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The Kalahari Desert is a large semi-arid sandy savanna in Southern Africa extending for 900,000 square kilometres (350,000 sq mi), covering much of Botswana, ...
The Kalahari Basin, also known as the Kalahari Depression, Okavango Basin or the Makgadikgadi Basin, [1] is an endorheic basin and large lowland area covering approximately 725,293 km 2 (280,037 sq mi) — mostly within Botswana and Namibia, but also parts of Angola, South Africa, Zambia, and Zimbabwe.
Central Kalahari Game Reserve is an extensive national park in the Kalahari Desert of Botswana.Established in 1961 it covers an area of 52,800 square kilometres (20,400 sq mi) (larger than the Netherlands, and almost 10% of Botswana's total land area), making it the second largest game reserve in the world. [1]
Terrain: Mostly high plateau; Namib Desert along the coast; Kalahari Desert in the east. In the north near the border with Angola there is a flat area that has been designated by the World Wildlife Fund as part of the Angolan mopane woodlands ecoregion. Elevation extremes: lowest point: Atlantic Ocean 0 m mean elevation: 1,414 m
The Kalahari is the largest continuous stretch of sand in the world, covering some 2,500 km 2. Karoo sediments, covered by younger basaltic lavas, underlie most of the Kalahari sands and about half of the country of Botswana. The sands of the Kalahari vary in depth from 5m to 200m. The climate is semi-arid.
Lying southeast of the Okavango Delta and surrounded by the Kalahari Desert, Makgadikgadi is technically not a single pan, but many pans with sandy desert in between, the largest being the Sua (Sowa), Ntwetwe and Nxai Pans. The largest individual pan is about 1,900 sq mi (4,921.0 km 2).
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]
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