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Lake Cumberland is a reservoir in Clinton, Pulaski, Russell, Wayne, and Laurel, counties in Kentucky. [1] The primary reasons for its construction were a means for flood control and the production of hydroelectric power. Its shoreline measures 1,255 miles (2,020 km) and the lake covers 65,530 acres (265 km 2) at the maximum power pool elevation ...
Lake Cumberland is a reservoir encompassing Kentucky counties like Clinton, Russell, Wayne, and more, according to Kentucky State Parks. It spans more than 60,000 acres of water with over 1,200 ...
Created in 1941 by the impoundment of the Columbia River by the Grand Coulee Dam. 26. Cayuga Lake. New York. 7,672,000 acre⋅ft (9.5 km 3) 435 ft (133 m) second largest of the Finger Lakes. 27. Rainy Lake.
The water cycle (or hydrologic cycle or hydrological cycle), is a biogeochemical cycle that involves the continuous movement of water on, above and below the surface of the Earth. The mass of water on Earth remains fairly constant over time. However, the partitioning of the water into the major reservoirs of ice, fresh water, salt water and ...
A lake ecosystem or lacustrine ecosystem includes biotic (living) plants, animals and micro-organisms, as well as abiotic (non-living) physical and chemical interactions. [1] Lake ecosystems are a prime example of lentic ecosystems (lentic refers to stationary or relatively still freshwater, from the Latin lentus, which means "sluggish"), which ...
The Wolf Creek Dam is a multi-purpose dam on the Cumberland River in the western part of Russell County, Kentucky, United States.The dam serves at once four distinct purposes: it generates hydroelectricity; it regulates and limits flooding; it releases stored water to permit year-round navigation on the lower Cumberland River; and it creates Lake Cumberland for recreation, the largest man made ...
Lake stratification is the tendency of lakes to form separate and distinct thermal layers during warm weather. Typically stratified lakes show three distinct layers: the epilimnion, comprising the top warm layer; the thermocline (or metalimnion), the middle layer, whose depth may change throughout the day; and the colder hypolimnion, extending to the floor of the lake.
27,700 acres (112 km 2) Surface elevation. 643 ft (196 m) [1] The Dale Hollow Reservoir is a reservoir situated on the Kentucky / Tennessee border. The lake is formed by the damming of the Obey River, 7.3 miles (11.7 km) above its juncture with the Cumberland River at river mile 380. Portions of the lake also cover the Wolf River.