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Lake Tight, named for geologist William G. Tight, was a glacial lake in what is present-day Ohio, Kentucky, and West Virginia, during the Ice Age the early Pleistocene before 700,000 years. [ 1 ] History
This ice sheet was the primary feature of the Pleistocene epoch in North America, commonly referred to as the ice age. During the Pre-Illinoian Stage , the Laurentide Ice Sheet extended as far south as the Missouri and Ohio River valleys.
On the Straits of Magellan, ice reached as far as Segunda Angostura. [74] A map of the world during the Last Glacial Maximum. During the LGM, valley glaciers in the southern Andes (38–43° S) merged and descended from the Andes occupying lacustrine and marine basins where they spread out forming large piedmont glacier lobes.
The Teays River was a north- and northwest-flowing river existing before the Pleistocene Ice Ages – before 2.5 million years ago. [10] The Teays flowed through southwest West Virginia, between Kentucky and Ohio, and northwest across Ohio (see illustration). [11]
A chronology of climatic events of importance for the Last Glacial Period, about the last 120,000 years The Last Glacial Period caused a much lower global sea level.. The Last Glacial Period (LGP), also known as the Last glacial cycle, occurred from the end of the Last Interglacial to the beginning of the Holocene, c. 115,000 – c. 11,700 years ago, and thus corresponds to most of the ...
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.
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Early Lake Erie; 11,800 – 8,700 YBP in Ohio, Ontario, Michigan, Pennsylvania, and New York and located in the Erie basin [1] Lake Lundy; 2,000 YBP [7] in Ohio, Ontario, Pennsylvania, and New York; Lake Elkton stage of Lake Lundy @ 620 feet (190 m) above sea level [7] Lake Dana stage of Lake Lundy @ 590 feet (180 m) above sea level [7]