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| Conemaugh River | |
|---|---|
Conemaugh River Lake Dam at low water
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| Location | |
| Country | United States |
| Physical characteristics | |
| Source | |
| • coordinates | 40°19′54″N 78°55′30″W / 40.3317406°N 78.9250255°W / 40.3317406; -78.9250255 |
| Mouth | |
• coordinates | 40°29′08″N 79°27′14″W / 40.4856220°N 79.4539299°W / 40.4856220; -79.4539299 |
• elevation | 827 ft (252 m) |
| Discharge | |
| • location | Tunnelton |
| • average | 2,431 cu ft/s (68.8 m3/s)[1] |
| Basin features | |
| River system | Allegheny River |
The Conemaugh River is a 70-mile (110 km) tributary of the Kiskiminetas RiverinWestmoreland, Indiana, and Cambria counties in the U.S. stateofPennsylvania.[2] The name means 'Otter Creek', originating from the Unami-Lenape language word kwənəmuxkw 'otter'.[3][4][5]
The Conemaugh River is formed at Johnstown (site of the Johnstown Flood) in southwestern Cambria County by the confluence of the Little Conemaugh and Stonycreek rivers. It flows generally west–northwest, in a winding course through the mountains along the northern edge of Laurel Hill and Chestnut Ridge. Northwest of Blairsville it is joined by Blacklick Creek. At Saltsburg it is joined from the south by Loyalhanna Creek to form the Kiskiminetas River. Along much of its lower course, the Conemaugh forms part of the boundary between Westmoreland and Indiana counties.
The Kiskiminetas-Conemaugh river basin flows through scenic mountainous country that forms the heart of the historic coal-producing areas of western Pennsylvania. Before the Dam was constructed, the town of Livermore served the area between Blairsville and Saltsburg as an important stop along the former canal, as well as the railroad. The watershed is considered among the most degraded in the state, largely from abandoned mine drainages. The recovery of the river has been an important ongoing ecological management project of state and private agencies.
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