Gatecliff Rockshelter (26NY301) is a major archaeological site in the Great Basin area of the western United States that provides remarkable stratigraphy; it has been called the "deepest archaeological rock shelter in the Americas".[2] Located in Mill Canyon of the Toquima Range in the Monitor Valley of central Nevada, Gatecliff Rockshelter has an elevation of 7,750 feet (2,360 m).[3] David Hurst Thomas discovered Gatecliff Rockshelter in 1970 and began excavations in 1971.[4] Full scale excavations occurred at Gatecliff Rockshelter for about seven field seasons in which nearly 33 feet (10 m) of sediments were exposed for a well-defined stratigraphic sequence.[4] The well-preserved artifacts and undisturbed sediments at Gatecliff Rockshelter provides data and information have been applied to a range of research topics.[3] Based on the analysis of the artifacts at Gatecliff Rockshelter, it can be determined that it was most likely a short-term field camp throughout prehistory.[4] The latest evidence for human usage at Gatecliff occurs between ca. 5500 B.P. to 1250 B.P.[4]
In August 1974, a short-film was created: Gatecliff: American Indian Rock-Shelter.[3]
In April 1979, Gatecliff Rockshelter was listed in the National Register of Historic Places.
^"National Register Information System". National Register of Historic Places. National Park Service. April 15, 2008.
^"David Hurst Thomas". American Museum of Natural History. www.amnh.org.
^ abcNational Register of Historic Places Inventory – Nomination Form. Name: Gatecliff Rockshelter (26NY301). Form prepared by Charles D. Zeier. December 1978.
^ abcdThomas, D. H. (1983). “Chapter 1 – Excavation Strategies.” The Archaeology of Monitor Valley: 2. Gatecliff. Anthropological Papers of the American Museum of Natural History. 59(1): 16-28.
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