P, CARTER, P.ENG. — GEOLOGIST

ONTARIO L3J

The President and Directors Metalline Resources Inc. 432 -12 Richmond St. East Toronto, Ontario M5C INI

63.3357 STRATHY

RECEIVED

SUMMARY REPORT ON DIAMOND PRILUNB STRATHY TOWNSHIP PROPERTY. ONTARIO

010

A drilling program to cover the four separate anomalous horiaons recommended for drill testing on the Company's Strathy Township gold prospect in the Temagami area of Ontario was completed re cently. Four holes totalling 1206 feet were drilled, one hole in each target area. Fracture zones, formational contacts and sparse sulphide mineralization associated with quartz-carbonate veining in part were found to account for the EM geophysical conductors, All such sections were assayed but only trace values in gold were found.

Prill Results

Hole No. l was drilled to 300 feet to test the most westerly con ductor. A well fractured section from 201 to 216 feet is credited with developing the EM conductor.

Hole HO. 2, located 900 feet east of No, l, and directed to testing the second conductive horizon, intersected a 1Q foot fracture zone at 288 feet with hematitic(iron) staining that is the probable cause of the conductance in thai area.

Hole No. 31 was drilled 700 feet east of No. 2 to test a 600 foot length cpnductive zone. A fractured and brecciated zone with quarts and pyrite mineralization at 2?5 feet plus minor mineralization in the adjacent rock was the origin of the conductor in that aroa.

Hole No. 4 was drilled 600 feet to the southeast to test a short con ductor. Minor pyritic mineralization associated with weak brecciation and quartz carbonates was intersected from 251 to 282 feet and is. the probable cause of the weak conductor,

Summary

The drilling program Just completed demonstrates ,that the four conductors investigated in the northern part of the property must be considered to have little potential as centres of gold mineralization. In each hole conditions were found, namely shearing, sulphide mineralization and

,2

quarte veintng, that normally favour gold deposition, however, in light of the very low assay results the negative assessment must be accepted* No further work can be recommended op this, part of the property at this tiroe.

Geophysical data and geological information on other sectionB of the holdings are currently being studied and reassessed toward the recommendation of possible additional exploratory programs,

Submitted fry

October 17 i 1975 0. F. Carter,Consulting Geologist

HONE 7O5-647-6426 BOX 1*O POJ 1PO

127 LAKESHORE RD. NEW LISKEARD. ONT.

JACK G. WlLLARSMINING GEOLOGIST

PROFESSIONAL ENGINEER

Aug. 20,

President and Directors 1'eta.ilino Resource^: Inc.,).i3.0 - 3.? Richmond St. K. TCRCUTO, Ont.

D.n.H. Mo. ?f' - l vn.c drilled from 2772'U, V^'H at a ninur h?0 angl^ in n ^ 12 0 ?.^ direction !.o :!.nvor;1,'.5;.-ito an elecytrome'ietic coirluctor. Ilie dn;'',h of the holes w. a 30f)' and dacite and ar.de site rocl'.c vorc intcrsocted. At .^ d^pt of '.! 01' to 2] 6' a uell .f racl uroo1 section 'r;rr; ob,c;orvod end thin was the cr-.usR of tho cr/nducto.v rosi'-r-nso. Tiro s?.nj?los taken from lop 1 tc r/V -md l?), 1 to T r!0' bo t; i af;r:oyed trace ariountp of

l^no drill is cur.ront'hr ho:lni; mov^d to tho rd*-o cf n.D.H, No, ?i;' - 2 at 18 H, I.;; "I t.o'te^t, rmothar conductor.

Yovtrr,

DIAMOND DRILL LOQ4MNTV }^AJ4#Hg-^^OUjxQjSS.-^lEIlV

O. D, HOLRNO.. 75-1

I*AOK t

TIST

9CO*S,600'W of No. l Post

-300.5-

BY

SIZE ^

I'brissette P* D.

,M-0

'10*

i^if**'

1

t

to

10'

11(5'

300'

300'

MM**..

CASINO

nACUB Medium grained black rock, hard, with finegrained unite specks of fibrous Icokinc mineralspotted throughout ~ V leucoxehe, Soamod with quertwveinlots at 1&0 to tho coro axi^.From h6 ! to 1*7' irregular quar|#, vain with vugs.Prom 135. 3 ' to 135.7' black medium coined dioritedikelet.

i

ANKSSrns Very fine grained, 9JU&P green colouredrock with ghosty banding at zjfr to the core axisin some sections, no bausting seen in other section s aMinor epidote. Short 4)rffl^0.ated sectiOTiS - nothingout of the ordinarjrj^Bra^leanics. From 197' to 198'is ground core. ^̂ 'Prom 201 ! to 23 6 ! ^g^.1 fractured section with redhematite stain on the fracture pianosi Probably theoauso of tho conduotor.

SAMPLES : From 169*,- .I7ji1 Qiiortr.-carbonate veinletvriLtJi aeagolA^ed pyr.rhotit/3 and pyrite, Prom 17li^*'^4Bo' Quarto-carbonate ve Inletwith a^sociatec1 pyrrhotite spd p^-'t^.

END OF HOLE.

NO.

; 20lJi

3 2815

CbMfe LtNOTH

5.0 i

6,0 1

AbiAY ttEBULT

TRACK Au

trace M

SIGNED —

JACK 6. LLAHsr^. A SC,F. ENG.CONSULTING MINING OEOUOGIST

2772W, IT25N

300

PROFILE SECTION D. D. K 75-1LOOKING WEST

METALLINE RESOURCES INC.STRATHY TWP, ONT

CLAIM 3 67806900*9, 600'W OF NO l POST

SCALE l " - 40'

AUC a O, 1979 ILLAB3

E 709-647.0420 Box 1 6O POJ 1PO

127 LAKESHORE RD. NEW LISKEARD. ONT.

JACK G. WlLLARSMINING GEOLOGIST

PROFESSIONAL ENGINEER

AUG.

President and Directors Metalline Resources Inc. 1|3? - 12 Richmond St, JSe TORONTO, Ont.

GentlemenIteport

D.D.H. No. 75-2 was completed at a depth of J)6', It was located at 1785 VJ, liJlJ and drilled at a minus 1&0 angle in a N 200 W direction to test an electromagnetic conductor, The elontronw,r:netic response uas duo to a fraoturc zono at 288. ̂ to 2?8.5' in the core. This was sampled and arrayed traco ariotm'ts of cold over 1C 1 , Another s:itnplo VPS trUcen nt 01!. to 92' in the core vhich assayed trace amount,*) of 601(^ over l 1 .

D.D.H. No. TJ - 3 is located at 12W, 17^0N to an olectromapnetic conductor 600' long.

Yours truly,

itOPBHTY.

DIAMOND DRILL LOG

/JBSPJfflCBS-JDlG*.

O. D. HOUE NO. vs - 3

PAGE l

LOCATI

COLLAR: LAT. -

DEPT.-

15 K1678014 TEST

178? W

DEPTH OF HOLE ——

STARTED AUg., 23,^975

SurfaceBEARING.

DIP ————mlnue

-vCORE SIZE

Korisaette D. D,

TO DESCRIPTIONSAMPLE

NO.CORE

UENOTHASSAY

RESULT

127 l

027'

zir

21 J 1

306'

306'

CASE!*DACITS Medium green coloured rock, medium grained

with viiite feldspar mottles, intruded by sparse white quartz-carbonata stringers (^" t/idth and dorm) at various angles to tho core codr. From 91 ' to ?2' flow brecnia. SAMPLE i i'Von 91' - 92' Flow breccia vith p;Tite

cubes. Quartg-carbonate veinlets*

ANDKSlTiJ Irregularly grained rock, mostjy very Tina grained oliveno green colour td.th scattered pillov/ rims that are epidptiaed,

2816 1.0' trace

As above at 1(0* to 187 *From 28B*J?' to 298.0' is a fracture zona with staining on the fracturos ^iida ure at 300 to tho cor a axis. Probable cause of conductor, 8AMPLBS l At 288.^' - 293..^' As above.

At 293*5' - 289.^' As above.

END OF HOIJE.

28172818

5.0* trace Autrace Au

SIGNED.J At K G. WiLLARS, B. A. 8c., p. ENG.

CONSULTING MINING GEOLOGIST

—.* zo" w t"-N^1J

PROFILE SECTION d D H. 75-2BOOKING WEST

METALLINE RESOURCES INC.: STRATHY TWP, ONT

CLAIM 367804' 700'S, 600'E OF NO 4 PQST

SCALE l " ' 40'

A UP, 2T, If IS WILLARS

1C 7OB M7.*42e BOX 1*O POJ IPO

If 7 LAKEtHONK MD. NEW LISKEARD. ONT.

JACK G. WlLLARSMINING GEOLOGIST

PROFESSIONAL ENGINEER

Sept. 2.1975,

President and Wrectors Metalline Resources Inc.h32 " 12 Richmond St, TORONTO,

GentlemanI^cgress lieport

D.D.U. No, 7? f 3 was eit-ed at 12W, 17?ON and c|rllled at a minus 1&0 ancle Jn a N U0 E direction to a total depth of 300' vrhile investigating an electromagnetic conductor, A fracture zone was intersected at ?75* in the coro and this is considered the cnuse of the electromagnetic response.

Samples taken from 271'to 277* anrayed trace anountg of gold and from 2?!?' to 300' a3sayed trace amounts of Cold over 6.0' and 5*.O' respectively.

D.D.H. Ho. 7? - h i s spotted at 6tt, 13N to test n single line conductor. The drill In currently "bftire roovod to this location.

Yours truly,

DIAMOND DRILL. LOG O. D. HOLE MQ. l ? r 3

PACE l

fl TESTCOLLAR: LAT. ——— 1750 H

DEPT.. 12 W

DEPTH OF HOLE

STARTED AUg^

COMPLETED. j, t)

ELEV.. Surface•CARING

air-,M

minus ICORE SIZE

r ROM

0lo*

'

66*a.

Ih7*f

1

i, f

TO

ID*

66**

1W*

300*

300*

DESCRIPTION

CASINO

ANDjjSIQS light groen colour, medium soft rock irf-tli 8to 10 ft whi^e quartz-carbonate stringers. Sowa short breccia flections, probably of volcanic origin.

MCITiS FUne grained to medium grained mottled unitemineral in a light gvean rook. At 91* and 109* each,1" banded quartz-carboante vein at 800 to the'Ccroaxis.

ANDESUE AB above at K) 1 to 66*. Ground core from232 ' to 233S At 27^' a vuggy pink carbonate veijiT-Moh could be the cause of the conductor.SAMPLES t From 271' - 277' Sections of brecciation

•idth pyrite. Vug of carbonate with honatitstain.From 29?' - 300' fyrito cubes in andesite

END OP HOJJS,

t

SAMPLE NO.

20199

2820

CORE LENGTH

6,0*

5.0*

ASSAYRESULT

trace, Au

Trace Au

SIGNED-'JACK G. WILUARS, s. A. se., P. EN.B.

CONSULTING MINING'GEOLOGIST

' l ' .lr .1"

500

PRQFILE SECTION a a H. 75-3LOOKING WCIT A

METALLINE RESOURCES INC.STRATHY TWR, ONT

CLAIM 367B04 SSO'S, 4*0'i OF NO l POST

SCALE- l " i 40'

SEPT Z, 1978 J G IHLLAUt

PM0NC 70S 647-6426 fcOX 16O POJ 1PO

187 LAKCCMOR.E HONEW LISKEARD. ONT.

JACK G. WILUARSMINING GEOLOGIST

PROFESSIONAL ENGINEER

Sept.

President and Directors Metalline Resources T-nc, Ii32 m 12 Richmond St. 13. TCBOHTO, Ont.

Gentlemqn *

Progress . Rapcrt'

D.D.H. No. 7^ - li was drilled in a N 30 B direction ut minus 15? from 6tf,13N to a total depth of 300'. The electromagnetic conductor tested was the contact between andesite and amygdaloidal andesite rocks. Samples taken from 2^1' to 2i?6' assayed trace amcunts of gold over Jj', from 2?1|' to 279' assayed, trace amounts of gold over I?', and from 279* to 282' aarsayed traco nmounts of ?rold over 3'.

The diamond drilling procrara has baen d3.scontlnuod for iho present*

' Yours truly,

DIAMOND DRILL LOG D. O. HOLE NO.. - li

'3TAM3 as? 3Mg, PAGE l

COLLAR: LAT. .

QfPT..

IVp^Ontt C] 13 K

TEST DEPTH OF HOUE•nnt

6 WSept,

"Surface H 30 B 1000'S, 200'K of Ho, l j post

Olf minus

PRILLED BY

CORE SIZE -

Morissetbe

TO OEBCRIPTION • AMPI.C NO.

coneLENGTH

ASSAYRESULT

O

22'22*

187*

187 300*

300*

(USING

AND33IIB Fine grained to medium grained, medium soft* olive green coloured rook, in part massive, in part banded and in part containing irregular white quartz- carbonate seams and stringers. Some ghort fine grainei epidotijed sections. From 1|2' to 1|2.8' pyrite in rusty vugs.

AMTODAtOIDAl AN])BSITlS Much the nama as above nt 22'* 18?' and containins shorl, sections of irregular shaped amygdulee of feldspar. From 237* to 2^6' is 15^ irregular whito quarts-carbonate stringers. From 256' to 277' is 8^5 quartn-carbonate-feldspar veinlxtts.

From 251'-258' I^nor pyrite in incipiently brecciated section containing quarts . oarbonato.From 27I4 1 - 279' Klnor pyrite and chalcopyr -ite in quarts-carbonate in any^dploidal andesite.From 279' - 282' I-'dnor pyrite and chalco pyrite.

KND OF HOlfi.

2821

2822

2023

5.01

5,0'

3,0*

trace Aa

fraoo Aa

trace Aa

•IONEO —k. *C., C. f HO.

CONSULTING MINING CCOUDCIIT

PROFILE SECTION D. O H. 75-4LOOKING WEST

METALLINE RESOURCES INC.STRATHY TWP. ONT

CLAIM 367803

1000'S, 200' E OF NO 4 POST SCALE' l "* 40'

SEPT 8, 1 91* J. 0. WILLAH1

. F^ CARTER, P.ENQ, r- csnoLOGiST' f '', ^

ONTARIO' WT- " ' -' '. ., ,

The President, end Directors.

A'32"- 12 Richmond Sb, East Toronto, '-Ontario M5C INI

- ' t4lfi.3fiJ.01ll

A y, , . , ' ''; ^;.' l)o h T V e - ^ -.V 1 '' "•••'•'. v' ;''"'' ' ' '' ' ; ' '

SUMMARY REPOOT ON DIAMOND DRILLINS PROGRAMS SrSTRATHY TOWNSHIP PROPERTY. ONTARIO ,, ; . , .

, . , . . l

A drilling program to cover the four separate anomaloushorizons ;'recommended for drill testing on the Company's Strathy,Township ' : gold prospect in the Temagami area of Ontario was completed re- 1 ''; cently. Four holes totalling 1206 feet were drilled, one hole Ir*; each target area. Fracture zones, formational contacts and sparse sulphide mineralization associated with quartz-carbonate veiling . in part were found to account for the "EM geophysical, conductors f ;, All such sections were assayed but only trace values in gold'were 1 .found. ., '.' i .'-.-'. '', * . -.' V'.:;: ' - - '. : '',:- '-\-- v'.. .vt

;'.;V Hole No. l was drilled to 300 feet to test the most westerly . . , ' \ductor. A wel}. fractured section from 201 to 216 f eet is credited ',

developing the EM conductor. '' -'; , ' ' , ! ."' ' ;' ' v ;

i .

•Hole No. 2, located 900 feet east o? No, l, and'directed to testing , f, ;, v the second conductive horizon, intersected a 10 foot fracture zone y'y y y; '

1 ,At 288 feet with hematitic(iron) staining that is the probable '-- ; cause of;the conductance in that .area. ; '.'. -- , '/y.". ' ^ y'':': : " '- ; ' ,".' 'H . . -. . . '. :, 'i-••.'.-•' - , , v-''---'^:'.^y'-y^'y^'-^y^v :-Hole No. 3r was drilled TOO feet east of No, '2'to'-'test 1 a."60ti'ffaott'|;'^H;'.';,y:;', .; i ;'

, ^ength conductive zone, A'fractured and brecciated zone with quar|ia;';;''and pyrite mineralization at 275 feet plus minor mineralization inv '.,',( ;";'

, the adjacent rock was the origin of the conductor in;that area. :fi y ! ^'\ ' : '

HolQ No, 4 was drilled 600 f eet to. the southeast to test a short cort"', ' ductor. Minor pyritic mineralization associated with weak brecciation; and quartz carbonates was intersected from 251 to 282, f eet and'is the V'AV'- ,

..probable cause of the weak conductor. ,. , ' ' .v:- .-,. :\-^, :̂ .,.',',:: ; " y ̂..y^;'''"

Summary ',, ', - . ' /'' ' ... ' ' 1 . .'''...- ,,'' ; , : y ' ; ''''.''V/'i " -" y ' ^^•'f;'^^f.^r\--'^^'';' -^'' "

The drilling program Just completed demonstrates\th9t the four conductors ' investigated in the northern part of the property must be considered to . y '

.' have little potential as centres of gold mineralization. In each hole '; : conditions were found, namely shearing, 1 sulphide mineralization and ;y, , ^ y

'^••':^^^!^^'-^'.•'y: ^^^-^^y'':\ ; y

1 ' '- *' *' * ^j' * .^ ' \' ' . ' -' '" -. i',

' f

quartz veijilng, that normally favour gold deposition, however,, in light of the very low assay results the negative assessment must be accepted. No further work can be recommended on this part of the property at this time.

Geophysical data and geological information on other sections of the holdings are currently being studied and reassessed toward the recommendation of possible additional exploratory programs.

October 17,

Submitted by

L^JU^T0. P, Carter, P,Big. , Consulting Geologist f

:;.;v vv.M-stW.'

"' Uox l GO PuJ l i-o NEW LISKEARD, ONT.

G. VVILLARSMINING GEOLOGIST

PROFESSIONAL ENGINEER

President and Directors net'illino Kesourcor Inc. ?;3'5 - l- Richmond St. w. TORONTO, Ont.

AUG. 20,197?

D.D.H, llo, 75 - 3. w. s rtrllleri from 2772 'W, 1722 'li at a minus )|S0 ando in n S 12 D W direction to inver: tigiifce an olectronuifnetic conductor. The depth of tho hole TO. D 300' ?jid dacite and andorite rocks -s-oro intorsocted. At a depth of 201' to 2] 6' a ufill fr^cturori rnction WP.S ol; served and this was tlie cnuse of tho conductor response?. Tv?o samples takon .from lo? 1 to n?!i' and vfl, ' to iBo"1 both nsnayed trace amounts of gold on3.y.

The drill is' currently heinp; movod to tho nit^ of H. D. H. No. 7 CJ - 2 at 18 IT, i;-: H Ko Lest nnothor condiici-or.

Yours truly,

\ *V"

TEST

900'S,600'W of No. l Post

OK

bRILLfeD B'

BIS! E

BIP

FROM

0

10'

!

i 1 ' -

i

t ' . 'i

i i

i

|

i.j i'J -'

l "; '

; ' '

'

. . -

!

i ; 'f '

1

t

f C*

10'

111'.'

.300'

•4

300'

^.mni.N

CASINOnAGITE Medium grained black rod:, hard, i/ith fine

grained vjhite specks of fibrous looking mlner.oll.potted tliro^xghout - ? leucoxehe, Soonod T.ri.th quortaveinlets at Ii50 to thn corn axis.From lj.6' to h? 1 irregular quart? vein vri.th vugs.From 135.3' to 135*7" black, medium grained dioritedikelet, . ,

ANDESITE Very fine grained, olive green colouredrock \d.th ghosty bonding at 1;50 to the core axisin some sections, no banding seen in other .sections.Minor epidote. Short brecciated sections - nothingout of the ordinary for volcanics. From 197 ' to 198'

' is ground core,From 201' to 21.6' Well fractured section nith rod

' hematite stain on the fracture planes. Probably thecause of the conductor.

'i ! 'SAMPLtS : From 1694 - 17lt f Quarto-carbonate veinlet

i/ith associated pyrrhotite and pyrite.From 17U 1 - lOO 1 Quarta-carbonate ve inletwith associated pyrrhotite and p;.Tltr).

. "'

END OF HOLE. ' '

' -' ' ' '' ' :' - . ' -" . " '''

; ' ; 1

' ' ' : i - ' , ' '\

1 J J

' " ' t 'i 1 1

•- : ' ' i ,

NO,

.

' . '

5 20^4

3 281^

't

:.

UfcNUTM

5.0'6.0'

S4

•' '.

t

'.•V'""

AB8AV

. '

TRAC* ..

trace A

"

• IQNID^. A. 1C., P. CHO.

CONSULTING MINING GEOLOGIST

*fROflLE SECTION D, D, K 75-1LOOKING WEST '

•f- METALLINE RESOURCES INC.STRATHY TWR, ONT.

CLAIM 367806 900'S, 600'W OF MO. l POST

SCALE ' l " - 40'

AUC 20, 1 979 J. G WILLANS

16O K)J 1PO127 LAKSSHOHE RO.

NEW LISKEARD, ONT

JACK G. WrLLARsMINING GEOLOGIST

PROFESSIONAL ENGINEER

Auc. 87,1975.'

President and Directors Metalline Resources Inc, U3? - 12 Ricbnond St. tt. TORONTO, Ont.

Gentlemen^Progress Keport

D.D.II, No. 7? - 2 was completed at a depth of .306', It, was located at 1?8? W, 1?N and drilled at a minus U?Q angle in a N 200 W direction to test an eleotromacnetic

. conductor. Tile electromagnetic response was duo to afracture zone at 288.?' to 290.?' in the core. This

1 '-Has,sampled and afsayod trace anounts of gold over 10', v' Another sample was taken at 91,!, to 92' in the core

assayed trace amounts of coW, over l 1 .

D.D.H, No, 75 - 3 is located at 12V!, 17&N to test an electrornagnetic conductor 600 |- lon2.

Youra truly,

U, U. U, HOLE NO.. - g

PAGE l

UOCATIC

COLUAHl L.AT,

BCARINQ.

DIP —————

TESTN . 1765 w

: Surface

DEPTH OF HOLE —

STARTED Allg,

fQMPLPTpn A\

pvEX 26,1975

Horissette D. D*

"mnus

' FROM TO DESCRIPTION SAMPUE NO.

CORE LENGTH

ASSAYBtSUUT

fcO'

1?7 !

aa?

306'

306'

CASTJO

Medium green coloured rock, medium grained with I'jhite feldspar mottles, intruded by sparse white quartz-carbonate stringers (i" width and down) at various angles to the core axis. Prom 91' to 92' flow brecnia. - SAttPLK i From 91' - 92' How breccia with pyrite

. - cubesa Quarts-carbonate veinlots.

ANDifiXTK Irregularly grained rock, mostjy very fins grained oilvene green colour with scattered pillow rims that ( are tepidotized, . ,.

2816 1.0' trace

DACrCfi As above at Ip' to 127* .From 288.5' to 298.5'-is a fracture sohe vdth hematitsptaining on the fractures which sre at 300 to the coraaxis. Probable cause of conductor..SAMPLES t.AJ^ 288.5' - 293*5 r As above.

At 293*5' - 289.5 f Ae above.

END CF HOLE.

28172818

5.0' trace Au trace Au

SIGNED —

lJSfcK. 7 - G. WILLARS, B, A. CC..P. ENG.

CONSUUTINC MININ^ OEOUOGIIT

PROFILE SECTION DON.. 75-2LOOKING WEST V

METALLINE RESOURCES INC.1 STRATHY TWP, QNT

CLAIM 3678O4 700'S, 600'E OF NO, 4 POST ,

SCALE ' l. 40'

AUG. 27, 1*78 G. WILLARS

o-^t- .--~. 127 LAKE8HORC NO. BOX 1 80 POJ 1PO NEW LISKEARD. ONT.

JACK G. WlLLARS

t Sept.

MINING GEOLOGIST PROFE6SIONAU ENGINEER

President and Directors ' -Metalline Resources Inc.

- 12 Richmond St, is,

Gentlemen J .IVo^rosn Report i,

D.D.H. No. 75 - 3 wag sited at 12W, 17^0N and drilled nt a minus 1&0 ancle 3ji a N if E direction to ft total depth of 300* while investigating an electromagnstiq '

. ' Qonduptor. A fracture Bone was intersected at 275' in -' the core and this is considered the cause of the .

. ' .electromagnetic response* , ' . * .1 ..'. , , - ' ' ' - ' - , ' ! i *

; . Samples taken from 271'to 277' assayed trace nmountsof gold and from 295' to 300' assayed trace ajnounts of

' cold over 6.0 1 . and,5oO' re^ectively,

^•.••.,-.DtD.H. Ho. 75 ~ k is spotted at 6W, 13N to tost n single Una conductor. The drill is currently boing moved to this location, , ' ; ^ .

' '

Yours truly,, ' V W

D. O. MOLE Ma. ^ "3

LOCATioN^B^ailur.COLLAR! LAT. ,

OEPT,

TEST DEPTH OF H 0t.fi

STARTED

PAGE 1

0I

12- 28,1975.

ELEV..

BEARING,——————H li0 ^'

DIP —————— mftnus li!?DRILLED

CORE

J)ogliSsatte

TO DESCRIPTION

CASINGSAMPLE

NO.cone

LENGTHASCAV

RESULT

10'

66*

300*

300'

groen colour, medium soft roclc with 8 to 10 # wjii^e quartz-carbonato stri.ncers. Some jjhort breccia sei^ions, probably of volcanic origin.

Fine grained to medium erained mottled unite mineral in a light green rock. At ?l f and 109' each, l" banded quartz-carboante vein at 800 to the - core axis. ,.

Acf above at 10' to ^6'. Oround con? from 232* to 233* * At 27^' a vuggy pink carbonate vein iThich could be the cause of the conductor. SAMPIES'i Prom 271 ' - 277' Sections of brecciation

•with pyrite. Vug of carbonate -with hematita stain. '

; Prom 295' - 300' I^rite cubes in andesite

2019

• 2820

END OP

6.0' trace Au

Trace Au

SIONIDOACK G. WILLARS, *. A. *c.. P

CONELILTINC MINING CEOUOQIST

-~-- . SWAMP

ac oS23 x ^ *t

; SURFACE

OVERBURDEf* ^ . *~

PROFILE SECTION Q'Oi H. ; 75-3LOpKINfi WEST ^ ,

METALLINE RESOURCES INC.STRATHY TWR, ONT.

- CLAIM 367804 j 550*8, 4BO'E. OF ^0. l POST

•;; : •.;.' ; ' ;'';. . j; SCALE' i " * 40', | ! ' ; - -'

SC PT. Z , 1 975 J. 6. WILtARS

, BOX 16O POJ H'U127 LAKEbHOHt HU.

NEW LISKEARD, ?ONT.

JACK G. WlLUARSMINING GEOLOGIST

PROFESSIONAL ENGINEER

Sept.

President and Directors Itetalline Bosources Inc, l-,32 - 13 Richmond St. 3. .

. TORONTO, Ont.

Gentleman t

s, Jfessxvrt

' n.D.fU No, 75 - li was drilled in a N 30 K direction fitminus l*!?0 from 6V?,13N to a total depth of 300', The

'electromagnetic conductor tested was the ccnt?.ct between andesite and amygdaloidal andesite rookst Samples taken from 201' to 2j?6' assayed trace amounts of gold over 5S from 27li' to 279' assayed trace amounts of cold over 5 *j and from 27P ! to 282' aanayed .trace amounts of gold over 3'. . , - - ', ' ' -. . :'- , .

diamond driD.ling procram has been discontinued for ' the present* ' \ , ' - ' , t . . "'

Yours truly,

J. O. Vail ara

, n. HOUE MQ "

'ETAU-TOS TKC, PAGE l

TEST DEPTH Of HOLE

COLLAR: LAT.

OEPT.

Septf 2j

SurfaceSetf h

1000'S, 200'tf of No. } \ postminus

FROM TO DESCRIPTION SAMPLE NO.

CORELENGTH

ASSAYRESULT

O22'

22'

300*

300*

CASINO

ANHuSITB Fine grained to medium grained, medium soft, olive groen coloured rock, in part massive, in part banded and in part containing irregular \jhite quar^z- carbonate seama and stringers. Some short fine graim epidotized sections. From 1,2' to 1^2.8' pyrite in rusty vugs.

AMXGDALOIQAJ/ ANJESITK ^di the same as above at 22'- l87' and containing short sectionfi of irregular shaped amygdules of feldspar. From 237' to 2J?6' la 15tf* irregular white quarts-carbonate stringers. From 2f?6' to 277' is 8# quart^-carbonate-.feldspar veinleta,

SAMPUSS i From 2^1'-2^8* Hlnor pyrite in incipiently brecciated section containing quartz -* carbonate, — -

, From 271* 1 - 279* Minor pyrite and chaloopyr -ite in quarte-carbonate in arycdnloidai

; . andesite, . . , ., From 279' - 282' J&nor pyrite and c^ialco-r

" ' . ; ' ' ' •,:' pyri'to*'. , : . '". . . '.''. ;.' ..' .

OP HOTJE. , , ""

2821

2822

2823

5.0 f

3.0 f

trace An

frace Au

trace Au

*IQNED-r

tCONSULTING MINING GEOLOGIST

i

PROFILE SECTION D, D H. v75-4LOOKING WE3T ' \

METALLINE RESOURCES INC,' STRATHY TWP, ONT

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