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The geology and paleontology of Tule Springs Fossil Beds National Monument, Nevada

December 20, 2018

On December 19, 2014, Tule Springs Fossil Beds National Monument, located in the Las Vegas Valley of southern Nevada, was established by Congress as the 405th unit of the National Park Service to “conserve, protect, interpret, and enhance for the benefit of present and future generations the unique and nationally important paleontological, scientific, educational, and recreational resources and values of the land” (P.L. 113-291, sec. 3092). Vertebrate fossils have been known from the region for more than a century, and recent work has established the Tule Springs local fauna as one of the most significant Pleistocene vertebrate faunas in the American Southwest. The sedimentary sequence that entombs the fossils represents a paleohydrologic system that responded dynamically to abrupt changes in climate throughout the late Quaternary. Work in Tule Springs Fossil Beds National Monument continues today through the efforts of scientists from the U.S. Geological Survey, National Park Service, and academic institutions across the country.

Citation Information

Publication Year 2018
Title The geology and paleontology of Tule Springs Fossil Beds National Monument, Nevada
DOI 10.3133/fs20183038
Authors Kathleen B. Springer, Jeffrey S. Pigati, Eric Scott
Publication Type Report
Publication Subtype USGS Numbered Series
Series Title Fact Sheet
Series Number 2018-3038
Index ID fs20183038
Record Source USGS Publications Warehouse
USGS Organization Geosciences and Environmental Change Science Center