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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Kanawha River is a tributary of the Ohio River, approximately 97 mi long, in the U.S. state of West Virginia. The largest inland waterway in West Virginia, it has formed a significant industrial region of the state since the middle of the 19th century. It is formed at the town of Gauley Bridge in northwestern Fayette County, approximately 35 mi SE of Charleston, by the confluence of the New and Gauley rivers. It flows generally northwest, in a winding course on…mehr

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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Kanawha River is a tributary of the Ohio River, approximately 97 mi long, in the U.S. state of West Virginia. The largest inland waterway in West Virginia, it has formed a significant industrial region of the state since the middle of the 19th century. It is formed at the town of Gauley Bridge in northwestern Fayette County, approximately 35 mi 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. Paleo-Indians, the earliest indigenous peoples, lived in the valley and the heights by 10,000 BCE, as evidenced by archaeological artifacts such as Clovis points. A succession of prehistoric cultures developed, with the Adena culture beginning the construction of numerous skilled earthwork mounds and enclosures more than 1000 years ago. Some of the villages of the Fort Ancient culture survived into the times of European contact.