hamilton prop - geology ontario

REPORT ON GEOLOGICAL, GEOPHYSICAL AND GEOCHEMICAL SURVEYS

HAMILTON PROPERTY, SEELEY TOWNSHIP

SAULT STE. MARIE MINING DIVISION, ONTARIO

s. 1 3714 SETLEY LAKE

r. * -. i . v t \010

Prepared for:

John Hamilton A2^Walr,icr 14d . Toronto, Ontario.

Prepared by:

Robert J. Di 11 man A 2 Springbank Dr. London, Ontario.

August 15, 1990

on

The Hamilton property lies l kilometre west of Coubran Lake in

Seeley Lake township, district of Thunder Bay. The property can be

reached by following a logging road which runs 'north of highway #17

just west of Mink creek, approximen tl y 24 kilometres west of the

town of Marathon, This road goes to Coubran Lake, A trail to the

property can bc found leaving the west shore at the narrows of the

lake.

The Hamilton property consists of 30 claims. All claims are held

by:

Annette Hamilton 426 W a liner Rd . Toronto, Ontario

Only 8 claims have been covered by geophysical, geochemical and

geological surveys. These claims are: 1111360-1111367 inclusive. The

recording of the claims occurred on October 12, 1989.

History

Although a number of old posts were found in the field no record

about previous work has been found. Between October 12th to October

20th, 19b9 a grid was cut over the property, The base line of the

grid runs east-west and north-south cross lines occur every 400 feet.

All lines have pickets every 100 feet. This grid was used for the

control of the surveys of: magnetics, electromagnetics, geochem soil

sampling, geological mapping, prospecting and trenching. These

surveys were carried out between May 28, 1990 to August 15 , 1990.

Surficial Topography and Geology

The Hamilton property is situated in very high and moderately

rugged terrain. Many of the lines are crossed by cliffs and sharpe,

deep draws. Creeks occupy some of the* draws either flowing on the

surface or below glacial till, or talis "debris , The creeks form

l

small swamps in low, flat areas. Eventually everything drains east

to Coubran Lake,

In the central and western regions of the grid large outcrops

dominate the surface. Over the entire property outcrop exposure may

total 5 O '/,.

Overburden in the area is generally confined to areas between

outcrops, within the draws and in the lower regions of the property,

Between outcrops soil stratigraphy is divided into a surfacial humus

layer consisting of vegetation debris underlying by black, decomposing

organic material. ]-ielow this a white, very fine clay like mat

erial exists, This humus horizon is the most continual soil on the

property since it also thinly covers much of the exposed outcrop,

Below tue humus layer is a charcoal and ash layer generally only

a few inches thick. The presence of this layer suggests that the area

was subjected to a forest fire at some point in its history.

In areas where soils thicken, below the humus and ash exists a

horizon of reddish to brown material. This layer is fine to gritty

in texture and was preferred during the soil sampling survey. This

horizon is not continual and is only confined to areas between out

crops where soil depth thickens,

Above bedrock except in areas of exposed bedrock lies a layer

of brownish soil containing, f rcfcuicnt d of disintegrating bedrock of

various sizes and frequency. There is no diffcnent boundary between

this layer and the overlying reddish to brown material but a distinc

tion can be made, by the presence of bedrock material. This horizon

is more continual than the overlying reddish to brown horizon since

it is present even as soils thin.

The occurrence of glacial till is very limited on the property.

Till usually is found within the draws, against cliffs facing the

direction of glacial advance which is thought to be from the north,

2

jior t h-east, and on the lee sides of hills to glacial direction. Most

of the till observed consists of locally derived mafic material and

granite boulders. The deposition of the till probably resulted from

the combination of lodgement and meltout processes by the glacier.

Vegatation on the property appears to be controled by elevation

and direction of slope. In the highest areas and on south facing

slopes occur birch and spruce. Poplar occurs on north facing slopes

and level areas. Spruce dominates the lowest areas and sometimes

becomes mixed with cedar.

The geology of t li e area consists of mafic and plutonic rocks of

the Port Coldwell mafic intrusive complex. On the property gabbro

is the most extensive rock, It occurs in the north and eastern sections

of the grid. On appearance it varies between dark greenish grey to

brownish grey in color. The grain size ranges from fine to medium

grained. Coarser grained gabbro appears to have resulted from an

increase in size by plagioclase. Magnetite is an important accessory

mineral and in places it was seen to total at least 1 7, o f the rock,

The magnetite occurs as very fine disseminations. Also seen as access

ory minerals are chalcopyrite and very rarely traces of native copper.

On a weataered surface the gabbro appears a light buffed grey. Some

times it is jointed especially near cliffs.

Basalt was observed within the map area, It occurs as small lens

shaped bodies within the gabbro and syenodiorite. It is fine grained

and olive green on a fresh surface. It weathers to a whitish green.

In many places the basalt showed weak to moderate chlorite alteration

and moderate silicification. Chlorite occurs along small fractures

and as small concentrations within the rock. Chlorite also occurs

in pea sized eyes of quartz. These chloritized quartz eyes are pro

bably a metamorphic feature and suggest the extent of alteration "has

entered the green schist facies. Traces of chalcopyrite and pyrite can

^^,ur in the quartz eyes. The existence of these minerals adds evidence

that the basalt has under gone some degree of hydrothermal mctamor phism.

Also noted within the basalt were small finely disseminated clots of

magnetite, The frequency of these magnetite clots increased as the

degree of silicification increased. Although the clots have no size,

in some instances magnetite may total 1 -2"/, o f the rock.

On the east side of t li e grid, J i ne s 36E to 42K and just south of

the base line, diabase was found forming two west and north-west trend

ing dykes, hot h dykes have short strike lengths, being roughly 400ft.,

and are both somewhat lenticular in shape. They have intruded into

the mafic rocks and the contacts have no apparent alteration. These

dykes have probably filled fractures. On a fresh surface the diabase

is a blackish brown occasionally being mottled by whitish feldspar.

The diabase " weat her s to a brownish white. The grain size changes from

a fine grain close to the edges of the dyke to a moderatly coarse

grain towards the center. Ophitic texture between the plagioclase

feldspars and pyroxenes also becomes more^pronounced in the inner areas

of tlie dykes, Magnetite is the major accessory mineral and is finely

disseminated throughout the rock.

Much of the south west of the grid area is dominated by a large

plutonic body of syenodiorite. On a fresh surface this rock is mostly

pink in appearance but is mottled by whitish plagioclase and quartz

and greenish black augite, There is very little color change on a

weathered surface. The grain size varies between sand sized grains

to fairly course grain. Moving inwards from the contact the grain size

randomly changes suggesting the pluton pulsed dur ing-:erupt ion 0 The

contact with the mafic volcanics is usually faulted but in the west*

this is not the case and the actual contact is visible. It shows that

the mafics adjacent to the contact have been intruded by small, ran

domly orientated veinlets of pinkish feldspar. Where this has happened

r the surrounding mafics show a pink discoloration due to an injection

feldspar into the rock. At one location, line 24E on the base line

the mafic-syenodiorit e contact does not show this feldspar contamin

ation but that the contact is very sharp. I'he mafics which in this ' :

case is basalt has developed strong cleavage plains that strike para

llel the contact and gently dip towards the syenodiorite at right

angles to the actual contact. This cleavage development is possibly

due to shearing along contact and has given the basalt a somewhat

schisty appearence. Along the cleavage plains chlorite has slickened

the sides and clots of chlorite have formed within the basalt. The

pink discoloration by feldspar in the mafics was observed in many

places not within close proximaty to the syenodiorite. Notably these

places are long cliff faces and along the walls of some of the long,

linear draws. At line 34E about 200 feet north of the base line this

feldspar contamination appears to have played an important part in the

development of copper mineralization.in the area. Here, the basalts

have feldspar veinlets and a moderate degree of silicification. Chlorite

is present in the veinlets and within quartz eyes which can be the size

of a quarter. Copper mineralization consisting of chalcopyrite, bornite,

and malachite are present in some of the feldspar injections. These

minerals can be present in the quar tz-chlori t e eyes as well. Traces of

native copper were observed in the veinlets and wallrock.

At ."35E' along the base, line a syenite dyke was discovered within

gabbro. This dyke was traced about 20 feet in a north north-east dir

ection and is roughly 2 feet wide. The dyke appears to have filled a

fracture which has possible tensile origins. The dyke is pegmatitic

in nature. Its principle minerals, orthoclase and hornblende, have formed

crystals as large as an inch. This syenite dyke was probably introduced

during plutonism of the syenodiorite and even though it is the only

one observed todate more probably exist on the property.

rDuring the field work many cliffs, cuts and draws were encountered.

topographic features generally trend west north-west and can

easily be recognized on an air photo, Intrepetation of these features

suggest that they represent faults. Although no evidence as to the

type of faulting or the amount of displacement was observed in the

field it is believed that they are normal faults and possibly low

angle thrust faults. In the northern and southern areas of the grid

cliffs and cuts probably represent normal faulting while in the cent

ral areas some of the draws may be thrust faults. This assumption is

made due to the general shape of the draws where one side of the drav;

may be steep and cliffed while the opposite side is generally gently

sloped towards the gut of the draw. The age of faulting is assumed to

be rather young since they intersect and cut some contacts. There is

some evidence to suggest that some.'of the faulting occurred during

plutonism because of tlie existence of pink feldspar veinlets and con

tamination in mafic rock adjacent to the fault axis. If this is the

case these faults may be important targets for future exploration

of copper mineralization..

Mineral Occurrences

Although a large percentage of the grid is outcrop prospecting so

ff*r has only been concentrated along grid lines. The most interesting

mineralization found so far is some copper mineralization located

between lines 32E and 36E at 2+OON. The principle rock here is basalt

which shows moderate silicification and weak shearing. Chlorite is

present along fractures, in small blebs and within quartz eyes. Pink

feldspar veinlets and injections are abundant. Chalcopyrite and

bornite are associated with chlorite and feldspar veinlets. In at least

three outcrops native copper was observed as very fine specks within

the basalt.

To the. north gabbro contacts the basalt and the contact may have

faulted.* . Pink feldspar injections and veinlets are present in the

outcrops adjacent to the contact. To the south the basalt also contacts

gabbro but no evidence of structure was seen. The mineralization in

the area is probably related to faulting and plutonism. Copper sulphides

may have been inplaced by the feldspathic intrusions along fracture

zones.

Another area of copper mineralization similar to that mentioned

above is located at 5+50N, line 34E. Here feldspar injections and

veining have occurred within a moderately silicified and chloritized

gabbro or basalt. There is also a weak degree of shearing. Chalcopyrite

and bornite occur as traces within vein Material. There appears to be

faulting to the north of this mineralization as the topography drast

ically steepens.

Tr enching

Between June 9 f 1990 and June 14, 1990, 17 trenches were blasted

in outcrops containing copper mineralization. Holes were drilled using

a Cobra plugger and blasts were cleared manually. Two men were involed

in the trenching:

R.J. Dil1man R. MacNally42 Springbank Dr. Sault Ste. Marie,London, Ontario. Ontario,

Trench #1 is located on line 34K, 1+25N. The rock in this trench

is a weakly silicified and sheared basalt. Pink feldspar and chlorite

are present, Fine chalcopyrite is disseminated in the basalt. Malachite

stains some of the fracture surfaces. Sulphides total less than 1 7,, T he

trench measures 5ft X 3ft,

Trench #2 is located on line 34E, 1+50N, The rock consists of a

weakly silicified basalt. Chloritized quartz eyes, feldspar veins and

injections occur. Only traces of chalcopyrite were observed. The trench

measures 6ft X 2ft.

Trench #3 is located on line 3AE, 1+75N. The basalt in this trench

is moderately silicified. Quartz eyes are abundant. Chlorite is present

in the eyes and as clots. Pink feldspar has discolored the basalt.

Chalcopyrite and bornite are disseminated in the basalt and quartz.

These way total 1 7.. Traces of native copper were observed. The trench

measures 15ft X Aft,

Trench #4 is located on line 33E, 2+25N. It was blasted in weakly

sheared and silicified basalt. Quartz eyes and pink feldspar contamin

ation occur. Traces of native copper and chalcopyrite were observed

in some of the freshly blasted rock. Malachite has stained some of

the joint surfaces. The total sulphides is less than 1 7,. The trench

measures 6ft X 3ft,

Trench #5 is located on line 3A4-30E, 2 + 50N. Malachite is present

on fracture plains. Traces of chalcopyrite occur in basalt but total

less than 1 7,. T he basalt is slightly chloritized and weakly silicified

and there is evidence of pink feldspar present, The trench measures

3ft X Aft.

Trench #6 is located on line 3A+60E, 1+50N. It was blasted in

moderately silicified basal t..Traces of native copper were seen in

the basalt. Malachite weakly stains some fracture plains. The trench

measures Aft X 2ft.

Trench #7 is located on line 3A+50E, 14-AON. The basalt is silici

fied and pink feldspar is present. Malachite staining occurs on

joint surfaces. No sulphides are present within the basalt. The trench

measures Aft X 2ft.

Trench #8 is located on line 3A+70E, 1+75N. The basalt has fract

ured along the walls of some of the pink feldspar veining and exposed

malachite staining. Chlorite clots occur in the basalt but no sulphides

were seen within the rock. The trench measures Aft X 2ft.

8

Trench #9 is located at line 35E, 1+75N. The basalt is moderately

.icified and sheared. Chlorite occurs along the fracture surfaces

and there is evidence of pink feldspar contamination. Traces of chalco

pyrite and malachite occur with the chlorite on the fracture plains.

The trench measures Aft X 2ft.

Trench #10 is located on line 35E, 1+OON. The basalt is weakly

sheared and moderately silicified. Malachite appears on fracture

surfaces. Traces of native copper and chalcopyrite are weakly dissem

inated in the. basalt but total no more than 1 7,, T he trench measures

8ft X 3ft.

Trench #11 is located on line 35 + 10E, 2 + 25H. Moderate silicifi

cation and weak shearing appear in the basalt. Pink feldspar veining

and contamination are evident. Chlorite clots are present in the

feldspar injections and in abundant quartz eyes. Chalcopyrite and

bornite were observed in the veining and quartz, These sulphides

and native copper were finely disseminated throughout the basalt

but only total about 1 7,, T he trench measures 8ft X 3ft.

Trench #12 is located on line 36E, 1+OON. It covers a l foot

wide zone of sheared basalt within gabbro. Shearing direction is

towards the north west. There is some feldspar contamination and

the basalt is magnetic. Less than 1 7, c halcopyrite occurs in the

basalt. Tile trench measures 8ft X 3ft.

Trench #13 is located on line 33+60E, 5+25H. Moderate silicifi

cation has occurred to either a gabbro or basalt. Pink feldspar

blebs and injections along with chlorite appear in the rock. Less

than 1 7, c halcopyrite occur in the chlorite and feldspar masses and

x^eakly disseminated throughout the rock. The trench measures 12ft X.

3ft.

Trench #14 is located on line 33+75E, 5+75N. Weak shearing and

silicification are present. The rock in the trench is either a gabbro

9

or basalt. Malachite is present on some joint surfaces. The trench

ures 15ft X 3ft.

Trench #15 is located on line 3AE, 6 + 10N. Less than 1 7, c halco

pyrite and traces of malachite are present on some fracture surfaces.

The rock in the trench is probably gabbro? The trench measures

6ft X 3ft.

Trench #16 is located on line 20+20E, (H-50N. The basalt in this

trench is strongly sheared and carbonated. There is some degree of

brecciation and chlorite has developed as thin coatings between the

fragments, l to 5 7, c halcopyrite was observed xfithin the rock. The

trench measures Aft X Aft.

Trench i/17 is located on line 20+AOE, (M-75N. The basalt here is

also carbonated and silicified but less sheared and brecciated. Very

fine pyrite can be seen to total less than 1 7,. T he trench measures

Aft X Aft.

VLF Survey

Between May 2, 1990 to June 3, 1990 a VLF survey was completed

over the eight claims. Readings were taken every 100 feet along the

north south grid lines, A total of 376 readings were taken over 6.73

miles of line. The instrument used for the survey was a Geonics EM-16

and tlie station received was Cutler, Maine which operates on a freq

uency of 2AKHz. The instrument was always orientated in a north

direction. The operator for the survey was:

R.J, DillmanA2 Springbank Dr.London, Ontario.

Results of the VLF Survey

Conductor A has been traced at least 800 feet crossing lines O, AE

and 8E at approximently 5+50N, The conductor occurs over a draw which

is wet in places. This draw could be a fault. No rock is exposed within

the draw but it is bordered by gabbro on either side. On the south side

10

of the draw the gabbro outcrops have been intruded by pink potassic

f^J.dspar veinlets and injections which cause a pinkish discoloration

in the gabbro. No significant mineralization other than traces of

magnetite were observed in the area. Since Conductor A is coincedental

with a topographic depression it is suggested that Conductor A might

represent a fault. This fault may be vertical or dip steeply to the

south. Sulphide mineralization may exist along this fault because of the

occurrence of pink feldspar injections similar to that encountered on

line 34E at 1+50H.

Conductor B has been traced for at least 2400 feet striking in a

north-west, south-east direction. It is coincedental with a draw that

runs for the entire length of the property and which can be easily

recognized on an airphoto. The.drew is.assumed to mark a nearly vert

ically dipping fault. No outcrop was observed at the base of the draw

instead, the draw is littered with talised'debris and mixed till. The

draw is also wet in places and at times of the year it possibly has a

creek flowing down it. Conductor B could be the result of the combin

ation of topography and the existance of a fault. This fault" may .not

bc a suitable environment for mineralization since the fault inter

sects and cuts the mafic-syenodiorit e contact, and in doing RO, places

the tirae of faulting after plutonism.

Conductor C follows a draw running between lines 30E, 3+60H and

34E, 2+25N. The north wall of the draw is cliffed by gabbro and talised

debris lies at the base. In places along the face, pink feldspar vein-

lets occur in the gabbro. Fine disseminated magnetite was also observed

in the gabbro. The floor of the draw is wet and eventually develops

into a swamp towards the east. The south wall of the draw is made up

of a gentle slope of gabbro and basalt outcrops. On the eastern end

of the draw basalt outcrops contain copper mineralization. The area

was the site of trenching but no sulphides were seen to be massive

11

enough to be conductive. Conductor C probably represents a fault

Iraa/or conductive overburden but with the presence of copper mineral

ization in the vicinity the conductor warrants further investigation.

Conductor D is a very short conductor crossing line 34E at 0+20N.

The conductor occurs over a si.iall, circular swamp. This area is almost

entirely surrounded by outcrops of gabbro excepted on the north where

basalt outcrops occur. This conductor is probably a result of the swamp

but because it is in the area of copper mineralization it should not

be overlooked and nay represent sulphides.

Conductor R crosses lines 32E at 5 + 90S and 36E at 6+75S. This con

ductor is coincidental with a small swamp on the gabbro-syenodiorite

contact. There is no explaination for the cause of this conductor other

than it could be caused by the swamp,

Conductor F crosses lines 4E at 5+20S, 8E at 6-I-65S, and 12E at

S+50S. The conductor occurs over a swamp and marks the south contact

of a lense of basalt within the syenodiorite. The contact is not

exposed. Conductor F may;-only be an effect of the swamp but it does

occur over an interesting contact and may warrant further work.

Conductor G is a short conductor on line 44E at 6+75S, The conduc

tor occurs in very rugged terrain where the actual anomaly is situated

at the bottom of a cliff. The surrounding rock is gabbro. No sulphide

mineralization was observed in the area. This conductor is probably an

effect of topographic relief,

M a g n e t o m e t e, r S u r v e y

Between May 28 to June 3, 1990 a inag survey was completed over

the eight claims. Readings were taken every 50 feet along 7.23 miles

of grid lines. The total number of readings taken were 765. The magnet

ometer used for the survey was a Gem Systems flux gate mag. Operator

for the suvey was: R. HacNallySault Ste. Marie, Ontario

12

A strong mag high exists on line 4E at 9+50N, The surrounding

pk in the area is gabbro. As much as 3 7, magnetite was observed as

fine disseminations within the gabbr o ,; The. pr esenc e of .vUiagnet it e

is probably tlie cause of the high magnetic intensity of the area.

A- weaker mag bi.gh is" located. on line 4E at 2-fOOS and trends to

line 12E at 6+OOS, Tliis anomaly represents a lense of basalt within

the syenodiorite pluton. The anomaly is more an effect of the basalt

having a higher magnetic response than does the syenodiorite. There4

are VLF conductors coincidental with the basal t-sygnodior it e contact

which may represent sulphides.

A strong mag high exists on line 20E at 1+OON, The high is situa

ted over silicified and brecciated basalt. Trenching in the area re

vealed weakly disseminated chalcopyrite and magnetite within the

basalt. Up to 5% chalcopyrite was obsevred in a l foot wide section

of basalt, l-2% fine magnetite may account for the magnetic high of the

ar ea .

There is a large area of low magnetic intensity on line 20E between

9 + 50N and 114-OON. Prospecting of this area revealed numerous outcrops

gabbro. No alteration such as silicification has occurred to the gabbro

and there is no evidence of potassic feldspar injections. No explain-

ation for the low magnetic intensity is apparant.

A small magnetic high is located on line 24E at 2+50N. The surround

ing rock type is gabbro with X-2% fine disseminated magnetite present.

This magnetite probably accounts for the magnetic high.

A mag high of moderate intensity occurs on line 28E at 4+OON. Gabbro

was the only rock found in the area. 1 -27, f ine disseminated magnetite

was observed in the garbro which may cause the high magnetic response.

On line 28E at 7+75N there is a mag high over gabbro. Fine dissem

inated magnetite was observed in the gabbro. No other mineralization

was seen. The presence of magnetite probably causes the mag high.

13

On line 32E at 1 + 50N and trending to line 36E at 2-fOON there is

area of moderately high magnetic intensity! This high occurs over

a moderately silicified, weakly sheared basalt. Copper mineralization

consisting of chalcopyrite, bornite and native copper are dissemin

ated and occur on fracture surfaces within the basalt. Fine, dissem

inated magnetite sometimes totalling as much as 3 7, was observed in

the rock. This nag anomaly may warrant further investigation since it

is coincidental with Conductor C.

Frora line 32E at 6+50N to line 38K at 6+OON there is an area of

moderately high magnetic intensity. This high occurs over a small

area of weakly silicified gabbro? which is somewhat .similar in appear

ance to the silicified basalt located farther to the south. Traces

of disseminated magnetite were seen in the gabbro. Chalcopyrite was

also observed as fine disseminations and subsequently trenched.

On line 40E at 3 + 75N a strong mag high occurs. The rock situated

at the high is gabbro but similar in appearance to that found on line

38E at 6 + OON. The gabbro contains roughly 1 7, m agnetite but no copper

Mineralization.

Max Min Horizontal Loop Survey

The max min survey was completed between June 18 to June 30, 1990,

Harry Ferderber Geophysics Ltd, of.Val D'or, Quebec supplied a Geonics

Max Min II and an operator by the name of:

Cord Hendrickson Val D'or, Quebec.

His assistant was R. MacNally. During the survey 3.84 miles of line

xvere traversed and a total of 258 readings were taken. The frequency

used for the survey was 888 Hz. The coil separation was 400 feet.

The following is a report of the survey supplied by the contractors:

14

H. FERDERBER GEOPHYSICS LTD. GEOPHYSICAL a GEOLOGICAL SURVEYS169 PERRAULT AVENUE, VAL D'OR, QUEBEC J9P2HI TELEPHONE 619-624-2075

Memo .on the Horizontal Loop Electromagnetic Survey

on the Property of John Hamilton in the Seeley Lake Area, Ontario

The recently completed horizontal loop electromagnetic (H.L.E.M.) survey delineated the location of 8 conductive zones on

the property of John Hamilton in Seeley Lake Area, Ontario.

Because of the great many changes in local topographic relief on the property, quantitative calculations, defining properties such as dip, depth and apparent conductivity, would be largely inaccurate. Qualitative descriptions of the conductive zones are

presented in the following table.

Conductive Zone

H

I

Topography

Gully - lineament

Magnetic Correlation

VLF-EM Correlation Geology

Along slopes

In a gully and along a slope.

In a gully.

Along cliff,down to the north.

Along a creek, gully and a slope.

Along a cliff, gully and slope.

Along a slope.

In a gully and along a elope.

Along magnetic Anomaly A on lows. line O.

Along the Anomaly B on edges of lines 16 and magnetic highs.

Near anomaly C on lines 32 and 34.

Anomaly E, line 32.

Along the edge of mag netic lows.

In lows and highs.

In a low in the east and a high in the west.

Along weak highs.

In a weak low.

In weak lows. Anomaly F, line 8.

In lows.

Along a lineament representing a shear in a shear in syenodiorite and gabbro and along a diabase dyke in the east.

Near a possible shear in the east in gabbro. 28.

Located over chalcopyrite mineralization in gabbro.

In mainly gabbroic rocks near chalcopyrite mineralization.

In gabbroic rocks.

In syenodiorite.

In syenodiorite.

In syenodiorite?

15

Correlating the results of the HLEM survey, known geology and

the results of the magnetic surveys, the best targets for sulphide mineralization containing possible gold values are conductor B,

which appears to be the best conductor on the property, conductors

C and D near chalcopyrite mineralization and conductor A along a potential shear fault zone. Possible drill targets are listed below:

LI

Posi

2E,

ton

9N

Azimuth

-180 0

Dip

-50 0

Depth

350'

Target

Strongest conductor - B

L16E, 1+50N -ISO0

L32E, 7N -ISO0

L36E, 3+50N 180'

-500 350 1

-500 350

-500 350'

intersecting basalt, gabbro and a contact at a bend in the conductor axis.

Conductor A along a magnetic low and fault zone, just east of a possible syenodiorite - basalt contact.

Conductor D, testing a contact between a magnetic low and high, west of chalcopyrite minera- 1ization.

Conductor C, a possible fault zone, and syeno- diori te-gabbro-rnaf ic meta- volcanic contacts near- copper mineral ization, and across magnetic lows and highs.

Further work could also be completed over conductors A, B and I on lines 32 and east of line 32.

R.A. Campbell, Geologist

16

S o il S ampl ing S u r v ey

^^ The soil sampling survey xvas conducted in two stages. From June 4

to June 8, 1990, 107 'li 1 horizon samples were taken, During the second

stage 403 samples were taken of 'B 1 horizon soils and humus. This sam

pling occurred between July 25 to August l, 1990. Iodate, 510 soil

samples have been taken off the property but only the results of the

first stage of sampling are described in this report.

Sample collection during the first stage v.-as conducted at 50 foot

intervals along the grid lines. Sampling concentrated on testing the

geophysical anomalies to an average length of 200 feet on either side

of the anomaly. The 'B 1 horizon soil collected was usually reddish

brown in color, silty to sandy in texture t and locally contained mafic

and/or syenodiorite rock fragments. The samples were collected from a

depth of 6 inches to 2 feet.

Samples were processed at Technical Sevices Laboratories in

Mississauga, Ontario. The samples were dried and sieved through -80

mesh. They were analyzed for gold and copper by atomic absorption

techniques. Anomalous values were checked by fire assay.

The soil sampling survey showed a number of geochemical anomalies

within close proximity of the geophysical anomalies. These values

range between 30 ppb to 1000 ppb with 25 ppb gold considered the maxi

mum limit for.background, No anomalous values for copper were obtained.

A significant gold anomaly extends from line 4E to 12E and contains

peak values of gold up to 60 ppb. The anomily is coincidental with

Conductor F, This conductor follows the south contact of basalt and

syenodiorite. Although some outcrops occur in the area no mineraliz

ation was seen to suggest cause of the anomalous gold values in the

soils. Another value of 145 ppb was obtained on line 4E at the base

line. The sample was taken on outcrops of syenodiorite. Prospecting

revealed no mineralization. It is possible that a value like this

17

way have been displaced by glaciation. If this the case f urther

^P^loration should be concentrated towards the north, north-east.

This is the direction from which the glacier advanced.

Another significant gold anomaly occurs between lines 12E to 20E.

This anomaly is somewhat coinc dental with Conductor B. Gold values in

this anomaly range up to 1000 ppb. The higher values appear to flank

the conductor axis. This pattern may be an effect of glacial dispersion

or an effect of topography. The surrounding rock in the area is gabbro.

Between line 2bE and line 32E gold values were obtained in soils

over copper mineralization in silicified basalt. Values in this area

peak at 400 ppb. Conductors C and D occur in this area as well as

the south east extension of Conductor B, Although prospecting of the

area uncovered outcrops with disseminated copper mineralization no

gold values were obtained during sampling.

On line 32E over the western extension of Conductor E gold values

in the soils readied 310 ppb. The sampling was situated -over a draw

that marks the conductor axis. Outcrops of gabbro bound the draw. No

mineralization was seen in these outcrops,

During the second phase of soil sampling humus samples were taken

over outcrops and areas that were wet. Many of the anomalous values

detected during the first stage of sampling were resampled and in

places of greater soil depth a soil auger was used to increase pene

tration. After the second phase of sampling there is almost complete

coverage of the eigth claims,

Conclusions and Recommendations

The property has been suffiently covered by geophysics. There is

good correlation between the VLF and the horizontal loop surveys al

though the horizontal loop survey discovered several new conductors

such as Conductor F which was not detected by the VLF. Correlation

between the magnetics and the electromagnetics show that most conductors

18

parallel the edges of the magnetic highs suggesting that the conductors

^my r epresent contacts or faults. Since there is coincidental geochem

anomalies with the conductors further methods such as drilling should

be employed to test the anomalies. The conductors that should be con

sidered for drilling are the VLF conductors F, B, and C,

Further prospecting is reccommended. This should be concentrated

in the northern and eastern areas of the property. Particular attention

should bc given to the horizontal loop conductor F since little is

known about this anomaly.

Respectfully Submitted

Robert J. Dillman

August 15, !990

19

Statement of Qual if leat ions

With regards to this report of August 15, 1990 prepared for

John Hamilton, l, Robert J. Dillman of 42 Springbank Dr., London,

Ontario do certify that:

l , I am currently enrolled in the geology, program at the

University of Western Ontario and I have completed 14.5

credits of the 15 credit B. Se. program.

2. I have been active in in y profession since 1977,

3. I have submitted assessment work to the Ministry of Natural

Resources on behalf of various companies and for my own

personal adventures and in all cases the work has been accepted

by the Ministry.

4. I have two letters of recommendations from previous employers

concerning the quality of work on file in Toronto,

5. The information given in this report is accurate to the best

of my knowledge.

August 15, 1990 Robert J. DillmanProspector

TECHNICAL SERVICE LABORATORIESDIVISION OF BURGENER TECHNICAL ENTERPRISES LIMITED

1301 FEWSTER DRIVEMISSISSAUGA. ONTARIO

L4W 1A2(416) 625-1544 FAX: (416) 625-8368

November l, 1990

RECEIPT

Invoice # 13203# 13291# 13292# 13333# 13316# 13376# 13397# 13431# 13432# 13537# 13806

S 355.10 S 149.25 S 312.25 S 77.85 S 806.65 S 42.00 S 8.85 SI,770.00 SI,247.85 SI,433.70 S 104.60

INVOICE

INVOICE NO. 13203

btHVIUt LABORATORIESDIVISION OF 8URGENER TECHNICAL ENTERPRISES LIMITED

1301 FEWSTER DRIVEMISSISSAUQA, ONTARIO

L4W1A2© (416) 625-1544 FAX: (416) 625-8368

"O: John Hamilton 425 Walmer Rd Toronto, Ontario M5P-2X9

CODE DESCRIPTION

9 II

106 Det. Cu - Geochem106 Sample Prep. - Drying s Sieving

July 13 1990

REF. NO. M7140 P.O. #

H020

UNIT PRICE TOTAL

2.30 S 243.80 1 -05 111.30

PAID JU26tt90

Please Pay

PLE.SB ENCLOSE COPV OF INVOICE WITH PAYMENT -355.10

TERMS NET 30 DAYS

1301 FEWSTER DRIVE MISSISSAUGA, ONTARIO

L4W 1A2

(416)625-1544 f AX: (416) 625-8368

CERTIFICATE OF ANALYSIS

.MPLEtS) FROM john Hamilton 425 Walmer Ra Toronto , Ontario M5P-2X9 921-9471

INVOICE tt: P.O.:

AL

3.801.30

AMPLE(S) OF

10

CL- CL- 120 CL- 121 CL- 122 CL- 123

CL- 124

Copper Cu

102834

413

Toronto CTA

jul 05/90 SIGNED

tsssisssssssssss^ Page 6 of 6

TECHNICAL SERVICE LABORATORIESDIVISION OF BUROENER TECHNICAL ENTERPRISE S LIMITED

1301 FEWSTER DRIVEMISSISSAUGA, ONTARIO

L4W 1A2(416! 625-1544 FAX (416) 625-8368


SAMPLE(S) FROM John Hamilton 425 Walmer Rd Toronto , Ontario M5P-2X9 921-9471

SAMPLE(S) OFSoil

REPORT No.

M7140

INVOICE #: P.O. :

CL- 6 CL- 7 CL- 8 CL- 9 CL- 10

CL- 11 CL- 12 CL- 13 CL- 14 CL- 15

CL- 16CL- 17CL- 18CL- 25CL- 26

CL- 27CL- 28CL- 29CL- 30CL- 31

Copper Cu ppm

151246

13

1127444412

264112228

8121559

COPIES TO:INVOICE TO: Toronto

Jul 05/90 CTA

SIGNED

for enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report

Page l of 6



L4W 1A2©(41616251544 FAX: (416) 625-8368



SAMPLE(S) OFSoil

REPORT No.

M7140

INVOICE #: P.O. :

CL- 32 CL- 33 CL- 34 CL- 35 CL- 42

CL- 43 CL- 44 CL- 45 CL- 46 CL- 47

CL- 48CL- 50CL- 51CL- 52CL- 53

CL- 54CL- 55CL- 56CL- 57CL- 58

COPIES TO: INVOICE TO:

Jul 05/90

Copper Cu ppm

299

143723

2630342914

16183

727

1112181536

Toronto

CTA

SIGNED

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report

Page



L4W 1A2 (416)625-1544 FAX: (416) 625-8368



SAMPLE(S) OFSoil

REPORT NO.

M7140

INVOICE #: P.O. :

CL- 59CL- 60CL- 61CL- 62CL- 63

CL- 64CL- 65CL- 66CL- 67CL- 68

CL- 69CL- 70CL- 71CL- 72CL- 73

CL- 74CL- 75CL- 76CL- 77CL- 78


Jul 05/90

Copper Cu ppm

102415157

415332197

53143456

3915143413

Toronto

SIGNEDCTA

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report.

Page 3 of 6

TECHNICAL SERVICE LABORATORIESDIVISION O F 8URGENER TECHNICAL E NTERPRISES LIMITED


L4W 1A2©(416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM

SAMPLE(S) OF

John Hamilton 425 Walmer Rd Toronto , Ontario M5P-2X9 921-9471

Soil

REPORT No.

M7140

INVOICE #: P.O. :

CL- 79 CL- 80 CL- 81 CL- 82 CL- 83

CL- 84 CL- 85 CL- 86 CL- 87 CL- 88

CL- 89 CL- 90 CL- 91 CL- 92 CL- 93

CL- 94CL- 95CL- 96CL- 97CL- 98

Copper Cu ppm

23645

1625

1338502211

1312544

10

16699

39


Jul 05/90SIGNED

CTA


Page 4 of 6

TECHNICAL SERVICE LABORATORIESDIVISION O F BURGENER T ECHNICAL ENTERPRISES LIMITED


L4W 1A2 (416)625-1544 FAX: (416) 625-8368



SAMPLE(S) OFSoil

REPORT No.

M7140

INVOICE #: P.O.:

CL- 99 CL- 100 CL- 101 CL- 102 CL- 103

CL- 104CL- 105CL- 106CL- 107CL- 108

CL- 109CL- 110CL- 111CL- 112CL- 113

CL- 114 CL- 115 CL- 116 CL- 117 CL- 118


Jul 05/90

Copper Cu ppm

1828112011

3030199

23

8262465

2299

2810

Toronto

SIGNEDCTA


Page 5 of 6

TO: John Hamilton 425 Walmer Rd. Toronto, Ontario MSP 2X9

TECHNICAL SERVICE LABORATORIESDIVISION OF BUROENER TECHNICAL ENTERPRISES LIMITED

INVOICE

INVOICE NO. 13291


L4W 1A2(416) 625-1544 FAX: (416) 625-8368

July 18 1990

REF. NO. M7219 P.O. #

H020

CODE

98

DESCRIPTION

15 Det. Au by FA/AA 2 Det. Au by FA

UNIT PRICE

S 8.65 9.75

TOTAL

129.7519.50

PAID JUL26890

—————— Please Pay —————— S 149.25

PLEASE ENCLOSE COPY OF INVOICE WITH PAYMENT - TERMS NET 30 DAYS



L4W 1A2 (416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton 425 Walmer Rd. Toronto, Ontario MSP 2 X9

SAMPLE(S) OF Soil

REPORT No.

M7219

INVOICE #: P.O. :

Old M7140

CL-CL-CL-CL-CL-

CL-CL-CL-CL-CL-

CL-CL-CL-CL-CL-

4243444546

4748505152

5354555657

GoldAu ppb

55

^0005

10

155555

105^5

10

Gold Au oz/t

0.016 (0.014, 0.017)


Jul 17/90

Toronto

SIGNEDCTA


Page l of l


TbUINIUAL btHVIOt LABOHAIUHIbS

INVOICE

INVOICE NO. 13292

DIVISION OF BURQENER TECHNICAL ENTERPRISES LIMITED


L4W 1A2© (416) 625-1544 FAX: (416) 625-8368

July 18 1990

REF. NO. M7238 P.O. #

H020

CODE

911

DESCRIPTION

23 Det. Au by FA22 Sample Preparation

UNIT PRICE

S 9.75 4.00

TOTAL

224.2588.00

PAID JUL26 1990

--------- Please Pay ---------

PLEASE ENCLOSE COPY OF INVOICE WITH PAYMENT

312.25

NET 30 DAYS



L4W 1A2©(416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM Jonh Hamilton 425 Walmer Rd. Toronto, Ontario MSP 2X9

REPORT No.

M7238

SAMPLE(S) OF RockINVOICE #: P.O.:

2080120802209012090220903

2090420905209062090720908

2090920910209112091220913

2091420915209162091720918


Jul 17/90

Gold Au oz/t

^.005 ^.005

^.005 ^.005

^.005 ^.005 *:0.005

^.005

^.005 <0.005 <0.005 <0.005 ^.005

<0.005 <0.005 <0.005 <0.005 ^.005

Toronto

SIGNED

CTA


Page l of 2

?TECHNICAL SERVICE LABORATORIES

DIVISION OF BURGENER TECHNICAL ENTERPRISES LIMITED


L4W 1A2 (416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM Jonh Hamilton 425 Walmer Rd. Toronto, Ontario M5P 2X9

REPORT No.

M7238

SAMPLE(S) OF RockINVOICE #: P.O. :

2091920920 NO NAME

Gold Au oz/t

^.005 ^.005 <0.005


Jul 17/90

Toronto

SIGNEDCTA


Page 2 of 2


TECHNICAL SERVICE LABORATORIESDIVISION OF BURQENER TECHNICAL ENTERPRISES LIMITED

INVOICE

INVOICE NO. 13333

CODE

9

DESCRIPTION

9 Det. Au by FA/AA


L4W 1A2 (416) 625-1544 FAX: (416) 625-8368

July 25 1990

REF. NO. P.O. # M7219 H020

M7289

UNIT PRICE

S 8.65

TOTAL

77.85

--------- Please Pay --------- v


77.85



L4W 1A2 (416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton 425 Walmer Rd. Toronto, Ontario MSP 2X9

REPORT No.

M7289

SAMPLE(S) OF RejectsINVOICE #: P.O.:

M7219

Gold Au ppb

CL 42 CL 43 CL 45 CL 46 CL 47

CL 48 CL 50 CL 51 CL 52

505

<5 <5


Jul 23/90

Toronto

SIGNEDCTA


Page l of l

TO: John Hamilton 425 Walmer Rd. Toronto, Ontario M5P 2X9


INVOICE

INVOICE NO. 13316


L4W 1A2© (416) 625-1544 FAX: (416) 625-8368

July 25 1990

REF. NO. P.O. #

H020

M7239

CODE

98

DESCRIPTION

91 Dst. Au by FA/AA 2 Det. Au by FA

UNIT PRICE

$ 8.65 9.75

TOTAL

787.1519.50

—— ——— Please Pay ——————— S 806.65




L4W 1A2©(416)6251544 FAX: (416) 625-8368


SAMPLEIS) FROM john Hamilton425 Walmer Rd. R EPORT N o 'Toronto, Ontario MSP 2X9

M7239

INVOICE #: SAMPLE(S) OF Soil P.O.:

Same as M7140

Gold Gold Au ppb au oz/t

CL- 6 145CL- 7 40CL- 8 5CL- 9 10CL- 10 < 5

CL- 11 5CL- 12 15CL- 13 15CL- 14 10CL- 15 10

CL- 16 5CL- 17 35CL- 18 5CL- 25 ^CL- 26 5

CL- 27 10CL- 28 ^CL- 29 5CL- 30 5CL- 31 5

COPIES TO: John Hamilton INVOICE TO: Toronto

Jul 19/90SIGNED

For enquiries on this report, please contact Customer Service Department. Page l of 5 Samples, Pulps and Rejects discarded two months from the date of this report.



L4W 1A2 (416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM john Hamilton 425 Walmer Rd. Toronto, Ontario MSP 2X9

SAMPLE(S) OF Soil

REPORT No. M7239

INVOICE #: P.O.:

Same as M7140

Gold Au ppb

Gold au oz/t

CL- 32 CL- 33 CL- 34 CL- 35 CL- 58

CL- 59CL- 60CL- 61CL- 62CL- 63

CL- 64CL- 65CL- 66CL- 67CL- 68

CL- 69CL- 70CL- 71CL- 72CL- 73

60 ^ 25

100225 (860, 30)

1515

520 30

135 (400,


Jul 19/90

0.015 (0.023, 0.007)

SIGNEDCTA


Page 2 of 5



L4W 1A2(416) 625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton 425 Walmer Rd. Toronto, Ontario M5P 2X9

REPORT No. M7239

INVOICE #:SAMPLE(S) OF goil P.O.:

Same as M7140

Gold Gold Au ppb au oz/t

CL- 74 110CL- 75 5CL- 76 125CL- 77 120CL- 78 10

CL- 79 75CL- 80 55CL- 81 ^CL- 82 ^CL- 83 120

CL- 84 30CL- 85 155CL- 86 310CL- 87 5CL- 88 145

CL- 89 140 (280, ^)CL- 90 ^CL- 91 40CL- 92 ^CL- 93 15

COPIES TO: John HamiltonINVOICE TO: Toronto

Jul 19/90SIGNED

For enquiries on this report, please contact Customer Service Department. Page 3 Of 5 Samples, Pulps and Rejects discarded two months from the date of this report.

TECHNICAL SERVICE LABORATORIESDIVISION OF 8URGENER TECHNICAL ENTERPRISES LIMITED


L4W 1A2 (416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton 425 Walmer Rd. Toronto, Ontario MSP 2X9

REPORT No. M7239

INVOICE #: SAMPLE(S) OF goil P.O.:

Same as M7140

CL- 94CL- 95CL- 96CL- 97CL- 98

CL- 99CL- 100CL- 101CL- 102CL- 103

CL- 104CL- 105CL- 106CL- 107CL- 108

CL- 109CL- 110CL- 111CL- 112CL- 113

GoldAu ppb

2017010

150 (300, 5)115 (210, 15)

^557511515

2010103075

^255

135<5

Gold au oz/t


Jul 19/90SIGNED

For enquiries on this report, please contact Customer Service Department. Page 4 of 5 Samples, Puips and Rejects discarded two months from the date of this report.



L4W 1A2(416) 625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton 425 Walmer Rd. Toronto, Ontario M5P 2X9

SAMPLE(S) OF

REPORT No. M7239

INVOICE #: P.O.:

Same as M7140

Gold Au ppb

Gold au oz/t

CL- 114 CL- 115 CL- 116 CL- 117 CL- 118

CL- 119 CL- 120 CL- 121 CL- 122 CL- 123

CL- 124

rt 10 rt rt rt

<5


Jul 19/90

John Hamilton Toronto

SIGNED

CTA


Page 5 of 5



INVOICE

INVOICE NO. 13376


L4W1A2© (416) 625-1544 FAX: (416) 625-8368

July 31 1990

REF. NO. P.O. #

H020

M7354

CODE

10

DESCRIPTION

5 ICP Multi Element Pkg.

UNIT PRICE TOTAL

S 8.40 S 42.00

————— -. Please Pay ———— — - $ 42.00


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3 3

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2".

13

32

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SS

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TO: John Hamilton425 Walmer Road Toronto, Ontario MSP 2X9


INVOICE

INVOICE NO. 13397


L4W 1A2© (416) 625-1544 FAX: (416) 625-8368

Aug. 2 1990

REF. NO. P.O. #

H020

M7446

CODE

911

DESCRIPTION

l Det. Au by FA/AA l Sample Preparation

UNIT PRICE

S 7.80 1.05

TOTAL

7.801.05

——-—.-- please Pay --------- S 8.85




L4W 1A2©(416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton425 Walmer Road Toronto, Ontario MSP 2X9

REPORT No.

M7446

SAMPLE(S) OF SoilINVOICE #: P.O.:

Gold Au ppb

CL-49


Aug 02/90

Toronto

SIGNEDCTA


Page l of l

TO: John Hamilton425 Walmer Road Toronto, Ontario MSP 2X9


INVOICE

INVOICE NO. 13431


L4W 1A2© (416) 625-1544 FAX: (416) 625-8368

Aug. 10 1990

REF. NO. M7452 P.O. #

H020

CODE

911

DESCRIPTION

200 Det. Au by FA/AA 200 Sample Preparation

UNIT PRICE

S 7.80 1.05

TOTAL

1560.00210.00

——— --— Please Pay ——----- S 1770.00




L4W 1A2©(416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton

425 Walmer Road Toronto, Ontario MSP 2X9

REPORT No.

M7452

SAMPLE(S) OF SoilINVOICE #: P.O. :

25012502250325042505

25062507250825092510

25112512251325142515

25162517251825192520


Aug 09/90

Gold Au ppb

1030

<5

<5 ^ <5 5

<5

<5 5 5^ <5

Toronto

SIGNEDCTA

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report. Page l of 10



L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7452


Gold Au ppb

25212522252325242525

25262527252825292530

25312532253325342535

25362537253825392540


Aug 09/90

<5<5

<5 <5 ^ <5 <5

<5 <5 ^ <5 <5

Toronto

SIGNEDCTA

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report. Page 2 of 10



L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7452


Gold Au ppb

25412542254325442545

25462547254825492550

25512552255325542555

25562557255825592560


Aug 09/90

<5 <5 <5

<5 ^ <5 <5 <5

<5 ^ 20 <5 <5

Toronto

SIGNEDCTA




L4W 1A2©(416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton 425 Walmer Road Toronto, Ontario MSP 2X9

REPORT No.

M7452


Gold Au ppb

25612562256325642565

25662567256825692570

25712572257325742575

25762577257825792580


Aug 09/90

10^5

<5 ^<5 <5 <5

<5 ^ <5 5

<5

Toronto

SIGNEDCTA




L4W 1A21(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7452

SAMPLE(S) OFSoil

INVOICE # P.O.:

Gold Au ppb

25812582258325842585

25862587258825892590

26012602260326042605

26062607260826092610

510

52555

155^50

10 5^ 5 5


Aug 09/90

Toronto

SIGNEDCTA




L4W 1A2(416) 625-1544 FAX: (416) 625-8368



REPORT No.

M7452


Gold Au ppb

26112612261326142615

26162617261826192620

26212622262326242625

26262627262826292630

<5^5

<5

<5<5^55

10 <5 ^ <5 <5


Aug 09/90

Toronto

SIGNEDCTA




L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7452


Gold Au ppb

26312632263326342635

26362637263826392640

26412642264326442645

26462647264826492650


Aug 09/90

55

10 ^ ^ <5

<55 ^<5 <5

Toronto

SIGNEDCTA




L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7452

SAMPLE(S) OF SoilINVOICE #:P.O.:

Gold Au ppb

26512652265326542655

26562657265826592660

26612662266326642665

26662667266826692670

<5t55^5

^5^55

^<55^5

1510^<55


Aug 09/90

Toronto

SIGNEDCTA




L4W 1A2(416) 625-1544 FAX: (4161 625-8368



REPORT No.

M7452

SAMPLE(S) OFSoil

INVOICE #: P.O.:

Gold Au ppb

26712672267326742675

26762677267826792680

26812682268326842685

26862687268826892690


Aug 09/90

55

105

105

105

55

10

Toronto

SIGNEDCTA


TECHNICAL SERVICE LABORATORIESDIVISION OF BURGENIER TECHNICAL ENTERPRISES LIMITED


L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7452


Gold Au ppb

26912692269326942695

26962697269826992700

27012702270327042705

27062707270827092710


Aug 09/90

1555

105

45

555

Toronto

SIGNEDCTA


INVOICE

INVOICE NO. 13432

TO: John Hamilton425 Walmer Avenue Toronto, Ontario MSP 2X9

out ivivxi-DIVISION OF BURQENER TECHNICAL ENTERPRISES LIMITED


L4W 1A2© (416) 625-1544 FAX: (416) 625-8368

Aug. 10 1990

REF. NO. M7453 P.O. #

H020

CODE

911

DESCRIPTION


UNIT PRICE

S 7.80 1.05

TOTAL

1099.80148.05

——————— Please Pay ——————— S 1247.85




L4W 1A2©(4161625-1544 FAX: (416) 625 8368


SAMPLE(S) FROM John Hamilton425 Walmer Avenue Toronto, Ontario MSP 2X9

SAMPLE(S) OF Soil

REPORT No.

M7453

INVOICE #: P.O.:

Gold Au ppb

27112712271327142715

27162717271827192720

27212722272327242725

27262727272827292730


Aug 09/90

<5 <5 <5 <5

<5 <5 <5 <5

<5<5<5 <5

Toronto

SIGNED//) ' dO Xx^--*-^-^^-xy--X' CTA


Page l of 8



L4W 1A2©1416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM john Hamilton425 Walmer Avenue Toronto, Ontario MSP 2 X9

SAMPLE(S) OF Soil

REPORT No. M7453

INVOICE #: P.O. :

Gold Au ppb

27312732273327342735

27362737273827392740

27412742274327442745

27462747274827492750

<55^ <55

10 5^ 5

<5


Aug 09/90

Toronto

SIGNEDCTA


Page 2 of 8



L4W 1A2©{416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton 425 Walmer Avenue Toronto, Ontario MSP 2X9

REPORT No.

M7453


Gold Au ppb

27512752275327542755

27562757275827592760

27612762276327642766

27682769277027712772


Aug 09/90

15

<5 <5 <5

5 <55

<5

Toronto

SIGNEDCTA




L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7453


Gold Au ppb

27732774277527762777

27782779278027812782

27832784278527862787

27882789279027912792

<5455

<5^

^5^5

15

^<5<5<5<5

^<5<5<5<5


Aug 09/90

Toronto

SIGNEDCTA




L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7453


Gold Au ppb

27932794279527962797

27982799280028012802

28032804280528062807

28082809281028112812


Aug 09/90

<5 ^ <5 <5 5

<5 ^ <5 <5 <5

Toronto

SIGNEDCTA


Page 5 of 8



L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7453


Gold Au ppb

28132814281528162817

28182819282028212822

28232824282528262827

28282829283028312832

^^^^^

^^^^^

<5^<5<5<5

<5^<5<5<5


Aug 09/90

Toronto

SIGNEDCTA




L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7453

SAMPLE(S) OFSoil

INVOICE # P.O. :

Gold Au ppb

28332834283528362837

28382839284028412842

28432844284528462847

28482849285028512852


Aug 09/90

80

10

55

<5 5^ 30 50

Toronto

SIGNEDCTA




L4W 1A2©(416)625-1544 FAX: (416! 625-8368



REPORT No.

M7453

SAMPLEISIOF 0 0 Soil P.O.:

Gold Au ppb

2853


Aug 09/90

Toronto

SIGNEDCTA

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report. o O o

TECHNICAL SERVICE LABORATORIESDIVISION OF BURQENER TECHNICAL ENTERPRISES LIMITED

INVOICE

INVOICE NO. 13537

TO: John Hamilton425 Walmer Avenue Toronto, Ontario MSP 2X9


L4W1A2© (416) 625-1544 FAX: (416) 625-8368

Aug. 17 1990

REF. NO. P.O. #

H020

M7498

CODE

911

DESCRIPTION


UNIT PRICE

S 7.80 1.05

TOTAL

1263.60170.10

— — -——— Please Pay —— —— -- S 1433.70


TECHNICAL SERVICE LABORATORIESDIVISION OF BUHGENER TECHNICAL ENTERPRISES LIMITED


L4W 1A2©(416)625-1544 FAX: (4161 625 8368


SAMPLE(S) FROM John Hamilton 425 Walmer Avenue Toronto, Ontario M5P 2X9

REPORT No.

M7498


Gold Au ppb

2070120702207032070420705

2070620707207082070920710

2071120712207132071420715

2071620717207182071920720

10105

55

5

5

5


Aug 16/90

Toronto

SIGNEDCTA

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report. Page l of 9



L4W 1A2©(416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton,-- , REPORT No.425 Walmer AvenueToronto, Ontario MSP 2X9

M7498

SAMPLE(S)OF c .. INVOICE *:Soil P.O.:

Gold Au ppb

20721 ^20722 ^20723 <520724 <520725 ^

20726 <520727 ^20728 <520729 <520730 ^

20731 <520732 ^20733 520734 520735 ^

20736 <520737 2020738 ^20739 <520740 ^


Aug 16/90 ( /fo^^^JL y**budL: Pi

For enquiries on this report, please contact Customer Service Department. o -F o Samples, Pulps and Rejects discarded two months from the date of this report. a^e O



L4W 1A2©(416)625-1544 FAX: (416) 625 8368


SAMPLE(S) FROM John HamiltonA^ , , , , REPORT No. 425 Walmer AvenueToronto, Ontario MSP 2X9

SAMPLE.SIOF Q .. nTICESoil P.O.:

M7498

Gold Au ppb

20741 ^20742 <52854 ^2855 <52856 <5

2857 ^2858 <52859 < 52860 <52861 <5

2862 ^2863 <52864 ^2865 <52866 <5

2867 ^2868 <52869 ^2870 <52871 <5


Aug 16/90 C^^J/Ji-^^L^^C.- c r^SIGNED

For enquiries on this report, please contact Customer Service Department. 0 *0 Samples, Pulps and Rejects discarded two months from the date of this report, "



L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7498


Gold Au ppb

28722873287428752876

28772878287928802881

28822883288428852886

28872888288928902891


Aug 16/90

<5 <5 <5

<5 <5 <5 <5

Toronto

SIGNEDCTA




L4W 1A2 ©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7498

SAMPLE(S) OF SoilINVOICE # P.O. :

28922893289428952896

28972898289929002901

29022903290429052906

29072908290929102911


Aug 16/90

Gold Au ppb

15 ^ 5

555

<5 <5

Toronto

SIGNEDCTA


TECHNICAL SERVICE LABORATORIESDIVISION OF BUROENEH TECHNICAL ENTERPRISES LIMITED


L4W 1A2©(416)625-1544 FAX: (416) 625-8368



REPORT No.

M7498


Gold Au ppb

29122913291429152916

29172918291929202921

29222923292429252926

29272928292929302931


Aug 16/90

5

5

<5

<5 ^ <555

Toronto

SIGNEDCTA




L4W 1A2 ©(416)625-1544 FAX: (416) 625-8368


SAM PLE(S) FROM -.^^n Han^ H-or,John Hamilton REPORT No. 425 Walmer AvenueToronto, Ontario MSP 2X9

M7498

SAMPLE(S)OF c .. INVOICE *: Soil P.O.:

Gold Au ppb

2932 ^2933 rt2934 rt2935 <52936 <5

2937 52938 rt2939 rt2940 52941 <5

2942 rt2943 <52944 52945 rt2946 <5

2947 52948 102949 ^2950 ^2951 5


Aug 16/90 fiSC^^jyt\ /^U4^4L* ^SIGNED

For enquiries on this report, please contact Customer Service Department.Samples, Pulps and Rejects discarded two months from the date of this report. rage f or y



L4W 1A2©(416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton 425 Walmer Avenue Toronto, Ontario M5P 2X9

REPORT No.

M7498


29522953295429552956

29572958295929602961

29622963296429652966

29672968296929702971


Aug 16/90

Gold Au ppb

15

515

555

10

52055

Toronto

SIGNEDCTA


4 11



L4W 1A2©(416)625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton^r- ,, -, , REPORT No. 425 Walmer Avenue

MSP 2X9

SAMPLE(S) OF

Toronto, Ontario M7498

c ..Soil P.O.

Gold Au ppb

29722973


Aug 16/90SIGNED

For enquiries on this report, please contact Customer Service Department. ^ ^ ^Pacrft 9 of 9Samples, Pulps and Rejects discarded two months from the date of this report. **y^ ^ "*

A/-

eft-

* 01*

II9'

n

\

TT x/? X A ~ ;

- x

z: y- z: X 7 2:' ^ c ^ S'-21 x s: x ^•t tf^JS X A Y 5V r X ?x 5

- H

- r,- i

TO: John Hamilton 425 Walmer Road Toronto, Ontario MSP 2X9


INVOICE

INVOICE NO. 13806


L4W 1A2© (416) 625-1544 FAX: (416) 625-8368

Aug. 31 1990

REF. NO. P.O. #

H020

M7538

CODE

101211

DESCRIPTION

4 Det. Pt, Pd4 Gold 4- 344 Sample Preparation

UNIT PRICE

$ 11.1511.004.00

TOTAL

44.6044.0016.00

—-———- please Pay ------—- S 104.60




L4W 1A2(416) 625-1544 FAX: (416) 625-8368


SAMPLE(S) FROM John Hamilton

425 Walmer Road Toronto, Ontario MSP 2X9

REPORT No.

M7538

SAMPLE(S) OF RockINVOICE #: P.O. :

Pt

1234

1019

Pd ppb

14108

18


Aug 22/90

Toronto

SIGNEDCTA

For enquiries on this report, please contact Customer Service Department. Samples, Pulps and Rejects discarded two months from the date of this report. Page l of l

f TECHNICAL SERV I CE LABORATORli \

Sample description AU A6 AS BA BR CA CO CR CS FE HF H6 IR HO NA NI R8 SB SC SE SNPPB PPM PPH PPM PPM i m m, m i m m m m m PPK PPH PPH PPH PPH i

i

1

t

2 l (5 6 200 {i 8 37 43 16 8^88 4 (l {5 {5 17300 {50 {30 U 28 (5 {0J23 {S XS Q 1 200 4 3 33.. 78.. 28.01 4 (l . tt 8 28000. . {50 O0 X6.2 21 {5 {0.024 9 (S 7 530 (i 5 34 67 4 8.55 3 {l 6 {524800 {50 {30 0.4 22 {5 {0.02

i r i

l

l

TECHNICA i ocrRVICE LABORATORIES M7538

C'*Mti SR TA TH U y 2K( LA CE ND SH EU IB YB LU? PPH m m m m PPN PPH PPH PPM PPM PPM .PPM PPH i i

1234

{0.05{0.050.10

{0.05

0

o

at

5.28.18.S0 'J

2.42.33.02.3

{411{4{4

{50280130110

696975.73

130130140130

6159

...68.62

8.58.2S.5 .9.0

2.8 {0.5 2.72 0.452.5 1.5 3.29 0.42

. 3.0 1.5. .2.48 0.512.9 {0.5 2.83 0.47

,J

I n^r o d u c t i p n

The Hamilton property is located adjacent to Coubran Lake in the

township of Seeley Lake, district of Thunder Bay. Access can bc made

by following a logging road running north of highway #17 at approximately

24 km west of the town of Marathon. The logging road takes you to

Coubran Lake and a short boat trip places you on the property.

The Hamilton property consists of 30 claims but only 8 claims were

surveyed. All claims are held by:

Annette Hamilton 426 Waliru&r Rd . Toronto, Ontario

The eight claims covered by various geological and geophysical

surveys arc: 1111360 to 1111367 inclusive. These cMiras were staked and

recorded on October 12, 1989. After staking, cutting of an east-west

baseline with north-south crosslines commenced from October 12 to October

20th, 1989.

Line spacing is 400ft and both the baseline and crosslines arc pickettcd

at 100ft intervals. Uetween May 28, 1990 to June 14, 1990 the surveys of

magnetometer, VLF, soil sampling, geological mapping, prospecting and

trenching were preformed over the e i gil t claims.

G cology

'J'h e eight claims lie t li e Port Coldwell ma-fcic intrusive complex. On

the north half of the grid the most dominate rock type is gabbro. It is

quite extensive, reasonably fresh looking and shows little to no altera

tion, basalt occurs within the gabbro as small isolated lenses. The

basalt shows minor shearing fractures and in places it is weakly silic

ified and carbonated. Botn rock types generally trend east-west. Also

noted in the mafic volcanics was a slightly higher than usual content of

(2)

the accessory mineral magnetite. This was especially evident in the

basalt.

A number of small discontinuous diabase dykes were observed in the

mafic volcanics. The dykes have an east-west trend.

In the southern half of the property syenodiorite is the dominate

rock type. It is thought to be the youngest rock type on the property

since in places, it forms small randomly oriented dykes that cross cut

the mafic volcanics*

f*

The mafic rocks also show sy.nite alteration and is evident by a

pinkish stain. The syenite alteration becomes pronounced along adjacent

rocks to faulting.

Running east to west across the property are a number of valley draws.

These characteristically have a cliff representing one wall and the other

consisting of gently rising outcrops. On an airphoto these features can

be easily recognized. The draws are thought to be low angle normal or

thrust faults. Their movement shows little to no alteration effects on

the rocks.

VLF Survey

From May 2, 1990 to June 3, 1990 a VLF survey was completed over the

8 claims. Readings were taken every 100ft along the north-south grid

lines. A total of 376 readings were recorded over 6.73 miles of lines.

The instrument used was a Geonic's EM-16 and the station used was Cutler,

Maiiie which operates at 16.8 KHz. The instrument was always orientated

in a north direction. The operator was:

R.J. Dillman42 Springbank Dr.London, Ontario

(3)

VLF Results

Conductor A was traced for at least 800ft crossing lines OK at

54-75i\, 4E at 5+50N and 8E at 5+40H. The conductor appears to occur

within gabbro. It follows a topographic depression which is wet in

places. Along the south side of the depression runs a small cliff

of gabbro tnat has been weakly altered by syenite. A weak mag high

is associated with this conductor. Outcrops adjacent to the conduct

or show no mineralization other than fine disseminated magnetite.

This conductor might represent a fault.

Conductor B trends in a easterly direction for at least 2800ft,

almost the entire length of the eight claims. This conductor follows

a topographic depression that can be easily recognized on an airphoto.

In the west end of the conductor, gabbro can be found on either side of

the valley walls. Towards the east gabbro dominates the north side of

the valley while syenodiorite occurs along the south. The gabbro side

is cliffed and talus ed and a creek runs through the base. The conduct

or associated with thisjvalley is a result of topography and faulting.

Conductor C follows a topographic depression running from lineSOE,

3+faON to line 34E, 2+25w. The north wall of the depression consists of

a cliff of gabbro with talus debris at the base. The gabbro along the

cliff is soue times altered by syenite. The south wall of the valley

consists of gently rising outcrops of gabbro and basalt.

Towards the easterly end of the depression (L34E,2+OON) numerous

outcrops in an area approximately 200 X200 feet were found to have

scattered copper mineralization. The mineralization consisting of

chalcopyrite, bornite, native copper and malic hite occur within thin

(4)

syenite filled fractures and unconsistantly disseminated through a weak

ly sheared and silicified basalt. This mineralization never totals more

than l 'A a nd could not account for the conductor.

Conductor D is a very short conductor on L34K, 0+20N. The area is

a low bog which is entirely surrounded by outcrops of gabbro on the west,

south, and east, and by basalt to the north. The conductor may be due to

the contact between gabbro and basalt but it is most liekly an effect of

tiie wet overburden.

Conductor K follows a topographic depression crossing line 32E, 5+90S

and line 36K, 64-75S. A cliff consisting of syenite altered gabbro marks

the north wall while syenodiorite dominates the south wall. A small

creek occuppies the base of the depression. This conductor is probably a

result of the syenodiorite - gabbro contact, which may be faulted, and the

topograpny of the area.

Conductor F crosses lines AE, 5+20S; L8E, 6+65S, and L12E 8+50S. The

conductor parallels a wet topographic low which marks the south contact

of a lense of basalt within the syenodiorite. No mineralization was found

in any of the adjacent outcrops although the actual contact was not ob

served .

Conductor G is a short conductor on L 4 4 E , 6 + 75S. l1 h e conductor is

situated in very rugged terrain and occurs at the base of a gabbro cliff.

'Ao mineralization was observed in the cliff or in talus debris at tiie

base. This conductor is probable a result of topographic relief.

Conclusions and Recommendations

While preforming the V L F survey all conductors were prospected.

Since the conductor axises predominately lie in topographic lows they

could not be observed. Adjacent outcrops where prospected but no mineral-

(3)

ization was seen. Due to the relationship of the conductor axis location

and topography interpretation of the conduc tor s., is. confusing . It is

therefore recommended that a max-min survey be preformed to filter out

any topographically induced conductors and establish sulphide conductors.

Since prospecting techniques failed in locating sulphides in any of the

conductor vacinities, except at conductor C, a max J—win survey may locate

non-surfacing sulphide mineralization. Particular attention should be

focused on conductor C because of the local copper mineralization. Also,

attention should be placed on conductor F which appears to occur along a

basalt-syenodiorit e contact.

Magnetometer Survey

A total of 7.23 miles were traversed with a magnetometer. Readings

were taken every 50 feet along the north-south running grid lines. The

total number of readings taken are 765. Eight claims were covered by the

survey;- 1111360 to 1111367 inclusive. The magnetometer used for the

survey was a flux gate mag made by Gem Systems. The operator was:

R. MacKallySault St. Marie, Ontario

The survey was completed between May 28 to June 3, 1990.

Results and Conclusions

During the magnetometer survey all mag highs and lows were prospected,

A strong mag high exists on L4E, 9+50N. The surrounding rock type is a

fine grained gabbro. It contains up to 3/i fine disseminated magnetite.

No other mineralization was observed.

On Line 4 K, 2-t-OOS and trending south east to L12E, 6+OOS is a weak

mag high. This is an interesting anomily since it represents a lense of

(6)

basalt held within the syenodiorite complex. T li ere is a coin cede ntal

VLF anomily over the ,mag anomily. It is possible that sulphides may

exist along the basalt-syenodiorite contact.

A strong mag high exists on L20E, 1+OON. Prospecting of this area

revealed a highly magnetic basalt which has been sheared and brecciated.

The basalt was strongly carbonated and silicified. Trenching in the area

revealed weak chalcopyrite in unconsistant disseminations through the rock.

Up to 52 chalcopyrite was observed in at least one narrow l foot wide zone

but could not be traced for any distance. Fine disseminated magnetite

was noted to be evenly distributed throughout the basalt. On L20E between

9+50N and l1+OON there exists a large area of low magnetic intensity.

Prospecting of the area revealed numerous outcrops of gabbro. This gabbro

showed no signs of silicification but fine disseminated magnetite was

present. No other mineralization was observed.

A small mag high exists on L24E 2+50N. The surrounding rock is gabbro.

Fine disseminated magnetite was observed but there is no presence of other

types of sulphide mineralization.

At L2SE, 4+OOK a mag high exists. This high lies in gabbro. Other

than fine disseminated magnetite no other sulphides were observed.

On L28E, 7+75N there is a strong mag high. The surrounding rock is

gabbro with fine disseminated magnetite. No other sulphide mineralization

was ob served.

On L32E at H-50N and trending cast to L36, Q+75H and 24-OON there is

an area of magnetic high intensity. This high represents a weakly sheared

basalt. Within a number of outcrops inconsis t ant ly d isseircina t cd copper

mineralization anti magnetite are present. The copper mineralization, also

seen on fracture plains consists of chalcopyrite, bornite, and native

copper. No'where was this mineralization seen to total more than 1 7, o f

(7)

of the rock. Numerous trenches were blasted in the area.

Also on line 32E at 6 + 50 there is a rnag high which extends from

L32E, 5 + 75N to L38K, 6 + OOK. This high represents a weakly sheared gabbro

which is somewhat similar in appearence to tiie sheared basalt found further

south. Fine disseminated magnetite occurs throughout the gabbro. On L34E

between 5+OON to 6-fOON weak disseminated chalcopyrite was observed and

trenched. The amount of chalcopyrite was always less than IX.

A strong mag high exists on L40E, 3+75N. The rock, a weakly sheared

gabbro, is similar in appearence to that of the mag high on L34E, 6+75N.

No mineralization was observed except for disseminated magnetite.

Recommen d a t ions

The only areas of high intensity magnetics that are of interest are

found L34E at 2-fOON and 64-75N. Because of the copper mineralization - ;.

observed in these areas further work is recommended. A max-min survey

is suggested so that near surface concentrations of copper sulphides could

be located.

Soil Sampling

To test the VLF anomilics geochemical soil sampling methods were

employed. Sampling of "li" horizon material over the conductors was con

ducted along grid lines at 50ft intervals. Samples were sent to Technical

Services Laboratories in Mississauga. The samples were dried and sieved

through 80 mesh screen and assayed for Au and Cu by atomic absorbtion

methods. Anomulous values were checked by fire assay.

Soil sampling was preformed in two stages. From June 4 to June 8, 1990,

107 "B" horizon samples were taken on average length of 200 on either

side of the conductor axis. After the results of this sampling were

oiWiined furtaer sampling of "ii" horizon material were taken to establish

complete coverage of the 8 claims. A total of 510 samples were taken

during the second stage of sampling. Sampling occurred between July 25

to August l, 1990.

Result s

At this time only the results of the first stage of sampling are

available. This sampling showed a. number of isolated anomilous values

within close proximity of conductor axis. Background for "B" horizon

is considered to be 20ppb Au and anomilous values range between 30ppb

and lOOOppb Au. Ko anomilous values for Cu were obtained.

South of tiie baseline on Line 4K, 8E and 12E sampling was preformed

over Conductor F, This conductor is believed to mark the contact between

syenodiorite and a small lense of basalt. An anomilous value of 60ppb

was taken on top of the conductor. Although outcrop occurs in the area no

mineralization was seen to suggest the cause of the anomilous Au value.

On L4ii on the baseline a value of 145ppb, Au was taken. Large outcrops

of syenite occur here and no explanation for the gold value was observed.

It is believed that glacial advance direction was northeast to southwest

so that this gold value may cone from an area farther to the north east.

Nortli of the baseline on L12E at 5N a value of lOOOppb Au was obtained

on top of a hill where large outcrops occur.During the second stage of ;

soil sampling this area was prospected and resampled. Due to the wide

expanse of gabbro outcrops in the area it is assumed that. this gold value

was influenced by glacial moveuent s and therefore the source may lie more

to the n o r t ii east.

On L20ii at 7+501^ a value of 860ppb Au was obtained in soil covering

gabbro outcrop. This location is north of conductor B and therefore the

gold value is probably a result of glacial movement from the north cast.

(9)

North of the base line from L28E to L34K sampling was preformed over

a draw the trends Northwest-southeast. This draw marks the axis of con

ductor C anomalous values between 115ppb and 400ppb Au were obtained on

each line over the draw. Since overburden in the draw is thick and no

outcrops occur within the draw, during the second stage of sampling a soil

auger was used to check these Au values. Depending on the second phase

of sampling more detailed sampling is reccommended in this area.

On L36ii at 4+OOS of the baseline an anomilous value of 125 ppb was

obtained in a draw marking the axis of conductor E. The values obtained

during the first phase of soil sampling were checked by using a soil auger.

Results of this sampling are not available as yet but more detailed ('a-tja-

jj-e-t aAioil a lil t; a-e- y-e-t- iMt-t- mo-t-e detailed] sampling may be warranted in this

ar ea ,

Trenching

Between June 9, 1990 and June 14, 1990, 17 trenches were blasted in

outcrops containing copper mineralization. Trench l is located on L34E,

1+25^. Tne rock in this trench is a weakly silicified basalt. Weak chal

copyrite totalling less than 1 7, is d isseminated throughout the basalt.

Malichite is present on some fracture plains. The trench measures 5ft X

3ft. Trench 3 is located on L34K, 1+7511. It contains weak chalcopyrite,

bornite, and native copper totalling less than 1 7, c ombined. The rock is

a weakly snear ed and silicified basalt. The trench measures 15ft X 4ft.

Trench 4 is located on L33E, 2+25N. It was blasted in weakly sheared

and silicified basalt. Traces of native copper and chalcopyrite were ob

served in fresh pieces. The mineralization totalled less than 1 7,,

Malichite is present on some fracture surfaces. The trench measures

6ft X3ft.

(10)

Trench 5 is located at L34 + 30E, 2 + 5001*. It was blasted into weakly

sheared and silicified basalt. The mineralization consisted of less than

l'/, chalcopyrite and malichite on fracture plains. The trench measures :

4ft X 3ft.

Trench 6 is located at L3A+60E, 1+50N. It was blasted into weakly

sheared basalt with traces of native copper and malichite on some fracture

plains. The trench measures Aft X 2ft.

Trench 8 is located at L3A+70E, 1+75N. The basalt contains malichite

on some fracture plains. The trench measures Aft X 2ft.

Trench 9 is located at L35E, 34-75N. The basalt contains traces^of :,:v

chalcopyrite and malichite on some fracture' plains. The trench measures

Aft X 2ft.

Trencii 10 is located at L35E. 14-OON. Traces of native copper and

malachite and chalcopyrite are inconsistantly disseminated throughout the

weakly sheared basalt. The trench measures 8ft X 3ft.

Trench 11 is located at L35+10E, 2+25N. 1 7, b ornite and chalcopyrite

and traces of native copper are found in a moderately silicified and

sheared basalt. The trench measures 8ft X 3ft.

Trench 12 is located at L36E, 1-fOON. 1 7, c halcopyrite was observed

in a l foot wide band of basalt in gabbro. The trench measures 8ft X 3ft.

Trench 13 is located at L33 + 60E, 5+25N. Less than 1 7, c halcopyrite

is randomly disseminated in a weakly sheared gabbro. The trench measures

12ft X 3ft.

Trench 1A is located at L33+75E, 5+75N. Less than 1 7, c halcopyrite

is randomly disseminated in a weakly sheared gabbro. Malichite is present

on some fracture surfaces. The trench measures 15ft X 3ft.

Trench 15 is located at L3AE, 6-I-10N. Less than 1 7, c halcopyrite and

traces of malichite are present on some fractures within a weakly sheared

(11)

gabbro. The trench measures 6ft X 3ft.

Trench 16 is located at L2 0+2 O li, 050N. Trace to 5 7, c halcopyrite was

found in a moderately sheared and brecciated basalt. The basalt was strong

ly carbonated and silicified. The trench measures 4 f t X 4ft.

Trench 17 is located at L20+40E, 0+75N. Very fine disseminated

chalcopyrite and pyrite total about 1/S within a moderately sheared and

carbonated basalt. The trench measures,4ft X Aft.

(12)

Qualifications

This report was written by:

R,J. Dillman42 Springbank Dr.London, Ontario

I am presently a student at the University of Western Ontario/ and

have completed 14.5 credits of the required 15 credits towards the B.S.C

program in Geology. I have been active in the geology field for 13 years.

During this time l have become very experienced with the surveys in this

report. l have also submitted assessment work for various companies and

for my own personal adventures. In all cases the Ministry of Natural

Resources had accepted and kept on file all my submissions.

June 20, 1990

H. FERDERBER GEOPHYSICS LTD. GEOPHYSICAL ft GEOLOGICAL SURVEYS 169 PERRAULT AVENUE. VAL D'OR. QUEBEC J9P2H1 TELEPHONE 819-B24-2O76

Memo on the Horizontal Loop Electromagnetic Survey on the Property of John Hamilton in the Seeley Lake Area, Ontario

The recently completed horizontal loop electromagnetic (H.L.E.M.) survey delineated the location of 8 conductive zones on the property of John Hamilton in Seeley Lake Area, Ontario. Because of the great many changes in local topographic relief on the property, quantitative calculations, defining properties such as dip, depth and apparent conductivity, would be largely inaccurate. Qualitative descriptions of the conductive zones are presented in the following table.

Conductive Zone

G

H

I

Topography

GulJy - lineament

Magnetic Correlation

VLF-EM Correlation Geology

Along slopes


In a gully.

Along cliff,down to the north.

Along a creek, gully and a slope.

Along a cliff, gully and slope.

Along a ' slope.


Along magnetic Anomaly A on lows. line 0.

Along the Anomaly B on edges of linea 16 and magnetic highs.

Near anomaly C on lines 32 and 34.

Along the edge of mag netic lows.

In lows and highs.

In a low in Anomaly E, the east and line 32. a high in the west.

Along weak highs.

In a weak low.

In weak lows. Anomaly F, line 8.

In lows.

Along a lineament representing a shear in a shear in syenodiorite and gabbro and along a diabase dyke in the east.

Near a possible shear in the east in gabbro. 26.

Located over chalcopyrite mineralization in gabbro.

In mainly gabbroic rocks near chalcopyrite mineralization.

In gabbroic rocks.

In syenodiorite.

In syenodiorite.

In syenodiorite?

Correlating the results of the HLEM survey, known geology and the results of the magnetic surveys, the best targets for sulphide mineralization containing possible gold values are conductor B, which appears to be the best conductor on the property, conductors C and D near chalcopyrite mineralization and conductor A along a potential shear fault zone. Possible drill targets are listed below:

Poaiton Azimuth Dip Depth Target

L12E, 9N -180 0

L16E, 1+50N -ISO0

L32E, 7N -1800

L36E, 3 + 50N 180O

-50 0 350'

-500 350'

-500 350'

-500 350'

Strongest conductor - B intersecting basalt, gabbro and a contact at a bend in the conductor axis.

Conductor A along a magnetic low and fault zone, just east of a possible syenodiorite basalt contact.

Conductor D, testing a contact between a magnetic low and high, west of chalcopyrite minera lization.

Conductor C, a possible fault zone, and syenodiorite-gabbro-mafic meta- volcanic contacts near copper mineralization, and across magnetic lows and highs.

Further work could also be completed over conductors A, B and I on lines 32 and east of line 32.

R.A. Campbell, Geologist

Uoiitiem Development and Mines

OntarioTW9004

Report of Work Mining Act (Expenditures, Subsection 77(19))

— ———— TTT~Type of Wr

——— j-formed 900

Recorded Holder

Address •- /fr.:Work Performed By

Name and Address of Author (of'Submission) Date When Work was Performed

T TDay | Yt. yDay | Yr.

All the work was performed on Mining Claim(s): Indicate no. of days performed on each claim. 'See Note No. 1 on reverse sWe _____

Mining Claim No. ofDayt Mining Claim No. of Diyt Mining Claim No of Days MinlngClaim No. ofpsys

Mining Claim No of Days Mining Claim No. of Dayi Mining CKIm No of Days Mining Culm No of Diyi Mining Claim No. of Days Mining Claim No. of Days

Mining Claim No of Days Mining Claim No. of Dayt MinlngClaim No. of Dayt Mining Claim No of Day; Mining Claim No. of Dayi Mining Claim No of Days

InstructionsTotal days credits may be distributed at claim holder's choice. Enter number of days credits per claim in the expenditure days credit column (below). _____________________

Calculation of Expenditure Days Credits Total Expenditures

Total Days Credits

Total Number of Mining Claims Covered by (his Report of Work

Mining Claims (List in numerical sequence). H space Is insufficient, attach schedules with required informationMining Claim

Prefix NumberExpend. Days Cr.

Mining ClaimPrefix

Total Number of Days Performed

7

NumberExpend. Days Cr.

Mining ClaimPrefix Number

——— B-Ff"KG*.JAN

MINING U

Total Number of Days Claimed. fTL-H— —— —~C7

Expend. Days Cr.

ftvO M

NDSS

Mining ClaimPrefix

EDi! —

Number

ECTION

Expend. Days Cr.

Total Number of Days to be Claimed at a Future Date

^Certification of Beneficial Interest 'See Note No. 2 on reverse side

l hereby certify thai, at the time the work was performed, the claims covered in this report of work were recorded in the current recorded holder's name or held under a beneficial interest by the current recorded holder.

Date

/9?oCertification Verifying Report of Work

l hereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, having performed the work or witnessed same during and/or after its completion and the annexed report is true.Name and Address of Person Certifying ~~~

For Office Use Only

676 (69(06)

Ministry otNorthern Developmentand Mines

Ontario

Type of

DOCUMENT No.W9004*

ActReport of Work(Expenditures, Subsection 77(19))

Instruction* ** ..i . - Please lyp. or punt flit A/J fi) Q)

. Refer lo Subsection 77(19), the Mining Act for assessment work requirements and maximum credits allowed under this Subsection.

- Technical Reports, maps and proof of expenditures in duplicate should bo submitted to Mining Lands Section, tjiperal D^/elopment and Lands Branch.

Recorded Holder

Mining Division Township or Area

.rr By '

Prospector'* Licence No.

Telephone No.

'me and Address ol Author (of Subrrijssion) ^40j ./s.ft AA) fc

No ol Days

Date When Work was Performed Fronv - a To; - v ,-,2Y -7 fa a # ?#/Pa/ l Mo l Yr L Ply | Mo | Vi

No ol Days No ol Days Mining C laim1 the work was performed on Mining Claim(s): Jsate no. of days performed on each claim.

5ee Note No. 1 on reverse side

Mining Claim Mining Claim lining Claim No ol Days

73ng Claim No ol Days

mg Claim No ot Days

Mining Claim No. ol Days Mining Claim No ol Days Mining Claim No ol Days

ming Claim No ol Days Mining Claim No ol Days

Mining Claim No ol Days Mining Claim No ol Days

Mining Claim No ol Days Mining Claim No. ol Days Mining Claim No. ol Days

-istructlons•tal days credits may be distributed at claim jlder's choice. Enter number of days credits per iaim in the expenditure days credit column

Calculation of Expenditure Days Credits Total Expenditures ,.

15

Total Days Credits

Total Number of Mining Claims Covered by this Report of Work

ning Claims (List in numerical sequence). K space is insufficient, attach schedules with required informationMining Claim

efix NumberExpend. Days Cr.


Expend. Days Cr.


Expend. Days Cr.


Expend. Days Cr.

/C'?6JCJ t Z&- re-3- J2i

}(x?/://?I&. -0- #4

7^lt?6Ml -20 ECEIV6D

ft* 3J. rcrre-A 't* iewta. MINIM LANDS S

^*/P9///6

•sotal Number of Days lo be Claimed at a Future Dateotal Number of Days ClaimedNumber of Days Performed

rtification of Beneficial Interest 'See Note No. 2 on reverse sidelereby certify that, at the time the work was performed, the claims covered in this report t work were recorded in the current recorded holder's name or held under e beneficial interest •y the current recorded holder. -^-—-—^——-—————^——^-——-^-—rtification Verifying Report of Work•ereby certify that l have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, hag performed the work or witnessed same jring and/or after its completion and the annexed report is true.ame and Address of Person Certifying

r Office Use Only

Ministry ofNorthern Developmentand Mines

Dntano

/DC of Survey(s)

:orded Holder(s)

DOCUMENT No.W9004'

ActReport of Work(Geophysical, Geological and Geochemical Surveys)

Instruction!- Please type or print- Refer to Section 77, the Mining Act for assessmenl

and maximum credits allowed per survey type.- If number of mining claims traversed exceeds s]

attach a list.- Technical Reports and maps in duplicate should bo submitted lo

Mining Lands Section, Mineral Development and Lands Branch:

requirehynts

irm,

jress

^^J?. S J

y Company

Prospector's Licence No.

-^?, ~fem Telephone No.

-i e and Address 'of Author (of Geo-Technical Report) Dal* o' Surve/ (from * "J) f

, .,ls Requested per Each Claim in Columns at right

jcial Provisions

- first survey.

er 40 days. (This includes i cutting)

ir each additional survey: -.mg the same grid:

nler ?0 days (for each)

.n Days

implete reverse side and 'er lolal(s) here

borne Credits

Note: Special provisions credits do nol apply to Airborne Surveys

Geophysical

- Electromagnetic t/LF '/W* /"//J

- Magnetometer

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Other

Geological

Geochemical

Electromagnetic

Magnetometer

Other

Days per Claim

jfofa

-&L- W

Days per Claim

— — ——

Days perClaim

tal miles flown over claim(s).•le Recorded Holder or Agent (Signature)

'ification Verifying Report of Work

Mining Claims Traversed (List in numerical sequence)Mining Claim

Prefix

"/Tfr.*ftj^

T, g,-fig.

r*irJg-

Number

lin 36o/t// 36 1///l 36?

JlUJZ&Lf//f/ J^5"////Jfc^////-T^ 7


DFClK C v. l

OCTS

MINING U\

Mining ClaimPrefix

4VJ6 UN

rorsf

Total number of mining claims covered by this report of work.

Number

J)

)

PTIANC1IUW

'8reby certify that l have a personal and intimate knowledge of the facts set forth in this Report of Work, having performed the work or witnessed same durina and/or i its completion and annexed report is true.

ie and Address of Person Certifying

to UT?*/ 6* -

r Office Use Only

Recorded Qet/L/to 0!i I f J 3TJ.OOOS.

Muietrvi M Mining Lands sectionMinistry OT . 5 9 Ce^ar street, 4th FloorNorthern Development ^SUDBURY, Ontarioand Mines P3B 6A5Ministere du Telephone: (705) 670-7264Developpement du Nord FftX! ( 705) 670-7262et des Mines your pile! W9004 . 4 2 o

Our File : 2. 13744

February 18, 1991

Mining RecorderMinistry of Northern Development and Mines435 James Street SouthP. O. Box 5000THUNDER BAY, OntarioP7C 5G6

Dear Madam/Sir:

RE: Notice of Intent dated January 14, 1991 for Geophysical (Electromagnetic fc Magnetometer) Geological and Geochemical Surveys submitted on Mining Claim TB 1111360 et al in Seeley Lake Area.

The assessment work credits, as listed with the above mentioned Notice of Intent have been approved as of the above date.

Please inform the recorded holder of these mining claims and so indicate on your records.

sincerely

R. C. GashinskiProvincial Manager, Mining LandsMines and Minerals Division

DM/dvl Enclosure

cc: Mr. W. D. Tiernan Resident Geologist Mining and Lands Commissioner Thunder Bay, Ontario Toronto, Ontario

Annette Hamilton J. Dillman Toronto, Ontario London, Ontario

PE

NIN

SU

LA

HA

RB

OU

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GR

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-i-jarry material

X l- — - i ~ - -NT ~ ~ ~ -\-~ - - -r ——— -

1658899 658915 |V i j !

16(58920 658933 1658938

P e n m s uio\ , 96 69 JC ' l ' j l l

9081^ ' 695912 'MSS13 1658621 '646R24 1645*25^86/4/168 |

655514 655520 '^49833 6458Z6^ 86 4167. . J. VWWWfc^F^-^—^-— ! V^WN* L V | ^^ ^1 V l S

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*555lO '6555I*/ 665S02 649822 645827 .864166 ,- - - -1- - - - -1- ~ - - -L - ~ ~-4 -c^K- —— - f - -

863942. 8639,40D i s1 t r i c t

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- - -- - -- -- -

Marath 1*58*8 ^v ^

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'658370 1658376l J ^645884^64 5889I'96l72l '961722 1961723 961724 1961

86279)3 ' 862798|96I730 1961729 '961728 |96l727j.L----J-r'""" Ti*W* "III** '•li

'•89661' ^- l - 1

l l 'Q--- l 8-! 3.87*'Ml'^l-i-

i i i i 65)941 I&SI936 l/---f—-H,

663998 '663997 '6888Q1

,- PROP0^,W1 ,| tttf lCRAIG'^ J'TT '•*sws 'aw*OT.; it*lr*lj?**.r?ILj

t l 'coaaAV . l iCIAL MATURE

AA J9Ol\*ts

6448OO[638I8J

08131 l 9O8IZ6

^ -^ -

i i|657433J 649708 I64570T

- - - —t— - -;ife6l68l l654 ' 9* /IX654I94 •54135'4———r--H-r-64569I '656554

656548 I6S6843I656638 .686532

//HA. ..jjo.

696524 656521 . 6S6SI9

i Exploratory Licence of Octapotion applied for

908510 1908514 .908537

l 908501 9O8496, 908495

-- ."863968'" ~ ~ ~

W^lO(C|W*TlO(i* C t ' O l O O** l OO 9

(V.fl jTAIAi-V f- Jl t f, t r . f*~~ 7

-Mussy Lake Area -ALL ISLANDS WITHIN 2 MILE LIMIT FORM PART OF NAT. Order Ne W ?5 73, deted Junr 6, 1973, File No 167249.

______RE FERENCES

AREAS WITHDRAWN FROM DISPOSITION

S.R. - SURFACE RIGHTS M.R. - MINING RIGHTS

Description Order No. Date Disposition File

WN.R 2/84

AT.CR 43/S!

WIMCR 17/84

WNCR 40/81

W1/85

WNCR 8/84

WNCR 4/85

WNCR

W 98/86

S R S M R WITHDRAWNSee '••~ L ontjroll

^.TriDRAWN

VklTHDRAWN

SR8MH

SR&MR

S h M TM^K-iA.'^

Sht ft MR WITHDRAWN

S.R -i MR A\T:I"RAWN"5c* .seel, t.*e i onjfollS R 8 M R. Wl THORAWN

S R a M R A, PnORAWN

S R 8 M R WITHDRAWNSee P ic Twp i ijndruii

LAND UNDER THE WATERS OF LAKE SUPERIOR WITHDRAWN FROM STAKING BY ORDER IN COUNCIL DATED APRIL 30, I9IE.

AREA SHO'VN THUS Ij ""- AND ISLANDS IN FRONT OF CONCESSION 2 TO CONCESSION 6, SUBJECT TO SECTION 118 OF THE MINING ACT.

AREA SHOWN THJ!: X-/..-X. IS V.'.T j r*RAWN FROM STAKING PURSUANT TO Thr f'SO'/iSiONS -,K SECTION 32 OF THE IV:,.v:NG ACT R SO 1980 CHAPTER 268.

ANNULLED PORTION OF SUBDIVISION OF TOWNSHIP SHOWN THUS - . '

Line

SAND B GRAVEL

GRAVEL 8 GRANITE FILE 90338

LEGENDHIGHWAY AND MOD ' l N

OTHER ROADS *

TRAILS

SURVF YF O l ,Nl STOWNSHIPS BASF (INrS t Tr

LOTS. MINING i. l AIMS PAHi F | s Ffi

UNSUHVE * k() l INF SLO1 LINtSPAHCt l BO" 'NOAH -.MINlNi, C l AiMS F 1 i.

RAILWAY AN[) UK,HI (if vVAN

UTILITY l INF.S

NONPERENNiAt STHtAM

FLOODING OH t-1 ODD INC, RIGHTS

SUBDIVISION ORTOMPOSin PI AN

RESERVATIONS '

ORIGINAL SHORr l INF

MARSH OR MUbKKi

MINES

TRAVERSE MONt )Ml N '

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT

PATENT SURFACE A MlNINCi Mh.HTS

SURFACE RIGHTS ONl i

MINING RIGHTS ONl V

LEASE. SURFACE K, M INING RIGHTS

" .SURf ACE HIGHTSONl Y

" , MINING RIGHTS ONLY

LICENCE OF OCCUPATION

ORDER IN COUNCIL

RESERVATION

CANCELLED

SAND ft GRAVEL ....

NOT6 M INING BIGHTS IN PARCELS pAreNTtopRiOR TO MAY 61913 VFSTEO IN O R11", l N A l PAT^NT^^ RV THt PUBIH LANDS ACT RSH ''i'O (.MAP JRO S8C 63 SUBSt.C '

SYMBOL

9 9 Q B H B T

OC 0

SCALE 1 INCH- 40 CHAINS

'000 ' * M

AREA

PIC TWPMN R ADMINISTRATIVE DISTRICT

TERRACE BAYMINING DIVISION

THUNDER BAYLAND TITLES/ REGISTRY DIVISION

THUNDER BAYMinistryof LandNatural Management

Resources Branch

•JANUARY 14^1917.._ ..

:)d " M/'RCH o 1982H umbel

G-630

I4N

12 N

ION

8N

6N

4N

2N

2S

4S

6S

8S

10 S

12 S

14 S

420165*88*5 Z . 13744 SEELEY LAKE

vte^^N**

4E 8E 12 E I6E - 20E 24 E 28E 32E 36 E 4OE 44 E

320

PROJECTt

AREA

Geord/9Lake

:A.C\ c hnin*

SEELEY LAKE ; Plain 6-613

Legend

A/A//V

cpyboCu

PY

DiabaseSyenodioriteGabbroSheared mafic Basalt

foliationstrike and dip of contactcontact i observed, assumedfault outcroptrench chalcopyrite bornite native copperpyrite *

creek

swamp claim post

2.113744

COUBRAN LAKE PROJECTHAMILTON GRID

Seeley Twp., Ontario

GEOLOGY

200 400 800ft.

Scale- I-2.0OO Aug. 1990

14 N

12 N

ION

8N

6N

4N

2N

2S

4S

6S

8S

IOS

12 S

I4S

4E 8 E I2E I6E 20 E 24E 26 E 32E 36E 40 E 44 e

SEELEY LAKE; Plain G-613

Legend

i?*o f* Sample location ^ swamp

—o-claim post

2 , 13744

420i6sweees 2.13744 SEELEY LAKE 230

COUBRAN LAKE PROJECT HAMILTON GRID


GEOCHEM; "B" HORIZON

0 200 400 80Oa.

Scale: l.2POO Aug. 1990

M AIVHL l UN


MAGNETICS

200 400 800 ft.

Scale 1:2,000 July I99Q

CD Oa

K) OD O O

rnX)en

PROJECT

AREA

O)ro o o

_______SEELEY LAKE; Plain G-613

2/137441600 NORTH

1400 NORTH

1200 NORTH

1000 NORTH

800 NORTH

600 NORTH

400 NORTH

200 NORTH

BflSE LINE

200 SOUTH

400 SOUTH

600 SOUTH

800 SOUTH

1000 SOUTH

1200 SOUTH

o

•'3744 SEELEY'U'KE"

PROJECT

AREA

SEELEY LAKE i Plain 6-6131600 NORTH

r-o oo o o

1400 NORTH

1200 NORTH

1000 NORTH

800 NORTH

600 NORTH

o *c-' LJw . ^..t i n

200 NORTH

Nflh BRSE LINE

200 SOUTH

400 SOUTH

600 SOUTH

800 SOUTH

1000 SOUTH

1200 SOUTH

43D16SWee05 2.13744 SEELEY LAKE 250

COUBRAN LAKE PROJECTHAMILTON GRID

Seeley Twp., Ontarioi

VLF' ELECTROMAGNETICS

OtE

200 400 —l —1^

Scale: 1:2,000

— y "** •4 X7 M* M. - -

800ftE^f

July 1990

1600 NORTH

1400 NORTH

1200 NORTH

1000 NORTH

800 NORTH

600 NORTH

400 NORTH

200 NORTH

BfiSE LINE

200 SOUTH

400 SOUTH

600 SOUTH

800 SOUTH

1000 SOUTH

1200 SOUTH

CLIENT

JPRO.JECT

HORIZONTAL LOOP ELECTROMAGNETIC SURVEY

J. HAMILTON

H. FERDERBER GEOPHYSICS LTD,

SCALE2OO*

DRAWN BY

Adrien Goyette

DATE

JULY J99H1MAP OR SHEET NO?

. 1 3744

\

LEGENDMEASUREMENT STATION ALONG PICKET LINESELECTROMAGNETIC READINGS - In Phase Component ( K)* ^ ii-ELECTROMAGNETIC HEADINGS - Out of Phase Component (55)

PROFILE - In Phase Component (Scale l" = eo?s)

PROFILE - Out of Phase Component (Scale l" ~ ea ft) COIL SEPARATION - -^OO Feet

INSTRUMENT - MAX MIN H

ELECTRICAL CONDUCTOR

FREQUENCY USED 3555

1600 N -^

1400 N

1600 N

.400 N

.1200 N

1000 N

1400 8

42Di6sweees 2.13744 SEELEY LAKE 360

hamilton prop - geology ontario

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