2 778

A Report on Airborne Geophysical Survey on the Nipigon Plate Property,

ofEAST WEST RESOURCE CORPORATION Red Granite Claim Group, Pillar Township

Thunder Bay Mining Division, Ontario Province of Ontario

forEast West Resource Corporation 402 - 905 W Pender Street Vancouver, British Columbia V6C 1L6

September 15th , 2002

Roger J Caven, BASc, P Eng, Consulting GeophysicistRR# 5, 479 Ocean View Drive, Gibsons, British Columbia, CANADA VON 1V5 Tel/Fax: (604) 886-0479, e-mail: rogei^caveiKg^telus.net (Sunshine Coast)

52I03NE2001 2.27784 PILLAR LAKE 010

TABLE OF CONTENTSSummary Page 3Introduction 3Location and Access 4Property - Description and Location 4Geological Setting of Host Rocks and Ore 4 General Geology of the Lake Superior - Nipigon Area 5Geology of Pillar Township 5Detail Airborne Magnetic Survey 6

Discussion of Results 6Radiometric Measurements 6

Discussion of Results 6Distribution of Work Performed 7Conclusions and Recommendations 7References 8

Certificate of Author 10

Operations Report- High Sensitivity Magnetic S Radiometric Airborne Survey, Red Granite Project, Lake Nipigon Area, Ontario, for East West Resource Corporation, by Terraquest Ltd, January 16, 2003.

Location MapClaim Map - Red Granite (Pillar Twp) Scale 1:40,000 Reduced Magnetic Contour Map, with claims Scale 1:40,000 Reduced Potassium Contour Map, with claims Scale 1:40,000 Reduced Thorium Contour Map, with claims Scale 1:40,000 Reduced Uranium Contour Map, with claims Scale 1:40,000

In PocketAirborne Magnetic Contour Map, with claims Scale 1:20,000 Airborne Potassium Contour Map, with claims Scale 1:20,000 Airborne Thorium Contour Map, with claims Scale 1:20,000 Airborne Uranium Contour Map, with claims Scale 1:20,000

SUMMARY 9 2 7 *7 S 4:

East West Resource Corporation holds several groups of claims in the Nipigon Plate, including the 185 claim units in the Red Granite claim group in the Pillar Lake area near the Havoc Lake area within the Nipigon Plate northwest of Lake Nipigon, Ontario. (Location map.)

This report deals with the recent airborne detail magnetic and radiometric surveys over the Red Granite claims.

INTRODUCTION

The following information has been abstracted from the "Report on the Nipigon Plate Platinum Group Element - Nickel - Copper Properties, Thunder Bay Mining Division, Ontario, for Canplats Resources Corporation", October 16th , 2000, by R Caven and K Gunnison ("Canplats Report"):

"The Nipigon Plate - Lake Superior area has been interpreted to be a favourable setting for Noril'sk type PGE bearing massive sulphide deposits. The tectonic setting and geological host rock types are identical to the Noril'sk region. The existence of major copper - nickel deposits in the region such as the Duluth Gabbro complex deposits, and the Great Lakes Nickel deposit within the Crystal Lake Gabbro, as well as the presence of PGE values in a previously unknown ultramafic body (Seagull Pluton) on the south side of Lake Nipigon, suggests that favourable mafic intrusive bodies occur in the Nipigon Plate."

"The Nipigon Plate is one of the largest areas of Proterozoic rocks in the world and it includes the second most extensive area mafic intrusions after the Bushveld Complex in South Africa. Between Thunder Bay in the south to Armstrong in the north, widespread diabase (dolerite) sills of olivine - tholeiite composition called the Logan Sills cover a 200 km by 250 km area (over 40,000 square kilometres). Adjacent to this area, beneath Lake Superior, the Keweenawan flood basalts occur with up to 30 km of thickness. These lavas and the diabase (dolerite) sills are similar in geological setting to the Noril'sk - Talnakh nickel - copper - platinum group metal producing region of north central Siberia."

"Within Lake Superior, the Mid-continental Rift extends south-westward to Texas and is the tectonic setting for the flood basalts. A failed arm of the Mid-continental Rift extends northward through the Nipigon Plate and takes the form of the Black Sturgeon Fault. The importance of this fault has now been recognized and has been extended northward another 150 km, by re- interpretation of the aeromagnetic data. It is now apparent that this fault and a series of parallel faults are the main structures that are related to the mafic intrusives of the Logan Sill event, as well as older and younger intrusives. Evidence for the presence of an older rift system in the Lake Nipigon Area was discovered during the course of this investigation which suggests the presence of an early basin, graben, or trough which controlled the deposition of the Sibley sediments and is related to a series of alkali felsic intrusions. This setting should also be explored for Olympic Dam- type mineralization in addition to exploring for Noril'sk type mineralization in the younger mafic intrusions. The older rift system was likely reactivated during the formation of the Mid-Continental Rift."

2 778 4

LAhh

NIPIGON

Location Map Red Granite Area

"It has been proposed for the last 10 years that there is a similarity between the Lake Nipigon - Lake Superior region and the Noril'sk area (Naldrett, A J, and Lightfoot, P C (1993), Duzhikov, O A, Distler, V V, Strunin, B M M, Krtychyan, A K, Sherman, M L, Sluzhenikin, S S, and Lurje, A M (1993), Society of Economic Geologists, Special Publication No 2, Giant Ore Deposits. Ed: Whiting, B H, Hodgson, C J, and Mason, R). Naldrett (1993) establishes this fact in a paper presented at Queens University as part of a symposium on Giant Ore Deposits and he concludes: "The Lake Superior area has the correct regional tectonic setting (triple junction and associated rifting), has a widespread development of basalt, and some of the basalts show evidence of chalcophile element depletion. What then is missing from the equation in the Lake Superior area that so far has precluded a "Giant", Noril'sk - type deposit being found there? One obvious point is the lack of recognition of major faults of trans-crustal magnitude, that have served as the locus for ore-bearing magma."

LOCATION AND ACCESSThe Nipigon Plate Red Granite property located at ~ 500 13' N l 890 10' W, 175 km north of Thunder Bay, and is road accessible via Hwy 527, which links Thunder Bay, Ontario, to Armstrong, Ontario. Local and forestry roads branch off the highway.

PROPERTY - DESCRIPTION AND LOCATIONThe Red Granite claim group is located in the north western part of the Pillar Township, about 20 km south of Armstrong, and is accessed from Hwy 527 via a logging road extending west of the highway into the property. The claim group consists of 13 claims recorded to East West Resource Corporation, containing 185 claim units for an area of 7400 acres, or 2960 ha.

Claim AreaTB3000993 Pillar TB3000994 Pillar TB3000995 Pillar TB3000996 Pillar TB3000997 Pillar TB3000998 Pillar TB3000999 Pillar TB3001000 Pillar TB3001001 Pillar TB3001002 Pillar TB3001003 Pillar TB3011083 Pillar TB3011084 Pillar

Units16161608161515121212151616

RecordedJun03-2002Jun03-2002Jun03-2002Jun03-2002Jun03-2002Jun03-2002Jun03-2002Jun03-2002Jun03-2002Jun03-2002Jun03-2002Jan06-2003Jan06-2003

Due DateJun03-2004Jun03-2004Jun03-2004Jun03-2004Jun03-2004Jun03-2004Jun03-2004Jun03-2004Jun03-2004Jun03-2004Jun03-2004Jan06-2006Jan06-2006

Work Req'd36,40036,40036,40053,20036,40056,00056,00034,80034,80034,80036,00036,40036,400

185

GEOLOGICAL SETTING OF HOST ROCKS AND ORE.

574,000

An extensive area of flood basalt covering and flanking widespread sediments containing sulphate evaporites and local coal measures (methane sources), which are in turn intruded by 30 - 350 m thick dolerite (diabase) sills, characterizes the geological setting of the Noril'sk camp. A major northeast trending fault known as the Noril'sk - Kharayelakh Fault is the main controlling feature that localized the mafic to ultramafic intrusions and dolerite sills. This fault is steeply dipping and is deep seated and may have tapped the mantle. The overall setting is a rift tectonic environment and is proximal to a triple junction of faults where two rift systems meet. All of the above characteristics are found in the Lake Superior- Nipigon area, including a major fault structure (the Black Sturgeon Fault) and a triple junction in Lake Superior associated with the Midcontinental Rift of North America.

GENERAL GEOLOGY OF THE LAKE SUPERIOR - NIPIGON AREA Sibley SedimentsThe Sibley Group of sediments occur on the north shore of Lake Superior and extend north-ward as far as Armstrong, Ontario, and form the base for the Nipigon Plate. This would be roughly a 200 km by 150 km area that has subsequently been intruded and capped by the Logan diabase sills. Age dating by Rb/Sr methods have suggested an age of 1339 +I- 33 Ma, Franklin (1970), however, mapping by Sutcliffe (1987) suggests that an older date is possible for the base of the Sibley. In the vicinity of English Bay on Lake Nipigon fragments of Sibley have been observed by Sutcliffe to be mixed with felsic volcanic fragments that are related to a high level alkali intrusion that yields an age of 1537 Ma. Fragments of a quartzite and grit - shale units were observed in the alkaline porphyry intrusive by Gunnison (Canplats Report), suggesting the Sibley or lower sections existed when the alkali body was intruded. Therefore this suggests that an older rift system existed, as old as 1537 Ma. Tanton (1931), Franklin (1970, 1980, 1982), Cheadle (1986), Mcilwaine and Wallace (1976), Wallace (1981), and Sutcliffe (1991) have described the stratigraphy and geological setting of the Sibley in detail.

The importance of the Sibley to the search for PGE - nickel deposits in the Nipigon Plate area is that a source of sulphur is desirable for the generation of sulphide deposits within the mafic - ultramafic bodies. Franklin (1970, 1982) notes that barite occurs in the lower and middle formations (Pass Lake and Rossport) and that gypsum and anhydrite occur in the middle and upper formations (Rossport and Kama Hill). In addition methane gas and hydrogen sulphide occur, particularly in association with stromatolite horizons in the Rossport and Kama Hill formations. It is therefore concluded that abundant sources of sulphur were available to later mafic - ultramafic intrusions to generate sulphide bodies. This same geological setting occurs at the Noril'sk and Talnakh PGE - Ni - Cu mining camps in northern Siberia, C l S (formerly USSR), where sulphate-bearing sediments and coal measures are in contact with mafic intrusions.

Mid Proterozoic Mafic IntrusionsThe mid Proterozoic mafic intrusions in the vicinity of the Nipigon Plate consist of two known suites of rocks, an early stage ultramafic - picrite event, the full extent of which is unknown, and the diabase - dolerite Logan Sills which are very extensive, 200 km x 120 to 250 X 200 km. These two events are followed by other mafic intrusives southwest of Thunder Bay, namely the Pigeon River dykes, which cut the Logan Sills and the Crystal Lake gabbro - Mollie dyke which cut the Pigeon River dykes. Further away to the east of the Nipigon Plate a series of carbonatite syenite complexes occur such as the Coldwell complex which contain phases of gabbro - norite hosting large low grade copper - PGE values. These intrusions are also related to a failed arm structure that trends northeast from the Midcontinental Rift beneath Lake Superior and are dated at 1.05 billion years, Good P J, and Crockett J H (1994).

The geology of the picrites and Logan sills in the Thunder Bay region has been described by Pye (1953), Blackadar(1954), Geul (1970, 1973).

GEOLOGY OF PILLAR TOWNSHIP

The 185 claim unit Red Granite property is situated in Pillar Township where a series of nickel- copper-platinum-palladium lake sediment geochemical anomalies are found associated with Proterozoic gabbroic mafic intrusives. Also highly altered Sibley sediments with hematite and actinolite veining have been observed to the south of the property, reflecting a second style of mineralization such as oxide-copper-gold mineralization, similar to the Olympic Dam mineralization in Australia, related to the English Bay event (1540 ma).

AIRBORNE DETAIL MAGNETIC SURVEY

The magnetic survey was conducted in early January of 2003, with poor weather conditions necessitating delays and reflights. The survey area was 7 km in north-south direction and 10 km in the east-west direction, with north-south flight direction. A total of 792 km was flown, including 52 km of tie-lines, of which 513.5 km of survey lines and 31.2 km of tie-lines cover the claims and are plotted on the maps. The flight line separation was nominally 100 m. The details of the equipment and flight operations are described fully in the attached Operations Report.

Discussion of ResultsThe results of the magnetic survey are shown on a map of contoured total field magnetics together with flight lines. The magnetic map has a highly magnetic anomaly feature in the south west of the area, as well as an arcuate magnetic high east thereof. The arcuate magnetic anomaly may identify the perimeter of an intrusive.

RADIOMETRIC MEASUREMENTS

Simultaneously with the magnetic survey, the survey also measured the potassium (K), thorium (Th), and uranium (U) radioactive elements. The results are shown in three separate maps, one for each element.

Discussion of ResultsIn the southwest of the map where there is a magnetic high both potassium and thorium levels are low, in contrast to the arcuate magnetic anomaly to the east which shows no distinct feature in these radio-elements. The areas to the north are mostly high in potassium and thorium, even over the magnetically low area. Uranium shows higher over part of the potassium - thorium anomalous areas. Further interpretation would benefit from better knowledge of the overburden and geology from mapping than is available to the author at present.

DISTRIBUTION OF WORK PERFORMED

The following work has been determined for each claim, the total coverage assigned including turnaround but excluding peripheral lines. IQ.% has been added to in-claim coverage:

Claim Area Units Recorded Due Date Work Req'dTB3000993 Pillar 16TB3000994 Pillar 16TB3000995 Pillar 16TB3000996 Pillar 08TB3000997 Pillar 16TB3000998 Pillar 15TB3000999 Pillar 15TB3001000 Pillar 12TB3001001 Pillar 12TB3001002 Pillar 12TB3001003 Pillar 15TB3011083 Pillar 16TB3011084 Pillar 16

Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jun03-2002 Jun03-2004Jan06-2003 Jan06-2006Jan06-2003 Jan06-2006

$6,40036,40056,40033,20036,40036,00036,00054,80034,80034,80036,00056,40056,400

185 units

Coverage27.227.127.212.827.225.9221.1219.8421.5518.8824.0027.2027.20

574,000 313.81km

(km) Assigned29.9229.8129.9214.0829.9228.5130.4921.8223.7120.7726.4029.9229.92

345.19 km

CONCLUSIONS AND RECOMMENDATIONS

The magnetic survey has provided a detailed view of the claim group, and will provide a database for further interpretation and exploration. The magnetic feature in the centre to east, which forms an arcuate shape may be the manifestation of the rim of an intrusion. The radiometric maps will provide a wealth of information when combined with mapping of the overburden and geology of the claims, which is highly recommended.

Respectfully submitted September 15th , 2003

rRoger J Caven, P

REFERENCES

Blackadar, R G (1954). Differentiation and assimilation in the Logan Sills. Ph D thesis, University of Toronto.

Canplats Report: "Report on the Nipigon Plate Platinum Group Element - Nickel - Copper Properties, Thunder Bay Mining Division, Ontario", for Canplats Resources Corporation, formerly International Colby Resources Corporation, by R Caven and K Gunnison, October 16th , 2000.

Cheadle, Burns A (1986). Alluvial - playa sedimentation in the lower Keweenawan Sibley Group, Thunder Bay District, Ontario. Canadian Journal of Earth Sciences, Vol 23, No 4, p 527-542.

Coates, M E (1972). Geology of the Black Sturgeon River Area, District of Thunder Bay; Ontario Department of Mines and Northern Affairs, Report 98, 41 p, incl maps 2233, 2234, 2235, and 2236, scale 1^ YZ mile.

Duzhikov, O A, Distler, V V, Strunin, B M M, Krtychyan, A K, Sherman, M L, Sluzhenikin, S S, and Lurje, A M (1993), Society of Economic Geologists, Special Publication No 2, Giant Ore Deposits. Ed: Whiting, B H, Hodgson, C J, and Mason, R

Franklin, J M (1970). Metallogeny of the Proterozoic rocks of the Thunder Bay district, unpublished Ph D thesis, University of Western Ontario, London, 317 p.

Franklin, J M, Mcilwaine, W H, Poulsen, K H, and Wanless, R K (1980). Stratigraphy and depositional setting of the Sibley Group, Thunder Bay district, Ontario, Canada, Canadian Journal of Earth Sciences, Vol 17, No 5, p 633-651.

Franklin, J M (ed. 1982). Proterozoic geology of the northern Lake Superior area, Geol Assoc of Canada Field Trip Guide Book 4, 71 pages.

Geul, J J C (1970). Geology of Devon and Pardee Townships and the Stuart Location. Ont Dept of Mines Geology Report 87, accompanying map 2207, re:Great Lakes Nickel Deposit.

Geul, J J C (1973). Geology of Crooks Township, Jarvis and Prince locations and offshore islands, District of Thunder Bay, Ontario Division of Mines, Geological Report 102, 46 p.

Good, D J, and Crockett, J H (1994). Genesis of the Marathon Cu - platinum group elementdeposit, Port Coldwell alkalic complex, Ontario: A mid-continent rift related magmatic sulphide deposit. Economic Geology, Vol 89, p 131 - 149.

Mcilwaine, W H, Wallace, H (1976). Geology of the Black Bay Peninsula Area, District of Thunder Bay, Ontario. Ontario Division of Mines, GR 133 incl map 2304, scale 1"z 1 mile.

Naldrett, A J (1993). Ni - Cu - PGE Ores of the Noril'sk Region, Siberia: A Model for Giant Magmatic Sulphide Deposits Associated with Flood Basalts,in Society of Economic Geologists, Special Publication No 2, Giant Ore Deposits. Ed: Whiting, B H, Hodgson, C J, and Mason, R.

Naldrett, A J, and Lightfoot, P C (1993), Society of Economic Geologists, Special Publication No 2, Giant Ore Deposits. Ed: Whiting, B H, Hodgson, C J, and Mason, R

Pye, E G (1953). A petrographic study of the textures of basic and ultrabasic igneous rocks; unpublished PhD thesis, University of Toronto, Toronto, Ontario, 93p.

Sage (1998). Operation Ignace- Armstrong, Obonga Lake - Lac des Iles Area, Geology of Area M: Part 1 - Super crustal rocks, Part 2 - Granites, Granite-Super crustal Relationships, OGS Open File Report 5978, 443 p, maps P. 962, and P. 963.

Sutcliffe, R H (1987). PhD Thesis, University of Western Ontario, London, Ontario.

Sutcliffe, R H (1991). Proterozoic Geology of the Lake Superior Area in Geology of Ontario, OGS Special Volume 4 pt 1, p 627 - 660.

Tanton, T L (1931). Fort William, Port Arthur, and Thunder Cape map areas, Thunder Bay District, Geological Survey of Canada, Memoir 167, 222 p.

Wallace, H (1981). "Keweenawan geology of the Lake Superior Basin", in Proterozoic Basins of Canada, Ed: F H Campbell, GSC Paper 81-10, pp 399 - 418.

10

CERTIFICATE OF QUALIFICATIONS

l, Roger J Caven, of 479 Ocean View Drive, Gibsons, British Columbia, hereby certify that:

1. l am a graduate of the University of Toronto, Faculty of Applied Science and Engineering, Engineering Science Course, Geophysics Option (1967).

2. l am a registered Professional Engineer in the Provinces of British Columbia and Ontario.

3. l am a Fellow of the Geological Association of Canada, and an Active Member of theSociety of Exploration Geophysicists, the Australian Society of Exploration Geophysicists, the European Association of Geoscientists and Engineers, and IEEE.

4. l am presently employed as an independent Consulting Geophysicist, with address in Gibsons, British Columbia.

5. l have been employed in my profession since graduation, by Barringer Research Inc as a Senior Geophysicist, and with UMEX Inc as Chief Geophysicist in charge of exploration, and as a Consulting Geophysicist since 1983.

6. The information contained in this report was obtained through a study of information listed in the references, airborne surveys over the property, as well as having worked extensively in the Canadian Shield, particularly in northwestern Ontario on the Thierry Ni-Cu-PGE deposit near Pickle Lake, on exploration for nickel sulphides and other mineralization in that region.

Dated at Gibsons, British Columbia, this 15th day of September, 2003

Rog^er J^Caven, P Eng, FGAC; Consulting Geophysicist

B-084

OPERATIONS REPORT

HIGH SENSIVITY MAGNETIC & RADIOMETRIC AIRBORNE SURVEY

RED GRANITE PROJECT

LAKE NIPIGON AREA

ONTARIO

for

EAST WEST RESOURCE CORPORATION

by

TERRAQUEST LTD.

January 16. 2003

TABLE OF CONTENTS

1.0 INTRODUCTION 2.0 SURVEY AREA 3.0 EQUIPMENT SPECIFICATIONS

3.1 AIRCRAFT3.3 AIRBORNE GEOPHYSICAL EQUIPMENT3.4 BASE STATION

4.0 SURVEY SPECIFICATIONS4.1 LINES AND DATA4.2 TOLERANCES4.3 NAVIGATION AND RECOVERY4.4 OPERATIONAL LOGISTICS

5.0 DATA PROCESSING 6.0 SUMMARY

2233356666677

APPENDIX I APPENDIX II

PersonnelCertificate of Qualification

MAPS1) Total Magnetic Field2) Measured Horizontal Gradient A Calculated Vertical Magnetic Gradient3) Potassium, (07o)4) Thorium. (PPM)5) Uranium. (PPM)

1.0 INTRODUCTION

Tliis report describes the specification and results of an airborne geophysical survey carried out for EAST WEST RESOURCE CORPORATION, 402 - 905 West Fender, Vancouver. BC, V6C l LA attention Mr. Bob Middleton, telephone 604-861-3154. fax 604-689-5930. The survey was performed by Terraquest Ltd., 1366 Boulder Creek Cres. Mississauga. Ontario. Canada L5K 4P5. telephone 905-403-0026. fax 905-403-0065 and email irifafl'.terraquest.ca.

The purpose of the survey of this type is to collect geophysical data that can be used to prospect directly for anomalous magnetic areas in the earth's crust which may be caused by or related to economic minerals. Secondly, the geophysical patterns may be used indirectly for exploration by mapping the geology in detail, including the faults, shear zones, folding, alteration zones and other structures.

To obtain this data, the area was systematically traversed by an aircraft carrying geophysical equipment along parallel flight lines spaced at even intervals and oriented so as to intersect the geology and structure in a way as to provide optimum contour patterns of the geophysical data.

2.0 SURVEY AREA

The survey area is in northwestern Ontario west of Lake Nipigon, approximately 175 kilometres north of the Thunder Bay. The survey block lies over and to the west of side of Highway 527 in the vicinity of Pillar lake. The survey block is rectangular measuring 7 kilometres north south and 10 kilometres east west. The centre of the area is approximately 50 degrees 13 minutes north and 89 degrees 10 minutes west. The survey coordinates as supplied by the client are as follows:

01222234567891011141617202130313839102

B084 LINESZ 16

340000.0350000.0350000.0340000.0340000.0

101100.0

340000.0340000.0

7510 -158

10.9996000000

2001010

340000.0CLARKE-1866

0201605

UTM

5567000.05567000.05560000.05560000.05567000.0

5559500.05567500.0

-187

0.0

5567000.06378206.4

9600 N 19600 0 1

AREA CORNER lAREA CORNER 2AREA CORNER 3AREA CORNER 4

NW WAYPOINTS lNUMBER OF LINESSPACING, m.MASTER LINE BLMASTER LINE TLMAX CROSS TRACK, m.DELTA X/Y/ZLOG FPR EVERY l SECS0.0 KO, X/Y SHIFTLINES EXTENDED BEYOND AREAFIRST LINE NUMBER

0.00 MASTER POINT, HEADING 294.9786982 5 ELLIPSOID

NO EQUATORIAL CROSSINGRS-232 PORT 2 INCOMING FORMATRS-232 PORT l OUTGOING FORMATUTM DATA TYPE, METRIC SYSTEMRACE TRACKUTM X/Y SCALE

2 .2 7784

3.0 EQUIPMENT SPECIFICATIONS

3.1 AIRCRAFT

The survey was carried using a twin engine Piper Navajo P A31-325 aircraft registration C-GXKS, which carries three high sensitivity magnetometers. The aircraft has been extensively modified to support a tail stinger and two wing tip extensions with pods which house the magnetometer sensors. Considerable effort has been made to remove all ferruginous materials near the sensor and to ensure that the aircraft electrical system does not create any interference or noise. The figure of merit using Geological Survey of Canada standards is approximately 9 nT uncompensated and approximately 0.8 to 1.2 nT compensated depending on the latitude and geological environment.

The aircraft is owned and operated by Terraquest Ltd. under full Canadian Ministry of Transport approval and certification for specialty flying including airborne geophysical surveys. The aircraft is maintained at base operations by a regulatory AMO facility, Leggat Aviation Inc.

3.2 AIRBORNE GEOPHYSICAL EQUIPMENT

Tlie primary airborne geophysical equipment includes three high sensitivity cesium vapour magnetometers and a gamma ray spectrometer with two crystal packs. Ancillary support equipment includes a tri-axial fluxgate magnetometer, video camera, video recorder, radar altimeter, barometric altimeter. OPS receiver. OPS receiver with a real-time correction sen ice. and a navigation system. The navigation system comprises a left/right-up/dovvn indicator for the pilot and a screen showing the survey area, planned flight lines, and the real time flight path. All data were collected and stored by the data acquisition system. The following provides detailed equipment specifications:

Cesium Vapour Magnetometer Sensor (mounted in tail stinger and wing-tip pods)Model CS-2Manufacturer ScintrexResolution 0.001 nT counting at 0. l per secondSensitivity +I- 0.005 nTDynamic Range 15.000 to 100.000 nTFourth Difference 0.02 nT

Tri-Axial Fluxgate Magnetic Sensor (for compensation, mounted in midpart of tail stinger)Model MAG-03MCManufacturer Bartington Instruments LtdInput 24-34 VDC. ^0 milliampsField Range +I- 100.000 nanoteslaInternal noise at IHz to l kHz: 0.6 nT rms.Bandwidth O to l kHz maximally flat, -12 dB/octave roll off beyond l kHzFreq. Response l to 100 Hz:-H7-0.50Xo; 100 to 500 Hz:*M.50Xo: 0.5 to l kHz^7-5.00XoCalibration. Accuracy +/-0.5%Orthogonality +/-0. S'Yo worst casePackage alignment +/-0.5% over full temperature rangeScaling Error absolute^7-0.507oi between axes: +/-Q.5%

Video Camera (mounted in belly of aircraft)Model ' VDC-2982 (colour)Manufacturer SanyoSerial Number 698000-30Specifications VT, 470hr. 1.3LX. 12 VDC. C/CS. EVES, backlite compensationLens Rainbow 2/3", 4.7 mm. FI.8-360, auto iris

Video RecorderModel 16-409. 12 VDC Manufacturer Memorex Media 8mm cassette Serial Number Q28-00712

Radar AltimeterModel KRA-lOAManufacturer KingSerial Number 071-11144)0Accuracy 5y0 up to 2.500 feetCalibrate accuracy \ a7oOutput Analog for pilot, converted to digital for data acquisition

Barometric AltimeterModel LX18001ANManufacturer SensymSource coupled to aircraft barometric system

Data Acquisition/Navigation SystemModel AGIS 100Manufacturer Pico Envirotec Inc.Operating System MSDOSMicroprocessor CPU Pentium basedPorts PCMIA for data storage and retrieval, COM ports for data inputGraphic display LCF TFT colour display, sun readable touch screen controlsPilot display position, left/right, up/down, navigational infoRecording media standard hard drive, removable memory cardsSampling selectable sampling for each input type: 1.0, 0.5. 0.25, 0.2. 0.1.0.05 secondsInputs 12 differential analog input with 16 bit resolution

Magnetometer Module ProcessorModel MMP4Manufacturer Pico Envirotec Inc.Input range 20,000 - 100.000 nTSampling 1.000 per secondBandwidth selectable 0.7, l.0 or 2.0 HzResolution 0.001 nT up to 100 sample per second

Gamma Ray Detector Packages:Tlie gamma ray detector s are comprised of two packages each containing four downward looking crystals and one upward looking crystal for a total of 8 down and two up. The packages are mounted inside the aircraft cabin orientated side by side with the long axis parallel to that of the aircraft.

Model PGAM 1024/256Manufacturer Picodas Group Inc.Dimensions 51 x 34 x 71 cmWeight 99 kg (217 Ib)Processor sub-transputer spectrometerAnalogue/Digital flash ADC 10 bit/1024 channel converter on each PMTPower stable power supply on each PMTMemory on board memory for crystal calibration constantsTemperature temperature sensor in side boxCase aluminum welded with thermal insulation and shock mounts

Gamma Ray Crystals: Manufacturer

Composition Dimensions Volume PMT

Resolution

Gamma Ray Spectrometer Board ModelManufacturer Board Input ChannelsSpectral Resolution System Resolution Energy Range Count rate Calibration

Linearity Control Dead Time Pulse Pile Up Almanac File

NalAlpha Spectra

4x4x 16inches (102x102x407 mm)256 cu inches (4.2 litres)3 " long each connected to an electronics module(see spectrometer processor board. PDAS boards)typically 9*^ or better

PGAM-1000Picodas Group Inc.transputer board 3A length IBM PC plug inup to 3 detector packages each with up to 6 crystals256 down, 256 up1024 channels internal, 256 enhancedautomatically calculated and continuously monitored foe each PMT50 keV to 3 MeV, cosmic channel ^ MeV, channel width 11.7 keVup to 100,000 cpscontinuous real-time automatic gain control using natural isotope, spectrumstabilizationautomatically adjusted for each PMTabsolute zero, achieved by using flash ADC on each PMTeliminated using flash ADC on each PMTsystem status recording, archive software a) spectrometer operating software b)diagnostics test and maintenance

Spectral Monitoring allows directional sensitivity (hence this is the reason the crystals are oriented parallel to aircraft in event one wishes to measure the horizontal gradient between crystals)

The Distributed Detector Acquisition (DDA) provides each individual crystal /PMT with an Analogue/Digital converter and a high voltage power supply and transfers the serial digital via a sub-transputer in the detector package to the master transputer in the spectrometer card. Addressing each crystal as an individual spectrometer enables real-time crystal specific calibration, and provides superior performance and quality of spectral data acquisition.

The spectrometer board was housed in a separate data acquisition system a PDAS 1000 by Picodas Group Inc. The GPS signal was imported into this DAS in order to log GPS time to correlate the AGIS100 which logged the magnetic data.

GPS Differential Receiver ModelManufacturer Serial Number Channels Position update Correction Service

AG132Trimble02240-02249120.2 second for navigationReal time correction service subscription - Omnistar

3.3 BASE STATION EQUIPMENT

High sensitivity magnetic base station data was provided by a cesium vapour magnetometer sensor in conjunction a magnetometer processor board by Picodas Group Inc and a 12 channel GPS Card receiver by Novatel, both housed in a P101 portable computer manufactured by Picodas Group Inc. The time stamp is taken from the GPS receiver to ensure that it is fullv svnchronized with the airborne data.

4.0 SURVEY SPECIFICATIONS

4. l LINES AND DATA

Survey lines 740 kmTie lines 52 kmTotal Survey 792 kmSurvey Line Interval 100 metresTie Line Interval 2 kmSurvey Line Direction 000 degreesTie Line Direction 090 degreesTerrain Clearance 100 metres (mean terrain clearance)Average Ground Speed 80 metres/secondData Point Interval 8 metres

4.2 TOLERANCES

Line Spacing: Reflights will take place if the final differentially corrected flight path deviates from the intended flightpath by +/-2S metres over a distance greater than l kilometre.

Terrain Clearance: The aircraft terrain clearance will be smoothly maintained at 100 metres MTC in a drape mode.Reflights will take place if the final differentially corrected altitude deviates from the flight altitude by +/-20metres over a distance of one kilometre or more.

Diurnal Magnetic Variation: The airborne survey will be confined to periods in which the diurnal activity is 6 nT or lessover a chord of 2 minutes in length.

GPS Data: OPS data shall include at least four satellites for accurate navigation and flight path recovery. There shall beno significant gaps in any of the digital data including GPS and magnetic data.

4.3 NAVIGATION AND RECOVERY

The satellite navigation system was used to ferry to the survey sites and to survey along each line. The survey coordinates of each area outline was supplied by the client and was used to establish the survey boundaries and the flight lines.

The flight path guidance accuracy is variable depending upon the number and condition (health) of the satellites employed. The selective availability normally imposed by the military was at a minimum during this period and consequently the accuracy was for the most part better than 10 metres. Real-time correction using the Trimble receiver and Omnistar broadcast services improves the accuracy to about 3 metres or less.

A video camera recorded the ground image along the flight path. A video display screen in the cockpit enabled the operator to monitor the flight path during the survey.

4.4 OPERATIONAL LOGISTICS

The base of operations was in Thunder Bay. Ontario. The base station (combined high sensitivity magnetic and GPS) was set up at the airport well away from cultural interference.

The survey was completed over a period totaling 8 days and encompassed 5 flights including lines, tie lines, boundary lines, compensation, reflights, testing and Figure of Merit Operations were hindered severely by weather at this time of the year.

5.0 DATA PROCESSING

The data were transmitted via an FTP site to Controlled Geophysics Inc. (CGI) processing laboratory in Thornhill. Ontario, Canada where it was reviewed thoroughly for quality control and tolerances on all channels. This included any corrections to the flight path, making flight path plots, importing the base station data, creating a database on a flight by flight basis, and posting the data. All data were checked for continuity and integrity. Any errors or omission or data beyond tolerances were flagged for reflight and the crew was notified by return FTP transmission, ready for their flight in the morning.

The final processing involved tie line leveling in the standard manner by tying the survey lines to the tie lines using GEOSOFT software. The total field was gridded and microlevelled in the Fourier domain (generally less than l nT corrections) to reduce any linear noise along the flight path without degrading the geologic signal. The vertical magnetic gradient was calculated from the final processed total magnetic field gridded data. The final levelled datasets were gridded and were contoured.

Tlie final processed magnetic data were plotted as maps of total magnetic field and calculated vertical gradient. The scanned image of the topography was included with the magnetic data as an underlay. The final processed database and gridded data are archived in a CD-ROM disk.

6.0 SUMMARY

An airborne high sensitivity magnetic and radiometric survey was performed at 100 metre mean terrain clearance. 100 metre line interval. 2 kilometre tie line interval, and data sample points at 8 metres along the flight lines. A high sensitivity magnetic and a GPS base station located in Thunder Bay, Ontario recorded the diurnal magnetic activity and reference GPS data during the survey for adherence to survey tolerances and post flight corrections in the flight path. The data were subjected to final processing to produce digital files and plots with topographic underlay of total magnetic field and calculated vertical magnetic gradient. Radiometric maps include Potassium. Uranium and Thorium. All data have been archived on a CD-ROM.

Respectfully Submitted. TERRAQUEST LTD.

Charles Q. Barrie. M. Se.

APPENDIX I

PERSONNEL

Field: Pilot Serge Malle Operators Paul Beaubien

Office: Chief Geophysicist Chris Vaughan (CGI) Manager Charles Barrie

APPENDIX II

CERTIFICATE OF QUALIFICATION

I. Charles Barrie, certify that I:

1) am registered as a Fellow with the Geological Association of Canada and work professionally as a geologist.

2) hold an Honours degree in Geology from McMaster University, Canada, obtained in 1977.3) hold an M. Se. in Geology from Dalhousie University, Canada, obtained in 1980,4) am a member of the Prospectors and Developers Association of Canada,5) am a member of the Canadian Institute of Mining, Metallurgy and Petroleum,6) have worked as a geologist for over twenty five years.7) am employed by and am an owner of Terraquest Ltd., specializing in high sensitivity airborne

geophysical surveys, and8) have prepared this operations and specifications report pertaining to airborne data collected by

Terraquest Ltd..

Mississauga, Ontario, Canada Signed

Charles Q. Barrie, M. Se. Vice President, Terraquest Ltd.

Terraquest Aeromagnetic Survey B-084 January 27, 2003

Red Granite Project, Ontario Aeromagnetic Survey Geosoft Format Final Archive

The Geosoft Oasis montaj database "84MagPro" contain the following channels:

LINE Line NumberX UTM Easting Zone 16 [NAD27] Canada (Manitoba; Ontario) (m)Y UTM Northing Zone 16 [NAD27] Canada (Manitoba; Ontario) (m)FIDJT Fiducial (s)Elev Aircraft Elevation Zone 16 [NAD27] Canada (Manitoba; Ontario) (m)RMg^n^FL Raw Wingtip Sensor Total Magnetic Intensity (nT)RMg2-nT-FL Raw Wingtip Sensor Total Magnetic Intensity (nT)RMg2-nT-FL Raw Tail Sensor Total Magnetic Intensity (nT)DT Measured Transverse Horizontal Magnetic Gradient (nT/m)

(referenced across survey direction) DL Measured Longitudinal Horizontal Magnetic Gradient (nT/m)

(referenced along survey direction)DNorth-F N-S Component of Measured Transverse Horizontal Magnetic Gradient (nT/m) DEas^F E-W Component of measured Longitudinal Horizontal Magnetic Gradient (nT/m) Diurnal Base Station Diurnal TMI (nT) GTIME GPS Time (s)LONJDEG Longitude [WGS 84] World (decimal degrees) LAT.DEG Latitude [WGS 84] World (decimal degrees) GALTJvl Aircraft Elevation {WGS 84] World (m) MagSIGRF IGRF corrected Tail sensor Total Magnetic Intensity (nT) LevMagS Levelled Tail sensor Total Magnetic Intensity (nT) Mag3D1 MicroLevelled Tail sensor Total Magnetic Intensity (nT) UAL^M Raw Aircraft Radar Terrain Clearance (ft) Radm Aircraft Radar Terrain Clearance (m)

The Geosoft Oasis montaj database "84RadPro" contain the following channels:

LINE Line NumberX UTM Easting Zone 16 [NAD27] Canada (Manitoba; Ontario) (m)Y UTM Northing Zone 16 [NAD27] Canada (Manitoba; Ontario) (m)FID Fiducial (s)Elev Aircraft Elevation Zone 16 [NAD27] Canada (Manitoba; Ontario) (m)GTIME GPS Time (s)GALT Aircraft Elevation [WGS 84] World (m)LON Longitude [WGS 84] World (decimal degrees)LAT Latitude [WGS 84] World (decimal degrees)Radm Aircraft Radar Terrain Clearance (m)CTEMP Ambient Temperature (0 C)TC 256-channel Down Spectrometer (counts)UJTC 256-channel Down Spectrometer (counts)TCJRAW Raw Windowed Spectrometer Total Count (counts)

Raw Windowed Spectrometer Potassium (counts)Raw Windowed Spectrometer Thorium (counts)

Raw Windowed Spectrometer Uranium (counts) UP-U Raw Windowed Spectrometer Upward Uranium (counts) COSMICJRAW Raw Windowed Spectrometer Cosmic (counts)

TCCORR Processed Total Count (counts)THCORR Processed Apparent Thorium Concentration (ppm)UCORR Processed Apparent Uranium Concentration (ppm)KCORR Processed Apparent Potassium Concentration ("ft)THCORRD1 Micro-levelled Processed Apparent Thorium Concentration (ppm)UCORRD1 Micro-levelled Processed Apparent Uranium Concentration (ppm)KCORRD1 Micro-levelled Processed Apparent Potassium Concentration (07o)

The following Geosoft 20-m cell FLOAT grids have been supplied:

84Mag3D1 Micro-levelled TMI (nT)84VG Vertical Gradient of Levelled TMI (nT/m)84K Micro-Levelled Potassium (07o)84U Micro-Levelled Uranium eU (ppm)84Th Micro-Levelled Thorium eTh (ppm)52L.3N Scanned Topographic base map

(Where required, Geosoft color ZON files have been supplied.)

Keymap.bmp Location map

The following Geosoft MAP files have been supplied:

B084TMI 1:20,000 scale TMI Contoured Colour ImageB084TMIBW 1:20,000 scale TMI Contours with Scanned Base MapB084GRAD 1:20,000 scale HG Vectors and VG Contoured Colour ImageB084GRADBW 1:20,000 scale HG Vectors and VG Contours with Scanned Base MapB084K 1:20,000 scale Potassium Contoured Colour ImageB084U 1:20,000 scale Uranium Contoured Colour ImageB084Th 1:20,000 scale Thorium Contoured Colour Image

Chris Vaughan, President and Chief GeophysicistCGI Controlled Geophysics Inc.189 Clark Avenue EastThornhill, Ontario, CanadaL3T1T3

tel. (905) 881-2059 fax. (905)881-9517 web. cgigeo@rogers.com

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SCALE 1 : 20 DCO Contour intervalsO.l, 0.5, 2.5ppn RjO q sqo t.*.r..] tapa ispo Mpo

ROGER J CAVEN. P ENG

EAST WEST RESOURCE CORPORATIONRED GRANITE CLAIMS, PILLAR LAKE

Thunder Bay Mining Division Thunder Bay, u n tar o

S ate: Aug 20. 2003 MAP: NTSra.n bg" R J Cavin Map: NAD 27

|Rad Granite Project Winter 2004 Drill Program - Hole RG04-01Start January 20, 04 Finish February 1,04 UTM 345350E

5564000N

Footage (m) Rock Type from to

Claim

Dip Azimuth Depth

(R. Middleton) |3000998

-55 deg. 145 deg. 7.58m f 2 r f*Jr)

Alteration, Mineralization ft Structure

7.58 Boulders of Syenite 'altered porphyry'altered basement gneiss (purple banding and hematization)(specular hematite and fractures)

* Hole to be continued

Purpose of Hole: To test airborne K, U, Th anomaly and core through Pillar Volcanic layer into basement.

________* Core is slightly radioactive as seen in trenches to west of similar glacial debris._______

COt-

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ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES.J

Work Report Summary

Transaction No: W0440.00845 Status: APPROVED Recording Date: 2004-JUN-03 Work Done from: 2004-JAN-20 Approval Date: 2004-JUN-08 to: 2004-FEB-01

Client(s):

128645 EAST WEST RESOURCE CORPORATION

Survey Type(s):

AMAG ARAD PDRILL

Work Report Details:

Claim*

TB 3000993

TB 3000994

TB 3000995

TB 3000996

TB 3000997

TB 3000998

TB 3000999

TB 3001000

TB 3001001

TB 3001002

TB 3001003

TB 3011083

TB 3011084

External Credits:

Reserve:

Perform11,130

St, 126

31,130

3536

31,130

312,475

31,141

3827

3890

3792

31,005

31,130

31,130

324,442

Perform Approve

31,130

31,126

31,130

3536

31,130

512,475

31,141

3827

3890

3792

31,005

31,130

31,130

324,442

30

Applied

SO

SO

soso

36,400

S6.000

36,000

SO

SO

SO

36,000

SO

so324,400

342 Reserve of Work

342 Total Remaining

Applied Approve

SO

5030so

36,400

S6.000

56,000

soSO

3036,000

so30

524,400

Assign

31,130

51,126

51,130

5536

SO

36,433

50

5827

5890

S792

50

31,130

51,130

515,124

Assign Reserve Approve Reserve Approve Due Date

1,130

1,126

1,130

536

0

6,433

0

827

890

792

0

1,130

1,130

515,124

SO

SO

SO

SO

so542

SO

SO

SO

so503050

542

50 2004-JUN-03

SO 2004-JUN-03

50 2004-JUN-03

SO 2004-JUN-03

SO 2005-JUN-03

S42 2005-JUN-03

SO 2005-J UN-03

SO 2004-J UN-03

SO 2004-JUN-03

SO 2004-JUN-03

SO 2005-JUN-03

SO 2005-JAN-06

SO 2005-JAN-06

342

Report*: W0440.00845

Status of claim is based on information currently on record.

52I03NE2001 2.27784 PILLAR LAKE 900

2004-Jun-16 11:40 armstrongjj Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date:2004-JUN-09

Ministers du Developpement du Nord et des Mines Ontario

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

EAST WEST RESOURCE CORPORATION905 WEST RENDERAPT 402VANCOUVER, BRITISH COLUMBIAV6C 1L6 CANADA

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

Dear Sir or Madam

Submission Number: 2.27784 Transaction Number(s): W0440.00845

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.ea or by phone at (705) 670-5855.

Yours Sincerely,

Ron C. GashinskiSenior Manager, Mining Lands Section

Cc: Resident Geologist

East West Resource Corporation (Claim Holder)

Assessment File Library

East West Resource Corporation (Assessment Office)

Robert Stuart Middleton (Agent)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:19497

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Thunder Bay Mininq DivisionThunder Bay. On t a r C o

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ROGER J CAVEN, P ENGfor

EAST NEST RESOURCE CORPORATIONRED GRANITE CLAIMS, PILLAR LAKE

Thunder Bay Mini nq DivisionThunder Bay, On t a r i o

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ROGER J CAVEN, P ENGfor

EAST NEST RESOURCE CORPORATIONRED GRANITE CLAIMS, PILLAR LAKE

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