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The Hiwassee River originates from a spring on the north slope of Rocky Mountain in Towns County in the northern area of the State of Georgia.It flows northward into North Carolina before turning westward into Tennessee, flowing into the Tennessee River a few miles west of what is now State Route 58 in Meigs County, Tennessee.
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
The Obed River rises in Cumberland County, Tennessee, just south of Crossville. It is bridged by U.S. Highway 70 between downtown Crossville and the municipal airport , and meets its confluence with the Little Obed River near a bridge on U.S. Highway 70N and an abandoned railroad bridge which was formerly part of the rail system linking ...
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
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 Harpeth rises in the westernmost part of Rutherford County, Tennessee, just to the east of the community of College Grove in eastern Williamson County.The upper portion of the river has been contaminated to some extent by the operation of a lead smelting plant located near the Kirkland community that recycled used automobile batteries from the 1950s until the 1990s.
According to the 2004 TVA River and Reservoir Operations Study, Watauga Lake is approximately 16.3 mi (26.2 km) long, with 104.9 mi (168.8 km) of shoreline. At the TVA summertime water level target "full pool", the lake surface covers 6,430 acres (26 km²) and the estimated depth of Watauga Lake is 265 feet (81 m) at the dam.
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.
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