m

Blind

010

GEOLOOI0AL H2PCRT

on tba

(Quirke Lake Property

KANIWiKI KID URANIUM MINING CORF. LTD.

in t be

Blind River Area, Ontario

BE R EMOVEDbITHB OFFICE GF THE RESIDENT

GEOLOGIST, ONT. DEPT. OF M|::gS

SAULT STE. MARIE. ONT.

JLLBSRT HOPKINSB.A.So., P. En g., M.C.I.M., F. G.A.C.

Consulting Mining Geologist

Ontario. 20 August

-' * s.'jl^iW^'flniifll'M't* '; f)f* ; n1 n4it.tM*h- ry.y\t'l^)!S,* *' .area/of abotit

,,, . v ... ,. jr- -j^,. W j lies os9mi3j9 northwest of quirke lake, half a :'^;/ alle south of'"Little tyii^rlce lake, nad 29 ttiriailea northeast of 'the ,v

of Blind River. .TJie-jiouthwest corner of t bs ^niwalcl Kid, property li ona title northeast of- thu hew five-oompartftent shaft: of the l lake ^ocperV}!'of A.l^om-.l?fanluni ii3jieX J-td. which property la

i-to euftd ooiitfc of the i*miwelci ?Ud.property. Thla is In the au or tor of t o wnsh ip 15 O, fil lad River area, Qud bur y : .lift In g

This property raay.be ra^ohod by dri^in^ -from the main Sudbury- hi^hway starting threo miloa east of Spraggo station on the C.P.H.

and t;;.5Pjy* rjorthward abput thirty wilJo s along th^ newly-oonstruoted road to 'the Ax^olV Quirke laVe ahaft area, and thwioe by trail for a nilo i5vT'*heastward'. Tite: ^oniwaki Kid property u^ay sleo bo raaohed by flyin?: fron tlie Lau-obna Airway* Ltd. airbaso at Alcona K;ills, Ont. on the Ju4hiry-Soo highway to Little Q,ulrke lake, a f.iifht of 26 railse, and thorqre by trail for half u wile southveaterly.

roport is based on tho current geological survey, and. on fieolor.ical reports and repu:-

•^"•••.t

the To l

Geol. ^urvsy of Canada - Lfeaioir 1AJ, 1925, "North Shore of Lake Huron"and "Blind TUvor" RQOlogical rr^p no. 1970,

by w. H. Collino.Ont. Sept. of Ulnea - 34th Annual Heport, part 4, 1925, "Tho tfhiake;

Ijako Area" by G. Vibert Douglas i L.F.Hindi*.

Geol. Purvey of Canada - Konioir 160, 19?0, "Tfie ^isappoarance of theHuronian11 by quirke and Collina.

* " " " - "Canadian .--epoaits of Uranium and Thorluza"by A.li, I^ang, 195?-.

" " " " (RaSionotive division) "Prospectinp forUranium in Canada, 1952.

Ont. Darpt. of uinos ~ Annual Hoport, 1952, part 4,"Geology ofBaldwin twp." by Jane a E* Thomeon.

" n " " . Preliminary Report no* 1953-2, "Geology, ofLong and Spragge twpa., Blind Hirer Area"

byjs.^i. - -

———————————————————————'——— ^^^^MHMMMBBBBBBS^S^HI

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Proo^brian terrain of thoA^riiWflk l Kid property and s .generally 'poverod by thlalr-soattered debris of glaoIaA

^0fcs.istiiig o* vifiuiue? drift pevriipliy scwrtsa loffiiXljf MF *Ji* alce'fliiron waters in ea rly nR 90^^*^180, Ab&ro tea glacial He* extwislva rldgea of Pra^eBibrlen rooka wMoh follpir a

aireotlonaX trend variously nortb-Boruth at the south iry' ar*a and eaet**' ^ In the oojtz^al acd norttiara \x3undary ' '' '

y tho deer liar Precambrian rocks of this area comprise a seg-•JKiJfi.tr oT the oitaisivfls Laurentien-Alstonan granite batholith which is flanked on ths oouth by a synclinal structure. This consists of

^I&a^bniian strata. forning a larga structural baoin oif^it to r4in^ niiles "in. width and over thirty mlloa lon^5, the syncllr.a terrainating easterly- a,t ffbi sHey lake.

"? A belt of Keevratiji la^ae is indicated by pravioxis toappinc to occur in tbo vicinity bf the aast ^nd of tho Maniwaki Xid pr^orty. A preponderance of plutonic dyfco rooks over thts volcanic type irfts the condition obsarvod on making the present geoloftioal flurvay. The dyke roc He are typically aassivo, and medium---t o oot\rse-^uinod. Uertain of *b9 lar'gor of tt v r,ibbro-diorite dykes whioh traverse the property trend f/outtoaet, thus forir.1 n;; a link rith oxt-jsisivo siuilar basic ^eiceeJiQ^ar gabbroic dykes. I oat nctnble of ^haso is ono r-flii-oh. la terj ill ea in ien/rih (west nf Ten idle lako), o&d tlie liabase dyV.e which traverses t)ja iluroniftn^Btrnta on ths south shore, of Whiskey

crossing vif. Urcnpbell island and thence oaatrard (seo the Lake sheet).

Tho granitic rooks are typically wassivo, aadiura- to coav. - ?d, ant'; rad in colour, notably the large hornblsnde-cyenit a, bose-

likc Intruuivos. An example io to be aean at tlio cl.oro of Kid Lake on r ickfjt line 2,000. Oranite of a gneissic typo io notably locking on the urcportjr,

;)f int-iroat with i*egard to basic intruoivas arc tho qxairta- diq*it*s and lariprophyree, t fee latter atteinir^ u width locally of a hundred feet on picket lino 4,300, southwest of Jog Lute.

Volcanic rooks appear to be United to tho eaot boundary area. Hero a minimum was seen of typical volcanic s tract UT o a such as lava flow line indications, amygdule horizons, and pillow-type struc tures. Tha intermediate lavas, duoite and rhyolite were 1.10re readily reuop.nized, however.

A considerable number of Algoman porphyrytic plutonic dykes were encountered, including a comparatively largo quart*-aplito porphyry at the 350-300-foot hill on Um southeastern corner of the property. The outcrop is throe hundred feet long by more than e, hundred faet in width.

, v Th* geological history find relation of the aereral epoona

in *hiftx j-sport can ^e suaoArized in a table whixih is drawa up here In ;reauiB.e briefly as follows:- . -

'. ., , . -

.laic* litaron, df' '

, cmd poasibly•- '" , . - ..x- 'art fiihgula,rly" '

, and" .-- ' - •, basic; -" "-on ths

, , , .' ;11 ^ifiartz-porphyry, fsldapAr-pdrpliyry, quartz- f o 3xl spar-porphyry

' ' apilta, d

i nteroala t od with andesite/ dacite, and rhyolite,

P 3-T.a G L O G Y - . -

* of t ho chief rook types enoounterod Aurinr. the asr^ing of the fcanlwaki Kin property sill be briefly in the ordar of ^eolotftoal aee, startiBS with the oldest:-

Andeaite: This voloanio ia seea aa a jBaditun-sre.ined, .or variouslyfine-grained, -massive to scsii-foliated rook in '.rhioh Q high

proportion, approximately thirty percent, of pla^ioclaeo I'oldapars OOP prise tiie rook 21 in oral a, the balance being the mafic ir.inorals. Konoe ths andosite appears ae'a dark groon to deop s^een colour, or is paler where transitional in oorupoaitlon to daolte.

Msalt: Tha basaltic phase of the volcanic roo-rs is dtrfc green to blaoH, lu appearance, and uaxmlly. ; fine-era i nad-, tha roo'c ooo-

riainr flcvra of varying thioknosBee. Vow oxnntplfts, only, were rooof-p.lzed on the property which raigfct be tentatively ascribed tobasaltic origin. The uti&ttlt ahOWa aconstituents.

I'aoite flov.'d *ore oboorved at Sight lake aorosb a naxiaum rdath of twp hundred feet, loentod botwaen andesite on the

west and rhyolite and '•amphibolite on the east side of the laVre. The rook is. fiiii3-tj;nalnad aynl nasoive, pala /^reon with a partially aiaorphoue silioooue appearance, ahcwing a proportion of felspathlo oonetttuonts of pop^ibly thirty percent. iDOlated (juarta phenoorysts were Hote^Voocasiona ly, whioli is oharaotoriotic of daoite.

3 '

ffSRirj? *v-v^.-.'^•v;:*"^^'' .a.:.-?'-"".*'- ' " ' , ','m^mmm^^' -^^-^feiipis

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mapped, on, t he Jien Iwaki Kid prop arty , - ,^ -..to dsptii of the green oolouap .typlctat re* feispathio; ponstitijeiita of toe

bf dark green hornblendea beln^ uacwlly about.medluDh*.to coarse-grained and

* the pexceatage of. quarts phenooryata varying wi dely f rota ' " tft;25 o* 30 perpent. There is a olear pink variety of

appears at the west side of the proporty containing a quaJrtz. content.

, , Syen'ii0v Ifhlfl ooour-e aa ftn'intruaive oloeialy aasoolated

and appeara to iiaye alternatively ponotrqited t lie granite .fts inflioateid on thn map { sea lino 800), An -ix.^apl3 of poseibly a larg* size xenolitU is t let t traversed oji l^Jie JfeOO, where syenite aa a boss^dy^ce surrounds a granite area four hundred foet in diameter. r Tlxe' ayoiitaR are typically a ooarse-prained rook,

dark green to pale red, or varying in places toproportion of tno two aa jor" constituent rainerals, feldspar aaid

being almost e4"aal. Silloeoiua varieties occur uot ooixtalnlng quartz phenoorysta to possibly fivo or seven

percent.Aplite *jnd quartz-porphyry: Thoao li^ht chalky or bei^e-tintod

rooks were noted to ooour sparingly, atconsiderable intervals of ej*too, ohlofly at the east Boundary area of t ho property, ifhero t ho intrunlve nature of tha rook is not clearly cho -an, leading a doubt that a volonnlo origin mij4lt bo proven. Here at iho eoutheast corner of tho prorierty on line o, 000 ooours an aplitio q-iartz-porphyry exhibiting" a porcelain-like ^roundsiass, and containing numorouo quartz phonocryots which attuln diameters of juat over a sixteenth of tm inch.

Qua rt z-f aid spar-Porphyry: This Intrusive olutonlo nppeara aa a coarao-pratxiuil diffaronfclat^ of a r^nitio !U'*lt at c'opth, ami com prises a rook reaonbllnp granite except for t ho presaioe of u ground- mass raottled with a hornlilor.rtlo-ohloritlo oonposition, In -shloh ooeur rcll-cpiCCd Q\'u"*i"vi plitJi^uui voto, approAii*** tirvj HOWO fiftwwn to iwsmiy peroont of the rook,

Dykes of foldepar-poinjhyry outcrop in few plaoea on the property, the widest dyke Indicated being

that noted at line 3,000 near the north boundary. The rook appears light groen with a groxui'Uaaas oonsifitlnp, of thirty to forty percent nafio silnerolfl and felapathio ooi;8tltuents, the bal&noo comprising of foldflpa? phonocrycta which average a length of only 3/?2 0^ aa iSOB

^

Amphibolite and Peridotite J Comparatively large composite dyke,* of 'awphibolite-poridotite oro aa t ne length of

iba property, following a direction north of woet. They are closely. . aasooiatdJ .ac a' segregate froci large ^abbrordiorite dyke*. The rook fariea from f iu^- grained through laediun-, to ooarse-^grainad texture* X& the latter a feat e, t ne rook le oowpooed of -, approadlBiately 95 percent liornblende crystals, variably oriented, wd measuring In er cess of

of en laohlin -Itngth. Th* peridotite is obaraoteriBtioally

mimimmt^m v**^1 .Vi V 3- i.**? **fc - *Vfc-;'.Tj; T* 'ri ^ . ' ^ -J ^ ' Jf ' ' . - ;

*l*o not*d to? be altered to a p*rti locally* 'She; /lattar typtof ,

o^;^

\i'X'

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jprcjaia.sat dyke of this type'of rook occupies thei* bf'*\ooitfai ridga, *nore the' laiaprophyre oooiiri

^•^csi^-i^^o|tBi^v'^'to^^^iwr^tz-diorii*'. {^oe lines 3^00 - 4800 on th* ^^l^i.^V^^t^vThe''laJa^rophyre attains a width of 150 f set, and on0 tdytct^ia) tra,oad^aatT*B*d ;to JSight lake, ^tffi rook is racogoized whare

tiBi; of, thtJ?ty; JQ forty p^oant; foldspare* The balance iare faiiie^Al pndnooryata which effect rosilts in n rooK dull-dark in colour with e minimum of tw to fifteen poroent of ground-

riliVix* .Vyritos wes obBervgfl to occur in blooa or cluatftrs in the ro^-k locally*

; i*ylcee of this iaaoliuu-grn Inod. rook occur south- :? : cant rally on linos J-600 to ?oOO and o.iatw&r-d. l-or

•At/.'iilfjjt lako t.h^y attain, a uaxlia-u^i v/idth of a hundred foet or moi'ia loOially, This rook cannot bo described as a typioc.1 . ;uartz- diorite, but it bwe^'s a roaociblanoe to amphibolite owing to Uie dense hcj."nblondio tulnoral oomposition . .\t diBtr.irt intervals onn b* fl*on iaol/ited quarts phenocrysts, u^d occasionally sporadic pyrites 3QaEi8 or crystals*

''foispathio oonstituontB oi* thr. rook ;iifiht ^vorape fifteen to twenty pereion t. A oloeely ooaparoblo quartz— Morite-r-orphyry tra-

l&npthwisa the ore host rook, "ouort-broceic." , at the ooppor mina property near i'.ashakowie, Ontario.

Thece sflditamts wero r.ot ohoorvod to ocjcar on tho Kid property.

Liorita-porphyry: A dyka of thin typo outcrops clo^.o to t'-e Alcornappears to ntriko north\vosterly, ^thero ti ra La t ad d.vk-s t?au uoted in e JUir^or oui^roppinp; Vrnoll on ti*e adjoining liolfoat l.inoo Ltd. pro}i0rty farther north, ^iorite-porphyries of tnis kind in ?hi 0)1 flodapar pUonooryats occur ruranduntly ftttaiainf; lonp.ths c f cv/or b/ilf an inoh, havo befen genornlly aaoribod to tho t-.alloyburlan tspoob. in the iirdlskanirwr t!istrio-i,, TV f-.o re the dyksn woro dated oy ralation to tho :^ronion strata.

Gabbro-dlorlto, Gabbro, end ^iabaod: ^ixtcnaiva, wide b'-sa-iykea ofe.abbro—diorlto ooauT)y al;aoat half

aroa'or thft ;Maniwaici f.'id proport.y. The -rock o:f th^ bantral lyice oa-a-i'a typically modiroct- to ooarse-tfra ined, oontainlng variably . y t j .fofttyi .porooat felapathio oonatituontB, Wieae aro duhedrally

4intribtitad ,th2^6u(5fciput tho roolc, oooasionally instituting a dlabaco rock typfr, ,in. whlo'h au abtmdnnoe of tbs; faldapara ne'y t*e noted.

^.

df Half .^irt-' IflfiLif ytoi^xjei are' o^ dy&afr .in vhiofo a 3fcepoAdernnoie of

have. apt-' '' ; "aa.

ai ff arent Ut*S. However j?9' ;iBfty be proton by geological fact era to represent

jKy ^^ upon popfltbld.disooydry of suoli ohoraotoristloa' ''- ' ',. , erf the gabbro-dioritee to*in

see the'dykes to the oast of Kid lake.; Tho ohilled. d large dyke can be seen against sya\ite on lino a 4400

'•and 4800j,, at IcoatlolB a few hundred ffjot to the novita of tlio *Jase

narrow, dar^-tinted, fino- R:r{iin0d trap ped. Th6 dyicoo apparently * flpyeaent tMe

i')ykes i A number ofdykeo wero mppe

star-^ of dyk* inject l on e. TheeVs, like oarliftr.dykes, follow a aortDweatorly diraotion. oaverttl or tho trap dykes can bo scon to travorco di orlte at a locality, lino J200, HOC foe- to the east of Kid Is'fQ* They 'a loo traTorajK ^nsivo oyonlte.

a a, v g t u H. A. L cv 0 L C G Y

of ^truoturaldii'^ction oT dyke injection

is ovldcrit on objJarv^tion of ttio accompanyinfj geological ottp of the Kid property. This strilces variably oast-woct, to north of

and northwasterli', tho majority of tVie Aylceo, notably too ooara-onoe. gabbro and amphibolite, trend! n# northwesterly. A

ouooecBion of pintonio rocks injaotod across the area of tho property Blgnlfien t.viat it la locatod upon tho locus of a structural line of

'waaSoiess through which raa^^aa molts fro..: abyssal depths nore forood to or notr surface at iutorvnls of tlrao ovar a lar^a part of all th*'Prootinibrlan ora*

o ton i ..Suboequont to tho epooh of dyke injootion,

and Keweenawan oottprescivo tcsctonio foroos vrero applied during a period of ucuntain-bullfiing goologioal events, isfcioh resulted in tiie dovolopE'.cnt of nunerous eomi-flhoared or slieared, and foliated roo'k oondltiona acrocs garrow widths of cot Kore than a few feet in width, locally, -An example of this lalRht bo oited^ ^oh ae diorite In oontaot vith emphibolits on lino IbOO couth of Kid lako, and fal4.spar^pQrj)hyry oomi-foliatod in a woat of north direotlon on lin* 7600 "*t the north boundary near tbo Baseline. A onloritio ahoar aon* , whioh le narrow, traVoariiea an amphibolite on line 1200* '

' In cotvtr&at'to oojaproflcivo differential directions bf move- a6iit,wi th, f Dilation "Jftnd shearing, a oontaot aone breQola type of . . ffli|reitatite;Was ^fid wJiere a trap ^yke interseot , a, syenite on line 7200', .300 te*t:;tp /tof.the ,4ojji^w .u,-'.- •••' -- ' '. 1 -' '' : :^- :

.#i....-,-:v/-..ttr

nwpr 1ii.*h:f.)APio4jBr ottl&Uenea ."co

6f ' -Vv.

'^ioi^^c^'^tis^i'''-^*!!^ 5 Shis tttu^bi^seVtyr the cool* "tOTp-of'.ttift.'.piutMib. dyitfts 'pf/, large 0iaby such aft th*

i;•^.ClBi^l^^8j^^.^o•t/•W:^^H%* t <9U!L3P:ta veins over two *, ; ^sf^^tgorei'nap.pad /^'ar^'c^'served .in outoyops* Xto prevailing '^ ' A3^^^^H"^Jr:-'*'^v :^^^'?--1 via'Bii' appear to be feet of north aafi

•-'-'"'Y*' AA'dxAtttpXe la^a ; tJureft-inoE Jinarty rein^br. line 800Bjiite-nenr^by. tb: - ;a 'fir o-ixkoh quarte vein which strike*

of "noifrtti* Aloo exoepti?mal is a three-inch o^uftrtx vein OB line ^V4000v:.iouth y, atrilciflg oast of north* .Typically ( a six-inch quartz vein

i'Iliio B000 ^cuthi etriKea to tlia v*eet bf ncrth.

2 CO 1C O K 'O LO ft- Y-

; . :;V; Huronian etrnto were not observed, on the koniwalci :lid property* ^v-'Phpee nisalnf! aedimontc are the usual favourable boat rocks for

utGjilujii occurrence in this Blind ^iver area. Likewiao, the Ooiger couiater t\iirvcy conducted f;irrtulttalooaEiy vith tnis gcologtoul mapping

no -i-uil" of

I'lie extant of vleiblo oulphide mi nora libation ispvrr!ictito, anfl chtdocpyrltos, la "the rorui of thinly

anl isolatad clusters, occur ooro or loas ubiquitously •within certain zonefl of the basic intrusives, notably euupliibolites, .peridotlt^s, quart ̂ -d lofite, and lanprophyre in t-'ie high" ridge terrain, which ia ocntT'ally located on the property.

-•oaeibly related to this typo 01' r-insr&lizntion, tuore oan bo seon a fifty-foot length of more or leas discontinuous thinly ruatod OORS only five to oix feot in ".vidtlu Thia travoreee a "wide onpliibolito dyko on line 1200, locate to the southwest of Kid lake.

Jhalcopyritcis-, tentutivoly iaciitifiod, wac not od to occur aa a contitituont of pronito on line 5^00 in ^he seoond outcrop to the north of the stream.

C O y. C L U 3 I O .11 ^

1. 'ffco look of Huronian sedi^onts, notably ^isaiusaf.i quartzite, the usufll nost rook for ureir.iu^ or^s in this area, plus the negative results obtained froci tho concurrent geiger counter survey, indicate concluBlvoly tfmt uranium is not likely to occur in

quantitiee on this property.

i!. Certain observations uiado during thin zoological iwrvoy nay be ifeaanarizod as factcu'a favourubla to the ocourranoe of juata llio sulphide minerals in the oheared oeotion of tho plutonic and vol canic rocita of tho pro party, via.

(a) A wide range of large-scale dyk:oo^ boaa-dyices, and segments pftljs Al-ouan grnnita batholith occupy the main area of the property t both uoid and basic dykos being represented by aevar&l varietieft of rook types. Volcanic rooks irange also through bast* It lo typed to rhyolitoe. The prevalenoo of nucierdua plutdnic rocks the. axiat^naV pi? a.major line, of atniotural iweaVcness

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e. of tlxe City of , An tneJSjyps^SiijtJfi'.iP*/..'-- ,, 1*1 , *t*H"** * wLffrwwio f vi.i,.'vuD w * *jr . vff \*Mk'*S^^4*^asSiri-nfliA or- Ontarici^ Ab 'h(M*'*lW'. rt*^*4 -r^ •*^**t^ Alpp^;K?v^^ ;;:|4 -;x,-^.^ . ; f,:,.^•^ft-^...'-I. .imsi^iiffuatierd -frosn tie Faovlty of Aypilefti ttoiocQ^and. ^S* .- , ! "' . ~' ' * 'i j .-i . l * ^ l; ".' -' iL -* ^ - ^ ~*d - i4i"' ^T. * - ' ' *. ^ * i ^k r** '.. . A- J^. ^y^** **' - __ \ j . *.. -.fcof the

fV in fc'of Toronto iUx JL937 with'

. . f -:ilva Aoaociatlon of i-rofassiojial

of ^Iv6 ^r-3Vtiwe of ^ntario; of tho Gon^diaji Itiotituto of ^Iniag fcmi ^ata-Il^gy; end a Follow of the Geological

of Canada.

3* I' havo boon praotietng the profession of raining am goolo^y ror ten

4, A rt;, ort is bae*il on the geolcgioal trQveraing and napping icttill by my tia ia 1st an t e and a.elf in August 1954 on the

id Uronitas ^ines Ltd, property, on ay eondral of tlio !3lind iiiver tiraa, and on the publishede^c'loEioal reports and aana referred to underin this rot)ort.

'I "hold no intoro^v, financial or otherwise, In any of the properties, stares, or sacurltios of Maniwaki Kid Uranium Sines* Corp. -l-t'J* , nor do I orpoct to rsooiv(3 any such interesttherein*

, Untaric, 20 August 1954.

Albert nopKinaSo., P.iSnR., f .C.I.M., l*. G. A. O, Consulting Mining Goologist

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, ITHE OFFICE O~ T! I" FCTlLEiiT

GEOLOGIST, C::T. r-rv. cr MINES

SAULT. ST.-:. r.'.Ar.iz, ONT* S

SCHEDULE "A"

Dates worked and names of Menon Vintern Mining Company 1 a Job

HA? IE

L.P. Kendall-Leicecter

Gerald f-ienard

Walter Mintcrn

tt n

Jas. Clavin

David hainville

Harold Darrach

Joy Dickinson

A. Gibeault

D. Suffel

Lorne Deocoteaux

A. Irabeau

llEwrr/uG Kayrnoncl

H. hoy

A. Puquette

E. hay n: one

hobcrt Coco

Frora To

25 July - 13 AUG.

25 July - 13 Aug.

19 July - 26 July

2 AUG. - 9 AUG.

25 July - 13 Auc.

25 July - 13 AUG.

17 July - 12 AUi..

25 July - 13 AUG.

17 July - 24 July

17 July - HA' July

17 July - 10 AUG.

17 July - 12 AUG.

17 July - 12 Auc.

27 July - 31 July

l AUL. - o Aug.

o AUG. - 12

25 Jul;; - 13

8 hour days

20

20

3

20

20

27

20

25

27

27

5

7

7

277 nan-diiv:;TOTAL

Divide- by no. of claimc Ib/lluj can-ii-ys

c-qual 6l can-dc.yo per c lai:

GEOLOGICAL'A

MANTMKI lTUOCATI

SUDBURY1842l SEPT. 1954

*- " ~f-v "~ — ~~t ~

849 /^J/f*

CENTRAL

LAME

3200^7 : 3600'

W. BOUNDARY LINE

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OF

JANI

WAK

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URY

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PT.

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4400

GEOLOGICAL AND TOPOGRflPHICJiL MAP

PROPER71842 LOCATED AT QUIRKE LAZE

SUDBURY HIKING DISTRI C T

A.HOPKIKS1954

6300-e

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