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Paleo Crossing site, also known as the Old Dague Farm site, [2] is an archaeological site near Sharon Center, Ohio in Medina County where Clovis artifacts dated to 10,980 BP ± 75 years Before Present were found. [3] The Cleveland Museum of Natural History conducted an excavation from 1990 to 1993. [4]
Nobles Pond site is a 25-acre archaeological site near Canton in Stark County, Ohio, and is a historical site with The Ohio Historical Society. It is one of the largest Clovis culture sites in North America. At the end of the Ice age, about 10,500 to 11,500 years ago, a large number of Paleo-Indians, the first people to live in Ohio, camped at ...
Wright and Olaf Prufer of Kent State University performed research by comparing artifacts found at the Welling site with those of other Paleo-Indian sites. They also wrote an article about the Welling site (10,000 to 11,800 BC) for the Ohio Archaeologist. [4] Based on their analysis, the Welling site is an early Paleo-Indian site.
Prehistory of Ohio provides an overview of the activities that occurred prior to Ohio's recorded history. The ancient hunters, Paleo-Indians (13000 B.C. to 7000 B.C.), descended from humans that crossed the Bering Strait. There is evidence of Paleo-Indians in Ohio, who were hunter-gatherers that ranged
Sheriden Cave is a Paleo-Indian archaeological site from the late Ice age in Wyandot County, Ohio. [1] Glacial deposits sealed off the cave more than 10,000 years ago. Sheriden Cave is a karst sinkhole on a dolomite ridge that crosses Hancock and Wyandot Counties. It is associated with the Indian Trail Caverns that opened in 1927.
Such large sites as Adams County, or "Sandy Springs" as it is also known, are rare among Paleo-Indian sites; most discoveries related to the people are isolated finds, [4]: 158 although a comparable archaeological district known as the Welling site has been discovered in Coshocton County, Ohio.
Archaeological sites in Belmont County, Ohio (3 P) Archaeological sites in Hamilton County, Ohio (17 P) Archaeological sites on the National Register of Historic Places in Ohio (116 P)
Southeastern Ohio was a swamp-covered coastal plain. [4] Ferns and horsetails were among the state's rich flora. [3] Ohio was only about 5 degrees north of the equator. Sand and mud deposited on local river deltas gradually filled in the swamp. Later in the Permian Ohio was subjected to geologic uplift and its sediments were eroded away ...
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