GEOLOGY REPORT on the

GOLD ROCK PROPERY Boyer Lake Area

Kenora Mining Division for

GOLDEYE EXPLORATIONS LIMITED

By:

W. S. Hamilton, P.Geo. W.S. Hamilton Geological Consulting Ltd.

July 31, 2007

Table of Contents

Page

1.0 Summary 1 2.0 Introduction and Terms of Reference 2 3.0 Disclaimer 2 4.0 Accessibility, Climate, Local Resources, Infrastructure and Physiography 2 5.0 Property Location and Description 4 6.0 History 4 7.0 Regional Geology 7 8.0 Current Work Program 13 8.1 Property Geology 13 8.2 Structural Geology 15 8.3 Mineralization 15 9.0 Sampling Method and Analyses 16 10.0 Interpretation and Conclusions 16 References 18 Certificate 21

List of Figures Figure 1 General Location Map Figure 2 Claim Map Figure 3 Regional Geology Map Figure 4 Local Geology Map Figure 4a Legend for Figure 4 Figure 5 Airborne Magnetic and EM Survey Map Gold Rock Geology Plan, scale 1:2,500 (in pocket)

Appendix Sample Description Sheets

1.0 Summary Goldeye Explorations Limited (“Goldeye”) engaged W. S. Hamilton Geological Consulting Ltd. to conduct geological mapping of a portion of Gold Rock property and to complete an assessment report describing this work. The Gold Rock property is located in the historic Gold Rock Mining Camp, about 35 kilometres south of the Town of Dryden, or approximately 900 km northwest of Toronto. The abandoned village of Gold Rock, situated at Trafalgar Bay of Upper Manitou Lake, is adjacent to the southwestern corner of the property. The approximate geographical coordinates of the claims are 49° 28’ N and 92° 42’ W, within NTS 52F/7 quadrangle. The property consists of seven contiguous unpatented claims registered 100% to Goldeye Explorations Limited. The claims comprise 27 units covering a nominal 432 hectares. Both surface and mining rights are attached to the claims. All of the claims are located within the Boyer Lake area (Claim Map G-2572) of the Kenora Mining Division, Ontario The western part of the Archean age Wabigoon Subprovince is underlain by supracrustal rocks consisting of volcanic and lesser sedimentary rocks ranging in age from 3.0 to 2.71 Ga, which are intruded by granitoid batholiths and gabbroic sills and stocks which range in age from 3.0 to 2.69 Ga. Ten greenstone belts have been recognized in this portion of the subprovince, of which the current property is situated in the Eagle-Wabigoon-Manitou Lakes greenstone belt. This greenstone belt trends northeast and is bounded on the northwest by the Atikwa granitoid batholith and on the southeast by the Irene-Eltrut Lakes batholith, and the Meggissi granitoid pluton. The northeast trending, steeply southeast dipping Manitou Straits Fault has been traced over a distance of 65 km along strike and bisects the greenstone belt. The author conducted a mapping and sampling program on Goldeye Explorations Limited’s Gold Rock property from July 16 to 25, 2007, which covered 12.35 km of pre-existing and new grid lines located on the southeastern shore of Double Lake. Grid line establishment, magnetic and IP/RES surveys were underway during the course of the author’s work. A total of 25 samples were collected by the author, and an additional 27 samples at were collected at various points on the lakeshore by JVX Ltd. personnel, who were conducting the grid establishment/geophysical surveying. The area mapped is underlain by a sequence of mafic, intermediate and felsic volcanic rocks, with local small intrusions of quartz-feldspar porphyry. The predominant trend of the foliation in the rocks in the area is northeast. Two east-northeast trending shear zones are interpreted to transect the area at approximately L 500 N and at L 1000N. These cross structures may represent zones of enhanced dilation, especially where they intersect northeast trending shear zones. Several of the IP/RES anomalies defined on the pre-existing grid were explained by the geological work, wherein pyrite mineralization locally associated with quartz veining was found generally within mafic volcanic rocks. In the absence of the analytical results from the sampling, as well as the results of the geophysical surveying, it is difficult to determine specific recommendations. However, the author is of the opinion that the geophysical surveying should be extended to the west over a portion of Double Lake during the winter months. The exact positioning and orientation of the grid lines should be determined upon receipt of all of the relevant data, in order to test the possibility that zones of exploration interest may strike both northeast, as well as east-northeast.

1

2.0 Introduction and Terms of Reference Goldeye Explorations Limited (“Goldeye”) engaged W. S. Hamilton Geological Consulting Ltd. (“WSHGC”) to conduct geological mapping of a portion of Gold Rock property in the Boyer lake area, Kenora Mining Division, and to complete an assessment report describing this work. This resultant report relies heavily on existing information, including regional geological and geophysical surveys, as well as local exploration and mining activities which are described in a Qualifying Report on Goldrock Property by G. A. Harron dated September 23, 2003. 3.0 Disclaimer This report is prepared solely for filing with the Ontario Ministry of Northern Development and Mines (“MNDM”) for assessment credit. This report has not been completed to National Instrument 43-101 specifications and is not intended for any other use than that previously specified. In writing this report, WSHGC has reviewed the reports of previous workers in the area, but cannot assure the accuracy of the data collected or the results of that work. Assay data reported by previous workers have not been confirmed, but are reported as data relevant to the property. In addition, information regarding land ownership and mining rights was obtained form files maintained by the MNDM; the MNDM disclaims the accuracy and subsequent use of these files. 4.0 Accessibility, Climate, Local resources, Infrastructure and Physiography The Gold Rock property is located in the historic Gold Rock Mining Camp, about 35 kilometres (“km”) south of the Town of Dryden, or approximately 900 km northwest of Toronto (Figure 1). The abandoned village of Gold Rock, situated at Trafalgar Bay of Upper Manitou Lake, is adjacent to the southwestern corner of the property. The approximate geographical coordinates of the claims are 49° 28’ N and 92° 42’ W, within NTS 52F/7 quadrangle. Year round access is best achieved by fixed wing aircraft or helicopter charter. Highway 502 connecting Dryden and Fort Francis passes approximately 2.2 km east of the eastern claim boundary. A 6 km long old wagon road connects Gold Rock village to highway 502; however, this un-maintained road is only traversable by all terrain vehicles in the summer, or snowmobiles in the winter. The author used Wilderness Air of Vermillion Bay for mobilization to and from the property. Accommodation was provided by Manitou Lodge located at the site of the old Gold Rock town site. Access to the property grid was either by foot following an old trail for a distance of about 1.5 km to L 500S. Alternatively, a trail leads northeast to a river which flows south from Double Lake. A boat can be taken upriver to the south end of Double Lake, where a short portage provides access to the lake. The prevailing climatic conditions are typical of the northern boreal forest, with warm summer days from mid-May to late September. Winter conditions are characterized by moderate snowfall and sub-zero temperatures. Most preliminary exploration activities can be carried out year round, except for geological and geochemical surveys, which are restricted to the summer months. Local resources on the properties include abundant fresh water, stands of pine, spruce, fir and poplar, as well as limited quantities of aggregates. Electrical power is available at a distance of about 35 km north of the claims. The Town of Dryden is the closest source of commercial enterprises and transportation facilities.

2

3

MANITOBA

.Kenora

() GOLD ROCK

Hudson Bay

James Bay

ONTARIO

QUEBEC

TImmins.

GENERAL LOCATION MAP

GOLDEYE EXPLORATIONS LIMITED

GOLD ROCK PROPERTY Upper Manitou Lake Area, Ontario

NTS 52 F/7

so 100 150ml

100 200 km

Ottawa

U. S. A.

SPECTRAL IP/RESISIVITV & MAG SURVEY

Survey by.NX Ltd. ref : 4-32, July 2004 Figure 1

The topography is typical of the Canadian Shield. The mean elevation is about 350 metres (“m”) above sea level, with local relief of about 20 m at the tops of rounded hills. The peneplaned surface is punctuated with lakes connected by short rivers and streams. Muskeg is abundant in the low-lying areas. Bedrock composition and geological structure, coupled with regional glaciation control the size, shape and distribution of the lakes and muskeg areas. Lakes adjacent property flow westward into Rainy River via Lower Manitou Lake. Drainage from this area flows westward into Lake Winnipeg and ultimately Hudson’s Bay. 5.0 Property Location and Description The property location of the Gold Rock property is shown on Figure 1, in relation to significant geographical features. The property consists of seven contiguous unpatented claims registered 100% to Goldeye. The claims comprise 27 units covering a nominal 432 hectares (“ha”) as shown in Figure 2. Both surface and mining rights are attached to the claims. All of the claims are located within the Boyer Lake area (Claim Map G-2572) of the Kenora Mining Division, Ontario. There are no liens or encumbrances to the title, nor are there any registered aboriginal land claims or any known adverse environmental issues associated with the claims. The details of the claims are listed in Table 1, as follows: Claim No. Units/Area (ha) Record Date Due Date Work Req’s ($) Reserve ($)K 1133981 4/64 2002 Aug 07 2007 Aug 07 1,600 0 K 1133983 9/144 2002 Aug 07 2007 Aug 07 3,600 0 K 1133984 7/112 2002 Aug 07 2007 Aug 07 2,800 1,611 K 1133985 2/32 2002 Aug 07 2007 Aug 07 800 0 K 1133987 1/16 2002 Aug 07 2007 Aug 07 400 0 K 1133988 3/48 2002 Aug 07 2007 Aug 07 1,200 0 K 1183935 1/16 2002 Aug 07 2007 Aug 07 400 0 Totals 27/432 10,800 1,611 In Ontario, land tenure is maintained by completing $400 of “assessment work” per claim unit commencing in the second year after recording. Excess work credits can be “banked” and applied to subsequent annual work requirements. The above table indicates that $9,189 of work is required to maintain tenure of the claims beyond August 7, 2007. 6.0 History According to Harron (2003), the first geological reconnaissance of the area was undertaken by W. McInnes (1902) for the Geological Survey of Canada in the 1896-98 period. Gold deposits and in the Manitou Lakes-Lake of the Woods areas are documented by Coleman (1895, 1897, 1898), Bow (1898, 1900), Bow and Carter (1901), Carter (1902, 1904, 1905), Miller (1903), Corkill (1906, 1907, 1908, 1909, 1910), Parsons (1911, 1912) and Bruce (1925). In 1932, Thomson mapped the geology in the Manitou-Stormy Lakes area, and in 1933 mapped the adjacent Straw-Manitou Lakes area (Thomson, 1934). In 1937, Thomson (1942) described the gold occurrences at Gold Rock. Detailed mapping was undertaken by Blackburn (1976, 1979, 1981) in the area during 1972 and 1975, which is summarized in a report (Blackburn, 1982). Airborne electromagnetic and magnetic surveys were completed over the greenstone belt in 1979-80 (OGS, 1980), and in 2001 (OGS, 2001). Gold was first discovered in the Manitou Lakes region before 1894, and the local “gold rush” occurred from 1895 till 1912. Historically there were about 20 “mines” in the Gold Rock area, which would be currently classified as prospects. The principal mines in the camp were the Big

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CLAIM MAP GOLDEYE EXPLOAA T1 0 NS LIMITED

GOLD ROCK PROPERTY J Upper Manitou Lake Area, Ontario

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Master (production 1900-06, and 1942-43), the Laurentian (production 1906-09), and the Jubilee (Elora) with production from 1906-1907, and 1939. Interest in the area was renewed in the 1930’s, and some of the old mines and prospects were re-examined. This period also saw additional production from the Elora (1939) and the Big Master (1942-43 and 1947) deposits. After this activity, the area was once again dormant until the 1980’s. The Gold Rock claim group was prospected in the 1895 to 1912 period; however, very little data from this work is available. The presence of old pits on claims 1133981 and 1133983 provide evidence of activity in the area. In 1974, F. V. Regan drilled two holes totaling 62.5 m in the eastern half of current claim 1133981. The drilling was designed to test the Little Master and Volcanic Reef gold prospects. Assay results are not available (Blackburn, 1981). In 1975, G. Plummer owned a claim in the central part of current claim 1133981, east of patented claim HP299. No records documenting any exploration activity on the claim are filed with the Ontario Ministry of Northern Development and Mines (Blackburn, 1981). In 1981, Ari Resources Ltd. undertook magnetic and very low frequency electromagnetic (“VLF EM”) surveys on a group of 21 claims located northeast of the old Gold Rock mines (Harron, 2003). Four of these old claims overlap the eastern parts of current claims 1133981 and 1133983. The magnetic data illustrates a northeasterly trend, similar to that displayed in the airborne magnetic information. The VLF EM data correlated positively with bogs which also show a northeasterly trend, parallel to the regional foliation. In 1985, J. W. Redden and associates acquired 85 claim units along strike to the northeast of the old Gold Rock deposits. In 1990, J. W. Redden undertook a stripping campaign on current claim 1133981, which uncovered a sheared carbonatized zone approximately 100 m wide containing quartz veining and a 1.5 m wide zone of massive pyrite (Redden, 1990). The shear zone was traced for a distance of 520 m to the northeast and 200 m to the southwest. Twelve grab samples reported values values from <5 to 1063 parts per billion (“ppb”) gold. The highest value was associated with a sample of leached semi-massive pyrite. Parsons (1911) described this sulphide occurrence and considered it to be at the same stratigraphic level as the Laurentian and Jubilee gold deposits. Also in 1990, Aerodat completed a combined airborne VLF EM, magnetic and electromagnetic (“AEM”) survey at a line spacing of 100 m over most of J. W. Redden’s claims. The survey covers all of current claims 1133981, 1133983, 1133985 and 1133987, as well as most of claims 1133983 and 1133984. The magnetic survey illustrates a northeasterly trend. The AEM data did not detect the known sulphide occurrence or any other conductive zones. The VLF EM data generally shows northeasterly and northerly trend of surficial conductive materials In 1994, J. W. Redden contracted a 2.55 km induced polarization/resistivity (“IP/RES”) survey over selected lines located on the northern portion of current claim 1133983 (Gledhill, 1994). Prospecting was then carried out over the anomalous areas. The results indicate that the coincident resitivity low and chargeability high located on lines 10+00 N and 12+00 N of the East Grid are related to sheared and altered (carbonate-pyrite-silica) felsic rocks. Also in 1994, a 0.5 km MaxMin horizontal loop electromagnetic (“HLEM”) survey was performed. No bedrock conductors were located by this work (Redden, 1994).

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During 1995, two IP/RES anomalies were explored by mechanical trenching in the eastern part of current claim 1133983 (Redden, 1995). The anomaly at line 10+00 N/36+00 to 36+50 W was found to be associated with sheared and altered mafic volcanic rocks intruded by irregular felsic dykes and a 0.5 m quartz vein. The area at line 3+00 N/1+00 W was found to be underlain by relatively fresh mafic volcanic rock. No samples were collected at either location. In 1995, J. W. Redden commissioned spectral IP/RES and magnetic surveys on the east-central portion of what is current claim 1133983 (Redden, 1995). Two chargeability anomalies flanked by resitivity highs were detected over a 250 m width. Interpretation of the data indicates one high, one medium and one low priority targets in this area (JVX, 1997). This area corresponds to the alteration mapped in 1991 by Redden, and subsequently explored by a previous IP/RES survey and a partially successful mechanical trenching program. The magnetic data indicates a northeasterly trend to narrow anomalous features (Redden, 1997). Broad areas of subdued magnetic responses are attributed to both felsic and altered mafic rocks. 7.0 Regional Geology According to Harron (2003), the western part of the Archean age Wabigoon Subprovince is underlain by supracrustal rocks consisting of volcanic and lesser sedimentary rocks ranging in age from 3.0 to 2.71 Ga, which are intruded by granitoid batholiths and gabbroic sills and stocks which range in age from 3.0 to 2.69 Ga. Ten greenstone belts have been recognized in this portion of the subprovince, of which the current property is situated in the Eagle-Wabigoon-Manitou Lakes greenstone belt. This greenstone belt trends northeast and is bounded on the northwest by the Atikwa granitoid batholith and on the southeast by the Irene-Eltrut Lakes batholith, and the Meggissi granitoid pluton. The northeast trending, steeply southeast dipping Manitou Straits Fault (“MSF”) has been traced over a distance of 65 km along strike and bisects the greenstone belt. This fault is also considered to represent the eastern extension of the Pipestone-Cameron Fault located on the southwestern side of the Atikwa batholith (Figure 3). On the northwestern side of the MSF, the Blanchard Lake group apparently occupies the axial portion of the Manitou Anticline (Goodwin, 1970) and is considered to be the lowest stratigraphic assemblage in the area northwest of the MSF. The axis of the anticline strikes northeast and plunges northeast; however, the anticline is overturned as both limbs dip southeast. The Blanchard Lake Group tholeiitic basalts are predominately fine-to medium-grained pillowed and massive flows with well-developed flow top breccias. The western portion of the assemblage has been metamorphosed to amphibolite grade due to the intrusion of the Atikwa felsic batholith. Unconformably overlying the Blanchard Lake basalts is a thick assemblage of coarse calc-alkaline pyroclastics of intermediate to felsic composition, with a subordinate amount of interbedded tholeiitic basalts occurring along the limbs of the Manitou Anticline and called the Upper Manitou Lake Group (Unit 2, Figures 4 and 4a). Interbedded tuff breccias, lapilli tuff and fine-grained bedded tuff are the main rock units. The upper stratigraphic contact with the Benson Bay Subgroup (Unit 1, Figure 4) of the Pincher Lake group is characterized by decreasing amounts of pyroclastic material and an increase in the quantity of basalt. The Benson Bay Subgroup tholeiitic basalts are amygdaloidal, mainly massive flows, with lesser amounts of pillowed flows exhibiting well-developed flow top breccias. The western part of this sequence also exhibits amphibolite grade metamorphism caused by the Atikwa bathloith. Near its margin, the batholith comprises porphyritic and fine-grained phases of quartz monzonite, granodiorite and trondjemite. Radiometric age dates and the presence of basalt xenoliths imply that the marginal phases of the batholith are synvolcanic.

7

8

o Volcanic rocks

o Sedimentary rocks

o Granitic rocks

_ Mafic intrusion

-- Major fault

* GOLD ROCK Property

• Gold occurence

S i o ux Lookou t

o 20 40 60

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REGIONAL GEOLOGY MAP

GOLOEYE EXPLO RATIO NS LIMITED

GOLD ROCK PROPERTY Upper Man~ou Lak .. Area. Ontario

NTS52F{7

Flg .. J(e 3

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GOLD EYE EXPLORA llONS LIMITED

GOLD ROCK PROPERTY Upper Manitou Lake Area, Ontario

Base: OGS Map 2437; 1981 .NX ref: 4-32, July 2004 Figure 4 I

All of the supracrustal rocks have been intruded by numerous northeast striking felsic dykes and sills of Archean age. Diabase dykes of Mesoproterozoic age also intrude the entire supracrustal rock sequence. Balckburn (1976) mapped the MSF as a > 60 metre wide zone composed of carbonate-altered, highly fissile, schistose rocks. As interpreted by Parker (1989), there is about a 4 to 5 km wide belt of discreet, anastomosing sheared and altered structures to the northwest from the MSF. This broad alteration/tectonic zone is referred to as the Manitou Straits Deformation Zone (“MSDZ”) and it extends northeast through the Gold Rock area and encompasses most of the gold occurrences and past producing deposits. Airborne magnetic maps of the area (OGS Maps 82164, 82168) show a strong magnetic pattern trending northeast along the margins of the MSDZ. Within the confines of the MSDZ, the magnetic fabric is more chaotic, reflecting the presence of carbonate alteration, subsidiary structures and a mixed lithology of felsic and mafic volcanics, as

10

well as both felsic and mafic intrusions. The MSF, as interpreted by Blackburn represents the southeastern boundary fault of the broader MSDZ (Figures 4 and 4a). Airborne magnetic data (Figure 5) shows a good correlation with the mapped geology. Elevated magnetic intensity occurs on areas mapped as mafic volcanic rocks, with a concurrent decrease in the magnitude of the response over areas of felsic volcanic rocks. Linear magnetic lows within positive magnetic features, which follow the mapped bedrock structures can be correlated with shearing and hydrothermal alteration. Detailed mapping by Leonard (1984) indicates that the basal portion of the Benson Bay Subgroup comprises mostly chlorite schist with abundant magnetite mineralization. This unit has the highest magnetic susceptibility shown in Figure 5, and its distribution helps in the definition of the Manitou Anticline. The past producing mines of the Gold Rock district also appear to be associated with this positive feature. Airborne electromagnetic conductors within the MSDZ either mimic the strongly developed northeast striking magnetic and structural/stratigraphic fabric, or appear as “S” or “Z”-shaped conductive zones extending over several kilometers (Figure 5). This is consistent with re-activation of portions of the fault system with both dextral and sinistral shearing. Parker’s (1989) study of the gold deposits in the district showed that vein geometries reflected a history of both dextral and sinistral deformation overprinted by later vertical movement. Outside of the MSDZ, the magnetic pattern is more random and the electromagnetic conductors are defined as discrete responses. There are 61 known gold showings, occurrences, prospects and deposits in the Upper Manitou Lake area (Gold Rock mining camp), including three past producers: Laurentian Mine (1906-09), Elora (Jubilee) Mine (1906-07) and the Big Master Mine (1900-06, 1942-43). Ninety percent of the known occurrences are located within the MSDZ. Shear zones internal to the MSDZ trending north-northeast, northeast and east-west are the principal mineralized structures in the camp. Northerly trending brittle cross faults in the area appear to be post-mineralization and are associated with brecciation and fracturing of the host rocks. The Jubilee vein at the Laurentian and Elora mines, as well as the veins at the Big Master mine are all spatially associated with feldspar phyric mafic volcanic rocks. Wallrock alteration consisting of bleaching at all three deposits comprises sericitization, chloritization, ferroan and calcium carbonatization, and pyritization (1-5%) accompanied by tourmaline and fuschite over widths of 1.5 to 1.8 m. The mineralized veins consist of numerous grey-white quartz veins, stringers and lenses with visible gold and minor pyrite. The mineralized structures have strike lengths of 1 to 1.5 km, and the veins within them vary from a few centimeters to 4 metres in

11

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Ie ANOMALY SYMBOLS~ Conductance ClassificatiOr"l 1:1 > JO siemens

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GOLD EYE EXPLORATIONS LIMITED

GOLD ROCK PROPERlY Upper Manitou Lake Area, Ontario

NTS52 F/7 AIRBORNE MAGNETIC

and ELECTROMAGNETIC SURVEY Figure 5

width. The highly variable width is attributed to boudinaging and/or tectonic thickening. Total production from the camp amounts to approximately 376.4 kg gold derived from 43,627 tonnes mined sporadically during the 1900-1943 period. 8.0 Current Work Program The current work program consisted of geological surveying and sampling of zones of interest on both the pre-existing grid, established in 2004, as well as a newly cut grid representing the northern extension of the old grid. The old grid consisted six cross lines (L 0+00 to L 500 S) trending 102° and a baseline which trends 012°. The grid encompasses a total of 5.825 km including the baseline. It is mostly situated on claim 1133984, although L 500 S extends onto claim 1133985. The existing grid had been surveyed by IP/RES and magnetics in 2004. In order to establish the new grid, a baseline/tieline was cut at 012° from L 0+00/150 E of the old grid to L 500 N. A second baseline/tieline was turned off at L 500 N/350 E extending at 012° to 1175 N. Crosslines were cut at 100 m intervals from L 100 N to L-1100 N, generally extending from 650 E to the eastern shoreline of Double Lake. The total new grid established was 6.525 km including baselines/tielines. The grid is located on the northeastern portion of claim 1133984, the land portion of 1183935 and the western part of 1133983. Mapping was conducted along all of the lines including the baselines and tielines, with particular effort devoted to attempting to explain the IP/RES anomalies defined on the old grid. The field work was conducted during the period from July 16 to 25, 2007. IP/RES and magnetic surveys were in progress on the new grid while the author was conducting the geological mapping. 8.1 Property Geology The mapping demonstrated that the property is underlain by mafic, intermediate and felsic volcanic rocks, locally intruded by quartz-feldspar porphyry. Andesite and basalt are the main rock types encountered, with andesite predominating on the south and east parts of the grid, and basalt predominating to the west and north. A felsic tuff unit was located on the extreme southeastern part of the grid. Please refer to the Geology Plan, appended. Mafic Metavolcanic Rocks 1a, 1b, 1c Basalt This unit ranges from fine-grained through to coarse-grained (gabbroic) basalt. The fine- and medium-grained varieties are generally chlotite-rich, especially where foliated. It generally weathers medium to dark green-grey, with local dark green chloritic spots and is dark grey-green on the fresh surface. With increasing degrees of foliation the rock grades into chlorite schist. The coarse-grained variety is mottled dark green and pale green to white, and it weathers medium grey-brown. It consists of about 40% mafic minerals and 60% feldspar. 1d Chlorite Schist This rock is generally fine-grained, chlorite-rich and is strongly foliated. It is dark green on the fresh surface, and weathers a dark green-grey colour. Intermediate Metavolcanic Rocks 2a, 2b Andesite The andesite varies from fine-grained through to coarse-grained and is generally fairly massive. The finer-grained varieties generally weather pale-medium grey, and are medium greenish grey on the fresh surface. The coarser-grained rock is mottled pale to medium grey and green with small dark green spots on the fresh surface. It weather pale-medium grey. The andesite is generally fairly hard.

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2c Intermediate Tuff This unit is fine- to medium-grained texturally, and it is greenish grey with light brown spots, consisting largely of feldspar and chlorite. It locally contains sericite-rich, more felsic bands, less than 25 cm thick. 2d Intermediate Lapilli Tuff This rock unit was observed at the western end of L 900 N. It consists of a matrix of fine-grained chlorite with lesser sericite, with a variable quantity of intermediate, and minor felsic fragments, which due to the strongly foliated nature of the rock, are now stretched up to 25 by 7 cm. The fragments are often only vaguely outlined. The rock weathers streaky pale-medium grey and medium-dark brown. At this locale, the rock contains several boudins of white quartz up to 1 by 0.3 m in dimension. The foliation trends 255°/70°NW and kink banding is locally present. 2e Chlorite-Sericite Schist This rock is strongly foliated and consists of chlorite and sericite in various proportions. It breaks apart into fairly thin plates. It generally weathers a tan to pale-medium green-grey colour with dark green streaks and pale grey patches. Fresh surfaces are tan with pale-medium green-grey streaks. It is generally fine-grained texturally. Locally can be silicified and very hard. Felsic Metavolcanic Rocks 3a Dacite The dacite ranges from aphanitic to fine-grained and is very hard. It is pale to medium grey on the fresh surface and weathers variably from pale to dark grey. 3b Felsic Tuff On the fresh surface the felsic tuff ranges from streaky pale grey-green and white with brown specks to pale grey-brown with a pale reddish tinge. It weathers a pale grey colour. It often contains up to 5% very fine-grained disseminated pyrite. It is generally fine- to medium-grained, locally containing minor quartz crystals and quartz crystal clusters up to 1 cm x 2 mm in size. 3c Sericite Schist The sericite schist is fine-grained, and it weathers from a tan colour to blotchy pale grey. Where minor disseminated pyrite is present, the partings are rusty. On the fresh surface it is shiny, and varies from pale to medium grey or greenish grey and tan coloured with local brown spots. It is very fissile and breaks apart into thin plates. Locally it is silicified and hard. Felsic Hypabyssal Rocks 5a Quartz-Feldspar Porphyry This rock generally comprises mostly feldspar, with 10-15% quartz pnenocrysts < 2 mm in size, and 10-15% mafic minerals. It is medium-grained texturally. On the fresh surface it is mottled pale grey, green and white, whereas it weathers pale grey with white spots to cream coloured. 8.2 Structural Geology Foliations on the southern part of the grid (L-500 S to L0+00) trend northeasterly, whereas two foliation readings around 100 E on L 300 N trend more northerly. From L 400 N to L 800 N, the foliation again exhibits a northeasterly trend. The presence of sericite schist near the eastern ends of line 600 N and 700 N, coupled with the presence of chlorite and chlorite-sericite schist around

14

150 E to 300 E between lines 400 N and 500 N, suggests the presence of a shear zone extending from near the east end of L 600 N to about L 400 N/150E. This interpreted shear zone would also explain the complex position of the lithologic units in this area. It is postulated that this shear zone strikes approximately 255° and dips 75° NW to vertically. A second shear zone is also interpreted at around L 1000 N, where the foliation again trends approximately 255°/65° to 70° NW, whereas foliations both north and south of this area trend in the more common northeasterly direction. A swamp/creek/beaver pond located in this area probably represents the trace of the shear zone. A quartz vein up to 2 metres wide associated with chlorite and chlorite-sericite schist trending about 040°/75° NW is located on a peninsula about 150 metres west of the western end of L 0+00 at UTM (datum NAD 27 Canada) 521249E/5478855N. It is possible that this zone also represents a shear zone trending northeast near the southeastern shore of Double Lake. If samples collected from this area report any gold values of interest, the intersection of this structure and the more east-west oriented structure located about L 1000 N may be of exploration interest. Mapping by Blackburn (1981) shows an assumed fault which trends north through the grid at about 400 E. While no direct evidence for the existence of this fault was observed in the field within the limited area mapped by the author, its interpreted location correlates with a northerly trending creek/cedar swamp. 8.3 Mineralization An outcrop of felsic tuff was observed at L 400 S/250 W. It contains 1-5% very finely disseminated pyrite and is moderately foliated at 225°/65°NW. This outcrop correlates with IP chargeability zone IP-2 (JVX, 2004), and it is probably the source of the anomaly. Sample 66465 was collected from this locale. Three small pits (maximum size 3 x 2 metres) over a length of about 12 metres were located at L 315 S/0 +05 W. These pits are aligned at 340° and are now mostly water filled. A small outcrop at the northwest end of the central pit is highly fractured at 210°/80°SE. Rubble around the pits locally comprises semi-massive pyrite in altered basalt (?), with minor quartz veining. Sample 66464 was collected from the mineralized rubble around the trench, and this material represents the explanation for IP anomaly IP-1a’. A small pit was observed at L 400 S/0 + 27 E. The north wall of the pit exposes moderate to highly foliated (055°/75°NW) basalt. Sample 66467 consists of white quartz with local hematite staining and 5-15% pyrite that was collected from the rubble around the trench, but was not observed in the trench. Sample 66468 comprises 10-25% pyrite, disseminated and as stringers in highly altered, bleached and sheared basalt. This material was also collected form the rubble and could not be observed in the trench. This material represents an explanation for IP anomaly IP-1a. Sample 66477 is located slightly west of this IP anomaly at L 425 S/0+15 E, wherein a small trench exposes semi-massive (30-40%) pyrite over a true width of about 1 metre. This material is undoubtedly associated with the anomalous IP responses located in this area as well. An outcrop of fine-grained basalt at L 0+20 S/185 E contains up to 5% disseminated pyrite. Another outcrop located at L 300 S/130 E also comprises basalt with up to 5% disseminated pyrite. Sample 66466 was collected from this latter area. This type of material probably provides an explanation for anomaly IP-1b.

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Samples 91901 to 91910 were collected by Joe Gamblin of JVX from a series of small outcrops located about 20 metres southeast of the point of a peninsula located about 150 metres west of the western end of L 0+00. This area is located about 250 metres south of the northern limit of claim 1133984. These small outcrops were under water when visited by the author. These samples represent quartz veining, locally with semi-massive pyrite mineralization, in chlorite schist foliated approximately 040°/75°NW. Sample 91916 is located on the point of the peninsula, and it is from a northeast trending white quartz vein up to 2 metres wide with local patches of pyrite hosted by andesite sheared at 225°/80°NW. A small pit measuring 5 x 2.5 x 3 m deep has been blasted into this quartz vein immediately northeast of sample 91916. The author collected grab sample 66471 from the 30 cm wide quartz vein on the northeast wall of the pit. Here the quartz is grey in colour and it contains 5-10% pyrite. Sample co-ordinates are 521249E/5478855N, and they are described in the sample description sheets appended to this report. This zone may be indicative of a northeasterly trending shear zone located near the southeast shore of Double Lake. 9.0 Sampling Method and Analyses The author collected grab samples of any rocks which appeared to be of interest. These include highly sheared material, quartz veined material as well as any material containing appreciable sulphide mineralization. Samples were located with respect to grid co-ordinates as well as UTM co-ordinates (datum NAD 27 Canada). Blank samples were inserted at random intervals into the sample sequence for quality assurance/quality control purposes. A total of 25 samples, including blank samples, were collected by the author. An additional 27 samples were collected by Joe Gamblin and Leo Villamor, who were part of the crew employed by JVX Limited to cut the grid and carry out the geophysical surveys. These samples were collected from the shore of Double Lake and were located by UTM co-ordinates. The author visited these sample sites and described the samples as per the sample description sheets attached. The samples were shipped to Activation Laboratories in Ancaster, Ontario for standard gold fire assay, as well as multi-element (34 elements) analyses. Analytical results have not yet been received. 10.0 Interpretation and Conclusions The author conducted a mapping and sampling program on Goldeye Explorations Limited’s Gold Rock property from July 16 to 25, 2007, which covered 12.35 km of pre-existing and new grid lines located on the southeastern shore of Double Lake. Grid line establishment, magnetic and IP/RES surveys were underway during the course of the author’s work. A total of 25 samples were collected by the author, and an additional 27 samples were collected by JVX Ltd. personnel who were conducting the grid establishment/geophysical surveying. Unfortunately the analytical results from the samples have not yet been receive, nor have the results of the geophysical work on the new grid lines been seen. Consequently, the interpretation and conclusions in this report are preliminary in nature and will be expanded upon when all of the data have been received. The area mapped is underlain by a sequence of mafic, intermediate and felsic volcanic rocks, with local small intrusions of quartz-feldspar porphyry. The predominant trend of the foliation in the rocks in the area is northeast. Two east-northeast trending shear zones are interpreted to transect the area at approximately L 500 N and at L 1000N. These cross structures may represent zones of enhanced dilation, especially where they intersect northeast trending shear zones. Several of the IP/RES anomalies defined by JVX (2004) on the pre-existing grid were explained by the geological work. Anomaly IP-2 is believed to be related to up to 5% pyrite occurring in a

16

felsic tuff at L 400 S/2+50 W (sample 66465). Samples 66467 and 66468 were collected from rubble around a small pit at L 400 S/0+27 E. The rubble contains quartz and 5-25% pyrite in altered basalt which explains anomaly IP-1a. Up to 5% disseminated pyrite in basalt probably is the source of anomaly IP-1b, and sample 66466 was collected from L 300 S/130 E within this anomalous response. Samples 91901-19910, 91916 and 66471 were collected from near the end of a small peninsula in Double Lake located at UTM 521249E/5478855N, about 150 west of the western end of L 0+00. This area is characterized by quartz veining up to 2 metres wide with local heavy pyrite mineralization. This material is possibly indicative of a northeasterly striking shear zone trending near the southeastern shore of Double Lake. If any gold values of significance are reported from the samples, this zone will represent an exploration target, especially at its possible intersection with the east-northeast trending shear zone interpreted near L 1000 N. In the field, the IP/RES crew was requested to survey the northern portion of baseline/tieline 3+50 E, in order to determine if the shear zone located around L 1000 N responds. If it does, this will further enhance the possible structural intersection mentioned above. In the absence of the analytical results from the sampling, as well as the results of the geophysical surveying, it is difficult to determine specific recommendations. However, the author is of the opinion that the geophysical surveying should be extended to the west over a portion of Double Lake during the winter months. The exact orientation of the grid lines should be determined upon receipt of all of the relevant data, in order to test the possibility that zones of exploration interest may strike both northeast, as well as east-northeast. William S. Hamilton, P.Geo. W. S. Hamilton Geological Consulting Ltd. July 31, 2007

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References Blackburn, C.E., 1976, Geology of the Lower Manitou-Uphill Lakes Area, District of Kenora; Ontario Div. Of Mines, Geoscience Report 142, 81p., accompanied by Map 2320, scale 1:31,680. Blackburn, C.e., 1979, Geology of the Upper Manitou Lake Area, District of Kenora; Ont. Geol. Surv. Report 189, 74p., accompanied by Map 2409, scale 1:31,680. Blackburn, C.E., 1981, Geology of the Boyer Lake-Meggisi Lake Area, District of Kenora; Ont. Geol. Surv. Report 202, 107p., accompanied by maps 2437 and 2438, scale 1:31680. Blackburn, C.E., 1982, Geology of the Manitou Lakes Area, District of Kenora (Stratigraphy and Petrochemistry) Ont. Geol. Surv. Report 223, 61p., accompanied by Map 2476, scale 1:50,000. Blackburn, C.E. and Hinz, P., 1995, Kenora Resident Geologist’s District-1994; in Report of Activities 1994, Resident Geologists, eds. Baker, C.L., Dressler, B.O., Laderoute, D.G. and Newsome J.A., Ont. Geol. Surv. Open File Rept. # 5921, p. 19-42. Bow, J.A., 1898, Mines of Northwestern Ontario; Ont. Bur. Mines, Ann. Rept, v. Vii, pt 1, sec 3, p. 35-84. Bow, J.A., 1900, Mines of Northwestern Ontario; Ont. Bur. Mines, Ann. Rept., v. IX, sec. 3, p. 35-88. Bow, J.A. and Carter, W.E.H., 1901, Mines of Northwestern Ontario, Parts 1 and 2; Ont. Bur. Of Mines, Ann. Rept., v. X, sec. 4, p. 69-112. Bruce, E.L., 1925, Gold Deposits of Kenora and Rainy River Districts, Ont. Dept. Mines, Ann. Rept., v. XXXIV, pt. 6, p. 1-42. Carter, W.E.H., 1902, The Mines of Ontario; Ont. Bur. Mines, Ann. Rept., v. XI, pt. 1, p. 231-298. Carter, W.E.H., 1904, Mines of Western Ontario; Ont. Bur. Mines, Ann. Rept., v. XIII, pt. 1, p. 58-87. Carter, W.E.H., 1905, Mines of Western Ontario; Ont. Bur. Mines, Ann. Rept., v. XIIV, pt. 1,sec. 3, p. 43-75. Coleman, A.P., 1895, Second Report on the Goldfields of Western Ontario; Ont. Bur. Mines, Ann. Rept. V. V, sec. 2, p. 47-106, accompanied by Maps 5A & 5B, scale 1:126,720. Coleman, A.P., 1897, Third Report on the West Ontario Gold region; Ont. Bur. Mines, Ann. Rept., v. VI, p. 71-124. Coleman, A.P., 1898, Fourth Report on the West Ontario Gold Region; Ont. Bur. Mines, Ann. Rept, v. VII, pt. 2, sec. 1, p. 109-150. Corkill, E.T., 1906, Mines of Ontario; Ont. Bur. Mines, Ann. Rept., v. XV, sec. 3, p. 47-107.

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Corkill, E.T., 1907, Mines of Ontario; Ont. Bur. Mines, Ann. Rept., v. XVI, pt. 1, sec. 3, p. 55-91. Corkill, E.T., 1908, Mines of Ontario, Ont. Bureau Mines, Ann. Rept., v. XVII, sec. 3, p. 58-94. Corkill, E.T., 1909, Mines of Ontario, Ont. Bur. Mines, Ann. Rept., v. XVIII, pt. 1, sec. 2, p. 79-140. Corkill, E.T., 1910, Mines of Ontario, Ont. Bur. Mines, Ann. Rept.., v. XIX, pt. 1, sec. 3, p. 78-130. Gledhill, T., 1994, Goldrock Project, Southwestern Part of Boyer lake Area, Kenora Mining Division, Ontario, 4p., 3 figs., AFRI # 2.1543. Harron, G.A., 2003, Qualifying Report on Goldrock Property For Goldeye Explorations Limited, Kenora M.D., Ontario, 27 p. JVX Ltd., 1997, Logistical and Interpretative Report on Spectral IP/Resistivy Survey conducted in the Boyer Lake Area, Kenora Mining Division, NW Ontario for J. Redden, H. Lundmark, & W. McAteer, 14p., pseudo-sections and plan. JVX Ltd., 2004, Report on IP/Resistivity and Magnetic Surveys, Gold Rock Property-Ontario for Goldeye Explorations Limited, 25 p., pseudo-sections, plus 5 plans. Leonard, K.W., 1984a, Report on a Geological Survey, Goldrock Claim Group; St. Joe Canada Inc., Ont Geol. Surv. Assessment File # 2.7374. McInnes, W., 1902, Manitou Lake Sheet, Geol. Surv. Can., Map 720, scale 1:253,440. Miller, W.G., 1903, Mines of Northwestern Ontario; Ont. Bur. Mines, Ann. Rept., v. Xii, pt. 1, p. 73-107. Neilson, J.N. and Bray, R.C.E., 1981, Feasibility of Small Scale Mining in Northwestern Ontario (parts of the Districts of Kenora, Rainey River and Thunder Bay), Ont. Geol. Surv. OF # 5332, 132 p. OGS, 1980a, Airborne Electromagnetic and Total Intensity Magnetic Survey, Manitou-Stormy Lakes Area, District of Kenora; by Kenting earth Sciences Limited for the Ontario geological Survey, Geochemical/geophysical Series, Map 80464, scale 1:20,000. OGS, 1980b, Airborne Electromagnetic and Total Intensity Magnetic Survey, Manitou-Stormy Lakes Area, District of Kenora; by kenting Earth Sciences Limited for the Ontario Geological Survey, Geochemical/Geophysical Series, Map 80465, scale 1:20,000. OGS, 1980c, Airborne Electromagnetic and Total Intensity Magnetic Survey, Manitou-Stormy Lakes Area, District of Kenora; by Kenting earth Sciences Limited for the Ontario Geological Survey, Geochemical/Geophysical Series, Map 80471, scale 1:20,000. Parker, J.R., 1989, Geology, gold mineralization and property visits in the area investigated by the Dryden-Ignace Economic Geologist, 1984-1987; Ont. Geol. Surv. Open File 5723, 306 p.

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Parker, J.R. and Perrault, M., 1988, Gold studies in the Manitou Lakes-Stormy Lake Belt, Districts of Kenora and Rainy River; in Summary of field work and other activities, 1988, eds. Colvine, A.C., Cherry, M.E., Dressler, B.O., Thurston, p.C., Barlow, R.L. and Riddle, C., Ont. Geol. Surv. Mics. Paper 141, 9 126-131. Parsons, A.L., 1911, Gold Fields of lake of the Woods, Manitou and Dryden, Ont. Bur. Mines, Ann. Rept., v. XX, pt 1, p.158-198. Parsons, A.L., 1912, Gold Fields of lake of the Woods, Manitou and Dryden; Ont. Bur. Mines, Ann. Rept., v. XXI, pt. 1, p. 169-204. Redden, J.W., 1990, OPAP Report, Boyer/Turtlepond Lakes Area, 8 p., plus Aerodat Survey, AFRI # 2.13808. Redden, J.W., 1991, Report on Geological Survey Claims K 1105369 et al, Boyer Lake Area, Kenora Mining Division, 12 p., AFRI # 2.14414. Redden, J.W., 1994, Report on 1994 maxMin Survry, Goldrock project Boyer Lake Area, kenora Mining Division, 4 p., AFRI # 2.15943. Redden, J.W., 1995, Report on 1995 Stripping, Goldrock Project, Boyer lake Area, Kenora Mining Division, Onatrio, 4 p. Redden, J.W., 1995, Preliminary Report on 1997 magnetic Survey, Goldrock project, Boyer Lake Area, Kenora Mining Division, 3 p., AFRI # 2.17635. Redden, J.W., 1997, Summary Report on 1997 Exploration Program, Goldrock Project, Boyer Lake/Turtlepond Lake Areas, Kenora Miming Division, Ontario, 3 p., AFRI # 2.18210. Thomson, J.E., 1934, Geology of the Manitou-Stormy Lakes Area; Ont. Dept. Mines, Ann. Rept., v. XLII, pt. 4, p. 1-40, accompanied by Map 42c, scale 1:63,360. Thomson, J.E., 1942, Some Gold Deposits near Goldrock, Upper Manitou lake; Ont. Dept. Mines, Ann. Rept. V. XLVII, 10 p., accompanied by Map 47k, scale 1’ = 400’. Vamos, P.J., 1981, Report on a Magnetic Survey, Goldrock Property, Kenora M.D., Ontario, for Ari resources Ltd., 2 p.

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WILLIAM S. HAMILTON 459 Millwood Road

Toronto, ON M4S 1K4

Telephone: 416-482-1097 Fax: 416-482-5203 Email: wshamil@aol.com

CERTIFICATE OF AUTHOR

I, William Hamilton, P.Geo. do hereby certify that:

1. I am a consulting geologist and President of W. S. Hamilton Geological Consulting Ltd., with a business address at 459 Millwood Road, Toronto, Ontario, M4S 1K4.

2. I am a graduate of Mount Allison University, Sackville, New Brunswick, with a

B.Sc. in Geology (1973).

3. I am a member of the Association of Professional Geoscientists of Ontario.

4. I am a member of the Canadian Institute of Mining and Metallurgy, the Prospectors and Developers Association of Canada, the Society of Economic Geologists and a Fellow of the Geological Association of Canada.

5. I have worked as a geologist for a total of 34 years since my graduation from university, including 17 years with Campbell Resources Inc. as Regional Geologist and Exploration Manager, four years with Corona Corporation as Senior Geologist, six years with Bitech Corporation as Exploration Manager and seven years as a consultant.

6. This Geology Report on the Gold Rock Property has been prepared for filing with

the Ontario Ministry of Northern Development and Mines for assessment credit.

Dated at Richmond Hill, this 31st day of July, 2007. “William S. Hamilton” ___________________ [Seal or Stamp] Signature of Qualified Person of Qualified Person] “William S. Hamilton” William S. Hamilton Print name of Qualified Person 21

A P P E N D I X

GOLDEYE EXPLORATIONS LIMITEDGOLD ROCK PROPERTYSAMPLE DESCRIPTION SHEET

Samples Collected by W. HamiltonJul-07

DATUM NAD 27 Canada

Sample # UTM E UTM N Width DescriptionLine E Line N

66454 522058 5479454 grab Chl-Ser-Qtz schist, str fol't 260/65N. Weath tan withdk gn streaks and pale gy patches. Fresh 350E 865N tan with pale-med gy-gn streaks. Tiny o/c. Hard, vfrg.

66455 522042 5479476 grab Chl schist, minor ser & Qtz, str fol't 255/70NW. Fragmental appearance with stretched frags to 325E 905N 25x7 cm, prob orig Inter Lapilli Tuff. Minor kink bands and Qtz boudins to 1x0.3 m. Fgr, weath

streaky pale-med gy & med-dk bn. Fresh = med gy.66456 522250 5479453 grab Ser-Chl schist, fgr, str fol't 220/85NW. Weath pale-med gy-gn & tan, blotchy, streaky. Fresh

545E 900N med-dk gn-gy with tan coloured partings. Predom chl, wk ser.66457 522270 5479354 grab Perdom ser schist with some bands? Chl schist. Mod-str fol't 235/75S. Ser schist weath

590E 800N shiny tan. Pale grey and tan on Fresh surface. Chl schist weath dk gy. Fresh dk gy-gn. Fgr.66458 522188 5479356 grab Mod-str fol't chl-ser schist.

503E 800N66459 522293 5479237 grab Chl-ser schist. Fresh is pale-med gy, weath pale gy to tan. Mod fol't 240/75NW. Trace py & qtz

630E 700N66460 522304 5479234 grab Ser schist. Str fol't 235/90. Very fissile, breaks in thin plates. Fresh pale-med gn-gy. Weath

645E 700N pale gy to tan, blotchy.66461 522269 5479197 grab Ser schist. Str fol't 050/82NW. Fresh pale gy, weath pale gy, loc bn patches. Rare tr py. Fgr.

595E 650N Mod sil.66462 522222 5479157 grab Mod sil ser schist. Fresh pale gy and lt bn to tan, streaky. Fgr. Weath pale gy to tan, rusty

565E 615N partings. Tr-2% py finely dissem.66463 521666 5478656 grab Fairly mass, med-dk gy-gn, fgr basalt. Minor sugary QCV in o/c rubble.

140E 0+0066464 521478 5478413 grab 3 pits, max size 3x2 m aligned 340 deg over 12m length. Water filled. Semi-mass py in altered

0+05W 315S dk gn basalt(?). Local qtz veining. Hi fract 210/80SE. Samp = grabs of semi-mass py, some QV and chl basalt from o/c rubble.

66465 521213 5478301 grab Felsic tuff mod fol't 225/65NW. Fresh streaky pale gy-gn and white with bn speckles. Weath 250W 400S pale gy. !-5% finely dissem py. Tuff mgr, loc qtz xtals and xtal clusters to 10x2 cm.

Sample # UTM E UTM N Width DescriptionLine E Line N

66467 521487 5478299 grab Pit. N wall = mod-hi fol't basalt 055/75NW. Dk gy-gn. Basalt contains tr-2% vfgr dissem py.0+27E 400S Sample of white qtz, loc hem stain. 5-15% py from o/c rubble (py zone not observed in pit).

66468 521487 5478299 grab Sample from same area as 66467. Sample = 10-25%py dissem and stringers in hi alt'd,0+27E 400S bleached and sheared basalt(?).

66469 520866 5478327 grab QV under water by lake shore. Attitude unknown, but at least 0.5m wide. White, grey & clear 600W 510S mottled qtz with 5-10% lt bn ankerite.

66470 521853 5478103 grab Felsic tuff. Pale gy-bn with pale reddish tinge. Hi sil, fgr. Wk-mod fol't 040/85NW. 2-3% fgr 430E 503S dissem py, minor QV <1cm.

66471 521249 5478855 grab Pit on peninsula about 150m W of W end of L500S. Pit 5x2.5x3m deep blasted in QV. SW side of pit QV is white, barren and 2 m wide. NE pit wall QV only 30 cm wide, but dense gy Qtz with 5-10% py stringers near vein margins. Sample of gy pyritic QV on NE pit wall.

66472 5211187 5478737 grab Hi deformed kink banded chl schist zones in orig prob pillowed basalt loc about 100m at 260deg from W end L0+00. Mod erratic white bull QV <10cm wide main trend 250/90. Grabs ofseveral of the small QV's.

66473 521029 5478687 grab Wk-mod sheared (235/80SE0 basalt. Approx 25% QV and Qtz blobs <25 cm wide over 2 mwidth. Samp = grabs of several of the QV's.

66474 521423 5479735 grab Blank sample. Med gr. Andesite. 1-2% dissem Py.66475 522229 5478945 grab Up to 30 cm wide sinuous QV gen 045/steep SE in mgr, med gy-gn andesite. Qtz is white.

630E 405N66476 521625 5478757 grab Several Qtz blocks to 40x30x30 cm, angular, near source but not observed in place.

0+60E 100N Mottled pale gy and white, minor honey-coloured staining. Host prob QFP ?66477 521488 5478323 grab Trench 5.1.5x1m deep. Altered basalt. Minor QV, mod sil. 5-15% py patches and stringers.

0+15E 425S Also semi-mass py (30-40%) over 1m true width. O/c prob not in place, but trend appears170/80E.

GOLDEYE EXPLORATIONS LIMITEDGOLD ROCK PROPERTYSAMPLE DESCRIPTION SHEET

Samples collected by Joe Gamblin and Leo VillamorJune/July, 2007DATUM NAD 27

Sample # UTM E UTM N Width Description91901 521231 5479051 grab Samp from island in Double Lake. Sericite schist, minor qtz, 1-5% py assoc with glassy qtz.

Samps 91901-10 are all from same location = outcrop now under water near island at W end ofL-0+00. Sample 91916 is nearby on the island by a small pit.Host is chlorite schist 040/75NW with loc. Very heavy Py in both schist and quartz.

91902 521231 5479051 grab As above but mostly mottled white & grey qtz with 1-2% mgr. py. Some sericite schist.91903 521231 5479051 grab White qtz with 1% Py, minor sericite schist.91904 521231 5479051 grab White and grey mottled Qtz, 1% Py, minor sericite schist.91905 521231 5479051 grab Mottled grey and white Qtz with 1-5% mgr. Py.91906 521231 5479051 grab Qtz-Chl schist, 5-8% cgr Py kink bands91907 521231 5479051 grab Chlorite schist impreganated with 30-40% white, lesser grey Qtz and 5-10% cgr Py.91908 521231 5479051 grab sheared basalt, mod-hi sil, 10% pale grey and white Qtz stringers and patches <5mm. 5% cgr

Py stringers <5mm kinked and assoc with Qtz.91909 521231 5479051 grab sheared basalt, mod-hi sil, 10% pale grey and white Qtz stringers and patches <5mm. 5% cgr

Py stringers <5mm kinked and assoc with Qtz.91910 521231 5479051 grab Sericite schist, sil and Qtz veined, 5-10% mgr Py.91911 grab Pale grey and white mottled Qtz, 1-3% Py dissem along fracts.91912 521423 5479735 grab Blank sample. Med gr. Andesite. 1-2% dissem Py.91913 521768 5479352 grab Chlorite schist, minor QV, 1-2% mgr dissem Py.91914 521768 5479352 grab Chlorite schist, weak QCV, trace Py.91915 521768 5479352 grab Chlorite schist, wk-mod QV, 1-10% fmgr Py.91916 521225 5479070 grab Silicifies sericite schist, 1-15% cgr Py dissem along schistosity.91917 521225 5479070 grab (Chl)-sercite schist, mod-hi QV (white), 10-15% cgr dissem Py.91918 521046 5476911 grab Fgr med gy-gn Andesite, very minor sericite schist, wk-mod QV, <1% dissem Py.91919 522043 5479811 grab Cgr, med-dk grey-green andesite, weak QV, 1-5% dissem Py.91920 521423 5479735 grab Chlorite schist, hi QV, 1-3% dissem Py.91921 521423 5479735 grab Massive basalt, minor Qtz on fract planes.91922 521667 5479149 grab Massive basalt, <1% Py.91923 521667 5479149 grab Weak shaered basalt, 5% dissem Py.

Sample # UTM E UTM N Width Description91924 522194 5479050 grab White to pale green felsic tuff(?). Minor QV, trace Py.91925 521423 5479735 grab Blank sample. Med gr. Andesite. 1-2% dissem Py.91926 522043 5479811 grab White Qtz with very minor sericite schist, 1-2% Py dissem along schist/Qtz contact.91927 grab Dk green basalt with wk-mod Qtz veinlets <5mm wide with <1% Py assoc with the Qtz.