dave saunders 2 - ontario · dave saunders 2.28406 ... saunders, david bruce (e30095) saunders,...

Pierre SimoncaiiConsulting-Experts in Geophysics

DAVE SAUNDERS2.28406

Electromagnetic VLF and Magnetometric surveyson

Lumby Lake Property

Norway Lake AreaThunder Mining Division

Ontario

REPORT

RECEIVEDSEP 1 O

-OSCIENCE ASSESSMENT OFFICE——

August 10 2004 Pierre Simoneau , geol. M.Se.

52G03SW2012 2.28406 NORWAY LAKE 010

TABLE OF CONTENTS

PAGE

1. INTRODUCTION............................................................................................................................ l

2. PROPRETY, LOCATION AND ACCESS ...................................................................................... l

3. PROPERTY OWNERSHIP AND CLAIMS .................................................................................... 2

4. PERSONAL AND INSTRUMENTATION ..................................................................................... 2

5. FIELD WORK AND PROCEDURE................................................................................................ 3

6. MAGNETOMETRIC SURVEY ..................................................................................................... 3

6.1 Process of data and work....................................................................................................... 3

6.2 Presentation of the results...................................................................................................... 3

7. ELECTROMAGNETIC VLF SURVEY ........................................................................................ 4

7.1 Process of data and work....................................................................................................... 4

7.2 Presentaqtion of the results.................................................................................................... 4

8. DISCUSSION OF THE RESULTS AND RECOMMANDATIONS.............................................. 4

9. CONCLUSION................................................................................................................................^

- Certificate of Qualifications

- Appendix A Claim Map and Abstract

- Appendix B Equipment Specifications

1. INTRODUCTION

At the request of Mr. Dave Saunders, prospector, Electromagnatic VLF and Magnetometric surveys were run on June 13, 2004 over a mineralized zone on the Lumby Lake Property. The VLF and Mag surveys were carried out by Pierre Simoneau.

2. PROPERTY, LOCATION AND ACCESS

The Lumby Lake Property is located approximately 180 km northwest of Thunder Bay or about 30 km north of Sapawe, Ontario, Thunder Bay Mining Division. Access to the property is afforded by a gravel road situated l km west of the grid and a winter road going east to Lumby Lake.

2. 28406

umoke English River

LacMilles Lac

Kashabowie40 60 80 kmi i . . ...Shafoa'tniia

l) Greenwater Lake

KakabekaU Falls

Figure 1. Location of the Lumby Lake Property.

- 7 -

3. PROPERTY OWNERSHIP AND CLAIMS

The property is comprised of 6 claim blocks and 3 claims ( figure 2 ). Dave Saunders is the recorded holder for the claims.

The I.P. survey covered 3 claims : claims # 1233453, 1233454 and 1233455

The 3 claim blocks ( 1232003 - 1232004 - 1232005 ) worth 11 units.

Figure 2. Claim Map.

4. PERSONAL AND INSTRUMENTATION

The Electromagnetic ( VLF ) and Magnetometer surveys were carried out by Pierre Simoneau, geol. M.Se.

GSM-19WMV GSM-19 senseur

Terraplus (Richmond Hill) n/s 632856 Terraplus (Richmond Hill) n/s 6111067

- Dave Saunders , line cutter.

-3-

The report was written by Pierre Simoneau.

The maps were finalized by Pierre Simoneau.

5. FIELD WORK AND PROCEDURE

The grid was cut at the same time than the surveys. The grid extends in a E-W direction with N-S lines from 1+00 W to 12+OOW, with 100 metres between each lines and about 300m long each lines. A base line intersects the grid at 0+00.

The Mag-VLF. survey covered a total of 3.5 km. Mag stations were read every 6.25m. Detail readings were taken because of important variations of the magnetic field in narrow zones that were notice between two adjacent stations.

6. MAGNETOMETRIC SURVEY

6.1 Process of data and work

The measurements for the magnetic total field were taken in a walking mag mode with a two (2) seconds sampling readings and label readings taken each 6.25 meters.

The magnetic readings have been corrected for diurnal variations in a loop mode using the readings on the old lines. The magnetometer system measures the value of the total magnetic field with a precision of 2.0 gammas.

A description of the instruments is given in Appendix B.

6.2 Presentation of the results

Geophysical data was processed and presented on maps using the computer software programs; Geosoft and Microstation.

The magnetic results are presented on a profile map ( no. 6500 ) and a total field contour map (no. 6501 ) at the metric scale of l : 2 500.

The property magnetic background is around 58 300 gammas with a maximum of 59 586 gammas and a minimum of 58 063 gammas. The magnetic field is very active in the property confirming the presence of pyrrhotite zones mainly around the known showings in the western part of the grid.

-4-

7. ELECTROMAGNETIC VLF SURVEY

7.1 Process of data and work

A GSM-19WMV was used on the field. The readings were taken at 6.25 meters spacing. The VLF survey was made with two main stations - Cutler (NAA, 24,0 kHz) station and Jim Creek-Seattle (NLK, 24,8 kHz).

7.2 Presentation of the results

The results are presented on profiles map No. 6502 for Cutler and No. 6503 for Jim Creek, at the metric scale of l: 2,500.

The VLF interpretation was drawn on the maps.

The VLF survey detected one (1) anomaly that crosscut the magnetic trend. It could be a topographic feature or a shear zone carrying nonmagnetic mineralization or conductive fluids. The VLF anomaly will be numbered EM-8, in continuation of the previous survey.

8. DISCUSSION OF THE RESULTS AND RECOMMANDATIONS

The geophysical campain gave detailed information about the mineralized zone previously identified on the property.

The high magnetic anomalies correspond to the known mineralized zones that are aroung line 12+00W and are crossing most of the lines. No VLF anomalies are follwing the magnetic trend. Instead, the VLF anomaly is cutting across the main magnetic anomaly. It could be a shear zone with or without mineralization. More work should be done by making trenches and sampling.

9. CONCLUSION

The geophysical campain gave interesting information about this property.

The previous work in the south part of the property showed that the mag and VLF anomalies were following closely the IP anomalies. We had a mix of Copper-zinc- pyrrhotite and pyrite.

Now, we have only the magnetic anomalies that are following the regular direction. The only VLF anomaly goes in a complete different anomaly. The magnetic anomalies could be indicators of zinc zones with low content of other sulphides like pyrrhotite-pyrite and chalcopyrite. Too disseminated to react with the VLF sensor.

-5-

CERTIFICATE of QUALIFICATIONS

I, Pierre Simoneau of 396 Brant Street, Thunder Bay, Ontario, hereby certify:

1. I am a graduate of University of Quebec at Chicoutimi (1987) with a Master degree in Earth Sciences M.Se.

2. I am presently employed as a project geophysicist and geologist with GEOSIG Inc. of 3700 Chaudiere Blvd., Sainte-Foy, Quebec.

3. I have been employed as an exploration geologist and geophysicist on a full time basis since 1987, prior to that as a geological assistant for four field seasons.

4. I am a member of the OGQ (Order of Geologists of Quebec) and I am a member of the CIM.

5. The information contained in this report was obtained from geophysical survey conducted on the Lumby Lake property carried out by Geosig Inc.

6. I own no direct, indirect or expect to receive any contingent interests in the subject property.

Pierre Simoneau, M.Se. geol.v S J \ '

Dated at Thunder Bay, Ontario, this 10th day of August, 2004

Appendix A

Claim Map and Abstract

2.28406

ONTARIOCANADA

Mining Land Tenur* Map

f'1T'J](DT2004

TOWNSHIP l AREA NORWAY LAKE AREA

PLAN O-OM5

ADMINISTRATIVE DISTRICTS l DIVISIONS

Mirflnj Cfvik" Thuntm Buy Ljnd TliKb^totiuy Dillon KENORA Mintavy cd Hmlurtl HHOUIEH DiUila FOfll FRANCES

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TOWNSHIP; AREA Claim Number Recording Date Claim Due Date Status Percent Work Totai Total Claim Option Required Applied Reserve Bank

NORWAY LAKE TB 1232004 1998-APR-21 2005-APR-21 A 100.00 07o 2373 12027 28 O

NORWAY LAKE TB 1232005 1998-MAY-15 2005-MAY-15 A IQO.00% 800 4000 O O

NORWAY LAKE TB 1233453 2001-JUN-15 2004-SEP-13 A 100.00 07o 400 400 70 O

NORWAY LAKE TB 1233454 2001-JUN-15 2004-SEP-13 A 100.00 "/o 400 400 O O

NORWAY LAKE TB 1233455 2001-JUN-15 2004-SEP-13 A 100.00 "/o 400 400 O O

Mining Lands - Mining Claims Abstract Summary Page l de l

Mining Lands - Mining Claims Summary

Thunder Bay - Division 40

CLAIM NUMBER:Unit Size:Township/Area:Lot Description:Staker:Recorded Holder:Recording Date:Due Date:Work Required:Total Applied:Work Performed:Total Reserve:Present Work Assignment:Claim Bank:Claim Status:

TB 1233453 (Click Claim Number for Details)

l

NORWAY LAKE (G-0545)\r\nSAUNDERS, DAVID BRUCE (E30095)SAUNDERS, DAVID BRUCE ( 100.00 !fe)2001-Jun-152004-SEP-1340040047070 (Click Reserve for Details)

OoACTIVE

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Copyright 2001 Queen's Printer for Ontario

This information is provided as a public service, but we cannot guarantee that the information is current or accurate. Readersshould verify the information before acting on it.

http://www.mci.mndm.gov.on.ca/Claims/CfClaims/elm csr4.CFM 04-09-07





TB 1233454 (Click Claim Number for Details) f" '"""""" ""

NORWAY LAKE (G-0545)\r\nSAUNDERS, DAVID BRUCE (E30095)SAUNDERS, DAVID BRUCE l 100.00 t*,)2001-Jun-152004-SEP-134004001404O (Click Reserve for Details)

1004OACTIVE

l Back l Main Menu J Mining Lands |

O Copyright 2001 Queen's Printer for Ontario


http://www.mci.mndm.gov.on.ca/Claims/Cf Claims/elm csr4.CFM 04-09-07





TB 1233455 (Click Claim Number for Details)

TNORWAY LAKE (G-0545)\r\nSAUNDERS, DAVID BRUCE (E30095)SAUNDERS, DAVID BRUCE ( 100^00 %J2001-Jun-152004-SEP-13400400939O (Click Reserve for Details)

539OACTIVE

l Back l Main.Menu.j Mining Lands |







CLAIM NUMBER: TB 1232004 (Click claim Number for Details)

Unit Size: 6TownshipXArea: NORWAY LAKE (G-0545)Lot Description:Staker: SAUNDERS, DAVID BRUCE (E30095)

Recorded Holder: SAUNDERS, DAVID BRUCE 0,00 . 00 Jfc)

Recording Date: 1998-Apr-21Due Date: 2005-APR-21Work Required: 2373Total Applied: 12027Work Performed: 14812Total Reserve: 28 (Click Reserve for Details)

Present Work Assignment: OClaim Bank: OClaim Status: ACTIVE

l Back l Main Menu | Mining Lands |







CLAIM NUMBER:Unit Size:Township/Area:Lot Description:Staker:Recorded Holder:Recording Date:Due Date:Work Required:Total Applied:Work Performed:Total Reserve:Present Work Assignment: OClaim Bank: OClaim Status: ACTIVE

TB 12320052NORWAY LAKE (G-0545)

(Click Claim Number for Details)

SAUNDERS, DAVID BRUCE (E30095) SAUNDERS, DAVID BRUCE ( 100.001998-May-152005-MAY-158004000OO (Click Reserve for Details)

2.284 06

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Appendix B

Equipement Specifications

magnetometer, GSM-19 filer/y/Cr/Geosig/Gem/gsm-19.htm

GSM-19Overhauser

Magnetometer l VLF

GSM-19 o verb a use r magnetometer Features ignetometer

Sensitivity - 0.02 nT Absolute Accuracy - 0.2 nT Sample Rates up to 5 Hz Low Power Consumption

General magneton ription

"Overhauser" Once you experience it, you'll never go back to proton. Overhauser technology brings you sensitivities one to two orders of magnitude better than proton, yet in a light weight package. This is because the Overhauser magnetometer consumes less power than proton magnetometer, allowing a lighter weight for batteries.

What is the Overhauser technique? The Overhauser sensor contains the electrons' fluid that has been added to a hydrogen rich in the form of "free radial". The resulting mixture yields a sensor with 5000 times gain in proton polarization. Since the Overhauser polarization effect does not require static magnetic fields, but uses radio frequency fields transparent to protons, measurement can be done concurrently with polarization. The result is a sensor with much greater sensitivity, that can be sampled much more rapidly than the standard proton sensor.

Overhauser magnetometer systems therefore maximize resolution while minimizing power consumption. Even with Walking Gradiometer systems, sampling at rates of once per second; Even in cold temperatures of - 40 zero degrees Celsius and greater, the internal rechargeable battery can still be relied on for a 10 hour day, or longer.

The GSM-19 Overhauser is a State-of-the-Art Magnetometer l VLF system and offers the data quality, reliability, and extensive list of capabilities, and options, that allow it to meet a very wide spectrum of applications.

Instrument Description

"Physical Overview"

The parts of the GSm-19 magnetometer/gradiometer are as follows :

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magnetometer, GSM-19 filer/y/Cr/Geosig/Gem/gsm-19.htm

The sensor is a dual coil type designed to reduce noise and improve gradient tolerance. The coils are elec trostatically shielded and contain a proton rich liquid in a pyrex bottle, which also acts as an RF resonator.

The sensor cable is coaxial, typically RG-58/U, up to 100m long.

The staff is made of strong aluminium tubing sections (plastic staff optional). This construction allows for a selection of sensor elevations above ground during surveys. For best precision the full staff length should be used. Recommended sensor separation in gradiometer mode is one staff section (56cm from sensor axis to sensor axis), although two or more sections are sometimes used for maximum sensivity.

The console contains all the electronic circuitry. It has a 16 keys keyboard, a 4 x 20 character alphanumeric display, and sensor and power/input/output connectors. The keyboard also serves as an ON-OFF switch.

The power/input/output connector also serves as RS232C input/output and optionally as analog output and/or contact closure triggering input.

The keyboard, front panel, and connectors are sealed i.e. the instrument can operate under rainy conditions.

The charger has 2 levels of charging, full and trickle, switching automatically from ont to another. Input is normally 110V 50/60HZ. Optionally, 12 VDC input can be provided.

The all-metal housing of the console guarantees excellent EMI protection.

"Software Version 4.0"

There are several major versions of software for the GSM-19. As of August 92, GEM Systems added a major software upgrade to its GSM-19 family, enhancing its capabilities. This new generation of software (version 4.0) has the following advantages:

Diurnal correction (reduction) with interpolation can be used in conjunction with other GSM-19 models with software version 4.0 (or special software for correction with an EDA Mag Base station). This allows the base mag to run with longer cycle time Previous software could do interpolation only with fast GSM-19 types.

Memory filing system. Now 50 files can be stored in a directory, and mode of operation can be changed without erasing memory. With the software previous to version 4.0, only 1 file could be retained in memory, and this would be lost when modes of operation were switched.

Line and station numbers have been enlarged. Lines can now be 5 digits as opposed to 4 digits in previous software. Station numbers are now 7 digits as opposed to 6 in the previous software.

Standard Features of the magnetometer

The GSM-19 magnetometer console features a real time graphic display of the current profile. In addition digital display of the current reading, current position, and warning messages are provided. The console design, with internal rechargeable battery pack, allows the unit to be completely sealed against the elements. With the built in heater for the display the GSM-19 magnetometer is ready to go wherever your surveys may take you.

Tuning is automatic worldwide, with provision for manual override. In high gradient conditions the GSM-19 magnetometer monitors the signal decay rate and displays a warning message when the gradient becomes too great. Filters for rejection of 50 or 60 Hz noise are provided.

Diurnal connections may be done in traditional fashion with one magnetometer unit as a base station and a second unit used as the mobile field unit. At the end of the survey the two units are connected and the field unit creates a corrected data file (which still includes the raw data file) based on the temporal drift recorded by the base station.

As a standard feature GSM-19 magnetometer also offer the capability of making tie point measurements for automatic diurnal corrections. To use this feature the operator records a base value and then loops back to this point periodically during the survey to record another measurement, and thus build a file of the drift. In this way a single instrument may be used to make diurnal corrections.

The RS-232 port on the GSM-19 magnetometer will output data as rt is collected. This allows interface to GPS

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magnetometer, GSM-19 file:WC:7Geosig7Gem7gsm-19.htm

loggers that will accept RS232 data. The standard GSM-19 magnetometer may be operated in a remote mode via computer. Memory storage is 512 K in the standard unit, and may be upgraded to 2 MB.

Grid coordinates are stored with either numeric or compass designations. A seven digit number may be used to designate lines and positions. Line and position spacing is entered so that with every reading the position may be automatically updated. An End of Line feature allows the next line to be quickly selected, plus changes the sign on the position spacing. If the previous line had been adding positions as the operator moved, then on the next line, positions will be subtracted as the operator moves. The operator may also easily manually enter his grid position for cases where gaps in the line are necessary.

"Walking Mag Option"

The GSM-19 magnetometer is the first to offer the "Walking Mag" concept. The reason for this is the outstanding advantage the Overhauser sensor has in this application. With the "Walking Mag" option the operator may select a sample rate of up to two samples per second. At this rate Overhauser technology can still deliver a noise level that is quite acceptable, about 0.1 nT, and the lower power consumption means that a full day of surveying can still be done with just the internal rechargeable battery.

As shown in Figure 1 the near continuous data from the "Walking Mag" technique provides increased definition for any type of survey. For surveys with densely spaced grids, such as archaeological or environmental surveys, field productivity is markedly improved, typically by a factor of five.

When in the Walking Mag mode the operator still presets his line and station spacing. When a known station is passed a grid update key is pressed and the current reading is tagged with this station. Readings taken between these marked positions are then linearly interpolated for their grid position when data is transferred to a computer.

A further refinement of the Walking Mag concept is the Hip Chain Option. This option uses a hip chain to trigger the magnetometer to take a reading at discrete intervals. A Hip Chain consists of an optical encoder that records revolutions of a wheel wound with disposable cotton string. The string is tied off at the beginning of a line, and as the operator walks the string is pulled out, and the magnetometer is automatically triggered. With the Hip Chain option sample rates up to five samples per second are supported.

Omnidirectional VLF

The GSM-19 VLF features a three coil design, with new larger coils in 1997, to achieve a non orientation capability with excellent sensitivity. Up to three VLF stations may be recorded, along with the magnetic reading, with the pressing of a single key.

As each VLF station is read the total field strength is displayed. This value may be used to determine if a station's signal is strong enough to obtain useful data. At the end of each reading the in phase, out of phase, and horizontal components are displayed and recorded for each station.

To determine what stations are available the Scan feature may be used. The entire VLF spectrum is scanned and stations with their corresponding signal strength are displayed. Automatic tilt compensation is provided up to ten degrees. Beyond this a warning message appears with display of the amount of tilt in each direction, enabling the operator to correct his position and take the reading again.

For Walking Mag applications a Walking VLF option is also available. With this option a single VLF station may be measured at sampling rates up to once per second. In this mode both magnetic and VLF readings may be collected at the one hertz rate.

Simultaneous Gradiometer

Many mining, environmental, and archaeological applications may benefit from using the gradient measurement. For near surface anomalies, generally twenty meters depth or less, the gradient anomaly will be larger, and narrower, than the total field anomaly. This permits the more accurate location of the target, and gives better sensitivity. The gradient measurement has the added value of being free from diurnal drift.

The most accurate gradient measurements are made when both sensors are polarized and measured at precisely the same time. In this way any slight movement of the sensor staff pole will not affect the reading. With the GSM-19

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Gradiometer Option the pressing of a single key will initiate measurement of both the total field and gradient. Both readings are displayed and stored.

Specifications

Overhauser Performance

Resolution: 0.01 nTRelative Sensitivity 0.02 nTAbsolute Accuracy: 0.2nTRange: 20,000 to 120,000 nTGradient Tolerance: Over 10.OOOnT/mOperating Temperature: -40"C to *600 C

Input l Output: 6 pin weatherproof connector, RS-232C, and (optional) analog output

Power Requirements: 12V, 200 mA peak (during polarization), 30 mA stanby. 300mA peak in gradiometer mode.

Power Source: Internal 12V, 1.9 Ah sealed lead-acid battery standard, others optional. An External 12V power source can also be used.

Battery Charger Input: 110/220 VAC, 50/60 Hz and / or 12 VDC (optional). Output: 12V dual level charging.

Operation Modes

Manual: Coordinates, time, date and reading stored automatically at min. 3 second interval.Base Station: Time, date and reading stored at 3 to 60 second intervals.Walking Mag: Time, date and reading stored at coordinates of fiducial.Remote Control: Optional remote control using RS-232 interface.Input/Output: RS-232 or analog (optional) output using 6-pin weatherproof connector.

Operating Parameters

Power Consumption: Only 2Ws per reading. Operates continuously for 45 hours on standby.

Power Source: 12V 2.6Ah sealed lead acid battery standard, other batteries available

Operating Temperature: -500 C to +60°C

Storage Capacity

Manual Operation: 29,000 readings standard, with up to 116,000 optional. With 3 VLF stations: 12,000 standard and up to 48,000 optional.

Base Station: 105,000 readings standard, with up to 419,000 optional (88 hours or 14 days uninterrupted operation with 3 sec. intervals)

Gradiometer: 25,000 readings standard, with up to 100,000 optional. With 3 VLF stations: 12,000, with up to 45,000 optional.

Omnidirectional VLF

Performance Parameters: Resolution Q.5% and range to ±20007o of total field. Frequency 15-30 kHz

Measured Parameters: Vertical in-phase 8n out-of-phase, 2 horizontal components, total field coordinates, date, and time.

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magnetometer, GSM-19 filerWCVGeosig/Gem/gsm-19.htm

Features: Up to 3 stations measured automatically, in-field data review, displays station field strength continuously, and tilt correction for up to ±10" tilts.

Dimensions and Weights: 93 x 143 x 150mm and weighs only 1 .Okg.

Dimensions and Weights

Console: 223 x 69 x 240mmSensor: 170 x 71mm diameter cylinderSensor staff: 4 x 450mm sections.Weight: Console: 2.1kg Sensor and Staff Assembly: 2.0kg

Terraplus Canada, 52 West Beaver Creek Rd., Richmond Hill, Ontario, Canada L4B1L9Tel (905) 764-5505 Fax (905) 764-8093

2.284 06

5sur5 11/08/2004 1:27 AM

ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No: Recording Date: Approval Date:

Client(s):

191663

Survey Type(s):

W0440.01414

2004-SEP-10

2004-SEP-13

Work Report Summary

Status: APPROVED

Work Done from: 2004-MAR-25

to: 2004-JUN-13

SAUNDERS, DAVID BRUCE

LC MAG VLF

Work Report Details:

Claim* Perform

TB 1233453 31,284

TB 1233454 31,665

TB 1233455 S1.665

S4.614

External Credits:

Reserve:

Perform Approve Applied

31,284 S800

31,665 S800

51,665 S800

S4.614 32,400

SO

32,214 Reserve of Work

32,214 Total Remaining

Applied Approve

3800

3800

3800

32,400

Assign

soSO

soso

Assign Approve Reserve

0 S484

0 S865

0 S865

30 32,214

Reserve Approve Due Date

S484 2006-JUN-15

3865 2006-JUN-15

3865 2006- J UN- 15

32,214

Report*: W0440.01414

Status of claim is based on information currently on record.

52G03SW2012 2.28406 NORWAY LAKE

2004-Oct-08 10:22 PRUDHOMMEI

900

Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2004-SEP-13

Ministere du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E 6B5

DAVID BRUCE SAUNDERS 962 EASTERBROOK AVE. BURLINGTON, ONTARIO P7E1K7 CANADA

Tel: (888) 415-9845 Fax:(877)670-1555

Dear Sir or Madam

Submission Number: 2.28406 Transaction Number(s): W0440.01414

Subject: Approval of Assessment Work

We have approved your Assessment Work Submission with the above noted Transaction Number(s). The attached Work Report Summary indicates the results of the approval.

At the discretion of the Ministry, the assessment work performed on the mining lands noted in this work report may be subject to inspection and/or investigation at any time.

If you have any question regarding this correspondence, please contact BRUCE GATES by email at [email protected] or by phone at (705) 670-5856.

Yours Sincerely,

/P,Ron C. GashinskiSenior Manager, Mining Lands Section

Gc: Resident Geologist

David Bruce Saunders (Claim Holder)

Assessment File Library

David Bruce Saunders (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:19816

ONTARIOCANADA

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58203581995819458191581965820858182

68241582995831758264 l582Q8f58213^663065845058412SW145838756337

98329S33185626358230562505839158566585475664256552 -t-5851658566585395840058504583785859558779 58667 58557

58244 58227 58218 58233 5823658245582555824758270582885840258287 /l582405823858246582255822958206

58224 58247 58235 58279 58201 58289 58282 58285 S8340 58259

582245821258217582195821758213582235623558212

582S7 58270 58269 58249 58256 58242 58254 58218 58208 58216 58223 58297 58444

64f 5B212\- 58273 58264 58259 58244 98291 58327 58419 58363 58514 59073

56230582225B2375822458217883225821458251S8217 j5822158212582265624458200581955817758238582255823758231S81975826358297582095821058231563595826058327

5632758304583105826258221582091582545848159576 58359

56334 56313 58301 58284 56271 58255 58261 58265 S6246 58251

58256 58244 58243 58184 S8204 58211 58254

58212582875828658333563465832458186/5812SL56320

58414583105B2BB58284582645K4358348584145816658259

58513584435835458324

58222 58219 58243 S8262 58265

58256582565826358222

5833 S83H S82S6 58260 58J15 58282 58207 58J27 58201 58253S6284 58290 682615630458315

MAG-10

-ir----ea

x—x

MAG-5

Geophysica Legend

-1000 -500

58550 TOTAL FIELD

•f 500 * 1000

Strong IP anomaly ( 0.9 > P > 0.7 )

Medium IP anomaly ( 0.7 > P > 0.4 )

Poorly defined IP anomaly( 0.4 > P > 0.2 )

IP Axis

- VLF anomaly axis

—x—x—x—x—Magnetic anomaly axis

Source of map: Federal topographic map 52 G 03The coordonote eyttem St in Universe! Troneverte Mercator ( UTM ) arid, N.A.D. 2.7, Zone 15.

The approximate mion declination It 0*04' East In 2000. The annual change decreasing 3.5'.

Location

;jjmby Lake

D ropertyEnglish River

Lac des\ Raith.Milles Lac

ashabowiehebandowan

MAGNETOMETRICMAP

Profiles and postingsPROJECT

Lumty Lake ProjectFOR :

ersBY: Pierre SimoneauPROJECT Lumby Lake

AREA

DISTRICT

N.T.S.

SCALE 1 : 2500

Norway Lake

Thunder Bay, Ontario

52 G 03—-——

D 25 50 75 100m.

Executed byPierre Simoneou, geol.

Geomatic by Pierre Simoneou

Interpreted byPierre Simoneau

Map no 6500Project no —.——.—

DATE

07-04

08-04 08-04

52G03SW2012 2.28406 NORWAY LAKE 210

•ii:

58527585045848258464584495843858425584135840258394583845837558365583585835058341583325832658318583095830158293582865827858269582605825358244582345822558216582055819458181581705815458137581155809258051

MAG-14

__Y__vA A

X——~

EM-8

Geophysico Legend


Medium IP anomaly ( 0.7 > P > 0.4 )

Poorly defined IP anomaly ( 0.4 > P > 0.2 )

IP Axis

VLF anomaly axis

—x—-x—x—x—Magnetic anomaly axis

Source of map: Federal topographic map 52 G 03The coordonate tyttem li In Unlvertal Trontverte Msrcotor ( UTM ) grid, N.A.D. 27, Zont \S.

The approximate maon decVnotion \t 0*04' Eojt In 2000. The annual change decreasing 3.5'.

Location

,

Lumby Lake

PropertyEnglish River

,, , . .Milles Lac Kashabowie

60 8.0 km

Greenwater Lake

Kakabeka Falls

MAP

MAGNETOMETRIC SURVEY284

Colored Total Field ContoursPROJECT

Lumby Lake ProjectFOR :

ersBY: Pierre SimoneauPROJECT Lumby Lake

AREA

DISTRICT

N.T.S.

SCALE 1 : 2500

Norway Lake


52 G 03————

O 25 50 75 100m.

Executed by Pierre Simoneou, geol.

Geomatic by Pierre Simoneau

DATE

07-04

08-04Interpreted by Pierre Simoneou 08-04

Map no Project no

6501

52G03SW2012 2.28406 NORWAY LAKE 220

i;

3.78.8 3.27.8 1.09.5 1.7

10.0 2.511.512.3

0.5 1,6

14.8 2.714.5 3.714.8tt.515.3 18.3 16.8 3.0 16.1 2.0 14.8 0.3 15.3 -0.3 14.5 -2.5 ( 14.1 -1.318.2 -0.218.3 1.117.7 -0.217.7 0.019.119.521.021,823.120,021,821.820.81t,220.719.721.123.223.S25.125.1 10.030.2 12.532.0 12.831.0 12.0

-0.2 8.0-O.i 8.5 0.6 8.1 4.8 9-3 6.3 9.8 4,5 8.3 9.0 10.8

10.8 9.0 10.1 9.3 11.S - - 14.1 9.8

6.4 8.6 5.4

12.112.3

13.1 12.312.6 6.812.8 10.014.6 11.816.3 10.314.0 7.916.016.2 15.0 5.0

15.3 5.S 15.8 18.8

6.15.3

17.5 4.5 19.2 5.0 - - 21.? 6.3 \.6 22.3 8.3 4\8 235 9.0 4lB 28.8 10.3 4.1 27.7 10.8

37,2 11.5 38.2H.3 39.4 12.1 42,2 14.1

114.3

42,2 10.846.7 11.651.0 13.1

—x—x

MAG-5

m

Geophysica Legend

In Phase Out Phase

-50 -25 O +2S +50S5

In Phase Out PI-15.4-4.4.

In Phase

Out Phase

—— -^

Total Field

Total Reid

O 5 10 1555

Total Reid


3 Medium IP anomaly ( 0.7 > P > 0.4 )

3 Poorly defined IP anomaly ( 0.4 > P > 0.2 )

IP Axis

VLF anomaly axis

x—x—Magnetic anomaly axis

Source of map: Federal topographic map 52 G 03The coordanate system IB in Universal Transverse Mercator ( UTM ) grid, N.A.D. 27, Zone IS,

The approximate mien declination \t 0*04' East In HOOO. The annual change decreasing 3.5'.

Location

;.umby Lake


Lac des\ Raith- , , 'Milles Lac Kashabowie

hebanddilr/any

x) Greenwater Lake

Kakabek^ Falls

ELECTROMAGNETIC VLF SURVEY Jim Creek, Washington, 24,8 kHz

MAP

Profiles and posting;j

PROJECT

Lumty Lake ProjectFOR : DBY: Pierre SimoneauPROJECT Lumby Lake

AREA

DISTRICT

N.T.S.

SCALE 1 : 2500

Norway Lake


52 G 03

25 50 75 100m.

Executed by Pierre Simoneou, geol.DATE

________ 07-04Geomotic by Pierre Simoneou

_______ 08-04 Interpreted by Pierre Simoneou 08-04

Map no 6503 Project no —————

52G03SW2012 2.28406 NORWAY LAKE 230

a

-S7.8 14.8-33.8 14.1 -9.9 1

-9.7 1-8.7 1-6.7 16-4.2 16-3.5 17.2-3.3 13.1-3.0 14.3-0.9 13.8I.2 13.8 2.0 13.3

"0.8 12.1 4.3 13,8 3.5 12.S 4.0 14,1 8.5 11.8 6.6 12.8 7.9 11.5 8.3 12.1 8.6 11.6 9.6 11.1 8.6 10.6 9.8 10.5

II.1 12.0 12.1 12.1 13.3 12.1 14.8 10.6 13.6 12.6 16.3 12.6 16.6 12.1 17.0 13.3 19.3 13.8 19.0 12.5 18.7 11.8

i.7 13.0 22.0 13.6 20.2 12.1 18.5 12,6 20.7 10.5 19.7 11.8 20.3 11.5 19.5 12.1 19.7 10.5

16.0 14.6 15.3

!5.9\16.1-13.0 \B,7-9,7 1-6,9-6.5-3,0 19.-2.0 18.6 0.6 19.2 2.5 16.6 5.1 19.6 6.1 19.2 3.2 16.1

-10.7-13.9-15.7

10.S-8.7 1-7.2-3.0 15.-3.3-1.0 15.8 0.5 17,6 2.7 16.1 3.0 (5.3 6.9 16.2 9.1 13.8

10.1 14.1 11.3 14.5 11.5 13.8 12.8 14.1 16.3 15.8 20.5 17.7 18.3 14.

3.5 2.9 4.0

13.1 2.2 12,6 2.9 14.3 13,8 14,1 12,3 11.3 -2.3 15.1 -0.2 15.8 0.3 15.0 -1.3 15.0 0.8 17.720.220.321.524,323,724.124,323.122.2 10.326.2 9.022,019.820.221.723.023.226.6 10.330.6 10.528.3 10.0

-2.0 14-5.1 14-5.1 16-0.9 15 0.0 15,8 3.0 17.3

-2.0 13.0-9.2 11.8 1.3 11.5 3.4 11.6 M 13.3 J.6 13.3 li.6 14.0 1?,J 13.1 18.5 10.3

- 19.025.8 17.726.6 18.0 8.3 15.3

S*,8 14.8 24.2 H.3

14.324,8 14.1 ~ 25,3 13.8 - !22, JI.2 13.5 21. 28.2 14.5 317 15.8 t,8 17.0

14.5

10.1 8.311.3 7.812.3 7.814.5 10.614.6 8.516.3 9.31S.3 7.814.6 10.613.3 9.314.8 8.115.6 10.316.3 8.816.2 11.112.8 8.XJ

.5 13.3 28.7 12.1 2S.7 10.1

9.3 30.5 10.3 3219 11.5 35.7 12.3

f'.O 12.8.0 9.0

11.837.4 13.036.0 12.640.2 13.041.0 13.8

11.312.6 8.612,6 10.013.6 9.312.5 10.6

40.9 13.142.4 14.547.9 15.8

MAG-3 MAG-4

Geophysica Legend

In Phase Out Phase

-50 -25 O *25 4-5055

In Phase Out Phfise l!-15.4-t.4

In Phase

Out Phase

~——- --v

Total Field

5 20 35 505?

Total Reid


Medium P anomaly ( 0.7 > P > 0.4 )

Poorly defined IP anomaly ( 0.4 > P > 0.2 )

IP Axis

- VLF anomaly axis

—x—x—x—x—Magnetic anomaly axis

Source of map: Federal topographic map 52 G 03The coordonate eyetem h In Universal Transverie Mercator ( UTM ) grid, N.A.D. 27, Zone 15,

The approximate mean declination li 0*04' East In 2000. The annual change decreasing 3.5'.

Location

;.umby Lake


Lac des\ Raith'Milles Lac

ashabowiehebandd^ar

ff^y

T) Greenwater Lake

Kakabek^ Fails

ELECTROMAGNETIC VLF SURVEY Cutler, Maine, 24,0 kHz

MAP Q. *Profiles and posffhgsPROJECT

Lumby Lake ProjectFOR :

BY: Pierre SimoneauPROJECT Lumby Lake

AREA

DISTRICT

N.T.S.

SCALE 1 : 2500

Norway Lake


52 G 03

25 50 75 100m.

Executed by Pierre Simoneou, g6ol.

Geomatic by Pierre Simoneou

Interpreted by Pierre Simoneou

Map no 6502Project no ———^^—

DATE

07-04

08-04 08-04

52G03SW2012 2.28406 NORWAY LAKE 240

dave saunders 2 - ontario · dave saunders 2.28406 ... saunders, david bruce (e30095) saunders,...

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