Climate
What are the salt lakes normally called?
Tunisia
Molten salt Salt Valley Lakes Serpentine Lakes Brine lake Lakes Aquarium
Molten_salt-Abstract Salt_Valley_Lakes-Abstract Serpentine_Lakes-Abstract Brine_lake-Abstract Lakes_Aquarium-Exhibits
Molten salt is salt which is solid at standard temperature and pressure (STP) but enters the liquid phase due to elevated temperature. A salt that is normally liquid even at STP is usually called a room temperature ionic liquid, although technically molten salts are a class of ionic liquids. 
The Salt Valley Lakes is a system of more than twenty lakes in Lancaster County, Nebraska. Many of the lakes are state recreation areas or wildlife areas. All of the lakes are within twenty-five miles of Lincoln, Nebraska. "These areas around Lincoln cover 15,039 total acres, with 4,438 acres of water."
The Serpentine Lakes is a chain of salt lakes in the Great Victoria Desert of Australia. It runs for almost along the border between South Australia and Western Australia. When full, the lakes cover an area of . Most of it is located in the Mamungari Conservation Park. The Anne Beadell Highway crosses the northernmost arm of the lake. The Serpentine Lakes are considered an important wetlands area. They form part of a major palaeo-drainage system, a now-inactive drainage system from the Palaeozoic era. The surface of the lake normally consists of dry clay, silt and sand, and is covered with a salty crust. The sediment is mostly quartz arenite. The lakes form the main channel of the palaeo-drainage system. Other channels are covered by sand dunes and are not well defined. Tektites high in magnesium have been found in these lakes. 
Brine lakes consist of water that has reached salt saturation or near saturation (brine), and may also be heavily saturated with other materials. Most brine lakes develop as a result of high evaporation rates in an arid climate with a lack of an outlet to the ocean. The high salt content in these bodies of water may come from minerals deposited from the surrounding land. Another source for the salt may be that the body of water was formerly connected to the ocean. While the water evaporates from the lake, the salt remains. Eventually, the body of water will become brine. Because of the density of brine, swimmers are more buoyant in brine than in fresh or ordinary salt water. Examples of such brine lakes are the Dead Sea and the Great Salt Lake. Bodies of brine may also form on the ocean floor at cold seeps. These are sometimes called brine lakes, but are more frequently referred to as brine pools. It is possible to observe waves on the surface of these bodies. Man-made bodies of brine are created for edible salt production. These can be referred to as brine ponds. 
The Lakes Aquarium contains both freshwater and salt water aquatic animals. 