Discover

(Redirected from Rift Valley Lakes)

The 'Rift Valley lakes' are a group of lakes formed in the Great Rift Valley which runs from south-western Asia through the whole eastern side of the African continent from north to south, with branches into Central Africa. These lakes include some of the oldest, largest and deepest lakes in the world, and many are freshwater ecoregions of great biodiversity, while others are alkaline or soda lakes supporting highly specialised organisms.
The World Wildlife Fund has designated the African Rift Valley lakes one of its Global 200 priority ecoregions for conservation.
In this article, the major lakes are listed, generally in order from north to south, and more detailed articles on each lake can be accessed through the linked names.

Contents

South-Western Asia Rift Valley Lakes

Ethiopian Rift Valley lakes

Eastern Rift Valley lakes (Kenya and Tanzania)

Western or Albertine Rift Valley Lakes

Southern Rift Valley Lakes

Other Lakes of the Great Rift Valley

See also

South-Western Asia Rift Valley Lakes

Two major lakes in the Great Rift Valley are located in Asia:

★ The Dead Sea

★ The Sea of Galilee

Ethiopian Rift Valley lakes

The Ethiopian Rift Valley lakes are the northernmost of the African Rift Valley lakes. In central Ethiopia the Great Rift Valley splits the Ethiopian highlands into northern and southern halves, and the Ethiopian Rift Valley lakes occupy the floor of the rift valley between the two highlands. Most of the Ethiopian Rift Valley lakes do not have an outlet, and most are alkaline. The major ones are

★ Lake Abaya (1160 km², elevation 1285 m), the largest Ethiopian Rift Valley lake

★ Lake Chamo (551 km², 1235 m)

★ Lake Awasa (129 km², elevation 1708 m)

★ Lake Zway (485 km², elevation 1636 m)

★ Lake Abijatta (205 km², elevation 1573 m)

★ Lake Koka (250 km², elevation 1590 m)
Lake Tana (3600 km², elevation 1788 m), the source of the Blue Nile, is not a Rift Valley lake, but lies in the Ethiopian highlands north of the Rift Valley.

Eastern Rift Valley lakes (Kenya and Tanzania)

South of the Ethiopian highlands, the Rift Valley splits in two. The Eastern Rift is home to the Kenyan Rift Valley lakes, while most of the Central African Rift Valley lakes lie in the Western Rift. The Kenyan section of the Rift Valley is home to eight lakes, of which two are freshwater and the rest alkaline. Of the latter, the shallow soda lakes of the Eastern Rift Valley have crystallised salt turning the shores white, and are famous for the large flocks of flamingo that feed on crustaceans.


★ Lake Turkana (6405 km², elevation 360 m), alkaline, is the largest of the Kenyan lakes, on the border of Kenya and Ethiopia.

★ Lake Logipi is a seasonal, shallow hot-spring fed soda lake in the Suguta Valley just south of Lake Turkana.

★ Lake Baringo (80 sq miles, elevation 1000 m) freshwater, second largest of the Kenyan Rift Valley lakes,

★ Lake Bogoria(34 km², elevation 990 m) shallow soda lake, a national preserve

★ Lake Nakuru (40 km², elevation 1759 m) shallow soda lake, has been a national park since 1968

★ Lake Elmenteita, shallow soda lake

★ Lake Naivasha (160 km² — varies somewhat with rainfall, elevation 1,890 m), freshwater lake, is the highest in this group.

★ Lake Magadi, shallow soda lake
The Tanzanian section of this group has two alkaline lakes:

★ Lake Natron, shallow soda lake

★ Lake Eyasi, shallow soda lake

Western or Albertine Rift Valley Lakes

The lakes of the Western or Albertine Rift, together with Lake Victoria, include the largest, deepest and oldest of the Rift Valley lakes. They are also referred too as the Central African lakes. Lakes Albert, Victoria, and Edward are part of the Nile River basin.
Lake Victoria (elevation 1134 m), with an area of 68,800 km², is the largest lake in Africa, but is not actually within the rift valley; it occupies a depression between the eastern and western rifts, formed by the uplift of the rifts to either side. Lakes Victoria, Tanganyika, and Malawi are sometimes collectively known as the African Great Lakes.
The Western Rift Valley Lakes are fresh water and home to an extraordinary number of species. Approximately 1,500 cichlid fish (Cichlidae) species live in the lakes (See Hubert Sauper's ''Darwin's Nightmare'' concerning a reduction in biodiversity). In addition to the cichlids, populations of Clariidae, Claroteidae, Mochokidae, Poeciliidae, Mastacembelidae, Centropomidae, Cyprinidae, Clupeidae and other fish families are also found in these lakes. The lakes are also important habitats for a number of amphibian species, including ''Bufo kisoloensis'', ''Bufo keringyagae'', ''Cardioglossa cyaneospila'', and ''Nectophryne batesii''.

★ Lake Albert (5300 km², elevation 615 m) is the northernmost lake in the western rift.

★ Lake Edward (2325 km², elevation 912 m) drains north into Lake Albert

★ Lake Kivu (2220 km², elevation 1460 m) empties into Lake Tanganyika via the Ruzizi River.

★ Lake Tanganyika (32,000 km², elevation 773 m) is the largest and deepest of the Rift Valley lakes (more than 1400 meters), and is thought to be the second-oldest lake on the planet (after Lake Baikal). It is part of the Congo River basin, feeding into the River Congo via the Lukuga River.

Southern Rift Valley Lakes

The Southern Rift Valley lakes are like the Western Rift Valley lakes in that, with one exception, they are freshwater lakes.

★ Lake Rukwa (about 5670 km² but quite variable) in Tanzania is the alkaline exception, lying south-east of Tanganyika, and has no outlet.

★ Lake Malawi (30,000 km², elevation 500 m), the second largest and second deepest of the Rift Valley lakes at over 700 meters, is drained by the Shire River, a tributary of the Zambezi River.

★ Lake Malombe (450 km²) is on the Shire River

★ Lake Chilwa (1750 km², elevation 622 m) has no outlet but extensive wetlands. It is the southernmost of the Rift Valley lakes.

Other Lakes of the Great Rift Valley

★ Lake Mweru (4350 km², elevation 922 m) lies in the Lake Mweru-Luapula graben which is a branch off the Albertine rift.

★ Lake Mweru Wantipa (1500,km², elevation 930 m) is a marshy lake between lakes Tanganyika and Mweru, and is endorheic but may overflow into Lake Mweru at times of very high flood.
In the Tertiary geological period, the Red Sea may have been the largest Great Rift Valley lake, as the Bab el Mandeb closed and cut off the sea from the Indian Ocean. It eventually dried out.

See also

★ Great Rift Valley