured that there were 1.250.000. tons of a high grade ore shown. They took a lease on

the property and paid ^2000. advance royalty thoron. A few weeks later war came and the

lease was cancelled owing to financial stringency. In mining this small areal of

about 850 ft, along the range, additional tonnages are apt to be found deeper down then

the tonnage was figured. Besides the high grade hematite ore there is a large tonnage

of hematite averaging about 40/* iron. Surface siderite samples taken from the lake shore

to the east boundary of Y453, averages as follows:

Natural ore. Fe MN P. S. Afl. Sio2 A1203 CaO MgO 36-54 2.13 .017 3.44 .11 9.27 2.31 2.72 4.53

Loss by Ignition 27.73

After Ignition, Fe Mn. P. S. As. Sio2 A1203 CaO MgO50-56 2.94 .023 .15? T. 18.83 3,20 3.77 6,27

The ore appears to be about self fluxing. The dry porous sintered ore would require

less fuel for smelting and the manganese content is of some importance to the steel

industry and gives the ore an additional value.

A careful scrutiny of the t±x drill plans, the lake basin the eastern valley and the

general geological features can leave but little doubt that this property merits a more

careful exploration, wiich in all probability will give rich results in hematite and

siderite ores, over *nO above the data now at hand.

Yours truly,

Alois Goetz

Sault Ste. Marie, Mich. Feb. 4, 1931.

42C02SE8779 0019 CORBIERE 030

IK tract fro* Annual Report for 1941ef

___SfSRRITT OCR DON MINES L IMITED

February S, 1948.

Joaephine stLae

A number of iron properties la the Michipicoten Area, including the Old Josephine Mine, were taken up in association with the *robieher Xxplor ation Company Limited. A total of 6,500* of diamond drilling vas done on the Josephine property in an endeavour to check up on the results which had been obtained in previous drilling campaigns. A detailed geological study of the property was also carried out. The results of the diamond drilling together with the da 11* obtained from the geological studies were very encouraging and tended to confirm the tonnage eaticstea which had been based upon the previous drilling. A very substantial tonnage of quartz-hematite breccia, averaging iron, aa well as a smaller tonnage of good grade hematite averaging about iron, was indioated by the diamond drilling. Results of mill test work carried out in our laboratory, indioated that a high grade hematite concentrate can be made from the quartz-hematite breccia.

On the strength of these results, a decision was mr.de to proceed with the underground exploration of the Josephine deposit. Camp e were erected and a mining plant was purchased and at the end of the year was in process of installation. It is proposed to sink a ehaft to a depth of between 1,000 and 1,100 feet and to explore the orebody on the 565* and 1015' levels. A pilot mill will be erected while the shaft la being sunk in order that the concentration of the quartz-hematite breccia can be tried out under eonditiona approximating commercial operation.

It is hoped that the shaft will be completed in time topermit some of the high grade banatite to be mined and shipped before the end of the 1942 season. Actual commercial production however could not be expected until the start of the 1943 ore shipping season.

It is also planned to diamond drill SOB* of the sideritedeposits which have been exposed by surface trenching on the other properties which we are holding in the area. If a substantial tonnage of siderite can be proven up on these properties, there is no reason why a profitable sintering operation, similar to the operation at the Helen Mine of the Algoma Steel Corporation, cannot be developed.

Mr. Thayer Lindsley, President, Miohlpicoten Iron Minos Limited, 25 King Street V/est, Toronto, Ontario.

Pour Mr. Lindsley,

In response to your roquo.'it for a further report on the Joseph ino Mine, giving details an to tho proposed production facilities and estimates of operating costa, ate., the follov/ing is subniitted for your consideration.

As the location, history, prelininary development and ^oology of tho Josephine Hine ere covered in roy previous report, dated January 20th, 1943, it la considered unnecessary to repeat those sections.

)

iJince tho beginning of this year a total of about 900 foot of drifting has been completed on tho 6th level. A number of lateral diamond drill holes havo been drilled on this 6th level drift to crosscut the orebody. One boxholo wao out on tho 6th lovel and a uruall otope started to produce lurap oro for teat sbipmenta. A second deep drill holo, JU-9, v/as drilled from tho 6th level station to cut the orebody ut a vortical depth of over 600 feat below the 6th lovel horizon. On the 5th loval tho raain crosscut tvas driven out throush the orebody and drifting in tho footwall, parallel to the orebody, is no?/ in progress* Two lateral diationd drill holes have been put out from the 5th level drifts to crosscut the orebody.

Tile tunnel to divert the nain feeder of Parka Lako has been completed, BO that this diversion ia nov/ ready to take care of the spring run-off. A ditch alon;; tho south side of tho Parks Lake basin has also been completed to take care of moat of tho remaining inflow. The diamond drill holea undurcrou.v.1 are bein^, allowed to run at capacity in order to drain tho orebody na rapidly as possible. The flow in no ra e of those holes ia already slackening off'.

ndicated Oro

The following ostiiaato of ore reserves is bused upon tho data obtained f ran diamond drill holes, both surface and underground. On account of tlio incomplete records available, holes drilled prior to 1941 are only used in tho osti.-y.it ion of possible ore. ^tensions 50 foot above the first level horizon and 50 feet below tho 6th level horizon have been assumed. Tho aoconpanyin^', vertical section J-25 and horizontal sections J-27. J-28 and J^29 illustrate tho areas used in calculating oro reserves.

-2-

A factor of 10 ou. ft. per Rrosa ton was used in tho calculations in ordor to make allowance for the porosity of the oro.

Vert i eal Rango TonnageBlock

A

B

C

D

Total

Horizon

4850

4800

4485

4050

4850

to

to

to

to

to

4800

4485

4050

4000

4000

( -'-•— - " — .—— . j r* "î™ i n t*t v f^ d i fj,XU.3tJ UUU3J ft

44,

535,

957,94,

1,630,

000

000

000

000

000

51

51

515451

Fo

.17

.47

.57

.34

.85

^ SiO^

13.

21.

18.

12.

19.

9518

92

51

16

1-30

ii0

1

.197

.522

.236

.236

.244

Complete analyses are not available for all tho drill hole intersections in the upper horizons, consequently a complete average analysis onnnot bo calculated for the above oro reserves. Tho following, however, lo an average analysis of a nunber of drill hole intersections and it is believed that it can safely be taken aa representative of tho ore reserve aa a whole.

0.025 O.Cbl 0.24 C.12

't. AloO* j ;.!fiO f. Igq. Loss

1.90 0.12 1.6?

Feasible oro is ostinattjd at a total of 2,000,000 tons with approximately tVe sarao gre-.do an the ubovu. The oroa ooverod by this cutinite is shovm on the aoconpanying vertical longitudinal flection J-25. This estimate in based upon tho results obtained in tv/elvo diamond drill }ioloa vrtiich intersected tho orebody within the outlines of the area shovm. It la believed that additional oro will be located in tho area between GootJ.ons L7. and LM, tho 4^00 horizon. {Uoe lection J-25).

Go no e ii t ra t lo ri

yurthor nill teata ôro carried out on mill feed taken from different placeri on the 6th lovol ar.d T.IMO froa the 5th level r.kiin oroascut. In seêral, the rasulta of tnoue tests confirmed the belief that a holtite ooncentrute \v ith an iron content of oO'^ und a silica content of approximately 9*5/* con be made by straight jibing. Tho ratio of concentration v/ould be 1.5 to l a i: d tho overall iron recovery v.'ould be approximately 80?j. Copies of the reports covering these siill teats aro appended*

Throe ccrloacls of open hearth lu.-np ora v/ero sorted out by hand cobbing. One of these carloads v/aa shipped to the AL~o:â Jtoel plant at Sault Sto. i-brio, Out. and the other tvra were shipped to the Dominion oteel and Coal Company's plant at 3ydney, 11.3. Tho analyses of these three oarloado \vsro as follows:-

Carlond

Algoma

Dosoo

Dosoo

-3-JO. 1. As 1, J ft, j, j jg^O j. CnO ^/i Lo s g

65.29 ;.55 *010 .025 .0^1 .10 Tr. Tr.

61.64 7.72 .040 .015 .0?

62.64 7.08

2.18 Tr.

Proposed Product ion Layout

In order to operate the Josephine Mine ooononioally, it would "bo necessary to reduce the silica content of the oro and to eliminate the aulphur fron the pyritiforoua hematite, v;hich occurs in certain sections of the orebody. The pilot rail l operation has shown that the silica content of the ore can bo reduced "by straight jibing. Wintering tests made on the jig conoontrotos have shown that a a inter of very good quality can bo made, and that any aulphur and arsenic con be satisfactorily eliminated. It nan also been demonstrated that by hand cobbing a very desirable open hearth lunp oro can be sorted out. This lunp ore has been tested in the open hearth furnaces of two different* steel plants v/ith very satisfactory results. In addition, none of the sinter, which was produced in the sintering testa run on the jift conoentrutos, was tried out as lunp ore in one of the open hourth furnaces at the Algona Jtuel plant. As a result of this test, the y. l go ma dtool Company's technicians are satisfied that the Josephine sinter would make a vory satisfactory open hearth lur.ip ore.

It ia recomendecl that the Josephine l.'.ine should be brought into production as quickly aa possible r*-? n oouroe of open hearth lump and sinter, v/hich would bo the equivalent of open hearth luirp. The necessary plant v/ould consist of a crushing and screening plant, with facilities for hand cobbing of open hearth luap, a j ir, plant and a sintev plant. Vt'ith the exception of a

Crusher, all the equipment end construction r.atoriul requiredfor this plant can be obtained in Canada. The I lord b erg Conoany have adviaod that they could nako delivery of a Synona Crua'o.or in 90 dnys frora Mil\vuukoo, on either an AA l or an AA2X. priority. copy of the proposed flow sheet accompanies this roport.

-' iniated Product ioi ^e Schedule

It is estimated that operating on a scale of 75o tons of ore per day a total of 1^0 tons of open hearth lump ur.d 550 tons of sinter could bo produced daily. If desired, it io estimated that upproxi^-itely '/O tons per day of plus 1/2" Jig concentrate could bo . sorooned out for Dh.ip~.ent either as blast furnace feed or for lining of open hearth furnaces. It is considered probable, however, that onoe the olntor plant was conploted and in operation it v/ould bo advisable to ninter oil the jits concentrate.

The plant vrould be operated on nn all year round schedule, QO that the yearly output should arnount to approximately 54,000 gross tons of open hearth lump ore and lc'6,000 tons of sinter, v/.iich v/ould bo tho equivalent of open hoorth lunp ore. It v.-ould take approxiirmte- ly five lannths to cet "the nine in shape for production. Production

-4-

could then be started on a scale of about 250 tons of oro per day and stepped up ovor a three to four month period to tho objootive of 750 tons of oro per day. This five nonths period of nine development would allow ample tino In which to complete the surface plant, with the exception of tho sinter plant. Tbe sinter plant would probably require a total of eight nonths to complete,' so that it should ba in operation by the tine tho nine attained its full scale output.

Assuming that this programme got started by June 1st,1943, tho 1945 output would ba estimated at 4,500 tons of open hearth

,. lurap oro and 2,000 tons of plus 1/2" ji;^ concentrate. The 1944 || output would be estiraatod at 50,000 tons of open hoarth lunp ore

and 100,000 tons of sinter. The 1945 output would be estimated at*B 54,000 tons of open hearth lump ore and 126,000 tons of sinter.

.ii'stinated Capitol Costs

oururaary

•;! Crushing plant #88,100Mill 79*600Winter Plant 308,300 Underground Machinery and Equipment 93*3^0Underground Development 130,300Surface Buildings and Equipment 218,900.Miscellaneous 52,8002nsinoering 26,OOP

Total 0997*000

V.'orkin,^ Capital required 5300,010

Tho A l go rsa Central Railway oro prepared to provide stockpiling and loading facilitios at Michipicoten Harbour, provided they are given a satisfactory ^uarantoo, either by ourselves or by the Dominion Government, that sufficient tonr.e.^o \;ill bo shipped to protect them on thoir investment. Tho cost of those facilities is oatinated by tho A.C.R. enginoers at 3205*000. This r.:atter is to be taken up with tho Dominion Goverrucervt without delay.

Plant

Building JlO.OOOP.oss Feeder 1,800l cloublo ooo:; screen 2,500i? s.inr;:lo cioci: soreens 51000i-'ioJ'.inv, bolt 2,000/J:io oro conveyor 4,000A-: o d conveyor to Symons 1,000Discharge conveyor fron oynons 2,OCOKyturn oonvoyor to 3y."ons 2,000Screen discharge conveyor 500 4' ,v;yr;ori3 standard cruuhor v/ith aptro spindle,

head, bowl and eccentrics 30j000

—5—

JLa^ icont.)

Crnv/1 nnd chain block vi*000Booster punp for wish viator 800Dev;atoring installation, Akins Classifier ton hur.d) GOO

Conveyor Galleriesriping, chutos and lightingElectricalCur spotter

Contingencies 1

Total

4,0005,5008,0001,200

080,1008.000

088,100

Datails

Ore Bin2 fead conveyors, 6 i^oed chutes, Heaves drivo32 V;ood J is Units

l Concentrate screenboootsr pump and pipo for j ip, v/ator?nilin.'j;o conveyorsTailing o conveyor snllerioaCoarsa Concentrate conveyor and fralleryCoai'DO Concentrate binFiii3 concentrato conveyor galleries"i'lne concentrate conveyors/.Itorationa to existing nill building•llootricalMiaoellaneoxjs pipingTcxilliL?. viator pi^e, 12" v;ood ntnvo•'.ill water supply punp•'•':111 v/ator :mpply pur.p houseMill v/atar pipe lino and trestlo, 8" v/ood stuve

pipe V.'ator tank

Continsenoiea

Total

l,3oo12,000

4,0001,5001,7003,6004,0002,000

30010,000

9,000 5,coo2,0001,500L', 000 2,500 1,500

2,5CO 2.000

7,200

;.'iin.t,or- Plarit

.jccavntion arid foundations, J i ri t e r b u i l d i n?, fi r.d fan i i o u 3 eointor r-ftchino• 'otora and installationConveyor oOoke orushin:', layout

515,600 69,000 92.0CO 10,100 25,000 20,000

-6-

Sinter Plant Dotailo (cont.)

Charge binsLightingPovror v/lringAir and vator lineaFuel oil tank and linea (for ignition)Stack and fluoo frora fan houseLoading facilities

Contingencies

Total

Undor^round jtochinory ^and ICquipmont ^Details

Underground cruahor inntalled 1 30" r. 4 2 M Jaw) Underground locomotive, comploto with charging

unit and threo battorios 12 Granby typo corn, 85 ou.ft. capacity 2 skipsRook drills, l? D. 89*3, 6 D . 7? '3, 6 R. 104' 3 itliao. U.G. equipuarit, coluruis, arna, oto. 4- tugsoz" hoists 2 double drum scraper hoists 2 hoifltiae ropos, 1,500 - 1-1/8 "

Contirxgenoies

Total

Underground Day elopT(ontDot p

shaft sinking v: ^100 por ft. 7th level station, 60' fc 3100 por ft. Skip loading station complete Crushor station complete without crushar oorvice drifts and crosscuts, 1000' ^ C^O per ft. 23 "boxholes O y675 ea* 1,400* raises u ^15 Ore and vmste passes, 550' ^ -JHO Sunp on 6th level Charging station excavation on 6th

ContinRonoies

Tot.-il

J21.7002,0004,200

6003,000

12,50051000,

0280,70028.100

, 800

20,20010,800

2,6008,0002,0002,0001,7001.000

134,800P.jQO

^15,000 6,000

10,00020,00020,00015,50021,0007,0002,0002.000

^113,500

-7-

Sjiirf ace Buildings and JSquipment Deta.ils

Headframa and Coarse Ore Bin and Wast* Bin 421,000MOT ing present hoist and hoist house 6,500Office Building with single staff quarters 15,000 2rtension and completion of present change house 5,000Two new bunkhouses 12,000Completion of present bunkhouses 1,000Addition to heating plant 3,000Substation and transformers 35,000 Addition to compressor house., 600 cu.ft. aa o hine 5,000Fire protection 5,000Outside pipe lines and water supply 5,000Hospital 5,000Ctorage 2,000Employees housing 75,000Additional dump truck 3 500

4199,000 Contingencies 10J 19.900

Total 4218,900

Mi s o e 1 1 a ne ou s

Railroad trackage (A. C. R. estimate) 4*5,000Conatruotlon tools 5*000Rental of dragline during construction 2,200

Total 152,800

426,000

Estimated Operating Costa apd Profits

Sumnary of Daily Operating Costa

Mining - 750 tons c 41.47 P*r ton 41*102.50Sorting - 150 tons t 40.70 per ton 105.00Crushing - 600 tons t 40*23 per ton 138.00Milling - 600 tons c 40.25 per ton 150.00Sintering - 350 ';ons c 40.99 par ton 346.50Mine General Expense - 750 tons c 40.25 per ton 18?. 50 Toronto Office expense - 750 tons w 40.05 per ton 37*30

Total operating cost per day 42,067.00

-8-

Satiiaatea Value of Products

A price of 11? Canadian, per unit of iron, 7.C.B. Josephin9 has been assumed for both the open hearth lump end •inter. The iron eontent of the open hearth lump la taken aa ( 2j* and the iron aontent of the sinter as eO*.

Daily Output

150 tons open hearth lump t 16.82 per ten U, 023*00 350 tons sinter b |6*60 per ton 2.310*00

Total Yalue of product per day 43i333*00

Estimated daily operating profit exclusive ofOnttrio Bounty 1,266.00

" yearly " " " " 4455,760.00

" " Ontario Bounty (if obtained) 4216,000.00

Negotiations with the Ontario Government with regard to thia bounty hare already been started.

De t a i Is of J^P ere t infi Co s t Est ima te s

Mining

System - shrinkage stoping with haulage levels at 300' intervals. Intermediate levels 150' *-ove the haulage levels. Boxholes at 30' intervals in haulage drifts. Raises driven on 50 slope between levels, at approximately 210' intervals.

The development for thia shrinkage stoping system would fit in equally well with the Sherritt Gordon systea of cublevel stoping. It is possible that the Sherritt Gordon system night be used in parts of the orebody, if ore and wall conditions were found to be suitable.

Development coste are based on a typical block opened up on the 6th level* This block has a length of 700* with an average width of l?', and woftJLd make 1,320 gross tons of ore per vertical foot. On this basis, a block 300' high would contain 396,000 gross tons.

Developaent

Haulage drift - 700' C 430 per foot 421,000Service drift and crosscuts - 900' C |20 per foot 418,000Boxholes - 24 t |6?5 each 16,200Raises - 1400' C |15 per foot 21,000Proportion of shaft and stations 20,000Proportion of main crosscuts 10,000 Proportion of Crusher Station and loading pocket 10,000Miscellaneous development lOfOCO

Total 4126,200

-9-

Dtvelopmint *o*t p*r ton

Underground Exploration (Diamond Drilling)

Stoping

Direct Labor JO.2?Explosives 0.09Drills and drill steel 0.0&Compressed air 0*05Miscellaneous supplies, eto. 0.05Underground general expense 0.10

Loading and traming Underground crushing Hoisting

Total cost of ore in bin on surface

Crushing and Sorting

Assumptions - 750 t,ons per day hoisted150 " -w gorted out as luap600 " " crushed

Sorting out lump

Screening37mons crushingConveyingPowerLaborSupervision

Total Crushing

Milling;

Water and reclamationPowerRepairsLabor and supervisionTailings disposalExperimentalHeat, Light and miscellaneousMill general expense

Total milling

Sintering

LaborOil fuel for ignitionCoke fuel ( &1* coke breeze)PowerRepairsGeneral expenses

Total Sintering

Jo.520.15

0.660.200.020.12

U.47

JO.70 per ton aorted

0.0330.0450.0110.0560.0780.005

10.228 per ton crushed

O. 030.0250.530.0?0.020.020.010.045

250 per ton nilled

jo. 160.14 0.40 0.12 0,0? 6.13

JO.99 per ton sintered

-10-

Mine ene^l experis^es (based on Sherritt Gordon) JO. 25 ptr tonmined

Toronto office expenses (based on Sherritt Gordon) 10*05 " "

JUtiieated Operating Grew

The necessary supervisory staff are already on the job at Josephine lil ne. The preparatory mine development work oan be done by a contracting outfit which is finishing off a shaft sinking contract at the Sherrltt Gordon Hine in Hay. An additional 60 men orer and abore the present o re w at the Josephine will be required for the permanent operating orew. Uncer existing regulations these men trill have to be obtained through the offices of National Selective Service. In this connection, it night be pointed out thot past experience indicates that it is easier to get men for a new operation like the Josephine Wine than It is to get men for an old established operation. The following is an estimate of the orew which .''li be required for permanent oper&tiom-

Mine

Cagers 3Uotormen 2Chute blasters ZLoaders 8Maintenance 2Traoknven and pipefitters 2Driftmen and Backers 18Ra i semen 4Stope miners and helpers JOSpare lShift bosses 2

Total Mine 75

CruahlnE Tpl&ntj mill and sinter pl^nt

PickersCrushing plant orewMill orewSinter plant orewSupervision, sampling and experimental

Total Crushing, Milling and Sintering 5 J

-11-Surfage Ciw

Cookhouse 7Xleotrioal Shop jCarpenter Shop 4Maohin* Shop }Blacksmith Shop 23teel Sharpening Shop 4Hoistraen }Cat Driver lTruck Drlvera 2Vfarehouoe 2Accounting Office 3Chtnioal laboratory 2 Engineering and geology 4Coraraon labor 7Superviaion -,,-,4-r

Total Surface

Total Crew 179

The followinc plane, sections, etc. are appended t -

Prints of Drill Logs SI to ^9 inclxujive.JU1 to JU9 inclusive.Test Holes, l, 3, 10, 16, 19, 22, 23, 51, 53, 57

Sections J-25, J-27, J-28 and J-29.

Geological plan of 6th level.

Geological section M.G.

Copies of pilot mill teat run reports.

Tours very truly,

Eldon L. Brown

Toronto. Ont. April 16th,

mm or no mats

KillRun

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RPT ON JOSEPHINE MINE - Geology Ontario

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Transcript of RPT ON JOSEPHINE MINE - Geology Ontario