|
Chobe River
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 bo ... [...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 nort ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Makgadikgadi
Lake Makgadikgadi ( tn, Letsha la Makgadikgadi, label=Setswana, ) was a paleolake that existed in what is now the Kalahari Desert in Botswana from 2,000,000 years BP to 10,000 years BP. It may have once covered an area of from and was 30 m deep. The Okavango, Upper Zambezi, and Cuando rivers once all emptied into the lake. Its remains are seen in the Makgadikgadi salt pans, one of the largest salt pans in the world. DNA research suggests the lake region is the homeland of ''Homo sapiens'', where humans first evolved as a distinct species about 200,000 years ago, before expanding to other parts of Africa about 70,000 years later. Origin and history Approximately 3 million years ago, strong easterly winds formed long dunes, which ran from east to west across the middle of the Kalahari Desert. During wetter times, these dunes channeled the great rivers of the area, the Okavango, Chobe, and Upper Zambezi, southeastward to join with the Limpopo River and drain into the I ... [...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 |
River Bifurcation
River bifurcation (from la, furca, fork) occurs when a river flowing in a single stream separates into two or more separate streams (called distributaries) which then continue downstream. Some rivers form complex networks of distributaries, typically in their deltas. If the streams eventually merge again or empty into the same body of water, then the bifurcation forms a river island. River bifurcation may be temporary or semi-permanent, depending on the strength of the material that is dividing the two distributaries. For example, a mid-stream island of soil or silt in a delta is most likely temporary, due to low material strength. A location where a river divides around a rock fin, e.g. a volcanically formed dike, or a mountain, may be more lasting as a result of higher material strength and resistance to weathering and erosion. A bifurcation may also be man-made, for example when two streams are separated by a long bridge pier. Scientific study of bifurcation River bifurc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barotseland
Barotseland ( Lozi: Mubuso Bulozi) is a region between Namibia, Angola, Botswana, Zimbabwe including half of eastern and northern provinces of Zambia and the whole of Democratic Republic of Congo's Katanga Province. It is the homeland of the Lozi people or ''Barotse'', or Malozi, who are a unified group of over 46 individual formerly diverse tribes related through kinship, whose original branch are the Luyi (Maluyi), and also assimilated Southern Sotho tribe of South Africa known as the Makololo. The Barotse speak Silozi, a language most closely related to Sesotho. Barotseland covers an area of 252,386 square kilometres, but is estimated to have been twice as large at certain points in its history. Once an empire, the Kingdom stretched into Namibia, Angola, Botswana, Zimbabwe including half of eastern and northern provinces of Zambia and the Democratic Republic of Congo's Katanga Province. Under the British colonial administration, Barotseland was a Protectorate of the Bri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Makololo Tribe
The Kololo or Makololo are a subgroup of the Sotho-Tswana people native to Southern Africa. In the early 19th century, they were displaced by the Zulu, migrating north to Barotseland, Zambia. They conquered the territory of the Luyana people and imposed their own language. The combination of Luyana and Kololo languages gave rise to the current Lozi language spoken by the Lozi people, descendants of the Luyana and nearby tribes. In 1864, the Kololo kingdom was overthrown and some chiefs moved to Chikwawa District, Malawi, with David Livingstone. Name The Kololo are also known as Makololo. When referring to Kololo people in plural, their endonym is Bakololo, which includes the Bantu clitic ''ba-''. The Kololo appear to be named after Kololo, the wife of their first chief, Sebitwane. Another theory is that it is a Luyana word meaning "bald" referring to their conqueror's hairstyles. History Origins The Kololo are said to have originated in the North Orange Free State region (c ... [...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[...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] |
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 ti ... [...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 R ... [...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] |
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 as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
