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About: Gatecliff Rockshelter     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : umbel-rc:Place, within Data Space : dbpedia.org associated with source document(s)

Type: ThingplaceBuildingyago:WikicatArchaeologicalSitesOnTheNationalRegisterOfHistoricPlacesInNevadageo:SpatialThingyago:WikicatRockSheltersInTheUnitedStatesarchitectural structureyago:Artifact100021939yago:GeographicalArea108574314yago:Location100027167yago:Object100002684yago:PhysicalEntity100001930yago:Region108630985yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntitybuildingyago:Shelter104191595yago:Site108651247yago:Structure104341686yago:Tract108673395yago:Whole100003553umbel-rc:Place New Facet based on Instances of this Class

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". 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). David Hurst Thomas discovered Gatecliff Rockshelter in 1970 and began excavations in 1971. 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. The well-preserved artifacts and undisturbed sediments at Gatecliff Rockshelter provides data and information have been applied to a range o