c cr l- O cr. K-

2 Z z o o S 55 r*rv (1

C p IS O *

-? ---^W

^ il^If ̂^

•••••' ^X

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^

41J13SW0006 0012 DAUMONT

"FW* 'j^ *x**'~' 010C'-:!^---fn'*t'

iff ' . - ~ ,•W ":^te

^4- : Introduction.................. ••" " - ;; ^".'-' ; ",..,.. -' ..; ' " * * * ** * * ** * . . . *. .. .., . 0 , . -1

p0^;: -v:' ^: ; ^^.•••••••••••••••••••••••••••••••••••••........ l

^^ ; t ooot l on and Means of Aocesa.......................... i

^ History.of the Property...............,,,............ 2

3S Geology of the Property.........,.................... 2,.;,*yj^ ..-- "" **

- - s**l* Potential r;urvoy................... ^: —— ^™'"********...**.. 4!

g Diamond toUHiia........,,........................^^ 4

aeooamendatlone and Conoluoiono*.............,...... . 5

J Appendix..............................

L; qpa;

Two plans and a soot ion aooojapany thiy

-V plan of thu stiir potonti;;i aui-voy, r. p?an of

of lha Kottunaao proporty inu a section tiirou^i holes

and 2 of the l!arboy property are included.

RBPOB3J OH JHS PHOPE!ffl33 O?

HOHAJUA0 RJS) lACJt GOLD MIHS3

ABD UARB07 1OHB3 inOT2Dr.

TOWBSHIP 23 RAHG3 10, DmifilOT OF AtGOMA

Introduotlon;i, ~~ "*During the sumaer and autumn of 1961 Ho&farmao Red

Take Gold Mines limited and ttarboy Vines limited carried out

an exploration programme on a ^roup of ol?.ims located in

Township 83 Range 10, District of Algoma* The work consisted

of a se^f potential survey and a diamond drilling programme.

Abat raot:

Results of the self potential surrey and the diamond

drilling programme are to be found within the body of this

report* Reoodaendatlons for future development work to be

carried out on the properties are to be found herein.

location and Means of Access:

The main iSoMarmao group consists of 12 unpatent

contiguous mining claims comprising approximately 460 acres.

: --- "---'-'---'''-'--' ^^'

.. ,- o3 alma are numbered as

.''-. ' ' - -*** ' -" '-, --:,V-**. : '/ '- . - . •'• i'^":' '"•''•'.i" .: ''-,m*' '- ' : .'-V ' ''

SSM 61659-60^61-68-65-64-65-66-67, S81I 61766-67-68.

The Jfarboy Hine a j.td. property consists of a group of

9 unpatent mining olajzas wrtiich adjoins the ttolfermao group on the*M ' . . (jg—

west. These ojaims comprise approximately 360 acres anl are

numbered as follows:

SSM 61739-40-41-42-45-44-45-46-47.

^ A second group of 6 claims numbered Si3J 62095 to

SSM 68100 inclusive were staked by McMaraao. These claims adjoin

the ttarboy group on t ho southwest.

A grots) of 6 claims numbered 'SJJ 61629 to 61834

inclusive are held for Hecmao Prospecting .Syndicate . These

claims adjoin the main Ko&armao group on the east.

?he ci aims are located In Township 23 Kan&e 10

and In Gaudette Township . *ult te. tferie i-'lninG division

Plstriot^of Altjoma, Ontario. The properties are readily

accessible from the Whitman Dam i-.oad which traversea the

western i:c^armao gi'oqp and runs to tho vinage of oarohraont

some 10 miles to tho southwest. tractor road runs from the

ford at tho Goal ala River to the area of tho ohowinsB on the

nain Mciaarmao group, jn the vicinity of Golf Tofco.

History of tho property;

Copper vKis dlsoo-vbred on what is now the main

MoL'amao olalra In ^eptwnber 1955 by l'r. Don '-utherland.

-3-— *.. - *.** . M

A total of l ,676 feet of diamond drilling was completed by the

Sutherland interests during 1958. An intersection of 1*84^

molybdenite over 2*0 feet was obtained in one of the drill hole*

^ The claims were subsequently allowed to lapse and

eventually were staked by the writer for the Mo&anaao and Varbo}

companies.

Geology of the Properties;

She claims are underlain by a highly metamorphosed

sedimentary series consisting of arkose, quartzite and argil i

The arkosic beds have been highly granitized while the argili

beds have been well chloritiaod. The quartzite beds have

remained relatively unaltered, r;ill8 and dykes of younger

diorite and gabbro intrude the sediments.

i'ho sediments strike east-woet and have stoep dips

usually close to vertical, strong north-south faulting uao

occurred on the ground es horiaontai displacements of anomalies

of up to 1,000 feet have been found.

In sawe ^reuo the quartzite has been fractured and

partly replaced by sulphides. 2he sulphidos are mostly pyrite

and pyrrhotite, however, chalcopyrite, sphalerite and molybdenit

"re also present in varying amounts.

Self Potential Purvey;

A self potential survey was carried out on some of

the claims during the poriod rrom June lOth. to .lugust iGth. 196

The purpose of the survey was to locate and traoe zones of

sulphide mineralization on the properties.

A Sharpe V.P.-6 Ground Voltameter *as used and natural

ground voltages were measured over intervals of 50 feet. An

east-west "base 3 ina was run through tho oonter of the ol aim

groups and north-south ore's lines were out every 200 feet.

The cross lines were extended for a distance of 1,350 feet on

eaoh side of the base line. Readings wore normally token at

130 foot Intervals, and in anomalous areas at 25 foot intervals.

The survey was suooossful in ouf ining a series of

strong east-west trending anomalies at intervals across the

properties. - ubsoquent diamond driving has chown that these

anomalies are usually due to the presence of heavy to massive

sulphides within the ..junrtsite horizon.

l.'ionond Drill ing;

-\] K cJ.'armao Property

totn1 of l ,C71r Toot of diamond drilling in 6 ho^oa

w.i3 oomplated on the f.'oL.irriao l rot or -y uurinj, the period from

Ootobor 30th. to :'ove: bor 30th. '901. ^ holur iotorseoted

su1 ; hida nine ra i i "ri 1 1 on be1 cr.7 iho ano.ir.*1 ion 'Jiid two of the

holes obtained interesting vn^uei' in copper ^nd sine. ' role rio. 7

returned vniues of .36^ copper over 1^.7 i'eot and also LOG'

copper over 2.7 r^et doojitji la the ho^e. :,'oi e rfo.^O ry turned values

of L 09.' sine over i E. O I'uet or .SO' rJno over 23.0 feot.

-5-

B) Carboy Property

A total of 421.5 feet of diamond drilling In two

holes was completed on the Mar boy Property during the period

from tecomber 1st. to 10th. These holes were drilled in seotion

to tost two parallel seliT potential anomalies. Both hoi os out

substantial widths of heavy pyrite mineralization within quartzite.

One of the holes Intersected scattered molybdenite mineralization

over 20 foot. A. vs.} us of .25*5 molybdenite over 1.5 feet was

obtained within this sone.

Kaca^aoada.tlons Conol aa ions ;

A. ) K Gfc'. arma o t rope r ty

Vthou-iih uo ore was encountered, tlio results or the

preliminary diamond drill in^ j-ro^ ~. rno :u'o considered to be

enooura^int;. Tov/ vrn uus o i' co;. r oi* ''.ad sine ovvu '.xp, rue i' '.b'' o

widths Vrlthin :i, P j -h i de r.onwfl .:.ur-i, be connideruc; :U ,-ortant.

In view of tht* fact tli.-v- most, o.' tlie anon:c.i oas area.* have not

yet been ezp?orod, it is fs 1 1 '^h'.u :-ddli- ioA'-."1 di^j.'Oiic1 uriT1 in,:;

le definitol y warrnntod.

\ minirai^, of ri, f.". O C I'u.j. tx' . di'viond drli 1 inc-, should

be carried out on the raain ,vci'ar^\o fgroup in order to explore

the various untested tmorja? out- area r. one hole should be

drilled 00 feet en st of ho? e :o. i, in v/h l eh sine vxluos were

obtained, in ordar to dotoj ' :IQ l i1 tho rone ejc'-encV.' to the oast.

One hols ,:hould "bo dri^^ud I r. iho violnity of ho^o :?o.4 \vhioh

encountered 1*84^ molybdenite over 3.0 feet near the oontaot

of a diorite dyke.

It In reoomendsd that the ael t potential survey beM" 4b*

continued on tho MoHarmao vest group as sulphide mineralisation

h?n boon observed rotated to a se? f potential anoraaly on the

boundary betwoon tha Varley property and these olains, nee.r the

Goulals Rivei1 .

\n adfiitilonn? \.TOC -oet of \: diinoad dri

shou"1 i be onrrlod out on i/ho I'^rboy property in or'lor to further

e^rp"? ore tho UifToroivt. -n-ariaMos. I-'o^^s should be dri^^ed 50 feet

to thu #\rt a nd to the -m ?t or hole Wo. 2 to investigate the

noi vbdenito sone onooiuitered In this ho1 o. It id intereotins

to note that the ^oiybOonito lainerii isation intorreo'-ed in

I?o.2 ho^o vms concentrated na-ii- the ooataot ot* a diorite dyke

within tho quart site horl.son. imi^ar goolo-sioal oonditlons

o:. i:: 1'., in tho vicinity of Uio Ve: s ma o ,!o.-l hole, o omo 4 ,JiOO foot

to tho noi-thonrt, wf;era a rloh moi;-bi!unlto iptei-no^

t, siot f u"1 "J y s u aa l - ted t

.

if-7-

APPBHDH

Technical Details of the Self Potential surrey;

The self potential survey was carried out on claims

held by Paul C. L'oieon In trust for Mouarmac Hed ir:ke Gold 15 i ne s

limited and Iforboy Wines limited. The claims are located In

Township 23 Range 10, sault ste. Marie Mining Division, District

of Algoma f Ontario* P he field work was carried out during the

period from June 10th. to August 18th. 1961*

The Instrument used was a 'harp V.P.6 Ground Voltameter

which was calibrated to read to Z jail 1 ivolts. A. toxa! of 22 miles

of picket lines were out and 2,573 readings were taken. The

picket lines were spaced at 200 foot interval s and readings were

taken every 50 feet, or closer.

Total j.!an pfiys Required for the 'urvey

a) Tine cutting L'r. j^ie Uye contractor 98 man days

b) Instrument operator I.e. Mcreun chief opemtor(2 nan required) 5C man days

o) Office ivork .; .G. .vclean t : nan days

1 hereby certify the preceding technical aetail s to be correct.

C. MoTean :v.\. .o.

41JI3SW9886 eel 2 DAUMONT

T OFFICE OF MINING RECORDER"

900

SAULT STE. MARIE MINING DIVISIONSAULT STE. MARIE. ONTARIO

I/

ONTARIO

DEPARTMENT OF MINES

March 6, 1962 .

MAR 9 1962TO

JC E. Hurst, ^ '—•i-i .Geologist,

"Bldgs.,. Toronto, Ontario.

Dear Sir:

I enclose herewith core logs and locational plans covering 2095.5' of d i--mond drilling on raining claims 3S.M b 1740 and 61659 et al, in Township 23 Range 10^ These were submitted by Mr. Paul C. McLean of NorthBay, Ontario.

Yours truly,

encl.p. A. Jcdouin, '•i i ri i m* .-tecorder.

4ui3swee06 ea 12 DAUMONT

Footage

Role Ho,l

^0-13.0

13.0-2C.O

26.0-35.5

35.5-85.0

85.0-11G.5

118.5-136.0

136.0-231.5

231.5

020NO.T5 TO B E REMOVED FROM

TOO oy DR3EL HOLSS E OFFICE OF THE RESIDEN11GEOLOGIST. ONT. DEPT. OF MINES

Marboy Win* Ltd. GEOU0^ ^

Bearing

"outh

Dip

-450Depth

231.5

Casing

Eark green chloritic rook, most likely a fine grained diorite; rather even grained and uniform in appearance.

oQuartzite, impure, pinkish to grey in colour.

Diorite R.C before, fine grained and uniform in appearance.50.0 coarser grained and gabbroic in texture.cuartzite, Ti^it to dark {jrey, impure.90.0-94.0 lOjS pyrite.1.00.2-101.5 lampyophyre dyke, dark groy.

TIeuvy sulphide section, almost massive Be o t ions up to 1.5 f era. 2O,J pyi-iye and pyrrhotite in last 25 feet. nr* chGlco. noted.

nuartzlte a r, before, sulphides rare. P^-ia bedding at 60 to-the core. 1G6.C-167.0 ioi?t core.

Jnfl of hole. ,,./

Footage

Hole Ho.2

0-16.0

16.0-110.3

110. 3-] t w. O

142.0-148.0

148.0-164.8

Fearing

outh

Dip

-450

Depth

190.0

Casing.

Quartzite, 1 igh.~grey and hard, al eo mixed light and dark ojoy. Tocr.l^y ^ood bedfling at 45 to the ooro.

-.G chloritic bed.'O.S Gmnitiaefl bed, pink in colour.

Mineralised zone, 1-ioiudor section or massive sulphides (pyrite) over i foot widths. 30;* sulphides throughout.

Quartzite, not mineralized and locally somewhat grnnitized.

Mineralized quartzite, 20# pyrite with the odd speck of molybdenite.

1&?tw(t-T

-8- Hole Ho. 2 eont,

^ 159.0-160.2 BolyMenlto miner Jl.atlon in

190.0 Un4 of

Core la stored In

J *~s'

bdxes at eat site of boles.

SECTION THROUGH HOLES l AND 2 MARBOY MINES LTD.

5

Sulphide Zone

Ouortzite

Granitized Sediments

Argillite

Diorite, Gabbro

SCALE:

100 O? DRILL HOLSS

Footage

Bole No* 6

0.0-5.0 5,0-38.0

58.0-48.0

48.0-54.6

54.6-61.2

61.2-87,8

87.8-100.0

100.0-111.1

111.1-120.0

120,0-126.0

1^5.5-128.0

328.0-204.5

204.5

Bearing

north

Pip -650

Depth

204.5

Casing ** - ~ Quartaite, impure greenish unite, locally a little fine pyrite* Very fine flakes of muscovite. 27.0-35.0 good bedding noted at 600 to the core. This

suggests a steep dip to the south*

Q,uavt8ite, light reddish brown, arkosic and granltlzedin appearance in erne flections.40*2 4" ooarse sulphides Including good chalcopyrite

Quartzite, dark grey, impure.

Granitised bed, pinkish in colour.

Quartzite, lmpurev~dark greyand rather massive in appearance. locally fine sulphides, mostly pyrrhotite 83.0 3" heavy fine pyrite and some chalcopyrite.

Grenltized bed, pinkish in colour.

Quartzite, dark grey and impure.103.3-1^0.3 Disseminated sulphides Appro* 15^ pyrite

with a little chalcopyrite

Granltized section, pinkish and r ax her ooarse grained. T oca! i y pat cho o of pyrite*

Impure'sediment, partly tedded tjuartzite ; dark grey* 120.0-122.5 fair pyrite mineralization.

Very heavy pyrite about 60# but no chalcopyrite.

Grading into a"soft green ohOlritlo rock which looks somewhat like lava or possibly altered ar^il^ite. Might also be a fins grained diorite* Becoming fresher in appearance from l 73 to the end of the hole.T88.0 splash~of chalcopyrite193.4 4" inclusion of graphitic sed. with a Tittle

pyrite. . ^2 00.0 Sons ali ea r Ing at 45" to the core. ~ f

of hole. v*- v

6**

-e-Bear ing

north

Pip

-580 B17.0

Casing

Pediments, granltiaed beds alternating with beds of impure quart* It e. 75# granltized. Tooally fractures well mineralized with pyrite*

disseminated molybdenite with pyrite.

Footage

Hole Ho*7

0-8.0^*

8.0-15.3

15.3-59.8 quartzite, grey, locally well mineralized with pyriteand some pyrrhotite and a little chalcopyrite. Occasionalnarrow granitizer jodu.15.3*17.6 Hear/ pyrite TOfC with 3" of about T/- copper.29.7 speck of molybdenite.31.4-33.0 4D*g pyrite in bands at 60O to the core, same

as the Adding. Ifinot pyrrhotite. A narrow seam of chalcopyrite at 32.8 feet.

34.0-35.0 About &S copper; saaras of ohaloo running with the ooro*

35.5-3r.2 Oranitiaed bed.3-7.2-42.6 Quartzite with 20# pyrite.41.5-45.0 quartzite with pyrite, pyrrhotite and ohaloo.

chalcopyrite in strings rB and disseminated.50.9-64.6 ZOOM of disseminated chalcopyrite and come

Chalcopyrite fractures f ve inlet s, . 'f his zone looks like the zone in the trench above.

59.8-70.2 Granitized bed, pinkish. Disseminated sulphides*

70. 2-113 ;fi Q-uartzite, ? ight s.rey.~ About 20# pyrite in fractures. 73.5 seam of chalcopyrite". 89.4-90.6 Chalcopyrite mineral iaat ion, about frfc 91.4-D2.4 Chalcopyrite in secjas in the quartzite. 97.4-100.0 25# pyrite in Swams. Senm of ohaloopyrlte

at 98.7 associated with heevy pyrite. TOD.O-T00.3 chalooj?yr?*-e.T01.0-T02.7 Good chalcopyrite mineralization. ^06.0-107.0 reverai narrow seams of chalcopyrite.

113.2-1 71.0 ^.eds. becoming puxed quartzite and dark grey beds andpinklsH graniticsd bad**, idsseminated pyrite, pyrrii4tite nnd a little chalcopyrite.T58.7 ~ npeok of molybdenite. ^^ 160.0-164.0 20# coarse pyrite with some pyrrjiiX^lte andr\

a traoe of chalcopyrite. ,- f&X" rtc.s\ot

171.0-195.0 Mixed sediments as above.

195.0-217.0

217.0

lcopyrite. ,- 0

e **co*

and97.0-1 97.6 chalcopyrite in fraet

207.0 2" of massive pyrite .

of hole. j ̂

-3-

footage

Hole flo.8**

0.10.0

10.0 -18.5

16.5 -35.3

35.3-97.5

97.5-145.1

145.1-152.5

158* 5-1 58.P

158 .8-166.3

156.3-176.5

176.b-a70.0

Bearing Dip

South -40 0

Oasing.

Argillite, darfc green and chloritic.

Depth

454.0

partly granitised qua r t site, locally bedded at 60 to the oore.

dM *

Diorite, dart groen and relatively uniform in appearance.36.5 ~ Narrow seam of ohaloopyrite.50.0-91.0 becoming ooarser grained, very freak looking

gabbro. 91.0-97.5 becoming xiner grained, similar to the top

oontaot.

Jttpur'B quart a it e and granitizod sods, oome~ned. sootionsof relatively unaltered quartzite. Ilinaralisod with theOdfl seam of pyrite and monor chai oopyrito.126.5 ~ Chalcopyrite and pyrite in soama.-13?. 0-1 39. 5 Q,uarteite with ohaloopyrite, njphaloriiio and

137.5-139.5 Fairly good~ohal oopyrite in seam running up the core, a! DO dioo&ainated. \bout 1^ ou.

Tight grey quartslte tied oofltalns rraoturea sphalerite and Q little ohaloopyrite* and some galena. Mineralization in fine, about 5^ sulphides throughout.

Quartzite.

Argil i it e, dart GTBOQ and chlorltio. Broooiated and carbonated at i 65. 0 feet.

Granltised sedjjvmts.

^oertzite, ll^iht ^rey with dark at 500 to the oore looaTly. ^ulphidea 203.0-204.0 Minor sphalerite."" 242.0-242.5 Tairly heavy sphalerite" in 245.5-247.0 10-,^ pyrite in bedding planes

bedded

45O to oore.

270.0-304.7 quartzite, nJiieralised with about 5# disseminated pyrite pyrrhotite and Bone ohaloopyrite, Took^-^bnil^^to the quartzite in holes 6 and 7. (^, "' \-.c.^v'J 273.0-275.0 Tost oore. \^*- - \\-- ^ 286.2-287.0 Tost oore. ^ ^ * Q' ' *v*' 289.6-290.0 lost oore. ^0 ^fv^ ^ v*- ^ o* 297.0-297.5 lost oore.

s '

Hole Bo.8 oont.**

304.7-454.0 Quartzite, impure, greyish in colour. Tho odd narrowpinkish granitized sections Quar t rite is hard* and contains a High # of quartz, possibly rextal^ized. Only scattered sulphides present. Tooal^y tedded seotions betvrotn 600 and 45 to the oore.

454.0 or hole.

gootage

Hole 9o.9

6-7.0

7.0-15.0

15.0-33.0

33.0-54.5

54.5-173.2

Bearing

r.outh

Dip -450 253.5

Casing.

, dark e^oen, sinilar to t ho material in end of hole No.6.redljaenta, mixed argillaceous chloritic dnd impure quartzite bads anC. granitite*! bods.

Pinkish quartzite bed.4*——

Grey quartsite vritb. occasional narrow --r i nit i a ad buds.5fi.5 4" of \tyj pyrite.83.7-05.7 GranitizoA ted.Tt 9.6-726.3 Pink c^anitized bod.153.0-7^7.0 Herrvy pyrite with somu chai cop.yrlto , 40jb

sulphides.f56.O pyrite and pyrrhotite, if8.5 t" seen of pyrite.

173.2-E01.5 ^uartaite with her.*// i'ine disseminated pyrrhotite.Approx ffT pyirhntito throughout the eone. GHal oopjritu associated with the pyrrhotite, boinc -bout 1O^ of the pyrrhotite miners i z at ion.

801.5-B53.5

E53.5

Footage

Hole Ho.lO

o-e.o6.0-82.0

2S.O-26.C

oa* hole.

f-oirth

before v/ith only soat^roA nulphides.

]-*.Ss S- A*"~b**0 .^'^^^'^•v

O^- o^*. 0 S27.0

^

^ickish red gractte,

fiorite intrusivo. Tine graiued and sheured.

-5-

Hole Ho* 10 cont.

86*0-87.8 Oranitlzed material.* ̂26*0-117*0 Intrusive, fine grained at "about 42~feot then becoming

coorctr. Park Groen in colour similar to tho intrusive in hole no.8. -Gabbro or diorite, uniform in appearance. 56.6-3-975 Fault zone, Breoolated with fault gouge* i. 0S. O-i 17.0 Becoming fine grained ao contact approached*

117.0-128.0 Quartzite, whitioh 6*07, bedding at 600 to tho oore.

128*0-124*8 Oro nit is od bed, pinkish in colour*

124*8-152.5 Quartzite, imp i ir o light grey, locally bedded at 45O to tile oore* Occasional narrow granitic od badb.

150;rO some serais of pyrite.152.5-1 TS'.O xrsi^llte bed dnrlr. greenish grey. ~

155.0-164.0 Shearing running para? "" el to tho oore.

173*0-174.9 : iiar t nit e , pinhffh with seome of pyrite.

174.9-205.2 Mineral izod sorm in~lmpure~quartr,ite pyrlto, pyr:i:ot;ite "^jhalerite and looa^ly chai oopyrlte. 192.2-195.5 Drko, brecciated and carbonated.

205.2-327,0 g.uart,s?.te , l leht. to dark grey Jn colour, bettted at 45O tu the oore. Toes"1 ''y pinkish sections. Toc^ erg. beds. 215.0 fine sph^^erit-e in j)atoheR. E20.0 fine splip^erite in patches.

327.0 .2nd of hole.

Dip Depth

Hole no.11 ' outh -45 0

0-C.O On c in,;.

6.0-79.2 Babbro, flark. ^eenich, iridium tn o oar c ^uinod, freoh 5ji appearance. OcoasJonal carbonate 75.0-71-.2 Ba c aa ins fine grained

79.2-92.0 nleliiy aitoTed scdi-ient , wenmarapoBite locally, i ooslblx. . a'rK84.5-92.0 Brecciated fau^^one/withvfaul t gouge

C " '

98*0-128.0** *-

138.0*146*5

146.5-163.2

163.2-175.5

175. 5-1 Ci*;. O

104. 0-202. O

rfM

202.0-218.0

218.0

Sediment s ,-nixed flark and pinkish bode, still altered particularly the darker beds which are ohloritiaed.

quartzite, dark grey and Impure.

Xrgilllto, looks much l ike fine grained lam. ~ 156.5-160. 7 dyke, dark brown lamprophyre , simitar teT

dyke in the mineral iaad x one in hole fto.10.

quartzite, partly granitizefi, pinkieh in oolour.

Quart E it e, dark ^reyt Ixipure*

pyrite and pyrrhotiteminei-aliied with about In f ree t us. ea Kiid irr ceamo. 194.9 A little oha"? oopyrite noted in stringer of

pyrrhotite.

, oalr uinor ^

j.nd of hoi e.

Oore is stored in box93 at the site of eaoh hole.

,4 -^

,

"31-

^.v

lV*

. v

S, *.^

^

.,^0

**

'f

if

i

6^,

M

f:

o*

o

1 ,

0

-̂o fe

'k k

TWP 23 RANGE XI M-1470 Z

161662 teteea 61664i~ — 4.. — -, — — — j- -~ —

en to

41JI3SW0006 0812 DAUMONT 200

N

PLAN OF DRILL HOLES

McMARMAC RED LAKE GOLD MINES LIMITED

LEGEND

Sulphide Zone

Quartzite

3 LJ Granitized S ediments

Argillite

Diorite, Gabbro

SCALE'-

l inc h ^ 50 feet

F EBRLJARY 1962

-43*

^ a3

313

A ,3

o-" 5 '

u-

u 4

o -'

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8\

?;

43'

-3

3

-20 1

3

O - 5 B

5

00