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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.
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 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 ...
Category: Bodies of water of Tennessee. ... Print/export Download as PDF; Printable version; In other projects
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 ...
For recreational purposes, it is managed by the Tennessee Resource Management Division, in cooperation with TVA. [7] The river features Class I through Class III rapids, depending on water levels. After exiting the mountains through a gorge, the Hiwassee broadens, meandering through rural Polk and Bradley counties in Tennessee. It is crossed by ...
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.
The outcome of the study was a class of vertical-beam depth sounders, which is still widely used. It simultaneously pinged at two acoustic frequencies, separated by more than 2 octaves, making depth and echo-amplitude measurements that were concurrent, both spatially and temporally, albeit at a single vertical grazing angle. [clarification needed]
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