The area is underlain by Upper Triassic Karmutsen Formation volcanic rocks of the Vancouver Group. To the east these are interbedded with, and overlain by a northwest trending belt of Quatsino Formation limestone (Vancouver Group) known historically as the "lime-belt". The Vancouver Group rocks are in fault and/or intrusive contact to the northeast with intrusive rocks of the Juro- Cretaceous Coast Plutonic Complex.
A shear zone up to 60 metres in width strikes 135 degrees into a hill slope consisting of amygdaloidal basalts (Minister of Mines Annual Report 1927). Other reports indicate a strike of about 080 degrees (Geological Survey of Canada Memoir 23).
Lenses and small veins of calcite hosting chalcocite and bornite occur within the shear. About 30 tonnes of ore were taken out prior to 1902, assaying over 25 per cent copper. Values of gold and silver are reported to be low.