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Lake Lanier Islands is a resort complex on the lake, opened in 1974, that includes a resort hotel called Legacy Lodge (formerly Emerald Pointe Hotel), a water park, and a golf course, among other amenities. The complex also included a second resort hotel, PineIsle, which operated from 1975 to 2005, and was demolished in 2008.
Fort Walton Beach, Destin Santa Rosa Beach, Freeport, Niceville, Shalimar, Valparaiso Choctawhatchee Bay is a bay in the Emerald Coast region of the Florida Panhandle . The bay, located within Okaloosa and Walton counties , is an inlet of the Gulf of Mexico and has a surface area of 334 square kilometres (129 sq mi). [ 2 ]
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Following is a list of dams and reservoirs in Florida. All major dams are linked below. The National Inventory of Dams defines any "major dam" as being 50 feet (15 m) tall with a storage capacity of at least 5,000 acre-feet (6,200,000 m 3 ), or of any height with a storage capacity of 25,000 acre-feet (31,000,000 m 3 ).
The ocean temperature plays a crucial role in the global climate system, ocean currents and for marine habitats. It varies depending on depth, geographical location and season. Not only does the temperature differ in seawater, so does the salinity. Warm surface water is generally saltier than the cooler deep or polar waters. [1]
Lake Lanier Islands is a resort complex built on a small group of islands on Lake Lanier, the largest lake in Georgia, located 60 miles northeast of Atlanta, Georgia.The resort complex was established in 1974 and includes a hotel, water park, golf course, multiple conference and meeting venues, beaches, boat docks, and a number of other recreational amenities.
A thermocline (also known as the thermal layer or the metalimnion in lakes) is a distinct layer based on temperature within a large body of fluid (e.g. water, as in an ocean or lake; or air, e.g. an atmosphere) with a high gradient of distinct temperature differences associated with depth.
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.