Pg. 76. Mentioned in summary of structural history of Great Basin province in Utah and eastern Nevada. Referred to as tongues of sandstone and conglomerate that lense eastward into dark-gray marine shales. Age is Late Mississippian.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1858-1859).
Pg. 1427 (fig. 3), 1433 (fig. 9), 1434-1435 (fig. 10). Illipah formation. As shown on correlation chart and diagrams, the Illipah underlies Ely, Callville, and Bird Spring formations and overlies Chainman, Rogers Spring, and Monte Cristo formations.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1858-1859).
Pg. 81-82, 83 (fig. 1), 84. Discussion of aspects of Chainman formation. The Chainman is recognized as a valid stratigraphic unit. Rather than formally recognize Diamond Peak and Scotty Wash as distinct units, the writer [Sadlick] prefers to refer to these as facies within the Chainman. Term Illipah (Christiansen, 1951) is suppressed as synonomous with Diamond Peak, and term should not be used for limestone sequence in upper part of Chainman.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1858-1859).
Pg. 99. Scotty Wash quartzite of Pioche district and Illipah sandstone of Hamilton district are same lithogenetic units. Scotty Wash quartzite has priority; recommended that name Illipah be abandoned.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1858-1859).
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