Gossanous volcanics outcrop over a 200 by 500 metre area 1 kilometre northwest of Sloquet Creek and 14 kilometres west-southwest of the north end of Harrison Lake.

The showing is underlain by silicified and sericitized dacitic tuff of the Lower Cretaceous Peninsula Formation, Fire Lake Group. These are intruded, from the west, by quartz diorite of the Upper Jurassic to Lower Cretaceous Pemberton Diorite Complex.

The tuff hosts veins and fine disseminations of pyrite, comprising up to 20 per cent of the rock. Fine disseminated chalcopyrite and pyrrhotite are also present in minor amounts. A grab sample of dacitic tuff, containing 1 to 2 per cent disseminated pyrite and chlorite rich fractures, assayed 0.540 grams per tonne gold and 13.5 grams per tonne silver (Property File - Carpenter, 1986, p.12, Sample 37691).