Kanawha River

The Kanawha River is a tributary of the Ohio River, approximately 97 miles (156 km) long, in the U.S. state of West Virginia. The longest inland waterway in West Virginia, it has formed a significant industrial region of the state since the middle of the 19th century.

Related Topics:
Ohio River - U.S. state - West Virginia - 19th century

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It is formed at the town of Gauley Bridge in northwestern Fayette County, approximately 35 mi (56 km) SE of Charleston, by the confluence of the New and Gauley rivers. It flows generally northwest, in a winding course on the unglaciated Allegheny Plateau, through Fayette, Kanawha, Putnam and Mason Counties, past the cities of Charleston and St. Albans and numerous smaller communities. It joins the Ohio at Point Pleasant.

Related Topics:
Gauley Bridge - Fayette County - Charleston - Confluence - New - Gauley - Allegheny Plateau - Kanawha - Putnam - Mason - St. Albans - Point Pleasant

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The river valley contains significant deposits of coal and natural gas. In colonial times, the wildly fluctuating level of the river prevented its use for transportation. The removal of boulders and snags on the lower river in the 1840s allowed navigation, extended after the construction of locks and dams starting in 1875. The river is now navigable to Deepwater, an unincorporated community about 20 miles upriver from Charleston. A thriving chemical industry along its banks provides a significant part of the economy of West Virginia.

Related Topics:
Coal - Natural gas - 1840s - 1875 - Deepwater

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