V 42A82SE8279 63.3382 CAIRO 010

iILi'CHEMICAL bUr'tl/t. V

on the property of

.-'ii:i(;.: ?B LTO.

Cairn Tnwnohip,

T immirui, L-ntr-ria ,

IMnv^mber "lil, 197!;

H. J. Hradshaui, P. Eng,,

ConBulting GR

INTj'ICiJUCjIDPJ

A HoiJ sampling progrHimriE was undertaken on the Majestic

Wiley property in Cairn Tcminship during the ppriad August 19 ta

October ^ , 197!v. This s??mplns wars analyzed for copper, lead and

zinc and plotted nn the appropriate plans.

Purpose of t; h H survey if to detect anomalous conditions

which may reflect base or precious metal deposits in ths granitoid

JckE of tne property.

, Lf;C'-'iTK.irj aM-) ACCifciSLi

Die property consists of 60 contitjuous unpatonted claims

numbered LM'J39a tn L'*1 c)ii5?; inclusive and L^?101fJ to L^21D1U

inclusive.

About *i.r! irij IPS wuutheast of Timmins, Ontario, near the

sinHll community tif flteittichGuan, the claim group is situated in the

centre of Cairo Tuwnahip.

An all-wt?Hthcr grHvel rne-id extends northerly through the

claim group, frnni higli'Tiy 66, thereby providing excellent access.

Apparently rio significant uxploration work has been under

taken on t h t-: area oP the ulnim urou;j.

TfJf'G[iR'\f H Y

tif nf thw ganernlly uell drained terrain does not

exceed 100 feet.. Distribution uf I'ock expo;u.trs compared to the

genarfr.l HTBB i H yHnernlly y o od avBraylng about 15 per cent.

Tne major portion of thy property is ary and covered by

light brown tu rv.i.idiBh sand and sandy limm. 'ITBOU of gravel de

posits oro cordon. L.uw lying minor areas of thtjoe glacial deposits

art", covered by wet organically derive? ri soils common! y known as

muskiig. U B UK j l y these a r e a M form nartn trenriiny lensairial shaped

d B p o s i t a h e t u e e n ri d g p, 3 .

Similarly, thn crooks, ponds 'i.un1 .laKni;; are oriented in

a north direction ^ith rir^iririgE tu thy south.

Jack pine, birch, em ri poplar, in that ordnr of abunriancBt

are pressnt OD che high grDimd. l':ostlv black spruce are confined

to the l oiu suami.;y

Thu QGolugy nf the arss is ahoun on Map 2*110, Powell and

Cairo TownshipH, by t.hfj Inturiri Dtrp^rtnir-nt of Natural RssourcBB.

7hH distrihut'lor. nf lattil nn|.per Bnd total molybdenum in felsic

plutonic rocks of the; area is shown on maps I 'J 7'12 and P733 respec

tively, by thn i'lntEiriu ynvt-.-rnment. Thf Ha JBatic-'Jiley property is

located tin lha Einuthwe^t portion of the Cairn :;touk which includes

thn felsic plut-.niic ronks of thi? arHa. finally, the Cairo Stock is

the subject nf a study by u). J. Wolf Ei of thy Ontario (jeological

Branch in Open Fi IP Report 5G91. In this report, tha results of

sampling i^vnra.l felsic intrusive^ rtiloted and unrelated to gold

campa ig df.;{it:ribftd enrl inturprated.

Tli e uren of the claim group is Blmoat totally underlain

by alkalic i ntrij^ive ruake, pfirt of the Cairn "itock, reprsnenteri

by H rnnynetic Inu. Alnnrj the west boundai'y of the property, over

B uiiiJth nf nhoul ^DiK.) f'e^t , coary!' tjrain'.'d svK'ii ie porphyry is

' oxpuKKfj. T h t-: rcri:1 .: rifitfr uf thrj property * '- u niJrrl :- ;)in by mudium

rjraintuj ^ycn.rtr?, ui ",h the exception rf the LTD t) tiiang the south

brunc'ary tnhinh ir. un r :;:r] fin by yrunozir coarr.? grf^ined nudiments

strikinq northern; i. !.iurth trtinrlino G' i B l.) ^ r: f clykt'9 intrude the

Cairo Stock.

ld-si iv/i^r jRpor-its have hean tninad in Powell Township

i.iif:-,t nf" Cfsiro Towntuiip. iJidftyprt-'Pc) occurrnncBS of

chalcopyrite, pyT'ite, gnlena, specular hematite, purple flunrite,

barite, iricjlybrlenltt: and touring]. inc hove bt-ien ohsnrvMri in thn Cairo

Stock. lhe c u;' mineral:"; are cciritmcn afssoRintt-H af gold in quartz,

ant] quart? nBrbon-jtB vuiria that 'jncupy fracturRf.; in' ond nunr the

syenite,

Arc-is'.; of thr-i Cairo Hj.kolir. intrusive corusidsrtjd tn bs

anomalous in noppFr ;:,nd mo] yhriantim, as-; Bhoun en trit^psi; P732 and ^733,

BTP. n ynorallv cnnf'n^rJ to thr rnarrjiny nf thr intruaivr. A relative

riBpi^tion uf .silir.ci Rxista aluno tht? m^ j." g in r, of ttie intrusive RS

co T "p::'rs! tu thf cBntrt:. ThR tiinriif icancp of copper end molybdenum

fri un i:ic?ps ('7"5k' and P733, ''.'ithin the claim group shall

fiiiBt t.fu- heodinri -''laurvny result.'; and Interpretationl

SLMULY HtSULTLi r.WJ ,

M btuciy of the mettil valuta indinateH that there are at

least three di' fan-in t pupj] r:tir;.nt of VEJlues buaf.'d on difffjring

sai j types. It, 5 1., riutsd, f' c, r example, thor, v'Jluea from muskeg

sainplBLj ,jre ,;,uoh fiigher ;,i'i,in t h us b samples from saruJs and gravela.

This fsc'turR rfitmlto frr.rn the fact that trm organic rnattHr of

swamps tend;:, to precipitate many of thp oro motalrj out, of ground

water solutions. Rather tfrbitrr-jrily, hut nevertheless baaed on

trie geology, '-soil type.1 :.;, and arithmetic averages of values together

with the ro.:;ult'.' of the rock R a m f.. 3 iny shoun on plans P732 and P733,

thi-- threshold v-'?luti ror each of tht; mstuls analyzed, namnly copper,

lead arui zinc;, was at?t -:t ^L3 part-;; par million, Although this

thrRsholr! r.^y tie: valid for tieteni'ininij wnncialous conditions in areas

of BBrir! nn;;l ^ravol, it is novioufi thnt B m uch highnr threshold is

rRquirsu1 for th:;-:-,t-- r.umplaB fro'n musiktiq. Over half the samples from

muskeg hfivu valun.'i ni-Rnt^.r than W p prn.

ilt3c:cjur,t of thfj Irarge riunib^r r-f sumplKa, huwevar, ein

adcquatB stHtisticrJ. tru^tnent of the data uuu.Td involve more

expcnditnrB then thin rRquij'r;ri for oxHmin^tion of rock exposure

adjacnnt to thrive obviously anomalous values.

fioil r.anflK'5 front the north hnj'f of the property uiera

analyzed for cooper, l r-: B d and zirr:. ;iinc:,n it, i j d B nubBBquently

dytRrmi ned f hat high .Tine value;-: alnur:t invarifjiily Rorreapondud to

hifjh co|ipor values;, tho asmpiHR frofli the south half of the; property

UJRTC anwly?f r.1 fur cor/p^r Eind IGEUJ only,

The copper, Itdiid und zinc: v^'luos for thn north half of

the property art! plotted snd cor'tuurrid on t wu plans at a ocale of

one inch to four hundred foot. [Jrie fjlon sufficfjss for displaying

results an the south h^lf of the property.

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Anomaly F - A number of isolated anomalous values form this

anomalous zone butwRcn Line 2 ^ Worth at the base line and Line i*

South, station 1b L'&at. High copper and zinc values were obtained

from muskeg samples. The largest anomaly of the zone is confined

to a swamp. Here t h R metal valuer; show relative impoverishment at

the centre of the swamp which ie characteristic of the precipita-

tion effect organic matter has on ground-water. , ,

.id ~ This anomaly is situfjted along luhiskeyjcick Creek on

the we?t side of the property. High copoer values form a linear

feature partially in lou ground paralleled hy high lead values along

tha Orec-jk. This rm cima l y correr-ponrir, to a rock capper anomaly on

Map P732.

fiOSSSilLJi *" ^^Qh cnpper-lead vnlut^s crc:3siru;i Linea Q, 1?, and 16

5out f 'i junt k'Rst of tht-j ro.':d ft;rm e;nomaly H. The values are situated

in and adjacent to musk no s^nmp. ( :

L - ^ yroup of anomalies eas.;t of the lake, between Linea

20 and **8 doutfi, farm this anomalous zone. The highs along the

lake share one creak BIF, confined to low ground, in pert, muskeg.

At trie intersection of Line 3 fi South uii.th the base line, the high

values, particuliarly lead, arc in sandy iufsm. This anomaly corres

ponds to the location of a lead-copper occurrence and rock molybdenum

anomaly on Map H733.

AnomglvTi J - Korniin^ a linear narst of t(-iB base line, between Lines

20 and 3 Ei I'inuth, thl;; copper anomaly is largely situated in dry

sandy noil '. /' . . V-

Anpmaly^H - 'jsvcral isolated lead anomalies in the vicinity of

Cameron Loku form this anomalous* zonfi. The values were obtained -

from dry sandy soils adjacent to rock exposure. , '

^nSIUSl^Li; ~ This "namely crosses linea 2B, 32 and 36 South near

the west boundary, f-icst uf the high copper values are from muskeg.

Anomaly M - A rwther small feature, this copper-lead high croBBe

lines 56, 60 and 6** Sou to near the east boundary. The high values

ara confined to shallow, dry, sandy loam. . :,

sy of their close relationship to copper or molyb

denum highs, from rock samples BB shown on plans F732 end P733,

anomaliea B, C, Q and I ore cnnairifred the moat impnrtant aa poe-

aible indicBtors if bass motc'l aulphidBB. The leat! anomalous

zone K rn FI y inriicfite the pruaenne of tjold-silvsr minereilization.

An nxiiminstian of the rock exposuro in the vicinity of

these anomalies and thR nthara herein df?9cribr;d might well bs,

aufficinnt in most instancRB to determine whether 'or not base or

precious mRtfil mineralization is related to the sail anomaliee,

Those anomalies, houiRver, having a lunnuidal shape, oriented

northuards, may reflect mineralized faults in topographic lows \ :'

Thest! type of onomnlien, in pBrticular, inclurJa t, G, H and J, and'

may require Berth trenching.

a

A [;rrjgrariiTiF; of detailed rnnk examination is recommended

at the locutions of the individual anomalies u)ith anomalies B,- C,

G and l meriting special attention. A minimum amount of S30QQ ;

shnuid he allac^tfid for this programme including same earth : :

trenching at Iocs t i on;.- to be* determined during the investigation.

Any detailed assaying of rock SHHin3.ini:; that fiay be TGquired would' " : (' " "

an additional Bxperiditurs.

ly submitted, -' -,'

\ SJ, SHIELD GtUPHYSICS LIMITED,:Vi ',-.\ l :""\ ' . - '

4 c-*- -j * f-\ y y f i V "* "

V /~*";i"**i4t*B ,t, "O J ''

TimmiriB, Untariin, \'^\. ^^ /"- *-'* Bradshew, F. Eng,,\?h^""^ 0Jr

cr 1 C, 197!:.. X^eopo^^ ConnuHing Geologist.

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42A02SEfc279 63.3383 CAIRO 900

CC~ - ^fc

l L ) L

'4I89\48 418949

T9X448 4 13 4491 419450

4210.141 419440 j 41 9439ez 676419435

419430 '419431 .419432

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1447 4 19408 4 l9f409 1419410419411

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401425 380689,4I93\54 4I ?.S4

380690|4I 9356 L"

"-40I33I 380693; 580692

Tt. O O l* t*1 SI ' M ' f ~~ - ~

LEGEND

Meosurement station along picket line

Parts per million of copper and lead in soil

Copper Isograd in ppm

Lead anomaly I.e. over 40 ppm

Low wet ground generally covered by muskeg

Muskeg sample

Area of rock exposure

Claim post

B.L. O

(South S heet)

GEOCHEMICAL SURVEYON THE PROPERTY OF

MAJESTIC WILEY CONTRACTORS LTD.CAIRO TOWNSHIP ONTARIO

BYSHIELD GEOPHYSICS LIMITED

CAIRO TOWNSHIPt;-

SCALE400 800J ^ ^

IZOO

-nth

FEET

NOVEMBER

SOUTH SHEET1975

42A82SE0279 63.3382 CAIRO200

^ 3 C/

LEGEND

Measurement station along picket line

Parts per million of copper, zinc and leod in soil

Copper isograd In p p m

Lead anomaly i.e. over 40 ppm

Low wet ground generally covered by muskeg

Muskeg sample

Area of rock exposure

Claim post

(North Sheet)

r' 1"). - - _- '^ T -

~ - i t: a

Whiskeyjack Lake

CAIRO TOWNSHIP

KEY MAP one inch to one half m ile

Beaver Pond

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s ir s a

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B.L.O

42A02SE0279 63.3382 CAIRO 210

GEOCHEMICAL SURVEYON THE PROPERTY OF

MAJESTIC WILEY CONTRACTORS LTD.

H

CAIRO TOWNSHIP ONTARIO

BYSHIELD GEOPHYSICS LIMITED

SCALE400 800

FEET

1200—j

OCTOBER 1975

NORTH SHEET

LEGEND

Measurement station along picket line

Parts per million of lead and zinc in soil

Zinc isograd in ppm

Lead isograd in pprn

J Low wet ground generally covered by muskeg

Muskeg sample

Area of rock exposure

Claim post

o-

/L4Z.IOI1 4194.4.1

(North Sheet)4ZI014. A I9440

Wh/s/reytoc* Lo*e

CAIRO TOWNSHIP

KEY MAP one inch to one ha f mile

Beaver Pond

~ \ *r rJ — - r- s \ "* "'r-

B.L.O

42A02SE0279 63.3382 CAIRO 220

GEOCHEMICAL SURVEYON THE PROPERTY OF

MAJESTIC WILEY CONTRACTORS LTD.CAIRO TOWNSHIP ONTARIO

BYSHIELD GEOPHYSICS LIMITED

SCALE4OO 8OO 1200

FEETOCTOBER 1975

NORTH SHEET