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GEOLOGICAL AND GEOCHEMICAL REPORT

THREE BEARS MINERAL CLAIMS

SXEENA MINING DIVISION

MORESBY ISLAND QUEEN CIlARLOTTE ISLANDS B C

NTS 103B J l2W

LATIXUDE 52 41 N LONGITlJDE 131 52 W

CLAIMS THREE BEARS MAMA BEAR PAPA BEAR

BABY BEAR HOT PORRIDGE

OWNER Gordon G Richards

OPERAOOR Ventures West Minerals Ltd

CONnlACTOR JMT Services Corp

DATES OF WORlC April 20 May 4 1982

MINERAL RESOURCEP lNCH

ASSESSMiNT REPORT

June 1982 1001j

it

ii

rTABLE OF CONTENTS

LIST OF ILLUSTRATIONS ill

INTRODUCTION

1 Location and Access

2 Claims

3 Work Summary

1

GEOLOGY I

GEOCHEMISTRY 4

CONCLUSIONS AND RECOMMENDATIONS 4

STATEMENT OF COSTS 5

STATEMENT OF QUALIFICATIONSGordon G Richards 6

Colin Earivel 7

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Figure

1

2

3

4

5

8

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LIST OF ILLUSTRATIONS

Property Location Map

Claims Map

Geology

Gold GeoChemistry

Arsenic Geochemistry

Hi

Page

2

3

In Pocket

I

l

1

J INTRODUCTION

1 Location and Access

The claims are located in the Lockeport area of Central Moresby

Island some 58 kin south of Sandspit The claims extend from tidewater

around Anna Inlet north and west to elevations as high as 3400 feet Access

can be made by boat or float equipped fixed wing aircraft using Trans Provin

cial Airlines Otters or Beaver to Anna Inlet or more easily by helicopter

from Sandspit using either Queen Charlotte Helicopters or Vancouver Island

Helicopters

o

2 Claims

The property was staked in

are presently in good standing

Name Record No

THREE BEARS 2986 5

MAMA BEAR 2987 5

PAPA BEAR 2988 5

BABY BEAR 2989 5

HOT PORRIDGE 3088 6

1981 by Gordon G Richards and the claims

units Record Date

20 May 4 198L

20 May 4 1981

20 May 4 1981

20 May 4 1981

4 June 9 1981

3 Work Summary

In 1982 280 samples were collected of which 17 were rock chips

60 were silt samples and 203 were soil samples The purpose of this work

was to provide broad scale samling to discover areas anomalous for Au and

As worthy of more detailed mapping and sampling

GIDLOGY

I

The oldest rocks on the property are armutsen Formation greenstones

that underlie most of the property In the north half of the THREE BEARS

mineral claim the larmutsen greenstones are overlain as elsewhere on the

Charlottes by Kunga formation limestones limy argillites and argillites

Felsite dykes cut the Kunga sediments in this area The south eastern limit

of a fine grained quartz diorite intrusion was mapped and is shown along

the eastern end of Anna Lake

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J M T SERVICES CORP

THREE BEARSPROPERTY LOCATION MAP

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THREE BEARS

CLAIM MAP

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4

iAn old trail leadsfrom the western end of Anna Inlet SOUthwesF to

Anna Lake where old trails are visible along both north and south shoreI

lines An old adit is supposed to lie about 30 metres uphill from the LCP

for BJlBY BEAR mineral claim but was not located during the present survey

The Karmutsen float on the hillside in this area contains small quartz

veinlets with very low sulphide content Another area of intense quartz

veining occurs east of the outlet of Anna Lake see Figure 3 This zone

may extend several hundred meters or more east onto flat bottom land

immediately southwest of the head of Anna Inlet There is a second quartz

showing in this flat land at B194

GEOCHEMISTRY

Samples were collected in standard kraft sample bags and shipped

to Chemex Labs Ltd 212 Brooksbank North Vancouver B C

Soil samples were taken from the B horizon at a depth of from 5 to

20 em Rock chip samples were made up of 3 to 10 chips and weighed 200 400

gm Stream sediments were taken from the active part of creek beds

Samples were analyzed using the following standard procedures

Gold

Perchloric Nitric Atomic Absorption Analysis

Fire preconcentration Neutron Activation Analysis

Arsenic

Arsenic results have outlined a large zone of 30 ppm As northwest

of the outlet of Anna Inlet over terrain underlain by Karmutsen greenstones

and Kunga sediments

A second zone of anomalous arsenic occurs at and around the area

of intense quartz veining east of Anna Lake

Other anomalous arsenic results occur in stream sediments collected

at the base of the northwest facing slope that faces Anna Inlet and Anna

Lake

Too few samples have been analyzed for gold to provide a proper

evaluation of the gold mineralization potential

CONCLUSIONS AND RECOMMENDATIONS

oarmUtsen greenstones overlain by Kunga sediments are exposed on

the property An area of intense quartz veining east of Anna Lake is the

5

J most interesting mineralization seen to date and corresponds with an area

of anomalous arsenic results Another zone of anomalous arsenic oc s

northwest of the outlet of Anna Inlet

All samples should be analyzed for gold Following the gold

analyses more prospecting and some detailed evaluation should be undertaken

The quartz veined area between Anna Lake and Anna Inlet should be mapped

and sampled in detail The northwest facing slopes above Anna Lake and

Anna Inlet should be prospected further

STATEMENT OF COSTS

Time

G Richards April 28 May I 3C Harivel April 28 May 1 3W Howell April 23 May 1 3M Hagamoen May 1 3

Truck Rental May I 3

3 days @ 250 750 003 days @ 250 750 00

3 days @ 250 750 002 days @ 150 300 00

100 00

Q C Helicopters 348 00 924 80Richmond ReproductionVancal ReproductionP W A freightAirfare one man Vcr SandspitFood and AccommodationB C Tel

Supplies flagging string flares bags etc

DraughtingTypingVancal sepias black lines and photocopyingOlemex Labs

Report

1 272 80

343 55

122 94

88 00

132 85

534 31

37 25

300 00

400 00

50 00150 00

1 881 50

500 00

8 463 20

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STAlEMENT OF QUALIFICATIONS

I Gordon G Richards of Vancouver British Columbia do hereby

certify that

I I am a Professional Engineer of the Province of British Columbia

residing at 6195 Lynas Lane Richmond B C V7C 3K8

2 I am a graduate of the University of British Columbia B A Sc

196B M A Sc m 1974

3 I have practised my profession as a mining exploration geologist

continuously since 1968

4 This report is based on my personal knowledge of the district

and mapping of the geology at the property

L idJGordon G Richards P Eng

rII

certify that

1

2

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3

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SrATEMENT OF QtmLIFICATIONS

II

I C01in Harive1 of VAncouver British 1umbia do herebyi

II

I am a geologist iresiding at 3996 WestI

Vancouver British Columbia

II

lOth Avenue

II

I am a graduate of the University of British Columbial

B Sc Honours Geology 1972i

I have practised my profession as a mining exploration

geologist continuously since 1972

I am a FellOW of the Geologica1 Association of Canada

Harive1 B Sc

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THREE BEARS PROSPECT

SKEENA MINING DIVISION NTS 103 B 12W

GEOLOGY AND

SAMPLE LO CATIO N

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Kunga Formation thin bedded argillite limy argillite limestone

Ku nga Formation black flaggy limestone

K un go Formation massive grey limestone

Kormutsen Formation massive basaltic flows and pillowlalias volcanoclastlcs greenstone

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THREE BEARS

D IV ISION

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PROSPECT

NTS 103 B 12WSKEENA MINING

ARSENIC

i urvey by

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150000 Mop Enlargement Hip Chain Barometer

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EXPLANATION

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Creek

Outcrop

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Sample location numberArsenic As Gold Au

ppm ppb

RAVE N I

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T HREE BEARS PROSPECT

SKEENA MINING DIVISION

GO LD

S rvey by

NTS 103 B 12W

GEOCHEMISTRY

I 50 000 Map Enla rge men Hip Chain Compass 80 Bara meter

FIG 5oI

100I

L EGENDI

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0 I L S

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15 25 ppb Au

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50 ppb Au

X PL AN ATION

SCALE I 5000200 300 400

I I I

METERS

trike and dip of bedding or contact

and dip of fault or shear zone

ute rop

Sloil sampleS lt

ock chip sample

Sample location numberArsenic A s Gold Au

ppm ppb

RAVEN I

Cove

rI

I

I

G

3j

18

514

4 5I

I 8818G74 0 88513

tLst

511

4c

Iz 045 2I j

509

1 2M

f JlllI

II

311Y

I

0 0Zl42

3

C928 0

8504

I2

4 3

d0

O IA484 v

7 1615 YI

d8481

66

C i I 8490 101I

0 4T 848 6 48 in 6400 41 46I 0

73837

t0214 1

G

112 36

6l I CUISOG2 i2

0G

4 0G 32

3211

oo0

ZI96221

Zl97

141oII90

41o

lIesoZ 187

551

500I

MINERAL RESOURCES BRANCH

ASSESSMENT REPORT

QROCKS

t 15 50 ppb Au

50 ppb Au4

I

I

CJ

J

I

iIIII