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Salt pan at Lake Karum in Ethiopia. Natural salt pans or salt flats are flat expanses of ground covered with salt and other minerals, usually shining white under the sun. They are found in deserts and are natural formations (unlike salt evaporation ponds, which are artificial). A salt pan forms by evaporation of a water pool, such as a lake or ...
The largest individual pan is about 1,900 sq mi (4,921.0 km 2). In comparison, Salar de Uyuni in Bolivia is a single salt flat of 4,100 sq mi (10,619.0 km 2), rarely has much water, and is generally claimed to be the world's largest salt pan. A dry, salty, clay crust most of the year, the pans are seasonally covered with water and grass, and ...
A salt evaporation pond is a shallow artificial salt pan designed to extract salts from sea water or other brines. The salt pans are shallow and expansive, allowing sunlight to penetrate and reach the seawater. Natural salt pans are formed through geologic processes, where evaporating water leaves behind salt deposits.
If its basin is primarily salt, then a dry lake bed is called a salt pan, pan, or salt flat (the latter being a remnant of a salt lake). Hardpan is the dry terminus of an internally drained basin in a dry climate, a designation typically used in the Great Basin of the western United States. [citation needed] The Chott el Djerid in Tunisia
Salt marsh showing salt pannes and ponds, spartina alternifolia and invasive phragmites communis in foreground. Brackish marsh panne variants occur in brackish marshes (short graminoid variant), one of the native dominant species is spike grass (Distichlis spicata), some brackish marsh pannes are dominated by the narrow-leaved cattail (Typha angustifolia) an invasive exotic species.
Hakskeenpan or Hakskeen Pan [1] is a mud and salt pan in the Kalahari Desert, in Southern Africa. It is located in the Dawid Kruiper Local Municipality region in the Northern Cape, South Africa, at 801 metres (2,628 ft) above sea level. [2] The pan covers an area of approximately 140 square kilometres (54 sq mi) [3]
The Sossusvlei pan Aerial view of Sossusvlei (2017) Pronunciation of Sossusvlei Satellite image of Sossusvlei (). Sossusvlei (sometimes written Sossus Vlei) is a salt and clay pan [1] surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia.
In the khor-lagoon-sabkha model, an initial rise in sea-level floods coastal areas and creates shallow water features. If the features silt up, or the land rises, or the sea level falls, then the trapped water evaporates, leaving a flat salt pan, or sabkha.