Imnaha Basalt of Columbia River Basalt Group (ID*,OR*,WA*)
[Columbia River Basalt Group adopted by the ID, OR, and WA Geol. Surveys, and the USGS (rules suspended).]
late Tertiary (early Miocene)*
Origin of name not stated by author, but probably named from Imnaha River, approx. 6 km west (as the crow flies) of Dug Bar, Wallowa Co., OR. Mapped area lies between Wallowa Mountains of northeastern OR and Seven Devils Mountains of western OR. Part of Snake River Canyon included (Vallier, 1967).
Type locality: at Dug Bar, on Snake River near the mouth of Imnaha River in extreme northeast OR (Hooper, 1974; see entry under Swanson and others, 1979).
Type [section] (base not exposed): exposures in cliffs on west side of Snake River above north end of Dug Bar, [near mouth of Imnaha River, Wallowa National Forest boundary, Lat. 45 deg. 48 min. 35 sec. N., Long. 116 deg. 41 min. 30 sec. W., BM 1005], Cactus Mountain quadrangle, Wallowa Co., OR. Base exposed at south end of Dug Bar (Swanson and others, 1979).
Reference sections: (1) near confluence of Lower Sheep Creek and Imnaha River; (2) anticline on north side of Lewiston Basin (center T. 11 N., R. 45 E.); and (3) lower Rocky Canyon, 25 km west of Grangeville, ID (Swanson and others, 1979).
Blue Mountains province*
Eastern Columbia basin*
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
Asterisk (*) indicates published by U.S. Geological Survey authors.
"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).
Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).