WORK REPORT

THOMSON CLAIMS

Dana Township

Sudbury Mining Division, Ontario

Mining Claim: S-1229380

July 26th, 2001

Prepared For:

Pacific North West Capital Corp2303 West 41 st Avenue

Vancouver, British Columbia, Canada V6M 2A3

and

Anglo American Platinum Corporation Ltd.(Anglo Platinum)

Johannesburg, South Africa

Prepared by:

2-21838S. Jobin-Bevans, M.Sc. J-B Exploration & Development Inc.

225 Ferndale Avenue Sudbury, Ontario, Canada, P3B 3C2

(705) 524-8060 ,———————————————————

RECEIVEDand

Steve Weatherup , M.Sc.Consulting Geologist

Vancouver, BC

JUL 2 B 2G01

GEOSCIENCE ASSESSMENTf^f*r~t *\l~

OFFICE - SUDBURYRECEIVED

JUL 2 6 2001 ^

41I09NE2017 2.21838 DANA010

TABLE OF CONTENTS

Table of ContentsSummaryl .0 Introduction2.0 Personnel St Contributors3.0 Location & Accessibility4.0 Claim Status5.0 Regional Geology6.0 Property Geology

6.1 Lithological Summary6.2 Alteration A Metamorphism6.3 Local Structure6.4 Mineralization

7.0 Topography Si Vegetation 8.0 Previous Work 9.0 Current Work

9. l Geological Mapping A Sampling 10.0 Analytical Results

10. l Sampling *fe Analytical Technique10.2 Background10.3 Analytical Results

11.0 Conclusions 12.0 Recommendations References Certificate of Qualification

FIGURES1. Location of Property in Ontario2. Location of Thomson Claims in Sudbury Area3. Claim Map G-2904: location of Thomson Claims

TABLES1. Distribution of unpatented mining claims2. Assays from geological mapping in 20003. Background concentrations for RVI4. Assays from current program

Page

i1244461010111111121212121313131417171819

357

41214

15 A 16

Appendices: l. Sample List and Descriptions 2. Assay Certificates

Maps: Claim Map from Dana (G-2904)Geological Map of Thomson Claim bloc (l: 1000 scale)

41I09NE2017 2.21838 DANA 010C

SUMMARY

The Thomson claim bloc lies within Dana Township, about 100 road kilometres (50 km direct)

northeast of the City of Sudbury, Ontario. The claim bloc consists of 3 unpatented mining claim

units in l bloc that cover 36 hectares (0.36 km2 or 89 acres); claim map G-2904 (Dana Twp.)

shows the claims as covering 48 hectares or 3 full claim units (119 acres). The Thomson property

is underlain by rocks of the River Valley Intrusion (RVI), a large mafic intrusion of

Paleoproterozoic age (ea. 2 .56 to 2.47 Ga).

Work on the Thomson claim group was focused on geological mapping and sampling, in order to

evaluate the potential for Platinum-Group metal (PGM) mineralization associated with sulphide

and/or oxide minerals within the main portion of the intrusion. To date, PGM with the best

chance for economic viability have come from disseminated Cu-Ni sulphide mineralization that is

hosted by an extensive breccia unit, occurring proximal to the northern intrusive contact. The

current program is, in part, aimed at evaluating the upper portion of the intrusion for it potential

to host PGM within a stratabound or "reef type environment.

The current exploration program on the Thomson Claims was successful in identifying several

new PGM showings and in mapping in greater detail the distribution of the rock types, structure

and alteration patterns. The highest concentration of PGM (0.99 g/t Pt and 0.56 g/t Pd) came

from sample 52913, a coarse-grained to very coarse-grained gabbro with trace to G.5% visible

sulphide. The current program also demonstrated that when prospecting in the upper parts of the

stratigraphy, the presence of visible sulphide is not a necessity in generating elevated PGM

concentrations. Moreover, the relative lack of Cu-Ni sulphide and low sulphur suggests that the

PGM are associated with some other phase such as an oxide (magnetite?) and/or the PGE are

present mainly as platinum-group metals.

1.0 INTRODUCTION

This report presents a summary of the work performed on Pacific North West Capital

Corporation's (PFN) Thomson claims which was completed between July 6th and July 26th, 2001;

the claims are situated in Dana Township, Sudbury Mining Division, Ontario (Figure 1). The

work program is aimed at evaluating the potential for PGM mineralization within the upper

stratigraphic units of the intrusive complex.

PFN's River Valley property, which is located just to the north of the Thomson claim group but

is non-contiguous, contains anomalous concentrations of platinum (Pt), palladium (Pd), rhodium

(Rh), gold (Au), copper (Cu) and nickel (Ni). These metals are associated with sulphide

mineralisation that is primarily hosted by a heterolithic breccia (autoliths of pyroxenite-gabbro-

leucogabbro-anorthosite and xenoliths of country rock) occurring along the northeast margin of

the River Valley Intrusion (RVI), over a potential strike length that is ^ km.

Terminology

In this report, platinum-group metals or PGM refers to total concentration of Pt+Pd+Au and is

also referred to as 3E; 4E refers to the total concentration of Pt+Pd+Rh+Au. PGM is

synonymous with platinum-group elements (PGE) and the two terms are used interchangeably.

Current Program

The current work program (July 6th-26th, 2001) consisted of:

1. Geological mapping and sampling along the perimeter of the claim bloc; this

included a GPS survey of the claim boundary using a Trimble Pro-XRS with

TSC1 Asset Survey, using Landstar Real-Time differential correction with sub-

meter accuracy;

2. geological mapping and sample collection across the claim bloc; and,

3. geological mapping at l: 1000 scale.

Figure 1. Location of the River Valley Thomson Claims, Sudbury Mining Division, Ontario, Canada.

2.0 PERSONNEL A CONTRIBUTORS

Scott Jobin-Bevans (Consulting Geologist)- Exploration Manager

Steve Wetherup (Contract Geologist)- Field mapping, geological mapping, sampling, drafting,report writing

Dave Lyon (Consulting Geologist) - Drafting, report writing

Bondar Clegg (Val d'Or, Quebec) - contract commercial laboratory

3.0 LOCATION A ACCESSIBILITY________________________________

The Thomson claims lie within Dana Township and located about 100 road kilometres (50 km

direct) northeast of the City of Sudbury, Ontario (Figures l Si 2). The claim bloc is centred at

approximately 558344mE and 5164731mN (UTM17/NAD27). The claims are accessed by

travelling northwest and then north along HWY 805 from River Valley, a distance of about 5 km

from the Temagami River (north end of the village of River Valley). Turn right onto a logging

road, at the Giroux house, following it for about 500 m, approaching the site of the old Dana

Black Granite quarry. At this point several skidder roads and access trails lead toward the interior

of the claim bloc.

4.0 CLAIM STATUS_________________________________________

The Thomson claim group consists of 3 unpatented mining claim units (l claim blocs) that

cover 3.59 hectares (0.359 km2), in south-central Dana Township (Figure 3 and Claim Map G-

2904).

Table 1. Distribution of unpatented mining claims on the Thomson Property.Claim

1229380Twp.DanaTotal:

Units33

Hectares3.53.5

DueJuly 26, 2001

AmountS1200.00S1200.00

Ownership10007oPFN

PFN = Pacific North West Capital Corp.

The claim block listed in (Table 1) is owned 100*^. by Pacific North West Capital Corporation

(PFN) and all claims (3 units) are subject to PFN's joint-venture with Anglo Platinum

Corporation Limited.

\ONTARIO \

Sudbury'.

X V -

^'v* i^^lA--—-*' [River Valley ! Property

outhern Province (Proterozoic!

Figure 2. Location of Paleoproterozoic (ea. 2.5 Ga) intrusive rocks (dark areas) in the Southern, Superior and Grenville Provinces, Ontario. The River Valley Intrusion (RVI)iswell preserved and hosts subeconomic Pt-Pd-R h rich sulphide mineralization. TheThomson Claims on the River Valley Property are covered by the shaded square. Other intrusions with similar geology and mineralization are the East Bull Lake (EBLI) and Agnew Lake or Shakespeare-Dunlop (ALI) intrusions - both of these bodies are currently being examined for their PGE-Cu-Ni potential.

5.0 REGIONAL GEOLOGY

The main River Valley property and Thomson claims are primarily underlain by rocks of the

River Valley Intrusion (RVI), a large Paleoproterozoic (ea. 2 .56 to 2.47 Ga) intrusion that forms

part of the Huronian-Nipissing Magmatic Province (HNMP), which is also referred to as the

Huronian Metallogenic Province (HMP). The HMP also includes intrusive bodies such as the

East Bull Lake and Shakespeare-Dunlop (Agnew Lake) intrusions (ea. 2 .48 Ga) and younger

intrusions (ea. 2.2 Ga) of Nipissing Diabase (gabbro), all of which are intrusive into

Paleoproterozoic sedimentary rocks of the Huronian Supergroup (ea. 2 .45 Ga). Northwest-

trending olivine gabbro dykes of the Sudbury dyke swarm (ea. l .2 Ga) crosscut all of the older

rock types.

The East Bull Lake, River Valley and Shakespeare-Dunlop intrusions are thought to be the

products of sulphide-undersaturated, low Ti, high Al, tholeiitic magmas related to Late Archean-

Early Proterozoic (2440-2490 Ma) rifting of the Superior Province, and the subsequent

development of the Southern Province. Although no feeder dykes have been confirmed for the

intrusions, diabase dykes of the Matachewan-Hearst swarm appear to be the best candidates.

These dykes have high background PGM contents, contain bleb to finely disseminated sulphide

and have a whole-rock chemistry that is similar to the estimated bulk chemistry (parent magma)

of the East Bull Lake Intrusion.

The RVI intrudes Archean granitic plutonic rocks (alkali feldspar granite and syenite), and

regionally folded migmatitic gneiss and paragneiss (Pardo gneiss) along its eastern boundary and

lies in fault contact with Huronian metavolcanic and metasedimentary rocks along its western

edge.

MMxroiANe*IM

C 2904

'DANA

1 igure 3. Location ofllic Thomson Claims and the mn in River Valley Project elaim boundaries in Dana Township* (i-2904). Ontario. Canada.

The intrusion consists primarily of leuconorite and leucogabbro with subordinate anorthosite,

gabbro and pyroxenite and was originally thought to be a Late-Proterozoic anorthosite massif

intruded across the Grenville Front boundary fault (Lumbers, 1973). However, recent age dating

and current mapping confirms that the RVI is in fact part of the East Bull Lake suite of mafic

layered intrusions.

The RVI covers more than 100 km2 and lies adjacent to, and straddles the Grenville Front

within the Grenville Province and the Grenville Front Tectonic Zone (GFTZ). The GFTZ

represents a complex zone, several kilometres wide and consisting of generally southeast-dipping

imbricate thrust faults. In the area of the River Valley property, the GFTZ is located along the

westernmost edge of the claims where it is represented by a system of eastward-dipping (l0-25 0)

thrust faults. This fault system separates the intrusive rocks of the RVI from younger

sedimentary and intrusive rocks of the Huronian Supergroup (includes Nipissing Diabase). It is

likely that intrusive rocks of the RVI are interdigitated with Huronian rocks along the fault-bound

western contact.

Within Pardo Township, a north-trending apophysis of the RVI is in fault(?) contact with older

(Archean Superior Province) mylonitic granitic rocks. In Dana Township the western boundary

is in fault contact with rocks of the Southern Province, and the eastern and northern boundaries

are in igneous contact with Archean migmatite and paragneiss of the Superior Province. The

eastern and northern boundaries were previously mapped as being in contact with parts of the

Grenville Province (cf. Lumbers, 1973).

The RVI can be separated into two main areas on the basis of structural coherence and

preservation of primary igneous features such as contacts and layering. The eastern part of the

RVI, located primarily in Dana and Crerar Townships, is represented by the best preserved

portions of the intrusion and as such is most prospective areas for discovery. PFN's River Valley

property covers about AO'Yo of this area including about l O km of highly prospective northern

igneous contact. Further to the west, in Henry, Janes, Loughrin, Street and Awrey Townships,

the geology of the western part of the RVI is complicated by the effects of Grenville

metamorphism. In this area the rocks are attenuated, folded and structurally modified such that

most of the primary features are absent.

Metamorphism and Deformation

Metamorphic grade within the RVI ranges from greenschist to amphibolite facies in the west

(Dana Lake Area), greenschist to lower amphibolite in the east-northeast (Lismer's Ridge) and

middle amphibolite or higher metamorphic grades in the southern portions (Crerar Township). In

the immediate area of the Thomson Claims, rock textures are largely well preserved showing

evidence of greenschist to lower amphibolite facies metamorphism. The Sturgeon River

Deformation Zone or Sturgeon River Fault, a major northwest trending feature located in the

southern part of Dana Township and the northern part of Crerar Township, appears to separate

RVI rocks of slightly higher metamorphic grade to the south from rocks of relatively lower

metamorphic grade to the north. The Thomson Claims lie to the north of this major fault system.

Primary igneous mineralogy and textures are well-preserved in "core" areas generally located

away from, and topographically above, major deformation zones, and structurally above but

proximal to thrust fault zones (Hrominchuk, 2000).

On the River Valley Property, the intrusion is cut by numerous thrust faults with the main

direction of thrusting toward the present northeast (Hrominchuk, 2000). Localized ^200 m

wide) mylonitic deformation zones (trending about 3 O0) cut through the main body of the RVI at

intervals ranging from 700 m to about l km between deformation zones. Other east-west

trending mylonite shears cut through the intrusion in the northeast part of the intrusion, near the

Pardo-Dana Township line; major deformation zones and faults are marked by linear topographic

features such as swamps and, creeks and rivers.

Regional Tectonics A Crustal Sequence

Easton (2000) suggested a crustal sequence across the Grenville Front in the River Valley Area

that represents a southward-deepening section of crust. Exposure of the section is thought to be

the result of north-northwest directed transport along Grenville-age thrust faults. Easton (2000)

interpreted various levels of crustal exposure to include:

(1) Archean(?) metawackes exposed immediately north of the Grenville Front

represent high-levels of crust;

(2) Pardo gneiss immediately south of the Grenville Front represent the middle to

lower part of a 10-15 km thick upper crustal layer dominated by supracrustal

and moderate- to high-level intrusive rocks (i.e. Huronian Supergroup,

Nipissing Diabase);

(3) Red Cedar Lake gneiss represent the basal portion of the 10-15 km upper

crustal layer; and

(4) Crerar gneiss (tonalite to granodiorite gneiss and plutons) represent part of a 10-

15 km thick middle crustal layer.

The RVI appears to have been emplaced at the interface between a domain of migmatized

supracrustal rocks and a domain of granitoid plutonic rocks (Easton, 2000). Depth of

emplacement of the RVI remains unclear and it is suggested by Easton (2000) that the depth

could range from relatively high in the crust (3-5 km depth) to mid-crustal levels (~10 km depth).

Still unknown, is the effect of tectonic unroofing and transport of the RVI due to thrusting during

the Penokean Orogeny (1850-1700 Ma). Structural modifications during the Penokean Orogeny

may have been a significant factor in allowing for uplift and exposure of the RVI during the

Grenville Orogeny.

6.0 PROPERTY GEOLOGY_____________________________________

Mafic intrusive rocks of the River Valley Intrusion, both altered and relatively unaltered,

underlie the three claim units of the Thomson Claims. The mafic intrusive rocks have been

subdivided into leucogabbro and gabbro/anorthosite, and comprise at least 95*^ of the rock

exposures (see attached Geological Map). A Sudbury Swarm (~1.1 Ga) dyke and altered gabbro

which is interpreted to be altered River Valley Intrusion, comprise the remaining 5 07o of exposed

rocks on the claims.

6.1 Lithological Summary

Gabbro/Anorthosite is medium to coarse grained, contains SO-90%, dark grey, subhedral to

euhedral, plagioclase and JO-50% interstitial clots of pyroxene and/or hornblende with minor

magnetite. Sulphide clots and blebs (generally chalcopyrite) are rare, as are quartz veins.

Locally, along quartz veins and fractures, mafic clots are altered to fine grained chlorite +

amphibole H-/- biotite/phlogopite +J- garnet with very rare blue quartz.

Leucogabbro/Gabbro consists of 60-90'Ki white to light grey plagioclase with coarse grained

to pegmatitic regions that help distinguish it from the gabbro/anorthosite unit. Leucogabbro

consists of SO-90% subhedral to euhedral plagioclase and lG-50% interstitial mafic clots. These

mafic clots are mostly comprises fine grained, prismatic, hornblende with minor chlorite, biotite

and rare garnet. Small clots of chalcopyrite are rare and very fine grained sulphides occur finely

disseminated in mafic clots locally. Overall, sulphide content is very low (*x^).

One outcrop of medium grained olivine-gabbro occurs along the northern claim line, trends in

a north-south direction, and is composed of approximately equal amounts of inter-grown

hornblende and white plagioclase. A few rusty spots suggest the presence of trace amounts of

sulphides. This unit is magnetic (~10'K) oxide) and is interpreted to be a Sudbury Swarm dyke.

10

Altered gabbro is generally a fine grained, calc-silicate rock consisting of granular plagioclase,

chlorite, light green amphibole, epidote, biotite/phlogopite, and garnet. These rocks outcrop

directly east of a north-south flowing creek/swamp and grade over a distance of 10m into

relatively fresh/recognizable River Valley gabbro. Another alteration mineral assemblage

comprises fine grained, light green minerals (tremolite /serpentine?) and -lO'J'o magnetite

outcrops on the opposite side (west) of the creek/swamp. This appears to grade into fresh gabbro

over 5 m. Both, alteration assemblages carry trace amounts of sulphides.

6.2 Alteration A Metamorphism

Alteration/metamorphism of the mafic minerals (to fine grained prismatic hornblende, chlorite,

biotite and garnet) occurs throughout the western half of the claims and along the NE-SW

oriented valley to the east (see attached map). This same alteration mineral assemblage is also

found on the eastern side of the claims but it is restricted to envelopes along fractures and quartz

veins.

6.3 Local Structure

Fracturing and small scale shears (l to 10 cm wide) are generally oriented NE-SW in the

southeastern portion of the claim bloc. The NE-SW orientation parallels a linear valley, which

cuts through the southern portion of the claims (see attached map), and coincides with

hornblende+Achlorite-b'-biotite-b'-garnet alteration. This possibly suggests a more substantial

shear zone/fault is located in the valley. Furthermore, the localization of carbonate alteration

along a N-S oriented valley that cuts through the centre of the two western claim units may also

indicate the presence of a shear zone/fault that acted as a conduit for hydrothermal fluids.

6.4 Mineralization

Gabbro/anorthosite and leucogabbro rocks generally contain trace to negligible sulphides.

However, rare sulphide pods and blebs 0.5 to 20 cm in diameter, and fine-grained disseminated

sulphides (within mafic pods or regions) occur locally in the gabbro/anorthosite and leucogabbro

units. Sulphides consist primarily of pyrrhotite and chalcopyrite with minor pyrite.

Altered gabbro contains trace amounts to \ 07o disseminated sulphide, along with small ^Imm

diameter) blebs of pyrite and subordinate pyrrhotite. Trace sulphide also occurs in the olivine-

gabbro dyke at the north end of the claim bloc.

11

7.0 TOPOGRAPHY AND VEGETATION

Topography on the claims consists of two north-south ridges separated by a creek valley that

runs along the western boundary and through the centre of the SE unit. Slopes are generally

gentle, except for local, 2-3 m step-like outcrops on western slopes of the eastern N-S ridge, and a

5-10 m high cliff along a NE-SW gully that dissects the eastern ridge. Vegetative cover varies

from mixed pine, spruce, scrub oak, poplar and maple forest along ridges and at hill-tops, to

dominantly deciduous poplar and birch forest in low lying areas.

8.0 PREVIOUS WORK ________________________________________

In the summer of 2000, PFN completed regional geological mapping along the perimeter of the

Thomson Claim bloc. This work was completed at the same time as the initial OPS surveying of

the claim boundary. At this time, three samples were collected from claim S-1229380 from

which one, sample LH-158, assayed 31 ppb Au, 683 ppb Pt, 566 ppb Pd (1280 ppb 3E), 101 ppm

Ni and 1 110 ppm Cu; this sample constitutes the Thomson Showing (see Geological Map). This

sample is described as coarse-grained, massive, anorthosite (leucogabbro) with about 3*^

disseminated and bleb sulphide (207o cpy, Wo po). Other assays from this area include 83 1 ppb 3E

(LH-148: medium-grained, melagabbro) and 675 ppb 3E (LH-157: coarse-grained, anorthosite-

leucogabbro).

Table 2. Selected assays from Geological Mapping, Phase 2 surface exploration (summer 2000). Sample Rock 07oVS 07oBQ Au Pt Pd 3E Ni Cu Pd:Pt Cu:Ni

(ppb) (ppb) (ppb) (ppb) (ppm) (ppm) m-———-^LH-14J8 niejagabbro _ 5̂ _ - - - 49^ 172 610 831 956 2200 __ 3.5 - 2.3 LH-T57 """anorthosite 3 ~ " 108 """"344 223 675 M ~61~1 O6~" "T^cT IJH-158 iinM:i^ite~~3^~^^^~~3T~~~iM3~~566 i280~ldl~~TTlO O8 lil)'

VS = visible sulphide; BQ = blue quartz; 3E = Pt+Pd=Au

9.0 CURRENT WORK

9.1 Geological Mapping A Sampling

The 2001 work program consisted of five days of geological mapping and sampling and three

days of report writing and drafting; a differential OPS survey of the claim posts and claim

boundary was also completed at this time. A two man crew, consisting of one consulting

12

geologist with assistant completed the fieldwork between July 6th and July 10th, 2001 and were

based out of the TC Hotel in Verner, Ontario; subsequently three days were required to complete

the drafting and report.

Field Procedures

The GPS survey of the claim boundary was completed using a Trimble Pro XRS with TSC l

Asset Survey, using Landstar real-time differential correction with sub-meter accuracy. Points

(claim posts) were averaged from readings taken over 5 minutes (collected at least 300 points).

Rock samples collected were given a UTM position using a hand-held Garmin 12-XL GPS unit,

bagged, and given a unique sample number before shipping to Bondar Clegg Laboratories in Val

d'Or, Quebec. Samples were taken from most exposures in the study area and were selected: (1)

due to presence of sulphide minerals, (2) to represent every distinct rock type, and (3) every 50 m

along traverses, if exposure was available. A representative hand sample was also collected and

these samples are stored in Sudbury.

10.0 ANALYTICAL RESULTS___________________________________

A total of 64 rock samples were collected during the Thomson claims work program and

submitted for Pt-Pd-Au-Cu-Ni analysis. Locations of the samples are shown on the Geological

Map (1:1000 scale) and are listed with descriptions in Appendix 1; assay certificates are provided

in Appendix 2.

10.1 Sampling St Analytical Technique

All grab samples were sent to Chimitec Bondar Clegg (Val d'Or, Quebec) where they were

analyzed for Pt-Pd-Au using standard lead fire assay, followed by dissolution with aqua regia,

and measurement with an ICP finish. Lower limits of detection (30 g sample) are l ppb for Au, 5

ppb for Pt and l ppb for Pd, and lower limits are 2000 ppb for Au, and 10,000 ppb for Pt and Pd.

Concentrations of Cu-Ni were determined by ICP methods and generally have lower limits of

detection of l .0 ppm for Cu and Ni; upper limits are 10000 ppm for Cu and 20000 ppm for Ni.

10.2 Background

Background values were determined from Pacific Northwest Capital Corp's, River Valley

Project Phase 3 drill program. These values were calculated from the arithmetic average of 271

13

samples with low Cu concentrations (*:100 ppm Cu), which is considered to be a close

approximation of low sulphur content (Table 3). The overall average background metal

concentrations, based on Phase l surface work and Phases l, 2, and 3 drill core sampling is 11.6

ppb Au, 49.9 ppb Pt, 71.8 ppb Pd (133.3 ppb 3E and 121.7 ppb Pt+Pd), 98.4 ppm Ni, 55.0

ppm Cu, 1.5 PdrPt and 0.6 Cu:Ni

Table 3. Estimated background concentrations from River Valley intrusive rocks.Exploration Phase

Phase 1 Surface Work - DanaPhase 1 Surface Work - Azen

Phase 1 Drill Core - DanaPhase 2 Drill Core - DanaPhase 3 Drill Core - Dana

Phase 3 Drill Core - Lismer's

No. Samples

27910429723527146

Au (Ppb)10.85.67.06.57.032.9

Pt (ppb)73.113.448.633.659.870.6

Pd(ppb)123.526.357.632.876.5114.3

3E (ppb)207.445.3113.272.9143.3217.8

Ni (ppm)152.1157.566.995.776.541.4

Cu (ppm)46.775.549.366.355.736.3

Pd:Pt

1.72.01.21.01.31.6

Cu:Ni

0.30.50.70.70.70.9

ZE^Pt+Pd+Au; averages based on samples with *:l 00 ppm Cu

10.3 Analytical Results

Of the 64 samples collected, 5 1 have concentration that are ^0 ppb Pt+Pd; these samples are

listed in table 4 and all 64 samples are described in Appendix 1. Of the 51 samples,

concentrations of Pt+Pd range from 20 ppb to 1546 ppb with the highest concentrations

associated with melagabbro to gabbro that contain very little ^l*/^) visible sulphide. The

arithmetic average of the 51 samples is 96.9 ppb Pt+Pd and 1.9 Pd:Pt ratio. The highest

concentration of PGM (0.99 g/t Pt and 0.56 g/t Pd) is from sample 52913, a coarse-grained

to very coarse-grained gabbro with trace to G.5% visible sulphide. This sample contains

relatively low Cu (80 ppm) and Ni (l l ppm) concentrations which corresponds to its relatively

low sulphur content of G.06%. Only four of the 64 samples contain Pt+Pd concentrations that are

higher than the "exploration" background level of 122 ppb Pt+Pd.

Overall, the base metal values are typically low and in the 51 samples, Cu ranges from 8 ppm to

3257 ppm (108.3 ppm average) and Ni ranging from 5 ppm to 1389 ppm (75.2 ppm average).

The highest Cu-Ni concentrations are from sample 52901, a fine-grained gabbro with t-5%

visible sulphide. This sample contains 3257 ppm Cu and 1389 ppm Ni and the highest sulphur

content at 1.2807o; sample 52901 also contains 865 ppb Pt+Pd and relatively high Cr at 147 ppm.

14

Table 4. Analytical results from 51 samples - Thomson Claims, River Valley Project.Sample Texture Rock Name TS Au Pt Pd Pt+Pd Cu Ni Co Cr S

"/o ppb ppb ppb ppb ppm ppm ppm ppm "/o5290152902529035290552906529075290952910529115291252913529145291552917529185291952920529225292552926529295293052932529335293552936529375293852939529405294252943529455294652947529485294952950529515295252953

fgmgegegegmgegeg

pegpeg

cg-vcgmgeg

mg-cgmgegmgmg

fg-mgfg-mg

PegPegmgfgfg

mg-cgmgegegmgmgegmg

mg-cgmg-cg

egegegegegeg

GabbroMelagabbroLeucogabbroAnorthositeAnorthosite

GabbroGabbro

LeucogabbroLeucogabbroLeucogabbro

GabbroAnorthositeAnorthositeMelagabbroMelagabbroLeucogabbroMelagabbro

GabbroCalc-silicate/Skarn

olivine-gabbroLeucogabbroLeucogabbroMelagabbro

Altered gabbroAmphibole schist

GabbroGabbro

AnorthositeAnorthositeAnorthositeAnorthositeAnorthosite

Gabbro/ An orthositeAnorthosite

Gabbro/ AnorthositeGabbro

Gabbro/ AnorthositeGabbroGabbroGabbro

Gabbro/ Anorthosite

l-507o

trtrtrtr

tr-0.5%

tr-0.5%raretr

tr-0.5%trtrtrtr

nil-trtrtrtrtrtrtrtrtr

tr-0.5%

trtrtrtrtrtrtrtrtrtr

tr-1%tr

5865411210822433

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23813162812912161413277

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291915351510122948362114792846388928815188

214525232640

865277928632724

2582371

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325737

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138918391115192532271311518

3891091372140257379

525318224251517

201814152113191414121014

707867101012129759882471733111867

112151891289

23569761188657

14799949594728087718296821151008493108101101197969876183193111758570728287716969937971777278

1.280.040.050.040.030.030.030.030.040.040.060.040.040.030.040.030.030.020.010.070.040.040.020.010.020.040.030.030.030.050.030.030.020.040.030.020.030.030.030.030.03

15

Table 4 (cont) Analytical results from 51 samples - Thomson Claims, River Valley Project.Sample Texture Rock Name TS Au Pt Pd Pt+Pd Cu Ni Co Cr S

"/o ppb ppb ppb ppb ppm ppm ppm ppm "/o52954529555295652957529585295952960529615296252963

egeg

mg-cgmgfg

pegpegPegpeg

mg-cg

Gabbro/ AnorthositeGabbro/ Anorthosite

GabbroGabbro

Altered gabbroLeucogabbroLeucogabbroLeucogabbroLeucogabbro

Gabbro

fa

rrI 07ofa

irtr-0.5%

fa

rr- 1 "/otr

60000000013

23718162178

202024

30152319381712301519

53224135592420503543

7041273881922492042

23161119

1696591231

10978

37557812

68788010010580727777103

0.030.030.040.040.020.040.030.040.020.03

fgr fine-grained; peg = pegmatitic; mg = medium-grained; eg = coarse-grained; tr trace; TS = total sulphide

The majority of the highest PGM concentrations occur in Unit l - a medium to coarse-grained,

gabbro to anorthosite with generally trace to Wo sulphide. The highest PGM concentration is

from Unit 2 - a coarse-grained to pegmatitic leucogabbro with trace to Wo sulphide. The region

of hornblende (+I- chlorite) + biotite alteration tends to have the highest overall PGM

concentrations; sample 52917 being the exception. The altered gabbro - Unit 4 - did not show

much PGM enrichment relative to other areas that were sampled.

16

11.0 CONCLUSIONS

The current exploration program on the Thomson Claims was successful in identifying several

new PGM showings and in mapping in greater detail the distribution of the rock types, structure

and alteration patterns. The highest concentration of PGM (0.99 g/t Pt and 0.56 g/t Pd) came

from sample 52913, a coarse-grained to very coarse-grained gabbro with trace to G.5% visible

sulphide. It is important to note that this sample contains low Cu (80 ppm) and Ni (11 ppm)

concentrations which corresponds to its relatively low sulphur content of G.06% and low visible

sulphide. This suggests that in the upper parts of the stratigraphy, the presence of visible sulphide

is not a necessity in generating elevated POM concentrations. Moreover, the relative lack of Cu-

Ni sulphide and low sulphur suggests that the PGM are associated with some other phase such as

an oxide and/or the PGE are present mainly as platinum-group metals. Samples 52917 and

52901, both with elevated Pt+Pd, do show some Fe enrichment relative to other samples,

suggesting the presence of an oxide phase such as magnetite.

In general, the pattern of elevated PGM is not well defined. The western ridge, along the

western boundary of the claim bloc, has the highest PGM values including those of the Thomson

Showing proper. Unit l had the most samples with elevated PGM, but the highest PGM values

came from Unit 2, along the western side of the claims.

12.0 RECOMMENDATIONS____________________________________

Although this program failed to recognize any stratigraphic continuity in PGM enrichment, it

did discover several new PGM showings on the Thomson claim bloc. It is recommended that

further fill-in sampling, primarily for geochemical detail, be completed over the claims and that

follow-up geological mapping and sampling also be completed. A surface geophysical survey,

such as Induced-Polarization, might be considered on the basis of the follow-up sampling and

mapping program; one might also consider a small trenching (stripping) and sampling program

should values improve with subsequent sampling.

17

REFERENCES

Easton, R.M., 2000. Variation in Crustal Level and Large-scale Tectonic Controls on Rare-Metal

and Platinum-Group Element Mineralization in the Southern and Grenville Provinces; in

Summary of Field Work and Other Activities, 2000, Ontario Geological Survey, Open File

Report 6032, p. 28-1 to 28-16.

Hrominchuk, J.L., 2000. Geology, Stratigraphy, Geochemistry, and Copper-Nickel-Platinum

Group Element Mineralization in the River Valley Intrusion; in Summary of Field Work and

Other Activities, 2000, Ontario Geological Survey, Open File Report 6032, p. 29-1 to 29-11.

Lumbers, S.D., 1973. River Valley Area, Preliminary Map P.844. Ontario Division of Mines.

18

CERTIFICATE OF QUALIFICATION

I, Scott Jobin-Bevans of 225 Ferndale Avenue, Sudbury, Ontario, Canada, do hereby certify that:

1. I am a consulting geologist with the mineral exploration company JB Exploration St- Development Inc. of Sudbury, Ontario.

2. I am a graduate of the University of Manitoba, Winnipeg, Manitoba with a B.Sc. (Mons.)

Geology - 1995, and M. Se. Geology - 1997.

3. I am a member of the Society of Economic Geologists and the Canadian Institute of Mining,

Metallurgy and Petroleum.

4. I have been an exploration geologist and prospector for more than 12 years.

5.1 am a member of the Association of Geoscientists of Ontario.

6. I have an active prospector's license for the province of Ontario (# HI 4027).

7. This report is intended to be an overview of the potential of the property or properties and/or a

specific geological program carried out on the property or properties with recommendations

and conclusions that are based solely on the available data. As principal author, I take full

responsibility for the information presented herein and for the recommendations made on the

basis of the data.

Scott Jobin-Bevans (B.Sc., M.Sc. Geology)July 26th, 2001Association of Geoscientists of Ontario, Member

19

APPENDIX I

Sample Descriptions:

Geological Mapping on the Thomson Claim Bloc

Pacific North West Capital Corp. Appendix 1 - Data Thomson Claims - River Valley Property

Sample

52901529025290352904529055290652907529085290952910529115291252913529145291552916529175291852919529205292152922529235292452925529265292752928529295293052931529325293352934529355293652937529385293952940529415294252943529445294552946529475294852949

Texture

Lmgegmgegegmgmgegegpegpeg

cg-vcgmgegeg

mg-cgmg

_ egmg

mg-cgmgmg

fc fg-mgfg-mg

egpegpegpegegmg

^Jimg

-J5mg-cg

mgegegmgmgmg

-Cg

mg-cgmg

mg-cgmg-cg

egeg

Rock Name

GabbroMelagabbroLeucogabbroMelagabbroAnorthositeAnorthosite

GabbroGabbroGabbro

LeucogabbroLeucogabbroLeucogabbro

GabbroAnorthositeAnorthositeLeucogabbroMelagabbroMelagabbroLeucogabbroMelagabbro

GabbroGabbro

AnorthositeCalc-si licate/SkarnCalc-silicate/Skarn

Olivine-gabbroAnorthositeLeucogabbroLeucogabbroLeucogabbroLeucogabbroMelagabbro

Altered gabbroMelagabbro

Amphibole schistGabbroGabbro

AnorthositeAnorthositeAnorthosite

GabbroAnorthositeAnorthositeAnorthosite

Gabbro/ AnorthositeAnorthosite

Gabbro/ AnorthositeGabbro

Gabbro/ Anorthosite

TS /o

l-507otrtrtrtrtr

tr-0.5%tr

tr-0.5%raretr

tr-0.5%trfa

rrtrtr

nil-trtrtrtrtrtrtrtrtrtrtrtrtrtrtr

nil-tr

tr-0.5%

trtrtrtr

nil-trtrtrtrtrtr

AuPpb5865341121

108224332

171322222111303513326

211100220123010010

Ptppb20312400930701357112898721130015161768011151807li198

357088

23813167

28120912161413

Pdppb66215398193320311

201124355912186

291915351015571012119

294811362181479284638899288815188

2145

Pt+Pdppb86527798

2863273

242582371

154633316

29124315216235182530111640671971288

22875154511051656208

2430243558

Cuppm3257

372732452515028636027648021281872482055161236131277310188090273424159

4776353853452328162259332323

Nippm1389

18391511151938253227131151812

389109137225140164125737616795

52531228224251517

20183814161521131914

Coppm707876710131012129759688247179

336141118169674

1121571891289

2317567976

118

Crppm147999493959472118808771829682115901008493108671018512610119725081969897761838719311175857072688287757169699379

S0Xo

1.280.040.050.030.040.030.030.030.030.030.040.040.060.040.040.050.030.040.030.030.030.020.030.020.010.070.060.030.040.040.030.020.010.030.020.040.030.030.030.050.030.030.030.030.020.040.030.020.03

25-07-01 1 of 2 Appendix 1 Sample Data

Pacific North West Capital Corp. Appendix 1 - Data Thomson Claims - River Valley Property

Sample

529505295152952529535295452955529565295752958529595296052961529625296352964

Texture

egegegegegeg

mg-cgmgfg

pegpegpegpeg

mg-cgmg

Rock Name

GabbroGabbroGabbro

Gabbro/ AnorthositeGabbro/ AnorthositeGabbro/ Anorthosite

GabbroGabbro

Altered gabbroLeucogabbroLeucogabbroLeucogabbroLeucogabbro

GabbroGabbro

TS"/o

trtr

tr-1%trtrtr

I 07o

trtr

tr-0.5%tr

tr-1%tr

Auppb

0000600000000136

Ptppb277

201623718162178

2020240

Pdppb25232640301523193817123015192

Pt+Pdppb52304656532241355924205035432

Cuppm34251544704127388192249204245

Nippm

1412101423161119169659123154

Coppm

865710978

3755781215

Crppm717772786878801001058072777710371

S"/o

0.030.030.030.030.030.030.040.040.020.040.030.040.020.030.04

25-07-01 2 of 2 Appendix 1 Sample Data

Pacific North West Capital Corp. Sample Descriptions Thomson Claim Bloc - River Valley Project

Sample

52901

5290252903

52904

5290552906

5290752908

52909

52910

52911

52912

52913

52914

52915

529165291752918

NAD 83Easting

558814

558631558631

558605

558626558657

558629558507

558321

558251

558186

558111

558070

558119

558203

558332558393558440

Northing

5164945

51647045164704

5164702

51647795164783

51647505164710

5164741

5164758

5164763

5164737

5164838

5164916

5164895

516496951650105165007

NAD 27Easting

558799

558616558616

558590

558611558642

558614558492

558306

558235

558171

558096

558055

558104

558188

558317558378558425

Northing

5164721

51644805164480

5164478

51645555164559

51645265164486

5164517

5164534

5164539

5164514

5164615

5164693

5164671

516474551647865164783

texture

fg

mgeg

mg

egeg

mgmg

eg

eg

peg

peg

cg-vcg

mg

eg

egmg-cg

mg

Rock Name

Gabbro

MelagabbroLeucogabbro

Melagabbro

AnorthositeAnorthosite

GabbroGabbro

Gabbro

Leucogabbro

Leucogabbro

Leucogabbro

Gabbro

Anorthosite

Anorthosite

LeucogabbroMelagabbroMelagabbro

Comments

Appears to be a float boulder on o/c

SO-60% plagioclase50/50 plag and marks; small section of

leucogabbro on the S end of the o/c.some leucogabbro which has wavy contacts with

melagabbro.2007o px Si 8007o plag.

20"7o px & SO'Ji plag; rare chlorite /amph. clots with rust specks.25-3507opx7hbl

400i euhedral to subhedral 3-10mm plag; 600i fg hbl +/•ch^,bt', little blue qtz.

W/a euhedral to subhedral plag.; mafic s dark green aggregates of hbl or chl which psudomorph

the orgmal eg px or hbl.

50/50 plag/mafic; mafic clots are fine grained homblende/chlorite; mafic clots ~5cm in diameter.

-20-300/. mafics (fg hbl/chl); rare VS

20-30'!^ mafics, 70-80"7o light gray to mauve plag; tr-0.5% py at margins of mafic clots; mafic clots appear to be interstitial to euhedral plagioclase;

mafic clots have a l-2mm tight green to olive rind.

lfl-20% interstitial mafic clots of fine grained hbl +A bt.

ID-20% mafic clots (lg hbW-bt,chl); mafic clots contain tr VS.

40"7o mafic clots.50"7o plag, 45"7o px, and S 1)* mt

Half plag and half mafics with S-10% mt

Alteration

amphibolite mmm?

amphibolite mmm 7

amphibolite mmm ?

amphibolite mmm ?

amphibolite mmm ?

chl

TotalSulpb.%

l-5"7o

trtr

tr

trtr

rr-0.5%tr

tr-0.5%

rare

tr

tr-0.5%

tr

tr

trtrtr

Mafic"7o

Felsic%

Cpy%

tr

Po.%

1^/0

fy%

tr- 0.5%

tr

Sulph.Text

disseminated

disseminated

blebs

BlueQtz

W,

Misc.

25-07-01 1of3 Appendix 1 Sample List

Pacific North West Capital Corp. Sample Descriptions Thomson Claim Bloc - River Valley Project

Sample

5291952920

5292152922

5292352924

52925

52926

52927

5292852929

52930

52931

5293252933

5293452935

52936529375293852939

52940

52941

52942

5294352944

529455294652947

NAD 83Easting

558456558519

558418558360

558331558232

558232

558193

558168

558098558077

558092

558092

558238558318

558338558431

558431558814558809558774558747

558671

558640

558561558527

558562558601558597

Northing

51649975165007

51655745165364

51653045165330

5165330

5165349

5165373

51653755165292

5165240

5165176

51651985165216

51652205165200

51652005164951516500851650695165077

5165072

5165034

51649675164899

516482951648385164856

NAD 27Easting

558441558504

558403558345

558316558217

558217

558178

558153

558082558062

558077

558077

558223558303

558323558416

558416558799558794558759558732

558656

558625

558545558512

558547558586558581

Northing

51647735 164783

51653505165140

51650805165106

5165106

5165125

5165149

51651515165068

5165017

5164952

51649745164993

51649965164976

51649765164727516478451648465164854

5164848

5164810

51647435164675

5 16460651646145164632

1

texture

egrag

rag-cgmg

mgfg

fg-mg

fg-mg

eg

pegPeg

peg

eg

mgfg

mgfg

mg-cgmgegegmg

mg

mg

egmg-cg

mgmg-cgmg-cg

Rock Name

LeucogabbroMelagabbro

GabbroGabbro

AnorthositeCalc-silicate/Skam

Calc-silicate/Skam

olivine-gabbro

Anorthosite

LeucogabbroLeucogabbro

Leucogabbro

Leucogabbro

MelagabbroAltered gabbro

MelagabbroAmphibole schist

GabbroGabbro

AnorthositeAnorthositeAnorthosite

Gabbro

Anorthosite

AnorthositeAnorthosite

Gabbro/ AnorthositeAnorthosite

Gabbro/Anorthosite

Comments

30-40"7o mafic clots of fghbl +I- b tchloritic equigranular gabbro with some rust

staining.30-40"7o mafic clots of fg hbl +I- bt

ZO-30% hbl; little epidote and chlorite alteration ofplagandpx

Minor leucogabbro zones.Granular carbonate alteration of gabbro?; hbl,

plag, ep, garnet (grossular) and possibly diopside.

Mostly dark green granular hbH/- ep,chl, and garnet.

(dyke?) 3mm grains of hbl and plag but some rust; unaltered

weakly aligned euhedral plagioclase laths (igneous); few cpy blebs

mafic clots are fine grained hbl needlesmafic clots are fine grained hbl needles; tr V'S as

blebs and disseminated within mafics.-10-2(^mafic clots are fine grained hbl needles

andbt.~10-200Xo mafic clots are fine grained hbl needles

andbt.few rust stains

Carbonate altered gabbro with garnet and biotite/phlogopite; blue qtz and qtz veins with tr

py-slight chlorite alteration

Light green foliated and lineated schist (sheared and altered gabbro) Az 135/65; appears to be discrete shears within unaltered gabbro which

comprises the majority of the outcrop.

mafic minerals are comprised of fg hbl.locally foliated/sheared (Az 220/90)

ID-20% mafics (px/hbl)

some sulphide blebs visible in o/c ~ 30 cm in diameter.

equal proportions of plag and mafics; mafics comprised of fghbl and contain diss sulphides

Chlorite altered with mauve coloured plag; trace cpy in blebs.

lfl-20% mafics (px/hbl)Locally chlorite-*-/- biotite altered associated with

fractures.Mafics are hbl/chl with ~207ogt.

lC-30% mafics (px?); some rusty spots (VS?)

Alteration

cbl

chlorite/epidote

carbonate

carbonate

carbonate

chlorite

chlorite

chlorite/biotite

chlorite

TotalSulph'/o

nil-trtr

trtr

trtr

tr

tr

r 5-

trtr

tr

tr

trtr

nil-tr

tr-0.5%

tr

tr

tr

trnil-tr

trtrtr

Mafic"/o

FelsicV,

CpyK

tr

tr

tr

tr

Po."/o

ty"/,

tt

Sulph.Text

blebs and disseminated

BlueQtz

W,

Misc.

25-07-01 2 Of 3 Appendix 1 Sample List

Pacific North West Capital Corp. Sample Descriptions Thomson Claim Bloc - River Valley Project

Sample

52948

5294952950

52951

52952

52953

52954

52955

52956

5295752958

5295952960

52961

52962

52963

52964

NAD 83Easting

558612

558642558642

558611

558556

558728

558715

558719

558398

558384558244

558097558067

558060

558227

558328

558382

Northing

5164873

5164914

5164934

5164931

5164911

5164882

5164928

5164935

5165138

51651375165120

51650885165008

5164904

5164900

5164948

5165052

NAD 27Easting

558597

558626558627

558596

558541

558713

558700

558704

558383

LJ58369

558229

558082558052

558045

558212

558313

558366

Northing

5164650

51646905164710

5164707

5164687

5164659

5164704

5164711

5164915

51649135164896

51648645164784

5164680

5164676

5164724

5164829

texture

eg

egeg

eg

eg

eg

eg

eg

mg-cg

mgfg

pegpeg

peg

peg

mg-cg

rag

Rock Name

Gabbro

Gabbro/AnorthositeGabbro

Gabbro

Gabbro

Gabbro/ Anorthosite

Gabbro/Anorthosite

Gabbro/Anorthosite

Gabbro

GabbroAltered gabbro

LeucogabbroLeucogabbro

Leucogabbro

Leucogabbro

Gabbro

Gabbro

Comments

20-300Xo px; with qtz veins which is accompanied by chl-gt-hbl-bt alteration selveges.

ID-20% mafics (fe hbl and locally chl)~ l S-25% mafics (mostly hbl with some chl);

disseminated sulphides within mafics20-30"7o mafics; small qtz vein with chl-bt-gt

alteration and tr cpychlorite altered; many rusty patches possibly

disseminated sulphides.

ID-30% mafics (px?); some rusty spots (VS?)

lG-20% mafics; trace cpy and a few grains of blue quartz.

lQ-20% mafics; rare blue quartz and trace VS.

30-401^ mafics; some quartz veining with sulphides.

SO-60% mafics (chW-amph4Y-gt)completely altered to actinolite/ tremolite possibly serpentine and 10"7omt; seems to extend for- 10m

W of creek.

mafics are fg hbl.mafics are fg hbl and occur as clots ~2-3cm in

diameter.mafics only partially altered to fg hbl unaltered

portions look to be px.Few rusty fractures; mafics completely altered to

hbl-bt-gt.Chlorite or actinolite alteration/nunm of px?; 30-

40"Xo mafics; few blue quartz grains.~20-30"7ci px slightly ehloritized.

Alteration

carbonate

chlorite

chlorite

actinolite

chlorite

chlorite

TotalSulph'/o

tr

trtr

tr

tr-1%

tr

tr

tr

P/o

trtr

tr-0.5%tr

tr-1%

tr

Mafic"/o

Felsicy0

Cpy"/o

tr

tr

Po."/o

Py"/o Sulph.Text

diss

diss

vein

diss

fractures

BlueQtz

tr

tr

tr

Misc.

25-07-01 3 of 3 Appendix 1 Sample List

APPENDIX II

Assay Certificates (Pt-Pd-Au, Cu-Ni):

Bondar Clegg

Val d'Or At 2 Q-.TUL.-2f.

BONDAR CLEGG

l Val d 'or, PQ, Canada l URGENT S CONFIDENTIAL

To! PACIFIC NORTHWEST CAPITAL CORPORATIONAttention : MR. SCOTT JOBIN-BEVANSReference :submitter : S.WETBERUP

our Fax No: (819) 825-0256Your Fax No: 1-705-674-5883

Number of Pages : 9 including this page.

Report : T01 -57159.0 Status l

Element Method Totl

| AD FIRE ASSAY-ICP 64 l Aq INDUC. COUP. PLASMA 64

En INDUC. COUP. PLASMA 64 Co INDDC. COOP. PI/ASMA 64

1 Afi INDUC. COUP. PLASMA 64 Mn INDUC. COUP, PLASMA 64 Cr INDDC. COUP. PLASMA 64

1 W INDUC. COUP. PLASMA 64 | Mg INDDC. COOP. PLASMA 64

K INDDC. COOP. PLASMA 64 Ga INDDC. COUP. PLASMA 64

| Se INDOC. CODP. PLASMA 64

! Z r INDUC. CODP. PLASMA 64

1 1

1 Sample Preparations Totl Sample Typel MUM ..B.

CRUSH, SPLIT 64 ROCK , PULVERIZATION 64

1

1 1

1

i COMPLETE

Element Method

Total number of samples ; 64

Totl Element Method Totl

PT FIRE ASSAY-ICP 64 PD FIRE ASSAY-ICP 64 CU INDUC. COUP. PLASMA 64 Pb INDUC. COUP. PLASMA 64 MO INDDC. CODP. PLASMA 64 Nl INDUC. COUP. PLASMA 64 Cd INDDC. CODP. PLASMA 64 Bi INDDC. CODP. PLASMA 64 3b INDDC. COUP. PLASMA 64 Fe INDDC. CODP. PLASMA 64 le INDDC. CODP. PLASMA 64 Ba INDDC. COUP. PLASMA 64

V INDDC. CODP. PLASMA 64 Sn INDOC. CODP. PLASMA 64 La INDUC. COUP. PLASMA 64 Al INDDC. COUP. PLASMA 64 Ca INDDC. CODP. PLASMA 64 Na INDDC. CODP. PLASMA 64

Sr INDOC. CODP. PLASMA 64 Y INDDC. CODP. PLASMA 64 LI INDUC. CODP. PLASMA 64 Nb INDDC. CODP. PLASMA 64 Ta INDDC. CODP. PLASMA 64 Ti INDDC. CODP. PLASMA 64

S INDDC. COOP. PLASMA 64

Totl l Size. | .

64 | -150 11 1 1 1 1 1 1 1

Fraction Totl Remarks

64

Notas :

11

If you do not receive the entire transmission in legible form, please call us at (819) 925-0178.

At 20-.XTL-2T

BONDAR CLEGG

LIHJT: PACIFIC NORTHWEST CAPITAL CORPORATIONREPORT: ioi-57l59.o ( COMPLETE ) DATE RECEIVED! 12-JUL-01

PROJECT: AZENDATE PRINTED; 20-JDL-01 PAGE 1A( l i 8 )

AMPLENUMBER

5290152902529035290452905

5290652907529065290952910

5291152912529135291452915

5291652917529165291952920

5292152922529235292452925

5292652927529285292952930

5293152932529335293452935

5293652937529385293952940

ELEMENT ADUNITS PPB

566534

1121

108

22433

2171

322

22211

13

a35

13326

2111*1^

2

PTPPB

2031240*5

9

307

^1357

1126

9672113

^^151617

6e

^1115

18^

71119

635

7^

e

623

81316

PDPPB

6621539

819

3320

311

201

1243

5591216

6291

91535

1015

57

10

1211

92946

113621

614

7928463689

AgPPM

1.70.2

0.30.20.2

0.20.20.2O.20. 2

0. 20. 20. 20.20.2

0.20.20.20.20.2

0. 20. 20. 20. 20.2

0. 20.20. 20.20.2

0.20.20.20.20.2

0.20. 20. 20.20.2

Cu PbPPM PPM

3257 537 *2

273 rt24 V52 2

51 rt50 rt26 rt63 V60 rt

27 rt64 rt60 221 V26 2

18 372 rt46 rt20 255 O

16 rt12 rt36 rt

131 rt27 rt

73 rt101 O

8 rt60 rt90 rt

27 rt34 rt24 315 rt

9 rt

47 rt76 rt35 rt36 rt53 rt

ZnPPM

3312111110

1315151416

1718171117

1437231612

1014

81914

2721141014

106230

e16

1415151412

Mo

PPM

*12122

21121

22222

3^

121

2*1

2 art

^i232

2^

22

Kl

21222

NiPPM

136918391511

1519362532

271311

516

12369109

1372

25140

164125

737616

79

5525

312262

24251517

201

Co

PPM

70767e

710131012

129759

66624

717

933

61411

1816

967

4112

157

16

912

89

23

Cd BiPPM PPM

0 . 2 ^0 . 2 *50 . 2 ^0 . 2 ^0 . 2 ^

0 . 2 ^0 . 2 ^0. 2 ^0.2 ^0.2 ^

O , 2 ^0.2 ^0.2 *50. 2 ^0 . 2 ^

0 . 2 ^0 . 2 ^0 . 2 ^0 . 2 ^0.2 ^

0. 2 ^0 . 2 ^O . 2 ^O . 2 ^0 . 2 ^

0 . 2 -cS0 . 2 ^0. 2 ^0 . 2 ^0. 2 ^

0 . 2 ^0 . 2 ^0 , 2 ^0 . 2 ^0 . 2 *5

0 . 2 ^0 . 2 -C50 . 2 ^0 . 2 ^0 . 2 ^

Val d Or At 20-..TUL-2001 09:13 Faae

BOIMDAR CLEGG

JLIENT: PACT ne NORTHWEST CAPITAL CORPORATION REPORT: T01-57159.0 ( COMPLETE ) DATE RECEIVED! 12-JUL-01

PROJECT: AZENDATE PRINTED! 20-JUL-01 PAGE 1B( 2/ 8)

1 AMPLENUMBER

5290152902529035290452905

5290652907529065290952910

5291152912529135291452915

5291652917529165291952920

5292152922529235292452925

5292652927529285292952930

5293152932529335293452935

5293652937529385293952940

ELEMENT AsUNITS PPM

rt C5rt C5

rt

rt C5

rt C5

rt

rtrtrtrtrt

*5<5<5<5rt

<5<5<5<5rt

<5<5<5rtrt

rtrtrt<5rt

*5<5<5<5rt

SbPPM

<5<5rt C5

* 5

<5<5rt<5* 5

<5<5rt<5<5

<5<5rt<5<5

<5rtrtrt<5

<5*5rt<5<5

<5<5 C5

<5<5

*5<5rt<5<5

faPCT

2.451.060.971.090.98

1.201.371.391.271.47

1.401.471.040.711.28

0.807.712.430.901.66

0.932.940.772.031.43

2.233.201.260.600.65

0.659.402.340.611.70

1.151.551.291.422.00

Mn TaPPM PPM

92 OO129 *10170 *10154 -dO120 00

131 -ao222 *uo257 ^0203 -CIO199 -CIO

187 OO222 ^0114 *;10

93 OO194 OO

121 00665 00261 *;10133 OO172 rio

139 OD302 riO

94 <10323 00216 riO

213 OD127 OO188 -ao106 OO

119 OO

97 OO1197 riO

306 OO113 OO271 OO

176 riO304 riO138 riO146 OO176 riO

BaPPM

6144274143

4440263727

5540664839

3732455637

3225444220

3359505651

4230

1193714

4929384467

CrPPM

14799949395

9472

1168087

71629682

115

90100

6493

106

67101

85126101

197250

819696

9776

18367

193

11175857072

VPPM

1514192317

3618211913

112216

921

1812231812

1012152436

82351

171715

111665

916

2135454429

SnPPM

00OOOOOO00

00oooo^20^20

^20OOOOoo00

00oooo0000

00oooooooo

oooooooooo

oooooooo00

oooo00oooo

wPPM

00oooooooo

oooooooooo

oo00oooo00

oooooooo00

oooooooooo

oooooooooo

oooooooo00

oooo00oooo

La AlPPM PCT

1 6.42*U 7.65li 3.29O 6.40O 7.22

ci 6.05 CI 6.16O 5.490 5.52*1 5.12

O 7.73^ 6.85O 7.95O 8.50O 6.66

*1 *10. 00 ci 3.76*:1 6.43O 7.81^ 6.32

O 5.87O 4.43O 7.11O 2.83^ 0 . 64

3 3.99^ 7.17

1 6.75O 7.99 Ci 6.33

Ci 6.06^ 2.1420 2.35^ 6.59O 4.08

O 6.41O 3.00

1 6.22^ 6.97

2 9.19

Val d Or At 20-JUL-2001 09:13 Pacre 4

BONDAR CLEGG

-LIENT: PACIFIC NORTHWEST CAPITA! CORPORATION

REPORT: 101-57is9.o ( COMPLETE ) DATE RECEIVED: IZ-JOL-OIPROJECT: AZEN

DATE PRINTED: 20-001-01 PAGE 1C( 3/ 8)

AMPLENUMBER

5290152902529035290452905

5290652907529065290952910

5291152912529135291452915

5291652917529165291952920

5292152922529235292452925

5292652927529285292952930

5293152932529335293452935

5293652937529385293952940

ELEMENTUNITS

00000

00100

00000

07101

02011

00000

06001

00001

MgPCI

.54

.38

.46

.42

.33

.35

.75

.23

.64

.75

.70

.59

.24

.31

.72

.51

.13

.27

.38

.01

.43

.01

.38

.34

.03

.93

.35

.68

.34

.43

.23

.96

.82

.37

.72

.63

.58

.33

.42

.36

CaPCT

3.614.322.113.744.06

3.463.573.523.453.08

4.574.114.564.865.46

6.432.473.464.583.66

3.312.654.051.880.95

2.364.063.934.665.04

4.661.421.333.642.67

5.002.203.513.665.43

NaPCT

1.041.210.561.001.16

1.021.000.760.830.90

1.111.091.241.261.17

1.250.701.021.160.97

0.970.731.110.440.06

0,501.131.091.321.35

1.290.390.281.010.54

1.210.511.051.111.22

KPCT

0.130.090.060.090.10

0.100.100.060.070.08

0.180.090.140.100.10

0.110.060.110.110.06

0.050.060.090.060.01

0.170.140.130.150.12

0.050.040.430.060.05

0.060.040.140.090.15

SrPPM

164188

65157177

148154159133125

179150174207212

281116170212161

146124176132

6

89165ISO166193

1977745

152130

21174

153166255

YPPM

•d*:1•rt•tt•a

i*i*5i

2^

^11

•a•a

•a•a•sic*rt

q•5i*ai2

2•a•ci•rt•rt

•rt•rt

s•d^

li

*iil

GaPPM

66

•5246

53

O2

V

54765

7337

tf

3O

5•C2rf

211

455

53

^5

rf

5^

575

LiPPM

34523

35444

64446

122

1143

1333

•ci

85555

23513

42563

NbPPM

343

3

44555

65544

34432

410

444

45443

53456

So Ta TiPPM PPM PCT

^ *;10 0.024^ *;10 0.014^ -clO 0.026*5 *10 0.024^ *10 0.017

^ •tflO 0.033^ ^0 0.020*5 ^0 0.013^ ^0 0.030•:5 ^0 0.017

^ *10 0.016•55 ^0 0.036•55 ^0 0.034^ *:10 0.023^ -SlO 0.018

•J5 *:10 ^.010•55 ^0 0.013^ ^0 0.023*5 *10 0.031•C5 -510 0.013

•^ "ttO 0.017^ *:10 0.013^ *?10 0.018

5 -CO 0.0256 *:10 0.050

^ *10 0.111^ ^0 0.116^ ":10 0.016^ <10 0.033<5 4510 0.023

•55 <10 0.020^ <10 0.014<5 <10 0.142^ <10 0.017<5 *;10 0.012

<5 <10 0.0256 *aO 0.041

<5 <10 0.033<5 <10 0.029<5 *10 0.032

At 2C1-JUL-2I:

BONDAR CLEGG

-LIENT: PACIFIC NORTHWEST CAPITAL CORPORATIONREPORT: T0i-57i59,o ( COMPLETE ) DATE RECEIVED: 12-JUi-oi

PROJECT: AZENDATE PRINTED: 20-001-01 PAGE 1D( 4/ 8)

.AMPLENUMBER

5290152902529035290452905

5290652907529065290952910

5291152912529135291452915

5291652917529165291952920

5292152922529235292452925

52926529275292S5292952930

5293152932529335293452935

529365293752 93 S5293952940

ELEMENT Z r SONITS PPM PCT

^ 1.28•CI 0.04Kl 0.05•C 0.03•a o.o4

a 0.03*:i 0.03*1 0.03a 0.03^ 0.03

•a 0.04^ 0.04^t 0.06*tt 0.04^ 0.04

*1 0.05^L 0.03*1 0.04*!1 0.03^L 0.03

^ 0.03^ 0.02^ 0.03^ 0.02*:1 0.01

2 0.07•?1 0.06^ 0.03^ 0.04^ 0.04

^ 0.03^ 0.0211 0.01^ 0.03^ 0.02

^ 0.04•CI 0.03^ 0.03^ 0.03C 0.05

FAXSR: Chimit.ec. Val d'Or At 2CI-..UTL-2001 09: 13 Paae if

BONDAR CLEGG

-LIENT: PACIFIC NORTHWEST CAPITAL CORPORATIONREPORT: TOi-57159.0 c COMPLETE ) DATE RECEIVED! 12-JUI-01

PROJECT: AZENDATE PRINTED: 20-joi-oi PAGE 2A( 5/ 8}

•AMPLENUMBER

5294152942529435294452945

5294652947529465294952950

5295152952529535295452955

5295652957529565295952960

52961529625296352964

ELEMENT ADUNITS PPB

2tl12

3fi

10tl

1•CI

tl

tltl•51

6<l

<ltltl<l<l

tltl13

6

PTPPB

72812t5

9

1216141327

7201623

7

la1621

76

202024tS

PDPPB

928

6a

15

188

214525

2326403015

2319361712

301519

2

AgPPM

0.2•CO. 20.2•CO. 2•CO. 2

to. 2tO. 20.2tO. 2tO. 2

tO. 2tO. 2tO. 2tO. 2tO. 2

tO. 20.20.2to. 20.2

tO. 20. 2to. 20.2

CuPPM

4523261622

5933232334

2515447041

2736

61922

49204245

PbPPM

Ot2t2t2t2

t2t2

2t2t2

t2t2t2t2t2

2t2Ot2<2

t2<2t2t2

ZnPPM

169

101013

1011171412

1010101415

1114211112

11141614

MoPPM

13221

22121

22121

22

•ci22

2212

NiPPM

638

141615

2113191414

1210142316

1119

16965

9123154

CoPPM

175679

76

1188

657

109

76

3755

76

1215

CdPPM

0.2tO. 20.2tO. 2tO. 2

0. 2tO. 20. 2tO. 20.2

0.20.20. 20. 20.2

0.20.20.20.20.2

0. 20. 20.20. 2

BiPPM

rft5rft5t5

t5tsrftst5

t5rfrftstS

ts^rft5rf

tsrft5t5

d'or At 20-JUL-2C

BONDAR CLEGG

LIEWT: PACIFIC NORTHWEST CAPITA! CORPORATION

REPORT: TQi-57159.0 ( COMPLETE ) DATE RECEIVED: 12-JUL-oiPROJECT: AZEN

DATE PRINTED! 20-JUI-01 PAGE 2B( 6/ S)

AMPLENUMBER

5294152942529435294452945

5294652947529485294952950

5295152952529535295452955

5295652957529585295952960

52961529625296352964

ELEMENT AsUNITS PPM

^*I5*5^*S

^^*5^<5

^<5<5<5<5

^<5<5<5<5

^<5<5<5

SbPPM

^<5<5^* 5

<S<5<5<5<5

<5<5<5<5^

<5<5<5<5^

<5<5<5<5

FaPCT

1.600.771.010.911.22

0.980.941.561.391.29

0.940.891.061.381.64

0.921.153.480.720.80

0.871.031.501.55

Mn TePPM PPM

193 *;1092 ^0

121 ^0106 *:10182 *10

111 OO113 *10208 -;10173 <10143 <10

104 ^092 <10

117 ^0162 <10155 <10

157 *:10182 <10397 ^0106 <10

92 <10

126 -CIO146 <10312 -dO177 <10

BaPPM

2943435147

4336643741

3642324140

4242233558

46784042

CrPPM

6882877571

6969937971

7772786876

80100105

8072

7777

10371

VPPM

139

201116

1928292031

2018373251

1729241313

15172516

SnPPM

OOOO00^20^20

^20^20oo^20^20

^20OOOOOO00

00oooooo00

oooo00oo

HPPM

oooo00oo00

oo00oooooo

oo00oooo00

oooooooo00

oooo00oo

La AlPPM PCT

-;1 7.07d 7.70^ 6.75•CI 7.40

2 5.07

^ 6.43^ 6 .52

4 5.32d 7.53^ 6.17

^ 6.90^ 7.59^ 5.75•a 4.61

1 5.76

^ 8.46O 7.60^ 2.47•CI 8.95^ 7.89

*U 7.24O 5.270 5.12•a 6.4i

BONDAR CLEGG

ilENT: PACIFIC NORTHWEST CAPITAL CORPORATION REPORT! T01-57159.0 C COMPLETE ) DATE RECEIVED: 12-001-01

PROJECT: AZENDATE PRINTED: 20-JDL-01 PAGE 2C( 7/ 8)

UMPLENUMBER

5294152942529435294452945

5294652947529485294952950

5295152952529535295452955

5295652957529565295952960

52961529625296352964

ELEMENT MgUNITS PCT

1.480.260.360.400.57

0.310.270.700.600.41

0.320.250.270.510.36

0.460.523.100.380.23

0.360.530.790.69

CaPCT

3.974.323.654.042.96

3.683.742.954.003.47

3.784.073.242.593.33

5. IS4.591.395.144.35

4.132.663.643.60

NaPCT

0.901.211.061.170.82

1.021.060.631.161.00

1.121.190.920.770.91

1.161.100.241.241.19

1.060.760.791.00

KPCT

0.100.100.090.100.10

0.080.090.310.100.09

0.120.060.060.080.09

0.080.060.050.090.13

0.090.240.050.09

SrPPM

191187167175124

157159121182152

162176132115141

211169

70194166

156117128159

YPPM

41414l41

2

4141

24141

414l4141

1

414l4l414l

414l

241

SBPPM

426552

55355

67535

65

4256

44242

4

LiPPM

134326

23664

33223

33354

3e23

MbPPM

55454

44465

55545

45465

5444

Se TaPPM PPM

45 41045 41045 41045 41045 410

45 41045 41045 41045 41045 410

45 41045 41045 41045 41045 410

45 41045 41045 410*5 41045 410

*5 41045 410

6 41045 410

TiPCT

0.0110.0110.0220.0170.031

0.0160.0230.0450.0180.030

0.0220.0210.0300.0310.036

0.0230.0290.0200.0200.032

0.0300.0470.0280.019

Val d or At 2O-.JT.TL-20O1 O9:i3 Pacre 9

BONDAR CLEGG

t CENT: PACIFIC NORTHWEST CAPITA! CORPORATIONREPORT: ioi-57iS9.o ( COMPLETE )

ELEMENT UNITS

Zr PPM

DATE RECEIVED! 12-JOL-01PROJECT: AZEN

DATE PRINTED! 20-JUI-01

S PCT

PAGE 2D( B/ 8)

5294152942529435294452945

5294652947529485294952950

5295152952529535295452955

•tt

2

•tt

•tt

0.030.030.030.030.02

0.040.030.020.030.03

0.030.030.030.030.03

5295652957529565295952960

•Ci0.040.040.020.040.03

52961529625296352964

•a0.040.020.030.04

ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No:

Recording Date:

Approval Date:

Client(s):

304294

Survey Type(s):

W0170.30507

2001-JUL-26

2001-SEP-18

Work Report Summary

Status: APPROVED

Work Done from: 2001-JUL-06

to: 2001-JUL-26

PACIFIC NORTH WEST CAPITAL CORP.

ASSAY GEOL

Work Report Details:

Claim*

S 1229380

Perform

S5.310

35,310

Perform Approve

35,310

35,310

Applied

32,400

52,400

Applied Approve

32,400

32,400

Assign Assign Approve

SO 0

Tin Tio

Reserve

32,910

32,910

Reserve Approve

32,910

S2.910

Due Date

2003-JUL-26

Status of claim is based on information currently on record.

41I09NE2017 2.21838 DANA 900

2001-Sep-25 12:55 Armstrong-d Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2001-SEP-19

Ministere du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

PACIFIC NORTH WEST CAPITAL CORP. 2303 WEST 41 ST AVENUE VANCOUVER, BRITISH COLUMBIA V6M 2A3 CANADA

Tel: (888) 415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2 .21838 Transaction Number(s): W0170.30507

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

If you have any question regarding this correspondence, please contact LUCILLE JEROME by email at lucille.jerome@ndm.gov.on.ca or by phone at (705) 670-5858.

Yours Sincerely,

Ron GashinskiSupervisor, Geoscience Assessment Office

Gc: Resident Geologist

Laurence Scott Jobin-Bevans (Agent)Pacific North West Capital Corp. (Assessment Office)

Assessment File Library

Pacific North West Capital Corp. (Claim Holder)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16405

o o CN

oM

OM

imwMIMING LAND TENURE

MAP

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m IM mMtny.wl hDiinbin DevriDpniHit to* M Mitt lor ^ mm a ttUi njHun^a im -itdi J5 General I nformation a nd Limitations

I hn mT* i *i at on ttiow It iwlvlH Hu*4aui "** WtlMkln IHt PcovHkCtal HlnHiH ^*ttfHlrV 0 rf ir^iknu M dowrioaliiq Hum intrfiinlvlnr HN*nrwrn Davuopmsni andMnii Mvb it*.

CDNinlrdirniMK. tPlDMhiCbiJ Hkilnn FI *rnri**' f OHr

M1lttbl*WIMiW LlMlPUJ.JRiifp^rL^em.iH

NW lignin: NM; HJ H(n|actwn ulmhi*B(

Date /Time of Issue Apr 26 2001

TOWNSHIP r AREA

DANA

14:Q9h E astern

PLAN

G -2 904

ADMINISTRATIVE DISTRICTS i D IVISIONSMining Division Sudbury

Land Tlttes'Reglstry Division NIPISSING

M i nl t try of Natural Resources District NORTH BAY

TOPOGRAPHIC LAND TENUBE

Q ——j "i in,,,,,™.,,

D ™.,...H, Q Qm

i CM ice j l

a a a Q

LAND TENURE WITHDRAWALS

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONS

IMPORTANT NOTICESi. ml HIOMI or condrloivt anlHlt* *r-*fl norm j. B'*im*ctix:.

218

PACIFICNORTH WEST CAPITALCORPORATION

; 52927O

52922: ^52925

,: (J 52924

52923 .

Meters 10 o 10 20 30 40 Meters

LegendGabbro/Anorthosite: Medium-coarse grained, SO-90% dark gray sub-hedral to euhedral plagioclase, and ID-50% interstitial mafic clots composed of pyroxene tAhomblende and minor magnetite; alteration of mafic clots to fine grained prismatic hornblende with lesser amounts of chlorite^-/-biotite+/-gamet; rare sulphide clots.52936

52935LeucogabbfO; Coarse grained to pegmatitic, 50-90 Vo dark gray plagioclase and Id-50% interstitial mafic clots containing fine grained prismatic hornblende with minor chlorite, biotite, and garnet; small clots of chalcopyrite occur locally; overall sulphide content is52931 -OKvine-Gabbro Dyke: Sudbury Swarm; medium grained, equal proportions of intergrown hornblende and white plagioclase; oxide bearing; trace disseminated sulphide.

hbl+7-chl, bt

Altered GttbbfO: Fine grained calc-silicate and lesser tremolitic amphibolite/serpentinite; calc-silicate consists of plagioclase, chlorite, light green amphibole, epidote, biotite/phlogopite, garnet, and tremolitic amphibolite/serpentinite consists of 80-90 Vt, tremolite and/or serpentine with S-10% magnetite.

5295.7 1^52956NO

THOMSON SHOWINGl^Sg/tPt+Pd Symbols

LH-157O.STg/tPt+Pd'-.

I r \ Shear zone(dip not apparent, vertical, inclined)

\ \ Bedding) Outcrop limits(vertical, inclined)

Trench/clearing Geological contact - observed

,"" '- ---'l Geological contact -assumedX X v Subcrop

Geological contact - gradational

Joint(vertical, inclined)

Diamond Drill Hole Collar Location

501x1 Sample location, ^52942 . O/

(vertical, inclined)

[ D S Claim post l Line post Sample location

Igneous Layering (vertical, inclined)

52960 529170.29g7t Pt+Pd ^52919

*samples with "LH" = year 2000 program

l 52901........o.'syg/tPt+pd

'OO 52954

OLH-HS0.78g7t Pt+Pd

^52962 52915 O

hbl+Achl, bt

5290 Ol .6g7t

1229380

52905 Q

52910 o.26g7t Pt+pd52909 .

^52908 .

41I09NB2017 2 .21838 DANA210

MINISTRY OF

NORTHERN DEVELOPMENT

AND MM E S

PROVINCIAL MMIHG

RECORDER'S OFFICE

MINING LAND TENURE

564 rjfJOE 555 OOOE 556 0006 557 OOOE 558 00 HE 559 00 DE 560000S 561 OOOE 562 OOOE 564 OOOE

,o,5 173 DOON ! J f-

5 17200QN

5 1710 DON

5 17 O O TON

5169000N

5 168000N

5 167 DOOM

5 16 6 O BON

5 165000N

5164 DOON

229230 230038

12292321229542

244435

1229218

122984123730

12292 29223

^^BEiae^SC~ "^SSPS**-1-:CS— B-^iKt-CT—-^. 235836

THOMSON CLAIM BLOC1229373

229380 12293U7

s 173 mm

5 172 DOON

5171 DOON

5 170 MOM

5 169 DOON

5168 DOON

5167 DOON

5 166 CM ON

5 165 DOON

5t64000N

5550006 556DOOE 557 00 Of 5580DOE 559 OOOE 560 OOOE 561 OOOE 562 00 DE 563 OOOE 564 OOOE

UTM Zone 17

1 000m Grid

Those wishing to stake mining claims should consult with the Provincial Mining Recorders' Office of the Ministry of Northern Development and Mines for additional information on the status of the lands shown hereon. T Ms map is not intended for navigational, survey, or land title determination purposes AS the information shownonthismapis compiled from various sources. Completeness and accuracy are not guaranteed. Additional information may also be obtained through the local Lands Titles or Registry Office, or me Ministry of Natural Resources.

The information, shown is derived from digital data available in the Provincial Mining Recorders' Office at the time of downloading from the Ministry of Nod hern Development and Mines web site.

General Information and LimitationsContact Information:Provincial Mm ing Record ers' Office To! FreeWHIet Green.Mittef Centre Tet.1 (888).415-994S933Ramsey Lake Road Fax: 1 (877) 670-1444Sudbury, ON P3E 665HomePage: www.gov.on.caJMHDMWINESfl.ANDs/mismnpoeJttm

Map Datum: NAD 83Projection: UTM (6 degree)Topographic Data Source: Land Information OntarioMining Land Tenure Source: Provincial Mining Recorders' Office

This map may not show unregistered land tenure and interests in land including certain patents, leases, easements, right of ways, flooding rights, licenses, or other forms of disposition of rights and interest from the Crown. Also certain land tenure and land uses that restrict or prohibit free entry to stake mining claims may not be illustrated.

Date l T ime of Issue Jun282001

TOWNSHIP/AREA

DANA

17:51 h Eastern

PLAN

G-2904

ADMINISTRATIVE DISTRICTS l D IVISIONSMining Division Sudbury

Land Titles/Registry Division NIPISSING

Ministry of Natural Resources District NORTH BAY

TOPOGRAPHIC LANDTENURE

D Admlnlstratrve Boundaries

Township

Concession, .Lot

Provincial Park

Indian Reserve

Cliff, P t and Pie

Contour

Contour.- Appro* .Auxiterypepresston

Shaft

M re H e ad 1r am e

r ra*

Natural. Gas Poeline

Hydro Line

Communication Una

Wooded A rea

Monument - C adastrol,. Historical, Morn .Control

Freehold Patent

^^J Surlace And Mining Rights

^2J Surface Right s Only

Jjj Mning Rights Only

Leaseholtt Patent

^^J Surface And MmlngR^jhts

^^J Surface RighlsOnly

^y Mming Rights Only

Licence of Occupation

^^J Uses not Speeded

^^J S urlace And Mining Rghts

^^J Surface RighlsOnly

^J Mining Rights Only

K:J Land U se P erm it

•**J Order In Council

Ej W ater Powet.Lease Aggreement

i 1234567 l Mining Claim l l

LAND TENURE WITHDRAWALS

Areas Withdrawn from Disposition Miring Act Wtthdr aval. Types

Surface and Mining Rights Withdraw*! WB Surface Rights Only Witfidra-ivn Mn M ining Rlgrts Only Withdrawn

Order mCounciVMthdrawal TypesWSrtl Surface and Mining R.ghls WithdrawWS Surface Bights Only WithdrawalW*m Mining Rights Only Withdrawn

IMPORTANT NOTICES

1000 .Q m

LAND T ENURE WITHDRAWAL DESCRIPTIONS

D BSC tlDlion

6295 Wsm

6353 Wsm

6416 Wsm

W-LL-C1B2/99 Wsm

Jan 1 2001 AP16080

Jan 1 2001 PENDHG PERMIT FOR AGGREGATE

Jan 1 2001 QP.24661 88fl9

Mary 11 1999 Sec. 35 W-LL-C1B2J99 ONT 11/05/99 M .ft S

IMPORTANT NOTICESAreas under which special regulations. l Irritations or conditions exist thai affect normal prospecting,

staking and mineral development activities.