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Kwando
The Cuando River (or Kwando in the non-colonial spelling) is a river in south-central Africa flowing through Angola and Namibia's Caprivi Strip and into the Linyanti Swamp on the northern border of Botswana. Below the swamp, the river is called the Linyanti River and, farther east, the Chobe River, before it flows into the Zambezi River. Course The Cuando rises in the central plateau of Angola on the slopes of Mount Tembo, thence flowing southeast along the Zambian border. Along this reach it flows in a maze of channels in a swampy corridor 5–10 km wide (map 1: the border with Zambia is the eastern bank of this floodplain, not the river channel). As with all rivers in south-central Africa its flow varies enormously between the rainy season when it floods and may be several kilometres wide, and the dry season when it may disappear into marshes. The Cuando continues in its marshy channel across the neck of the Caprivi Strip of Namibia (map, 2) and then forms the bord ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caprivi Region
The Zambezi Region is one of the 14 regions of Namibia. It is located in the north-eastern part of the country. It is largely concurrent with the major Zambezi River where it gets its name from. The region has eight constituencies and its capital is the town of Katima Mulilo. The self-governed village Bukalo is also found in this region. The Zambezi Region had a population of 90,596 in 2011. As of 2020, it had 47,884 registered voters. Politics The region comprises eight electoral constituencies: * Judea Lyaboloma * Kabbe North * Kabbe South * Katima Mulilo Rural * Katima Mulilo Urban * Kongola * Linyanti * Sibinda In the 2015 regional elections SWAPO won in all eight constituencies and obtained 77.5% of all votes ( 2010: 80%). In the 2020 regional election SWAPO still had the vast majority of votes (45.4%) but lost four of the eight constituencies, three to independent candidates and one to the Independent Patriots for Change (IPC), an opposition party formed in A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 |
Zambezi River At Junction Of Namibia, Zambia, Zimbabwe & Botswana
The Zambezi River (also spelled Zambeze and Zambesi) is the fourth-longest river in Africa, the longest east-flowing river in Africa and the largest flowing into the Indian Ocean from Africa. Its drainage basin covers , slightly less than half of the Nile's. The river rises in Zambia and flows through eastern Angola, along the north-eastern border of Namibia and the northern border of Botswana, then along the border between Zambia and Zimbabwe to Mozambique, where it crosses the country to empty into the Indian Ocean. The Zambezi's most noted feature is Victoria Falls. Its other falls include the Chavuma Falls at the border between Zambia and Angola, and Ngonye Falls near Sioma in western Zambia. The two main sources of hydroelectric power on the river are the Kariba Dam, which provides power to Zambia and Zimbabwe, and the Cahora Bassa Dam in Mozambique, which provides power to Mozambique and South Africa. Additionally, two smaller power stations are along the Zambezi Rive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kalahari 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 |
Zambezi River
The Zambezi River (also spelled Zambeze and Zambesi) is the fourth-longest river in Africa, the longest east-flowing river in Africa and the largest flowing into the Indian Ocean from Africa. Its drainage basin covers , slightly less than half of the Nile's. The river rises in Zambia and flows through eastern Angola, along the north-eastern border of Namibia and the northern border of Botswana, then along the border between Zambia and Zimbabwe to Mozambique, where it crosses the country to empty into the Indian Ocean. The Zambezi's most noted feature is Victoria Falls. Its other falls include the Chavuma Falls at the border between Zambia and Angola, and Ngonye Falls near Sioma in western Zambia. The two main sources of hydroelectric power on the river are the Kariba Dam, which provides power to Zambia and Zimbabwe, and the Cahora Bassa Dam in Mozambique, which provides power to Mozambique and South Africa. Additionally, two smaller power stations are along the Zambezi Ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zambezi
The Zambezi River (also spelled Zambeze and Zambesi) is the fourth-longest river in Africa, the longest east-flowing river in Africa and the largest flowing into the Indian Ocean from Africa. Its drainage basin covers , slightly less than half of the Nile's. The river rises in Zambia and flows through eastern Angola, along the north-eastern border of Namibia and the northern border of Botswana, then along the border between Zambia and Zimbabwe to Mozambique, where it crosses the country to empty into the Indian Ocean. The Zambezi's most noted feature is Victoria Falls. Its other falls include the Chavuma Falls at the border between Zambia and Angola, and Ngonye Falls near Sioma in western Zambia. The two main sources of hydroelectric power on the river are the Kariba Dam, which provides power to Zambia and Zimbabwe, and the Cahora Bassa Dam in Mozambique, which provides power to Mozambique and South Africa. Additionally, two smaller power stations are along the Zambezi Riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kalahari
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] |
River Capture
Stream capture, river capture, river piracy or stream piracy is a geomorphological phenomenon occurring when a stream or river drainage system or watershed is diverted from its own bed, and flows instead down the bed of a neighbouring stream. This can happen for several reasons, including: *Tectonic earth movements, where the slope of the land changes, and the stream is tipped out of its former course *Natural damming, such as by a landslide or ice sheet *Erosion, either **Headward erosion of one stream valley upwards into another, or **Lateral erosion of a meander through the higher ground dividing the adjacent streams. **Within an area of karst topography, where streams may ''sink'', or flow underground (a sinking or losing stream) and then reappear in a nearby stream valley *Glacier retreat The additional water flowing down the capturing stream may accelerate erosion and encourage the development of a canyon (gorge). The now-dry valley of the original stream is known a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Liambesi
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kasane
Kasane is a town in Botswana, close to Africa's 'Four Corners', where four countries almost meet: Botswana, Namibia, Zambia and Zimbabwe. It is at the far north-eastern corner of Botswana where it serves as the administrative center of the Chobe District. The population of Kasane was 9,244 in 2011 census. Kasane briefly obtained international fame as the location of the remarriage of Elizabeth Taylor to Richard Burton, in 1975. Transport The town lies on the south bank of the wide Chobe River which forms the border with the extreme tip of Namibia's Caprivi Strip. The Namibian island of Impalila lies opposite the town on the north bank of the river, and there is a border crossing by passenger ferry to Namibia. About to the east of Kasane is the village of Kazungula, where Botswana has of frontage to the Zambezi river immediately below its confluence with the Chobe River. Here the Kazungula border post serves the Kazungula Bridge crossing to Kazungula in Zambia on the north b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kazungula Ferry
The Kazungula Ferry was a pontoon ferry across the Zambezi River between Botswana and Zambia. It was one of the largest ferries in south-central Africa, having a capacity of . The service was provided by two motorised pontoons and operated between border posts at Kazungula, Zambia and Kazungula, Botswana. It linked the Livingstone-Sesheke road (which connects to the Trans–Caprivi Highway at Katima Mulilo and forms part of the Walvis Bay Corridor) to the main north–south highway of Botswana through Francistown and Gaborone to South Africa, and also to the Kasane-Victoria Falls road through Zimbabwe. It served the international road traffic of three countries directly (Zambia, Zimbabwe and Botswana) and of three more indirectly (Namibia, South Africa and DR Congo). Whether Botswana and Zambia actually shared a common border, or whether the ferry was illegally crossing into Namibian or Rhodesian territory, was the subject of dispute. In 1970, South Africa (which at the time oc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boteti River
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
