DD RPT 10 PERCY L - Ontario · It)8.o-l8fc.0t Kleaaahiati wbltleh-gray, danea. 17is. 8-174. 4i cor Mating lOii. 0-18^.5 1 megnatlta and gurnet In hornblende aohiat* * 18C.9-185.6t

t e PERCY LAKE

Diamond Drilling

010

Area of Percy Lake Report NQ 10

Work performed by: The Anaconda Co . (Can,)Ltd.

Anaconda Iron Ore (Ont.) Ltd, et al

Claim NQ

KK 7446

KK 7426

KK 7427

KK 7552

KK 7699

KK 7430

KK 7445

KK 7429

KK 7441

Notes:

Hole NQ

12F-231

1AF-243F-244F-246F-260

2A

5AF-301A-9021-C2-C3~C

F-202F-203

F-207F-208

F-227F-248F-249F-263

F-230F-232F-233

Footage

435'348'

360'498'570'502'703'

360'

600'252'

2167'40'213.7'87,3'

405'401'

453'406'

655'816'766'701'

699'648'648'

Date

Sept/54July/56

Feb/55Aug/56Aug/56Aug/56Sept /5 6

Feb/55

Jan/55June/56Oct/57Aug/55Aug/55Aug/55

Jan/56Jan/56

Jan/56Jan/56

June/ 56Sept/56Sept/56Sept/56

June/56July/56July/56

Note

(l)

(2)

(D

(O{2)

W(2)(3)

(3)(3)

(3)(3)

AWL.005(7-69) rev.9-72

.continued.

Diamond Drilling

Area Percy Lake (continued) Report NQ 10

Work performed by:

Claim NQ

KK 7670

KK 7548

KK 7877

KK 7698

KK 14268

KK 7867

KK. 22050

KK. 14268

KK. 14096

Hole NO Footage Date Note

F-302 F-304 Ar-901

F-306 A-903

F-401 Fr402 NPL-3

430' 300'

1512'

136' 550'

503' 505' 894.6'

July/56 July X 56 Oct/57

July/56 Oct/57

Aug/56 Aug/56 Oct/61

F-600

PL-1

J~3 J-4

NPL-1

650*

3336'

4571' 451'

881.5'

Oct/56

A-606 Ar-607

A-614NPL-2

430' 450'

630' 468.6'

June/57 June/57

Aug/57 Oct/61

Oct/61

Oct/61 Oct/61

Oct/61

Notes:(1) Lake Superior Iron Ltd.(2.) Technical Managers Inc.(3) Frontenac Expl. S Dev. Co. Ltd.

-Anaconda acquired property in 1956

'AWL. 005(7-69) rev. 9-72

l M. t. MT^BIOK 1ROK MMITKD

.HO.U LO

BOU ...EQ t II.

Lo on t i on i Line Fi- w SE, etation 4*20

O 48.0

46

Ho l jQ

Core l

48.0 05*6

00.6 145*0

145,0 iae.6

106.6 806.9

806.9 JS12.8

818.8 iiiO.O

880.0 tBb. O

4S6 feat September 20

beptemier lib l-ierr* Mauff*tte, Oo&sulting 0*ologlti, 0tpt* E 6/64

Rook DeaorlDtloa

CasingHornblende mloct-aebiet 48.0-66.0i gerneta in irregular banda 4 6" in width, 77.8-78,81 79,1-79,01

86. 6-90, Ot much aotlnollt*(8,0-98,91 quartslS2,4-lfc5d.9t nandvtoa*140.0-146.0i quartt. ftldepar and tpidottIn

146.0-lbO.Ot highly llloaou* pateh*0fsparse *0ftn* of magnet i t*148.8-149. 4| gmnlte160. 0-168. Os *ioa*iehiat, *tdlu* gray,dana*, aparea baoda of bornblanda aahlat.It)8.o-l8fc.0t Klea*aahiati wbltleh-gray,danea.17is. 8-174. 4i cor* MatinglOii. 0-18^.5 1 megnatlta and gurnet Inhornblende aohiat* *18C.9-185.6t Blea-scbUt, îghi grandense.

Megnetite bnd quartzite} alternating layara fron 1/8 (o l 1/6" in width.

Mleaoeoua ûerttltaj whitlah-grajr, danaa, uniform texture.

Magnetite i Irregular bttndlng. ^^Kbttdatonat hlt

texture, dealntegrataa*Jlijrr,/-^

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256*4 289.0 299.0 336.0 340.0

350,0

357.0

289.0 299.0336*0

3/tO.O350.0

209 -i 'c /riv •tit" 1 vlth seattortrd jv i;ic.-i litshUt.5cr-.m-xtitft.

347.0 ~ 350, Oi core wis

351.0 - 357,0i

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323.9

326.6

la237.824? *S

224.8237.8

242,8

274.0 3*3.9

ft 344.3

344.3 * 350.0

JS0.0 355.5

115.5 360.0

360.0

Ho ak DAB c ri ut ion

Iron Forw.\tlonj *ithas atovu, faulted,

arid/or calcite filling.

ryrit® and ohlorit*. with 0utos*qu*nt

pyrite, ol3.orit* f oaloltt,

* 300 bed 'ing 300 - 315 plight jointing

r t o en t faulting. 299.4 * 300. Oi flares mi 306.5 ~ 307.71 * 312.0 - 313.71 "

of

310.0 - withFin*- ^-;rain btsddcrt rock with qu^rti f*ld*par and/or mica ae c nutituanta.

325 - 360 bftddin/: anfl* 80*Magnetite. '

331.0 ~ oort i roek|

5 - 344. 3 1Chlorite ac' i r* t with l*yor* ofdieei'iRin ! .t"d tyrit*-j oalclte in 346.9 - 349.lt corn

6 . 350*01 H

ftldtpar^ ehlo'ritt^

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ton*

a® ehl.ori.te

'^ntJ of ô

( but ear* h-8 leat grttnith ting* ofinto a d* nant, li^ht gray, nioft *c int.

di r rt 300 f*#t, 34e

1

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i

D1AMOKO DRILL HOLE LOO

NO . A

Location! /Northern boundary e* c lain 76TO, VOO t of River,Dipt 450 8

Total daptfei 600 f00t

Hol0 stBrtadi January B7golf, Offap I* t0 fl i February ftCore loftgad by i pierra Meuff0U0, Oon0ulting a001ogl0t.

from jo ' . . Rook da00riptio* . '

O 84 Oaaing.

64 118 Mioa-*chl0t|100*118 badding angle Irregular, 0r*nuiationa.

118 180 Pegmatite j116*144} ttfeitt 144*1661 plBkl0h 185*1101 0pecklefl

wbltlah

180 1VE k'lcft-BOhittj180*198 b04dlDg angle *0* 186*1981 grading Into pegaaiite,

198 1V5.4 Pegmatite.

186.4 844 iitOa-BOhiitJ200-^85 bedding angle irregular. 886-890 " " not eTident.

844 846,6 Pegmatite.

B46.G MS. 4 Miea*00hi0t,

848.4 840. fi

849.8 878 ilcfi-eohlBtt a860*870 bedding eagle 66 , not very evident.

89*8 884.5 Pegmatite. ' y ^^''KWf :870-8fBi core '

888. S- 886-8861

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FRONTENAC EXPLORATION AND DEVELOPMENT CO. LTD.

TWO MILE LAKE AREA

LOG OF DIAMOND DRILL HOLE MO* F-202

Hole Drilled fort

Inclination:

Depth:

Bearing:

&S2*

Date Drilledt

Frontenac Exploration and Development Co, Ltd., Room 1313, 320 Bay St,, Toronto, l, Ont,

Canadian Longyear Contract Diamond Drillers Ltd* North Bay, Ontario*

-45V '. ^J ; :; ; .i;/^ 1 --";''-:';:;-'; :---'

405 feet. ;

Southwest

January, 1956.

Pore Logged by:

Core From

. 024

35.5133

153.5186

215227

:v-V '. : . -.247

252

Distance

24

35*5

133

153*5

186

215

22?

247

252

254.5

P, K* Brown, Geologist*

. . ' ' A . ' '

Rook Descriition Cased; glacial debris. - .Well-banded, strongly magnetic iron formatlonj with

garnet, epidote, and pyrite noted* 'Quartz biotite schist; local bands of garnet*Dense, fine-grained, siliceous, sedimentary rook(?) j

appears to be of a cherty nature.Strongly magnetic, well-banded, iron formation*

Quarts, biotite schist with local bands of garnet; same minor bands ot magnetite j schistosity tvV

Strongly magnetic, well-banded, iron formation*

Predominantly quartz biotite schist; fair stringers of magnetite; schistosity 650 to core axis*

Barren quarts biotits schist, f

Strongly magnetic, well-banded, iron formation.

(Coht'd.)

Page 2 - lob of Diamond Drill Hole No. F-202

Core Distance

254,5 274.5

274.5

327.5

332

339

327.5

332

339

405

405

Rock Description

Interbedded quarte biotite schist and fine-grained sedementary bands of garnetized sediment s.

Strongly magnetic, well-banded iron formation.

Coarsely crystalline pink pegmatite; orthoclase and grey quart?.

(Same as 274.5' to 327.5').

Coarsely crystalline grey-white pegmatitej Bones ofpink orthoclasej grey color due to more grey quartzj muscovite mica, and calcic feldspars*

Bottom

Core has been properly boxed and marked and is presently being stored in a cabin on the property, Two Mile Lake Camp.

.

FRONTENAC EXPLORATION AND DEVEIftPMENT 00. LTD*

TWO MILE LAKE AREA

LOG OF DIAMOND DRILL HOIS NO. F-203

Hole Drilled fort

fiC'

Jnolinationt

Deptht

Bearing:

Size:

Date Drilled;

Core Logged by:

Frontenac Exploration and Development Co, Ltd., Room 1313, 320 Bay St., Toronto, l, Ontario.

Canadian Longyear Diamond Drill Contractors, North Bay, Ontario*-450

401 feet.

South-west

AXT

January, 1956.

P. K. Brown, Geologist.

Core Distance From To

O

4

25

41

53*5

58*5

63.5

72

89

4

14

25

41

53.5

58.5

63*5

72

89

103.5

gock Description

Cased; glacial debris.

Inter-banded iron formation with barren quarte biotite schist*

Intermixed narrow and irregular bands of pink pegmatite and quartz biotite schist*

Strongly magnetic, well-banded iron formation with abundant dark-green hornblende*

Coarse-grained pink pegmatite; orthoclase and quartz*

Barren quartz biotite schist*

Coarse-grained pink pegmatite*

Barren quartz biotite schist; schistosity 650 ,

Strongly magnetic, well-banded iron formation with abundant epidote and hornblende*

Fine-grained, quartz biotite schist with local pegmatitic textures; Epidote and magnetite irregularly spaced*

(Cont'd.)

Page 2 - log of Diamond Drill Hole No. F-203

Core Distance From Jo Rock Description

103*5 121 Barren quartz biotite schist; occasional hornblende*

121 139 Coarsely crystalline pink pegmatite; essentiallypink orthoclase and grey quarts; minor Ferro magnesian minerals*

139 145 Barren quartz biotite schist*

145 147 (Same as 121' - 139 1 )*

147 168 Barren quartz biotite schist with bands ofgarnets; locally very siliceous*

163 254 Strongly magnetic, well-banded, iron formation;occasional bands of massive magnetite up to one foot vide; isolated blebs and masses of epidote, coranon; schistosity 600 to core.

254 264*5 Barren quartz biotite schist*

264*5 269 Coarse-grained, grey-white pegmatite,

269 401 Barren quartz biotite, schist; schistosity 650 to750 .

401 Bottom

Core has been properly boxed and marked and is presently stored in a cabin on the property at Two Mile Lake Camp.

i'OR

M

l f.)

C "i

X

A- *

1XI^y

!-

*,i

t* - fi- '. n

f- N

li, 0

x* a X

\.

(^

f -

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~0 N 5

X

X

x

\

CP

l" J c n X) r~ D A '|T

7x

o7

r7

^ ?

^ j

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3 F

o '!A

-i-i.J

-Jx1

^ i

^ f

l b,

^ 5

^ tJi -j

i o* ^ (

j- Nv

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iji ^

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/^ ,f^

4 ^

Vw

w ^

1? F

ft

fr f

-t f u

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l V

***-

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t'tti?

(T'

fi n i n i W S? 0 o •J 0 P c

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r~ j

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33

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t

-A^ a,,..FRONTENAC EXPLORATION AND DEVELOPMENT CO.. UP

TWO MILE LAKE AREA

LOG OB DIAMOND DRILL HOLE NO. F-207

Drilled fort

Location;

Depth;

Bearing i

Size;

Date Drilled t

Logged by;

Drilled by;

Frontenac Exploration and Development Co* Ltd. Room 1313, 320 Bay St., Toronto, l, Ont.

105' E of Picket Line 40 W at 1400 N.-450

453 feet

Westerly

AXT

January - February, 1956

P. K. Brown, Geologist.

Canadian Longyear Diamond Drill Contractors, North Bay, Ont.

Core Distance From To

O

33

66

102

122

185.5

194

270.5

231

312.5

3386

102

122

185.5

194

270.5

281

312.5

330

Rook Description

Glacial debris; overburden.

Quartz, biotite, hornblende schist; locally abundant dark green amphibole; Pyrite noted; schistosity 550 to 650 to core axis.

Quartz biotite schistj weakly magnetix.

Hornblende, biotite schist; generally weakly magnetic.; schistosity 700 to core,

Strongly magnetic, well-banded, iron formation; common veinlets of epidote*

Quartz, biotite, hornblende schist with bands of magnetite; weakly magnetic.

Quartz biotite schist; pale green, soft, metamorphic (?) mineral occurring sparcely at 260' to 270'; schirtMity at 70.

Strongly magnetic, well-banded, iron formation.

Quartz, biotite sohistf. schistosity at 75O ,

Metfium-grained pink pegmatite; orthoclase, quartz, some bidtit*, few crystals of ferro-mag. minerals,

(cont'd.)

r ,Page 2 ~ Log of Diamond Drill Hole No. F-20?

Core Distance From To Rook Description

330 378 Strongly magnetic, well-banded, iron formation*

373 337 Quartzose, biotite schist*

337 392 Weakly magnetic, quartzose biotite schist;Lw grade I,F*

392 412 Strongly magnetic, well-banded, I*F*jschistosity at 75O .

412 453 Quartzose biotite schist*

453 Bottom

Cora has been properly boxed and marked and is at present being stored in a cabin on the property at the Two Mile Lake Camp*

Toronto, March 16th 1956

FRONTENAC EXPLORATION fe DEVELOPMENT CO.LTD.

TWO mm LAKE AREA. ONTARIO

DIAMOND PRILL HOLE LOG

HOLE NO. Fr20a

Hole Drilled fors Frontenac Expl. ft Dev. Co.Ltd.Room 1313, 320 Bay Street, Toronto, Ontario

by! Canadian Longyear Contract Diamond Drillers North Bay, Ontario

Inclination: ~45ODepth: 406 feetBearing: WesterlyCore Size j AXTDate Drilled: January-February 1956Core Logged by: W.T. Swensen, Geologist, P. Eng., Ontario

Core Distance From To Bock De scription

O 50 Cased; glacial debris - overburden

50 51 Good, banded biotite schist; seams of good magnetite.

51 65 Quartzose biotite hornblende schist.

65 72 Typical pink pegmatite; pink orthoclase, gray quarts.

72 113 Banded quartz biotite, hornblende schist; narrow l" to4n bands of strongly developed magnetite, garnet and some pyrite, Entire section weakly magnetic - narrow seams strongly magnetic.

113 197 Strongly banded iron formation. Strongly magnetic;quartz biotite hornblende schist; local strongly developed bands of garnet along thin seams. Magnetite concentrated in thin interbanded seams less than l" to 6"; locally strong contortions - complete tiny folds visible in AXT core.

197 211 Quartz biotite schist

211 238 Same as 113' to 197'

23# 312 Barren quartz biotite schist; occasional isolated develop ment of garnet.

312 321 "White, coarsely crystalline pegmatites, granite. Occasion al dark ferro-*aagnesian mineral; irregular masses of coarsely crystalline muscovite mica.

continued -

Page - 2

Hole No. F-208 - continued

Core Distance From To Roofr Description

321 347 Barren quartz biotite schist

347 378 Same as 312 to 321

378 398 Barren quartz biotite schist

398 406 Same as 312 to 321

406 Bottom

Core has been properly boxed and marked and is at present being stored in a cabin on the property at the Tt*) Mile Lake Camp*

W. T. Swensen, P. Eng.

V'il. An.0 .i.: JM (!://

J/iG OF l O Air 'i!-) PHI LI. H 'I.K F-227

J/K'-ATJON: Line 6+00 W nt 9*40 N]-; Corel AXB ear in p,: J-outh-1. cst Lopped by i K. C, FranaonDip: -60* Date j Juno 24th 1956

Hole UrilU'd by: Cviua'iian I/mpyeur Ltd., liorth Bay, Ontario. ,

fVon To J)cuRcrJj)tion Koct

O 38 C ir;:' i.r;

38 66.3 QuartK bj.otitc Bchist, pyrite, talc on parting tse

66.3 69 Ulvite peftU'itite.

69 76 OiUD'tK biotite schist.

76 99.5 K'hUc76' to S?' Many snail garnets,B? i to 99.5' Oarnots and jl" chryeitals pink orthoclase.

Gchistosity 60* to cor© axi.s.

99.5 12'i UnrU biotito schist.

123 131.5 V'M.t e pognaiite vri.th small

131.5 13fi ('u-irt?, biotito schist.134' to 135' Mo core,

138 140.6 Pink })o,p,j(iat:lto vri.th f.arncta.

1A0.6 157.5 CAiartz biotite r.chist with a aonc (145 1 to 156') mostly biotiteann hornblende \fith Rarnot porphrpblasts and quarts; bands. Cupper Bulphid o stain on parting surfacos.

157.5 164 l*iuk pof.,ivitito with sfiall garnets.

164 200 Good iron formtion, v;ell banded, but' locally contorted.nhly !ian;nritic, FooOi(*), ^mrtfi {*), B:'totj..te(-), Hornblende (s ),

to 1R9 1 Pink r*or.'

200 y\h Oood Ii'Oii Formation, bandinf,, highly contorted :(iarkinp, dip anglesvfuy greatly over small uroassj highly mannctic, locally rich in hornblcndo, Fe304(*), 'Qunrta(*), Hiotite(-), Horn\)londo(-), l'-pidote(-).215' l" strinpior of peûiatito, 251 1 " " H ' ii 298' to 299' B" and 6" band of permit He, 301.5' to 302' No Gore.

Hole K-?,2?, continued

From To i&iiS FeH

31A 370,5 Quart?, bjotite schist, Scattered bauds rich in garnot por-phroblatstfl, pyrite on Borne partings. Non-ma/rnoticj banding nearly undiotinquinhnblej Ouarta(*)i B5otite(*)* Clarnct(-), Pyrlto(-). 355' to 370' l" to 9" bands of i iron formation.

370.5 402,5 Good iron formation, well bandedj highly magnetic, Fo30A(*),Ouarta(-0j Biotite(-), Hornblende^-)*

^02.5 500 f .nari Si biotite tjchiet; non-Magnetic j very siliceous, poorly visiblejr/ritc and chlorite appear on some partings j hornblende -

locally; Quartn( 4 )* Biotitet(*'), Hornblendo(-*) ( Pyrlte(-), Onrnet(-), } ;;nstfttite(-),

431* to 434' N o core441' to 444' ' J~0 GOTO462' to 464' J,'o core

500 539 nuart?. biotite n/ihist; )dRlily sillceounj non-na^netic( poorlybanded j so?:r chj^rite parti iifê; C,*uartE(*), B;iotite(*), Oaraet(-), ilornblondo(-), (/iiorito(-), iyrite(~).515' to 5l6t5' Hand of peginntite, quartz, and feldspar,526,5' to 529' Quarts and Foldspar.'529' to 529.0' Good I.F.

539 6-4 Good J, F,, well banded j hipjily raaftnetioj sj.X)tted liornblende.rclntively abundant epidote} Ke3o4(*), Quartz(*) f Biotito(-), Hombloride(-), I^yriteC-), Kpidote(-).

624 626 ouartB bjotite uchint, sliphtly i

62,6 655 Pofrh'it.ite, pink near I,F, contact, get tin/* whiter toward 655't632' to 633.5' No core.

W.T. ft,'j;MJ3;N, Chief Geologist

*? - V- lo?LV)). '

I/JO OK ip Ai:;i;;u j^g, ;,j, HOIK F-23Q

LOCATION l Lino "H" at 2*60 ME of Hole i 13 Corel AXTBearing: .kmth-YIest Lopôd by i F,K* HrovmDipi -70* Date i June 26, 1956

Hole drilled by i Canadian Lonryuar Ltd., JJortVi Jfay, Ontario,

From To jjoscriptipn

O 31

31 111 Quartz idea schist, Generally hifth in quarta, withabundant dark brovm laica. Attitude seems at ritfit

JB to core axle.

Ill 133 (lunrtfc amphibole ochiat vritli FeS2, Lnrtfe radiating chrystala

133 140,5 AmnhiVolo? FyroxUo? fichiot pradinp; to J. F

140,5 147 iSediUM to coarse gr('ijncd pink

147 230 Very rood, abundant mesivo I. F. Best grade noted to date?In general contorted,

230 232.5 Minor irrtûlnr bands Fo3o4 in quarts; pyroxit© fjchlst*

232,5 249,5 (Juar-ta r/dca chlorito schist,242' to 243' W.I. F.

249.5 ^53.5 f Mi to fine gained pink jjogj urtite,

253.5 302 vSiU.ci.fiod quartz biotite schist. Abundant .quart e stilngere

2C6' to 287' I. F.

302 362.5 Very nood l, F, Very contorted,

362.5 376 QuurtK biotite sold nt with r.dnor bands of Fe3o4,

376 481 Rood l.F,376' to /jOC)' Contorted 400' to 4^1' Voll banded 470' to 471' /o core.

4f !l 515 i.'uartK baotite pchir;t vrJt!) Minor bando of Fo304,491' to 49^' Mo core.

c F-230, continued

Fix* m To DoBcri^tionFeet ~~

515 535 Fair l.F.

535 554.5 Quartz biotite Schist vdth p.arnot bands and FeS2.

554.5 5^4 Chlorite .and pyroxito rich J.F. Attitude steep, 80* to 90*.

584 580 Quartz biotite schist,

58ft 598.5 Very pood l,F. Fine quarts bandings,

59^.5 605.5 Quartz biotite schist, attitude steep) BO* to 90*.

605.5 606.5 Coarse pegmatite,

606,5 621 Quarta biotite schfiot, rainor pyrite , pegmatite banding*

621 623 Coarse vfhite pegmatite,

621 647 (,*uaiita biotite schist - riinor pyrite .arajMbole on parting eeains,

647 6^3 Pink coarse pegmatite,

653 654 Qwarta biotite schist.

654 660 Iln'c pen-uatite with garnets.

660 699 (,'uarta biotite echiet, pyrite - talc -* serpentine onP r*1 't - \ Y"' "V t' n ; *. J w J *;, '.' U

699 I:;ND OK no j

V.'.T.' ffi'JEHSKN, Chief Geologist

ym A?;Aco;;j)A &QJIPAIJY y (C4ijADA)r JID, lpg OF ujAi'oi;]) niau, HOU'; F-231

33*55 W at 0*85 N Cores AXTBearing: South Lopped by j I). B, HarrisonDipt ~50* Date i July 7 1956

Hole drilled by i Canadian Jon^year Ltd., 1'orth Bay, Ont.

Froi'i To Doncrjfition

Foot

O 15 Casing

15 l? (HinrlK biotli.e Bcliitit.

17 19 Magnetite, hornblende, chlorite.

19 20 Schist,

20 177 Handed Fe3o4, Quarts, hornblende and chlorite, corn© schist -Good I, F,53' Cuart'/i inclwdon,70' to 100' Slight increase in schist110' to 110.5' Pink pegmatite.12y to 130' Orthoclase, ix^niatito and come pyrite,14M to 146' Oranite texture, abundant orthoclase^ Bonio F©3o4

chrystals attcniptod to fonn,At 260' 2" quartz, 172' to 173' V/hite pof;uatite,

177 102.5 17V to 162.5* Schist and chlorite.

102.5 I(i5 Banded F

Ift5 205 Gariiot studdod ochist.

205 207 Banded Fc3o4, schist, chlorite.

207 213 Sol 1 1 rt vdth minor Fe3oA bands*

213 215 Core rdssing,

215 217 Schifit with Tairior Fo3o4 banrls.

217 232 Bedded Fo3o4, fichiot.

232 235 Core idBoing.

235 239 Garnot nturicJod r.ohist,

- 2 -

VIolc P231, conWriucd

From To I Peot

239 2V* i 00/j unipldbolo, absence of garnet*

2Wj. 256 fichicit, abundant garnet B evenly distributed.

256 2^7,5 Bamhid I'o3o4* Schist arid chlorite - 0,1.F.

257.5 260 link popinviti.te with maHil aruber colored parnots.

?6C) 307 I. F.

282' to 20/1.' W.nk Popuatite with Braall Kc3o/* incluaions.266' to 288' " " " " " "29B' 6" quartz, ooino feldspar

307 309 lichir.t

309 310 VMtc pofynatite.

310 322 Sclvint, f.oiae dra^foldod.

322 323 \Jiiitc ixjf;iiiatite vdth very owill pink Rarnetr,.

323 3/t^ (,'u'vrtz biotite schist, ninor cerpontine on parting planes,

Co ,17.T. P.WI-.1WK1I, Chief geologist,

THE .ANACONDA COMPANY (CAMADA) MD.

LOG OF DIAMOND DRILL HOLE F-232

Location: line 7+50N fit 32+Orf Core: AXT Bearing: West Logged by: F.J.Pranson and Dip: -650 D.B.Morrison

Date: July l, 1956.

Hole Drilled byt Canadian Jongyeor Ltd., North Day, Ontario.

jProm To DesqrijvtionFeet

O k l Overburden

41 134.5 Quartz-biotite schist} minor pyrite.75* Attitude steep 89" to 900 137.5'-134.5" Schist mixed with hornblende end garnet, 133' 6" zone qunrtzj hornblende and biotite. C2.5' 8" wjiite pegmntite with a light green

translucent mineral; no cleavagejhardness and serpentine??

134,5 205 Iron foimetion; fair from 134.5 to 139} bands of quartz?hornbDende and biotite grading into good around 139J minor pyrite,3.45' Some bands massive and very magnetic. 173' Attitude steep 800 - 900 186' Attitude steep " - " 175' Serpentine? on parking plane. 193' Iron forraHion goes to fair at 193; bands of

schist appear, 193' 6" pegmatite at 193.

205 259 Quartz-biotite schist,21/^' 6" quartz zone.219' 6" pegmatite zone.223' 6" zone of 20# garnet.23B 1 4" zone of quartz,240' l* zone of 2056 garnet,230' to 250' Attitude steep 60" - 900 .

259 ?62 Iron formation} banded with schist; small garnets,

262 266.5 Quartz-biotite schist} non magnetic,

266.5 268.5 Fair iron formation with garnet.

266,5 2?0 Non-magnetic schist.

270 349 Ctood iron formation.285' Moderately contorted} well banded quartz-biotite .311' Disserainoted epidote,316' to 334' Iron formntion well banded with quartz and

biotite and quartz-biotite schist, to 334' 2' zone iron formation with garnet.

- Page 2 -

.Hole No, F-232 continued

Prom Tp Desorigtiqn Feet

349 364 Quartz-biotite schist with bands of iron formation.361' to 364' 8' zone of 10-2056 garnet} fairly magnetic, 355' to 358' Zone of elongate white highly altered

amphibolite in quartz-biotite schist.

36/* 375 Quartz-biotite schist.365' to 372' Zone of elongate white, highly altered

amphibolite in quartz-biotite schist.

375 400 Iron formation with schist bands; well banded; moderatelycontorted.

Schistosity 60-90" to ooreaxis.388' 2" of iron f emotion j garnet and epidote, 39^' Disseminated epidote.

400 435 Good iron formation} interbedded with schist and chlorite.422' l" quartz stringer.

435

443

447

454

460

443

447

454

460

500

Weak iron formation; abundant schist.

Good iron formation.

Non-magnetic schist.

Iron formation and schist.

Abundant FeÔj bands and quartz bands; weakly magnetic quartz-biotite schist

interbedded with bands; good iron formation

500 555 Goovi f 3^4 find ecUiat and chlorite; more homogenous;tendency for magnetite bands to be less distinct j good ironformation.545' to 555' Bands very distinct.449' l" garnet parphyroblasts.

Schistosity 50-800 to core axis.

555 561 Quartz-biotite schist,

561 568 Schist and chlorite; minor FeoO^ l weak iron formation.

568 585 Massive iron formation with thin quartz stringers interbedded.

585 539 Weak iron formation.

589 597 Quartz-biotite schist; non-magnetic.2" garnet parphyroblasts,

597 601 White pegmatite.

601 612 Highly contorted quertz-biotite schist,

612 6l6 Whit o pegmatite,

6l6 617 Core m

- Pfige 3 - Hole No. F-2.32 continued

{[From To Feet

61? 626 Quartz-biotite schist.

626 6^7 Core miBsing.

6P7 631 'white pegmatite.

631 6^8 QuartK-biotite eohiatj non-magnotic,6W to 645' Core missing,

Schistosity ?0*K)0 to core axis,

KMD OF HOLT?,

60 '

W. T. Sv:enscn, Chief Geologist

t Tiiii AHACOHDA COMPANY (CANADA) LTD.

LOO QF DIAMOND DRILL HOLE F-233

Location: Line 11+80N at 35+10'*' Core j AXTBearing: Wont lodged by: F.J.FrensonDip: -650 Date: July 11, 1956.

Hole Drilled by: Canadian longyear Ltd., North Bay, Ontario,

From To Description Feet "*"

O ,?3 Overburden.

?3 49.5 Quartz-blotite schist,43' to 44* l 1 contorted zone with tale.

49.5 60,5 Gneissic rockj quartz-biotite-plagioolase;fine grained} sharp contacts,

60,5 #9 QuartB-biotite schist vdth bands of mostly biotite andamphibolite.60,5' to 61,5' Core missing, 76' to 79' Core missing.

89 91 Biotite-amphibolite schist.

91 100 Quftrta-biotite schist with bands of biotite and amphibolite.Schistosity 70-BQ 0 to core axis.

100 173 Quarta-biotite schist; bended with amphibolite Bchist whichhas little quartz; lot of biotite and amphibolite; allamphibolite bands are contorted.

173 '503 Hornblende schist with eome quartz-biotite and garnet jcontorted jweakly magnetic bands.184' to Ift6* 2' zone of great change in schistosity.


203 339*5 Very good iron fomationj fine quartz banding; contorted;attitude RO-90 0 .315' Some garnet and amphibolite in iron formation;

attitude steep throughout 80-900 ,

339.5 347 Quartz-biotite schist with bands iron formation,

347 393 Fine grained quartz-biotiteschist; a little garnet andamphibolite.

393 400 Good iron formation with garnet end amphibolite.Schistosity 00-850 to core axis,

400 416 Good iron formation; banded with amphibolite and quartz;some gqrnet,

416 417 Pink pegmatite.

417 426.5 Good iron formation; 2 schist bands,419' to ;,20' l' zone attitude li0 to core.

"' ; -

" ^^Hole No,

FromFeet

V-.' 426.5

' 436.5

445.5

478

485

500

5QO

526

529

536

538

587.

588

F-233

To

436.

445.

478

485

500

520

526

529

536

533

587

588

600

- Pfige 2 -

continued.

peacriptiqn

5 Pink pegmatite,

5 Good iron formation} amphibolite and quartz.

Quartz-biotite schist} weak iron formation bandsj mostly fine grained} some garnet, 450' 6" peffaatite.

Good iron formation} banded with amphibolite and quartz. 481' 6" pegmatite.

Iron formation} with* few bands of schist. Schistosity 75-800 to core axis.

Good iron formation with a few schist bands. 500.5' to 502' 1,5' slighly magnetic with quartz and biotite, Fine grained rookjquartz-biotite} feldspar} amphibolite} looks granitic} oharp contacts. 522' 4" band iron formation} sharp contacts.

Iron formation} banded with schist.

Very good iron formation} quartz banding} contorted,

Pink pefjnatitej coarse.

QuartK-biotite achiet} non-magnetic. 546' Drag fold. 556' to 557' 1' contorted zone} some feldspar.

White pegmatite.

Quartz-biotite schist.590' to 591' Gore missing.

600 640 Quartz-biotite schist.613' to 614,5' Core missing.6l6' to 618' Core missing.638' to 639' Core missing.

640 644 Fine grained rock} quartz-biotite} feldspar} lobks granitic.to 644' Core

644 643 Quartz~biotite schist.647' to 648' Core missing.

Schistosity 80-900 to core axis,

648 END OF HOIK,

W.T. i5wensenj Chief Geologist

t THK ANACONDA COMPANY (CANADA) LTD,

LOO OF DIAMOND DRILL HOLE F-243

Location: Line 18+65W at A3+30N Core: AXBearing: North Loflged by: D.B.MorrisonDip: -A50 Date: August 10, 1956.

Hole Drilled by: Canadian Longyear Ltd., North Bay, Ontario.

Froia To DescriptionFeet

O 19 Casing.

19 22,5 Pink 'granite texture 1 Pegmatite.

22,5 29 Quartz-biotite schist with thin quartz bands interbedded.

29 29,5 Schist replaced by plagioclase; tremolite? and minor garnetand quartz,

29,5 37 Prominent biotite bands.


38 39 Microcline and quartz and minor schist.

39 125*5 Salmoin Pink pegmatite; large microcline crystals) quartz andminor muscovite and plagioclase 'lumped 1 biotite to chlorite inclusions.64* 'Graphic granite' appearance in places. 74' Schist inclusions. 116' 'Salmon Pink' large crystals.

125.5 12S Schist inclusion.

128 147 Salmon Pink pegmatite; large crystals; plagioclase; microcline.

147 157 Dark green ohlroite with garnets and minor calcite? andpyrite on bedding planes.

157 183 Pegnatite; 'granitic' with blood red tinges on feldspars andsmall brownish-orange garnets, 172' Chlorite and garnet inclusion.

183 192 Chlorite; garnet schist and minorSchiotosity 30*S50 to core axis.

192 207 Interbedded chlorite; FejO/^ bands and few wide, contortedquartz bands,

207 213 Contorted bfrren schist with fine quartz.

213 255 Interbedded Fe-jOi bands and fine, thin quartz bands; goodformation.

245' to 2/,? ' Chloritized biotite and calcite (contorted).

- Page 2 -

|Hole No. F-243 continued

From To Feet

255 26? 'Salmon Pink' pegmatite with biotite and ohlorltlaedbiotite inclusionB.

267 268 Biotite.

268 281.5 Interbedded Fe-jO^ and thin quartz bands,

281.5 282.5 Pink pegmatite.

282.5 290 Schist} chlorite and FeÔ,.

290 293 Schist.

293 308 Interbedded chlorite with garnet and schist and quarte bands,

308 332 Quartz-biotite schist; medium grained.


333 335 Core missing.


336 347.5 Quartz-biotite schist- medium grained.346' to 347' Cor* missing.

347.5 353 Quartzj plagioclase} small garnets.

353 400 Quartz-biotite schist) coarse; prominent biotite banding]generally contorted} scattered, email quartz and plagioclase in-clusione,368' to 370' Cora missing.362' Pyrite on seam.371* 2" garnet porphyroblast*; contorted.


400 497 Quartz-biotite schist} biotite finely banded} contorted anddrag folded locally; contortion usually quite uniform. 415' 6" white pegmatite. 425' 4" white pegmatite. 452' to 4561 'Salmon pink 1 pegmatite. 461* to A63' Pink pegmatite. 482' 6n white pegmatite.

Schistosity 60-75* to core axis.


498 KND OF HOU-:.

UO.

THK ANACONDA COMPANY (CANADA) LTD.

LOO OF DIAMOND PR TII, HOLE F-244

Location! Line 19+55W at 43+75N Corei AXBearing: North Logged by: D.B.MorrisonDipt -450 Datei August 13, 1956,

Hole Drilled by; Canadian longyear Ltd., North Bay, Ontario,

From To Description Feet

O 5 Casing.

5 20 Quartz-biotito schist; fairly homogeneous gossan on seams. 12' to 13' Core missing.

20 24 Interbedded ohlorite-garnet bands and schist; occasional weakFe-jO^ band

24 33 Chlorite bands with garnets; quartz inclusions; schist bands.

33 45 Quartz-biotite schist with oriented amphibole crystal* and minorgarnet.

45 50 Fairly massive chlorite; minor schist with reddish, Adamantine(metamorphic?) mineral between biotite plates; (feldspar??)

Schistosity 60-65" to core axis.

50 55 Massive chlorite (no structure).

55 76 Pink pegmatite; large orthoclase crystals, quartz and largebiotite inclusions.

76 142 FdjO^ bands; interbedded with thin quartz bands and occasional,thin chlorite; schist bands. 64' to 85' Banded chlorite. 125' to 127' Weak iron formation, 137' to 138' Schist.


142 143 Schist.

143 159 Banded chlorite-garnet bedding; schist bands; quartzinclusions and occasional weak Fe304 band,

159 192 Quartz-biotite schist with minor quartz inclusions.160' to 170' Minor garnet.

Schistosity 3D-35" to core axis.

192 207.5 Pink pegmatite; large microcline crystals; quartz and minor biotiteinclusions, ('graphic granite' texture in places.)

207.5 254 Quartz-biotite schist; occasional coarse biotite banding; minorpegmatite inclusions; calcite and pyrite on parting seams.(300). 211' 6" pegmatite,


- Page 2 -

Hole No. F-244 continued.


254 256 White pegmatite with soft, white fibrous mineral tale?

256 261 Some ai from 207.5 to 254.

261 271 White pegmatite; plagioclase, quartz and small garnets.262' to 263' Core missing.

271 359 Quartz-biotlte schist; minor pegmatite inclusions in schist.309' to 310' White pegmatite withanall garnets. 319' Coarse biotite banding; contorted slightly*

330' Coarse biotite banding; contorted slightly, 331' 5" white pegmatite. 345' Blue-gray calcite on seams. 350' Contorted biotite banding.


359 364 White pegmatite; plagioclase with small gamete and microcline;'granitic' texture in places.

364 400 Quartz-blotite schist,369' 6" whit e pegmat it e. 397' to 398,5' White pegmatite.

400 406 White 'salmon* pink pegmatite; microcline; plagioclase;quartz; muscovite.

406 500 Quartz-blotite schist; fairly homogeneous and medium grained.t to 429.5 Salmon pink pegmatite.

Micaceous quartzite. 438' to 43V Graphic granite. 440* to 441' Pegmatite inclusion.450' to 455* Salmon pink pegmatite} microcline, albite;

quartz; weathered biotite; muscovite and garnets.

458' to 4^0' White pegmatite} albite and (jiarta and serpentine. 479' to 432' illite pegmatite; 'granite' texture; albite; quartz

and altered biotite. 400' Serpentine on ee&m.


500 555 Quart z-biotite schist; medium grained through-outj minorcrenulations of biotite.


555 565 Light 'salmon pink 1 pegmatite; large microcline crystals;albite; quartz; altered biotite.

565 570 San* as from 500 to 555.Schistosity 550 to core axis.

570 END OF HOLE.

"-

THE ANACONDA COMPANY (CANADA) LTD.

LOQ OF DIAMOND KlIIX HOLE F-246

Locations Une 20+98W at 48+64N Corei AXBearing.' North- East Logged by t D, B. MorrisonDipi "450 Date: August 20, 1956.

Hole Drilled by i Canadian Longyear Ltd., North Bay, Ontario.

To

O 22 Casing.

22 41 Quarta-biotite schist with quarte inclusions; biotite bandscoarse and contorted.

41 53 Whlto pegmatite plagioclase; quartz; muscovite and smallgarnets.

53 66 Quart&'biotite schist; fairly homogeneous,6V 5" white pegmatite.

66 114 White pegmatite; minor schist inclusions* (same as previous peg.)105' to 114' Minor 'salmon pink 1 pegmatite.

11A 121 Quertz-biotite schist.

121 123 înk pegmatite with schist inclusions.

123 127 Quartz-biotite schist.

12? 128 'salmon pink 1 pegmatite.

128 143 Contorted quartz~biotite schist; coarse banding.143' Calcite and platey pyrite on tight seam.

143 147 V/hite pegmatite; medium grained; plagioclase; quartz andmuscovite .

147 151 Contorted schist.

151 162 White pegmatite; (aani&as previous); minor garnet.

162 200 Quartz-biotite schist; medium to coarse biotite banding withoccasional crenulations and quartz inclusions; calcite (blue-gray);

pjatey pyrite on tif.ht sea-ue. lf)0 f Serpentine on tight seam.

200 204 White pegmatite; plagioclase; quarta and muscovite.

204 225 Quartz-biotite schist; medium grained.

225 228 Ff.le 'salmon pink' pegmatite; microcline j plagioclase; quartzand muscovite.

228 237 Schist.

- Page 2 -

(Hole No. F-?4^ continued

From 12 DeBgription Feet

237 240 White pegmatite; blue-gray; calcite on fractures,

240 249 Qrenulated coarse biotite bands.Schistosity 40-50" to core axis.

249 272 'Salmon pink' pegmatite; large microcline crystals;quartz; muscovite; small reddish-orange microcline crystals inplaceB,259' to 260' Schist inclusion.

272 285 Quertz-biotite schist; prominent biotite banding.Schistosity 50C to c ore axis.

285 296 Interbedded schist and chlorite garnet bends,

296 320 Interbedded bands of chlorite-gamct schist (quartz-biotite)and occasional thin FeoO^. 310' to 320' Increased schist.

Schistosity 30-40" to core axis,

320 341 Interbanded PeÔ^j minor schist and ohlorite and thin quartzbands,

341 352 Contorted, coarse banded schist with pink and white pegmatiteinclusions.34B' to 349' Core missing. 350' to 351' Core missing.

352 400 Interbedded Fe30^ bands and thin quartz bandsj minor ohloritebands; calcite on tight eeajis. 354.5 to 355' Banded chlorite. 373' 4" quartz inclusion and minor pyrite.

Schistosity 30-650 to core axis.At 395 1 O 0 ,

400 439 Interbedded PeoO^ bands and thin quartz bands; minor chlorite bands;calcite on tight seane. 404' Schistosity 0-20e ,4?2' 3" mieroclino; quartz inclusion; finegrained. 420' to 440' Sohiet and ohlorite increase.

Slight PeoOi decrease,Schistosity 50-80" to core axis.

439 443 Contorted chlorite-garnet and schist bands.

443 478 'Salmon pink' pagraatite; large Microcline crystals (graphicgranite); quartz; minor biotite,

483 Quartss-biotite schist,483' Contorted biotite.

'Salmon pink' pegmatite.

489 494 Schist.

^^l

- Page 3 ~

No. F~2lv6 continued,

from To

50? 'Salmon 'pink 1 pegmatite,

502 EWD OF KOLK.

W.T, S'vensen, Chief Geologist,


LOO OF JIAMOND DRILL HOLE F-248

Location: Line 8+OOW at 15+OON Corel AXTBearing: South-West Logged by! D.B.MorrisonDip: -700 Datej Sept. 6, 1956.

Hole Drilled byi Canadian Longyear Ltd., North Bay, Ontario.

Frofl|i To DeBcriptiQn Feet

O 18 Casing.

18 326 Quartz-biotite schist} medium grained with occasional greenish- yellow alteration mineral} (serpentine) and thin tale stringers between bedding planes} calcite and pyrite on seans. 32' 2n quarts.41' Tight seam with calcite wash and platey pyrite. 80' to 100' Core broken up into small fragments, 83' to 85' Core missing. 91' to 93' Core missing. 148' to 150' Core missing. 150' to 180' Biotite slightly coarser grained. 163' l" pegmatite inclusion, 210' to 211' White 'graphic granite' 216' Biotite shows 2 bedding planes. 237' 6" white pegmatite. 245' Biotite shows 2 bedding planes. 25?' Drag folding of white pegmatite stringers. 2?8' Calcite and pyrite on tight se&n.

Schistosity 70-850 to c ore axis,

326 331 Schist with garnet and chlorite and minor FeÔ^.

331 338 'Salmon-pink' pegmatite} microcline} plagioclase} quartz.

338 360 Interbedded FeÔ/^ { thin quartz bands} chlorite and minor schist.

360 369 Interbedded schist} and chlorite-garnet zones} minor bands FeÔ^.

369 470 'Salmon-pink' pegmatite; large to small microcline crystals}quartaj (graphic granite')} minor muscovite and plagioclase and weathered biotite,

470 496 Quartz-biotite schist with occasional ohlorite-garnet-FeoO^ band.


497 567 Interbanded FeoOij fine grained quartz and schist bands} biotitein schist altering to chlorite.

Schistosity 45-800 to c ore axis.

567 728 Quartz-biotite schist} minor quartz inclusions} biotite banding}medium grained} occasional ehlorite-garnet band} pyrite and blue-gray calcite on tight seams. 575' ?" quartz inclusion. 581' Oarnet-ohlorlte band.

- Page 2 -

No. F-248 continued.


626' to 627 ! Core missing.665' to 700' Small, indistinct garnets, disseminated in schist.


728 730 Contorted Fe~0,j quartz; chlorite-garnet.

730 732 Quartz-biotite gneiss.

732 733 Fe30/. cnlorite end schist.

733 734 Pink 'graphic granite'.

734 735 ê304 chlorite and schist.

735 737 Pink 'graphic granite'.

737 768 Intorbanded Fe-sO^j fine grained quartz and schist bands jbiotite in schist altering to chlorite and chlorite bands.

768 770 QuartK-biotite schist; minor quartz inclusions; biotite bandsaltering to chlorite.

770 7?2 Good iron formationj highly magnetic} well banded} minorhornblende.

772 775 Pink pegmatite.772' 6" pink pegmatite.

775 7#2 Good iron formationj highly magnetic) well banded} minorhornblende.


782 816 Non-magnotic quartz-biotite schist; rich in hornblende,788' to 790' Core missing. 794' to 796' Core missing.

816 END OF

00 .

W.T. Sweneen, Chief Geologist.

THE ANACONDA COMPANE (CANADA) LTP.r

LOG OF DIAMOHO DRILL HOLE F~249

Location: Line 12+OOW at 13+50N Core: AXTBearings South-West Logged byi J.A,CameronDip: -750 Datei Sept. 15, 1956.

Hole Drilled byj Canadian Longyear Ltd., North Bay, Ontario.

From To Prescription Feet

O 16 Casing.

16 208 Quartz-biotite schist} non-magnetioj locally highly siliceous}minor hornblende} garnet and pyrite. 68' 3" quart a stringer 71' 3" quartz stringer I6li to 162" Core missing. 1?6' to ISA' Core missing. 193' to 195' Core missing.


206 239 Quartz-biotite schist; non-magnetic, except for several bandsof weakly magnetic schist} area is very rich in hornblende} garnet and pyrite.

239 260.5 Good iron formation} highly magnetic} well banded; minor hornblendeand epidote} iron formation slightly contorted.

260.5 277.5 Pink pegimtite.

277.5 310 Good iron formation} highly magnetic} well banded} minorhornblende and epidote} iron formation slightly contorted.

310 322.5 Non-magnetic quartz-biotite schist with numerous b ande ofminor hornblende and garnet. 313' 6" pink pegmatite.

322.5 326 Pink pegmatite.

326 326 Quartz-biotite schist} non-magnetic.


338 351 Quartz-biotite schist} non-magnetic.

353 361 Non-magnetic quartz-biotite schist with frequent bands of Fe.jOi,

361 376.5 Good iron formation} highly magnetic and well banded} slightlycontorted.

376.5 3B4 Non-magnetic quartz-biotite schist.Schistosity 75-850 to core axle,

384 AGO Medium grained pegmatite} some pink but mostfcwhite.

- Pa/je 2 -


From To Feet

^00 416 Medium grained pegmatite} Borne pink but mostly white.

416 4?2 Qunrtz-biotite schist j non-magnetioj locally highly siliceous}minor hornblende and garnet and pyrite.

422 M 1.5 Sane ae 400 to 416.

441.5 U3 Same as 416 to 422.

44-3 454.5 Same as 400 to 416.

454,5 591.5 Same as 416 to 422.553' 3" quartz stringer. 575' 3" quartz stringer.

591.5 594.5 White pegmatite.

594.5 657.5 Quartz-biotite schist} non-magnetic j minor hornblende}garnet and pyrite; locally highly siliceous.

657.5 661 Medium grained pink pegmatite.

661 663 Interbedded quartz-biotite schist and FeÔ^} area rich inhornblende and garnet.

663 675*5 Good iron formation} highly magnetic} well banded.

675*5 679 Medium grained pink pegmatite,

679 766 Quartz-biotite schist} non-magnetic} minor hornblende}garnet and pyrite} locally highly siliceous.


766 END OF HOU:.

W. T. Swensen, Chief Geologist

V*"***THIS ANACONDA COMPANY (CANADA) LTD.

TOG OF DIAMOND DRILL HOLE F-260

location: Line 16+OOW at 41+85N Corei AXBearings North Logged byt D. B. MorrisonDip: -450 Hat e i Sept. 5, 1956.

Hole Drilled by: Canadian Longyear Ltd., North Bay, Ontario.

From To I)0sori..^tion Feet

O 60 Casing.

60 150 Quartz-biotite schist j generally medium grained withoccasional small zones of coarse, slightly contorted biotitebands; calcitewash and occasional platey pyrite on tightseams.70' Occasional thin tale plates on bedding planes j

alteration product. 107' Soft, greenish-yellow alteration mineral]

serpentine and calcite on sean. 113' Second bedding plane (biotite) j not as

prominent as first. Schistosity 300 to core axis, 115' to 116' Core missing.


lf)0 157 White pegmatite with schist inclusions} plagioclase;quartz; microcline; biotite,

157 228.5 Saino as from 60 to 150,160' Thin bend (slightly contorted) of fine

grained microcline on seam.183' Blue-gray calcite wash on tight seam, 3.90' to 191' White pegmatite; quarts; microcline; (large

crystals); 'graphic granite'.

228,5 287 'Salmon pink' pegmatite; 'graphic granite 1 } large orangieh-brownish microcline crystals; minor quartz; minor hornblende inclusions; plagioclase very limited. 252' to 254" Quartz-biotite schist, 254.5 to 255.5 Core missing. 257 ' to 262' 'Blood-red' tinge to feldspars; smaller crystals;

increase in quartz.262' to 270' Increase in plagioclase and quartz. 274' Small garnets. 274.5' 'Fossil' bedding plane of schist as indicated

by bands of altered biotite (now bleached) endsmall garnets,

287 3ffl Quartz-biotite schist; fine grained to give dense, homogeneousappearance.189' Minor quartz inclusions, 192 ' i* M K 1931 H H H305' Sofr, greenish-yellow alteration mineral on seams.313.5' 2" white pegmatite.320' 6" white pegmatite.

- Page 2 - .

I'lole No. F-260 continued.

From To Inscription

320' to 340' Quartz-biotite schist generally medium grained with occasional small B ones of coaroej slightly contorted biotite bands; calcite wash end occasional platey pyrite on tight seams.


398 412 Biotite altered to chlorite; minor calcite and quartz?disseminated pyrite throughout. 402' to 403' Pink pegmatite. 405' to 406' Pink pegmatite.

412 422 'Salraon-pink' pegmatite j microcline} email to large crystals}mall hornblende inclusions throughout} difficult to see any quartz.

422 517 Biotite altered to chlorite* minor calcite and quartz?dlsnaninated pyrite throughout, 428' Bedding planes visible. 433' to 434' Pink pegmatite. 440 ' to 450' Brecciation aone; angular pieces of

microcline in a chlorite matrix. 454' to 455' Brecciation Bone. 445' to 455 ' Massive looking chlorite. 460' to 490' Massive chlorite with pyrite disseminated throughout;

occasional small fine grain pink feldspar crystalswhich show angular outline of former largefragment.

473* Minor epidote.4#3' Small inclusion of brecciated microcline, 489' Small FeoCK inclusion 490' Same, 491' Same. 49R 1 Microcline inclusion. 513' to 514' Brecciated microcline.


517 525 Interbedded Fe} chlorite and quartz} weak iron formation,

925 533 f'®~0, j quartz and chlorite bands.3 4

533 534 Medium grained microcline; plagioclase and quartz.

534 535 Interbedded Fe-jO, 5 quartz and chlorite bands.

535 536 Medium grained microcline; plagioclase and quartz.

536 550 Interbedded R*,,0 ; quartz and chlorite bands.547' to 548' 3PSnk pegmatite.

550 551 Brecciated microcline.

551 559 Interbedded FeÔ, j quartz and chlorite bands.556' to 55fl' Microcline crystals.

559 564 Fine grained feldspar crystals; hornblende and chlorite.

- Pege 3 -


From To Description fget

564 574 Interbedded FeÔ/^j quartz; minor chlorite.

577 Biotite altered to chlorite.

577 593 'Salmon pink 1 pegmatite; 'graphic granite'j large microclinecrystals; quartz;plagioclase. 581' to 58?' Core missing. 588' to 593 f Schist inclusions.

593 600 Quarta-biotite schist; generally medium grained with occasionalsmall zones of corase; slightly contorted biotite bendsj calcite v;aah end occasional plotey pyrite on tight seams. 6W to 64 5' Core missing. 649' to 651' Core misoing, 650' to 657' Core missing. 6?2' 2" quartz.

680 703 Quartz-biotite schist; fine grained to give dense; homogeneousappearance. 691' to 69?' Core missing.

Schistosity 45-800 to c ore axis.

703 EHD OF HOLR.

\ -^.c-o-^

W.T. Swensen, Chief Geologist.


LOG OF DIAMOND DRILL HOLS F-263

location: Line 16W at 12+50N Corel AXTBearing J South-West Logged byt F.J.FransonDip: -700 Date! Sept. 20, 1956.

Hole Drldled by: Canadian Longyear Ltd., North Bay, Ontario.

To Description Feet "~

O 26 Casing.

26 190 Non-magnetic quarta-biotite schist; pyrite and carbonate onparting soaras.43' to 44' l 1 white pegmatite. 120' to 122' Core missing. 131' to 133' Core missing. 181' to 182' lJ Quarts. 183' to 186' Core missing.


190 199 VMte pegmatite vdth few schist stringers,

199 232 Non-magnetic quartz-biotite schist) dense) fine grained) beddingnot very distinct) minor hornblende) pyrite) garnet) few quartz stringers,

232 258.5 Biotite hornblende schist with a little fine grained quartz)minor pyrite and garnet) just a trace of magnetism.

258.5 302.5 Strongly magnetic iron formation) fine quartz-biotite-hornblendebands) minor pyrite) few l' to 2' zones very dense and massive. 203' to 284' l' nonmagnetic quartz-biotite-hornblende schist. 301' to 302* Core missing.

302.5 330 Non-magnetic quartz-biotite schist with hornblende) minor pyrite)garnet) with narrow magnetic bands.


330 376 Fine grained massive non-magnetic quartz-biotite schist)high in quartz) minor pyrite) garnet) feldspar.337' )341' ) Pyrrhotite stringers.346* )

376 386 Quartz-biotite-hornblende-garnet schist,081' 6" quartz.

386 553 Pegaatite) pink) very coarse grained) quartz) feldspar) muscovite) aeome red garnet; very minor biotite and tourmaline) muscovite generally yellowish. 482' to 483.5' Non-magnetic quartz-biotite schist.

553 667 Quartz-biotite schist; non-magnetic.Schistosity 65-900 to core axis.

~ Pnge 2 -

Die No. F~263 continued.

From jTo DescriptionFeet

613' to 6l/*' Core missing.6l6' V schist with Fe30^ bands.637' 4" pegmatite} some fine disseminated FeS in

quartz.648 1 to 649 1 Core miefiing.661' to 663' Core missing.665' to 665.?' 8" rich in red garnet.

66? 67-5 Iron formation? strongly magnetic.

675 684 Iron fonnationj interbedded querte-biotite schist and Fe-jO^bands,generally less than i"j strongly magnetic,

684 688.5 Non-magnetic quartz-biotite schist j rich in fine grained quartz.686' 3" pink pegmatite.

688.5 700 Iron formation; interbedded quarta-biotite schist and FeÔ^ bands,generally less than ^"j strongly magnetic.

Schistosity QO-900 to core axis.

700 701 Pink pegmatite} coarse grained.

701 BMD OF HOW.,

W.T. Swensen, Chief Geologist,

Approximate

E S O

N

u

i

Claim-75S2

Ho/a F'306 -130' -50*5

S/ HOI* F-303-472'-90LP

Cofner

Hole, F-301 ~ 252' ~SOCS

Claim 767O

Hole F-304 ~ 300' ~5O*S J.

i\Hole F-302~430'-5Cfs

byV

*\*'

To Accompany Reporf- of A^be^stncnt \fjoi-k onGroup l ; 7540 7541 7542 7S'43 7545 7546

7547 7549 75 5O 755; 7552 75537S5-7 7555 7556 7557 7555 75&0

Group 2: 7544 767 ;

75623: 7559 756 ; 7562 75t3 75(^4 75657566 76i^C. 7(^67 7668 76^9 7&7O7677 7676 76S2 7653 7664 7685

i! K ANAC.ONDA C-OWI-ANYl' AfJ/'.f ;A' l IK' 1 i C O

SKETCH SHOWING LOCATION OF D.D. HOLES F-3O/-3O4

lil AWIt l V.R M.C.

DWJ. fi'

THE ANACONDA COMPANY (CANADA) LTP.

OF DIAMOND DRILL HOLE F-303

Location: Claim 7552^ Cores EXTBearing i South**"0 Logged by t P. K. BrownDip; -50" Datei June 14th 1956

Hole Drilled by: Canadian Lonjgrear Ltd., North Bay, Ontario

From To Description.Feet

O "34* Overburden

34 41 Fine grained, white pegmatite

41 56 Quartz biotite schist53 * - 53.5' Core missing Schistosity 750 to core axis

56 57.5 Fine grained, white pegmatite

57.5 112.5 Quartz biotite oohist Schistosity 55* to core axis58' - 60.5' Core missing 68' 2" white pegmatite 71' - 73' Core missing 80' - 82' Core missing 85' - 87' Core missing 971 -99.51 Core missing 100* - 100.5' White pegmatite 103' - 104 ' Core missing

112.5 117.5 Amphibole rock; medium grained actinolite andtremolite; some brown biotite; locally some pale green feldspar (plagioclase); no banding evident. 116' - 116. 5 1 Core missing

117.5 172 Quartz biotite schist; fine grained; locally veryhigh in quartz Schistosity 80" core axis

172 173 Core missing

173 178.75 Dense, fine grained, light grey look (to dark grey);not hard; many thin irregular veinlets of CacO^ (white); no banding evident; possibly some ZrtS (some HjjS with HC1 acid).

178.75 221.5 Quartz biotite schist Schistosity TO0 to core axis169' - 192' Core missing 192' - 193' White pegmatite; quartz ~ un

identified mineral; hard (6 or more) ;cleavage appears to be oolumner

193 f - 195' Core missing 202' 4M White pegmatite

221.5 240.5 Pink pegnatite; coarse grained; feldspar, quartz and somebiotite and muscovite. 238' - 239' Core missing

continued -

* ** Page - 2

Hofe No. F-301 ~ continued

Frog To Feet

240.5 250 Quartz biotite schist Sohietoeity 400 to core axis241' 6" pegmatite 242' 6" pegmatite

250 252 Pegmatite

252 BOTTOM OF HOIB

W.t. Swenflen, Chief Geologist


LOG OF DIAMOND DRILL HOLE F-302

Location: Claim ?6?0 Core: EXT Bearing: South Logged by: D. B. Morrison b Dip: -500 F. J. Franson

Date: July 5th 1956

Hole Drilled by: Canadian Longyear Ltd., North Bay, Ontario


O 50 Casing

50 430 Quartz, biotite schist; minor hornblende; slightlycontorted; fairly homogeneous with occasional quartz stringer. at 55* Schistosity 90* to core axis

8?' - 88' Pink pegmatite 99 ! Pyrite on parting planes

120' 2" pegmatite 122.5 - 123.5 Pink pegmatite 12? - 128 Pink pegmatite 135 - 136.5 Pint pegmatite

at 143 ' Schistosity 90" to core axis 151 - 152 Pegmatite and quartz 160 Calcite and flaky pyrite on seams 175 - 176 Pink pegmatite

at 184' Schistosity 900 to core axis(approx. attitude only due to natureof schist)

190 Small pyrite cubes 195 Bedded quartz contorted

212 2" pegmatite and pyrite228 Pyrite and green alteration mineral242 l" fine grained scattered pink

feldspars and hornblendeat 258' Schistosity 600 to core axis

262 Blue-grey, clay-like alterationmineral on seams

268 - 271 White pegmatite 268 Serpentine on seam 275 Pyrite on seam 280 - 283 Quartz inclusions 310 - 315 Higher quartz content 315 - 316.5 White pegmatite 333 l" pegmatite 353 Pyrite on seams 354.5 - 356.5 White pegmatite 370.5 Pegmatite inclusions 373 - 376 Massive salmon-red feldspar with

quartz inclusions; very distinctiveat 395 ' Schistosity 600 to core axis

400.5 Quartz bands drag folded^30 ^28 Calcite and pyrite on seams; prominent

END OF HOLE small quartz banding

W.T. Swensen, Chief Geologist


LOO OF DIAMQNP DRILL HOLS F-302

Locations Claim ?6?0 Corer EXT Bearing: South Logged byt D.B, Morrison Dip: -500 F, J. Franson

Datei July 5th 1956

Hole Drilled by: Canadian Longyear Ltd,, North Bay, Ontario

From To Description

O 50 Casing

50 430 Quartz, biotite schist} minor hornblende} slightlycontorted; fairly homogeneous with occasional quarte stringer. at 55* Schistosity 90* to core axis

a?' - 88' Pink pegmatite 99' Pyrite on parting planes

120' 2" pegmatite 122.5 ~ 123.5 Pink pegmatite 127 - 128 Pink pegmatite 135 - 136.5 Pint pegmatite

at 143' Schistosity 900 to core axis 151 - 152 Pegmatite and quartz - 160 Calcite and flaky pyrite on soams 175 - 176 Pink pegmatite

at 18Ji' Schistosity 90* t6 core axis(approx, attitude only due to natureof schist)

190 Small pyrite cubes 195 Bedded quarta contorted

212 2" pegmatite and pyrite228 Pyrite and green alteration mineral242 l" fine grained scattered pink

feldspars and hornblendeat 258' Schistosity 600 to core axis

262 Blue-grey, clay-like alterationmineral on seams

268 - 271 White pegmatite 268 Serpentine on seam 275 Pyrite on seam 280 - 283 Quarts inclusions310 - 315 Higher quarts; content . 315 - 316.5 White pegmatite 333 l" pecraatite 353 Pyrite on seaais 354.5 - 356.5 White pegmatite 370.5 Pegnatite inclusions 373 - 376 Massive ealaon*red feldspar vd,th

quarta inclusions} very distinctiveat 395 r Schistosity 606 to core axis

400,5 Quarts bands drag folded^30 ^8 Calcite and pyrite on ;searasi prominent

END OF HOLE 8mal1 â^* banding

W.f, Swen sen, Chief Geologist

THE Ak'ACONOA COMPANY (CANADA) UP. ^ ji *t*

100 OF .DIAMOND' DRILL HOLE P-304

Locations Claira 7670 Corel EXT :Bearing! South Logged byi D.B. MorrisonDip: -500 Datei July lith 1^6

Hols Drilled bys Canadian Longyear Ltd., North Bay, Ontario

From To Description.Feet ' : ' ' '" .' : '

O 30 Casing

30 45 Quartz, biotite sohist Schistosity 20e to core axis31' Quartz veinlets drag folded32* 3" white pegmatite; abundant muscovite.

45 47.f) White pegmatite interwoven with contorted biotite and horn*blende; altering to chlorite

47.5 59 Quartz biotite echist Schistosity 700 to core axis

59 62,5 Pegmatite; abundant muscovite

62,5 153 Quartz biotite schist Schistosity 800 to core sxii66' Calcite and pyrite on seams 77' Yellow-green alteration lalnerel on

seam.79' - 87' Finer grained schist 87' ~ 89' Oore missing 102t - 10?' Finer grained schist ,

Schistosity 55" to bbre axis 108' Biotite well banded and contorted

153 156 White pegmatite

156 180 Quartz biotite sohist

180 184.5 White pegmatite

184.5 192 Quartz biotite schist187' Drag folded quartB veinlets.

192 195.5 White pegmatite

195.5 230 Quartz biotite schist Schistosity65* to core axis220' Pyrite and calcite on seams225' Some calcite in schist

230 239 White pegnatlte; abundant biotite and muscovite MAQuartz.

239 256 Quartz biotite schistj Schistosity 250 to core axisapproaches quartzite; fine grained biotite. '"V Bluish-white quartz

5 Banded biotite

continued -

Page - 2

No. F-30A continued -

From To De script ion

256 261 Whit© pegmatite

261 2?6 Quartz biotite schist; approaches quartzite; fine grainedbiotite. Schistosity 600 to core exit

278 279 V.'hite pegaatite

279 2C1.5 Quarts biotite schist

281.5 282.5 White pegmatite

282.5 300 Quartz biotite schist Schistosity 65* to core axis283 f Contorted schist

300 END OF HOLE

W.T. Swensen, Chief Geologist

THE ANACONDA COMPAN? (CANADA) LTD.

LOS OF DIAMOND DRILL HOLE F-306————————————————————i..

Location! Cleir^jj4jL-^ Cores KXTBearings South logged bys F.J, FransonDip: -500 Datei July 14th 1956

Hole Drilled by: Canadian Longyear Ltd., North Bay, Ontario

From t To; Description Feet "~

O 18 Overburden

16 25 Fine grained quarte biotite sohiet

25 28 White pegnatite with garnet

28 45 QuartB biotite schist

45 49 Quartz biotite schist45* to 48' Core missing

49 59 Quartz biotite schist49.5' 6" Pegmatite

59 '/2 Salmon-red pegnatite

72 77 Quartz biotite schist72' to 73' Core missing

77 102 fialmon-red pegmatite with altered garnet.

102 133 Quartz biotite schist

133 END OF HOLE

6-*W.T. Swensen, Chfcf Geologist

•2 -t-YlIjJ ..AHAJgQNpA, COMPANY (CAHAPA,) IffI),

OF DIAMfflPJjRIIJ, HOIJS F-4Q1

Location! Claim 7#77t Une 19 SB @ 1*003 Bearingt Southwest Dipi -45*

Corei EXTLogged byi J. A* CameronDate August 10th, 1956

Hole drilled byi Canadian Longyear Ltd,, North Day, Ontario

F.rom

O 20

25

151.5

166

17S.5

183.5 192

201

ai

212.5

215

219

2025

49.5

49.5

63.5

70

77

63.5

70

77

123

166

173.5183.5193

CasingSlightly magnetic and non-magnetic quarts biotite schist and

minor epidote and hornblende.

Good iron formation j well banded highly magnetic minor epidote and hornblende*

Alternating bands of woakly magnetic schist and

Quarts biotite schist, eorae of which is slightly magneticSchistosity 50-65* to core axis*

Quarts biotite rock showing no schistosity! carbonate stringers showing preferred dip of 30*40* j non magnetic.

Alternating non-magnetic and slightly magnetic quarta biotite schist; poorly foliated, almost massive) locally rich inhornblende and garnet.

151.5 Ctood iron fonnationi highly magnetic, except for occasional band of weakly magnetic schist* I,F. is highly contorted and jointed with numerous small scale faulting) minor epidote and hornblende. Schistosity 60* to core axis.

Mixed; non-magnetic end weakly magnetic quarta biotite schist with FejO^ and a hornblende and biotite rook; minor pyrite.Medium grained pink pegmatite with numerous tourmaline crystals,

Biotite hornblende schist; bands slightly magnetic*

Rook composed mostly of hornblende and biotite with minor quarts.

Biotite hornblends schist containing narrow bands of relatively abundant pyrite.

211 Quartz biotite cellist; weakly magnetic; several bands of Fe*0.,

212*5 Kock composed iiwstly of hornblende and biotite with minor quarts and

215

219

229

Same as ehovm for 201 to 211 ft*

Same as shown for 211 to 212,5.

Hornblende biotite ochiet) poor foliation; non-magnetic; chlorite partings; minor pyrite.

continued -

- 2

continued

Frog Vo Foot

229 .^3.5 Hoclc corajjosod raootly of hornblende and biotite with minor(;uarta and

233.5 240 Jiocl: oora}joBod inainly of hornblende vdth abundant froo quarts.

240 248 Slightly limnetic quartz biotite schist; nearly raassive2401 to 241 1 Clood l.F. Schistosity 15* to oore axle.

24B 252,5 Rod; ooaposod walnly of hornblende biotite with minor quartson partings.

252,5 S&& slightly MOKnotio cuarta biotite eohict; nearly mosalve*to S55.5 Good l.F. to to

268 289 Hock corajjosod mainly of hornblende biotite -with minor quartaon partings* to ^S5 fiMghtly r/wignotlo quartz biotite Bohlet.

289 W& Slightly r^notio quarts biotite Bohieitj nearly r-uieaivo,293 to 295 Good l.F,

298 315 tltmlj PoqO^j slightly magnetic quarta biotite eohlet and non-(iagiK)tlo hornblende biotite rockj area contorted vdth many Joints end amall faults. Schistosity 75* to core axis.

315 31# A groon hornblende biotite rock containing iidnor quarts andFoSg; ocoasional area with frequent JolntSj^g and omall ocole faulting, containing

31B 3*^*5 VJooltly isiagnotic cfuartz biotite schist containing bands ofnggnotito*

320.5 342.5 Bamo aa 315 to 3X8 foot.

34^.5 377 V0ry coarse brecciaj rarxiom oriented quarts biotite ochlot andgood iron formitlonj breccia vdth hornblende biotite quarts rocks ooiaantirigj possibly oorao chlorite?? and eorpon tine.

377 392 Quarta biotite schist and quarts biotite rocks with much palegroon mpliibolo??} posolbly eorno brocola with no iron formation} bcmdlng very poorly defined j possibly son© chlorite and eer- pontino.

392 394.5 J'lo3^4 'u^d tjuartz * hornblendei generally flat boddlng| manyDifuJjL fractures*

394,5 400.5 Quarta biotite schist) undefined bedding,

400,5 /J&5 l tedium to otiw^ly i-iagnetic Iron foraationi uoiao to muchlocally mch garnet; locally eoriW epidote) generally Associa vrith

Paô - 3

Hole F-401 - continued

From To Description

400*5 465 continued *40^,5 to 410 Much vory fine, pale pink (clear) garnet.

465 470 Biotite fiarnet quartz rocks; minor FeoOi j some hornblende bands*

470 476 Quartz biotite schist, non magnetic} minor hornblende and garnet}471 to 472 Core missing Schistosity 30-50* to core axis.

476 4^3 Quarte ** hornblende* biotite- rocks} medium to strongly magnetic,bands FOj penerally aa breccia,

483 486,5 Quartz** hornblende** biotite rocks; poorly banded} non-aiagnetlo*

486.5 492,5 Same as 476 to 4#3 feet,

492.5 503 Sarao as 4#3 to 486,5)503' Iris t 2" seems to be quarts biotite schist} non magnetic.

503 END OF HOUB

W, T. Swsen, Chief Geoogist

Till; A!,aGOKi)J\ COjiPAMY. (CANADA)

KX) OF IflATO) PII JjOIft .

Xooatiom KUdia 7#77i Line 20GE o 3*003 Corel KXTBearing! SW togged byt J, A* CaiaaronDipt -45* Date August 14th, 1956

Holo Drilled by i Camditun Jjongyoar Ltd., North Boy, Ontario

O 24 Casing

24 44 Missive rook, composed for the roost part of hornblende butcontains come abundant feldsparj

44 47 1 5 Hornblende biotite echiotjSchistosity 55* to core txtde*

47*5 48,5 Itodiura grfdiiod jlsik po^matitei contains tcumaline.

48.5 49 Saras as 44 to 47.5 feet.

49 60.5 Some as 47*5 to 46.5 foot.

60.5 B5 Good iron foiioationj looalJy very eilicoousj moderately contorted} iiiliK)r hornblende eaid epidote*,

#5 89.5 \7enk3y naftnotic cjuartss biotite ochiet with bands FejO^,09*5 93 Homblendo biotite schist} non-magnetic.

Schistosity 40* to core axis*

93 X47*5 Good iron fonaation} highly contorted and locally brecciated} Vory rich in liornblendo} nAnor garnet, 121* to 12?* Area rich in garnet only moderately mag*

147*5 150 A rock composed mainly of hornblende with rdnor quarta, maoBivoto laediuw K**ained} non-macnetic.

150 156 Good iron formation and slightly laagnetio rpartis biotite schist.Itoglon higlily brecciated} no attitude possible,

156 ?JB Saws aa 147.5 to 150 foot.

210 220.5 Wetikly mngnotio quartz biotite cellist} almost massive.

220.5 36 Alternating wealcly ciagnetic hornblende biotite schist and horn-blemlo quarta rook, with a couple of bands of FeO} rfdncr

261 Fine nrainod rook ooaposod chiefly of homblwdW' and quart*-}minor pyrite.

261 313 todiwa grained rook} coinposod chiefly of hornblende* and quarta-dlenendnated spooks of FeSgj uon-4aasnotio.

313 228 SOT*) as 236 to 061 feet,

continued *-

IV 'Paê - 2

Hole F-402

FroTa Jb Description Feet

33# 350.5 Fair iron formationj highly siliceous; rich in hornblende!scattered pyrite cubesj slightly contorted) minor epidote*

350.5 454 Alternating fine and raedium grained hornblende*, quart e- r©ckwith disseminated speck of pyrite; non-magnetic*

Schistosity 30-40* to core axle.454 470,5 Good iron formation; vrell banded; highly magnetic; rich in

hornblende; slightly contorted; minor pyrrhotite.

470*5 474 A rock composed mainly of hornblende with minor quart?, and FoqOislightly magnetic; fine grained.

Schistosity 60* to core axle,

474 486.5 Sarao as 454 to 470.5 feet.

486.5 493.5 Sane as 470,5 to 474 feet.

493*5 505 Alternating fine and ruadium grained hornblende*, quartz- rookwith disseminated speck of pyrite; non-magnetic*

505 BOTTOM OF HOIJS

60* . SwenBen, Chief Geologist

KK 7697

K K ^699

KK 7698

•f600-650'

KK 7700

Sose

JUN6FRAU LAKE

Locotion ot Diamond Drill Hole*

Soolt: l"* 200'


LOG OF DIAMOND DRILL HOLE F- 600

Location: Line 28K at 8+50N Bearing: South Dip: -520

Core: AXTLogged by: E. BurganDate: Oct. 5, 1956.

Hole Drilled by: Canadian Long/ear Ltd., North Bay, Ontario.

From To Feet

O

90

90

334.5

334.5

387*5

387.5

448.5

448.5 512

512 650

Description

Casing.

Interbedded iron formation] weakly magnetic schist and non magnetic quartz-biotiteschist. Some hornblende and red garnet locally; minor epidote and FoSg, hornblende, generally associated with good iron formation bands. 212' to 214' Many small red garnet.233' 255'

Some white CaCo- in fracture.6" light yellow-white rock; appears to show banding of schist; but biotite completely altered to sericite??

280' to 281.5 ' Core missing.295' 6" white massive quarts.


Generally non-magnetic quartz-biotitt schist; some red garnet; locally minor FeSo and epidote. 3?6' to 378' Core missing.

Interbedded weakly magnetic schist, non-magnetic quartz-biotiteschist and good iron formation; some red garnet; minor epidoteand F 682*395' to 397' Core missing,398' J" pink pegmatite.401' 3" pink pegmatite.422. 5 'to 423.5'Corefnissing.42?' to 429' Core missing.446' l" white quartz.

Generally fair to good iron formation with local bands ofweak iron formation; some hornblende bands associated withiron formation; soiae red garnet; minor epidote and Fe32.457' to 458' 2" pink pegmatite.483.5' 3" quartz.485 ' 3" and l" quartz.490.5' li" quartz.492 ' 5" and 2" quartz.


Non-magnetic quartz-biotite schist; locally some red garnet; sonic thin fractures; 1/16 yellow-white color alteration of unifies j sericite??; minor epidote. 514' to 515' Core missing. 513' l" quartz veinlet.

1 ' * * '

**

Ho 3 e No. F- 600 continued.

From ToFeet

544.5'547'549.5'

550' to558'574'576' )577' )578' )585*595'601,5'608,5*612 1616.5'623'625.5'628'630'639'

- Page 2 —

Description

to 555'to 549. 5 '

550.5'

to 575'

to 587'to 599'to 605'to 611.5'to 616'to 622.5'to 625'to 627.5'to 629'to 635'to 643'

No Core,No Core,J" breccia, generally altered to yellow-white.mineral.No Core.|" quartz.Ho Core,

1" quartz.

No Core.No Core.No Core,No Core.No Core.No Core.No Core,No Core.No Core.No Core.No Core.


650 END OF HOU!.

W. T. Sweneen, Chief Geologist.

CI. 14269

\, \

1 THE ANACONDA COMPANY l ^ " (CANADA* LIMITED l

CLAIM GROUP 19

Dote June 1957 Scole l"-?00'

; -

THE ANACONDA COMPANY (CANADA) LIMITED

DIAMOND DRILL CORE LOG

HOLE NO. A - 606

Location: Line 8+00 W O 2+00 N Bearing: SSW Inclination: -450 Logged by: R.W.M. Core: EXT

From To DescriptionFeet

O 55 Casing

55 63.5 Quartz-biotite schist. Generally fine grained with minorred garnet, hornblende, FeS2. Banding due to variation of quartz-mafic ratio, in general not pronounced.

59 to 63.5 Quartz-biotite schist - standard rock type but increase in red garnet porphyroblasts, fine to - 3 mm, associated with increase in chlorite. Schistosity: 80-

63.5 69 Quartz-biotite schist, standard rock type, alternatingwith quartz-biotite Fe304 schist bands weakly magnetic. Increase in distorted chlorite, red garnet, porphyro blasts associated with Fe304 bands.

69 102 Strongly magnetic iron formation. Banding contrastsstrongly developed, local contortion. Very few red garnet porphyroblasts, much chlorite.

102 253.2 Quartz-biotite schist. (?) Schistosity: 60* to 75'

116 to 119.5 Quartz-biotite schist - standard rock type,but loca^. increase in red garnet porphyroblasts fine to - 3 mm.

153 Small band of quartz.198.6 to 199 Quartz, muscovite, red garnet porphyroblasts,

fine to * 2 ram.216 to 217.8 White pegmatite with inclusions of quartz-

biotite schist, standard rock type. Pegmatite mostly quartz with some red garnet (fine crystals), some FeS2, Quartz milky to pink.

230 to 243 Quartz-biotite schist, standard rock type,but local appearance carbonate veins (calcite?) some transecting schistosity fine to * 6 mm.

253*2 28? Strongly magnetic iron formation, approximately 34# Fe.Banding strongly developed, contortion evident. Increasein hornblende and/or chlorite. Some pyrrhotite present.

Schistosity: 70* to 80*

D.D. Hole A-606 (continued)

From To Feet

Description

287

295

295

430

430

Schist (?)

295 to 297.5

319 to 319.5 325 to 328

348 to 350

360 to 361.5375 to 396400 to 402

420.5 to 430

END OF HOLE

Quartz-biotite schist, standard rock type but local appearance of carbonate veins (cal cite?). Fine to * 5mm with or transecting schistosity. Milky quartz inclusion. Quartz-biotite schist - standard rock type with carbonate stringers fine to * 1/10' and transecting schistosity (calcite?). Quartz-biotite schist - standard rock type with reappearance of carbonate stringers fine to ^ 4 nun. Quartz-biotite schist. Quartz-biotite schist. Quartz-biotite schist, standard rock type but with reappearance of carbonate stringers fine to * 4 mm with transecting schistosity. Quartz-biotite schist, standard rock type also with carbonate stringers fine to * 4 mm with or transecting schistosity.

Schistosity: 70" to 75*

Drilled by Heath and Sherwood, Kirkland Lake, Ontario.

a)W.T. Swensen, Geologist.

tr V- lo 3THE ANACONDA COMPANY (CANADA) LIMITED

DIAMOND DRILL CORE LOG

HOLE NO. A - 607

Location: Line 0+70 W @ 2+00 N Inclination: -450 Core: EXT

From ToFeet

32

42.5

234.5

240.5

32

42.5

234.5

240.5

315

Bearing: South 100 West Logged by: R.W.M. Date: June 21, 1957

Description

Casing

Quartz-mica pegmatite. Mostly quartz, muscovite, some biotite, some white feldspar. Fine grained blu mineral present, likely Fluorite. Some red garnet porphyroblasts fine to * 3 mm. Ingeneral fairly coarse grained. Schistosity: 75 0 to 80*

Quartz-biotite schist generally fine grained with minor FeS2, hornblende, red garnet, epidote, some chlorite especially in distorted areas. Banding due to variation in quartz-mafic ratio in general not pronounced.

62.570.075.085.092119140155174176

to 66 Core mito 72 " Mto 78.5 " "to 86.5 " "to 96 " wto 122.5 " "to 142.5 " "to 157 " "to 175 " "to 187 Quartz-!

232.5 to 233

Schistosity: 75" to BO"

Quartz-biotite schist, standard rock type, but local appearance carbonite veins (calcite?) with or transecting schistosity (zones of weakness). Milky quartz veins. R^ ct.rtc1t.v , 65'Schistosity: to 70'

Iron formation. Bands quartz-biotite schist alternating with bands quartz biotite Fe304 schist weakly magnetic and bands quartz-biotite Fe304 schist strongly magnetic. Local increase in distorted chlorite associated with orion formation, also much FeS2. Banding pronounced due to variation of quartz mafic ratio. Some hornblende associations. 30^ Fe approximately.

Quartz-biotite schist, standard rock type*Schistosity: 85"

271 to 275 Quartz muscovite pegmatite with some white feldspar,some black tourmaline, biotite, fluorite, somecrystals red garnet fine to * 2 mm,

5 to 290 Core missing n H

287,295303

to 297 to 305 Schistosity: 60 0 to ?00

D.D. Hole A - 607 (continued)


315 3?-3 Iron formation with increase in chlorite, hornblende, bandingprominent, highly contorted.

315 to 319 Quartz-biotite schist, standard rock type alternating with bands weakly magnetic biotite Fe304 schist.

319 to 323 Strongly magnetic Fe formation, quartz biotiteFe304 schist. Highly contorted, banding prominent. 25^ Fe approximately.

323 341 Quarzt-biotite schist, standard rock type.Schistosity: 70* to 75"

341 450 Quartz-biotite schist, standard rock type alternating withbands quartz-biotite Fe304 schist weakly magnetic and bands quartz-biotite Fe304 schist, strongly magnetic.

351 to 359.5 Quartz-biotite schist, standard rock type, but local appearance numerous carbonite veins fine to * 3 mm with and transecting schistosity. ~

390,5 to 394 Core missing421 to 423 " " Schistosity: 70* to 75"430.5 to 432 " "

450 END OF HOLE.


W.T. Swensen, Geologist

CI. 7866

CI. 7877

C l 78C.fi

\\ \ CI 76 7 E!

THE ANACONDA COMPANY (CANADA) LIMITED

CI AIM GROUPS L'.-14-iL.

Dote Sept I9.r i/ Scok l ?^'''

THE ANACONDA COMPANY (CANADA) LIMITED DIAMOND DRILL COM LOG

HOU: NO, A -location: line 14+00 E i 2*25 N Bearing: South-WestInclination; -45* Logged by C. H. W.Core: EXT Date: August 16, 1957.


O 54 Casing

54 57 White pegmatite - mostly quarts with minor garnet and somemuscovite. Also some schist inclusions. Fairly coarse grained.

57 90 Quartz-biotite schist, standard rock type, generally finegr&ined with some red garnet and some discontinued FeS2* Also a few bands of weakly magnetic quarts-biotite Fe304 schist* Also one band of white pegmatite as described before. Banding fairly well developed due to quartz-mafic ratio*

90 104.5 White pegmatite, mostly quarts with some muscovite. Also sometourmaline. Generally coarse grained*

98' to 101' Core missingSchistosity: TO0 to 80*

104.5 108 Quartt-biotite schist, standard rock type*

108 111 Pink pegmatite, mostly pink feldspar with quarts, somemuscovite and some tourmaline. Generally coarse grained*

111 120 Quartz-biotite schist, standard rock type with one band weaklymagnetic quarts-biotite Fe304 schist.

120 134.5 Pink pegmatite as described before.

134.5 144 Quarts-biotite schist, standard rock type with some weak ironformation as described*


152 168 Quarts-biotite schist, standard rock type with band* ofweakly Magnetic quarts-biotite Fe304 schist*

168 176.5 Weak iron formation, generally fine grained, weakly magneticquarts-biotite Fe304 schist, approximate H of Fe 10*.

176*5 212 Quarts-biotite schist, standard rock type, tome inclusions ofpink pegmatite as described before*

212 221 Strong iron formation alternating bands of weakly andstrongly magnetic quarts-biotite Fe304 schist, also bands of

non-Magnetic quarts-biotite schist, standard rook type.

l. Hole A-6U (continued)

PromFeet

To Description

221

230.5

252

270.5

274.5

281.5

315

324.5

329

400

405

230.5

252

270.5

274.5

281.5

315

324.5

329

400

405

434

Quarta-biotite schist, standard rock type*

228' to 230* Core missing

Pink pegmatite, standard rock type, as described before*

231' to 234.5' Core missing 240* to 241 1 " "

Schistosity! 70*

Iron formation, alternating bands of weakly magnetic quart*- biotite Pe304 schist, and non-magnetic quarts-biotite schist, standard rock type.

Pink pegmatite - standard rock type, as described before.

Quartt-biotite schist, standard rock type*

Schistosity: 55* Pink pegmatite - standard rock type.

298' to 299* Core missing 307' to 308' " "

Iron formation, strongly magnetic quarta-biotite Fe304 schist, with an occasional band of weakly magnetic quartz-biotite Fe304 schist. H of Fe 2056.

317' to 319' Core missing.

Pink pegmatite - standard rock type.


Iron formation, consisting of alternating bands of weakly and strongly magnetic quartz-biotite Fe304 schist with bands of non-magnetic quartz-biotite schist, standard rock type. Local occurance of abundant red garnet. Discontinued FeS2. Approximate 1 of Fe 10jC.

Schistosity: 60e to 65*

383' to 385' Core missing

Core missing.

White pegmatite, mostly quarts, with local occurance of abundant red garnet. Also some black tourmaline and SOB* muscovite. Generally coarse grained.

416* to 417* Core missing.

D.D. Hole A-614 (continued)


434 490 Quartz-biotite schist, standard rock type, generally fin*grained with local occurance of abundant red garnet porphyroblast*. Minor hornblende and discontinued FeS2. Banding not well developed. Also contains a few carbonate stringers transectingschistosity*

441' to A42 1 Core missing

490 483 Weak iron formation - very weakly magnetic quarts-biotiteFe304 schist. Approximate 5f of Fe 6^.

483 630 Quartz-biotite schist, standard rock type, as described before.


557.5 to 560' * " Schistosityt 400

561' Weakly magnetic

609' to 610 Core missing.

630 END OF HOLE.


W.T. Swensen, Gedlgist

JdkM 100*

K

A HO 3 v* JK A ^V

i ,.,k

f ft.;'

.... y,670.

^tVf

A

/t-

tic.'/

f 302.

^303

/S 1 ?/ a^" .3 ,

THE ANACONDA COMPANY (CANADA) LIMITED ^"/'"" X/.7

DIAMOND DRILL COKE IOG

HOLK NO. A - 901

location: Jjne A @ 54 00 S Bearing: NorthI ne ]i tuition: -BO0 logged by: P,B.A.Core: KIT Date:


O 52 Casing

52 334 Quartz-biotite schist; standard rock type, generally fine grained withlocal occurances of red garnet porphyroblastsj discontinued FeS2. Banding not well developed. Also presence of carbonate stringers transecting schistosity.

134 139 Pink pegmatite, chiefly coarse grained pink feldspar. Also minor red garnet and some black tourmaline, also some muscovite,


205 208 Pjnk pegmatite, as described before.


Schistosity: 609 to ?08

31/4 315 Pink pegmatite, standard rocktype, as described before.

315 AGO Quarta-biotite schist,standard rock type, as described before.

Schistosity: 609 to 808

AOO A5A Quartz-biotite schist, generally fine grained, with minor amounts FeS2, epidote, red garnet porphyroblast s. Some local cai'bonate stringers with and transecting schistosity. Banding due to variation in quartz-mafic ratio in general not pronounced. Some local zones of contortion.

411 to /tl8 Quartz-biotite schist,standard rock type, but highly siliceous. Banding fairly prominent.

/i54 456*5 Pink pegmatite - quartz, muscovite, pink feldspar with some schist inclusions.

456.5 522 Quartz-biotite schist, standard rock type.

492 to 495 Quartz-biotite schist, standard rock type, but highly siliceous with some pink feldspar.

522 533 Pegmatite. Coarse grained, quarta, muscovite, some pink feldspar with some schist inclusions. Some biotite inclusions?

D.D. Hole A - 901 (continued)


533 542 Quartz-biotite schist, standard rock type, but highly siliceous. Some contortion.

542 553 Pegmatite as found 522' to 533'.

553 554 Quartz-biotite schist, standard rock type,

554 555 Pegmatite.

555 619.5 Quartz-biotite schist, standard rock type.

561 to 562 Core ndssing,

6.19.5 621.5 White pegmatite. Mostly quartz, some muscovite, minor pink feldspar. Some white feldspar.

Schistosity: 65* to 70"

621.5 655 Quartz-biotite standard rock type schist,

655 657.5 White pegmatite and some schist intrusions.

657.5 676 Quart '/-biotite schist, standard rock type.

676 678 Core missing6?8 679 Quartz-muscovite pink feldspar pegmatite,679 680 Core missing

680 681 Quurtz-muscovite pink feldspar pegmatite,

681 682.5 Core missing

682.5 789 Quartz-biotite schist; standard rock type.

683.5 to 685 Core missing687.5 to 690 " "707 to 709 " "7.12 to 713 " "

789 800 Pegmatite, fairly coarse grained, mostly quartz, muscovite, Some pink feldspar, some white feldspar.

Schistosity: 70*

800 803 Pink pegmatite, mainly quartz and pink feldspar with minor red garnet and some muscovite generally coarse grained.

803 887 Quartz-biotite schist,standard rock type, generally fine grained with ndnor red garnet, some discontinued FeS2. Banding not well developed, also occasional carbonate stringers transecting schistosity.

882 to 887 Pink pegmatite - standard rock type, as described before,

D.D. Hole-A - 901 (continued)


88? 933 Quartz-biotite schist, standard rock type, as described before,

933 93# White pegmatite - generally coarse grained, composed chiefly of white feldspar and quartz, with minor red garnet and black tourmaline and some muscovite.

938 967 Schist ?

967 975 White pegmatite, standard rock type, as described before. Also containes ome schist inclusions.


Schistosity: 60" to 70*

984 to 985 Core missing 1031 to 1033 Core missing 1038.5 to 1041 " " 1054 to 1057 " "

1069 1072,5 White pegmatite as described before.

1072.5 1126 Quartz-biotite schist,standard rock type, as described before.

1072.5 to 1075 Core missing.

1126 1128 White pegmatite, standard rock type, as described before.


1156 1157 White pegmatite, standard rock type, as described before,

1157 1200 Quartz-biotite schist, standard rock type f as described before,

1186 to 1187 Core missing

1200 1419.7 Quartz-biotite schist, standard rock type, medium coarse grained, generally uniform in attitude. Quartz and biotite show definite banding.

1219.5 to K1.5 Core missing.1238 to 1240 Core missing1248 to 1250 " "At 1245' the quartz-biotite schist becomes coarse grained and

thereafter alternates withithe finer grained variety (this coarseness is notieable at previous footages)

1265.5 to 1268 Core missing.Schistosity: 75* to 80*

1281 to 1283 Core missing.1290 to 1291.5 " "1317 to 1318.5 " "1329 to 1330 " "1342.5 to 1344 " "1358 to 1359 " "

- D.D.Hole A - 901 (continued(


1373 to 1374.5 Core missing 1379 to 1380 " " 1396 to 1398 " "1410 to 1419*7 Quartz-biotite schist becomes very coarse grained

and with the injection of some plagioclase

1414.5 to 1416 Core missing

1419.7 1422 Core missing

1422 1436.5 Medium grained diabase (plag. - amphibole) massive and slightly magnetic; approximately ^ 1& average magnetite*

1436 1474 A transition zones of mostly quartz-biotite schist with minor basic rock, very highly contorted and fractured,

1436.5 to 1438 Core missing 1455 to 1457.5 " " 1460 to 1461 " "


1475 1512 Massive fine grained diabase, and/or andesite, very slightly magnetic, less than 1# magnetite, many minor calcite veinlets. Fractured to a high degree resulting in blocky drilling. Massive apperance sometimes grades into banding giving a likeness to S.I. chlorite schist (similar to rock in F-262) disseminated FeS2 scattered throughout.

1492 to 1492.5 Core missing. 1496,5 " 1497 " "

1512 END OF HOLE.


W.T. Swensen, Geologist.

' -''' ''' : ' 1

location: 3*90N at

Inclination; -90'

Core: EXT !

t'.'.' Vi,'! -..C- " .^"'. •i-'C-i'.'^'!.-* ,*1VC , l K'i'", .., .^(..rl.-LfS

,:îi'li^^W:: Jiî^îyti:*^J*^

Quartzred gai^rwt po

schist inclusions

-.

mm

îytf

i|i^ teî*^••.fevmtfctf-i.

Hole No. From

355

387

394400

412

414.5416.5

A-902 continued

T

435

438

442

446

447

453

455

458

466.5

469.5

471.5

530

549,5

587

602

615

ittiitffi^;ffi?^rtr"^:; if^y^r^-^f^^^^f:-';^: rii^-iiiSi^j^^387 White pegmatite, as

394 Quartz biotite schist, as ^^•400 ' White pegn^tilie, sia^; ^cl^ tyj*,4 ^ ?b- i:;":-W'; ''; -' . ;"H",,-v; 'f';;/,'-;" ':'' ;"\~; '

; ; ...-; 1 :-,'.'--:''1 :'.'. ftL-Sniîrt'-iMwi* .i-^tttt *.A ^Cfn A AOi ,-hA 4O9 W: A ^•...••.•..;\ :i

Quarts bib•v '": -fr

: - ;:^.,,.,T _^ ,. ,.,,,,,,^.-r.,.,-, ...,...

-' 414.5 'White' pegmatite,same 'r^b^ypei;:-Y**iy v : .,^'"';. ^^^^fi^^^'î.^^'-^.'^•l - -' . ' -. ' ','-j. ' l, .V- 'V. . . V'' •\-* i-'f'^."l-: t '',~;''?'fi:''fy'Ji'! n '''i*''''; t 'i'l'.'f'''-;' i ^^

' i.'Yf) K , OUartZ *** "* * * "' '**'*Vt4 e4- . anlHA '•.'.MA'Jiljt. *.w*l*"! l,?J 1 .y" . ''L ; .. .'.. ", '', ".^'*. '.-.t-f':-''V;' . ;t"". ' ...: . t'W

;- 430 White pegmatite, satte

435 Quartz

tit e, -||ifl,ji,ie'ybok1 i 'fcyp(i/'.'.. •. ;,:'- t; '--.J;.'- vi'i... •''•-•- /.^v-^-i'.fi/-''*-'^-^..'^^ •• ii;i - '^

te^dchiet, ;-js(ajHi.e^c^^ê^;; \ ^{-^^ff^y^j^ 'Â -J; iiWhite pegmatite

442 Quartz \Jptite- . ' ,' "' j ' *- .-" '" ' ^' ' ,' , '"' ."'' .•.'-••'- - 1 'i;',: ''.:''. l -'-"'.'.j.^.', '.-'N.'.'. '•'.:v -i'' \.,?. .'^••.-'.••'-."y•446' -. ": White- pegmîte^;"(saj^''-roc;kV^f;'' ''-^ '^'^•^•'•- '-Witf* " " t " i " :

447 Quartz biotite

453 White p6^^fat^#6w'to^ :tySQ*^fo

t- earn? -rooK î;-. .^ ^:'^î^^,^:^; a '' f -.' ''-";-t;'. :'.i,'.'" : . ; . ,;-w ;^.?-;X:'-;:'^;,''' !,v^-^r,^h:-blv.*'-: V

'-i '.'.""V-. ,' 1 "'' " 'v "\ X ''vv. *'-*: ,,'-'*" ;;!"';''-"v" ''-'. . - ""•'••/"•.•.•'f ? ! '.." .•••: 0 "*' ';'.; -5 ' - .''.'

''.'' ; ''"r.:-. ••'•.•i v'' ^.x^rj&ife*. r\:' ;:.'; s '-.'4v:;!. *!' :-^\^titi-'', -W- "v .,-:i.-v',.;v-'- :j J! f-. ..;.,h-....^,.i- 1 .-: r 1-.-VWJJf/^v.^./.-'.lv' :- ', -: ^^'•j^^]i; ':::'ls':'' i;^''?:v:"''-:

; 455' ' Quartz :biotitp':j;ehis^, ! 'same;;:.r^^^ ?"fe^:i.'i5^v:^5S'-lv' ':''^'--

458 : ^Core missing-,/: :?; : : ;,v, ' -^f-r?^ .i)?^ 1??^^^.1 '..^"; s^ft^S^^^vÂ!;

466.5 Quartz biotite, /schist,

469.5

471.5 Quartz bioti,ti isc!••''530-'.-'..; '-White; : pegiraatitei ':ê::Wok';:*3î'^-.^-V'-.v ''^K :,.:1W'^'*."|^: :^^vV:!'v;-U

: , ' 483.0 to IMti ''Qu|rt*'-1iio,ii*:jli^^î,^.i' ; '. ,. ' ,".'' ; .-,'..H^'^re'missing-a J-w*^w*Â^t^v''-v.';^,-;y.r^w,k ^-;.-i.: .-: J

549.5 Quartz biotite schist^: Schietosil.^

589 White pegiaatite' . - -:. •'.•''•''"'.'."•'i-i&f*

602 QuaHz

)f :'tp,;*

Core mAssing615 White pegmatite

624.5 Quartz biotite^schist:

.s)' ! ','-:^., ff""-i : ", --fe,,-:: ^m:fe'Sv |fefe*K'4'ft^'vv,"rM*"'1 '*-/' 5' f

HHy&j'p:

•Pv irfl/'Apig*?;

|Ktp:*

fPtHP'' . . M, :.. 1 l.

N'S* i.M ^' r f. '' •"'sto:.v

686

691.5

697

705

750

764.5

770.5

"772.5

800

805

807

820

823

832

836

893 ;5

sTUf-iw.;;--i* -. ,-' - " 'KHsiLVtf r*'**' :* *, 's '.^070''"K8^-^-4? -" 'VfVO 'Ifet^l';,'; ,:, .-' ;

691,5 Quartz:-^^^^^^^^î^^W^^

schist inclusions. ;696

697 Quartz biotite e

705 ; White,Agmatite,

750 Quartz biotite 1Schistosity' " ' "' ". "'. ;,. V 'V ; '.r^''i', --'fV^v.r ." î:.^^'^;'^-''-^ - . •;.-'1

. . . /. ; . , - . . •...,.. .., . ,. •.•' i ': i ,'.'.-.V",''.^ ..aV^';"",;:-;,:;,':,.^':.:,.!,',/:'';^.^;.-.-,";.-:./ 1•764.5-' White^^pegir^ê/âme.'rock^^t^'v^T^f;^

; .7?0*'5 .'' Quartz biotitersohisti same '.rock^'fiS^j''^^1^'^^ ''-y''''^^ ';^)|6^/^; •77P'*ip'^;i^ :':;' : .""lK-:i^H ;''''::;. - ^

••'.•-' . j; omu.cn/yaj.i/j" " " '"' "^'--••-••;J - j ' •-•-"'- ''-- •--.-- -- ' -

772.5 White

SOO Quarta biotite schist, -' ' " ' ' '-: ' 1( . ; '"'•/idorji^ja;

. '... . ~- - ."^Schist!

805 White pegmatite,Csaifflei'-'^^'ij

807 Quartz Biotite

820 White pegmatite

823 Cor* incasing

8)2 Quartz

836 White p^gmatl-te' wLth

tâ^S&Lii^**V!Qi^^^îi^^^M^^^^' '" *-.'::i,'*#r-i''t'.-': .r^ :-'-,;.*v :;" tr^^':^;V;. '•^v^^M^^li.-'v^v^^. . ' , -,'| -,.'..--,'' .' . ,-..: . ' -' ' ' -' \ ' L " w ' " ' .;-: ;4 : : ' '. , i -,';:i ' '-, ' *. A' i- i', * -.\,-' ; ,' .X/1 -; •••,. ,^. . L .^^, ; ., .. |k .. ,. [lfj , '., ^ * , i: '-- ,^. ": -,;Z*s t - \'". .1 v- v *' -' - 1--' i 1 '^'--

*f^v V*, W V/VIM.O V: ; ! ', ,- ^ . " iK.T H1 ' * " "V...1O ." : ^ '. -* ', "'":, :'' ' •-- ; '^ 1 - "i*' Y.^^sV'i.^'V 1'-^"'''11 i ,-'-" "''.' j'1 ' r'...

: ^: ; ;'.';^^'-;'^-:'',l':'-:;i?:/^^^^^

'^^"T* ?,~'9 f ft *"^Y~ :*

'.'\i--\ '-V-*

890.5 Quartz biotlt^ Bohiei,^:.; v;: •••.,-. '^:;-': ^:;;:;v^ ::M*^l^fPI^893.5 White

979.5 Quartz

982.5 White 3egmatit*|---Aame; -TOÎ^,;' ."W&j* s'ri^-''-:f - ;--'.^"^-,v,-;-',:i1^.^ i. ': ;v-v'./•^Ks^'v^v'^V'^ji-^^S^-i^v'^^^^^V;-^0iî;:l^!;:;îi^rt^^ : ;;^

Hi^'

mjK,'XlW&^'-r'."

fiitei;-^

''

'

Hole A-902 continued

To

Page/- ;4

Feet

982.5

984.5

986

991

993

994

996

1002

1044

1052

1092

•1694

1100

1103.5

1108

1109.5

lib. 5

1137

984.5 Quartz Biotite

• ,, L ;;; ? lS;'"^'^''"V: '"•••- V-!" ;•f *.Vi : -W '/.i ,:vyv^;; -.'A;::;v rvf^;y^.. ;^V'

•-.'•ii,:' "v.'Vv'iiiifc'-^'-'.''.'i. 1 ?';' ' ''-j ' R;*-- ; V." : Is®11* '; : *; t- : *r- 4",r ;

986.0

991

993

994

996

1002

1044

1052

1092

1094

iioo1103.51108

1109.5

1113.5

1337

1815

White pegmatite* âme J*pck." . •'• ? i" J ./\.V ; ' ' -.'t ' -- "' ' , T 'r'.

Quartz biotite schist,^SiWDi

White Pegrtatite, same roclf:

Quartz biotite '"-:^^ 'va^v..-^ ^.^ pj.i' i.- * f" .*,. j ..i,..^,'^ j, ,

^

White pegmatite^ fSaifte ^

Quartz ;bioiite

•iV!f.-..'iii:e^ 5Same .TOOK;iiype -; - -':-; - ••.•-.^j, ;-; ; -v; ^., :-^!^WmiJy.^ *.:''.* . \ '' V-',.'- •• 1 '':. 1 - , •'.' ''- ^ ''i' 'u ! .-; *.'i',-; :;"y. 'i,V' J- '" ,V-:,, ''lv1'" V3 :*"-,' 1:.'''•'Sr^lrVv-Ji i' 1-"''^! 'ii ^'"i ,' "-.-' -J '^t-' '•,*^'--.-;-: bj' '^'i^'-, i.* : :-- i ± J*i-'-i.'if'*-;'-i-': ,:*'-*'- l - ---- '•••- "^-•r , •.'^v^-.^v':^'-'-Vv.. ll1 ^."V:-v.'-'' i; *-, -'•Bîsti''•'sanje'.-'rop^^'l^pe-'V':^.- •.•.'^r^'^'^ :^ v-sf''?* v l'-i.-^.r ;*

. : :^re.-^ssihg '••4: i ^M'^'l^^t^^^W^ '-^^.; •" ' ; - --' s -' i ' i ":- : '-'Vv ! -V : - ^-^'^îil^^M'Wi*^-^!''^'^ ' :'''' 1- ; '" ;;; -: "- : " v ' .; -.;,..;' : ..' : 'V 4chistodity: :^7p. *;i^6-'^''^x^^f '.0^ :J-^*

White pegnjatite.,: ;'s1 ame": :3roclcvt^peij,;:V.^

Quartz biotite,.' -' -•- V 1 .^^.^s^s^fi^jr'vld"' ' ' ' ' -.'-. * " •'-'-- " ' '. : - " ."..'". ' ' *'-~*

White pegmatite, s ame ro.ck

.Quartz. bio.tite, chist, *same,, ^j^f^,î^'^Q^ ;;; v; .^/3^.'.[•/^':c.',1-K'' ;'-^"

Quartz bio•" vvV'.^VivVViQpf*

White pegmatite^ same

Quartz biotite t6hi^t:-'(,',-''':^- !'

White -pegniatitp, same

Quartz•\'.. '''.'''rj,' '.-•: ,'-, i" ''.." ^' \' .'." H .'"','' '.' . "t 1- - . ''" L 'lr !^' ' '*J''^t .^~L . t^ i: ^ 'ÔjiS1-: 1 - ; ' N; ''. .'.'^''v. 1 ,.^ ^"''" ,:-^ ^''1^' ^'i 1 -' 1

otite '.'schist. '-'Sanie iô.clc^t^l?e'.. ii .'-1i'": - . *'; '' ''"'."'^ nt"*'ri "H ^.^'i.^-^... 1 - 1 . fi .! v^,' 1 -" 1 '

' t; :, ; ' ! ' : '" : .. '•• : '."'•'' ' ' !:" : ;'.''\-J7ff : ''V? J'i-1.75'*Qf'"''^-''^ ; -'-'-''': ' ; ''- ^ : - -'~'i 1 '^'^ ':- j ' v '' i'v.v;"' ..••'.•••'' -'." •••."""',' J li79'*'0 ^V."l|JS6^0^V^.K,^t0'^

•y-V;,t .,-''''"-V :''- ; ' ,:i'.. '^V.-^'ii'îi|,'"iOV4^?iji5fii.: iO,' :( ': ' ; ^^'i) ' :'-^;-^V^^'i;^î l - ; '^V--^

'^.'/.r -- ' '•••:.; ' . .f •/''•X'v/.v'i'jgf'iO-td 1230*0 '^•T*''V^-V;v. ?;i i'': t V : fV-'^: ' v ;'

"*'"' - v-"' 1299.0',to.

".0 ' White, '' ;" 1-" '-'- ''

fc:sX; : v-. From ' -Tol.Gi ^V 1 .' 1 j . n ' j^^ •^•^•^•^ ^ -W*BB^

fe Feeti?.iv:?-vrVftV-' 1 '

!?KCvs

-J:*KV:r:,fe^C/' ;(p*r,/ - . :P::::&M/- ;SWVr:.-.\ ',

W'-.-'iT?."'-. '

!^|P.iP^ N "i' ""~ " -

P:i'fr; ', f . -.'- ''tfejM^-'.V'- '- ' '-|f!';^,-,,r;p^'^clv^::-pCaJJ.:.r..i:;V:,'

rf it-/.:- ;*'^ff; ? * ::

Jl^'v

.^.3-A-":/-,' '

Rs5'i'iK'-'-.i'.v-i/--{e,!:;; ;:-

ffli&V^'^:-tMese,"-'-'--'-

1137 1815 , (continued)

1815 1826

1905

Page - 5

Description { '

'-•". \--. -.i '-- ::;'-1; .;/;;...' ^^^-^^l^^^^^^'^lv^^^,vSphlstoBltir;^Wi -'"4"^-^"—;: "^''^"•--'•:n: -^' r-

- - - -- :- H, "^ : ; :^!' ;S A'^W^^y&f^^1397.0 'td. '.lÔZ.O White- pe;jgni^tite', .'-'--.^ ^r;; : - r-vi:'' 1:.^"-^^^'-^:"'••/ ; ' ;1 ' ? ';

\ ' ^''''L'j^^Jore'.'inie'sing'^ ;14^b.0''^'1j^33V0'^'^^^Pîitvi^-^;.LU;

. . .1488.0 to '391.0.White

Schistosity ?O*75"''to

^W^Jpîi 4^^''-^^--'.^7 '-^'^".--. 1 ^:TQ--l^;Âilihi:,;:V: A :;5'n,v,.;: . ;?,;,, ; , ;';?;

Weak iron f|rm^t3Lbil; ;geneâlly finebiotite Fe^;?chi8t, with ûnd^b^^^.u^^woj ^BO/--.^:* ;minor arapuflLo'* ,':f0Si j: there de 'sOTJ6t',0ohi0rtiorij '* : Wi^H ••^^'^'•j-^•UM V\ftV\^4^r^'Alft . ' J* J J .Jfc*l—— i. J- 1 *- A --1- ~ lm ',1 "" , .,V'- ; .*'.- rV '-,-'/ .L -' '.. . ' ' ' ;J'-, V '* .' . - *. -,?*'. 1 .' '^^,l : ^" ' ' ' ''.'-" ' i: .Lfl6 DaudJin^mafic ratiJ

JE,-. -:- ifc ' r O* J "1^'^- ' •r.^-w-ww -^w** V T*^ *****^**^ .*t*y)OW W JO* ' S'"-' *' ' - - T'

*l*.falrly wtell d*Velo)i*4^4u*^'t6 the;!qii(ii'U':.vK:'; ; A,;fe'^ i:v:t:'îlM^î^MiSîilll^F^

- /' -' ''-i;.' 'y,'-' '-y'*'.'i--'':?'? 'K :C 'i:','^':'^'\Y'^---':''".'l ' " " ' -..".^ "Jtt. .':*v - ' ^ . r.;:.. . •,-:- .,,'-\' , . . ''•^^;î?''tx?:'^'^'^~'^-' i,- : ':*

"x ''. "". : 'b1 ^..-^''' .\VH "^ ; - s\/^ '. ' .' ' '*: ™" 'T '-~.''-- '-." ;' -

si'ftM 1^.

From: To Feet

1826 1905 {continued)

1905

1925

1938

1978

1993

2005

2009

2040

2047

2050

2071

2073

1925

1938

1978

1993

*Q05

2009

2040

'2047

2050

2071

20732075

ntfW^tf^îpP'^''A . i.*V i*'.* ' -' K*^ f M ' Ml . "' * i ' ' , -- .V ' - "' .

': ' \. ' ' ' : 'j !: ' -\' -l tit A.*Vi*Y H-^^'-'\^ J/Q''"^ 1 '''' "*V- "' '''V ' "" !'' 'i- '' rht '"' j ' "- 1 l '*' - ••" ! - " •' 1 ' ' f JL - * i v JJ TT y 5M.r' f L JLfflfit J, A'\r "' ,-'t' Vs.- "'' '""v^r' 'i f-'/ ' ' ' v l ' - : : "-

•,.;'.' ; ''r;^:;';'!:':'::^4*a;^^^; .-v-.. ^^••:•^;^•.1^0:^'t^^|^10 '^fc*^ '^l;: : ^;; -- i: 'U^M:3J^^^^^^^^^^'^:^f^^-,-: ! ','-".;:---T^s^^^^^-^H^^^^n^?;-';^

l"''' '.^.': : ' ';; " ' : --' ''-,', v* -^- •.'-'.••A VV:: : -'- v"..' ;i ^ : -', k" ', A ,:: i c', v ;:v. ! '

Quartz biotite schist' •••- .'"••'•.-^•••'Core

Quartzspotty quartz por; quartz l^St^J b contorted at I^l1 .

Strong iron J Fe30^ schistj matitej " contorted^

* : :*'fr .-••;' : V^•^'•^vv'')';';^,^v:- ;: ' v'.Y^-tf; ;,:;;y-i-;-- ; '' ^. ; '•; n#dJLt|ft ;^;^M'?^

ieY8lop|dl} îp^lîifoo^ w vri .-' ;.^;^^^5.;^^?^:f^.^'.'^v}.

?|^lîS;^:-.-^

Weak iron percentage' 1 1

. •.,- . .. v' Strong •irbn',.!5fo'mation as'' d0' .local 1"-2HôbricentrationsS

Strong iron; small tii

-. -, s^,ide.s^^^^*;v;,--. V; :': \:^- ^^^^-^.^•' '':-:.' -" ^^*K:-v^ :.v.s-;

Weak iron; fptifeation due to, lo cal 3 "-^'flfitreak? barrett

.high-'FeSg. j^nteltt-.':".'.^ " i:..'.:/,.-

Weak iron f(Mation 48

Very' wesk.'^pilcoarsely ci^lquartz bioti|e^chistj

jj;-;'l gv""- ; '"; ,v

^M^Y;;;;Ham^

1-3-.-,.*'','*"

From 22 Feet

2075 2079

2079 3100

2100 2125

2125

2167

Quarts biotite ehlorit-e 86hift|! 4uarta porphyry j -.feÔi,' gracing {JQ&t

- ', J - •-, , ,,** ! . ' J '-.-'i '!'~*'1i'. WAX.',*:

Quartz biotite well deyelî locally FeSg on

SqhistOsJL^y ! Qore aliasing a'20i•vi'r.."'. V . . -. -. .•"' '.' . •'•'•"l';l-:'..fr: ,

.^î^j-^SlW;W*^-^fo^-;^^^.^k^;; t!;- 1 : BfJ::^,^^^0t^^1^^:^'.-^^"*^^^;^^^2080.5 tp 2Q8.;0

î8'f;:^,'df:s;:i|^^|^^•i ivi'^.^lwî 'ftr*1 iB"**'aîî1i* p-*iriAfe:i.'* 1Xk'Vl.iiLiVc-;s'. *i.'!J.'.;'"v '\ l '.:'.,'t'- li.; '-' : ;'','??'*!'

coarser and Banding y^w^P^^^ffi-^.-^

iy-^5* ''"to: '^âfi(|;' :^ "; : : ^^^-M^^^^'if'1^^^^^559^31^:^^^^^.^;^

2^67 '..''"'- Quartz bio^t^^îif fc:-'^ ;4?:8*^b^;;^ : .''. . : slightly • ;^Jirger4 X bandli^:'iM66i)aSiûliAîp|iir^6i;.'"banding ''"iôn^^ i 1"v'Cor^'. mining'^^^'fy^'-^^fo'-:^* ;' :vBv^^^^'v,:; '-' '-'-i'":]

'l^.-^^ •.-•'^l^^^'',\:^

. L-•"•••i i' " - - j- — V i i : . . aw- * i ' ^ '.' . . fl J i? rf'St? V i-. '.. ^ ' , ^.-7**, r ^.^t" */A'' ' * ,.' 4.. \- ." ,

ENDiOF Acid test

Drilling'' '" by: Heath A Sherwood Kirkland '-'':f-"-,":^^^^^'j:^, •••\':\ V'^^j^^vr^vV:;- v;f::?.f!!.i;:

..••',-\*.: ,Vi'.'^.' "'I'';"; . f:. ,' , Stf ' !r.kr.:;;,:' : •.•../'.•. ',..}.\..*\-?S?' " ' '• 1 '''''' ' " '""'

* - .•.- - i. ... ..f '"'.Lî^w^,^;..-',*^^?..

i";;f .

:' -,..

75V?

Locations Claim 7548

Inclination! -90*

Corel EXT

THE ANACONDA COMPANY (CANADA)

LOG OF DIAMOND DRILL HOIE HQ.A*9(S

tt

From To Feet

Description

O

56

114

233.5235240.5

294305

318320

56114

136.5

136.5138

179182

183

138179

182

183

233.5

235

240.5294

305318

320

338

Casing

Granite pegmatite} coarse grained) salmon pink} feldspar, quartz, muscovite} minor biotite altered to chlorite,

Core nissing - 106.0 to 107.0 ....Quartz mica schist j medium grained, black to dark grey; uniform texture; banding inconspicuous} monderately strong schistosity} minor FeSg filming on fractures.

Core missing -116.0 td 121.0122.5 to

Schistosity 30*40* to core axis

Pegmatite as desoriped above.

Quartz mica schist, as described above.Schistosity 70-60* to core axis

Core missing

Pegmatite as above

Schist as aboveSchistosity at 189 ft - 90* Core missing - 196.0 to 197 f 5 Schistosity at 199 t* - 40* Core missing - 202.5 to 204.0 Schistosity at 206 ft -60* Core missing -* 213.0 to 214,0

Schist as above - 80# quartz

Pegmatite as above

Schist as above .Schistosity 65-80* to core axis

Pegmatite as above - included schist

Schist as above

Pegmatite as above

Sohist as above

22 Feet

338 486

436 550

Page -2

Description

Pegmatite, aa described aboveCore missing - 375.5 to 377iO

382.0 to 384.03*9*0 t*m*0 394*0 to 395.0 397*0 t? 398.0 399*0 to 400.0-409*0 to 3X0.0 412.0 to 414*0 419*5 to 422.0 4^63 to 423.0;^4.0 to 436.0 4^0.0 to 442*0 453,0 to 454.0 475*5 to 476,0 431.5 to 483*0 484.5 to 485,0

Schist as described aboveSchistosity 60-80*. to core Cpre ndBsing - 494*0 to 495*0

501.5 to 503 PegmatiteCore missing - 507.0 to 500,0

522*0 to 523*0 524,0 to 525*0 529.0 to 530.0 534,5 to 5?6.0539,0 to 541.0543.5 tc 546

Schistosity 85* to core axis

550 END OF HOIfi

byi Heath and Sherwood Drilling Ltd. Kirkland Lake, Ontario

kx-ms

DIAMOND DRILLHOLE *J*.L.i

fcEAMWe ' S -6* SI'Bt'-.W

tIP i T6 *

ISEPTH i 3SS* '

LOCATION i PERCY LAKE

ANACONSA IRON OfU (t)NT,J

LOCAT.tOKI MAP

J.D, H *" f L, l

JATE - MAY*t"-*l SCALE' l""400'

ANACONDA IRON ORE (ONTARIO) LIMITED

LOG OP DIAMOND DRILL HOLE PL-1

Location: KK 22050 Bearing: SouthDip: 70

Feet

From

0.0

24.0

Tp

24.0

2943.0

2943.0 2993.0

2993.0 3003.0

3003.0 3044.5

3044.5 3049.5

3049.5 3086.0

3086.0 3336.0

Cor* Size: AXTLogged by: P. W. WestDate: October 24, 1961

DESCRIPTION

/-s- ' S.

Overburden.

Non magnetic quartz biotite schist of the quartz rich and mica rich varieties. Sequence shows some folding and is intruded by innumerable white, feldspar pegmatites. Average schistosity at 70 degrees to core axis.Fracture patterns are of two general types: one at a very shallow angle to core axis, the other at 30 degrees to core axis. Fracture planes are commonly coated with calcite and pyrite. Slippage along planes of schistosity is also evident.Light green alteration zones in schist usually associated with the fracture system approximating the core axis. Alteration products are sericite, kaolin and minor chlorite.

Strongly magnetic, thinly banded iron formation with first five feet showing marked amounts of green actinolite with atten dant pyrite. Zone is highly folded.

Weakly to mediumly magnetic, thickly banded iron formation with alternating schist bands.

Mediumly magnetic, banded, folded iron formation with alternating weakly magnetic schist zones.

Non magnetic, quartz biotite schist.

Strongly magnetic, thinly banded, folded iron formation with some specular hematite.

Non magnetic quartz biotite schist with white pegmatite intrusions throughout.

End of Hole

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LOG OF DIAMOND DRILL HOLE NO. J-3

Location: KK 14268 Core Size: AXTBearing: South Logged by: P. W, WestDip: 550 Date: October 23,1961

DESCRIPTION

Feet

From: To;

0.0 67.0 Casing.

67.0 76.0 Non magnetic quartz biotite schist,

76.0 78.0 White, feldspar rich, pegmatite.

78.0 108.0 Strongly magnetic, folded, actinolitic iron formationwith schistosity at 85 degrees to core axis.

108.0 222.5 Non magnetic, quartz biotite schist with minor pegmatiteintrusion.

222.5 263.0 Folded, strongly magnetic, iron formation with minorpegmatite veinlets,

263.0 457.O Non magnetic, quartz biotite schist.

At 267'-269' — Calcite cemented fault breccia.

Schistosity at 80O to core axis.

End of Hole


LOG OF DIAMOND DRILL HOLE NO. J-4

Location: KK 14268Bearing: SouthDip: 510

Core Size: AXTLogged by: P. W. WestDate: October 23, 1961

DESCRIPTION

Feet

From: To;

0.0 83.0

53.0 131.5

131.5

171.0

171.0

257.5

257.5 264.5

264.5 271.0

271.0 451.0

Casing.

Non magnetic quartz biotite schist with the last 7.0 f a mixture of white pegmatite and actinolite schist.

Folded, strongly magnetic, banded iron formation with last five feet weakly magnetic. Banding at 80 to core axis.

Non magnetic, quartz biotite schist with white pegmatite veinlets between 204* and 2191 . Folding is quite appar ent.

Strongly magnetic, iron formation.

Non magnetic, actinolitic quartz biotite schist with garnet.

Non magnetic, quartz biotite schist with minor white pegmatite veinlets.

Schi st sequence is traversed by innumerable hairlike fractures with attendant epidotization at 15 to core axis.

At 432*,a calcite cemented fault breccia 0.5' in width.

I

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DEPTH 88 l '. 5

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ME i MARCH 24,1961 i-C. A LL-. l '-


LOG OF DIAMOND DRILL HOLE NO. NPL-1

Location: KK 14096 Cor* Size: AXTBearing: South Logged by: P. W, WestDip: 450 Date: October 23, 1961

DESCRIPTION

Feet From To^^

0.0 32.0 Overburden.

32.0 68.9 Non magnetic, quartz, biotite, schist, locally chloritizedwith intrusions of white pegmatite. Average schistosity at 50 degrees to core axis.

68.9 117.5 White pegmatite with abundant garnet and black tourmalineand red garnet and containing inclusions of non magnetic schist. Lower contact at 65 degrees across schistosity.

117*5 143*0 Non magnetic quartz, biotite schist,

143*0 196.5 Non magnetic schist with numerous, weakly magnetic ironformation bands.

196.5 275.5 Non magnetic, quartz biotite schist with minor blebs andand veinlets of white pegmatite. Several quartzite bands are prominent; heavy actinolite zones noted between 238* and 240'.

275.5 307.5 Thinly banded, non magnetic quartz biotite schist withmediumly magnetic iron formation zones.

307.5 322.6 Thinly banded, tightly folded, strongly magnetic ironformation with actinolite and minor pyrite. Portions are schistose.

322.6 471.4 Non magnetic quartz biotite schist with intrusions ofwhite pegmatite.

471*4 552.7 White, feldspar rich pegmatite with minor amounts of in cluded schist between 472 1 and 475'. Pegmatite contains minor amounts of red garnet and black tourmaline generally near contacts with schist.

552.7 859.0 Non magnetic, quartz biotite schist with pegmatite in trusions throughout, most prominent of which are at:

614.5 ! - 626.8' 639.8' - 678.4 1

859.0 879.5 White pegmatite with minor amounts of red garnet.

879.5 881.5 Non magnetic quartz, biotite schist.

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Location: Bearing: Dip:

FeetFrom

0.0

51.0

95.0

105.0

122.0

146.0

158.0

173.5

190.0

260.0

280.0

335.0

370.0

LOG

KK 7867 .Southwest 45 Degrees

To

51.0

95.0

105.0

122.0

146.0

158.0

173.5

190.0

260.0

280.0

335.0

370.0

468.6

OF DIAMOND DRILL HOLE NO. NPL-2

Core Size: AXT Logged by: P, W. West Date: Oct. 23, 1961

DESCRIPTION

Casing .

Non magnetic to weakly magnetic, quartz, biotite schist — both quartz rich and mica rich varieties.

Olive green to dark grey, aphanitic, igneous rock, - Diabase,

Weak iron formation, thickly banded with white, "quartzite11 appearing band at 114' to 116' .

Medium banded, mediumly magnetic, iron formation.

Non magnetic quartz, biotite schist with weakly magnetic garnet schist zones.

Diabase.

Non magnetic quartz, biotite schist. Average schistosity at 80 degrees to core axis.

Weakly magnetic, quartz, biotite schist - thickly banded.

Barren schist.

Weakly magnetic quartz biotite schist with mediumly magnetic Iron Formation bands throughout.

At 325' to 330 1 the schistosity changes rapidly from 80 degrees to about 20 degrees to core axis*

Non magnetic, quartz, biotite schist.

Mediumly magnetic, banded iron formation with actinolite,pyrite and minor pyrrhotite.

End of Hole

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•l LOG OF DIAMOND DRILL HOLE NO. NPL-3

Location: ;1 JflC 7877 Core Size: AXTBearing: Southwest Logged by: P. W. WestDip: 500 Date: October 23, 1961

DESCRIPTION FEET

From To

0.0 34.5 Overburden

34.5 H4.5 Gray, banded, non magnetic quartz, biotite schist with weaklyto mediumly magnetic, iron formation zones between 78' and 93'* Average schistosity at 45 degrees to core axis. Schist and iron formation show minor folding.

114.5 124.5 Weakly magnetic, quartz biotite schist alternating with mediumlymagnetic iron formation bands.

124.5 205.7 Non magnetic quartz biotite schist with mediumly magnetic ironformation zones between 142.5' and 163.O 1 . Pyrite and actinolite commonly associated with iron formation. Local concentrations of garnet occur throughout.

205.7 233*5 Medium to strongly magnetic, strongly folded, banded, ironformation with weakly magnetic schist zones between 205' and 221'.

233.5 258.7 Non magnetic quartz, biotite schist with green porphyritic,equigranular rock of feldspar, actinolite, quartz and bronze- like mica at 236.0' to 237.5'.

258.7 301.0 Weakly to mediumly magnetic broken and folded iron formationwith fine grained granite at 266.7' and 278.1'.

301.0 679.0 Dark green, holo crystalline, igneous rock composed dominentlyof actinolite with minor feldspar and biotite mica. Appears to have a finer grained border phase. Possibly an amphibolite porphyry. 388.8 1 to 395.0* - included zone of strongly magnetic, folded iron formation.

679.0 680.2 Non magnetic quartz biotite schist.

680.2 699.5 Diabase.

699.5 706.0 Breccia composed of schist and amphibolite.

706.0 709.0 Non magnetic, gray, dense, quartz rich schist.

(continued)

Anaconda Iron Ore (Ontario) Limited Page 2 Loe of Diamond Drill Hole No. NPL-3

Description Feet

From To

709.0 785.0 Highly folded, broken, contorted, medium to strongly magneticiron formation with schist zones. Iron formation is thinly banded and contains Hocal concentrations of garnet. Average schistosity at 60 degrees to core axis.

785.0 789.0 Russet coloured garnet schist. Non magnetic.

789.0 831.0 Amphibolite porphyry with inclusions of non magnetic quartzbiotite schist.

831.0 849.2 Non magnetic quartz biotite schist intruded by white,feldsparrich pegmatite between 837.8' and 840.O 1 .

849*2 894.6 Amphibolite porphyry with angular blocks and fragments ofschist and banded iron formation.

End of Hole

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Location of Diamond Drill Holes

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DD RPT 10 PERCY L - Ontario · It)8.o-l8fc.0t Klea*aahiati wbltleh-gray, danea. 17is. 8-174. 4i cor* Mating lOii. 0-18^.5 1 megnatlta and gurnet In hornblende aohiat* * 18C.9-185.6t

Documents

DD RPT 10 PERCY L - Ontario · It)8.o-l8fc.0t Kleaaahiati wbltleh-gray, danea. 17is. 8-174. 4i cor Mating lOii. 0-18^.5 1 megnatlta and gurnet In hornblende aohiat* * 18C.9-185.6t