The High 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 High 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 metres 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 High View vein showing comprises one main vein up to 6 metres width. It is a breccia zone composed of a box-work of vuggy quartz cementing angular, altered fragments of lapilli tuff. Numerous other veins and lenses up to 3 metres width were noted as splays off the main vein. Pyrite is less than 1 per cent, minor sphalerite noted. Fluorite is locally common. Gold ranges up to 0.44 gram per tonne and silver to 27.7 grams per tonne (Assessment Report 14531). Sixteen samples were collected in 1984.

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