claim n9 hotono footage€¦ · e lev at 1c' from 0.0 1 t? .0 1 to tf.o. **7 - *? | t* . fi...
TRANSCRIPT
ssoeeseeiee saoeesEecu KAWASHE LAKE 010
Diamond Drilling
Area of KAWASHE LAKE Report W 18
Work performed by: Cochenour Willans Gold Mines Ltd.
Claim N9
PA 280875
HotoNOB-30-70-6
B-30-70-7
B-30-79-9
B-30-70-10
B-30-71-13
B-30-71-1U
B-30-71-15
B-30-71-16
Footage101.0
103.0
103.0
102.0
101.0
131.0
175.0
133.0
DataAug/70
Aug/70
Aug/70
Aug/70
July/71
July/71
July/71
July/71
Note(D
(D
(D
(D
(D
(D
(D
(D
TV TV* L-.
Notes: (i) From cancelled files for mining claims;Lands Administration Branch, Patricia Mining Division. Assessment Credits - #22-1974
t 005{7-69)rav.9-T2
CasingMafic meta volcanics: fine to med. grained dark green mod.to highly amph'd S chlor'd, massive, occasional fracturesfilled with qtz-ncarb.
27.5 39.6 Tuffaceous greywacke; fine to med. grained, finely, wellbanded coarse banding of fine grained dark grey tuff, grey wacke S lighter grey tuff greywacke with med. grainedfrag. S qtz. feldspar xtals, coarse bands way from a fraction of aninch to approximately a foot in thickness, banding at 55" toC.A.29.0-30.0 LOST CORE40.0-40.6 LOST CORE
39.6 55.0 Mafic meta volcanics: med. to dark green, med. grained, shearbanded at approx. 55 to C.A., amph'd chlor'd, somesegregation of mineralis giving slightly mottled appearanceS-10% blue qtz eyes, occ. qtz-carb. strgs.54.0-55.0 highly sheared S, altered
55.0 55.4 Massive sulfides. 401 cpy, 401 Po 201 inclusions55.0-55.2 ground core recovery of some broden core- similarto core described above. Sharp conformable lower contact withtuff greywacke at 60 0 to C.A.
55.4 101.0 Greywacke- tuff- dark grey, finely well banded at 55" to C.A.occasional coarser section with tiny feldspar 6 qtz ztals.generally uniform tecture.59.5-60.1 lost core62.2-63.0 lost core
DUPLICATE COPYPOOR QUALITY OR1G1UAL
TO FOLLOW
•y-^ygygaife^^.^ Q^ COCHEKOUR WILLANS-SELCO - LAKAJX TH sfe^swesifaeiSfBSs s****!
LO C ATI- C C ^Sv?'^CORE Si, PE LEV AT 1C'FROM
0.01 T? .0
1TOTf.O.
**7 - *? | T* . fi
•'
3?. 6r
t
' 55.0
li
' 55.4
:
i
55.0
55.4.
101.0
C- Ffir R \Xrf it-o T*
*m
T^rn'/.nF.^. Cni1) .^O - Lyj Ltdrv'.rS3 icTA^P D 17/8/70 llrj^lV^WFD 18/C/708 E A S INC Grid KLATrrHDE31CC*3O L O G 1 C A Ln*
r Vctft Votc.-Ptci!^Mr. -T-^t,? T, rt
or* tHtTi ot^-errb.Tnff,-c"pnn "rfv-Tnclrr- -
b ' *\Ti t
v/i ei:
D' p -/3 DcPTSOl.C* r--; V LOGGED PY I.. C. Chant!. orpocRTURF L-GOCO U
P F S C R 1 PT lOM -
-f in e to r ? d . crn I n/* d , d n ri; r,r LC on , rod.Ll-r'd, r.-n^lvo, ocr.nnionftl fr,-rt"r**s
fine to rrrt. rralrod. f^r*^T". w**ll
cd t coarse banding of fine rraincd dark TTCT tuff. rrcT-—o r, *4.^rl.^ HrT,r,
rv.~cT. r* of-~ ^ •foid'ST-r
C. A.
, r -r~v ^,ff pro'v.-rV*. ^ th r— rf ^-nlni-rf
IT- Xt.it*, oonr-np hcnds vny fror? a fraction* ^ i ^ rt i "i O L ni^f'^^'mt ^ *^ri ^ fi l Tl ^ ST. t S T * rt
i
20.O-30.O - LOST CORE/Q.O^/n.fi - LOST CORE
K.-.fic Keta Volcanics*.,T**^ -f n^T-T-O^ *1
SAM Pt F ^N'O.
of nn
: red. to dark p.rccn, red. grained, shear 1to C. A., act-h*^. cl*Xortf?. sor*e
ac^rcration of clncralis i^ivinc slirhtly mottled appearance5-10^ blue qts eycr.54.0 - 5^5.0 - highlyKassivc Sulfides, 40'
occ. otz-carb str/js.sheared tf altered
H Cpy, 40^ Po, 20^ inclusions55.0-55.2 - rround core — rccorcry of some broken core - slnil.to core described aborc. Sharp conformable lover contact vithtuff ^reyvacke at 60O to C. A.GrcTvacke - tuff - dark rrcy, finely veil banded at 55 to C. A.ccccsioaal coarser section vith tiny feldspar t/ qtz Xtals,generally unifona texture.59.5-60.1 - Lost Core62.2-63.0 - Lost Core
FROM
ir
TO
x^
A,"^
W 1 DTH
. C-^ *^——r- —————
-iCLE NO. 'T-lC-TC-r,D AT F 21/.-/7CASSAYS
i
t- f
UJ E
^ i K 1 C iAINING DIV.
•^"^Wjh*^*
^
'.i !e !! v 'v || ||JU Ptio 27197t4 "^AM
1 ^^ - ' 0 ,f '
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x^ /.v.- ^S,-..:
jj7 f
1 x
FW. M. J 1
———
1r~ T,
•••••••••••••••••••••••^••••••••••^•••••••••1tj^^^v?^:--"^
lA^lMJi^^J^-RH't^l:^^^/^^:!^/'^'''' ^COCHENOUR WILLANS -'Sl^CO'^BKMfi
LoofiTlOJvlV
(Loee s i -z EEl-EVAT/ml-
- : - " "" . : ' ' 1 - - - '
rOrtft 1 VrV
0.0 7.0 7.0 41.0
:y ^ DRUM LAKE AREA,- GRID 30 J.EDWARDS
; ' XRP "BERfclfJQ GRID N
LflTVTUOE. "2700 'S
DIP -65 -bEPTJi 103 - 0sroerEO 19/8/70U
TVrPQl?Tl }pC" L— 8000 W
VFcMiSHcD 20/8/70
L.C.CHASTKO tflSS^5OBV:
^P^PlPT\00Casing Mafic meta volcanics, fine to med. grained, amph'd green
^Af^PLK
MD Vttom TA
-"W,
VioLE Mo- B-30-70-7^Orr 21/8/70
^JU^ ** 1 Cf
fiS^AMSLO/jJrtU
highly amphibolitized, amph. xtals up to 5 mm., moderately fractured, 10% qtz-carb strgs., massive to sheared fi foliated at approx. 45 0
41.0 59.2 Greywacke-Tuff - alternate bands of fine grained dark greyfinely banded greywacke S mottled grey, fine grained greyish brown matrix with medium grained xtals feldspar 6 felsic frags approx. l mm, in diameter, coarse banding varies from inches to a foot, occ. qtz-carb strgs, banding at 40-45 0 to C,A,
59.2 80.0 Mafic meta volcanics; med. grained, mottled green, highlyamph'd, shear banded at 40-45 0 frequent x fractures 15% qtz- carb-tour stringers, Tr. Po Py, fine qtz eyes in mafics last 2 feet, have a very finely banded appearance possibly a mafic tuff- poss. whole section is a mafic tuff.
80.0 80.9 Massive sulfides; 80.0-80.1 - 80% Po, l-3% Cpy80.1-80.9 - 70% Py, l-3% Cpy, Tr. ZnS, lS-20% inclusions, section is broken S crushed.
80.9 103.0 Tuff - greywacke - similar to before.
103.0 FOOT OF HOLE,
SSUCATE COPY
DIAMOND DP ILL HOU 1.OG COCHEKOPR VII.LAKS-SEI.CO~ BAMAJI PROJECTLOG AT ION- PP.t-M
CORE SIZE ynpELEVATIONFROM
0 0
7. Cr
41 .O
^9.2
eo.o
eo.oji
TO G E7.0
-SI. CI
*Q.?
PO.O
F0.9
103.0
103-0
P,^,
v-fiM -'i
^,.^
LflFB ARrtA-r CHIT) 1
L ATI TUDE o~rrtr
O L O G 1 C A L* rf
f j,^.. Tr 0 1 r .nMr*
7r nr,^iT, 0Tt*t-!^
O ""' -'
DIP -C.-5
CFPAPTIIRPD
fi*** tro r. srph. rt
jijKIlJLcD feT lU^JLt-- , , , lU^.li. .-r^. . .1 J. T.d— •^fT*- !CTAf?TPni -. lo/P/Tf! IciNlCWFO 2C/P/70DEPTHin^^ H V LOGGED BY L. C. CbastTco
T-Rr.nn wF S C R 1 PT 1 0 M
p*?. Tainciif n7nTTi'o r prp'innlr* TIP to 5 IMS., rodcrntcl-rr ,,^^^ i-o ^i^ni-P*! F/ foU.^f*.^
f- - /x0Grcy-^cVe-Tnf f - alternate bands of fine trained dark irrcr
finclv banded rrcwracke & mottled ^rey, fine /trained Tcvishbrown r.atrix^vith ccdiac rrained Xtals feldspar tt felsic fra^saprrOT - ^ rn ' in^diaT?ctcr. coarse banding varies fron inches tca foot. occ. ots-ccrb strns bnndin*c at 40-450 to C. A.Knfi c ?'.eta Volcanics!
*(?. shear banded
Ned. grained, cottled green, highlyat 40-450
cr.rb-totir s±r^x strinners, Tr.freqncn^t X fractures 15/C qtz-Po Py, fine qtz eves in rafics 1
2 fe^t. hare a. verr flnclr banded ftprcrance -possibly a nafictuff - ross, whole section is aHasr.ive Sulfidest 80.0-80.1 -
cafic tuff802 Po, 1C 1-32 Cpy
CC.l-eo.9 - 702 Fy, 1-32 Cpy, Tr. ZnS, 15-202 inclusions,section is brolten ff crushed.Tuff - greyvackc — sicilar to before.FOOT OF HOLE,
.
:,,. :,.,:,v:;;-- ^', -*^^,^
5 A M P 1 F ^MO.
ast
FROM
i
,-:^
TO
1
,v:^, .
W 1 DTH
f
^ ~~~
-iCLE NO. n-30-70-7
D AT F 21/S/70ASSAYS
t
f . J~;• ——— MM ^
1
11 1
i
Xl
1 ^7
/'
"'.'"/^r"8"""
.--r-.- r
l
(ffl'ffilU^ilSI^
(OfvI V 'r-^KJK : 'il^'-'-'KB^-f^GTSj^^^^^:-:^;.-^' :J. EDWARDS v i?SUn 23/8/70 24/8/70 - B-30-70-9
EX
0.0 9.0
27.0
29.8
2750siU 'i
103.0, Ji. V
L-8200 W
KV: C . CHASTKO j^ 25/8/70
9.0 Casing , 27.0 Tuff; coarse ash - to fine Lappilli 50-60** felsics, 40% amph-
chlor., mottled greenish S grey appearance. Diss. blebs Po Py,occ. speck Cpy, overall 2%.25.5-26.5 poss. fault zone, carb-qtz. strg. walls bio'd Sfoliated at 40 0 to C.A.
29.8 Tuff-fragmental - fine Lappilli SO-60% felsics, 20-30% maficsflecks generally biotitic giving rise to a mottled greyish Zbrown appearance, foliation at SO-55% to ea.
78.2 Tuff - Greywacke, fine ash - greenish to greenish grey, finelywell bedded, chloritic S biotitic, foliation S. bedding 45-50 0 toc.a. Grades into a greyish brown tuff- greywacke at 34.0 similarto before coarse banding of fine grained biotitic tuffS coarse grained fragmentals - gradation generally is fromcoarse to fine grained from top to bottom of hole.52.0-52.8 - l" qtz-carb - lost core - l inch qtz carb53.5-54.0 - Lost core55.0-53.9 Qtz carb strgs.60.0-60.6 Lost core66.6-67.0 Lost core
78.2 103.0 Tuff-fragmental - coarse ash to fine Lappilli, generally felsicash S Lappilli in a mafic amph - chlor matrix giving a mottledgreenish appearance, generaly decrease in fragments Si fragmentalsize with depth.78.2-78.4 contact between mafic tuff fragments Si greywacke
V tuff - carb'd fine stringers Po with minor Py S traces Cpy,conductive, overall S-10% sulfides.
'.COPY
TO FOLLOW
DIAMOND OPILL HOLE LOG COCriEKOl; ILLANS-SELCO - BA*LOG AT 4-O-fsj - - T^ipvCORE SlZErrELEVATIONFROM
0.0
Q .O
27.0
or p
i J
79.2
TOe.o
29.8
t
7P.7
-i-
103.0
G EO-MTTuff
C*CCL -
TAFF i rr t CTJTTv
SFARING Crir! \'
•*0 --w JUKILUE
DIP -45 IDEPTH1C3.Ci AT i TUDE 5?s^s IDFPARTURF 1-8200 w0 L 0 G l C A L D F S C R t
r^^Vrfa ~? !cfAfefrF TH lv
P T f 0 M
) i-V^/70 - 1LOGGED BY
-
: Coarse ash - to fine La^pilli 50-603 felsics, 40 1? ar.ph.-f*^ r '-a±±l^(! T**f*h i,h p. ^ r ** 3r,T,*.ir^cft.
* wcck C'fi'r^ overall 2#.
25.?-2*5^5 - rosa., fr.nlt son*, cp.rb-ots.strfoliated tt 400 to C. A.
Dlss. blebs To
j^jfalls Mo f d f Cr
TT,
T-aff-frarrcntnl - fine Latirilli 50-60^ fclsics, 20-30? caficsfi cclL- ir f^rternllr biotitic civin'r rise to ahrovn XJJTSnrX arpe?r*rs
r.ottlcd pre^isb Irco. foliation at 50-55 to C. A.
Tvff — Cr**vv?irf:c . fine PS^I"— "recnish to ^rccnish *rcv. finolvveil'C. fi.
bedded, chloritic Cr bidtitic, foliation J/ bedding 45-S00toGrades into a prcyish brown tuff-greyvacke at 34.0 sinila
to before coarse banding of fine grained kita biotitic tufftf CO
c on r
S ANO.
rl
-"•e grained frar^oentals - gradation r.cnerallr is froo-2 to fine trained froia top to botton of hole.
52.C-52.8 - ln qtz-carb - lost core - 1 inch qt* carb53.5-54.0 — Lost core55.0 -S3. 9 - Qtz carb strgs.60.0-C0.6 - Lost core66.6-G7.0 - Lost core "*.-..-Tuff-frartcntal - coarse asb to flac Lappllli, rencrally felsicnrhrrccciro7C.2
C' Lr.rnilli in a cnfic nnrh - chlor natrix rivinj^a aottled::i:h aprcarcnca,rith depth.
rcncraly decrease in frarcents C' franncntc
-7S.4 - contact between rafic tuff fracccnta O cr*yvackctt: f f - cr.rb*d, fine strinrcro le- vith r.inor Ty b trr-ces Cpy,conductive, ovcr.-.ll 5-1055 sulfiilcs.
1
-/-.
-(^JlCHFD-J^/P/TO .t. C. ChastkoM P 1 F c;
FROM TO V 1 DTK
l
/ll 1
V ~"— . ——
HOLE NO^-?0-70-9
DATF 25/8/70A 5 S A Y S-
/'^
— " "
r-T ~4-SL—'/(..•K' :
fc:;J^li^Tl\QM ^: ^tOCHENODI^WlLLl
LjDC-ATlO/vT DRUM LAKE AREA, GROUP-30 '?J
• "^'.f-M'^' ..i.-**-.-'.-* i : .
0.0 15.0
47.749.2
Sl-Ze: EX
ir*
Grid3050'S
J.EDWARDS
X)(P ^ 102-0
;' 25/8/70
15.0 Casing47.7 Tuff-fragmental, ash to Lappilli felsics in amph - chlor
matrix, gradation of fragment from ash to large lappilli insections, Tr.Po Py37.0-47.7 large felsic lappilli with sulfides along fragmentoutlines, generally ID-15% sulfides. 10% Po, 5% Py, k* ZnS. Tr.Cpy, sections of sulfide in massive stringers, conductive 5%carb.
49.2 Tuff-ash fine grained, massive, It. greenish grey 102.0 Tuffaceous greywacke, fine felsic fragments, slightly biotitic
25/8/70
L.C.CHASTKO
yptom T&.
B-30-70-10
LJ* 26/8/70
jaiil
3056 37.0 47.7 10.7
DUPLICATE COPYPOOR QUALITY ORIGINAL
TO FOLLOW
PiAMOND DP L L HOLE LOG ^COCHEIfOUK WIttAKS-SELCO ~"DAKAJI PROJECT^ /-•^^..•^.••.^--.U 'JUV1 ',, .^r^'J/.Ui,^-^,^.,,.- ————————————————————
LOCATIONS™?- T*CORF SIZE EXELEVATIONFROM
c. rJL5.0
1 47,7i
i j
TO15.0
47,, 7
49. 2
JL02..CL
1
1
G E
bf *r**r* ( Crotin VIBEARING Grid i:LAT i TUDE 3cro*f;O L O G 1 C A l
jUKlH-t
DIP -45 iDEPTHlOZ.ODEPARTURC' L-8200 V
D F S C R 1Cn si*1 ".
Tuff*-i*r^f.f.t-
37.0
- rrnfTT.cnt.-'.l , ash to 1.1^01111 felsicsl^i C 1"^1-*1* 10^ nf
-47.7 - l?r-c fei
frf^r-r-nt fron ash to 1
hi v^ii 0 l^yrp n 25/8770:-:^ I^i1\i\ wpn 2 s/s/70Vi i ' ILCGGED ev L.C. chastico
P T 3 M
in anph - chlorar-ff lapilli in
sic In^rilli vith sulfidcs alon* fra/^ncntpMt-.i ine* . -e a** r si Ir 1C -IS1? siilfides. 105? PC
Oy,c-**" T*
Tuff*" -i -f -"
^ 51? PT. '.'Z ZnS. Tr.sections of aii\flde In r-assire stringers, conductive 53
- ash. fine grained, cassivc. It. prccnish grey,^,,, ^t.^V!, M. 1. flno' f^l.nic frar-r-cntti, nllrhtlj Motitic
SAM P L F ^NO.
3056
-
.
FROM
37. O
TO
47.7
-
WIDTH
i
10.7
fl/
^-.""---^n —
HOLE NO, B.30-7C-10DATE 26/8/70
A S S .A Y 5
-
r\\ \v.'
'
-
^ /^^V-^xx
,,, f^: ^
i
BAMAJI PROJECT
30, BAWASHE LAKE AREA
XT Grid N
J.EDWARDS
110 1L
Mot* Mo- B-30-71-13
10/7/71
0.0
15.0
21.6
35.4
48.0
190'N
To
L-8050 W
PT\ C O15.0 Casing
21.6 Mafic meta volcanics - dark green massive, amphiboliti2ed 20% amphibole5% crystals up to l cm in length 70^* feldspar Trace Po in desseminated blebs
35.4 Tuffaceous greywacke, dark greenish brown, fine grained well banded at 55-60" to C.A. cyclic bands, fine grained material S med. grained quartz S feldspar crystals in fine grained material. Graded bedding in coarser bands with coarser fraction grading to finer with depth.
48.0 Mafic meta volcanic dark green med. grained 10% amphibole 10% chlorite 5% biolite, tr disseminated Po
48.15 Massive sulfides **brecciated med. grained, 10% Cpy, 50% Po, 2% Sphal, 15% quartz blebs,S 1! biotite, sharp moderately contorted contacts, biotite developed along contacts
48.15 101.0 Tuffaceous - greywacke, cyclic banding, same as above.
END OF HOLE
DUPLICATE CPOORWAUTYORI
TO FOLLOW
~
[^IJjJAJjJJIjJJMl " "KHSHSDM(33*1931^^1
3 30* " -.vashe Lake Area-T i C^ING Gp*^ ^ D' P
~ L EV AT 1 C : !"UDcl**0*V CF^yFROM
0.0Q
15,0 .l
21.6
35.4
4S.O
42.15i i
TO
15.0
21.S
35.4
..
48.0
48.15
101.0
G E . . O G I C A t
AJI IZOJECV -••^-,--f; -••v^rf^-pr(r:!iww^^^; ... -- . - - : l !*''^:'-*:*^^fo^'^\)^^ffi^
~4S* D^PTH 11 -Jfo'
-RTLIRE J -5050 1LP E S C R I P T !
v ••• :;v'--" '
CM
f^Stfo/r/Ti7 '"'"LQGGED bv " L.C.Chastko
* '
Casing^
Kr.f!c 1'ctp Volcanics - dark ^reen rasniTC, urcphiboU5? crystals UTJ to lcn in length 7055 feldspar
Itized 20* nTrace Po i
Tuffaceous rrev^.-ackc. dark crcenish brcvn. fine f-^^ned well b*cyclic bands, fine grained material ff ccd grained quartz 6rfine grained naterial. Graded bedding in coarser bands vitgradicc to finer vith depth
J'.afic Hcta Volcanic dark green nee* grained 1C5C anrhibola10^ chlorite SjS biolite, tr disseninated Po
- -
1'ossivc Snlfidcs **brecciated iced crained, iQH Gap^, SO* Po, 25* Spbal, 15J5S?, biotite, sharp coderatcly contorted contacts
qua, biotite de-
Tuffaceous — preyirccke, cyclic banding saxoe as above11
. •'••'. . .:' ', '
EKD OF IIOL
5 A MN'O.
^Jiibjttlt disse
ided ftt
P l F ^FROM
eainatec
.SS-6
TO
blebs
oc t** n.'cldspalr crrsti coarser f rae
•t st blejbs,relopod{ along
D
als In1 1 on
contac
VIDTH
9
(1\ ^
V ^
JC.I.C NO. rif-3c-7l-l3 ..•\ j T F 10/7/71
ASSAYS
-
\li
x*
/5
\ ^^k?7vy
i
f ^x^^^
^J
1.0
11*11' Casing - overburden
35' Mafic volcanic (mafic, tuff?)
Minerology:Chloritized amphiboles (approx 30%) calcic? plagioclace (approx 60%) mica (sericite S biotite (ID-20%)
Pyrite and Pyrrhotite (tr) along foliation
Texture:F.g. to m.g. - equigranular - clastic or smeared crystals
35'
38.6
fet:
Structure:Well foliated; sharp contact with next rock type
38.6 Mafic TuffMinerology: (dark green in color)
(a) chloritized amphiboles and calcic? plag. Texture: very fine grained to med. grained (cyclic) Structure: very fine banded: grades into next rock type
59.1 Tuffaceous GreywackeMinerology (dark grey in color) a dark minerals, biotite, other clay minerals, b) calcic? plagioclase.
--^'-'^••^^•'^•^^fe^^^^'^-^^^r.^. 1 :-V Texture: very fine grained to medium grained (cyclic)Structure: well foliate: v.f. layered (l mm to l cm layera)
sharp contact (?) with next (?) type.
2 36.6 38.6 2
DUPLICATE COPYPOOR QUALITY ORIGINAL
TO FOLLOW
"' - " '' 4''' J -'
--- ' '- - ^^i- -^ i ^ ms? -~ "^^s^s^^^^.--,.^.-..-,v*J
LO v.'AT I&BJP*^ '-"BANANA LAKE - Croui* 30 " - ^^t^X&fil&m te^1#Jfi?i^iTSttfiBH^^ .. "COR 'EJ SIZE *RP" BEARING S-N loJP -45O DF/PT^'l'sVtlri''^^ELEVATION- LATITUDE 79 'K501bFPAPTl!RP 147N ' "FRONtf0.0
11*
35*
38.6
-,^ - --V
tTO"
35*
38.6
59.1
G E O LOG t C A L O E S C R' 1 PT 1 O M "Casing — overburden
Mafic volcanic (tafic, tuff?)
MincrolflgyjChloritixed ccphibolcs (npprox 30^)
' calcic? plagioclace (approx 60^)
"S 'A^ : M : P""f--'"t'~"s-
K' O.
nica (sericite O biotite (10 - 20g)Pyrite and Pyrrhotite (tr) along foliation *
i . ,
Texture J ' lF. g. to B. g. - equigranular - clastic or sneared crystals
Strtrctnre:Veil foliated; sharp contact vi t h next rock type•*-
Mofic TuffHincrolofsr: (dark crcen in color)
a) cliloritized acphiboles and calcic? plan.Tcxturci very fine grained to ccd. rnvincd (cyclic)Rtructu ' ^^'T ficft banded; ^rxf^n Into ne*t rock type
' .- -* x; ••" - ' - 7; - - .-' ^" ' -' •-.-y^^^S^^t^S^:^-!^ ,-/. -/;-v. ': -- ' -"
Tuffaceous GreywackeKincrolo^y (dark grey in color) c) dark cincrals, biotite,
other cloy minerals, b) calcic? plagioclase.
Tf*'*"f'l'T'f* t vj~i- f*-?r." J^ x*n ^ ** o *" r*r*r|^nm p^-^^^j*J ^pv.^,'j^ o j
Stri!Ctt!rov veil '"•"'Lite: v.f. Ir— ---d (1 rn to 1 cp IpTerc)- ' 'Sharp c *t vith n*^r-t ' •-^ty^V'^' 1 ""'" •' ;:; '- '"' ' '
2 ;
FROM"
-,
36.6
H - ' . " -j.
*- •'••-••,.
* TO"- - ' - 1 .''-
38.6
^
VIDTH
-
2*
(l
f(jt^~—
PAT? Jnl-T 12/71^''A ' C C, A Y S
•\ x"/
Cf i
"A, ^^*^ijf
|*y*
. -. -
^f
\
l LQ^.^ii^Wlifi^pS
-•X'*S-:
^BANANA LAKE - GROUP 30 ^.-3-30-71-14
DM M.R^A.MS
59.1
PAGE 2
114.8 Mafic volancics - same description as for 11' to 35'
114.8 115.0 Contact between rock immediately above (Mafic volcanics) and rock immediately below (Tuffaceous greywacke) Minerology:
(a) massive pyrrhotite (about 98%) \(b) chalcopyrite blebbs (thin 0.5 mm continuous
layers parallel to soliation) (about 2%)
115.0 131.0 Tuffaceous greywackeas described for 38.6 to 59.1
TO
DUPLICATE COPYPOOR QUALITY ORIGINAL
TO FOLLOW
^-^•/;*-'^^J^0il?fJ5^f4?"t^^'H®^^ ,-e-/ -: ''v;,--;-,,. •~-....,,. :;. -v. , .-.-.••- ",: ^•rv&^^mm^^^^m^^^^^^^^^Tl^O^P^^ y-^IH-cU -^J^^fe^j^^ffjr^^^^feS^\ - -- -:; - --.•-. - •,;--,^'!v^.,:- - - : . -vr-.y 1 ."'-- :'- ' 'i 1-;-'-- :- , ' ' '
ELEVATION ' LATTITtlDEFROM
55.1
33 4 . P
31S.O
•-,/, --
-TO"
114. P
TT;. r
l.n.o
*
G E^oWoG 1 C. A lKnfle volcrniea - srr
nonf.., rr hr-tv^r-T, t-ArV
end rock iis?!ediatcly
OIP IDF.PTHCFPARTLIRF
- OPS c R r
l^.^flT,.'! rl^n-r^ ft'* 1
below
H V llCGGEr) BY
PT 1
it * rt tc
r^ T^o*
O NJ ^v
rtt )
(Tuffp.ccoua crcyvocko)Kinerolocyt
a) itasciTo pyrrhotite (about SEjS)b) chalcopyrite blcbbs (thin o. 5 EC continuous
iRTcrs pnrnllel to soliation) (about 25)* ^. ' ' ' ' - - "^
Tnffr.ceous fre-rvaekcAa described for 38^6 to 59.1
-
•, ..
. "* - -.
*
•----- . U.i^:/ ^.V:^-. •.•:...v*:-:-
.
. :,-: ---.- . . : .- -.- -' .-i.'-'--'- -- : :- V'- -P'v^-^;-; -" "-•"-^- •-
S ANO.
f
..-: 1
- , , T . ^ . .V .
|8S9BS9efi^pWN!W?^)lW^^?f^c^F!^'^!®2^'^^- IpCl'" F ;; - 'N 3*3^71"' *?^iil
-"-•" : ^"""'": ' - {DATE"'" 1 '' - . - v -- -' ^ :;-v ;
M PI F ^FROM
- ' '; ' v ~
':'. -. .•J-^'^i
— :
.-:A,,;^;
TO
---- .
:.-.;"
— -
. - :'
. - -
''i r.
finli(\
V 1 DTH
-
2^^
A ^ ^ Ach ^r 0 "s
fa f\^L-^^f
•' - :'-
5
.
t t1///0//Ufca'
'
-
-^-
-^-'
. .i"-'- : ' ".
- -
Cft..'--.
'"
r^2#^^^w^*^Ce^RE-^'VZEXRP^-'"ELEVATION '^ ^FROM0.010.0
10.2
36.0
40.956.0
*TO10.010.2
36.0-
40.9
56.057.9
G-E
C? F*~ A\ " F^ 1 l^Jt *- ^J*"J^ /-"••H.-;. V .
LATlfuDESl-MOO 1•o'^il" ;6'G;'--rc"A^L
D!P? -450
tEPARTUREv-^-^vSW''" O
^ikhV]DEPTH17S'
150 Np v *v
Ga sin s -overburden •^v' :;-^.-'; '-v '^ -:-vV- .C R 1
taWafdsp^lfe^^ui^ F^rfo.^ B ^3a^?7l-^i:H^e-'-^: Y|v^:^,- - - ..-.•-:.- - -v--..,.
PT t 0 M
Mafic Volcanic (mafic tuff?)Mineralogy:
a) chloritized araphiboles (about 30^)b) calcic plagioclase (about 60#)c) Kica (Sericite Gr biotite) (about 10-20JOd) possible Quartz pebbles
Texture: fine grained to oed grained; equigranular; fractureand smeared clasts or crystals.
Structure: well foliated;1 contact with next rock type belowwas destroyed by drilling (powdered)
Tuffaceous Greywacke29.0 to 29.6 — no coreMineralogy:
a) dark minerals (biotite; other clay niherals) (about 70-81b) calcic? plagioclase (about 15-20^)c) vhite chert bands or quartz stringers parallel tofoliation (S-lOjS) Bands are Inn
Texture: very fine grained toto 3nro thick
nediun grained (cyclic)Structure: Knife edge contact with next
foliated, very finely layered (laxa toMafic Volcanic (naf ic tuff?)
rock type; welllcn thick layers)
As described for 10.0 to 10.2but with definite intcrbandcd quartz pebbles (about lcm to2cn In diameter) layers. Pebbles thenselvcs have been fra*
Tuffaceous rrcvwacke - 03 described for 10.2 to 36.0Mafic Tuff.Mineralogy: (dark green In color)
a) chloritized anphibolcs If biotite .ffs---- ;v ' ^•~^- -b)- Calcic plagioclase ' Y^^f- :'S^f
SAM PI E SNO.
-
5?)
itured.
FROM
, -~""•i'""
* t', - "
,\. '-4' '.7, ,-' .-
TO
~-
*- -
MDTH*
-- - -- .
,-... . -
ev^5*ffCTC
QATE JulT 15, 1971 r- P
A 1 SAY S -"
-V; '- :
( b (
WU^
X
^
fi Sirl/t//^f'
- - -- -
: :- . -.
i
-
*
^ continued. . .^ -Y Y^Y
HBMMMMMBMMBBMBIMMBiMMBBBPBBBBi
ijp^l^^• g' DEPTH' ;: H V_____IICGGED PY
-. --— -•±Q\ E NO. 3-30-71^
CORE SIZE DIP CATF Page Ko,ELEVATION L AT l TIIDES ; '--'i DF-PARTIIRF 5 A M Pt AY
FROM D- ; E^ T O' NO. FROM TO v l PTH56.0 ! 57.9 continued)
Texture: very fine grained, equigranularStricture; moderately foliated,, contnct with
ground in hole57.9 j 85.10^ Mafic Volcanic * (nafic tuff?) as described for 10.0 to 10.285.10-J 87.1^ Contact zone between mafic volcanic* and tuffaceous greywacke*^ 47860 85. 86.6 J!L Tr 30 n tal
Mineralogy:a) massive pyrrhotite (about 853)b) blebbs (lcna to 2mm) fr (2nn to leo) of chalcopyrite
parallel to foliation (about 2-52)c) finely disseainated galena? (fine grained crystalline) ibout 5 -105?d) blebbs of sphalerite (0. 555 to
87.1-S- 165.0 Tuffaceous grayvaclre** as described for 10.2 to 36.0
oq.7-Ton.7 - Al ^o gontaineg string •yg
Cr veinlets discordant to foliation. Between 143.6 and 144.0fainor pyrite generalization along contact betveen discordantquartz veinlet 6f tuffaceous greywacke but in quartz only.
Grades into next rock type below.165.0 165.1C Mafic Tuff as described for 56.0 to 57.9 Contact with next ro- fc is s larp.165.10 176.0 Mafic Volcanic friafic tuff?) .1 fot* T o. o in-3
also with concordant and discordant (to foliation) quartzveinletsj and quarts pebbles? (lcn x 2cra to 5cm) stretchedparallel to foliation nBetween 175.7 and 175.8 - minor pyrite mineralization near
discordant (to foliation) quarts vcinlot but in wr.fic volcanic
fEnd of Hole
D i AMD NO"* DP t L L-"v- HO Is E*^"-f L O G ^ -^ "OJECT-*^^'-^3**L^^A''T-4':Qr4Y^Ban: a^a^rLakeYA^CORE SIZE vXRPELEVATIONFROMo.or9.0
- "— \...TO ,9.09.6
9.6
-
.9
t
*- :"
39.6 48.10
G E
BEARING G-^ -
LATITUDESH-Om/0 L O G 1C A l
D' j p-600N--
CFPARTIIRF.
Casing — overburden v ~ Y.
1 "' "" " "; ' fjf "t t - ' tit r- OTTI1-^ " ' A -J -J a
^50' ; N : ;:— ;
F S C^R lV* " . - . - i -'.--•-•-••- -••' ^ -. ,--'
^js^^^SYS^S^J^^IJ..- 't l'-*"'--.'-. jii'lG'A-Lt*.'*'-'*rr"-N T' •'-••i .'V-.:--"v -V ' H}*4-I- ***" -" •"•••3-0 **f-r- —.f,v 'f 1. - —rEdwards^l^PTFR^JulT IS/Ti^iNlcWFDJnly 17/71HCLE^^.K*- |v llCGGED PY R.McCulloch"^'Y v '- 1 : ' . ~ ' '
'P T l 0 K!
Seritised mafic volcanic (mafic tuff ). Mineralogy:
a) sericite (about 40^)b) calcic t plagioclase (about 50J5)c) amphiboles (about 10^)
Texture:medium grained, equigranular, highly schistose
Structure:highly foliated, contact vith next rock type destroyed by *
Tuffaceous Greywacke (grey in color)Mineralogy* .
a) dark minerals (biotite,b) Calcic ^ plagioclase —c) very silcous bands (lornand regular concordant (to
other clay minerals — about 70 115 to 2055to lcm) irregular discordant,foliation). Kay be quartz veinl
d) minor pyrite mineralization (from 36.3 to 36.5)c) xxnf Percent of minerals varies from layer to layer.
Texture:very fine grained to fine grained, varies from layer to la]
Structure- -veil foliated, layering parallel to foliation linn, to 3cm w:contact vith next rock type appears to be gradational.
Mafic TuffMineralogy:
2*1 ^*^T^^^*^*-^—-..I ^— 1. 1*. -i ^ -— j -i —j— .b) clacic? plagioclase (about 20JJ)
S A M P l E ^NO. FROM
1
---'
rillin
,o 8055)
S-
1 3, anjl/or qu
1
er
de.
t /Y. JA..TA. . * *. ^
i
Texture: , . . . Y., . -.-. ..-. , ,--. ..- , .-. -. . Y; ..' '"-"'"^ ":- Y"Sr;5'" 1 V" '-' --''A- "- - --^
GO'jlww,j y
TO
art z pi
MDTH
bbles.
.
f
1-4—L^jS^.l J ~~~
v- - '.-- :- . -.-^~-.— CSs
p ATF July 17/71 Y
A ^ S AYS :
- -
^•"\--' ^^
^
h
- ' Y : •Y'"""
j
/nri/K/./Uu^
s.i//S/* J
: - .Y.YY
'^•??S',"*^V:".*-*^': \YY Yt
LOO AT lON^-w^-^CORE" sfzF"^-'^-LEVA'FROM39.6
48.10
54.655.1157.070.0
114.6
117.6
i —i
J120.1
TION— —— r TO
48.10
54.6
55.1157.070,0114.6
117.6
120.1
133.0
G E
•'•,y^i-.^fi^f::;. -, ^ s*, •-v 5^jt'5sjw*ftf-- -. ..-.' -v-i.-.. ,- --..,, ;jir'.-:y;t^ '
SEARINGLATITUDEO L O G 1 C A 1
Texture:' "'••^l^/'-'-'A''-^
.-^/-AK^fs&p'.D j'pV;-;^5iv
CFPARTURFD
®:^Sf^|-^V~.--: -w-.-.-- *"- ?*i-*'-p?ii-.',W;i':'
DEPTK^^
F c C R 1
r^^fiW*WlWAOTP7?e^.;^:;Ti :sw.vR(Kiiev4Pn - | o. c NO. B-30-71-16j4afts^stw*s*Si*'r s***v,3^--~!s-.~-\' :~'^'---- '-~ -' ' : - - - - - .H*fe^'^' V'^:"— ILCGGED PY ^ " - '-'.v?C'fr''- :i^'"-"-i'" " - ; .'' . -' P ;"T --V-o'M - -'" :''•; ?i|5?:;:S^ ?;,K- --' - '"-'^ ±'
very fine grained to coarse grained (cyclic)Structure:
veil foliated - layering (lima to 10cm) parallel foliationcontact vith next rock belov appears to be gradational.
Mafic volcanic (mafic tuff) -
Mineralogy:a) chloritized amphibole ft biotite (about 30^)b) clacic plagioclase (about 70/5)c) discontinuous sileous bands 'Inm to 3nn) (about 1J5)d) quart* veinlets (about IjS)
Texture:coarse grained, equigranular
Structure:veil foliated, contact vith next rock
Mafic Tuff - as described forbelov gradational
39.6 to 48.10(no core) contains contact vith next rockTuffaceous Greyvacke - contact with nextMafic volcanic (mafic tuff) as described
belovrock gradationalfor 48.10 to 54.6
chloritized anphiboles and biotite, contact vith rock belov g]84..0 to 85.6 - nafic tuff as described for 39.6 to 48.10Mafic Tuff as described for 39.6 to 48.10 - contact vith nextrock" belov is broken. . - 1Tuffaceous greywacke as described for 9.6jc to 36.9117.11 to 118.5 Conductor - pyrrhotite (90JS)chalcouvrite (Tr); Sphalerite (1J*). Contact vith rock below iknife edge sharp.Mafic volcanic as described for 48.10 to
SAM Pi F ^NO.
ad- tio
47.,-:
,
54.6 but with fine :' ,,
FROM
11,
tial
117.10
TO
118.3
VIDTH
5.5"-ft.'-^
rs-Te- - Page No. 2^..l-fc. — ————————————A C ?, A Y S
Tr
N••'^- -,-v
. L... t
-
30 neti
™ (|OUl.*ftn'tS*-P
.
1
/'•x?t —
;;.,;''. . . -" '^
f
, -:-'-
— —— —
H*i*" •• l "!*m^--:^ -^mm
irO^F SIZEELEVATIONFRO.V.
120.1
-
'••':\
TO
133.0
-
•-7:^-
C- F
,J;-,K.V^V.:, -r- .:y-\, . .v:-^:-^7^^:v.-^:^^|^l^^P^ij^|^^
BEARINGL AT t HID E0 L OG 1 CAL
DIPCFPAPTURF•"•'r*
DEPTH y :
F .-S C R 1
H^,::-X,;:;--;'-jvfefeB^S^^^^^Jt&^l'eO'FD v "; "- :^^^^T.-.-'. ---.- .Wv f -j, iMS",?V^i,.OJ-v-.rX i-.'Si-:.J' •..•v-GV --. ' rv . ,-, jj i, ; ' - -f , li "^ C- ED P Y '
. , ^ . .- -. r^,: .^..^.^.4 'p ";T^- r O : Nl - ~' '-^
V,--^ - .:.,V'ft-:~*'
(continued)fine (lorn to 3cm) bands of biotite and fine (In)felsic (vhite) bands. -'Contact vith next rock belov 5 s gradational
i "J "
' ;. ,' .~ -
.
End of Hole. '.:
'
.. . : - - ; .-.. -*-: ' /x: - '-- - - - •-•
^••^m---' ^.^•^gfc^-m-- . .••••v^^^*/^^^^^
SAM PI E ^NO. FROM
i
••*te-^
!
•^ ^^
TO
t*
MDTH
.
*^-C^-.
*^^ "*^-
-
^Of f f\i O. B-30-71-16
DATE ,. —— * ———————Ja^^c S, A Y S
-/^
\^^
-
j
f1 1 /XT-
1
^ *
x
i ; 12' ,. '''\A'f' ;•* : ':?^ .^-y-'y
l\JSj
MAP (5) IbEMT/F/eb
j/v life/M TTtE FoLLOiJ|M(
5EQU.ENC6 (.X)
,-AV-
z ROM TO G E 0 L O G f C A*V 'C. C ! 11. 0 ' Casing.
jLjL eta 2*-t^3* —— AJO'T — SM* OC'-a' '| —— — ——— — — — — —— — ~—
D E C- C P I P ~ 1C*v,~*ix ' ^ i f
j ,t
CRO^ Tf^ 'A l DTH tJ T^
! 11.0 j 27.5 | Mafic Meta Volcanics: fine to med. grained, dark green, mod. i (Ho ji t i ' i r to highly amph T d &1 chlor'
filled with qtz-carb.d, massivej occasional fractures '
: 1 ' 27.5 | 39.6 ; Tuffaceous greywacke: fine to med. grained, finely, well
i i
39.6
55.0
ii
55.4
|
•- banded, coarse banding of
wacke b 3bbdc3bc lighter gr
55.0
55.4
^.^
Cs4.0y' '
fine grained dark grey tuff, grev-
ey tuff greywacke with roed, grainedfrag, f/ atz — feldspar Xtals. coarse bands way from a fractioninch to approximately a foot in thickness. banding at 55 O toC.A.29.0-30.0 - LOST CORE
40.0-40.6 - LOST CORE
.
of an
Mafic Meta Volcanics: med. to dark green, med. grained, shear
banded at approx. 55 tosegregation of raineral^s5-10# blue qtz eyes, occ.
C. A.. ajnph*d^ chlor*df somegiving slightly mottled appearanceqtz-carb strgs.
54.0 ~ 55.0 - highly sheared l/ alteredMassive Sulfides, 40# Cpy
55.0-55.2 - ground core -to core described above.
tuff greywacke at 60 0 to
, 40JC Po, 20# inclusions
recovery of some broken core — similaSharp conformable lower contact with
C.A.Greywacke - tuff - dark grey, finely well banded at 55 to C.A.occasional coarser section with tiny feldspar fr qtz Xtals,generally uniform texture.59.5-60.1 - Lost Core62.2-63.0 - Lost Core
r i
i
r~-
^6.0
;
y•'•'
i;
l T,
\
\
\
' \/; '
^_^_]l . ^-- -**
3i,ii
3^3
53- ^ iJ^T^ ,
. s.-'
; ' *
* . . L.
. . -,
i
i
j
,~ : - , ,
••'4* ±.;-ff r-r.r
"" — — i — —
1
j
f
jj,
^-/'
~zZ— * '
_ QjQ i 27.0 l Tuff: Coarse ash - to fine Lavpilli 50-60^ felsics^ 40^ amph.- [3. 2^ i iti
27.0
25.8
78.2
*.
29.8
78.2
103.0
i
chlor.. mottled ^greenish fr grev appearance. Diss. blebs Po PT J
occ, 5"Deck Cp-v. overall 2'fc .
25.5-26.5 — poss. fault zone, carb-qtz. strg walls 3bio T d, tt
foliated at 40 to C.A.
Tuff -fragmental ~ fice Lappilli 50-60J& felsics, 20-30^ mafics
flecks generallv biotivic giving rise to a mottled greyish fr
brown XS3553EX appearance, foliation at 50-55 to C.A. j
Tuff - Greywacke, fine ash' - ereenish to ereenish erer. finelrwell bedded, chloritic fr blctitic* foliation Gr bedding 45-50 to'C.A. Grades into a greyish brown tuff —grey wacko at 34.0 simila
t to before coarse banding of fine grained k±±x biotitic tufffr coarse grained fragmentals - gradation generally is from
coarse to fine erained from top^ to bottom of hole.52.0-52.8 — ln qtz-carb - lost core - 1 inch qtz carb
53.5-54.0 — Lost core55.0-55.9 - Qtz carb strgs.
60.0-60.6 - Lost core66.6-67.0 — Lost core
Tuff— fragiieatal - coarse ash to fine Lappilli, generally felsic
ash (f Laupilli in a mafic amph - chlor matrix eirine a mottledgreenish appearance, generaly decrease in fragments fc fragmentasize with depth.78.2-78.4 - contact between mafic tuff fragments (f greywacketuff - carb*d, fine stringers Po with minor Py S* traces Cpyjconductive, oTerall 5-lOjC sulfides.
;
ii fj
tr '
i ;
'
\i
\
1 \
\\~TL.
3?.g
73, l 11^^
i
is
1t
iii1iii
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-
t
1(
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—— .
f
f*'.—'''^
\ t
SiriiSTRY OF N
R fc K.MAR
. e;ua;^:.rjSICW
'
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i
TL.SAL rE?0',-
t-1 " ""^ y
V S- a-
1 o 1976rrtpncrrSOFr
C LOOKOUT
CES
CE
——— 4-
c.o i15.0 i
i 1
i
47.7
49.2
1i
15.0 i
47.7 !
49.2
(ioTo^^-s
Casing. i
Tuff — Fragmental, ash to Lappilli felsics in am p h - chlor i
matrix > gradation of fragment from ash to large lapilli in 1sections, Tr. Po Py37.0—47.7 — large felsic lappilli with sulfides along fragment
outlines, generally 10-15# sulfides^ 10?6 Po , 5# Py, i# ZnS, Tr.
Cpy, sections of sulfide in massive stringers, conductire 5/6carb.Tuff — ash, fine grained, massiYe, It. greenish grey
Tuffaceous erevwacke f fine' felsic frae-ments f sliffhtl-r bio-titic
1
-
"
;
t
t
3056
i
37.0
,
47.7
f,l/
:^^ —
ir
10.7 |
V
—— 1
—— 1
^*-v.
i jl1
l Y-
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(H /'W , l
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'
——
/")// - -,y^r//
/
i
1
^
jt
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, w, '
52006SE8ie6 530865688 H KAWASHE LAKE
THF MINING ACT REPORT O
To tKe Recorder of .Pftfcrl.Cl C........................................................................................Mining Dh
j Cocbenour Willans Ooid VUnee Ltd, jnome of Recorded
.9P.?.^6..n0.H?.|. P.?#.?# ?
Miner'.* Licence
Post Office Addressdo hereby report the performance of ,..,...,
not before reported to be applied on the following contiguous claims
Claim No. Days Claim No. Days
Pe. .224932." .78, 224992...' ...77. .7JL 22.4,79,3..: ...7.7.
days ofI2ie2Qnd..dxd.Lline}t
Claim No.
type of work
Days
. 22.4?9p.
..78..
..7.8.280823..." -W-
.138.
.m.224991- " .7?.. 280375..^ -53-All the work was performed on Mining Claim (s) ......V....../.T...!..........;...(In the case of geological and/or geophysical survey (s) where more than 18 claims ore involved attach a schedule) '
READ CAREFULLY; THE FOLtOWING INFORMATION IS REQUIRED 8Y THf MINING RECORDER, ."
For Mongol Work, Stripping or Opening up of Mines, Sinking Shafts or Other Actual Mining Operation! - Home* and ^addresses of the men who performed the work and the dates and hours of their employment. - -i ft.-'i;-.:' '' Si t:For Diamond ond other Cere Drilling - Footage, No. and angle of holes and diameter of core. Name and address of ;-;owner a operator of drill. Dptes when drilling was done. Signed core log ond sketch in duplicate. '. -. ";-. ,;For Compressed Air or Other Power Driven or Mechanical equipment s -, . iType of drill or equipment. Names ond addresses of men engaged in operating equipment ond the dotes and hours oftheir employment.For Power Stripping - Type of equipment. Name ond address of owner or operator. Amount expended. Dates on whichwork was done. Proof of actual cost must be submitted within 30 days of recording.With each of the above types of work sketches ore required to show the location and extent of the work in relationto the nearest claim post. In the case of diamond or other core drilling the sketch must be submitted in duplicate.For Geological and Geophysical Survey - The names ond addresses of men employed os well as dotes. Type ofinstrument used in the case of geophysical survey. Reports ond mops in duplicate must be filed with the Ministerwithin 60 days of recording. ,For Land Survey - the name and address of Ontario Land surveyor.
The Required Information is os Follows: (Attach 0 list kf this space Is insufficient)RblTTl
B-30-70-6B-30-70-7B-30-70-9B-30-70-10B-30-7CM1fc-30-71-13B-30-71-14B-30-71-15B-30-71-16
L Date.,
w, AngTB-45 S-65 ."^ ^-45 ^-45 '-45'-45-45-69 *f
Fobruery
Core ui ts.7/8 "7/8*7/8"7/8"7/8-7/8"7/8"7/8"7/8"
19 th, 1974
Depth101''103''103''102"105"101"131"176"133' '
CI elm No.280875280875280875280875224993280875280875280875280875
l••KH
Covering De t* s17/8/70 18/8/7019/8/70 20/8/7023/8/70 24/8/7025/8/70 25/8/7024/8/70 26/8/709/7/71 10/7/7110/7/71 11/7/7113/7/71 15/7/7115/7/71 17/7/^1
f-^. L..,S-^ 1 , . .rAr-yTj**^*TSip^^ \* ' ' ' ^fri^ ^i t— Signature of Recorded
ContractorCoe he nour VillaGold Uines Ltd.
/t^K*. /*S*fas.^Jt-J **^*~'
'^L*'*cV-**"^ -*^
'COSf'Holder or Agent
Th* Mining Act Certificate Verifying Report of Work
l. L. C. Chestko
o*t Office Addrej*)hereby certify:
1. Tho 'ing per f
2. That the annexed report is true.
1. That l hove a personal and Intimate knowledge of the facts set forth in the report of work annexed here to, having performed the work or witnessed some during and/or after its completion.
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' A FEBE71974AH
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B -3 0-^0 -10-4102
B- 30-71 -1-1-45
3 -30 -70 - 9 -45103
B- 30 -71
-30 71 B -30 -71 -1
DRUM LAKE AREA O.D.N/!. MAR.V13050
CLAIM NO: PA.-28O875
SCALE 1 *- 200'
580.6SEe.14 KAWASHE LAKE 200