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Kivu

Region in the Democratic Republic of the Congo

Kivu
Summary

Region in the Democratic Republic of the Congo

Map of eastern Democratic Republic of Congo
[[North Kivu]] and [[South Kivu]] ("the Kivus")

Kivu is the name for a large region in the eastern Democratic Republic of the Congo that borders Lake Kivu. It was a Région (read 'province') of the country under the rule of Mobutu Sese Seko from 1966 to 1988. As an official Région in 1986 it was divided into the three "Sub-Regions" (Sous-Régions in French) of: Nord-Kivu, Sud-Kivu and Maniema, Those three became the current provinces in the reorganization of 1988.{{Cite journal |url=https://journals.openedition.org/espacepolitique/1296 |accessdate=7 March 2025 |last=Bruneau |first=Jean-Claude |title=Les nouvelles provinces de la République Démocratique du Congo : construction territoriale et ethnicités |language=fr

History

Kivu has been repeatedly subjected to major conflicts since the early 20th century. Under Belgian colonial rule, it was the site of several religious revolts such as the 1944 Kivu uprising. Following independence, it was a battleground of the Simba rebellion, First Congo War, and Second Congo War, and has been the site of an ongoing military conflict since the early 2000s. In 2025 substantial parts of the area came under the control of the March 23 Movement.

From August 2018 to June 2020, an Ebola epidemic affected the region.

Geography

Kivu is also the name for the entire region surrounding Lake Kivu, including the portions in Rwanda which contain the vast majority of the lake area's population (the contiguous towns of Goma in the Democratic Republic of Congo and Gisenyi in Rwanda, with a combined population approaching 1,000,000, form the largest urbanised area in the Lake Kivu area). The area is characterized by lush vegetation and an extended growing season due in part to its high elevation (1500 m or 4900 ft at the lakeshore) and the volcanic nature of its soil. The Kivu region represents the high point of the East African Rift Valley.

The lake itself contains a massive amount of carbon dioxide in its depths, and there is some concern that tectonic activity (rifting) and/or volcanic activity might cause a limnic eruption, a sudden release of this captured carbon dioxide. If this were to happen it would devastate the population around the lake; however, the likelihood of this occurring is in dispute.

Approximate correspondence between historical and current provinces

Belgian CongoRepublic of the CongoZaireDemocratic Republic of the Congo190819191932194719631966197119881997201522 districts4 provinces6 provinces6 provinces21 provinces + capital8 provinces + capital8 provinces + capital11 provinces11 provinces26 provinces
Bas-UeleOrientaleStanleyvilleOrientaleUeleOrientaleHaut-ZaïreOrientaleBas-Uele
Haut-UeleHaut-Uele
IturiKibali-IturiIturi
StanleyvilleHaut-CongoTshopo
Aruwimi
ManiemaCostermansvilleKivuManiemaKivuManiema
Lowa
KivuNord-KivuNord-Kivu
Kivu-CentralSud-Kivu

References

References

  1. [[International Crisis Group]]. (9 July 2009). "Congo: A Comprehensive Strategy to Disarm the FDLR".
  2. (18 April 2012). "Democratic Republic of Congo: Mobility and Methods of Transportation between Grand Kivu and Kinshasa". [[Immigration and Refugee Board of Canada]].
  3. Stearns, Jason. (2012). "North Kivu: The background to conflict in north Kivu province in eastern Congo.".
  4. "Lake Kivu Home Page".
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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