Unit is named the Walker Lake Bed of the Salt Wells Member of the Mono Basin Formation. Is located in the Lake Lahontan area, NV. Consists of a layer of rhyolitic tephra about 1 cm thick that contains glass-encased biotite phenocrysts and has a high silica, low magnesium content. May represent a dense, crystal-rich fraction of the Turupah Flat Bed (new) of the Salt Wells. Source is believed to be Mono basin because of its geographic distribution south of Carson Sink. Age is Holocene, about 1.2 ka. (B1565)
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
Asterisk (*) indicates published by U.S. Geological Survey authors.
"No current usage" (†) implies that a name has been abandoned or has fallen into disuse. Former usage and, if known, replacement name given in parentheses ( ).
Slash (/) indicates name conflicts with nomenclatural guidelines (CSN, 1933; ACSN, 1961, 1970; NACSN, 1983, 2005, 2021). May be explained within brackets ([ ]).