Unit is named the Pinto Basin Tuff Member of the Pinto Peak Rhyolite. Consists of white air-fall vitric crystal tuff and breccia, tuffaceous sandstone. Underlies the Sierra Springs Tuff Member of the Pinto Peak. Age is Oligocene based of eight radiometric (K-Ar) ages averaging 34.6 Ma. (B1520)
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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