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The paleolithic period (13000 B.C. to 7000 B.C.) occurred during the last centuries of the Ice age. The native people of Ohio descended from those who crossed the Bering Strait land bridge from Asia to North America. The Paleo Indians are the earliest hunter-gatherers that ranged across what is now the state of Ohio.
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.
Laurentide ice sheet. The maximum extent of glacial ice in the north polar area during the Pleistocene period included the vast Laurentide ice sheet in eastern North America. The Laurentide ice sheet was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States ...
Teays River. The Teays River network, which existed before disruption by glaciers during the Pleistocene. Reconstruction is based on the discovery of large buried valleys in West Virginia, Ohio, and Indiana and other evidence. The Teays River / ˈteɪz / [1] (pronounced taze) was a major preglacial river that drained much of the present Ohio ...
Journal of Paleolimnology 47:493-511. Early Lake Erie was a prehistoric proglacial lake that existed at the end of the last ice age approximately 13,000 years ago. The early Erie fed waters to Glacial Lake Iroquois. The ancient lake was similar in size to the current lake during glacial retreat, but for some period the eastern half of the lake ...
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 ...
An artist's impression of the last glacial period at glacial maximum [4]. The LGP is often colloquially referred to as the "last ice age", though the term ice age is not strictly defined, and on a longer geological perspective, the last few million years could be termed a single ice age given the continual presence of ice sheets near both poles.
The glaciers of the Ice Age soon began to block the Teays, effectively damming the river and forming Lake Tight, near what is now Chillicothe, Ohio. The lake has been the repeated topic of research over the past 100 plus years. In geologic terms, the lake's life span was short; the lake appears to have formed in the Lower or Middle Pleistocene.