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Ruzizi River

From Wikipedia
Ruzizi River
transboundary river
Official nameRusizi Edit
Origin of the watercourseLake Kivu Edit
Mouth of the watercourseLake Tanganyika Edit
TributaryKaburantwa River Edit
Drainage basinCongo Basin Edit
Basin countryRwanda, Burundi, Democratic Republic of the Congo Edit
CountryBurundi, Democratic Republic of the Congo, Rwanda Edit
Coordinate location3°21′52″S 29°16′6″E, 2°29′25″S 28°53′35″E Edit
Heritage designationRamsar site Edit

De Ruzizi (dem sanso sometimes spell Rusizi, French; Rivière Ruzizi; Dutch: Ruzizi Rivier) be a river, 117 kilometres (73 mi) long,[1] wey dey flow from Lake Kivu to Lake Tanganyika insyd Central Africa, wey dey descend from about 1,500 metres (4,900 ft) to about 770 metres (2,530 ft) above sea level over ein length.[2] De steepest gradients occur over de first 40 kilometres (25 mi), wer dem build hydroelectric dams. Further downstream, de Ruzizi Plain, de floor of de Western Rift Valley, get gentle hills,[3] wey de river dey flow into Lake Tanganyika thru a delta, plus one anaa two small channels wey dey split off from de main channel.[2]

De Ruzizi be a young river, dem form about 10,000 years ago wen volcanism associate plus continental rifting create de Virunga Mountains. De mountains block Lake Kivu ein former outlet to de drainage basin of de Nile den instead force de lake overflow south down de Ruzizi den de drainage basin of de Congo.

Course

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Ruzizi River dey flow into Lake Tanganyika

Along ein upstream reaches, de river dey form part of de border between Rwanda on de east plus de Democratic Republic of the Congo (DRC) on de west.[2] Further downstream, e dey form part of de border between de DRC den Burundi, den ein lowermost reach dey lie entirely within Burundi.[2][4] To de west, de Fizi Baraka mountains tower over de river.[5] De Bridge of Concord, Burundi ein longest bridge, dey cross de river near ein mouth.[6] Tributaries of de Ruzizi River dey include de Nyamagana, Muhira, Kaburantwa, Kagunuzi, Rubyiro den Ruhwa, among odas.[7]

De Ruzizi River, wey dey flow south into Lake Tanganyika, be part of de upper watershed of de Congo River. Nineteenth-century British explorers such as Richard Francis Burton den John Hanning Speke, uncertain of de direction of flow of de Ruzizi, think say e fi flow north out of de lake toward de White Nile. Dema research den follow-up explorations by David Livingstone den Henry Morton Stanley establish say na dis no be de case. De Ruzizi dey flow into Lake Tanganyika, wich dey overflow into de Lukuga River about 120 kilometres (75 mi) south of Ujiji. De Lukuga dey flow west into de Lualaba River, a major tributary of de Congo.[8]

References

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  1. 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.
  2. 1 2 3 4 "Google Maps". Google Maps. 2013. Retrieved 14 January 2013.
  3. "Burundi Wetlands" (PDF). Ramsar. pp. 2–4. Retrieved 14 January 2013.
  4. Mokoso, Jean De Dieu Mangambu; Kavusa, Kambale; Sefu, Aruna; Milenge, Ladislas Witanene; Kiswele, Prince Kaleme (31 March 2022). "Hippopotamus amphibius Linnaeus 1758 at Ruzizi River and Lake Tanganyika (Territory of Uvira, South Kivu, DR Congo): population census and conservation implications" (PDF). Elewa.org/Journals. ELEWA. p. 3. ISSN 1997-5902. Retrieved 23 November 2024.
  5. Doyle, Mark (25 November 2004). "Retracing Che Guevara's Congo Footsteps". BBC News. Retrieved 14 January 2013.
  6. Murison, Katharine (ed.). Africa South of the Sahara (32nd ed.). Europa Publications. p. 147. ISBN 978-1-85743-131-5.
  7. "Acme Mapper (terrain)". Acme Labs. Retrieved 14 January 2013.
  8. Ondaatje, Christoper (1998). Journey to the Source of the Nile. Toronto: Harper Collins. p. 166. ISBN 978-0-00-200019-2.
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