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The Tennessee water resource region is one of 21 major geographic areas, or regions, in the first level of classification used by the United States Geological Survey to divide and sub-divide the United States into successively smaller hydrologic units. These geographic areas contain either the drainage area of a major river, or the combined ...
The TVA established the stairway of nine dams and locks that turned the Tennessee River into a 652-mile-long river highway. Dams and reservoirs on the main stem of the river include the following (listed from the furthest upstream to the furthest downstream): Fort Loudoun Dam impounds Fort Loudoun Lake; Watts Bar Dam impounds Watts Bar Lake
[8] [1] Public boating access areas, Panther Creek State Park and other public parks, commercial boat docks, lakefront resorts, RV and tent campgrounds, and a state wildlife management area on the shores of the lake attract extensive recreational use, such as swimming, boating, paddling activities (such as canoeing, kayaking and paddleboarding ...
[1] [2] Douglas Dam is located just over 32 miles (51 km) upstream from the French Broad River's confluence with the Holston River in Knoxville, to form the Tennessee River. The Douglas Lake reservoir inundates about a 40-mile (64 km) stretch of the French Broad River between the Douglas Dam and the Irish Bottoms area near Newport .
J. Percy Priest Lake is a reservoir in north central part of Tennessee. It is formed by J. Percy Priest Dam , located between miles six and seven of the Stones River . The dam (easily visible from Interstate 40 ) is located about 10 miles (16 km) east of downtown Nashville and impounds a lake 42 mi (68 km) long.
It was created in 1944 by the Tennessee Valley Authority's impounding of the Tennessee River via Kentucky Dam for flood control and hydroelectric power. [2] The 160,309-acre (649 km 2 ) lake is the largest artificial lake by surface area in the United States east of the Mississippi River , with 2,064 miles (3,322 km) of shoreline.
Currently, drought conditions are the worst in four western Middle Tennessee counties, west of Interstate 65 near the Tennessee River. Water continues to flow at Duck River in Centerville, Tenn ...
Dye traces establish the origin of their water as originating from Grassy Cove, [5] the pastoral limestone sinkhole located to the north-east. The Sequatchie River follows the general trend of the Sequatchie Valley, flowing south-west for 182.12 mi (293.09 km). [6] Sequatchie River in Pikeville, Tennessee
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