Named as basal member of Dry Hollow Formation for exposures on east side of Wales Canyon in Millard Co, UT in Great Basin province. Extends east into Sevier Co on Wasatch uplift. No type locality designated. Is an ash-flow tuff containing 30 to 40 percent phenocrysts (mostly feldspar, hornblende, and biotite). The groundmass is fine grained and glassy, and occasionally finely vesicular. Forms an outcrop with platy weathering. Is about 100 m thick. Overlies Bullion Canyon Volcanics; underlies Clear Creek Tuff Member (new) of Dry Hollow Formation. Assigned a Miocene age. Geologic map.
Source: GNU records (USGS DDS-6; Denver GNULEX).
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