Technical Report on the Harricanna Mine Project Technical Report

GM 61393 TECHNICAL REPORT ON THE HARRICANNA MINE PROJECT TECHNICAL REPORT

ON THE

HARRICANNA MINE PROJECT VAL D'OR MINING CAMP

NTS 32C/04

BOURLAMAQUE AND DUBUISSON TOWNSHIPS

QUEBEC, CANADA

REÇU AU ~Ri-i:bmP

0 d MAI 2004 FOR BUREAU GU REGESTR,6y1RE

SOCIETE MINIÈRE RIVIÈRE HARRICANA INC.

HARRICANA RIVER MINING CORPRATION INC.

Kian A. Jensen, B.Sc., P.Geo. Timmins, Ontario April 17, 2004

Reproduction of this report, in whole or in part, is not permitted without the prior written consent of K.A. Jensen.

MRNF-GÉOINFORMATION 2005 04 1 21 0 1 3 GM 61393 2

2.0 TABLE OF CONTENTS

1.0 TITLE PAGE 1 2.0 TABLE OF CONTENTS 2 2.1 LIST OF FIGURES 4 r 2.2 LIST OF TABLES 6 2.3 LIST OF APPENDICES 7 2.4 GLOSSARY OF NON-GEOLOGICAL TERMS AND ABBREVIATIONS 8 2.5 GLOSSARY OF TERMS RELATING TO MINING AND MINERAL PROPERTIES 9 2.6 CONVERSION 10 3.0 SUMMARY 11 4.0 INTRODUCTION AND TERMS OF REFERENCE 20 5.0 DISCLAIMER 22 6.0 PROPERTY DESCRIPTION AND LOCATION 23 7.0 ACCESSIBILITY, INFRASTRUCTURE, CLIMATE, LOCAL RESOURCES, AND PHYSIOGRAPHY 31 7.1 ACCESSIBILITY AND INFRASTRUCTURE 31 7.2 CLIMATE AND LOCAL RESOURCES 32 7.3 PHYSIOGRAPHY 33 8.0 HISTORY 33 8.1 VAL D'OR AREA 33 8.2 HARRICANA MINE PROJECT 35 83 HARRICAN MINE 39 _ 9.0 GEOLOGICAL SETTING 41 9.1 REGIONAL GEOLOGY 41 9.2 LOCAL GEOLOGY 43 - 9.3 PROPERTY GEOLOGY 44 9.3.1 HARRICANA MINE 46 - 9.3.2 AUR AREA `A' OPTION 50 10.0 DEPOSIT TYPES 50 10.1 QUART VEIN GOLD DEPOSITS 50 10.2 PYRITIC GOLD DEPOSITS 52 11.0 MINERALIZATION 53 12.0 EXPLORATION 61 13.0 DRILLING 63 14.0 SAMPLING METHOD AND APPROACH 73 15.0 SAMPLING PREPARATION, ANALYSES AND SECURITY 73 16.0 DATA VERIFICATION 73 17.0 ADJACENT PROPERTIES 74 17.1 FERDERBER MINE 74 17.2 SIGMA LAMAQUE MINE 75 17.3 KIENA MINE 77 17.4 NORTHERN ABITIBI MINING CORPORATION 78 3

24.0 TABLE OF CONTENTS

18.0 MINERAL PROCESSING AND METALLURGICAL TESTING 78 19.0 MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES 78 19.1 DEFINITIONS 78 19.2 DATABASE 80 19.3 GEOLOGICAL INTERPRETATION 81 19.4 ESTIMATION METHOLOGY AND PARAMETERS 81 19.5 STATISTICS 82 19.6 RESOURCE CLASSIFICATIONS 85 20.0 OTHER RELEVANT DATA AND INFORMATION 97 21.0 INTERPRETATION AND CONCLUSIONS 97 22.0 RECOMMENDATIONS AND BUDGET 99 23.0 REFERENCES 102 24.0 CERTIFICATE 105 25.0 APPENDICES 4

2.1 LIST OF FIGURES

Figure 1: Location Map of Harricana River Mining Corporation Inc. Harricana Mine Project, Bourlamaque and Dubuisson Townships, Abitibi East, Quebec, Canada. 25

Figure 2: Location Map of Harricana River Mining Corporation Inc. Harricana Mine Project, NTS 32C/04, Val d'Or Area, Quebec, Canada. 26

Figure 3: Mining Claim Map of Harricana River Mining Corporation Inc. Harricana Mine Project, Bourlamaque and Dubuisson Townships, Val d'Or Area, Quebec 27

Figure 4: Generalized Geology and Location of Quartz Vein Deposits and Massive Sulphide Polymetallic Deposits for the Malartic — Val d'Or area, Quebec 43

Figure 5: General Geology Map of the Harricana River Mining Corporation Inc. Harricana Mine Project, Bourlamaque and Dubuisson Townships, Val d'Or, Quebec 45

Figure 6: Underground Development and Known Vein Structures at the Harricana Mine, Bourlamaque Township, Val d'Or, Quebec 49

Figure 7: Surface Plan of Diamond Drill Holes and Gold Bearing Zones of Hanicana River Mining Corporation Inc., Bourlamaque and Dubuisson Townships, Val d'Or, Quebec 60

Figure 8: Hydro Zone Longitudinal with Constat Petroleum Corporation Diamond Drilling., Hanicana Mine Project, Val d'Or, Quebec 61

Figure 9: Composite Longitudinal of the Upper, CL-49, RDD and Lower Zones with Constat Petroleum Corporation and International Baslen Enterprises Limited Diamond Drilling, Hanicana Mine Project, Val d'Or, Quebec 62

Figure 10: Location Map of the 2002 Geophysical Survey Grid and 1988 Belmoral Mines Diamond Drill Grid, Aur Area A Option Mining Claims of Harricana River Mining Corporation Inc. Harricana Mine Project, Bourlamaque Township, Val d'Or, Quebec 64

Figure 11: Location Map of Diamond Drill Holes on the Aur Area A Option Mining Claims of Harricana River Mining Corporation Inc. Harricana Mine Project, Bourlamaque Township, Val d'Or, Quebec 65

Figure 12: Section 0+00, Aur Area A Option 66

Figure 13: Section 2+00 East, Aur Area A Option 67

Figure 14: Section 4+00 East, Aur Area A Option 68 5

Figure 15: Section 6+00 East, Aur Area A Option 69

Figure 16: Section 8+00 East, Aur Area A Option 70

Figure 17: Section 10+00 East, Aur Area A Option 71

Figure 18: Section 12+00 East, Aur Area A Option 72

Figure 19: Scatter Diagram of the 118 Duplicate Samples with Gold Values Greater Than 0.005 opt. 85

Figure 20: Zone Quartz Vein Vertical Polygonal Longitudinal 87

Figure 21: Zone North Shear Vertical Polygonal Longitudinal 88

Figure 22: Zone North Shear Horizontal Polygonal Longitudinal 89

Figure 23: Zone No.1 Horizontal Polygonal Longitudinal 90

Figure 24: Zone No.2 Horizontal Polygonal Longitudinal 91

Figure 25: Zone 3A Horizontal Polygonal Longitudinal 92

Figure 26: Zone 3B Horizontal Polygonal Longitudinal 93

Figure 27: Zone 4A Horizontal Polygonal Longitudinal 94

Figure 28: Zone 4B Horizontal Polygonal Longitudinal 95 6

2.2 LIST OF TABLES

Table 1: Current Mining Claim Status for Aur Resources Inc. Aur Area `A' 28

Table 2: Current Mining Claim Status for the Harricana River Mining Corporation Inc. Aur Area `B' 28

Table 3: Current Mining Claim Status for Harricana River Mining Corporation Inc.Area `C' 29

Table 4: Significant Assay Results from the 1988 and 1989 Diamond Drilling Program by Belmoral Mines Limited at the Aur Area `A' Option 55

Table 5: Significant Assay Results from the 1981 Diamond Drilling Program by Provinces X Exploration Inc. at the Harricana Shaft Area 55

Table 6: Significant Assay Results from the 1986 Diamond Drilling Program by Canstat Petroleum Corporation at the Hydro Zone and High Voltage Zone 56

Table 7: Significant Assay Results from the 1986 and 1987 Diamond Drilling Program by Canstat Petroleum Corporation at the Hydro Zone and High Voltage Zone 56

Table 8: Significant Assay Results from the 1989 Diamond Drilling Program by International Baslen Enterprises Ltd. at the High Voltage Zone 57

Table 9: Significant Assay Results from the 1988 and 1989 Diamond Drilling Program by Belmoral Mines Limited at the Aur Area `A' Option 57

Table 10: Statistics of 625 Raw Assays Greater Than 0.005 opt Gold 84

Table 11: Correlation Coefficient between the Original Assay and the Check Assay for the Gold Bearing Zones at the Aur Area `A' Option 84

Table 12: Frequency Distribution and Cumulative Frequency Distribution of Uncut Assays for Each Gold Bearing Zone at the Aur Area `A' Option 84

Table 13: Inferred Resource Estimations for the Aur Area `A' Option 96

Table 14: Proposed Exploration Budget 102 2.3 LIST OF APPENDICES

Appendix A: Harricana Amalgamated Gold Mines Inc. 1936 Diamond Drill Holes Appendix B: E & B Exploration Inc. 1981 and 1983 Diamond Drill Holes Appendix C: Province X Exploration Inc. 1981 Diamond Drill Holes Appendix D: Canstat Petroleum Corporation 1981 Diamond Drill Holes Appendix E: Canstat Petroleum Corporation 1986 Diamond Drill Holes Appendix F: Belmoral Mines Limited 1988 and 1990 Diamond Drill Holes on the Aur Area "A" Option Appendix G: International Baslen Enterprises Limited 1989 Diamond Drill Holes Appendix H: Recommended Additional Sampling of the Belmoral Diamond Drill Core Appendix I: Quartz Vein Zone — MINERAL RESOURCE Appendix J: North Shear Zone — MINERAL RESOURCE Appendix K: Zone No. l — MINERAL RESOURCE Appendix L: Zone No.2 — MINERAL RESOURCE Appendix M: Zone 3A — MINERAL RESOURCE Appendix N: Zone 3B — MINERAL RESOURCE Appendix O: Zone 4A — MINERAL RESOURCE Appendix P: Zone 4B — MINERAL RESOURCE 8

2.4 GLOSSARY OF NON-GEOLOGICAL TERMS AND ABBREVIATIONS

The following are definitions for terms used in this Technical Report:

2629-2482 Quebec Inc. the original company which was renamed on March 12, 2004 to Harricana River Mining Corporation Inc.

"Aur" or "ARL" Aur Resources Limited

"HRMC" Societe Min ère Riviere Harricana Inc. or Harricana River Mining Corporation Inc.

"IBEL" International Baslen Enterprises Limited

"JVA" Joint Venture Agreement

"KAT" K.A. Jensen, an independent consulting geoscientist

"NPIR" Net Profit Interest Royalty

"NSR" Net Smelter Return or Net Smelter Royalty

"OGS" Ontario Geological Survey

"TSE" The Toronto Stock Exchange 9

2.5 GLOSSARY OF TERMS RELATING TO MINING AND MINERAL PROPERTIES

"DDH" means a diamond drill hole

"diamond drill" paeans a machine designed to rotate under pressure, using an annular diamond studded cutting tool to produce a more or less continuous sample of the material that is drilled.

"EM" means an electromagnetic geophysical survey method

"g/t" grams per (metric) tonne

"HEM" means a horizontal loop electromagnetic geophysical survey method

"HLEM" means a horizontal loop electromagnetic geophysical survey method

"km" means kilometres

"m" means metres

means a total field magnetic geophysical survey

"mineralization" means a natural aggregate of one or more minerals, which has not been delineated to the extent that sufficient average grade or dimensions can be reasonably estimated or called a "deposit" or "ore". Further exploration or development expenditures may or may not be warranted by such an occurrence depending on the circumstances.

"NTS" National Topographic Survey that publishes topographic map sheets for Canada.

"ounce" means troy ounces

"ppb" means parts per billion

"ppm" means parts per million

means reverse circulation drilling by a machine designed to rotate under pressure, using a tricone cutting tool to penetrate unconsolidated material and to return that material with the recirculation of the drilling water.

"strike length" means the longest horizontal dimension of a body or zone of mineralization. 10

"tpd„ means tons per day or tonne per day "VEM" means a vertical electromagnetic geophysical survey method "VLF-EM" means very low frequency electromagnetic geophysical survey method "VMS" means volcanogenetic massive sulphides

2.6 CONVERSION

-- The following table sets forth certain standard conversions from the Standard Imperial units to the international System of Units (or metric units).

To Convert From To Multiply By Feet Metres 0.305 Metres Feet 3.281 Miles Kilometres 1.609 Kilometres Miles 0.621 Acres Hectares 0.405 Hectares Acres 2A71 Grams Ounces (troy) 0.032 Ounce (troy) Grams 31.103 Tonnes Short tons 1.102 Short tons Tonnes 0.907 Grams per tonne Ounces (troy) per ton 0.029 Ounces (troy) per ton Grams per tonne 34.285 11

3.0 SUMMARY

Harricana River Mining Corporation Inc. (formerly 2629-2482 Quebec Inc.) has retained K.A. Jensen (KAJ) to perform a technical review and prepare a Technical Report concerning the exploration results to date on the company's Harricana Mine Project located in Val d'Or, Quebec and to complete a resources estimation for the gold bearing zones on the Aur Area `A' Option portion of the property.

At present, the Harricana Mine Project consists of three contiguous claim blocks known as the "Aur Area A" and "Aur Area B" located in Bourlamaque Township and "Area C" located in Bourlamaque and Dubuisson Townships. The total area of the property is approximately 1,338 .4 ha (3,307.2 acres) and lies within NTS map sheets 32C/04. The property is within the city limits of Val d'Or, Quebec and extends 5.6 km to the northeast of the city center.

The coordinates of the centre of the Aur Area A property in Bourlamaque Township, are approximately 294,960mE and 5,335,460mN (UTM Zone 18, NAD 83), Aur Area B property in Bourlamaque Township, are approximately 293,350mE and 5,335,360mN (UTM Zone 18, NAD 83) and Area C in Bourlamaque and Dubuisson Townships, Quebec, are approximately 292,890mE and 5,332,835mN (UTM Zone 18, NAD 83).

Aur Resources Ltd. is the beneficial and recorded owner of a 100% undiluted interest in 9 mining claims, known as Aur Area `A'. The company, Harricana River Mining Corporation Inc., is the beneficial and recorded owner of a 100% undiluted interest in 26 mining claims, known as Aur Area `B'. The above-mentioned properties are the subject of the option agreement between Aur Resources Ltd., International Baslen Enterprises Ltd. (IBEL) and 2629-2482 Quebec Inc. dated September 24, 2001. Under the agreement International Baslen Enterprises Ltd. and 2629-2482 Quebec Inc. have the sole and exclusive right and option to acquire 100% undiluted interest in and to the Aur mining claims by completed expenditures of $50,000.00 by September 30, 2002 and $150,000.00 by September 30, 2004 on the Aur Area `A' mining claims. 12

By an instrument of Transfer dated September 25, 2001, IBEL transferred all of its rights under the Aur Agreement to 2629-2482 Quebec Inc. The company 2629-2482 Quebec Inc. changed their name on March 12, 2004 to Societé Minière Rivière Harricana Inc. or Harricana River Mining Corporation Inc. hereafter sometimes referred to as "HRMC".

Upon the completion of a Technical Report by a qualified person as defined by rational Instrument 43-101 which indicates 1,000,000 ounces of gold in the indicated and/or measured mineral resources, Aur has an option to acquire a 50% working interest and the companies shall enter into a Joint Venture Agreement (JVA). This resource can be found either in Aur Area `A' or Aur Area `B' or from the combined areas.

Aur is required to match the funds which Harricana River Mining Corporation Inc. has committed, after which time the expenditures shall be on a pro rata basis. Should either party elect not to participate and defanks twice then their interest in the TVA shall not be eligible to further participation. Should that party's interest in the JVA be reduced to 20% or less, their interest shall automatically be converted to a 20% net profit interest royalty (NPIR).

Also, the company Han icana River Mining Corporation Inc. is the beneficial .and recorded owner of a 100.3/0 undiluted interest in 47 n'i'xing claims, known as Area `C' adjacent and to the south of the two claim blocks referred to above.

The Abitibi and Pontiac sub-provinces form the southern part of the Superior Province of the Canadian Shield in Quebec.

The Abitibi Subprovince is the largest, one of the most studied and among the richest Archean greenstone belts in the world. It comprises numerous granitoid intrusions and volcanic and sedimentary belts orientated approximately east west, dating between 2750 .and 2670 Ma. Volcanics units are composed of ultramafic to mafic, mafic, or mafic to felsic assemblages. Sedimentary rocks occur along narrow bands that separate the volcanic assemblages. They are generally composed of clastic units that represent former deep-water 13

rocks), whereas smaller bands located along major faults in the southern part of the Subprovince represent shallow-water basins (Timiskaming-type rocks). The clastic units generally contain units of polymictic conglomerate and commonly contain oxide-facies banded iron formation. Plutonic rocks are subdivided into eight magmatic suites.

The Pontiac Subprovince is separated from the Abitibi Subprovince by the Cadillac-Larder Lake Break, a structure that extends from east to west for more than 100 km in Ontario and Quebec. The Pontiac Subprovince comprises granitoid intrusions and orthogneisses in its central portion, along with detrital sedimentary rocks and paragneisses with a few volcanic sequences. The volcanic sequences consists of ultramafic, mafic and locally felsic assemblages in the southwestern portion of the Pontiac Subprovince. A few thin bands of mafic to ultramafic volcanic rocks are also present in the northern portion of the Subprovince. Undeformed sedimentary rocks of the Proterozoic Colbalt Group unconformably overlie (in erosional unconformity) the southwestern Pontiac and farther north, a segment of the Cadillac- Larder Lake Break.

Metamorphism, which has affected all rock types including the late kinematic intrusions, is dominantly of the greenschist facies, with local areas of prehnite-pumpellyite and lower amphibolite facies. Regional metamorphism in the Val d'Or district occurred approximately at 2680 Ma.

The Abitibi belt also contains a few crustal-scale faults zones known as "breaks", typically 50 to 200 km in length and up to a few kilometres wide. In the Eastern Abitibi, the most important are the Cadillac (Cadillac-Larder Lake), Porcupine-Destor and the Casa-Berardi Breaks. There is a significant component of vertical elongation or thrusting took place along these fault zones during the Kenoran Orogeny. The Abitibi belt is transected by several major reverse or normal faults oriented east-west to northwest to southeast, as well as by sinistral northeast trending and dextral southeast trending faults that dissect volcano-sedimentary domains into lozenge-shape segments cored by intrusive rocks. 14

The Abitibi .Subprovince is world renowned for the great number and high grade of its precious metal (gold and silver) and polymetallic (copper-zinc-gold-silver and copper-gold) ore deposits.

The Malartic-Senneterre-Val d'Or area form the southeastern part of the Abitibi Subprovince. The Cadillac-Larder Lake Break separates the Abitibi rocks from the Pontiac Subprovince to the south. Metavolcanics of the Malartic Group dominates the area, which consists mainly of basal submarine flood basalts and komatiites overlain by calc-alkaline volcanic sequences of the Val d'Or Central Volcanic Complex. Narrow groups dominated by ultramafic and mafic, the Piche Group, and by greywacke and other metasedimentary rocks, Kewagama Group, were involved during the formation of this tectonic zone. The Cadillac Break, which is approximately east-west trending fault zone, lies 3 kilometres south of Val d'Or. The Pontiac Group located south of the Cadillac Break, consists of intercalated greywackes and conglomerates. The above Ethological units have been intruded by syn- to post tectonic and synvolcanic tonalite, granite and gabbro. Diabase dykes of Proterozoic age have cross cut all lithological units within the Val d'Or area.

Two distinct geological units dominate the property, these being the ultramafic and mafic volcanics belonging to the Jacola Formation and the granodiorite, quartz diorite and sediments in the northern half belong to the Bourlamaque Batholith and surround area.

The central portion of the property is underlain by the southern extension of the Bourlamaque Bathoiith. The granodiorite is generally coarse grained and consists of approximately 50% to 60% plagioclase, 20% to 25% quartz and 20% to 25% ferromagnesian minerals. The composition is variable and mafic xenoliths are locally abundant.

Diorite, quartz diorite, diorite porphyry, feldspar porphyry and syenite porphyry dykes have been reported to exist in Dubuisson Township. Some of these dike cross cut the 15

Bourlamaque Bath°lith. The dykes are commonly associated with gold mineralization and are an important exploration target.

Quartz vein gold deposits, the most abundant type of deposit in the Eastern Abitibi, generally consist of quartz-carbonate veins, disseminations and replacements in shear zones and to a lesser extent, veins in extensional fractures, stockwork zones and breccias. At a district scale, mafic volcanics rocks dominantly host this type of deposit. At a deposit scale, they show a marked spatial association with felsic intrusions, typically syn- to late-kinematic felsic porphyritic plugs, sills and dykes. However, they are found in all rock types including the late tectonic intrusions.

The structure of this type of deposit consists most commonly of individual or groups of parallel-mineralized shear zones. More complex networks comprising splays, conjugate sets of shear zones, combinations of shear zones and extensional fractures and three dimensional shear zone networks are also common. In addition, mineralized breccia and breccia veins are also present in a number of deposits.

Mineralized shear zones represent third-order structures, which are typically a few hundred to a few thousand metres length. Mineralized shear zones and discrete faults typically contain several lenticular ore bodies separated from one another by barren segments of shear zone. The ore bodies are commonly elongate and in many cases the long axis bears a geometric relationship to the slip direction. Shear zone hosted ore bodies consist of alteration or replacement of the rocks within and adjacent to the shear zones, or of veins - parallel or slightly oblique to the smear zone. The majority of the mineralized shear zones exhibit mixed continuous — discontinuous (brittle — ductile) behaviour. Usually these veins have been emplaced relatively late in the evolution of the shear zones and are not significantly deformed, however at the Ferderber mine these veins have been deformed and folded which indicates continued shearing after vein emplacement. 16

The Harricana Mine Property .contains at least 4 areas of gold mineralization, namely, the original Harricana Mine, north-northwest of the mine known as the Hydro Zone, north of the mine known as the High Voltage Zone and the Aur Area `A' Option zone.

The Harricana Mine was developed by a 2 compartment, 782 foot deep vertical shaft with approximately 2,179 feet of lateral drifting and cross cuts on the 100, 200, 300, 520, 640 and 760 foot levels. Currently the mine structures have been removed and a concrete cap covers the shaft.

The author has reviewed all the geophysical surveys conducted within the boundaries of the Harricana Mine project. It is the opinion of the author that all surveys have been conducted in a professional and good workmanlike manner. The interpretation of the geophysical anomalies from the VLF-EM surveys was a result of either water filled shear zones, sulphide mineralized shear zones or the composition of the overburden.

The use of geophysical survey is a primary exploration and evaluation tool. The magnetic surveys, both airborne and ground, have assisted in the identification of lithological units, and structural features such as folding and faulting. The -vertical component of the magnetic surveys, vertical gradient, will add increased knowledge and better identify structures contained within a single lithological unit.

The HLEM and IP surveys are the most effective geophysical survey to detect the gold style mineralization associated with sulphides. Generally, the gold style quartz veined mineralisation with lower percentage of sulphides has been detected more successfully with the induced polarization (IP) surveys. 17

KAJ has conducted a reviewed of the available data and prepared an Inferred Mineral Resource estimate for the Aur Area `A' Option, located north of Val d'Or, Quebec. The deposit has been interpreted as a stacked series of relatively flat to shallow dipping quartz vein gold bearing tension shear zones between two near parallel, moderately to steeply dipping quartz vein gold bearing ductile shear zones located within and in close proximity to the contact of the Bourlamaque Batholith.

The use of the Val d'Or style of gold mineralisation model is a very valuable guide for the evaluation of the property, understanding the complex relationship between stratigraphy and mineralization and for prioritization of diamond drill targets.

The database generated by the author for the Aur Area `A' Option is relatively error free and is generally suitable for use in resource estimation. KAJ notes, however, that the check sampling by Belrnoral Mines indicates that a sampling bias may exist. The effect that this possible bias would have on the resource estimate is not known and cannot be determined at this time. Further check sampling will be required to determine if this bias does, in fact, exist and what affect it might have on the Mineral Resource estimate. Following the re-sampling and check assaying, if the bias is found, the gold grades in the database should be averaged with the results of the re-sampling, and the Mineral Resource estimate should be redone.

The Inferred Mineral Resource estimate for the Aur Area `A' Option using a cut off value of 0.03 opt gold is 1,244,158 tons at an average uncut grade of 0.168 opt gold. The Inferred Mineral Resource estimate using a cut off value of 0.05 opt gold is 1,172,214 ton at an average uncut grade of 0.168 opt gold. And the Inferred Mineral Resource estimate using a cut off value of 0.075 opt gold is 991,634 tons at an average uncut grade of 0.197 opt gold. The above estimates are based on the 200 foot radius polygons.

Finally, the recommended sampling to identify extensions of the zones and the proposed infill diamond drilling will assist in the refinement of the current geological model and the extent of 18 the gold bearing mineralization which could result in a more .accurate definition of the zones and an increase confidence level of the resource estimation

KAJ has reviewed the technical information for the various geophysical, geochemical and diamond drill programs for the Harricana Mine project. In summary, the author's recommendation is that all geophysical, geochemical .and drill data for the property be reviewed, digitally compiled, and re-assessed with respect to untested exploration potential. The Aur Area `A' merits further exploration diamond drilling.

Specifically, the following work is recommended: • Geophysical data should be reviewed, compiled and interpreted with respect to the results obtained from the diamond drilling programs. • A uniform GPS system should be established to correlate the numerous diamond drilling campaigns, survey grids and geophysical .anomalies. • Prior to the commencement of the following fieldwork, the grid should be brushed out and re-chained and replace any missing pickets. All pickets should be labelled with metal tags. The baseline, tie lines and the ends of the grids lines should have GPS coordinates. • It is recommended that the remainder of Area B, specifically Lac Blouin establish a grid and surveyed by total field magnetic and gradient magnetic surveys. • Zones of interest should be surveyed with IP prior to future diamond drilling. It is recommended that the IP survey parameters be with spacing of a= 50 metres with readings N=1 to N=6 in a pole-dipole configuration. A drill hole to surface Mise a la Masse IP survey may be beneficial in tracing individual mineralized shear zones to assist in the correlation of the various zones on the Aur Area `A' claims. • It is recommended that the 1988 and 1990 diamond drill core be checked for additional technical information and sampling of drill core along strike and down dip projections of known gold bearing mineralization zones. It is estimated at a total of 4,624 feet of additional sampling is recommended. • At least 10% to 15% of the existing split core should be %4 split for check assaying. 19

Additional recommendations are as follows: KA.J recommends that the quality control (QC) and quality assurance (QA) for assaying the diamond drill core be put in place prior to the above recommended sampling and diamond drill program All pulps and rejects should be returned to the company for secure storage and future uses such as metallurgical testing and bulk density testing; and KAJ recommends that the proposed and future diamond drill programs be completed with NQ diamond drill core size. Also, it is recommended that the drill core be cut by a diamond saw rather than with a hydraulic or hand sputter.

A three-phase program involving re-sampling the existing diamond drill core, in-filling diamond drilling and exploration geophysical surveys with follow-up diamond drilling is recommended with Phase 1 having a cost of $100,092, Phase 2 having a cost of $296,717 and Phase 3 having a cost of $239,076.

Dated at Timmins, Ontario, this 17`h day of April, 2004.

Kian A. Jensen, B.Sc., P.Geo. 20

4.0 INTRODUCTION AND TERMS OF REFERENCE

Mr. Robert N. Granger of Societe' Minière Rivière Harricana Inc. or Harricana River Mining Corporation Inc. (formerly 2629-2482 Quebec Inc.) has retained K.A. Jensen (KAJ) to complete a technical review and prepare a Technical Report for qualifying purposes concerning the exploration activities and results on the Harricana Project, located in Bourlamaque and Dubuisson Townships, Quebec, Canada.. The property is located within the city limits of Val d'Or, Quebec and extends 5.6 km to the northeast of the city center.

KAJ's objective is to prepare an independent exploration summary Technical Report on the Harricana Mine Project, in compliance with National Instrument 43-101 (NI 43-101) and the CIM Standards.

The scope of the technical review includes the recommendation of further exploration work, if deemed warranted by KAJ, along with a budget estimate.

The objective of Harricana River Mining Corporation Inc. exploration program is the development of a Ferderber style Archean deposit hosting auriferous quartz veins (lobe gold deposits) and disseminated gold rich sulphides along strike. Current experience in the Val d'Or gold camp directs HRMC to the use of proven geophysical techniques such as Max Min II horizontal loop electromagnetic (HLEM), ground total field and vertical gradient magnetic, and Induced Polarization (IP) surveys and geophysical and geochemicai modeling to select drill targets.

Full and cooperative discussions were held with Mr. Bill Jackson, President of Harricana River Mining Corporation Inc.; Mr. Lan Vu, M.Sc.A., APGGQ, former chief geologist for Belmoral Mines Ltd. from 1981 to 1992; Dr. John L. Kirwin, Exploration Manager for HRMC; and Mr. Philippe Cloutier of Aur Resources Limited during the preparation of this report. Mr. Kian A. Jensen, B.Sc., P.Geo., is the Qualified Person (QP) with respect to this technical report and is independent to Harricana River Mining Corporation Inc. 21

The majority of the data used in the preparation and contained ui this report has been derived from technical maps, drill sections, compilation maps and reports prepared for mining and exploration companies and by their representatives. The author also relies on over 25 years of experience in the exploration and mining industries.

KAJ have researched and reviewed geotechnical information filed for assessment work with the Resident Geologist's office, Val d'Or, Quebec on the Harricana Mine Project and the surrounding area. KAJ also studied several recent government reports on the Val d'Or area and the gold mineralization.

The companion policy 43-101CP to NI 43-101, Standards of Disclosure for Mineral Projects requires under Section 6, a personal inspection of the property by the author (or at least one author if several have contributed) of a Technical Report. The author conducted a property inspection on August 28, 2003 and re-examined the diamond drill core on November 7, 2003.

The 1988 and 1990 diamond drill core is stored at the core storage site of Aur Resources Limited property south of the Peter Ferderber mine northeast of Val d'Or.

The 1989 diamond drill core of International Baslen Enterprises Limited was stored at the Hunter Mine property in Porcupine, Ontario, and was later destroyed at no fault of IBEL.

The grid lines require re-cutting with new pickets as many areas has significant re-growth of vegetation. 22

5.0 DISCLAIMER

• KA.1 has relied on the property descriptions in Section 6.0 and on the available data., published and unpublished reports and maps, which have been prepared by or for the company.

• ICU has not checked title to the mining claims with the Mining Recorder in Val D'Or, Quebec and hereby disclaim all responsibility for such matters. The mining claims listed in Tables 1, 2 and 3 were obtained from the Quebec Government's web site as of November 14, 2003.

• ICU is unaware of any technical data other than presented by company or researched at the Resident Geologist office in Val d'Or, Quebec. 23

6.0 PROPERTY DESCRIPTION AND LOCATION

The Harricana Mine Project consists of three contiguous claim blocks known as the "Aur Area A" and "Aur Area B" located in Bourlamaque Township, and "Area C" located in Bourlamaque and Dubuisson Townships. The total area of the property is approximately 1,338.4 ha (3,307.2 acres) consisting of 82 mining claims, which lies within NTS map sheets 32C/04 as illustrated, in Figures 1 and Figure 2. The property is within the city limits of Val d'Or, Quebec and extends 5.6 km to the northeast of the city center.

The coordinates of the centre of the Aur Area A property in Bourlamaque Township, are approximately 294,960mE and 5,335,460mN (UTM Zone 18, NAD 83) consisting of 9 mining claims with an area of 170.258 ha (420.708 acres), Area B property in Bourlamaque Township, are approximately 293,350mE and 5,335,360mN (UTM Zone 18, NAD 83) consisting of 26 mining claims with an area of 341.166 ha (843.020 acres), and Area C in Bourlamaque and Dubuisson Townships, Quebec, are approximately 292,890mE and 5,332,835mN (UTM Zone 18, NAD 83) consisting of 47 mining claims with an area of 827.007 ha (2,043.534 acres) as illustrated in Figure 3.

Aur Resources Ltd. is the beneficial and recorded owner of a 100% undiluted interest in 9 mining claims, known as Aur Area `A', as listed in Table 1. The company, Harricana River Mining Corporation Inc., is the beneficial and recorded owner of a 100% undiluted interest in 26 mining claims, known as Aur Area `B', as listed in Table 2. The above-mentioned properties are the subject of the option agreement between Aur Resources Ltd., International Baslen Enterprises Ltd. (IBEL) and 2629-2482 Quebec Inc. dated September 24, 2001. Under the agreement International Baslen Enterprises Ltd. and 2629-2482 Quebec Inc, have the sole and exclusive right and option to acquire 100% undiluted interest in and to the Aur mining claims by completed expenditures of $50,000.00 by September 30, 2002 and $150,000.00 by September 30, 2004 on the Aur Area `A' mining claims.

By an instrument of Transfer dated September 25, 2001, IBEL transferred all of its rights under the Aur Agreement to 2629-2482 Quebec Inc. The company, 2629-2482 Quebec Inc. 24

changed their name on March 12, 2004 to Societé Minière Rivière Harricana Inc. or Harricana River Mining Corporation Inc. hereafter sometimes referred to as "HRMC

Upon the completion of a Technical Report by a qualified person as defined by National Instrument 43-101 which indicates 1,000,000 ounces of gold in the indicated and/or measured mineral resources, Aur has an option to acquire a 50% working interest and the companies shall enter into a Joint Venture Agreement (JVA). This resource can be found either in Aur Area `A' or Aur Area `B' or from the combined areas.

Aur is required to match the funds which Harricana River Mining Corporation Inc. has committed, after which time the expenditures shall be on a pro rata basis. Should either party elect not to participate and defaults twice then their interest in the JVA shall not be eligible to further participation. Should that party's interest in the JVA be reduced to 20% or less, their interest shall automatically be converted to a 20% net profit interest royalty (NPIR).

Also, the company Harricana River Mining Corporation Inc. is the beneficial and recorded owner of a 100% undiluted interest in 47 mining claims, known as Area `C', as listed in Table 3. Area `C' is adjacent to and south of the two claim blocks referred to above.

All of the mining claim units are active without being leased from the provincial government. Neither the property boundary nor any of the mining claim units have been legally surveyed. The north property boundary is the legal surveyed Bourlamaque and Dubuisson Township line and the boundary between Aur Area `A' and Aur Area `B' is also the north — south legal surveyed township line. 25 ~ Baffin

jivik Salluit

Hudson Bay Akulivik Quagtaq

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100 0 100 200 300

Figure 1: Location Map of Harricana River Mining Corporation Inc. Harricana Mine Project, Bourlamaque and Dubuisson Townships, Abitibi East, Quebec, Canada. PROVINCE OF ONTARIO PROVINCE OF QUEBEC

• VILLEBOIS

• LA SARRE

• IROQUOIS FALLS

4 3)- DUPARQUET MATHESON

ROUYN-NORANDA KIRKLAND LAK

SCALE IN KILOMETRES 0 20 40 60 80 100

TO MONTREAL TO TORONTO Figure 2: Location Map of Harricana River Mining Corporation Inc. Harricana Mine Project, NTS 32C/04, Val d'Or Area, Quebec.

-) 7

1 É C 1 k ~ k 1 1

owpwwwww- ~ i1MO/ANAY777 ,3127111111944 _ s 347 909 mN

CANTON OE VASSNI V7sSAN TOWNSHIP C.AN1O11 DE 3E,, SEN1EVIlETaîr. A22922 • 3E 7tE HI71 . . . CANTON OE Dt1Stl155ON . B135 0•0 Imer OUSUSSONTOWNSHIP 3424143 1424144 312442 4,0~ ~ ~ -ANTON DE SOUISAMAOUE 1611923 ^ ~3.9134.- 3449321 9OUPLAM.5OUE TOWNSHIP I

AUR RESOURCES 3494142 3494151 1649221 144 38129]4 AUR RESOURCES AREA El OPTION 5275401 AREA A OPTION 3.9115~~ p 5202ri4 ~H' 1236551 I ]638555 `~w. .194141 I 5 333 000 ..N 5 ]]5 000 mN 24161 3424153 _.______. __—_-. 3549224 ~~ I 48. Or E 3638317 34345N 1534545 3815111 1.9225 i , } 449214 } 1A12115 3635314 lA1,J,J ]549191 I 3449201 SULLIVAN MINES 14497 334 000 r031 ~ . 5 33‘ 000 niN 7674278 _?1011]2! :- .... . 3649192 ]449202 -----= -- -13e38323 ]S35321 1434]21 3614331 ' I '36M737 ~ . Î • / J549t4t 32491î1 1549191 ]549201 r 1549154

3641,12 ~ 5 333 000 n. 5 333 000 RIM 1.9114~ 4 3.5144 3.9142 Industrial Park I_ 1649tî1 C

'7949144 L. 3.9121

Industrial Park

312 000 m14 5 353 oE A4N

HIGHWAY 117 4f 0.11P

• 3a7 11611 m71

RgINPAY 717

VAL D'OR 5 3300E 01 5 330 000 mN

P L G 1 i 9 ~ ! = g >3 CY k 5 322 0904W ~ F. AIN LL Z _., IN METRES C7 4 KIAN A. JEN N ~ 1000 500 0 1000 PRACTISING MEMBER • 0558

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Figure 3: Mining Claim Map of Harricana River Mining Corporation Inc. Harricana Mine Project, Bourlamaque and Dubuisson Townships, NTS 32C/04, Val d'Or Area, Quebec. 28

`fable 1: Current Mining Claim Status for the Aur Resources Inc. Aur Area `A'

AUR RESOURCES OPTION "AUR AREA A" - BOURLANIAQUE TOWNSHIP Claim Range Lot Ownership Date of Expiry Status Area (ha) Number Registration Date 3494141 39 6 100% 11/26/74 11/7/04 Active 16 Aur Area A 3494142 41 6 100% 11/26/74 11/7/04 Active 16 Aur Area A 3494143 42 6 100% 11/26/74 11/7/04 Active 16 Aur Area A 3494144 42 7 100% 11/26/74 11!7/04 Active 16 Aur Area A 3494145 42 8 100% 11/26/74 11/7/04 Active 16 Aur Area A 3494151 40 8 100% 11/26/74 11/8/04 Active 16 Aur Area A 3494152 40 7 100% 11/26/74 11/8/04 Active 16 Aur Area A 3494153 41 7 100% 11/26/74 11/8/04 Active 16 Aur Area A 3494154 41 8 100% 11/26/74 11/8/04 Active 16 Aur Area A

Table 2: Current Mining Claim Status for the Harricana River Mining Corporation Inc. Aur Area `B'

HARRICANA RIVER MINING CORPRATION INC. "AUR AREA B" - BOURLAMAQUE TOWNSHIP Claim Range Lot Ownership Date of Expiry Status Area (ha) Number Registration Date 3822972 42 1 100% 4/27/79 4/5/05 Active 6.79 Aur Area B 3822973 41 1 100% 4/27179 4/5/05 Active 16.37 Aur Area B 3822974 40 1 100% 4/27/79 4/5/05 Active 17.47 Aur Area B 3822975 41 2 100% 4/27/79 4/5/05 Active 12.29 Aur Area B 3838311 39 3 100% 11/29/79 11/7/04 Active 20.11 Aur Area B 3838312 39 4 100% 11/29/79 11/7/04 Active 9.56 Aur Area B 3838551 42 4 100% 11/29/79 11/10/04 Active 14.01 Aur Area B 3838552 42 3 100% 11/29/79 11/10/04 Active 18.64 Aur Area B 3838553 41 3 100% 11/29/79 11/10/04 Active 9.44 Aur Area B 3838554 41 4 100% 11/29/79 11/10/04 Active 10.19 Aur Area B 3838555 40 4 100% 11/29/79 11/10/44 Active 13.95 Aur Area B 3838581 40 3 100% 11/29/79 11/10/04 Active 17.27 Aur Area B 3838582 39 2 100% 11/29/79 11/10/04 Active 12.88 Aur Area B 3838583 39 1 100% 11/29/79 11/10/04 Active 8.42 Aur Area B 3838584 38 1 100% 11/29/79 11/10/04 Active 19.00 Aur Area B 3838585 38 2 100% 11/29/79 11/10/04 Active 16.67 Aur Area B 3849134 000A 9 100% 3/17/80 2/23/05 Active 4.91 Aur Area B 3849135 000A 8 100% 3/17/80 2123/05 Active 23.31 Aur Area B 3849221 42 5 100% 11/29/79 11/10/04 Active 10.74 Aur Area B 3849222 40 5 100% 11/29/79 11/10/04 Active 6.85 Aur Area B 3849223 41 5 100% 11/29/79 11/10/04 Active 18.61 Aur Area B 3849224 40 6 100% 11129/79 11/10/04 Active 18.94 Aur Area B 3849225 39 5 100% 11/29/79 11/10/04 Active 14.40 Aur Area B 5177698 42 2 100% 8/19/98 8/18/04 Active 9.52 Aur Area B 5225401 40 2 100% 6/22/98 6/21/04 Active 2.71 Aur Area B 5225402 41 10 100% 6122/98 6/21/04 Active 6.13 Aur Area B 29

Table 3: Current Hiding Claim Status for Harricana River Mining Corporation Inc. Area C

HARRICANA RIVER MINING CORPRATION INC. AREA `C' - BOURLAMAOUE TOWNSHIP Claim Range Lot Ownership Date of Expiry Status Area (ha) Number Registration Date 3838313 38 3 100% 11/29/79 11/7/04 Active 18.33 Aur Area C 3838314 37 2 100% 11/29/79 1117104 Active 14.02 Aur Area C 3838315 37 1 100% 11/29/79 11/7104 Active 17.47 Aur Area C 3838321 37 4 100% 11/29/79 1114/04 Active 17.66 Aur Area C 3838322 37 3 100% 11/29/79 1114/04 Active 13.54 Aur Area C 3838323 36 1 100% 11/29/79 11/4104 Active 13.01 Aur Area C 3849094 33 2 100°l0 1/7/80 12/17/04 Active 6.25 Aur Area C 3849111 36 3 100% 1/23/80 1/22/05 Active 19.74 Aur Area C 3849112 35 3 100% 1/23/80 1/22/05 Active 17.00 Aur Area C 3849113 34 3 100°!0 1/23/80 1/22/05 Active 17.74 Aur Area C 3849114 35 4 100% 1/23/80 1/22105 Active 11.93 Aur Area C 3849115 33 5 100% 1123/80 1/22/05 Active 3.96 Aur Area C 3849121 34 4 100% 1/23180 1/22/05 Active 13.31 Aur Area C 3849141 36 2 100% 1/7/80 12/17/04 Active 15.05 Aur Area C 3849142 35 2 100°l0 1 /7/80 12/17/04 Active 14.80 Aur Area C 3849143 34 2 100% 1/7/80 12/17/04 Active 15.80 Aur Area C 3849144 33 1 100°10 1/7/80 12/17104 Active 17.91 Aur Area C 3849145 34 1 100% 1/7/80 12/17104 Active 16.07 Aur Area C 3849173 32 1 100% 11/29/79 11/9/04 Active 16.55 Aur Area C 3849174 31 1 100% 11/29/79 1119/04 Active 26.28 Aur Area C 3849175 29 1 100% 11129/79 11/9/04 Active 12.76 Aur Area C 3849184 35 1 100°10 1/7/80 1119/04 Active 18.72 Aur Area C 3849185 32 2 100% 11/29/79 11/9/04 Active 15_$2 Aur Area C 3849191 38 4 100% 11/29f79 11/5/04 Active 14.74 Aur Area C 3849192 37 5 100% 11/29/79 11/5/04 Active 15.07 Aur Area C 3849193 36 4 100% 11/29/79 11/5104 Active 15.22 Aur Area C 3849201 38 5 100% 11/29/79 11/4/04 Active 11.11 Aur Area C 3849202 37 6 100% 11/29/79 1114/04 Active 11.23 Aur Area C 3849203 36 5 100% 11/29/79 1114/04 Active 14.16 Aur Area C 3849204 35 5 100°l0 11/29/79 11/4/04 Active 12.73 Aur Area C 3849205 34 5 100% 11/29/79 11/4/04 Active 12.02 Aur Area C 3849211 38 6 100% 11/29/79 11112/04 Active 11.02 Aur Area C 3849212 38 7 100% 11/29/79 11/12/04 Active 12.48 Aur Area C 3849213 37 8 100°10 11/29/79 11/12/04 Active 14.86 Aur Area C 3849214 37 7 100% 11/29/79 11/12/04 Active 11.99 Aur Area C 3849215 36 6 100°10 11/29/79 11112/04 Active 14.45 Aur Area C 30

Table 3: continued

HARRICANA RIVER MINING CORPRATION INC. AREA `C' - DUBUISSON TOWNSHIP Range Lot Ownership Date of Expiry Status Area (ha) Registration Date 3838324 36 41 100% 11/29/79 11/4/04 Active 10.86 Aur Area C 3838325 36 40 100% 11129179 11/4/04 Active 14.7 Aur Area C 3838331 35 40 100% 11/29/79 11/7/04 Active 18.02 Aur Area C 3838332 35 41 100% 11/29779 11/7/04 Active 17.84 Aur Area C 3838333 8 58 100% 11/29/79 11/7/04 Active 42.61 Aur Area C 3838334 8 57 100% 11/29/79 11/7/04 Active 42.5 Aur Area C 3849151 8 60 100% 11/29/79 11/9/04 Active 42.61 Aur Area C 3849152 8 59 100% 11/29/79 11/9/04 Active 42.61 Aur Area C 3849161 8 62 100% 11/29/79 11/9/04 Active 27.96 Aur Area C 3849162 8 61 100% 11/29/79 11/9/04 Active 42.61 Aur Area C 5012347 8 71 100% 2127/89 2/26/05 *Active 1.44 Aur Area C 5012347 8 72 100% 2/27/89 2/26/05 *Active 2.04 Aur Area C 5012347 8 73 100% 2/27/89 2/26/05 *Active 1.19 Aur Area C 5012347 8 74 100% 2/27189 2/26/05 *Active 1.08 Aur Area C 5012347 8 75 100%) 2/27/89 2/26/05 *Active 0.29 Aur Area C 5012347 8 78 100% 2/27/89 2/26/05 *Active 0.56 Aur Area C 5012347 8 76 100% 2/27/89 2/26105 *Active 0.09 Aur Area C 5012347 8 77 100% 2/27189 2/26/05 *Active 0.6 Aur Area C 5012347 8 77 100% 2/27/89 2/26/05 *Active 0.07 Aur Area C 5012347 8 78 100% 2127/89 2/26/05 *Active 0.17 Aur Area C 5012347 8 79 100% 2/27/89 2/26105 *Active 0.32 Aur Area C 5012347 8 80 100% 2127189 2/26/05 *Active 0.81 Aur Area C 5012347 8 81 100% 2/27/89 2/26/05 *Active 0.14 Aur Area C 5012347 8 82 100% 2/27/89 2/26/05 *Active 0.13 Aur Area C 5012347 8 83 100% 2/27/89 2/26/05 *Active 0.32 Aur Area C 5012347 8 84 100% 2/27/89 2/26/05 *Active 0.39 Aur Area C 5012347 8 85 100% 2/27189 2/26/05 *Active 0.82 Aur Area C

Note: * This claim has been found on more than one surface

7.0 ACCESSIBILITY, INFRASTRUCTURE, CLIMATE, LOCAL RESOURCES, AND PHYSIOGRAPHY

7.1 ACCESSIBILITY AND INFRASTRUCTURE

Val d'Or is approximately 108.8 km (67.56 miles) east ofNoranda along Highway 117. Val d'Or is located at the junction of Highways117 and 397.

The southern portion of the property is located within the city limits of Val d'Or and a municipal industrial park and cottage area around Lac Blouin occupies the remainder.

Access to the property is extremely good, with roads and city streets crisscrossing the majority of the area. The northern portion and the Aur Area A is accessed via Highway 397 approximately 5.96 km (3.62 niiles) north and northeast of the city center and then westwards along Chemin Val Des Bois for approximately 1.65 km (1.02 miles) to the cut east-west property baseline. The western portion of the project area can be accessed by country roads either by Sentier Des Fougeres near and along the west shore of Lac Blouin or by a more northerly route eastwards along Chemin Harricana. The road access to and around the property is illustrated in Figure 3. Access along the shoreline of Lac Blouin can be obtained by boat from spring to fall and by snowmobile during the winter.

The only mining infrastructure located on the property is a capped mine shaft known locally as the Harricana Mine which gives access to one of the gold mineralization zones. Additional access may also be available from underground workings from the adjacent Stabell and Jacola mines to the west of the property.

The Canadian National Railway provides railway services in the region. Electric energy is relatively inexpensive and is supplied by Hydro-Quebec. The main railroad and a Hydro Quebec high voltage transmission line also crosses the property in an east-west direction.

Val d'Or is a major mining centre, which can provide all the specialized and technical support and services, a highly skilled labor force, mining equipment, supplies and contractors and 32 adequate infrastructures to the mining industry. Additional exploration personnel can be provided from Malartic, Cadillac, Amos and Rouyn-Noranda, Quebec and Kirkland Lake, Ontario.

7.2 CLIMATE AND LOCAL RESOURCES

The climate is temperate with four distinct seasons, typical of the Southern Shield, and moderated by the proximity of the Great Lakes to some extent and by James Bay. Other than Lac Blouin, exploration activities can be completed year around with preference in the winter months. Water for diamond drilling on the Harricana Mine project can be obtained from a small kettle lake near Aur Area A or from Lac Blouin.

The average temperature during the winter range from 0°C to 23°C with extreme lows of — 43°C recorded in January. The average temperature during the months of summer range from 6 °C to 23 °C with extreme highs in the 30°C+ recorded from May to September. Average rainfall is 630 mm with the largest amount of rainfall recorded from June to September. The average snowfall is 317.6 mm with the maximum amount recorded November to February. The average number of sunshine days per year is approximately 1903 hours.

The property lies within the Boreal Forest Region and is subdivided into two subsections, the Northern Clay and the Hudson Bay Lowlands. The Northern Clay Subsection has large stretches of black spruce, which cover the gently rising ground as well as the lowland flats, where the trees alternate with extensive sedge and sphagnum moss swamps. Better-drained areas contain mixed stands of white birch, poplar and white .and black spruce. Stands of jack pine are found on outwash deposits, old beaches and eskers. The vegetation is a mixture of second-generation coniferous and deciduous forest.

A wide esker on the eastern portion of the property is a source for sand and gravel. Numerous gravel pits are located along the length of the esker. 33

7.3 PHYSIOGRAPHY

The area is generally flat with minor hills associated with the glacial drumlins and an esker located on the eastern property boundary. The lowest portion of the property is Lac Blouin located in the northwestern portion of the property. The highest portion near the property is located to the east at the Sigma Mine. A minor amount of outcrop exists along the shoreline of Lac Blouin.

The first glacial advance of the Wisconsinan ice over the area was in a southeast direction that deposited a sandy till. After the retreat of the ice about 8400 years BP, Lake Barlow- Ojibway was formed and deposits of varved clays, silt and fine sand were formed. These glaciolacustrine deposits are only exposed south of the project area approximately. The project area and northwards these same glaciolacustrine deposits are covered by the Cochrane till. About 8100 years BP, the second phase of the Cochrane lobe re-advancement covered the area, which modified and capped the eskers and the Lake Barlow-Ojibway lacustrine deposits with a clayey till and molded drumlinoid landforms with southeast orientation.

8.0 HISTORY

8.1 VAL D'OR AREA

The Val d'Or — Malartic region represents a major gold producing area within the Abitibi Subprovince in Quebec. According to Desrochers et. al. (1996) the area has produced approximately 450 tonnes of gold from 27 producing mines. Forty four major discoveries of either gold or polymetallic deposits have been made in the region from 1911 to 1985 with the majority of the early discoveries made by prospecting while since 1945 geophysical surveying has accounted for approximately 34% of the total discoveries (Lulin, J.M., 1990).

The Val d'Or and surrounding area have been subject to previous geological surveys and reports as early as 1927 by Bain, G.W. on the Geology and Mineral Deposits of the Harricana and Bell River Basins (C1MM Bull 178, p 201-247), to detail reports on the 34 various deposits and mines in the area from 1931 to 1936 by L.V. Bell, and from 1941 to 1943 by G.W.H. Norman, to the more recent report in 1996 by J.P. Desrochers, C. Hubert and P. Pilote.

The Val d'Or area has seen many significant gold discoveries and mine development over the years. The first gold discovery in the Malartic — Val d'Or region was in 1911 by J.J. Sullivan and Hertel Authier that resulted in the mining operations at the Sullivan Mine in 1928. Gold bearing veins were discovered on Siscoe Island in 1913. The Siscoe Mine was developed by a shaft sunk in 1926 with milling operations starting in 1929 at the rate of 100 tons per day. Historically the Siscoe Mine is ranked as the fourth largest gold mine of the Val d'Or district, that produced 3,280,186 tons of ore at 9.22 g/t (0.269 opt) gold and 3.2 g/t (0.93 opt) silver from1929 to 1949.

Heber Bambr ck discovered the Sigma Mime in 1933 with mining and milling commencing in 1937. The Lamaque Mine commenced production in April 1935. The polymetallic ore body of Manitou Barvue Mines Limited was discovered in 1923 with commercial production commencing in 1942.

Peter Ferderber discovered gold mineralization in 1975 within the Bourlamaque Batholith, which lead to mine development in later 1978 at the Belmoral Mine.

The Val d'Or area was one of the first mining camps to be surveyed by a regional airborne magnetic survey in 1948 by the Geological Survey of Canada (Senneterre Map 7083D, scale 1:250,000). In 1969 and 1970, Questor Surveys completed an airborne magnetic and electromagnetic survey of the area for the Quebec Ministry of Energy and Resources. During 1980, The Geological Survey of Canada resurveyed NTS Sheet 32C/04 using an experimental high-resolution airborne magnetic gradiometer. 35

8.2 HARRICANA MINE PROJECT

Harricana Gold Mines Limited discovered geld in 1920 as a result of the intense exploration that followed the gold discovery nearby by at the Sullivan Mine in 1912.

During 1920, Kienawasik Gold Mining Company held lots 59 and 60, range VIII, Dubuisson Township (Denis, T.C. 1921).

In 1927, additional claims were obtained by the amalgamation with Kienawisdc Gold Mining Company Limited to form the Harricana Amalgamated Gold Mines Incorporation.

Harricana Amalgamated Gold Mines Inc. held mining concessions east of the Greene-Stabell property that included lots 59, 60, 61 and 62, range VIII, Dubuisson Township and blocks 13 and 14 in Bourlamaque Township (Hawley, J.E. 1931).

In 1934, Harricana Amalgamated Gold Mines Inc. held lots 59, 60, 61 and 62, and the north half of lots 57 and 58, Dubuisson Township and blocks 13 and 14 in Bourlamaque Township (Bell, L.V. 1934).

Ross, S.H., et. al. (1938) indicates that the property of Harricana Amalgamated Gold Mines Inc. consisted of mining concessions 139, 158, 143 and 190 in Dubuisson Township and blocks 13 and 14 in Bourlamaque Township.

The following description refers to the current project area (Assessment file GM 00052 and 01079A-B):

In 1934, some mineralization was discovered near the current location of the Harricana shaft. Trenching in 1935 resulted in the delineation of Vein Number 13. Reported sampling averages yielded an average grade of 0.257 opt gold over an average width of 42 inches for a strike length of 150 feet (Assessment file GM 08149 36

and 31842). Harricana Amalgamated Geld Mines Incorporation conducted exploration activities until 1939.

The property was optioned in 1936 by Mining Corporation of Canada (Noranda) and became associated with International Mining Corporation and Gold Fields American Development Company. In the same year, approximately 10,965 feet of diamond drilling in 20 drill holes was completed which resulted in the determination of the down dip extension.

In 1937, Harricana Amalgamated Gold Mines Incorporation completed 10 diamond drill holes. Hole 9 intersected a 4-foot wide quartz tourmaline vein and hole 22 intersected a quartz vein between 2 porphyry dykes just north of Vein 13. The company changed their name to Harricana Gold Mines Incorporated in 1939 (Assessment file GM 06816A-B, 06889, 10653 and 10654).

The available coordinates for the above diamond drill holes completed by Harricana Amalgamated Gold Mines Incorporation are summarized in Appendix A.

The property was inactive during the Second World War. In 1945 a magnetic survey was completed on the property, which was followed by approximately 20,000 feet of diamond drilling in 38 drill holes to test targets identified from the magnetic survey. During 1946, 6 surface diamond drill holes (B1 to B6) totalling approximately 4870 feet were completed in the southwest part of Lot 59, Dubuisson Township and the last 1,500 foot drill hole was completed in the northern part of Lot 60. The coordinates, drill logs and assays are not available for drill holes completed in 1945 and 1946.

In 1960 the company was renamed to New Harricana Mines. 37

Over the following years, the property has been subjected to several exploration activities by Sullivan Consolidated Mines Limited completed a property report in 1939 and 2 diamond drill holes in 1941(Assessment files GM 06976A and B), Blouin Lake Mines Limited completed a geological plan with locating diamond drill holes in 1937 and a property examination report in 1939 (Assessment files GM 06816A and B), Lamaque Mining Company Limited conducted a property examination and assaying in 1942 completed 2 drill holes in 1962 followed by a single drill hole and reconnaissance geological survey in 1963 and a one drill hole in 1966, and reconnaissance geological survey and a diamond drill hole during 1963 and 1966 (Assessment files GM 06913, 06914, 12501, 13405, 13406 and 19161), Mid-North Engineering completed 2 diamond drill holes in 1963 (Assessment file GM 13005) and Leitch Gold Mines Limited completed a diamond drill hole in 1963 (Assessment file GM 12973).

The corporate charter of New Harricana Mines Limited was annulled and the claims reverted to the crown in 1974 (Assessment file GM 30041).

In 1979, F.N. Charlebois staked the entire property, which is close to the current mining claim status, and commenced exploration activities (Assessment file GM 37156).

In 1981 and 1982, Provinces X Exploration Inc. and E & B Explorations Inc. completed several geophysical surveys followed by 3 short diamond drill holes. Bourlamaque Assay Laboratories Ltd completed the assaying. The available coordinates for the diamond drill holes completed by E & B Explorations Inc. are summarized in Appendix B and the coordinates for Provinces X Exploration Inc. drill holes are located in Appendix C. In 1981, VLF-EM surveys were completed with approximately 42 km using Cutler, Maine and 43 km using Annapolis, Maryland as transmission stations and 37 km of magnetic survey. During 1982, Laduboro Enterprises Limited acquired 42% of Provinces X and by several mergers obtained control of the property. The company was renamed Laduboro Limited in 1987. 38

Canstat Petroleum Corporation had an option on the property and completed 91 diamond drill holes totalling 24,077.82 metres (15 holes in the CB series in 1986 and 76 holes in the CL series during 1986 and 1987) which resulted in the discovery of several gold bearing mineralization zones as well as a gold and copper mineralization in the northeast portion of the property (Assessment files GM 36588, 36672, 37302, 38034, 39962, 40632, 43932 and 44971). The location coordinates for the CB and CL series of the diamond drill holes are summarized in Appendix C and D respectively.

On February 27, 1987 and after extensive diamond drilling, Canstat Petroleum Corporation completed a resource calculation for the Hydro Vein. The calculation was completed by a polygonal method on a vertical longitudinal plane accounting for the dip of the zone and using a density factor of 3.1278. Their preliminary calculations yielded a resource of 23,897 tonnes with an averaged uncut grade of 3.79 g/t. This estimate has not been recalculated by the writer and is considered as "exploration information" only and not a "resource" in the terms required by NI 43 101.

Northern Abitibi Mining Corporation held the mining claims adjacent to the northern boundary of the current property in Senneville Township. Northern Abitibi Mining Corporation and Golden Rule Resources completed a ground magnetic survey of their property adjacent to the north boundary in 1978 (Assessment file GM 34250). It has been reported their diamond drilling program intersected several gold bearing mineralization zones near their southern boundary.

In November 1975, Belmoral Mines Limited contracted Prospecting Geophysics Limited to complete a total field magnetic survey of their property, which included a portion of the current project area. The grid lines were 600 feet apart with reading intervals at 100 feet.

Between 1988 and 1990, Belmoral Mines Ltd. completed a diamond drill program on their property, which included the current optioned property, Aur Area `A' Option (Assessment file GM 47649). The diamond drill hole program consisting of 28 drill holes on the Aur Area 39

'A' Option, totalled 31,106.04 feet and the hole coordinates are summarized in Appendix F. This drilling located several quartz tourmaline gold bearing veins and mineralized shear zones. Be!moral completed a magnetic and VLF-EM surveys in 1975.

From 1975 to 1990, Belmoral Mines Ltd. and its successors owned the Aur Area `A' property. In 1990, the company was taken over by Aur Resources Inc. who acquired 100% ownership of their mining claims. As stated in Section 6.0, a portion of the current property is covered by an option agreement with Aur Resources Inc.

8.3 HARRICANA MINE:

The following description refers to the development activities at the former Harricana Mine:

Norman, G.W.H. (1943a) reported that " During 1937-1938 the shaft was to 325 feet and about 1,800 feet of lateral work were done on the 100, 200 and 300 foot levels".

In 1938 Harricana Amalgamated Gold Mines Incorporation completed a vertical two compartment 320-foot shaft with stations on the 100, 200 and 300-foot levels, also 1560 feet of lateral workings was completed mainly on the 200 and 300-foot levels. A Northern Miner article on May 25, 1944 indicated that practically all of the approximately 200 feet of development was done in ore on the 200 foot level while at least 600 feet was completed on the vein on the 300 foot level. A further 10,000 feet of underground diamond drilling was completed which resulted in defining a zone of 20,000 to 30,000 tons ranging from 0.257 to 0.286 opt gold (Marleau, 1982). This estimate has not been recalculated by the writer and is considered as "exploration information" only and not a `resource" in the terms required by NI 43 141.

In 1945, Harricana Gold Mines Incorporated deepened the shaft to 782 feet with level stations developed on the 400, 520, 640 and 760 foot levels. Also, 619 feet of lateral workings were completed and approximately 4870 feet of underground drilling was completed on the lower levels (Assessment files GM 00052 and 01079A-B). 40

Graham, R.B. et. al. (1953) reported Harricana Gold Mines Incorporated "During 1946 the company contracted for shaft deepening from 320 feet to 1,000 feet, and for 2,000 feet of lateral work. Most of the work was done on the three new levels at 520 feet, 640 feet and 760 feet, respectively".

The following is quoted from l_,atuiippe, M. (197+6) in regards to the mineralization located at the Harricana Mine shaft: "In this zone, on the 200 foot level, the "C" shoot returned 0.53 oz. Gold per ton for a length of 78 feet and a width of 2.0 feet. On the 300 foot level the "C" shoot returned 0.45 oz gold per ton for a length of 60 feet and a width of 2.0 feet. At the northeast end of the zone on the 300 foot level the "D" shoot returned 0.26 oz gold per ton for a length of 50 feet and a width of 2.0 feet. The total tonnage calculated from these shoots carried only 25,000 to 30,000 tons of ore grade material."

A very limited amount of inforrnation is available regarding the above mentioned activities. 41

9.0 GEOLOGICAL SETTING

9.1 REGIONAL GEOLOGY

The Abitibi and Pontiac sub-provinces form the southern part of the Superior Province of the Canadian Shield in Quebec. The Abitibi Subprovince is the largest, one of the most studied and among the richest Archean greenstone belts in the world. It comprises numerous granitoid intrusions and volcanic and sedimentary belts orientated approximately east west, _ dating between 2750 and 2670 Ma. Volcanics units are composed of ultramafic to mafic, mafic, or mafic to felsic assemblages. Sedimentary rocks occur along narrow bands that separate the volcanic assemblages. They are generally composed of clastic units that represent former deep-water basins (Abitibi-type rocks), whereas smaller bands located along major faults in the southern part of the Subprovince represent shallow-water basins (Timiskaming- type rocks). The clastic units generally contain units of polymictic conglomerate and commonly contain oxide-facies banded iron formation. Plutonic rocks are subdivided into eight magmatic suites.

The Abitibi belt also contains a few crustal-scale faults zones known as "breaks", typically 50 to 200 km in length and up to a few kilometres wide. In the Eastern Abitibi, the most important are the Cadillac (Cadillac-Larder Lake), Porcupine-Destor and the Casa-Berardi Breaks. There is a significant component of vertical elongation or thrusting which took place along these fault zones during the Kenoran Orogeny. The Abitibi belt is transected by several major reverse or normal faults oriented east-west to northwest to southeast, as well as by sinistral northeast trending and dextral southeast trending faults that dissect volcano- sedimentary domains into lozenge-shape segments cored by intrusive rocks.

The Abitibi Subprovince is world renowned for the great number and high grade of its precious metal (gold and silver) and polymetallic (copper-zinc-gold-silver and copper-gold) ore deposits.

9.2 LOCAL GEOLOGY

The Malartic-Senneterre-Val d'Or area forms the southeastern part of the Abitibi Subprovince. The Cadillac-Larder Lake Break separates the Abitibi rocks from the Pontiac Subprovince to the south. Metavolcanics of the Malartic Group dominate the area, which consists mainly of basal submarine flood basalts and komatiites overlain by calc-alkaline volcanic sequences of the Val d'Or Central Volcanic Complex. Narrow groups dominated by ultramafic and mafic, the Piche Group, and by greywacke and other metasedimentary rocks, Kewagama Group, were involved during the formation of this tectonic zone. The Cadillac Break, which is approximately east-west trending fault zone, lies 3 kilometres south of Val d'Or. The Pontiac Group located south of the Cadillac Break, consists of intercalated greywackes and conglomerates. The above lithological units have been intruded by both syn- to post tectonic and synvolcanic tonalite, granite and gabbro. Diabase dykes of Proterozoic age have cross cut all lithological units within the Val d'Or area. The generalized geology and location of quartz vein deposits and massive sulphide Polymetallic deposits for the Malartic to Val d'Or area is illustrated in Figure 4. BELMORAL MINE BARNAT MALARTIC ` )` •• • SULLIVAN MINE* ANADIAN MALARTIC • EAST • . KIENA • MALARTIC

FOURNIERE LAKE

OREN ZONEZ

LEGEND SCALE IN KILOMETRES IN= DIABASE DYKE SYN TO LATE TECTONIC FELSIC INTRUSIVE 0 5 10 PRE TECTONIC FELSIC INTRUSIVE CADILLAC GROUP (SEDIMENTARY ROCKS) PONTIAC RIVER GROUP (WACKE, MUDSTONE SEDIMENTARY) P G PONTIAC RIVER GROUP (ULTRAMAFIC LAVA) s Î_-1 BLAKE RIVER GROUP (VOLCANIC ROCKS) ~ o KEWAGAMA GROUP (CONGLOMERATE, WACKE, MUDSTONE SEDIMENTARY ROCKS) i W ~ UPPER MALARTIC GROUP (MAFIC / FELSIC VOLCANIC AND VOLCANOCLASTIC ROCKS) Z EM LOWER MALARTIC GROUP (ULTRAMAFIC / MAFIC VOLCANIC AND VOLCANOCLASTIC ROCKS) ti O GARDEN ISLAND GROUP (SEDIMENTARY ROCKS) KIAN A. JE SEN ~ ~ I KINOJEVIS GROUP MAFIC VOLCANIC ROCKS) PRACTISING EMBER FAULT OR SHEAR ZONE • • GOLD SHOWING, QUARTZ VEIN GOLD DEPOSITS 0558 • ■ GOLD MINE MASSIVE SULPHIDE POLYMETALLIC DEPOSITS N rAR% POLYMETALLIC MINE

Figure 4: General Geology and Location of Quartz Vein Gold Deposits and Massive Sulphide Polymetallic Deposits for the Malartic - Val d'Or Area, Quebec (Modified Geology after Avramtchev and Lebel-Drolet (1981), Couture (1991) and Roberts (1989)). 44

9.3 PROPERTY GEOLOGY

According to Imreh (1984), the Jacola Formation is marked by a repetitive sequence of the following units, from the base upwards: ultramafic flows, basaltic flows and volcanic breccias.

The central portion of the property is underlain by the southern extension of the Bourlamaque Batholith. The granodiorite is generally coarse grained and consists of approximately 50% to 60% plagioclase, 20% to 25% quartz and 20% to 25% ferromagnesian minerals. The composition is variable and mafic xenoliths are locally abundant.

Diorite, quartz diorite, diorite porphyry, feldspar porphyry and syenite porphyry dykes have been reported to exist in Dubuisson Township. Some of these dike cross cut the Bourlamaque Batholith. The dykes are commonly associated with gold mineralization and are an important exploration target.

Figure 5 illustrates the general geology of the current Han icana Mine project and surrounding area, with past and current mines and reported gold bearing mineralization trends. 45

PL GE GRANODIORITE DACITE O ~ TONALITE ; INTERMEDIATE VOLCANICS ~ ~'/ O -~~ DIORITE, QUARTZ DIORITE ANDESITE GABBRO BASALT L ~ MAFIC INTRUSIVES, ~ .1 ~~I/il z iiDIABASE PICRITE ~ MINERALIZATION ULTRAMAFIC VOLCANICS KI N /i. ZONE • SHAFT ~ NSE~~ FAULT / SHEAR ZONE PROPERTY BOUNDARY PRACTISIN MEMBER c ~ 0558 • SCALE IN METRES

1000 500 0 1000 NTAR“)

Figure 5: General Geology Map of Harricana River Mining Corporation Inc. Harricana Mine Project, Boutlamaque and Dubuisson Townships, Val D'Or Area, Quebec. 46

9.3.1 HARRICANA MINE

The author has included the several following sections on the description of the geology at and near the Harricana Mine shaft as the majority of the area is now a residential subdivision with very little exposed bedrock. The original shaft has been capped. The author has converted the reported dollar value of gold into ounces per ton (opt) gold using a conversion factor of $35.00 Canadian to 1 ounce of gold.

The following description pertains to the discovery of Vein 13 at the Harricana mine site (Hawley, J.E. 1931: "On lot 62, a one foot quartz vein is exposed for 100 feet, lying along the contact between a trachyte breccia and a green carbonate andesite or basaltic flow. The quartz carries moderate amounts of chalcopyrite and a little pyrite. It strikes S 72° E and dips 88° N. On lot 59, an easterly trending shear zone in pillow lavas is injected with several quartz stringers and minor amounts of pyrrhotite and chalcopyrite. The sulphide impregnation may be traced for about 100 feet. On the north hanging wall, quartz stringers appear, striking N 20° E for a distance of 120 feet. One of these is displaced by a fault striking N 80° E, the north side of which is moved 15 feet west."

In an article published in the Northern Miner April 23, 1938, it stated that: "The vein was not developed on the first level, but on the 200 foot level drifting revealed a length of 75 feet averaging $9.75 (0.278 opt) across 43 inches plus an additional 20 foot section running $12.10 (0.346 opt) across 34 inches. On the third level two shoots were developed, one 60 feet long and $16.60 (0.474 opt) grade across 23 inches while the other was 50 feet long running $8 (0.228 opt) across three to four feet".

Ross, S.H., et. al. (1938) describes the geology and mineralised setting at and near the Harricana shaft as follows: "The gold bearing vein upon which the shaft was sunk is in block 13, about 1500 feet to the south of the contact between the Bourlamaque granodiorite batholith and the 47

Keewatin volcanics. The vein borders a dyke of granodiorite porphyry, which dips towards the shaft at 70°.

The following notes are based upon information supplied by Mr. MacPherson: - The granodiorite dyke to the southeast of the shall ranges from 2 to 12 feet in width. The strike is arcuate, convex to the southeast, and the dip is about 70°, towards the shaft. The dyke is mineralized with pyrrhotite and the borders are sheared. The vein lies on the footwall side of the dyke. It has been traced over a length of about 200 feet, with average width of 42 inches. It is mineralized with pyrite and chalcopyrite, and it carries $9.20 per ton of gold (0.2628 opt gold). On the hanging wall side, at about diamond drill hole 6, there is a little white quartz containing coarse free gold but no sulphides. Both vein and dyke are faulted at the west.

The granodiorite dyke to the northeast of the shaft is presumably the continuation of the one to the southeast. There is a little quartz on the footwall side, which carries about $2.00 per ton of gold (0.057 opt gold).

The vein 4,000 feet to the west of the shaft is of gold bearing quartz. The maximum exposed width is about 12 inches.

Quoting from memory, Mr. MacPherson reported the following diamond drill intersections: Hole 1 50 foot shear. Values about $2.40 per ton (0.068 opt gold) Hole 4 6 inches. $5.00 per ton. (0.143 opt gold) Hole 5 Visible gold. Average value $9.00 per ton (0.257 opt gold); width 42 inches. Hole 6 Values in greenstone hanging wall, but not in quartz or the dyke. Hole 11 Visible gold in strong shear over core length of 11 feet at 866 footage. True width probably 6 feet; much core lost. Values $3.15 per ton (0.090 opt gold), sludge $65.per ton (1.857 opt gold). 48

Hole 22 52 inches in vein material, of which 18 inches assays $8.00 per ton (0.228 opt gold), sludge 10 feet at $25 per ton (0.714 opt gold). Hole 27 About 48 inches at about $2.00 per ton (0.057 opt gold). Shaft Vein encountered at 200 feet; 18 inches at $6.30 per ton (0.180 opt gold)."

Ingham, W.N. (1945) reported that during 1944: "The fourth hole, located 170 feet southwest of the shaft, cut a well mineralized quartz vein assaying an average of $31.00 (0.886 opt) in gold per ton for a core length of 2.5 feet. The hole is vertical and cuts the vein close to underground workings following it southwest from the shaft."

Figure 6 illustrates the underground development and the known vein structures at the Harricana Mine. 49

5900 NORTH N '

1 HARRICANA SHAFT -, LENS'Er \ , 05600 NORTH ~Ue ~~ LENS C ~~ Spa of Of LENS 'C' ...... } c- G,>O Z .. C SURFACE a' N --..c a p G.., ~m co J~~

5300 NORTH `A L G F O 100 FOOT LEVEL O , S 200 FOOT LEVEL \ 520 FOOT LEVEL ~.•i m 520 FOOT LEVEL 1 Z 640 FOOT LEVEL LL -760 FOOT LEVEL KIAN A -JE EN — SCALE IN FEET o PRACTISING EMBER c ME 100 0 100 0558 Q ô $ U NTARO) 5000 NORTH ~

Figure 6: Underground Development and Known Vein Structures at the Harricana Mine, Bourlamaque Township, Val d'Or, Quebec, Canada (Modified after Kirwin, 1999). 50

9.3.2 AUR AREA `A' OPTION

The dominant lithology of this area is a medium to coarse grained, equigranular granodiorite, of the Bouriamaque Batholith sometimes referred to as a tonalite, which is composed of chloritized hornblende, greenish gray feldspar and a lesser amount of quartz. This felsic intrusive is overlain by an aphanitic to fine grained, dark to medium green, massive mafic metavolcanics and ultramafic metavolcanics. The western margin of the property has the metavolcanics in a relatively tight fold structure. The contact between these lithological units is approximately northeast.

The shear zones transgress the contact of the granodiorite along its approximately east-west trending strike and its northerly 70° dip. The shear zones for the most part display a distinct fabric or foliation, weak to moderate development of alteration, with trace to 1% to 2% euhedral pyrite with or without quartz stringers, veinlets and veins.

Gold mineralisation has been detected in one of the more steeply dipping shear zones and several of the shallow dipping shear zones.

10.0 DEPOSIT TYPES

There are significant differences in the geological attributes to distinguish a few types of gold deposits in the Eastern Abitibi. Two major classes of gold deposits can be defined: gold-vein deposits and pyritic or sulphide-rich gold deposits.

10.1 QUARTZ VEIN GOLD DEPOSITS

porphyritic plugs, sills and dykes. However, they are found in all rock types including the late tectonic intrusions.

Mineralized shear zones represent third-order structures, which are typically a few hundred to a few thousand metres length. Mineralized shear zones and discrete faults typically contain several lenticular ore bodies separated from one another by barren segments of shear zone. The ore bodies are commonly elongate and in many cases the long axis bears a geometric relationship to the slip direction. Shear zone hosted ore bodies consist of alteration or replacement of the rocks within and adjacent to the shear zones, or of veins parallel or slightly oblique to the shear zone. The majority of the mineralised shear zones exhibit mixed continuous — discontinuous (brittle — ductile) behaviour. Usually these veins have been emplaced relatively late in the evolution of the shear zones and are not significantly deformed, however at the Ferderber mine these veins have been deformed and folded which indicates continued shearing after vein emplacement.

Veins in extensional fractures are commonly present within shear zones. These veins may also extend outside the shear zones and are common in the Val d'Or district where they are typically sub-horizontal. At the Sigma mine the dimensions and grades of these sub-horizontal extension veins can be exploited and mined.

The hydrothermal breccias or breccia veins are typically composed of angular fragments of altered wallrock in a matrix of hydrothermal minerals such as quartz, carbonate, albite and tourmaline. Hydrothermal breccias commonly occur where shear zones transect competent — lithologies, such as at the Sigma mine, or intersect other shear zones. 52

A small number of quartz vein gold deposits occur in moderately to steeply plunging Z-shaped folds of the dominant foliation along the Cadillac Break. Two types of fold association exist. Veins that lie parallel to the dominant foliation were folded with this foliation as represented at the Orenda Zone 4 deposit. The second type consists of vein networks within a small felsic intrusion in the nose of such an asymmetric fold.

The vein mineral assemblage consists mostly of quartz and carbonate, with variable proportions of pyrite, arsenopyrite, chalcopyrite, tourmaline, albite, chlorite, and smaller amounts of scheelite, tellurides and native gold. The Val d'Or deposits are characterized by abundant tourmaline and most gold deposits hosted by or adjacent to clastic sedimentary rocks are characterized by arsenopyrite as the dominant sulphide rather than pyrite.

Wallrock alteration is generally characterized by carbonatization, potassium metasomatism and pyritization. Alteration envelopes are typically zoned which reflects progressive replacement of metamorphic minerals, ferro-magnesian silicates by carbonate minerals, and closer to the veins by sericite and pyrite.

10.2 PYRITIC GOLD DEPOSITS

Pyritic gold deposits consist of ore bodies dominated by disseminated to massive sulphides or by abundant pyrite-rich veinlets. All of these deposits occur within or adjacent to major deformation zones and in volcanic units known to contain VMS deposits.

In contrast to quartz vein gold deposits, the environment of pyritic gold deposits are dominated by felsic volcanic rocks that are partially converted to a sericitic schist and they lack the small porphyries (plugs, sills and dykes).

Pyrite rich veins are generally a few centimeters thick and up to several metres. Their orientation ranges from parallel to slightly oblique with respect to the foliation, crosscutting and locally folded and to high angle to foliation and variably buckled. 53

Disseminated pyrite also accompanies these vein type ore bodies. Several generations of disseminated pyrite may occur including syn-volcanic, deformed pyrite, syn-tectonic pyrite and disseminated pyrite in alteration fringes around late tectonic iron dolomite veins.

The mineral assemblages of the sulphide vein and massive ore bodies are dominated by pyrite, accompanied by variable amounts of chalcopyrite, pyrrhotite, sphalerite, arsenopyrite, galena and magnetite.

Large volumes of altered rocks are present around and in the vicinity of pyritic gold deposits, but the alteration is not necessarily directly associated with or distributed only around ore bodies.

11.0 MINERALIZATION

Gold is the principal metal known on the property and is usually very fine grained. Minor amounts of silver, copper and zinc have been reported to occur within the property boundary.

The mineralization for the Harricana Mine is described in Section 9.3.1 of the Property Geology. An undated plan map of the 200 and 300 foot levels of the mine indicates that the gold values converted to ounces ranged from trace to 0.71 opt gold over quartz vein widths from 10 to 49 inches and 0.04 to 0.51 opt gold over quartz vein widths of 11 to 32 inches for zone `C', respectively, and 0.03 to 0.65 opt gold over quartz vein widths of 11 to 46 inches for zone `D' on the 300 foot level. Significant gold mineralization intercepts from the various diamond drilling programs are listed in Tables 4 and 5.

The mineralization of the zone northwest of the Harricana Shaft is known as the Hydro Zone, which contains gold mineralization in narrow quartz veins steeply dipping to the south within the intermediate metavolcanics or at the contact of the intermediate and ultramafic metavolcanics on the south side of a lobe from the Bourlamaque Batholith. Canstat Petroleum Corporation drilled the Hydro Zone and High Voltage Zone and the significant gold mineralization intercepts are listed in Tables 6 and 7. 54

The High Voltage Zone is very similar to the mineralization at the Ferderber Mine, which are hosted within the Bourlamaque Bath°lith. This zone is located north of the by-pass highway and is near the Quebec high voltage transmission line. Significant gold mineralization intercepts from the IBEL diamond drilling campaign is listed in Tables $.

Table 9 lists some of the significant gold mineralization intercepts from the Belmoral diamond drilling campaign on the current Aur Area `A' Option.

Currently, the gold mineralization located within the property boundary would be similar to the quartz vein gold deposits rather than the pyritic gold deposits described above. 55

Table 4: Significant Assay Results from the 1936 Diamond Drilling Program by Harricana Amalgamated Gold Mines Inc. at the Harricana Shaft Area.

Hole No From To Width Gold Au (opt) Comments (feet) (feet) (feet) $35.00/oz H-1 75.00 80.00 5.00 $ 1.40 0.040 90.00 95.00 5.00 $ 0.35 0.010 95.00 100.00 5.00 $ 2.45 0.070 100.00 105.00 5.00 $ 1.40 0.040 H-5 99.50 100.00 0.50 $ 31.50 0.900 VG 100.00 102.83 2.83 $ 5.25 0.150 102.83 103.33 0.50 $ 0.70 0.020 103.33 104.33 1.00 $ 0.35 0.010 H-6 100.00 101.00 1.00 $ 3.50 0.100 H-11 376.33 378.00 1.67 $ 3.15 0.090 VG at 876.33 H-15 301.50 303.50 2.00 $ 1.05 0.030 H-17 237.00 238.50 1.50 $ 1.05 0.030

Table 5: Significant Assay Results from the 1981 Diamond Drilling Program by Provinces X Exploration Inc. at the Harricana Shaft Area.

Hole No From To Width Au (opt) Au2 (opt) (feet) (feet) (feet) (check) HP-1 192.00 192.30 0.30 0.120 0.045 265.00 267.00 2.00 0.030 0.060 267.00 268.25 1.25 0.640 0.750 268.25 269.75 1.50 0.140 0.070 276.00 278.00 2.00 0.110 0.020 HP-2 140.50 141.00 0.50 0.750 141.00 144.00 3.00 0.060 158.60 160.00 1.40 0.090 160.00 161.00 1.00 0.260 0.215 204.20 206.20 2.00 0.180 0.195 HP-3 61.00 63.75 2.75 0.040 63.75 65.75 2.00 0.060 65.75 67.00 1.25 0.040 0.048 HP-4 272.50 273.00 0.50 0.510 HP-10 56.00 57.00 1.00 0.070 0.080 57.00 58.00 1.00 0.560 0.510 69.00 70.00 1.00 0.460 56

Table 6: Significant Assay Results from the 1986 Diamond Drilling Program by Canstat Petroleum Corporation at the Hydro Zone and High Voltage Zone.

Hole No From To Width Au (g/t) Au (opt) (metres) (metres) (metres) CB86-3 169.50 170.50 1.00 0.070 977.00 978.50 1.50 0.050 CB86-4 433.00 434.50 1.50 0.190 CB86-5 334.40 335.70 1.30 0.200 703.50 704.50 1.00 0.060 708.00 709.60 1.60 0.240 CB86-6 844.30 845.30 1.00 0.080 CB86-7 137.10 138.70 1.60 0.090

Table 7: Significant Assay Results from the 1986 and 1987 Diamond Drilling Program by Canstat Petroleum Corporation at the Hydro Zone and High Voltage Zone.

Hole No From To Width Au (g/t) Au (opt) (metres) (metres) (metres) CL-5 29.52 30.26 0.74 4.66 0.136 CL-9 61.80 62.30 0.50 11.50 0.335 CL-17 151.70 152.72 1.02 3.96 0.116 CL-18 223.50 224.45 0.95 10.18 0.297 CL-25 82.63 83.16 0.53 8.92 0.260 CL-28 85.15 86.15 1.00 22.40 0.653 CL-31 91.30 91.80 0.50 7.50 0.219 CL-36 184.70 185.62 0.92 4.40 0.128 CL-45 150.33 150.83 0.50 3.55 0.104 152.57 153.13 0.56 4.50 0.131 CL-49 152.52 153.62 1.10 19.30 0.563 CL-51 385.14 385.64 0.50 3.60 0.105 CL-52 157.90 158.80 0.90 1.25 0.036 CL-53 139.60 140.34 0.74 4.79 0.140 CL-78 127.98 128.48 0.50 5.30 0.155 57

Table 8: Significant Assay Results from the 1989 Diamond Drilling Program by International Baslen Enterprises Ltd. at the High Voltage Zone.

Hole No From To Width Au (opt) Au2 (opt) Au3 (opt) (feet) (feet) (feet) (check) (check) IB-1 579.00 580.00 1.00 0.034 580.00 583.00 3.00 0.270 I B-5 438.71 443.25 4.54 0.058 0.065 0.063 IB-6 771.42 775.16 3.74 0.148 0.154 0.156 I B-7 357.30 362.22 4.92 0.040 550.40 554.10 3.70 0.034 I B-9 520.00 523.00 3.00 0.115 0.145 0.133 523.00 526.50 3.50 0.225 0.203 0.215 IB-11 684.00 685.00 1.00 0.414 685.00 687.00 2.00 0.007 687.00 688.00 1.00 0.093

Table 9: Significant Assay Results from the 1988 and 1989 Diamond Drilling Program by Belmoral Mines Limited at the Aur Area `A' Option.

Hole No From To Width Au (opt) Au2 (opt) (feet) (feet) (feet) (check) B88-28 683.90 685.00 1.10 0.380 688-49 906.40 907.40 1.00 2.540 915.80 917.00 1.20 0.880 917.00 918.10 1.10 0.860 918.10 920.00 1.90 1.040 944.70 945.20 0.50 0.500 B88-51 232.30 233.00 0.70 0.460 680.10 681.50 1.40 0.420 696.90 697.30 0.40 0.420 B88-53 761.60 762.70 1.10 0.460 763.60 764.20 0.60 1.940 764.90 765.20 0.30 0.580 768.00 768.80 0.80 0.540 B88-54 802.80 803.40 0.60 0.400 806.40 808.00 1.60 0.980 810.60 811.40 0.80 3.940 811.40 812.30 0.90 0.340 830.00 832.20 2.20 1.700 841.50 842.10 0.60 1.220 1.300 862.60 863.30 0.70 0.260 0.440 879.00 879.50 0.50 0.520 0.560 1011.00 1011.80 0.80 0.200 0.180 58

Table 9: continued

Hole No From To Width Au (opt) Au2 (opt) (feet) (feet) (feet) (check) B88-54 1025.80 1026.00 0.20 0.940 0.920 1026.30 1026.70 0.40 0.580 0.620 1026.70 1027.50 0.80 2.380 2.200 1035.40 1036.00 0.60 0.240 0.120 1044.20 1045.00 0.80 1.260 1.360 1051.00 1052.10 1.10 0.380 0.360 1052.10 1053.0d 0.90 0.300 0.340 B88-55 745.60 748.00 2.40 0.380 0.360 752.30 753.00 0.70 0.200 0.160 939.70 940.50 0.80 2.100 2.280 1019.50 1020.10 0.60 1.480 B88-56 497.50 497.90 0.40 8.160 8.020 497.90 498.70 0.80 1.700 1.200 499.40 500.10 0.70 0.280 B88-58 933.00 933.40 0.40 0.240 933.40 933.60 0.20 1.040 1.080 B88-59 656.80 657.90 1.10 0.260 657.90 658.60 0.70 0.280 1059.10 1059.90 0.80 0.280 0.340 1072.70 1073.40 0.70 0.200 0.160 B88-60 855.50 856.20 0.70 0.320 0.320 B88-68 806.60 808.10 1.50 0.280 0.240 B88-73 542.00 542.8d 0.80 0.308 591.10 592.30 1.20 0.280 0.160 B88-77 856.30 858.50 2.20 0.226 0.181 858.50 861.10 2.60 0.410 0.513 B90-10 384.40 384.90 0.50 0.640 0.200 B90-13 272.90 273.90 1.00 0.300 292.00 293.10 1.10 0.460 465.50 467.50 2.00 0.220 59

12.0 EXPLORATION

Figure 7 illustrates the location of the diamond drill holes and the gold bearing zones from the various drilling campaigns in the southern portion of the Harricana property.

Canstat Petroleum Corporation completed 91 diamond drill holes totalling 24,077.82 metres (15 holes in the CB series in 1986 and 76 holes in the CL series during 1986 and 1987), which resulted in the discovery of several gold bearing mineralization zones as well as an area of gold and copper mineralisation in the northeast portion of the property. Figure 8 illustrates the diamond drill hole longitudinal for the Hydro Zone.

During 1988, International Baslen Enterprises Limited (IBEL) purchased the property through their then wholly owned subsidiary 2629-2482 Quebec Inc. In 1989 IBEL completed 11 diamond drill holes totalling 9,413 feet under the supervision of Earth Resource Associates. The diamond drill hole coordinates covering the area north of the Harricana shaft are summarized in Appendix F. Figure 9 illustrates the diamond drill hole longitudinal for the High Voltage Zone located north of the Val d'Or by-pass Highway.

The Aur Area `A' is the subject of the option agreement between Aur Resources Ltd., International Baslen Enterprises Ltd. (IBEL) and 2629-2482 Quebec Inc. dated September 24, 2001. By an instrument of Transfer dated September 25, 2001, IBEL transferred all of its rights under the Aur Agreement to 2629-2482 Quebec Inc.

During late 2001 and early 2002, 2629-2482 Quebec Inc. contracted H. Ferderber of Prospecting Geophysics Limited of Val d'Or, Quebec, to complete a ground magnetic survey and a VLF-EM survey on the Aur Area A option property and all or a portion of 5 additional mining claims in Area B adjacent and to the west. The grid was established at 200 foot line spacing with reading intervals at 50 feet.

\ ryo) ; ) \ \ 3838331 LAC BLOWN `~ ~ I 849184 ~ I 10,000N(11) 3 i SEN TIER CESFOUGERES \` • ` t 9e39332 ~ 3849141 = ~~ Ru C42011•4 ~ 3a49111 ~ ~" , ~~ ~ ~ I~ .0. j ~_~ , ~/ ~...... RUE ~1 ~~ 1 .,, . sa .,, tl 4, `" 3849094 ; ~ ' :''lit __ •- • 3849112 v _ ilpPFR ZO~E --- ------ — --~~ - A uc srABEu o> ` CL-49 ZONE y - ~ RDD ZONE y 5-333 mN- - LOwtiiZtfNE . _ I ~— ~ 8,000 N(n) — 3849145 3849142 ~ 3849113 f`1 DUBUISSON TOWNSHIP BOURLAMAQUE TOWN~HIP ~

.. 3849 44 384..143 7,000 N(n) 1 --aou~cwRanErr+w ~= T 1 i~=s-- -- Î — — —J—J ~-~-- ., F ~~ i'". I 1I I HYDRO ZONE I 1 . _ ~ ---1 oco Nro) ~ , ~ I , M •-~r 3849173 ~ • 1 ( I ltt ... ( 11,000m N 1 , /MIA I a: ~ --- ••------•------~--... I ,t ij.-~t - , ~1 ~ ^~ . .. 1 .. +- ~T ~ I ---_ ` ~ M I Î ~ ~ ,~..r-~~849185 1 ~ ./." 1 ~~ ~ _— ~— 1 N.R~RAIIWAY ~_.~ ' I _ - _ S 772 OOD C. i~ mN---_- 5 111 N(I) ---... a - - ~, I ..1 1 A L G. ,--- M N F 0 I ~ ~ â1~ I rn~ ~ ~I ~ 3849174 / ~•~ ~o ~ Nit I " A A ~ i / y 00rî ~ I a W "el / U. ~~ ' Z I HIGHWAY 111 ~ / v , aÿOO N(n) É W W É Q ~ ~ É âE ~qAN A: JE EI~ ' — 1 w 1.1 5W~ /~ $ $ y ~rL4CI7SIN6 ~ ' $ ~ R,cRwAr v 1 ô Mf~f~ Y ~ i R _, 0558 _ ~ SCALE IN METRES SCALE IN FEET ~ 100 0 lao zoo 400 0 soo 1000 2000 TAR ~ Figure 7: Surface Plan of Diamond Drill Holes and Gold Bearing Zones of Harricana River Mining Corporation Inc., Bourlamaque and Dubuisson Townships, Val d'Or Area, Quebec.

w w WEST E E EAST 0 0 0 0 M W W W ~ W W C.J1, ô O _ô ~ô ô CO N M M ~ V V SURFACE SURFACE (FEET) (FEET)

OVERBURDEN

-100 -100

-200 CL-9 CL-24 • 0.335/1.64 0 0.06813.15 • CL-30

• CL-19 • 0.260/1.74 • b5313.28 -300 _ -300 •~~ • CL-73

CL-78 0 CL-75 00.057/1.92 0.014/1.8 -400 400 CL-82 CL-53 0 0.07611.64 • 0.140/2.43

CL-80 0 0.070/3.28 • CL-76 -500 CL 64 -500 CL-52 • 0 0.036/3.0

• CL-79

CL-63 -600 • •CL-6z

• CL-43 CL-42 -700 • AL\'i G LEGEND •1• ¢ CL-2b DRILL HOLE NUMBER 1" vy 0 653'3.28 OUNCES GOLD PER TON l FEET O KIAN A: JE SEN _ p, PRACTISING MEMBER

SCALE IN FEET 0558 AR 0 0 100 200 400 ON T

Figure 8: Hydro Zone Longitudinal with Constat Petroleum Corporation Diamond Drilling (Modified after Kirwin, 1999). 62

SURFACE (FEET) i ~ 1 e e e • • e , • a • , •• e e ~ • ••• • •. e. e • • v • • e • e• • CL-18 • • e • 'a • -100 • • w110040.0. -100 e • a •• • IB-6 e a • e 0.004/3.4 • • • • e . . : IB-3 • IB-5 CL-18 0.006/5.0 0.009/3.0 -200 0.003/1.5 • IB-4 -200 CL-17 ~ no assays 0.05/1.75 • IB-2 0.005/1.5 • IB-9 IB-1 -300 0.013/4.0 • M07/3 0 -300 CL-48 • 0.024/3.4 • IB-11 0.004/4.0 IB-8 CB86-4 • CB86-5 • 0.10/1.5 0.20/1.3 1B-9 0.006/2.0 • IB-6 partially 0.177/6.5 • trace -400 sampled -400 • CB8a-5 IB-3 no assays IB-7 • 0.003/5.0 • 0.015/13.0 • IB-9 • IB-10 0.011/5.0 • IB-3 • IB-5 -500 I6-11 • no assays nn~e -500 trace 0.012/2.5 CL-17 IB-8 CL-48 • 0.115/3.3 • 0.027/5.0 0.02/7.7 % CB86-5 0.240/1.6 IB-11 • 0.13/4.0 CL-49 IB-4 -600 0.560/3.0• -600 • IB-2 • 0.015/5.0 CL-18 0.011/4.5 • IB-6 0.296/3.0 0.153/3.5

• IB-1 • IB-7 0.171/5.0 -700 • 1B-10 0 024/4 5 -700 trace • CL-48 0.040/1.6 IB-10 • IB-2 IB-5 • trace 0.018/4.0 • 0.003/3.0 -800 -800

• IB-7 IB-1 0.008/5.0 • trace

-900 • It3-4 0.013/8.0 tu LL • UPPER ZONE CL-49 DRILL HOLE NUMBER 0.560/3.0 OUNCES GOLD PER TON / FEET • CL-49 ZONE K KIAN A JE • RDD ZONE PRACTISNG LOWER ZONE SCALE IN FEET • Oô58 • 100 0 100 200 ? AR A Figure 9: Composite Longitudinal of the Upper, CL-49, RDD and Lower Zones with Constat Petroleum Corporation and International Baslen Enterprises Limited Diamond Drilling, Harricana Mine Project, Val d'Or, Quebec. (Modified after Kirwin, 1999). 63

The intersection of Line 0+00 and the Baseline 0+00 North was established at the intersection of the Township Line and the shoreline of Lac Blouin. Exsics Exploration Limited of Timmins, Ontario, completed the data reduction. Figure 10 illustrate the location of the Aur Area `A' option with the 2000 geophysical survey grid and the 1988 Belmoral Mines diamond drill grid. Geophysical survey Line 8+00 East is approximately at Belmoral Mines drill grid Line 0+00.

13.0 DRILLING

During 1989, International Baslen Enterprises Limited (IBEL) purchased the property through their then wholly owned subsidiary 2629-2482 Quebec Inc. (currently HRMC). In 1989 the company completed 11 diamond drill holes (IB series) totalling 9,413 feet of BQ core size, north of the Val d'Or by-pass highway known as the High Voltage Zone, under the supervision of Dr. John Kirwin of Earth Resource Associates, Timmins, Ontario.

The drill core was stored at the Hunter Mine facility in South Porcupine, Ontario, which was later dumped down the Hunter Mine shaft during the mine site rehabilitation. The company has not conducted additional diamond drilling on the property since 1989.

During 1988 and 1990, Belmoral Mines Ltd. As part of their regional exploration completed a 28 hole diamond drill program totalling 31,106.04 feet on the current optioned property known as the Aur Area `A'. Figure 11 illustrates the location of the diamond drill holes and the gold bearing zones from the various drilling campaigns in the northern portion of the Harricana property. The Line 0+00 of the diamond drilling is located approximately 200 feet east of the western boundary of the 9 claim Aur Area `A' Option and approximately correlates to Line 10+00 East on the geophysical grid.

The following series of drill sections, Figures 12 to 18 illustrates the general geology, shear zones, gold bearing zones used in the resource estimation and significant assays on Lines 0+00, 2+00 East, 4+00 East, 6+00 East, 8+00 East, 10+00 East and 12+00 East, respectively. 64

w w E 0 8 LAC BLOUlN E

~ 000m

N 3 22, g E ~ 8 8 ~ $ 8

~ ~ 10.00 E

V V i i ï NE SENNEVILLE TC WNSHIP ~ { r". 4t.oeem44 ~ B LAMARUE TOWNSHIP / 2.00 S . I 000 mN 4.00 8 . (336 44.1' 6.00 a , 1 6.00 a 143 3494144 3490145 18.000'N( ) 3494 10.00 9

6400 a . `f t.00a,

dary 3849223 3494142 3494150 349415.1 Boun ty

l er

16,000 h ~ Prop Aur Opt10 ArL ' 3838555 3494141 13.000m N r- 9224 34 151 Î 53 5 000 mN

.5;860Y. m. • - i 34941 2 48° 08' 00"

t+~ CO 383E312 L G Property Boundary A S 14,000 e W -• - tc% ô 3849225 ~ 38492111 ô 3849212 8 ô Z

SCALE IN METRES A. EN PRACTISING M 100 100 200 400 2002 GEOPHYSICAL SURVEY GRID SCALE IN FEET BELMORAL DIAMOND DRILL GRID 0558 500 1000 2000 NTAR Figure 10: Location Map of the 2002 Geophysical Survey Grid and 1988 Belmoral Mines Diamond Drill Grid, Aur Area `A' Option Mining Claims of Harricana River Mining Corporation Inc. Harricana Mine Project, Bourlamaque Townships, Val d'Or Area, Quebec.

cv cki O CV / N_ 2 W W W W W W W WW O O O O O Ô Ôp j 00 O O O O O + + + 890-5 • O J O ÔD N v B89 3 c+ B89-4 c+0 ~ N m W , / U Z Z Z Z Z Z Z ZZ Q J J J J J J J J JJ

B89-2 _ _ BASE LINE B89-1 • S ENNEVILLETOWNSHIP !' / i 88877 Bô8- BBB-59 Bgg~, BOURLAMAOL E TOWNSHIP' 14,000m N + ~S \ { • B88-81 i B88-62• ~ 888-56 B88~ B88-54. 888-65 / f' / + ~}~ S` B88-53 ~r. 888 30 _888-58•_ 888-60 I ,+ __ i / ,r/ B88-79 ~— B9p0-11, .. -- yn^^ c +, i' , - B88-49 , _. / ,' 5 336 000 mN I . , B8-8-83 • - _;_~ B88.St, .~ ~ ------_ ---: ---:---- -^ ------88828♦ _ /' % +00 S . •B911-12 ~ B88-76 • - l B90-9 , -- - 3494144 ~" ... B88-37. B88-31 8+00 S . 890-10 3,494143 18,000 N(ft) - . ...... i 10+00 S .

) ~ I .... E B87-144 • 12+00 S _ 3849221 ., ---~BB7-147 AUrArea B 1 14+00 S .

---• AurArea 'A' 16+00 S _ 13,500 N ~ -,. - ------38'9223 18+00 s ; 3494153 17,000 N(ft) . - 20+00 S - ^ '

x 22+00 S _ c - p L G 3494142 Q~ oW ' ô ô wo W ~ ' ~ ~ ô ~ ~~~• c 'c:- A , tut,' ArVek . - - z :

SCALE IN METRES d KIAN A. JÉNS N PRACTISING MEMBER 50 50 100 200 SCALE IN FEET 0558 o 0 250 500 1000 NTAR Figure 11: Location Map of Diamond Drill Holes on the Aur Area `A' Mining Claims of Harricana River Mining Corporation Inc. Harricana Mine Project, Bourlamaque Townships, Val d'Or Area, Quebec.

SOUTH NORTH

890-12 B90.11 B88-62

d 4 I

ZONE No.1 I

NORTH 0.008 / 17.50 ` SHEAR ZONE

104 / 22.8 9,500 9,500 `é

\ \ \ \ SOUTH \\ \\ SHEAR \\ \\ ZONE `\ ZONE No.2 I

\ \ \\\ \ 1 ~ • • ZONE No.3A \ \ --•'• • `~~` I ZONE No.36 9,000 _ _ 9,000 \ \\ ZONE No.4A \ \

\ \\ \ \ \ \ \\ 1\

\ \ \ \ \1 dI \ \ \ \ 1 ;I~ \ \ \ \ \ â • J \ \ \ \ d `\ \\ I W \\\ 0I \ TH \ 1 CO • 0) \\ W_

SOUTH \ \ ~

_ 8,500 0 8,500 _ +00 SOU W I \ \ \ 10 5+0

_ m - _ I \ \

HARRICANA RIVER MINING CORPORATION INC.

HARRICANA MINE PROJECT - AUR AREA 'A' OPTION SECTION 0+00 EAST - LOOKING DUE WEST

LEGEND OVERBURDEN IAN A. EN - I ~ GRANODIORITE PRACTISING EMBER I I VOLCANICS 0558 SHEAR ZONE I I AURIFEROUS ZONE NrAR\ 0.314 / 22.90 GOLD (OUNCES PER TON / FEET) °

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. DATE: REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30, 2004

Figure 12: Section 0+00, Aur Area `A' Option 67

I ~ I ~

SOUTH NORTH B90-13 » B90-10 B90-9 688-83 B88-51 B88-53 B88-77

•N, \ 0.032 / 10.

0.156 / 5.10 ` `CV/

`, NORTH , SHEAR \\ ZONE

9.1120 / 8.70`, \ 9,500 \ .002 / 28.00 9,500 _

\ ~\

\ \ 0.138 ),0.30 _ZONE No.2 `\ 0.106 / 6.80 \ \ • "4.4

69./ 17`2 07 \v 1,0.168 / 12.50 'moi QUARTZ VEIN SOUTH SHEAR • ZONE No.3A ZONE ) ZONE No.3B _ 9,000 9,000 — I ZONE No.4A •

I •

•

~ ô ~ _ 8,500 0 8,500 0ô ~I~

HARRICANA RIVER MINING CORPORATION INC. HARRICANA MINE PROJECT - AUR AREA 'A' OPTION SECTION 2+00 EAST - LOOKING DUE WEST

LEGEND OVERBURDEN I GRANODI ORITE 0, PRACTISING MEMBER y I ~ VOLCANICS 0558 I 1 SHEAR ZONE AURIFEROUS ZONE 0.314 / 22.90 GOLD (OUNCES PER TON / FEET) • °Nrmoo •

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. DATE: REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30, 2004

Figure 13: Section 2+00 East, Aur Area `A' Option

W SOUTH `m NORTH B88-37 B88-31 B88-28 B88-49 B88-55 89-3 90-5

•

ZONE No.1 ` -- -- ~ • ‘~ . ``s• • NORTH `' ` •, `p.019/Éî.90 SHEAR 1 ZONE ' 9,500 9,300 ` ~' 9.000/9.40` ` • s. `, '\` I •

SOUTH `‘ ` • ` `~~ ~~ SHEAR ~~ ` ` ` ZONE ZONE Na2~! s. ' - '0.026 / 6.10 0.131/4.50 ` ~ `• `.1 \ \ si ~''.‘4''s `‘ ~ QUARTZ VEIN ~ 10.118 114.70 0.002/17.50 ` 0.007/8.10 ~z. ~~ :~~ . ~ —.ft.__~ I. 10.043/7.20

``♦ `~ ` `` , O. 64/11.10 ` - -``` . ` ` `• . `` `~ 0 ~ 53/9~ 30 ~ • .101/2. ~ _ ~ ~~ ` OZONE Na3A ~ÈONE No. 9,000 3B 9,000 1 `` ' 0.070 / 16.30 s ~'~ ZONÈ• No.4A ,, . 1 •

~ s 8,500 ~ 9,300 â â

HARRICANA RIVER MINING CORPORATION INC.

HARRICANA MINE PROJECT - AUR AREA 'A' OPTION SECTION 4+00 EAST - LOOKING DUE WEST

LEGEND OVERBURDEN I GRANODIORITE I VOLCANICS I SHEAR ZONE AURIFEROUS ZONE GOLD (OUNCES PER TON / FEET) SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. DATE: REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30, 2004

Figure 14: Section 4+00 East, Aur Area `A' Option 69

W SOUTH M NORTH B88-56 m 89-3 90-5 B88-30 B88-54 B88-59 89-1 89-4 90-6 • • a 9 a ▪ 89-4

I 90-6 NORTH SHEAR I ZONE No.1 ZONE 89-3 I s s ~ 0.441 /12.10 9,500 I 9,500

90-5 '

0.000/9.00

`f-I __ SOUTH 0.000 0 0 ZONE 2 SHEAR ZONE

~ w ZONE No.3A ZONE No.3B T 9,000 9,000 ` O 1 0.088.1 5.20 JJ ZONE No.4A 0.071 ZONE No.4B W 0.143 12.81Y. ‘,0.21 IL I

~ 8,500 8,500 8

HARRICANA RIVER MINING CORPORATION INC.

HARRICANA MINE PROJECT - AUR AREA 'A' OPTION SECTION 6+00 EAST - LOOKING DUE WEST

LEGEND I I OVERBURDEN KIAN A. NS N I I GRANODIORITE PRACTISING ME BER I I VOLCANICS 0558 I SHEAR ZONE • • MIEN AURIFEROUS ZONE 0.314 I 22.90 GOLD (OUNCES PER TON / FEET)

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. DATE: REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30, 2004

Figure 15: Section 6+00 East, Aur Area `A' Option 70

W 2

SOUTH NORTH B88-76 B88-73 B88-58 B88-63 89-2

• a < d

G 4° d \ a~ SOUTH \\ SHEAR \ ZONE \\ \ \

0.118 / 3.28 9,500 ,\ 9,500 _

•

• `NE2 ZONE No.1 89-3. B88-73

1188-88 0.089 / 1.70 ~ `` • Si' • 89-2 0.0144 17.00 � 90-5 \ 0.1013/ 3A 0.052 / 1.31 ••••. 93 / 1.2 • _ 9,000 9,909 _ v '4'.2414441 ZONE No.36 ZONE No.4A

I ZONE No.46 ~

;I~

â ' ~

g. w ~ Z ôI W 02.0 ~ W~ ~ _ 8,500 ~ 5 8,500 _ E 688458 I ~I I ! I bI I I I

HARRICANA RIVER MINING CORPORATION INC.

HARRICANA MINE PROJECT - AUR AREA 'A' OPTION SECTION 8+00 EAST - LOOKING DUE WEST Avi,it~; LEGEND N A. JE SEN OVERBURDEN co I I GRANODIORITE PRACTISING EMBER y I I VOLCANICS 0558 ~ ~ SHEAR ZONE • AURIFEROUS ZONE o 0.314 / 22.90 GOLD (OUNCES PER TON / FEET) N

SCALE IN FEET COMPILED BY: K.A. JENSEN. P.Geo. DATE: REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30. 2004

Figure 16: Section 8+00 East, Aur Area `A' Option W 2

V SOUTH m NORTH 888-79 B88-60

4 ' • ^â , ' I• a a d ^• • •a — a

' ~ e

• \ • I • \ • I ZONE N4.1` NORTH • SHEAR I • ZONE • s s 9,500 • I • • ZONE N0.Ÿ I

89-4' 89-3

SOUTH \ I SHEAR

ZONE 4%4, — ~ 90-6 \ \\ ~ ~L30

%a*~~ ` ZONE No.3A ~ \\ 0.038 / 2.30 t..* ~. ZONE No.3B 90-5 \ \ ~ ~•; ZONE No.4A • _ 9,000 \ \ 9,000 \ I \ \ O ZONE No.4B

~ _ 8,500 8 8,500 _ a ~I I I I

HARRICANA RIVER MINING CORPORATION INC.

HARRICANA MINE PROJECT - AUR AREA 'A' OPTION SECTION 10+00 EAST - LOOKING DUE WEST

LEGEND KIAN A. J N • EN � OVERBURDEN co I J GRANODIORITE PRACTISING MEMBER y I I VOLCANICS 0558 I I SHEAR ZONE MOM AURIFEROUS ZONE 0.314 / 22.90 GOLD (OUNCES PER TON / FEET) NTARo

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. DATE REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30, 2004

Figure 17: Section 10+00 East, Aur Area `A' Option 72 ~ I I

ova" n

• • • • • d °a

9,500 9,500 _

ZONE No.3B 9,000 I 9,000 _ ZONE No.4A

ZONE No.4B

dl 3. a• ;I~ â• J

5 . w re Z ôlw m . fq 2 8,500 I 8,500 _ NW 4• m _

HARRICANA RIVER MINING CORPORATION INC.

HARRICANA MINE PROJECT - AUR AREA 'A' OPTION SECTION 12+00 EAST - LOOKING DUE WEST

LEGEND 0 KIAN A. N : EN OVERBURDEN CC- I I GRANODIORITE y PRACTISING MEMBER I I VOLCANICS 0558 I I SHEAR ZONE AURIFEROUS ZONE NTAR\ ° 0.314 / 22.90 GOLD (OUNCES PER TON I FEET) • ° •

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. DATE: REVISED: AUGUST B, 2003 200 0 200 400 MARCH 30, 2004

Figure 18: Section 12+00 East, Aur Area `A' Option 73

14.0 SAMPLING METHOD AND APPROACH

Core splitting was done by a percussion hand splitter with one half of the core left in the core box. Of the 1985 samples for this project, 52 samples were greater than 5.0 feet with the maximum footage of 8.5 feet, 210 samples were of a 5.0 foot length and 549 samples were less than 1.0 foot in length.

Of the 1985 original samples by Belmoral, a total of 154 samples or 7.75% were re-assayed of which 118 samples were greater than 0.005 opt gold. The author is not aware if the check assaying was completed on the pulps or the rejects from the original assaying done in-house at the Ferderber Mine assay lab. The author is not aware if any blanks or standards were submitted to either of the assay laboratories for quality control or quality assurance.

15.0 SAMPLING PREPARATION, ANALYSES AND SECURITY

KAJ did not observe first hand the sampling; assaying or security procedures employed at the Harricana Project and so cannot comment on them. Communications with Lan Vu, former chief geologist at Belmoral Mines Ltd. during the diamond drilling on what is now known as the Aur Area `A' Option, communicated the following: " Diamond drilling in the West Contact Zone (Lac Blouin) area has been performed under my supervision during 1988 and 1990. Cores were analysed in-house at the Ferderber mine and random high or low assays were verified through Bourlamaque Assay Laboratories Limited."

16.0 DATA VERIFICATION

The assays and geology for the surface diamond drill holes were input into the BORSURV Version V drill hole database management program.

The databases contained the available information regarding the geology and assay values from the surface drill holes. The system required the input of collar coordinates, northing, easting, elevation, dip and azimuth, along with the coded geological units and assay results. 74

It should be noted that the dollar value of gold in the mid 1930's was $ 35.00 per ounce. The assays for the historical data at the Harricana. Mine were quoted in a dollar value.

The author had created the diamond drill hole database in June 2002 for the purpose of generating diamond drill sections for presentation purposes. During the preparation of this NI 43-101 report, the author checked the database for any errors or emissions by verifying all assays, checking all unusual sample lengths, and drill hole coordinates. The author located 3 errors in the duplicate or check assay data and were considered by the author as low severity.

17.0 ADJACENT PROPERTIES

The following are summary descriptions of the various important mines within the vicinity of the Harricana Mine project. The following assist in describing the various geological setting and gold mineralization that may be potential targets of future exploration activities for the Harricana Mine project.

• KAJ have no relationship to and is independent to any of these companies.

• KAJ have not attempted to verify any of the information presented here.

• The information is not necessarily indicative of the mineralization on the Harricana Mine project.

17.1 Ferderber Mine

Historically, the mines surrounding the Bourlamaque Batholith have produced gold at considerably higher average grades than in the rest of the Val-d'Or district. According to a compilation by Mannard and Vu, in 1992, the total production in and at the periphery of the batholith is some 13.6M tons averaging 0.24 oz /ton Au compared to the 0.16 oz /ton Au average for the rest of the Val-d'Or camp.

The deposit generally strikes ENE and dip steeply to the south. The host rock is wide, highly fissile with abundant fault gouges. A blocky cleavage pattern and moderate to strong rusty 75

colour alteration due to hematization characterize the hanging wall. Anastomosing shears are present but rarely host economic grade mineralization. Randomly plunging ore shoots characterize the deposit.

Gold is associated with quartz-tourmaline veining containing mostly pyrite and chalcopyrite. The sulphides are found as stringers within the veins and/or shear zone but many locally form blebs or patches within the vein. Multiple parallel quartz-tourmaline veins are common within the shear zone and gold mineralization can be found in any or all the veins.

At the Ferderber mine, a total of 1,877,704 tons (short) of ore averaging 0.201 oz/ton Au was produced since the opening of the mine in February 1979. Production came from 74 stopes (as of December 1, 1994) developed over nine (9) levels along three (3) principal structures, the Ferderber vein being the main orebody. Underground development covers a total lateral extend of 7600 feet. The orebodies can be accessed via a 3300 foot inclined ramp to a depth of 560 feet and a 1300 foot vertical shaft located east of the ramp.

The total average mining cost at Ferderber Mine, based on the February 1994 Monthly Production Report, was estimated at $71 per ton.

Over 15 years of operation at Ferderber, gold recovery from the mill averaged nearly 95% for a total of 362,000 oz of gold.

17.2 Sigma-Lamaque Mine The following summary was obtained from the McWatters website: "The Sigma-Lamaque Complex is located at the eastern limit of Val—d'Or in north- - western Quebec. Gold was first discovered at the Sigma underground mine in 1933 with the first production beginning 1937. The Lamaque underground mine was discovered in 1923 and the first production occurred in 1935.

The Sigma-Lamaque Complex is the largest of a group of shear-zone related quartz- tourmaline vein deposits occurring north of the Cadillac, Tectonic Zone. The deposit 76

consists of an extensive vein network hosted by andesitic flows and volcaniclastic rocks, intruded by an irregular mass of subvolcanic porphyritic diorite. A swarm of high-level feldspar porphyry dykes, striking east-west and dipping steeply to the south, overprints both rock types, and is in turn locally cut by steeply plunging non- porphyritic diorite-tonalite stocks.

All intrusive rocks are overprinted by conjugate reverse-oblique shear zones, striking east west and dipping moderately to steeply north or south, with which the mineralized veins are associated.

The auriferous vein network extends over an area of 2 x 1.5 km on surface and to a depth of 1.8 km. It consists of laminated veins within extending shear zones, locally accompanied by jigsaw pn771e breccias, of sub horizontal extensional veins laterally away from shear zones into lower strain rocks, and of stacked extensional veins within competent intrusive rocks, locally grading into stockwork zones. Zoned alteration halos generally extend up to several metres away from the veins and consist of progressive carbonatization, sericitization, pyritization and local albitization; pyritized wall rocks commonly carry ore-grade gold concentrations.

Quartz veins commonly contain locally abundant tourmaline, lesser pyrite and gold, and minor pyrrhotite and chalcopyrite. Gold is predominantly in the native form and occurs as individual grains, coarse aggregates and seams. These minerals also occur within altered wallrock where gold is related to the second phase of hydrothermal alteration. The gold is associated with thin quartz and quartz-tourmaline veinlets, wispy fractures, and sulphide grains and occurs as disseminations, coatings and fracture fillings within secondary pyrite, pyrrhotite and chalcopyrite.

Since their start-up, the Sigma. and Lamaque underground mines have produced approximately 9,000,000 ounces of gold. Nearly 27,000,000 tonnes of ore at an average grade of 5.49 g/t Au have been extracted from the Sigma underground mine. 77

Until it's closing in 1985 by the former owner, the Lamaque underground mine had yielded historic production of 26,600,000 tonnes of ore at an average grade of 6.17 g/t Au.

McWatters and its partner SOQUEM have started development of the Sigma-Lamaque open pit mine. McWatters has a 60% interest in Sigma.-Lamaque and will operate the mine. Sigma-Lamaque is planned to produce an average of 150,000 ounces of gold per year once full production is reached in the second half of 2003, at cash costs of US$165 per ounce and total costs, including capital, of US$212 per ounce. Starting during the fourth quarter of 2002 and to the end of 2008, a total of 856,000 ounces of gold are expected to be produced."

17.3 Kiena Mine The following summary was obtained from McWatters website: "Gold was first discovered on the property in the early 1920s. After the blind discovery of the North Zone (5.25 g/t Au 9.5 metres), funding was made available to sink the first 139 metre deep shaft on the property. Operations continued from 1936 to 1939, but were then suspended due to the outbreak of World War II, which resulted in a shortage of manpower and funds. Exploration drilling resumed in 1961 and intersected a major gold zone grading 7.7 g/t Au named the 5-50 Zone. By 1965, a total of 2,500,000 tonnes grading 7.9 g/t Au had been outlined, but poor ground conditions hindered early attempts to develop the ore body. By 1979, technological progress and rising gold prices made it possible to raise sufficient funds to complete the development of a 400 metre shaft and production started in 1981 and was expanded to 2,000 tpd in 2000.

The Kiena Mine, which entered production in 1981 and operated continuously until it was shut down in September 2002, produced a total of 1.56 million ounces of gold from 10.7 million tonnes of ore grading an average 4.8 g/t Au. The elevation of the shaft bottom is 922 metres below surface, however an internal ramp extends to a depth 78

of 959 metres. Mining methods include 45% primary long hole (back-filled), 35% secondary long hole (back-filled), 15% sub-level retreat, and 5% mechanized cut and fill. As of December 2001, the mine production was around 2,000 tonnes per day. Mine put on care and maintenance in the third quarter of 2002."

17.4 Northern Abitibi Mining Corporation

The former mining claims of Northern Abitibi Corporation was adjacent to the north property boundary of the Aur Area `A' Option reported in their 1989 Annual Report several intersections in NA89-02 of 1.08 opt gold over 1.25 metres (4.1 feet) and NA89-03 of 0.21 opt gold over 2.0 metres (6.56 feet) and are shown on Sections 4+00 East to 10+00 East.

18.0 MINERAL PROCESSING AND METALLURGICAL TESTING

No mineral processing and or metallurgical testing have been carried out on samples from the Harricana Mine project.

19.0 MINERAL RESOURCE AND MINERAL RESERVE ESTIMATES

19.1 DEFINITIONS

Mineral Resource: A Mineral Resource is a concentration or occurrence of natural, solid, inorganic or fossilized organic material in or on the Earth's crust in such form and quantity and of such a grade or quality that it has reasonable prospects for economic extraction. The location, quantity, grade, geological characteristics and continuity of a Mineral Resource are known, estimated or interpreted from specific geological evidence and knowledge.

Mineral Resources are sub-divided, in order of increasing geological confidence, into Inferred, Indicated and Measured categories. An Inferred Mineral Resource has a lower level of confidence than that applied to an Indicated Mineral Resource. An Indicated Mineral Resource has a higher level of confidence than an Inferred Mineral Resource but has a lower level of confidence than a Measured Mineral Resource. 79

Inferred Mineral Resource: An `Inferred Mineral Resource' is that part of a Mineral Resource for which quantity and grade or quality can be estimated on the basis of geological evidence and limited sampling and reasonably assumed, but not verified, geological and grade continuity. The estimate is based on limited information and sampling gathered through appropriate techniques from locations such as outcrops, trenches, pits, workings and drill holes.

Indicated Mineral Resource: An `Indicated Mineral Resource' is that part of a Mineral Resource for which quantity, grade or quality, densities, shape and physical characteristics, can be estimated with a level of confidence sufficient to allow the appropriate application of technical and economic parameters, to support mine planning and evaluation of the economic viability of the deposit. The estimate is based on detailed and reliable exploration and testing information gathered through appropriate techniques from locations such as outcrops, trenches, pits, workings and drill holes that are spaced closely enough for geological and grade continuity to be reasonably assumed.

Measured Mineral Resource: A `Measured Mineral Resource' is that part of a Mineral Resource for which quantity, grade or quality, densities, shape, physical characteristics are so well established that they can be estimated with confidence sufficient to allow the appropriate application of technical and economic parameters, to support production planning and evaluation of the economic viability of the deposit. The estimate is based on detailed and reliable exploration, sampling and testing information gathered through appropriate techniques from locations such as outcrops, trenches, pits, workings and drill holes that are spaced closely enough to confirm both geological and grade continuity.

Mineral Reserve: A Mineral Reserve is the economically mineable part of a Measured or Indicated Mineral Resource demonstrated by at least a Preliminary Feasibility Study. This Study must include adequate information on mining, processing, metallurgical, economic and other relevant factors that demonstrate, at the time of reporting, that economic extraction can be justified. A _ Mineral Reserve includes diluting materials and allowances for losses that may occur when the material is mined.

Mineral Reserves are sub-divided in order of increasing confidence into Probable Mineral Reserves and Proven Mineral Reserves. A Probable Mineral Reserve has a lower level of confidence than a Proven Mineral Reserve.

Probable Mineral Reserve: A `Probable Mineral Reserve' is the economically mineable part of an Indicated, and in some circumstances a Measured Mineral Resource demonstrated by at least a Preliminary Feasibility Study. This Study must include adequate information on mining, processing, metallurgical, economic, and other relevant factors that demonstrate, at the time of reporting, that economic extraction can be justified.

Proven Mineral Reserve: A `Proven Mineral Reserve' is the economically mineable part of a Measured Mineral Resource demonstrated by at least a Preliminary Feasibility Study. This Study must include adequate information on mining, processing, metallurgical, economic, and other relevant factors that demonstrate, at the time of reporting, that economic extraction is justified. 81

19.2 DATABASE

The author originally created the database in June 2002 in Excel, which was exported in the form of ACSII database. This database was imported into the BORSURV diamond drill hole management program. During the commission of this NI 43-101 report, the author checked all assay information and found it to be relatively error free and suitable for the mineral resource estimation (see Section 16.0 entitled Data Verification).

19.3 GEOLOGICAL INTERPRETATION

The author compiled stacked drill sections for the interpretation and attitude of the gold bearing intersections and grouped the results into several independent zones after verifying the geology, composition and alteration. The majority of the zones are confined to chloritic and carbonated shear zones with stringers, veinlets and veins of quartz with or without tourmaline and disseminated to massive blebs of sulphides, usually pyrite. The shear zones are not solely confined to the granodiorite and may extend into the overlying volcanics.

The shear zones trend approximately east west and dip either vertical (Quartz Zone), -45° dipping northwards (North Shear, Zone 1), and 25° dipping northwards (Zones 2, 3A, 3B, 4A and 4B).

The author completed the original set of drill sections for the company in June 2002 for presentation purposes, which were later revised in June and July 2003.

19.4 ESTIMATION METHODOLOGY AND PARAMETERS

KAJ employed a 2-D polygonal method for the resource estimate. The first estimate was completed in June and July 2003 and revised August 8, 2003. The 2-D models were constructed as a series of nine longitudinals, 1 vertical and 8 inclined either at -25°, -45 ° or -65 °, one for each zone. The inclined calculated polygons were projected to a horizontal plane. The near surface polygons were trimmed at the bedrock and overburden interface and that portion excluded from the resource estimate. A similar process was completed for the zones, which intersected the South Shear Zone and the north property boundary

The radii of the polygons used in the resource estimates were 100 feet and 200 feet from the zones pierce point on the longitudinals.

The resource estimations used the uncut assays and were subjected to a series of cut-off grades, which were 0.03 opt, 0.05 opt and 0.075 opt gold. KAJ acknowledges that the use of a cutting factor at the early stage of a project is inexact and involves a certain degree of — subjectivity. KAJ recommends that with the proposed additional sampling, increased duplicate sampling, the recommended density determinations and the recommended in-fill diamond drilling, a cutting factor would be more appropriate at that time.

As no density determinations were conducted, the author utilized a tonnage factor of 12 cubic feet per ton.

19.5 STATISTICS

The statistics for all the uncut samples greater than 0.005 opt gold for the Aur Area `A' Option are listed in Table 10. Of the 625 raw assays greater than 0.005 opt gold, only 7 assays are greater than 1.0 opt gold. Table 11 lists the correlation coefficient between the 118 original assay value greater than 0.005 opt gold and those of the check or duplicate assay value. Table 12 lists the statistics on all assays within each of the zone boundaries.

Figure 19 illustrates the scatter diagram of the original and duplicate assay values from the 118 samples greater than 0.005 opt gold. The top diagram is missing the single comparison of 8.16 and 8.02 opt gold assay.

A total of 40.2% of the 82 assays equal to or less than 0.10 opt gold yielded higher values on the check assaying with the most severe differences of+0.12 opt (B88-55 from 731.2 to 732.9 feet) and —0.02 opt in 10 intersections. 83

A total of 44.8% of the 29 assays greater than 0.10 opt to 1.0 opt gold yielded higher values on the check assaying with the most severe differences of +0.18 opt (B88-54 from 862.6 to 863.3 feet) and —0.44 opt (B90-10 from 384.4 to 384.9 feet).

A total of 57.1% of the 7 assays greater than 1.0 opt gold yielded higher values on the check assaying with the most severe differences of +0.18 opt (B88-55 from 939.7 to 940.5 feet) and —0.50 opt in (B88-56 from 497.9 to 498.7 feet). 84

Table 10: Statistics of 625 Raw Assays Greater than 0.005 opt Gold

Mean 0.097 Minimum 0.005 Maximum 8.160 Standard Deviation 0.437 95.0 Percentile 0.318 97.5 Percentile 0.819 99.0 Percentile 1.637 Mean at 89.18%

Table 11: Correlation Coefficient between the Original Assay and the Check Assay for the Gold Bearing Zones at the Aur Area `A' Option.

118 pairs of Original Assay Check Assay (opt) samples (opt) Mean (opt) 0.251 0.248 Standard 0.841 0.824 Deviation Maximum 8.160 8.020 (opt)

Table 12: Frequency Distribution and Cumulative Frequency Distribution of Uncut Assays for Each Gold Bearing Zones at the Aur Area `A' Option.

Aur Area 'A' Number of Maximum Mean Standard 95 97.5 99 Mean at Zone Name Assays Assay (opt) Deviation Percentile Percentile Percentile Percentile (opt) (opt) at (opt) at (opt) at (opt) (%) North Shear 91 8.160 0.133 0.872 0.198 0.422 5.200 93.040 Quartz Vein 22 0.410 0.098 0.117 0.340 0.395 0.428 79.230 Zone 1 9 0.640 0.156 0.235 0.605 0.628 0.641 77.780 Zone 2 53 1.940 0.112 0.292 0.467 0.534 1.897 83.690 Zone 3A 31 3.940 0.365 0.887 2.495 3.873 3.919 87.100 Zone 3B 66 1.700 0.126 0.318 0.835 1.185 1.584 84.900 Zone 4A 57 2.380 0.154 0.408 0.965 1.407 2.293 86.120 Zone 4B 28 1.260 0.118 0.247 0.310 1.180 1.222 79.980 South Shear 59 0.140 0.009 0.022 0.047 0.049 0.091 58.350 All assays of 625 8.160 0.097 0.437 0.318 0.819 1.637 89.100 all Zones Combined 85

2.5 ♦

♦ ô 2 b ô C7 ♦ >,Vi H 1.5 Q ♦♦ iu ♦ _• A 1 • ♦ ♦ ♦ 0.5 ♦

♦ `♦ ♦

0 0 5 1 15 2 25 3 Original Assays Gold (opt)

I ♦ 0.9

0.8

â 0.7 © ♦ 0.6 ♦ C~ (A ♦ HV 0.5 d :3 ♦ ~ 0.4 ♦ â Â 0.3 ♦ ♦ ♦ Z ♦ ♦ 0.2 $: ♦♦♦♦ 0.1 dot' ♦ ~♦ ♦ 0 ♦• 0 O1 02 03 04 05 O6 07 O8 09 Original Assays Gold (opt)

Figure 19: Scatter Diagram of the 118 Duplicate Samples with Gold Values Greater than 0.005 opt. Note top diagram missing the 8 opt Gold sample. 86

19.6 RESOURCE CLASSIFICATION The longitudinal projections are illustrated in Figures 20 to 28 for the Quartz Vein, North Shear Zone Vertical, North Shear Zone Horizontal, Zone No.1, Zone No.2, Zone 3A, Zone 3B, Zone 4A and Zone 4B, respectively, and the calculations are listed in Appendix I to P. The inferred resource estimation for the Aur Area `A' Option is listed in Table 13 by zones using a cut-off grade of 0.030, 0.050 and 0.075 opt gold. The author has classified the resources as Inferred Resources based upon several factors. • Numerous intersections were only partially sampled and these were excluded from the resource estimate. • Individual zones projected from one section to another section may project through a section of a drill hole, which was not sampled. The author did not substitute a 0.00 opt grade to limit the area of the polygons. The author examined the drill core for several of these projections and found weak to moderate alteration, weak to moderate development of foliation/shearing, traces to 1% to 2% disseminated pyrite and/or quartz stringers. • The density determinations, a vital component for the resources calculations was missing, and the author recommends that during the proposed additional sampling, the assay laboratory perform a suite of density calculations from either the lh or 1/4 split drill core. • The low number and percentage of duplicate assays, 118 samples greater than 0.005 opt gold out of a total of 625 samples with values greater than 0.005 opt gold or 154 samples out of total assay data set of 1985 samples which is 7.76%. A total of 8 intersections were sampled but did not have any recorded assay results. A standard for gold exploration is to re-assay samples which are greater than 0.05 opt gold from the rejects, which would also assist in the determination of any nugget effect. • The drill hole spacing of approximately 200 feet does not support the confidence level of geological control and gold assay value continuity. KAJ recommends infill diamond drilling. 87

Ÿ r

WEST : EAST

ELEVATION ELEVATION (FEET) (FEET)

10 000 10 000

9.800 ~.

9,700 9,700

9,600 - 9,60D

9.500 - / - 9.500

/ 0.028 \ \ -:•.0.028 '... ) \\ 9.80 9400 - / .9.400

\______

/ \ 9 300 / 3 \>_, 9 300 i 88&55 \\\ • 0.118 14.70

9 200 / \\ - 9 200 / \ ` / 88&77 \ • 0.168 \ \ 12.50 9100 - 9100 \\` /

9.000 9.000

8900 - 8.900

8 800 8.800

8,700 - 8700

3 8 S $ o m3 '67', • 7. COLOUR CODE FOR 100 FOOT AND 200 FOOT POLYGONS / 0.00 to 0.03 opt Au ( 0.03 to 0.05 opt Au O 0.05 to 0.075 opt AuO 0.075 to 0.10 opt Au (r....\\ 0.10 to 0.25 opt Au 0.25 to 0.50 opt Au O

HARRICANA RIVER MINING LEGEND A L G CORPORATION INC. N C) • CENTRE OF ZONE WITH ASSAYS 888-54 HARRICANA MINE PROJECT DRILL HOLE NUMBER CD C. 0.447 AUR AREA 'A' OPTION GRADE(optAu) Co ~ ~ 13.79 VERTICAL WIDTH (ft) + CENTRE OF ZONE NOT SAMPLED LL ' Z QUARTZ VEIN ZONE N/S ZONE NOT SAMPLED PAS ZONE PARTIALLY SAMPLED /KIAN A. - ENS ' LOOKING DUE NORTH EOH END OF HOLE BEFORE ZONE INTERSECTED PRACTISING ME ' BER y INCLINED POLYGONALS PROJECTED TOAVERTICAL PLANE PROPERTY BOUNDARY • 0558 •

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. N T A R DATE: REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30, 2004

Figure 20: Zone Quartz Vein Vertical Polygonal Longitudinal, Aur Area `A' Option

o A A Ÿ

. .. . ~ .~ WEST .. . ~ ~ . ~ ... ..EAST .

ELEVATION ~ ~ ~ ELEVATION (FEET) (FEET)

10 000 10,000

. ~ ♦ ~~ 9.800 B8851 . . \ \ I i~~ . /~: • 0.066 / / • \\ ~ 6.93 / ~ ~ B88-28 \\ \\ ~/ ~• 0.006 / ~B88-73~ •\ / \ \ 1032 : ~/ ~ ~0.002 ~ \\ / ~ \\ . . . . . . ~ . . / .\ i I \ / / \ .. ~700. ~ ~/ . . . • 1598::. .. ~ ~ 9700 . . / ..\ ______/ .\ \ ' \ . .. '.~~~ ~ .~.BB&79.\ . ... . . / \\ . . . ~ ,. ~\ \ ~~ 0.000 . . . i ~ B90-11 \\ . \ / \ ~ \ / ~- .B8830 \\ ~: B88 68 \\ \ . ~.12.44 ~ • 0.008 • B88-31 ~~ ~ .B8831 \ / • :OA00 ~ \ \ ~ ~ ~0.002 \ ~/ ~ . • ~ • 24.75 • ARILLED ~~ ~~ 0.015 • /• ~~ • ~ 2.97 / - 29.56~~ \ g600 ~ i / DOWN DIP ~ 10.47 \\\ \ ~ ~ / . . / I \ . ~ / . 9600 B8885 .~B8g65 ` ~ / / \\ P/8 / . . . / i \\ ~ • B88d9 \ :.0.000 ~ / . \ ~ /1 . \ ~ 0.019 \ -~~ 6.08 ~ . . ~ / ~ . . \\\ 976 ~ 1 \ i/ / 588-53 \\\ i/ l ' / ~ 'I;G> : ';) 9.500 ~ . .\ ': • 0.002 ~ : \\\ i - 9.500 . . • .39.60.

. i / ~ / / ~ 888-62 \ \ \ \\\ .:~ B8B64 \ / -~~ ~\\ ~ '.BB&58~ \\ B88.62 0.000 \\ . ., .~. I • 0.015 \\ ~ $B8B80 \\ 88858 ..• \-______/ / ( / 0.000 ~ \ WS ; PiS • 10.04 / /` . ~\ . ~~ - 18.95 ~ PIS ~ . \ . ..25.74 ~ i 9,400 ~ \\ . 9.400 / ------. . \ \ \\ - - -e-B88-61 . i/ 888-55 • \ ~ S•\ \ \ . • \\1 . .0.026. / B88¢9~ / . ~^ N5 . . ~ \ \\. / \ / ..\ \\ ~. 8 63 ~ i / ~ 0.098 .. ~ 888-77{1. . \\ ~'. i ~ 976 ~ i . N/S '008003 ~~ \\ . . . . ~ . . ~ : .. 9.300 ~ . ~ . ` / / • <16.40 ~:~ ~\/ . . . ~.9.300 NORTH ~ NORTH' - \ ~ ~ _~~~~ ' ~ ~ ~ \ BOUNDARY BOUNDARY - NORTHORTH ~ / \\ i/ ~ NORTH . ~ $, BOUNDnRY~~ \ ~ ~ ~ ~~ ~ ~ ~ ~ ~ $BOUNDARY NORTH BOUNDARY . ~ ~ ~ ~ 9,200 . ~ ~ ~ . ' ~ .. ~~ ~ 9,200 NORTH . . 9 . . . . ... . ~ ~. BOUNDARY ~ NORTH BOUNDARY . .. ~ .. . .

. .. .. . . .. . . .. . . . . , 9,100 .. .. . . . . ~ ~ . . . . . . ~..9.100

. . . . ~ 9,000 . . 9.000

. . . _ . . . . . ~ . . . . . .. . .. 8,900 ~ ~ ~ ~ - . ... . . . ~ . 8.900

8,800 ~ . . ~ ~ . ~ ~ ~ 8800

... . . ~ . . ~ . ~ ~ . ~ . . ~ ~ . ~ . ~ . : . ~. . . ~ . .. ~ 8709 ~ . . 8 700 . $ ~ .. m ! m A Y COLOUR CODE FOR 100 FOOT AND 200 FOOT POLYGONS / 0.00 to 0.03 opt Au ( 0.03 to 0.05 opt Au O 0.05 to 0.075 opt Au 0.075 to 0.10 opt Au 0.10 to 0.25 opt Au 0.25 to 0.50 opt Au O O

HARRICANA RIVER MINING LEGEND CORPORATION INC. N P L G F O • CENTRE OF ZONE WITH ASSAYS ~ HARRICANA MINE PROJECT B88-~ DRILL HOLE NUMBER g ~ ~ ~C~ 0.447 AURAREA'A'OPTION GRADE (optAu) Co / ~ 13.79 VERTICAL WIDTH (ft) W [ ~ + CENTRE OF ZONE NOT SAMPLED LL N/S ZONE NOT SAMPLED ZONE NORTH SHEAR 0 • P/S ZONE PARTIALLY SAMPLED KIAN A. JE }E'EN LOOKING DUE NORTH EOH CL END OF HOLE BEFORE ZONE INTERSECTED pRACTISING lifEMBER ~ INCLINED POLYGONALS PROJECTED TO A VERTICAL PLANE PROPERTY BOUNDARY y ~ • 0558 •

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. O N 7' A R \ ~ DATE: REVISED: AUGUST 8, 2003

200 D 200 qoo MARCH 30, 2004

Figure 21: Zone North Shear Vertical Polygonal Longitudinal, Aur Area `A' Option

3 S m S 8 S 8 8 °!.' e m

3+OON 3+00N

2+00N O 2+OON

1+OON I 1+OON

PROPERTY B DUNDARY PROPERTY BOUNDARY

g % ' • 0.026 1 / _ \ 8.63 -' 88868 -:~\ B8N/S 77 \\ i/ \ •\ \ / t • 0.098 \\ 9.76 -// \\ 1+DOS / 688-63 • B88-63 \~`. / \ 1+00S /~ \ P/S 0.000 \ / 088.81 \ \• - 16.40 \\\ /~ \\ \ \\ / 9 P/S 888b2 ..: \\ / / / 888-54 \ • 0000 \\ / 00023 . 0.015 \1 \\ 10.04 / •\ 18.95 j / / \ 2+00S • 39.60 / `\\ MI 2+00S \\\\ \\ • B88-58. • 888-58 • 888-60 i 0.000 / \ /P/S\\\ • N/S \\ 2574 j a \L \\L / B88-31 B88-31 \ /SRILLED 0.015 \ \~ t 3+00S / /DOWN DIP • 1047 \ 4 % 88865. \ 3+00S / • B88-49 • ) .j / BBBb5 0000 ~\ ({v (\ 1 \\ • - 0.019 , P!S • 6.08 \\ •\\ 976 . •;/ \\\ \\\ , ... ,... 888-68 \\ \\\ % / • 0 081 / / ,/ /~-B88-68 24.75 • \\ / P/S 9'999 • \\ • • 29 56 i / \\\ 4+005 / B88-79 • 4+00S tl88S1 \\\ \ // / / / I--- '--- \, (/ 88830 B88-30 \\ • B88.73 ,• 0.000 , \ i 88873 • \ •0 066 i ~\ • P/S • 0.002 / \\ P/S 0.002 \\ 12.44 / ` \ 6.93 / \\ 2.97 /• 15.98 / / \ \ / 888-28 \\ • 0006 \ / ♦ \\- / 5+005 -. \PŸI \ / • ______... ATSX \ 10.32

6+00S 6+00S 890-12 OVERSHOT B90-9 OVERSHOT ZONE 6 ZONE

7+00S - 7+00S

8+00S 8+00S

9+00S 9+00S

10+005 _ _ 10+00S

11+00S 11+00S

3 3 3 8 8 8 tri e re m m P.

COLOUR CODE FOR 100 FOOT AND 200 FOOT POLYGONS ~I 0.00 to 0.03 opt Au( 0 0.03 to 0.05 opt Au O 0.05 to 0.075 opt Au 0.075 to 0.10 opt Au 0.10 to 0.25 opt Au ', 0.25 to 0.50 opt Au O O

HARRICANA RIVER MINING LEGEND CORPORATION INC. N p L G • CENTRE OF ZONE WITH ASSAYS O S 888-54 • HARRICANA MINE PROJECT DRILL HOLE NUMBER CO ^ 0.447 i •e" ... AUR AREA 'A' OPTION GRADE (opt Au) 13.79 VERTICAL WIDTH (k) IL 'l 4 - CENTRE OF ZONE NOT SAMPLED LL A Z ZONE NORTH SHEAR N/S ZONE NOT SAMPLED ✓ —I P/S ZONE PARTIALLY SAMPLED N A. J ' BEN EOH END OF HOLE BEFORE ZONE INTERSECTED d y INCLINED POLYGONALS PROJECTED TO A HORIZONTAL PLANE PROPERTY BOUNDARY d PRACTISING MBER y 0558 SCALE IN FEET • O O • COMPILED BY: K.A. JENSEN, P.Geo. I~ T A R \~ ! f DATE: REVISED: AUGUST 8, 2003 ..0 200 0 200 400 MARCH 30, 2004

Figure 22: Zone North Shear Horizontal Polygonal Longitudinal, Aur Area `A' Option 90

S $ $ Ÿ S 8 8 8 8 8 8 S q

3+00N 3+00N 4

O 2+00N 2+00N

1+00N 1+00N

PROPERTY B 3UNDARY PROPERTY BOUNDARY

1+00S 1+00S

2+00S 2+00S

3+00S 3+00S

4+00S 4+00S

5+00S 5+00S

SOUTH SOUTH BBBEB SHEAR SHEAR ~EOH 6+00S 6+00S ? 1388-30 -ED-

890-9 EOH i „`\~ -1, j 88&73..;~~ 7+00S 7+00S s 9.05

8+00S / 8+00S B88-76 690-10 \ \ \ 9. N5 0.099 4.30

9+00S 9+00S

\\ i/

/ B90-13 \ " 10+005 ~~ 0.156 / 10+00S 3.03

11+00S 11+00S

3 Q $ 2y $ $ $ $ $ $ $ $ $ S N i .j f:

COLOUR CODE FOR 100 FOOTAND 200 FOOT POLYGONS / O 0.00 to 0.03 opt Au (~ 0.03 to 0.05 opt Au O 0.05 to 0.075 opt Au ( 0.075 to 0.10 opt Au 0.10 to 0.25 opt Au - 0.25 to 0.50 opt Au

HARRICANA RIVER MINING \ LEGEND N p L G F CORPORATION INC. o~ • CENTRE OF ZONE WITH ASSAYS \O , HARRICANA MINE PROJECT B88-54 DRILL HOLE NUMBER 0.447 GRADE (opt ID CO ! "WI / ` AUR AREA 'A' OPTION 13.79 VERTICAL WIDTH (ft) W ~ 4- CENTRE OF ZONE NOT SAMPLED ZONE No. 1 WS ZONE NOT SAMPLED 0 • ~ P!S ZONE PARTIALLY SAMPLED KIAN A. N ` N 07 EOH END OF HOLE BEFORE ZONE INTERSECTED d INCLINED POLYGONALS PROJECTED TO A HORIZONTAL PLANE PROPERTY BOUNDARY PRACTISING MEMBER Y • 0558 • SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. N T A R0 DATE: REVISED: AUGUST 8, 2003 MARCH 30, 2004 200 0 200 400

Figure 23: Zone No. l Horizontal Polygonal Longitudinal, Aur Area `A' Option

0+ s g s g g g s â

3+00N 3+OON 4

2+00N O 2+OON

1+OON 1+O0N

PROPERTY NDARY ■■■ ■■■ PROPERTY: OUNDARY 888-77 i B8855 ~ / • 0.022 • 0.043 \ / 1 81 7.94 / `~\ B8859 / 888-59 0.000 u 1+00S / / I • P/S • 77.03 \` ■■■■ 7+005 ___• r~~ \ • NE 888-81 2+00S ■ ~ / / / 0.1693 \,~~, ``` :: 98&54 / — — ' — — — ■ 2+00S • ‘011 68 07 CONTACT i ~~ B. _COL~ \\,'• u 8940 9`///` ``• j / ` `~// 3+OOS / ~~. 3+005 88851 / \ rs Imo/ S NOTS \ 0.106 ------§ / 750 I i\ II / 888-56 \~ ♦_ _ _ _ BBB86 0.000 El `\~\ i 888-28 `\ P/S 9.93 4 00 —_ —_— 0.137 \• 4 00 / ~\ / _ _ _ _ _` 880-17 '... ~______/ 4.97 / ` P/S ~ i

\\ i I/ B88-79 `\ / +\ ♦__ __/ / 96&79 0.003 \ 5+00S / 888-83 ~ , 1 P/S 8.05 / 5+00S __ ___~ 8 1 \ P/S .c 0.33. ~, / 111 PLTE- TION ~ \ , NOTS LIPLEDI// VOLCANIC \ / j 88837 ~ 88830 6+00S CONTACT ,.. ,, -.,. /98837 ?i x ) : SO 6+00S P/S 10.37 SWTH sSOUTH SHEAR SHEAR ` i/ \SOUTH SWTH i/ SHEAR ' SHEAR ______SOUTH :: SHEAR 7+005 7 00 SHEAR

8+005 ■■■■■■ ■■■■ ■■■■ 8+00S

9+00S 9+005

10+00S 10+00S

11 00S 11+00S

s s N s s $ s $ s s ct 41 ! 8 a

COLOUR CODE FOR 100 FOOTAND 200 FOOT POLYGONS O 0.00 to 0.03 opt AuK ( /• 0.03 to 0.05 opt Au 0.05 to 0.075 opt Au ( 0.075 to 0.10 opt Au ®0.10 to 0.25 opt Au - 0.25 to 0.50 opt Au

HARRICANA RIVER MINING \ LEGEND CORPORATION INC. N P • CENTRE OF ZONE WITH ASSAYS `O L G O HARRICANA MINE PROJECT 888-54 DRILL HOLE NUMBER Gj ~0 0.447 GRADE (opt Au) ~Ake e .••• AUR AREA 'A' OPTION 13.79 VERTICAL WIDTH (ft) W"eh / 0 # CENTRE OF ZONE NOT SAMPLED LL Z i ZONE No. 2 N/S ZONE NOT SAMPLED O / .ate. - rl P/S ZONE PARTIALLY SAMPLED KIAN A:J '• EN - EOH END OF HOLE BEFORE ZONE INTERSECTED d ti INCLINED POLYGONALS PROJECTED TO A HORIZONTAL PLANE PROPERTY BOUNDARY tY PRACTISING MEMBER Y • 0558 •

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. N T A R ‘ O DATE: REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30, 2004

Figure 24: Zone No.2 Horizontal Polygonal Longitudinal, Aur Area `A' Option

3 "' 8 8 8 8 ! it l'

3.00N 3.00N 4

2+00N O 2.00N

1+00N 1+00N

PROPERTY B]UNDARY PROPERTY•OUNDARY _. _ _.. \ B88-55 888-77 • 0.384 WS 5.96 -e-ws 59'.. 1+00S • \ 1+OOS 5 B8883 , 1 + P/S %

,~)'' '' $ 888.81 888-53 / e VOLCry.IC / 1., 2+00S WS rnurnnl / 888-54 S8g`~ 2+00S . 0.691 ,/ P/S e 68882 - B88-49 `5 • 13.79 NS /• 0.264 ‘ / 888-58 5~ 12.25 i 9 NIS 888- ~ __ ___, B••.^ 3+00S N/S S ` 3+00S

,888-28~ - _ - 888-56 \\• 4+00S - 888-56 0.00 ' 4+00S NS 9.21 890-11 4 88885 N5 DNS SOUTH / $ SHEAR ` / S+OOS `79 S+OOS SOUTH 88&79 7 688.6, 988-79, Z. SHEAR 0.000 BBBA3 1 P/S 8.81 EOH WS 8 888-37 SOUTH / / P/S SHEAR SOUTH `5~ i 8.005 SHEAR / 6+005 ____ SOUTH SOUTH SHEAR SHEAR 88830 SOUTH 8 OVER SHOT SHEAR 7+00S 7+00S

8+00S BOOS

9+00S 9+00S

10+00S 10+00S

11+00S 11+005

s S $ S ô 8 s

COLOUR CODE FOR 100 FOOT AND 200 FOOT POLYGONS / O 0.00 to 0.03 opt Au ( ® 0.03 to 0.05 opt Au O 0.05 to 0.075 opt Au ( ~ 0.075 to 0.10 opt Au ® 0.10 to 0.25 opt Au - 0.25 to 0.50 opt Au

HARRICANA RIVER MINING \ LEGEND p L G E CORPORATION INC. N CENTRE OF ZONE WITH ASSAYS ~O S HARRICANA MINE PROJECT B88"54 DRILL HOLE NUMBER 0.447 GRADE (opt Au) q AUR AREA 'A' OPTION 13.79 0 VERTICAL WIDTH (ft) W / Z -* ENTRE OF ZONE NOT SAMPLED U. ~ , C ZONE 3A N/S ZONE NOT SAMPLED 0 _ P/S ZONE PARTIALLY SAMPLED KIAN A. É N EOH END OF HOLE BEFORE ZONE INTERSECTED Ce. INCLINED POLYGONALS PROJECTED TO A HORIZONTAL PLANE PROPERTY BOUNDARY PRACTISING M MBER Y • 0558 •

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. ON T A R N O I I DATE: REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30, 2004

Figure 25: Zone 3A Horizontal Polygonal Longitudinal, Aur Area `A' Option 93

3 S 8 ! •• S S 8 8 S

3+00N 3,00N

2+00N O 2+00N

1+00N 1+00N

PROPERTY BOUNDARY PROPERTY BOUNDARY

88855 +888- 77 $N85 WS • 1+00S 1 ,__ i+OOS F —.m : .. ..:...... ~. plc ~ 88853 i • .-.. 888- 63 • 0.014 ' ~1 'P/S 5.41 088-61 1 • Bfie-s1• Bee-s3. `:.;.... OA) 00 1 2+00S NS \1 ... B88.54 ~ , ~ P5 6 3_ 2+00S • ~138&62 ~ 88819 \ IS 51.82 • • ` WS 1' • 0.453 BM-58 1 10.26 `1 7 • 0.020 888-51 / / 14.23 5 3+00S N5 6 3+00S • 0.069 • 3.64 .. $888-28 `s / 4+005 - /, 888-56 888-58 • • _ _ _ _ 4+005 -- P/S 0.019 .G.890-11 5.52 .~_ WS 08855 888-65 • SOUTH 6. 7~ / / ~ P/S • 0.033 • SHEAR 1~~ 7 5.63 6+00S 5+00S • . • _ __ 888-83 SHEAR SOUTH 888-79 1 EOH SHEAR 888-68 ` • • 0.100 • 0.016 • {p~. • " 138837 SOUTH 10.26 ~• 5.96 SHEAR \ 6+00S P/S 1 / 6+00S SOUTH SOUTH $SHEAR SHEAR SHEAR 888-30 9 OVER SHOT

7+00S 7+00S

8+00S 8+005

9+00S 9+00S

10+00S 10+00S

11+00S 11+00S 3 8 8 8 S 8 S 8 8 8 8 8

COLOUR CODE FOR 100 FOOT AND 200 FOOT POLYGONS / O 0.00 to 0.03 opt Au ( ~ 0.03 to 0.05 opt Au O 0.05 to 0.075 opt Au 0, 0.075 to 0.10 opt Au 0.10 to 0.25 opt Au ®0.25 to 0.50 opt Au

HARRICANA RIVER MINING LEGEND CORPORATION INC. N P L G • CENTRE OF ZONE WITH ASSAYS 0 HARRICANA MINE PROJECT B88-54 DRILL HOLE NUMBER g ' ~• 0.447 GRADE (opt Au) AUR AREA 'A' OPTION 0) 13.79 VERTICAL WIDTH (ft) W , Z 4- CENTRE OF ZONE NOT SAMPLED N/S ZONE NOT SAMPLED v ZONE 3B _ P/S ZONE PARTIALLY SAMPLED KIAN A..IEN • N EOH END OF HOLE BEFORE ZONE INTERSECTED CL INCLINED POLYGONALS PROJECTED TO A HORIZONTAL PLANE PROPERTY BOUNDARY !y PRACTISING MEMBER Y 0558

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. • O N r A R‘ • DATE: REVISED: AUGUST 8, 2003 200 D 200 400 MARCH 30, 2004

Figure 26: Zone 3B Horizontal Polygonal Longitudinal, Aur Area `A' Option 94

8 8 8 8 Ÿ f

3+00N 3+00N

O 2+30N 2+00N

1+00N 1+00N

PROPERTY BOUNDARY PROPERTY B 3UNDARY \

688-7]7 \ B88-55 ' _ 888 776, 0.031 \ t • 0.070 , / PIS 17.99 5.52 / i ♦ 1♦00$ iOp$ / 08657 \ / / /______\ ` i • 0.000 / \ B88-63 \t / / 18.43 • 0.020 1 `11 6.07 / / / ~3

2+00S / , I, \~ / 0.0001 1 2+005 2.69 / g888L2 a WS 63 / 688-09 • 4~9 ~-\ 888-SC \t ~ \ \fit / F/S •3.09 • 0.128 888-58 `, / 1\ NIS 24.83 B88-53 • 0.056 / \1 3 ______2 B88.51 /~~ 1 P/S 796 3+003 N/$ `\~ / ~\ 3+00S ______2 B88-60 s. 11\ / • 0.022 + \ 4.52 /n 8888-28 % .~NI S " . 4+003 ~, 4+003 B90-11. NIS +18:-56 *sourH ws SHEAR B88-65 69611 N/S 5+00S S+ppS 0.023 SOUTH SHEAR 14.60 888-83 '9-SHEAR SHEAR -9 EOH SOUTH SOUTH -8- -e- SOUTH 88837#SHEAR SHEAR SOUTH 9 SHEAR 88688 SHEAR N/S 9 EOH 6+00S 6 +OOS

7+00S 7+00S

8+00S 8+00S

9+00S 9+00S

10+00S 10+005

11+00S 11+005

3 3 8 8 8 o gg 8 F 8 0 m .1..- m â 3

COLOUR CODE FOR 100 FOOT AND 200 FOOT POLYGONS

0.00 to 0.03 opt Au f s $ 0.03 to 0.05 opt Au O 0.05 to 0.075 opt Au 0.075 to 0.10 opt Au ~® 0.10 to 0.25 opt Au - 0.25 to 0.50 opt Au O O

HARRICANA RIVER MINING LEGEND N p L G F CORPORATION INC. • CENTRE OF ZONE WITH ASSAYS ~0 HARRICANA MINE PROJECT B88-54 DRILL HOLE NUMBER CO / ~0 0.447 ' GRADE (opt ID y Z AUR AREA 'A' OPTION 13.79 ~1: VERTICAL WIDTH (ft) W ~ 4- CENTRE OF ZONE NOT SAMPLED U. ZONE 4A N/S ZONE NOT SAMPLED 0 , s---~ -tom P/S ZONE PARTIALLY SAMPLED KIAN A. JE 'EN — EOH END OF HOLE BEFORE ZONE INTERSECTED d PRACTISINGMEMBER INCLINED POLYGONALS PROJECTED TO A HORIZONTAL PLANE PROPERTY BOUNDARY tY Y • 0558 • O O SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. N T A R \ DATE: REVISED: AUGUST 8, 2003 200 0 200 400 MARCH 30, 2004

Figure 27: Zone 4A Horizontal Polygonal Longitudinal, Aur Area `A' Option 95

g $

3+00N 3+00N

O 2+OON 2+00N

1+00N 1+00N

PROPERTY BOUNDARY PROPERTY BOUNDARY

" 888-55 \ EaN S ± N/S 1+00S 1+OOS \ 11 88869 1 7 ' • 0.053 88863 ~• 18.76 • '0.002 ~ 7 ~~ 10.92 ' B8861 11 2+00S / \ 7 i' 2+OOS BB6-53 i •. ..•• gN/S 4.68 , NB -e-r1 B8g84 \ • ______11 N5 • 0.217 / //' B88-51 9.71 9 888-58 WS $ N/S 3+00S r; % 3+OOS

X138860 6 888-28 N/S N/S 4+00S 4+00S

890-11 9 N/S SOUTH +ENT% SOUTH SHEAR N~ $SOUTH B8865 S+OOS 5+00S SP6pc aSHEAR 4,^OUTII 9(\IRR H N/S SHEAR 4 ~. 888-83 SOUTH EOH SOUTH SHEAR 4 SMEAR B8868 eEOH 6+00S 6+00S

7+00S 7+00S

8.005 8+00S

9+00S 9+00S

10+00S 10+00S

11+00S 11+00S

ç 8 . $ $ 8 8 r ! cr `! 4. m 8 ... COLOUR CODE FOR 100 FOOT AND 200 FOOT POLYGONS / \ 0.00 to 0.03 opt Au (_ 10.03 to 0.05 opt Au O 0.05 to 0.075 opt Au 0.075 to 0.10 opt Au 0.10 to 0.25 opt Au 0.25 to 0.50 opt Au O O

HARRICANA RIVER MINING LEGEND CORPORATION INC. O~ • CENTRE OF ZONE WITH ASSAYS Q ~ A L Gf HARRICANA MINE PROJECT B88-54 DRILL HOLE NUMBER CO ~,, O 0.447 GRADE (opt ID "It i AUR AREA 'A' OPTION 13]9 VERTICAL WIDTH (ft) W , ± CENTRE OF ZONE NOT SAMPLED Z N/S ZONE NOT SAMPLED ZONE 4B 0 411/ f P/S ZONE PARTIALLY SAMPLED KIAN A. EN — ce. ti EON END OF HOLE BEFORE ZONE INTERSECTED PRACTISING MEINBER INCLINED POLYGONALS PROJECTED TO A HORIZONTAL PLANE PROPERTY BOUNDARY • 0558 •

SCALE IN FEET COMPILED BY: K.A. JENSEN, P.Geo. O N T A R ‘ O DATE: REVISED: AUGUST 8, 2003 ...... 0 200 0 200 400 MARCH 30, 2004

Figure 28: Zone 4B Horizontal Polygonal Longitudinal, Aur Area `A' Option 96

Table 13: Inferred Resource Estimations for the Aur Area `A' Option.

Note: Density =12 cu ft / ton; Cut Off = 0.03opt; Cutting Factor = none ZONE NAME LONGITUDINAL POLYGONS POLYGONS INCLINATION 100 foot radius 200 foot radius Tons Au (opt) Tons Au (opt) QUARTZ VEIN Vertical 50,252 0.141 173,326 0.142 SOUTH SHEAR -65 NORTH SHEAR -45 54,057 0.217 81,418 0.200 ZONE 1 -45 17,618 0.131 48,981 0.128 ZONE 2 -25 67,533 0.130 118,291 0.130 ZONE 3A -25 57,316 0.365 156,195 0.364 ZONE 3B -25 148,434 0.143 341,806 0.166 ZONE 4A -25 99,362 0.091 203,287 0.093 ZONE 4B -25 47,683 0.109 120,854 0.116 TOTALS 542,256 0.159 1,244,158 0.168

Note: Density =12 cu ft / ton; Cut Off = 0.05opt; Cutting Factor = none ZONE NAME LONGITUDINAL POLYGONS POLYGONS INCLINATION 100 foot radius 200 foot radius Tons Au (opt) Tons Au (opt) QUARTZ VEIN Vertical 50,252 0.141 173,326 0.142 SOUTH SHEAR -65 NORTH SHEAR -45 44,483 0.257 66,404 0.238 ZONE 1 -45 17,61 0.131 48,981 0.128 ZONE 2 -25 56,033 0.148 99,254 0.146 ZONE 3A -25 57,316 0.365 156,195 0.364 ZONE 3B -25 139,793 0.150 326,854 0.172 ZONE 4A -25 90,313 0.098 180,347 0.101 ZONE 4B -25 47,683 0.109 120,854 0.116 TOTALS 503,490 0.169 1,172,214 0.176

Note: Density =12 cu ft / ton; Cut Off = 0.075opt; Cutting Factor = none ZONE NAME LONGITUDINAL POLYGONS POLYGONS INCLINATION 100 foot radius 200 foot radius Tons Au (opt) Tons Au (opt) QUARTZ VEIN Vertical 50,252 0.141 173,326 0.142 SOUTH SHEAR -65 NORTH SHEAR -45 35,549 0.305 47,549 0.306 ZONE 1 -45 17,618 0.131 48,981 0.128 ZONE 2 -25 56,033 0.148 99,254 0.146 ZONE 3A -25 57,316 0.365 156,195 0.364 ZONE 3B -25 133,068 0.154 309,879 0.177 ZONE 4A -25 48,481 0.125 110,099 0.124 ZONE 4B -25 16,306 0.217 46,351 0.217 TOTALS 414,622 0.192 991,634 0.197 97

Zone No.2 has a cluster of intersections on the western side and has not been terminated as drill hole B88-62 was not sampled and B90-11 was only partially sampled. The cluster is represented by drill holes B88-53 at 0.169 opt over 18.98 feet, B88-51 at 0.108 opt over 7.50 feet, B88-83 at 0.138 opt over the partially sampled length of 0.33 feet, and B88-28 at 0.131 opt over 4.97 feet. With a minimum amount of the recommended exploration work, this cluster could be up graded to a drill indicated resource.

Similar clusters with higher gold grade intersections for Zones 3A and 3B are terminated at the north property boundary. These clusters are surrounded by drill hole pierce points, which were either not sampled or only partially sampled. With a minimum amount of the recommended exploration work, this cluster could be up graded to a drill indicated resource.

To date, the results of the inferred resource estimation has not been subjected to any audits or reviews. 98

20.0 OTHER RELEVANT DATA AND INFORMATION

The writer is not aware of any other relevant data or information available on the Harricana Mine project.

The author is not aware of any outstanding issues regarding either environmental, permitting, legal, title taxation, socio-economic or political issues that would adversely affect the Harricana Mine project.

21.0 INTERPRETATION AND CONCLUSIONS

The use of geophysical survey is a primary exploration and evaluation tool. The magnetic surveys, both airborne and ground, have assisted in the identification of Ethological units, and structural features such as folding and faulting. The vertical component of the magnetic surveys, vertical gradient, will add increased knowledge and better identify structures contained within a single lithological unit.

The HLEM and IP surveys are the most effective geophysical survey to detect the gold style mineralization associated with sulphides. Generally, the gold style quartz veined mineralization with lower percentage of sulphides has been detected more successfully with the induced polarization (IP) surveys.

gold bearing tension shear zones between two near parallel, moderately to steeply dipping quartz vein gold bearing ductile shear zones located within and in close proximity to the contact of the Bourlamaque Batholith.

The use of the Val d'Or style of gold mineralization model is a very valuable guide for the evaluation of the property, understanding the complex relationship between stratigraphy and mineralization and for prioritization of diamond drill targets.

The database generated by the author for the Aur Area `A' Option is relatively error free and is generally suitable for use in resource estimation. KAJ notes, however, that the check sampling by Behnoral Mines indicates that a sampling bias may exist. The effect that this possible bias would have on the resource estimate is not known and cannot be determined at this time. Further check sampling will be required to determine if this bias does, in fact, exist and what affect it might have on the Mineral Resource estimate. Following the re-sampling and check assaying, if the bias is found, the gold grades in the database should be averaged with the results of the re-sampling, and the Mineral Resource estimate should be redone.

Finally, the recommended sampling to identify extensions of the zones and the proposed infill diamond drilling will assist in the refinement of the current geological model and the extent of the gold bearing mineralization which could result in a more accurate definition of the zones and an increase confidence level of the resource estimation. 100

22.0 RECOMMENDATIONS AND BUDGET

KAJ has reviewed the technical information for the various geophysical, geochemical and diamond drill programs for the Harricana Mine project. In summary, the author's recommendation is that all geophysical, geochemical and drill data for the property be reviewed, digitally compiled, and re-assessed with respect to untested exploration potential. The Aur Area `A' merits further exploration diamond drilling.

Specifically, the following work is recommended: • Geophysical data should be reviewed, compiled and interpreted with respect to the results obtained from the diamond drilling programs. • A uniform GPS system should be established to correlate the numerous diamond drilling campaigns, survey grids and geophysical anomalies. • Prior to the commencement of the following fieldwork, the grid should be brushed out and re-chained and replace any missing pickets. All pickets should be labelled with metal tags. The baseline, tie lines and the ends of the grids lines should have GPS coordinates. • It is recommended that the remainder of Area B, specifically Lac Blouin establish a grid and surveyed by total field magnetic and gradient magnetic surveys. • Zones of interest should be surveyed with IP prior to future diamond drilling It is recommended that the IP survey parameters be with spacing of a= 50 metres with readings N=1 to N=6 in a pole-dipole configuration. A drill hole to surface Mise a la Masse IP survey may be beneficial in tracing individual mineralized shear zones to assist in the correlation of the various zones on the Aur Area `A' claims. • It is recommended that the 1988 and 1990 diamond drill core be checked for additional technical information and sampling of drill core along strike and down dip projections of known gold bearing mineralization zones. It is estimated at a total of 4,624 feet of additional sampling is recommended as indicated in Appendix H. • At least 10% to 15% of the existing split core should be 1/4 split for check assaying. • During the assaying procedures, it is recommended that the laboratory complete density determinations representative of each of the zones. 101

• KAJ has recommended a multi-phase diamond drill program for 2004-2005. A three- phase program involving re-sampling the existing diamond drill core, in-filling diamond drilling and exploration geophysical surveys with follow-up diamond drilling is recommended with Phase 1 having a cost of $100,092, Phase 2 having a cost of $296,717 and Phase 3 having a cost of $239,076.

Other Recommendations: • KAJ recommends that the quality control (QC) and quality assurance (QA) for assaying the diamond drill core be put in place before the above recommended diamond drill program All pulps and rejects should be returned to the company for secure storage and future uses such as metallurgical testing and bulk density testing. • KAJ recommends that the proposed and future diamond drill programs be completed with NQ diamond drill core size. Also, it is recommended that the drill core be cut by a diamond saw rather than with a hydraulic or hand sputter.

A budget for the recommended work as outlined above is summarized in Table 14.

Dated at Timmins, Ontario, this 17th day of April, 2004.

Kian A. Jensen, B.Sc., P.Geo. 102

Table 4: Proposed Exploration Budget for the Harricana Mine Project:

Phase 1: Aur Area 'A' Option Amount Cost per Unit Total Cost Re Log and Sampling Core: Phase 1 Personnel 60 days 450.00 27,000.00 Personnel 60 days 250.00 15,000.00 Transportation 60 days 75.00 4,500.00 Accommodations 60 days 60.00 3,600.00 Assaying - core 924 samples 20.00 18,480.00 Check assaying 507 samples 20.00 10,140.00 Sub Total 78,720.00 Contingency Re-Logging, Sampling Program 10% 7,872.00 Compilation, Drafting, Report 30 days 450.00 13,500.00 Estimated Total for Phase 1 100,092.00

Phase 2: Aur Area 'A' Option Amount Cost per Unit Total Cost Grid - brushing (km) 11 km 250.00 2,750.00 Transit surveying drill holes (est) 5,000.00 IP Survey (km) 11 km 1,500.00 16,500.00 Drill Hole Gyro Survey 20,000.00 Diamond Drilling' Phase 2 Drilling (metres) 2,641 m 65.00 171,665.00 Assaying - core 867 samples 20.00 17,340.00 Personnel 29 days 450.00 13,050.00 Personnel 29 days 250.00 7,250.00 Transportation 29 days 75.00 2,175.00 Accommodations 29 days 60.00 1,740.00 Sub Total 257,470.00 Contingency on Drilling Program 10% 25,747.00 Compilation Personnel 30 days 450.00 13,500.00 Estimated Total for Phase 2 296,717.00

Phase 3: Area 'B' Claims Amount Cost per Unit Total Cost Grid - line cutting (km) 20 km 385.00 7,700.00 IP Survey (km) 20 km 1,500.00 30,000.00 Diamond Dril ing: Phase 3 Drilling (metres) 2075 m 65.00 134,875.00 Assaying - core 800 samples 20.00 16,000.00 Personnel 23 days 450.00 10,350.00 Personnel 23 days 250.00 5,750.00 Transportation 23 days 75.00 1,725.00 Accommodations 23 days 60.00 2,760.00 Sub Total 209,160.00 Contingency on Drilling Program 10% 20,916.00 Compilation, Drafting, Report 20 days 450.00 9,000.00 Estimated Total for Phase 3 239,076.00 103

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Cie Montreal Trust (1986) 15 Drilling Logs of Holes CB-86-1 to CB-86-15, Cie Montreal Trust, 61 pg, 1 map. GM 43932 104

Cie Montreal Trust (1986) Report on Diamond Drilling Program and Ore Reserve Calculation with 91 Logs of Holes CB-86-1 to 15, CL-1 to 9, 9A, CL-10 to 32, CL-34, CL-36 to 60, CL-62 to 68 and CL-73 to 82, Harricana Property, Cie Montreal Trust, 504 pg, 127 map. GM 44971

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Harricana Amalgamated Gold Mines Inc. Harricana Gold Mines Ltd. (1944) Bourlamaque, Dubuisson, 5 Diamond Drill Hole Logs and Information Report, Harricana Amalgamated Gold Mines Inc. Harricana Gold Mines Ltd.GM 01079-B

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Redland Resources Ltd. (1983) Senneville, Report on Magnetic Survey, Redland Resources Ltd. GM 39962

Robert, F. (1990) An Overview of Gold Deposits in the Eastern Abitibi in The Northwestern Quebec Polymetallic Belt: A Summary of 60 Years of Mining Exploration, C1M, Special Volume 43, p93-105.

Ross, S.H., Denis, B.T., Asbury, W.N., Longley, W.W. and Auger, P.E. (1938) Mining Properties and Development Work in Abitibi and Chibougamau Regions during 1937. Department of Mines and Fisheries, Quebec Bureau of Mines, P.R. No. 120, p17-18.

Sullivan Bourlamaque Gold Mines Ltd. (1945) Bourlamaque, 2 Diamond Drill Holes, Sullivan Bourlamaque Gold Mines Ltd. GM 06976-A

Sullivan Bourlamaque Gold Mines Ltd. (1941) Bourlamaque, Examination Report and 2 Diamond Drill Holes, Sullivan Bourlamaque Gold Mines Ltd. GM 06976-B

Tasmaque Gold Mines Ltd. (1946) Bourlamaque, Report on the Property and 3 Diamond Drill Hole Logs, GM 00052

Valroy Explorers Ltd. (1981) Dubuisson, Report on Magnetic and Electromagnetic Surveys, Valroy Explorers Ltd. GM 37156 108

CERTIFICATE

I, Kian A. Jensen, P.Geo., do hereby certify that:

1) I am consulting geologist of Societé Minière Rivière Harricana Inc. or Harricana River Mining Corporation Inc.

2) I am a graduate of the University of Waterloo with an Honours B.Sc. in Earth Science, Geology Major (1975) with over 25 years of professional experience since graduation.

3) I am a member in good standing in the following associations: a) Geological Association of Canada - Fellow, 1983 b) Association of Professional Geoscientists of Ontario (APGO) — Member 00558

4) I have worked as a geologist for a total of 26 years since my graduation from University.

5) I have read the definition of "qualified person" set out in National Instrument 43-101 (NI 43-101") and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirements to be a "qualified person" for the purposes of NI 43-101.

6) I am responsible for the preparation of all sections of the technical report titled "Technical Report on the Harricana Mine Project, Val d'Or Mining Camp, NTS 32C/04, Bourlamaque and Dubuisson Township, Quebec, Canada for Societé Minière Rivière Harricana Inc. or Harricana River Mining Corporation Inc." the "Technical Report". I did visit the Harricana Mine Project on August 28, 2003 and re-examined the diamond drill core on November 7, 2003.

7) 1 have had prior involvement with 2629-2482 Quebec Inc. (currently HRMC) in the creation of presentation diamond drill sections in June of 2003 and the initial resource estimation in June and July of 2003.

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

9) I am independent of the issuer applying all of the tests in section 1.5 of National Instrument 43- 101.

10) I have read National Instrument 43-10 and Form 43-101F1, and the Technical Report has been prepared in compliance with that instrument and form.

Dated this 17th Day of April, 2004

Kian A. Jensen, B.Sc., P.Geo. 109

APPENDICES

Appendix A: Harricana Amalgamated Gold Mines Inc. 1936 Diamond Drill Holes Appendix B: E & B Exploration 1981 and 1983 Diamond Drill Holes Appendix C: Province X Exploration 1981 Diamond Drill Holes Appendix D: Canstat Petroleum Corporation 1981 Diamond Drill Holes Appendix E: Canstat Petroleum Corporation 1986 Diamond Drill Holes Appendix F: Belmoral Mines Limited 1988 and 1990 Diamond Drill Holes on the Aur Area "A" Option

Appendix G: International Hasten Enterprises Limited 1989 Diamond Drill Holes

Appendix H: Recommended Additional Sampling of the Belmoral Diamond Drill Core Appendix I: Quartz Vein Zone — MINERAL RESOURCE Appendix J: North Shear Zone — MINERAL RESOURCE Appendix K: Zone No.1— MINERAL RESOURCE Appendix L: Zone No.2 — MINERAL RESOURCE Appendix M: Zone 3A — MINERAL RESOURCE Appendix N: Zone 3B — MINERAL RESOURCE Appendix O: Zone 4A — MINERAL RESOURCE Appendix P: Zone 4B — MINERAL RESOURCE 110

Appendix A: Harricana Amalgamated Gold Mines Inc. 1936 Diamond Drill Holes Hole No Eastings East Error Northings North Elevation Azimuth Dip Length (feet) (+) (feet) Error (+) (feet) (feet) H-1 2100 6010 353 -42 999 H-2 2110 6000 173 -35 316 H-3 4545 5585 183 -45 264 H-4 4415 5640 183 -45 422 H-5* 6275.83 -0.17 5585.17 0.67 116.08 -45 136.75 H-6* 6275.83 -0.17 5585.17( 0.67 185.38 -40 410.5 H-7* 6198.41 0.91 5666.52 0.52 355.82 -45 406 H-8* 6101.75 1.75 5390.38 -0.62 984.25 164.62 -42 158.5 H-9* 6144.77 1.27 6322.75 1.25 180.40 -50 336 H-10 4600 6780.6 180 -45 333.5 H-11 4600 6780.6 360 -90 997 H-12 450 6780.6 360 -90 735 H-13 4500 5729.6 360 -45 502 H-14* 2116.79 1953.69 2.98 -45 536 H-15 4500 6090.6 360 -50 1203 H-16* 2098.00 1420.04 2.98 -50 596 H-17 4500 6680.6 180 -50 600 H-18 5000 1466 360 -53 501 H-19 5028 2066 360 -53 508.33 H-20 5000 2666 360 -53 500 H-21 5000 3266 360 -53 496 + H-22 6445 6322 180 H-23 + H-24 6253.5 6099 115 + H-25 5842.5 6323.5 180 + H-26 5857.5 5876 180 + H-27 6346.5 6322 180 + H-28 6143.5 6072 115 + H-29 6123.5 5835 91 H-30 H-31 + H-32 5828.5 5702.5 102.5

Notes: (*) Surveyed Coordinates with the remainder obtained from diamond drill logs. A coordinate correction of 142.09 feet North required to correlate with the 1981 grid system. A major error exists between the above coordinates and the survey plan map for drill hole H-10 of approximately 200 feet. (+)Amount of error from drill logs and E&B Exploration 1"=100' plan map. 111

Appendix B: E & B Exploration 1981 and 1983 Diamond Drill Holes

Hole No Eastings Northings Elevation Azimuth Dip Length Comments (feet) (feet) (feet) (feet) 81-B-1 9760 17140 987 200 -54 1,637.00 no drill log available 81-B-2 12675 11490 1020 180 -45 817.00 log 81-B-3 11920 11840 1023 198 -45 1,424.00 log 83-B-4 12200 10275 240 -45 1,085.00 no drill log available 83-B-5 11560 11700 223 -45 875.00 no drill log available 83-B-6 12790 9675 180 -45 875.00 no drill log available 83-B-7 12525 9900 230 -45 1,085.00 no drill log available 83-B-8 5675 6990 180 -45 650.00 no drill log available 83-B-9 3425 5950 180 -45 875.00 no drill log available 83-B-10 2675 5940 180 -45 1,085.00 no drill log available

Hole No Eastings Northings Elevation Azimuth Dip (metres) (metres) (metres) 81-B-1 5224.27 2974.85 300.84 200 -55 81-B-2 3502.15 3865.34 310.9 180 -50 81-B-3 3608.83 3633.22 311.81 198 -50

Note: The above information obtained from Surveyor's notes. I 1 1 1 1 1 1 1) 1 1

112

Appendix C: Province X Exploration Inc. 1981 Diamond Drill Holes

Hole No Eastings East Northings North Elevation Azimuth Dip Length Louvicourt Core Comments (feet) Error (feet) Error (feet) (feet) Elevation Size (+) (+) (feet) HP-1 5950 7 5535 2 990.5 360 -90 750.00 4997.104 BQ drill log available HP-2 6130 -1 5530 -4 991.3 360 -90 553.00 4997.348 BQ drill log available HP-3 6325 -9 5540 -10 1000.2 360 -90 161.00 5000.061 BQ 1 pg summary HP4 6075 22.5 5633 0 988.2 360 -90 504.00 4996.403 AQ 1 pg summary HP-5 * 5992 -2 5601.5 48.5 985.3 4995.514 AQ HP-6 * 5924 -3 5627.5 4 983.7 4995.032 AQ HP-7 5848 -12 5602 6 982.4 360 -90 715.00 4994.636 AQ 1 pg summary HP-8 5773 -7 5578 6 982.6 360 -90 750.00 4994.697 AQ HP-9 5661 -6 5639 11 986 112 -60 536.00 4995.733 AQ drill log available HP-10 5689 11 5771 -4 986.8 128 -70 1,184.50 4995.977 AQ drill log available HP-11 6091 -1 4938 -5.5 990.5 360 -90 1,414.00 4997.104 AQ HP-12 6111 8 5279 -3 990.1 360 -90 1,886.00 4996.983 AQ drill log available HP-13 5782 -15 5878 33 983.9 180 -80 1,453.00 4995.093 AQ drill log available

Notes: These drill holes have been identified as "H", "HP", "HAC" and "H". Original shaft elevation surveyed as 1000.00 feet. Coordinates of the southwest corner of shaft are 6,200.00 feet East and 5,653.00 feet North. (*) Coordinates scaled from Surveyor's Plan map, remainder obtained from diamond drill logs. (+) Amount of error from drill logs and E&B Exploration 1"=100' plan map. 113

Appendix D: Canstat Petroleum Corporation 1981 Diamond Drill Holes 1981 Diamond Drill Holes Hole No Eastings Northings Elevation Azimuth Dip Length (metres) (metres) (metres) (metres) CL-1 19881.99 9994.9 4994.775 360 -90 271.69 CL-2 19881.99 9994.9 4994.775 190 -74 209.40 CL-3 19881.99 9994.9 4994.775 10 -75 228.00 CL-4 19881.94 9994.9 4994.775 100 -72 200.30 CL-5 19869.48 9963.7 4994.704 190 -87 374.29 CL-6 19869.48 9963.7 4994.704 108 -78 121.90 CL-7 19842.8 9938.74 4994.998 360 -90 342.60 CL-8 19842.8 9938.74 4994.998 87 -72 154.80 CL-9 19336.76 10174.81 4994.682 346 -60 282.20 CL-9A 19336.76 10173.81 4994.682 346 -50 47.60 CL-10 19336.76 10174.81 4994.682 180 -62 294.30 CL-11 19444.74 10012.87 4994.949 360 -52 654.10 CL-12 19095.91 10310.38 4991.526 180 -58 91.74 CL-13 18744.99 9990.23 5003.961 180 -55 229.50 CL-14 18838.65 9974.82 4998.119 180 -55 218.50 CL-15 19842.8 9938.74 4994.998 113 -79 185.30 CL-16 19803.93 10452.1 4993.862 180 -61 249.90 CL-17 19734.55 10932.35 4990.118 360 -90 183.50 CL-18 19734.55 10932.35 4990.118 180 -56 230.00 CL-19 19336.07 10146.58 4994.418 360 -57 271.27 CL-20 21736.17 11205.96 4998.508 180 -55 398.10 CL-21 19675.29 10933.58 4988.85 180 -55 36.00 CL-22 19675.29 10933.58 4988.85 164 -90 200.60 CL-23 19675.29 10933.58 4988.85 360 -58 261.50 CL-24 19349.66 10176.85 4994.024 360 -63 78.00 CL-25 19304.26 10165.42 4994.589 360 -62 123.80 CL-26 21704.48 11614.82 4999.061 185 -56 425.00 CL-27 19612.78 10950.55 4986.972 360 -55 44.80 CL-28 19350.73 10146.3 4994.766 360 -56 206.30 CL-29 19322.42 10147 4994.189 360 -56 230.40 CL-30 19361.96 10158.06 4994.616 360 -50 230.40 CL-31 21431.97 10773.92 4997:468 360 -55 397.50 CL-32 21703.58 11127.6 4998.152 360 -56 428.60 CL-34 21702.24 10852.53 4997.615 180 -57 169.50 CL-36 19737.14 10727.05 4993.635 360 -72 247.06 CL-37 21704.13 11744.04 4999.948 360 -55 398.10 CL-38 21702.75 12177.07 5002.422 180 -55 392.00 CL-39 21706.63 12293.95 5007.12 180 -62 421.50 CL-40 19796.14 10862.74 4988.409 180 -61 236.80 CL-41 19796.14 101362.74 4988.409 360 -53 258.50 CL-42 19332.69 10344.48 4994.461 185 -51 352.40 114

1981 Diamond Drill Holes (continued) Hole No Eastings Northings Elevation Azimuth Dip Length (metres) (metres) (metres) (metres) CL-43 19363.79 10344.75 4994.426 180 -53 365.80 CL-44 19461.45 10334.42 4994.769 180 -83 365.80 CL-45 20033.6 10863.15 4995.053 180 -53 267.60 CL-46 20033.6 10863.15 4995.053 360 -52 353.40 CL-47 19262.33 9998.17 4994.26 360 -52 367.60 CL-48 19733.58 11023.72 4986.975 180 -73 225.00 CL-49 19827.1 11020.42 4988.506 180 -74 222.50 CL-50 20280.09 10885.92 360 -50 426.10 CL-51 20280.09 10885.92 4995.582 180 -55 419.40 CL-52 19351.01 10122.76 4994.535 360 -58 199.00 CL-53 19335.61 10120.81 4994.636 360 -56 184.70 CL-54 19336.11 10102.12 4994.724 360 -58 200.00 CL-55 18439.62 10207.9 4992.83 360 -55 256.00 CL-56 18439.27 10223.77 4992.808 180 -55 256.60 CL-57 18444.02 9957.61 4998.295 360 -52 267.00 CL-58 21183.54 13661.16 4995.37 180 -55 403.90 CL-59 19322.47 10124.6 4994.221 180 -55 374.60 CL-60 21215.47 13231.35 4994.546 360 -55 396.24 CL-62 19351.08 10091.09 4994.465 360 -63 245.70 CL-63 19324.32 10091.32 4994.291 360 -56 233.50 CL-64 21277.23 11991.87 5007.856 180 -55 309.70 CL-65 18437.47 9986.73 4998.359 180 -55 336.20 CL-66 19000.34 11799.65 4984.853 360 -87 122.50 CL-67 18987.73 11812.94 4985.159 315 -54 398.10 CL-68 18998.26 11785.34 4985.642 180 -57 404.20 CL-73 19348.96 10125.43 4994.632 360 -56 130.50 CL-74 19348.96 10125.43 4994.632 360 -64 121.30 CL-75 19348.96 10125.43 4994.632 15 -59 154.80 CL-76 19379.23 10103.46 4994.697 360 -58 200.60 CL-77 19334.97 10124.19 4994.675 360 -63 146.10 CL-78 19322.47 10124.6 4994.297 360 -53 154.80 CL-79 19322.47 10124.6 4994.297 337 -67 198.10 CL-80 19348.96 10125.43 4994.632 360 -64 154.80 CL-81 19599.01 9985.92 0 30 -53 304.80 CL-82 19322.47 10124.6 4994.297 337 -51 154.80

Note: CL-50 drill log was not located. (*) Drill holes were not surveyed. 115

Appendix E: Canstat Petroleum Corporation 1986 Diamond Drill Holes 1986 Diamond Drill Holes

Hole No Eastings Northings Elevation Azimuth Dip Length (metres) (metres) (metres) (metres) CB86-1 18745.95 10261.21 4992.589 180 -50 197.21 CB86-2 18851.01 10168.28 4993.342 180 -50 118.26 CB86-3 19746.43 10695.67 4993.117 180 -50 476.10 CB86-4 19746.87 10683.07 4993.872 360 -50 267.61 CB86-5 19796.43 11063.93 4987.669 195 -50 286.51 CB86-6 19852.77 11252.02 4987.381 190 -50 350.22 CB86-7 19846.88 11217.25 4987.042 22 -50 294.74 CB86-8* 20082 11629 0 215 -50 365.15 CB86-9* 20067 11611 0 35 -50 264.57 CB86-10* 20291 11936 0 215 -50 349.91 CB86-11* 20303 11946 0 35 -45 264.57 CB86-12* 20490 12220 0 215 -50 240.18 CB86-13* 21200 12623 0 30 -50 504.75 CB86-14* 21722 11835 0 180 -55 175.56 CB86-15* 22000 11846 0 180 -65 230.43

Note: Drill core size BQ. (*) Drill holes were not surveyed. 116

Appendix F: Belmoral Mines Limited 1988 and 1990 Diamond Drill Holes on the Aur Area "A" Option

Hole No Eastings Northings Elevation Azimuth Dip Length (feet) (feet) (feet) (feet) B88-28 400 -565 10000 360 -73 1,005.00 B88-30 600 -160 10000 180 -55 1,939.00 B88-31 400 -700 10000 360 -45 908.00 B88-37 400 700 10000 360 -77 1,208.00 B88-49 400 -410 10000 360 -75 998.40 B88-51 200 -480 10000 360 -75 1,088.00 688-53 200 -180 10000 360 -90 1,226.00 B88-54 600 -160 10000 180 -90 1,306.00 B88-55 400 -20 10000 180 -89 1,365.00 B88-56 600 -160 10000 180 -75 1,338.00 B88-58 800 -185 10000 180 -87 1,548.00 B88-59 600 -30 10000 180 -89 1,288.00 B88-60 1000 -200 10000 180 -85 1,267.00 B88-61 1200 -100 10000 180 -87 1,327.00 B88-62 0 -150 10000 180 -88 1,747.00 B88-63 800 -40 10000 180 -88 1,247.00 B88-65 800 -185 10000 180 -73 947.00 688-68 800 -185 10000 180 -63 862.00 B88-73 800 -185 10000 180 -52 937:00 B88-76 800 -600 10000 180 -70 747.00 688-77 200 -20 10000 180 -90 1,277.00 B88-79 1000 -300 10000 180 -75 968.00 B88-83 200 -480 10000 180 -90 753.00 B90-9 200 -650 10000 180 -90 498.00 B90-10 200 -800 10000 180 -90 665.00 B90-11 0 -350 10000 180 -88 1,229.00 690-12 0 -600 10000 180 -90 910.00 B90-13 200 -800 10000 180 -60 508.00

Note: Survey Coordinates were not located, the above coordinates are related to their geophysical survey grid. Drill core size BQ. 117

Appendix G: International Baslen Enterprises Limited 1989 Diamond Drill Holes

Hole No Eastings Northings Elevation Azimuth Dip Length (feet) (feet) (feet) (feet) IB-1 5635 9295 0 180 -75 956.00 IB-2 5635 9295 0 180 -60 806.00 I B-3 5635 9295 0 180 -45 802.00 I B-4 5735 9297 0 180 -75 956.00 IB-5 5735 9297 0 180 -60 806.00 IB-6 5735 9297 0 180 -45 796.00 I B-7 5520 9242 0 180 -75 947.00 I B-8 5520 9242 0 180 -60 703.00 I B-9 5520 9242 0 180 -45 1,027.00 IB-10 5458 9361 0 180 -75 807.00 IB-11 5459 9239 0 180 -55 807.00

Note: Survey coordinates for these drill holes were not located. Northing and Easting are only approximate and were obtained from inserting location map into the imperial and metric grid coordinate system for the property. Drill core size BQ. 118

Appendix H: Recommended Additional Sampling of the Behnoral Diamond Drill Core

Section Drill Hale From To Zone Name Comments Total (feet) (feet) footage Sec 0+00E B90-12 170.00 North Shear 456.30 472.00 South Shear 15.70 494.80 500.00 South Shear 5.20 B90-11 395.50 400.00 North Shear 4.50 598.70 613.00 Zone 2 14.30 636.50 678.00 Zone 2 41.50 823.00 839.60 Zones 3A, 3B not sampled 16.60 840.00 854.90 Zones 3A, 38 not sampled 14.90 855.50 867.00 Zones 3A, 3B not sampled 11.50 912.70 926.00 Zone 4A, South 13.30 Shear B88-62 568.00 582.00 North Shear not sampled 14.00 731.00 754.00 Zone 2 not sampled 23.00 759.00 800.00 Zone 2 not sampled 41.00 880.00 930.00 Zones 3A, 3B not sampled 50.00 930.00 1000.00 Zone 4A 70.00 119

Section Drill Hole From To Zone Name Comments Total (feet) (feet) footage Sec 2+00E B90-13 455.50 461.80 #4 expand assay zone 6.30 0.22/2.0 463.40 465.50 #4 expand assay zone 2.10 0.22/2.0 468.50 474.00 #4 expand assay zone 5.50 0.22/2.0 600.00 alteration zone B90-9 449.90 450.4013512 sampled but values 0.50 missing 471.40 476.80 Zone 1 not sampled 5.40 477.30 498.00 Zone 1 not sampled 20.70 B88-83 146.00 165.70 North Shear 19.70 600.00 623.50 Zone 2 partially sampled 23.50 0.138/0.3 623.80 642.00 Zone 2 partially sampled 18.20 0.138/0.3 714.00 734.00 South Shear alteration zone 20.00 B88-51 703.60 764.20 Zone 2 alteration zone 60.60 793.00 908.00 alteration zone 115.00 909.00 1000.00 Zones 3A, 3B, 4A 91.00 B88-53 750.80 752.5010364 sampled but values 1.70 missing 771.60 773.00 Zone 2 not assayed 1.40 771.60 773.0010383 sampled but values 1.40 missing 806.60 827.50 alteration zone 20.90 829.00 845.60 alteration zone 16.60 846.10 850.30 alteration zone 4.20 850.80 869.60 alteration zone 18.80 870.60 873.0010400 sampled but values 2.40 missing 873.00 951.40 Zones 3A, 3B, 4A 78.40 951.40 952.0010453 sampled but values 0.60 missing 952.00 965.00 Zones 3A, 36, 4A 13.00 1015.30 1015.801.0454 sampled but values 0.50 missing B88-77 635.00 690.00 North Shear 55.00 874.70 989.00 Zones 3A, 3B, 4A 114.30 994.00 1030.00 Zones 3A, 3B, 4A 36.00 120

Section Drill Hole From To Zone Name Comments Total (feet) (feet) footage Sec 4+00E B88-37 184.50 190.10 North Shear 5.60 190.90 199.50 North Shear 8.60 217.20 228.90 North Shear 11.70 234.00 242.30 North Shear 8.30 243.10 276.20 North Shear 33.10 758.20 763.6010302 sampled but values 5.40 missing B88-28 257.30 265.70 North Shear 8.40 675.20 682.00 Zone 2 sample length too large 6.80 735.50 824.00 alteration zone 88.50 850.00 916.30 Zones 3A, 3B, 4A 66.30 917.70 921.80 Zones 3A, 3B, 4A 4.10 925.60 937.20 Zones 3A, 3B, 4A 11.60 941.50 945.00 Zones 3A, 3B, 4A 3.50 B88-49 401.80 406.30 North Shear 4.50 406.80 423.50 North Shear 16.70 429.80 435.50 North Shear 5.70 446.00 500.50 North Shear 54.50 740.00 746.10 Zone Z2 6.10 746.80 749.90 Zone Z2 3.10 933.00 944.00 Zone 4a partially sampled 11.00 0.101/2.8 946.80 966.00 Zone 4a partially sampled 19.20 0.101/2.8 B88-31 500.00 539.60 North Shear 39.60 540.40 546.30 North Shear 5.90 547.30 562.60 North Shear 15.30 570.00 582.70 North Shear 12.70 583.70 586.00 North Shear 2.30 593.50 604.80 North Shear 11.30 870.60 877.00 alteration zone 6.40 878.00 893.00 alteration zone 15.00 B88-55 955.40 1002.40 Zones 3B, 4A 47.00 1015.30 1016.3011471 sampled but values 1.00 missing 1023.20 1039.00 Zone 4A 15.80 121

Section Drill Hole From To Zone Name Comments Total (feet) (feet) footage Sec 6+00E B88-30 435.00 450.80 North Shear alteration zone 15.80 452.90 456.00 North Shear alteration zone 3.10 458.00 462.30 North Shear alteration zone 4.30 470.00 472.30 North Shear alteration zone 2.30 474.80 482.20 North Shear alteration zone 7.40 490.00 524.00 North Shear alteration zone 34.00 756.00 812.00 South Shear, alteration zone 56.00 Zone 1 868.00 890.00 alteration zone 22.00 888-56 470.00 485.00 North Shear 0.441/12.10 bracket 15.00 zone 693.60 707.00 Zone 2 alteration zone 13.40 716.00 773.00 Zone 2 alteration zone 57.00 818.00 953.50 Zones 3B, 4A, 4B 135.50 B88-54 671.30 714.60 Zone 2 alteration zone 43.30 780.00 797.00 Zone 2 partially sampled Z2, 3A 17.00 0.447/12.50 815.30 830.00 Zone 2 Zones Z2, 3A, 1.700/2.2 14.70 945.50 994.10 Zones 3A, 3B 4A alteration zone 48.60 0.105/49.5 1085.00 1088.80 Zone 4B alteration zone 3.80 1089.50 1092.70 Zone 4B alteration zone 3.20 1093.30 1095.00 Zone 4B alteration zone 1.70 1097.20 1102.00 Zone 4B alteration zone 4.80 1103.00 1135.00 Zone 4B alteration zone 32.00 B88-59 734.60 766.20 Zone 2 31.60 782.80 830.70 Zone 2 47.90 862.40 905.00 Zones 3A, 3B, 4A, alteration zone 42.60 4B 918.80 986.40 Zones 3A, 3B, 4A, alteration zone 67.60 4B 1003.10 1027.30 Zones 3A, 3B, 4A, alteration zone 24.20 4B 1078.90 1130.00 Zones 3A, 3B, 4A, alteration zone 51.10 4B 122

Section Drill Hole From To Zone Name Comments Total (feet) (feet) footage Sec 8+00E B88-76 131.00 154.40 South Shear, sample all alteration 23.40 Zone 1 167.30 178.80 South Shear, sample all alteration 11.50 Zone 1 182.20 213.00 South Shear, sample all alteration 30.80 Zone 1 216.20 227.50 South Shear, sample all alteration 11.30 Zone 1 0.011/5.0 240.00 243.20 South Shear, sample all alteration 3.20 Zone 1 249.00 274.20 South Shear, sample all alteration 25.20 Zone 1 278.30 302.00 South Shear, sample all alteration 23.70 Zone 1 317.00 329.00 South Shear, sample all alteration 12.00 Zone 1 0.077/0.5 329.50 357.00 South Shear, sample all alteration 27.50 Zone 1 0.077/0.6 369.00 425.70 South Shear, sample all alteration 56.70 Zone 1 445.80 449.10 South Shear, sample all alteration 3.30 Zone 1 450.80 492.00 South Shear, sample all alteration 41.20 Zone 1 496.70 543.80 South Shear, sample all alteration 47.10 Zone 1 556.10 640.00 South Shear, sample all alteration 83.90 Zone 1 B88-73 425.00 437.60 expand assay zone 12.60 438.30 463.00 expand assay zone 24.70 463.20 468.50 expand assay zone 5.30 470.10 479.20 expand assay zone 9.10 492.20 500.60 expand assay zone 8.40 500.90 539.10 expand assay zone 38.20 540.10 542.00 expand assay zone 1.90 0.305/0.8 542.80 560.70 expand assay zone 17.90 0.305/0.8 759.80 818.80 South Shear, 59.00 Zone 1 888-68 478.60 492.20 North Shear alteration zone 13.60 499.70 507.20 North Shear alteration zone 7.50 511.60 539.50 North Shear alteration zone 27.90 549.90 562.20 North Shear alteration zone 12.30 563.50 578.00 North Shear alteration zone 14.50 580.60 591.00 North Shear alteration zone 10.40 123

Section Drill Hole From To Zone Name Comments Total (feet) (feet) footage Sec 8+00E B88-68 591.70 613.20 North Shear alteration zone 21.50 613.90 620.40 North Shear alteration zone 6.50 634.90 650.00 North Shear alteration zone 15.10 685.00 709.60 Zone 2 alteration zone partially 24.60 sampled 739.60 744.50 Zone 2 alteration zone partially 4.90 sampled 745.70 760.00 Zone 2 alteration zone partially 14.30 sampled 760.00 798.80 Zones 3B, 4A, 4B partially sampled 38.80 0.120/3.9 821.30 829.40 Zones 3B, 4A, 4B partially sampled 8.10 831.20 838.40 Zones 3B, 4A, 4B partially sampled 7.20 839.70 862.00 Zones 3B, 4A, 4B partially sampled 22.30 B88-58 579.40 598.60 North Shear not sampled alteration 19.20 zone 743.00 857.60 Zone 3A not sampled 114.60 944.30 975.00 Zone 4B not sampled 30.70 B88-63 699.20 739.00 Zones 2, 3A, 3B alteration zone partially 39.80 sampled 768.50 813.00 Zones 2, 3A, 3B alteration zone partially 44.50 sampled 833.00 853.00 Zones 2, 3A, 3B alteration zone partially 20.00 sampled 874.00 888.50 Zones 2, 3A, 3B alteration zone partially 14.50 sampled 908.50 933.20 Zones 2, 3A, 3B alteration zone partially 24.70 sampled 1021.60 1127.00 Zone 4B not sampled alteration 105.40 zone B87-147 sample all alteration 0.00 sections 124

Section Drill Hole From To Zone Name Comments Total (feet) (feet) footage Sec B88-79 357.00 395.00 North Shear not sampled alteration 38.00 10+00E zone 493.00 516.20 Zone 2 partially sampled 23.20 alteration zone 534.20 588.00 Zone 2 partially sampled 53.80 alteration zone 595.30 600.00 Zone 2 partially sampled 4.70 alteration zone 680.00 689.20 Zones 3A, 3B, 4A, partially sampled 9.20 South Shear alteration zone 706.80 714.30 Zones 3A, 3B, 4A, partially sampled 7.50 South Shear alteration zone 715.00 719.80 Zones 3A, 3B, 4A, partially sampled 4.80 South Shear alteration zone 724.50 731.60 Zones 3A, 3B, 4A, partially sampled 7.10 South Shear alteration zone 763.40 807.00 Zones 3A, 3B, 4A, partially sampled 43.60 South Shear alteration zone 820.80 920.00 Zones 3A, 3B, 4A, partially sampled 99.20 South Shear alteration zone B88-60 585.00 617.00 North Shear alteration zone 32.00 651.00 660.00 North Shear alteration zone 9.00 661.60 690.00 North Shear alteration zone 28.40 690.00 792.00 Zones 2, 3A not sampled alteration 102.00 zone 802.00 828.00 Zones 2, 3A not sampled alteration 26.00 zone 901.10 1025.60 Zones 4A, 4B not sampled alteration 124.50 zone Sec B88-61 710.00 760.00 North Shear, Zones alteration zone 50.00 12+00E 2, 3A, 3B 760.30 897.40 North Shear, Zones alteration zone 137.10 2, 3A, 3B 903.50 968.70 North Shear, Zones alteration zone 65.20 2, 3A, 3B 1211.00 1285.00 not sampled alteration 74.00 zone B87-144 hole not sampled 0.00 Total required footage to be sampled 4624.20 Estimated total number of recommended samples 924,84 125

APPENDIX I: QUARTZ VEIN ZONE - MINERAL RESOURCE

Note: Density = 12 cu ft / ton; Cut Off = 0.03 opt; Cutting Factor = none ZONE QUARTZ VEIN - Polygons = 100 foot radius, Vertical Longitudinal -90 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B88-55 22,170 14.70 14.70 325,899 12 27,158 0.118 3 B88-77 22,170 12.50 12.50 277,125 12 23,094 0.168 TOTAL: 44,340 603,024 50,252 0.141

ZONE QUARTZ VEIN - Polygons = 200 foot radius, Vertical Longitudinal -90 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B88-55 74,835 14.70 14.70 1,100, 075 12 91,673 0.118 3 B88-77 78,387 12.50 12.50 979,838 12 81,653 0.168 TOTAL: 153,222 2,079,912 173,326 0.142

Note: Density = 12 cu ft / ton; Cut Off = 0.05 opt; Cutting Factor = none ZONE QUARTZ VEIN - Po ygons =100 foot radius, Vertical Longitudinal -90 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B88-55 22,170 14.70 14.70 325,899 12 27,158 0.118 3 B88-77 22,170 12.50 12.50 277,125 12 23,094 0.168 TOTAL: 44,340 603,024 50,252 0.141

ZONE QUARTZ VEIN - Polygons = 200 foot radius, Vertical Longitudinal -90 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 888-55 74,835 14.70 14.70 1,100, 075 12 91,673 0.118 3 888-77 78,387 12.50 12.50 979,838 12 81,653 0.168 TOTAL: 153,222 2,079,912 173,326 0.142

Note: Density = 12 cu ft / ton; Cut Off = 0.075 opt; Cutting Factor = none ZONE QUARTZ VEIN - Po ygons = 100 foot radius, Vertical Longitudinal -90 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B88-55 22,170 14.70 14.70 325,899 12 27,158 0.118 3 B88-77 22,170 12.50 12.50 277,125 12 23,094 0.168 TOTAL: 44,340 603,024 50,252 0.141

ZONE QUARTZ VEIN - Polygons = 200 foot radius, Vertical Longitudinal -90 deorees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B88-55 74,835 14.70 14.70 1,100, 075 12 91,673 0.118 3 B88-77 78,387 12.50 12.50 979,838 12 81,653 0.168 TOTAL: 153,222 2,079,912 173,326 0.142 126

APPENDIX J: NORTH SHEAR ZONE - MINERAL RESOURCE

Note: Density = 12 cu ft / ton; Cut Off = 0.03 opt; Cutting Factor = none ZONE NORTH SHEAR - Polygons = 100 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 5 B88-51 15,469 4.90 6.93 107,200 12 8,933 0.066 9 B88-56 15,065 12.10 17.11 257,762 12 21,480 0.441 11 B88-59 17,298 6.90 9.76 168,828 12 14,069 0.098 18 B88-83 7,886 10.30 14.57 114,899 12 9,575 0.032 TOTAL: 55,718 648,690 54,057 0.217

ZONE NORTH SHEAR - Polygons = 200 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 5 B88-51 32,649 4.90 6.93 226,258 12 18,855 0.066 9 888-56 20,269 12.10 17.11 346,803 12 28,900 0.441 11 B88-59 22,929 6.90 9.76 223,787' 12 18,649 0.098 18 B88-83 12,366 10.30 14.57 180,173 12 15,014 0.032 TOTAL: 88,213 977,020 81,418 0.200

Note: Density = 12 cu ft / ton; Cut Off = 0.05 opt; Cutting Factor = none ZONE NORTH SHEAR - Polygons = 100 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 5 B88-51 15,469 4.90 6.93 107,200 12 8,933 0.066 9 B88-56 15,065 12.10 17.11 257,762 12 21,480 0.441 11 888-59 17,298 6.90 9.76 168,828 12 14,069 0.098 TOTAL: 47,832 533,791 44,483 0.257

ZONE NORTH SHEAR - Polygons = 200 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 5 B88-51 32,649 4.90 6.93 226,258 12 18,855 0.066 9 B88-56 20,269 12.10 17.11 346,803 12 28,900 0.441 11 B88-59 22,929 6.90 9.76 223,787 12 18,649 0.098 TOTAL: 75,847 796,847 66,404 0.238 127

APPENDIX J: continued

Note: Density = 12 cu ft / ton; Cut Off = 0.075 opt; Cutting Factor = none ZONE NORTH SHEAR - Polygons = 100 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 9 B88-56 15,065 12.10 17.11 257,762 12 21,480 0.441 11 B88-59 17,298 6.90 .9.76 168,828 12 14,069 0.098 TOTAL: 32,363 426,591 35,549 0.305

ZONE NORTH SHEAR - Polygons = 200 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 9 B88-56 20,269 12.10 17.11 346,803 12 28,900 0.441 11 B88-59 22,929 6.90 9.76 223,787 12 18,649 0.098 TOTAL: 43,198 570,590 47,549 0.306 128

APPENDIX K: ZONE No. 1 - MINERAL RESOURCE

Note: Density = 12 cu ft / ton; Cut Off = 0.03 opt; Cutting Factor = none ZONE 1 - Polygons =100 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B90-10 21,291 3.90 4.30 91,551 12 7,629 0.099 3 B90-13 21,291 5.10 5.63 119,868 12 9,989 0.156 TOTAL: 42,582 211,420 17,618 0.131

ZONE 1 - Polygons = 200 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B90-10 67,662 3.90 4.30 290,947 12 24,246 0.099 3 B90-13 52,722 5.10 5.63 296,825 12 24,735 0.156 TOTAL: 120,384 587,771 48,981 0.128

Note: Density = 12 cu ft / ton; Cut Off = 0.05 opt; Cutting Factor = none ZONE 1 - Polygons = 100 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B90-10 21,291 3.90 4.30 91,551 12 7,629 0.099 3 B90-13 21,291 5.10 5.63 119,868 12 9,989 0.156 TOTAL: 42,582 211,420 17,618 0.131

ZONE 1 - Polygons = 200 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B90-10 67,662 3.90 4.30 290,947 12 24,246 0.099 3 890-13 52,722 5.10_ 5.63 296,825r 12 24,735 0.156 TOTAL: 120,384 587,771 48,981 0.128

Note: Density = 12 cu ft / ton; Cut Off = 0.075 opt; Cutting Factor = none ZONE 1 - Polygons =100 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B90-10 21,291 3.90 4.30 91,551 12 7,629 0.099 3 B90-13 21,291 5.10 5.63 119,868 12 9,989 0.156 TOTAL: 42,582 211,420 17,618 0.131

ZONE 1 - Polygons = 200 foot radius, Inclined Longitudinal -45 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B90-10 67,662 3.90 4.30 290,947 12 24,246 0.099 3 890-13 52,722 5.10 5.63 296,825 12 24,735 0.156 TOTAL: 120,384 587,771 48,981 0.128 129

APPENDIX L: ZONE No. 2 - MINERAL RESOURCE

Note: Density = 12 cu ft / ton; Cut Off = 0.03 opt; Cutting Factor = none ZONE 2 - Polygons =100 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-28 21,189 4.50 4.97 105,309 12 8,776 0.131 4 B88-51 21,282 6.80 7.50 159,615 12 13,301 0.106 5 B88-53 21,083' 17.20 18.98 400,155 12 33,346 0.169 6 B88-55 17,381 7.20 7.94 138,005 12 11,500 0.043 12 B88-83 22,170 0.30 0.33 7,316 12 610 0.138 TOTAL: 103,105 810,401 67,533 0.130

ZONE 2 - Polygons = 200 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-28 35,121 4.50 4.97 174,551 12 14,546 0.131 4 688-51 42,671 6.80 7.50 320,033 12 26,669 0.106 5 B88-53 35,870 17.20 18.98 680,813 12 56,734 0.169 6 B88-55 28,772 7.20 7.94 228,450 12 19,037 0.043 12 B88-83 47,420 0.30 0.33 15,649 12 1,304 0.138 TOTAL: 189,854 1,419,495 118,291 0.130

Note: Density = 12 cu ft / ton; Cut Off = 0.05 opt; Cutting Factor = none ZONE 2 - Polygons = 100 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-28 21,189 4.50 4.97 105,309 12 8,776 0.131 4 B88-51 21,282 6.80 7.50 159,615 12 13,301 0.106 5 B88-53 21,083 17.20 18.98 400,155 12 33,346 0.169 12 B88-83 22,170 0.30 0.33 7,316 12 610 0.138 TOTAL: 85,724 672,396 56,033 0.148

ZONE 2 - Polygons = 200 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-28 35,121 4.50 4.97 174,551 12 14,546 0.131 4 B88-51 42,671 6.80 7.50 320,033 12 26,669 0.106 5 B88-53 35,870 17.20 18.98 680,813 12 56,734 0.169 12 B88-83 47,420 0.30 0.33 15,649 12 1,304 0.138 TOTAL: 161,082 1,191, 045 99,254 0.146 130

APPENDIX L: continued

Note: Density = 12 cu ft / ton; Cut Off = 0.075 opt; Cutting Factor = none ZONE 2 - Polygons =100 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-28 21,189 4.50 4.97 105,309 12 8,776 0.131 4 B88-51 21,282 6.80 7.50 159,615 12 13,301 0.106 5 B88-53 21,083 17.20 18.98 400,155r 12 33,346 0.169 12 B88-83 22,170 0.30 0.33 7,316 12 610 0.138 TOTAL: 85,724 672,396 56,033 0.148

ZONE 2 - Polygons = 200 foot radius, inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 888-28 35,121 4.50 4.97 174,551 12 14,546 0.131 4 B88-51 42,671 6.80 7.50 320,033 12 26,669 0.106 5 B88-53 35,870 17.20 18.98 680,813 12 56,734 0.169 12 888-83 47,420 0.30 0.33 15,649 12 1,304 0.138 TOTAL: 161,082 1,191,045 99,254 0.146 131

APPENDIX M: ZONE 3A - MINERAL RESOURCE

Note: Density = 12 cu ft / ton; Cut Off = 0.03 opt; Cutting Factor = none ZONE 3A - Polygons =100 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 888-49 22,170 11.10 12.25 271,583 12 22,632 0.264 2 B88-54 22,170 12.50 13.79 305,724 12 25,477 0.447 3 B88-55 18,537r 5.40 5.96 110,481 12 9,207 0.384 TOTAL: 62,877 687,787 57,316 0.365

ZONE 3A - Polygons = 200 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-49 61,967 11.10 12.25 759,096 12 63,258 0.264 2 B88-54 62,427 12.50 13.79 860,868 12 71,739 0.447 3 B88-55 42,680 5.40 5.96 254,373 12 21,198 0.384 TOTAL: 167,074 1,874,337 156,195 0.364,

Note: Density = 12 cu ft / ton; Cut Off = 0.05 opt; Cutting Factor = none ZONE 3A - Polygons =100 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-49 22,170 11.10 12.25 271,583 12 22,632 0.264 2 B88-54 22,170 12.50 13.79 305,724 12 25,477 0.447 3 B88-55 18,537 5.40_ 5.96 110,481 12 9,207 0.384 TOTAL: 62,877 687,787 57,316 0.365

APPENDIX M: continued

Note: Density = 12 cu ft / ton; Cut Off = 0.075 opt; Cutting Factor = none ZONE 3A - Polygons = 100 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-49 22,170 11.10 12.25 271,583 12 22,632 0.264 2 B88-54 22,170 12.50 13.79 305,724 12 25,477 0.447 3 B88-55 18,537 5.40_ 5.96 110,481 12 9,207 0.384 TOTAL: 62,877 687,787 57,316 0.365

ZONE 3A - Polygons = 200 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H. W. VOLUME T.F. TONS Au opt 1 888-49 61,967 11.10 12.25 759,096 12 63,258 0.264 2 B88-54 62,427 12.50 13.79 860,868 12 71,739 0.447 3 B88-55 42,680 5.40 5.96 254,373 12 21,198 0.384 TOTAL: 167,074 1,874,337 156,195 0.364 133

APPENDIX N: ZONE 3B - MINERAL RESOURCE

Note: Density = 12 cu ft / ton; Cut Off = 0.03 opt; Cutting Factor = none ZONE 3B - Polygons =100 foot rad'us, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-49 22,170 9.30 10.26 227,464 12 18,955 0.453 2 B88-54 22,170 49.50 54.62 1,210, 925 12 100,910 0.105 5 B88-60 22,170 3.30 3.64 80,699 12 6,725 0.069 8 888-65 18,418 5.10 5.63 103,693 12 8,641 0.033 9 B88-68 15,441 9.30 10.26 158,425 12 13,202 0.100 TOTAL: 100,369 1,781,206 148,434 0.143

ZONE 3B - Polygons = 200 foot rad'us, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-49 75,534 9.30 10.26 774,979 12 64,582 0.453 2 B88-54 49,437 49.50 54.62 2,700,249 12 225,021 0.105 5 B88-60 55,960 3.30 3.64 203,694 12 16,975 0.069 8 888-65 31,869 5.10 5.63 179,422 12 14,952 0.033 9 888-68 23,716 9.30 10.26 243,326 12 20,277 0.100 TOTAL: 236,516 4,101,671 341,806 0.166

Note: Density = 12 cu ft / ton; Cut Off = 0.05 opt; Cutting Factor = none ZONE 3B - Polygons =100 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 888-49 22,170 9.30 10.26 227,464 12 18,955 0.453 2 B88-54 22,170 49.50 54.62 1,210,925 12 100,910 0.105 5 888-60 22,170 3.30 3.64 80,699 12 6,725 0.069 9 888-68 15,441 9.30 10.26 158,425 12 13,202 0.100 TOTAL: 81,951 1,677,513 139,793 0.150

ZONE 3B - Polygons = 200 foot radius, Inclined Longitudinal -25 decrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 888-49 75,534 9.30 10.26 774,979 12 64,582 0.453 2 B88-54 49,437 49.50 54.62 2,700,249 12 225,021 0.105 5 888-60 55,960 3.30 3.64 203,694 12 16,975 0.069 9 B88-68 23,716 9.30 10.26 243,326 12 20,277 0.100 TOTAL: 204,647 3,922,248 326,854 0.172 134

APPENDIX N: continued

Note: Density = 12 cu ft / ton; Cut Off = 0.075 opt; Cutting Factor = none ZONE 3B - Polygons =100 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-49 22,170 9.30 10.26 227,464 12 18,955 0.453 2 B88-54 22,170 49.50 54.62 1,210,925 12 100,910 0.105 9 B88-68 15,441 9.30 10.26 158,425 12 13,202 0.100 TOTAL: 59,781 1,596,814 133,068 0.154

ZONE 3B - Polygons = 200 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-49 75,534 9.30 10.26 774,979 12 64,582 0.453 2 B88-54 49,437 49.50 54.62 2,700,249 12 225,021 0.105 9 B88-68 23,716 9.30 10.26 243,326 12 20,277 0.100 TOTAL: 148,687 3,718,554 309,879 0.177 135

APPENDIX O: ZONE 4A - MINERAL RESOURCE

Note: Density = 12 cu ft / ton; Cut Off = 0.03 opt; Cutting Factor = none ZONE 4A - Polygons = 100 foot radius, inclined Longitudinal 25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 888-49 22,170 2.80 3.09 68,505 12 5,709 0.101 3 B88-54 20,671 22.50 24.83 513,261 12 42,772 0.128 4 B88-55 19,842 16.30 17.99 356,958 12 29,746 0.070 5 B88-58 20,542 6.40 7.06 145,027 12 12,086 0.056 10 B88-77 19,672 5.00 5.52 108,589 12 9,049 0.031 TOTAL: 102,897 1,192,340 99,362 0.091

ZONE 4A - Polygons = 200 foot rad-us, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B88-49 64,922 2.80 3.09 200,609 12 16,717 0.101 3 B88-54 45,130 22.50 24.83 1,120, 578 12 93,381 0.128 4 888-55 30,399 16.30 17.99 546,878 12 45,573 0.070 5 888-58 41,941 6.40 7.06 296,103 12 24,675 0.056 10 B88-77 49,869 5.00 5.52 275,277 12 22,940 0.031 TOTAL: 232,261 2,439,445 203,287 0.093

Note: Density = 12 cu ft / ton; Cut Off = 0.05 opt; Cutting Factor = none ZONE 4A - Polygons = 100 foot rad-us, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B88-49 22,170 2.80 3.09 68,505 12 5,709 0.101 3 B88-54 20,671 22.50 24.83 513,261 12 42,772 0.128 4 888-55 19,842 16.30 17.99 356,958 12 29,746 0.070 5 888-58 20,542 6.40_ 7.06 145,027 12 12,086 0.056 TOTAL: 83,225 1,083,750 90,313 0.098

ZONE 4A - Polygons = 200 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 B88-49 64,922 2.80 3.09 200,609 12 16,717 0.101 3 B88-54 45,130 22.50 24.83 1,120, 578 12 93,381 0.128 4 B88-55 30,399 16.30 17.99 546,878 12 45,573 0.070 5 888-58 41,941 6.40 7.06 296,103 12 24,675 0.056 TOTAL: 182,392 2,164,168 180,347 0.101 136

APPENDIX O: continued

Note: Density = 12 cu ft / ton; Cut Off = 0.075 opt; Cutting Factor = none ZONE 4A - Polygons =100 foot radius, inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 2 888-49 22,170 2.80 3.09 68,505 12 5,709 0.101 3 B88-54 20,671 22.50 24.83 513,261 12 42,772 0.128 TOTAL: 42,841 581,766 48,481 0.125

APPENDIX P: ZONE 4B - MINERAL RESOURCE

Note: Density = 12 cu ft / ton; Cut Off = 0.03 opt; Cutting Factor = none ZONE 4B - Polygons =100 foot rad'us, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-54 20,151 8.80 9.71 195,666 12 16,306 0.217 2 B88-59 20,071 17.00 18.76 376,532 12 31,378 0.053 TOTAL: 40,222 572,198 47,683 0.109

ZONE 4B - Polygons = 200 foot rad'us, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 688-54 57,283 8.80 9.71 556,218 12 46,351 0.217 2 B88-59 47,656 17.00 18.76 894,027 12 74,502 0.053 TOTAL: 104,939 1,450,244 120,854 0.116

Note: Density = 12 cu ft / ton; Cut Off = 0.05 opt; Cutting Factor = none ZONE 4B - Polygons =100 foot rad'us, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt ~ 1 B88-54 20,151 8.80 9.71 195,666 12 16,306 0.217 2 B88-59 20,071 17.00 18.76 376,532 12 31,378 0.053 TOTAL: 40,222 572,198 47,683 0.109

ZONE 4B - Polygons = 200 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1 B88-54 57,283 8.80 9.71 556,218 12 46,351 0.217 2 B88-59 47,656 17.00_ 18.76 894,027 12 74,502 0.053 TOTAL: 104,939 1,450,244 120,854 0.116

Note: Density = 12 cu ft / ton; Cut Off = 0.075 opt; Cutting Factor = none ZONE 4B - Polygons =100 foot radius, Inclined Longitudinal 25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1B88-54 20,151 8.80 9.71 195,666 12 16,306 0.217 TOTAL: 20,151 195,666 16,306 0.217

ZONE 4B - Polygons = 200 foot radius, Inclined Longitudinal -25 degrees POLYGON HOLE AREA WIDTH H.W. VOLUME T.F. TONS Au opt 1688-54 57,283 8.80 9.71 556,218 12 46,351 0.217 TOTAL: r 57,283 556,218 46,351 0.217