regal goldfields limited - ontario€¦ · held by the duvan copper company limited in 1964....

JAMES E. TILSLEY ft ASSOCIATES LTD.

32005SE8039 a. 12191 BEN NEVIS 010

REGAL GOLDFIELDS LIMITED

Exploration Program - 1988

BEN NEVIS PROPERTY

Larder Lake Mining Division Ontario

James E. Tilsley Si Associates Ltd. Consulting Geologists and Engineers Gp. BOX 115, R.R. #2 Aurora, Ontario, Canada L4G 3G8

February 06, 1989.

JAMES E. TILSLEY 8c ASSOCIATES LTD.

33DeSSEee39 2.18191 BEN NEVIS 010C

TABLE OF CONTENTS

SUMMARY AND CONCLUSIONS

INTRODUCTION .

LOCATION AND ACCESS .

CLIMATE, TOPOGRAPHY AND LOCAL RESOURCES

PROPERTY .

SURFACE RIGHTS .

HISTORY .

GENERAL GEOLOGY .

MINERALIZATION

PRODUCTION .

RESERVES .

GEOLOGY AND DIAMOND DRILLING .

SAMPLING .

GEOPHYSICAL SURVEYS .

MAGNETIC SURVEY .

VLF-EM SURVEY .

RECOMMENDATIONS .

ESTIMATED EXPLORATION COSTS

REFERENCES .

CERTIFICATES .

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3

4

5

6

7

7

10

12

13

13

14

20

23

25

26

27

30


Appendices

Appendix I

Appendix II

Diamond Drill Logs Diamond Drill Sections

Copies of Assay Certificates

MAPS

Surface Geology 1:2500

Magnetometer Survey 1:2500

VLF-EM Survey 1:2500

North Sheet South Sheet



in pocket

JAMES E. TILSLEY 8t ASSOCIATES LTD.

SUMMARY AND CONCLUSIONS

Geophysical surveys have been completed over most of the

Ben Nevis property of Regal Goldfields Limited. Geological

mapping of 17 of the 35 claims was done before snowfall obscured

the outcrops. The surveys indicated four separate targets which

were diamond drilled by N. Morissette Canada Inc. of Haileybury,

Ontario. A total of 2008 lineal feet of NQ core was drilled in

five holes.

The best gold assay values returned from the core samples

taken included 0.688 g/t, 0.249 g/t, and 0.232 g/t, from an area

showing a magnetic anomaly with approximately 5?; pyrite mineral

ization (Diamond drill holes #2 and #3). Silicification,

carbonatization, quartz-carbonate veining, and zones of shearing

were observed in the core from all holes. These features

indicate conditions favourable for gold and for base metal

mineralization.

Further exploration of the property is recommended. The

suggested work program is designed to test for base and precious

metal bearing shear zones similar to those being explored on the

claims adjoining to the north. This work can be done most

effectively during the summer months.

Special attention should be paid to the most northwesterly

claims since the structure that hosts the most important

mineralized zones on the adjoining property strikes southwest

from Ranger Lake toward the north end of Pushkin Lake. Any


extension of that favourable zone would likely pass through

claims L-1015656, L-1015657, and L-1015658.

The cost of the recommended exploration program is

estimated at $46 639.00.


INTRODUCTION

In November, 1988, Regal Goldfields Limited acquired a

group of thirty-five mining claims in Ben Nevis Township, Larder

Lake Mining Division, Ontario. A base line was established

across the property in a northwest-southeast direction (azimuth

320 0 ), with profile lines cut every 100m. Stations were estab

lished at 25m intervals along the profiles.

Geological mapping of the property commenced on November 24

and continued until snow cover became too deep on November

29. Detailed geophysical surveys were then performed over most

of the property, finishing on December 13. This involved a

magnetic survey and a VLF-EM survey using an IGS-2 system

manufactured by Scintrex of Concord, Ontario. Claims L-1015655

and L-1015656 in the northwestern corner of the property were

not gridded nor surveyed. However, parts of these claims were

included in a ground electromagnetic survey by the Duvan Copper

Company Limited in 1964.

The geophysical surveys outlined several anomalies on the

property. Four of these targets were diamond drilled by N.

Morissette Canada Inc. of Haileybury, Ontario. A total of 2008

feet of NQ drilling in five separate holes was done between

December 19 and 31, 1988.

The work discussed in this report was completed at the end

of December, 1988. Maps with magnetic and electromagnetic data

as well as logs and sections of diamond drill holes are included

in the appendix.


LOCATION AND ACCESS

The property consists of a group of thirty-five mining

claims located in southeastern Ben Nevis Township, Larder Lake

Mining Division, Ontario.

The claims are situated approximately 25km north of Larder

Lake Station, 34km northeast of Kirkland Lake, Ontario and 48km

west of Rouyn-Noranda, Quebec. Co-ordinates for the property

are:

48 0 17' 00"N; 79 0 40' 00"W

The Ben Nevis property can be reached by following a

gravel-surfaced forest access road for 25km north of Larder Lake

Station, which is 2.8km north of Highway 66 along the Larder

Lake Station Road. Station Road is 1km east of the town of

Larder Lake, Ontario. The forest access road is not maintained

in winter and is thus restricted to snow machines or four-wheel

drive vehicles during those months. It is easily passable by

two-wheel drive vehicles during dry weather.

Larder Lake can be reached by taking Highway 11 north from

Toronto, through North Bay to Englehart. From Englehart,

Highway 624 is followed for 44km to the town.

An Ontario Northland railway line passes 25km to the south

of the property at Larder Lake Station. Daily air service to\

other major centers is available in both Kirkland Lake and

Rouyn-Noranda.


CLIMATE, TOPOGRAPHY, AND LOCAL RESOURCES

The area has warm summers and cold, relatively dry winters.

Summer maximum temperatures in the 30 0 C range are not uncommon

during July and August, as are winter minimums of -40 0 C during

December, January and February.

Total annual snowfall amounts to between one and two

meters, usually covering the ground from mid-November to April.

The Ben Nevis claim group covers moderately rolling ground,

with average relief of less than 15m. Several outcroppings of

bedrock rise abruptly through the glacial sands and gravels to

produce relief of over 60m. The central part of the property

has an elevation of 330m above sea level, while that of the

northeast corner of the property exceeds 380m above sea level.

Several small lakes are included, at least in part, within

the property boundaries. Pushkin Lake in the northwestern cor

ner and Captain Lake in the northeastern corner are each approx

imately 25ha in area, while Sylvia Lake in the southwestern

corner of the claim group is approximately 20ha.

Drainage from Pushkin Lake is initially into the Misema

River, while captain Lake and Sylvia Lake drain first into the

Little Misema River before reaching the Misema. From the Misema

River, drainage is to Blanche Creek, Lake Timiskaming, and the

Ottawa River.

While all water on the Regal Goldfields Limited property

eventually drains southward, water only 1km north of the


property is on the other side of the Arctic drainage divide and

flows northward via the Magusi and Abitibi Rivers into James

Bay.

Mining equipment, supplies, and services are available in

the nearby mining towns of Kirkland Lake, Cobalt, and Rouyn-

Noranda. Skilled labour is readily available in Kirkland Lake

and the surrounding area.

A small medical center is located in Larder Lake, while

hospital facilities are available in Kirkland Lake and Rouyn-

Noranda.

Industrial power and telecommunications facilities

parallel the railway line 25km south of the property.

A substantial part of the property has been logged and is

now dominated by second growth birch, poplar, and assorted

deciduous shrubs. Mature spruce and a few other conifers cover

the remainder of the claim group. All accessible merchantable

timber has been removed from the property.

PROPERTY

The property consists of thirty-five mining claims located

in southeastern Ben Nevis Township. The claims were staked by

Ron Crichton of Kirkland Lake for Thomas Obradovich and are

under option to the company.

The individual claims are on record at the Mining


Recorder's office in Kirkland Lake. Claim numbers are:

L-1015655 to L-1015689, inclusive.

SURFACE RIGHTS

The claims cover Crown Land and include only mineral

rights.

HISTORY

Larder Lake has a long history of prospecting and mine

development dating back to 1906 when it was the site of the

first gold rush in northeastern Ontario. The Kerr-Addison Gold

Mine, still in production today, was the first of several mines

in the Larder Lake area and began preliminary work in 1906. All

the other workings have since ceased operation.

Prospecting activity began in Ben Nevis Township soon after

gold was found in Larder Lake. Gledhill's 1928 study included

several observations of mineralization. Copper, molybdenum, and

gold were discovered in small amounts south and southeast of the

Clifford Stock (approximately 8km west of the Regal Goldfields

Limited property) by Captain Snipe and J. Bain (Jensen, 1975).

Copper, lead, zinc, and gold were found west of the

Clifford stock by E. O. Ehrhart and J. Martin, while copper,

lead, zinc, gold, and silver were found by P.- Roche and E. O.

Ehrhart approximately 2km north of the property (Jensen, 1975).


Laying out a grid over Captain Lake - December, 1988.

The Ben Nevis property looking northeastward along L1600E. Patterns in sky and snow are from frost crystals which formed on film at -29 0 C.

JAMES E, TILSLEY ft ASSOCIATES LTD.

ft

Three exploratory shafts were sunk on this latter prospect

between 1927 and 1929 by the Interprovincial Exploration Company

Limited. In 1936, the property was acquired by Canagau Mines

Limited, with dewatering and sampling commencing in 1937. Later

years saw several attempts to outline further extensions of the

mineralization. Electromagnetic and magnetometer surveys

covered the area in 1960, while a bulldozer was used to strip

the overburden in 1962.

Several other properties in Ben Nevis Township are known to

have overgrown pits and trenches near zones of minor

mineralization, but to date no production has occurred in the

township. (Jensen, 1975)

Parts of the two claims in the northwest corner of the

Regal Goldfields Limited property {L-1015655 and L-1015656) were

held by the Duvan Copper Company Limited in 1964. Magnetometer

and electromagnetic surveys were completed, but no anomalous

conditions were reported.

Cominco Ltd. filed an airborne electromagnetic survey flown

by Scintrex in 1971 which included that part of the property

north of an east-west line that passes through the outlet of

Captain Lake. This survey showed the peak of an anomaly in

claim L-1015658 just east of the access road at approximately

L900E/300N.

In 1979, an airborne electromagnetic and total intensity

magnetic survey was flown over Ben Nevis Township by Questor


Surveys Limited of Toronto, Ontario for the Ontario Geological

Survey. Flight lines were north-south, while the airborne

survey done for Cominco in 1971 had flight lines which were

oriented at 280 0 . The electromagnetic anomaly indicated

by the 1971 survey was not detected in the 1979 O.G.S.-sponsored

survey.

Finally, on November 7 of 1988, Westbank Resources reported

in the Northern Miner that it had discovered a polymetallic

showing in Ben Nevis Township immediately north of the Regal

Goldfields Limited property. Sampling was reported to have

yielded the following assays of lead, zinc, gold, and silver in

silicified shear zones:

Sample l - 11.^ Zn, 1.0 oz/ton Ag, 0.036 oz/ton Au, tr. Pb. Sample 2 - nil Zn, 7.3 oz/ton Ag, 0.83 oz/ton Au, 0.0 Pb. Sample 3 - tr. Zn, 6.0 oz/ton Ag, 0.632 oz/ton Au, tr. Pb.


GENERAL GEOLOGY

The geology of the Ben Nevis Township area was first

investigated in 1901 by W. J. Wilson who examined the rocks

along the canoe route from Kennedy Lake to Verna, Keith, and

Webster Lakes (published in Western Part of the Abitibi Region;

P.117A-130A in Summary Report, pt.A, Geol. Surv. Canada, p.271,

Vol. XIV.). After nearly 20 years of prospecting activity,

another study was done by C. W. Knight in 1919. (Ben Nevis Gold

Area; Ontario Dept. Mines, Vol. 29, pt. 3, p.1-27.).

Reconnaissance mapping continued in 1927 as part of a study

of several Ontario base metal areas by T. L. Gledhill. (Ben

Nevis, Munro, Kamiskotia, and Other Base Metal Areas, Districts

of Cochrane and Timiskaming; Ontario Dept. Mines, Vol. 37, pt.3,

p. 1-52).

A detailed study on the geology of the area was done by

L. S. Jensen of the Ontario Division of Mines, published in

1975 (Geology of Clifford and Ben Nevis Townships, District of

Cochrane; Ontario Div, Mines, GR132.). Geochemical exploration

in the township was completed in 1977 by W. J. Wolfe (Geochem

ical Exploration of Early Precambrian Sulphide Mineralization in

Ben Nevis Township, District of Cochrane; Ontario Geological

Survey Study 19). Several samples with anomalous values of

both zinc and copper were collected on the Regal Goldfields

Limited property in the area south of Captain Lake.

A table of the lithologic units in the Ben Nevis area

follows. (from Jensen, 1975)

10


Table 1TAHLE OF LITHOLOGIC UNITS FOR THE CLIFFORD-HEN NEVIS AREA.

CENOZOIC

QUATERNARY

RecentPeat, alluvium.

PleistoceneGravel, sand, till and clay.

Unconlotinily

PRECAMBRIAN

MIDDLE TO LATE PRECAMBRIAN (PROTEROZOIC)

MAFIC INTRUSIVE ROCKSOlivine diabase, quartz diabase.

Intrusive contact

EARLY PRECAMBRIAN (ARCHEAN)

FELSIC INTRUSIVE ROCKSGranodiorite, quartz diorite, diorite, syenite, feldspar porphyry and

quartz-feldspar porphyry.

Intruiire contact

MAFIC TO INTERMEDIATE INTRUSIVE ROCKSGabbro, quartz gabbro, hornblende gabbro and diorite.

Intruiivt contact

VOLCANIC ROCKSFelsic Volcanic Rocks

Rhyodacite and rhyolite: Massive, flow-breccia, tuff-breccia, tuff nnd lapilli-tuff.

Intermediate Volcanic RocksAndesite and dacite: Massive, pillowed, flow-breccia, tuff, nrgillite.

Mafic Volcanic RocksBasalt: Massive, pillowed, flow-breccia, tuff-breccia.


Jensen, (1975) stated that Ben Nevis Township is favourable

for precious and base metal exploration because of its proximity

to two economically important structures, namely the Destor-

Porcupine Fault to the north and the Larder Lake Fault approx

imately 25km to the south. Secondly, the township is situated

in a belt of volcanic rock contiguous with that of the Noranda

area in Quebec.

Regal Goldfields Limited's Ben Nevis property is underlain

by rocks of the Abitibi belt, an Archean aged greenstone belt

which extends from west of Timmins, Ontario, to east of

Chibougamau, Quebec. The rocks are Early Precambrian layered

volcanics of intermediate to felsic composition, with a few

interbedded sedimentary rocks.

Low-grade regional metamorphism has affected the bedrock of

the Ben Nevis area.

The township was glaciated during Pleistocene time and is

covered by till and glacial outwash deposits through which

bedrock is exposed. Several sand and gravel deposits have been

utilized for local road construction, including one at

L2000E/700S.

11


MINERALIZATION

In exploration activity since 1906, galena, sphalerite,

chalcopyrite, silver, and gold mineralization have been noted in

Ben Nevis Township,

The showing which has received the most attention over the

years is a prospect in east-central Ben Nevis Township,

approximately 3km north of the Regal Goldfields Limited

property. Originally staked by Peter Roche in 1926, develop

ment work has in later years been carried out by the Inter-

provincial Exploration Company and Canagau Mines Limited. This

prospect is found to be closely associated with strongly

foliated, carbonitized, and sericitized rhyolite tuff, tuff-

breccia and lapilli tuff of the lower rhyolite pyroclastic unit.

Mineralization is near the hinge-line of an anticlinal

structure which plunges south. The core of this structure is

occupied by the structurally thickened lower rhyolite

pyroclastic unit. Sphalerite, galena, chalcopyrite, pyrite,

pyrrhotite, silver, and gold occur in veins or massive

replacements in shear zones within altered rhyolite tuff, or as

disseminated minerals in adjacent sheared tuff. Alteration

products in the mineralized tuff include sericite, chlorite,

talc, and carbonate. Surface and underground work suggest that

the vein strikes east for 120m with a proven vertical depth of

99m, although it appears to be more accurately represented by a

vein stockwork rather than a single vein (Wolfe, 1977).

12


PRODUCTION

There has been no production of metallic minerals from the

Ben Nevis property of Regal Goldfields Limited, although gravel

has been mined for local road construction.

RESERVES

There are no known metallic mineral reserves on the

property.

13


GEOLOGY AND DIAMOND DRILLING

The geology of the Regal Goldfields Limited property was

mapped in part by R. Mueller between November 24 and 29, 1988.

The following claims were covered before the survey was term

inated for the season because of snow:

L-1015657 L-1015678L-1015662 L-1015679L-1015664 L-1015682L-1015669 L-1015683L-1015673 L-1015684L-1015674 L-1015688

L-1015689

Most of the property is underlain by Archean age volcanic

rocks of intermediate to felsic composition. Intermediate

volcanics underlie much of the central part of the claim group.

These include massive and pillowed flows of andesite and dacite,

as well as some flow breccia and tuff. Massive units are homo

geneous and grade upwards into pillowed flow units at the upper

and lower contacts of the lava flows. Pillows are found to be

elliptical and between 30cm and 60cm in diameter, with smooth

curvatures and bottoms with tails pointed downward, perpen

dicular to their long axes. These have been noted at

L1800E/900N in claim L-1015669, where light-coloured pillows are

surrounded by dark green selveges between lcm and 3cm thick.

Selveges are soft and weather deeper than the pillow.

Flow breccia contains fragments which are similar in

composition and colour to the matrix, with approximately 15*

subangular to subrounded fragments between lcm and 30cm in size.

14

JAMES E. TILSLEY 8e ASSOCIATES LTD.

Compositionally, andesite is made of 60 to 70?. plagioclase,

20 to 25?; augite, with accessory minerals quartz, magnetite, and

pyrite. Alteration has caused chlorite, calcite, saussurite,

albite, and quartz to form from the plagioclase and augite.

Dacitic members contain 70 to SO 1! plagioclase, 5 to 10% augite,

and 5 to 15?; quartz, with pyrite and magnetite as accessories.

Felsic volcanics include massive rhyodacite and rhyolite

with minor tuffaceous rhyolite and rhyodacite. Quartz and

feldspar porphyries are noted in the southwest corner of the

property in claims L-1015684 and L-1015689. The felsic rocks

are light-coloured and aphanitic with a white or buff weathered

surface.

Intruding the volcanics in the area of L2200E/100N is a

small plug of hornblende gabbro also of Archean age. This is a

dark green to black massive rock, having a composition of 40 to

45?; hornblende, 30 to 351; plagioclase, 5 to 101; biotite, and up

to 10?; quartz, with magnetite as an accessory mineral.

Structurally, the property is traversed by an anticlinal

axis that trends 030 0 through claims L-1015666, L-1015667,

and L-1015669, and leaves the northern part of the property

through Captain Lake.

Jensen shows two major faults cutting across the property.

The first is a north-trending fault that passes through claims

L-1015661, L-1015669, L-1015674, L-1015679, L-1015684, and

L-1015689. There is no surface expression of this fault. Its

15


position is interpreted on the basis of an abrupt change in the

strike of the volcanics.

A second fault is northeasterly trending (065 0 ) and is an

offshoot of the north-trending fault in claim L-1015689.

Several fault zones have been indicated by the VLP-EM

survey. Three of these were targets of diamond drill holes

#1, #4, and #5. D.D.H. #2 and #3 tested a magnetic anomaly.

D.D.H. #1 was oriented grid north (OSO 0 ) and drilled so

that it intersected a conductive axis which was located by the

VLF-EM survey in claim L-1015683 between L2200E/150S and

L2400E/200S. The electromagnetic survey showed the axis to

trend at 330 0 . A possible surface expression of this structure

is a small creek which drains into Little Misema Creek. The

hole was drilled 497 lineal feet at an angle of -45 0 . It was

collared at L2400E/225S.

A fault zone with quartz and carbonate infilling was

intersected between 202 and 204 feet below the collar. Most of

the hole was in a fine-grained, dark, grey/green, porphyritic

andesite. Quartz stringers of less than 1mm in width were

encountered along most of its length, with several larger veins

of up to 18" in width. The larger veins were often bounded by a

zone of brecciated andesite, making the orientation of the vein

difficult to ascertain.

Samples were taken from this and the other core sections

which appeared most likely to host mineralization. These were

16


sent for assay at Accurassay Laboratories in Kirkland Lake.

Preparation of the samples included pulverization to 90*6 -80

mesh. The pulps were screened through 80 mesh wire cloth and

the entire +80 mesh fraction was then assayed, as were two 1AT

cuts of the -80 mesh product. The best value from D. D. H. #1

was 100 ppb Au over 2 feet.

D. D. H. #2 and #3 were drilled to test the magnetic anomaly

in claim L-1015679. D. D. H. #2 was collared at L2200E/362.5N,

while D. D. H. #3 was collared at L2150E/350N.

D. D. H. #2 was inclined at -45 0 and oriented grid north

(050 0 ). Core from this hole shows a fine-grained, grey-green

chloritic rhyo-dacite with between 3 and 5% pyrite and a trace

of pyrrhotite. These sulphides were found usually along or near

the edges of very narrow (less than 2" width) quartz stringers.

The amount of pyrite was remarkably consistent throughout the

267 foot length of the hole and decreased to below 3% only at

the 235 foot mark in the core. The best gold assay returned

from the samples taken from this hole was 232 ppb over 1.5 feet.

D. D. H. #3 was inclined at -50 0 , oriented grid north

(050 0 ) and drilled to a distance of 250 feet from the collar.

Fine-grained, soft, grey-green, and chloritic rhyo-dacite was

again encountered. A maximum of 7% pyrite with a trace of

pyrrhotite was found intermittently throughout the hole.

Several narrow zones of brecciated rhyo-dacite infilled by

quartz were noted. The best assay returned from Hole 13 was 688

17

JAMES E. TILSLEY b ASSOCIATES LTD.

ppb Au over 2 feet .

D. D. H. #4 was positioned to test the second conductive axis

indicated by the VLF-EM survey. This axis was found to strike

at approximately 110 0 in claims L-1015659 and L-1015667 between

L1100E/350N and L1400E/525N. The hole reached a distance of 497

feet from the collar at -45 0 . It is oriented grid south (230 0 )

and collared at L1300E/475S.

Fault zones were intersected in the core between 131 and 147

feet, as well as between 423 and 426 feet. Drill core from this

hole consisted primarily of a rhyo-dacite, again fine grained

and grey/green in colour. A quartz porphyry was found for the

first 146 feet below the collar, while quartz stringers less

than 1mm in width were encountered frequently along the length

of the hole. Some carbonate was also noted, including a 3"

vein of white and pink calcite at 246 feet. A maximum of

between 5 and 71 disseminated pyrite was logged in a zone of

brecciated rhyo-dacite infilled with quartz at 305 feet. The

best assay of the samples taken from core in this hole was 66

ppb Au over 2 feet.

The third conductive axis indicated by the VLF-EM survey

trends roughly parallel to the forest access road in the

northern end of the property. The main conductive axis appears

to trend at roughly 350 0 through claims L-1015658, L-1015666,

and L-1015671 between L1000E/275N and L1500E/025S. An offshoot

of the main axis trends approximately 310 0 , splitting at

18

JAMES E. TILSLEY Bc ASSOCIATES LTD.

L1100E/200N. Also, a Scintrex airborne anomaly was indicated in

this area in 1971. These axes were drilled for 497 feet at an

angle of -45 0 . The hole was collared at L1050E/281N and drilled

grid south (230 0 ).

Fault-related fracturing was noted between 80 and 90 feet

below the collar, with a second, coarser fracture zone at 97 to

100 feet. Soft, grey andesite was logged at the beginning of

this hole, with a porphyritic andesite starting at 153 feet.

A six inch quartz-carbonate vein was encountered at 61 feet.

Several zones of brecciated andesite infilled with quartz were

also noted and sampled. A 2" quartz vein with S-5% pyrite was

intersected at 152 feet. The highest value returned was 201 ppb

Au over l .5 feet.

19


SAMPLING

Sampling of the Ben Nevis property of Regal Goldfields

Limited included four large samples of the exposed bedrock near

the magnetic anomaly in claim L-1015679, and 26 samples from the

2008 feet of core obtained during the diamond drilling program.

Five of the 26 samples of drill core were sent for a detailed

26-element geochemical analysis.

The four samples averaged 18.15kg and were collected in the

area of L2200E/350N where up to 5% pyrite was visible in outcrop

just south of the magnetic anomaly. Preparation of these sam

ples included jaw crushing the rock to 1/4" and then to -20 mesh

using a rolls crusher. The -20 mesh product was screened to

remove any coarse gold which might have been present in the

samples. After initial screening, a 500g cut was sent to Accur-

assay Laboratories where it was pulverized to approximately 80

mesh. The pulp was screened using an 80 mesh (850 micron)

sieve. Two 1AT cuts of the -80 mesh fraction were assayed, as

was the entire +80 mesh product. The following is a summary of

the results obtained by sampling of this area:

Sample Number Sample Weight Estimated(kg) Grade Au (g/t)

8301830283038304

12.72520.07521.80018.000

0.0410.0720.0100.039

72.600 kg

20

JAMES E, TILSLEY 8c ASSOCIATES LTD.

During the diamond drill program, a total of 26 samples

was taken from selected lengths of drill core which appeared to

be favourable for hosting gold mineralization. Preparation of

these samples involved pulverization to nominal 80 mesh and

screening using an 80 mesh sieve. Two 1AT cuts were taken of

the -80 mesh fraction while the entire + 80 mesh fraction was

assayed. Detailed assay results are shown on the diamond drill

logs.

Five samples from the core were analyzed for each of 26

elements, including Ag, Al, As, Au, Ba, Bi, Ca, Cd, Co, Cr, Cu,

Fe, K, Mg, Mn, Mo, Na, Ni, P, Pb, Pd, Pt, Sb, Sn, Sr, U, W, and

Zn. These were compared to the values established by W. J.

Wolfe and reported in Geochemical Exploration of Early

Precambrian Volcanogenic Sulphide Mineralization in Ben Nevis

Township. (Ontario Geological Survey Study 19, 1977).

Wolfe took 920 samples and established an average zinc

value of 70 ppm, with a standard deviation of +J- 30 ppm. Of

the five test samples from drill core, four exceeded the mean

and one (120 ppm) was almost 2 standard deviations above the

mean.

Wolfe's copper analysis yielded an average of 45 ppm with a

standard deviation of */- 37 ppm. Copper values from the test

drill core samples collected were all above the mean, with a

high of 572 ppm (over 14 standard deviations above the mean!).

Values of 254 ppm {over 5 standard deviations above mean) and

21


226 ppm (over 4 standard deviations greater than the mean) were

also reported.

An average nickel content established by Wolfe in 1977 was

81 ppm, with a standard deviation of +/- 50 ppm. Assays from

four of the five samples from the core were determined to exceed

the average, although none were deemed truly anomalous by

exceeding the mean by two standard deviations.

Of the trace elements, the average manganese value of 708

ppm was exceeded in one of the five samples, but only by 23 ppm.

Cobalt was found by Wolfe to have an average abundance of

21 ppm with a standard deviation of +/- 10 ppm. The mean was

surpassed in all five core samples, including a value of 67 ppm

which was more than 4 standard deviations above the mean.

Assay certificates are appended.

22


GEOPHYSICAL SURVEYS

The geophysical surveys employed a Scintrex IGS-2

(Integrated Geophysical System) fitted with sensors and

processing circuits to permit collection of total field magnetic

and vertical magnetic gradient data (MP-4), and to measure three

components of the VLF-magnetic field (VLF-4). The system

includes a solid state memory in which measurements are stored

in ASCII 7 bit, no parity format. Data retrieval is by RS-232C

serial interface to digital printer, modem, microcomputer, or

cassette tape recorder.

Both the IGS-2 field unit and the magnetic base station

have solid state memories expanded to 48 kilobytes. This

permits readings at up to 800 field stations before data dump is

required. The magnetic base station is usually operated by an

automotive 12 volt battery, which provides ample, steady, and

reliable power. The expanded memory allows magnetic field

measurements to be recorded each two or three seconds for

continuous periods of ten to twelve hours.

The field magnetic data were microprocessor corrected for

diurnal variation using a pre-programmed routine resident in the

memory of the IGS-2 field unit referenced to continuous magnetic

records obtained by an MP-3 proton magnetometer operating in

base station mode, time synchronized with the IGS-2/MP-4 field

unit. Resolution is O.lnT.

Three components of the VLF magnetic field are recorded at

23


Setting up the magnetic base station sensor at L1580/BLO.

Geophysical survey in progress during the late afternoon of December 11, 1988.


each survey station. One, two, or three navigation station

signals can be received and vertical in-phase, vertical

quadrature, and horizontal amplitude of the magnetic component

of the VLF electromagnetic field can be read sequentially in

less than one minute.

At the end of each field day during the surveys, all data

were recovered in hard copy on a dot matrix digital printer.

When hard copy had been obtained and verified, the solid state

memories of the magnetic base station and the field unit were

erased in preparation for the next survey day.

The magnetic base station was set up near the center of the

property where the base line intersects the access road near

L1580E/BLO. Magnetic data are presented on two map sheets drawn

at a scale of 1:2500 to cover the area within the property

boundaries. The scale was chosen to permit plotting of closely-

spaced measurements. Both the corrected total magnetic field

determinations and vertical magnetic gradient data are shown on

the plans. The total magnetic field data are plotted on the

east side of the lines and the magnetic gradient to the west.

The total field is in the order of 58 SOOnT (base field). The

first and second digits of the total magnetic field are normally

omitted. Only the last three digits are plotted, unless the

field is changing from above 58 OOOnT to below 58 OOOnT (or vice

versa).

The VLF-EM survey sheets have the vertical in-phase

component determinations plotted to the west of the lines and

24

JAMES E. TILSLEY Be. ASSOCIATES LTD.

the vertical quadrature to the east. Both are expressed in

percent. The horizontal amplitude vector of the magnetic

component of the electromagnetic field transmitted by the

navigation station being measured is shown where relative change

indicates the axis of a conductive structure. These values are

not absolute values but are instantaneous measurements of the

primary field strength which is known to vary diurnally. Since

the strength of the primary field has not been monitored by a

VLF recording base station, no data exist to permit

normalization of these values. Therefore, the values are

indicative of the location of conductive axes, but cannot be

used comparatively.

MAGNETIC SURVEY

The magnetic survey of the Ben Nevis Township property was

designed to indicate any areas of bedrock which may contain

magnetic sulphide mineralization, namely pyrrhotite, as well as

providing detailed structural information about the volcanic

rocks which underlie the claim group. A total of 3523 readings

was taken at 12.5m intervals along profiles spaced at 100m.

There was no difference in magnetic expression between the

felsic and the intermediate volcanics, indicating that a fairly

similar chemical composition is shared by the two rock units.

One anomalous area in claim L-1015679 was indicated by the

survey along lines 2150E and 2200E approximately 400m north of

25


the base line. Values as high as 59 711nT (l 411nT over the

base field of 58 300nt) were recorded. Between 5 and 7% pyrite

was noted in the intermediate volcanics just south of the sur

face expression of the anomaly. Two diamond drill holes were

located to intersect the magnetic high. D.D.H. #2 was collared

at L2200E/362.5N and D.D.H #3 was collared at L2150E/350N. As

much as 71; pyrite mineralization was encountered through the

entire length of each hole. A trace amount of pyrrhotite was

also found to be present with the pyrite, thus accounting for

the magnetic anomaly. The anomaly appears to indicate a single

elongated plug with a maximum axis of about 75m.

VLF-EM SURVEYS

A VLF-EM survey was completed over the property using

signals from the transmitting station in Cutler, Maine (NAA)

which broadcasts at a frequency of 24.0kHz.

Several conductive structures were outlined by the survey

and became targets for the diamond drilling program. Drill

results, as discussed earlier, indicated fault zones to explain

the anomalies. Also present were some quartz and quartz-

carbonate veins, as well as zones of silicification and

shearing.

The locations and orientations of the three major

conductive axes were discussed earlier as part of the descrip

tion of D.D.H #1,4, and 5.

26


RECOMMENDATIONS

To this point, there have been no economic amounts of gold

or base metal mineralization found in the Ben Nevis Township

property of Regal Goldfields Limited. There are, however,

several indications that mineralization processes have occurred

which would warrant further exploration on the property.

From drill core, silicification, carbonitization, and minor

shearing were noted. Sampling yielded anomalous abundances of

zinc, copper, and cobalt. Secondly, the property is in very

close proximity to other prospects which have recently reported

showings (Northern Miner, November 7, 1988).

First of all, geological mapping should be completed on the

entire property. Only 13 of the 35 claims were mapped before

excessive snow cover forced the termination of the survey for

the season.

Next, a reconnaissance humus geochemistry survey should be

carried out over the entire property. Such a survey will

indicate the presence of base and precious metals through the

overburden cover as long as the overburden is not too deep. We

have found collection of forest mull (or 'humus') to be the most

effective geochemical survey sampling technique, since this

material will indicate the chemistry of the soils and rocks

penetrated by the roots of the trees and shrubs from which it is

derived. This gives a greater depth of effective sampling than

can be expected when inoroganic material is collected from the

27


uppermost soil horizons developed on transported overburden.

Normally, humus samples are taken on a relatively wide spacing

since there tends to be a dispersion and mixing of leaves,

needles and bark fragments from individual trees or groups of

trees growing on mineralized ground with similar material from

trees not in contact with mineralized bedrock. This results in

broad, low amplitude, metal anomalies from restricted source

areas.

Reconnaissance sampling is recommended over areas of the

property which are not covered by swamps, areas of great over

burden thickness where vegetation is unable to reach bedrock, or

areas where bedrock is directly exposed. The spacing for recon

naissance sampling should be 50m along lines not more than 100m

apart. Detailed sampling would have samples taken on not more

than a 40m square grid, with a 20m square grid density in

selected areas.

The humus samples respond well to analysis by neutron

activation techniques and are particularly suitable for

determination of gold content in the parts per billion range.

We have found that other elements are often useful indicators

of mineralization and usually opt for the total 16 element

package {Au, Sb, As, Ba, Br, Cr, Co, Fe, Mo, Se, Ag, Ta, Th, W,

U, and Zn) at a slight additional analysis charge.

Interpretation of geological and geochemical results with

reference to information collected during geological mapping of

28


the survey area should be followed by trenching, stripping,

washing, detailed geological mapping, sampling, and assaying, as

required and possible under overburden and drainage conditions

existing in those areas where data indicate the possibility of

mineralized bodies.

Finally, attention should be given to the two claims

(L-1015655 and L-1015656) in the northwestern corner of the

property which were not included in the magnetic and VLF-EM

surveys. A base line should be cut in a northerly direction

from the end of the present base line. East-west trending

profile lines should be spaced at 100m intervals along this new

base line.

The estimated costs of the recommended exploration work

are tabulated on page 30.

29

JAMES E, TILSLEY A ASSOCIATES LTD.

ESTIMATED EXPLORATION COSTS

The cost of the recommended exploration work is estimated

as follows:

Lines 5km at $263.50 l 317.50

Geophysical surveys; total magnetic 637.50 field, magnetic gradient, VLF-EM 2TX, 3 parameters 150 sta. at $4.25

Geochemical surveys; humus sampling, 5 100.00 16 element analyses, 300 stations at $17.00

Geological mapping; 22 claims at $350 7 700.00

Stripping/Trenching/Washing 7 500.00

Sampling l 000.00

Assaying l 000.00

Supervision 4 500.00

Consulting, reporting 6 750.00

Drafting, secretarial, printing, 2 000.00 binding, et cetera

Communications, courier 875.00

Equipment allocations (pumps, hose, l 594.00et cetera)

Vehicle (incl. fuel, insurance, l 940.00 et cetera)

Travel, room S board (60 man/days) 4 500.00

Insurance 225.00

TOTAL 5 46 639.00

30


REFERENCES

Downes, M. J.1981: Structural and Stratigraphic Aspects of Gold Mineralization in the Larder Lake Area, Ontario; p.66-69 in Genesis of Archean, Volcanic-Hosted Gold Deposits, Symposium Held at the University of Waterloo, March 7, 1980, Ontario Geological Survey, MP 97, 175 p.

Gledhill, T. L.1929: Ben Nevis, Munro, Kamiskotia, and Other Base-Metal Areas, District of Cochrane and Timiskaming; Ontario Department of Mines, 1928, Volume 37, pt. 3, p.1-52. Accompanied by Map No. 37g, scale l inch to l mile.

Hurst, Tracy et. al.1987: Tegousie Wabie: The Story of Larder Lake, Ontario. Copyright Larder Lake Public Library, 99p.

Jensen, L. S.1975: Geology of Clifford and Ben Nevis Townships, District of Cochrane; Ontario Div. Mines, GR132, 55p. Accompanied by Map 2283, scale l inch to 1/2 mile.

Jensen, L. S.1981: Gold Mineralization in the Kirkland Lake-Larder Lake Area; p. 59-65 in Genesis of Archean, Volcanic-Hosted Gold Deposits, Symposium Held at the University of Waterloo, March 7, 1980, Ontario Geological Survey, MP 97, 175 p.

Jensen, L. S., and Langford, F. F.1985: Geology and Petrogenesis of the Archean Abitibi Belt in the Kirkland Lake Area, Ontario; Ontario Geological survey, Miscellaneous Paper 123, 130p. Accompanied by Maps P.2434 and P.2435, scale 1:63 360 or l inch to l mile and sheet of microfiche.

Knight, C.W.1920: Ben Nevis Gold Area; Ontario Dept. Mines, Vol. 29, pt. 3, p.1-27. Accompanied by Map 29e.

Northern Miner Press Ltd.1988: Westbank Find in Ben Nevis, November 7.


Ontario Geological Survey1979: Airborne Electromagnetic and Total Intensity Magnetic Survey, Kirkland Lake Area, Ben Nevis Township, District of Cochrane; by Questor Surveys Limited zor the Ontario Geological Survey, Prelim. Map p.2254 Geophys. Sur., scale 1:20,000. Survey and compilation, February and March 1979.

Ploeger, F., Campbell, A., and Grabowski, G.1979: Ben Nevis Township, District of Cochrane; Ontario Geological Survey Preliminary Map P.859 (Rev.), Kirkland Lake Data Series. Scale 1:15 840 or l inch to 1/4 mile. Data Compiled 1979.

Wolfe, W. J.1977: Geochemical Exploration of Early Precambrian Sulphide Mineralization in Ben Nevis Township, District of Cochrane; Ontario Geological Survey Study 19, 39p.

Wilson, W. J.1901: Western Part of the Abitibi Region; p.l!7A-130A in Summary Report, pt.A, Geol. Surv. Canada, p.271, Vol.XIV. Accompanied by Map No. 760, scale l inch to 16 miles.

JAMES E. TILSLEY a ASSOCIATES LTD.

CERTIFICATE

I, Ralph P. Mueller, of the town of Newmarket, Province of

Ontario, hereby certify:

1. I am a Project Geologist and reside at 438 Tecumseth St., Apt. 2, Newmarket, Ontario.

2. I am a graduate of McMaster University, 1988, B.Se., Geology.

3. I have been employed as a geologist since graduation.

4. This report is based on my work and personal observations of the property in November and December of 1988, as well as information obtained from current technical literature, and reports published by the Ontario Department of Mines, Ontario Division of Mines, the Ontario Geological Survey, and the Geological Survey of Canada.

5. I have no interest, direct or indirect, in the propertiesor securities of Regal Goldfields Limited, or anyaffiliate, nor do I expect to receive any such interest.

Dated at Aurora, Ontario this 06 day of February, 1989.

Ralph P. Mueller, B.Se.


CERTIFICATE

I, James E. Tilsley, of the town of Aurora, Province of

Ontario, hereby certify:

1.

2.

3.

4.

5.

6.

I am a Consulting Geologist and reside at 5 Steeplechase Avenue, Aurora, Ontario.

I am a Geology.

I am a Engineers Engineers Engineers Britian),

graduate of Acadia University, 1959, B.A.

member of the Association of Professional of Ontario, The Association of Professional

of Manitoba, The Association of Professional of Nova Scotia, Chartered Engineers {Great and designated Consulting Engineer, Ontario

Association of Professional Engineers, 1975.

I have been employed as a geologist since with consulting groups since 1964 and practice since 1980.

graduation, in private

This report is based on geological and geophysical surveys carried out under my supervision, observations made during visits to the property between December 10 and 16, 1988, and on the study of records relating to the property as available from the assessment files of the Ministry of Natural Resources, province of Ontario, maps and reports published by the Ontario Bureau of Mines, the Ontario Department of Mines, the Ontario Geological Survey, and the Geological Survey of Canada.

I have no interest, direct or indirect, in the proper ties or securities of Regal Goldfields Limited, or any affiliates, nor do I expect to receive any such interest.

Dated at Aurora, Ontario this O ebruary, 1989.


APPENDIX I

DIAMOND DRILL LOGS, SECTIONS


APPENDIX II

COPIES OF ASSAY CERTIFICATES

ACCURASSAY LABORATORIES LTD.P.O. BOX 604

KIRKLAND LAKE, ONTARIO, CANADA P2N 3J5 TEL.: (705) 567-6343

President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Ont.i, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T,

Certificate of Rnolysis-J. E. Tilsley Associates

23769 5 Steeplechase Avenue Aurora, Ontario L4G-3G8

SAMPLE NUMBERS Accurassay Customer

159257159258159259159260159260

83018302830383048304

Gold ppb

Page: l

Date:December 7

Work Order Project

881307

41 72 10 39 27 Check

1988

LF-30 Per:

ORIGINAL

BY:XEROX TELECOPIER 7010 ; 1-12-89 5:06PM ;

Jan. 12M9 17:05 0000 ACCURASSAY LABS

705 568 S368-*

TEL705-568-8368

A168413029;W 2

PflGE 02

ACCURASSAY UBORATORIES LTD.P.O. BOX 604

KIRKIAND LAKE, ONTARIO, CANADA P2N 3J5 TEL.: (706) 567-4343

President: Dr. GEORGE DUNCAN, M.SC . P* o., c. a*m luw.i. c eh** iu x i. M.C.I c . M.R.S.C., A.B.C.R.T.

Certificate of AnalysisTilsley Associates9/JO71 -- . sey ssoca

t*IO(J.t; steeplechase- AvenueAurora, Ontario L4C-3G8

Date: January 12

VorK Order # : 690031 Projec-t :

Accurassay # Customer # Pulp weight gram

164982 155029 1405.330

1649fid 105031 2621.130

164984 155033 642.730

1649ttb 155035 1047.030

1*14986 155036 971.030

104987 155037 1348.430.

Z Df. G. DuT^n "l\kX, CHEMIST Jjj

Subsaaple

30.250 30.340 4.600

30 . 170 3U.240 36,770

30,110 30 , 030 20.310

30.290 30 . 020 7.770

30.130 30.110 2,650

30.090 30.110 6.030

Read weight mg 0.004 0.000o.ooo0.000 0 , 003 0.000

0.000 0,001 0.003

0.000o.ooo0.000

0,002 0.001 0.000

0 . 008 0 , 004 0.003

A

IfOO Per:

ORIGINAL

ROJ BY:XEROX TELECOPIER 7010 ; l- 9-89 6:36PM ;

Jan. 9 '89 18:35 0000 ACCURASSAY LftBS

705 568 8368-)

TEL705-568-8368

4168413029;8 29

PAGE 02


KIRKLAND LAKE. ONTARIO. CANADA P2N 3J5

TEL.: (705) 567-6343

President: Dr. GEORGE DUNCAN, M.S:.. f*, o., c ChcmiOnt.i, c. ChwiUKl. M.R.I.C. M.K.S.C., An.c.S.T.

Certificate of Rnalysis'*F' T ,lle.ley Associates Steeplechafa-B Avenue

Page: l

Data:January 9 69

*- "- Aurora. Ontario L40-3G6 Vork Order # ,- 881524

rrojsct :

Accuraesay # CuotoraQr # Pulp weight Subsample Bead weight gran gran rag

163600 IhSOOl 771.630 30,120 0.002 30.040 0.002 16,110 0.001

163601 155002 993,130 30.300 30.270 29.080

0,002 0,000 0,011

163602 155003 Sample missing

163603 IbbOOi 1228.230 30.340 30.180 0.340

163604 lf,5f)007 2155.830 30,230 30.040 26.480

163605 155008 1493.530 30.120 30.150 3.930

163606 15R009 S91.130 30.180 30.150 5.960

10360V 155011 1474.330 30.170 30.010

X^^TT^ 15.130

0.001 0.005 0.000

0.000 0.000 0,000

0.001 0.002 0.000

0,001 0.006 0.002

0.004 0,008 0.004

A j'' ^riAi^ r L nr r) '\Ji'/.

f V. r ^Mfifi.Tn"

Pur: 4^Ly- j6#**Ae*H**rORIGINAL

U BY!XEROX TELECOPIER 7010 ; l- 9-89 6:37PM ;

Jan. 9 Q| 18:35 0000 ACCURASSAY LABS

705 563 8368-)

TEL705-568-8368

A 1 684 1 3029; tt 3

PAGE 03


KIRKLAND LAKE, ONTARIO, CANADA P2N 3J5 TEL.: 1705) 567-6343

Dr. GEORGE DUNCAN, M.SC.. ci. D . c. CHn IOM.I. c o*v IU.K.I. M.C.I.C M H.S.C.. A.R.C.S.T,

Certificate of Analysis

9A9K7c H to 1

Accuraesay163608

163009

103610

163611

163612

163613

163GU

163915

(fiit.* \*

J. B. Tllslev Associates Dst*. January5 Steeplechase Avenue Aurora, Ontario L40-3G8 Vork Order # :

Project i

# Customer # Pulp weight Subsample gran gram

155012 1036.130 30,320 30,360 27.610

Ibb013 1032.830 30.230 30,310 14.460

Ibb015 843.030 30.090 30.290 31.600

155016 1628.430 30.050 30.100 28 , 700

155017 1052.530 30.280 30 . 330 37.860

155018 1106.630 30.240 30.300 19.000

IbbOlQ 1056.930 30.180 30.030 10.020

1S5020 1070.030 30.280 ^ZrTr-^ 30.350jXoS.W'^'x As^v 15 A W in

\3s* —— y\ '/CrtA.Rl6RED\6\ L~. ——— ~- —— iT\ sDr. G. Duncan SS v^

, Q/ ^t/

?iK^X^ ^

Page: 2

d 19 89

881524

Bead weight mg -

0.002 0.001 0.007

0.013 0.001 0.000

0.003 0.001 0.001

0.003 0.003 0.001

0.002 0,008 0.001

0.007 0.001o.ooo0.002 0.003 0.005

0.000 0,000 0.001

9 fi7 w\S\j WV\V '^X/*^

ORIGINAL

BY:XEROX TELECOPIER 7010 ; l- 9-89 6:38PM ;

Jan. 94fc9 18:36 0000 flCCURRSSAY LPBS

705 568 8368-* 4168413029;** 4l

TEL705-568-B368 PAGE 04


KIRKLAND LAKE, ONTARIO. CANADA P2N 3J5 TEL.: (7051 667-6343

President: Dr. GEORGE DUNCAN, M.S*., rt, n r. cum ton-.i. c c** IU.K *, M.Ci.e.. M R.B.C.. A.R c RT.

Certificate of Analysis

24268

Accurassay

163616

363617

163618

163619

163620

J, E, Tilslev Associatfis Dam- Januaryfi Steeplechase Avenue Aurora, Ontario L4C-3G8 Vork Order # :

Project f

# Customer # Pulp weight Subsanpla gran gran

Jbb021 1847.630 30,360 30.030 24.740

155023 1380.130 30.300 30,230 8.550

155025 1575.530 30.250 30,060 16,440

155026 1841.630 30.330 30.250 5.860

155028 1746.230 30.370 30.100 1.140

Per: ff

Page t 3

9 19 89

881524

Bead weight mg 0,024 0.017 0.019

0,004 0.011 0.001

0,001 0.005 0.001

0.002 0.000 0.000

0.000 0.000 0.001

.

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Ont.l, c. Chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of flnalysisJ. E. Tilsley Associates 5 Steeplechase Avenue

Ontario

LF-30

Assay results are as follows:

SAMPLE NUMBER Accurassay Customer

163607 155011163608 155012163611 155016163616 155021163618 155025

163607163608163611163616163618

163607163608163611163616163618

163607163608163611163616163618

155011155012155016155021155025

155011155012155016155021155025

155011155012155016155021155025

Page #1

- 01/23/89 19

Work Order

4

Agppm1.21.21.21.31.4

Catt

0.891.164.660.504.40

Ktt

0.340.310.820.210.85

Ptt

0.030.040.060.030.04

Altt

7.396.696.717.083.71

Cdppm2.31.11.21.31.7

Mgtt

3.151.911.551.791.56

Pbppm8877

1046359

Asppra1071321197886

Coppm2925216744

Mnppm390355731460514

PdppmNDNDNDNDND

881524

AuppmNDNDNDNDND

Crppm96

1151134644

Moppra

53374

PtppraNDNDNDNDND

Bappm124448116439

Cuppm2549171

572226

Natt

0.671 .080.800.340.74

SbppmNDNDNDNDND

Bippm

5ND3

ND4

Fett

5.143.653.463.946.19

Nlppm117113928764

Snppm1371047

Per: ^ ,6O(Xx*A

ORIGINAL



President: Dr. GEORGE DUNCAN, M.SC., Ph. D., c. Chem (Ont.i, c. chem (U.K.), M.C.I.C., M.R.S.C., A.R.C.S.T.

Certificate of flnalysis

2525^J. B. Tilsley Associates 5 Steeplechase Avenueurora, Ontario40-308

Assay results are as follows:

SAMPLE NUMBER SrAccurassay Customer ppm

163607 155011 54163608 155012 49163611 155016 63163616 155021 27163618 155025 85

Page #2

Date: 01/23/89

uppmNDNDNDNDND

Work Order 881524

W Znppra ppmND 128ND 87ND 85ND 73ND 65

19

Note: ND is not detected

LF-30 Per:

ORIGINAL

a.12191 BEN NEVi s 900

Mining Lands Section 3rd Floor, 880 Bay St. Toronto, Ontario M5S 1Z8

Phone: (416) 965-4888

Your file: W8908-006 Our file: 2.12191

March 15, 1989

Mining RecorderMinistry of Northern Development and Mines4 Government Road E.Kirkland Lake, OntarioP2N 1A2

Dear Sir: j

Re: Notice of Intent dated February 23, 1989 f Geophjosical (Magnetometer fi Electromagnetic) l Survey on Mining Claims L 1015657 et al in *- Ben Nevis Township

w* 80 889 l

^SJH^EDJ

The assessment work credits, as listed with the above-mentioned Notice of Intent, have been approved as of the above date.

Please inform the recorded holder of these mining clains and so indicate on your records.

Yours sincerely,

W.R. CowanProvincial Manager, Mining LandsMines St Minerals Division

RM:eb

Enclosures

cc: Mr. G.H. FergusonMining and Lands Coronissioner Toronto, Ontario

cc: Resident Geologist Kirkland Lake

cc: Regal Goldfields Ltd. 1100-350 bay St. Toronto, Ontario M5H 2S6

/y-ir-i^ "i"" i lobiiuiuai /-vasei VVI Northern Development ,., . . ,. LjjJ and Mines Work CreditsKario

"Iirom 2.121915at* 1 Mining Recorder^ Report of

Feb 20, 1989 pfe9oVo06

Recorded Holder

RFRAI GOLDFIELDS LIMITEDTownship or Ares

BEN NEVISType of survey and number of

Assessment days credit per claimGeophysical

on

Inriurert polarization fl"V'

Other flays

Section 77 (19) See "Mining Claims Assessed" column

Geological rtay.

Rfinrhemiral riayi

Man days Q Airborne Q

Special provision ffi Ground Q?)

Q Credits have been reduced because of partial coverage of claims.

Q Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims AsMCsed

L 1015657 to 684 inclusive 1015686 to 689 inclusive

Special credits under section 77 (16) for the following mining claims

10 days Electromagnetic 10 days Magnetometer

L 1015656

No credits have been allowed for the following mining claims

[X] not sufficiently covered by the survey Q insufficient technical data filed

L 1015655 1015685

The Mining Recorder may reduce the above credits if necessary in order that the total number of approved assessment days recorded on each claim does not exceed the maximum allowed as follows: Geophysical - 80; Geologocal - 40; Geochemical - 40; Section 77(19) - 60.

828 (85/12)

Instructions: Please type or print. If number of mining claims traversed

exceeds space on this form, attach a list. Note: - Only days credits calculated in the

"Expenditures" section may be entered in the "Expend. Days Cr." columns.

Do not use shaded areas below.

Geochemical and Expenditures) W8903*

Survey Company i Oat* of Survey (from At tp)

E .Ta-s L&V 4 ASSOCIATES Ijo oft i At. i 3ft l ffi j LZ"" ~ ~~

M6HTtotaT Miles of line Cut

Name and Address of Author (of Geo-Technical report)ETTi-Si-ErVr' S

• y . 11 MB *- l ' t- OO .pSy.l.Mo. j 9P l Day j MiT | VrT \ ^-——

AV&, ftvtZ&G^, dff.Credits Requested per Each Claim in Columns at riSpecial 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 ajfid enter total (s) here

JAN 8 1989

.irborne Credits .^ "-UECEHNote: Special provisions

credits do not apaly^ to AirbcjrnJ- ^rvf&'sy

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

- Electromagnetic

lilirJ

Geo!

G*O(

\ f 1

Magnetometer

ladiometric

)ther

igical

lemical

D

gntDays p*r

Claim

10

to)

Days per Claim

Days per Claim

Electromagnetic j

Worn.,.,

Radiometric

Mining Claims Traversed (List in numerical sequence)

Type of WoVV Performed

Performed on Oaim(t)

Calculation of Expenditure Da y t Credits

Total Expenditures

S -i- 15

Total Days Credits

s

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

Mining ClaimPrefix Number

/0/5655

IOI.5&&CNl__

10/5

1015665

JO/5

lots 10/5

l*'/'

i /Q667? r

Expend. O&ysCf.

^

HI

Mining ClaimPrefix I Number

li/oifi^Z^IQlS&bQiL IQIS&8I

101548S*./.—.

10I5MT

Expend. D^ayt Cr.

Total number of mining claims covered by thisfCDO't O* \\Ofk

Certification Verifying Report or Work

For Office Use OnlyTotal Os vi Cr-iDa, Reco

Reco

^ s ig^q . jAts, ^! ApMOved ft Recorded Branch Dirtr.tor ~~

l hereby certify that l have /personal and intimate knowledge of the facu set forth in the Report of Work annexed hereto, having performed the work or witnessed tame during and/or after its completion and the annexed report is true.

Name and Pottal Addrett of Perton Certifying

Ministry ofNorthern Developmentand Mines

ntario

-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.

Type of Survey(s) c ' eTownship or AreaClaim HolHer(s) Rft

—————— d ——— i ——— 3 ——————————————————/3tn ê v/s

a A 1 (y t W -frc Id J i iNmi' ^fc(Jta —————————————————— —————————————————————

Survey Company Jei*v,e.j E. f.'/C/Cv and nStoduseS Ltd,

Author of Report

Address of Author **

Covering Dates of Surv

Total Miles of Line Cut

R. Mne/ller J r.'/j/Cy

Stapkd,ft!B /Vê /\Lrcra OjJf mo- 3fr8ev Af*/ 15, M?8 - Dec. l/ . tfltf

(linecutting to office)

Tr Am

SPECIAL PROVISIONS DAYS CREDITS REQUESTED nû...:..! *""ta

ENTER 40 days {inc line cutting) for first survey.ENTER 20 days for i additional survey usit same grid.

ô *^

—Electromagnetic -^-M, ,,... udes -y f.

— Magnetom^tT ,...,..^T ^— Radi^mpfir

:ach —Other1K Geological

AIRBORNE CREDITS (Special proviiion credit* do not apply to airborne surveyi)

Magr""t"TTt''t*"''. . M,, .Fl^rtr^rnagnptir , ,. RaHinm^trir(enter days per claim) *~

n.™. F*b fM,v um .mM .™.., 4M^m\ i

Res. Geol.

Previous SurveysFile No. Type

Xuthorôf. 5?poj[t or Agent

Qualifications

Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

l - JOI5&57(prefix) (number) ^

L - lcxs 45^L ~ Jois 65y^ -. /0/5 b&Q

L - /6/s ^^(L - '^5 az J

,..,,,.4,,,........:.....J^5...M^,,.,....J

,.,.,, ..................,,...........,.,,, jL - /C"(5 66^ aL - /0(5 4^7

L - |0i5 ^68

L ~ /op ^fL *~ lolS 47O

L - /a/5 67/

L - lo^67ZL - lo^^L -yo/ 5 b?*/

L - 1015 676jL - lOtStTIL - J^S^7^

TOTAL CLAIMS ^

837 (85/12)

r J

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L-

L - lois L -

L -

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L -/OS 659

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\___ j —— •"—' J -' IV^VEVF , rw^VCK^ l i

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Daughter Lake 3 M *, r•rKatrine, Twp. (M.357)

JOH*. JACKSON 1911'2 M

T

DATE OF ISSUE

32D0SSE®e39 2.12191 BEN NEVIS

THF TOWNSHIPor

BEN NEVISOF

COCHRANE

LARDER LAKE ,MINING DIVISION "

. \ SCALP t;!NCM 40 CHAINS'

LFGENl)•

©neO , J

M fr;

.4 # f

fa

NOTES

400* Surface rights reservation olopfc the shores of^ all lakes and rivers , .

SAND AND GRAVEL

QUARRY PERMIT

AflEAS WITHDRAWN FROM plSPO|lT!ON

M.R.O. - MINING RIGHTS ONLY

S.R.O.-SURFACE RIGHTS ONLY

" ^M.*S. - MINING AND SURFACE RIGHTS ,*" — —

OBKription - Order No. Oat* x tiispoMtion' Fjia

R Ste 36/80 'w'5/83'. P8/6/83 MSS ^'-'-W

(5)SURFACE AND MININQ RIGHTS WITHDRAWN FROM x STAKING SECTION 36 ORDER NPW-6/85 DAT^D , ;

'*,1.*. 1 .1.1 .....,.. i t,URFACE a MINING RIGHTS WITHDRAWN FROMSTAKING SECT. 36, ORDER W 01/8'SL

N " M.325ONTARIO ' v, ;*

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regal goldfields limited - ontario€¦ · held by the duvan copper company limited in 1964....

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