42A0SNE0337 2.2957 CARSCALLEN 010

n t P o R T

on the

BRIU SiHlUt) SYNDICATE

Tpunnhlp, Hntorio

wt, Ontario,

November TJ, 1976.

H. J. UrmiBhaw, !J .

Gctnloglat.

Magnetic rand elitctrowngnRtic eurvoyi! HBVB boon conducted

on the to r BC ill l t;n Tourmhip property huXd by the Bold Shield

The picket lint; yrid wen established on tho property

duriny October, 197B, ond the survey work WHS completed November

12, 197B.

Several gold ucourruncun on ihu clBltRB uerct oxplorecJ by

Oowucy Dimton Ooid M i rum in 19*46. The geophysical survey work Is tha

firat atn(]8 of an uxplortition, development programme to he undar-

tnkctn tin the 'ci Him group. ''

j, LOCATinU AfO /iCg.!^

The property is cofopritmd of oix claims staked In Juno,

1978, num!,erud PS16QStt t 516051, 51671*7, 5167(*6, 516761* end 516765.

The property covers an iiroii of previously patented cluimo which ex-

piruri on Juno 1, 197B, l)ODftutHi of nonpayment of taxes.

Located in ttouth-contral Cnracalltm TounBhip, thu claim

group in nbout ?.U m iltto uisttt-southwent of the Kity of timmins.

From highway 101, about a mile o nut h of the claiRR, the

property is nccRBBibJe by gravel roed. The rond on tha wnst tihore

of Unrlton Liike hno buen rebuilt to tho Donton-CaracBllen Township

boundary Inaa thnn B hnlf mile from the claim group.

uork on the property has bfien reported in the

Northern Miner, ritiinly in 19'*6. Nel0 HOQQ, a former

- 2 ~

t for the Porciipinit ercm, reportnd on tha cliiitnu bhnod on

e wRtik'a lix&mintttlon In 191*6. His report describing the various

gold nt:currtmcit8, can ho uxaralnert in provincial governnerit aasjQtis-

nmnt work filiHj. Thii thrtJO mont nignificant gold dapoait*) tsre

lb'id UK the 1010 und Oowooy voiiiB, end thR wire gold shoulng.

Thn 1910 viiin IB Inntsttfri on claim 1*516765 nlong base line

Accurdint) to Hogy, it BtflktiB north, dips utifit and was traced

wittimtly for n disttince of 700 foot. TJ.JO ehnfts fciern aunk

on the vein mi nhoun on the a'cconpsnying plan; thti north nnd south

Bhart?*, 3DO fefft epart, ere ^ H tuJ 19 fei't deep ruspHctivdiy. Thn

vein WHSI invttetigattul tu e depth of 200 feet by 1'* drill holes;

hciuiBvtfr, no BHIIpliny renulto are prouidtid in the Hogg report. The

Northern Minor of Ouwj G, 19t*6, Btfitua thtst thu 1010 vi?in hod been

trtmehRif for :' di H time R of BRvitral hundred ffttit shcwlny htiavy pyrite

and Brtwminyrito minpreliirntion for uidtfm uaryiny from six inchea

tfs ont! foot ant! thbt fHimpliHi taken owar on avaruyu width of about 6

inches ynvt? vu)utMJ tif 2.26 OK,, O.i*6 02., O.'*'* oz., 3.31 oz., U. 12

ox., 1.72 Di?, s'fui 1,'i 1 or. Thujiu aaaaya ovtiroge 1.3',) oz.

Tin* .lounuy vi'in li? located on clcsitp P5160S*1. According to

Hogg, it sirikftci nortt'i oni! dipis Rowt und wau truced fur about 70U

font. A yuld btutrititj vein on the eouth boundary of thu proporty

may rupryet-nt thy isouthuurd cxtermion of tho Jouuuy vein otructure.

Hoyy dttacrittffii this pruiiRnce of two main pito on thu vein, U30 feut

apart, wml having dtiptits of 2d and 1G font. Hs furthnr o to tt; e that

nix h;;lrn tMirtt drilJrtJ to B depth of 300 fuot on the vein structure

luit no vnluuu n ttt g i van. Trm fturthftrn Minor of June 6, 19'*6, in

rtjfnrunei! to tho Joufmy vejn (tiet&n thut sampling rauu Its showed

6.0 o*. over 0.7 fmjt, 3.1 ox. over 1.2 feet, A. ft oz. over 0.0

foot, fi.?.? ut. l iver 1.0 f wo t and 5. M ox. uviir 0.7 fuot, ** chip

eamplu takpn from t)fr-vim;l pli*c;oo on thu vein tiimnyad J?. 66 o?. In

tlm July 11, 19**G, inane, ono drill holts IB m ported; Ht B depth

of C.H feet, ti Bifctiuri of 1.1 foe t aseuyid ;!.B2 oz. ooltl.

According to Nalo HOQQ, thrs wire fjnld untwine) on claim

f'51liiOSU WHS a BtJftctHuuliir diacovtsry uhich rlid not tixtfind to depth.

Much of thti ore ir* en iron formation ended up in wlnnrel collections

throughout thi? country, iiurfwce HxplorBtion in the iwwodiwtR area

f oil od tt find eniditianfil mineralization.

the* cloit\ group ife oituutud ut thti want entl

of thii r-Drcupino yold cimij* juat north of tho Briiitol foult, ths

ut(ffti.unrri pxtBnnion of thtz f-orcupinB-Ueotor ftiult, o ntruttturn com*

men to mont pant Rod pritntrnt produnurft.

Tho five wont unsstorly clainiB oru riowinftntly undorlain by

e grey yrtsnitoid rock,, rwf erred ko ua a granite by pruviouu workers

Thin medium to coursu gruinud intrusive may un;ier Johorutory nxam-

irttition ha clasnifittd in tho qucrtr monzonite* grnnodirrito yreup.

The moat eattturly cltiiw i a undurlnin by intorensdiKti* metBvolcsjnice

with nnrmui ht*du of iron formution. Thn voin structuron, faulting

en rf dinhaan dyketi in the immtsdint ereo Btrike generally north.

Sumplino, undertaken In thi* vicinity Df 1Q10 and Jouaey

veins is fjRocrihutJ In the Appendix.

TlC SU'lUilV KEJiULTa AND INTtHWlTATJON

The muQnutonu?tnr wurvuy data in plotted and contoured on

thn occnmpanyinfj plwn at e ucnle of one inch. to two hundred feet.

Tha InfitruTitmt find ourvtiy .mtithod tre deacribed in the Appnndix to

thi B report.

A poorly defined north trend uf the iBomagnoticu le Bp-. * , - - ". ; , . - ; '. ,- •••. " r

parunt uith thra mngnutic hHckyrotind in the 300 to SUO gawwp range.' '.- -. ' * ,' ' ; ' ; '' '*' ':

This rengs nnd inteinsity of magnet i p yai,Uff8 is distinctly

diffnront on nluim P516030. Thio clcim is underlnin f y:: ' ; ' . . .. ' ;: .', ~"i - - .\'---'*' -^ - -vnlcBnicn and iron fnrmatinn utrlking nhuut north. The north

trnndintj crnok opproxiwrttnly mwrkn thri cnntant hatWfjen ths?

intriifiilww to thR uuist and mntovnlcnnipa to tho ennt.

On the rnmoinder of the property fi*w obvinua wiagnetic

fentures t*r# auprirent. MouinvMr, a unnk north trondinc) magnetic

enoniAly cnirinidrsn with thfi 1010 gold vein on claim P91&765* Along

the east oldo of thin cljilw on the lake ahDru part of a nimilur

to he present.

This wiqnifinHnno of yn iBolated wngnutic Hifjh ot Stntlon

1K1C on Lint? I!'iN ia not rendily

TIC SUHULV lUjjiULTS AND

nlontromfiynptic survey date IB plotted nnri contoured

thn ocKampBnyJrvj plitn at B Benin of tine inch to two hundred fact

- 5 -

The instrument and Bun/ey K^thnd oro dftserlbmi in thB Appimdix to

t hie report.

Thi) dip unglft prof i Inn on thu property eru generally

characteristic of i.wVk conductivity. *'rofiiaa on claim f ''51 6765,

tt long thu Inkn, ItMicntn n poanibln strong conductor (striking north

in the l nku.

Conductor1 A in ths northetiut saction of thu property, o

, epptifiri! to corriittpcmtl to the contact bdtuaon wuto-

to thn tuiut nml tht; fnXuiu intruuive to thu uout.

A Dorion of wuuk conductora, Utisiynatod U on thu uwat uide

of thu propurty, oxtend north usj a ztinis f rani thw snail luke. Theeu

rHprunent o P.*j^or fuult rone.

The oiQnlf icttncR of wonk conductor C tin tho uoov Hide of

n ''51C763 in nut rucdUy ppnrunt. Uther poorly defined croaa-

rtt on the property do not iippwur to ruprw&esnt aignificont con

ductivity.

A uttek tnugntttic tmomaly correspnnda to thw 1010 vain

Incotitm. tJith this oxcoptiun, significant mnymttic or ulcctro-

tnaynutit; fttuturttB do not correspond to known yold winurnlizntion

on thti ci uim group.

Thore in, howover, o good indication that t* north trending

magnetic high may corrnnpond to a nonductivfs zone in thei lake along

thu ooist boundary of claim rf.167^5. Thit. poisiiiUllity should be

chncktid by BdditJonritl wuynKtic wnd. alectwjmBQnetic; survey work

this winter.

on prfiJiniimiry SBmpliny for yold, it in

that thu property bf? QE;O logical! y mapped and that this various gold

oceurruficoB rocttivo particular attention. The ror.k area in the

vicinity of ttuf gold occur r linea B ahoulu bs re-iaxpoued aa Much as

potiBibliJ utS listing iiuitBblt: power equipment thareby au ti i o t i no, the

gtuiloyict'l rowppiny and providing w dunn surface foi rock stunpliny.

T ho uHff.pl imj enu nuippiny would provide the necnitliary i nformntinn to

whorn oholloui diiwond drilling its necnBSwry to nutline

gradu gold winarallZBtion.

of the pvntjratsne i n outlined r*a follm-m:

. , , . . . . . . . . . . . . . . . . . S 2,OPD.

Bull dozer rcnttil . ,, , , . . . , . . . . , . . . . . . . 10,000.

Hock trenching and tuirfpling . . . . . . . . . . . . . . . 3,000,

diBBinntl drilling . . , . . . . , . . . . . . . . . 10,000.

To tHl i; 3 3. ODD.

Thie uurk nrm nnst iiffnrtivBly he undcrtHknn in the

spring pnti os?rly aumwtvr of' 1979.

Respectfully' ' : ' ' ! ' -

KM! t: LO !K:'WHY!iJC:i IJHITrt),

ntano

Ministry of Nati

GEOPHYSICAL - GEOLOG TECHNICAL DAT •1PA05NE0337 CARSCALLEN

TO BE ATI ACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

900

Type of Survcy(s) __Maijnii.tic S .Township or Area... J^arscal lcn JputnshlEi__————-Claim Hoklcr(s). ..W.. J. Bradbhftw (MIGKD)

Survey Company ̂ . Jihiiilli li t: D fully si Hii ..Lilliiiilll—.—

Author of Report ^....K,. J. BnarlaLiaiii.-....-....-——^^^—-.—.

Address of Author. { J .,U. Bnx MO, T.immins, Ontario

Covering Dales of Survey.——

Total Miles of Line Cut_ .

-.... (linecutting to office)

.SPECIAL PRO VISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

Geophysical

Electromagnetic.

- Magnetometer—

- Radiometric.

- Other____——

Geological ——.—^—

Geochemical -^——

DAYS per claim

1*0

20

AIRBORNE CREDITS (Special provision credits do not apply to airborne surveys)

Magnetometer ——

DATE:

. Electromagnetic ___,._ Radiometric (enter days per claim)

SIGNATURE:uthor of Report or Agent

Res. Gcol..

Previous Surveys File No. Type

Qualifications ^

Date

' i " ! ' ;Claim Holder

MINING CLAIMS TRAVERSED List numerically

.........P..............5.16.9.5CL....(prefix) (number)

.........................5.16051......

.........................5.16.7.WL....

.s

1

g •o

TOTAL CLAIMS.

GEOPHYSICAL TECHNICAL DATA

(ik( )UNI ) SI 'UYI'.YS II n K M e 1 1 i,i 1 1 one survey , sjiccily data for each type of survey

Number of Stations.

Station interval.

Profile scale.

Contour interval.

EM 320..Number of Readings ..

^^ Line spacing. ... ....

1" :

1CID - magnetic

oHo

Sharpe M.F',-1 fluxgate .magnetometer ,....,.Instrument.

Accuracy Scale constant - "t OF "- 1D

Diurnal correction method. ....... .

Base Station check-in interval (hours). Check lifMjciSfj station at-less than Base Station location and value. iiitorvfils located a long base linrj at^QCL .

font i ntervals .^ .^. .........l ......J

u

,,

O

PT

Instrument .

Coil configuration .

Coil separation .

Accuracy.

Method:

Frequency.

Parameters measured.

Honka LM 16

Vertical Infinite

H nr - 19o

l.x! Fixed transmitter 21.'. Kh*.

L l Shoot hack L l In line L'.l Parallel line

Annapolis, Maryland(specify V.L.F. station)

fit'ld S quadrature components

o

hisliuinent .

Scale consUinl .

Collections made.

Base station value and location .

Klevalion accuracy.

^N!

T3

'St

lnstruinc.nl .

Method [ l Time Domain

Parameters On time .

Off time .

Delay time.

Integration time

Power.

Kleclrode anay.

l'',leclrode spacing .

Type of electrode .

[ l Frequency Domain

^ Frequency....

..-. Range.

Turnbull Twp.- M.316

DANA and JOWSEY LAKES

,' WITHDRAWW.FROM ( STAKING l

Denton Twp.- M.273

42A05NE0337 2.2957 CARSCALLEN S00

CD CVJ

l

d

. w*k. CD

THE TOWNSHIP

ARSCALLENDISTRICT OFCOCHRAliE

PORCUPINE'MINING DIVISigiSt W;~'-''" ' t- '..'^'

SCALE: 1-INCH ^ 4O CHAINS

i LEGEND

PATENTED LAND

CROWN LAW) SALELEASES -*LOC4T10 L ANDLICENSE OF OCCUPATIONMttftN* RWTf OMLVv-SURWCC EIGHTS ONLYROADStMPftOVeO " ROADSKING'S HIGHWAYSRAILWAYSPOWEfl I&S& A. 'MARSH OR MUSKEGMINES v ^" .CANCELLED -PATENTED S.R O.

v-t v'

u-M i O,S.R.Or

, co

NOTES,x4QO' Surfocft. Rights Reservotjon orownd all lakes and nvers •\-,, f "

This township lies within t he M unicipjoKfy of CITV of TIMMINS. ' ^

PLAN NO. M* " *

()\'l 'SK in

MINISTRY OF NATURAL RESOURCESSURVEYS AND MAi'!-;NG BRANCH

Sr- -- M"- 1

LEGEND

Measurement station along picket line

Relative value of the vertical component of the earth's magnetic field in gammas

40OMagnetic contour

f ) Magnetic depressionU*Z00-^

+ Bo*e station location

Au Gold occurrencea Shaft1 Rock trench

INSTRUMENT: Sharpe M.F.-l fluxgate magnetometer

MAGNETOMETER SURVEYON THE PROPERTY OF

GOLD SHIELD SYNDICATECARSCALLEN TOWNSHIP ONTARIO

by SHIELD GEOPHYSICS L IMITED

SCALE o_______290 490_____6QO

FEET

NOVEMBER 19764aA05NE0337 2 .2957 CARSCALLEN 210

LEGEND

Measurement station along picket line

In-phase reading (Ve) plotted to left

Quadrature reading CVW plotted to r ight

Profile scale : l" = 40Va

In-phase profile

Quadrature profile

Conductor - well defined, weaker

ELECTROMAGNETIC SURVEYON THE PROPERTY OF

GOLD SHIELD SYNDICATECARSCALLEN TOWNSHIP ONTARIO

by SHIELD GEOPHYSICS LIMITED

SCALE Q_______290 4yo______600

INSTRUMENT: Bonka EM 16, No. 36FEET

NOVEMBER 1978