SUMMARY RPT BIRCH-UCHI PROJ - Geology Ontario

SUMMARY REPORTon the

2003 SUMMER FIELD PROGRAMBIRCH-UCHI PROJECTRED LAKE DISTRICT

prepared for

JILBEY GOLD EXPLORATION LTD.

Report # 857

A.C.A. Howe International Limited Toronto, Ontario, Canada

Felix Lee, B.Sc., P.Geo.

Effective Date: October 31,2003

RECEIVEDAPR U b 2004

GEOSCIENCE ASSESSMENT OFFICE

52N08NE2003 2.27483 KEIGAT LAKE 010

TABLE OF CONTENTS

SUMMARY ...................................................................................................................^^

1.0 INTRODUCTION AND TERMS OF REFERENCE ........................................................l1.1 General..........................................................................................................................!1.2 Scope and Conduct....................................................................................................... l1.3 Units and Currency .......................................................................................................l

2.0 PROJECT LOCATION, ACCESS, DESCRIPTION AND PHYSIOGRAPHY ..............22.1 Project Area Location And Access...............................................................................22.2 Project Claim Descriptions And Status.........................................................................32.3 Project Area Physiography, Vegetation fc Climate......................................................3

3.0 GEOLOGICAL SETTING ....................................................................................................43.1 Uchi Subprovince..........................................................................................................4

3.1.1 Volcanic Sequences..........................................................................................53.1.2 Sedimentary Sequences ....................................................................................63.1.3 Igneous & Metamorphic Events.......................................................................6

4.0 EXPLORATION HISTORY .................................................................................................8

5.0 2003 SUMMER FIELD PROGRAM ..................................................................................105.1 Overview..................................................................................................................... l O

5.1.1 Evaluation of Targets for Kimberlite Potential............................................... l O5.1.2 Other Targets .........................................................^..........i)...^'.^.:^.

5.2 Sampling & Survey Overview and Methodology..............^.....^...fr'......... ..t:. x...I5.2.1 Mobile Metal Ion (MMI) Sampling................................................................155.2.2 Ground Magnetics...........................................................................................165.2.3 Till Sampling..................................................................................................175.2.4 Notes on Navigation and Establishment of Location.....................................175.2.5 Logistics.......................................................................................................... 18

6.0 SUMMARY OF RESULTS .................................................................................................196.1 MMI 8i Ground Magnetic Results by Anomaly.........................................................19

6.1.1 MMI-B Soil Results........................................................................................ 196.1.2 MMI-B Lake SedimentResults......................................................................236.1.3 MMI-D"DeBeers"SoilResults.....................................................................236.1.4 MMI-D "DeBeers" Lake Sediment Results....................................................236.1.5 Interpretation of Ground Magnetic Data.........................................................24

6.2 Rock & Soil Sample Results.......................................................................................246.2.1 Shabumeni Lake East Zone ............................................................................24

6.3 Till Sample Results.....................................................................................................27

7.0 CONCLUSIONS AND RECOMMENDATIONS..............................................................29

A.C.A. HOWE INTERNATIONAL LIMITED Report No. 857 October 31, 2003

SOURCES OF INFORMATION

CERTIFICATE

FIGURES2.1 Location of the Birch-Uchi Project, NW Ontario.........................................................23. l Distribution of Supracrustal (Greenstone) Belts within the Uchi Subprovince .........A3.2 Stratigraphic Correlation of the Volcanic Cycles across the Red Lake & Birch-

Uchi Belts.................................................................................................................... 53.3 Regional Geology, N.E. Birch-Uchi Belt .....................................................................75.1 Use of the OGS Sampler.............................................................................................165.2 Example Ground Magnetics andMMI Soil/Lake Sediment Survey ..........................16

TABLES4. l Historical Gold Production of the Red Lake District as of December 31, 2001 .......... 85.1 Birch-Uchi Project: Airborne Magnetic & E.M. Anomalies......................................116. l Calculated 25 Percentiles and Backgrounds for Soils and Lake Sediments fc

MMI-B and MMI-D Response Ratios for Soils and Lake Sediments......................206.2 MMI-B and MMI-D Anomalies.................................................................................216.3 Evaluated Airborne Magnetic *fe E.M. Anomalies......................................................256.4 Rock Sample Locations and Analytical Results.........................................................266.5 East Zone Soil Sample Locations and Analytical Results..........................................28

PLATES6. l Exposed Quartz Vein in Pit Wall at the Main Zone, Shabumeni Lake East Zone .....24

APPENDICESA: List of Claims 8i StatusB: Target Anomaly Maps: Ground Magnetics and MMI Sample Locations C: Analytical Certificates, SGS LaboratoriesD: Overburden Drilling Management Limited, Till Sample Analysis fc Standard

Processing Flow Sheet for Gold Grains & KIM Indicators

POCKETMap A: 2003 Summer Field Program Work, Compilation Map

A.C.A. HOWE INTERNATIONAL LIMITED Report No 857 October 31, 2003

SUMMARY

At the request of Mr. Gregory P. Isenor, President of Jilbey Gold Exploration Ltd ("Jilbey"), A.C.A. Howe International Limited ("Howe") prepared and carried out a summer exploration program between May 28 and September 21, 2003 on the company's Birch-Uchi Project in the Red Lake-Birch Lake area, Red Lake Mining District in north western Ontario.

This report summarizes the results of the 2003 Summer Field Program that consisted of ground magnetic surveys, Mobile Metal Ion ("MMI") soil geochemical sampling surveys directed at 170 airborne magnetic and EM anomalies targeted for ground investigation. In addition regional till sampling was completed. Of the 170 anomalies across the Project area identified for ground investigation, 37 were evaluated during the 2003 summer program. The program yielded 374 MMI samples, 74 rock samples, 15 soil and 15 till samples.

The Birch-Uchi Project is composed of numerous properties that are held 100*M) by Jilbey Gold Exploration Ltd. The Jilbey owned claim blocks are located throughout the Birch-Uchi greenstone belt, including the Birch Lake, Shabumeni Lake, Bathurst Lake, and Woman-Uchi- Confederation Lake areas. The Project area hosts several past producing gold, silver, and copper mines and workings that date back to the early 1900s and Jilbey's claim blocks are strategically positioned to cover historic gold occurrences, regional deformation zones, and individual target anomalies representing possible intrusions of kimberlite. The adjacent Red Lake greenstone belt is host to some of the most prolific and lowest cost gold mines in the world. Gold deposits such as the Placer Dome's Campbell Mine and GoldCorp's Red Lake Mine (formerly the Dickenson Mine) have produced over 23 million ounces (500 tonnes) of gold since the early 1940's. Geologically, gold mineralization within the Red Lake Belt is controlled by large, regional-scale, deformation zones, a fact that has guided gold explorations efforts throughout the Red Lake greenstone belt as well as the adjacent Birch-Uchi Belt.

Based on the current understanding of the tectonic evolution of the Birch-Uchi and Red Lake greenstone belts and the Uchi Subprovince in general, there is evidence to suggest that the region has the potential to host primary diamond deposits (kimberlite). As yet, no systematic exploration for diamond occurrences has been conducted within the region.

Jilbey identified 170 high priority geophysical target anomalies (magnetic and coincident magnetic-EM anomalies) representing possible kimberlite intrusions within the Birch-Uchi Belt after a comprehensive review of existing geological data for the region and a re-analysis of digital airborne geophysical survey data obtained from the Ontario government. Claims were staked to protect these targets.

The target anomalies were prioritized (A-D) for evaluation by ground magnetics, soil/lake sediment geochemical sampling, and visual inspection of outcrop if possible. Ground magnetics was employed to better pinpoint and delineate the airborne magnetic anomaly(ies) on the ground. Soil/lake sediment geochemical sampling utilized a relatively new geochemical analytical process known as Mobile Metal Ion ("MMI") that is effective in identifying gold, base metal and nickel mineralization and kimberlite intrusives hidden beneath unrelated overburden such as till, lake sediment or soil.

A .C.A. HOWE INTERNATIONAL LIMITED Report No. 857 October 31, 2003

Airborne magnetic anomalies within Gold Canyon Resources Inc.'s "Springpole Property" in the Birch Lake-Springpole Lake area (Round Pond and Long Skinny Pond) were also evaluated for kimberlite potential via ground magnetics and MM sampling

The MMI and ground magnetic surveys of the 2003 Summer Field Program appears to have confirmed the prospectivity for kimberlite in several of the targeted anomalies. On this basis Howe recommends the following be completed during the upcoming winter and summer field seasons:

* Diamond drilling of prospective targets. The winter months should provide the best opportunity to accomplish this work since a diamond drill can easily be moved around via the lakes. One hole per anomaly should quickly and definitively evaluate the anomaly as kimberlitic or not;

* Continued evaluation of target anomalies via ground magnetics and MMI analysis. Over half the targeted anomalies remain untested. Howe recommends a review of the remaining targets to determine which ones can best be evaluated during the winter season. Anomalies situated within lakes or ponds can still be evaluated during the winter using the OGS sampler to collect lake sediment samples for MMt analysis.

Jilbey also evaluated several old gold occurrences along the southeast shore of Shabumeni Lake that were identified from government assessment reports and collectively known as the East Zone. The workings of five occurrences were located and exposed and representative rock samples collected from four of the five occurrences. On the basis of favourable assay results obtained from the rock samples further work is recommended for the East Zone. It is possible that the occurrences are indicative of a larger mineralized system and Howe suggests a program of stripping, geological mapping, trenching and sampling be completed during the upcoming winter months in order to delineate the strike and dip extensions of the known occurrences and to identify other nearby veins or zones of mineralization or alteration. The winter months will provide the best opportunity to accomplish this work since heavy machinery such as a backhoe can be efficiently moved into the area over land and lake.


.^ *w " i-"* Q1.0 INTRODUCTION o */ '{ . ^ O' *-*

1.1 GENERAL

At the request of Mr. Gregory P. Isenor, President of Jilbey Gold Exploration Ltd ("Jilbey"), A.C.A. Howe International Limited ("Howe") prepared and carried out a summer exploration program consisting of geochemical and geophysical surveys on the company's Birch-Uchi Project in the Red Lake-Birch Lake area, Red Lake Mining District in north western Ontario.

This report summarizes the results of the 2003 Summer Field Program conducted between May 28 and September 21, 2003, that consisted of ground magnetic surveys, MMI soil geochemical sampling over targeted airborne magnetic and EM anomalies and regional till sampling.

The Birch-Uchi Project consists of numerous properties, strategically located throughout the Birch-Uchi greenstone belt, that are held 100% by Jilbey Enterprises Inc. Jilbey is a public resource exploration company that was incorporated in the province of British Columbia in 1983. Jilbey's corporate head office is located at 155 University Avenue, Suite 1710, Toronto, Ontario, Canada M5H 3B7. The company is currently listed on the TSX Venture Stock Exchange. At present Jilbey holds various interests in diamond and precious-base metals exploration projects in Canada and Africa.

Howe is an international geological and mining consulting firm that was incorporated in the province of Ontario in 1966 and has continuously operated under a "Certificate of Authorization" to practice as Professional Engineers (Ontario) since 1970. Howe provides a wide range of geological and mining consulting services to the international mining industry, including geological evaluation and valuation reports on mineral properties. The firm's services are provided through offices in Toronto, Canada, and London, U.K.

1.2 SCOPE AND CONDUCT

This summary report was prepared by Mr. Felix Lee, B.Se., P.Geo., an Associate Consulting Geologist with Howe. Mr. Lee has over 15 years experience in the mining industry including a background in international precious metals mineral exploration including project management, evaluation and valuation experience.

In preparing this report Howe reviewed geological reports, maps, miscellaneous technical papers, and other public as listed in Section 9.0 "Sources of Information" of this Report.

1.3 UNITS AND CURRENCY

Unless otherwise stated, all units used in this report are metric. Standard abbreviations are used, such as silver (Ag), and gold (Au), metre (m), kilometre (km). Grades of silver and gold are expressed in grams of gold per metric tonne (g Au/t, g Ag/t) or parts per billion (ppb). All currency is expressed in Canadian dollars (SC) unless otherwise stated.

A.C.A HOWE INTERNATIONAL LIMITED Report No. 857 October 31, 2003

2.0 PROJECT LOCATION, ACCESS, DESCRIPTION AND PHYSIOGRAPHY

2.1 PROJECT AREA LOCATION AND ACCESS

Jilbey's Birch-Uchi Project encompasses an area of over 180 square kilometres and is situated within the northeastern portion of the Archean Birch-Uchi greenstone belt in northwestern Ontario. The Project area lies approximately 50-80 km east-northeast of Ear Falls and 75-150 km east of the town of Red Lake (see Figure 2. l).

Several separate claim blocks comprise the Birch-Uchi Project. These can be reached by either boat from along the South Bay Road originating out of Ear Falls, or by float plane out of the Ear Falls area. Red Lake, or Pickle Lake. Several long established and well equipped, fishing/hunting lodges operate throughout the Project area during the summer months and can provide both boat and accommodation as required. Numerous floatplane operators can be found in the Ear Falls and Red Lake areas, offering Cessna, Beaver, Norseman and Single Otter planes. A network of secondary logging roads may also be relied upon to provide access to parts of the Project area.

Fi jure 2. l Location of the Birch-Uchi Project, NW Ontario^^^ ^^^^^^^^ ^^^ ^^^^^^^^^

The proximity of the Project area to the communities of Red Lake and Ear Falls ensures good access to ancillary services such as ground transportation, mail A courier services etc. All necessary supplies can be obtained locally or from Winnipeg, Kenora and Thunder Bay.

Red Lake and Ear Falls can be reached by taking Highway 105 northwards from the town of Vermillion Bay situated along the Trans-Canada Highway (Highway 17), which passes E-W between Winnipeg and Thunder Bay south of Red Lake and Ear Falls. Red Lake is also serviced by regular scheduled air flights from Winnipeg and Thunder Bay.

A C. A. HOWE INTERNATIONAL LIMITED Report No. 857 October 31, 2003

2.2 PROJECT CLAIM DESCRIPTIONS AND STATUS

The Birch-Uchi Project consists of 85 claim blocks containing 1,037 individual mining claims covering approximately 44,200 acres or 178.8 square kilometres (see Map A, in pocket). All the claims are unpatented and 100070 held by Jilbey. Claims have not been surveyed. Appendix A provides a list of the claims comprising the Project and relevant claim information.

The Project area hosts several past producing gold, silver, and copper mines plus workings dating back to the early 1900s. Jilbey's claim blocks are positioned to cover historic gold occurrences, regional deformation zones, and individual target anomalies representing possible intrusions of kimberlite. Since the Birch-Uchi Project area is quite considerable, the claims have been grouped into four geographic areas for ease of reference. These are the Birch Lake, Shabumeni Lake, Bathurst Lake, and Woman-Uchi-Confederation Lake areas.

2.3 PROJECT AREA PHYSIOGRAPHY, VEGETATION A CLIMATE

The Project area is generally flat and characterized by swamps and low rolling hills with elevations ranging from 360 to 400 m above sea level. A thin veneer of glacial clay and till covers much of the area and outcrop is generally scarce. This overburden generally ranges from 0.5 to 15 m in thickness.

Vegetation in the Project area is controlled by both lithological and glacial factors. Glacial ridges (topographic highs) generally support hardwood growth- typically birch and poplars, while topographically lower, boggy, ground supports spruce, tamarack and alder growth. Parts of the Project area, particularly those adjacent to Hwy 105, are actively being logged and have been clear-cut, leading to excellent access.

The climate in the Red Lake area is characterized by extremes in temperature and can range from -400C in winter to 4-3 00C in the summer. Precipitation ranges from a low of 30 cm in December to a high of 90 cm during the months of June and July. Total precipitation averages 60 cm with an average total snowfall of 150-200 cm.


3.0 GEOLOGICAL SETTING

The Birch-Uchi Project is situated in the north eastern portion of the Birch-Uchi greenstone belt within the Uchi Subprovince of the Archean Superior Province (see Figure 3.1). In addition to the Birch-Uch Belt, the Uchi Subprovince also includes the NE-trending Red Lake, where the bulk of the exploration and mining activity in the region has taken place.

Figure 3. l Distribution of Supracrustal (Greenstone) Belts within the Uchi Subprovince______________

SACHIGO

BERENS —^r Preiectftrea k Btrch-Uchl

from Ontario Geo l. Survey Misc. Paper 129 Volcanology SL Mineral Deposits, 1986

3.1 UCHI SUBPROVINCE

The Red Lake and Birch-Uchi greenstone bells are similar to other Archean granite-greenstone terrains found throughout the world, consisting primarily of east-west belts of basic to felsic volcanic rocks, sedimentary rocks and syn-volcanic intrusives. The belts are bounded on all sides by granitic gneiss terrain or granitoid batholithic masses. The belt has been dated at 2.75 to 2.73 Ga (billion years). The Ontario Resident Geologist's report of 1991 (OGS 1991) describes the regional geology of the area as follows:

The belts are, "composed of mafic, intermediate and felsic, metavolcanic flows and volcaniclastic pyroclastic rocks with subordinate melasedimentary rocks.

The south and south western margins of the belt consist of linear units of metavolcanic rocks alternating with thick sequences of clastic metasedimentary rocks."

The metavolcanic-metasedimentary assemblage has been intruded by large, composite, granitoid complexes and by smaller, late, mafic to felsic stocks, plugs, dikes and sills.

Supracrustal rocks are commonly metamorphosed to green-schist grade assemblages over wide areas while amphibolite grade rocks are more locally concentrated within the contact aureoles of the large granitic batholiths and smaller intrusions."

AC A HOWE INTERNATIONAL LIMBED Report No. 857 October 31. 2003

3.1.1 Volcanic Sequences

The Uchi Subprovince volcanics are divided into assemblages- thought to represent three complete volcanic cycles (see Figure 3.2). From oldest to youngest, the assemblages and cycles are: the Balmer and Ball Assemblages at 2.900 to 3,000 Ma (Cycle I), the Bruce Channel and Woman Assemblages at 2,800 lo 2.900 Ma (Cycle II), the Confederation Assemblage at 2,730 to 2,800 Ma (Cycle III).

* The Balmer Assemblage rocks form the core of the Red Lake & Birch-Uchi greenstone belts and are host the large and prolific Campbell and Red Lake (Dickenson) gold mines. The Balmer consists of basaltic tholeiite and komatiite flows with intercalated magnetite-quart/ iron formation. Felsic pyroclastic rocks occur as comparitively thin units Small mafic to ultramafic intrusives cut all the asemblages.

The Ball Assemblage is slightly younger than the Balmer and is composed of calc- alkalic mafic flows and intermediate to felsic calc-alkalic flows and tuffs. Well preserved stromatolite dolomitic carbonate rocks are found in the upper part of the Ball Assemblage in Ball and Todd Townships.

* The Bruce Channel and Woman Assemblage rocks are composed of basaltic flows capped by minor felsic pyroclastic rocks with a common age of 2894 Ma and clastic and iron formation melasediments.

* The Confederation Assemblage is predominantly ca!k-alkalic with substantial amounts of felsic pyroclastic deposits that can be correlated stratigraphically with similar rocks in the Birch-Uchi greenstone bell.

Figure 3.2 Stratigraphic Correlation of the Volcanic Cycles across the Red lâke Si, Rirch-Uchi Bells

CyctelCycle liCycte mU/Pb (my) zircon age

from Ontario Gcol. Survey Misc. Paper 129 Vnkanolgy & Mineral Deposits, 1986

The generali/ed geology of the project area is presented in Figure 3.3. It should be noted that the stratigraphic relationships between the various assemblages throughout the belt are still under much study and the subject of much debate.

A.C A. HOWE INTERNATIONAL LtMITEO Report No. 857 October 31. 2003

3.1.2 Sedimentary Sequences

The sedimentary rocks that dominate the eastern part of the Birch-Uchi Belt were subdivided by Thurston (1980) into: 1) a "regional sequence of unknown age"; 2) a younger turbiditic association, and; 3) a still younger "Timiskaming assemblage". The "Timiskaming sequence" centred on Birch Lake is typical of the numerous Timiskaming sediment filled "pull-apart basins" in the project area and is composed of polymictic conglomerate and sandstone units that are believed to represent alluvial or fluvial facies. These sedimentary sequences are considered to stratigraphically overlie the Cycle in felsic volcanics (Thurston, 1981). This fairly extensive Timiskaming sedimentary sequence has been interpreted as evidence of late extensional tectonic development within the Birch-Uchi Belt. The presence of relatively late, extensional pull-apart basins is considered favourable for the emplacement of possible mantle derived intrusives.

3.1.3 Igneous Si Metamorphic Events

The chronology of the plutonic and metamorphic events in the Birch-Uchi Belt is difficult to interpret due to a general lack of geochronological determinations throughout the belt.


Figure 3.3 Regional Geology, N.E. Birch-Uchi Bell

EARLY PRECAMBRIANEARLY FELSIC IGNEOUS AND

METAMORPHIC ROCKS*mr~~'t GiWKxfiwKe, ttarxinpfmite, Oua/ll dtorffc.Rjt '. . qutttt mon/anjfe. granite, syenite,Kg \ QOJX t r and felspar pofpnyries, peymt-

tile, apl'lc. urwifferenflaW'rf

EARLY MAFIC AND ULTRAMAFIC IGNEOUS ROCKS'"

Diotite, gaOtiio. voiac.wtO aWrfe. dunite, serpentinite.

METASEDIMENTSConglomerate, greywacke, t/ftose.

e. argillite. tJale. marMp, formation. miner i/olcarties

t related m/ui^ttitfs.

METAVOLCANICS'FELSIC TO INTERMEDIATE

METAVOLCANrCS"

M Hnrolrte. r/iwtfiKrfc eno tfscrfe ffroiw, ^^H tuffs, 9"t) ()i(Ttut5j, ftieit. iron jtorfns. ^^B (idn, mi'nof intlKfdimcfts fKt intru

sive rocks, anO related nji'pmafjfes.

MAFIC METAVOLCAMICS"^H Bastff. anOe&te f/fows, '"ffs and Arec-^H etas), chert. /Von^r (wn. firpoi-Tw/i-^^1 sctf/nwfs and intrusive rocks, ana re-

A.CA HOWE INTERNATIONAL LIMITED Report No 857 October 31,2003

4.0 EXPLORATION HISTORY

The Red Lake area hosts some of the most prolific and lowest cost gold mines in the world. Gold deposits such as Placer Dome's Campbell Mine and GoldCorp's Red Lake Mine (formerly the Dickenson Mine) have produced over 23 million ounces (500 tonnes) of gold since the early 1940's.

The discovery of gold at Red Lake in 1926 precipitated approximately 10 years of extensive prospecting activity throughout the Red Lake-Birch Lake area. This prospecting led to the discovery of numerous showings and several mines throughout the Project area. Table 4.1 summarizes the historic gold production data of the Red Lake District and gives some indication of the level of activity the area has experienced.

Geologically, gold mineralization within the Red Lake camp is controlled by large, regional- scale, deformation zones, a fact that has guided gold explorations efforts throughout the Red Lake greenstone belt as well as the adjacent Birch-Uchi Belt.Table 4. l Historical Gold Production of the Red Lake District as of December 31, 2001'

MINE

CAMPBELLGOLDCORP (DICKENSON)MADSENCOCHENOUR- WILLANSMCKENZIE RED LAKEHOWEYHASAGASTARRATT OLSENBERENS RIVERUCHIJASON (ARGOSY)H.G. YOUNGSACHIGO RIVERMCMARMACGOLD EAGLEJACKSON MANIONRED LAKE GOLD SHOREHUDSON PATRICIABUFFALOABINOLAKE ROWANKOSTYNUK BROTHERSBOBJOBATHURSTRED SUMMITMOUNT JAMIESOL D'ORMCFINLEYTOTAL

YEARS OF PRODUCTION

1949 - PRESENT0'1948 - PRESENT(2)1938 - 1976, 1997(4) - 19991939-19711935 - 19661930- 1941, 1957(7)1938 - 19521948 - 19561939 - 19481939 - 19431934 - 19521960 - 19631938- 19411940 - 19481937- 19411934 - 19401936 - 19381936 - 19371981 - 19821985 - 19861986 - 19881963 - 196619291927 - 19371935 - 193619761933 - 19361987

ORE MILLED (SHORT TONS)

17,979,8518,619,0088,678,1432,311,1652,353,8334,630,7791,515,282

907,813560,607757,074276,573288,17946,457

152,978180,095105,35786,33311,22831,9862,733

13,023577

N/A562591552458

N/A49,511,237

GOLDTROY

OUNCES10,335,2483,736,7042,452,3881,244,279

651,156421,592218,213163,990157,3411 14,467101,87555,24452,56045,24640,20427,14221,100

1,8571,6561,3971,2981,126362(9)

307277265258

N/A19,847,562

PRODUCEDOUNCES 1

TON0.575

0.434(3)0.283 (5)0.538(6)

0.2770.09 1 (8)

0.1440.1810.2810.1510.3680.1921.1310.2960.2230.2580.2440.1650.0520.5110.1001.951N/A

0.5460.469

0.480.563

N/A0.401

(1) Includes final production figures for 2001, (2) For 1997, 1998 and 1999 no production due to strike by unionised employees, (3) From 1970, includes production from Robin Red Lake, (4) Includes clean up ore and materials from the mine site, (5) Historic grade, actual grade for 1999 was 0.14 ounce per ton gold, (6) Includes production from Annco and Wilmar properties, (7) Continuous production 1930 to 1941; includes 268 ounces recovered from clean up in 1957, (8) Ore mined at Howey, before sorting totalled 5,158,376 tons. Avg. production from run-of-mine ore was therefore 0.0817 ounce per ton gold. , (9) Not included in total production figure.

1 Ontario Geological Survey, OFR 6079: 2002 Report of Activities 2001, Red Lake Regional Geologist Report: Red Lake and Kenora Districts

A.C.A HOWE INTERNATIONAL LIMITED Report No. 857 October 31, 2003

Some base metal exploration was carried out in the region during 1950s through to the late 1960s, when in 1968 the South Bay copper-zinc-silver volcanic hosted massive sulphide deposit was discovered by Selco Mining Corp. on the east shore of South Bay on Confederation Lake.

Due in part to GoldCorp's recent new spectacular discoveries at the Red Lake Mine there has been renewed interest in the region with respect to gold exploration, within both the Red Lake and Birch-Uchi greenstone belts. Junior exploration companies participating in this resurgence of activity include Rubicon Minerals Corporation, Metal Corp Ltd., Fronteer Development Group Inc., First Au Strategies Corp., and Wolfden Resources Inc. Their activities are outlined in the Ontario Geological Survey's Resident Geologist's "Report on Activities for the Red Lake and Kenora Districts" that is released annually and can be accessed via the Internet.

Oo fr


5.0 2003 SUMMER FIELD PROGRAM

5.1 OVERVIEW

Based on the current understanding of the tectonic evolution of the Uchi Subprovince and the structure and mineralization its greenstone belts, there is evidence to suggest that the Uchi Subprovince has the potential to host primary diamond deposits (kimberlite). As yet there has been no systematic exploration for primary or secondary diamond occurrences within the region.

After a comprehensive review of existing geological data for the region and a re-analysis of digital airborne geophysical survey data obtained from the Ontario government (1985 dataset), Jilbey identified approximately 170 high priority geophysical target anomalies (magnetic and coincident magnetic-EM anomalies) located throughout the Birch Lake-Uchi Lake region that represent possible kimberlite intrusions. Claims were staked to protect these targets. The reader is asked to refer to Map A (in pocket) for anomaly locations and their priority-ranking.

5.1.1 Evaluation of Targets for Kimberlite Potential

The 2003 Summer Field Program was designed to evaluate as many target anomalies as possible during the summer months via ground investigation to determine the target's prospectivity as a possible kimberlite intrusion warranting further investigation.

Anomalies were prioritized (A-D) for evaluation by ground magnetics, soil/lake sediment geochemical sampling, and visual inspection of outcrop if possible. Ground magnetics was employed to better pinpoint and delineate the airborne magnetic anomaly(ies) on the ground. Soil/lake sediment geochemical sampling utilized a relatively new geochemical analytical process known as Mobile Metal Ion ("MMI") that is effective in identifying gold, base metal and nickel mineralization and kimberlite intrusives hidden beneath unrelated overburden such as till, lake sediment or soil. Table 5.1 lists the target anomalies and their priority ranking. For reference purposes, the anomalies have been divided into four geographic areas: Birch Lake, Shabumeni Lake, Bathurst Lake, and Woman-Uchi-Confederation Lake areas.

5.1.2 Other Targets

In an arrangement with Gold Canyon Resources ("Gold Canyon"), Jilbey investigated two magnetic anomalies within Gold Canyon's Springpole Property in the Springpole Lake-Birch Lake area that were identified as being possible kimberlite intrusions. The two anomalies are located approximately l km north of Gold Canyon's exploration camp at Round Pond and Long Skinny Pond. Both were evaluated by ground geophysics and MMI sampling.

During the 2003 Summer Field Program Jilbey staked claims over several known gold occurrences along the southeast shore of Shabumeni Lake that were identified from government assessment reports. The occurrences are collectively referred to as the East Zone. Old pits and trenches from five occurrences- the Main Zone, Snake, Iceberg, Clap, and Zone 7- were successfully located and exposed. Representative samples were collected from four (the Main Zone, Snake, Clap and Zone 7) and submitted for fire assay. Two lines of MMI sample were completed over the Main Zone.

A.C.A. HOWE INTERNATIONAL LIMITED Report No. 857 10 October 31, 2003

Table 5.1 Birch-Uchi ProjectAirborne Magnetic S E.M. Anomalies

Anomaly I Anomaly Center (UTM)Xnad83

Birch Lake AreaE01

E02 E03~

E04EOSE06E07EOSE09E10E11E12E13E14 EI 5™iTe~~E17E18i'i'g" ———E20E21E22 E23""

E24 E25""""

E26 "'""E27E28E29E30E31E32E33E3435

E36E37E38E39E40E41E42N01N02N03 NO™

N05N06N07N08N09 —— ...™....N09~"

N10

554174 554353551365 """"""551967

554343563158565153569148569765572922571947572345574386576369582908 '""""""581943

'"""""583544

579916572958

" 572964571723569739569585 567415567152 """""566356

'"""""561365

5617555581465584705577665513515505455501 34550350557034555924556527556557556959560170580991582983534147530058530743 528933529098529713530910533891534936 534323 534313532260

Ynad83MagneticPriority

5698553 56985155699060 """""5697627

57043305699038569935157055515706422570804257091825706468570387457051755699986 5697509 """""5695197

56913565693301 5694890569475256935765693307 """"5692871

5693439 5691197 """"5694666"

5691937569344356896085692106569079956896285689950568157356821205676601567589656779265677868567353756733425672138571700057217315721823 g———

57238305724452572423157181955714390 """"5714507

5714579"5713667

A BA A ""'"ECBBccDABC

3""" """"""

BB A —————— '

BDB ...........,...........

B A —————— '

fABc~

AABAEAAABBACAAA

CA:j

B ^ ....................

D

EM 1 Comments on Magnetic Anomaly Priority l

Comments on EM Anomaly

D AA.""""""""

. ————— ..........

. ————— ..........

. ——— ,.............

::::::::

- — ' — -

- — - — -B

Perfect fit 8. model excellent fit. Good modelGood fit to weak anomaly, jjpod modelPerfect fit. Good modelOK fit, strange anomaly, too deepperfect fit, excellent model except too deepfairly good fit, very good model except dipvery good fit and modelexc fit, fiar model, too deep

perfect fit, good model,perfect fit, good mode^ shallow dipgood fit to very weak anomalyGood fit,, fair ..mode], a bit deep ^ __ - 3ood fit but bad modei: Too deep Effect fitL good model except deepVery good fit. Base line too low. Dip too shallowVerY i^d fi jSjMojjrnodej. perfect fit, good modelgood fit, good modelair fit, too shallow dipexc fitjjood modelpert fit, good model except too narrow and shallow dipjerfectfit, ver^cjood model jerfect fit, good model jood f it,, good model exc dip

good fit, excellent modelexcel lent f it , good modelonly fair fit, too shallow dipair fit, good model ecxept high magntit and too deepPerfect fit. Good modelgood fit, good model excpt deepExcellent fit, good modelExcellent fit and model

soso fit, poor modelPerfect fit 8, modelPerfect fit S modelPerfect fit S modelPerfect fit a modelexcellent fit, fair modelperf fit and modelair fit, fair model, too shallow dipExcellent fit and modelgood fit St modelexcellen^fjt&jTiodel good fit but vejy poor modei. Fiat thin surface feature. Flow?On[y fair fit, poor model, dip too shallowvery good fit, good modelgood fit but very poor model. Flat thin surface feature. Flow?air fit, too deep, high susc

some em looks related to large magnetic formation to north definite coincidental conductor. No conductivity on adjacent mag fml

small but definite conductor

. —— ....,. ————————————— ............................. __ ,..................... __ .............

........,.. ——————————————— ............ ——————— ... —— ,...................

....., ———— . ——————————— ... —————————————— ..... —— .

—— .................. —————————— __ ...... ——— ___ —— _ ..........mm....,,....

™ ———— ™......~. ———————————— ————— . ——— .. ——— ..,......M

jood fit^gartialjinomaly;. Dip too shallow but 'Jjay.b.^be^due to ..missing po nts ôor fit. OK model, ecept shallow dip ] 30or fit, high susc, probably i. F. jgood fit, wrong modei, too high susc, i. F? ]em: corid = 0 0128

Anomaly

N11N12N13N14N14N15N16N17N18

Anomaly Center (UTM)Xnad83

5461 7C541843533133531386531305535338541338546105546757

YnadBS571005557061975707793570327157034245704210570521757032045705026

MagneticPriority

DAAABBBCC

EM Priority

A

Comments on Magnetic Anomaly

Poor fit to distorted anomalyPerfect fit, very good model, a bit deep maybePerfect fit and model.excellent fit and model except dip. Negative suscep!!fair fit. Model agrees OK with other lineSurprisingly good fit to jjood part of distorted anomaly. Good modelExcellent fit. Good model except high susc.almost perfect fit, good model except susc too highVery poor fit, comples anomaly, em response, keep.


definite small emShabumeni Lake AreaW01W02W03W04 — -~

W06 WOT"™""™

W08W09

Wl'6""~

W11 W12""

W13

W14W15W16W16W17W17vi/—"W\9~~~~~

W20W21W22W24W25W26W27W28W29woo""""" ]W3"i ""W32W33 W34~"' W35""~

W36

538999550162549752549573

" 549804549320 """"""'543967

540744533789 533741 """""528069

537735 " 551609

545809 545931546138545531544142544365540030540002""""""537516 — — —

531928526011525423518766522442536908536755536940536153 525108 526201526050526009 ™--

527193544736

5699812569726856970385696490 56959245695603I569267056944665691565 5691560 5688818568805256910785686193 5686112568571656861785683735568368156809955680967 5682811' 5683596"568342056809815680789568197856864335695925569540656949335695143 5685216 568582056862285685003 5684229 568437?5689664

ABAB ABBBA A A'"""~ """'

ABA

BBBBAB ^

A "' 'AAABDEAAAmizziA """"B

B \____ ...—mr ""~ "" A" 'C

. —— ———— .

. ———— . —— .

. ————— .....

D A

A

.. ——— . —— ,.

A

good fit, good model except too shallow dipGood fit, good enough modelperfect fit, perfect modelveryôodfi^gpod^model ^ fair fit, excellent modelExcellent fit.jgood mpde[excepj shallow dip Good fit to noisy anomaly Model OK^deepExcellent fit, good modelPerfect fit and models on both lines And models on ^!.h.J!.n.es.confirm eachjrther _ m __ - 1 ______ n Perfect fit^ excellent modelperfect fit^ perfect model __ Fairiy good fit to weak anomaly, excellent modelExcellent fit, excellent model

Excellent fit, good model except shallow dipVery good fit, good model but a bit too deepgood fit, dip too shallowgood fit, dip too shallowêrfect fitL excellent modelSiLt'L6.?.?.?']?.!? IS?.?.! ______ ........ fair fitjgood model, except dip too shallow perfect fit, perfect modelvery good fit, excellent modelperfect fit^ perfect modelvery good fit, perfect modelgood fit, good model, dip a bit shallowjgood fit, much too shallow a dip and too high susc. Maybe suphidesfair fit to poor anomaly^ bad mode^ but keepperfect fit, almost perfect modelPerfect fit, very jjood modelGood fit to disturbed anomaly. Good model.^SSlMÊSS'.'S'^S^^^JSlSL^Lî^.îXS^... _ ___ ,. ••xoeTlent fit and irnodel " ~"Excellent fit to west half of double anomaly. Good modelalmost^rfect fitêxcellent model, a shade deep êrfect fif.Excellerit model ^rfe^f'firExceiTent'modeT'"' '

good fit to partial anomaly. Fair model, high susc., suspect sulphides

............. —— ..... —— ... ——————— ... ——— . ——— . —————————— ..

. ———————— ——————— .... ————————————— M _ — .............

. ———— - —— ...™ —————————— ————————— . .................. .... —— ..

weak channel two em anomaly definite small em, corx^ .036no em; small anom 180 m north

—————— ™ ————————— ............ ———————— ,. —————— ......

strong double peakLdc=210

————————— ................... ——— ....... ___ ....... ______ .. _____ ..

—— ——— ————————— .... — . ——— ™ ————————— .. ——— —

strong coincident em anomalyBathurst Lake AreaH01H02 'H03H04H05H06H07H08H09

499819 '"""""499575

501784500501501020506603509866510478504338

5687862 56876215685885568374956842395686378568284956823495677471

B B """"""

CBACCAB

——— .........

CB

fair fit, good mode[ecxept high magntit good fitsurprisingly good fit, fair modelgood fit good modelexcl fit, good modelust fair fit, fair modelAnomaly too complex fo modelling. Still possib;eExcellent fit and modelvery good fit to complex shape

—— ...... ——— ...,.,. —————————————— ,................ ———— ,.............

CPQ72strong 7200

Anomaly

H10 Hl'i"""""""""""

H12H13H14H15H16H17H18mg""""H20H21

Anomaly Center (UTM)XnadBS

503725 •••••••••••••504092

507623505765503404502791501333501940501979 '"""'562728

503909510023

Ynad835678213 56732615680071567630856798695677036567842156787285678205 '567892056786995679415

MagneticPriority

B 6""" "AA~

EDDA A"""""

BB

EM Priority

. ——— . —— ..

ÊDEAB m-

C


Perfect fit. Good model poor fit, poor model, still interestingExcellent fit and modelfairly good fti, excellent modelGood fit on complex anomaly.Good fit to unusual shape. Thin surface layerfair fit but poor model. Thin surface formpoor fitExcel lent f tt t good model perfect fit, excellent modelpert fit to weakanom. Good modelexcept dipit OK, good model eccept deep


......,. —— ..-... ————— . ———————————— ............ ———— ........... ——— . —— ...

definite 7200weak 7200 hz anomalydefn 7200 &Q900 on NE flankQ7200 weakQ7200 weakstrong em (both)

Q on both frqsWoman-Uchi-Confederation Lake Area301302soT"305 306"""

S07308 "" ——~~sTo~"~311 S12™~si's'""314S15316S17S18S19320321S22S23324S25S26327 328""""

S29330331 332""" 333"""""""""" 334""" 335""""

S36337338339340S41S42343344345346S47

512693515846 577496509519 ""'""""513926

513994 " 513387 " 513386' "'"""""578742

517605 517282' '""""""519303

519849520238522826522971525316528867532346535267537840542837537220536487537709542303 ~——~

537777537014537252 """535118

535099 534353 532644533189531756531562530147526836527288525378523326517026517272508062511291

56784385680986 56750185673808 56758055676210 """""5674207

5673831 56811885677416 5676432 """"5671552"

567156356718085671216567059656740595671804566841 75667000567098656727385663161566256756616115655436 """"5655637

565882456559915655806 5658616 5659390 5656574 5658403566176956600475660799565979156580365657762565676156568005660778566039256645785669602

BE B"""""

|——————

A -— —

B A" "'

3 '""""

A 'EBAEAr^BQ

B^

DCA A""'" ""

^D

T'" ~""""'

LlIIIIII.3 ~ 'BBBDCAABDBQ

A

. ———— . ———

g------ — -

B""""' '"""

A -M

A "" "

A

C

C

good fit, excellent model, although a bit deepE^ceJ^lent. fjt to.a.flat-lyin^thin tense __ m-Mi ___ Exc fit, good modely.e.Qf..99.9.!?..3J0 conptex anomaly. Good model Poor fit, good modelfair fitjair model __ - _____ ̂ perfect fit^ perfect model

good fit good modelOnly fair fit, fair model, em part of larger anomaly joodfit, good model perfect fit perfect modelgood fit to thin slab. Flow?very good fit , good modelvery good fit, good modelGood fit. poor model^ flat sheetexcellent fit 8t modelonly fair fit , model too deep^ discard??Good fit, OK modelfair fit, good modelair fit, fairmodel

fair fit, fair modelgood fit, too deepExcellent fit, model too shallow dipVery good fit, model too shallow dip

excellent fit il modelGood fit to disturbed anomaly. Model OK, a bit deeppoor fitExcellent fit and model __ _ ...lm.... m __ . jxc fitj fair mod

3ood fit, poor model 3erfect fit. Dip'a I b"it shallow "'""""" ~" ~

very good fit, good modelêrfectfit, good model except dip

Good fit. Shallow dip.Shallow flat magnetic and conductive formation.exclnt fit. Square prism. Only fair modelPerfect fit and good modelêfect fit, good model

Good fit to weak anomaly, good model

good fit, good modelgood fit, fair model, too deep 8, shalow cipPerfect fit and model.

. ——— .......,. ———————— .....,.,,.,,..,,..... —— . ———————— . —— ...,........

smal; almost coincident conductorno em definite small em, grade Adefinite small em, grade A

definite small em, grade A

Definite medium em

strong em conductor- .341

jEEEEEEEjEEEjEEEEEEg3 '

definite em conductor ij^no em, (200 metres away]very weak em anomaly on two channels. Looks weak but real —^

. Tl 'i^

p~

Anomaly

S48S49550

Anomaly Center (UTM)Xnad83

5103175166Q9515147

Springpole Lake Area

Ynad83566719356683925669600

Magnetic Priority

3B-

EM Priority


fair to poor fit. Fair model, shallow dipGood fit to weak anomaly, good modelVery good fit. Dipole mode - boulders, pipeline etc


In/a In/a In/a (n/aEast Zone Area, Shabumeni LakeMain ZoneSnakeIcebergClapZone/

n/an/an/an/an/a

n/an/an/an/an/a

n/an/an/an/an/a

n/an/an/an/an/a

5.2 SAMPLING A SURVEY METHODOLOGY

5.2.1 Mobile Metal Ion (MMI) Sampling

The MMI geochemical process is a relatively new proprietary analytical technique that takes advantage of the well-documented fact that metal ions "migrate" vertically from a buried mineralized body (from deep as 700 m) to accumulate in low concentrations at surface, a few l O's of cm below the soil/air interface. These "mobile" metal ions attach to the surface of individual soil particles near surface, remaining "mobile" for only a very short time before being bound up by soil forming processes to become part of the soil. The actual mechanism by which the ions are transported from depth to surface is poorly understood but it is believed that there is a constant flow of mobile ions upwards to the surface from the mineralized body below. By measuring the amount of mobile ions in the soil, the MMI process produces sharp geochemical responses directly above the source of the mobile ions thereby identifying the location of a mineralized body.

A typical MMI sample consists of 500-700 grams of inorganic material; including moisture/water. Based on advice from Dr. M. Fedikow, an MMI specialist who visited the Red Lake area on behalf of Jilbey, samples were collected from a fixed horizon 10-20 cm from the base of the organic layer (the soil type collected is irrelevant). Sample material was collected using a plastic trowel from a 1-2 foot diameter, 30-50 cm deep hole dug by shovel. The possibility of contamination by metal ions coming off the shovel is eliminated by scraping the sides of the hole clean with the plastic trowel. Any coarse gravel and pebble-size material was removed from the sample before bagging in watertight plastic snap seal (Ziploc) bags. In boggy ground, where the organic layer can extend for some depth, an extendable Dutch auger was used to reach down to depths of up to 4 metres if necessary to sample the inorganic substrate.

East-west and/or north-south sample lines were extended over target anomalies and samples collected at 50 m intervals. In situations where a sample line extended into a lake or where the target anomaly is overlain by a lake, a specialized lake sediment sampler designed by the Ontario Geological Survey was used to collect the MMI sample. The sampler is essentially a gravity coring apparatus that can allow for precise sampling of specific depths of the lake sediment substrate (see Figure 5.1)

The Jilbey MMI geochemical database contains analyses for both the MMI-B (Au, Ag, Ni, Co and Pd) and MMI-D (Mg, Ti, Cr, Co, Ni, Rb, Y, Nb, Pd, Ba, Ta, La, Ce, Pr, Nd, Sm, Gd, Tb, Er, Yb and Sr) elemental suites that allow for the detection of underlying precious metal mineralization and ultramafic lithologies respectively. An enhanced MMI-D analysis, referred to as the "DeBeers package", incorporates additional elements into the analysis that allows for further differentiation of kimberlite from the ultramafic lithologies. The soil and lake sediment samples collected during the course of Jilbey's summer field program were submitted to SGS Analytical Laboratories in Toronto for analysis by both MMI-B and MMI-D "DeBeers" suites in order to assess target anomalies for possible association with precious metal mineralization or kimberlite. Analytical finish is by inductively coupled plasma-mass spectrometry (ICP-MS). Samples submitted for analysis did not include field duplicates, replicates or standards although analytical duplicates were utilized to monitor analytical reproducibility.


Figure 5. l Use of the OGS Samplertwo*

tMd m W

Ai tfw uuCTfciy *trw tn nCtw bil x putflM u rv uckaf tn ugi ft/ mttf movmg ipuaro •nuqM tw tvAw cv**

L

Ungti

KS lake Setthnem Sampler

5.2.2 Ground Magnetics

A GEM Systems GSM-19 magnetometer (proton precession) with GPS and GSM-19 base magnetometer were used to carry out the ground magnetics survey. Both units are continuous- read magnetometers and were set to take readings every 3 seconds. East-west or north-south survey lines extended over target anomalies at 100 m line spacing. Figure 5.2 gives an example of geophysical and MMI geochemical survey lines that would have been extended over a target anomaly.

Where outcrop was encountered, a handheld KT-9 Magnetic Susceptibility meter was used to quickly determine the magnetic signature of a particular lithology and whether it was the source of the magnetic anomaly.

Figure 5.2An example of a "typical" ground magnetics and MMI soil/lake sediment survey planned for a target anomaly showing geophysical survey lines (shown as thick black lines at 100 m line spacing) and MMI survey lines and sample stations (represented by the black hollow- dots at -50 m sample spacing).

Useful waypoint coordinates are marked for navigation purposes using handheld GPS units.

A.CA HOWE INTERNATIONAL LIMITED Report No 857 October 31. 2003

16

5.2.3 Till Sampling

The purpose of sampling specific types of glacial sediments is to identify the down-ice "dispersal train" of minerals indicative of sub-cropping mineralized bodies that have been eroded during glacial advance. The dispersal train of minerals are traced back up-ice to the source mineralized body. The most common glacial material sampled is till, poorly sorted debris that is eroded/removed from the bedrock surface during a glacier's advance, dragged along the base of the glacier until deposition within depressions or hollows in the bedrock surface during glacial retreat. In general, very little Quaternary research has been directed at the Birch-Uchi area and consequently the glacial history of the area is poorly understood. On the basis of glacial striae in outcrop the postulated last known direction of glacial advance was from the northeast to the southwest at an approximate bearing of 2400. ^ . ^ **~J

A , '^ * ~'During the summer field program, a line of till samples perpendicular to the projected NE-SW down-ice direction from the Jilbey claim blocks was collected along the Joyce Lake Road at the extreme southwest end of the Project area. Samples were collected at 2 km intervals and analysed for gold grains and kimberlite indicator minerals (see Map A in pocket for till sample locations). Care was taken to ensure that the material sampled was pristine till, as till can be re- mobilized along paleo-slopes, reworked, transported and re-deposited, leading to erroneous interpretation. Samples averaged 15-20 kg in size; enough to ensure the availability of at least 10-12 kg of material for analysis after preparation. Coarse (cobble to pebble-size) material was manually discarded prior to bagging.

5.2.4 Notes on Navigation and Establishment of Location

Cut grid lines were not established over any of the target anomalies for the 2003 Summer Field Program. Navigation and establishment of location was accomplished exclusively though the use of small, rugged handheld geographical positioning system ("GPS") units such as those manufactured by Garmin and Magellan. The Gem Systems GSM-19 magnetometer utilized during the program featured a built-in GPS system that was used for determining the location of survey lines. The average positional accuracy of the GPS units typically ranged between 2-5 metres depending on tree cover and terrain.

Sample locations and the locations of other points of interest were recorded in UTM coordinates (datum NAD83) using the GPS units.


5.2.5 LOGISTICS

In carrying out the 2003 Summer Field Program, Howe employed the following individuals and services.

Senior Geological ConsultantDr. Wayne Ewert P.Geo.10 Langford Court, Brampton, Ontario L6W 4K4

Geological Field CrewGeologists

Technologist

Felix N.F. Lee, B.Sc., P.Geo. (APGO, APEGS)35 Church Street, Suite 314, Toronto, Ontario, M5E1T3

Raymond J. Knowles, B.Sc., P.Geo. (APGO) 79-13* Street, Etobicoke, Ontario, M8V3H5

Andrew Kamo, P.Eng. (APEO)

Steven Woodward

Geophysical ServicesAnomaly Interpretation and Analysis

Roger Watson, P.Eng., Consulting Geophysicist Geomapping Ltd., Toronto, Ontario

Analytical ServicesMMI and Soil Analysis

MMI Study & Interpretation

Till Sample KIM Indicator Mineral Analysis

SGS Mineral Services, Toronto, Ontario

Dr. Mark Fedikow, Consulting Geochemist, Winnipeg, Manitoba

Overburden Drilling Management, Nepean, Ontario


18

6.0 SUMMARY OF RESULTS

Across the Jilbey Project area a total of 170 target anomalies were identified for quick ground investigation (see Map A in pocket). The 2003 Summer Field Program evaluated 37 of these anomalies, of which 23 warranted a combination of ground geophysics, MMI sampling, and prospecting following field inspection. The summer program also saw five previously documented gold prospects near the eastern shore of Shabumeni Lake area ground evaluated. When warranted, rock and soil samples were also collected and submitted for analysis.

In total, the program yielded 374 MMI samples, 74 rock samples, 15 soil and 15 till samples.

'~\ ^y '6.1 MMI A Ground Magnetic Results by Anomaly 4} "7 /,A-- . -' v

A thorough examination of the MMI-B and MMI-D analytical results was performed by Dr. Mark Fedikow at Jilbey's request and involved the determination of selected element response ratios ("RR"), inter-element associations, and threshold determinations for each of the target anomalies in order to determine geochemically anomalous zones for follow up.

Table 6. l a summarizes the calculated 25th percentiles and derived background values for each of the MMI-B and MMI-D "DeBeers" elements. The backgrounds are used to calculate the response ratios; the basis for geochemical interpretation. Table 6. Ib provides a description of the MMI data and also provides a summary of threshold values. Concentration ranges, 25th percentiles, backgrounds and threshold values are presented separately for soils and lake sediments. Due to significant differences in concentration, the 25th percentiles, and backgrounds and thresholds between the soil and lake sediment data for both MMI-B and MMI-D elements, MMI-B and MMI-D geochemical data were considered separately when making interpretations. For further details regarding the statistical treatment of MMI data, the reader is referred to Dr. Fedikow's report, "A.C.A. Howe International Limited, Mobile Metal Ions Process Technology Survey (Jilbey), Red Lake Area", dated June 16, 2003.

Analytical data indicative of potential MMI-B anomalies (precious metal mineralization) and MMI-D "DeBeers" anomalies (kimberlite-ultramafic lithologies) are presented in Table 6.2.

6.1.1 MMI-B Soil Results

The response ratios from MMI-B analyses presented in Table 6.2 are generally of low contrast in one or two samples. The East Zone anomaly comprises several low contrast Co responses and a maximum response for Au and Ag of 13 and 27, respectively. These responses however are from a number of different samples collected from the magnetically anomalous area and as such offer very little focus. A two sample Ni anomaly with response ratios of 28 and 34 occur in association with the Peninsula anomaly. A coincident Au (RJ^15) and Ag (RR=45) response is documented from anomaly Sil and represents a low contrast follow-up precious metals target. Anomaly S17 is marked by a two-sample Co-Ni response, which could be indicative of mafic-ultramafic lithologies with or without mineralization. The most significant anomaly identified in the soil MMI-B data appears to be from a single sample response from magnetic anomaly HI 3. This response comprises low to moderate contrast responses for all five MMI-B elements.

A.C. A. HOWE INTERNATIONAL LIMITED Report No. 857 19 October 31, 2003

Table 6.1a Calculated 25th Percentiles and Backgrounds for Soils and Lake Sediments

MMI-BElement

AuCoNiPdAg

MMI-DElement

MgTiCrCoNiRbYNbPdBaTaLaCePrNdSmGdTbErYbSr

SOILS25th Percentle

0.054.60

22.800.051.24

SOILS25th Percentle

15220.500.500.501.50

12.800.280.500.0596.000.250.160.260.050.120.050.050.050.050.05

58.30

SOILSBackground

0.052.8013.500.050.70

SOILSBackground

8720.500.500.501.506.800.140.500.05

75.800.250.070.110.050.060.050.050.050.050.0535.90

LAKE SEDIMENTS25th Percentle

0.059.60

62.200.050.52

LAKE SEDIMENTS25th Percentle

48472.400.500.501.50

20.800.520.220.50

126.000.250.550.540.520.520.220.430.500.500.50

81.50

LAKE SEDIMENTSBackground

0.056.30

51.700.050.25

LAKE SEDIMENTSBackground

41340.970.500.501.50

15.300.420.150.50

92.600.250.420.390.420.420.140.280.500.500.5072.00

Table 6.1 b MMI-B and MMI-D Response Ratios ("RR") for Soils and Lake Sediments.

ELEMENTMMI-B

AuRRCoRRNiRRPdRRAgRR

MMI-DMgRRTiRRCrRRCoRRNiRRRbRRYRRNbRRPdRRBaRR

TREE RRSrRR

RANGE IN RESPONSE RATIO (RR)Soils

1-20.01-81.01-34.01-6.01-46.0

1-31.01-1728.01-178.01-44.01-54.01-15.01-29.01-4.01-4.01-7.0

9-906.01-17.0

Lake Sediments

1-7.01-27.01-6.01-5.01-43.0

1-3.01-180.01-10.01-8.0

1-11.01-4.01-6.01-3.0

11-22.0

10-80.01-6.0

CUM. FREQUENCY THRESHOLDSoils

81812217

1525025121199

1.51.54

1808

Lake Sediments

4113314

2.3702.233

2.32.82.5

17

362.3

NOTE: 'TREE" refers to "total rare earth elements' or the sum of all REE analysed in the MMI-D sute.

Table 6.2 -B a MMI-D Anomalies

ANOMALY | SAMPLE | ANOMALOUS RESPONSES | COMMENTJllbey Soils MMI-B Anomalies.East Zone(n=38)

Peninsula(n=18)

H13(n^16)

S17(n^8)

H08(n-13)

H21(1=7)

LSP(1=5)

S11(1=9)

S16(1=4)

2593229378

2939629396, 29435

29395, 29435

29552

2946129465

2949129573

29546

Au: 13RRAg: 27RRCo: several anomalous responses in the range 24-8 1RR

Au(12RR)-Ni(12RR}-Ag(33)Au: 11-12RR

Ni: 28-34 RR

Au(10)-Co(49)-Ni(16)-Pd(4)-Ag(25)

Co (44RR)-Ni (16RR)Co (27RR)-Ni (27RR)

AURR9-17

Co(57RR)-NK17RR)Co(39RR)-NK15RR)

No anomalies

Au(15RR)-Ag(45RR)

No anomalies

ndividual responses only-no corresponding anomalouselements

Au-Ni anomaly for sample 29435

Low contrast but multi-element anomaly

Four samptes, low contrast and no correspondinganomalous elements

Precious metals target

Jllbey Lake Sediment MMI-B Anomalies.W30(1=22)

Peninsula(1=7)

S17(1=2)

RP(1=8)

LSP(1=5)

E32/33(1=11)

SO4(1=11)

29414

2945429455

29495

29519

Au(4RR)-Ag(17RR)

Au(4RR)-Co(14RR)-Ni(5RR)-Pd(3RR)Au(6RR)-Ni(4RR)-Pd(3RR)-Ag(22RR)

Au(5RR}-Ag(25RR)

Au(4RR)-Ag(43RR)

very low; 8/32 samples have very low contrast Co with all samplesreporting 1-6RRforAu

No anomalies

tow contrast but multi-element for both samples

very low contrast

No anomalies)

very low contrast

verylowAu(1RRto7RR); low contrast NhPdresponses in 9/1 1 samples.

Jllbey Soils MMI-D Anomalies.S14(1=8)

W09^20)

W15(1=6)

S17(rF26)

H09(1=8)H21(1=7)S11

2931529325

29376

29464

Ti(968RR)-Cr(30RR)-TREE(313RR)Ti(800RR)-Cr(28RR)-TREE(325RR)

Ti(1728RRyCr(178)-Co(38RR)-Ni(54RR)-Rb(RR13)-Y(29RR)-Nb(4RR)-Pd(4RR)-Ba(7RR)-TREE(906RR)

Ti(586RR)-Cr(40RR)-Co(16RR)-Ni(12RR)-Y(18RR)-Nb(3RR)-TREE(451RR)

No anomalies

Ultramafic response

Kimberlite Lithology

Possible kimberlite; low Nb

No anomalies

No anomalies

No anomalies

(1=9)S16(1=4)S13rp10)S14(1=8)

S15(1=7)

S37(1=11)

S38(1=10)

29665 Mg(19RR)-Ni(12RR)

No anomalies

No anomalies

No anomalies

Low contrast

No anomalies

Five of 10 samples have anomalous Mg responses and3/1 0 have low contrast Nb; possible ultramafic signal

Jllbey Lake Sediment MMI-D Anomalies.W03(n'25)

E01(ns20)

E03(1=19)

W09(n=•|)

W04(1=21)

W02 (ns2)

W30(0=18)

S17 (n^2)H09 (nM)RP ^8)

E32/33(1=11)

SO4(1=11)

29284-2928929277-29280

29341

2940629407

29522

2953629537

Ti

TiTK70RR-96RR)TK70RR-132RR)

Multiple low contrast responses

Ti(76RR)-Co(8RR)-Ni(3RR)-Y(3RR)-Nb(3RR)

Ti(98RR)-Y(3RR)-Ba(8RR)Ti(100RR)-Y(3RR)

Ti(78RR)-Ni(3RR>Y(4RR>TREE(80RR)

Ti(70RR)-Cr(4RR)-Y(3RR)Ti(180RR)-Cr(8RR)-Co(4RR)-Ni(4RR)-Y(6RR)-Nb(3RR)-TREE(53RR)

6/25 samples have anomalous Ti responses between 60RR and 104RR;no corresponding element anomalies

1 1/20 samples have anomalous TiRR between 70-132 includinga 6 sample cluster 29284-29289 aid a 4 sample cluster 29277-29280;cluster 29284 - 29289 also has 5/6 YRR of 3-4 and TREE RR of 36-48;cluster 29277 - 29280 has 4 YRR of 3-4; possible ultramafic lithology

9/19 samples including 29292-29299 have TiRR of 70-1 16; 8 sampleswith YRR of 3-4 and 6/8 samples with TREE RR of 37-56; ultramaficf?)

No anomalies

Very low contrast

No anomalies

Low contrastLow contrast

No anomaliesNo anomaliesNo anomalies

Low contrast

Low contrastLow contrast, multi-element; ultramafic lithology possible

6.1.2 MMI-B Lake Sediment Results

There are few anomalous responses recognized in the MMI-B dataset for lake sediments. The range in concentration for AuRR is 4-6 and AgRR 17-23. The low concentration levels (and hence low response ratios) for Au, Ni and Pd are indicative of the absence of an anomalous data population for these elements. Anomaly S17 has two samples (out of two samples collected) that have very low contrast responses for Au, Co, Ni, Pd (sample 29454) and Au, Ni, Pd, Ag (sample 29455). The suppressed MMI-B responses in these data are indicative of a lack of a precious/base metal mineralization signal in the lake sediments.

6.1.3 MMI-D "DeBeers" Soil Results ^ # ~ * "^ t*

MMI-D interpretations are provided in Table 6.2 and are based on the same method of interpretation as the MMI-B results. Data has been assessed to identify anomalies indicative of kimberlite lithologies. Significant numbers of ultramafic/kimberlitic anomalies were not observed in these data. Of 13 aeromagnetic test areas, 8 anomalies did not have any MMI-D signatures associated with them that were suggestive of ultramafic or kimberlite rocks at depth. The remainder of the magnetic targets have MMI responses that could be attributed to either of these lithologies. Anomaly W15 contains l sample out of a population of 6 soils that has a multi element response suggestive of kimberlite. The elements that comprise this response include Ti, Cr, Co, Ni, Rb, Y, Nb, Pd, Ba and TREE. Another possible kimberlite signature is observed from anomaly S17 (single sample) with Ti, Cr, Co, Ni, Y, Nb and TREE although the magnitude of these individual responses is less than those from anomaly W15. The remainder of the responses including W09 (Ti, Cr, TREE) and S38 (multiple Mg responses with lesser low contrast Nb) are more likely to represent ultramafic lithologies.

6.1.4 MMI-D "DeBeers" Lake Sediment Results

A total of 12 aeromagnetic surveys were sampled and analyzed for MMI-D. Of these 12 sites 5 are interpreted to have no anomalies associated with them. The remainder of the magnetic anomalies is characterized by low to very low contrast responses with individual element response ratios (Ni, Co, Cr, Y, Ba, Nb) less than 10. Of interest is anomaly E01. This site is marked by 11 of 20 samples with anomalous TiRR between 70-132 including separate 6 and 4 sample clusters. Both clusters have low responses for Y (3-6) and a TREE RR of 36-48 associated with the six-sample cluster. This signal may be related to an ultramafic lithology or the low Y responses may simply be a reflection of random background variation. A similar response is obtained from anomaly E03 that is characterized by multiple low contrast responses for Ti, Y and TREE. A similar origin for these responses seems plausible as was indicated for anomaly E01. Singe element anomalies, such as those observed with anomaly WO3, may also be indicative of an ultramafic lithology. This anomaly has 6/25 samples with anomalous TiRR ranging between 60 and 104. The only multi-element MMI-D response observed in these data occurs in association with anomaly SO4. This low contrast response comprises Ti, Cr, Y, Co, Ni, Nb and TREE and is suggestive of an ultramafic lithology. Kimberlitic responses are absent from these data.


Interpretation of the MMI-B and MMI-D is summarized below. Anomalies representing precious metal mineralization are:

* On the basis of soils: Anomalies H13. Sil and the Peninsula Zone' On the basis of lake sediments: Anomalies S17, E32/33 (very low contrast), and Round Pond

Anomalies representing ultramafic lithologies are:

1 On the basis of soils: Anomaly W09' On the basis of lake sediments: Anomalies E01, E03, SO4, WO3

Anomalies representing kimberlite lithologies are:

f On the basis of soils: Anomalies W15, S17

6.1.5 Interpretation of Ground Magnetic Data

All ground magnetic data was processed and interpreted by Mr. Roger Watson, P.Eng., consulting geophysicist with Toronto-based Geomapping Ltd. Table 6.3 summarizes the target anomalies evaluated during the 2003 Summer Field Program and their MMI and ground magnetic interpretations. Individual target anomaly maps showing ground magnetics and MMI sample locations are presented in Appendix B.

6.2 Rock & Soil Sample Results

A total of 74 rock samples were collected from target anomaly areas where items of geological interest were identified or observed, such as quartz veining, alteration and sulphides. Samples include both grab and chip-type samples. Rock samples were submitted to SGS Laboratories in Toronto, Canada. Sample locations and results are presented in Table 6.4.

All samples were entirely crushed using standard crushing and milling to 200g in Cr steel, with silica sand cleaner used in the standard jaw crusher between each sample and prepared for analysis. Each sample was analyzed for gold and, where warranted, 31 other elements including silver, copper, lead and zinc using a 30g fire assay sample with AA/ICP finish for gold (with a gravimetric finish on samples exceeding 2,000 ppb or 2 g Au/T) and, for the 31 element suite, an 80g ICP sample with multi-acid digestion.

6.2.1 Shabumeni Lake East Zone

19 rock samples were collected from the Shabumeni Lake East Zone occurrences: 12 samples from the Main Zone vein (shown in Plate 6.1), 2 samples from Snake, l sample from Clap, and 4 samples from Zone 7. Several samples returned notable gold and copper values (Table 6.4). The Main Zone, Snake, Iceberg, and Clap were ground evaluated.

A total of 15 soil samples (B-horizon) were also collected across the Main Zone vein in order to provide a comparison with the MMI. Samples were collected at 25 m intervals from along the MMI sample line. Results however appear to show the soil survey failed to detect the Main Zone, returning negligible gold and copper values (Table 6.5).


Table 6.3 2003 Summer Field Program, Blrch-Uchi Project Evaluated Airborne Magnetic and E.M. Target!

Anomaly

Birch Lake AE01

EOSE32633

Shabumeni LW01W02W03W04W05W07W09

W13

W14W15W25W26W27W28W29W30W31W32

Bathurst UkH08H09H13H21

Woman-UchS04308S09S11S13SUS15S16SI-

324S25S26S 38S37S38

Anomaly Center (UTM) 1 MagneticXnadtS | YnadM l Priority

rea554174554353551967550545550134

.ake Area536699550162549752549573549804543967533789533741545808545931546138545531522442536908536755538940536153525108526201526050

e Area510478504338505765510023

-Confederatf517496513387513386517605519303519849520238522826522971537220536487537709533189531756531562

5698553569851556S762756896285689950

5699S12569726856970385696490569592456926705691565569156056861935686112568571656861785686433569592556954065694933569514356852165685820S686228

5682349567747156763085679415

on Lake Area56750185674207567383156774165671 5525671563567180856712165670596566316156625675661611566176956600475660799

Springpole Lake AreaLSPRPEast Zone Area, Shabumeni LakeMain ZoneSnakeIcebergClapZone 7Peninsula

ABAAB

ABABABAAA

BBDEAAADAB

ABAB

BABCAEBAECDCBBB

EM 1 MM)Priority l Samples

DAA

DA

A

CBCC

BAEA

C

20

1911

22521

21

6

22

1312167

11

910874

28

1110

108

38

25

RockSamples

1

2

7

5

4

2

4512

122

14

SoN 1 Preliminary Observations on Ground Magnetic Data 1 FinalSamples l Does ground magnetic data support kimberlite Interpretation? | Grade

15

yes

yesno complex, multi-peaked anomaly Probably zonedyes

Yes. Oval. 130 x 300 metres, 500 gammas, zoned anomalyyesyes Oval. 110 x 160 metres, good anomalyyes Oval 190 x 80 metresPerhaps. Complex anomaly, but well defined boundaries - could be kimberliteyes Oval 240 x 160 metresProbably yes, but not well enough covered to be sure. Complex anomaly along edges where covered.Yes, but small. 110 x 80 metres or so.

No Part of W 1 3No. Part of a long northeast trending formationNo. FormationalNo Part of a long northeast trending formationPossibly. Need confirmation from geochem. Could also be part of adjacent formationNo. Part of a long northeast trending formationYes Oval 290 x 140 metres, good anomalyPossible but unlikely . Looks formational Underlies heavily prospected Snake. Clap, IcebergPossible but unlikely . Looks formational. Underlies heavily prospected Snake,Clap,lceberg

yesNo. Formational anomaly striking e-wyesNo. Clearly a dike striking e-w

No A multi element formational sourceNo Too small {1/2 width 16 m)Maybe. 90 metres 1/2 wdth But strong inverse component Much too high suscepMaybe Is zoned and too complex to model Susceptibility also very high. 100 m wdthYes 90 metre width 3000 gammas - very strong At surface. Geochem essentialYes Oval. 120 x 300 metres, 600 gammas, zoned anomalyNo A linear formation with no kimberlite potentialYes Very shallow at surface 200 metres wideNo, Formational anomalyYes. Well defined on 3 fit lines. Oval 250x1 50m, good anomaly. Susc. 0.0032Yes. Well defined on 2 m lines. Oval 250x100m, good anomaly. Susc. 0.0029Yes. Well defined, double peak anomaly on three lines. Fair model on east peak.Yes, Three lines give good definition.No Formational anomalyNo, Formational anomaly

n/an/a

n/an/an/an/an/an/a

C

ABD

EBBAAA

D

CD

n/an/an/aE

n/aACC

cn/aE

n/a

n/aEEBAB

n/aC

n/aAABA

n/an/a

Fedikow ObservationsMMI-B and MMI-D combined

Ultramafic (L)

Ultramafic (L)PM MineralizationPM Mineralization

Ultramafic (L)

Ultramafic (S) 293) 5, 29325

Ultramafic - Kimbertitic (S) 29376

Ultramafic (L)

Ultramafic - Ross Kimberlitic (S) 29464 t PM Miner

PM Mineralization

PM Mineralization

Blue/Red = Anomalies with work conducted on themRed - Anomalies s associated with precious metal mineralization or ultramafic / kimberlite lithologies

374

2.27483

31201312023120331204313053120631207312083120931210312113121231213

31214312153121631217 3t2183121931220312213122231223 3122-)

t ANOMALY

W27 area bush zone N contactW27 area bush zone N contactW2 area bush zone 5 contactW2 area bush z en e S. contactW2 area Lake side zoneW2 area Lake side zoneW2 area Lake side zonefelsic dyke at IHe W02WOSW05lamp on man id. to BfCh Lk. Camplamp on mam rd 10 9rch Lk Campdiatremebx

silicified zonenounte zone. East Trenchsfea py zoneflounle.cpy.mal.spril?)diatreme eas of mam trenchQFP.moly.dratreme facies, silicified. SK pyW30 area Island py slwwmgsW30 area IslandW30 area Island pv showngsW30 area Island w ShowingsW30 area Islflnrt py1 ;nowmg?Sau zc-ne Mart zone SE set NWvam

EASTING NORTHING

536305536805536805536805536870536870536870

56954155695415569541856954185695418

Bia 2cSi*.W*n:ioita HW Island FV showmg 56B&456

5686467 5690644 5690644 5690644

Uppw Snatwmeni pc*H chem sed Upper Shabumeni pewit chem sed

1242 Upper Shabumeni pant chem sedPenntisuter Zone r* sharing Pwnlnsufar Zon* NE showing

31248 Veins ©Anomaly HOS

31249 Veins @ AnomaV H0831250 Veins® AnomaV H08

Veins Q Anomaly H0831252 Veins @ Anomaly H0831253 Anomaly H21

AnornalyH21 5679585569429656942965608075

31255 Westsh31256 Westsh

5675182567518256752035674215674215674215674215674215673636567383656776185677518

3127031271312723127331274

DUP-31274

312633126431265312663126731268312693127031271312723127331274

Anomaly S04 Anomaly S04 Anomaly 304Anomaly 508 pt a aa Anomaly SOB pit sea Anomaly SOS pit area Anomaly S03 northerly french Anomaly 508 north a V trench AnomalyS09 Anomaly S09Py showing west o( Anomaly Si 1 FV showing west of Anomaly S11

Plate 6. l Hxposed Quark/. Vein in Pit Wall at the Main /one, Shabumeni Lake Fit si 7one

6.3 Till Sample Results

Results of the regional till sample survey are generally inconclusive. Of the 15 samples collected, two returned KIM indicator minerals of significance. Sample RJK-31111 returned a single ilmenite and RJK-31112 a single pyrope garnet. The samples all returned numerous grains of gold. It is the opinion of Overburden Drilling Management that the two indicator minerals represent a possible distant kimberlite source, possibly from as far away as the Attawapiskat region within the James Bay Lowlands area. Excerpts from Overburden Drilling Management's till sample report can be found in Appendix C.

It should be noted again, that very little quaternary research exists for the Birch-Uchi area and the glacial history of the area is poorly understood. It is possible thai the till samples were not taken in the actual down-ice direction for the region, thus explaining the lack of KIM indicator minerals in the samples. In addition, the general lack of indicator minerals does not definitively preclude kimberlite occurrences in the region. For example, the recently discovered diamondiferous kimberlites near Wawa Ontario do not contain any of the indicator minerals commonly used to explore for kimberliles such as ilmenite and pyrope garnet.

AC.A HOWE INTERNATIONAL LIMITED Report No 857 October 31. 2003

28

(\

Tib f* 65SOIL SAMPE LOCATIONS i ANALYTtCAL RESULTS

SAMPLE*

29575

29576295772957829579295602958129582295532956429585295ES29567

295S829569

ANOMALY

East Zone

East ZoneEast ZoneEaslZoneEast ZoneEast ZoneEast ZoneEBS! ZoneEast ZoneEast ZoneEast ZoneEas! ZonaEast Zone

East ZoneCast Zone

L RESULTS

EASTING NORTHING

526580 5686480526607 5686475526633 5686475

526525 5686480

526475 5686480

566425 5686482 526649 5686554

526601 5686552

566580 5686552

Samp/e /VentScheme CodeAnalysis Un/tDelsct/on Utnil

DUP-29575 295762957729578

29580

29582

29584 29585

29587 DUP-2S587

29588

AuFA301Opt)

3 83

1

4

6 5

238

A'j

FA30Gg/mt

003

-

-

-

-

SeICP90opm

05

11

09

1 2

1 1 09

09 091 4

NaICPBOW

00)

225 2252 182 18

J

1 98

24 203

206 2081 82

MgICP60K

007

056 07106306

039

097

054 043

053063

AlICP80\

OQ1

6.39 66

654653

58

69

641

636622

Picpeoi/,

001

006 006005006

003

009

008

002003

KICPQO%

oor

74 6565

59

02

78

1 71 36

Ca•'CPao"4

00!

1 77 1 791 66T 67

1.44

207

1 93

1 541 34

SeICP3Qppm

05

6 3 7 16763

48

82

6 1

65978

T//CP80y.

001

0 2 023021C 21

0 17

026

02

022 02203

VICPBOopm

46 555

70

45 54

54 5476

CrtCPdoPpm

'

22 312726

18

39

2021

26 2746

MnICPBOopir,

2

147 372250270

177

251 216

233 236244

CQ(CP80%

oor

69 1206

67

43

61 72

M 0379

CoICPBOppm

1

NiICPBODflm

f

519

2

7

4 2

5 6

24

Ci//CP80opm

05

7

ZnICP80opm

05

22 36 1263289

175

508

259 25 1

236 27

335

AsICP30opm

3

S35

'•Z

03

SricpeoOpm

05

85 726781

58

41

2455

58 619666

y/CPaoopm

05

69 8

6 7e

4 7

11 2

86 4 9

52 54

ZrICP80ppm

05

17 060823

OS

13 26

13 12

Mo(CPflOppm

j

i11

1

1

1

1

1

Ag/CPflOppm

02

09080 9

08

04

07 1

09 08

1

CdICP90ppm

1

SnICP80opm

10

Q 000

0

0

00

0 0

10

Sbicpaoppm

5

^

S

3aICP80ppm

587 546564586

546

626

598 584

573 576482

La/CPflOopm

OS

104 14 1

1196

iV/CP60opm

10

0 000

0 1010

PbICPBOppm

2

00

BiICPBOppm

656

6

57

L)ICP80opm

1

7 141111

7

22

7

10 10

AgAA73y/mt

03

"nn

7.0 CONCLUSIONS AND RECOMMENDATIONS

Though final analysis of the MMI and ground magnetic surveys have not yet been completed, the 2003 Summer Field Program appears to have confirmed the prospectivity for kimberlite in several of the targeted anomalies. On this basis, Howe recommends that several of the anomalies warrant further investigation and suggests the following be completed during the upcoming winter and summer months:

* Diamond drilling of prospective targets. The winter months should provide the best opportunity to accomplish this work since a diamond drill can be easily be moved around via the lakes. One hole per anomaly should quickly and definitively evaluate the anomaly as kimberlite or not.

* Continued evaluation of target anomalies via ground magnetics and MMI analysis. Over half the targeted anomalies remain untested. Howe recommends a review of the remaining targets to determine which ones can best be evaluated during the winter season. Anomalies situated within lakes or ponds can still be evaluated during the winter using as the OGS sampler to collect lake sediment samples for MMI analysis.

As many of the targeted anomalies should be evaluated as quickly as possible to determine whether Jilbey should continue to hold certain claims or not.

Further work is recommended for the East Zone on Shabumeni Lake on the basis of the favourable results obtained from the rock samples collected from the existing workings. It is possible that the occurrences are indicative of a larger mineralized system. Howe suggests a program of stripping, geological mapping, trenching and sampling be conducted to delineate the strike and dip extensions of the known occurrences and to identify other nearby veins or zones of mineralization and alteration. Again, the winter months provide the best opportunity to accomplish this work since heavy machinery such as a backhoe can be efficiently mobilized into the area via the lakes.


SOURCES OF INFORMATION

Fedikow, M., (Mount Morgan Resources Ltd.)A.C.A. Howe International Limited, Mobile Metal Ion Process Technology Survey (Jilbey), Red Lake Area. Dated June 16, 2003

Lichtbau, A., Ravnaas, C., Storey, C.C., Raoul, A., Kosloski, L., and Wilson, S.2002 Report of Activities 2001, Red Lake Regional Geologist Report: Red Lake and Kenora Disrricts;Ontario Geological Survey, Open File Report 6079.

Sanborne-Barrie, M., Skulski, T., Parker, J.Three Hundred Million Years of Tectonic History Recorded by the Red Lake GreenstoneBelt, Ontario; Geological Survey of Canada, Current Research 2001-C19.

Watson, R., (GeoMapping Limited)Jilbey Gold - Birch Lake Project. PDF Files of Ground Geophysics and Geochemistry,2003 Summer Field Program, (maps on CD-ROM)

Wood, J. and Wallace, H., ed., 1986.Volcanology and Mineral Deposits; Ontario Geological Survey, Miscellaneous Paper 129.


CERTIFICATE

A.C A. HOWE INTERNATIONAL LIMITED Report No. 857 October 31, 2003

FELIX LEE

3 5 Church Street, Suite 314, Toronto, Ontario, M5E1T3 Tel: 416-368-7041 Fax: 416-368-2579 Email: [email protected]

CERTIFICA TE of A UTHOR

I, Felix Lee, P.Geo., do hereby certify that:

1. I am currently an Associate Consulting Geologist with: A.C.A. Howe International Limited 330 Bay St., Suite 830 Toronto, Ontario, Canada M5H 2S6

2. I graduated with the degree Bachelor of Science, Geology from McMaster University m 1986.

3. I am a Fellow of the Geological Association of Canada and member of the Canadian Institute of Mining and Metallurgy and the Society of Economic Geologists and a Professional Geoscientist (P.Geo.) registered in the Provinces of Ontario and Saskatchewan (APGO no. 0758, APEGS no. 10497).

4. I have worked as a geologist for a total of 17 years since my graduation from University.

5. I am responsible for all sections and authorship of the technical report titled "Summary Report on the 2003 Summer Field Program, Birch-Uchi Project, Red Lake Mining District, prepared for Jilbey Enterprises Inc." dated March 31, 2004 (the "Summary Report") relating to the Birch-Uchi Project in the Red Lake Mining District, N.W. Ontario, Canada.

6. I am not aware of any material fact or material change with respect to the subject matter of the Summary Report that is not reflected in the Summary Report, the omission to disclose which makes the Summary Report misleading.

7. I consent to the filing of the Summary Report with any stock exchange and other regulatory authority and any publication by them, including electronic publication in the public company files on their websites accessible by the public, of the Summary Report.

Dated this 31 st day of October 2003.

Felix Lee, P. Geo.


APPENDIX A.

Jilbey Enterprises Inc. Birch-Uchi Project

List of Claims & Status

9 483

Jilbey Enterprises Inc. Birch-Uchi Project Claims and Status

Claim No.

1247895

1247880

1247881

1248604

1248605

1248606

1248607

1248609

1248611

1248612

1248613

1248614

1248615

1248616

1248617

1248618

1248619

1248620

1248622

1248623

1248624

1248625

1248628

1248629

1248630

1248631

1248632

1248633

1248634

1248635

1248636

1248637

1248638

1248640

1248641

1248642

1248643

1248644

1248645

1243646

1248647

1248648

1248649

1248650

1248651

1248657

Township/ Area

SHABUMENI LAKE

CASUMMIT LAKE

CASUMMIT LAKE

WAVELL LAKE

BROWNSTONE LAKE

BROWNSTONE LAKE

BROWNSTONE LAKE

SEAGRAVE LAKE

HAILSTONE LAKE

BROWNSTONE LAKE

CASUMMIT LAKE

SHABU LAKE

SHABU LAKE

SKINNER TWP

SKINNER TWP

SHABU LAKE

SHABU LAKE

SKINNER TWP

SHABU LAKE

SHABU LAKE

SHABU LAKE

SKINNER TWP

SATTERLY LAKE

SATTERLY LAKE

SATTERLY LAKE

SATTERLY LAKE

SKINNER TWP

SHABUMENI LAKE

SKINNER TWP

CASUMMIT LAKE

CASUMMIT LAKE

CASUMMIT LAKE

CORLESS TWPLITTLE SHABUMENILAKELITTLE SHABUMENILAKE

DENT TWP

DENT TWP

GOODALL TWP

GOODALL TWP

GOODALL TWP

GOODALL TWP

GOODALL TWP

UCHI LAKE

UCHI LAKE

COSTELLO TWP

SHABUMENI LAKE

Claim Recording Date

2003-JULY-28

2003-JUL-17

2003-JUL-17

2002-APR-08

2002-APR-08

2002-APR-02

2002-APR-08

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-08

2002-APR-08

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-02

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-02

2002-APR-02

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-02

2002-APR-10

2002-APR-08

2002-APR-08

Claim Due Date

2005-JUL-28

2005-JUL-17

2005-JUL-17

2004-APR-08

2004-APR-08

2004-APR-02

2004-APR-08

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-08

2004-APR-08

2004-APR-02

2004- APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-02

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-02

2004-APR-02

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-02

2004-APR-10

2004-APR-08

2004-APR-08

No of Claims

6

1

3

12

g16

12

16

16

9

12

6

16

16

16

16

8

16

9

16

16

9

16

9

16

16

9

16

16

12

16

12

9

9

16

12

9

9

g9

15

15

16

12

9

15

Work Required

52,400

5400

St, 200

54,800

S3.600

56,400

54,800

56,400

56,400

53,600

54,800

52,400

56,400

56,400

56,400

36,400

53,200

56,400

53,600

56,400

56,400

53,600

56,400

53,600

56,400

S6.400

53,600

56,400

56,400

54,800

56,400

54,800

53,600

53,600

56,400

54,800

53,600

53,600

53,600

53,600

56,000

S6,000

56,400

54,800

53,600

56,000

Total Applied

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

Total Reserve

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

SW Corner Easting

549725

549238

533250

533660

545800

546770

556100

555200

541300

540820

502780

501840

503450

503450

501850

501040

505050

499100

500060

509500

50g470

545060

546640

547780

549340

512g40

525000

512640

543350

536040

538410

507630

530770

532340

522200

522200

522160

5ig320

518140

517000

517060

524780

531 240

532840

525560

SW Corner Northing

5697471

5696426

5717420

5716220

5708800

5704630

5676970

5675280

5705510

5704290

5679440

5677490

5677630

5676040

5676140

5677370

5675360

5686900

5682980

5681580

5678690

5685260

5686280

5688940

5688940

5674590

5680000

5673080

5691820

5694790

5699080

5663660

5702420

5691570

5667000

5665800

5670530

5671250

5670860

5674000

5676000

5655440

5659790

5660600

5683140

Jilbey Block No

0

0

0

46

50

55

59

115

114

56

58

92

90 nw

90ne

90se

90sw

91

89

148

145

141

140

7

8

121

120

80

16

79

3

17

1

67

57

6

39 north

39 south

27

26

25

83 south

83 north

40

42

41

61

Claim No.

1248658

1248659

1248660

1248661

1248662

1248663

1248664

1248665

1248666

1248667

1248668

1248669

1248670

1248671

1248672

1248673

1248674

1248675

1248676

1248677

1248682

1248683

1248684

1248685

1248686

1248687

1248688

1248689

1248690

1248691

1248692

1248693

1248694

1248695

1248696

1248697

1248698

1248699

Township/ Area

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

COSTELLO TWP

SHABUMENI LAKE

SHABUMENI LAKE

SHABUMENI LAKE

COSTELLO TWP

SATTERLY LAKE

SATTERLY LAKE

SHABUMENI LAKE

SATTERLY LAKE

SATTERLY LAKE

KEIGAT LAKE

COSTELLO TWP

KEIGAT LAKE

KEIGAT LAKE

KEIGAT LAKE

SEAGRAVE LAKE

KEIGAT LAKE

CASUMMIT LAKE

ZIONZ LAKE

ZIONZ LAKE

KEIGAT LAKE

KEIGAT LAKE

KEIGAT LAKE

ZIONZ LAKE

ZIONZ LAKE

ZIONZ LAKE

Claim Recording Date

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

2002-APR-08

Claim Due Date

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

2004-APR-08

No of Claims

9

4

g16

15

16

16

15

3

15

15

16

12

4

6

g15

16

9

9

16

9

16

16

16

16

16

9

16

16

16

16

16

8

16

16

16

Work Required

53,600

51,600

53,600

56,400

56,000

56,400

56,400

56,000

51,200

56,000

56,000

S6.400

34,800

51,600

S2.400

S3, 600

S6.000

56,400

53,600

53,600

56,400

53,600

56,400

56,400

56,400

56,400

56,400

S3, 600

56,400

56,400

56,400

56,400

56,400

53,200

56,400

56,400

56,400

Total Applied

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

Total Reserve

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

SW Corner Easting

526760

526760

527600

531 1 80

517550

524000

524000

522800

522800

522800

521600

534700

520000

519200

519200

537180

541000

536420

525560

549800

545060

553650

536160

560800

557550

557550

557550

561310

549729

574000

575580

565700

566700

568320

569100

570660

572230

SW Comer Northing

5683940

5683140

5688000

5682170

5680306

5684800

5683200

5683200

5685200

5687200

5687200

5666200

5684800

5684800

5684000

5660810

5681940

5681430

5685150

5681000

5686860

5698080

5662000

5692900

5692250

5690650

5689050

5691060

5695719

5702900

5703780

5690600

5692200

5692270

5692320

5693700

5693940

Jilbey Block No

61

61

37

14

21.22

61

61

61

61

61

61

30

61

61

61

100

12

11

61

113

5

101

99

109

111

112

152

122

103

130

131

126

125

124

123

138

137

APPENDIX B.


Target Anomaly Maps Ground Magnetics and MMI Sample Locations

BATHURST LAKE AREA

H08 A-

.̂4-3- '29567

.295651252 -

it raw

LEGEND©28487 MMi sod sampte location * number • 3124B Rot* grab-ctiip sample location * n, X2W87 Soil sample locatkxn-number

m Ground magnetics Iraverse lines (continuous read magnetometer)

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTTARGET AREA H08. Claim#1248624 -TOTAL MAGNETIC FIELD

GEOMAPING LTD.-TORONTO

-25 O 25 SO 75

A.C.A. Howe International Limited

504 300

248616

248^7 BATHURST

504100 504200

LEGEND* 29487 MMI soil sample location * number 1 31246 Rock grab-diip sample location -i- number x 29687 Soil sampte location -t- number

Ground magnetics traverse lines (continuous read magnetometer)

504400

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTTARGET AREA H09. Claim#l248616S617-TOTAL MAGNETIC FIELD


-26 O 29 30 75

AMORUSTMnnelfi


Au 10 Co 49 Ni 16 Pd 04 \ Ag25

S056QO

LEGEND29487 M Mi soil sample location -f numbef

1 31248 Rock grab-ctiip sample location * number x 29687 Sol sample location t number


JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTTARGETAREA H13

GROUND MAGNETIC SURVEY


500700

LEGEND* 2M87 MMI soil sample location * number 131248 Rock grab-criip sample location -t- number x 23687 Soil sample locatwn * number


JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTTARGET AREA H21-TOTAL MAGNETIC FIELD

GEOMAPING LTD -TORONTO


BIRCH LAKE AREA

jsroc LfifiEMO

929497 MM l six! sample location f number B 31248 Rock grab-chip sample location * number x 296B7 Soil sample location -t- number

Ground magnetics traverse lines0\ (continuous read magnetometer)

JILBEY GOLD EXPLORATION LTD.BIRCH LAKE AREA. ONTARIO!

GROUND MAGNETIC SURVEY, TARGET E01

-ffi O 2S 50 76

A C. A Howe International Limited

551800 552000 552200

s johnson island

293080- - -,' - -'

Johnson Island

551800 552QQO 552200

LEGEND* 2W87 MMI soil sample location t number 131248 Rock grab-chip sample location * number X29687 Sod sample location * number

Gfound magnetics traverse lines (continuous read magnetometer)

JILBEY GOLD EXPLORATION LTD.TARGET E-03, BIRCH LAKE AREA

GROUND MAGNB1C SURVEY

-26 O 25 60 75

Metres NADB3ASTMzonelS


LEGENDo 29487 MMI soil sample location * number 1 31248 Rock grab-chip sample location * number x29687 Soil sample location t- number

m Ground magnetics traverse lines (continuous read magnetometer)

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTGROUND MAGNETIC SURVEY. Aug 2003.TARGETS H21-TOTAL MAGNETIC FIELD



539200 S3B300

K O 25 SO '6

JILBEY GOLD EXPLORATION LTD - BIRCH LAKE PROJECTTARGET AREA W01 - GROUND MAGNETIC SURVEY

TOTAL MAGNETIC FIELD

LEGEND. 2M87 MM l soil sample location * number

n 31I4B RocK grab-chip sample location * number x 2958T Soil sample tocalion * numberi f\ Ground magnetics traverse hues \ \ \ (continuous read magnetometer!


i i' pth - : Dip ~ 91 '2 Susc ^ O s": lOOSI

29 O M SO T5

JILBEY GOLD EXPLORATION LTD - BIRCH LAKE PROJECTTARGET W-07 - GROUND MAGNETIC SURVEY

GEOMAPPING LTD., TORONTO

LEGEND© mar MMI soil sample location t number9 5124* Rock grab-chip sample location * numberx 26617 soil sample location * number

m Ground magnetics traverse lines . . .[continuous read magnetometer)


533 J 00 S3WnC

LEGEND

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECT 29AS7 MMI soil sample location * number

TARGET W09 - GROUND MAGNETIC SURVEY GEOMAPPINGLTD., TORONTO

31248 Rock grab-chip sample location * number 29SB7 Soil sample location * number

i (\ Ground magnetics traverse lines(conbnuous read magnetometer)

.C.^. Howe International Limited

JILBEY GOLD EXPLORATION LTD.BIRCH LAKE PROJECT - TARGET W15


LEGEND• 29487 MMI soil sample location + number H 31248 Rock grab-chip sample location * number x 29687 Soil sample location -f number

0\ Ground magnetics traverse lines (continuous read magnetometer)

A. C,A. Howe International Limited

M93DC 5494CQ 54S5QO S4S60D 543700 549800 549900 55CQOO 550100 650200 550300 550400 4 W 600

Johnson Island ^—

^J N

548300 546400 649500 649600 549700 54B8DO 549800 550000 550100 E5030C 550300 550400 550500

JILBEY GOLD EXPLORATION LTD - BIRCH LAKE AREALE&MQ

* 2*4*7 M Ml soil sample kxatiofi * number GROUND MAGNETIC SURVEY, TOTAL FIELD, TARGETS W02 &W03 amw Rock gmtKtiip sample location number

GEOMAPPING LTD., TORONTO x28687 Soil sample kxatw * numberl f\ Ground magnetics traverse linest! i (continuous rasd magnetometer)

.C.^. Howe International Limited

546100 543200 S4g300 54BBOD54860054970054B800648900550000560100560200560300

?4*^^^r 'W04 (B)

549100 64BIQO S4B300 549400 549600 5436DO MB 7 00 549600 M B BOO 56020S 560300

LESENDBIRCH LAKE PROJECT - TARGETS W04 AND W05 , 29lW7 MMI son sample locatai * m

GROUND MAGNETIC SURVEY - MODELING RESULTS IN YELLOW -~-™* Rock grab-chip sample beaton * mimtoerGEOMAPPING LTD., TORONTO * ™" ôil MHmple locf'i0^ * number

' i \ \ Ground magnetics traverse tines\\ \ (continuous read magnetometer)


M J H 'B l*

JHfiEY GOLD EXPLORATKW LTD. BIRCH LAKE AREATARGETS W26, W27, W2B, W29

GROUND MAGNETIC SURVEY - TOTAL FIELD

LEGEND2S487 MMI soil sample location * number

K 31248 Rock grab-chip sample location * number x 2HB7 Soil sampie location * number



WOMAN-UCHI-CONFEDERATION LAKE AREA

Tt-70,Cr-4,Y-3Q!9536

- SO-liB 1.295*4

a -j -A -M is

JILBEY GOLD EXPLORATION LTD.BIRCH LAKE PROJECT - TARGET AREA StM

GROUND MAGNETIC SURVEY. TOTAL MAGNETIC FIELD

LEGENDc 29487 MMI soil sample location * number B 31248 Rock grab-crilp sample location * number x 29M7 Soil sample location * number



51TBOO S17700 517800

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTTARGET AREA S11

MAGNETIC FIELD AND MMI SAMPLE LOCATIONS

LEGEND® 29487 MMI soil sample location * number B31248 Rock grab-chip sample location * number x 29W7 Soil sample location * number



29613519100 519200 519400 519500

metres

LEGEND2WS7 MMI soil sample location -t- number 31248 Rock grab-chip sample location t number 29S87 Soil sample location * number

Ground magneucs traverse lines (continuous read magnetometer)

JILBEY GOLD EXPLORATION LTDBIRCH LAKE PROJECT - TARGET S13


519500

NA

W -*C\- E


25

519700-92 043' 519800 519900 520DOO

Z ± -IDip = 92.5 Susc = 0.0160SI

25 50

519700

75

519600 519900 520000

metres NAD63/UTU zone f 3JV

JILBEY GOLD EXPLORATION LTD.BIRCH LAKE PROJECT - TARGET S14

GROUND MAGNETIC SURVEY with MODELED SOURCE

LESEND

• 2M87 MM! soil sample location * number• 31248 Rock grab-chip sample location t number x 29687 Soil sample location * number



S 20200

JILBEY GOLD EXPLORATION LTD.BIRCH LAKE PROJECT - TARGET 315


52MOD 82*4230'

LEGEND* 2M87 MM! seul sample location * number s 11248 Rock graft-chip sample location * number x 2*687 Soil sample location * number

m Ground magnetics iraverse lines (continuous read magnetometer)


a a aJILBEY GOLD EXPLORATION LTD.

BIRCH LAKE PROJECT - TARGETS SQ8 t SOBGROUND MAGNETC SURVEY

LEGEND• 28487 MMi soil sample location * number 1 31248 Rock grab-chip sample location * number x 29587 Soil sample location * numberi f\ Ground magnetics traverse lines iJ \ (continuous read magnetometer)


522500 522800 522700 522800 S22900 S23GOO 523100 523300 523300 533400

S16i{A).^T-^,. . /7*VP . J.

Deptft ^ 22 Dip' 4 62. l

^ 0.01DOSI

Ti586 •lCr40

Cot6HUH' 12Y 18Nb3TREE

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTGROUND MAGNETIC SURVEY - TARGETS S16 AND S17

] GEOMAPING LTD.-TORONTOMMI profile of SGS KimOerlite signature (nine elemenls) in red

LEGEND• 2MB? MMI soil sample location * number 1 31248 Rock grab-cnlp sample location * number x 29687 Soil sample location * number

Ground magnetics traverse lues (continuous read magnetometer)


0 WABUNK BAY

60 O M 100 150

JILBEY GOLD EXPLORATION LTD., BIRCH LAKE PROJECTTARGET AREAS S37 4 S38

Detailed airborne magnetic survey, Sept 2003 - Vertical magnetic gradient

• 2M87 MM l soil sample location * number• 31248 Rock grab-chip sample location * numberx 28S87 Soil sample location t number


A. C.A. Howe International Limited

SHABUMENI LAKE AREA

T*l

W ~*Ct*~ EY s

1248667 .

'/.ff/Wl

lPeninsular

Zoney

jAu.po.py

f/J ' 'f/f/f/ff" n -" ' O G O O O Q Q O

JI1.8EY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECT SHABUMENI PENINSULA MMI SAMPLE LOCATIONS

o 29487 MMI soil sample (ocation * number0 31248 Rock grab-chip sample location * numberX29B87 Soil sample location * number



jurr OOID BtpUMAtiw LTDSfBJH LUE BBOJECI - SHMljMEW

UftOWtlC SUTVfY d fkquil BID Solh •#mpJ* too*t-

Wo we International Limited

J*b

O: oi

(D Q.

-9T38' 525500 525600 525700

534800 5347QO 5248m 534800 525000 525100 525200 5253QG 525400 525500 525600 5 J 5700

50 O 50 100 150

metresHMXS/U7U mne tOH

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECT LEGENDTARPFTWV1 -;-29447 MMl soil sample locauon* number

131248 Rock grab-chip sample location * numberGROUND MAGNETIC SURVEY XWM7 50,1 samp.e kxôn , number

i ft GfourW magnetics traverse lines li S (continuous resd magnetometer)

—————————————————————————————A.C.A.HowehInternational Limited l

APPENDIX B.


Target Anomaly Maps Ground Magnetics and MMI Sample Locations

&T27483

BIRCH LAKE AREA

K a w M '5

JILBEYGOLD EXPLORATION LTD.BIRCH LAKE AREA. ONTARIO

GROUND MAGNETIC SURVEY, TARGET E01 FIG. 1

551800i

552000 552200 r

. . . Johnson Island

. . Johnson Island

551800 552DOO 552200

JILBEYGOLD EXPLORATION LTDTARGET E-03, BIRCH LAKE AREA

GROUND MAGNETIC SURVEYFIG 2

JILBEY OOID EXPLORATION LTD BIRCH LAKE PROJECTGRCX.ND MAGNETIC SURVP", Aug 3003. TARGETS El? l E33

. TORONTO Fig. 3

SHABUMENI LAKE AREA

638300

539100 •WWW

JILBEY GOLD EXPLORATION LTD - BIRCH LAKE PROJECTTARGET AREA W01 - GROUND MAGNETIC SURVEY

TOTAL MAGNETIC FIELD

-H-

54930C WWQG WBMO MB6CD S4BTOQ S 4880 O 5*8600 &5000C 560100 550200 550300 5KMQQ

W93CO 5494M 548500 519WO 5*9700 546800 54GBOO 5SQOM 550100 550100 560300 550400 560500

JILBEY GOLD EXPLORATION LTD - BIRCH LAKE AREAGROUND MAGNETIC SURVEY, TOTAL FIELD, TARGETS W02 &W03

GEOMAPPING LTD., TORONTOFIG. 15

O O 7/' r^ T^v * "-: 4.

ip z 91 .' JSusc ^ OC:',OOSI

JILBEY GOLD EXPLORATION LTD - BIRCH LAKE PROJECTTARGET W-07 - GROUND MAGNETIC SURVEY

GEOMAPPING LTD.. TORONTOFIG. 17

JtLSEYGOLD EXPLORATION LTD. - BIRCH LAKE PROJECTTARGET W09 - GROUND MAGNETIC SURVEY

GEOMAPPING LTD., TORONTO

FIG. 18

H MOO

JILBEY GOLD EXPLORATION LTD.BIRCH LAKE PROJECT - TARGET W15

GROUND MAGNETIC SURVEYFIG. 19

549100 549200 540300 M9400 54B500 549600 W97DD 548800 549BDD 560000 550100 560700 660300

Dip - 89.0 Susc s OO'^StJS't

M9IDO M9200 M84K1 543500 549600 549700 546000 549800 55BQOO 5W100 560 IDO 550300

BIRCH LAKE PROJECT - TARGETS W04 AND W05GROUND MAGNETIC SURVEY - MODELING RESULTS IN YELLOW

GEOMAPP1NG LTD., TORONTOFIG. 16

Scale 1:5,000JILSEY GOLD EXPLORATION LTD.

BIRCH LAKE PROJECT - TARGET W25GROUND MAGNETIC SURVEY

-fi-

se o so loo

JILBEY GOLD EXPLORATION LTD 3IRCH LAKE AREATARGETS W28. YV27. W28, W29

GROUM5 MAGNETIC SURVEY - TOTAL REID FIG. 20

-* r t

to

CO

534600 534700 574800 534900 526000 525 DO 575200 535300 555400 575500 525600 575700

534BOO 53*700 534600 524800 626000 525 IDD 525 200 526300 525400 525500 525800 -82-38' S3 6700

JILBEYGOLD EXPLORATION LTD. -BIRCH LAKE PROJECTTARGET W30


JUCT MLO EttUMMDH LTD.ncH LMccmcueci - SUWJWM cm

OHOUOUMMETICSlRVEr JM^JJ

y a n ME

JtLBEY GOLD EXPLORATK3N LTD - BIRCH LAKE PROJECTSHABUMENI PENINSULA MMI SAMPLE LOCATIONS

648900 WBOGO 549100 6492QO 5493 00 54940Q 649600 549700 548BOQ 648900 550000 6501 OD 55020D 6503DO

g*

548900 643000 549100 549200 549300 549400 -ffi*t7'4S* -8Z'ir30-

549600 549600 549700 549800 548SCQ-ffi**?' 65 0000 55D100 550200 550300 -WW45*

150

JILBEY GOLD EXPLORATION LTD BIRCH LAKE PROJECTROUND POND AREA - GROND MAGNETIC SURVEY AND MM! SAMPLING

TOTAL MAGNETIC FIELD ft MMI SAMPLE SITES

-FI-

BATHURST LAKE AREA

M O K W 7S

JILBEY GOLD EXPLORATION LTD - BIRCH LAKE PROJECTTARGET AREA H08, Claim #1248824 - TOTAL MAGNETIC FIELD

GEOMAPP1NG LTD. - TORONTOFIG. 4

f ) BATHURSTO29477

JILBEYGOLD EXPLORATION LTD -BIRCH LAKE PROJECTTARGET AREA H09, CLAIM #1248616A617 - TOTAL MAGNETIC FIELD

GEOMAPPINGLTD. TORONTOFIG. 5

-~ o 3.

AU 10 Co 49 Ni 16 Pd04 Aa 25

505600

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTTARGET AREA H13


508700

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTTARGET AREA H21 - TOTAL MAGNETIC FIELD

GEOMAPPING LTD. TORONTOFIG. 7

WOMAN-UCHI-CONFEDERATION LAKE AREA

S O S H R

JILBEY GOLD EXPLORATION LTD.BIRCH LAKE PROJECT - TARGET AREA SOA

GROUND MAGNETIC SURVEY - TOTAL MAGNETIC FIELDFIG. 8

JILBEY GOLD EXPLORATION LTD.BIRCH LAKE PROJECT - TARGETS SOB S SOS

GROUND MAGNETIC SURVEY FIG. 9

517500

S11 (C)

517500 61 TBM smoo -92-44-45- 517BQO

JILBEY GOLD EXPLORATION LTD. - BIRCH LAKE PROJECTTARGET AREA S11

MAGNETIC FIELD AND MMI SAMPLE LOCATIONS

FIG. 10

29613519100 519500

519500

metres

JILBEYGOLD EXPLORATION LTDBIRCH LAKE PROJECT - TARGET S13


519700 519600 519900 520000

Z ± -lDip ^ 92.5 Susc ;r 0.0160SI

25 25

metres

50

519700

75

5198QD -92*43' 5199DG 520DDD

JILBEYGOLD EXPLORATION LTD.BIRCH LAKE PROJECT - TARGET S14

GROUND MAGNETIC SURVEY with MODELED SOURCE

FIG. 12

520000-92*42-30'

530400

S15(B

JILBEY GOLD EXPLORATION LTD.BIRCH LAKE PROJECT-TARGET S15

GROUND MAGNETIC SURVEY FIG. 13

5225DO 522800-92-4030-522700 522BOD 523900 523000 533100

-82*40' 523200 533300 533400

Deptfo = 22 Dip" f 63. l

^ 0.01DOS1

T1586Gr 40CoteNi12Y 18Nb3TREE

532500

JILBEY GOLD EXPLORATION LTD - BIRCH LAKE PROJECTGROUND MAGNETIC SURVEY - TARGETS S16 AND S17

GEOMAPPINGLTD., TORONTO MMI prolle of SGS Kimberlite signature (nine elem&ntsjin red FIG.14

•tra?

E324-DD 92-31'7 S"

w Q M UK ten

JILBEY GOLD EXPLORATION LTD., BIRCH LAKE PROJECTTARGET AREAS S37 S, S38

Detailed airborne magnetic survey, Sept 2003 -Vertical magnetic gradient

-f!-

APPENDIX C.

Analytical Certificates SGS Laboratories

3727483

SGSCERTIFICATE OF ANALYSIS

Work Order: 073206To: A.C.A. Howe International Ltd

Attn: Wayne EwertSuite 830330 Bay StreetTORONTOONTARIO, CANADA M5H 2S8

Date 10/07/03

Copy 1 to

P.O. No. Project No. No. of Samples Date Submitted Report Comprises

58 Soil (MMI) 27/06/03 Cover Sheet plus Pages 1 to 6

Distribution of unused material: Pulps: STORE Rejects: STORE

Certified By

, General Manager

ISO 9002 REGISTERED

ISO 17025 Accredited for Specific Tests. SCC No. 456

Report Footer: L.N.R. = Listed not received l.S. - Insufiicient Sample n.a. = Not applicable -- ^ No result *INF - Composition of Lhis sample makes detection impossible by this method M after a result denotes ppb to pprn conversion, Va denotes ppm to "/o conversion

Subject to SGS General Terms anri Conditions

Minerals Services 188J Lesl e Street Toronto ON VnR?M3 t !41B| 445-5755 f 14161 44p-415Z wwwsgs.ca

SGSWork Order: 073206

Method. Dcl.Lini. Unit*.

2925029260292612926229263

2926429265292662926729268

2926929270292712927229273

2927429275292762927729278

2927929280292812928229283

2928429285292862928729288

Date: 10/07/03 FINAL Pai*

MgMMI-D

100ppb

76806050909050003030

39204680796078703500

38704840526083706590

86005310586042804550

58505690881080106980

62504640468052905400

TiMMI-D

Ippb

< 14o

1729

4440

1<}37

523711

CI28

1233323635

fi642

27

14837354249

(YM.MI-1)

1ppb

<]cici<\CI

Ci1

CICI<lcici

2•CI^: I

Ci<l<<<

<<c<l

<l<l<[<[ci

CoMMI-D

1ppb

ciCI< 1<l

4

"Ci•c 1<lO<l

<\1

<l•Ci

ci

<l<l< 1<l<l

11

ci<lci

1ci•cici

1

NiM.M1-U

3ppb

•c 3<3c 3C3C3

C 3<3<3OC3

<3<3c 3C3c 3

c 3C 3Oc. 3

5

fiO0oc 3

<3<3<3c30

RI)MMI-D

1pph

2831563U22

2626333924

2726324744

3327242424

2931383726

2425262528

SrMMI-D

0.1ppb

161135168105

70.5

65.273.7163163

59.6

65.082.3125142147

17795.4

10172.581.5

11.11110144156160

11376.977.786.795.7

YMMI-D

O.Ipph

CO 10.3

O.I0.61.2

1.11.0

"C O.IO.I

1.0

1.62.10.3

CO.lC 0.1

CO.l•7T

1

2

8.1

•--O.Ico ico.i

1.61.31 21.51.5

M)MMI-D

O.IPph

0 101

c: o.i0.10.2

0 30.2

CO.lCO.l

0.2

0.302

CO.]•CO.]O 1

0.10.20.20.30,2

0.50.3

•CO.l•CO.ltO 1

0.30.20.30.20.3

PelMMI-D

0.1ppi.

•c 0.1•CO.l•CO.L•CO.l•co.i

•CO.l•CO.lco.i•co.io.i

•co.ico.i•CO.l"CO iO.I

O.IO.ICO.lO.IO.I

0.1co.iCO.lCO.lCO.l

co.iCO.lCO.lCO.lCO.l

BaMMI-D

O.Ipph

755542370416344

136153947978

97.3

145102135182207

342126152

95.9106

115119250231196

14699.692.1

101118

LaMMI-D

O.Ippb

co.il). 3

O.I0.92.6

3.22.1

0.1CO.l

2.8

3.93.70.5

O.ICO.l

0.22.62.62.53.4

4.02.8

CO.lCO.lCO.l

3.33.32.63,14.1

TaMMI-D

0.5pph

CO. 5CO. 5CO. 5CO. 5CO. 5

C 0.5CO. 5CO. 5C 0.5CO. 5

C 0. 5C 0.5c 0.5CO. 5C 0.5

CO. 5C 0.5C 0.5CO. 5CO. 5

CO. 5C 0.5C 0.5CD. 5CO. 5

CO. 5c 0.5CO. 5CO. 5CO. 5

ftM.M1-D

0.1ppb

CO.l0.5

CO.l175.2

5.03.6O.I

CO 14.2

666.31.1

CO.lCO.l

0.34.64.44.14.4

7.44.4

CO.lCO.lCO.l

6.35.54.75.27.9

FiMMI-D

0.1ppb

CO.lc() 1CO.l

0 20.7

0 70.4

CO.lco.i

0 6

0 90 80.1

CO.lCO 1

CO.l0.70 50.60.6

0 90.6

CO 1CO lCO.l

0.80.80.60.709

N(lMM1-L)

0.1ppi,

CO.l0.3

CO.l0.82.2

2.61.6

CO 1CO.I

2 1

3.22.70.4

CO.lCO.l

0.12.32.02.02.2

3 62.2

c 0.1co.iCO.l

2.62.72.32.53.0

SGSWork Order: 073206 Date: 10/07/03 FINAL

Kk'iiu-nl. Method. Det.Lim. Units.

2928929290292912929229293

2929429295292962929729298

2929929300293012930229303

2930429305293062930729308

2925 l29252292532925429255

292562925729258 Dup 29259*Dup29271

MS Ti Ci Co Ni KbMMI-D MMI-D M.MI-D MMI-D MMI-D MMI-I)

100pph

37501030075407140

10300

•16504670443042805920

549(176904750

1060011300

113001020071706970

12000

1210510930460

5150

25702860364078805570

1pph

4475

584T

1039373642

351

3654

ci\

30-)

< 1

69

179785

294359

28

1ppi)

c 1< 1O

1ci

< i<[cici<l

< l<l<[ci

l

ciciciciO

CI<\<\•CICI

<l<l<l•ciCI

1PPI'

3CIci<l<[

<

cici

<\<\CIci<l

<l112

•CI

<l42

ci<l

3pph

c 3<3<:3<3O

C3O<3c 3O

9OOOO

C3O<3

6c j

C3<3C 3C3C3

^3C3C3OC3

1pph

2726292926

2625252423

2638263233

3232242738

4265744612

579

2933

SI MM [-D

O.Ipph

75.5ISO168134125

81.181 077.172.3102

93.6156

76.4170180

17818610915!187

35.537.844.513.4138

63.980.265.2162135

YMMI-D

O.Ipph

1 0•C O.Icd.i

1.51.3

1.31.51.51.41.4

1.2Cd. l

1.3•CO 1CO.l

CO.l•CO 1

1.10.1

co l

0.2CO 1

O.I0.5(1,6

0,90.82.8

CO.l02

NbMMI-I)

0.1pph

0.3CO. 1cO.l

0.30.2

0.20.20.20.20.2

0.2CO.l

0.2CO.lCO.l

CO.l0.20.30.10.1

CO.l0.10.20.40.5

0.20.20.4

CO.lCO.l

PA BaMMI-1) MMI-D

0.1 0.1ppi) ppi)

CO.co.CO.CO.CO.

co.CO.CO.CO.co.co.co.cOCO.CO.

CO.CO.co.co.co.

CO.CO.CO.CO.CO.

96.7297204156151

98.196.391.492.5

139

MR297

90.9221212

255265157212276

265151211

90.855.6

CO.l 50.1CO.l 79.6CO.l 68.1CO.l 843CO 1 151

LaMMI-D

0.1pph

i TCO.lCO.]

3.12.3

3.85.15.45.23.8

2.8CO.l

5.1CO.l

0.1

CO.lCO.l

2.6CO.lCd.l

(1.2CO.l

0.20.70.7

281.887

CO 10.4

T.iMMI-D

0.5pph

C 0.5C 0.5C 0.5CO. 5CO. 5

CO. 5c 0.5CO. 5C 0.5CO. 5

C 0.5CO. 5CO. 5CO. 5c 0.5

CO. 5CO 5CO. 5CO. 5CO. 5

CO 5CO. 5CO. 5CO .5CO. 5

CO. 5CO. 5CO. 5CO. 5CO. 5

CiMMI-D

0.1ppi)

5.50.7O.I5.64.5

5.98.39.18.47.3

4 9CO.l

9.00.20.1

CO.lCO.l

4.90.2

CO.l

0 40.20.41.61.6

4.72.9

14.9O.I0.8

I'r

MMI-D0.1pph

0.6co.iCO.l

0.60.5

0.71.01.11.10.9

0 6CO.!

1.1CO.lCO.l

CO.lCO.l

0.6CO.lCO.l

CO 1CO.lCO.l

0.20.2

0.60.41.7

CO.lCO.l

NilMMI-D

0.1ppb

2.6CO.lco.l

2.42.0

2.53.43.53.52.9

2.2CO.l

3.6co.ic 0.1

cO.lco.l

1.90.1

co.i0.3

co.i0.20.80.9

2.41.76.6

cO.l0.3


Elemeiil. Method. Di't.Um. l nils.

'Dup 29283*Dup 29295*Dup 29307

MgMMi-n

100PI*

678046806790

liMMi-n

1p]ib

<l35

4

CrMMI-D

1|)|)b

<lO0

CoMMI-I)

1ppb

01

O

NiMMl-U

3ppb

O6

0

RI)M.M1-D

1ppb

282628

SrM M 1-0

0.1ppli

15581. K

150

YM.MI-I)

O.Ippb

f- 0.11.102

NI)MM1-I)

O.Ippb

c: O.I0.2O.I

Pd\1MI-0

0.1ppb

*:0.1 iO.I CO. l

BilMMI-D

0.1ppi)

228101200

lM

MMI-I)O.Ippb

*;o l4.50.2

TaMMI-D

0.5ppb

o.).5<0.5<0.5

CeMMI-D

0.1ppb

f^(i.l8.00.3

Pi-

MMI-0O.Ippb

c;d 10 8

<(| 1

NclMMI-D

O.Ippb

c; O.I2.80.2


Elcincni. Mithnd. Det.Lim.

2920 1 29262 292()3

292W29265292662926729268

2926929270292712927229273

2927429275292762927729278

2927929280292812928229283

2928429285292862928729288

SinM.M1-D

0.1pph

OJ0.30.2(1.30.5

0.60.40.50.50.4

0.60.50.10.1

*:().l

0.20.40.40.40.4

0.70.50.10.10.1

0.50.40.50.5o.r.

CdMMI-D

0.1pph

*.'() 1<0. 1*:0.1

0.20.4

0.40.3

•CU.I<0.1

0.4

0.50.4

•cO.l<0.1^0.1

•CO.l0.40.30.40.3

0.60.40.4

<0.1oj.l

0.40.40.30.50.5

TbM.MI-I)

0.1ppi)

-r 0.1<o.l*:0.lco.i•'0.1

•co.i•cQ.l•CO.l^;o.i•o) i

-C O.I01.1f. O.I•co.i^0.1

•c. 0.1•CO.l<0.1^:0.1<0.l

•i 0.1<0.1c: 0.1•CO.l•cO.l

•CD.l<0.10).l^,0.1<0.1

lM.MI-

0.PP

<^}.<o^:0<0.

0.

0.;o<0^;o.

0.

00.

<^J.<o.c:().

<0.0.00.0

00

fi Q.•CO*;0

0.0.0.00

r Y bJ MMI-D1 0.1l ppi)

c 0.1•CO.lo),l•CO.l

0.1

J 01•co.i<(l i^;o.i

01

! 0 2! 0.1

cO.l<0.1s:().l

•cO.l0.10.10.1

•c 0.1

0,2<(l.lttO.l<0.1^;() 1

0.10.10.10.20.1


Element. Method. Det.Lim. l nils,

2928929290292912929229293

2929429295 2929d2929729298

2929929300293012930229303

29304 293(15293062930729308

2925129252292532925429255

2925629257 2925S*Dup 29259*Dup29271

SinMMI-l)

0.1ppi)

0.30 2

cO.l0.50 5

0.40.60 0().()0.6

0.40.20.50.10 1

0.10.10.50 1O.I

02•CO 1

0.2020.2

0.40.3Lil0,10 l

CclIMMI-D

0.1PI'''

0.3•CO. lt O.I

0.504

0.50.50.40.50.5

0.4CO. l

0.5CO.lcO.l

CO.lcO.l

0.4cO.l01. l

CO 1•CO. 1cO.l

O.I0.2

0.30.31.0

CO.lCO. I

Tb EiMMI-D MM1-D

O.I 0.1pph pph

-.'O. 0.1•O).

<o.•((}.CO,

co.<o.<o.co.co.

0)co.CO.<(lCO.

co.iCO.l

O.I0.1

0.10.20.10.20.2

01CO.I

0.1CO.lcO.l

•au <o.lCO. CO.lco. o.iCO. CO.Ico.i co.i

CO.I CO.ICO.! CO.ICO 1 cO.lcu.i co.iCO.I cO.l

co.i co.ico.i co.i

0.1 0.2cO.l CO.lCO.l CO.l

YMMI-l

0.

pp

CO.COCO.

o.:0.

0.20.1O.I0.1O.I

0.1co.i

0.1CO.CO.

CO.CO.

0.co.co.

CO.co.CO.CO.co.

co.CO.

0.3CO.lCO.l


Klemelil. Method. Det.Uin. Units.

*Dup 29283*Uup 2')2'XS 'Dup Vi 307

Sin

MMI-I) 0.1 PI*

0.1 (l.S 0.2

Date: 10/07/03

GilMIMI-D

0.1 PPI'

Tb MMI-D

0.1 ppi)

Er MMI-D

0.1 ppi)

Yb MMI-D

0.1 pph

FINAL

CERTIFICATE OF ANALYSIS Work Order: 073280

To: A.C.A. Howe International Ltd Attn: Wayne EwertSuite 830330 Bay StreetTORONTOONTARIO, CANADA M5H 2S8

Date 1 7/07/03

Copy 1 to

P.O. No. Project Mo. No. of Samples Date Submitted Report Comprises

Jilbey21 Soil (M M l)03/07/03Cover Sheet plusPages 1 to 2


Certified By

Dr. fHuah de Souza, General Manager

ISO 9002 REGISTERED


Report u ooter: L.N.R. = Listed not received l.S. = Insufficient Sample n.a. = Not applicable -- = No resull 'INF - Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, "/o denotes ppm to "/b conversion

Subject to SGS General Terms and Conditions

Minerals Services 18651 RsliR Street 'oronto ON M3B2M3 K416M455755 f M'6) 445-4152 www.sgs.ca

Member o' the SGS GrojD ISocieTe Generale de Surveillance*


Element. Md hud. Det.Lim. Units.

2930929.310293112931229.31.3

2931429315293162931729318

2931929320293212932229323

2932429325293262932729.328

29329*Dup 29309*Dup 29321

Date: 17/07/03 FINAL

M KMMI-D

100ppb

2330208003107880

1901)0

15900764013901210790

214007103280202(1

15700

92507310

10300119000990

1280023703170

TiMMI-D

1ppb

275

2556

< 1

•Ci

48446

5205

521

191

•C l

11400•CI< i62

•CI23

2

CrMMi-n

1ppb

1•ci< 1

T

•C 1

< 115

1<l

4

•ci4

•ci12

j14

<\^,1

8

3<l•ci

diMMI-D

1ppb

4•ci

12<l<\

Ci327

1

1ci

31

< 1

< 1542

-Ci

c 153

NiMMI-D

3ppb

3790

•C3

<3•C 3

4O

4

40OO

4

Oc 3OOC3

O•C 3^3

KbMMI-D

1ppb

399

171213

2847346861

4111373313

939605725

153739

SrMMI-D

O.Ipph

69.0595249300221

232101

58.040. 418.3

72.5205215261426

324110242282189

41072.8203

yMMI-D

O.Ippi)

0.40 20.40.6

co l

•JO 11 50 20.1O 9

0 10 20.30 8

•CO 1

0 71.7

•CO 10,10 7

0.30.40 3

NI).MMI-D

0.1ppb

•CO.lCO 1•CO.l•CO.l•CO.l

•CO.l1.2

•CO.lCO.l

0.5

CO.l•CO.l•CO.l

0.1CO.l

•CO.l1.2

•s; 0.1•CO.l•CO.l

cO.l•CO.!•CO.l

PdMMI-D

O.Ippb

•cO.l•CO 1•co.iCO.l•co.i

•co i*:o.iCO 1CO.lcO.l

<0.1<0.l<0.l<0.1<0.1

co.i0.2

<0 1CO.l•CO.l

0.2-co i•CO.l

B;lMMI-D

O.Ippb

26050.8

11867.190.9

109121

76.7138111

40671.0233

74 174.7

9K.9157105145

94.9

126269244

LaMMI-D

O.Ippb

090.40.82.20.1

•CO.l5.60.40.33.1

0.30.60.62.0

•CO.l

0.91.80.20.2l. 7

(I.40.90.7

TaM.MI-D

0.5ppb

co. 5•CO 5CO.5c 0.5CO. 5

CO. 5•CO. 5•CO.5•CO 5CO, 5

•CO. 5CO. 5•CO. 5•CO. 5•CO. 3

CO. 5•cO.5•CO 5•CO.5C l). 5

CO. 5•CO.5C 0.5

Ci-MMI-D

0.1ppb

2.00 92.05.00.2

CO 111.2

1.30.6

11.5

0.71 5i.y4.5

•CO.l

1.912.80.50.33.7

0.72.12.2

PrMMI-D

0.1ppb

0 2*"0 1

020 5

<0 1

CO 11.20.1

CO.l07

CO 10 1020 5

•CO.l

0.21.2

•CO 1*r.0.l

04

•;0.10.20.2

[NilMMI-D

0.1ppb

0.80.30.92.00.1

•CO.l4.20.40.32.9

0.40.50.72.0

CO.l

0.81.60.20.21.4

0.40.90.8


I'.kimiK. Method. Dcl.Uni. liiits.

2930929310293112931229313

2931429315293162931729318

2931929320293212932229323

29.32429325293262932729328

29329*Dup 29309*Dup 29321

SinM.MI-D

0.1ppb

0.2CO.]

0 20.3

CO 1

01.10.7

<0.10.10.5

0.2O.I0.20.3

•c 0.1

0.20.80.1

CO 10.3

0.10.20.2

l, t!MMI-D

0.1ppb

O.Ico.i

0.10.3

<().l

co.i0.7

CO.l<0.1

0.4

CO.lCO.l<().l

0.3<0.1

0.20.7

'-O.I<n.l

0.2

co i0.20.1

Ih KrM.MI-D MMI-D

O.I 0.1ppb ppb

•COf.',}coO.}-.'.0

co<0.ci)COci).

coCOcdCOCO

CO.lCO.lcO lCO.Ico.i

CO 10.2

CO 1CO I

0.1

co.iCO.lCO.lCO.lcO.l

CO.l CO.lCO.l 0.2cO 1 CO.lcol co.iCO 1 CO 1

co.i co.iCO 1 CO.lCO 1 CO I

VbMMI-D

0.1ppb

cO.lcO.lCO 1CO.lCO.l

CO.l0.2

CO.lCO.lco.i

•CO.lcO.lCO.lCO.lCO.l

CO.l0.2

c 0.1CO.Ico.i

CO.lCO.lCO 1




Date 1 7/07/03

Copy 1 to


Jiibey43 Soil (MM!)07/07/03Cover Sheet plusPages 1 to 4

Distribution of unused material:Pulps: STORE Rejects: STORE

Certified By

Dr. Hugh pe Souza, General Manager

ISO 9002 REGISTERED


Report Footer: L.N.R. = Listed not received ita. = Not applicable 'INF M afte

l.S. - Insufficient Sample ~ No result= Not applicable — = No result

^ Composition of this sample makes detection impossible by this method ir a result denotes ppb to ppm conversion, "/o denotes ppm to ",'a conversion


-. Mnera s Services 188b Leslie Street Torortc ON M3B2M3 1(4151445-5755 f 1416] 445-4152 www.sgs.ca

Membe- of the SGS Group (Sociele Generale de Survei'lance'

Work Order: 073325 Date: 17/07/03 FINAL I'aijc l ,.l'

F.lfiiicnl. Method. Del.Lim. Unils.

29.13029331293322933329334

2933529.136293372933829339

29340 293-11 29342 293-1329344

2934529346293472934829349

2935029351293522935329354

2935529356293572935829359

MgMMI-D

100ppb

44208430535085909800

9500Q66099SO73106200

60905020735078308750

9790') 540

1050093706880

66305960422060303860

58205700503034905470

liVIMl-1)

1ppb

2425ci

3ci

7•SI

26

0

3238231

34

c 1<\

3

22

318

29

3291739

7

CiMM1-1)

1ppb

•cicic 1cic 1

•ci< 1cici<l

<[ci<lc 1CI

••-l< 1<lcic 1

o•ci< l< 1CI<lCI<lo<]

CdM.MI-I)

1ppb

112

CIci

c 1<lC 1<l<l

34

•ci<l•CI

o<lc 1•CI<l<l<l

2<l

T

<lci

231

NiMMI-D

3ppb

65

12C 3C3

OOc 3

3O

65

•c 334

4O

33

O

54y

c 34

O5484

RI)MMI-D

1ppi)

2032173148

2323402540

2220283741

2535442729

2627272420

3723292124

SiMMI-D

0.1ppi)

65 81 17

95.6129143

161134144144136

1(1379.1

145164135

151135147150139

145120

8(1.8101

67 9

126104110

67.298 5

YMMI-D

O.Ipph

121.2

cO 10.2

•CO. I

CO.lCO 1•CO.lco 1CO 1

1 71.402

CO.lCO.l

•CO.lCO 1•CO.lCO.l

02

0.20.31.60.51.4

0.31.4I.I1.80.6

M)MMI-I)

O.Ippi)

•CO 1•co.ico.]•co. 1•CO.l

•CO.l•CO.l•co.ico.i•co.i

•co.i•co.i•CO.lCO.lc: o.i

•CO.l•co.iCO.l•CO.lco.]

•co.icO.lco.iCO.ICO.l

CO.ICO.]CO.l•CO.lCO.l

PllMMI-D

0.1pph

•'0.1co.iCO.l•co.iCO.l

co.icO 1CO.lCO.lCO.]

CO.l•CO.l•CO.ICO.]CO.l

•CO.lcolco.i•c 0.1CO.!

CO.I•CO.lc(UCO.!CO.l

CO.lCO.lCO.lCO.lCO.l

It.iMMI-D

0.1ppb

1772 'M117421336

299344449532

1059

504383665706598

299361315476561

549748561703240

341369469405529

l,aMMI-D

0.1ppli

2.01.4

c U.I0.2

CO.l

CO.CO.CO.cO.co.

2.42.50.20.3

CO.l

c 0.10 1

CO.lc 0.1

0.3

0 20.23.50.42.7

0.31.71.15.00.7

TyMMI-D

0.5ppb

CO. 5CO 5CO. 5CO. 5CO. 5

CO. 5CO 5Cd. 5CO 5Cd. 5

CO 5CO. 5COSCO. 5CO. 5

CO. 5CO 5•CO. 5C 0.5CO. 5

Cd-5CO. 5CO. 5C 0.5CO. 5

•C0.5C 0.5C 0.5CO. 5CO. 5

l eMMI-D

0.1ppb

4 3290 20.4

•CO.l

O.ICO.lCO.l

0.7co.i

5.54.90.30.1

CO.l

•CO.l0 2

•CO.ICO.I

0.5

0 J0.47.91.05.8

0.53.82.5

K). S1.4

PrM MI-1)

0.1ppi)

0 50.3

c 0.1<(]^CO.]

co.ico.iCO.lCO.ico.i

0.60.5

CO.lco.iCO.l

cO.lC01CO.lCO.lCd.l

cd lCd.]

d. 8d.l0.0

CO.I0.40.31.1O.I

NilMMI-D

0.1ppb

2.21.30.10.2

CO.l

CO.co.•Cd.Cd.cd.

2.32.20.2

CO.lcO.l

cO.lCO 1CO.lCO.l

0.2

0.20.23.4d. 52.8

0.21.71.24.70.6

Work Order: 073325 Date: 17/07/03 FINAL

Method. Del.Liin.Units.

2936029361293622936329364

2936529366293672936829360

293702937129372*Dup 29330*Dup 29342

*Dup 29354*Dup 29366

MSMMI-D

100ppb

49404380438052203660

65906650505018801410

10903640526040007300

39406570

TiMMI-D

Ippb

1729301220

32

8644422

8543

10930

c l

341

CiMMI-D

1ppb

cic 1ciC 1c 1

c 1ci89

1CI

3•ci

4•CI

c i

ci< 1

CoMMI-D

Ippb

21

^: lCI

3

CIci

1912

32

221

CI

3•CI

NiMMI-D

3ppb

44445

33

8154

65

1184

66

RbMMI-D

1ppb

2622211920

3737892983

5746202225

2036

SiMMI-D

0.1ppb

87771.168281 663.1

1-13147166158

372

380907

10764 9

145

689150

YMMI-D

0.1ppi)

1.01.31.40.81.2

•C 0.1CO 1

4.10.30.2

0.40.11.31.50.2

1.5-CO.l

1MbMMI-D

O.Ippb

CO 1•CO. 1•S 0.1CO.lCO.lco.i•CO.l

? ico.i•co.i

•CO.lco.iCO.lco.iCO.l

CO.lCO 1

PdMMI-D

0.1Ppb

c 0.1•CO.lcO.l•CO.lcO.l

cO.lCO.l

0.2;:0.1CO.l

CO.lCO.lcO.lCO.lcO.l

CO.lcO.l

BaMMI-D

0.1ppb

526162139161322

338320506

95.7129

128246170166653

210323

l,aMMI-D

(I.IPl'l'

1 42 02 31.02.5

CO 1CO.l13.30 80.2

0.80,31.52.40.1

3.3CO 1

TilMMI-D

0.5ppb

C 0.5CO. JCO. 5CO. SCO. 5

C 0.5CO. 5C0.5C0.5C 0.5

C 0.5CO. 5C 0.5CO. 5C 0.5

CO 5CO. 5

CeMMI-D

0.1ppb

3.24.34.72.15.6

CO.l0.1

32.11.70.5

2.91.15.45.10.3

6.4CO.l

P.MMI-D

0.1ppb

0.40.30.60.20.6

CO.lCO.l

3.60.2

CO.l

0.2CO 1

0.40.6

CO.l

0.8CO.l

NclMMI-D

0.1ppb

1.52.12.21.02.5

CO.lcO.l14.40.90.2

1.0031.92.60.2

3.0c 0.1


Method. Dct.Lim. l nits.

2933029331293322933329334

2933529336293372933829339

2934029341293422934329344

2934529346293472934829349

2935029351293522935329354

2935529356293572935829359

SinMMI-D

0.1ppi)

0.40.3

t: O.I0.20.1

O.I0.10.20.20.4

0.70.50.3O.J0.2

•c 0.10.10.10.20.2

0.20.30.70-40.5

0.20.50.40.90.3

GelMMI-D

0.1ppi)

0.40.3

< Q lCO.I•--0.1

<0.1CO iCO.l<0.1<(l.l

0.504

CO.l<0.1<0.1

<0.1CO 1<().lCO.I<(i.l

<0.1•CO.l

0.50.10.5

CO.l0.40.30.70 2

TbMMI-D

0.1Pl'l'

CO 1•.-.o.iCO.l<0. l•,0 1

CO.lCO.lCO.]CO.lco.i

CO 1co.iCO. JCO.lCO.l

co iCO lCO.lCO.LCO l

CO 1co iCO.ICO 1c U.I

CO 1CO 1co.iCO.ICO 1

F.iMMI-D

O.Ippi)

O.IO.I

CO 1CO 1CO.l

co.ico.ico ico.ico i

0 1O.I

CO 1co.iCO.l

CO 1co.ico iCO.lCO.l

CO.lCO.I

0.2co i

01

co.i0.20.10.2

CO.l

VI)MMI-D

0.1PI*

0.10.1

CO 1co.iCO.l

co.iCO 1CO.]CO 1CO.l

0 1O.I

CO.lco.]CO.l

CO.lCO.lco.iCO.lco.iCO.lCO.I

0.2co.i

0.1

CO.l0.1

CO.I0.2

CO.l


Method. Det.Liin. llniK

29360 29J6I293622936329361

2936529366293672936829369

293702937129372*Dup 29330*Dup 29342

'Dup 29354 'Dup 29366

SmMM 1-0

0.1ppb

0.50.40 40 30.5

0.1CO.l

2.40.2

CO.l

0.2O.I0.40.50.3

0.60.1

(MMI

0PI

0(l000

<()CO

20

-;0

0000

CO

0CO

;d T1) \1MI-I

1 0.)b pp

3 co.4 CO4 "id.3 CO4 -cd.

1 CO1 c 00 (I..

1 cd1 CO.

1 cdi cd4 Cd.5 CO.1 CO.

5 cd1 CO.

l) Er} IMMI-0

0.1b ppb

0.1O.I0.1

C 0.10.1

c o.iCO 1

0.5c 0.1cO.l

C 0.1CO.l

0.10.1

C 0.1

0.2co.i

VI)M.MI-I)

0.1ppi}

CO 101

CO.l0 10.1

CO.lCO 1

0.5CO 1cO.l

CO 1CO.l

0.20 2

CO 1

0 1CO.l



Attn: Wayne EwertSuite 830"30 Bay StreetTORONTOONTARIO. CANADA M5H 2S8

Date 29/07/03

Copy "i to

P.O. No. Project No. No. of Samples Date Submitted Rennrt Comprises

Jilbey25 Rock 1 8/07/03 Cover Sheet plus Pages 1 to 1

Distribution of unused material:Pulps: Discarded After 90 Days Unless Instructed!!! Rejects: Discarded After 90 Days Unless Instructed!!!

Certified By

Dr. Hugh de Souza, General Manager

ISO 9002 REGISTERED


L.N.R. " Listed not received l.S. - Insufficient Sample n.a. - Not applicable - - No result " INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, "/o denotes pptn to "A conversion

Subiect to SGS General Terms and Conditions

Minerals Services 1885 Leslie StrfiRt 'oronto CN M3B2M3 11416''145-5755 f (416) 445-4'52 wwwsgs:a

Member of the SGS Grojp ISociete Ganerale de Sun/e'Hanca!

SGS\Vork ()rdcr: 073537 Date: 29/07/03 FINAL Page i of i

AllF A 30 1

I

4106?047112S

232 20

^. l < l ^ l

< l 1.1< l 10 14

182154

00

.'04 < l3.1711941176

21.101



Attn: Wayne Ewert Date : 31/07/03Suite 830330 Bay StreetTORONTOONTARIO, CANADA M5H 2S8

Cony 1 to :

P.O. No. :Project No. : JilbeyNo. of Samples : 12 RockDate Submitted : 18/07/03Report Comprises : Cover Sheet plus

Pages 1 to 3

Distribution of unused material:Pulps: Discarded After 90 Days Unless Instructed!!!Rejects: Discarded After 90 Days Unless Instructed!!!

Certified By : p f y y '-i-. \ '4*-.-..:


ISO 9002 REGISTERED


R: pu:! u ootor: L.N.R. = Listed not received l.S. = Insufficient Sample n.a. ^ Not applicable -- - No result 'INF = Co-npusition of this sample makes detection impossible by this method M after a result denotes ppb to opm conversion. ah denotes ppm to 94 conversion


SGS Canada : nc. Mineral Services 1885 Leslie Street Toronto ON MSB 2M3 1(^15)445-5755 f (416)445-4152 www.sgs.ca

SGSWork Order: 073338 Date: ..•07/03 FINAL

Element.Method.Dct.Lini.Units.

3 1 22631227312283122931230

3123131232312333123431235

3123631237'Dun 31226

AuFA301

1ppi)

765326740233

5^000

17(16268

1384^000^000

^000943804

UiFA30G

0.03g/int

3.22

22.06.7

5.7-

Ik-ICP80

0.5ppin

n.a.ti-;in.an.an.a

n.an.a.

*:0.5<(}.S•S0.5

n.a.n.a.n.a

NaICPSO

0.01•n

.a.

.'A.

.a.

a..a.

n.a.n.a.

0.141.560 07

n.a.n.a.n.a.

MBICPSO

0.01"k

n.a.11 H

n.a.n.a.n.a.

n.a.n.a.

0.070.600.02

II LI.

n.a.n.a.

AlICPKd

0.017c

l .:l.i at a.i a.i a.

n an.a.

0.303.3*10.13

n a.n.a.n.a.

PICP80

0.01K

n.a.n.a.n.a.n.a.n.a.

n.a.n.a.

0.020.01

^1.01

n.a.n.a.n.a.

KICPSO

0.01K


n.a.n.a.

0.070.870.03

n.a.n.a.n.a.

C;iICPSO

0.01•ft


n.a.n.a.

0.220.220.01

n.a.n.a.n.a.

St1C PSI)

0.5ppm

n.a.n.a.n.a.n .'.n.a.

n.a.n.a.n.66 3

•CO. 5

n.a.n.a.n.a.

TiICPXO

0.019r


n.a.n.a

0.010.16

•c 0.01

n.ii.n.a.n.a

\ICPSO

2ppm

n.a.n.an.an an.a.

n.a.n.a

672O

n.a.n.a.n.a.

C rICPNO

1ppm

n.a.n a.n.a.n an.ii.

n a.n.a.223213196

D. an.a.n.a.

MnICPSO

2ppm

n.a.n.a.n.a.n an.a.

n.a.n.a.

55124

36

n a.n.a.n.a.

FeICPHO

0.01ci


n.a.n.a.279

10.95463

n an.an.a.

CoICPSO

1ppm

n.a.n n.n.a.n an.a.

n.a.n.a.

8176

u. a.n.a.n.a.

SGSWork Order: 073538 Date: 3107/03 FINAL

Element. Method. Det.Liin. Units.

3122631227312283122031230

3123131232312333123431235

3123631237 "Dup 31226

NiKT8U

1PI""

li a.M a.

1] LI.

n a.li. a.

11. a.li. a.

319740

n a.n.a.n.a.

CuKT80

0.5PI""

n.a.ii.ii.n.a.nn.n n

n.a.n.a.

> 1000058100050

n.a.n.a.n.a.

/nICL'80

0.5ppin

ii-u.n.;i.n.a.n.a.n.a.

n.ii.ii. a.6.0

18.21 6

n.a.Il.il.n.a.

A-,ICP80

3ppin


n.a.n.aO

4^3

n.a.n.a.n.a.

Sricpsn

0.5ppin

n.a.n.y.n.a.n.a.n.a.

n.a.n.a7.1

35.0•CO. 5

n.an.a.n.a.

Y1CTSO

0.5ppin

n an.an.an.a.n.a

n.a.n.a

*C0.53.1

<(}.5

n.H.n.a.n.a.

ZiICP80

0.5ppin

l ala.i .a.i a.i .a.

n.a.n.a.Ci. 4

()4.ft6.3

n.a.n.a.n.a.

MnICPSO

1ppin

n an.a.n.a.n.a.n.a.

n.a.n.a.

413

H

n . a .n.a.n a

V|!KT80

0.2ppin

n.iin.a.n a.n.a.n.a.

n.n.n a4.8

:> 10.0>l().()

n a.n a.M.a.

CdICP80

1ppin


n.a.n a<\

o*:l

n.a.n.a.li. a.

SnICP80

10ppin

n an.an.a.n.a.n.a.

n.a.n a

•C 10*:l()•S 10

n.a.n.a.M.a.

SbICP8U

5PI""

n an.a.n.an.a.n.a.

n.a.n j<5

6•C 5

n.A.n.a.n.a.

Ba1CP80

1ppin

n. an.a.n.H.n.H.n.a.

n.a.n.a.

21183

13

n.a.n.a.n a

LaICP80

0.5ppin

n an.a.n.a.n a.n.a

n.a.n a.1.23.0

^).5

n.an, a.n a

\\rcpso

10ppi"

n an.a.n.a.n.a.n.a.

n.a.n.a.

•CIO

16^0

n.a.n.a.n a.

PI)KPSO

2PPI"

n.an.a.n.a.n.a.n.a.

n.a.n.a

121516

n.a.n.a.n.a.

SGSWork Order: 073538 Date: 31 07/03 FINAL

F'.k-Mitnt. Method. Det.Lim. ('nils.

3122631227 3122S 3122 l;31230

3123131232312333123431235

31 236 31237 *Dup 31226

Hi ICP80

PPI"

n a n.a.

n.a. n.a.

n.a.n a

7 7 ft

n.a. n.ii. n.a.

LiICP80

lppni

n.a. n.a. n.ii. n.a. n.a.

n.a.n.a.

l5

n.a. n.a. n a

Au AA73

0.3g lilt

2.0 0.6 1.1

•C0.3 5.6

7.30.55.7

60.015.2

15.') 2.1 1 i




Date 01/08/03

Copy 1 to ray. knowles @sympatico.ea


Jilbey73 Soil (MMI)l 8/07/03Cover Sheet plusPages 1 to 6


Certified By

, General Manager

ISO 9002 REGISTERED


Report Footer: L.N.R. = Listed not received l.S. — Insufficient Sample n.a. = IMol applicable — = No result *INh = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, 07o denotes ppm to "/o conversion


SGS Canada Inc. Mineral Services 1885 Leslie Street Toronto ON MSB 2M3 1(416)445-5755 f (416)445-4152 www.sgs.ca

SGSWork Order: 073539 Date: 01/08/03 FINAL i^ i ,,i ,,

20.17320374203752037620377

20378 20370 20380 20381"20382

203832038420385 2038d 20387

20380203002030120302

2030320304203052939620397

2930820390

2940129402

MHMMI-U

100

n.a.n a.n.a.n.a.n.a.

n.a. n.a.n.a.

n.a.n.a.n.a.

n.a.


n.a.11.3.

n.ii.n.a.n.a.

n.a.ii.a.n.a.

881011710

Ti MMI-D

1


n.a.n.a.

n.a.n.a.ii.ii.

n.a.

n.a.11 an.a.n.a.n.a.


n.a.n.a.n.a.

1<l

(, M.M1-I)

1

n.a.n.iin.a.n.iin.a.

n.a. n.a.n.a.

n.an.a.n.a.

n.a.

n.a.n.a.n.a.n.ii.n.ii.

n.an.a.n.j.n.a.n.a.

n.a.n.a.n.a.0•ii

di MMI-D

1

n.a.n.a.n.a.n.a.n.a

n.a. n.a.n.a.

n.an.a.n.a.

n.a.



n.a.n.a.n.a.ci•CI

Ni MMI-D

3

n.an.iin.an.itii.a

n.ii n.ii.n.ii.

n.a.n.iin.a.

n.a.

n.ii.n.a.n.a.n.an.a.

n.an.a.n.a.n.a.n.a.

n.a.n.a.n.a.0C 3

Kb MMI-D

1

n.a.ii.a.n.a.n.a.n.a.

n.a.n.a. n.a.n.a. n.a.

n.a.n.a.n.a.

n.a.



n.a.n.a.n.a.

3745

Y MMI-D

0.1


n.a.n.a. n.a.n.a. n a.

n an.a.n.a.

n.a.


n.a.n.a.n.a.n.a.n.ii.

n.a.n.a.n.a.0.1

CO.I

M) MMI-D

0.1

n.a.n.a.n.a.n an.a.

n.a.n.a. n.ii.n.a. n.a.

n.an.a.n.a.

n.a.

n.a.n.a.n.ii.n.a.n.a.


n.a.n.a.n.a.0.1

CO.I

I'd

M.M1-I) O.I

n.a.ii.ii.n.a.n.a.n.a.

n.a.n.a. n.a.n.a.n.a.

n.an.a.n.a. n.ii.

n.a.n.a.n.an.an. a

n.an.an.a.n.a.n.a

n.an.an.a.

CO.I<0.l

Ua MMI-D

0.1

n.a.n.a.n.a.n a.n.a.

n.a.n.a. n.an.a. n.a

n.an.a.n.a.n.a. n.a.



n.a.n.a.n a.294475

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SGSWork Order: 073519 Date: 01/08/03 FIN A l

(Clement. Method. Rul.ljin. Initv

2940.'

29104294052940629407

2940829409291102941129412

29413

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29418 2941') 291202942129422

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F'.lr infill.Method.Det.Lim.Units.

2443129434294352943ft29437

2943829439294402944 129442

294432944429445*Dup 29373*Dup 29385

*Dup 29397"Dup 29409'•Dup 29421'Dup 29433*Dup 29445

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SGSWork Order: 073539 Date: 01/08/03 FINAL I'auc 4 o! d

Elt'iiU'iit. Method. Det.Lini. I'liits.

2937329374293752937629377

2937829379293802938129382

2938329384293852938629387

2938829389293902939129392

2939329394293952939629397

2939829399294002940129402

OdMMI-D

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1 330.733.121.712.73

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21 57.520.5823.12.57

1.221 .05O.KI0.942.37


KlemeiH. Method. Di'l.Liin. I'nils.

2940329404294052940629407

2940829409294102941129412

2941329414294152941629417

2941829419294202942129422

29423 29-121294252942629427

29-128 2942 ')294302943129432

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0.160.1 'J0.150.140.13

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0.190.180.31

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0-179

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12542292666

1716276623

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1635

453

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567475

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0 164.332.132.562.26

1 .020 76j. 060.511.31

0.702.008.721.442.01

5.617.334 835.204.64


Element. Method. Del.Lin). Units.

2943329434294352943629437

2943829439294402944129442

294432944429445*Dup 29373*Dup 29385

*Dup 2()397*Dup 29409*Dup 29421*Dup 29433*Dup 29445

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677087

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4.3S9.73H.I17.23.71

2.310.960.21(1.440.17

0.200.241.201.454 69

2 990.180.734.191.06



Date 04/09/03

Copy 1 to


Jilbey72 Soil (MMI)14/08/03Cover Sheet plusPages 1 to 6


Certified By 4L-7U ^-±o,-. Hugh de Souza, General Manager

ISO 9002 REGISTERED


Report Footer: L.M.R. = Listed not received l.S. = Insufficient Sample n.a. ™ Not applicable - = No result 'INF = Composition of this sample makes detection impossible by this method M after a result rlenntes ppb to ppm conversion. c!6 denotes ppm to Vo conversion

Subject to SGS General Terns and Conditions

SGS Canada Inc. Minerals Services 1885 Leslie Street Toronto ON MSB 2M3 1(416)445-5755 f (416) 445-4152 www.sgs.ca

Member of the SGS Group (Societe Generals de Surveillance)


EltlllL'llt.

Mf t hod. Del.Liin. Units.

2944629447294482944929150

2945129452294532945429455

2945629457294582945929460

2946129462294632946429465

2946629467294682946929470

2947129472294732947429475

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13050

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18601550

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O.Ippb


n.a.n.a.n a.0.2

CO.l

1.72.4

CO.l2.22.6

0.23.27.55.807

0.1CO.I

0.50.2

CO.l

0.20.50.50.20.2

SinMMI-D

O.Ippb

n.:tn an.an.a.n.a.

n.a.n.a.n.a.01

co.i

0.30.40.10.40.5

0.10.51.11.00.3

0.10.20.

COCO.

CO.t).02

CO.l0.1


FUiin'iil. Method. Del.Lim. Knits.

2947629477294782947929480

2948129482294832948429485

2948629487294882948929490

2949129492294932955129552

2955329554295552955629557

2955829559295602956129562


MBMMI-U

100ppi)

8903920393039005020

162801618018220

n a.n.a.

n . ;i .n. a.n.a.n.a.380

71502639026710

n.a.n.a.

n.a.n.a.n. ri.n.a.n.a.

n.a.490

152016310

740

TiMMI-U

1pph

1 115141916

135

n.a.n.a.

ii.ii.n.a.n.a.n.a.O

311

n.a.n.a.


n.a.91

125•ci

3

(rMMI-l)

1ppi)

ci<]CI< 1-ci

< \ci

2n.a.n . ;i .

n.a.n.an.a.n.a.ci

ci4N

D. a.n a

n.a.n.a.n.a.n.a.n.a

n.a.613

Ci

CoM.M1-D

1ppi)

2•CI•CCl

< 1o

•CI

< 1

<ln.a.n.a.

n.a.n.a.n.a.n.a.< 1

3O< 1n.a.n.a.

n.a.n.an.a.n.a.n.a.

n.a.CI

1•ci

2

NiAIMI-D

3pph

4<3

73

C3

44

On.a.n.a

n.a.n.a.n.an.a.C3

1944

n.a.n.a.


n.a.0

34

C3

KbMMI-D

1pph

(.610101010

4104

n.a.n.a.

n.a.n.a.n.a.n.a.

33

154

n.a.n.a.

n a.n.a.n.a.li a.n a.

n.a.29286

61

VMMI-l)

0.1pph

cU.l0.50.40.40.5

CO.lCO.lCO.l

n.a.n.a.

n.a.n.a.n.a.n.a.

cO.l

0.2CO 1CO l

n.a.n.a.


n.a.1.7(1.5

CO.lcd .1

NhMMI-1)

0.1pph

CO 1CO 1

0.1O.I

cO.l

<0.1<0.1CO.l

n.a.n.a.

n.a.n.a.n.a.n.a.

•c 0.1

<0.1co i<0. l

n.a.n.a.


n.a.0.50.4

CO.lCO.l

I'd

MMI-UU.Ipph

< 0. 1•CO.l•CO.lCO.l<().l

•CO.lCO 1<0.1

n.a.11. a.

n.an.an.a.n.ii.

•CO.l

•CO.lCO.lco.i

n.a.n.a.

n.an.a.n.a.n.a.n.a

n.a.•r 0.1<().l<0.1'CO.l

BaMMI-D

0.1pph

12960.759.05f).664.0

10892.9111n.a.n.a.

n.a.n.a.n a.n.a.354

10067.265.3n.a.n.a.

n an.a.n.a.n.a.n.a.

n.a.87.760.7

11389 3

LaMMI-D

0.1pph

CO.l0.90.91.00.9

CO.l0.20.2

n.a.n.a.

n.a.n.a.n.a.n.a.

CO.l

03CO 1CO.l

n.a.n.a.

n- an.a.n.a.n.a.n.a.

n.a.3.00.9

CO.lCO 1

TaMMI-U

0.5pph

CO 5CO. 5C 0.5Cd. 5CO 5

CO 5CO. 5CO. 5

n.a.n.a.

n.a.n.a.n.a.n.a.

C 0.5

C0.5CO. 5CO. 5

n.a.n.a.

n.a.n.a.II.H.n.a.n.a.

n.a.CO. 5C0.5•C0.5C05

('e

MMI-D0.1pph

0 21.91.71.91.9

CO 10204n.a.n.a.

n.a.n a.ri. a.n.a.0.2

0.6CO 1CO.l

n.a.n.a.

n a.n.a.H an.a.n.a.

n.a.7.62.0

cO.l0.2

FiMMI-D

0.1pph

CO 1020.20.20.2

CO.lCO.lCO.l

n.a.n.a.

n.a.n.a.n. a.n.a.

cO.l

cO.lCO 1cO.l

n.a.n.a.

n.H.n.an.an.a.n.a

n.a.0.80.2

cO.lCO.l

NilMMI-D

0.1pph

010.70.70.80.8

CO.lCO .1

0.1n.a.n.a.

n.a.n.a.11. a.n.a.

CO.l

0.3CO.lCO.l

n.a.n.a.

n.a.n.a.1 1 . a .n.a.n.a.

n.a.2.90.9

CO.lCO.l

SmMMI-1)

0.1ppi)

cO.l0.20.10.20.2

CO.lc() 1CO.l

n.a.n.a.

n.a.n.a.ii a.n.a.0.1

cO.lCO.lCO.l

n an a.


n.a.0.60.2

CO.lCO 1


r.leiiicnl Method. Del.Li in. Units.

2956329564295652956629567

2956829569295702957129572

2957329574*Dup 29446*Dup 29458*Dup 29470

"Dup 29-482*Dup 29551 'Dup 29563


MBMMI-D

100ppb

10202230n.a.n. a.li. a.

n.a.n-a.n.a.n.a.

< KX)

11.140970li. a.

836015340

1ft 170n.a.860

TiMM1 D

1ppb

397

11 J

n.a.n.a.

n.a.n a.n.a.n.a.

7

6282

n a•CI

2

5n.a.

36

CiMMI-U

1ppb

<[O

n.a.n.a.n.a.

n.a.n.a.n.a.n.a.ci

3•CI

n a2

CI

<In.a.•ci

CoMMI-D

1ppb

7

1

n.a.n.a.n.a.

n.a.n.a.n.a.n.a.0

2CIn.a.CICI

cin.ii.

3

NiMMI-D

3pph

c3<3

n.a.n.a.n.a.

n.a.n.a.n.a.n.a.•c 3

5<3n.a.

33

< 3n.a.<3

KbMMI-D

1pph

7266

n.a.n.a.n.a.

n.a.n.a.n.a.n.a.

31

-T

26n.a.

1816

10n.a

67

YMMI-U

0.1ppb

0.1co.i

n.a.n.a.n.a.

n a.n.a.n a.n.a.(1.2

1.50.6

n aCO.lCO.l

<0.1n.a.0.3

MbMMI-D

O.Ip|il)

0.1CO.l

n.a.n.a.n.a.

n.a.n.a.n.nn.a.

<0.1

0.30.4n.a.

CO.l<0.1

CO.ln.a.0.2

P.IMMI-D

0.1ppi)

•co.iCO.l

n.a.n.an.a

n.a.n.a.n.a.n.a.

<0.1

CO L<0.1

n.a.•CO.lCO.I

<0.1n.a.

<0. 1

HaMMI-D

0.1pph

154277n.an.a.n.a.

n.a.n.a.n.a.n.a.137

104118n.a.349145

93.9n.a.144

l.aMMI-D

0.1pph

0.2Oil

n.a.n.a.n.a.

n.a.n.a.n.a.n.a.0.3

2.31.4

n.a.•CO.lCO.l

0.1n.a.0.3

TaMMI-D

0.5ppb

•.-0.5co 5

n a.n a.n .1

n.a.n an.a.n a

•en. s

•CO 5•CO. 5

n.a.•CO. 5c 0.5

•CO. 5n.a.

CO. 5

C fMMI-D

O.Ipph

0.50.2n.a.n.a.n.a.

n.a.n.a.n., i.n.a.0.8

4.52.9n.a.

•CO.l0.1

0.2n.a.0.6

PrMMI-I)

0.1ppb

CO.l•co.i

n. a.n . a .n.a.

n.a.ii. a.n.a.n.a.

CO.l

0.60.3n.a.

-CO.lCO.l

CO.ln.a.

CO.l

Nil.MMI-U

O.Ippb

0.2CO.l

n.a.n.a.n.a.

n.a.n.ii.n.an.a.0.4

2.21.1

n.a.co.iCO.l

0.1n.a.0.3

SinMMI-I)

O.Ippi)

0.10 1n.a.n .a .n.a.

n.a.n.an.a.n.a.O.I

0403n.a.U.I

CO.l

CO.ln a.0.1

SGSWork Order: 073901 Date: 04/09/03 FINAL 1'ai.v l

Method. Di-t.Lini. Liiits.

2944ft29447294482944929450

2945129452294532945429455

2945629457294582945929460

2946129462291632946429465

2946629467294682946929470

2947129472294732947429475

CdIMM1-D

0.1ppi)

M i)

n.a.11 'A

n.an.a.

n.a.n an.a.

CO.lCO 1

0.20.3

CO 10.30.5

CO.l051 0o yO.I

CO ICO l

0<0.cd.

co.0

COCO.CO

ThMMI-D

0.1ppb

n.a.n.a.ti.ii.n.a.n.a.

n.a.n.a.n.a.

CO.l*:0.1

<0.1<().lcO.l<0.lCO.l

cO.lCO.l

0.10.1

CO.l

CO.<0.co.<0.<0.

<0.co.•co.<0.^0

ErMMI-D

O.Ippi)

n.an.a.ii.ii.n.a.n.a.

n.a.n.an.a

•S 0.1CO.l

CO.lCO.l<0.1CO.I

0.2

CO.I0.10.30.3

•CO.I

CO.ICO.ICO.lCO.ICO.I

CO.ICO.ICO.ICO.ICO.I

YbMMI-D

0.1ppb

n an.;in.a.n.a.n.a.

n.a.n.a.n.a.

CO.ICO.I

co.iCO.ICO.ICO.I

0.2

CO.I0.10.30.2

CO.I

CO.ICO.ICO 1CO.ICO.I

CO.ICO 1CO.ICO.Ico.i

AuMMI-B

0.1ppb

CO COCO.co.co.

CO.CO.0.700,190.31

CO.ICO.I0.24

CO.ICO.I

0.10cO.lCO.ICO 10.21

c 0.1CO.lc 0.1cO.lCO.I

CO.l

n a.n.a.n a.n a

CD

MMI-B1

ppb

23

1271

1133

8765

249

482110

12421233775

ft2880

(.4

14n.a.n.a.n.a.n.a.

NiMMI-B

3ppb

i)

212024

8

281738

265225

7530

2216'J

108

21012011017435S

.1143512391

90n.a.n.a.n.a.n.a.

I'd

MMI-BO.Ippb

CO.COCO.coci)

CO.CO.0.290.17(i. 14

0.11CO.lCO 1û0.11

CO.lCO 10.100.100.10


co.in.an.a.n.a.n.a

.•VKMMI B

O.Ippb

O 872 096.343.300.4(1

5.323.33j. 402.915.52

1.141 112.080.661.79

0.982.031.500.687.88

6.572.151.311.2219.7

5.21n.a.n.a.n.a.n.a.


I'.U-mtnt. Method. Del.! lin. l'nits.

2947629477294782947929480

2948129482 29'! 832948429485

2948629487294882948929490

2949129492294932955129552

29553 2955'!295552955629557

2955829559295602956129562

G(\M.MI-D

0.1ppb

CO 1O.I0.10.10.2

CO.lco ico.i

M. a.

n.a.

n.a.n.a.n.an.a.

co.i

co.i<0.1<().l

it an.a.

n.a.n an.u.n.an.a.

n.a.0.60.2

CO.l<O.I

TbMMI-D

0.1ppb

CO.l<0.]CO.lco.icO.l

cO.l<0 1CO.l

II. H.

n.a.

n.a.n.a.n.vn.a.

CO.l

CO.lCO.lCO.l

a a.n u.

n a.n.a.11. a.n a.n.a.

n a.cO.lCO.lcO.lco.i

K.IMMI-D

O.Ipph

co.iCO.lCO.lco.iCO.l

CO.lcO.lco.i

n.a.n.a.

n.ii.n.a.n.a.n.a.

cO.l

cO.lCO.ICO 1

n.a.n.u.


n.a.0.2

CO 1CO.lCO 1

YhMMI-D

O.Ippi)

CO 1CO 1c() 1CO.lcO I

CO.lCO 1CO.l

n.a.n.a.

n.a.n.a.n.a.n.a.

CO.l

CO.lcO.lCO.]

H. ci.

n.a.


n.a.c 0.1co.icO.lcO.l

AuMMI-B

O.Ippb

n a.n.nn.a.n.ii.n.a.

n.a.n.a.n.a.

0.22CO.l

0.210.530.570.83

CO.l

0.121.00

CO.lCO 1

0.50

CO.ICO.l0,14

CO.l0.14

CO.lCO.lco.i0.37

CO 1

CoMMI-B

Jppb

n.a.n.a.D. a.n.a.n.a.

n.a.n.a.n.a

314

4252

13

1594

1610

136

133730

521

547

2214

NiMMI-B

3Ppb


n.a.n a.n.a.106114

1210

c3C314

236c 311935

215

2322

19030

125

2233188631

I'd

MMI-B0.1ppb

n an.a.n a.n a.n.a.

n an a.n a

CO.ICO.l

CO. tcO.lcO 1cO.lcO.l

c O.IcO.lCO 1CO.!0.19

CO.IcO.l0 12

CO.lCO 1

co.icO.lCO.lCO.lcO 1

AyMMI-B

O.Ippb

n a .n a.n.a.n.a.n.a.

n.a.n.a.n.a.5.782.59

1.256994086.591.28

1.578.431.760.3517.3

0.480.152.240.874.17

0.311.100.9632.02.92


Element. Method. Del. Urn. l.nits.

2956329564295652956629567

2956829569295702957129572

2957329574*Dup 29446*Dup 29458*Dup 29470

*Dup 29482 "Uup 29551*Dup 29563

(.dMM1-D

0.1ppb

•CO.]<().l

n an.ait a.

n. a.n.a.n.a.n a

<0.1

0.40.2n.a.

•C 0.1<0.1

*:().ln.a.

•CO.l

II)MMI-D

O.Ippb

•CO.l<().l

n.a.n.a.ii. a.

n.a.n.a.n.a.n.a.

<(M

•CO.l•CO.l

n.a.•CO.l•CO I

^11n.a.

•CO.l

trMMI-U

0.1ppi)

•co.i<0.1

n.an.a.n.a.

n.a.n.a.n.a.n.a.

•CO.l

0.2<0.1

n.a.•CO.l•CO.l

<0.1n.a.

<0.1

VI)MMI-D

0.1ppb

<0.1•CO.l

n.a.n.a.ii.ii.

n.a.n.a.n.an.a.

•CO.l

0.1•CO.l

n.a.•CO.l•CO 1

*;0,1n.a.

<0.1

AuM.MI-B

0.1ppb

•CO.l-CO.l0,150.17

<()A

(1.34•CO.l0.290.43

-C U.I

0.10^.1•CO.l0.27

•CO.l

n.a.01.1•c O.I

CoMMI-B

1ppb

44

11488

g3453

808'J

566

n.a.H)4

NiM.MI-B

3ppb

22311761

133

7373

8109

10

20223

722000

n.a.y)25

I'llMMI-B

0.1ppi)

•co.i•CO.l•CO 1Û•CO.l

•CO.l<0 1•CO. l<(} l<0.1

<0.1•CO.l•co.i•CO.l<n i

n.a.•CO.l•CO.l

\UMMI-I!

O.Ipph

4.240.682053.953.54

24.02.051.01y. 980.27

5.370.390.751.8917.1

n.a.0.50'1.33



Date 04/09/03

Copy 1 to


Jilbey7 Rock14/08/03Cover Sheet plusPages 1 to 1


Certified By izz \ w—ci-ui.Dr. Hugh de Souza, Genera! Manager

ISO 9002 REGISTERED


Report Footer:

SGS Canada Inc.

L.N.R. - Listed not received l.S. - Insufficient Sample n.a. = Not applicable -- = No result "INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, "/o denotes ppm to "m conversion


Minerals Services 1885 Leslie Street Toronto ON M3B 2M3 1(416)445-5755 f (416) 445-4152 www.sgs.ca

Member ol the SGS Group (Societe Generate de Surveillance)

Work Order: 073902Kleuitmi. Method. IK-U.ini. I'nits.

Au FA301

I ppb

lT

•C1

l < l

Date: 04/09/03 FINAL Page l of l

3125-4 '''Hup M248

138

1

CERTIFICATE OF ANALYSISWork Order: 074033


Date 1 6/09/03

Copy 1 to


Jilbey22 Rock and Soil25/08/03Cover Sheet plusPages 1 to 3

Distribution of unused material:Pujps: Discarded After 90 Days Unless Instructed!!!Rejects: Discarded After 90 Days Unless Instructed!!!

Certified By


ISO 9002 REGISTERED


Report Footer:

SGS Canada Inc.

L.N.R. = Listed not received l.S. ^ Insufficient Sample n.a. - Not applicable -- = No result *INF = Composition of this sample makes detection impossible by this method M after a result denotes ppo to ppm conversion, Va denotes ppm to "/o conversion


Minerals Services 1885 Leslie Street Toronto ON M3B 2M3 t (416) 445-5755 f (416) 445-4152 www.sgs ea

Member of Ihe SGS Group (Societe Generale de Surveillance)


Method. Del.Mm. Units.

2957529576295772957829579

2958029581295822958329584

2958529586295872958829589

3125531256312573125831259

3126031261*Dup 29575*Dup 29587

AuKA3IH

lppb

28365

15456

5O

28

O

0O

9^000

78

301163

33

Au Bel'A30(i ICTKII

0.03 0.5g'nil ('pin

1.01 .01.01.00.9

0.91.01.21.21.1

0.91.40.91.41.0

n. a.n. a.

•^0.5•1.83 0.6

0.8

c:0.50.71.009

NaICI'SO

0.01"k

2.322.252.182.182.02

2.002.151.982.372.40

2.032.102.081.822.10

n.a.n.;i.

0.025.633.63

t: 0.014.312.252.08

MgICI'SO

0.017r

0.570.710.630.600.58

0.390.710.970.630.54

0.480.680.540.630.47

n.a.n.a.

0,020010.24

cO.Ol0.230.560.5?

AlICPKO

0.01It

6.61fi. 606.5-16.536.51

5.806.596.91.)6.586.41

6.036.816.346226.57

n.a.n.a.

0.046.325 86

0.046136 396.36

PICPSO

0.01ft

0.060060.05006003

0.030.070090.09008

0.010.020.020030.04

n.a.n.a.

•CO.OI0.030.03

^.010.030.060.02

KICPKO

0.01•a

1.781.651.651.721.67

1.591.782.021.821.78

1.751.861.711.361.70

n.a.n.a.

•C 0.01O.'ll1 20

0.020-801.741.70

CaICPSO

0.01"h

1.821.791 .661.671.50

1.441.972.072.031.98

1.481.601.551.341.54

n.a.n.a.1.260.170.61

•C0.010.671.771.54

SeICPSO

0.5ppm

6.37.16.76.36.7

4.87.38.26.86.1

5.77.56.07.85.9

n.a.n.a.0.50.62.2

<().52.16.35.9

TiICPSO

0.01ft

0,200230.210.210.24

0.170.230260.220.20

0.220.250.220.300.22

n a.n.a.

•CO. 010.010.02

*C0.010.020.200.22

VICPSO

2ppm

4654515362

4757705145

5456547655

n.a.n.a.^1328

2214654

CrICPSO

1ppm

2331272633

1833392820

2128264628

n.a.n.a.

395545

144342227

MnICPSO

2ppm

248372250270244

177306328277251

216272233244210

n.a.n.a.14083

160

45194247236

FeICPSO

0.01"h

1.752.122.062.282.29

1.672.142.431.861.61

1.722.042.042.791.84

n.a.n.a.

0.262,591 .06

1.040.891 692.03

CoICPSO

1ppm

f9776

48965

475•7

4

n.a.n.a.< 1346

4455


Element. Method. DtU.Lim.Units.

2957529576295772957829579

2958029581295822958329584

2958529586295872958829589

3125531256312573125831259

3126031261*Dup 29575*Diip 29587


NiICT80

1ppm

1421192118

1220271714

1221152412

n.a.n.a.

92824

17201516

Cu1CP80

0.5ppm

6.39.1

11.68.66.9

3.110.313.79.43.8

3.45.55.5

16.73.1

n.a.n.a.2.4

17.45.2

5.83.46.66 1

Zu1CP80

0.5ppm

22.436.126.328.926.9

17.534.550.826.625.9

25.131.123.633.521.7

n.a.n.a.1.73.0

10.8

2.99.6

22.027.0

AsICP80

3ppm

C 30

35

C3

O0ooc3o0o

3O

n.a.n. it.OOC3

4Oc 3O

Si1CP80

0.5ppm

392372367381350

358373341418424

355362358296366

n. a.n.a.12.7183265

32.1230385361

Y1CP80

0.5ppm

6.98.06.76.05.7

4.710.011.29.88.6

4.97.15.26.85.8

n.a.n.a.

CO. 5CO. 5

1.7

C0.51.26.95.4

ZrICP80

0.5ppm

127106108123119

98.5112108129113

126107113119113

n.a.n.a.1.6

68.3669

3.570.3

117112

Mo1CP80

1ppm

CI•CI

<\c 1•CI

<i<l-CI

<\ci0CIooci

n.a.n.a.

218

2

7CI<\•Ci

AgICP80

0.2ppm

0.90908

- 0909

0.80.9040.90.7

1 01.00.91.01.0

n.a.n.a.

C0.2^0.0

0.6

0.40.90.80.8

CdICP80

1ppm

ci•CI

CI< 1•ci

•CI•cio•CI•CI

•CI•CI•CI

ci^ J

n.a.n.a.CI<\.^ |

CiCI0o

Sn(CP80

10ppm

•C LO•C LOclOCIOClO

cioCIO•CIOclO•C 10

CIOCIOCIOc 10CIO

n.a.n.a.CIOC 10c 10

c 10CIOc 10CIO

SbICP80

5ppm

C 5C5C5C 5c 5

C5C5C5C5C 5

C5C5C5C5c5

n.a.n.a.C5C5c 5

C5C 5C5C 5

BaICPXd

1ppm

5835465C4586569

546603626599598

584619573482581

n.a.n.a.

2180621

4190376587576

LaICP8II

0.5ppm

10.814.111.0969.0

6920.625.718615.5

7.612.88.0

12.09.6

n.a.n.a.063.17.0

CO. 56.9

10/18.8

WICPHO

10ppm

C H)CIOCIOCIOCIO

C H)CIOCIOCIOc 10

CIOCIOCIOCIOclO

n.a.n.a.ClOCIOClO

CIOCIOCIOCIO

PbICPHO

2ppm

1010101111111156139

1111119

12

n.an.a.C221

6

649

10


Element. Method. Det.I.im.Units.

2957529576295772957829579

2958029581295822958329584

2958529586295872958829589

31255 n.a. n.a. n.a.31256 n.a. n.a. ".a.31257 O O -:0.331258 6 O 8.531259 <5 -CI <(}^

31260 <5 <\ 0.531261 O l 0.6*Dup 29575 O 7 n.a.*Dup 29587 5 10 n.a.

RiICP80

5ppm

<56566

<S565

<5

<56577

LiICP80

1ppm

814111 112

71422

97

g1510H10

AgAA73

0.3g/mt

n.a.n.an.a.n.a.n.a.

n.a.n.a.n.a.n.an.a.




Date 1 8/09/03

Copy 1 to




Certified By X l

Dr. Hugh de'Souza, General Manager

ISO 9002 REGISTERED


Report Fnnter: L.N.R. = Listed not received l.S. = Insufficient Sample n.a. - Not applicable — = No result 'INF - Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, 07o denotes ppm to aA conversion

SuDjcct to SGS General Terms and Conditions

SGS Canada Inc. Minerals Services 1885 Leslie Street Toronto ON M3B 2M3 t (416) 445-5755 f (416) 445-4152 www.sgs.ca

Member ot tne SGS G-ODP (Sociele Generale de Surveillance)


Mttbocl. Dct.Lim. t nits.

20494 29-195294962949729498

2949929500295012950229503

2950429505

- 295062950729508

2950929510295112951229513

2951429515295162951729518

2951929520295212952229523

Hate: 18/09/03 FINAL

AuMMI-B

0.1ppb

0.200.23

CO 1CO.lco.i

c 0.1<[).l<0.1c 0.1<0.l

CO.l10.1co.ico.i0.25

co.iCO.ICO.l0 120.16

CO 10.130.250.130.12

0.180.140.120.13

CO.I

CoMMI-B

1ppb

3130t18

1517

'156

73•1

232

265

183027

311424

78

2079

1131

IViMMI-B

3ppb

17692602650

5655156662

738877O58

42227544

107

3895

12210798

5910693

11348

I'dMMI-B

0.1ppb

CO 1CO.l0.16CO.lCO.l

CO.l•CO.l•CO.lCO.l0.11

CO.l0.150.14

•CO.lco 1

•CO.lCO.l0.11

•co.i•CO.l

•co.i0.16

•CO.l0.110.15

CO.l0.120.140.190.33

AyMMI-B

O.Ippb

1.376.20

1 040.511.27

CO.l0.6R0.271.381.58

1.501.631 433.46292

3.901 950.203 352 50

1 061.384 302.482 71

10.81 411.541.780.43

MgMMI-D

100ppb

112309750624049904610

595063606430n.an.a.

n.a.n.a.n.a.n.a.n a

n.a.n.a.n.a.

63306380

54603740594035904140

8660375027104780n.a.

liMMI-D

1ppb

6•CI

1167

6138

n.a.n.a.

n.a.n.u.n.a.n.a.n a.

n.a.n.a.n.a.c 132

<l649

16

<l57

39n a.

CrMMI-D

1ppb

<]O<\•cici

cic Icin.a.n.a.


n.a.n.a.n.a.cC

<^<CI

CI

CI

ciCI

1n.a.

CoMMI-D

1ppb

ccccc

CIciCIn.a.n.a.

n.a.n.a.n.a.n.a.n.a

n.a.n.a.n.a.ciC 1

ci^ccc

c<CI

1n.a.

NiMMI-D

3ppb

C 3C3

43

C3

C3C3C3n.a.n.a


n.a.n.a.n.ac 3•C 3

C3C3C3C3C3

c 3c 3C3

4n a.

RI)MMI-D

1ppb

322034129

68

11n.a.n.a.

n.a.n.a.n.a.n.a.n.n.

n.a.n an.a.

3839

4317531820

39181518

n.a.

YMMI-D

O.Ippb

0 1CO.l

0.50.20.1

0.20.40.3n.a.n.a

n.an.a.n.a.n.a.n.a.

n.a.n.a.n.a.

CO.l0.6

CO.l0.30.20.40.8

CO.l0.40.31.6

n.a.

IS'b

MMI-D(IIpph

0 1030 2020.1

0.2O.I0 1n.a.n.a.

n.a.n.a.n.an.a.n.a

n a.n.a.n.a.0.10.2

0.10.1

CO ICO 1CO 1

CO.lCO.lCO.l

0.1n.a

PelMMI-D

0.1ppb

CO 1CO.lCO.lco.iCO.l

CO.lCO.lCO.l

n.a.n. a.

n.a.n.a.n.a.n.a.n.a

n.a.n.an.a.

CO.lCO.I

CO.lCO.lCO.lCO.lcO .1

CO.lCO.lCO.l

0.1n.a.

li..MMI-D

0.1ppb

225256

58.938.055.5

134134

59.5n.a.n.a.

n.a.n.an.an.a.n.a.

n.a.n.a.n.a.324349

341103500135132

386119

91.3150n.a.

I.M

MMI-D0.1ppb

O.ICO.l

3.20.50.6

0.81.90.8n.a.n.a.

n a.n.a.n.a.n.an a .

n.a.n.an.a

CO.l1.8

CO 11 60 31.44.1

CO.I2.01.18.5

n.a.


Element.Method.Dct.L.im.("nits.

2952429525295262952729528

2952929530295312953229533

29534*Dup 29494*Dup 29506*Dup295l8*Dup 29530

AuMMI-B

0.1ppb

0.16co l<0.1CO. lco.i

0.110.170.140.05

CO.l

<0.10.17

CO 10.120 17

CoMV11-B

1ppb

Mi30

55d

1012621

46

53649

28

NiMMi-B

3ppb

10255251257

10541376221

17198

819642

I'dMMI-B

0.1ppb

CO.l•C 0.1cO.lcO.lCO.l

cO.l<0.1<0.1<0.1<0.1

CO.lcO.l0.110.18

<0.1

AyMMI-B

0.1ppb

5.090721.322.301.50

3.630.563.214 .171.12

4.551.381 652.410.58

MSMMI-D

100ppb

n.ii.n a.11 a.n, a.n. a.

n. a.n . a .n. a.n a.n. a.

n. a.10860

n.a.3530n.a

liMMI-D

1ppb

n.a.n.a.n.an.a.n.a.


n.a.7

n.a.17

n.a.

(rMMI-D

1ppb



n.a.•CIn.a."CIn.a.

diMMI-D

1ppb

n.an.an an a.1 1 . a

n, an.a.n.an.a.n.a.

n.a.On.a.<\

n.a.

NiMMI-D

3ppb

i .a.i .a.i .ai .a.i .a.


n.a.O

n.a.O

n.a.

KbMMI-D

1ppb

n.a.n.a.n an.a.n.a.

n.a.n.a.n.a.n.an.a.

n.a.34

n.a.18

n.a.

YMMI-D

0.1ppb

n.a.n, a.n.an.a.H. a.


n.a.0.3n.a.0.9n.a.

NhMMI-D

0.1ppb

n.a.n.an an.a.n.a.

n.a.n.a.n, a.n.a.n.a.

n.a.CO.l

n.a.CO l

n.a.

I'dMMI-D

0.1ppb

n.an.an.an.a.n.a.

n.a.n.a.n.a.n.an.a.

n.aCO.l

n.a.CO.l

n.a.

KaMMI-D

0.1ppb

n.a.n.an.an.a.n.a

n.a.n.a.n.a.n.an.a.

n.a.240n.a.128n.a.

LaMMI-D

0.1ppb


n.an.a.n.a.n an.a.

n.a.0.2

n.a.3.9

n.a.


Element. Method. Del. Urn. Units.

29405294962949729498

2949929500295012950229503

2950429505295062950729508

2950929510295112951229513

2951429515 2951ft2951729518

2951929520295212952229523


laMM1-D

0.5ppb

CO. 5•co. 5•z 0.5C 0.5•CO. 5

CO. 5<0.5<().5

n.a.n.a.

n. a.n.a.n.an.a.n.a.

n.a.n.a.n.a.

<0.5•c 0.5

c l). 5•c 0.5<0.5<0.5•CO. 5

C0.5COS<0.5C0.5

n.a.

CeMMI-D

0.1ppb

0.2CO.l

4.40.70.9

1.22.91.2

n a.n.a.

n.a.n.a.n a.n a.n.a.

n.a.n.a.n.a.

CO.l3.6

"C U.I2.40.42.16.1

0.12.71.6

136n.a.

I'r

MMI-D0.1ppb

<0.1•CO.l

0.5<0,l

01

0.20.30.1n.a.n.a.


n.a.n.a.n.a.

•-'0.10 4

•a) l0.3

CO 10.30.7

CO 1030.21.5

n.a.

NdMMI-D

0.1ppb

co.iCO 1

1.20.40.3

0.51.00.5n.a.n.a.


n.a.n.a.n.a.

CO.l1.4

•co.i0.80.21.02.1

CO.l0.80.64.8n.a.

SinMMI-D

0.1ppb

•CO.lO.I0.2

•CO.lCO.l

0.10.1

to. in.a.n.a.


n.a.n.a.n.a.

•CO.l0.4

0.10.10.20.10.2

0.1O.I0.10.6n.a.

(idMMI-D

0.1ppb

•co.i•CO.l

0.1•CO.l•CO 1

•CO.l0.1

CO.ln.a.n.a

n.a.n.a.n.a.n.an.a

n.a.n.an.a.

c 0.10.2

CO.lCO.lc 0.1

0.10.2

CO.lCO.lCO.l

0.6n.a.

I'b

MMI-D0.1ppb

co.CO.l•COCO.lCO.l

CO.lCO.lCO.l

n.a.n.a.


n.a.n.a.n.a.

CO.CO.

co.<().CO.co.•co.

CO.lCO.lco.iCO.l

n.a.

KrMMI-D

0.1ppb

CO.cOCOCOCO

COco.CO.l

n.a.n.a.


n.a.n.a.n.a.

CO.CO.

CO.CO.COCOCO

CO 1CO 1CO.l

0.1n.a.

VI)MMI-D

O.Ippb

CO.lco.iCO 1CO 1CO 1

CO 1CO.lCO.l

n.a.n.a.


n.a.n.a.n.a.

CO.lCO.l


CO.lCO.lCO.l

0.1n.a.


Element.Method.Det.Lim.Units.

2952429525295262952729528

2952929530295312953229533

29534*Dup 29494*Dup 29506-Dup29518"Dup 29530

TaMMI-D

0.5ppb

11 'A

n an a.n a.n.a.

n a.n.a.n a.n.a.n.a.

n.a.•C0.5

n.a.<0.5

n.a.

CeMMI-D

O.Ipph

n a.n.a.n.a.n.a.n.a.


n.a.0.3

n.a.5.6

n.a.

PiMMI-D

0.1ppi)

11-3

n.a.n.a.n.a.n.a.


n.a.•CO.I

n.a.0.6n.a.

NclMMI-D

0.1ppb



n.a.0.2n.a.2.0n.a.

SinMMI-D

0.1ppb

n.an.a.n.an.an.a

n an.a.n.an.a.n.a.

n.a.•CO.l

n.a0.3

n.a.

GdMMI-D

0.1ppb



n.a.•C 0.1

n a.0.2

n.a.

TbMMI-D

0.1ppb



n.a."CO. l

n a.^1.1

n.a.

EiMMI-D

O.Ipph

n.a.n.a.n.an.an.a.


n.a.•CO.l

n.a.^.1

n.a.

YbMMI-D

0.1ppb

n.a.n a.n an.a.n.a.

n.a.n.an.a.n.a.n.a.

n.a.^).l

n.a.•CO.l

n.a.

,,ai!c l ,,,-



Date 1 8/09/03

Copy 1 to




Certified By •'iA H.,.Y

le SiDr. Hugh de souza, General Manager

ISO 9002 REGISTERED


Rcpon Footer: L.N.R ** Listed not received l.S. = Insufficient Sample n.a. = Not applicable — ^ No result *INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, ?'o denotes ppm to Vo conversion


SGS Canada Inc. Minerals Services 1885 Leslie Street Toronto ON M3B 2M3 t (416) 445-5755 f (416) 445-4152 www.sgs.ca

Member of tne SGS G'oup (Rociele Renerale de Survei'larce)


Element. Method. Det.Lim. Units.

2953529536295372953829539

2954029541295422954329544

2954529546295472954829549

29550296012960229603 2960'!

*Dup 2953;*Dup 29547

AuIMMI-B

0.1ppi)

0.200.260 20

C 0.1co.]

cO.l<f).lcO.l0 330.27

0.280.760.180.16

CO.l

CO.<0.CO.COCO.

0.160.17

CnMMI-B

1ppb

503019

79

998

5142

2719

100

773

105

458

Ni.MMI-B

3ppb

151171181100132

144137137203175

12369656326

344020W41

14261

I'dMMI-B

0.1ppb

0.140.180.240.110.13

0.170.120.130.160.18

0.14CO.lCO.Ico.iCO 1

cO.lCO.lCO.l•CO. 1•CO. 1

0.180.12

ABMMI-B

0.1ppb

1.021.751 750 55098

0.900.690.494532.35

3.5231.66.297.23407

9.942.5413.54.189,15

0.886.82

MgMMI-D

100ppb

65408830730048605060

49704920401060507680

956018720221036303410

39703140276022201730

66702140

liMMI-D

1PPI)

133590

89

10106

ci10

22

3123

13102

11569

1129

Ci-MMI-D

1ppb

224

CICI

<]"CI

1CI

4

-Ci

22

CIci

ci<\

l43

<l3

CoMMI-I)

Ippb

<\< 1

2CI<\

CIC 1<\CI<\CIciCICI

3

^

^

CIci

NiMMI-D

3ppb

C 3C3

6C3C3

C3C3C3C3

9

C3<3C 3C3

4

C3C 3C3C3C 3

C3C 3

KbMMI-D

1ppb

2119221719

1819163819

17S

443840

59647080

103

2144

YMMJ-D

0.1ppb

1.013240.50.4

0.6060.1

cO.l0.5

CO.lCO.l

0.5CO.lCO 1

c 0.10.3

cO.l0.70.6

l.U0.6

MiMMI-D

0.1ppb

0 20,20.4O.I0.1

0.1CO 1CO.lCO 1CO.l

CO 1co.]

0.1CO.lco i

CO.lco.iCO.l

040.2

CO 10.1

PelMMI-D

0.1ppb

CO.lCO.lCO 1co.iCO.l

CO.lCO.lco.ico iCO.l

co.iCO.lCO.ICO.lcO.l

CO.lCO.lco.iCO 1CO.l

CO.lCO.l

l!.iMMI-I)

0.1ppb

195171196120119

122117

99.2332189

.31 y117102122343

321133296104

88.3

190105

l.!l

MMI-D0.1ppb

161.84.62.01.4

2.82.81.6

CO.l0.6

CO.l0.12.10.20.1

0.20.30.12.51.5

1.42.4


Element. Method. Det.l.iin.Units.

2953529536295372953829539

2954029541295422954329514

2954529546295472954829549

2955029601296022960329604


-Dup 29535-Dup 29547

TaMMI-D

0.5ppb

O.5<0.5<0 50.5<() 5

c: 0.5<0.5•c.0.5<0.5<().5

<0.50.5O.5O.5<0.5

<0.50.5O.5<[).50. 5

<0.50. 5

OMMI-D

(l. lppb

2.83.37 72.92 2

'1.24.32 4

o.i1.1

O.IO.I

3.90.3(•.2

0.30.90.26.73 3

2.54.3

PrMMI-D

0.1ppb

(1.30,40 00.30.3

0.50.50.3

O.IO.I

O.IO.I

0.4O.IO.I

O 1O.IO 1

0.50.3

030.5

NclMMI-D

0.1ppb

1.21.5.1.61.309

1.51.40.8

O.I0/1

O.I0.21.40.101

0.20.3

O.I1.81.3

0.91.7

SmMMI-D

0.1ppb

0.30.40.80.20.1

0.20.20.10.10.2

0.10.1

0.3O.I

0.1

0.10.10.10.30.2

0.20.3

GilMMI-D

O.Ippb

0.20.30.70.1

O 1

O.I0.20.1

O.I0.1

0. 1O.I

0.20.1O.I

* 0. 1O.IO.I

0.30.2

0.20.2

TbMMI-D

0.1ppb

0.1O.IO.IO.IO.I

O.I0.1O.IO.IO.I

O.IO.IO.!O.I0.1

O.I0.1O.IO.IO.I

0.10.1

ErMMI-D

0.1ppb

0.1O.I

0.3O.IO 1

O.I0.1O.IO.IO.I

O.I0.1O.IO.IO.I

0.1O.IO.IO.IO.I

O.IO.I

YM.MI-I

0.PI'

0.0.o.;

0.0

o.o.o.o.o.o.o.o.o.o.

o.0.o.o.o.O.IO.I



Date 18/09/03

Copy 1 to


Jilbey13 Rock29/08/03Cover Sheet plusPages 1 to 3

Distribution of unused material:Pulps: Discarded After 90 Days Unless Instructed!!! Rejects: Discarded After 90 Days Unless Instructed!!!

Certified By


ISO 9002 REGISTERED


Hepnrt hooter: l.S. = Insufficient Sample s No result

L.N.R. = Listed not receivedn.a. - Not applicable - - ,-.,' INF = Composition of this sample makes detection impossible by this methodM after a result denotes ppb to ppm conversion, "A denotes ppm to 0A conversion


SGS Canada Inc. Minerals Services 1885 Leslie Street Toronto ON MSB 2M3 t (416) 445-5755 t (416) 445-4152 www.sgs.ca

Member of the SGS Group (Societe Generate de Surveillance)


Element. Method Det.Liin. I'nils.

3126231263312643126531266

31267 3126S312693127031271

312723127331274*Dup 31262*Dup 31274

AuF'AJOS

5ppb

9735

1212435

4758O<^40

69C 5<5163-S 5

BcICP80

0.5ppm

^1.5•c l). 5<n.5^1.5

1.3

2.62.70.80.72.8

2.42.02.2

•C0.52.1

Na1CP80

0.01"/c

0.600.110.860.220.23

0.910.930.850.030.05

0.042.892.580.612 S3

Ml!ICP80

0.01OK

1.451 311 354.990.73

0.330.342.370,101.00

0.921.261.351.461 33

AlICP80

0.01"la

4.973 036.207.432.12

5.235.397.001.155.68

5.098.328.595.00841

PICP80

0.01c,i

0.020.020.050.030.02

0.040.040.040.010.04

0.040.06fi. 060.020 06

K1CP80

0.01Ve

0.330.060.410.050.89

1.982.052.010.491.81

1.580.970.970.340.95

C.iICP80

0.01'k

0.621.360 180.591.83

0.160.176.190.180.98

1.032.353.2(10.613.15

Se1CP80

0.5PPI"

13 I5.6

12.132,55.3

12.81.3.727.02.0

10.3

9.811.618.713. -118.2

TiICP80

0.01Ve

0.020.020,050.110.03

0.050.050.070.020.19

o.i y0.420.600.030.59

VICP80

2ppm

SO3575

18926

5054

1551162

5510015884

152

C rICP80

1PPI"

622448

31238

4041

1372152

4846776570

MnICP80

2PPI"

4? 2674334

17801710

402424

108012402130

2500875999456970

FtICP80

0.01"JB

5-15.008.33

12.79> 15.00

9.21

> 15.00> 15.00

8.804.96

14.89

> 15.005.55626

> 15.006.18

PuICP80

1ppm

3116202060

179191371315

7717283327

NiICP80

1ppm

1273952

11993

2342451062930

1404467

13566

Work Order: 074092 Date: 18/09/03 FINAL l';is!f 2 nl *

Element. Method. Dtl.Lim. Units.

31262 31203 31264 3 J 26531266

3126731268312693127031271

312723127331274*Dup31262*Dup 31274

CiiICPSO

0.5ppm

8') 330-266.639.6257

878906113

86.4209

53962.985.488.884.6

inICPSO

0.5PPI"

86.679 881.2

1111330

35203710

105743393

166090.591.394.7

101

VsICPSO

3ppm

682455175

O•O29OO

O•c 3o72O

SrICPSO

0.5ppm

12143.320116.060.7

30.932 11229.4

50.7

53.2523574122559

YICPSO

0.5ppm

4.45.06.76.04.9

9.210.07.62.66.9

7.416.114.84.4

14.4

ZrICPSO

0.5ppm

41.935.688.635.440.1

114122

51.917.098.5

89.984.478.443.675.3

M,iICPSO

1ppm

O< 1

1•CI

o

23

<lO

\

2î

< i< \

ASICPSO

0.2ppm

0 6<0.2

0.5<().>

0.4

1.716

•CO. 2*:02

0.2

0.6•CO. 2•CO 2

07•co. 2

CclICPSO

1ppm

•CI•CI•CI•CI

3

99

O2

0

4•CI•CI•C 1

< 1

SnICPSO

10ppm

•CIO•CIO•CIO

OO•CIO

00OO•CIO•C 10OO

"CIO•UO•c 10<IO•CIO

SbICPSO

5PPI"

9•c 52113

t: 5

07

OO

6

5O•C514

•C5

B;iICPSO

1ppm

14527

1582390

116no292

39383

92402367149358

LilICPSO

0.5PPI"

7 58.1

13.02.07.5

18 620.1

9.34.962

10021 121.1

7.520.4

\\ICPSO

10ppm

•C 1000•CIO•cio00

0012

< K)00OO

OO•C 10onOO00

PhICPSO

2ppm

5617543240

959926

846

6235375939

ItiICPSO

ft

ppm

^ s•c; 5<5Oc: 5

O^•C50O

OO•C 5•C 5•C5


FJtnicnt. Li Method. ICI'SODtt.Lim. lUnits, ppin

31262 2631263 2131264 2731265 4331206 4

31267 831268 831269 1731270 l31271 14

31272 1231273 1731274 18*Dup3l262 26*Dup31274 18



Date 24/10/03

Copy 1 to




Certified By

Tim Elliott, Operations Manager

ISO 9002 REGISTERED


Report Footer:

SGS Canada Inc.

L.N.R. = Listed not received l.S. = Insufficient Sample n.a. = Not applicable - = No result *INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, 0A denotes ppm to % conversion


Minerals Services 1885 Leslie Street Toronto ON M3B 2M3 t (416)445-5755 f (416) 445-4152 www.sgs.ca

Member of the SGS Group (Sociele Generate de Surveilance}

SGSWork Order: 074743 Date: 24/10/03 FINAL Page l of 4


2960529606296072960829609

2961029611296122961329614

2961529616296172961829619

2962029621296222962329624

2959029591295922959329594

2959529596295972959829599

MgMMI-D

100ppb

5505960

10910149106070

1320125709690

128406300

11403910

191904130

700

22250143701590022950

760

6100910054005160

19510

132208380

1366026103290

TiMMI-D

1ppb

13•ci•cioci

52CI•CI

2CI

o28

•CI1

42

CIS912

CICI•Ci

<l•CI

o•CI

ci3635

CrMMI-D

1ppb

Ci•ciOO•CI

Cici•ci•ci0•ci•CI•CI•ci•ci

ooo•CI•CI

CICI<]•cici

CIciCICICI

CoMMI-D

1ppb

154

CI6

3104

CICI

12

ciCI

1

ciCICIcici

2ciCICICI

l1225

NiMMI-D

3ppb

C39

106

12

315106

C3

C35653

65665

898

c35

91016

511

RbMMI-D

1ppb

273643

248

3634341232

5090426928

42534

560

6050845414

3547784259

VMMI-D

0.1ppb

0.60.10.10.10.2

0.40.3

CO.l0.4

CO.l

CO.l0.2

CO.l0.1

CO.l

0.10.10.10.10.2


CO.lCO.l

0.1CO.l

0.4

NbMMI-D

0.1ppb

0.1CO 1CO.lCO.lCO.l

0.3CO.lCO.lCO.lCO.l

CO.l0.1

CO.lcO.l

0.2


CO 1CO.lCO 1CO.lcO.l

CO.lCO 1CO.lCO.l

0.2

I'dMMI-D

0.1ppb

CO.lCO 1CO.lCO 1CO 1

CO 1CO 1CO.lCO 1CO.l

CO 1CO 1CO.lCO.lCO 1

cO.lCO.lCO 1CO.lCO 1

CO.lCO.lco.iCO.lCO.l


UaMMI-D

0.1ppb

51.7184232

66.4220

95.2248270105181

188114157129

92.2

141152181157329

266236150

73.5122

116306180126235

LaMMI-D

0.1ppb

0.80.3030.10.4

0.60.60.20.40.1

0.10.40.10.201

0.10.60.20.20.5

CO.l0.1

CO.lcO.lcO.l

0.20.10.20.20.9

TaMMI-D

0.5ppb

C0.5C0.5COSCO.SC0.5

cO.5CO.SCO.5CO.SCO.S

CO.SCO.SCO.SCO.SC 0.5

CO.SCO.ScO.5CO.5CO.S

CO.ScO.5CO.ScO.5C 0.5

cO.5cn.scO.5cO.5co.s

CeMMI-D

0.1ppb

1.80.40.7

CO.!0.8

1.30.60.30.80.2

0.31.10.30.51.2

CO.l1.60.60.41.1

0.10.20.1

cO.lCO.l

0.30.20.40.52.0

PrMMI-D

0.1ppb

0.2CO.lCO.lCO.CO.

0.CO.CO.

0.CO.

CO.l0.1

CO.lCO.lco.i

co.i0.1

CO.lCO.l

0.1


cO.lCO.lCO.lCO 1

0.2

NdMMI-D

0.1ppb

0.90.20 30.20.3

0.60.30.20.5

CO.l

0.20.40.1020.2

0.10.40.20.30.5

CO.l0.1

CO.lCO.lCO 1

0.2CO.l

0.20.20.8

SmMMI-D

O.Ippb

0.20.101

CO.l0.2

0.20.20.10.1

CO.l


CO.l0.10.1

CO.l0.2

0.10.1

CO.CO.CO.

CO.0.0.2

CO 10.3

Work Order: 074743 Date: 24/10/03 FINAL Page 2 of 4

Element. Method. Dct.Lim,Units.

29600 2Q651296522965329654

2965529656296572965829659

2966029661296622966329664

29665*Dup 29605*Dup29617*Dup 29594*Dup 29656

MRMMI-D

100ppb

2650900970

61703480

9306140127017802420

4440590580

933012550

16310590

1779020220

6210

TiMMI-D

1ppb

<lCi31

sil

8

73144

O

9O•CI•CI

13

o15

CIci

2

CrMMI-D

1ppb

<lci•ci•ci•CI

•CI•ci•ci•ci<lCI•ci<l<lci<l•ci<lcici

CoMMI-D

1ppb

101274

2•Ci

214

<\1

•Ci

4•CI

21

•CICi<l

NiMMI-D

3ppb

10O

499

56

C36

C3

C3C3<319

7

183758

RbMMi-n

1ppb

6831547071

7118596153

575561

62

2927481120

YMMI-D

0.1ppb

CO.l•CO 1

0.10.1

CO.I

0.70.2

•CO.I0.2

•CO.I

CO.l•CO.I•CO.]

0.12.1

0.20.6

•CO.ICO.l

0.3

NbMMI-D

0.1ppb

CO 1CO 1•CO.ICO.I•co.)

0.3cO.lCO.!CO.ICO.I

CO.ICO.ICO.ICO.I

0.2

CO.ICO 1CO.IcO.lCO 1

PdMMI-D

0.1ppb

CO.lcO 1CO.ICO 1cO.l

CO.ICO.lCO.lCO.lCO.l

CO.lCO. ICO.l

0.1CO.l

co.icO.lCO.lcO.lCO.l

BaMMI-D

0.1ppb

434321118187262

164197139343280

16894.7192193188

25465.2190140204

LaMMI-D

0.1ppb

CO.lCO.l

0.10.20.1

2.20.4

CO.l0.2

co.i

CO.lco.icO.l

0.11.7

0.50.80.1

CO.l0.5

TaMMI-D

0,5ppb

C0.5CO. 5C0.5CO. 5CO. 5

C0.5C0.5C0.5C0.5cO.5

C0.5CO.5CO.5c 0.5CO.5

CO.5CO.5CO.5CO.5CO.5

CeMMI-D

0.1ppb

CO.]CO.l

0.30.40.3

6.10.50.20.6

CO.l

0.1CO.lCO.l

0.23.7

0.41.70.4

CO.l0.7

PrMMI-D

0.1ppb

CO.lCO 1CO.lCO 1co i

0.60.1

CO 1CO.lCO 1

CO.lCO.lCO.lcO 1

0.5

0.10.2

CO.lCO.]

0.2

NdMMI-D

0.1ppb

CO.lCO 1

0.1020.1

2.10.4

CO.l0.4

CO.l

CO.lCO.lCO.lCO.l

1.6

0.40.90.2

CO.l0.6

SmMMI-D

0.1ppb

0.20.2

CO.l0.10.1

0.40.1

CO.l0.20.1

CO.lCO.lCO.l

0.10.4

0.10.20.1

CO.l0.2



29fi0529606296072960829609

2961029611296122961329614

2961529616296172961829619

2962029621296222962329624

2959029591295922959329594

2959529596295972959829599

Date: 24/10/03

GdMMI-D

0.1ppb

0.2CO 1cO.lcO.l<0.1

CO.lcO.l<0.1<0.1CO. l

cO.lCO.lO.I<0.1<0.1

<0.1CO.l<0.l<0.1<O.I

CO 1Cd 1<0.1CO 1CO l

<0.1CO.lCO 1CO 1

0.1

TbMMI-D

0.1ppb

<0.1•CO l<0.1<0 1CO. l

CO.IO) lCO 1CO lco i

cO.lCO.lco.iCO 1CO.l


CO.lCO.lCO.lcO.lCO.l


ErMMI-D

0,1ppb

CO.lCO 1CO 1CO 1CO l

CO 1CO 1cO.lcO.lCO .1

CO.lCO.]co.icO.lcO.l

cO.lCO.lCO.lcO.lCO.l

CO.lCO.lCO.lCO.lcO.l

CO.lcO.lcO 1CO.lcO.l

YbMMI-D

0.1ppb

CO.lCO.lco.iCO.lCO.l

CO.lco.ico.iCO.lCO.l

co.iCO.lCO.lco.iCO.l


CO.lCO.lCO.lCO.lCO.I

CO.lCO.lCO 1CO.lCO.l

FINAL Page 3 of 4


Element. Method. Del. Lira. Units.

2960029651296522965329654

2965529656296572965829659

2966029661296622966329664

29665*Dup 29605*Dup29617*Dup 29594*Dup 29656

Date: 24/10/03

GdMMI-D

0.1ppb

co.ico.lCO.l<O.I<0.1

0.3•CO.]<0.1CO.l<0.1

CO.l<0.1<0.1<0.1

0.4

CO.l0.2

<0.1<0.1

0.1

Tb EMMI-D MMI-I

0.1 0.ppb pp

CO.l t:0CO.l <:0.<0.1 c-.o<0.1 co.<0.1 CO

<O.I co.co.l cO<0.1 <0.<0.1 ^.0.<0.1 ^:0.

<0 1 -ai.<0.1 <0.1<0 1 ^'01^.1 <0CO. I 0.2

<0.1 'TO.<o.l ^:o.<0.1 <0.-co l ";o.<0 1 <0.

r VbD MMI-D

0.1i ppb

<0l^.1cO.l•CO 1CO.l

CO.lCO 1co.lCO.lCO 1

CO.lco.lCO 1CO.l

02


FINAL 4 of 4



Date 04/11/03

Copy 1 to


poh# 0740347 Soil (MMI)09/10/03Cover Sheet plusPages 1 to 1


Certified By

Tim Elliott, Operations Manager

ISO 9002 REGISTERED


Report Footer: L.N.R. = Listed not received l.S. = Insufficient Sample n.a. = Not applicable -- ^ No result *INF = Composition of this sample makes detection impossible by this method M after a result denotes ppb to ppm conversion, 'W denotes ppm to 'W conversion


SGS Canada Inc. Mineral Services 1885 Leslie Street Toronto ON M3B2M3 1(416)445-5755 f (416)445-4152 www.sgs.ca

Wembet of the SGS GrouD (Socwfe Generate cje SurveiHance!

Work Order: 074795 Date: 04/11/03 FINAL page i of iElement. AuMethod. FA301Det.Um. lUnits. ppb

29494 529495 H29496 1629497 H29498 12

29499 1429500 5 *Dup 29494 6

ONTARIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Work Report Summary

Transaction No: W0420.00552 Status: APPROVED

Recording Date: 2004-APR-08 Work Done from: 2003-MAY-28

Approval Date: 2004-JUL-15 to: 2003-OCT-07

Client(s):400647 LES ENTREPRISES JILBEY LTEE 1 JILBEY ENTERPRISES LTD.

Survey Type(s):

AMAG ASSAY GCHEM MAG

Work Report Details:

Claim*

KRL 1247880

KRL 1247881

KRL 1247895

KRL 1248617

KRL 1248620

KRL 1248624

KRL 1248625

KRL 1248628

KRL 1248631

KRL 1248634

KRL 1248641

KRL 1248644

KRL 1248645

KRL 1248646

KRL 1248647

KRL 1248648

KRL 1248650

KRL 1248663

KRL 1248665

KRL 1248666

KRL 1248667

KRL 1248683

KRL 1248691

External Credits:

Reserve:

Perform51 1 ,494

36,896

36,896

S6.896

36,896

36,896

34,597

39,195

36,896

36,896

39,195

39,195

39,195

39,195

36,896

36,896

39,195

36,896

36,896

34,597

36,896

36,896

59,195

3174,701

Perform Approve

311,494

36,896

36,896

36,896

36,896

56,896

54,597

59,195

3)6,896

56,896

59,195

59,195

39,195

59,195

36,896

36,896

59,195

56,896

56,896

54,597

56,896

36,896

59,195

5174,701

50

Applied

5400

51,200

50

56,400

56,400

56,400

33,600

36,400

56,400

36,400

36,400

53,600

53,600

53,600

56,000

36,000

54,800

56,400

56,000

51,200

56,000

53,600

56,400

5107,200

567,501 Reserve of Work

567,501 Total Remaining

Applied Assign Approve Assign Approve

3400

51,200

50

56,400

56,400

56,400

53,600

56,400

56,400

56,400

56,400

53,600

33,600

53,600

56,000

56,000

54,800

56,400

56,000

51,200

56,000

53,600

36,400

5107,200

Report*: W0420.

so50505050505050

SOSO50

SOSO

SOso5050

SO3050soSO

soso

00552

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

0

so

Reserve

311,094

55,696

36,896

5496

5496

S496

S997

52,795

S496

5496

52,795

55,595

55,595

55,595

5896

5896

54,395

3496

3896

33,397

5896

53,296

32,795

567,501

Reserve Approve Due Date

31 1,094 2006-JUL-17

55,696 2006-JUL-17

36,896 2005-JUL-28

5496 2005-APR-02

5496 2005-APR-02

5496 2005-APR-02

S997 2005-APR-02

52,795 2005-APR-02

5496 2005-APR-02

5496 2006-APR-08

52,795 2005-APR-08

35,595 2005-APR-08

35,595 2005-APR-08

55,595 2005-APR-08

S896 2005-APR-08

S896 2005-APR-08

54,395 2005-APR-10

5496 2005-APR-08

5896 2005-APR-08

53,397 2005-APR-08

S896 2005-APR-08

53,296 2005-APR-08

52,795 2005-APR-08

567,501

Status of claim is based on information currently on record.

2004-Jul-27 14:40 armstrong-d52N08NE2003 2.27483 KEIGAT LAKE 900

Page 1 of 1

Ministry ofNorthern Developmentand Mines

Date: 2004-J U L-15

Ministere du Developpement du Nord et des Mines Ontario

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

LES ENTREPRISES JILBEY LTEE l JILBEYENTERPRISES LTD.1488 BIRCHDALE AVENUEHALIFAX, NOVA SCOTIAB3H 4E3 CANADA

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

Dear Sir or Madam

Submission Number: 2.27483 Transaction Number(s): W0420.00552

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.

Thank you for your prompt response to the 45 Day Notice dated June 29, 2004. The deficiencies outlined in the Notice have been corrected. Accordingly, assessment work credit has been approved as outlined on the Declaration of Assessment Work Form that accompanied this submission.

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

Yours Sincerely,

BRUCE GATES by email at

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

Gc: Resident Geologist

Felix Lee (Agent)

Les Entreprises Jilbey Ltee l Jilbey EnterprisesLtd.(Assessment Office)

Assessment File Library

Les Entreprises Jilbey Ltee l Jilbey EnterprisesLtd.(Claim Holder)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:19643

ONTARIOCANADAMining Land Tenure

Map

to o o

523000E 5240006 525000EIT"" HI 826000E 527000E 52SOOOE 529000E 530000E S31000E 533000E S34000E

seesoooN*!;

M580DON I

S6SOOOON1

UTM Zone 15 1000m grid

5662000N

6668000N

i'- T 5653000N

5852000N

5240006 530000E

rrww *fading lo w* to niwni ctewm itwutw CIWHHIH wtlMtw PFOrtxMtMfiW'u Hawid#is* onto oi thu* WnWtfyo* MM

BKorTuOan nuy altv bv eMeftml tiro*ih Un be*J Und THhn er RaghHy Of(fco.*( IN* MiMn ft Nnlural Rntdumv

General Information and Limitations

Date / Time of Issue: Frl Aug 06 13:18:43 EOT 2004

TOWNSHIP l AREA PLAN UCHI LAKE AREA G-1901

ADMINISTRATIVE DISTRICTS l DIVISIONSMining Division Red LakeLand Titles/Registry Division KENORAMinistry of Natural Resources District RED LAKE

TOPOGRAPHIC land Tenure

Z'j BWfaW UfljMa Olty

r MfrwMufe

lotfl OrJitr IfiCauna* (Not uy*n tor tt

LAND TENURE WITHDRAWALS

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONS

Wftm Jnn l, SOU l MNHfUf L UACHGWorn tan \, HW MMR FUEL ft*CMEWitOi jhn t, 30CM HimimraTnnwi tnxatti

W-KRL K.'1'S **m

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o

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542000E 543000E 544000E 54SOOOE 546000E S4TOOOE 548000E

8702000N l 5702000N

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5620006 SS3000E 554000E 5S5000E

uu wnninv PUIVHKHI Minnu ^nw-ni' onlce 01 ttwMltiertrôt Monrnin DHWWplrnm tm Mhw* .mlana l*w MtBfirt™inti puimun M in* Wfoiirwlfcn show ("l ilitinwp HdQmrtteB "nil *ano *' L*i*l Tfttoa ur NaqiMn Otlft*-01IM Minteliv cINaluxXnvteMR'ii.


M MWIIV RlKanMK' OfticnCnvmn. Alvi wrijH) fcmd twiuw otni lirj KM* Wwt vntitl or onhiMl tnu antry leatato H**IH tlalrm rr

ONTARIO SSSS^ !̂S^ Minin9 Land TenureW CAN ADA SEKSSySSBS. MaP

Date l Time of Issue: Fri Aug 06 08:48:27 EOT 2004

TOWNSHIP l AREA PLAN CASUMMIT LAKE AREA G-1751


TOPOGRAPHIC Land Tenure

(l "*"Burticn An^ MBilna Kh

SurHtee WgbDt My

a

[i —

B B

3tirtaui Aral Miring F&

OnJir bf Ottunot; (Not upon Ivr

1 (83408? 'L ™ ™ m *- *.


*T j IMPORTANT NOTICES

*B*I* 1:3*OD*


Oft o -tib

•oo

•O * J CD

3

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ONTARIOWNHTRT OF NORTHERN DBVKLOPMftHT AND MIMRS

CANADA SSS&SArm*

Mining Land Tenure Map

loas

10-J

ir1sM

to to o

511000E 512000E 513000E 5140006 515000E 5160006 517000E 518000E 81SOOOE 520000E 521000E 522000E 523000E

S981000N

6870000N -

5S81000N

,M S680000N

S677000N 1

5672000N

5160006 624000E

UTM Zone 15 1000m grtd


W Mlrtfij Rnttiffi*™.' OHIcttC™wii, JtHswflMm Uirt tanuio niia laid o**t ttwrt wstiiel ut pKrtWt hw et*rv lo slain

Dale ; Time of Issue: Mon Aug 09 08:52:21 EOT 2004

TOWNSHIP 7 AREA PLAN GOODALL G-3750


TOPOGRAPHIC Land Tenurerw**KJW Pulpit

a *"*"'

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if] 'ra -a -E! 'B 'El 'i litMtftr

LAND TENURE WITHDRAWALSf" i

W "pi Miwvj WBWI oiv tw ""l.

.. -: l. . h. ! IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONSDate Oewrtptlori

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l

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527000E 528000E S30000E S31000E S32000E 537000E 538000E

S6960OON

SflflTOOON

5694000N !

5693000N .,

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M89000N

56 SWOON

UTM Zone 15 1000m flrW

527000E

seeeoooN

5686000N

528000E 53200CE 5330CXE

inina to Mite irtmnj GlDnn ifluowcuffluswllfiitw PitH'tncMi Wfky r*pconhns- OHtca ol i(w MnHtry-oi Nminain DtrmtnpniMH urn Mfntn la

in imi' *l*o H efatalrod llwujh Itn lots l Land 7ft*ti 91 RssWry Off w, di itw Mlnhto st Mhiro! nQwurvei.


ONTARIOCANADA !E2SSi"S!!R.

Mining Land Tenure Map

Date/Time of Issue: FriAu006 13:12:24 EOT 2004

TOWNSHIP l AREA PLAN LITTLE SHABUMENI LAKE ARBM810



Corewcston. Lot

Surfeit* Anil Mvitoa Ka

(Mew* fiighl* On*

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tiv AI.H AltW'iiwul Types

IMPORTANT NOTICES


J Q!

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Map

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524000E 525000E 929000E 5320006 533000E

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5683000N

l- S680000N

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k*HmHhn ntn-9^ N ^bla^nl INn*)h Ih* bc4l Unit Tttn a, fteflMty niiu, ei tm MnMly ol Milunil niît


&VM1. AhocarMiittnd tafluwaiij M^ u*a*ttifll ttutiwl w BWWW INvanto lweiato irtr*w ttoh™ m

Date f Time of Issue: Fri Aug 06 09:00:10 EOT 2004TOWNSHIP l AREA PLAN SHABUMENI LAKE AREA 6-1881



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IMPORTANT NOTICES


HIMKTUT OF NORTHERNDimuwiiiNT MD iimn

CANADAMining Land Tenure

Map

Ul M 2; O 00

H

i-3

g M

(Oin o

M20006 513000E 514000E StSOOOE 516000ESOMME 506000E 5070COE M8000E 5090006 S100006

6673000N

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607000E 613000E 5160006

General Information and LimitationsTtoc wHIUno totlfte mwnj cwitra vhnuw c*wuM 'Win nw p^vttKK' Mrlnp rewowkm' (W(co '?1 I'm MlnBtfy ot

'âriNtian (roy flit* b* eMokwf tnnmh Un tool Ui)4 TKtot or ffeablfy C4IM. o' lin M'HAIfy ol Uilural naiowfcrmp KKomrMM ficmunrtout'KWfMv. tpntteicrKWS ana m;cuts(;f aw tm (iw

TnK nup TOY IM il*a* mmaohntresl Mm tenure eiyl ItKcnEtlii MIUM uclullnq cBMtnUHKflfe. *x"^^'

Craml. AKuutrldirll4ndl4nu'oarid tallj UM* IM wlllttl at elvrnbM Ile* ftntrj ItrvlDlia n*llrg olfllim t

Date / Time of Issue: Fri Aug 06 08:58:14 EOT 2004

TOWNSHIP l AREA PLAN SKINNER G-3758



Svrtass Awl Mtnina ffl

SurtsEe Right* Only

SurtHCB WHO MCHrij fti

i.? l "^

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ixl ""* '*

fttc] MiHbCuuntal*cHuptIi)vr*t

r"n ifîB-niwuMLl^t ! m*. I'iTfllK t


O lid'In OoMtidl 'i*W!**iml li

Will Vim;!') Msynn OiV Vi'S'iJ'iiwi

N, i IMPORTANT NOTICES


HimsTAT OF KOniHEI DffVlLOPHINT AND Ml

CANADAMining Land Tenure

Map

o

H H

toOlo

540000E S41000E 542QQOE 543000E 54500QE 553000E

S69WOON

541000E 542000E 543000E S44000E

UTM Zone 15 1000m aria

General Information and LimitationsowtawtilfW to Ml w mnW) cleNTniftBi*! ciwsim will ilw pmvvtlt! MWne wrcaMoiv Ortlca HI ino Mlnwtry o( M^ntum DvuHnvimm

tonMItwt may alto ti# GblalrHd thnwh lin bcvl uii'd UVn oi Rc^Mfy Onto. OF tin MMan D) rtotuiDI (VtGimKb. PRMAxMI Mining RteoM*™.' Ofllc*

TrUt rmp mty r^t itKW UDKOI&K'iBtl Wrrl lanwK RI l intDBKsi* In lend mciitlimj w win (wwtiti. i rotherliirrmoHRpo*itKinotrt9ft*imi nlpi

Date l Time of Issue: Fri Aug 06 13:06:69 EOT 2004

TOWNSHIP l AREA PLAN SATTERLY LAKE AREA 6-1874



Suitue Aral Mittlna Ki

f "y j

a ajei g]

' POWOT UaB* Ajr*9di*

MitWVt Oiftim

f'HHd CV*f Mnbii';mtir


t* j IMPORTANT NOTICES


Target Anomalies* EM

Evaluated Anomaliessampled, not sampled

SAMPLES Rock Sample

Soil Sample

T*A 2004 Jilbey Till Sample

QE10IO)

(T)E09(C)

Dirt-Gravel Road Hydro-Line /Trail

08(C| QEII(A)

31201h31207 B01IAJ

31209-31210

31240-3124731221-31225 31257-31261

-4 ^flW31226-31237

^3(0 31248-312529575-29589

W19(A)crjn623 J W -*-

MAP A

JILBEY GOLD EXPLORATION LTD BIRCH-UCHI PROJECT

Red Lake District212748ROCK AND SOIL SAMPLE

LOCATION MAP

A.CA Howe International Limited

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Documents

SUMMARY RPT BIRCH-UCHI PROJ - Geology Ontario