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GUICHON EXPLORCO LIMITED

SUMMARY OF PERCUSSION DRILLING

AND

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INDUCED POLARIZATION GEOPHYSICAL SURVEYS

ON THE

GN 1 8 CLAIMS

rCLINTON MINING DIVISION

NTS 92 P 14W

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nLC GEOLOGICAL BitASSESSMENT RE

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D GAMBLE

SEPTEMBER 1983II

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TABLE OF CONTENTS

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Page

SECTION 1

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INTRODUCTION

LOCATION AND ACCESS

TOPOGRAPHY AND VEGETATION

CLAIM STATISTICS

PREVIOUS WORK

GEOPHYSICAL SURVEYS

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SECTION 2

A GEOPHYSICAL REPORT BY PETER E WALCOTT

AND ASSOC LIMITED NOVEMBER 1982

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SECTION 3

A GEOPHYSICAL REPORT BY PHOENIX GEOPHYSICS

LIMITED JUNE 1983

SECTION 4

PERCUSSION DRILL PROGRAM

SECTION 5

COST STATEMENT

SECTION 6

CERTIFICATE OF ANALYSES

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SECTION 7

o CERTIFICATE

CERTIFICATE OF AUTHOR

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LIST OF ILLUSTRATIONS

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FIG 1 LOCATION MAP OF THE GN CLAIMS

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FIG 2 LOCATION OF GN 1 8 CLAIMS WITH

DETAILED TOPOGRAPHY

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FIG 3 LOCATION OF GN GRID AND

GN SUBGRIDS NOS 1 8

1 50 000

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SECTION 1

INTRODUCTION

LOCATION AND ACCESS

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TOPOGRAPHY AND VEGETATION

CLAIM STATISTICS

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GEOPHYSICAL SURVEYS

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rNTRODUCTION

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Two Geophysical Induced POlarization and Resistivity surveys

were conducted over the GN claims by Guichon Explorco Limited

Gin November 1982 and in June 1983 using geophysical contractors

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During the same periods two percussion drilling programs

totalling twenty 20 percussion drill holes 3355 feet were

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ocompleted

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This report contains the results obtained from these work

programs

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rLOCATION AND ACCESS

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UThe GN 1 8 claims are located 12 kms northeast of Lac la

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Hache B C The co ordinates of the centre of the property

are 51055 N 121023 W on N T S map sheet 92 P 14

DAccess to the property is gained via the Timothy Lake Spout

Lake road and then via a series of logging roads that lead

r toward the centre of the property See Fig 1 Location Map

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jTOPOGRAPHY AND VEGETATION

IJRelief is rolling throughout the claim group becoming steeper

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j to the south Timothy Creek valley trends northwest across

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the claim group with steeper valley slopes in the south compared

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to a broad valley in the north part of the claim group

Elevations vary from 3400 feet to 4400 feet asl

r Vegetation consists of fir and pine forests with some logged

J off sections et swampy conditions exist along Timothy

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CLAIM STATISTICS

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All the claims are in the Clinton Mining Division and are

registered in the name of Guiehon Exploreo Limited of Toronto

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The names record numbers number of units and recorded date

are as listed

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riClaim Name Record No units Record Date

GN 1 1125 20 August 28 1981

GN 2 1126 20 August 28 1981

GN 3 1127 18 August 28 1981

GN 4 1128 20 August 28 1981

GN 5 1129 20 August 28 1981

GN 6 1130 20 August 28 1981

GN 7 1131 20 August 28 1981

GN 8 1132 12 August 28 1981

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nSee Figure 2 Location of GN 1 8 claims with detailed

topography

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nPREVIOUS WORK

fluA geochemical reconnaissance soil survey was conducted over

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the GN claims by Guichon Explorco Limited in 1981 and followed

up in 1982 by more detailed soil grids filed for assessment

in 1982 The GN grid system and sub grids were utilized in

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the current work presented See Fig 3 Location Plan of

GN Grid and Sub grids Nos 1 8

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GEOPHYSICAL SURVEYS

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Geophysical survey lines were selected to cover soil geochemicalIf

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anomalous zones from a previous survey

The selected lines were brushed out to I P survey standard

The grid preparation was accomplished using Amex Exploration

IIL Services Limited and company personnel under field supervision

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of G Owsiacki under the direction of D Gamble

fTwo Induced Polarization surveys were carried out over selected

grid lines under the supervision of A Wynne

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The first survey was conducted in November 1982 over 25 1 line

nkilometres by Peter E Walcott and Associates Limited The

c report and results of this survey are enclosed as part of this

work report

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The second Induced Polarization survey was conducted in June 1983

over 6 0 line kilometres by Phoenix Geophysics Ltd The purpose

I of this survey was to further delineate anomalous I P responses

discovered in the November 1982 geophysical survey The report

n and results of the second follow up Induced Polarization survey

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are enclosed and form part of this work report

nThe following two sections contain the contract geophysical

reports and results of the surveys A location map Figure 3

n shows the GN grid system with all the geophysical surveyed lines

indicated on 1 50 000 scale plan

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THE G N GRIDTIMOTHY LAKE AREA B C

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I ISECTION 2

o A GEOPHYSICAL REPORT

1IBY PETER E WALCOTT AND

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ASSOCIATES LIMITED

NOVEMBER 1982

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PETER E WALCOrr It ASSOC LTD

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A GEOPHYSICAL REPORT

ON

oINDUCED POLARIZATION SURVEYS

nTimothy Lake Area Clinton M D B C

510 55 N 1210 23 W

N T S 92 P 14W

ilClaims Surveyed TY 1 2 5 6

GN 1 2 3 5

7

ndSurvey Dates October 27th

November 22nd

1982

1LFOR

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S E Leo INC

Vancouver British ColU@bia

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o Peter E Walcott P Eng

PETER E WALCOTT ASSOC LIMITEDr

U Vancouver British Columbia

o JANUARY 1983

TlILJ

01n GEOPlIYSICAJ SERVICES

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PElBR E WAJ CO rr IASSOC LTD

DTABLE OF CONTENTS

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Page

INTRODUCTION 1

1lPROPERTY LOCATION AND ACCESS 2

PURPOSE 3

o PREVIOUS WORK 4

GEOLOGy 5

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SURVEY SPECIFICATIONS 6

DISCUSSION OF RESULTS 8

SUMMARY CONCLUSIONS AND RECOMMENDATIONS 11

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APPENDIX

COST OF SURVE i

PERSONNEL EMPLOYED ON SURVEy H

CERTIFICATION Hi

LOCATION MAP TY 1 2 5 Scale 1 50 000 iv

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LOCATION MAP TY 6 GN 1 2 3 5 7

Scale 1 50 000

LOCATION MAP GN 1 2 3 5 7 Scale 1 100 000

PSEUDO SECTIONS OF I P v

oGEOPHYSICAl SERVICES

D PEllm E WAJ COlr ASSOC LTD

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INTRODUCTION

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Between October 27th and November 22nd 1982 Peter E

Walcott Associates Limited carried out limited induced polarizationsurveys for Selco Inc on th ir properties in the Timothy Lake area

of British Columbia

The surveys were carried out over preselected lines 17 in

all of seven reconnaissance compass and chain soil sampling grids

These lines were supposedly cut and rechained and in some

cases established across the geochemical grids to I P specificationsbut in many cases evidence of this was hard to find

1Measurements of apparent chargeability the I P response

parameter and resistivity were made along these lines using the

dipole dipole methof of surveying Readings were made with a 50 metre

dipole and first to fourth separation measurements obtained

nL The data are presented in pseudo section form on individual

line profiles bound in this report

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1IiJ GEOPHYSICAl SERVICES

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PROPERTY WCATION AND ACCESS

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The properties are located for the most some 12 kilometres

east of Lac La Hache in the Clinton Mining Division of British Columbia

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Claim Name Record No Units Record Date

TY 1 1133 20 August 28th 1981

TY 2 1134 16 August 28th 1981

TY 5 1137 20 August 28th 1981

TY 6 1138 12 August 28th 1981

GN 1 1125 20 August 28th 1981

GN 2 1126 20 August 28th 1981

GN 3 1127 18 August 28th 1981

GN 5 1129 20 August 28th 1981

GN 7 1131 20 August 28th 1981

Access is easily obtainable by 2 wheel drive vehicle from

Hwy 97 at Lac La Hache via the Timothy Lake road and numerous loggingroads that exist in that country

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PURFOSE

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The purpose of the survey waa to search for possibleoccurrences of sulphide mineralization within and around the largeairborne magnetic feature on which basis the ground was obtained

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PREVIOUS WORK

Previous work in the area is believed by the writer to

have consisted of prospecting geochemical and geophysical surveyingand drilling on the Coronex property to the east However the reader

is referred to detailed information held by Selco Inc

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GEOWGY

The reader is referred to reports and material held bySelco Inc

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SURVEY SPECIFICATIONS

The induced polarization IP survey was carried out

using a pulse type system the principal components of which are

manufactured by Huntec Limited and Phoenix Geophysics Limited ofMetropolitan Toronto Ontario

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The system consists basically of three units a receiverHuntec a transmitter and a motor generator Phoenix The trans

mitter which provides a maximum of 2 0 kw d c to the ground obtainsits power from a 2 0 kw 400 c p s three phase alternator driven bya gasoline engine The cycling rate of the transmitter ia 2 secondscurrent on and 2 seconds current off with the pulses reversing

continuously in polarity The data recorded in the field consistsof careful measurements of the current I in amperes flowing throughelectrodes Cl and C2 the primary voltage V appearing between thetwo potential electrodes PI and PZ during the lurrent on part ofthe cycle and the apparent chargeability Ma presented as a directreadout using a 450 millisecond delay and a 650 millisecond samplewindow by the receiver a digital receiver controlled by a micro

processor

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The apparent resistivity Pa in ohm metres is proportionalto the ratio of the primary voltage and the measured current the

proportionality factor depending on the geometry of the array usedThe chargeability and resistivity are called apparent as they are

values which that portion of the earth sampled would have if itwere homogeneous As the earth sampled is usually inhomogeneous thecalculated apparent chargeability and resistivity are functions ofthe actual chargeability and resistivity of the rocks

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The survey was carried out using the dipole dipoleelectrode array This electrode configuration and the methods of

presenting the results are illustrated in the appendix Depth penetration with this array is increased or decreased by increasing or

decreasing a and or n

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In practise the equipment is set up at a particular stationof the line to be surveyed three transmitting dipoles are laid out

to the rear measurements are made for all possible combinations of

transmitting and receiving dipoles the latter consisting of two

porous pota filled with an electrolyte copper sulphate solution a

feet apart up to the fourth separation i e n 4 the equipmentis then moved 3 a feet along the line to the next set up

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SURVEY SPECIFICATIONS cont d

A 50 metre dipole was used on the survey and first tofourth separation measurements were made

In all some 35 9 kilometres were covered using the above

omethod

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PElER E WALCOTT ASSOC LTD

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DISCUSSION OF RESULTS

The chargeability results in general showed the areas

surveyed to exhibit a very low chargeability background in theorder of 1 to 3 milliseconds probably occasioned in places by the

fairly thick overburden cover Thus although areas exhibiting chargeabilities of 3 to 4 milliseconds are shown as possible anomalousareas they probably in most cases reflect a change in backgrounddue to a rock type change etc

The widths of the anomalous zones shown here are themaximum possible and in all probability are considerably less thanillustrated

The areas surveyed will now best be discussed on an individual basis

GRID GN 1

Four lines were traversed with the IP method in thisarea As can be seen from the pseudo sections of Lines 56 60 64and 68 S re pectivily the resistivity results reflected the topography and underlying bedrock as can be seen by the higher valuesover the h ll to the east and the lows over the lake swamps etc

Two zones of poor to moderate I P response and limitedstrike extent can be seen striking across the eastern ends of Line60 and 64s respectively

A possible anomalous zone open to the west is observedat the western extremity of Line 68S This zone should be delineatedby additional work

Another possible zone that could extend to the southis observed at depth in the middle of Line 68S

GRID GN 2 3 5

Here five lines were traversed using the I P techniqueLines 24 28 32 36 and 40S respectively and yielded the most

interesting results

Numerous anomaloua and possible anomalous zones are

discernible on the pseudo sections two of which stand out as better

targets for further investigation They are 1 the zone s between

the BL and 6W on Line 40S and 4W and 8W on Line 36S and 2 the zone s

GIWPIIYSICAf SHRVICI S

PElER E WAI COrl lit ASSOC LlD

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DISCUSSION OF RESULTS cont d

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centred around 12 and 13W on Line 28S and extending from Line 32S

to Line 24S

oThe former is open both to the east and the south and

requires further delineation there whereas the latter is also

open north of Line 24S but appears to be eakening in response

nA case could also be made for extending the latter all

the way through to Line 40S but the writer believes this to be a

separate zone or joined to those on the southernmost extremities

of Line 28 and 32s

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Low resistivity readings are obtained east of TimothyCreek on Line 28S and in the swamp on the eastern end of Line 32S

GRID GN 7

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No resistivity and or IP contrasts are observed on the

two lines traversed here

TY IGRID

A large resistivity low most probably reflecting deepoverburden conditions is observed between 13 and 19 NE on the onlyline traversed here Low chargeability values are coincident with

this feature

Another resistivity break occurs at the 20 meter deepravine circa 5NE as evidenced by the lower resistivity values to

the southwest

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Anomalous chargeability conditions appear to exist all

the way across the line but would seem to be caused by changedin background due to the changes in rock type It could well be that

anomalous conditions only exist southwest of the ravine but in

any case additional work is needed to further investigate this

TY 2 GRID

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A moderately strong double peak anomaly suggestive of a

body of limited depth extent is observed striking across the south

western ends of Lines G l and 2 respectively

GEOPlIYSICAI SEUVrCFS

pmEn E WALCOlr ASSOC LTD

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DISCUSSION OF RESULTS cont d

oA zone of higher chargeability open to the north east

can also be observed at the other ends of the lines

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Low chargeability readings are obtained over the out

cropping topographic rises clearly discernible on the resistivityresults

TY 5 GRID

Here the resistivity survey suggests four rock type changescirca 4 7 8 5 and 14SW respectively A resistivity low appears to

occur at depth at 13 SW This complex resistivity pattern is attribut

able to patches of outcrop and or boulders encountered in ne emplacement of electrodes from 11 to 13SW It also gives rise to a complexIP pattern Itwould appear that a small zone of anomalous chargeability readings exis s around 11SW and that the reat of the higherreadings on the line are due to a background change caused by changesin bedrock and or oberburden cover Again more work is necessary to

sort out these responses

TY 6 GRID

A strong response caused by a shallow body 0 limited

depth extent is observed centred around 18N on the baseline This

would appear to be associated with a contact indicated by a

resistivity change at 17N

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It would appear that a second possible deeper zone could

be associated with the higher resistivity at 16N

Another resistivity contact could exist at 8 5N

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Three possible anomalous zones are observed on Line lOWwith the southernmost two probably indicative of a background changeas the chargeability values are fairly consistent over some 500 metres

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SUMMARY CONCLUS IONS AND RECOMMENDATIONS

Between October 27th and November 22nd 1982 Peter E

Walcott and Associates Limited carried out reconnaissance I P

profiling over several soil sampling grids for Selco Inc over

their Timothy Lake properties Clinton Mining Division British

Columbia

Several anomalous zones worthy of further investigationof one kind or another are observed over the low chargeabilitybackgrounds

These zones are noted in the previous section

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Although definition of these zones is sufficient on

GN 2 3 5 for investigation by diamond drilling further I P

work is necessary for better delineation of the rest of the I P

hopefuls

As a result the writer recommends that the results be

studied in conjunction with the limited geology the soil samplingresults and the results of the percussion drilling programme before

committing to further work of any description

o

Respectfully submitted

PETER E WA OTT AS OCIATES LIMITED

dQ J IhPeter E Walcott P Eng

Geophysicist

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Vancouver

British Columbia

January 1983

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COST OS SURVEY

Peter E Walcott Associates Limited undertook the

survey on a kilometre basis so that the total cost of services

provided was 29 770 10

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PETEn E WALCOn ASSOC LTD

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Name

Peter E Walcott

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PERSONNEL EMPWYED ON SURVEY

Occupation

Geophysicist

GeophysicalOperator

Typing

Address

Peter E Walcott Assoc605 Rutland Court

Coquitlam B C

V3J 3T8

Dates

Oct 27thNov 22nd 1982Jan 10 12 1983

Oct 27thNov 22nd 1982Nov 25 29th 82

Dec 12 20th 82

Oct 27thNov 22nd 1982

Jan 14th 1983

GEOPIIYSICAI SERVICES

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PETER E WALCOrr ASSOC LTD

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CERTIFICATION

I Peter E Walcott of the Municipality of CoquitlamBritish Columbia hereby certify that

o 1 I am a Graduate of the Univeraity of Toronto in 1962 with

a B A Sc in Engineering Physics Geophysics Option

o2 I have been practising my profession for the last twenty

years

o3 I am a member of the Association of Professional Engineers

of British Columbia and Ontario

4 Ihold no interest direct or indirect in the Timothy Lake

properties nor do I expect to receive any

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o VancouverBritish Columbia

oJanuary 1983

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o GEOPIIYSrCAL SERVICES

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ANOMALOUS ZONE

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SECTION 3

A GEOPHYSICAL REPORT BY

PHOENIX GEOPHYSICS LIMITED

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JUNE 1983

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PHOENIX GEOPHYSICS LIMITED

REPORT ON THE

INDUCED POLARIZATION

AND RESISTIVITY SURVEY

ON THE

TIMOTHY LAKE PROJECT

CLINTON MINING DIVISION

BRITISH COLUMBIA

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SELCO MINING CORPORATION LIMITED

Latitude SlOS2 N Longitude 121018 W

N T S 92 P l4

OPERATOR SELCO MINING CORPORATION LIMITED

BY

Paul A Cartwright B Sc

Geophysicist

Dated

September 16 1983

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PART A

1

2

3

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6

7

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PART B

PART C

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TABLE OF CONTENTS

REPORT 11 pages

Introduction

Presentation of Data

Discussion of Results

Summary and Recommendations

Assessment Details

Statement of Cost

Certificate Paul A Cartwright B Sc

Certificate John Marsh

Certificate Peter Gardner

Notes on Theory and Field Procedure

ILLUSTRATIONS

Plan Map in pocket

1P Data Plots

Location Map

Dwg IP P B 4027

Dwgs IP 5832 1 to 15

Figure 1

PAGE

1

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2

4

7

8

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1 Introduction

on

An Induced Polarization and Resistivity survey has been completedon the Timothy Lake Project Clinton Mining Division British Columbiaon behalf of Selco Mining Corporation Limited

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The project area is located immediately northeast of the communityof Lac La Hache B C which is on Highway 97 Access to the

individual grids on the property is via gravel logging roads from

Highway 97

Previous work during 1982 included airborne magnetic surveyingIP and Resistivity surveying was then used to further evaluate anomalous

magnetic responses

Objective of the present IP and Resistivity survey was to providemore complete coverage over some of the anomalous IP zones outlined

during last seasons work

A Phoenix Model IPV 1 IP and Resistivity receiver unit was used in

conjunction with a Phoenix Model IPT l IP and Resistivity transmitter

powered by a 2 Kw motor generator IP effect is recorded directly as

Percent Frequency Effect P F E at operating frequencies of 4 0 Hz and0 25 Hz Apparent resistivity values are normalized in units ofohm meters while Metal Factor values are calculated according to theformula M F P F E x lOOO 7 Apparent Resistivity

D Dipole Dipole array was utilized to make the majority of themeasurements with a basic inter electrode distance of 50 meters

Four dipole separations were recorded in every case Number ofline kilometers surveyed during the present survey was 14 35 linekilometers

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Field work was carried out during June 1983 under the supervisionof Mr John Marsh and Mr Peter Gardner geophysical crew leadersTheir Certificates of qualification are included with this report

2 Presentation of Data

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The Induced Polarization and Resistivity results are shown on the

following data plots in the manner described in the notes Part B

following this report

Grid Line Electrode Interval

58 008 50 meters

62 008 50 meters

66 008 50 meters

76 008 50 meters

78 008 50 meters

79 00S 50 meters

Dwg No

GN 1 5832 1

5832 2

5832 3

GN 4 5832 4

5832 5

5832 6

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SELCO MINING CORP LTC

LOCATION MAP

TIMOTHY LAKE PROJECT

CLINTON M D B C

N TS 92P 14 SCALE 600 000 FIG

D2

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n

Grid Line Electrode Interval Dwg No

TY I I OOW 50 meters 5832 7

2 00W 50 meters 5832 8

TY 2 l OOE 50 meters 5832 91 00W 50 meters 5832 10

TY 5 1 00S 50 meters 5832 11

TY 6 200E 50 meters 5832 12

2 00W 50 meters 5832 134 00W 50 meters 5832 146 00W 50 meters 5832 15

CDnLI

nLAlso enclosed with this report is Dwg IP P B 4027 a plan map of

the Timothy Lake Project area at a scale of 1 20 000 The definite

probable and possible Induced Polarization anomalies are indicated bybars in the manner shown on the legend on this plan map as well as on

the data plots These bars represent the surface projection of theanomalous zones as interpreted from the location of the transmitter and

receiver electrodes when the anomalous values were m a ureaDj

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Since the Induced Polarization measurement is essentially an

averaging process as are all potential methods it is frequentlydifficult to exactly pinpoint the source of an anomaly Certainly no

anomaly can be located with more accuracy than the electrode interval

length i e when using 50 meter electrode intervals the position of a

narrow sulphide body can only be determined to lie between two stations

50 meters apart In order to definitely locate and fully evaluate a

narrow shallow source it is necessary to use shorter electrode

intervals In order to locate sources at some depth larger electrode

intervals must be used with a corresponding increase in the

uncertainties of location Therefore while the centre of the indicated

anomaly probably corresponds fairly well with source the length of the

indicated anomaly along the line should not be taken to represent theexact edges of the anomalous material

GnL

11

The topographical geologic magnetic and grid information shown on

Dwg I P P B 4027 has been taken from maps made available by the staffof Selco Mining Corporation Limited

G 3 Discussion of Results

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Six separate grids lying within the Timothy Lake Project area have

been investigated by the present Induced Polarization and Resistivitysurvey and are shown on Dwg I P P B 4027

Results from each grid are discussed separately below

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3

Grid GN l

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Two anomalous IP zones are interpreted in the data acquired on the

three lines surveyed on this grid

D

Both zones are weakly to moderately anomalous with the more

western trend being open towards the west as well as to the north and

south The best defined individual anomaly occurs on the eastern IP

trend in the vicinity of Line 58 00S between station 36 00E and station37 50E Small concentrations of mostly disseminated material are the

probable source of these anomalous IP effects seen on Line 58 00S as

generally high apparent resistivity values are evident coincident with

the higher than background Per Cent Frequency Effect P F E values

While a narrow zone of lower resistivity material is evident near the

western margin of the zone it is not clear if more conductive

mineralization is present or if an ionic conductor such as a fault is

the causeCrL

Depth to the source of the IP response is indicated to be less than

50 meters in the case of the northern end of the east zone with the

zone apparently plunging towards the south Additional surveying would

be required to fully define the western margin of the second IP zone

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Grid GN 4

The IP and Resistivity results recorded on the three lines from

Grid GN 4 are interpreted to show three separate weakly anomalous

trends all striking north south There is some uncertainty in this

evaluation due to the fact that the most westerly zone is undefined

along its western mar in

The highest magnitude IP response is noted on Line 76 00S

interval between station 5 50W and station 5 00W where a local

high exists set within a background of less anomalous values

the source in this case is less than 50 meters subsurface

in the

P F E

Depth to

rLGrid TY 1

nJTwo lines were surveyed on this grid area during the 1983 IP

program Strongly anomalous responses are evident in the data from both

lines In each case there appears to be a central zone of concentrated

mineralization surrounded by considerable widths of less sulphide rich

rock

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oThe highest magnitude response is detected on Line 1 00W centered

on station 2 00N where depth to the target is less than 50 meters

subsurface

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Although the lines are orientated north east the core of the IP

zone may strike in a more northerly direction and appears to be more

deeply buried towards the south

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Grid TY 2

The most encouraging results Been in the IP data collected on this

grid are noted on Line 1 00E between station 1 00N and station 2 00Nwhere a moderately anomalous response is interpreted A flat lyingshallow conductive zone appears to cover the area between station 0 50Nand station 2 50N and may be caused by a superficial deposit such as

thick swamp However depth to the top of the polarizable material is

less than 50 meters

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On the second line Line 1 00W the IP response is much lessanomalous while displaying a more complicated signature Two separatenear surface sources are interpreted in the data

Grid TY 5

rI Line l OOS was the only line surveyed on Grid TY 5 during the

present IP program Two weakly anomalous responses are outlined by the

data The western anomaly consists of somewhat anomalous IP effects

accompanied by moderate magnitude apparent resistivity values situatedon the eastern flank of a very resistive rock unit which seems to be

hosting small amounts of disseminated sulphide judging by the

relatively high magnitude of the P F E values recorded within the highresistivity rock unit

on

e

On the eastern end of the line small concentrations of polarizablematerial are the probable source of the IP anomaly

Grid TY 6

r

l

One very anomalous IP zone is evident striking roughly in a

northwesterly direction It is seen in the data on all four lines

surveyed with the highest magnitudes being indicated on Line 2 00W

between station 0 50N and station 1 50N The source of the trend lies

within 50 meters of the surface on the three most northerly lines but

appears to be slightly deeper in the case of Line 2 00E as well as

being wider

o Although apparent resistivity values in the general area of the

anomalous IP effects seem to be quite low in absolute terms there does

not appear to be any clear correlation between the P F E patterns and

the resistivity patterns This suggests that the sulphide rich zone is

hosted by loosely consolidated or weathered rockserL 4 Summary and Recommendations

CThe Induced Polarization and Resistivity survey of six separate

grid areas within the Timothy Lake Project area has recorded anomalous

values in every area

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5

Grid GN I

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UTwo anomalous IP zones are evident A drill hole located so as to

pass through a point 75 meters tinder Line 58 005 station 36 50E wouldtest the source of the eastern zone

DIU

Additional IP coverage is required to fully outline the westernmargin of the other zone before drill testing is considered

Grid GN 4

oAlthough three separate weakly anomalous zones are interpreted in

the IP data from Grid GN 4 only the center zone which is slightly more

anomalous than the others should initially be considered for drilltesting unless other information is available to recommend them Adrill hole spotted so as to intersect a point approximately 50 metersbelow Line 76 00S station 5 25W is suggestedr

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Additional IP and Resistivity surveying is needed to close off thewestern side of the most westerly zone

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Grid TY I

uOne highly anomalous IP zone is detected on this grid

hole situated so as to pass approximately 75 meters beneathstation 2 00N is recommended to test the source of the most

response

A drill

Line I OOWanomalous

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Grid TY 2

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One anomalous IP zone is detected on Grid TY 2 A drill holelocated to intersect a point approximately 50 meters under Line I OOEstation 1 75N would test the most anomalous response

Grid TY 5

n A single line was surveyed on this grid and two weak IP anomaliesare noted in the data The western response could be drill evaluated on

a low priority basis by a drill hole spotted to pass approximately 50meters beneath station 10 85W on Line I OOSc

Additional IP and Resistivity surveying using shorter electrodeintervals is recommended to better define the source of the eastern

anomaly before drilling is considered

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A very anomalous IP zone is outlined by the data from this grid A

drill hole located so as to intersect a point approximately 50 meters

below Line 2 0 station 1 00N is recommended

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PHOENIX GEOPHYSICS LIMITED

UJJ LIAPaul A Cartwright B Sc

Geophysicist

Dated September l6 1983

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nU ASSESSMENT DETAILS

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PROPERTY Timothy Lake Project MINING DIVISION Clinton

SPONSOR Selco Mining Corp Ltd PROVINCE British Columbia

LOCATION Lac La Hache B C

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TYPE OF SURVEY Induced Polarization

and Resistivity

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OPERATING MAN DAYS 27 DATE STARTED June 8 1983

EQUIVALENT 8 HR MAN DAYS 40 5 DATE FINISHED June 19 1983

CONSULTING MAN DAYS 4 NUMBER OF STATIONS 302

DRAFTING MAN DAYS 6 NUMBER OF READINGS l716

TOTAL MAN DAYS 50 5 KILOMETERS OF LINE 14 35

SURVEYED

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cCONSULTANTS

Paul A Cartwright 4238 W 11th Avenue Vancouver B C

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FIELD TECHNICIANS

J Marsh 200 Yorkland Blvd Willowdale Ontario

P Gardner 393 Connaught Avenue Willowdale Ontario

G Richardson 4161 C own Crescent Vancouver B C

DRAUGHTSMEN

R C Norris 2499 Linwood Street Pickering Ontario

o

cPfZG1f J iPaul A Cartwright B Sc

Geophysicist

fDated September 16 1983

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USTATEMENT OF COST

Selco Mining Corporation Limited

onu

Induced Polarization and Resistivity Survey

Timothy Lake Project Clinton M D Lac La Hache B C

Crew J Marsh P Gardner G Richardson

Period June 8 1983 to June 19 1983

n14 35 lkm @ 780 00 lkm 11 193 00

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PfiE1S2fLEPaul A Cartwright B Sc

Geophysicist

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Dated September 16 1983

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CERTIFICATE

I Paul A Cartwright of the City of Vancouver Province ofBritish Columbia do hereby certify that

1 I am a geophysicist residing at 4238 W 11th Avenue

Vancouver B C

2 I am a graduate of the University of British Columbia B C

with a B Sc Degree

3 I am a member of the Society of Exploration Geophysicists and

the European Association of Exploration Geophysicists

4

5

I have been practicing my profession for 13 years

I have no direct interest directly or indirectly in the

properties or securities of Selco Mining CorporationLimited or any affiliate

6 The statements made in this report are based on a study of

published geological literature and unpublished privatereports

7 Permission is granted to use in whole or in part for

assessment and qualification requirements but not for

advertising purposes

DDated at Vancouver B C

This 16th day of September 1983 fJJ 4 aL 0Paul A Cartwright B Sc

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iCERTIFICATE

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I JOHN MARSH of the Municipality of North York OntarioNorth York Ontario DO HEREBY CERTIFY THAT

l I am a geophysical crew leader residing at

200 Yorkland Blvd Willowdale Ontario

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2 I am a graduate of the City of Norwich Technical CollegeU K ordinary National Certificate Electrical Engineering

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3 I worked with McPhar Geophysics Company from 1968 to

1975 as a geophysical crew leader

r4 I am presently employed as a geophysical crew leader by

Phoenix Geophysics Limited of 214 744 West Hastings Street

Vancouver B C

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Dated at Vancouver B C

This 16th day of September 1983 L ft1afJohn Marsh Ir

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oCERTIFICATE

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I Peter Gardner of the City of Toronto Province ofOntario DO HEREBY CERTIFY THAT

o1 I am a geophysical crew leader residing at

393 Connaught Avenue Willowdale Ontario

U 2 I am a graduate of Radio College of Canada inElectronics Technology

r11 3 I have been practicing my vocation about six

years

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4 I am presently employed as a geophysical crew

leader by Phoenix Geophysics Limited of 214 744 West HastingsStreet Vancouver B C

Dated at Vancouver B C

nThis 16th day of September 1983 PJ

Peter Gardner

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PART B

o PHOENIX GEOPHYSICS LIMITED

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NOTES ON THE THEORY METHOD OF FIELD OPERATION

AND PRESENTATION OF DATA

I

FOR THE INDUCED POLARIZATION METHOD

c Induced Polarization as a geophysical measurement

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refers to the blocking action or polarization of metallic or

electronic conductors in a medium of ionic solution

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conduction

This electro chemical phenomenon occurs wherever

electrical current is passed through an area which contains

metallic minerals such as base metal sulphides Normally when

current is passed through the ground as in resistivity measure

ments all of the conduction takes place through ions present

nL

in the water content of the rock or soil i e by ionic

conduction This is because almost all minerals have a much

Qr

higher specific resistivity than ground water The group of

minerals commonly described as metallic however have

specific resistivities much lower than ground waters The

Ginduced polarization effect takes place at those interfaces

where the mode of conduction changes from ionic in the solutions

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filling the interstices of the rock to electronic in the

metallic minerals present in the rock

rJL2

The blocking action or induced polarization mentioned

oabove which depends upon the chemical energies necessary to

allow the ions to give up or receive electrons from the metallic

1L

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surface increases with the time that a d c current is allowed

to flow through the rock i e as ions pile up against the

metallic interface the resistance to current flow increases

Eventually there is enough polarization in the f rm of

excess ions at the interfaces to appreciably reduce the amount

Jof current flow through the metallic particle This

polarization takes place at each of the infinite number of

o

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D

solution metal interfaces in a mineralized rock

When the d c voltage used to create this d c

current flow is cut off the Coulomb forces between the charged

ions forming the polarization cause them to return to their normal

position This movement of charge creates a small current flow

which can be measured on the surface of the ground as a decaying

potential difference

nJ

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From an alte nate viewpoint it can be seen that if the

direction of the current through the system is reversed

repeatedly before the polarization occurs the effective

Cnu

resistivity of the system as a whole will change as the frequency

of the switching is changed This is a consequence of the fact

that the amount of current flowing through each metallic inter

J

or

face depends upon the length of time that current has been

passing through it in one direction

The values of the per cent frequency effect or F E are

a measurement of the polarization in the rock mass However

since the measurement of the degree of polarization is related

to the apparent resistivity of the rock mass it is found that the

o metal factor values or M F can be useful values

nw

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determining the amount o polarization present in the rock

mass The MF values are obtained by normalizing the F E

ovalues for varying resistivities

The Inducep Polarization measurement is perhaps the

n most powerful geophysical method for the direct detection of

o

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metallic sulphide mineralization even when this mineralization

is of very low concentration The lower limit of volume per

cent sulphide necessary to produce a recognizable IP anomaly

will vary with the geometry and geologic environment of the

source and the method of executing the survey However sulphide

mineralization of less than one per cent by volume has been

detected by the IP method under proper geological conditions

UThe greatest application of the IP method has been

in the search for disseminated metallic sulphides of less than

n120 by volume However it has also been used successfully in

the search for massive sulphides in situations where due to

r source geometry depth of source or low resistivity of surface

layer the EM method cannot be successfully applied The ability

on

to differentiate ionic conductors such as water filled shear

zones makes the IP method a useful tool in checking EM anomalies

which are suspected of being due to these causes

In normal field applications the IP method does not

differentiate between the economically important metallic minerals

nL such as chalcopyrite chalcocite molybdenite galena etc

j and the other metallic minerals such as pyrite The Induced

Polarization effect is due to the total of all electronic

rU conducting minerals in the rock mass Other electronic conducting

c

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materials which can produce an IP response are magnetite

o pyrolusite graphite and some forms of hematite

ILIn the field procedure measurements on the surface

oo

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are made in a way that allows the effects of lateral changes

in the properties of the ground to be separated from the

effects of vertical changes in the properties Current is

applied to the ground at two points in distance X apart

The potentials are measured at two points X feet apart in

Gline with the current electrodes is an integer number n times

the basic distance X

The measurements are made along a surveyed line with

nu a constant distance nX between the nearest current and potential

uelectrodes In most surveys several traverses are made with

various values of n i e n 1 2 3 4 etc he kind

n of survey required detailed or reconnaissance decides the number

o

o

o

of values of n used

In plotting the results the values of apparent

resistivity apparent per cent frequency effect and the apparent

metal factor measured for each set of electrode positions are

plotted at the intersection of grid lines one from the center

nL

point of the current electrodes and the other from the center

point of the potential electrodes See Figure A The

oresistivity values are plotted at the top of the data profile

above the metal factor values On a third line below the

M

U metal factor values are plotted the values of the percent

frequency effect The lateral displacement of a given value is

o determined by the location along the survey line of the center

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D

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D

point between the current and potential electrodes The

distance of the value from the line is determined by the

distance nX between the current and potential electrodes

when the measurement was made

The separation between sender and receiver electrodes

is only one factor which determines the depth to which the ground

is being sampled in any particular measurement The plots then

when contoured are not section maps of the electrical properties

of the ground under the survey line The interpretation of the

results from any given survey must be carried out using the

combined experience gained from field results model study

results and the theoretical investigations The position of

the electrodes when anomalous values are measured is important

in the interpretation

In the field procedure the interval over which the

potential differences are measured is the same as the interval

over which the electrodes are moved after a series of potential

readings has been made One of the advantages of the Induced

Polarization method is that the same equipment can be used for

both detailed and reconnaissance surveys merely by changing the

distance X over which the electrodes are moved each time In

the past intervals have been used ranging from 25 feet to 2000

feet for X In each case the decision as to the distance X

and the values of n to be used is largely determined by the

expected size of the mineral deposit being sought the size of

the expected anomaly and the speed with which it is desired to

progress

on

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The diagram in Figure A demonstrates the method used

in plotting the results Each vaiue of the apparent resistivity

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apparent metal factor and apparent per cent frequency effect

is plotted and identified by the position of the four electrodes

when the measurement was made It can be seen that the values

measured for the larger values of n are plotted farther

from the line indicating that the thickness of the layer of

the earth that is being tested is greater than for the smaller

valUeS of n i e the depth of the measurement is increased

The IP measurement is basically obtained by measuring

the difference in potential or voltage b V obtained at two

operating frequencies The VOltage is the product of the current

U

o

o

through the ground and the apparent resistivity of the ground

Therefore in field situations where the current is very low

due to poor electrode contact or the apparent resistivity is

very low or a combination of the two effects the value of

AV the change is potential will be too small to be

numeasurable The symbol TL on the data plots indicates this

situation

o In some situations spurious noise either man made

or natural will render it impossible to obtain a readingrI i The symbol N on the data plots indicates a station at which

it is too noisy to record a reading If a reading can be obtained

oo

but for reasons of noise there is some doubt as to its accuracy

the reading is bracketed in the data plot

In certain situations negative values of Apparent

o Frequency Effect are recorded This may be due to the geologic

nL

Q

n

oo

7

environment or spurious electrical effects The actual negative

frequency effect value recorded is indicated on the data plotj

however the symbol NEG is indicated for the corresponding

value of Apparent Metal Factor In contouring negative values

nL

the contour lines are indicated to the nearest positive value

oin the immediate vicinity of the negative value

The symbol NR indicates that for some reason the

QnJn

operator did not attempt to record a reading although normal

survey procedures would suggest that one was required This

may be due to inaccessible topography or other similar

reasons Any symbol other than those discussed above is unique

to a particular situation and is described within the body

oof the report

nU

PHOENIX GEOPHYSICS LIMITED

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METHOD USED IN PLOTTING DIPOLE DIPOLE

INDUCED POLARI2ATION AND RESISTIVITY RESUL TS

x 7 nx re x

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Stations on lins x Electrods sprsad lenothn Electrode ssporation

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P P P P P1 2 34 2 3 4 5 3 4 56 4 5 6 7 5 6 7 8

9

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n 2 M F M F M F M F M F1 2 4 5 23 5 6 3 4 6 7 4 5 7 8 5 6 S 9

n 3 M F M F M F M F1 2 6 2 3 6 7 3 4 7 8 4 5 8 9 Apparent Mstal Factor

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o n

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FE FE E El 2 5 6 2 3 6 7 3 4 7 8 45 8 9

F E F E F E1 2 6 7 2 3 7 8 3 4 8 9

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EXPLORATIONSELCO InC WESTERNCANAllA

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I p CONDUCTORS NOVSZ SoMEY

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THE G N GRIDTIMOTHY LAKE AREA B C

9

Scale I 50 00OIl H IV OAT H T S

1P 1FIGURE

fIIlAC 0 Y 3J S JULY I n

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PERCUSSION DRILLING

o

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During the period November 19 1982 through to December 17

1982 sixteen 16 percussion drill holes totalling 2555 feet

779 m were completed to test soil geochemical anomalies that

had been previously outlined in earlier surveys

In addition during the period May 26 1983 through to May 30

1983 four 4 percussion drill holes totalling 800 feet

244 m were completed to test Induced Polarization anomalies

outlined in the November 1982 I P survey Drill hole locations

are tabulated in a summary table and drill hole collar locations

are shown on the accompanying GN Grid plan Fig 3

IU

o

o

o

on

Summary Table

Sub GeochemicallyP D H grid Coordinates Dip T D Elevated Values

GN 82 1 2 L36 00mSj 6 00mW 900 1201 AsGN 82 2 2 L32 00mSj 8 00mW 90 100GN 82 3 2 L28 00mSj 8 00mW 90 1651 AuGN 82 4 5 L28 00mSjlO 50mE 90 200GN 82 5 6 L12 00mSj10 00mE 90 200 CuGN 82 6 7 L2 00mS j 9 00mE 90 200 CuGN 82 7 7 L4 00mS 12 00mE 90 200 CuGN 82 8 2 L32 00mSj 3 00mW 90 1801 AsGN 82 9 2 L40 00mS 2 00mW 90 180GN 82 10 2 L42 00mS 3 00mW 90 180GN 82 11 4 L76 50mSj 4 50mW 90 190 I Ag AuGN 82 12 4 L77 50mS 4 50mW 90 110 Ag AuGN 82 13 1 L63 00mSj31 00mE 90 150 AgGN 82 14 1 L64 00mS 33 00mE 90 200 Cu Ag As Au Pb ZnGN 82 15 1 L62 00mSj33 00mE 90 80 AgGN 82 16 1 L59 00mS 33 00mE 90 100 AgGN 83 1 2 L40 00mSj 1 00mW 90 200 AgGN 83 2 2 L36 00mSj 4 50mW 90 200 Ag AsGN 83 3 3 L32 00mS 12 50mW 90 200 AgGN 83 5 1 L64 00mSj 3 50mE 900 200 Cu Ag

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D

A record of each hole was constructed on a wooden slat by

washing and sieving a portion of each drill chip interval The

cleaned and dried recovered coarse fraction was then glued to

the appropriate scaled off intervals on the grooved slat The

log chip boards for each hole were then examined under a bino

cular microscope and logged Accompanying this report are drill

logs for each percussion hole

DRILL RESULTS

The drill holes returned low uneconomic values for copper

silver arsenic gold lead and zinc There are however

elevated geochemical responses that offer some encouragement

The maximum concentrations from all holes are 276 ppm copper

25 0 ppm silver 67 ppm arsenic 120 ppb gold 750 ppm lead

and 382 ppm zinc The elements that are geochemically elevated

in each hole are tabulated in the summary table

The following holes offer the best results

Q

o

o

P D H

GN 82 6 140 ppm Cu over ISO 50 200

GN 82 7 135 ppm Cu over 40 150 190 I

GN 82 11 3 15 ppm Ag over 60 10 70

GN 82 11 82 5 ppb Au over 20 130 150

GN 82 12 3 83 ppm Ag over 65 15 80 I

GN 82 14 193 5 ppm Cu over 20 30 50

GN 82 14 1 05 ppm Ag over 201 30 50

GN 82 14 660 ppm Pb over 20 30 50

GN 82 14 280 ppm Zn over 20 30 50

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P D H

GN 82 14

GN 82 14

GN 83 5

GN 83 5

25 0 ppm Ag over 10

115 0 pp Au over 10

229 0 ppm Cu over 10

4 2 ppm Ag over 10

180 190

180 190

130 160

130 160

CONCLUSIONS

Encouraging geochemically elevated values only were obtained

in a number of the percussion drill holes Percussion drill

hole GN 82 14 was the most encouraging and further examination

in this area seems warranted

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1111I11

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STARTEDDec

8

82

COMPLETEDDec

8

82

FIIlOM

AMPLE

COlliE

CORE

ASSAYS

TO

DESCRIPTION

FIlOM

TO

EC

V

REMARKS

NO

LENGTHItlll

Cu

Aa

As

Au

0

20

O

B

n

nl

lOa

g

20

180

DIORITESILTSTONE

I

siliceous

2173

20

30

10

29

1

43

10

EllI

nediurnlioht

amvfine

chins

2174

30

40

10

28

1

27

10

UIllErmicro

finemanular

texturedandilooks

2175

40

50

10

28

1

50

10

0

a

siliceoussedinentH1atis

lioht

to

12176

50

60

10

33

1

22

10

rrrIlnsh

teinrolour

1

n

n

n

5

wellde

biotite

talsu

to

5

mnin

7n

An

1n

1

size

An

n

In

1

tlace

ovrite

2180

90

100

10

29

1

11

10

carIonate

12ll180

asinterstitial

2181

100

liO

10

31

1

10

10

IlBoneticsusceotibilitv

2182

liO

120

10

32

1

li

10

1

c

a

s

2ll90

2183

120

130

10

29

1

11

4

C

rT

S

9ll180

2184

130

140

10

30

1

12

5

2185

140

150

10

29

1

15

5

b2186150

160

10

32

1

17

1n

122187160

170

10

29

1

14

15

2188

170

180

10

27

1

16

15

MERRITTFUNK

n

J

LJl

l

l

I

rlor

CJ

L

J

CJ

l

L1

o

C

C1

C

lJ

cl

L

lJ

C1

SELeoMININGCORIORATIONLIMITED

SAMLE

COlliE

COilE

ASSAYS

FIIlOM

TO

DESCRIPTION

FftOM

TO

REMARKS

NO

LENGTHG EllIE

Cu

Acr

1

Au

Zn

0

10

om

o

10I

Cisina

10

70

SnllSIDNE

2189

10

20

10

51

2

6

17

10

lichtcnev

todatkcnev

withSOlle

bladfi

i22l90

20

30

10

28

2

0

50

10

arainedsiltstonechips

bOlo

30

40

10

32

A

20

10

5

disselllimted

PVritethmuchoutentilesection

b102

40

50

10

30

4

1

14

5

nechimcne

rrassiveovritewhile

othezsshow

g

so

60

10

33

19

12

5

te

strinF

b294

60

70

10

52

3

0

12

5

stJOnqintezstitia1

camonate

6070

lichtcnev

siltstonebedf

l

70

100

lINIE3ITEIDFFSEllIMENT

b

g

70

80

10

61

0

2

oalecneentorediun

cneentocnev

tuffsedinentb

g

RO

gO

10

59

n4

fi

araid

b

o

gO

nn

10

59

0

1

7

5

noaerateto

stronq

intertitialcarlonate

100

160

SnllSIDNEHANllESlTETUFF

Imoo1

00

lln

n

I

n

0

0

oalecneen

calaueotBfinecnainedsiltstone

b100

1110

l

n

10

11R

I

R

nocerateto

stronqcazIa1ateintezstitial

000

TOn

TOn

n

7

n

0

0

n

whitefeldsparcrvstalnieCESin

chi

on

TOn

An

n

OT

n

0

n

oon

no

lAn

Tn

In

19

n

0

22203150

160

10

42

0

8

3

5

Mmitt

FUTk

L

STARTEDtee

9

820IOLEVATION TOTAL

DEPTH190FEEr

3

2

CORESIZE2

INCHDRY

COMPLETEDIec

9

82

PERCUSSIONDRILLRECORD

HOLENo

GN82

ll

SHEETNo

1

LOCATIONL765CnS4

50nW

PROPERTYGNPROJECTSUBGRIDJt4

BEARING DIPCOLLAR900

0

c

G0

oel3

cJ

0

J

L

q

SEJRING

3L

OU

COM

900

STRTEP

Dee9

82

COI

ASSAYS

flEMRS

co

coJlf

ot5CR1P1ION

SAtE

0

0

tUTtt

o

n

frlOtoll

0

NO

cu

l

0

n

01

0

o

0

0

on

0

n

no

Innno

on

no

n

n

are

finerainedse

i

1011

on

nn

n

n

n

0

0

n

disseminatedtl

rouahoutall

10

70

interl

Je

troni

ersi

i

0c

S

7

7a

SIGNED

SEtCOt

ItlltlGCORpOR

OtltIM

lED

PERCUSSIONDR

RECORD4

3

EEY

TIOll

TOT

DEpTH1

90

FEE

2

CORESI7

E2Il

CIl

Ollll

COplefEO

pec

9

82

tlO

itlfl

SEJRING

OU

CovR

900

82

jo

OtENO

GN82n

SHEEfNO

2

oCTION1

76

S0mS4

SOnW

a

uEOt

11

CJ

L

I

rJ

0

J

Cl

tICc1JLt

ct

CJ

CJ

lt

LJ

rJ

CJ

SELCOMINING

CORPORATIONLIMITED

FIlOM

TO

OESCRIPTION

SAMLE

COllE

COilE

ASSAYS

NO

FIlOM

TO

lENGTH

tco

REMARKS

P

CU

Ag

As

Au

n

T

D

0

10I

casina

15

no

SlLlS1DNE

ANIESITE

lUFF

n7

15

20

5

25

5

0

10

55

EDFl

1530

e

fine

d

stroninterstitial2220820

30

10

26

2

5

9

10

cmlonate

22209

30

40

10

38

1

9

11

25

tJaoatoU

disseminatEdovrite

2221040

50

10

44

6

0

12

15

fn

T

m

ensedinents

2221150

60

10

57

2

5

10

55

50

30

1e

creamwhiteto

le

fine

2221260

70

10

17

7

5

15

stronercarlx1ate

2221370

80

10

27

2

0

14

15

80110

Me

n

tobuffa

lowed

fire

hd

22214

80

90

10

54

10

10

10

2221590

100

10

50

0

1

15

10

Mi

eticSUSCEotibilitv

22216100

110

10

54

0

5

12

5

0

1

c

er

s

thronolYut

section

I

Lovof

L

DRILLEDBY

ttFulk

SlGNED

J

STARTEDDec

9

820ELEVATION TOTAL

DEPTH110FEET

3

2

CORESIZE2INCHDRY

COMPLETEDDec

9

82

PERCUSSIONDRILL

RECORD

HOLENoGN82

12

PIlOPERTY

GN

PROJFCT

SUBGRIDlJ4

SHEETNo

LOCATION1 L77

50mS4

50mW

BEARING DIPCOLLAR

90c

CJ

1

1

l

J

CJL

I

I

1

HOLENO

GN8213

SHEETNo1

LOCATIONL63HJQnS

3HOOrrE

PROPERTY

1

I

l

I

rJ

l

l

CJ

SElCOMININGCORPORATION

LIMITED

PERCUSSIONDRILLRECORD

GNProJECT

SlEGRIDU

BEARING DIPCOLLAR

900

STARTEDLee1782

1

cJ

rJ

CJ

CJ

rJ

01ELEVATION TOTAL

DEPTH150FEEr

3

2

CORESIZE2

DRY

COMPLETEDIec

1782

FIIOM

TO

DESCRIPTION

SAMPLE

COlliE

COIlE

ASSAYS

NO

FIIOM

TO

LENGTHIlIECV

REMARKS

11111

CU

In

As

Au

n

n

nlR

010

Cisinq

n

n

It

2217

10

20

10

31

2

5

5

mH

2

5

nmm

l

2218

20

30

10

27

1

3

5

a

microsCOD

2219

30

40

10

25

1

3

5

l

tn

an

withwhitefe1dsoar

2220

40

50

10

29

2

3

5

i

1

0

n

1

50

60

10

42

3

3

5

1enh

0722260

70

10

51

1

4

5

n1

2223

70

80

10

20

1

4

5

ntyITSllQIlQlJ

n

n

ar01

22224

80

90

10

38

5

5

5

hnl

2222590

100

10

26

1

3

5

i

i

is

0

0

a

S

nur

enMre

100

I

n

10

62

6

3

5

1

7

11n

I

2n

0

43

2

3

5

InnR170

1

0

10

47

4

2

10

2222Q120

140

10

44

2

2

5

b

On

TAn

n

0

50

3

4

5

MLttFIlnk

7

CJ

Cl

I

I

cJ

L

J

CJ

1

CJ

cJ

l

1

r

1

CJ

C

I

J

I

cJ

CJ

C

I

CJ

1

SEtCOMININGCORPORATIONLIMITED

PERCUSSIONDRILLRECORD

OM

SAMrE

COIlE

COllE

ASSAYS

TO

DESCRIPTION

FROM

TO

REMARKS

NO

LENGTH1110

0

11I

Cu

Aa

As

Au

Ph

Zn

0

10

ANIE

TUFF

n

Tn

Tno

Tn

Tn

57

213

I1Ediun

fire

inedwithmitefelA

r

withmitefaldsoarlmncrvstal

Piecessorre

rusty

tTlssanolS

Dits

weakcazbanate

10

80

ANIESITEBllSALTFIlM

I

10

20

10

29

0

1

6

5

8

li3

finerined

daDqzey

basaltfl

witl1occasional2223320

30

10

33

0

1

6

5

10

81

olivire

tals

SOIlemite

faldsoarlaths

12234

30

40

10

250

1

2

10

5

750

382

weaktoncderate

interstitialcarlxmate

2235

40

50

10

137

0

9

10

5

570

178

12223650

60

10

51

0

1

9

5

70

79

80

90

ANDESITETUFF

I

n

n

n

n

85

173

mleareen

anCEsitetuffmiJed

withnTPV

basalt

20

0

00

10

I

o

22

liO

d

fDnnabve

22

1

0

90

10

13

0

2

7

5

II

107

mle

n

finearainedwitl1mitefeldsoarchips

tzacecvriteandchalOOPYrite

o

analrusty

8OOnschio

weakcaJxmate

interstitial

90

100

ANDESITEBASALTFLOW

on

nn

ln

n

l

17

98

ren

ahaniticflowas

nrevious

traceweakcarbonate

V

f

dZ

DRIUEDBY

MiitbFmk

SIGNED

STARTED

01ELEVATION TOTAL

DEPTH200FEET

3

2

CORESIZE2

INCHDRY

Dec

14

82

COMPLETEDDec16

82

HOLENo

SHEETNo

LOCATIONGN82

14

PIlOPEIlTY

1 L6400mS33

00mE

N

PlIDJFrfI

lmRTn11

BEARING DIPCOLLAR

900

CJ

C

c

rt

CJ

CJ

HOLENo

GN82

14

PROPERTY

SHEETNO

2

LOCATIONL6400ms33

00lllE

CJ

cJ

Cl

Cl

I

J

CJ

CI

CJ

SELCOMININGCORPORATIONLIMITED

PEReUSSIONDRILLRECORD

GNPROJECT

SUBGRIDU

cJ

L

J

CJ

J

CJ

01ELEVATION TOTAL

DEPTH200FEET

3

2

CORESIZE2

INCHDRY

STARTEDDec

14

82

COMPLETEDDec

16

82

BEARING DIPCOLLAR

900

0101

TO

SAMLE

CORE

CORE

ASSAYS

DESCRIPTION

FROM

TO

REMARKS

NO

LENGTHce

v

111111

Acr

AS

An

Pb

Zn

nn

2n

MIXEDBASALTFLOW

ANDESITETUFFFRAGS

22241100

liO

10

29

0

5

6

46

170

darkorev

basaltasor

gnL

unitmixed

0

11n

n

n

00

n

41

164

withpaleto

mediumqreen

andesitetuff

fracnnentsasinfOllowingunit

weaktomoderateinterstitial

carbonate

n

TAn

TUFF

on

TOn

10

T

n

n

23

138

Dalecreen

finegrained

10n

4n

n

0

on

175

199

stronqcarbonateinterstitial

occasionalfeldspar

crystalsinchios

tracepvrite

130140rusty

aossanouschios

151

40

170

ANDESITEBASALTFLOW

22245140

150

10

42

0

6

16

10

50

144

lasprevious10

80

22246150

160

10

4l

0

1

9

5

17

103

arevfine

arainedflow

22247160

170

10

67

18

35

10

147

173

occasionalbleachedandesitefraamPntsfrom

160170orobab1vreoresentinothebeoinnino

ofthe

underlyingunit

weakto

moderatecarbonatecontentthat

with

andesitefraaments

Dresent

traceto

euhedralpyritecrystals

7L

hA

MerrittFunk

0

ooooCJ

o00

L

J

l

LJ

evtullG

5

33

oomJ

PIPCOIvR

900

COpIETEO

Dec

6

82

STRTEP

Dec

4

82

SSIYS

flEtA

RKS

co

colE

SA

E

F

O

0

LE

HJf14

1lJC

ll

lb

In

oESCftlPtlON

0

0101

0

235

202

n

n

1

n

0

0

no

ll

UESrc

tJI1F

l

I

1JO

210

110

02249SO

90

10

250

20

stron

carbonate

intersti

tia

n

4

0

2

0

111

ale

reenfine

rainedcalcareous

tuff

2250

00

I

on

t

ssib

a

sedl

tllentasiltst

Onel

trace

euheoral

Iyrite

crystals

nn

n

gQs

n

n

n

n

n

n

l

n

O

n

02

0n

nO

1J

f

1

sG

ED

5

SEICO1I

GCORPOR

O

11I

EO

lJ

RcllSsrONORll

RECOROGR1D

3

EiEVI

TlOll

OT

pEpTZOO

FEJT

l

CORESIZE2

rNClltDRl

ao

1Y

evRIllG

PIPCOIvR

900

OlE

110

GNS2

14

stEET110

3

n

Rf

JO00

00000r

CJ

A

eoRING

3

0

PIP

COvR

90

OEC

3

82

CO

0

STARTEDIo5S

5

P

E

R

co

t

GOfte

l

PlO

TO

tENO

r

AU

O

RlyT1Oto

NO

C1

AS

O

TO

n

0

n

n

n

tt

L

on

n

n

0

bean

to

U

0

nn

n

0

n

n

0

n

Q

n

reducedto

2

andost

air

1

ieeS

a

L

forcedto

abandOn

n

n

L

n

T

retUrn

on

0

0

T

n

n

n

hOeat

80

n

n

on

8

0

4

225660

10

0

10

80

0

55

0

5

30

2251

n

S

O

n

0

oft

0

bl

71lj

SIGNED

o

SECOMlt

INGCORPORA

Ot

I1EO

PERCIlSSI0N

DR

RECORD

3

EII

TION

I

01I

pEPTt80

FEET

2

CORESItE

3

INCllOl1Y

cOtAPffED

pe

3

82

0

11

eoRING

o

PIP

CovR

90

HOENO

GN82

l5

StEET

NO1

I

ollIEaf

NerJitt

FuTk

CJ

cI HOLENO

SHEETNO

LOCATIONCJ

CJ

CJ

C

CJ

CJ

CJ

Cl

Cl

CJ

C

SELCOMININGCORPORATlONLIMITED

BEARING DIPCOLLAR

CJ

CJ

J

CJ

cJ

r

J

0ELEVATION TOTAL

DEPTH100FEET

3

2

CORESIZE3

INCHDRY

COMPLETEDDEC12

83

GNPROJECTSUBGRIDl

PERCUSSIONDRILLRECORD

LE

COPlE

COlliE

ASSAYS

FIIIOM

TO

DESCRIPTION

FIIOM

0

Rev

REMARKS

NO

LENGTHmm

Aa

As

Au

0

20

ANDESITETUFF

n

In

In

4

17

0

10

CaRing

paleareen

andwhitechioswith101rusty

In

n

1

n

0

1

chins fineqrained

stronacarbonateinterstitial

n

n

ANDESITEBASALTFLOW

n

n

In

1

7

mediumarevto

darkgrey

fineqrained

2226

0

4n

n

1

7

porphvritic

qreenmafics

6

4n

n

n

4R

1

6

moderateinterstitial

carbonate

50

100

ANDESITETUFFas

previous

6

n

n

n

EOB

n

7n

1

n

In

1

4

Maanetic

susceotibility

7n

on

n

11

0

20

0

0

c

q

s

on

00

1

n

7

7

20

50

0

3

c

a

s

226

on

nn

n

0

11

50

1000

0

c

q

s

j

j

Mo

1

1

GN8216

1 L5900mS33

00mE

PIlOPEIlTY

900

STARTEDDEC12

82

CJ

cJ

CJ

IJ

L

J

C

J

Ll

CJ

CJ

CJ

l

I

CJ

cJ

CJ

CJ

CJ

Ll

clCJ

SELCOMININGCORPORATIONLIMITED

403

2

PERCUSSIONDRILLRECORD

GNPROJECT

SUBGRIDt2

HOLENo

PROPERTY

GN

83

2

1 L3600mS4

50mW

ELEVATION TOTALDEPTH

SHEETNO

LOCATION

200Feet

BEARING DIPCOLLAR

CORESJZE

2

InchWet

STARTEDMay27

1983COMPLETEDMay27

1983

900

SAIolLE

CO

COIllE

ASSAYS

ftOM

TO

DESCRIPTION

I

OM

TO

REMARKS

NO

LENGTHIICC Cill

O

Cu

Ag

As

Au

0

20

O

B

20

100

DIORITEMONZONITE

2255820

30

10

39

0

3

63

15

Disseminatedpyritees

tirnated

mediumgrey

finegrainedoverall

59

30

40

10

47

0

4

53

5

2

overinterval20100feet

subhedralwhitefeldsparlathsina

medium60

40

50

10

40

0

3

61

5

greysiliceouslookinglookingfine

61

50

60

10

44

0

3

81

5

grinedgroundmass

Finecrystalline

62

60

70

10

4l

0

4

99

5

biotite

impartsa

brownishtingeunder

63

70

80

10

38

0

1

101

5

themicroscope

64

80

90

10

36

0

3

92

5

disseminatedpyrite

magnetitethroughout2256590

100

10

34

0

2

75

5

traceepidote

weakmoderate

interstitialcarbonateplus

occasionalcarbonatechip

Thisrockunit

possiby

magneticsusceptibilityismoderate0

4

representsa

contactor

border

to

0

5

as

explainedbythe

presenceof

phaseto

theunderlyingclean

1

disseminatedmagnetite

Monzonite

1

MerrittFunk

n

lAL

CJ

CJHOLENO

SHEETNo

LOCATIONCJ

rJ

cJ

J

L

J

CJ

CJ

CJ

l

I

CJ

C

CJ 03

2

GN83

2

cont

2 L3600rnS4

50mWPROPERTY

CJ

C1clrJ

SELCOMININGCORPORATION

LIMITED

PERCUSSIONDRILLRECORD

GNPROJECT

SUBGRlD12

BEARING DIPCOLLAR900

STARTEDMay27

1983COMPLETEDMay27

1983

CJ ELEVATION TOTALDEPTH

CORESIZE

200Feet

2

InchWet

TO

5

1E

COlliE

CORE

ASSAYS

1110101

DESCRIPTION

FiliON

TO

REMARKS

NO

LENGTH11

0

l

Er

CU

Ag

As

Au

100

200

MONZONITE

22566100

liO

10

32

0

1

77

5

Disserninatedpyrite

estimated

EOH

whiteto

lightgrey

feldsparrichchips

67

liO

120

10

31

0

1

53

5

2

overinterval100200

feet

Occasionaleuhedralwhitefeldspar

crystals68

120

130

10

27

0

4

30

5

inwhitetogrey

whitefeldspathicground

69

130

140

10

21

0

3

24

15

mass

22570140

150

10

26

0

3

30

5

1

mmbiotiteeuhedralto

subhedralcrystals71

150

160

10

24

0

1

32

5

Patchygreen

alterationassociatedwith

72

160

170

10

26

0

1

35

5

thebiotitecrystals

73

170

180

10

28

0

2

36

5

traceepidote

74

18Q

190

10

26

0

1

36

5

approxirnated15

ofchips

aresimilarto

22575190

200

10

29

0

1

50

5

ChipsfrompreviousDioriteinterval

Contactappears

gradationalbetween100

to

120 Magneticsusceptibility

100120feet

0

4

c

g

s

120200feet

0

1

c

g

s

weaktomoderatecarbonateinterstitial

andminor

carbonatechips

I

1

MerrittFunk

j

1

Cl

cJ HOLENO

SHEETNO

LOCATIONcJ

CJ

L

J

rl

CJ

l

J

CJ

cJCJ

cJ

CJ

CJ 03

2cJ

cJ

J

cJ

l

J

ELEVATION TOTALDEPTH200Feet

QiI83

3

1

L32HlOrrS

1251lnW

PIlOPEIlTY

SEleaMINING

CORPORATIONLIMITED

PERCUSSIONDRILLRECORD

GNPROJECT

SUaGRID13

BEARING DIPCOLLAR900

STARTEDMay28

CORESIZE

2

InchWet

1983COMPLETEDMay28

1983

FJIlOIoil

TO

DESCRIPTION

SAMPLE

COlliECOJllE

ASSAYS

OM

TO

REMARKS

NO

LEIIIClTH

OYCIIC

CU

Ag

As

Au

0

60

o

a

60

200

DIORITE lightgreyto

mediumgrey

colouredchips

22567

60

70

10

38

0

2

6

5

Finegrainedchipsize

generallyfinegrained

77

70

80

10

42

0

2

6

5

60to

120feete

occasionalcream

whiteeuhedralfeldspar78

80

90

10

49

0

4

7

10

crystalsin

greysiliceouslooking

79

90

100

10

39

0

1

7

5

Traceto

1

pyrite1oca11Ya

aphaniticgroundmass

80

100

liO

10

53

0

4

10

5

disseminatedmagnetite11

81

liO

120

10

55

0

3

li

5

magneticsusceptibility0

2

to

0

3

o

g

s

82

120

130

10

45

0

3

10

5

moderateinterstitial

carbonate

83

130

140

10

47

0

2

7

5

84

140

150

10

40

0

4

6

10

85

150

160

lOr

46

0

4

7

15

86

160

170

10

42

0

3

7

5

87

170

180

10

38

0

3

7

15

88

180

190

10

36

0

3

7

10

22589

190

200

10

36

0

2

9

5

1

A

AL

MerrittFunk

cJ

JHOLENo

SHEETNo

LOCATIONC

cJ

cJ

J

cJ

cl

cJ

cJ

CJ

CJ

cJ

SElCOMININGCORPORATION

LIMITED

PERCUSSIONDRILLRECORD

GNPROJECT

SUBGRID2

BEARING DIPCOLLAR900

STARTEDMay26

1983COMPLETEDMay27

1983

CJ

CJ

cJCJ

GN83

1

PIlOPEIlTY

1 L4000

1

00mW

CJ

CJ

AD3

2

ELEVATION TOTALDEPTH

CORESIZE

200Feet

2

InchWet

IlO

TO

DESCRIPTION

5AMLE

COIlE

COIlE

ASSAYS

IIOhl

TO

REMARKS

NO

LENGTHtcov lI

t

Cu

Ag

As

Au

0

10

O

B

22539

10

20

10

31

0

5

39

15

GOodchip

recovery

40

20

30

10

35

0

4

14

15

15

200

MONZONITE

41

30

40

10

31

0

4

12

15

Disseminatedpyriteis

found

EOH

chipsarelight

greyto

greygreenin

42

40

50

10

29

0

3

24

10

throughoutthe

following

colour

uniformthroughout

43

50

60

10

28

0

2

9

10

intervals

chipscnosistofeuhedralto

subhedral

44

60

70

10

30

0

4

11

5

10

30

1

romfeldsparcrystalsthat

varyfrom

45

70

80

10

26

0

4

10

5

60

170

creamwhite

bufftan

palegreygreen

46

80

90

10

I

32

0

5

14

10

lyingina

finegrained

greygreen

ground

47

90

100

10

30

0

5

15

10

mass

48

100

110

10

28

0

4

7

15

nondescriptgreenandblackcoloured

49

110

120

10

26

0

3

7

10

mafiasthatareveryfinegrained

50

120

130

10

44

0

4

12

5

pyritedisseminatedlocallythroughout

51

130

140

10

30

07

10

10

fromtracetoupto51

oversome10

foot

52

140

150

10

29

0

8

10

5

intervals

53

150

160

10

30

0

5

9

10

moderatecarbonatealterationthroughout54

160

170

10

31

0

5

20

5

entirehole

55

170

180

10

33

0

5

11

10

magneticsusceptibilityis

lowthroughout56

180

190

10

32

0

2

19

5

hole0

0

to

0

2

c

g

s

22557190

200

10

31

0

1

10

10

1

Merritt

Funk

1

I

faeU

oj

L

J

HOLE

No

SHEETNo

LOCATIONcJ

cl

CJ

CJ

CJ

cI

cJCJ

CJ

J

IJ

CJ

GN83

5

PROPERTY

1 L6400mS

31

50mE

SELCOMININGCORPORATIONLIMITED

PERCUSSIONDRILLRECORD

GNPROJECT

SUBGRIDU

BEARING DIPCOLLAR900

J

CJ

CJCJ

cJ

03

2

ELEVATION TOTALDEPTH

CORESIZE

STARTEDMay29

1983COMPLETEDMay3D

200Feet

2

InchWet

1983

OPo

0

DESCRIPTION

SMPlE

CO

E

COlliE

ASSAYS

NO

FIIOM

0

LENGTHIlKv

REMARKS

elle

Cu

Ag

As

Au

0

10

OIB

10

200

ANDESITETUFF

22501

10

20

10

46

0

6

3

15

EOH

mediumgreenandpalegreenish

grey

2

20

30

10

40

0

5

3

5

colouredchips

3

30

40

10

22

0

3

4

10

finegrainedgranulartextureexhibited

4

40

50

10

l2

0

3

3

15

bygreen

maficandwhitefeldspathic

5

50

60

10

l2

0

3

4

10

fragmentsandroundedsiliceousgrainsin

6

60

70

10

13

0

4

4

10

eachchip

7

70

80

10

14

0

3

4

10

someclayalteredfeldspar

8

80

90

10

20

0

8

5

5

stronginterstitialcarbonatethroughout

9

90

100

10

8

0

5

3

5

entirehole

22510100

liO

10

6

0

5

4

10

magneticsusceptibilityis

0

0

to

0

2

0

9

5

li

liO

l20

101

5

0

2

4

5

novisiblesulphides

l2

l20

130

10

71

1

8

4

10

13

130

140

10

260

5

1

5

5

14

140

150

10

276

5

1

4

5

15

150

160

10

150

2

5

5

5

16

160

170

10

101

1

8

5

5

17

170

180

10

46

0

9

4

5

18

180

190

10

34

0

4

5

1

10

22519190

200

10

39

0

4

5

5

Merritt

Funk

r

u

1

I

1i

I

J

o

o

ne

SECTION 5

COST STATEMENT

o

o

o

o

o

o

o

o

II

II

I

nI

U

o

c

u

oo

o

ontJ

1

o

o

o

o

o

o

o

o

o

o

c

o

o

COST STATEMENT

GN 1 8 RECORD 11125 1132 INCL 150 units

Road and Drill Site Preparationa November 1982

D8H Tractor bulldozer work

as per Invoice November 10 1982

Katchmar Construction Ltd

27 5 hrs @ lOO OOjhr 2 750 00

b May 1983

Moving charges for D6 Tractor

bulldozer as per Invoice

May 26 1983

R McMillin 167 75

c D6 Tractor bulldozer work

as per Invoice May 31 1983

McNeill Sons Logging Ltd

applying 80 of 1210 00 968 00

2 Percussion Drilling

a November December 1982

16 Percussion drill holes

totalling 2555 feet

GN 82 1 to GN 82 16

as per Merritt Funk Brothers

Drilling Co Ltd Invoices

dated

i December 2 1982

6153 75 2540 00

ii December 23 1982

13 197 00 315 00 12 882 00

3 613 75

I

L

oo

o

o

o

nrlJ

o

o

o

o

D

o

o

o

o

o

o

2

2 Percussion Drilling Con t

b May 1983

4 Percussion drill holes

totalling 800 feet

GN 83 1 to 3 and 5

as per Merritt Funk Brothers

Drilling Co Ltd Invoice

dated May 31 1983

10 109 88 1522 00

c Low bed service to move

drill between holes

as per R McMillin Invoice

May 29 1983

3 Field Supervisioni flagging in drill roads to drill sites

6 man days @ 138 75 day4 man days @ 204 00 day

ii supervision of drill road construction

and site preparation6 man days @ 138 75 day

iii drill supervision November 20 1982

December 17 1982 May 25 1983 May 30

34 man days @ 138 75

iv drying and splitting of percussion

chips packaging8 man days @ 138 75

2 man days @ 204 00

v preparing drill chip logboards logging drill holes

5 man days @ 138 75

2 man days @ 204 00

1983

8 587 88

77 25

832 50

816 00

832 50

4 717 50

832 50

408 00

555 00

408 00

IILJ

oo

o

o

o

o

o

o

o

o

o

oo

o

o

o

o

3

4 Accommodation

Cabin rental @ 485 00 month

1lmonths

5 Food

67 man days @ 22 50 day

6 TransportationVehicle operation41 days @ 25 00 dayLease charges @ 375 00 month

6 weeks @ 93 75 week

7 Field Supplies

Sample bags flagging tin

foil drying pans wooden

drill chip log boards

shipping charges

8 Geochemical AnalysisChemex Labs Ltd as per

Invoice 18214717

December 15 1982

60 samples @ 12 96 each

777 50

1 574 50

1 025 00

562 50

350 00

II

IIIII

777 60

r

I

n 4

n 8 Geochemical Analysis Con It

0Chemex Labs Ltd as per

Invoice 18214950

January 10 1983

n 96 samples @ 12 974 each 1 245 51

0 Chemex Labs Ltdil as per

Invoice Rl8310121

G January 31 1983

51 samples @ 12 96 each 660 96

c Chemex Labs Ltd as per

Invoice 18311616

l June 10 1983J19 samples @ 13 32 each 253 08

0Chemex Labs Ltd as per

r Invoice HI8311644IL June 10 1983

n 51 samples @ 13 32 each 679 32

IJ

I

Chemex Labs Ltd I

Qas per

IInvoice HI8312356

IJuly 13 1983 I0 20 samples @ 2 52 each 50 40 i

I

0 iIi

n 9 Report Compilation Reproduction Typing JIo J 3 man days @ 204 00 612 00

0 Reproduction costs typing of report 300 00

0

0

rLJ

00

10

L

011

L

CCD

G

0

0n

0

0nu

0

00

5

Reclamation Costs

Slash cleanup along drill site access

roads and at drill sites as per

Amex Exploration Services Ltd Invoice

July 30 1983

Cost per drill hole 7 000 00 30 holes

20 holes @ 233 33 per site 4 666 60

51 983 60

o

o

onLi 1

onL

CGC

DrJ

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o

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j

oFlLJ 3

n

o

COST STATEMENT

GN 1 8 RECORD H1125 1132 150 units

Grid Preparation to I P Standards

a November 1982

19 8 kms @ 137 34 km

as per Invoice November 15 1982

Amex Exploration Services Ltd 2 719 33

5 3 kms by Company personnel5 man days @ 204 00 day 1 020 20

b May 1983

6 0 kms @ 188 60

as per Invoice June 3 1983

Amex Exploration Services Ltd 1 131 60

Induced Polarization Surveysa November 1982

25 1 kms @ 829 25

as per Invoice January 1983

Peter E Walcott Associates Ltd 20 814 18

b June 1983

6 D kms @ 780 00 km

as per Invoice H3677

June 30 1983 Phoenix Geophysics Ltd 4 680 00I

II

IIII

iI

IIII

II

i

Field Supervision for Linccutting I P Surveys12 man days @ 204 00 day 2 448 00

o

rilJ

4

n

rLJ

5

rl

D 6

Cr

nnI 1

7

I

l

nlJ

D

o

c

cij

2

Accommodation

Cabin rental @ 485 00 month

2 weeks @ 485 00 2 242 50

Food

17 man days @ 22 50 day 382 50

TransportationVehicle Operation14 days @ 25 00 dayLease charges @ 375 00 month

2 weeks @ 375 00 2

350 00

187 50

Report Compilation Reproduction Typing

3 man days @ 204 00 day 612 00

400 00Reproduction costs typing of report

34 987 81

r

i IJ

lC

Cn

rLJ

cc

on

Qnnu

V IL

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o

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cn

AMEX EXPLORATION SERVICES LTDA A AB ABLETT

rrConfidential Work

BUS 376 0433

RES 376 7490

BOX 286

KAMLOOPS B C1714 CLIFFORD AVE

V2B 4C6

November 15 1982

Dr Hugh SquairGuichon Explorco Limited402 535 Thurlow Street

Vancouver B C

STATEMENT OF ACCOUNT

Re Field projects lac La Hache B C as listed below

CORE 1 3 4 mineral claims Grid layout and Soil Collections

44 8 km grid layout @ 144 50 km44 8 km soil collections @ 19 50 km

6473 60

873 60

7347 20 7347 20

CORE 5 CORE 6 and CORE 7 Fr Staking

Staking 41 units @ 45 86 unit 1880 26 1880 26

GN 4 7 Grid cleanout to IP standard

19 8 km grid cleanout @ 137 34 km 2719 33 2719 33

TY 9 Staking

Staking 6 units @ 89 17 unit 535 02 535 02

TY 1 Grid Layout cleanout to IP standardLINE IG

2 2 km grid IP standard @ 281 km 618 20 618 20

TY 2 Grid Layout c1eanout to IP standard

LINES G1 andIG2

2 6 km grid IP standard @ 281 km 730 60 730 60

Total requested 13830 61

Respectfully submitted

tt pre

9 E ior t ion Services Ltd

OVER 125 000 MINERAL CLAIMS AND UNITS STAKED FOR THE MINING INDUSTRYu n In r f l ICUr eIlDlE Ve I U CT VIP I I U IC IITTIIlr C IIRlI V t lf eTr

AMEX EXPLORATION SERVICES LTDA A AB ABLETT

BUS 376 0433RES 376 7490

Confidential Work

L

Cnu

1714 CLIFFORD AVE

V2B4Gf

BOX 286KAMLOOPS B C

June 3rd 1983

rLJ

Selco Inc

402 535 Thurlow Street

Vancouver B C

CrU

Attention Mr Dave Gamble

STATEMENT OF ACCOUNT

or

G

Re Grid Preparation on GN TY

Mineral Claims Lac La Hache

Clinton MininK Division

area

jl

GRID BREAKDOWN

TY 1 2 2 km @ 188 60 km

TV 5 1 0 km @ 188 60 km

TY n 9 4 8 km @ 188 60 km

TV 2 2 2 km @ 188 60 km

GN 1 3 0 km @ 188 60 km

GN 4 3 0 km @ 188 60 km

414 92

188 60

905 28

414 92

565 80

565 80

J ikl

TOTAL REQUESTED

on Respectfullv submitted

fl A A Ablett President

Amex Exoloration Services Ltd

nAmex Job Number 83 80

onL

AAA da

o

oOVER 125 000 MINERAL CLAIMS AND UNITS STAKED FOR THE MINING INDUSTRY

MANnnMnFR ANn rmfHEMICAL SURVEYS CLAIM STAKING LINE CUTTING SURVEYING ETC

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TERMS NET 15 DAYS INTEREST AT

2X Ell MONTH ON OVE OUE ACCOUNTS124r ANNUM

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CARlBOO LATH CO LTD TRUCKINGBOX 647 100 MILE HOUSE B C VOK 2EO

RADIO PHONEPHONE JS 7LOl

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McNeil Sons Logging Ltd

P O BOX 70 100 MILE HOUSE B C

phone 604 395 4604

iay 1 198

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3elco Incorporated7182 Blackwell Rd

i R 2

Kamloops B Cn2J

oco

To D 6 cat rental May 26 27

191 2 Hrs 60 00 1170 00

1 day P U Rental 40 00

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YUKON N W T BRITISH COLUMBIA AIUfmA USA

I

IeMEtatt Junk BlOt uu fbtdti129 COlnpan1ilnlted

Explol tlon Ind Dev lopm1nt

G fllll nl fllnll

c rl Funk

1 0 J H l1O Of H6I1333

Abordoon Ro d Lo NIcOl B CP O BOt 2077M IIt 8C VOK 280

DEe 6 982

Dccb8r 2 1 2

SILCO INCSuite I 4025 5 Thurlo Street

Vancouver I B C

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Attentions Dr H Squair

Dear Sire I4O DO v

Cg l5Re I ACCOUIlTS PAYABLE

The follo ing is our inY01c for Percussion Drilling on yourTi othy Lake Property during t pr1od of Nov 16 to Nov 27 1962

Hole NoTY6 82 5TY6 82 6eN 82 1eN 82 2eN 82ell 824

Dellth of OYertNrden Dellth of Hole Sbe of Hole later Su1l1lly

80 feet 200 t et 2 1nch truck

55 teet 200 teet 2 inch 400 w l

0 teet 120 feet 2 inch 100 1f120 feet 100 t et 2 inch 100 w

feet 165 teet 2 inch 00w

150 feet 200 teet 2 inch 00 1

Drilling ChArgea 2 965 feet 5 75 per foot 5663 75Water Supply Charsea water Une 1200 teet 10 00 per 100 120 00

water truck 1 hole 200 00 per 200 00

Moving Charges frail TY6 62 6 to eN 62 1 k4 hrs toW 2 hra 8S 00 per hour 170 00 V

Total Charges 6153 75AdYanees

TOIAL AIfUNlroB 6153 75

Thank youYours truly

rCary E Funk

Merritt Funk Brothers

Drilling CompanyLilli tad

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YUKON N W r 1J11111S11 COLUMIJIA ALlJ 1l1 US

cMElutt Junk 23toth a tiLing Company LimitEdExploration and Development

C fuunlllFunk

Cilly E FunJo

T lnllllon Jill 41J2 0 J7112J J

AbtJfd en Road LOWQf Nicola B C

P O Box 2077M rrlll B C VOK 2BOjfN 3 983

December 2 11932

C1 1 1

Ri r Ult

DrJcr 0

G rN310 1or rORr y ril

1

Attention Dr H Squair k r OOf

Dear Sirs 0 l We

Re ACCOUNTS PAYABLE

The foUowinlis 0 iorferculrnt1l1f Di ng on yourTimothy Lake Property during the period of lov 30 to Dac l 19821HOLE No Depth of O B Depth of Hol S1ze of lole dater SU1 lY OtherGN 92 5 90 feet 200 feet 2 I 00 I

II 1 2t hr move

GN 82 1 50 feet 200 feet 2 200 II I

N 82 7 20 feet 200 feet 2 100 w lGN 82 8 10 feet 180 feet 2 airCN 32 9 10 fest 180 feet 2 airGN 32 10 20 feet 190 feet 2 airGN 92 11 10 feet 190 feet 2 airGN 32 12 15 feet 110 feet 2 airGN 82 i6 0 feet 100 feet 3 air

GN 32 15 0 feet 120 feet s O 0 2 airGN 82 14 10 fset 200 feet 2 airGN 82 1 10 feet 150 feet 2 air

SliLCO INC

Suite 402

535 Thurlow Strset

Vancouver D C

V6E L2

1t hr move

hr move

1St hr move

6 hr move

Drilling Charges 2 1830 feet5 75 por foot 10522 50190 feet7 40 per foot 1 2 00

Water Supply Charges 2800 ft waterl10A @ HO OO 100 210 00Co

I

Moving Charges I 21 hrs total 11 hrs @ l5 00 por hr il062 O 1 J 5Total Charges h31 rOO I J

II IIAdvances

TOTAL AMOUNT DUE 17t9oOOI

C ITHANK YOU AND WISHING YOU AND YOURS

THE MERRIEST OF CHRISTMASES AND THE Yours truly

BEST OF THE NEW YEAR

eJ fl ICary E Funk

Merritt Funk Brothers

Drilling CompanyLimited

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YUKON NWr BRITISH COLUMBIA ALBERTA U S A

i eMEnLtt Junk BtOthE t1 rptL rng Company mLtEdExplorltlon nd Oevelopmonl

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a Eug n Funk

C lyE Fun

TlJhtphon 118 41 2 01 3112333

Aberdeen Road Lower NlcolB B CP O Bo 2077Merritt B C VOK 2BO

l y 31 t911i T r

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lay 25 mobil1 e1 to Lac Lo iac 5 hra ay 2 moved to 1 5st up

and Iul lf1 ay 27 111110i t moved to C r lr111od t 2

11lY 21 moved to C 1 2 hra drilled G J So from previoW iisitas

all ztole 1 a lionoj dua to lack vf dcce 31 ay29 waite1 for

lowbad and moved to 1 5 1 hl6 total I fvJY JO lrilled CIl I l Ve l to

irll13d moved from lalt sl o r I 1y 3t 1oM nl oi f

I i t h 3or O

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DRTI LING G IARCS 1000 f e I 7 fl psr foot ll O

M03ILPATION Q uaG J tepat to first site 2 25DiMOSILI ATIO 1 CilAHGtI 3 last 81 to to depot

f

r 5I W G iA G 2 to 2 blurs 2 2 asp97 75 l n

GN l to GN 5 3 hours 3 2 f 97 75 50Toto1 Chac es Hl1 9 n

J lvance5 ttTOTAA OJJiT DlJ 10109 33

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1tn y IYours truly

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lllnk

iordtt Funk l3rotlErl

Dr1l1ing 00 Ltd

AMEX EXPLORATION SERVICES LTDA It AI AILETT Conridcnllal Wort

i

BUS 3760433

RES 376 7490 1714 CLIFFORD AVE

V2B4G6

BOX 286

KAMLOOPS l C

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July 30 1983

Selco Inc

402 535 Thurlow Street

Vancouver B C

Attention Mr Dave Gamble

STATEMENT OF ACCOUNT

oRe Slash clean up along drill site access roads

Lac La Hache Area Clint ion Minin Division

o Amex Feel

IiI

10 kilometers @ 700 00 per kilometer 7000 00

total requested 7000 00

Respectfully lubmitted

Ameresident

oration Services Ltd i

1

I

I

1

Amex Job No 83 81

OVER 125 000 MINERAL CLAIMS AND UNITS STAKED FOR THE MINING INDUSTRYnnUITI R AMn m nrIlFMIr AI IJRVrY 1 AIM RTAKINr UNF CUTTING SlJRVEYING ETCfJ

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PHOENIX Geophysics Limited

200 YORKlANO alVO WIl I OWllAl I ONT ARID rANAOA M Jill lflEPHONE 4161 4916350r I 06 986856

Cab PHEXCO TORONTO

INVOICE

INVOICE No 3677DATE June 3D 1983

Selco Mining Corp Ltd55 University AvenueSui te 1700Toronto OntarioM5J 2f7

OUL J 198

REFERENCE Geophysical Survey Contract PV 1405IP and Resistivity Survey Lac La Hache B C

J Marsh P Gardner G Richardson

June B 1983 to June 19 1983

CREW

PERIOD

14 35 l klll 780 0011 km

One Operating Day SSO OO day

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C ll 193 0fz Mr

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NQAl Ii VANCOUVE R B C

CANADA VI 1 2Cl

ANALYTICAL CHEMISTS GEOCHEMISTS

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SELCG MINING CORPORATION LTD

REGISTERED ASSAYERS

IUfPIIUNI IOU4 9U4 0221

1 EL X 043 2597

IInvoice N 18214717

o DEe 1 982 DateP O

Project

liJ OEC JNONE

10145

STE 402 535 ThURLCW STR ETVANCOUVER B C

V6E 3L2

O n o fnr onalytl ol nLk reportea on

Analystld for

011ant ity cIHla de sc ript lOA120 002 Cu pnm

006 Ag pprn

013 AS ppm

100 Au FA AA OPD

cer U f I c tls LJR 1471 7 nnl t L1llLl

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o II 90 1428 00

o Sawple preparation and othtlr ch rJe

120 205 Rock geochem RING 2 50 300 00

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TOTAL

01 scount 10 l

S 1128 00S 172 80

Please pay this amount S 1555 20

ORMS NET 30 DAYS5 per month 118 per annum charged on overdue dccounts

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ANALYTICAL CHEMISTS GEOCHEMISTS

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SELCO MINING CORPORATIDN LTO

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CANADA V7J 2Cl

LLtPHONF 1604 984 0221

REGISTERED ASSAYERS I Ll x 043 52 91I

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CHEMEX LABS LTO

Invoice N 18214950

STE 402 535 THURLOW STREET

VANCOUVER B CV 6 E 3 L 2 1fN

985

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10 JAN 83

NONE

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repo teCl on s t ifJe3 A8214950 001

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11 90 111B 60

2 002 Cu

005 Zn

006 Ag013 AS

100 Au 12 65 25 30

ppm

pprn

pprn

pprnppbFA AA

Sawple preparation and other charges

96 205 Rock geochern RING 2 50 24C 00V

TOTAL S 1383 90D scolJnt 10 t S 138 39

Please pay this a ount S 1245 51

NET 30 DAYS

per month 18 t per annum charged on overdue ccounts

00TE GCI lSnECE1i

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ANALYTICAL CHEMISTS GEOCHEMISTS REGISTEREO ASSAYERS HIIX 0401 97

u n U i O I E JJSELCO MINING CORPORATION LTD Invoice 18310121

STE 402 535 THURLOW STREETVANCOUVER B CVbE 3L2

CJlVOi e for analvtlcal wOrJL UlllQLt ed on

Analysed for

code dAscr iJl1LQD002 Cu ppmOOb Ag ppm013 AS ppm

100 Au FA AA ppb

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Project

3l JAN 83

NONE10145

cer tif i cateLsl A83 10lllllOl ill lO2

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11 90 bOb 90

Sample preparation and other charges

51 205 Rock geochem RING

00

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2 50 127 50

TDTAL S 734 40DI scount 10 t 73 44

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DATE GOODS CEB9

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TELL PHONE 16C 904 0

TELEX 043 525 1

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SELCQ KI INC COPPC ATION LTC

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109 20

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PRICES OK

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INVOICE N 18214717DATE 15 DEC 82P O H NONE10145

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STS 402 535 THURLO STREETVf NUlUVtR 5 CV E 3L 2

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J8scription codenntz 04 1 za5

22042 205

22043 20522044 20522045 20522046 205

22047 20522043 2 5

22049 20522050 20522051 20522052 20522053 20522C54 2022055 20522056 205

22057 20522058 20522059 20522060 20522061 20522062 20522063 205

22004 20522065 20522006 20522067 20522068 205

22069 205

22070 203

22071 205

22072 20

22073 205

2 074 20522075 20

22076 20522077 20522078 2052 079 0522000 205

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CANAUlAN TESllNAssociATION

IEC 91

CC SELCO KAMLOOPScu A A S

ppm ppm ppm29 l 5

6 0 2 4

5 0 1 4

5 0 1 35 0 1 3

36 0 1 3

40 0 1 345 0 1 3

48 0 1 4

45 0 1 6

35 0 2 6

35 0 1 933 0 1 6

37 0 1 9

35 0 2 9

51 O I 1254 0 3 7

60 0 1 671 0 1 6

53 0 1 6

59 0 2 4q76 0 1 3552 01 4

51 O I 43

32 JI 43

55 0 1 3845 001 46

38 0 3 3960 0 1 63

57 0 1 10

64 0 1 1452 0 1 16

4d 0 1 16

46 0 1 1643 0 1 16

53 0 1 16

46 0 1 16

63 0 1 1461 0 1 16

55 0 1 25

212 BROOKSBANK AVE

NORTH VANCOUVER B C

CANADA V7 J 2C1

Au FA AA

ppb5

5

5

555

5

5

55

5

53

5

55

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5

5

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5

55

55

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Certified hy

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CHEMEX LABS LTD

STc 402 535 THURLOVAlCO JV R 3 C

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ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

r J J A T A LY 1SELCO lNING CCRPO AT N LTJ

Ol SIACKI

Prepcode

205205

205

205205

205

205205

205

205205

205

205205

205205205

205205

205

205

205

205

205

205205

205

205205

205

l05205

205

205205

205205205205

205

STKEt T

ec 3ELClCu

ppm

6943

48

5365

64

8057

61

27

31

27

2729

71160

80

53

7053

7643

50

49

180104

125

114121

123

109102

135270

141

139liB220157130

12 BROOKSBANK AVE

NORTH VANCOUVER B CCANADA V7J 201

TELEPHONE 604 96 0221

TELEX 043 52597

CERT

INVOICEDATEP o

10145

A8214717 0031821471715 C C 82

lOJElEe 1 9S

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49ppmo I0 1

0 1

0 1

0 1

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0 1

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ATTN GEORGE

fi samTe

descr iption2206122082

22083

2208

22085

22036

2208722088

22069

2209022091

22092

2209322094

220952209622097

2 09822099

22 100

2210122102

22103

221042210522 I06

22107

2210822109

221102211122112

22113

2211422115

22116221172211822119

22120

o MEMBERCANADIAN TESTING

ASSOC1ATION

AS Au FA AA

PpfTl ppb22 516 5

12 20

L 4 5

II 5

19 5

23 5L 2 5

L I 5

6 5

5 5

4 5

4 55 5

6 5

10 10II 5

L L 5

12 1014 5

12 10II 5

II 5

12 10

L 4 56 5

6 5

6 55 5

5 5

4 55 5

6 5

6 56 56 10

5 5

5 5

5 5

5 5

lC rtifiod by

ILJ CHEMEX LABS LTD 212 BROOKSBANK AVE

NORH VANCOUVER B CCANADA V7 J 2C 1

U 1 ELIoPHONE 604 984 0221

ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS TELEX 043 S2597

0 1 Eii i FIe A T EU O F A LY S IS

TO SHCO lINING CCRPORATION LTD CERT H A8214950 QOl

IC INVOICE II 18214950STE 402 535 THURLOW STREET OAH 10 JAN B3 IVANCOUVER B C P O I NONEV6E 3L2 p H0I

o GAM8LE lCAMLOOPS 1

IjSal1 p Ie Prep Cu Zn Ag AS Au FA AA

L description code ppm pprn pprn pprn ppb22121 205 115 0 1 9 1022122 205 49 0 3 7 10

II 22123 205 55 0 1 9 5J 22124 205 12 0 1 11 5

22125 205 61 0 1 10 5

0 22126 205 57 0 1 11 1022121 205 35 0 1 9 1522128 205 61 0 1 9 5

022129 205 46 0 1 10 10

22130 205 18 0 1 10 1522131 205 83 0 1 5 1022132 205 54 0 1 5 15

n 22133 205 49 0 1 10 5L 22134 205 112 0 1 11 10

22135 205 125 0 1 20 10

n 22136 205 192 0 1 15 5

J 22131 205 112 0 1 19 10

22138 205 51 0 1 11 10

G22139 205 45 0 1 61 1022140 205 55 0 1 61 10

J 22141 205 14 0 1 27 522142 205 19 0 1 32 5

n 22143 205 19 0 1 32 10I 22144 205 83 0 1 55 5

22145 205 80 0 1 33 5

n 22146 205 15 0 1 29 10

L1 22141 205 82 o 1 19 522148 205 15 0 1 17 10

n22149 205 12 0 1 25 522150 205 10 0 1 27 10

d 22151 205 55 o 1 32 522152 205 45 0 1 39 5

0 22153 205 10 0 1 30 522154 205 80 0 1 45 5

22155 205 84 0 1 45 5

022156 205 42 o 1 25 522151 205 31 0 1 24 5

22158 205 39 0 1 12 10

022159 205 41 o 1 16 5221 60 205 45 0 1 11 15

0 MEMBER Certified byCA NADIAN TESTING

ASSOCIATION

CHEMEX LABS LTD 212 BROOKSBANK AVE

NORTH VANCOUVER B C

0CANADA V7J 2Cl

TELEPHONE 6Q4 98 0221ANALmCAL CHEMISTS GEOCHEMISTS REGISTERED ASSAVERS TELEX 0 3 52597

0 rH n

uQ1 IFICA E F NALYSISJ hTO S EL CO I INING CORPORATION LTD CERT N AB214950 002

n INVOICE N 18214950

LJ STE 402 535 THURLOW STREET DATE 10 JAN 83VANCOUVfR B C P O N NONE

V6E 312JJ

0 j 1CC D GAMBLE KAMLCOPS

Sample Prep Cu In Ag AS Au FA AA

I descr I pt ion code ppm oom ol2Jr pom opbC 22161 205 43 0 1 9 5

22162 205 17 0 1 7 10

0 22163 205 57 0 1 14 522164 205 17 0 1 11 522165 205 24 0 1 14 5

022166 205 25 0 1 14 522167 205 26 0 1 12 5

2216B 205 26 o 1 11 5

22169 205 26 0 1 15 5

0 22170 205 24 0 1 14 522171 205 56 0 1 11 522172 205 27 01 10 10

022173 205 29 0 1 43 1022174 205 2B 0 1 27 1022175 205 2B 0 1 50 10

n22176 205 33 0 1 22 1022177 205 55 0 1 43 5

Li 2217B 205 51 0 1 39 522179 205 30 O 1 30 5

r 22 180 205 29 0 1 11 1022181 205 31 0 1 10 10

221B2 205 32 01 11 10

n22183 205 29 0 1 11 5

J 22184 205 30 0 1 12 5

22185 205 29 0 1 15 5

Q22186 205 32 O 1 12 10

22187 205 29 0 1 14 1522188 205 27 0 1 16 1522189 205 51 2 6 17 10

0 22190 205 28 2 0 50 1022191 205 32 5 3 20 1022192 205 30 4 1 14 5

022193 205 33 1 9 12 522194 205 52 3 0 12 5

2 2 1 5 205 61 0 2 7 5

22196 205 59 0 4 6 15

L 22197 205 59 01 7 522118 205 53 0 2 9 5

iO22199 205 18 1 8 6 5

22200 205 27 0 2 9 10

C fJCertified byMEMIER

CANADIAN TESTINGASSOCIATION

ANALYTICAL CHEMISTS GEOCHEMISTS REGISTERED ASSAYERS

IL R T F C E NA LY S S I fTO SELCO NING CORPORATION LTD

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CHEMEX LABS LTO212 BROOKSBANK I

NORTH VANCOUVER

CANADA V7 J

TELEPHONE 604 984

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A8214950

1821495010 JAN 83

NONESTE 402 535 THURLCW

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1

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CERT H

INVOICE II

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Sampledescription

22201

22202222032220422205

2220622201

2220822209

2221022211

2221222213

2221422215

22216

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KAMLOOPS

Prep Cu

code ppm

205 21

205 19

205 42

205 62

205 44

205 40

205 25

205 26205 38

205 44

205 57

205 17205 27

205 54

205 50

205 54

Ag AS Au FA AA

pprr DPm ppb0 1 9 120

0 2 3 45

0 8 3 5

0 1 6 10

0 1 14 10

0 2 25 5

5 0 10 55

2 5 9 10

1 9 11 25

6 0 12 152 5 10 55 I7 5 6 15 I

2 C 14 15 I

1 0 10 10

0 1 15 10

0 5 12 5

In

ppm

90

84

MEMBER

CANADIAN TESTINGASSOOATION

Certified by

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SECTION 7

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CERTIFICATE OF AUTHOR

I George Owsiacki of 631 Lyne Road Kamloops British Columbia

hereby certify that

1 I am a geologist residing at the above address

2 I am a graduate of Queen s University Kingston Ontario

with an Honours B Sc degree in Geology 1981

3 I have practised my profession for more than 1 year full

time and for 4 summer field seasons

4 I co supervised the field activities described herein

5 I hold no interest direct or indirect in the GN 1 8

Claim Group which is the subject of this report

Respectfully submitted

G Owsiacki

Field Geologist

Kamloops B C

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CERTIFICATE OF AUTHOR

I Alan Wynne of 8573 Eboy Terrace Sidney British Columbia

hereby certify that

1 I am a geophysicist residing at the above address

nu 2 I am a graduate of the University of British Columbia

with a B Sc in Geology Geophysics 1976

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3 I have practised my profession for more than seven years

4 I supervised and interpreted the geophysical work described

herein

5 I hold no interest direct or indirect in the claims

which are the subject of this report

Respectfully submitted

IlJ

A Wynne

Geophysicist

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Vancouver B C

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CERTIFICATE OF AUTHOR

I Dave Gamble of 7182 Blackwell Road Kamloops British Columbia

hereby certify that

1 I am a geologist residing at the above address

2 I am a graduate of the University of Ottawa with an

Honours B Sc degree in Geology 1973 and have completed

two years graduate studies leading to a M Sc at

Laurentian University

3 I have practised my profession for more than 7 years

4 I supervised the survey work on the GN 1 8 Claims and

interpreted the results of the survey described herein

5 I hold no interest direct or indirect in the GN 1 8

Claim Group which is the subject of this report

Respectfully submitted

A P D Gamble

Project Geologist

September 1983

Kamloops B C