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The East Wenatchee Clovis Site (also called the Richey-Roberts Clovis Site or the Richey Clovis Cache) is a deposit of prehistoric Clovis points and other implements, dating to roughly 11,000 radiocarbon years before present or about 13,000 calendar years before present, found near the city of East Wenatchee, Washington in 1987.
This is one of the main reasons why the claim of a pre-Clovis component at this site has been greeted with much more credibility than at most other potential pre-Clovis sites. The Buttermilk Creek complex has yielded 15,528 pre-Clovis stone artifacts which have been separated into macrodebitage, microdebitage, and tools. The macrodebitage was ...
In either case this should not be considered a Pre-Clovis site. [citation needed] Cueva Fell [70] and Pali Aike Crater sites in Patagonia, with hearths, stone tools and other elements of human habitation dating to at least as early as 11,000 BP. The Big Eddy Site in southwestern Missouri contains several claimed pre-Clovis artifacts or geofacts.
Additionally, the Clovis presence at the Gault site occurs in unprecedented abundance. A preliminary count of Clovis artifacts at the site numbers around 650,000 (including flakes, cores and formal tools), suggesting that a large number of people aggregated at the site and/or people resided at the site for an extended period of time. [9]
The previous excavations had not found any artifacts below the top 100 centimetres (39 in) from the ground surface, with evidence of fluted points (possibly Clovis or Folsom points) at the 90 to 100 centimetres (35 to 39 in) level. In hopes of finding pre-Clovis artifacts, the 1998 excavation was extended below the 100 centimetres (39 in) level.
The bead is made of hare bone, providing experts with the first solid evidence that people in the Clovis era, a prehistoric era in North America, used bones from the rabbit cousin for personal ...
Pages in category "Pre-Clovis archaeological sites in the Americas" The following 49 pages are in this category, out of 49 total.
Clovis fluted points are named after the city of Clovis, New Mexico, where examples were first found in 1929 by Ridgely Whiteman. [3] A typical Clovis point is a medium to large lanceolate point with sharp edges, a third of an inch thick, one to two inches wide, and about four inches (10 cm) long. [4]