The showing is a quartz vein which crosscuts Lower Jurassic Hazelton Group volcanics of the Telkwa Formation which is comprised of andesitic to rhyolitic flows, tuff and breccia.

The mineralized quartz vein strikes 030 degrees and dips gently northeast. At 2,027 metres in elevation, an open cut in the vein exposed quartz with galena, chalcopyrite and malachite staining. A selected sample assayed 48 grams per tonne gold, 1,200 grams per tonne silver, 0.5 per cent copper and 20 per cent lead (Minister of Mines Annual Report 1929, page 167).

A few other mineralized quartz veins outcrop on this property.