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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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The northern Gros Ventre Mountains and Mount Leidy Highlands area is in western Wyoming south of Yellowstone National Park. This area was a shelf zone bordering a deeper part of the Rocky Mountain geosyncline during the Paleozoic and Mesozoic eras. Therefore, the sediments deposited were relatively thin as compared with those on the west and southwest. The rocks range from pre-Cambrian to Tertiary in age, with all of the systems present, excepting possibly the Silurian. The Paleozoic strata are about 3,5O0 feet thick, and the Mesozoic about 12,000 feet.
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