Shoshone Volcanics is applied to rhyolite flows and tuffs in the southern Eagle Mtn. and northern Shoshone 15' quads, Inyo Co, CA. Age is early and middle Pliocene.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Shoshone Volcanics of Haefner (1974) are exposed almost continuously in a belt about 26 km (north to south) in the southern part of the Eagle Mtn. and the northern part of the Shoshone 15' quads, Inyo Co, CA. Is equivalent to part of the older volcanics of Drewes (1963) in the Funeral Peak 15' quad. Consists of four lithotypes: 1) gray perlitic vitrophyre, 2) red-brown to pinkish-gray felsophyre, 3) yellow felsophyre, and 4) yellow devitrified tuff. Is as thick as 900 m. Unconformably overlies Cambrian sedimentary rocks, Cenozoic quartz monzonite plutons, and older [Cenozoic] acid volcanic rocks; underlies Greenwater Volcanics. Age is early to middle Pliocene based on stratigraphic position.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Shoshone Volcanics (lower part) in the Dublin Hills, Inyo Co, CA are of [Miocene] age based on K-Ar ages of 8.2 +/-0.2 (plagioclase), 7.6 +/-0.2 (plagioclase), and 8.7 +/-0.1 (glass) Ma.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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