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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
Watauga Dam is located 37 miles (60 km) above the mouth of the Watauga, at a point where the westward-flowing river veers north to slice a water gap through the middle of Iron Mountain. The dam is about 5 miles (8.0 km) downstream from Butler, Tennessee , and 10 miles (16 km) upstream from Elizabethton.
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 ...
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.
Center Hill Lake has a storage capacity of 762,000 acre⋅ft (940,000,000 m 3) of water. The lake has approximately 415 mi (668 km) of shoreline, with the deepest point at 190 ft (58 m). The watershed area for the lake is 2,174 sq mi (5,630 km 2). The lake is well known for water recreation and fishing. Sunset over Center Hill Lake
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).
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