Etosha Pan
Big endorheic salt ville in Namibia's north From Wikipedia, the free encyclopedia
The Etosha Pan is a large endorheic salt pan, forming part of the Cuvelai-Etosha Basin in the north of Namibia. It is a vast hollow in the ground in which water may collect or in which a deposit of salt remains after water has evaporated. The 120-kilometre-long (75-mile-long) dry lakebed and its surroundings are protected as Etosha National Park, Namibia's second-largest wildlife park, covering 22,270 square kilometres (8,600 sq mi). The pan is mostly dry but after heavy rains it is flooded with a thin layer of water, which is heavily salted by the mineral deposits on the surface.
| Etosha Pan | |
|---|---|
 Looking across the savannah to the hot, dry, salt-encrusted Etosha Pan | |
  | |
| Location | Namibia |
| Coordinates | 18°47′07″S 16°15′50″E |
| Official name | Etosha Pan, Lake Oponono & Cuvelai drainage |
| Designated | August 23, 1995 |
Etosha, meaning 'Great White Place' in Oshindonga, is made of a large mineral pan.
The area exhibits a characteristic white and greenish surface, which spreads over 4,800 square kilometres (1,900 sq mi).[1] The pan is believed to have developed through tectonic plate activity over about ten million years. Around 16,000 years ago, when ice sheets were melting across the land masses of the Northern Hemisphere, a wet climate phase in Southern Africa caused the Etosha Lake to be filled up. Today however the Etosha Pan is mostly made up of dry clay split into hexagonal shapes as it dries and cracks, and is seldom seen with even a thin sheet of water covering it.
It is assumed that the Kunene River fed the lake in the distant past, but tectonic plate movements over time caused a change in river direction, resulting in the lake running dry and leaving a salt pan. Nowadays the Ekuma River, the Nipelo River, the Cuvelai River and the Omurambo Ovambo River are the sole seasonal sources of water for the lake. Typically, not much river water or sediment reaches the dry lake, because water seeps away into the riverbed along its 250-kilometre (160 mi) course, reducing discharge along the way.
In the colonial era, the first non-Africans to explore this area were the Europeans Charles John Andersson and Francis Galton in 1851.
The surrounding area is dense mopane woodland which is occupied by herds of elephants on the south side of the lake. Mopane trees are common throughout south-central Africa, and host the mopane worm, which is the larval form of the moth Gonimbrasia belina, and an important source of protein for rural communities.
The salt desert supports very little plant life except for the blue-green algae that gives the Etosha Pan its characteristic colouring, and grasses like Sporobolus spicatus which quickly grow in the wet mud following good rains. Surrounding the pan, grasslands provide food for grazing animals.
This harsh dry land with its sparse vegetation and insufficient amount of salty water, supports little wildlife all year round, but is sometimes inhabited by a large number of migratory birds. The hypersaline pan supports brine shrimp and a number of extremophile micro-organisms tolerant of the high saline conditions.(C.Michael Hogan. 2010.) In particularly good rainy seasons the Etosha pan is turned into a shallow lake approximately 10 cm in depth and becomes the breeding ground for flamingos, which arrive in their thousands and great white pelican (Pelecanus onocrotalus).
The surrounding savanna is home to thousands of mammals that will visit the pan and surrounding waterholes when there is water. These include quite large numbers of zebra, wildebeest, gemsbok, springbok and eland, as well as black rhinoceros, bush elephants, lions, leopards, and giraffe.
The Etosha Pan is situated completely within the boundaries of the Etosha National Park and is designated as a Ramsar wetland of international importance and a World Wildlife Fund ecoregion (Etosha Pan halophytics).
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