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GEOLOGICAL REPORT ON THE PERRIER BIG MAC

MASCOT JULIUS CAESAR AND SILVER HAWK CLAIMS

I1LJ r1J1N T S 82F 6W

490N 1170E

by Roy V Beavon B Sc Ph D

for

C ABER RESOURCES LTD

Vancouver B C 1st August 1982

MINERAL RESOL RCEs E RANCH

ASSESsttNT REPORT

TABLE o F CONTENTS

I INTRODUCTION

II PROPERTY

III HISTORY

IV GEOLOGY

1 Stratigraphyi Metasedimentary Rocks

ii Metavolcanic Rocks

iii Intrusive Rocks

2 Structure

i Foliation

ii Folding and Lineation

iii Faulting

3 Mineralization

V

VI

VII

VIII

IX

CONCLUSIONS AND RECOMMENDATIONS

BUDGET ESTIMATE

STATEMENT OF QUALIFICATIONS

COST STATEMENT

ILLUSTRATIONS

Map 1 Location of Property

Map 2 Claim Map

Map 3 Geological Map 1 540

Map 4 Plan and Section Perrier Mine 1932

PAGE NO

1

1

2

4

4

5

5

7

9

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14

15

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17

oI INTRODUCTION

The work described in this report was executed 5

to 7 km south of the city of Nelson B C in the drainagesof Cottonwood and Selous Creeks Cottonwood Creek runs

northward alongside the paved Highway No 6 and parallelto the Burlington Northern Railway Map 1 Access is

therefore on foot and by 2 wheel drive vehicle The mineral

showings may be reached by 4 wheel drive vehicles along old

logging roads that are currently in need of maintenance so

that access for this work was on foot Elevations of the

mapped area range from 3100 to 5300 ft

II PROPERTY

The property consists of thirteen claims which

include three reverted Crown Grants eight two post claims

one fraction and one reduced modified grid claim consistingof twelve units Map 2 Table 1 The writer checked legaland initial post locations for the Silver Hawk Big Mac and

Perrier Claims on the ground and these are shown on the

geological map Map 3 The precise location of the reverted

Crown Grants Julius Caesar and Mascot is doubtful and would

require tracing back to the original surveys

The thirteen claims shown in Table 1 are legallyand beneficially owned by Mr C pitman and Associates of

Nelson B C

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ABER RESOURCES LTD

BEAVON CONSUlJING LTD

SELOUS CREEK PROPERTYNELSON M D B C

LOCATION MAP

200 BRITISH COLUMBIA400

100 200M LES SCALE I 120mil s FEB 1982 FIG I

CTABLE 1

CLAIM SCHEDULE

CLAIM LOCA TlON NO EXPIRY DA TE

Lizzie C 1852 July 3 1983

Mascot 1807 June 30 1983

Julius Caesar 1808 June 30 1983

Silver Hawk 1899 September 12 1982

Perrier 1 2033 December 1 1982

Perrier 2 2034 December 1 1982

Perrier 3 2035 December 1 1982

Perrier 4 2036 December 1 1982

Big Mac 1 2296 June 1 1983

Big Mac 2 2297 June 1 1983

Big Mac 3 2298 June 1 1983

Big Mac 4 2299 June 1 1983

Big Mac Fraction 2300 June 1 1983

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III HISTORY

There are few records of the early history of the

claim area The Perrier gold prospect was staked in 1910

and produced 2 804 tons of between 1 01 and 0 62 oz ton Au

in the early nineteen thirties Cockfield 1936 An under

ground plan by O Grady 1932 is enclosed Map 4 No records

of the other three reverted Crown Grants could be found

In 1960 Sheep Creek Gold Mines held an option on

the Big Mac claims and drilled five diamond drill holes for

a total footage of 791 feet beneath two lead zinc silver

showings shown as the North and South Showings on Map 2

Three holes were drilled on the South Showing and two holes

were drilled under the North Showing All the holes were drilled

eastwards but their precise location is not known Mr J

McIntosh of Delta C kindly supplied information from drill

logs in his possession that had low assay values in lead zinc

and silver See also B C M M Rept 1960

In 1970 the Big Mac claims were restaked as Silver

and Sam claims owned by Cop Mac Mines Ltd Geophysicalwork was done on the North and South showings including

electromagnetic VLF and JEM surveys which were found to be

ineffective in discrimination of mineralized ground In

addition a property wide geochemical survey was done at 400

ft line spacings and samples taken every 100 ft Copperlead and zinc were determined and several anomalies were

found and trenched without encouragement Assessment Report

3091

3

oA geological report was submitted to Warrior

Resources Ltd in 1978 on the John Claims restaked on the

Silver and Sam claims There are references to trenchingin 1971 and the North and South showings are documented

with assay plans by Tough and Taylor The geology was

outlined briefly and a detailed geological survey was

recommended B C Assessment Report 7377 Subsequentlyin 1979 the southern portion of the property was surveyedgeochemically for lead zinc and gold Anomalous goldvalues were found over gravel deposits west of the Perrier

prospect Assessment Report 3091

o

The purpose of present report is to document de

tailed mapping as recommended in Assessment Report 7377

and this was done in order to study the geological controls

of the base metal mineralization to study the gold occurrences

and to make recommendations for future work if warranted

Unfortunately the underground workings are in poor condition

and would require extensive work before they could be safelyentered

o

An area of 5 sq km within and adjoining the

claims was mapped geologically at a scale of 1 6720 using1980 air photographs courtesy of Crestbrook Logging Co of

Cranbrook B C These photographs which were blown up from

1 12000 to 1 6000 enabled precise definition of outcrop and

talus derived from outcrop together with old roads and old

trenches Traverses between known points were scaled usingtopo chain compass traverses A total of six working dayswere spent on the ground which contains at least six old

prospects All of the claims were covered with the exceptionof the less accessible parts of the Silver Hawk Claim where

line cutting will be necessary

o

o

4

IV GEOLOGY

The general geology of the Nelson and Yrnir areas

is well known from reports by Leroy 1912 Drysdale 1917

Cockfield 1936 McAllister 1951 and Little 1960

Mesozoic sedimentary and volcanic rocks of the Ymir and

Rossland Formations are deformed and intruded by the Nelson

granites The property under discussion is located to the

west of the main body of granitic rocks and is surrounded

by satellitic intrusions All the supracrustal rocks have

been affected by lower amphibolite grade of regional meta

morphism with the imposition of a variably developed folia

tion The results of the mapping are included in Map 3

1 Stratigraphy

The stratigraphy of ancient volcanic areas is often

difficult to establish due to the lack of abundant faunas to

the presence of faulting alteration and metamorphism and

to volcanic facies that do not behave in a layer cake

fashion The Nelson area is no exception but the writer

has attempted to break down the succession as far as is

practicable

By far the greater area of the claims is underlain

by metavolcanic rocks of the Rossland Formation but the

western and north western parts of the property contain meta

sedimentary rocks classified by Little 1960 as Unit B of

indeterminate age

o

o

o

5

i Metasedimentary Rocks

The metasedimentary rocks consist of we bedded

argi lites and si ty grits that contain poorly developedgraded bedding The fine grained shaly interbeds contain

abundant 15 disseminated pyrite Although graded beddingsuggests that these metasediments are older than the Rossland

Formation it is more likely that they are contemporaneouswith the volcanism since intercalations of similar rustysediments occur within the Rossland Formation near its

northwestern contact with the metasedimentary rocks

Near their northwestern contact with the Nelson

batholith the metasediments are transformed into schistose

grits and fine grained pelitic quartzites with increasingbiotite con tent

Southwest of Cottonwood Creek the metasediments

are clearly intercalated with schistose and massive green

stone lithologies Accordingly the Unit B of Little 1960

is here recognized as the Ymir Rossland transition rather

than a separate unit of indeterminate age

ii Metavolcanic Rocks

The bu k of the claims are underlain by andesitic

flow rocks cognate tuffaceous biotite schists and thin

intercalations of limestone and rusty argillite Proceedingfrom northwest to southeast across the claims the followingascending sequence of lithologies has been recognized Table 2

6

oTable 2 Subdivision of the basal Rossland Formation

d

c

b

a

Lithology

Biotite tuffites

Coarse porphyroblastic flows

Pillowed flows

Flow breccias pillow breccias

Approx thickness in m

240

550

30

425

Note that minor sedimentary and tuffaceous units are included

in all four subdivisions

a The flow breccias are typical hyaloclasticdeposits that are best observed on weathered surfaces Theyare usually moderately to well foliated greenstones containingflattened angular and ellipsoidal clasts in a similar green

matrix Phenocrysts are not common and since the foliation

is trans cted by hornblendic porphyroblasts these are

suspected to be of metamorphic origin Where present the

hornblende is often rounded as though replacing primaryamygdules

The flow breccias where poorly foliated contain

fragments 5 cm in diameter Minor differences in clast

composition can be attributed to subaqueous alteration rather

than accidental inclusions Pillow breccias contain flatten

ed ellipsoidal clasts up to 30 cm in length containing chill

ed margins reminiscent of pillow rims Note that the North

Showing occurs within the flow breccia horizon

o

b The true pillow lavas have an exposed thickness

of only 30 m They occur in massive jointed outcropsreminiscent of intrusive rocks pillow rims are well developedeven in unweathered situations but no top determinations

could be made The inter pillow areas are occupied by triang1alarareas of recrystallized chert

7

oc The pillowed zone is overlain to the south

east by 500 m of massive coarsely porphyritic porphyroblasticamphibolites that have been previously regarded as augiteporphyries Foliation is weakly developed and flow structures

are usually absent in this subdivision The coarsest

amphibolites reach gabbroic proportions immediately south

east of the South Showing

o

d The easternmost and uppermost member of the

volcanic succession consists of 250 m of medium to well

foliated biotitic tuffites These are often well banded with

sedimentary layering parallel to schistosity This member of

the Rossland Formation can be traced as far south as the

Perrier gold prospect where it hosts a narrow strattform

showing of base metals including magnetite Lucky Boyadit The subdivision of the volcanic rocks indicates that

three stratiform showings of base metals North South and

Lucky Boy occur at three different stratigraphic horizons

as defined by the volcanic facies of the Rossland Formation

iii Intrusive Rocks and Metamorphism

Major intrusive rocks of the Nelson Batholith

outcrop to the west and northwest of the property and fingerinto the claims on the west side of the Cottonwood ValleyThese intrusions consist of porphyritic biotite granite near

the western margin of the Silver Hawk Claim and equigranularbiotite granite on the Julius Caesar Claim

U

Only one normal contact was observed in a railwaycutting north of the northernmost railroad trestle This

contact appears concordant with quartzitic argillites but

when mapped northwards its behaviour is obliquely discordant

in relation to the wall rocks The south westernmost granite

8

ooccurrence is interpreted as a fault wedge but no contacts

are exposed So far as the writer is aware no granite was

recorded previously on the Mascot and Julius Caesar claims

Minor intrusive rocks were observed at several

localities notably feldspar porphyry basaltic feldsparporphyry and lamprophyre The feldspar porphyries are

common southeast of Cottonwood Creek where they occur as

northward striking transgressive sheets that dip to the east

at 50 degrees They vary in texture from a crowded feldsparporphyry 70 phenocrysts to virtually non porphyriticfelsite or rhyolite No flow structures were observed but

the marginal porphyries are often brecciated indicatingnear surface emplacement Locally these intrusions are

foliated but generally speaking they tend to be massive

o A narrow 1 m dike of crowded feldspar porphyryoccurs at the North Showing where it forms the footwall to

mineralized calcareous biotite tuffite horizon

Biotite lamprophyres occur in sill like narrow

intrusions at several localities As in the case of the

metavolcanic rocks the lamprophyres are massive to weaklyfoliated They are usually fine grained with 3 rom flecks of

biotite and an altered chloritized mafic phenocrysts set

in a dark green to black fine grained matrix In all cases

observed the contacts dip parallel to the bedding and folia

tion of the wall rocks The age of these ultramafic minor

intrusives is uncertain but they have not been observed

cutting any of the other intrusive rocks

o

9

oBasaltic porphyries were observed only in two

trenches one near the North Showing and one north of the

Lizzie e shaft Float samples near the former localitycontain xenoliths of feldspar porphyry A Tertiary age is

indicated by the fresh appearance and lack of foliation of

the basaltic porphyries

2 Structure

o

The most widely developed structure of the area

mapped is a steeply dipping foliation that varies in strike

from northeast in the northern two thirds of the claims to

southeast in the south Attendant folding is difficult to

recognize aside from small scale folds where foliation is

difficult to recognize The importance of faulting has not

been emphasized in previous reports but there is topo

graphic and quartz vein evidence of northwest to southeast

faults in several parts of the property

i Foliation

Foliation is developed with variable intensitythroughout the map area and wherever observed in conjunctionwith sedimentary bedding is usually a parallel structure

This implicates that isoclinal folds may be present but no

repitition of the volcanic horizons occuring across the strike

is evident from the mapping

Because foliation is absent in some members of the

andesitic volcanic rocks and well developed in others the

presence or absence of foliation in certain rock types is of

little value in age diagnoses

o

10

oThe variation in strike of the foliation from

northeast in the north to southeast in the south Map 3

is accompanied by a shallowing of the westward dip of

foliation in the intervening area notably west of Cottonwood

Creek This broad warping is clearly due to a mild late

folding of the foliation accompanied by a similar variation

in the plunge of b lineations

ii Folding

o

As stated above folding that accompanied to

formation of the foliation has not been recognized in the

claim area Minor folds which plunge south eastward have

been observed in argillites near the Lizzie C and in limyhorizons of both North and South showings Map 3 The plungeof the minor folds is similar to the southwestward plungeof the b lineations which are common in the foliated meta

volcanic horizons Together with the fact that most of the

granitic contacts are semi concordant with the supracrustalrocks this observation suggests that the intersection of the

granite with the mineralized horizons will be quite deep and

should not interfere with any drilling

iii Faulting

The structure of the claims is dominated by NW to SE

faulting that appears to control the direction of Cottonwood

Creek The evidence for this comes partly from an undergroundplan Map of the Perrier prospect by O Grady 1932 part y

from the distribution of rock types west of the valley Map 3

from physiographic evidence on air photos and from quartzvein occurrences throughout the claims

o

1

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11

JThe physiographic evidence comes from sudden

changes in the hillside slopes to the north of Selous Creek

One of those faults may contain a surficial deposit of

travertine seen in float and coatings on outcrops At one

stage during mapping it was thought that the North showingand South showing were either separated by the NW faults or

repeated across the strike by folding but the mapping in

dicates that they are probably located at two different

horizons within the volcanic rocks and only indirectlyassociated with the northwest faults

o

Judging from O Grady s map of the Perrier Map 4

the NW striking faults dip steeply to the NE but they may

be vertical in other cases The throw of the NW fault at

the Perrier is down towards the SW so that this fault can

be classed as a high angle thrust fault In addition to

the Northwest trending faults a west north west strikingfault is shown on O Gray s map but none of these were

identifiable in the surface mapping A northeast strikingfault of unknown throw passes through the Lizzie C shaft

and is identified by fault gouge in one of the trenches

3 Mineralization

Three types of mineralization occur on the subjectclaims i quartz veins with gold potential ii dissemi

nated pyrite in meta tuffites and iii stratiform showingsof Pb Zn Ag Cu of possible contact metamorphic origin

u

i The close relationship between gold mineralizationat the Perrier prospect with northwest thrust faulting is

probably repeated at the Julius Caesar adit Both veins are

gently dipping at 27 to 30 degrees although the northeast

strike of the Perrier does not parallel the east to west

strike of the Julius Caesar It should be noted that magnetitecommonly accompanies pyrite in some of the mine dumps near

the Perrier

12

oThe Julius Caesar vein is hosted by quartz

feldspar porphyry that shows a tendency to quartz stockwork

developments Chip samples in and around the adit returned

only trace amounts of gold Table 3

ii About 550 m north of the Perrier a considerableamount of disseminated pyrite 15 30 occurs in bedrock andfloat composed of biotite tuffites of the Rossland volcanicformation Again chip samples failed to return any goldvalues Table 3

iii Three stratiform showings occur on the propertyOne of these is a narrow zone 45 cm wide about 150 m southof the Perrier shaft Known as the Lucky Boy adit the

assays shown in Table 3 were obtained

J TABLE 3

Assays and Rock Geochemistry Selous Creek Area

Assays

Locality

Lucky Boy dump grabLucky Boy portal across 45 cm

Lizzie c grab sample

Cu

165

190025

Pb

3 35

3 6640

Zn

10 75

5 75

3 49

Ag2 623 34

58

Au

031

079001

Rock Geochemistry

Locality

1 Dissem pyrite 550 m north of Perrier ProspectAu ppb

Sample No 0228 bedrock rock chip 5

Sample No 0229 bedrock rock chip 10Sample No 0230 float rock chip 5

Sample No 0231 float rock chip 5Sample No 0232 float rock chip 20

2 Julius Caesar aditAu ppb Ag ppm

Sample No 0233 bedrock chip 20 0 6Sample No 0234 bedrock chip 20 1 7

13

JThe values occur within schistose biotite tuffites

which exhibit weak to moderate sedimentary banding Minerali

zation consists of sphalerite galena magnetite and chalco

pyrite and appears to be crudely banded

The remaining stratiform occurrences were consideredto be skarn or shear zone desposits by previous workers

The North and South showings are described and sample results

are given in Assessment Report 7377 so this aspect of the

mineralization is not repeated here Suffice it to say that

erratic values of Zn Pb Ag Cu Au were returned over

mineable widths and short 100 to 150 ft strike lengths

The host rocks consist of a limey tuffaceous

biotite schist at the North showing and similar lithologiesgrade into limestone and marble host rocks at the South showingThe North showing contains well banded sphalerite indicative of

a volcanogenic or sedimentary deposition Sphalerite laminations

appear to thicken into the hinge zones of minor folds indicat

ing a pre foliation emplacement of mineralization

In addition to the sphalerite galena chalcopyriteand pyrite the writer identified magnetite at the North showingbut failed to find similar material at the South showing As

noted previously magnetite crudely banded was also found at

the Lucky Boy adit

o

The presence of an isolated 1 m dike of feldsparporphyry at the North showing is not repeated at any of the

other stratiform occurrences and is therefore not considered

a likely source for the mineralization It may be concluded

that a syn volcanic origin can be proposed for the base metal

showings of Selou Creek but that a replacement or skarn

origin cannot be ruled out of consideration From a practicalviewpoint it is surprising that no magnetic survey has been

undertaken on the Selons Creek property in spite of the use

of more sophisticated EM methods

14

v CONCLUSIONS RECOMMENDATIONS

The Selous Creek Property has received considerable

work in the past all without the recognition of magnetite in

two stratiform showings and the Perrier gold quartz area A

magnetometer survey could perform the dual service of outlin

ing interesting mineralization together with increasing geo

logical knowledge of this poorly exposed property

J

15

oVI BUDGET ESTIMATE

Stage 1

Line Cutting 20 000 m @ 150jkmMagnetometer Survey @ 150jkm

including base station rental

3 000 00

4 000 00

Total 7 000 00

Stage 2 contingent on results of Stage 1

Diamond Drilling 600 m @ 130jm 78 000 00

Signed R ovJLR V Beavon

Consulting Geologist

o

16

oVII STATEMENT OF QUALIFICATIONS

I Roy V Beavon of the City of Richmond in

the Province of British Columbia DO HEREBY CERTIFY

That I am a Consulting Geologist and a principalin Beavon Consulting Limited with offices located at

8720 Millmore Road Richmond British Columbia

I FURTHER CERTIFY THAT

l

U K

I am a graduate of the University College of Wales

with degrees of B Sc 1957 and Ph D 1960

2 I have been practising my profession continuouslyfor the past twenty two years

3 I am a Fellow of the Geological Association of

Canada of the Geological Society of London and of the

Geological Society of America and a Member of the Societyof Economic Geologists and the Canadian Institute of Miningand Metallurgy

4 The information for this report was obtained from

personal examinations of the properties on June 8 to June 131982 and from private reports and government publications

5 I have no direct interest in the property examined

this propertynor do I expect to receive any interest in

DATED at Richmond British Columbia this first dayof August 1982

8 MRoy V Beavon

Consulting Geologist

17

JVIII COST STATEMENT

Geological Mapping June 8 June 13

@ 250 per day 1 500 00

Transportation June 7 Richmond to

Nelson June 18 to Richmond800 miles @ 12 1 48 00

Board Lodging Meals7 days @ 40 280 00

Report Preparation 350 00

Assays and Rock Geochemistry Min En Labs Ltd 195 50

Air Photographs Pacific Survey Corp 103 98

Total 2 477 48

Note Receipts for 1st four items may be obtained from

Beavon Consulting Limited 8720 Millmore Rd

Richmond B C V7CIS9

Signed W6 J

J

REFERENCES

LEROY L E 1912 G S C Map 62A

DRYSDALE C W 1917 Ymir Mining Camp British ColumbiaG S C Memoir 94

O GRADY B T 1932 Plan and Section of the Perrier MineTo accompany B C Bureau of Mines Report by Resident

Engineer Nelson B C 1932

COCKFIELD W E 1936 Lode Gold Deposits of Ymir Ne1sonArea British Columbia G S C Memoir 191

MCALLISTER A L 1951 Yrnir Map Area British ColumbiaG S C Paper 51 4

LITTLE H W 1960 Nelson Map Area West Half BritishColumbia G S C Memoir 308

B C ASSESSMENT REPORTS 7377 7393

B C MINISTER OF MINES REPORTS 1910 1931 1960

JB C DEPARTMENT OF MINES BULLETIN 1932 pp 96 97

J

MIN EN Laboratories Ltd705 WEST 15th STREET

NORTH VANCOUVER B C CANADA V7M 1T2

TELEPHONE 604 9BO 5814

ANALYTICAL REPORT

Project Ne1son E aton a Date af reportJune 25 82

File No Z 22 Date somples recejved Jlgl e l 2 8 2

Samples submitted by

Report on

Aber Re s o urce

10rocks Geochem samples

Company

y4 Assay samples

Copies sent to

1 Abel Resources V ancouver B C

2

3

Somples Sieved to mesh Ground to mesh 80 rock ge oche m

100 assayPrepared samples stored Xl discorded 0

rejects ass aystored discarded iii geochem

Methods of analysis Assays Cu Pb Zn Ag Ac id d iges tion ch emica 1 ana lys i

Au Fire 1 s say G eQchem C u PbZn Agnitric p erch1oric d ig e s ti n

A A Au Aqua Regia A ARemarks

SPECIALISTS IN MINERAL ENVIRONMENTS

yTO Ab er

MIN EN LABORATORIES LTD i

705 WEST 15TH STREET NORTH VANCOUVER B C V7M 1T2 fPHONE 604 9905BI4 OR 604 9BB4 24

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