52H09SE2003 2.22514EVA

010

ASSESSMENT REPORT

GEOLOGICAL MAPPING AND SAMPLING

ON

CLAIMS:

TB1245915, TB1245916, TB1245917, TB1233078, TB1245414,TB1245415, TB1245417, TB1240302, TB1240303, TB1240304,TB1240305, TB1240306, TB1240492, TB1240493, TB1247044

EVA AND KITTO TOWNSHIPS

THUNDER BAY NORTH DISTRICT

ONTARIO

NTSLATITUDELONGITUDE

52 H 9 49033N 88008W

By

Darrel Johnson, P.Geo.

Hunter Dickinson Group Inc.

... U ' ,','Gt ASSESSMENT" " "

November 16, 2001

TABLE OF CONTENTS

SUMMARY PAGE1

INTRODUCTION and TERMS of REFERENCE 1

PROPERTY DESCRIPTION and LOCATION 1

ACCESS, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE and 2

PHYSIOGRAPHY

HISTORY 3

2001 WORK COMPLETED 3

GEOLOGICAL MAPPING 3

ROCK SAMPLING 3

GEOLOGICAL SETTING 3

REGIONAL GEOLOGY 3

SUPERIOR PROVINCE STRATIGRAPHY 4

MINERALIZATION 4

THE NORILSK MODEL 6

PROPERTY GEOLOGY 7

ROCK SAMPLING 7

INTERPRETATIONS and CONCLUSIONS 8

REFERENCES 8

STATEMENT OF COSTS 10

AUTHOR'S CERTIFICATE 11

APPENDICES

APPENDIX l Accurassay Laboratories Certificate 200140438

FIGURES

Figure 1 Location After Page 2

Figure 2 Claims 3

Figure 3 Regional Geological Setting 4

Figure 4 Property Geology 1:10,000 In Pocket

Figures Rock Sample Locations 1:10,000 In Pocket

SUMMARY

Early in 2001, Hunter Dickinson Group Inc. entered into an option agreement with East- West Resource Corporation and Maple Minerals Inc. whereby HDGI might earn a majority interest in the Eva Kitto project, Lake Nipigon area, Ontario. The geological environment and structural setting at Eva Kitto was presented as a 'cone intrusion' model, prospective for 'Noril'sk1 type Ni, Cu, PGM deposits. RAO Noril'sk Nickel operates several very large nickel, copper and platinum group metal (PGM) mines at Noril'sk and Talnakh, Siberia, with estimated annual production of approximately 51 07o of the world's palladium, about 1807o of the world's platinum and substantial tonnages of copper and nickel. During August 2001, HDGI personnel conducted geological mapping, prospecting and rock sampling on the Eva Kitto property aimed at discovery of Noril'sk style mineral deposits.

Geological mapping confirmed the presence of a layered ultramafic intrusive complex with an apparent thickness of 1.5 to 1.8 km, forming an apparent ring 10 to 12 km in diameter. The complex is emplaced into Early Precambrian (Archean) metasedimentary and mafic metavolcanic rocks. This mapping did not substantially alter previous interpretations of the geology of the area; however it improved the understanding of the lithology and orientation of the Eva Kitto intrusive complex. Preliminary, widely spaced rock sampling indicated low, generally non anomalous contents of platinum, palladium, gold, copper and nickel. This muted geochemical response in not inconsistent with the blind (ie no surface expression) nature of deposits at Noril'sk - Talnakh.

The exploration work described in this report was completed at a cost of S16,000.

INTRODUCTION and TERMS OF REFERENCE

Hunter Dickinson Group Inc. has entered into an option l joint venture agreement with with East-West Resource Corporation and Maple Minerals Inc. for the purpose of exploration of the Eva Kitto claims, Lake Nipigon, Ontario, in a search for Noril'sk style Ni, Cu, PGM mineralization.

This report describes exploration work conducted on the Eva Kitto property by J. L. Oliver, Ph.D., P.Geo. and N. W. Baker P.Eng. during August 2001. Material derived from published reports, maps or other information sources are appropriately cited in the References section of this document.

Units of measure in this report are metric; monetary units are Canadian dollars.

PROPERTY DESCRIPTION AND LOCATION

The Eva Kitto property comprises 15 Ontario staked (non patented) mineral claims, comprising 179 claim units, covering a gross area of 2,864 hectares. Claims are described in Table 1 and shown on Figure 2. Claim expiry dates shown in Table 1 are before acceptance of the assessment work credits substantiated by this report.

Table 1

Claim Number Number of unitsTB 1245915 TB 1245916 TB 1245917 TB 1233078 TB 1240302 TB 1240303 TB1240304 TB1240305 TB1240306 TB1240492 TB1240493 TB1245414 TB1245415 TB1245417 TB1247044

TOTAL

12161216161012114

121216135

12

179

Area, Hectares19225619225625616019217664

192192256208

80192

2,864

Expiry Date2003 January 222003 January 222003 January 222002 February 172002 May 242002 May 242002 June 142002 June 142002 June 142002 March 132002 March 132002 July 202002 July 202002 July 202003 May 14

Claims are jointly held by East West Resource Corp. and Maple Minerals Inc. by option from underlying vendors Don Leishman and Ken Fenwick of Thunder Bay and Lyle Holt of Beardmore Ontario.

The claims lie along the eastern side of Lake Nipigon, 155 km northeast of Thunder Bay and 15 km west of the historic gold mining town of Beardmore.

Under the terms of an agreement dated April 6, 2001, HDGI can earn a 6007o interest from East West and Maple by:

incurring exploration expenditures totaling S2 million within 5 years;making cash payments to East West and Maple totaling S48,000 within 35months of the agreement date, and;making annual cash payments totaling 578,000 to the underlying vendors, onbehalf of East West and Maple, before May 10, 2004.

The underlying vendors retain a Net Smelter Return royalty of 3*y0 , which can be reduced to 1.507o by a cash payment of Si .5 million.

ACCESS, CLIMATE, LOCAL RESOURCES, INFRASTRUCTURE AND PHYSIOGRAPHY

The Eva Kitto area is well serviced by provincial highways, secondary roads and forestry access roads. Ontario Highway 11 passes 10 km southeast of the claim block. Access to the northern portion of the property is provided by a secondary road to South High Hill Harbour on Lake Nipigon. The western portion of the claim block is boat accessible along Lake Nipigon.

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mg

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*af fiiaftir^nestjrvu '"' r-. ^ v ,l

j^rfMafiflWin^.jJixV J .

4 ( •THUNDER BAY™ff

7i? accompany assessment report 60 Km dated November 16, 2001 ^^^m^EOmOES by Darrel Johnson

FIGURE lLOCATION AND INFRASTRUCTURE

HUNTER DICKINSONINC

EVA KITTO

PLATINUM GROUP METAL PROJECT

Climate in the Lake Nipigon area is typical of much of northern Ontario. Winter extends from late October through early April, with lengthy periods of sub -100C temperatures and occasional overnight lows to -350C from December through February. Summer temperatures can reach 250C. Mineral exploration is commonly ongoing year round throughout northern Ontario, although access to swampy areas may be dependent on frozen ground.

Thunder Bay, 155 km to the Southwest of the Eva Kitto property is a modern city, population 125,000, with excellent infrastructure including railway, international airport, and seasonal deep sea shipping. All labour, contract services and specialized supplies and equipment needed to support exploration and mining operations are readily available. Basic supplies and services are available in Beardmore, population 450, located 15 km east of the property on Highway 11.

Terrain is moderately rugged. Elevations range from 258 meters at Lake Nipigon to 370 meters at the summit of one of the small rounded hills which form a range about 1 km east of the lakeshore.

Vegetation consists of scrub spruce and cedar. Much of the forest cover was destroyed by a major forest fire in 2000, resulting in thick underbrush and extensive areas of windfall which greatly increased the difficulty of traversing.

HISTORY

Although numerous gold deposits have been explored and exploited in the Beardmore area about 15 km east of the property, there is very little documentation regarding historical mineral exploration of the area currently covered by the Eva Kitto claim block .

WORK COMPLETED, 2001

GEOLOGICAL MAPPING

Geological mapping by J. L. Oliver, Ph.D, P.Geo. concentrated on the intrusive complex portion of the Eva Kitto property (Figure 4).

ROCK SAMPLING

Concurrent with the geological mapping described above, 26 rock samples were collected. Samples were submitted to Accurassay Labs of Thunder Bay , for analysis for Au, Pt, Pd, Cu, and Ni. Sample sites are shown on Figure 5 and Accurassay Certificate Number 200140438 is attached as Appendix l.

GEOLOGICAL SETTING

REGIONAL GEOLOGY

The area north of Lake Superior is dominated by an extensive package of Early Precambrian (Archean) rocks of the Superior Province. The 2 million square kilometer Superior Province is a stable, largely undeformed area of metavolcanic and metasedimentary rocks surrounded and cut by granitoid batholiths. Sediments and

volcanics of the Southern Province overlay the Superior Province. Mafic to ultramafic intrusions of two distinct ages (1 Ga and 1.8 Ga) are widespread through the region. Simplified regional geology and selected mineral occurrences are shown on Figure 3.

SUPERIOR PROVINCE STRATIGRAPHY

Traditionally, the Superior Province has been subdivided into subprovinces. These subprovinces are partially faulted bounded areas of similar rock types, structural style, metamorphic grade, geophysical characteristics and mineral deposit style. Within the Lake Superior-Lake Nipigon region, which encompasses the Eva Kitto property, three major easterly trending subprovinces have been recognized:

the Wabigoon Subprovince, which consists largely of discrete greenstone belts surrounded and cut by granitoid rocks, including the Northwind lake Batholith and the Onaman Lake Batholith;

the Quetico Subprovince, a 70 to 100 km wide linear strip of dominantly metasedimentary rocks, plus migmatitic and anatectic derivatives. The surface trace of the Quetico Fault, the northern boundary of the Subprovince, crosses the northern portion of the claim block. Granitoid intrusive rocks are of two main types; biotite- hornblende-magnetite bearing bodies of mixed mafic and felsic composition ranging in age from 2,685 to 2,690 my. and a slightly younger, (2,665 to 2,670 my) family of one-and two - mica ieucogranites and

the Wawa Subprovince which lies approximately 75 km south of the Eva Kitto claims and comprises two major greenstone belts of metamorphosed komatiite basalt, dacite and rhyolite with associated metasedimentary rocks, surrounded by extensive areas of granitoid rocks.

MINERALIZATION

Two styles of intrusive related PGM (± Ni, Cu) mineral deposits, widespread throughout the greater Thunder Bay region, have attracted exploration activity by prospectors and numerous junior and major companies.

PGM mineralization related to Archean intrusive complexes is known at several sites in the Lac des Iles area, 95 km north of Thunder Bay.

At the Lac des Iles minesite, North American Palladium is currently expanding an operating open pit mine to 15, 000 tonnes per day, and reports reserves plus resources totaling 146 million tonnes containing 7.4 million ounces of palladium. At Lac des Iles, palladium dominant mineralization occurs as disseminated sulphides (chalcopyrite, pyrrhotite and pentlandite) in pyroxenite and as disseminations and coarse interstitial blebs in a heterolithic breccia. Specific platinum group minerals include vysotskite, sperrylite, merenskyite and a palladium arsenide.

The Tib Lake, Buck Lake, Legris Lake and North Elbow Lake intrusions are being explored by several companies seeking Lac des Iles style PGM mineralization.

v Lake Superior

INTRUSIONS

INTRUSIONS

LegendARCHEAN

INTRUSIONS

PROTEROZOICLOGAN Diabase

SIBLEY Sediments

WAKINOO SUBPROVINCE

QUETICO SUBPROVINCE

WAWA SUBPROVINCE

FIGURES REGIONAL GEOLOGY

HUNTER DICKINSONINC

EVA KITTO

PLATINUM GROUP METAL PROJECT

Major zoned 1.1 b.y. mafic intrusive bodies occur in a broad arcuate zone extending 600 km northeasterly from Duluth Minnesota past the northern tip of Lake Superior to Marathon Ontario. Several large, low grade sulphide deposits have been recognized within or related to these intrusives.

Table 2

Tonnes Cu 07o Ni07o PGM (gpt)Duluth 930 million 0.32 0.085 0.4Great Lks.Ni 46 million 0.344 0.186 0.8Marathon 21 million 0.40 1.66

THE NORILS'K MODEL

Exploration work at Eva Kitto is targeted on discovery of one or more mineral deposits analogous to the giant Cu-Ni-PGM ore deposits of the Noril'sk - Talnakh region, central Siberia, Russia. Naldrett et al, (1999) states these deposits comprise the second largest economic concentration of Ni in the world, second only to the Sudbury Complex, Canada. In terms of PGM content, the district is second only to the deposits in the Bushveld complex, South Africa.

Vermaak, (1995) quotes tonnage for the Noril'sk - Talnakh district, for both disseminated and massive ores, as 770 Mt grading Q.81% Ni, 2.1 07o Cu, 1.87g7t Pt, 6.33g7t Pd Production is from 6 mines. Note that these figures include large tonnages of lower grade disseminated ores; actual massive ores, a lesser portion of the global tonnage, commonly grade over A-% Ni.

Several key features of the Noril'sk-Talnakh district have been recognized which can be applied to exploration in the general Lake Nipigon area and in particular to the Eva Kitto property.

The Noril'sk orebodies are associated with Triassic tholeiitic mafic intrusives, which were feeders or conduits for flood basalts, and served as centres of igneous activity and Cu- Ni-PGM mineralization.

Magmatic Cu-Ni-PGM deposits of the Noril'sk region are associated with the deep seated Noril'sk-Kharayelakh fault structure and all have similar geological settings and ore controls. Mafic subvolcanic intrusives migrated upward along the Noril'sk- Kharayelakh fault to penetrate the overlying Proterozoic argillaceous sediments, Devonian evaporites, Carboniferous limestones and coal.

Mineralized intrusions in the Noril'sk region are fully differentiated basal picrite overlain by picritic dolerite followed by an upper felsic phase. The intrusives are sill-like, lensoid to trough shaped in cross-section, and measure up to 12 km x 2 km x 350m in size. The magmatic sulphide orebodies reflect the assimilation of sulphur from the bounding sediments by the ascending mafic magma. Cu-Ni-PGM mineralization is developed within the sills, from the basal contact up to the picritic phase and also downward into the underlying metamorphosed country rock. PGM mineralization occurs in all ore types with highest grades developed in the high grade copper phases in the lower portion of

massive sulphide bodies and copper rich veins. Disseminated ores comprise about 7007o of total ore, massive ores about 1007o and vein ores about 1307o (Naldrett, 1999). It should be emphasized that many of the Noril'sk-Talnakh ore deposits are lacking in surface exposure.

As with the Noril'sk-Talnakh setting, the Eva Kitto ring intrusive complex was emplaced along a major deep-seated crustal break which is the locus of cyclic mafic to ultramafic plutonism.

Similarities of the Eva Kitto property to the Noril'sk-Talnakh district are summarized in Table 3.

TABLE 3

Comparison of Key Geological Features of the Noril'sk-Talnakh District and Eva KittoProperty

Noril'sk -Talnakh Eva Kitto

Structural Setting 1. Yenisey - Gulinsky 1. Mid Continent Rift2. Noril'sk-Kharayelakh fault, 2. Nipigon plate

Intrusives Tholeiitic mafic intrusives Eva Kitto Ring IntrusiveComplex

Sedimentary Rocks Argillaceous sediments, Quartzites and fine grainedevaporates, limestones, coal turbidites

Sulphur source Evaporites Iron Formation

Volcanic Rocks Flood Basalts Logan Diabase

1. Continental scale 2. Regional scale

PROPERTY GEOLOGY

The Eva Kitto property covers a 10 km by 7 km semicircular 'cone' or 'Ring' Intrusive Complex. This intrusive complex, believed to be age equivalent to the Keweenawan Supergroup, at 1.1 billion years, consists of three main units, diabase, peridotite and gabbro/granodiorite. Field observations indicate that the complex occurs as a westerly dipping sill, intrusive into Archean volcanic and sedimentary units.

Geological mapping during August 2001 by J. L. Oliver, Ph.D, P.Geo. concentrated on the Ring Intrusive Complex portion of the Eva Kitto property (Figure 4). Oliver's geological mapping confirmed the presence of the Ring Intrusive Complex and improved understanding of its composition and attitude. The exposed intrusive complex is apparently one sill-like limb of a much larger complex probably centred under Lake Nipigon. Although Oliver observed several scattered outcrops of pyroxenite, his work did not define a continuous, cohesive pyroxenite 'layer'. This lack of surface expression of such a discrete layer may result from limited outcrop exposure combined with the widespread, large scale nature of the reconnaissance mapping completed.

Oliver differentiated the following lithological units, based on field observations. No petrographic studies were undertaken.

Ring Intrusive Complex Hocks

Gd Granodiorite

Gb Gabbro

Op Peridotite (Opx)

Peridotite (Opxp)

Md Diabase

Archean Rocks

Sediments

Qa/T Argillaceous Quartzite (Qa) and Siltites (T)

Volcanics

medium grained non foliated granodiorite containing abundant, ;*1507o potassic feldspar and 1007o fine quartz

medium green weathering, non foliated gabbros. Plagioclase 30 - 5007o, clinopyroxene 4007o, olivine absent

Brown Weathering olivine rich peridotite, translucent yellow green olivine to 70^o rock volume, frequently irregular 'warty weathering' due to the presence of significant pyroxene poikiocrysts. May grade to dunitic members

Olivine rich peridotite containing 10 20 070 euhedral, cm scale, clinoyroxene poikiocrysts

Medium to coarse grained tan to light grey weathering diabase

Light grey, well bedded locally graded bedded quartzites and fine grained turbidites

Mv, Chloritized-actinolite Actinolite- chlorite ± epidote, are representative of the Mvp mafic flows (Mv), regional metamorphic field, lower greenschist

locally pillowed flow(Mvp) sequences.

Mt Mafic Tuffs Compositionally laminated, cm scale, chloriticcompositional layers and partings

ROCK SAMPLING

Concurrent with the geological mapping described above, 26 rock samples were collected. Samples were submitted to Accurassay Labs of Thunder Bay , for analysis for Au, Pt, Pd, Cu, and Ni. Sample sites are shown on Figure 5 and Accurassay Certificate Number 200140438 is attached as Appendix l.

No anomalous metal contents are immediately apparent. This apparent lack of metal associated to the Eva Kitto ring intrusive complex is not inconsistent with the 'blind' nature of many of the NoriPsk-Talnakh deposits.

DISCUSSION AND INTERPRETATION

Geological Mapping

The geological mapping described in this report provided greater understanding of the composition and orientation of the Eva Kitto intrusive complex. The Eva Kitto Ring Intrusive Complex appears to dip gently to the west-southwest, rather than the previously interpreted steep dip.

Rock Sampling

Concurrent with the geological mapping described above, 26 rock samples were collected. Samples were submitted to Accurassay Labs of Thunder Bay , for analysis for Au, Pt, Pd, Cu, and Ni. Sample sites are shown on Figure 5 and Accurassay Certificate Number 200140438 is attached as Appendix l.

No anomalous metal contents are immediately apparent. This apparent lack of metal associated to the Eva Kitto ring intrusive complex is not inconsistent with the 'blind' nature of many of the Noril'sk-Talnakh deposits.

REFERENCES

Geological Survey of Canada, 1991 Open File 2177 Regional Lake Sediment and Water Geochemical Data, Northwestern Ontario

HSBC, 2000: The Global PGM Book

Lucas S. B., St Onge M. R. 1998 Geology of the Precambrian Superior and Grenville Provinces and Precambrian Fossils in North America. Geological Survey of Canada

Mason l. M. 1991 The Norils'k Ore Field Geology and Models, A Blueprint for Canadian Exploration

Naldrett, A.J, and Lightfoot, P.C. 1999. Ni-Cu-PGE deposits of the Noril'sk Region, Siberia; their formation in conduits for flood basalt volcanism, in Keays, R.R., Lesher, C.M., Lightfoot, P.C. and C.E.G. Farrow (eds) Dynamic processes in magmatic ore deposits and their application in mineral exploration, Geological Association of Canada, Short Course Volume. 13, p.195-249

Sutcliffe R. H. 1991 Proterozoic Geology of the Lake Superior Area, in Geology of Ontario, Ontario Geological Survey Special Volume 4, pages 627 to 658

Sutcliffe R. H. 1986 Regional Geology of the Lac des Iles Area, District of Thunder Bay Summary of Field Work and Other Miscellaneous Activities 1986, Ontario Geological Survey Miscellaneous Paper 132

Sutcliffe R. H. and Greenwood R. C. 1985. Precambrian Geology Lake Nipigon Area, Livingstone Point Sheet, Thunder Bay Area, Ontario Geological Survey Map P2839

Vermaak C. F. 1995: The Platinum-Group Metals Mintek

ITEM

Geological Wages

Geological consultant fees

Graphics

Transportation

Assays

Base Map

Statement Of Costs

DETAILS

N. W. Baker, field,

D. L. Johnson, report prep

J. L. Oliver

Wages

Supplies

Field Supplies

Communications Courier

Telephone S Fax

Living expenses Accomodations

Meals etc.

Vehicle rental and fuel

Commercial Air

Boat charter

Accurassay Labs #

200140438

Digimap # DM 5887

5,000.00

4,000.00

1150.00

65.00

224.00

65.00

55.00

1597.00

485.00

548.00

1148.00

243.00

568.71

856.00

TOTAL

9,000.00

1,215.00

224.00

120.00

2,082.00

TOTAL

1,939.00

568.71

856.00

316,004.71

10

12.0 STATEMENT OF QUALIFICATIONS

l, Darrel L. Johnson, of the City of Coquitlam, British Columbia, DO HEREBY CERTIFY THAT:

l am an employee of Hunter Dickinson Group Inc. with a business address at 1020 - 800 West Render Street, Vancouver British Columbia,

l am member of the Association of Professional Engineers and Geoscientists of British Columbia,

l am a graduate of the University of British Columbia with a Bachelor of Science degree in Geology, received in 1970,

l have practiced my profession continuously since 1970,

l prepared this report based on discussions with Nelson Baker P.Eng and J. L. Oliver, Ph.D, P. Geo, and study of their field notes, photographs and field sketches made during August 2001. l have not visited the Eva Kitto property..

Dated at Vancouver British Columbia, this 16th day of November, 2001.

Darrel L. Johnson, B.Sc., P.Geo.

11

APPENDIX l

Accurassay Laboratories Certificate 200140438

ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.

1070 LITHIUM DRIVE, UNIT 2 THUNDER BAY, ONTARIO P7B 6G3

Certificate of Analysis PH?5!i KTuesday, August 21, 2001

Hunter Dickenson Inc.1020-800 West FenderVancouver, BC, CAV6C2V6

St.Date Received : 15-Aug-Ol

Date Completed : 21-Aug-OlJob #200140438

Reference :

F y#- rfifui 667 89S6 -~~ ' Sample #: 26 RockEmail nbaker@hdgold.com, davidj@hdgold.com C^V/'O*"" \N^\ l \ f-J

Accurassay #

11916

11917

11918

11919

11920

11921

11922

11923

11924

11925

11926 Check

11927

11928

11929

11930

11931

11932

11933

11934

11935

11936 Check

11937

11938

11939

Au Pt PdClientld ppb ppb ppb197959 <5 <15 <10

197960 <5 23 <10

197961 <5 <15 <10

197962 <5 -s 15 ^0

197963 <5 <15 *:10

197964 <5 25 22

197965 <5 <15 <10

197966 <S 17 <10

197967 <5 -05 < 10

197968 <5 <15 -s 10

197968 <5 <15 <10

197969 5 28 < 10

197970 <5 <15 14

197971 <5 *:15 <10

197972 <5 <15 *:10

197973 <5 18 10

197974 <5 <15 20

197975 <S <15 <10

197976 <5 16 00

197977 <5 <15 < 10

197977 <5 <15 <10

197978 <5 <15 15

197979 ^ <15 <10

197980 50 *:15 13

Rh Ag Co Cu Feppb ppm ppm ppm ppm

43

34

66

103

25

180

4

127

30

11

13

102

132

33

30

42

121

47

41

18

19

137

33

106

Nippm

751

673

961

448

479

49

137

58

990

210

217

90

74

396

718

864

146

843

642

943

994

135

954

95

PROCEDURE-CODES: AL4APP, AL4Cu, AL.4NJ l""\^^ ^ .

Certified By^-OJPTX^ ^J^

Pb Znppm ppm

Page 1 of 2

AL917-0206-08/21/2001 04-.42 PM

ACCURASSAY LABORATORIESA DIVISION OF ASSAY LABORATORY SERVICES INC.

Tuesday, August 21, 2001

Certificate of Analysis1070 LITHIUM DRIVE, UNIT 2

THUNDER BAY, ONTARIO P7B 6G3 PHONE (807) 623-6448

FAX (807) 623-6820

Hunter Dickenson Inc.1020-800 West Fender St.Vancouver, BC, CAV6C2V6Ph#: (604) 684-6365Fax* (604)662-8956Email nbaker@hdgold.com, davidj@hdgold.com

Date Received : 15-Aug-Ol Date Completed : 21-Aug-Ol

Job #200140438 Reference :

Sample #: 26 Rock

Accurassay #

11948

11949

11950

11951

Client Id

197953/54

197955/56

197957

197958

Au Pt Pd Rh Ag Co Cu Fe Ni Pb Znppb ppb ppb ppb ppm ppm ppm ppm ppm ppm ppm8 16 -c 10 51 60

12 93

<5 30

<5 19

•c 10

-c 10

36

39

17

63

591

259

PROCEDUR^CODES: AL4APP, AL4Cu, AL4Ni

Certified By:,AL917-0206-08/21/2001 04:42 PM

Page 2 of 2

MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Work Report Summary

Transaction No: W0140.31178 Status: APPROVED Recording Date: 2001-DEC-04 Work Done from: 2001-AUG-10 Approval Date: 2002-JAN-03 to: 2001-AUG-16

Client(s):

128645 EAST WEST RESOURCE CORPORATION

137052 MAPLE MINERALS INC.

145589 HOLT, LYLE HENRY

3001 18 FENWICK, KENNETH GEORGE

303544 FENWICK, MARILYN CHRISTOPHER

Survey Type(s):

ASSAY GEOL

Work Report Details:

Claim*

TB

TB

TB

TB

TB

TB

TB

TB

TB

TB

TB

TB

TB

TB

TB

1233078

1240302

1240303

1240304

1240305

1240306

1240492

1240493

1245414

1245415

1245417

1245915

1245916

1245917

1247044

Perform

31,400

S1.400

S900

S1,080

S1,000

3400

31,080

31,080

S1.400

31,120

3500

31,080

31,400

31,080

31,080

316,000

Perform Approve

31,40031,400

390031,08031,000

340031,08031,08031,40031,120

350031,08031,40051,08031,080

316,000

Applied36,400

30

30SO

SOSO

34,800

SO54,800

SO50

30

SO

SOSO

316,000

Applied Approve

56,400

SOSO

SOSO

SO34,800

3034,800

SOSO

SOSO

SO

so316,000

Assign

5051,400

5900

51,080

51,000

S400

SO

51,080

SO

51,120

5500

51,080

31,400

31,080

31,080

512,120

Assign Reserve Approve Reserve Approve

1

1

1

1

1

1

1

11

512

0

,400900

,080,000

400

0,080

0,120

500

,080,400

,080

,080

,120

SO

SOSOSO

SO

SOSO

so505030soSOSO

soso

so30SO

sososoSO

so50

5050soso30

SO

so

Due Date

2003-FEB-17

2002-MAY-24

2002-MAY-24

2002-JUN-14

2002-JUN-14

2002-JUN-14

2003-MAR-1 3

2002-MAR-13

2002-JUL-20

2002-JUL-20

2002-JUL-20

2003-JAN-22

2003-JAN-22

2003-JAN-22

2003-MAY-14

Status of claim is based on information currently on record.

52H09SE2003 2.22514 EVA900

2002-Jan-07 22:08 Armstrong-d Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date: 2002-JAN-08

Ministers du Developpement du Nord et des Mines Ontario

GEOSCIENCE ASSESSMENT OFFICE 933 RAMSEY LAKE ROAD, 6th FLOOR SUDBURY, ONTARIO P3E6B5

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

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

Dear Sir or Madam

Submission Number: 2.22514 Transaction Number(s): W0140.31178

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 GashinskiSupervisor, Geoscience Assessment Office

Cc: Resident Geologist

East West Resource Corporation (Claim Holder)Maple Minerals Inc. (Claim Holder)Kenneth George Fenwick (Claim Holder)

Assessment File Library

East West Resource Corporation (Assessment Office)Lyle Henry Holt (Claim Holder)Marilyn Christopher Fenwick (Claim Holder)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:16730

oVO

la nto o o

to toUI

to oO

Dale l Time of Issue Jan 2 2002

TOWNSHIP/AREA

MARYJANE LAKE AREA

MINING LAND TENURE

MAP

13:42h Eastern

PLAN

G-0080

ADMINISTRATIVE DISTRICTS / DIVISIONSMining DMtlon Thunder Bay

Lend Tittas/Sugistry Division THUNDER BAY

Ministry ol Natural Resources District NIPIGON

TOPOGRAPHIC

' j-jr.-s}?

g I'll" In c"!™*.

LAND TENURE

Q v,w.-..-

E] ...*..*.,. I

nih*wn on Wft mi* h MiipUwJ from v*r*iu* MKIGeneral Information and LimitationsCortJcllifoiniBdim:

' Once ta*.n** Hff BaluTfi HW) 81 Ciil|Kl*ori: LJlMiQ ilpnii Tupagraprik: D flirt SULULJ Hln'iia t 01.4 ff-PMifl ^ui

Q Qa

0ED

LAND TENURE WITHDRAWALS

f *^f l * rH" W^'^Wi '""to ffriwiHiHi t""""*t*"* tnirwni JtctwmiitiMt lypw*

rf,l IMPORTANT NOTICES

: LAND.TENURE WITHDRAWAL DESCRIPTIONS

Jia l Ml DA l-T HtEtKVt F HOU 1MH COH1OUH lUH.t.fJ.t.

H 0.2 i MOI M l iliif md hirf*.l i luhta ^*dr*.pl ttclkin M al IM N

v W.ii .3 ac* f i CUT How. Jt, Jdm MMI: mis nnumvy i

m* m h Ing piGpbM

NW J i juoi Minig ma turfm i

K WU-2H1AI ON!

Ih* W ttl^u tiapou

KMr^l .1*11 IMrlt HMI tMrlKB (

li* NHh#*Ml t*cl* i X Di IMMirrill AM FISU tSW gi0H

n.ZI.ZDDi Mo l*. (rihb*imdBlXUink(ffi*Hntt{hi VH

H. Zt.2dlMHahg diHtHuMl vy ctai* rpf mnti HH HH

Til iKiiMlbn tra rnur It nibtaUu rMr1h*i thai)*.

IMPORTANT NOTICESAipM Midt, r q4i^ ••KJAl iRf uUnni. Imt

Mpirg mq miriril m**pifi*ii flftfi"'*!

EVA KITTO RING COMLPEX

Claim Diabase. Medium to coarse grained, tan to light grey weathering .Peridotite (OPxJ. Brown weathering olivine-rich peridotites, translucent yellow-green olivine to 70"7o rock volume. Frequently irregular "warty weathering", due to the presence of significant pyroxene poikiocrysts, May grade to dunitic membersBoundary Peridotite (Opxp). Olivine-rich peridotites containing ID-20% euhedral, cm scale, clinopyroxene phenocrysts.

Gabbro. Medium green weathering, non-foliated gabbros. Plagioclase 30-5007o, clinopyroxene 400Xo, olivine absent.

Granodiorite. Medium grained, non-foliated granodiorites, containing abundant, s-15% potassic feldspars and fine quartz.

l 7 J Argillaceous Quartzites (Qa) and Siltites (T). Light grey, wellbedded, locallv graded bedded quartzites, and fine grained turbidites

Chloritized-actinolitic mafic flows (Mv) and locallv pillowed Flow (Mvp) sequences. Actinolite - chlorite -t-/- epidote are representative of the regional metamorphic field, lower greenschist

1240492

l ~ ~| Mafic Tuffs. Compositionally laminated, cm scale, chloritic compositional layers and partings.VA'

SYMBOLS AND ABBREVIATIONS

Joint surface as dip direction

SI Foliation as dip direction

SO Bedding orientation as dip direction; overturned

Orientation of shear plane as dip direction

Orientation of talc-serpentine vein as dip direction

Outcrop with station number

Small, point source outcrop

Navigational or traverse conotrol point, no geological information.

Claim post.

"r" is a modifier to the rock code indicating boulders or rubble, not inplace outcrop

Fault trace, no movement inferred. Fault trace with ball on the downthrown block.

(1) Stations O-l to O-30 have reduced toporaphic and location control.

(2) Contacts external to the main intrusive system are modified front the work of Shanks, OGS open file KS821

1240304

1210732

f 1245417

1240302

1240303

Limit, of Mapping12459,115

HUNTER DICKIN SON INCEva Kitto Ring Comple

Property Geology1000mSea e: 1:10000 Datum: NAD 27, Zone 16 Date: Nov. 15, 2001

Drawn by: Jim Oliver Plotted by: S Parker Figure: 4Limit of Mapping

52H09SE2003 2.22514 EVA 210

EVA KITTO RING COMLPEX LEGEND

Claim Diabase. Medium to coarse grained, tan to light grey weathering

Peridotite (OPx). Brown weathering olivine-rich peridotites, translucent yellow-green olivine to IQ^/o rock volume. Frequently irregular "warty weathering", due to the presence of significant p}ioxene poikiocrysts. May grade to dunitic members

Boundary Peridotite (Opxp). Olivine-rich peridotiles containing lu-20% euhedral, cm scale, clinopyroxene phenocrysts.

Gabbro. Medium green weathering, non-tohated gabbros, Plagioclase 30-5007o, clinopyroxene 4007o, olivine absent.

[ J Granodiorite, Medium grained, non-foliated granodiontes, containing abundant, M507o potassic feldspars and 10"Xo fine quartz.

Argillaceous Quartzites (Qa) and Siltites (T). Light grey, well bedded, locally graded bedded quartzites, and fine grained turbidites

Chloritized-actinolitic mafic flows (Mv) and locally pillowed Flow (Mvp) sequences. Actinolite - chlorite +I- epidote are representative of the regional metamorphic field, lower greenschist.1240492

Mafic Tuffs. Compositional^ laminated, cm scale, chloritic compositional layers and partings.

SYMBOLS AND ABBREVIATIONS

Joint surface as dip direction

SI Foliation as dip direction

SO Bedding orientation as dip direction; overturned

Orientation of shear plane as dip direction

Orientation of tak-serpentine vein as dip direction

Outcrop with station number

Small, point source outcrop

Navigational or traverse conotrol point, no geological information.

Claim post.

"r" is a modifier to the rock code indicating boulders or rubble, not inplace outcrop

Fault trace, no movement inferred. Fault trace with ball on the downthrown block.

(l) Stations O-l to O-30 have reduced toporaphic and location control.

(2) Contacts external to the main intrusive system are modified from the work of Shanks, OGS open file #5821

#2330/7/8

1210732

1245417

Lions Bay

Limit of Mapping

HUNTER DICKINSON INCEva Kitto Ring Comple

Lithogeochemistry1000mDatum: NAD 27, Zone 16 Date: Nov. 15, 2001Scale: 1:10000

Figure: 5Plotted by: S ParkerDrawn by: Jim OliverLimit of Mapping

52H09SE2003 2.22514 EVA 220