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42Et0NEeeS1 2 .8iae CROLL 010

GERALDTON PROJECT

I croll/Coltham Townships Thunder Bay Mining District

Geraldton, Ontario

GEOLOGICAL SURVEY

Golden Pond Resources Ltd./ Metallgesellschaft Canada Ltd. Joint Venture

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lJanuary 1984

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B MAY If, 1985

MINING UNDS SECTION

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42EieNEeesi a .eiaa CROLL

TABLE OF CONTENTS

INTRODUCTION

LOCATION AND ACCESS

TOPOGRAPHY AND VEGETATION

HISTORY BEARDMORE-GERALDTON GOLD CAMP

SURVEY PARAMETERS Line Cutting General Geology

PROPERTY GEOLOGY Croll StockMetavolcanics and Metasediments Diabase Dykes

VLF-EM 16 SURVEY

CONCLUSIONS AND RECOMMENDATIONS

BIBLIOGRAPHY

APPENDIX I APPENDIX II APPENDIX III

BudgetGeology Maps l, 2 , 3Geology Maps 4, 5, 6

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INTRODUCTION

The Geraldton Project encompasses a total of 291" contiguous

claims located in Croll and Coltham Townships, near Geraldton,

Ontario (Fig. l, 2 and Appendix 2). The claim group is held jointly

between Golden Pond Resources Ltd. and Metallgesellschaft Canada

Ltd. :

Golden Pond Resources Ltd. Metallgesellschaft Canada Ltd.169 Perreault Ste. 3100, 2 Bloor St. EastVal d'Or, Quebec J9P 2H1 Toronto, Ontario M4W 1A8

The epigenetic origin of the Geraldton gold deposits is similar

to some of the deposits in the Val d'Or area of Quebec. Within the

vicinity of the Bourlamaque Batholith, gold-bearing zones of

shearing and faulting extend from the volcanics into the intrusive.

Examples of such mineralized structures are to be found in the Bra

d'Or and Belmoral Mines. Following the discovery of the Belmoral

Mine, a number of areas were explored for similar geological

environments, however, it would appear that the Croll Lake Stock was

overlooked. Therefore, the Croll Lake property was acquired by

Golden Pond and Metallgesellschaft with the intention to explore

within the stock for zones of shearing and faulting which may be

favourable hosts for gold mineralization.

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A geophysical survey consisting of a VLF-EM 16 and magnetometer

survey was conducted early in 1984 (Scammell 1984). This was

followed by the geological mapping program described herein, which

was conducted between August 20 and September 25, 1984.

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I The Croll claim group covers part of a northeast-trending felsic

m batholith (Croll Lake Stock) which is up to 5 km wide on the

property and has intruded predominantly mafic volcanics. Quartz

l veins with varying amounts of feldspar, chlorite, tourmaline and

' sulphide minerals are common throughout the Croll Lake Stock but are

l most frequent in the porphyritic "nose" at its west end. Sulphide

minerals of the veins there comprise pyrite, pyrrhotite,

chalcopyrite and molybdenite. Molybdenite mineralization reaches

l across the porphyritic margin of the stock into the metavolcanics to

the west.

l' Most of the economic deposits in the Geraldton area are spacially

associated with a series of east trending faults, particularly the

j Bankfield-Tombill and Little Long Lac faults.

I If these fault systems are projected eastward from Geraldton, ,,

then they should intersect the Croll Lake Stock. There is a

i considerable amount of evidence that the volcanics and sediments on

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both sides of the stock have been faulted and subsequently

M mineralized with sulphides and gold (no economic deposits have been

outlined but a number of showings are known). Also, there is some

l evidence which would indicate that the stock itself has been

subjected to a similar period of faulting and possibly to

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mineralization: the granitic stock has a tear drop shape, elongated

towards the southwest. This shape could be the result of a series

of dextral (right hand) fault movements (the Bankfield-Tombill Fault

is a dextral fault).

It is obvious that the Croll Lake Stock intruded the Beardmore-

Geraldton greenstone belt and is therefore younger than its

enveloping rock units. The stock is, however, weakly foliated and

could be contemporaneous with the mineralizing event or even older.

Based on the literature available, the sequence of events leading up

to the deposition of the gold deposits in the Geraldton area are:

1. Deposition of volcanic and sedimentary rocks

m 2 . Intrusion of the Croll Lake Stock

3. Intrusion of the porphyries

l 4. Folding major (Regional Fi)

5. Folding minor (F2)

6. Faulting, following an east-west trend parallel to the FI folding, which continues throughout and after the period of mineralization

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7. Injection of auriferous solutions of at least two generations:

a) High temperature deposition characterized by the presence of tourmaline, arsenopyrite and pyrite

b) Low temperature deposition characterized by the presence of galena

lIf this sequence of events did indeed lead to the formation of

the Geraldton gold deposits, then it follows that the Croll Lake

Stock must have been subjected to the same deformation as the

surrounding volcanics and sediments. This, together with the

physical characteristics of the intrusive, should make the Croll

Lake Stock a prime target for gold exploration.

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LOCATION AND ACCESS

The claim group is located to the southeast of the No. 11 Trans

Canada Highway. Its western boundary is situated approximately 10 km

to the east of the town of Geraldton (Fig. 2).

m Although the No. 4 claim post of claim TB 736192 is conveniently

located at the side of highway 11, in general/ the majority of the

l claims are only accessible by walking or by helicopter and during

the winter also by skidoo. A number of logging roads transect the

l property as shown on the 1:50,000 topographical map (Geraldton

M 42-E-10). However, many of these roads are covered by secondary

growth, in particular tag alders, which precludes them from being

l used for access except by heavy equipment. This growth is often so

dense that it makes even walking along these trails extremely

difficult.

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TOPOGRAPHY AND VEGETATION

- The general physiography of the claim group reflects the

l underlying Precambrian and Pleistocene geology. The northern part of

the property is underlain by the Croll Granodiorite Intrusion. Its

P topography is characterised by one of low relief and poor drainage.

. Pleistocene glaciation from the northnortheast with its subsequent

deposition of moraines and eskers obscures the bedrock topography.

lIt has also disrupted the pre-ice drainage systems. As a

l consequence, sand and gravel deposits have imposed an alignment on

many of the swamps, creeks and lakes parallel to the ice direction.

H The logging roads are generally restricted to the glacial ridges and

B consequently these too reflect the glacial fabric of the area.

l Since the moisture content of the soil is one of the main factors

determinng the type of vegetation which grows in that area, then in

l a crude way the vegetation on the property does reflect the glacial

m morphology. The poorly drained swamp areas, interspersed around the

glacial deposits, are generally covered by two types of tree growth,

consisting either of dense cedar growth or open swamp which supports

a stunted growth of tamarack and spruce. By comparison, the sand and

l gravel deposits are well drained and support a tree population

consisting mainly of mature balsam, pine and spruce. These deposits

generally attain a maximum elevation of 15 m, above the level of the

l surrounding swamp.

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ll * Basic volcanics and volcanoclastic sediments underly the

l southern part of the property. Here, at the granite/volcanic

contact, the volcanics form a steep north facing scarp which has a

l corresponding low angle dip slope to the south. It rises to a

maximum hight of 40 m above the level of the swamp. As a

" consequence, the ground is well drained and devoid of glacial

j deposits. The overburden is generally thin and supports a mature

growth of balsam, spruce, poplar and occasionally birch. The

l poplar growth is generally restricted to dip slope where the "A"

horizon is better developed and the moisture content is higher.

HISTORY BEARDMORE-GERALDTON GOLD CAMP

Gold was first discovered near Geraldton during World War I and

l in the Beardmore area in 1925. Gold finds at Lake Kenogamisis in

1931/32 led to the development of the Hard Rock, Little Long Lac and

several other mines.

lProduction from eleven bigger and eight small mines between 1934

l and 1968 totalled over 4 million ounces of gold and half a million

g ounces of silver with the major producer being MacLeod-Cockshutt

Mine near Geraldton (1.47 mio oz gold, 0.1 mio oz silver).

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By 1970 most of the mines were closed and it was not until 1980

H that efforts were made again by several companies to bring the camp

back to life. Among others are Mining Corporation of Canada

l Limited (Consolidated Louanna Gold Mines), Roxmark Mines Limited

and Sheritt Gordon Mines Limited (Magnet Consolidated Gold Mine),

l Pancontinental Mining (Canada) Limited and Dome Mines Limited,

m which have all explored various claim groups in the general area,

mostly looking for the traditional deposits related to oxide iron

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SURVEY PARAMETERS

Line Cutting

A 10.2 km base line was established at an azimuth of N55E and a

total of 319.4 km of grid lines were cut perpendicular to the base

H line. The spacing between consecutive lines was 150 m and stations

were established along those lines by means of a marked picket at

l 25 m intervals. The orientation of the base line was chosen on the

basis that it was generally parallel to the main structural

l features, associated with auriferous mineralization within the

Geraldton area. In addition, it is approximately parallel to the

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stratigraphy of the volcanic and volcanoclastic rocks underlying

the southern part of the property.

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General Geology

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The Geraldton area lies at the southern boundary of an

east-trending isoclinal ly folded Early Precambrian (Archean)

metavolcanic-metasedimentary sequence of the Wabigoon Subprovince.

These have been intruded by a series of felsic batholiths, stocks

and sills as well as lenticular shaped gabbros, also of Archean

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l- Unconformity -

PrecambrianMiddle to Late Precambrian

l Mafic Intrusive Rocks

age. During the Late Precambrian north-trending diabase dykes were

intruded into the older formations.

The following is generalized geological succession in the

vicinity of the map area:

PhanerozoicCenozoic

Quaternary Recent

Organic swamp and aullival deposits

PleistoceneOutwash deposits and moraine (sand, gravel, clay, silt and till)

Diabase, porphyritic diabase

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Early Precambrian (Archean) Felsic Intrusive Rocks

Quartz porphyry, granodiorite, quartz monzonite


Intermediate to Mafic Intrusive RocksHornblende gabbro, gabbro, diorite


Metavolcanics and Metasedimentsl Metasediments

Interbanded wacke and mudstone, coarse grained sandstone, conglomerate, banded metasediment or tuff

Chemical sediments, ironstone, chert, ferrugenous chert and graphitic schist

MetavolcanicsFelsic to Intermediate Metavolcanics

Tuff, lapillistone, lapilli tuff, quartz and of feldspar porphyry, felsic dykes

Intermediate to Mafic MetavolcanicsPillowed and/or amygdaloidal flows, pillow breccias, flow breccias, coarse-grained volcanic rocks, inter flow banded tuffs

Most known gold deposits of the area are spatially related to

iron formation and to east-trending fault zones, i. e. the Paint

Lake Fault, Bankfield-Tombill Fault, Little Long Lac Fault. It is

postulated that this period of folding produced zones of weakness

which failed when subjected to subsequent lateral tension. The

mineralization is not associated with anyone lithological unit and

it appears that the physical properties of the rock were more

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important for gold deposition than its lithology. Gold

mineralization is associated with the more competent units which,

when subjugated to strain, produced zones of fracturing or

f brecciation. The fracturing provided a plumbing system for

M hydrothermal auriferous fluids. The favourable rock types in the

Geraldton camp are banded iron formation, the greywackes and the

l intrusions. Quartz is the principal gangue material filling the

fractures. The gold mineralization, in addition to quartz, is also

J associated with ankerite, tourmaline, arsenopyrite, pyrite, galena

and chalcopyrite. There is a definite relationship between the

sulphides and gold, thus there is an absence of gold in quartz that

j does not contain any sulphides. There are at least four

generations of silicification and it is postulated that gold was

l deposited in the second and third generations of quartz veining.

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No evidence for a synsedimentary origin of the gold deposits has

been found so far. Field observation rather suggests a

structurally controlled, hydrothermal, epigenetic emplacement of

l gold, quartz, tourmaline and sulphide minerals in veins,

accompanied by an intense, local carbonatization of the wallrock.

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- 12 -l l The regional metamorphic rock is greenschist in the vicinity of

* the Croll Lake property, however, it increases to lower amphibolite

l to the east. Generally, the outcrop distribution is sparce being

covered by Pleistocene sand and gravel deposits as well as more

l recent organic and alluvial deposits.

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lPROPERTY GEOLOGY

l Approximately 801 of the claim group is underlain by the felsic

intrusive known as the Croll Lake Stock. This has been intruded

into predominantly mafic to intermediate volcanics which outcrop on

the northwest and southeast sides of the property.

l The composition of the felsic intrusive varies considerably.

Work by Dr. A. J. MacDonald of the Ontario Geological Survey over

l the last three years suggests that the intrusive is zoned with an

m equigranular granitic core being surrounded by rinds of quartz

monzonite, diorite, plagioclase-phyric diorite and quartz porphyry

(Figure 3). This sequence is best developed and exposed immedia

tely west of the property at the western tip of the intrusion

where it was studied in detail by MacDonald. Quartz with varying

amounts of feldspar, chlorite, tourmaline and sulphide mineralsM

are found throughout the Croll Lake Stock and intruded into the

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J . metavolcanics and metasediments. However, they appear to occur

r m most frequently in the porphyritic "nose" of the intrusion. This,

l however, may be a function of the availability of outcrops rather

than an incrase in the abundance of quartz veining.

lWithin the porphyritic "nose" the quartz veins are mineralized

l" with pyrite, pyrrhotite, chalocpyrite and molybdenite. Molybdenite

B mineralization occurs also in quartz veins within the metavolcanics

that are in contact with the porphyritic stock.

lCroll Stock

The felsic intrusive underlying the Croll property varies in

composition from granodiorite to quartz monzonite. At the margins

of the intrusive where it is in contact with the metavolcanics,

l xenoliths of metavolcanic material are common. Generally, these

have been metamorphosed to amphibolite. The contact itself where

l it is exposed is sharp with little or no assimilation of the

m country rock. Occasionally, the volcanics are intruded by narrow

dykes and sills which have a similar composition to the main stock.

lThe stock is weakly foliated. However, only one area of minor

l shearing with associated alteration was located on Line 1950E at

3175S. The alteration is fairly typical consisting of quartz,

* feldspar, chlorite tourmaline and carbonate over a width of one

metre. No sulphides were observed within the zone of alteration.

lOther alteration observed within the stock was potassic

l alteration along fractures, epidotization of the feldspar

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constituents and the occasional development of blue quartz eyes.

Most of this alteration appears to occur near the contacts with the

diabase dyke and was of a very localized nature.

Metavolcanics and Metasediments

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Approximately 201 of the property is underlain by metavolcanics

l with minor metasediments. They occur on the northwestern and

southeastern boundaries of the claim group striking in a west to

northwest direction. The best exposure of these rocks is found on

B the southeastern part of the property where, as has already been

mentioned, they form a series of low hills.

lThe southern contact with the granodiorite intrusive is exposed

l in several places and appears to dip to the north. The

m metavolcanics in contact with the stock have been recrystallized

and are occasionally hornfelsic. Here the predominant rock types

l are basic to intermediate pillowed and/or amygdaloidal flows with

only minor interflow volcanoclastic tuffs and sediments. These

l flows are generally massive and exhibit little or no foliation.

M Flow breccias were observed on Line 1950W and 2100W between 3200S

and 3250S, and again on 3500W and 2500S.

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Southwards from the southern contact of the intrusive, the

l amount of tuffaceous material increases and appears to become more

m felsic in composition. The tuffs are generally fine-grained and

often well laminated. In addition, they are schistose and are

l often mineralized containing fine-grained disseminated pyrite,

particularly in the more felsic units, i. e. Lines 1800W to 2700W

l from 3150S to 3600S. In this area several quartz veins were

m observed. One of particular interest occurs on Line 2550W at

3450S. This 30 cm wide shear zone consisted of a number of quartz

l veins within altered host rock. The veins contained chlorite,

feldspar and tourmaline with pyrite, pyrrhotite and minor amounts

l of chalcopyrite. This area of mineralized dioritic tuffs certainly

deserves more detailed exploration.

l On the northwestern boundary of the property, the metavolcanics

are poorly exposed but appear to consist of basaltic flows some of

P which are coarse-grained. No shearing was observed but because of

the lack of outcrop no statements can be made as to the economic

importance of these metavolcanics.

Diabase Dykes

l As mentioned previously, these dykes postdate the granitic

intrusion and crosscut all the consolidated rocks in the map area.

* Many of the dykes are porphyritic and contain sufficient magnetic

l minerals to produce a strong magnetic response on the ground

magnetic survey.

l They trend in two principal directions: northwest and

l northnortheast. Where they were mapped they are less than 55 m

wide, usually exhibiting sharp chilled margins. The magnetometer

l survey indicates that many of them are persistent extending across

the full width of the property (5 km) while others have a limited

* extent, usually of less than 500 m.

lMany of the dykes are porphyritic containing altered laths of

l feldspar up to 40?, in a fine- to medium-grained dark green/black

matrix. These dykes appear to be less resistent to weathering than

B the granite. Consequently, the erosion of these dykes leaves small

M scarps of granite with remnants of the diabase occuring on the

scarp face.

lA particularly good example of this can be found on Line 3000S

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from 1800S to 2200S.

l" VLF-EM 16 SURVEY

lThe VLF-EM 16 survey outlined a number of weak to strong

l electromagnetic conductors (Scammell 1984). All of these anomalies

occur in areas covered by either Pleistocene or more recent

* deposits and, as a consequence, they have no surface expression.

j Most of the anomalies occur within the granite, however, the last

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two described below occur within the volcanics:

2550W to 3300W between SOON and 700N -

This weak conductive trend occurs in an area of flat ground and

is probably due to conductive overburden.

2250W to 3550W between the baseline and 150N -

This moderately strong VLF anomaly is located beneath an area

covered by glacial debris. It may represent a bedrock conductor

and should be surveyed using the IP method.

3300W to 3950W between 1500S and 1800S -

Located beneath an area of swamp, this conductive trend is

probably due to the effects of conductive overburden.

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This moderate to strong conductor coincides with the southern

l contact of the Croll Lake Stock and the metavolcanics. The contact

in this area is covered by two small lakes and a series of cedar

l swamps. The anomaly is therefore probably a function of ground

m water along the intrusive/volcanic contact. However, because of its

position at the contact, a few IP lines across this conductor are

l recommended.

1550E to 1800W between 2400S and 2600S -

m This moderate to strong conductor runs parallel and beneath

Croll Lake and part of Kinonge Creek. It appears to be due to

l conductive lake bottom sediments. However, the stronger responses

associated with this trend should be tested with IP.

lm 9 00E to 450W between 250S and 400S -

Located beneath an area of glacial till, this anomaly may

l represent a bedrock conductor.

300W at 750S -l This is a strong one line VLF anomaly, immediately to the east

of a northwest trending diabase dyke. This conductor should be

tested by an IP survey.

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1150E to 4050E between 150S and 1000S -

There are a number of weak to moderate VLF conductors occuring

in this area. Many are located beneath areas of wet cedar swamp

between areas of granodiorite outcrop. It would appear that they

are due to conductive overburden, however, selective anomalies

could be tested with IP.


l This medium to strong conductor is located beneath an area of

swamp and may represent conductive overburden.

m 1 800E to 3600E between 1150S and 1450S -

This trend consists of two enechelon VLF conductors occuring

l beneath an area of swamp between two areas of granodiorite

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outcrop. In all probability, these represent conductive

overburden, however, the stronger part of the trend should be

tested with IP.


This strongly conductive zone appears to be related to the

bedrock and should be tested with IP.

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l This weak conductor is located beneath Jackfish Bay and appears

to be related to conductive lake bottom sediments.

l 2050W to 2600W between 3650S and 3700S -

This weak VLF anomaly occurs near the southern boundary of the

l property where the metavolcanic/metasediment outcrop dips beneath a

cedar swamp. It therefore probably represents conductive

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This weak VLF conductor is located within the metavolcanics and

probably represents a bedrock conductor.

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CONCLUSIONS AND RECOMMENDATIONS

l The potential for epigenetic gold deposits hosted by Croll Lake

Stock still exists. However, the overburden cover, particularly on

l those claims underlain by the intrusive, has made it impossible to

identify potential zones of shearing and faulting. These by their

very nature would be less resistent to glacial erosion than the

M surrounding rock. Consequently, they would be restricted to the

lower areas now covered by swamp. There are a number of these

l areas as shown on the geological map which are generally aligned

parallel to the ice direction. Many,of these correspond to weak to

strong conductive trends.

The VLF-EM 16 survey, while it has identified these trends,

does not indicate whether these responses are due to conductive

overburden or conductivity associated with bedrock features. It is

therefore recommended that the stronger VLF-EM 16 anomalies be

surveyed using the Induced Polarization (IP) method. Much of the

gold mineralization in the Geraldton area is associated with only

minor sulphide mineralization. In this regard, the IP unit is

particularly useful since it responds to zones of weak

mineralization where the conducitivity is low. Once this IP survey

has been completed, and favourable zones been delineated then an

effective drilling program can be mounted.

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lM The outcrop density is much greater over the metavolcanics than

over the intrusive. In addition, there is only a thin overburden

l cover. Consequently, the area is a suitable one for a soil

geochemistry survey. A number of interesting prospects have been

l identified by the geological mapping and it is therefore

recommended that a soil sampling program be conducted over the more

favourable area. This area would be from L O to L 3600W between

l 2800S and the southern boundary of the property. Once completed,

areas of anomalous gold values could be trenched and if necessary,

l be investigated by diamond drilling.

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BIBLIOGRAPHY

D. R. Scammell (1984): Geraldton Project, Croll/Coltham Townships (Tunder Bay Mining District), Geraldton, Ontario. December 1984.

S. E. Amukun (1984): Geology of the Klob Lake Area, District of Thunder Bay; OGS Report 235.

J. K. Mason 6 C. D. Mcconnell (1983): The Geology of Gold in Ontario, Gold Mineralization in the Beardmore- Geraldton Area; OGS Misc. Paper 110, pp.84-97.

A. J. MacDonald (1983): The Geology of Gold in Ontario, The Iron Formation-Gold Association Evidence from the Geraldton Area; OGS Misc. Paper 110, pp.75-83.

H. C. Horwood fc G. G. Pye (1951): Geology of Ashmore Township; 60th Annual Report of the Ontario Department of Mines, Vol. LX, Part V, 1951.

H. W. Fairbairn '(1937): Geplogy of the Northern Long Lake Area; 46th Annual Report of the Ontario Department of Mines, Vol. XLVI, Part III, 1937, pp. 1-22.

1l11111111111111111

^ APPENDIX I

BUDGET

Phase I

Geochemical surveys, 1700 samples @ 512/sampleAccommodation, 40 mandays @ 575/mandayTransportationIP survey, 15 miles @ 51000/mileDraftingSupervisor

Contingency

TOTAL

Phase II

Diamond drilling, 1500' @ 530/ftAssays, 65 samples @ 515/sample Accommodation, 30 mandays @ 575/mandayTransportationSupervision Drafting

Contingency

TOTAL

GRAND TOTAL

'

520,4003,0003,00015,0002,0003,000

546,4003,600

550,000

545,000975

2,2502,00013,500 1,500

565,2259,775

5 75,000

5125,000

V)

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s)

Township or Area

Claim Holder(

J^

Survey Company

Author of Report

Address of Author 2So

b. (L. SCAKK&LL

} IttrtHfriJb MmCovering Dates of Survey_

Total Miles of Line Cut

(linecutting to office)

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

Geophysical

Electromagnetic.

DAYS per claim

-Other.

Geological. Lo

AIRBORNE CREDITS (Special provision credit! do not apply to airborne mrvcyi)

Magnetometer. .Electromagnetic.

DATE:.

(enter days per claim)

SIGNATURE:.Author of Report or Agent

Res. Geol. .Qualifications.

Previous Surveys File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

(prefix) (number)

TB 736171 - TB 736455

TB 732801 - TB 732803

TB 766698 - TB 766700-

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291

9*37 "

Mining Claims

Prefix Number Prefix Number

TB 736 171 TB 736 192

172 193173 194

174 195

175 196

176 197

177 198

178 199

179 200

180 201

181 - . 202182 203

183 204

184 . 205

185 . 206186 207

187 208

188 209

189 210

190 211

191 212

213

214

Mining Claim Prefix Number

T3736 21S

216

217

218

219

220

221

222

223

224•••f- 225

226

227

228

229

230

231

232

233

234

235

236

237

238

239

240

241

242

243

244

Prefix Number

736 245

246

247

248

249250

251252-

253.

254255 .

256

257

258

259260

261

262263264

^265

266

267

^268

269 270-

271272273

; 274

Prefix Number

736 275 .

276

277

278

279 280-

281 '

282

283

284.i-

- " ,, 285

286

287

288

289

290

291

292

293

294

295

296

297

298

299

300

301

302

303

304

TTt-91C

SAC

OK

6CE

8CC

CiC

BO*

sot*

TieOZ.C

69C

sec

S9C

66C

96C

S6C

T9C

09C

6SC

8SC

isc9SC

ESC

2SE

iseSK

sse

oie

osesoe

8iC

LLlgoe soe

Mining Claim

Prefix Number o-0 ^ v-^ "™ "' -- 1 " i * ^ *. w ~ -.A

736 41-3' 7 36

414 rf,,44241 5

. 443416 x^^444417 A Att445418 A AC446419 447

- 420 448

421 449

422 450

' 4 23 451

424

425

426

427

428

732 .801430

431 803432

433 . 766 698434 699435

436 766 700437

438

439

440

a. e i aa CROLL 900

Mining Lands Section

Control Sheet

Pile No

TYPE OF SURVEY GEOPHYSICAL

GEOLOGICAL

GEOCHEMICAL

EXPENDITURE

MINING LANDS COMMENTS:

tfc

Signature of Assessor

l

Date

* Minislryol Natural

'sourcesOntario

Report of Work(Geophysical, Geological, Geochemical and Expenditures)

Mining Act

Instructions: - Pleose type 01 print.II number of mining claims traversed exceeds space on this form, attach a l ist.

Note: - Only days credits calculated in the "Expenditures" section may he entered in the "Expend. Days Cr." columns.

— Do not use shaded areas below.Type of SiKvey(s)

Claim Holder(t)Geological

Township or Area (^ -*WI J f

Croll/Coltham Twps.K'-

Golden Pond Resources Ltd.Prospector's Licence No.

T 1655Address , B,C-Survey Company

JMetallge.sells.ahaft. Canada Ltd,Date of Survey (from S to) Total Miles of line Cut

198.5(319.4 kmName and Address of Author (of Oeo-Technical report)

D. R. Scammell, 298 Ruggles Ave., Richmond Hill, Ont. L4C 1Z1Credits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

Geological

Geochemica'l

Airborne Credits

Note: Special provisions j Electromagnetic credits do not applyto Airborne Surveys. Magnetometer

Radiometric

Mining Claims Traversed (List in numerical sequence)Days per,

Claim

Days per Claim

i

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

\(

Mining ClaimPrefix

TB

W

MM

Number

736-171

172

173

174

175

176

177

178

179

180

181

182

183

* 184

185

.. —......1.86 . ..-...—.187

——.....188...

—— 11 n il flfl...Ministry pf^at

REC'E

Expend. Days C'.

—— —— —

—— — ——

... ... ...

•MHMH

Jra! RwVEO

•MM

Dur

N Prefix

TB

•MMMU

ces

"Total nt. claims c

'

lining Claim Number

••-

736-192

193

194

195

196

197

198

t 199

200

201

202

203

204

205

— -

206

207

208

20?

211

212

213

214nber of mining vcroH lw thi*.

—— .

Expend. Days Cr.

— —- —

-------

— —— - ——

291

in columns at right.

Date i l

/1/0-3/rSRecorded Holder or Agent (Signature)

Certification Ver i tying Report of Work1 hereby certify that 1 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 Postal Address of Person Certifying

D. R. Scammell, 298Richmond Hill, Ont.

Rucfcrles Ave.Date Certified

L4C 1Z1 'V 05/Certified by (Signature) i

f O ^ /W f^** CA^w^-r^C-^V.13G2 f81/9)

Mining ClaimPrefix Number Days Prefix Number Days Prefix Number DaysTB736 215 1

216 (

217 (

218 (

219 (

220 *

221 (

222 (

223 (

224 (

225 (

226 (

227 (

228 i

229 (230 (

23JL (232 (

233 i

234 (

235 (

236 (

f TB736 245 1

( 246 (

247 (

1 248 l

249 (

250 *

251 *252 1253 (

l 254 (

255 . (256 (

1 257 ( . 258 (

) 259 (l 260 () 261 . (

262 *i 263 *i 264 (b 265 (b 266 (

237 j b ' 267 1

238 (

239240'241

) 268 1) 269) 270-D 271 i

242 It. 272 i

243 E|O 273 i

244 H) 274 lt

TB736 275276 .277278279280-

281282 1283 1284285 1286 1287 ( 288 1

' . 289 (290 (291 (292 f

l 293 (l 294 (1 295 (

296 (297 *298 t299 (300 (301 (302 (

i 303 (304 (

f

J

1lli

'

Mining Claim

Prefix Number Days Prefix Number Days Prefix Number DavsTB736 305

306307308 l309 *310 (311 i312 (

313 ( 314 f

.315 1

316 (

317 f

318 (

319 1

320 (

321 (

322 (

323 (

324 (

325 f

326 (

327 (

328 (

329 (

330 (

331 (332 f

333 C

334 (

335 (

336 e337 f

338 6

339 6

340 6

I TB 736 341342 1

343 (

344) 345) 346) 347) 348) 349 ( ) 350) 351) 352 . l) 353) 354) ' 355 () 356 1

) 357 (

) 358

) 359 1

) 360

) 361) 362

) 363 1) 364 {

) 365 (

) 366 1

) 367 (

) 368 f369 (

370 (

371 (372 C

373 t

374 (

375 t

376 *

l TB 736 377) 378

) 379) 380) 381) 382

) 383) 384

1 385 386

) 387) 388

389) 3901 391i 3.921 393i 394) 395l 396) 397 1

1 398 i

) 399 il 400 i1 401 1

) 402 l

) 403 1) 404 1) 405 (

) 406 (

407 (

408 (

409 (

410 (

411 (

412 (

i* i

i

i

1

l

Mining Claim

Prefix Number Days Prefix NumberTB 736 413

414

415 (416

417

418 i

419

420

421

422 i

t l TB 736 441

442

( 443(j 444

Q 445

| 446

j 447

| 448

| 449

J 450

423 J! 451424 i \ 4 52425 (

426 (

427 (

428 i (

429 f

430 1

453454'455 X

732 801

f 802431 Jf 803432 l \

433

434 i (

435 ( (436 i (437 1 (

438 l C

439 Jc

440 1C

- -. 766 698699

766 700

Ministry ofNaturalResources

ano

1985 06 03

Mining RecorderMinistry of Natural ResourcesP.O. Box 5000Thunder Bay, OntarioP7C 5G6

Dear Madam:

Your File: 127 Our File: 2.8120

f

Enclosed are two copies of a Notice of Intent with statements listing a reduced rate of assessment work credits to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain the other. In approximately fifteen days from the above date, a final letter of approval of these credits will be sent to you. On receipt of the approval letter, you may then change the work entries on the claim record sheets.For further information, if required, please contact Mr. R.J. Pichette at 416/965-4888.

Yours sincerely,

S.E. YundtDirectorLand Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3

S. Hurst:mc

Ends.

cc:

cc:

845

Golden Pond Resources LtdSuite 1520609 Granville StreetBox 10352Vancouver, B.C.V7Y 1G5D.R. Scammell298 Ruggles AvenueRichmond Hill, OntarioL4C 1Z1

cc: Mr. G.H. FergusonMining X Lands Commissioner Toronto, Ontario


Ontario

Notice of Intent

for Technical Reports

1985 06 03

2.8120/127

An examination of your survey report indicates that the requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on his record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.

If you are of the opinion that these changes by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.

If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.

If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days" method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted direct to the Land Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked will be issued.

B AB ISS/B)

Ministry of Natural

sourcesOntario

Technical Assessment Work Credits Date

1585 06 03

File

2.Ri?nMining Recorder's Report of Work No.

1?7

Recorded Holder

GOLDEN POND RESOURCES l TDTownship or Area

i /mi TH&M

Type of survey and number of Assessment days credit per claim

Geophysical

Flertrnmagnntir

Mflgnntnmpter

Rudinmetrir

Induced pnlari;ation

Other

Section 77 (19) See "Mining Cleimi Assessed'

Renlngiral 20

finnr.hRmiral

days

days

days

days

days

' column

dayt

days

Man days C3 Airborne D

Special provision Q Ground Cj3

O Credits have been reduced becausecoverage of claims.

Q Credits have been reduced because ofto work dates and figures of applicant.

of partial

corrections

Mining Claims Assessed

TD "1 O C1 7 1ID 7 OD 1/1

736174 to 313TOCO1 C7 00 JlD

736317 to 325736327 to 372736374 to 421736423 to 445736447 to 455732801-02-03766698-99766700

Inclusive

inclusiveinclusiveinclusiveinclusiveinclusive

Special credit! under section 77 (16) for the following mining claims

10 DAYS

TB 736172736314-16-26-73

5 DAYS

TB 736173 736422-46

No credits have been allowed for the following mining claims

LJ not sufficiently covered by the survey LJ Insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 77 (19)—60:028 (83f6t

1985 07 03 Your File: 127 Our File: 2.8120


Dear Madam:

RE: Notice of Intent dated June 13, 1985 Geological Survey on Mining Claims TB 736171, et al, 1n Croll and Coltham Townships

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.

Yours sincerely,


Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1M3 Phone:(416)965-4888

S. Hurst:mc

cc: Golden Pond Resources Ltd Vancouver, B.C.

cc: Resident Geologist Thunder Bay, Ontario

Encl.

cc: D.R, ScammellRichmond Hill, Ontario

co Mr. G.H. FergusonMining fi Lands Commissioner Toronto, Ontario

Ministry of Natural

f P-sourcesf; Ontario, \ J

Technical Assessment Work Credits

D8W 1 985 06 13

File

? fti?nMining Recorder's Report of Work No.

1?7

Recorded Holder

Township or AreaGOLDEN POND RESOURCES lin

i /rni TH&M

i"

fi

f"

T:

fF

f'

:"

j

'f

Fi;l

a-'

F

E

,.

Is

i-

Type of survey and number of Assessment dayt credit per claim

Geophysical

Electromagnetic '

M tomntor

Inrluf-art polarization

nth.r

Section 77 (19) Se* "Mining Clalmt Aliened'

ftpnlnniral 9Q

fipnrhpmif*Al

days

dayi

dayt

days

days

' column

dayt

dayt

Man days CD Airborne CD

Special provision Q Ground Cxl

Q. Credits have been reduced becausecoverage of claims.

Q Credits have been reduced because ofto work dates and figures of applicant.

of partial

corrections

Mining Claims Assessed

TB 736171736174 to 313736315736317 to 325736327 to 372736374 to 421736423 to 445736447 to 455732801-02-03766698-99766700

inclusive

InclusiveinclusiveInclusiveinclusiveinclusive

Special credits under section 77 ( 16) for the following mining claims

10 DAYS

TB 736172736314-16-26-73

.5 DAYS

TB 736173 736422-46

No credits have been allowed for the following mining claims

LJ not sufficiently covered by the survey O Insufficient technical data filed

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40; Section 77 (19)—60:828 (83/6)

llano


1985 06 13 Your File: 127Our File: 2.8120


Dear Madam:

Enclosed are two copies of a Notice of Intent with statements listing a reduced rate of assessment work credits to be allowed for a technical survey. Please forward one copy to the recorded holder of the claims and retain the other. In approximately fifteen days from the above date, a final letter of approval of these credits will be sent to you. On receipt of the approval letter, you ma,y then change the work entries on the claim record sheets.For further information, if required, pi eas.e contact Mr. R.J. Pichette at 416/965-4888.

sincerely,

i.E. YXmdt lirex

Land Management Branch

Whitney Block, Room 6643 Queen's Park Toronto, Ontario M7A 1W3

-S. Hurst:mc

Ends.

cc: Golden Pond Resources LtdSuite 1520609 Granville StreetBox 10352Vancouver, B.C.V7Y 1G5

cc: D.R. Scammell298 Ruggles AvenueRichmond Hill, OntarioL4C 1Z1

cc: Mr. G.H. FergusonMining a Lands Commissioner Toronto, Ontario

845

REGISTERED

May 13, 1985 Work Report 1127

Golden Pond Resources LimitedSuite 1520609 Granville StreetBox 10352Vancouver, B.C*V7Y 1G5

Dear Sirs:

RE i Mining Claims TD 736171 et al in the Townships of Croll and Coltham.

I have not received the reports and maps (in duplicate) for the Geological survey on the above-mentioned claims*

AB the assessment "Report of Work" was recorded by the Mining Recorder on March 22, 1985, the 60 day period allowed by Section 77 of The Mining Act for the submission of the technical reports and maps to this office will expire on May 21, 1985.

If the material is not submitted to this office by May 21, 1985, I will have no alternative but to instruct the Mining Recorder to delete the work credits from the claim record sheets.

For further information, please contact Mr. Arthur Barr at (416)965-4688.

Yours sincerely,


Whitney Block, Rm 6643 Queen's Park Toronto, Ontario M7A 1W3 Phones (416)965-4888

S.Hursttsc

cct D.R. Scammell 298 Ruggles Ave Richmond Hill, Ont

cct Mining Recorder Thunder Bay, Ont*


Ontario

Notice of Intent

for Technical Reports

1985 06 13 2.8120/127

An examination of your survey report indicates that the requirements of The Ontario Mining Act have not been fully met to warrant maximum assessment work credits. This notice is merely a warning that you will not be allowed the number of assessment work days credits that you expected and also that in approximately 15 days from the above date, the mining recorder will be authorized to change the entries on his record sheets to agree with the enclosed statement. Please note that until such time as the recorder actually changes the entry on the record sheet, the status of the claim remains unchanged.

If you are of the opinion that these change's by the mining recorder will jeopardize your claims, you may during the next fifteen days apply to the Mining and Lands Commissioner for an extension of time. Abstracts should be sent with your application.

If the reduced rate of credits does not jeopardize the status of the claims then you need not seek relief from the Mining and Lands Commissioner and this Notice of Intent may be disregarded.

If your survey was submitted and assessed under the "Special Provision-Performance and Coverage" method and you are of the opinion that a re-appraisal under the "Man-days" method would result in the approval of a greater number of days credit per claim, you may, within the said fifteen day period, submit assessment work breakdowns listing the employees names, addresses and the dates and hours they worked. The new work breakdowns should be submitted direct to the Land Management Branch, Toronto. The report will be re-assessed and a new statement of credits based on actual days worked will be issued.

646 I82/&)

MmiSlryol

Natural , Resources

Ontario i

Report of Work {Geophysical. Geological, Geochemical a nd E xpenditures)

736-17Mining Act

Instructions: -

Noir -

Plr.isf UP' O' prmi.11 mimln 1 ' o' minifip f Unrris l r^vcr sr l I'nfiTtJi iit.it*1 on this io'm, fllt,(th a O'^v ^'W- ci *'(I'K call u lair M , n i h "t *f)'' n i;l!luiCi" srctit,)n fn.^v Ix 1 entert in ttip "Expcnci. Days C' " column Do nol yif shaded arras below

Type o' Su'veyUI

___ _ _GeologicalClaim Hofder(i)"

Golden Pond Resources Ltd.

J l ownihip o r Area V/^ - *i*4 ' *

jCroll/Colthaml ^ ^ ^ ^ ^,,

Prospector's Licence No.

T 1655Addreti

Survey Company

...JMet.allge.sellschaft Canada .Ltd,,

.

Date of Survey (from A to)

O-

Total Miles of line Cut

198.5(319.4 kmt)Name and Address of Author (of Geo Technical report)

D. R. Scammell, 298 Ruggles Ave., Richmond Hill, Ont. L4C 1Z1Credits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:

Enter 40 dayt. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total(s) here

Mining Claims Traversed (List in numerical sequence)Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

- Magnetometer

- Radiornetric

—- Othe

Geological

r r Mther,, V*- t'"

Geochemica

Airborne Credits

Note: Special provisionscredits do not apply to Airborne Surveys.

r'-' ' AW l-*' 1'-'''Electromagnetic

Magnetometer

Radiometric

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total Expenditures

S -h 151-11,1.-,. i.nm

Total Days Credits

=

in columns ai right

Date Record cd Holder or Agent (Signature)

Certification Verifying Report of Workl hereby certify that l have a personal end intimate knowledge of the (acts 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 repon is true.

Name and Postal Address of Person CeMityinfl

— .-P.*.—R.-'-. .^cajiynelJL. j-...29.8—Rug.gle.s-Ave..- Richmond Hill, Ont. LAC 1 Z1

Date Certified Certified by (Signature)

136? (81/9)

Mining Claim Prefix Number

TB736

T ..- VX

Days Prefix Number Days Prefix Number DaysTB736

•2TT

ti TB736

ZTT

Mining Claim Prefix Number Days

TB736

ttST

(to

Pre fix Number Days Prefix Number Days

TB 736 -34-t- 4f) TB 736 *3TT

-34-4-

t ,

Mining Claim

TB 736

42:

Prefix Number Days TB 736

732 .801-

766

766 JLOO

G-3

OT

OA

KE

ST

WP

SLO

NG

LA

CA

LF

RE

DL

AK

E

736335/

736

349

l 7

36

36

6

736

377

7362

51

73

62

70

7362

81

736

296

7593

11

736397 [

73

64

12

736427

——

-——

—l—

——

L——

—l

j l

J_

\

l__l_

__l

__

_

736

348

73

6 36

7 |7

36

376

736252

7

36

ZG

9 l 7

36 2

82

7

36

29

7

73

6 3

12 l

736V

396

| 73

6 4

13

7364261736444

VI_

___U

——

a

-ra

l

TR

l_____ '_

__

__

__

_._

__

__

__

__

__

__

__

.__

__

__

__

__

__

_J_

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L_

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_-l—

——

__

_f-

——

——

—L

.TB

TT

B T6

T

TB

TB

IT

B

TB

TB

ITB

. j&

J i

73

6224

l 73

6239

1 7

3625

31 7

36

26

8

736283

73

6 2

96

l 7

3B

3 1

3JJ7

36 3

95 l

73

6 4

14

l 73

6 4

25 |

73

6 4

45

736

-315

(1-7

36 3

37

&H

.——

——

——

——

——

——

——

—y^/

jg

(736

187

736)9

8 |7

362"ll

J 7

36

22

5

73

62

38

|736 2

54 j

73

6 2

67

| 73

6 28

4 |

736

295

l 736

314

736394

736

l T

D

\T

0

.-m

^

~R

B^^

|TB

l™

94^7

31 3

15^7

36 3

93

736

73

6 1

86

736

199

736

210

73

62

26

l

73

62

37

736255

73

62

66

7

36

28

5

-^—

4-—

—K-

----J

——

4-—

—V

'^.^^

03 S

7

36

185

l 7

36

20

0

736209

73

6 2

27

17

36

23

6 1

736

256736 2

65 736296736 2

9317363891736 3

92p36*l7

;736)4

22

736

45

3

736

340

17

36 3

44

173

6 37

1 73

6 37

2X

l

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—-f

- '—

——

l——

—

64

|73

6

28

7I7

36

29

2L

73

6 3

8817

3639

1 7

36

41

8i

f i

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—-i

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fri

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p - —

l

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73

62

9

17

36

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4

1736

2581

,736

263

73

6 28

8 73

6 29

1 7

36

387

'. 73

639O

J73

6 41

9 I7

3642

OC

RO

LL

TW

PC

OLT

HA

M

T W

P'b

m C

736 1

82

736203

736206

r 7

36

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t

736233

736

204

[736

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t7

3623

2| 7

36 2

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6 73

6 28

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736

181

73

62

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86

99

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10

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128

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)

FE

LS

IC

TO

IN

TE

RM

ED

IAT

E

INT

RU

SIV

E

RO

CK

S

5

Un

sub

div

ide

d5a

M

ass

ive

5b

Fo

lia

ted

5c

Gra

nite

5d

Dio

rite

, Q

ua

rlz

dio

rite

, G

ran

od

iori

te

MA

FIC

T

O

UL

TR

AM

AF

IC

INT

RU

SIV

E

RO

CK

S

4

Un

sub

div

ided

4a

Ga

bb

ro,

Ho

rnb

len

de

ga

bb

ro

ME

TA

SE

D1M

EN

TS

3 U

nsub

divi

ded

3a

Co

ng

lom

era

te

3b

San

dsto

ne,

Are

nit

e,

Ark

os

e,

Wac

ke ,

Qu

art

zit

e

3c

Sil

tsto

ne

3d

Arg

illite

, P

hylli

te,

Mud

ston

e,

Sha

le

3e

Gra

phite

3f

Iron

form

atio

n

FE

LS

IC

TO

INT

ER

ME

DIA

TE

M

ET

AV

OL

CA

NIC

S

2 U

nsu

bd

ivid

ed

2a

Rh

yolit

e (m

as

siv

e,

foli

ate

d,

sh

ea

red

)

2b

R

hyo

lite

po

rph

yry

, Q

ua

rtz

- fe

ldsp

ar

po

rph

yry

2c

Dac

ite,

Rhy

odac

ite2d

L

apill

i-tu

lf,.

C

rysta

l!-t

uff,

Lapilli-t

uff

2e

Ser

icite

sc

hist

MA

FIC

T

O

INT

ER

ME

DIA

TE

M

ET

AV

OLC

AN

ICS

l U

nsu

bdiv

ided

la

Basa

lt to

andesi

te :

mass

ive,

folia

ted

Ib

Ba

salt

to

an

de

site

; sc

his

tose

, sh

eare

d

le

Bas

alt

to

ande

site

- pi

llow

edId

B

asal

t to

an

desi

te:

porp

hyrit

ic!e

B

asal

t to

an

desi

te;

amyg

dalo

id,

vesi

cula

rIf

C

hlo

rite

sc

his

t

lg

Tu

ff

Ih

Vol

cani

c br

ecci

a (a

gglo

mer

ate,

la

pill

i-tu

ff,

tuff -

brec

cia)

•c? Q x

Geo

logi

cal

cont

act

Out

crop

Ou

tcro

p ^

4 s

q. m

)

Are

a

of

ou

tcro

p

Sch

isto

sity

(ve

rtic

al)

Sch

isto

sity

(di

p de

term

ined

) S

chis

tosi

ty

(dip

no

t de

term

ined

)

Cle

avag

e (v

ert

ical)

Cle

avag

e (d

ip

dete

rmin

ed)

Cle

avag

e (d

ip

not

dete

rmin

ed)

Join

t (v

ert

ica

l)Jo

int

(dip

d

ete

rmin

ed

)

Join

t (d

ip

not

dete

rmin

ed)

Cla

im

po

st

(loc

ated

)

Cla

im

po

st

(no

t lo

ca

ted

)

Stre

am

(dire

ctio

n of

flo

w i

ndic

ated

)S

tream

(inte

rmitt

ent)

Sw

amp

Bea

ver

dam

Tre

nch

Fault,

she

ar

ser

serici

tized

pot

pota

ssic

al

tera

tion

carb

carb

on

ati

zed

chl

chlo

riliz

ed

sil

silic

ifie

dep

id

epid

ote

tour

tour

mal

ine

qtz

q

uart

z

q.v.

quar

tz

vein

mag

m

agne

tite

cpy

ch

alc

op

yri

te

py

py

rite

po

pyrr

ho

tite

sph

spha

lerit

em

o m

oly

bd

en

ite

hem

he

mat

itepb

le

adAu

go

ld

cgf

coar

se

grai

ned

flow

amph

am

phib

olite

xen

xe

no

lith

SC

AL

E:C

OO

OM

ET

RE

S

O 5

0

100

3OO

5OO

META

LLGE

SELL

SCHA

FT

CANA

DA

LIMITE

DG

OLD

EN

PO

ND

/MC

L JO

INT

VE

NTU

RE

Cro

ll T

owns

hip,

Th

unde

r B

ay

Min

ing

Div

isio

n,

Ont

ario

N.T

.S.

42

E X

10

Wo

rk

byD

ate.

Dra

wn

byD

PS

Dat

e:J

an

1

98

5

' 500O

Dra

win

g

No

shee

t l

of

6

750

V

/"28

0

736195 lo

(cg

f)

LE

GE

ND

PLE

IST

OC

EN

E

Till

UN

CO

NF

OR

MIT

Y

PR

EC

AM

BR

IAN

MID

DL

E

8

LA

TE

P

RE

CA

MB

RIA

N

MA

FIC

IN

TR

US

IVE

R

OC

KS

6

Dia

base

Ga

Por

phyr

itic

diab

ase

EA

RL

Y

PR

EC

AM

BR

IAN

(A

RC

HE

AN

)

FE

LS

IC

TO

IN

TE

RM

ED

IAT

E

INT

RU

SIV

E

RO

CK

S

5 U

nsu

bd

ivid

ed

5a

Mas

sive

5b

Fo

liate

d5c

G

ran

ite5d

D

iorite

, Q

ua

rtz

dio

rite

, G

ran

od

iori

te

MA

FIC

T

O

UL

TR

AM

AF

IC

INT

RU

SIV

E

RO

CK

S

4 U

nsu

bd

ivid

ed4a

Ga

bb

ro,

Ho

rnb

len

de

gab

bro

ME

TA

SE

DIM

EN

TS

3 U

nsub

divi

ded

3a

Con

glom

erat

e3b

S

ands

tone

, A

renite

, A

rkos

e, W

acke

, Q

uart

zite

3c

Silt

ston

e3d

A

rgill

ite

, P

hylli

te,

Mud

ston

e,

Sha

le

3e

Gra

phite

3f

Iron

fo

rma

tion

FE

LS

IC

TO

INT

ER

ME

DIA

TE

M

ET

AV

OL

CA

NIC

S

2 U

nsub

divi

ded

2a

Rh

yo

lite

(m

assiv

e,

foliate

d,

sh

ea

red

)

2b

Rh

yolit

e p

orp

hyr

y,

Qu

artz

- f

eld

spar

p

orp

hyr

y

2c

Dacit

e,

Rh

yo

dacit

e

2d

L

ap

illi-t

uff

, C

rysta

ll-t

uff,

Lap

illi-t

uff

2e

Se

ric

ite

s

ch

ist

MA

FIC

T

O

INT

ER

ME

DIA

TE

M

ET

AV

OLC

AN

ICS

l U

nsu

bd

ivid

ed

la

Bas

alt

to

ande

site

- m

assi

ve,

folia

ted

Ib

Ba

salt

to

an

desit

e--

sc

his

tos

e,

she

ared

le

Bas

alt

to

ande

site

; pi

llow

edId

B

asalt

to

an

desit

e:

po

rph

yri

tic

le

Basalt

to

a

nd

es

ite

: am

yg

dalo

id,

ve

sic

ula

r

If

Ch

lorite

schis

t

lg

Tu

ff

Ih

Vo

lcan

ic

bre

cc

ia (

ag

glo

me

rate

, la

pilli-

tuff

, tu

ff-

bre

ccia

)

Q

Geo

logi

cal

cont

act

Out

crop

Out

crop

^4

sq.

m)

Are

a of

ou

tcro

p

Sch

isto

sity

(ve

rtic

al)

Sch

isto

sity

(di

p de

term

ined

)S

chis

tosi

ty

(dip

no

t de

term

ined

)

Cle

avag

e (v

ert

ical)

Cle

av

ag

e

(dip

de

term

ine

d)

Cle

av

ag

e

(dip

no

t d

eter

min

ed)

Join

t (v

ert

ica

l)

Join

t (d

ip

de

term

ine

d)

Jo

int

(dip

n

ot

dete

rmin

ed

)

Cla

im

post

(lo

cate

d)

Cla

im

post

(no

t lo

cate

d)

Str

ea

m

(dir

ec

tio

n

of

flow

in

dic

ate

d)

Stre

am

(inte

rmitt

ent)

Sw

amp

Bea

ver

dam

Tre

nch

Fau

lt, s

hear

ser

se

ric

itiz

ed

po

t p

ota

ssic

alt

era

tio

n

carb

c

arb

on

ati

zed

chl

ch

lori

tize

d

sil

silic

ifie

dep

id

epid

ote

tou

r to

urm

alin

e

qtz

q

uart

z

q.v.

q

ua

rtz

ve

in

mag

m

agne

tite

cpy

chal

copy

rite

py

py

rite

po

pyr

rho

tite

sph

sph

ale

rite

mo

mol

ybde

nite

hem

h

em

ati

te

pb

lead

Au

g

old

cgf

coar

se

grai

ned

flow

amph

am

phib

olit

exe

n xe

nolit

h

SC

ALE

: 5O

OO

ME

T R

ES

O

50

1O

O3

00

5OO

META

LLGE

SELL

SCHA

FT

CANA

DA

LIMITE

DG

OLD

EN

PO

ND

/MC

L

JOIN

T V

EN

TU

RE

Cro

ll To

wns

hip,

Th

unde

r B

ay

Min

ing

Div

isio

n,

Ont

ario

NT

S. 4

2 E

f 1O

GEO

LOG

YW

ork

byD

ate

Dra

wn

by

DR

SD

ate;

Jan.

19

85

Sca

'e

1 5

0O

O

shee

t 2

of

6

42

E1

0N

Ea

e5

1

2.8

12

0

CR

OL

L21

0

42E

ieN

E(W

51

2.8

12

* C

RO

LL

LE

GE

ND

PLE

IST

OC

EN

E

Till

UN

CO

NF

OR

MIT

Y

PR

EC

AM

BR

IAN

MID

DLE

a

LA

TE

P

RE

CA

MB

RIA

N

MA

FIC

IN

TR

US

IVE

R

OC

KS

6 D

iaba

se6a

P

orph

yriti

c di

abas

e

EA

RLY

P

RE

CA

MB

RIA

N

(AR

CH

EA

N)

FE

LS

IC

TO

INT

ER

ME

DIA

TE

IN

TR

US

IVE

R

OC

KS

5 U

nsu

bd

ivid

ed

5a

Mas

sive

5b

Fo

liate

d5c

G

ranite

5d

D

iorite

j Q

ua

rtz

dio

rite

, G

ranodio

rite

MA

FIC

T

O

UL

TR

AM

AF

IC

INT

RU

SIV

E

RO

CK

S

4 U

nsub

divi

ded

4a

Gab

bro,

Hor

nble

nde

gabb

ro

ME

TA

SE

DIM

EN

TS

3 U

nsub

divi

ded

3a

Con

glom

erat

e3b

S

andst

one,

Are

nite

, A

rkose

, W

acke

, Q

uart

zite

3c

Silt

stone

3d

Arg

illite

, P

hylli

te,

Mud

ston

e,

Sha

le

3e

Gra

phite

3f

Iron

form

atio

n

FE

LS

IC

TO

INT

ER

ME

DIA

TE

M

ET

AV

OLC

AN

ICS

2 U

nsub

divi

ded

2a

Rhy

olite

(m

assi

ve,

folia

ted,

sh

eare

d)2b

R

hyo

lite

porp

hyr

y,

Quart

z -

feld

spar

porp

hyr

y

2c

Daci

te,

Rh

yod

aci

te

2d

La

pill

i-tu

ff,

Cry

sta

ll-t

uff.

Lapilli-t

uff

2e

Ser

icite

sc

hist

MA

FIC

T

O

INT

ER

ME

DIA

TE

M

ET

AV

OLC

AN

ICS

l U

nsub

divi

ded

la

Bas

alt

to

ande

site

- m

assi

ve,

folia

ted

Ib

Bas

alt

to

ande

site

-- s

chis

tose

, sh

eare

dle

B

asal

t to

an

desi

te;

pillo

wed

Id

Bas

alt

to

ande

site

; po

rphy

ritic

le

Bas

alt

to

ande

site

- am

ygda

loid

, ve

sicu

lar

If

Ch

lorite

sc

his

t

lg

Tu

ff

Ir

Vol

cani

c br

ecci

a (a

gglo

mer

ate,

la

pill

i-tu

ff,

tuff

- br

ecci

a)

a x

Geo

logi

cal

cont

act

Out

crop

Outc

rop ^4

sq.

m)

Are

a

of

outc

rop

Sch

isto

sity

(ve

rtic

al)

Sch

isto

sity

(di

p de

term

ined

) S

chis

tosi

ty (

dip

not

dete

rmin

ed)

Cle

avag

e (v

ertic

al)

Cle

ava

ge

(dip

d

ete

rmin

ed

)

Cle

avag

e (d

ip

not

dete

rmin

ed)

Join

t (v

ert

ica

l)Join

t (d

ip

dete

rmin

ed)

Join

t (d

ip

not

dete

rmin

ed)

Cla

im

post

(lo

cate

d)

Cla

im

post

(no

t lo

cate

d)

Stre

am (

dire

ctio

n of

flo

w i

ndic

ated

)St

ream

(in

term

itten

t)S

wam

pB

eave

r d

am

Tren

chF

au

lt,

she

ar

ser

se

ricitiz

ed

pot

pota

ssic

al

tera

tion

carb

ca

rbo

na

tized

chl

chlo

ritiz

edsi

l si

licifi

ed

epid

ep

idot

eto

ur

tour

mal

ine

qtz

q

ua

rtz

q.v-

q

ua

rtz

vein

mag

m

agne

tite

cpy

chal

copy

rite

p y

pyrite

po

pyrr

ho

tite

sph

sph

ale

rite

mo

mo

lybd

en

ite

hem

he

mat

itepb

le

ad

Au

gold

cgf

coar

se

grai

ned

flow

amph

am

phib

olite

xen

xenolit

h

SC

AL

E:

SO

OO

ME

TR

ES

O 5O

10

03O

O5

00

META

LLGE

SELL

SCHA

FT

CANA

DA

LIMITE

DG

OLD

EN

P

ON

D/M

CL

JOIN

T

VE

NT

UR

EC

roll

Tow

nshi

p,

Thun

der

Bay

M

inin

g D

ivis

ion,

O

ntar

io

——

N.T

.S.

42

E f

10

GEO

LOG

YW

ork

byD

ate:

Dra

wn

by-

OPS

Da

te;

Jan

1

98

5

Sca

le' 5

00

0D

raw

ing

No-

shee

t 3

of

6T

RA

NU

-AR

LE

GE

ND

PLE

IST

OC

EN

E

Till

UN

CO

NF

OR

MIT

Y

PR

EC

AM

BR

IAN

MID

DLE

S

LA

TE

P

RE

CA

MB

RIA

N

MA

FIC

IN

TR

US

IVE

R

OC

KS

6 D

iab

as

e

6a

Porp

hyritic

dia

base

EA

RL

Y

PR

EC

AM

BR

IAN

(A

RC

HE

AN

)

FE

LS

IC

TO

IN

TE

RM

ED

IAT

E

INT

RU

SIV

E

RO

CK

S

5 U

nsu

bd

ivid

ed

5a

Mas

sive

5b

Fol

iate

d5c

G

ran

ite5d

D

iorite

, Q

ua

rtz

dio

rite

, G

ran

od

iori

te

MA

FIC

T

O

UL

TR

AM

AF

IC

INT

RU

SIV

E

RO

CK

S

4

Un

sub

div

ided

4a

G

ab

bro

, H

orn

ble

nd

e g

abb

ro

ME

TA

SE

DIM

EN

TS

3 U

nsub

divi

ded

3a

Co

ng

lom

era

te

3b

S

an

dsto

ne,

Are

nit

e,

Ark

os

e,

Wa

ck

e ,

Qu

art

zit

e

3c

Sil

tsto

ne

3d

Arg

illite

, P

hyl

lite,

Mud

ston

e, S

hale

3e

Gra

ph

ite

3f

Iron

fo

rmatio

n

FE

LS

IC

TO

IN

TE

RM

ED

IAT

E

ME

TA

VO

LC

AN

IC S

2 U

nsu

bd

ivid

ed

2a

Rh

yo

lite

(m

assiv

e,

foli

ate

d,

sh

ea

red

)

2b

R

hyo

lite

porp

hy

ry,

Qu

art

z -

feld

sp

ar

po

rph

yry

2c

Dacit

e,

Rhyo

daci

te

2d

La

pill

i-tu

ff,

Cry

sta

l!-t

uff

, L

apilli-t

uff

2e

Ser

icit

e sc

his

t

MA

FIC

T

O

INT

ER

ME

DIA

TE

M

ET

AV

OL

CA

NIC

S

l U

nsu

bd

ivid

ed

la

Bas

alt

to

and

esit

e - m

assi

ve,

folia

ted

Ib

Bas

alt

to

and

esit

e ; s

chis

tose

, sh

eare

d

le

Basa

lt to

a

nd

esit

e ;

pillo

wed

Id

Ba

sa

lt

to

an

desit

e:

po

rph

yri

tic

le

Bas

alt

to

ande

site

? am

ygd

alo

id,

vesi

cula

r

If

Chlo

rite

sc

his

t

lg

Tu

ff

Ih

Vo

lca

nic

b

reccia

(a

gg

lom

era

te,

lapill

i- t

uff

, tu

ff-

bre

ccia

)

D

Geo

log

ical

co

nta

ct

Ou

tcro

p

Out

crop

^4

sq.

m)

Are

a of

ou

tcro

p

Sch

isto

sity

(ve

rtic

al)

Sch

isto

sity

(di

p de

term

ined

)

Sch

isto

sity

(d

ip

not

dete

rmin

ed)

Cle

avag

e

(vert

ical)

Cle

avag

e (d

ip

det

erm

ined

)

Cle

avag

e

(dip

n

ot

de

term

ine

d)

Join

t (v

ert

ica

l)Jo

int

(dip

de

term

ined

)Jo

int

(dip

n

ot

de

term

ined

)

Cla

im

post

(lo

cate

d)

Cla

im

post

(n

ot

loca

ted)

Str

eam

(d

ire

ctio

n

of

flo

w

ind

ica

ted

)

Stre

am

(inte

rmitt

ent)

Sw

amp

Beav

er d

amT

renc

hF

au

lt,

sh

ea

r

ser

serici

tized

pot

pota

ssic

al

tera

tion

carb

c

arb

on

ati

zed

chl

chlo

ritiz

ed

sil

silic

ified

epid

e

pid

ote

tou

r to

urm

alin

e

qtz

q

uart

z

q.v.

q

uart

z

vein

mag

m

agne

tite

cp

y

ch

alc

op

yri

te

py

py

rite

po

p

yrr

ho

tite

sph

spha

lerit

em

o

mo

lyb

de

nit

e

hem

h

em

ati

te

pb

lead

Au

gold

cgf

coar

se

grai

ned

flow

amph

am

phib

olite

xen

xe

no

lith

SC

AL

E:

SO

OO

ME

T R

ES

O 50

100

3OO

50

O

META

LLGE

SELL

SCHA

FT

CANA

DA

LIMITE

DG

OLD

EN

PO

ND

/MC

L

JOIN

T V

EN

TU

RE

Cro

ll-T

owns

hip,

Th

unde

r B

ay

Min

ing

Div

isio

n,

Ont

ario

——

—N

.T.S

. 42

E X

10

GEO

LOG

YW

ork

by

Dat

e-

Dra

wn

byD

RS

Dat

e,

Jan

1985

Sca

le'5

00

0

Dra

win

g

No.

shee

t 4

of

6

42

E1

0N

Ee

e5

1

2.8

12

0

CR

OL

L2

30

5 d sh

, qv

, ca

rb,

chl,

tour.

)

LE

GE

ND

PLE

IST

OC

EN

E

Till

UN

CO

NF

OR

MIT

Y

PR

EC

AM

BR

IAN

MID

DLE

8

LA

TE

P

RE

CA

MB

RIA

N

MA

FIC

IN

TR

US

IVE

R

OC

KS

6 D

iaba

se6a

P

orph

yriti

c di

abas

e

EA

RL

Y

PR

EC

AM

BR

IAN

(A

RC

HE

AN

)

FE

LSfC

T

O

INT

ER

ME

DIA

TE

IN

TR

US

IVE

R

OC

KS

5 U

nsub

divi

ded

5a

Mas

sive

5b

Folia

ted

5c

Gra

nite

5d

Dio

rite

, Q

uart

z dio

rite

, G

ran

od

iori

te

MA

FIC

TO

U

LT

RA

MA

FIC

IN

TR

US

IVE

R

OC

KS

4

Un

su

bd

ivid

ed

40

Gab

bro

, H

orn

ble

nd

e

gab

bro

ME

TA

SE

DIM

EN

TS

3 U

nsub

divi

ded

3a

Con

glom

erat

e3b

S

ands

tone

, A

renite

, A

rkos

e ,.

Wac

ke ,

Quart

zite

3c

Silt

stone

3d

Arg

illite

, P

hylli

te,

Mud

ston

e, S

hale

3e

Gra

phite

3f

Iron

form

atio

n

FE

LS

IC

TO

INT

ER

ME

DIA

TE

M

ET

AV

OL

CA

N IC

S

2 U

nsub

divi

ded

2a

Rh

yo

lite

(m

as

siv

e,

foliate

d,

sh

ea

red

)

2b

R

hy

oli

te

po

rph

yry

, Q

ua

rtz-f

eld

sp

ar

po

rph

yry

2c

Da

cite

, R

hyo

da

cite

2 d

Lapill

i-tu

ff,

Cry

sta

l!-t

uff,

Lap

illi-t

uff

2e

Se

rici

te

sch

ist

MA

FIC

T

O

INT

ER

ME

DIA

TE

M

ET

A V

OL

CA

NIC

S

l U

nsu

bd

ivid

ed

la

Basa

lt to

andesi

te ;

ma

ssiv

e,

folia

ted

Ib

Bas

alt

to

ande

site

: sc

hist

ose

, sh

eare

dle

B

asal

t to

an

desi

te -

pill

owed

Id

Bas

alt

to

ande

site

: po

rphy

ritic

le

Bas

alt

to

ande

site

-- a

myg

dalo

id,

vesi

cula

r

if

Chlo

rite

sc

his

t

lg

Tu

ff

!h

Vol

cani

c br

ecci

a (a

gglo

mer

ate,

la

pill

i-tu

ff,

tuff -

brec

cia)

Q

Geo

log

ical

co

nta

ct

Ou

tcro

p

Ou

tcro

p ^

4 s

q.

m)

Are

a

of

ou

tcro

p

Sch

isto

sity

(ve

rtic

al)

Sch

isto

sity

(d

ip

dete

rmin

ed)

Sch

isto

sity

(d

ip

not

dete

rmin

ed)

Cle

ava

ge

(ve

rtic

al)

Cle

ava

ge

(dip

dete

rmin

ed)

Cle

ava

ge

(dip

no

t d

ete

rmin

ed

)

Join

t (v

ert

ical)

Join

t (d

ip

dete

rmin

ed

)

Jo

int

(dip

n

ot

de

term

ine

d)

Cla

im

po

st

(loca

ted)

Cla

im

po

st

(no

t lo

cate

d)

Stre

am

(dire

ctio

n of

flo

w i

ndic

ated

)S

tream

(in

term

itten

t)S

wam

p

Bea

ver

dam

Tre

nc

h

Fault,

sh

ear

ser

se

ric

itiz

ed

pot

pota

ssic

al

tera

tion

carb

carb

on

ati

zed

chi

chlo

rttiz

ed

sil

silic

ifie

dep

id

epid

ote

tou

r to

urm

ali

ne

qtz

quart

z

q.v.

q

ua

rtz

ve

in

mag

m

agne

tite

cp

y

ch

alc

op

yri

te

py

py

rite

po

p

yrr

ho

tite

sph

- sp

hale

rite

mo

m

oly

bd

en

ite

hem

he

mat

itepb

le

adAu

go

ld

cgf

coar

se

grai

ned

flow

amph

am

phib

olite

xen

xenolit

h

SC

AU

EO

OO

OM

ET

R

ES

5O

10

0300

50

0

META

LLGE

SELL

SCHA

FT

CANA

DA

LIMITE

DG

OLD

EN

P

ON

D/M

CL

JOIN

T

VE

NTU

RE

Cro

ll To

wns

hip,

Th

unde

r Ba

y M

inin

g D

ivis

ion,

O

ntar

io —

——

N.T

.S,

42

E

/10

GEO

LOG

YW

ork

by

Dra

wn

by'

DRS

Dat

e;

Jan

. 1

98

5

Sca

le

5OO

OD

raw

ing

N

o

~

——

~

shee

t 5

of

6

LE

GE

ND

PLE

IST

OC

EN

E

Till

UN

CO

NFO

RM

ITY

PR

EC

AM

BR

IAN

MID

DLE

S

LA

TE

P

RE

CA

MB

RIA

N

MA

FIC

IN

TR

US

IVE

R

OC

KS

6 D

iaba

se6a

P

orp

hyr

itic

diab

ase

42E

10N

E80

51

2.8

12

0

CR

OLL

RB

T

RA

NS

UU

t

EA

RL

Y

PR

EC

AM

BR

IAN

(A

RC

HE

AN

) F

ELS

fC

TO

INT

ER

ME

DIA

TE

IN

TR

US

IVE

R

OC

KS

5 U

nsub

divi

ded

5a

Mas

sive

5b

Fo

liate

d5c

G

rani

te5d

D

iorit

e , Q

uart

z d

iorite

, G

ran

od

iorite

MA

FIC

T

O

ULT

RA

MA

FIC

IN

TR

US

IVE

R

OC

KS

4 U

nsub

divi

ded

4a

Ga

bb

ro,

Hor

nble

nde

gabb

ro

ME

TA

SE

DIM

EN

TS

3 U

nsub

divi

ded

3a

Con

glom

erat

e3b

S

ands

tone

, A

ren

ite,

Ark

ose

, W

acke

, Q

ua

rtzi

te3c

S

iltst

one

3d

A

rgill

ite,

Ph

ylli

te,

Mud

ston

e, S

ha

le

3e

Gra

phite

3f

Iron

form

atio

n

FE

LS

IC

TO

INT

ER

ME

DIA

TE

M

ET

AV

OLC

AN

ICS

2 U

nsub

divi

ded

2a

Rhy

olite

(m

assi

ve,

folia

ted,

shea

red)

2b

Rhy

olite

porp

hyr

y, Q

ua

rtz-f

eld

sp

ar

porp

hyr

y2c

D

acite

, R

hyod

acite

2d

La

pill

i-T

uff

, C

r ysta

ll-tu

ff,

Lapilli-t

uff

2e

Se

rici

te

schi

st

MA

FIC

T

O

INT

ER

ME

DIA

TE

M

ET

AV

OL

CA

N I

CS

l U

nsub

divi

ded

la

Bas

alt

to

ande

site

; m

assi

ve,

folia

ted

Ib

Bas

alt

to

an

de

site

; sc

hist

ose,

sh

eare

dle

B

asal

t to

an

desi

te :

pillo

wed

Id

Bas

alt

to

ande

site

; porp

hyr

itic

le

Bas

alt

to

ande

site

--

amyg

dalo

id,

vesi

cula

r

If

Chl

orite

sc

hist

lg

Tu

ff

in

Vol

cani

c b

recc

ia (

ag

glo

me

rate

, la

pill

i- t

uff

, tu

ff-

bre

ccia

)

Q xxxx

x x

Geo

logi

cal

cont

act

Out

crop

Out

crop

^4 s

q. m

)

Are

a of

o

utc

rop

Sch

isto

sity

(vert

ical)

Sch

isto

sity

(di

p dete

rmin

ed)

Sch

isto

sity

(d

ip

not

dete

rmin

ed)

Cle

avag

e (v

ert

ical)

Cle

avag

e (d

ip

dete

rmin

ed)

Cle

avag

e (d

ip

not

dete

rmin

ed)

Join

t (v

ert

ical)

Join

t (d

ip

de

term

ine

d)

Join

t (d

ip

not

dete

rmin

ed)

Cla

im

post

(loca

ted)

Cla

im

post

(n

ot

loca

ted

)

Str

eam

(d

irect

ion

of

flow

indic

ate

d)

Str

eam

(in

term

itte

nt)

Sw

amp

Bea

ver

dam

Tre

nch

Fa

ult,

sh

ear

ser

serici

tized

pot

pota

ssic

a

ltera

tion

carb

ca

rbon

atiz

ed

chl

chlo

ritiz

ed

sil

sili

cifie

dep

id

e prid

e t e

tour

tourm

alin

e

qtz

quart

z

q.v.

quart

z ve

in

mag

m

ag

ne

tite

cpy

chalc

opyr

ite

py

pyr

ite

po

pyrr

ho

tite

sph

sph

ale

rite

mo

mo

lyb

de

nite

hem

h

em

atit

e

pb

lead

Au

gold

cgf

coar

se

grai

ned

flow

amph

am

phib

olit

exe

n xe

no

lith

SC

AL

ES

OO

OM

ET

RE

S

O

50

!0

03O

O500

META

LLGE

SELL

SCHA

FT

CANA

DA

LIMITE

DG

OLD

EN

P

ON

D/M

CL

JO

INT

VE

NT

UR

EC

roll

Tow

nshi

p,

Thun

der

Bay

M

inin

g D

ivis

ion,

O

ntar

io —

——

N.T

.S.

42

E X

10

GEO

LOG

YW

ork

byD

ate:

Dra

wn

byD

RS

Dat

e,Ja

n

19

85

Sca

le-

'50

0O

No

shee

t 6

of

6

l received mining unds section - ontario

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