DIAMOND DRILLING TOWNSHIP: McVITTIE TWP, REPORT NO: 46 ... · tIMetalic Minerals; Magnetite and specularite are present and abundant throughout. Specularite is coiion on fracture

$Page 1: DIAMOND DRILLING TOWNSHIP: McVITTIE TWP, REPORT NO: 46 ... · tIMetalic Minerals; Magnetite and specularite are present and abundant throughout. Specularite is coiion on fracture$
32D04NE0076 46 MCVITTIE 010

DIAMOND DRILLING

TOWNSHIP: McVITTIE TWP, REPORT NO: 46

WORK PERFORMED FOR: LAC Minerals Inc.

RECORDED HOLDER: Same as Above [xx]: Other [ ]

Claim No.

L 767470

L 801135

L 801174

L 801134

Hole No.

LV88-10

LV88-11

LV-88-12 LV-88-13

LV-88-14

Footage

655'

900'

547' 607'

898'

Date

Sept/88

Sept/88

Sept/88 Sept/88

Sept/88

Note

(D

(D

(D (D

(D

NOTES: (1) W8908-191, date filed June/89

DRILL HOLE DATA

Hole # depth dj. p Azm___start date

LV88-10 655ft -45o 180o 6 Sept/88

LV88-11 907ft -45o 360o lo Sept/88

LV88-12 547ft -45o 360o 15 Sept/88

LV88-13 607ft -45o 360o 19 Sept/88

LV88-14 900ft -45o 360o 24 Sept/88

end date, core size

9 Sept/88 BQ

14 Sept/88 BQ

18 Sept/88 BQ

22 Sept/88 BQ

29 Sept/88 BQ

Total Footage ^ 3616 ft

Lac MineralB Exploration - Drill Hole? Summary

r r i. j j esr. i. Property Hole No,

Logged By Date

Hole Type Start" DateEnd Date

Core S i 7. eRecovery

ne v j. i i iti

LV88-10..M...^ — .-.-..^ — ... .-,... — . - ..-. ,- . ..- . ,— ̂-.-

John Koval a January 1989

DDH

i..' lxooyt (.J /*

uocatxon — Line : Station ;

Length s Units :

Azimuth :

ElevationCollar :Bottom

L.8E 13+OOS 13+009

J. Ci K Mc) *j OFr tr rr T ^. . -. — . ^.. — . — -". — ™ — ..- LÎ.. 1

A*- o

i O ("l* ... ,—— ,—— ... -. ™ .M .. ....... -,JLD'.'

Target MAGNETIC HIGH,, EM16R RESISTIVITY LOW

Assay Cert No.

Hole : LV88-10 - Survey Data

Distance Asi Dip Type Remarks;

Lac Minerals Ltd Drill Hole ! LV88-10 Geological and Assay Data

!K From To Reoarks

Hole collared on bedrock D.O 2.0 Casing

2.0 14.1 MASSIVE FINE GRAINED INTERMEDIATE VOLCANICSDull grey green, fine grained nassive,non-iagnetic. No priiary texturesevident.Abundant carbonate in MatrixNo sulfides. Brown naterial (liionite), trace specularite on brokencore surfaces(U qtz carbonate stringers.Minor sericite present loner in section with silicified carbonatealtered sectionsLower contact not distinct.

11.1 50.7 ALTERED LAPPILLI TUFFIntensely carbonate, silicified K-spar chlorite altered, (patachy)Colour varies fros light green to black, auch of the section has a lottledtexture of light green rock containing patches (spots) of green chloriteand qtz carbonate and K-spar stringers and lasses that are lost often quiteirregular.Minor sericite present. No sulfides.5 - 87. qtz K-spar carbonate lasses and stringers at all angles to CoreAxisPossible lappilli size fragments, light green in colour set in a dark greento black matrix present betxeen 39' and 50.7'.

14.1 to 28.2 Intensely qtz carbonate K-spar altered. K-spar carbonate masses and stringers.

28.2 to 39,4 Mixed dark green-black sections containing possible light green to black lappilli fragnents and intensely altered sections siiilar to 14.1 to 28.2.

39.4 to 32.5 Doninantly dark green to black Matrix laterial, chlorite altered containing 10-15X lappilli fragments.

30,0 to 32.5 Broken Core

Lac Minerals Ltd Geological and Assay Data

X From To

Drill Hole : LV88-10 F F

1

: sRemarks i N

38.0 to 39.0 Alternating light grey and green patches elongate at 45' to Core Axis.

50.7 66.6 HASS1VE FINE BRAINED INTERMEDIATE (?) FLOHMassive, fine grained, non-iagnetic, dull grey green. Sinilar to 2' to 14.1'. No Primary textures evident. Abundant carbonate in tatrix. Cut by 4 to li qtz carbonate * K-spar veins .5 to 2ci Hide. Veins at doninantly 30* to Core Axis. Often vuggy. Trace chalcopyrite.

Lower contact not distinct i 35* to Core Axis

66.6 161.0 ALTERED SHEARED LAPPILLI TUFFColour varies fro* light green Kith black spots and irregular stringers to to dark green black and to sheared bands lediui to light green in colour.

66.6 to 122.0 Appears siniclar to 14,1 to 56.7 .Fragments present. Appear elongate at 43' to Core Axis

122.0 to 148.0 The section is oioderately sheared at 50' to 60* toCore Axis. Elongate dark patches 0.5 to 1.5cm x 1.2 to O.Scs are present in a light green to white iatrix of qtz carbonate and chlorite (t epidote?), 2 to 41 < 1m sericite occurs throughout.

148,0 to 159.0 Intensely altered to light green but foliation not Hell developed.

159.0 to 161.0 Fault ZoneFault gouge froi 159.5 to 160.3. Angle of fault not distinguishable. Minor l iionite on fracture surfaces,

FBH carbonate qtz veins ) O.Sci present over entire section, Qtz carbonate occurs dominantly as tortuous lasses elongate parallel to foliation 8 50' to 60' sonetioes 90' to Core Axis.

FLac Minerals Ltd Geological and Assay Data

Drill Hole : LVBB-10

K From To Remarks

No sulfides present, non-eagnetic.

161.0 164.8 LAPILLI TUFFGrey green, 5 to lOX light and dark green lapilli fragments in a greygreen isatrix, non-aagnetit.Trace pyrite.2 - 3X qtz carbonate stringers.Carbonate is abundant in latrix.Trace pyrite.Lacks intense alteration to light green and no sericite is evident.Lower contact 8 80* to Core Axis.

164.8 655.0 CRYSTAL TUFFMassive section consisting of 2 to 40X plagioclase crystals l to 4im longin a fine grained dark green natrix, l - 37. < lil specularite crystalsand l to 3X ( l Rm aagnetite crystals occur throughout the latrix.Moderately to strongly fagnetic.Carbonate throughout natrix.0.5 to 37. qtz carbonate t K-spar stringers.K-spar alteration iron 205.0 to 210.0 causes pink colouration (weak tomoderate) of the aatrix, veins and feldspars. Above section is siliciousand carbonate rich and Host a greater acount of quartz carbonate K-sparveins (ie-2 to 5)1) and occasional sericite.

Felspars 20 to 40!! occur as patches separated by sections of 2 to 10Z feldspars. Most patches appear elongate, contacts vary between patches patches froi sharp to gradational.

Contact ie at 560 - 47* 538 - 36' 573 - 47* 542 - 39*

Trace chalco with quartz carbonate stringers. Trace disseminated pyrite.

190,0 - 200.0 Six 2 to 20ci qtz carbonate veins often containing

Lac Minerals Ltd Drill Hole i LVB8-10 f Geological and Assay Data F

X From To Renarks ! l

chlorite 8 50 to 60' to Core Axis.

295.8 to 296.7 Sheared dark green to black fine grained rock. Minorpyrite, 30X quartz carbonate and sericite, sheared at 20' to Core Axis.

295.0 to 410.0 K-spar, qtz carbonate altered as previously described.

tIMetalic Minerals; Magnetite and specularite are present and abundantthroughout. Specularite is coiion on fracture surfaces..

442.0 to 447 Minor vuggs present in core.

8 639.5 Trace chalco in quartz carbonate stringers.

655.0 655.0 END OF HOLE

1NOTE: Hole drilled through corresponding Magnetic and EM16R Resistivity anomaly. Magnetic anonaly caused by high lagnetite content of core. LOH resistivity values are probably due to conductive overburden overlying area of drill target and or possible fault ! 159 to 161'.

XX

Lac Minerals Exploration ~ Drill Hole Summarys :s as 5S s::: K: s- w s

i- r o j e? c T; Property Hole No.

Logged ByDate

Hole TypeStart DateEnd Date

Core S i K e Recovery

I'lCVA 1 1 it:.

LV88~ii* - * *.. .. .-. . -. * ...— .-.-.

DAVE ADAMSONSeptember 15th, 1908

*- M. ~ .^. W.———.^,.. .~-. ......... WH4mn. HIW ...-.*- M.. -...——— W.. *,. .——— -. . . *^-~ .———

DDHSeptember 10th, 1988September 13th, 1988

-.

BQ

uocation —— - — -— - —— --•-•- —— ...,..,....™-,.,.- Line : 11^755, 36E GRID B Station :

Length : 900' -— — ™ ————unitis s lee t — ——

|-\j r.. . yltro .....MM .™.~.-..*.~.....M _ I J J. P S 'i D "7

Hzimuun s oov

Elevation — — — ~...— m ..™.. .-—-.™— Collar s ———— ........——fi f-\ 4" 4- ̂ "V **\ m u* M m. Ma .BH H.* M,, -,-DOutom * — — -...-.~--.....— ~.

Target : IP Anomaly arid EM Anomaly

Assay Cert No

Hole : LVB8--11 - Survey Data

Distance

307.0 607 .0 907 . O

Asi Dip Type

45" ACID

45"

Remarks

j ONTARIO GEOLOGICAL SURVEY j

A S t; ir i S iVI f.: NT FiLtSOFFICE;

.H'M ZZ

RECEIVED

IssssssszrsarsssssEsrssssssssssssassrsssssrssxssrcsrssrsrsErstsxsxsszsESBCcrsccsiXBSBSlsssssESs

Lac Minerals Ltd Drill Hole : LV88-11 Geological and Assay Data

X Fro* To Reiarks

0.0 29.4 OVERBURDEN

TEHISKflMINB SEDIMENTS

2?.4 44.0 QUARTZITE, tiediut grey, -tinor ((2') intercalated black, soft ludstone l 43.8 - 44.0'Mineralization: 36.8 - 37.6; 3 - 5X fine grained pyrite along 'bedding' acconpanied by i - 21 yellow phyllosilicate alteration cba's average 60*

44.0 44.6 GREYWACKE, light grey, fine grained Kith occ. ludstone clasts, Clasts identical to rudstone bed C 43.8 - 44.0'

44.6 67.0 GREYWACKE, altered, light grey cut by numerous quartz * carbonate stringers.Stringers aligned 8 30 - 50* to core axisSone of the ssaller veins Kim) accoipanied by light to lediui green chlorite Veining accompanied by pyrite in places (see belon)

80.4 - BO.5 Rudstone interbedmuch of the section contains carbonate in the groundless and reactsweakly with HCLcba's : 55*

Mineralization: Pyrite t 84.8' cba = 90* Pyrite 6 76.9' cba * 40 f Pyrite 6 75.45' cba * 20'

45.6 - 45.7 broken core (fault)

87.0 103.0 6REYNACKE, moderate to heavy shearing, light grey, BrayNacke forts fragments separated by black carbonaceous iatrix (3- - 40X), Sole fragments are rounded, and this unit nay be badly sheared congloierate. Thus, Bore likely sheared greyKacke/iudstone unit. Matrix is soft but not graphitic, probably chlorite-rich. Light grey

Lac Minerals Ltd Drill Hole l LVB8-11 Geological and Assay Data

X From To Remarks

fragments have been carbonated.Foliation/core axis angles 45 - 65*97.2 - 97.3 Quartz-carbonate-chlorite vein t 60* to core axis101.2 - 102.2 Quartz-carbonate-chlorite vein

Mineralization: in-wide pyrite veinlets with well defined crystals i 94.0' 94.9'

103.0 107.8 HETEROLITHIC CONGLOMERATE, gradational upper boundary. Pebbles vary in size from a fen m to lOci and average 401 of the section. Matrix is sheared lediun grey greywacke. Pebble types: (in approxiiate order of abundance)

light grey siliceoussilky unite siliceousblack ludstoneyellow clay-richgreen fuchsitic (ninor)

107.8 134.4 BREYUACKE, nediui grey, altered120.3 - 120.5 contorted quartz vein130.9 Guartz-carbonate-chlorite vein 10* to core axis

134.4 137.4 CONGLOMERATE, with 60 - 701 subrounded clasts upto iOci in size.Matrix is coarse grained greynacke containing quartz-feldspar-*aficsand yellow phyllosilicate alterationPebble cosposition as in above congloierate description.

137.4 158.4 GREYWACKE, coarse grained, (l - lOiil with O - 51 2.5ci pebbles, cba's 45'144.5 Quartz-carbonate-chlorite veinlet cba * 30* 146.4 - 146.5 Quartz-carbonate vein 148.3 - 148.4 Quartz-carbonate vein cba * 35* 149.1 - 149.2 Carbonate-chlorite t ludstone band 151.1 - 157.4 Extensive quartz-chlorite-carbonate veining Nith

carbonaceous material

Lac Hinerals Ltd Drill Hole : LVBB-li Geological and Assay Data

X From To Reiarks

158.4 192.5 CONGLOMERATE, Hell preserved (little altered) l clasts * 30 - 80 Pebble types:

light grey porphyritic rhyoliteyellowish sedimentsquartz pebblesdark grey mudstonenilky white volcanic/granitic

green chloritic(list is in order ol abundance) Matrix is coarse grained greywacke

192.5 192.6 MUDSTONE, band cba 70*

192.6 192,7 CONGLOMERATE,

192.7 193.8 6REYHACKE, coarse grained

193.8 195.2 CONGLOMERATE

195.2 201.B GREYWACKE, coarse grained Hith tudstone clasts. l clasts increases donn hole. Kay up therefore is to SOUTH.

201.8 202.8 MUDSTONE, dark grey to black fine grained.

202.8 204.0 MUDSTONE, sheared. Disrupted bedding * quartz veining. cba's 10 - 40*

204.0 204.7 GREYWACKE with nudstone clasts

204.7 207.9 CONGLOMERATE, 'Bedding' of pebbles * 70' - 80 1 to core axis

207.9 208.0 CHLORITIC, (green) shearing

208.0 341.2 BREYKACKE, tassive, tediui grained graded beds face SOUTH t 243 - 247'

c Hinerals Ltd Drill Hole : LVB8-11 F Geological and Assay Data t

EErEEIEEEEriSESISSErrsrEZrEZEEEErErrrEEESrirrrEEEEErEEEEEEEEEEEEEEEEEIIEESEEEEEEErEEESEESEEEESEEBl

X Frosi TD Renarks ! l

6 240 - 242, sub-angular, quartz-rich clasts upto lOci in size.

Mudstone clasts i 259.1 - 259.2257.8 - 260.5267 - 267.8269.9 - 270.0275.0 - 275.8284.3 - 286.2297.8 - 297.9300.85 - 301.0304.8 - 304.9

Numerous sudstone interbands between 311' and 327', Load casts indicateNay up to SOUTH.f 347' load casts indicates way up to NORTH.veining E 276.1 - 276.2 (carbonate-quartz)

300.8 - 301 {quartz t carbonate) 307.75 - 308 (quartz - carbonate) 307 - 310 (carbonate stringers 8 70' to core axis)

Fault i 286.2 - 286.5 (broken core)

Mineralization:268.3 - 268.5, 15 - 20X pyrite along bedding (cba * 45*)

cba's of greywacke 65 - 75'. Individual tudstone beds tay indicate topsof bouia sequences.

341.2 347.8 INTERBEDDED 6REYHACKE/KUDSTONE

347.8 381.0 CARBONATIZED GREYWACKE, Hith dark grey quartz stringers Stringers 60 - 90' to core axis

372 - 372.1 Quartz-carbonate-chlorite vein

Mineralization!

Hinerals Ltd Drill Hole s IVB8-11 Geological and Assay Data

X From To Reiarks

367 - 367.4 Py veinlet 5* to core axis 369 - 369.2 5X pyrite 40* to tore axis

381.0 411.0 CONGLOMERATE, extreaely sheared and carbonated. Soie pricary pebbles visible, but most heavily altered and sheared.

390.2 - 390.5 Quartz veining 60 - 90' to axis of core

Mineralization; 389.8 trace pyrite

411.0 416.8 GREYWACKE, lediun grained

416.8 502.2 CON6LOHERATE, altered and sheared. Extensive carbonate alteration. Minor pyritic zones.

Gross fining indicates Hay up to SOUTHBreywacke sections 8 430.4 - 431

431.4 - 431.6431.7 - 433.4

Mineralization: Minor pyrite sections 8 421.4 - 421.5427.75 - 427.8 429.0 - 429.7 cba's 55 - 80' 442.6 - 422.8

Quartz-carbonate-chlorite vein with linor pyrite * chalcopyrite 6 444.2 - 445.0. Pyrite t chalcopyrite * 0,5* cba 20',

Pyrite t 445 - 445.7

Pyrite t trace chalcopyrite * 446.1 - 446.3

447 - 448 Extensive quartz-carbonate veining and alteration . Primary congloierate texture aliost destroyed.

469 - 502.2 Highest grade lineralization section. Core is heavily


K Prod To Renarks

altered, dark grey to black (carbonaceous), priiary conglonerate texture still visible.

469 - 475.3, Finely disseninated pyrite in sheared congloierate latrix. cba 55*

475.3 - Chalcopyrite-bearing Q-cab vein

477 - 487.5 Uniineralized interbedded conglwerate (BOX) and greywacke.

487. 5 - 505.3 Disseminated pyrite and 'blebby' chalcopyrite492 - 493.4 3 - 5X chalcopyrite i - 21 pyrite493 - 497.5 l - 2X chalcopyrite O - li pyrite rest of intersection Cp O - IX

502.2 732.0 ftLTERED SECTIONExtensively carbonatized rock with carbonate * quartz net veining. Veins traverse light greenish grey sassive rock, Hhich generally has no priiary textures. Veins are dark grey, carbonaceous and weakly lineralized by pyrite. (O - IX) 'cba's of veins 45 - 65'

Original rock type is difficult to discern, flay be:a) altered and sheared tassive greywacke

i

b) carbonatized lava unit.

In places, the section has a 'aottled' texture similar to that in less altered nafic lavas deeper down the hole, (ie; Kinojevis Group volcanics). This interpretation would place the upper lineralization described above at the Temiskasiing-Kinojevis (487 - 505.3')

HINERftLIZftTION:Section contains scattered pyrite cubes, soie of which are partly oxidized, may be another nineral intergrown with pyrite causing oxidation. Pyrite concentrated around cross-cutting veinlets. Rarely exceeds MX of section, Very cinor anounts of chalcopyrite sporadically developed.


Drill Hole i LVBB-il

X From To Renarks

i 539 - 541.7 Fault zone, abundant carbonate, liionite, goethite

Fault also at 597,3 - 601.7 640.2 - 640.7

732.0 907.0 Gradational contact into green ALTERED MAFIC VOLCANICS of the Keewatin series, amygdaloidal sections 6 733.2 - 734.2

788.8 - 790.3 quartz-carbonate veins l 739.9 - 740.1

750.8 - 751.1814.9 - 815839.5 - 836

flow tops * 801.7 802803.6 - 804.9809 - 811.6876 ( May up SOUTH)

cba's 45*

vein/core axis angles 10 - 55*

Mineralization:835.1 Py veins 839.5 - 836 Fy veins 763.2 - 764.8 Py veinlet 739.9 - 740.1 trace pyrite

907.0 EOH

Lac Minerals Exploration - Drill Hole Summary

Project. Property Hole No,

Logged By Date?

Hole Type Start Date End Date

Core Bine Recovery

MCVITTIE GRID B

LV88-12.. M .... -M.. . "' ""'

DAVE ADAMSON October 18th, JL98B

DDH September 14th, JL988 September J.6th, JL988

B Q 98"/.

lf-tf--ft4-**-t|-L M .., M ..L, D c ci 1. 1 on " ' Line : 36E 20+253 Station t

i — -- -- o. t- . ci /i "7 * . . -. -,- M.. -4. M. . ,I— enyun S D*r/ —-..—M™ — .1 Ir-* -i 4- *- m M *.. -. .M. -H. .- wun i t s s ..-— "- — .—.-.-M— -~

r\^r-k a /l Ci * ™. .*.- — — -*. .,U X p i *t D ™ "~ "" •* " "" 'Azimuth : 360 0 — -— ——— - —

Elevation ..-— — — — .. — ..™.......... -.-.....~— .,.r^*îi-*w- * HM .* UD /i 4- 4- i-i m i .... ™- .. ,. — M- . __ m—.—tiottom s ...~.— — — - ~

Tarqe?t TESTING IP AND EM ANOMALY

Assay Cert No.

Hole : LV88-12 - Survey Data

Distance Azi Dip Type Remarks

300. O 547 . O

45 045"

ACID

JNVARIC GEOLOGICAL SURVEYi K, - .., l "r-rf f i! '.QAotsciji)W ! t-iv i f it-t-o

HIM

RECEIVED

Lac Minerals Ltd Drill Hole : LV88-12 Geological and Assay Data

K Front To Reaarks

0.0 15.0 OVERBURDEN

TEMISKAHING GROUP 15.0 70.9 GREYWACKE, iediui grained lassive Mith congloierate bands

43.6 - 45.4 - conglomerate, contact is at 60' to core axis

70.9 75.2 CONGLOMERATE contact Kith above unit M5 ' to core axis- pebble types:

- greenstone- quartz (occ. py-bearing)- felsic porphyritic volcanic

75.2 98.9 GREYWACKE with occasional MUDSTONE CLASTS and < li pebbles

98.9 190.1 CONGLOMERATE- pebble types:

- aediui grey felsic volcanics- Mhite quartz- light green felsic volcanics- light grey felsic volcanic/quartz- black carbonaceus ludstone- dark grey nafic volcanic- granite

Pebbles 50 - BOX - fraiework supported lower contact 8 50* to core axis

190.1 193.8 GREYHACKE fine grained with chlorite-rich beds cba's 20*

198.3 196.7 CONGLOMERATE (as above description)

196.7 197.8 GREYWACKE fine grained, May up to SOUTH (up hole)

197.8 325.3 CONGLOMERATE lassive Mith 51 coarse greywacke - 264.6 - 265.1 ludstone

Lac Minerals Ltd Drill Hole i LV88-12 Geological and Assay Data

K Proa To Remarks

conglomerate as above * li fuchsite pebbles cba's 55 1

325,3 382.6 CARBONACEOUS SCHIST (prob cause of anoialy). Abudant quartz-carbonate- chlorite veins. Very disrupted bedding, no consistent direction. No visible generalization.

382.6 547.0 DAC1TIC TUFF, grey-green containing:quartz and plag phenocrysts and H fuchsitic lithic fragsents

sections silicified and light grey

whole section cut by ninor quartz-carbonate stringers.

467 - 449.7 carbonaceous shear cba 65'457 - 470 abundant kffi quartz veins fi 60' to axis470 - 470.2 Ion angle quartz vein483.5 - 487.3 partially broken core, liionitic stain489.3 - 490.6 broken, lost core497 - 543 tr - li pyrite

547 EOH

Lac Minerals Exploration

MCVITTIELV88--I3

Drill Hole Summary

Project F1 r o pt? r t y Hole Mo.

- n 4- 4 r~\r* -.^...— .^.M.,..^,....^.....^....... ,- .~.™.....- ci L, x onLine i 26+25S, 36E BRID B Station :

Logged By Date?


DAVE ADAMSON August 27th, 1988


Length Units

Dip : -45" Azimuth : 360"

Core Sisie Recovery

B Q 987.

Elevation Collar : Bottom :

Target : IP Anomaly

Assay Cert No.

Hole : LVS8-13

Distance Asi Dip Type

Survey Data

Remarks

307.0607 .0

ACID

ONTARIO OSiOLOGIOAI. SUBVCiV SbSSMbK'T FILES

OFF-'ICF.

.HIM Z2 1989

RECEIVED

X

Lac Minerals Ltd Ecological and Assay Data

Frosi To

Drill Hole i LV88-13

ii i

Retarks !

O 71.9 OVERBURDEN

TEMISKAMING GROUP 71.9 87.3 MAFIC TUFFS

- equivalent to porphyritic trachyties of DBS- Fedlspar-phyric. Feldspar replaced by carbonate- fine grained dark green groundiass- black lithic fragments- overall composition probably andesite or basaltic andesite- fragments flattened in plane of foliation- unit weakly stratified - probably as ash floH deposit- cba's average 45*

B7.3 89.5 TUFF-BRECClfi- 75X medium to light grey lithic fragients in a aatrix siiilar to that

of above unit- fragments sub-angular - flattened in plane of foliation- fragments 2cm - 5ci across- cba's average 45'

89.5 97.5 HAFIC TUFFS- as in above description, crystal and lithic fragients

97.5 109.3 CARBONATED HAFIC TUFFS- texturally similar to tafic tuffs, but carbonate alteration gives core

a fiediun grey colour- gradational upper and lower contacts

109.3 115.9 Broken Core - 501 recovery - silicified tuff-breccia unit

115.9 126.4 BLEACHED HAFIC TUFFS- crystal (feldspar) and lithic (dark lafics)

114,8' - 5c* fragment of black porphyritic rhyolite

- abundant carbonate veining at 50 - 75'- minor pyrite 8 323.5

yssssssssssssissszzsssssssssssssssssssssssssssssssssssasssssssxfsssxsttasssstssttfssxsxssstssm

! Lac Minerals Ltd Drill Hole : LVBB-13 ' Geological and Assay Data

IX Front To Remarks

121.1

126.4 133.2 HETEROLILTH1C AGGLOMERATE- subangular fragments 2 - )10ci, total SOI- matrix supported- composition of fragments: light grey porphyritic volcanic -

hornblende phyric dark green line grained volcanic dark grey felsic volcanic

- bleaching adjacent to carboante veins i 127,6 - 128,4 l 45*135.1 - 135.8 l 35'

133.2 147.4 DARK GREEN AGGLOMERATE- 10 - 20X iafic fraguents- felsic fragsents absent- natrix supported

147.4 163.5 HETEROLITHIC AG6LOHERATE- as previously described- 10 - 151 carbonate stringers and veins f 25 - 70* to core axis- O.Sci pyrite cubes t 161.4'- lei oxide stain in sheared section i 162 - 162.5

163.5 213.3 INTERMEDIATE CRYSTAL LITHIC TUFFS- altered and veined sections- lighter colour (light grey) than MAFIC TUFFS at top of hole, probably

due to pervasive alteration- quartz veins l 164.2 - 164.6

165.8 t 60' to core axis166.3 - 166.5 l 50' to core axis167.8 * 45' to core axis168 f 35*168.6168.8179.6 - 180.3

Lac Minerals Ltd Drill Hole s LVB8-13 Geological and Assay Data

i X Fron To Reiarks

- quartz veins white, except t 179.6 where it is white and tan- Altered section! 190.3 - 191.4, carbonate t quartz stringers- bomb of light grey felsic volcanic 8 192.3

212.1 - 213.2 quartz vein i 45', abo l 214214,4 - 214.5

213.3 216 FINE GRAINED DACITE TUFF- (51 dark grey siliceous frsgients- nediu* grey colour

216 250.7 MAFIC LITHIC TUFF- contains dark green to black frgaients (20 - 30/1) up to let in size222' Quartz-carbonate vein 8 5*242' Pink quartz * carbonate vein t 30'

250.7 252.8 DARK FRAGMENTAL AGGLOMERATE

252.8 254.5 PINK FRAGMENTAL AGGLOMERATE- ping granitic to trachytic fragients- fragments 70X, latrix supported

254.5 259 ALTERED SECTION- light green to pinkish grey- pink quartz-carbonate veins l 255.3 - 256.9

256' cherty part of vein257.3' black cherty section258.5' white quartz * black chert i 3* to core axis

259 260 K-SPAR MEGACRYSTIC TUFF- lcs Kspar aegacrysts (after leicite?) - 2 - 3X- whitish lithic fragsents 51- cherty (black) fragients IX- fine grained pinkish groundlass - cba's 80*

260 264.1 PINK FRAGMENTAL AGGLOMERATE

Lac Minerals Ltd Drill Hole : LVBB-13Geological and Assay Data

X From To Renarks

- BOX trachytic (?) pink blocks (up to lOci across)- fragment supported- lilght to cediun green tatrix

264,1 307 DACITE TUFF- grey green- 10 - 20X dark green lithic l - Sai across- abundant white and pink quartz stringers fi 45' (10X)

65. 5 - 266. l folded white and pink quartz veins- also at 269.2 - 269.B

271.2271.8 - 278 278 - 280.2 fi 3* to core axis

- jiinor si-size pyrite cubes fi 294.8299.4 304.7 (vein fi 45' to core axis)

307 310.1 TUFF-BRECCIA- veined and altered- light to tedium green- 5X 2cD angular fragients, dark green, aphyric- veins l 60 - 70*

307.6 - 308 Milky white quartz vein fi 65' * trace sericite and fuchsitic chlorite

- scattered pyrite cubes in vein l 307.6

310.1 315 MASSIVE GREYWACKE- lediui grained- irregular contact with aggloierate/tuff above fi 20' to core axis

315 352 DACITE TUFFS- light grey-green- altered and veined sections- generally cassive and structureless

Lac Minerals Ltd Drill Hole : LVB8-13 Seological and Assay Data

X FroA To Reiarks

- 5X lafic fragments aligned 6 60' to core axis- 5X quartz veins- larger veins at: 313.7 - 315

325 334.4 347.4 348.2 352

- iinor pyrite 8 325.7 - 3*1 cubes IX1X) 329.5 342.8 352

352 354 TUFF BRECCIA- extensive quartz veining- 2 generations of quartz, one at B - 10', the other at 60 - 70' to

core axis

354 357.7 DACITE TUFF

357.7 360.3 INTERMEDIATE TUFF- interbeds of epiclastic congloierate, abundant rounded felsic fragments

360.3 364 COARSE EPICLASTICS- siedium to light grey clacitic groundiass- l - 5X felsic rounded clasts

364 367 ALTERED INTERMEDIATE TUFFS- 5X chloritized uafic fragients- light green/grey

367 377.5 DACITE TUFF- light grey-green- 551 green, chloritized tafic fragients

377.5 382 SILICIFIED TUFFS

Lac Minerals Ltd Drill Hole : LVB8-13 Geological and Assay Data

X From To Reiarks

- pink/grey- fine grained- 205! quartz stringers surrounded by pink carbonate haloes- stringers fi 65' to core axis

382 387 INTERMEDIATE TUFFS- lediuni grey- IX epiclastic interbeds

387 391.6 CHLORITE SCHIST- 60)1 quartz veins fi 10 - 20* to core axis- cba's approxiiately 20*

391.6 395.7 FELDSPAR CRYSTAL TUFF- 30 - 40X Sun feldspar crystals- light grey siliceous groundless

395.7 496 FINE GRAINED TUFFS/SEDIMENTS- dark grey to black- pervasive carbonate veins parallel to 'bedding'- scattered 'pods' of carbonate, probably replaced clasts

401 - 401.7 Carbonaceous Mudstone 409 - 410 Carbonate 'clasts'

also at 412.5 - 413.3 434.4

417.9 Carbonate 'clasts' t quartz pebble (5ci)

417.7 Mudstone clasts

- linor quartz veining fi 397 - 398 450.4 fi 10' 464.6 fi 10' 490.1 fi 50'

486.5 - 487.3 Mudstone

Lac Minerals Ltd . Drill Hole : LV88-13 Seological and Assay Data

l

X From To Reiarks !

- cbajs 50 - 65*- contact i 488.6 8 25'

496 502.5 MAFIC TUFF- fine grained, dark green- cba's 45*

502,5 507.6 BRAN1T1ZED TUFFS- IOH 'cba's' 0-5'- quartz-Kspar-thlorite alteration- trace chalcopyrite along section- 503.6 - trace galena?

507.6 511 ALTERED CHLORITIZED 6REYHACKE- lediusi grained, grey/green

511 594.6 GREYWACKE- fedius grained to coarse grained, grey

511.8 - 512 Mudstone clasts520.5 - 520.8 Fine grained light grey sediient

UCT 8 35'531.4 - 532 Quartz veins l 65*

also at: 533534 - 536.1537.6539.5540.1542 - 545

542 - 548.7 Altered tuff - brecciated and cut by 101 Quartz veins

- Neak (l - 21} pyritization of greyNacke6 511 - 512.1

514 - 516.4517 - 520


Drill Hole : LV88-13

X Froffl To Remarks

525.5 - 526.7534.6 - 534.8 (i - 3X pyrite)539 - 539.5 pyrite veinlets l 30' to core axis545.1 - 547 bleached core, 2-31 3i* pyrite cubes547 - 548.7 UX pyrite586.7 - 587.2593.2 - 594.6 l - 21

594.6 598.6 QUARTZ-CHLORITE BRECCIA (FAULT?)

59B.6 607 6REYHACKE

607 EOH

Lac Minerals Exploration Drill Hole Summary

Project. Property Hole No.

MCVITTIELV88--14

Location ——-————Line :Station :

Logged By Date


DAVE: ADAMSONOctober 28th, 1988


Length ! 898'Units :

Dip : 45"Azimuth : 360*

Core -SiEe Recovery

BQ 9 9 X

Elevation ——- Collar : Bottom :

Target :

A s s a y C e i" t N o

Hole i LV8B-14

Distance A;-: i Dip Type

Survey Datass SL* ™ 35 ™ cr 2S s: ss zn: ss st ss; ss ss STJ cs ES r- K; " s™ ri! st'. ST. 52: -^ IK: ES ss: ™ s^: s

Remarks

306 . O 509 . O 897 . O

45*45"45"

Acid

jONTAWio rtf;c

Joi:ciîOFFICE

.'"M ^ W)

.RECEIVED l~~——•—•••..——-,. Ji

Minerals Ltd Drill Hole i LV88-14 Beological and Assay Data

:zzzzzzzzzzzzzzzzzzzzzzzzzz:zzz:zzzzzzzzzzzzzzzzzzzzzzzzzzzrzzzr::::zz:::K:z::zEE::3r:srz:Err3E::i it l

l Front To Renarks !

0.0 13.0 Overburden

13.0 15.1 TENISKAMING SEDIMENTSSilicified and sheared conglomerate, lipossible to distinguish priiary pebble types, all are light grey and siliceous. Matrix to sheared pebbles is olive green and chloritic.

Mineralization; einor pyrite l 14,0' cba's 78 - 80'

15.1 17.4 Duartz-chlorite schist, lore altered variety unit described above.

Mineralization!section is weakly pyriticcba's 70'

17,4 54.0 Laminated, interbedded fine-grained greywacke and chloritic ludstone with minor interbeds (10-20cn) of nediui-grained greywacke, Proportion of greywacke is approximately 70:30. Overall colour of section lediui green. uediuffl grain-size greywacke beds ! 25.7 - 25.9

26.2 - 26.3 26.7 - 27.2

cba's 50 - 60'

54.0 57,0 medium grey, coarse-grained greywacke

57.0 56.0 massive itediun-grained

58.0 72.3 Interbedded fine-grained greywacke and chloritic ludstone. Greywacke! Rudstone - 85:15

72.3 77.4 coarse-grained greywacke with (51 pebbles up to 6ci across. Greenstone and felsic vole pebbles dominant aligned 8 45* to core axis. Pebbles nore numerous at base of unit, gross fining is to the SOUTH.

77.4 79.7 conglomerate 60)1 matrix supported pebbles is a coarse-grained greywacke

Lac Minerals Ltd Drill Hole s LVB8-H P Ecological and Assay Data P

i 5 IX From To Renarks ! k

Ratrix. Pebble types: quartzfelsic volcanic sediments (yellowish) greenstone

79.7 81.6 coarse greywacke with (51 pebbles

81.6 86.2 conglomerate (as above description)

86.2 87.5 fiediun greywacke

87.5 B8.9 conglomerate (as above description)

B8.9 94.2 banded nediuft greywacke * chloritic Rudstone (5X) and l - 3* pebbles

94.2 122.2 fine-grained thinly laiinated to lasinated Rudstone with fine-grained greywacke interbeds.

cba's 60* Mineralization: minor pyrite i 108.6

109.7 - 109.9 associated with Quartz veining 2 generations of quartz; a) RediuR-grey

b) white, later and consulting 50' to core axis.

122.2 123.B coarse-grained t (51 pebbles

123.8 124,3 Thinly laminated nudstone (black). Upper .contact is 45' to core axis way up to the SOUTH

124.3 125.7 Fining upwards sequence of coarse greywacke with pebbles (base) to fine greywacke t nudstone (top)

125.7 126.0 black cabonaceous Rudstone

126.0 128,2 nediuit-grained greywacke with(5I pebble bands. Pebbles nicely felsic

Lac Minerals Ltd Drill Hole : LVB8-14 Beological and Assay Data

!K Fron To Remarks

up to 3cn across. 5X interbeds of cabonaceous mudstone, cba's 55'

128.2 129.2 Fine-grained greywacke

129.2 164.8 Hatrix supported conglomerate with the following pebble types: tea-coloured felsic volcanics (porphyritic) nilkly white quartzgrey felsic to intermediate fine-grained volcanics yellow sediaents (fine-grained)

in approximate order of abundance Absence of : Rudstone * greenstone * clast types

Total pebble X * 20 - 6-X, size Uci - 15ciniatrix i) medium-grained greywackecba's 60* from moderate flattening on pebbles

Mineralization! minor py t 121

131.6

164. B 176.4 coarse-grained greywacke. Minor pebble bands t 170.6 - 171.3 and 176.3 - 176.4. massive with little bedding visible

176.4 177.6 Heavily contorted mudstone - dark grey and carbonaceous with lighter grey (silt?) interbeds,

177.6 182.2 Fine-grained greywacke with mudstone interbeds. Breywackejmudstone ratio s 90:10 cba's 45 - 50*

182.2 182.4 Cabonaceous Mudstone

182.4 187.0 Medium-grained greywacke with 151 mudstone interbeds cba's 55* Mineralization

Lac Minerals Ltd Drill Hole ; LV8B-14 l Geological and Assay Data

IK From To Reaarks

183 - 186 minor pyrite along bedding plains

187.0 192.5 Laminated Rudstone - siltstone contorted bedding, abundant interfolial felds approx cba's in less folded sections s 50*

192.5 193.4 eediun-grained greywacke with tudstone clasts and interbeds

193.4 194.0 conglonerate

194.0 194.6 fining upwards (to SOUTH) lediui greywacke (base) to laiinated iudstone (top) cba's 35*

194.6 195.3 coarse-grained greywacke

195.3 195.7 conglomerate


196.7 237.0 Conglonerate Mith approxinately 21 coarse-grained greywacke beds* 219.3 - 219.8

223.8 - 224.6234.7 - 235.1236.2 - 236.8

noderate to strong flattening on pebbles cba's l 202' - 50'

217' - 55' 223.8' - 50'

generally fraitework supported 70X pebbles. Pebble types as described above (8129.2') with addition of li black ludstone clasts

237.0 258.8 poorly bedded coarse-grained greywacke

258.8 261.4 Mudstone Hith abundant white quartz veins and tinor fine-grained greywacke

Lac Minerals Ltd Drill Hole : LV8B-14 Geological and Assay Data

X From To Remarks

261.4 281.2 Thinly bedded nediui-grained greywacke Hith (51 ludstone interbeds cba's 58*

281.2 283.2 Fine-grained greywacke with ludstone interbeds (10-201) cba's 65*

2B3.2 286.5 Graded greywack bed. May up to SOUTH

286.5 292.0 Fine-grained greywacke with ludstone 8 286.7, 288-289 Rudstone clasts l 291.8 - 292, 290.4 cba's 50 -55'

292.0 292.3 carbonaceous sudstone

292.3 293.3 Altered light grey greywacke t 5X eudstone beds. Silicificate * carboante alteration widespread

293.2 293.4 black cabonaceous nudstone

293.4 297,0 Fine-grained greywacke with 15X .See Rudstone beds cba'5 55'

297.0 309.2 Dark grey fine-grained greywacke cba's 45'297.45 - 297.65 ludstone (qtz veined) cba's 60'

309.2 309.3 black ludstone cba 60'

309.3 310.9 Fine-grained greywacke with ludstone clasts

310.9 311.3 Graphitic audstone t Quartz veining cba's 50'

311.3 319.1 Fine-grained greywacke with li ludstone clasts cba's 50*

f

x

^c Minerals Ltd Geological and Assay Data

From To

Drill Hole s LV88-14 Project Proper!

i i Sanple

Remarks ! Nunber

319.1 319.9 As above with iOX tudstone clasts upto 5ci long, flattened in place of foliation

319.9 321.9 fine-grained greywacke with l - 6*1 abundant ludstone interbeds

321.9 322.3 Dark-grey, quartz veined nudstone

322.3 325.4 fine-grained greywacke with thinly lacinated ludstone bands

325.4 325.7 Quartz-veined ludstone cba's 55'


346.9 347.4 sheared conglomerate, heavily altered by carbonate sericite clasts total 807., strongly flattened. Matrix is nudstone. KB This is the lithology that in LVBB-11 carried 51 chalcopyrite mineralization, cba's 55'

347.4 349.7 medium-grained greywacke with congloierate f 346 - 34B.3

349.7 351.4 Heavily serialized altered congloierate cba's 60'

351,4 353.2 nediua-grained greywacke

353.2 355.6 Quartz-veined fine-grained greywacke with 20X cudstone laiinae

355.6 358.0 conglomerate with sudstone natrix. Heavy shearing and alteration cba's 65'. Spotted cabonate alteration

358.0 359.1 Graded greywacke with Rudstone clasts. 40X clasts at base, 101 at top Nay up to SOUTH 2 types of Rudstone: black graphitic and brown, fine-grained

Lac Minerals Ltd Drill Hole s LV88-14 Geological and Assay Data

!X Froa To Reiiarks

359.l 366.3 cediun-grained greywacke with IOX ludstone laiinae

366.3 368.6 Black tudstone with 207, fine-grained greywacke bands. Abundant IDM angle (5* - 10') quartz veins

368.8 367.3 medium-grained greywacke

369,3 369.7 black tudstone * quartz vein i 55' to axis

369.7 371,8 mediun grey greywacke

371.8 372.6 cabonaceous nudstone

372.6 375.0 medium-grained greywacke

375.0 375.4 Braphitic ludstone cba's 70'

377.8 382.1 Greywacke with IOX cabonaceous laiinae

382.1 382.3 Graphitic ludstone cba's 70'

382.3 383,4 fine-grained greywacke with ludstone clasts

383.4 385,3 sheared congloeeratecba's 65*. Sediientary clasts doiinant

385.3 385.6 graphitic mudstone

385.6 389,1 Sheared conglomerate with greywacke catrix. 801 flattened clasts. Clasts are felsic volcanics and sediients cba's 60'

389.1 389.7 greywacke

389.7 390.5 sheared congloserate

Lac Hinerals Ltd Geological and Assay Data

Drill Hole : LVBB-14

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IX From To Reiarks

cba's 45*Clasts total 60X in matrix supported greywacke. 1/3 of clasts aretan coloured sediments.


393.2 401.0 sheared conglonerate with St ludstone clasts. cba's 64' Majority of clasts are felsic volcanics

401.0 401.9 coarse greywacke

401.9 407.7 Sheared conglomerate with 75X clasts lade up of quartz, felsic volcanics and tan-coloured sediments. Large ludstone clasts concentrated at base of unit.

407.7 407.1 Braphitic ludstone with 5X felsic clasts.

409.1 415.7 sheared and chloritized congloierate cba's 60' Mineralization Pyrite 8 411.4

415.7 419.8 broken core, quartz-carbonaceous fault gouge

419.8 422.7 graphitic ludstone

422.7 423.5 fault gouge

423.5 430.0 Heavily sheared and altered congloierate with ludstone clasts I+ felsic * quartz).NB: Kudstone clasts are noted as lain leans of distinguishing conglomerates fron the NORTH close to the Keewatin unconforiity froi those to the SOUTH cabonate vein i 430' Mineralization: Pyrite t 429'

Hinerals Ltd Drill Hole : LVBB-14 Pr Geological and Assay Data Pr

'X From To RemarksSa Nu

430.0 444.0 sheared, altered lassive felsic volcanic cut by dark grey anastaiosing quartz veinlets. Sericite-clay alterations. Original rock type is very difficult to discern. Hay be felsic vole, or badly altered lafic volcanics

444.0 575.0 dark to light grey felsic volcanics, generally cassive with porphyritic sections 8 489 - 495Cut by randoily orientated dark grey/blue-grey l - 3n quartz veins 6 500 -509' O* - 3' quartz-carbonate vein, no visible Mineralizations 509 - 536.6 anastanosing carbonate stringers

536.6 - 537.6 Quartz carbonate vein 10* to axis

572.6 - 10* Quartz-carbonate vein with inclusions of country rock. No attendent tineralization also S 585 - 593.2

Mineralization:trace chalcopyrite 8 536.B

595.0 614.0 Porphyritic felsic volcanic. Hediui grey Hith 21 blue 'quartz eyes' in a cassive fine-grained *atrix

S 605 5* 2cn Mide Quartz vein

f 611 Quartz segregations t l - 3X dark green chlorite.

Unit had gradational boundary Hith Hedging unit

614.0 797.6 Heavily altered internediate volcanics. Hassive, light green to aediui grey. Sections quartz-veined along Hith calcite and dark green chlorite.

chlorite replaces aafics (crystals?) fi 645 - 646.4649 - 650.4659.8 - 664.7

Hinerals Ltd Drill Hole : LVBB-14 Pro; Geological and Assay Data Pro)

f ii Sai)

X From To Renarks ! Null

66? - 679.4

679.4 - 698.3 - heavy quartz - carbonate t chlorite veining. 60 - 70X of core is vein aaterial. Veins have inclusions of country rock.

Mineralization:very minor sporadic pyrite and rare chalcopyrite grains across section679.4 - 698.3. No other visible nineralization.

623.4 - 626 broken core - fault?628.3 - 628.6 Quartz vein 8 40'630.6 - 631.5 quartz carbonate - chlorite vein 6 35'

Mineralization trace chalcopyrite

636.2 - 637.3 Quartz - chlorite vein637.3 - 640 broken core - fault?640 - 640.5 quartz carbonate vein731.4 - Sen quartz vein t 10*

silicified section l 744 - 746

753.5 - 754.2 broken core758 - 761 siliceous section768.4 - 768.7 Quartz - carbonate - chlorite vein t 50'

Mineralization: Diner pyrite * Cp

776 - 780 Ion angle 5' quartz vein787 - 7B9 'bedding* (45') parallel quartz and ION angle (3*) quartz

veinsMineralization ainor pyrite

797 - 797.6 quartz - carbonate vein t 25'

Lac Minerals Ltd Drill Hole i LVB8-H Geological and Assay Data

l X From To Retarks

777.6 808.1 Altered basic volcanic, abundant epidote veinlets and patchy alteration

608.1 898.0 altered intermediate nassive volcanics Nith pervasive Quartz-carbonate alteration

Quartz - carbonate veins * BIZ - 812.7 l 55*BH.7 - 815,5 6 20* 824.4 - 825 8 15* 844.8 - 845.5 849 - 850.8852.8 - 853.2 - 2 greenstone of veins, older

blue-grey G 20', younger white t 45'

860.1 - 860.7 - t wall rock inclusions 857 - 857.2 - t 30' 864.2 - f 10' 867 - 868 - carbonate vein 870.7 - 881 -

868 - 878.4 heavy shearing and alteration (cabonate doiinated)

Mineralization minor pyrite t 863

846.5849 - 850.8860.2 - 860.5866.2 - 865868.3 - Pyrrhotite?867.6 trace chalcopyrite876.5 - B76.6 IX pyrite

B98.0 EOH

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Ontario

Name end Postal Addtess of Recorded Holder

LAC Minerals Ltd.

eh v). )rt fid

900

6 Al Wende Avenue, P.O. Box 670, KIRKLAND LAKE, Ontario P2N 3K1Summary of Work Performance and Distribution of CreditsTotal Work Days Or. claimed

3616for Performance of the following work. (Check one only)

Q Manual Work

Q Shaft Sinking Drifting or other Lateral Work.

Q Compressed Air, other Power driven or mechanical equip.

Q Power Stripping

JJ] Diamond or other Core drilling

Q Land Survey

All the work was performed on Mining Claim(i):L767470. L801174. L801134. and L801135

Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)Drill logs and loc

McKenzie Drilling P.O. Box 1054 WESTBANK, British VOH 2AO

Total Footage LV88-10 * LV88-11 (see attached shee Total Credits appl Credits Banked for

i

ii 'M 9 -J IMS:)r-

Certtficatian Merifytna Repw v v' 1 '' ^^ ,^n J. .P,®.r.Syy.SWtif y.xh*t-J J**ve-

or witnessed seme during an

ation sketch submitte

Ltd.

Columbia

•f LV88-12 * LV88-13 4- t for breakdown by ho ied = 5754 3 S 7?^ future use s 42--'

"" LARDER L A K iiM1MNO O'.V.

MAY 0 b19By ;AM 1 'Ô (^^f/

7 iSiS'Willi 1 ? 1 1|2^5 jî?. t ?

d with Report of Work.

Drill Hole Data: see attached sheet

LV88-14 - 3616 feet (3616 credits)i*\ ,,, .——i '

RECORDED

MAY 5 1989

nnnntnt t —

Dst* of Riaort R*rnrri^rl|W^lrUJ/ or Agont (pi ffr).tiirtl

May 3rd, 1989 1 /If )L^^)rtofWork r/ "personal and intimate knowledge of the facts set forth In the Report of Work annexed Kareto, heving performed the work

d/or efter Its completion and the ennexed report Is true. '

Name and Postal Address of Person CertifyingDavid Adamson, 6 Al Wende Avenue, P.O. ^r 1 1""- f^j tt f t, AJ-S f, Ot^cecmj îsS. -ffi a KL. jostKIRKLAND LAKE, Ontario P2N 3K1

Box 670 ft ...- p A 46 /fit &HST jiCKtt) \y^. **** 1 1 *— ~Oat* C*rtlfl*d CcrtlflwWw (Slgnajurc)

May 3rd, 1989 J^^^C^^"

ONTAf

AS)

Table of information/Attachments Required by the Mining RecorderType of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compretted air, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

Land Survey

Specific Information per type

Nil

Type of equipment

Type of equipment and amount expended. Note: Proof of actual cost mutt be submitted within 30 days of recording.

Signed core log ihowing; footage, diameter of core, number and angln of hole*.

Name and eddress of Ontario land turveyer.

Other Information (Common tqyZor more typei)z.\~

Namet end eddresses of men who performed manual work /operated equipment, together with date* end hours of employment.

Namet end addresses of owner or operator together with dates when drilling/strippingdone.

Nil

Attachments

Work Sketch: these are required to show the location and extant of work in relation to the nearest claim post.

Work Sketch (es above) In duplicate

Nil

768 (81/3T

DIAMOND DRILLING -Distribution of Credits

Total days claimed - 3616

Applied to:

100 days

60 days

54 days

20 days

L 799522 \L 799524^L 801129\L 801131^L 801144^L 801 146 AL 801148*L 801150 'L 801153 xL 801167^L 801175V

L 801133*L 801168L 801170L 801172 ^L 767701 v

L 799523^L 801128*L 801130VL 801132*L 801145VL 801147L 801149 VL 801151 1L 801166\L 801174*L 802384\

L 801134 *L 801169-L 801171^L 801173^

L 801135^

L 767405- L 767408' L 767416 L 767419

767427 767435

L 767438 L 767444 L 767447 L 767453. L 767456 L 767461- L 767464

L L

L 767406 L 767409 L 767417 L 767425 L 767428

767436 767439

L 767445 L 767451 L 767454 L 767457 L 767462 L 767465

L L

L 767407 L 767415 L 767418 L 767426 L 767429 L 767437 L 767443 L 767446 L 767452 L 767455 L 767460 L 767463 L 767466

Total - 3574 days .

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Documents

DIAMOND DRILLING TOWNSHIP: McVITTIE TWP, REPORT NO: 46 ... · tIMetalic Minerals; Magnetite and specularite are present and abundant throughout. Specularite is coiion on fracture