42A15SE001S OP93-Q2B EDWARDS

010

MOOLLEY LAKE CLAIMS

REPORT OH PROSPECTING. VLF-EM.

MAGNETOMETER AND GEOLOGICAL SURVEYS

EDWARDS TWP. ONTARIO

NTS 42A/15

LARDER LAKE MINING DIVISION

September 10, 1993 Wayne Benham 921 Hillowdale Ave. fiillowdale, Ontario M2M 3C2

42A15SE0015 OP93-02B EDWARDS 01OC

TABLE OF CONTENTS

l.O INTRODUCTION.. .. .. ... . . .. . . . .. .... ... . . . . . . . . . . . . . . . . . . . . . . l

2.0 PROPERTY, LOCATION and ACCESS............ . . . . . . . . . . . . . . . . . . l

3.O GEOLOGY.................................................... 4

4.0 PREVIOUS WORK. .... .. .. .. . . . . . . . . . ... .. . . . . . . . . . . . . . . . . . . . . . 4

5.O WORK DONE.... . . ... .... . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6

5.1 Prospecting.......................................... . 6

5.2 Linecutting.......... . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6

5.3 VLF-EM Survey... . . . . . . . . . . . . . . . . . . . . . . . . . . . ........... 9

5.4 Magnetometer Survey................................... 9

5.5 Geological Mapping.................... . . . . . . . . . . . . . . . . 9

6.O EXPLORATION RESULTS....................................... 10

6.1 Prospecting.................. . .. . . . . . . . . . . . . . . . . . . . . . 10

6.2 Geological Mapping......................... . ... . ... . . 11

6.3 Magnetometer Survey.................................. 19

6.4 VLF-EM Survey.................. . . . . . . . . . . . . . . . . . . . . . . 20

7.O CONCLUSIONS and RECOMMENDATIONS... .. .. ... . ... . . . . . . . . . . . . . 20

8.O REFERENCES................................................ 22

TABLE l Daily Prospecting Log

TABLE 2 Grab Sample Descriptions

APPENDIX I Geophysical Instrument Specification and Geophysical Technical Data

FIGURES l Location Map2 Claim and Grid Location Map3 Prospecting Location Map

MAP l Geology Map, i" = 200'2 Magnetometer Survey, l" ^ 200'3 VLF-EM Survey Profiles, l" = 200'4 VLF-EM Survey Fraser Filter, l" =200 I

OPAP FINAL REPORT WOOLLEY LAKE CLAIMS EDWARDS TWP. ONTARIO

1.0 INTRODUCTION

This report describes the results of prospecting, VLF-EM ,

magnetometer and geological mapping surveys carried out from

June 19 to July 26, 1993 by the writer on the Wooiley Lake Claims

located in Edwards Township, Ontario. This work was funded by the

Ontario Prospectors Assistance Program (OPAP), File Number

OP93-028. The writer was assisted in the field by E. Benham. The

results of this program are presented on Maps I to 4 at a scale of

l" = 200' .

2.0 PROPERTY. LOCATION and ACCESS

The Wooiley Lake property consists of two claim blocks,

L.1187113 of 12 units and L.1187114 of 8 units, for a total of 20

claim units. The claims were recorded on February 3, 1993 in the

name of Wayne Russell Benham. The property is -located in the

central portion of Edwards Township in the Larder Lake Mining

Division about 10 kilometres north of the Town of Iroquois Falls

(Claim Map Sheet G-3496, NTS: 42 A/15, Latitude 48 0 51' Longitude

80 : 38', Figures l S 2).

Access is by the Detour Lake Road leading northwards from

Iroquois Falls to Kilometre Eight, east for 2.0 km and then north

for 0.4 km along Abitibi Paper Company Ltd. logging access roads.

Except for outcrop areas, the property has been logged of within

the last five years and partially reforested.

Adjoim Map 2161 Coral RapM

*rrt

LOG ATI OH MAP

Scale: l" = 4 miles

Modified after O.G.S. Map No. 2205

Figure l

x r

Dv5

HOOLLEY LAKE CLAIMS

EDWARDS TOWNSHIP

LARDER LAKE MINING DIVISION

Scale: l" = 1/2 mile

Plan No. G-3496

Figure 2

Since adequate accommodations could not be found in the

Iroquois Falls area, the writer travelled daily to the property

by car from Tarzweil, Ontario and the home of L.M. Dyment and

J. A. Kidston whose kind hospitality was greatly appreciated. The

round trip distance to the property and back to Tarzweil is 264 km.

3.0 GEOLOGY

Edwards Township is underlain by Archean sedimentary and

volcanic rocks which are intruded by diabase dykes and gabbroic

stocks.

The volcanics consist of felsic ash to lapilli tuffs and mafic

flows. The sediments consist mainly of graywackes with interbedded

volcaniclastics, siltstones and graphitic argiilites. The

sediments and volcanics strike N20 3E to N40 : E and are steeply

dipping. The diabase dykes are associated with the north northwest

striking Timiskaming Lake structural zone.

Previous drilling and surface trenching during the 1960's in

the west-central portion of Edwards Township, discovered semi-

massive pyrite and pyrrhotite with geochemically anomalous nickel,

copper and zinc contents.

4.0 PREVIOUS WORK

Research of the Kirkland Lake Assessment Files for Edwards

Township showed that the township was flown by Canadian Aero

Mineral Surveys for Canadian Javelin Ltd. in 1964. An extensive

zone of bedrock conductivity with magnetic correlation was located

Page 4

to the west of Wool ley Lake. During 1965 Canadian Javelin Ltd.

carried out horizontal loop EM, magnetic and geological mapping

surveys to explore this conductive zone. Subsequent drilling

intersected semi-massive sulphides in graphitic sediments, altered

felsic volcanics and gabbroic intrusives. Geochemically anomalous

copper, zinc and nickel assays ( up to Q.13% Cu, Q.14% Zn and

Q.10% Ni ) were reported.

Survey lines were cut north-south at an acute angle to the

strike of the volcanics. Therefore, it appears that the ground

electro-magnetic survey was not interpreted correctly. The strikes

of the magnetic anomalies, which correlate closely to the strike of

the volcanics, are almost perpendicular to the interpreted strikes

of the EM conductors. The Canadian Javelin holes were drilled along

the strike and down the dip of the volcanics. Although the holes

intersected conductive graphite and sulphides with anomalous

basemetal assays, the strongest conductor probably was not tested

due to the improper orientation of the drilling.

In 1964, Inco drilled a hole which was located approx

imately 1.5 km to the north along strike of the Canadian Javelin

conductors. The Inco hole intersected semi-massive sulphides but

no assay results were reported.

Edwards Township was flown in I960 by Amax and Cominco however

both these companies followed up anomalies to the north and south

of the current Wooiley Lake claims.

During 1988, an airborne electromagnetic and total intensity

magnetic survey of the Detour-Burntbush-Abitibi area was flown by

Geoterrex Ltd. for the Ontario Geological Survey. Map No. 81240,

which covers most of Edwards Township, shows similar EM and

Page 5

magnetic anomaly patterns as the Canadian Javelin airborne survey

but in greater detail.

5.0 WORK POKE

Only 24% of the work was done on claim L. 1187114 while 76% of

the work and all of the sampling were done on claim L. 1187113.

5.1 Prospecting

The property was prospected for five days from June 19th to

23rd inclusive by the writer and field assistant E. Benham. The

main purpose of this work was to locate the previously reported

sulphide showings, confirm the interpreted strike of the volcanic

rocks and locate the starting point for the proposed grid. Four

grab samples (Nos. 88901 to 88904) were collected and assayed for

Au, Ag, Cu, Pb, Zn and Ni. (See Table l for prospecting log and

Figure 3 for prospecting sample locatons).

5.2 Linecutting

A 10.01 mile grid was cut July l to July 8, 1993 under

contract by Thomas Obradovich of Kirkland Lake. The western part

of the grid consists of a baseline, starting at post No. l of claim

L 1187113, at 030 : Az and cross lines at 400 foot intervals from

4+00 S to 36+00 S with pickets every 100 feet. The eastern part of

the grid consists of baseline 28+00 S at 1200 Az and cross lines at

800 foot intervals from 00+00 to 32+00 E with pickets every 100

feet.

The location of the grid with respect to the claim boundaries

and topographic features is shown on Figure 2.

Page 6

Table l

Prospecting Daily Log

Date Work Performed

July 19 Prospected reported outcrop area along northern

claim line of claim L. 1187113.

Three samples taken nos. 88901 - 88903.

July 20 Prospected outcrops in the north central part of

claim L. 1187113. One sample no. 88904.

July 21 Prospected outcrops in the central portion of

claim L. 1187113 in the area of previous work by

Canadian Javelin.

July 22 Prospected outcrop hill in south central part of

claim L. 1187113.

July 23 Prospected east central outcrop area of claim

L. 1187113 and located claim post no. l of claim

L. 1187113 for the starting point of the planned

picket line grid.

Note: Grab sample locations were flagged, relocated during the

mapping survey and tied into the picket line grid. The prospecting

grab samples are plotted on the geology map.

Page 7

WOOLLEY LAKE CLAIMS

PROSPECTING LOCATION MAP SHOWING SAMPLE LOCATIONS

Scale: l" = 1/4 Mile Dates: June 19 - 23, 1993

V

5.3 VLF-EM Survey

The VLF-EM survey was carried out by the writer from July 10

to 13, 1993 with a Crone Radem VLF-EM unit. The dip angle in

degrees of the magnetic field component from the horizontal was

measured. The number of readings taken at 100 foot intervals was

514. For the western part of the grid, the transmitter station

used was Annapolis, Maryland which operates at a frequency of 21.4

KHz. The eastern part of the grid was surveyed using transmitter

station Seattle, Washington which operates at a frequency of 18.6

KHz. The instrument specifications are listed in Appendix I.

5.4 Magnetometer Survey

The magnetometer survey was carried out by the writer from

July 14 to 17, 1993 using a Barringer proton magnetometer. Model

GM-122. This instrument measures the earth's total magnetic field

to an accuracy of l gamma. Additional specifications are given in

Appendix I. Diurnal variations were monitored by establishing base

stations and completing hourly closed survey loops. A total of 984

readings were taken at 50 to 100 foot intervals depending on the

magnetic gradients along the surveyed lines.

5.5 Geological Mapping

The property was mapped by the writer and field assistant

E. Benham from July 18 to July 26, 1993 by traversing the grid

lines. Traverses between the grid lines were made in the vicinity

of any sulphide showings. The outcrops located in the south

western portion of claim L. 1187113 were not covered by the cut

picket line grid. These outcrops were mapped by a pace and compass

Page 9

line at 48+00 S from baseline 0+00 to the western claim boundary.

Twenty-two grab samples (Nos. 5057 to 5064, 13589 to 13600)

were collected and assayed for Au ppb, Cu ppm, Ni ppm and Zn ppm.

Two samples (Nos. 13592 and 13598) were assayed for Pt ppb and

Pd ppb. Whole rock analysis were completed for samples 5058, 5063,

13590 and 13593.

6.0 EXPLORATION RESULTS

6.1 Prospecting

Prospecting traverses in the western portion of claim

L. 1187113 found the volcanic and sedimentary rocks to strike 205:

to 215' Az. Only intrusive rocks, i.e. diabase and gabbro, were

located in the central eastern part of claim L. 1187113 and no

outcrop was found on claim L. 1187114. However, the airborne

magnetics for the area indicate that the strike of the underlying

formations is 120 3 Az in the eastern part of the property.

In the northwestern part of claim L. 1187113, disseminated

pyrite and pyrrhotite were discovered in finely bedded siliceous

volcaniclastic sediments. The sediments are intruded by irregular

narrow, l" to 6", blue-white quartz veins. These sulphide showings

are located to the north of the previous work reported by Canadian

Javelin. Three grab samples (Nos. 88901 -88903) of the sulphide-

bearing material and one grab sample (No. 88904) of the quartz

veins were collected and assayed. Samples of the sulphides were

weakly anomalous in nickel and zinc. All four samples assayed Nil

gold. The sample locations are shown on geology Map l and the

results are listed in Table 2.

Page 10

As a result of the prospecting work it was decided to

establish a picket line grid with a baseline at 030' Az in the west

and a baseline at 120 3 Az in the east to investigate a possible

synclinal fold structure.

6.2 Geological Mapping

The Wool ley Lake property is underlain by Archean volcanic and

sedimentary rocks which are intruded by related gabbroic masses,

granodiorite and Matachewan diabase dykes. No outcrop was found on

the eastern claim block L. 1187114 where the overburden consists of

wet clay deposits in the southwest part of the claim and sand

plains to the northwest. On the western claim block L. 1187113

four outcrop areas were located. Each area is marked by a

prominent hill which is due to a diabase dyke. The results of the

geological mapping are shown on Map l at a scale of l" = 200'.

6.2.1 Sedimentary Rocks

The sedimentary rocks consist of graywackes, siltstones,

argillites and volcaniclastics intercalated with minor associated

felsic to intermediate pyroclastics.

The graywackes and siltstones are grey-green, fine to medium

grained and massive to finely bedded. The argiliites are black,

carbonaceous, pyritic and finely laminated. They occur as large

3'x 2' xenoliths in the gabbro intrusives at 2 + 00 E to 3 + 00 E

along line 28+00 S.

The volcaniclastic rocks consist of thickly bedded units with

lapilli of sedimentary and felsic volcanics in a fine grained

biotitic graywacke matrix. The most dominant ciasts are resistive

Page 11

sub angular, fine grained, dark grey, felsic lapilli up to 0.5"

wide.

6.2.2 Volcanic Rocks

The volcanic rocks consist of fine grained, dark green to grey

green, massive to well pillowed basalts with associated pillow

breccias and hyaloclastites. The pillowed lavas are best exposed

along the eastern edge of the outcrop hill at 48+00 S.

6.2.3 Intrusives

Three, 100'to 200' wide, northerly striking, nearly vertically

dipping, diabase dykes cut the volcanic and sedimentary

stratigraphy. The diabase is brown weathered, dark green, medium to

coarse grained and moderately to strongly magnetic.

A large gabbro mass is located 200' to 400' to the east and

west of the diabase dyke on line 28+00 S between 00+00 and 8+00 E.

The outer limits of this body is unknown. The gabbro is medium

grained, dark green, massive, weakly magnetic and locally dioritic.

Minor granodiorite intrusives are located along lines 20+00 S

and 28+00 S to the west of a diabase dyke. The granodiorites are

black and white, biotite * hornblende * feldspar * quartz, massive

to schistose, medium grained intrusives.

6.2.4 Structure

The volcanics and sediments strike 1803 to 215 : Az in the

western part of the property and are interpreted from the magnetic

and VLF-EM results to strike 120" Az in the eastern claim block.

The sedimentary rocks are steeply dipping at 80 3 to 85 : to the east

Page 12

and west. The pillow lavas indicate stratigraphic tops to the

east. The volcanics and sediments probably are folded synclinally

with a fold axis striking 075: Az.

Two shear directions were noted during the survey. The first

is located to the west of the diabase dyke on line 28+00 S where

narrow shears zones strike ISO 3 Az and dip 80 : to the east. Blue-

white, I" to 18" wide, quartz ladder veins are associated with

these shear zones. The second set of shears strikes 295 : Az and

dips 80 ; to the north as seen at 24 + 00 S, 14 + 00 W. These shear

zones contain graphitic, pyritic, banded white quartz veins.

6.2.5 Mineralization

A total of 24 grab samples were collected during the mapping

and prospecting surveys. Sample locations are shown on Map I and

the results and sample descriptions are listed in Table 2.

Siliceous sulphide - rich sediments and volcaniclastic rocks

were found on line 12+00 S at 8+00 W to 12+00 W, 20-00 S at 21+00

W and 26 + 00 S at 10 + 50 W to 14 + 00 W. The sulphides consist of

trace to 5%, finely disseminated to wispy 0.1" wide pyrrhotite

lenses and trace to 2% finely disseminated pyrite. Samples of the

sulphide mineralization returned geochemically anomalous nickel

assays of up to 503 ppm Ni.

Sample 13596 from the graphitic, pyritic shear zone at 26+00

S, 14+00 W assayed 327 ppm Cu, 232 ppm Ni and 425 ppm Zn.

The pyritic carbonaceous argillite xenoliths, located along

line 28+00 S, assayed up to 127 ppm Cu, 197 ppm Ni and 173 ppm Zn.

All samples, including samples of the blue-white quartz veins,

assayed Nil to trace gold.

Page 13

6.2.6 Whole Rock Analysis

Whole rock analyses were completed on four representative

samples of the fine grained to coarse grained volcaniclastic

sediments. The results show these rocks to be alumina-rich and

silica-poor. See report no. M 2691 on following page for the

complete whole rock analyses results.

Page 14

Table 2

Grab Sample Descriptions

Sample No.

889018890288903889041358713588

13589135901359113592138931359413595

13596135971359813599136005057505850595060506150625063

Rock Type

Volcaniclastic sediment Fine grained sediment Fine grained sediment Blue-white quartz vein Blue quartz ladder veins Finely laminated graphitic argilliteGraphitic argillite xenolith Fine grained sediment Finely laminated sediment Siliceous biotitic sediment Finely laminated sediment Dacitic breccia, chloritic Siliceous, sericitic, finely laminated sediment Ribbon graphitic quartz vein White quartz vein Volcaniclastic tuff Siliceous, biotitic sediment Siliceous sediment

laminated sedimentvolcaniclasticsediment

sediment sediment

SiiiceousSiliceousSiliceousVolcaniclasticVolcaniclasticSiliceous laminated sediment Biotite hornblende schist

Mineralization

1^ py, tr po 2-3% po, J.% py I-2% po, tr py tr py tr py tr py

tr py, sptr py, l% magtr po, py<l.% p o, tr magtr po, pyno sulphidesi-2% po, tr py

l^fe py, tr cptr py, poi*fc pol*fc pol\ po, tr py2% po, l% pyS-5% po, tr pyl-2% po, < I* pyS-5% po, tr spl* py, tr po25% pyno sulphides

Note l Sample locations are shown on geology Map l

Note 2 Assay results are listed on attached assay certificates.

Page 15

Established 1928

Swastika LaboratoriesA Division of Assayers Corporation Ltd.

Assaying - Consulting - Representation

Geochemical Analysis Certificate 3W-1868-RG1

Company: W.R. BENHAM GEOLOGICAL SERVICES Date: JUN-28-93Project:Ann:

We hereby certify the following Geochemical Analysis of 4 ROCK samples submitted JUN-24-93 by .

Sample Au Au Ag Cu Ni Pb Zn Number PPB PPB PPM PPM PPM PPM PPM

88901 NIL 3 0.1 83 160 38 10688902 NIL 0.1 86 151 4 10088903 NIL 0.1 81 132 5 8788904 NIL

Certified by

P.O. Box 10, Swastika, Ontario POK1TO Telephone (705) 642-3244. FAX (705)642-3300

Swastika LaboratoriesA Dmskm of TSL l ASSAYERS INC.

Assaying - Consulting - Representation

Assqy Certificate

W-R.BENHAM GEOLOGICAL SERVICES

3W-2080-RA1

AUG-26-93

We hereby certify the following Assay of 22 ROCK samples submitted JUL-26-93 by.

Sanple Natter5057 5058 5059 5060 50615062 5063 5064 13587 1358813589 13590 13591 13592 1359313594 13595 13596 13597 1359813599 13600

Au An PFB PPB

7 10 14 17 14 1010 7 10 34 7 103 10

NIL 3 33 10 3 3 37 3

Oi PIM98 79 77 94 11784 73 127

52144 76 105 96 8991 66

327

7476 82

Ni PIM144 116 226 257 158213 84

248

45197 63 456 503 448291 379 232

382301 140

Zn WAPIM Ik93 75 49 86 91117 31 34

105173 28 48 19 2247 100 425

6647 49

Pt Pd PPB PPB

-CIO 15

CIO 10

Certified by.

P.O. Box 10. Swastika. Ontario POK1TO Telephone (705)642-3244 FAX (705)642-3300

W.R. BENHAM GEOLOGICAL SERVICES

3W-2

0BO-

RA1

TSL/ASSAYEI

laboratories

1270 FEU8TER DRIVE, UNIT 3 MII8I8SAUGA.ONTARIO

L4W-1A4

PHONI U

t (416)625-1544

FAX #1 (416)206-0513

I.C.A.P.

WHOLE ROCK ANALYSIS

Lit

hium

mta

Bo

rtt*

F

usio

n

REP

OR

T N

e.

:

Pag*

N

o.

i l

of l

Fil

*

No.

t

AU

04R

A

Dlt

*

: A

UO

-01-

1993

SAM

PLE

#

8102

A

1203

-

P*2

03

5058

5063

1359

0

1359

3

49.5

2

15

.38

53.5

0

14

.10

50.1

4

13.7

5

52

.72

13.4

0

11.1

1

10.2

7

11.6

510

.80

8.9

5,,

.41

Nc2

0

2.5

1

2.8

0

3.0

9:

K20

0.6

8

0.20

:' MnO

P

205

0.7

4*^1

0:2

0

0.7

9';'

;^ 0

/23'

0.10

-

0.1

2,

B*'.

PPB

325

220

. 51

100

sr :

: -

ppm

.

126'

"".v

154

-'123

;.~ .

77 .

-,::'

ir*

;

PPM s

64' 6I 65 47

Y PPm 16 18 18 10

"o PPB

" " 41,

40 *0 42

LOI

ft 3.50

1.23

1.25

0.45

TOTAL

' *

;.-

. ' ~

97.6

4

98.9

997

.61

97.70

fes"'"^

'u

TS

L/9

3SI

GN

ED

:

6.3 Magnetometer Survey

The contoured magnetic results are plotted on Map 2 at a scale

of I" = 200'. The anomalies of interest are labelled A to G.

The magnetic patterns are complicated by the northerly

striking strongly magnetic diabase dykes which intrude pyrrhotite -

bearing volcanics and sediments. The diabase outcrops produce

magnetic dipole effects along their contacts which usually mark the

edges of the prominent outcrop ridges.

In the western part of the grid, 50 to 250 foot wide, 500 to

2500 gamma, linear magnetic anomalies (A to E) have a predominant

strike of 030' Az. These anomalies are interpreted to be due to

disseminated to massive pyrrhotite zones.

Anomaly F is 100 to 1200 feet wide and at least 2400 feet

long. This 1000 to 3500 gamma magnetic anomaly has a linear

southern contact and a convex northern boundary, i.e. a half moon

shape. It may be due to a northerly dipping disseminated to

massive pyrrhotite lens, a buried magnetic gabbroic body or

possibly an irregular shaped kimberlite pipe(?). There is no

outcrop in the area of this anomaly. The weakly anomalous eastern

strike extensions of VLF-EM anomalies D and E' appear to be

associated with this magnetic anomaly.

Anomaly G is poorly defined because of the widely spaced grid

lines. This 2000 foot diameter, roughly circular, 100 to 450 gamma

anomaly is centred on a 700 foot circular bog at 16+00 S on line

8+00 E. The source of this anomaly may be a gabbroic stock or a

kimberlite pipe(?).

Page 19

6.4 VLF-EM Survey

The VLF-EM dip angles are shown in profile on Map 3 and the

Fraser Filtered dip angles are contoured on Map 4. The scale of

both maps is l" = 200".

The VLF-EM results show seven subparailei weakly conductive

horizons, labelled A to K on the maps, which strike 010 : to 030 3 Az

in the west and I20 : to 135" Az in the east. Contouring of the

results in the west is influenced by northerly striking diabase

dykes which interrupt the continuity of the conductivity along the

mineralised horizons. The strongest conductor F* is located at

13 + 00 W on line 28+00 S. Disseminated and narrow l" to 2" wide

bands of semi massive pyrrhotite and pyrite were found along strike

of this anomaly. No outcrop was located in the vicinity of the

interpreted northern strike extension of the conductor F-F* at

18+50 W on line 16+00 S.

A moderately strong conductor E 1 is located at 10+00 S on line

8+00 E. This conductor is flanked to the south by a strong 900

gamma magnetic anomaly. There is no outcrop in this area.

At 20+00 S on baseline 0+00, a moderately strong conductor was

detected, but again no outcrop was found.

The VLF-EM anomalies in the eastern portion of the grid are

very weak possibly due to the depth of overburden.

7.0 CONCLUSIONS and RECOMMENDATIOHS

Previous drilling in the area reported sulphide mineralization

associated with rhyolite lapilli tuffs; however, the recently

completed mapping found the fragmental rocks which are exposed in

Page 20

outcrop to be volcaniclastic sediments.

Samples of the pyrrhotite-rich sediments returned geo

chemical ly anomalous nickel contents. Although no ultramafic rocks

were found in outcrop, previous drilling reported intersecting talc

* carbonate * serpentinite rocks. The geological setting of the

Wool ley Lake claims may be similar to the geology of the Redstone

Nickel Deposit located in Eldorado Township to the south of Timmins

(Fyon, J.A. et al, pgs. 45 to 49).

Some unexplained VLF-EM and magnetic anomalies were located by

the geophysical surveys. Of particular interest are magnetic

anomalies B-B', C-C', F and G and electromagnetic anomalies F-F',

E-E', C', A and G.

The Wool ley Lake claims have some potential for the discovery

of nickel * copper disseminated to massive sulphide deposits

associated with komatiitic volcanics or gabbroic intrusives. Also

the magnetic results indicate that there may be some potential for

the discovery of kimberlite pipes associated with faults intruded

by the diabase dykes. These faults are located within the

TirTi.iskaming lake structural zone.

A horizonal loop electromagnetic survey is recommended to

further investigate the VLF-EM and magnetic anomalies on lines 8-rCO

S to 32+00 S and 0+00 to 32+00 E. Depending on the results of the

horizontal loop survey, induced polarization survey of lines 8+00

E to 24+00 E also should be considered to search for disseminated

versus massive sulphide basemetal deposits.

Wayne Benham

September 10, 1993

Page 21

8.0 References

1. Kirkland Lake Area Assessment Files.

2. Map P.153, Edwards Township, Scale: i" = 1/4 mile,

?. M. Ginn, O.D.M., 1961.

3. Map 2205, Timmins-Kirkland Lake Geological Compilation

Series, Scale: 1: = 4 miles, D.R. Pyke, O.D.M., 1973.

4. Map P.853, Kirkland Lake Data Series,

Scale: l" = 1/4 mile, H.L. Lovell, O.D.M., 1973.

5. Map 81240, Geophysical/Geochemical Series, Airborne

Electromagnetic and Total Intensity Magnetic Survey,

Detour-Burntbush-Abitibi Area, Pyne, Mortimer,

Aurora and Edwards Townships, Scale: 1:20000,

by Geoterrex Ltd. for the O.G.S., 1989.

6. Open File 2161, Geological Survey of Canada, Geology

and Ore Deposits of the Timmins District, Ontario,

Field Trip 6, Edited by J.A. Fyon et al.

Page 22

Append!x I

Geophysical Instrument Specifications

and

Geophysical Technical Data

CRONE GEOPHYSICS LIMITED3607 WOLFEDALE ROAD, MISSISSAUGA, ONTARIO, CANADA, L5C1V8

Phone: (416) 270-0096

Cable: CRONGEO, TORONTO

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.

SPECIFICATIONS

SOURCE OF PRIMARY FIELD: VLF Communication Stations 12 to 24K hz

NUMBER OF STATIONS: 7 switch selectable

STATIONS AVAILABLE: The seven stations my be selected from:

Code Station ft Location FrequencyCM Cutler, Maine.............................................................. .17.8 KHz

SW Seattle, Washington........................................................ .18.6 KHz

AM Annapolis, Maryland ....................................................... .21.4 KHz

H Laulualei, Hawaii .......................................................... .23.4 KHz

BOF Bordeaux, France .......................................................... .15.1 KHz

E Rugby, England............................................................ .16.0 KHz

MS Gorki, Russia.............................................................. .17.1 KHz

OD Odessa (Black Sea)......................................................... .15.6 KHz

NC Australia, N.W.C. ......................................................... .22.3 KHz

YJ Yosamai, Japan............................................................ .17.4 KHz

HN Hegaland, Norway ......................................................... .17.6 KHz

TJ Tokyo, Japan .............................................................. .20.0 KHz

BA Buenos Aires .............................................................. .23.6 KHz

CHECK THAT STATION IS TRANSMITTING: Audible signal from speaker.

PARAMETERS MEASURED:

(1) DIP ANGLE in degrees of the magnetic field component, from the "horizontal, of the major axis of the polarization ellipse. Detected by a minimum on the field strength meter and read from an inclinometer with a range of 90* and an accuracy of Vi 0 .

(2) FIELD STRENGTH (total or horizontal) of the magnetic component of the VLF field, (amplitude of the major axis of the polarization ellipse). Measured as a percent of normal field strength established at a base station. Accuracy 2*34* dependent on signal. Meter has two ranges: O 300^o and O 600*^.

(3) OUT-OF-PHASE component of the magnetic field, perpendicular in direction to the resultant field, as a percent of normal field strnegth, (amplitude of the minor axis of the polarization ellipse). This is the minimum reading of the Field Strength meter obtained when measuring the dip angle. Accuracy 1207o.

OPERATING TEMPERATURE RANGE: -30e C (-20"F) to |50 0 C (120'F)

DIMENSIONS AND WEIGHT: 9 x 19 x 27cm 2.7Kg (6 Ib)

SHIPPING: Instrument with foam lined wooden case,shipping wt. G.OKg (13 Ib)

BATTERIES: 2 of 9 volt Eveready 216Average life expectancy 20 hours for continuous operation

UNITS AVAILABLE ON A RENTAL OR PURCHASE BASIS. CONTRACT SERVICES AVAILABLE FOR FIELD SURVEYS.

SPECIFICATIONS

Ronge:

Accuracy:

Sens!tlvlty:

Gradient Tolerance:\

Power:

Power Consumption:

Polarizing Power:

-GROUND MAGNETOMETER

MODEL CM-122

20,000 to 39,339 In 12 ranges

1 y through operating temperature range

1 T

600 y/ft. * '

12-"D M cells

< 50 Joules (Wsec) per" reading

0.8 A 8 13.5 V for 1.5 sec". (3 second

Number of Readings with l Battery Set:

Frequency of Readings:

Controls:

Output:

Indicators:

cycle)

0.8 A e 13.5 V for 3 sec. (6 second cycle)

2,OOO - 10,000 depending on type - of batteries

l every 3 seconds l every 6 seconds

Pushbutton switchRange Selection switch - Slide switchfor 3 and 6 sec. located on P/C Board

5 digit Incandescent filament . readout

LEO pointLo'ck Indicator - last three digitsof the display blanked off whenphaselock not achievedSegment Function Indicator -allsegments light up to permit visualInspection of the display function :

I

f

Mechanical:

Instrument: Dimensions - 7" X 3.5" X 11" .(18 cm X 9 cm X 28 cm)

Weight - 8 Ibs (3.6 kg), including .batteriesm *

Sensor: Omnidirectional noise cancellingtoroidal sensing head

Dimensions - k 7/8" (12 cm) diameter- 4 3/8" (II cm) height

- 3 Ibs (1.4 kg)Weight

Ambient Conditions:

Envlronnental

Operating Temperature Range -

-40 0 F to 131 "f C-40"C to 55"C)

Relative Humidity - O to 100?

Instrument and sensor case made of high impact plastic

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of Stations———Station interval VHProfile -A VI* /"-SO0

/Oo' M o-g S"C/ -.Number of Readings VLf '

JLine

Contour .A .J

- /O .

CJ

w•z c

Instrument. i no g V P roTt n Pi CtCt TieT&m *"t C V" . ~ /Z2-

Accuracy — Scale constant. Diurnal correction method. Base Station check-in interval (hours)———Z.

* -

Base Station location and value.l f t JJL UE&T ^A^g. o T 'TTi t. O,

, MA.OL.

,je s -f-di'o* s -k r c.l*SeJ J oof s

T ^f* JCKTM c^'rt. ai SM.^// g-rc^.

Inctniment L! V Q r* t^ \//.^-

Coil configuration .Coil separation ——i hAccuracy.Method:Frequency.

f

S] Fixed transmitter Q Shoot back O In line O Parallel linek Ut, j .SW44k- 6Ja* lunula n 78.6 fe A/2.

(specify V.LF. nmtion) *Parameters measured ftif* H i^te. o^-lil*, ma^ftdfc. ^i'e(c/ eompon.c^- ^nx- 4i\e, riov-l^oi.-(Q.(

id

Instrument.Scale constant.Corrections made.

Base station value and location.

Elevation accuracy.

InstrumentMethod D Time Domain r~l Frequency Domain

INDUCEF OLARIZATIO

Parameters — On time

s-. Off timeEH Z? — Delay time

^b — Integration time

td Pnu/erCd

Electrode array . .Electrode spacingTYIM* nf ••lTtr~l''

Frequency

Rance

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT. SURFACE fit MINING RIGHTS ,,—..^. ~, SURFACE RIGHTS ONLY.—-L.—.-—

" . MINING RIGHTS ONLY ..._...,.__.LEASE SURFACE b M INING RIGHTS....,——

" .SURFACE RIGHTS ONLY.__.,.—,.~__.__ H " . MINING RIGHTS ONLY...—————....-,~ H

LICENCE OF OCCUPATION .___ ..__...,™__..__. T ORDER IN COUNCIL - —......,.- .—-...........—.. OC

RESERVATION .......m__ ^ — . ^ .-......,CANCELLED __.........,,.. ^,............SAND 4 GRAVEL __.™.___......,..—--.

NOTE. MlNINU 8IQMTS IN PARCELS PATENTED PRIOR TO MAYIfilJ VESTED IN ORIGINAL PATENTEE 0V THfc PUBLIC LANUS ACT H80 IW'O, CHAP MO. 86C. O. SUMiC 1

NOTES4OO' surface right* rtstrvotion along th* ihorot of all la k* t and riv*rt.

ANNULMENT CERTIFICATE

The tubdimion of thi* Township into Lots and ConcMiions is wholly Annulled on 29 May, 1963

Lands below contour levels 826* Q 88l' covered by L.O. 8674.

MORTIMER V OWNSH1P

II90I8I

Application ptndlng tor Surfoct Right* undtr Public Land* Act

U86863

COPY OF THIS MYLAR ARCHlVr.D KEb. 05/93TEEFY TOWNSHIP

4ZA166Ebbi'60P83-ba8 EDWARDS

CL Xen•z.o

LEGEMO

HIGHWAY AND ROUTE No

OTHER ROADS

THAILS

SURVEYED LINtSTOWNSHIPS, BASELINES ETCLOTS, MINING CLAIMS PAfiCFLS, ETC

UNSURVfcYtD LINESLOT LINbS -PARCLI BOUNDARYMINING CLAIMS ETC -

RAILWAY ANU RIGHT OF WAY

UTILITY LINES

NON PERENNIAL STREAM

fLOOniNGOri FtOOniNG RIGHTS t;

SUKOIVISION OR COMHOSITL Pt AN

RESERVATIONS

ORIGINAL SHOHt LINE

MAnSH OH MUSKEG

MINtS

MONUMENTf O

NOTICE OF FORESTRY ACTIVITYTHIS TOWNSHIP / AREA F ALLS WITHIN THL ,——. IROQUOIS FALLS MANAGF.MCNT UNITAND" MA Y "BE~S"UB jfc~f" TO "FORE STRY'OI^F"^AT JON sTHE MNR UNIT F OWF5TER TOR T HIS A HtCA C AN BL CONTACTED AT. P O BOX 730

THlf^D AV[

SCALE: 1 INCH - 40 CHAINS

l QUO .'OOU MUM

O JOO MtTHtj

l OOOl 1 KM) (V

ACRES

40

HECTARES ~~1

THE INFORMATION THAT APPEARS ON THIS MAP MAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT C 1 '/ ^NTLtU THObb WISHING TO STAKE MIN ING CLAIMS SHOULD CON

WITH THE MINING F1F.CORUEH, MINISTRY OH NOMTHC-RN OEVLI OPMtNT AND MINES, hOH AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HFREON

TOWNSHIP OF

EDWARDSDISTRICT

COCHRANE

MINING DIVISIONLARDER LAKE

Ministryof Ministry ofNatural Nor'hern DevelopmerResources and Mines

Ontario

0*u ae Plan No

L II87II4L 87 3

Base Station 58,538 lOOOFeet South

Magnetic Dec) motion l O 0 West

LEGEND

O Gamma C ontour Interval

5OO " " "

1000 " " "

2000

3000 " " "

l Magnetic Anomaly

A Base Station

Instrument Proton Ground Magnetometer Barringer Model GM-122

Base Level 58,OOOv-

SCALE:

200 2OO 4OO

FEET

NTS : 42 A /19

WOOLLEY LAKE CLAIMS

EDWARDS TWP ONTARIO

MAGNETOMETER SURVEY

Sept (993 W. BENHAM MAP: 2 ___________l____________l_________

WOOL LEY

L AK E

L II87II4LM87II3

42A15SE0015OP9M2B EDWARDS

Magnetic Declination !0 0 West

LEGEND

30

40

Contour Interval

il M

l* II

II II

South Lines at I20 a Az

Surveyed Using- Annapolis Maryland, 2I 4 KHz

East Lines at 030 0 AzSurveyed Using Sea tie Washington, IS 6 KHz

Instrument Crone Radem VLF-EM Unit

SCALE:

200 200 4OO

FEET

NTS : 42 A/IS

WOOLLEY LAKE CLAIMSEDWARDS TWP ONTARIO

VLF- EM SURVEY FRASER FILTER

Sept I993 W. BEMHAM MAP: 4 J____________l_______

WOOL LEY

Magnetic Declination 10 a West

LEGEND

South Lines at 120* A z Surveyed Using Annapolis, Maryland 21-4 KHz

East Lines at 0300 Az Surveyed Using Seatle, Washington 86 KHz

nstrument: Crone Radem VLF-EM Unit

SCALE

LII87II3 L l 87114NTS : 42 A/15

WOOLLEY LAKE CLAIMS

EDWARDS TWP O NTARIO

VLF-EM SURVEY PROFILES

Sept. 1993 W BEMHAM MAP: 3 l t

WOOL LEY

LAKE

LII87II3 L II87II4

i

LEGEND

Diabase

Gabbro

Diorite

Granodiorite

Biotite Hornblende Schist

Argillite

Siliceous, Sulphide- Rich Sediments

Graywacke

Volcaniclastic Sediments

a, Fine Grained b, Coarse Grained

MaftC Volcanics

p, Pillowed Basalts

c h Chloriticfol Foliatedgf Graphiticmag Magneticp Pillowedpbx Pillow Breccia

po Pyrrhotitep y Pyrite

f q v Quartz Veins

Pillows

Foliation

Bedding

Fault

Claim post, located

Tractor Road

Gravel Road

Outcrop

Geological Contact

Grab Sample Location

Fold Axis- Syncline

Magnetic D eclination 1 0 0 west

SCALE

2DQ

FEET

NTS : 42 A/15

WOOLLEY LAKE CLAIMS

EDWARDS TWP ONTARIO

GEOLOGY MAP

Sept 1993 W BENHAM MAP J_____________l