summary rpt on expl program - search … · and report that the recommended exploration program was...

42A82NW8188 2 .9683 CLEAVER 010

SUMMARY REPORT

ON THE

1986 EXPLORATION PROGRAM

ON THE CLEAVER TOWNSHIP

LARDER LAKE MINING DIVISION

PROPERTY OF

CLEYO RESOURCES INC.

PROJECT #6436

RECEIVED

MINING ILANDS SECTION

Timmins, Ontario by: Stephen Conquer, B.Se.

December 19, 1986 for: David R. Bell

Geological Services Inc.

TABLE 42A02Nweie8 2.9683 CLEAVER 010C

I.0 SUMMARY l, 2

2. O INTRODUCTION 3

3.0 LOCATION AND ACCESS 4

4.0 PROPERTY AND OWNERSHIP 4

5.0 PHYSIOGRAPHY AND CLIMATE 5

6.0 POWER AND WATER 6

7.0 ANCILLARY SERVICES 6

8.0 PREVIOUS WORK 6, 7

9.0 REGIONAL GEOLOGY AND STRUCTURE 7

9.1 REGIONAL GEOLOGY 7, 8

9.11 METAVOLCANIC ROCKS 8

9.12 METASEDIMENTS 9

9.13 INTRUSIVES 9, 109.2 REGIONAL STRUCTURE 10

10.0 PROPERTY GEOLOGY AND STRUCTURE 10

10.1 PROPERTY GEOLOGY 11

10.1.1 MAFIC FLOWS 11, 12

10.1.2 INTERMEDIATE TO MAFIC TUFFS 12

10.1.3 INTERMEDIATE TO FELSIC FLOWS 12, 13

10.1.4 FELSIC INTRUSIONS

10.2 PROPERTY STRUCTURE 13, 14

II.0 MINERALIZATION AND 14 MINERALIZED SHOWINGS

11.1 A-ZONE 14, 15

11.2 B-ZONE 15, 16

12.0 GEOPHYSICS 16 , 16a

13.0 CONCLUSIONS 17

14.0 RECOMMENDATIONS 18, 19

15.0 COST ESTIMATES 19, 20, 21

CERTIFICATE OF QUALIFICATIONS

REFERENCES

TABLE OF CONTENTS cont'd

List of Figures

Figure l

Figure 2

Figure 3

Figure 4

Figure 5

Figure 6

Figure 7

Figure 8

Figure 9

Figure 10

Location Map - Provincial

Location Map - Regional

Claims Configuration

Topography

Sand and Gravel Resource Map

Timmins-Kirkland Geological Compilation (OGS Map 2205)

A-Zone: Geology, Assays and Sample Locations

Magnetometer Survey

VLF-EM FRASER FILTER

Induced Polarization - Filtered Data: 7, Frequency Effect

List of Tables

Table l

Table 2

List of Maps Map 6436-86-3- Map 6436-86-4-

Map 6436-86-5-

Map 6436-86-5-

Map 6436-86-5-

Map 6436-86-5-

Map 6436-86-5-

Map 6436-86-5-

Claim Status

Previous Regional Exploration Activities

l Sample Location and Assay Planl Geology Map

1 Pseudo Sections L4E

2 Pseudo Sections L2E

3 Pseudo Sections LO

4 Pseudo Sections L2W



Apendicies

Appendix l

Appendix 2 Appendix 3

Sample Locations and Assay Results

Assay Certificates

Whole Rock Geochemical Results

Technical Data Statement

1.

.O SUMMARY

The Cleyo Resources-Cleaver Township property is

located in an area which has only seen sporadic exploration

since the early 1900's. In the spring of 1986, Mr. Cleo

Clement in the company of the property vendor, undertook a

site examination. From this property visit several grab

samples were collected, from which highly anomalous assay

results (0.10-0.20 range) were received. These encouraging

results, prompted Mr. Clement on behalf of Cleyo Resources

Inc. to approach the firm of David R. Bell Geological Services

Inc. with a request that a property visit be made and intro

ductory report be prepared. It was as a result of this visit

and report that the recommended exploration program was initi

ated. In light of the late start to the program and the early

arrival of winter, the proposed program could not be completed

and as a result, only the mapping and IP surveys were finished.

A minor amount of stripping was completed late in

the program, with these new exposures to be examined during

the recommended program.

The property was found to be underlain by a series

of interbedded intermediate to mafic flows. These flows show

a variety of flow features, strike northeast-southwest, dip

steeply to the south, and vary from non-magnetic to highly

magnetic.During the mapping program two auriferous zones were

located. One of these showings is located in the same outcrop

as the "Main Showing" that had been previously visited by the

author. Examination of this showing, which was limited by a

lack of good weather, found a highly brecciated, altered and

mineralized rock that gave assays of up to 0.088 oz Au/ton.

The second gold showing, also the site of some earlier trench

ing, was hosted by intermediate to mafic volcanics that have

2.

silicified and mineralized. Assays from this zone of

up to 267 ppb Au were received. The results from both zones

are found to be very encouraging in light of the limited

work that has been completed. These zones also show a cor

relation with either magnetometer, VLF-EM, or IP anomalies.

Due to these promising results, a three phase

exploration program totalling S263,000.00 has been recommended.

The initiation of this third phase will be contingent upon the

receipt of encouraging results from the first two phases.

..O INTRODUCTION

In October of 1986 the firm of David R. Bell Geolo

gical Services Inc. was contracted to initiate a exploratory

program. This program was recommended as a result of a prop

erty visit made during May of 1986 and a search of all pertin

ent company and government information. The McNeil-Cleaver

Township area is the location of several gold showings, but

at the time has received only sporadic exploration activity.

One showing in McNeil Township is hosted by mineralized rock

that contains visible gold.

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Property Location

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Savld R. Bell Geological Services Inc.

CLEYO RESOURCES INC.

LOCATION MAP

PROVINCIAL

Tw^/Area cleaver Two..Mining DivisionRclorcooo*

; DrawnScale

Larder Lake

Ore f todOat* June 17/86

Bovine* ont.Project 6436N.T.S.ChocKod

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.0 LOCATION AND ACCESS (see Figure l and 2)

The Cleyo Resources property is located 29 miles southeast of the city of Timmins in Cleaver Township, Larder Lake Mining

Division, in the District of Timiskaming, Ontario. This claim

group is found in the west-central portion of the township at 48.13 degrees north latitude and 81.47 degrees east longitude.

Access to Cleaver Township is gained by travelling approx imately 30 miles on the Langmuir Road, an all weather lumber road that runs southwest from the town of South Porcupine. Once in the vicinity of the property, three routes can be used to access the

northwest, north-central and south-central portions of the claim group. These access routes can be travelled using a two-wheel .

drive vehicle, but spring and fall weather may necessitate a

vehicle with four-wheel drive capabilities.

4.0 PROPERTY AND OWNERSHIP (see Figure 3)

The Cleyo Resources, Cleaver Township property is com posed of 27 contiguous unpatented mining claims (see Table 1) which are held in trust by Mr. Cleo Clement of Timmins, Ontario.

The property was optioned from Mr. William Dellaire of Timmins, Ontario, in January of 1986 and at that time consisted of only 23 claims. After reviewing the results of previous geo physical surveys and noting the location of the primary showing, the author recommended that an additional four claims should be staked. The acquisition of these claims would give complete coverage of this principle showing and any possible strike exten sion. These claims were subsequently staked in April of 1986, bringing the total number of claims to the present twenty-seven.

At the present time the 23 original claims (various recording dates in 1983) are under extension until Dec. 31, 1986, and require 40 days of assessment credits. The filing of this report for linecutting and geological survey credits will fulfill the necessary requirements to keep all claims in good standing until their respective anniversary or next filing dates in 1987 and 1988.

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David R. Bell Geological Services Inc.CLEYO RESOURCES INC.

LOCATION MAP

REGIONAL

Twp/Ar*. CLEAVER TWP. Pro vine o ON TMining Division LARDER LAKE Pro)* C t 6430

DrawnScat* 1:266000

DraftedDate JUNE

N.T.S. 42-A

Shoat FtQ.1

i as 11!s ..- - — -J - -

David R. Bel! Geologlcat Services Inc.CLEYO RESOURCES INC.

CLAIMS CONFIGURATION

Twp/Arca C leaver Twp.Minim OMttoii Larder Lake Pro)*ct 6436

H.T.S. A 2A/3

TABLE l

CLEYO RESOURCES INC. - CLEAVER TWP. PROPERTY

PROJECT 6436

CLAIM STATUS

Claim No. Recording Date

L724470 June 30, 1983

L724474 July 25, 1983

L725147 September 15, 1983

L725148 September 15, 1983

L725149 September 15, 1983

L725150 September 15, 1983

L725151 September 15, 1983

L725152 September 15, 1983

L725153 September 15, 1983

L725154 September 15, 1983

L725155 September 15, 1983

L725156 September 15, 1983

L725158 September 15, 1983

L725161 September 15, 1983

L725162 September 15, 1983

L749741 August 23, 1983

L749742 August 23, 1983

L749743 August 23, 1983

L749744 August 23, 1983

L749745 August 23, 1983 .

L749746 August 23, 1983

L750507 September 15, 1983

L750508 September 15, 1983

L916183 April 30, 1986

L916184 April 30, 1986

L916185 April 30, 1986

L916186 April 30, 1986

*Claims under extension until Dec Report of Work submitted Dec. 9,

Next F iling Da te

June 30, 1986

July 25, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

September 15, 1986

August 23, 1986

August 23, 1986

August 23, 1986

August 23, 1986

August 23, 1986

August 23, 1986

September 15, 1986

September 15, 1986

April 30, 1987

April 30, 1987

April 30, 1987

April 30, 1987

31, 19861986

No. of Days Required

40

40

40

40

40

40

40

40

40

40

40

40

40

40

40

40

4040

40

40

40

40

40

20

20

20

20

5.

0 PHYSIOGRAPHY AND CLIMATE ( see Figure 4)

The Gleyo property is situated in an area of mixed topography. A general pattern of low relief dominates this region with the elevation ranging from 1050 to 1150 feet above sea level. In the west half of Cleaver Township an area of moderate to high relief is present, here the terrain attains a maximum of 1500 feet above sea level. This north trending area of higher ground is probably caused by the Middle-Precam- brian Sediments of the Cobalt Group.

The claim group is drained by numerous lakes and rivers of the Nighthawk River system. This river system flows north and eventually drains into Nighthawk Lake.

Vegetation and overburden are typical of Northern Ontario. Sand, gravel and moderate to well developed "B" soil horizons are found in the higher better drained areas of the claim group, where poplar, birch, spruce and local stands of balsam fir are located. The lower lying areas of this property are covered by clay and water rich organic soils. It is in these areas that stands of cedar, spruce and alder dominate. In all areas, numerous types of mosses and grasses are present.

As a result of the Northern Ontario Engineering Geology Terrain Studies that were completed by the Ministry of Natural Resources, several sources of sand and gravel were located in this region (see Figure 5). In fact one such source is located on the Cleyo property. This source is a north trending esker that is found in the southeastern portion of the property. The Ministry has estimated that these local sources have a medium to high poten tial for coarse aggregate. These coarse aggregates will be valuable if the construction of access roads or mining facilities is ever initiated.

The climate of the area is characterized by hot, humid summers and long winters. An abundance of snowfall, and extreme cold are common during the winter months.

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RESOURCES

TOPOGRAPHY

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i ^ R* BeH Geological Services foe.CLEYO RESOURCES INC.

SAND AND GRAVEL

RESOURCE MAP

Cleaver Twp.givWon Larder Lake

00.000DrsrtedData June 17/86

A2A/SEChecked M .B. R

Fig. 5

..O POWER AND WATER

The power requirements for any early stages of explora

tion or development would have to be supplied by diesel generators

Although a major north-south power line is located 12 miles due

east of the Cleaver Township property, it may be more cost effect

ive to construct a power line from Matachewan, which is located

approximately 21 miles to the southeast. This is due to the fact

that the appropriate sub-stations are already present and there

fore construction costs may be minimized.

An abundant water supply for any exploration or early

development programs is present within the boundaries of this

property. If greater quantities of water are required, then

accessing the larger lakes to the southwest, or Nighthawk Lake

to the north, should meet any foreseeable requirements.

7.0 ANCILLARY SERVICES

All goods or services that would be needed for any of

the various exploration or mining phases could be acquired from

the city of Timmins.

8.0 PREVIOUS WORK

Prospecting and exploration for gold had begun in the

Matachewan district in as early as 1909, but the attention of

the prospectors soon swung to silver, as the discoveries near

Gowganda and Elk Lake were made. When the news of a major gold

discovery within the Porcupine Camp (1909) became wide spread,

the Matachewan area saw a renewed interest in gold exploration.

Numerous occurrences were uncovered in the townships of Powell,

Cairo, Alma and Baden. As well as private exploration, several

geological and topographical surveys were conducted by govern

ment agencies during the 1910's, especially in the vicinity of

the then, most current gold discoveries.

It was not until 1923 that any gold discoveries were made in the Cleaver-McNeil Townships area. Three Indians named Isador, Micmack and Tom Fox uncovered a gold showing in the south-central part of McNeil Township. This discovery led to the uncovering of several more occurrences in McNeil Township and eventually, Mr. Dan O'connor located two gold showings in the west-central section of Cleaver Township. Apparently nothing of significance ever came of these discoveries.

The Cleaver-McNeil area received very little attention during the intervening years between the 1920's and the 1950's. When exploration activities again increased, the bulk of the work was concentrated in the west half of Cleaver and the eastern part of McNeil Township. The companies and their respective explora tion activities as conducted in Cleaver Township are listed in Table 2.

The only work that has been recorded for the vicinity of the present Cleyo Resources property, has all been completed since 1974. Stripping and trenching have been completed by J. Boissoneault and R. Rousseau on ground that is now covered by claims L724470 and L724474. Linecutting, magnetometer and VLF-EM surveys were completed in early 1984 under a previous option agreement. The assessment credits for this work are still valid and in fact are being used to keep the claims in good standing. These surveys have outlined several areas of interest that have as yet not been examined.

9.0 REGIONAL GEOLOGY AND STRUCTURE (see Figure 6)

9.1 Regional Geology

Cleaver Township, and subsequently the Cleyo Resources property, is underlain by rocks that are entirely Precambrian age. The majority of the bedrock belongs to the Abitibi Green stone Belt, which being Early Precambrian or Archean in age, is a tectonically differentiated portion of the Superior Province

l

iTABLE 2

CLEYO RESOURCES INC. - CLEAVER TWP. PROPERTY

PROJECT #6436

PREVIOUS REGIONAL EXPLORATION ACTIVITIES

Jjleaver Twp.

ompany

Airiax

1 mperial Oil

JFeck

Joranda

tomstate Res. td.

w 'Connor

Jiamothe , Charles

T'exmont

Lang, Bert W.

1cNeil Twp.

fcompany

Noranda

C)ominco

1

1

Activity Year Assessment File No.

trenching, assaying, Oct. 76-Oct. 77 429441

HLEM, Max-Min

ground EM and Mag 1982 420367

Seismic, mag, drilling 1980-1981 537428

for placer gold

mag, HEM 1981 2.4423

mag, EM ? 2.4762

correspondence 1924 330

EM, drilling 1956 T-643

EM profiles 1965 ?

EM 1966 63.1838

Activity Year Assessment File No.

EM, mag ? ?

EM, mag ? ?

ii

8

'f the Canadian Shield. Rocks of Middle and Late Precambrian

age are respectively represented by Cobalt Group sediments and minor intrusions of diabase.

The Abitibi Greenstone Belt, in the vicinity of Cleaver Township, is composed of variably metamorphosed igneous, sedi

mentary and volcanically derived rocks (Pyke, 1978).

9.11 Metavoleanic Rocks

The metavolcanic rocks of this area are represented by at least two cycles of volcanism. The ultramafic rocks occupy

the lowest position of each cycle, while the mafic, intermediate and felsic rock types sit in respectively higher stratigraphic locations. The lowest of these two cycles, trends in a north-

south direction through Fripp, McArthur, Bartlett and English

Townships. The dominant, or upper cycle, shows an east-west, as opposed to the expected northerly trend. This may in part

be the result of the intrusion of the Geikie Pluton, even though the regional magnetometer survey suggests that this east-west trend, is more typical of the Cleaver-McNeil area.

The ultramafic metavolcanic rock types are by far the most sparcely distributed. Massive, polysutured and spinifex textured flows are the most common of these rocks, while pyro clastic units are found locally.

The most dominant of all rock types in this area are the mafic to intermediate metavolcanics. Lithological varieties included within these units are the massive, pillowed and vario

litic flows. In conjunction with these flows, pyroclastic rocks in the form of tuff, lapilli tuff and volcanic breccia are found.

The felsic metavolcanic rocks are represented by massive

and pillowed flows as well as the aforementioned types of pyro clastic rocks. Centers of felsic volcanism are located in the

area of Douglas-Fallon-Fasken and McArthur-Bartlett-English-Hutt Townships.

.12 Metasediments

Metasediments apparently, form only a very small portion

of this section of the Abitibi Greenstone Belt, comprising no more

than five percent of the exposed area. Where noted by previous

workers, the Early Precambrian metasediments are found to be assoc

iated with the intermediate to felsic volcanics (Pyke, 1978).

Middle Precambrian metasediments are represented by the Cobalt

Group, which in this area is composed of arkoses, greywackes and

argillites. These rocks lie in a thin band that runs in a north-

south direction through Montrose, Hincks, Cleaver and Fallon Town

ships .

9.13 Intrusives

The intrusive rocks which are present in this area,

range in chemical composition from felsic to untramafic.

The major felsic intrusions, such as the Peterlong Lake

Complex, and the Adams and Geikie Plutons, are composed of feld

spar and quartz porphyries, trondhjemites, granodiorites, quartz

diorites and diorites. Smaller intrusions of the same relative

compositions are also present in this area along with intrusions

of syenitic composition such as the Fallon Stock.

A large zone of mafic to ultramafic intrusions, is found

in the central portion of the lower most volcanic cycle, sitting

at the contact between the mafic and the intermediate to felsic

volcanics. There appears to be a genetic relationship between

these intrusive bodies and the more "felsic" rock types, as is

noted by their close spatial association in the Bartlett-McArthur

and Zavitz-Hutt Townships area. These intrusives may be composite

bodies of the following, gabbro, gabbroic anorthosite, pyroxenite,

serpentinized peridotite, and quartz gabbro. Other gabbro intru

sions have been noted in McNeil Township. As a result of the

10

linear magnetic trends in the Cleaver-McNeil area and the mag

netic anomalies in Cleaver Township it is possible that other

mafic stocks or plugs may be located within the vicinity of the

project area,

9.2 Regional Structure

As previously noted, the volcanic rocks of this area

show two major trends. The lower cycle trends north-south, gen

erally dips to the east at 65 to 80 degrees (local variations

are present), while tops face east showing that these units have

not been overturned. Except for major north-south faults these

rocks do not appear to have been severely deformed, at least

folding on a large scale is not evident.

The upper volcanic cycle, has undergone deformation,

by both folding and faulting. Numerous anticlinal and synclinal

structures are located within Douglas, Zavitz and Hutt Townships,

These are crosscut and offset by the northerly and northwesterly

trending faults that transect this area.

Details as to the structural make-up of the Cleaver-

McNeil area are limited due to the lack of any detailed explor

ation by either government or private industry.

10.0 PROPERTY GEOLOGY AND STRUCTURE

During the course of the mapping program approximately

200 bedrock outcroppings were examined for geological, mineral

ogical and structural information. Although this sounds like a

substantial amount of exposure, it in fact represents only about

ID-15% of the entire property. In so far as this is the situ

ation, geophysical (magnetometer and VLF-EM) data from previous

surveys was used as an interpretational aid to develop a geolo

gical framework from which further exploration could be recom

mended.

11.

10.1 Property Geology (see Map 6436-86-4-1)

The Cleyo Resources-Cleaver Township property is

found to be underlain by rocks that are of early Precambrian

age. Through field examinations the following rock types

have been recognized; magnetic and non-magnetic mafic flows,

intermediate to mafic flows and minor felsic intrusions.

10.1.1 Mafic Flows

By far the most dominant rock types that were seen

during the mapping program, are the mafic flows. Visual clas

sifications, based upon colour and mode of occurrence, suggest

that these rocks are of basaltic composition. Major and trace

element geochemical analysis has for the most part confirmed this

assumption.The geochemically determined rock types were dominantly

found to be of the tholeiitic chemical trend, while being of

either basaltic or "iron-rich" basaltic composition. A few

exceptions were noted. One exposure located at L8W at 0+30N

is still of the tholeiitic chemical trend but is of andesitic

composition. This is not uncommon by virtue of the fact that

the exposure sits near a flow top environment and may only be

an isolated occurrence. The other exception, located on L16W

at 28+50N and while being of basaltic composition is found to

be of the calc-alkalic chemical trend. This analysis matches

with the magnetometer survey which shows a trend of lower suscep

tibility in the area.These basalts are found as both massive and pillowed

flows, while well developed sections of flow top breccia are

locally noted. The massive flows being green to dark green in

colour range from aphanitic to coarse grained in texture, with

the fine to very fine grained varieties being dominant. It is

only within the coarse grained sections that the mineraology can

be discerned, and then only the plagioclase feldspar from the

mafic (pyroxene-amphibole) component. Well developed sections

of pillowed flows are seen to top the massive sections, with

12.

^pndividual pillows attaining dimensions of at least four feet

in length and three feet in width. Locally the pillows may contain well developed vesicules which can be used for tops

determination. The selvages are seen to contain both vario

litic growths and hyaloclastite (glass shards). The flow top breccia are characterized by angular to sub-rounded flow brec ciated fragments in a chloritic matrix, which may contain both

variolites and hyaloclastite.All varieties of basalts, whether massive, pillowed

or flow breccias were found in both magnetic and non-magnetic phases. The magnetic and some non-magnetic sections have been chemically defined as iron-rich tholeiites, while the non-mag netic sections are represented by iron-rich tholeiitic basalts,

tholeiitic andesites and basalts, and calc-alkalic basalts.

10.1.2 Intermediate to Mafic Tuff

Only one exposure of tuffaceous rock was round during the course of the mapping program. This outcrop, located on L16W at 17+40N is composed of a grey to grey-green rock, which weathers to a buff colour and shows definite, clastic features when examined closely. The rock is composed of approximately equal proportions of rounded to sub-rounded quartz and feldspar clasts, that are supported by a chlorite-muscovite-carbonate rich matrix. Both orthoclase (pink) and plagioclase (zoned) are found to represent the feldspar minerals in the portion of the clasts.

10.1.3 In t ermediat e to Felsic FIows

Exposures of the intermediate to mafic flows have been located in the south-central section of the property. These exposures all appear to be part of the same northeast trending unit. This horizon is coincident with a zone of low

susceptibility, as is expected from visual examination,

rocks are characterized by their pale grey to green and

locally grey green colour, dominantly aphanitic texture and

lack of magnetic response.

Geochemical analysis of these rocks has returned rhy-

olitic compositions of both the calc-alkalic and tholeiitic

chemical trends. This is in agreement with the gross visual

aspects of these rock units.

An exposure of these flows is located at 6+OOW and

7+20S, these rocks are found to contain up to 102 fine grained

disseminated pyrite, and are extremely hard. At this time it

is unknown whether these features are of primary origin or are

a result of an alteration process. Samples from this outcrop

have been collected and analyzed, the results are discussed in

the mineralization and alteration section.

10.1.4 Felsic Intrusions

Two felsic intrusive exposures were located as a

result of the geological mapping. The first of these, located

on L8W at 0+80N, is a rock of intermediate composition, that

shows a dominantly grey colour with green to dark green mafic

clots, and has an aphanitic texture. The exact nature of the

mineralogy is undiscernable due to the microscopic grain size.

The second exposure is located at 15+OOW-5+85N. This

rock is of syenitic composition. This classification is based

on colour alone, as the fine grained nature of the rock does

not allow for mineralogical determinations. The pink colour

represents the dominant orthoclase feldspar, while the black

mineral (S-5%) represents the mafic component.

10.2 Property Structure

The Cleyo claim block is underlain by a northeast-

southwest trending series of intermediate to mafic metavolcanics,

with isolated felsic intrusions. Direction or tops determination

can be made due to the well developed and exposed flow structures.

These features or structures, are found in the form of flow top

breccia and pillowed horizons, and in conjunction with the ob

served grain size gradation in the massive flows, indicate

14.

4fea south facing (tops face south) sequence of variable magnetic

to non-magnetic volcanic flows. Since these rocks dip steeply to the south it can also be said that they are not overturned.

This information can be of incalculable value when trying to

determine possible extensions to known auriferous showings, as well as located areas of potential mineral wealth.

Two cross structures have been located via the surface

mapping. These structures have a northerly trend and are seen

to truncate and cause an offset to the geological continuity.

One structure a northeast trending shear zone has been located

on L8W at 15+85S. The exact extent of this shear is unclear,

but striking at 027 0 and dipping at 080 0 E it is believed that

it extends northwards to the baseline, as is also shown by the

offset in a southwest trending VLF-EM conducting (L12E at 3+OOS

to L12W at 12+50S). The second mapped structure is found in the vicinity of the principle showing at 0+40W and 1+10S, and

has a strike of 156 0 and a dip of 82 0 to the southwest, with a relative movement of west block-south and east block-north

being noted.

11.0 MINERALIZATION AND MINERALIZED SHOWINGS

All rock types, as mapped during this program display at least minor degrees of metallic mineralization, whether it

be primary pyrite or magnetite as in the mafic volcanics, or secondary pyrite as seen in the breccia-alteration zones, with

pyrite being the dominant form. Two areas of interest were located, but received only a limited degree of exploration due

to the early snowfall. Anomalous assay results were received from grab sampling that was independently conducted at both

locations.

11.1 A-Zone

The "A-Zone" was located in the same outcropping as the previously named "Main Showing", but these two targets at

15

present appear unrelated. A diagram of the A-Zone (Figure 7)

showing sample locations and assay results has been included.

This showing is located within a dark green, brecciated, car-

bonatized and magnetic rock that shows silicified and carbon-

atized fragments with 1 0-157, f ine grained disseminated pyrite.

Due to the types and degree of alteration and mineralization,

it was believed that these rocks would contain at least anoma

lous quantities of gold. The assays of up to 0.088 oz Au/ton

that were received from grab sampling of this zone show that

this was in fact the case (see Appendix I). This showing is

coincident with an T.P anomaly. (See the geophysics section

for a further description)

11.2 B-Zone

The second target or the "B-Zone", located at 6+OOW

and 7+20S, is the site of previous trenching. As is the case

with the A-Zone, the B-Zone has not received a thorough nor

complete examination. This showing is found within the inter

mediate to mafic volcanics, and is distinguished by the apparent

silicification, silica filled fractures and S-7% pyrite mineral

ization. Grab samples collected from this showing have returned

anomalous assays of up 267 ppb Au (0.008 oz Au/ton, This showing

is found to be coincident with a southwest trending "mag" depres

sion (L4E-5S to L8W-9S), as well as a similar trending VLF-EM

conductor (see Figures 8 and 9).

The IP survey has highlighted an area that shows

slightly higher chargeability. This zone is also coincident

with the Mag and EM, but the exact form is unknown as the sur

vey boundaries prohibited a full disclosure of this anomalous

zone. It is these multiple-overlapping anomalous zones, along

with anomalous assay results that place the B-Zone as a very

promising exploration target, which will require a thorough

field examination next season.

very fine-fine g magnetic mafic f

-0018

C(

(fine grained, blac "\tnagnetic mafic flo

0053

/•brecciated, altered, •| mineralized rock ^extent unknown

—•Fault

-0015-0014

very fine-fine grained, vesicular magnetic mafic flow

magnetic

Sample No.

6436-0014-0015-0016-0017-0018-0019-0020-0021-0022-0023-0024

6436-0051-0052-0053-0054-0055-0056

Assay Results ppb Au o z Au7ton

107

141977

0.08834

5493433494902210

9600.1080.0280.0420.036

*samples 6436-0051 to -0056 collected


A-Zone

Geology, Assays and Sample Locations

Twp/Aroa C leaverMining Division Larder LakeRoforonoooDrawnScalo

.s.w.c.l n"56 T Draftod S .W.C.Date Dec.. 1 986

Province On t.Proleot 6436N.T.8. - 42A/2 S 3 ChockedShoot 7

16

The "Main Showing" as described in a previous report (Conquer, 1986) did not receive any further examinations during this phase of exploration. Although this showing would appear to be of less importance than both the A- and B-Zones, it should still be examined during any further phase of exploration.

The anomalous assay results in conjunction with the coincident geophysical anomalies present both the A- and B-Zones as high priority exploration targets, that should receive a more detailed examination during the next field season.

12.0 GEOPHYSICS (see Figures 8-10 and Maps 6436-86-5-1 to -6)

An orientation Induced Polarization survey was con ducted as part of this exploration program. This newly acquired geophysical data was used in conjunction with previously acquired "mag" and VLF-EM data was used to interpret geological and miner alogical trends.

When the A-Zone was found, it was observed that the pyrite content was not high enough to produce a VLF-EM response, but with the observed 2-^3^ pyrite concentration, would be suf ficient to give an IP response. This survey did outline an elliptical zone that extends for approximately 1,000 feet from 3+OOW to 7+OOW and is about 500 feet wide straddling the base line. Also from this survey a second weak but distinct charge able zone was located. As previously mentioned, this zone is coincident with other anomalies that highlight the B-Zone.

The structure which is inferred to be associated with the B-Zone is shown to be at least 5,000 feet long by the VLF-EM and the mag surveys. This does not appear to be one continuous structure, but may be composed of several dependent sections.

Several other parallel to sub-parallel structures can be inferred from the mag data, but apparently lack the similar EM association as is found with the B-Zone. An attempt should be made to further delineate the B-Zone geophysical structure in light of the current evidence.

— 8+00 S


INDUCED POLARIZATIONFILTERED DATA

K FREQUENCY EFFECT

Twp/Area Cleaver TownshipMining D ivision Larder LakeReferencesDrawn S. W. C.Scale I "e400'

Drafted S. W. C.Dato ec. 1986

Province OntarioProject 6436N.T.S. 4 2A/2, 3CheckedSheet 10

16a

ft Analysis of the magnetometer date reaffirms what has been seen from the mapping and that is a series of magnetic to

non-magnetic flows. At least within the confines of the Cleyo

property, a definite magnetic trend can be seen to exist. This

trend shows that the southern portion of the property is domin ated by a series of highly magnetic, presumably, "iron-rich"

tholeiitic basalts. While other highly mganetic "zones" are

defined, they decrease in both length and width becoming only

isolated occurrences. As has been shown by the geochemistry, a correlation can be drawn between the high magnetic suscep

tibility zones and the tholeiitic basalts, as well as the less susceptible or non-magnetic zones and the calc-alkalic rocks.

•C

O

— 40+00 N

- 20-t-O" N

-,.,. ..^'1 ; V— 20-t-OO S

~ 40+00 S

59,00'J

59,500

;:0,,000

59,000

59,500

60,000

zn.l - n

degression

David R. Belt Geological Services inc. iCleyo Resources Inc.

MAGNETOMETER SURVEY

Twp/Aroa Cleaver TwpMiiinq Oiv's io " : Larder LakeR o f ? r -? o c o sOrawn:S.W.C. DraftedSca'u - l": I000 1 'Offer Dec. 1 986

r.iC'i': Ontorio Ject 6436 |S'- 42 A/2, 3 f

-f. llS n f w t a

— 40-*-00 N

- 20+0^ N

— Baseline

- 2O+00 S

- 40 + OO S

David R. Bei! Geological Services inc.Cleyo Resources Inc.

VLF-EM FRASER FILTER

T w p/A r ;* o : Cleaver TwpM in: "q D i vis ie r*; Larder Lake

D ' s w f ' S.W.C- S -j 3 i fi : l " ; 1000* ' D 3 ; e : Dec. 1986

O rov : nce: Ontario " O ro;'';t : 6436

h H e t

17

.3.0 CONCLUSIONS

The geological mapping program which was completed

over the 27 claim Cleaver Township property of Cleyo Resources, was done so for two reasons. First, to gain a better under

standing of the local geology, mineralogy and stratigraphy such that a better insight could be gained into the source of and to

extend to the gold bearing zone of the "Main Showing." Second,

to locate other areas of possible economic significance. This

mapping program was in fact only one part of a previously recom

mended multiphase exploration program.It was found that the property was underlain by a

series of magnetic to non-magnetic basalts, intermediate to mafic flows and tuffs and localized felsic intrusions. These rocks have a northeast-southwest strike, dip steeply to the south and show a tops up configuration. From geochemical analysis it would appear as if the basalts, both magnetic and non-magnetic varieties are of the iron-rich tholeiitic trend, while the intermediate to mafic flows were magnesium-rich tholeiites.

The amount of structural data acquired through the mapping, precludes any meaningful interpretation beyond the mention that cross-faults or structures are known to exist. Their influence on any auriferous zones is at present unknown, and will only be understood as a result of future exploration.

In light of the completed work, two promising aurif erous zones were located. Both the A- and B-Zones were only examined in the most precursory fashion, due to the sudden arrival of winter. These zones have given definitely encour aging results, such that further work is a necessity. There fore the following recommendations are made.

18.

.4.O RECOMMENDATIONS

With the discovery of two gold bearing zones on the Cleyo Resources property, it is recommended that a two and possibly three phase exploration program be completed, such that these showings can be properly evaluated. The work that has been completed to date was only a small part of a larger scale program, that due to deteriorating weather conditions, could not be completed.

The first phase will consist of linecutting and geochemical sampling. The lines will be cut to facilitate completion of program segments from all phases of work. The sampling and subsequent analysis of the humus and "B"-horizon material across both A- and B-Zones, will serve to generate a "geochemical signature", which it is hoped can be used to show the aeria^. extent of these auriferous zones, as well as a base against which future geochemistry results can be compared. This work by its very nature must be completed before the stripping is started and the overburden is forever disturbed.

Phase two is designed to actually open up and physi cally examine both showings plus geochemically investigate other areas on the property. This phase will consist of strip ping, trenching, sampling, assaying and geological mapping. Through this work an overall geological picture can be developed, so as to further define the potential economic significance of these showings.

The other areas of interest that are outside the principle showings and that are either geologically or geophysically inferred should be examined. This examination may be best completed via geochemical sampling, especially in areas of poor exposure and shallow overburden (less than 20 feet).

The budget for the geochemical sampling has been calculated for coverage of the entire property. This may in fact not be practical due to overburden thicknesses, but it should be included in the planned program.

19,

Diamond drilling is proposed for the third phase of this program, and will be contingent upon the results of the two previous phases. At the present time a 5,000 foot drill program is envisioned for the two known showings. The planned footage is based upon an equal split of 2,500 feet per showing, Program modifications may be made upon in field results.

The above recommended three phase program is esti mated to cost S263,000.00

15.0 COST ESTIMATES

Phase I

Linecutting

-estimated @ 5 miles for grid extension and detailed lines-5 miles @ $325./mile 1,625.00

Orientation Geochemistry Survey on the Detailed Grid,-^-^^^-^—^

-50 foot sample intervals-360 samples of both humus and B-horizon therefore 720 samples

-720 samples @ 76 samples/day = 9 .6 days-9.6 days @ $200./day

Soil Analysis

-720 samples @ $ll./sample

Supervision

-3 days @ 3300./day

1,920.00

7,920.00

900.00

Meals and Accommodation

-13 man days @ $40./man/day

contingencies Phase I total

520.0012,885.001,288.50

S14,173.5O

20.

II

Stripping and Trenching

-20 days @ $l,000./day 20,000.00

Assaying

-200 samples @ 511. /sample 2,200.00

Geological Mapping

-geologist and assistant

-20 days @ 5500. /day 10,000.00

Property Geochemistry

-100 foot sample interval

-1,689 samples @ 75 samples/day-23 days @ 5200. /day A, 600. 00

Soil Analysis

-2,409 samples @ 511. /sample 26,499.00

Supervision

-10 days @ 5300. /day 3,000.00

Meals and Accommodation

-53 man days @ 540. /man/day 2,120.00

Supplies 2,000.00

Secretarial

-5 days @ 5160. /day 800.00

Report and Drafting

-10 days @ 5500. /day 5.000.0076,219.00

102 contingencies 7,621.90 Phase II total 583,840.90

21

III

Diamond Drilling

-5,000 feet @ 330. /foot all incl . 150,000.0010^ contingencies 15,000.00Phase III total S165,000.00

Total

Phase I 14,173.50 Phase II 83,840.90 Phase III 165,000.00

263,014.40 say $263,000.00

Respectfully submitted by,

December 19, 1986 Stephen Conquer, B.Se. Timmins, Ontario

CERTIFICATE OF QUALIFICATIONS

I, Stephen W. Conquer, hereby certify:

1. that I am a geologist employed by David R. Bell

Geological Services Inc., 261 Third Avenue, Timmins, Ontario

2. that I am a graduate of the University of Waterloo, holding a Bachelor of Science

degree (1979)

3. that I have been practising my profession as

a geologist since 1979

4. that I do not have nor do I expect to receive

either directly or indirectly, any interest in this property or the securities of Cleyo

Resources Inc.

rTimmins, Ontario Stephen W. Conquer, B.Se. December 19, 1986

REFERENCES

Conquer, S.W. 1986 Introductory Report on the Cleaver Township,

Larder Lake Mining Division, Property of Cleyo Resources Inc., Project #6436 - internal Company Report)

Cooke, H.C. 1919 Geology of Matachewan, District Northern

Ontario, Geological Survey, Department of Mines, Ottawa

Guy, Kenneth 1984 Report on a Ground Magnetic and Electro

magnetic Program for Melrose Resources Ltd.

Hopkins, Percy E, 1924 Notes on Gold in McNeil and other Townships,

Ontario Department of Mines, Volume 33, pt.3 pp 37-40

Lee, Hulbert A. 1979 Northern Ontario Engineering Geology Terrain

Study, Sand and Gravel Resources Map, Kirkland Lake, Ontario Geological Survey, Map 5032, scale 1:100,000

Pyke, D.R. 1978 Geology of the Peterlong Lake Area, Districts

of Timiskaming and Sudbury, Ontario Geological Survey Report 171, 53p, Map 2345, scale 1:50,000

REFERENCES cont'd

1968 NTS 42-A "Timmins" Surveys and MappingBranch, Department of Energy Mines and Resources, scale 1:250,000

1970 Map 8442 G "Radisson Lake" AeromagneticSeries, Department of Energy Mines and Resources, Geological Survey of Canada

l scale 1'^ mile

•i,

l 1970 Map 84476 "Peterlong Lake" Aeromagnetic

Series, Department of Energy Mines and

• Resources, Geological Survey of Canada scale l"=% mile

l 1975 NTS 42a73 "Peterlong Lake" TopographicSeries: Surveys and Mapping Branch

l Department of Energy Mines and Resourcesscale 1:50,000

1975 NTS 42a72 "Radisson Lake" Topographic

• Series: Surveys and Mapping Branch Department of Energy Mines and Resources

. scale 1:50,000

l

l

l

l

l

l

APPENDIX I SAMPLE LOCATIONS AND ASSAY RESULTS

DAVID R. BELL GEOLOGICAL .SERVICES INC.

SAMPLE LOCATION SHEET

1H1KD A VI . I-UIlt C

l If flNS. OUT AMD

K H 9JS

Cleyo Resources—Ijir,.mM PROJECT Wo. 6436

llt'P..MTS: 42A/2 and 3

^Mpte /Jo.

136-0001

-0002-0003

1 -0004-0005

| -0006

* -0007

1 -0008

-0009

- -0010

| -0011

-0012

| -0013-0014

| -0015

-0016

| -0017

-0018

1 -0019-0020

. -0021

1 -0022

- -0023

1 -0024

-0025

| -0026-0027

l -0028

" -D029

1 -0030'

ncjid Wtwib(yi

CRC-SWC-001

-003-004

-006-008

-010

-Oil-013

-016 '-019

-022

-024

-026-029

-030

-031

-032

-033

-034-035

-036

-037

-038

-039

-040

-041

-043a-044

-045

-046

Location

L4E/9+30N

LAW/O+^N

L4W/7+60N

L12W/5+36N

8+20W/1+37N

9+20W/6+20N

11+50W/1+80S

11+50W/1+20S

L8W/5+44S

8+80W/8+90S

7+20W/16+80S

L8W/15+85S

L8W/15+85S

0+45E/1+75S

0+35E/1+70S

0+32E/0+88S

0+36E/0+85S

0+34E/0+73S

0+24E/0+51S

0+24E/0+51S

0+44E/0+20S

0+54E/0+02S

0+54E/0+02S

0+56E/0+11S

51+20W/23+60N

•jO+SOU/^^-l-ftnN

55+20W/10+40S

464-40W/40+40S

44W737-fOOS

43W/34+60S

Au ppb

43

2011

466

35256

4

3

a414110

71419

0.0??pz AU/ ton

34

549343•349

4900

4

aa

wriiM,^.Rocfe

. AM&U&LLBT

AT

FT

FT

FT

FT

FT

FT

RC

FT

FT•DC

•FT

BTFTBT

FT

FTFT

——^vnma^^^^ —— —— — *—— *—— MM

^ ______ r. ,j *, -i ' - J" - r—— - ' ___ - 1 m

DAVID R. BELL GEOLOGICAL SERVICES INC.

l l l

THIRD AVI . tunt eI'O* 1750

SAMPLE LOCATION SHEET

CMPAW: Clevo Resources Inc.

K H 7J5

PROJECT Wo. 6436

lC'P. (AREAJ: Cleaver Township : A 2A/2 and 3

JJPU to.6436-00311 -0032

-0033

| -0034-0035

1 -0036-0037

1 -0038-0039

1 -0040

-0041-0042

1J ————

1 ————-1

|

1:

1 ———.

TMU lUe*CRC-SWC-049

-051

-054-057-058-059-060-061-062-063

-064-065

L)

—— ——— ——— —— ——— L.

LocationL16W/20+70N15+10W/5+10N

BL/14+50W

LO/7+OOS

LO/17+10S4+30W/10+OOS

4+30W/10+OOS

6+OOW/7+20S

6+OOW/7+20S

6+OOW/7+20S

6+50W/7+40SL4W/4+90S

1 .

Au ppb

41^1

^ 146

4!25

193221

12267

2728

•MBMMII^^^^^M

wrtv-v-t-

Rocfe

BCBT

FT

RC

FT

RT

AC

^^^•^^^M^^M

/, tomb

ir

APPENDIX 2 ASSAY CERTIFICATES

I /Pfftrr^Xv'***'-""''*

/y J————————— J

— vj*;-,vsi: '.'; -*L; .-

1 \svik\3^^^V5WW****'' 1'

1,-jo. 189

| SAMPLEfS

M S AMPLE (S

1

1

1

1

1

1

1

1

1

1

1

1

, H ~ : :osr*"JCE™' *-, c. f TO" ;T - : '. -T" ' C L ~ * * .. i . -. ' f " r '- i - ~

• •C* LOt S l;- * 4

•^ r^\ \ A iy D ELL -WniTE ANALYTICAL LABORATORIES LTD.y P .O. BOX 187. HAILEYBURY. ONTARIO TEL: 672-3107

(Errtifiratp nf AnalgBtB2 DATE: November 13, 1986

' OF: Rock (li) RECEIVED: November 1986i FROM: M r - Stephen Conquer, David R. Bell Geological Services Inc.

PROJECT; #6436

Sample No. Gold ppb Oz. Gold

6436-0008 2566436-0014 106436-0015 7 6436-0016 146436-0017 196436-0018 776436-0019 0.088** 6436-0021 549**6436-0022 343**'6436-0023 349** 6436-0024 490**

** Checked

-

*

-,TH tos9 ...T*Bt,*Mto NOPTM . BELL-WHITE ANALYTICAL LABORATORIES LTD.NLtfS T S f CC 'IC*LLV fT4TCD *}

O t.LVfB V*ii.TS. Rr.rOSTfD ON ;r f ^^f •-OT PTfN 1O. L'fTIO TO COv'fN- y^^' " ^^^•*? O *".!1 'M-ttLM IN THt TIRE ^— ~^-~T^ m* P KOClaS.

•*^^-' —— ^"^^ ^CH^.,^^' ,, ——— ,....... , , ,.. ,.

BELL-WHITE ANALYTICAL LABORATORIES LTD.P.O. BOX 187, HAILEYBURY, ONTARIO TEL: 672-31O7

(Brrttfirate of AnalgBtaNO. 2133 DATE: December 10, 1986

SAMPLE(S) OF: Core (5) RECEIVED: December 1986

SAMPLE(S) FROM: Mr. Stephen Conquer, David R. Bell Geological Services

_________________________________________PROJECT: #6436_____________

l

i i i i i i i i i

Sample No.

6436-003789

6436-0040l

I ACCORDANCE WITH LONG.ESTABLISHED NORTH A'CAS CJSTOM, UNLESS IT IS SPECIFICALLY STATED

tr-EBWISE COLD AND SILVER VALUES REPORTED ON t ME*L SHEETS HAVE NOT SI-EN ADJUSTED TO COMPEM.

IE FOR LOSSES AND GA'NS INHERENT IN THE FIXE ASSAY PROCESS.I

Gold ppb

19322112

26727

BELL-WHITE ANALYTICAL LABORATORIES LTD.

rr

If "1V ''. r 1 ""Il l l l l l l

APPENDIX 3

l WHOLE ROCK GEOCHEMICAL RESULTS

l

l

l

l

l

l

l

l

l

l

CERTIFICATE OF ANALYSIS

TQ: DAVID R. LT.LL GEOLOGICAL SERVICES J MCATTN: STHMU. ' i c o'OUE^.?ol THIRD /.VENUE T I f, M INS, ONTARIOP'*?,' IE e

CUSTOMER NC.

DATE SUSMITTED5-NOV-86

621

REPORT 30104 REF. FILE 25683-H3

13 ROCK PROJ. 6436

WERE ANALYSED AS FOLLOWS:

AU PP3l.'RMAJ tMG P P ',P PP.",CA PPMMN P P MF- E P P y.CO P P MNI PPMCU PPM2N PPMURMIN PPMMO PPXPD PP3A G PPMCD PPMf' T PPBP B P P M

METHODFADCPWRCCPDCPDCPDCPDCPDCPDCPDCPDCPW RDCPFAOCPDCPDCPFADCPDCP

DETECTION LIMIT1.0000.01C

100.00010.000

100.0002.0002.0001.0001.0000.5000.500

10.0001.0002.0000.5001.000

10.0002.000

X-RAY ASSAY LA

DATE 19-NCV-86 CERTIFIED BY

l

l

iX-RAV ASSAV LABORATORIES LIMITED -1885 LESLIE STREET - DON MILLS, ONTARIO M3B 3J4 - (416) 445-5755' TELEX 06-986947

19-NOV-P6 REP

SAJ'.F'LE

6436-CG016436-OLD26436-00030436-C00464 36 -DC 056436-0006(.436-00076436-00096436-00 106436-00116436-00126436-00136436-0020

2 ft T 3C104

AU PP3

432011

t,66

3543

C lCIci34

REF*riLE

MG PPM

37000170002000029000350002900013000320001900

19000220006900

21000

25688-H3

P PPM

490110044057C44030047048050

500940630560

PACE 1 OF

C A PPM

890032000200002600015000200004300680037CO4100

3^000240005200

l lK-RAY ASSAY LABORATORIES LIMITED - 1885 LESLIE STREET - DON MILLS, ONTARIO M3B 3J4 - (416) 445-5755' TELEX 06-986947

l11111

VL9-NOV-&6 R

SAMPLE

64 3 6 -GC 016436-OCDt6*3^-00031)436-01,0';6436-000:;6436-00066436-ODD?6 43 6-00 OP6436-0 D 1 D 6436- DC 116436-00126436-00136436-0020

LPOr.T 30104

;v- r PH

1000l 4 0 0 14001 - 0 013001 8006EO1300160

110015007801000

REF. FILG

r E P P M

7600075000 B 20 005300090000990005400010000011000 80000960003300086000

2568C-H3

CO PPK

4451

325 55428544

40341037

PACE 2 O F

N! PPW,

7460 5156597526264

20278

22

lX-RAV ASSAY LABORATORIES LIMITED * 1 885 LESLIE STREET * DON MILLS, ONTARIO M3B 3J4 * (416) 445-5755 * TELEX 06-986947

19-NOV-66 RIP

s AMP L L

6436-OCOl6436-00026436-00036436-00046436-000564? 6-00 066436-CC076436-00096436-0010t-436-00 1 16436-00120436-00136436-0020

:;''.T 30104

CU PPI'.

100.160.90. C69. D

ISO.94.091.069.069.077.044.013.037.0

KEF.FIL

ZN PPM

120.1400.leo.110.160.150.85.0

160.17.0

120.140.59.0

140.

E 256B8-H3

MO PPM

aooo<lt\oooao

i1 1

PJ.GE 3 DF

PD PPB

^^2

<2C2<2<2^<2<2<2<2^

X-RAY ASSAY LABORATORIES LIMITED - 1885 LESLIE STREET * DON MILLS, ONTARIO M3B 3J4 - (416) 445-5755' TELEX 06-986947

l

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CERTIFICATE OF ANALYSIS

TO: DAVID R. BELL GEOLOGICAL SERVICES INC.ATTN: STEPHAN CONOUER CUSTOMER NO. 621l 261 THIRD AVEMUETIMMINS, ONTARIO DATE SUBMITTED

1E3 20-NOV-86

REPORT 30316 REF. FILE 25895-PH

13 PULPS ON HAND RE:WO#25688

UERE ANALYSED AS FOLLOWS:

METHOD DETECTION LIMITC02 Z WET 0.010S S XRF 0.010

X-RAY ASSAY LABORATORIES LIMITED-TXTz^^ DATE 08-DEC-86 CERTIFIED BY~..r..VT. .

•KM ASSAY LABORATORIES LIMITED -1885 LESLIE STREET - DON MILLS, ONTARIO M3B 3J4 * (416) 445-5755' TELEX 06-986947 i 1

08-DEC-86 REPURT 30316 REF.FILE 25895-PH PAGE l OF l

SAMPLE C02 Z S 2

6436-0001 0.73 NIL6436-0002 4.1i 0.156436-0003 2.25 NIL6436-0004 3.19 NIL6436-0005 1.72 NIL6436-0006 2.77 NIL6436-0007 0*27 NIL6436-0009 0.33 NIL6436-0010 0.43 NIL6436-0011 0.08 NIL6436-0012 4.46 NIL6436-0013 2.77 NIL6436-0020 0.60 NIL

t-TTAY ASSAY LABORATORIES LIMITED * 1885 LESLIE STREET * DON MILLS, ONTARIO M3B 3J4 * (416) 445-5755 - TELEX 06-986947

X X RRRRR A LLXX XX RR RR A AA LL

XX XX RR RR AA AA LLXXX RR RR AA AA LLXXX RRRRR AAAAAAA LL

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XRF - WHOLE ROCK ANALYSIS

DAVID R BELL GEOLOGICAL SERVICES INC.AUn: STEPHAN CONQUER CUSTOMER No. 621261 THIRD AVENUETIWINSi ONTARIO IiATE SUBMITTEDP4N 1E8 5-NOV-86

REPORT 3O1O4 REF. FILE 25688 19-NOV-86

XRF W. R. A. SUMS INCLUDE ALL ELEMENTS DETERMINED. FOR SUMMATION ELEMENTS ARE CALCULATED AS OXIDES.

X-RAY ASSAY LABORATORIES 19-HDV-86

SflKPLE

M36-OM1

H3&-0032

6136-0033

6436-0004

4436-0005

M34-000&

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49.

49.

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12.7

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123

12.4

13.6

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7.13

5. 50

5.84

4.50

4.20

4.50

5.49

3.88

0.72

5.64

6.26

3.97

1.04

KGD

7.05

3.30

4.24

4.90

5.82

4.94

4.37

5.01

0.48

4.30

3.73

1.38

3.52

REPORT 30104 REFERENCE FILE 25688

NA20

1.21

0.64

3.64

2.70

2.98

2.52

4.71

1.67

5.17

146

2.57

3.16

4.35

K20

0.09

3.12

0.42

0.38

0.09

0.13

0.17

0.71

1.47

0.15

0.32

2.39

0.25

FE203

14.2

10.9

14.4

12.4

15.6

16.6

15.1

18.3

1.60

17.5

15.5

4.43

15.6

two

0.18

0. 20

0.23

0.21

0.21

0.28

0.19

0.27

0.03

0.23

0.21

0.11

0.15

T102

1.22

1.69

1.49

1.26

1.47

1.24

1.57

1.87

0.12

1.82

1.63

0.68

1.62

P205

0.11

0.25

0.13

0.13

0.11

0.08

0.12

0.14

0.02

0.14

0.22

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0.13

PAGE l

CR203 LOI SUM

0.02 4.62 99.4

tt. 01 6.7? 99.3

O.Oi 4.70 98.7

0.01 6.31 99. l

0.01 5.08 99. l

0.01 5.93 99.4

a. 01 1.85 98.8

m 01 3.85 99.2

0.01 1.39 99.7

'CO. 01 2.54 99.5

0.01 7.23 99.3

CO. 01 4.47 100.1

tt. 01 3.16 99.2

X-RAY ASSAY LABORATORIES

SMPLE

6436-0001

6436-0002

6436-0003

6436-0004

6436-0005

6436-0006

6436-0007

6436-0009

6436-0010

6436-0011

6436-0012

6436-0013

6436-0020

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90

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120

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220

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160

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120

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50

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80

120

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110

110

140

90

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160

90

REPORT 30104 REFERENCE FILE 25683

KB

20

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X-RAY ASSAY Lfcl'OOttESJEIS3: CATiD;; LOT KITH C:,,-.J;:Y iiinuncfiTiou GRAPH ifaVIH R. L-ELL CTOLOOIC^ i^VICES INC ( Pf;OJ: W36 )

19-DEC-84

SA!?LE S\r,::j'. CODE AL203 t,30 FE203*MHT102

6436-0001^136-0002W 36-000364&-00046436-00056136-00066436-00076436-0009M36-OOIO6436-00116436-00126436-0013M36-0020

1 BT -52. 042 fiT M. 833 FT 44. 76', FT 46. 695 FT 43. 206 FT 43. 977 FI 44. 558 FT 39. 55S' RC 87. 69

10 FT 40. 87li Fi 46.2512 DC 73. 4913 FT 43. 96

CODE REFERENCE - JENSEN

UK - ULWili'nC KOMATIITE UK -FT - IRON F:ICH BftSALT NT -AT - THO.EIITIC A;-;DESITE DT -RT - THOLEIITIC RHYOLITE BT -AC - CflLC-f'ilMLIKE AMESITE K -RC - CALC-ALKOE RHYOLITE DC -H - NOT DEFINED

27. 36 30. 6115. 26 29. 91IS. S-0 36. 3421. 92 31. 3322. 71 34. 0919. 62 36. 411&. 79 36. kb19. 73 40. 714. 33 7. 98

17. 92 41. 2016. 04 37. 719. 10 17, 42

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CATION PLOT

BASALTIC KOfttTIITEHIGH MAGNESIUfl BASALTTHOLEIITIC DACITETHOLEIITIC BASALTCALC-ALKALINE BASALTCfiLC-ftLKftLlNE DACITE

L S. JENSEN (1976): A O CATION PLOT FOR CLASSIFYING SUBALKALIC VOLCANIC ROCKS. ONTARIO DIV1S10M OF MINES, MISC. PAPER 66.

E. C. GRUMSKY (1981): HO. 16 AN ALGORITHM FOR THE CLASS IFICATION OF SUBALKALIC VOLCANIC ROCKS USING THE JENSEN CATION PLOT. SUMrtftRY OF FIELD KDRiC ONTARIO DIV. OF MINES, MISC. PAPER 100.

X-RAY ASSAY LABORATORIES 19-DEC-86 JENSEN CATION PLOT GRAPH l

DAVID R. BELL GEOLOGICAL SERVICES INC ( PROJ: 6436 )

FE203+TI02+MNO

10

20

30

40

50

60

70

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CODE SYMBOL CODE SYMBOL

1 -Q

2

3 A

4

5 x

6 4

7 *

8 x

9

10 y

H

12

13 i

14

15

16

17

18

19

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CERTIFICATE OF AMALYSIS

m

TO: DAVID R. BELL GEOLOGICAL ATIK: l).*. BELL 261 THIRD AVENUE TIXtMINS* ONTARIO P'*N 1E8

SERVICES INC.CUSTOMER MD.

DATE SUBMITTED 3-DEC-86

621

REPORT 30513 REF. FILE 26052-G1

PROJ. 6436

WERE ANALYSED AS FOLLOWS

AU PPB GOZ XWRKAJ K KG PPM P PPM S ZGA PPM KN PPM FE PPM CO PPM NI PPM CU PPM ZN PPM WRMIN PPM MO PPM PD PPB AG PPM CD PPM PT PPB PB PPM

DATE 19-DEC-86

METHOD FADCP WETW RDCP DCP XRFD:PDGPDCPDGPDCP DCPD:PH RDCPFADCPDCPDCPFADCPDCP

DETECTION LIMIT1.0000.0100.010

100.00010.0000.010

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10.0002.000

X-RAY ASSAY

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X-KAY ASSAY LABORATORIES LIMITED - 1885 LESLIE STREET - DON MILLS, ONTARIO M3B 3J4 - (416) 445-5755 - TELEX 06-986947

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19-DI-C-86 REPORT 30513 R E F . F I L E 26052-01

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6436-0025- CI 2.00 29000o436-CC?i. 4 0.56 23000 6/, 36-CU27 CI 0.18 38000 6436-002:. CI 2.05 160000*36-002? CI 4.41 240006436-0030 CI 0.69 15000 6436-0031 CI 1.31 350006436-0032 CI 4.65 400006426-0033 CI ?.29 29000 6436- 002*- 46 0.23 10006436-0035 CI 3.45 210006436-0036 25 0.38 1000 o436-00-'.2 2 ti 6.41 15000

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XRF - WHOLE ROCK ANALYSIS

MVID R BELL GEOLOGICAL SERVICES INC.ftltn: D. R FELL241 THIRD AVEKJETIKiilNS,?W 1 E8

CUSTOhER No. 621

DATE SUBMITTED 3-DEC-84

REPORT 3O513 REF. FILE 26O52 19-DEC-86

XRF W. R. A. SUMS INCLUDE ALL ELEMENTS DETERMINED.FOR SUMMATION ELEMENTS ARE CALCULATED AS OXIDES.

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X-RAY ASSAY LABORATORIES 19~DEC-86 JENSEN CATION PLOT GRAPH l

DAVID R. BELL GEOLOGICAL SERVICES INC ( PROJ: 6436 )

FE203+TI02+MNO

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20

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CODE SYMBOL CODE SYMBOL

In 14

2 c

3 A

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15

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N = l

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N * l

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COMPANY : ...CJE.O

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ELECTRODE CONFIGURATION —X-*-————N X———*-*-X—*

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PHOENIX IPV-I IPT-1

REMY BELANGER ENRG.

APPROVED

~DATE^ December 19, 1986

INDUCED POLARIZATION AND RESISTIVITY SURVEY

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FREQUENCY EFFECT (APR) IN 0X0

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COMPANY

PROPERTY :

!NE NO.-

6^36-86-5-5

ELECTRODE CONnGURAT ION ——X-*-*————N X———*"^-X—*-

______i . t.

PLOTT'NG POINT •y x*

SURFACE PROJECTION OP ANOMALOUS ZONES

PROBABLE M M l l l l l

D OSSI8LE / X S / /

INSTRUMEN""

CONTRACTOR

DATE SURVEYEDay-

FREQUENCIES. . 25

NOTE CONTOURS AT LOGARITHMIC INTERVALS l ,i.5,2 .3,5.,75 , '00

PHOENIX IPV-Ij p T- l

REVY BELANGER ENRG. APPROVED

OPERATOR Ke-'Hy DATE: December 19, 1986


-v- o o o

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COMPANy:

^ VE NC - 3. +00

r L E C"*" RODE COS' tr 'GURA"l"ON'

• V x=

SURFACE PROJECTION 0^ ANOMALOUS ZONES

FREQUENCIES-

DROBABLE l l l l l l l l l N'O^E CONTOURS AT LOGAR'TMM'C 'NTERVALS

i , '5,2 ,3 ,5 , 7 5 . '00

ENRG.

DATE SURVE V E: A-PROVED

3.*-178(0

OPERATOR fi z f* f DATE December 19, 1986


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FREQUENCY EFFECT (APR) IN 07o

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COMPANY :

PROPERTY : TO//?

LINE NO.- o

o A/ y/^yf /o

Map 6436-86-5-3

ELECTRODE CONFIGURATION -—x-*-————N X———*~--X—*-

PLOTTING POINT

SURFACE PROJECTION O 17 ANOMALOUS ZONES

PROBABLE M l l l l i M

D OSSIBLE / / / / /

FREQUENCIES^ . V-O /y~

NOTE CONTOURS AT LOGARITHMIC INTERVALS 1,15, 2 .3,5,75 , !0.0

INSTRUMENT : PHOENIX IPV-IIPT-!

CONTRACTOR REMY BELANGER ENRG.

DATE SURVEYED APPROVED

_ ^ y o*.i o.a.'g^ ago- SLJL- /v86 ^x7.

OPERATOR ""' OATE: December 19, 1986

INDUCED POLARIZATION

AND RESISTIVITY SURVEY

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FREQUENCY EFFECT (APP) IN 0Xo

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METAL FACTOR ( APP)

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N '5

COMPANY : C LjE.ro

PROPERTY '

LINE NO-

6^36-86-5-1

ELECTRODE CON^'GURATION —X~*-*————N X———*-^X—^

PLOTT'NG POINT

SURFACE DROJECT:ONO c ANOMALOUS ZONES

PROBABLE l l l l l M l l

D OSSIBLE / / / / /

FREQUENCIES^

CONTRAC T OR

DATE SURVEYED

3 f-

NOTE CONTOURS AT LOGARITHMIC INTERVALS ! , :5,2 .3,5,75 . 'O C

! PV-ItPT-l

REVY BELANGER ENRG.

APPROVED

OPERATOR DATE: December 19, 1986


42A82NW8108 8 .9683 CLEAVER 900

March 20, 1987 Your File: 521/86 Our File: 2.9683

Mining RecorderMinistry of Northern Development and Mines4 Government Road EastKirkland Lake, OntarioP2N 1A2Dear Sir:RE: Notice of Intent dated February 9, 1987

Geological Survey on Mining Claims L 724470, et al, 1n Cleaver Township

The assessment work credits, as listed with the above-mntloned 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,

J.C. Smith, A/ManagerMining Lands SectionMineral Development and Lands BranchMines and Minerals Division

Whitney Block, Room 6610 Queen's Park Toronto, Ontario H7A 1H3

Telephone: (416) 965-4888

DK/raccc: Cleo Clement (In Trust)

1165 McLean DriveTimmins, Ontario

Mr. G.H. FergusonMining i Lands CommissionerToronto, Ontario

Stephen Conquer 261 Third Avenue Timmins, Ontario P4N 1E2Resident Geologist Kirkland Lake, Ontario

Encl.

Ministry ofNorthern Developmentand Mines

Ontario

Technical Assessment Work Credits

t

AMENDED

Dm

February 9, 1987

Flit

2.9683Mining Recorder'* Report ofWorkU- 521/86 ,

Recorded Holder

CLEO CLEMENT (IN TRUST)Townthlp or Area

CLEAVER TOWNSHIPType of survey and number of

Assessment days credit per claimGeophysical

Elartrnmagnetir Hays

Magnetometer riays

Rariinmetrir riays

Induce^ polarization riays

Other. riays

Section 77 (19) See "Mining Claims Assessed" column

40Genlogical riays

Rftorheminal days

Man days | | Airborne l l

Special provision [X] Ground (5T)

j l Credits have been reduced because of partial coverage of claims.

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

Mining Claims Assessed

L 724470 724474 725147 to 56 inclusive 725158 725161-62 749741 to 46 inclusive 750507-08 916185-86

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

20 DAYS GEOLOGICAL

L 916183 - 84

Mo credits have been allowed for the following mining claims

Q not sufficiently covered by the survey Q insufficient technical data filed

The Mining Recorder may reduce the abeve 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; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.

628 (85/12)

Natural Resources (Geophysical, Geological,

Geochemical andgca, i

Expenditures) CT"^ l (SL~, /\ Ct lJ CX. l /O^" ) l U?

' W .

The Mining Act

exceeds space on this fort Note: — Only days credits calq

"Expenditures" section in the "Expend. Days Cr." co*rafhns.

— Do not use shaded areas below.Type of S ^^

Claim Holdensj

Cleo Clement (In Trust)Address

1165 McLean Drive, Timmins, OntarioSurvey Company Date of S

David R. Bell Geological Services Inc. Day r

Township or Area

Cleaver TownshipProspector's Licence No.

M 20951 *

Survey (from Si to)

i/io. | Yr. j uay | "N2 86rTotal Miles of line Cut

25 milesName and Address of Author (of Geo-Technical report)

Stephen Conquer c/o 261 Third Ave., Timmins, OntarioCredits 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

i iW-entef'totaHs) here "X.

iff OB tt wi ' ^y ^s*-*^vv^

* *""-^--"^)

Airborne Credits ^

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geoph

'JL;. O1

Geolog

Geoch

ysical

:tromagnetic

jnetometer

Jiometric

ter

cal

mical

Electromagnetic

Magnetometer

Radiometric

Days perClaim

40

Days per Claim

Days per Claim

Expenditures (excludes power stripping)Type of Work Performed

Performed on Claim(s)

Calculation of Expenditure Days Credits

Total ExpendituresTotal

Days Credits

InstructionsTotal Days Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

Date

Dec. 9/86Certification Verifying Report of Work A.

Mining Claims Traversed (List in numerical sequence)Mining Claim

Prefix Number

724470724474725147725148725149725150725151725152725153725154725155725156725158725161725162749741749742749743749744749745749746750507750508

Expend. Days Cr.

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

For Office Use OnlyTotal Days Cr. Recorded

Date rded, o, o ,-rir1 tt 1986 Mining Recorder

i.rl 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 Postal Address of Person Certifying

Stephen Conquer, 261 Third Ave.. Timmins OntarioDate CertifiedDec. 9/86

1362 (81/91

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.

l*o

Type of

Township or Area. Claim Holder(s)—

GeologicalCleaver TownshipCleo Clement (In Trust)

Survey Company David R. Bell Geological ServicesInc Author of Report Stephen Conquer________________*

Address of Author c/o P.O. Box 1250. 261 Third Ave.Covering Dates of Survey Sept 12/86-Dec 19/86

(linecutting to office) Total Miles of Line Cut 25 miles____________

SPECIAL PROVISIONSCREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

DAYS~ i-i per claim Geophysical

—Mapnefnmptpr

— R adiometric ...,,,,..,--Other

t f\

r^nrr^miral

AIRBORNE CREDITS (Special provision credits do not apply to airborne survey i)

Magnetometer. .Electromagnetic(enter days per claim)

DATR- Dec. 19/86 SIGNATURE

Res. Geol. _ Qualifications.Previous Surveys

File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

L72447.0.....(prefix)

.U.2M7A.,,L.725.14.7,

L725.H8,

L725.14.9, L72.51.5.Q,

L725m,

L725.15.2,

liZmSA, L72.5.1.5.5,

L7Z5.15.6. L.725.158..

L.7,25.161.

L.7,2.5.1.6.2..

(number)

M tt

3U7.4.9.2.4.3.......,....,..,..,

L7.4.9.7.4.4....................L7.4.9.7.4.5........................L7..4.9.7.4.6.....................L750507

TOTAL CLAIMS 27

837 (5/79)

GEOPHYSICAL TECHNICAL DATA

GRQUNJj^SUKVKYS - If more than one survey, specify data for each type of survey

Number of Stations

Station interval

Profile scale

val I,ine sparing

*rval

Instrument —.

Accuracy — Scale constant.

Diurnal correction method.

Base Station check-in interval (hours)

Base Station location and value

lZQ

SwW

Instrument —Coil configuration

Coil separation _

Accuracy —————

Method:

Frequency,—-——

Q Fixed transmitter D Shoot back CD In line d Parallel line

Parameters measured —

-s)

(specify V.L.F. station)

lO

Instrument -——

Scale constant ——

Corrections made.

Base station value and location

its

Elevation accuracy.

Instrument

ZO

N

QttCc z

w

Method D Time Domain

Parameters — On time .—.—.

- Off time ——.

— Delay time ——-

— Integration time.

Power.

Electrode array — Electrode spacing .

Type of electrode

Frequency Domain

Frequency _____

Range ——^-————

cRemaining Claims

L750508 L916183 L916184 L916185 L916186

ly

SELF POTENTIAL

i Instrument_________________——————————————————————— Range. Survey Method ______________————————————————————————————

Corrections made.

RADIOMETRIC

Instrument -——-Values measured .

l*i Energy windows (levels) —

Height of instrument ____________________________ Background Count .

Size of detector _____________________________________________•lOverburden

(type, depth - include outcrop map)

OTHERS (SEISMIC, DRILL WE] ,L I .OGGING ETC.)

Type of survey ,—.——---^——-^-^—-————-—-———

Instrument --——-———--.-———^—~———-^————

If Accuracy-————— i Parameters measured.

Additional information (for understanding results).

AIRBORNE SURVEYS

"* Type of survey(s)

Instrument(s) ——(specify for each type of survey)

Accuracy^———————————————(specify for each type of survey)

Aircraft used-——————————^^——————-—^^^-^—^—^^—

Sensor altitude.Navigation and flight path recovery method.

T? ________________________________________

Aircraft altitude________________________________Line Sparing

Miles flown over total area_______:__________________Over claims only..

or.(^Hjrir..ivijijrtij aur

Numbers of claims from which samples taken

TotaJ Niimher of Samples

Type of Sample(Nature of Material)

Average Sample Weight

Method of Collection.

Soil Horizon Sampled.Horizon DevelopmentSample Depth.,Terrain

Drainage DevelopmentF-StimHtpd Range of Overburden Thickness

SAMPLE PREPARATION(Includes drying, screening, crushing, ashing)

Mesh sire of frartion iiserl for analysis.

General . —

i VE, I - riUJL.r,lJUK.tt KE.C.UK1J H

—— ANALYTICAL METHODSValues expressed in: per cent D

p. p. m. CDp. p. b. D

Cu, Pb, Zn, Ni, Co, Ag, Mo, As.-(circle)

Olhprs

Field Analysis (. tests)

Extraction Method

Analytiral Method

Reagents I Iserl

Field Laboratory AnalysisNo. (. . tests)F.vtrartion Methorl

Analytical MethodReagents Used

nommerrial Laboratory ( tests)

Name of Laboratory

F.Ytrarlion MethoH,

Analytiral MethoH

Reagents IJs*"d .

General . ————————————————————————————

li

1

1

1

1

1

1

1

1

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1

1

1

1

1

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j

1

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X1,

Xx"XX1XA

xlxx x"7xX1

xxx1xxll~

S:

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FALLON TWR

o:

UJ

UJ O

K VL8B3I9B | L 833I97 l^'^LT 'L l

849537,649340

-- -J i 1867133 r/867136 l ~B67I37 l "867136

849543^ — - .4- -- J

IB49S38f. .v. i . l1867131 !A86713Z ' L867133 l L*67I34

l

— JL— — -L ~ -

"18672101867^29,867228 .867122

867116:8313796 .183795 168/3794 1867123

.L - - +L- -749700 749899 1 74

-749695.749694

867Z3S 867234 A |- — -|7427BS[ 742784 6723318"496IIJ

LLp N.ghthawki - -i L l /L

, .l 858944 l |B58

j^L-- V-

—' ' 763148 j V,7^3147753206 753193

l-l- -

^ 4 . ^4 .. j. t^L ^L .T^L J f \

N\ i-/- j.-/ri. - j838964 j 842761 | 6-\ ('Z7SZ | 856*70'

60 0 36'W'

HINCKS TWR

42A92NW8I08 3.9663 CLEAVER 200

NOTES

400' surface r ights reservation along the shores of all

lakes and r ivers.

AREAS WITHDRAWN FROM

M.R.O. - MINING R IGHTS ONLY

S.B.O. - SURFACE RIGHTS ONLY

M.+ S. - MINING AND SURFACE RIGHTS

DMcription Or d w No. Dm Disposition Fit*

•4*

©or 0"

LEGEND

PATENTED LAND

PATENTED FOR SURFACE RIGHTS ONLY

LEASE

LICENSE OF OCCUPATION

CROWN LAND SALES

LOCATED LAND

CANCELLED

MINING RIGHTS ONLY

SURFACE RIGHTS ONLY

HIGHWAY * ROUTE NO.

ROADS

TRAILS

RAILWAYS

POWER LINES

MARSH OR MUSKEG

MINES , ^

'used only with summer resort locations or when space is limited

LO.

C.S.

Loc. C.

M.R.O. S.R.O.

TOWNSHIP OF

CLEAVERDISTRICT OF

TIMISKAMING

LARDER LAKEMINING DIVISION

SCALE : 1 INCH - 40 CHAINS (1/2 MILE)

DR.

DATE JULY I 986PLAN NO. G-3619

Ministry of Ministry ofNatural Northern DevelopmentResources and Mines

Ontario

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Cro

wn

Res

erve

min

e P

atte

rson

Cop

per

min

e P

rest

on M

ines

Ltd

. P

orcu

pine

Lak

e m

ine

Rom

field

Bui

ldin

g C

orp.

Ltd

.B

uffa

lo A

nker

ite m

ile

Rus

tex

Min

ing

Cor

p.

. . .

.. . .

. ... .

. .

Suv

ercl

aim

Lak

e M

ines

Ltd

.S

hane

-Dar

ragh

min

e Si

scoe

Met

als

of O

ntar

io L

td.

Bon

sall

min

e . .

....

....

....

....

....

...

Mili

eret

t m

ine

. . . .

. . .

..Si

scoe

Met

als

of O

ntar

io L

td.—

Cas

:ie D

ivis

ion

(leas

e fro

m M

cint

yre

Por

c.jp

ine

Min

es L

td.)

Cap

itol

min

e . .

. . ..

. ....

. .

Cas

tle-T

reth

eway

rin

eW

als

h m

ine

. . .

. . .

. . .

. . .

. . .

. . .

. . .

. . .

. , .

. . .

Sis

coe

Meta

ls o

f O

ntar

io L

td.

{leas

e fr

om M

annd

gs

Min

es L

td.)

Mannm

me

....

....

....

....

..,.

....

....

....

..

Re

eve

-Do

bie

miie

. .

. . .

. ..

. ...

..

. . .

Syl

van

ite G

old

Min

es L

td.

. . .

.. . .

. . ..

. ..

.

Tec

k C

orp.

Ltd

. —

Tec

k H

ughe

s M

irin

g D

ivis

ion

kirk

land L

ake

min

e . ,

.. . .

. . ..

. . .

. ..

.. .

.T

eck-

H jg

he

s m

ines

.

T ro

t h e

wa

y-O

ssia

n m

ire

. . .

. ..

Tyr

an

ite M

ines

Ltc.

. .

. . .

. . ,

, , ,

.. .

. . . .

. . .

Upper

Canada M

ines

Ltd

.U

pp

er

Be

ave

r (A

rgo

na

ut)

^ne (

man

agem

ent

agre

em

ent

with

Lak

e B

eave

rhou

se M

ines

Ltd.

Upper

Ca

na

da

min

e U

nite

d O

ba

lski

Min

ing C

o. L

td.

West

field

Min

era

ls L

td.

Conia

uru

m m

ine

Wrig

ht-

Ha

rgre

ave

s M

ines

Ltd

. Y

oung-D

avi

dso

n M

ines

Ltd

.

The

lis

t of

pa

st-p

rod

uce

rs is

lim

ited

to m

ines

with

met

al p

rod

uct

ion

valu

ed i

n exc

ess

of

225,

000.

MIN

ER

AL

PR

OD

UC

TIO

N A

ND

RE

SO

UR

CE

S

Ir 1

97",

min

es l

oca:

ed w

ithin

the

Tim

min

s-K

irkla

nd L

ake

shee

t pr

oduc

ed g

old,

silv

er,

coba

lt, c

oppe

r, zi

nc,

lead

, ni

ckel

, iro

n, c

ad

miu

m, s

ulph

ur a

nd a

sbes

tos.

Bar

ite is

soo

n sc

hedu

led

for

prod

uc

tion

in Y

arro

w

l ow

nshi

s. T

he a

rea

also

con

tain

s de

posi

ts o

f m

oly-

b

de

njm

. ur

aniu

m,

tung

sten

, bi

smut

h,

palla

dium

, pl

atin

um,

mag

nesi

um, n

ephe

line,

mar

l, sa

nd a

nd g

rave

l. T

wo

kim

berli

te d

ikes

ar

e kn

own

to o

ccur

; on

e in

McC

ool

Tow

nshi

p, a

noth

er in

Gau

thie

r To

wns

hip.

Gol

d is

pr

oduc

ed a

t th

e P

orcu

pine

(lim

min

s),

Kirk

land

La

ke-

Lard

er L

ake

min

ing

cam

ps,

and

in H

islo

p To

wns

hip

sout

heas

t of

M

athe

son.

Fo

rmer

pro

duct

ion

incl

uded

the

Mat

ache

wan

and

Elk

Lake

cam

ps.

~\ he

lar

gest

pro

duce

r of

silv

er is

the

Kid

d C

reek

min

e no

rth o

f Ti

mm

ins.

Silv

er i

s al

so r

ecov

ered

at a

ll th

e pr

oduc

ing

gold

min

es,

in a

dditi

on t

o th

e op

erat

ing

min

es i

n th

e G

owga

nda

area

. Fo

rmer

pr

oduc

tion

incl

uded

the

Mat

ache

wan

, El

k La

ke a

nd C

obal

t (C

asey

To

wns

hip)

are

as.

Zinc

, co

pper

, le

ad,

cadm

ium

an

d su

lphu

r ar

e pr

oduc

ed

by

Ecs

tall

Min

ing

Lim

ited

{Kid

d C

reek

min

e).

Cop

per

and

zinc

are

pr

oduc

ed i

n th

e K

amis

kotia

are

a w

est o

f tim

min

s an

d at

the

Pot

ter

min

e ea

st o

f M

athe

son.

Cop

per

is al

so p

rodu

ced

at t

he M

cint

yre

Por

cupi

ne m

ine

near

Tim

min

s, t

he M

iller

Lak

e-0'

Bne

n m

ine

near

G

owga

nda

and

the

Upp

er B

eave

r m

ine

near

Lar

der

Lake

. M

inor

co

pper

has

als

o be

en p

rodu

ced

in t

he E

lk La

ke,

Mat

ache

wan

and

G

owga

nda

area

s.

Min

or l

ead-

zinc

was

for

mer

ly p

rodu

ced

m t

he

Mat

ache

wan

are

a,N

icke

l pr

oduc

tion

com

men

ced

in

1971

at

the

Te

xmon

t m

ine

loca

ted

sout

h of

Tim

min

s. N

oran

da M

ines

Lim

ited

will

sho

rtly

be

prod

ucin

g ni

ckel

fro

m L

angm

uir

Tow

nshi

p, s

outh

east

of T

imm

ins.

N

icke

l was

for

mer

ly p

rodu

ced

at th

e A

lexo

min

e, lo

cate

d no

rthea

st

of T

imm

ins.

Iron

ore

is p

rodu

ced

at t

he A

dam

s m

ine

of D

omin

ion

Foun

drie

s an

d St

eel

Lim

ited,

loc

ated

in

Bost

on T

owns

hip,

sou

th o

f K

irkla

nd

Lake

.N

early

all

the

asbe

stos

pro

duct

ion

has

com

e fro

m t

he a

rea

east

of

Mat

heso

n, a

nd m

ost

of t

his

has

been

fro

m t

he M

unro

min

e, a

pa

st p

rodu

cer

of C

anad

ian

John

s-M

anvl

lle C

ompa

ny L

imite

d. H

ed

man

Min

es L

imite

d is

prod

ucin

g as

best

os i

n W

arde

n To

wns

hip,

an

d C

anad

ian

John

s-M

anvi

lle is

cur

rent

ly p

repa

ring

a pr

oper

ty fo

r pr

oduc

tion

in

Gar

rison

To

wns

hip;

bo

th

loca

litie

s ar

e ea

st

of

Mat

heso

n.C

obal

t is

pr

oduc

ed

in t

he G

owga

nda

area

, an

d w

as f

orm

erly

m

ined

in

the

Llk

Lake

and

Cob

alt (

Cas

ey T

owns

hip)

are

as.

Tota

l va

lue

of m

iner

al p

rodu

ctio

n fro

m t

he m

ap a

rea

to th

e en

d o'

19

69

was

ap

prox

imat

ely

S3,5

51.0

00,0

00.

Qua

ntity

of

min

eral

s pr

oduc

ed i

s as

fol

low

s:

HO

W T

O

OB

TAIN

AD

DIT

ION

AL

INFO

RM

ATI

ON

Pub

lishe

d ge

olog

ical

m

aps

cove

ring

this

she

et a

re i

ndic

ated

on

Inde

x M

aps

2079

, 20

80 a

nd 2

081

of th

e O

ntar

io D

ivis

ion

of M

ines

, M

inis

try o

f N

atur

al R

esou

rces

, Tor

onto

, and

on

Inde

x sh

eets

31,

32,

41

, and

42

of th

e G

eolo

gica

l Sur

vey

of C

anad

a, D

epar

tmen

t of E

nerg

y,

Min

es a

nd R

esou

rces

, O

ttaw

a.P

ublis

hed

geol

ogic

al

repo

rts c

over

ing

this

she

et a

re l

iste

d in

B

ulle

tin N

o. 2

5 of

the

Ont

ario

Div

isio

n of

Min

es,

Min

istry

of

Nat

ural

R

esou

rces

and

in

the

Ind

ex o

f P

ublic

atio

ns,

Geo

logi

cal

Surv

ey o

f C

anad

a, 1

961,

197

0.T

opog

raph

ic m

aps

of th

e ar

ea c

an b

e ob

tain

ed f

rom

the

Div

isio

n of

Lan

ds, M

inis

try

of N

atur

al R

esou

rces

, Tor

onto

, or t

he T

opog

raph

ic

Sur

vey,

Dep

artm

ent

of E

nerg

y, M

ines

and

Res

ourc

es, O

ttaw

a.A

ir ph

otog

raph

s m

ay b

e ob

tain

ed f

rom

(he

Silv

icul

ture

Sec

tion,

D

ivis

ion

of L

ands

, M

inis

try o

f N

atur

al R

esou

rces

, Tor

onto

. Ont

ario

, or

fro

m

the

Nat

iona

l A

ir P

hoto

grap

hic

Libr

ary,

D

epar

tmen

t of

E

nerg

y, M

ines

and

Res

ourc

es,

Otta

wa.

Aer

omag

netic

map

s'co

verin

g th

is s

heet

can

be

obta

ined

from

the

Geo

logi

cal

Sur

vey

of C

anad

a.

Parti

al c

over

age

may

be

obta

ined

fro

m t

he O

ntar

io D

ivis

ion

of M

ines

.Th

e na

me

an

d o

wne

rshi

p of

man

y m

iner

al o

ccur

renc

es s

how

n on

th

is s

heet

are

giv

en o

n M

ap 2

148,

Ont

ario

Min

eral

Map

, 19

68.

Info

rmat

ion

on g

eolo

gy,

min

es a

nd m

iner

al o

ccur

renc

es m

ay b

e ob

tain

ed a

t th

e o

ffice

of

the

loca

l R

esid

ent

Geo

logi

st (

Tim

min

s.

Kirk

land

Lak

e or

Sud

bury

).M

inin

g cl

aim

map

s an

d ge

nera

l in

form

atio

n ca

n be

obt

aine

d at

th

e of

fice

of t

he M

inin

g R

ecor

der

at T

imm

ins,

Kirk

land

Lak

e, o

r .^

urlh

iirv

cir

st t

he D

ivi^

inn

nf L

ands

. To

ront

o.

ON

TAR

IO

DIV

ISIO

N O

F M

INES

HO

NO

UR

AB

LE L

EO B

ERN

IER

- M

inis

ter

of N

atur

al R

esou

rces

W. Q

. MA

CN

EE

, Dep

uty

Min

iste

r o/

Nat

ural

Res

ourc

es

G. A

. Jew

ett,

Exec

utiv

e D

irect

or, D

ivis

ion

of M

ines

E.

C. P

ye, D

irect

or, G

eo/o

gica

l Bra

nch

Adj

oins

Map

216

1 C

oral

Rap

ids

Coc

hran

e

Mal

oney

\

\ \

\ T-

ake

f \

G7 \

IGisf

V

KIN

GS

MIL

LN

l, R

EAD

ME

'it

|7 •'.'EDW

ARDS

win

Fal

ls..

. Gi

l lE

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\(

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sh

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Spr

ing

FR

EC

HE

VIb

LE

le ^

Au

BA

RN

ET

TH

AC

KE

RA

Y

tafe

—T

-Sil

J O

SNE

BO

E

MCKE

OWN

Gil

Gil

Gll

f

11 ^ P

fkR

AN

D

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SHE

BA

AR

GY

LE

94

Jiu.

Cu,

M

NO

RT

HR

UP

GIOc

way R

AT

TR

AY

12b

BA

NN

OC

KB

UR

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^

MO

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t Lak

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l. Si

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00"

W

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14

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t

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42A

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2.9

683

CLE

AV

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ME

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M

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RA

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RE

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E

21

0

Sem

i-det

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d an

d re

conn

aiss

ance

map

ping

; 1"

to

Y m

ile:

r to

1 m

ile;

1" t

o 2

mile

s

-— —

war

n ru

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AR

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OO

D T

OW

NS

HIP

AR

EA

13

12b

12b

Map

2205

TIM

MIN

S-K

IRK

LA

ND

LA

KE

Geo

logi

cal C

omp

ilat

ion

Ser

ies

CO

CH

RA

NE

, SU

DB

UR

Y A

ND

TIM

ISK

AM

ING

DIS

TR

ICT

S

Scal

e 1:

253,

440

or l

Inc

h to

4 M

iles

SE

CT

ION

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RD

ER

LA

KE

AR

EA

l

11

'1C^ wtVj , \\l

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i la

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\

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4

\ \ i

/i

\

\ /'

^le

W

le

Scale

, 1 in

ch to

4 m

iles

SE

CT

ION

—R

ED

ST

ON

E R

IVE

R A

RE

A

ID18

SO

UR

CE

S O

F I

NF

OR

MA

TIO

N

Geo

logi

cal c

ompi

latio

n by

D,

R. P

yke,

L. D

. A

yres

, an

d D

. G

. In

nes,

197

0,19

71.

Pre

viou

s co

mpi

latio

n by

Gin

n,

et a

!, M

ap 2

046,

196

4.

Geo

logy

fro

m p

ublis

hed

map

s of t

he O

ntar

io D

ivis

ion

o! M

ines

, G

eolo

gica

l S

urve

y of

Can

ada,

and

unp

ub

lishe

d m

aps

of m

inin

g c

ompa

nies

.

Car

togr

aphy

by

C.

Harr

is a

nd a

ssis

tant

s, D

ivis

ion

o/"

Lane

's,

Min

istr

y of N

atur

al R

esou

rces

, 19

72.

ease

map

s co

mpi

led

from

Nat

iona

l To

pogr

aphi

c S

erie

s,

shee

ts 3

1 M

jNW

; 32

D1N

W;

32 D

/SW

; 41

PjN

W;

41

PIN

E;4

2A

INE

;42

AIN

W;4

2A

ISW

;42

AtS

E.

2030

Ki

om

etre

s

T~

T"

1

H

H

Scale

, 1 in

ch tt

4 m

iles

SE

CT

ION

—G

OW

GA

ND

A A

RE

A

FIG

UR

E 6

Map

220

5T

imm

ins-

Kirk

land

Lak

e G

eolo

gica

l Com

pila

tion

Ser

ies

Scale

, l in

ch to

200

mile

s

N.T.

S. r

efere

nce

31M,

32D

.41P

.42A

LE

GE

ND

CE

NO

ZO

IC

PL

EIS

TO

CE

NE

AN

D

RE

CE

NT

Till,

var

ved

clay

, sa

nd, g

rave

l, pe

at.

UN

CO

NF

OR

MIT

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MES

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IC

INT

RU

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E

CO

NT

AC

T

PA

LE

OZ

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LO

WE

R A

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M

IDD

LE

SIL

UR

IAN

18

Tho

rnlo

e F

orm

atio

n: li

mes

tone

, do

l om

ite,

sand

ston

e.

Wab

i For

mat

ion:

lim

esto

ne.

Sha

le.

MID

DL

E A

ND

U

PP

ER

OR

DO

VIC

IAN

17

Daw

son

Poi

nt F

orm

atio

n; s

hale

. Fa

rr F

orm

atio

n: l

imes

tone

. B

ucke

For

mat

ion:

lim

esto

ne,

shal

e.

Giii

guen

For

mat

ion:

san

dsto

ne.

UN

CO

NF

OR

MIT

Y

PR

EC

AM

BR

IAN

LA

TE

P

RE

CA

MB

RIA

N

MA

FIC

IN

TR

US

IVE

R

OC

KS

16

Dia

base

: dik

es.

INT

RU

SIV

E

CO

NT

AC

T

MID

DL

E P

RE

CA

MB

RIA

N

AL

KA

LIC

IN

TR

US

IVE

RO

CK

S

15

Syen

ite,

neph

elin

e sy

enite

.

14

Dia

base

, gr

anop

hyre

: sh

eets

an

d di

kes.

MA

FIC

IN

TR

US

IVE

RO

CK

S

INT

RU

SIV

E

CO

NT

AC

T

HU

RO

NIA

N

SU

PE

RG

RO

UP

CO

BA

LT

GR

OU

P

Lorr

ain

For

mat

ion

13

Qua

rtzite

, ark

ose.

Gow

gand

a Fo

rmat

ion

12

Uns

ubdi

vide

d.12

a Fi

rstb

rook

Mem

ber:

argi

llite,

gre

y wa

cke,

silt

ston

e, a

rkos

e.12

b C

olem

an M

embe

r: co

nglo

mer

ate,

ar

kose

, gr

eyw

acke

, qu

artz

ite,

argi

l lit

e.U

NC

ON

FO

RM

ITY

EA

RL

Y P

RE

CA

MB

RIA

N

MA

FIC

IN

TR

US

IVE

R

OC

KS

*

11

Diab

ase:

dike

s.

INT

RU

SIV

E

CO

NT

AC

T

FE

LS

IC I

NT

RU

SIV

E R

OC

KS

C

Ida

Qua

rtz

porp

hyr

y, q

ua

rtz-

feld

spa

r po

rphy

ry,

feld

spar

por

phyr

y, g

ran

ophy

re,

fels

ited

Wb

Tro

ndhj

emite

, gr

anod

iorit

e,

quar

tz

mon

zoni

te:

sim

ple

bath

olith

s an

d st

ocks

tf10

c T

rond

hjem

ite,

gran

odio

rite.

Q

uartz

m

onzo

nite

, quart

z dio

rite

, a

plit

e,

pegm

atit

e,

mig

matite

: co

mple

x ba

thol

iths.

9 S

yenite,

monzonite,

feld

spar

porp

hyry

d

ME

TA

MO

RP

HO

SE

D

MA

FIC

A

ND

U

LT

RA

MA

FIC

RO

CK

S*

fi G

abbr

o, d

iorit

e, l

ampr

ophy

re.

7 P

eridotite

, dunite,

pyro

xe

nite

, se

rpentin

itef

6 C

ongl

omer

ate,

gre

ywac

ke, s

i/ist

one,

sl

ate,

arg

illite

^

5 G

reyw

acke

, si

ltsto

ne,

slat

e, a

rgill

ite

and

min

or p

ebbl

e co

ngio

mer

atet

INT

RU

SIV

E C

ON

TA

CT

ME

TA

SE

DIM

EN

TS

ff

ME

TA

VO

LC

AN

ICS

S

ALK

ALIC

M

ET

AV

OL

CA

NIC

S"

Tra

chyt

e,

/euc

itic

trac

hyte

; fle

ws,

ULT

RA

MA

FIC

ME

TA

VO

LCA

NIC

S

3 Se

rpen

tiniz

ed d

uniti

c an

d pe

rido-

FFLS

IC

ME

TA

VO

LCA

NIC

S

2a

Pyr

ocla

stic

roc

ks

INltR

ME

DIA

TE

A

ND

M

AF

IC

ME

TA

VO

LCA

NIC

S/

la

Inte

rmed

iate

How

s.1b

In

term

edia

te p

yroc

last

ic r

ocks

1c

Maf

ic f

/ow

s an

d py

rocl

astic

roc

ks.

If

Iron

form

atio

n an

d fe

rru

gino

us

cher

t(o

ccur

s as

a m

embe

r o; s

trat

igra

phic

units

1,2

,4,

and

5).

S

Sul

phid

e m

iner

aliz

atio

n.

aFor

mer

ly c

lass

ified

as

Nip

issi

ng i

n pa

rt.

^No

rth

-tre

nd

ing

dik

es a

re p

art of M

atac

hew

an s

war

m.

cFor

mer

ly c

lass

ified

as

Alg

oman

.

eFor

mer

ly c

lass

ified

as

Hai

leyb

uria

n.

fMay

in

part

be

com

pose

d of

ultr

am

afic

flo

ws.

in t

hese

gro

ups

are

subd

ivid

ed l

ithol

ogic

al/y

an

d th

e or

der

does

not n

eces

saril

y im

ply

age

rel

atio

n sh

ip w

ithin

or a

mon

g gr

oups

.

^For

mer

ly c

lass

ified

as

Tim

iska

min

g.

/For

mer

ly c

lass

ified

as

Kee

wat

in.

The

lette

r "G

" pr

eced

ing

a ro

ck u

nit

num

ber,

for

ex

ampl

e "G

14

", i

ndic

ates

int

erpr

etat

ion

from

geo

phys

i ca

l dat

a in

drift

cov

ered

are

as.

SY

MB

OL

S

Faul

t.

Line

amen

t.

isso'

Alti

tude

in f

eet

abov

e m

ean

sea

leve

l.

Rai

lway

with

sta

tion

or fl

agst

op.

Prov

inci

al h

ighw

ay.

Mot

or ro

ad.

= H

O

ther

road

.

Airc

raft

land

ing

faci

litie

s.

Larg

er c

omm

unity

.

Smal

ler

com

mun

ity.

Prod

ucin

g m

ine.

Past

pro

duci

ng m

ine.

Min

eral

occ

urre

nce.

Res

iden

t Geo

logi

st's

, Min

ing

Rec

orde

r's

offic

es,

Kirk

land

Lak

e, T

imm

ins.

Min

ing D

ivis

ion

with

bou

ndar

y.

Inte

r pro

vinc

ial

boun

dary

.

Dis

tric

t bo

unda

ry.

Tow

nshi

p bo

unda

ry.

A

B

Line

of

sect

ion.

SE

CT

ION

— T

IMM

INS

AR

EA

TH

E M

AP

IN

DE

X

The

red

lette

rs a

nd n

umbe

rs in

the

bord

ers

prov

ide

a lo

catio

n re

fere

nce

syst

em b

ased

on

that

of

Map

20

24, O

ntar

io M

iner

al M

ap.

(DinGO*fr-l

CMto CM-J

CO

-J00

UJ CO-J

Ul CO

TL 15 OON

— 40+OON

— 30+00N

— 20+OON

TL 25 00 S

A-ZONE assa resul ts

-0002 s;vOii' lot:. LI ion and number

20;AT Au assav (pph); Geochemical Rock

Gen l t vi cal Con t rir L"

sO '--n nviru-'Lic data

B D

Tree

S - spruce

P - pine

B - birch

F - b als am fir

A - alder

C - cedar

Pop - pop l a r

Thole i. i tic SuiteFT - iron-rich tholeiitic basalt BT - tholeiitic basalt AT - tholeiitic andesite RT - Lhol e i i. L i c T hyol i t., e

Cal c-Alka! i c Suit,.BC - cal.c-alkalir basalt AC - ea l c-a Ik a l i c a p.-k's 11 e RC - calc-alk-ilit: rhyolite Df; - cal c-alkalic dac i re

-OOH-0015-0016-0017-0018-0019-0020-0021 549 ppb-0022 343 ppb-0023 349 ppb-0024 490

10 ppb 7 ppbH ppb19 ppb77 ppb0.088 oz Au/ton3A ppb

r e;; i-i l l s

y? 1

Trench l-0038 221 pnb-0039 12 ppb-0040 267 ppb

Trench 2-00'd 27 ppb

— 10+OON

— Baseline

— 10+OOS

—20+OOS

30+OOS

David R. Bell Geological Services IncCleyo Resources Inc.

Sample Location and Assay Plan

Twp7Ar68 : Cleaver Twp.

Mining Division : L ardor Lake

•\ u u

{Drafted :4- -

,Dai*j . t)*.. , t LI ~ui

Prov : Ontario

Project No : 0 430

NTS fvlo : 4i? A/? ,o

--V- ^

Ht? . f 1 'i i-

5.9663 CLEAER

CD if)

OD

-J

O

-l

OJro S

* 00

UJ 00

UJ CD

TL 15 OON

— 40+00N

30+00N

20+OON

TL 25 00 S

MAFIC ROCKS

l l Noii-iT.a^ru: t i c

B -basal fs undif ferentIn

Bm -nia^s i ve f l ows

Bp -pill LiWL'd flows

Bpy -flow E ^p brooc i n

1U - t Vlf !'.H?.'PM:-i

[ "j M "l '.!H'I T/

H h.i :..i l t -i tind i t" l" f i.'i'iit. i .'i

Bm :!i,i':'. i vo f l ovs

j^ ill .'V.'J, l l ,^-:

INTEKMKDLATK - FELSIC ROCKS

Q Non-rr.agnet ic

A -andeaiteundifferentiatted

Am -mass i ve flows

FELSIC INTKLISFVKS

FI -uiuuibdivided

Geologi cal Contact

based on magneti c data and geology

based or. geol ogy a n ci g e o e h e m i s t r y

cla ini post, local I on and number found , assumed

e leva Lion contours hash marks show down slope

e s k e r

road

swampy ground

Trt^e Typ^ s

S - spruce

P - pine

B - birch

F - balsam fir

A - alder

C - cedar

Pop - poplar

vesicular

hyaloclastite

variolitic

magnetic

g - geophysically inferred

sh z - shear zone

vesr

hyal varmag

Scale

10+OON

— Baseline

10+OOS

20+OOS

—30+OOS

David R. Bell Geological Services IncCleyo Resources Inc.

GEOLOGY

Twp/Area : Cleaver Twp.

Mining Division : Larder Uko

References :

Drawn : '1./JJ -

Scale : i" fl'io'Drafted : y A '

Date : nr^, , t Hfin

PrOV : Ontario

Project Wo : 0430

NTS No : 4y A/? ,n

Checked : /,, '

Sheet No : n*i'^ "fi. . .^ , ^.* t

42A*2NWataB 2 .96B3 CLEAVER 230

summary rpt on expl program - search … · and report that the recommended exploration program was...

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