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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 2010 Tennessee floods were floods in Middle Tennessee, West Tennessee, south-central and western Kentucky and northern Mississippi areas of the United States of America as the result of torrential rains on May 1 and 2, 2010. Floods from these rains affected the area for several days afterwards, resulting in a number of deaths and widespread ...
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.
The reservoir has a surface area of about 28,780 acres (11,650 ha), a flood-storage capacity of 749,406 acre-feet (924,379,000 m 3), and nearly 400 miles (640 km) of shoreline. [2] In a normal year, the lake water level fluctuates over a range of about 27 feet (8.2 m).
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.
Chickamauga Lake is a reservoir in the United States along the Tennessee River created when the Chickamauga Dam, as part of the Tennessee Valley Authority, was completed in 1940. The lake stretches from Watts Bar Dam at mile 529.9 (853 km) to Chickamauga Dam at mile 471.0 (758 km) making the lake 58.9 miles (94.8 km) long.
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