 The type locality for the Steens basalt, which covers a large portion of the Oregon Plateau, is an approximately face of Steens Mountain showing multiple layers of basalt.The oldest of the flows considered part of the Columbia River Basalt Group, the Steens basalt, includes flows geographically separated but roughly concurrent with the Imnaha flows.Older Imnaha basalt north of Steens Mountain overlies the chemically distinct lowermost flows of Steens basalt; hence some flows of the Imnaha are stratigraphically younger than the lowermost Steens basalt.