52J82SE8785 2.2868 SQUAW LAKE ( RECEIVED€¦ · 52J82SE8785 2.2868 SQUAW LAKE (7)1(7) RECEIVED...

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52J82SE8785 2.2868 SQUAW LAKE (7)1(7) RECEIVED GEOLOGY - MORGAN ISLAND INTRODUCTION; Durinq the early fall of 1974 the author and his partner, J. R. Nixon, spent a week on Sturqeon Lake endeavouring to trace the location where, during the late 1930's, a pair of prospectors discovered a larqe number of quartz boulders well mineralized with gold. The boulders were crushed by the prospectors and the gold recovered bv panning. The location was either at the south end of the lake near Granite Bay or at King Bay, twelve miles to the north. Granite Bay and surrounding area was explored during the early fall with negative results and plans made to explore King Bay durinq the fall of 1975. In early January, 1975, preliminary map No. P. 968 by N. F. Trowell was published which covered part of King Bay. Dr. Trowell pointed out an area of carbonate breccia on Morgan Island which ran anomalously high in gold and, as Morqan Island lay four miles up the glacial strike from King Bay, it was decided to stake the carbonate breccia formation on Morgan Island. On.the 27th of April, 1975, Robert Andrews and the author engaged a Pegus Helicopter from Dryden and staked claims No.'s 431450 to 431454 inclusive. On September 8, 1975 two employees of Bayhill Develop ment Ltd., Kingston, a company in which the author is a shareholder.

Transcript of 52J82SE8785 2.2868 SQUAW LAKE ( RECEIVED€¦ · 52J82SE8785 2.2868 SQUAW LAKE (7)1(7) RECEIVED...

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52J82SE8785 2.2868 SQUAW LAKE (7)1(7)

RECEIVED

GEOLOGY - MORGAN ISLAND

INTRODUCTION;

Durinq the early fall of 1974 the author and his partner,

J. R. Nixon, spent a week on Sturqeon Lake endeavouring to trace

the location where, during the late 1930's, a pair of prospectors

discovered a larqe number of quartz boulders well mineralized

with gold. The boulders were crushed by the prospectors and the

gold recovered bv panning. The location was either at the south

end of the lake near Granite Bay or at King Bay, twelve miles

to the north. Granite Bay and surrounding area was explored

during the early fall with negative results and plans made to

explore King Bay durinq the fall of 1975. In early January, 1975,

preliminary map No. P. 968 by N. F. Trowell was published which

covered part of King Bay. Dr. Trowell pointed out an area of

carbonate breccia on Morgan Island which ran anomalously high

in gold and, as Morqan Island lay four miles up the glacial

strike from King Bay, it was decided to stake the carbonate

breccia formation on Morgan Island. On.the 27th of April, 1975,

Robert Andrews and the author engaged a Pegus Helicopter from

Dryden and staked claims No.'s 431450 to 431454 inclusive.

On September 8, 1975 two employees of Bayhill Develop

ment Ltd., Kingston, a company in which the author is a shareholder.

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left Kingston for Savant Lake in a three quarter ton pickup.

This vehicle was necessary to transport the estimited one .-."thousand

pounds of rock samples to be collected on the claims and returned

to Kingston. The two employees, Kevin Kehoe and Jack Howes, were

to be engaged in line cutting and sampling. The author flew to

Thunder Bay and was picked up and driven to Savant Lake by the

two employees on September the tenth. The party was joined by

J. R. Nixon on Sunday, September the fourteenth and the work com

pleted by.the evening of September nineteenth.

LOCATION;

Morgan Island, an island in the Northeast arm of

Sturgeon Lake lies 130 air miles north-west of Thunder Bay. It

may be reached by car from Thunder Bay via Highway 17 to Ignace

(180 miles) and north via Highway 599 to Savant Lake (77 miles).

The town of Savant Lake lies one mile north of the north-west

corner of Sturgeon Lake. The party was picked up at the landina

south of Savant Lake and driven bv Mr. Art Mousseau to his

fishina lodge on the northeast arm of Sturgeon Lake, a distance

of eighteen miles. This lodge is located one mile south west

of the claim group on Morgan Island. There is an air base on

Savant Lake which will fly passengers to the Lodge in a flying

time of ten minutes.

TOPOGRAPHY;

In. flying over or circling the island by boat the

topoaraphy appears to rise gently from the southern boundary of

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the claim group towards the north east for a distance of about

1500 feet to an altitude of ninty feet above the lake level.

From there it appears to gradually flatten towards the north and

west. On the qround the terrain is much nore rugged. In general

the central carbonate core of the island has low relief, seldom

rising more than thirty feet above the lake level while the

volcanics on either side stand out in much higher relief. The

ground over the carbonates tends to be swamoy with a heavy growth

of spruce, fir, cedar, iack pine and poplar. These trees attain

a thickness of as much as three feet. The growth over the volcan

ics is much more stunted, due to the acidic nature of the rocks,

and, in the highest sections, is practically nonexistant. It is

this uneven growth pattern that tends to give the island the

appearance of a gentle even topography.

Line cuttina was particularly difficult due to the

heavy growth, swamp, irregular topography over the volcanics

and the dense windfall. Fifty-one hundred feet of base line was cut"L.^.,^^^^,,^^ - ~

the lines set with a transit and chained and staked at 200 foot

intervals. The base line was trimmed out of undergrowth and fallen

trees for a width of six feet.

REGIONAL GEOLOGY;

According to N. F. Trowell (Preliminary Map No. P. 968)

Morgan Island lies near the juncture Of two rr.etavolcanic

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assemblages, one lower mafic to intermediate metavolcanic

sequence and another higher, finely intercalated sequence of

mafic to intermediate and intermediate to felsic metavolcanics.

North of the area rapid alternation of mafic to intermediate and

intermediate to felsic metavolcanics suggests that both are

occuring simultaneously. The fragmental rocks of the area show

bedding, laminations and well rounded fragments suggestive of

subaqueous reworking. Metasediments in the area are volcaniclastic,

Sills, dikes and irregular bodies of metagabbro and metadiorite

have intruded both the metasediments and metavolcanics. Three

syenite-monzonite complexes intrude the metavolcanics and met

asediments in the Vanessa and Vista Lake areas to the east and

south. A nepheline scapolite alkalic complex occurs north of

Vista Lake on Squaw Lake.

The area is dissected by a major penetrative shear

zone trending north-east alonq the north-east arm of Sturgeon

Lake. Associated shear folding with north-east trending axial

planes and subvertical fold axes have been observed in the

shear zone. This has been super imposed on regional flexual

slip folding with east-west trending fold axes. Warping of

foliations around the syenite complexes and other intrusives

has further complicated the structural relationships.

CLAIM AREA GEOLOGY;

The rock formation on the northern peninsula of Morgan

Island covered by the five mining claims has been subdivided into

five basic units. These units, from west

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to east, are the Dacite Unit, Felsic Carbonate Unit, Mafic

Carbonate Unit, Andesite Unit and Agqlomerate Unit. These have

been intruded, in places, by metadiorite and metagabbro. An

examination of the qraded beddinq and contact relationships be-

een the mafic carbonate and agqlomerate units suqgest that

x - are to the east with the Dacite Unit at the footwall side

of- the carbonates. The field examinations of the two carbonate

units, the upper part of the dacite unit and the lower part

of the agqlomerate unit sugqest that they have been subjected

to aqueous sedimentary processes and, in fact, were deposited

in a marine environment.

DACITE UNIT:*

This unit consists of subangular to subrounded felsic

clasts from .5 to 25 cm. measured along their axes. The clasts

contain subhedral quartz phenocrysts up to 5 mm. in a matrix of

chert and chlorite and constitutes about 7096 of the rock. The

matrix contains ash sized fragments of plageoclase (2096) quartz

(25%) and chlorite (1C^) with some chert. There are local zones

where the fragments are smaller and can be classified as a

lapilli tuff. There is a narrow zone 50 feet o f dacite tuff

at the top portion of the unit which is highly sheared and altered

and has numerous quartz phenocrysts. The alteration appears to

be sericite - pyrophyllite - talc series and, the uniformity in

grain size suag.ests it may have been water lain.

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FELSIC CARBONATE UNIT;

This unit overlies the Dacite Unit and is, in olaces.

interbedded with the Mafic Carbonate Unit. In qeneral, the

unit is composed of 2 - 3 mm. lonq clasts, subangular to rounded

and forming 50 to 8096 of the rock. The cement, mostly ankerite

with minor calcite and chlorite, surrounds the brown and greenish

clasts and in turn is often cut by narrow pinkish carbonate

veinlets. Some of the clasts show reaction rims and carbonate

filled amygdules. In places the rock has been extensively

sheared and altered, the effect of which is to elongate the

clasts and facilitate the development of fuchite which qives a

pale apple-qreen colour to the zone.

MAFIC CARBONATE UNIT:

The mafic carbonate unit consists of subangular to

subrounded clasts 2mm. to 3cm. in lenqth. They occupy from

50 to 80'?6 of the rock and consist of chlorite, epidote, megnitite.

leucoxene and, necleating alonq the edges, stilpnomelane. The

carbonate cement is usually ankerite but calcite and siderite

are also present. Towards the hanqwall side of the unit breccia

fragments of up to 2 feet in length were noted some of which were

seen interbedded with the agglomerate unit. In places there

are zones of felsic clasts suqgesting seme interbedding of the

two carbonate units.

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ANDESITE UNIT:

In this zone massive mafic volcanics grade upwards into

pillowed mafic volcanics with calcite filled amvgdules occupving

309i of the rock. The pillows are rounded, from 2 to 3 feet in

width with a H inch selvage. The andesites are fine grained and*-

consist of chlorite, magnitite. plaqeoclase. leucoxene, epidote

and a small amount of carbonate.

ACID AGGLOMERATE UNIT;

Althouah the clasts and matrix are somewhat similar in

composition to the Dacite Unit the clasts are more rounded and

show strong evidence of subaqueous reworking with beddinq of

ash size particles quite common. The unit, particularly the

lower partion. could be properly called a volcanic conglomerate.

There are numerous zones of verv well rounded boulders up to

three feet in diameter. Periods of quiescence are represented

by thin bands of chert and weathered horizons. The matrix is

generally a mixed zone of intermediate lapilli tuff and tuff

breccia.

METADIORITE INTRUSIVES;

The dacite unit is interrupted along the northwest

shore of the island by a local intrusion of metadiorite. The

metadiorite still shows residual vestiqes of original egneous

texture although extensively altered to a chlorite, epidote,

albite assemblage of minerals typical of greenschist facies of

metamorphism. In the east central portion of the map area a

porphyritic metagabbro dyke was encountered cutting the

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agglomerate unit. This dyke had the unusual spotted or lepord

texture resulting from metamorphism.

STRUCTURE;

Sedimentary structures found in the field were very

variable in type and distribution. Bedding was most evident

in outcrops along the shore with bedding directions being

deformed considerably due to folding. Both the mafic and felsic

units are bedded but, due either to soft sediment deformation or

secondary remobilization, it was not always apparent. Towards

the top of the mafic carbonate unit bedded clasts of carbonate

breccia 2 to 3 feet in length and up to one foot in width are

found as well as in the overlying agglomerate unit.

According to N. F. Trowell the Northeast arm of

Sturgeon Lake is a major shear zone. This is most evident on

Morgan Island at both the footwall side of the felsic carbonate

and on the hanging wall side of the mafic carbonate unit. The

outcrop of the carbonate are usually shear faces one to three feet

in height and from two to thirty feet in length. The shearing

direction varies from N. 10 E. to N. 60 E. and is nearly

vertical. There is a fairly strong fault scarp striking N. 30 W.

cutting the claim group. The fault scarp is very noticable in

the dacite and agglomerate units (up to 50 feet in height) but

disappears in the carbonate units.

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It is hoped that there are; within the carbonates,

a number of maior shear zones that could be localizing agents for

gold bearing solutions.

ASSAYS;

Fifty hand specimens and three 250 pound samples were

collected in the field and assayed by combined fire assay and

atomic adsorption methods. The purpose of the assays was to try and

determine if; in fact, there was a low uniform synqenetic gold

content in the carbonates. Samples were taken that were free

of quartz veins or heavy alteration that would suggest any con

tained gold was introduced or secondary and thus qive an anomalously

high reading. One sample, collected near the hanging wall of the

mafic carbonate unit, was highly sheared and ran anomalously high

gold (4535 ppb).

Of the 20 samples of mafic carbonate assayed 8596 ran be

tween 40 and 95 ppb, two ran less than 40 and one ran over 95.

The averaqe (excluding the anomalously hiqh value) was 60 ppb.

Of the sixteen felsic carbonate samples assayed, eleven were

between 35 and 145 ppb, three less than. 35 and two were greater

than 148 ppb. The averaqe was 82 ppb. The eight samples of

volcanics assayed ran from N. D. to 100 (Sheared dacite) and

averaged 46 ppb.

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CONCLUSIONS

The detailed mapping has located the carbonate units

in some detail and. within the claim group, has an average width

of 420 feet and a strike lenqth of 4200 feet. The carbonates

do contain a low syngenetic qold contenet but it appears to be

too low to be of economic significance. The shear zone adjacent

to the hanging wall does contain, apparently, a significantly

higher gold content but there is insufficient data to assess its

importance. The present plans call for the drilling of a diamond

drill hole across the carbonate units this fall to try and locate

any major mineralized zones.

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REFER EN C E S

N. F. TROWELL Preliminary Map P. -968

Northeast Arm -SQUAW LAKE SHEET

WAGNE GORDANIER Unpublished thesis University of Ottawa

Geochemistry of a Carbonate Breccia

Unit in N. W. Ontario.

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ASSESSMENT WORK BREAKDOWN

1. TYPE OF SURVEY.... ...................Geological

2. AREA.......................... Patricia Mining DivisionSturgeon Lake

3. MINING CLAIM NUMBERS.......... 431450431451431452431453431454

4. LENGTH OF LINE CUT AND CHAINED......... 5185 feet.

5. SUMMARY OF DAYS WORKED(a) Total technical work........ 68 days

(b) Total line cutting and sampling... ISdays

(c) Assays...................... 19 days_____

105 days

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ASSESSMENT WORK BREAKDOWN

TECHNICAL WORK

W. H. Hiqgins980 Bourne Cresc., —Geoloqist -Sept. 11-19 (incl.) 9 X 7 ^ 63 daysKinqston, Ontario

J. R. Nixon P. Eng. —Assistant -Sept. 15-19 (incl.) 5 days

LINE CUTTING AND SAMPLING

Kevin Kehoe —Labourer -Sept. 11-19 (incl.) 9 days 23 John Street Apt. #9 Kingston, Ontario

Jack Howes —Labourer -Sept. 11-19 (incl.) 9 days R. R. #3 Odessa, Ontario

ASSAYING

Bondar Clegq -Oct. 9, 1975 .......... . . .. . . . 237.50Bondar Clegq -Jan. 14, 1976................... 23.75

Technical Services -Oct. 27, 1975 ... . .............. 35.00296.25

Assessment 296.25 , rt ,——————— - 19 days

Total 105 days

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QUALIFICATIONS Wilfrid H. Higgins

EDUCATION;

Experience:

B. A. -geology, mineralogy - Queens University, 1949 B.Se. -mining engineering - Queens University, 1953

-2 years government geological survey

-4 years - party chief mining exploration parties-4 years -in charge of exploration on 8,000 square

mile concession in NewFoundland.

-7 years -Assistant Mine Superintendent -Buchans

Unit of American Smelting and Refining in NewFoundland

-2 years -Superintendent of Mines for three producing

mines in NewFoundland.

-4 years -Resident Engineer Terra Nova Explorations

in Quebec City -mining subsiduary of the Price

Company Ltd.

- 3 years - Member of Board of Directors of Terra

Nova Properties -owners of Buchans Operations.

MEMBERSHIP - Professional Engineers of Ontario

- Canadian Institute of Mining and Metallurgy

- Prospectors Association of Canada.

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n * CHEMICAL HCCCAMCM AND

* CO^TMACT LABOOATOHICB

Bta EVANS AVE.. TORONTO. ONT.. M8W 2V4 CANADA

TELEPHONE: 7525895- AREA 416

CABLE ADDRESS TECSERV

l '

CERTIFICATE OF ANALYSISSAMPLHS) FROM Dr. J. H. Brown,

L/ClSClJ, blJl^Jlk Wi AVi***A**{j .U**^*,***-^ * ***t)f ' *"~ '

Queen's University, REPOS Kingston, Ontario. K7L 3N& T - 9

Inv.

SAMPLES) OF PULP

*

Gold (Au) ppm

1 (a) 0.04

1 (b) 0.02

2 (a) *:0. 02

2 (b) *:0. 02

3 (a) 0.02

3 (b) 0.02

T NO. 900

#1190

Samples. Pulps and Rejects discarded after two months

DATE October 27th. 1975.__________ SIGNEDCTA

TORONTO. MONCTON. and SPOKANE. WASH.

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BDNDAR-CLEGG S, COMPANY LTD.784 BELFAST ROAD, OTTAWA, ONTARIO. K1Q OZB PHONE: S37-311O

Geochemical Lab ReportExtraction.

Method

AU HNO, -"- " ' " "- " "' -J. ——

P.A.-A.A*

Fraction Used. -100 Hooks

Report No..

From

Date .

M*.

October 9 19 75

SAMPLE NO.

1-13

13 - 10.- 13 - 20

13 - 30

13 -1*0

13 - 50

25- 13

BL - 5

EL2 - 610

SE - 1312E -120

18E - LOO

210B - 230

210B - 350

2122 - 50

212B - 270

a8E - 30022E - 200

22E - 3UO

22E - 800

28E - 300

2V- 115

UV - 85

8V- 60

10V - 5

10V - 2UO Ugh

10V - 2J40 dazk

10W - 360

12V- 65

12V- 14*5

13V - 380

i

fe

k&t

220

230

160

95

375

7590

100

mo7515

955080

35UO

J*5

80

575

35U560

5060

95H.D.

80

35no

'

*

SAMPLE NO.

ILW - ISO

lltV - UlO

16W - 500

16w - 5SO

lew - mo18W - 500

18W - 6UO

210W - 110

210V - 160

212Y7 - 50

212\/ - 160

21LV7 - 320

21LW - 500 .

216V - 190

218W - 350 .

22W - 1UO

22\/ - 200

28\/ - 50

28V - 820

Note t N.D. - Ki )t Detec

ftb10

50

.J!-75

—ll.fi*. 520

Hi*

10

5560*100

856S

65

60

35

50

20

ted

"•"* '

!.

50

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BDNDAR-CLEGG S C D M PAKIV784 BELFAST ROAD, OTTAWA, ONTARIO, K1G OZS PHONE: S37-311O

Geochemical Lab Report- . au - riiiu^-n^J. fcim^cjion. . .....,,. , 3

M..KOH F.A.-A.A.

Report N

From.

JU-U n

4r. W.Tf. Hlppiiris.

P,,r,i™, )t.H -100 rocks. n^ J .anuary 1 14 , ^ 76

SAMPLE NO.

1-13

10W-13

12E-120

13-320

IE-61* 0

'

Au-jyjli —

20

565

65

30

~

—— —— .

REMARKS

~

. -V-.

-'-

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BQNDAR-CLEGG S. COMPANY LTD.764 BELFAST POAD, OTTAWA, ONTARIO. K1G OZS PHONE: S37-311O TEUEX: O53-354B

Mr. W.H. Higgins, 1015 Hudson Drive* Kingston. Ontario*

INVOICE: N 2 6188

DATE: October 9. 1975.t

REPORT NO: 975'5

PROJECT:

50

50

Analyses of Gold

Sample Prep, (rocks)

' S3. 50

1.25

TOTAL

$175.00

62.50

S237.50

MINISTRY OF NATURAL RESOURCES

RECEIVEDOCTo 1976

RESIDENT GEOLOGIST'S OFFICE SIOUX LOOKOUT

THIS IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED .^./•3fc-. : :-

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NDAR-CLEGG GL COMPANY LTD.ROAD. OTTAWA. ONTARIO. K1B CZ5 PHONE: 237-311O TELEX: O53-354B

INVOICE: N2 6702

DATE: January lU, 1976.i

REPORT NO: 10-6

PROJECT:

Mr. H. W. Higgins, 980 Bourne Crescent, Kingston, Ontario.

5

5

Analyses of Gold

Sample Prep. Crocks)

6 S3.50

6 1.25

TOTAL

$17.50

. 6.25

^23.75

MINISTRY OF NATURAL RESOURCES

RECEIVEDOCT8 1976

RESIDENT GEOLOGISTS OFFICE SIOUX LOOKOUT

THIS IS A PROFESSIONAL SERVICE ACCOUNTS DUE WHEN RENDERED

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DEPARTMENT OF MINING ENGINEERING

GOODWIN HALLQu.een's University Kingston, CanadaK7L 3N6

February 16, 1976

Mr. W.H. Higgins, 1015 Hudson Drive, Kingston, Ontario.

Dear Mr. Higgins:

This letter will serve as your receipt for the amount

of $35.00 , for analyses and expenses in gold evaluation.

Yours truly,

J.H. Brown,Professor of Mining Engineering.

JHB/dl

MINISTRY OF NATURAL RESOURCES

RECEIVED

RESIDENT GEOLOGIST 1? Of RCE ilOUX LOOKOUT '

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Ministry ofNaturalResources

52Ja2SE87e5 2.2068 SQUAW LAKE 300

August 19, 1976

Mr. Harry L. BellMining RecorderMinistry of Natural ResourcesBox 669Court HouseSioux Lookout, OntarioPOV 2TO

Dear Sir:

C'-r i le r.jmt/tr 2 .2068

Vojr liie r.gmoer

Re: Mining Claims Pa. 431450 et al , Squaw Lake, File 2.2068 ————^———-———

The Assaying of Bulk and Grab samples Section 86(18, 19, 20) and Geological assessment work credits as shown on the attached statement have been approved as of the a'jove date.

Please inform the recorded so indicate on your

Yours very truly,

c these mining claims and

J. If. McGinnfree tor

Lands Administration Branch

Whitney Block, Room 1617Queen's ParkToronto, OntarioM7A 1X1Phone: 416-965-6918

DN/mw

cc: Mr. Wilfrid H. Higgins Kingston, Ontario

cc: Resident GeologistSioux Lookout, Ontario

Page 22: 52J82SE8785 2.2868 SQUAW LAKE ( RECEIVED€¦ · 52J82SE8785 2.2868 SQUAW LAKE (7)1(7) RECEIVED GEOLOGY - MORGAN ISLAND INTRODUCTION; Durinq the early fall of 1974 the author and

'•."H

ONTARIO

THE MINING ACT REPORT OF WORK

A separate form Is required fer each type of work lo be recorded.

To the Recorder of ...........t..?L:..O.

nome of Recorded

^ Division

/,^Miner's Licence

Post Office AddYessdo hereby report the performonce of ........../.S....................... doys of ........../j..5.S.S.fl.(.ff8i........ .....y^.^..^,.,.......,....,..

not before reported to be opplied on the following contiguous claims

Cloim No. Doys Claim No. Doys Claim No. Days

3aologrc(H--Branch O D MASSESSMENT FILESRESEARCH O FFICE

•SEf 23 1976

RECEIVED

AH the work wos performed on Mining Cloim (s) ..................................................................................... -(In the cose of geological and/or geophysical survey (s) where more than 18 claims ore involved 'attach oi schedule)

READ CAREFULLY; THE FOLLOWING INFORMATION is REQUIRED BY THE MINING RECORDER.

For Monuol Work, Stripping or Opening up of Mines, Sinking Shafts or Other Actual Mining Operations - Names ondaddresses of the men who performed the work and the dates and hours of their employment.For Diamond ond other Core Drilling - Footage, No. ond angle of holes ond diameter of core. Nome and address ofowner or operator of drill. Dotes when drilling wos done. Signed core log and sketch in duplicate.For Compressed Air or Other Power Driven or Mechanical EquipmentType of drill or equipment. Names and addresses of men bngoged in operating equipment ond the dotes and hours oftheir employment.For Power Stripping - Type of equipment. Name and address of owner or operator. Amount expended. Dotes on whichwork was done. Proof of actual cost must be submitted within 30 days of recording.With each of the above types of work sketches are required to show the location ond extent of the work in relationto the nearest claim post. In the case of diamond or other core drilling the sketch must be submitted in duplicate.For Geologicol ond Geophysical Survey - The names ond addresses of men employed os well os dates. Type ofinstrument used in the case of geophysical survey. Reports ond mops in duplicate must be filed with the Ministerwithin 60 days of recording.For Land Survey - the name and address of Ontario Land surveyor.

The Required Information is os Follows: (Attach a list if this space is insuMINISTRY OF NATURAL RESOURCES

RECEIVEDOCTu 1976

RESIDENT GEOLOGIST'S OFFICE SIOUX LOOKOUT

sfifoH

UJ

Ofa.

x 55OfO

UJH

yuZ POf UJu fif

Ofoo.Ul Of

Dote ...../.ft.Signature of Rec/orSeJ Holder or Agent

The Mining Act Certificate Verifying Report of Work

^(Post Off ice Address) ^

hereby certify:1. That l hove a personal and intimate knowledge of the facts set forth in the report of work annexed here-

5; to, having performed the work or witnessed same during and/or after its completion.

Dated.

2. That the annexed report is true,

......... .19

, i. i J C. l A

Ul

3Ult/*Ju.

ZDf

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z

ignature'

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Natural Resources

: 'Ontario

Lands .AdministrationBranch

UnitTechnical Assessment Work Credits

FH*

2.2068

Recorded Holder

Township or AreaWilfrid H. Higgins

Squaw Lake

Type of survey and number of Assessment days credit per claim Mining Claims

GeophysicalElectromagnetic

Magnetometer.

Radiometric —

Induced polarization.

Section 86 (18) —

Geological ——— 23

Geochemical.

.days

.dayst.days

.days

.days

.days

.days

Man days E]

Special provision D

Airborne LJ

Ground LJ

Notice of Intent to be issued:

O Credits have been reduced because of partial coverage of claims.

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

Q No credits have been allowed for the following mining claims as they were not sufficiently

' covered by the survey:

Pa. 431450 to 54 inclusive

- ; [' ^ 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 — 60; Geological — 40; Geochemical — 40;'' ''-'' - : ' ' - -

Page 24: 52J82SE8785 2.2868 SQUAW LAKE ( RECEIVED€¦ · 52J82SE8785 2.2868 SQUAW LAKE (7)1(7) RECEIVED GEOLOGY - MORGAN ISLAND INTRODUCTION; Durinq the early fall of 1974 the author and

Mm.-iUv Ci'NaturalHesourcos

Ontario

LandsAdministrationBranch

Unit Technical Assessment Work Credits 2.2068

Recorded Holder

Township or AreaWilfrid H. Higgins

Squaw Lake

Type of survey and number ol Atte*sment days credit per claim

Geophysicalelectromagnetic

Magnetometer —

Radiometric ——.

. clays

. days

Induced polarization ,

-— days

_days

Section 86 (18) .19, s. 2 0

Geological .—-———.—— .days

Geochemical. . days

Man days C]

Special provision O

Airborne D

Ground LJ

Notice of Intent to be issued:

fi Credits have been reduced because of partial coverage of claims.

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

CD No credits have been allowed for the following mining Claims as they 'vara not sufficiently covered by the survey:

ASSAYING

3 Bulk samples

50 Grab samples

collected from mining'claims Pa. 431450 to431454 inclusive.

Amount expended on assaying of samples * S296.25

Total assessment days credit allowed - 19 days

The assessment work credits of 19 days is to be

proportioned on the above 5 mining claims as

3.5 days for each claim.

Apnroved - August 19, 1976

The Mining Recorder may reduce the above c redits if necessary in order that the total number of approved assessment days recorded on Bach claim does not exceed the maximum allowed as follows: Geophysical — 80; Geological — 40; Geochemical — 40;

Page 25: 52J82SE8785 2.2868 SQUAW LAKE ( RECEIVED€¦ · 52J82SE8785 2.2868 SQUAW LAKE (7)1(7) RECEIVED GEOLOGY - MORGAN ISLAND INTRODUCTION; Durinq the early fall of 1974 the author and
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Ministry o' Natural Resources

Ontario

OFFICIAL RECEIPT

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CUSTOMER'S COPY

- 685 GARDINERS ROAD,DIVISION OF DACON CORPORATION LTD.

KINGSTON. ONTARIO K7M 3Y4

l

SOLD TO:.

ADDRESS: .

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STORE —— 389-4440OFFICE ———389-5084 ACCTNG. ——— 389-6542

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wLilism A. H i c v ins Const

, . September 15ird r 1*315

re : Tv.-o weeks, services for two men.

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4.80 384.00

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THE BANK OF NOVA SCOTIAC23 O AROINCR'S ROAD KINGSTON. ONT,

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RESTAURANT

"*--oe

v; THE SUM OF

;^;v REFERENCE

THE COMMODORE MOTOR HOTELSAULT STE. MARIE. ONTARIO

igh&k; TELEPHONE

? SV MEALS

•Mini

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THUNDER BAY. ONTARIO N? 1776 T.B.

CASH 'CREDITWf ACKNOWLEDGE RECEIPT OP THE AMOUNT PRINTED BELOW WHICH HAS WEN CREDITED TO YOUR ACCOUNT. PtXASf RETAIN THO COPY TOR REFERENCE. U

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ROOM AMT. PAID

THANK YOU CALL AGAIN

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MAC ANU fO S* Y

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