The region in which the Mary Ann showing occurs is underlain mainly by rocks of the Lower Jurassic Telkwa Formation of the Hazelton Group. These are intruded by intermediate to felsic plutons of the Lower Jurassic Topley Intrusive Suite.
The showing comprises chalcopyrite and malachite in limestone interbedded with mafic volcanic rocks (Pennsylvanian-Permian Asitka Group).