Triassic volcanics, consisting of rhyolites and andesite flows, are intruded by quartz diorite and granodiorite of the Cretaceous to Tertiary Coast Plutonic Complex. The volcanics are cut by feldspar with associated quartz veins.
Several east trending veins occur within the volcanics over a 200 metre width. The veins carry chalcopyrite, bornite and pyrite. A 60 centimetre sample of one vein assayed trace gold, 35 grams per tonne silver and 8.5 per cent copper (Minister of Mines Annual Report 1928).
Two trial shipments, totalling about one tonne, assayed 0.6 grams per tonne gold, 55 grams per tonne silver, and 5.8 per cent copper (Minister of Mines Annual Report 1928).