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CONSULTING GEOLOGISTS
, 688-4134
OUVER I , B.C.
TAR AND LOU CLAI
THE UNIVERSITY OI- 13RI'I'ISt I COI I 1 ,Ll lii:\
V A N C O U \ I I{ X , ( 4 \ \I) \
DEPARTMENT OF CEC71.0GY
Mr. G.P.E. White Gordon P.E. White and Associates 521 West Pender Street Vancouver 1 , British Columbia
Dear Mr. White:
RE: Polished Sections, Terrace Area
In answer to your letter of January 13, 1970 1 have the following to report: 1
I Hand Specimen: This consists of a fine grained leucocratic
porphyritic rock composed apparently mostly of feldspar and quartz, somewhat brecciated and weee mineraliz~d by bornite and chalcopyrite,$he bornite is altered along cracks to covellite. Both malachite and azurite have formed on the metallic mineral surfaces and along fractures in the rock,
Grain size of the sulphides is coarse, suggesting easy separation. Much of the primary mineralization appears to lie on fractures.
We handled your request to search for the silver carried in the ore by I )polished section examination, 2)concentration of dplphides, visual examination anci analysis for Ag along with other elements, 3)microprobe traverse of sulphides in the specimen, 4)x-ray fluorescence scan of sulphide concentrate.
The content of silver in the rock according to in- formation supplied by you is 5 to 1 ounce per ton, No silver mineral was found in polished sections and no sllver was detected in the microprobe traverse, but thjs is a relatively insensitive technique.
Mr. G.P.E. White - page 2
by atomic absorption is in the range of 500-1 000 [,pa (in excess of 15 OZ. per ton). The same sample cxrTrcAr; m:,jora copper and 200-500 ppm lead.
X-ray fluorescence scan of the s u l p h ~ UL c o n ~ t nt,r,Lte shows the presence of copper, iron and silver. Without spiking the sample it is impossible to estlmate sllv~r content by this technique but it is probably in the 100 to 1000 pprn range.
I therefore conclude that the copper ifon sulphides (notably bornite) are the silver carriers, and that n~ 1-ier will be recovered in a copper concentrate.
Sincerely,
,' J . A . Gower
Associate Professor
J A G / ~ V ~
Enclosure
- p- p- -
WHEN R E P L Y I N G PLEASE REFER TO
FILE NO.
EUM RESOURCES
December 10th 1969
M r . Gordon P.E. Gordon P.E. White
VMCOWER 1. B.C.
Dear Gordon:
Following your letter of December 2nd and our telephone conversation of December 8th. I have re-examined some of the t h in sec t ions from Kitselas Mountain, checking t h e degree of a l t e r a t i o n i n t h e mineralized zones. A t best. a l t e r a t i o n cons i s t s of t h e development of very f i n e s e r i c i t e i n a s i l i c eous matrix. Briefly. here i s a summary of my examination of nine t h i n sect ions .
A specimen from &-A Creek - "pophyrit ic gabbro" was seen t o contain 4 mn. phenocrysts of plagioclase (andesine) which make up
s' 30 t o 402 of the rock. These are set i n a fine-grained (0.05 - 0.10 mm. matr ix of quartz, b i o t i t e and green hornblende. Metal l ic minerals occur i n t e r s t i t i a l l y . The rock exh ib i t s l i t t l e a l t e r a t i o n of any of t h e consti tuents. and could probably be ca l led andesi te porphyry. This rock d i f f e r s from the volcanic at the po r t a l of the Copper King a d i t by size of t h e plagioclase phenocrysts. and t h e f a c t t h a t t h i s rock i s schis tose ,
Four t h i n sect ions front t h e "At1 zone on upper Ki tselas Mountain indicate t h a t the rocks here are ca t ac l a s i t e s derived from c r y s t a l - l i t h i c t u f f s and breccia. of probable dac i te compesition. The coarser v a r i e t i e s (t'conglomeratet') contain elongate l i t h i c fragments (volcanic rock) t o 1 centimetre size plus corroded. angular 2 t o 4 mm. plagioclase c rys t a l s which a r e remarkably f resh. These c r y s t a l s a r e omiented i n pa ra l l e l fashion and l e n t i c u l a r s t r i nge r s a l s o lend a planar f ea tu re t o the rock. The c rys t a l and l i t h i c fragments a r e s e t i n a very fine-grained matrix of quartz and some s e r i c i t e and carbonate. A specimen col lected a t a lower elevation. containing born i te as dis- seminations and i n ha i r l i ne f rac tures , appears t o be a rhyo l i t e o r dac i te flow. Very fine-grained s e r i c i t e i s bes t developed adjacent t o mineralized h i s a rea a r e s imilar t o t h e coars l i t h i c fragments.
8, '$/\ L'" ,,v\
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Mr. Gordon P.E. White P. Eng.. December 10th 1969
A specimen of dyke material from the "B" zone indicates that the dykes preceded deformation and metamorphism, since plagioclase (andesine1,biotite and chlorite are oriented in parallel fashion. Carbonate and metallic minerals occur interstitially. A specimen of dyke rock near Creek Fault displays a sub-ophitic texture with 0.5 to 1.0 nun. euhedral andesine laths enclosed by a matrix of biotite, chlorite and carbonate.
I hope these descriptions will be of some use to you. Thanks for the copy of your report.
NCC : bg
Yours very truly.
N. C. CARTER
SUM?v$kn, i;"k 7
Pereonnal of New Cold %tar ~ ~ B s L B ~ 6 : i ~ : ~ , t l : ~
past field seasan by ~yrternatic preapactinfr: ;eL:.l i E r d 11. C - t j :
in 5edr0ck on the Gold Star Claim Groilp t'rzve *:PSL*
copper an 3 eilvar mlnerdizaticac in a ii~ela:-;ko1'~. ; t. P. ,
eedimsrxf m d fa a p~xphyrific gabbr~. A lt(XZ.~u* ' rys i - . i ! : ,
eersnc~triic quantity at this tirze, wtth a posk~iblt.: , q $ t , L ~ t - ~
eource rock snd with the amaunt of etai.nErng E ? L ~ : , ! .+I- c : ? c ! ~ i ~ ~ c
in the ~~edimunermto, erxplorstlarn work t~ raeotfark-ie-l : t 4 c i ?:J
search for copper and ~ i lver .
T k i ~ ~epc~rrt. includes work ~t?ir t~pleteri t,;.r. t ' : -
Edau C%aim al*~a,xp,
G O R D O N P. E. WHITE & ASSOCIATES LTD. CONSULTING GEOLOGISTS
TABLE OF Cd'I1XT b2..:1.1'4. ,J
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C P l k I l ? " f S . . ........................................ . . . . . . . . . . . . . . . . . . . . *sCCESf; &NY9 T,CGAT.IClN.......
?T[ .< ;-,,- ,: ., a --.- %?' * - - $ I A : . dh+??X? VKG~T"X"T'TTT~. . . . . . . . . . . . . . . . . . . 1;"3;1,:.~ """C - GCIZB STAR B r ; ; i : f L y i i . . . . . . . . . . . . . . . . .
.,.,. -~ '*i.t".:\t: - L,C>U @.ROUI~. . * . . . . . . . . . * . . . . . . . ‘ . . . ...
c(- a,ch ;:vi i, C ~ ~ W P . . .............................. Ck'NL,,J.L C;XOZS)CY.. ....................... ,r i -1 " ' a.dt:r, {,L*GY r3F 4!IA CR.EF;Pk SIiC:' LN:.T. . . . . . . . . . . . * i - ? T I 7 . . ...... ?2 ''E:THgCSDS .. . . . . . . . . . . . . . . . . . . . . . . . . . . . . : : , * 1 3 5 t , l ' S . . * . . . . . . . . . . . . . * , ' . . , . . . . . . .
I I . . "_"r'.x:.. . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3"f!XFJ:1':;'?1~6 CfP. . . . . * . a . . . . . . . . . . . e . . . . . . e . . a . e
. . . . . . . . . . . . . . . . . . . . . . . !+'i . <:r ' :-+TX-*).LClt23?. I ')- " '~ L * X b .... : :- . , " . j! .. 1 ; ... i " ? - ! . . . . . . . .
. .................................... -l if [j - j " 6 1 4 ~ : j P . T . 9 1 ' .
CL & - < . ! ~ . ' Y * . . . * . . ' . * ... . . . . . . . . . . . . . . . .
............................... "1?! ,':\ P. ,r l v ;:~":~71~~~.*~,+ ;? i f ; ~ ~ ; ~ ; ~ ~ - ~ ~ ~ r c : ~ u Y . . . e . * * . . * . * * * ' . * , 6 5 " . +
~;<:~l'~?cL~~7:!$xc~N:: :%.i84r> R E c ~ ~ ~ ~ ~ . 4 ~ ~ ~ ~ ~ ~ ~ ~ ~ g ~ ~ ~ f,, e v s , e . . , :il?;l.C i3vld4 li Y C.j;' I:":$ 21, h?G e.7 7 3 13 tl.fj .5., %;G 11 4 3 . . . . . . . . . . . . . . . .
:-:ci'iF,, : ; ~ f i , ?"i,c:;.. 1 . . ts"91^1. NC). 2
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GORDON P. E. WHITE & ASSOCIATES L.T'T). =- CONSULTING GEOLOGISTS
- -- _ . _-"_-_ . _ . .r;n S ~ L V ~ Z ~ S S V ?B 3 1 1 ~ ~ '3 'd P . ~ O ~ ~ Q S
u n ~ 1,.,17332{ l s n w s s v o d a u uno w o r l d SLDVMLXI a N v 5 ~ 0 1 s n ~ 3 N 0 3 'SLNIW h l a 3 d ~ ~ d ~ V I L N ~ ~ I ~ N O ~ SHL sv ~ I L L I W R ~ S 9nv S L H O ~ P M i ~ v 'SIA~SSM~O a
" ...... ,, ." ...$ " 9m..... ."" .....................................
f 1YQd32i lN3\';SS3SSV
se3ancssc,r wnelod+ed pue sau!W
40 +uau+.redaa
4~ " t z dnQJ'EPD n07 %a$hlk 'E:~-E-;?S~ 9:"."rN
I I . I il.IlOUD 8 V l S CTTOD ':\?%?>;:-:: ~p ~ : C J N 9~
< . l d I I d l l i ~ H l f ) 8'dV;s;S C;I?r313 '::ci N;;% 21. $:I>N
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*%;I"! (" r 'd q -2 41-,3; J , 5 " i a t csi ; 4.3119 XVAS aricx~
~1'43'\1 bEr'3ilV301 m O :+. : \ . ' x f 4 i 7 " 3 Z:Q!\J 7~
" { i c 2 -- 1 rrll.:.,2lC kr 'ii J'S CT?QD '4 $,y$ ; $1 .jf*a:,a 1 : aka
&Y:.13*3c: :;dqLq' 6
I i " " " " I3~03) SLN3 J,,N33 d ~ T ~ V J ,
This report covers the recent f ield ,worlc b y N e w ~ ; ~ 3 ; 1 ! >f.a; br ines Y,td
personnel under the management of Mr. W . 3. '~'i.1 t i , ] , ; a iaf tSes1im?3e
of previous exploration on New Gold Star ' s G.ild ,it-is c! 3 ; I I J ~ O i l ~ ' , a s
, a we l las recornmenda t ionsfor the 1970fic;l .dseaso:1. ' " ! ~ e , I - : . T ~ I ~ ~ ~ , >
drilling on the Lou Claims was contracted to I;leeg 2,x-i I1 i ~ 1 Y . j f I X * . I I J ~ > ~ > ~ S .
Map No: 2 accompanying this report as t raced f - ir..? .\ '7. ter~
photograph No: 40'32 44 enlarged approxirn.cztely tvi c c a i , r l - ; , , E L : _j t : ~
were plottec' from nylon chain and Brwztoa s-arveyn. 1 e 2 :,E r. I ~e i 0
magnetic declination in this a rea i 6 N 28 E.
During 1968 and 8969 5 and 12 days ree2ectively weye i-;;;e% F, r: t ) * e f 2 r
Star claim g r o q a , while 6 days in 1968 and 196? >\e lbe sr;cilt 1 1 I; i e
Low claims and on Lou core.
Reference has heen made to maps and reports h y Ges- 'T ,-l~.: :eF'..- .> - 4 < the Gold Star gronr,r a.nd in particular to e reptlrt ( 'ate" I ' I ? Y ~ * : ~ ~ ;t-i
1867 by Mr. D. H. Cochrane of Geo-X Sursreys.
C9 ibe reported clai1-n holdings of New Cold Star Mines i . , t~ i r ! I'pe i i :~ , i w
h4sunta.in and Z'iankin Greek area , herein designated a#?; t *e c 2' "*t<>
grorlp, are as follows:
Gold Star , Gold Star I - 19 iacl. , 30-39 inel. , 99 - 514. i o*fc'. r 1
Eastern Star, li;=as"eef Star 1 - 39 inol.
ZS'RT #I and #2
All; #1 and $2
TO PROTECT OUR CLIENTS, THE PUBLIC AND OURSELVES. ALL REPORTS ARE SUBMITTED AS THE CONFlDCNTlAL PROPERTY AUTHORIZATION FOR PUBLICATION O F STATEMENTS. CONCLUSIONS A N D EXTRACTS FROM OUR REPORTS MUST RECEIVE OUR W R I
r GORDON P. E. WHITE & ASSOCIATES LTQ. I I
CONSULTING GEOLOGISTS
The Lou claims straddle Cedar Rivcnr. ap:~ril'bxi< 113; *>By 5;' I L ~ L F C ' 'tturtk~
and slightly west of Terrace in the ik~*r~uni-t ' t l i n i r n p j 1 l r r t i ~ ) n .
C IALU A T t' -*"
Hcavy rainfall and deep winter snow in hi.gl-~c:r :~~(;l,;.*t-i ii: I'~:~'I~YIG i . ~
csrn,=onpliace in the Terrace district and he1 is-orst:s r f . ~ i + ~ ' k . l 3 i ) r . i ~ ~ 5OFl
feet elevation is ewbject to rapid change fa clvurf ;.ad kt- fog c ~ r ~ d i l i . > n s ,
l'letablcd study om winter snow conditiora~ .,waald be C * 91. E t( 1 k ~ t ~ f a ~ ~ . ~ * ; + e l k
statement could! be made of the pssaibillty of cuper;~ti:t!~ 81.1 om:;.*; : i l - -ii:r
during winter rsrcp&.kltB on #itrelas Mot@%taa in,
' T O Y J t y C , R h r-'kB.'f A lq3TQ VEGETATION -- .---,-.- - .,.- - The summit af Kits elas Mountain f r reparted to be .ll;.i? t'6 ii- p r A ! , l e * ~ t ' ,.,- a
level whirs riie lowor camp i s at an elaaivation 0% E 970 fee t , f ave iige- 0
slope of the .r~ioa:*kain wodd be about 3%) betweera eno. 9e.xt ,.nld t'l~,l I:* b g : r
camp in % straight line, and although there are s t + ~ a s l i - t ~ . a F f I"ia't ?'r .x l t
b .. 3 " vertical cliffs stsad steep box canyons, czesene: part r a!' t . ) r , % .-Lr.;1:: -:I.: * + '- * i Z1r
arccssaihle on, f i ~ s k ,
i"hc tvorhrh 0$11 Oh@ is1>a clair:ls w a s carried cr-at: in tlw L,L.*~~<.,:,P~ 5 t ~ - ~ : I G - k t L' j 2
the hills on eiQkey aide of &be Cedar River are rstxitc ~ [ P F Y J
V4eav-y stands elf B V B F ~ ~ B B B t r e s ~ are present (lsa bath ac:la*: a o r & a ~ i * . r v ~~4':. rr* )st.
.ra,bovc 4000 feet om Kitockos lviovult~in where G~eea becob- 1s. t(db14.,,6"r'-X4.1
TO PROTECT OUR CLIENTS. THE PUBLIC AND OURSELVES. ALL REPORTS ARE SUBMITTED A S THE CONFIDENTIAL PROPERTY AUTHORIZATION FOR PUBLICATION O F STATEMENTS. CONCLUSIONS A N D EXTRACTS FROM OUR REPORTS MUST RECFIVE OUR WRIT
GORDON P. E. WHITE & ASSOCIATES LTD. ""--- ---
--- A
CONSULTING GEOLOGISTS ----- --- -
pp-p-
3sorrpccting by .Hen Gold Star X.Xiiu.ie:, rgeea"b,t ,r ,net , i,,, b c r ' ~ ,, I i , t C - , t < ining
and copper anrir~eral~ over a wide area on t k j ) ~ c r . ' : i f r8,s?- + , n 1 f - i : j 6 i : ~
part w h i l e ;:eurr.nlng for eogpar ~ l r ~ s r i i s p r .;cG ~L:z' ! ' : ( 4 i r i 1;' , :* r ' c .~or t s,
> " ,n 22 foot chip e.arnole Lakenof s.ockErx g~lw.ca c ~ q e , i ~ y ~ b ~ L 1 I A e 3 5 - i ~~ . i~ i
P L ~ 0. 1 ae;/P and coneequently a f ly carr?rs \ V ~ L ;;,-20;1:3telj lipC . , t v \ ' K ~ J I * :
the 3900 to the 4700 foot level where l,ie\l i n ~ r i c " 1 s, C X ~ : " I $ 7 : t , f ~ r ~ . l l ~ r ~ ~
blarjrtcd nr-c! krea<:'ncd sreaa were made i n $(*.'roc. ' + * *r . 8
;:I '
ats.??rhcd l e k t e in Or?~e season and chip, gssb end, i;, oil.! . - 7 l l . k c 1
s a i r ~ p l e ~ $&ere taken from the trenches and s e d e ycg;. ! : : j $1 , 7 - . I
mapping w a s startad in these three areas 0% trena:hio,., ;:r . $ - 5 : i.'ll; , , :#
and C son"^.
ucovered by orar%pscthg wao trenched, blabted, sarn:lkzc ;;nd n : . ! ~ ~ ; i ~ ~ t . * i ~ LKI
, . oh averburden sad ;.bedrock have been dieplz~ctbt. ~ I , . J ~ L i . \ f - - $ 4 ~ :
D.nrisng &Et$SE; ,, g::.ir! l i i r~o~ soil 8artsb:pIing for c 3;. pblr z::" '
h;r~ii;t cb the trenches on<.; asBay F Q I ~ U ~ ~ ~ G of t h e ctta7rcwt L r ~ % ~ ~ ~ > ; i ' l : ~ , L I P C ' -
v.4 hiave becu plotted on mspe a e ~ ~ m ~ n y i a g th ig i ; ~ j ~ r ) r l . , $ 1 4 - 1 ' 3 ~ i s o $ 1'6 yr8*u
ttu main trench o n . $ 3 ~ * ~ g'nx.ee1.t. East af :.ill r,";l..sckki.
.;?lavatian, near 62% .t- 8 . 23.E ~ o n the grid, 'i% trar"rx st : Qif ~ + y : -6 9-
TO PROTECT OUR CLIENTS. THE PUBLIC AND OURSELVES. A L L REPORTS ARE SUBMITTED AS THE CONFIDENTIAL PROPEHiY ALITHORIZATION FOR PUBLICATION O F STATEMENTS, CONCLUSIONS A N D EXTRACTS FROM OUR REPORTS MUST RECEIVE OUR WRI
GORDON P. E. WHITE & ASSOCIATES LTL1.
- - --
CONSULTING GEOLOGISTS - - - - - -- - --
5
b l x ~ s t c d orat on a eteep slope. f + n t i5 C ieeek a w*rei iC. . I i [ ? 3 by 4 feet w a s
i 3 rrkade irt, a ~ ~ ~ i n ( ! r a l i i ~ e d area. YJp ti) : ~ ~ ~ ~ f - ~ : i , . . : b: "', :it) t;;yz of
i.n a"$,:,. i . Arrkex axad 6 c a s e s of powder vi'erc! u~.. ' 1; . ! * 3 i r C 6 ~ l n d tile
w o r k was 1.1 progress from k ~ i a & period uLL i l < r l 'c. ,., . a : < ,
Sawrtple~ of ,r,irsrlralined rock t~ic r e su!si-l~~t': . t c : t., - ' :I> - r.f rf 6 : a i r : of:
Geology at LT. 13. Q;. and their finrfiligs~ are .re:ri:--t P I, .iiaz-r ' ' * . ; f ~ l ~ r a l u & y . ' .
E'P.LL2 ::$ C* xClS - LOU GK4=UT7 -----om-
Blasting and trenching 40 by h LeeL, 60 by I, feet 2.1 i t ; / ' * 1 f+.?i al, i 6 t :
20 bag8 of Amex and 3 c a r e s uf powder -\ltas f ( a l l i . , i , v j c ; * ~L,L?< ~ l ~ b ~ i ~ ~ - . c J L
mapping and 1000 feet of AQ w i r e Pine diarnsna cs r ~ l l j r . , , ~ irai .J I ' 2 1 n i L Q ~ I I :
in ~ i + e e ~noPes. Several sections sf core i v ~ r t : ; x ~ i i a y i::! Ai3'.' I, ( a r i ' E
locations &rat! tabulated aoaay results are recor dcd B ' ; i A r , :2 ;. -; ,:. . : w I Y ~ ' , ~ ; J
this rre-z3art. ('-leaee see M a p No. 6) . 2 . , 1 t .ti,&
accomr ;kny this reyert.
General C;e&m - 'T'ze principal rock w i t s frsxxx .?le?.nx,fi t ~ n - i ~ g ' z : c
f r i t~e las .F+# :lqii.~tain are ;ixzdesi&e and b s s a ? . ~ t & ~ ; a : he , <> t ia* I %
. , 73orphyritle gailbro and a siliceoue, cherty, quart;,lv:l: a , &! ~:i~;;g1~3,~ic. r a t \ .
series sf nrxetorn~or~hosed sedimentw . &.I1 u;~lt o inc"hLc 6: 5 - J r ;i i:xrr~c;e,,," by
black basic: dike socks possibly saeociatad w l k h tinc: y, : i 7 \ . r y p i f i r : ~ Q ' J ~ o .
aikeg: and rjnxul.1 plugs of grandlorite intrudes.$, t,E~s a, cr 1 i".i ~ i * " ,, : i l I - 11 : i~ it
b u t : p i a ~ e not been ceen an npper Kitselas I *?acantL,i a, 1 : . FA n L- ,T
sltka:,clrlgh only ane traverse w a s mads acrsrse :tist J~rt".cc * I !;+ . L e ~ iy tr .
T O PROTBCT O U R CLIENTS. T H E PUBLIC A N D OURSELVES, A L L REPORTS ARE SUBMITTED AS T H E CONFIDENTIAI- AUTHORIZATION FOR PUBLICATION O F STATEMENTS. C O N C L U S I O N S A N D EXTRACTS FROM O U R REPORTS MUST RECEIVE
GORDON P. E. WHITE & ASSOCIATES LTD. CONSULTING GEOLOGISTS
?V% ;.ire volcanic rocks outcropping f rom tlra b r i d s r or: I > U r r 9 r ii 3rkkl:i < * r e e k
to tne area near t he lower caui~psitas ~ a i i ; d i i i 0: , i : f of
green, hard, fine-grained to aphinilic, f e r r o i . ~ , , ~ ~ ~ , . i:i. t,, ;; *.g t l 1 3 % r e e n
weathering andesitc with 1 to 3 f ~ o t o v a l p ~ u , L C i k:!;k,rj 5 A & + i t le i i ~ ~ t r lenses
ard 1 to 2 inch vein8 of a yellow gxeanz i n i l x e ~ a! b&i,l.r:~ ,::J *, 1 ue air ~ P ~ J X L -
ricbolivine. thctions of the andesite ore p0rt, ,ryril:1~ J 11 , '~ k i i ; t t t , ~
rr~ediurn groiued, pole! lathie of white fcldsnar, ~ b . s t ; r :'d 'ri>i;fiel J I ' D ~ C ec3
in an aphinitic green matrix. &h,guetic, bla eii, a 3 t 1 ~ . , r L? L .. ~ r ~ ~ a i ~ l t * ~ ;S r i d
present but the predonrincmt rock t yge i a aa nt-sde~it~:. : i - ', , L r u r s ? y Y'
reported a~"rxyydulas and crude pillowa along BL t ' r e a k .
'rhe contact between the volcanic8 and the overlyin$ (chethqks : f ~ 1 3 ' 1 b , L , Q
report dated Sc~temoer 12, 1963) metanlorphssed , ~ ~ b i t r .enB,r. ;.jipc;irss
be gradatiurarcl ;zlmd snarked in part by a fine- grainatd, j r r pw:r, c x = c ~ l r . a - i ~ r , ? f i 4 c : c 1 ~
f ine ly l a ~ ~ i n a t e d , andosite sandetone containin:4 bsc.,aa lcail%i,, s , cir *-:I 2 ar",
f i ~ c h plus, granitu pebbles a s seen in outcrop 205 fa(:, ;- : o h P I \ $ ,iii~;
Cz.2e.k on #6 Creek. A nlediurn to cear se grained g,%abr o c::,-u; ~ : t Lei;
regirsn of axid -?arallei t o the cantact zone, prubably i ~ t r ,,,; e k , .zt. : I I + ,
W T L-eas: the source of $4 Greek the gabbro becarmes very c o a r a ~ G"-;L~;~LL., Z~.I?!
xriatsoive in appearance. Black dikes of unhcrwn ce.sr-~>poritio~~ c:i-r-vi* Im al!
rock fyneo 1;3tk~ough tfic ralstiors of the dike$ Oa the g r a ~ r c i?!,~ .!'. ' b I. v i ~ .>
%he limit8 of the coarsely osrpklyritic gabbro at tnc: head ) J : ' . ' i ? & 7 E : h n L*
I I not bees defined in the field but based on ths ccrarat? ~ s a t ~ i :,- >bf i :- : I ~ : I . ' ;i I
pfzanocrystw set in an aphinitic, green srratrfx, t.ha,st-c is -i) d b 3 y 2 7 x
ci:n\,->ida.rsblo body z l l gabbrois ruck preleaent. A u p ~ ~ ~ i n + 2.t r i . ~ ii
i ~ v c ~ r w r d over the gabbro rtnd the gahbro tn i i y :,,e :.*B
**am.rut.lc:l tun time corata~t cone which strike& a g p ; ~ ~ s ~ i ~ r ~ , 3 t t ? ; J ~ ~
TO PROTECT OUR CLIENTS, THE PUBLIC AND OURSELVES. ALL REPORTS ARE SUBMITTED AS THE CONFIDENTIAL PROPERTY OF AUTHORIZATION FOR PUBLICATION OF STATEMENTS, CONCLUSIONS AND EXTRACTS FROM OUR REPORTS MUST RECEIVE OUR WRITTE
GORDON P. E. WHITE & ASSOCIATES LTD. -
rrvc tsadkments ara probably in uxz+:.;s of 201):;1 f ?, r . r . * , A, L ;. . % \ r i , ~ b ? ) m a
aea consprihed sf greyuvacke, r j u i ~ r t ~ i t c ~ l i l ~ n i 2 . ' ~ ; . r ; \ ) i f t:;;xt.:$t: -!fit$.
ilndelaite aandbtoneer, coarrely bedasu, us,~; , l ' r f p S; ; , + . $ , i r ~ i, ~ * , i , i y
sorted, S I - Y L ~ Z S P B generally arilicsous ~adr,a,ti~~.a; 5 , j r a ,<; r .
and pErti.a%Ly grsefeetic. Ghrert i s fairly ~ . ~ r , - i i ~ ~ + . ~ r r ~ ~ t t ~ ' I * . ~ n,' I : - B , . . ~ c I * YL.
which kaa coarse cong1omerat;ic irct L-.:oz~L w i tii i r ~ l ; ,uia t . $ 1.. ; 1 9 A 9di
sr;";?.ac;.cd % inch to 2, inch poorly sortt.6 fr4s$;ric;i.k:tr , , * s I a [ k:, .
weathering andeoite aatndrstonas, fairly r m i f i r ~ i ~ i i ~ t l : r v i , r i a i + i +;;, ::a*& ur i n
20 tcr, JQ foot thick bed8 about every S Q , 3 Es?itt ill YO!.: . . * - , ,
Tns r-rreta.~.~.s<, .;xisrri of the ~~edimenks has probably r2;;c:iha . r , ,+ : r : .- r e r - c
related to major 8 yncliagll folding statig a aorthwc83B &,;L* I , , - t . ,-x4 : a
attm:z.nkPt of Kitselas Bdtauatain, Dip directions ;arf2, .Y i w a 3 . . i d J + ,-;
steeper to the scstkth and aouth9rst; on &a uppet .t*,"~sji.&& L , F ~ ! . i ~ ~ c ? k , , ~ ~
f:-o.rr ~rriginal bcddkz~g phk~ers but the =%'?<ifS foot c % % L i i i i . Z i l i :'it T ! - , L b & : ~ a * x i
0 3 3+' schi8tc58ity strikes 80 to 85 in one saterap wine % t:h+ : : ; i i * c - ~ ' ~ , . L v - , i l ~ i !
and ssblimcenri;~ as sxraaiit dilcrsa as 30 to "$0 Isot uXwg% ; i~*tai 3 i La * A A t 3
i?rr~~~.a,alia~its bedde8~ iiava beeti @@en above tile + B G ~ ) O #"cat)$ j + : ; i , ': t , r +
a.rass trawerwsd, iirlthsxaga pegnxatkte-like arr&tet*igl vv t, r 8 , v r , , . ! c ~ :
~l.i;)cbilt t k ~ l e ? ( aPav%t%~s*
'1:xci Zikas %YH ~ ~ T $ Y ? C ~ I O U B ia the $f&djrae~dib 914 ~ , i i f k ~ ~ ~ " , ~
4 . 3 . f'.,,:'r'i?'lg ~ $ 8 81 -;;;A1 9 fool plugr;, 69 foot widti di'r6sn
larger 50 by 100 feat rnaases. Tt:c . r ~ ~ r ' i e ~ t c r ; l i r \ - + , I . , >. b r 1 : & * ' , I J I C , : ~ ~
dikes' cnnsi~t of several varietie.; 3% d d ~ l i r'c.)ch, ' g I i j t < 4 f r*~le f 1 1 y a l
and alteration eharactariestico. T'aeae r:tj : i e : * 4 : 4 l . t i i. + - P. P . . 1
nli.cra brown, so f t , altered, blocky, b3ac=l~ wb+: 'LC: i i ... $ 4 . ' a ,+ ,I: y ! t b ~ -
biotite s?i ehistoee, green weatharim g ~ c ~ ~ : l e , :.r-. a l - t ! - , g r : L ,
fine grained, didonee-like rock cnutai.nlrr(-. t ~ T - ~ ~ ) ~ ? ~ ~ ."" , I 11 b - 4 , t IoscJy I I I I
packed, plagiocllasc; crystals, and i 12 a bl8.r.b, ~ . $ I u : ~ ; v - i ! , . -I.. C a l i ~ ~ ~ a ~ t - like rack. Upon first observation the achi s t n s a , -.I I r i =,$ E . ' , j j 8 : ii -k
~ v s s ccn~icxered as a possible i~terhvclciatt u e d j ~ i ? . ; ~ t k t ' , ; , % atl
ZaLea' . A ~ o . P ~ revealed these small bodieg (i; O by r , t , ; ? ?
nowherc, S";rtx:e E,X &I1 of these rockg t.rrky be c: ~i>:.l ,ae:.+ f . 2 . 1 ? ' > ) - Y
ywhich ;s 13ra~~l2rat below the 3700 foot level OM ?<'a;fts\i'a ; I t , i i n r ! ,
. . CGa~tbir~g and is.errr:hi~~ has expaeed a pas t:.ible k; ill . L ? l : r i . - ' ' jr: , ! . I
3 % r * . \
0, tG0 fact in strike length IN70 EE) where e~.pohc??ti i i i P , $ - i t * . $ t?: ' f ' t , r - i
? IQ trae width, dippiyiy JU noi-.thwest. The: ~ P . D $ L * $ . I is 'F. .r!:t l I::? . I c: l i is ii;l
, t S andewi~ea snd k,a.s;nIts ipnei 2" to 2 fast: wid^ r"asi%"r:r L ~ L I . . > ,- , . , t I t :
acs.om~panir;d oy Iiiirorlite, gucrge aad w a l l a oo:ls, L V i'",hiqrcq
aiteratiau ii3.u changed the ruck to a soft* b r ~ ~ v ~ F r i , ; .. ,- $ , J , ? t
r>;tli.ex"*;'d L ' O ~ .C +ir* L & * I ~ ~ r " ~ t d ~ t ~ ~ \ e , ~ i l . ' t &%db~ ~ r f ,:':" t s ~ h ? . * . . r e ; . ' .
.". L 4 ~ Z ~ -. i s -altered3 ~tnlphidcs ara not visible d-o I!lc LL.! .. ' .. - ,, - a 4 , % a
1 1 L * i r y i , c S c 1 i n faalted aonu cornfcaindng limonite and go - r A C , r * * /I 1
I
I
TO PROTECT OUR CLIENTS. THE PUBLIC AND OURSELVES. ALL REPORTS ARE SUBMITTED AS THC CONFIDENTIAL PROPFRTY O F CLI 1 AUTliORIZATION FOR PUBLICATION OF STATEMENTS. CONCLUSIONS AND EXTRACTS FROM OUR REPORTS MU'rT RECEIVE OUR WRITTFI* APPROVAL
I .--- ".--- -. - -- --
----- I 1 GORDON P. E. WHITE & ASSOCIATES LTC. ~ - - - ~ ~ Z = - - ~ - -:------- ---dG
- - CONSULTING GEOLOGISTS --
II 1
F ,&A4 -LXXG kIFTFIODS --------- Channel and chi? samples are not sl~aor!:ed - ~ 1 ~ 1 e 3 r "' ;' f % I + safr-k in
place. Crab tramples as defined i a t thiza :-~-mctl-i- : : .=a? 6 - 1 1:7 " 1 s . 1 a -* . I I + (IF8
taken at 1 fep;>t average intervals i'r,.r .: r f z , . ~ ~ ' . 7 t ~ l y :-::I : 7 t , d l , < x t . - f 7 1;6s7.j
rock averagirxg 4 feet in width avid 1 fael in : . i g - ~ f j , -'-, ,*. . - . . ." Li?.ib
type of sa.n;plinq was to give tsornc i.ikdic'.iti~n .nf t \ o l c , r 9 1 ! > - % - "-?f11'"~
t he rock becnzna coverad with snow. Tlre c.i:.z?lnn*tF ,\I," F41 +I , . : 2 % ~ n t $
were t a k a at 10 foot intervals acroan a tyeni; '~ C ~ ~ Q ~ L ' O i i. v t t > j 7 l t ?<'.ta-c
bv./)tere the t ; rn~ wag read incarreckjy 5eca:x:se crf qs:,rstb - t . I*' 9
, I eye-qlaen,cs, and not for any p r e f ~ r 3 % ~ <:LLX?$: I:> J 4 . p , t , , . : * , A *
eelected interval had been w e d , i. E , , 13 beer. in?! p i c : , i t ] *t d ' * ' T t : ~ ? - . 1 (1
- < - width of the sa~nple was taken aerosa thr;: tre.qclr :17;s3'.L;.: Z L i ( b : 1334ml
of the I;-L;neralii;otfon. A cornpariaon of grab r 3 K l * a y Z T 3 ' - :" :- -, 1 .Lac? - r ~ - t s J i ~ ; ~
over tho approxlxxite eame dietance i;rz t l . ~ CFLT?kt? l,:rai:ft-~: : a **it ;t
a w follow a .
, r; .. A feet ah cinips %r~~^a l blasted ::.ozk -. r;\ rzs gt ;:: . , - I,a : c if 1- aft
I I ! ~ : c z C - I ~ J . i c rr;ineraI ~331~~t3+r& of tha rack. I I
TO PROTECT OUR CLIENTS. THE PUBLIC AND OURSELVES, ALL REPORTS ARE SUDMlTTED AS THE CONTIDENTIAL PROPERTY OF CLIENTS AND AUTHORIZATION FOR PUBLICATION O F STATEMENTS. CONCLUSIONS AND EXTRACTS FROM OUR REPORTS M U S r RECEIVE OUR WRITTEN APPROVAL
"- - .-- . - - - -. - GORDON P. E. WHITE & ASSOCIATES LTD.
CONSULTING GEOLOGISTS
In the A aone, on the 4700 foot level approaiirr~~tnlur, I C - ~ Z X ~ L ~ ~ P ~ : :'-m 11(-415
of average horizontal width 3. 8 feet (awe rage 1 x ~?rlcl: v+i c i ' i I ~ ) cavc?sv 10
feet weighted over 102 feet aasaryed Cu. 1. f"r?4~, i r (k f * C , : t . i h I l ' f o f ~ t
c:ltp sample, appruxintistely 280 feet ) 1 . ) 1 110~4a11'~ 1 ! ' I : : t , : ~ J I ' ~ ~ , ~ > : ~ t
1 5 0 feet vsrticatly below, not in a t r enc l~ , srsf iaucel C:rl. I . ' + : ' , Q i j e 1 a > / t m
hJIinesz~liaation OGCUXB in trenche~ between thebe t , 1 9 v b 0 , F a r ? { hai' " : n ~ ax.act
limits of the fi?.i~~eralieation are vuicertzitii, L ; ) ; ~ G T zg.1, pi s :; ,:-. - ,~ ie
adjacent t j - m c h ran, 32 foot chip, Cu, 0 . :;)ITL7,, A::. ?I. '1 I t . , A i t t , f L- : - . L ~ X J V \ ~
Cu. 0. 325, Ag. 0 . 4 s z / t . 20 foot cEzlp, Gu. 8 . J3%, L ~ i l . . 1 * k , t :t
extensianra of tns main trench in the A zone, rtssagrn rai-: ! f , l 1 t: a t > ,
> i Cu. 3. r)87$, '$3. t1.2 ox / t . , 60 foot chig: Cu. 3. '>?!', c . 7 : , r s . 8
preli~ninary earnyrling m a y indicate a sons apprcximatalv 2 i;: tee? . I < ?
w i t h a preiitcut akr i_b.e length cad-ves t hif o v e r ?&!i isc!t - 3 ' i' : ; e 7 i - 1 k
e,xpreeeisn of a? ilcsa~lt 950 feet because of the b ; ! c s g r ( I. Je CL::~". 5r.e
?,Tap Nia. -2)
In t h e B eanc, 89 feet of grab sampling %row? Lf a s t e t ? sr-k . a 6 % .tll
Gu. d. Sick and Ag. 0. 8 oz/t . Chiunneb earrtyjea in 4 koi ;" " 2 ; ~ . 1 ! h ' ..+;jnyp<
- 1 "I Cc. 1%. 3 2 5 , ,%g. 1. :! oaz/t., over 4. 5 feet and Cu, f:, "17'!:. , - * f ,
ever 5 . '7 Feel;. Tranclms above these tv:o zclnc,~ in a 73 " I 4 % i . *, ' . P ' 1 '., . * * ' 8
At?;. 13. 6 s e J t . , 35 f ~ a t grab, Cu. 0. 12%, Ag. 0. 3 c7aPt:. , s ! t t ~ i . is ;.:- ' 4 t 2 ~ +*.
on a 2 5 foot vertica! rack face, Cu. O . O 9 % , .A:$. C. 4 O Z J '
h 15 foot gr;> flr j r n a trench fxa the C zone ran i=u 0. O;4Y,E/i. a ,, a . . ' 4
( T h e ptrsili\m o f the A, B asid C zones ara sb4:uxrxa r,jra R": .Q,~ . ,G. * " * j . 2 > a -
.-, ::i-!'l,t ~: r rzp ie at t?,a t7C8 fact l ~ v e f in t h e C r r h ~ ~ g : ~ c : t : v - * i i b
+ ,$ , T: r$rl, Pr>??r~n!ke ~ t a l n p d roc!-, r m Ca 0. 03%, . % f l ~ f t . ' * f , . I .,t---.--: ' I (GI - a , 8 -*.,
1 ' ! 6 : . - .;\ & - -- kJer: ' " a ";
I :-- .- b . , - - , . ,:, 4 - %
\ ' -J L u , z
I
; " ' TO ..a TEC. OUR CLIENTS. THE PUBLIC AN. OUR..L,ES. ALL REPORTS ARE s ...IT TED AS THE C.N.I,...Tl*L ... .... ,b:.q\J:,,,,;N,;, A U T H O R ~ Z A T I O N FOR PUBLICATION OF STATEMENTS. CONCLUS~ONS AND EXTRACTS FROM OUR REPORTS MUST HECLIVL OJR w b ~ ~ ~ h l L h ~ ~ ~ 6 ' v ~ ! ,?'
. . " J - .----- - - - > - " "" 2\:>;;~*2&~<""- GORDON P. E. WHITE B( ASSOCIATES LTD. - ^ . - - 7 - - - - - - & , --- CONSULTING GEOLOGISTS I I
subrvlittcd for 30 slarnient raaxriiquax~tita t it L:: t, p c ~ . i . " t . b t h u , ...I $i 3
indicated r3~21y P ~ O M B ~ O U B copper ~ r t d 9 i l ~ i ' ~ " " .
nq IOWC? Td-itnel.;iw St'io~mtain at anyr~*oxi: atl-'hy thc i , p ! l l ( Y ".i t el t , ' & * ; % " ,
#&.A creek, a xve6gtited aeeay of 6 . 5 fee?, :>f ra.l=?ts*r: kv IAI. ' r . r m n * - * : , I 1 >1.c
and 16 beet of soft, altered gouge a. i&t; te~iaI , botv c i*fs~nrl i rJ \ * : , + ~ T I T ~ " : ; rse8js
/I,., 3 p t - l was Gra 0, 2 9 XI , 3 g 0 .4 os/ t and Hi C r , ' i;e r c* - -. other and erouthea~t. wide of #4h <;reek beck in s1terl;r.i I ~ V I ;IT r q 2 i 7
Cu 0. 07'ii;,, Ag 0, 4. QJZ /t for 17 feet; and C*z i Q. 85"a, ' y, ,.E f a , 1 ; e i / c j
2 foot: ?rkanm.cl sam7la of limonite :~.n.d n.lscz r:s..:gg.$ .- (-7 , \ r .:; ; ;a1 ,?'.;$
-4 1 5 foot ch i ? sample on #4 Creek at np~rcswim-r3t- , t *~~~ V?= ' . Y 72.:.t,?'1
la gabhro s ,ee3gec: , Cu 0. 3370, Ag 0 . 05 oi: / t .
**, , , <- 3- &, ,,.J ,, !a'J,1*Tps'!3 PTS --- - Cc?y??bir and silver neclsr as fracture filBinr.:a 3 0 4 s, 2; % - itc lb-triL i r q :
~edirnernt an ihr~a lespyr i t e and bornite arc.! p r ~ . ; g ~ i . . i # ~ . #;. , 1 $rte.:P. s .a;
tv yak.; k$l~~~:$e:ked~ altered as?d contain I i rnr~ni t~e 4*7.1fi R F~P P; i: e t ,*
? I PZnd, fins, cl.oeo1.i; saaced Eracturse.
C s . i ~ r to tye~).~~kgin;y +1~3skyirjg~ t h e 0reJ;j 2virlasr.lc. .!. ~k I :
rn , ;:r*b?ae&lhi.ts ?;:r).,ix: -32d UCC~=%~~~~C)XI,&'! b ~ p r ~ f k ~ f f i l f ~ c f . f ; 4 3 '
TO PROTECT OUR CLIENTS. THE PUBLIC AND OURSELVES. ALL REPORTS ARE SUBMITTED A S THE AUTHORIZATION FOR PUBLICATION OF STATEMENTS. CONCLUSIONS AND EXTRACTS FROM OUR REP0
GORDON P. E. WHITE B( ASSOCIATES LTD. CONSULTING GEOLOGISTS
A zone. mnaralization was oboaerved in t-he esdirncntu as w e i k ~8 tn ;ant2
on the edges of the black dike rocks. T t a wol li :0 <!i~t e L > I I ~ : , I E C?,S a
correlation between the inten~lity of dikes arid the riejzr'oa OLL ~ n i ~ e r ~ i l i z a t i o n
and that the gabbra is the rsrource rock,
I?n 11 Creek st approxin~atelg 2600 f s : t . ? t , I rb . : : l i t~ ; "; * L . 3-C. . ; i i t~ B :e
found a e dise@minatisnrs in a porphyritic g a b l r o . The suXpl-ides I<avt* ;.Fie
appearance of being original rather than tr;:rociixced.
MINEKAIKtGV ---- Bornite and chalcopyrite occur as diel~~aminrationta arrd f r a .nti!.va -till i r ~ p t.;
acc~mp~enied by secondary malachite and dark spatted ole$,f r tnq.r i, 7.e
dcr~r lwi t ic ci"c:~:nBai;ioa~ believed to h e a fc+rn.': of CI-,:~:~,?J. 5 '1 .- ; ; ] f r . c - ;,: , sediarlentary host rock. Bornite, chalcopyrite and pyri te (.;-,c.v.ta a s s'i,ne
* s specks, Intimately associated with mafie mliiner~r~l.~ ZE r: F C Y t l i5 I i t ; ' : 3eL;!22 J.
to the Departinsnt of Geology a& the University of" BritkslqL 3c 1 i ~ - l , t i i i t m i i f
chalcnpyrite ,%rid bosnite! were identified with B B C O J I ~ P F ~ ~ e:ict!: i.r-rhldi, a:;.r37rk . ' k ; i l ~
and limonite. lda,gnletfe i e present but rnaybbe oripiasl ~ - ~ ~ i : + . t ~ r . ~ 1 . e
the rre&rner%t.
g"atcmipts were rrlsde. to determine the nature cf the si&vcr r u ~ i ~ a ~ , ?.?j 1: -es~1,1t ,
but Lhe quaneitf ea present in the empleh~ w e r e cons iderer~ till: :. n,\II, I<: b o - .
t2ekarrrL;ned by paliedled sectjomi a-nsthocl~.
ECONC hi%G GEOEBCP ----
sxibc:coaicar-~3ic but ss*m?. to i ~ d f c s t e a different E ~ u . ~ c c ? ' and t !%, t ; ,'I , % I '
a1faoraiieatia.8~ tllzaxz hjllrsr hitherto been sl~nspected preaant,
GORDON P. E. WHITE & ASSOCIATES LTD. CONSULTING GEOLOGISTS
The rocks along Creek Fault are alie.qe,*; alld ! ~ : I L , . , I 61 i t Aact anr' si the
porphyritic gabbro proves to be the S O ~ S I C ~ rock ( ( 2 v'ie .t:r.*i~~.llic . ~ i i n e r a % ~ ,
the area between the intrusive ant1 the ta:p o f Z , i % s r i x ~ r* ,'?iirilt aiu \ - ;odd k~e
a good exploration area to attempt $0 u.n;cotver ceisrrczn:ic- 1 t rlc:enl; ~ t i u n s
of copper and aslver.
Field evidence t c s date, particularly the mature of t h ~ 1 ~ 4 i t~rsr;;cii ~ati131.b in
the gabbro an #4A and #4 Creeks seean t c ~ point to the ,,ia.r : I , , y i f kc iyalalr::
a s being the source of the copper /a~ilver aninea~alizakic~~k, Lzl ;,:t:ke?~a?:
therebore, the area peripheral to the gabbro is econ~idev c i. 1 .te
exploraticrn tar get.
CGNGL'USIGNS t RECOMMENDATIONS -- Although not colm(elueive, it is possible that copper a ~ ~ : a k i t * ~ L* i n r n l a ; r >Aka
have been introduced dong fault toners i s a sedi.ne:cr~ar~r itcust :,13txk i*fit:
&at the m~ineralizing eolutionle came from a p o r g ~ ~ yritia. gcsbhrb I t?de!?t
on the clairxrst. 19ni ;,ttetnpt rjibould bo inade to pgrlrve ax" c l I . ~ i 3 ~ ; v c : Y:;
theory and in cluing so, the extent ms9 eanterri of the . ~ ~ e & ; . i i i a ~ , ~ . . ~ i i . ~ J : G;l~e
present should be inve~figated.
uontirruad sn.So~q, wick a detailed prospect ing ar,d ~ ~ b p l ' l s P. :"$3 L':L k " + 11
uppar Kiitss laa Morntailla more apecificdly:
" ' , * foot; levels with separate kitchen and w%e:*jre~u:l i i ~ c ~ . , ~ ~ i e t .
Grid line8 sk~srird be ceatabl.%~hed sla t;7e u11_*';":' : I : :, $28 5 t .i - cll.nims, 400 foot spaced lineg with 200 f c ~ . < t $ 3
- 6 - $ *. s ,I a<
\*. s P
I( A'
TO PROTECT OUR CLIENTS. THE PUBLIC AND OURSELVES, ALL REPORTS ARE SUBMITTED A S THE COKrlDENTlAL PHOPERTY'@F, CLIENTS ANY' AUTHORIZATION FOR PUBLICATION O F STATEMENTS. CONCLUSIONS A N D EXTRACTS FROM OUR REPORTS MUST RECEIVE OUR WRI~~E-&~~~,",<~AL
P GORDON P. E. WHITE & ASSOClATES LYD
-
A barometer survey should he rurx oa e r the g r ir" to
ee;tabtPsh elevations.
Geological mapginrg e f the7 :2ai i a C r t * 1'- F'? i ? i : ?cka ??I,.!
detailed prospecting of all the e l n i '36 cr 'nr ' r~ : f , , i *>P t: aub*iet.i
present on the claims.
The 'Copcot drilling ant:! blastir~p, of t:,-et~c~*rt s i$hs~ul;t hc
continued, defining -the! liadtn of tire 7.d : 6 ' ' -L ~ $ 6 s
%ad extending the t r e n c h ~ s dov11). tCle ?.;:-.POL. ? t -lr z $ r * z b
The ores on #4 Creek at 26460 feet silou.i? !YJ txsra;-v~ivted
further by trenching a1d rapp ing . b Fax t l ~ E ~ E Y , ! 9"'
main trench in the A zone a'rraulf! i s 3 ~ i t 5 k ? ~ 8 ~ i ti % - i!? 3 9 e -
. 1 sa,~*f,?lad to try to get he1fa.z~ e i t he r ,, 1 r. : % I - -&-:I
OP Peaching by surface effect.
* . X t w o d d be better if the saase: persor& \ d i , t L r * 1 c:
the preferred metl~od to Re ~ l i ~ e c ? .
69.1 d4A Creek, a hePfport would +jp<.$ (9r f &*I. -, - ,
kranspostat%on corsths froin &he camp t,, k: lL ,:" <>. f s r
blasting srspg82es, The trenching ah0111 3 irt:! ci-? t ; ri? . + t i
hare to t r y t~ get b a h w altsratiou zaaa:? : c 3 L ; r %
somtP east.
-- - -
The e~tirnnted expenditurea required arc? rrs ft>l.lc-+l s + :
Caxnp improvement lawer camp
Heliport construction
Gamps, construction #4A Creek helicopter traneport and it-bstahhatfoi~ at 3700' and 4700' ; r , >,:* 5 % ~
3 radio telephoner, installatior?, r.en.tal. and service coet j p r o x s :
$ r - Transportation, Terrace area '!,, , . +,j
Gr id lines, 44 rniles @ $140/bh4
Barometer Survey
Gsoleagicd mapping and prospecting r p i * ' , , \:
Trenching, Copco drilling and bPa~ting ; ! j , ; ! f : : k G -17
Engineering
Contingencies
Tt rr:a)p k J ~ c o m e desirsahPe to accelerate this ;2r~gr:eri:.-::ti~ !:- :-;,%> , ? b c * I /
:-r~zdo as BO further exploration sf this natare, 0-r LC ti 1 y t:' - I I
TO PROTECT OUR CLIENTS. THE PUBLIC AND OURSELVES, ALL REPORTS ARE SUBMITTED AS THE CONFIDENTIAL PROPERTY O F C L Y ~ & @ - AUTHORIZATION FOR PUBLICATION OF STATEMENTS. CONCLUSIONS AND EXTRACTS FROM OUR REPORTS MUST RECEIVE OUR WRITTEN APPROVAL
--- GORDON P. E. WHITE & ASSOCIATES LID. =-- .-
CONSULTING GEOLOGISTS
A. 'j?E-l'AfT I a m a registered ::'x.cft>t~si~~i;.nX :. J , : , . ' *
the F'rovfnee of British Gc~l \kn~$ iz .
9 < * A E k l I a m a: graduate c i 'tu C! Ci.?f-~os**:~ ; i. y ' . ,
wit!- a degree of Bachelor sf Scfeace ( I$ i 3 ) .
3. 'FI-IAT 1 a m o Consulting C;eal@dist wit11 c f f k ~ r ~ I I , i \ ,
v;!'ese Pendar Street, Vaacaxx-rer 1, B. C.
4. 3'1' t; 'T i have visited the property disc ~ n a c < i :,. ! :it., :*,!pc L.
5. TP'" A T 2 have practiced as a geologist fa?, .-.ac., . (9 : 11;g.n 1 I :
year examining and reporting 023. px* ,.fi \ 1 f.6 2 . a;
i ~ r ~ ' ~ k + ~ * i C:J F{ 14 Africa.
THiiT 1 have personally checked the sRa!:inq - f 8 , ) ;
the r : l a i r n ~ listed. is thisr raycr t k i , : : ~ L,,~:? , , : P:,, = * pss'$.s, t a g and elairx-rr lines ta be pr"r-~t,e 1.1 y r: a. r
7. 'I'IE1IT I have no interest, direct nT izc~= -6-c;., b s j
co t r parltr L C ~ U D I P I D ~ F:Y i~tf?ndli~g to <.:c; " v ' -ii
Ltd. "ilVt:r .a:: 1 have m y inte;*f~ibt. :Q ti .: I , . sr t rair,,e:%, raier r e d to 69s t).a;s re,zori.
TO PROTECT O U R CLIENTS. T H E PUBLIC A N D OURSELVES, A L L REPORTS ARE SUBMITTED AS T h E CONFIDEN'TIAL PROPERTY O F CLIENTS AND AUTHORIZATION FOR PUBLICATION O F STATEMENTS. CONCLUSIONS A N D EXTRACTS FROM O U R REPORTS M U S T RECEIVE OUR WRITTEN APPROVAL
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--- G O R D O N P. E. WHITE & ASSOCIATES LTD. ~ ~ ~ - ~ - ~ - - - - - - - - - - IN
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