The property is underlain by Shuswap Metamorphic Complex rocks consisting of quartz-biotite schist with local bands of marmorized limestone.

A probably Cretaceous porphyritic biotite quartz monzonite intrudes the metasediments developing a garnet-diopside and scheelite-pyrrhotite-chalcopyrite skarn.

Mineralization occurs in numerous boulders up to 1000 metres along Canyon Creek. Similar mineralization occurs with a rusty granitic dyke at 1040 metres elevation.