'i . if-;.t.

IA-

k*

eei7 CORBIERE 010

REPORT OK THE "EDWARDS" GOJ.D rPHOPr.RTY.

TOWNSHIP 2fl. R/yNflE XXV. (Rf j.,

DISTRICT OF ALGQ!-1A. OKTARIQ.

C-F.OLOGISTi;T t.

by W.A, HESSE

1 h e Hoard of Directors. Peter-Rock Mining Company Ltd, Ajax, Ontario.

Gent]omen

Hawk Junction, Ontario, which

PROPERTY:

P. ENG. July 30, 195C.

NOT TO BE REMOVED FROM

THE OFF.CE OF THE RES.DENT

SAULT GTE. MARIE, ONT,

I beg to submit the .following report or. a gold prospect nearir, known AS the "Edwards" Property."

Tho property consists of eicht rcininf. claims, nur-ibcrod 3&70 to 3677, incl., in Townnhip 2#, Range XJ'V. District, of Alro-na, Ontario. This Township is part of a land t;rant nadc to thn Al^or.n Central Railway,, and the claims are held under the ten? o^ a 99 year lease from the railway company. These lenses are held by the estate of the late Peter Edwards of Sault Ste.'-aiJ-ie, Ontario,

LOCATION AND ACCESS;

The location of the property is about two Miles and a half north of Hawk Junction, n Division Point on the Alpoaa Central Railway, and lers than a mile west of ''Mile l'39 n on the railway, At th t .ne ttr.Edv/ards opera ted the property, it wns connected with Havk Junction by a road, passable by truck. This road is probably p;rov:n over and partly washed out by now, but, could be restorer! at a relatively small expense, the terrain not bein^ too difficult,

.'JFOLOGY AND HISTORY OF THE A31.A :

The property is situated - approximate..'.y in the middle - on a belt of Keewatin formation consisting niainly of lav; s, Greenstones, schist and tuffs. 7his belt extends frorri the northeast corner of Lake Superior - around the mouth of the .'.ichipicotc-n River - to the township of Rennie about sixty miles to the northeast, The width of the for:ntion varies frorr. ten to twenty miles.

This belt has aroused much interest and in yoarft pa r. t attained prominence aa o, v ery mineral rich section of the- country. The southwest part, the |-i irch,i p jwc.o t en ^A r ua^, Contains the l a j t;e iron deposits of the "Michipicoten 'Iron Ranren, lT Host oft.'icse dc-pori*..'-. are owned by the Alf,o.r*a I5teel Coj'por^t.ion whose "helen I'.iiic" has a capacity of 60DO tori r. poj* day, Ooid vac firstj. diccovured in i'icdpicotnn in 1897. Kurac-rous gold finds, r, o m e displaying spectacular free ^.olc, liavibc-en nad e in thoarea. i'x;veral mint;s have been in operation off r.iid on and produced f,old for a nunber of years; the "j'-atto" "Parkhill*1 and ''Gr^ce" (Darwin) were t hfi nostinportant.

fS'v"". -There is no sharp boundary, but the Algorr.a Central Railway line •i'.v going north from Hawk Junction, is generally taken as the dividing lino lv between the Kichipicoten Area dnd the Ooudreau Area to the northeast. ; This area, stretching froni the A.C.R. to Localsh, on the C.P.R. and Dog H.Lake, has likewise been kno-.m as a gold country and seen a good deal of development. Here "Goudreau Gold Mines," "Edwards Gold Lines" a'decline Mines" opnrated and produced gold in the Thirties.. The area also contains

: large deposits of pyrite.

Across Dog Lake and constituting the northeast end of this belt, is the jj'issinaibi Area which sav; a gold rush in the early Forties and has produced "Kenabie Minos" a profitable gold nine with a daily, capacity of600 tons. . - r

The above short account makes it evedent that the geology of this belt is favourable for tho occurrence of gold, './hile, so far, the history of I-ttchipicoten and Goudreau is that of rich but snail de-posits with lack of prominent structure, the chances of finding an iupbrtant and Liore persistent gold deposit have uy no means exhausted.

HISTORY OF T:IE PROPERTY

This property was purchased by .Ir. Edwards from tv;o Hawk Junction nen in 1939* After a limitet. amount of exploration h e erected a srr4all "Gibson" nill on tho property nnc1 treated ore from open pits. It v/as found that the ore v;ac not free nillinr and that very little of the gold could bc recovered by a:.ia3.ganatio:: . Mowever, several small batches of concentrates v/ere produced which r;r.r.ayed 25. OJ os, 53.13 os, 9i5.3^ 02, and 31^.3'- 02, rospoctively, in gold p:'r ton, according to asuay records. Duo to nctalluip.cal difficultier., ar.d nrcbibly nlr-o because sufficient ore could not be ra nod in open cut, th^ rail! operated only a few ..;o:.ths.

A Rhiprjcrit of ore to l.'oranda i lines allegedly ter. tons, csr.cycd .3015 02 in zoid p . t. ' ,

The writer visited t.ht proptrt-y repeatedly in 19AO. His inpressio of the pr'.^erty -,/ar. favourable E.lthou..h } \v Uiought tliat lldw^rds was making E ni,-tc'-:v in concentrating c-xj/enditurci; and efforts on one place, neglecting systematic explor?tion of tV v:hole property,

GEOLOGY OP THE P?.OPi:f:VY ;

The location of the. property ir. about o. c nile and a half vest of the contact between the ;'.eeW..tin fornation ari the great granite batholith (Laurentian) which under l it f. the country to the east. It is also only or.e r;ilc north of the sr.iall granodiorite plug a; t the oast end of the . '.rtlett Iron !(ange.

The property is underlain lv Keev.'atin },ocl:s. '..'hils. rear the south Lcuncictry basic volcanics,' :ianely andesite ana basalt, prevail, the for.M-.tior. bcco.'ucs rnor.t schistose to the north. In t:it. i.iiccle of tht property, near the eart-wes't clain line, biotite ant', chlorite schists are dominant. On the north part of t-tc property, r6 inly ci i^s 3 (J?1 and 3o?2, outcrops of quart snorjphyry, probably intrusive, have btt-n observed. Thr extent of thir- intrusive- rlug, if it ir t r;: i , is r.ot knov.Ti. The contact v;ith t.hi. schists to t:u- soutn ir- re.', her inJefir.ite.

^^H ^K|*-'*^.* '-. - " t ^ ' - J1 ' v , ; - .

•ll^v : ; ' '-- - ' ' " -'- -•%^-v.'' - ~ IK• "i-'V- - ^^ . '•|s^ r ^

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. i . "itfci-!- - ' - - - ' - ' ' f ' - -i ' 'O- : . -i.- . . . -. ' ' . . '*- ' . \ ^^jAi .... . ——— fc..,.. ..i.. .- , - - ' - —————

: JvKSULvr* or PREVIOUS CX^LOP.AVIUK.•,' - 'l . --; *

Several f.old bearing veins have bt-.cn discovered on the property. The noct inportant of these occurs in the contact area between qua r t porphyry and schist. It strikes ca5;t-vest across the boundary betwee^ clair.s 3671 and 3672, about 150 feet north of tho south boundaries of these clains. The- vein has b en followed, and - explored by mriorous trencheu and pits, for a dir-tance of about one thousand feet. It is a stron** structure, varyinr in width fron one and a half to seven ftet. It ip silicified sht.ar with quartz stringers rather than a true fir.sure vein.

Kurnerous samples have been taken, and values fron "Trace" to .'i'll.1.75 in fol^ p.t. over two feet ^re reported. Tno vein was channel sampled but the records available are not o.iplett enough to permit a calculation of avert^o lenr^th-'i/idth-valuo. Hov/ever, the conclusion is justified that tro'ld uire ralization is v;iduspread. in pold'v/ere obtained fror, this vein at po.nts over ni^e hundred feet apart.

About thirteen hun dred feet to the east, and lying on strike of the first one, another vein occurs on clain 3&70. Tiic hSs been followed fora length o* two h enured i'cet and explored by 3 pits. As sample running .;'15.00 in pole p.t. over seven foet is; reortcd fro~ the diddle ore. Thu location is on the north shore of t sr.iall lake.

The Edv.-ards property in Towr&hip 25 A^r.-:e 25 has a good location, clone to railway. It is e pror.asinr C0 ^^ prospect vdth favourable f.colof-y ftr.tl warranti. ^n t-j.ter.sivc exploration pr

liceptctfvilly submitted,

V../. .i-Iuf.sc , r'.Lng,

lCi' "~"*-' - -fetce. " ..*' * ' ""

^ ree. 22/39: ; - Jan 3/40

Jan 3/40Jan.nMay 2S/40

j, ""June 28/40July 12/40Sept. 16/40tiSept. 2 5/40wSept. 27/40

M

Oct. 22/40ttnH

Nov. 16/40fIov.25/40Dec. 2/40"

" 20/40Dec 20/40

Jan 2/41Jan 11/41"Jan 23/41

1!

It

Jan. 31/41March 10/41n

tin

Aoril 22/41Ilay 12/41ti

nMay 27/41

June 20/41

July 21/41 itti"

A,: L' AY 5 3Y ALGOi'A

Assav Mo.

396400401402403419A20421440336496497503504506507529530531 .•"32535536537533539543544545549550551592593594

•JOo6096106116266326336346366376426436446/^5651 652653654

* *-* n. M

•jf;:T:iAi, ?..ML.:AY AS. AY oriicr. EK j02. Gold nor ton. i

!

17.2011.7710.37

.4325.623.74

.91• 71

7.50.2207

159 (Mill Tailings)' '12.30

.05

.91 (..'est end)314.32 (Concentrates)

.019ti.3o Concentrates .''o.l

4.71 " No. 21.32 *' last run

53.13 Concentrates.37 Tailir.ra

6.65 Concentrate!;1.S2

.13 1-ilin?:s5.17.06 Tailincs

7.97 Concencrates17.72

.735.471.742.632.302.16

.59 Cabin Pit1.20 314 ' Kast

.23 tted pit 15 ' fror. extreme v;est

.38 Concentrates

.70.05 hillside vein To.l

.36

.36

.02 croor.it t- hill

.03 " "

.02

.18

.11

.35

.Ot! Hole Uo. 1 23' x 20'

.06 " 5' x S'lG"

.04 " *io' x 14"

.04 " 72' x 10"

W^'^'ti^' . ' '-.i^l'V,"^''' ' '

f!*sS^v-^-'-A-., '^Pf^.i^:^' 1 ,'.', j ,

Oct. 2/46

July 26/47

Sept. 25A7

ASSAY NO.

655

653

139013911629163016311726

~ 2 -

OZ. GOLD P!J? TOM.

.01 Hole -:o.2 16* x 3' to 21'

1.03

.08

.01Trace1.02

Trace1.65

;43 C, HALSTEAD F. CNO.

;vA**oc i W T c* rtcK'- *t-' ' '

C. Ot H. MINE CONSULTANTS LTD.

eO4 QUEEN STREET. CAST

SAULT STE. MARIE. ONTARIO

42cesNEeeis eei? CORBIERE

REPORT

On The

PROPERTY

fleld By

PETER ROCk UXBXKO CO* LTD.

IMCPCCTIOM*

(XVtLOPHtNT

MAMAOCHCNT

OSO

In 28, R

On Tho

^ HUPSCI.S BAYIflimiO LA!,'DS

DISTHICT OP AirTOKA,02;TARlO,CAr!ADA.

Hy;

li. C. i;ALL3Tii;kD, 13.Se., P.HIG.

P', t cd:Ai:-:uot 26th, 1959.

G. 8. H- MINE CONSULTANTS LTD.

6i)4 QUEEN STREET. CAST

SAULT STE. MARIE. ONTARIO

M. C. HALSTEAD P. ENG.

AND ASSOCIATES

Office - AL. *-O(*l

INSPCCTIONt

DIVIIOPMCNT

MANAOIMCMT

REPORT ON TUB KBlHG PROPERTY HELD BY PETER ROCKUIlilKC COttFAKY, LIMITED Hi TOYiHSHIP 88, RANGE 25,

DISTRICT OF ALGOttA, ONTARIO, CAUADA.

BDICiARY

Petqr Rook Mining Co. Limited holds JO contiguousl

raining claims, eight of v/hich ere held under 99-year lease

with the Algoaa Central end Hudsong Day Hallway,,^ .——— . - ^ - -

Tho property la closo to roil transportation and

very accessible.

Electric energy lo available v;ithin Q milo of the

property, with tirr.bor and v.oter aleo available.

v/ork done nbout 1959 by Peter Hdv.'ords indicated

a strong voin cyoten which he enjapled sho'.vlng Gold to occur

along the ontiro structure exposed by tronohing.

Sanples token by the writer confirms this v/ith

Gold voluos running Tron Thirty-five cento to Tv.'onty-one

Dollnro por ton. Mr. Edwrrds reports valuso up to AlAl.95

per ton.

Sampling of i tailings nt tho five ton nill Bhcv;ed

0.4& oz. Gold per ton !v;ith r. value of .'15.28 per ton at

?53.44 Gold.

Tho vein hcs been opened up for 1000 feet by

24 treiichcs and 5 pito 14CO for'; ^o the otst tp]:f,r.r to bo

on 5itri!:e.

-2-

I believe this to be a good Gold prospect andt

I am recoirmending a minimum of 2,000 feet of diamond drilling

to check the veins.

PKOPSRTY

The property cons lo t s of 22 contiguous unsurveyed

and unpatented mining olnica numbered A.O. 6224 to A.C. 62JO

inclusive; A.C. 682? to A.O. 684J inclusive, containing

880 acres more or leas, and 8 surveyed mining claims held

under 99-year lease from the Algoma Central and Uudsona Boy

Railway nnd .numbered A.O. J&70 to A.C. 3677 inclusive,

containing 497^73 acros or a total of 1,377*73 acres now

held by the Conpcny. The claims -are all located in the

south oast corner of To'.vnship 28, Range 25, in the District

of Algoma, Ontario, Caneda.

ACCESS

The property lies north of the City of Sault Ste.

Lterle alontj the Alfjoica Central nnd Hudsona Boy Railvoy at

lailoago 1&9* and approximately t /o and e quarter miles

north of tho To\vn of Hawk Jurctlon*

A truck road Wos built to the property froa Hov;k

Junction. It Is ncm usoble for about one and a hnlf nilen,

at thin point a crook has to be bridged and the rond rcpoired

from hero or. in to tho nine,

OJOLOOY

Tho property JIBS rot b:; en rJ2ppc.-d Geologically.

.•.o;:cver in cror;o!n.7 the property the c^^nito contcct ivith

tViO bnsic Ir. ve o to t;io north v:-s noted rbout one li&lf c

south of the vein system.

Tho vein oy o t era Iles In o wide shearing on mining

claina A.C. J&71 tind. A.C* ?6?0 with another rein on claim

A.O. ^75.

The quartz veins are found in a silicified shear

zone along with considerable chlorite schist* The eh oar

contacts were not cxplosed except in one pit at the west

end of the trenching, here the north contact of the shear

ID \vith granodiorite* Lying between the vein system and

the granite to the south* quartz porphyry v?ns noted in

tv/o snail outcrops.

GOLD..YSIKS

Tho vein system la nado up of parallel veins of

from a f OY/ inches to 6 feet in width. The voins strike

about onst v/est and lio Q little over 100 foet to the

north of the south boundary line of clniras A.C. J&72 and

A.C. 3671.

A number of yecrs DCO *4- trenches v:ero dug clons

1000 fc6t of the shearing. Tho original sampling of these

tronohes es reported by ?etor Sdv;ords ehows the Gold values

to have run frou f1.14 to C141-95 per ton.

Govcrnl of these trenches v;ero recently cleaned

out nnd orunples of thoso token by the writer essnyod froa

..'0.35 to |21.00 per ton in Gold.

About 1400 fc-ct to tho ertst of thsso trenches nnd

en triko r.rc throo t :oi-e trenoL^s, these lio juct t D the

north 01 J.'.:-, r.rds Lnlro. I did not nr,~plo theno.

Ur. Edwards reports the centre trench as assaying (12.00

across 7 feet.

Approximately six hundred feet east of the main

trenches and two hundred and fifty feet south a vein is

reported by J-eter Edwardo which assayed yB.10 across

2.5 feet.

PO'^SR

Power is available froa the Great Lakes Power

Conpany \vhose pov?or lines run to Hmvk Junction and north

v/ithin a nil o of the proporty.

WATER

Water is available on the proporty for any

c: operations.

Uino ?imbar is available in tho iranodinte area.

A five ton Gibson Hill still remains on the

property by Sdvmrda liolce. It is evident by the tailings

pilo thnt no c^cat tbnna^e v;ns nilled end recovery nusti

have boon low, RQ th(i equipment ras not ndequato for

Gold recovery.

I took a ccniple of tho tailings. They assayed

0.46 or. Cold per ton, or ..15.28 per ton vrith Gold nt

-5-•P'

! This IB evidence In Itself that recovery was ~i l poor, and also that the grade of ore to the mill oust

i have been i

It appears on examining the various pita that

the ore delivered to the laill cane fron three trenches

l No. 18 - 24 and 2?.

l CONCLUSIONS ft RECOTat.H!DATl01'IStj The property Is accessible with a road to the

l property from Hawk Junction on the Algona Central and Hudsons Bay Railway ivhioh serves this area.

Gold values are found in ell the trenches v/here

quartz veins v/ero exposed.

Frora inspection it appears that tho ore milled

in the five ton nill cane frora three trenches. Tho values

rGTjninins in the trillings indicates that connercial oro

v/as obtained from thu vein in those trenohc3.

I fira recorapndlns that the raain vein systoa be

diacond drilled and fcbat sons dinnond t-ri 11 hoies bo put

down in the 1400 foot Boction betv.'een the coin trenches

end the trenches at !sdv;nrds LR!:O.

A nininun of 2,000 fcot of dicnond drilling is

nooossnry r\nd I an roconnondins that a contract be lot for

thin orDun*;. The eir'tinated ooot for this v;ork is ^10,000*00.

r.ccp&ctfully eub.-jitted,

G. ft H, MINE CONSULTANTS LTD.

6O4 QUEEN STREET. EAST

SAULT STE. MARIE. ONTARIO

V M. C. HALSTEAD P. EMO.

.: AND AF. 60CIATE6

'f f "MANAGEMENT

CERTIFICATION

I, Hilton O, Halstead, of the City of Sault Ste* Kerle, Ontario, Canada j hereby certify t

l*. -That I ea a Klnlns Enclneer v?ith officen at Suite 12, 604 .iuoen Street Eat-t, Sault Ste. i'nrlo, Ontario.

2. 'That I aa a gra&uate of the University of Manitoba, )3.So. (1?29), and n r.eaber of tho Association of Professional Englnsora of tho ^ -ovlnoe of Ontario.

3. That I havo no Interest either direct or Indirect in the property or socuritios of the Ccrapnny and that I do not expect ecy Interact in the property or securities of tho Company, }-eter Itocl: i:inins Conpany, Liinitod.

4. That tho accompanying report lo be.sefl on personal examination of the property on Au^uot 19th, 1959*

5. That old v.-oi'klngs cro as reported.

b. That tliis Certificate allies to the following ninlng cloibs: Unpntentod clnicis HOB, A. C. 6224 to A. C. 02^0 inclusive, A. C, 6U2? to A.C. C84J inclusive, nnd patented clcinn i'on. A. C. 5fe?0 to A. C. 5C77 inclusive, oil loottod in Tov.^Bhip 28, Banco 25, in the District of Algona, Ontario.

- ^ 4. ,- J t/J. u OCX *

26ta,

' , , August I960.aai? CORBIERE 030 " " ' ' '"' ' ' - -.

\ j', "ftepbytoh Peter Rock^Mines.^ (9.E,Corner Twp.2g.-Hange 25*)

'property was brpvight to our attention by A.Spy when" Peter Rock Mining Co.. h'ad preparations underway for a diamond drill program* The purpose was td gain first hand knowledge of the property in the event optionihg becamts a possibility in the future.

The property is well located as shown in the accompanyiny sketch.

'A study of the complete history was not undertaken. Evidently it has been examined many times and numerous trenches completed. Among past examiners wes Sherrit Gordon. So far as la known the property has never been drill tested.

Eleven Pits were examined covering a strike distance of approximately 1000 ft. Six samples were taken from five pits.

Narrow quarts veins and quartz-calcitt velnlets occur in biotite-chlorite schists. In the pits examined there was only minor variation from east-west strike of the schiet,osity and dip of 60 N. The velnlets followed and in ne place cut across the schistosity.

The veins are narrow, the maximum width encountering being 18?.

Sulfide mineralization varies fron minor to massive.

The relative position of the pits, a description ami sample reults are given in sketch 2,

Recommendations and Conclusions,

Past reports indicate that hif'.i values were obtained from surface pits. However, only one sarule returned a value (0.86) comparable to thooe previously obtained - and this was over a very narrov/ vein.

The occurrences exhibited no strong structure, in all cases the veins and veinlets are conformable with cchistosity of the country rock. The maximum vein width encountered is IB".

There was no immediate evidence of a croec. structure (S) that could act as loci for ore deposition.

The property la not promising. No further work is recommended by us at present.

-; 6 -

Town ah J. p 23. Ran F; e ? 5 ,

(1) k brief visit was made to the t'eter Hock group of claims located 2i miles north of Hawk Junction. The property has buen examined several times, •A series of tranches expose en east-west trending quartz vein system in Keewatin schists. The zone is rourhly 7' wide ind is mineralized with scattered to massive F.ulnhldei. . The vein system has been exposed for over 1000' by trenches.

The property has been drilled recently, and several diamond drill holes were ''ound . At-, examination of the- core boxeo beside each hole indicated the rock t^pe to be predominantly Keewatin1 schists, and carbonated sericite schists. Quartz porphyry was noted near the vein system.

(li) A traverse was made northward across the Holdsworth property, now owned by Dupont. The traverse began at the north end of a small lake at Mile 2 on the A.M. R. branch line. A ID 1 quarts vein occurs to the north of the lake fcnd is unclosed by sheared Keewatin greenstone . Iht: vein conoiats o milky quarts with pyrite ard ankerite, anc! occupies o fYiult. A sample SA-112 was taken across a 5 1 nection of tilt vein.

The traverse proceeded for 2700 f north to a high hill composed of tuff. Hock types during the course of the trav^rst included intermediate volcanics, pillov/ lava and equivalent schists,

(iii) A brief visit was nit de to t h t- Josephine .inr located in the south western section of Township 28 Hantro i; 5. The prop, -rt y is ov.-ned by iiherritt Gordon and has beer idle since 19^7,. It is runourec tyiat trit: property may produce apain.

The Josephine is unique, nccordJnn to J. D. X. report. Vol. 40. 1946, in th t the ore is mainly henatitt. and w&t deposited by hydrothermal agencies. Gone manganite ami rhodochrosite have been founu associated with the ore.

The main purpose of tMe visit war to become acquainted with rocK types. It was felt thm, thin would assist ir.tho identification of similar rockr. occurring elsewhere,

The wine buildings art b'-.-ln- :.-.pic!ly attacked by the elementa, and ver.etfttion hac apread extensively over formerly clearfcd areas.

C.K,Kustra . July 1961.

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i42ce2NEeais 0017 CORBIERE 040 r. H. LAVCOC. MCHCTMV

PETER ROCK MINING CO. LTD.HEAD OFFICE: AJAX, ONTARIO TELEPHONE WHITEHALL 2-I57O

V-, /n ,/ty/ Ayy^.

W P. P. pCOUIPIC. PWUIOCNT , P. HUXTM. TMUCUnu P. H. lAYCOC. MorrAHr

PETER-ROCK MINING CO. LTD.HEAD OFFICKi AJAX. ONTARIO TELEPHONE WHlTIHALL 2-1S7O

ri?firi]Tfn^

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N.B Gold, shown, at i. C-S., sontplw by M..C

C. t. H. s* ... * S. Ft .Huxter

4....

p l* T-l 0-69. 0:77

PETER-ROCK MINING CO. LTD HAWK JCT. ONT.

PLAN OF TRENCHES l SAMPLING

BY PETER EDWARDS

CS. CHECK SAMPLES BY M.C.HALSTEAD

SCALE: l* TO 50'

DATED AUG. 24 1959

FRRHe S•"SHK

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pyrite j n iroon . f Au. 1

Sample 1723-Blue qtz. etrs. Jt

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