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42J*1tCMI1 2.9361 KIPLIM6 01O
GEOLOGICAL A ELECTROMAGNETIC SURVEY REPORT
on the
KIPLING TOWNSHIP
KAOLIN/SILICA SAND PROSPECT
for
KAOLIN OF CANADA INC.
July, 1986 H.P. Hutteri, H.B.Sc.
^r- c
42JCUEM11 2.9361 KIPLING O1OC
TABLE OF CONTENTS
Page
INTRODUCTION.................................. 1
LOCATION AND ACCESS........................... 1,2
PROPERTY DESCRIPTION.......................... 2
TOPOGRAPHY AND VEGETATION..................... 2,3
PREVIOUS WORK............... .. . .. . . .. . . . . . .. . 3,4
REGIONAL GEOLOGY............. . .. . . . . . . . . . . .. . . 4,5,6
GEOPHYSICAL SURVEY
Introduction..... .. .. ...... . ...... . .. ..... 6,7
Procedures................. .............. 7
Interpretation............................ 7,8
GEOLOGICAL SURVEY........ . . . . .. . . .. . . . . . . . . .. . 8,9
CONCLUSIONS i RECOMMENDATIONS................. 9,10
REFERENCES................. ..... ...... . . ...... 11
CERTIFICATE................................... 12
APPENDIX .. . . ............ .. . . ... . ... .......... 13
List of Figures
Figure 1 - Regional Location Map
2 - Claim Location Map
3 - Moose River Basin Map
4 - Geology of the Hearst-Kapuskasing
Area-Map 2166
Geological Map of Kaolin/Silica sand
prospect
VLF-EM Profile Map
Tables
i
Table I - Table of Formations for the Moose River Basin
Ka
olin
of
Can
ada
Smoo
th M
ock
FoM
?\-?
oc
REG
IONA
L LO
CATI
ON
MAP
ff-il 0
.""':
•' L^
..•..'.
••.•:-
:t.--
.....f
.S
CA
LE
(00
80
O
100
i—k
^L
—i
KU
.OH
CT
HC
3
-1-
INTRODUCTION
Geological and VLF electromagnetic surveys were
conducted over a 20-claim-property located in Kipling
Township, Porcupine Mining Division of Northeastern
Ontario, on behalf of Kaolin of Canada Inc. The
geological survey was performed in order to locate any
surface exposures of the Cretaceous Mattagami Formation
which consists of potentially economic concentrations of
Kaolinitic quartz sand, clays and lignite. The VLF-EM
survey was conducted in order to locate lignite, some
of which has been reported along Adam Creek, approximately
two miles* to the east of the surveyed area.
LOCATION AND ACCESS
The subject property is located in east central
Kipling Township, Porcupine Mining Division, Northeastern
Ontario. It lies 64 air miles northeast of Smooth Rock
Falls and access to Kipling Township can be gained by
travelling Highway 11 to Smooth Rock Falls, then north
ward along Highway 807 through Fraserdale where a dirt
road continues past Smokey Falls to the Kipling Dam.
From here a dirt road follows for approximately one-half
mile to an old diamond drill road which goes eastward
approximately 3.5 miles to the claim group. The Ontario
-2-
LOCATION AND ACCESS cont'd
Northland Railway lies 21 miles to the east of the
property and power is readily available from the Kipling
Generating Station located 3 miles to the west.
PROPERTY DESCRIPTION
The Kipling Township Kaolin/Silica Sand prospect
consists of twenty (20) unpatented mining claims
(approximately 800 acres), all located in Kipling Township,
Porcupine Mining Division, Ontario. The property is
further described as follows:
Claim No. No. of Claims Date Recorded
P825792 - 811 20 Aug. 07, 1984
The claims are currently held for Kaolin of
Canada Inc. by Don Hillier, General Delivery, Connaught,
Ontario PON 1AO.
TOPOGRAPHY AND VEGETATION
The property consists dominantly of low lying
wet spruce bogs with relief up to 30 feet around rivers
rl
KIPLING TOWNSHIP
825802825809 825810
KIPLING:
mllM
SCALE
MILES
KAOLIN OF CANADA Inc.
CLAIM LOCATION MAP
Figure 92H.P.Hutttrl
-3-
TOPOGRAPHY AND VEGETATION cont'd
and along a ridge on the southern boundary. The swampy
areas contain mainly spruce with lesser alders, tamarack
and cedar trees, while the higher areas contain spruce,
popular and jackpine. Thick alders surround the main
river which winds through the claim group. Outcrop
comprises less that 155 of the property and is confined to
high areas in the southeast corner. A relatively thick
blanket of overburden covers the claim group and consists
of clay underlain by till.
PREVIOUS WORK
The general area in which the Kipling Township
Kaolin/Silica sand prospect lies has been explored
intermittently over the past 100 years.
Towards the end of the 19th century the Geological
Survey of Canada and the Ontario Bureau of Mines mapped
the basic geology. They reported the existence of
deposits of lignite, fireclay, kaolin, silica sand,
gypsum and iron. In the late 1920's and early 1930's,
the Ontario Department of Mines conducted an extensive
program of development and feasibility studies of the
minerals within the James Bay Lowland, Extensive drilling
-4-
PREVIOUS WORK cont'd
was also carried out in the Onakawana lignite area.
Since 1966, the Moose River Basin has been
actively studied by the Ontario Geological Survey. Explor
ation programs have consisted of geological mapping, geo
physical studies and three sonic drilling programs.
In 1982, Lignasco Resources Ltd. and joint
venture partner, Selco Inc. completed linecutting and a
magnetometer survey covering most of the subject property.
A magnetic anomaly was outlined and a sonic drill was used
to drill one hole (J-1-2) in order to test for diamond
iferous kinberlites. Bedrock was not reached and drilling
was stopped at a 147 metre depth.
The Kipling Township Kaolin/Silica sand prospect
is currently being assessed for its potential to host
large reserves of Kaolin and silica sand by Kaolin of
Canada Inc.
REGIONAL GEOLOGY
The Kipling Township Kaolin/Silica sand prospect
lies along the southern margin of the Moose River Basin
which is located within the James Bay Lowlands of North
eastern Ontario (figure 3). According to Telford and
Verma (1982), the Moose River Basin represents a basin of
intermittant Phanerozoic sedimentation containing considerable
thicknesses Q f Paleozoic and Mesozoic sedimentary
MOOSE RIVER BASIN
Moose River Basin
Figure f 3
OGS Study 21, 1982
-5-
REGIONAL GEOLOGY cont'd
rock sequences (Table 1).
The Paleozoic sedimentary sequence Consists of
a 700 metre section of marine limestone, shales and
evaporates. The Mesozoic sedimentary sequence consists
of non-marine formations, the Middle Jarassic Mistuskwia
Formation and the overlying Cretoceous Mattagami Formation.
The Mistuskwia Formation consists of unconsolidated
calcareous clays with thin horizons of quartz sands.
The Mattagami Formation occupies the southern and south
western portion of the Moose River Basin and can be
divided into a stratigraphically lower portion, Type A,
and the upper Type B. The Type A formation is characterized
by lignite seams and black carbonaceous clay whereas the
overlying Type B formation consists mainly of thick
sequences of unconsolidated kaolinitic quartz sand,
kaolinitic clays and non-calcareous clays. The Mattagami
formation is then overlain by two Wisconsin till sheets
consisting of silty till overlain by glaciolacustrine
clays, silts and sands overlain by muskeg. An errosional
unconformity separates the Cretaceous sediments from the
Devonian limestones and shales in the southern part of
the Cretaceous basin, and from the Jurassic 'Mistuskwia
Formation in the northern part of the basin. Post Middle
BASIN
Phanerozoic Cenozoic
QuaternaryPleistocene and Recent
Till, clay and muskeg -- —— —————— -- — -unconformity
Mesozoic
Cretaceous:Mattagami Formation (upper-Type B formation):
unconsolidated kaolinitic quartz sands and
clays.Mattagami Formation (lower-Type A formation):
unconsolidated carbonaceous clay with lignite*
seams.
Middle JurassicMistuskwia Formation: unconsolidated calcareous clays with lesser quartz sands.
- ——— - —— ---------unfonformity------ — - — —————
PaleozoicPost Middle Devonian
Lamprophyric and kimberlitic intrusions------------—--intrusive contact--——----—---.
DevonianMarine carbonate rocks, shales and evaporates,
and minor marine and continental clastict
sediments
Precambrian Archean
Biotite-quartz-feldspar gneiss - mafic to intermediate metavolcanic rocks
-6-
REGIONAL GEOLOGY cont'd
Devonian lamprophyre and Kimberlite intrusions have also
been noted in the region which lies immediately west of
the Kapuskasing Structural Zone.
Another unconformity separates the Paleozoic
sediments from the precambrian basement rocks. The
basement rocks from OGS Map 2166, appear to consist
mainly of Archean Biotite-quartz-feldspar gneisses. A
narrow Archean greenstone belt has been interpreted to
trend northwest under the Moose River Basin, however,
its location below the basin is not known.
The southern edge of .the Moose River Basin is
clearly defined by a Precambrian escarpment of gneissic
rocks which strikes in an east-west direction. The
feature may be fault controlled as it truncates the
Paleozoic and Mesozoic strata of the basin. Sediments
within the basin dip 3 to 5 degrees towards the centre but are downwarped adjacent to this feature.
GEOPHYSICAL SURVEY
Introduction
An electromagnetic VLF survey was completed on 28.8
Kilometres of flagged grid lines using the Geonics EM16
unit. The transmitting station used for the survey was
Seattle, Washington, which has a transmitting frequency
-7-
GEOPHYSICAL SURVEY cont'd
of 24.8 Kilohertz. The instrument specifications are
located in Appendix I. A total of 960 readings were
taken at 30 metre intervals along grid lines spaced 100
metres apart, trending 354 . The survey was conducted
by Mike Tremblay of Timmins, Ontario in May, 1986.
Procedures
Grid lines trending 354 were surveyed facing
north at 30 metre intervals. The in-phase and quad
rature values were recorded and plotted on the profile*
map. The values on the left side of the survey line
represent the in-phase values and those on the right
side represent the quadrature values.
Interpretation
One extensive zone of conductivity was detected
and is hereafter referred to as conductor "A". Several
small and relatively weak conductors were detected,
however these are believed to be caused by conductive
overburden (rivers, swamp etc.) and variable topography:
since, the crossovers are poorly developed, the quad
rature profiles generally follow the in-ph'ase profiles
and some of the crossovers coincide with mapped creeks
and hills.
-8-
GEOPHYSICAL SURVEY cont'd
Conductor "A"
This is the strongest and most extensive con
ductor on the property. It has a moderately strong
in-phase response and the crossovers are fairly well
developed. Conductor "A" is located along the southern
margin of the claim group. It is evident in the eastern
and western sections, however, it passes out of the
property in the central section. The conductor also
coincides in part with an easterly trending ridge
located along the southern property boundary. It is
believed by the author that Cpnductor "A" represents the
faulted contact between the Cretaceous Mattagami
Formation to the north and the Archean basement gneisses
to the south.
GEOLOGICAL SURVEY
A geological survey was carried out over 28.8
kilometers of flagged grid lines, spaced 100 metres apart
and trending 354 . All outcrop, rivers, creeks, swamps,
hills and tree types were mapped and tied into the grid.
The survey was carried out by the author of this report.
According to O.D.M. Map 2166 covering the Hearst-
Kapuskasing area, the subject property is underlain
dominantly by Precambrian basement gneisses (figure 4),
Geol
ogy
of t
he H
earst-Kapuskasing
Area
MAHO
NEY n
Map
2166
Kaolin/Silica
Sand P
rospect
KAOL
IN OF
CAN
ADA
INC.
Porc
upin
e Mi
ning
Div
isio
n, Ontario
Scale: 1:253,440
"
" Figure #
4
lit
Jtl
flft
t H
tntt
nit
: M
MIf
tAff
.
AH
CH
IAN
AN
D M
IOT
KM
OZ
OIC
**A
*e*
HH
MM
IVI
rnoT
Cfto
zoic
C
AMO
IUTI
TI c
oim
ju**
j, sss
sr-
-9-
GEOLOGICAL SURVEY cont'd
however, this is not the case. While the geological
survey was being conducted only a few small rock exposures
in the southeast corner of the property were located.
The exposures were located on an east-west trending ridge
and consisted of biotite-quartz-feldspar gneisses. These
gneisses varied greatly in grain size and mafic mineral
content and had an easterly trending foliation. No other
outcrop was located on the property, however, in 1982,
Selco drilled a hole (J-1-2) in the south-central portion
of the property using a sonic drill and encountered
kaolinitic quartz sands and clays at a vertical depth of
55 feet. The VLF-EM survey, described previously, located
an extensive conductive zone along the southern margin of
the claim group immediately north of the east-west trending
ridge. This is believed by the author to represent the
actual faulted contact between the Cretaceous sediments
of the Mattagami Formation to the north and the Precambrian
basement gneisses to the south.
CONCLUSIONS 6 RECOMMENDATIONS
VLF-electromagnetic and geological surveys were
carried out over 20 claims held by Kaolin of Canada,
within Kipling Township of Northeastern Ontario.
-10-
CONCLUSIONS A RECOMMENDATIONS cont'd
The property is underlain primarily by kaolinitic
quartz sands and clays of the Mattagami Formation. The
contact between the Mattagami Formation and Precambrian
gneisses to the south is believed to be along the southern
boundary of the subject property and is represented by a
strong electromagnetic conductor which lies immediately
north of an east-west trending ridge along the same
boundary.
No lignite was detected by the electromagnetic
survey, however, the area is underlain dominantly by
swamp which may have hindered .its detection.
It is recommended that a systematic sonic drill
program be implemented in order to determine the tonnage
and grades of the kaolin and silica sand present.
-11-
REFERENCES
Bennett, G., Brown, D.D., George, P.T. and
Leahy, E.J., 1967 Operation Kapuskasing.
O.D.M. Miscellaneous Paper 10 and O.D.M. Map 2166.
Pitcher, D.H. and Barlow, R.B., 1979 Multi-
frequency Airborne Electromagnetic Profiles
and Interpretation Cretaceous Basin Area-James
Bay Lowlands. O.G.S. Open File Report 5270.
Telford, P.G. and Verma, H.M., 1982 Mesozoic*
Geology and Mineral Potential of the Moose River
Basin O.G.S. Study 21.
Pertinent assessment files.
-12-
CERTIFICATE
I, Henry Hutteri, of Timmins, Ontario hereby certify
that:
1) I hold an Honours Bachelor of Science Degree
in Geology from Laurentian University,
Sudbury, Ontario having graduated in
June, 1985.
2) I have based my conclusions and recommendations
contained in this report on knowledge of the
area, my previous experience and on the results
of field work conducted on the property.
3) I hold no interest directly or indirectly in
Kaolin of Canada Inc. or in this property other
than professional fees nor do I expect to
receive any interest in the property.
Henry P. Hutteri, H.B.Se.
-13-
APPENDIX I
E M16 YLF Electromagnetic Unit
Pioneered and patented exclusively by Geonics Limited, the VLF method of electromagnetic surveying has been proven lo be a major advance In exploration geophysical Instrumentation.
Since the beginning of 1965 a large number of mining companies have found the EM16 system to meet the need for a simple, light and effective exploration tool for mining geophysics.
The VLF method uses the military and lime standard VLF transmissions as primary field. Only a receiver Is then used to measure the secondary fields radiating from the local con ductive targets. This allows a very light, one-man instrument to do the job. Because of the almost uniform primary field, good response from deeper targets is obtained.
The EM16 system provides the in-phase and quadrature components of the secondary field with the polarities indicated.
Interpretation technique has been highly developed particularly to differentiate deeper targets from the many surface indications.
Principle of OperationThe VLF transmitters have vertical antennas. The magnetic signal component is then horizontal and concentric around the transmitter location. - .
II Specifications
i Source of primary fMd
Transmitting •tallow used
Operating frequency rang*
••remelera matured
Reading lime
"••hod o! wading
VLF IranamHUng stations.
Any desired station frequency can be supplied with the Instrument In the form of plug-In tuning units. Two tuning units can be plugged In at one time. A switch selects either station.
About 15-25 kHz.
(1) The vertical In-phase component (tangent ol the till anole of the polarization ellipsoid).(2) The vertical out-of-phase (quadra ture) component (the short axis ol the polarization ellipsoid compared to the long axis).
In-phase from a mechanical Inclino meter and quadrature from e calibrated dial. Nulling by audio tone.
In-phase ± ISO*; quadrature ± 40X. Shipping weight
10-40 seconds depending on slgni strength.
Operating temperature range —40 to 50* C.
Operating controls
Power Supply
Dimensions Weight
Instrument wppJItd with
ON-OFF switch, battery testing pt button, station selector, switch, volume control, quadrature, dial ± 40X. Inclinometer dial ± 1501
6 size AA (penllght) alkaline cells, Ule about 200 hours.
42x14x9cm(16x5^xX5lnJ i.6kg(3.5lb*4
Monotonlc speaker, carrying cas manual of operation. 3 station set plug-In tuning units (additional In quendea ere optional), set of bell
4.5 kg (10 UM.)
tesjr of Newfoundland 6 Labrador Corp. Ltd.
Ann olVLF SignalsCoverage shown only lor well-known stations. Other reliable, toffy operational stations exist. For lull MormaUon regarding VLF signals In your area consult Geonic* Limited. Extensive We/d experience has proved that the circles ot coverage shown are very conservative and ate actually much larger hi extent.
EM 16 ProHle over Lockport Mine Property, Newfoundland illonal case Nstories on request
horizontal coil
T T"T10 - O * IO
ilatlon Selectori tuning units can be plugged one time. A switch selects r station.
Receiving Colls Vertical receiving coil circuit in Instrument picks up any vertical signal present. Horizontal receiv ing coll circuit, alter automatic 80* signal phase thill, leeds signal Into quadrature dial In series wtth the receiving coil.
In-Phase Dialshows the tilt-angle of the Instru ment lor minimum signal. This angle Is the measure ot the vertical In'phase signal expressed In percentage when compered to the horizontal Held.
Quadrature DialIs calibrated In percentage mark- Ings end nulls the vertical quatf- raiure signal la the vertical coN circuit.
sleeting e suitable transmitter station as a source, the [16 user can survey with the. most suitable primary field
f EM 16 has two receiving coils, one for the pick-up of the ontal (primary) field and the other for detecting any lalous vertical secondary field. The colls are thus ortho-
Llonal. and ara mounted Inside the Instrument "handle".
' actual measurement Is done by first tilting the coll I^f*mWy lo mml(nlu the signal In the vertical (signal) coll and
t further sharpening the null by using the reference signal Tick out the remaining signal This la done by a calibrated
The tangent of the till angle Is the measure of the vertical In-phase component and the quadrature reading Is the signal at right angles to the total Held. All readings are obtained in per centages and do not depend on the absolute amplitude of the primary signals present
The "null" condition of the measurement Is detected by the drop In the audio signal emitted from the patented resonance loudspeaker. A lack is provided for those preferring the use of an earphone Instead.
The power lor the Instrument Is from 6 penllght cells. A battery tester la provided.
42J*IIEM1I 2.9361 KIPLING900
Mining Lands Section
Control Sheet
File No
TYPE — PURVEY lX GEOPHYSICAL
.X GEOLOGICAL
GEOCHEMICAL
EXPENDITURE
MINING LANDS COMMENTS:
Signature of Assessor
Date
Ministry of Natural Re es
Ontario
Report of Work(Geophysical. Geological. Geochemical and Expenditures)
Mining Act
Instructions: — Please type or print.— If number of mining claims travel sect
exceeds space en this form, attach a list. Note: — Only days credits calculated in tne
"Expenditures" section may be entered in the "Expend. Days Cr." columns.
— Do not use shaded areas below.Type of Survev(s)
Am Hel/Lf -*
Townshipor Area
Claim Hblaer(t)
i /Y,/-~f~l
Prospector's Licence No.
^Q^- t?Survey
Name and Address of Author (of Geo-Technical report)
Date of Survey (from 81 to)
Or//
Mo. l Yr~mTotai Miles of line Cut
! /
Credits Requested per Each Claim in Columns at rightSpecial Provisions
For first survey:
Enter 40 days. (This includes line cutting)
For each additional survey: using the same grid:
Enter 20 days (for each)
Man Days
Complete reverse side and enter total (s) here
Airborne Credits
Note: Special provisions
credits do not apply
to Airborne Surveys.
Geophysical
- Electromagnetic
- Magnetometer |
- Radiometric
- Other
Geological
Geochemical
Geophysical
- Electromagnetic
- Magnetometer
- Radiometric
- Other
Geological
Geochemical
Electromagnetic
Magnetometer
Radiometric
Days per Claim
f/
3*0
Days per Claim
Days per Claim
Mining Claims Traversed (List in numerical sequence)
Expenditures (excludes power stripping)Type of Work Performed
Performed on Claimd)
Calculation of Expenditure Days Credits
Total Expenditures
' -5- 115
Total 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.
Mining ClaimPrefix
eNumber
1*1-773
9 1*9/0
*-VK-juy
Expend. Days Cr.
Mimng ClamnPrefix ! Number
**m JUM i••^ . Jfrl———————"M "
Exoenc. J Days C- ;
i
RECEIVED
NG LANDS
Total number of mining claims covered by this
Certification Verifying Report of Work1 hereby certify that 1 have a personal and intimate knowledge of the facts set/brth in the Repon of Work annexeoTTereto. 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
M4tf /f r c f? /^/tftf^/Z O ^ /.
UDate Certified
Ministry ofNorthern Developmentand Uinas
Order of
tileOntario
Mining Act
Room G610- "h't""V Block Queen's Park Toronto. Ontario M7A1W3 416/96S4888
In the matter of mining claims:P 825792, et al ,
In the Township of Kipling
as listed on Report of Work
1174.
Don HillierOn consideration of an application from the recorded holder, ————under Section 77 Subsection 22 of the Mining Act, l hereby order that the time for filing reports and plans in support ofGeophysical (Electromagnetic^ Geological____assessment work recorded cm June 2,______1986——
he extended until and including' September?, 1986
list, o-)O*t* Signature of Director. Land Msnagamant Branch
Copies:
Don Hillier General Delivery Connaught, Ontario PON 1AO
Mining Recorder Timmins, Ontario
Maurice HI board Cedar Hill Connaught, Ontario PON 1AO
Henry HutterlA- 8 Strachan AvenueP.O. Box 1256South Porcupine, OntarioPON 1HO
1333(85/12)
INGAMAR EXPLORATIONS LIMITEDCEDAR HILL CONNAUGHT. ONTARIO Pt* 1*0
TCL (70SI.00 0501 .M705, 433 3021 7-^ (735, 363.3100
oc7oi5oa 363-4267
August 20,
otf Natural Whitney Block, Room Queen'4 PaJtk Toronto, Ontario M7A 1W3
ATTENTION: E. P. AMPERS0M, P^ Loncf Afcinagement BAraneft
SUBJECT: GEOLOGICAL S ELECTROMAGWETIC SURl/EV REPORT on -tne K4.pf.-ing Township Kaolin/ Si&ica. Sand
Enclosed kmewith ate. two cop-te* o^ -tne above AepoA-t. At4o included ate. copies 0& the. voonk
and signed nup4.
Ingama* Ex.ploMvti.onA Limited Kaolin oi CanadjtC Inc..
End.
SANBORN TWP. M-1088
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_________LEBENP
HIGHWAY AND ROUTE No OTHER ROADS\ TRAILS *SURVEYED LINES
TOWNSHIPS. BASE LINES. ETC -LOTS. MINING CLAIMS. PARCELS. ETC
UWRVEYED LlNBS. - LOT LIN*S
PANCELBOVNOARlMlW i*O CI AIMS ETC.
RAILWAY AND RIGHT O* WAV UTILITY LINES NON PERENNIAL STREAM FLOODING OR FLOODING RIGHTS SUBDIVISION OR COMPOSITE PLAN RESERVATIONS ORIGINAL SHORELINEMARSH OR MUSKEG t^*~, MINES TRAVERSE MONUMENT -
DISPOSITION OF CROWN LANDS
TYPE OF DOCUMENTPATENT. SURFACE ft MINING RIGHTS .
.SURFACE RIGHTS ONLY......" . MINING RIGHTS ONLY ___.
LEASE SURFACE tt MINING RIGHTS..." . SURFACE RIGHTS ONLY........" . MINING RIGHTS ONLY___—.
LICENCE OF OCCUPATION .———-... OROER-IN-COUNCIL .,.~-..—..—,... RESERVATION .__.-..—_..........CANCELLED ____.__.......^^.SAND li CRAVf L ——.,-.———™..-.
SYMBOL
MIMINO MIOHT* IN fANCIl* P ATI NT! O PNIOM TOMAV t. 1*1*. VISTfD IM OMtaiNAl PATIMTCC *V T H* PUBLIC LAND* ACT. N4 O 1*JO. CHAT 100. MC. O. AU Ml C 1.
•NOTES-
400* surface right* rtstrvatton along th* thartt of oil laktt and rivvrt. .
Mlftlncik ing t/under
I97Cection 49)
titleMM*
Js tiND 8 GRAVEL
l W i'.f V
tHAVCL
141,9 A- o
2^60
me levitflU •K*l
ritet t t
Jo
SCALE; 11NCH - 40 CHAINS
MfT AM
-* .r
S IttO* JODO' MKMt (IKMl
- ' ACRES HECTARES
f
t l'' i
4' ' \
TOWNSHIP OF
/KIP
DISTRICTCOC H RANI
MINING DIY1SIOI
*' A-
JUM 05
9M. N•r
Ontario
Natural, Resources Branch
,* i.." i
V
ST*-.
Spruce
Mned ock /Spruce
Forest
600 N
)3
Spruce
Spruce
300 N
Base Line
300 S
600 S
13 ^5^482 ) Alders
Scr-ce
Sjrjce
^Spruce
± .
Sorice
;f r ,ce
Oo o
o*
IO
o o o
o•*-ro
oo
oo6
Ulo o
Ulo o(VI
Ulo o*
IO
Ulo o
Uloo
4
i-
13yC. . .^x * -
825811 ' -ljl Sgruce/Jackpine* .—'' ^ " ^~ '
^.- —— '- ^
Spruce ~"
Mixed Forest
lil OO*
tO
UJ o o
lil o o*
CD
Ulo o*o*
o o
t 6O O
UJo o
600 N
300 N
Base Line Az. 84 0
3OO S
60U S
900 S
LEGEND
PhanerozoicCenozoic
P etstccene end Recent
\-2
Mesozoic
C'etuceous
Mattagarri( Formation: kaolinitic quartz sand, fireclay, clcy, (ignite
Precambrian
Archeangneiss
x X
SYMBOLS
Interpreted Contact
Outcrop
Small Outcrop
Claim Post {located,assumed)
Approximate Location of Sonic Drillhole
River
Creek
Old Drill Road
Steep Slope
Pond
Swamp
Fo rest consists cf spruce, poplar ±]cckpine
SCALE
200
KAOLIN OF CANADA
KAOLIN/SILICA SAND PROSPECT
KIPLING TOWNSHIP, ONTARIO
GEOLOGICAL SIRVEYProject No
Scale- t cm ^ 25m
No
Twp/Arta Kipling
Drown; H.P.M.
Date May
INGAMAR EXPLORATIONS LTD
600 N
8^25807
300 N
Base Line
300 S
6OO S
o*.-* O*: 0*0tt
-X- x* o*.- 1
/'
0*0
o*;- 10*0
of44 :
0*0
0*0
600 N
i 4
825808
M0*0
coo
! lO
o*.-'
o* -
O'
^ o*: (
0*0
c *C
**2
'•2*0t t- (
Oo-f- (O
o o*
IO
o o
o o*
K)
Oo•l-
CM
Oo
o o
Ulo o
Ulo o•*-
CM
Ulo o•*
10
UJo o
Uloo•* IO
•/i*
o o o
o•fr OD
— l '
l- \ -lfa x-5 + i- 9 i
II42J*TICMU 2.9361 KIPLING
300 N
Base Line Az 84 0
300 S
l
600 S
900 S
\
LEGEND
STATION SEATTLE, WASHING TON ( Z4 8 kHr )
CONDUCTOR
ATJRE
IN PHASE
SCA^E C OR EM READING
CLAIM POST (LOCATED,ASSUMED
RIVER
CREEK
CLJ DR.LL ROAD
STEEP SLOPE
SCALE
_i _ ^—50 100 150
METRES
200
J 7 31* l
KAOLIN OF CANADA
KAOLIN/SILICA SAND PROSPECT
KIPLING TOWNSHIP, ONTARIO
VLF Sl'RVEYProtect No
Scale, l cm : 25m
Drawing NoHP.M
Dafe May , 1986
INGAMAR EXPLORATIONS LTD
