RPT ON THE PHASE I EXPL PROG - Geology Ontario

42L03NW2004 2.19111 OBOSHKEGAN 010

19111

OBOSHKEGAN PROJECT

REPORT ON THE PHASE X

EXPLORATION PROGRAM

for

"RECEIVED"

c:: ' s '393GEOSCSENCf ASSESSkAENT

OfHCt

Douglas P. Parker September 3, 1998

TART.K QF COM'i'KMTS 42L03NW2004 2.19111 OBOSHKEGAN 010C

INTRODUCTION...................................... lLOCATION................................... . . . . . . . lACCESS................................... . . . ...... l

REGIONAL LOCATION MAP........................ 2PROPERTY.................................... . . . . . . 3PREVIOUS WORK..................................... 3

CLAIM MAP.......................... . . .. . . . . . . 4REGIONAL GEOLOGY MAP......................... 6REGIONAL GEOLOGICAL COMPILATION MAP.......... 7

GEOLOGY........................ . . . . . . . . . . . . . . . . . . . 8CURRENT STUDY....................... . . . . . . . . . . . . . . 9

GEOLOGICAL+GEOCHEMICAL COMPILATION MAP....... 10GEOPHYSICAL COMPILATION MAP.................. 11

RESULTS............................ . ..... . . . . . . . . . 12CONCLUSIONS AND RECOMMENDATIONS................... 14

APPENDIX I: Rock Sample DescriptionsAPPENDIX II: Assay CertificatesAPPENDIX III: Geophysical Survey Theory and ProcedureAPPENDIX IV: Report by M. LavigneAPPENDIX V: Report by F. GlassAPPENDIX VI: Diamond Drill Hole Logs

MAPS IN BACK POCKETMAP l Magnetic Contours (1:5000 scale)MAP 2 VLF Profiles (1:5000 scale)MAP 3 VLF Fraser Filtered Contours (1:5000 scale)MAP 4 HLEM 444Hz Profiles (1:5000 scale)MAP 5 HLEM 1777HZ Profiles (1:5000 scale)MAP 6 HLEM 3555Hz Profiles (1:5000 scale)MAP 7 IP Section Line HE (1:5000 scale)MAP 8 IP Section Line 12E (1:5000 scale)MAP 9 IP Section Line 13E (1:5000 scale)MAP 10 Diamond Drilling Section (1:500 scale)FIG 5 Geological+Geochemical Comp. (1:2500 scale)FIG 7 Geophysical Compilation (1:2500 scale)

INTRODUCTION

The Oboshkegan Lake Property is located 230 kilometres northeast of Thunder Bay and is underlain by rocks of the Wabigoon subprovince part of the Superior structural province of the Canadian Shield.

The area around the Oboshkegan Lake Property hosts numerous significant occurrences, deposits and past and present producers of gold and base metals yet the project area is largely unexplored.

The rationale of the project was to investigate the potential for economic gold mineralization along the strike extension of Knucklethumb Deformation Zone which contains significant gold mineralization on Cameco Gold's property immediately to the west.

From the fall of 1997 to July of 1998 Landis Mining Corporation undertook a systematic exploration program. Due to a lack of bedrock exposure and perceived thick overburden, the program relied heavily on geophysics with followup testing by diamond drill.

LOCATIOM

The project is located 230 kilometres northeast of Thunder Bay and 14 kilometres south of Tashota, a railroad siding on the C.N.R.'s northern line (Fig 1).

Claim Map Sheet: G-173 Oboshkegan Lake, Thunder Bay MiningDivision

ACCESS

The project area is accessed by traveling on the all weather Kinghorn Road which departs north from Highway 11 about 6 kilometres east of the town of Jellico. At kilometre 92 on the Kinghorn Road, a skidder trail turns southeastward through cutover for about four kilometres where it crosses Red Paint Creek and proceeds to Landis's 1998 drill setups. Access is also achieved by float plane on Gledhill and Oboshkegan Lakes.

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Oboshkegan Lake PropertyLandis Mining Corporation

Figure l : Property Location50 kilometres

PROpjKRl'Y

The property consists of 17 contiguous unpatented mining claims (191 units, 7,640 acres) recorded in the Oboshkegan Lake Area of the Thunder Bay Mining Division as follows (Fig 2):

1215526, 1215527, 1215528, 1215529, 1215530, 1215531,1215532, 1215533, 1215534, 1216579, 1216582, 1216583,1216584, 1216585, 1216586, 1216651, 1228183

PREVIOUS WORK

Lavigne (1998) describes the exploration history of the area.

Portions of the Oboshkegan Lake property were explored for iron, and two significant exploration programs explored portions of the property for base metals. No record exist of any gold exploration on the property. From 1973 to 1977, Noranda Exploration Co. Ltd. conducted ground EM and Mag, soil and basal till sampling, and diamond drilling on a claim block bordering on Oboshkegan Lake, extending southeastward (MNDM files 2.1304, 2.1979, 2.236). A government airborne survey found a high density of strong EM anomalies in this area(OGS Map 81291, 81292, 81285). Soil anomalies with values as high as 96 ppm Cu and 460 ppm Zn, and basal till samples with values as high as 625 ppm Cu and 625 ppm Zn were generated. Five coincident EM-soil^asal till anomalies were drilled, only one of these holes was on the property (hole OB4-77). The results were consistently disappointing in that zones containing pyrrhotite and graphite with low base metal values were intersected. Hole OB4-77 was selectively assayed. Only sulphide rich portion were assayed. Significantly, sericitic volcanics with fine disseminated sulphides described in the drill logs were not assayed. Some soil and basal till samples did not coincide with EM conductors. One such zone, on the south shore of the north end of Oboshkegan Lake, called the North Zone by Noranda, was not drilled. At this location the soil anomalies were broader, and only partly coincided with two EM conductors. Holmer Gold Mines conducted an extensive airborne survey in 1984. Their southeast boundary is the south shore of Oboshkegan Lake, and the overlap between their survey and the present property was minimal.

Of greater significance to the mineral potential of the Oboshkegan Lake Property is the historical and current activity and the geology of the Knucklethumb property, which lies to the west, and is bounded south and east by the

-3-

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V'#,

"t 1207198———— -n. . ——— .—— ————i 1207146 1210507 I2I53I3 F—-*

•^16586

121552.9


Figure 2 : Claim Map; Oboshkegan Lake, G173

Oboshkegan Lake Property (Figs 3+4). This property contains six gold showings that define an east-west trending structure within a felsic volcanic package. Both the structure and the host lithology continue onto the Oboshkegan Lake property. The Knucklethumb property has been under option to Cameco Gold Inc. for the past two years. Exploration on the property has been escalating, and a second diamond drilling campaign is planned for early 1998. Gold was originally discovered on this property in 1915 and the property has been explored intermittently ever since, often for base metals only.

The northernmost two zones are the Etilahxe and the MVP zones. The Etilahxe zone has been described as laminated cherty tuff and pyrite, 0.2 m wide, traced for 75 m. Grab samples assay results were as high as 1.58% Cu, Q.98% Zn, 0.64 opt Ag, and 0.017 opt Au. At the MPV zone, pyrite and chalcopyrite bearing veins and veinlets are hosted by silicified mafic volcanics. The zone is 1.2 to 1.5 m wide and contains up to 5% pyrite. A grab sample collected by the Ontario Geological Survey assayed 0.49 opt Au. On the southern trend of the gold occurrences, the westernmost is the Jazz occurrence. The mineralization consists of massive, stringer, and disseminated pyrite in iron carbonate altered felsic volcanics. Surface samples assayed 0.71 opt Au over 1.52 m. To the east, the Claimlin zone consists of coarse gold, chalcopyrite and pyrite in sheared, sericitic felsic volcanics that contain up to 3% pyrite. This east trending zone was traced for "several chains". Drill intercepts assayed 0.16 opt Au over 5.8 m and 0.21 opt Au over 3.0 m. The Rhyne zone consist of sheared and altered felsic volcanics containing fine disseminated pyrite. The zone is east striking, 10 metres wide, and may extend for 120 m. A grab sample of altered felsic volcanics containing disseminated pyrite assayed 0.670 opt Au. The most easterly zone, the Cabin zone, has produces assays from grab samples as high as 0.137 opt Au. One kilometre east of the Knucklethumb property, along the same trend, the Kipper- Cameron gold prospect received much attention prior to WW2, as evidenced by a shaft and trenches. This mineralization is described as a shear zone along a mafic and felsic volcanic contact.

It is evident from the above compilation of gold occurrences on the Knucklethumb property, that they are contained within a one kilometre wide corridor containing numerous mineralized shear zone. This corridor can be traced for 10 kilometres, onto the Oboshkegan Lake Property to the east. Collectively, these numerous shear zones found at the sites of gold mineralization, and mapping in 1996 by the Ontario Geological Survey which characterized much of the rock as strongly deformed (OGS Map P3365), defines a deformation

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D

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Figure 3 : Regional Geology,

i^s-i

OBOSHKEGAN LAKE PROPERTY BEARDMORE - GERALDTON AREA

GEOLOGICAL COMPILATION

ETIAKXE ZONE 0.017opl Au. 0.64cpl Ag,

JAZZONE0.71oplAu, 0.l6oplAg/ l .Em

and 0.40floct Au,

LANDIS MINING CORPORATION (LIS - ASH)

1 kilometre

PROPERTY LOCATION

METASEDIMENTS

MAFIC INTRUSIVES

FELSIC INTRUSIVES

GOLD OCCURRENCE

SHEARING

LANDIS MINING CORP.

PROPERTY

zone, which will be referred to as the Knucklethumb Deformation Zone. Thios deformation zone is a significant crustal structure, that has served as a pathway for mineralizing fluids, that can be projected onto the Oboshkegan Lake Property with confidence. It has produced various styles of mineralization, a common one being the occurrence of gold in pyritized felsic volcanics over substantial widths. This style of mineralization is more common to larger tonnage gold deposits, and is a favoured target type.

GEOLOGY

Lavigne (1998) describes the geology of the area.

The "Oboshkegan Lake" property is underlain by Archean age volcanic rocks of the northeastern portion of the Onaman- Tashota greenstone belt in the eastern Wabigoon Subprovince of the superior Province in the Canadian Shield (Figs, l, 3+4). They consist of east-west trending altered mafic and felsic volcanic rocks which contain an abundance of interflow, sulphide bearing, graphitic mudstone and iron formation. These rocks have been intruded by numerous gabbroic bodies. The belt is bound by late tectonic plutons of granodiorite to monzodiorite. The volcanic rocks have been metamorphosed to greenschist facies with amphibolite facies rock located in the thermal aureoles of the plutons. Alteration in the area consist of; synvolcanic chlorite alteration of the matrix in rhyolite autobreccias, (hornblende in higher grade rocks); syntectonic iron carbonate alteration (*/- chlorite, sericite, and minor green mica) is associated with gold mineralization in sheared mafic and felsic volcanics and gabbro; and post tectonic calcite, epidote and albite along fractures. Tourmaline is common accessory mineral in veins, and kyanite an exotic alteration mineral in felsic volcanics.

The north-eastern portion of the Onaman-Tashota greenstone belt, an area 1400 square kilometres in size, contains an abundance of mineral deposits. The first discovery in this area was made in 1904 by a survey crew for the Transcontinental Railway. Their initial discovery of iron led to many more. Soon after the completion of the railway in 1913, the first of many gold discoveries was made. Minor production came from the Tashota-Nipigon Mine, 8 km SW of the property and the Consolodated Louanna Gold Mine, 40 km to the northeast. Base metal occurrences are also common in this area. Much of the exploration activity in this area in the last 40 years has been the search for volcanogenic massive sulphide deposits. The largest deposit found to date is the Marshall Lake deposit, which contains 2.2 mt averaging 1.22% Cu, 4.2% Zn, 62.45 opt Ag and 0.012 opt Au.

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CURRENT STUDY:

From the fall of 1997 to July of 1998 Landis Mining Corporation undertook a systematic exploration program on the Oboshkegan Lake Property which examined the projected eastern extension of the Knucklethumb Deformation Zone in order to identify gold mineralization. Due to a lack of bedrock exposure and perceived thick overburden, the program relied heavily on geophysics with followup testing by diamond drill.

A 40 kilometre cut grid was established on the eastern boundary with Cameco Gold's property. The base line was cut at 070 degrees with lines turned off at 100 metre spacings with stations at 25 metre intervals. Mike Tremblay of Quantec Consulting Inc. of Timmins supervised the line cutting.

Magnetometer and VLF EM surveys were conducted across the entire grid. Mike Tremblay of Quantec Consulting Inc. of Timmins supervised the surveys. Survey data is plotted at 1:5000 scale on Maps #1, 2 + 3. Instrumentation and survey procedures are described in the appendix.

Max-min EM was conducted over 8.8 kilometres of line on the northeastern part of the grid. Larry Mealey of Grey Owl Resources of Thunder Bay supervised the survey. Survey data is plotted at 1:5000 scale on Maps # 4, 5 + 6. Instrumentation and survey procedures are described in the appendix.

IP EM was conducted over 3.3 kilometres of line on the northeastern part of the grid. Larry Mealey of Grey Owl Resources of Thunder Bay supervised the survey. Survey data is plotted at 1:5000 scale on Maps #7, 8 + 9. Instrumentation and survey procedures are described in the appendix.

A technical report and interpretation of VLF/magnetic/IP data was prepared by F. Glass in March, 1998 and is included in the appendix.

16 soil, 25 peat and 5 rock samples were collected from the northeastern part of the grid under the supervision of M. Lavigne and were analyzed for Au, Ag, Cu, Pb and Zn by Chemex Labs Ltd. Assay results are listed in Appendix I and plotted on Figure #5.

28 rock samples were collected by the author during prospecting of the northeastern part of the grid as well as on Oboshkegan Lake and were analyzed for Au by Accurassay Labs of Thunder Bay. Assay results are listed in Appendix I and plotted on Figures 15+6.

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9+OON

8+OON

7+OON

6+OON

5+OON

4+OON

3 + OON

964 (^) A 963 ^5) A 962(4)

SDA1

LIGEND

J FELSIC TUFF

2 WTERUEDIATE TUFF

1 MAFIC VOLCANIC

Fotatiwi Vvticol.

Outcrop

0 1998 Diomond Drill Hoto

4 * Soil SompU Au (ppb)

Crab Sompta Numtxr (Au ppb)

Port of Claim 1215531

150

L9E L10E L11E L12E L13E L14E

LANDIS MINING CORPORATION

DBDSHKEGAN PROPERTYOEOJXilCAL AND GEOCHEMICAL COPILATIDN

FIGURE 3

DOUG PARKER

Sample No. Au(ppb)965 ^966 ^967 <5968 <5969 ^970971972973974975976977

<5 <5 <5

11 13 9 <5

1215527

1.0

LANP1S MINING COKPOKATION

DBDSHKEGAN PROPERTYPROSPECTING SAMPLE UEAT1QNS

FIGURE 6

SDA GBOLOfflCAL SERVKRS UHRED

94'

8+OON

7+OON

6-t-OON

5+OON

4+OON

3+OON


GEOPHYSICAL COMPILATION

- x UN; PROFILES ( i cm - 500 nr) v BOM Lrm 58700 nT

Q] f CHARGEABILITY

IP RESISTMTY

f "'i V\f FRASER FILTER CONTOUR

Port of Clolm 1215531


DBDSHKEGAN PROPERTYGEDPYSICAL COHP1LATICN

FIGURE 7

MUG PARKER

Three NQ diamond drill holes totalling 500 metres tested the eastern part of the grid. Forage St Lambert under the supervision of Marc Bourgela conducted the drilling. The author provided geological supervision of the drilling program. 96 samples were split and analyzed for Au by Accurassay Labs in Thunder Bay. The drill section is plotted at 1:500 scale on Map #10.

RESULTS:

Lavigne (1998) describes the results of the magnetic and VLF-EM surveys, (Maps #1, 2 * 3).

In the southern portion of the survey, well defined northeast trending conductors are coincident with magnetic highs. These are the same conductors that Noranda Exploration Co. found in the course of their surveys, and later discovered by diamond drilling to be barren massive pyrrhotite and graphite. These are interflow sediments and corresponding EM conductors are formational. These strong conductors mask the disseminated sulphides within hydrothermally altered felsic volcanics that were intersected in Noranda's drilling, and not assayed for gold. Within the north half of the grid, the conductors found are parallel to the Knucklethumb deformation zone. Several half kilometre long, east trending conductors are stacked in an area that is transitional from "normal" magnetic response to one that is low and flat.

The anomalies which Lavigne describes within the north half of the property occur from Line 9E to Line 14E and from 1+OON to 10+OON. He suggests that the low flat magnetic response may be attributed to hydrothermal alteration of felsic volcanic rocks possibly related to gold mineralization and that the VLF-EM conductors may be produced by zones of shearing.

Limited prospecting and soil sampling was undertaken over the most prominent anomaly in this area which is centered from Line 9E to Line 14E from 5+50N to 8+OON. The area of the VLF-EM anomaly is extensively covered by cedar swamp with linear outcrops of felsic to intermediate volcanics occurring immediately north and south of the indicated anomaly. Of the five rock samples collected, all returned ^ ppb Au. Lavigne describes the results of the soil sampling. Of the 16 soil samples collected, 2 were clearly anomalous in copper, and 3 in zinc. These anomalies coincide perfectly with the conductors. The 25 peat samples collected established a threshold level of 8 ppm for copper, 3 samples exceeding that value, Ippm for lead, 3 samples exceeding that value, 50 ppm for zinc, 4 samples exceeding

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that value. These geochemical anomalies also coincided with the conductors, but tend to be on the north side.

On the basis of the geophysical and geochemical anomalies and the geological setting Lavigne suggested that both VMS and mesothermal gold mineralization similar to that which exists at Les Mines Selbaie, a major producer of Cu-Zn-Ag-Au in northwestern Quebec, may be present in this area.

Max-min EM surveys were then conducted over this area but failed to indicate the presence of strong conductors or confirm the previously identified VLF-EM anomalies, (Maps#4, 5 * 6).

IP-EM was conducted over three lines which crossed the VLF- EM anomalies, (Maps f 7, 8+9) . Frank Glass, a consulting geophysicist, identified resistivity low and chargeability high anomalies which occurred immediately north and south of the VLF-EM anomaly, (Figure #7). These IP anomalies correspond well with outcrop exposure of felsic to intermediate volcanic rocks containing local concentrations of fine disseminated pyrite, quartz-tourmaline stringers and ankerite alteration.

Three diamond drill holes were used to fence across the main VLF-EM anomaly as well as test the southern IP-EM anomaly which appeared to become stronger with depth, (Map #10). The northern IP-EM anomaly was partially tested by LO98-02 which collared in the anomaly but was not completely tested by drilling due to extensive exposure of outcrop in the anomaly area and a desire to limit the program to 500 metres. The drill holes intersected intermediate crystal to lapilli tuff with minor felsic tuff and mafic dykes south of 6+45N and felsic crystal to lapilli tuffs with minor mafic dykes to the north of 6+45N. Slightly elevated gold values 10-50 ppb occur with very fine grained pyrite mineralization and quartz tourmaline stringers. The highest gold value returned was 135ppb.

Of the 28 rock samples collected by the author, only sample 956 located on TB1215531 at 13+OOE 8+65N returned significant gold (276 ppb Au) from a selective grab of a 10cm quartz tourmaline vein with rusty spots and irregular folding, (Fig #5).

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CONCLUSIONS AMD

The Oboshkegan Lake Property exhibits stratigraphy, alteration and mineralization similar to that found on Cameco Gold's Knucklethumb Property located immediately to the west. The Oboshkegan Lake Property is along the projected strike extension of the Knucklethumb Deformation Zone which may be a significant control of regional gold mineral i zat ion .

The lack of bedrock exposure on the northern half of the property is a hindrance in evaluating the strike extension of the Knucklethumb Deformation Zone, however, overburden thickness may be minimal over a large portion of this area.

The next phase of exploration should concentrate on identifying gold and base metal mineralization in rock and soil followed by appropriate geophysical methods to prioritize targets for mechanical stripping and diamond drilling.

An orientation geochemical survey should be undertaken on lines 2E to 8E north of the baseline. Humus and B horizon should be sampled at 25 metre intervals. Analysis by neutron activation for multi-elements should include Au, Ag, As, Cu and Zn as a minimum.

Airphoto analysis could be used effectively to identify areas of outcrop and aid in prospecting and reconnaissance mapping over the entire property.

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STATEMENT OF QUALIFICATIONS

I, Douglas P. Parker do hereby certify:

I ara a resident of 365 Lark Street, Thunder Bay, Ontario, P7B 1P4.

I am a graduate of Lakehead University, Thunder Bay, Ontario (HBSc Geology 1985).

I have been employed as an exploration geologist for government and industry since 1985.

I am a member in good standing of the Canadian Institute of Mining and Metallurgy and the Northwestern Ontario Prospectors Association.

I have not received nor do I expect to receive any direct or indirect interest in the company or its properties.

Douglas P. Parker

APPENDIX I

Rock Samole Descriotions

970 (TB1215528 NORTH SHORE OF OBOSHKEGAN LAKE) ^ ppb Au Representative Composite Grab: cherty felsic volcanic with quartz vein stockwork, ankerite and tourmaline.

971 (TB1215528 SOUTH SHORE OF OBOSHKEGAN LAKE) ^ ppb Au Representative Grab: cherty felsic volcanic, up to S-5% pyrite.

972 (TB1215528 ISLAND IN OBOSHKEGAN LAKE) ^ ppb Au Representative Composite Grab: shear zone 3mxlm 060-080N, intermediate to felsic tuff l-3% fine to medium grained pyrite.

973 (TB1215528 NORTH SHORE OF OBOSHKEGAN LAKE) ^ ppb Au Representative Composite Grab: quartz stringer zone over 40cm in medium grained gabbro.

974 (TB1215528 NORTH SHORE OF OBOSHKEGAN LAKE) 11 ppb Au Representative Composite Grab: irregular quartz vein pod with minor pyrite and ankerite.

975 (TB1215528 NORTH SHORE OF OBOSHKEGAN LAKE) 13 ppb Au Representative Composite Grab: graphitic argillite, 25cm, 3- 5% pyrite, rusty.

976 (TB1215528 @ 975) 9 ppb AuRepresentative Composite Grab: intermediate to felsicvolcanic, S-4% very fine pyrite.

977 (TB1215528 @ 975) ^ ppb AuRepresentative Composite Grab: felsic lapilli tuff, rusty,S-5% very fine grained pyrite and pyrite clasts.

960 (TB1215531 10+30E 5+20N) <5 ppb Au

Selective grab: felsic-intermediate tuff, minor ankerite,trace pyrite, minor quartz-tourmaline stringer.

961 (TB1215531 11+90E 8+17N) <5 ppb AuSelective grab: felsic tuff It very fine grained pyrite.

962 (TB1215531 11+90E 8+25N) <5 ppb Au

Selective grab: felsic tuff It very fine grained pyrite,rusty.

963 (TB1215531 11+90E 8+32N) ^ ppb AuSelective grab: felsic tuff ^* very fine grained pyrite,rusty.

964 (TB1215531 11+85E 8+40N) <5 ppb AuSelective grab: 2cm quartz tourmaline stringer, minor rust.

965 (TB1215528 NORTH SHORE OF OBOSHKEGAN LAKE) ^ ppb Au Representative Composite Grab: quartz tourmaline stringers l-3cm.

966 (TB1215528 @ 965) ^ ppb AuRepresentative Composite Grabintermediate tuff hostingquartz stringers

967 (TB1215528 NORTH SHORE OF OBOSHKEGAN LAKE) ^ ppb Au Representative Grab: quartz vein 5cm minor ankerite, flat dip.

968 (TB1215528 @ 967) ^ ppb AuRepresentative Composite Grab: felsic volcanic, cherty,silicified?, It very fine grained pyrite.

969 (TB1215528 NORTH SHORE OF OBOSHKEGAN LAKE) ^ ppb Au Representative Composite Grab: cherty horizon in felsic tuff, 2-3 % very fine pyrite, numerous sinistral offsets Imxlm along 3300 vertical slips.

SAMPLE NUMBER. LOCATION, ASSAY AND DESCRIPTION

951 (TB1215531 12+30N 5+30E) ^ ppb Au

Selective grab: quartz-tourmaline stringer with tr. py 4cmin intermediate to mafic volcanic minor ankerite andsericite.

952 (TB1215531 12+25E 4+95N) ^ ppb AuSelective grab: quartz-tourmaline stringer with tr. py 10cm in intermediate tuff moderate ankerite and sericite, irregular folding.

953 (TB1215531 11+50E 4+50N) ^ ppb AuSelective grab: quartz-tourmaline stringer 8cm inintermediate tuff moderate ankerite and sericite, irregularfolding.

954 (TB1215531 11+OOE 4+40N) ^ ppb AuRepresentative Composite Grab: quartz-tourmaline vein up to0.75mx5.0m moderate ankerite and sericite, rusty.

955 (TB1215531 11+50E 7+75N) ^ ppb Au Representative Composite Grab: felsic tuff l* fine disseminated pyrite, 1(^ quartz tourmaline stringers.

956 (TB1215531 13+OOE 8+65N) 276 ppb AuSelective grab: 10cm quartz tourmaline vein irregularfolding, rusty.

957 (TB1215531 13+OOE 8+65N) 7 ppb AuRepresentative Composite Grab: felsic tuff, rusty, minorvery fine grained pyrite.

958 (TB1215531 10+05E 3+80N) ^ ppb AuRepresentative Composite Grab: mafic volcanic, ankerite,minor fine grained pyrite

959 (TB1215531 10+30E 4+60N) ^ ppb AuSelective grab: 10cm quartz tourmaline vein trace pyrite,minor ankerite, at contact of felsic and intermediate tuffs.

APPENDIX II

Assay Certificates

ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.

Landis Mining Corp.Suite 400, 604 1st Street SouthwestCalgary, AlbertaT2P 1M7

1070 LITHIUM DRIVE, UNIT 2Paae THUNDER BAY. ONTARIO P7B 6G3

PHONE (807) 623-6448 FAX (807) 623-6820

July 21, 1998

Jot* 9840466

SAMPLE # Accurassay Customer

1234567891011 Check12131415161718192021 Check2223242526272829

501502503504505506507508509510510511512513514515516517518519519520521522523524525526527

Goldppb

^31142053

5^

613^^^^^^

5^^^^^^15

86^^^<5

GoldOz/t

^.001^.001^.001•eO.0010.002

^.001<0.001<0.001^.001^.001^.001^.001^.001^.001<0,001<0.001^.001^.001•sO.OOI^.001^.001<0,001<0.001^.001<0.001^.001^.001^.001•^0.001

Certified By:

t?e:0Q f 6617 To/SO


Landis Mining Corp.Suite 400, 604 1st Street SouthwestCalgary, AlbertaT2P 1M7

1070 LITHIUM DRIVE. UNIT 2Paae JHUNDER BAY, ONTARIO P?B 6G3

PHONE (807) 623-6448 FAX (807) 623-6820

July 21, 1998

Job* 9840466


3031 Check32333435363738394041 Check42434445464748495051 Check5253545556575859

528528529530531532533534535536537537538539540541542543544545546546547548549550551552553554

Goldppb

^^^109

135

1823355051271776^

6^10897

135^^^^^^

GoldOz/t

•^0. 001<0.001^.001^.001^001^.001^.001^.001<0.001

0.0010.0010.001

^.001^.001<0.001^.001^.001*:0.001^.001^.001<0.001^.001^.001

0.004^.001^.001^.001O.001^.001^.001

Certified By:

sawn : 00 f66T/ li /S0


Landis Mining Corp.Suite 400. 604 1st Street SouthwestCalgary. AlbertaT2P 1M7

1070 LITHIUM DRIVE, UNIT 2Paae JHUNOER BAY, ONTARIO P/B 6G3

v PHONE (807) 623-6448 FAX (807) 623-6820

July 21, 1998

Job* 9840466


6061 Check62636465666768697071 Check72737475767778798081 Check8283848586878889

555555556557558559560561562563564564565566567568569570571572573573574575576577578579580581

Goldppb

^<5<511*5

12<5^^2136651717161118^14^^<5<5^

5<5<5<5^

GoldOz/t

<0001^.001^.001^.001

^.001^.001<0.0010.0010.0010.001

0.0010.002

0.0010.001O.001O.001O.001O.001O.001O.0010.001O.0010. 001O.001O.001O.0010.001O.001O.001

Certified By:


Landis Mining Corp.Suite 400,604 1st Street SouthwestCalgary, AlbertaT2P 1M7

1070 LITHIUM DRIVE, UNIT 2Pan** THUNDER BAY. ONTARIO P7B 6G3r aye f PHONE (807) 623-6448

FAX (807) 623-6820

July 21, 1998

Job* 9840466


9091 Check9293949596979899

100101 Check102103104105106107108109110111 Check112113114115116117118119

582582583584585586587588589590591591592593594595596951952953954954955956957958959960961962

Goldppb

^^^^^^^^

53331331545^^

5^^^^^^

2767^<5^^<5

GoldOzrt

O.001^.0010.001O.001O.001O.001O.0010.0010.0010.001O.0010.001O.001

0.0010.0010.001O.001O.001O.001O.001O.0010.001O.001

0.0080.0010.0010.0010.001O.0010.001

Certified By:

-qy f|R T

OlJH h ax Jui 2y Oy: 52

ACCURASSAY LABORATORIESDIVISION OF ASSAY LABORATORY SERVICES

Landis Mining Corp.Suite 400, 604 1st Street SouthwestCalgary. AlbertaT2P 1M7

SAMPLE #Accurassay Customer

120121 ChecK122123124125126127128129130131 Check132133134135136

963963964966966967968969970971972972973974975976977

1070 LITHIUM DRIVE. UNIT 2Page SHUNOER BAY, ONTARIO m eoaPHONE (807) 623-6448

FAX (807) 623-6820

July 21, 1998

Job* 9840466

Gold Goldppb Oz/t

*S ^0.001*5 *0.001^ O.001•C5 0.0010 O.001^ O.001O O.001*S O.001*5 0.001O O.001o 0.001<5 O.001<6 <0.00111 O.00113 O.001

9 0001<5 O.001

*"——5

Certified By.

9289E 33/108 T

APPENDIX III

Geophysical Survey Theory and Procedure

GEM Systems Inc. VLF-2 GSM-19GEM Systems Inc.52 West Beaver Creek Rd. Unit 14Richmond Hill, OntarioCanada L4B 1L9

Phone: (905) 764-8008 Fax : (905) 764-9329

Specifications

Frequency Range: Parameters Measured:

Resolution:Number of Stations:Storage:

Terrain Slope Range: Sensor Dimensions: Sensor Weight:

physical Overview

15 - 30.0 kHz.Vertical In-phase and Out-of-phase components aspercentage of total field.2 components of horizontal field.Absolute amplitude of total field.D.1%.Up to 3 at a time.Automatic with: time, coordinates, magneticfield/gradient, slope, EM field, frequency, in-andout-of-phase vertical, and both horizontal componentsfor each selected station.QO - go 0 (entered manually).14 X 15 X 9 cm. (5.5 X 6 X 3 inches).1.0 kg (2.2 Ib).

*The sensor is a dual coil type designed to reduce noise and improve gradient tolerance. The coils are electrostatically shielded and contain a proton rich liquid in a pyrex bottle, which also acts as an RF resonator.*The sensor cable is coaxial, typically R.-58/U, up to 100m long.*The staff is made of strong aluminum tubing sections (plastic staff optional). This.construction allows for a selection of sensor elevations above ground during surveys. For best precision the full staff length should be used. Recommended sensor separation in gradiometer mode is one staff section (56cm from sensor axis to sensor axis), although two or more sections are sometimes used for maximum sensitivity.

*The console contains all the electronic circuitry. It has a 16 key keyboard, a 4 X 20 character alphanumeric display, and sensor and power/input/output connectors. The keyboard also serves as an ON-OFF switch.

*The power7input/output connector also serves as RS232C input/output and optionally as analog output and/or contact closure triggering input.*The keyboard, front panel, and connectors are sealed i.e. the instrument can operate under rainy conditions.*The charger has 2 levels of charging, full and trickle, switching automatically from one to another. Input is normally 110V 50/60HZ. Optionally, 12 VDC input can be provided.*The all-metal housing of the console guarantees excellent EMI protection.

principal of OperationThe VLF transmitting stations operating from communications with submarines have concentric horizontal magnetic fields around them. When the fields meet conductive bodies in the ground, there will be secondary fields radiating from these bodies. The VLF-2 16 measures the vertical components of these secondary fields. The instrument is simply a sensitive receiver covering the frequency band of the selected station with means of measuring the vertical field components.

Magneti c Survey Theory; *

The magnetic method la based on measuring alteration in the shape and magnitude of the earth's naturally occurring magnetic field caused by changes in the magnetization of the rocks in the earth. These changes in magnetization are due mainly to the presence of the magnetic minerals, of which the most common is magnetite, and to a lesser extent Ilmenite, pyrrhotite, and some less common minerals. Magnetic anomalies in the earth's filed are caused by changes in two types of magnetization; (1) Induced, caused by the magnetic field being altered and enhanced by Increases in the magnetic susceptibility of the rocks, which is a function of the concentration of the magnetic minerals. (2) Remanent magnetism is independent of the earth's magnetic field, and is the permanent magnetization of the magnetic particles (magnetite, etc..) in the rocks. This is created when these particles orient themselves parallel to the ambient field when cooling. This magnetization may not be in the same direction as the present earth's field, due to changes in the orientation of the rock or the field. The unit of measurement (variations in intensity) is commonly known as the Gamma which is equivalent to the nanotesla (nT).

Method:

The magnetometer, GSM-19 with an Overhauser sensor measures the Total Magnetic Field (TFM) perpendicular to the earth's field (horizontal position in the polar region). The unit has no moving parts, produces an absolute and relatively high resolution measurement of the field and displays the measurement on a digital lighted display and is recorded (to memory). Initially, the tuning of the instrument should agree with the nominal value of the magnetic field for each particular area. The Overhauser procession magnetometer collected the data with a 0.2 nanoTaala accuracy. The operator read each and every line at a 12.5 m interval with the sensor attached to the top of three (56cm) aluminum tubing sections. The readings were corrected for changes in the earth's magnetic field (diurnal drift) with a similar GSM-19 magnetometer, ^base stations which automatically read and stored the readings at every 30 seconds. The data from both units was then downloaded to PC and base corrected values were computed.

(9)

GEM Systems Advanced Magnetometers GSM-19V 4.0

6EN Systems Inc52 West Beaver Creek Road, Unit 14Richmond Hill, Ontario Phone; (905) 764- 8008Canada, L4B-1L9 Fax ; (905) 764- 9329

1.0 Instrument Description The sensor is a dual coil type designed to reduce noise and improve gradient tolerance. The coils are electrostatically shielded and contain a proton rich liquid in a pyrex bottle, which also acts as an RF resonator. The sensor cable is coaxial, typically RG-5E/U, up to 100m long.

The staff is made of strong aluminum tubing sections. This construction allows for a selection of sensor elevationsabove the ground during surveys. For best precision the full staff length should be used. Recommended sensorseparation in gradiometer mode is one staff section, although two or three section separations are sometimesused for maximum sensitivity.The console contains all the electronic circuitry. It has a sixteen key keyboard, i 4x20 character alphanumericdisplay, and sensor and power input/ output connectors. The keyboard also serves as an ON-OFF switch.The power input/output connector also serves as a RS232 Input/output and optionally as analog output and contactclosure triggering input.The keyboard front panel, and connectors are sealed (can operate under rainy conditions)The charger has two levels of charging, full and trickle, switching automatically from one to another. Inputis normally 110V 50/60HZ. Optionally, 12V DC can be provided.The all-metal housing of the console guarantees excellent EM protection.

2.0 Instrument SpecificationsResolution 0.01 nT, magnetic field and gradientAccuracy 0.20 nT over operating rangeRange 20,000 to 120,000 nT automatic tuning, requiring initial setupGradient Tolerance over 10,000 nT/mOperating Interval 3 seconds minimum, faster optional. Reading initiated from keyboard,external trigger, or carriage return via RS-232Input/Output 6 pin weatherproof connectorsPower Requirements 12V, 200mA peak, 30mA standby, 300mA peak with GradiometerPower Source Internal 12V, l.SAh sealed lead-acid battery standard, external sourceoptional.Battery Charger Input; HO/ 220VAC, 50/COHz and/or 12VDC

Output; 12V dual level charging Operating Ranges Temperatures; -40*C to *60*C

Battery'Voltages; 10.0 V min to 1S.OV maxHumidity; up to 901 relative, non condensing

Storage Temperature -50*C to *65*C Dimensions Console; 223 X 69 X 240 cm

Sensor Staff; 4 x 450mm sectionsSensor; 170 x Tl am diameterWeight; Console 2.1Kg Staff 0.9Kg Sensors; I.iKg

(8)

LOGISTICS AND OPERATIONAL REPORTLANDIS MINING CORP.

OBOSHKEGAN LAKE PROPERTY

INTRODUCTION

This report summarizes work completed during the month of February,

1998, on Landis Mining Corp.'s Oboshkegan Lake Property. Horizontal Loop EM

and Induced Polarization surveys were carried out over select portions of an

already established grid which had Magnetic and VLF-EM surveys carried out

over it previously.

LOCATION AND ACCESS

Landis Mining Corp.'s Oboshkegan Lake Property is located in the

Oboshkegan Township approximately 90 kilometres north of Jellicoe, Ontario,

NTS 42L/3. Co-ordinates for the centre of the property are approximately 87

degrees 28 minutes west and 50 degrees 10 minutes north.

Access to the property can be made via the Kinghorn logging road which

departs Highway 11 approximately 6 kilometres east of Jellicoe and thence to

mileage 87.5 where a cut and skid road leads to the southeast to the north shore

of Oboshkegan Lake. A trail leads to the base line or the creek from the northeast

end of the lake can be used to get to the base line and thence into the property. A

log bridge had to be built over the creek for access during the IP survey. Access

from the Kinghorn Road at mileage 87.5 was via snowmachine and sled.

PROPERTY

The property consists of an option to acquire 1000Xo interest in 9 mining

claims numbered TB: 1215526, 1215527, 1215528, 1215529, 1215530, 1215531,

1215532, 1215533 and 1215534 containing 117 claim units and a further 8 claims

staked by Landis Mining Corporation numbered TB: 1216579, 1216582, 1216583,

1216584, 1216585, 1216586, 1216651 and 1228183 containing a total of 74

units. All of this claims are a contiguous block of 7,640 acres. The claims are

located on the Oboshkegan Township claim map G-173, located in the Thunder

Bay Mining Division of the Province of Ontario.

PERSONNEL

Horizontal Loop: Gary Rollick Thunder Bay, Ont.Jim Mealey Murillo, Ont.

IP Survey: Gary Rollick Thunder Bay, Ont.Jim Mealey Murillo, Ont.Steve Shore Thunder Bay, Ont.Dave Brown Thunder Bay, Ont.Josh Guthrie Thunder Bay, Ont.Mike Duguay Thunder Bay, Ont.

GEOPHYSICAL EQUIPMENT

Horizontal Loop Apex Max Min 11 Serial 441

IP Units Receiver: Model: Iris Elrec 6 SerialiseTransmitter: Model: GDD 1400W Serial Tx 208Generator: Model: Honda EZ 1800

Specification Equipment data is appended to this report

SURVEY DATES

Horizontal Loop January 28, 29, 30, 31, 1998

IP Survey February 13, 20, 21, 1998.

Reports March 5, 6, 8, 9, 17, 18, 1998.

SURVEY COVERAGE

Horizontal Loop

IP Survey

Lines 8E to 15E inclusive from baseline to 1200N Total of 9.6 kilometres

Lines 11 E, 12E, 13E from baseline to 1200N Total of 3.6 kilometres

REPORTS

Logistics A Operational: G. L. Mealey

Technical Frank Glass

G. L. Mealey, GET General Manager

CERTIFICATE

I, George Lawrence Mealey of 132 Mining Road, Murillo, Ontario, POT 2GO, do certify that:

1. I am a prospector and mining exploration contractor and owner of 757410 Ontario Limited operating as Grey Owl Resources.

2. I attended Cambrian College of Applied Arts and Technology in Sault Ste. Marie, Ontario and obtained a Diploma for the two year course for Geological technician in 1969.

3. I have practised my profession continuously since my graduation and have been employed in the mining exploration industry since 1969.

4. I am the author of this report

5. The information in this report is based upon personal knowledge and the authors and sources quoted in the report

6. I am a Member of the local Chapter of the CIM.

7. I am a Director and the Treasurer of the Northwestern Ontario Prospector's Association.

8. I am a Certified Senior Engineering Technician registered with the Ontario Association of Certified Engineering Technicians and Technologists.

Dated at Murillo, Ontario, this /B day of .M * A c u ,

George Lawrence Mealey, GET

"X

••anxt-rj-ea ^ -*^ ] -JJ]

.

Five frequencies: 222, 444, BBS, 1777 and 3555 Hz.

Maximum coupled C horizontal-loop 3 operation with reference cable.

Minimum coupled operation with reference cable.

Vertical-loop operation without reference cable.

Coil separations: 25, 50,100,150,800 and 25Om C with cable l or 100,200,300,400,600 and BOD ft.

Reliable data from depths of up to IBOm C BOO ft 3.

Built-in voice communication circuitry with cable.

Tilt meters to control coil orientation.

. BBS. 1777 and 3555Hz.

r ' — sKrssiar MAX: Transmitter coil plane and re ceiver coil plane horizontal CMax-coupled; Horizontal-loop mode]. Used with refer, cable .

M IN: Transmitter col plane horizon tal and receiver coil plane ver tical CMin-coupled mode). Deed with reference cable.

V.L. : Transmitter coil plane verti cal and receiver coil plane hori zontal (Vertical-loop model. Used without reference cable , in parallel lines.

.-i --.-ions' 25.50.100.150,200 S25Om CMMin or 1OO. 2OO, 3OO. 4OO.SOO and BOO ft. CMMHF}. Coil separations in VL.mode not re stricted to fixed values.

cwcri. P.c2r:d . |n-Phase and Quadrature compo nents of the secondary field i n MAX and M IN modes.

- Tilt-angle of the total field in V.L. mode .

-- - Automatic, direct readout on 3D mm C3.5 "5 edgewise meters in MAX and MIN modes. No null ing or compensation necessary .

- Tilt angle and null in 3D mm edge wise meters in V.L.mode .

-•- - '-r••••- In-Phase: *2Or..±1OC)r. by push button switch .

Quadrature: ±2O V.. ±1OO*/. by push button switch .

Tilt: *75"/. slope .NullCVLJ: Sensitivity adjustable

by separation switch.

In-Phase and Quadrature : O.2S V. to 0.5 V. ; Tilt: 1 V. .

±O.25V. to±1V. normally, deper on conditions, frequencies ana separation used .

- S22Hz : 22OAtma- 444 Hz : 2OO Atm2- BBSHz : 12OAtm2- 1777HZ : BOAtm2- 3555 Hz : 3O Atm2

9V trans, radio type batteries Life: approx. 35hrs. continuou ty (alkaline, O.5 Ah), less in weather.

12V B Ah Gel- type recharg; battery. [Charger supp

Light weight 2- conductor t cable for minimum friction. Uns ed. All reference cables opt at extra cost. Please spt

Built-in intercom systenr voice communication betweer ceiver and transmitter opere in MAX and MIN modes, vu ference cable .

Built-in signal and reference ing lights to indicate erron readings .

-4O*Cto*SO0C (-

Bkg (13 IbsJ

13kg (23-lbs.)

: - " Typically BOkg (135lbs.3, de ing on quantities of refer cable and batteries inclu Shipped in two field/shipping c:

Specifications suoject to cnange without notific-

Vcisr. -i

Dut+ftrr

MULTICHANNEL IP RECEIVER FOR MINERAL EXPLORATION

. Six simultaneous d i poles

. Ten programmable chargeability windows

. High accuracy and sensitivity

Time '2s

i f,it 1,1 J. '::-.rrrr3

programmable

logarithmic l

Vlogarithmic 2

' ELREC 6 SAMPLING MODES

ELREC 6 is a six dipole Time Domain Induced Polarization receiver designed for nigh productivity surveys in mineral exploration.

ELREC 6 has been designed for being both a user friendly and very sensitive EP receiver.

ELREC 6 OUTSTANDING FEATURES. Six dipole :

The six channels of the receiver permit to measure six dipoies simultaneously, which provides a high efficiency in the field.

. Ten programmable windows :Beside the classical preset logarithmic and arithmetic modes, ELREC 6 also offers ten fully independant programmable windows which the operator can define by himself according to the way he wants to sample the EP decay curve.

. Automatic measuring process :A microprocessor fully controls the synchronization, the gain ranging, the stacking, and the display of the results including the apparent resistivity.

Monitoring display : During the acquisition, the chargeability the six dipoles can be displ simultaneously on the LCD display f global visualization of the readings : standard deviations of these chargeabi. can also be displayed simultaneously : real time monitoring of the quality of th going readings.

Internal memory :The memory can store up to 2500 read each reading including the full se parameters characterizing the measureme the date and time of the reading, give: the Real Time Clock of the instrument. also stored. A serial link permits to tnu the data to a printer or a micro computer

Remote control :ELREC 6 can be fully driven by a r computer through the serial link :"or re; operation applications.

Frequency mode :The frequency effect and the phase between the fundamental and the harmonics may be measured for a Freque Domain waveform (ON+, ON-), or f c Time Domain waveform (ON + , OFF, C OFF}.Time Domain waveform (ON-l-, OFF, O' OFF).

Field proof instrument : ELKEC rt operates m a wide temper:: range and features a fiber-glass case resisting to field shocks and vibrations.

Instruments

ELREC 6 measuring process has been optimized to provide the best possible accuracy in real field conditions.

ELREC 6 features:. A cots* monitoring system :

A monitor function enables the operator the check the level of noise observed on each dipole before the measurement : the digital voltmeter function displays on the LCD the raw instantaneous value of potential. In particular, it is possible to numerically observe the presence of a pulse square waveform corresponding to a primary voltage signal and showing the operation of a transmitter. This function is also available during the acquisition of a reading.'

. A line check/ground resistance measurement which permits to check that all seven electrodes are properly connected lo the receiver.

. A low-pass analog filter which reduces the effect of higher frequency natural and cultural noises (50-60 Hz).

. Automatic SP compensation, including linear drift correction (up lo l mV/s) through a digital filter.

. Automatic gain ranging, within a voltage range of ± 10V.

. Automatic synchronization process : ELREC 6 automatically synchronizes with the signal through a waveform recognition process ; besides it automatically re- synchronizes at each new pulse to avoid errors due to a possible shift in the period of the transmitted signal.

. Automatic digital stacking to enhance the signal-to-noise ratio for as long as the operator wants, with a maximum of 220 stacks. During the stacking, the operator can monitor either the instantaneous value (to observe the level of noise), or the cumulative value (to observe the convergence of the average value).

. A continuous quality test procedure, which stops the averaging process when the noise level becomes loo high, but keeps the previously stacked data. The averaging procedure starts again when noise decreases. This procedure optimizes the time of data acquisition in very noisy areas.

. A resolution after stacking of l jiv for primary voltage, and of 0.01 mV/V for chargeability, for pointing out low amplitude anomalies. The standard deviations of the chargeability of the six dipoles are displayed dunng and after the acquisition to give an indication on the noise level.

. A Normalized chargeability option : The Normalized chargeability option refers the chargeability to a standard IP decay curve, and permits to point out any EM coupling effect on the measured signal.

Automatic calibration

Automatic synchronization

SP compensation

Digital ranging

HOI4E

Digital sucking

- M,}'/ N)'"

Standard deviation

' OIPOIC OIPOU MtASUMMtNTS WITH CLHfC t HCCEIVf H

teroplteTERRAPLUS INC.,

52 West Beover Creek Road, Unit 1 4,

'.icnncnc Hill. Ontario Telephone: (905] 764-5505 :cx: !905! 764-8093

" Signal waveform :Time Domain (ON+, OFF, ON-, with pulse duration of 0.2, l, seconds;

* Up to ten arithmetic, logarithm! programmable IP chargeability wi

* Computation of apparent resistivi chargeability and standard deviatii

* Input impedance 10 Mohm

' Input ovcrvoltagc protection up tc

' Input voltage range: each dipole : 10V max sum of voltage of dipoles 2 to 6 :

' Automatic SP bucking ± 10V drift correction up to l mV/s

* 50 to 60 Hz power line rejection

" Sampling rate : 10 mS

* Common mode rejection ' 100 dB (for RS ~ 0)

" Grounding resistance measure 0. l to 467 Kohm

* Battery test : manual and auto: each measurement

" Primary voltage :resolution : l ^V after stacking accuracy : typ. 0,3 SS

* Chargeability :resolution : O'.Ol mV/V accuracy : typ. 0.65S

* Memory capacity : 2500 reading

" RS 232 link for data transfe computers and printers (300 to rate)

* Remote control through the seri:

FREQUENCY MODE

" Signal waveform :(ON-r-, ON-) or (ON-h, OFF,

" Pulse duration : Is or 2s

' Frequency effect and relati fundamental and third harmonic

* Resolution : about 0.01 degree

GENERAL FEATURES :" Dimensions : 31x21x21 cm

" Weight : 6 kg with dry cells8 kg with internal batt

* Operating temperature : -20-C to -4-70*Cto -l-70'C optional)

Power supply :12V internal battery,or six 1.5V D size dry cells.In both cases, a 12V extern:also be used.

The Tx II1400-W I.P. Transmitter

l Only S 12,500 CAD -One-year warranty m Protection against short circuits even at

zero (0) ohms j Output voltage range: 150V-2000V

nis

Power source: 120V 1 60 Hz -Optional: 220V/50 HzOperates from a light backpackable standard 120 V generator

igh-quality I.P. surveys in all possible field conditions.Manufactured by Instrumentation GDD inc.

The Tx I11400-W I.P. TransmitterSpecificationsGENERALl Size: 21 x 34 x 39 cml Weight: approximately 20 kgl Operating temperature: -40"C to 65'C

E ZC73SCAL CHARACTERISTICSm Used for time-domain I.R.: 2 sec. ON, 2 sec. OFFB Output current range: 0.005 to 10 Am Output voltage range: 150 to 2000V

CONTROLSm Power ON/OFFm Output voltage range switch: 150 V, 350 V, 500 V,

700V, 1000V, 1400V, 2000V

C.SPLAYSm Output current LCD: reads to ± 0.001 Am Standard LCD heater for very cold weatherH Total protection against short circuits even at zero

(0) ohms B Indicator lamps:

- High voltage ON/OFF- Output overcurrent- Generator over or undervoltage- Overheating- Logic failure- Open loop protection

F JWE3m Recommended motor/generator set:

standard 120 V 1 60 Hz backpackable Honda generator (650,1400, or 1900 W)

C JSTl The Tx II1400-W I.P. transmitter including shipping

box: S 12,500* (CAD); r Optional backpack frame for transmitter or generator:

S 500* (CAD).

SERVICEH Any instrument manufactured by GDD that breaks

down while under warranty or service contract is replaced free of charge upon request, subject to instruments availability.

WARRANTYH A one-year warranty on parts and labour.

Repairs done at GDD's office in Sainte-Foy.

Instrumentation GDD inc.

3700, boul. de la Chaudiere Sainte-Foy (Quebec) Canada G1X4B7Tel. : (418) 877-4249 Fax:(418)877-4054http://www.qbc.clic.net/-gdd E-Mail: [email protected]

* Prices and specifications subject to change without notice. Taxes, transportation and duties are extra, if applicable.

instruments available for rental or sale.

© Copyright 1997 Instrumentation GDD inc.

APPENDIX IV

Report Bv M. Lavigne

"OBOSHKEGAN PROPERTY"

Recommendations for Exploration

Prepared by:

Maurice LavigneMatawin Mineral ExplorationJanuary 31,1998

EXECUTIVE SUMMARY

Landis Mining Corporation's Oboshkegan Lake property is the on strike extension of a polymetallic gold bearing structure that has been mostly explored for base metals, and whose gold potential has only recently been recognized. Currently, Carneco Gold Inc is conducting an exploration program on this structure and is commencing its second diamond drilling program. Their property contains at least six gold occurrence with values as high as 0.16 opt Au over 5.8 metres, in a structure than can be traced for ten kilometres, prior to crossing onto the Oboshkegan Lake property. Sheared, hydrothermally altered and mineralized rock found on the Oboshkegan Lake property likely represent the eastern extension of this structure. First pass geophysical and geochemical surveys discovered anomalies sufficiently encouraging to justify continuing a exploration program. The initial 40 km grid should be expanded and additional electromagnetic surveys should be conducted to better define previously located anomalies prior to diamond drilling.

CONTENT

INTRODUCTION...............................................................................l

LOCATION AND ACCESS................................................................2

REGIONAL GEOLOGY.........................................;...........................2

EXPLORATION HISTORY................................................................6

CURRENT PROGRAM.......................................................................8

CONCLUSIONS AND RECOMMENDATIONS................................ 9

PROPOSED WORK PROGRAM.........................................................10

FIGURES

Figure l ; Location map.......................................................................3

Figure 2 ; Claim map............................................................................4

Figure 3 ; Regional geology..................................................................5

Figure 4 ; Property geology..................................................................?

APPENDIX

Statement of qualifications

I; bedrock Au assays

H; bedrock Ag, Cu, Zn, Pb assays

m ; soil analysis, C.of A. A9654163

IV ; peat analysis, C.of A A9654162

INTRODUCTION

Matawin Mineral Exploration was commissioned by Abraham Drost, S.D.A. Geological Services, to generate mineral exploration recommendations, but not the costing, for Landis Mining Corp.'s Oboshkegan Lake property in the Onaman-Tashota Greenstone Belt. The recommendations are based on an evaluation of the geology and mineral occurrences in the area, previous and current exploration activities, and a one day site visit on December 18th, 1997. During this visit, Abraham Drost and the author collected soil and humus samples, while property vendor, John Temowsky, prospected. This visit was restricted to claim 1215531.

LOCATION AND ACCESS

Landis Mining Corporation's Oboshkegan Lake property consist of an option to acquire a 1000Xo interest in 9 claims, numbers 1215526, 1215527, 1215528, 1215529, 1215530, 1215531, 1215532,1215533 and 1215534, which amount toll7 claim units in total; and 8 claims staked by Landis Mining Corporation, numbers 1216579, 1216582,1216583, 1216584,1216585, 1216586, 1216586, and 1228183, which amount to 74 claim units (Fig.2). All of the above claims are contiguous, and form a claim block which is 7,640 acres in size. These claims are located on claim map G-173, Oboshkegan Lake, Thunder Bay Mining Division, Province of Ontario, Canada. The property is located 14 km southeast of the railroad siding Tashota, on the C.N.R 's northern line, 230 km northeast of the city of Thunder Bay (Fig.l). From Thunder Bay, the l property is accessed by driving 220 km northeasterly along Hwy 11, to the Kinghorn Rd, 5 km east of the village of Jellicoe. From 80 to 100 km north of Highway 11, along the Kinghorn Rd, secondary and tertiary logging roads access western parts of the property.

REGIONAL GEOLOGY

The "Oboshkegan Lake" property is underlain by Archean age volcanic rocks of the north eastern portion of the Onaman-Tashota greenstone belt in the eastern Wabigoon Subprovince of the Superior Province in the Canadian Shield (Figs. 1& 2A 3). They consist of east-west trending altered mafic and felsic volcanic rocks which contain an abundance of interflow, sulphide bearing, graphitic mudstone and iron formation. These rocks have been intruded by numerous gabbroic bodies. The belt is bound by late tectonic plutons of granodiorite to monzodiorite. The volcanic rocks have been metamorphosed to greenschist facies with amphibolite facies rock located in the thermal aureoles of the plutons. Alteration in the area consist of; synvolcanic chlorite alteration of the matrix in rhyolite autobreccias, (hornblende in higher grade rocks); syntectonic iron carbonate alteration (+J- chlorite, sericite, and minor green mica) is associated with gold mineralization in sheared mafic and felsic volcanics and gabbro; and post tectonic calcite, epidote and albite along fractures. Tourmaline is common accessory mineral in veins, and kyanite an exotic alteration mineral in felsic volcanics.

The north-eastern portion of the Onaman-Tashota greenstone belt, an area 1400 square kilometres in size, contains an abundance of mineral deposits. The first discovery in this area was made in 1904 by a survey crew for the Transcontinental Railway. Their initial discovery of iron


Figure l : Property Location 50 kilometres

ok.^

7 1207198 ——.^.—.— ——,'^07146 J 1210507^1 1215313

i 1202236 ! 12


Figure 2 : Claim Map; Oboshkegan Lake, G173

x F!.----IFi- s- r r f" P1

- U

f, : //iniifrtfj).'.'*u^!S^

i ""l-,, t ut

*\j- -/^./J,^^P"^ -r 7"^4tfr ii^-:f""3iiiiS^S^ .''^'"i '^^f^^SallitS^ . ..'jr^Q. . ., ,x. a *,... !

: i/ ir^M^SSiMlif -i -•-••-".,./.HCV

D

lif^p;t-^'Si^-aifciwiK,

H uttv/j^-'1 ,^X"

^Xl LttkC

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x


Figure 3 : Regional Geology;

led to many more. Soon after the completion of the railway in 1913, the first of many gold discoveries was made. Minor production came from the Tashota-Nipigon Mine, 8 kin southwest of the property and the Consolidated Louanna Gold Mine, 40 km to the northeast. Base metal occurrences are also common in this area. Much of the exploration activity in this area in the last 40 years has been the search for volcanogenic massive sulphide deposits. The largest deposit found to date is the Marshall Lake deposit, which contains 2.2 mt averaging l .2207o Cu, 4.207o Zn, 62.45 opt Ag and 0.012 opt Au.

EXPLORATION HISTORY

Portions of the Oboshkegan Lake property were explored for iron, and two significant exploration programs explored portions of the property for base metals. No record exist of any gold exploration on the property. From 1973 to 1977, Noranda Exploration Co. Ltd. conducted ground EM and Mag, soil and basal till sampling, and diamond drilling on a claim block bordering on Oboshkegan Lake, extending southeastwards (MNDM files 2.1304, 2.1979, 2.2236). A government airborne survey found a high density of strong EM anomalies in this area (OGS Map 81291, 81292, 81285). Soil anomalies with values as high as 96 ppm Cu and 460 ppm Zn, and basal till samples with values as high as 625 ppm Cu and 625 ppm Zn were generated. Five coincident EM-soil-basal till anomalies were drilled, only one of these holes is on the property(hole OB4-77). The results were consistently disappointing in that zones containing pyrrhotite and graphite with low base metal values were intersected. Hole OB4-77 was selectively assayed. Only sulphide rich portion were assayed. Significantly, sericitic volcanics with fine disseminated sulphides described in the drill logs were not assayed. Some soil and basal till samples did not coincide with EM conductors. One such zone, on the south shore of the north end of Oboshkegan Lake, called the North Zone by Noranda, was not drilled. At this location the soil anomalies were broader, and only partly coincided with two EM conductors Holmer Gold Mines conducted an extensive airborne survey in 1984. Their southeast boundary is the south shore of Oboshkegan Lake, and the overlapp between their survey and the present property was minimal.

Of greater significance to the mineral potential of the Oboshkegan Lake Property is the historical and current activity and the geology of the Knucklethumb property, which lies to the west, and is bounded to the south and east by the Oboshkegan Lake property (Fig. 4). This property contains 6 gold occurrences that define an east-west trending structure within a felsic volcanic package. Both the structure and the host lithology continue onto the Oboshkegan Lake property. The Knucklethumb property has been under option to Cameco Gold Inc. for the past two years. Exploration on this property has been escalating, and a second diamond drilling campaign is planned for early 1998. Gold was originally discovered on this property in 1915 and the property has been explored intermittently ever since, often for base metals only.

The northernmost two zones are the Etilahxe and MVP zones. The Etilahxe zone has been described as laminated cherty tuff and pyrite, 0.2 m wide, traced for 75m. Grab samples assay results were as high as 1.5807o Cu, Q.98% Zn, 0.64 opt Ag, and 0.017 opt Au. At the MPV zone, pyrite and chalcopyrite bearing veins and veinlets are hosted by silicified mafic volcanics. The zone is l .2 to l .5 m wide and contains up to 5"7o pyrite. A grab sample collected by the Ontario

m- m

OBOSHKEGAN LAKE PROPERTY BEARDMORE - GERALDTON AREA

GEOLOGICAL COMPILATION

ETIAHXE ZONE 0.017opt Au, 0.64opl Aa

PROPERTY LOCATION,

Liiatl^lW*fail

LEGEND

METASEDIMENTS

MAFIC INTRUSIVES

FELSIC INTRUSIVES

COLD OCCURRENCE

SHEARING

PROPERTY

LANDIS MINING CORPORATION (LIS - ASE)

Geological Survey assayed 0.49 opt Au. On the southern trend of gold occurrences, the westernmost is the Jaz occurrence. The mineralization consist of massive, stringer, and disseminated pyrite in iron carbonate altered felsic volcanics. Surface samples assayed 0.71 opt Au over 1.52 m. To the east, the Claimlin zone consist of coarse gold, chalcopyrite and pyrite in sheeted veins in sheared, sericitic felsic volcanics that contain up to 30Xo pyrite. This east trending zone was traced for "several chains". Drill intercepts assayed 0.16 opt Au over 5.8 m and 0.21 opt Au over 3.0m. The Ryne zone consist of sheared and altered felsic volcanics containing fine disseminated pyrite. The zone is east striking, 10 metres wide, and may extend for 120 m. A grab sample of altered felsic volcanics containing disseminated pyrite assayed 0.670 opt Au. The most easterly zone, the Cabin Zone, has produced assays from grab samples as high as 0.137 opt Au. One kilometre east of the Knucklethumb property, along the same trend, the Kipper- Cameron gold prospect received much attention prior to WW2, as evidenced by a shaft and trenches. This mineralization is described as a shear zone along a mafic and felsic volcanic contact.

It is evident from the above compilation of gold occurrence on the Knucklethumb property, that they are contained within a one kilometre wide corridor containing numerous mineralized shear zone. This corridor can be traced for 10 kilometres, onto the Oboshkegan Lake property to the east. Collectively, these numerous shear zones found at the sites of gold mineralization, and mapping in 1996 by the Ontario Geological Survey which characterized much of the rock in this area as strongly deformed (OGS Map P 3365), defines a deformation zone, which will be refered to as the Knucklethumb Deformation Zone. This deformation zone is a significant crustal structure, that has served as a pathway for mineralizing fluids, that can be projected onto the Oboshkegan Lake property with confidence. It has produced various styles of mineralization, a common one being the occurrence of gold in pyritized felsic volcanics over substantial widths. This style of mineralization is more common to the larger tonnage gold deposits, and is a favoured target type.

CURRENT PROGRAM

In the fall of 1997, Landis Mining Corporation conducted a magnetometer and VLF-EM survey on a grid with 40 km of cut line at a position designed to test and find mineralized zones within the strike extension of the east trending, gold bearing deformation zone from the adjacent Knucklethumb property of Cameco Gold. In the southern portion of the survey, well defined northeast trending conductors are coincident with magnetic highs. These are the same conductors that Noranda Explo. Co. found in the course their surveys, and later discovered by diamond drilling to be barren massive pyrrhotite and graphite. These are interflow sediments and the corresponding EM conductors are formational. These strong conductors mask the disseminated sulphides within the hydrothermally altered felsic volcanics that were intersected in Norandas' drilling, and not assayed for gold. Within the north half of the grid, the conductors found are parallel to the Knucklethumb deformation zone. Several half kilometer long, east trending conductors are stacked in an area that is transitional from "normal" magnetic response to one that is low and flat. Based on government mapping, this area should be entirely underlain by felsic volcanics, and the change in magnetic signature is possibly a reflection of magnetite destructive

hydrothermal alteration associated with gold mineralization. The VLF-EM conductors in such an environment can be produced by highly sheared rock, with or without mineralization. A cursory, one day ground check of these conductors by soil sampling and prospecting revealed that the bedrock consisted of strongly foliated felsic volcanics that have undergone sericite and chlorite alteration, contained quartz veinlets and disseminated pyrite. Five samples collected from bedrock north of the conductors did not contain anomalous gold values.

Augers were utilized with the intent to collect B horizon soil sample. In most cases this consisted of the first 15 cm of soil beneath the thick cover of peat. At 4007o of the sample sites, peat was collected as the soil depth was greater than the reach of the auger. Of the 16 soil samples collected, 2 were clearly anomalous in copper, and 3 in zinc. These anomalies coincided perfectly with the conductors. The 25 peat samples collected established a threshold level of 8 ppm for copper, 3 samples exceeding that value, l ppm for lead, 3 samples exceeding that value, 50 ppm for zinc, 4 samples exceeding that value. These geochemical anomalies also coincided with the conductors, but tend to be on the north side.

CONCLUSIONS AND RECOMMENDATIONS

The Oboshkegan Lake property encompasses the on strike extension of the gold bearing, east trending Knucklethumb Deformation Zone which extends for at least ten kilometres to the west. The discovery potential for gold within this deformation zone is perhaps demonstrated by the commitment made to h by Cameco Gold Inc. No record exists of prospecting for gold on the Oboshkegan property, partly due to its remoteness, and to the amount of overburden. Although not amenable to standard surface prospecting techniques, this situation can be dealt with by dependance on geophysical and geochemical techniques. Discovery will depend heavily on the use of geophysical and geochemical techniques and diamond drilling. The presence of graphitic horizons, barren massive pyrrhotite and pyrite, conductive unmineralized shear zones in the midst of the possibility of several styles of gold bearing mineralization, such as sulphide bearing quartz veins, disseminated sulphides and semi-massive to massive sulphides are all possible geological environments which may be present or are expected on the Oboshkegan Lake property. A variety of geophysical responses may therefore be expected.

A similar situation exist at Les Mines Selbaie, a major producer of Cu-Zn-Ag-Au in northwestern Quebec discovered by airborne EM survey. The overall geological environment has affinities to both VMS and late mesothermal gold deposits, as is the case in Oboshkegan. A similar mix of barren sulphides and Cu-Zn-Ag-Au bearing suphides exist. These targets were resolved by using several geophysical techniques. At Oboshkegan, the VLF-EM and magnetic data should be supported by Max-Min EM in order to increase the level of confidence in the selection of diamond drill targets.

The styles of mineralization found at the Knucklethumb property of Cameco Gold would likely respond well to an Induced Polarization E.M. survey. However, thick overburden conductivity such as expected on the Oboshkegan Lake property, require a more judicious use of this expensive method.

In addition to geophysical exploration methods, mineralization can be effectively discovered by prospecting in those portions of the property with outcrop. Many of the areas perceived as

having few outcrops, in fact have flat bedrock with a thin moss cover. It is unlikely that this remote area has ever been systematically, and thoroughly prospected for gold.

PROPOSED WORK PROGRAM

All the geological data for the property and adjoining areas should be scrutinized and compiled. Even though this area has seen more base metal and iron exploration, observations and data generated by these programs may lead to gold mineralization. Based on the amount of data available, 5 to 10 days should be allocated to complete this task.

The present grid and VLF-EM and Mag surveys should be expanded by 160 km to cover the northeast extension of the favourable host rocks and the Knucklethumb Deformation Zone. Forty kilometres of Max-Min EM should be allocated to detail the VLF-EM conductors, and an equal amount of IP-EM should be allocated for additional definition of conductors. Selected geophysical anomalies should confirmed by soil and rock analysis where possible. One thousand gold and base metal analysis should be allocated.

In order to better define the geological structures, delineate zones of higher discovery potential, and discover surface mineralization, the bedrock should be mapped and prospected. The potential of both the east trending and northeast trending structures should be evaluated.

It should be expected that this property could generate fifty or more targets. Twenty of the best targets, those which are confirmed by all the generated data, should be diamond drilled. At least two 100 metre holes per target should be allocated (4000 m).

Data compilation...................................................................53,000.00Geological mapping and prospecting..................................5150,000.00Geochemical analysis, 1000 samples....................................520,000.00VLF EM and Mag survey, 160 km.......................................568,000.00Max-Min EM, 40 km...........................................................514,000.00IP EM, 40 km......................................................................560,000.00Diamond drilling, 4000 m................................................. 5400,000.00

Total..........5715,000.00

STATEMENT OF QUALIFICATIONS

OBOSHKEGAN PROPERTY, LANDIS MINING CORPORATION

I, MAURICE JEAN LAVIGNE, of 193 East Amelia Street, Thunder Bay, Ontario, do certify that

1) I am a graduate of Brock University (H.BSc. Geology, 1979) and McMaster University (M.Sc. Geology, 1983)

2) I have practiced my profession for 19 years since my graduation from Brock University

3) I am a Fellow of the Geological Association of Canada

4) I have no beneficial interest, expressed or implied, in the property discussed in this report nor in the securities of Landis Mining Corporation, nor do I expect to receive any in the future.

Maurice Jean Lavigne January 31, 1998


i

l

l

l

l

1070 LITHIUM DRIVE, UNIT 2THUNDER BAY. ONTARIO P7B 6G3

PHONE (807) 623-6448FAX (807) 623-6820

Page l

SDA GEOLOGICAL Dec 19, 1997 215 VAN NORMAN ST.THUNDER BAY, ONTARIO Job* 9741124 P7A 4B6

SAMPLE # Gold GoldAccurassay Customer ppb Oz/t

1 SDA l ^ ^.0012 SDA 2 ^ CO.0013 SDA 3 ^ -cO.OOl4 SDA 4 ^ -cO.OOl5 SDA 5 ^ .cO.OOl6 Check SDA 5 ^ cO

Certified By:


1070 LITHIUM DRIVE. UNIT 2THUNDER BAY. ONTARIO P7B 6G3

PHONE (807) 623-6448FAX (807) 623-6820Page l

SDA GEOLOGICAL 215 VAN NORMAN ST. THUNDER BAY, ONTARIO F7A 4B6

Dec 19, 1997

Job* 9741124


12345

SDA l SDA 2 SDA 3 SDA 4 SDA 5

Silver ppm

2•ci 2 2

Copper ppm

48

22193

Zinc ppm

1685497518

Lead ppm

1613105

18

Certified By:

Chemex Labs Ltd,Analytical Chemists " Geochemists * Registered Assayers

5175Timbertea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163

To: **un v^i JAL Si., . . .OES, . . — .

215 VAN NORMAN ST. THUNDER BAY, ON P7A4B6

Project : OBOSHComments: ATTN: ABRAHAM DROST

jeNu :1 Total Pages :1 Certificate Date: 30-DEC-97 Invoice No. : 19754163 P.O. Number : Account :NCW

CERTIFICATE OF ANALYSIS A9754163

SAMPLE

L12E-5+OOH L12E-5+12N L12E-5+25N L12E-5+37N L12E-5+50N

L12E-5+62N L12E-5+75N L12E-5+87N L12E-6+25N L12E-7+62N

L12E-7+87N L12E-B+OON L13E-8+50N L13E-B+75N L13E-8+B7N

L13E-9+OON

PREP CODE

201 201 201 201 205

201 201 201 205 201

201 201 201 205 201

205

238 238 238 238 203

238 238 238 203 238

238 238 238 203 238

203

Au ppb EXT-AA

1 < 1

2 < 1

1

3 2 3 1 3

32

< 1 1 4

2

Cu ppm

5 7 5

19 16

12 25

1047 6

157 6 B

55

18

Pb ppm

2 < i

2 5 3

< l 3 3

< 13

15a4

< 1 < 1

1

Zn ppm

17 17 14 29 28

32 55 60 27 15

2426 26 21 26

42

Ag ppm Aqua R

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

< 0.2

CERTIFICATION:.

ChelTleX Ltu.Analytical Chemists ' Geochemlsls * Registered Assayere

51 75 Timberlea Blvd., MississaugaOntario, Canada L4W 2S3PHONE: 905-624-2806 FAX: 905-624-6163

To: snA GEO! OGICAL SERVICES. LTD.

215 VAN NORMAN ST. THUNDER BAY, ON P7A4B6

Project: Comments:

O BOSHATTN: ABRAHAM DROST

Huinuei . i ~ talPf :1 oertifica.e uate:31-ucv-.-97 Invoice No. : 19754162 P.O. Number : Account :NCW

CERTIFICATE OF ANALYSIS

SAMPLE

L10E-7+OON L10E-7+12N L10B-7+25N L10E-7+37N L10E-7+50N

L10B-7+62N L10E-7+75N L10E-7+87N L10E-8+OON L12E-6+OON

Z.12B-6+12N L12E-6+37N L12B-6+50N L12B-6+62N L12B-6+75N

L12E-6+87N L12E-7+OON L12E-7+12N L12E-7+25N L12E-7+37N

L12E-7+50N L13E-9+12N L13E-9+25N L13E-9+37N L13E-9+50N

PREP CODE

217 217 217 217 217

217 217 217 217 217

217 217 217 217 217

217 217 217 217 217

217 217 217 217 217

238 238 238 238 238

238 238 238 238 238

238 238 238 238 238

238 238 238 238 238

238 238 238 238 238

AU ppb EXT-AA

< 1 2

< 1 < 1< 1

< 1 < 1 < 1 * 1< 1

< 1< 1 < 1 * 1 < 1

< 12 2

< 1 < 1

2 1

< 11 2

CU ppm

5 5 55 5

6 4 5 6

11

10 68 67

65 6 5 5

153 3 2 3

Pb ppm

3< l < i < l< i < i < i< l < i< i < i < i< i < l< i < l * l< l < i10

* i < i< i

2

Zn ppm

35 22 23 37 38

3348 4457 62

45 46 5542 43

33 39 3350 43

4430 32 32 55

Ag ppm Aqua R

< 0.2 •c 0.2 * 0.2 < 0.2< 0.2

< 0.2 < 0.2 < 0.2 < 0.2 < 0.2

< 0.2 < 0.2 < 0.2 < 0.2 •c 0.2

< 0.2 < 0.2 * 0.2 < 0.2 < 0.2

< 0.2 * 0.2 < 0.2 < 0.2 < 0.2

A9754162

i —— r-* ————— *V-

APPENDIX V

Report Bv F. Glass

LANDIS MINING CORPORATIONTECHNICAL REPORT 4 INTERPRETATION

OBOSHKEGAN LAKE PROPERTY

Interpretation of VLF/magnetic/IP data of Onboshkegan Lake Property.

An IP survey using the dipole-dipole configuration with a 50 metre dipole

was completed over lines 1100E, 1200E and 1300E from the baseline to 1200N.

Readings were taken with dipole separation nz 1 to r\^G. VLF and magnetic data

of the area of interest was also interpreted to improve the selection of potential

drill targets. Horizontal loop EM surveys were also completed over lines 800E to

1500E at 3 frequencies with a 100 metres cable separation.

Profiles of the magnetic data were plotted for lines 10E to 14E (O to

11+50N). These profiles were interpreted and indicate a non-magnetic rock type

to the north. This rock type is quite uniform in magnetic intensity. A meta

sediment or felsic/granitic intrusion may be present. The magnetic contours show

a broad zone of uniform low intensity in the northern sector of the grid.

On lines 10E to 14E from about station 0+00 to about 5N on line 10E and

to about 8N on line 14E, a 600 nT anomaly is present. This anomaly shows

multiple sources and the northern contact is also irregular. In contrast the

southern contact (0+20N on line 10E and about 2N on line 14E) is better defined

as a single contact. Some of the northern contacts are also faulted; dip is to the

north or vertical (see the compilation map at 1:5000 scale). The irregularity of

the magnetic profile for the 600 nT anomaly is similar to what could be expected

from contact metamorphic effects or from intrusive events, intruding concentric

2

faults or a series of sub-parallel faults. Note that portions of the interpreted

contacts for the 600 nT anomaly have linear trends striking approximately NE.

Depth to source for some of the magnetic anomalies is less than 15

metres for some of the more shallow anomalies and up to 25 metres for some of

the deeper anomalies.

The VLF profiles were interpreted and the conductive zones or conductor

axes have been placed on the compilation map. Between stations 6N and 7N on

lines 10E to 13E, a broad VLF conductor is present; from profile amplitude and

gradient, the source of this anomalous zone is also quite shallow (likely less than

15 metres for the contacts nearest the surface). North and north-west of the local

grid area, the VLF profiles are quite uniform and regular with a subdued

amplitude. Using this relationship, a contact has been interpreted which cuts

across the entire grid, striking approximately NNE to NE. On the north-western

side of the VLF contact, the magnetic field is both subdued and uniform.

Both the resistivity and chargeability data of the IP survey were

interpreted. The resistivity contrasts are more pronounced and better defined

than for the chargeability data. Two conductor zones of bedrock origin varying

from about 20 to 25 metres in depth to about 35 metres in depth have been

delimited; these conductors have resistivity contrasts in excess of 10 to 1 (and

therefore should exhibit the characteristics of EM current channeling). The fact

that the deeper conductors delimited by the IP survey have not been equally well

defined by the VLF or the HEM survey may be explained as follows:

3

i) The broad, near surface horizontal conductive zone between stations 6N

and 7N delimited by VLF will not be defined by a 50 metre dipole-dipole array

because of minimum coupling.

ii) The IP conductors of likely steep near vertical dip with good depth extensions

will not be defined by VLF if a layer of conductive overburden is present. The

IP conductors have depths estimated in excess of 20 metres which is the limit of

detection for the VLF method in conductive overburden. (The resistivity psuedo-

sections do not indicate the presence of excessive overburden near the

interpreted conductor axes; on line 1300E, overburden could be deeper where

bedrock troughs have been interpreted to the south).

iii) The HEM method will typically define only 5007o of those anomalies defined by

the IP resistivity method which exhibit EM characteristics. In addition, large cable

lengths reduce the saturation of EM conductors.

The bedrock conductor areas and possibly a third, situated in a bedrock

trough have been defined by the IP survey. The two most important are situated

near station 8N and near 5N. The third conductor, likely associated in part with a

bedrock trough is near 2N on lines 12E and 13E. The two bedrock conductors

have chargeability response surrounding them but because of the high resistivity

contrasts, the chargeability readings are not stable. These two IP conductors

bracket the VLF conductive zone. The IP conductors also coincide with or are

near faults (same rock) or faulted contacts (different rocks) as have been

interpreted from the profiles of the magnetic survey data.

It is general practice to drill examine a survey line that is bracketed on

each side by survey lines showing a similar geophysical response, particularly for

IP where strike determinations can still result in a well defined response on a

nearby line. For this reason, line 1200E should be selected even if the responses

on line 1100E have higher conductivity. However, the magnetic profiles show

continuity of response on line 1000E, so it should be acceptable to drill examine

the conductor on line 1100E. The drill section for line 1100E is enclosed.

Selecting just one line will be better if fence drilling is later contemplated.

The two drill collars on line 1100E may be positioned at 5+75N, dip 45 degrees

south and at 9+OON, dip 45 degrees south.

The length of both holes will be in excess of 150 metres each; the drill

collars have been positioned to test the conductors at 50 metres below surface

allowing for 15 metres of fresh rock below top. The drill site geologist may

terminate both holes near 150 metres if each anomaly has been adequately

explained. However, the drill at 9+OON may be extended slightly if the fault,

predicted near 150 metres along the hole has not been intersected by that depth.

There should also be a change of rock type.

F. Glass, Geoscientist, Quebec, Que. March 6th , 1998.

CURRICULUM VITAE

FRANK GLASS

71, avenue Wilfrid-Laurier Quebec (QC)

G1R2K6 Tel Z Fax : (418) 522-6105

EDUCATION

1993 Waste Management and Groundwater Resources, special studentGraduate Studies, Department of Civil Engineering Z Applied Mechanics McGill University, Montreal (Quebec)

Project: Co-ion competition effects in metal bio-adsorption (Ni, Cd, Zn)

1992 Global Seismology, Tectonophysics, Graduate Studies, Department of Earth andPlanetary Sciences, McGill

Project Intraplate seismicity and reactivation of relict lineaments

1987 Advanced Electromagnetic Methods in Prospecting GeophysicsSchool of Graduate Studies, Department of Physics University of Toronto, Toronto (Ontario)

1978 M.Sc.(A), Mineral Exploration Program, Department of Geological SciencesMcGill

Project Nuclear industry and processing of carbonatites

1971 B.Sc.(Honours), Geophysics and Geology, Department of Geophysics and Astronomy,University of British Columbia, Vancouver (BC)

1966 Mining Diploma with DistinctionThe Technical College, Bulawayo, Rhodesia

1963 Lord Byng High School (University Program)Vancouver (BC)

F. Glass (cont'd)

WORK EXPERIENCE

1993-present

1987-1991

Contract geophysicist and geologist (exploration manager, project manager) West Africa, North America, S. E. Asia.

. detailed soil geochemistry (insttu regolith) for structural control (Burkina Faso)* structural analysis of reactivated crust for mineralisation controls (West Africa,

central B.C., N.E. Malaysia) and civil engineering (Ha Noi - deltaic loading).* recognition of structural corridors and collapsed blocks from airborne geophysics

(West Africa, Kalimantan).* transported soil and palaeo-laterite recognition.* surficial faulting (civil engineering - Syracuse).* rigid and parallel faulting of iron formation (N.W. Ontario, Labrador) - shortening and

diiational opening.* calibrated aeromag surveys (mining and petroleum), Indonesia, B.C.. Falkland

Islands.* linear regression analysis of regolith conductivity contrasts (multi-frequency AEM -

Ghana).* DDH, RC., company registration and office setup.

Contact mining geophysicist

* Execution of advanced surveys for:

- mining exploration (U/G and surface).- engineering and scientific projects (MT and calibrated TEM for crustal depth

sounding - B.C., geothermal - Japan).- structural mapping (S,, S,, S, - Nova Scotia) and helicopter supported claim

staking (carbonatjtes - Ontario/Quebec).- interpretation of regional and detailed data bases for gold. -

1981-1986 Reid geophysicist (Australia, North America, Mexico) using :

- UTEM.* ground probing radar (digital and analog; low and high frequency) and TOR.- high resolution roll-over seismic.* hole-hole gee-electric.- airborne EM and mag.* advanced digital signal enhancement

Applications :

mining sites (U/G and surface; VMS and brecia pipes).dams (site investigation and discharge control).sub-bedrock profiling and ground water mapping.solid and liquid mudear waste mapping.permafrost mapping (pipe lines).sono-bathymelry (contaminated basins).rock mecanics (P and S - mine tunnelling).rock cavities (stopes, karst topography and potash mines).

F. Glass (cont'd)

1971 -1981 Senior geophysicist for Geoterrex Ltd (Ottawa)

- airborne EM (INPUT) and ground follow-up surveys of AEM (Australia, U.S.A.).. advanced aero-mag interpretation (CGG method).' multi-disciplinary programs (mapping, DDH, geochemistry).

Project manager/chief geophysicist SOQUEM (Quebec).

- DDH, lake geochem, mapping.- daim administration.

1968-1970 Reid geophysicist and chief sampler (U/G and surface lithogeochem). Canada.

1964-1967 Learner mine official; hard rock tin mine in schist horst (O/C and U/G - 50 000 t/mo),concentrator and smelter. Billiton, Kamativi, Zimbabwe.

- mine surveying (U/G and surface).- ore reserves and sampling (DDH and venturi).- U/G mapping (structural, faces).

RECENT SHORT COURSES

Jan. 1994 Structural geology ; G.S.C., Ottawa

Jan. 1997 Tropical geochemistry ; M.R.D.U., Vancouver

APPENDIX VI

Diamond Drill Hole Loas

Diamond Journal de Complete this lorrn and1 Wl Nonnern ueveiopmem ueveioppemenl au Hora DrM|ina forage BU w""*d **lch In duplicate. Fill in on every page Hole No. Page No SJ 8ndMine8 8ld88MineS LOQ diamant R.n,P,,r en deux ex.mpl.,re. ,. Retirees cases a t 01113110 L09 """"am presente tortnule et le croqule annex* chaque page F Lo ao 0, | /x

Drilling Company Collar Elevation Compagnie de forage Elevation du collier

Date Hole Started Dale Completed Date Logged Date de commencement du forage Date d'achevemenl Date description au

journal

JULY 12 , l^nS7 -JU/.V S.mS* OT/isAlo*Exptoratlon Co.. Owner or Optionee ' Date Submitted Compagnie d'exptorallon, proprieialre ou titulalre d'oplion Date de depot

L- f\*~SV3\ ^ fA i M i K) (S CDFLPOfeATioN

Footage/AvancementFrom/De

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llfO.t

Rock Type Type de roche

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J/uTEBLMrfrk/AT?

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Betrmg of nolt Irom true Total Footage Dip ol Hole at ' NomvPositiHi du foreoi Avancement total du Indlnaison du forage au pv ripport au md vrai forage

34O 0 2.3lrsA co..,,co*.r| - 4 5 0Logged by Inscrltpar -.f- , ne. O

(JO IA-C? rftRJCE K- 'Submitted by (Signature) l c/^...,-.! .. (J C. 1' Depose par (^gnalure) 1 WM fim \ —— 1L3—-

\. ^*\. S 7'j\ 1 in* N. N x^ ^ jJr-^ f"p| l ~ 4t

F1./PII

Description (Colour, grain size, texture, minerals, alteration, etc.) Description (Couleur, granulometric, texture, mlneraux, transformation, etc.)

L-,Gu-r f^RLAV T P

P. ft K.\ c rrKiTTt qTi

P"C L-t) S P Afe (i R- ft

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\ •For features such as foliation, bedding, schistosity, measured from the long axis of the cor*.•Examples de caractertstlques : foliation, schlstoslte, stratification. L'angte est mesure par rapport a I'axe longitudinal de la carotte.

t Additional credit available. See Assessment Work Regulation.t Dei credits luppMmentalrei lonl offerti. Contulter let reglementi relatlft aux travaux devaluationNota : Ding cette formuto. lorequ'U detigne dm peraonnet. to muculln m utilise au wni neulre

Diamond Journal de Complete this form amtV2^ an^Min.,"" r e, des Mm., " " Drilling forage au Ontario Log diaiTiant——————————————————————————————— T" —————— 1 ————

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t Additional credit available. See Asaessmen Work Regulation.'t Des credits suppMmentaires sem offerts. Consulter lea reglemaws ralatils aux (ravaux d'evaluatNoli : Dam cam tonnule. lonqu'U Maori* m pcnonnn. li muculin ut uiuii* iu wni niuiri

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wimstry o* Mimstere du Diamond Journal deNorthern Development Developpement du Nord I. ?" iand Mines et des Mines Drilling forage 8U

Log diamant

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t Additional credit available. See Assenrnem Work Regulation.t Des credits suppMmentairm son ofletts. Consutt.r tos regl.mems relatifs aux Iravaux d'.valuatNou : Dim cm* torniule, loraqu't (Meqnt an pwionnn. K muculm til ullliX iu wnt n*uira

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M04IU/I1) -For features such at foliation, bedding, schistosity, measured from the long axis of the core. T Additional credit available. See Assessment Work Regulation. ' Examples de caractertstiques : foliation, schistosity stratification. L'angle esl mesure par rapport a I'axe longitudinal de la carotte. t D*s credits supplemental^ sont oflerts. ConsuBer les reglemenis relatifs aux Iravaux d'evalual

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Ontario Ministry ofNorthern Developmentand P*ne8

Declaration of Assessment Work Performed on Mining LandMining Act, Subsection 66(2) end 66(3), R.S.0.1990

Transaction Number (office use)

Assessment Files Researcntmaging

subsection 65(2) and 66(3) of the Mining Act. Under section 8 of the Mining Act, issesment work and correspond with the mining land holder. Questions about this lorthem Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury,

42L03NW2004 2.19111 OBOSHKEGAN 900Thunder Bav

Instructions: - For work performed on Crown Lands before recording a claim, use form 0240. , . .^^- Please type or print in ink. L..,, i 5 '~^o

1. Recorded holders) (Attach a list if necessary) xU^Ciii V &UName John Edward Temowesky SAddress 132 Robinson DriveThunder Bay, Ontario M5H 3V5Name

Address

Client Number 200961Telephone Number (807) 767-1862Fax Number (807)767-1528Client Number

Telephone Numberp 1 Q

FaxNumbefC* * JL *7 1 1 12. Type of work performed: Check (S) and report on qpJ/ONE of the following groups for this declaration.n Geotechnical: prospecting, surveys, i-' assays and work under section 18 (regs)

Physical: drilling stripping, trenching and associated assays

Rehabilitation

work Type Diamond Drilling, geological evaluation, assays and reports.

Dates Work From To Performed Day 1 j Month 10 | Year 1997 Day 14 | Month 09 | Year 199S

Global Positioning System Data (if available) Township/Area Oboshkegan

M or G-Plan Number G-173 Oboshkegan Lake

Office UseCommodityTotal S Value of Work ClaimedNTS Reference

Mining DivisionResident Geologist District

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. Pereon or companies who prepared the technical report (Attach a list if necessary)Name Douglas P. ParkerAddress 365 Lark Street Thunder Bay, Ontario P7B 1P4Name Matawin Mineral Exploration (Maurice Lavigne)Address 193 East Amelia Street Thunder Bay, OntarioName Frank GlassAddress 71, Avenue Wilfrid-Laurier, Quebec (QC) G1R2K6

rRECFiVED"—— D|CJ5 ;"j ——

3 -306 dutuhutlYCE ASSESSMENT

—— Q^IHF

Telephone Number (807) 345-3860Fax Number



4. Certification by Recorded Holder or AgentI.. ~ , do hereby certify that l have personal knowledge of the facts set forth in

(Print Name)this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, the annexed report is true.Signature of Recorded Holder or Agent

Agent's Address Landis Mining CorporationSuite 400, 604 - First Street SW Calgary. Alberta T2P 1M7

Telephone Number (403)263-2118

Fax Number (403)263-0135

0241 (03/97)

1C

5. Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to the mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany this form. i - - i..-, . c )

Mining Claim Number. Or rf work was done on other eligible mining land, show in this

column the location number indicated on the claim map.

eg

eg

eg

1

2

3

4

5

6

7

8

9

10

11

12

13

14

15

TB7827

1234567

1234568

1216584

1215528

1215529

1215530

1215531

1215532

1215533

1215534

1215526

1215527

Column Totals

Number of Claim Units. For other mining land, list hectares.

16 ha

12

2

9

15

10

10

15

12

15

16

8

16

Value of work performed on this claim or other mining land.

526,825

0

$ 6,892

S407

S5971

110,322

S77.790

SWA

1101,004

Value of work applied to this claim.

N/A

524,000

54,000

S3,600

56,000

KOOO

54,000

56,000

54,800

56,000

56,400

53,200

56,400

f^

S50,400

Value of work assigned to other mining claims.

524,000

0

0

529,222

T! Q 1

S29.222

Bank. Value of work to be distributed at a future date

52,825

0

54,892

16322

S42.568

S1.714

1 Tl

S50,604

i. , do hereby certify that the above work credits are eligible under(Print Full Name)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim where the work was done.Signature of.'JJeewdedHoldei

, l YU^t'riling Date

6. Instruction for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check (S) in the boxes below to show how you wish to prioritize the dejetion of credits:

Q 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated.D 2. Credits are to be cut back starting with the claims listed last, working backwards; orD 3. Credits are to be cut back equally over all claims listed in this declaration; orO 4. Credits are to be cut back as prioritized on the attached appendix or as /oil

Note: If you have not indicated how your credits are to be deleted, credits will be cut back followed by option number 2 if necessary.

For Office Use Only_______________^_Received Stamp

0241 (03/97)

Deemed Approved Date

Date Approved

Date Notification Sent

Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

. '5 .

Statement of Costs for Assessment Credit

Transaction Number (office use)

Personal information collected on this form is obtained under the authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining Act, this information is a public record. This information will be used to review the assessment work and correspond with the mining land holder. Questions about this collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 6B5.

Units of work Work Type Depending on the type of work, list the number of

hours/day worked, metres of drilling, kilometres of grid line, number of samples, etc.

Line cutting 41.25km

Magnetic and VLF surveys 41 .25 km

Assays 148

Max min (HLEM) survey 1 1 km

IP Survey 3 Km

Diamond Drilling 500 mGeology, prospecting, core splitting, etc 44.5 days Digitizing and plotting

Average cost per day

Associated Costs (e.g. supplies, mobilization and demobilization).

Associated Costs Phone, Fax, and other supplies

~

Transportation Costs ^

Air, Boat mileage

Food and Lodging Costs

Food

Lodging| RECEIVED

Cost Per Unit of work

S321

S1 33.75

S86.187m3249/day

.1911)

DEC 1 6 I., 3 JTotal Value of Assessment Work

GEOSCI?N'CF ASSESSMENTOfFiCE

Total Cost

SI 3,240 '

55 517

S2.540

S5.072

S5,450

S43.091311,085 S406.60

52,412

S7.673

S2.631

51,887

3 101,004

1. Work filed within two years of performance is claimed at 10007o of the above Total Value of Assessment Work.2. If work is filed after two years and up to five years after performance, it can only be claimed at 50"7o of the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0.50 Total S value of worked claimed.

Note:- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 45 days of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifying costs:

____, do hereby certify, that the amounts shown are as accurate as may reasonably(pteaseprint full name)

be determined and the costs were incurred white conducting assessment work on the lands indicated on the accompanying

Declaration of Work form as(recorded holder, agent, or state company position with signing authority)

l am authorized to make this certification.

0212 (OV97)

Sinature Date

;5

OntarioMinistry of Ministere duNorthern Development DeVeloppement du Nordand Mines et des Mines

Geoscience Assessment Office 933 Ramsey Lake Road

March 10, 1999 6th FloorSudbury, Ontario

ABRAHAM PETER DROST P3E 6B5304 OTTO STREETTHUNDER BAY, Ontario Telephone: (888) 415-9846P7A-2T9 Fax: (877)670-1555

Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Dear Sir or Madam: Submission Number: 2.19111

Status Subject: Transaction Number(s): W9840.00678 Approval

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact Lucille Jerome by e-mail at [email protected] or by telephone at (705) 670-5858.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 13474

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2.19111

Date Correspondence Sent: March 10,1999 Assessor: Lucille Jerome

Transaction NumberW9840.00678

First Claim Number1216584

Township(s) 1 Area(s) OBOSHKEGAN

StatusApproval

Approval Date

March 10, 1999

Section:17 Assays ASSAY 14 Geophysical IP 14 Geophysical MAG 16 Drilling PDRILL 14 Geophysical VLF 14 Geophysical EM

Assessment work credit has been redistributed, as outlined on the attached Distribution of Assessment Work Credit sheet, to better reflect the location of the work.

Correspondence to: Recorded Holder(s) and/or Agent(s):Resident Geologist David BirkketThunder Bay, ON CALGARY, ALBERTA

Assessment Files Library ABRAHAM PETER DROST Sudbury, ON THUNDER BAY, Ontario

JOHN EDWARD TERNOWESKY THUNDER BAY, ONTARIO

Page: 1Correspondence ID: 13474

Distribution of Assessment Work Credit

The following credit distribution reflects the value of assessment work performed on the mining land(s).

Date: March 10, 1999

Submission Number: 2.19111

Transaction Number: W9840.00678

Claim Number Value Of Work Performed

1216584 5,971.00

1215528 407.001215530 10,322.001215531 77,790.001215532 6,514.00

Total: S 101,004.00

Page: l

Correspondence ID: 13474

NOTES!- : cationt W Open For Staking Ste. IHcl

42L03HW2004 2.19111 OB03HKEOAN 200THF INK iMMATU )N 1HA1APPEAR:, ON THIS MAPHAS RF EN COMPILED fHOM VARIOUS oOURCtS ANO ACCURACY IS MOT GUAHAN T E t IJ i rnjL.i.WISHING TO STAKE MIN ING CLAIMS SHOULD OON SUIT WITH THE MINING RECORDER. MINISTRY OF NORTHERN DEVELOP MENT AND MINES FOR AD- DITIONA1 INFORMATION ON THE STATUS' OF THE LMNDS SHOWM HE-REON

uD

-l

IjJ

u. J

o

GZOWSKI TP. (G - 182)

1215349 VI2I590U

'1216519i 1216^18

^•^"^216625

121601215534 216626

1216007 ^15657 T s* —— lL.^s,^ j207198

1207146 ' 1210507 ! 1215.513

i 1202236 120*8282;i^-'2; 5?b3 2.264 ,' 3145

—r.-i--*-i2i36i5yiS; 12105051210506 215530l l l—— l **f ***r ^r ^" f j p—.-"-—

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ASS A^ \3RAHSTROM

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COUGHLAN LAKE (G-26) ONAMAN LAKE (G-IOf-)

APR Q fi

H;JHV r AND .^•*

TRAILS SURVCV C 0 LlN'ES

TOWr.n HP?. 3' F L TS. elfLOTS, '.'i' 1 1C, CLAIMS. PARC. ' S.

UNSURVtYED '.i SSjLOT LINESPARCEL BOON;MININC CLAI'V ETC

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UTILITY LINES NON-PERENNIAL. .1!:-*,., P LOOPING OR FI 00.: r, - .iGUin SUBDIVISION C:. 0. i; .;. TE PLAN Rt 'E^^'AT'ONS

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SCALE: 1 ifJCH - 40 CHAINS

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THUNDER 5A VL^NH TITLES ' REGIST" V DIV.SION

3AY

Ministry of ; ]Natural Monags ientResources Broncti

Ontario

Date P'.nNo.February , 1981 'l

G-173

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42L03NW2004 2.19111 OBOSHKEGAN 210

LANDIS MINING CORP.OBOSHKEGAN LAKE PROPERTY

Oboshkegan Lake Area. ON (42L/3)GROUND MAGNETIC SURVEYTOTAL FIELD CONTOUR PLAN MAP

(Diurnal Corrected)Magnetic Datum- 58, ."500 nTMagnate Indinofon: appro*. 77degNMagnetic Declination; - aponw. 5degWDiurnal Correction- Base Staliofi (60 sec/gyc)Station Interval; 12.5 metres Bow L&sd (temwed on Postings 'SSQQOnTGridding Metliod; RandomGrid Cell Size; ' -'25mContour Interval: 5Q; 250, 1000 nTOdour .Zoning; Equal Area / Colour. Vi-

Survey Date; Inatnjmentation:

, .1997 GEM GSM 19 (MarVLf)

KES - MFnsmbby.

QUANTSC CONSULTING /JVC

500W 400W 300W 200W 100W O 100E l

200E 300E 400E 500E 600E l

700E 800E 900E 1000E 1100E 1200E 1300E 1400E 1500E 1600E l l l

1700N -

1600N-

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1400N-

1300N -

1200N -

1100N-

1000N

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600N-

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6005-

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22.6 v 17 25.1 --16-.0 20.3 - 19.5)f -Jfl.O - -17

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GEOSCIENCF ASSESSMENT OfFlCE _

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2C.3 - 17.S 27.* -- 17.3 X Scale 1:5000

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Oboshkegon Lake Area, ON (42L/3)VLF EUECTROMAGNETIC SURVEY

IN PHASE/OUT PHASE PROFILE PLAN MAP Cutter. Maine, USA (NAA) -

-24,0'hHz qpprox. NtOO deg

. 12.5 metres Neq-lo-Pos heading H or t 20 (bgBe^o.possrt.fieg^rt]

In Phase: ' sialid Line wilh box. Posted. Top/Left Out ot Phase:DdSheiJ Line with X,

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42L03NW2004 2.19111 OBOSHKEGAN 230

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VLF EM SURVEYIN-PHASE FRASER FILTER PLAN MAP

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42L03NW2004 2. 19111 OBOSHKEGAN 240

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OBOSHKEGAN LAKE AREA NTS: 42 L/3HLEM SURVEY 444 Hz

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42L03NW2004 2.19111 OBOSHKEGAN 250

Note: In-Phasfl Profile Base Level

UNDIS MINING CORP.OBOSHKEGAN LAKE PROPERTY

OBOSHKEGAN LAKE AREA NTS: 42 L/3 _____HLEM SURVEY 1777 Hz_____

Instrument: Max-Min II Coil Sep. 100 mProfile Scale: 1 cm ^ 2.535In-Phase Profiles: Solid Line

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42L03NW2004 2 . 19111 OBOSHKEGAN 260

Note: In-Phase Profile Base level 6S


OBOSHKEGAN LAKE AREA NTS: 42 L/3HLEM SURVEY 3555 Hz

Instrument: Max-Min II Coil Sep. 100 mProfile Scale: 1 cm = 2.5X

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42L03NW2004 2.19111 OBOSHKEGAN 270


OBOSHKEGAN PROPERTY (MAP 10)

SECTION 1200EBAR SCALE 1cm. - 25 ppb Au

DOUG PARKER

DATE: 98/09/03 SCALE: 1/500

RES394CL

1970.

IP MF 22., 6.5.

3.2-

oJ o. i i t i \ /\ i lvl i i VK i i i i y

•\v jV - ——————— J

MF iP -6.5 r22

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RES ..3940

625

)N | .2+00 N t 3tOON | | 4+00 hi | | 5+00 N, | 6+pO N ( ^ 7+00 N^ f | B+OOJj^

1645 2234 1578 696 495 1968 1922 2305 3288 3024 876 836 28H 358Z 1361 642

t 10*00 N | , 11+00 N

666 422 398 431Resistivity

n*l 6M 635 \ 337 ^ W -^ 122 111

n*2 725 wVja m^™^(1 = 3 569 617 622 1 288^ \m 1230

n^4

n=5 647

n-6

519 ( 614.' Jjjfy^'™ "^sl^V

" i^.y^y^ ^333 ^ 'ffi8341 — iOK^ 471*641

1159 1060 —J+W ^r 1228 2003 VVM4

1+00 N 2+00 N 3+00 N 4+OON 5tODN 5+OON 7+00 N 8+OON

0.64 0.43 0.90 0.68 0.46 -0.75 -2.3 1.8 2.3 -3.2 0.95 -J.6 -2.2 2.8 1.6 7,4 -0.80 -7.9 20 0.44 0.12Chargeability

0=1 0.88 , ^65

0=2 0.93 0.93, , 0.71 0,46 -0,18

0=3 1 f'.' '0.28 " 0.44 -0.47

0=4 0.47 -0.062 -0.25

0=5 0.25 -0.29 . O

^=6 0.0030 0.38 " f 2

0.53 - - 0.49 0.20 0.26 O.SO 0 = 10.81——1.53.7 3.3 \ Q. 44 ^ '-\ ' ( .2.5 2.4" —— ~ 1.9 s 1.3 f 4.S

0.67^t-2.45 -3.4 ~ 0. -1.3 -36 0.031-.47 -1.1 -7.8 1 .3 "- ~ T.57 S 2.Srt ' 1 - B

'^ste.- ^^^0.60 ' 3.2 - -8 0.19 0.41 — 1.3

0.1GJ.2 4.4

1.5 -t. 2 -10 -1,9 -119

0.92-^1.9 -C" 1.2.'t// ) L' . X

1+00 N 2+00 N 3+00 N——l———————H

6+00 N———l———i———H7+00 N 8+OON 10+00 N

———l———————h-11+OQN

l 0.62 1.4 1 0.57 -27 -83 -2489 1.3 O.E2 -115 0.22 -2481 -29 2.3 -0.79 -15 -8.4 5.9 1.3 1.3Metal Factor

0=2

1-4 1 3.4 3.3 4.8 4.4 1.2 1.8 0.84 0.88 O.J7 Q. IS 3.1 3.2 7.7 3.4 i. B 3.5 3.6 2.6 4 t.4 r^1

1.3 1.5 1.7 1.4 -1,8 0,72 2 1.2 1.7 2 1.2 7.9 1.4 2.8 -9.2 1.6 2.2 1,3 2.2 0.66 3.9 11=2

1.8 0.43 0.70 -1.6 0.74 1.3 0.87^-0.55 1.7 1.5 0.6S 0.44 0.66 1.1 -6.6 0.37 -20-44 1.3 -1.5

0.90 -0.076 -0.43 0.24 1.1 0,62 ;" , 15 -68 0.88 1.8 0.11 1.8 -13 -J46 0.55 __ 5 ' 4^fC-S)T '5 ' S 0 - 3*

0.38 -0.36 0.15 0.35 0.72 -8 -1003 1.7 6.2 0.48 0,25 -3.1 -10 -80 19 \S 0.74 "*1.8 -7.2

0.0047 0.0+5 0.2D O 32 -6.4 -318 -14 -30K 0.56 0.42 -0.29 3.8 *"-^5 ** -58 2.8 0.46 0.63

[1=3

0=5

[1=6

Line 1100 E

Dipole-Dipole Arraya na a

r8!a = 50 M

V plot point

Logarithmic Contours 1, 1.5, 2, 3, 5, 7.5, 10,

INTERPRETATION

B Strong increase in polarizationaccompanied by marked decrease in resistivity.

O Well defined increase in polarization without marked resistivity decrease.

d Poorly defined polarization increase with no resistivity signature.

T Low resistivity feature.

SCALE 1:500050 O 50 100 150 200 250 300

•d......'Si(metres)

MAP 7

LANDIS MINING CORPORA! ONINDUCED POLARIZATION SURVEYOBOSHKEGAN UVKE PROPERTY

OBOSHKEGAN LAKE AREA ON. NTS 42L/3Date: 98/02/26Interpretation:

GREY OWL RESOURCESCeosoft Software for the Earth Sciences

42L03NW2004 2.19111 OBOSHKEGAN 280

RES IP 4760- 4.6-

2380-

MF 22-,

2.4J 11.

OJ 0.

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RES ^4760

-2380

1-+OON 2+00 N 3+OON 6+00 N 10+00 N

0 = 1

500Resistivity

2588

11=2

(1=3

11=4

11=5

11=6

5tOON 7+00 N 9+00 N 10+00 N 11+OON0.41 1.1

n-1

n=2

^=3

(1=4

11=5 0=6

3.7 1,8 3.6 1.6 -0.28 2.2

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-3.1 0.073 0.53 -0.38Chargeability

-0.039 -0.45

-0.19 -2.e -5.9

0.34 0.30 0.086 0.22 0=1

.5 0.11 0.29 -0.23 0=2

-2.1 -0.080 -0.13 0=3

-0.33 0=4-4.3

Q.SB ' 1.9 Z.4

11=5 11=6

2+00^ 5+OON 4+OON 5+OON 6MMN 7+00 N &+OON 10+00 N 11+QON0.62 1.1 0.62 8.9 3,2 -5.4 20 -14 -45 -5.4 -S.9 -11 -16 -42 -2.8 -0.61 -2.3

45 s 0.81 --- 1. -9 0.83^^-t1.1's -7,2 D.M 1.JJ/ -2.3

-27 -15 0.28 '-sCi^jL -12 -0,42 ' "'-0.56

-31 -66 -3,5 -1.6 A. 1"- 5 * -9 ' 7 -1-5

-86 -33*"^ 2.1 ^-2i -19

0.25 -S.4 -18 -41 -361

Metal Factor

O LU

UJoUJ DC

Geosoft Software for the Earth Sciences

oo

Q

oo

oUJ

Line 1200 E

Dipole-Dipole Arraya na a

liter

' d ^ 50 M

Vplot point

Logarithmic Contours 1, 1.5, 2, 3, 5, 7.5, 10,

INTERPRETATION

B Strong increase in polarizationaccompanied by marked decrease in resistivity.

D Well defined increase in polarization without marked resistivity decrease.

O Poorly defined polarization increase with no resistivity signature .


SCALE 1:500050 O 50 100 150 200 250 300

BS b(metres)

MAP 8

LANDIS MINlsfG CORPORATIONINDUCED POLARIZATION SURVEY OBOSHKEGAN LAKE PROPERTY

OBOSHKEGAN LAKE AREA ON. NTS 42L/3Date: 98/02/26 Interpretation:

GREY OWL RESOURCES

42L03KW2004 2.19111 OBOSHKEGAN 290

RES IP MF 4421-, 3.8^ 6.1

2210. i.d1.9J 3.1.

OJ 0.

WF IP RES n6.1 ^3.8 ..4421

Li. 9 ,

o Lo

2210

.-O

1+00 N 2+00 N 3+OON 5+OON 6+OQN 7+00 N &+OON 9+00 N 10+00 N 11+flON

1055 506 760 !!29 747 1*26 1921 263! 3380 1Z21 1676 1430 4019 2626 1196 7S4 672 635 522 555

436 464 353 Nl l 2563 ^^441

N. 1556 -811

5B7\ 1672 - 951 ^l .-x ^X\

2091 3589 1617 1368 2313' MOK —' 7668 '' 5!7 549 271-^-795 887

Resistivity

1+00 N 2400 N 3+OON 4+OON-H———l———H5+OON

0.80 5.9 3.5 -4,4 -t.3 1.4 1.5 !.B

6+00 N | 7*O)N 2.2 2.4 1.S 2.6 3.4

-Sff^———52^———n^ Chargeability5 1.4 1.9 O.J5 0.71 D.7D

6+OON—t———'———h' .

3 2.5 1.4 1.9 0.75 0.71 0.70

-71 0.55 1,5,1- 0X,64 Vl.6xVV ^, .^ ) X

-90 I.I 1.3 ' 0.44 1-9

1+00 N 2+00 N J+OON 4+OON 9+00 N 10+00 N 11+00 N k i , , r ,^—'—'——'——'——'— Metal factor3.8 -147 1.2 2.6 4,4 -42 -56 2.2 2.4 1.7 1.5 2.8 1.2 5.6 1.1 0.89 2.5 3.1 4.5 1.2 1.5 1.3

5.2 2.8,— 2.

2.3 __ 2.4 t V 0.21 0.92 [1=24.1 1.8 2.8

,40 0.29 0.39 .9- -0.14 -x 1.5

1=1 7.4 M -0.77 ,,Z, 5.4

0=2 2,6 |[( -0.

[1=3

(1=4 2.7 rZ M UJk'K.ti. —— i.* "J,

^=5 275"^ -516 E TOT' 0.'[1=6 iU -790 0.51' 0.36 0.27 0.15

Line 1300 E

Dipole-Dipole Arrayno

Filterr0"!

a = 50 M

Vplot point

LogarithmicContours ^ 5 7 5 10 ' J ' D ' ''*' 10 '

INTERPRETATION* Strong increase In polarization

accompanied by marked decrease in resistivity.

D Well defined increase in polarization without marked resistivity decrease.

D Poorly defined polarization increase with no resistivity signature.


SCALE 1:500050 O 50 100 150 200 250 300~ "- ———"" d i b """————————

(metres)

MAP 9LANDIS MINING CORPORATION

INDUCED POLARIZATION SURVEYOBOSHKEGAN LAKE PROPERTY

OBOSHKEGAN LAKE AREA ON. NTS 42L/3Date: 98/02/26Interpretation:

GREY OWL RESOURCESGeosoft Software for the Earth Sciences

42L03NH2004 2.19111 OBOSHKEGAN 300

9+OON

8+OON

7+OON

6+OON

5+OONorHm

ra

l

4+OON

3+OON

LEGEND

3 FELSIC TUFF

2 INTERMEDIATE TUFF

t MAFIC VOLCANIC

Foliation Vortical, Inclined

Outcrop

LOW43 0 1990 Diamond Drill Hole

4 * Soil Sample Au (ppb)

966(279) A '•rob Sample Number (Au ppb)

Part of Claim 1215531

Scale 1:2500O 50 100 150

(meters)



OBOSHKEGAN PROPERTYGEOLOGICAL AND GFJKHEMICAL COMPILATION

FIGURE 5

DOUG PARKER

9-fOON T

8-r-OON

7+OON

6+OON

5+OON

o w m

ea Oea o 4+OON

3+OONl")o

L9E L10E L11E L12E L13E

50

L14E

GEOPHYSICAL COMPILATION

' ^ MAG PROFILES ( 1 cm - 500 nT)

N Bow Lev*) 56700 nT

O) IP CHARGEABILITY

ft f. IP RESISTMTY

VtF FTWSER riLTER CONTOUR

Part of Claim 1215531

LU

UJO LUOC

Scale 1:2500O 50 _100

(meters)

CO CDCO

CO ^'— i-u —CJ " 0uj a Q ^

150

LAMIS MINING CORPORATION

OBOSHKEGAN PROPERTYGEDPYSICAL COMPILATION

FIGURE 7

DOUG PARKER

RPT ON THE PHASE I EXPL PROG - Geology Ontario

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