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52L10NW0003 2 .11369 EAGLE LAKE010

REPORT ON

THE GEOPHYSICAL SURVEYS.

BEE LAKE PROPERTY,

KENORA DISTRICT. ONTARIO

NTS 52L/10.11

PREPARED FOR

GANDY RESOURCES CORP.

DERRY, MICHENER, BOOTH * WAHL

R. W.

Toronto, Ontario June 17, 1988

Ref.: 88-62

This report may not be reproduced, in whole or in part, without the written permission of Derry, Michener, Booth 6c Wahl.

DERRY, MICHENER, BOOTH a WAHL

11 '11111111111111111

111 lllllllll^ 52L10NW0803 2.11369 EAGLE LAKE 010C

INTRODUCTION

PROPERTY LOCATION, DESCRIPTION AND ACCESS

PROPERTY GEOLOGY

SURVEY PARAMETERS AND PRESENTATION

Magnetic SurveyElectromagnetic Survey

RESULTS AND CONCLUSIONS

Magnetic SurveyElectromagnetic Survey

RECOMMENDATIONS

CERTIFICATE OF QUALIFICATIONR. W. Woolham, P.Eng.

APPENDIX I: INSTRUMENT SPECIFICATIONSAPPENDIX II: TECHNICAL DATA STATEMENT

LIST OF FIGURES

Figure 1: Location MapFigure 2: Claim Map

LIST OF DRAWINGSOn Map Pocket)

Fluxgate Magnetic Survey, Scale 1:5,000

88-62-01: West Sheet, Values88-62-02: East Sheet, Values88-62-03: West Sheet, Contours 88-62-04: East Sheet, Contours

DERRY, MICHENER. BOOTH ft WAHL

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After Page

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LIST OF DRAWINGS (cont'd.)l

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Horizontal Loop Electromagnetic Survey, Scale 1;5000 444 Hz Frequency! Profiles and Values

88-62-05: West Sheet 88-62-06: East Sheet

1777 Hz Frequency, Profiles and Values

88-62-07: West Sheet 88-62-08: East Sheet

Miscellaneous Maps

88-62-09: Interpretive Geophysical Compilation, Scale 1:10,000 88-62-10: Claim and Grid Map, Scale 1:10,000

DERRY. MICHENER. BOOTH ft WAHL

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-1-

INTRODUCTION

Geophysical surveys, utilizing the magnetic and electromagnetic methods,

have been completed on the Bee Lake claim group of Gandy Resources Corp. The surveys were performed by the staff of Derry, Michener, Booth to. Wahl (DMBW)

under the direct supervision of the author. The surveys were conducted during the periods June 22 to July 22, 1987 and February l to March 15, 1988. This report

describes the results of the geophysical surveys.

In the 1987 summer field season, DMBW staff carried out a geological

mapping program designed to evaluate the potential of the property for hosting

auriferous iron formation (ref. 87-95). At that time a magnetic survey was

completed over most of the land portions of the claim block. Final evaluation and

interpretation was deferred until all of the geophysical work was completed on

the water portions of the claim block.

PROPERTY LOCATION. DESCRIPTION AND ACCESS

The Bee Lake property is located 10 km east of the Manitoba-Ontario

border, approximately 110 km northwest of Kenora, Ontario and 80 km northeast

of Lac du Bonnet, Manitoba (Figure 1). The property consists of 109 contiguous staked claims covering approximately 1,744 hectares (Figure 2). The claims are as follows:

951398 - 951400 inclusive 951970 - 952007 inclusive 951451 - 951458 inclusive 952010 - 952033 inclusive 951476 - 951481 inclusive 952050 - 952069 inclusive

. 951492 - 951501 inclusive

The claims are under extension to June 30, 1988.

The property straddles the southeast half of Bee Lake and continues

eastward to cover much of Eden Lake. The property is accessible with float- or

ski-equipped aircraft which can land on either Eden Lake or Rickaby Lake which

lies immediately south of Bee Lake. The nearest road is approximately 25 km


l ONTARIO J BEE LAKE Jdr PROPERTY

BEE LAKE PROPERTY

Snowshoe Lake

Trapline Lake

ERNER LAKE

FIGURE 1

LOCATION MAP

l95*00'w

WINGISKUS

LAKE

RICKABY LAKE AREA

G-2638

9S2OS4

991400

l mile

l kilometre

952O33

*. 395I4SI

95131

EAGLE LAKE AREA

G-2615

952OS2

951398

952051

951453

951 SOI

^51492*

952050

951454

951500

931458

95M55

951499

951457 -

951496

951498

9514*5

50*40*11 -

EDEN

•\ LAKE

FIGURE 2

BEE LAKE PROPERTY

CLAIM MAP95*00' W


-2-

south of Bee Lake. It connects Gordon Lake, Ontario, site of the old nickel-copper mine of Consolidated Canadian Faraday Ltd., with Lac du Bonnet, Manitoba. Gordon Lake could be used as a staging point for helicopter airlift of a diamond drill to Bee Lake.

PROPERTY GEOLOGY

The property is underlain by acid metavolcanic and clastic

metasedimentary rocks with lesser interbedded acid tuff and quartzite, iron formation and basic metavolcanic rocks. A small body of hornblende-biotite quartz monzonite intrudes the rocks at the east end of Rickaby Lake.

The main acid metavolcanic unit, composed of tuffs, flows and agglomerates, is central to the property. It reaches a maximum thickness between Bee and Anderson lakes but decreases in thickness southeastward as it interdigitates with metasedimentary rocks. The rocks are fine-grained, poorly foliated and weather light grey. The matrix of the agglomerates is dark grey to green.

Metasedimentary rocks comprising predominantly arkose, arkose conglomerate and phyllite are also abundant in the central part of the property. Minor biotite-feldspar quartzite occurs immediately north and south of Rickaby Lake. Interbedded acid tuff and biotite-feldspar quartzite occurs along the northern property boundary.

Iron formation extends southeastward across the property in two discontinuous bands. The thicknesses of the bands range from a few centimeters to approximately 23 m but they are usually about 9 m to 12 m across. Well- bedded magnetite with accessory quartz forms 596 to 1596 of the total volume of the iron formation unit. Magnetite beds are usually 5 cm to 8 cm thick but may vary from less than 2.5 mm to 61 cm. The remainder of the iron formation is phyllite with local lenses of black chert or thin beds of jasper, arkose or dacitic tuff.



-3-

Basic metavolcanic rocks, namely dark grey to black, fine-grained,

foliated amphibolites and epidote amphibolites are present along the southern

property boundary.

Several small faults crosscut the stratigraphy. The faults generally trend

north-northeast but a few also trend east-southeast.

Geochemically anomalous gold values up to 3,465 ppb were obtained from grab and chip samples in the vicinity of line 1,100 west and 200 north. This

mineralization occurs within a sulphide replacement zone in magnetite iron formation.

SURVEY PARAMETERS AND PRESENTATION

Magnetometer Survey

A Scintrex MF-1 Fluxgate magnetometer was used to measure the vertical magnetic field (see instrument specifications Appendix I). Readings were

taken every 25 m along the grid lines on lake portions of the property and at

12.5 m intervals on land portions. The main target definition on the property was

iron formation, therefore, diurnal correction control was not required for this

property. Base stations were monitored three times a day, however, in the event

a major magnetic storm developed. Survey line separation was 100 m. A total of

approximately 170 line km of magnetic data were collected and plotted in the

field for preliminary evaluation. Subsequently, office compilation consisted of

entry of the data values on the field maps into the DMBW computer system. These values were then machine plotted using a plotting facility at Markham Data

Ltd. Survey maps were generated at a scale of 1:5,000 with appropriate title and

legend. The values were plotted on separate maps from the contours (Drawings

88-62-01 to 88-62-04).



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Electromagnetic Survey

The electromagnetic instrument was an Apex Parametrics Ltd. Max-Min II unit. Instrument specifications are contained in Appendix I. A coil spacing of

150 m was used for the survey with a station reading interval of 25 m. Survey lines were 100 m apart. Accurate leveling of the coils was monitored at each

station and correct coil distance was maintained using the picket line chainages. The in-phase and quadrature readings at frequencies of 444 Hz and 1,777 Hz were

measured at each station. A total of about 170 line km of two frequency data or

about 27,000 readings were collected on the property.

The values were plotted in the field for preliminary evaluation at a scale of 1:2,500. Subsequently, office compilation consisted of entry of the data values

on the field maps into the DMBW computer system. These values were then

machine-plotted using a plotting facility at Markham Data Ltd. Survey maps were generated at a scale of 1:5,000 with appropriate title and legend. The

in-phase and quadrature values are represented as solid and dashed profile lines,

respectively (Drawings 88-62-05 to 88-62-08 inclusive).

RESULTS AND CONCLUSIONS

Magnetic Survey

Within the main iron formation units that occur on the property, the magnetic amplitudes exceeded 5,000 nanotesla (nT). Lower values of 1,000 nT to

5,000 nT were recorded over narrow iron formation units. Other magnetically

anomalous trends, probably related to mafic flows and tuffs, having amplitudes of

250 nT to 1,000 nT are present throughout the claim block. The trend patterns

formed by these lower amplitude anomalies assist in identifying more subtle

structures related to folding and faulting.

Map 88-62-09 is an interpretive compilation of the magnetic trends and

shows what are thought to be the main iron formation horizons as well as the

lower amplitude magnetic trends. The major iron formation horizon starts at the

DERRY, MICHENER, BOOTH ft WAHL


-5-

northwest corner of the claims and strikes east-southeast through Eden Lake. At

the east end of Eden Lake the formation forms an "S" fold with the top of the "S" showing a pronounced westerly plunge anomaly pattern. The bottom of the "S"

trends east-west but terminates at line 2,000 east. A possible sheared and/or

faulted portion of the horizon resumes a few hundred meters to the west. About

400 m to the south a second sub-parallel horizon is present. This horizon

terminates abruptly to the east, possibly fault bounded, and trends off the

property to the west. Examination of airborne magnetic data available from

assessment file information suggests that this southern unit folds back on itself to

join with the northern unit. The exact structural continuity of the iron formation

horizon is difficult to determine further to the west. Strike and cross faults have

produced a complex pattern. It is suggested, however, that the major high

amplitude magnetic horizons represent a single horizon folded on itself to form a

major synclinal structure with a plunge to the west. Within this syncline minor

parasitic "S" and "Z" folding is locally present.

Major cross-faulting patterns are apparent in the western part of the

north limb of the iron formation between lines 2,000 west and 3,500 west. Here

the flanks of the magnetic anomaly broaden abruptly suggesting a combination of increasing width and depth of burial. In this area iron formation outcrops on

islands in the lake. This suggests that a change in width and dip are producing the

broader anomalies rather than relative depth of burial.

The gold mineralization in iron formation, reported in the geology section

of this report, is coincident with an extensive high amplitude magnetic horizon

stretching from line 400 east to about line 1,500 west. A portion of this horizon is

conductive, to be discussed in the next section and probably represents the extent

of the sulphide alteration and potential gold mineralization in this area.



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Eleetromagnetie Survey

The electromagnetic response is dominated by two types of conductive sources. The first is related to conductive lake bottom sediments which produce

edge effect anomalies along the shore of Eby Lake, especially at the east end of

the lake and in the middle of the lake. The second source is related to the iron

formation. Within the iron formation horizons there are conductive sulphide

and/or magnetic oxide phases. As just mentioned, if sulphides are present they

may be related to alteration processes and can be a harbinger of gold

mineralization.

The flat sheet-like conductive lake bottom sediments generally have a

specific electromagnetic signature having poor conductivity and anomaly profiles

very different from the typical near vertical bedrock conductor. In this situation

such conductors can be easily recognized by their in-phase and quadrature

response signatures. With the iron formation horizons, however, the

electromagnetic response can be complex as two opposite electromagnetic fields are operating. High concentrations of magnetite produce a susceptibility effect

that produces a positive in-phase response. On the other hand, a conductive

source such as massive sulphides or graphite, produce a typical negative in-phase

response with flanking positive shoulders. When an iron formation contains both sulphide and magnetite phases because of either natural facies changes or

alteration processes, the electromagnetic profile is distorted. Where the iron formation is in proximity to areas where conductive overburden effects are

present further anomaly distortion occurs making it difficult to correctly interpret conductive effects due to possible sulphides and other effects of no

interest. Collection of electromagnetic data at two different frequencies sometimes helps to resolve these difficulties.

There are several locations along the iron formation horizons where a

conductive response occurs coincident or nearly coincident with the magnetic response, indicating the possible presence of sulphides. Unfortunately, graphite,

which is often common in a sedimentary environment can also produce similar conductive effects if it occurs in close proximity to the iron formation.



-7-

Nevertheless, those portions of the interpreted iron formation that are conductive

are prime exploration targets.

The interpretive geophysical compilation map designates the conductive portions of the magnetic horizons as sulphide iron formation. As mentioned

previously, the gold mineralization already discovered on the property is associated with the iron formation horizon between lines 400 east and 1,500 west

just north of the baseline. The compilation map indicates that only the east part of this magnetic horizon is conductive. The gold mineralization occurs at the

west end of the conductive portion of the iron formation near an interpreted crosscutting fold/fault structure. Thus a major strike length of favourable iron

formation exists in this area.

Portions of several other iron formation horizons are also conductive. Of

most interest is an area between line 2,400 west and 3,400 west. Here, the highest conductivity response of the whole survey was recorded. Reconnaissance mapping and sampling discovered the presence of a highly altered pyrite iron

formation unit. No significant gold values were obtained from grab samples in

this area, however, only a very small portion of the horizon was sampled. Many of

the other favourable horizons on the property that occur in suboutcrop areas were not sampled because of time and budget limitations.

RECOMMENDATIONS

The geophysical surveys have delineated several conductive and magnetic

iron formation horizons. Gold mineralization is known to be associated with one

of these horizons. Sampling of other portions of the iron formation has been very

limited to date. Therefore, it is recommended that a comprehensive and detailed mapping, sampling and stripping program, designed to explore the most favourable

iron formation horizons, be planned for the Bee Lake property. This work will

direct a follow-up drill program designed to test, at depth, targets defined by the

surface exploration work.



-8-

CERTIFICATE OF QUALIFICATION

I, Roderick W. Woolham of the town of Pickering, Province of Ontario, do hereby certify that:-

1. I am a geophysicist and reside at 1463 Fieldlight Blvd., Pickering, Ontario, L1V 2S3.

2. I graduated from the University of Toronto in 1961 with a degree of Bachelor of Applied Science, Engineering Physics, Geophysics Option.

3. I am a member in good standing of the following organizations: The Association of Professional Engineers of the Province of Ontario (Mining Branch); Society of Exploration Geophysicists; South African Geophysical Association.

4. I have been practising my profession for a period of more than 25 years.

5. I am an Associate with Derry, Michener, Booth fc Wahl, Consulting Geologists and Engineers.

6. I have not received, nor do I expect to receive, any interest, directly or indirectly, in the properties or securities of Gandy Resources Corp. or any affiliate.

7. I personally was involved with the technical supervision of the survey and wrote the report.

8. I consent to the use of this report in submissions for assessment credits and for similar regulatory requirements.

Toronto, Ontario June 17, 1988



APPENDIX I

INSTRUMENT SPECIFICATIONS

DERRY, MICHENER. BOOTH a WAHL


i,.

i.

1. Range Switch

2. Meter3. Main Switch

4. Level

5. Battery Pack

6. Battery Connector

7. Silica Gel

8. Protection Cap

9. Latitude Adjustment Control Fine

10. Latitude Adjustment Control Coarse

11. Carrying Strap

MODEL MF-1 FLUXGATE MAGNETOMETER

SHARPE INSTRUMENTS

a division of .

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MODEL MF-1 FLUXGATE MAGNETOMETEROperation of the M*t*r1.) Remove all magnetic objects from operator's person, e.g. keys, coins, buttons, etc.

Zippers should be non-magnetic.2.) C onnect Battery Cable, Figure 6, to magnetometer receptacle on bottom of main hous

ing. This connection must be secured by lock-ring.3.) Attach battery pack (Fig.S) either in back pocket or on belt behind operator.4.) Switch on Main Switch (Fig. 3) to iirst position, which is the battery check. Indicating

meter needle should rest within red arc. Replace batteries if reading below red arc.5.)LatitudeA3justnent -To adjust the latitude setting to read O gammas is a simple operation.

a. After indicating meter needle (f ig.2) shows voltage okay, switch Main Switch (Fig.3) to next position which is the positive reading with the Range Switch (Fig. 1) set at the 100K step. (100,000 gamma range)

b.If needle goes full arc to left past O, switch main switch (Fig. 3) to last position which is the negative reading range.

c. Figures 10 am! 9 indicate the latitude adjustment controls - Coarse control is Fig. 10 and Fine control is Fig. 9. If scale reading is mote than 17,000 gammas rotate coarse control (Fig. 10) in steps of 7,000 and switch range down to more sensitive range until scale is reading less than * 7,000 gammas. Remove protection cap on fine control (Fig. 8) by pulling straight off. Then rotate fine control switch (Fig. 9) until scale reading Is O gammas. Check reading by switching main switch from positive to negative (or vice versa) to ensure O reading both polarities. Replace fine control protection cap.

6.) Calibration -This meter is calibrated at the factory prior to delivery. Field tests show that only by severe misuse (i.e. constant dropping, rough handling, improper shipping)

can the calibration of this instrument be effected. It is therefore not necessary to re calibrate in the field and if through Misuse calibration becomes necessary, the meter should be returned to the factory. 'All parts are guaranteed against defect for a period of one year and will be replaced free of charge.

This guarantee does not apply to batteries or the connecting cable.7.) Trouble Shooting - Under normal conditions the only field problem will be batteries or

the connecting cable. 11 alter completion of step (4) under "Operation of the Meter" the meter still does not indicate voltage, check cable for faulty connection or broken cable. If after this procedure, meter still does not indicate current, teturn unit immedi ately to your supplier or directly to the factory.

Regional Latitude SettingsNormally each unit is pre-set at the factoiy for the Northern Hemisphere. However, if the unit is required for Equatorial or Southern Hemispheric regions, the unit will be pre-set at the factory for these areas. If a unit is going from one of the above regions to another, reset instructions will be supplied on request.Field Procedure1.) Select Base Control station. This station should be selected in relation to one or

both of two things.1. General magnetic background (i.e. not anomalous) if possible. l. Accessibility-in relation to area being surveyed.

2.) Set magnetometer to read between O and 200 gammas.(For contouring and to avoid small negative readings, an arbitrary value of 1000-800 gammas should be added to allreadings.

3.) For effective diurnal control, control stations should be permanently marked and read ings should be taken at the same height and location each time; a simple method is to have the control stations' pickets hammered into the ground with the top about waist height. Rest the probe end of the magnetometer on the top of the picket. In barren country,a mound or large piece of rock or some other material should be used.

4.) Continue survey the same as any other method of magnetic surveying.5.) Remove and replace Silica-Gel (Fig.7) when deteriorated. The silica gel is located

in the removable probe housing. The Silica bag should not be placed on the bottom of the probe housing.

6.) Do not pass powerful magnet closer than l foot to instrument.7.) During winter operation, batteries should be kept in pocket or under parka. Warning: - Do not leave batteries in battery case when unit is being stored. Always be

be sure meter is turned elf after use. Disconnect battery cable when meter not in use.

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MAXMIN II

SPECIFICATIONS :

Frequencies: 222, 444, BBS, 1777 and 3555 Hz. Repeatability:

Modes of Operation: MAX: Transmitter coil plane and re ceiver coil plane horizontal C Max-coupled; Horizontal-loop mode). Used with refer.cable.

M l N: Transmitter coil plane horizon tal and receiver coil plane ver tical CMin-coupled mode). Used with reference cable.

V. L. : Transmitter coil plane verti cal and receiver coil plane hori zontal (Vertical-loop mode). Used without reference cable , in parallel lines.

25,50,100,150,200 a25Om CMMB) or 1OO, 2OO, 3OO, 4OO.6OO end BOO ft. C MM H F ) . Coil separations in VL.mode not re stricted to fixed velues.

Vo to f\'/, normally, depending on conditions, frequencies and coil separation used.

Transmitter Output i - 222Hz : 175A6ma- 444HZ : 16OAtma- aSS Hz : 1COAtnn2- 1777 Hz : SOAtma-3555 Hz: 3OAtma

Coll Separations:

Parameters Read: -

Readouts:

Scale Ranges :

Readability:

In-Phase and Quadrature compo nents of the secondary field i n MAX and M IN modes.

Tilt-angle of the totel field in V.L. mode .

- Automatic, direct readout on 9Omm C3.5") edgewise meters in MAX and MIN modes. No null ing or compensation necessary.

- Tilt angle end null in 9Omm edge wise meters in VL.mode .

In-Phase: 2Oy., 1OOV. by push button switch .

Quadrature: S2O'/., 1OO V. by push button switch .

Tilt: 75 "/i slope .Null CVLJ: Sensitivity adjustable

by separation switch.

In-Phase and Quadrature: 0.5 ".4. Tilt: 1Vo

Receiver Batteries

Transmitter Satte r l e s :

Reference Cable :

Voice Link:

Indicator Lights:

Temperature Range:

Receiver Weight;

Transmitter Weight:

Shipping Weight:

9V trans, radio type batteries (4). Life: approx. 35hrs. continuous du ty (alkaline, O.5 Ah), less in cold weather.

12V7.5Ah Gel-Cell rechargeable batteries C S x 6V in series).

Lightweight 2-conductor teflon cable for minimum friction. Unshield ed. All reference cables optional at extra cost. Please specify.

Built-in intercom system for voice communication between re ceiver and transmitter operators in MAX and MIN modes, vis re ference cable .

Built-in signal and reference warn ing lights to indicate erroneous readings .

-4O"C to+SO'C C-4O"Fto*14O'F).

6kg C13lbs.)

13kg (29lbs.)

Typically SOkg C135lbs.), depend ing on quantities of reference cable and batteries included. Shipped in two field/shipping cases.

Specifications subject to change without notification.

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PAHAMETP3CS LIMITED2OO STEELCASE RD. E.. MARKHAM, ONT. CANADA, L3R 1G2

Phone: C 416) 495-1612 Cables: APEXPARA TORONTO Telex : OS-966773 NORDVIK TOR


APPENDIX H

TECHNICAL DATA STATEMENT

DERRY. MICHENER. BOOTH St WAHL

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Ministry of Natural Resources

GEOPHYSICAL - GEOLOGICAL - GEOCHEMICAL TECHNICAL DATA STATEMENT

File.

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

TECHNICAL REPORT MUST CONTAIN INTERPRETATION, CONCLUSIONS ETC.

Type of Survey(s)

Tonrnchip or A*-~-

Claim HnlHer(s)

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Author of Report

Address

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Covering Dates of Survey 3u*faVJt*l*y S7. Fe^(linecutting to office)

Total Mitoe-of Line Hut l

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SPECIAL PROVISIONS CREDITS REQUESTED

ENTER 40 days (includes line cutting) for first survey.

ENTER 20 days for each additional survey using same grid.

Geophysical

Electromagnetic.

DAYS per claim

1.0

-Other-

AIRBORNE CREDITS (Special provision credit! do not apply to airborne lurveyi)

Magnetometer -Electromagnetic. . Radiometric(enter dayt per claim)

; Ju^e 17 /g g SIGNATURE:ior of Report or Agent

Res. Geol.. . Qualificationsfa*

Previous Surveys File No. Type Date Claim Holder

MINING CLAIMS TRAVERSED List numerically

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Ontvio52L10NWe803 2.t 1369 EAGLE LAKE

Report of Work i DOCUMENTN

(Geophysical, Geological, J W8801' l VO Geochemical and Expenditures)

900

Type of S urveyd)

Mqg-vY-H&'VicTownship or Area t-.f)fZ

ProspectoriiUlcence No.

rClaim HotdJr(s)

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Address

rincon ADate of Survey (from ft to)

VVSHSurvey Company

Name and Aidress of Author (of GeO-Technical report)ts.2.2- . Ot. tt .Day | Mo. | Yr. \ Day | Mo. | Yr.

Total-WTTW of line Cut

Credits Requested per Each Claim in Columns at rightSpecial Provisions

For first survey:

Enter 40 days. (This includes line cutting)

For each additional survey: using the same grid:

Enter 20 days (for each)

Man Days

Complete reverse side and enter total (d^iet* f* r

JUl

MIKING Ul

Airborne Credits

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

Geophysical

- Electromagnetic

- Magnetometer

- Radiometric

- Other

Geological

Geochemical

Geophysical

I v^1Wagnetlc- Magnetometer

7 I98^mstric- Other

U&JiEGTION

Geochemical

Electromagnetic

Magnetometer

Radiometric

Oayt per Claim

40

2X3

Days per Claim

Days per Claim

Mining Claims Traversed (List in numerical sequence)

Expenditures (excludes power stripping)Type, of Work Performed

Performed on Clalm(s)

Calculation of Expenditure Oayt Credit!

Total Expenditures

S 4-15

Total Days Credit!

"d

Instructions Total Deyi Credit! may be apportioned at the claim holder's choice. Enter number of days credit! per claim selected in columns at right.

E N O R AMINING DIV.

3 9? Total number of mining claims covered by this report of work.

Oat Recorded t (Signature)

rtification Verifying Repcffof Workl hereby certify that l have a personal and intimate knowledge of the fact* let forth in the Report of Work annexed hereto, having performed the work Of w itnessed same during and/or after in completion and the annexed report li true.

Nema and Poitel Addreu of Penon Certifying

h 4to Si, E^ USC.tlf led (Signature)

Ministry ofNorthern Development

Ontario"W Technical Assessment

Work CreditsDate

August 15. 1988

File 2.11369

Mining Recorder'1 Report of Work W W880 1-168

Recorded Holder

Gandy Resources CorporationXJWWOXKXr Area

Rickaby and Eagle Lake

Type of survey and number of Assessment days credit per claim

Geophysical 40

Electromagnetic Ha ys

Magnetometer days

Induced polarization days

Other day*

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

Geological rfays

Geofihpmir.fll Hays

Man days | | Airborne [~l

Special provision [x] Ground 0

l | Credits have been reduced because of partial coverage of claims.

f"! Credits have been reduced because of corrections to work dates and figures of applicant.

Mining Claims Assessed

K 951398 to 400 inclusive 951451 to 58 inclusive 951476 to 81 inclusive 951492 to 95 inclusive 951498 to 501 inclusive 951972 to 85 inclusive 951987 to 99 inclusive 952000 to 006 inclusive 952011 to 15 inclusive 952017 to 27 inclusive 952029 to 33 inclusive 952050 to 67 inclusive 952069

Special credits under section 77 (16) for the following mining ci aim t

10 days 20 days

K 951986 K 951496952007952016

30 days

K 951497952010952028952068

No credits have been allowed for the following mining claims

not sufficiently covered by the survey

K-951970-71

insufficient technical data filed

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.

Ministry ofNorthern Development

Technical Assessment Work Credits

OntarioDate

August 15. 1988

File

2.11369Mining Recorder's Report of Work No.

W8801-168

Recorded Holder

TWWOMWXvt Area

Gandy Resources Corporation

Rickaby and Eagle Lake

Type of survey and number of Assessment days credit per claim

Geophysical

Pleetromagnetir

Magnetometer

RfldjOTV?trir

Induced polarization

Othpr

Section 77 (19) See"

Geological

Geocheminal

Man days j |

Special provision Q{j

ria y s

20days

rlaye

day?

days

Mining Claims Assessed" column

Hays

riays

Airborne (~1

Ground [jfj

1 l Credits have been reduced because of partial coverage of claims.

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

Mining Claims Assessed

K 951398 951451 951476 951492 951498 951970 951987 952000 952011 952017952029 952050 952069

to to to to to to to to to toto to

400 inclusive 58 inclusive 81 inclusive 95 inclusive 501 inclusive 85 inclusive 99 inclusive 007 inclusive 15 inclusive 27 inclusive33 inclusive 67 inclusive

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

}O 38 days

K 951496 952016

days

K 951497 951986 952010 952028 952068

No credits have been allowed for the following mining claims

l l not sufficiently covered by the survey Q insufficient technical data filed

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)

C l

^o^U. UL* CLr^ 0^s

DOCUMENT No.

W8801- /^^

Kqs\

452

^80

^51 4:80

HSiooo

'^ AS2.0 M

•' ^5202.1

* ^52022.

OS2

August 31, 1988 Your Filei Our File i

W8801-168 2.11369

Mining RecorderMinistry of Northern Development and Mines808 Robertson StreetBox 5200Kenora, OntarioP9N 3X9

Dear Sirt

ONTARIO GEOLOGICAL SURVEYASSESSMENT FILES

l OFFICE

;,' SFP T 3 1988

RE c e iv E DRE: Notice of Intent dated August 15, 1988

Electromagnetic and Magnetometer Survey submitted on Mining Claims K 951398 et al in the Areas of Eagle and Rickaby Lake.

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 claims and so indicate on your records.

Yours sincerely,

W.R. Cowan, Manager Mining Lands Section Mines (t Minerals Division

Whitney Block, Room 6610Queen's ParkToronto, OntarioM7A 1W3Telephones (416) 965-4888

AB: se

cc: Gandy Resources Corporation cox Suite 50067 Richmond Street W. Toronto, Ontario M5H 1Z5

ccs Mr. G.H. Ferguson oci Mining fi Lands Ccranissioner Toronto, Ontario

Mr. R.W. Woolhara Suite 41020 Richmond Street E. Toronto, Ontario M5C 2R9

Resident Geologist Kenora, Ontario

950 00'

500 45 —.

50 0 37'30"

WOODLAND

—500 45

59 57'55 53'

52 5149' 48' 47 1 46'

52L10NW0003 2.11369 EAGLE LAKE

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200

500 37'30"

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LEGEND

HIGHWAY AND ROUTE No.

OTHER ROADS

TRAILS

SURVEYED LINES;TOWNSHIPS. BASE LINES. ETC.LOTS, MINING CLAIMS, PARCELS. ETC

UNSURVEYED LINESLOT LINESPARCEL BOUNDARYMINING CLAIMS ETC.

RAILWAY AND RIGHT OF WAY

UTILITY LINES

NON-PERENNIAL STREAM

FLOODING OR FLOODING RIGHTS

SUBDIVISION OR COMPOSITE PLAN

RESERVATIONS

ORIGINAL SHORELINE

MARSH OR MUSKEG

MINES

TRAVERSE MONUMENT

DISPOSITION OF CROWN LANDS

TYPE OF DOCUMENT SYMBOL

PATENT, SURFACE 8t MINING RIGHTS......—.. .....— 0

.SURFACE RIGHTSONLY....^.-...-......-m ©

. MINING RIGHTS ONLY ^....................^ O

LEASE, SURFACE St M INING RIGHTS-. —.—.......—. H

" .SURFACE RIGHTS ONLY._...,......-.....-m H

" .MINING RIGHTS ONLY........................... Q

LICENCE OF OCCUPATION .._......................... T

ORDER-IN-COUNCIL ......._.........,................. OCRESERVATION ___......__.........,——........,..—. (J)

CANCELLED ___......,__———^..-............L... ®

SAND S. GRAVEL __......_.........._......™...... ©

NOTE: M INING RIGHTS IN PARCELS PATENTED PRIOR TO MAY 6. 1913, VESTED IN ORIGINAL PATENTEE BY THE PUBLIC LANDS ACT. H.S.O. 197O. CHAP 380. S EC. 63, S UBSEC 1.

REFE R ENCESAREAS WITHDRAWN FROM DISPOSITION

M.R.O. -MINING RIGHTS ONLY

S.R.O. -SURFACE RIGHTS ONLY

M.-f S. - MINING AND SURFACE RIGHTS

Description Order No. Date Disposition File•"~"~~~V; -NORA: ! . rs,;J3 D IV.

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Ministry ofNaturalResources

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ORPHS BY.- i.L-B

N.T.5-

WLID/tl

DOTE JUNE 20. 193s

DMC- NO-

88-62-04

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sou

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INSTRUMENT: APEX MAXMIN

IN-PHASE VALUES SHOWN ON WEST SIDE OF LINE. IN-PHASE PLOT SHOWN AS SOLID LINE.

QUADRATURE VALUES SHOWN ON EAST SIDE OF LINE. QUADRATURE PLOT SHOWN AS DASHED LINE

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GRNDY RESOURCES CORP .BEE LflKE PROJECT

EHGLE LflKE flREfl

MnXMIN SURVEY 444 HZ

.EflST GRID SECTION

PROFILE SCRLE 10X PER CM

COIL SEPnRflTION 150 METERS

DERRY, MICHENER, BOOTH t W flHL

FlLEr

LCRC^PE-PLT

LCRC4-ttt-PLT

B&RW'Mt-PLT

DRRHN BY^ 'j L- B

N-T-0-

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DHG-'W-'

88-62-06

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14Q,O

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ffiINSTRUMENT: APEX MAXMIN

IN-PHASE VALUES SHOWN ON WEST SIDE OF LINE. IN-PHASE PLOT SHOWN AS SOLID LINE.

QUADRATURE VALUES SHOWN ON EAST SIDE OF LINE QUADRATURE PLOT SHOWN AS DASHED LINE.

Mf ESS/0,,

50 Q SG 10C ISO

St RLE l-'iCGD2. 1 1369sour

H GflNDY RESOURCES CORP .BEE LflKE PROJECTEflGEE LflKE flREfl

MRXMIN SURVEY 1777 HZ

ERST GRID SECTION

PROFILE SCflLE 107, PER CM

COIL SEPflRflTION 150 METERS

DERRY, MICHENER, BOOTH 4 WRHL

F:LE-LGR:77Pc-PLT

LCRC777^.PLT

BCRC777E-PLT

DRfiHN BY- 'j L- B

N-T.-i.WLio/i:

DRTE JUNH ?U. ;088'

'DHC NO-,

88-62-08

rpt on geoph sur bee l prop€¦ · south of bee lake. it connects gordon lake, ontario, site of...

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