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CON-SHAWKEY GOLD MINES LIMITED

Striker Township

District of Algoma Sault Ste. Marie Mining Division

Ontario

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iSEP 13 1967

BRESIDENT GEOLOGIST

SAULT

December J8, 1967 GHD Consultants Limited

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LOCATION

ACCESS

RESOURCES

HISTORY

TOPOGRAPHY

VEGETATION

LINE CUTTING

GENERAL GEOLOGY

CONCLUSIONS AND RECOMMENDATIONS 6

CONCLUSIONS

RECOMMENDATIONS

ESTIMATED COST OF PROPOSEDDRILLING

CERTIFICATE

ACKNOWLEDGEMENTS

APPENDIX "A"

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'3jjj!tMiPROPERTY

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?pTh* claim group consists of thirty-aix contiguous unpatehted-..,.^^,,,,^•A -;:-""" "' ' ' ."''' ; v--'-.y.--'-'-V-*'-*'''- . ;'-- ' '-V^lS^ij^v*'' • ^••:-.^'.^-''ii.'^'^t'^'.:i^t.^^.

Striker Township,v Sault Ste; Marie M&lng bivisiorf ofvOhtario^* -- - - -... v - ' - -•-•'•-••V'. '-.-i- -. . - . •--.•-j

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•" "iSa iifllitj as Jfoliowsrv'."-;!;^1 ''-^The claims are numbered by the Ontario Department of Mines as follows:

SSM 80989 to SSM 81006 inclusive (18 claims)

SSM 76690 to SSM 76707 inclusive (18 claims)

LOCATION

The property is situated in the northeast quadrant of Striker Township

of the Sault Ste. Marie Mining Division of Ontario. The group abuts

the eastern boundary of the Township with Long Township and extends

from the north shore of Lake Lauzon to within two claim lengths of

the Township's north boundary.

ACCESS

The property is readily accessible from Sudbury or Sault Ste. Marie

via Trans-Canada Highway #17 to villages of cither Algoma Mills or

Blind River. From village of Algoma Mills, access is by boat across

Lake Lauzon, a matter of only seven miles. From village of Blind River,

access is via Highway #555 to McGiverin Lake and then a bush walk for

about two miles to the north-west corner of the property. Suvibury and

Sault Ste. Marie are both served by Air Canada and Canadian Pacifi:

Railways.

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Hydro electric power is available from the Ontario Hydro grid which

supplies the Sudbury-Sault Ste. Marie-Blind River area.

Timber and other building materials are available locally.

Transport via Highway #17, the Canadian Pacific Railway and/or Air

Canada to Sudbury or Sault Ste. Marie is no problem.

An old lumber road trending north-east passes through the property.

It has been obscured by later beaver work and is overgrown at places.

On the accompanying geological and magnetometer survey maps, the

road has been shown by double dashed lines where obvious and by a

single dashed line interspersed with question marks where flooded or

too overgrown to recognize.

HISTORY

The general area of the property has been prospected for copper over

many years and for uranium during the 1953-1956 era. Some of the

drilling done in this general area is inconclusive as a fe\v of the drill

holes failed to reach the basement. The location of the earlier diamond

drill holes is shown on the attached property map and the drilling da:a

, , . .. . . .,..-.' . - '-fs. rfr "*:-'j.';t'j*f:y.ti, : SyV-'ii,*;"

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1. A diamond drill hole was completed by Algbina pre.Pro^ertle?*"^^" Ltd., in 1955 in the now claim #SSM ^'--^ ^ ^'^^-- ^'' '^

.v* carried to a depth of 1365'j- it hit the basement at a depth of -v ^S

1201', but no uranium bearing quartz pebble conglomerate was

encountered.

2. Gwillim Lake Gold Mines Ltd., drilled a hole in 1955 to a

depth of 830' in now claim #SSM 80991. The hole passed

through quartzites up to a depth of 267' and between 267' and

823' it ran through diabase. From 823* onwards the hole was in

hornblende granite (basement) but no radioactive conglomerates

were encountered.

3. Fitzpatrick Uranium Mines drilled seven holes in now claim

HSSM 76697 in 1955. All the holes were very shallow (ranged

in depth from 25' to 59") and ended in quartzite.

TOPOGRAPHY

The relief of the country is fairly high and a scarp and dip slope topography

prevails in the sediments. The drainage is controlled by the geology,

creeks flow either along the strike or along the weak zones, i. e. contart

zones. The diabase dykes of the Keweenav.ar. type are less resistant to

erosion and usually form small stream channels. There has been fairly

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Both coniferous and deciduous trees are common. A lot of forest cover "-- 1 1

has been destroyed by previous forest fires and there is practically no

soil over the quartzite areas.

LINE CUTTING

Line cutting was done on the property during the month of November, 1967

and a total of 46 miles of lines were cut. Three major east-west base

lines were necessary and cross lines were cut north-south from the

base lines at 300 foot intervals.

GENERAL GEOLOGY

The property lies on the southern limb of Chiblow anticline and is

underlain by a thick (about 500') gabbro body in the eastern part and by

Huronian sediments belonging to Lower and Middle Mississagi Formations

in the western part. In the north eastern part of the property Archean

basement rocks of granitic to granodioritic composition outcrop. These

formations are cut by a number of thin east-\vest running diabase dykes.

A vertical fault of no significant throw runs cast-west in the middle of

the property. Following is a brief description of the formations h

chronological order.

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r^-v-y".-- "- - " '. : - - "' - - ' ' - "' . -•^Diabase Dykes (Keweenawan)

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^^These dykes are olivine bearing and cut all the older formations. The

trend is east-west to slightly north of west./: They are usually

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^y; thin (of the order of 20' - 30'), can be traced over lenghts of 200'-300'.; ' '' '- -' ' ' 'They cut the host rocks at steep angles and in certain cases are almost

vertical.

Nipissing Diabase

The gabbro sill is about 500" thick and covers about 307r of the map area.

At its contact with quartzites it shows a chilled edge. The body is almost

barren and only at one place (Line 18W. 18N) slight traces of sulphide

mineralization were observed.

Lower and Middle Mississagi Formations

Middle Mississagi Formation outcrops in the western part of the area and

is represented by arkosic quartzites and interbedded argillltes. Lower

Mississagi Formation outcrops in the central and north-west part of the

property and is represented by pink to light colored quartzites and light

greenish arkosic quartzites. The quartzites arc medium to fine grained

and fairly well sorted. The sediments are frequently cross bedded and

show well developed mega-ripple marks, which suggest north westerlyt

current directions. At the contact with Nipissing Diabase the quartzite*

arc slightly bleached and show slich*. concent rations of magnetite anrl

othor mafic minerals.

m

Magnetometer Survey

A magnetic survey using a Sharpe Fluxgate magnetometer MJ

carried out during November, 1967. Magnetometer readings•: ; itaken both on base lines and cross lines at 100* intervals. Technical

details of the instrument can be found in Appendix "A".

Discussion of the Magnetometer Survey Results

A base control station arbitrarily assigned a magnetic value of 1500

gammas was established at HOON, 33+50E and all the readings were

adjusted to it. Ir. general, the quartzites and arkosic quartzites produce

fairly constant magnetic susceptibility but higher readings are obtained

on the diabase body. Some of the highs in the diabase may be attributed

to concentration of magnetite in the diabase, other high readings occur

on the tops of ridges where tile soil cover is minimum. Higher magnetic

readings were also obtained in the stream channels, this is probably

due to concentration of magnetite in the sand in the stream bed.

Discussion of Scintillometer Results

A scintillometer traverse \\as run following the old road and then along

Line 6W from base line 39 + 60N. The instrument used was a S. R. A. T.

scintillometer of S. P. P. 2. NF type. Usuall-- very low counts were

obtained on the sediments but some of the higher readings correspond

to more arkosic and sericitic bands in the quartzite.

M*

. f :K- I , ' - ! -CONCLUSIONS AND RECOMMENDATIONS

It is suggested that at least two vertical diamond drill holes (size

i*

fefe

should be put on the property.,; There are gobi

basement within 1500

holes is marked on the

foot in each hole. The position bf ;the 'suggested-

•^ a ccompanying geological map.^jThe^ old/winter- : --^v - - .. . ...W;. ;--'^," •i-itiKvj-i ^^^eVi^^**^*!^-' ,. ' . - -,- .v ' ."- *.v-:. "'•'T-^V.vT " ^.-^?,.:-,wv-iP3i.^j-:'t(|^

road passing through the property can be used for this purpose and -

plenty of water is available for any such purpose.

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CONCLUSIONS-- :

The results of the geological survey indicate that the general picture

of rock type distribution as shown in the Ontario Department of Mines

P304 and Compilation Series 2108 is quite accurate. The detailed

geological map accompanying this report shows the detail as mapped.

The magnetometer survey suggests no unexpected complications relative

to intrusives with the readings being generally rather uniform.

The diamond drilling carried out by earlier exploration efforts give

inconclusive results in view of either their local and/or the failure to

penetrate to sufficient depth.

In view of the presently known geological data, it would appear that the

obvious location for any exploratory drilling to cross section the favorable

lower Mississagi Sediments in the vicinity of the basement complex,

would be from the middle Mississagi outcrop area on the south and west

part of the claim group.

H ECOMM EN DA TICKS...——————————————— . . ^y

i i is suggested that diamond drilling be carried out from a site or sites

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^ iwithin the area underlain by the middle Mississagi SedimentsK^S'ti*-"- : ,- : ' \ - : - : --' - . .-,-.v;:;. : -' - \:.:V-, ".^V;, t: ••Vv**V.-'*i^Sfc?,:* ^K'V..-:..---- • •'•-' - -' - - - - -':"' ; ' - ; " -' - -!. s-!v --, ' \:-"'.-\ ••',^??-"ifor the favorable lower Mississagi conglomerate at or nea

l''-:: 'l;4''basement rocks. A suitable location for the initial drill hole might be

on claim #SSM 76690 with actual collar location dependent on local

topography. It would be advisable to provide for a minimum of three

holes with any decision relative to the second and third drill dependent

on the data resulting from No. 1. These holes should reach basement

at approximately 1500 feet, thus three holes would involve a total or

an estimated 4500 feet of drilling.

ESTIMATED COST OF PROPOSED DRILLING

Initial D. D. hole 1500 feet @ S8. 00 S12, 000. 00 TV.o additional D. D. holes (if advisable)

3000 feet @ S8. 00 24, 000. 00 Engineering, supervision and Transportation 7, OOP. 00

Total 343,000. 00

Respectfully submitted

GHD CONSULTANTS LIMITED

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W. Boyes, P. Eng. F. G. A. C.

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That I am a geologist and reside

SS . Weston, Ontario,

2. That I am a graduate in Honour Geology from the University

of Western Ontario,

3. That I am a member of the Professional Engineers of Ontario

and a Fellow of the Geological Association of Canada,

4. That I have been engaged in the practise of geology for

twenty years,

5. That I have no interest, nor expect to receive any interest,

directly or indirectly in the property or the securities of

Con-Shawkey Gold Mines Ltd.

6. That the accompanying report is based on personal knowledge

of the area, on government reports and maps and as otherwise

referred to in acknowledgement. "

DATED at TORONTO, this 28th day of December, 1967.

William T. Bo/es, P. Eng. F. G. A. C.

-^ - - . -,i- t?^-^vv-ff'i *v*s*w^*s/r\ift-,iit- .ri ,- 'V 1 -- ,. 1 -Ontario Department of Mines .'^jf ̂Geological Report No. 20^fl^'A-.**1 "..'^-' ''." ; . '/" \ ' . - 1 .. 1 '.'-" '" ' "' ' - -

*^|; Geological Report No. 13 71 v;' Ontario^Dep^rtmenfjo'rMines . s

Geological Circular No. 6 Ontario Department of Mines-.".- - - "'~ ' '- ' - :-''. •••' '".

Preliminary Map P. 304 Ontario Department of Mines

Compilation 2108 Ontario Department of Mines

Report GHD Consultants Limited (July 10th, 1967) David A. Duff, P. Eng.

Field Geological Mapping Z. Aziz, M. Se.

Geophysical Survey GHD Consultants

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SPECIFICATIONS

SV" v\•"ste"---.

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MF-1 Standard surveying and prospecting magnetometer ;^with s elf-levelling sensor. - -'- ' -- . : .-. - .^v*-^. : '•••'• :';: ,.::-- , '•-.^'i-'{.', .^"'x^.-/

•*-'.' " ^ ^ '- ' '" , ~'~.."'" .' ''-' '- . ' -' - '."' ', - .•^(•/V.^'."'-'' - ' "i ;' ' - .'- ''r'.-'^".' :" ••': ',' - - "-J^" Vv '-..T V- l^ - '- "v^. ^/"'" ~ "- ' - HV',1.',

jlanges! Plus or minus - l, 000 gammas l. s e. 3, 000 M

10,000 "30,000 "

100,000 "

Sensitivity: 20 gammas por. div50 "

200 "500 "

2000 "

Meter: Taut-band suspension, l, 000 gamma scale: l 7/8" long 50 div3, 000 " " l 11/16" long 60 db

Accuracy^ l, 000 to 10, 000 gamma ranges - 0. 57c of full scale 30, 000 to 100, 000 gamma ranges t jyf of fuu scaie

Operating Temperature;

Temperature Stability:

Bucking Adjustments';

- 400 C to 400- 400 F to 1000 F

OLess than 2 gammas per C (l gamma/ F)

10, 000 to 75, 000 gammas by 9 steps of approximately 8, 000 gammas and fine control by l O-turn potentiometer. Con vertible for Southern hemisphere or t 30, 000 gammas equatorial.

Batteries; 12 x 1. 5V - flashlight batteries ("C" cell type)(AC Power supply available)

Consumption;

Dimensions:

Weights;

50 milliampercs

Instrument; 6 1/2" y 3 1/2" x 12 1/2" -165 x 90 x 320mm

Battery Pack: 4* x 2" x 7" -- 100 x 50 x180 mm

Shipping Container: 10" dia. x 16" -255 mm dia. x 410 M-:

Instrument: 5 Ihs. 12 oz. - l, t Battery Pack: J Ihs. -l o z. -l Shipping; l ' '"i.

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CON-SHAWKEY GOLD MINES LTD.TWP 4 ALGOMA M1MIMG DIVISION, OMTAR-IO.

MAGNETOMETER 8 GEOLOGICAL SURVEY

G.H.D. CONSULTANTS LTD.

Base Line IQ5+60N

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LOCATION MAP

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76701 l ^UDBURV

76695 76694

76693

CON'SHAWKEY GOLD MINES LTD.TXA/P, ALGOMA MINING DIVISION, O NlTArZ\O.

Base Line O+QO

GEOLOGICAL SURVEY

GHD CONSULTANTS L.TD.

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FAULT

STRIK.E AND DIP OF

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SCINTILLOMETER READING (COUNTS PER SECOND)

PROPOSED DIAMOND DR.ILL HOLE

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