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Robert Bruce Horsfall (1913). Life restoration of a herd of Mammuthus columbi, or Columbian mammoths. The extent of the fur depicted is hypothetical. Charles R. Knight (1909). Restoration of a herd of alarmed Miocene-Pleistocene peccaries of the genus Platygonus.
Spiro Mounds (34 LF 40) [3] is an Indigenous archaeological site located in present-day eastern Oklahoma. The site was built by people from the Arkansas Valley Caddoan culture. [4] that remains from an American Indian culture that was part of the major northern Caddoan Mississippian culture. The 80-acre site is located within a floodplain on ...
The Domebo site (also referred to as Domebo Canyon) is located in the west-central region of Oklahoma known as Caddo County. Caddo County has more than 451 archaeological sites. One hundred and fifteen of those sites date to the Plains Village era (A.D. 1000 to 1500). [3] In contrast, the Domebo site dates to approximately 11,000 years ago.
Paleontology in Oklahoma refers to paleontological research occurring within or conducted by people from the U.S. state of Oklahoma. Oklahoma has a rich fossil record spanning all three eras of the Phanerozoic Eon. [1] Oklahoma is the best source of Pennsylvanian fossils in the United States due to having an exceptionally complete geologic ...
The McLemore Site, designated by the Smithsonian trinomial 34WA5, is a prehistoric archaeological site of the Southern Plains villagers located near Colony in Washita County, Oklahoma. It is the site of a prehistoric Plains Indian village, dating from AD 1330-1360, during the Washita River phase. [1] The site is of historic importance for being ...
The Southern Plains villagers were semi-sedentary Native Americans (American Indians) who lived on the Great Plains in western Oklahoma, Texas, Kansas, and southeastern Colorado from about AD 800 until AD 1500. Also known as Plains Villagers, the people of this pre-Columbian culture cultivated maize and other crops, hunted bison and other game ...
The Arbuckle Mountains are an ancient mountain range in south-central Oklahoma in the United States. They lie in Murray, Carter, Pontotoc, and Johnston counties. [1] The granite rocks of the Arbuckles date back to the Precambrian Eon some 1.4 billion years ago which were overlain by rhyolites during the Cambrian Period.
In 1987, the Oklahoma Legislature and governor approved a law (70 OK Stat §70-3309.1) that designated the Stovall Museum as the official Oklahoma Museum of Natural History. In the early 1990s, a group of concerned citizens in Norman, Oklahoma , began to lobby for a new museum facility to better care for the state’s collection of natural and ...