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REFERENCES

AREAS WITHDRAWN FROM D ISPOSITION

S R vim AC! '••K.H'.S V! R MINING RIGHTS

ilssj i . piiiMi Ouli-r No D*t* Difpoliliun File

) SECJ6/80 W 18/82 24/11/82 S. R 181089

) SEC. 36/80 W 28/83 20/8/83 S R 188541

Reserve F looding R ights t o contour 905* G. S.C. on Aguasabon R iver 9 Big Duck C reek for H.E.RG ofOntario File: 132730.

Land under L"oke Superior withdrawn from stoking by O.C - 30 April 1912. '

T errace Bay Township extends to the International Boundary .

LEGEND

A:J[. R(.M

OTHER R' '-MIS

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REPORT ONTHE SCHREIBER PYRAMID PROPERTY

PRISKE TOWNSHIP

NTS 42 D/14E

THt

RECEIVEDMAR -

MINING LANDS SECTWM

A. Jolin Feb. 8, 1985

REPORT ON THE SCHREIBER PYRAMID PROPERTY

PRISKE TOWNSHIP

NTS 42 D/14E

INTRODUCTIONGround magnetometer, HEM and VLF surveys were carried out over the

Schreiber Pyramid property by Northwest Geophysics from November 15, 1984 to November 25, 1984. A total of 10.9 km of picket and base lines which cover the 6 claims, were surveyed. The property is accessible by an old bush road between Cook Lake and a hydro line which is immediately north of the property.

PREVIOUS WORKThe 6 unpatented claims cover the old Schreiber-Pyramid Gold Mines

property on which 2 gold-bearing quartz veins were exposed and trenched by Kenecho Gold Mines in the 1930's. The property was held by several

groups during the late 1950's and early I960 1 s but no significant work

was done. In 1969 Zenmac Metal Mines Ltd. drilled 5 shallow holes on

a base metal occurrence south of one of the veins. One foot of massive

sulphides (cp-sph-po) grading 4.56* Cu and 19. 21 In was intersected at

a vertical depth of about 50 feet. The sulphide zone occurs at the

contact between cherty sediments and pillowed mafic flows. The property was mapped by M. Carter of the Ontario Geological Survey in 1980. It is

underlain by mafic flows with thin, conformable, northwesterly trending beds of chert-magnetite iron formation. Stratigraphic 'tops' are interpreted to be to the northeast.

RESULTS OF THE GEOPHYSICAL SURVEYS

The anomalies outlined by these geophysical surveys are discussed in the appended technical report prepared by A. Lambert of Northwest Geophysics. Copies of maps of the data are also included with this report.

- 2 -

CONCLUSIONS

Two conductive zones were located by the geophysical surveys.

The one north of the baseline on line 5W has a coincident magnetic

high associated with it and it is also along strike with known copper-

zinc mineralization. A weak conductor on lines 2W and 1W is coincident

with trenches associated with gold-bearing quartz veins. Follow-up

geological mapping and stripping is recommended to evaluate the extent,

significance and relationship of the conductors and mineralization.

A. Jolin

February 8, 1985

STATEMENT OF QUALIFICATIONS

I, Andre" Jolin hereby certify that:

1) I am a Geological Technician residing at 476 Dawson Street, Thunder Bay, Ontario. I have worked as a geological and geophysical technician since graduation.

2) I earned a College Diploma in Mining Technology from Le College du Nord-Ouest (Rouyn, P. Quebec) in 1979.

^V^vQ-

Andre" Jol in February 12, 1985 Thunder Bay, Ontario

42D14SEM7* 2.7856 PRISKE 020

NORffiWEST GEOPHYSICS LID.

GEOPHYSICAL SURVEYS

SCHREIBER PYRAMIDS PROPERTY

42DMSEM7* 2.7856 PRISKE020C

TART .E OF CONTENTS

Summary of Results and Recommendations

PAGE

1

1,2

2

3

4

Chart I

Introduction

Geology and History

Survey Procedures

Discussion of Results

Conclusions

SUllARY OF RESULTS AND RBOCMEMaTIONS

One geophysical surveys of the Schreiber Pyramids Property have

yielded two interesting anomalous features. Zone SP-1 appears to be

on strike with five previously drilled exploration holes, one of which

intersected high grade copper-zinc mineralization over one foot. The

other zone SP-2 is also interesting in that it appears to have been

worked for gold content and further work on it would be encouraging.

There are also some minor magnetic features to investigate as well.

The grid should be mapped in detail, it will be iirpDrtant to

locate and resample as many of the old workings as possible. Some

of them are on the anomalies we have discovered/should help in

evaluating them. It is also important to locate the holes drilled by

Zenitac in 1969, the logs are available for them and the information

available will be significant in the evaluation of zone SP-1. Mapping

will also help identify the sources of the less prominent magnetic

features as well.

If warranted, consideration should be given to having intermediate

grid lines cut and surveyed on some parts of the grid, particularly

over zones SP-1 and SP-2.

It is also recommended that additional claims to the east and the

northwest be acquired as these anomalies strike off the grid in these

directions, particularly the east.

INTRODUCTION

Northwest Geophysics Ltd. was contracted in November 1984 to cut

lines and conduct geophysical surveys on six unpatented mineral claims

in the Schreiber area. This claim group comprises part of a group of

claims that was originally known as the Schreiber Pyramids property.

The property is accessible via a bush road that leaves Schreiber

and passes west and then north of Cooke Lake, depending on road conditions

you may drive within 1-2 miles of the property.

Baselines and tielines were cut with powersaw, picket lines were

cut at 100m intervals and stations picketed every 25m1 s along the lines.

A total of 10.9km of line were cut.

The geophysical surveys that were carried out were magnetometer,

VLF-EM and horizontal loop EM. The purpose of the surveys was to locate

previously discovered zones of gold, copper, lead and zinc mineralization,

possibly extend these zones and/or located new or undiscovered zones

of mineralization.

GEOLOGY AND mSTOBY

The showings on this property appear to have been originally discovered

in 1934. Since that time there have been eight diamond drill holes

(totalling 2,400 feet) reported. There are also numerous trenches, an

adit and an open cut located on the property.

The area was napped in 1980 by the O.D.M. and a preliminary map

of this information (Map P-2417) at a scale of 1" to 1/4 mile is

- 2 -

available. The geological and historical information in this report

was taken from that map.

The property is underlain mainly by mafic roetavolcanic rocks with

some minor gabbro, amphibolite intrusives. There also appears

to be tvro narrow metasedimentary hanfla intruding from the northwest. There

are several mineralized zones on the property including 5 known quartz

veins carrying gold mineralization. There are also occurrences of

copper, lead and zinc.

SURVEY PROCEDURES

MAGNETIC: The magnetic survey was carried out with an EDA 375 magnetometer,

an EDA Omni IV base station magnetometer was used for diurnal control.

Readings were taken at 12.5 meter intervals along the lines.

VLF-EM; The instrument used for this survey was a Geonics EM-16 unit,

readings were taken along the lines at a 25m spacing and 12.5m spacing

over the anomalies. The transmitter used was Cutler Maine ( freq^V.ohz)

and all readings were taken facing north. Both inphase and quadrature

readings were taken.

HORIZONTAL LOOP; An Apex Parametrics Maxmin II+ unit was used for the

survey, inphase and out-of-phase readings at two frequencies ( 1777 t

444 hz) were taken every 25m along the lines. Coil spacing was 100 meters.

All of the geophysical results have been plotted at a scale of

1:2500 and comprise 4 map sheets which accompany this report.

- 3 -

DISCUSSION OF RESULTS

There are two prominent anomalous features and several minor

features on the grid. The first zone SP-1 is a dipole magnetic

anomaly, peaks on line 400 W, has a coincident VUF anomaly along its

entire strike length and a coincident horizontal loop anomaly on line

500 W only. The maxmin anomaly is short, narrow and maybe located off

line to the east. It has been interpreted to have a conductivity in

the order of 15 mhos and a depth of 40 meters. A profile plot of zone

SP-1 has been incorporated with this report. This zone is probably

associated with a mineralized contact between the metasediments and the

mafic metavolcanics.

Zone SP-2 is a strictly magnetic anomaly having no coincident

horizontal loop or VLF anomaly. It is also a dipole anomaly, its peak

is on L-200 W at 125 S on the south shore of a small pond. This anomaly

appears to be within a band of mstasedimentary rocks and is likely caused

by magnetite mineralization within them. It also should be noted that

there are indications that this feature may fold east of the grid and

come back onto the grid south of anomaly SP-2.

One other anomaly SP-3 should be noted, it is a 2000 gamma anomaly

and may have a very weak coincident VLF-IM anomaly, however, it is very

narrow and short.

There are several other minor magnetic features, both highs and

lows, throughout the grid. They are probably of little significance as

they are generally short isolated features and have no coincident electro

magnetic anomalies. This does not mean however that they should be

overlooked in further evaluation of the property.

- 4 -

CONCLUSIONS

The linecutting and geophysical surveys on the Schreiber Pyramid

property were carried out between November 15 and November 25, 1984.

The grid is at 300 to the strike of the geology and this has led to

minor problems in the plotting and interpretation of the magnetometer

results. There is a powerline located just north of the grid, this

affected the YLF survey in the northern part and the readings in that

area are of little value. However, the maxmin and magnetometer survey

were unaffected and it is unlikely that anything has been missed because

of this. Extreme relief in some areas affected the horizontal loop

survey, however these effects are obvious and do not appear to complicate

the interpretation of the results.

This report was written by A. J. Lambert a geological technician

employed by Northwest Geophysics Ltd. who personally supervised the work

on this property.

Submittal and acceptance of this report and the accompanying maps

fulfills the obligations of Northwest Geophysics Ltd. for the Schreiber

Pyramids property.

Signed A. J. Lambert

Northwest Geophysics Ltd.

-So

l i(y g: o - f+oo w/

y

Ministry of Natural

Ontar.

Report of Work(Geophysical. Geological. 4J tfT Geochemical and Expenditures)

42014SEM7* 2.7856 PRISKE

Mining Act

90O

. Do not use shaded areal below.Type of Survey(s) HORTZONTflf".owolh'p or

GEOPHYSICAL AND LINECUTTING; VLF-EM; MAGNETOMER; LOOP-EM T PRISKEOaim Holder(s)

ANDRE JOLINProspector's Licence No.

F.-W76Address

APT. 1. 476 DAWSON STREET. THUNDER BAY.. OMTARTpSurvey Company

NORTHWEST GEOPHYSICS LTD, THUNDER BAY. -ONT.

P7A 3V9 - -. —.-——Date of Survey (front A to) Total Miles of line Cut

10.9 KmName and Address of Author (of Geo-Technical report)

ANDRE JOLIN, APT, l, 476 DAWSON STREET. THUNDER BAY. ONTARIO P7A 3V9Credits Requested per Each Claim in Columns at right Mining Claims Traversed (List in numerical sequence)Special 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 totaKs) here

Airborne Credits

Note: Special provisions credits do not apply to Airborne Surveys.

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other m p.gu

Geological

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

-Other

Geological

Geochemical

Electromagnetic

Magnetometer

Radiometric

'Days par Oaim

40

20

20

Days per Claim

Days per Claim

Expenditures (excludes power stripping)Type of Work Performed

Performed on Cujim(s)

Gale ulation of Expenditure Day* Credits Total

Total Expenditures Days Credits

s 1-1^1=1 1Instructions

Total Day* Credits may be apportioned at the claim holder's choice. Enter number of days credits per claim selected in columns at right.

Date 1 Recorded Holder or Agent (Signature)

FRRRIIARY 12 . 1 QRS A-^/xfj ^ * JdvXx^-^

Mining OaimPrefix

TB

iSwniSsJ^iSSS^JStf!:

^•^•"Vic""!"^.'

r* - ; ~ y* -

^P

^. I-"..', '-"lv

Number

773591

592

593

594

S9S

77-jSQfi

mi

Expend. Days Cr.

^ w* *Rt(i. L L}

•WG U

7

/Vi

For Office Use Only

Recorded

W

FpJ^. 15/^5

XI. j. 7

Mining ClaimPrefix

'-V"';:

- '. -.'

m m'v^l

Number

D^ ^3 m

.•''-'"^•iti -,

m ——

Expend. Days C'.

Total number of mining claims covered by this r report of work. D

"^^^^/^^

JSI^DE^^^,

Certification Verifying Report of Work , S J\ hereby certify that 1 have a personal and intimate knowledge of the facts set forth in the Report of Work annexedllereto. having performed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Penon Certifying

ANDRE JOLIN, APT. 1 476 DAUSON STRFF/r THUNpF.R RAY, ONTARIO P7A 3VQ1 Date Certified

FEBRUARY 12.1985Certified by (Signature)

1362 (81/9)

Ontario

Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

TO BE ATTACHED AS AN APPENDIX TO TECHNICAL REPORTFACTS SHOWN HERE NEED NOT BE REPEATED IN REPORT

TECHNICAL REPORT MUST CONTAIN INTERPRETATION. CONCLUSIONS ETC.

l

a ubu. O

MINING CLAIMS TRAVERSED List numerically

Type of Survey(s) mrnPHYSTr.AT. SURVEYS VLF. MAGNETOMETER, HORIZONTAL LOOP E-M, LINECUTTING

Township or Area PBTSKE TOWNSHIP MAP G-631^-^—-^—^— Claim HrtlHgrft) AwnRE ^JOLIN, Ant, l - 476 Dawson Street

Thunder Bay. Ontario P7A 3V9______

Survey nnmpany NORTHWEST GEOPHYSICS LTD. THUNDER BAY

Author of Report ANDRE JOLIK_^_______^^_______ Address of Aiiihnr APT. 1. 476 DAWSON ST. THUNDER BAY. ONT

Covering Dates of Survey NOVEMBER 15.1984 - FEB. 8. J985(Enecutting to office)

Total Miles of Line r...t 10.9 Km.^__^___^_______

SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.ENTER 20 days for each additional survey using same grid.

Geophysical—Electromagnetic—40—Magnetometer 20

—Radiometric—————

DAYS per dana

VLF-EM 20

Geological.Geochemical.

AIRBORNE CREDITS (Special pre credits do not apply to airborne furvcyt)

Magnetometer. .Electromagnetic. . Radiometric

D ATE:

(enter days per claim)

SIGNATURE: i. ^-/cyv-v^^^of Report or Agent

Res. Geol.. .Qualifications.Previous Surveys

Fife No. Type Date Claim Holder

TB(number)

773591

.592.

XB.

•k*

i

TOTAL CLAIMS-

837 (5/79)

GEOPHYSICAL TECHNICAL DATA

GROUND SURVEYS — If more than one survey, specify data for each type of survey

Number of gta t;™.c 872 -Magnetic: 436 HEM S VLF Nnmtvr Of Readings l P**r Si-aMnn

Station interval 12.5 m (Magnetic); 25 m (HEM S VLF) Line sparing 10Q M^———^—- Profile "-a!* l cm = 25% (VLF AND HEM)——^^——^—^^^^—^^^^-^—^————^—- Contour interval 500 gammas (Magnetic)-^^^^^^^^^^^———-——^^^^^^^^—

c

Instrument. EDA 375 Magnetometer and EDA Omni IV Base Station

Accuracy — Scale constant Q-3—gamma Diurnal correction method. at-at-irm

Base Station check-in interval (hours).Base Station location and value Lake south of R-niin T .alee: S Q. OOP Pammag

yHwzssiHu(dJbQ

soio

InstrumentCoil configuration HORIZONTAL

Coil separation ———25 M.———————Accuracy______0.2^ to l.QQZMethod:

MAXMIN II; GEONICS EM-16

Freq uen cv M I

O Fixed transmitter O Shoot back

t A LL.L W-r-^^—^——rnt-ler- Maine (2A.O Hz)

line [D Parallel line

Parameters measured(specify V.L.F. station)

smA nni--nf-phag^ response as percentage of primary field (HEM)In phase and quadrature readings (VLF)

Instrument.Scale constant.Corrections made.

Base station value and location.

Elevation accuracy.

Z OH

N

O au

w (ja z

n

Instrument __________ Method D Time Domain Parameters — On time ———

- Off time ——— Delay time ___— Integration time.

l l Frequency Domain _ Frequency _____ _ Range -————^——

Power.Electrode array — Electrode spacing. Type of electrode

Ontario

Ministry ofNaturalResources

February 26, 1985.

MEMORANDUM TO:

D i rectorLand Management BranchRoom6643, Whitney BlockQueen's ParkToronto, Ontario oM7A 1W3

SUBJECT: Technical Data - Mining claims TB773591 et al Work Report #Bk - Andre Jolin __

Enclosed please find duplicate copies of technical datacovering mining claims TB773591~96 inclusive submittedby Andre Jolin.

Gather i ne J. All am Acting Mining Recorder Thunder Bay Mining Division Ontario Government Building 435 S. James Street P.O. Box 5000 Thunder Bay, Ontario P7C 5G6

Telephone: (807) ^75-1311

:cg

Encl .

RECEIVEDMAR - .'i 1985

MINING LANDS SECTION

Mining Lands Section File No . /oSCs

Control Sheet

TYPE OF SURVEY tX GEOPHYSICAL

_____ GEOLOGICAL

____ GEOCHEMICAL

EXPENDITURE

MINING LANDS COMMENTS:

Signature of Assessor

r s Date