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Okavango Basin
The Kalahari Basin, also known as the Kalahari Depression, Okavango Basin or the Makgadikgadi basin, is an endorheic basin and large lowland area covering approximately 725,293 km2 covering most of Botswana and Namibia, as well as parts of Angola, South Africa, Zambia, and Zimbabwe. The outstanding physical feature in the basin, and occupying the centre, is the large Kalahari Desert. The perennial river bifurcation of Selinda Spillway (or Magweggana River), on the Cuando River, connects the Kalahari basin to the Zambezi Basin.Is this Harry and Meghan's honeymoon hotel? The Telegraph. 29 may 2018. General characteristics of the basin The |
Angola
, national_anthem = " Angola Avante"() , image_map = , map_caption = , capital = Luanda , religion = , religion_year = 2020 , religion_ref = , coordinates = , largest_city = capital , official_languages = Portuguese , languages2_type = National languages , languages2 = , ethnic_groups = , ethnic_groups_ref = , ethnic_groups_year = 2000 , demonym = , government_type = Unitary dominant-party presidential republic , leader_title1 = President , leader_name1 = João Lourenço , leader_title2 = Vice President , leader_name2 = Esperança da CostaInvestidura do Pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Damaraland
Damaraland was a name given to the north-central part of what later became Namibia, inhabited by the Damara (people), Damaras. It was bounded roughly by Ovamboland in the north, the Namib Desert in the west, the Kalahari Desert in the east, and Windhoek in the south. In the 1970s the name Damaraland was revived for a bantustan in South West Africa (present-day Namibia), intended by the apartheid government to be a self-governing homeland for the Damara people. A centrally administered local government was created in 1980. The bantustan Damaraland was situated on the western edge of the territory that had been known as Damaraland in the 19th century. Damaraland, like other homelands in South West Africa, was abolished in May 1989 at the start of the Namibian War of Independence, transition to independence. The name Damaraland predates South African control of Namibia, and was described as "the central portion of German South West Africa" in the Encyclopædia Britannica Eleven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mopipi Dam
Mopipi is a village in Central District of Botswana. It is located close to Makgadikgadi Pan. The population was 3,066 in 2001 census. This village was named after a tree called Mopipi, which is commonly found in the region. This area has witnessed steady acidification and desertification since the Pleistocene, but perhaps most dramatically since the 19th century.Michael Main (2001) ''African Adventurer's Guide to Botswana'', Published by Struik, . 304 pages In particular, the Boteti River used to flow year around in this area on its way to discharge to the Makgadikgadi Pans The Makgadikgadi Pan (Tswana pronunciation ), a salt pan situated in the middle of the dry savanna of north-eastern Botswana, is one of the largest salt flats in the world. The pan is all that remains of the formerly enormous Lake Makgadikg ...,C. Michael Hogan (2008The Megalithic Portal, ed. A. Burnham/ref> but presently this flow is only in the rainy season. The village has grown since 2001, nowa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boteti
The Boteti River (also Botletle RiverHelgren, David M. (1984) "Historical Geomorphology and Geoarchaeology in the Southwestern Makgadikgadi Basin, Botswana" ''Annals of the Association of American Geographers'' 74(2): pp. 298–307, page 298Johannesburg Sheet 34, Edition 5, TPC, 1970 Series 2201, U.S. Army Map Service or Botletli) is a natural in . It derives flow from the core |
Lake Xau
Lake Xau is a lake that is sometimes a dry lakebed in Botswana. It is fed by the Boteti River and the Okavango Delta The Okavango Delta (or Okavango Grassland; formerly spelled "Okovango" or "Okovanggo") in Botswana is a swampy inland delta formed where the Okavango River reaches a tectonic trough at an altitude of 930–1,000 m in the central part of the en .... The lake has been described as "when it holds water, ... one of the most important wetlands for waterfowl in Southern Africa". References Xau Xau {{Botswana-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Ngami
Lake Ngami is an endorheic lake in Botswana north of the Kalahari Desert. It is seasonally filled by the Taughe River, an effluent of the Okavango River system flowing out of the western side of the Okavango Delta. It is one of the fragmented remnants of the ancient Lake Makgadikgadi. Although the lake has shrunk dramatically beginning from 1890, it remains an important habitat for birds and wildlife, especially in flood year Lake Ngami had many famous visitors during the 19th (and into the 20th) century. In 1849 David Livingstone described it as a "shimmering lake, some long and 20 [30 km] wide". Livingstone also made a few cultural notes about the people living in this area; he noticed they had a story similar to that of the Tower of Babel, except that the builders' heads were "cracked by the fall of the scaffolding" (''Missionary Travels'', chap. 26). One of the illustrations is known to have been made on the basis of a sketch by Mr. Alfred Ryder (1825-1850) son of Artist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Makgadikgadi Pan
The Makgadikgadi Pan (Tswana pronunciation ), a salt pan situated in the middle of the dry savanna of north-eastern Botswana, is one of the largest salt flats in the world. The pan is all that remains of the formerly enormous Lake Makgadikgadi, which once covered an area larger than Switzerland, but dried up tens of thousands of years ago. Recent studies of human mitochondrial DNA suggest that modern ''Homo sapiens'' first began to evolve in this region some 200,000 years ago, when it was a vast, exceptionally fertile area of lakes, rivers, marshes, woodlands and grasslands especially favorable for habitation by evolving hominins and other mammals. Location and description 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 . In comparison, Salar de Uyuni in Bolivia i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kalahari Desert
The Kalahari Desert is a large semi-arid sandy savanna in Southern Africa extending for , covering much of Botswana, and parts of Namibia and South Africa. It is not to be confused with the Angolan, Namibian, and South African Namib coastal desert, whose name is of Khoekhoegowab origin and means "vast place". Etymology ''Kalahari'' is derived from the Tswana word ''Kgala'', meaning "the great thirst", or ''Kgalagadi'', meaning "a waterless place"; the Kalahari has vast areas covered by red sand without any permanent surface water. History The Kalahari Desert was not always a dry desert. The fossil flora and fauna from Gcwihaba Cave in Botswana indicates that the region was much wetter and cooler at least from 30 to 11 thousand BP (before present) especially after 17,500 BP. Geography Drainage of the desert is by dry black valleys, seasonally inundated pans and the large salt pans of the Makgadikgadi Pan in Botswana and Etosha Pan in Namibia. The only permanent river, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flooded Grassland
Flooded grasslands and savannas is a terrestrial biome of the WWF biogeographical system, consisting of large expanses or complexes of flooded grasslands. These areas support numerous plants and animals adapted to the unique hydrologic regimes and soil conditions. Large congregations of migratory and resident waterbirds may be found in these regions. However, the relative importance of these habitat types for these birds as well as more vagile taxa typically varies as the availability of water and productivity annually and seasonally shifts among complexes of smaller and larger wetlands throughout a region. This habitat type is found on four of the continents on Earth. Some globally outstanding flooded savannas and grasslands occur in the Everglades, Pantanal, Lake Chad flooded savanna, Zambezian flooded grasslands, and the Sudd. The Everglades, with an area of , are the world's largest rain-fed flooded grassland on a limestone substrate, and feature some 11,000 species of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
