GEOPHYSICAL REPORTON A

MAGNETOMETER AND HLEM SURVEYON THE

REDSTONE RIVER PROPERTY SHAW TOWNSHIP

8

Submitted by: Steve AndersonDecember,

2004

42A06NE2040 2.28981 SHAW 010

TABLE OF CONTENTS

PAGE NO. CONTENTS

1. INTRODUCTION2. LOCATION AND ACCESS2. CLAIM STATUS2. PERSONNEL3. PREVIOUS WORK4. WORK PROGRAM6. SURVEY RESULTS6. CONCLUSIONS AND RECOMMENDATIONS7. CERTIFICATE

LIST OF FIGURES

NO. l LOCATION MAPNO. 2 REGIONAL LOCATION MAPNO. 3 CLAIM SKETCH

APPENDICES

APPENDIX "A" - GEM-GSMT-19 APPENDIX "B" - APEX MAX MIN 11

MAPS-1:5000

POSTED MAGNETOMETER POSTED AND PROFILED HLEM

INTRODUCTION

The following report will deal with the results of a magnetometer and HLEM survey carried out on the Redstone River Property located in Shaw Township, Porcupine Mining Division, District of Cochrane, Ontario. A total of 14.5 km of grid lines were established and surveyed with magnetometer and HLEM between November 15th and November 30th' 2004.

The purpose of this program was to provide ground geophysical data that would aid in the geological interpretation of the area. Also, this program will further test a number of AEM conductors shown to occur within the claim group. The subject area lies just north of the Shaw Dome, which has hosted a number significant Nickel deposits as well as past producing mines.

Ontario GEOLOGY ANDPRINCIPAL MINERALSOF ONTARIO

. fHUDSON

BAY

Major Mnetai Deposits Past ana Present

• GoWt Srivet A ironT Copper-Nckel H Zinc-Copper

Plat mom Palladium 4" Uranium

Indusuial Mnerats

150 1*1**

LEGEND8fv

MESOZOICCRETACEOUS

T ' j Sedmenury roctu

PALEOZOtC DEVONIAN

^U Sedmenlary rocks

SILURIAN^—g•B Sedmemafy rocks

OREXJVtClAN ^^H Uedvnsntary rocks

CAMBRIAN

PRECAMBRIANUHtNVILLt WUVINVt

PROTEROZOICNEP- TOMESOPROTEROZOIC

^^11 hkgmatltic rocks and gneisses

^^H UaHc lo uNramaf tc plutonic^^^^^1 roctcfl

^^^H febc plutonic rocks, derived••B gneissas and miomairtes

^^•Uetavolcanicand•••l rmUMoVneniarv rooXs

SUPERIOR AND SOUTHERN PROVINCES

^^H Frtsfc intrusive rocks

j____l Mahc tatnnin rocks

•HH Volcanic and sadinwntary rocksPALEOPROTEROZOIC

HjjH Mafic Krirunve rocks

^^^B MetaEedmentary and nwtavotcanc ^^^B rocks

Cu&KRica fvto'.ttvce ARCHEAN

NEO- TO MESOARCHEAN

• Massiw to totaled granodhnai lo granrtej l Fohaud to gnnsxic tonaUe tot ..-. l granndkvtte

|^HB Melasedbnentary rocks and rJerivwt

^^^H Metavolcanic and melasedimantarv

MESOARCHE ^^m Uetavc ^H rocks

1 Phanerozoic i*

MIKE CARONREDSTONE RIVER PROPERTY

LOCATION MAP FIGURE m

LOCATION AND ACCESS

The Redstone River Property is located approximately 13km. South-east from the city of Timmins, Ontario. It lies within the south central portion of Shaw Township (Figure #3). A legal description of the claim locations can be found under the Claims portion of this report.

Access to the proposed work area is gained by taking Stringers Road south from the town of South Porcupine for approximately l Okm. At this point there is a fork in the road, which is approximately 800 meters east of the property. A network of old logging roads heading west from Stringers road provides access to the eastern portion of the property (Figure #3).

PERSONELL

The people directly involved in this work program are as follows:

M. Caron...............................................TimminsA. Belisle............................................ .Timmins

PREVIOUS WORK

This is the first phase of work carried out by the current claim holder. Previous work carried out in the immediate area includes geophysical surveys; AEM, magnetometer and VLF which was followed up by a limited amount of diamond drilling. The following is a list of work carried out in the area by previous land holders.

International Nickel Company Ltd. 1972:

- Diamond Drilling

Canadian Nickel Company Ltd. 1984:

- Diamond drilling

O. Hicks. 1990:

- Magnetometer Survey- VLF-EM Survey

~* i — '*ii-Tju,*n ""tJUr^a^ ^.j. . - K e.1 1 '-*'~T—-f*, m, NE—jE' A™ uKiWR Ti*Wl --;^L,7. ^

PROJECT

LOCATION\™t-j/^a

'K,

i.^1*. ^

MIKE CARONREDSTONE RIVER PROPERTY

REGIONAL LOCATION MAP1:600,000

FIGURE #2

CLAIMS

The claims that make up the Redstone River Property are all located in Shaw Township, Porcupine Mining Division. All are recorder in the name of Mike Caron, and are as follows:

1226494.....................9 units..............N172 Lot 6, Con INl/2 of S1/2 Lot 6, Coni El/2 of Nl/2 Lot 7, Con I NElMofSU2Lot7,ConI

1235964...................... 4 units...........Nl/2 of Sl/2 Lot 5, Con IINl/2 of Sl/2 Lot 4, Con II

3000702...................... 16 units..........Nl/2 Lot 5, Con INl/2 Lot 4, Con INl/2 of Sl/2 Lot 5, Con INl/2 of Sl/2 Lot 4, Con I

3 claims 29 units

WORK PROGRAM

The first stage of this work program involved establishing a grid over which the geophysical surveys could be carried out. The grid was set up with an east-west base line and north-south cross- lines at 100-meter intervals. The lines were then picketed ever 25 meters. A total of 14.5km of grid was established and then covered with a magnetometer and HLEM Survey.

The following is a brief description of the geophysical methods and parameters used:

SHAW TOWNSHIP PROPERTY rrS. MMng LM0 T.

H

Eldorado Township

J

KMMMF'MttA MAW

rumO-MM

MIKE CARONREDSTONE RIVER PRCPERTY

CLAIM AND GRID SKETCH FIGURE #3

MAGNETOMETER THEORY

A GEM GSMT-19 Proton Precession magnetometer was used to carry out the magnetometer survey. The instrument is synchronised with a GEM GSMT-19 recording base station to help eliminate magnetic diurnal variation. This should ensure an accuracy of less than l .0 Nt.

The Proton Precession method involves energising a wire coil immersed in a hydrocarbon fluid.This causes the protons in the proton rich fluid to spin or precess simulating spinning magnetic dipoles.When the current is removed the protons precess about the direction of the earth's magnetic field,

generating a signal in the same coil which is proportional to the total magnetic field intensity, hi thisway, the horizontal gradient of the earth's magnetic field can be measured and plotted in plan form withvalues of equal intensity joined to form a contour map.

This presentation is useful in correlating with other data sets to aid in structural interpretation. Individual magnetic responses can be interpreted for dip, depth and width estimates after profiling the data.

The following parameters were employed for the survey:

Instrument - GEM, GSMT-19 Proton Precession MagnetometerStation Interval -12.5mLine Interval - 100mDiurnal Correction Method - GEM GSMT-19 Recording Base StationData Presentation - Data posted and contoured plan map

-1:5000 scale- Contour interval: lOOnT- Datum Subtract: 56,OOOnT

HORIZONTAL LOOP SURVEY

The Horizontal Loop EM survey was carried out with an Apex Max-Min II instrument. These surveys are commonly called "Max-Min" surveys in recent times.

The Max-Min II instrument can operate at five frequencies (3555HZ, 1777HZ, 888HZ, 444HZ, 222HZ). and is capable of coil separations from 25 meters to 200 meters. Although it can be used in the vertical loop mode as well as minimum coupled, it is most often used in the Maximum Coupled, Co-Planer mode which is in effect a Horizontal Loop Electromagnetic Survey.

The instrument records the "hi-Phase" and "Out-of-Phase" components of the anomalous resultant field from a conductor as a percentage of the primary field strength. Both components are used in

5the interpretation of the results. Generally, the larger the ratio of peak negative responses between In-Phase and Out-of-Phase, the higher the conductivity of the anomaly. A ratio of l: l is considered a medium conductor.

The purpose of reading more than one frequency is to obtain more information about the conductor itself as well as the conductivity of the overburden etc. The higher frequencies will respond to weaker conductive features such as faults, conductive overburden etc. As a result the signal from these frequencies can attenuate very quickly, possibly not penetrating to the bedrock at all. The lower frequencies having a longer wavelength tend to penetrate deeper and generally only respond to anomalies with a higher order of conductance, Thus as with most geophysical techniques it is a trade off as to depth of penetration vs. conductance threshold detectable. The use of multi frequency surveys helps to alleviate this problem at a minimal extra cost.

The HLEM survey was carried out using the following parameters:

INSTRUMENT: Apex Parametrics, Max-Min IIMODE: Co-planarPARAMETERS MEASURED: In-phase and quadratureCOIL SPACING: 100 metersFREQUENCIES: 444Hz., 1777Hz. And 3555Hz.LINE INTERVAL: 100 metersSTATION INTERVAL: 25 metersDATA PRESENTATION: Profiled plan maps, 1:5000PROFILE SCALE: lcm = 1007o

SURVEY RESULTS

The geophysical program conducted on the Redstone River Property was successful in outlining a number of areas of interest. The magnetics show a number of areas with strong magnetics. The magnetics however are somewhat erratic, with a number of one line anomalies that are between 6,000-20,000 nT above background.

As with the magnetics, the results from the HLEM survey were also somewhat erratic. One of the stronger responses occurs on LI 3 00 W at 0+25 S. This zone remains open to the west and appears to a weak magnetic correlation. The second feature outlined occurs on line 900W and extends from 0+50N to 2+50N. This shows up as either a zone that is 200M in width or multiple conductors. There is a strong magnetic correlation with the central portion of this zone yet its response appears to extend beyond the influence of the magnetics.

Similar to the previous zone the last conductive zone may be the result of multiple zones. It is situated on L700W and extends from 2+25N to 3+25N, showing a width of 100M. This zone differs from the previous two as it does not have a strong magnetic correlation. It is situated between two relatively strong magnetic responses to the north and south.

RECOMMENDATIONS AND CONCLUSIONS

The conductive zones discussed above are all worth of some type of follow-up work. The geophysical results seem to indicate that there are three areas of interest.

The first two zones tend to be associated with strong magnetics which may be the result of iron formation. However, the second zone discussed shows a zone that is fairly wide, which may be the result multiple zones. The third zone may also be the result of multiple zones but lacks the strong magnetic correlation that is typical of iron formation. All three zones are worthy of follow-up work.

Initially, this data should be compiled with any additional geophysical or geological information that may be available. If after this, the conductive zones remain unresolved additional testing is warranted.

As the last two zones discussed may be the result of multiple zones, additional HLEM using a 50M or 25M coil separation may help delineate the conductors. This will only be affective if the overburden depths are no to great. A second geophysical method to consider would be Induced Polarization. This method should also help determine whether multiple zones exist by providing detailed resistive characteristics over the conductor.

During the summer months a geological mapping program should also be carried out on the property in an attempt to explain some of the geophysical responses.

Due to the past success of exploration within the Shaw Dome, if after this additional testing any of the zones remain unresolved they should be tested with diamond drilling.

CERTIFICATION

I, Steve Anderson of Timmins, Ontario hereby certify that:

1. I hold a three-year Technologist Diploma from Sir Sandford College, Lindsay, Ontario, obtained in May 1981.

2. I have been practising my profession since 1979 in Ontario, Quebec, Nova Scotia, New Brunswick, Newfoundland, N WT, Manitoba, Saskatchewan and Greenland.

3. I have been employed directly with Asamera Oil Inc. Urangellschaft Canada Ltd. Nanisivik Mines Ltd., R.S. Middleton Exploration Services Ltd., and Rayan Exploration Ltd.

4. I have based conclusions and recommendations contained in this report on knowledge of the area, my previous experience and on the results of the fieldwork conducted on the property during 2004.

Dated this 28th day of December 2004 at Timmins, Ontario.

APPENDIX "A" GEM-GSMT-19

GEM GSM-19

INSTRUMENT SPECIFICATIONS

MAGNETOMETER l GRADIOMETERResolution: 0.01 nT (gamma), magneticfieW and gradient.

0.2 nT over operating range. 20,000 to 120,000 nT. Over 1 0,000 riT/m

:3 seconds minimum, fester optional. Readings initiated from keyboard, external trigger or carriage return "via RS-232-C. 6 pin weatherproof connects; RS-232C, and (optional) analog output 12 V, 200 mA peak (during po/ariration), 30 mA standby. 300mA peak in gradiometer mode.Internal 12 V, 2.6 Ah sealed iead-add battery standard, others op tional An External 12V power-source can also be used Input 110 VAC, 60 Hz. Optional 110/220 VAC, 50/60 Hz. Outoufc dual level charging. Temperature: -40 *C to +60 *C Battery Voltage: 10.0 V minimum to 15V maximum. Humidity: op to SQft, rdafive, non condensing. -SCTCto+GS^CLCD:240 x 64 pixels, or 8 x30 characters. Built in heater for opera tion bdow -20^0 Console: 223 x 69 x 240mm. Sensor staffc 4 x450mm sectiorts. Sensor 170 x 71 mm dia. Wejghfc Console 2.1 kg. Staff 0.9kg, Sensors l .1 kg each.

Accuracy: Range:Gradient Tolerance:

. Operatingtntervat.

Jnput/Output Power Reo,uirernents:

Power Source: "

Battery Charger:

Operating Ranges:

Storage Temperature: DtspJay:

Dimensions:

YLFFrequency Range: Parameters Measured:

Resolution:Number of Stations: Storage: ;

Terrain Stope Range: Sensor Dimensions: Sensor Wefcht:

15-30.0 kHz.Vertical In-phase and Out-of-pha^e components as percentage of total

2 components of horizontal field.Absotute arnpCtude of total fieJd. Q.1%.Up to 3 at a time.

, EMJn-' components for each selected station.O*- 900 Centered manuallyj.14 x 15 x 9 on, (5 J5 x 6 x 3 inches).1-Oki?G.2[hl.

arxi both

APPENDIX "B" APEX MAX MINI l

P f*!* l**w tow* ft prat f pent paar K ff . ORTAIBLE BIVI

C Five; frequencies: 222, 4*3.4, 388,1777 and 3555 Hz.t Maximum coupled C horizontal-loop 3 operation with

reference cable,

r Minimum coupled operation with reference cable. •' Vertical-loop operation without reference cable.

Coil separations: 25, 50,100,150,200 and 25O m C with cable 3 or 100,15100,300,400,600 and BOO ft.

Reliable data from depths of up to ISO m C GOO ft 3.

Built-in voice communication circuitry with cable.

Tilt mete r s to control coil orientation.

-jes : 222, 444, BBS. 1777 and 3555 Hz . P.

: Ci p E-ac i or:; MAX: Transmitter coil plane and re ceiver coil plsine horizontal [Max-coupled; Horizontal-loop T: mode]. Used with refer, cable .

M l N: Transmitter coil plane horizon tal and receiver coil plane ver tical (Min-coupied mode J. Used with reference cable.

Coil Separs-ions:

V. L. : Transmitter coil plane verti cal pnri recei^'esr canil plar"? hori^ zontal CVertical-laop mode). Used without reference cable, in parallel lines.

25.5O.TOD.15O.elOO S25Om CMMID or 1OO. 2OO, 3OO. 4OO,BOOand BOO ft. C MM H F :i . Coil separations in VL.mode not re stricted to fixed values .

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

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

Readouts: - Automatic, direcg, readout on9Omm [3.5''^5e"dgewise meters in MAX and M IN modes. No null ing or compensation necessary .

- Tilt angle and null in 9Omm edge wise meters in V.L.mode .

Scele Ranaes In-Phase: ±2DV.,±1OO 0/. by puE5h- button switch .

Quadrature: ±2O Vo. i1OO 0/. by push button switch .

Tilt; ±75 '/o slope .Null [VLJ: Sensitivity adjustable:

by separation switch.

t e 3 ci E a i l i t; y : In-Phase and Quadrature: Tilt : 1-/0

D.5

±D.5"Xoto ±"1^, normally, depending on conditions, frequencies and coil separation used .

- 222Hz : 175 Atm2 444Hz : 1SO Atm2

- BBS H z : 1OOAtm2- 1777 Hz : BOAtm2-3555 Hz : 3OAtm2

.ec:srv-er Betre-ies: 9V trans, radio type batteries (4). Life: approx. 35hrs. continuous du- Ly lalKaline ," Q.a Ah 3, less in cold weather .

i ransmitrcer E ette rie E :

Voice L.ink :

12V 7.5Ah Bel-Cell rechargeable batteries C 2 x 6V in series ] .

Light weight 2-conductor teflon cable for minimum friction. Unshield ed. AJI reference cables optional at extra cost. Please specify.

Built-'n intercom system for voice communication between re ceiver and transmitter operators in MAX and MIIXI modes, via re ference cable .

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

Temperature Range; -4O"C to *BO"C [-4D

Receiver Weight : Bkg C 13 IbsJ

Transmitter \Weight: 13kg C2SlbsJ

Shipping Weight: Typically BOkg C135lbs.3, depend ing on quantities of reference cable .and batteries included. Shipped in two field/shipping cases .

Specjf ications subject: t-o change witnout n o ci f i c anon

PARAMETRICS LIMITEDSOO ErrEHELCASE RD. E., MARKHAM, ONT. CANADA, L3R 1B2

Phone: 495-1612 Cables: APEXPARA TORONTO Telex : OB-3BB773 NORDVIK TOR

MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No: Recording Date: Approval Date:

Client(s):116051

Survey Type(s):

W0460.019862004-DEC-30

2005-JAN-04

Work Report Summary

Status: APPROVEDWork Done from: 2004-NOV-15

to: 2004-DEC-30

CARON, MICHEL GEORGE

EM LC MAG

Wqrk Report Details:

Claim*

P 1226494

P 3000702

External Credits:

Reserve:

Perform Applied Perform Approve Applied Approve

SO SO 33,600 53,600

813,489 313,489 36,400 36,400

313,489 313,489 310,000 310,000

30

Assign

SO

33,600

33,600

Assign Approve Reserve

0 SO

3,600 33,489

33,600 33,489

Reserve Approve Due Date

SO 2005-DEC-30

33,489 2005-DEC-30

53,489

33,489 Reserve of Work Report*: W0460.01986

33,489 Total Remaining

Status of claim is based on information currently on record.

42A06NE2040 2.28981 SHAW 900

2005-Jan-11 11:18 ARMSTRONGI Page 1 of 1

Mir.'stry ofNorthern Developmentand Mines

Date: 2005-JAN-05

Ministere du Developpement du Nord et des Mines Ontario

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

MICHEL GEORGE CARON 253 LOIS CRESCENT TIMMINS, ONTARIO P4P1G7 CANADA

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

Dear Sir or Madam

Submission Number: 2.28981 Transaction Number(s): W0460.01986

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 STEVEN BENETEAU by email at steve.beneteau@ndm.gov.on.ca or by phone at (705) 670-5855.

Yours Sincerely,

Ron C. GashinskiSenior Manager, Mining Lands Section

Cc: Resident Geologist

Michel George Caron (Claim Holder)

Assessment File Library

Michel George Caron (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:20225

42A06NE2040 2.28981 SHAW 200 ONTARIOCANADAMINISTRY OF NORTHERN MVELOPMINT AND MINI*

PROVINCIAL MINING RECORDER'S OFFICE

Mining Land Tenure Map

5355000N

\( 30195861 490000E

UTM Zone 17 5000m grid

Those wishing to stake mining claims should consult with the Provincial Mining Recorders' Office of the Ministry of Northern Development and Mines for additional information on the status of the lands shown hereon. This map Is not intended for navigational, survey, or lend title determination purposes as the information shown on this map Is compiled from various sources. Completeness and accuracy are not guaranteed. Additional information may also be obtained through the local Land Titles or Registry Office, or the Ministry of Natural Resources,

The Information shown Is derived from digital data available in the Provincial Mining Recorders' Office at the time of downloading from the Ministry of Northern Development and Mines web site.

General Information and LimitationsContact Information: Tot! Free Map Datum: NAD 83Provincial Mining Recorders' Office Tel; 1 (888) 415-9846 ext 57ftoiection: UTM (6 degree)Willet Qreen Miller Centre 933 Ramsey Lake Road Fax: 1 (677) 670-1444 Topographic Data Source: Land Information OntarioSudbury ON P3E 6B5Home Page: www.mndm.gov.on.cayMNDM/MINES/LANDS/rnlsmnpge.htm

This map may not show unregistered land tenure and interests in lanti Including certain patents, leases, easements, right of ways, flooding rights, licences, or other forms of disposition of rights and Interest from the Crown. Also certain land tenure and land uses

Mining Land Tenure Source; Provincial Mining Recorders' Office 'l™' restrict or prohibit free entry to stake mining claims may not beIllustrated.

Date 7 Time of Issue: Thu Jan 13 09:37:47 EST 2005

TOWNSHIP 7 AREA PLAN SHAW G-3999

ADMINISTRATIVE DISTRICTS 7 DIVISIONSMining DivisionLand Titles/Registry DivisionMinistry of Natural Resources District

PorcupineCOCHRANETIMMINS

TOPOGRAPHIC

r ( Administrative Boundaries

i * Township

Concession, tot

Hi Provincial Park

liilsl Indian Reserve

\"": Cliff, Pit S Pile

m

A

Contour

Mine Shafts

Mine Headframe

Railway

Road

Trail

Natural Gas Pipeline

innes

Tower

Land Tenure

Freehold Patent

nn Surface And Mining Rights

FT] Surface Rights Only

nn Mining Rights Only

Leasehold Patent

r^~| Surface And Mining Rights

r^l Surface Rights Only

Fgl Mining Rights Only

Licence of Occupation

fs") Uses Not Specified

Surface And Mining Rights

Surface Rights Only

Mining Rights Only

m m m

Land Use Permit

Order In Council (Not open for starting)

Water Power Lease Agreement

Mining Claim

Filed Only Mining Claims

LAND TENURE WITHDRAWALS

1234 ] Areas Withdrawn from Disposition

——————i Mining Acts withdrawal TypesWsm Surface And Mining Rtgtm WithdrawnWs Surface Rights Only WitndrawnWm Winino Rights Only Withdrawn

Order In Council Withdrawal Types W0srrt Surtac* And Mining Rigrttt Withdrawn Wes Surface Right* Only WttKtrtwn W"m Mining Rights Only Withdrawn

IMPORTANT NOTICES

Sole 1:39170

LAND TENURE WITHDRAWAL DESCRIPTIONSIdentifier Type Date Description

03017622 WOT Jul 5,2004 ^ href*" http^/www.mci.mndm.gov.on.ca/Clalms/Cf.Claims/cim^cssmClaim.Viow_Claim.Number-03017522'*

03018751 Wsm Jul 7,2004 ea href*" http://Www7md.mndm,gov.on.ca/Claims/CT.CIaims/dm^cssmClaim View_Claim Number*03018751":xa^

3469 Wsm Jan 1,2001 REC.PURP, SEC.3 PLA 188543 3690 Wsm Jan 1, 2001 DUCKS UNLIMITED - PENDING APPLICATION UNDER THE PUBLIC

LANDS ACT S.R.O. WITHDRAWN 3592 Ws Jan 1,2001 DUCKS UNLIMITED - PENDING APPLICATION UNDER THE PUBLIC

LANDS ACT S.R.O. WITHDRAWN3605 Wsm Jan 1,2001 APPLICATION PENDING UNDER P.L.A.-SURFACE RIGHT WITHDRA W.97/77 Ws Jan 1,1980 W.97/77 15/12/77 S.R.O. 86555

(Oft

NJ H" O

8

50Scale 1:5000100 150 200 250 300 350

(metres)

MIKE CARONHLEM SURVEY 444Hz.

REDSTONE RIVER PROJECTSHAW TOWNSHIP

to w o

c\o

^1

50 50Scale 1:5000100 150 200111111 'l

(metres)

250 300 350

MIKE CARONHLEM SURVEY 1777HZ.

REDSTONE RIVER PROJECTSHAW TOWNSHIP

APEX MAX- 1crr^10

1:5000

toU)o

50 50Scale 1:5000100 150 200

SI (metres)

250 300 350

l____

MIKE CARONHLEM SURVEY 3555Hz.

REDSTONE RIVER PROJECTSHAW TOWNSHIP

APEX MAX-MiN ^crr\ = ^Q70

1:5000

1 300WOJo o

1200W i

NO O O

QQW TOQQWo o

oo oo o o o o o

50*o o

40lJiiVo o o o

' f

*-.

M

Scale 1:500050 Q !.Q 1 C f. ' : O .00 250 5CC

(metres)

MIKE CARONMAGNETOMETER SURVEY

REDSTONE RIVER PROJECTSHAW TOWNSHIP

GSM-19 MAGNETOMETERA T1 " -MBTRACT 56COOnT

. JRED @ 1CC-T 1:50 C C