EM & MAG SUR EAST & WEST HOODOO LAKE GRPS & … · cktf.Oed p Jd - linftp sf'acrc) fit ICO foot intfrvals - wa* established on pfirtc of olfiii.H 33349'' * 93 - 95 - 9f*' to five

010

'

K' TO; Y.). .Th'jr, rupMiLY ::r;3,i, iiw-io:-; J H' n'.-u ' :. '.' : '-'*. ,-.. ..

, ; l l. i i): ' J i 5' M S

'j I.- foVif.i-.il.;: j.j.i.)-i 6( !,er.il' f- t!. c j:i fjji!i,vf: Jc: 'i MI we y r corno]

' /.' . i - '."•"••'••'it.,''. J o!.'.; -l -.MjVU Uo, Lii.i-U'i cOMntfi JoO(,t?ri ir: K*1 .H h 'j o^fr.hlj*, ;:il.*

-0^'.,- !'-\j' ' .r, j novJhjc of ")!-.t,;.vjo. 'J}J*M. eJMt,;.-. rrr o.ivj(3*wi into tbrt r f.: t:JiM-iifr

'-i''i'j- i l)if!.' l"-\. J- .' (^-.-if-.ti t? o r.;, l!..- !'-3r.tM-ofk J.; l-'. , }:!,'.i hoodoo J..;. l:* I.VIH i.*.-. i

,: f,'-- ciif-lhin- of ] 'h:}-.- i j.-in-f; u r* conLri eied to Jfiaj Aliv

.- i!'U''o of ' ; J i^ 1 ')*-, c.;'- l- c-, i'jclol jlh'f- 'jio.cro (.1 /.(K) fOO |. ir-i.c rvt-l^ \-.n-t cut

i l ).i;'lii MiJ'(, lo 4 i f. i.-'.it r. i, trc ttd.-iN." h:,',f Jinff; oi.i t')l thr*:t frouji;:. f-M-iVl d*l;1]'C'

(siof (Jlh-f i}.,.f-cl d j(ij foot- ini.f. )-vi;'i..s) VM-*. rf,i^b"iif:hf o oh t ;.cl. of the, f;j-oii;.!. ov. r

: .f/; {-f.?,;.! it^t.- (V!f.r-.( r.i).: t,''o MI"!) 'Mf, t i n i. j t.'U x; i.joH. j'jck.if. vrr. f":b r ^ rv* lv f*0

5*; i ; ui),t ; l}/- off- ( i jiivf^ 1..,' clôr,':; r.

i' - ; ?.. io;. 1'v f IM-VV.;. J)^ \.j.f. c-'iviuaif';'- \ ^\ j * Co.x i.r,,l ];,, Krl'y, f -*' o jili.v^.nV''.!

(i/ ii.ifO-f. eh:" P:' f. In. t. i.. \-5tl, Oi.n-.rlJM J; h:i',-:Vt.vJ.J'U Or-. )J':.Jie,l, u-.5h,' (; J;,"(?.)v^. r t-;)j":

:'-*. i MI: 1. 1. i.';'-;!).. f i.fVv i-..cviivt ,-l (i ;-'j, m^ J,f) foot, jnlf.-i-Vi T s r'tnt,;, l!,* off.* rt 3ir..-f.

- ri):(-'''(, . u '. o* ; -: !-* '-i I'j'Oi. i'n :ii,U!rO\.\ of tfif!. U'n'lf 'iOv;! h, - f co -i :''t5r.rr., 'j'l^ j-fM'"'tf

t- i!.-', f "D'l,;. ; v, d, M, i.; (,i- i!-* ; CH.-0!-, ',: f .yj li," ''Cf f'-!''.; fj'-iJe Gofiioi'i- lOrt"'1 ot.- i MM. l*.

C ' (i). -' t t':} l .;U- 'lv I'CU ff ( t.

IM'c-iju.. , t i -i f. f.iu-vi'v:'tr: v;.'. ervrj*;"; out V'V l. f '.coli run (;. l

j Oj'lAjjcf'i C'j 1 r(.i,.,}, \ili. t!î. UC');':-i v\. L KoisV.t. l.'sT-J: JV li u-J i-.o!.t.|-.-"| Ilo^p ty

V ll-f.1 f CO- {."i" of t!" : l" Vt\.ilr; W.itli t h* OCi-Jitiiol! Of Ihf !lO':frJ' f.;iv f)':1'-!-- of \ \.-'

l.' i i'. !\*:.'\ J ,', l', f J. -i';'. I'f to *l;uij':-i J'l fViJUr,. j. S'oJ'lif.V VO-l5e4,-"l JoOJi l-rComj.'ii f. SJ.ii

u '.t ^ ; ' u t;", fro- li'''" VVi;-)-. }' l f nt-j-oK.' ,"ti' t J (- )-tM^h't: \,r)-. 3x coruf Ci ti f .C*

5-io-vi'i'. t ''oh/ lil' of j "t. 't ;Miff. fi'1,1 UK r*(.u"!tf. of thl*. i. or) MV shoîi on th'

j. ',vji.. ' ;,'N i-ij-o:- ;T i o o rrof^J' J'J'.hs'- on i.' f iCf^'k. of" on- jficiti rr ; u?.J', ^(X' ftfl,

J'n:*, ) -v.'?.i"i J -.li- 'i 5t.'io (L- f t; Ho}, of 1-!ii? voi-J- Vf ri i ho. 3 . f.j)Oi-'.:H)i:Mt.y of Hi

)-.'-V'j, J .'{-; j f -.'i', "i U.o!io; jf.l i.'il' 0:',-('5f,i, .loLn- -J'j.'ivj Jl**- Co, Mr,i*it-o r.t I'^l

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M'jij' )1\ J J'*'- C'f ; !cu'i( of' cr 3 f. oli tqii'*ir i(K)0 fVtt.

v.r* rur-

Vi. * ' j'ifvcc'i J rk* (.j-oUj' of c''?. 1?!;- i f. J ooftfit' 5f; th? : r- u-Un crt j-: rt

r. f i - i 5 1 i. 'j o.;. Mi. j.i'"- J f )-. tfxHy f f-ct ' fJh)*! IH )ifift Uii.11r;jh^ thf 5-5h.'*{l Vj-er f Ml

f .'i' \ : )x).-i J: i-. \ - -\'.)-* ,-\ t f j*!;-*.-" 't r- c ].!.':* CM; b: n ueh^C" by os j- fir trook i '- ru MX

5? f.'iv/i*;' r i'.b/ li.; -MIMJ, s j ri c of' Hifhi.iA ?f.KU ri l fTJFtfihof. of" f Jijd'Co iutt lv K'

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J'- -l 1 ' li' j r 5 t ;.M~ \ ' : i- Kocxloo l ' k* (;j-ouj.s of cOfJp'. m. Jr-t-flrti iii the

( i'!.}; "i j-; vi c; li; '.i o. j, : Mj) ;,r.'. i rt ! - 1: l i-tr/ojv {cctSf-.llO f by 5-:.{i f roi Hoj-f.C'M'i

.' l', ' -'ti l!-- t I'f.o.ioo J '.V' ^f. i H X'' "' "l;, r bz,y of HOJ-./OOC'! l.'l'f M.:" tlu ivo f-t-viij^

{ ^" t-.i- ii - rv. ; ii.m.i.t r" v.it[.'ii. tlnx o- ;a''.rt* r-5 of t r 3')* to tht ( f 'l J;*ti i* Rt of Ih-^

r -ri.!' ri.."' o ( 11" J ' k- . ii'ij-i O';t"i J^.l 1 ' CM. b* j-t i.-ohr^ VA- cur or trooV by jv-ootruih;;

i !TOI\ l- )(.j'\f[ l'- iln ve M.-(X M-I-K'I f. j o e of" i-fi^ J.;!:*,

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. . .- t i i.', ("f D' \ - . jx'i-l l '' ! '' f'ivi*.; j . xl( r^.t'f i-t.Uff to t Mf r-tot-loii of thr rO'.tt-rC'C'l'

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Oil tho i'ilaterock Luke* Group of claims a bane 3 in* vms fct&rtftfl from

thf. t-.ast boundary of cluiUi f--13354l at a di&tanc* of 100 feet north of th- Ifo. ?

Post and vms out to t h* v,*j;t for a l**nf,th of G400 feat. Pick*- 1 Hn^R were ^Fjtab-

3ifih'-.d (it /4 00 foot iirUrvnl*. and \,er* cut to th* north t in! south to the HmHfl of

the. property. A detailed p.rid - 3Jn*s npaoed at 100 foot intervale - w a* established

over p.M-tE of clulritj 133SA1 -42- A3 - /*V * ^B - 49 to oov^r

To the pout h c* ri th*t li^Rt Hoodoo Lnkft Group of claims a b^se

Fitfirtfci f'l'ojii thf Vfctt houtii-if.vy of o.lnjin 13X^8 6n the Township centre line raxl v;ow

cut to the cf.st for H 3*nf;th of 2^00 feet. Ticket linâ v-isr* eRtab3ishfrl at //K)

foot inttrvfJ.B n'tfl v,'er*i out to the north nnd pouth to th* litnltn of thf' propc-rty.

A d f tnDfo f rid - linen ftpi,ofd at 100 foot Intprvnls - was established on cltdtn

333fjO:? fain pjirt of 333503 to Riv* ruorft ooverfiga over assumed emlphide zonns*

fin the. Jjtist Hoodoo Lake Group of claims , a bîRi* 31 w wrts ntart**d from

the No. 3 1'opt of ol? .i l ri) 333495 on thft Township centre lin© s rid v t\s cut to thf vest

for H l *"ni;th of /.OOO feet. A^tdn, picket lines w^re er-tabliRhed at 400 foot

i nt t r val s i*rv) v.f.r. out to t h* north ami south to the limits of the property, A

cktf.Oed p Jd - linftp sf'acrc) fit ICO foot intfrvals - wa* established on pfirtc of

olfiii.H 33349'' * 93 - 95 - 9f*' to five r-nr*- ooveraf'** over asRuiuftd sulphide zonss*

VJtli the pxof ption of the Jower row of olaimp on the 'ilatirrotik L(iV*

Grc'Up a'!"! lin? euttJr^ t?n.1 ohainin/r v.'fre contracted to J. A3 lv Company Mwitpd of

Val d'Oi-, QiK-bfeO, Or- the 3o\vfsr rov.1 of thr Slntsrock Lake Group the work vfe.s carried

out- by C;* Poti-er and V.. Scott of Kirklrnr! Lak*, Ont.ario.

Note try t on all three groups of clnirna, pickets v^r© fjved every 50

fert alor^''. tlit offset J5twB by chf.lnnf;*,

/. tot?*l of 41*6 JiiJles of line \*UB cut and chainwl during the- oourtf of

t M i-: vork. On thf- f-lfiterock Lakt- O roup i?3t.^ iiJloa were required v,'.ith 5*5 on t h*

l r b t Hoodoo lv -.k *-. (;roup atid 1^.5 on thei Kost Hoodoo Ltike Group,

- fj -

j'f^tv; toi-if tt r Hu/ vr-y f

A iv.r-,nt tomc-tf.r t.nrvfc;v wi.f, conuuctfc-:! ovar the Keith Township

b;' T. Geo mil l;. H':3csy, f;(ciphyfdef,]. oprrfitort; and fi*3*lmjin v.'Hh Ganurlian J

iv.v.viji? Co. MriKtri. H, l-cT)ouf',all ar/; I', I'oUhri stit-. asaisteK" tJuHn;1, part f; of thft

I'nf-.ne tic j-fii^'n^R v*rre re corded m in;; a Jalaivler typs irxr trui iMit

tU'Yin;*, fch1 '..-! t:K.lt']r'; of DO, 30 and 3.00 Eamiifs p^r division for f.cale.ri l, e', i.inf 3,

j-f-i-.j'f etivfOy. Ynlfi instrum^ht hwl ln?f-n ohook*cl itmnfîiatfely prior to B tart i np the

Kf Jth Vownr(hi j* f xu-vty t-, M utjj.iv.5nf, tlie vaiu* of h fiver! known Company bast station

*;t thf- foy-j,:'!- Kunr-C' Titi' n't-r t*Eithpfeortf ^ ^,aT;';a valvif of 3.2?0 on thr

v.C'Ulo' coivjT*pon1 c"Jorc.iy vith t,n titeolnte valu^ of 57,599 - 35 gfmT*.s

Of th" plf(lT;if. Furvf-yrd, base control fitation1* v.rr* f-r.tfibHf,h"f''

3. f;;utf-rock

l'.. C. i.. J Jo. j

i.. G. f:, feu 3i.. c. r.. ?i-.. 4J.'./.I Ik.^clOO. J-1,1li " ^ f' l'- 'l J'. Ut iJ ei Iv-N . Jl'., o. !'.. i;,-., i'

' S.'orth on Mm 10*00\',lit-? on lin*- ?0400i;

" or, Diiie•* on riirsf '

on Mrw 2P400W on 'Jin*;

va'lvc ~

~ IB W

velu*

. 3320J!. G. f'.. 'Ju, J - b: f.;( .lints - on lir* ^0400.. - - - ~J.* C* fi. 5'n. ^ ~ " " - on 3ins JÔOu * - - -J 1.. G. S'., l.o. 3 - l( | ; - on linti 144.00;. - * - -

JHuJn th: uouti.r of the sm'Vf.y, Ix&ti control

ri rfi.uTi'j- ' i Urv.''.K (four resu"!'n,",s p-.r opy) as n oh^ck on ths* work'nj; connltiot,

of i hi in--! i-.j'.;riit t""- to r* ecml thf dally duirnal variation, fitntiou'; ver* e

tt ?5 civ 50 f o c .t .'vui rV( li f. til'-':;; tl* offset lines. - Bpacinf, rv aa dependent upon the

liift'-.ii'tic 3rtt.ns5tv of t ho

* f. .l'; fi toh' t() .''V.'.yi1 -/.' (conl-'o)

A lot r T of /. f l'3'' jv: f'-'rtt-'p vj;?5 rtoorcVcl flurinc t h*- oourr** of th* maf;-

i c ten • •(•a i .uvvi'.v* Ov; -t.hr P-Jr-tf roc-V ]."ke Groxtp 2,61? v.-era reefonSfcfl with l^.^n on

i!. i: J.; *i Tloouo-.- 1.:'"' (-roi';' f: M,' Yv1,'' on the Vrst KroOoo J.?ike Group*

}',"u.etror." ['ju lie /;i'vye,Yt

An t !f' c-lr-oin f P!4.5e n v.rvty v*ra eorrUiotfrt over thr Kf-lth Township oH?5nis

V l. f'c- -it f t^ (;, 3-fiivov, êoj)^'4?joi;'J: opej'ators •wjtii OuiV'tlititi ,lo

0'. J .'1 M '. 1 1 (i* 0. Anorx '. .T. i--e-.r3fit i'c' duvlnf. the greater pivrt of IWs

i 5th th( o u*']'t:'-O)i of the. 3ov.'(ir tier- of olnlni?. on tho ^luteronk l/iVo

{••j-oiipj a"! J o"lr J 5i- v t'jv ri)i'V:',V(v mir\". o lionkr. f'srk .TV horizontal loop tyjx^ unit,

'.i'!r; !'. mf!t tr^' ; ; J^v,;;) c-^'i r. pin-. j n;-. of J'CX") ft.et an/I h/*! Iv-.cii SKtrord ir-vawliatttlj' priorN

to t JK s i t'll f '-f t h ci K'-Hh 'j 'OY;hr.Wp MU-Vf-J1 .

'j'rf.t fu-v*yf. h^vt bf-fh copijOf tfd w H h this: unit over o.

a r j r,-- .lv,' fnOj-'-'u'.? s;,:))!!: ctvl a r. i P s c r. J natecl fiulpMoe Bone as clfle In interpreting

th' j'*-r ultf. oMfi^hcr'i or* wo fOorf-6 ol?.1ir,s |;rou}'?. The: follov/in^ rfrsults weir*:

obl-fi'' f'f o ouv^''-; t h* .".fi tc-.rtM ~

? t i V r J ve b i/^ pM f! t, t.om- *— t; f.trortf' po?-itlv* ri8.fr on the in ph^r.o follov.frr! by

a': jtii.'-n; t. )" prlH-: v'ith a jvf;uj.ipt5oK to Efro or hftar f*ro whf-n the t'4

v ti' off ll! 1 ctir/iuotr-;-. The out of pliM^. eora;)onsnt rc-nviinticl vithin -

2* Pi f f - t -i ' n v (^ M'Jph'f'f '/.f.n^ -- niri!lMi to J*o. l but v:ith lower i .ti phn? -v

3* (irt.'))lutJo j-.oii.v. — Ijoth thf- in jihfvRfr an/i oxxt of phase conpoiif-nte.

O IK. {ihn'lh-i M i,": fol'lt'ViCic! tht JXt.ttcj'H ()f I le.) t 3 *

it t.!ion'J(* fclKO bt- notoil thnt coil epaoinr; (shoulLrt be exactly liCX* fuel)

urio tht aii,". .'V. of th^ oculfi to thr horj ?.ontt.l (cfX'h coil e houle! IKI horizontal)

i.O 'A- a ii'^y.* ii:. ••i .in t!ii c - vork* Kri-ors in one or both of thf: above nif^' ce.use

anoSi'Oicf. of fiUff.xcJ'-ni, rnaf.hltxt'ie to indicates the iir-Miftnoe of a discer.dnivlftf'

ruOph^cif- v,:iiK-r C.oti^r-viU'-ul.ii.^ topcic.riiphy j P an important factor in this typ* of

t-v *.

. 7 .

1 3/- (lkj li1'!? ill1!' y..0' ' ;11J y.ty ' (coni 1 d)

J 'ne to equipment f td lure, the survey on the lov.'er rot; of claims of

the- r.lateroek link'- Group vvas carried out uoinf, a I'cPhar vertical loop reconnaiss

ance eO.ftctromfif-.wti.o unH on b frequency of 1000 cycles per second . The I.'ol'har

unit Jj; EiultibJk for une ut; a reconnaissance and relatively detail electromagnetic

unH, enployinj; thr*f Hep: rate oonfifiuimtions for different peolofjiocJ con;litiorw,

In thin cfiftfr tli e tronr-idtter v/us held vertically at a distance of 4,00 feet from

the i-r-cH Jverj thf i-rceiver vns tinted ahout the nacis joining thfj tv.'o ooil.s until

ti mil] Whs obsr.rved* This configuration is the wost euitable for steeply dipping

ocinHiotoi'f! t fdvSn; 1 (i t.i'rdtaU"i response from flat-lying overburden, tind is unaffected

by elevation differences*

Thr trt-nsii'itter and receiver were moved on separate lines, ^00 feet

apM't f'.nd rftftf'in/.o \iere. recorded at 50 foot intervals. Under these operating

ooni'iit.lniv;, t, dfrjith j)enetrt'ution of 200 feet v.ould be attained. Null widths which

vc.re fxtr*'i..o jy 'Jov; vrei-c recorded at each station but have not been shown on the

nctooiiipuny j n,'; pi an**,

V,f.l.ki-TtO-k:i unHf. were used by operators of the transmitting arid re-

ceivinK eoSls for position control during the survey.

A tot 1 1 of 2110 readings was recorded during the courr,e of the electro-

imir-u.-tie fiurv^y with station,^ spaced at |}0 foot intervals. On thr. ftlateirook Lake

Groui), 3399 rfradjnê v.-era recorded with C'38 on the Hast Hoodoo Lake Group and 273

on thf V w;t Hoodoo l.tikf" G

'rhf f;eolot';y of the north part of Keith Township wos iaa.pped in detail

\\}' V . K. I'rerit for the Ontario Pept. of fines. The rer.ultr, of this; work werfc pub-

lif-hed 3 d the Hftt\ -Ninth AnnunJl Keport entitled "Oftolof*y of the Keith-I'uakep.o

Tov ti'-hii) Art!." and r*re ehown on the accompanying 10C)0 seal* geological plan. A?.

Borr. details' of tho (:eolo{;y shown on the geophysical plans ucooiujianyinft this report

hf.v* bfit.ii ttilr^n f roil J'rtf.t'fi plan, the following "Table of Formations" has teen

- B -

?',liL j '5lo I'X* ( c o nt ' d )

copird directly from )'ar;e 5 of tha Hepartra-snt of Mines Report*

Cii'JiJT. 110 (Glficio-fluvial sands and gra Mi-ist.octr' j (Till.

!':ntr.oh*-vmm

( Quart 2; ve 5 us , o arbo nate v** i ns .

Al.f;omint (Oranite, granite nnflies| granodiorite, hornblende(quM-tf, c'j.orlte, syenito; porpiiyrieB*

porphyry .(Granite porphyry aasooiated feldspar porphyry.

(?)j (Quar t?, -f ft 3 {Is pur porphyry.(Felsite tmrl felsite breccia.(Quart?, porphyry nn" quai'bz porphj'ry breccia,

y burl fin (?)j (Oronodiorit*-, quartz diorite, diorite, p/Jbbro,

Jifev.ctirs ('/)j Feldspar porphyry, granite porjihyry*

(Banded iron formation.(Con/jloineratft, m-kose, graywacke, argillite} phyllite,(sif tt* .(Acidic volcanicB an^l associated intrusivesj winor(dioritic tuffs and 'Ikes j derived r.chints.(Jntern'K'o'att) to bfieic volcanics and associated in-(trusivftsj minor acidic volcanics and sediments;(derived

'j 'h*- rock*- urô-Iiyin;, th? thi-et Coniptny Grouj^ of claims ere undfcj-laln

by 3DU-i-i.itd3z.tr to br^jo volcnnicr, 5.nterb*c"decl with ba^s of aoid volcanics, oediicents

and iron foriititiots, 1'orphj'r.Hio, clioritlo and diabase dikâ and sill-like Iwdies of

ultrf-banlo rook'i Jnlru?le- thesf- formations. Algoman granites occur in the extreme

north md r.outh part r. of the K rea wapj*;' by 1'rest,

I'-itnils of tht! ecology on thfj clnlias group v*il3. be discussed undesr the

rfitMtlon of HH;' 1 '"^0^^'!' Purvey."

of ?'i;;;n"to|n'vtfrr . gw^fjt' ' t

T h*: i\f.iu"Jt5i of thf. ii.'inrif torii^tfti1 Mirv*y art depicted on tht acoorjputiyin;;

Contour- j'l?,nn" on v r calft of on** inch equttls 2CX) feet. Contour lines

~ 9 -

at J on of J^'ifi^t^rjifttejr^Puynifi^ ' (cont 'd )

of rqu/'.l i.i'-i'.h 1 tic intensity have be^n drawn tt 1000 fjeunnia Intervals from O to 6000

UB required* InlM-prt-tation has be^n baaed upon a study of the contoured magnet*

o) i* ter p3f"ti!:, rîon/J fôlonioul tind p;eophysieal data, V. K, Prest 's paoloîcal

ji'.!t:*i and t'lifi'l pbotop.raphe,

Oil tho r.laterock Lake Group of claims the major portion of the eurveyrd

fin b SB undMOain by intr.rMfdiatfc to basic volcanic rocks. Magnetic rfradin^s over

tlif-.fif fori-" tior^- rîi^fc i n Mi'iu.^ from 300 to 2200 fjwjunns, ho^ftvsr, thw nveref,* in-

teii-rdty of the vo3.canios it. b^twê -h 130C) and 1700 ptiMnuis. T h B volcunioo in the

fiouih*)f!pl part of thii croup hitvt ecatterwl sjohae with values well bflov* the 1000

f;t).V::-.i'j vtslu':-. Tliifi jnf^ bf oW) to t h* oocurr©MOft of irrftgulur ncidio flown,

Jn thfi northeast purt of thes proup a narrow jiona of enst-v^st striking

in/ ,1-ijf tic "hl(;hf i; ooeuj-fi. I'of/.netlo râ/iinîs ovftr these "hif.hs" ran^^p in intensity

froi'i J'CX'O to J J* 00 p,w;ii'iU9 and trfc br31cvftd to be due to thft occurrence of a band of

A h'.vjxVi! lcnii'i of r-otlinionts ooours in the, northeastern part of the- p

which sho'iiS: r vidff ri'.n^ft of values , This May b* du** to the* ocourrenoft of an

aniph5.bo3H5v.f-c" voDcfOilc or i * maf'.n^titf-rlch aedimwntary band. Râdin^fi over th*se

f^dii'!- tits i'-fiM,''.e in i,i ( "[;n-tio Jntftusity from an foctr*m* n^fâtive to 3500 ^nmîfts.

/, r.rrJcfi of acidic intriiiivr rooks cut the volcanics in the ftnst and

Citilr//! pavti'- of the proup f.ncl pti'ikw in n pftnoral westsrly direction. l'ttf?n*tio

V'f Milirîf, ovr5' th*r;f JntruîVftB runê Jn intfinisity fron I7f00 to 1800 {'amnns. AB it

i R ii.-roi'f'ibl*-. to diffvrt; ntJatc thf- intrusive from the aurrourvlint; volcanion on a

iu',(;ti tic b'.?-,ift, the; ouil^rit! of the. intrusive has been taken from V. K. Prost's

Gf o'kvJct/i I'lf ri,

3n Hit fo:treiWT aouth port of t ho claim??, n nurrovj sill-like body of

uHriAîJc i-ocV.fi c*ocurf, iii t ho volcanic foj-mutioni. This intrusive strikes in a

\:':f;ifrJy to fIMnht)y fiouthv^st^rly direction, ranges Jn width from 100 to 600 feet

i. tt' f .j'pt- 1- rv-; to h*.vc- t. t'-31j4it dip to th*~ north. !'afrifttic reaîn^s over the

. 10 -

,1 '-l'.L -Diii^lEiiitîfiE-tiVDi^l (oont'd)

wilts ill?" d peridotite-, r* n(;f in m?tf ustic intensity fro rt 2^00 to over 35,000 g

bovrvtr, thfr W WW v tiiJHf! j-atij'.o fron 3000 to 5000 nnra'.ifi*.*

^riivs of' hi {-lily itltt-red uHri.hti!;lo rook* which now consist mainly of

occur nlon,^ the north oontuot of the intrusive awl t.ro toost pro-

r-t to a fisrlfs of dons etruoturfcB. I'apn^tic values over thef;e* ta'Jo-

rt -r^'t'- J n vf.lxi': from 2000 to 2700 ganmar..

P.tru-"ituial5j-| three oronB ftuiltn htve bf en inrlicatrd hy tlm m&firwtonifrtftr

RUrvty. Thffif ftructurcp offset the ultrabasic intruflive in thft southv/eist part of

the- cliiî^ (j ox.'i) cr,xtc ..1 n;i; (Hifiplf'CfcTif-ntrs up to /tOO fpat. In till cusets the tnovftment

hfi'i be eh Vff4, R i rt ft to the- f;outh. No doubt iletciil^rl f;eolo{;ioal nuippjrv, would show a

profu iinii of crop;; ptriKitur^B 3ri thin rrpf..

0:, the V-.t1st lioocloo I-nks C^roup of clnlmfi fi Irtrê portion of the

tj-f'.i* tppc.firf to be uncierlr.ln by umphlbolltlgecl volcanic rocks. Magnetic

over thfttifr iy-r*f,ulm*ly ooourriH'; formations j'tmge in intensity from ?0(K) to 4900

fwn: 'ii,R , hov.'fvtr, a Majority rarj{;r. bftweftn 5000 and 3000 gGmmofl. î'ht reraairtlftr of

th" o3fdi!'fi (;roup IP afvr.umw' to Ix-^ utir'erlftin by interm^ciiate to bisaio volcanic rooks

which hnve- vt.lir-f- rr-.^''.!^ 3n Mfipnetic intennlty from 3200 to 2000 paramos, Avernf',6

over theff' volotinlch vniê from 3/00 to K-00 p.ti.i.-uoc,

îv orofip ftiultj v;hich etr^Vcfta in t \ nnrthwly direction, has bsen linUoa-

by tin Tii/^.ti'towto- r.ur-vry and oocuj'B i n the t) c r. t pM't of the* proup. This

ciin-v offs.tif. the* uv.phlbolitiKccl voôcnicF, r horizontal cii^tnnoc of approximnttly

f r fit. It ivoulr! Lffilrt. tippf^y that th^ v;fpt r.ide has been rnnved to the south.

Or. the I'.ant Hoodoo l.r.V? Group of coltas the mujoi' portion of thr pi-ojxirty

JB uridM'lfiln by interfiled i ute "to basic volcanic rooks v/hioh have VKlu'-r, rfin^ln^ 5n

r:,a,':rif tlc 5rit* n'^Hy fror.; Rllfhtly ]i~s'-, thtn 1000 to 2300 (;nnrmn. Hnv.rver, f, t-mjorHy

of th^ rtac^nff-. r;.n4 -f ', .-t..w6ftn 3300 end IC-OO pfim^tts. Narrow, irropulor bamlB of

h''!0y f:!ii-)hib:)Hti?'; d mritcrJal. occur horo&s th? south-oentral prrt of thft HUfveytd

limit iVi^ri\tJo rf t/iin^r. over thf.-r.t- aniphibolitep ran^ê in uapni'tic jnt^nsjty fron

- 13...

il&'^HX^J^^.n. Sit . ''•'VIliiiiSlK-l'VSE JlBl'.YHill (cont 'd )

2000 to V2CO ya^'-if'';* hov.-fvcr, o Majority of tha values rniif.fc between 2000 und 3500

A tor^-.ur nf {;r;,nitic rocks Intrudes the volcanics in the southeast

pi;rt of" tht cOtili'.s. As tht 1,-jtifMw-tic intensity over this intrusive is identical v^lth

thr.t r j cord t O ovt r tht vo!! earner. , the contacts huvft bten transferred directly froiu

V. J;. Prest 't; (;*-olo['.icii l J'iUi, The norihwer.teriy tre idling diabise dike has also

trc.Ji trt.ri'-ff-X'i'f c- ("ircotly froi.-, I'rest's ?icn t

A t:troi\; o roe. s fuu3t f!trik*:s in fi soulht.tir.terly direction across th*

c}',1i:ir {;rcxi^ {.*!fl l'',;" bt.ch inoicated by previous geolop.loal wappinp, to the north of

the r.ui-vo.ytO Dta. L ii'irl.htirl,V trc-rulint", branch utruotm'6 offsets the amj)hibolite

ir, o ho Jti thf Vf,t.t-etntVt;l jiurt of tho p,ro\xp. Pue to the^ relative uniformity of the

tii'^rw tic ivr/iin^r, i.o othei' struc. 1 ' -t'f.a v.rrt iiKlioutecl by this survoy*

Tht result r, of thirs em-vey are. ehoirni on the accompanying "Electro-

. J'j'Oi'il* llari.'; 1 ' on u t; o i- It of on*; inch MjU&ls 20C) feet. 1'nlfirprfttation has

bfitii b 'j?, od uptit i n tufly of thf profile plnu;; and tojKigraphic data,

Or* tho [ilatftrook LnVii (iroup of claims u stroijf; oorKluotir^ zone has;

bcfii de J j ri-, tltcl a"Joi\', the bar,e, lin* in the northeast section of the block. This

conductor hot; r.he,rp ''irv-phaf.e: 11 pe.ake with liiurkecl crossovers. Th* out-of -phase cow-

.t vci'k'iy pai-i'"O?3s tht "ih-phas*" curve t Examination of thifc conductor shows

to b* ci-u-'.t.d by ii.'x'ieri.tt pyrite i'iln?,raliaatioii, An a uy i up; and t petrographic

sit: of c#l',cttd f, rub ea^plcs I'u5lt;^ to reveal an,v sulphides of interest. A

i;! zone; c.cciu i; on 3iri* /+4CKJ Vost to tht north of the bar.e. line. Afjain a sharp

h'.pjc " \ n-h\. u ith t ]"c!^r3;erl "cro^sove-.r" occurs ov^r this zona. Aa this coivluctor

i'.c! by ov? i-l'inil^h, te.fitiii^ utdr^ "(jeochcui1 ' nw t hoc! c woulcl bn tu'lvieabl^ for

e-valu ! :13on pat'i'or.t-E. . Note* that th&f-f ti.'o conductors \jer* d e li rift i. toe! xtslh;; t!i©

J.yjnVL, unit.

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