52Fiisween 63.879 LINE LAKE010

tba Month of April 3.957* a uwUnata* amtnay i*a potf orwixl for Coulcw Load ail 2Ino HAnea Lljndt d ow 11 c&aJta* in tha Bopukaai late* Araa of tha Kanetm dljBtrtot, Oitario.

Intarost wu» arouaad in tha aroa in 1955 fcy tha of ovor 3/4 at a latXUen tone of »J.p!iii]« uatarla.t

oottbiixid (wppajMiioIcai on the f omor K«»xxi HlOkal J'-inw jiroiJOi-ty At ItjjxOx'ofl I^iai* Tho Cgiilw c)*l>'te ma* ntaked to oow cxmiral am21 ahcMinga of

iddch waoru d^xjowrort oloaa to tho projoetod of Uia hrpulr>jii Iitai dopcwi.lt* Ati ct tl*t t!w j«,7wtic! oaitiwat. t^otvoan the '

ooid and baaio i\«3lc§ ri*j^ht t« uaoti to i^loot tboir ctruo-

Tha aunrq/ diatuaaod in thU rwort vaa porfonwd aa an aid in the aotroh fcr baao twtal danoaUft. ita ob^aota wart to Irrtioeta tha oxUnt of the ua0i«tio ou^Mda nirmmliBiitim at tha ahowlnga* to auuiaat t>* looationa of eiwilar loatorial laa^xiw, and to fain a " two inforwaUv*) ploturo of tha undarl^iit faology^ lha

vaa to delineate tha anonaloMa naiaatlo aonaa in the hopa thut thaao wwCUt ariaa from m^MAn idnaraliaatlon or aa

faatura*

Haf afanoa ia oada in thla report to tbo reavata of andiloh wu> aA»o fiarfonsd on tiit jroparty. A rtlaouaaion of ttda

i* oonUlmd in a aofarata raport,

A lars» riuuboi* of ixxKtttca iBgnetlo anomlloa wiying to llJOO faat in lanith and ovw 6,OJO gvtiaa in atrantJth, woro found by tha

Tbo tm>3rity aro rook*

to Ho in an am untedain by

It ia not known with ocift*.tnty what tho oauaoa of any of tha anonaliea ara* A blanioat of otw irfdcli oovarad tha olalx* Chirinft thaaurweQr jufwynto^' tho raootprdi ioti of outcrop vcrlCiofttlorw It la thoutfit U«t ttioy aria fron lc>oalitatlona of mpnitlo rJiMvala and/or

owfld tharaf art rtfltct Cue anocaly

a tioat ajjvoaoh to awfao* ty bad-rook* thtyadiMftliisKl nonta OP baaio ditoa or bod-rook tofx*0rviflanks a thawing and nty trao* an txtontton of wt rTht aooond tiiowinc; hfct no attooiatad anonalj and ia thtraf ortto bo of mill tedtnU Tht abaanoo of t&tttrital oorrobcrationtha anoeallta anggtata that none rafl«et naaivt iulphli* boditfe

A js-ograa hta boan r*xu.findcd to aaaaaa tho atoiifioanat of aaalt anont^ *n\ thorobgr iwltwt thoae Khloh naH.% drilling* Tht node

ocpootlj^ and aoil anfil^npof in orvJor to dotcniiro ootild havo aaaooiatod baao Mtal»» Kltvert have ^efttant crvxs to bogin with*

irioludo iliioh ftrm-itll ehoaea aa Uia

'

Tht elAiwo egeaeincid for Ooulot load and Zinc Uinoo linittd* art lootstod at tha yjust end of Doworhotiit latet* in tho DjUftriat of Konora*

Hotwhouat lAkt 1* 8 wlltt north oust of hwwloua Zatot and oouth oftgt of tht town of I^fwra* The ttnf^noBOMito Ixtitudt ,

wlimtiotu vbart untffootad by looil attraction it 6* aaatf

Tht btat Tbtrtart

Tht pop&iV tonaiffta of a DX*UJP of U oonti^uout oltlnt Khtah imlsult pwi of tlit utfttfti ond of DtKvarhooao ]Lako» An outline of ttit yropartjr it ahoi«i on tbt Kaj Hap «hioh aooocfaniaa tldo roport.

Tht Hat by siMfeir of tht olaintt toftthtr with tht wot atwarad by tho aurvtr will bo fott*1 in tht Afptodix to thlj rtport*

of aoooat i» toy air fms Kaoora to BatvwrhMtt atvtral oowitroial flyinc oorn«nitf at fonora*

Iht etalo&r of the asm in diaoaafad in & report \yy tht QUttrf*Dtftrtmant of Warn inane*! in 1956 «:rf ontitlod A h*glirdmiy Rapnrt * on th» Ooola^y of iht ftifDiloPiia Ijfe* Arat* Tha Canadian I^oifie Sailer Occnmj e^qpObored tbn Btawtiouao lafet arta and dtveoriNA it 'IA thfdr report }JoavpuXcftit lakt* Thty havt boon intrudtd by nmtU* and (jal^x^Lo ttUtos and atll^ At PIKWIOOB Ukt« a atrito of flat aO^dAt l«rw««

intru*iv* j/t or near « major northeast - atrittng fault ion** Dovelopafefrt wot* lua shown rx 0,000 tona of thaae pdjtildM to contain 1,5 pewotJt ofl*4»in«l oopptr nioJstl, Th» surface oqmaalana of thie deposit nr reputed to htvt been vary $OOP*

Shearing and fanning in the ana ooinclrite idth topographic linear* and are r«jjrea»rtfc«d by

• 4-

500are

hav» bom narkad by*

in pxtfondng tho rwrv

nan* thanfora aft ttatajfct to wflaot naaalvt

Tha aftjpatio wOttf ia qntta fiat aa* of tha oraak itdeh fiona t the bottm of tha &M* Idna Into D**v«touo« Uka. Ihia auggaata

that tba am ia arttrUl* by pmiU and thai tha eraak apfradnaiat a oooMiM, wUb the volowilw to U» woat. AmftJaa wait of iha Oft**

therefor* ba not* pwpitlo** for baa* natala.

ten boon la**** *Ath

W^F

tointtiar *ith one to tha north en Hal KB ia thtmgf ;ia^ •HpUnM^nr *^^njpia^^^Miw JUBW^^

Jtoj pwopprwo «i^rw jo

S2F11SWe»G

tobo toart^i for dirotf, work ori

of badoto fja"£! S« tho oT th

AIID KOfMf (F VRDPfKff

Tbo aLbJn» wuvijnecl for 0«,OUwi load and X5joo located at th@ wasfc GI*J a? Doawtiouiw l*ke, in the Lletrict of

Kmora* CVitario* BoawrJiC'uao l*kt» ie 0 rdloe north c«0t of wir'. 43 fdla* ipouth o*tt (xf tho tout) of ttinart* It*

of U>» olaSBS In 49*-The doalitmtiai \Afrw iamff«oU»d lay loot! attraction ia 6* ittit

of io by toat

irclulofitoperty occwiffta of o (jwij> cf 11

oC .the wwCivif O.K! «? OeovwhouM l iu D!JCWH m t,h*j J.'CQ- 1;'«^> ijt'dch

olaSuo A:i otit,lin« ftf this report*

tte* iun" Vfill bt f ovtvi in tl»vlthto this ruport*

of t ' K> UVA tc digauat^d in A report b.. thct CkiUrlo of i lVKs in^j^J in ly£6 and ontltlixl A ProAiwiittcr/ r port

cci th» Goolxvjf of tlrt i\>^0/A.'jt Ww Aroci. The Carmdlari l^cljtio OotgAncr' ecgtt^rod tl»o DosivmixAi»3 lAko urot arid doooi-ibid it in thidr rcfiort BeAVVfldKiuao Lak« orat fb* ? by li« I/* Uartlcy, 1954*

Tha it>)d a'.' of a WIXTOW bolt of bfnuU

to

to JJLVO bwoo wry

-; in

thit

by or l oifr IkVffoiolt hum; bom iiitmJled tr/ caUiro am

oocwldmd to bo t)ja £aoct i^jaturrf. loot for i-divtmLiaation*In tho nirNaa ^vo a l.i«£ory al looal «l£idtim of rioet outcry nail outorope in W/doh toot pAta hod boon put dowi «i

ihcMn on the

av tb» tiwo

geology for1 the *r«a (Cttterio L\jp&rt»enl- of I'dbmse) show* tl« ciains to lie tutrid* a fssnwid nctthHKNith ocntwit between bttio volctmioa to UM> w&tA. ist< i^zwdtt to tlte ocisto Trm rotALltir ofthe Etti/«et'it B'ji'.tf,/ pc/.rfo$Twl m t^io e'i&i/os iweBW* thidt thin oc*^«wt

fcOloim 4 ero«$c ^!iluh rona tlirougit the ppofwtj arid into eitou£«i Lfcko* Vt;;. wlwnioi And $m;iite fore a

into R Htlib^oJx) itttMOiVd '.,; I '.13.O to

Tno if£>xfJUt^6 «i v.ld^i. tt« tctit pit& 2mw bo«n jxit dewn, ocnsift , of dlwwuJjiRtod pim^^lto («be*& 3 to 5- jwoart) with wliwr cislooiporfi in & aall'.c.lf iu'i iKivicwito. Ikwjsci of the UuJtod lu-oc* of oxyocf>t rook

ielfc^i tl-oruxvi!.1 IN'- *sv**» a. f«*r ftjawrd foc^. in wush ttfu«»» MM ctfUrft of iiw Kl'V£idi?At,k*i cxxilrf not tc- (.kAiwitiaU uoth '. 34/9 o3.cx» to & ptM,dm*r, toi>o

vltl< i» (tf\«^ fk

The pjrpoat of this type of away ia to looaia those tenet w)deh art good olcctricol omUicrtcwrtt* Thaa* wiH incite my or acu* ootibinaiictt of meuslw 0til|Jtid*0 or ffr*j>hi&«t wet fawlte er Bhoera* «ir*i\wlive interfwot KB in wet clay bod% and in aona aiaea

A )pf«roqaiiilto for tMootion ia tba inUitormwtlon af pziio!bt0^ oo that podu or diaawdnttiona ivy not bo looatad

an av4cdu The el&otrlcttl axwi B>XIMI on tba map will ooow vertlwlly &bow Use x^j^j1 o*i|ji» of a, tiody wlioM dii> ia 45* or taopi* At tha dip of, tht tK>V diidrd«h«»j» the location of thia aad« will nova farther down* dip,

TUi utrm^h of cxi:*.1uo'tor riiapoooa (for a givm tiwiaadtta? -. ' . diatanoe) ulH ikspaw oa ths omdootivity* Iw^th and dopth in tamt of width of tl«9 t^ti1^-* A tjm&Jcop oonducrtor th«r«for«» will rafleot taoro )ioorly oaidtKitlrci dusper or narrower bcxHo® or aotan ocni>imtloa of the 1

to bo underlain bj «r«niU. Tiiia watfld

Mi

pw»

uo

to e@uo

• •t •

MINES LIMITEDCOULEE LEAD ANDSURVEYELECTROMAGN

CLAIM GROUPBEAVERHOUSE LAAREA

DMSIONKENORA MINI

Scale - 1 inch tfl ZOO feet

KEY MAP

K. 26338

K. 27723

K. 27726 2633727725

, Swamp,marsh mlh boundary.

"~ Boundary of rock outcrop.

Claim posts or comer with assumed dorm ine.

location and number.

station with Inclination (degrees to the horizontal) dKection of resultant magnetic field. Westerly inclinations

easterly inclinations positive (no sign)

of readings taken from transmitterrx

ofoJrection and amount of inclination of lagneffc field to scale I inch equate 2O

(Northerly or westerly tndhatians (negative)of or beto» traverse tine; sotMherfy or easterly

'positive) to right of or atone ttoverse tine.

axes and direction of dip of conducting body from geophysical data.

Arts deSned.

Ads assumed.

S2FITSM*I4 63.879 L (NE LAKE

MAP N» 1957-90COULEE LEAD AND ZNC MNES UMTTEO MAGNETOMETER SURVEY BEA/ERHOUSE LAKE CLAIM GROUP POPULOUS LAKE AREA ONTARIO

COULEE LEAD AND ZINC MINES LIMITEDMAGNETOMETER SURVEY

CLAIM GROUPBEAVERHOUSE LA

KENORA MINBIG DIVISION

ONTWO

Scale: I tnch ft» 200 feet

KEY MAP

SYMBOLS

OO—42$ Picker t'ne numbers

on picket line.

Higher ground

S*amp, marsh mriri boundary

Boundary of rock outcrop.base srat/cn with artntrar/ value of vertical t of eartrt's magnetic field in gammas

Claim posts or comer with assumed ctatn line

station *itti fe/ertve value of verfjcat aortiponent magnetic *iekt tn gammas.

of equal vericc! magne^c intensify in

magnetic trrtensffy of less than O gammas.

\Jtricai rragnetic intensity of O to fOOO gammas

mtiaal magnetic intensify offOOO to 2OOO gammas

magnetic rrtensty of2OOO to 3OOO gammas.

magnetic intensify ofSOOO to 4OOO gammas.

intensify of greater than 4OOO gammas.