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Added to NRHP. October 15, 1966. The Cumberland Gap National Historical Park is a United States National Historical Park located at the border between Kentucky, Tennessee, and Virginia, centered on the Cumberland Gap, a natural break in the Appalachian Mountains. The park lies in parts of Bell and Harlan counties in Kentucky, Claiborne County ...
Clendening Lake is a reservoir located in Harrison County, Ohio, in the United States, formed by damming Brushy Fork, 0.5 miles (0.80 km) East of Tippecanoe. [1] Clendening Lake in September 2009. It is part of the Muskingum Watershed Conservancy District, which was created in 1933 to control flooding in the state of Ohio, primarily due to the ...
Muskingum River. The Muskingum River (/ məˈskɪŋ (ɡ) əm / mə-SKING- (g)əm; Shawnee: Wakatamothiipi) [4] is a tributary of the Ohio River, approximately 111 miles (179 km) long, in southeastern Ohio in the United States. An important commercial route in the 19th century, it flows generally southward through the eastern hill country of Ohio.
May 27, 1971. Morristown National Historical Park is a United States National Historical Park, headquartered in Morristown, New Jersey, consisting of four sites important during the American Revolutionary War: Jockey Hollow, Ford Mansion, Fort Nonsense, and Washington's Headquarters Museum. The sites are located in Morristown and Harding ...
963 ft (294 m) to 977.5 ft (297.9 m) [2] Leesville Lake is a reservoir located near Ohio State Route 212 and Leesville, Ohio. [3] The lake is formed by Leesville Dam 40°28′6″N 81°11′41″W[4] across McGuire Creek, [5] a tributary of Conotton Creek . The lake is named for the village of Leesville. The McGuire Creek forms the south branch ...
The Blue River in late summer, just south of Fredericksburg, Indiana. The Blue River is a 57-mile-long (92 km), [2][3] two-forked stream that runs through Harrison, Crawford and Washington counties in Indiana. The headwaters of the North Fork arise near Salem in Washington County and flow south, and the headwaters of the South Fork arise near ...
Added to NRHP. March 27, 1975 (original) December 15, 1988. Kelleys Island is both a village in Erie County, Ohio, and the island which it fully occupies in Lake Erie. The island has a total area of 4.41 square miles (11.42 km 2) and was formed by glacial action on limestone and dolomite.
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.
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