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The Teays system in Ohio is known as the Parker Strath. The Teays River extended across Ohio in a northwesterly direction from Huntington, West Virginia. It splits away from the Ohio River near Sciotodale/Wheelersburg and goes north and west through Minford, Stockdale, and Beaver before merging with the Scioto River valley
The Allegheny Plateau (/ ˌ æ l ɪ ˈ ɡ eɪ n i / AL-ig-AY-nee) is a large dissected plateau area of the Appalachian Mountains in western and central New York, northern and western Pennsylvania, northern and western West Virginia, and eastern Ohio.
Pages in category "Indiana counties on the Ohio River" The following 13 pages are in this category, out of 13 total. This list may not reflect recent changes. C.
Ohio counties on the Ohio River — located within the Appalachian Ohio region. Pages in category "Ohio counties on the Ohio River" The following 14 pages are in this ...
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 .
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: Allen County, Ohio 872 feet (266 m) Two miles south of Lima: Allen County, Ohio 895 feet (273 m)
The other outwash deposits on the Allegheny, Ohio, and Beaver River terraces have no names. These deposits are typically red rust-colored, deeply weathered gravels composed of small, rounded pebbles generally less than 1 inch (2.5 cm) in diameter. Up to 10% of the pebbles are granites and other crystalline rocks.
In general, the glaciated lies to the north and west of the unglaciated, and forms an arc in northeastern to southeastern Ohio lying between the glacial till plains and the Unglaciated Allegheny Plateau. The Glaciated Allegheny Plateau extends into a belt of southern New York State and the central Susquehanna River basin.