Geological Mapping and Diamond Drilling Report

Of the

Caltor Property, Laurie Township

For

Landore Resources Ltd.

Daniel Courtney BSc Clark Exploration Consulting

August 2002

52A12SW2025 2.24197 LAURIE 010

2 241 97

TABLE of CONTENTS

1 Introduction

1 Location and Access

1 Claims

Figure 1 Location Map

Figure 2 Claim Map

2 Conclusions and Recommendations

3,4,5 Previous Work

6 Regional Geology

7,8 Local Geology

8 Local Geophysics

8 Mineralization

9 Diamond Drilling

10,11,12 Sample Descriptions

13 Statement of Qualifications

Appendices Geology Map Drill Sections Drill Logs Certificates of Analyses

INTRODUCTION

This report details the geological mapping, lithogeochemical sampling, and recent diamond drilling done on the Caltor property in Laurie township of the district of Thunder Bay, Ontario, NTS 52 B/9.

Myself, and prospector Craig Maitland carried out seven days of fieldwork during the early part of August 2002. This work was confined to the area of a 12.5 km grid that was cut by Landore in 1998, and is situated on claim 1242507. A total of 48 rock samples were collected and sent to Accurassay Labs in Thunder Bay for whole rock and base metal analysis (See appended Certificates of Analyses). As well a geological map was created and is appended to this report. This work was intended to help evaluate the potential for a VMS type base metal deposit and to assist in diamond drill hole targeting.

Two diamond drill holes were drilled on this property from August 25 to 28, 2002 to test the lithologies, alteration, and VLF anomalies for potential base metal mineralization. This drilling totaled 300 meters (90 and 210 meters respectively). The core was logged, and 27 samples were split from the core of both holes and assayed for Au, Ag, Cu, Pb, and Zn. The samples were selected in sections of strong alteration and pyrite enrichment.

LOCATION and ACCESS

The property is situated approximately 60 kms west-northwest of the city of Thunder Bay, Ontario, within Laurie township (G-669). It was accessed via the Shabaqua road, which travels south from Shabaqua on highway 11 for approximately 6.5kms. From there a network of logging roads and an AW (snowmobile) trail was traveled for 3.4 kms to the property site.

CLAIMS

The area in question represents a portion of a block of 14 contiguous, non- patented claims comprising 145 units. All claims are held 1000Xo by Landore Resources Inc. and presently in good standing. (See Claim map).

CALTOR PROPERTY Beardmore

Manitouwadge

oL

50

Scale

100

Km

150 200 l

LANDORE RESOURCES LTD.

CALTOR PROPERTYTHUNDER BAY AREA. NORTHWESTERN ONTARIO

REGIONS-SCALE UKATTON MAP

i Cortmroptiy: ft Cmrtn^

CLARK EXPLORATION CONSULTING

MINING LAND TENURE

MAP

General Information and Llm Ile lions

D*t* l Tim* of IHIM Sap g 2002

TOWNSHIP/AREA

LAURIE

10i48hE**t*rn

PLAN

Q-0669

ADMINISTRATIVE DISTRICTS l DIVISIONSMining Dhrliton Thunder Bay

Land THlei/Ragldry Division THUNDER SAY

MlnUtry of Natural R e to ore*. District THUNDER BAY

TOPOGRAPHIC LAND TENURE

Q -~"...0 ™.M,Q .™.

a —.^,EI"a"Q Q Q

B B Q

LAND TENURE WITHDRAWALS

IMPORTANT NOTICES

LAND TENURE WITHDRAWAL DESCRIPTIONS

t M HUH umf

IMPORTANT NOTICES

CONCLUSIONS AND RECOMMENDATIONS

The package of felsic to intermediate pyroclastics along with the bedded chert in CT-02-01 represents favorable lithologies for a VMS type base metal deposit. Hydrothermal alteration within the mapped area and in drill core is variable in strength but likely represents a significant system in size and intensity. The area mapped and the drilling done covers only a small portion of this volcanic belt and Landore's claim block. As such further exploration is recommended. Cutting a control grid, geological mapping and lithogeochemical (whole rock and base metals) surveying is suggested for a first phase of exploration. This exploration work should aid in any delineation of favorable (exhalative) horizons, areas with the strongest intensity of hydrothermal alteration (Na -depletion etc.), and base metal enrichment. Contingent to the results of this first phase, a second phase of exploration should involve a penetrative Deep EM or large loop geophysical survey, oriented properly for good coupling on favorable horizons. Finally if these phases of exploration prove encouraging, a diamond drill program could then be designed maximizing efficiency and potential.

PREVIOUS WORK

The first work reported was in 1896 by a government geologist (ResidentGeologist's Files). A gold showing on the shore Gold Creek in auriferous,siliceous, pyritic schist, and became known as the "Old Quartzite Mine".Evidence of these workings is visible today in the west part of claim # TB-1233796.Minor exploration has been conducted in the area from this time until presently,for gold, base metals, and iron.

1943-1944; Gunflint Iron Mines Ltd conducted surface prospecting, trenching, channel sampling, and diamond drilling on a block of 56 claims containing the "I- Zone". Twelve holes were drilled totaling 2,796 feet (852 meters) were drilled testing gold showings and part of the Matawin iron formation.

1956-1957; Monpre Mining Company Ltd. Conducted geological mapping, magnetometer surveys and diamond drilling 10,592 feet (3,288 meters) on the Matawin iron formation central to Duckworth and Laurie townships. 100 million tons of 30*ft iron was delineated.

1958; George Chilean excavated four trenches and drilled ten holes totaling 564 feet (172 meters) on the "Chilean Occurrence" which is along the northwest shore of Sand Lake in Laurie township

1972; D.Scali and V. Borschneck completed airborne magnetometer and electromagnetic surveys near Gold Creek on a block of 31 claims. Several of the resultant anomalies were tested with three drill holes, which totaled 1,605 feet (489 meters).

1972-1973; T.C. Byrne, the Caltor Syndicate, Noranda Exploration conducted 3,371 feet (1,028 meters) of diamond drilling in the southern portion of the property in the search for base metal mineralization.

1983; Jalna Resources Ltd conducted an exploration program that included ground and airborne geophysical surveys, geological mapping, geochemical surveys, trenching, and overburden drilling.

1984-1985 (winter); Anaconda Canada Exploration Ltd followed up Jalna's program with thirteen drill holes totaling 3,665 feet (or 1,117 meters). Due to financial difficulties, Jalna terminated the option of their "Gold Creek" property (415 mining claims), and the property was subsequently optioned to INCO in November 1986.

PREVIOUS WORK (continued)

1987-1989; INCO began a significant exploration program. A control grid was cut over the majority of the claims, geological and magnetic surveys were conducted, and select areas of anomalous gold mineralization were stripped and trenched. This in turn was followed up with 14 drill holes comprising 4,753 feet (1,449 meters). In 1988 stripping and trenching was undertaken on 15 areas of gold mineralization. Four holes were drilled in in the south central portion of the property in April totaling 2,004 feet (611 meters), and in October and November of that year twelve more holes were drilled (3,752 feet or 1,144 meters). A 1 km all weather road was also constructed to access the "l-Zone" (dyke 10). In 1989 more stripping, trenching and detailed channel sampling was done, and a further eleven holes (4,175 feet or 1,273 meters) were drilled on this zone. INCO also conducted a bulk sample cyanide leach test on the channel samples from the I- Zone, and proved a QG.2% recovery. The sample averaged 1.05 g/t Au. From surface the chip samples averaged 1.5 g/t Au, but it remains uncertain whether all of the samples were included in the leach test.

1995; Laminco Exploration completed a limited diamond drilling program on the I- Zone (dyke 10). A total of 1,000 linear feet (305 metres) was drilled at a low angle to the felsic dyke in order to obtain a longer section through the dyke for assay purposes. Seven (7) short holes were completed. Hole # A W -95-4 has been assayed by conventional method in one metre sections and the rest of the holes were saved for leaching tests.

1996; A ground geophysical survey totaling roughly 80 kilometres of grid lines was completed across the central part of the original claim block during the period of March to May.

The systematic electromagnetic VLF-Em 16 survey along with locally a magnetic survey, in the northern part of the grid, were oriented at locating some of the major geological structures known to be present within the surveyed area, namely the north and south contacts of the Timiskaming sediments, the extension of the Crayfish Creek Fault and the presence of a gabbroic plug.May 1996; An area of approximately 150 metres by IOO meters was detailed on former claim # TB-786756 in. The hand stripping and mapping exposed an ENE trending syenite dyke intruding well foliated felsic lapilli breccia. This syenite dyke is exposed across a width of about 70 metres. Previous work by Inco (1987) returned a grab sample grading 1.76 ppm Au from the general area. The dyke itself is un- deformed but is veined and fractured, especially near the northern contact. Also in May 1996, an additional 2,000 linear feet of diamond drilling has been completed within the southern part of the study property in order to investigate different targets within the felsic volcanic belt. Three holes (747 feet) were drilled in the area of the "North Zone" to establish the stratigraphy in the area which returned 3.10 gpt Au over an average width of 2.43 metres along a 54.9 metres strike length in surface sampling by previous operators. Another three holes totaling 737 feet, were drilled on the "South Zone" where a previous drill hole by Inco (hole # 78411-0) returned anomalous gold values of 1.63 gpt Au over 7.5 meters. Surface sampling in the area also returned values of 0.64 gpt Au from 63 samples covering an area of 14 meters by 22 meters.

4

PREVIOUS WORK (continued)

The last three holes were drilled on new structures (cherty horizon, sericite schist zone, syenite dyke) within the felsic volcanic belt to obtain a cross section of the geology in these areas,

1995 and 1997; Landore Resources Inc. acquired the property as part of a major transaction completed in October 1997. Very limited exploration programs were completed intermittently on the claims, principally to satisfy the requirements of assessment work. The exploration work included ground geophysics and prospecting-mapping on and adjacent to the present claim holding. The most significant work completed by Landore was diamond drilling on the l-zone in (now claims TB-1240535 and TB-1233500).

2000; Wilson completed a satellite imagery study, and consultant J. Stockley completed an evaluation on the claim blocks also in 2000. All of the above information is available within the assessment work files at the office of the Resident Geologist's in Thunder Bay.

REGIONAL GEOLOGY

The Gold Creek property is situated in the western portion of the Shebandowan-Wawa greenstone belt, which is part of the Superior Structural Province of the Canadian Shield.

Keewatin volcanics including rocks of komatiitic, calc-alkalic, high potassium calc-alcalic and shoshonitic affinities are the main constituents of the belt. These also locally contain intercalated 'flysch' sediments. Mafic and felsic intrusives, such as the Shebandowan Lake stock, cut all rock types. Timiskaming type sediments and associated high potassic calc-alkalic and shoshonitic volcanics occur above an unconformable contact with the Keewatin lithologies. All rock types are cut by late diabase and lamprophyre dykes.The Ministry of Northern Development and Mines have recently recognized the area as a potential new gold belt within the Thunder Bay Mining District. The Ministry also published in 1994 a compilation map of all the gold showings closely related to what they referred to as the Matawin Gold Belt

LOCAL GEOLOGY

The mapping and sampling pertaining to this report represents a limited area approximately 1km by 1km in size. As mentioned this work covered the ground of a previously established control grid. This grid is situated approximately between UTM coordinates (NAD 83): 5,378,800 to 5,380,OOON and 281,000 to 282,200 E. The baseline is oriented at 55 degrees, and the lines run at 145 degrees, accommodating the general strike of 45 to 65 degrees to the rocks of this area, (see appended geology map)

Topographically the northern half of the mapped area is witnessed to rise some 30 to 40 meters above the lower half of grid, probably due to the competency of the 'ridge1 of Felsic Pyroclastics that occupy this space. Outcrop exposure here can reach up to 8007o. To the south the ground is lower and results in a paucity of outcrop. This area is covered with mature and typical Boreal forest of Jack pine, Spruce, Poplar, Birch, Balsam, and Alder.

The vast majority of the bedrock encountered is an extensive and thick unit of Felsic to Intermediate Pyroclastics, and occupies most of the northern portion of the grid. This unit varies from ash tuff to lapilli tuff to agglomerate with fragments up to 10cm in size. The material is very fine grained to aphanitic, is cream, grey, and grey green in colour, and is quite hard and competent where it is not strongly foliated. Locally quartz eyes or crystals were observed in ash - crystal tuff.

Alteration observed in this unit is nearly ubiquitous and ranges from weak to strong. Sericite is the prominent alteration mineral, and appears to have replaced original feldspar, occupies selvages to fragments, can be intimate with a cherty groundmass, or is cleavage and shear related. Lesser chlorite was encountered and displays a similar habit to the sericite. Calcite and spotted or wispy ankerite appears to be fracture-cleavage and or shear related. Silicification may be present but is difficult to discern given the aphanitic and siliceous nature of the protolith. Fine disseminated Pyrite occurs in trace or very minor amounts, but reaches up to 207o at sample site DC025 as coarse-grained cubes. Sample DC020 contains up to 1 0Xo disseminated Pyrite (or feox after Pyrite) as streaks which might be bedded in a very cherty host. Structurally these rocks typically display at least a weak amount of foliation, which is likely resultant from superimposed shearing and or folding. The majority of this rock unit displays a moderate to strong degree of schistosity. Crenulation and kinking of the fabric was seen at sample sites DC001, DC014, and DC026. Local areas of relatively massive material were witnessed near sample sites DC011, DC019, DC029 and DC037.

Three outcrops of a Qz Diorite (Andesite?) were discovered south of the baseline, and interpreted to form a narrow unit trending slightly discordantly at 45 degrees. This strike may be coincident with a fold limb that has been interpreted east of the mapped area. This rock is massive and relatively pristine. It is hornblende phyric (psuedomorphic after pyroxene?) with a very fine-grained dark green - beige groundmass. It contains only traces of disseminated Pyrite, and no contacts were found. The mode of emplacement of this unit is questionable.

7

LOCAL GEOLOGY (continued)

The third rock type within the mapped area was encountered in only two bedrock exposures, namely DC003 and DC008. These both occur in areas of lower ground and poor exposure. The rock is a clastic metasediment with polylithic rounded to sub-angular fragments. The groundmass is very fine-grained black and slaty, and the clasts observed were cherty, feldspathic, very fine grained mafic, or slaty. These two exposures were massive which may account for there standing in relief. They contained very weak fracture related chlorite and a trace of fine disseminated pyrite.

LOCAL GEOPHYSICS

Previous geophysical work has delineated two extensive VLF conductors that appear coincident with Sedimentary - Volcanic contacts. Within the map area the continuity of the conductor is broken and together with magnetic data, this volcanic- sedimentary conductive contact appears to be displaced in several locations by probable northeast trending structures. North of the baseline three discreet (discontinuous) VLF conductors exist within the western portion pyroclastic package, and may represent a sulphide rich horizon within the volcanics. Airborne electromagnetic anomalies are numerous and sporadic but appear to concentrate within the metasedimentary package, only locally are they coincident with the volcanic-sedimentary contact (and VLF anomalies).

MINERALIZATION

Other than the pyrite mineralization found at sample sites DC020 and DC025, heavy to massive sulphides have been reported in drill core. Previously drilled (1972 a 1973 by the Caltor Syndicate) hole number M1-72 encountered 2.7 meters of heavy to massive pyrite at the brecciated and faulted volcanic- sedimentary contact. Deeper in this hole and within a deformed conglomerate, T. Antoniuk reports: "abundant fine fractures , carbonate filled, some contain traces of light brown sphalerite and occasional traces galena. Scattered pyrite throughout, with a few sections heavy pyrite. 369.0 - 1" massive sphalerite, minor Cpy, traces py at 70 degrees to core". In Caltor's drill hole M3-73 "traces of Po and occasional Sph S Cpy" is also reported near the top of this hole, as well as "Abundant pyrrhotite as patches, up to 6 inch massive seams and disseminated in matrix" in a 'Quartz boulder Conglomerate'. Also at 291.4 feet is 3 inches of massive pyrrhotite, and at 371.1 S 375.6 are 1 inch seams of massive Po and 4 inches of heavy Po at 380.7 feet in intermediate volcanics. Given the structural overprint of probable folding, strain and shearing, it is possible that the observed base metal mineralization may represent remobilization from a primary VMS type deposit. With the surface sampling only two samples returned anomalous base metal values. DC016 contained 370 ppm Zn in a Felsic Pyroclastic, and DC045 returned 120 ppm CU in a mafic dyke.

Within the two holes drilled recently Py enrichment exists locally, but only a trace of base metal (Cpy) mineralization was observed. With the core sampling only one sample returned anomalous in base metals. Sample 72963 contained 112 ppmZn.

8

DIAMOND DRILLING

Holes CT-02-01, and CT-02-02 were diamond drilled on the property by Chibougamou Diamond Drilling Ltd., from August 25, 2002 to August 28, 2002. The first hole was collared at grid coordinates L4E at 1+50N, while CT-02-02 was collared on the same grid on L7E at 2+35N. Both holes were set to a bearing of 145 degrees with a dip of-45 degrees. These holes were designed to test the volcanic lithologies, alteration, VLF anomalies, and for possible base metal mineralization.CT-02-01 was collared and ended (at 90.0 meters) in the variably altered and vertically dipping package of felsic to intermediate pyroclastics. This hole also encountered a narrow mafic dyke and feldspar porphyry breccia (with up to y/o disseminated Py), which might be causing the surface VLF response. However, of interest was the intersecting of a finely bedded intra-formational argillite * chert. At 1.7 meters (true width) this horizon represents a period of relative quiescence within an explosive regime. With S-5% finely bedded anhedral Py and up to 300Xo interbedded chert this unit is arguably exhalative in nature and may offer an alternative explanation to the VLF anomaly (depending on the true dip of the rocks here). (See appended drill log and section).CT-02-02 was drilled through two surface VLF conductors. The first VLF response close to the collar may be explained by 2-30Xo of matrix hosted Py found between 20.7 and 24.0 meters, or the strong chlorite that is intimate with chert. The strong shear zone encountered from depths 167.8 to 169.8 meters easily explains the second VLF anomaly. This shear with intense chlorite also contained 1 07o disseminated and laminated Py as well as local clay rich gouge. (See appended drill log and section).Hydrothermal alteration in both of these holes appears nearly ubiquitous to a weak degree, and local sections are strongly altered. Sericite and chlorite are the predominant alteration assemblages. This alteration is pervasive in nature, however the fragmental matrix appears preferential in areas of weaker alteration intensity.Structurally the rocks of this belt have interpreted to be folded. Evidence of a structural overprint exists with the various degrees of intensity in their foliation and local crenulation and kinking. Also the dips of rock fabrics were witnessed to swing from a steep southerly dip in the central portion of the grid through vertical and then a steep northerly dip in the northern portion of the grid. Previous drilling (holes M1-72, and M3-73) shows a major structure and unconformity between the volcanic sediments and Timiskaming sediments.

SAMPLE DESCRIPTIONS

DC001 Felsic tuff, vfgr-aphanitic, mod sericite, mod fol'n (shear), +I- chl Tr feox, cherty texture, cream-grey-green

DC002 Felsic ash tuff, wk ser, local wispy ankerite, tr-,5% Py, wk fol'n

DC003 Clastic metasediment, polylithic frag's, chl alt grndms, tr Py

DC004 Felsic ash tuff- agglomerate, relatively mass, siliceous, tr Py Local 5cm rounded bombs, wk ser

DC005 Felsic tuff - agglomerate, mod fol'n, mod ser, str sericite, wk calcite (sil'd?), tr Py

DC006 Lapilli tuff, mod-str fol'n, mod ser, tr wfgr Py, *7-chl

DC007 Felsic pyroclastic, mod fol'n, mod ser, +/-CN, mottled cream colour Wk feox

DC008 Clastic metasediment, rounded polylithic clasts, black soft aphanitic grndms, tr Py

DC009 Dioite (Andesite?) fgr with mm hornblende phenos, mass, pristine

DC010 Felsic lapilli tuff, angular b rounded lapilli, siliceous wk ser, wk calc, tr fecarb

DC011 Felsic ash tuff, generally mass, mod ser

DC012 Felsic ash tuff, mod fol'n, mod ser, (sil'd?), fracture related chl, tr fecarb

DC013 Felsic pyroclastic, mod-str fol'n, mod ser, tr py

DC014 Felsic pyroclastic, (crystal tuff- local qz eyes), schistose, str ser + wk chl, crenulated fabric

DC015 Felsic pyroclastic (tuff), str fol'n, mod ser, *7-chl, tr - .50Xo Py

DC016 Felsic tuff, str fol'n, str alt'n - str ser + wk laminated chl

DC017 Felsic pyroclastic, str fol'n -curvilinear fabric, mod ser, tr - .507o Py

DC018 Felsic (intermed ) lapilli tuff, mod-str fol'n, str ser, mod chl, tr calc

DC019 Felsic lapilli tuff, relatively mass, mod ser, cherty grndms, tr py10

SAMPLE DESCRIPTIONS (continued)

DC020 Felsic tuff (bedded?), cherty and qx flooded -ci 07o streaky feox/py

DC021 Felsic tuff, relatively mass, aphanitic cherty, tr -1 0Xo Py/Po

DC022 Felsic tuff, wk fol'n, siliceous, aphanitic, pale cream colour, tr Py

DC023 Quartz vein, 10-25 cm (boudined) spotted fecarb

DC024 Felsic crystal tuff (local lapilli), grey green, wk fool'n, wk-mod ser, tr Py/Po, qz crystals

DC025 Felsic tuff, wk fol'n, mod ser, 1-207o cgr euhedral Py

DC026 Felsic tuff, mod ser, mass (local wk fol'n), mottled, tr Py

DC027 Felsic pyroclastic, wk fol'n, mod ser, tr py

DC028 Felsic pyroclastic, wk-mod fol'n, str ser, mod chl, tr Py

DC029 Felsic crystal tuff, relatively mass, aphanitic -siliceous, spotted chl, qz crystals

DC030 Felsic Pyroclastic, mod fol'n, siliceous, str ser, lesser chl

DC031 Felsic pyroclastic, relatively mass, str ser, up to 50Xo fracture controlled Py

DC032 Felsic pyroclastic (agglomerate), wk-mod fol'n, str ser lesser chl mostly around selvages to 'bombs', rare tr Py

DC033 Felsic tuff, str-mod fol'n, str ser, wk chl, tr feox, tr fecarb

DC034 Felsic pyroclastic, wk-mod fol'n, str ser, tr Py

DC035 Felsic pyroclastic, relatively mass mod ser, rare tr Py

DC036 Felsic ash/lapilli tuff, pale cream, generally mass, str ser, tr ultra fgr Py

DC037 Felsic pyroclastic - rhyolite, relatively mass and homogenous, siliceous, wk-mod ser

DC038 Felsic pyroclastic, wk fol'n, local coarse clasts, mod ser

11

SAMPLE DESCRIPTIONS (continued)

DC039 Felsic lapilli tuff, wk fol'n, mod-str ser

DC040 Felsic pyroclastic, local fol'n, mod ser, aphanitic

DC041 Felsic-intermediate pyroclastic, str ser b chl, minor carb 8t feox

DC042 Intermediate pyroclastic, wk fol'n, dark grey-green, wk ser mod-str chl, tr feox

DC043 Felsic Pyroclastic, wk-mod fol'n, mod ser, tr fecarb, siliceous

DC044 Felsic (-intermediate) ash tuff, relatively mass and pristine, wk ser? Mm angular clasts, siliceous competent

DC045 Qz Diorite (Andesite??), speckled black (slightly hornblende phyric), mass, competent

DC046 Felsic to intermediate tuff, mod fol'n, str ser * chl, darker grey- green, carb?

DC047 Qz Diorite, mass, speckled black and beige, pristine

DC048 Felsic tuff, relatively mass, wk ser?, siliceous, black flecks

12

STATEMENT of QUALIFICATIONS

l, Daniel Courtney , of Kaministiquia, Ontario, Canada, hereby certify:

-That l am a practicing Exploration Geologist, residing at RR#1 Kaministiquia, Ontario, Canada, POT 1X0

-That l hold a BSc degree in geology from Lakehead University in Thunder Bay.

-That l have practiced my profession as an exploration Geologist since 1984.

-That l have received no interest, direct or indirect, in the mining claims and property described in this report.

Dated at Thunder Bay, Ontario this 9th day of September 2002

13

Preliminary AnalysisTuesday, September 10, 2002

Clark Consulting 1000 Alloy Dr. Thunder Bay, ON, CAP7A6G5Ph#: (807) 622-3284 Fax* (807)622-4156 Email gjclark@tbaytel.net

Date Received : 09-Aug-02 Date Completed : ]6-Aug-02

Job # 200240537 Reference : Shebandowan

Sample #: 47 Rock

Accurassay #20147

20148

20149

20150

20151

20152

20153

20154

20155

20156

20157 Check

20158

20159

20160

20161

20162

20163

20164

20165

20166

20167 Check

20168

20169

20170

20171

20172

Client: tdDC-001

DC-002

DC-003

DC-004

DC-005

DC-006

DC-007

DC-008

DC-009

DC-010

DC-010

DC-011

DC-012

DC-013

DC-014

DC-015

DC-016

DC-017

DC-018

DC-019

DC-019

DC-020

DC-021

DC-022

DC-024

DC-025

A, z o3"/o

10.124

[2.780

14.362

17.344

13.229

13.781

10.991

11.264

10.408

13329

9.973

12.212

12.439

12.691

12.148

18.928

13.218

14.145

14.488

12.247

13.026

5.569

14.921

12.431

13.383

13.418

CaO

%1.133

3.239

8.692

3.460

2.751

3.348

1.697

5.453

5.081

2.916

4.114

3.377

3 191

2.907

2.341

2.560

3.930

2.686

2.514

1.474

2.027

2.678

1.501

2.710

9.932

4.704

Fe2 03

"/o

2.697

3.290

10.430

1.983

1.508

3.520

2.472

7.934

7.180

5.074

3.903

4.442

4.494

3.134

3.454

3.114

1.788

7.618

5.863

6.650

1.534

2.067

7.375

4.527

2.886

5.943

K2 0

%1.086

2.049

0.877

0.510

1.076

1.381

0.883

0.673

0.926

1.907

1.244

1.745

1.335

1.867

0.895

1.571

0.933

0.675

1.626

0.930

1.387

0.467

1.109

1.692

0.892

0.742

MgO

"/o

0.806

0.863

5.861

2.001

0.747

1.097

0.942

3.921

3270

2.103

2.154

2.054

1.116

0.733

1.175

0.724

0.959

1.780

1.379

1.616

0.769

1285

1.494

1.281

1.491

2.363

MnO

"/o

0.022

0.067

0.135

0.050

0.036

0.059

0.035

0.118

0.106

0.065

0.049

0.063

0.078

0.041

0.045

0.054

0.041

0.058

0.088

0.091

0.027

0.041

0.095

0.067

0.142

0.070

N,0

"/O

2.992

3.941

2.917

8.477

4.324

3.175

3.708

2.507

2.437

4.184

4.353

4.083

3.065

3.158

2.840

6.456

5.634

3.543

4.273

2.753

4.508

2.541

2.761

3.773

4.287

3.849

Pz o5"/o

0.089

0.143

0.079

0.116

0.108

0.106

0.143

0.078

0.087

0.123

0.089

0.108

0.964

0.127

0.098

0.127

0.110

0.071

0.088

0.084

0.098

0.038

0.093

0.113

0.096

0.104

Si02

"/o

42.402

52.875

37.352

44.786

53.648

38.793

50.913

47.465

39278

56.598

53.987

47.735

58.835

44.890

42.137

50.514

52.344

51.523

42.697

51.885

54.643

57.739

56272

41.692

34.162

35.775

iS"/o

0298

0.357

0.820

0.375

0.351

0.367

0338

0.566

0.467

0.371

0.268

0.294

0.346

0.378

0.283

0.360

0.347

0.498

0287

0.361

0.400

0.123

0.532

0.491

0.263

0.268

LOI

"/o

1.835

2.733

5.347

2.802

1.865

4.866

1.582

4.401

6J205

2.410

1.116

0.532

2.505

3.516

2.496

2.174

3.340

3.386

2.421

3.723

0.924

0.684

1.411

0.785

7.394

2.800

Total

'/o

63.484

82.337

86.872

81.904

79.643

70.493

73.704

84.380

75.445

89.080

81.250

76.645

88.368

73.442

67.912

86.582

82.644

85.983

75.724

81.814

79.343

73232

87.564

69.562

74.928

70.036

PROCEDURE CODES: AUCu, AUZn, ALICPWR Page l of 3

AL918-0049-OW10/2002 0327PM

Tuesday, September 10, 2002

Clark Consulting 1000 Alloy Dr. Thunder Bay, ON, CAP7A6G5PI* (807) 622-3284 Fax*: (807)622-4156 Email gjclark@tbaytel.net

Preliminary Analysis

Date Received : 09-Aug-02 Date Completed : 16-Aug-02

Job # 200240537 Reference : Shebandowan

Sample #: 47 Rock

Accurassay #20173

20174

20175

20176

20177 Check

20178

20179

20180

20181

20182

20183

20184

20185

20186

20187 Check

20188

20189

20190

20191

20192

20193

20194

20195

20196

20197 Check

20198

Client tdDC-026

DC-027

DC-028

DC-029

DC-029

DC-030

DC-031

DC-032

DC-033

DC-034

DC-035

DC-036

DC-037

DC-038

DC-038

DC-039

DC-040

DC-041

DC-042

DC-043

DC-044

DC-045

DC-046

DC-047

DC-047

DC-048

AI 2 03

"/o

15.383

13.795

14.238

13.353

12.906

12.599

12.638

8.731

12.392

13.174

11.975

9.646

8.844

11.931

14.797

11.603

8.974

12.983

9.540

13.771

11.088

14.049

11.131

11.235

10.978

13.766

CaO

K2.594

3.682

2.890

2.208

1.318

1.251

5.224

3.706

1.881

1.576

1.611

2.006

1.098

2.322

2.043

2.965

2.691

3.404

4.511

3.744

3.176

6.790

3.631

8.340

7.401

1.557

FC2 03

"/o

3.603

3.200

4.338

1.806

2.670

1.732

3.250

3.505

1.243

t.682

2.710

2.090

1.346

2.899

2.458

3.548

3.515

9.317

4292

4.056

3.843

9.092

10.178

8.293

9.919

3.560

K2 0

"/o

3.076

1.149

1.720

1.319

1.155

1283

0.931

0.467

2265

1.350

1.372

1.105

0.943

0.778

0.686

1.216

0.931

1.025

1.014

1.649

0.801

0.732

0.430

1.235

1.150

1.709

MgO

"/o

1220

0.996

1.016

0.815

0.486

0.623

1.251

1.234

0.313

0.377

0.889

0.652

0.530

1.046

0.893

1.340

1.146

6.303

2.861

1.615

1.066

2.848

1.692

2.621

2.733

1.004

MnO

"/o

0.041

0.047

0.057

0.027

0.026

0.029

0.095

0.043

0.034

0.043

0.041

0.022

0.021

0.042

0.030

0.028

0.042

0.078

0.068

0.043

0.055

0.117

0217

0.094

0.088

0.134

N^O

"/o

5.576

4.951

3.985

4.725

4.509

2.961

3.643

2.859

3.375

4.502

3.522

3.432

3.099

5.067

6.178

3.928

2.829

2.432

2.150

4.385

4.884

3.502

2340

2.724

2.658

4.777

P2 os"/o

0.117

0.093

0.139

0.107

0.099

0.300

0.095

0.181

0.099

0.105

0.102

0.086

0.138

0.081

0.082

0.110

0.844

0.125

0.143

0.196

0264

0.144

0.108

0.115

0.104

0.269

SiO2

"/o

49.641

46.006

38.628

46224

43282

48.802

51.895

34.138

57.011

60.967

44.262

34.865

45.870

44.349

47.281

49.695

36.163

44.830

40.374

53.173

38.463

43.003

48.226

32.977

42.436

40.977

1"/o

0.351

0.324

0.442

0.355

0.354

0.350

0.393

0.326

0.427

0.451

0.385

0.264

0.233

0231

0.241

0.389

0.301

0.401

0.397

0.420

0.424

0.483

0.556

0.397

0.396

0.439

LOI

"/o

1.020

4.966

3.431

1.849

1.669

2.390

6.855

3.929

2.752

2.329

1.769

0.962

1.763

1.120

0.717

2.582

2.998

2.691

1.751

1.573

1.511

0213

11.667

0.000

0.000

0.000

Total

"/o

82.622

79.209

70.884

72.788

68.474

72.320

86.270

59.119

81.792

86.556

68.638

55.130

63.885

69.866

75.406

77.404

60.434

83.589

67.101

84.625

65.575

80.973

90.176

68.031

77.863

68.192

PROCEDURE COOES: ALACu, AljtZo, ALICPWR Page 2 of 3

AL91g-0049-OWl(V2002 03:27 PM

Preliminary AnalysisTuesday, September 10, 2002

Clark Consulting 1 000 Alloy Dr. Thunder Bay, ON, CA P7A6G5

Email gjclark@tbaytel.net

Date Received : 09-Aug-02 Date Completed : 16- Aug-02

Job # 200240537 Reference : Shebandowan

Al O CaO Fe O K O MgO MnO Na O P O SK) TiQ LOt

Accurassay # Client [d ya "/0 y0 y0 y0 "/0 y0 "/0 y0 y0 y022620 SY41 17442 7 -030 5 -970 '-035 0 -696 0 -061 6 -729 0 -095 42 -672 O-281 4 -218

22621 SY42 I6 -75i 6 - 740 5 - 508 l -058 0 -690 0061 6 - 5M O-090 39954 O-241 5 -631

Total

"/o

86^29

83.258

PROCEDURE CODES: AL4Cu, AL4Zn, AUCPWR Page 3 of 3

AL918-0049-09/10/2002 03:27 PM

Q /tccurassayX LO BIO iCwtC) P 1 OS A DIVISION OF ASSAY LABORATORY SERVICES INC.

MINERAL ASSAY DIVISION

SUnOlHU CW^OI 01 CjTJfia

Palt. tJ4orio-4iWTiJ4

1070 LITHIUM DRIVE, UNIT 2 THUNDER BAY, ONTARIO P7B 6G3 PHONE (807) 626-1630 FAX (807) 623 6820 EMAILaccuracy@tbaytel.net WEBwww.accurassay.com

Certificate of AnalysisTuesday, September 10, 2002

Clark Consulting 1000 Alloy Dr. Thunder Bay, ON, CAP7A6G5 Ph#: (807)622-3284 Fa)*: (807)622-4156 Email aclark@tbaytel.net

Accurassay #

26079

26080

26081

26082

26083

26084

26085

26086

26087

26088

26089 Check

26090

26091

26092

26093

26094

26095

26096

26097

26098

26099 Check

26100

PROCEDput COUtsT-AJJ

Certified Bftr^^^

Au R Pd Client Id . . ppb ppb ppb70453 ^

70454 32

70455 cs

70456 10

70457 5

72951 5

72952 6

72953 9

72954 ^

72955 6

72955 -C5

72956 9

72957 22

72958 6

72959 5

72960 ^

72961 24

72962 13

72963 ^

72964 cS

72964 ^

72965 ^

tAti3, ATteg, AL4Cu, AL4Pb,AO2n ""N

fcS^Z. - - r ̂

Date Received : 09-Apr-02 Date Completed : 09-Sep-02

Job #200240666 Reference: Landore-Caltor

Sample #: 25 Core

Rh Ag Co Cu Fe Ni ppb ppm ppm ppm ppm ppm

*:l 22

17 20

1 21

1 14

1 77

^ 16

CI 23

< 1 23

CI 14

si 10

<l 10

<l 22

ci 30

<l 34

ci 19

<l 21

<l 16

*:l 18

<l 28

ci 25

<l 27

41 26

Pb ppm

16

14

18

17

21

12

17

15

14

10

11

10

11

11

16

16

15

11

13

10

13

12

Page

Zn ppm

31

21

32

31

36

51

84

26

19

11

11

14

19

12

34

64

51

26

112

21

13

14

Iof2

AL917-0049-09/10/2002 03:24 PM

•T- Laboratories A DIVISION OF ASSAY LABORATORY SERVICES INC. MINERAL ASSAY DIVISION

1070 LITHIUM DRIVE, UNIT 2 THUNDER BAY, ONTARIO P7B 6G3 PHONE (807) 626-1630 FAX (807) 623 6820 EMAIL accuracy@tbaytel.net WEB www.accurassay.com

Certificate of AnalysisTuesday, September 10, 2002

Clark Consulting 1000 Alloy Dr. Thunder Bay, ON, CA P7A6G5Ph#: (807)622-3284Fax#: (807)622-4156Email gjclaric@tbaytel.net

Date Received: 09-Apr-02 Date Completed : 09-Sep-02

Job # 200240666 Reference: Landote-CaltorSample #: 25 Core

Accurassay #

26101

26102

26103

26104

26105

Client Id

72966

72967

72968

72969

72970

Au R Pd Rh Ag Co Cu Fe Ni Pb Znppb ppb ppb ppb ppm ppm ppm ppm ppm ppm ppm

6 < l 29 12 16

•ci 21

29

4

13

10 30

15 29

15 20

10 14

PROCEI

Certified Byi\AL917-0049-09/KVM02 03:24 PM

g, AL4Cu, Page 2 of 2

/iccurassay Laboratories A DIVISION OF ASSAY LABORATORY SERVICES INC.

MINERAL ASSAY DIVISION

1070 LITHIUM DRIVE, UNIT 2 THUNDER BAY, ONTARIO P7B 6G3 PHONE (807) 626-1630 FAX (807) 623 6820 EMAILaccuracy@tbaytel.net WEBwww.accurassay.com

Thursday, August 15, 2002

Clark Consulting 1000 Alloy Dr. Thunder Bay, ON, CA P7A6G5Ph#: (807)622-3284 Fax#: (807)622-4156 Email gjclaric@tbaytel.net

Certificate of Analysis

Date Received: 09-Aug-02 Date Completed:

Job #200240537 Reference: Shebandowan

Sample #: 47 Rock

Accurassay #

20147

20148

20149

20150

20151

20152

20153

20154

20155

20156

20157 Check

20158

20159

20160

20161

20162

20163

20164

20165

20166

20167 Check

20168

PROCEDUEtCOOES^fc-

Au Client Id .

ppb fDC-001

DC-002

DC-003

DC-004

DC-005

DC-006

DC-007

DC-008

DC-009

DC-010

DC-010

DC-011

DC-012

DC-013

DC-014

DC-015

DC-016

DC-017

DC-018

DC-019

DC-019

DC-020

hCjj^AL4Zn, ALICPWR f ~

L/-L' ^^

R Pd Rh Ag Co Cu Fe Ni Pb Zn ppb ppb ppb ppb ppm ppm ppm ppm ppm ppm ppm

10

18

65

4

18

20

16

57

25

28

28

9

13

17

16

10

12

23

19

14

14

4

53

33

104

23

15

58

80

126

85

73

74

19

62

55

53

45

370

132

76

61

59

15

Page l of 3

AL917-0049-OS'15ao02 08:39 AM

Laboratories A DIVISION OF ASSAY LABORATORY SERVICES INC. MINERAL ASSAY DIVISION

1070 LITHIUM DRIVE, UNIT 2 THUNDER BAY, ONTARIO P7B 6G3 PHONE (807) 626-1630 FAX (807) 623 6820 EMAIL accuracy@tbaytel.net WEB www.accurassay.com

Certificate of AnalysisThursday, August 15,2002

Clark Consulting 1000 Alloy Dr. Thunder Bay, ON, C A P7A6G5Ph#: (807)622-3284FaxX: (807)622-4156Email gjclarfc@tbaytel.net

Date Received: 09-Aug-02 Date Completed:

Job #200240537 Reference: Shebandowan

Sample #: 47 Rock

Accurassay #

20169

20170

20171

20172

20173

20174

20175

20176

20177 Check

20178

20179

20180

20181

20182

20183

20184

20185

20186

20187 Check

20188

20189

20190

PROCEDURE^ODES: M*

Certified B)fA ^-"AL917-0049-OgnS0002 08:59 AM

Au Client Id ppb

DC-021

DC-022

DC-024

DC-025

DC-026

DC-027

DC-028

DC-029

DC-029

DC-030

DC-031

DC-032

DC-033

DC-034

DC-035

DC-036

DC-037

DC-038

DC-038

DC-039

DC-040

DC-041

ICu, AL4Zn, AUCPWR x-\i ^****\. ~* * l

H---O- -- ~~

R Pd Rh Ag Co Cu Fe ppb ppb ppb ppm ppm ppm ppm

15

14

12

20

8

10

30

21

22

H

16

17

34

25

14

1

8

6

6

5

12

14

^

Ni Pb Zn ppm ppm ppm

20

44

45

61

56

49

73

12

13

40

51

79

21

24

40

11

27

31

32

63

61

119

Page 2 of 3

A DIVISION OF ASSAY LABORATORY SERVICES INC. MINERAL ASSAY DIVISION

1070 LITHIUM DRIVE, UNIT 2 THUNDER BAY, ONTARIO P7B 6G3 PHONE (807) 626-1630 FAX (807) 623 6820 EMAIL accuracy@tbaytel.net WEB www.accurassay.com

Certificate of AnalysisThursday, August 15, 2002

Clark Consulting 1000 Alloy Dr. Thunder Bay, ON, CA P7A6G5Ph#: (807) 622-3284Fax#: (807)622-4156Email gjclark@tbayteljiet

Date Received: 09-Aug-02 Date Completed :

Job #200240537 Reference: Shebandowan

Sample #: 47 Rock

Accurassay #

20191

20192

20193

20194

20195

20196

20197 Check

20198

Client Id

DC-042

DC-O43

DC-044

DC-045

DC-046

DC-047

DC-047

DC-048

Au PI Pd Rh Ag Co Cuppb ppb ppb ppb ppm ppm ppm

13

15

31

120

28

88

84

11

Fe Ni Pb Znppm ppm ppm ppm

85

59

34

82

88

67

67

16

PROCEDUR&CODES

Certified

AL4Zn, ALIC

AL917-0049-0&IW002 08:59 AM

Page 3 of 3

DIAMOND DRILL LOG Hole CT-02-01 CLARK

Drilling Company: Chibougamau Diamond Drilling Ltd.Hole Started: August 25, 2002Exploration Co., Owner or Optionee: Landore Resources Inc.

METERAGEFROM

0

17.40

41.70

45.00

54.10

TO17.40

41.70

45.00

54.10

74.35

ROCK TYPE

Overburden

Felsic to Intermediate Pyroclastic

Mafic Dyke

Feldspar Porphyry Breccia

Felsic Intermediate Pyroclastic

Collar Elevation: Bearing: 1450

Hole Finished: 26-Aug-02Date Logged: 27-28-Aug-02Date Submitted:

Total Meterage: 90.00 m

Logged By: D. CourtneySubmitted

sA^srt

By: (Signature)roa*3n.e*i

Dip of Hole at Collar: -450

90.00 m 400

DESCRIPTION (colour, grain size, textu/e, minerals, alteration, etc.)

Felsic to Intermediate. Pyroclastic, locally massive but generally bedded and moderately foliated at500 to core axis. Cream, beige, green and grey. Polylithic clasts from mm scale to 5 cm. Clasts are typically angular, cherty or feldspathic as well as up to 507o clear quartz crystals.Material is relatively pristine, however weak sericite and local chlorite is ubiquitous. Locally clastscan have diffuse margins and are weakly silicified and sericite altered. Generally quite hard andsiliceous with weak white quartz veining and pervasive sericite alteration. Trace to .507o pyrite mostlyas fracture coatings. Weak local wispy ankerite veinlets - typically conformable with fabric.1 07o mm to 1 cm random orientations but generally cross-cutting foliation. Clasts are aphaniticin very fine-grained siliceous host.

37.70 - 39.00 m: Darker (moderate to strong chlorite) and finely bedded.

Fine-grained dark green massive mafic dyke. Upper contact in broken rubbly core. Lower contactirregular. Pristine, competent. S-4% quartz veining, hairline to 1 cm, mostly at 40" and 150 axis.

to core

70-8007o large cm-scale feldspar porphyry fragments or clasts? These fragments have diffuserounded margins and mafic matrix is very dark green, strong to weakly chloritic and contains upto 3 07o fine anhedral disseminated pyrite.

51 .80 - 52.20 m: Irregualr quartz vein - bull-white.

52.80 - 53.00 m: Bull-white quartz vein upper contact at 45", lower contact irregular.

As in 17.40-41.15 m felsic to intermediate pyroclastic. Pale cream, typically felsic clasts from mmquartz crystals to 5 cm aphanitic quartz/feldspathic sub-rounded clasts. Relatively hard andsiliceous fine-grained groundmass with weak sericite±chlorite alteration. Trace to .5 07o disseminated

Drill Hole Location: M /VO #3. 1^0 'i 85 G- ^ ymo *JCore Stored At:

Location:

Hole#: CT-02-01Page 1 of 2

Property Name: CaltorSAMPLES

No.

7045370454

FROM

45.0046.50

TO

46.5048.00

LENGTH

1.501.50

ASSAYSAu ppb check

DIAMOND DRILL LOG

Sheet OF

METERAGEFROM

74.35

76.80

90.00

TO

76.80

90.00

ROCK TYPE

Finely bedded argillite and chert

Felsic to Intermediate Pyroclastic

DESCRIPTION (colour, grain size, texture, minerals, alteration, etc.)pyrite. 1 07o mm - 1 cm white quartz veining moderate foliation at 400-500 to core axis. Grey-green and pale cream, mottled, competent generally weakly fractured.

54.10 - 59.30 m: Dark green fine-grained mafic matrix with weak chlorite alteration. Blotchy mottled appearance with multi-cm diffuse 'clasts1 of more siliceous material that is flecked with 1507o mm angular to strained siliceous fine fragments (ash??) trace - 507o disseminated anhedral pyrite.

Fineiy beded dark grey-green argillite - 20-3007o interbedded creamy grey chert (exhalative??), 3-507o fine anhedral bedded pyrite, bedding is at 500 to core axis. Well fractured mostly along bedding planes. Weak sericite and chlorite.

Weak to moderately foliated felsic to intermediate pyroclastic as in 17.40-41.15 m. Clasts are rounded to sub -round locally with diffuse margins - very weak silicification and sericite alteration. Very fine-grained to aphanitic up to 2 or 307o fine anhedral matrix supported disseminated pyrite weak blocky fracturing.

48.20 m: 6 cm bull-white quartz vein at 250 to core axis, sample 70457 has S-4% disseminated matrix hosted anhedral pyrite.

End of hole

SAMPLESNo.

7045570456

70457

FROM

74.3575.50

82.20

TO

75.5076.80

83.70

LENGTH

1.151.30

1.50

ASSAYSAu ppb check

CT-02-01

DIAMOND DRILL LOG Hole CT-02-02 CLARK

Drilling Company: Chibougamau Diamond Drilling Ltd.Hole Started: August 26, 2002Exploration Co., Owner or Optionee: Landore Resources Inc.

METERAGEFROM

0

8.70

TO8.70

67.60

ROCK TYPE

Overburden

Felsic to Intermediate Pyroclastic

Collar Elevation: Bearing: 1450 Total Meterage: 210.00 m Dip of Hole at Collar: -45"

Hole Finished: 28-AugJ:02 Logged By: D. Courtney 210.00m -37"Date Logged: 28-31-Aug-02 Submitted By: ^Signa-ture)Date Submitted: \Tte*\ ( ouA^K&U

DESCRIPTION (colour, grain size, textures/minerals, alteration, etc.)t

Felsic to Intermediate Pyroclastics. Ash-lapill tuff? Pale cream, grey and grey-green, fragmental. Clasts are ash sized to 5 cm, irregular ragged and weakly strained. Locally they become diffuse with patchy areas of weak to moderate, sericite, silica, chlorite alteration. Sericite coated margins are common. Matrix is very fine-grained and typically weakly sericitic. Clasts are felsic to intermediate in composition with sections of more mafic (chlorite altered). A weak to moderate foliation (bedding??) is at 500 to core axis. Relatively hard, weakly fractured. Local traces of pyrite as mm blebs. Local minor wispy ankerite veinlets.

20.70 - 24.00 m: Pale beigey colour (bleached), aphanitic quartz-feldspar clasts are somewhat less distinct. Section appears moderately silicified and sericite altered.

21.50 - 24.00 m: 2-307o disseminated anhedral pyrite, hosted in matrix.

24.00 - 28.20 m: Moderately altered. Matrix displays moderate dark green chlorite. Clasts are diffuse, includes a 5 cm barren white quartz vein at 26.0 m - 350 to core axis.

28.20 - 29.00 m: Strong chlorite and lesser sericite intimate with 3007o chert, probably bedded but disrupted. Minor iron carbonate as wispy veinlets.

29.00 - 30.00 m: Intermediate composition, dark green strained clasts are weakly chloritic but rock is quite pristine, blue-grey-green.

37.20 - 38.75 m: 2507o quartz flooded-veined, which are irregular and at various orientations.

39.00 -49.10 m: Ash luff-quite felsic, hard and siliceous, weak sericite, chlorite and silica? alteration. 2"7o quartz±chlorite veining mm-1 cm irregular often discontinuous and barren. Local

Drill Hole Location: M^Oe^ 5-fl^Tbx5^3-796lCAJCore Stored At:

Location:

Hole#: CT-02-01Page 1 of 5

Property Name: CaltorSAMPLES

No.

72954

72951

72952

72953

FROM

21.50

24.00

28.20

45.00

TO

24.00

25.50

29.00

46.50

LENGTH

2.50

1.50

0.80

1.50

ASSAYSAu ppb check

DIAMOND DRILL LOG

Sheet OF

METERAGEFROM

67.60

76.35

TO

76.35

122.90

ROCK TYPE

Mafic Dyke (Diabase?)

Felsic to Intermediate Pyroclastics

DESCRIPTION (colour, grain size, texture, minerals, alteration, etc.)quartz crystals-subangular 1 to 3 mm.

49.10 - 67.60 m: Intermediate pyroclastics as described in 8.70-67.60 m, fairly dark grey-green or blue-grey-green. Weak to moderate chlorite, lesser sericite (and local silicification?). Moderate foliation at 50" to core axis. 207o mm scale white quartz veinlets-orthogonal or semi-conformable to fabric. Weakly fractured.

66.70 - 67.60 m: Pale cream, bleached and weakly sericite-silica altered.

Fine-grained massive dyke, dark green to brownish. Pristine, competent and weakly to moderately fractured. Locally weakly magnetic. 2 07o mm white quartz veinlets at various orientations, sharp contacts at 45".

As in 8.70-67.60 m.

76.35 - 81.50 m: Silicified, bleached and pale coloured moderate sericite with matrix, large (1-5 cm) clasts are diffuse, hard.

81.50 - 90.60 m: Intermediate in composition, grey-gieen to dark blue-grey-green. Relatively pristine; weak chlorite and sericite. Moderate foliation at 50" to core axis. Weakly fractured. 1 07o hairline to 1 mm quartz veining.

90.60 - 97.70 m: Pale grey-green (bleached) silicified? Relatively homogeneous and hard, weak pervasive sericite. Wispy and veined chlorite (minor). Remnant quartz and feldspar crystals are diffuse. Ash tuff 1-207o quartz±calcite±chlorite veinlets. Very weak foliation, weakly fractured. One 2 mm speck of chalcopyrite in 2 cm quartz vein at 97.30 m.

97.70 - 121 .50 m: Fragmental nature becomes coarser and more mafic. Diffuse quartz and uralitized mm crystals remain but become patchy (1007o overall). Generally intermediate in composition. Weak to moderate sericite alternates and varies with chlorite in matrix. Weakly foliated at 50" to core axis. 1 07o quartz±feldspar±calcite veining. Weak to moderately fractured.

SAMPLESNo.

729557295672957

72958

FROM

76.3578.0079.50

96.00

TO

78.0079.5081.50

97.50

LENGTH

1.651.502.00

1.50

ASSAYSAu ppb check

CT-02-02

DIAMOND DRILL LOG

Sheet OF

METERAGEFROM TO ROCK TYPE DESCRIPTION (colour, grain size, texture, minerals, alteration, etc.) SAMPLES

No. FROM TO LENGTHASSAYS

Au ppb check

122.90 132.00 Mafic Ash Tuff

132.00 167.80 Felsic toIntermediatePyroclastics

109.90 -112.00 m: 1 07o disseminated fine-grained euhedral pyrite.

110.45-110.65 m: Ground core.

110.65 -111.20 m: Strongly fractured, strong sericite, also quartz/chlorite/sericite filled fracture or narrow shear at 50 to core axis.

119.20 -119.80 m: Patchy 'blebs' of anhedral up to 1 07o.

120.15 -120.50 m: Strong to intense chlorite, kinked and quartz flooded; may represent a weak localized shear.

121.50 -122.90 m: Patchy, moderate to strong silica/sericite and bleaching in a fine but diffusely bedded ash tuff. Section has 2-307o very fine- to medium-grained euhedral pyrite as disseminations or along fractures - mild fabric at 55" to core axis.

121.70 -122.00 m: Has S-7% disseminated pyrite.

Dark green, fine-grained massive mafic tuff. Generally homogeneous and featureless, however, faint bedding and fine ash fragments are locally discernable. Competent and weakly fractured 1 07o <mm to 5 mm quartz, feldspar, chlorite±flourite veining. Faint bedding at 50" to core axis. Gradational contacts.

As in 8.70-67.60. Ash and lapilli tuff. Pale grey, green-grey and blue-grey. Weak foliation at 50" to core axis. Weak to moderate pervasive sericite is mostly matrix hosted or coating clasts. Local sections of siliceous or feldspathic ash clasts become diffuse. Minor chlorite appears structurally or fracture related. Some rounded clasts up to 5 or 6 cm are compositionally similar to matrix. Weak to moderately fractured. 1 07o white quartz veinlets mostly discontinuous; trace disseminated pyrite. Very local wispy ankerite (minor).

136.00 -136.80 m: Quartz flooded with 4 white quartz veins crosscutting fabric at 450 - 300 to core axis.

72959 109.90 112.00 2.10

72960 119.00 120.50 1.50

72961 135.20 137.00 1.80

CT-02-02

DIAMOND DRILL LOG

Sheet OF

METERAGEFROM

167.80

169.80

TO

169.80

210.00

ROCK TYPE

Chloritic shear

Felsic to Intermediate Pyroclastic

DESCRIPTION (colour, grain size, texture, minerals, alteration, etc.)141.50 - 147.10 m: 307o random mm scale white quartz±calcite veinlets.

146.20 m: Crenulated fabric.

149.50 - 154.30 m: Very pale blue-green-grey. Very hard aphanitic possibly weakly silicified; sericite+chlorite appears, fracture related on rims the mm - 4 cm rounded siliceous clasts. Disseminated euhedral pyrite 0.5-1 .007o throughout.

154.30 - 167.80 m: Material remains siliceous and hard, clasts are more angular and occasionally ragged, 2-307o quartz veining with very minor calcite.

Strong shear zone. Intense chlorite at 40" to 600 to core axis. 1 5-20"7o quartz-feldspar veins or laminations, often discontinuous. Up to 1"7o disseminated pyrite which can be laminated with fabric.

169.50 - 169.60 m: Clay rich gouge. Upper contact at 400 and lower contact at 500 to core axis. Fabric can be crenulated and distorted.

169.80 - 175.80 m: Very siliceous and very hard/brittle. Rhyolitic. Very fine-grained to aphanitic. Relatively homogeneous and consistent. Local very faint hints of bedding. Weak but pervasive sericite as fine flecks throughout. 307o mm quartz/feldspar veinlets, 0.5 07o chlorite/sericite veinlets. Trace 0.1 07o disseminated pyrite. Fragmental nature returns at 174.00 m.

175.80 - 177.90 m: Quartz vein-quartz flooding. Bull-white and barren upper contact, irregular, lower contact at 35" to core axis and cross-cuts foliation.

177.90 - 195.00 m: Coarse fragmental texture returns as described in 8.70 to 67.60 m. More intermediate in composition. Weak sericite is mostly confined to matrix or on selvages to clasts. Clasts are subangular. Overall quite pristine with a moderate foliation at 50". *:1 07o cm scale white quartz veins. Weakly fractured.

195.00 - 203.70 m: Rhyolitic. Mass, homogeneous, hard and brittle, local ash to lapilli sized

SAMPLESNo.

72962

729637296472965

729677296872969

72970

FROM144.50

148.50150.00151.50

167.80168.80169.80

176.80

TO146.00

150.00151.50153.00

168.80169.80171.20

177.80

LENGTH1.50

1.501.501.50

1.001.001.40

1.00

ASSAYSAu ppb check

CT-02-02

DIAMOND DRILL LOGSheet OF

METERAGEFROM

200.20

210.00

TO

201.00

ROCK TYPE

Mafic Dyke

DESCRIPTION (colour, grain size, texture, minerals, alteration, etc.)clasts. Blue-grey, quite pristine with very weak pervasive sericite. 1-207o mm scale quartz veinlets. Trace very fine disseminated pyrite. Gradational contacts.

Fine-grained, massive dark green mafic dyke. Pristine and featureless. Contacts at 550 to core axis.

203.70 - 210.00 m: Intermediate composition, rounded clasts. Sericitic matrix otherwise fairly pristine. Very weak foliation. 2-307o mm - 2 cm quartz veining, discontinuous and random, weakly foliated.

End of hole

SAMPLESNo. FROM TO LENGTH

ASSAYSAu ppb check

CT-02-02

ONTMIO MINISTRY OF NORTHERN DEVELOPMENT AND MINES

Transaction No: Recording Date: Approval Date:

Client(s):303814

Survey Type(s):

W0240.01440

2002-SEP-11

2002-NOV-26

Work Report Summary

Status: APPROVED

Work Done from: 2002-AUG-25

to: 2002-SEP-10

LANDORE RESOURCES INC.

ASSAY GEOL PDRILL

Work Report Details:

Claim*

TB

TB

TB

TB

TB

TB

TB

TB

TB

1237721

1237728

1237729

1242507

1242508

1242509

1242510

1242604

1242605

Perform

SO

SO

soS43.485

SO

SO

SO

SO

SO

543,485

External Credits:

Perform Approve

soSO

so343,485

SO

SO

SO

SO

SO

S43.485

SO

Applied

54,800

S6.000

56,000

SO

56,400

S6.400

S2.400

S4.800

52,400

539,200

Applied Approve

54,800

56,000

S6.000

SO

56,400

56,400

52,400

S4.800

S2.400

539,200

Assign

SO

SO

SO

539,200

SO

SO

SO

SO

50

S39.200

Assign Approve

0

0

0

39,200

0

0

0

0

0

539,200

Reserve

SO

SO

SO

S4.285

SO

SO

SO

50

SO

54,285

Reserve Approve

50

50

SO

54,285

SO

SO

SO

SO

SO

54,285

Due Date

2003-SEP-12

2003-SEP-12

2003-SEP-12

2003-JUL-21

2003-SEP-12

2003-SEP-12

2003-SEP-12

2003-SEP-12

2003-SEP-12

Reserve:54,285 Reserve of Work Reportt: W0240.01440

S4.285 Total Remaining

Status of claim is based on information currently on record.

52A12SW2025 2.24197 LAURIE 900

2002-Nov-28 16:04 Armstrong-d Page 1 of 1

(winistry ofNorthern Developmentand Mines

Date: 2002-NOV-26

RICHARD JAMES GARBER LANDORE RESOURCES INC. 3-1070 LITHIUM DRIVE, THUNDER BAY, ONTARIO P7B 6G3 CANADA

Ministers du Developpement du Nord et des Mines Ontario

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

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

Dear Sir or Madam

Submission Number: 2.24197 Transaction Number(s): W0240.01440

Subject: Approval of Assessment Work

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

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

If you have any question regarding this correspondence, please contact LUCILLE JEROME by email at lucille.jerome@ndm.gov.on.ea or by phone at (705) 670-5858.

Yours Sincerely,

Ron GashinskiSenior Manager, Mining Lands Section

Gc: Resident Geologist

Landore Resources Inc. (Claim Holder)

Assessment File Library

Landore Resources Inc. (Assessment Office)

Visit our website at http://www.gov.on.ca/MNDM/LANDS/mlsmnpge.htm Page: 1 Correspondence 10:17754

J* WITH* OFftDRTHClW DFVFLWNEHT

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MINING LAND TENURE

MAP

General Inform at ion and Limitations

Date r Time of Issue Jun282002

TOWNSHIP r AREA

LAURIE

11:51 h Eastern

PLAN

O-0669

ADMINISTRATIVE DISTRICTS y DIVISIONSMining Division Thunder BayLand Titles/Registry Division THUNDER Q AY

Ministry of Natural Rtiourcts District THUNDER 8AY

TOPOGRAPHIC LAND TENURE

f F*t*(*) Pitml

tjfl*n Right* O

QQ

B

LAND TEN URE WITHDRAWALS

IMPORTANT NOTICES

L AND TENURE WITHDRAWAL DESCRIPTIONS

IMPORTANT NOTICESAIIH UMlk wkkft *H*ql4l rHrf*Hn.lM

fllUng Wl MFHH^ Mvriopmwl MIMttaL

asaurca: .LMM Mn.mamr iimuu,a

\

5,380,OOON

5,379,50QN

5,379,OQON

\

\

Post #4 to claln 124E507 is 400 meters west of arrow point.

\

\

sericite V'041

\

\

040chlorite \

\ t

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\

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\ clastic netasedinents O 50 100

\ \

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\

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L14E

TRUE

E

S

LEGEND

outcrop

Sample site (all are prefixed DC)

Geological contact (inferred)

cut grid line (nost removed for clarity)

Foliation

Shear

VLF Conductor

N. Diamond Drill Hole

Py - pyrite, Qv - quartz vein

UTM coordinates - NAD 83 datum

LANDORE RESOURCES

CALTOR PROPERTYThunder Bay Mining Division

Geology and Sample Locations

N.T.S. Map Sheet: 52 B/9

Geology by D. Courtney

August 2002Digital Cartography by D. Courtney

CLARK EXPLORATION CONSULTING

Ooin cu03cu

52M2SW2Q25 2.24197 LAURIE 210

o in

o in

z o

zo in

cu

VLF Conductor Axis VLF Conductor Axis

i28U70E 5,379,610N

-50

\

-50

-100 -100

\

210,On CT-02-02

-150 -150

U) -J

MtoO

LANDORE RESOURCES LTD.

CALTOR PROPERTYThunder Bay Mining Division, Laurie Township

DRILL SECTION 7EN.T.S. Map Sheet: 53 B/9

Digital Cartography by D. Courtney

September 2002 Scale 1'500

CLARK EXPLORATION CONSULTING-200 -200

oin

rin o

-t-

cu

OE OE

VLF Conductor Axis

280.985E, 5,379,370N

-50 -50

90,0mCT-02-01

-100 -100

-150 -350

LANDORE RESOURCES LTD.

CALTOR PROPERTYThunder Boy Mining Division, Laurie Township

DRILL SECTION 4EN.T.S. Mop Sheet: 53 B/9

to w o

Digital Cartography by D, Courtney

September 2002 Scale Ii500

-aoo -200 CLARK EXPLORATION CONSULTING