ASSESSMENT REPORT ON PROSPECTING AND TRENCHING ON KIMBERLITE TARGETS IN LORRAIN TOWNSHIP, LARDER LAKE MINING DIVISION

UTM Zone 17 - NAD 83 Projection 5238300N to 5240000N UTM 606000E to 607500E UTM

RECEW OEC 2 0 2007

GEOSel NCI! AsseSSMENT OF Ie

PREPARED BY:

Elaine Basa, P.Geo. ON Grupo Moje Limited

For Tres-Or Resources Ltd December 8,2007 2 • 3 7 4 SUMMARY

Tres-Or Resources Ltd. ("Tres-Or") is exploring for diamonds on several large blocks of contiguous claims covering parts of 53 townships in the Temagami - Kirkland Lake area. The Lorrain Twp block consists of 2 claims (8 units) straddling the Cross Lake Fault - part of the Lake Temiskaming Structural Zone (Figure 1). The claims are along a contact between Nipissing diabase and Lorrain granite. A circular, isolated mag high was identified within a larger circular structure (Figure 2). The claims were recorded in December 2004 and prospected, initially, in January 2005 when a till sample was collected. Follow-up prospecting was carried out in the fall of 2005 followed by a ground magnetometer survey. All this work has been previously submitted as assessment. Work included in this report consists of additional prospecting on the western target area and trenching across that target area in preparation for possible drilling.

This report covers the prospecting and trenching descriptions and photos with the incurred costs associated with the work and the writing of the report.

Although trenching uncovered magnetic Nipissing gabbro, the possibility of kimberlite intrusion has not been eliminated as these intrusions can be emplaced with little structural disruption even in close proximity to the contact. The target is still prospective particularly due to its location with respect to the Cross Lake Fault - one of the several comprising the Lake Temiskaming Structural Zone known to be of importance in the emplacement of the numerous kimberlites in the Cobalt-New Liskeard Kimberlite field as well as the Kirkland Lake and Attawapiskat Pipes.

Further work is recommended including additional till sampling and possibly diamond drilling.

11 TABLE OF CONTENTS

SUMMARY ..•..•.•.•....•••••....•.••...... ••..•.••.....••••...••••...... •..•.•.....••....••.....•..•....••..••...••..•••... II TABLE OF CONTENTS ...... 111 INTRODUCTION ...•.•....•...... ••.....••...•..•...... •...... •....•...... •.•.....•...•...... •.... 1 PROPERTY DESCRIPTION AND LOCATION ...... 3 PREVIOUS WORK.•...... •....• "' ...... •...... •...... •...... ••...•...•....••...... •..•••.••....•• 5 REGIONAL GEOLOGY ...... 7 REGIONAL STRUCTURE ..••..•..••..•.•...... •...••.•...... •...... •..•....•••..•...•....•.....•...•.••.•.•..••••• 8 GLACIAL DEPOSITS ...... 8 WORK PROGRAM SUMMARY ...... 9 CONCLUSIONS AND RECOMMENDATIONS ...... 14 REFERENCES ....•...... •.•..••...... •••....•••...... ••...... ••••..•..•...... •...... •.••.•...••••..•...•...• 15 STATEMENT OF QUALIFICATION...... •.•.•...... •....•..•••...•.... 16 APPENDIX I PHOTOS OF TRENCHING ...... 19 APPENDIX II SUMMARY OF COSTS ...... 20

List of Figures

Figure 1. Regional Geology Map ...... 2 Figure 2. Lorrain Twp - regional magnetic geophysical data ...... 4 Figure 3. Lorrain Twp Access Map ...... 10 Figure 4. Prospecting Map over Ground MagnetiCS ...... 11 Figure 5. Trench Location Map over ground magnetics ...... 12 Figure 6. Plan and Sectional View of Trenching ...... 13

List of Tables

Table 1: Lorrain Township claims list...... 3 Table 2: Lorrain Twp exploration budget...... 14

iii INTRODUCTION

Tres-Or Resources Ltd. (Tres-Or) has 2 claims (8 units) straddling the Cross Lake Fault - part of the Lake Temiskaming Structural Zone in Lorrain Twp southeast of Cobalt, Ontario. Tres-Or holds a 100% interest in these 2 claims in the southern limits of the Larder Lake Mining Division of northeastern Ontario covering NTS map sheets 31 MIOS and is exploring for diamondiferous kimberlites. Tres-Or's claims cover part of the Lake Timiskaming Structural Zone - an ancient, deep-seated northwest trending structure cutting the Archean Superior Craton and extend into Parautochthonous Belt of the Grenville Province. The Superior Craton is the largest Archean craton in the world, and has yielded some encouraging diamond exploration results recently. More than 30 kimberlite pipes and dykes are known in the Kirkland Lake and New Liskeard areas, some of which are diamondiferous. The kimberlites form a northwest-southeast trend that extends into the Tres-Or property with indicator chemistry and possibly diamond contents improving to the south (Sage, 1996). Allan (2001) reported in a recent Ontario Geological Survey (OGS) open file the recovery of kimberlite indicator minerals, including G10 pyropes and diamond-inclusion chromite from the Tres­ Or property area, supporting improving chemistry south of the known kimberlites. Tres-Or Resources Ltd Regional Geophysical - Mag data 500 o 1000 Meters Lorrain Twp - - - -

40'000 608000 610000 PROPERTY DESCRIPTION AND LOCATION

The Lorrain Twp claim group consists of 2 contiguous mineral claims, totalling 8 units (Table 1). The claims are on Crown land, with no private surface rights holders. The Lorrain Twp claims are 12 km SE of the town Cobalt and 13 km NW of the historic mining camp of Silver Centre along the secondary Hwy 567. The claims are accessed from either the east or west Although traversing access is easiest from the east via Hwy 567 south from Hwy 11 B at a point approximately half way between Cobalt and Haileybury in North Cobalt, this trail is not accessible to heavier equipment (hoe or drill). Access from the west is via mining roads behind Cobalt. Truck access reaches to just past the former Mayfair Mine. Additional trails exist beyond this point to the hydro lines and significant work was required to allow access for equipment for trenching.

Table 1: Lorrain Township claims list.

Claim Recording Claim Work Total Total Township Number Date Due Date Required Applied Reserve - LORRAIN 3014163 2004-12-20 2007-12-20 $2,400 $0 $533 LORRAIN 3014164 2004-12-20 2007-12-20 $800 $0 $5139

3 E

Tres-Or Resources Ltd Regional Geology Map (OGS fv1ap 2361 ) Lorrain Twp Claims

600000 605000 610000 615000 PREVIOUS WORK

Diamond exploration in Eastern Ontario has a long history, extending back at least to 1906, when the United States Geological Survey and several newspapers made reference to a 100 carat yellow stone that came to be known as the Nipissing Diamond. The story of the Nipissing Diamond, and the early history of diamond exploration are described in more detail in Sage (1996). Thin kimberlite dykes were intersected serendipitously in drill holes as early as 1948 in Michaud Township, and in 1968 in the Kirkland Lake area. Falconbridge and Monopros (the then exploration arm of De Beers Ltd.) led diamond exploration programs in the late 1970s and 1980s, which resulted in discovery of many of the Kirkland Lake and New Liskeard area pipes.

At least 16 kimberlites have been discovered in the New Liskeard and Notre-Dame-du-Nord area, where the Lake Timiskaming Structural Zone crosses the Ontario-Quebec border. The kimberlites are apparently associated with northwest trending faults that define the Lake Timiskaming Structural Zone (Sage, 1996). This northwest structural trend is also associated with the kimberlite field at Kirkland Lake, Ontario, and extends on to the Attawapiskat kimberlites, including the Victor Pipe, in the James Bay lowlands. In the New Uskeard and Notre Dame du Nord area, the Lake Timiskaming Structural Zone forms a graben. Kirnberlites are known on both the west flanks of the graben in Ontario, and the east flank in Quebec. About half of the New Uskeard area kimberlites have tested as weakly to moderately diamondiferous, with the most significant results to date being reported by Sudbury Contact Mines for the 95-2 pipe on the west side of the graben. From the 95-2 pipe, Sudbury Contact reports that 229 diamonds have been recovered from 2393 kg of kimberlite, the largest stone weighing 0.14 carats (Sudbury Contact Mines press release, April 3, 2003). The company, later called Contact Diamonds and now part of Stornoway Diamond Corp, discovered two new pipes several kilometres to the west in Klock and Van Nostrand Twp, which subsequently evaluated with definition drilling and initial bulk sampling. Tres-Or Resources discovered a large, +21 ha pipe within the Round Lake Batholith in May of 2005 based on evaluation of the Discover Abitibi's Airborne Mag/EM survey covering the Round Lake Batholith released in 2004. Subsequent diamond drilling has found 440 rough diamonds in just under 4 tonnes of material in caustic fusion alalysis. Continued evaluation is ongoing.

A regional stream sample study covering the Temagami-Marten River area by the Ontario Geological Survey (OGS) recovered kimberlite indicator minerals suggestive of derivation from diamondiferous mantle, and concluded that the area had good potential to host diamond-bearing kimberlites (Allan, 2001). The Cr-pyrope chemistry reported from this study includes distinctly more abundant sub-calcic grains (G10s) than known pipes in the New Liskeard

5 kimberlite field to the north. A second OGS kimberlite indicator mineral study extended sample coverage east to the Montreal River, and again recovered grains suggesting potential of the area to host diamond-bearing kimberlite (Reid, 2002).

The Ontario Geological Survey (OGS) collected and sorted 258 sediment samples in and south of the Lorrain Twp area for kimberlite indicator minerals (Allan, 2001). The samples were regionally spaced at 1 per 42 km2, and typically collected from streams. The methods and results of this work are described in the OGS Open File Report 6043 (Allan, 2001), which concludes, in part, that " ... the potential for kimberlite or related rock in the region is highly probable". The 258 samples yielded more than 1500 total indicator grains, including some sub-calcic (G10) pyrope garnets, Mg-ilmenites, and diamond associated chromites. Due to the success of OGS Open File 6043 recovering indicator minerals, the OGS expanded the study and collected additional samples east to the Quebec border.

The comparison of available indicator mineral chemistry points to an increase in the proportion of G10 pyropes near the Temagami East Property than in known pipes from Kirkland Lake and the New Liskeard area. Importantly, the distinct and better pyrope and Mg-ilmentite chemistry down-ice of Adroit's Temagmai East Property occurs in regional sediment samples which probably average more than one pipe. That the regional 'average' near the Tres-Or Adroit's Temagmai East Property is distinct from and more promising than the most favourable known pipes to the north strongly supports derivation from different sources. Therefore, although the diamondiferous New Liskeard area kimberlites are not necessarily indicative of mineralization on the Temagami East Property, the trend of improving chemistry to the south is encouraging for further exploration.

Eastern Ontario is the oldest and most important mining district in Canada. Sudbury, located 90 km to the west, has been one of the world's most important nickel producers since the 19th century. The Cobalt silver camp is the oldest mining camp in Canada.

6 REGIONAL GEOLOGY

The regional geology is marked by the structural suture marking the boundary between the Grenville Province to the south and the Superior and Southern Province to the north. Rocks of the Southern Province in the area comprise the Huronian Supergroup basinal sediments including the lowermost Coleman Member (primarily conglomerate with interbedded argillites and wackes) and the overlying Firstbrook Member (finely bedded, grey to maroon coloured, shaley mudstones and siltstones with some coarser wackes) of the Gowganda Formation - the primary host of the Ag-Co veins in the historic Cobalt Camp. Overlying the Gowganda Formation are the quartzites and arenites of the Lorrain Formation.

The Nipissing gabbro is an intrusive sill undulating throughout the area. Many mineral occurrences, most notably the well-known silver-cobalt-arsenide vein deposits of the Cobalt area, the centre of which is approximately 12 km to the north, and the productive Silver Centre silver mining camp lying within 8km to the southeast, are associated with either or both the upper and lower contact of this sill.

The Superior Province is characterized by mafic and intermediate to felsic metavolcanic rocks as flows, tuffs and breccias. The Superior Province volcanic rocks are poorly exposed in the area except in small windows. A significant window of Archean basement rocks is well exposed in the Silver Centre silver mining camp, an outlying associated camp to the main Cobalt Camp. Two inliers to the east consist of northwest-trending mafic and intermediate flows bordering the western margin of the Lorrain Granite. The volcanic inlier to the southwest consists of massive mafic flows along Hwy 11 west of Rib Lake (Born et ai, 1988)

Intruding the Keewatin metavolcanic and Timiskaming sedimentary rocks is an Algoman-age batholith from the Kenoran orogenic cycle (Jambor, 1971a). Locally, the Lorrain granite - a massive, uniformly pink, medium to coarse grained body - intrudes the basement and is partially overlain by sedimentary rock of the Huronian Supergroup and subsequently intruded by the Nipissing gabbro.

Additionally, the structure in this area is very significant. The Lake Temiskaming Structural Zone (LTSZ) or the Lake Temiskaming Rift Valley is a part of the Ottawa-Bonnechere Graben system, which joins with the St. Lawrence Graben system, all of which have been related to the opening of the Atlantic Ocean (Reid, 2002).

7 A number of northwest trending faults in the claim block area, the most significant of which is the Montreal River Fault, are associated with this structural zone, which, along with the Ottawa-Bonnechere Graben system, remains seismically active (Sage, 2000).

Because these structures are deep-seated, they form a major plumbing system and therefore conduits for not only kimberlite-associated rocks, but mineralizing fluids as well. This system of faults has been associated with kimberlitic and similar intrusions from Cobalt-New Liskeard through to Attawapiskat.

REGIONAL STRUCTURE

The major structural feature south of the property area is the Grenville Front boundary fault, which strikes east-northeast across Milne township, separating the Superior Province in the north with rocks affected by the Grenville orogeny to the south. The Lake Timiskaming Structural Zone (LTSZ) consists of numerous northwest trending faults spatially associated with kimberlites of the Kirkland Lake and New Liskeard fields. The Lorrain Twp claims straddle the Cross Lake fault - one of the major faults within the LTSZ.

GLACIAL DEPOSITS

Glacial drift was deposited across the properties by the Late Wisconsonian Laurentide ice sheet. Typically, a thin discontinuous layer of till covers the area, with local accumulations of glacio-fluvial deposits (Allan, 2001). Several directions of glacial ice movement have been identified, but the dominant sediment transport directions is oriented north-northeast to south-southwest (approximately 200°) across the claims (Veillette, 1988; Allan, 2001). Thus, kimberlite indicator minerals occurring in till samples south-southwest (down-ice) of the claims may project back to sources on the property. The front of the Laurentide ice sheet retreated past the Tres-Or property area between 11,000 and 10,000 years ago. Following the retreat of the ice-front, proglacial Lake Barlow-Ojibway formed. These large glacial lakes fed by the melting ice and restricted by limited outflow, covered extensive areas of western Quebec and northeastern Ontario. The New Liskeard area and parts of the Ottawa River Valley were flooded, covering the areas with thick glaciolacustrine deposits (Veillette, 1994).

8 WORK PROGRAM SUMMARY

The claims were recorded December 20, 2004. Previously-reported work by Tres-Or Resources includes initial traversing, till sampling and ground geophysics.

A crew of Temiskaming First Nations, led by Simon Chief, cut 4km of trail before the hoe and dozer were brought in. The equipment and operator was supplied by James Lathem Excavating Limited of Haileybury and supervised by C.J.Laidlaw and/or Martin Ethier.

Prospecting of the western anomaly was conducted in more detail by C. James Laidlaw in November 2005 (Figure 4) followed by trenching across the anomaly in late November 2005. A series of 6 trenches were completed (Figure 5 & 6) (See also Photos in Appendix I). Samples were taken but no analyses were done.

Two trenches were not entered due to rapid flooding and collapse of trench walls. No samples were taken, no mapping was completed in theses two trenches (Tr001 and Tr005). The four remaining trenches all encountered granophyric diabasic gabbro (Nipissing diabase). Three of these were strongly magnetic while the fourth ,and most southern of the trenches, exhibited weak to spotty magnetism.

9 602000 604000 606000 608000 610000

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Lorrain Twp Trenching Access Map 1000-- - o 1000- 2000 Meters 602000 604000 606000 608000 610000 waypolnt Name Waypoint description UTM-E UTM-N Elevation 44 Location on upgraded drill trail for vehicle parking. Start of ATV access. 603429 5242492 1204 ft

45 Point on upgraded trail; high-hoe has problem, left track comes off. Track is subsequently repaired and makes headway to Stop 072 at the end of the day 604997 5240174 1276 ft 46 Point on trail were fuel for heavy equipment is cached in ATV trailer. 605298 5239258,1257 ft 47 Position on access trail were high hoe dears access to. 605284 5238968 48 Centre of a 100m wide ash-alder swamp. Potential access impediment due to water and high organic nature of the overburden. 606432 5239053 1263 ft 49 North flowing stream. 607162 5239454 1237 ft Outcrop, rusty surface. Very strong magnetic attraction. Coarse-grained granophyric diabase, 5% disseminated cpy, po and Py. Exposure about 8m long 50 by 3m wide. Sample a composite grab selection from within this area. Sample number LO 50. Long duration GPS reading. 607265 5239629 1227 ft 51 Grid 290N 687E. Gabbro outcrop (the "Erratic"), massive medium-grained, dark green. weak to strong magnetic attraction. 607283 5239691 1175ft 52 Grid BL 300E 675N. North edge of peat-alder bog in contact with till that continues to the north, abutting against gabbro outcrop area. 607283 5239688 1171 ft 53 Grid BL 300E 700N. Till overburden, level, open birch treed. Slope gentle North and East. "Unreliable GPS reading'" 607291 5239693 1175 ft 54 Grid 280E 704N. Gabbro diabase rubble cropping (?), medium-grained, dark green, non-magnetic. "Unreliable GPS reading'" 607290 523970511181 ft 55 Grid BL 300E 725N. Till. 607291 5239691 1211 ft 56 Grid BL 300E 750N. Till. 607287 5239715 1211 ft 57 Grid BL 300E 800N. Till. 607300 5239791 1247 ft 58 Grid BL 300E 850N. Till. 607308 5239821 1234 ft Grid 350E 850N. Station at the west edge of a low level peat-alder swampy ground. No outcrop. Traverse from Stop 058 to 059, ground cover of till with 59 Igranite and gabbro erratics 607359 5239856 1230 ft 60 Grid 375E 850N. Edge of low level area, till overburden. and gabbro and granite erratics. No grid co-ordinates. 607377 5239847 1286 ft Grid 368E 835N. South edge of low level area between Stops 059 and 060. Medium-grained dark green gabbro diabase, strong magnetic attraction. 61 Reference sample LO 61 collected. 607366 5239847 1178 ft 62 Grid 350E 700N. Till covered level gentle slopes north and east. Relative topographic high. Magnetic anomaly area. "Unreliable GPS reading"! 607345 5239668 1171 ft 63 ~ till covered area. Relative topographic low to Stop 062. "Unreliable GPS reading'" 607319 5239687 1217 ft 64 Grid 350E ered gabbro outcrop. Relative topographic high to Stop 062. 607363 5239667 1217ft 65 Grid 375E 650N. Till covered relative topographic high. 607370 5239637 1234 ft Grid 350E 650N. Till covered relative topographic high, lower than Stop 065. Float of moderate spotty magnetic, medium-grained, dark green gabbro 66 diabase. Edge of bOI:! at 344E 650N. 607340 5239645 1260 ft 67 Grid 325E 650N. Alder-birch-ash bog, level, peat overburden, dry. GPS reading ok(?). 607318 5239642 1355 fI 68 Grid 30DE 662N. Alder-birch-ash bog, level, peat overburden probed to 80 cm depth, excavation fills with water. GPS reading ok(?). 607289 5239669 1220 ft Grid 225E 700N. Level swamp. Gabbro diabase outcrop at 221E 700N, non-magnetic.LO 69, reference sample of coarse-grained, sausseritized gabbro 69 diabase taken at 256E 7ooN. 607217 5239682 1168 fI Grid 238E 703N. In level swamp, coarse-grained (granophyric) varied-texture, gabbro diabase outcrop(?), very magnetic, reference sample LO 070 70 taken. 607240 5239699 1198 ft Grid 275E 650N. In level swamp, medium-grained granophyric epidotitized gabbro diabase, occurs as large tabular angular block(s), strong magnetic 2 71 attraction, reference sample LO 071 taken. Outcrop >10m , of non-magnetic gabbro diabase at grid 265E 650N, (at edge of swamp). 607261 5239646 1214 ft 72 Lathem Excavating high hoe at this point on access trail at the end of the day. 605185 5238720 1247 ft PARK •Parking area and float truck drop-off location at the former Mayfair Mine site. 602486 5244395 1142 ft

G02 Glacial observation, whalesback granite o.C. at 175°. 605685 523848811234 ft HOE1 End of day for trail construction, 21-Nov-05. Start of drill access trail 22-Nov-05 2.6 km of trail to Stop Tr002. 605356 5238452 1280 ft TFN3 Flag marks the end of TFN Forestry cutting activity, at grid 310E 697N. 607299 5239696 1237 ft Tr002 Tr002, Trench 2, grid 297E 696N. TiII1.5m over gabbro diabase. Photos TrO02Gabbrodiabase stngMA Photos 011 012 & 013.jpg, 607285 5239700 1214 ft Tr003, Trench 003, estimated UTM coordinates from map inspection. granophyric gabbro, 1.2m boulder silty sandy till, .8m peat. Sample TrOO3. Grid Tr003 293E 675N. Photos Tr003 0.c.TiII1.2m,Peat.8m 006, 007 & ooa.jpg, 607282 5239883 Tr004, Trench 004, peat, silt and till over granophyric gabbro diabase, very magnetic, sample TROO4 collected, Photos TrOO4 TrO04 0.c.TiIl1.0m,SiltySand.5m,Peat.8m 014015,016 & 017.jpg 607279 5239669 1211 ft TrO05, Trench 005. Grid 290E 645N. 0 sample obtained. No direct observations of bedrock due the unstable nature of trench walls. Tr005 Photo Tr005 0.c.,tiIl1.7m,.30mSiltySand,1.2Peat 019 & 020.jp!), 607286 5239650 1211 ft Tr006, Trench 006. No 9r1d. Weak spotty magnetic attraction, gabOro dlaOase, at edge of swamp. No sampling. TrOOG Photos TrOO6_o.c.,Peat.5m,TiII1.2m_022.jpg, 607278 5239646 1201 ft 607200 607300 i07400 i ~~~--~~----~~~~~~~~~~~~H-~~~ l/')

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607200 i0738 0 607400 607250 607300 N Trench Location Map over ground mag

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( 1 1----" o :5 10 ISn, CONCLUSIONS AND RECOMMENDATIONS

The western magnetic anomalies have been prospected and trenched. Four of six trenches over 60m identified weakly to strongly magnetic granophyric diabasic gabbro. Although this would explain the magnetic high anomaly as seen in Figures 4 and 5, there are a number of kimberlite intrusions where little evidence is seen - even very proximally to the intrusive contact. The Peddie Pipe, for example, in Bucke Twp, is in direct contact with magnetic Nipissing gabbro. Additional work is required to determine the potential of a kimberlite instrusion. Additional till sampling and possibly diamond drilling is warranted.

Table 2: Lorrain Twp exploration budget.

I EXPLORATION ACTIVITY unit $ Geologie data compilation and field program planning $1,000 Access trail to site $10,000 Field logistic support (truck rental, fuel, accommodations, $200 15 man days $3,000 etc,) Diamond drilling - 300m $100/m $30,000 Till sampling -10 samples $350/sample $3,500 Supervision - geologist $500 15 man days $7,500 Office expenses (field office; office equipment) $4,000 Contingency 20% $11,100 Program Total $66,600 !

14 REFERENCES

Allan, S.E., 2001; Regional Modern Alluvium Sampling of Temagami-Marten River Area, North-eastern Ontario. Ontario Geological Survey, Open File Report 6043,194 p. Davidson, A. 1998; An overview of Grenville Province Geology, Canadian Shield. Chapter 3 In Geology of the Precambrian Superior and Grenville Provinces and Precambrian fossils. Geological Survey of Canada Geology of Canada v. 7, p. 205-270. Dyke, A. S. and Prest, V. K., 1987; Late Wisconsinan and Holocene Retreat of the Laurentide Ice Sheet; Geological Survey of Canada, Map 1702A, scale 1:5000 000. Cookenboo, H. 0.,8asa, E.,Ethier, M., 2004; Report on Adroit Resources Inc.'s Temagami North Cobalt South and Temagami East exploration properties in northeastern Ontario, 43.101 report, 95 p. Jambor, J.L. 1971a. General Geology, p.12-33 in The Canadian Mineralogist, vol. II, part 1, edited by L.G.Berry. Sobie, P.S., 2003. Report on the Timiskaming Diamond Project, NE Ontario and NW Quebec of Sudbury Contact Mines Limited. Unpublished report in format of NI 43101, www.SEDAR.com. 91 p. Sage, R. P., 1996; Kimberlites of the Lake Timiskaming Structural Zone. Ontario Geological Survey, Open File Report 5937, 435 p. Veillette, J.J., 1989; Ice movement, till sheets and glacial transport in Abitibi­ Timiskaming, Quebec and Ontario. In: DiLabio, R.N.W. and Coker, W.B. (eds), Drift prospecting, Geological Survey of Canada, Paper 89-20, 139-154. Veillette, J.J., 1994; Evolution and paleohydrology of glacial lakes Barlow and Ojibway. Quaternary Science Review, 13,945-971 Villeneuve m.e, ross, g.e., theriault, r.j., miles, W., parrish, r.r., and broome, j .. 1993; tectonic subdivision and u-pb geochronology of the crystalline basement of the alberta basin, western canada. Geological survey of canada bulletin 447, 86 p.

15 STATEMENT OF QUALIFICATION

To accompany the report entitled: Assessment Report on Trenching and Prospecting in Lorrain Township, Larder Lake Mining District for Tres-Or Resources Ltd., December 8, 2007.

I, Elaine Basa, of the city of Temiskaming Shores, in the Province of Ontario, Canada, hereby certify as follows concerning my report on the Tres-Or Resources Ltd.'s Lorrain Township property, Ontario, 2007:

1. I graduated from Carleton University in 1985 with a degree of Bachelor of Science, Honours Geology. 2. I am a Professional Geologist and a member of Professional Geoscientists of Ontario (member number 0895). 3. I have worked continuously in the mining industry for the past 20 years. 4. The attached report is a product of: a) data provided to me by the property owner b) data, field notes, maps and discussions with C.J.Laidlaw c) reports identified in the reference section of this report d) knowledge gained from working in the area over much of the past 20 years 5. I am acting as consulting geologist and Project Manager of the Temagami North Extension Property for Tres-Or Resources Ltd. have verified the reported work and all related expenses.

Dated this 8th day of December, 2007 in Temiskaming Shores, Ontario

Elaine Basa, P.Geo.

16 LIST OF PERSONNEL

Prospecting PersonneVTrail Supervision:

C. James Laidlaw R.R # 3, Madoc, ON KOK 2KO 613-473-5065

Martin Ethier, M.Sc. Box 304, Haileybury, ON POJ lKO 705-672-5814

Supervision, Geology, Report Writing

Elaine BaSa, P.Geo. Box 847, Haileybury, ON POIIKO 705-672-5644

C.lames Laidlaw RR # 3, Madoc, ON KOK 2KO 613-473-5065

Contractor

James Lathem Excavating Limited (1989) Box 176, 35 Niven Street Haileybury, ON POIIKO 705-6722-5576

Temiskaming First Nations Contact: Terence McBride 819-723-5333 ext 232 APPENDIX I .- PHOTOS OF TRENCHING

APPENDIX II - SUMMARY OF COSTS

!;~~~~I~r.) ,r i' "I~!I~~C~~~[:li ~"'rv'~;n;'-~~;~~~q I ivehlCle rentaL~ 11'.::1 rc ileage iTraH cutting (11(1 CO!ltmct(}rs' tr'Jck r ; 1tal: 2840 'Trail contructiOI"i an'; trenching - tOlal excavating contractor's :::ost 9384 I Geotech MOB 216 food/accor.) 1200 communicatiom,/priltl,",g 170 supplies 74 postagefshlpPlng 29 Access Notes from Simon Chief (Temiskaming First Nations - Contractor)

Waypoint Name OatelTime UTM-E UTM-N Elevation TRUCK 27/10/2005 8:08 6032521 5242670 1243 ft CLAIMPOST 27/10/200514:35 605 5238778 1267 ft BIGROCK 27/10/200514:38 605807 5238738 1271 ft FIRESTOP 27/10/200514:44 605712 5238581 1272 ft SWAMP 27/10/200514:47 605656 5238472 1267 ft ROCKYAREA 27/10/200514:50 605551 5238474 1271 ft HOLE 27/10/2005 14:52 605484 5238453 1255 ft HILLTOP 27/10/2005 14:53 605462 5238428 1253 ft SWAMP1 27/10/200514:56 605332 5238450 1279 ft ROCKTOP 27/10/2005 14:581 605269 5238429 1266 ft LEVEL 2 27/10/200515:00 605218 5238464 1243 ft LEVEL 1 27/10/200515:01 605187 5238478 1270 ft GULLY 27/10/200515:03 605168 5238493 1290 ft THIS SIDE 27/10/2005 15:04 605172 5238520 1260 ft RIDGE 27/10/200515:06 605194 5238572 1278 ft BOTTOM R 27/10/200515:07 605175 5238610 1275 ft 3-SPRUCE 27/10/200515:09 605194 5238701 1266 ft UP 27/10/200515:11 605213 5238767 1381 ft DOWN 27/10/200515:13 605269 5238799 1280 ft SLOW SLOPE 27/10/200515:15 605306 5238909 1257 ft NICE 27/10/200515:18 605302 5238994 1275 ft GOING UP 27/10/200515:19 605302 5239057 1260 ft ROUGH 27/10/200515:2'1 605295 5 1296 ft ROCKYAHEAD 27/10/200515:23 605317 5239227 1264 ft SLANT 27/10/2005 15:25 605321 5239320 1253 ft START 0 RB 27/10/200515:28 605354 5239438 1253 ft POND 27/10/200515:30 605390 5239403 1246 ft OLDTR END 27/10/20 605342 5239478 1253 ft PICKED UP 27/10/2005 604635 5240972 1255 ft 1605100 52395001 1606000 52395001 ~ ~

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Waypoint Name DatefTime UTM-E UTM-N Elevation ACCROSS 02/11/2005 8:57 605185 5238485 1269 ft AULDERS 02/11/200511:01 607274 5239632 1230 ft BIG STUMP 02/11/20058:40 605315 5239201 1239 ft BURNED 02/11/2005 8:54 605192 5238583 1305 ft CP 3014164 31/10/200514:31 607062 5239274 1331 ft CREEK 02/11/2005 11 :09 607186 5239485 1200 ft DETOURWAT 02/11/20059:07 605693 5238498 1270 ft DOWN 02/11/20058:56 605168 5238509 1285 ft LTD 02/11/2005 8:37 605318 52393451 0 ft LT1 02/11/20058:52 605189 52 LOOKUP 02/11/200511:11 607121 523941 1219 ft PINE RIGHT 02/11/2005 11 :04 607221 523958 1231 ft RTO 02/11/20058:34 605384 523937 1467 ft RT 1 02/11/20058:47 605301 5238875 1267 ft RT2 02/11/2005 9:05 605637 5238479 1255 ft 02/11/2005 8:43 605300 5239040 1259 ft ~o 02/11/2005 8:45 605303 5238909 1274 ft TL3 02/11/200511:06 607223 5239537 1203 ft TL4 02/1112005 11 :18 607106 5239256 1297 ft TOP 02/11/2005 8:501 605207 5238741 1285 ft UP 02/11/20058:49 605274 5238798 1279 ft WATER 02/11/2005 11 :23 607011 5239213 1252 ft WATER BIT 02/11/2005 9: 10 605784 5238759 1279 ft WILLOWS 02/11/2005 9: 13 605899 5238807 1257 ft ZAG 02/11/2005 11 :21 607039 5239218 1260 ft ZIG 02/1112005 11 :22 607030 5239218 1242 ft "- , '. '. I, \ \ , "- "- I " \ , , \ '\'" • I..... \ \, " \ • \1 - X, I I I I , I .» I \ \ I \ ,"->, \ " .... \ •\ \ \ \ '-. \ \, • \ ~::~. \, \ \ ;".,;\/". ,. ) I \ \ \. " I I \ \\ ~ .~,,:; } \ \ ) I, •\ \, I I, 'Y~ \ .' •\ \ . "X'. I, \ ....,. \ t' '. I \ .. \" -- ---' \ -\ I •, I • I, 1 \ •, , ) •\ "- • " '. \ , •I \, ., \ ... •.. \, \ \. • 1606000 5239500\ \ '. -\-\ ~

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300 m GPS Mop Detail CanMapCe, DMTI Spatial and the DMTI Spatial logo are trademar1ul of DMTI Spatial Inc., Markham , Ontario. C Garm ln Ltd. or ilS subsidiaries 1995-2004. C2003 DMTI Spatial Inc.