The Cobalt Rainbow. Airborne geophysical maps show that a north trending aeromagnetic high suggests further undiscovered mineralisation.

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1 The Cobalt Rainbow The property is located on Greenstone Creek, approximately 4.8 kilometres south west of the creek mouth. The property is located about 24 km due west of Campbell River, in the east-central area of Vancouver Island. Good road access is available by a network of logging roads in the general area of the claims. The property covers a magnetite-pyrrhotite-chalcopyrite skarn exposed in Greenstone Creek Minfile # 092F 237 was worked from 1916 to 1917, resulting in the mining of 83 tonnes of ore producing 14, 018 kgs of copper, 4,074 gms of silver and 31 gms of gold. Workings consisted of several large open-cuts and two adits, with possibly three more adits driven in the years following (pre-1955). Chip samples taken by Gunnex Mines in 1965 along a 45m length of canyon wall on Greenstone Creek (main showing) returned an average of 1.18% Cu largely from the magnetite-pyrrhotite skarn band. In 1967, underground and surface drilling (>1000 feet) was conducted on the Greenstone Creek Property by Georgia Mines Ltd. This work showed high grade lenses (up to 4% Cu and up to 5m intersections) within a diopside garnet skarn approximately 5m lower than the main surface showing. A follow-up airborne geophysical and ground geochemical surveys on the Greenstone Creek Showing, Reverted Crown Grants L1215 and L1216, northwest of Becher Lake was conducted in Airborne geophysical maps show that a north trending aeromagnetic high suggests further undiscovered mineralisation. The main skarn showing seems to form a lens or lens-like body about 3 metres thick and 46 metres long, dipping about 20 degrees to the north. Minerals present in the skarn include fibrous greenish amphiboles, garnet, possibly vesuvianite, calcite, chlorite, magnetite, pyrrhotite, pyrite, chalcopyrite, and minor sphalerite. The magnetite and pyrrhotite are massive and most abundant. The chalcopyrite is more erratic and patchy but, at one location, does occur massively, over a width of 30 centimetres.

2 In 1965, sixteen samples taken along a 45 metres strike length of the main showing yielded from 0.15 to 4.6 per cent copper with an average of 1.18 per cent copper (Assessment Report 699). In 1996, sampling of a mineralized vein exposed in an adit assayed 2.53 per cent copper, 4.0 grams per tonne silver, grams per tonne gold, per cent cobalt, per cent cadmium and greater than 5.0 per cent zinc over 0.6 metre (Assessment Report 24571). In 1998, sampling of the No.2 adit yielded values up to 6.17 per cent copper, 17.8 grams per tonne silver and per cent zinc (Sample A7; Assessment Report 25809).

3 The old mine workings are on the north side of a deep canyon, through which Greenstone Creek flows, and about 30 metres above the river bed. As of 1916, the workings consisted of several large open cuts and two adits, the latter 18 and 9 metres in length. The South Side showing is located on the south side of Greenstone Creek across from the main workings. Locally, disseminated chalcopyrite is hosted by a volcanic breccia. In 1998, grab sampling yielding up to 10.0 grams per tonne silver and per cent copper ; previous sampling of the zone has reportedly yielded up to 1.0 per cent copper (Assessment Report 25809). The Canyon showing is located approximately 100 metres downstream of the main workings and consists of chalcopyrite filling fractures in a porphyritic basalt. In 1965, Gunnex Limited completed a program of geochemical sampling, geological mapping and ground magnetic and electromagnetic surveys on the area as the M and Thelma claims. In 1969, Georgia Mines completed an airborne magnetic survey on the area. This work identified four areas of anomalously high response and three areas of anomalously low response to the north of the former workings (Assessment Report 2507). In 1996 and 1998, A. Doiron completed programs of geological mapping and rock and soil sampling on the area as the Allana claims. The Stellar occurrence is located on a small hill, approximately 1 kilometre west of Becher Lake. The area is underlain by Upper Triassic Vancouver Group, Quatsino Formation limestone and calcareous shales overlain by Karmutsen Formation volcanics. These Karmutsen rocks consist of andesitic tuff, andesitic volcanic breccia and flows with interbeds of argillite, siltstone and limestone. Intruding the stratigraphy are plutonic rocks of the Jurassic Island Plutonic Suite. These plutonic rocks on Vancouver Island vary in composition from gabbro to quartz monzonite but are mainly granodiorite and quartz diorite. The showing is associated with intrusions of a medium to coarse grained diorite with associated regions of coarse grained magnetic gabbro. These

4 intrude a fine grained moderately silicified andesitic lava which is locally bleached and cut by epidote and calcite veins. The mineralization occurs in a silicified-carbonate shear structure occurring within a 6 metre wide rusty orange zone. This structure is enveloped in a 10 to 15 metre wide zone of prominent chlorite/magnetite replacement occurring as kidney shapes and amoeboid blobs in the host rock. The zone is mineralized with massive to semi-massive pyrite plus or minus chalcopyrite and sphalerite. Associated with the sulphide mineralization is quartz and sericite. In 1987, sampling of high grade sulphide material yielded values up to 2.84 per cent copper, 16.4 grams per tonne silver, 3.24 per cent zinc and 7.12 grams per tonne gold (Assessment Report 17405).

5 Previous surveys indicate that fairly high Vanadium, Gold and Copper in the North West part of the property occur in soil samples. Assaying was done by Chemex Labs Ltd. of North Vancouver using standard ICP. Some elements required nitric-aqua regia digestion. Dry Sieve to -80 mesh. Gold Values in soil Range from 10 ppb to I60 ppb. Vanadium Values Range from 4 ppm to 586 ppm. Of 215 samples, 180 showed well above background. A good correlation appears to exist with Vanadium. The volcanics, probably Karmutsen, consist of a dark green, amygdaloidal, basic volcanic flow overlain by tuffaceous andesitic rock, the contact dipping gently to the north. The tuffs contain several bands of limestone and limy argillaceous beds in which most of the economic mineralization occurs. These rocks are all cut by mafic porphyry dykes. The results of the historical sampling indicate significant copper, zinc, silver, gold, arsenic, cobalt, and cadmium. The high values are as follows over a vein width of, about 2 feet. The vein is up to about 8 feet in width are as follows: 25,300 ppm Cu, >50,000 ppm Zn, 4 ppm Ag, 160 ppb Au, 410 ppm As, 460 ppm Co, and 465 ppm Cd. Other significant magnetite skarn type deposits in the region include the Blue Grouse Claim north of Beavertail Lake and massive magnetite within a sandstone horizon of the Nanaimo Group south of Beavertail Lake, both on the north edge of the Mag-High ; the Argonaut Mine (in production from 1951 to 1957, producing 3,657,168 tonnes of ore),on the south side of the Mag High ; the Iron River deposit (3,175,000 tonnes of 0.517% copper and 38.48% iron and 1,450,000 tonnes of 0.349% copper and 26.46% iron), on the eastern edge of the regional Mag High ; and Camp Lake a copper-goldmagnetite mineral discovery made in 2003, on the west side of the Mag High, south of Upper Campbell Lake.

6

7 This property has excellent further discovery potential This property is offered for sale by way of working option to purchase. For further information please contact Craig Lynes: Rich River Exploration Ltd. PO BOX 131, GRINDROD BC V0E-1Y0 Cell: Web:

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