The Oyama Shale showing is located 20 kilometres southwest of Vernon, west of the north end of Wood Lake.
In this area, Devonian to Triassic sediments of the Harper Ranch Group are intruded by Middle Jurassic granitic rocks. These are intruded by granite and hypabyssal equivalents of the Eocene Coryell Intrusions. Patches of Eocene Penticton Group volcanic rocks overlie the older rocks.
Intensely fractured Coryell granite in a talus slide has been quarried for industrial use (Personal Communication - Discovery Consultants, 1993).