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See also: Etosha Pan and Ekuma River, Salar de Uyuni | |
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Makgadikgadi Salt PansPosition of center of photo (Lat/Long): [-20.511/26.07] |
![]() ![]() The salt pans of Botswana - an easily recognizable visual feature for astronauts aboard the ISS - lie at the low point of a vast, shallow continental basin. Rivers draining from as far away as central Angola, more than 1000 kilometers away, supply water to the pans. During several wet climatic phases in the recent geological past, the pans were filled with water for thousands of years, only to dry out when climates fluctuated to drier conditions. During dry phases, water only reaches the pans underground. This underground, salty water supports the ash and salt industry. During wet phases, when open water exists, waves build up beach ridges. One of these ridges crosses the lower part of the view. |
Source of material: NASA |
Further information: WikiPedia article on Makgadikgadi Salt Pans