Pahranagat Lakes Formation of Quichapa Group. Pahranagat Lakes Tuff is single ignimbrite, and consists of light-colored nonwelded tuff. Contains about 16 percent penocrysts by volume, mostly quartz, sanidine and plagioclase, and minor biotite. Overlies Condor Canyon Formation. Underlies Harmony Hills Formation. Age is Miocene.
Recognized in southwestern Utah and southeastern Nevada. [Type locality not stated. Probably named from Pahranagat Lakes, Lincoln Co., NV.]
Source: US geologic names lexicon (USGS Bull. 1350, p. 550).
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