PROGRESS RPT ON THE CATHARINE-PACAUD TWP PROP · in the winter with the Winki Drill. The geophysical work did reveal some conductors on both grids, which although they do not appear

31M13NW8897 63.3246 PACAUD 010

PROGRESS REPORT

ON

THE CATHARINE-PACAUD TOWNSHIPS PROPERTY

OF

WARREN EXPLORATIONS LIMITED

BOSTON CREEK AREA

DISTRICT OF TEMISKAMING

ONTARIO1C L-

j

By: J. A. Pollock, P.Eng.Dated at Haileybury, Ontario February 12, 1975.

SUMMARY OF WORK PROGRAM

CATHARINE-PACAUD TOWNSHIPS PROPERTYof

WARREN EXPLORATIONS LIMITEDBOSTON CREEK AREA

DISTRICT OF TEMISKAMING ONTARIO

(1) The property consists of two groups of patented and unpatented

claims totalling 1,272 acres.

(2) From September, 1974 until January, 1975 linecutting, geophysical

work, prospecting, trenching and diamond drilling were carried out.

(3) A VLF electromagnetic survey revealed four areas of minor

conductivity which should be confirmed with another type of

instrument.

(4) Trenching revealed scattered copper mineralization over a length

of 400 feet.\

(5) Drilling two short holes encountered only minor copper mineralization.

(6) The exploration program was aborted due to the arrival of winter.

(7) A further exploration program is recommended to further test

the main group of claims worked on, as well as to explore the

group of claims to the south to verify airborne anomalies.

(8) The recommended program should be considered in two phases:

Phase I - Geophysical work and mapping. Cost ... $11,500.00

Phase II - Depending on the results of Phase I,and supervision.

Cost ... $28.000.00

Total ... S39 1 500.00 '* l

POLLOCKr id "" " "

February 12, 1975. ' ~n A. Pollock, P.Eng.

- 2 -

INTRODUCTION;

In the early 1920's the Boston Creek Area was actively prospected

for gold and a limited production was obtained from two properties*

In 1926 copper was discovered along a zone extending south

easterly for 2-1/2 miles from the village of Boston Creek. Between

1927 and 1930 a limited production was obtained by underground development

of three properties.

Similar rocks extend in a semicircular belt along the periphery

of the granite through Catharine Township and contain a number of known

gold and copper showings.

During 1974 Jonpol Explorations Limited purchased two contiguous

patented lots for $6,000.00 cash and a 3 7, royalty based on net smelter

returns to a maximum of one million dollars, thereafter the royalty will

be reduced to 2% of net smelter returns t Jonpol Explorations Limited

vended the property to Warren Explorations Limited for a stock consideration.

In October 1974 the adjoining area was prospected as well as the

original Warren patented claims. The examination of the copper showing

reported on in 1929 by Victor James of Wright, Boydell James and Associates

led to the acquisition by optioning and staking all available adjoining

favourable ground.

A limited geophysical program was undertaken as well as" prospecting,

drilling and trenching. The arrival of winter brought an end to the operation

on January l, 1975. Work was confined to 952 contiguous acres around the

Old Mindoka Mines property.

- 3 -

The following reports, maps and drill logs have been referred

to and incorporated in this report:

Cunningham, L.J. - Mining Engineer - Report on Catharine-Pacaud

Townships Property of Warren Explorations Limited and

amendment July 3, 1974;

Cunningham, L.J. - Report on a VLF-EM survey on a limited grid in

Lot 11, Con.IV., Catharine Township, District of Temiskaming

for Warren Explorations Limited, February 10, 1975;

Cunningham, L.J. - Report ^n a VLF-EM survey on a limited grid over

parts of 2 patented lots, Catharine-Pacaud Townships, District

of Temiskaming for Warren Explorations Limited, February 10, 1975;

Pollock, J.A. - Professional Engineer - Letter to Shareholders of

Warren Explorations Limited, January 18, 1975;

Pollock, J.A. - Diamond Drill Records of Holes W-l and W-2 drilled

December, 1974;

James, Victor A. - Mining Engineer - Report on Mindoka Mines Limited,

July, 1929;

Grant J. A. - Geologist - Geological Map 2043 to accompany O.D.M.

Geological Report No.18, July, 1963.

LOCATION AND ACCESSIBILITY;

The property lies approximately 14 miles southeast of the

town of Kirkland Lake. The claims are 8 miles east of Highway 112.

- 4 -

Highway 564, an all-weather gravel road, extends easterly from Highway

112 through the village of Boston Creek and then turns southerly to

cross the centre of the property along the Pacaud-Catharine Township

line.

A high tension power line of the Ontario Hydro Electric

Commission and the Ontario Northman d Railway are located about 3/4

of a mile southwest of the property. The railroad is accessible by

an all-weather gravel road, the distance from the property being

three miles.

PROPERTY DESCRIPTION AND LOCATION;

The present Warren Explorations Limited holdings contain 952

contiguous acres and a separate group of claims containing 320 acres.

The description and status of their holdings may be described as follows:

Patented Lots held 10(^ by Warren Explorations Limited

Pacaud Township - S-l/2 lot l Con IV

Catharine Township - S-l/2 Lot 12 Con IV

Patented Lot owned by Gawley Estate Optioned to Warren Explorations Limited

Catharine Township - S-l/2 Lot II Con IV

Unpatented Claims held by Mr. Dave Bell and optioned to Warren Explorations Limited

L-380998 - SE 1/4, N 1/2 Lot II Con IV Catharine Township

L^-380999 - SW 1/4, N 1/2 Lot II Con IV Catharine Township

L-381000 - NW 1/4, N 1/2 Lot II Con IV Catharine Township

L-381001 - NE 1/4, N 1/2 Lot II Con IV Catharine Township

- 5 -

Unpatented Claims held by Warren Explorations Limited

L-406691, 92, 93, 94 being the N 1/2 Lot H Con III, Catharine Township.

L-406695 being the NW 1/4, S 1/2 Lot 10 Con IV, Catharine Township.

L-406696 being the SW 1/4, S 1/2 Lot 10 Con IV, Catharine Township.

L-406697 being the NW 1/4, N 1/2 Lot 10 Con III, Catharine Township.

L-400698 being the SW 1/4, N 1/2 Lot 10 Con III. Catharine Township.

TOTAL: 952 Acres

The company also holds a group of 8 contiguous mining claims

in the southwest corner of Catharine Township which may be described

as follows:

Unpatented claims held by John Duncan and optioned to Warren Explorations Limited

L-401751 - NE 1/4, N 1/2 Lot 11 Con 2 Catharine Township

. L-401752 - SE 1/4, N 1/2 Lot 11 Con 2 Catharine Township.

Unpatented claims owned by the Company

L-418698 - NW 1/4, N 1/2 Lot 11 Con 2 Catharine Township

L-418699 - SW 1/4, N 1/2 Lot 11 Con 2 Catharine Township

L-418700 - NW 1/4, S 1/2 Lot 11 Con 2 Catharine Township

L-418701 - SW 1/4, S 1/2 Lot 11 Con 2 Catharine Township

L-418702 - NE 1/4, S 1/2 Lot 11 Con 2 Catharine Township

L-418703 - SE 1/4, S 1/2 Lot 11 Con 2 Catharine Township

TOTAL: 320 acres

There was no work done on the above 320 acres during the 1974

exploration season.

- 6 -

GEOLOGY;

(1) General Geology.

(2) Geology of Property.

(3) Economic Geology of the area.

(4) Economic Geology of the property.

For the above, please refer to the incorporated reported by L. J. Cunningham,

June 25, 1974.

1974 EXPLORATION PROGRAM;

During the period between September, 1974 and January, 1975

an exploration program following the recommendations made by L. J.

Cunningham was conducted.

Picket lines were cut at 200-foot intervale over the known vein

areas and .V.L.F. surveys completed over the two grids. (Ref: enclosed

surveys by L. J. Cunningham.)

Several trenches were blasted into, on the Gawley option, and

the area around these was prospected. The mineralization in the trenches

did not respond to the V.L.F. instrument. The late season did not allow

us to map in detail these trenches but we expect to do this next spring.

An excellent description of the trenched area is given by Victor James,

Mining Engineer, in his Report on the Property of The Mindoka Mines

Limited, which is enclosed herewith.

Two short diamond drill holes were put down under what appeared

to be the best mineralization in the trenches. It was necessary to stop

drilling with inconclusive results due to the light drill equipment and

the cold weather. The two short holes revealed only scattered blebs of

chalcopyrite. (Ref: enclosed drill records logged by John A. Pollock, P.Eng.)

*- 7 -

A study was made of the results of the Questor Mark M.K.V.

input survey which was flown over Catharine Township in 1970. Four

conductors were indicated by this survey to the south of the Warren

property and eight mining claims were acquired to cover the interesting

areas. No conductors showed up on the Warren property itself.

The results of this survey are available at the Mining

Recording Office, Kirkland Lake, Ontario.

CONCLUSIONS AND RECOMMENDATIONS:

The fall program in 1974 of linecutting, geophysical work and

very limited trenching and drilling did not reveal any economic deposits

of copper ore. The work was confined to known occurrences and did not

cover a large part of the property.

The trenching did reveal scattered copper mineralization over

a length of four hundred feet north of the Gawley shaft.

The diamond drilling showed only scattered chalcopyrite under

the best mineralization but the possible plunge of the pipe could easily

have been missed. Two short holes are not a very good test of mineralization

which stretches for fbur hundred feet, but it was impractical to continue

in the winter with the Winki Drill.

The geophysical work did reveal some conductors on both grids,

which although they do not appear strong should probably be tested with

more sophisticated instruments.

The group of 8 mining claims to the south which were staked to cover

weak airborne anomalies was not worked on at all due to the lack of time and

men on the project.

-f 8 -

It is recommended that:

Phase I; (1) Detailed magnetometer and electromagnetic surveys

be conducted over the present grids to verify

anomalies outlined by the V.L.F. survey.

Cost ... $ 6,000.00

(2) Detailed mapping be done on the grid areas

to tie in mineralization with geology.

Cost ... $ 1,500.00

(3) Anomalies on the southern group of claims

be verified by V.L.F. and further checked

with a more sophisticated instrument if

necessary. Cost ... $ 4,000.00

Phase II: Diamond drilling if warranted be completed to:

(1) finish testing the known mineralization

(2) test anomalous zones.

Cost 2,000' @ $12.00/ft. Cost ^24,000,00

Supervision 4.000.00

Total:

CERTIFICATE

I, John A. Pollock of 651 Latchford Street, Haileybury,

Ontario, do hereby certify that:

1.

2.

3.

4.

5.

6.

7.

I am a practicing Professional Engineer with offices at Suite 600, 85 Richmond Street West, Toronto, and Haileybury, Ontario.

l am a registered Professional Engineer of the Province of Ontario.

I have been working in the mining exploration business intermittently for 25 years and hold a 1950 Ontario Prospector's Licence.

I am an employee of Pioneer Consultants Limited and have been working as an engineer for them for over five years.

This report was compiled from information received from various consultants as well as first-hand knowledge gained by supervising the exploration program in 1974.

I was on this property many times between September, 1974 and January, 1975.

I am the President and major shareholder of Warren Explorations Limited. The control of Warren Explorations Limited is held by Jonpol Explorations Limited which is a private company controlled by myself.

Haileybury, Ontario,

February 12, 1975.

John A. Pollock, P.Eng.

31M13NW0097 63.3246 PACAUD

A VJ-iJ. —^fa^jt iM/wAt VAJ.L ON A LIMITED GRID

OVER PARTS OF 2 PATENTED LOTS CATHERINE-PACAUD TOWNSHIPS

BOSTON CREEK AREADISTRICT OF TEMISKAMING

ONTARIO

020

LOCATION 6 ACCESSIBILITY

The property consists of 2 contiguous patented lots, one in Pacaud

Township, the other in Catherine Township.

They are unnumbered but are described as follows?

Pacaud Township S^ Lot l Con. IV 160 acres

Catherine Township S^ Lot 12 Con. IV 152 acres

The property lies approximately 14 miles southeast of the Town of

Kirkland Lake. The claims are B miles east of Highway 112. Highway 564, an all-

weather gravel road, extends easterly from Highway 112 through the village of

Boston Creek and then turns southerly to cross the centre of the property along

the Pacaud-Catherine Townships line.

GEOLOGY OF THE PROPERTY

The eastern margin of the Round Lake pluton underlies parts of Lot 12

along the western edge of the property. The Keewatin rocks occur as a steep

anticlinal belt around the granite. Grant (O.D.M. G.R. 18) has subdivided these

rocks into three stratigraphic formations, from west to east and from oldest to

youngest as follows:

A. Interbedded tuff and tuffaceous sedimentary rocks; with minor iron formation

This division lies next to the Round Lake pluton and is traversed by numerous

small dikes and sills. The total thickness is unknown, but is about 1,300 feet here.

B. Dioritic, dacitic, and andesitic lavas. Pillowed lavas are common in this division, which has a thickness of about 10,000 feet.

C. Porphyritic and aphanitic, intermediate to acid volcanic rocks, largely

pyroclastic, and agglomerate. The thickness of this division is also about

10,000 feet.

ECONOMIC GEOLOGY

Two miles to the northwest of the Warren ground copper shoots have

been mined as replacement bodies in iron formation at the contact with acid tuff,

The mineralized zones are pipe-like and of high grade (5 to 10#

copper per ton) with maximum dimensions of 50 feet in length by 5 feet in width.

Warren, Boston Creek - 2 ~Feb. 1975

tThey appear to be localized at cross faults which cut the iron formation.

The ore consists of chalcopyrite with varying amounts of bornite,

chalcocite, pyrite and pyrrhotite. Mineralization grades rapidly from massive

chalcopyrite to barren pyrite and pyrrhotite.

Within 200 feet of the Pacaud-Catherine Township line in the north

west quarter of Lot 12, Con. IV Catherine Township, the caved collar of a small

shaft can be seen with a small rock dump. Caved and flooded trenches indicate the

presence of two veins which are described by Victor A. James, Mining Engineer, in a report dated 12th July, 1929 as follows:

"The westerly vein system occurs practically on the Pacaud-Catherine

Township line, very close to the granite contact. The contact itself lies in low

ground, but has been established by diamond drilling. Granitic dykes (or small

sills) also occur along the bedding planes of the tuffs near the veins.

The veins consist of stringers of fairly massive chalcopyrite,

together with about two feet of banded pyrite and chalcopyrite mineralization in

silicified tuffs. The veins follow the bedding of the tuffs and dip about 82

degrees east. Two of the main stringers are 45 feet apart. A vertical 2-compart-

ment shaft 100 feet deep was sunk on the easterly one, and 55 feet of crosscutting was done at the 100-ft. level."

FIELD PROCEDURE

A grid totalling 2 miles (8 lines 9 1,300 feet each) was centered over

the shaft which is located on line 0 + 00 approximately 250' west of the township

line in Pacaud Township. Readings were taken every 100 feet along the lines which

run approximately east-west. 110 readings were taken using the transmitter

station at Cutler, Maine.

An appendix is attached describing the VLF-JEM procedure.

INTERPRETATION OF RESULTS

The roads separate the areas of outcrop from the overburden-covered

areas. East of the main north-south road and north of the east-west road which

crosses L 10 4- 00 S, the ground is high with much outcrop. In this area is

located the shaft and a number of pits; however, no conductors were encountered.

The balance of the property is covered by clay overburden cut by deep,

steep sided ravines. All of the conductors were located in a north-south

direction lying 100 to 300 feet west of and roughly parallel to the main road.

Overburden in this area is estimated at a minimum of 25 feet. The conductors

appear conformable with the general geology. It has been the writer's

Warren, Boston Creek- 3 -

Feb. 197i

experience that topographical conditions as exist here commonly produce a conductc

at or near the interface between the clay overburden and the rock outcrop. This

is not the case here - the conductors lie a minimum of 300 feet west of the

overburden-outcrop interface.

Because the conductive zone parallels the known mineralization it is

recommended that it be tested by more sophisticated geophysical techniques.

Dated atKirkland Lake, Ontario10th February, 1975

L. J." Cunningham, B.Sc., P. Eng., Mining Engineer

' * , * ' 1 ; * * *

*

f" T v- i ,r,l/ittl L-..'.53^^.:.'..V'^- 1 "V^ f •Ci^v 't v'^^•VUoslon.~ii...-k:-^™: - L.

497322

*-

^

'M 'x

v^ *

V

S\

)

fi

S,

3 , y .

*)••~E)V

1797*5 't :\t.?

r lo V.. t

207107

(p\•\\^\-

6^V.( " L:;" ,. ";"\ ".

— **^- - i,. '\ (FV1

\ *\

--.J... -X- - .X Xor-ip) -Vi-'

ff5v^)

S© C©

— -^^^-7-\-B V

, 1 ..L

\©

B .

i i'vjo, ^ r.'v ji**

^ Ju1 104 3 &I

JI098S 'r ~' jt'

"\ ! 5I6DP4it!':^

^K

Y

^'•i! t ^A \u ' - *-'ri l - ' t'j'io

*i." "©j r "or,op v r ' *S^23?

-^.--1. .--*

. (p.' V,f \

** '^- V \

,

©'S.-— ~- **---^ \jf^^^ -*^

^v

S'Julh V^- Minjoko ^,

@ \

\^/rl^^^'

© .

--7 (p)h-0^i \r^

i \

f'") ! C- ,i/.if".jr i -r-t '

j•i.t

5IB905I 5IE3COL"~" |Ll^IC'0^'

CON. V— . . ^

vx^^~"^\

t.CGN.IV^

S

A,,..,,, ,,^r•V ^V

x^CON. Ill -v— v; — T~ "—-^'^

X ^A X ^C

^ - ' '

©

COW. IIl \^^^

^x i \r\l *?-^K 'v 0 i

^ 0 )7'.-.! 1.' (/y3 ri

o x (fI7HJO IT937

x •v

" (p)s. ^y

~~\

\ ^x)

(p) lyi oi t -(,' 'y

.r

\' '

L OD'.L Oj)1 '

1r 1 r ,

*1 *M p *****i *V^ '^

..Q L. ©i./*" 1'-o .'-(P)

^At*™,,,-™.^.\j '

JV-Sy — - - - -

Xt

SW••,

V-

(D ',V , 'L-'

.1 -VjnVpTi1[Tti.,ijI|isiiiZ/60 "'I J;*tcn?.*io rr^!- k ij.

' ' , '- *J

"•-**^-

A, '"•"•/p""

"

' 'O

•0

____ _ —^ _ __ _ L ^— .

r

r,-'

1

V t

2*B579 ?1207S© -r-nr--~~i :

.

ntumtwrntc—i A'crag f.

© i......^.^j ^- ^v— - A --;

A © ^\^ .V^'

/(B^ r\ f

*

,x^l•©

' S 1 ',4 s

)'

©) .

^v^^v ' --. ' '\ ' ;

m^rS

5^060 i 3T5 1

^^\.j

'. l'"t *

L |

H

'.* *.

-. " M"

Ir '

f" IT '^^'. :-^

*"

** ;

'C')-MHO

"r ~~ If" - - - " '

-- 1 —

t

1 1 '

|r-p-

Ji^ITjJ'i'^L' ..HL.... ' l.

*iW. ^2^2L. l

?425M ^<?S7^

, -'- '

-4 i— ,M "^•0 7 '. **

lv iiC,7)'-V-

i

•-li

-*.r ~ -

l:^ :-

L. l. i ,jv

242577 212576'-TL.""~~"T.~~"""

lr2425ei 1 i^'t^n, | L ,t?251^----

124251T | 2425F6r~y-u— |i:

2125'JJ l 2*2592

'i ' ;

' ^ '

-r

,j

^

U.'';J,J...J1 '

- ——— ~

*

' ! ^ '.VAPJ^EN EXPLORATIONS LD1ITED .^ . PACAUD-CATliKPJ'NK TWPS.

i

lj. "~ ~ - ' 2bale 1" - 1/2 mile .^ ! . 2ndiIUly, 1974 L.J.Cunninehoia,V""" ' ' B.Sc., P.Eng. - * ^3) i

-- ti : i. 5ii 1 1 . . i '

^

i

H O X

hadars •equij-iwnt oiraply utiilxoo a radio r^coiwr cowtrin^ the band of V 'LS* tivnnriittor aUitiona (scattered ov^r thia continent and

parts of tho world. 'ttwaa tr-ittccdtter tesoa ara aafx/cially construct ed tawora which tr.ink*it on the VLF froqtnmcy (vory low frequency) tvxprfcosly Tor cojaunicut.'.on with tiuLr^u-Anuu x/fiich they do effective!,/ through depths of salt water. Thsroi'om It ia underfit ndable that penetration into i\*ck lo substantial bJiould the** be rio cc-fKixicti^o ovorlaii-dlon acting ao an inhibitor.

st&tiona transmit in t!io 17 Tea. to 26 f'cu. run- re. A station Is choaciii DO t?u;t Uia elttctroria, .^ictic lines of i'orctt of tl;o horiac*iuj,lly cc-nctsitric i'ioid are i^rjxmilicular to Uio istriko of the or corv.Juotrore which tu-o boii^ oou^ht in the rc&ion of JUttcr^at. Iho VU' jj^itiona available jikiictr it u slwjjlo natUu" to aoloct U:o oppropri;.ito

fitud ill/'oetion rti^iiirud which vf;ia the Cutler, f*kino sUition ij.i tho ce&e. 'ilso troncsuittfrr stiitiois way olwwt bc conslcUirod as loeateci r.t i tliorciors; the primry fluid io uiiforo ft.nd parallel iri a givers area.

Coupling due to a at conclary induct flold is raeaour^d by a tiltis accoui.vLi^hoci by tvirning the rwcoiver around a vertical axifj

to a position of Kiniriu;^ oi;?tial ond then tiltiiif, around a hori;;wstal axis to a pooitifin of no ui^i-al or "null". Tula wvlo is wtsiimir^d in tio&roea txtjtil UK*

oi dip ia luxttd. Thw receiver la trarked JK) thut wtien t,llt*Mt fmfistn^v-Ttt rsoir.t tcwani tho axis oi' the conductor, /.t) thtj

conductive axis io Hci\)cDod over" the arrow r^iiittt v^rticalXv liown wid tho dip iiriglo is ccro. Vho Uc,-jrye of tilt or amplitude io gonoi'.-iily a r -^svrfc of tho intensity of iho conductor. The './idtt; bot^.1' ori tho jxsftka of the uaplitucis ia generally mi isulle.;tlori of tho depth of tho conductor. The mrrowt'r upre/td of

pucUc in'iicatin/} a conductor noaror curface.

JUidom InoVrMKient raist bo used \*ith a *jrofit doal of (ll9cr*;tion and the froo,uc-*icirso ua*xl eiftjdlar3.y ax.teniiaito Uu'ifd itiotailic conductora

otrwig surficial ionic couuuotore. 'iije roaaltant conduetivo aonoa raay to aulphidoi}f faults, v?et alioara or surficial conductive clay.

This is a rugged, simple to operate, ONE MAN EM unit. It can be used without line cutting and is thus ideally suited for ground location of airborne conductors and the checking out of mineral showings. This instrument utilizes higher than normal EM frequencies and is capable of detecting disseminated sulphide deposits and small sulphide bodies,, It accurately isolates banded conductors and operates through areas of high hydro noise. The method is capable of deep penetration but due to the high frequency used its penetration is limited in areas of clay and conductive overburden

The dip angle measurement detects a conductor from a considerable distance and is used primarily for locating conductors. The field strength measurement is used to define the shape and attitude of the conductor. *

31M13NW0097 63.3846 PACAUD 030

t

i

t

REPORTON

A VLP-EM SURVEYON A LIMITED (HODIN LOT II CON. XVCATHERINE TOWNSHIP

DISTRICT O? lEMISKAMINQONTARIO

LOCATION t ACCESSIBILITY

The area lies in the KB 1/4 of the 8 1/2 of Lot H Con. IV, Catherine Township.

The property lies approximately 14 miles southeast of the fown of Kirkland Lake and 8 miles east of Highway 112* Highway 564, an all-weathor gravel) road, extends easterly fron Highway 112 through the village of Boston Creek and then turns southerly to parallel ths Buoaud-Catherino Townships line* Near the centre of the S 1/2 of Lot 12 Con* XV a tractor road extends northeasterly to the NE 1/4 S I/2 Lot 11 Con. XV, a distance of approximately one Rile.

GENERAL GKOLOQY

Keewatin volcanic rooks underlie most of tho aroaj immediately to the west is the Round Lake granitic pluton, with its Margin convex to tho oast* In general conformity with this margin are i (a) banded tuff, (b) basic to inter mediate lavas and intrusions, (o) Intermediate to acid fragmental rooks, and (d) coarse-grained volcanic rooks.

The Keewatin rooks were intruded first by ultrabasic to intermediate dikes snd sills, and then by numerous, small acid to intermediate, and lampro- pyriokdikes - probably r associated with the emplacement of the Round lake pluton.

*"t " : ,;; , '

QEOLQQY OF THS GRID AREA

The band of basic to intermediate lavas with intrusive* is approximately two miles wide* The flows strike northerly. The grid is oontfced on a shaft which is located on a felsic tuff horitton intercalated within the volcanic flows.

PltOCBDURE

A grid totalling 14,000 feet was out over the shaft area. From a base line (approximately north-south), 14 lines, 1000 foot in length, were out at 200 foot centres. Using Cutler, Maine as a transmitter station, a survey was conducted over the grid. Approximately 140 readings were taken*

An appendix is attached describing the VLF-SH procedure.

l

t

Karren, Boston Creek

INTERPRETATION OF RESULTS

Wb. 1975

The terrain is one of considerable outerop separated by Mall areas of overburden. Two streams traverse the ground*

Two conductors are considered to be worthy of further investigation by nore sophisticated geophysical teohniques* They fret(1) The conductor which crosses 1*12861143 at approximately l -f 50 west of base line and(2) the conductor which crosses X* 14 S and L 16 3 approximately 100 feet oast of base line.

The remaining four conductors are strongly suspected of being due to conductive overburden.

Signed,

Dated atKirkland Lake, Ontario10th February, 1975

Engineer

- .

ro 3i

P.

i t?

9M

P

x

/**

^

w

l-J

0 -J *-

wr*

^

* *

.CO

e-

g 0 ^ c: S 5 C2

t^3

r'^ t-J

.

^M S i s t*i S 5 H t-

i

0

^3 5 f!

" s

0

P r B M) .X

kadota oquirwmt aiwply utilises a radio receiver covering the frequency band of VL;' ir nadtior stations eeiituirod ovtr this continent wnd other parts of tb*j world* 'iticso tr*mordtu?r buaoci arc oapociolly constructed towers which tr.yVa-.iit at the VIJ.' frocjwmcy (vary low frequency) exprfcosly ior (xx:*iuriicat.v.on ViJiti; ouUyjr.urieu wriich tJwy do effectively through depths ol

vator, 'flwrei'ore it ia underat nda:.lo th&t penetration into rock ioLe no conductive ovor burden acting ao taj inhibitor.

"ticac trrsnasittcr atitions trana-sit In tho 17 Kca. to 26 ?rca. run --e A station is cJtosRi! RO t!iat - .-!.a isiectra^. rnofcic linuo of fore** of tlie horiacii tally cwcoi-itrie i'ioid are ixurixmdioular to i ho etriko oT the Tcr^itic-n or cwi'.luotore wJiicJ*. ar*s "woitvj fcoufht -In tiie re^oti of interest, 'the numerous VU' atistiorjo available mko it ci siaplo natter to select U:o ftppi-oprifito priJ.!K',ry I'if.-idi d.L- ic:ction rt^iiir-wd wJi.icJi v^ao the Cutler, .-feiijici ettition in tho

case. 7h0 trcins&ittor atation r.say uljsoat bc c*^isi(J^rod as loeatcd at thwel'ore l he priraitry field io uniform fmd parallel in a given area.

Coupling due to a ot condary iridxiced flold is neaaurwd by a tilt Tills is accoi^xLish'Jt! by tiutiing the rwcoiv^i* around a vcu^tic-ii axis

to a r*o3iticn of ninii::ui': sij^rial ^md thun tiitliy, around tt horizontal a^cis to s position of no uiyyri-al or "null". Thio fiiv.*lo is r.easuryd in do,^rowo 'JJd tlie direction oi tlip io noted. Thw rcceivor ia catted so thut wtion tilt*M.t on arrow on LJ;o inotrj-^vr.t ix/ir.t towaixi Uio ajtia OA tho cc^idu^tor* , .o the conductive oxio io "crocood ovs^r" the torow iwitits vertically viwfln euid tho dip iini^Lo is ccro. Vho dc;;rue ol tilt or amplitude io gtsnoivuly a r .w*suj^ of tho intensity of tho ctjnductor. Tbo wi-ith betw- ori the pu^ks oi the amplitude ia gesaerfj.ly mi ln;ilc.vtiori of Urn depth of the conductor. The narrowor spre^id of tho ]xx*Jc Inviicfiitin/j a conductor nearer eurl'tice.

Iladcra instrument nust bo us^d vith ft ^jrcat deal of (d9cr*;tion and exjx^rienco; the fre*.:uenciGo uaod eimilarly attitfiuato Luri*id not&lllo conductoi*0 atid otrung ouj-ficiol ionic coiciuotore*. The resultant conductive ?x)ru*a raoy to graphite, oululiicioi?, Iiiults, v;et trtioara or surficial conductive clny*

This is a rugged, simple to operate, ONE MAN EM unit. It can be used without line cutting and is thus ideally suited for ground location of airborne conductors and the checking out of mineral showings. This instrument utilizes higher than normal KM frequencies and is capable of detecting disseminated sulphide deposits and small sulphide bodies,, It accurately isolates banded conductors and operates through areas of high hydro noise. The method is capable of deep penetration but due to the high frequency used its penetration is limited in areas of clay and conductive overburden,,

The dip angle measurement detects a conductor from a considerable distance and is used primarily for locating conductors. The field strength measurement is used to define the shape and attitude of the conductor,

WAKRfH emo* 040

FIELD OFFICE 8U1TE 4O ,P.O. BOX 38, HAILEYBURY, ONT. 36O BAY ST.. TORONTO. ONT.

PHONE 705-672-3311 PHONE 416-363-7381

WRIGHT, BOYDELL, JAMES & ASSOCIATES

REPORT

on property of

MINDOKA MINES LIMITED

Boston Creek Area,

Ontario.

SUMMARY;

Property of 640 acres, five miles by road south-east

of Boston Creek Station, three-quarters of a mile east of

Mindoka station on the T. S N. 0. Railway, to which road

is being completed by Ontario Government. Power line one-

half mile to west. Motor road crosses the property.

Two known vein systems, about three-quarters of a

mile apart, both striking west of north. The west vein

system is probably a southerly continuation of the Amity

break. The limited work done so far, including a shaft

100 feet deep, 55 feet of crosscutting, and 1100 feet of

diamond drilling discloses narrow widths of high grade

chalcopyrite and some disseminated low grade ore.

The east vein is newly discovered and appears to hold

such larger possibilities. It is in fact one of the best

surface copper showings in the whole district. The break

is strong and structurally well-defined. It has already

been traced for 1500 feet and it has every appearance of

continuing much further. The property covers the strike

for over one mile.

- 2 -

l! fl;

ll

channel eonploe token 10 and 14 faot bolov ourfaoo

in an Inollno ohnft guv a an average of 2*2;# copper over 4.5

.foot in width. Copper appearo coning in (nore strongly vi th

depth in thin shaft, aa tho surface eh owed no rely stringers

of copper oarbonatoa lying in tho broak. i

About 6DO foot north of this shaft, n discovery of

hi eh grade oro in thin voin was nade At tho tino of riuit,

undo r an apt urn o J. troo root* L c. re o e-nsulftr fragnonts ad

hering to tho troo root ohowod high crado o hale o pyrite oro

and on otripping, oro of the s aa e character was found in

pi GO o ovor ft width of fivo foot* — T*t6

this ohowing gavo 20*20^ copper over 6*0 foot and--'~

.. toaothor wi th trnooe of

gold* Stripping lo continuing on thie inportnnt discovery,

and chalcopyrite hao been found in tho vein for ndiotance- '-\- ' ' ." ' ' '."- '

of oeyorjil hundred foot* ?ho oro is of the replnoenont

typo* trith vory little Toin quarts*

Thio voln occurs as a troll-dofinod o true tar&l break in

Keewatin rocko, no ro or lose paralleling the contact of the

largo grnnito batholith to tho woot f a oot of conditione

which nay bo r^c/xrdod no vory favourable for otrongth end

continuity of ore in depth*

S'ho active dovolopcont of the o rv o t voin on thi o prop

erty, particvxlarly i ho area noar tho now discovery* is ro* oonnendol* : , ' :- .' : . - ; ;. :'. : .. -'. ; '- •"'-• i '" :-.' ;: '" ; . ; :','-.' : -

*#

P.J

*31!'

n:'

P HO ?V RT Y f

: ' ' ' ' ' - " , ' , ' r - -1 ' '

property conprleoa 640 aoroo in the surveyed totrn- ohips of Cftthorlne And Paoaud, Larder Lake Mining Pivloion,

Toniokanins District, Ontario* It includes tho whole of Lot

11 nnd tho south half of Lot 12, Cathorino toonshlp, and the

south half of Lot l , Pacaud township. -

Sono of thlo eroand is held, ae faro land e, carrying

both ninoral and earfftoe righto* Other portions are e take!

aa raining olalrne* Mo eoaroh of tho titloo waa nade*. ^ ' ' . - . . ' - ' 1

LOO A 'i

property lioa cloao in and lo onoily roaohod* Tho

orunpo nro oito&toi fivo nlloa oouth—eaat of Eooton Crook

station T)y road* night-of— tray la already oat for road to

Hind oka station on tho ?. ft W. O* Hailcay, a dietonco of

about l i: lailoo. Tho Ontario ,;ovornnont hne undertafcon to

conploto this road thio ounwor* tfho diroot dictanoo froa

tho proporty to tho railway le loss than ono-half nilo*

transnin.ionUino of tho Korthorn Ontario light

and Power Company pao808 a Bhort di O tanoo weot of tho; Prop.

orty.iuid i. vithlh onoailo of; alaoo t ony part of tho grptxp.

It io aloo po 03 lbl^ that* otoppod-dowi Toltano oould

obtained from .omo of tho noarby de Volo'p,ed :'; pro partio.."

A ' f^ ^

,p*',L 'it!-'.",-

'A sot of now camp building ha. bocn orectod/Uoo-

prioinc offloo, oookory nnd bunkhouno mifflolont for a

(Continued)

o row of 20 non. Several email crooks oro go tho claims and

domootio water la obtained frora veils* Tho country le

nootly burned over but thoro is sufficient standing dry

tinber for diamond drilling nnd domestic purposes* /Fuel

la not a problem horo on account of ready transportation*. ' , ' , .1 . ' : ' ' ' '" ' . ; : '~\ ."' , . " 'i :; ' L; ' ' , : ' "- ". .''"J • ••'. -'" ' i' ". ,. ' ' " ,

ns Y P ?.o P "R " '''''A nanber of othor coppor properties are boihn dovelopod

nearby. Chief amongst those aro tho OcoIan-TrethoBoy,

Patterson Copper andJAnity Copper, which lio to tho north of

the I'ihdofcft" fjroap in . tho order n&nod* ffhe voot veins on

the liindokn probably represent 'the southern extension o f

tho vein oy o 1 45i on tho above properties, on which pro perti ea' * '-' : ' "' " V ' - - S, ' ' . '.'' . .'.' ' , ' . ' ' r ' - , " " -' ' " ' . ' ,

ondorfrround work io at prooent procooding. A nxunbor of'.•••- ,'.':' - '' '-' '- ' ~ ' " ' ( ' ,V'y.;'".:':'- ; f y ' l'\,' V 'W:.V.' ' : ' :"' ' ' -" ; '"',

partly dovolopoi col* projw*rtioo ftloo lie to iho east and

' north or tho mndokn* , l -, . '-' ''' : ;V •:^:^^;i^-^A^;';";;'^^vK, :;l ; --:i.;-;iv.^ ; -.- ' . -' :v . . ' . ' . Si' ^ '•'.•,;:- - j. . ^^M/.r'^^''' 1 '''^.:^ '"i"; W'; '7" : "^vi"V : ,' :

G"OLOflYl

She ecology of the district and of the property is

relatively oitnplo* Tho Xeovmtin volcanics on the oast have, -'. ' ' - ' . ' - '-- : ' :'^.\. t: ^;f:^;I:ii^•:^^'^V^^^^-V••^ ; •'••

been intruded by a h use granite batholith which extends for: tsnny nileo to tho west and south* ?he intrusive contact

follows an arc having n-^onornl northwesterly trend* On '

tho ^Indokzv pro po r t/j, th e contact strikes f.bout 2S]de(?roo0

*eut of north, -Ahilo;farther to tho north r.oar Boston Creek

station it striJcoo nbout M650 weat. floar: :;thfli contnc* with'|.k

the volcnnico the fjrAnito tondo to naaumo a distinotly^ - t;;-

cuoinelo bcnilod utructuro. Lyinc next to tho uranite con*fix

tact io a band up to half a nllo t'ido of b o tide d tuffs and O

. 5 .

l c o n tlvolcanic fra^nontal rooks* Thin le ouooooiod to tho oant

by pillow Invan with nro&o of old diabase* narrow eranitio and

foloitJ.o dykoo occasionally occur cutting tho JToowatln rookfu

Tho ochlotooo Dtrixctura of tho Koowatin fratfraontal rooks and

tuffo conforno to thq gonoral dlrootion of tho granite contaoto

Aa noted lator,, thoro nro n imrabor of treriovoroo faults, ftl ong

t?hich tliero hao boon a oli{jht oovoncnt*

Moar tho northonct corner of tho property two apparently

asparuto tntruoionn of oonoidorablo else occur. Tho

Intraoion le A RIROB of cabbro^ crowded t-ith mgnotito

To tho woat of thlo thoro lo a largo dyfco^ 75 foot or nore

of nlcfv Innprophyro. Thooo two intraolono nro oopftratol by t*.

drnw or rolloy otrlktn^ poat of north*

(TAffi •W-'-.-'-v-.'** Wl

principal volno, or vein eye tons, oro knorn to

cxlot on tho proporty. She weotorly ,vcln syotcn occnro

practically on tho Pacaud-Cnthorino i'ownohip lino, very

clooo to th-j nrnnlto contact* Tho contact Itsolf lloo

In low croond, but har boon ootabllnhot! by dlcnond drill

!nc* Ornnltlo dykon { or onn.ll oille) also occur

tho boidJn,'j planoo of tho taffo near the volns.

5?ho voino consist of etrln^oro of fatrly

chalcopyrito, to;;othor vith txbout tvto foot of banded

pyrito juid cJmloopyrlto tilnoi-allftation in sillctfied

tuffs. 1'ho voins follow tho bncldinj of the tuffe nnd dip

aV.out b 2 rto^rnoo nay t* Two of tho nniri otrln -ore nro

foot ftpr*rt. A vortiorvl 2-oowpa rtr,c*nt shaft 100 foot

'.k on t!u o a j: t i? r J. y ono e r*.nd DD foot of

•rg

: Mf- 6 -

(Continod)

done at tiio 100-ft lovol. Vhoao workings nro now under

uator and tho Information below, obtained fron the nupor-

Intendont in charge, lo given RB ft rant tor of rooord.

Two drift roands on tho vein fron the vest oroon oat

shotjod 4?j copper over a cridth of 4 foot and 5^ copper over

4 foot, ' l

Foar dlsnond drill holes wore aloo pat dot?n. Throe of

thooo diocloeod oondltiono r&n^lng; froa nlnoralizntion to

oro. Tho boot holo showed 21 Inchon of core, roprooonting

10^ pluo inches true width, of rmaotvo ch&lcopyrito fxsnay-

2lcJ coppor. A 70-dogroe hole out 6 foot of vein natter~-.—— . -: -~~~ .

is 2.6)* copper*

In nonoralp it ntxy bo oald that this depth exploration

slightly bottoroii tho condition nppoarins on oarfftco, bat

the dlnonoionn ootabllohod to (Into nro rather too ecinJLl to

const!tato an ooononic deposit*

Ti'.ST V'.'IKi"--"

ffhio lo a parallel votn occurrlnc throe-quarters of R

nilo onot of tho i?oot voin end tho cane dietanoo onot of

ihe flranlto contact. Vhig lo a aaoh otrpn^er broak nnd

on.ro to hold wu oh Inr^or poonl bllltioo than tho voat voin*

Tho nroutrrr diotanco fron tho granite Is conoidorotl to

ijo an advr*,nt.-\no, rnthor thnn othornloo. Ihe ffonoral trend

of thlo vein lo north 20 degrees t/oot (nacnotlo) tind ite

ftvora^ro dip 7.0 do^roos onnt. A picket lino ran i n tho above

diroottor. wnn found to follow the roln fairly closely. The

vein' hno bo.-in traoed for 1500 foot on tho otrlko, and thero

lo no doubt obout l to furthor contlnutvnco oopeclnl Xy to

7

" o nt l nuod J

voin in plucoo followo a sheared or f united

contact botwocr. t\n o ld aie-bnne on tho voet nnd pillow Ifttrn

on tho or-.nt,, and It lo rmrJcoJ. by tho proatucoof a no. x- r or

dyko or rib of n, dontso greenish felsitic rock*

2? h o oro in tho voln lo of tho roplnoenent typo, tvoc-

orapnnlod by vory little c-ti\RrtP.a Chalcopyrite and, pyrJ.to

ropleco tho country rook B ooaetinos In frr.cturos And .fine

diosoninfttlono adjaoont to fine qanrtz otrlncorso sor.io*-

timoo oulphldoa rcplr.co It nltaost conplotcly in vhlch

caoo hi,-'h*.grr.do oro is tho rooa.lt*

' Xt io ftloo notable th&t n pinfc nranltic dyfce eovorol

foot wide outcrops within thirty foot to the vent of thia

rein In oovoral placoo*

A oorloa of trnnovorao faults^ otrlklnn raoro or JOBS

oaot and woo t, cat tho voln In ntxny placoo and diDplnco It.

f rota o- fow inohoo to R fow footo 'i'ho dl.splacenont in n early

alwayo to tho oust on tho north eldo of tho fi\Ult* Tho fault

flocuroo nro oonotinoo flllol with a fow Inchoc of qunrtsi

and tho voin nor\r them lo of ton onrlchod vi th quar t c and

nloo oul nhldo' nlnornllzatlon* Thlo action nppoare

Of tho diotrict* It lo notod ixloo on tho coot voln

on tho Ant t y Coppor lo tho nortl.vtoot, eh oro the "quarts

fftultn" dlsplftoo tho vein In the cfttae mariner ftnd oauoo ore

enrichment o In It* Tho qunrts t\p?oars lo onfxnftto i'ron tho

Crixnlto, vhich lo probnbly also tha coaroo of tho ooppor*

An incline ohaft lo bcinn sunk on tho oaat voin at

about tho centre of tho couth-OMitoriy ICO acres* At this

point tho ourfaoe thotto chiefly iron pyrite in tho voin,

with otrlji/roro tiiio^inR cooper curbonatoo nnd a littlo

l

chalcopyrtto. fho north t/nll of tho ohuffc choco chalco—

pyrl to coning In o4ulto ntron.;ly a o far R.O tho present bottom

of tho nhnft0 nt 15 foot. TTTO average or-7,plos acrono this

nail nt 10 foot r*nd 14 foot la dapth respectively shosrod

Io96;? coppor ovor 5 foot rind 2*6/5 coppor ovor 4 foot. She

appofcranco of tho oro lo bottor than thla and farther

check onnpllng till bo aono* She south wall of tho ehnft

ahotra IOSD chalcopyrlto bat lo hs.-vviljr shcnrod and shows

r. blr.olcinh jnlnornl rocenblins K^aphlto* Tho dyko or rib of

fnlslto npponro en tho hnnginn vrall*

Pron horfl tha rein is traced At froqaont intervale for

GOO foot to tho pouth c,nd 900 foot to the north. In man.?

plftcoj) it n.^poarc at tho ourfaco noroly aa a runty ^oosmn

eovorul foot ir. width, ohor/ing very liltlo r-alphide until

froohly blaotcd into* Cooper ninorclisation a;ipoc.rs rtron/jor

toward tho north. Tho bost indi vidu.nl oho&iiif; Wfto found

at tho tino of visit* Trr-cnonto of oro in nn uptxirnod

troo root woro found to bo ovorlyinc hi^h-ffrade ore in

oita* fitrippinj? disoloocd a width of nore than fire feet

of nearly nixon i vo oulphidoa, chiefly chalcopyrite. Channel

fjnnplo 'lo. 1001 noilnd r-crooo C. O foot hero ticrnyod 20.20^

copper, and n traoo of /:old. A fov foot tc the south,

nJm.nn*il o-;iplo Ho. 1502 Rcros^ ''...6 font r.fxvo c,lC;,^ copper Rttd

QQ*CO in paid, /."car tho t-nut:. end of Ihia ctrifiping sono

^rxlona vr.3 noted in the doooraposnd vain cu&ttor, a picked

cpccinon of vhich mn 12.00^ in load r.nd 50.0 os. eilvor,

also a traoo of .,old^ n rceult w hi o h lo ourpriein^ and, to

ony tho l o. tit, intoroBtin^. Snnploo 1901 nnd 1S02 vero not

(Continued)

a f-\"t'-: 't

S!

assayed for oliver, "but thin will now bo dona* in view o f

ft'oovo reuulta. '

Tho above eho*-ins is atout GbO foot north of tho in-

cXino ehaft. Strlpplnc wno proceeding north of thin again,

In tho courao of trhloh cood showings of chalcopyrite had bem

partly oxpooed in r* nunbnr of placoso Tho felsite dyko

follova.tho voin poraistontly rhorovor fiaao has boon exposed*

A, nunbor of irregular Quart* lonooe nlso occur, apparently near

tho trnnovor&o faulte, but tho oro doe o not AB c. rule occur

In tho 'qu'nrts itsolf*

Pyrrhotito cnpoara prftc*ioally nbocnt f row thle vein fctt

*

surfnoo, bat It will jaoat probably cono in Bt gro&tor depth

In tht* chief dove-loped copper property in tho dlotrict,

pyrrhotite nr\do ito firot appeixranoo at the COO-ft. lcvol,

trhoro it occurs in wr.ocivo ctrincoro. ^!he r.inernl l e not

of vr.luo in Itsolf, but Ito tendency towardo o noy replace—

r.ont by cluxlcopyrito lo voll-ootftT)liohod*

0?H "I

Two cuarts Tolno hcxvo been found e&tJt of thle smin vein,

Aloo o vnin of pure c&loito, but values of oonooqucnoo hnvo

not os yot boon found in thooo voino* '

Oron of r.iodiuci to hl^h crado brought out in the courao

of davnlopnioui o^-uld bo ohippad to the X o r and a emolter, on

r.o-onnt of tho oxoeptlonnlly favourable oltuatlon of tho

pro;j'.?rty v.-iti; regard to transportation* There le very

litilo of n rofrnotury nataro In tho oro, nhich should be

fit 'ho ordlnr^ry l^aoo rato of Ktout C-^*00 por ton*

- 10 -

l?A7u:r: Ajn nini'o,:;^;. up GJP-:^It lo bollovel that tho "breaking point" for profitable

shipments would bo about flvo ?or cent copper* A carload

of oro runv.lnfT between flro and ton por cent could probably

bo assembled alnou t Ir.noilatoly frora tho dunps of ; tho ttro

veins* Thorn la a vorj reasonable hope thai cufiloiont

ore sill bo dovolopoJ In thlo dlatrlctto juotlfy tho ©root-

ion of a flotation qonocntrator*

tt -'O or . :^:iii T r ONn i

l* Thn incline shaft should be continued to Ito pronont ol'jootivo of 50 foot*

2. ^ho vein area to tho north find south of tho nen dts-* oovoryx ahoiild bo thoroughly otripped t/SvcroTfor dopth of overburden and water conditiono porralt*

S* Tho vein Itoelf chould bo bladt trenched nt Intervale of oay 50 mot and toct pita ohould bo put dovfn at f?,riov,3 polnto to dotcrraino any chan;;oe in character of nineraliaation*

4* tho plokot lino striklnr? north 20 flogreos nctlc) should bo oxtondoJ both north nnd couth to f\ituro tronchlnc nr.d drilling operation©*

weettxs a guido

5. Tondoro ohould bo c&lled for t^o thouocnd foet of dlancnd driljlr./r- Thi0 foota^o cou.ld bo usefully omployod in drill in,; a nerioo of SOO-ft holca to tost both structure r-, r. A vein ut vortical depths of rk pproxtnately 200 foet. To do t.'. ir it v.'oulil *oo nccococry to drill fr^ri tho enst ir. to*ardo tho dip of tho voin, ;;i7inr; tho hoi 03 nnd initial dip of tilout 55 dogmas voat* Uitoo for ouch drill holes to bo ocl^otod on tho results of tho curfp.co work novr being

out.

6. A nnf-notonotT c urvoy would proo&bly proro ofIn trr.tiin- o;;t th* nnrth.-rr. oxtor.olon of tho voin {cnotvoln) In thr lov, ovrrburdonod ,-ruur.d3.000 font rort.'i of Iht* ii.oli;^ rJ-.rvft.a vory Intrr^ntin^ nron* ;. fow northtV.** pick-C'tO'I VMIC )ino eho.ild Vo ni;f flono t -kon ri t protablli li os r.'or^ r-'-*'*rV"

l a hru^

rr.Mch begins rTM o le potontlnlly

rnd south linoo i\oar obnervat-

Thointervale of 100 foet olon; theoo linoo* r.ro that the otriice of tho v ein w i 3 1 turn tTr.rd tho north, in Conformity with tho u/.i of tho country* -

ft

- n -

H *3or.y?3m tri ON s i

7* Cnro should be taken that nocousftry that p -i r t of tho property hold no raining performe-i and recorded*

assessment work. on alaina la duly

4'ifIr l-1

IL

8* Should tho a'lowinca In tho neighbourhood of the non dis- oov**ry otand up to thoir pronnnt pronlna in the coiireo of further work, tho sinking of another exploratory incline Bhtvft in thio r. roo. w j aid bo

Aosayo wore nad o by tho Provincial Assayere Office, ?arliat3ont Buililin^s, toronto, froa vhon pulps for checking purpoo os can to ob tained nt Any titio within cix months*

9RIOHT* BOYI*v:Ll. f JAIISS ft ASSOCIATES Consul ting i-ir.iiij;

Par

VOHOJITO, July 12, 1929*

COMPANY ^.Wajrr en.. ExplQ.j:a,t.jLana..Limited-...

PROPERTY ......Gawley...Opt.....Catharine...THp-...-...

DIAMOND DRILL RECORD HOLE NO. ...Hinki. J.,

SHEET NO. l DATE Dec. 23, 1974

DIP ANGLES

0' - 450

FOOTAGE

0-9'

9' - 36.5'

36.5 - 38

38 - 45

45 - 46.5

46.5 - 78

78'

^

^P

NAME OF ROCK

Casing

Dacite

Andesite -Gabbro

Gabbro

Andesite -Gabbro

Andesite

BEARING 2680 Astronomical ;LENGTH 78 '

LOCATION Grid Line 4 N 80' E

LATITUDE 200' south of northDEPARTURE Boundary

ELEVATION 5,1/2 Lot II Con IV

ROCK Basic to intermediate volcanic rocks.DESCRIPTION

Overburden (Casing left in hole).

Quite siliceous pale gray green fine grainedoccasional calcite stringers up to 1/4 inch inthickness at 45O to core axis. Minor and veryOccasional pyrite.

Contact zone possibly flow contact breccia or intrusivcontact. Slightly darker than above

Dark rather crystalline fine to medium grained black.Minor calcite stringers at 45O to core axis. Someslight fragmentation on contacts of zone. Minorchalcopyrite blebs but less than 5 7, sulphides

Similar to 36.5 - 38

Pale green, occasional calcite stringers at 45O to

core. Volcanic flows. .r

End of Hole.

^W

^^^——•••••^^^^^^^^^^•••^^••^^•••••••••^^^^^^^^^H"

STARTED

STOPPED

LOGGED

Nov. 25, 1974Dec. 10, 1974

BV J. A. PollockCORE SAMPLES NQNE

SAMPLE NO.

;

CorePiom

^•^M

WIDTH

4

ir (l*n —*vV-y\^

storeier Co

FOOTAGE

^t***^

*fcfo

^\

fL

ONAL ,

^ijy^^\\P

U^'-*^\fws^i^^VjjWlH^,

in Hailsultants

ASSAY ASSAY ASSAY

X'^\l

jr ^ 11

rf) i 1s Ej\o*V|

:yburxLtd.

^^1^P|

^^M^BH^^M

COMPANY Warren Expdorations Limited

" PROPERTY Gawley Opt ^ Catharine Twp.

DIAMOND DRILL RECORD

SHEET NO. l

HOLE NO. .

DATE Jan, 3, 1975

DIP ANGLES

0' - 500

BEARING 2680 AstronomicalLENGTH 5g 1

LOCATION Grid 325' N 90' E

UTITUDE 275' South ofDEPARTURE North Boundary

ELEVATION s| Lot II Con. IVROCK Basic to Intermediate Volcanic Rocks

FOOTAGE

0' - 5'

5' -, 29'

29'

29' - 34'

34' - 56'

56'

A™

A

NAME OF ROCK

Casing

Andesite

(Breccia)

Gabbro

Andesite

DESCRIPTION

Overburden Casing pulled out,

Pale green fine grained*6alcite ^stfeingers at V450to core axis no mineralization (greenstone)

Contact Zone

Flow or intrusive, calcite stringers^medium grainedto fine. Some scattered blebs of Cholcopyrite

As above.

End of hole Core stored in Haileybury at Pione

Reason for Drilling W-2To test depth possibilities of chalcopyritemineralization in trench.

RESULT OF DRILLING W-2

Results inconclusive as light equipment froze up incold weather. Hole not completed.

- -:- ;-- -- - - - .v- . . -. s--..- ' . . ''- -'.- ,--- - - . '.-, ,. .. . . . ' ' ' '' '' , '

1 -

•' V - ; 'V:--V ?: ' '. •f;;:-r.- ' .- 1 ' . -'.

,. . .. . ;-. ,. ; . .. ,-.;:j*^..

SAMPLE NO.

ir Cons

s ' ' -\ -S" "

•v;#-/-

STARTED Dec, 10, 1974STOPPED Dec, 16, 1974LOGGED BY J. A. Pollock

CORE SAMPLES NoneWIDTH

ultant

Jrcinjfri ui-^ f^ii

^. xO^S(t C

FOOTAGE

S,

tfVT-^"*filLr\rJpScfi^'- '

ASSAY ASSAY ASSAY

x'-VAf.,, i -' '--"li * j

jff^W^\ 't ^ l yi r^ vi .o JHyffii-^^Nc r.o*^"^••iiiiifl*^^

f/

4Lr

^'v 1mCOMPANYPROPERTY Ga*Lle? Opt^Catharine Twp.

DIAMOND DRILL RECORD

SHEET NO. 2

HOlE NO.DATE Dec. 23, 1974

DIP ANGLES BEARING LATITUDE

LENGTH DEPARTURE

LOCATION ELEVATION

ROCK

FOOTAGE

*

0

NAME OF ROCK DESCRIPTION

-Reason for Drilling Hole 47*0.Pile of hirarade ore (approx, 75 tons) of copper-^silver ore beside pit which assayed 8Z Cu. and 1 oz ofAg per ton led us to believe that there could be aplumb of ore large enough to mine and ship to acustom mill. Note Grab Samples only.

Result of Drilling Hole W-lW-l undercut the pit at approx. 20' and encounteredonly minor chalcopyrite mineralization.

Conclusion:More detailed drilling would hayje to be done alongstructure to eliminate possibilities of lenses ofore.

^

STARTED

STOPPED

LOGGED BY J, Pollock

CORE SAMPLESSAMPLE

NO.

Core

Pion

WIDTH

/Y

f

\"t

v'*

''X

\

Store*

:er Coi

FOOTAGE

,.'*"1

P

1 ' .ytribr

"-**i

adfHnvf"

ASSAY 1 ASSAY ASSAY

x''A" '-' )-* ^~: -

- ifi ™ " l^ s f AF---' ./A/lC i

l in Hail

isultants

•s

iybury

Ltd.

^1

iitnmaFIELD OFFICE

P.O. BOX 39, HAILEYBURY. ONT. PHONE 703-672-3311

To the Shareholders, Warren Explorations Ltd.

Your directors are pleased to submit herewith the initial report on the company's progress since incorporation.

Based on the successful completion of a financing program designed to provide $150,000 in working capital through the placement of 500,000 shares at 30(fc, a preliminary v/ork program was carried out on a 24-claim holding in Catherine and Pacaud Twps., southeast of Kirkland Lake in Northern Ontario.

These claims covered a high-grade surface showing of copper mineralization with supplementary silver values. Your company's program involved geophysical work, limited drilling, and supporting surface work. Two shallow holes were completed, following which work was suspended for the winter months. Drilling will be resumed later to check out some geophysical features.

More recently, and in reflection of the high interest generated by drill-hole confirmation of a new uranium potential in the Sandfly Lake district northwest of Lac LaRonge in Saskatchewan, your company has acquired a 60-claim property to the south of the Thor Explorations discovery group, on which Noranda Mines and Brascan De velopment are financing and conducting an extensive ex ploration program .

The Warren ground lies on strike of the discovery zone, and within the favourable meta-sedimentary belt, The discovery group attracted attention when an extensive assembly of boulders in which encouraging uranium values were obtained were located over an area some 5,000 ft. in length and 300 ft. in width. The Noranda-Brascan team, in their initial diamond drilling, reported an intersection of 3.52 Ibs. U308 over a core length of 13.3 ft.

A field program for the VJarren ground is now being considered, and shareholders will be advised of developments,

...7

smoRATtoHs LIMIT f DFIELD OFFICE

P.O. BOX 39, HA1LEYBURY. ONT.

PHONE 705-673-3311

SUITE 40136O BAY ST.. TORONTO. ONT.

PHONE 416-363-7381

- 2 -

At the same time, your company is pursuing active con sideration of an overseas gold exploration project, but at this point negotiations have not advanced to the point where the potential commitment could be considered as finalized.

On beha3rl\ of the Board of Directors,

Q.hn Pollock, President.

January 18, 1975-

31M13NW8897 63.3246 PACAUD 050

REPORT

ON

THE CATHERINE-PACAUD TOWNSHIPS PROPERTY

OF

WARREN EXPLORATIONS LIMITED

BOSTON CREEK AREA

DISTRICT OF TEMISKAMING

ONTARIO

by L. J. Cunninghon, B.Sc., P.Eng.,Mining Engineasr

dated at Kirkland Hake, Ontario3rd July, 1974

TABLE OF CONTENTS

, Page

SUGARY

INTRODUCTION l

LOCATION fc ACCESSIBILITY 2

GENERAL GEOLOGY . 2

GEOLOGY OF THE PROPERTY 2

ECONOMIC GEOLOGY OF THE AREA 3

ECONOMIC GEOLOGY OF THE PROPERTY 3

CONCLUSIONS ft RECOMMENDATIONS 4

CERTIFICATE

MAPS:

1. Location Map - Kirkland-Larder Area

2. Claim Map - Part of Catherine fe Pacaud Tovmships

3. Map 1957-4 - Geology of Boston Township and

part of Pacaud

In pocketof

report

SUMMARY OF A

REPORTON

THE CATHTJilNE-PACAUD TOWNSHIPS PROPERTYOF

WARREN EXPLORATIONS LIMITEDBOSTON CREEK AREA

DISTRICT OF TEMISKAMING .ONTARIO

1. The property consists of two contiguous patented lots, one in Catherine

Township, the other in Pacaud Township of the Larder Lake Mining Division,

Ontario,

2. Small b\it rich pipe-like copper deposits are found associated with volcanic

rocks in a zone extending for at least three miles along the eastern margin of

the Round lake batholith.

3. Shaft sinking and mining has been done on 4 of these deposits and a limited

tonnage of high grade copper has been shipped as direct smelting ore.

4. The Warren ground includes the former Mindoka property on which a 115 foot

shaft was sank and from which 225 tons of 8ft copper were shipped to the Noranda

smelter.

5. The property has been idle since 1929.

6. A program of line cutting, magnetometer and EM surveys, and a 2,000 foot

drilling program are recommended to test for zones of massive copper-bearing

sulphides.

Estimated cost of the program is $33,000.00.

3rd July, 1974

KEPORTON

THE CAT11ERINE-PACAUD TOWNSHIPS PROPERTYOF

WARREN EXPLORATIONS LIMITEDBOSTON CREEK AREA

DISTRICT OF TEMISKAMINGONTARIO

INTRODUCTION'In the early 1920's the Boston Creek Area was actively prospected for

gold and a limited production was obtained from two properties.

In 1926 copper vras discovered' along a zone extending southeasterly for

2-J, miles from the Village of Boston Creek. Between 192? and 1930 a limited

production was obtained by underground development of three properties.

Similar rocks extend in a semicircular belt along the periphery of the

granite through Catherine Township and contain a number of known gold and copper

showings.

During 1974 Jonpol Explorations Limited purchased the property for

^6,000.00 cash and a yfa royalty based on net smelter returns to a maximum of one

million dollars, thereafter the royalty will be reduced to 2# of net smelter

returns. Jonpol Explorations Limited are vending the property to Warren

Explorations for a stock consideration.

The property covers the favourable copper bearing horizon and is

considered a base metal prospect.

The following references have been utilized:

Grant, James A. Geologist, Ontario Department of Mines Geological Report No,18 Catherine fe Mater Townships

Lawton, K.D., Geologist, Ontario Dept. of Mines "Geology of Boston Townshipand Part of Pacaud Township" Vol. 66 pt. 5, 1957 with map 1957-4

Koiles, R.G. Ph.D., Geological Report on the Trethewey-Ossian Lease of the GoldenArrow Mines Ltd., Pacaud Township, Boston Creek Area, Ontario dated June 15th, 1952

Ennis, G.F., Mining Engineer, Report on Ossian-Trethewey Copper Property, PacaudTownship, Ontario dated January 25th, I960

Bell, R.A., Geologist, Report on the Induced Polarization and Resistivity Resultsfrom the Boston Creek Property, Pacaud Township, Onta rio for Fidelity Mining Investments Limited dated ?th December, 1961

Cunningham, L. J. Mining Engineer, Report on Patterson fc Trethewey-Ossian CopperProperties, October, 1966

James, Victor A., Mining Engineer, Report on Mindoka Mines Limited, July 1929

Hughes, Frank W., B.Se., Mining Engineer, Report on Copper in Pacaud Township,November, 1953

/arren Exploration, Horton Creek

LOCATION 6 ACCESSIBILITY

i 2 July 1974

Tlie property consists of 2 contiguous patented lots, one in Pacaud

Township, the other in Catherine Township.

They are unnumbered but are described as follows: -ri Pacaud Township Sg Lot l Con. IV 160 acres

Catherine Township S| Lot 12 Con. IV 152 acres

The property lies approximately 14 miles southeast of the Town of

Kirkland Lake. The claims are 8 miles east of Highway 112, Highway 564, an all-

weather gravel road., extends easterly from Highway 112 through the village of

Boston Creek and then turns southerly to cross the centre of the property along

the Pacaud-Catherine Townships line.

A high tension power line of the Ontario Hydro Electric Commission,

and the Ontario Northland Railway are located about 3/4 of a mile southwest of the

property. The railroad is accessible by an all-weather gravel road, the distance

from the property being three miles.

GEHKPJVL GEOLOGY

Keev.-atin volcanic rocks underlie most of the areaj immediately to the

west is the Hound Lake granitic pluton, with its margin convex to the east. In

eneral conformity vtith this margin are: (a) banded tuff, (b) basic to inter

mediate lavas and intrusions, (c) intermediate to acid fragmental rocks, and (d)

coarse-grained volcanic rocks.

The Keewatin rocks were intruded first by ultrabasic to intermediate

dikes and sills, and then by numerous, small acid to intermediate, and lampro

phyric dikes - probably associated with the emplacement of the Round Lake pluton.

JEOLOGY OF THE PROPERTY

The eastern margin of the Round Lake pluton underlies parts of Lot 12

along the western edge of the property. The Keewatin rocks occur as a steep

anticlinal belt around the granite. Grant (O.D.M, G.R. 18) has subdivided these

rocks into three stratigraphic formations, from west to east and from oldest to

youngest as follows:

A. Interbedded tuff and tuffaceous sedimentary rocksj with minor iron formation.

This division lies next to the Round Lake pluton and is traversed by numerous

small dikes and sills. The total thickness is unknown, but is about 1,300 feet

here,

B. Dioritic, dacitic, and andesitic lavas. Pillowed lavas are common in this

division, which has a thickness of about 10,000 feet.

I'/urren Kxplcration, Boeton Creek

C. Porphyritic and aphanitic, intermediate to acid volcanic rocks, largely

pyroclastic, and agglomerate. The thickness of this division is also about

10,000 feet.

Thus the following sequence of rocks exists across the property from

;est to east:

1) a north south strip of granite ~ 1/2 mile wide being the edge of the pluton

2) a belt of interbedded tuff and tuffaceous sediments, 1/4 mile wide, striking

jortherly with steep easterly dips

3) a band, 2 miles wide, of basic lavas with similar strike and dips 0

A basic sill some 500 feet in v;idth parallels the granite contact

jithin the basic volcanics and forms the east boundary of the property. It is a

dark grey, medium grained quartz gabbro.

Minor amounts of Keweenawan diabase and Algoman syenite, quartz

porphyry arid lamprophyre occur as small irregular intrusions or dikes*

A number of faults extend radially to the east from the granite

Dluton into the Warren ground. :

SCONCMIC CPJOLOGY OF THE AREA

- 3 ~ July, 1972,

Two miles to the northwest of the Warren ground copper shoots have beei

nined as replacement bodies in iron formation at the contact with acid tuff.

The mineralized zones are pipe-like and of high grade (5 to 10^ copper

per ton) with maximum dimensions of 50 feet in length by 5 feet in width. They

appear to be localized at cross faults which cut the iron formation.

The ore consists of chalcopyrite v/ith varying amounts of bornite,

chalcocite, pyrite and pyrrhotite. Mineralization grades rapidly from massive

halcopyrite to barren pyrite and pyrrhotite.

Three adjoining properties, the Amity, the Patterson and the Trethewey-

Ossian, were explored by underground development. Some stoping was done and limit'

tonnages of direct anelting copper ores were shipped to Noranda during the 1920's.

Since that time, these three properties have been leased and a small

amount of high grade (5# ~ 10#) copper has been salvaged. Limited drilling has

been done on some of these properties.

ECONOMIC GEOLOGY OF THE PROPERTY l , ,

Within 200 feet of the Pacaud-Catherine Township line in the northwest

quarter of Lot 12, Con. IV Catherin Township, the caved collar of a small shaft

can be seen v/ith a small rock dump. Caved and flooded trenches indicate the

presence of two veins which are described by Victor A. James, Mining Engineer, in

arren Explorations, Boston Creek~ 4 -

July, 1974

, report dated 12th July, 1929 as follows:

"The westerly vein system occurs practically on the Pacaud-Catherine

ownship line, very close to the granite contact. The contact itself lies in low

round, but has been established by diamond drilling. Granitic dykes (or small

sills) also occur along the bedding planes of the tuffs near the veins.

The veins consist of stringers of fairly massive chalcopyrite, together

;ith about two feet of banded pyrite and chalcopyrite mineralization in silicified

uffs e The veins follow the bedding of the tuffs and dip about S2 degrees east.

Two of the nain stringers are 45 feet apart. A vertical 2~corapartment shaft 100

feet deep was sunk on the easterly one, and 55 feet of crosscutting was done at

he 100-ft. level. These workings are now under water and the information below,

obtained from the superintendent in charge, is given as a matter of record.

Two drift rounds on the vein from the west crosscut showed 4# copper

over a width of 4 feet and 5# copper over 4 feet.

Four diamond drill holes were also put down. Three of these disclosed onditions ranging from mineralization to ore. The best hole showed 21 inches of

ore, representing 10y plus inches true width, of massive chalcopyrite assaying

2I?3 copper. A ?0-degree hole cut 6 feet of vein matter assaying 2.6# copper.

In general,,it may be said that this depth exploration slightly

bettered the condition appearing on surface, but the dimensions established to

date are rather too small to constitute an economic deposit,"

Frank W. Hughes, B.Se., Mining Engineer, in a report on the copper

properti.es of the Boston Creek Area dated l?th November, 1955, described the

lindoka property as follows:

"Mindoka Mines; Shaft 115 ft.- one level established. 3 D.D. holes

from surface. D.D, Hole #1 intersected 18" true vddth massive chalcopyrite at

vertical depth of 250 ft. D.D. holes #243, along strike for an overall lengthi

of 400 ft. intersected 2" to 3" stringers of chalcopyrite over 6 to 7 ft. at

vertical depth of 250 ft. Previous operators shipped to Noranda in 1929: 225 tons

of S?3 copper."

INCLUSIONS St RECOMMENDATIONS

The property has been idle since 1929. Consequently caving, flooding

and the overgrowth of brush and trees has obliterated almost all evidence of the

two known veins. However there is no doubt that Mr. James and Mr* Hughes are

describing the occurrences on the Warren ground.

Work to date on the Boston Creek copper belt has produced small, rich

'/arren Explorations, Boston Creek - 5July, 197/1.

pipe-like bodies of copper mineralization. However, this does not preclude the

possibilities of finding zones of rich mineralization of a size to permit economic

xtracvtion. The geology is favourable and the physical features, such as good

road access, close proximity to rail shipping facilities and smelter, operations

(Koranda, Quebec) are distinct advantages in the successful mining of small or

large ore bodies.

In 1970 an airborne Questor Mark MKV input survey was flown over the

area by Moncrieff Uranium Mines Limited. Mo conductors were reported on the Warrer

ground but a re-exanination of the flight tapes is recommended. The Warren ground

was not held by Moncrieff, consequently little attention may have been given to

this portion of the survey.

It is further recommended that:

(i) Lines be cut at 200 foot centres across the Catherine half of the property

(ii) Lines be cut at 400 ft. centres across the Pacaud half of the property

(iii) A magnetometer Si a VLF survey be completed over the property

The Catherine half of the property be mapped(iv)

(v)

Estimated Cost

$ 1,300.00

700.00

2,500.00

1,000.00

Diamond drilling be completed to test:(a) anomalous areas(b) the known veins at shallow horizon and in the

vicinity of the shaft

2,500 feet @ 10.00/ft.

Supe J'vision

25,000.00

2,500.00

$ 33,000.00

Signed,

Dated atKirkland Lake, Ontario3rd July, 1974

L. J. Curininghara, B.Sc,, P.Eng., Mining Engineer- . '-

V W

rMATsONVILLE:-i"" ~

~/- ', s*'- L^sL- s -

* * *

* * * * * * /*

* * *

*

i-'.v- x l-*N . ^ s j

* * * * * * *) * *

* * ** * *

* *

* ir * * * ** ' * *S . \ t * * * * ^ * * *VN, 'X

0^* . \ BUA.N * *I\ \K-}* ^*] * * * t tt ** * \* *'jgss^-* * * * * * * t * * * *

C7 la-' ' - -Ww? r/Vfc KJ-C'N-- vS* r ~* ' -'"'i-,, ^.'- '~' X z " -- -~, ' "1-1;^ '-^i^i/T^tf^ i"'^'i~ x 1 '-* l '-^'- l - x 'x',-'"- 1! x!*' - ' - ' ?^r^y.y^^tex':^xl/^ Jc^^L.^K'or^viy^o^/c. ' ^^erl^'.v-^ 'v-- --\ -^- . ^ ov:yr -!S^S^^^f e

' ' Be^^tiJ^VTT^X

mm^m-V.-^^-S:'--'™**r:-:mm-^z&gym

''' u"MARQUIS

* * * * -

mm^?-

Amity Patterson ' Trethe srey-Ossian KIRKLAND LAKE — LARDER LAKE AREA SHOWING PROPERTY LOCATIONS AND GENI

Warren Explorations Ltd.

;-::-::-.::"

am

! **

A

PROVINCE

OF ONTARIO

PROVINCE

OF QUEBEC

ONTARIO

DEPARTMENT O F MINES

HON. (i. O.WAKDKOPK, M inister of Mint*

IX P. Douglas1*. Deputy Ministcr M . K. Hurst, D irector, Geahffica! llranch

Map 2043Catharine a nd Marter Townships

WAEEEN

LIMITED

T a*^f ; iCsr ^

SYMBOLS Scale, l inch to 50 miles

N.T.S. reference 31 M/13,32 D/4,: ^ ! ^: iGlacial striae,

Small rock outcrop.

Boundary oj rock outcrop.

Geological boundary, defined.

Geological boundary, approximate.

Geological boundary, assumed.

^' ;^m r

H, f A .,

anrf tf/p o f schistosity,

Strike of vertical schistosity.

Strike and dip of gneissosity.

Strike of vertical gneissosity.

Jointing, inclined.

;1M v*} ^

PLEISTOCENEClay, sand and gravel.

PRECAMBRIAN**PROTEROZOIC

KEWEENAWAN

\ a '' ' i ^- \ \ feb ,'-' )'",*;' "\ ^ )-\ * '''' -r-, f /l/V^----- \ 3t \ M \ \ \ i \ l f f V-^ . \ 1*^-'( i, o N i 26; r /~'

,—— ' V-' l\* '"^ -""' 7 ^'

HURONIAN COBALT GROUP

GOWGANDA FORMATION5a Conglomerate. 5b Greywacke. 5c Arkose, quartzite. 5d Argiiiite.

ARCHEANALGOMAN?

4a Syenite.4b Granodiorite,4c Granodiorite gneiss (Round Lake

pluton). 4d Albite porphyry, quartz-slbite

porphyry. 4e lamprophyre. 4! Felsite.

3a Diorite.3b Gabbro.3c Serpentinized peridotite.3d Diorite porphyry, dacite porphyry.

KEEWATINBASIC TO INTERMEDIATE

VOLCANIC ROCKS(prodom;nantly lavas)2b Dacite and andesite, including

2 pillow lavas.2c Diabase, diorite and gabbro. 2f Sheared volcanic rocks. 2g Fragments/ iavas. 2v Variolitic lavas.

INTERMEDIATE TO ACID VOLCANIC ROCKS

(predominaitly pyrcclastic)1a Porphyritic dacite and andesite,

mostly crystal tuff.Jb Dacite and andesite, mostly

aphanitic tuff.1d Banded luff and tuffaceous sedimen

tary rocks with minor iron formation1f Sheared volcanic rocks.1g Agglomerate.1r Rhyolite.

CATHARINE

LOCATION PLAN OF MINING PROPERTIESScale, l incti to 2 miles

?. Burnand-Gzowski.2. Cam p bel!.3. Canoro (Q&tmm).4. Catharine Gold.5. Connett-McDonougn.6. Cotter.7. Daley.8. Gold Hi!!. 3. Hounsiow.

W. Katyniuk.11. Kennedy-Boston.12. Kordo! Explorations Ltd. (Gold Bank).13. Kordo! Exolorations Ltd. (Gold Ridge).14. Minaoka.15. Mirado Nickel Mines Ltd. (Caihroy Larder). W. Ostrom.17. Roger-Barnett.18. Sawka Aiisrd.W. Tyrzonc Explorations Ltd. (Hilltop).20. Walsh-T ay lor.21. Wojcieszyn,

Map 2043

CATHARINE AND MARTER TOWNSHIPSTIMISKAMING DISTRICT

20©

Sralt- 1:31,680 or l Inch tn '/j Milr

Feet 1000 &.000 10,000 Feet

6+00

+QON

2*00*

•MOt

-10-f

.X -* —i—— -~^^^ \ 0 \^^--^ u* ^ ^ X* . —L- -~~Hi ir \ ^^^^-V^ 9. X *- , — -*-— " \ i \*i *? o o/"^ ——- *" — ~~ \ —— * " *T (O f|\

0 / \±——^~"^ \ -v o o ^ ^\^^^ \ i ffi o U \

^-^— - ~ ^"^ \ N 0 M111 ^ ^—— — — -"^\ ut * o *\r — \ *i o ^ ©\^ \ * o o * J*0* t, 0 * J i

s 1 * t- -^ * *\0* *\oll\^\ o\*\Tfl\ M\?S\*\

; O\ ^i*\

tp* O O m RADEM SURVEY PROFILE ' SCALE l" - 20*

RADEM SURVEY CONDUCTORS - —————— —

STATION USED - CUTLER, MAINE

WARREN EXPLORATIONS LTD.:

3IM13NW0C97 63.3246 PACAUD 320

RADEM SURVEY

PACAUD 8. CATHERINE TWPS

SCALE I'VIOO' JAN. 1975

C A

TH

ER

INE

T

OW

NS

HIP

PA

CA

UD

T

OW

NS

HIP

RA

OE

M

SU

RV

EY

M

AG

NE

TO

ME

TE

R

SU

RV

EY

210

2ffO

RA

DE

M

SU

RV

EY

P

RO

FIL

E

"- S

CA

LE

RA

DE

M

SU

RV

EY

C

ON

DU

CT

OR

S

20

ST

AT

ION

U

SE

D -

CU

TL

ER

, M

AIN

E

31Ml3NWe097

63.3246 PACAUD

23

0

WAR

REN

FX

PL

OR

AT

ION

S

LT

D.

IMAG

NETO

METE

R a

RADE

M SU

RVE

PA

CA

UD

a

TWPS

!C*L

EJA

N