The claim (Lot 7591) is underlain by Lower Jurassic Hazelton volcanics comprised of fractured red and green andesitic flows, tuffs and breccia. Quartz veins hosting galena, sphalerite, arsenopyrite and pyrite crosscut the volcanics.

The main vein, striking 065 degrees was explored by several open cuts. There is a considerable amount of black oxidized earthy material on the surface of the vein which extends approximately 152 meters. The black oxidized material was identified in 1908 as pyro- lusite. Beneath this decomposed area, the ore is comprised of sphalerite, arsenopyrite, galena and pyrite with quartz gangue and altered dike rock that is shattered and brecciated. In 1908 a sample assayed 1.02 grams per tonne gold and 355.5 grams per tonne silver. In 1929, a 0.6 metre sample of the northern extremity of the vein assayed 8.2 grams per tonne gold, 733.7 grams per tonne silver, 15 per cent lead and 25.6 per cent zinc.