In this area the geology from northeast to southwest, consists of northwest trending Karmutsen Formation andesites with minor limestone and Quatsino Formation limestone, both of the Upper Triassic Vancouver Group. The Vancouver Group rocks are overlain by Lower Jurassic Bonanza Group shales which are in fault contact with the Karmutsen Formation.
In the northeast block of the Karmutsen Formation, a quartz- chalcocite vein, 0.1 metres wide, is exposed in a roadcut in andesite (Assessment Report 1719).