IB TABOR LAKE 010

Diamond Drilling

Area Tabor Lake Report NQ 15

Work performed by: Monte christo Resources

Claim NQ

K 594305

K 590672

Hole NQMC-1MC-2MC-3

Footage275375276

DateDec/83Jan/84Jan/84

Note(i)(1)(i)

Notes: (!) #52-84

AWL 005(7-69)rev 9-72

Report

on

Diamond Drilling

Monte Christo Resources

Kuryliw - Sakoose Melgund Property

District of Kenora, Ontario

I'Vbruary '}_'•>, 1 ()H/-t Chester .1. Kuryliw, M.Sr., P.Kng,Consu It ing (it>o 1 <>g i st

Index

Titie Page

Property, Location and Access

]ntrodneti on

General Geology

Economic Geology

Table of Formations

Results of Diamond Drilling

Conclusi ons

Reconimendat i ons

Cert i ficatc

1). Drill Logs MC-1

I). Drill Logs MC-2

I). Drill Logs MC-3

Vert ical Section MC-1

Vertical Section MC-2

Vertical Section MC-3

JLLOCATION MAP

SCAl £ /" */? IV !'-

Property, Location and Access

The property consists of a single group of twenty claims. 3;our

claims are located in the south part of Melgund Township and sixteen

claims in the unsurveyed Tabor Lake Plan. This claim group is located

about 30 miles due east of Dryden, Ontario.

The property is accessable from Trans-Canada Highway Number 17

at a point about 30 miles east of Dryden, Ontario. A branch gravel

road to the south at Bcvutops Corners traverses the western part of the

claim group about four miles south of Highway 17. The CPR rail line

is located about six miles north of the property at Dyment, Ontario.

The Property

The claim group consists of the following twenty claims:

In Me!gund Township: K 594295K 594296K 594297K 594298

Jn Tabor Lake Plan M 2653: K 594287K 594288 K 594289 K 594290 K 594291 K 594292 K 594293 K 594294 K 594299 K 594300 K 594301 K 594302 K 594303 K 594304 K 594305 K 590672

Introduction

This claim group was staked in May 1982 over ground that appeared

to have geologic potential for the discovery of a gold deposit with

associated base metal mineralization similar to the mineralization of

the underground Sakoose Mine veins.

The line culling was carried out by contractors Adrian and Judy

Kuryliw on I he main grid during June and July of 1982. This consisted

of 1.8 miles of base lines and 17.2 miles of picket lines.

The geologic mapping was carried out in the field on the main

grid by Chester J. Kuryliw (this writer) during July and August 1982.

The mapping dala was plotted on a plan scale 1" = 200 feet which

accompanies this report.

A detailed line grid was cut in the southeast corner of the claim

group to obtain more detail along a EM conductor that extended under

Lake and Bog. This line cutting was carried out on contract by

A. Grail on of Wawa, Ontario from November 28 to December 3rd, 1982.

Unusually favourable weather conditions occurred where lake and bogs

were fro/en but the ground was bare of snow. This writer mapped the

area immediately after the line cutting and this mapping data was

plotted on the same plan scale 1" = 200 feet that covers the main grid.

This coloured plan 1" = 200 feel accompanies this report.

In December 1983 diamond drilling was started to test the two

conductors located on claim 594305 and one conductor located on 590672,

This drilling was done by Kenora Diamond Drilling for Monte Christo

Resources, who opt ioned the claim group. The diamond drilling was

completed January 15, 1984. Three holes were drilled totalling 92(>

leet .

General Geology

The rocks of the area are precambrian age. The genera] geology

of the region is covered in OGS report 202, "Geology of the Boyer

Lake - Meggisi Lake Area" by C.E. Blackburn.

The volcanic belt of the area with some included sediments extends

from Lake of the Woods to the west and to Melgund Township on the east

at the Revel Granite Batholith. The precambrian volcanic sedimentary

series occurs as major synclinal structures and their trends are

largely governed by the location of surrounding granite batholith

intrusions. The rising diapiric granite batholiths were in many cases

the tctonic engines that forced the folding and crumpling of the pre

cambrian volcanics and sediments. The trends of the folds occur as

accommodating directions related to the granites.

Some strong faults are known in the region such as the Manitou

Straits Fault.

Numerous gold occurrences are known in the area, some were small

producers but to date no major producer has been found.

The Revel Batholith which occurs along the eastern boundary of

the property appears to have caused the crumpling of the volcanic

scries which underlies the property. The series of Felsic and Volcanic

tuffs and flows were crumpled into a series of anticlines and syn-

c lines that appear' to form part of a major syncl inorlum. The fold

axes trend northeasterly and incline northwesterly at 60 - 70 .

Two anticline's and one syncline were recogni/ed in the form of

"M" in cross seel ions with their individual axes nearly 2 mile apart.

ll is interpreted that there is a relationship of gold and associated

base metal minerali/ntion that occurs along the projected trace of

the fold axes in rhyolitic tuffs.

Economic Geology

No known go]d deposit has yet been located on the property, but

the property surrounds the site of the old Sakoose - Van Houten gold

mine on three sides.

The Sakoose property was first operated in 1899 - 1902 at which

time 7,735 tons of gold ore were shipped by rail to a mill in Keewatin

Ontario. The remnants of that gold deposit show a flattened portion

that attained a thickness of up to seven feet and according to report

dated February 1935, by Charles Spearman, sampling of mine pillars

averaged 0.28 oz gold and 0.26 oz silver.

A bulk sample sent for experimental metallurgical tests to the

mines branch in Ottawa was assayed, it ran 0.28 oz Au; 0.24 oz Ag;

0.28% Cu; 0.50% Zn; 0.05% Pb; and 0.03% As. The most recent tonnage

estimates indicate 44,000 tons at 0.25 oz gold.

The original decision to explore the property surrounding the

Sakoose Mine was based upon the possibility that the associated

Pyrite and base metal mineralization which occurred with the gold

deposits could be picked up by electromagnetic surveys if another

such deposit occurs.

The discovery of an EM conductor under overburden bog and

lake in the south-west corner of the property is most encouraging.

This conductor should be tested by diamond drilling of at least two

drill holes to determine if gold mineralization is present in the

conduct or.

Table of Formations

Genozoic

Pleistocene and Recent

Sand

Clay

Organics - Muskegs

Rock!and Ridges

Precambrian

Quartz Veinlets

Acid Intrusives

Grani te

Quartz Porphyry Dykes

Feldspar Porphyry Dykes

Volcanics

Rhyolitic Formation

Rhyolite - Massive

Rhyolite - Sheared

Rhyolite - Porphyritic Tuff

Rhyolite - Tuffs

Rhyolite - Agglomerate

Andcsite - Dioritized, Metagabbro

A n d e s i 1 e

Dacite

Rhyolitic Tuffs - Magnetic

Results of Diamond Drilling

The diamond drilling program was successful in intersecting the

indicated electromagnetic conductors that were the targets of this

test drilling.

Drill Hole MC-1

The conductor intersected was discovered to be films of graphite

along fine and numerous fracture planes.

Drill Hole MC-2

In this drill hole two conductors were intersected, each consisted

of a combination of iron sulphides and graphite in a banded felsic tuff

that carried a few visible traces of chalcophyrite and sphalerite. In

spite of the presence of the sulphide mineralization there was no sign

ificant si 1icification with the result that gold values were not

encountered in the sampled sulphides.

Drill Hole MC-3

In this drill hole the conductor consisted of a series of narrow

bands of pyrrhotite in andesitic Luffs with visible traces of chalco-

pyritc and sphalerite. No significant si 1icification was present

and no gold values were encountered in the sampled sulphide.

Conclusions

The diamond drilling program was successful in intersecting the

conductors and also the sulphide mineralization or graphite that

formed the conductive trends. Unfortunately no significant si 1 dei

fication accompanied the mineralization so that the assaying of the

samples did not indicate any significant gold values.

The potential of the property for hosting gold bearing structures

has not been ruled out. Activity on adjoining properties to the

north and to the south by Teck Corporation may uncover some new

gold bearing structures.

This drilling will be filed for assessment work and the claim

group will be put on hold to await development.

February 2 5, 1 984 Chester J. Kuryliw, M.Sc., P.ling.Consulting Geologist

Recommendations

No further work is recommended on the property at this time.

Any significant discoveries on the adjoining properties would warrant

a re-evaluation and further work would then be recommended.

February 25, 1984 Che iw, M.Sc., P.EijgConsulting Geologist

CERTIFICATE

I, Chester J. Kuryliw of 50 Thunder Drive, Dryden, Ontario, do hereby certify that:

(1) I am a Professional Engineer and I am currently employed as a Consulting Geologist for several mining companies.

(2) I am a graduate of:The University of Manitoba B.Sc. Degree, 1949 The University of Manitoba M.Sc. Degree, 3966

(3) I am a registered Engineer of the Association of Professional Engineers of Ontario and also Manitoba. I am a fellow of the Geologic Association of Canada, also a member of the Canadian Institute of Mining and Metallurgy.

(4) I have practiced by profession for over 31 years, most of those years at gold mines, during which time I often planned, super vised and directed underground exploration, development and production.

(5) My report is based upon my own work, which consisted of thesupervision of the diamond drilling program, examining, logging and sampling of the core. I also drafted the drill hole sections incorporated in this report.

'ebruary 25, 1984 Chester J. Kuryliw, M.Sc., P.Eng

\

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NamJ^^J"ostal Acid. ess of Recorded Holder , ',(1 "I KjM>L'.r! Ofl. 52F«9SW0e26 15 TABOR LAKE 300

Summary of Work Performance and Distribution of CreditsTotal Work Days O. claimed

for Performance of the following work. (Check one only)

[~~1 Manual Work

Qshaft S inking Drifting or other Lateral Work.

Q Compressed Air, other Power driven or mechanical equip.

Q Power Stripping

[^DiDiamond or other Core drilling

Survey

All the work was performed on Mining Claim(s):

Required Information eg: type of equipment, Names, Addresses, etc. (See Table Below)

Date of Report okier/6r Agent

Certification Verifying Report of Work

1 hereby certify that 1 have a personal and intimate knowledge of the facts set forth in the Report of Work annexed hereto, havLnjKperformed the work or witnessed same during and/or after its completion and the annexed report is true.

Name and Postal Address of Person Certifying , / ^.. .... 1 1 e-r. n CiifCHESTER J KURYLIW, M.sc., P.BJG,COM C ULT!MG Gmin£KT , ' j

bOTHUNDEHDR. o y^ c^^^f.) ^

Table of Information/AttachmentsTJequired^y^p, Mining Recorder ' / ss \/f

Type of Work

Manual Work

Shaft Sinking, Drifting or other Lateral Work

Compressed air, other power driven or mechanical equip.

Power Stripping

Diamond or other core drilling

Land Survey

SpecifJ§7nf?)?rM(iai>er type

Nil

Type of equipment

Type of equipment and amount expended. Note: Proof of actual cost must be submitted within 30 days of recording.

Signed core log showing; footage, diameter of core, number and angles of holes.

Name and address of Ontario land surveyor.

Other information (Common to 2 opmore types)

Names and addresses of men who performed manual work /operated equipment, together with dates and hours of employment.

Names and addresses of owner or operator together with dates when drilling/strippingdone.

Nil

^f Attachments

Work Sketch: these are required to shov the location and extent of work In relation to the nearest claim post.

Work Sketch (as above) in duplicate

Nil

768 (81/3)

D.D.HOLE M.C.-I S-30°-E

MONTE CHRI5TO RESOURCESKURYLIW, SAKOOSE-MELGUND CLAIM GROUP

DIST. OF KENORA, ONT.

VERT. SECTION D. DRILL HOLE M.C.-f

SCALE; I"* 20.O

ZTS'OOf 1

52F09SN0026 15 TABOR LAKE£00

D. D. HOLE M.C.-3 S-5O°-E

MONTE CHRIS TO RESOURCESKURYLIW, SAKOOSE-MELGUND CLAIM GROUP

DIST. OF KENORA, ONT.

VERT SECTION D, DRILL HOLE M.C.-3

SCALE- I"* 20'. O

52Ffl9S#«026 15 TABOR LAKE 210

MONTE CHRIS TO RESOURCESKURYLIW, SAKOOSE-MELGUND CLAIM GROUP

DIST, OF KENORA, ONT.

VERT. SECTION D. DRILL HOLE M.Q-2

SCALE: /"*2OfO

52F09SW0026 IS TABOR LAKE 230