CHESTER J. KURYL.IW. M.Sc.. P.ENG.

46 IMCAU, DR. DRYDEN, ONTARIO fm *BT

S2C10NWD041 2 16122 HALKIRK 010

PHONE 807-223-6080

g. 16122

REPORT

ON

ARMSTRONG - COPPER PROSPECT

HALKIRK TWP. RAINY LAKE AREA OF ONTARIO

EM - 17 HORIZONTAL LOOP

ELECTRO MAGNETIC

GROUND SURVEY

FEBRUARY 20, 1995 CHESTER J. KURYLIW

- 2 -52C10NWOO41 2.16122 HALKIRK 01OC

TABLE OF CONTENTS

Project Location

Location Maps

Access to Project Site

Regional Geology and Mineralization

Local Geology and Interpretations

Instrument. Unit and Method

Results of the Survey

Conelus ions

Recoinmendat ions

Cert ificate

Plan of Electromagnetic Survey Scale l" = 200

- 3 -

(a) PROJECT LOCATION

PINE POINT COPPER PROSPECT: Halkirk Twp., Rainy Lake, Ont.

Located on Claim Map G-3808 of Halkirk and Farrington Twps.

N.T.S. C-ll, Latitude 480 38N., Longitude 93*01* W.

(b) LOCATION MAPS;

Claim Map, Halkirk fc Farrington Twps. (scale: l" = 1/2 mile)

Ontario Geology Survey Map (scale: l" - 340 Kms)

Road Map and Geology (scale: l" = 25 Kms)

(c) ACCESS TO PROJECT SITE:

There is a good access to the Property from Dryden. 151 Kms to

the South from Dryden along Hwy. 502 to the junction of

Hwy.ll, then 5 Kms East along Hwy 11 to Bears Pass, then over

ice by Ski-doo for 5 Kms. to the drill site.

(d) DESCRIPTION OF PROPERTY: PINE POINT COPPER. HALKIRK TWP.

CI. Blk.K-U50126, K-996076, K-996077, K-996078, K-996079,

K-996080, K-996081, K-996082, K-996083, K-996084, K-996085,

K-975470, K-975471, K-975472. A total of 14 Claims (25 Claim

units).

Owned 90% by George Armstrong, and 10/6 by Chester J. Kuryliw.

(e) DESCRIPTION OF REGIONAL AND LOCAL GEOLOGY;

REGIONAL GEOLOGY:

The Area is located in the Precambrian Wabigoon sub-province.

This Area embraces two major East-North-East trending

Ant i forms, separated by the Swell Bay steep sided Svnclinal

trough.

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SCALE : l""25 Km. PLAN OP ACCESS ROUTES TO ARMSTRONG DRILLING 1995

bc-I-S Phanerozoic ProterozoicGranitoid rocks: piutons. old sialic crust

and unspecified gneisses ___ Metasedimentary and gneissic rocks55j**i Metavolcanic-metasedimentary

greenstone belts' Subprovince boundary

*v

Sketch\maD of tne\Si^xf;or Province showing major lithologic ana suoprovincs boundaries.

Ontario Geological Survey Miscellaneous Paper 132

1986

——— A3N3T SONG -JOHNSON GOLD. STURGEON LAKE

ARK3TRONG-KURYLIW NICKEL PROSPECT. RAINY LAKE ARMSTRONG COPPER PROSPECT, RAINY LAKE

- 4 -

REGIONAL GEOLOGY CONTINUED:

In Cross-Section you have a "M" shaped structure over six

miles across. The South Antiform is intruded by the Bad

Vermillion Lake Gabbro-Anorthos i te Complex. The North

Antiform (Dome) is intruded by the Nickel Lake Gabbro-N'or i t e

Complex. A strong circular magnetic high about 1/2 mile

across near the trace of the Swell Bay Synclinal Axis is

interpreted to be a Peridotite? plug, historically related to

the Antiform basic to ultrabasic intrusions.

An interesting feature of the Bad Vermillion Lake Gabbro-

anorthosite Complex is, the North and South flanks are

bordered by Granophyric "differentiates".

The area of Mineralization falls into a Single Major

structural feature and an epoch of related Major Basic to

Ultrabasic intrusions. Generalizations using the "Single

Chapter of Geologic History" as its basis, leads to some

logical conclusions about existing and known mineral

occurrences and projections towards undiscovered deposits.

MINERALIZATION;

The Nickel Lake-Mine Centre - Rainy Lake AREA has a great

variety of Base Metal and Gold occurrences. What this writer

finds very significant, is that specific metals fall into

"ZONES".

- 5 -

MINERALIZATION CONTINUED:

These Zones are spatially related to: Precambrian

stratigraphy: the antiforms-synclinal structure of the BIG

"M": the Basic Antiform intrusions.

For example:

A Gold Zone is located in the Granophyric differentiate rocks

that lie on the Southern Flank of the Southerly Bad Vermillion

Lake Antiform.

A Copper-Zinc Zone is located in a Basic Lava Formation that

lies immediately on the North Flank of the Eaci Vermillion Lake

Ant i form.

A Zinc Zone is located in a Rhyolitic Formation with Quartz-

porphyry on the Northerly Flank of the Bad Vermillion Lake

Antiform. This Rhyolitic Formation is located about 4000 Ft.

North of the anorthositic intrusion. The Zinc Mineralization

has widths of over 100 Ft. in places. The Zinc Mineralization

has been traced intermittently over a length of over 25 Miles.

A Copper-Nickel Zone of occurrences is located in or near the

Gabbro-Norite intrusion along the Southern Flank of the North

Rice Lake Dome.

A Nickel-Copper? deposit may occur in the Swell Bay Syncline

Peridotite? intrusion, as indicated by the strong Magnetic

high anomaly and also the strong Air E-M Conductors.

- 6 -

LOCAL GEOLOGY; THE PINE POINT COPPER PROSPECT

This Group is also known as the "Pine Point Group.

This is essentially an untested area the exhibits several

favourable features. A mapped alteration Zone occurs a Pine

Point that is comparable to the alteration Zone which also

occurs to the South of the "West Bay and Wind Bay" Zones.

Secondly, the Ontario G.S. Airborne E.M. Survey, 1980, picked

up several "one line" Conductors in a Basic Lava Fm. and also

in Spherulitic Rhyolite Fm. and in "QE Rhyolite Fm. The "one

line" Conductors in the Basic Lava may indicate sulphide

deposits mineralized the Cu-Zn?. The one or two line

Conductors provide a higher priority target for Base metal

mineral deposits compared to the "Long Formational

Conductors." The small Port Arthur Mines Copper deposits some

25 miles to the E-N-E, occurs in the same Basic Volcanic

Member of the stratigraphic section, as do the Pine Point E-M

Conductors.

Several short drill holes are needed to test these Conductors

subsequent to a detailed Lake Ice Ground E-M Survey and a

ground Magnetic Survey.

Accompanying this Local Geology are:

A Geologic Map of the Pine Point Area (Scale l" = 1/4 Mile)

includes line Grid and Air E-M

Input Anomalies.

- 7 -

LOCAL GEOLOGY; THE PINE POINT COPPER PROSPECT CONTINUED;

An M.N.R. Map of the Port Arthur

Copper Mine (Scale l" ^ 50 Ft.).

Geology and Description

An O.G.S. Airborne Electromagnetic

Survey Map 80499 (Scale l" = 1/4 Mile)

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Zn—bearing Bedded Tuff Rhyolite with Stringer Sulfides

Mafic Breccia—Vesicular*

Rhyolite with Chlorite Seams

r.s&ZzZ^?-; Mafic Row•^•-•-i t^^v-,^-^ -

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100 ft

STOP 3 - PORT ARTHUR COPPER

FROM 1991 M.N.R. FIELD TRIP (C. BLACKBURN)

Figure 7. Sketch nap of geology at Port Arthur Copper Mine

105NOTE t THE STRATIGRAPHIC SEQUENCE SHOWN HERE IS THE SAKE

AS OCCURS AT THE ARMSTRONG PINE POINT PROSPECT. HO Km. TO THE W-3-W

807-223-60*0

CHESTER J. KURYLIW. M.Sc.. CONSULTING GBOI.OGISCT

16 INGALL DR.DRYitKN. ONTARIO I"*N 3HT

LOCAL GEOLCQY (con't)

* Stop 3; The Port Arthur Copper Mine

The open cut was developed during the winter 1916-17 and later in 1917 a 30 m deep shaft with a first level drift 65 m long were developed. In total, "several" carloads of ore grading 3 to S.5% Cu were shipped to Trail B.C.. The property was further developed by a shallow drill program in 1956 by Stratmat Ltd. and a complex distribution of copper and zinc has been interpreted from the results of that program (Fig. 3b and Poulsen-, 1984). The recent stripping has been performed by Minnova Ltd., Thunder Bay who kindly provided the accompanying sketch (Pig. 7) as -a guide to the many features in the outcrop.

The southernmost exposure is that of a medium grained metadiabase that cuts the altered and mineralized zone. The overlying chloritized and sericitized intermediate to--mafi.c. amygdaloidal flows and breccias contain variable amounts of spnaiefTte, cnaicopyrite and pyrite with quartz and iron carbonate as^ evidenced by Jth'e ^arxaEI e Intensity of rusty "wea'tHering .

"Representative samples orTlEhe "mineralized materiaT may~sTf:QT~ be found locally in the dump to the west. The mineralized zone is capped to the north by a narrow zone of banded silicified and sericitized rock with local pyrite seams. This is overlain, in turn, by successive spherulitic rhyolite flows and mafic amygdaloidal breccias with local vague pillow forms and which locally are cut by mafic dykes and quartz veins. Massive sulfides have been intersected in drilling at the top of the northernmost of the mafic units. This mafic unit is overlain by vesicular and amygdaloidal rhyolite containing stringer sulfide mineralization and capped by a 5 m thick sequence of carbonate- and sphalerite-bearing bedded tuffs or sediments. This unit appears to cap the hydrothermal alteration and mineralization in this area and is overlain by a substantial thickness of unaltered quartz-eye rhyolite.

* From Kenora J4.N.R. Fieldtrip (C. Blackburn)

Note, The Same Formation and Sequence of Members occurs at the Port Arthur Copper, as Mapped by Minnova at the Pine Point Copper prospect. (C.J.Kuryliw)

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IBSTHDruatf UMU AND

The instrument used was an E-M 17 Electromagnetic

survey unit, the horizontal loop mode of operation wa*. used at

300 foot coil separation - ';

The instrument is designed and manufactured by Geonics

Ltd., 2 Thorncliffe Park Drive, Toronto, Canada.

Basic Principle

The basic principle behind E-M surveying is that

certain orebodies are electrically conductive, and can be

excited electrically by an "applied primary E-M field." The

orebody then produces a "secondary E-M field" which may be

- detected above ground. t- -s In the E-M 17 the primary field is produced by the

transmitting coil which is fed an oscillatory current by the

transmitter itself.

The secondary field, together with some primary field

coming directly from the transmitter, is picked up by the

receiving coil and is measured in the receiver console.

Because the secondary field is quite small compared

with the primary it is necessary to "buck out" the primary field

in the receiving coil before main Tig secondary field measurements.

This is done by means of the reference cable which carries some

of the primary signal directly into the receiver. This signal

also serves as a reference by which the secondary field can be

L resolved into its two components, one in-phase (real) and one

out-of phase (imaginary) with the primary, and compared with the

primary in amplitude. The relative strengths of the real and*

imaginary components are a guide to the conductivity-width product

of the buried conductor, which is usually related to the quantity

of conducting minerals present.

The strength of the secondary field increases as the

orebody gets larger or more conductive (higher metallic or

electrolytic content). The secondary field is weaker if the

orebody is deeper under the ground or if it is covered "by a layer

of absorbing material such as conductive clay or salt water. By

measuring the strength, character and distribution of the

f- secondary field on the ground surface, it is possible to locate U-

conductive orebodies and tell something about their size and nature.

Field Operation

Orientation and Separation. The En-1? is a two component

instrument (real and imaginary), also called in phase and out of

phase, as distinct from single-component instruments such as

those that measure dip angle only. This is an advantage as it

enables the user to discriminate more easily between different

types of conductors and to determine more accurately the depth

and shape. The primary field from the transmitter is bucked out

by the compensation circuit for a particular coil separation and

providing the coils are coplanar.

Choice of Coil Separation*

The depth of penetration increases with coil separation.

On the horizontal-loop mode used in this survey the limits of

depth penetration are in the order or 2/3 the coil separation,

i.e. for conductors buried with 200 feet of overburden a 400

foot coil separation would be necessary to pick up the conductor.

The background effects of conductive overburden are greater at

larger coil separations. Accuracy with the HI-1? is still good

at a separation of 400 feet though the readings take a little

longer to determine, however, the automatic electronic readout

of the null on the EM-1? eliminates operator errors common to

determining nulls on broad angle nulls common to areas with

conductive overburden.

For steeply dipping conductive bodies the horizontal

or coplanar configuration results in stronger anomalies where

the conductor is buried at a depth of less than one half the

coil separation.

This QI-17 survey was carried out using a horizontal

coil separation of 300 feet over most of the area with some areas

covered at 500 foot coil separation. E-M readings were taken on

stations at 100 foot intervals along lines and the readings are

plotted on plans at the mid point between the coils.

Figures l, 2, 3a. *at 6, 8 are included (next) to

give rule-of-thumb procedures an interpretation.

gote;Such rule-of-thumb procedures should be used with

caution especially when conductive overburden is present.

The Effects of Ground Conductivity;

Ground conductivity usually affects the imaginary

component more than the real. They can produce either positive

or negative effects most commonly negative in the imaginary

and positive in the real component. The profiles produced by

conductive overburden are commonly broad and "wavy" without

distinct shoulders. The anomalies produced are larger at the

larger coil separations and they also tend to be negative at the

larger coil separations.

The Effects of Magnetite;

Magnetite in sufficient quantities at least 3O# of

volume can cause reversal of the real component with little or

no anomaly in the imaginary component. If such a body ia also

/r

Connectinq \ l . \coble X '

\Eddy currents excited In orebody

Primary field— -*- — — --- Secondary field

PRINCIPLE OF EM SURVEYING

FIGURE l

a.

b.

c.

d.

e.

-200-

-200-

V \

Rlght

Right

Wrong

Wrongx V.

Wrong

Imaginary plane

ORIENTATION AND SEPARATION EFFECTS

FIGURE 2

-soy.-*-VARIATION IN ANOMALY

WITH DEPTH

COPLANAR SYSTEM FIGURE 3a

•f 30%-r

•1-207*--

I070--

-107.- -

-307o- -

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-507.J-

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VARIATION IN ANOMALY WITH DIP

COPLANAR SYSTEM FIGURE 4 o

IO+

:vVLF (EM-16)

5-4-

104

19-1-

^.*—v

x;----/ \y

V-,

\s..Real Component Imaginary Component

HORIZONTAL LOOP (EM-17)

X - 200 ft.

300 ft.

^'^*^fcl i 2 400 ft.

200ft.

EM-17 PROFILES, LOUVICOURT TWP. QUEBEC

FIGURE 6

AXIS

FINDING CONDUCTOR LIMITS

FIGURE 8

- 8 -

RESULTS OF THE SURVEY

Several E.M. conductors were located in the survey. The

conductors range from low to medium in intensity and most

conductors are only a few hundred feet in length. The E.M.

profiles indicate a northerly dip of about 60*.

The stronger conductors located by this survey correlate well

with M.N.R. Air input E.M. surveys with one major exception.

There is an error of about 100 meters in the M.K.R. plot of

the conductors related to topographic features. The E-W plot

appears to be accurate but the N-S flight line plot is 100

meters too far south of topographic features.

CONDUCTOR "A"

This is a medium strength conductor about 400 ft. long that

dips at 50 - 60 Northwards. It is located at the basic

lava-spherul i tic rhyolite contact and it has an associated

magnetic high "shoulder" anomaly to the North that rises 3000

gammas above background. This magnetic "shoulder" extends for

about 300 ft. in length along tht conductor.

This conductor on line l i-W traces a classic In-Phase to Out-

Of-Phase profile over a good conductor.

This conductor "A" should be tested by a 175 ft. drill hole.

- 9 -

CONDUCTOR "B"

This conductor on line 10-W, 0+50S is a weak to medium

conductor of short length next to the fault 11-W.

CONDUCTOR "C"

This conductor on line 10-W occurs within the spherulitic

rhyolite and is strongest near the fault at 11-W. It is a

weak to medium strength conductor.

CONDUCTOR "D"

This is a strong conductor about 300 ft long within a fault

block, on line 10-W near the fault at 11-W. This conductor

shows a northerly dip of about 50*- 60*.

Conductors "B" * " C" should all be tested by one drill

hole, 300 Ft. Long. Conductor "D" should be tested by one

drill hole 175' long.

CONDUCTOR "E"

This conductor on line 0-W. 2-W and 4-W at 3-S is a medium to

strong conductor that occurs between the contact of

spherulitic rhyolite and quartz porphyry. The E.M. profits

indicate a 50* - 60* to the North. This conductor appears to

extend eastwards beyond this grid. This conductor should be

tested by one drill hole 175 Ft. long.

- 10 -

RESULTS OF THE SURVEY CONTINUED

CONDUCTOR "F"

This conductor appears to occur along the spherulitic rhyolite

basic lava contact. It trends at a 45* angle to the survey

lines giving profiles that appear to indicate a thicker

conductor than is the actual case. This is a medium strength

conductor that is strongest on line 4-W near the fault and it

weakens easterly at line O-W.

A 1"5 Ft. drill hole should be drilled along line 4-W to the South

to test "F".

CONDUCTOR "G"

This is a good one line conductor that occurs on line 10-W

near the fault at 11-W and it occurs at the gabbro-basic lava

contact .

CONDUCTOR "H"

On lines 14-W, l6-W and 18-W a weak conductor is located at

about 2+50S, this weak conductor is strongest on line 18-W.

This conductor may mark the northern contact of the

spherulitic rhyolite and quartz porphyry.

- 11 -

LOCAL GEOLOGY AND INTERPRETATIONS

Please refer to Plan of Geology Scale l" = 1 /4 mile.

The stratigraphic series on the Pine Point grid consists of a

gabbro from 16-S to the south end of the grid overlain by a

basic lava that is about 800 ft. thick. This basic lava

exhibits a flat magnetic relief and no E.M. conductors.

Overlying the basic lava is a spherulitic rhyolite member that

is about 500 ft. thick. It exhibits a scattering of local

magnetic-high anomalies most often near its contacts.

Electromagnetic conductors also occur near its North and South

contacts. It is significant that the intensity of the

conductors is more pronounced in proximity to the cross

cutting faults that occur at 5-W. 7-W. and 11-W.

It is also significant that the fault block along line 6-W is

barren of conductors but reinforces the location of strong

conductors to the East and West of the block as indicated by

high positive in-phase readings between the conductors on

e i ther s ide.

It is interpreted that the crosscutting faults served as

conduits to the mineralization in the conductors and

consequently indicate that the conductors trace sulphide

mineralization that was introduces and therefore increases the

possibilities that base metals occur with sulphides.

- 12 -

CONCLUSIONS;

The horizontal loop E.M. survey succeeded in locating and

defining the conductors indicated by the M.K.R. air input E.M.

survey. These conductors occur in a favourable known

environment for base metals mineralization. These conductors

represent high priority targets.

February 20, 1995 Chester J. Kuryliw

- 13 -

RECOMMENDATIONS

Five drill holes are recommended to test the conductors for

base metal mineralization.

Drill hole - 1. depth, 175 ft.

To test conductor "A"

Drill hole - 2. depth 175 ft.

To test conductors "E" and "F".

Drill hole - 3. depth 175 ft.

To test conductor "F".

Drill hole - 4. depth 300 ft.

To test conductors "B" and "C"

Total Drilling = 1000 Ft. 6 $21.00 per Ft S 21,000.00

February 20, 1995 Chester J. Kuryliw

CERTIFICATE

I, Chester J. Kuryliw of 1*6 Ingall Drive, Dryden, Ontario, do hereby certify that:

(1) I am a Professional Engineer and I am currently employed as a Consulting Geologist for several mining companies.

(2) I am a graduate of:The University of Manitoba B.Se. Degree, 1949 The University of Manitoba M.Se. Degree, 1966

(3) I am a registered Engineer of the Association of Professional Engineers of Ontario and also Manitoba. I am a fellow of the Geologic Association of Canada, also a member of the Canadian Institute of Mining and Metallurgy.

(A) I have practiced my profession for G-. arlv5 years, most of thoseyears at gold mines, during which tine l often planned, supervisednn-j -"^ir^cT^^ *ir. "ierc r "".'jrd exclorst^'^r.. d o vt^l , - J ~\ t ~.i. ard orO'J M r ' ;-'~.

(5) My Report is based upon My personal field supervision of the Magnetic and Ele c tromagnetic surveys and upon my personal plotting and evaluation of results obtained,

Feb. 20, 1995Chester J. Kuryliw, M.Se., P.Eng.

PHONE 807-223-6080

CHESTER J. KURYLJW. M.Sc.. P.ENG. CONSULTfNG CBOIXMSMTT

46 INGALL DR. DRYDEN. ONTARIO PON aB7

S2C10NW0041 2.16122 HALKIRK 020

REPORT

ON

ARMSTRONG - COPPER PROSPECT

HALKIRK TWP. RAINY LAKE AREA OF ONTARIO

GROUND MAGNETIC SURVEY

FEBRUARY 20, 1995 CHESTER J. KURYLIW

o 1 6 l 2 2

S2C10NW0041 2 16122 HALKIRK 020C

- 2 -

TABLE OF CONTENTS

Project Location

Location Maps

Access to Project Site

Regional Geology and Mineralization

Introduct ion

Instrument, Unit and Method

Results of the Survey

Conclus ions

Recommendat ions

Certificate

Plan of Magnetic Survey Scale l" = 200

- 3 -

(a) PROJECT LOCATION

PINE POINT COPPER PROSPECT; Halkirk Twp., Rainy Lake, Ont.

Located on Claim Map G-380S of Halkirk and Farrington Twps.

N.T.S. C-ll, Latitude 48e 38N., Longitude 93*01* W.

(b) LOCATION MAPS:

Claim Map. Halkirk fc Farrington Twps. (scale: l" = 1 /2 mile)

Ontario Geology Survey Map (scale: l" = 340 Kms)

Road Map and Geology (scale: l" s 25 Kms)

(c) ACCESS TO PROJECT SITE:

There is a good access to the Property from Dryden. 151 Kms to

the South from Dryden along Hwy. 502 to the junction of

Hwy.ll, then 5 Kms East along Hwy 11 to Bears Pass, then over

ice by Ski-doo for 5 Kms. to the drill site.

(d) DESCRIPTION OF PROPERTY: PINE POINT COPPER. HALKIRK TWP.

CI. Blk.K-1150126, K-996076, K-996077, K-996078, K-996079,

K-996080, K-9960S1. K-996082, K-9960S3, K-9960S4, K-9960S5,

K-975470, K-975471, K-975472. A total of 14 Claims (25 Claim

units).

Owned 9055 by George Armstrong, and ^ 0% by Chester J. Kuryliw.

(e) DESCRIPTION OF REGIONAL AND LOCAL GEOLOGY:

REGIONAL GEOLOGY:

The Area is located in the Precambrian Wabigoon sub-province.

This Area embraces two major East-North-East trending

Ant i forms. separated by the Swell Bay steep sided Svnclinal

trough.

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GEORGE ARMSTRONG HOLD

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^^^?^^fe^J:

F^-^^r-Ki 'r"';' ^--^^r- racr"" ^^a^**^i'-**d!5* -:;**'-z?—,*e- ^ I^T^feP^Ss'iNU^. 7 •^ssfc^?^^^?™ !.-.---------. TSssS* ---'*; r -..^'2*ftU.- ^ta^w.-.'^ ^Sfr3^^''""" ^-^ ^-C^rv^''' 7:-^-*

,^3^^'"ll "3 - - ^^^--^M

SCALE : 1 M *25 Km. PLAN O? ACCESS ROUTSS TO ARMSTRONG DRILLING 1995

-; Phanerozoic ProterozoicGranitoid rocks: plutons. old sialic crust " v

and unspecified gneisses Metasedimentary and gneissic rocks

l Metavolcanic-metasedimentarygreenstone belts

Subprovince boundary

CT."u^r"—3wv^r^-r:

^* ^t r.

'-^ieriiP'V^\\m-5T-- ^PO^ACV^ ^^\\\\\^

vLake Huron\

S'xercr. mar c.' :r.e\Svcsr:zr ~rsw.~cs sn:vfirg frater :i;nctcgic arc sacorovir.cs Scur.tiaries.

Ontario Geological Survey Miscellaneous Paper 132

1986

.AHKSTSONG-JCKXSGK GOLD. STURGEON LAKE

A?j.:3THc;;c--?:ur.YLiw NI:?:;L PROSPECT, RAII.T LAKEA-ObSTRONG COFFER PROSPECT, RAINY LAKE

- 4 -

REGIONAL GEOLOGY CONTINUED:

In Cross-Section you have a "M" shaped structure over six

miles across. The South Antiform is intruded by the Bad

Vermillion Lake Gabbro-Anorthosite Complex. The North

Antiform (Dome) is intruded by the Nickel Lake Gabbro-Nori te

Complex. A strong circular magnetic high about 1/2 mile

across near the trace of the Swell Bay Synclinal Axis is

interpreted to be a Peridot ite? plug, historically related to

the Antiform basic to ultrabasic intrusions.

An interesting feature of the Bad Vermillion Lake Gabbro-

anorthosite Complex is, the North and South flanks are

bordered by Granophyric "differentiates".

The area of Mineralization falls into a Single Major

structural feature and an epoch of related Major Basic to

Ultrabasic intrusions. Generalizations using the "Single

Chapter of Geologic History" as its basis, leads to some

logical conclusions about existing and known mineral

occurrences and projections towards undiscovered deposits.

MINERALIZATION;

The Nickel Lake-Mine Centre - Rainy Lake AREA has a great

variety of Base Metal and Gold occurrences. What this writer

finds very significant, is that specific metals fall into

"ZONES".

- 5 -

MINERALIZATION CONTINUED;

These Zones are spatially related to: Precambrian

stratigraphy: the antiforms-synclinal structure of the BIG

"M": the Basic Antiform intrusions.

For example:

A Gold Zone is located in the Granophyric differentiate rocks

that lie on the Southern Flank of the Southerly Bad Vermillion

Lake Antiform.

A Copper-Zinc Zone is located in a Basic Lava Formation that

lies immediately on the North Flank of the Bad Vermillion Lake

Antiform.

A Zinc Zone is located in a Rhyolitic Formation with Quartz-

porphyry on the Northerly Flank of the Bad Vermillion Lake

Antiform. This Rhyolitic Formation is located about 4000 Ft.

North of the anorthositic intrusion. The Zinc Mineralization

has widths of over 100 Ft. in places. The Zinc Mineralization

has been traced intermittently over a length of over 25 Miles.

A Copper-Nickel Zone of occurrences is located in or near the

Gabbro-Norite intrusion along the Southern Flank of the North

Rice Lake Dome.

A Nickel-Copper? deposit may occur in the Swell Bay Syncline

Peridotite? intrusion, as indicated by the strong Magnetic

high anomaly and also the strong Air E-M Conductors.

- 6 -

LOCAL GEOLOGY: THE PINE POINT COPPER PROSPECT

This Group is also known as the "Pine Point Group.

This is essentially an untested area the exhibits several

favourable features. A mapped alteration Zone occurs a Pine

Point that is comparable to the alteration Zone which also

occurs to the South of the "West Bay and Wind Bay" Zones.

Secondly, the Ontario G.S. Airborne E.M. Survey, 1980, picked

up several "one line" Conductors in a Basic Lava Fm. and also

in Spherulitic Rhyolite Fm. and in "QE Rhyolite Fm. The "one

line" Conductors in the Basic Lava may indicate sulphide

deposits mineralized the Cu-Zn?. The one or two line

Conductors provide a higher priority target for Base metal

mineral deposits compared to the "Long Formational

Conductors." The small Port Arthur Mines Copper deposits some

25 miles to the E-N-E, occurs in the same Basic Volcanic

Member of the stratigraphic section, as do the Pine Point E-M

Conductors.

Several short drill holes are needed to test these Conductors

subsequent to a detailed Lake Ice Ground E-M Survey and a

ground Magnetic Survey.

Accompanying this Local Geology are:

A Geologic Map of the Pine Point Area (Scale l" = 1/4 Mile)

includes line Grid and Air E-M

Input Anomalies.

- 7 -

LOCAL GEOLOGY: THE PINE POINT COPPER PROSPECT CONTINUED:

An M.N.R. Map of the Port Arthur

Copper Mine (Scale l" * 50 Ft.).

Geology and Description

An O.G.S. Airborne Electromagnetic

Survey Map 80499 (Scale l" = 1 /4 Mile)

- 3 -

INSTRUMENT. UNIT AND METHOD

The Pine Point Grid,

was surveyed using a portable Scintrex

model MP - 2 precession magnetometer.

The sensitivity of the instrument is (+J l gamma. The

principle of operation is based upon the fact that a proton

rich fluid such as kerosene when placed in a magnetic field

will have its protons align along the magnetic field vector.

The magnetic field is induced in the sensor upon depressing

the instrument push button, then this field is suddenly

removed. Protons which behave as elementary gyroscopes will

start to align with a precession frequency that is directly

proportional to the magnetic field of the earth. The

magnetometer counts this frequency, divides it by the

appropriate constant to obtain a reading in gammas and

displays the reading in the form of a five digit number.

A base station was established on base line 00-N at 00-W. The

base station reading 58&M gammas. The main base

station was read at the start and finish of each survey day to

check for diurnal variations and the instrument operations.

To correct for diurnal changes all baseline stations on 00-N

at the picket line crossings were established as secondary

base stations. This was accomplished by checking in at the

main base station then reading the baseline stations and

checking back into the main base station within an hour.

- 4 -

These secondary baseline stations were corrected and plotted

and then these served as alternate base stations for check-ins

during the surveys of picket lines. In this manner all picket

line stations which were read at 50 foot stations along picket

lines were corrected for diurnal variations before plotting on

the plans. The readings were plotted on the survey plans

scale l" = 200 .

Contouring of the corrected and plotted magnetic readings was

carried at 1000 gamma intervals.

RESULTS OF MAGNETIC SURVEY

The magnetic survey over the Pine Point Grid is one of

relatively flat magnetic relief with the exception of the

gabbro-basic lava contact. The gabbro rises in magnetic

relief over 2000 gammas above the relatively flat relief of

the basic lava. There is a marked increase in the magnetic

relief on lines 2- W to 10 - W at about 16 - S on the grid.

There is an obvious shift in the gabbro contact of about 200

ft. northwards centered on 6- W and there is also an increase

of about 12.000 gammas in the gabbro near the fault. This

fault block shift is very useful in interpreting the

electromagnetic conductor extensions.

A second belt of slightly higher magnetic relief occurs in the

spherulitic rhyolite.

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Quartz— eye Rhyolite

Zn— bearing Bedded Tuff Rhyolite with Stringer Sulfides

^ Htoafic Breccia— Vesicular*s.Rhyolite with Chlorite Seams

^

l Mafic Flow

Spherulitic Rhyolite

Chloritic and MineralizedIntermediate/MaficVolcanics

Gabbro

100 ft

STOP 3 - PORT ARTHUR COPPER

FROM 1991 M.N.R. FIELD TRIP (C. BLACKBURN)

Figure 7. Sketch map of geology at Port Arthur Copper Mine

105NOTE; THE STRATIGRAPHIC SEQUENCE SHOWN HERE IS THE SAME

AS OCCURS AT THE ARMSTRONG PINE POINT PROSPECT. bO Km. TO THE W-S-W

CHESTER J. KURYLIW. M.Sc-..CONSUI.TIMG CKOUIGIifT

16 INGALL Du. DRYJIKN. ONTARIO r** mi

LOCAL GEOLCGY ( con't)

* Stop 3; The Port Arthur Copper Mine

The open cnt was developed during the winter 1916-17 and later in 1917 a 30 m deep shaft with a first level drift 65 ra long were developed. In total, "several* carloads of ore grading 3 to S.5% Cu were shipped to Trail B.C.. The property was further developed by a shallow drill program in 1956 by Stratmat Ltd. and a complex distribution of copper and zinc has been interpreted from the results of that program (Fig. 3b and Poulsen, 1984). The recent stripping has been performed by Minnova Ltd., Thunder Bay who kindly provided the accompanying sketch (Pig. 7) as -a guide to the many features in the outcrop.

The southernmost exposure is that of a medium grained metadiabase that cuts the altered and mineralized zone. The overlying chloritized and sericitized intermediate to--maf.ic. amygdaloidal flows and breccias contain variable amounts of sphalerite, chalcopyrite and pyrite with quartz and iron carbonate' ' '^ evidenced by Jth'e^ variaBIe i intensity ' of rusty ' wea'tHer ing .

"Representative samples' of the mineralized materiaT may "stxlTT be found locally in the dump to the west. The mineralized zone is capped to the north by a narrow zone of banded silicified and sericitized rock with local pyrite seams. This is overlain, in turn, by successive spherulitic rhyolite flows and mafic amygdaloidal breccias with local vague pillow forms and which locally are cut by mafic dykes and quartz veins. Massive sulfides have been intersected in drilling at the top of the northernmost of the mafic units. This mafic unit is overlain by vesicular and amygdaloidal rhyolite containing stringer sulfide mineralization and capped by a 5 m thick sequence of carbonate- and sphalerite-bearing bedded tuffs or sediments. This unit appears to cap the hydrothermal alteration and mineralization in this area and is overlain by a substantial thickness of unaltered quartz-eye rhyolite.

* Prom Kenora ?fl.N.R. Pieldtrip (C. Blackburn)

Note, The Same Formation and Sequence of Members occurs at the Port Arthur Copper, as Mapped by Minnova at the Pine Point Copper prospect. (C.J.Kuryliw)

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- 8 -

INTRODUCTION

During the period of January 29 to February 06. 1995 Jack

Cureatz of Wawa, Ontario laid out the line grid and carried

out the instrument survey with assistant G. Gratton of Wawa,

Ontario. The plotting, draughting, interpretations and report

were done by this writer.

- 5 -

RESULTS OF MAGNETIC SURVEY CONTINUED;

Several local magnetic high anomalies occur spread out along

the southern contact of the spherulitic rhyolite and basic

lavas. Some of these magnetic high anomalies form "shoulders"

to E.M. conductors. This would be significant if the local

magnetic highs are caused by pyrrhotite with magnetite.

- 6 -

RECOMMENDATIONS

Several horizontal loop E.M. conductors were located with

suppoiting magnetic patterns These conductors should be

drilled to determine if base metal sulphides occur in these

conductors.

February 20. 1995 Chester J. Kuryliw

- 7 -

CONCLUSIONS

The magnetic survey was successful in tracing the formations

and it is immensely useful in recognizing and locating faults

that appear to be pre-sulphide mineralization in age.

February 20, 1995 Chester J. Kuryliw

CERTIFICATE

I, Chester J. Kuryliw of Jj-6 Ingall Drive, Dryden, Ontario, do hereby certify that:

(1) I am a Professional Engineer and I am currently employed as a Consulting Geologist for several mining companies.

(2) I am a graduate of:The University of Manitoba B.Se. Degree, 1949 The University of Manitoba M.Se. Degree, 1966

(3) I am a registered Engineer of the Association of Professional Engineers of Ontario and also Manitoba. I am a fellow of the Geologic Association of Canada, also a member of the Canadian Institute of Mining and Metallurgy.

(4) I have practiced a1.y profession for cv3r^5 years, most of thoseyears at gold mines, during which tiue l often planned, supervised2nd ~. ! recT'r'i 'jr.'!er~r''-"r. ;1 exclorati^Ti. devel . ^.Tient and oro^vrt. •L-'.T.

(5) My Report is based upon My personal field supervision of the Magnetic and Ele c tromagnetic surveys and upon my personal plotting and evaluation of results obtained.

Feb. 20, 1995Chester J. Kuryliw, M.Se., P.Eng.

JUL-27-95ITHU) 09:05 NINIHG/GEOLOGY-IEII TEL:I0746I2I23 P. 002

Itoport of Wortc Conducted After Recording Ctebn

Ontario f•ri

i typ* or print and won* bi dupttoaai Refer to ttw Mbring Aot md AoguMom forRocordw. . . ,. s?r.inNwno4i f -IBIT? HAI A MparaM copy of two form muatba compMBd foroach Work Group. Todhrricri rvportt and map* mwl atcompanyHiform In dupacahx ^ AtfMch, cnowlng th* dakMttio work b aailBnod lo. muat aooornpany Ms form.

""fa- onn

(Check Ono Worn Group Only)

mdudkiQ DMng

Total Ai aimed on the AtNokK The

MOfCoMi S l U or part of mo i

hoklar caimot warty axpendliiraa oWmad bi ma statement of coats wflhln 30 day* of a requaot tor

and Survey Company Who Parfotmad the Work (OK* Nama and Addraao of Aomor of Rapon)

h Mi Wo* npon. hntag pMtoimd A* verti or

•t.i.ndiiy OfNorthern-Oevetopmentand Mines

Ontario

Report of Work Conducted After Recording Claim

Mining Act

Transaction Number

tinPersonal information codected on this form Is obtained under the authority of the Mining Act. This information will be tised for correaporKJer^ffris coBection should be directed to the Provincial Manager. Mining Lands. Ministry of Northern Development and Mines. Fourth Floor, 150 Cedar Street.Sudbury. Ontario. P3E 6A5. telephone (705) 670-7264. .-f

--m V assessment

Instructions: - Please type or print and submit in duplicate.- Refer to the Mining Act and Regulations for requirements of filing

Recorder.- A separate copy of this form must be completed for each Work Group.- Technical reports and maps must accompany this form in duplicate.- A sketch, showing the claims the work is assigned to, must accompany this form.

work or consult the Mininge

Work Performed (Check One Work Group Only)WorkGroup Type

Geotechnical Survey

Physical Work. Including Drilling RECEIVEDRehabilitation

irttnrOther Authorized Work

AssaysAssignment from Reserve t

"otal Assessment Work Claimed on the Attached Statement of CostsMote: The Minister may reject for assessment work credit all or part of the assessment work submitted if the recorded

holder cannot verify expenditures claimed in the statement of costs within 30 days of a request for verification.

arsons and Survey Company Who Performed the Work (Give Name and Address of Author of Report)Name Address

Au" — S* 6r-X4T7"

v)

tach a schedule H necessary)

rtMcatlon of Beneficial Interest * See Note No. 1 on reverse side;ertify that at the time the work was performed, the claims covered in this work port were recorded in the current holder's name or held under a beneficial interest

the current recorded holder.

tlffcation of Work Report•*rtily that l have a personal knowledge of the facts set forth in this Work report, having performed the work or witnessed same during and/or after

completion and annexed report is true.ie and Address of Person Certifying

ftf' ifrt

Office Use Onlyai Vahie Cr. Recorded DateReArbed "

Deemed Approval Dale

0+r f f i?? f

Mining Recorder *-^ v-

Oate Approved

Date Notice for Amendments Sent

Deceived Stamp

-. ,- - -- - 'rt

i -

A911 *

N s lfe -^i!

CQ -^ S3

s )C 3

ci

V/i 10op4'

\

-.-**

V

^ o'

i Credits you are claiming in this report may be cut back. In order to minimize the adverse effects of such deletions, please indicate from i which claims you wish to priorize the deletion of credits. Please mark (^) one of the following:

1. G Credits are to be cut back starting with the claim listed last, working backwards.2. D Credits are to be cut back equally over an claims contained in this report of work.3. D Credits are to be cut back as priorized on the attached appendix.

In the event that you have not specified your choice of priority, option one will be implemented.

Note 1: Examples of beneficial interest are unrecorded transfers, option agreements, memorandum of agreements, etc., with respect to the mining claims.

Note 2: If work has been performed on patented or leased land, please complete the following:

l certify that the recorded holder had a beneficial interest in the patented or leased land at the time the work was performed.

Ontario

Miriist/y ofNortnem Developmentand Mines

Ministere du Deveioppement du Nord ei des mines

Statement of Costs for Assessment CreditEtat des couts aux fins du credit d'e valuation

Mining Act/Lot sur les mines

Transaction No IN' de transaction

Personal information collected on this form is obtained under the authority of the Mining Act. This information will be used to maintain a record and ongoing status of the mining ctaimfs). Questions about this collection should be directed to the Provincial Manager. Minings Lands. Ministry of Northern Development and Mines. 4th Floor, 159 Cedar Street. Sudbury. Ontario P3E 6A5. telephone (705) 670-7264.

Les renscignements personnels contenus dans la presenle formule sent recueillis en vertu de la Loi sur les mines ei serviront a tenir a jour un reg s're des concessions minieres. Adresser toute question sur la cdiece ae as renseignements au chef provincial des terrains miniers. ministere do Oeveioppement du Nord et des Mines. 159. rue Cedar. 4* etage. Sudbury (Ontario) P3E 6A5. telephone (705) 670-7264.

1. Direct Costs/Gouts directs

Type

Wag*. SaJaires

Contractor's and Consultant'sF***' Drafts de rentrepreneur•t d* Cexpert- conaell

Supplies used Foumitur**, -ftn m * — —uniwavs

Equipment Rental Location de materiel

Description

Labour Main-d'oeuvreField Supervision Supervision sur le terrain

Typ5~ ,3/64 31/•' 'l-tS*'t~t^//''*^fk S*f'*6T. 4?*?

\*. fit.-sfa73Type

Type

Amount Montant

S /M./

Total Direct Costs Total des couts directs

Totals Total global

i

3/6?

l l

2. Indirect Costs/Gouts indirects" * Note: When claiming Rehabilitation work Indirect costs are not

allowable as assessment work.Pour le remboursemeni des travaux de rehabilitation, les couts indirects ne sont pas admissibtes en tant que travaux d'evaluation

Type

Transportation Transport

Food and Lodging Nourriture et hebergementMobilization and Demobilization Mobilisation et demobilisation

Description

Type

-

Amount Montant

Sub Total of Indirect Costs Total partlel des couts indirects

Amount Allowable (not greater than 20* of Direct Costs) Montant admissible (n'excedant pas 20 H des couts directs)Total Value of ASM (Total of Direct and f indirect costs)

ssment Credit Valeur totale du credit utowaMe d'evakMtion

Totals Total global

i !

i

^./e)(t indVacts admistMes

tot*: The recorded holder will be required to verify expenditures claimed in this statement of costs within 30 days of a request for verification. If verification is not made, the Minister may reject for assessment worn all or part of the assessment work submitted.

Note : Le titulaire enregistre sera tenu de verifier tes depenses demandees dans le present etat des couts dans tes 30 jours suivant une demande A cet effet Si la verification n'est pas effectuee, le mimstre peut rejeter tout ou une partie des travaux d'evaluation presentes.

siting Discounts

i. Work filed within two years of completion is claimed at 10046 of the above Total Value of Assessment Credit.

Remises pour depot

1. Les travaux deposes dans les deux ans suivant tour achevement sont rembc^Jrsesa100%delav3leurtotalesusf^1ention^^ducreo^to"evahJatk)n.

?. Work filed three, four or five years after completion is claimed at 504fe of the above Total Value of Assessment Credit. See calculations below:

Total Value o* Assessment Credit Total Assessment Claimed

x 0.50

2. Les travaux deposes trois, quatre ou cinq ans apres lour achevement sont rembourses a 50 *to de la valour totale du credit devaluation susmentionne Voir les calculs ci-dessous.

Valour totale du credit devaluation

x 0.50Evaluation totale demandee

Certification Verifying Statement of Costs

hereby certify:tat the amounts shown are as accurate as possible and these costs ere incurred while conducting assessment work on the lands shown i the accompjnying^epprtpf'Vvork form/

tet^

make this certification

Agent. PofiOSn in Company)

Attestation de I'etat des couts

J'atteste par la presents :que les montants indiques sont le plus exact possible et que ces depenses ont ele engagees pour effectuer les travaux d'evaluation sur les terrains indiques dans la formule de rapport de travail ci-joint.

am authorized Et qu'a titre de je suis autorise(trtulaire enregislri. repntsentant. post* occup* dans la compagnie)

a faire cette attestation.

Signaiure

Nota : Dans cane formula. topoVil design* des pmsonnes. to masculirtest utilis/ ausens neotre.

OntarioMinistry ofNorthern Developmentand Mines

Ministere du Developpement du Nord et des Mines

Geoscience Approvals Section 933 Ramsey Lake Road 6th Floor Sudbury, Ontario P3E 6B5

Telephone: (705) 670-5853 Fax: (705) 670-5863

August 31, 1995Our File: 2.16122 Transaction f : W9510.00066

Mining RecorderMinistry of Northern Development808 Robertson StreetP.O. Box 5200Kenora, OntarioP9N 3X9

Mines

Dear Mr. Rivett:

Subject: APPROVAL OF ASSESSMENT WORK CREDITS ON MINING CLAIMS 966083 et al. IN HALKIRK TOWNSHIP

Assessment credits have been approved as outlined on the report of work form. The credits have been approved under Section 14 (Geophysical) of the Mining Act Regulations.

The approval date is August 31, 1995.

If you have any questions regarding this correspondence, please contact Steven Beneteau at (705) 670-5855.

Yours sincerely,

Ron C. GashinskiSenior Manager, Mining Lands Section Mining and Land Management Branch Mines and Minerals Division

SBB/sb

cc: Resident Geologist Kenora, Ontario

vAssssessment Files Library Sudbury, Ontario

________NOTES_______

400* surfoce rights reservation along tht shores of all lakes and rivers.

All Islands in Rainy Lake WITHDRAWN FROM STAKING under Sec.39 tub.(c) of Mining Act R.S.O. I960.

AREAS WITHDRAWN FROM DISPOSITIONMRO- Mining Right* Only

SRO- Surfoce Right* OnlyM * S -Mining and Surface Rights

Description Order NoC*j) 420*30 IMO)

5) PUBLIC HeSERVe

l 4SIMOI670) W 88/73

Date Disposition9*16/69 8RO

I98T S MO

6/12/79

RE-OKNRQ NW.R 14/84 T/I8/M

481*801670) W 44/71 ie/06/TB

WASTE DISPOSAL W B 9/S8 86/01/66

SAKMR

MO

6 MO.

File165474

165475

176403

7411 V 6

J6IMO I860) W 67/86 14/04/66 MtS

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OBIKOBA LAKE M.2126 PORTER INLET M.2459

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NORTH RANGE

———I.————

SOUTH RANGE 9147 j 939148 939143 l 732364

l l l—XZ—l———-,— tT l * TS?S6'~]"K 17-- j K

|"*' BI y 939180 j 939149 | 939.46 939 146 93*44

NORTH RANGE *yp im i95*183 |Bi0l82

r391841927866 |94r864

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1150058

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5OIP8

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1178217

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THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED FROM VARIOUS SOURCES, AND ACCURACY IS NOT GUARANTEED THOSE WISHING TO STAKE MIN ING CLAIMS SHOULD CON SULT WITH THE MINING RECORDER, MINISTRY OF NORTHERN DEVELOP MENT AND MINES, FOR AD DITIONAL INFORMATION ON THE STATUS OF THE LANDS SHOWN HEREON

gf ACTIVE DATt

LEGEND

HIGHWAY AND ROUTE No

OTHER ROADS

TRAILSSURVEYED LINES.

TOWNSHIPS, BASE LINES, ETC LOTS. MINING CLAIMS, PARCELS, ETC

UNSURVEYED LINES LOT LINES PARCEL BOUNDARY MINING CLAIMS ETC

RAILWAY AND RIGHT OF WAY UTILITY LINES

NON-PERENNIAL STREAM FLOODING OR FLOODING RIGHTS

SUBDIVISION

ORIGINAL SHORELINE

MARSH OR MUSKEG

MINES

DISPOSITION OF CROWN LANDS

TYPJLPJ. DOCUMENT

PATENT SURFACE A MINING RIGHTS

SURFACE RIGHTS ONLY

MINING RIGHTS ONLY

LEASE, SURFACE A MINING RIGHTS SURFACE RIGHTS ONLY

MINING RIGHTS ONLY

LICENCE OF OCCUPATION

CROWN LAND SALE

ORDER-IN-COUNCIL

, RESERVATION

CANCELLEDSAND A GRAVEL

SYMBOL

B BV cs oc

(D

SCALE : 1 INCH 40 CHAINSaoo loop too 4000 eooo

FEET

METRESO tOO 4OO (00 100 l KM

ACRES HECTARES

TOWNSHIPS

HALKIRK FARRINGTONDISTRICT

RAINY RIVER

MINING DIVISIONKENORA

Ontario

Ministry of Natural ResourcesSurveys and Mapping Branch

Date APRIL 1970

Whitney Block Queen s Pork, Toronto

Plan No.

G-3808

62C10NW0041 2 18122 HALKIRK 200

PDCUT n a

BASE LINE-00

IMAGINARY (OUT-OF-PHASE)

REAL UN-PHASE) }

READINGS

INSTRUMENT* GEONICS E-M*I7

MODE.' HORIZ. LOOP

COIL SEPARATION: 3OO1&0

2. 16122

16 S

20 s

ARMSTRONG PINE POINT COPPER PROSPECTHALKIRK TWP.. RAINY LAKE, ONT.

PLAN OF ELECTROMAGNETIC SURVEY

l62C1QNWCKM1 2 16122 HALKIRK

SCALE: l"*200'

FEB. 1395 C. d KURVLIW210

i5*CM

i CM

ocvi

BASE LINE-00

4S

12 S

16 S

•12

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INSTRUMENT: GEONICd E-M-17

HORIZ. LOOP SURVEY

COIL SEPARATION- 30O'L V

ARMSTRONG PINE POINT COPPER PROSPECTHALKIRK TWP., RAINY LAKE, ONT.

PLAN OF ELECTROMAGNETIC SURVEY

SCALE: I"*2OO'

FEB. 1995 C. d62C10NW0041 2 '10122'HAkKIRK 220

BASE LINE-OO

690MZ

4S

8S

12 S

16 S

20 S

PLEGENDINSTRUMENT: SCINTREX PRECISION MAGNETOMETER MP-2TOTAL MAGNETIC FIELD, SENSITIVITY: (±) l-GAMMA CONTOUR INTERVAL; 1000 GAMMAS, . * , * . GROUND EM-17 CONDUCTOR

HORIZ. LOOP, 30O'COIL SEP'N.

ARMSTRONG 'PINE POINT'COPPER PROSPECT HALKIRK TWP., RAINY LAKE, OA/T

PLAN OF MAGNETIC SURVEY

SCALE: l"-200!

FEB. 1995 C.J.KURYLIW

s*** \ ^vBASE LINE-00 a

^i"^^^^3

165

2OS

62C10NWOM1 2 16122 HALKINK

INSTRUMENT: SCINTREX PRECISION MAGNETOMETER MP-2 TOTAL MAGNETIC FIELD, SENSITIVITY: (±) l- GAMMA

INTERVAL^ 1000 GAMMAS. . . . . GROUND EM-17 CONDUCTOR

HORIZ. LOOP, XOO'COIL SEP'N.

ARMSTRONG 'PINE POlNT'COPPER PROSPECT HALKIRK TWP., RAINY LAKE, - 0A/7T

PLAN OF MAGNETIC SURVEY

: l**200f

FfB. 1995 C.J.KURYLI240