mineral expl proj 1999 geophys & geol survs … · mat was borrowed from the mndm in kirkland...

\\'assennar Properly Strathcona Twp. 2.20529NTS 31 M/4

31M04SE2007 2.20529 RIDDELL 010

MINERAL EXPLORATION PROJECT 1999 WASSENAAR PROPERTY

Strathcona Township

Geophysical Surveys Magnetometer, VLF-EM, Induced Polarization, Beep Mat

Geological Surveys Geological Mapping and Prospecting

Sudbury Mining District, Ontario

RECEIVED

SEP 1 5 r:iGEOSCIENCE ASSESSMENT

OfFICE

Meegwich Consultants Inc. Box 482 Temagami. Ont. POH 2HO tel (705)569-2904

ff/7/ew Wassenaar OPAP Final Submission Wassenaar Pr.nnertv Strathcona Twp.

TABLE OF CONTENTS

INTRODUCTION:Page

CO H 1O O

Property LocationAccessProperty DescriptionSummary of Work Done

PROSPECTING SURVEY:

IntroductionBeep Mat ProspectingProspecting

GEOPHYSICAL SURVEYING:

Magnetometer SurveyVLF-EM SurveyI.P. SurveyConclusions and RecommendationsInstrument specifications MagnetometerInstrument specifications VLF-EMCertificate of AuthorReferences

456

7891112121314

toU)

lf

O H OO

LIST OF FIGURES

Figure l Figure 2 Figure 3

Location Map Claim Map Geology

LIST OF MAPSMAP l Prospecting and Compilation Map MAP 2 Total Field Magnetic Contour Map MAP 3 VLF-EM Profile Map MAP 4 I.P. Pseudo sections L 550 W, 300 W, 50 W and O

Mecgvvich Consultants Inc. Box 482 Temagami. Ont. POH 2HO lei. (705)569-2904

\V\\lemWassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

APPENDIX I

Geological Mapping Report- A.W. Beecham consultant Dec 1999.-report and geology map (pond area)

APPENDIX II

Assay Certificate

Meegwich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904

MANITOBA,,''

X

ONTARIO

QUEBEC

TIMMINS-

.SAULT

,STE. MARIE O

.SUDBURY

TEMAGAM l

AREA

150ml

200 Km

FIGURE l '. LOCATION MAP TEMAGAMI PROJECT

PROPOSED ZONE 2 GRID

I23I4ZI'I (EXISTING)

-•A—,-~. ~

CLAIM fc GRID LOCATION MAP

WASSENAR PROPERTY,V -/tftJii

STRATHCONA TP

U'illem Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

Property Location:

NTS: 31M/4Township: Strathcona (Upper Twin Lake)Mining Division: SudburyResident Geologist: Cobalt/Kirkland Lake - Gary GrabowskiLatitude: 47-00-00Longitude: 79-46-00Nearest town: Temagami (7 km to the north-northwest)

Access:

The property is situated 7 km south-southeast of Temagami as the crow flies Access to the claims is by traveling eastward on a logging road departing Hwy 11 about 10 km south of Temagami where the Trans Canada Pipeline crosses the highway. At a point 4 km east of the highway an equipment trail (where a backhoe has traveled) winds in another 300 meters to stripped showings which was the central area of detailed gridwork, geophysics, geological mapping and comprehensive sampling ( Zone 1).

Property Description:

The property consists of a group of 14 contiguous claims for a total area of 830hectares (54 units of+/-16 hectares). The claim numbers of the property are asfollows:1191010 16 units 1140888 4 units1191002 l unit 1191004 l unitl 191005 l unit 1191006 3 unit1191007 3 units 1191008 l unit1076960 l unit 1076969 l unit1076974 l unit 1231421 5 units1140887 4 units 1191009 12 units

Summary of Work Done:

Basically the northwest corner of an 830 hectare property was covered with a detailed grid pattern with line spacings of 25, 50 and 100 meters. 14.50 km of line was chainsawed and picketed at 25 meter intervals. Magnetometer and VLF-EM covered the entire grid. I.P., Geological, Beep Mat and Prospecting covered


ll'illem IVassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

areas that are considered high priority for followup from the current Mag/VLF-EM survey and previous geological work.

Totals Dates Preliminary kmLinecutting 14.50 July 1-25,1999 Magnetometer survey 13.90 Aug. 15-22, 1999 VLF-EM Survey 12.90 Aug 15-22, 1999 DetailedGeological Survey 4.00 Nov. 14,15, 1999 Prospecting 3.00 May 23, Aug l, 1999 Beep Mat Survey 5.00 Oct 23,24, 1999 I.P. Survey 2.425 Dec. 17

The primary objective of the program was to outline and explore for significant gold mineralization over Zone 2 where a 59 g/tonne assay was picked up and also to do Phase Two followup (I.P.) over the anomalous base metal Zone l. The results of the surveys have indicated drill targets near Zone l. The results over Zone 2 are not as conclusive at present however there are faint indications of a zone trending east to west.

Zone l should be drilled for a base metal deposit while Zone 2 should be only x-ray drilled for more geologic information and to test for continuity of the high grade gold occurrence. In total there are 5 drill targets based on thorough surface work funded by the applicant and the OPAP program.

Thanks to the OPAP program the option status of the property has been moved along to the drill stage.

Meegwich Consultants Inc. Box 482 Temagami. Out. POH 2HO tel. (705)569-2904

ll'il/eni H'assenaar OPAP Final Submission Wassenaar Propertv Strathcona Twp.

Beep Mat Surveying and Prospecting ReportWassenaar Property

Strathcona Twp.


Willeni Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

January 04, 2.ooa

BEEP MAT SURVEYING AND PROSPECTING REPORT

BEEP MAT SURVEY:

Introduction: ^

A beep mat survey was carried out on Oct 23,24 with a travel day on the 22nd and , 1999. The prospectors were Willem Wassenaar, Sy Wassenaar and Siek Wassenaar. The beep mat was borrowed from the MNDM in Kirkland Lake. The objective of the beep mat survey was to explore for sulphide mineral along the length of the conductors picked up by the VLF-EM survey and to prospect in general. There was about 5.0 km covered.

Instrument:

The beep mat i s a mini-EM system with a transmitter and a receiver enclosed in a durable plastic sled about 3 ft in length. When the mat is dragged over a sulphide occurrence by hand the unit will indicate such by a beeping noise. The location of the beeping is then dug up to investigate. It is only successful in area of light overburden cover. This method was successful in detecting the main showing area at O, O on the grid in the past. The sled is dragged across the conductor at right angles at approximately along the length.

The targets surveyed are as follows:

Conductor G: This anomaly was covered with the beep mat with no hits. The west end of the conductor is high and dry while the eastern part of it drops off into a low lying area. While there were no hits from the beep mat there could still be mineralization down past the 5 ft limit of the beep mat. This anomaly should be checked with HLEM.

Conductor H: This feature was field checked for sulphides with no hits. Part of the anomaly lies in a small pond so it was not totally resolved however the land portion has been covered.

Conductor M: This feature lies in a topographic low. It was covered along the full length to the lake from the end of the "boot bay".

Conclusion and Recommendations:

The results of the beep mat surveying were disappointing. There were no significant or 1 ' detectable sulphides encountered. This means there are no occurrences within 5 ft. of surface. A more sophisticated unit such as HLEM should be deployed to investigate the possibility of deeper occurrences. (SEE COVERAGE ON MAP ONE)

Meegwich Consultants Inc. Box 482 Temagami. Ont. POH 2HO tel. (705)569-2904

inilem Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

PROSPECTING SURVEY:

(Only a minor amount of prospecting was done by the applicant due to a heavy work schedule from other commitments). The areas prospected (stripping and sampling) are discussed as follows:

Main showing area Augl:

25 W, 25S Following a property visit by Wayne Benham of Queenston in May 99 it was thought some higher grade samples within chemical sediments with abundant sulphides (chalcopyrite, pyrite, pyrrhotite) near the main showing would indicate a more widespread picture and expand the dimensions of the zone. W. Wassenaar spent Aug l stripping and sampling. Of the 10 samples taken one was assayed at X-RAL Laboratories. A whole rock analysis was done and the more interesting results were 563 ppm Co, 772 ppm Ni and 308 ppm Cu.

Beaver Pond area May 23:

May 23 was spent prospecting a rock ledge on L 550 and 600 W at 300 N. There was gossan staining along the face containing minor pyrite. The rock type was mafic volcanic.

The northwest side of the pond was prospected and a 2 cm quartz vein in diabase containing abundant chalcopyrite along fractures was discovered but not assayed.

(see Map One for areas covered)


Willem Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

GEOPHYSICAL REPORT

Magnetometer/VLF-EM/Induced PolarizationWassenaar Property

Strathcona Twp.


7

IVil/em ll'assenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

Geophysical Surveying

MAGNETOMETER SURVEY^—^^-——-^^——^——^^^^^————

Instrument specifications:;

A total of 13.9 km ( l 150 readings) was surveyed using a micro-processor based GEM Systems GSM-19 Mag/VLF unit. The instrument is capable of +I- 1 7100th of a gamma resolution. The instrument was used in the mobile mode The diurnal variation was corrected for using a base station set up near the grid. This base instrument was an EDA Omnf IV capable of 1710th of a gamma resolution.

Dates of survey:

The survey was done by D. Laronde of Meegwich Consultants Inc. from Aug. 15-22, 1999

Results and Interpretation:

The data set is presented in colour contour format on plans at 1:2500 scale and discussed as follows: Readings were taken at 12.5 meter intervals.

The most obvious feature outlined is a massive high and low combination or di-polar response trending ESE across the north part of the grid. This is interpreted as a concentrated magnetic mineral band, probably magnetite, within a diabase or gabbro intrusion. This feature is linear and might be indicating a lineament or fault. The values on the low side range down to 56,360 nT while the high side range is as high as 58,291 nT.Further to the north and again in the diabase are a few isolated highs and lows that can be again attributed to pockets of magnetite concentrations. Co-incidently there is a drop in topography where the magnetic low trend occurs and a definite east-west lineament flanks the low to the north.

The area around the north part of the pond contains a few isolated highs on L 550 W at 475 N and on L 300 W at 300 N. Also the area between these two highs is elevated in magnetism. A similar situation occurs between L 210 W at 450 N and O at 600 N. These highs suggest the magnetic mineral content of the diabase varies in a massive fashion.

The central part of the grid is fairly uniform with a few outliers of a few hundred gammas.

At the south end of the grid a linear magnetic high runs from L 300 W at 162 S to L 200 E at 75 S. One could interpret a narrow (5-10 meter) dike here. The area to the north of this feature has a very irregular magnetic pattern. Within this pattern however are several subtle possibilities of linears and masses.


8ll'illem Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

VLF SURVEY_____________________________________________

Instrument specifications:

A total of 12.90 km was surveyed (1070 readings) with the same GEM Systems GSM-19 Mag/VLF-EM receiver unit. The transmitting station was Cutler, Maine at 24.0 kHz This instrument measures the in-phase of the vertical magnetic field as a percentage of the horizontal primary field. The resolution is +I- I 07o.

Dates of Survey:

The survey was done by D. Laronde of Meegwich Consultants Inc. on the following dates: August 15-22, 1999. Readings were taken in detail at 12.5 meter stations.


The interpretation of VLF conductors is based on whether or not the source of the anomaly is metallic.

The survey picked up seven new conductors and some very weak responses. The labeling is a continuation in sequence from a previous survey which used the A-F labels on a detailed grid over the 0,0 showing area. The anomalies from this survey are G-M and are discussed as follows:

Conductor G: This weak anomaly is short along strike, 200 m, with the strongestresponse on L 210 W at 120 S. It trends northwest which is the strike of a local fractureset. The source would appear to be non-metallic.Conductor H: This conductor occurs on a lineament marked by a topographic lowtrending due east. This is a strong indication that this anomaly could have a non-metallicsourceConductor I: Anomaly I occurs within the pond and seems to be indicating a nearhorizontal conductive layer such as the sediment in the lake bottom and/or the trend issimilar to H and it could be a continuation. In any regard the source is likely non-metallic.The I.P. survey has confirmed there is no metallic anomaly here so the source is definitelynon-metallic.Conductor J, K and L: These anomalies are in the pond area as well and are not welldefined due to the closeness. Although the location is suspicious for having a non-metallicsource, it cannot be determined from VLF. The I.P. survey did not detect an anomalyover this area.Conductor M: C onductor M is a strong response that runs along a topographic low It has been field checked with a beep mat survey along its length and no mineral wasdetected.

Meegwich Consultants Inc. Box 482 Temagami, Out. POH 2HO tel. (705)569-2904

\VilleniWassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

INDUCED POLARIZATION SURVEY

Instrument Specifications and Survey Configuration:

A total of 2.425 km was surveyed with a di-pole di-pole, 3=25 meters configuration. N 1- 6 was read to better the chances of detecting small pockets of mineralization associated with Zone 2 containing a 59 g/tonne assay. The depth penetration is down to 225 feet or 68 meters. The survey employed the following state-of-the-art equipment:

-an IP T-3 Phoenix Transmitter 3.0 kW-an IP V-5 Receiver (Phase)-a MG-1 Phoenix Generator 2.0 kW

Dates of the survey:

The survey was done by Remy Belanger Geophysique of Rouyn-Noranda, P.Q.. There were seven crew members from the Belanger team and D. Laronde supervised and selected lines based on results at the end of each line. Crew members were Remy Belanger, Carl Belanger, Jean Yves Robin, Mario Robin, Jean-Marc Raymond, Steve Lacourse and Mike Kirovac.


The system is designed to respond to conductive horizons such as inter-connected metallic grains and also metallic grains that are not connected electrically. The latter is the great advantage over conventional EM systems. The results incorporate a resistivity profile that is compared in contrast to the phase profile. Anomalies with a drop in resistivity and an increase in phase are considered priority. There were four profiles or lines done and are discussed individually as follows:

L 550 W

Objective: This line was to test a series of three VLF-EM conductors occurring in or near an east-west trending structure that is thought to be a possible controlling factor in the deposition of a gold deposit. The 59 g/tonne Au assay is on trend.

Results: At 650 N there is a drop in resistivity accompanied by a wide phase anomaly. The peculiar thing about this anomaly is that the phase zone is much wider than the

Meegvvich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904

Willeni Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

resistivity low. The underlying rock is probably diabase or gabbro. Surface prospecting has uncovered some chalcopyrite which may be in this particular feature. The anomaly is probably caused by mineralization which should be followed up. This is a low prioritydrill target.

L 300 W;

Objective: This line crosses over the area of the 59 g/tonne Au assay. The purpose was to define a drill target over this zone. Since disseminated pyrite is a common accessory mineral.

Results: The zone does have a co-incident response centered at 325 N. There is a slight elevation in the phase and also the resistivity. This is not what was expected however it is a response that is over the projected zone. H igh priority drill target.

The north end of the line centered on 675 N is a wide chargeability zone with a wide high resistivity zone which is typical of the underlying diabase or gabbro. This anomaly is a priority target.

L 50 W

Objective: To test the area of base metal mineralized showings on surface for continuity along strike and at depth.

Results: There is a shallow, N^l,2, phase anomaly from 200 S to 100 S. The corresponding resistivity low is in the order of 500 to 1000 ohms/meters. This location is co-incident with the end of a VLF-EM anomaly. There is some correlation to a magnetic high here. Another anomaly, only narrow, occurs at 25 S. This is co-incident with the strike of the mineralized showings. The resistivity response is shallow. These two drill targets are high priority.

LO

Objective: To test the area of base metal mineralized showings on surface for continuity along strike and at depth.

Results: There are two strong increases in phase accompanied by a low in resistivity centered on 150 S and at 25 N. These are encouraging since there are surface showings around 0,0 grid co-ordinates. These are h igh priority drill targets.An increase in phase occurs at 150 N but is accompanied by a resistivity high as well Low priority anomaly.


nH'/Hern Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

Conclusions and Recommendations:^^———^^^^———^—^——^^^^—-^^-^^

Zone 2 (beaver pond area and north half of grid):

The magnetic survey and VLF-EM survey from the OPAP phase of work did not define any massive sulphide bodies. Most of the conductors seem to have non-metallic sources. All the conductors were followed up with I.P. and beep mat prospecting with disappointing results. The surveys over the beaver pond gold zone 2 have faint indications of corresponding responses that are quite marginal at best, nevertheless present in magnetics, VLF-EM and I.P. . Because of the high assay it would still be advisable to at least x-ray drill ( small core, portable drill) for geologic information. The gold zone may be very narrow but high grade enough to be economical.

Zone l

The IP survey lit up four targets to drill on a high priority basis This is encouraging The IP. anomalies flank existing VLF-EM conductor zones with widths up to 15 meters One l.P. response on L 50 W at 150 S may be as wide as 50 meters. Some of the assays from previous work are Cu 4070 ppm, Au, 3.98 g/tonne, Ag 18 g/tonne, Pb 1190 ppm, Zn 8790 ppm, Co 1460 ppm.

There has been enough surface work done geologically and geophysically with the end result of 5 locations to drill test. The holes need only be 300-400 feet deep amounting to a total of 1500-2000 feet. This could be done for about SIS/foot on present prices for a grand total of 522,500-530,000. It is advisable to approach mining development corporations at this time since to finance the drill project.

End

Meegvvich Consultants Inc. Box 482 Temagami, Ont. POH 2HO tel. (705)569-2904

INSTRUMENT SPECIFICATIONS

MAGNETOMETResolution:

Ace u ra c/:

Range:

Gradient Tolerance:

Operating interval:

Input/Output:

Power Requirements:

Power Source:

Battery Charger:

Operating Ranges:

Storage Temperature:

Display:

Dimensions:

ER 7 GRADIOMETER0.01 nT (gamma), magnetic field and gradient.

0.2 nT over operating range.

20,000 to 1 20,000 nT.

Over 10,000 nT/m

3 seconds minimum, faster optional. Readings initiated from keyboard,

external trigger, or carriage return via RS-232-C.

6 pin weatherproof connector, RS-232C, and (optional) analog output.

12 V, 200 mA peak (during polarization), 30 mA standby. 300mA peak

in gradiometer mode.

Internal 12 V, 2.6 Ah sealed lead-acid battery standard, others op

tional. An External 12V power source can also be used.

Input: 1 10 VAC, 60 Hz. Optional 110/220 VAC, 50/60 Hz.

Output: dual level charging.

Temperature: -40 "C to +60 "C

Battery Voltage: 1 0.0 V minimum to 15V maximum.

Humidity: u p to 90"Jo relative, non condensing.-500CtoH-650C

LCD: 240 x 64 pixels, or 8 x 30 characters. Built in heater for opera

tion below -200C

Console: 2 23 x 69 x 240mm.

Sensor staff: 4 x 450mm sections.

Sensor: 170 x 71 m m dia.

Weight: Console 2.1kg, Staff 0.9kg, Sensors 1.1 kg each.

VLFFrequency Range: Parameters Measured:

Resolution: Number of Stations: Storage:

Terrain Slope Range: Sensor Dimensions: Sensor Weight:

15 -30.0kHz.Vertical In-phase and Out-of-phase components as percentage of totalfield.2 componenis of horizontal field.Absolute amplitude of total field.Q.1%.Up to 3 at a time.Automatic with: time, coordinates, magnetic field/gradient, slope, EMfield, frequency, in- and out-of-phase vertical, and both horizontalcomponents for each selected station.O0 - 900 (entered manually).14x15x9 cm. (5.5 x 6 x 3 inches).1.0 kg (2.2 Ib). ________________

Systems lin .

13ll'illem ll'assenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

CERTIFICATE OF AUTHOR

. David Laronde of the town of Temagami, Ontario hereby certify':

1. That I am a geology engineering technologist and have been engaged in mineral

exploration for the past 20 years.

2. That I am a graduate of Cambrian College in Sudbury

with a diploma in Geology Engineering Technology 1979

3. That my knowledge of the property described herein

was acquired by field work and documentation.

Dated at Temagami this 12th day of January 2000.

Dand Laronde


14WilleinWassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

References

1978 Bennett. G. Geologic Report - Geology of Northeast Temagami Area Ontario Geologic Survey

Meegwich Consultants Inc. Box 482 Temagami, Out. POH 2HO tel. (705)569-2904

ll'illem H'assenaar OPAP Final Submission Wassenaar Properly Strathcona T\\p.

APPENDIX l

Geologic Report

A.W. Beecham


It'i/leni Wassenaar OPAP Final Submission Wassenaar Property Strathcona Twp.

APPENDIX II

Assay Certifcate


F. JBB XRAL LaboratoriesA Division of SGS Canada Inc.

Work Order: 056245 Date: 1 7/08/99 FINAL Pigc l of J

Mrfcod. Det-Lon-Unit*.

O1-99 •Dup l 99

AuFA301

1PI*

PiFAJOt

10PI*

PdFA301

1PI*

ft*. •H:ICF70

O.Sppol

NaICF70

0.01*

MlICP70

001*

AJ1CP70

0.01"V

P1CP70

0.01*

K1CT70

0.01*

CaICF70

0.01n

StICF70

O.Sppm

TlICT7*

0.01f

VICT70

1PPtn

Oricrro

ippm

Mnicrn

2ppm

FeICT70

0.01*

4648

1412

n15

•COS 0.040.04

0.660.69

0.860.91

•CO.Ol•COOI

001001

0.22024

2.5 2.8

0.04005

3637

5455

579603

17.8 IS.7

XRALO

XRAL LaboratoriesA Division of SGS Canada Inc.

Work Order: 056245 Date: 1 7/08/99 FINAL Page 2 of 3

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CoICPTO

1ppm

r*ICPT*

1ppm

diICPTO

0-5ppm

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3ppm

STICPTO

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YICFTi

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ZrICPTO

0-Sppm

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10ppm

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199 •Dup l 99

553 748772

297308

67.5710

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4.7 5.1

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5.558

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2430

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XRALK}O

XRAL LaboratoriesA Division of SOS Canada Inc.

Work Order: 056245 Dale: 1 7/08/99 FINAL Pjgr 3 of 3

Ekmtrt. Q Mrtbod

Dints.

Pta Bt ACICPTO ICT7O AA73

2 5 03ppm ppm

l 99•Dup 1-99

118122

2724 4 4

invoice/Facture No.: 081:031658

XRAL XRAL LaboratoriesA Division of SQS Canada inc.

INVOICE

Invoice To/Facture A:W. Wassenaar MD Attn: Willem Wassennar

7 Roxville AvenueTORONTOONTARIO, CANADA M4G 3P7

Submitted By/Soumettez Par:W. Wassenaar MD Attn: Willern Wassannar


Work Order:. Invoice Date: Date Submitted: Shipped Via:

Qnty

1

1

1

1

1

Code

PG205

FA301

ICP70

AA73

GST

056245 Customer No.: 401705 17/08/99 Your P.O. No.: 06/08/99 Your Project No.: SELF Waybill No. :

Description

Drying, Crushing St m illing { hardened st

1AT Au Inst. Fire Assay

ICP, Aqua RegieSilver by AA

T& G ST Rg No. R105082572

# Ele Unit Cost

55.25

3 51 3.30

31 58.15

1 54.75

$2.20

Amt/Montant

$5.25

$13.30

$8.15

$4.75

52.20

PREPAY Advance Payment Received 533.65

TOTAL IN CANADIAN FUNDS l TOTAL EN DOLLARS CANADIEN 533.65

PI**** r*mtt to / S.V.P. *nvoy*f votr* p*J*m*nt i:P.O. Box 9581 Station 'A' Toronto, ON Canada M5W 2K3

PI**.** courier to l S .V.P. *nvoy*r par courl*r *:1885 Leslie StreetDon Mills, ONCanada M3B 3J4Tel: (416)445-5755Fax: 1416)445-4152

Please Quote I nvoice Number l S .V.P. Specifier le numero de facture 081:031658

Note/N.B.: 1 .5** per month interest on Overdue Accounts l I marSt de sur Comptes Arrieras de 1 . S 1* Par Mois: Terms Net 30 days

ORIGINAL INVOICE

Member of the SGS Group (Societ* Generals d* Surveiltanc*)

XRAL XRAL LaboratoriesA Division of SOS Canada Inc.

1 885 Leslie Street Don Mills, Ontario Canada MSB 3J4 Telephone (416) 445-5755 Fax (416) 445-4152 CERTIFICATE OF ANALYSIS

Work Order: 056245To: W. Wassenaar MD

Ann: Wlllem Waasennar


Date 17/08/99

Copy 1 to

Copy 2 to

P.O. No. Project No. No. of Sample* Date Submitted Report Comprise*

1 ROCKS 06/08/99 Cover Sheet plus Pages 1 to 3

Distribution of unused material:Pulps: Discarded After 90 Days Unless Instructed!!!Rejects: Discarded After 90 Days Unless Instructed!!!

Certified By

Dr. Hiifeh de Souza, General Manager XRAL Laboratories

ISO 9002 REGISTERED

Report Footer: L.N.R. - Listed not received l.S. ~ Insufficient Sample n.a. - Not applicable -- - No result •INF - Composition of this sample makes detection impossible by this method M a fter a result denotes ppb to ppm conversion, "ft denotes ppm to "ft conversion

Member of the SOS Group (Sodete Genera* de Survvtlarx*)

. 2 O 5Wassenaar Claims SE. Strathcona Township,, Temagami Area, NE. Ontario

DI H 10Oo -J

MO U1

Geological ObservationsS gIntroduction gp

The Wassenaar claim group is located in southeastern Strathcona and southwestern Riddell townships, some 7 km. (map distance) south of the village of Temagami. Regionally this area is part of the Southern Province of the Canadian Shield. The basement rocks are Archean and consist of complexly folded mafic volcanics intruded by trondhjemite (Na-granite) batholifhs. This is overlain 0 unconformably by the Proterzoic Gowganda Formation sediments. Gently g undulating, gabbro sills, known as Nipissing diabase intrude mainly the Gowganda Formation, but also extend into the Archean basement rocks. In the area of the claims most of the Gowganda Formation has been eroded, but a sill of Nipissing Diabase remains in the northern part of the group.

The following comments are based on only 2 days (14th and 15th Nov. 1999) field work under somewhat adverse weather conditions. The comments are intended to accompany a more comprehensive report rather than as a 'stand-alone report. (No location map, property description or detailed description of previous work is included.) The purpose of the work was to examine the geology and evaluate the mineral occurrences at the following localities: (1) around the SE corner of the Beaver Pond where significant gold values had been obtained under the water line of the pond; (2) outcrop area west of the Beaver Pond; (3) the "quartz pits" along the stream between the Beaver Pond and Upper Twin Lake and (4) quartz veins in the northeast area around Line 100W and SOON.

The author is familiar with the general area from work done around Lowell Lake in late 1970's for St. Joseph Explorations (a subsidiary of the old American mining company St. Joe Minerals previously St. Joe Lead.) and from updating the Mineral Deposits Inventory for the MNDM in 1990-1991.

Description of Work Done

David Laronde of Temagami described the property and provided copies of relevant maps and reports describing previous work, mostly by the present owners. He also guided the author to property.

On the 14th the area around the southeast corner of the Beaver Pond was examined and part of the outcrop mapped. This was a reasonably good day for observation, but there was some snow on the northwest outcrop slope on the large outcrops over-looking the southeast corner of the Beaver Pond and these outcrops

could not be examined properly because of the danger of slipping into the pond. On the second field day, 15th November, a heavy snow squall held up work early in the morning and dropped 2 to 3 cm. of wet snow. The outcrops could not be brushed clear of this snow and the only way to view the surface of the outcrop was to strip off areas of moss. This made for slow progress. However, something was accomplished. On the west side of the Beaver Pond, one cross section was roughly mapped along line 600W. A cursory examination of two quartz veins in Nipissing Diabase were made, one on line 600W, northwest of the Beaver Pond and the other referred to as Showing "D" along the stream, north of the Beaver Pond. A rough cross-section was also mapped east of the Beaver Pond on the return traverse to locate the diabase volcanic contact.

Five chip samples of mineralization and veins were taken. Mapping and observations are shown on the accompanying map at a scale of 1:2500. The legend has been expanded to allow for other rock types in case more mapping is done.

The data provided by D. Laronde were reviewed and summaries of the more significant assays from work by the claim owners were added to the 1:2500 scale map. No review of data in the MNDM assessment files was made.

General Geology

A major contact striking about grid EW passes through the south part of the Beaver Pond. South of this contact the rocks are mainly fine grained pillowed and flow structured to massive mafic volcanics. North of the line, the area is underlain by a coarse to medium coarse grained gabbro. This gabbro has the textures of the Nipissing Diabase sills seen elsewhere in the Temagami and Cobalt areas and it is recognized as a Nipissing Diabase sill by Bennett. Towards the south, this gabbro seems lighter- coloured and contains areas of varied textured to pegmatite-like material. Northward it seems a little darker and generally finer grained. i.e. The diabase seems to be differentiated or layered. On line 100W at about 350N on a west facing scarp face, an Archean assemblage of mafic volcanics and feldspar porphyry intrusive appears to overlie Nipissing diabase. (This observation was made late in the afternoon and it was a bit rushed in order to get out of bush before nightfall.) This observation combined with the previous comment on apparent differentiation of the diabase, suggests that the Nipissing diabase here is a gently south dipping sill and this contact marks the top of the sill.

The pillowed to massive flows exposed south and east of the 'Beaver Pond' are typical Archean mafic volcanics, except that they contain irregular patches and streaks of silicification and some sort of feldspar (probably albite) alteration, and they are relatively hard. The impression was gained that they have been hornfelsed (rock that has been re-crystallized around an intermediate to felsic intrusive.). The hornfelsing would not be due to the Nipissing diabase, but likely the large surrounding trondhjemite batholiths.

Structural Geology

The mafic volcanics, where examined, except for pillows, are fairly massive and no strikes and dips were measured on them. In places the fine grained mafic flows grade into medium to coarse grained (gabbro-like) rocks. These units usually mark certain individual flows and cores of thick flows and mapping their contacts with the fine grained units usually give strike directions. However, none of these contacts were traced far enough to indicate a strike direction for the flows. Bennett does show the mafic volcanics trending about grid E-W and dipping south.

Three prominent fault and fracture directions are recognized. A nearly N-S set is most conspicuous southeast and east of Beaver Pond. The second, a HO0 trend is marked by the south contact of the Nipissing Diabase and parallel structures within the sill to the north. Although the prominent scarps along this contact seem to be caused by contrast in the weathering resistance of the diabase and altered mafic volcanics, this 110" trend is a regional fracture set and the diabase at this point may be intruding along these pre-existing fractures. A third set is recognized at the quartz vein (showing "D") located between 'Beaver Pond' and Upper Twin Lake. Here a prominent valley sub- parallel to the quartz vein marks a common regional 0700 trend.

Mineralization and Hydrothermal Alteration

Within the area examined, as noted above, there is wide spread, pale brown- grey alteration of the mafic volcanics. This is a combination of silicification and some sort of feldspar alteration (probably albite). This occurs as irregular patches and in pillow selvages along fractures. No particular orientation was noted. Pyrite, as trace amounts up to a few percent, accompanies this alteration . Although some of the alteration follows pillow selvages, this is not a common primary volcanic feature. It is the author's opinion that it is due to a later hydrothermal event. This type of alteration is, typically associated with gold mineralization and one of the two samples, B-3 from near the southeast corner of the Beaver Pond, does carry anomalous gold levels (74 ppb Au).

The two showings examined in the Nipissing Diabase consist of massive white, glassy quartz, with variable amounts of pyrite and chalcopyrite. On the NW showing, a 70 cm. wide quartz vein is accompanied by calcite and there is a wide (alteration) selvage of dark chlorite along the vein and pyrite and chalcopyrite (with malachite) are fairly abundant. This vein strikes NW-SE and dips vertically. A sample of the vein containing pyrite and chalcopyrite, returned a surprising 953 ppb gold. It also contained anomalous levels of both Ag, 5.6 ppm and Co, 95 ppm. This veins does not appear to be related to any prominent nearby structure. The veins at Showing D, (along the stream), on the other hand, occur along a prominent topographic feature which probably marks a major fracture or fault. These veins dip at about 450 and appears to occupy fractures subsidiary to the main structure along the stream valley. A grab sample from showing "D" returned anomalous Co, 102 ppm, but no gold or silver.

Table I List of Samples and AssaysField

#

B-2

B-3

B-4

B-8

B-9

Lab.#

14968

14969

14970

14971

14972

N

190N

314N

340N

642N

770N

Ref. Line

3 50 W

350W

300W

600W

400W

from line

10W

17E

16W

9W

8E

ppb Au

7

74 34

2

953

9383

ppm Ag

n/a

n/a

n/a

5.6

0.1

ppm Co

n/a

n/a

n/a

95

102

Remarks

sil, f.sp.alt'n patches & streaks with minor Py

tt U

check assay of original pulp'flat' fault, with earthy, red hematite, gossan, qv.70cm. glassy, white qv + blebs Py, Cp, mal

check assay of original pulp30-40 cm glassy, white rusty, calcite-qtz vein

n/a = not analyzed

Discussion

Because of the very limited field work, and the poor field conditions, conclusions reached are necessarily tentative. However a few comments can be made.

Quartz and quartz calcite veins in the Nipissing Diabase are fairly common. An example is the Gosselin vein located 11 kilometres to the NNE in Cassels Township. The Gosselin contains sections of heavy chalcopyrite, some cobalt mineralization, low silver values and isolated gold values. In spite of a lot of exploration no ore shoots have been found in the Gosselin vein. North of Lowell Lake, a St. Joseph Explorations, 1978 drill hole intersected significant gold values in quartz carbonate veins in a Nipissing Diabase intrusive (6.5 g/t Au over 30cm . All the mineralization is from a 2.5 cm vein diluted in a 30 cm. sample and one would expect selected grabs from this to be as high as 10 times this assay;). To the east, between Upper Twin Lake and Wagkich Lake, another St. Joseph drill hole intersected some low gold values in mineralized Huronian sediments, (0.85 g/t Au over 0.5 to 1m as well as I can remember). This information is in the assessment files and also in the OGS Mineral Deposit Inventory. The veins on the Wassenaar claims and at Lowell Lake appear to be similar to the Ag-Co arsenide veins in the Cobalt and Silver Centre areas except that silver and cobalt levels are lower, gold levels are higher and the veins are mainly quartz instead of mainly calcite.

The quartz (+S- calcite) veins on the Wassenaar property seem to be fairly strong structures and at least one of them is well mineralized with Py and Cp. The gold values reported at the southeast corner of the Beaver Pond are unusually high. Although there has been no gold production from quartz-carbonate veins in the Nipissing diabase, the possibility of such a deposit cannot be ruled out.

This general area carries mineralization with elevated gold levels, both in the Proterozoic (Huronian sediments and Nipissing Diabase) and in the older Archean rocks. Whether or not the area has potential for economic gold deposits is not known.

The high values reported from veins in the Nipissing Diabase seem encouraging. However, it is important to look at the geometry and grade of these structures to see if there is a chance of economic concentrations. It must be borne in mind that minimum mining width is about 1.5m and that a 30 cm. wide vein would have to grade something like 40 to 60 g/tonne gold to be economically viable and there would have to be sufficient volume to pay for development and plant costs. These diabase hosted quartz veins are not typical gold bearing structures in the Canadian Shield. This could however, be a new type of mineralization, possibly an epithermal type of gold mineralization which is common in the younger fold belts, such as the Cordilleran or Appalachian belts.

The author did not examine the Area 004 mineralization and hence, the following comments are speculative. Most of this mineralization as described by Hart appears to be within or closely associated with interflow sediments or exhalite beds. This mineralization is similar to showings west and southwest of Lowell Lake.. Here sub-economic Cu and Zn occur in pyrrhotite-rich cherty, exhalite beds within mafic flows. This mineralization has been mapped SSW towards Herridge Lake to about Highway 11. From this point a series of airborne EM anomalies (from an unpublished survey by St. Joseph Explorations cl977) extends eastward for about 3.5 km and then through a series of folds into the area just south of the Wassenaar claims. One of these conductors, not far east of Highway 11 was drilled. Sulphides similar to the Lowell Lake showings were intersected and the EM anomalies to the east are thought to mark similar sulphide-rich beds. At Lowell Lake the beds have been fairly extensively sampled and some drilling has been done without locating any economic mineralization. The best values encountered here are 0.65 "/o Cu, and 0.39 % Zn over about 5 m. The pyrrhotite beds at Lowell Lake are very similar both in their make up and in their geological setting to the interflow sediments that commonly form the 'roots' of many silver veins in the Cobalt camp. Here, too a lot of exploration has been done for base metals, but the best concentrations found have grades of only about 2% Zn and 0.5 to 0.75 9o Cu over 3 to 5 m thickness. Even this grade is well below economic levels. The Lowell Lake and Cobalt interflows are similar to the exhalite beds that mark productive horizons in Archean, massive sulphide base metal camps, except that here they occur within mafic volcanics rather than in close association with felsic volcanics as in the productive camps.

Recommendations

More work is warranted on the auriferous quartz veins in the Nipissing Diabase. It is recommended that one or two of the best veins be well exposed and systematically channel sampled to determine grade and continuity of mineralization.

Some re-examination of the showings in Area 004 is recommended. Although the base metal potential is not rated very good, the gold values could be interesting if they are actually in the exhalite where values could have better continuity than in veins.

Airphotographs would help in mapping and particularly in identifying faults and prominent fractures, which may control the quartz veins in the Nipissing Diabase in the north part of the property.

Soil geochemistry could be helpful on this property. Sampling of small areas around and 'down ice' (in the direction of Pleistocene ice movement) from known gold showings could be useful to see if the technique works. The B-2 soil horizon generally provides the best sample medium. The author has had some technical success with soil geochemistry in locating a large low grade gold deposit (as yet sub-economic) in the Tyrrell-Knight area west of Gowganda. The technique should detect major, subcropping gold concentrations.

In summary, although no mineralization typical of known gold ore bodies has been recognized, the unusually high gold values found in some of the quartz veins warrant further exploration. In this case where the geological model is unfamiliar, it is generally best to be guided by metal values.

A.W. Beecham Haileybury, Ontario 2 Dec. 1999

References

Beecham, A.W.April 1978

Bennett, G. 1978

Born, P.1989

Hart, I.R.May 1998

Laronde, D.Aug. 1999

Drill log 189-1, St. Joseph Explorations Ltd. MNDM assessment files;

Geology of the Northeast Temagami Area, Dist, of Nipissing, Rep. 163 and Map 2324, Ont. Geol Survey Geol.;

Precambrian Geology, Cassels and Riddell Townships Report 271 and map 2526, Ont. Geol. Survey

Geological Report, Wassenaar Property NTS 31-L-13, Strathcona Twp.

Wassenaar Property, Strathcona Township, Ontario, Ground Geophysical Surveys, Meegwich Consultants Inc. Map 1:2500;

Appendix

Assay Certificate

Swastika LaboratoriesA Division of Assayera Corporation Ltd.

Established 1928 Assaying - Consulting - Representation

Geochemical Analysis Certificate 9W-3653-RG1Company: A .W. BEECHAM Date: NOV-23-99Project: WassenaarAttn: A.W. Beecham

We hereby certify the following Geochemical Analysis of 5 Grab samples submitted NOV-17-99 by .

Sample Au Au Check Ag Co Number PPB PPB PIM PIM14968""""""""""""""""""""?"""""""-""""""""-""""""-""""""""""""""""

14969 74 3414970 214971 953 938 5.6 9514972 3 - 0.1 102

One assay ton portion used.

Certified by

l Cameron Ave., P.O. Box 10, Swastika, Ontario POK l TO Telephone (705)642-3244 Fax (705)642-3300

andMinesDeclaration of Assessment Work Performed on Mining LandMining Act, Sub**ctlon 65(2) and 66(3), R. S. O. 1990

Transaction Ni,T.t*r (office

UJOO'fOAssessment F iles Pessaran 'r.ag -i g

)l subsections 65(2) and 66(3) of ihe Mining Act. Under sociion 8 of :f a review the assessment work and correspond wiih ihe m n r g lane! hcice' Recorder, Ministry ol Northern Development aid Mines, 5;i Flo;-

31M04SE2007 2.20529 RIDDELL 9QQ 2.2052Instructions: - For work performed on Crown Lands before recording a claim, use form 0240.

- Please type or print in ink.

1. Recorded holder(s) (Attach a list if necessary)o t,

Name . ^ ' ^^^\ ~m j* * ^ "C

to So Address f — s\?tt- 'oft 9 1? S t ^ fc C*J t"SS *- ^ ^ * ^ jrSc*'**- ^ " '

'~*6n J . U . U/* iJ^^^r- (^^ /9 - T20JJ

'~*lT9 ^ ^l^~ (sJ ^sx-^**-r J /9- rZoJ-7/^ ? 6 Tf?^ f _______ -^ —- —————

AOCress "7 /T o X" \ it(e- /O^c-.

"7~oro^7u, 0^^. M ij- G- S ?7

Client Number ,2d^ ^*// ( U/t-lt^

Telephone Number

Fax Numbeff^,cj ^v-- 3y?2-Client Number

Telephone Number

Fax Number

2. Type of work performed: Check (^) and report on only ONE of the following groups for this declaration.Physical: drilling stripping, n RehabilitationGeotechnical: prospecting, surveys,

assays and work under section 18 (regs)n *-* trenching and associated assays D

Work Type /** - f 0

Oates Work From ^ x o— ^^ ^o 3 / S i- ^9Performed Day | Montti | Year Day | Montn | Year

Global Positioning System Data (rf available) Township/Area ^~j-rc,jj, c.e^x? ~7^ .

M or O-Plan Number

Office UseCommodity

Total S Value of Work Claimed /G", ^7C

NTS Reference

Mining D,v,s,on ^d^(l ^ (J

Resident Geologist , 7 District *?(,rlkfansJ ACL^-^

Please remember to: - obtain a work permit from the Ministry of Natural Resources as required;- provide proper notice to surface rights holders before starting work;- complete and attach a Statement of Costs, form 0212;- provide a map showing contiguous mining lands that are linked for assigning work;- include two copies of your technical report.

3. PersonName

Aodress

Name

or companies who prepared the technical report (Attach a list if necessary)

MEEGWICH INC.P.O. BOX 482

POH 2HOAddress

Name

Address

Telephone Number "7 o 5^ -TV? - 2 9o Y

Fax Number

Telephone Number

Fax Number

Telephone Number

Fax Number

4. Certification by Recorded Holder or Agentt do hereby certify that l have personal knowledge of the facts set forth in

(Pnnt Name)

this Declaration of Assessment Work having caused the work to be performed or witnessed the same during or after its completion and, to the best of my knowledge, tlje annexed report is true.Signature of Recorded Holder or Agent Date

Agent's Address Telephone Number Fax Number

3211 (03*71 RECtlVbbSEP 15 :::3

GEOSCIENCE ASSESSMENT OfFlCE

5. Work to be recorded and distributed. Work can only be assigned to claims that are contiguous (adjoining) to tie mining land where work was performed, at the time work was performed. A map showing the contiguous link must accompany form

Mining Claim Number. Or if work was done on other eligible mining land, show in this

column the location number indicated on the claim map

eg

eg

eg

i,/

i *'•C-'

30.'"

" J1

5 }

6 ^

7 ,)

8 ,J

9 ^

1C

1 1

12

13

14

TB7827

1234567

1234568

/o 7t ?6a/o-?Z 969

/o7t ??Y/(*tl o o 2-f l f f oo Y

f (*i l oo S

X/ f/ *30^

//?/ 0 ^7//f/ o of

15

Column Totals

Number of Claim Units. For other mining land, list hectares.

16 ha

12

2

Xs

/7ff

fyf

/jr

Value of work performed on this claim or other minjng land.

526,825

0

S 8,892

Vo3ff/,t7fZ,?-'?*'

2-,2-Oc

/.rros 7 004 0&

z&r 2*0

/t, *7* -

Value of work applied to this claim.

N/A

324,000

54,000

2., o ^ 02,ooo

Z , OCJe.

2 , ô "

2 , ** t*o

2. ,oo o

/, ^ô

S, Z&&(,2--7* **

St*7o -

Value of work assigned to other mining claims

524.000

0

0

Z y ^2^

- —

2.7

Zclti

' ——

. —

- —

*/êr —

- —

2.?y2.^

Bank. Value of -vcxk :c De districted ai a future date

S2625

3

S4B9C

OS

)

—— ±i ————

, do hereby certify that the above work credits aie eligible underl.___________________(Pnnt Full Name)

subsection 7 (1) of the Assessment Work Regulation 6/96 for assignment to contiguous claims or for application to the c;aim

where the work was done.

Signature of Recorded Holder oi/"^ ~\

^gentAjJthorized inytfrhidox' Date M/J^, 2.o*o -——————————————————————————— --(^ ~ —— ————— -- ——— — —————— . ——— -y- • ••••-

6. Instruction for cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check fV) in the boxes below to show how you v/ish topnontize the deletion of credits:

® 1. Credits are to be cut back from the Bank first, followed by option 2 or 3 or 4 as indicated. D 2 Credits are to be cut back starting with the claims listed last, working backwards; or fas 3 Credits are to be cut back equally over all claims listed in this declaration; or D 4. Credits are to be cut back as prioritized on the attached appendix or as follows (describe):

C? ;P| t^ ^ Q

Note: if you have not indicated how your credits are to be deleted, credits will be cut back from the Bank first, followed by option number 2 if necessary.

For Office Use OnlyReceived Stamp

RECEIVEDSEP 1 5 2000

GEOSCIENCE ASSESSMENT OFFICE

Deemed Approved Date

Date Approved

Date Notification S e T.

Total Value of Credi'. Approved

Approved for Recording by Mining Recorder (Signature)

Minislry ofNorthern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Number (office us*)

Personal information collected on (his form is obtained under the authority of subsection 6(1) ol the Assessment WorK Regulation 6/96. Under section 8 ol the Mining Act, the information is a public record. This information will be used lo review tr-.e assessment work and correspono *nri the mining land holder. Questions about this collection should be directed to the Chief Mining Racordar, Minirtry of Northern Development a 10 Mines. 6th Floor, 933 Ramsey Lake Road, Sudbury, Onlario, P3E 685. rt Ci X* t-v J ,,

4b m 6 \J *J' *~' v

Work TypeUnits of Work

Depending on the type of work, list the number ol hours/days worked, metres ol drilling, kilo metres ol grid line, number of samples, etc.

Cost P er Unit of

Total Cost

A; /y.~U-

I/CF

-J^f

-To'*

. e* fc.~-

Associated Costs (e.g. supplies, mobilization and demobilization).

^ J& rri+.^J'

Transportation Costs

f

Food and Lodging Costs

Total Value of Assessment Work

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at IOQ.% of the above Total Value of Assessment Work2. If work is filed after two years and up to five years after performance, it can only be claimed at 5 n(Vo ol the Total

Value of Assessment Work. If this situation applies to your claims, use the calculation below:

TOTAL VALUE OF ASSESSMENT WORK x 0 .50 Total S value of worked claimed.

Note: '- Work older than 5 years is not eligible for credit.- A recorded holder may be required to verify expenditures claimed in this statement of costs within 4 5 d ays of a request for verification and/or correction/clarification. If verification and/or correction/clarification is not made, the Minister may reject all or part of the assessment work submitted.

Certification verifying costs:

l, hereby certify, that the amounts shown are as accurate as may(please print full name)

reasonably be determined and the costs were incurred while conducting assessment work on the lands indicated on

the accompanying Declaration of Work form as

to make this certification.(recorded holdeff agenti or state company posiiton with signing aui

RECEIVEDSEP 151;: J

GEOSCIENCE ASSESSMENT _____OFFICE

am authorized

Signature Dale

Ministry of Ministers duNorthern Development Developpement du Nordand Mines et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road

January 5, 2001 6th FloorSudbury, Ontario

JOHN LIEUWES WASSENAAR P3E 6B57 ROXVILLE AVENUETORONTO, ONTARIO Telephone: (888) 415-9845M4G-3P7 Fax: (877)670-1555

Visit our website at: www.gov.on.ca/MNDM/MINES/LANDS/mlsmnpge.htm

Dear Sir or Madam: Submission Number: 2 .20529

Status Subject: Transaction Number(s): W0070.00167 Approval After Notice

We have reviewed your Assessment Work submission with the above noted Transaction Number(s). The attached summary page(s) indicate the results of the review. WE RECOMMEND YOU READ THIS SUMMARY FOR THE DETAILS PERTAINING TO YOUR ASSESSMENT WORK.

If the status for a transaction is a 45 Day Notice, the summary will outline the reasons for the notice, and any steps you can take to remedy deficiencies. The 90-day deemed approval provision, subsection 6(7) of the Assessment Work Regulation, will no longer be in effect for assessment work which has received a 45 Day Notice. Allowable changes to your credit distribution can be made by contacting the Geoscience Assessment Office within this 45 Day period, otherwise assessment credit will be cut back and distributed as outlined in Section #6 of the Declaration of Assessment work form.

Please note any revisions must be submitted in DUPLICATE to the Geoscience Assessment Office, by the response date on the summary.

If you have any questions regarding this correspondence, please contact BRUCE GATES by e-mail at [email protected] or by telephone at (705) 670-5856.

Yours sincerely,

ORIGINAL SIGNED BYLucille JeromeActing Supervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 15573

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2 .20529

Date Correspondence Sent: J anuary 05, 2001 Assessor:BRUCE GATES

First Claim Number1076960

Township(s) l Area(s)STRATHCONA

StatusApproval After Notice

Transaction NumberW0070.00167

Section:14 Geophysical MAG 14 Geophysical VLF 14 Geophysical IP 9 Prospecting PROSP 12 Geological GEOL

The 45 days outlined in the Notice dated November 16, 2000 have passed.

Assessment work credit has been approved as outlined on the attached Distribution of Assessment Work Credit sheet.

Approval Date

December 31, 2000

Correspondence to:Resident Geologist Kirkland Lake, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):David Laronde TEMAGAMI, ONTARIO

JOHN LIEUWES WASSENAAR TORONTO, ONTARIO

SIEK WASSENAAR STOUFFVILLE, ONTARIO

SYBREN L WASSENAAR TORONTO, ONTARIO

WILLEM WASSENAAR TORONTO, Ontario

Page:1Correspondence ID: 1 5573

Distribution of Assessment Work Credit

The following credit distribution reflects the value of assessment work performed on the mining land(s).

Date: January 05, 2001

Submission Number: 2.20529

Transaction Number: W0070.00167

Claim Number Value Of Work Performed

1076960 3,770.00

1076969 1,678.00

1076974 2,005.00

1191002 2,200.00

1191004 1,480.00

1191005 1,430.00

1191006 600.00

1191007 1,757.00

1191008 200.00

Total: S 1 5,120.00

Page: l

Correspondence ID: 1 5573

31M04SE2007 2.20529 RIDDELL 200

Ministry of Ministry ofNatural Northern DevelopmentResources and Mines

THE INFORMATION THAT APPEARS ON THIS MAP HAS BEEN COMPILED f ROM VARIOUS SOURCES, AND ACCURACY IS HOT GUARANTEED. THOSE WISHMG TO STAKE MININGCLAIMS SHOULD CONSULT WITH THE M IM1NO RECORDER HIMSTRY OF NORTHERN DEVELOPMENT AND MINES. FOR ADDITIONAL INFORMATION OH THE STATUS OF THE LANDS SHOWN HEREOM.

1231127 INDEX TO LAND DISPOSITIONG.H A

TEMAGAMIPU*

G -3450TOWNSHIP SUDBURY

UNC Tflltl; JttBIS ^ MtUOH

NIPISSINGSTRATHCONA

AKA MEMft-M Ait* W fCH

M (WDIFWVTSU iiMj;

12307,31AREAS WITHDRAWN FROM DISPOSTiON

M.R.O. - MINING RK3HTS ONLY S-R.O -SURFACE RIGHTS ONLY M.tS. -MINING AND SURFACE RIGHTS

Boundary

Township, Meridian, Baseline

Rood allowance: surveyed . - .

Psrcel;unmrvaywl

Rlglit of way; roadrailway .

utility

^eaervatkin

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Road; higrnvajr, county, townshipaccess . . . . . - . . . . . . . . . . . .Ifjil.toush---------- ......

ShoreHrn (nrigirul) . . . - - . . .

SKYLINE RESERVE

DISPOSmON OF CROWN LANDSPat*nt

Surface A Wninil Rk|M* Surface N ights Only. Mining Rights Onry.....

LM6*

Surfaca 4 Mining Rights Surface R ights Only

.,v '--' ^ ^K. ,.jL*K- - . ^rf ~ ^- ^-. ' -J Al *a.— - -.- - . j J.l -

MAJOR AMENDMENTS TO NORL STAKWG

L^-:^ "? PLEASE NOT!: THK fSLAMD ON LAKE TWACAMl Nm-O^I" W|TH*'^WN AND Wlil TMMGAMIUOEonx TontDspEcrmc AND STAKING our

In. aru riwwn H SKYLINE HURVE Ma**te hurt cmnd by IM wun ut LAKE TEMAGAMI on rill* BM* will bg jubjrct to OMMM Refulilicw WWIS tradi undar rhc furlic Lnh AM.

on tte type md Tim'*! of yo*r*xplof*icn wwk you may require a Wort Permit. Ft* ftrilivniifbrnutlnripltaie contact Qw**(d Mcytf, RegfonU KMidrac G*otD|ltt it (701) X7.H42 ar

[7Wrl3*n*irr —— ——— —

TOWNSHIP

. *nod"- —"O-, drafcr- j 8i""i i Hid rv-.ipein;

NUpper

\Tw i n

/

\Lake

O C 7

V

C 7 fe 9 7 4

1^19555li

\

tx*o '

GEOLOGICAL LEGEND

PROTEROZOIC

\ l 9 Late diabase dykes (Sudbury Type)

t ' 1 8 Nipissing Diabasel -----J (a) Coarse grained gabbro mcl varied textured typesl l (b) Medium, uniform textured gabbrof "l (f) Dark fine grained, magnetic diabase

ARCHEAN

B Granitic, Plutonic Rocks(a) Trondhjemite(b) Pegmatite

___ 5 Mafic to Intermediate Intrusivesl l (a) Gabbro (b) Diorite

l l 4 Sediments(e) Sulphide rich exhalite, cherty sediment

3 Intermediate to Felsic Subvolcanic Intrusives(a) Quartz feldspar porphyry mtrusives(b) Feldspar porphyry mtrusives

en 2 Felsic Volcanics

1 Mafic Volcanics(a) Massive to foliated(b) Pillowed(d) Medium to coarse grained(c) Flow breccia

ABBREVIATIONS

aftC-9chlCpCIGhemm gmalqcqvPoPysil

SYMBOLS

X : i.

hydfothermatty alteredcoarse grainedchiorite alterationchalcopyriteclaim linegossanhematitemedium grainedmalachitequartz-calcite veinquartz veinpyrrhotitepyritesilicified, silicification

outcrop, area of outcrop

sca r p

geological contact

geological contact showing dip

sctvstosity, foliation

lineation

pillows

fault

low angle or thrust fault

topographic lineament, prominent fracture, fault

silica *Meldspar alteration. +J- pyrite

sample point; Au ppb, Ag ppm. Co ppm,

summary of assays by claim owners

rock pit, trench

earth trench

diamond drill hole

swamp

open, grassy swamp

claim post located

property boundary

all weather road

track, winter road

Note:Picket line locations, claim lines and topography modified after Laronde Aug 1999

31M04SE2007 2 .20529 R IDDELL 210

CV-. ,' 9 o p o DI ppm

l/1/assenaar PropertySE Strathcona Twp

District of Nipissing

GeologyUpper Twin Lake Area

Scale: 1:2500Drawn by. AW Beecham

Date. Nov 1999

Revisions NTS31U13, 31M/4

-v

A

x, O

Claim post, assumed

Claim post, found

Trench

Ledge

Main Showing

Conductor Axis, Defined

Conductor Axis, Interpreted

Conductor Zone

Outcrop

Gra b Sample (Aug 1, 1999 56245)

IP. Anomaly

(high priority drill target)

IP. Anomaly

(low priority drill target)

Area of beep map prospecting

Area prospected by W.Wassenaar

Upper Twin Lake

N-

(Astronomic)

1219555

Hwy.#11 4km

2.2052931M04SE2007 2 .20S29 RIDDBLL 220

Instruments: GEM Systems GSM-19 MAG / VLF Serial #806862

GEM Systems GSM-19 Base Station Serial#58479

GEM Systems GSM-19 Magnetometer Senal #58479

Scintrex EDA Omni IVBase Station Serial#228225

Geonics EM-16 VLF Receiver Serial # 10585

VLF Station: NAA 24.0 kHz Cutler Maine

50

Scale 1:250050 100 150

metre

Wassenaar PropertyStrathcona Township, Ontario

Prospecting and Compilation Map

Data Processing and Interpretation by: Meegwich Consultants Inc.

Scale 1:2500

December 1999

NTS31 L/13&31 M/

31M

04S

S20

07

2.2

05

29

O

r, c?

1191

008

Stra

thco

na T

wp.

Ridd

ell T

wp.

(Astronomic)

Conductor Axis, Defined

Conductor Axis, Interpreted

Profile Scale: 1 cm ^ 2QV,

31M04SS2007 2 .20529 RIDDELL 240

Instruments: GEM Systems GSM-19 MAG / VLF Serial #836862

GEM Syst&ns GSM-19 Base Station Serial #58479

GEM Systems GSM-19 Magnetometer Serial #58479

Sdntrex EDA Omni IV Base Station Serial #228225

Geonics EM-16 VLF Receiver Serial # 10585

VLF Station: NAA 24.0kHz Cutler Maine

50Scale 1:2500

50 100 150

motre

Wassenaar PropertyStrathcona Township, Ontario

Ground Geophysical Surveys

VLF - EM Survey Profiles of the In-Phase and Quadrature

Data Processing and Interpretation by:

Meegwich Consultants Inc.Scale 1:2500

December 1999

NTS 31 U13 A 31 M/'

2.20529

4894.

Rt 3ISTIVITY OHM-METERS

oin(N

g PHASEK M RAO

fNM W

OJ

i T~" 7 i r i 'r i ; i f T ' j j i i i rPOO RQO

_48 9738

K 24 .4894

Lo

l f 50 2+0) 2+50 3+00 N 4400 N 4+y) 5+00 N 6+00 N 6+50 N

Filter 8356 5610 S032 5631 5904

n-2

0=5

3351 3260 1867 3132 12ffi, 2tK 2453 1W 2 564 2ffii Wl 5233

975 1579 \V I6K

8698 4J84 "43 Filter

3868 3495\ / t l \ y J \ l

5910 6S7! 7438 WU ' 5473 l 3682 -^ 21i1 2448 ' 1 807 5478 ' , I 51S ^-i

7091 6116 6211 5B4B ^ 4721 ^ JJM^ 7lSB 1988 ' 2BS7 ' 1 085 1121" \J?S/ 17SC ,Xi 5SJ-^ 2255 \ ~ SQJ 1 S1E - MH " ^ 12K/, S17J 5583 6458

7IB4 4763 72M +411 , 5995 — 672t \ 27IZ

\

\ 1012 1224 \ 23i2 — 4B24 1279 21EJ 1S21'53S9 5141 5B57 5586/1*; \ 5616 — W68 //824' ( 465 ^-. B56 . (" 1907 \ 1457 ff, 1 8K \ li 3867 -, 2622 ""- 15*.! I486

5630' 4207 8231 949B 316J 1W^ ' 11E! ' 583 V 357 - 2213 S l IK ' 4920 JK4 x 1013 "^742 737 - x 5503

5060 896!

514J 7860V

11 = 4

.5+50 N 4 KX) N 4+50 N 5+00 N 5+50 N 6+00 N 6 + 50 N

Filter

11=6

5 f.E 92 l? 17 21

,1 1.3 _ 1 1.8 j i, 11 \ 23 v 4418 H , , 7J 81

~"\ f ' ( '\22 19 t 1 0 V s.B l\ l x\-J yx ^v ) \ x \ x^^— li C L-T ) n \ \ 2 6 '"-. 36 K^^^J ) V . "N,

\ \ M 43 41

4? 44 4H

14 /VV 1.6 -' 1.5 1.5 2.4 A '- 91 S ,

Filter

v..'' y?j ' M' 25 "29 36

RESISTIVITY OHM-METERS

PHASEM RA D

Line 550 WDipole-Dipole Array

no

Filter

o ^ 25.0 M

© . plot point

Logarithmic Contours 1, 1.5, 2, 3, 5, 7,5, 10,...

INTERPRETATION

Strong increase in polarization accompanied by marked decrease in resistivity.

Well defined increase in polarization without marked resistivity decrease.

Poorly defined polarization increase with no resistivity signature.

Low resistivity feature.

Scale 1:2500O 26 50 75 100 125

(metreiQ]

g . 2 052^?^ ^f ^j*^"*^^^^"W.WASSENAAR

INDUCED POLARIZATION SURVEYWASSENAAR PROPERTY

STRATHCONA TOWNSHIP , ONTARIO

BELANGER (GEDPt-frSICW- COfWVCICR)

PBOI ?K

8274.

oj

RESISTIVITYOHM-METEKS

PHASEMRAD

MOO ^

1d .

0.

Filter

n^l i

11=2

n^3

11=4

11 = 5

n=6

Filter

1^=1 t

r^2

11=3

n-4

n=5

11=6

s'\

"^-^

y,

x19K

2

' f

13

i i i i . . i i i

\_____

—— ^^\

Ot-50 N 1+00 N 1+5C

UK IOK 35T3 (Ml 6055

8795 12K IOK —i. 85J6 MO

1 672? x "86 UK ) 6715 5822\\ \ \ l X f

UK \\M9Q \ 12K B50B 673?

IlKX. 7495 ^ 9250 9576 l IWiC\\ \ r") x 7 v-17K \ 6100 \ 1 0K 7 3821\s \ y/ ,--

I4K N- ~ 7184 ~~ t.51'1 -~ M40

0+50 H 1 +00 N 1+5C19 20 20 22 21

16 -^ n 2 4 yj* J4 i

M 19 25 26 Z4

19 l') 7 24 21 ?2r ^^

23 20 - —— 20 l/ ^ — 15 l ^,.'-

2S 1 15 15 11

20 15 12 H

. iniiiiiiinnii

. , 1 1 , , 1 1 , , , , , 1 , 1 , r , . , . , , , , . . , , , , , , , , , ,

~"^ ——— ^^^^ ^"^——— —— ^^ /^

V

N 2+00 N 2fWN 3+00 fJ 3+50 N 4+00 H 4+50 N 5+00 N 5+50 N 6+00 N

5053 3Blb 5414 3608 2706 1134 2763 2170 1013 890 613 656 B42 872 1175 1582 16BJ 2Mlf. V92

7220 2550 . 7119 x 16E? 1226 x 5ZB8 — 46.12 1901 , 1121 U2S , , 40B , 295 M * 264 m , 537 ^ —— 895 13S4 v x !OK/SI i \ \ . N\X^ X X/ JV /. \ ^ ^- —— N \ r-} l /'^^—, \ rv \V\\\\^ 2170 6803 6.MI x 16M — 1576 ^ 3155 i254 x J 466 9?? 791 \ J27 W 5 99 \ 173 l f /, I Bt7 \ 1 ) \ -^ \ m

1B2!T 7 4591 ^ 5JOJ &I67 ''^1737 1559 \ Ji90 ' 1JJ6 1044 7 5BO 595 "~~~ i!3 716 7 BJ " ' 308 7 l' '?5ffl ^ 1446 - 1404 -- 2544 s^^ s " \ \\ i v—-' /v r — /' f — , ^ — . y ^^s ' V ^ — - \ V^\N V, 560e 4CM 4514 5571 ^ 1545 , 76T3 1817 955 x 637 7 J90 \ (900 ^"682 x 412 /^, 9 ?B ^1 1510 ^- 2202 Z3B4 1106 x 277

•^ '^^ \ ^^ ^ ' \ f f 1 1 r^N l I ///^ ——— N ^ \ \ \ ^ 44JO 311? iE90 J938 "" 5108 2367 1401 1J88 1 7Qi f 431 V 60S , ( I1IJ 1 432 -S 1 084 ' ?917 \ 1364 \ 29dli 1649 N 1161~X l' \ \ \ / M V— \ s— i " //s,// / \ \ \ ^ \

4127 3025 1175 3486 8048 x 1185 111J 1082 ' 54J 725 781 715 - 1219 ^ mi 2 715 1672 2378 IMS 110

it

1 4 1 1 4 1 h 1 1 1 1 1 i i- 1 1

1N 2tOO N 2+M N 3+00 N i+50 N 4+00 N 4+50 N 5+00 N 5+M N ^ 6(00 N

17 15 16 14 13 13 15 12 10 5.2 5.2 41 * 4ft 5; 74 10 1- 15 27

22 ^ 11 , IS i 7.2 —— 8.6 16 - 13 , 16 - 11 ID , , 3 3 , , 1.1 12 1.4 11 1.1 - S.I .'1 -, 46f/ ( \ ^ \ s f //f- t l /~'-——- ) ' v/'-"/ f \ xf l 1 1 15 15 10 ——— - 10 14 "-^ li ( 12 10 7 4.7 l ' 1.1 -' , 2 I.B ,' 1 1 1.1 ^',- 9.5 - lb ' 1'2 \. Je7 \ ^, /- \ y ( -, \^--" x. \ tf/^ -' -

14 12 x 16 IB 'V II 12 V IB 16 10 7.8 46 ^ 2,4 ; ^ IS 11 /;^, U ^-- If 16 .. 17 \

^ — \ x, v-... -^ \ ^, \ i A J s ssS -'' ' ) ' ' 17 \ ir \ is is x 11 it M iz ) g.fi B.J V j-.. ? c i9 12 - y ^ r' ia ,.' n X ;.j) -- . \ r~ ,.^r^x ^ * v-~ :^-- ^ 'i ^ '^ - ' l-

17 17 "~-- 15 * 70 20 \ 9.8' 57 ^^- 11 ^ j; 9 .7 8.9 , 7? 6.7 "'"-. 2.9 ^ i 1 j //^. 19 - —— 20 -~ ~ IS /' 1.5 /' 19 '~\ \ \ u ,'" N.X ^ f — x\ •^zystf//' \ i~~ . 1 7 '" 2I 16 JO ' 18 X ' 4.2 J9 ~"-- L '., !1 ~' 6.2 ' 9 .9 78 ' .3.6 ^ ? 1 K ?: 14 ' 13 1'

*i

III 111 II II II 11 111 III Hill Illl '

' ' ^ ' ' ' '^ \

. ^ — —

6+50 M 7+00 N

5659 7M8 7910 6697 79

5Z&5 . 9964 7159 — 776J 611 xv \

~ 7265 ^ Vm 9000 9018

9544 6597 UK 5070,\ -^ V 's 85J? 8302 IOK

\.\, \N 2Sll' \ flT^ 7SJCx\\\o

} J21.5 ^ 99W

i

E. 1 10 M 7+00 N

29 ,M i? 1? 29

ii 4.i 37 39 . 2;

.W 31* 2* ~" ~ 32

4; 36 31 \ ?5

•a w u' 20 " . J' 30

'.: J !

POO 37

.19

,0

3 Filter

S 11 = 1

0 = 2

11 = 3

0 = 4

r^5

0 = 6

filter

n^l

0 = 2

r^i

n-4

ii-S

n-^ 1:

ROD ^K

1'

.6274

l

Lo

RESISTIVITYOHM-METERS

P H AS LM RAf.i

Line 300 WOipole-Oipole Array

a ru.i o

rOH rHg^, Filter 11 11

* * t \ S

o - "'5,0 Mx /

plot point

Logarithmic , 1 , , 5 ? Contours '' ' ' Ol ^ 0 | O l X A I U —

INTERPRETATION

M Strong increase in polarization accompanied by m arked decrease in resistivity,

Q Well defined increase in polarization without marked resistivity decrease.

D Poorly defined polarization increase with no resistivity signature.

T Low resistivity feature.

Scale 1:250025 0 25 50 75 100 126

(metres)

W.WASSENAAR

INDUCED POLARIZATION SURVEY WASSENAAR PROPERTY

STRATHCONA TOWNSHIP , ONTARjQ

Dote: W /:?/]?, inteipic'tolion: [D CHARM' (CLOLOCO) PHOL'NIX VX. RX

REMY BELANGER (GEDPhffSIG^L OWRACIVR)Software fur /he forth Sciences ) 5

31M04SE2007 2.20529 RIDDELL 260

31M04SE2007

2.20529

RIDDELL

270

li

O

LO

o to-H K

oo

o

o

fi II

II li

t

S!

t

t?

CTi

PO

fe

i

CTV

en

uLi

v

s X ;-

x 2

\ fcs

N^

it

\ \

B

\ K

\

x \

S

'! K g

^\

St

\

\ 11

\s

i

-

\ \ \ // \\

M n

U:

-:.n

00 (J1

oo

g

o

T)

Vitf;

RTRE OEN

00 00 m z

. w"

IT,

^,

a 8

D

f D

LT.

~

-i 0

S o

Bg

.0 —

—

.

n

g-0

'ft

! Q

ir,

en - —

, ^.NJ

ro

b

uo

CD

'-

S o

J-

ci

O 00

aHK

in o

H tn *p oH

ROO POCr- r? 7 r. T -r

.'938 J l y

OJ Oj

RESISTIVITY OHI/-METER3

PHASE

M RAO

POO ROO

ll

.19 L2938

L

LO Lo

Filter

2 f (fi S 1+50 S HOP S 0+50 S^

676 724 S&3 I2C8 1401 1204 1*1

Of 00 Q+50 H____ l f (xj M 1+60 N 2+00 N_____ g 150 N_____|

13-76 2+75 2791 3+50 3M8 J593 4S8 5341 51)68 5087 48I + 4759 5291 Filter

i982 - 118? -— 897

0 = 2 1IM ; 413 ~—- 587 7 TT^O- '

n-3 Mi 7134 -^-., 573IK n i0=4 Ml N.—— 174

(1=6

474^^-924 v fil ? v 1626 xx 405 ^-' 90J^ 1584 ^ 3S35 3E2S HIS 5862

940 ^ T77J i VA X 666^—- 451 ' /'S\ V \ 7 ///., ^

... . ... , , ..., -— — 2749 1579 2B34 3647 +COS 7g1l \\ \ I II/' 11 i l /' \ '~J \ \ "^ \ 7

2273 N 1521 ^ ( tBTj^, 942 5063 , 5401 2461 2126 I2E2 4S62 . M52 TO* TOS l SW1 y

6C4\ X I2?7 v 20IM j 10Q8 1559 — 1/64 5SS7 ^823 "2958^ 2476 i 1050 W06 4630 ^ 624J ^ 474S -^ 740J

109i 795 16+4 ~" |j45"'--' IfiSO 2752 J087 4865 5364 34IZ 3452

4MB 302? 3596 3123 2747 ZSJl~——-- vi ^ /^^-, \ J t

3DM 3500 \, 6571 6105 -^ 3979 +917 2W4 6515

4702 42W~" 4+94 9320

2-KX) S

Filter 21

11=1

HW S 0+50 S 0+50 N I+OO N 1 + 50 2+00 N 7+50 N

3C W .51 21 50 M

v - (?4 N 37 40 - ?2 ?1

35 H 13 ^-.. J2: 31 2f' ?7 19

34 ^29 L'6 24 '"'. IB

n=5

l l j14 7 54 55

52 J5

^ \ 21 ' K ( 3 3 +S W'

UN 17 17 \ 44 43 . i5 7 X 10

\ \ l \4fi 52 \ 15 ,' 2 7 . ) 9 . ^

'- 35 \

7 V '' \ J M " '^--S2H /' 14 11 —— 15 \ 24 - 20

?4 25

31 — 28

23 21 Filter

20 16 n =]t

^j i ^

U n -- j

RESISTIVITY OHM-METERS

PHASEMRAD

Line 000 W011 x 'l*-- Dipole Act a

na

Filter

a = 2 5.0 M

Logarithmic Contours

plot point

l, 1.5. 2, 3, b, 7.5, 10,..

INTERPRETATION

Strong increase in polarization accompanied by marked decrease in resistivity.

Well defined increase in polarization without marked resistivity decrease.

D Poorly defined polarization increase with no resistivity signature.

Low resistivity feature.

Scale 1:250025 50 75 100 12525___O

(met res')

W.WASSENAAR

INDUCED POLARIZATION SURVEYWASSENAAR PROPERTY

STRATHCONA TOWNSHIP , ONTARIO

rvite: 99/12/24 Interpretation: ED CHARTRE (CtiOLOGISl) PHOENIX V--5 RX

BELANGER (GEDPW3&L COWWC1VR)

mineral expl proj 1999 geophys & geol survs … · mat was borrowed from the mndm in kirkland...

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