December, 2006

REPORT ON GEOPHYSICAL SURVEYS TAHOE LAKE PROPERTY

MacDOWELL LAKE AREA RED LAKE DISTRICT, ONTARIO

NTS 53C17

2.33825 Paul Chamois, M.Sc. (A), P. Geo.

D JAN 0 4 2007

GEOSCIENCE ASSESSMENT OFFICE

REPORT ON GEOPHYSICAL SURVEYS TAHOE LAKE PROPERTY MacDOWELL LAKE AREA

RED LAKE DISTRICT, ONTARIO

Table of Contents Summary Introduction Location & Access Property Description Geological Setting

History

Regional Geology Local Geology

Rock Types Metamorphism Structure

Previous Work by Other Parties Government Mapping Regional Exploration Property Exploration Geology Geophysical Surveys Diamond Drilling

Previous Work by Candor Ventures Work Performed Interpretation Conclusions & Recommendations References

Table 1: Table 2a: Table 2b: Table 3:

TABLES

Tahoe Lake Property Claims Data North Spirit Lake Assemblages North Spirit Lake Intrusions Tahoe Lake Lines

Page

1 2 2 2 5 5 8 8 9 9 9 9 9

10 10 11 11 11 12 13 15 16 17

2 5 6

13

Figure 1: Figure 2: Figure 3: Figure 4:

FIGURES

Tahoe Lake Area Location Map Property Geology Geological Assemblages Tahoe Lake Lines

APPENDICES

Appendix I Specifications and Descriptions of Instrumentation. -GEM Systems GSM19 Magnetometer -Apex Parametrics Limited MaxMin I System

Appendix II Stacked Profiles of Surveyed Lines -Line "A" Scale 1 :2500 -Line "B" Scale 1 :2500 -Line "c" Scale 1 :2500 -Line "D" Scale 1 :2500 -Line "E" Scale 1 :2500

11

3 4 7

14

SUMMARY

The Tahoe Lake property is located approximately 170 kilometers north northeast of the town of Red Lake, Ontario within NTS 53CI7. The property is wholly owned by Candor Ventures Inc. (Candor) and consists of three unpatented mineral claims totaling 768 hectares. The property is accessible by float/ski plane from the town of Red Lake. The winter road from Red Lake to North Spirit Lake is located approximately 15 kilometers to the west of the property.

The most recent government mapping is by Wood (1980 and 1988). Prior to Candor's acquisition of the property, the only documented exploration was in 1976-1977 by The Hanna Mining Company who conducted geological mapping, ground magnetic and Max-Min surveys and 512 meters of diamond drilling in six holes. In 2005, Candor completed an AeroTEM II helicopter-borne electromagnetic and magnetic survey of the property resulting in the identification of several high priority conductors.

The Tahoe Lake property is underlain by mafic to intermediate volcanics and pyroclastics, intermediate to felsic volcanics and pyroclastics, clastic metasediments and chemical metasediments. There is evidence to suggest that the volcanics are hydrothermally altered. Mineralization consists of pyrrhotite and pyrite occurring together as massive seams, stringers and disseminations in both the matrix of felsic tuff-breccia and cross-cutting felsic and intermediate tuff and lapilli-tuff. Chalcopyrite occurs in a few instances as specks, stringers and seams associated with pyrrhotite and pyrite.

The geological setting of the Tahoe Lake property, including the hydrothermally altered intermediate to felsic pyroclastic rocks and folded chert magnetite iron formation with associated grunerite-chlorite-gamet alteration indicates the potential for gold and base metal mineralization.

Work in 2006 consisted of line cutting and reconnaissance ground geophysical (magnetic and HLEM) surveys across five AeroTEM II anomalies identified in 2005. Four conductors were identified on the ground that could be considered drill targets. Three of these are associated with strong magnetic anomalies thought to be iron formation related. The fourth conductor occurs in the vicinity of felsic volcanic rocks and may be prospective for massive sulphide mineralization.

It is recommended that the immediate area of the four target anomalies be geologically mapped in order to prioritize them for diamond drilling.

1

INTRODUCTION

Candor Ventures Corp. (Candor) wholly owns three contiguous claims totaling 48 claim units in the MacDowell Lake area of Ontario. Previous work by Candor had identified helicopter-borne electromagnetic anomalies on the property. The property is considered to be prospective for volcanogenic massive sulphide (VMS) mineralization.

This report describes the results of horizontal loop electromagnetic (HLEM) and magnetic surveying completed during October, 2006 and makes recommendations for additional work.

LOCATION AND ACCESS

The Tahoe Lake property is located approximately 170 kilometers north northeast of the town of Red Lake, Ontario (Figures 1). The property is located in the Red Lake Mining District on the Mattson Lake Area (G-1819) claim map sheet, NTS 53CI7, and is centered on co-ordinates 5 800 OOON / 512 500E (UTM Zone 15, NAD83).

Access to the Tahoe Lake property is best by float or ski plane from the town of Red Lake. Since Tahoe Lake is too small to land on, access is from Mattson Lake and then north by foot along an old winter road for 3.0 kilometres to Tahoe Lake. The main winter road from Red Lake to North Spirit Lake is located approximately 15 kilometres to the west. The First Nations settlement of MacDowell Lake is located 17 kilometres to the south on the southwest shore of MacDowell Lake. The North Spirit Lake First Nations settlement is located 22 kilometres to the northwest on the southwest shore of North Spirit Lake.

PROPERTY DESCRIPTION

The Tahoe Lake property consists of three unpatented and unsurveyed mineral claims (3004452-3004454 incl.) totaling 48 units and 768 hectares (see Table 1 and Figure 2). The property is wholly owned by Candor.

CLAIM # CLAIM UNITS SIZE(HA) RECORDING DATE 3004452 16 256 January 30, 2004 3004453 16 256 January 30, 2004 3004454 16 256 January 30, 2004

Total 48 768

Table 1: Tahoe Lake Property Claims Data

2

Hudson Bay

/

/

MANITOBA /" ONTARIO /

/

/

/ .TAHOE LAKE ! PROP R I

I

o Red Lake

.. _ .. f) -"-"\. .. -"' ... ,

.y-.. - .. _ ......... \. .. ,. .. ,.

USA

o kilometres

500

QUEBEC

\

\

Tlm~ins '\

o Sudbury "-' ,. ..... '\" -d /

Ottaw~/

TAHOE LAKE PROPERTY ONTARIO

TAHOE LAKE AREA LOCATION MAP

FEBRUARY 2004 Figure 1

.~ .

------swamp

. ~\

\ .-... .-... \ 4 6

3 \

\.....L..

o kilometre

MAFIC VOLCANIC

FELSIC TO INTERMEDIATE

:

:::: SANDSTONE MUDSTONE

CHERT-MAGNETITE py po cp PYRITE / PYRRHOTITE /

--- FAULT HANNA DRILL HOLE

\ \ \ \ \ \ \ \

LAC SEUL MORAINE

TAHOE LAKE PROPERTY ONTARIO

JANUARY 2004

PROPERTY GEOLOGY

2 •

Figure 2

3 825

GEOLOGICAL SETTING

The following is taken from Waldie (2004).

Regional Geology

The North Spirit Lake greenstone belt lies 170 kilometers north northeast of the

town of Red Lake, within the southwest part of the Sachigo Subprovince. The belt

is elongated northwest for 40 kilometers and attains a maximum width of 17

kilometers.

The North Spirit Lake belt comprises a variety of 3.02-2.73 Ma ultramafic to

felsic volcanic rocks and abundant metasedimentary rocks that have been

assigned a number of assemblages by Thurston et al. (1991) and updated by Stone

(1998). Refer to Table 2a and Table 2b and Figure 3 for more information.

Volcanics constitute a volumetrically important part of the North Spirit Lake belt

with felsic to intermediate rocks exposed over a larger area than mafic to

intermediate rocks. Ultramafic rocks are restricted to the northeastern edge of the

belt (Wood, 1980). The ultramafic volcanics often show spinifex texture. Mafic to

intermediate volcanics show the presence of feldspathic minerals on weathered

crust. Intermediate to felsic volcanics often contain recognizable phenocrysts of

quartz and/or feldspar.

Isoclinally folded volcanics and metasediments have been intruded by stocks,

dikes and sills of ultramafic, mafic, intermediate and felsic igneous rocks.

Numerous northwest trending faults (sub parallel to the regional Bear Head Fault)

transect the North Spirit Lake belt with subordinate northeast faults in the

southern portion of the belt.

Rocks of the North Spirit belt have been metamorphosed to greenschist facies

metamorphic rank, except those close to the Margot Lake intrusion (northwest

side of belt) where the metamorphism is of homblende-cordierite facies rank

(Wood, 1980).

TABLE 2a: North Spirit Lake Assemblages

Assemblage Main Rock Types Interpreted Environment Age (Ma)

North Spirit mafic flows, felsic tuffs, iron arc volcanism 3023±2

formation Disrupted mafic flows, intermediate to felsic arc sequence 2900 to

flows and pyroclastic rocks, iron 2950

formation Nemakwis quartz arenite, iron formation, platform 2986±3

komatiite unconformity

Makataimik conglomerate, arenite, iron formation, alluvial fan grading to <2900 to

marble, minor volcanic rocks fluvial and lacustrine 2950 >2735

Hewitt mafic flows, intermediate to felsic arc volcanism 2735±10

pyroclastic rocks, clastic sediments

Bijou Point intermediate to felsic tuffs, clastic late alkalic volcanism, 2731±2

sediments fluvial sedimentation

TABLE 2b: North Spirit Lake Intrusions

Intrusion Main Rock Types Structure; Notes Contact Age (Ma)

Relations

Hawley biotite tonalite to fo liated, cut by relation to North 2925±10

Batholith granodiorite tonalite, granite Spirit belt unclear

Pakwan biotite tonalite to strongly foliated, unclear 2726±8

Stock granodiorite elongated

Wokokotai biotite micro- possibly unclear 2743±2

Stock tonalite subvolcanic magma chamber

Makataiamik biotite hornblende foliated, plagioclase intrudes <2735?

Stock tonalite to altered to albite, Makataiamik

granodiorite sericite assembl~e

Bijou Stock diorite, altered to intrudes 2731±2

granodiorite greenschist supracrustal

minerals, foliated; rocks of Bijou

tourmaline and Point assemblage

sulJ:>hides ~resent

Shrimp quartz diorite ultramafic intrudes <2735?

Stock intrusions metasediments

Hawthorne K-feldspar inclusions of intrudes eastern <2735?

Batholith megacrystic supracrustal rocks North Spirit belt

granite Throat biotite large batholith in inclusions of 2697±2

Batholith granodiorite to the area; magnetic most other rock

granite high units

The North Spirit Lake and Favourable Lake greenstone belts appear to be

dismembered parts of an originally continuous supracrustal belt (Corfu et aI.,

1998). Both exhibit wide, fan-shaped greenstone segments broadening to the

southwest and long, attenuated limbs to the northwest. The dextral Bear Head

Fault traverses the southern edge of both belts. In a regional context, the North

6

N

~ 93"00 ' + 52°35'

o 5 - --kilometres

HAWLEY BATHOLITH

• FELSIC INTRUSIVE ROCKS THROAT

ASSEMBLAGES OF THE NORTH SPIRIT LAKE GREENSTONE BELT

BATHOLITH

NORTH SPiRIT ....................... 3.02 Ma

• DISRUPTED ...... ...................... 2.95 Ma

NEMAKWIS .............................. 2.98 Ma

MAKATAIAMIK ........................ 2.85 Ma

HEWiTT ....................................... 2.74 Ma

BIJOU PT COMPLEX ......... 2.73 Ma

--- FAULT

HAWTHORNE BATHOLITH

~CANDOR I~\ VENTURES CORP.

NORTH SPIRIT LAKE BELT ONTARIO

GEOLOGICAL ASSEMBLAGES

JANUARY 2004

92"20 '

52° 15 +

Figure 3

2.33825

Spirit Lake belt is interpreted to be synformal.

Features of the North Spirit Lake belt indicate that the rocks were formed in an extensional or transtensional setting between 3020 and 2730 Ma in a back-arc environment behind the main arc developing in the region of the Uchi Subprovince (Corfu et al., 1998).

In the eastern part of the Red Lake greenstone belt, complex Au-hosting deformation zones formed under a regime of northeast directed shortening (Zhang et aI., 1997). A similar northeast directed compression could explain the southeast trending antiforms and synforms of the North Spirit greenstone belt. This local direction is perpendicular to the dominant northwest compression throughout the Superior Province (Corfu et al., 1998).

Local Geology

The details of the geology in the vicinity of the Tahoe Lake property are poorly known because of the low outcrop density and the major northwest trending faults that are expressed as zones of intense shearing. Rock types consist of mafic to intermediate volcanics and pyroclastics, intermediate to felsic volcanics and pyroclastics, clastic metasediments and chemical metasediments. The following is summarized for Wood (1980 and 1988).

Rock Types

Mafic to intermediate volcanics in the vicinity of Tahoe Lake are fine grained, foliated flows generally without original textural characteristics. There are however pillowed, amygdaloidal and coarse-grained flows and some thickly laminated mafic tuffs documented. The volcanic rocks are dark grey-green on fresh surfaces and weather dark green to green-black.

Intermediate to felsic rocks near Tahoe Lake generally consist of massive flows and pyroclastics that differ markedly in fragment size. All the flows weather to a light grey or buff colour and are shades of grey or black on the fresh surface. The felsic flows in the Tahoe Lake area are tough and splintery on outcrop, which is a reflection of their strong silicification and/or albitization compared to similar volcanics in the area. Sericite alteration is well developed in the area, which is in marked contrast to the rest of the region. Pyroclastic rocks consist of lapilli-tuff and tuff-breccia with ellipsoidal fragments. They are similar to the flows around Tahoe Lake in that they are more siliceous that other pyroclastics rocks in the area. Geochemically, outcrops of intermediate pyroclastic rocks south and east of Tahoe Lake are strongly altered as highlighted by their high Hashimoto index (81%), which is indicative of altered rocks associated with VMS mineralization. Drilling by The Hanna Mining Company (see History section above) indicated

8

that the intermediate to felsic rocks contain alteration minerals such as grunerite, chlorite, garnet, sericite, carbonate, epidote and biotite. This indicates that the rocks have experienced high fluid flow and hydrothermal alteration.

Clastic metasediments consist of lithic wacke and mudstone. The lithic wacke units are fine grained and only weakly metamorphosed. No sedimentary structures other than bedding were noted. The rocks weather to a light brown to grey-brown colour. Mudstone units consist of shale and siltstone and are medium to thinly bedded. These rocks are dark grey to black on the fresh surface and weather to a brown colour. It is important to note that all metasediments in the Tahoe Lake are muscovite/sericite-bearing. This is in sharp contrast with most of the metasediments in other areas that lack muscovite/sericite or other potassium-rich minerals.

Chemical metasediments consist of chert, ferruginous chert and chert magnetite iron formation. Chert is typically layered from 1 mm to several centimetres and weathers grey to grey-black. Ferruginous chert weathers yellow-brown, due to sulphides, and chert magnetite iron formation weathers black.

Metamorphism

The metamorphism in the area of the Tahoe Lake property is interpreted as low pressure (below 3-4 kilobars) and at temperatures between 350 to 6500 C representing greenschist to cordierite-amphibolite facies (Wood, 1988).

Structure

The Spirit Lake belt is assumed to be a synclinal structure based on limited facing directions. Due to the extensive overburden cover in the area of the Lac Seul Moraine, correlation of the stratigraphic units in the area of the Tahoe Lake property is difficult. The numerous north northwest trending faults in the area also complicates the geology.

PREVIOUS WORK

Previous Work by Other Parties

Government Mapping

The first mention of prospecting in the North Spirit Lake area was by the Ontario Department of Mines (Hurst, 1930). In 1937, Bateman (1939) made a general reconnaissance geological survey of the area at a scale of 1 inch to 1 mile. This work defined a sedimentary-volcanic belt extending southeast from North Spirit

9

Lake through Hewitt Lake to MacDowell Lake. In 1960 and 1962, the Geological Survey of Canada perfonned reconnaissance mapping of NTS area 53C (Donaldson, 1961; 1969), which did little to change Bateman's 1939 map.

The most recent mapping in the area of the Tahoe Lake property is by Wood (1980 and 1988). This work was carried out in the summers of 1972-1973 and 1975 respectively at a scale of 1 inch to 'l'4 mile. Another geological report by Wood (North Spirit Lake, 1977) covers the area to the north.

Published regional maps of the area include Map 2262 (Favourable Lake - Berens Lake, 1973) at a scale of 1 inch to 4 miles and Map P.3382 (North Spirit Lake, 1998) at a scale of 1 :250,000.

Regional Exploration

Mineral exploration activity in the general region began in the 1920's with the first documented discovery of gold in 1936 on the south shore of North Spirit Lake, as described by Bateman (1939). Several companies explored extensive banded iron fonnation on the southeast shore of North Spirit Lake from 1953 to 1970. In 1977, Cominco Limited flew an airborne magnetic survey of the belt (not filed for assessment) and ground geophysical, geologic and geochemical surveys and diamond drilling by a variety of companies ensued (Stone, 1992). Most exploration was directed at gold and base metals in mafic to ultramafic volcanic and metasedimentary rocks on the east side of the North Spirit greenstone belt.

Property Exploration

The area of the Tahoe Lake property has seen minimal mineral exploration with the only documented work by The Hanna Mining Company (Muhic, 1976, 1977). This work involved line cutting, geological mapping, 18.8 line kilometers of ground magnetic and Max-Min surveys and 512 meters of diamond drilling in six holes.

Work in the area by The Hanna Mining Company was prompted by Ontario Department of Mines Preliminary Map P.1183 (Wood, 1976) that indicated the presence of felsic volcanic tuff and tuff breccia in the vicinity of Tahoe Lake. A reconnaissance Radem VLF survey in the summer of 1976 discovered a conductor east of Tahoe Lake. Subsequently, the work mentioned above was carried out and delineated six electromagnetic anomalies (Muhic, 1976). It is believed that these anomalies were drilled by holes TL-77 -1 to TL-77 -6 by The Hanna Mining Company. Sulphide mineralization consisting of pyrrhotite, pyrite and minor chalcopyrite was intersected in all the drill holes.

10

Geology

The geology of the Tahoe Lake property (Muhic, 1976) was noted as consisting of a series of basic lavas, intennediate tuffs, rhyolite tuffs and tuff-breccias. Lean chert magnetite iron-fonnation and associated siliceous metasediments occur with the felsic and mafic volcanics. The rocks are defonned and sheared especially in the northern portion of the property. An inferred fault runs approximately through the centre of the property and trends subparallel to the baseline of the grid (355°).

Geophysical Surveys

The 18.8 line kilometer magnetic survey was perfonned using an Mf-2 Fluxgate magnetometer which delineated several north to north-east trending magnetic anomalies (Muhic, 1976). The strongest anomalies, due to magnetite-chert iron fonnation, average 15 to 30 meters in width and are continuous along strike for 1,000 meters.

The electromagnetic survey was perfonned on the same grid lines and the magnetic survey. Detailed infonnation and maps of this survey were not available in the assessment records. It is assumed that the drill holes targeted the electromagnetic anomalies.

Diamond Drilling

The 512 meter, six hole diamond drill program (TL-77-1 to TL-77-6) was carried out in the winter of 1977 to test the electromagnetic and associated magnetic anomalies identified the previous fall (Muhic, 1977). The holes average 85 meters in length with the deepest being 135 meters. Core recovery was excellent, averaging 98%.

All of the holes intersected felsic volcanics and pyroclastics (tuff to tuff-breccia) with intennediate lapilli-tuff noted in most of the drill holes. Other lithologies intersected include banded chert magnetite iron fonnation and silicate facies iron fonnation. Andesite was intersected in only one hole. All of the drill holes intersected sulphide mineralization consisting of massive seams, stringers and disseminations of pyrrhotite, pyrite and minor chalcopyrite. No assays or sample intervals are reported on The Hanna Mining Company drill logs.

The main alteration minerals observed in the drill holes includes (in order of abundance) grunerite, chlorite, gamet, sericite, carbonate, epidote, biotite and quartz-carbonate veinlets. Mineralization includes (in order of abundance) pyrrhotite, pyrite and chalcopyrite. Graphitic bands and seams occur in three of the holes (TL-77-2, 5 and 6) Grunerite occurs as bands, seams, stringers, veinlets

11

and rimming fragments. It is noted most often associated with felsic tuff and tuff­breccia units as well as iron formation. The occurrence of grunerite in iron formation indicates the rocks have been altered and possibly mineralized. Grunerite associated with felsic volcanics and pyroclastics is rarely documented and its significance unknown.

Chlorite and garnet generally occur together in the matrix of felsic tuff-breccia, often associated with pyrrhotite and pyrite. Chlorite also occurs as fracture fillings.

Garnet, in addition to occurring with chlorite and sulphides in the matrix of felsic tuff-breccia, occurs as scattered disseminated grains in mafic rocks.

Sericite is generally noted as occurring pervasively in felsic volcanic and pyroclastic rocks.

Carbonate is noted as either pervasive or as stringers in felsic and intermediate rocks.

Epidote was only observed in a few cases, generally as stringers and seams.

Biotite was noted in only one hole associated with bands of mafic rocks containing garnets.

Pyrrhotite and pyrite generally occur together (5: 1 ratio of pyrrhotite to pyrite) as massive seams (cm-dm scale), stringers and disseminations in both the matrix of felsic tuff-breccia and cross-cutting felsic and intermediate tuff and lapilli-tuff.

Chalcopyrite was noted in holes TL-77-5 and 6 as specks, stringers and seams associated with pyrrhotite and pyrite.

Previous Work by Candor Ventures

In mid-November, 2005 Aeroquest Limited completed a combined helicopter­borne electromagnetic and magnetic survey of the Tahoe Lake property under contract to Candor. The survey was flown in a N -S direction with a nominal line spacing of 100m. A total of95.4line-km were flown (Rudd, 2005).

12

LINE

itA" "S" "C" ti~''

"E"

WORK PERFORMED

Work on the property was completed from October 2nd to 13th• The work was

based out of North Spirit Lake and travel to and from the property was by helicopter chartered from Forest Helicopters Inc. of Ken ora, ON.

A total of five, 800m long lines were cut perpendicular to the axes of selected helicopter-borne EM anomalies by Beaverhead Line Cutting of Thunder Bay, ON. Table 3 indicates the locations and azimuth of the lines. See Figure 4.

FROM AT TO METERAGE Northing Easting Northing Easting 5799150 511 590 0000 5799950 511 590 800 5 799 800 513500 0000 5800 600 513500 800 5 799 600 513 000 0000 5800400 513 000 800 5799950 512300 0300 5800650 512700 800 5 799400 512500 0000 5800 200 512500 800

Table 3: Tahoe Lake Lines

Mtec Contracting Inc. of Murillo, ON completed magnetic and HLEM surveying to ground truth the AeroTEM II anomalies (Milani, 2006). A total of 4,000m of magnetic readings were taken at 12.5m spacings along the lines using a GEM Systems GSM-19 proton precession magnetometer measuring variations in the total field with a sensitivity of 0.1 nT. The diurnal variations were monitored and recorded using a GEM base station.

The HLEM survey was completed using an Apex Parametrics Limited MaxMin I instrument in the horizontal co-planar mode with a 100m coil separation. Measurements of the in-phase and quadrature values were taken at 25m stations at 1777 mHz and 3555 mHz frequencies. A total of3,500m ofHLEM surveying was completed.

The description and specifications of the instrumentation used can be found in Appendix 1.

13

I N 512,OOOE

f

3004452

3004454

/ "0"

"8"

- 5,800,OOON "e"

"E"

"A"

3004453

CA~ reso",rces. inc.

0 500 TAHOE LAKE PROPERTY

metres ONTARIO

LINES

OCTOBER 2006 Figure 4

{.) LJI .(;."i, ';1 .. ",/

INTERPRETATION

The reader is referred to the stacked profiles for each of the lines surveyed which can be found in Appendix II.

Line "A"

One strong but thin (~ 5m) conductor located at 4+10 N was detected. It dips moderately to the north and has a depth to the top of the conductor of about 10-15m. There is little or no significant magnetic association.

Line "B"

Two conductors were detected on this line. A strong but thin (~ 5m), steeply north dipping conductor was detected at 3+35 N. The depth to the top of this conductor is estimated to be 5-10m. There is a strong positive magnetic correlation.

A second, much weaker conductor was detected at 4+85 N. It is thin (~ 5m) and may also dip steeply to the north but interference from the conductor crossing the line at 3+50 N clouds this interpretation. This conductor closely flanks a strong magnetic feature.

Line "C"

Two features thought to represent end effects of other conductors were detected at about 2+15 N and 4+60 N. The southern portion of the line crosses a broad, elevated magnetic feature.

Line "D"

A broad, possibly compound feature was detected on this line. A moderately strong, possibly steeply north dipping conductor was detected between 2+75 N and 3+00 N. This conductor is thought to have a depth of about 30m. A thinner parallel, weaker feature crossing the line at 3+75 N was also detected. A very weak, possibly overburden related feature exists at about 5+60 N. The magnetic correlation along this line is generally positive but somewhat erratic.

Line "E"

A relatively broad (10-20m) and strong conductive feature was detected centered

15

about 3+30 N. It is interpreted to have a depth of about 30-40m and to dip steeply to the south. It appears to flank a strong positive magnetic feature lying immediately to the south.

A second, much weaker and thinner (S 5m), possibly fault related conductor was detected at about 4+50 N. It also appears to flank a strong positive magnetic feature.

CONCLUSIONS AND RECOMMENDATIONS

The combined HLEM and magnetic surveys completed on the Tahoe Lake property have successfully located the AeroTEM II anomalies on the ground. Four possible drill targets have been identified. It is recommended that lines "A", "B", "D" and "E" be geologically mapped prior to drill testing. Particular attention should be paid to evidence of alteration in the surrounding lithologies which might increase the relative attractiveness of these targets.

Those targets on lines "B", "D" and "E" are related to strong magnetic features and are thought to be prospective for iron formation hosted mineralization, particularly in the vicinity of faulting. The conductor on line "A" is located in the vicinity of felsic volcanic rocks and may be prospective for massive sulphide mineralization.

Respectfully submitted,

Paul Chamois, M.Sc (A), P. Geo. December 20, 2006

16

REFERENCES

Bateman, J.D. 1939. Geology of the North Spirit Lake Area; Ontario Department of Mines, Annual Report for 1938, Vol. 47, Pt. 7, p. 44-78. Accompanied by Map 47G, scale 1 inch to 1 mile.

Beakhouse, G.P. 2003. A magmatic hydrothermal model for Archean lode gold deposits: a working hypothesis. Ontario Geological Survey poster.

Corfu, F., Davis, D.W., Stone, D. and Moore, M.L. 1998. Chronostratigraphic constraints on the genesis of Archean greenstone belts, northwestern Superior Province, Ontario, Canada; Precambrian Research, Vol. 92, p. 277-295.

Donaldson, J.A. 1961. Geology, North Spirit Lake, Ontario; Geological Survey of Canada, Map 50-1960.

Donaldson, J.A. 1969. Geology, North Spirit Lake, Ontario; Geological Survey of Canada, Map 1201A.

Favourable Lake-Berens Lake, 1973. Geological compilation series, Map 2262, scale 1 inch to 4 miles.

Hurst, M.E. 1930. Geology of the Area between Favourable Lake and Sandy Lake, District of Kenora (Patricia Portion); Ontario Department of Mines, Annual Report for 1929, Vol. 38, Pt. 2, p. 49-84. Accompanied by Map 38a, scale 1 inch to 2 miles.

Milani, M., 2006. Logistical Report. Magnetic and Max Min HLEM Surveys. Shrimp and Tahoe Lakes Area, Northwestern Ontario. A report prepared for Canstar Resources Inc.

Muhic, J.F. 1976. Tahoe Lake magnetic survey; The Hanna Mining Company, Ontario Assessment Report # 53C07SW0001, 3p. Accompanied by magnetic survey map at a scale of 1 inch to 200 feet and geology map at a scale of 1 inch to 1320 feet.

Muhic, J.F. 1977. Tahoe Lake diamond drill logs, Mattson Lake area; The Hanna Mining Company, Ontario Assessment Report # 53C07SW0003, 33p.

North Spirit Lake, 1998. Precambrian geology, Map 3382, scale 1 :250,000.

17

Rudd, J., 2005: Report on Helicopter-borne AeroTEM II Electromagnetic and Magnetic Survey, Aeroquest Job #05046, Shrimp Lake-Tahoe Lake Project, Red Lake Area, Ontario. A report prepared for Canstar Resources Inc.

Stone, D. 1992. Project Unit 88-34. geology of the MacDowell Lake-Trout Lake area, northwestern Ontario; Ontario Geological Survey, Precambrian Geoscience Section, Summary ofField Work and Other Activities 1992, Miscellaneous Paper 160, p. 4-12.

Stone, D. 1998. Precambrian geology of the Berens River area, northwestern Ontario; Ontario Geological Survey, Open File Report 5963, 116 p.

Thurston, P.C., Osmani, LA. and Stone, D. 1991. Northwestern Superior Province: review and terrane analysis; in Geology of Ontario, Ontario Geological Survey, Special Volume 4, Part 1, p. 81-142.

Waldie, C.J., 2004: Geological Report on the Shrimp Lake Property, MacDowell Lake Area, Red Lake District, Ontario, NTS 53CI7. A report prepared for Candor Ventures Corp.

Wood, J. 1977. Geology of North Spirit Lake area, District of Kenora (Patricia Portion); Ontario Department of Mines, Geoscience Report 150, 60p. Accompanied by Map 2362, scale 1 inch to ~ mile.

Wood, J. 1980. Geology of the Hewitt Lake area, District of Kenora, Patricia Portion; Ontario Geological Survey, Report 186, 122p. Accompanied by Map 2408, scale 1 inch to ~ mile.

Wood, J. 1988. Geology of the MacDowell Lake area, District of Kenora, Patricia Portion; Ontario Geological Survey, Report 261, 52p. Accompanied by Map 2497, scale 1 inch to ~ mile.

Zhang, G., Hattori, K. and Cruden, A. 1997. Structural evolution of auriferous deformation zones at the Campbell mine, Red Lake greenstone belt, Superior Province of Canada; Precambrian Research, Vol. 84, p. 83-103.

18

APPENDIX I

Specifications and Descriptions of Instrumentation

GSM-19 o VERHAllSKR Magnctcm9ter/VLF

System

Fcaturcs

Ahsolulc Accuracy - 0.2 I1T

Sampk Ratc~ uJllo 5 Hz

Low Power Consumption

(~DCnll

"O~erhau.cr" Once you experience it, you'll nevCT gu back to pToton_ O"crhBw;cr Icdn",]ogy brings you scru;ilivitlCli one 10 two order, ot ma!!lIitude lIettcr than proton. yet in • Iighl weight J1Ockagc. Thi, i, because it COMumcs an order of magnitude lells power than prot01l, allowing a lighter weight for hattLTic,

What IS the OH..-Ioauscr teehniquc" The Ovcrhauscr sensor cOl1tail1~ the c]eelTon.,· fluid d.1I has heen added to a hydrogen rich in the form of "frec radial" The resulling mixture yiclcb; a Focnsor with 5()(x) times gain

In proton polarization Since the Ovcrhaul'\C'T polan7atlfll1 ctTCL'"t rloc:J not require static

lnagnclic lields, but u.~s radio ~qUL'f\L'"Y

fields Iran,;parent to protoAA, mca.~uremcnt can be done concurrently with polarization. The result IF. a !licn""OT With mtkh grca.k:r scllf\ltrv­ity. that can lie MmJlled much more raJlidly than the standard proton scnsor

Overhauscr fiy.tem. therefore maximize re""lution wllile minimi7ing power eon.umJl­tion. Even wilh Walking Oradiomctcr

systems, :;.ampling at rates of (tTlCC per scL:ond or bcttcrare p<l8ible; E,en in cokllcmpeT8-n"e~ of minus 40 zero dewees Ccl.iu~ and greater, the internal rechargeable battery can

still he relied on for a 10 hour day, or longer.

The OSM-19 <he-rhau"-,, magnetometer is thu. truly a SIUle-nrlhe-Arl Magnelomctefl VLF 'y,lcm. Thc GSM-19 otters dhe data quality. reliability, and cxlcmive li~t of capabilities, and option., that allow it to mect a Hry wide .pectrum I>f apJllicatil>m.

Stand ... " Fcatun:s The OSM-19 eon""le teatures a real time graphic disJtlay of the current profile In addition digital display of the current reading, currellt po~itiol1, and warning mcMagcs arc pmvided. The console design, with inlcT\lal rechargeable battery pack, allows the unit to be completely ","led against d,e elt..-nents_ With the built in heater tOr the display the

GSM-19 ia ready to go wherever yoor surveys may takeyoo

Tuning IS automatIC worldwide, with J1ro\,;i~lon tor manual override In high gradient eOllditioos the <iSM -I CJ monitors the signal decay raIC an<l diaplay. a warning message when the wadient becomes too great. Fillet'!: for rejection of 50 or tiO H7 noise arc Jlmvided

Diurnal corrections may be done in flilditional fluJlioll with one unit a.. a base station wld a second unit 11""d "'< the mobile fidd unit. At dhe end of the ~cy the two unit< arc conJ1Ccted and the field unit creates n corrected data file (which slill includCR the

r Terraplus Inc. Tel: 905-764-5505 ,'2 \\ie.t Bea>u Cr. Rd HII. Rietunon<l Hill. ON. ,,,,,,,,[\;0 L4B lL9 Fax: 905-764-8093

14 AGNETOMETERS

GSM-19 o VERHAUSER Magnetcrneter/

VLF System

raw data tile) ba.,«i on the lC1nporal ,!rill rccorded by the ba<e ~tation.

A. a standard tcature the OSM-J9 aIM, otte" Ihe capubility of making tic poinl mew;urc­mcnts far automatic diurnal corrections 111 usc d,i. fi:ature the operator records" base value and then 100". back to this flOint pl.-riodically during tl", su~cy to record .nodher mca.~urcmellt, and thus build a tile lIt

the drift. In this way a single " .. !rUment Ill"} be used to make diurnal CorrCctlO""

The RS-232 port on the GSM-19 will output data a. it is colleded. Thi. allow. interlace I" (iPS log~r. that will accept RS232 data. The .talldard GSM-J CJ may be operated in a remote mode via cOlllJluter. M~..-nory storagc j,; 512 K in the standard unit, and may be uWraded to 2 MB

Orid coordinate!'> arc ~torcd with either numcnc OT r.mnpa.c;,s dcfolgTlutlOtlfi. A ~'rcn

diF,it number may be ugd to dchlgnatc line;;.

and p""Iions L,ne and pi,slli,," .pacl"!' " entered so that with every reading the posi"on may he automatically updated An End of Line feature allows the ncl<tline In be quickly ",lected, plus changes the sign on the 1""iti'>II I\pil.cil1~ If the prc ... lous line had heen ;]ddllll? position~ fiR the operator mo\"cd, then on the next line, posit;on.<; will be ~u"tractcd as thl'

operator movelC The operator may al>o .asil) InanuaJly cntLT his wid posilillfl fnl cases where gafM\ in the line arc nccc"\.."WJTV

r<mai.1: terrnpJus@?compuserve.com I Website: www.terraplus.com )

MAGNETOMETERS

Equatorial ScolKlr

In "<lmto"al region:;, I'clltcT.lly :\0 dogre .. , north or "llIth ;i the eqllator, maF'11Ctie fields rench a nearly h()f!zontal angle with the earth'!'. surface [IllS n.quircs a conventional proton ficnhlFf l\} be l,If"Cd In an mvcrtcd J'OSitiun, and rcquirc:l the operalor tn collect ciata only on [a.'W·west lines to maximi7(' the maftllct!c signal 1 his j~ a problem that i~ r1

ma~l1itudc worse for cesium magnctom~tcrs

flx: 0\ t.:rhau~ , h:dmit..tuL dllows dt:~igJl nt iJll

nptiOfHIi sensor completely fru: ofUlI.,,> problem" a ~nS(lT that rcquircfi. no orientation no matter what the latitude of yOUT cxplnra­ti{~l. Thi:, can be a major advanta~c wlx:n

working In diver", aT<a.' arcrund the world, <md when needong to ITa in local operators who~c fin;.f lan~':UaF:c may not be YOllr nwn

"WalJ<iJJg Mag Option~

Tile GSM-I 'I map:nrl<1melCr was the li"t to oftCr the "Walking Malt concept rhe reason

f<" this IS tile <Jul'tand Ing advanta~e the OvcrhnuscT sensor has 111 thu; aprlicntlon With the "Walking Mag" option the oper",,)! mny slicC'r a sample ratc of 1.Jfl fO two sampks per second At this rntc Ovcrhau"cf tcchnol­

~lg.v t.:<ln .... till (klt\o(.:r a l1oil\c. 1c\>d tJlallt. quitl.: ,:u .. ccptan1c, about n 1 nT, ~lIld th!'" tnWL"T POWCf cun,umption ml'llns that. fun day of surveyin~ can still he d,me with just the internal rc(har~cablc battery

A~ shown In fll ... 'l,JrC I th, ncar \:ontinuolU> dalt! frprn the "Walkmg Mag" techmquc pm,ioc,

increa.'\Cd dctil1ltion for any IYpe of .uney Fc>r slJnev, with den""lv spaced ~'Tid" ,uc'h Q::l archaeological or cnvironmcntal.'mTVC):~,

field productiVity l.!-. markedly nnprovco. typically by a. factor of five

Wh", In .he Walking M"l' mode the opcra'", still presets hi~ line and Fitntinn sflocing

When a known station i~ passed a grid urdntc key \~ prcsloocd and til(.' current rt.:adil1ll 15

la!,ged with thi, stati"". R"ildings taken Dctween thc:c.c marked positions arc then linearly interp.,lated for their p:rid p<lsitinn when data IS tTan'i.fcrrcd to a computer

A further refinement of the Walking Mag

concept" the H." Chain Option Tills option uses a h.p chain to trigger the magnetometer to take a rcudi'lj1 at di...crote inten'al, A Hip Chain cmsifit~ 4;fan orJlical cm:ndt"1' that rc~ud~ H.·"()lution~ of a whe(.:l WOlDUj with

Tcrraplus Inc.

H ('.a t C (j nl-f1lH) Llb SI..1LVeys.tn P lOve D~! tidJJ n t;.J L

M aqn~ti: AnofTl a.le;t;

"000

di'posablc cottOll string. Tile 'tnl\~ 15 tied on at the heginning of a line, and no the opemtor walk. ... fh~ ."ttring IS pulled nlH, f1rxi the magnetometer is automllllcally tTig~crcd With the !I.p Chain opt.on sample rat<;. up to tlV~ r.ampkfo per second arc supJKlrtcd

Omaidircctioual VLF

riM.: nSM-19 VLF featur~~ a three t.:oiJ dcsib.'11, wi.h new larr:cr coil.<; in 1997, to udtic\"c a non orientatl0n capability with cxcclk."t scn~iti",ity Ur ttl three VlF ~tatlOnl', may be recorded, along WIUl the rn""nctic readin!!. with the prehsing of a ,in~1c key

As elJch VLf sralion isread the tulfll1idd ""ength is di.'played lhis value may he u,ed tndctcrmlnc it'a st.atlun's.slg.nlll issfTong

enough to obtain u",ful data, At the clld of each rcading the in phase, out "I' ph .. ", and hori/onlal c~)mponC"1\t" arc di3f'laycd and recorded for each station

To dctcnnme what statiOlcs arc avdilable the Scan tCature may be uocd The entire VI.F ~pt:ctru1n 1ft :'iCanlled and f,taljon~ with their

corrcsrooding signal strength 31'(' displnycd Automatic tilt compcn.qtiot1 is J'rovidcd ur" to ten ocpJ'ccs B~yo"d tim. a warning message appear, with di~J>lay 1'1' the amount of t.1t ;n each direction, cru,blin~ the <>pCfator to cnnccf his p{)~irjon and take the rcadinJl a~ain

For Walking 1\1ag "pplical'orl.' a Walkinlt VLF option is also available With this option a ""I!k: Vl.F .tat.o" may be meWiUred at sampling ratc~ up to ont.:C JK-"f ~ccond (11 this mnde hoIh magoctic and VLF readings may

Simultaa.,., .. Gradiomctcr

MQI1)' mining, (.'11" ITonmcntal, and aILha.~o

logical applications Tnay hcndir from ufiill~ the gradient mC8!rufcmcnt For ncar surface an()l1\alics, generalty twenty mctcr.s depth 01

k5~. the ~udi(''1l1 anomaly will oc larger. aud narrower, than the total field all(,mHly Tili, pcnniffi the more aCCLJfatc loc::ttion of the tJJrgCl. and !!ive, better ,enfiiti~itY I he gradient mcaFourcmcnt haJo, tJlC added ..... ahH.: ul

b<:ing free hom diumal drill.

The most accurate gradient mC,JfiuremenL, arl made when both ~n~orf> arc polall:/cd and mCfI,",urcd at precisely the same time In {hi~ way any slight movement of the sensor ,tan poil: will 11<11 atlect the rcwiinH With the

GSM-19 Gradiomctcr Option the pre,,";n!, of a single key will initiate measurement of both

the total field and !!Tadien' Hotl> f('adinl" arc dlSpl.yed and Morcd

Intcgratl'd DGPS

W,UI the (iPS Log Optl0l1 the (j!)M- t') will display and .tore OT'S data using ot.andard NMEA fonnat. POf.itton acc.uracy 15 (icpcn­dant on the user's DGPS system

AI,,, offered i. an intcmally mountc<i GPS hoard that may he integrated with mdio modem lor OOPS mode A range of OPS hoa.ds Inay be "lfCT~d to .m;et customer F-pccit1cd accuracy I hese arc quoted Oil J

case by case b~js to take advantage nfcurn.nl tcchn~lo~ Crnnplct£: s.y:\tcms, with ba.<;c atalmll, and DGPS snftwarc arc {1fo\ildcd

52 We"t lleav('r l·r RI1 1117, Richmond Hill, ON CaM(\! L4A 11.9

Tel: YOS-764-5505 fax: 905-764-8093

Email: terraplu..ir<:~e.com

Website: www.tcrrnpius.com

Fdcndcd Remote (:ontrol As an option the OSM-19 ma) b<; compl<tdy controlled through the RS132 '"teTrace Thi. "plIOI1 illC lude. all cOl1lrol. available from the Krypad. ~uch as rlower on/~ff. tuning. etc ThlF. OfKlOll if, most u"-Cful tor obt;crvarorv ;tpplic(ltion~ .

Marine Magncto...,,,, ...

1 he Ovcrhau.<,o..:r effect I." a major benetit in marine applkatlon.., The OSM-19 1m . .:; beCTl

developed illlo two marille models: the (,SM· 19M f()r shallow tow application."\ with cable

icngth!' of up to 1 f)O 1Tlt.:tL:r~: and the standard n'j:M-19 tr.r tow aJlPlitatlll!l.S with c'lbk kl1JZlh'<' of ,0 mctcr.'\ Ph.:()..\c ~.:C pt1(ll'h ',",1 hn the GSM-19M

A ~t.andafd GSM -19 may be UM:d with il mmmc ~cn:;m wldl up to !l JO meter cable Tn this way the ftIltnC C0I1501c may be \lFocd for both lanc1and marmc applications Users consicicrmf!: this option may Wanl to focus on

~Jlso II1dudmg the Walkinp. Mag option so that they will h;J~C ~amrlc rates that arc more appropriate for marine "rPlicati(lns

Overhauocr Perrorma"""

Rc .. ollllion. n 01 nT

Rdatih SClL",lti,,!ty: ()()2 oT

Ah:\o!utc Accuracy' f1.'nT

Ranfc 20,OOf) 10 120,00011 I

(iradlc.11t lo1crancc: (h."(,T lOJ)()OIl rim

Operation Modes

Manual: Coomtmtf"Ci,. time. dafe <tOO It~adtng ~tOf"('d auk)f1l;:>ltn.:all y ~1 mltl J ~t.:.ood interval

R;)sc Slilfion' TIme. (1i111:" ,,00 f1:'3dlng ~orf.d (I' :. 10 60 '\ew·nd intl"r .... al~

Walkmg MaJ,!"' Timf'. claIr and rndln~ 'li1on::r1l1t

coordi/litte\ of flrlucli'tl

Remote (:()ntTnl' OptiOfUtl Il"mote conlmt U~I"f.

RS-232 Ink'rface

InpuUJutplJi: RS-2Y2 ()f an;:th~ (Vph{)n.11\ outpul

wing fl-PHl \ .. ·t'illthr:rpr(l()f ('."onnf:clnr

Operating Parameters

POWLT CUII!\Umptuwl' Only ~W, pc:r rt':iuting

()pc':ralr:r. conhnuously for 45 hour.'! on ~'andb.,.

Power Source 12V '2 flAh ~r;ilkd Il':o:td a{;lel

battery 'litandard. other batknc~ iII ... ·"II .... blc

Storage Capacity

MHnual Operation: 29JM"Xl re.ulmg." sfitncbrcl with ufll0 Ilf>.nOO optt(ln~1 "lith 3 Vl.F ~,,,'illfl'" 12.1)1)0 ~I<tnrhlld and up to 48J)OOnpltonal

B;u;c Station: lO~,OOO rei1lrlinf':~ I"tanchuri. , ... ·.th liP 10 41Q.Clno ('op1I~1 (~8 hnur.;. or 1·1 c1ay:r.

nnlRtf'mlpt~ npr'n,lion \, ... Ih 1 ~e(" tntP.rv,,\,)

(rradiometer' 2~.OOO ~"din~ ~"'nr1ard.. with up I() lO(tOOO opflOMI With -' Vt.t qatlon~ 12.fJOn with un to ,1S.000 opltontlL

Omnidirectional VLF

Pqtonnancc Pamlnclt:"T:"O Hr.<I(tillll{lf1 () 5·~, IHIfI

"HlgC te "'20( •• /" of l('Ital field.

Frt:quenc~ 1.\ 10 30 kHz

MC::lsurcd P>lramclcrs Vet1i(~~1 .n-rm:tY: &. Ol.Jf­

("If-prune 2 horizontal cort1p<"rr.nK l(ltal fiel c1

('onmi Mtf'~. rliIk:. "Ali time'

FCilI"trrc:\' Ull to , ~tMt(ln~ tnr.:/I:\lJrrd ~ulnfTl<\tlcall).

lIl·fleld data rlC"I!,!W. dl~pt3"'fi ~Iation held ,-.Ircngth ("OfllU1u~ly. ~nd hit t.n~("IJnn f('r ur' h~ ~ 1(),'

fil"'.

I}imcnsl()n~ and Ylcip.hL" en," 143'( 150mm anl"i ,"ei~h.'1 onl.,.· 1 ilkg

Tcrraplus Inc Tel 905-764-5505 52 \\i",I!Je'Hr(r Rrl "17. R,chn~n<t Hill. ON ,-,""<to L~lllLq Fax:905-764-H091

MAGNETOMETERS

DlmcnsiOIlI and Weights

COMok' 7.23::\ fiC) x 240mm

SctlfoOT" 170:'( 71mm rllamc:ter cyllnct.er

Weigh':

Console- 2 1 kg

Scn~or and Slr'1tl A.~<;Lmbly: 2 ftkg

Standard Components (,SM. I q uln'o~. harnr~". battery Ch3~(I. !>h'PPlng ~. !'oeru.or with Ulble. staff. m5truclwfl manu"l, data tnansfer Clble and !>Ofiwan:'

Ord!r::i.r.g lilformatiaJ \)c.cription Order Number

G91J-19 Otrerlawer Maq. 350·170 fJC~l -...r qti::n 'B}- )1I)-1lOCI

VQt:ial . :m-J"lH'ml <36~qr.Im Hl-11tl·OJ1!1 M~'JK)ry ~~ ~T :JJ/. 1<'iu·l7n 0Q( ... '"

Jmbj WIlt . B}-l"Xl «*J _ qtim :H>-llO-illll

11 o.lid:!J;j Mt.g Cldm ~·rm-ocm

ClIiM-19 a.J.Jcor MlrtD! PUb _350-170-O10~ ~ __ qIticn 3 "'11!HI1l4

Email: terrapllL<;(4:0mpu.·it2VCUJJTI ') Website: wwwtemlpl\L<;com ___ -.J

FREaUF NCIES Uo.220.440 .•. I1IO.3&20.1040"'-H% SURVEY DEPTH F_ ........ llll.5 .... ctI ........ PENETRATION fur ..... IIIItIiIIIII ...... 0.15 ... call

COIL IItHlO.1: 12.11. 25. 50. n. '00. 121. 1 •• 2111. ................ , ............. .".... SEPAF!I\ TIONS. 2M. ,.. .... 4OD .... 11M ....... ...,.

lIfT 110. 2: 10.211.411." aI. 100. 1211. till. 2111. RFFFRENCE ~""""412..-.cc. ............ 2." 3211 .... 1s ...... lIiIIpot ..... CABLE lor ....... .,.,... .............. ..... If). lor ................ lET IIO.S· 50. 100. 2111. 300. G. !iOO ...... 1Il10. 12GG .... 1_ hIeIl .... IId •• 1M INTERCOM Voice _ ....... IiIIIprwi4ldIor ......... SIIIItt_."'._1 ..... ..--.......

TRANSMITTER 110Hz: 220 .. 1110Hz: 11011.'" TEMP RANG!:' 1Ii_ 40 ...... eo.,.. C8IIin ......... DIPOlE 220 Hz 215 A .. ' 362011z: alA .. ' MOMfNTS 440Hz' 210AW' 7MIIHz: 41111."- RFGFIVER r_IIllldlnIV· 0.1 All ........... L*

_Hz.2ODAIIII' 140lI0 Hz: 2011..' BATTERIES 25 ...... c..-...." ..... i ............ ~1.2A11--.. .............

MOOESOF IIAX 1 _ ................... __ __ I' •• lIIdlor.., .... ......., OPERATION .. _ .... aiI .... _ ........ ~.

IIAX 2: V ..... ~ ......... ......,... TRANSMITTER ..... .....-• .....". ........ ,ZV· ........ caiI ...... ' ......... ~_ BAT1ERIES 14M_(4 •• V-l.2A11) • .,... .... ~ 1111 I' ,.".... ....... 1 - ....... call 0pII0MIr I ..... IE ... Me 12 V - f4 AIL ...... HriDaWMd_.ccIiI ............ .................. 12hl.2V-7M) .. II .. 2: ...., III, ... , .... 2 ......... call 1Ii-ftf ....... ·beIt.oicI lor ......... .... ,..ee ......... call .... IIanzIImI

TRI\NSMITTER l ....... ...., ....... : 1 ..... V.t2li,., .... PARAMETERS 1.'fIIeM n4 ......,. e.-,. ... 01 ... BATTERY JMnLrr clillllr.l.4 A. II V ............ MEASURED .-...Illy ........ tWd. ill .... ...-, I11III. CHARGERS. 0peIwIaLt .... If. -120 1M! 220- 240VAC. II·

80Hz ... 12- 15VDC ........ READOUTS AaIIog ............ ,...,. fur iLl·

............... A~ .... lCO RECEIVER • II • ..,.., ....... CiMI .............. _pnI'Ii .... IILe ........... C~. WEIGHT • .,... ........... , •• 1t ..... ..,C~. ................... -..-..... ... ,..., .... "'.WC TRANSMITIER WT ,. Kg ClflYiIII __

RANGFSOF 1iIIIcII ........... iLI ............ SHIPPING .I .... H ....... fA,.-- ..... ~ RfADIJU1S ..... :D1: ..... h:20,. .. O"' ............ WEIGHT ""' .......................

':1:1 •• ,. ............... l1li<:. AIIIotI iI ................ ' ...... -. .b 15 .. "bit .......... IIIIC.

SrA"O~O .,..---....,.-~ RESOlUTLOli "-Ioot..- ........... 0.1.'" 01 SPARES ......, ..................... ...-,fiII4 ......................... O·I1 ..... -.....IIIIC; till.,. .... c .. --. .... .,.._01 .............

OPTIONS AND .IIIIC ....... c...,... ..... REPEATABIlITY 0.01 II ... aI f'IiLI18IJ 1iIhI. typiC8l ............ ACCE SSORIES. • o.IIIi ... p .. r .............. .......-. '*"'-'. CIIII .......... d COAIIiIIoLIs. PI [ASE SPECIFY . . ......................... ,...... SIGNAL

• R--.CIIII1 ............. "-"" ~ .. ,. cOLLti __ spllellc lOiN ........ 1.'. ,'IlL ......... IIIni.

flUE RING .................. ~.-... -. .R ............................. • T--'1kaI1IIIIIPIJ • c ...... apIiDIL

WARNING --............... nc .............. • M ............................ kit lIGIlTS i ...... ...-... eodioM.

5poc*a_ .... .,ct.9I_1 ""'-

93·10 .15

APPENDIX II

Stacked Profiles of Surveyed Lines

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0.21 1.6 -489

* 1 CI) ~ -530

0.5:1 2.8

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1.1 ~ 2.1 '~ " 335 I-

" 178 ~ ~ c C; E 8 m II

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9 9 1-114

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