Geochemical Analysis Certificate 5W-2840-RG1 HI I 12 1995 Company: WMC INTERNATIONAL LTD J UL Date: JUL-06-95 Project: 4054 PO# 4054-G L O Attn: A

Home , Claw (piercing)

41P11NW0020 2.17094 CABOT 010

EXPLORATION

REPORT ON THE 1995 - 97

EXPLORATION PROGRAMS,

CLAW LAKE PROJECT (4054) 1997

ALAN J. SEXTON SENIOR GEOLOGIST

ANNE COLLINS DATABASE GEOLOGIST

ROMAN TYKAJLO SENIOR GEOPHYSICST

FEBRUARY 20 , 1997

WMC International Limited Americas Division Exploration 22 Gurdwara Road Nepean, Ontario Canada K2E 8A2 Tel (613) 727-3937 Fax (613) 727-3970

A member of [he WMC Limited group o/ companies TABLE OF CONTENTS

1. SUMMARY...... !

2. LOCATION, ACCESS , PHYSIOGRAPHY AND CLAIM STATUS...... 2

3. PREVIOUS WORK...... 2

4. 1995-97 EXPLORATION PROGRAMS...... 8

5. REGIONAL GEOLOGY...... 9

6. GEOCHEMICAL PROGRAM RESULTS...... 12

7. GEOLOGICAL PROGRAMRESULTS...... 13

8. GEOPHYSICAL PROGRAM RESULTS...... 16

9. CONCLUSIONS AND RECOMMENDATIONS...... 18

10. REFERENCES...... ^

CERTIFICATES OF QUALIFICATION

LIST OF FIGURES

FIGURE l Location map, Claw Lake Project, 1:10,000,000...... 3

LIST OF TABLES

TABLE l Ridout Lake Project claim list ...... 4

LIST OF MAPS

MAP l Grid and Claim Location, 1:20,000...... In pocket

MAP 2 East Sheet Geology, 1:5,000...... In pocket

MAP 3 West Sheet Geology, 1:5,000...... In pocket

41P11NW0020 2.17094CABOT 0 1 OC MAP 4 East Sheet Lake Sediment and Rock Samples Locations, 1:5,000 ...... In pocket

MAP 5 East Sheet Au - As - Sb Geochemical Results, 1:5,000...... In pocket

MAP 6 East Sheet Ag - Mo - Cu Geochemical Results, 1:5,000 ...... In pocket

MAP? East Sheet Pb-Zn - Ni Geochemical Results, 1:5,000 ...... In pocket

MAP 8 West Sheet Lake Sediment and Rock Samples Locations, l: 5,000 ...... In pocket

MAP 9 West Sheet Au - As - Sb Geochemical Results, l:5,OOO...... In pocket

MAP 10 West Sheet Ag - Mo - Cu Geochemical Results, 1:5,000...... In pocket

MAP 11 West Sheet Pb-Zn - Ni Geochemical Results, 1:5,000 ...... In pocket

LIST OF APPENDICES

APPENDIX A: LIST OF EXPENDITURES

APPENDDC B: ANALYTICAL RESULTS, 1995 LAKE BOTTOM SEDIMENT SAMPLES

APPENDIX C: ROCK ASSAYS, REGIONAL AND GRID MAPPING, 1995 - 96

APPENDDC D: GEOPHYSICAL PROGRAM DATA AND LOGISTICS REPORT, 1997 1.0 SUMMARY

The Claw Lake project is located near the western margin of the Abitibi Greenstone Belt (AGE). The purpose of this exploration project was to explore for Archean shear zone hosted gold deposits similar to those of the Kirkland Lake and Timmins gold camps. The ENE - striking Cadillac - Larder Lake Break (CLLB) crosses the southern edge of the property. Several east - northeasterly trending shear zones occur north of the CLLB and represent secondary structures associated with the CLLB. These shear zones are analogous to the gold producing, northeast striking, shear zones of the 25 M oz Kirkland Lake Gold Camp.

The geological mapping outlined several l to 5 metre wide, 800 metre long, 080 trending shear zones in the area of the Galena, Molybdenite and Hillside Veins. Several rock samples were auriferous (ie. 300 ppb to 17.9 g/t). This mineralization consisted of quartz-ankerite-pyrite veins in sheared and ankeritized quartz and quartz-feldspar porphyry dykes, the trace of the Beaver shear zone was extended 300 metres further to the northeast from its location by previous workers. Minor anomalous gold (ie. < 300 ppb) was outlined in bedrock. In the area of the Rapids and First Rapids Veins well developed shear zones containing quartz-ankerite-pyrite stockworks and veins with locally very well developed silicification. Gold values ranged from < 300 ppb to 4. l g/t.

The geophysical surveys outlined low amplitude chargeability IP, high amplitude resistivity and comples magnetic anomalies that coincide with the auriferous quartz-ankerite-pyrite veins in sheared quartz and quartz-feldspar porphyries of the Galena, Molbdenite and Hillside Veins. 2.0 LOCATION, ACCESS , PHYSIOGRAPHY AND CLAIM STATUS

The Claw Lake property is located in the Claw Lake area of the 1:50,000 NTS topographic sheet 41 P/11 , approximately 15 kilometres northwest of the village of Shining Tree , Ontario (Figure 1). The centre point of the property is located at approximately longitude 81 22© and latitude 47 41©.

The property consists of 35 contiguous claims (464 units) covering 7424 hectares in Cabot , Churchill, Connaught and Kelvin Townships (Table l, Map 1). Presently 3 claims (34 units) are under option to WMC International Limited from Mr. Thomas Obradovich and Mr. Glen Mullan. Thirty - two claims (430 units) are I0007o owned by WMC International Limited with a retained interest by Messrs. Obradovich and Mullan.

The overall relief of the property is low with the maximum elevation difference being 46 metres. However , the area around Claw Lake has very steep relief locally and is in terrain underlain by granitoid rocks of the Claw Lake Stock. The northern half of is a gently undulating sand plain which forms part of an esker complex on which sand dunes, convex southwards occur. Cedar and alder covered swamps occur over 40©^ of the property. Drainage is southerly and westerly for the western portion of the area, and is carried by Claw Creek and its tributaries westward into Mattagami Lake, which is immediately west of the property. Kelvin, Bigfour and Marne Creeks in the eastern portion of the property drain southwards into Bigfour Lake and Michiwakenda Lake.

Access to the northwestern portion of the property is good via the Marne Lake all-weather gravel road which intersects the all-weather gravel Grassy Lake Road about 20 kilometres north of highway 560. Eleven (11) kilometres west of this intersection a drill l ATV l ski-doo trail turns south off the Marne Lake Road and proceeds for about five (5) kilometres to the northwestern corner of Claw Lake. However, access to this remainder of the property is limited to float plane, helicopter, boat and ski-doo.

3.0 PREVIOUS WORK

Sporadic exploration has been conducted over this property since 1919 to the mid-1970©s. Parts of the property have been covered at various time by magnetic, EM and mapping surveys. Most of the exploration work carried out in the Claw Lake area was done on three showings known as: the Hillside Vein (Saville©s No. l showing), the Galena Vein (Saville©s No. 2 showing), and the Molybdenite Vein (Saville©s No. 3 showing). Numerous short holes ^60 m) have been drilled on these showings which contain gold, chalcopyrite, molybdenite, galena, silver, and pyrite mineralization. Early exploration activity was for gold deposits , but from 1961 - 1975 activity was for copper-molybdenum porphyry-type deposits. A summary of significant recorded work done on the property follows. WMC International Limited Americas Division Exploration

CLAW LAKE PROJECT

LOCATION MAP

DRAFTED: L Wu PN: 4054 PUN; OMTPROV

DATE: IB FEB 97

O N T A R l O

200 FIGURE 1 TABLE 1 WMC CLAW LAKE PROJECT CLAIMS

CLAIM NO. UNITS RECORDING TOWNSHIPS DATE

1188885 16 01/06/1992 CABOT 1188886 16 01/06/1992 CABOT 1189039 2 01/06/1992 CABOT 1201701 13 02/22/1995 KELVIN, CABOT, CONNAUGHT, CHURCHILL 1201702 6 02/22/1995 KELVIN, CHURCHILL 1201703 12 02/22/1995 CHURCHILL, CONNAUGHT 1201704 14 02/22/1995 CABOT, CONNAUGHT 1201705 11 02/22/1995 CABOT 1201706 16 02/22/1995 CABOT 1201707 14 02/22/1995 KELVIN, CABOT 1201708 10 02/22/1995 KELVIN 1201709 11 02/22/1995 KELVIN 1201710 16 02/22/1995 KELVIN, CABOT 1201711 16 02/22/1995 CABOT 1201712 16 02/22/1995 CABOT 1201713 16 02/22/1995 CABOT 1201714 16 02/22/1995 CABOT, CONNAUGHT 1201715 16 02/22/1995 CABOT, CONNAUGHT 1201716 12 02/22/1995 CABOT 1201717 2 02/22/1995 CABOT 1201718 16 02/22/1995 CABOT 1201719 16 02/22/1995 CABOT 1201720 16 02/22/1995 CABOT 1201721 16 02/22/1995 CABOT 1201722 16 02/22/1995 CABOT, CONNAUGHT 1201723 16 02/22/1995 CABOT, CONNAUGHT 1201724 16 02/22/1995 CABOT 1201725 16 02/22/1995 CABOT 1201726 16 02/22/1995 CABOT 1201727 1 02/22/1995 CONNAUGHT 1211788 16 12/06/1995 CABOT 1211789 16 12/06/1995 CABOT 1211790 16 12/06/1995 CABOT 1211792 16 12/06/1995 KELVIN 1211793 4 12/06/1995 KELVIN

35 claims 464 units In 1919, recorded exploration activity in the area began with the discovery and staking of gold mineralization on the northwest shore of the western arm of Claw Lake in central Cabot Township by Thomas Saville of Shining Tree, Ontario. These showings became known as the Rapids Vein and Second Rapids Vein.

In 1922, Thomas Saville discovered and staked gold and galena in veins on the central peninsula of Claw Lake. These showings became known as the Galena, Hillside and Molybdenite Veins That were optioned to Ventures Limited who carried out extensive rock trenching. In 1925, Finley (Gledhill 1926) examined the geology of the showings.

In 1946, Paymaster Consolidated Mines Limited drilled some of the veins in the area for Claw Lake Gold Mines Limited whose property included all the showings. The Rapids Vein was described in the company reports as having a complex structure due either to drag folding or to actually consist of several disconnected veins. The vein material is quartz and the veins strike N30W and dip 60*^. The inferred length of the vein is 152 metres and it outcrops on both sides of the rapids. The best assay from an unknown type of surface sampling by Claw Lake Gold Mines Limited in 1946 was 0.58 oz. Au per ton across .46 metres (Cartier, 1986). Eight diamond drill holes totaling 747 metres were drilled to test the vein system along a length of 122 metres by Paymaster Consolidated Mines Limited in 1946 for Claw Lake Gold Mines Limited. The best intersection was 0.16 oz. Au per ton across 0.6 metres (Cartier, 1986). In addition, 9 diamond drill holes for a total of 843 metres were drilled on the Hillside and Galena Veins. During this time the Central part of the claim group was also mapped geologically by Claw Lake Gold Mines Limited. The Hillside Vein (Saville©s No. l Showing) was described by Laird (1934, p. 68) as consisting of an intricate stockwork of quartz stringers ranging in width from a fraction of an inch to several inches and cutting what appears to be a diorite stock. The showing was exposed by exploration activity consisting of four north-south trenches across the strike. The showing was exposed for a length of nearly 150 metres, and for widths as great as 75 metres (Laird 1934, p. 68). The strike of the veins is N70E and the dip is northerly. Vein breccia structure was observed, and a series of three parallel quartz-feldspar porphyry dikes ranging from .5 to 4.5 metres in width cut across the showing in an east-west direction (Laird 1934, p.68). The altered tuff is strongly impregnated with fine iron pyrite, and locally the quartz carries notable quantities of molybdenite, specular hematite, and locally the quartz carries notable quantities of molybdenite, specular hematite, and galena (Lair 1934, p.68). No gold assays were recorded but gold values over suitable mining widths were reported to be low (Laird 1934, p. 68). Sampling of an unknown kind by Claw Lake Gold Mines Limited in 1946 returned a best assay of 0.79 oz. Au and 15.9 oz. Ag per ton over .76 metres over a length of 11 m (Cartier,1986). Four diamond drill holes totalling 276 metres were drilled in 1946 by Paymaster Consolidated Mines Limited to test the showing. As assay of 0.01 oz. Au per ton over 1.37 metres was reported from a vertical depth of 34 metres (Cartier, 1986).

The Galena vein (Saville©s s No. 2 Showing), was originally described by Laird (1934, p. 68) as consisting of two parallel quartz veins striking east-west and dipping steeply south. The north vein is 0.4 metres wide, and the south one .25 metres wide occurring in a fresh-looking reddish 5 granite. They were exposed in a north-south cribbed trench 9 metres in length (Laird 1934, p. 68). The quartz was said to be mineralized with pyrite, galena, molybdenite and chalcopyrite. Claw Lake Gold Mines Limited in 1947 described these veins as averaging .60 metres in width and lying 1.22 metres apart in a sheared and carbonatized porphyritic granite near its north contact with volcanics. Selected sampling of the veins in drill core carried out by Claw Lake Gold Mines Limited assayed 0.45 oz. Au per ton over .91 metres at a vertical depth of 47 metres (Cartier, 1986). Molybdenite was encountered in some of the holes. The best assay from grab samples taken from dump material was 0.95 oz. Ag per ton and 0.57 oz. Au per ton as reported by Claw Lake Gold Mines in 1942 and 1947 respectively, and Q.21% MoS2 as reported by Claw Lake Molybdenite Limited in 1960 (Cartier, 1986).

The Big Vein is a quartz vein located 610 metres south-southwest of the Second Rapids at the western end of Claw Lake. It was traced for a length of 152 metres and had a maximum width of 3.0 metres. Mineralization consisted of molybdenite, galena, and chalcopyrite but the vein material was assayed only for gold. The highest assay was 0.05 oz. Au per ton from an unknown kind of sampling done by Claw Lake Gold Mines Limited in 1946 (Cartier, 1986).

The Draw Vein is a quartz vein located 215 metres north of the Big Vein. This vein was said to give consistent gold assay results from an unknown type of sampling, the assays averaging 0.13 oz. Au per ton over .46 metres for a length of 18 metres as reported by Claw Lake Gold Mines Limited in 1946 ( Cartier, 1986).

In 1960, Claw Lake Molybdnum Mines Limited examined some of the showings to assess their molybdenum content. The Molybdenite Vein ( Saville©s No. 3 Showing), located at the northwest shore of the east arm of Claw Lake was originally described by Laird (1934, p. 68) as two parallel vertical quartz veins, each about .50 metres in width, which strike N70E in a highly schisted quartz-feldspar porphyry. The showing which had been trenched by an unknown group in the summer of 1961 was re-examined by R.B. Graham for Claw Lake Molybdenum Mines Limited in November of 1961, who described it as consisting of a split vein 16 metres long and varying from 0.5 to 2 metres wide occurring in pink granite porphyry containing SVo muscovite. The strike of the vein is N70E and the dip is 76^. The country rock is shattered, sheared, carbonatized and silicified in the vicinity of the vein. Mineralization in the south vein was described by Laird (1934, p. 68) as being an unusually heavy concentration of molybdenite and its yellow oxide, molybdenite. The molybdenite occurs both in the massive state and as thin films in tiny fractures in quartz (Laird 1934, p.68). An assay of this material by the Provincial Assayer gave Q.74% Mo S2 (Laird 1934, p. 68). Results from the assaying of grab samples of the split vein by Claw Lake Molybdenum Mines Limited as reported in 1960 was Q.96% MoS2 and 0.07 oz. Au per ton (Laird 1934, p. 68). The results of chip sampling by Claw Lake Molybdenum Mines Limited in 1961 was Q.27% MoS2 and O.pt oz. Au/ton over 0.55 metres (Cartier, 1986). In 1965-66 this company drilled five diamond drill holes for a total of 583 metres on the Galena Vein and the Molybdenite Veins. The best intersection from this drilling was a sludge sample yielding Q.36% MoS2 over 3.1 metres on the Molybdenite Vein (Cartier, 1986). In 1960, Jonsmith Mines Limited discovered occurrences of chalcopyrite-bornite-magnetite-gold and, in some places, nickel in metavolcanics, metasediments, dirorite, and gabbro in central Cabot 6 Township. Thirteen packsack drill holes were drilled by the company in that year to evaluate the showings. In 1961, geological and geophysical surveys along with some pitting and trenching were completed. During this time, silver-cobalt-nickel mineralization associated with copper, lead and zinc was discovered. In 1962, prospecting work was continued and was followed by diamond drilling in 1963. No significant results were encountered so further work was not carried out.

In 1969, prospecting, trenching, rock sampling and geological mapping was conducted by Kennco Explorations (Canada) Limited in southeastern Cabot Township on the Elmer Galata property. This was followed in the next year, 1970, by geophysical work carried out by Geosearch consultants for Kennco Explorations (Canada) limited. The geological work consisted of the preparation of a detailed geological map at a scale of l inch to 400 feet. The property was described as being underlain by Precambrian rocks comprising intermediate to felsic volcanic rocks cross cut by diabase dikes. The volcanic rocks were descirbed as consisting of relatively thick, massive felsite flows that range from pillowed to agglomerate and tuff. The felsic volcanics predominated in the southern half of the claim group and the andesites in the northern half of the property. The volcanic rocks are interlayered with meta-argilitte and sericite schist. These rocks have an east-notheast strike and near-vertical dips. Major strike-faulting was described as occurring in the claim area. Mineralization was described as consisting of small occurrences of pyrite and chalcopyrite occurring mostly in felsic rocks located in the centre of the property. Pyrite occurs very lightly disseminated in this unit where it is brecciated and fractured and intruded by andesite. Chalcopyrite occurs in late fractures. The best assay was Q.1% Cu in 6.1 metres in chip samples (Cartier, 1986). The geophysical survey, by the Turam electromagnetic method, was carried out to locate possible near-surface, massive-sulphide mineralization in what had appeared to be a favourable geological environment. The results indicated that no significantly large bodies of massive-sulphide mineralization were present near the surface within the claim group. No further exploration work was conducted.

During 1971-72, Canadian Johns-Manville Company Limited carried out geological, geophysical and geochemical work on all the Claw Lake showings to determine whether the occurrences constituted an example of copper-molybdenum prophyry-type mineralization. The work consisted of geological mapping, magnetic and electromagnetic surveys, biogeochemical surveys and soil geochemical surveys. The geological survey described the Claw Lake Stock as a granitic plug elongated in an east-west direction roughly parallel to the intruded volcanic rocks. The composition of the stock changes from a diorite in the south, through grandiorite to a granite on the north contact. The volcanics on the north contact are cut by swarms of quartz l feldspar porphyry dikes up to 6 metres wide. It is in these late stage dikes that the original showings occur. The results of the geophysical surveys located weak conducting zones, but none was considered to warrant further exploration work. The biogeochemical surveys were carried out using birch, balsam and alders, and analyses were made for copper, molybedenum, lead, zinc, and silver. The purpose of the surveys was to determine whether the molybdenum showings were part of a copper-molybdenum, silver, and lead mineralization. The overall results from the geological, geophysical and geochemical work indicated that the possibility of occurrence of a low-grade, copper-molybdenum deposit within the Claw lake Stock was remote. 7 In 1992 Trinity Explorations Ltd. completed grid cutting, mapping/prospecting and Mag/VLF- EM surveys as part of OPAP grant OP92-513. This work was completed in the area of the Rapids and Second Rapids Veins. All these showings were resampled with similar results as those of previous exploration programs. The most significant result of this work was the discovery of a new mineralized shear zone called the "Beaver Zone" 600 metres north of the Rapids Vein. This strongly ankeritized northeast trending zone was 200 metres long by 25 metres wide and contained 5-20 centimeter wide quartz veins which assayed 3.5 to 10 g/t in several grab samples.

In 1994 Trinity Explorations Ltd. conducted an IP survey and drilled four diamond drill holes totalling 432 metres. The first two holes were drilled 150 metres apart and tested the Beaver Zone. Both holes intersected the strongly sericitized-ankeritized shear zone within mafic tuffs and volcanics. Cross cutting feldspar porphyry and syenite dykes alsp occur. The highest gold assays were 50 ppb at 91 metres in hole l (96 m) and 161 ppb at 56 metres depth in hole 2 (106 m). Drill holes 3 (107 m) and 4 (123 m) tested the Rapids Vein and were drilled 100 metres apart. Both holes intersected strongly silicified-hematized-brecciated diorite withwell developed quartz veining and cross cutting feldspar porphyry dykes. The highest gold assays were 180 ppb at 103 metres in hole 3 and 2.4 g/t at 76 metres in hole 4.

4.0 1995-97 EXPLORATION PROGRAMS

The 1995 exploration program on the Claw Lake property consisted of the following:

(1) 20 kilometres of regional geological traverses, (2) 163 rock samples sent for geochemical analyses, and (3) 10 lake sediment samples.

The 1996 exploration program on the Claw Lake property consisted of the following:

(1) 64.175 kilometres of grid cutting, (2) 60 kilometres of grid mapping, (3) 15 kilometres of regional geological traverses, and (4) 60 rock samples sent for geochemical analyses. The 1997 exploration program on the Claw Lake property consisted of the following:

(1) 16.15 kilometres of IP survey, and (2) 34.77 kilometres of magnetic survey . 5.0 REGIONAL GEOLOGY

Regional Bedrock Geology

The Claw Lake property is situated near the southwestern edge of the Abitibi Greenstone Belt (AGE) within the Superior Province. The regional geology has recently been described by Jackson and Fyon (1991) from which the following overview was taken.

The AGE is bounded to the south by the Ramsey-Algoma granitoid complex, the Cobalt Embayment and the Pontiac Subprovince; to the north by the Archean Opatica Subprovince; to the west by the Ivanhoe Lake cataclastic zone, which marks the western boundary of the Kapuskasing Structural Zone; and to the east by the Proterozoic Grenville Province.

The AGB is unique amongst greenstone belts of the Canadian Shield in that it: has a high ratio of supracrustal to intrusive rocks; is the largest greenstone belt in the world; has a generally low metamorphic grade; and contains a diverse spectrum of richly mineralized deposits.

Historically, the western limit of the AGB has been associated with a north-trending chain of Archean granitoid complexes including the Kenogamissi Batholith and complexes west and northwest of Timmins. The boundary between these granitoid complexes and the southern AGB is spatially associated with the northern extension of faults related to the western margin of the Cobalt Embayment. These faults are generally east-side-down normal structures with a component of apparent sinistral horizontal displacement. Consequently, the region west of these faults, that extends northward from the western margin of the Cobalt Embayment, may simply represent a deeper erosion level of a once-continuous greenstone belt extending at least to the Ivanhoe lake cataclastic zone.

The AGB consists of a northern (internal) belt and a southern (external) belt. The northern belt is characterized by abundant tonalite-trondhjernite-granodiorite intrusions, large anorthosite complexes, paucity of ultramafic flows, and greenschist or higher regional metamorphism. The southern belt is characterized by fewer tonalite-trondhjemite-granodiorite intrusions, abundant ultramafic flows, and greenschist or lower regional metamorphism. In Ontario, only a limited part of the northern AGB is preserved in the Detour and Burntbush areas, north of the Lake Abitibi Batholith. The following overview is mainly concerned with the southern AGB.

In the southern AGB, matavolcanic and associated metasedimentary units, and synvolcanic peridotite to granodiorite intrusions formed between -2.75 and -2.70 Ga. Relatively old rocks, such as the -2.8 billion-year-old felsic metavolcanic rocks of the Obatagamau Formation near Chibougamau, have not been found in the southern AGB. Between -2.70 and -2.68 Ga, large volumes of foliated tonalite-granodiorite batholiths were emplaced followed by more massive granodiorite, granite, feldspar quartz porphyry, and syenite bodies. During and subsequent to this magmatism, alluvial-fluvial clastic metasedimentary rocks and alkalic metavolcanic rocks formed and are now in spatial association with regional, steeply dipping shear zones (ie. 9 Porcupine-Destor deformation zone and Larder-Cadillac shear zone). Regional deformation occurred prior to, and after, formation of the alluvial-fluvial clastic metasedimentary rocks and associated alkalic metavolcanic rocks. Metamorphic grade within the supracrustal rocks is generally subgreenschist to greenschist facies and rises to amphibolite facies near some intrusions.

Bedding and tectonic fabric in the southern AGE generally dip steeply to moderately (900 to 450); however, shallow dips are present in some areas such as the core of the Blake River group, southwest of Timmins, in the northern Swayze area and the area adjacent to the Kenoramissi Batholith. Folds are generally east or west trending and upright. There are south-verging thrust faults that predate and postdate deposition of the younger alluvial-fluvial metasedimentary and alkalic metavolcanic rocks.

Major gold camps (ie. Timmins, Kirkland Lake, Kerr Addison and Val D©Or) are spatially associated with steeply dipping shear zones, such as the Larder-Cadillac shear zone and the Procupine-Destor deformation zone which transect the belt for over 300 km in a general easterly direction. In general, steeply dipping foliations and steeply plunging stretching lineations and minor folds characterize these zones and both dextral and sinistral horizontal components of displacement are reported. The shear zones are spatially associated with the youngest supracrustal and plutonic assemblages and, in part, deform these assemblages. These obervations indicate that the shear zones were active late in the history of the greenstone belt; an earlier history is difficult to substantiate, but has been suggested. Correlation of rock assemblages across these shear zones has not been unequivocally demonstrated. The Larder-Carillac shear zone, in part, marks the boundary between the southern Abitibi greenstone belt and the Pontiac Subprovince.

Local Bedrock Geology

The Claw Lake property lies within the Shinning Tree area which is bounded to the northwest by the Kenogamissi Batholith; southwest by the Ramsey - Algoma granitoid complex; and east by uncomformably overlying Paleoprotezonic rocks of the Hurnonian Supergroup. The area has been broadly subdivided into five main assemblages ( after Jackson and Fyon , 1991). these assemblages are : Natal, Cabot-Kelvin, Shining Tree, Sinclair and Ridout. Of regional significance to the Claw Lake property are the Cabot - Kelvin , Shining Tree and Ridout assemblages.

The Cabot-Kelvin assemblage underlies most of Cabot and Kelvin townships and consists mainly of calcalkalic mafic to felsic metavolcanic rocks. It is underlain by tholeiitic basalts of the Shining Tree assemblage to the north and west.

The Ridout assemblage is the youngest assemblage in the Shining Tree area and unconformably overlies the Cabot-Kelvin assemblage to the south and consists of turbidites, arkose and conglomerate with minor interbeded units of metavolcanics and iron formation. The conglomerate contain pebbles of chert, vein quartz, basalts, andesite, porphyritic rhyolite and jasper fragments. The Ridout assemblage underlies part of Cabot, Connaught and Churchill 10 Townships in the southern portion of the Claw Lake property. It is thought that the Ridout assemblage is temporally and tectonically related to the Timiskaming assemblage of the Kirkland Lake area.

The rocks of these assemblages have been affected by greenschist facies metamorphism.

The felsic intrusive rocks occur as parts of large batholithic complexes and as elliptical and circular stocks intrusive into the metavolcanics-metasediments. The batholithic masses are mainly massive and prophyroblastic but are gneissic along their borders and are believed to be syntectonic. The main batholiths are the Togo Batholith located in the northwest of the property and the Miramichi Batholith south of the property. These are separated by an east-west trending band of metavolcanics-metasediments. The eastern boundary of the Togo Batholith is in faulted contact with the metavolcanics and metasediments but locally shows intrusive relationships with these rocks along the southern boundary. The Miramichi Batholith shows intrusive relationships on its northern, northeastern, and eastern contacts with the enclosing metavolcanics- metasediments. These contacts are parallel to the regional structure and this batholith is therefore also syntectonic and probably mesozonal. Both batholiths are comprised of quartz monzonite, massive and porphyroblasitic granodirotie, and trondhjemite.

The elliptical and circular stocks are entirely enclosed by the metavolcanics and measediments. Only the 2 largest of these bodies have been given names: the Claw Lake Stock, located within the property and the Milly Creek Stock, northeast of the property. The rocks are late tectonic and consist of diorite, quartz diorite, syenodiorite and trondhjemite.

The Ketchiwaboose Lake Fault is a major 10 to 11 kilometre long NW trending fault that crosses the property in the west and continues into Connaught Township where it becomes the Elephant Head Lake Fault. This fault has been interpreted to be downthrown to the west (Carter, 1986).

Government geologists (Cartier, 1986) have indicated from strike and dip measurements that there is a syncline with an axis striking N50E northwest of the property.

The past-producing Tyranite and Ronda gold mines in the Shining Tree assemblage, located near the village of Shining Tree, are the only known significant mineralization within the Shining Tree area (Carter, 1987). These two mines produced 34,079 oz of gold and 9690 oz of silver in the period 1939-42 (Carter, 1987). The gold is associated with quartz veins within carbonatized northwest trending shear zones.

Quaternary Geology

Sand deposits forming sand plains cover most of the northern portion of the property and comprise glacial outwash deposits (Boissonneau 1965). The sands are pale brown, yellow and white and are angular fine sands. Occurring on those plains are narrow steep ridges of sand, up to about 19 m in relief, forming a set of sand dunes convex to the south-southeast. Also associated li with the dunes are glaciofluvial esker deposits comprising sand and lesser amounts of gravel trending west-southwesterly. These features are best seen along the northern edge of the property. Swamp deposits consisting of muskeg form large areas in the southern part of the property.

The western half of Claw Lake is reported to contain a marl deposit (Cartier, 1986). This material is impure calcium carbonate that occurs on the bottom of the lake and probably represents the remnants of a former glacial lake.

6.0 GEOCHEMICAL PROGRAM RESULTS

Lake Sediment Sampling Program

As part of the regional gold exploration program lake bottom sediment samples were collected from Claw Lake during July, 1995 (Maps 4 and 8).

Ten (10) samples (95CL001 to 95CL10) were collected from a 12 foot fiberglass boat using a Hornbrook sampler. The samples consisted of black to black-green gytta mixed with grey-green clay rich "marl" and were collected from an average depth of 4.4 metres with a maximum depth of 10 metres.

Sample preparation and analysis was performed by Bondar-Clegg in Ottawa, Ontario. Samples were dried, ashed and pulverized with a ceramic ring to ^00 mesh (*^150microns). Au was determined by FA/DCP (30.0g) and a subsequent split (1.0 g) was then analyzed for 34 elements by ICP/MS following an aqua regia digestion. Analytical methods and laboratory results for the lake bottom sediments are presented in Appendix B. Sample locations and results are located on Maps 5,6,7,9,10 and 11.

All the lake bottom sediment sample results reported at or near the lower detection limit for Au and all other elements. The highest reported value for Au was 11 ppb from the standard inserted with these samples (ie.95CL011). It was anticipated that results could be affected by the "marl layer" and the lack of anomalous results would appear to confirm this.

12 7.0 GEOLOGICAL PROGRAM RESULTS

The portions of the Claw Lake property that do not contain grid were mapped/ prospected and rock sampled by conducting traverses along existing roads, trails, power lines, lake shores, streams and compass/pace lines through the bush.

A brief description of the main rock types that were observed over the entire property follows:

Conglomerate: light to moderate grey with a fine to medium grained groundmass with polymictic cobble to boulder sized clasts of felsic volcanic, mafic volcanic, quartz porphyry and granite.

Chert: buff brown to grey and massive.

Felsic tuff: light grey to grey-green and fine to medium grained with minor feldspar crystals and chloritized lithic fragments.

Intermediate tuff: moderate grey to grey-green and fine to medium grained with minor feldspar crystals and chloritized lithic fragments.

Mafic tuff: dark grey to grey-green and fine to medium grained with minor feldspar crystals and chloritized lithic fragments.

Felsic dyke: light grey to buffbrown and fine grained to massive.

Quartz porphyry dyke: light grey to buffbrown with a massive groundmass and S-15% fine to medium grained quartz phenocrysts.

Quartz feldspar porphyry dyke: light grey to buff brown with a massive ground mass and S-20% fine to medium grained quartz and feldspar phenocrysts.

Granite: light to moderate grey to reddish, medium to coarse grained with K-spar , quartz and biotite as the main minerals present.

Granite porphyry: light to moderate grey to reddish, medium to coarse grained with K-spar and quartz as the main minerals present.

Diorite: dark grey-green and medium to coarse grained with plagioclase and amphibole as the main minerals present.

13 Diabase: dark green to black and fine to coarse grained with plagioclase, amphibole and magnetite as the main minerals present.

Felsic volcanic: light grey to buff brown and fine grained to massive.

Intermediate volcanic: grey-green and massive to fine grained with ^0/* amphibole phenocrysts.

Mafic volcanic: grey-green to black and massive to fine grained with ^0/* amphibole and/ or pyroxene phenocrysts.

Schist: light to moderate grey-green, fine grained and strongly sheared with chlorite or sericite as the main mineral present.

The western portion of the Claw Lake property in Connaught Township (Map 3) is underlain mainly by the Shining Tree assemblage with lesser amounts of the Ridout assemblage present (Jackson and Fyon, 1991). This area contain little outcropped and those observed consisted of moderate to dark grey-green, fine to medium-grained mafic volcanics that are locally strongly sheared to sericite and/or chlorite shist. Structurally, S2 is moderately developed with variable strikes 070-110 degrees with steep (75-85) north or south dips. Alteration is locally well developed with strongly ankeritized mafic volcanics containing 1-3 "/o hairline to 5 centimetre quartz-ankerite-pyrite (trace) veins.

None of the rock samples (Map 8) assayed were anomalous in Au-As-Sb (Map 9, Appendix C), Ag-Mo-Cu (Map 10, Appendix C) or Zn-Pb-Ni (Map 1 1, Appendix C).

The Ridout assemblage outcrops in the southern part of the property (Map 2) and consists of moderate grey-green, fine to medium grained mafic volcanics and light grey to brown polymictic conglomerate with mafic volcanic and quartz pebbles. These rocks are cross-cut by quartz porphyry dykes that are either parallel to or at a low angle to S2. There is well developed alteration consisting of quartz-ankerite-pyrite (trace to minor) veins and variable ankeritized chlorite schists and conglomerates. Structurally, S2 is very well developed, as shearing is moderately to very strongly developed, with 090-120 degree strike and variable (45-90) north dips. Old trenches were mapped and sampled (Map 3). The chlorite-sericite schists in these trenches are very strongly sheared and highly ankeritized (40-90^. Narrow (ie. l metre) quartz- feldspar porphyry dykes with quartz-ankerite-pyrite (minor-2%) veins occur at low angles and parallel to S2 .

None of the rock samples (Map 8) assayed were anomalous in Au-As-Sb (Map 9, Appendix C), Ag-Mo-Cu (Map 10, Appendix C) or Zn-Pb-Ni (Map 1 1, Appendix C).

14 The area centered on Claw Lake (Map 3) is underlain mainly by rocks of the Cabot-Kelvin assemblage and the Claw Lake Stock. Work here was along grid lines (1996) cut at 200 metre centres and along regional compass/pace traverses (1995).

The most common rocks are the mafic and intermediate metavolcanics. Characteristically they are aphyric, aphanitic massive flows varying in colour from dark green to medium grey, respectively. Where porphyritic, these flows exhibit equant feldspar phenocrysts 1-5 mm in diameter. Structure is generally absent in the mafic metavolcanics with good foliation developed only at zones of contact. Mafic to felsic tuffs also occur that lack bedding and sorting. The tuffs are generally massive and unstratified ranging from fine grained ^ .5 mm) to coarse grained (2 mm) along. The felsic meatavolcanics are light grey to pale pink in color and are aphanitic.

The intrusive rocks consists of massive, fine to medium grained biotite granite, granite porphyry and diorite. Quartz porphyry and quartz feldspar prophyry dykes cross cut these rock types and the metavolcanics. North-westerly trending black, massive, medium to fine grained and highly magnetic diabase dykes occur locally in the metavolcamics. Structurally, S2 is best developed within the known mineralized showings and strikes 070-090 degrees with variable dips both north and south.

Geological mapping in areas of known mineralization outlined several l to 5 metre wide, 800 metre long, 080 trending shear zones associated with the Galena, Molybdenite and Hillside Veins. This mineralization consisted of quartz-ankerite-pyrite veins in sheared and ankeritized quartz and quartz-feldspar porphyry dykes. Several rock samples were auriferous (ie. 300 ppb to 17.9 g/t). The sample locations and assay results for the rock samples (Map 8) assayed for Au-As-Sb (Map 9, Appendix C), Ag-Mo-Cu (Map 10, Appendix C) and Zn-Pb-Ni (Map11, Appendix C) are attached at the back of this report.

The trace of the Beaver shear zone was extended 300 metres further to the northeast from its location by previous workers. Minor anomalous gold (ie. < 300 ppb) was outlined in bedrock. The sample locations and assay results for the rock samples (Map 8) assayed for Au-As-Sb (Map 9, Appendix C), Ag-Mo-Cu (Map 10, Appendix C) and Zn-Pb-Ni (Map11, Appendix C) are attached at the back of this report.

In the area of the Rapids and First Rapids Veins well developed shear zones containing quartz- ankerite-pyrite stockworks and veins with locally very well developed silicification were mapped and sampled. Gold values ranged from < 300 ppb to 4.1 g/t. The sample locations and assay results for the rock samples (Map 8) assayed for Au-As-Sb (Map 9, Appendix C), Ag-Mo-Cu (Map 10, Appendix C) and Zn-Pb-Ni (Mapll, Appendix C) are attached at the back of this report.

15 8.0 GEOPHYSICAL PROGRAM RESULTS

Introduction:

A program of reconnaissance level induced polarization and resistivity (ip/res), and total field magnetic profile surveying was conducted to test the possible large scale extent of known shears and auriferous quartz-veins striking EW to NE through the Claw Lake Stock.

Both total field magnetic, and, IP/res surveying was completed over selected lines of the Claw Lake Grid from January 17, to February 8, 1997, under contract by JVX Ltd. of Richmond Hill, Ontario. Survey specifications, instrument descriptions, and names of survey personnel are documented in a contractor©s report in Appendix D.

Total Field Magnetic Survey:

In total, 34.77km of diurnal drift corrected total field magnetic surveying was completed. Survey profiles with data values posted are presented at 1:5000 scale in Plate 7 in Appendix D.

Magnetic data profiles indicate high amplitude (MOOOnT), short spatial wavelength anomalism along most lines surveyed. Line-to-line correlation of anomalies is difficult with the wide (200-400m) line spacing used in the survey.

IP/Resistivity Survey:

A total of 16.15km of time domain IP/resistivity surveying was completed over selected lines using the pole-dipole array with a dipole spacing (a-spacing) of 50m, and readings at n^ through 6. A Scintrex TSQ-3, 3kW transmitter and IPR-12 receiver were used for the survey.

Survey results are presented as standard pole-dipole pseudosections of apparent resistivity and chargeability, in Plates l through 6 of Appendix D. Also appearing on the pseudosections, but not considered in the interpretation below, are two computed Cole-Cole spectral parameters, namely M-IP and time constant tau.

16 Geophysical Data Interpretation:

Anomalous polarizable (IP) and resistive zones are highlighted with bars on the pseudosection plots in Plate l through 6 of Appendix E. The IP anomalies are graded subjectively into definite, probable and possible anomalies based on their amplitude and anomaly form. Definite anomalies have recognisable "pantleg" anomaly form and chargeability amplitudes exceeding lOmV/V. Possible anomalies have poor or absent pantleg anomaly form and low chargeability amplitude. Most IP anomalies in the survey are associated with high resistivity which makes them interesting even at low chargeability amplitude.

IP and resistivity anomalies are compiled, and several key anomalies are identified as significant, in a geophysical data interpretation in Plate 8 of Appendix D. Key anomalies outlined on Plate 8 are summarized as follows:

Zone A: There are two, weak anomalous trends within Zone A. Trend XX© is a weak IP and resistivity high anomaly that can be spatially correlated with a complex EW striking magnetic anomaly trend. The magnetic anomaly trend suggests magnetite or pyrhotite spatially associated with disseminated sulphides that cause the IP anomaly. High apparent resistivity suggests silicification along the trend.

IP anomalies Y and Z taken together, appear aligned parallel to trend XX© however only anomaly Y is magnetically anomalous. Trend XX© , and IP/res anomaly X are spatially associated with mapped outcrops of sheared quartz and quartz-feldspar porphyries that contain auriferous quartz-py veins.

The continuity of Zone A, east of anomaly Z, into Claw Lake, and also west, remains undefined.

Anomaly B: Anomaly B is the only definite IP anomaly detected in the survey. The anomaly correlates with a resistivity high but has no appreciable magnetic correlation. Up to \*A disseminated pyrite in mafic volcanic rocks is outcropping in the vicinity of the anomaly. Anomaly B is of no further exploration interest.

17 CONCLUSIONS AND RECOMMENDATIONS

The geological mapping outlined several l to 5 metre wide, 800 metre long, 080 trending shear zones in the area of the Galena, Molybdenite and Hillside Veins. Several rock samples were auriferous (ie. 300 ppb to 17.9 g/t). This mineralization consisted of quartz-ankerite-pyrite veins in sheared and ankeritized quartz and quartz-feldspar porphyry dykes, the trace of the Beaver shear zone was extended 300 metres further to the north-east from its location by previous workers. Minor anomalous gold (ie. < 300 ppb) was outlined in bedrock. In the area of the Rapids and First Rapids Veins well developed shear zones containing quartz-ankerite-pyrite stockworks and veins with locally very well developed silicification. Gold values ranged from < 300 ppb to 4. l g/t.

The geophysical surveys outlined low amplitude chargeability IP, high amplitude resistivity and complex magnetic anomalies that coincide with the auriferous quartz-ankerite-pyrite veins in sheared quartz and quartz-feldspar porphyries of the Galena, Molbdenite and Hillside Veins. A second low amplitude IP and high amplitude resistivity anomaly occurs 500 metres north-east of the above anomaly and can be explained by the presence of 0.5 - l *Yo disseminated pyrite in mafic volcanics.

Drill testing of the Galena, Molybdenite and Hillside Veins area is recommended.

18 10.0 REFERENCES

Jackson, S.L. and Fyon, A.J., 1991: The western Abitibi subprovince in Ontario; in Geology of Ontario, OntarioGeological Survey, Special Volume 4, Part l, p. 405-482.

Boissonneau, A.N. 1965: Surficial Geology : Algoma, Sudbury, Timiskaming and Nipissing. Map S465, scale 1:506 880 or 8 miles to l inch. Ontario Department of Lands and Forests.

1980: Geology of Connaught and Churchill Townships, District of Sudbury; Ontario Geological Survey Report 190, 81p. Accompanied by Geological Map 2414, scale 1:31 680 or l inch to ©/2 mile.

Cartier, M. W. 1986: Geology of Cabot and Kelvin Townships, District of Sudbury. Ontario Geological Survey report 249. 52p.

1987: Geology of the Shining Tree Area, Districts of Sudbury and Timiskaming. Ontario Geological Survey Report 240. 41 p.

Coleman, A.P. 1901: Iron Ranges of the Lower Huronian; Ontario Bureau of Mines, Volume 10, p. 182

Gledhill, T.L. 1926: Notes of the South Part of the Grassy River Area; Ontario Department of Mines, Volume 35, Part 6, p. 77082 (published 1927). Accompanied by Map 35j, scale l inch to Vi mile.

Laird, H.C. 1934: Geology of the Makwa-Chruchill Area; Ontario Department of Mines, Volume 43, Part 3, p. 37-80 (published 1935). Accompanied by Map 43c, scale l inch to l mile.

Parks, W.A. 1900: Niven©s Base Line, 1899; Ontairo Bureau of Mines, Volume 9, p. 127, 141 Accompanied by unnumbered map, scale l inch to 8 miles.

19 EXPLORATION

CERTIFICATE OF QUALIFICATIONS

I, Alan J. Sexton, of the City of Nepean, Province of Ontario, do hereby certify that:

(1) I am a Senior Geologist with WMC International Linited, residing at 118 Fieldgate Drive, Nepean, Ontario, K2J 1T9.

(2) I am a graduate of St. Marys University with an Honours Bachelor of Science degree in Geology (l982).

(3) I am a graduate of Acadia University with a Master of Science degree in Geology (1988).

(4) I have been practising my profession continuously since 1982.

(5) I am a member in good standing of the: Prospectors and Developers Association of Canada (PDAC) Porcupine Prospectors and Developers Association (PPDA) Association of Exploration Geochemists (AEG) Northern Prospectors Association (NPA) Association of Economic Geologists (AEG) Quebec Prospectors Association (QPA)

(6) I supervised the work relevant to this report from June 20 , 1995 to February 15 , 1996.

Signed at the City of Nepean, this 15th day of February , 1997.

WMC International Limited Americas Division J © ©*\l/© VJ Exploration

Alan J. Sexton, M.SC. 22 Gurdwara Road Nepean, Ontario Canada K2E 8A2 Tel (613)727-3937 Fax (613) 727-3970

A member of the WMC Limited group of companies STATEMENT OF QUALIFICATIONS

I, Anne collins, of the city of Ottawa, Province of Ontario, do hereby certify that:

1) I am a Database Geologist with WMC International Limited, resident in the City of Ottawa, Ontario. 2) I am a graduate of the University of New Brunswick with a Bachelor of Science degree in Geology (1982). 3) I am a graduate of Memorial University of Newfoundland with a Bachelor of Science degree in Geography (1992). 4) I have been practicing my profession continuously since 1995. 5) I compiled the geochemical data relevant to this report.

Dated at the City of Nepean, this 21"* day of February, 1997.

Anne Collins Database Geologist Certificate of Qualification

l, Roman Tykajlo, of the City of Nepean, Province of Ontario, do hereby certify that:

1) l am a geophysicist with WMC International Limited, residing at 74 Stonebriar Drive, Nepean, Ontario, K2G 5X9

2) l am a graduate of Lakehead University with an Honours Bachelor of Science degree in Geology l Physics (1978).

3) l have been practicing my profession since graduation.

4) l am a member of: Society of Exploration Geophysicists (SEG) Association of Professional Engineers, Geologists and Geophysicists of Alberta (APEGGA)

5) l supervised the work relevant to this study from January 2, to February 19, 1997.

Dated at the City of Nepean, this 19th day of February, 1997.

BSc, PGeol. APPENDIX A : LIST OF EXPENDITURES Man days worked on the Claw Lake property for the work covered in this report.

NAME POSITION DAILY NUMBER OF DAYS SALARY RATE WORKED TOTAL 1995 1996 1997 Alan Sexton Senior S 250.00 20 21 5 S 11,500.00 Geologist Roman Tykajlo Senior S 250.00 026 S 2,000 Geophysicist Anne Collins Database S 200.00 224 S 1,600 Geologist Pam Chiles Land S 250.00 1 1 1 S 750 Manager Lo Wu Senior S 200.00 224 S 1,600 Draftsman Tyler McKinnon Junior S 100.00 700 S 700 Assistant Geologist S 150.00 0 15 0 S 2,250 Manfred Hebel Geologist S 150.00 800 S 1,200 Craig Finnigan Junior S 100.00 030 S 300 Assistant Steve McGlade Junior S 100.00 900 S 900 Assistant

TOTAL S 22,800 The following expenditures were incurred on the Claw Lake property exploration program between June 20, 1995 and October 15, 1995.

TYPE OF WORK EXPENDITURE COMPANY PAID Salaries ( mapping, sampling) S 8,850.00 WMC International Ltd. Float plane flights S 800.00 Derry Air Ltd. camp rental and boat rental S 1200.00 Geochemical survey costs: - Rock assaying (sample prep S 3446.00 Swastika Laboratories and analyses). - Preparation and analytical S 249.99 Bondar Clegg te Company processing of lake sediment Ltd. samples. Transportation charges S 129.81 Esso Radio rental S 291.60 Christie & Walther S 163.08 New East Communications S 2000.00 Spectrum 2000 TOTAL (exclusive of GST) S 17,130.48 The following expenditures were incurred on the Claw Lake property exploration program between June l, 1996 and December 20, 1996.

TYPE OF WORK EXPENDITURE COMPANY PAID Salaries (mapping .sampling) S 9350.00 WMC International Ltd. Grid cutting S 25,670 Shortt Exploration Services Float plane flights S 1000.00 Derry Air Ltd. boat rental S 272.00 Geochemical survey costs: S 1247.75 Swastika Laboratories - Rock assaying (sample prep and analyses). Transportation charges S 526.01 Esso Radio rental S 1,546.32 Ottawa Communications ATV rental S 1,299.61 Kenogami Garage St, Marine

TOTAL (exclusive of GST) S 40,911.61 The following expenditures were incurred on the Claw Lake property exploration program between January l, 1997 and February 15, 1997.

TYPE OF WORK EXPENDITURE COMPANY PAID Salaries (report writing, S 4,600.00 WMC International Ltd. geophysical survey supervision). Geophysical survey costs: JVX Limited - IP survey S 42,857.00 - Magnetic survey S 3,824.00 Helicopter transportation S 23,575.80 Skytech Aviation Ltd. Radio rental S 500.00 Ottawa Communications TOTAL S 75,357.60 APPENDIX B: ANALYTICAL RESULTS, LAKE BOTTOM SEDIMENTS

SAMPLES, 1995 Geochemical Bondar Clegg Lab :^^ Inchcape Testing Services Report

UMC INTERNATIONAL MR. TERRY GOODWIN 22 GURDWARA RO. NEPEAN, ONTARIO K2E 8A2

Bondar-Clegg Si Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical Bondar Clegg Lab Inchcape Testing Services Report

^REPORT: 095-40435.O ( COMPLETE ) REFERENCE: -

CLIENT: WMC INTERNATIONAL SUBMITTED BY: T. GOODWIN ;PROJECT: 4054 G10 DATE PRINTED: 23-AUG-95

NUMBER OF LOWER i ORDER ELEMENT ANALYSES DETECTION LIMIT EXTRACTION METHOD

1 AU GOLD FIRE ASSAY 11 1 PPB FIRE ASSAY FIRE ASSAY-DCP 2 Ag Silver 11 0.2 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA

3 Cu Copper 11 1 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA 4 Pb Lead 11 2 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA 5 Zn Zinc 11 1 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA 6 Mo Molybdenum 11 1 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA 7 Ni Nickel 11 1 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA

8 Co Cobalt 11 1 PPM HCL:HN03 (3: D INDUC. COUP. PLASMA ; 9 ea Cadmium 11 0.2 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA 10 Bi Bismuth 11 5 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA i 11 As Arsenic 11 5 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA 12 Sb Antimony 11 5 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA

13 Fe Iron 11 0.01 PCT HCL: HN03 (3: D INDUC. COUP. PLASMA 14 Mn Manganese 11 1 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA 15 Te Tellurium 11 10 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA 16 Ba Barium 11 1 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA 17 Cr Chromium 11 1 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA

18 V Vanadium 11 1 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA 19 Sn Tin 11 20 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA 20 W Tungsten 11 20 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA i 21 La Lanthanum 11 1 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA 22 Al Aluminum 11 0.01 PCT HCL: HN03 (3: D INDUC. COUP. PLASMA

23 Mg Magnesium 11 0.01 PCT HCL: HN03 (3: D INDUC. COUP. PLASMA : 24 Ca Calcium 11 0.01 PCT HCL: HN03 (3: 1) INDUC. COUP. PLASMA 25 Na Sodium 11 0.01 PCT HCL: HN03 (3: D INDUC. COUP. PLASMA 26 K Potassium 11 0.01 PCT HCL: HN03 (3: D INDUC. COUP. PLASMA 27 Sr Strontium 11 1 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA

28 Y Yttrium 11 1 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA 29 Ga Gal l i urn 11 2 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA 30 Li L i th i urn 11 1 PPM HCL: HN03 (3: D INDUC. COUP. PLASMA 31 Nb Niobium 11 1 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA 32 Se Scandium 11 5 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA

33 Ta Tantalum 11 10 PPM HCL: HN03 (3: 1) INDUC. COUP. PLASMA 34 Ti Titanium 11 0.01 PCT HCL:HN03 (3: 1) INDUC. COUP. PLASMA 35 Zr Zirconium 11 1 PPM HCL:HN03 (3: D INDUC. COUP. PLASMA 36 LOI Loss on Ignition 11 0.01 PCT GRAVIMETRIC

Bondar-Clegg & Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical Bondar Clegg Lab ^^ Inchcape Testing Services Report

REPORT: 095-40435.0 ( COMPLETE ) REFERENCE: -

CLIENT: WMC INTERNATIONAL SUBMITTED BY: T. GOODWIN PROJECT: 4054 G10 DATE PRINTED: 23-AUG-95

SAMPLE TYPES NUMBER SIZE FRACTIONS NUMBER SAMPLE PREPARATIONS NUMBER

LAKE SEDIMENT 11 -100 11 AS RECEIVED 1 CERAMIC PULVERIZE 10

REPORT COPIES TO: MR. TERRY GOODWIN INVOICE TO: MS. DIANA CAMPBELL BY FAX: T. GOODWIN ALAN SEXTON

Bondar-Clegg St Company Ltd. 5420 Canoiek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical Bondar ^^ Inchcape Testing Services Report

DATE PRINTED: 23-AUG-95 REPORT: 095-40435.0 ( COMPLETE ) PROJECT: 4054 G10 PAGE 1A

SAMPLE ELEMENT AU Ag Cu Pb Zn Mo Ni Co Cd B i As Sb NUMBER UNITS PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM ...... ^...... 95CL01 1 O.2 17 3 48 3 16 2 0.3 ^ *5 95CL02 *:1 0 .2 22 3 43 9 10 2 0. 2 ^ ^ ^ 95CL03 O O.2 32 2 72 5 26 5 0.4 ^ ^ ^ 95CL04 1 O.2 22 2 53 6 14 2 0. 2 ^ ^ ^ . 95CL05 0 O.2 6 2 24 0 9 3 0.2 ^ ^ ^ ...... ^...... 95CL06 1 O.2 12 5 82 1 19 8 0.3 ^ <5 95CL07 0 0.2 9 7 61 1 15 6 0.3 *5 5 <5 95CL08 <1 0. 2 11 7 69 1 17 6 0.4 ^ ^ <5 95CL09 1 0. 2 13 9 73 1 19 6 0.3 ^ 6 ^ ; 95CL10 <1 0.2 8 8 68 1 18 6 0.2 G 5 <5

95CL11 11 0.3 20 19 167 42 32 0.5 39

Bondar-Clegg A Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KU 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical Bondar Clegg Lab ^^ Inchcape Testing Services Report

DATE PRINTED: 23-AUG-95 REPORT: 095-40435.0 ( COMPLETE ) PROJECT: 4054 G10 PAGE 1B

; SAMPLE ELEMENT Fe Mn Te Ba Cr V Sn W La Al Mg Ca NUMBER UNITS PCT PPM PPM PPM PPM PPM PPM PPM PPM PCT PCT PCT i 95CL01 (3.64 94 ^0 45 18 11 ^0 ^0 10 0 .30 0 .13 1.02 95CL02 .19 392 *:10 60 10 9 ^0 <20 13 0 .20 0 .30 MO. 00 l 95CL03 .62 184 -dO 49 25 19 ^0 <20 16 0 .45 0 .25 2.82 95CL04 ().85 296 <10 50 14 11 ^0 <20 11 0 .27 0 .37 MO. 00 95CL05 ().34 72 ^0 13 30 7 ^0 ^0 8 0 .26 0 .14 0.57

95CL06 .54 558 <10 43 40 19 ^0 <20 18 0 .76 0 .42 0.78 95CL07 .04 428 *:10 34 31 16 ^0 <20 14 0 .60 0 .33 0.66 95CL08 .09 479 <10 42 34 18 <20 <20 15 0 .68 0 .36 0.89 95CL09 .08 450 ^0 45 37 20 ^0 <20 14 0 .76 0 .40 0.93 95CL10 .07 324 ^0 29 35 16 <20 ^0 13 0 .54 0 .36 0.55

95CL11 2.73 1009 105 21 13 45 2.10 0.37 0.15

Bondar-Clegg & Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical j—/au ~^^ Inchcape Testing Services Report

DATE PRINTED : 23-AUG-95 REPORT: 095-40435.0 ( COMPLETE ) PROJECT: 4054 GIO PAGE 1C

: SAMPLE ELEMENT Na K Sr Y Ga Li Nb Se Ta Ti Zr LOI ; NUMBER UNITS PCT PCT PPM PPM PPM PPM PPM PPM PPM PCT PPM PCT i 95CL01 0.01 0.03 17 4 ^ 2 O ^ ^0 0.01 3 58.94 ! 95CL02 0.01 0.02 77 2 ^ 2 ^ ^ <10 ^.01 2 49.50 95CL03 0.01 0.03 32 5 ^ 4 ^ ^ <10 0.02 6 55.88 95CL04 0.01 0.02 75 3 ^ 3 O ^ <10 <0.01 3 50.59 : 95CL05 0.01 0.02 14 3 ^ 3 O <5 :10 0.02 1 14.11

95CL06 0.01 0.05 19 5 ^ 7 <1 <5 <10 0.03 2 23.12 95CL07 0.01 0.04 16 4 ^ 6 <1 ^ <10 0.03 1 19.53 95CL08 0.01 0.05 18 4 ^ 6 <1 <5 ^0 0.03 1 25.51 95CL09 0.01 0.05 19 4 ^ 6 <1 <5 <10 0.03 1 34.07 95CL10 0.01 0.04 14 3 ^ 5 ^ <5 ^0 0.03 1 14.55

95CL11 0.07 11 11 ^ 30 <1 <5 <10 <0.01 2 24.45

Bondar-Clegg & Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical Bondar Clegg Lab ^^ Inchcape Testing Services Report

DATE PRINTED: 23-AUG-95 REPORT: 095-40435.0 ( COMPLETE ) PROJECT: 4054 G10 PAGE 2A

STANDARD ELEMENT AU Ag Cu Pb Zn Mo Ni Co Cd B i As Sb NAME UNITS PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM

UMT-1 CANMET STD 46 ------Number of Analyses 1 ------Mean Value 46.0 ------Standard Deviation ------Accepted Value ------

BCC GEOCHEM STD 5 0.7 84 8 75 3 34 19 0.2 G 21 <5 Number of Analyses 1 1 1 1 1 1 1 1 1 1 1 Mean Value 0.74 83.5 7.9 74.9 3.4 34.0 18.9 0.10 2.5 20.7 2.5 Standard Deviation ------Accepted Value 0.7 90 11 80 2 40 18 0.1 1 8 1

ANALYTICAL BLANK O.2 *1 ^ <1 <1 <1 O O.2 *5 <5 *5 Number of Analyses 1 1 1 1 1 1 1 1 1 1 1 Mean Value 0.10 0.5 1.0 0.5 0.5 0.5 0.5 0.10 2.5 2.5 2.5 Standard Deviation ------Accepted Value 1 0.2 1 2 1 1 1 1 1.0 2 5 5

Bondar-Clegg & Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical Bondar Clegg Lab ^^ Inchcape Testing Services Report

DATE PRINTED: 23-AUG-95 iREPORT: 095-40435.0 ( COMPLETE ) PROJECT: 4054 G10 PAGE 2B

: STANDARD ELEMENT Fe Mn Te Ba Cr V Sn W La A l Mg Ca l NAME UNITS PCT PPM PPM PPM PPM PPM PPM PPM PPM PCT PCT PCT

:UMT-1 CANMET STD ; Number of Analyses Mean Value ;Standard Deviation Accepted Value

;BCC GEOCHEM STD 5 3.93 690 160 38 96 20 2.61 1.73 0.83 ;Number of Analyses 1 1 1 1 1 1 1 1 1 1 1 1 Mean Value 3.929 690.1 5.0 159.7 38.2 96.1 10.0 10.0 20.3 2.613 1.733 0.829 Standard Deviation i Accepted Value 4.74 720 200 54 133 3.09 1.83 1.08

^ANALYTICAL BLANK 0.01 O ^0 O :1 ^0 ^0 <1 O.01 0.01 i Number of Analyses 1 1 1 1 1 1 1 1 1 1 1 1 ;Mean Value 0.005 0.5 5.0 0.5 0.5 0.5 10.0 10.0 0.5 0.005 0.005 0.005 Standard Deviation . . Accepted Value 0.05 -O -O 0.01 O.01

Bondar-Clegg b Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical Bondar Clegg Lab ^SF" Inchcape Testing Services Report

DATE PRINTED: 23-AUG-95 iREPORT: 095-40435.0 ( COMPLETE PROJECT: 4054 G10 PAGE 2C

STANDARD ELEMENT Na K Sr Y Ga Li Nb Se Ta T i Zr LOI i NAME UNITS PCT PCT PPM PPM PPM PPM PPM PPM PPM PCT PPM PCT

UMT-1 CANMET STD Number of Analyses :Mean Value Standard Deviation Accepted Value

BCC GEOCHEM STD 5 0.05 0.28 31 5 *2 23 <1 7 •dO 0.18 9 Number of Analyses 1 1 1 1 1 1 1 1 1 1 1 Mean Value 0.048 0.280 31.0 5.2 1.0 22.8 0.5 7.4 5.0 0.177 9.2 Standard Deviation Accepted Value 0.06 0.26 39 9 - - - 18 1 9

ANALYTICAL BLANK Number of Analyses 1 1 1 1 1 1 1 1 1 1 1 Mean Value 0.005 0.005 0.5 0.5 1.0 0.5 0.5 2.5 5.0 0.005 0.5 Standard Deviation

Accepted Value •eO.OI KO.OI •:1 •d •d •d <1 •d *1 *0.01 *1 *0.01

Bondar-Clegg A Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical Bondar Clegg Lab ^^ Inchcape Testing Services Report

DATE PRINTED: 23-AUG-95 :REPORT: 095-40435.0 ( COMPLETE ) PROJECT: 4054 G10 PAGE 3A

SAMPLE ELEMENT AU Ag Cu Pb Zn Mo Ni Co Cd B i As Sb NUMBER UNITS PPB PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM PPM

95CL01 1 0. 2 17 3 48 3 16 2 0.3 ^ ^ ^ Duplicate

95CL06 1 ^.2 12 5 82 1 19 8 0.3 ^ ^ ^ Duplicate O ^.2 12 6 83 2 20 9 ^.2 ^ 6 *5

95CL10 O -:0.2 8 8 68 1 18 6 0. 2 ^ 5 ^ Duplicate

Bondar-Clegg & Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical ___ Bondar Clegg Lab -^r Inchcape Testing Services Report i DATE PRINTED: 23-AUG-95 REPORT: 095-40435.0 ( COMPLETE ) PROJECT: 4054 G10 PAGE 3B

SAMPLE ELEMENT Fe Mn Te Ba Cr V Sn W La At Mg Ca :NUMBER UNITS PCT PPM PPM PPM PPM PPM PPM PPM PPM PCT PCT PCT

95CL01 0.64 94 -dO 45 18 11 ^0 ^0 10 0.30 0.13 1.02 Duplicate

95CL06 1.54 558 ^0 43 40 19 ^0 ^0 18 0.76 0.42 0.78 Duplicate 1.61 571 ^0 44 42 20 ^0 ^0 19 0.80 0.45 0.81

95CL10 1.07 324 ^0 29 35 16 ^0 ^0 13 0.54 0.36 0.55 Duplicate

Bondar-Clegg & Company Lid. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 Geochemical Bondar Clegg Lab Inchcape Testing Services Report

DATE PRINTED: 23-AUG-95 REPORT: 095-40435.0 ( COMPLETE ) PROJECT: 4054 G10 PAGE 3C

SAMPLE ELEMENT Na K Sr Y Ga Li Nb Se Ta T i Zr LOI NUMBER UNITS PCT PCT PPM PPM PPM PPM PPM PPM PPM PCT PPM PCT

95CL01 0.01 0.03 17 0.01 3 58.94 Duplicate 58.77

95CL06 0.01 0.05 19 0.03 2 23.12 Duplicate 0.01 0.05 19 ^ 0.04 2

95CL10 0.01 0.04 14 fs 0.03 1 14.55 Duplicate 15.04

Bondar-Clegg Si Company Ltd. 5420 Canotek Road, Ottawa, Ontario, KIJ 9G2, Canada Tel: (613) 749-2220, Fax: (613) 749-7170 APPENDIX C : ROCK ASSAYS, REGIONAL AND GRID MAPPING, 1995 - 96 Swastika Laboratories A Division of TSL/Assayers Inc. Assaying - Consulting - Representation Established 1928

Geochemical Analysis Certificate 5W-2840-RG1 HI i 12 1995 Company: WMC INTERNATIONAL LTD J UL Date: JUL-06-95 Project: 4054 PO# 4054-G l O Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 5 Rock samples submitted JUL-04-95 by .

Sample Au Au Check Ag As Cu Mo Ni Pb Sb Zn Number PPB PPB PPM PPM PPM PPM PPM PPM PPM PPM CRT 02505 1354 1466 9.5 ^ 188 2 51 177 1 17 CR1 02506 495 446 0.6 ^ 113 1 69 15 1 39 CR102507 9 - 0.1 ^ 21 1 23 54 1 50 CR 1025 08 5 - 0.1 ^ 24 1 20 1 1 76 CR1 02509 5 - 0.1 <5 6 1 11 2 1 37

One assay ton portion used.

Certified by

P.O. Box 10, Swastika, Ontario POK1TO Telephone ( 705) 642-3244 F AX (705) 642-3300 Swastika Laboratories A Division of TSL/Assayers I nc. Assaying - Consulting - Representation Established 1928 Page l of 3 Geochemical Analysis Certificate 5W-3082-RG1 company WMC INTERNATIONAL LIMITED Date: AUG-04-95 Project: 4054-G10 Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 66 Rock samples submitted JUL-27-95 by .

Sample Au Au Check Ag As Cu MO Ni Pb Sb Zn URA Number PPB PPB PPM PPM PPM PPM PPM PPM PPM PPM S Minors

CR- 104601 Nil 0.1 ^ 42 8 73 1 ^ 79 Results CR- 104602 7 0.1 ^ 30 1 65 1 ^ 153 to CR- 104603 Nil 0.1 ^ 95 1 96 3 ^ 83 follow CR- 104604 15 7 0.1 ^ 66 1 95 68 ^ 112 CR- 104605 Nil 0.1 ^ 159 1 96 1 ^ 105

CR- 104606 Nil 0.1 ^ 115 1 119 1 ^ 99 CR- 104607 Nil 0.1 ^ 25 1 58 40 ^ 36 CR- 104608 Nil 0.1 *5 100 1 111 1 ^ 98 CR- 104609 Nil 0.1 *5 99 1 114 1 •:1 96 CR- 104610 Nil 0.1 ^ 105 1 68 1 ^ 85

CR- 104611 3 0.1 ^ 53 1 65 1 ^ 53 CR- 10461 2 5 0.1 ^ 124 1 101 1 ^ 89 CR- 10461 3 51 48 0.6 G 1 0 52 19 8 •O 9 CR-104614 2 0.1 ^ 55 1 14 1 ^ 55 CR- 10461 5 Control 2004 0.4 424 11 19 1 61 44 8

CR-104616 2 0.1 *5 107 1 84 1 ^ 102 CR- 10461 7 Nil 0.1 ^ 65 1 132 1 ^ 84 CR-104618 Nil 0.1 ^ 58 1 77 1 ^ 38 CR- 10461 9 Nil 0.1 ^ 67 1 104 1 ^ 66 CR- 104620 3 0.1 *5 73 2 85 3 *:1 65

CR- 104621 Nil 0.1 ^ 134 1 188 1 ^ 105 CR- 104622 Nil 0.1 •e5 124 1 119 1 ^ 175 CR- 104623 Nil 0.1 0 83 1 171 1 ^ 78 CR- 104624 3 0.1 G 79 2 107 1 •0 75 CR- 104625 Nil 5 0.3 ^ 8 2 22 8 ^ 10

CR- 104626 7 0.4 ^ 92 1 66 3 ^ 98 CR- 104627 67 2.8 *5 73 2 62 5 ^ 81 CR- 104628 3 0.2 ^ 8 4 8 1 -:1 13 CR- 104629 65 1.8 ^ 17 11 39 4 •d 30 CR- 104630 Control 1793 0.3 422 11 19 1 59 44 9 One assay ton portion used. y-ri. . /) J A \ L "J Certified by X/ W"W

company WMC INTERNATIONAL LIMITED Date: AUG-04-95 Project: 4054-G10 Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 66 Rock samples submitted JUL-27-95 by .

Sample Au Au Check Ag As Cu Mo Ni Pb Sb Zn WRA Number PPB PPB PPM PPM PPM PPM PPM PPM PPM PPM S Minors CR- 104631 165 6.9 •eS 14 15 25 84 •el 18 CR- 104632 17417 17966 350.5 ^ 374 4 24 1290 •el 8 CR- 104633 471 12.1 ^ 11 18 51 51 ^ 35 CR- 104634 10 0.3 ^ 8 2 17 2 •el 8 CR- 104635 117 1.2 ^ 7 35 11 9 *1 5 CR- 104636 10 0.8 ^ 1120 3 39 2 ^ 45 CR- 104637 57 2.3 •e5 13 2 18 1 •el 28 CR- 104638 101 3.5 •cS 17 2 15 4 ^ 39 CR- 104639 1565 1406 41.8 ^ 12 4 21 3 ^ 8 CR- 104640 7 0.3 ^ 28 2 16 1 *:1 65 CR-104641 5 0.4 •c5 23 2 16 3 •e! 46 CR- 104642 2 0.7 ^ 25 3 53 9 •el 35 CR- 104643 55 5.3 34 76 2 32 1060 •el 392 CR- 104644 2 1.1 ^ 52 2 26 10 •:1 10 CR- 104645 Control 1910 0.4 436 12 20 1 60 41 9 CR- 104646 33 2.2 ^ 801 3 43 17 *1 30 CR- 104647 12 0.7 ^ 79 1 86 10 ^ 86 CR- 104648 24 2.0 ^ 778 1 47 8 ^ 39 CR- 104649 2 Nil 0.2 ^ 32 4 37 2 •el 15 CR- 104650 3 0.3 ^ 316 1 27 2 •el 16 CR- 104651 2 0.3 ^ 177 2 35 6 •el 22 CR- 104652 17 4.9 *5 24 7 36 10 <1 13 CR- 104653 3 0.1 8 87 1 79 1 <1 56 CR- 104654 2 0.2 46 66 1 86 1 <1 113 CR- 104655 7 0.4 ^ 46 1 334 1 15 62 CR- 104656 14 0.1 ^ 20 2 42 1 *1 28 ' 1 CR- 10465 7 Nil 0.1 ^ 152 1 66 <1 80 CR- 104658 5 0.1 ^ 20 1 79 1 <1 59 CR- 104659 43 0.2 •eS 12 1 17 1 <1 27 CR- 104660 Control 1922 0.3 439 11 19 1 61 42 9 One assay ton portion used. /J . s) /f /} 1 VJ© l^"/V Certified by ^ LAs*u©n^f

P.O. Box 10, Swastika, Ontario POK 1TO Telephone (705) 642-3244 FAX (705) 642-3300 Swastika Laboratories A Division of TSL/Assayers Inc. Established 1928 Assaying - Consulting - Representation Page 3 of 3 Geochemical Analysis Certificate 5W-3082-RG1

Company: WMC INTERNATIONAL LIMITED Date: AUG-04-95 Project: 4054-G10 Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 66 Rock samples submitted JUL-27-95 by .

Sample Au Au Check Ag As Cu Mo Ni Pb Sb Zn WRA Number PPB PPB PPM PPM PPM PPM PPM PPM PPM PPM S, Minors GR -104661 Nil - 0.1 ^ 44 2 8 1 •d 105 CR- 104662 2 - 0.1 ^ 8 2 18 1 •^ 12 CR- 104663 Nil - 0.1 ^ 33 2 10 1 •el 82 CR- 104664 Nil - 0.1 ^ 9 1 22 1 •el 138 CR- 104665 Nil - 0.1 <5 24 1 26 1 •el 90 CR-104666 5 - 0 .1 ^ 52 1 52 1 <1 116

One assay ton portion used.

Certified by

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244 F AX (705) 642-3300 Swastika Laboratories A Division of TSL/Assayers Inc.

Established 1928 Assaying - Consulting . Representation Page l of 4 Geochemical Analysis Certificate 5W-3081-RG1 company WMC INTERNATIONAL LIMITED Date: AUG-04-95 Project: 4054-G10 Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 99 Rock samples submitted JUL-27-95 by .

Sample Au Au Check Ag As Cu Mo Mi Pb Sb Zn WRA Number PPB PPB PPM PPM PPM PPM PPM PPM PPM PPM S, minors CR- 104501 2 0.3 *5 38 1 54 4 ^ 100 Results CR- 104502 456 5.5 ^ 18 1 75 7 ^ 40 to CR- 1045 03 67 0.9 ^ 44 5 57 3 ei 36 follow CR- 104504 113 0.7 ^ 22 2 15 16 •O 11 CR- 1045 05 84 86 1.3 ^ 62 1 46 10 •O 84 CR- 104506 122 1.2 *5 6 1 15 2 ^ 6 CR- 104507 55 0.8 •e5 8 1 12 3 ^ 18 CR- 104508 14 2.2 ^ 41 156 54 156 •ci 81 CR- 104509 72 7.4 ^3 6 7 21 111 ^ 10 CR-104510 4457 4320 3.4 ^ 14 4 55 35 •O 25 CR-104511 497 0.7 -c5 44 3 61 5 •el 30 CR-104512 267 0.8 ^ 41 3 43 1 <1 30 CR-104513 823 857 1.6 ^ 17 4 79 2 <1 12 CR-104514 377 0.2 ^ 92 1 59 1 <1 38 CR-104515 Control 1927 0.3 438 10 19 1 60 42 9 CR-104516 48 3.6 ^ 74 8 112 35 <1 105 CR-104517 31 3.9 G 27 35 123 27 <1 107 CR-104518 315 17.0 ^ 33 7 68 57 <1 53 CR-104519 5 0.8 ^ 404 1 31 3 <1 6 CR-104520 39 0.4 ^ 32 1 51 2 "1 34 CR-104521 3703 3326 13.1 ^ 19 3 26 200 ^ 21 CR- 104522 3154 8.3 ^ 101 1 17 16 <1 3 CR- 104523 4183 4320 6.3 •c5 326 4 44 11 <1 9 CR- 104524 3017 5.4 ^ 291 3 31 20 <^ 4 CR- 104525 34 0.5 ^ 16 4 13 1 ^ 5 CR- 104526 24 0.4 ^ 10 60 18 2 *1 17 CR-104527 2 0.2 ^ 138 1 19 1 <1 74 CR-104528 5 0.1 *5 60 1 39 1 <1 119 CR- 104529 3 0.4 ^ 31 10 43 6 <1 51 CR- 104530 Control 1941 0.3 444 10 18 2 60 41 8 One assay ton portion used. A j l /) J f 7 C-p4^ s•"7^ Certified by ,x

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244 FAX (705) 642-3300 Swastika Laboratories A Division of TSL/Assayers Inc. Assaying - Consulting - Representation Established 1928 Page 2 of 4 Geochemical Analysis Certificate 5W-3081-RG1 company: WMC INTERNATIONAL LIMITED Date: AUG-04-95 Project: 4054-G10 Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 99 Rock samples submitted JUL-27-95 by .

Sample Au Au Check Ag As Cu Mo Ni Pb Sb Zn WRA Number PPB PPB PPM PPM PPM PPM PPM PPM PPM PPM S minors CR-104531 9 10.2 ^ 9 54 25 28 *:1 5 CR- 104532 Nil 0.1 ^ 66 1 32 1 ^ 64 CR- 104533 Nil 0.1 ^ 45 2 90 1 •O 115 CR- 104534 27 0.2 *5 7 7 18 1 ^ 48 CR- 104535 2 0.1 ^ 5 1 24 1 ^ 14 CR- 104536 103 1.8 ^ 15 8 26 1 ^ 6 CR- 104537 53 57 0.6 ^ 32 2 23 1 ^ 50 CR- 104538 67 2.6 ^ 32 1 23 12 ^ 53 CR- 104539 5 0.1 ^ 54 1 90 1 ^ 61 CR- 104540 2 0.1 ^ 52 1 119 1 •:1 94 CR- 104541 3 0.1 *5 83 1 93 1 ^ 77 CR- 104542 Nil 0.1 ^ 62 6 43 1 *:1 93 CR- 104543 Nil 0.1 ^ 7 4 25 2 ^ 8 CR- 104544 149 1.8 ^ 15 1 54 3 ^ 25 CR- 104545 Control 1835 0.3 439 10 20 1 60 41 9 CR- 104546 132 1.2 ^ 7 4 42 2 •:1 16 CR- 104547 9 0.1 ^ 5 1 67 1 ^ 82 CR- 104548 3 0.1 ^3 7 1 6 1 ^ 34 CR- 104549 7 0.1 *5 6 1 6 1 ^ 28 CR- 104550 36 0.2 ^ 45 1 33 5 ^ 42 CR- 104551 9 0.1 ^ 23 2 56 1 ^ 52 CR-104552 17 0.1 K5 24 1 69 1 ^ 86 CR-104553 9 0.1 ^ 38 1 67 1 ^ 120 CR- 104554 17 17 0.3 ^ 92 30 48 3 ^ 27 CR-104555 5 0.1 ^ 9 2 13 2 •:1 18 CR- 104556 7 0.2 ^ 3 8 9 10 <1 17 CR- 104557 9 0.1 ^ 43 2 28 1 *:1 70 CR- 104558 745 18.4 ^ 13 2 18 12 <1 13 CR- 104559 103 1.3 ^ 8 4 10 3 *c! 11 CR- 104 560 Control 1851 0.3 425 10 19 1 59 41 9 One assay ton portion used. d , /li 4 Certified by .X7 nlf-t/H

P.O. Box 10, Swastika, Ontario POK 1TO Telephone (705)642-3244 FAX (705)642-3300 Swastika Laboratories A Division of TSL/Assayers I nc. Assaying - Consulting - Representation Established 1928 Page 3 of 4 Geochemical Analysis Certificate 5W-3081-RG1 company WMC INTERNATIONAL LIMITED Date: AUG-04-95 Project: 4054-G10 Ann: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 99 Rock samples submitted JUL-27-95 by .

Sample Au Au Check Ag As Cu Mo Ni Pb Sb Zn URA Number PPB PPB PPM PPM PPM PPM PPM PPM PPM PPM S, m inors

CR- 104561 19 0.3 ^ 9 3 25 3 •0 31 CR- 104562 446 447 0.2 ^ 52 5 23 -ci 39 CR- 104563 14 0.2 ^ 552 6 17 •0 32 CR- 104564 58 0.9 ^ 11 2 12 ^ 56 CR- 104565 2 0.1 *5 61 1 35 tl 118

CR- 104566 240 1.7 ^ 18 9 29 ^ 35 CR- 104567 Nil 0.1 ^ 8 2 42 ^ 99 CR- 104568 Nil 0.1 ^ 29 1 19 1 ^ 91 CR- 104569 5 3.8 17 42 2 78 49 ^ 215 CR- 104570 Nil 0.1 ^ 4 1 9 1 *c1 108

CR- 104571 Nil 0.1 ^ 5 1 12 1 ^ 155 CR- 104572 9 0.1 ^ 3 1 9 1 ^ 17 CR- 104573 31 14.8 ^ 38 10 49 46 -:1 395 CR- 104574 26 0.9 ^ 126 15 22 1 ^ 4 CR- 104575 Control 1884 0.3 423 10 20 1 59 40 8

CR- 104576 21 0.5 ^ 85 2 60 4 •ci 167 CR- 104577 5 0.1 G 1 4 1 28 1 ^ 51 CR- 104578 Nil 0.1 ^ 6 3 27 1 *:1 100 CR- 104579 101 0.4 ^ 8 219 13 12 ^ 12 CR- 104580 651 633 2.0 ^ 52 12 22 27 •0 15

CR- 104581 Nil 0.1 •eS 48 3 69 1 *1 98 CR- 104582 72 1.7 ^ 64 11 18 3 15 15 CR- 104583 187 0.5 ^ 10 6 17 1 *:1 13 CR- 104584 82 0.3 ^ 47 6 14 1 •t1 42 CR- 104585 84 0.4 ^3 7 12 18 3 •0 13

CR- 104586 81 0.6 ^ 36 15 50 1 *1 72 CR- 104587 22 0.3 ^ 11 188 72 8 <1 58 CR- 104588 350 374 3.4 ^ 23 35 16 18 ^ 20 CR- 104589 14 0.4 ^ 12 3 17 4 <1 12 CR- 104590 Control 1889 0.3 429 10 19 1 58 43 9 One assay ton portion used. rf. X7// A r, Certified by X ^If

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705)642-3244 FAX (705)642-3300 Swastika Laboratories A Division of TSL/Assayers Inc. Assaying - Consulting - Representation Established 1928 Page 4 of 4 Geochemical Analysis Certificate 5W-3081-RG1 company WMC INTERNATIONAL LIMITED Date: AUG-04-95 Project: 4054-G10 Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 99 Rock samples submitted JUL-27-95 by .

Sample Au Au Check Ag As Cu Mo Ni Pb Sb Zn WRA Number PPB PPB PPM PPM PPM PPM PPM PPM PPM PPM S minors CR- 104591 43 0.5 ^ 13 4 11 1 ^ 10 CR- 104592 127 0.7 ^ 201 147 22 11 K1 40 CR- 104593 46 0.5 ^ 11 2 15 1 *:1 9 CR- 104594 2918 2777 75.8 ^ 9 12 22 230 ^ 12 CR- 104595 10 0.4 ^ 17 4 11 3 ^ 16 CR- 104596 626 5.1 ^ 8 373 22 21 <] 5 CR- 104597 15 1.4 ^ 494 5 48 6 ^ 53 CR- 104598 14 0.5 ^ 11 2 13 1 ^ 13 CR- 104599 10 0.2 G 46 4 59 1 ^ 92

One assay ton portion used.

Certified by

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244 F AX (705) 642-3300 Swastika Laboratories A Division of TSL/Assayers Inc. Assaying - Consulting - Representation Established 1928

Geochemical Analysis Certificate 6W-2074-RG1

Company WMC INTERNATIONAL LIMITED Date: JUN-14-96 Project: 4054 G-10 Attn: A.Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 13 Rock samples submitted JUN-12-96 by .

Sample Au Au Check Number PPB PPB CR1 04600 5 CR1 04667 7 CR104668 5 CR1 04669 3 7 CR104670 Nil CR1 04671 2 CR104672 17 17 CR104673 Nil CR104674 Nil CR104675 Pulp 1851 CR104676 9 CR104677 Nil CR104678 2 -

One assay ton portion used.

Certified by

P.O. Box 10, Swastika, Ontario POK 1TO Telephone (705) 642-3244 FAX (705) 642-3300 Swastika Laboratories A Division of TSL/Assayers Inc. Assaying - Consulting - Representation Established 1928 Page l of 2 Geochemical Analysis Certificate 6W-2235-RG1 company WMC INTERNATIONAL LTD Date: JUN-27-96 Project: 4054 GIO Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 33 Rock samples submitted JUN-24-96 by .

Sample Au Au Check Cu M) Number PPB PPB PJM PFM CR1 04679 12 43 1 CR1 04680 12 9 2 CR1 04681 9 7 2 CR1 04682 5 16 1 CRl 04683 9 43 4 CR1 04684 3 43 1 CRl 04685 3 32 1 CRl 04686 3 6 1 CRl 04687 7 19 1 CRl 04688 2 28 3 CRl 04689 50 6 1 CRl 04690 Pulp 1577 10 18 CR104691 12 33 2 CR104692 3 3 13 2 CR104693 15 25 2 CRl 04694 7 23 3 CRl 04695 14 32 1 CRl 04696 14 350 12 CRl 04697 7 5 42 1 CR104698 9 21 2 CRl 04699 2 60 1 CRl 04700 Nil 8 2 CR104701 Nil 27 1 CR104702 Nil 7 1 CR104703 134 6 1 CR104704 173 166 8 1 CR104705 2 5 2 CR104706 Nil 9 10 CR104707 2 24 1 CR104708 Nil 29 2 One assay ton portion used.

Certified by

Geochemical Analysis Certificate 6W-2235-RG1

Company: WMC INTERNATIONAL LTD Date: JUN-27-96 Project: 4054 GIO Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 33 Rock samples submitted JUN-24-96 by .

Sample Au Au Check Cu Mo Number PPB PPB PPM PPM CR104709 89 - 6 l CR104710 62 - 9 3 CR104711 12 15 6 2

One assay ton portion used.

Certified by

Company WMC INTERNATIONAL LIMITED Date: JUL-03-96 Project: 4054 GIO Attn: T.Goodwin/A. Sexton We hereby certify the following Geochemical Analysis of 32 Rock samples submitted JUN-27-96 by .

Sample Au Au Check Ag Cu M) Pb Zn Number PPB PPB PPM PPM PPM PPM PPM CR104712 12 - 0.1 6 1 29 127 CR104713 10 - 0.1 51 3 2 68 CR1 04714 156 149 0.1 4 1 1 51 CR104715 Pulp 1611 - 0.3 10 16 54 7 CR104716 7 - 0.1 17 1 1 132 CR104717 7 - 0.1 23 1 1 74 CR104718 10 - 0.1 23 2 1 157 CR104719 15 - 0.1 14 5 2 62 CR104720 14 - 0.1 17 4 5 40 CR104721 24 - 0.2 144 1 8 46 CR104722 26 - 0.1 110 1 1 51 CR104723 15 12 0.1 104 11 1 213 CR104724 14 - 0.1 25 2 173 82 CR104725 5 - 0.1 22 2 1 61 CR104726 3 - 0.1 19 3 1 58 CR104727 9 - 0.1 5 1 19 68 CR104728 9 - 0.1 9 2 1 53 CR1 04729 111 122 1.6 5 6 2 5 CR104730 Pulp 1611 - 0.4 9 17 52 7 CR1 04731 3 - 0.1 11 1 1 52 CR104732 10 - 0.2 31 5 88 51 CR1 04733 3 - 0.1 4 2 1 43 CR1 04734 5 - 0.1 21 4 1 56 CR104735 46 34 0.3 11 4 8 80 CR104736 12 - 0.2 9 7 53 136 CR104737 43 43 0.3 21 2 6 132 CR104738 14 - 0.3 12 7 3 29 CR104739 3 - 0.1 18 3 5 157 CR1 04740 3 - 0.1 12 2 1 51 CR1 04741 12 - 0.2 7 7 36 53 One assay ton portion used.

Certified by

Company: WMC INTERNATIONAL LIMITED Date: JUL-03-96 Project: 4054 GIO Attn: T.Goodwin/A. Sexton We hereby certify the following Geochemical Analysis of 32 Rock samples submitted JUN-27-96 by .

Sample Au Au Check Ag Cu M) Pb Zn Number PPB PPB PPM PPM PPM PPM PPM CR104742 5 - 0.1 10 4 1 74 CR1 04743 2 0.1 4 1 1 45

One assay ton portion used.

Certified by

Company: WMC INTERNATIONAL LTD Date: JUL-30-96 Project: 4054 G-10 Attn: A. Sexton/T. Goodwin We hereby certify the following Geochemical Analysis of 9 Rock samples submitted JUL-23-96 by .

Sample Au Au Check Cu M) Number PPB PPB PPM PPM CR1 04744 2 20 5 CR1 04746 5 36 1 CR1 04747 3 3 33 6 CR1 04801 3 41 4 CR104802 5 12 2 CR1 04803 7 24 2 CR1 04804 38 37 7 CRl 04805 1262 1131 14 15 CR104806 310 326 8 14

One assay ton portion used.

Certified by

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244 FAX (705) 642-3300 APPENDIX D : GEOPHYSICAL PROGRAM DATA AND LOGISTICS

REPORT, 1997 F::: 2 r::?

LOGISTICAL REPORT ON SPECTRAL IP/RESISTIVITY AND MAGNETOMETER SURVEYS CONDUCTED ON THE CLAW LAKE GRID CABOT TOWNTOWNSIP, ONTARIO

FOR WMC INTERNATIONAL LIMITED

JVXLtd. LOGISTICAL REPORT ON SPECTRAL IP/RESISTIVITY AND MAGNETOMETER SURVEY CONDUCTED ON CLAW LAKE GRID CABOT TOWNSHIP ONTARIO

For: WMC INTERNATIONAL LIMITED Americas Division - Exploration 22 Gurdwara Road Nepean, Ontario Tel.: (613) 727-3937 Fax: (613) 727-3970 Attention: Roman Tykajlo

By: JVX Ltd. 60 West Wilmot Street, Unit #22 Richmond Hill, Ontario L4B 1M6 Tel: (905)731-0972 Fax: (905)731-9312

Contact: Blaine Webster

JVX Ref: 9687 February 1997 J VX

TABLE OF CONTENTS

1. INTRODUCTION -i

2. SURVEY SPECIFICATIONS AND PRODUCTION SUMMARY 2

3. PERSONNEL 4

4. FIELD INSTRUMENTATION 5

4.1 IP TRANSMITTER 5

4.2 IP RECEIVER 6 4.2. l The Pole-dipole Array 6

5. DATA PROCESSING 7

5.1 IP AND RESISTIVITY 7

5.2 MAGNETICS g

6. SUMMARY s J VX

LIST OF FIGURES

Figure l : Location Map Figure 2: Grid/Claim Map

LIST OF TABLES

Table l: Specifications for the IP/Resistivity Survey Table 2: Spectral IP/Resistivity Production Summary Table 3: Survey Summary for IP/Resistivity Survey Table 4: Survey Summary for Magnetometer Survey Table 5: Field Production Summary

LIST OF APPENDICES

Appendix A: Instrument Specification Sheets and Pole-Dipole Array Geometry Appendix B: Plates J VX

LIST OF PLATES

Plate l: Chargeability, Resistivity Spectral M-IP and Time Constant Pseudosection LI 1800E, Scale 1:5000 Plate 2: Chargeability, Resistivity Spectral M-EP and Time Constant Pseudosection L12600E, Scale l :5000 Plate 3: Chargeability, Resistivity Spectral M-IP and Time Constant Pseudosection L13000E, Scale 1:5000 Plate 4: Chargeability, Resistivity Spectral M-EP and Time Constant Pseudosection L13400E, Scale 1:5000 Plate 5: Chargeability, Resistivity Spectral M-EP and Time Constant Pseudosection L13800E, Scale 1:5000 Plate 6: Chargeability, Resistivity Spectral M-EP and Time Constant Pseudosection L14200E, Scale 1:5000 Plate 7: Total Field Magnetic Profiles with Posted values on top of the Base Topographical Map, Scale 1:5000 J VX

1. INTRODUCTION

JVX Ltd. conducted time-domain spectral induced polarization (IP), resistivity, magnetometer surveys from January 17 through February 8, 1997 on behalf of WMC International Limited. The work was positioned on the Claw lake grid in Cabot Township, Ontario (NTS 41 P/ll). The survey location is shown in Figure l and the survey grid is shown in Figure 2. The purpose of this survey was to locate areas sulphide mineralization associated with gold bearing quartz veins in shears cutting the quartz feldspar porphyry Claw Lake stok.

The Claw Lake Grid covered the following claims: Cabot Twp: 1201705 1201713 1201706 1201717 1201711 1201718 1201712 1188886 SURVEY AREA

LOCATION MAP WMC INTERNATIONAL LIMITED CLAW LAKE PROJECT Cabot Twp., Ontario N.T.S. 41 P/ll

Scale : l : 1,725,000 Surveyed by JVX Ltd. Jan.-Feb., 1997 Figure l 201718

8 8 g

GRID l CLAIM MAP WMC INTERNATIONAL LIMITED CLAW LAKE PROJECT Cabot Twp., Ontario N.T.S. 41 P/ll O 200 400 600 Surveyed by JVX Ltd. Jan.-Feb., 1997 J VX

2. SURVEY SPECIFICATIONS and PRODUCTION SUMMARY

Transmitter Scintrex TSQ3/3.0 Kw Receiver ScintrexIPR-12 Array Type Pole-Dipole Transmit Cycle Time 2 sec Receive Cycle Time 2 sec Number of Potential Electrode Pairs 6 Electrode Spacing 50 metres Number of Lines Surveyed 6 Survey Coverage 16 ISOmetres

Table 1: Specifications for the IP/Resistivity Survey

Instrument Scintrex Envimag Magnotemeter Sensor Type Proton Precession Continues Mode Readings 2 sec sample interval Survey Coverage 35 370 meters

Table 2: Specifications for the Magnetometer Survey The production summaries are listed in the following tables:

Line From To Distance No. of Station Station (m) Readings 11800E 10000N 7000N 3000 63 12600E 10000N 7550N 2450 47 13000E 10000N 7300N 2700 53 13400E 10000N 7250N 2750 56 13800E 10000N 7000N 3000 60 14200E 10000N 7750N 2250 45 Total 16150 324

Table 3: Survey Summary for IP/Resistivity Survey

Line From To Distance Station Station (m) 11800E 7730N 10000N 2270 12000E 8500N 10000N 1500 12200E 9100N 10000N 900 12600E 7450N 10000N 2550 12800E 8050N 10000N 1950 13000E 7000N 10000N 3000 13200E 8800N 10000N 1200 13400E 7300N 10000N 2700 13600E 9050N 9998N 950 13800E 7000N 10000N 3000 14000E 9050N 10000N 950 14200E 7000N 10000N 3000 14400E 8800N 10000N 1200 14600E 7300N 10000N 2700 14800E 8550N 9200N 650 15000E 6950N 10000N 3050 10000N 11800E 15000E 3200 Total 34770

Table 4: Survey Summary for Magnetometer Survey J VX

3. PERSONNEL

Ivan Bizev (Geophysicist) Mr. Bizev operated EPR-12 receiver and was responsible for data quality and preliminary processing of EP data in the field.

Ted Lang (Geophysical Technician©) Mr. l^ang carried out magnetometer survey

Mike Fecteau (Technician) Mr. Fecteau operated EP transmitter

Four field assistants were also engaged by JVX : Jason Kwieciarz Larry Robidox Ryan Weeks WacleAxell

Dagmar Piska (Draftsperson): Ms. Piska carried out the manual and ACAD drafting on the figures/plates and assembled this report.

Aleksandra Savic (Geophysicist): Ms. Savic processed and plotted the data, prepared this report and it is responsible for data storage.

Andrew Hwang (Geophvsicisf): Mr. Hwang assisted in processing the data.

Slaine Webster (President. JVX Ltd.): Mr. Webster provided overall supervision of the survey.

The following table lists the field survey production in detail: J VX

January 17 1997 Mobilization January 18-21 Stand-by January 22-24 Production January 25-27 Stand-by January 28-February 5 Production February 6 Stand-by (equipment breakdown) February 7-8,1997 Demobilization

Table 5: Field Production Summary

4. FIELD INSTRUMENTATION and POLE-DIPOLE ARRAY

JVX supplied the geophysical instruments specified in Appendix A.

4.1 IP TRANSMITTER

The transmitter consists of a power source and an electronic control unit. Power is derived from a Motor-Generator. The Motor-Generator Set consists of a 10 H.P. Briggs and Stratton four stroke engine, coupled to a brushless permanent magnet alternator. The transmitter employs solid-state components both for power switching and control circuits. Output waveforms and frequencies are switch selectable-square wave continuous for frequency domain and square wave interrupted for time domain. The programmer is crystal controlled for high stability. The TSQ-3 features overload, underload and thermal protection for maximum safety. Stabilization circuitry ensures that the output current is automatically controlled to within lQ07o input voltage variations. Voltage, current and circuit resistance are presented on a LED digital display.

Basically, the Motor-Generator and Transmitter function as follows. The motor turns the generator (alternator) at twice the rated speed, which produces 800 Hz, three phase, 230 V AC. This energy is transformed upwards according to a front panel voltage setting in a large transformer housed in the TSQ-3. The resulting AC is then rectified in a rectifier bridge. Commutator switches then control the DC voltage output according to the waveform and frequency selected. J VX

4.2 IP RECEIVER

The Scintrex DPR-12 Time Domain Induced Polarization/Resistivity Receiver is primarily used for precious and base metal mineral deposit exploration. The IPR-12 accepts signals from up to eight potential dipoles simultaneously which are then recorded in solid-state memory along with automatically calculated parameters. It is compatible with transmitters that output square waves with equal on and off periods and polarity changes each half cycle. These periods can vary in duration from l to 32 seconds with the IPR-12 measuring the primary voltage (Vp), self potential (SP) and tune domain induced polarization (Mi) characteristics of the received waveform. The primary voltage, self potential and individual transient windows are continuously averaged and updated every cycle. Depending on the receive time, 10 to 14 predetermined windows are measured simultaneously for each dipole, hi addition to these, a user selectable window is also available.

The total receive time is selectable from l, 2, 4, 8, 16 and 32 seconds. K-factors, resistivity, statistical and Cole-Cole parameters are calculated and recorded in memory with the measured data and time. The Cole-Cole parameters, true chargeability (M) and time constant (^ for a fixed C or 0.25 can be used to distinguish between different chargeable sources based mainly on textural differences.

4.2.1 The Pole-dipole Array

The "pole-dipole" survey configuration was used. Typically, it is made up of 8 mobile electrodes, one current electrode Ci and seven potential electrodes (Pi to P? connected to the receiver by means of the "Snake"). The infinity current location C2 is maintained at a large distance from the grid. This distance is about 10 times the potential electrode spacing "a" times 6 (the maximum number of "n" used in the pole-dipole survey).

Each Ci line current location consisted of one or two stainless steel W current electrodes with salt water added. This procedure was necessary since the terrain was sometimes rocky and highly resistive ** i i i i r i CZ vU- a —•i*—a *U a .'4 a -VU- o —JU- q ——

ARRAY GEOMETRY

Apparent Resistivity:

s 2ir Vp/I

where Ai r apparent resitivity {ohm.m) n - dipole number (dimensionless) a = dipole spacing (m) Vp r primary voltage (mV) I - p rimary current (mA)

Pole-Dipole Array Array Geometry and Formula for Apparent Resistivity J VX

4.3 MAGNETOMETER

The Scinterex ENVI System was used. This magnetometer can be operated in the traditional stop end measure mode, or in the "walking" mod. The Magnetometer can sample at 0.5 second, l second and 2 second intervals. A two second sample interval was used. A base station was used to correct for both diurnal variations and reference field values.

5. DATA PROCESSING

After being transferred to a field computer at the end of each survey day, the data were examined, corrected, and organized by the instrument operator. The results were plotted on a D STAR NX-80 colour dot-matrix printer These plots were used to monitor progress and data quality, and to make an initial interpretation. Thus survey parameters and design were altered when necessary.

5.1 IP AND RESISTIVITY

The data were sent by courier to the head office of JVX in Richmond Hill, Ontario. They were processed and results were plotted on the following printers as was necessary: D HEWLETT PACKARD DESIGNJET 750C 36 inch colour plotter D HEWLETT PACKARD 5L Laser printer

The processing procedure is outlined below: 1) JVX software was used to perform spectral analysis of the time-domain data. This step was crucial to maximizing the information that can be obtained from IP data. This software analyses the shape of the IP decay curve, giving information about: G the grain size (indicated by the parameter tetu), G the uniformity of the grain size (indicated by c), and D the magnitude of the chargeable source (indicated by M-IP).

The GEOSOFT IP Package was used to generate colour and black and white pseudosections of chargeability and resistivity data. 2) The GEOSOFT Mapping Package was used to process plan and stacked maps. J VX

3) Plan maps of both chargeability and resistivity data were produced using JVX in-house software and the GEOSOFT Mapping Package. Additional drafting on these maps was done manually or through AUTOCAD.

Step l, was performed both in the field and in the head office. Steps 2, 3 and 4 were performed at the head office.

5.2 MAGNETICS

1. The profile of the magnetic data are generated in the head office using the GEOSOFT Line Processing packages. A sample interval of 12.5 meters was used for posting values with magnetic profiles.

At the head office, the AUTOCAD computer-aided drafting package is used to add Topographic Base Map provided by WMC.

6. SUMMARY

JVX Ltd. conducted time-domain spectral induced polarization (IP), resistivity, magnetometer surveys on behalf of WMC International Limited on the Claw lake grid in Cabot Township, NTS 41 P/ll. The IP/resistivity survey was done over six lines, totaling 16150 m, and the magnetometer survey was done over 17 lines, totaling 356370 m.

Data were collected, processed and presented in this report according to the Geophysical Service Contract dated as of December 20, 1996 by and between WMC International Limited and JVX Ltd. J VX

If there are questions with regard to the survey or its interpretation please call the undersigned.

Respectfully submitted,

JVX Ltd.

Aleksandra Savic, M.Sc. Geophysicist

Slaine Webster, B.Sc. President APPENDIX A l PR-12 Time Domain Induced Polarization/Resistivity Receiver Specifications

Inputs Synchronization Ancillary Rechargeable Batteries l to 8 dipoles are measured simultaneously. Self synchronization on the signal received An additional eight rechargeable Ni-Cad D at a keyboard selectable dipole. Limited to cells may be installed in the console along Input Impedance avoid mistriggering. with the Standard Rechargeable Batteries. 16 Megohms Used to power the Display Heater or as Filtering back up power. Supplied with a second iP Bucking RF filter, 10 Hz 6 pole low pass filter, sta charger. More than 6 hours service at ±10 volt range. Automatic linear correction tistical noise spike removal. -30'C. operating on a cycle by cycle basis. Internal Test Generator Use of Non-Rechargeable Batteries nput Voltage (Vp) Range 1200 mV of SP; 807 mV of Vp and 30.28 Can be powered by D size Alkaline batter 50 uvolt to 14 volt mV/VofM. ies, but rechargeable batteries are recom mended for longer life and lower cost over Chargeability (M) Range Analog Meter time. J to SOOmillivolt For monitoring input signals; switchable to " "au Range any dipole via keyboard. Operating Temperature Range -30'C to H-50'C l millisecond to 1000 seconds Keyboard 17 key keypad with direct one key access Storage Temperature Range Reading Resolution of Vp, SP and M to the most frequently used functions. -30'C to *50'C /p, 10 microvolt; SP, 1 millivolt; M, 0.01 nillivolt/volt Display Dimensions 16 lines by 42 characters, 128 x. 256 dots, Console: 355 x 270 x 165 mm Absolute Accuracy of Vp, SP and M Backlit Liquid Crystal Display. Displays Charger: 1 20 x 95 x 55mm Setter than 1 0X0 instrument status and data during and after reading. Alphanumeric and graphic dis Weights Common Mode Rejection plays. Console: 5 .8 kg At input more than 100db Standard or Ancillary Rechargeable Display Heater Batteries: 1 .3 kg 'p Integration Time Available for below -15'C operation. Charger: 1 .1 kg 1007o to 800Xo of the current on time. Memory Capacity Transmitters available P Transient Program Stores approximately 400 dipoles of infor IPC-9 200 W Total measuring time keyboard selectable mation when 8 dipoles are measured TSQ-2E 750 W at 1, 2, 4, 8, 16 or 32 seconds. Normally simultaneously. TSQ-3 3 kW 14 windows except that the first four are TSQ-4 10kW lot measured on the 1 second timing, the Real Time Clock irst three are not measured on the 2 sec Data is recorded with year, month, day, ond timing and the first is not measured on hour, minute and second. •he 4 second timing. (See diagram on iage 2.) An additional transient slice of Digital Data Output .ninimum 10 ms width, and 10ms steps, Formatted serial data output for printer and with delay of at least 40 ms is keyboard PC etc. Data output in 7 or 8 bit ASCII, .electable. one start, one stop bit, no parity format. Baud rate is keyboard selectable for stan ransmitter Timing dard rates between 300 baud and 51.6 In Canada Equal on and off times with polarity change kBaud. Selectable carriage return delay to sach half cycle. On/off times of 1, 2, 4, 8, accommodate slow peripherals. Hand 222 Snidercroft Rd. Tel.: (905) 669-2280 Concord, Ontario Fax: (905) 669-6403 6 or 32 seconds. Timing accuracy of shaking is done by X-on/X-off. ±100 ppm or better is required. Canada. L4K1B5 Telex: (905) 06-964570 Standard Rechargeable Batteries In the U.S.A. "xternal Circuit Test Eight rechargeable Ni-Cad D cells. Ul dipoles are measured individually in Supplied with a charger, suitable for 85 River Rock Drive Tel.: (716)298-1219 sequence, using a 10 Hz square wave. 110/230V, 50 to 60 Hz, 10W. More than Unit # 202 Fax: (716)298-1317 The range is O to 2 Mohm with O.lkohm 20 hours service at *25'C, more than 8 Buffalo, NY ssolution Circuit resistances are dis- hours at -30'C. USA 14207 •layed and recorded. Technical Transmitter Console

Description of Output Power 3000 VA maximum TSQ-3/3000W Time and Frequency Domain Output Voltages 300, 400, 500, 600, 750, 900, 1050, 1200, 1350 and 1500 volts, switch selectable IP and Resistivity Transmitter Output Current 10 amperes maximum

Output Current Stability Automatically controlled to within ±0.1 "/o for up to 500Xo external load variation or up to ±10"Xo input voltage variation

Digital Display Light emitting diodes permit display up to 1999 with variable decimal point; switch selectable to read input voltage, output current, external circuit resistance. Dual current range, switch selectable

Absolute Accuracy ± 3"Xo of full range

Current Reading Resolution 10 mA on coarse range (0-10A) 1 mA on fine range (0-2A)

Frequency Domain Waveform Square wave, continuous with approximately 60A od time at polarity change

Frequency Domain Frequencies Standard: 0.033, 0.1, 0.3, 1.0 and 3.0 Hz, switch selectable Optional: any number of frequencies in range O to 5 Hz.

Time Domain Cycle Timing t:t:t:t,on:orf:on:off;automatic

Time Domain Polarity Change each 2t; automatic

Time Domain Pulse Durations Standard: t - 1, 2, 4, 8, 16 or 32 seconds Optional: any other timings

Period Time Stability Crystal controlled to better than .01 07o. An optional high stability clock provides stabiliza tion to better than 1 ppm over -20/ + 50" C.

Efficiency .78

Operating Temperature Range -300 C to * 50" C

Overload Protection Automatic shut-off at 3300 VA

Underload Protection Automatic shut-off at current below 100 mA

Thermal Protection Automatic shut-off at internal temperature of H-850 C

Dimensions 350 mm x 530 mm x 320 mm

TSQ-3 transmitter with portable motor Weight 25.0 kg. generator unit Power Source

Type Motor flexibly coupled to alternator and installed on a frame with carrying handles.

Motor Briggs and Stratton, four stroke, 8 HP.

Alternator Permanent magnet type, 800 Hz. three phase 230 V AC.

Output Power 3500 VA maximum 222 Snidercroft Road Concord Ontario Canada Dimensions 520 mm x 715 mm x 560 mm L4K 1B5 Weight 72.5 kg. Telephone: (416) 669-2280 Telex: 06-964570 Total System FAX: (416) 669-5132 Shipping Weight Cable: Geoscint Toronto 150 kg includes transmitter console, motor generator, connecting cables and re-usable wooden crates Geophysical and Geochemical Instrumentation and Services T ENVI GEOPHYSICALSXSXEMi Total Field Operating Range l stop bit, no parity format. Selectable carriage return delay 20,000 to 100,000 nT (gammas) (0-999 ms) to accommodate slow peripherals. Handshaking is done by X-on/X-off. High speed Binary Dump Total Field Absolute Accuracy: ±1 nT Analog Output 0-999 mV full scale output voltage with keyboard selectable range of Sensitivity: l, 10, 100, 1000 or 10,000 full scale 0. l nT at 2 second sampling rate Power Supply Tuning Rechargeable 'Camcorder1 type, 2.3 Ah, Lead-acid battery Fully solid state. Manual or automatic keyboard selectable 12 Volts at 0.65 Amp for magnetometer, 1.2 Amp for gradiometer Cycling (Reading) Rates External 12 Volt input for base station operations 0.5, l or 2 second sensor, l/Zm (20 inch) staff extender and Optional external battery pouch for cold weather operations processor module Battery Charger Gradiometer Option 110 Volt-230 Volt, 50/60 Hz Includes a second sensor, Ifim (20 inch) staff extender and Operating Temperature Range processor module Standard: -40' to 60"C VLF Option Dimensions 8i Weight Includes a VLF sensor and harness assembly Console: 250mm x 152mm x 55mm ©WALKMAG© Mode 10" x 6" x 2.25" 0.5 seconds for walking surveys, variable rates for hilly terrain 2.45 kg (5.4 Ibs) with rechargeable battery T.F. sensor: 70mm x 175mm Digital Display 2.75"dx7" LCD 'Super Twist', 240 x 64 dots graphics, 8 line x 40 characters l kg (2.2 Ibs) (sensor) alphanumerics Gradiometer sensor and staff extender: 70mm x 675mm Display Heater 2.75"dx26.5" Thermostatically controlled, for cold weather operations 1.15 kg (2.5 Ibs) (sensor) Keyboard Input T.F. staff: 25mm x 2m 17 keys, dual function, membrane type I"dx76" .8 kg (1.75 Ibs) Notebook Function VLF sensor Head: 140mm x 130mm 32 characters, 5 user-defined MACRO'S for quick entry 5.5"dx5.1" Standard Memory .9kg (2 Ibs) Total Field Measurements: 28,000 readings VLF Electronics Gradiometer Measurements: 21,000 readings Module: 280mm x 190mm x 75mm Base Station Measurements: 151,000 readings 11" x 7.5" x 3" VLF Measurements: 4,500 readings for 3 frequencies 1.7kg (3.7 Ibs) Expanded Memory Total Field Measurements: 140,000 readings SCIMTREX Gradiometer Measurements: 109,000 readings Base Station Measurements: 750,000 readings Head Office 222 Snidercroft Road, Concord, Ontario, Canada L4K. 1B5 VLF Measurements: 24,000 readings for 3 frequencies Tel.: (905) 669-2280 * Fax: (905) 669-6403 - Telex: 06-964570 Real-Time Clock In the U.S.A. Records full date, hours, minutes and seconds with l second 525 Fort Worth Drive, Suite 216, Denton, Texas U.S.A. 76201 resolution, ± l second stability over 24 hours Tel.: (817) 591-7755 ' Fax: (817) 591-1968 In Australia Digital Data Output 1031 Wellington St., West Perth, West Australia 6005 RS-232C interface, 600 to 57,600 Baud, 7 or 8 data bits, l start, Tel.: (619) 321-6934 - Fax: (619) 481-1201 APPENDIX B Ministry of Transaction Number (office Northern Development Declaration of Assessment Work and Mines Performed on Mining Land Assessment Files Research Imaging Mining Act, Subsection 65(2) and 66(3), R.S.O. 1990

Personal informatioi id 66(3) of the Mining Act. Under section 8 of the Mining Act, the infor work and correspond with the mining land holder. Questions about tr [ Northern Development and Mines, 6th Floor, 933 Ramsey Lake F

41P11NW0020 2,17094 CABOT 900 Instructions: n, usese2.17094 form 0240. - Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary) Name Client Number

Address Telephonephone Number fat -3) 7 27-372*7 Fax Number 2. Name Client Number

Address Telephone Number

Fax Number

2. Type of work performed: Check ( ^ ) and report on only ONE of the following groups for this declaration. rr^Geotechnical: prospecting, surveys, r— i Physical: drilling, stripping, r— i Rehabilitation i^-J assays and work under section 18 (regs) ' —' trenching and associated assays ' —' Work Type Office Use

Commodity Total S Value of t P- Work Claimed Dates Work ~ ~2O tt YS^ ~ /a *jr Performed From 2/ . Q& , l* To '*'|t NTS Reference Global Positioning System Data (if available) Township/ Area Mining Division M or G-Plan Number Resident Geologi 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. Person or companies who prepared the technical report (Attach a list if necessary) Telephone Number 7 2.7 -393J Address Fax Num

Telephone Number

Address Fax Number RE C ElV E D Name Telephone Numt ir u FFB25 1997 Address Fax Number

MINING LANDS BftANnH

4. Certification by Recorded Holder or Agent l, , do hereby certify that l have personal knowledge of the facts set (Print Name) forth in this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the besj of my knowledge, the annexed report is true. li /' 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.

Mining Claim Number. Or if Number of Claim Value of work Value of work Value of work Bank. Value of work work was done on other eligible Units. For other performed on this applied to this assigned to other to be distributed mining land, show in this mining land, list claim or other claim. mining claims. at a future date. column the location number hectares. mining land. indicated on the claim map. 1 if 1 1 ' JL ^L 2 * *K eg TB 7827 16 ha S26, 825 N/A S24,000 32,825

eg 1234567 12 0 S24,000 0 0

eg 1234568 2 S 8, 892 S 4,000 0 R892

1 neBBBS' /b /862S~ O 0 /66Z^ 2 f (ffi* 3 6 /G ^330S~O 2 /TOYS' /X?7tr

3 {13*103*! ^ Z02O 0 &8D O 4 izo-l 7oH W 6/8 &&OO 0 O 5 /zo/ 70^ /l *?Z37 WOO ta3*t O 6 /2OI 7ofc /G 20723 6^00 MJZf O 7 tZOl7// /b Z013 6100 /G S* 0 8 /ZPT7/Z tt /0 1 7 H 640O 377*1 O 9 S2Pf~7f3 to* 9?2*S~ 640O JHzS' O 10 /2Ot7W /b 3V7O fot/OO 0 c 11 /2CH7/S- 16 acft &/CO O 0 12 fcOf 7/6 (2- ^631 qxoo O 0 13 t2.0/7/7 Z. JLOt^ SCO /Z& 3 14 /ZO/7/8 ^ Gft'7 6VCO ^77 0 15 /Z.017/7 /t* S02O e^oo o 0

Column Totals l, -fmmGTl*/^ ^O/X^-cEIS______, 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 toe work was done.

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

Some of the credits claimed in this declaration may be cut back. Please check ( ^ ) in the boxes below to show how you wish to prioritize the deletion of credits: \St 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; or D 3. Credits are to be cut back equally over all claims listed in this declare D 4. Credits are to be cut back as prioritized on the attached appendix or "" FEB 2 5 1997

.MINING LANDS BRANCH

Note: If you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary. For Office Use iJffRuftE' Received Stamp Date Notification Sent ,.;1HING.D1V1SIO / Total Value of Credit Approved 97 F to 8 Approved tor Recording by Mining Recorder (Signature)

0241 (02/96) 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.

Mining Claim Number. Or if Number of Claim Value of work Value of work Value of work Bank. Value of work work was done on other eligible Units. For other performed on this applied to this assigned to other to be distributed mining land, show in this mining land, list claim or other claim. mining claims. at a future date. column the location number hectares. mining land. indicated on the claim map. 0 1 F 22 i A eg TB 7827 16 ha S26, 825 N/A *924,dloJL 1 \) jg^2S^

eg 1234567 12 0 S24,000 0 0

eg 1234568 2 S 8, 892 S 4,000 0 S4.892

1 /zjonzo /t 23^7 fc*iOO 0 0 2 S20 1 721 tt O 6100 O O

3 f20 f 7ZZ- /b 30^ (MOO O O

4 /20(7Z*3 /(b 926 6160 0 0 5 /2Of72^ /(h O 6400 0 O 6 IZ.OI 7Z5~ /(0 /o^ 0 /O3 O

Column Totals *f33HOO efXf sao 4X^68 O^GxiO

l, , do hereby certify that the above work credits are eligible under (Print FuH Name) subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the claim where the workwasworkjoa done.

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

Some of the credits claimed in this declaration may be cut back. Please check ( ^ ) in the boxes below to show how you wish to prioritize the deletion of credits: D 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; or CH 3. Credits are to be cut back equally over all claims listed in this declaration; or D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe): ~HtCEIVED

1997

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

For Office Use Only Received Stamp Deemed Approved Date Date Notification Sent

Date Approved Total Value of Credit Approved

Approved for Recording by Mining Recorder (Signature)

0241 (02/96) , Ministry of Northern Development Statement of Costs Transaction NoVN" de transaction and Mines for Assessment Credit Ontario Ministere du l-itat des couts aux fins Developpement du Nord et des mines du credit devaluation Mining Act/Lol sur les mines 2.17094 Personal information collected on this form Is obtained under the authority Les renseignements personnels contenus dans la presente formula sont of the Mining Act. This information will be used to maintain a record and recueillis en vertu de la Lol sur les mines et serviront d tenir d jour un registre ongoing status of the mining claim(s). Questions about this collection should des concessions minieres. Adresser toute quesrton sur la collece de ces be directed to the Provincial Manager, Minings Lands, Ministry of Northern renseignements au chef provincial des terrains miniers, ministere du Development and Mines, 4th Floor, 159 Cedar Street, Sudbury, Ontario Developpement du Nord et des Mines, 159, rue Cedar, 4e Stage, Sudbury P3E 6A5, telephone (705) 670-7264. (Ontario) P3E 6A5, telephone (705) 670-7264.

1. Direct Costs/CoQts directs 2. Indirect Costs/CoOts indlrects

Amount Totals * * Note: When claiming Rehabilitation work Indirect costs are not Type Description Montan! Total global allowable as assessment work. Pour le remboursement des travaux de rehabilitation, les Wages Labour couts indirects ne sont pas admissibles en tant que travaux Salalres Main-d©oeuvre ttSD devaluation. Field Supervision fii--ff^--: - Amount Totals Supervision sur le terrain ^5O© Type Description Montant Total global Type Type Contractor©s Transportation and Consultant©s 45S4yM6- 3W& Transport 8OO Fees ,VteA Drolts de 130 I©entrepreneur M^Z^A /^51 2fO (3lr ffG^^j^^j et de I©expert- consell *3(Zfo Type Supplies Used Foumitures utilises* -^SJsD Food and Lodging Nourrlture et 1^111" v •- , '/K hebergement Mobilization and Type Demobilization Equipment Mobilisation et et -s-, Rental Gh*S*-JSo*T S200 demobilisation Location de Sub Total of Indirect Costs materiel /WO ^^sy Total partiel des coots Indlrects H?o Hfctfr# Amount Allowable (not greater than 20H of Direct Costs) limP" Montant admissible (n'excedant pas 20 H des coOts directs) Hft Sg*.1**?^.- Total Direct Costs Total Value of Assessment Credit Valeur totals du credit (Total of Direct and Allowable d'evaluation Total des couts directs ndlrect costs) (Total del eodtt dlractt life •t Indirect! idfnlttlblM

Note: The recorded holder will be required to verify expenditures claimed in Note : Le titulaire en registry sera tenu de verifier les depenses demandees dans this statement of costs within 30 days of a request for verification. If le present etat des couts dans les 30 jours suivant une demande a. cet verification is not made, the Minister may reject for assessment work effet. Si la verification n'est pas effectuee, le ministre peut rejeter tout all or part of the assessment work submitted. ou une partie des travaux devaluation presentes.

Rling Discounts Remises pour depot

1. Work filed within two years of completion is claimed at 10016 of 1. Les travaux deposes dans les deux ans suivant leur achevement sont the above Total Value of Assessment Credit. rembourses h 100 "to de la valeur totaie susmentionnee du credit d'evaluation.

2. Work filed three, four or five years after completion is claimed at 2. Les travaux deposes trois, quatre ou cinq ans apres leur achevement 5007o of the above Total Value of Assessment Credit. See sont rembours6s a 50 "/b de la valeur totaie du credit devaluation calculations below: susmentionne. Voir les calculs ci-dessous.

Total Value of Assessment Credit Total Assessment Claimed Valeur totaie du credit devaluation Evaluation totaie demandee x 0.50 x O, E Q F l V F-

Certification Verifying Statement of Costs Attestation de l'6tat des co( is FEB251997

l hereby certify: J'atteste par la presente : that the amounts shown are as accurate as possible and these costs que les montants indiques sont were incurred while conducting assessment work on the lands shown depenses ont 6t6 engagees pour effectuer les travaux devaluation on the accompanying Report of Work form. sur les terrains indiques dans la formule de rapport de travail ci-joint. that as cS500*g- authorized Et qu'fc titre de je suis autoris6 (Recorded Holder, Agent, Position in Company) (titulaire enregistre, representant, poste occupe dans la compagnie) to make this certification faire cette attestation.

0212 (04/91) Nota : Dans cette form mnes, le masculin est utilise au sens neutre. Ministry of Transaction Number (office use) Northern Development Statement of Costs Ontario and Mines for Assessment Credit

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, the 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 the Chief Mining Recorder, Minjstry of Northern Development and Mines, 6th Floor, 933 Ramsey Lake Road, Sudbury, Ontario, P3E 685. 1708 Units of Work Work Type Depending on the type of work, list the number Cost Per Unit Total Cost of hours/days worked, metres of drilling, kilo metres of grid line, number of samples, etc. of work CS

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

Transportation Costs /ODD

Food and Lodging Costs RECEIVE D FEB 25 1997

MINING LANDS BRAN Total Value oTTCsTessmenTWoTR"

Calculations of Filing Discounts: 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 SO'Vb 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 (please print full name) reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on the accompanying Declaration of Work form as ___ l am authorized (recorded holder, agent, or state company position with signing authority) to make this certification.

Data

0212(02/96) Ministry of Ministers du Northern Development Developpement du Nord and Mines et des Mines Ontario Geoscience Assessment Office May 7, 1997 933 Ramsey Lake Road 6th Floor Sudbury, Ontario Roy Spooner P3E 6B5 Mining Recorder 4 Government Road East Telephone: (705) 670-5853 Kirkland Lake, ON Fax: (705) 670-5863 P2N 1A2

Dear Sir or Madam: Submission Number: 2.17094 Status Subject: Transaction Number(s): W9780.00119 Approval After Notice

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.

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

NOTE: This correspondence may affect the status of your mining lands. Please contact the Mining Recorder to determine the available options and the status of your claims. If you have any questions regarding this correspondence, please contact Steve Beneteau by e-mail at [email protected] or by telephone at (705) 670-5855.

Yours sincerely,

ORIGINAL SIGNED BY Ron C. Gashinski Senior Manager, Mining Lands Section Mines and Minerals Division Correspondence ID: 10810 Copy for: Assessment Library Work Report Assessment Results

Submission Number: 2 .17094 Date Correspondence Sent: May 07, 1997 Assessor: Steve Beneteau

General Comment:

Transaction First Claim Number Number Township(s) l A rea(s) Status Approval Date W9780.00119 1188885 CONNAUGHT Approval After Notice May 06, 1997 Section: 12 Geological GEOL 14 Geophysical IP 14 Geophysical MAG Thank you for your letter clarifying your costs, dated May 02, 1997. As a result of this clarification, assessment credit has been approved as originally submitted.

Correspondence to: Recorded Holder(s) and/or Agent(s): Mining Recorder Alan Sexton Kirkland Lake, ON WMC INTERNATIONAL LIMITED NEPEAN, ONTARIO Resident Geologist Cobalt, ON

Assessment Files Library Sudbury, ON

Page: l

Correspondence ID: 10810 C c LEGEND Burrows Twp. HIGHWAY AND ROUTE No. OTHER ROADS TRAILS SURVEYED LINES: C TOWNSHIPS, BASE LINES, ETC. *J LOTS, MINING CLAIMS, PARCELS, ETC UNSURVEYED LINES: LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC. RAILWAY AND RIGHT OF WAY - II It: UTILITY LINES NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS 2 SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINE MARSH OR MUSKEG MINES V TRAVERSE MONUMENT

l______J DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT. SURFACE'* MINING RIGHTS— . SURFACE RIGHTS ONLY— —— .. '' , MINING RIGHTS ONLY ... _ ..... Q LEASE, SURFACE ft MINING.RIGHTS— — H " .SURFACE RIGHTS.ONLY...,..^,-.. H -l 12070 " .MINING RIGHTS ONlY.-—-^^-4--——-—— B LICENCE OF OCCUPATION .. _ -.— —— —— ...... — ... T ORDER-IN-COUNCIL ... _ . __ ...... —— ...... —— . OC RESERVATION ___ ...... — ...— .....—. © DC i CANCELLED _ —— ...... ——...,...... — .. ® C cL ci SAND ft GRAVEL ...... — ...... ® t THAPL INC CABIN __ . ____ ...... ____ ... .. __ ...... T o 'J*c O) l 1201712 .1 SCALE: 1 INCH - 40 CHAI . 1.70 9 4 s FEE T k O 1000 2OOO 4000 D O 20O 1000 2000 MtTRES 11 KM) (2 KM) FEB25 1997

MINING LANDS CH

TOWNSHIP DATE OF ISSUE CABOT o o CM TIMMINS MINING DIVISION LARDER LAKE LAND TITLES/ REGISTRY DIVISION THE l FORMATION THAT APPE/i S ON THIS MAP SUDBURY HAS JEEN COMPILED FROM VARIOUS SOURCES, AND CCURACY !S NOT GUAF kNTEED. THOSE Ministry of Ministry of WISHI G TO STAKE MIN Natural Northern Development ING C MMS SHOULD CON I20I722*X * SULT WITH THE MINING i Resources and Mines RECO D^R, MINISTRY OF NOTICE OF FORESTRY ACTIVITY Ontario NOR! 1ERN DEVELOP iND MINES, FOR AD- MENT THIS TOWNSHIP/ARE A FALLS WITHIN THE Numbtr DITIO AL INFORMATION Connaught Twp. Datf II ON T STATUS OF THE 5HININGTREE MANAGEMENT UNIT AND LAND: SHOWN HEREON. MAY BE SUBJECT TO FORESTRY ARCHIVED FEB. 21/95 G-960 b.k. OPERATIONS. THE MNR UNIT FORESTER FOR THIS ' 71 rtv o AREA CAN BE CONTACTED AT P.O. BOX 129. TELEPHONE 705-894-2000 i LOW AVENUE, GOGAMA, ONTARIO, POM IWO CD CD O TRIM LINE BRUNSWICK TWP

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210 Line 11800 E

84+00 N 87+00 N BB+OON 89+00 N 90+00 N 93+00 N 94+00 N 95+00 N 96+00 N 07+00 N 90+00 N 99+00 N . 75+00 N 7B+QO N 77+00 N 7B+OON 79+00 N 80+00 N Bl+OON 02+00 N B3+OON B5+OON B6+OON 91+00 N —————92+00 N lau ——^——i——t-71+00 N 72+00 N 73+00 N Lau ni s c; o in sec Pole—Dipole Array 0=1 16 m 0.10 0.10 0.10 0.10 ^.00 - 0.10 0.10 0.10 OaO-.UO 0.10 0.10 0.10 IB-** O- J--WO .uu — u.iu -usî 0.50U.MJ 0.50u.au -s 250 --.x-, IB -, , 0.20 . 3.9 11=1 i^Ji^^^^^ûarm^ //^"^-vwe? na 11=2 7.6 11, 0.10 0.50 0.10 0.10 0.10 B 0.10. 0.10 O.I ^-^\C^^^JS^^feSs4 ^ '•00 11=2 —-""^ ^-——-- A \^—'V/ j^~~^ i uL^L^T 1 M ""fTJtfO ' - jliL^ f 31. •CM', h l*// 82^0,10 ^VSr 0.20*^,0.10 11=3 0.90 0.10 0.10 0.20 B o.io a ' az )) ojo 0.10 -^/^^m* 7.8 SSg 3.9 vv 0.50H O-MBw/^jfoTfeâ ^T 0.10 ^ 2.5 ^ î^^^fc^ y v^ 11=3 n^4 3.1,(( feT ); 0.20 0,10 JL iilUl 0.10 f^ u 1.10 X 62 \ \ 0.60 Jt) 31 ^^ 3) 62 11=4 J±L ^Kmv, 'X^\\ V^^k^^^^ 11=5 0.10 0.10 rS- 3.1 .-C 7.8 -^ 0.10 :â* *mt^~^w 11=5 11=6 0.10 0.60 *" 0.10 *^ 7.8 -^- SI -"^ 0.10 ^ 0.20 (TlO — 0.10 11=6 s v a = 50.0 M plot point

E C E i M E D 74+00 N 75+00 N 78+00 N 77+00 N 78+00 N 79+00 N BO+OON Bl+OON B2+OON BB+OON B9+OQN 90+00 N 91+00 N 92+00 N 93+00 N 94+00 N 95+00 N 96+00 N 97+00 N 9(1+00 N 99+00 N M-IP 71+00 N 72+00 N 73+00 N ——i——*——*™ — i - , --t- -t ——— -f-— -t - -t ——— -r-—— t- M-IP mV/V mV/V

120 - 172 , 133 163 . 79 40 NJ,. - 263 66 61 56 -^106 143 168 , 110 110 116 133 121 100 116 101 v - 66 - i 1)7 106 110 v 78YU 87OY . 135l*! ^^ BOMl -.-, 112Di! 72K i 166I DD il 4846 , 46 163 (81 65 s 8B 94 , 74 . ' 127 , 76 80 -O" X. ra \ 128 134 yx 42 74 N. 186 ; 117 11=1 0=1 61 \\ ^ ( 7 S ^ \\ 36 46 64 l 46 X x 170 J l 40 "5 56 53 38 ] N 100 146' 124 121 121 102 121 124 133 124 106 106 105.N O71 V. V93 ^78 ^77 r^46 vV) 97 -~1" i V^- 107 60 74 93 70 56 \ 84 78 76 X Hi l 78 V. 186 \ 133 107 Ml\ 138 11 = 2 84 ~x 93. 161 U7/ . 74 .__ 60 X^ 133 133 ^ 169 \\\ S l Y^—'/^^ ^ ^_) \ \ r^ ••••" A f ~\~ / "X v -y ~~s f 3 LAMPS HI (ANCH 0=3 -J 66 f 41 —J 61 —— 66 —-. 64 8lJ 66 67 x 07 -—— JW 124 119 169 \ 97 . 121 146 143 p'(l^^^ fi\^K 76 , \ -J* ^ \^ M1 ^M 60r, \ m l HO 71 61 82 \ 77 M --~~ K B8 X, 138 ^ Oil 110 l 136 11 = 3 Logar Contours T 1.5, y, 3, 5, 7.5, 11 0=4 1 f lil ^v M 64 —— 44 , (fl7~^ 96 ( 40 ——- 48 — - 65 66 67 67 s 76 -~— 67 66 \^^9fl 90 JOO V 61 71 72 108 122 J 74 —~. 103^- 6U 60 ( 48 76 — !6 73 71 86 67 , 75 .101 ^71 06 S 76 77 ^ 73 ri-4 ^ \ \ \ \ ^/^^-TT-^N. s—^ \ rt 0=5 121 t 170 161 IB 7S —— , 74 V \ 172 ~///.-. . ^^ - .-^) ^ \ .-.^s^... 75 C^\ " \' 4" xX"11 67 \ 106 \ 86 f 07 'L-— Bl1 M ^- 5( \ B7 ^ -^0'^^- 49 60 80 80 74 66 80^^103' 75--' 80 75 " " 77 85 11=5 2.1 0=8 ^\46 - ' 172 ^i 76 s 77^ \\76 —— 97 ~^- 45/64 53 64 II — 40 —— 66 ' © 111 ^ x 46 46 88 '74 02 *. SB - DI ^~^ i? ^ 49 71 *7 ** ins - 70 -~- Bl us l mi 138la^X^ ^ ^ AH68 ———- B787 inn100 ^^^72 n AK66 l 06 85 80 78 74 ' 138 91 B7 HI 96 85 n-B

11' Anomaly

Definite Chargeability 71+00 N 72+00 N 73+00 N 74+00 N 75+00 N 78+00 N 77+00 N 78+00 N 78+00 N 80+00 N Bl+OON 82+00 N aa+ooN B4+OON 85+00 N Bfl+OON— t - ---*——i 95+00 N__ 96+00 N 9J+00 N _ 99+00 N Chargeability

mV/V mV/V Probable 3.6 - 2.6 1.1 , 3.4 v 2.4 s 2 2.1 1.4 1.6 1.5 1.4 x 2.4 \ 0.82 ^ 1.3 1.3 1.6 x 6.2 1.2 x 2.6 \ 3.4 -. 2.3 .1 ^^ 2.4 2.2 2.7 s 3 ^ 2.2 3.2 v 2.2 2.1 __ 2.3 2.0 3.3 2.4 - - 3.3 3.3 4.2 2.8 7 3.4 8.7 l US 2.1 3.6 2 2.1 2.1 --- 1.8 1.9 1.7 1.9 2.6 \ 1.6 — 1.6 0.3 7.1 7.8 6.8 7.3 7.6 .6 4.6 4.7 ^— 6.2 6.5 6.5 3.8 3.3 3.2 4.1 2.6 2.0 J 3.3 2.3 3.1 --^ 2.7 4.0 3.1 3.5 ( 6.7 l 4.3 3.7 11=2 Possible - , --J 3.3 3.8 \ 2.1 2.1 2.6 2.1 5.4 7.1 J 7.2 8.7 6.6 7.4 8.0 8.3 5.3 1.6 :^O 3.4 6.1 5.6 6.5 2.0 3.6 3.6 4.3 ( 78 ^ m 2.6 2.7 ~ -, 3.1 3.6 3.6 3.2 3.3 \ 2.4 11=3 6.4 7.3 6.6 6.3 5.9 \ 8.7 6.2 l 3.3 \\ 0.64 ^ 2.6 4.9 5.4 6.7 V 3.2 3.7 4.6 e?*** 3.1 ' 2.7 2.7 \ 3.4 3.9 3.8 3.2 3.3 4.6 3.6 3.8 ii^4 2.4 2.6 2.4 \ 3.6 4 4.2 x 2.7 2.9 2.7 2.9 2.4 2.4 2.6 2.8 3.1 2.4 \ 1.7 3.1 4.B B.8-. 6.5 6.6 6.3 5.8 l 4.1 6.1 3.6 3.6 3.4 4.5 3.2 2.B 3 3.7 4.3 4.3 3.6 3.8 3.g 4.5 4.4 4.2 4.4 4.3 11=5 1.8 2.7 2.7 4 4.1 4.6 v 2.7 2.7 2.4 2.G 2.6 2.6 2.7 2.6 ^ 3.3 2.1 2.0 4.3 - 6.1 6.9 7.4 6.9 4.9 5.8 " 3.6 ' 1 .6^ 0.43 2.2 - 3.6 4.5 6.4 3.0 3.6 4.6 x I.I ~ 3.2 4.4 3/3.3 4 4.6 5.2 ^ 4.6 4.7 0=6 Scale 1:5000 50 Q 50 _100 150 200 250_300 (meters)

71+00 N 72+00 N 73+00 N 74+00 N 75+00 N 76+00 N 77+00 N 78+00 N 79+00 N BO+OON Bl+OON B2+00 N 83+00 N 84+00 N - —— -f- * ~ - t- ——,~ - — -f- 05+00 N ae+ooN 87+00 N BB+OQN 89+00 N 90+00 N 91+00 N 92+00 N 94+00 N 95+00 N 9B+OON 97+00 N 9U+00 N 99+00 N Resistivity - - f ' Resistivity ohm m o h in in PLATE 1

11=1 112 '.- IIM s,s, 384~-~- 221 ^ . v ^y 821 .2168.^ 2678,, , 12UO 1062 607 , 1214 ssS60 y 1440 1403 1720^.1071^. s628s y 771 185 , .111. l,,,, j 496 1216 - M 489 892. 1428 1222 i 877 . 1060 ^ 677 543 134 x - 349 x 726 411 , 7IC - y 204 , 390 210, 197 0=2 2M (( IBM //BM 660^ 227227 ~ HI ^ S3fl SS 41 —— 60 WMC INTERNATIONAL LIMITED 1773 ^ 992^ 1249 ^"'1774 -^ 1M7 1293 /B90 1039 1017 ^ 7 317 l 637 \240 0=3 1379 973 1489 J 621 J 034 536 "\ 461 '636 INDUCED POLARIZATION SURVEY V. ,© 0=4 ; z rcy\\\ 1 \v\\y 646 269 166 166 x\ 810 f 212 — 1017 l 341 336 -0s- 124 131 __ 144 200 241 211 161 101 \\452 1685 \ 1108 1093 1018 "^^ 616 r 925 782 971 706 \ 1231 x 19691961 1421 1027 774 1065 l 1657 XX 341 1002 \ 4901 536 102! 1257 747 700 ' 850 685 BIB HIM 576 874 510 CLAW LAKE PROJECT \ X———^ - - l O \ l \ \ \ 0=5 ^283 ^161 187 A N 1348 3170 'l \ 701 146 164 ^— 201 283 274 230 206 \ 124 443 660 (16 734. X J|63 1266 i 1580 B76/ M 6111 - 1013 lOffi —— 075 888 813 CABOT TWP., NTS 41 P/ll ..N^ . .. \ \ x 431 l { 1332 X. 741) 7M 0=8 307 ' 210 * 27127i "l ' ' 3331aaai - 1181 ^- 108 ^ 800 183 166 ' 266 287 ' 318 ^295 286 224 603 622 ^ 333 ^704 768 ' 1349 1021 1017 1271 1327 l 2360 ^863 '1104 3472 1644 \ 403 ' diir, H4i i 1207 l UH ' 824 87Ii H;i2 K62 ' 200 x 670 ' 1621)^^062 Dale: DV

Season Software for the Earth Sciences JVX Ltd. ret. no. 9687 Line 12600 E lau 77+00 N t 7B+00 N _^ J79+JX) N__^^80+00 N^ __81+00 ^ ^_^ 824*) N ( 83+00 N | 84+00 N 85+00 N | 86+00 N 87+00 N ___88+00 N | 89+00 N 90+00 N 91+OON^ 92+00 N 93+00 N 94+00 N 95+00 N 98+00 N 98+00 N 99+00 N tau m sec m sec Pole-Dipole Array 0=1 0.10 0.50 — 0.10 0.10 0.10 0.10 0.10 0.10 ix 63 ^. 0.10 ^ 0.10 ^250 0.10 ss^ 16 ^ 7.8 â 0.10 0.10 j, 2.5 -^- 0.10 0.60 Ô^/^^S^ ^^^^^KJ?^^^^^ a na a 11 = 2 0.10 ^(([jaf)) J1-1-0 O-10 D-10 0-10 0-10 0-'a S QJP- ,(V ( 250U); 0.10 S OJO *|- 0.10 0.10 V\. 16 JJl 0.20 0.10 MO 1.00 — 0.30 Cd 31 ) 62 0=3 0.10 H O.M 0.10 8 0.10 0.10 0.10 0.10 0.10 ~'^~2.5 saif 2.5 *S 0.10 - 'l.f? - 0.10 0.10 — 0.10 0.10 0.10 0.10 7 , 2000 10 ^: 0.1 0.60 1.00 "i. 0.20 - JJKfirS^m^ ".ISb^S^^saiKVV. 0=4 0.10 H.0.10 (( 2000 )) 0.10 0.30 0.10 0.10 0.10 0.10 f( 250i)l, 0.10 0.10 0.10 0.10 0.10 0. .10 — 0.10 Si 1 .3 "B 0.10 0.20 0.10 1000 -K 0.10 ^ 0.10 0.10 0.80 3.D 0=5 0.10 0.10 0.10 0.10 fT, 2.5 ^ 0.10 s 0.10 0.10 0.10 0.10 0.10 0.30 0.10 S 0.60 - 0.10 B O.I 0.20 ~g 0.10 f/7 31 ) 0.50 ^5. 0.10 a = 50.0 M 0=8 2.5 ^ 0.10 0.10 — 0.10 x 62 —' 0.10 " 10 "' ' 500 0.10 0.10 — 16 ^ 0.50 0.10 — 0.80 ^ 7.1 REG SJtîE D

M-IP 77+00 N 78+00 N 79+00 N 80+00 N Bl+OON 82+00 N 63+00 N 84+00 N 85+00 N 88+00 N 87+00 N 88+00 N 89+00 N 90+00 N 91+00 N 92+00 N 93+00 N 94+00 N 95+00 N 98+00 N 97+00 N 98+00 N 99+00 N M-IP MINIM'"' i Ar\'i),': i !1 iANCH o mV/V mV/V CO CM 0=1 67 ——— 54 -102 121 114 101 87^ 107 v 78 x 111 110 104 117 107 v 73 , W ^^ IQ6 "' "9 IM -^.92 —110 V. 74 108 108———107 106 124 119 97 151 112 80 ^ 88 v\ 89 - 106 87 0=1 N l ry \ X 0=2 133 \\VV 58 V 103.__103.___106 106 116 V.l 8889 l( 1111 11 103 87 V\ 133 109 f 8S!f^N. ^N. 106 106 v 84 87 .^ 101 106 133 114 l 10 \101\\ 108 \ 86"R " ,."* ' ™ ^ ... —— 109 108 90 ^ 138 V 74 J) 77 3 71 . 80 ^ 106 0=2 0=3 Logarithmic , . o n ^ 7 c i n 187 1 "\\N ^^^-64 X. 8'1 —^sx^^"12 117i? ^^^-98' a. 106/90me; 7 on Mmy 1,^33 v92™ 90noy ) l 100,na |06106-^98 -^. ^98 ^-^98 102 118 121 110 N.v\ 77 102\ 106 103 \ 70 \] 76 —~~ 89 X. 108 'N 90 0=3 Contours l l L5' 2' 3' 5' 7'5' l 0'" 0=4 •~" Iff/,Ml ) ),10B 117 117 ^. 90 90 (.111 115 ^97,^108 118 111 103 111 100 106 114 111. 74 102/87 92 78 89 96 122 C ( 549 ' / 159 173 ^y 64 \ 84^—' 87 92 ^-^87 74 —,~ 74) < 78 0-4 0=5 5* (( 541' /^ 71 7^ 90 "0^\ 117 ^ 92 92 85 \ 114 102 105 118 116 ~ tt ^TVI 1 106 110 105 ( 90 \ 70 \ 02 89 -96 M y'M r"N . 0=5 0=8 M V ^- 87- --J 111 -^ 97-^* ' 1 11 " 90^ x 114 102- 105- 109- 121- ^117 "0107- '^ 92 ^ 101 105^-\V 111 .7——— loD 67 - 112 103 94 112 17 —— 67 k 41 — 80 84 N 68 0=8 2.17094 li1 Anomaly

Definite Chargeability 77+00 N 78+00 N 79+00 N 80+00 N Bl+OON 82+00 N 83+00 N 84+00 N 85+00 N 86+00 N 87+00 N 88+00 N 89+00 N 90+00 N 91+00 N 92+00 N 93+00 N 94+00 N 96+00 N 96+00 N 97+00 N 98+00 N 99+00 N Chargeability

mV/V mV/V Probable — — — - - J

11=1 0.32^ 1.8 5.8 1.8 6.7 5.4/ 4.5^4.0 4.1 6.2 5.5 4.9 3.2 3.9 4.8 7.1 6.5 4.9 ^^— 5.9 v 3.8 4.7 5.4 4.7 1.2 x 2.9 2.3 1.9 --, 0.33 5.8 5.2 1.3 7.5 7.2 4.5 4.5 3.7 3.8 3.8 3.7 4.7 3.8 3.5 0=1 Possible 1.9 3.4 4.4 . 1.3 1.5 4.7 5.2 J 4.7 5.5 \ 3.8 4.5 5.2 8.8 4.3 5.4 V^ 4.5 3.9 8.4 4.9 6.5 5.3 5.1 ~^- 4.8 3.9 3.6 3.8 0=2 L.-.-! 1.4 ^ 0.57 ' )'4.5 I 6J 5.7 "~ 4.8 4.7 4.1 6.3 5.4 x 4.8 0=3 B-8 B B 4.4 5.2 8.2 6.3 6.8 4.9 3.8 N. 5.9 5.1 5.8 5.5 \ 4.7 3.3 3.8 3.4 3.2 0=4 8 ~ '1 43 S.4 6.5 4.6 . 6.9 5.7 6.4 8.8 8.7 3.1 X 5.1 4.7 4.9 0.83 \ N 3.7 32 1.9 3.3 5.2 6.7 6.8 0=5 2-8 "^ 0.64 n 3.9 4.1 4.9 4.7- 5.7 5.1 4.0 1.1 5.7 6.4 1.4 7.2 3 3.3 x 6.8 ^ 4.7* 5.9 1.2 ^ x 3.6 4.S - 2.1 x 3.6 - 2.1 2.9 ^ 0.95 :rr" 1.7 Z.2 2.2 N 3.8 N 5.3 5.7 5.5 ' 4.3 x 2.3 0=6 Scale 1:5000 50 O 50 100 150 200 250 300 •d Ei (meters)

Resistivity 77+00 N 78+00 N 79+00 N 80+00 N Bl+OON 82+00 N 83+00 N 84+00 N 8&+00 N 86+00 N 87+00 N 88+00 N 89+00 N 90+00 N 91+00 N 92+00 N 93+00 N 94+00 N 95+00 N 98+00 N 97+00 N 98+00 N 99+00 N Resistivity PLATE 2 ohm ra ohm m

0=1 58 ——. 80 v \v 407. \ 1198 1547 2029 , 8BT —- 1188 1690 2106 1961 v B92 631 ^ 1033 -^ 254 \ 1333 1357 1208 1016 2019 , x 461 K 1098 x 421 2101 -^ 739^ 1447 — 101 1403 1264 . 2623 2079 1279 874 1014 1003 ——918 , 2201 ; 151 922 0=1 V \, WMC INTERNATIONAL LIMITED 0=2 1447 1197 S 1271 1289 1066 1297 l 3282 \ 2243 \ IHO 1870 1717 — 2109 1580 417 903 822 1455 2522 \67a 1447 1061 — 1117 x 1939 i 1 160 1296 1831 , \ 708 \ 1106 1387 ^ 1731 , 1360 \ 588 0=2 l ( \\ ^\ \N,.- 7 \\ INDUCED POLARIZATION SURVEY 0=3 19M 1319 1527 1077 1024 1765 2977 2285 ~I 1597 1998 1392 2179 2178 ; 1522 1262 301 946 ~ 716 1329 1429 -^ 881 ' 1153 1382 I486 1689 1569 N. 733 2001 1311 1145 0=3 0=4 " \ \ CLAW LAKE PROJECT 2131 \ 1499 1258 1037 1328 1860 3054 36il \ 1938 2004 468 2967 2012 1305 839 1179 817 909 1741 1743 1547 1533 ^ 1478 1116 0=4 CABOT TWP.. NTS 41 P/ll 0=5 t©&X^ 2400 \ 1237 1183 1284 1325 1753 l 4419 3998 \ 1815 1037 1246 1017 - 669 306 361 223 827 848 flM 838 \ 1117 2109 1534 1771 1759 128 1237 0=5 - Date: 97/02/10 0=8 ^ 1162 1379 1209 1420 3621 1541 186l ~ 328 ^** 1301 1944 1382 1322 1063 x 316 N l' 1723- ^ 1097 © 711 282 ' 408 483 x 281 N ' 954 DM" 1159 ^ 81 105 ^ 504 740 ' 1325 1920 1710 1818 -^ 2100 ^ 662 ——-970 0=8 JVX Ltd. ret. no. 9687 Ivosoft Software for the Earth Sciences Line 13000 E lau 74t(X)N '/lit(HI N 7(1 KX) N 771 (KIN '/HUMIN 711100 N MilHX) N 111+00 N 82+00 N KI+OON i t -t B4+OON 85+00 N 88+00 N^ ^ 87+00 N 88+00 N 09+00 N 90+00 N 91+OON 92+00 N 93+00 N 94+00 N _| ^ 95+00 N 96+00 N 98+00 N v fljHOO N lau m sec m sec Pole—Dipole Array 0=1 0.10 0.10 -^JUO O.IO O.IO 0.10 0.10 O.JO -^0.10 0.10. p0.10 0.10 *0.50 0.10 M, 0.1(1 0-1" O-'" 31 3-' - MO I'M 500 x// 0.10 ^ 11 P:!fi o.io, o.io 0=2 o.io 'Cc z~-^ o.30 o.io o.io — o.io o.io "^ 3.9 75* 0''0 "o."io aar ^ O.ID ^ D.IO o.io - o.io o.io ~-- 3.9 t o.io . o.io ^ o.so ss^r\fcA\\ . a_ _ ja^ _a_ M/r-x^., '—' ~~ ~" ' Hfei/r^lfeyl^l .^ 12 ^C 0.10 niY 31 —" /lT(" 31 iXf) ^^^ 2 fe;; Q.IQ 0.10 S 0.10 * H 0.10 0.10 \\. IB 0=2 0=3 0.50 ( 3.9^ 0.20 O.IO 7 l 62 )) 0.10 U^ 16 -^* 0.10 0.10 OJO 060 UllOjS^V 7.1 S^ 31 J j) 3.9^/31^ O.IO O.IO O.I 0=3 *———®-| . ~ . r J^^ f ^-C^SW/^XX " ~ •^JV^y \m(^^s-r ji\(( \ \Nrn 0=4 0.10 "- 0.10 tfl. 7.1 ^-- 31 -^ 0.20 f i 16 f 31 \3 0.20 O.IO 3.9 (( 62 \ O.IO 0.20 0.10 ', 1.3 yyy 31 —-v 12 Vi o.io ** i.oo XL' 11 . \ 3i -i^ 0.10 o.io 0=4 ''////^^ \(far mi-; ; ~- -—-^////(c^S^)j///^ frfftr--f^^^—^x\ \ l^"--vsSiBiv-'' jf^-^-îc^t ,,r.^Wi\\\X"^^vXNN ^ * li f——-^^jâL. x^^* 0=1) o.io o-5LA( L 62 ) /.J-50 Mi..-7,- 3i. .- — 3i ^.' 0.20 — o. 125 — 12 ^fl.10v^f l (126 Vm* 2V- 0.30 Li 11 l ( BJ \ \ 0.10 O.I 0=5 0^—^51 0=6 0.10 ' f 250 •^^•rii^VJliMii00.^x^ K12 M\Vô.60 r— K ^-* ojo M iff/,ff^. 3I \ \\Vjj \ \\^p*(2 X- 0 10 0=6 a ^ SO.O M plot point

RECEIVED 74+00 N 75+00 N -, 76+00 N __ 78+00 N 7'J+OO N 80+00 N 81+00 N t ^ ^^ M-IP 84+00 N B+OON. B7+OON (W+OON 89+00 N 90+00 N 91+00 N | 92+00 N 93+00 N 94+00 N 95+00 N 96+00 N 97+00 N ——96+00t —— N- —— t 99+00 N M-IP mV/V raV/V

91^-^130 v 70 i 117 117 120^ OH , 203 U3 , , 87 v 170....- 136 53 91 v 117 ; v 39 59 - , 170 - 120 131 116 >^ 77 90 , 1 11 107 101 124 122 102 111 101 110 131 I7B - 1Z\ s ,to N 48 19 .-^ 41 79 0=1 ^--^ \\ \\\////^ ^v f -——- 'y/^ i\ •to 0=2 48 41 \ 99 . 130 V^ 51 l ) 153 187 ) 134 105 116 \JM-X/ 110 tj)3 \ 111 109 117 121 102 117 105 100 "^ 69 60 100- 17 —— 85 ^ 80 V 53 — 56 l 97 J 71 52 15 63 0=2 f -t. . i MINING LANDS l J CM 0=3 80 v V 143 y 71 M 5.1 53 40 -x 62 \ 63 \x 39 ' 58 55 60\ 169 130 85 ~^. 122 101 104 119 117 117 ^ 93^ 117 108 106 121 104 110 100/63 81 -' 93 C 87 . 66 100 ——^ 11 61 65 , 10 19 0=3 ContoursLogarithmic ''^-^ i.'T *,\ © J. ' ,d' ..;—^7'l)' 1 0 '" \ / \\ ^ l ^-, 0=4 71 '/^ 172 / . 76 54 71 00 Oil (W ^ 40 ! 73 x\ 41 3H \-\x\\ 64 98 \ 40 \ 63 52 i(' ' 117 ' ' 119 r( 170^ \\( \ 84^^- ^ 97 ——"101—^,^109 121 IM 105^ 161 98 -v 108 J/~^ 85 X 119 104 117 )l 79l 13 (/ ^\ W^I 74' \71 "" 133 l 13 f 48 (T 70 ^Sm ) M 0=4 ~x \ \ V \ { s \X\ \ \\ \ \ \\ v-- i s/'- — \ S \ \ /' ^—I-// \ l I f- ( 0=5 203 f 07 7 52 (^107 59 72 69 40 x 59 ^ 43 44 \V\ . 122 \\ H } m M \\ IM 12* "X 153 )) 51 70 - 14 J 1 10 121 102 111 f BB ) 19 90 17 \ 121 110 f BO 71 ^ 74 - 87 | 77 10 73 51 y 49 f f 130 71 0=5 V.X l l w\ ^ 0=0 119 ' 70 66 ' 153 ^ ' 60 ' 1 12^ " 66 70 87 48 40 10 131 ^x 46 71 61 94 126 ''64 BO -' 203 x 105 119 110 101 15 ^ 109 ' 15 BO BO ' 143 ^ 70 40 - 52 ^M28 130 11=6 94 DefinitB Chargeability 74+00 N 75+00 N 77+00 N 7B+IH) N 79+00 N 80+00 N Bl+OON 82+00 N Kl+OON 84+ON JB+OO N _ Ofi+OON 87+00 N BB+OON 89+00 N 90+00 N 95+00 N 98+00 N 97+00 N 98+00 N 99+00 N Chargeability

rnV/V mV/V Probable 0=1 ^^ 1 .9 15^ 2.2 2.6 - 1.7 1.1 ^J.l ^.4 •/?"^ IJ ^----^2.7 2.7 2.7 \^0.10 - 1.9 2.1 2.6 s 3.1 3.1 \ 8.5 ~ 4.1 5.2 4.7 4.0 5.4 7.4 7.1 6.1 - 4.9 5.4 2.2 v v 1.2 1.6 __. 1.4 0=1 11=2 2.7 2.2 2.5 2.7 2.7 ^ 1.1 /2.2 1.9 2.2 34 Possible v1.6 ^1.6—~\ 1.6\ -—^—^ 1.3 ~-\ \1.9 \ 3.1 ^^ 2.9 \N 1.2 \ 1.1 4.7 1.1 5.2 5.B 3.3 5.2 6.6 6.fl 3.1 —— 2.9 ,—— 3 1.7 l 2.5 \ 9.S 3.1 v 2.1 \ N 1.3 1.1 11=3 3 2.3 3.1 V 2.1 C 3.3 \ 2.2 3.2 ~-\ 2.6 2.6 2.7 2.2 2.5 \ 0 04 0.113 \ 2.3 3.3 3^ \. 1-4 V 2 2.3 2.8 v 3.3 3.8 1.2 7.2 5.5 5.1 \ 3.3 6.4 5.4 6.8 7.1 8.3 6.B 2.2 3.1 3.2 J.4 x ^ 1.5 1.3 1.1 2.B ~— - 3.1 4.3 N2-* 11=4 3.1 2.5 \X 3.1^ J 2.6^O ^3 ---^2.7 V\ 3.3V--^ 3 2.7 2.7 2.Z (J 1 .8' ^ 0.95 S 1.5\ \\ 2.5 \\ 3.5 \3.3 \\\\x\ 1.4 J 2.1 2.5 2.5 \ 35 3.7 7.2 6.2 5.7 4.3 \2.2 3.1 3.2 S.6 1.7 1.4 11=5 3.2 2.3 2.9 2.5 \ 3.7 2.9 \ 3.5 3^2 x 2.7 C*.\ 2.1 1.4^ 1.4 1.5 \ 2.1 3.8 3.6 \ N 1.7 ^ 2.4 2.4 2.8 \ 3.4 4 3 *l4 2'3 3 a 3'4 s-7 2.1 Z.6 " 1.9 N 4.2 11=8 2.4 2.8 Scale 1:5000 50 0^60 100 150 200 250 300 (metera)

Resistivity 74+00 N 75+00 N 78+00 N 77+00 N 7B+IK) N 79+00 N BO+00 N 81+00 N B2+00 N 83+00 N 84+00 N 85+00 N 80+01) N 87+00 N BB+OON 89+00 N 90+00 N 91+OON 92+00 N 93+00 N 94+00 N 95+OON 96+00 N 90+00 N 99+00 N Resistivity PLATE 3 ohm m ohm m

0=1 154-^^674 s 429 ^ 854 , 2149 \-305 297 236 :- 97 61 12 -61 56 64 113 124 " 124 110 . 129 146 183, 521 -695 , 1936 v V40B , 1 154 N,^ 314 864 IB*497 IHU140 li II2BBCOO \ CIOO \ DM1KH .' il 2959lUDH xv MlDO l x IWJ4W */* S 282 46 -..... 53 37 47 49 12 ^ * 125 y 271 223 741 417 v 93 - 164 ...... 114 0=1 l l l V- V- -') \\\^——~^/ y f WMC INTERNATIONAL LIMITED 1715 ^N.B03 803 ^^4Slfl 423 [ l 2175 2321 ) J044 *~ 1^^201 ") 795 405 341 290 409 299 1392 1183 1331 75B '741 992 1717 1762 — 228B 2775 j \ tit -— 415 /— 632 132/266 , 371 419 \ 1M 361 INDUCED POLARIZATION SURVEY 1602 ^B91 -^ 862 V 2075 7X776 C t 2I4^\74I llV V 301 335 k 236 ~~' 221 O 139 / m S ^^^ ( 375 318" 312 361 433 ^-- 481 365 441 1217 ( IB73 9BB 1MB 1550 3005 1B2 833 166 ~-^ - ' - xXV. X\ \ __^-^^--^^ ^ ^ CLAW LAKE PROJECT 0=4 1575 ~. 1737 \ 744~^\ 1354 ^ 957S\; 299 \ \ 972 1102 '^- fS02 468 349 311 x 174 J 224 m 524 "^~^ 440^X657 ^^~ 459 ^ 622 j 322 494 397*^2913 2134^\-1617 ^2149 11S6 1146 Oil^~ l 2269 2214 191 257 191 253 210 117 ^-367 \ Ml 720 1079 \ CABOT TWP.. NTS 41 P/ll 0=5 2814 l 1400 \ 502 \ 1112 390 \\ ".1193 r 1122X^823 622^^^440 356 \ 218 30o' 110 591 765- 611 S 435 403 438 473 CV 2841 r' 3191 1591 \ 2542 607 1293 1161 1334 340 1311 1925 \\ \\ V Date: 97/02/10 0=6 2140 ' 986988 5M-564- v 1973 " 1484 N "" 479 - x 1649 I860 ^ 78ir ~-756 4B4 432 ^~ 296 374 479 ' 145^"^ 715 973 N 419 524 353 501 423 X N 3073 3221 N 1475 3001 ~^ 133 ^~ 1270 1496 910 191 ^672 639' 182 "- 447 ~^ 1717 2629 - 1089 x 359 428 291 262 201 392- 1114 JVX Ltd. re/, no. 96B7 'leasoft Software tor the Earth Sciences Line 13400 E

70+00 N BO+OON 81+00 N 82+00 N 83+00 N 84+00 N 86+00 N 88+00 N 87+00 N 88+00 N 89+00 N 00+00 N 91+OON - ^92+00 N 9:1+00 N 94+00 N _ 95+00 l 96+00 N 97+00 N Jfl+OOJV .^W+OO !L tau 74+00 N 75+00 N 78+00 N 77+00 N 78+00 N tau m set: m see Polo-Dipolr Array 0=1 0.10 0.10 0.10 o.20,.x^3.B^xx o.io 0.50 ^o.io ^ o.io "LH-J&. 0-10 ixx^- 04v D-ID 0'10 040 0'10 0'10 0'10 0'10 B'10 0'10 D'10 0'20 ,j|x'"\Vj 0.50 0.10 0.30 250 1.00 0.10 — 0.10 0.50 500 //A 0.10 wr- 7.8 -, -- 250 x^j 0.10 . ., ^ \ ... - - ?"^--~^. ... . i^/ ,. l\V..u.wJ'—j.1*^ n..^4^7^x; HID 0|o 040 mo o.|o ^0.10 0.10 0.10 O.IO 0.10 0.10 0.20 /f 31 \\' JV20 ".fw^.1 11=2 a ria a 0=2 1.00 j 0.10 0.10 0.10 ~ 0.10 23 0-10 0.20 .f. 16 16 V\ 0.50 0.10 Ss- 62 500 500 / 0.10 0.10 250 - 0.10 1^=3 0.10 0.10 0.10 0.10 0.10 ^ ^^ ij!L- O-'" '-l8 0.10 ^^5 ^Si 0.10 0.10 0.10 OJO OJO O.W J\( 31 31 16 j 0.10 0.10 11=11 m 0.10 :( 62 \ V 3.9 -ST 7.8 is 0.10 0.10 ((i~t7 )) 0.10 0.10 6.10 0.10 0.10 0.10" iSx 31 3.9 ( [ 125_ ^ 62 3^ 0.10 0.10 0.20 16 C& '0.10 0.10 11=4 !Z-^.l __ Jlf^L. 11=4 0.10 0.10 0.10 0.10 0.10 ''CS^jV, 0-111 JJM ** Wi."Jjl\\\\ \N*fc-^^ ^^^sr *®Mi , .10 *2 11 A 62 )1 7.8 ,/y 31 0.10 0.10 0.10 m 0.30 0.10 ^ 0.10 0.20 O.IO 0.10 0.10. A [62 82 0.10 62 0.60 ^ 0.30 S 0.10 fi(l 31 --—- 16 .V, 1.00 - 0.20 A 62 7.8 "Ci 31 /-/z'i&mt 0.10 O.IO 0.10 < 31 ST* 0.20 f 1000 \V 16 H- 0.10 0=5 0.20 0.10 0.10 0.10 m 0.10 " OJO 0.10 0.10—t-sE: vx ^- ^s ///j^^ l 7X x x M . 11=6 0.30 — 0.10 0.10 0.10 0.10 0.30 '' 7.8 "^x O.IO 0.10 0.20 : 1.00 0.50 31 ^** 0.10 ~~ 16*^ O.IO —^ 2 " "^^ 2 *^- 31 — 82 -"— 125 s NX 0.10 " 125 1.00 -7.8 ' M26 v-x-- 16 —7.8 0.10 0.10 0.50 *™ 0.10 x 11 "~-- 500 ^^ 11 11=0 a - 50.0 M V plot point RECEIVED

75+00 N 76+00 N 77+00 N 78+00 N 79+00 N 80+00 N 81+00 N 82+00 N 83+00 N 84+00 N 85+00 N 88+00 N 87+00N 88+00 N 89+00 N 90+00 N 91+OON 92+00 N 93+00 N 34+00 N 95+00 N 96+00 N 97+00 N 98+00 N 99+00 N M-IP 74+00 N ————l————l————l————c————l————,— M- IP 1 H n! 5 1997 1 mV/V inV/V 67 67 17 67 17 v. 100 100 x y 41 v\xl30_x x m ,/ li 46 \ - 103 8696 ^117 109 111 101 v ~ 57 64 74 -~, 48 v 98 163 -170 J5I V \ 44 ^ 90 155 n-l MINING LANDS CRANCH S \\-~^y V—— S \\\ \ \\\ V \ \^ o M 48 U v 47 VA ut J 86 87 -~-^10B106 106 103 \ 58 T! ( 130 A N 66 VV 118//38 ON 19" 117.^^71 \ 1 21 V 11=2 in 47 (9'IX.64^^- 80 85 78 \"l 111 iV. 90V ^-- 67 \XzJ60 87 i\ Xcr/i60 ^~ 70 V v44 11=3 Logarithmic i 5 p 3 5 7 5 10 CN ^^ \ i V \ i Contours L l l l{)' ^ li' a- '-1' 1 U- N^ 40 ^— 5) \\ 1I9\\ 62 72 80 .... 80 N\1H HI 107 v 70 \ 61 80 5N3^^. 117 11=4 'xxS s \ X x \ * r" x ' N \ ^^^*- " 129^ li 48 l fllTJ , 04 79 X"" /^W~~~~~~ 98 74 74 11=5 88 ^T"67 \^ 128 l/^78 ( Ô\\ 118 ^1 136/*- 1 1 u V1^-^/ \ Xl/ IST^ 82 - 90 ' 52 ^ ' 172 ' ' 47 ' I22\ ' 42 N 87 W 49 54 79 ^ 67 65 17 70 49 —— 58 73 ' 79 97 90 91 100 11 59 ^ 64 11=8 *f 2.17094II 1 Ali o in aly •* ^^S 9 •mn — Chargeability 74+00 N 75+00 N 76+00 N 77+00 N 78+00 N 79+00 N BO+OON 81+00 N 82+00 N Kl+OON 84+00 N B5+OON 86+00 N 87+00 N aa+ooN 89+00 N 90+00 N 91+OON 92+00 N oa+ooN 84+00 N 95+00 N 96+00 N 97+00 N 98+00 N 99+00 N Chargeability mV/V rnV/V X/'/X P robable g" 2.6 2.7 2.6 2.8 2.8 x. 3-9 2.8 2.1 2.8 0. . l 0.99 0-75 0.62 0.54 ,0,63 1.1. 1.3. ^ 1.7. 1.7. 1.8. 1.6 , 2.6 . 4.3 v 5.7 8.3 6 4 2.5 ''-. 1.9 2.9 2.1 2.7 2.4 2.5 y 3.7 2.8 5.4 3.9 ,, 3.0 7.3 s -0.080 ^ 5,7 -^ 0.00 I.I 11=1 S ^ — — -. \ V r~~ i 'A r ~\ \ "~-^ l \ / ^ —— 3.2 3.1 ——— 'S~~) 2.9 2.5 \ 3.6 \ 2.6 L J.Q \ lv 0.82 0.76 0.61 0.801.80 \ 1.3 f 1.8 1.8 S 2 1 2.E 2.2 2.9 4.6 \ 6.5 6.2 J 4.6 4.6 2.6 2.1 2.4 2.7 3 ' 1.7 \ 2.9 4.2 3.8 11=2 . . Possible ÎB f \v ^^ ^ \ X-——"^"~~ "—— \ f——"\ /^\ Xj \ 3.4 3.3 J 2.8 2 ——— 2.1 \ 3.3 3.1^ 2 2.8 1.2^ tt.n \ 1.2 v v -0.27 ~Xl8 \ I.I ———-l "X 0.61 0.81 0.080.98 1.6 1.9 S 2.1 2.5 2.8 2.6 2.8 4.6 4.2 6^—4.8 4.7 3 V I.B \ 2.7 2.11 i 3.2 . 2 3.2 5.2 5.8 11=11 m N\ N \\\ x\ \ xi. / \ i \ c —-\ \ x" A y \ \ •M 2.1 2.7 \ 1.4 \ 0.88 1.1 NN -0.25 X 1-8 X '-! 1.1 0.88 — 0.98 1.2 \|.8 2.1 2.4 2.8 __ 3 2.6 2.9-—-3.3 4 \ 5.3 5.2 4.9 3.1 ^-2 2.9'"^ 3.1 3.3 \ 2.1 \ 7.1 11=4 2.9 3.8 \ 2.2 2.7 X 1.6 ^ Ojl 1.2^ -O.ll ;V\ 2 ^ N 1.3 1.3 1.1 1.3 ûj 1.9 2.4 2.7 3 ~3^ 2.1 ^ 1.1 \ 3.4 4.2 \6.3 6.3 4.9 3.4. 2.2 \ 3.2 3.2 3 4 \ 2-6 \ 5-2 6.3 ' l,; 11=5 H l fi 2 B sa\ 24 2.1 \ ' I.I 12 12^ niunX 8i n~) li i H s i n in ? i f t. 90 2.8 3.| |.B u \ 3.1 4.3 \ 5.6 5.3 \2 3.2 2.3 \ 3.2 3.3 3.8 " 3 4.8 0.57 0.74 6.37 *^''2.7 8.8- " '3.5 11=1) Scale 1:5000 g 50 0 50 100 150 200 ;'f,() :U)0

Resistivity 74+00 N 75+00 N 76+00 N ohm m l-'rninljvilv ohm m PLATE 4 .24 .44 ..-lil - 161 472 780 824 878 x 2133 593 632 N 1091 - y 329 326 Vlffl 1783 v Ml) , 206 , 430 54 103 n-li, -1 620 6,0 ix m m m -\ \ \\\V s s- ---,\^ 390 VA II3B 1811 \ 2231 2232 I 'M 355 415 74(1^71 WMC INTERNATIONAL LIMITED 340 i* 464 8,3 504 345 ,78 W INDUCED POLARIZATION SURVEY 3,7 3,7 47667, " -" . il 1127 liM4"^"l7S 27* . 224 750 740 1360 983 1383 B77 n -1 CLAW LAKE PROJECT 3094 1891 \\411 443 309 403 306 2,6 - - 203 CABOT TWP., NTS 41 P/1 1 1394-383 1001- 2,63 17,,N 674 370 li f' 280 222 226 in ^210 "' 127 172 436 ^ 1318 2110 2488 11=0 Interpretation: Geoaoft Software for the Earth Sciences JVX Ltd. ref. no. 9687 Line 13800 E

N 98+00 N 99+00 N B8+00 N - ^ 87+00 N B9+OON 90+00 N 91+00 N 9^+00 N __ f 93+00 N 94+00 N i- -. t - ~ *- t - . t . 1 lau 78+00 N 79+00 N 80+00 N 01+00 N B2+00 N 83+00 N 84+00 N 85+00 N ,————^————,———— t——^— -i — — *-- 71+00 N 72+00 N 73+00 N 74+00 N J75+OON ^W+OpJ^ ~ 77+00- -i-— N-* — t —-i- ,- lau m Mm: Pole-Dipole Array m sec 0.20 0.50 — 0.10 ,, ^ 500 ^ 0.50 N ^ I. 82 - ^- 250 ..^ 250 11=1 \Hj^, 0,0 0.10 0.10 0,0 0,0 0.10 O.IO 0.10 0,0 0,0 0.10 0,0 0.10 0.10 0,0 0.10 0,0 _a na a 11=1 .^7.8 - 3.8 7, "•^lI 'b.io ~ D.IO o.io o.io o.io a.io o.io o.io 0.10 0,0 0.10 0.10 0,0 0,0 0,0 O.IO O.IO 0.10 0.10 0=2 V\A\ 11=3 0,0 0.10 0.10 0.10 0.10 0.10 0,0 O.IO 0,0 0.10 0.10 0.10 *- 0,0 0.20 D.IO 0,1) 0.10 - 0=3 11=4 0,0 0.10 0,0 0.10 0,0 0.10 0.10 0.10 o.io o.io o.io 0.10 o.io — o.io 0,0 (^fly^~ 0.10 o!io ^ 0,0 ^. JI^L^rS- 0-10 -^ fl- 10" 11=4 -1-* 1*^^J-S 4X x Jl iiii "•IM ^^-L *" -——' ^V,kV\ V. 11=5 •*^MsP'''mx SS^Ufc *fc^0* 010 010 010 0.10 —. 0.10 0.10 0.10 0.10 0.10 0.10 0.10 0.10 T^ ?.s All. MI o-M ~ w* "JLsi -i*5*^Sr*a^-. a = 50.0 M 11=5 0.20 3 0,0 ^ 0.80 ^/^wJl^^w^leS ^rr-r^SSSfe——WJf ^^Vir- ^g^s^i. W 11=0 ^ 0,0 ^ 1.00 — 0.10 0.30 7.8 O.IO"^ 7.8 ^ 0,0 0.10 0,0 0,0 O.IO O.IO 0.20 0,0 0,0 '2 11=6

97+00 N Ufl+Ofl N 99+00 N B4+00 N 85+00 86+00 92+00 N M-IP 75+00 N 77+00 N ^TB+MN 79+00 N 83+OON M-IP 71+00 N_ 72+00 N 73+00 N 74+00 N raV/V MINING LANJDSJ352NCH. mV/V 67 67 67 87 B7 87 -w 138 107 -^119———126 ^-28 ^. Tl - 62 HI 74 75 68 y 80^—— 87 74 , IWI - 80 106 ^81 M 76^111 122 v\ 38 \xvl43 103^-.M M ——^88 66 tt J 88 78 ' 60 l 107 ^ 88 8fl 88 90 l 124 91 11=2 67 87 67 67 67 87 67 -^. 79 ^\\ 56 ^k (VV. 133 J 85 -—^ 80 67 67 65 87 87 87 ^~\ \ l J J 7, ^62 ^ ^ 5, Q /"^//^~v 108 N. 80 __ 77 102 vv 80 83 87 s^ 109 133 11=3 Logarithmic . f 67 67 67 67 87 65 C 48 I f 1 38 \ ContoursPrxT^fniivu ' * ' ' W 71 64 86 87 —— 77 ' \^j S,™ 11=4 o 67 67 87 87 67 66 r^\. 108 108 1081 74 -^ M V 108 ^* 91 80 \ I04 1 14 CO f Wn 78 81 11=0 CN 66 /"n~' 67 67 67 , * lUj ' 00 87" ~^~7l W 98 87 88 \ 110 ^ 87 88 \^ 103 B6\6B 44183/56 " ^—^ 38"^ 67 67 67 67 67 67 64 A 79 85 56^ 128*^87—- 86 92 82 90 ^^03^ 85 88 81 118 103 99 H' Auoiualy

IS Definite 94+00 N 95+00 N 96+00 N 97+00 N 9H+00 N 99+00 N 79+00 N ao+oo N Bi+oo N 82+00 N B3+00 N 84+00 N^ ^__ 85+OOJj ^ ^ HV+OON 88+00 N 89+00 N +00 91+00 N 92+00 N 93+00 N Chargoahilily 71+00 N 72+00 N 73+00 N 74+00 N 7B+OON Chargeability mV/v Probable mV/V 1.9 2.4. 4.3 4, --2.2 , 3.8 4, 3.8 -5.3 2.8 . -3 3.8 4.3 ^ 6.7 4.0 .^ 5.3 0=1 2 2.4 2.7 . It - 2.6 1.8 1.6 1.5 ^ 1.4 1.3 0.80 0.71 l ' 0.55 0.71 0.75 0.68 0.68 0.86 0.72 0.76 0.76 0.86 1.5 r 11=1 4.3 v 1.8 x 2-6 1.4 2.1 3.2 4.6 4.8 .8 I.B -2.2 2.4 Possible 1.2 N 0.86 -^ 1.2 0.86 "- 0.88 ' 0.92 0.85 0.75 " 0.80 x 0.64 0.8* 0.77 0.82 0.94. 1.3 \ I.B s 2.1 2.1 2.1 2.7 f 3.B 4.8 , 4.9 3.7 4.4 x 5.1 - ~ 4 4 4.H 5.5 7.8 -N 5.4 1.7 1.8 y 3.1 4.5 4.2 4.8 2.7 V 1.8 \ 2.1 2.6 2.1 2.6 2.2 2.4 2.7 2 1.7 1.8 4.8 5.6 DU 8. 0.66 fl-l 0.88 0.83 0.84 0.77 0.78 0.90 0.92 2.2 2.3 2.8 3.2 4 2.3 2.4 l 4.2 3.7 3.8 4.8 Z.8 \ 1.8 2.2 2 2.2 ^---2 2.3 2.3 2.7 2 I.I 15 1.4 1.3 1^ 0.89 0.80 0.78 0.84 0.93 ^ 0.09 1.2 2.3 2.7 2.8 \ 3.3 4.4 4, 4.1 4.H H.b 5.4 6.5 B.3 7.1 11=4 3.6 35 4.8 2.8 l.9 2.2 21 2.3 2.3 2.8 I.I 1.9 1.8 v^- 1.6 ' 1 .7 1.8 x^ 1.3 0.87 0.86 0.87 0.92 5 6.7 6.3 y 4 4.7 , -J 5.3 6.8 6.1 11=5 3.1 3.6 4.8 2.1 2.3 2.6 2.8 1.7 1.8 1.8 1.7 V. 1.4 . 1.6 1.2 1.4 3.4 4.2 6, 5.5 6.2 4.2 4.5 ' 8.3 5.4 7.8 B.B 11=6 Scale 1:5000 1.9 ' 2.3 1.8 I.* ' 2.1 2, 2.3 1.8 1.6 I.B I.B 1.6 1.8 1.6 l, 1.5 0.81 0.*5 ' 0.4* 0.57 N 0.88 1.2 1.3 1.1 N 1.9 2.8 ' 3.8 4.7 3.1 6.1 3.6 ^ 2.6 ^ 5.3 3.B 50 O___50 1(10 150 L'OO 250 HOO

(meterH)

fl'J+00 N J7+OON 78+00 N 79+00 N 80+00 N 81+00 N ( ^ 82+00 83+OOJI ^ 84+00 N 85+00 N 86+00 N 67+00 N 88+00 N 89+00 N 90+00 N 91+00 N 92+00 N 911+00 N 94+00 N 95+00 N 98+00 N 97KX)N 9B+00 N Resistivity Resistivity 71+00 N 72+00 N 73+00 N 74+00 N 75+OON 78+00 N - -i- ——*——^ — --* - ( t - ohm m PLATE 5 ohm m ^- \1A ^ 264 271 276 366 \I45 118 ...120 102—^71 64 - 95 136 153 , 260 268 x 623 x 1122 706 v 431. - 1323 1258 ^, 405 ^x. 2052 -^. 1088 842 - 584 275 359 219•~ 223 11=1 285 , \ WMC INTERNATIONAL LIMITED 2347 \ 880" 933___ 8B3J .510 537 "490 . 232 262 314 ~317 421 426 \- 224 J 761 ~~- 148 -— 155 235 278 438 287 689 ( 2624 x 1106 INDUCED POLAKIZATION SURVEY 206 ^144 124 107 111 114 "v-* 86 83 115 m / 180 248 ' :t'9 364 47B 383 ) 1181 K 329* ^ 1377 ^ 844 \\ 3429 1665 ^ 1207 1233 I3UI \. 832 /97I 11 = 3 44* —— 606 k 1092 261 ,, J 380 \880 2*2 392 4*0 664 \ 272, 189 , ^—^ / i r - J \\\\ x\ V"-^x\ V\\ 368 ^\' 21165 1426 IBM IN4:i "(187 CLAW LAKE PROJECT 326v 425 ll 588 862 \ \"316 240 223 264284 ^^"- 1*61*8 m "... ~ 146 147 "'— 156166 -^- ^\ 121 III 144 ""••--133 ^161 157 139 "166 -""188 ' 238 i1108 385 381 \ 675 612 \J vI486 x \3558 "^ 2046 \\\ 882 x\ 3573 M 4 CA1JOT TWP., NTS 41 P/ll 343 283 241 l M8 600 678 l 788 x 382 302 268 f 3U 250 230 IM 199 20B I6B 151 198 1711 204 I'lfi 188 !!I7 3 M' \ IMO 'W,' :\W\ Hill H.'l ' II.IHI . 4811 I'lllll V IIIW ,:u,.'ll (Hl\\ KM II r. ,V\. .... "- .... \ ...... \i ... ^...) ...... ^.' ...... —...... v ..... M-M \ lliri ^^ Ni -XA x -A \ A x v\\A Da Ir: 97/1)2/10 306 268 38* ' 664 782 852 472 363 304 M 318 288 248 261 262 205 200 256 228 287 277 239 266 253 L'85 308 377 635 v 1073 6115 ' L'0116 4641 1934 700 1'IXiB 1362 ' 446 2881 WU II II JVX Ltd. ref. no. 9687 eosoft Software for the Earth Sciences Line 14200 E

09+00 N 94+00 N 95+00 N 96+00 N 97+00i N. i ' 98+00i N' Lau 79+00 N BO+OON 81+00 N 84+WN 85+OON 88+00 N lau 111 H(!i: le-Dipo]e Array in sec 250 '—- 125 ,vx 1000 ; , 0.10 11=1 1997 . N 0,0 -. 0.30 ^ 16 ^Vx 250 '^-r 125 xx 10 a _ n n^ _ _ a_| ^l 0,0 0.10 0.10 0,0 0,0 v IJIO X 0.10 0,0 0,0 sg^x. 0.50 050-0,0 0.10 0,0 0.10, J \^r-^\wS^îi28fefe: t ^Z 0,0 0,0 0.20 0,0 0.20 0.10 0.10 OÔjj^JO o.io ^ M S)* o-io o-10 0-1(1 M "•lo aig " m "-*u ^tu^^r-- "r^-i^^^:: INING LAND? BRANCH (D- ••JfS 0.504^^")^!S WO a. 0.10^ 0,0 0.10 0,0 0,0 0,0 0.10 0.10 O.fo " ^.^^^^ 0=3 0.10 - J'OO -iÔ.20 0,0 0.10 0.10 0.10^ \60 0,0 0,0 0.10 0.10 "* 0,0 0.11 ^^S^y^^^^^^^^- o'10 (uo D'10 o'"1 WD o'10 ^^Q^î(S 0=4 0.10 l ' - 62 f^s, 0.20 *K 16 H = 50.0 M 1.00 ,' 0,0 0.10 0.10 0,0 0,0 ^1.00 i - lOYlO*^*w^j^^©jWs2--*-9 C^^-"11"-' 0'10 "•10 0'10 tM 0'10 0'10 0'10 "* alflw^ , \ 0=5 \ l fmrÔ K^ fl t/l J .n ^*Vo ^ napû"^ 7II ^^^^J"^ 0.10 0.10 0.10 0.10 0.10 0.10 0,0 0.30 0,0 — .10 0.10 0,0 0.10 0.50 0,0 - LOO 0.60 V 0=6 plot point

94+OON 95+00 N 96+00 N 97tOfi N 98+00 N 99tOON M-IP 88+00 N 87+00 N aa+ooN 89+00 N 90+00 N 91+00 N 83+00 N 84+00 N ————85+00 t-———*- N M-IP 79+00 N BOtUON 81+00 N 82+00 N mV/V mV/V 2.17C94 M 48 ^ 66 63 B7 IOB ^76 81 IOH 163 11 = 1 121 182 143 -^...203 .- 133 v 83 62 v 91 67 54 60 s. 3" 129 v 172 .__ 159 172 75 52 73 W 55 IDfl 11=2 8?——~f 62 " 67 87 ^ 67 67 ' 66 62 "', 46 \" 99 J .44 47 V M "iJ 'joa 169 123 119 119 O69 \ ^"' ~\ ^-J rx Logarithmic , - 2 ., 5 ? r , 0 ^ V "X l N \ N ,7D,y 91 ) 68 66^ 52 75 48 j 73 ---- 73 82" \ ^ Illfl"^ 86 v 66 J l 120 11=3 r, i It I . t J, (i, O, iJ. f . tv. lw,.. 66 k 91 ) 67 68 67 67 67 (7 64 67 ——^-—^ 67 l^-^ 41 ^ —__ -- 47 V\ J 56 Contours 72 64 \ 86 70 87 80 81 - 100 n-4 66 (43 ---. 57 67 62 67 87 67 8767 6566 ((36 36 ) 6B ( 101 ) 51 'BS BO^__ 66 ,- 70 71 98 \ 62 72 16S 170) 119 172 W / IK V_ ^ ^——^ X N —— ^ f \ ( \ \ p^, 52 " 77 "^ 73 80 107 78 \ 39 \ 85 87 02 67 67 67 67 87 64 49 45 j' 66 fl.1 Q 153 \ 71 64 66 6U ^ 61 l 71) 58 7 110 153 ( 1 19 117 " " 67 -""W v 53 64 110- 72 67 86 77 60 78 —" 81 88 83 80 ~^~ 67 n=a 89 ——— 94 60 —— 80 55 72 ^ 39 ~~ 49 67 -^92 ^ 67 65 67 67 67 " 99 128 N 159 170- 126 II 1 Anotuitly

Definite 97+00 N 90+00 N 99+00 N 87+00 N aa+ooN 80+00 N 90+00 N 91+00 N 92+00 N 93+00 N 94+OON 95+00 N 96+00 N Chargeability 79+00 N BO+OON Bl+OON 82+00 N B3+OON J4+00 N — - 85-KMN 86+00 N Chargeability rnV/V /S l Probable mV/V 2.9 2.8 v^ 3.6 3.4 6.4 - 3.4 6.1 5.0 7.2 x 2.3 n=l 1.5 1.9 2.6 2.4 2.8 2.7 2.7 2.6 2.1 2.8 2.8'..t 3.2 |, M"/ I-" 1-9 ^--JjT.j-y 0.62 , Possible i 4 3.2 -^, 2.7 --, 3.4 3.6 7.3 J 2.5 ~" 54 0=2 ^ 0.88 1.2 1.4 1.3 1.8 x 2.4 ^ 1.B k 2.2 x, x 1.3 V \ 2.7 -^ 3, ^ 2.2 ( 4, 2,0 n-g j.6 2-__2, 2.4 2.5 2.6 2.8 2.3 2.3 2.6 l 3.6 J IJ^-— 1-3 1.6 080 — 0.96 "" 0.74 11=3 0.76' 0.89 13 ——- l. 4.1 ' 2.8 \ 3.8 2.4 l 4.1 ^ 6.3 0=3 ^ 1.7 2 2.3 2.8 2.8 2.6 2.5 2.2 2.8 2.8 ,- 2 \ 2.1 2.8 2.2 2.7 2.5 3.6 4.4 3.2 3.8 2.8 4.8 3.4 ~ 3.2 11=4 1.2 \ 1.6 \ 2, z j z (| z 6 2.6 2.4 2 3 I t/ 2.2 2.6 \~1.6' l.l" \^ 0.70 , \1.2 'OJll 0.87 0.77 l 0=4 11=5 0.88 0.75 " 0.48 f 0.76' 1.2 1.2 \ 1.6 \ 2.2 2.6 2.8 2.3 2.3 2.1 2.7 2.2 2.3 2.8 \ 1.1 1.6 \\ 0.86 \ 1.2 0=5 11=0 Scale 1:5000 1.00 ' 0.23 b.67y ' 1.8 2.7 2.4 x 3.2 ~— S. l 3.6 3.3 4.3 3.3 3,5 2.1 s 4.8 4.8 6.S ^* O 0=8 "l.4 2, 2 2.6 2.3 ^~\A - 2.4 2.2 2.8 1.1 - 2.5 2.8 x 1.6 1.9 ^ 0.20 ^ 1.4 o f)0 ion iTio : (uiftcrn)

B4+OON 85+00 N 86+00 N 87+00 N ^ 88+00 N U9+OQN 90+00 N 91+00 N 92+00 N 9M+00 N 94+OON 1)0 HK) N 9U+OON 97+00 N 1)11+00 N 99+00 N Rrsisl i vi i y 79+00 N __ 80+00 N 81+00 N 02+00 N 83+00 N PLATE 6 Resistivity ohm m ohm m 462 i 871 -. 406, 1103 -, BIB xv 1606 — 1607 - s 4M ; 687 11=1 0=1 WMC INTERNATIONAL LIMITED 591 l . 83^1 -^ X309' V 744 805 \ " 4BO \ 855 V. 734' 0=2 INDUCED POLARIZATION SURVEY 519 \ 916 903 ——— 713 661 11=11 0=3 \ n /^"" CLAW LAKE PROJECT 523 \, 8U5 --.. 881 1026 J 537 633 II--1 0=4 ^ f / \ CABOT TWP., NTS 4-1 P/ll 264 301 JBB x 731 \ 1316 ,\ 203 N 4*0 \ 954 U6U ^ ( 457 M5 h fi 0=5 . IJjilc: JIV/OJi/K) 0=8 206 228 250 l.1*11 174 6M) I4*:i x W. II II JVX Ltd. ret. no. 9687 eoaoft Software for the Earth Sciences 11111 J. J. nil 11 J. Igslisisisisss?

HONVda SQN\H 9NINM

Scale 1:5000 100 200

PLATE 7 WMC INTERNATIONAL UMITED CLAW LAKE PROJECT CABOT TWP., NTS 41 P/ll TOTAL FIELD MAGNETIC PROFILES Positive to East; l cm rep. 500 nT Base Field 57500 nT JVX Ltd. ref. no. 9687 LEGEND

Resistivity Anomaly

Extent of Surveyed Line

120171,3 Extent of Surveyed Line

.17094 4OO

PLATE 8

WMC International Limited ® Americas Division — Exploration

HON fUBSQNbTfflty^ LAKE PROJECT

SSi S &ifo* al Anomaly Compilation A 130^ Data Interpretation

COMPILED: RT SCALE: 1:5000 PN: -4054

DRAFTED: LWu REVISION: PLAN: CLAWGPHY 1 DATE: 21 FEB 97 DATE: MAP No.: 1211789 1211792

1201719 1201711 120N726 1201718

1888860 1201725 1201706

1201724

1201721

1201701

1201704 1201722 i MINING LANDS BR/ 1201715 1201723

WMC InTerncmonal Limited Americas Division — Exploration

CLAW LAKE PROJECT

Grid, Claims Se Topography

DATE: 09 JAN 96 DATE: 19 FEB 97 MAP No.: 1201712

-1201710

Mv(in)-py o Mv-(py)-(svni) C J Mt-(py)

, Mv-QFP '' Mv-py-qvni py-oK-qvn

1201707

^ XT"*-py v\ 706 1 188 886

1201717

201705

20 713

LEGEND

Grqnite

Diorite

Felsic dyke

Diabase dyke Quartz porphyry dyke Quartz feldspar porphyry dyk* Granite porphyry Mafic volcanic Intermediate volcanic Felsic volcanic

iGfy\44f# . ' tx Mafic tuff Intermediate tuff Felsic tuff Schist Chert Conglomerate

201704 Outcrop

Scattered outcrop

Small outcrop 1201714 Boulder Boulder Se rubble crop

inclined; vertical

S, Inclined; vertical

S, inclined; vertical

Jointing inclined; vertical

trend if plunge

brecciated strike zone

trench swamp 01727 vegetation boundary

SJCt-Moa-py-q* WMC International Limited Americas Division - Exploration

CLAW LAKE PROJECT EAST SHEET Geology 1201718

1201726 1201719

ffliaaui j&oaac* (Se

1201720 885 120 725

j&aaue* at

89039

1201724

120172

1201716

kanat* &C

201722 01715 1201725

WMC International Limited Americas Division - Exploration

CLAW LAKE PROJECT WEST SHEET Geology

41P11NVUD020 2.17094 CABOT 320 fYT7094 201712

201710

x CR-104549 CR-104550 CR-104551

CR-104554y CR-104561 X /X CR-104546 CR-104544

CR-104589 CR-104591 CR-I04592 CR-104593 X X XXX CR-104507 1201707 X CR-104506 CR-104588 CR-104505 CR-104504 CR-104583 CR-104582 201706 X CR-10453B CR-104584 CR-1Q4580 X CR-104684 1 188886 X CR-104685 X CR-104634 CR-104633 CR-104633 HONVHQSQNVn CR-104631 CR-104629 CR-1046S8 CR-104627 /66L S Z 83 J CR-J04626 CR-104625 CR-104599 Q3AJ303U

CR-104637 CR-10463B CR-104639 CR-104640

201717

201705

CR-104609 X X CR-104610 1201713

LEGEND

Lake Sediment Sample 1201714

SAMPLE LOCATION

\CR-1047H ^ CR-104733

CR-104713 CR-104716

CR-104712

201727

500 -H

WMC International Limitedted Americas Division — Exploration•ion

CLAW LAKE PROJECT EAST SHEET Geochemistry

PN: 4-054t

•SAMP

MAP No.:

MAP 4 201:712:;

M l (5 l (l 43 l O l (l 127 X (5 1201707 55 x a x a 46 l G l (\ X X X 122 X (5 X (l 350 l (5 X 84 X (5 7 (l 187 y (5 72 l (5 7 15 l (5 X X 67 X (S 7 88886 651 l ft X O X 3 7 -99 1 -99 X 3 X -W l -99 X 10 l (5 X (l 471 X O X 17417 X (5 X (l 165 X (5 X O 65 X (5 X O 3 X (5 X fl 67 X (5 X (l 7 X (5 X O Ml X tf X (l 10 X (5 X (l

1201717

201705

Nil X (5 X fl X X W X (5 X (l 1201713

LEGEND -W04

iment Sample FEB25 1997 1201714

Au - As

AM - Au value In ppb

BBS - As value in ppm

CCC - Sb value in ppm

< value below lower detection limit 201727 -99 not analyzed

WMC International Limited Americas Division - Exploration

CLAW LAKE PROJECT EAST SHEET Geochemistry

DATE: 21 FEB 97 DATE: 1-201/1

201

X U 11 l b 02/1/15 ft! l l l 23

0.4/3/12 15/4/13 0.7 / 147 / 21)1 03X2/11 XX 1201707 3.4 / 35 / 23 05/6/10 17 / U / 64 X 24X1X32 03 / fi l 47 l 12 l 52 x -99 x t x 43 188886 x -99/1X32 x OJX2X8 12.1 1 is i \\ 3505 / 4 l 374 6,9 / 15 / 14 1.8 / 11 / 17 12/4/8 18/2/73 0,4/1/92 OJXJX8 02/4/46

2J / 2 X 13 35/2/17 418/4/12 U / 2 / 2B

1201717

1201705

OJ X l X 99 X X OJ X l X 105 1201713

LEGEND

Lake Sediment Sample

Ag — Mo

HfcB25 1997

BRANC BBS — Mo value in ppm

CCC — Cu ! value In ppm

< value b aJLdefcctren liwm 01727 -99 not analyzed

WMC International Limited Amerlcas Division - Exploration

CLAW LAKE PROJECT EAST SHEET Geochemistry 1201

1201710

x 1/28/6 5/42/33 1/52/56

4/12/17 1 1 10 / 11 11/40/22 /S/15 X 1201707 3/18/12 X 2/6/15 18 / 20 7 16 10/84/46 1/13/17 3/15/18 188886 X-99/-99/-99 X-99/-W/-99 X B / 17 51 X 35 7 51 1290 / 8 / 24 64/18/25 4 / 30 l 39 1/13/8 5/81/62 3/98/66 8/10/22 1/92/59

1/28/18 .' 4/39/15 3/8/21 1/65/16 X X

201713

LEGEND 201704

Lake Sediment Sample 1201714

CEIVED M/51/-J9 ' l /43y-99 f - Zn value in ppm 1.17004 < * value below lower detection limit 201727 —99 not analyzed

WMC International Limited Americas Division - Exploration

CLAW LAKE PROJECT EAST SHEET Geochemistry 1201718

1201726 1201719

X CR-104697 X CR-104698

X CR-104699 x X CR-104703 CR-104701 X CR-104705 X CR-104704

CR-104577 X X CR-104710 CR-104709

1201720 88885 201725 GR-104 CR-102505 CR-10 CR-102506 X

X CR-104524 CR-104S33 CR-104522

X CR-104518 CR-104517 CR-104516

89059

CR-104663 Xx CR,]04666 X X CR-104661

1201724

1201721

120

X CR-104671 LEGEND CR-104670

Lake Sediment Sample

SAMPLE LOCATION 120 01715

WMC International Limited Americas Division - Exploration

GLAW LAKE PROJECT WEST SHEET Geochemistry 201718

201726

X l t -B l -39 XX134/-99/-99 W 7 -99 X -99 X 2 ; -99 7 -99 X173 l -99 7 -99 57(5/1 97(5/1 xxv M 7 e/ o w x c x 240 l (S X Z X fi X 58 l (5 X 14 X (5 X (

5 l Q l fl X X ffi X -99 X -95 89 X -99 X -99

1201720 88885 3 X (5 X (l 2 X (5 X 1201725 24 X (5 X O X

X 315 X (5 X O 31 X (5 X (l 48. X (5 X O

1189039

NH X (5 X (l XX 5 7 (5 X C MI X (5 X (l . X X NH l (5 X (l

1201724

1201721

201716

LEGEND

Lake Sediment Sample

201722 01715 AM — Au value in ppb BBB - As value in ppm 1201723 CCC — Sb value in ppm

< value below lower detection limit -99 not analyzed

WMC International Limited Amerlcas Division — Exploration

CLAW LAKE PROJECT WEST SHEET Geochemistry 201718

1201726 1201719

X -997 1 1 11/1/3 V X X -99X1X6 •99/2/8 g -99/1/27 -99/2/4 05/2/85 X 14.8 X 10 X 38 X

li l I 7 2 U/2/8 1.7 X 9 X 11 U X l l 6 0.9/2/1 02/6/55

0.1 1 1 / M X X -99/3/9 - -99 1 VI t

1201720 88885 03/1/316 1)2 X 4 / 32 1201725 2,0 X l X 778 X 3.4/4 95 / E / 188 M X 3 X 0.6 / l / 113

X 17.0X7X33 3.9/35/27 M / B / 74

1201724

1:201721

201716

X -99 / -W / -19 •99 X -W X -W

- :,' X . X. -9JX-WX-99 LEGEND •99 X-99 X-W e

Loko Sediment Sample

Ag - Mo - Cu 1201722 075 AM - Aq ' value i 1201723

FEB 25 1997

WMC International Limited Amerlcas Division - Exploration

CLAW LAKE PROJECT WEST SHEET Geochemistry

41P11NVW020 2.17094 CABOT 120

201726

X-99/-99/-99 X-99 l -99 / -99

X-99/-99/-99 X X -99 t -99 l -99 1/17/9 -99 / -99 / -99 tt -99 7 -99 l -99 4 / 167 1 60 X-99/-99/-99

X -99 1 -99 1 -99

51 / 28 X X -99 / -99 / -99 -99/-W/-W

1201725

1201724

1201716

x X -99 / -99 l -99 LEGEND 99 / -99 / -99

Lake Sediment Sample

RECEIVED 01715 AM - Pb value in ppm 1201722 BBB - Zn 201723 value in ppm MINING LANDS BRANCH

< value below lower detection limit —99 not analyzed

WMC International Limited Americas Division - Exploration

CLAW LAKE PROJECT WEST SHEET Geochemistry

DATE: 21 FEB 97 DATE: