The Camp View showing of the Cole property area is underlain by a sequence of volcanic and sedimentary rocks of the Lower Jurassic Telkwa Formation of the Hazelton Group. Host rocks consist of thick-bedded purple to green lapilli tuffs and volcanic breccias dip steeply northwest and are commonly cross-cut by intermediate dikes. Black mudstone and siltstone occur in the vicinity.

The Camp View showing is associated with a northwest trending system of veins that contains both northwest trending veins and north to northeast trending veins. It is an acutely branching array of veins that split, splay and horsetail. It is an acutely branching array of veins that split, splay and horsetail. The individual veins are associated with minor shears and pinch and swell from stringer-stockworks to masses up to and in excess of 3 meters width. Veins dip steep (60 degrees) to vertical. The overall mineralized vein system is traceable intermittently for in excess of 4 kilometres. Vein quartz types include massive, banded, vuggy and coxcomb quartz generally white in colour but locally beige, grey, clear, red and rarely amethystine. At least 10 discrete zones or showings have been documented and sampled over part of the 4 kilometre length. Most of the showings are low in sulphides containing less than 1 per cent pyrite, locally to 15 per cent.

The Camp View showing comprises a single main vein traceable intermittently through talus and overburden for some 300 meters. It comprises grey, banded, fine-grained vuggy quartz. Minor stringers are associated. It pinches and swells from stringer width to 1 metre width, mainly less than 50 centimetres. Twenty-one samples gave values up to 0.43 gram per tonne gold, confirming the values to 0.64 gram per tonne acquired in 1983 (Assessment Report 14531). A proximal float sample of quartz yielded 1.63 grams per tonne gold and 25.6 grams per tonne silver (Assessment Report 14531).

Refer to Main Creek showing (093E 110) for further geological and work history details.