Swamp Creek Member of Saddle Mountains Basalt of Columbia River Basalt Group. Present in upper North Fork area of the Clearwater embayment in Idaho. Consists of medium- to coarse-grained olivine basalt containing abundant olivine phenocrysts; has normal polarity. Lies above the basalt of Weippe in the Pomona Member of Saddle Mountains Basalt. Age is late Miocene.
Type locality: Swamp Creek, North Fork of the Clearwater River, [Little Green Mountain 7.5-min quadrangle], Clearwater Co., ID.
Source: US geologic names lexicon (USGS Bull. 1565, p. 314); GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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