The Vick is a polymetallic vein showing hosted by andesitic flow breccias and feldspar crystal tuffs of the Powell Creek Formation. It is located on a steep mountain directly west of the narrows at the north end of Lower Taseko Lake. Two exploration audits' were driven into the east side of the mountain at about 1700 meters (5500 feet) elevation in 1935. A four-wheel drive access road to the 2407 meter (7898 foot) peak around the south side of the mountain was made in the early 1980's.

Mineralization consists of gold, silver and copper-bearing quartz-sulphide veins within a northeast-striking shear zone that can be traced across the top of the peak on the east face. Diorite dykes roughly parallel the fault zone. The quartz veins contain iron carbonates, pyrite, and chalcopyrite concentrations parallel to the walls of the veins. Malachite and azurite are common. In upper parts of the vein shear system, specularite pseudomorphs pyrite. Significant precious metal assays are generally associated with the sulphide-rich sections of the veins (Assessment Report 16873).

A chip sample assayed 72 grams per tonne gold, 86 grams per tonne silver and 0.2 per cent copper (Bulletin 81).