20 3-S

4?A08NW0118 63.2035 BOWMAN 010

SUMMARY

''\ C 'jiv.biner."! ra^netic/elcctrurw jnetic survey has

been CT.ij.'vletr ' on the jv-v.roan Township property of Devil's

F:lbot- Miiieo Lir.it .CK*.

The ninrrnU /od r-nnea Ttno'/n on the property ohow

ulosopiinatiKi a.'JLphwJrifl iron which none copper values in

oxcoisa oi 2.00;i liave been obtaineii.

11 jo r,lftctroiua"jnutic Survey v/ao intcnuccS to outline

the cxtcnsionn of the known mineralised rono where oboc^rod

by ovcrburc'ca, and trj indicate other roneo of poosibly

cconir.dc rv.i.i; -ral I ;i

JuU?rjing frorr, the electromagnetic response recorded

ovor tho Known mineral i zat ion other mineralised zones could \

bc indicates! bv nimilai: weak anomalies. Three previously

nnhtiown -onca warrantinrj investigation by diamond drilling

hnvo boon izicli.cated. Tho location and particular o concerning

the rccoiiv.uendoO tlrillinrj follows i

E lo lo Jto\t, ggjy.gr^ j^catioi^ Dojyth Inclina t ion

500* ~S5 0

250' -45 0

j 'Xi' n")xth of: Station 250* -45* .MOUV.' line l;.'-fDOS

3n* tirvith o f. Station 2-JliOii li;sc 20-:OOS

iJaoo liacj - Ctation

A. C . A . HOWK * AKSOCIATKK LTD

Inclination

100 ' north of Station 21*0* -45" Due Gouth

Hi 0 ' n^i:th o I 5tatio,j ::ifi* -^5* D-ac Oouthj.;- ;'iO\; iino 4 f?:OOr,

•J'a j o.';!: oT Cue t.lrilli".q j)ro-irani ia c st l ra t. ccl to

total S l or i r* ?. r n.

A. C. A. HOWK ft AHS(M:IATKS LTD.

- 2 -

The property conoioLo oi forty (40) cont i-j

i m *at e ne o u tni.ns.rvj claims ior.nuno, a block two and o a-hali:

U.oti i r OP' emit. to west at the vitleot point And one and ono*

a3 J" miles north to so sth at the wKlctst poi ; t anc* containing

s :-aLoIv 1600 acres. Thi-- claxiT\ nuubero arc; aa i'oil^wot

'jJ'JO to 0000*1to 00526 inclusivo to t JObliG inci' oxvf'

The property in oituatcd fo.u {niloo to the oo-rth

oi the To.,:* 'il Ilatbonon. ITio claai'.sjj arcs located in L-ote

/i( S, G, 7 nivi (f,, Ranyo I, li ancl HI in Uoijnan Tovmahip,

itxGtrict o i. Cochrane, J^ird^j: Ijako Mlninj Division, Ontario.

Accents to tho propt*Jrty iu easily available by

rxiane o t" a r on*, i u^iioh travornfia tho property XroiTi r*arth to

eonth. In ac.ci3.tion, a b j eh trail runs to tho shoiany on

Olairr.a 1^-80524 ft ne! 1^-80525. Tliio trail is accesaiblc by car

in the suranar. It can oloo bo used aa a winter road.

The Ontario Northland Railway paaooo through f-Sath-

esoii, lo a uilca to tho north no ciooe also the Trantt-Canaua

Pipo Lino and Llio Hydro Electric t*oi or Line.

A. C. A. HOWK A ASHCK:IATKS I;ri).

- 3 -

Tho terrain lo mainly flat lying with numerous

rrve\ 01 ••tcropw on tho southern half *jx the property. Trea

nu connista mainly of second jrowth tree a.

Copper mineral i::ation iiaa !jccn Xnowri to occ *.r on the

property lor many y car a. In 105C,, Sylvanite GolO r.ines took

an option on the property. Three ohoxt drill holeu had bcxsn

pit Jiov.-n provioasly and .sylvanite put ticn^n three laoro v/ith a

total length of 650 loot. Considerable trench i ny waa aldo dono.

Astray D of chip snnipJLes ta^on b*/ Sylvanite were reported to be

l.fiTa copper aoro33 G. 1 ".' foet an\ : 0.6/i copper U--VTJBS 5.6 feet.

Tho main inter out of aylvanito at that time wao in

the poawibie oixxotanco of 'jol" valuco, howevex no ijolc, values

axe reported. Tho option v,-ao oubneq 1 cntly dropped aiio no

farther war!; io roj5ortetl on tho property ainc© that date,

other than ovtiiaco aaiq)lin(j and prospecting.

iX^ivii*o liJ-ixav/ Ilim^a Linitcu holdd an option to acquire

tho property.

Tho property ovorl ioa v^^lc^iuc roc?'8 ol Keewatin Aye.

A. C. A. HOWK A AHSOCIATKK ivrn.

These coaxial ol ;;^3ai\fc and pillow lav.ia an well au minor

-jaboroic ana acid intr p s i vos.

tk.rJ';e:cou3 tfiabaae elyX.es havo intruded theecs roc K. a.

A large granite l^atholith occurs S'*uth o J; the? property and

i to north contact vith the v^lcanicn i ios alony the oo thorn

r'U-;;r" o j? tJic jjro;.*erty. The volcanic roc*:c have a atriXro dir

ection ?:aii;,inj rrow north 4?*' wcBt to north 70" xvoot.. Dips

are variable laTVjj.n..; i'rotn vertical tvi otocply north OIKI

oolith.

iiarint) proupectimj of the tiiea carried o it in the

early part oi the Century, lov ^old values arc rot-iorttid to

occ^v in q sartre vcino in tho area. Old reports neat ion

lota 2, i*, 7 anu B o j; Coucoaaion II v/hich correajjond to the

t'soal.horn or^a -ti the property ot Devil'a Elixiv; Mxnco JLiimiteci.

In nckl4t-v.ra, old rc^xsrtn i.ontion tho O)pper ahov;in^ i.. the

aaine area. Consider ab l o trenching v^ia done In the location

o i: tho oritjinnl whovxni., ao voll aa in the aojace.it a r on.

The showing CDnoiato of aplaslies of naosivo chaleo—

pyrito in n ^rey fcIOspar porphyry and along tho contacts of

tho porphyry and oneida i n^j volcanic rocKo.

In audition, ulioacainatocl clialcopyrite occ *ra within

tjch.iatoiic vi.*loanicfi o ve i' n './i Jo area on the? oolith B i o o oi the

contact. .s.Hi'Jo yalo'iu '-'aa al&o obaervtxi in the areas oi

A. C. A. HOWK * AHSOCIATKS LTD

vs om

An /JLeict rvyfi. piet le . ffiurycy covering the entire

i-, -an complied uuriivj June,, 1:X)6.

eY cover inc. a^proxiroataiy one

hall' oi1 the ,;'in;5ca:ty was alno corral* ft ou.

n• -./an acme ..lairiy a

J. L. M. Unit. Tiio motliot] .uocl is v3encrally }'.

aa th:: sho-vt n^Ci- tc-chnicjue, aiace toth coils are capable of

tranomittin i aixJ rccQiv.lno and at each station tho operators

alternatively tx*ansriit and rocoivo. Tlio iinaX reaclinrj,

plotted at t.he point nitnv-ay heti.^w©a the t.w*:* otiila is thi

XTi;3'';ltant oi ti.e tv.-o dip ancjlc-n soct*r f.'ttxi by thts operators.

Tho hitjh txetjnoncy oijivnl (1800 C. l?, s. ) x^s used

tJhicotKjbor.t t'ho .survov except vhero anw&lrmu or^nciitiovia appeared

t o cxitit ; iu tala caso ocvoral chec". atationa WCJTC: read on

t.ho Imj (480 C.P.c^. ) frequency. A positive res l tan t generally

occurs ovor the ajrtu ol a vertical or near vertical conductor

uith no^ative rea iltnnta at tho ecJ.jea of the eond'icttjr.

A description ol tho inatrtimeut ia ttppcnc3o^ to this

2 O'..o s: t .

A. C . A . IIOWK * AHSdCIATKK LTD

. 6 -

The L. waa dona naiivj a Jhai-p&'a

e Ma^netorieter. Rcadincjs weie tal;en on lines ap

at ^00 it. intervale; atation interval 100 ft. Corrections

v.'cif* inack* tor diurnal variation ,.-ith no circuit time greater

than o no ho. i x v .-i thry.it n bane? lj.no chcc"-;.

Technical t'ato portaininj to Mie 1,^0 •j

-.i t v* t h. l o rep

The. Magnetic Curve- pr^dncev) rcanlts which

in interpretation of *^o'*lo. pjical atrnct'-.rfta arjc' niOcd

eva i ant in cho i."ioct.rona jttotic animal

net, i? j jriv

in

T?io ohnr\vin j ax-oa ' 'as teatotJ in Detail uain-j the*

J. K. H. Unit, linea at. 1 00 tt. Inter val o ovor part -)i the shoeing.

Those i t now wftro ootabliahdl to oivablc the .(OophyeicaJ. operator a

to iJctotitane a reasonable criteria i'or itttozprctin , rea(.\lto

i roil tho x eel- o I tno property.

Tile mineral i r.at xin j.n th*j nLowin art,-*i is relatively

t: iauoinl'iottH.1 t.horofoxo only n weak fiiootrintja'-.m't ic it^

c v^ i i ci bo expected. 'lt\e (.'tutali envoy i,n the iiicii v t w nh

ia.j cstabliohtvJ ni'iniixcant valuen i^r thia tvpt )1

A. f. A. HOWK A ASHOCJATKK lvl l)

- 7 -

Five area*; wore invest itiatou in octal l . Areas

virthy of f.r.rtlier .investigation Ixave I 'ceii oxitlineu.

Ar oa^ JL - Conductive iono A (orijinal

Thia area has been Grille*! on two previous occasions.

The in for ration recorded fro.t this drj.llin'i IK incopplcte?,

t;:x:c*?pt to chov/ cMaaerunatccl minoral ivntion ovex a width oi

npproxlt\.atel', 100 i:t. in a ijhcar j-one Heveio^eu in r^cta—

ocxiinicnLta alon-j nn ii.inof^ua contact.

Tiie elc'ctronvajnetie anosaaly i.* L-roaci and vveav, possibly

in-.iicat.injj a wide but poor conci"Ctor near surface or a stronger

eo:;ductor at ;n ator i.lepth. The conduct. i. ve Jx>dv appears to

dip t 'i the sonth '.'fat: .

Orif; 5 DO tt. drill hoio iocattv* at a jxiint SO It. j*outh

oi station 230 l Aiot , lint; 2^*OOiJ inclines at -*15* , bearing

H2C e L is reccy.ysrncimJQd to tent the rone at uc;pth (iJ.J3.H. Mo. 1).

/urea^JL - CancUtct ivo Son* B

Tiiis auoinaJLy is alas wt-aV b iL roiativoly wxv'e. The

sar,\c poesibilltics aa in Comluctivo Tone A apply.

The probable dip o f. the conduct i va rone io to the

nnrth. T'-n chart holco to test the ea )fie 01 this* anonvaly arc

iJ.,,),H. 'Jo. 2 - Location - Saue lino at station 120CS. j -15*

A. C. A. JIowK A AHHOCIATKS I;ri).

- 8 -

t?3?)*v/; lcnuth - 250 ft.

D. D, H. No. i - Location - 50 ft. north o i station S-iOOVv, lin*

1200S; -45*; C300 H; l ength - 250 ft.

anomalioa occur in thin area. One on lino

s opproxirnato.lv Ji600 ft. x/oat of the bane line lo aoaociated

uith a raa^notic anorttaiy.

The narjnotic anomaly inay rcproseat i'a^.itin j or ohear-

iny in approximately aa t-aot-i/ost dircsctioa. The indicated

conductor folio a t ho Magnetic tron*l. The condMctot dips to

the north, one drill hole (O.D.H. J*^. 4) 250 ft lony, located

100 it. north oi1 Station 2500W, line 56-*OOS lo rccO' Jaoixioo ,

Iliisi hole i3ho'?10 bo drilled Azimuth 130*, inclimxj nt -rt5*.

Tho second anomaly in Area 2 lico along lino 'Jd+OOS,

from iitatio -, ^7^00^ to approximately Station JX+OOW.

'X*hc conductor appear o to dip to tho north. This

conductor tihoulO ho tcatcxJ by a 250 ft. drill Iwl© (D.l).il. Ho. 5)

iroiii a point-. .150 ft. iv*rth oi Station 30tOO;; on line rta-K)OS,

drilled al; -45*, Azimuth 1B00 .

A.iditional v/ork will depend on the reaulta oi thie

initial o^'lova

A. C. A. IIOWK /t AKHtH'IATKK I.TII

Tho fjcophysical 13 trvoys have outline*?. three new

?o iea warrant i ny additional investigation.

One tieep hole (500 ft.) i a reconiueu^esj beneath the

trenches on tho original onowimj to establish whether or not

thero in nn increase in rfanarali-nt Ion with depth.

Fovtr ^rospcctinfj holes arc reo'W^ucnciexi to exrplore

c of tiic riev anoraalioo. Th^DO holco will each Us® 2 50 it.

in

A total ot 1500 ft, ol diamoml drill in i will bo

reqi irod. The location

no follow.

other particvtlnirs arc a

.Ho . Colar

50* ootith of Station 2-fDOi; lino 2*v*00.'J

Barso line — Station

50' north of Station IMOOW lino 1

100* north ot Station 25-iOOVr lino 5

ISO 1 north oi stationO^OOV' line 4 B l COS

500

230

250*

250*

230*

M20"E

S 30* VI

S3 O0 W

South

Duo South

In ordctr to dofinitffily csotablish the mineral potential

A. C. A. IIOWK * AHSOCIATKK I ;i'l).

- 10 -

ol the iJovj.i'i; r1 ; v-*r., ; ?',)iu,"fi Limited, Bov-wan Township, Ontario

an initial total of 1SOO j?t. or diamond drill. i

-..•ill bo rfxj irod. AcMiti mal work will fJcpcncJ! 0:1 the

rco :lta of fhlsj oq.^loratory uianiou:" Or *. li i MM.

It ir. r* G'jr. ^ern'od that the outline*'! drilling bc

carriccJ O'^t.

Tli o cost o r tho ixri.ll.inri pro-^x'ari ip estimated as

1. luarwnd ijrillirvj - 1500 i;t. at fcfi.'.?Q por foot

2. Mobilisation ^f drillljv.; eq-.slp

.i. spa 1 1 in .j ox, 'Jriil liolea,vio.io'i of program, lo^-jtnij of core a SK i rejxwrtiny.

4.

Q 7 50n. 00

C 00. 00

1500.00

C 10000.00

Rospectfully er,hr?dtted, A. C. A. IKKW C, A^

/•r'

9(7J. 3R. Tilaley. F.G.A.C.

A. C. A. HOWE A ASSOCIATKS LTD.

Crone J.E.M. Dual Frequency unit

Each coil is a combined transmitter - receiver

Frequencies - High 1800 C.P.S.

- Low 480 C.P.S.

Input to transmitter: - 0.6 x 12 Watts

Receiver sensitivity - 1800 C.P.S. approx. 0.10 microvolt

480 C.P.S. approx. 0.10 microvolt

Methode.of operation.' , Jlp.'M.',(shoot,back)

(Ref. Interpretation Theory in Applied Geophysics'Grant fe

West - McGraw Hill - Page 448.)

f, l" ^ U ix-l i t P

t, : i )^ - j ^-} ^

VERTICAL INTENSITY FJ-TJXGATE MAGNETOMETER M F -j.

S ? E CIFIC ATIONS .

MODEL MF^-l Standard surveying and prospecting magnetometer with self- ^ levelling sensor.

Ranges: Plus o r minus -1000 gammas f. se. .Sensitivity:. 20 gammas per div. 30CO " ' 50 ' " '

10,000 " , . 200 30,000 " 500 " "

. " . 100, 000 " 2000' ; . "

Meter: - Taut-band uujper.^ion. 1000 gamma scale: l.T/S'/'lcng - 50 div.3000 " " : l r 1 1/ 16''.' long -60 div.

Accuracy; ' 1000 to 10, 000 gamma ranges ^ Q.5% of 'full scale30, 000 to 100/000 gamma ranges -irj.% of full seals (

Operating Temperature; . . . --10 O C to 440 O C.' ' -iO 0 F to -i-100 0 F i' '' '''.i .1, '. ,.., . .•' ; ' 1 .',

Temperature Stability: Less than 2 gammas per OC (l gamma /OF) : .'i i

Bucking Adjustments: 10, 000 to 75, 000 gammas by 9 steps bf approximately : (Latitude) 8,000 gammas and fine control by 10-turn

potentiometer. Convertible for Southern hemisphereor -i- 30,000 gammas equatorial^' — i

l\otUvruMi: 12 x 1. i.V-1'kihiilirrht battorict; ("C" coll typo){AC Power supply available) '

Coiuiuinption: i) O milliampcres

Dimcniiions: ' Instrument: 6 1/2". x 3 1/2" x 12 1/2" - 165 x 90 x 320 mmBattery pack: -i" x 2" x 7 " ' .^ 100 x 50 x 180 mmShipping Container: 10" dia, x 16" ' - 255 mm dia.x 410 mm

Weights; Instrument: 51ba.l2o2, - 2.6kg. Battery pack: 2 lbs,4 02. - l kg. Shipping: '13 ibs.

Quarts

—J Gram

L _ .J i asas

DEVIL'S ELBOW MINES LTD

Source OD M mops 2O7I E M-333

CLAIM NO. HAYS

TtU'Al, OK PAYS

l A LAl M

l Al Al Al Al Al A1A l A l A l A l A

Mil!

Carr Twol

McCann Twp

THE TOWNSHIPOF

BOWMANDISTRICT OF COCHRANE

LARDER LAKE MINING DIVISION

SCALE : l-INCI-^40 CHAINS

LEGENDPATENTED LAND

CROWN LAND SALE LEASES

LOCATED LAND

LICENSE OF OCCUPATION MINING RIGHTS ONLY

SURFACE RIGHTS ONLY ROADS

MPROVED ROADS KINGS HIGHWAYS

RAILWAYS POWER LINES

MARSH OR MUSKEG

MINESGEODECTIC STATION

or C S.

©Loc .L.O.

M.R.OS. R.O

NOTES•4OO ^URl ACF R

ALL LA K, t.',

fONT. DEPT. OF MINES j MINING LANDS BR.

'' T HIS MAP FOR CHECKING , PURPOSES ONLY - MUST

NOT BE SOLD.

PLAN NO.- M-333

DEPARTMENT OF MINES ONTARIO

79998799908000080001

8052680642 806438000580002

8000480003

80524

8064580525

80523799968052279997

79995 799937999479992

8065680655 80654 80653

BASE LINE No 2

station along picket me.

4oo Relative value of the vertical component of the earth's magnetic field in gammas..

Magnetic contours, contour interval 1OOC gammas

Magnetic depression .

Claim po?t

9ca)e- linch to 1/2 mi le

INSTRUMENT : Sharpe M.F.I Fluxgate Magnetometer

42A08NW0I18 63.2035 BOWMAN 21O

map by dee O'^honnessy /9t

AREAT4]

AREA lCONDUCTIVE ZONE

AREA 2

AREA 3 j

•79993

MAP

BASE LINE No

BASE LINE No-2

SURVEY AREA

B OWMAN ^ T OWN4SWIP

Scale i inch to 1/2 m i le

Instrument - Crone J.&.M. (dual frequency)

Method' 'Shootback' -200ft. coil spacing \ High frequency profile ('Qoo c p.-s J v Lotu frequency profile C 480 " )

Scale of profiles l inch fo lO"Conductor?

Trench

42A08NW0118 63,2035 BOWMAN220

SYMBOLS

station a long picket line.

4oo Relative value of the vertical component of the earth's magnetic field in gammas

Magnetic contours, contour interval 1OOO gammas

Magnetic depression .

Claim post

INSTRUMENT : Sharpe M.F.I Fluxgate Magnetometer.

WEST GRID (No.l)

DEVILS ELBOW MINES LTD.BOWMAN TWP, LARDER LAKE MINI DIVISION ONT.

MAGNETOMETER SURVEY

A.C A. HOWE S ASSOC. LTD.

TOO 2CO 4OO GOO eoo

FEET

7

AREA 4 j

AREA lCONDUCTIVE ZONE

l l

AREA 5 jAREA 3

•79993

Instrument -- Crone J.L.M. (dual frequency ) Method- 'Shootback' 200 ft coil spacing High frequency profile t ieoo C-P--S.I

Lotu frequency profile C 480 " J

Scale of profiles l inch fo \O 0

Conductor?

Trench

WEST GRID (No.l)

DEVILS ELBOW MINES LTD.BOWMAN TWR, LARDER L AKE MlNJ. DIVISION^ ONT.

ELECTRO-MAGNETIC SURVEY

A.C.A. HOWE a ASSOC. LTD-7

TOO -2CO 4OO 6OO eco

FE&T

3 - July 'GC-