Caney Fork River

The Caney Fork River is a river that flows through central Tennessee in the United States, draining a substantial portion of the southwestern Cumberland Plateau and southeastern Highland Rim regions. It is a major tributary of the Cumberland River, and is part of the Cumberland, Ohio and Mississippi basins. The river is 143 miles (230 km) long, and its watershed covers 1,771 square miles (4,590 km2) in eleven counties. Monterey, Baxter, Sparta, Smithville, McMinnville, Altamont, Spencer and Gordonsville are among the towns that are at least partially drained by the river.

Caney Fork River
Canoeing on the upper Caney Fork
Caney Fork watershed
Location
CountryUnited States
StateTennessee
Physical characteristics
SourceNear Campbell Junction in Cumberland County
  coordinates36°02′36″N 85°09′30″W
  elevation1,960 ft (600 m)
MouthCumberland River (Old Hickory Lake) at Carthage
  coordinates
36°14′20″N 85°56′29″W
  elevation
446 ft (136 m)
Length143 mi (230 km)
Basin size1,771 sq mi (4,590 km2)
Discharge 
  locationGreat Falls Dam powerhouse(mean for water years 1915-1983)
  average3,177 cu ft/s (90.0 m3/s)(mean for water years 1915-1983)
  minimum25 cu ft/s (0.71 m3/s)
August 1951
  maximum210,000 cu ft/s (5,900 m3/s)
March 1929
Basin features
Tributaries 
  leftRocky River, Collins River, Smith Fork Creek
  rightCalfkiller River, Falling Water River, Mine Lick Creek, Indian Creek

The Caney Fork flows through two impoundments Center Hill Lake and Great Falls Lake both of which create sizeable artificial lakes. The river's basin is home to numerous protected lands and recreational areas, including five state wilderness areas, six interpretive areas, and a wildlife management area. Two state parks Edgar Evins State Park and Rock Island State Park are located along the river, and three others Fall Creek Falls State Park, Burgess Falls State Park and South Cumberland State Park are located within its basin. The river is a popular stream for canoeing and kayaking.

The name "Caney Fork" comes from the dense cane breaks that grew along the river's banks when European explorers first arrived in the area.

The river is a major drainage feature of the Cumberland Plateau and the largest tributary of the Cumberland River.

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