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4iNi6SEeeea OUILLUCI SAUNDERS ^*-i^-;;--"-.y7' 010 'T--:;~:a;

THE CONSOLIDATED AND SMELTING COMPANY OF CANADA LIMITED;

^r^ Exploration Division

N.T.S. 41-N.

Eastern District

ELECTROMAGNETIC SURVEY

LOST LAKE (NORTH) PROPERTY

TOWNSHIP 28, RANGE 2 2, ONTARIO (QUILL)

June 25, 1965 John M. Hamilton

SUMMARY

A horizontal loop electromagnetic surveywas done to check a known conductive zone on a nJ/fe-claim group optioned by Cominco from the Algoma Central and Hudson Bay railroad.

The position of the conductor was confirmed, although its indicated length was reduced from about 1000 feet to about 1200 feet. A drill check is warranted.

INTRODUCTION

Nine claims, number SSM-66988 to SSM-66993 inclusive, and SSM-66994 to SSM-66996 inclusive, are located in Township 25, Range 22, and can be reached by air from Wawa (32 miles). A one- mile trail from the north end of Lost Lake provides access to picket line 20NE. The claims are held by Cominco under option from ( ) whose staff carried out geological mapping, a vertical loop electromagnetomecer survey, and a magnetometer survey over the entire group on lines spaced 400 feet apart.

ELECTROMAGNETIC SURVEY

The present survey was carried out with an (Minigun horizontal loop electromagnetometer, frequency 3520 c.p.s. coil spacing 200 feet, by J. Hamilton and B. Bentley on June 11, 1965 Reading interval was nominally 100 feet, and this was reduced to 50 feet over conductive zones. A total of 4,000 feet of line was surveyed.

Conductive zones apparently join in the manner shown. The strongest anomaly, at 28E on Line 28NE, has excellent conductivity. Apparent depth to top is 25 feet at that point, and indicated depth is the same at Line 24 NE. Apparent dip is south, increasing from 60 0 at Line 28NE to steep at Line 24NE. The conductor has an indicated width of about 20 feet at Line 28NE, and electromagnetic response is compatible with thah obtained over massive sulphide bodies.

This conductor should be tested by collaring a diamond drill hole at least 350 feet long at or near the point 26+70NE, 3+75SE. If this drill site is unsuitable, a new site could be chosen, within 100 feet of the present one, along a ^.ine parallel to the indicated conductor. Bearing of recommended hole is 350 0 , dip -45 0 .

2 -

i 5 There is ho magnetic anomaly associated with.this conductor. Magnetic anomalies in the area trend northeast.

CONCLUSIONS:

1. One conductor, having good to excellent conductivity and an indicated width of up to about 20 feet, was found.

2. The position, length and attitude of the conductor are believed to have been determined more accurately than was possible with vertj cal loop data.

RECOMMENDATIONS

One drill hole is warranted, as outlined in the section entitled "Electromagnetic Survey".

Submitted by:John M. Hamilton Exploration Assistant.

Endorsed byGeorge B. Tikkanon Senior Exploration Gepphysicist.

JMH:heJune 25, 1965Attachments (1)

Exploration Div. MtlTrail

Chief Exploration Geologist Eastern District Property File Toronto Office JMH

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6.

2. Rock tynee encountered in diamond drill hole;

A) Altered baotc volcanics

Thio is a dark crey medium to Cine stained, fairly hard' rock, moderately well foliated, Calcite ac veins and elongate flecks parallel to the foliation is conmon. The rock is chlorlti- zed either evenly throughout unit, or a s narrow chlorite rich bands parallel to the foliation.

b) Hornbl onde r.abbro

Thia iis a dark green, coarse grained, massive, hard rock, with well developed large interlocking crystals of about 601 hornblcndo and smaller crystals of feldspar. The relationship '.of the gabbro to the adjacent units is uncertain. A opccimcn collected frccj a nearby cr.posuro that had been napped by AC and HDR staff aa part of a diabase dyke resembled exactly the gabbro from the core. Although tho change froa the gabbro to adjacent unita in the core occuro over a very short diotanco there ara no chilled contacts. Thus if these gabbro unito arc dykes eorae assimilation with ourround- ing rocko muot have taken place.

c) c) Chlorite schict

This rock is unlike the chlorite schists interoectcd on other properties in colour, grain size, and texture. It is a medium grained, green, highly cMoritized, coft rock with a wavy crcnulated foliation.

3. Minaral.izntton.;

Tracea of pyrite and pyrrhotite occur aa small diob- cainatc-d specks and crystal.', alor.2 parts of tho volcanice and gabbro. Pyrrhotite also occurs in the volcanics betuecn 120 and 128 feet a a :hin irregular veins cutiuated at 257. over the 8-foot length. A few 63ull scattered blebs of chalcopyrite occur in the volcanics and gabbro associated with calcite veir.ing.

4 . Sarp.nl in^:

Hole Mo, Ncnsnrcr^nt

DL-1 120'-12i}'

Assay Width Dencrintion Cu

3' Altered basic .031 volcanics with Po veininc*

Ni

Trace

5. Geophysical Interpretation;

The ) - feet of pyrrhotite veining in Cho volcanics between 120 and 123 feet adequately explains tho E-i ar.oz.aly. The conductor fitted the geophysical model in location and in dip.

E. Ponsibilitics; Nil

A. S^xncnd 1 1.* ir c sl . Cyoer.di.ti:ro. St

Staff claries Geology Geophysics SiuparviBion

Total

1,003.10315.06

1.485.07

2,803.23

Conr'd.,/10

S S M - 7 3 G

-10-

GeophysicsDiso-.or.d Drill ing

Trar.cportation Charter flishts

accounts

Tenure FeesACR exploration worltACU staking cootsClaim transfers S abstracts

Ccxn^unications

Miocallancous

Adainictrativo Services

f 40.00 15,237.01 ^13,277.01

2,837.001.A79.76 $ 4,316.76

$li,COO.OO 1,600.00

176.00 $13 I 576.00

$ 136.00

$ 78.97

536,571.21

S 3.657.14

540,223.35

2. Unit Cos t a ;

B.

csoftd Drillir.2 Cost/ft. Mobilization S dc.r.obilizition 0 6,026.00 4.06 Direct 9,063.51 6.11 Xcnlo 142,50 .10

nc Charters 2,337.00 l . 9112. IS/ft.

l . Torrcs of the A^roc-nrinr. batT.?can Comlrico nr.d AC and HBR

a) Conir.co haa exclusive prospcctins, exploration, drilling, end devclc^.T.ont ri^tc on the claims between April l, 1965 and December 31, 1966.

b) The claino arc held under option by Cominco t: oa AC andH3R.

Cont-d..../li

11-

c) li Co:.'ii.CG intci. 1..". to o::o.vci3-:- the nation it

::o 'o:-,i^ on or b^ow r^yi^ba/ 31 I:,-:ur cr:r;x:::itu--- of ft 3.r:,?t C'^,000.00 in X'.:,r; ^t-liv;, ^':: ilc-;vt3Qn,C.riliir:;;, fitr'hl'y.', and in t;. c or,,;!:, o::1 a-cnloxvtion uorh by AC imJ. IC'.~( Ctrl'?.

3) ilc-ro y Ir., ir." ir. r;ood cU^-air.;.; t;'.v-iji'j currency of option by r.ib-.i-cti;:" rc-c-r^c-t

•l) If tbo o;;:;;loii is ••:c-.-".:^~^., c. n cv ccrr.viv' nlvOl bc 5ncc:-:c vuviil er; -'a.lituvo^ by AC ,..V l r/ i c::d C,x.J.nco. c;.:cu:vb to 01*000,000.

In e/.c-esc oi ;;.i;0,0^0.

1) AC r.-.d I-:-;: ^Ijrj.l contribute l[;'; j cjid Cor.iinco "5/' o i' o::;-c;-iv.l:.';xv.'cr:

2) 'il.o ^VK--.-^:; ic:;uol ;.itU rrcpoet to tl.e Kcpoixliturca bc cliv^/vi .''O,'!, to Ca^iuco w:d ^0;' to AC and

c) vO.c-u cr.i IT crr:c::.-J.tvuX'3 by AC cr.^l r^'^atcoc-rl ,1U,000,000. or ;MO,000 rj.;::;i;'i?:i ch.ili bc divido.I CO^ to Cininco and 2

AC crjii iar;.i') tirj ic u

tozrir.r.tloii,;.?:Lr^- u::y". :. otic o ;'v.:;t bc c^ 1-^ of r.') Ci...'..-..i :.-;.^ bc i; i coou oi.:.j;.:ii 3) Cc^:;;';o i;'..;\ll dcl:lvcr (^) t:-;xn;,i^c of tl

(b) oo- -lo.-; or c.H n:o-, r^r-Pi'ta, c\ir\cya, lo^s,i'. cuu,.

7. L

by -lv.. d:l::.-o;:-: ur.L2i V.ol';.; tc^;- c;' t:;c L";; o I.-,'.: c .:o:-'j'.-. ci.

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; ^j.c^ cut P^J-.I tlio

'.: to ^-O.IV.L::.- t':o a-:.:-::.\l:.-:t ctxy':v.-;ti-. itlcr. rocox-Jcd on thecti; ci" c..'i i'-i'oot senn of

l.c (:z"b -c::: tvJ.co'.::-.tc'V ::c.-.-;:!...-". i^. i.Ow'ntiv.iio.v; o- cc

o-^; in t'.io clvill cores hcj '.r iio profitciblo

;^•-.^->^•• — r - i' •'-Tt'.' ' ' - '~ - '-~--u--*' : '

l;;;; i.- --o c;-::. l1:: e o.itioa a': t-a t:::: /0"nc.v:-. Cc::trnl

ic,; ci1 t;:o t.x*.,Li,r.,tio:; b:, bcicvc July 23,

9. i^;'-5^"l::

c-.) C-v:' .-.l ("J I c.-;, l /r. 'f- -tic) 1:1:-;^, of Lo^t lake

by AC t:

ContJd.,,/32

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INSTRUMENT; ABEM VHMIGUMCOIL SP*vCIK!G : 200 FT FREQUEMCY : 352O c.p.s.

J M PHASE ONJ THE LEFTOUT OF PHASE OKI THc RIGHT

CONDUCTORS: , ————Weak.

CONDUCTIVITY.-- G.-GOOD - ?.- FAIR ?.~ POOF*. K/.ARSH: - 4/x. z .- EXCELLENT

l he Consoiidoted Mining and Srr,e!iing Cor.'.pony ov Ccr.cda LimitedTHACCD 111. ELECTROMAGNETIC

LAKE (wftmj ppopfffn—_.__,-w_i: —i—-O—-:- V/A AREA,

Hole Un LLM-1 Sheet No.-l

.Property

: ' - - ' ' ' '^''^. ;:^f- :'J'W^ The Consolidated Mining and Smelting Company of Canada Limited;^^?v^^^-S;-y;'v-.*".;^ i:V ;

DIAMOND DRILL SAMPLING RECORDt T , n "7t I *i*'n TTnrth "1

Sault Ste. Maria.nr*A T,,ly -H 10fiS

^ July 23, 1965.

1 i*, .gf h

, Bearing

Dip

300 f go t-. —————350

-4 S0To determine

Ut

pi™,caur.e of E. M. conductor.

Hrir, fomp.FtrK Bi- _ jTnie DipObjective .

q?O

T.77 TT 4+70 SP:

Var. Comp.^ ^

Total Recovery ^^jrLogged by

FOOTAGE

FROM

0

23.5

p-..

\

TO

23

119

DESCRIPTION

5 Casing ~ Overburden fine pale prey sand.

Cliloritc Schist23.5-104.5 medium grey to pale RVCCMI Rrey, fine r.rained fairly soft, veil foliated at 45 to lonr. core a^is. ??any narrowcalcite (F.st. 5^) veins parallel to foliation, r.etween 31^-104.5 short ^0.5* long) leny.ths of core are a darker **reyin colour. Moderately chloritlzed. Pyrrhotite (F.st. 0^57.)occurs as snail flattened dissenlnatcd blebs parallel tofoliation. A few sn;all specV.s chalcopyrite.104.5-114 pale green r.rey (113-114 sll Bht purple tint) soft,moderately veil foliated at 45O to core loa f; axis, granular appoar.- fine Grained tl'.ough coarser than overlying unit Calcite (Hct.5^) occurs as narroi/ irregular veins and ar, sriall tenticleaparallel to foliation. Toper contact p.r.-ulntlonal tr.oderatcly chloriti^cd. Tyrrhotite (Hst. trace) occurs between 113 and114 as small disseminated blebs. The unit has the pcneralappearance of an altered tuff.H'i-119 Sane as 23.5-104.5. Pyrrhotite (Hst trace) occurs assuallodisseuinated blebs. Upper contact Rradotlon.il. roliationat 55 to core lon.f, axis. A few snail disseriinatcd blebs ofchalcopyrite occur.Sampled 115-119.

SHORTS

FEET

ICC,

*

SAMPLE

NO.

'1L'(.-C- 7

i

LENGTH

FEET

.y; -

ANALYSIS

T L,

. *" ' ?*

*

K.

f-

Ci"

RECOVER

7.

I

*~ \

'3

-

1

COMIHCO .1*41

";-'Ho3eNa..................Sheet.........J^.... DIAMOND DRILL SAMPLING RECORD' Property ....Los.t. J.nkSL..IJ.o.r.Clu........... ..Length ..........—— .....— — — — — .— Lat. .................——— ——— ...— .......Kor. Comp. ——— . —— ...——— — Ver. Comp. — ..........—— — ................~.

District .............—.......—.———————Bearing . .......————————————Dcp. .................. ———— ————— .......Etch, at...———— ————.————.Total Recovery 5^——. ... ...— — ..... ...... .Commenced ..... — ........ ... . .... .... ...Dip . —————.-.—..———.Elev. ..... —— — ——— — .... ,....... .......True Dip — —— — — ——— — ..............Logged by ... .... ———————— ..................Coinpleted ....................———..————Objective ..--.....--------—....--.--...-—-—............-.--..----..————..———..—Location ..... —— ——— ... .......... .... ——— .— — — — — .... — — ... ... — — .... .........——— . .

FOOTAGS

From

119

122

163

164

To

122

163

164

233

DESCRIPTION

Mrtbnsc-i'cdium r.ruy, r^ditn frnineJ, slio'.;tly folljitnd r.lnorirregular c.ilclto ('"st. <2/:) voinn. r.oth contrscts shnr^ st73 to coro lonjT axis. i't;ll cievolo^.d biotite -.y--on. ^vrrlmtltfi(f'at 0.5") aa flattened r.-isuss In r.lxMr plsnrs htit nlro r. aiHGsci.ilii.3ted blebs throughout; unit. A fov srall blc'^r. of clinlcop 1-occur arcxmd 12u*.

Cliloritc "c'.tist.122-145 - Cnc:.7 a-. 23.^-104.5. DnrV.nr j:rcv arour-.d 737* .ind 13^ f .Tollotlon u t 5 0 e to Ion?: core axl^. ^yrr!iotltc (' r.t f^.5") occursan r,r.t\l I 'tssnr-ftir.tocibla'.s .-md t racnr. e ^ -.-kyvltc no.! a Co-..- sr.nl lop-ccka cf c'lnlco^yrlte occur. 01A5-151 - r^dlu-; }.;rcpn rrn;-' t only rrvJorntoly folirtnA a t 50to core lonr nxln. ''^(MuT f.riJm' 1 ; fairly soft, "nly vnrv flnorcalcite volnlii" r-ostly }T.rnll-il to ff-U ntlor.. Fr.T-r-^nts? ofcalcite (up to 0.15') lcn^ occur lietvocr. IV). 5 nnd 151. '/oJor.itclclilc/rltlzcrl. Uppfir cont.ict f ra Kitlo.;.-.!,151-163 - Sai c ar. 23.5 - i:)4..ru roll.it Ion at r*00 to corn lcrn^ .-p^lL'ppor contact p.raJatlcnal. ryrrhotttn (rr.t 0.*;":) occurs ns a fo.wdisseminated blebs. Trnco of pyrite occurs.

Ftotitc Talc Sc?(ipt kr.ile r.rtfcn jrroy, r r-.V r.Ttclv follntcd, tint'tvK! v.r.-ilrad, fnlrly r.oftveil ilcvalcpcd biotite (tint ?f)7) r.r-v-.-:t.-il^ ^:it!l sor:o t.-ilc and cMorCore broken around cent nets 1-nt t'ley fl^po.ir r!inrj'.

5 diorite Scblst164-224 Sara .ir. 23.S-10A.5. rollnttnn -Tt 50 rt to coro lont nxi.ipyrrhotite (T'at 0.5;.') and trnca pyrite occur .13 mail b In r. 3 annocI.-.tcd wltli cAlcltc vclulni^.

Shorts

Feet

•itCT

,

t c-.

S'-.mple

No.

40GC4

Length

Feet

l 9

ANALYSIS

CM A?

t r. ice

'.u

tr.Tca

RECOVERY

*

~ ;;

r -j

: - -'

: ,(

Ksare^* ^•'•'--vfkaaiwm^-;- • jr -ri t;. J*;. -

•r*"-

—.——..Sheet........3..—- DIAMOND DRILL SAMPLING RECORDLe*t Lak.3 Sort r*.

Property ...._.—....—.—.....——.——...Length ......................————.....——.....Lat. ——...—.............—————.....—Hor. Comp.—....—————...—————Ver. Comp.District ...........................................Bearing...........-..-.-......--...............--..-..—-Dep..........——..—..———......—..-..Etch, at..—..........—................—.........Total Recovery %.Commenced .........——.—...-....—...-......Dip ......——..——.——.—...——..——....Elev. .......—..———.———————..True Dip —.——————..———...—..—Logged by ......——Completed —...————— ...———......Objective ................——...................................................—.............—.—..—...——Location ..——....—.........—...————...————.........———.

FOOTAGE

From

25-;.'

207.'

2cc.r

To

257

7 C,-,

265

DESCRIPTION

22V- 210 — Sari-* aa 10-4.5 — 114. '"oMattc^ nt 60* t-^ cere lout:axis, Unr-or con.ti'.ct f, r aJ-itlou.il. A fov s-\ill Mobs of - vrr*'ot?ti

230-203.5 S.-xrj RU 23.5-104.5. IZcocr cc-.itiict ,*rAv'ctlc:^lPVrTliofcUc (Hdt O. .'5'') ns sr-.jill c'ltnnT-Jn.ifcc.l M.;!-.-,. A few fi -.-j* 11blcl.s of pyrite rfno chalcopyrite (list S^th tr.-.ce) alnci rro;r.

.5 rraphlto Edil*t* * QDjl""i i'.f'J/ Co UilJC^-j lOii^t.Ot; ^C 05 to cot'O Ifuit* f!xi:' fllta^rrain^d, uo^^ clr.or ';u:irt2 .)::ti e^c'tc- Vi'l.tjs occur an-J .1 n.*rrovre] ijrcvn ha:*-JI-.iv. parall*:! to foli.iLiiy.. Uppor contact (-.^nr? r.s-fcrV.CKriJJ:;t -.'i'llh f ci l .iclrni.203.5-254.1 Ccptaiiia ?yrttc (r. -.r 10V.-?Cr) .ir. IrivraL-r v^lr.c T!--to .023* -..-IGU .iin.l aa tM3*rt':Ir..ittnl MoSsi. 204.1-257.5 ctv.-.Mlnnir.^ly r -l r. o r pyrite (2'.:-3?.) ^i v^lo.leCB.

.5 riMalvc Pyrlt*.Lnrr.c *7;)rl.itio3 lu crystal -t'a*-.. "Lr.or r^i.trtz j?iu! calc?ri* .-.uIrro;~ul.'.r ;-c?tc!ie3. t^:;\^r cTifciicC o'prrori:-1 ! (c^rii Vroufssi) I-.ut

0 T.-.lc C'il^clte ''-chlsc. o

vlt^ folist ton. 2;^'. 5-26?."., pyrttr. crvitcnt ro'jd^.-s .i'.. our ?"'" .IR

Vyrllo (Vst i" - 5") AS s-all i.l.V.^ m*.;l vt-tnlots-

Shorts

Feet

Sample

No.

AOW.5

'""'.'.of.

Length

Feet

3*

*****

ANALYSISLU

trac-;

t rr-c e

'"•'

tr,T-'•t 1 1; :.t

Au

MlVC Si t

Ml

c.

RECOVERY

,

/'

'

Hole No. ....Sheet ...... DIAMOND DRILL SAMPLING RECORDProperty —..l^.t...V.n*?...U?.?.-.n..........Length ———.....—. ................................Lat ............——.....-.........——-.....Hor. Comp.................................................Vcr. Comp........District..-..—.-_———............—-.....Bearing———....-—...——...-..-..............Dep. —....................——......———_Etch, at .....................................................Total RecoveryCommenced .....—.......——............ .......Dip —..-.....................——...—...............Elev. ........ ...—.......................-.............True Dip ........—.............—....... ...——.Logged KyCompleted ...._...........———.——......Objective ..............—.—.—...........................—...................--..............—————Location ...,.....———....———................—.——. ———.. ———————————

FOOTAG

From

265.

2F.1.

E

To

\ 2?.

3- i

DESCRIPTION

.5 CropMta

s1i2.-"- plan:;? NarrvTv c;uarCi and calcite vaSra prcuftit. 276-2.7.1.3 ccnca'ne lii^hly annular r.\t,\rt.r, r.i.I ree'; fra*? cnts. Iv^tji: copt.ioc uJisrp w\il c^cordavit wttti f o It at itxi. i ! ;*rito ("st i*-"j.') uccura as Mr-hly lrriv.ul.ir Vflnlots oT r.rMU cr;-r.t.iln.

•Ha^rse; ro-llu^ jr-jv fn.-CTi, unfr-llatoo, f tit vttb .1 f-*v r.ht-.-^r plariC'.i. ^ctlu:^ r.r.i!.ic-J,'-.:*r(!. A fcv narrtr: cdTclrc vnlna r-rffr**r.t. ::-i,'.-ri-talv c';lor!t(;:;:t!.Cwt.-'Ct witi, ovcrlyiiir-, -.r.lC ts obnoiriv! (con? bro'ri-r,) v-uc 3 )-*( ) .'ara s':.-;o nru* -Tt ••'.'.•ait tv."'C to core 10;^ a^rf rvrr'.7tita cn.-I pyrite (i.'^c l5nt*i tr^co) as ?^^ll ^issftr-inatoi! ^1;-*'

Core recovery - 9?i^

Shorts

Feet

Sample

No.

length

Feet Cu A"ANAL::Au

"SIS UKCX3VERY

*

"

'

v

LEGEND

OVERBURDEN

CHLORITE SCHIST

DIABASE

MASSIVE PYRITE

TALC CHLORITE SCHIST

GRAPHITE

GRAPHITIC SCHIST

SSM-736.The Consolidated Mining and Smelting Company of Canada Limited

MVIU0 ir OATI irviuo vi OATIDRILL HOLE SECTION LLN-I

AGAWA PROJECT

TWP25 R22 ONTARIO—— ——— SCALl:|".40 FEET |ruTit

l COMINCO

pjp^vc

^t***^-;- ** ' - --^Tfe -" - i .. -"•r •i-.r, -s-'•f^--:

- Y-F:?.i- * . ^..- -.*,. a 2507-i 'J^-i*

^;^^^vf-v ' . " - i ^-. -.'^f^^ffS^^^^;iS^j^;-:-'--..- ' . . 'v /^^-.?-t;T;?^SH^^^-1'v -

-J ":'.'" '*'^-t -*V -.""' , - ' " " -" ^ "* "^•'vv'.jf ...- '5 , ".•'** ' --'. " "

DIAMOND DRILL GEOLOGICAL tOG1 'OBJECTIVE: 7 ""^ SAMPLED: 164-169 116-121

To investigate cause of E. M. conductor. f e c f* \OGGED BY: s. R. Snodin. DATE' Aun. 3/65. *""ts*J! COMPOSITES:

^OST i-A*.^ fwtrn o i at 0*^-45 •LOCK. Lost Lake North. *ECT., aS-FSSl-r^/SOrr.J PLACE: S: jit Pte. Marie. APP. BEAU.: 170 AKp.t oipjjt 300 f ~— 7tNG TM: 366*

r.-?., rv I f \

FROM

n

31-

t ii) —————

ll "" —————————

*

————— l

TO

31-

254

"" ' - Started .Tnly 25, 1965.DISCARD! REASON: , , , .~i ,^x-finished July 27, 1965.

—— Caqir.;:; " C^/oy'jurdoa-, — if**?^ — p.ray -and b ge1^ sartd-t —————————————————— ——————— - ——————————————————————————————

Altered Uasic X'olcanics.— 'jiJL-^yii'alt-'-'f^' i-.iK'otve' voleani-c^; — Prccny-^rcy, ?'jssive,-njrdi-51--f.2 cc-!. tTnli-.i-d. —————————————— ————————————— —

62-67; iced, fine-finn (jra^rtod. Hhanp'e in uraln nf.^c rradational. Trr.T-ul.nr C'jldoto vein*; around 4^*. T'fr:r,n finegrained diloritiacd r-aterial ^;itb random orientation throughout unit. Unit nli^htly chlorltlzcd. pyrite (^nt. rj.5?,)

—— ST'sll f IctUto.'.cJ di.-:-; em.nnU;d-hluhs. A~ ft:w i-.:i:)ll b Ir. L s of chalcopyrite l^oti.vcn 64-(;tS. 11)1-, urtlt is r-ifopal'ly p .jrc~~of an altered Inva.67-90: Altered banded volciinics. iV.rVhnn preen r,i-'V, faJrlv rM.-.sivo, fine ^rained, narrow wavy f-rev TCC'i and nnlc

—— - — ""w:!*)*-*-— i- S B ^** .-..^ . n *

—— f-.rntni u.mi'iua; parallel no ;j \-CaU toliacion de l* 0 td cote Ion- axis.' ! :nall oval pale r.r*?y incluslonn (prob;i')ly calcrfcT a feu nnrrov ciidoto, nin'-.i.-.b. ourrfr and rnloltro v,"fnn, Ho"r-r ro^^f!.'^ no^ ehnrn .. (v-f-r^n nf ov.-'rl"*."-' i-i'itt incUi-'cd IIL >banded volcanics) i*nd at about 45" to cove lonp .ixis. ^ock in nodorntrly chloritistcd. Tyrltc and pyrrhotite (rat. 0.5'aa f-.all flac uisj5uv.iri-:i:oe l)le!*r.. A lev s:::a.tl iiletju or ciiiJlcopyrito (IT^t. trace) alno occur. Tliis unit in possibly a ruff.90-147; sar.x2 as 31-67 90-02; fine grained, 92-113 reditci grained , 113-147; rcdlun fine-fine ^raintd. Upper contr-.ctS'.l.'Jrp i^uc vwvy ;jt 50 to core ion-; axis. Pyrite and pyrrhotite (Fst. both .5") as sr:vill dlnocr.inntfid blobfj. A fox/ sv.all blob's of r'-.nlrfvrif-o (T^.';^ rr-if-r*) •fi r--il.tnr^ ^ofn*-.flar.pled 116-121.

147-1^'); R.-sn.'' nn r-7-00 ^^r>l1.>^ hnorTin" i-n-n- f vtv^ni^*- T-..? irv'^ w' .^t f'--"' 1 1 -'-^ to r^ro Ion" ;u'Jr '•—••or rr-tT*t c'l'^r^>—vavy, concordant with banding. A fe" snail blebs of pyrite (r.nt. trace) and a fev snail blebs of chalcopyrite in acalcite vein cit i4)i'.]AO-1 r,Sj S-;-xf . n n V-67 bnf t i-ri? . pj:.ain^iL-th.rj?.ii.^tinii.?- . .f^-JU* .^ fl^A.' laqr.l-^ ^f..r^ rft 1*rnf r •T^rtcria'1 tnclu''^ ' ''— JCr

contact sh..rn, t.-a'/y at 40 to core lonr. n^ic. ^yritc (Kst. trace) ar, srall disser'inated blobs. A feu r.mall blobs ofchalcopyrite occt*r bet'..v?cn 152—11)5. 111-172; aa:a. re f.7-qi. — ^n^lva-q;!.".rt^ wi~vitnii-^r^*^4- lv'?* .1.1^ 17^?-, — r^~f?i^*^-ftt-^5^-feo-e^Fe- Ion'*— p^ia. I?p{v*'tf eiMfc**etEh;irp t concordant uitb bnndtn^. Pyrite and pyrrhotite (Cst. 0,51)as cr.iall flattened blebs and crystals.Sanpled 164-lf.y C ORe S IIE

n A i

HOLE NO PACC

Uti-2 l

J u",*; ..,,- : - " ; - ' ' -',.;^, --,..:. . . ^ , - 4, ' .

' * .' ' ""'^

4O SCALC

coioit nor m Off 1 ox CLM*C* K AV"

o — — . ——————————

)

S.-r-nlc "r:0669C

0668C

•.

i CO^5

*N i

CO03

lenrf'i5*

r5*

Cu.Ol'fc

,ow

COMtf&O 29O7-M*.*.

DIAMOND DRILL GEOLOGICAL LOG SCALC

OBJECTIVE:

LOGGED BY:

TO

254

273

272

3*5"

DATE:

SAMPLED:

COMPOSITES:

PLACE: APF. BEAR.! APR.: OIP.T

DISCARD: REASON:

^.-r.:c as 31-67* 172-17A rn-U-~tno t-ratncd. 170-^4 rad. trained,. 20A-207 fine! ^.r-^.n^d._T'pldctc v?tn3 around 1R9 nn.d^ 2CO. Upper contact sharp, concordant v;ith kandIng of ovnrlytiif, unit near confnct at A5 0 to core lon^ .txin. A few srsall

(r;;L. tT^cc^—uccut" In ualL.—————————— —— ———————— ———————————————————————————— —————lUrZZP-ja^e -s G7-'JO. 211-2?") slt^htlv (tad-or in colour. Ti-.ro..^-Hko md bro--,i v^tnr. .

K.-uidinp, at 20 to corn lcnp. n:-ci?. Upper contact irror/.ul.-ir, r-aterial pertly Incltulcd In o--^rlylnr. unit. Co\itact ccracor. ~f.*i L'n l^.iiii.r'.. — Tj'xiLc- (''GL. O.I;."') — rnr

1Q^5.ft.L.8-TnQ as 31-67 ??fi-??5 finn ^ralnfld._2?..r)-25Aper contact shar-.i (at 40 to core lorif. r.xlc) and concordant vith br-ncltn?. of ovorlyluvt unit near contact. Pyrrhotlto (

0.5/i) us i,;.all JisJ^OLilrsnCirit hlctrrri "^, Cov; KT^ll^ulelja of pyrite 7m?l~cTiTitcopyrT^i; (Er.fc. CotTi~

oricntn in t

La.:ct.

Praphtte Schist; 254-255; dark p.rcy , veil foliated (at 450 to coru long ax l r*) soft, fine ^rainert. Thin "Calcite vctns jjarallcl co foliiitlun. upper contact Ki\5rp~~coT:coi'dant witli toliatiofu iilcbs or pyt l?c (T:r,t. l/') oc~cur~

to fQllrflnf._____________________________________________.__________________________ ——60?! and calcite 30^ n.iln constituents, talcite, vo.ty x/avy Foliation, no^t snd fine ^rnlncr'.

as vnvy ve in .'j and i ).';v ;i^o n t syr,t

parallel to foliation. Upper contact frrndatlenal.

Kit 3 1-^7, 272-202; fine rra^.novl, 2S7.-318 r..cd. rrafno--!, 31"-222 fine crntncd. At 3?.0 T red hrov-n italnln^.contact fairly sharp at \5 to core Ion?, nxln. ^"isns of prapliito Included In volcanics near contact. Pyrrliotitc("ot CW^!Iv^—as infill flafct-ovi^;! Mt^rrn——iV-fei/ LlcvMr; aC pyrita ,i\\d ^ :Tlxrrr.iyrlte Cr^t. Lctii Hacc)—ocr:ur.————————

. o at A5 to corg Ion" axir.. '''-rtf.e (V r.t:. 2/1) as

foliation.

. trrorttlnr voinl.nta /*nd patrhc*3 nr.-'l

CORE S I T E

MOLE No PACE

2

:n.

COMfVlCO 2S07-w.o^

DIAMOND DRILL GEOLOGICAL LOGOBJECTIVE:

LOGGED BY: DATE:

BLOCK.

347

353

-A5X

TO DISCARD:

347

348

354

-jot

SAMPLED:

COMPOSITES:

APP. BEAM.: APR.: DIP.:

Altered r.,i-.ic ^--m l •..vi Volcanic?,Sans aa^67-50. Bonding concordat with upper and loxjcr contact. Upper contact sharp at. 10O to core lor.**, axis. Pyrite (Z:.t. l"f) j s thin wisra pTirul lo l~T3~lranv.] Irtp,.——————————————————————————————*— ———————'————'——————————-

Irlack, clues trained, wrt\."y-folia'ticni (at AO to core lcnj: axis). "TfrsT '^TTEc~IncIu!.!ion"; of volcHvfic n;ift-"rTaU eo-itrct- rhnrp coouordaat '..-ith-f

"A! t cre.'l )i jo le Tol Irj t j Vo IcajTTcTf^.P ro r: rrnlrijt1 , r. X Inl^ly— Caltnt".tl t~o— CA :uj^ _ L'ppci

con'j.-ict glnrp concordant with foliation. Chloritized. ryritn (J'r.t. 0.57) nn snail Mnbr, and crystals.

I'r'.Xi as 34r;-352; with lil;;hly Irroy:\ilar y.ra:)hit-'; brntls a.ir! nron-j of pytlto Olst. 5") '-arallel to bnivJtnir. '*o nhnrp upper nncl lower contacts. --—- -

r,g:?ic rolintetl volcanics; snrv* aa

j- x- a Hteir inclus-iottn of v^^-^ffoliatlcn r.t 40 to cora lon^ a:<i^.. Pyrite (r?,t. 45') as thin vclnlcta parallel to foliation.

-e tincalcite and cvyidptc vain:i. U^r'Ct con t not sharp (nfc 35 to cere*, lciny. ax Ir.). 1'yvlto and pvrrl'.otttc (r:it. hoth trace) at 361' and 304* a fev/ snail blobs of chalcopyrite.

HtvJ of Hole.

S" lO S?^ t q .y.jr-* y

1 "7*

CORE sire

MOLE No

40 SCALE

COlO*.*t.Or A Ou

1

i

1

1

1

f'O

l

C/3CO

kt'-:- WK'

N.

LEGEND

OVERBURDEN

ALTERNATIONS OF MASSIVE AND BANDED ALTERED BASIC

VOLCANICS

ALTERED BASIC MASSIVE VOLCANICS

ALTERED BASIC VOLCANICS W!TH THIN GRAPHITE BANDS

GRAPHITIC CCHIST

S.

The Consolidated Mining and Smelting Company of Canada Limited

MVIUO *V OAT l

TIACID IY:

irmio IY DATEDRILL HOLE SECTION LLN-2

AGAWA PROJECT TWP 25 R 22 ONTARIO

1966 -' UOMINOO

^

SS M 66989

S S M

66992

LEGEND Claim Line

EM Conductor

lorill Hole O

The Consolidated Mining ai:d Smelting Company of Canada Limited

MVIU0 IV DAT!

TiACfO IY:

trvruo ir ot,nPLAN DDH LLN-I LLN-2

AGAWA PROJECT TWP 25 R 22 ONTARIO

200 FEET DAn:AugustBOMINCD

REMOVED PROM THE OFFICE OF THE RESfDENT

' EOLOG.ST. ONT. DEPT, OPM,NES

SAULT STE. MAR.E, ONT.

C/.

SAULT STE. MARIE MININC DIVISIONSAULT STE. MARIE. ONTARIO

ONTARIO

DEPARTMENT OF MINES

August 30th, 1965

4iNi6SEa8aa QUILL 11 o SAUNDERS

The Consolidated Mining Se. Smelting Co. of Canada Ltd. ,Exploration Division, 1170 Beaver Hall Square t Montreal, Quebec.

Attn: Mr.S.R.Snodin

Gentlemen:

Further to your letter dated August 26th, 1965, I have this day filed work reports for diamond drilling as follows:

74 days on each of SSM 669B3-96'inclusive

27.2 days on each of SSM 66997-67005 inclusive

40.8 days on each of SSM 67660-73 inclusive.

Yours truly,

/w i. A. Jodouin, Mining Recorder.

300

SSM-736 j

'vXXfLORATION DIVISION S f EASTERN DISTRICT'

Mining and Smelling Companyof Canada Limited

BEAVER HALL SQUARE CRANE BLDG. — 4TH FLOOR

MONTREAL

MAILING AODRCHP.O. BOX IS1O. STATION *B*

MONTREAL 2. O NADA

May U, 1966

Central Railway ilw Leo Avenue SauD.t Ste. M^rie, Ontario.

Attention: D.E. SmithMnerals Evaluation Pi-oject 1-imager

Dear Mr. Snith;

Regarding the A^awa Properties, A.C.R.-Coninco Oat ion Asreerr.er.t, please find enclosed, copies in triplicate of all data pertaining to the exploration vrork completed by Cominco on the properties, as requested in your letter of April lU, 1966 to our y.r. I.V.". Wor;cr.an.

Also enclosed are throe copies of a letter which ve received i'rcr. the I-'inin^ Recorder indicatinfj thit s^sessrr.ent vork carried out "by Coninco has been properl" credited to these properties.

Yours truly,

-JACrbp Encl.

r NOT T O

THF.OFFICE Or

SAULT.^

RcCHlVED PROM ALGOMA C ENTRAL RAILWAY

.••J.A. Collins Exploration Geologist

-. iSSM-736.

MAY 24 I95f

RESIDENT GEOLOGISTSAULT ETE. MARIE

•••'• ;. .: ' ;-.: ^ *^i: ^^?^Ml^i--f^^

: The Consolidated Mining and Smelting Company of Canada LimitedOMA*rK B'

LOCATION MAP AGAWA PROJECT

y VPWLtf ROAD^F-S&jT, -,, . -: - v/^^SsSSH^y^j ; ;^CLAIMS: ^^^/la^sr^^^jmi ,