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The River's headwaters were near Blowing Rock, North Carolina; it then flowed through Virginia, West Virginia, Ohio, Indiana, and Illinois. (Hansen, 1995). [ 4 ] The largest tributary to the Teays River was the Old Kentucky River (Teller 1991), which extended from southern Kentucky through Frankfort and subsequently flowed northeast, meeting ...
The Laurentide ice sheet (LIS) 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, multiple times during the Quaternary glaciation epochs, from 2.58 million years ago to the present.
The Zimmerman Kame (also called the "Zimmerman Site"; designated 33HR2 [2]: 1 ) is a glacial kame and archaeological site in McDonald Township, Hardin County, Ohio, United States, near the community of Roundhead.
Till plains are large flat or gently sloping areas of land on which glacial till has been deposited from a melted glacier. In some areas, these depositions can be up to hundreds of feet thick. The morphology of the till plain is generally reflective of the topography of the bedrock below the glacier. Another term for till plain is ground moraine.
The river's path traveled through modern-day West Virginia, Kentucky, Ohio, Indiana, and Illinois, finally emptying into the Gulf of Mexico, which at the time extended to southern Illinois. 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.
Williams County, Ohio: 873 feet (266 m) Summit west of Hicksville: Defiance, Ohio: 849 feet (259 m) Wabash-Erie channel. head of Maumee River: Allen County, Indiana: 737 feet (225 m) Summit east of Ft. Wayne: Allen County, Indiana 813 feet (248 m) Summit, section 112, Madison: Allen County, Indiana 846 feet (258 m) Two miles south of Spencerville
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The Glacial Kame culture was a culture of Archaic people in North America that occupied southern Ontario, Michigan, Ohio, and Indiana from around 8000 BC to 1000 BC. The name of this culture derives from its members' practice of burying their dead atop glacier-deposited gravel hills .