Dixie Valley formation. Conglomerate grading locally to fanglomerate, sandstone and shaly limestones and dolomites. Forms massive steplike ledges, prevailingly yellowish to brownish red or maroon. Maximum thickness about 600 feet; 280 to 300 feet at south end of Tobin Range. Underlies Favret formation (new), contact gradational; overlies Tobin formation (new). Age is Early Triassic.
Type locality: northwest part of Augusta Mountain, north end of Dixie Valley, north-central NV.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1125).
Age of the Dixie Valley Formation is modified from Early Triassic to Early and Middle Triassic.
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 ([ ]).