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Река Рузизи

Координаты : 03 ° 21′51 ″ S 29 ° 16′04 ″ E / 3,36417 ° S 29,26778 ° E / -3,36417; 29.26778
(Перенаправлен с реки Рузизи )
Река Рузизи
Бегемопотами в реке Рузизи в Бурунди
Расположение
Страны Доктор Конго (ДРК)
Руанда
Бурунди
Физические характеристики
Источник Озеро Киву
• расположение border between Bukavu
и Cyangugu , South Kivu , DRC
 • coordinates02°29′27″S 28°53′35″E / 2.49083°S 28.89306°E / -2.49083; 28.89306[1]
 • elevation1,472 m (4,829 ft)[2]
MouthLake Tanganyika
 • location
west of Bujumbura, Burundi, Bujumbura Rural Province
 • coordinates
03°21′51″S 29°16′04″E / 3.36417°S 29.26778°E / -3.36417; 29.26778[1]
 • elevation
768 m (2,520 ft)[2]
Length117 km (73 mi)[3]
Discharge 
 • average100 m3/s (3,500 cu ft/s)[4]
Карта

Рузизи голландский (также иногда пишется Русизи , Французский : Ривиер Рузизи ; ) : Рузизи Ривье ) - это река, 117 километров (73 миль [ 3 ] Это течет от озера Киву до озера Танганьика в центральной Африке , спуская около 1500 метров (4900 футов) до примерно 770 метров (2530 футов) над уровнем моря по своей длине. [ 2 ] [ 5 ] Самые крутые градиенты встречаются в течение первых 40 километров (25 миль), где гидроэлектростанции . были построены [ 4 ] Далее вниз по течению, на равнине Рузизи , пола Западной Рифт -Долины , есть нежные холмы, [ 6 ] И река течет в озеро Танганьика через дельту , с одним или двумя небольшими каналами, отрывающимися от главного канала. [ 5 ]

Рузизи - молодая река, образованная около 10 000 лет назад, когда вулканизм, связанный с континентальным рифтингом, создал горы Вирунга . Горы заблокировали прежнюю розетку озера Киву в дренажный бассейн Нила бассейну и вместо этого заставили переполнение озера на юг вниз по Рузизи и дренажному Конго .

Along its upstream reaches, the river forms part of the border between Rwanda on the east with the Democratic Republic of the Congo (DRC) on the west.[5] Further downstream, it forms part of the border between the DRC and Burundi, and its lowermost reach lies entirely within Burundi.[5] To the west, the Fizi Baraka mountains tower over the river.[7] The Bridge of Concord, Burundi's longest bridge, crosses the river near its mouth.[8] Tributaries of the Ruzizi River include the Nyamagana, Muhira, Kaburantwa, Kagunuzi, Rubyiro and Ruhwa, among others.[9]

The Ruzizi River, flowing south into Lake Tanganyika, is part of the upper watershed of the Congo River. Nineteenth-century British explorers such as Richard Francis Burton and John Hanning Speke, uncertain of the direction of flow of the Ruzizi, thought that it might flow north out of the lake toward the White Nile. Their research and follow-up explorations by David Livingstone and Henry Morton Stanley established that this was not the case. The Ruzizi flows into Lake Tanganyika, which overflows into the Lukuga River about 120 kilometres (75 mi) south of Ujiji. The Lukuga flows west into the Lualaba River, a major tributary of the Congo.[10]

Geology

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Rifting, the slow pulling apart of a tectonic plate, has produced the East African Rift system and its many basins and lakes. The system, on the boundary between the African Plate (Nubian Plate) and the Somali Plate, has two branches, both oriented north–south. Rifting in the western branch, called the Albertine Rift, began between 25 and 10 million years ago.[11] The Ruzizi River lies along the western rift, which includes, from north to south, lakes Albert, George, Edward, Kivu, Tanganyika, Rukwa, Malawi, and others.[11]

Uplift associated with the rifting altered the connections among the region's water bodies.[11] About 13,000 to 9,000 years ago, volcanic activity blocked Lake Kivu's former outlet to the watershed of the Nile.[11] The volcanism produced mountains, including the Virungas, which rose between Lake Kivu and Lake Edward, to the north.[12] Water from Lake Kivu was then forced south down the Ruzizi.[11] This, in turn, raised the level of Lake Tanganyika, which overflowed down the Lukuga River.[11] Variations in uplift and climate have caused the Ruzizi and Lukuga to open and close multiple times since then.[11]

Hydroelectricity

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The Ruzizi I Hydroelectric Power Station was built at the Ruzizi River outlet from Lake Kivu in 1958. The Ruzizi II Hydroelectric Power Station was added in 1989.[13] Ruzizi I and II are operated by a tri-national company (Burundi, Rwanda and Democratic Republic of the Congo) owned by the Economic Community of the Great Lakes Countries. The consortium is planning two more dams, Ruzizi III and Ruzizi IV.[13]

Ruzizi I has a generating capacity of about 30 megawatts (MW) and Ruzizi II about 44 MW. Ruzizi III, to be built downstream of the other two, is projected to have a capacity of 145 MW when it becomes operational in about 2027. As part of the Ruzizi III project, Ruzizi I and II are to be refurbished. If eventually built, Ruzizi IV will be positioned between Ruzizi II and Ruzizi III and is projected to operate at more than 200 MW.[13] On January 16, 2020, the African Development Bank allocated €8 million for technical assistance on the Ruzizi IV hydroelectric project.[14] It is expected to provide 287 MW to the Democratic Republic of the Congo, Rwanda and Burundi.[14]

Fauna and flora

[edit]

Reed swamps are common along the lower main stem of the river and its tributaries. Near the mouth, the riparian swamps are up to 3 kilometres (1.9 mi) wide. The swamps' total area in Burundi has been estimated at 12,000 hectares (30,000 acres) with reeds varying in height from 2 to 4 metres (6.6 to 13.1 ft), depending on the degree of inundation. Residents use the reeds for thatching and other domestic purposes. Further from the river, much of the lower river valley consists of grassland, heavily grazed by cattle.[6]

A widely publicized man-eating crocodile, Gustave, roams the banks of the Ruzizi River and the northern shores of Lake Tanganyika. Gustave, estimated to be about 6 metres (20 ft) long and to weigh about 900 kilograms (2,000 lb), is said to have killed and eaten many people.[15] In the film documenting Gustave ("Capturing the Killer Croc"), the narrator states that "In the 1950s, buffalo, elephants and common warthogs inhabited the plain; but they were progressively exterminated by man. The only survivor amongst the large mammals has been the hippopotamus. And they share the river, in an uneasy co-existence, with the nile crocodiles."

See also

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References

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  1. ^ Jump up to: a b Geolocation with Google Earth
  2. ^ Jump up to: a b c Derived from geolocation with Google Earth.
  3. ^ Jump up to: a b Felton, Anna A.; Russell, James M.; Cohen, Andrew S.; Baker, Mark E.; Chesley, John T.; Lezzar, Kiram E.; McGlue, Michael M.; Pigati, Jeffrey S.; Quade, Jay; Curt Stager, J.; Tiercelin, Jean Jacques (2007). "Paleolimnological Evidence for the Onset and Termination of Glacial Aridity from Lake Tanganyika, Tropical East Africa". Palaeogeography, Palaeoclimatology, Palaeoecology. 252 (3–4): 405. Bibcode:2007PPP...252..405F. doi:10.1016/j.palaeo.2007.04.003.
  4. ^ Jump up to: a b Lamers, Alfred (1990). "Ruzizi II - A Fine Example of Regional Cooperation". Human Info NGO Library for Education and Development. Archived from the original on 19 April 2013. Retrieved 14 January 2013.
  5. ^ Jump up to: a b c d "Google Maps". Google Maps. 2013. Retrieved 14 January 2013.
  6. ^ Jump up to: a b "Burundi Wetlands" (PDF). Ramsar. pp. 2–4. Retrieved 14 January 2013.[permanent dead link]
  7. ^ Doyle, Mark (25 November 2004). "Retracing Che Guevara's Congo Footsteps". BBC News. Retrieved 14 January 2013.
  8. ^ Murison, Katharine (ed.). Africa South of the Sahara (32nd ed.). Europa Publications. p. 147. ISBN 978-1-85743-131-5.
  9. ^ "Acme Mapper (terrain)". Acme Labs. Retrieved 14 January 2013.
  10. ^ Ondaatje, Christoper (1998). Journey to the Source of the Nile. Toronto: Harper Collins. p. 166. ISBN 978-0-00-200019-2.
  11. ^ Jump up to: a b c d e f g Danley, Patrick D.; Husemann, Martin; Ding, Baoqing; Dipietro, Lyndsay M.; Beverly, Emily J.; Peppe, Daniel J.; et al. (2012). "The Impact of the Geologic History and Paleoclimate on the Diversification of East African Cichlids". International Journal of Evolutionary Biology. 2012: 1–20. doi:10.1155/2012/574851. PMC 3408716. PMID 22888465.
  12. ^ Clark, J. D. (1969). Kalambo Falls Prehistoric Site, Volume 1. London: Cambridge University Press. p. 34. Retrieved 16 January 2013.
  13. ^ Jump up to: a b c "Sizing Up African Hydro". Water Power. 4 October 2011. Retrieved 14 January 2013.[permanent dead link]
  14. ^ Jump up to: a b "EAST AFRICA: AfDB grants €8 million for the Ruzizi IV hydropower project". Afrik 21. 2020-01-16. Retrieved 2020-01-16.
  15. ^ McRae, Michael. "Gustave the Croc Surfaces to Strike Again". National Geographic (February 2008). Archived from the original on August 5, 2008. Retrieved 14 January 2013.
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