- -.... , —,. ...i miummtl 52M01SWei90 1 7 BALL TWP

010

Diamond Drilling

Township BALL Report N9: 1 7

Work performed by: FALCONBRIDGE NICKEL

Claim N9

KRL. 48277

KRL. 48264

KRL. 48265

KRL. 48268

Hole NQ

F4 F6

TB-1 TB-2

TB-3

64-5 64-6

Footage Date

Mar/ 6 2 Mar/62

Mar/ 6 4 Mar/64

Mar/ 6 4

Sept/64 Sept/64

Note

Notes:

AWL.004(7-69)rev.9-72

FALCONBRIDGE NICKEL MINES LIMITED

REPORT OF ASSESSMENT WORK

Ball Township

The Red Lake Mining Division

The Kenora District, Patricia Portion^ Ontario

Date; July 5, 1962

REPORT OF ASSESSMENT WORK

Ball Township

The Red Lake Mining Division

The Kenora District. Patricia Portion, Ontario

Introduction

This report describes the results of a diamond drilling program submitted herewith as assessment work against 18 claims located in Ball Township, Red Lake Mining Division, Ontario. The claims numbered KRL 48264 to 48278 inclusive and 49874 to 49876 inclusive are located as shown on the attached plan.

The drill hole was positioned on claim KRL 48277 to investigate the results of a ground magnetometer survey performed during the winter of 1962.

Reports of work which accompany this report detail the status, location and registered ownership of the above claims.

Diamond Drill Results

Diamond drill hole number F-6 was located to intersect a magnetic anomaly detected by a ground magnetometer survey. The hole was drilled to a final depth of 450 feet of which the initial 280 feet is herewith submitted for assessment credit.

The hole intersected magnetite iron formation interbanded with tuffs, amphibolites and garnetiferous quartz chlorite schists from 70.3 foot to 229.9 feet* The iron formation is described as a thinly bedded chlorite amphibole type with 20 to 60# magnetite* Minor pyrite occurs along the bedding claims. The tuff is described as a very fine grained banded rook with considerable chloritic alteration and with occasional finely dissem inated sulphides. The amphibolite varies from a fine to medium grain type with occasional sparcely scattered sulphides.

The accompanying drill plan, section of log and assay sheets indicate the location and orientation of the drill hole and the relative position of the various rock units.

Conclusion

The diamond drill hole has satisfactorily explained the reason for the magnetic anomaly in this area.

Respectfully submitted,

FALCONBRIDGE NICKEL MINES LIMITED

DSK.lh

LOCATION

LOGGED

STARTED,,

FINISHED*.

CASING .,,.

CORE

FROM

** HOLfc NO.",J

....OIP,^ JSL.. PROPERTY, (CORRECTED)

BAY

TO

o2.0'

61.0

63.2

67,5

129.0

169. t

2.0

61,0

62.3

67.5

169.4

187.3

229.4

240*0

252.5

Cfifring '"' ," ; '. : ;' i ''' ;: . ..- ' .; ; -

AndecHt* Kediuv graln*d, light griiy-greftn In

Wfft. fin* crained, Bidding ftt SO*5" to

tuff (??) Cofcwe gr*ine*d uryslttl tuff,

Pin* to medium gridnM iA08iv e Amphibolite. 67.5 - 96.0 IrrftgtJii&r carbon a|*, quirt* undl quart t,: ''"'

. . 95*0 * 97.5 Spfcr**iy iJifts*?ftin*tta pyrite an* pyrrhotite. 100,0 * 129*0 HABsive wtdiutt frainea

' toSohitftfd, ilnift to w*diu* grftinsid. Sptdiiting At

't139.0 -141.0 mgn*tit6130.0 -145*0 ' r mostly

'3155.0 *eeaiirfrttd pyHt* * 30^

Iron Fom&ti 4n s AmpliiK'3.**ehlori te banded iron CcrnwW oin J(j :30^ tifei{^e'tite* Verywith layix highly oilioeou* band*. Doainsint air*ctipn of* '

is.it

Anphiboiittt to ' amphibolite vith itparosly''

Pornf.ti|^i A*j)hibolo^chloirit e b&nded iron f orationi * J - ill l . lil . . J ^ ^It* ' ——,.^--\.JJ~'- '' u. J. '^ l, ^ "^v. ^.^XLkllj i- ' \t ̂ iL*.-**. ' '±rn"t t* *i''

Of Cj

(V?) fclttrirt W

;*ut 35 sulphide*^ mostly pyritft. Very Uopyrite end pyrrhotite.

y fin* gr*tnedhr-:-.:"-- 1 ,, : '

LOCATION ̂

LOGGED BY.

STARTED ^

FINISHED.

CASINO ,^.-.

CORE SIZE..

moM

252,5

264.0

275.0

301.8

307.1

310,0

340.0

345.0

360.0

417,0

*a.o

TO

264,0

275.0

301.8

307.1

310,0

340.0

345.0

360.0

417.0

421,0

499,0

l^iCON&jJIDGE NICKfc'L MINES UMJTEDf AMQND DRIUJ^QQ

. .., ... . _ ____ BEARING.. __ ,. HOLE NO.^Jl*^. ,

.^ELEVATION.. _______ rDIP .PROPERTY^. .T" uTf. .

. ., . TESTS (CORRECTED)

i n , (y j . ' : - " . . , . ' ' ' '

' ' - !' 1 ' ' " ' : ' ' ' ' : ' '- ' " 'Iron Forwitloni AHjphlbolo*chloritt iron fonaa tl on * 50J6

256lo * 257.2 tedding tt 300, 400 and p&rftXlel with core, Mteeiiinated pyrite thixw^hout iron formation MA oonoentyaud tlong the contacted bedding plane,

Amphlbc-litot Fin* ftr*ined and chloritic, 2.69,6 2" DAgnetlte * 5055 magnetite 2M.2 2" wAgnetite * 50JK magnetite 26ii,0 - 267.0 Approx, 3^ pyrrhotite, (Saroplfe 609) 269,3 t 270.0 DieBcmlnftted pyrrhotite,

^artt-chlorite-g&rnet cneleti Red g&mets averaging | w In diwfteter tfi ebundent from 275' to 295' (Spec 13 at 263')

Vusrtn Milte aintrtlieed milky quart*.

QuriYia-ohioritt-garttot g/ieUe*' ' f.;"- ' " ' ' . : . . . :. ; -. ' , . . . ' .

ChloritlCjIad.^ttntfj Finely bodied chloritic 8edimentBv.lt h Irr^guHr.pu'^rt* velnSriS. Bedding at 70* to core, (*^poc 14 '1*. 3241 ) ' : ' ' - ' ' . ' . . . ',; : : V . ; ' . ' '. : v; ,/ '

AreillH^ Bliftk ftrgllUceouti tedlwents.

Chloilti* ^5i*ant*t As in eeotlon 305.0' to 34C",0 but vith le*i qairtt, Soaio pyrrhotite on bedding planes,

^ * : il\ ' ' ' : ' " " ' ' ; ; 'y ' o' ' -to wi1*, "l^fSte 4'id pyrrhotite occur In ceriedn seeUom bvt J4i nwfwts If 1*1 than 2^ by volume, Oreatest'-cdiricerttjr'at^'. ; ion? of f^lttldet are in sectioni-t- 364' - 366'

'li'.. . ' -- . -' .'"370' ^ 372''.. -i; ;'".:;;' ; . [:'.'^\::- (SpeolMt^l') , : . . . . ,. .' .'-.- ;. ..375' ;-.3?8' : ', ,: ^ •^•••^•^••^Ohloi'Jtic if ptrticj ( 't *Hered tuff ) Irregular ^juarUv^iis

plimee, ; *A PkV6 ;i : :499 :Urge;;cryi.tal*"; ̂ ^if^^i^^^g- '. '.:v,

^^l * i

*

*

MCQ{iEy*ij^BIAMOH5LPBMJ.QG

LOCATION Ij998 S 10,300 W BEARING W HOLE NO. F. 6

LOGGED BY.

STARTED..

FINISHED.,...

CASING ^...,...

CORE SIZE..

FROM

0

7.0

64.2

70.3

73.0

94.5

97.5

126.0

146.0

152,0

157.0

224.0

229.9

237.5

W. B.G.Walker ..ELEVATION^ : ' .. . DIP A50 .PROPERTY Trout Bajr

March.,l6j 1Q62 !. , m.\ ... . -' '... TESTS (CORRECTED) '

March.!0,, 19&2. ,.... ^ : ..

I-Cfiei..^^ .^-., __ ...- __ .j ___ . At 300 feet - 430 ' ' ,

M ' ' - ' ' '' - ' ' ' ' ' ' ' ' ; ' ' ' -

TO

7.0

64.2

70.3

73.0

94.5

97.5

126.0

346.0

152.0

157.0

224.0

229.9

237.5

250.0

- ' 'i i' ' , .DESCRIPTION

Casing

Amphibolite; Massive very fine grained

Tuff; Finely bedded at 800 and 900 to core. . ' : . ' " '

Iron Formation; Thinly bedded chlorite-amphibole type of iron formation. (* - 20^ Magnetite) *- 0.5^ pyrite on bedding planes. Bedding at 80O to core.

Amphibolite; Medium-find grained amphibolite. Very sparsely disseminated sulphides, 90,4-90.6 Calcite.

Iron Formation; Bedding at 70 to core (*- 10# Magnetite), Chlorite smphibole type of iron formation.

Tuff; Very fine grained banded rock, with considerable chloritic alteration. Probably tuff. Finely disseminated sulphides, (Spec 18 at 103 feet)

Amphibolite; Fine to medium grained massive amphibolite.

Iron Formation; Siliceous banded iron formation. Bedding at 800 to core. (*~ 60# Magnetite),

Iron Formation; Amphibole chlorite type of iron formation ( *~5i# magnetite) Magnetite bands widely spaced.

Amphibolite; Medium to fine grained. Probably andesite or tuff in places. 193.8 - 194,1 Magnetite *- 505S and quartz.

Iron Formation; Amphibole-chlor^te type of iron formation (t- 20# magnetite) Bedding at 80 to core. Contact at 229.9 at 700 to core, i (Spec 19 at 229.9)

Quartz-chlorite schist; Scliisting developed at 700 to core, ", Garnet developed a^. 231,01. Traces of sulphides.

Tuff: Fitfe grained tuffaceous rocks.

LOCATION..

LOGGED BY.

STARTED......

FINISHED..,,

CASING ....™

CORE SIZE.,

FROM

MLQOI^MI^LMCM. MtiisjJMJjgWAMgND.DRJLLLOG

_,.. ̂ ,._., . ....BEARING..,,.M.. ..^.HOLE NO. ̂

... ELEVATION.__... ^.._..^DIP_.__...PROPERTY_.

-.... ............_.-^..._.......- TESTS (CORRECTED). . ;

250.0

278.8

290.0

295,2

334.7

361.2

391.7

437.5

442.0

TO

278.8

290.0

295.2

334.7

361,2

391;?

437.5

442,0

450.0

450.0

DESCRIPTION

Tuff; Coarse crystal tuff (??) possibly porphry intrusive. (Spec 21 at 278')

Argillite; Fine grained sediments with black argillaceous bands. Bedding at 80O to core.

Armphibolite

Argillite; Disseminated pyrite streaks in shaley sections. 307,3 - 309,8 Crystal tuff St porphyry intrusive. See spec.21. , . ' ' . . ' . ; . : . .'

Amphibolite: Medium to fine grained. Occasional quartz stringers.

Argillite; Approjc. 4~# pyrite in fracture planes and bedding planes, ' -

Amphibolite: Massive fine grained amphibolite with irregular quartz veins at 90O to core.

Tuff; , Fine .grained banded chloritic rock. Probably 'altered tuff. Banding at 900 to core. Occasional quartz stringers.

Amphibolite: Massive and medium grained. Banded appearance in core. Minor trace pyrrhotite. (Spec 22 446.2')

Bind of Hole

f .1 - ,JA PROPERTY: TROUT BAT

1 SAMPUE FVO. FRO"W | TO UENGTH;

Mi-

616 228.3 229.2 0.9 .03

i 617 231.2 232.8 1.6 Tr.i" ' ' ' ' - -t- —' " - :-[^ 618 237.2 237.6 0.4 Tr.

L 619 ^324.0! 324.8 0.8 r Tr.

j 620 375.9 l 376.4 0.5\ .

Tr.' - .. :̂ . ..j :: - . : L -

621 110.3 111.3 -1.0 Tr.

———— : ——————————— ———— ———•-•--. '-i - •-•--

- . - - I.... -" - ' - --i.- . j . . -. - - i, - -•"••" - \ i ' A :

. - .- -

- . "- ' -

- - ~ -'- ;* ': '

. . . ' ' .

.

1 "-v r - j ' " .-' -

- " ' ..-.-- - : '\ ;..-v: t-'- '"-- Y"- — - ———— ."."i-:.--:"-..: . - . ;, - - -f ". ; ""•••.

- : - - " ' " " - ' ' . "— — ; — — —— ——— - ——— i —— ; —— : ——

"i 1 - " - - -' -" ' - - - -. .--' l - . - ' l. .. - - . ,- - -i' -:-

V ;, V ;: ' .b: :'-. - ' v.-'.

i . ! - - " -"'

FALCONBRIDGE NICKEL MINES U/VUTED ' ,' - x—————————————————— - ————— : ————————————————————— ' HOUEMO.F.O

SAMP^ RECORD 0 ^SE i

ASSAYS

l f l 1

•CM. 1 i

w

-

i.- i i - - .- - ^.05 i j Fine disseminated pyrrhotite. ^t-

.02

.06 T

'- - ' . '-- - . . v Disseminated pyrite

Disseminated pyrite K. - - i - . - - , i i - - -- l -iv j i ' - -- ' - - - - - :-

.02 ,| . J j Pyrite in shale. :

.02 i i 4: r 'L .04 j j

r

" *

- " :;,,-j- . \ . . /"-"•-.-I.- '

. . - -

,

•- .^^::---:

: ' '- :

- - ;

t. - .-. -- - -i . . - ' - ' -..~ ~ ——— 1—— ——\- V -: j , -- -— r— ~'- : ^

". ; ••••:-

" - . :. -

- . - .. ' --.-

-, -

- - - -- : ; : -

--:------.

-. - - -"-' .

V

. : -r-'j ;

; ....

•::;--;if^;rv^; : ,-., - wzM/ll - - : v .v ; -. . - ; ,j . v , . : ; . | , :; -..J.;.,;-, : -v

-..... ^.... ,. L... . - ....-',.,j~.'.r -

- V..-:

•- :v" .C:':-

";-.

; -.'

- ---,- ..^'- -, -: : : :j

V

'- . :

Pyrite in shale.- .... - -- -- -- -- - .- - ^---.---- --- - - --

Pyrite. . . -

- - . - -.' - - - - - - --. ; v

. - - . . - - - - - .- . -- ~ - - " -- . ~

- - ' * . --:- ' ' " ' ~ ..- .. ' - V -" " - " " - '- -- .- - "' . - ' " v -

-•-, - . ' ' -. -". . " . - -..- " - - - . ~. . - - ; . - . - : - - - ', --'

; - ". ' , . .': . . . ,-:- - ' "" -'-,- " : - " --.- , - -- ' ' ' -" ' ': " " :""" .

•-. . -. " . ~ ~ ' -. - . ~ ' - - ' - ~ - -- - ' ' ^ ' ' ' - - ' " "

: " . " .

- ' - " ' . v '. - : ' - -. - - - . !,- ' :* "^ ' '- ' :. v ' ' --

r: ;: rV";v-,-.;. : ; '-'V '- V-^ : ; ; , '- ' -'--—

DIAMOND DRILL RECORDPROPERTY.^______Tiiaut—Bay... Copper_____________ HOLE NO,_TB //l._ ^

NUMBER ..............j)ML....—.-.-. — .- SECTION FROM_______JTO_______ STARTED__J!flrfih-jLQaL..JL9M-

LATITUDE .. .......,...............-. ....,.........,. DATUM_flJmia, KHL—4826fr._______ COMPLETED-Jtarch—J^iiu-l^,

DEPARTURE......... .^ ̂ ..,....._ ., ^ ^ .. . BEARING___gouth 7 S degr.ft.ps Das t ULTIMATE DEPTH___121j.Pl.™.

ELEVATION . .. . .. ...,_,. ..^...^......--.....-.... DIP_______minus ./tO degrees_____ PROPOSED DEPTH,.

DEPTH retT FORMATION .AM^LI NO. O^'AMPLE COLD t

O.O^J^.OJ . . , -mjDfising,_(.JiatorJ-——-—————-—————----.————-—- .J?* P *. .8*1 _ ..GaeisBJ o appearenoeji pose j bly sheared eedlMent. (Mi oaei 'UB)

8 •l^.±'..-8ji3.....^^ _Lave, aridoeitio, ^chlprj^ti zed, some amygdules?,^^.^ ** -?*6^ gneifisic, SB above, few pink goraete.^^^^^^^^^

^946.^.0^10.^.,^. .^.,J'Syft.i,.M.,a^Qyo*_________________________ ^-0,0 -15.0 Q-nelzzio as above, with few narrow bands Lava ?

jiL.t—15t2L.-.— Narrow.^uarte^i)rii\gers, gparse pyr.ite and oheloopyri 15.2-^18.0^ _Gneissic es above. ^^^.^^^^^..^^..^^^^^^^^^^ 19,0 ^23*0 k8V ®* ond es i to, oh l ori t j zed.——-—-—-———-—————-—

8

J3^CLj-. J5.'.0..r-A9j2.

few narrow bands of lave Lava, andeslti o, ohlorftj zed.

28^2,

.75.^.^-8.6,0.

l^'eldspar porphyry d j ke, narrow bajr'j-3.u quartz veinletat contecte,Andesitic Java, ohloritlzed,GaeiBsic, as fibove, ^3 to 59 section. Silicified contact.———-—-——————

3*3.5 ^.3!i?JL 9/J.5 - 96.8

Feldspar orphyry, Dike.

^S*2.

Andesi te, l ava, si li cfied, alterftd, 10^ quartz o^b-

Qijated, whJth chlorite, porphyrytized,.^.^...^.^^^^ .Feldspsr porphyry dike.____________________

•r^Ti

98,2 *- 321. Biliclf j.ed t ^porphyrytl^6(3 ( Qtz Stgrs ffi 107^^,10^N.M.P., TORONTO-STOCK FORM NO. SOI REV. 12/51 111.8, in.5

SIGNED

DIAMOND DRILL RECORD lPROPERTY_,-.J^out—J!Sy--—OafifiS3:_______________ HOLE NO.. I*B .2 .

NUMBER -.......Jpno......,.................. -— SECTION FROM________TO_______ STARTED.....

LATITUDE ,, .. . . ......,.............. . . .^ . DATUM clairo, KRt 4B26/J ___ COMPLETED

DEPARTURE. ........^.....^ ...........,... BEARING South 20 West________ ULTIMATE DEPTH

ELEVATION. ... .. . .. .... ^.... .... .. . DIP______Mnua 40 degrees,. PROPOSED DEPTH.

DEPTH rctf F ORMATION SAMPLf No. O^'AMPLI

t. ,... J we terj..._—. m-—-——————-——————---—-————

20.0 -43.0 Leva, gneiss!.o 1 1. few neiypawbonds of a morci massivooarbonnto altereation, ^ 27*2 to 28*5

Vein3,et Q36*2* fey; gernetsthroughput,jthis seotion QQuld be altered sediinar)t.)

J,evs^ andesltioj ohloriti^ed, few nuryow bands, of jgiiQlssic

O-oi:

OOLD t

f- F; 15 3 1965Kt

N.M.P., TORONTO-STOCK FORM NO. 601 REV. 1Z/SI

SIGNED

DIAMOND DRILL RECORDPROPERTY,

NUMBER LATITUDE ..... .......DEPARTURE .. . .. .. .ELEVATION.........

Trout Kay uoppar,^^^.^.

——- SECTION FROM ——-—.

DATUM cleira KRI-

HOLE.TO.

BEARING

DIP

South 10

STARTED ...^J^ COMPLETEDULTIMATE DEPTH

PROPOSED DEPTH

-l.10A*0-

DEPTH FEET

0.0 - 8,0*

8.0 - 13.013,0 ~ 22,022,0 ~ J9.0

39.0 -55*0

5^.0 ~ 56^,j6.Lr.^2.o..

8/1.5 - 10/4,0

^̂

FORMATION

C os in ['i, { water-)Gnois&ic appeoranco, poesibly sheared sediment.Lava , andesJtfifj chloritic, (bad cave at 15 feet,)GneiBsic, or. ebove, fov; ern&ll pinMeh garnets, j^oseiblvpediment, (Drilled cosing to 25 ft, to Btop cave.)Leva f ondoeitiOj f:omo quartz oerbonete alteration^ whitquartz stringer e 53. ̂ to 5St5j barren of mineral.feldspar porphyry dike.Leva, andesi ti c , chl ori tS c .Feld&por jxjrjjljyry dike.J-eva, silicified, altered, 10-15^ guartz carbonate, f©v,hite quartz stringers, barron,

Hole stopped or account of cave.

• AMPLt NO.

J

If

WIDTHor SAMPLC

/^(C\\^

GOLD t

(ftyf'Mittfl

IFif. ^^

^f,^^S^i

ftSW

•*'"**1**.^G' ^SN*yx- \

!9ft) l^ Jf^^^

N.M.P.. TORONTO-STOCK FORM NO. 801 REV. 18/51

DRILLED BIT ..........j*...Currle.. SIGNED

DIAMOND DRILL RECORDPROPERTY____Trout Bay Copper

•:ET NUMBER . ^,.. ...On* .^ ̂ ,. ^ ,,., -.m-

LATITUDE . r\;R,)r——*1 B- ^1 j6i.. S-... - -

DEPARTURE^ . -...,.............. ^............... BEARING__

ELEVATION . ,. ............^..........,,....... ^ ...^^ . - DIP.^ Minus

HOU NO.

SECTION FROM.

DATUM ———..

-TO. STARTED . ....

COMPLETED

8th

North 800 Weet ULTIMATE DEPTH

PROPOSED DEPTH ̂ .

DEPTH FEET

00 ~ 3.03.0 - 13.3

13.3 - H. 8l/,. 8 - 15.535.5 - ^5.7

..15^,.^ 23,0

' 23.0 - 26,0

26,0 - 26.9...26,9.^^27.* 9...

27.S. " 28 * 628,6 - 36.5

^6*1,- ?e*5

FORMATION

OasirigGrey silicoous sediment, quartzitic, Altered eraphiboDefew rusty seems at top, gray green bending, someblue quertz in blebs end bands, no ml ne re 1*Block sediments, oonsidereble garnets, no mineral.Grey siliceoxis pediments, quartzitic.Black sediment,, , spine garneteuGrey blue siliceous* quartzitic sediment, bending 30Oto core, Kerne ts in darker bands ©'17*3 to 17.8, 18,1,20.2 to 20,/t.Grey blue siliceous, quartzitic sediments, less band~

, i ne,Block sediments, considerable garnets, somopy 6t Po,Gray blue sediment, poor bending, ligfet greenishinclusions.

Black sediments, mull garnets, ( 1. mm )sorae Po in b(Grey blue sediments, good banding, few narrow veinletiof Ib. loss than I fo

Grey blue sediments, poorly banded, more green grey....mineral , not metBllic, ( ac W noli te) whl te quartz and

tourmaline fSlil.in^ frecturey C* 51,7 to 52.5 annd 66.6

• AMPLC NO.

nds..

WIDTH OF VAMPLt OOLD t

yuuppgOOLD f"

N.M.P.. TORONTO-STOCK FORM NO. 801 REV.

DRILLCO BY SIGNED..

DIAMOND DRILL RECORDPROPERTY. HOLE l

WiHET NUMBER

LATITUDE...........

DEPARTURE-.-. . ,

ELEVATION......

SECTION FROM.

DATUM^^—^.

STARTED .

BEARING.

-— COMPLETED-^

ULTIMATE DEPTH

DIP. PROPOSED DEPTH..

DEPTH FtET

78.5 ^ 83.3

.8J..^-...2I.6...

97.6 . 97.997.9 - 98.598.5 - 110.5

130.5 - H0.9110.9 - 112.8

112.8 - 134.01H.O ~ 117.0117.0 - 119^2119.2 - 322.2

^ -*^P

FORMATION

67.2 to 67.5, bonding coiitorted et 67,0 tp 68.0Mixture of black sedlmonts with gamete end some PO fe Pjend e,i^y green bands of siliceous meter! el, {quartzl t} c)considoreble folding of bonds, some bends messive Po @79.8 to SO.Zj, 80. k to 80.9, 81.7Grey siliceous? sediments, baling contorted, elightJjryellowish eel euler mineral (actinolite)

Dark fine grained cranular rock, (dike)Grey green sllioeour sediment, as above.Dark fine, granular sediment, few garnets , not magnet^Brown siliceous band,Grey blue bendfcd sediments, fine granular., some brownbends @ 31K*8 to 112.2 Quartz and alteration # HP t ft

Ground core.Dark fine granular sediment, with few small garnets*Brown grey banded sediments, mice noted a 117.6Grey green siliceous sediment, few cherty sections.

End of hole 32^9

• AMPLE NO. WIDTH OF SAMPLE GOLD t wm

N.M.P.. TORONTO-STOCK FORM NO, SOI REV.

er.-?..' SIGNED....,..............,....CVg:,xA j^y

DIAMOND DRILL RECORDPROPERTY. Trout Bay popper HOU NO.. 64 - 6

lEET NUMBER .....

LATITUDE .... ..................

DEPARTURE.. .......,

ELEVATION............

SECTION FROM________TO_______ STARTED,

DATUM __Glaim-JCiO.--48268________ COMPLETED __S

BEARING Southf ̂ Woot__________ ULTIMATE DEPTH

DIP_______Mirj UP M deByQ.gSi_______ PROPOSED DEPTH

t.JI964—-

DEPTH FtfT

0.0 - ^8.^

53,^ - 81.3

81.5 - 93.7

53-7 - 9/1.394,3^115.1.....

" " 1I8V3" J 15. B ~ ttfrS3j^3 *. 125.5P

FORMATION

Dark green, remnant coorse grajnod toxturo, large 8jpejj-lotchoo, petohes, A ran X 6 wu.. o f feldspar, maficintorgrowth t* iu FJne f rained greenish amphibole" GABBRO ^Oraflue3 change to epottea rock, irregular angularfragments} xlle?, light grey buff white, intermixedquartz end feldspar? - altcsi'ed, size 2*nm x 4 Jwi to8 win x 16 wu, bookgrciund greenish fine grainedchloritic, porphyritic flow? sill?, related to coarseKebbrolc rock above,Sharp oh'ange to Medium grained gabbroic rook, d&rkKreenish, slightly sheared.Lost core.Banded cherty sediment, minor garnets, aomo epidotealteration, banding .mo ro predominant, in argillaceous .eextlons, trace sal phi des t some balck carbonaceoustsoctionB^miner chloritic sections.J/wprophvre clike^ blackish brown.....Siliceous sediment, chert*

• AMPL.C No. WIDTH OF SAMPLE OOLD t

_____ y^-j^

\

\

8LUDOE OOLD f

^,.,.,-,.~-...^,vX tii'hi

-fttm

^frTTTKr^•*i;,i;.:,..:,..,.:

——————— l—

.

^TOi^

^A,X

K^

^1yr

N.M.P,, TORONTO-STOCK FORM NO. SOI REV. 18/SI

DRfttco ev-...P.o.oM^y.-r.,^.M1A..OfK.^ A ...,P.^.31or. J. Corrie. SIGNED.

HOLE F-4

DEPTH 499'

DIP -45 0

WEST -f-

AMPHIBOLE

f-ELD. POR.DIO.

AMPHIBOLE

GABBRO

TUFF AGO

RON FORM.

O

GABBRO

IRON FORM -AM PHI BOLE

-IRON FOftM AMPHIBOLE SCHIST

METASEDIMENTS QTZ VEIN

METASEDIMENTSARGILLITE

'- -TUFFACEOUS GREYWACKEARGILLITE

TUFFACEOUS GREYWACKE 'ARGILLITE

-GREYWACKE TUFF& ARGIL.GREYWACKE

GREENSTONE

ARGIL, a TUFF. GREYWACKE

END OF HOLE

SCHIST

LOCATION S KETCH

KRL 48877

MULCAHY TWP

KRL 33768

Location PlanSeal*t l" " 200' FALCONBRIDGE NICKEL MINES LIMITED

WEST 4-

~T.UFE.- -GABBRO

"TUFF. AGG.

GABBRO IRON FORM.

-CASING

AMPHIBOLITE

RON FORM.

-GABBRO

IRON FORM,•--—-G REYWACKE

-ARGILLITE-----DIORITE PORPHYRY

iGREYWACKE"AMPHIBOLITE

^— -ARGILLITE

-GABBRO

BLK. CARB. SL ATE,

HOLE F-6

DEPTH 45O'DIP -45 0

-GABBRO

END OF HOLE

1996 S

Amphibolite

Iron Formation

Amphibolite

Iron Formation

Line 10300 W

Feldspar Porphyry

Argillite

Argillit

Amphibolite

Argillite

Tuff Amphibolite

F-6 -

Scale; l" *

Iron FormationQuart?, Amphibolite Garnet Schist

Tuff

FALCONBRIDGE NICKEL MINES LIMITED D.D.H, Section F-6

(fiw

cc:r—O)

CMruOfVj—iae^

i"\*~^ Q

.—

uJ

^

-~\ /X7

V

* Y

S v

V-. ^

i S

Vi

- rV̂

~.

^."N

T

0

0

X

^

V

Z-

r^

^

^

.J A

^CC

N"'x^

^

ôi

x̂.

w/F -*

ll~^

LO

F

SIIS

-"

f-—

CO

1

^fe

P

.\\^

^

\\5 ^.

X̂-v

^te

— a7oJ*, 1CQ"U^^—

< oI:

c/):

oiD

N^n o

rvjcO ^

K R L 48?.6b

K K L 2 O 2 2

KRL 482 64

Of:

D. D. H OLt T B No. 2

STRIKE S 2 O0 W

D l P — ' 4 O0

D L P T H 6 4. S

A/K R L 49876

BALLTOWNSHI P LINE

MULCAHY

/y

DRILL HOLE. NO 3.1.B

oSTRIKE. S l O" W

D l P — 4 O0

Df F'T H l CM F Ft-T

K RI.

48268

KRL 48267

4 8 2 6 S

BALL.T OWNSH l P l.IN F.

M U L. C AH Y

LOCATION SKED. D.H 64-5

•TCH

K R L 48268

f.

N

t). P. H O IF 64*6

STRIKE S ftS 0 W

P l P — 4 C)0

DF PT H -- l 26 '

K K L

48277K R L 48 268

K R l.

48265

BALL TWRTOWN SH l P t IN E

MULCAHY™