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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.
- 2 -
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
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
- 4 -
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
- 5 -
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.
- 6 -
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.
- 7 -
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
- 8 -
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.
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.
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.
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.
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
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
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.
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.
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
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-.
-'-
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-. : :-
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
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 '
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
'•."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
>• H
o.
z
ignature'
;.. ^
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;'' ''-'' - : ' ' - -
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;
rf-
(O
if -S p
"A--fn -/ro —J. '
- s-
Ministry o' Natural Resources
Ontario
OFFICIAL RECEIPT
CUSTOMER'S COPY
- 685 GARDINERS ROAD,DIVISION OF DACON CORPORATION LTD.
KINGSTON. ONTARIO K7M 3Y4
l
SOLD TO:.
ADDRESS: .
'H!6S
STORE —— 389-4440OFFICE ———389-5084 ACCTNG. ——— 389-6542
CUSI. ODDf* NO.
DELIVER TO:...--.
ADDRESS:____
r/!ii
QUANTITY
^r.r
IN'V(
QUANTITY SHIPPED
*rs~•3
CASH"""! elb
DICE
MATERIAL DESCRIPTION
^^^. XX 2— X 2 x ^^?^ 3^ y X ^-jc'3 ' "^?c*t-v^^^y
,.0. \ O N ACCT. iMTJifTRFI'n ?AID OUT ! JOS REF.
: 1i i
SOLD BY ~j *Hi^to M
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