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The Southern Rift Valley lakes are like the Western Rift Valley lakes in that, with one exception, they are freshwater lakes. Lake Rukwa (about 5,670 square kilometres (2,190 sq mi) but quite variable) in Tanzania is the alkaline exception, lying south-east of Tanganyika, and has no outlet.
The rift is occupied by Lake Albert, Lake Edward and Lake George, along with the horst block of the Ruwenzori Mountains. Modern sediment depths in the Rift Valley are believed by 1.8 to 4 kilometers. Although volcanoes are no longer active in Uganda, the country has some remnant hot springs. [2]: 265
The African Great Lakes system, (in blue) Map of larger region including the East African Rift and the entire so-called Great Rift Valley The African Great Lakes (Swahili: Maziwa Makuu; Kinyarwanda: Ibiyaga bigari) are a series of lakes constituting the part of the Rift Valley lakes in and around the East African Rift.
The southern section of the Rift Valley includes Lake Malawi, the third-deepest freshwater body in the world, which reaches 706 metres (2,316 ft) in depth and separates the Nyassa plateau of Northern Mozambique from Malawi. The rift extends southwards from Lake Malawi as the valley of the Shire River, which flows from the lake into the Zambezi ...
Western (Albertine) Rift, IV. Eastern Rift. V. Southern Rift, VI. Eastern Highlands, VII. Drakensberg. The Afromontane regions are subregions of the Afrotropical realm, one of the Earth's eight biogeographic realms, covering the plant and animal species found in the mountains of Africa and the southern Arabian Peninsula.
Lake Victoria receives its water additionally from rivers, and thousands of small streams. The Kagera River is the largest river flowing into this lake, with its mouth on the lake's western shore. Lake Victoria is drained solely by the Nile River near Jinja, Uganda on the lake's northern shore. [26] Lake Victoria and the Great Rift Valley
Lake Tanganyika is situated within the Albertine Rift, the western branch of the East African Rift, and is confined by the mountainous walls of the valley. It is the largest rift lake in Africa and the second-largest lake by volume in the world. It is the deepest lake in Africa and holds the greatest volume of fresh water on the continent ...
The lake was formed about 18,000 years ago by a volcanic eruption blocking a valley in the Ruchiga mountains near the present day village of Muko on the north-west tip of the lake. [12] The lake's current outlet is a small stream also by Muko which flows into the Ruvuma swamp (this in turn flows into the Ruhezaminda river that ends at Lake ...
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