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42A06SE2004 2.18708 LANGMUIR 010

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REPORT ON LINECUTTING AND

GROUND MAGNETIC SURVEY

BLACK PEARL MINERALS INC.

WEST LANGMUIR PROPERTY

LANGMUIR TOWNSHIP

DISTRICT OF COCHRANE

ONTARIO

BRIAN K. POLK B.Sc.

POLK GEOLOGICAL SERVICES

TIMMINS - ONTARIO

AUGUST 16,1998

ATHERTON GEOLOGICAL SERVICES

42A06SE2004 2.18708 LANGMUIR 0 10C

TABLE OF CONTENTS

1.0 INTRODUCTION

2.0 PROPERTY LOCATION AND ACCESS

3.0 PREVIOUS WORK

4.0 GEOLOGY

4.1 REGIONAL GEOLOGY

4.2 GEOLOGY OF THE PROPERTY

5.0 LINECUTTING

6.0 MAGNETOMETER SURVEY

7.0 SURVEY RESULTS

8.0 CONCLUSIONS AND RECOMMENDATIONS

9.0 REFERENCES

MAPS AND FIGURES

FIGURE 1 PROPERTIES LOCATION MAP

FIGURE 2 CLAIM MAP

FIGURE 3 GENERAL GEOLOGY

FIGURE 4 WEST LANGMUIR GEOLOGICAL MAP: SCALE 1:25000

FIGURE 5 MAGNETOMETER PLAN WITH GRID (1:2000)

APPENDIX A:

INSTRUMENT SPECIFICATIONS AND OPERATIONS

-2- POLK GEOLOGICAL SERVICES

1.0 INTRODUCTION

Facilitated by the cutting of a 3.2 line kilometer grid a ground magnetic survey was

conducted on the West Langmuir group of claims on behalf of Black Pearl Minerals Inc.

from August 11-12, 1998. The purpose of the program was to map the bedrock geology

and identify the potential for economic base metal and\or gold mineralization of the

property. The program consisted of clearing out the claim boundaries, cutting and

surveying an East-West Baseline (BL 12 N), the cutting of 9 100 m spaced crosslines

(L16W to L24W), and running a magnetometer over the entire cut grid.

2.0 PROPERTY LOCATION AND ACCESS

The West Langmuir property is located in the south west quarter of Langmuir Township

near the boundary between Langmuir and Fallon Townships, in the district of Cochrane,

Porcupine Mining Division of Ontario, Canada. The geograghical coordinates are Latitude

48 17' N and Longitude 81 03' W. (Fig 1).

The property is located 30 km southeast of the City of Timmins. It is accessible by an all

weather gravel road 31 km south of South Porcupine to within 14 km west of the property.

A seasonal tractor road passes through the north west part of the property.

The property consists of 2 unpatented mining claims held by Mr. D. Meunier of South

Porcupine. The property is currently under option to Black Pearl Minerals Inc. The claims

are listed below and are shown on the accompanying Property Map (fig 2).


•aitm Group/ D (W Option stol Group i . f l l

Black Pearl Minerals Inc.

Properties Location Map

Figure 1 May 1997

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Black Pearl Minerals Inc.CLAIM MAPMeunier Option

Langmuir ft Fallon Twps., ON

Figure 2 June 1997Polk Geological Services

Claim # Type Recording date Status Due Date

P.825716 staked Aug. 171984 Active Aug. 171998

P. 825717 staked Aug. 171984 Active Aug. 171998

3.0 PREVIOUS WORK

Early 1900 - Porcupine Miracle sank a shaft to 200 feet. This is located a few meters

north of claim P. 825716.

1983- Mercier Exploration Limited conducted radiometric, EM, ground magnetic

and geological surveys over a claim group that spanned the Langmuir/

Fallon Township boundary. The West Langmuir Property was part of this

group. Significant gold, silver and base metal assays were obtained from

the mafic volcanics located 1.5 km east of the property.

1984 - 86 Lac Minerals conducted geological, ground magnetic and EM surveys and

diamond drilling over a claim block east of the West Langmuir Property.

Anomalous base metal results were obtained from diamond drilling the mafic

volcanics.

1992 - Trinity Exploration conducted line cutting, ground magnetic and VLF surveys

and geological mapping on the Porcupine - Miracle Property adjacent to the

north section of the property. Sampling of the old muck piles in the vicinity

of the shaft returned gold assays up to 495 ppb.


4.0 GEOLOGY

4.1 REGIONAL GEOLOGY

The rocks underlying the area are part of the Abitibi Greenstone Belt which is part of the

Abitibi Sub-Province of the Superior Province of the Canadian Shield. The part of the

Abitibi Greenstone Belt that underlies Langmuir Township is composed of volcanic,

sedimentary and intrusive rocks that strike northeast in the northwest part of the township

and almost east-west in the southern part of the township. This is illustrated in figures 3 S

5. The volcanic, sedimentary and mafic to ultramafic intrusive rocks are located between

three plutons. The most westerly of the plutons is a small trondhjemite stock which

extends from Eldorado Township eastward into the west-central portion of Langmuir

Township.

The Fallon Stock is classed as a monzonite (Pyke 1981). It is predominantly located to the

south of the property in Fallon Township and does extend north into Langmuir Township.

The Blackstock Granodiorite ( Pyke 1970) extends west from Blackstock Township into the

extreme east-central part of Langmuir Township.

The volcanic, sedimentary and mafic to ultramafic intrusive rocks are draped around these

plutons and the variable strike and dip of these rocks are as a result of this. These rocks

are grouped into three assemblages (Jackson and Fyon 1991). The assemblages are

arrayed from northwest to southeast with the oldest rocks to the northwest and are

described below.

The Deloro Assemblage consists of pillowed, amygdaloidal, feldspar phyric calc-alkaline

basalt and andesite (Pyke 1982). The volcanics have been intruded by mafic to ultramafic

intrusive rocks which have been classified as gabbro and serpentinized dunite by Pyke


1970. The contact between the Deloro Assemblage and the overlying Eldorado

Assemblage is thought to be stratigraphic (Jackson and Fyon 1991).

The Eldorado Assemblage consists of intermediate to felsic volcanic rocks, iron formation,

fine clastic sediments and ultramafic flows and intrusives. The contact with the overlying

Bowman Assemblage is conformable (Jackson and Fyon 1991). The volcanic rocks are

primarily rhyolitic to dacitic tuffs. Sedimentary rocks are oxide and sulphide facies iron

formation, chert, fine-grained sandstone and shale (Pyke 1982). Ultramafic rocks are

classed as peridotitic komatiites. The ultramafic intrusive rocks are described by Pyke

1982 as serpentinized dunite.

The Bowman Assemblage is a south facing series of peridotitic and basaltic komatiitic

flows interlayered with magnesium rich basalts.

Late diabase dikes occur throughout the area and are grouped into three types. The north

striking dikes are part of the Early Precambrian Matachewan swarm. Pyke 1982 has

shown the north-east trending dikes are divided into the Middle Precambrian Abitibi and

Late Precambrian Keewanawan swarms.

The area is covered by a blanket of Pleistocene glacial and post glacial sand, gravel and

clay.

Structure

The major structural feature in the area is the Montreal River Fault which cuts the township

in half in a northwest-southeast direction. It has a vertical dip and movement along the

fault is left handed. There are several other parallel to sub-parallel faults cutting across the

area. One northeast trending fault is known to cut across the area in the vicinity of the

Forks River ( Figure 5).


J '

WEST LANGMUIR CLAIMS GROUP'. - -. . .....——————,.. v

FIG. 3 REGIONAL GEOLOGY OF TIMMINS AREA *W ABITIBI AND SWAYZE GREENSTONE BELTS;"

ARCHEANNEOARCHEAN (2,5 to 2.9 Ga)

INTRUSIVE ROCKS Dlorite-nepheline syenite suite 9":

n

lnn

n

NEO- TO MESOARCHEAN (2.5 to 3.4 Ga)fi9"P

_____ INTRUSIVE ROCKS ^•H Massive granodiorite to granite: m massive to foliated granodiorite lo granite

15a Potassium feldspar rnegacrystic units^^^H Diorite-monzonite-granodiorite suite:^IH diorite. tonalite, monzonite, granodiorite,

syenite and hypabyssal equivalents (saturated to oversaturated suite)

lq l Muscovite-bearing granitic rocks:^ \ m js covite -b i oti le and cordiente-biotite

granite, granodiorite -tonal ile~ l Foliated tonalite suite: tonalite to

| granodiorite — foliated to massive

Mafic and ultramafic rocKs 0: gabbro, anorthosite, ullramaficrocKs

NEO-ARCHEAN (2.5 to 2.9 Ga)______ SUPRACRUSTAL ROCKS

. Coarse clastic rnetasedimentary ____ rocks''; mainly coarse clastic

metasedirnentary rocks, with minor, mainly alkalic, mafic to felsic meiavolcanic flows. tuffs and breccias

Nl- O-TO MESOARCHEAN (2.5 to 3.4 Ga)SUPRACRUSTAL ROCKS

Migmatized supracrustal rocks e9:metavolcanic rocks, minor metasedirnentary rocks, mafic gneisses of uncertain protolith, granitic gneissesMetasedimentary rocks 8^: wacke, arkose, argillite, slate, marble, chert, iron formation, minor metavolcanic rocks 7a Paragneisses and migmatites 3 7b Conglomerate and arenite

Felsic to in ter rued late metavolcanic rocks!?': rhyolitic, rhyodacitic, dacitic and andesilic flows, tuffs and breccias, chert, iron formation, minor metasedimentary and intrusive rocks; related migmalites

Matic to intermediate metavolcanic rocks9': basaltic and andesitic flows, tuffs and breccias, chert, iron formation, mmor metasedimentary and intrusive rocks, related migmatites 5a Andesitic flows, tuffs and breccias

with minor rhyolites" Malic to ultramafic metavolcanic rocks*": mafic metavolcanic rocks with minor komatiite, minor metasedimentary and pyroclastic rocks

/l Mafic and related intrusive rocks' \Sl 21a Preissacswarm: d iabasedikes

21b Marathon swarm: diabasedikes 21c Kenora-Foft Frances s warm:

diabase dikes 21d Wipissmg site (2213Ma). d iabase

sills, dikes and related granophyre 21 e Malic dikes and plutons of uncertain

agel Felsic intrusive rocks ( Murray G ranite

. . | 2388 Ma, Creighton Granite 2333 Ma]:granite

HURONIAN SUPERGROUP(2.2 Ga to 2450 Ma)

"*5^51 ! Cobalt Gp,"; conglomerate, wacke, l arkose,quartzarenite, argillite

j Quirke Lake Gp.; Hough Lake Gp.j ——l Elliot Lake Gp.

tsa Conglomerate, wacke, arkose, quart; arenite, argillite, limestone, dolostone

18b Volcanic rocks of the Elliot Lake Gp.

INTRUSIVE ROCKS /l Mafic and ultramafic intrusive rocks

l 17a Matachewan and Hears! smarms(2454 Ma)': d iabase dikes

17b Gabbro, anorthosite

SYMBOLS

Fault (traceable on surface, traceable in subsurface) ..

Iron formation

Granulite facies

Railway .....

Multilane highway ......

King's highway ....

Secondary highway ..,....... -. -, -,., ———————Elevation (land, water) ....... . ....., sasmThe positions of all boundaries and surveyed lines are

approximate.

CREDITS

Cartographic Services unit of the Ontario Geological Sur vey, as noted m the Explanatory Notes and Legend (OGS

Every possible effort hasbeenmadeto ensure the accura cy of the information presented on this map; however, the Ontario Ministry of Northern Development and Mines does not assume any liability for errors that may occur Us ers may wish to verily critical information.

Issued 1991.

Information from this publication may be quoted if credit is given. It is recommended that reference to this map be made in the following form.Ontario Geological Survey 1991. Bedrock geology of

Ontario, east-centra l sheet; Ontario Geological Survey.Map2543,scalel;1 000 000.

4.2 GEOLOGY OF THE PROPERTY

Outcrops on the property are generally restricted to the flanks and top of a topographic

high located on claim P. 825716. Four rock types were identified on the property and they

are described in the following section. The distribution of the outcrops is shown on the

West Langmuir Geological Map.

The property is underlain predominantly by metamorphosed mafic volcanics and ultramafic

peridotite flows. A 20-30 meter wide, North northwest trending diabase dike traverses the

property in the central portion of claim P.825716. An occurrence of porphyritic intrusive

was unearthed near the top of the claim group at the top of line 21 W.

Overburden

The overburden consists of a variable mantle of lacustrine silt and clay. The property is

well drained with a fairly mature forest cover of white and black spruce mixed with poplar.

The western end of the property is low-lying with local cedar and alder swamp.

Peridotitic Komatiite

The peridotitic komatiitic rocks (Bowman Assemblage, Jackson and Fyon 1991) are of a

flow nature. Good examples of this are found at the South end of L 18 W. There, a large

outcrop displays excellent spinifex and polysuturing textures. The orientation of these

flows is apparently 030, which is more northerly than other rocks seen on the property.

This may be explained by this outcrops proximity to the North Northwest diabase dike.

Most of the flows tested were weakly carbonitized.

.7. POLK GEOLOGICAL SERVICES

Mafic volcanics

The mafic volcanics observed on the property are quite similar in composition to the

ultramafic volcanics. They are set apart only by a finer grain size and an increase in

hardness. They tend to be very fine grained and dark grey green in colour and weather

to a dull brown as opposed to the rusty weathering of the ultramafic volcanics. Property

scale banding of the mafic and ultramafic volcanic units may represent cyclical

differentiation of the flows over time during deposition.

Diabase Dike

A large North Northwest trending dike (^20 M wide) cuts the property in the central portions

of claim P.825716. The dike is generally coarse grained but, some finer grained phases

were observed. The dike is generally magnetic but, so are the ultramafic flows.

Porphyritic intrusive

At the intersection of the Base Line (12 N) and Line 18 W , a small outcrop on the North

West corner of a sub crop related topography high was shown to host a significant volume

of porphyritic intrusive material. Within the outcrop is also some mafic volcanic material

contacting the porphyry in 2 ways: 1) fault contact along north trending fault or shear zone

and 2) irregular east west contact. It is apparant that the mafic volcanics are a raft caught

up in the felsic intrusive. The contacts showed no more than mineralization than did the

porphyry in general but, sampling was done with the possibility in mind.

This porphyry is pink in colour with some degree of hematization present. The porphyritic

phase is generally feldspar and the blasts are generally between 1 and 4 mm in dimension.


LAN

S AVCZ. x/je-ST C-UiviH

KMUIR TOWNSHIPFALLON TOWNSHIP

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LEGEND

ri Diabasic Dykes

j ~1 Intermediate-Fslsic Intursives

l l Ultcamaflc/Maflc Intmsives

L l Intermediate-Felsic Volcanics

r.~1 Mafic Volcanics

Ultramafic VolcanicsScale

400 200 O 500 inelers

Black Pearl Minerals Inc.

GEOLOGY MAPMeunier Option, Langmuir S Fallon Twps.

Figure 4 June 1997

Polk Geulo[|iC3l Services

Mineralization within the unit consists of 1 to 407o disseminated and fracture bound dirty

pyrite as well as 1 to 207o specular hematite as disseminated anhedral crystals and masses

less than 2 mm across.

5.0 LINECUTTING

A linecutting program was carried out between July 27-31 1998 by Brian K. Polk, Jean

LaForest and Jim Perello all of whom reside in Timmins, Ontario. The grid consists of one

baseline (BL 12 N), 4 feet wide, with 9 cross lines (L16W to L24W), 3 feet wide, at 100

meter spacings for a total of 3200 meters. Pickets with labeled aluminum tags were

stationed every 25 meters and the grid was tight chained from the baseline with the

Baseline/ L24W intersection as an origin. The grid is shown in Map 1 (Magnetometer plan

with grid).

5.1 GPS SURVEY

In order to establish accurate survey control for this property and other Black Pearl

Minerals property in the area, Differential Positioning GPS was used to establish sub-

centimeter UTM coordinates for the end points of the base line. The coordinates are as

follows:

LANG 1 (BP9801) nail in stump 11.75 along BL 12 N from #4 claim post P.825717

NAD 27 for use with OBMs

5347526.427 N 496156.183 E 296.299 el.

NAD 83

5347744.933 N 496173.281 E 296.299 el.


LANG 2 etched cross in large float boulder .6 m south and 3.85 m West of 16+14 m picket

on baseline 12 N

NAD 27 for use with OBMs

5347474.724 N 496925.106 E 304.767 el.

NAD 83

5347693.230 N 496942.209 E 304.767 el.

6.0 MAGNETOMETER SURVEY

The magnetometer survey was conducted by Kent Robinson of Timmins, Ontario between

August 11-12 1998. The ground magnetic survey was carried out using a (Gem Systems)

GSM-8 Proton Precession magnetometer. A base station was established at Hussey

Geophysics Inc. at 714 Mclean Drive, Timmins, Ontario using an identical continuous-

recording Gem Systems magnetometer to reduce diurnal variations. The magnetic datum

used in this case was 58,000 gammas. Readings were taken at 25 meter intervals along

the 100 meter spaced lines for a total of 3200 meters, with local fill-in readings in areas of

high magnetic intensity (300 meters). Refer to Appendix A for instrument operations and

specifications.

7.0 SURVEY RESULTS

The magnetometer survey was successful in outlining the basic geology of the property.

The contoured magnetometer map (MAP 1) shows the rocks trend Northeast to East

north-east across the property and are divisible into somewhat discrete magnetic units.


Geologically the property is apparently underlain by 3 series of volcanic rocks, each with

ultramafics at the base differentiating into mafic flows to the north. The magnetometer

readings in the Southeast portions of the property are definitely substantiated by the

geology observed at those stations (i.e. high mag over ultramafics and diabase). The

diabase dike is fairly obvious but, because the surrounding rocks are generally magnetic

as well, the dike signature is locally obscured. Perhaps the most interesting feature is

found near the BL around L20 W then trending SW to terminate at 10+50 N at

approximately L21W. This magnetometer low feature represents the lowest magnetic

signature on the property and trends onto the historic Porcupine-Miracle mining property.

On this property, 2 shafts, one of which goes 200 feet down, were driven within a

mineralized felsic intrusive body (porphyry). The magnetometer survey indicates that this

porphyry does underlie some, if not a significant amount, of Black Pearl's property.


8.0 CONCLUSIONS AND RECOMMENDATIONS

The magnetometer survey was successful in providing a good general geology for the

property in question. The survey agrees well with observed geology at a few locations on

the property and indicate the presence of a historically mined and mineralized porphyry

body on the property.

Recommendations for future work include geological mapping with some hand or

mechanical stripping around the porphyry occurrence outlined by prospecting and indicated

by the magnetometer survey.

Brian K. Polk B.Sc.

Polk Geological Services


9.0 REFERENCES

Jackman, S. L. and Fyon J. A., 1991, The Western Abitibi Sub-Province in Ontario: In

Geology of Ontario, Ontario Geological Survey, Special Volume 4, Part 1 p. 405 -

484

Pyke, D. R. , 1970, Geology of Langmuir and Blackstock Townships; Ontario Department

of Mines, Geological Report 86. Accompanied by Map 2206 ; Scale 1" to Yz M ile

Pyke, D. R., 1982, Geology of the Timmins Area, District of Cochrane, Ontario Geological

Survey Report 219. Accompanied by Map 2455; Scale 1:50,000


CERTIFICATION

l Brian K. Polk hereby certify that:

1) That l am a consulting geologist, and reside at 376 Patricia Ave., Timmins, Ontario,

P4N 6Y6

2) That l graduated from Lakehead University with a Bachelor of Science

Degree in 1994

3) That l have practiced my profession continuously since 1994.

Timmins, Ontario Brian K. Polk B.Se.

August 14, 1998


APPENDIX A

-1 5- POLK GEOLOGICAL SERVICES

G S M -

PROTON PRECESSION MAGNETOMETER

INSTRUCTION MANUAL

GEM SYSTEMS, INC. 105 SCAHSDALE ROAD, DON MILLS (METRO TORONTO) ONTARIO, CANADA, M3B 2R5 TEL: ( U16) WH-3210 TELEX: 06-966566

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- 4 -1.2 EARTH'S MAGNETIC FIELD

Figure l shows nominal distribution of Earth's magnetic field in kilogammas, with dotted lines separating equatorial and polar re gions. In polar regions an inclination of magnetic field vector is closer to vertical, while in equatorial regions it is nominally horizontal. To obtain the best precession signal and superior qua lity of operation, the sensor must be aligned accordingly. Orien tation line at the side of the sensor should be oriented vertically in polar regions and horizontally in equatorial regions. Although maximum signals are achieved by aligning the sensor orientation line close to the actual direction of the magnetic field, it is ge- ncraly not necessary to go beyond horizontal/vertical orientation mentioned above.

Range position on a front panel of the instrument should initially be selected closest to a nominal value of magnetic field shown for particular region in fig.l. As local distributions of magnetic field could be considerably altered, a proper range position should be determined by first valid reading of the magnetometer (first two digits of the display show a real magnetic field value for the place of measurement). During a survey, the field value may change beyond initially used range and the Range switch position should be adju sted accordingly, although the GSH-B will generally work correctly on several adjacent ranges.

Local ferromagnetic objects like screws, nuts, pocket knives, nickel coins, wristwatches, tools etc. may impair the quality of measurement by modifying the value of local magnetic field being measured or in drastic cases by even destroying the proton precession signal due to excessive gradients. For best results ferromagnetic objects should be kept away from the sensor. NiCd batteries, al though slightly magnetic, do not produce visible effect on measu rements if the sensor is installed on the staff and kept at arms length away from the operator and the console. For back-pack in stallation of the sensor a nonmagnetic set of batteries is recom mended .

2. SPECIFICATIONS

- 5 -

RESOLUTION:

ACCURACY:

RANGE:

GRADIENT TOLERANCE:

OPERATING MODES:

OUTPUT:

EXTERNAL TRIGGER:

POWER REQUIREMENTS:

POWER SOURCE:

BATTER? CHARGER:

OPERATING TEMPERATURE:

DIMENSIONS:

WEIGHT:

l gamma, 0.5 gamma optional

±1 gantna over operating range

20,000-100,000 garnna it) 23 overlapping steps

Up to 5000 garmaAietre

MMWAL PUSHBUTTON, new reading every 1.85 sec., display active between readings

CYCLING, pushbutton initiated, 1.85 sec. period

SELFTEST, pushbutton controlled, 7 sec. periodVISUAL: 5 digit l cm (0.4") high Liquid Crystal Display, visible in any anbient light

DIGITAL: Multiplied precession frequency and gating pulse

ANALOG: Optional 0-99 or 0-999 garma

Permits externally triggered operaticn with pe riods longer than 1.85 sec. (optional minimum period 0.9 sec.)

12V 0.7A peak, 5mA standby

INTERNAL: 12V 0.75Ah NiCd rechargeable battery 3,000 readings per full charge

EXTERNAL: 12-18V

Input: 110/220V 50/60HZ; output: 14V 75mA DC

-35 to +55C

CONSOLE: ISxfixlSon (6x3)06")

SENSOR: 14x7on dia (5"jx3" dia)

STAFF: 175cm (70") extended, 53cm (21") col lapsed, or 4 45cm (18") sections

2.7kg (6 Ib) per standard corplete with batte ries

••rf-, E V^v'-lr*'' r ' 'i'.'ifl'r'iii*1, '-••- :". ."' ^ ^^C".'-XVi"jC*- t ,"H''*^^;^' ; ' '-''^;'"' ;^^^..*" :-^?"--^

—- j ------ ma - - - :: - - --JL-

Figure 3.1

3. OPERATING INSTRUCTIONS- 7 -

3.1 INSTRUMENT DESCRIPTION

Major parts of the magnetometer are shown in fig. 3.1

(1) SENSOR, optimized for high sensitivity and gradient tolerance

(2) FILLING PLUG, to fill the sensor with proton rich liquid (kerosene or similar)

(3) CABLE CONNECTOR

(4) CABLE

(5) ORIENTATION LINE

(6) STAFF

(7) SHOULDER STRAP

(8) SENSOR CABLE CONNBCILR/ON-OFF SWITCH

(9) RANGE SWITCH

(10) DISPIAV WINDOW

ill) PUSHBUTTON, to initiate a desired mode of operation

(12) CHARGER/INTERFACE CONNECTOR for digital/analog output and external trigger, charger or external batteries

3.2 SET-UP AND OPERATING PROCEDURES

GSM-B is shipped with fully charged internal batteries, ready for field opera tion. To set-Lip the instrument, the sensor should be attached to the staff with correct direction of the orientation line and the staff extended. Connecting the cable to the front panel sets the instnnent in standby state. The display may or may not light at this point.The Range switch should now be switched to position closest to the local total iragnetic field intensity as shown in fig. 1.1Operation of the GSM-8 is internally nonltored and incorrect readings (due to external interference, excessive gradient or internal breakdown) are marked by two decimal points appearing after third and fourth digit of the display. Readings marked by decimal points should be disregarded.For best results the Range switch should always be set to the position closest to the first two digits of the displayed value of magnetic field. During surveys this may need occasional correction.

There are three modes of operation Of GSM-B l

b)

c)

a) Short depressinq of the pushbutton will initiate a SINGLE READING. Initiation is marked by a colon after second digit of the display. The colon stays liqhted only durinq polarization interval. The value of measured magnetic field appears on the display in gammas after about 1.85 sec. and stays displayed until the next reading isl taken or the instrument switched off. Incorrect readings are markej by decimal points, which stay displayed with the reading.

In SELFTEST MODE the pushbutton is pressed permanently. This mode consists of one normal reading of magnetic field, display test (displaying 88888) and battery test. Battery voltage is shown in ij although accurate only about 5*. This cycle is being repeated as long as the pushbutton is depressed.

In CYCLING MODE the pushbutton is depressed during polarizing infc until a new reading appears on the display and then released. Aft' display and battery tests, the instrument will start cycling auto matically at the rate of one reading in about 1.85 sec. A short depression of the pushbutton at any time will stop cyclina (after completing the cycle under way).Cycling mode is very convenient for base station and vehicle born'? operations or Cor a quick check-up of instruments consistency. . However, as it results in a large number of readings and relatively fast draining of the batteries, the cycling mode can optionally be disabled to prevent accidental initiations in a field.

Before starting a survey the batteries and the display should be checkej Battery voltage for fully charaed batteries must be above 12,500 on tht display. No survey should be started with battery voltaae being below 11,000 mV as shown on the display.

3.3 EXTERNAL BATTERIES

4. MUNftHftTCE AND REPAIR

- 9 -

GSM-8 is generaly^Rintenance free except for occasional cleaning and visual inspectioitfjtfi*chard.cal conditions of the cable, sensor and display window. Due tpjiosnblUties of gathering magnetic dust, the sensor, cable and staff should be periodig&ly washed with soap or detergent and water. Beycnd that a normal "carmen oonfe care" should ensure lasting use in rough field conditions.

When not uaeZr for longer periods the instrument should be returned to the car rying case, with sensor disconnected from the console.* i'Batteries should be kept charged when storing,the instrument. As NiCd batte ries have a memory , cycles of partial charging and discharging may result in reduced capacity. This can be cured by few cycles^ of full discharging and charging. Relatively fast discharge can be achieved by'setting^the instrument into cycling. Normal charging will take 14-16hr, while'fast charging using special charger (available from the manufacturer) can be'completed, within 3-4hr Spare NiCd batteries are readily available fron the manufacturer.'^.

'*- Ir ttt - ,.frSensor cable might occasionaly get damaged or broken iff heavy use. Vten repai ring be careful to connect centre wire to positivanerninal of the sensor and. pin A of input connector. All other wires and a shield are connected to negative terminal of the sensor and pin B of input connector. Pins C and D of the input connector must be shorted; the short acts aa J the main switch.

Use of improper external battery or short circuit in the sensor-cable assembly may blow a fuse (instrument appears completely dead). Spare fuses are found on the smaller of the two boards. The fuse must be soldered in, but it is highly reccnmended that the cause of malfunction be previously determined and removed. If sensor short is suspected, an ohm-meter can be used to measure a resistance between pins A and D of the input connector. It must be within 15-20 Chm. '"j;.-,** T^- - * .

While internal batteries satisfy any requirements for normal hand held (portable) operation even in cold weather, use of external batteries nu™, be necessary for base station or vehicle borne operation where automatic cycling is needed. For this purpose any 12V car battery will be satis factory, although lightweight external battery packages with sufficient^ capacity for 6-8hr of cycling operation may be ordered from the manufacl urer. \ Leads of the car battery can be connected directly to pins D (positive) and E (negative) of the Charger/Interface connector at the side of the console. Use of higher voltage batteries (up to I8v) requires that in ternal NiCd batteries be disconnected by opening an internal two pin , connector. Alternatively the batteries can be removed from the consolo by removina the instrument out of the case and then removing two screws at the range switch side of the larger PC board, pivoting the board for 90 degrees and undoing four screws holding the battery pack. Use of batteries of more than Ifiv may damaqe the instrument.External battery packs for disposable C or D size batteries, special . Alcaline or Mercury flat pack batteries are available from manufacture*!

S. WARRANTY

The GSM-8 is warranted against defects in material* and worhnanship for a pe riod of 15 months from the date of shifplag. . --*- -, f p .* ' •',-J.^-' J-\-,[ t----' '-'i' l '*'""Any defects resulting from npxml oM-in-thlf tauacanty period will be repaired free of charge by CTH "-

Instruments will be ——r —— returned to the custofttCJ),

rfThis warranty does not cover if the instrument is jopened orGEM Systems.

1

hipped prepaid, and will be

it and will be void not authorized by

Ontario Ministry ofNorthern Developmentand Mines

Declaration of Assessment Work Performed on M ining Land

Mining Act, Subsection 65(2) and 66(3), R.S.O. 1990

Transaction Number (office use)

Assessment Files Research Imaging

Drity of subsections 65(2) and 66(3) of the Mining Act. Under section 8 of the ed to review the assessment work and correspond with the mining land holder, ining Recorder, Ministry of Northern Development and Mines, 6th Floor,

42A06SE2004 2 .18708 LAKQMUIR 900

Instructions: - 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) *5) . JL O w O

Name"t^^M^- VA^VXvAvE-ii^

Address-4^*-^ T7X*}*JL^" -^"V •*1W*-? vc^rA^- ^ \-

Ô*JC"\y\ I^PX^JtÂA^^fr-fei^T-i OV-XT

Name

Address

Client Number\I Q O '"!/ IvO v T"f(0

Telephone Number

Fax Number

Client Number

Telephone Number

Fax Number

2. Type of work performed: Check ( s ) and report on only ONE of the following groups for this declaration.

Geotechnical: prospecting, surveys, assays and work under section 18 (regs)

i—i Physical: drilling, stripping,l—l trenching and associated assays |~~1 Rehabilitation

Work Type

IA M^ cortex vi^.Office Use

Commodity

Total S Value of Work Claimed

Permed* *omDay Month Year

To O&Day Month Year

NTS Reference

Global Positioning System Data (if available) Township/ AreaMining Division

M or G-P!an Number Resident Geologist District

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

Name Telephone Number

Address Fax Number


AddressFax Number


G&VÂddress

AUG 18

4. Certification by Recorded Holder or AgentGEOSCIENCE ASSESSMENT

OFFICE

. do hereby certify that 1 ha\__ ___________ , __ f . -.,.,.^., J ,. .acts set(Print Name) ' " ""'"""""

forth in 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, the annexed report is true.

Signature of Recorded Holder Date

Agent's Address Telephone Number Fax Number

* f s\ S* ^V*

must accompany this form.

Mining Claim Number. Or \1work was done on other eligible mining land, show in this column the location number indicated on the claim map.

eg

eg

eg

1

2

3

4

5

6

T8 7827

1234567

1234568

T** iy t -3 "T \ \p

^^ f3L''J (C"^t t'^1

78

g

10

11

12

13

14

15

Number of Claim Unit*. For othermining land, list hectares.

16 ha

12

2

\

l

Column Totals

Value of work performed on thib claim or other mining land.

S26, 825

0

S 8, 892

GTO.75W63S

jE•^

13f^.5D

f xapp'.-U to thia claim.

N/A

S24,000

S 4,000

Gtbtf^e*fi

"- 1 87

V3T7-*SOt -•* L|l j,-1 ^^f. -——

Value of work •Mlgned to other mining claims.

S24.000

0

0

—

—

Q Q

*—-

Bank. Value of *wk to be distributed at a future date

S2.825

0

34,892

-

r*.

•K ———

, do hereby certify that the above work credits are eligible under(Prim Full Name)

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

the claim where the work was done.

Signature of Recorded Holder or Agent Aut d in Writing

ViceDate

6. Instructions lor cutting back credits that are not approved.

Some of the credits claimed in this declaration may be cut back. Please check ( s ) in the boxes below to show how

you wish to prioritize the deletion of credits:

D 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

D 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):

Note: tt you have not indicated how your credits are to be followed by option number 2 if necessary.

RECEIVED^ \0 l,V\^

AUG 18 1S9S

GEOSCIENCE ASSESSMENTf plptpri ri rJJiHM*h"'li *" a f

For Office Use OnlyReceived Stamp

from the Bank first, , PORCUPINE - ^

Deemed Approved Date

Dale Approved

Date Not.f'Cation Sent

Total Value of Oed't Ap

Approved tor Recording by Mining R&corder (Signature)

Ontario Ministry ofNorthern Developmentand Mines

Statement of Costs for Assessment Credit

Transaction Number (office use)

Personal Information.collected on this form Is obtained under the authority of subsection 6 (1) of the Assessment Work Regulation 6/96. Under section 8 of the Mining

Act, this Information Is a public record. This Information will be used to review the assessment work and correspond with the mining land holder. Question* about this

collection should be directed to a Provincial Mining Recorder, Ministry of Northern Development and Mines, 3rd Floor, 933 Ramsey Lake Road Sudbury Ontario P3E

6B5.

Work Type

^/N/E^jUTHr^6p*5 tSUiZve'/

Ui^UETOMeiEK

Units of workDepending on the type of work, list the number of hours/days worked, metres of drilling, kilometres of grid line, number of samples, etc.

Z*5'7kuA /^2-LuJ————— ̂ ————— * ———— i —— "2 ptp\A,-V?b

"3-"Z~ I^H^

————— ———————————————————— O ————— *

' 1

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

Transportation Costs

Food and Lodging Costs

Cost Per Unit of work

2?5 -•?s-'0

*S"

^ ? Q q———— vy ^ ————

( Total Value of Assessment Work

Total Cost

10 Z®"Isro^

7Z1 50

-

/,3?? s

Calculations of Filing Discounts:

1. Work filed within two years of performance is claimed at 10Q 0Xo of the above Total Value of Assessment Work.

2. If work is filed after two years and up to five years after performance, it can only be claimed at SO'/o of the Total

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

TOTAL VALUE OF ASSESSMENT WORKx 0.50 s 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 45 days 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:

,, do hereby certify, that the amounls shown(please print full name)

be determined and the costs were incurred while conducting assessment work ( n

RECEIVEDA MP i B ' ''C"~!

vn are as accurate as may reasonably

tie accompanying

Declarat! a !? W/l^^M holdar.Tgftnt. or slate company posilion with signing authority)

'zsi* \y i ^ M f

0212 (03/87)

am authorized to make this certification.

Signature Dale

Ministry of M inisters duNorthern Development Developpement du Nordand Mines et des Mines Ontario

Geoscience Assessment Office 933 Ramsey Lake Road

October 5, 1998 6th FloorSudbury, Ontario

DAVID MEUNIER P3E 6B5P.O. BOX 1624403 DOME STREET Telephone: (888) 415-9846SOUTH PORCUPINE, Ontario Fax: (877) 670-1555PON-1HO

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

Dear Sir or Madam: S ubmission Number: 2 .18708

Status Subject: Transaction Number(s): W9860.00740 Deemed Approval

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 Lucille Jerome by e-mail at [email protected] or by telephone at (705) 670-5858.

Yours sincerely,

ORIGINAL SIGNED BYBlair KiteSupervisor, Geoscience Assessment OfficeMining Lands Section

Correspondence ID: 12912

Copy for: Assessment Library

Work Report Assessment Results

Submission Number: 2 .18708

Date Correspondence Sent: October 05, 1998 Assessor: Lucille Jerome

Transaction Number

W9860.00740

Section:14 Geophysical MAG

First Claim Number

825716

Township(s) l Area(s)

LANGMUIR

Status

Deemed Approval

Approval Date

September 29, 1998

Correspondence to:

Resident Geologist South Porcupine, ON

Assessment Files Library Sudbury, ON

Recorded Holder(s) and/or Agent(s):

Brian PolkTIMMINS, ONTARIO, CAN

DAVID MEUNIERSOUTH PORCUPINE, Ontario

Page: 1Correspondence ID: 12912

G-3226

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DiabasePorphyritic Intrusive Mafic Volcanics Ultramafic Volcanics Linear Interpreted Geological contact

Scale: 1 : 2 000

50 100m

42A06SE2004 2 .18708 LAKGMUIR 210

BLACK PEARL MINERALS INC.MAGNETOMETER SURVEY St INTERPRETATION

West Langmuir Claims Langmuir Twp., ON

Map 1 August 1998

Polk Geological Services

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