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Serorome River
The Serorome River is a river in the Central District of Botswana, a tributary of the Limpopo River. Geology At one time the western Kalahari Region was a large, shallow inland lake, draining into the Limpopo through the Serorome Valley. Later geological upheavals re-oriented the rivers in the region to mainly flow northeast into the Zambezi. The Serorome valley is the exception, still leading to the Limpopo via a rift fault. Climate Today the river flows through relatively flat, semi-arid country with savannah grasslands, shrubs and trees. The river flows occasionally in the rainy season, which lasts from November to April, and for the remainder of the year it is dry. It flows below its confluence with the Bonwapitse River due to run off in the Bonwapitse catchment. David Livingstone visited the region in 1857, and described the Serorome as "... a lovely spot in the otherwise dry region. The wells from which we had to lift out water for our cattle are deep, but they were w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limpopo River
The Limpopo River rises in South Africa and flows generally eastward through Mozambique to the Indian Ocean. The term Limpopo is derived from Rivombo (Livombo/Lebombo), a group of Tsonga settlers led by Hosi Rivombo who settled in the mountainous vicinity and named the area after their leader. The river is approximately long, with a drainage basin in size. The mean discharge measured over a year is per second at its mouth. The Limpopo is the second largest river in Africa that drains to the Indian Ocean, after the Zambezi River. The first European to sight the river was Vasco da Gama, who anchored off its mouth in 1498 and named it Espirito Santo River. Its lower course was explored by St Vincent Whitshed Erskine in 1868–69, and Captain J F Elton travelled down its middle course in 1870. The drainage area of Limpopo River has decreased over geological time. Up to Late Pliocene or Pleistocene times, the upper course of the Zambezi River drained into the Limpopo River. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central District (Botswana)
Central is the largest of Botswana's districts in terms of area and population. It encompasses the traditional homeland of the Bamangwato people. Some of the most politically connected Batswana have come from the Central District, including former President Sir Seretse Khama, former President Festus Mogae, and former President Lt. General Seretse Ian Khama. The district borders the Botswanan districts of Chobe in the north, North-West in the northwest, Ghanzi in the west, Kweneng in southwest, Kgatleng in the south and North-East in the northeast, as well as Zimbabwe also in the northeast (Matabeleland North and Matabeleland South Provinces) and South Africa in the southeast (Limpopo Province). As of 2011, the total population of the district was 576,064 compared to 501,381 in 2001. The growth rate of population during the decade was 1.40. The population in the district was 28.45 per cent of the total population in the country. Main population centers in Central include Palapye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bonwapitse River
Bonwapitse is a river in Central Botswana Botswana (, ), officially the Republic of Botswana ( tn, Lefatshe la Botswana, label= Setswana, ), is a landlocked country in Southern Africa. Botswana is topographically flat, with approximately 70 percent of its territory being the Kalaha .... The river is estimated at approximately 886 meters above sea level, and has a total area of 1,202,985 ha. The name of the river exists in several forms: Bonapitse River, Bonapitsi, Bonwapitse.Today the river flows through relatively flat, semi-arid country with savannah grasslands, shrubs and trees. The river flows occasionally in the rainy season, which lasts from November to April, and for the remainder of the year it is dry. It flows below its confluence with the Serorome River. Rivers of Botswana {{Botswana-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
David Livingstone
David Livingstone (; 19 March 1813 – 1 May 1873) was a Scottish physician, Congregationalist, and pioneer Christian missionary with the London Missionary Society, an explorer in Africa, and one of the most popular British heroes of the late 19th-century Victorian era. David was the husband of Mary Moffat Livingstone, from the prominent 18th Century missionary family, Moffat. He had a mythic status that operated on a number of interconnected levels: Protestant missionary martyr, working-class "rags-to-riches" inspirational story, scientific investigator and explorer, imperial reformer, anti-slavery crusader, and advocate of British commercial and colonial expansion. Livingstone's fame as an explorer and his obsession with learning the sources of the Nile River was founded on the belief that if he could solve that age-old mystery, his fame would give him the influence to end the East African Arab–Swahili slave trade. "The Nile sources", he told a friend, "are valuabl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North-South Carrier
The North-South Carrier (NSC) is a pipeline in Botswana that carries raw water south for a distance of to the capital city of Gaborone. Phase 1 was completed in 2000. Phase 2 of the NSC, under construction, will duplicate the pipeline to carry water from the Dikgatlhong Dam, which was completed in 2012. A proposed extension to deliver water from the Zambezi would add another to the total pipeline length. The NSC is the largest engineering project ever undertaken in Botswana. Climate Botswana has an arid climate, with little in the way of surface water supplies. Until recently, groundwater wells were used to meet about 80% of demand for water. Some of the groundwater accumulated long ago when the climate was wetter. "Groundwater mining" is not sustainable in areas where the water is not being renewed from the surface. The more populous eastern portion of Botswana lies in the Limpopo River basin, which is considered "closed". In the South African portion of the basin, water usa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Letsibogo Dam
The Letsibogo Dam is a dam on the Motloutse River in Botswana, built to initially provide water to the industrial town of Selebi-Phikwe and surrounding local areas, with potential for use in irrigation. The dam now supplies Gaborone, the capital of the country, via a pipeline, as well as major villages along the pipeline route. Location and climate The dam is located near the village of Mmadinare. The climate is tropical and semi-arid, with 90% of rainfall during the period from November to March. Mean annual precipitation is about in the catchment area above the dam. It is very variable, with rainfall less than 40% of the average expected in one year in seven. In August 2012 the dam was only one third full, prompting concerns that there could soon be water shortages in the areas of the areas of Palapye, Mahalapye and Gaborone. Some blamed the problem in part to slow repair of leaking pipelines. Structure and operations The dam was designed for the Ministry of Minerals, Energy ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mmamabula
Mmamabula is a planned coal mine and coal-fired power station to the east of the main road and rail corridor in Botswana between Gaborone and Francistown and south of the Serorome River. The power station would be near to the village of Mmaphashalala. It is about north of the capital city of Gaborone. Coalfield The Mmamabula coalfield is considered to be a western extension of the Waterberg Coalfield in the Ellisras Basin in South Africa, to the east, which contains about 40% of South Africa's coal resources. CIC Energy of Canada owned two prospecting licences in the coal field and conducted extensive exploratory drilling between 2005 and 2012. The portions of the coalfield for which CIC Energy held licences are estimated to have 2.4 billion tonnes of thermal coal of a quality suitable for export, for local power generation and for coal gasification. Deposits were roughly 360 million tonnes in the Central block, 643 million tonnes in the Western block, and 1,392 million ton ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
