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Lakeview PropertyBernhardt /Teck Twps.
NTS 42 A/1 80 0 04'W 48"11'N
RECEIVED8.7
MAR 2 5 2002
GEOSCtENCF ASSESSMENT OfFICE
Prepared By:Eric Marion
42A01NE2043 2.23250 BERNHARDT 010
INDEX
Property Location................................................................................................................3
Access.................................................................................................................................^.
Previous Work.,....................................................................................................................?
Present Work..................,.....................................................................................................?
Results............................^
Conclusions.........................................................................................................................^
Readings -E-W Lines..................................................................................... .........9, 10, 11
Readings - N-S Lines....................................................................................... 12, 13, 14, 15
Magnetometer Specifications... ........... ............ ............ .......... ........ .............. ............ ...........ii
FIGURES
Fig-1 - Location.................................................................................................................!
Fig-2 - Claim Map............................................................................................................^
Fig-3 - Geology (general)..............................................................................-...-.-. .........4
Fig-4 - Claim Area Geology - Bernhardt Twp..................................................................5
Fig-5 Claim Area Geology - Teck Township........... ......................................................6
IN BACK POCKET
Magnetometer Survey Compilation fc Profiles - E-W Lines
Magnetometer Survey Compilation Se Profiles - N-S Lines
EDITION 3 42 A/1
05
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The centre of your map is in: Division: Larder Lake Township: TECK G-Plan: G-3719
Marchl7,2002pg1of2
PROPERTY LOCATION
The property is located in the Larder Lake Mining Division approximately 3.5 kilometers north of the town of Kirkland Lake.The claims straddle the Teck-Bernhardt twp boundary between the two and three mile post mark and extend into each township about eight hundred meters.This property lays amongst the many arms of Amikougami Lake which gives good access to much of the property.This area is in the Kirkland Lake Resident Geologists District and can be found on NTS 42 A/1 with the geographic center being at approximately 80 04 W and 48 11 N.
ACCESS
Heading north from Kirkland Lake on Goodfish Road for 6 kilometers will bring you to a gravel road Continuing north on this road for 5 kilometers brings you to a logging road heading west. Following this for 6 kilometers will bring you to Lancaster Lake where a boat can be launched.Heading south by water for l .5 kilometers will bring you to the northern border of the property.
CLAIMS
This property consists of 4 contiguous staked mining claims totalling 10 claim units, recorded on Plan G-3719 of Teck Twp. and Plan G-3207 of Bernhardt Twp. The claims are as follows: CL#1206262 -4units, CL#1206409 -l unit, CL#1206410-1 unit, and CL# 1225873 -4units.
GEOLOGY
This area is in the southern Kinojevis Assemblage of the Abitibi Greenstone Belt. The rocks are predominantly greyish green to dark green pillowed and flow tholeiitic basalts. The Blake River Group, a series of mostly calc-alkaline rocks are mapped as occuring five kilometers to tl e north of the property. There are many strike and cross fat Its in the area as indicated by ODM map 2193. Several gabbroic or dioritic mafic intrusives are mapped as occurring in the area and on the claims.The Winnie Lake Stock, a 4 kilometer wide somewhat circular granitic intrusive occurs approximately 3 kilometers due west of the claim area. The Kirkland Lake Main Break, a prolific gold bearing splay of the Larder Cadillac Deformation Zone, with an average strike direction of 065 0 , is located less than four kilometers due south of this claim group, hosted within structurally deformed, altered and intruded fluvial sediments of the Temiskaming Group.Most of the gold mineralization in the area appears to be structurally controlled, intrusion related, hydrothermally focused vein type occurances.
LS.fENSEN
ProterozoicKeewmnawan diabaw (not shown)
12 Cobalt Group Arcnaan
Matachewan diabase {not shown) Granitic rocks
11 GranodioritB, monzonite, quartz monzonite,syenite
10 Mauiv* to gneissic quartz diorite, tonalite, trondhjemite
Upper Supergroup9 9a* Timiskaming Group, 9b*" Deitor-
Porcupine Complex 8 8a,8n, Blake River Group, Se*** Blake
River (Upper Fm.. Tisdale Group)
7*. 7b, Klnojevis Group, 7c Klnojevis Group,(Middle Fm., Tisdale Group)6* Larder Lake Group, 6b StoughtonRoquemwire Group, 6c Lower Fm^ TisdaleGroupSe Porcupine Group
Lower Supergroups4 4a Skead Group, 4b Hunter Mine Group, 4e
Upper Fm., Deloro Group 3 3a Catharine Group. 3c Middle Fm., Deloro
Group 2 2a Wabewawa Group, 2c Lower Fm. Deloro
Group 1 U Pacaud tuffs""
*a refers to Kirkland Lake Area, south limb of synclinorium (Jensen 1978c, 1979)."b refers to Kirkland Lake Area, north limb of synclinorium (Jansen 1976.1978b)." c refen to Timmini Area {Pyke, 1980). *" (Goodwin, 1965).
Figure-3 - General
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4 ^T*w*fl dflM *tf *^**i4f*T 40gbmT'i*ri4tCi'i mtf kVfL.Ji V Dft-fM: (-***tJj-T (V*et*** tta-tfjc gr inoif }^|jc forf fl^clB^
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Figure-4 - Claim Area Geology :Bernhardt T\vp
HON. LESLIE M. FROST, Minister o} Mines
H. C. Rickaby, Dep 'linitster M. E. Hurst, Provincial Geologist
Adjoins Black River Area Map No. 30c
"
-'.' -' l-'-
-- ' ,- .'
//;.; ^•/1— — ^-^^^-\Figure-5 - Claim Area Geology :Teck Township
PREVIOUS WORK
Considering the proximity to the many historic mines just south of here, undoubtably many individuals prospected this area during the many boom eras of mining and exploration in the Kirkland Lake Gold Camp. In spite of this, there is very little submitted or reported exploration work on these claims. Several old pits and trenches on the property would indicate some prospecting activity, but no records of this work could be found.No records of any ground based geophysics ever being performed on any of the claim area prior to the author's programs were located.
Yellowknife Bear Mines drilled a program of five short holes in the region of the north-east arm of Amikougami Lake in the 1960's that did not report encountering anomalous values. Some of these holes broke into the lake bottom before going very deep and judging by placement and direction of the drill holes, that they broke into the lake would indicate N-S faulting on either side of the rock islands 600 meters due south of the rock islands in the present grid area. These features should cross this area if they continue on strike. From the information submitted, it is undetermined as to what the target of the drilling program was at the time.
Tlie author of this report has been actively prospecting in this area for some time now and has conducted line cutting ,VLF surveys, stripping, trenching ,sampling and some mapping.Most recently efforts have been directed towards a virtually untouched area of the claims, the vast areas covered by the waters of Amikougami Lake. Though the location limits the timing and type of prospecting, it is still possible to define significant features and track them to shore or target them for winter drilling when ice conditions allow.
PRESENT WORK
During the first quarter of 2001, approximately 880 magnetometer readings were taken on 5.5km of re-established grid ,which was chained and picketed at 25m,with lines oriented N-S at 50meter spacing apart .During the first quarter of 2002, an additional 2 km of grid was chained and picketed at an E-W orientation, on which an additional 335 readings were taken. This was done to get some sort of magnetic correlation of anomalous features defined by previous geophysical (VLF) work done during the winter of 1999-2000.Because of adequate control points,both subsequent re-establishments of parts of the grid are accurate to within plus or minus 2 meters. A magnetometer survey was done over the grid, taking readings of the vertical component of the magnetic field every 6.25meters, using a fluxgate type,Scintrex 321 Model MF-1 Magnetometer.
RESULTS
Upon profiling, the most striking feature defined by the magnetic surveys is an average 20 meter thick dyke-like body which is present from L-2+OOW at 8+25N through to L- 1+OOE at 9+25N dominating the south-west part of the grid. The anomaly is averages about 800 gammas above background and peaks at 1700 gammas above background on L-0+50W at 9+OON.
The tilt and shape of the anomaly profile suggests that the body dips to the north. This feature coincides almost identically with a very strong VLF conductor axis previously interpreted as a dyke like VLF response. The westward continuation of this anomaly has yet to be ground located on shore but this could be done with or without ice on the lake. It would appear though, that in the area where one would extrapolate the continuation in this direction that it does not outcrop, but would lay in an overburden covered trough. The eastern direction of the anomaly appears to be truncated or butt up to a possible fault(dyke) feature that somewhat follows N-S along L-1+50E. Viewing the mag-survey E-W profiles, one can perceive a N-S "break" in this area which shows up as a narrow slightly higher mag " ridge". This may indicate possible later intrusion along this N-S "fault" feature. The anomaly was not detected east of this feature possibly indicating further displacement than the grid area covers.A three line mag anomaly of undetermined cause, which runs from LO+50E at 8+50S over to L1+50E at 8+OOS, has no associated conductor typeVLF-EM response and has a suggested dip to the south.
As to what the anomalies actually are, one can only speculate. The average strike of about 48 0 tends to be outside the typical N-S orientation of the generally more magnetic "Matachewan" type diabase intrusive dykes common in the region. That the unit does not outcrop may indicate preferential erosion of a softer, possibly syenitic rock,( which can be more magnetic) also common to the area.
CONCLUSIONS
Barring getting an outcrop exposure further along strike of the "A"anomaly, the only way to positively identity the cause would be to core a drill hole across it,or into it. To get immediately over the target would require a hole drilled from north of the axis on the ice in winter time. Drilling an angle hole from on the rock peninsula paralleling the anomaly about 50 meters to the south would possibly take excess footage to cross the target (if at all) as the target would be dipping away from the collar area. Perhaps prospecting down ice along the rock peninsula for magnetic rocks may encounter locally derived tallus which could assist in determining the cause of the magnetic anomaly More assesment and consultation will be required before a definite plan of action can be developed.
Magnetometer Readings : E-W Lines
Meterage L-9+OON L-10+OON L-11+OON L-12+OON
2+50W 4400 -—— 4400 4375 4375 4400 4375 4375 4375
2-K)OW 4375 —— 4375 4375 4375 4375 4375 4375 4400
1+50W 4375 —— 4400 4375 4400 4375 4375 4375 4375 4400 4375 4450 4400 4500 4375 4575 4350
1+OOW 4600 —— 4300 4625 4225 4775 4225 4825 4200 5000 4200 5100 4200 5250 4200 5425 4200
0+50W 5625 —— 4200 —— —— 5750 4200 5650 4200 5450 4225 5300 4225 5175 4300 5200 4350 5100 4375
0+00 5000 ~~ 4375 -- 4400 4825 4400 440048CO 4400 4400 420C 4700 4400 4400 4200 4700 4400 4400 4200 4600 4400 4400 4300 4600 4400 4400 4375 4600 4400 4400 4375
0+50E 4600 —— 4425 ~— 4400 —— 4400 4600 4425 4400 4400 4600 4425 4400 4400 4625 4450 4400 4375 4700 4425 4400 4225
4400 4425 4200 4400 4400 4200
4775 4400 4500 4200
Magnetometer Readings : E-W Lines
Meterage
l+OOE
I+50E
2-KJOE
L-9+OON
47754775477547754800477547504625457545004450445044504425445044504450445044254425
2+50E
3+OOE
3+50E
4-fOOE
L-IO+OON
44004400440044254500457545754550450044504400437543504300430043004300435043004300430043004250425043004250422542254225422542504250430042504300430043004250425042254225422542004200420042004200420042004200417542004200420041754200
L-II+OON
45004500450045004500450045504575457546004600460045754550450044504450442544254450442544254400442544254500450045004500455045504500450045004500450045754600
460046004600450045004500450045004500450045004500457545004575450044004400
L-12+OON
42004225422542254300430042504300422543004300440043754275425042254225422542254225422542254300420043004375430043004225422542504300430043004300430043004300430042504250422542504225422542254225422542254225422542254225430043004350
10
Magnetometer Readings : E-W Lines
Meterage
4+50E
L-9+OON L-IO+OON
4200
L-II+OON
5+OOE
4400440044254450445045004575457545504500450044254425
L-12+OON
43754375435042004225422542254225420042254300
5+50E
11
Magnetometer Readings * N-S Lines
Meterage L2+OOW L l +50W L I +OOW LO-50 W LO+00
IO+50N
41754200420042004200420042004200
10+OON
4225430043004350430043754400
9*50N
9+OON
8+50N
8-KXJN
422542404225422542254225430043754400460047755000522554255500542553005175
440044004425442545754625482550005 1 00515050254875
4250425043004350437544004425445045504600475048255000505052oo5225495046254500
44504450450045754600465048255175557561755900550051754800
440044004400440044004400440044504600480049755100520052005000477545004500437542254225422542254225422542254225422543004300430042254200420042004100410040253800
3800 12
Magnetometer Readings : N-S Lines
Meterage
I3+50N
LO+50E LI i GOE LI+50E L2+OOE
13+OON
12+50N
12+OON
11+50N
111OON
10+50N
10-K)ON
4400440044504400450045004500457544254425440044004375440044004400435043754375430043004300430043004300435043504300437543754400440044004400445045004500450046004600
44004425442544004400440044004400440044004400440044254425442544004500450045004500450045004400442545004400440044254500450045004450442544254425442544254500442544254425450045004500450043004500460045004600460046004600
4400 4400437543004300430042504225422542254225422542254225422543004300430044004400437544004400440044004425442544004425440044004425442544254425450044254500450045754575460046004600460046004575465045004425440044004400440044254600
4400442545004500450045754575450045004450450044504400442544504500455046004600460045004425445045004425460046004600460046004600460046004600460046004400440044504500450046004600460046004600460046004425442544004400
43004300440044004400440044004400437544004400437544004400440044004400437543754400440044004400440044004400440044004400440044004400
13
Magnetometer Readings : N-S Lines
Meterage LO+50E
IO+50N
9+50N
9+OON
8+50N
8-KJON
4600460046254625465047754775482550005000500050005000495048004625460045754500450044004400440044004400440043504375430043004300430043004400445046004800485050004600
7+50N
Ll+OOE
460046004600462547754775477547754800500050005025510051005000500049004800477546504600460046004600450044254425440044004425460048505000497548254700460046004600455044254400440044004350
7+OON
L1+50E
46254600460045754575457546004600460046004600455046004600450045004500450045004500442544254400440044004400440046005000517551004950480046754775462545754575450045004425442544254425442544254450455045004450
L2+OOE
4500460046004600460046004600460045004600460046004575457545004425440044254400440044004300430043004200410039004000390040004200420042004200420042004250
L2+50E
4375440044004400437544004400
14
Magnetometer Readings : N-S Lines
Meterage L3+OOE L3+50E L4+OOE L4+50E L5-K)OE
13+OON
I2+50N
12-KJON
11+50N
Il+OON
10+50N
10+OON
417541754175417541504175417541754 J 7542004200420042004200420042004200420042004200420042004200422542254250422542254250430043754375430043004300425043504250422542254225420042004200420042004200
4000 40004000400038253900390038503800380038003800380038003800380038003900390040003950400040004000405041004100417542004200420042004200420042004200420041754175417541754200417541004175
4450 4500 4500 4500 4600 4600 460045754500450044504425442544254425442544504400440044004400440044004450445044504450450045754575457545754575460046004600450045754500450045754500450044504450440044004400440043754375
4375 4375 4375430043754375437543754375437543754375437543754375437543754375437543754400440044004400440044004400440044004375440044254500450045004425437543504250422542004200420042004200
4425445044004375440044004400440045004600460046004600460045504600460046004575450044254400440044004400
9+50N15
BIBLIOGRAPHY
-ODM REPORT 84Geology of Bernhardt and Morrisette Twps
R.J. Rupert and H.L. Lovell
-GEOLOGY OF TECK TWP. Map No. 1945-1
Compiled by Jas. E. Thomson
-ODM VOL 57 PART 5Geology of Teck Township and Kenogami Lake Area
Jas E. Thomson 1948
MF-1 FLUXGATE MAGNETOMETER
A first order fluxgate type vertical com
ponent magnetometer. Advanced transis
torized circuitry and extensive temperature
compensation is the core of its accuracy
comparable to precision tripod mounted
Schmidt type magnetometers.
It is a hand held instrument and needs
only coarse levelling and no orientation.
Features such as direct reading of gamma
values and the possibility of accurate zero
setting at base stations ensure simplicity
of operation and higher field economy.
The Model MF-1 Fluxgate Magnetometer is designed for accurate ground surveys in the mining industry as well as a basic
component for air surveying by small aircraft Technical data and comparison charts available on request.
SPECIFICATIONS
20 |ammw.ftwTT ni!* iByltlcmJ on 1000 nmrni MAXIMUM RANGEt . . * 100,000 gammasi. IATITUOE A^gTMENT RANGES. ' 10,000 to 75.000 gammas, Northern
' convirtlblj to;10,000 to 75,000 gonmai, Southern hemiiphtra
: or * MW) {arnott tquitorfi).BATTERTCASO 7*14*118" ;
WEIGHT. (INCLUDING BATTERY CASE 9 to.BATTERIESi 12 Flashlight Battirfas ("C" call).
MINISTRY OF NORTHERN DEVELOPMENT AND MINES
Transaction No:
Recording Date:
Approval Date:
Client(s):164694
Survey Type(s):
W0280.00525
2002-MAR-25
2002-JUN-28
Work Report Summary
Status: APPROVED
Work Done from: 2001-JAN-01
to: 2002-MAR-22
MARION, ERIC JOSEPH
LG MAG
Work Report Details:Perform Applied Assign Reserve
Claims Perform Approve Applied Approve Assign Approve Reserve Approve Due Date
L 1206262 S2,866 S2.866 SO SO S380 380 S2.486 S2.486 2003-APR-24
L 1206409 SO SO 3380 S380 SO O SO SO 2003-APR-24
32,866 S2.866 S380 3380 S380 S2,486 32,486
External Credits:
Reserve:
so
32,486 Reserve of Work Report*: W0280.00525
32,486 Total Remaining
Status of claim is based on information currently on record.
42A01NE2043 2.23250 BERNHARDT 900
2002-Jul-04 10:23 Armstrong-d Page 1 of 1
Ministry ofNorthern Developmentand Mines
Date: 2002-JUN-28
Ministere du D^veloppement du Nord et des Mines Ontario
GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5
ERIC JOSEPH MARION 126 DUNCAN AVENUE KIRKLAND LAKE, ONTARIO P2N 1Y5 CANADA
Tel: (888) 415-9845 Fax:{877) 670-1555
Dear Sir or Madam
Submission Number: 2.23250 Transaction Number(s): W0280.00525
Subject: Approval of Assessment Work
We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.
At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.
The revisions outlined in the Notice dated June 11, 2002 have been corrected. Accordingly, assessment work credit has been approved as outlined on the Declaration of Assessment Work Form that accompanied this submission.
If you have any question regarding this correspondence, please contact LUCILLE JEROME by email at [email protected] or by phone at (705) 670-5858.
Yours Sincerely,
Ron GashinskiSenior Manager, Mining Lands Section
Cc: Resident Geologist
Eric Joseph Marion (Claim Holder)
Assessment File Library
Eric Joseph Marion (Assessment Office)
Visit ourwebsite at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:17222
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MINING LAND TENURE
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General Information and Limitations . .pawn*, i Hilt, MHniiHtt. rlglt Lri*^i h r*adhf( iipMi,liaiMiH, W DEn*rTarm* 4r^4|!iiJ*]rt arrhjtilt nri Intanrt flora di Ciom. Aim trtrin Iwttf tamrp on* tond inn (but rii*fcr*i pro MM frit HVyli Mihe raining clrin*may ncl h* HU*T
Date V Tim o of Issue May B 2001
TOWNSHIP/AREA
BERNHARDT
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PLAN
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