Pg. 434-439; H.T. Stearns, 1932 (Corr. chart of Idaho compiled by M.G. Wilmarth, dated Sept. 1, 1932). Bliss basalt. Brecciated subaqueous flow composed chiefly of vitreous porphyritic basalt, containing pillow structures. May be subaqueous facies of McKinney basalt or, possibly, of Sand Springs basalt. Thickness 100+/- feet. Age is Pleistocene.
Type locality: exposures at Bliss Cone and Bliss Bridge, in sec. 11, T. 6 S., R. 12 E., Twin Falls Co., also at Bliss Spring, Gooding Co., southern ID.
Source: US geologic names lexicons (USGS Bull. 896, p. 212; USGS Bull. 1200, p. 384).
Pg. 78-79, pl. 5. Bliss volcanics. Thickness of volcanics about 100 feet. Contemporaneous with McKinney basalt and probably a part of it. Age is Pleistocene.
Source: US geologic names lexicon (USGS Bull. 1200, p. 384).
†Bliss Basalt. Pillow lavas comprising unit are assigned to newly named Bancroft Springs Basalt and term Bliss Basalt is abandoned.
Source: Modified from GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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