Named as 4th from lowermost member (of 6) of Chainman Formation along UT-NV boundary. Consists of molassic conglomerates and coarse clastics which thin eastward away from the ancient Antler orogenic belt. Unit is about 250 ft thick. Overlies Camp Canyon Member; underlies Willow Gap Limestone Member (both new and of Chainman Formation). Age of Chainman Formation is Late Mississippian based on faunal zone analysis.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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