The African Great Lakes are a series of lakes constituting the part of the Rift Valley lakes in and around the East African Rift. These lakes, located within the tropics, include Turkana, Victoria, Tanganyika, Kivu, Edward, Malawi and Albert.
The lakes are shared by 10 countries, namely Ethiopia, Uganda, Tanzania, Ethiopia, Rwanda, Kenya, Burundi, Zambia, Malawi, Democratic Republic of Congo DRC and Mozambique. The African Great Lakes are all part of the rift valley lakes and are endowed with a plethora of uniqueness.
Collectively, the lakes command approximately 25% of the total global unfrozen freshwaters and covers a total surface area of about 138,447km2. The great lakes of eastern African are home to some of the largest and most ecologically diverse freshwater systems in the world, supporting millions of people with drinking water, food and livelihoods.
The lakes are important habitats for a number of fish and amphibian species, abundant birdlife and numerous crocodiles. In the surrounding lake region, one finds elephants, gorillas, hippos and other wildlife in the Great Rift's mountains and valleys.
Despite their beauty, the great lakes rank as one of the world's most endangered water systems.
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The highlands are relatively cool, with average temperatures ranging between 17 °C (63 °F) and 19 °C (66 °F) and abundant rainfall. Forests are dominant in the lowlands of the Congo-Zaire Basin, while grasslands and savannas (dry grasslands) are most common in the southern and eastern highlands. Temperatures in the lowlands average about 35 °C (95 °F). Around Lake Turkana, the climate is hot and very dry.
What Is The Significance Of Lake Victoria To East Africa? - Ecosystem Essentials
The Western Rift Valley lakes are freshwater and home to an extraordinary number of endemic species. More than 1,500 cichlid fish species live in the lakes, as well as other fish families. The lakes are also important habitats for a number of amphibian species. Nile crocodiles are numerous.
The Lake Turkana area is home to hundreds of species of birds endemic to Kenya. The flamingo wades in its shallows. The East African rift system also serves as a flyway for migrating birds, bringing in hundreds more. Vegetation ranges from rainforest to savanna grasses. In some lakes, rapidly growing invasive plants, like the surface-choking water hyacinth and shore-clogging papyrus, are problems.
Formation and Geological Significance
Until 12 million years ago, the bountiful waters of the equatorial plateau either flowed west into the Congo River system or east to the Indian Ocean. This was changed by the formation of the Great Rift Valley.
A rift is a weak place in Earth's crust due to the separation of two tectonic plates, often accompanied by a graben, or trough, in which lake water can collect. This rift began when East Africa, impelled by currents in the mantle, began separating from the rest of Africa, moving to the northeast.
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Lake Victoria is not actually within the Rift Valley. Around two to three million years ago, Lake Turkana was larger and the area more fertile, making it a center for early hominids. Richard Leakey led numerous anthropological excavations in the area, which yielded many important discoveries of hominin remains. The two-million-year-old Skull 1470 was found in 1972.
It was originally thought to be Homo habilis, but some anthropologists have assigned it to a new species, Homo rudolfensis, named after the lake (previously known as Lake Rudolf). In 1984, the Turkana Boy, a nearly complete skeleton of a Homo erectus boy was discovered.
Various rivers provide interlinkages between the great lakes. For example, Lake Kivu connects to Lake Tanganyika through Rusizi River while River Nile flows from Lake Victoria to Lake Albert through Lake Kyoga situated in central Uganda and then flows out as White Nile towards South Sudan finally emptying her waters into the Mediterranean Sea.
Semliki River links Lake Edward with Lake Albert. Lukuga River flows from Lake Tanganyika into the Congo River which snakes into the Atlantic Ocean. The Shire River empties Lake Malawi into the Zambezi River which discharges its water into the Indian Ocean.
All African Great Lakes are transboundary resources and hence nations in this region are encouraged to collectively come up with similar legal mechanisms to govern these treasured gems for posterity.
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Individual Lakes: Key Features
Lake Victoria
Lake Victoria, shared by Kenya, Tanzania and Uganda, acts as a reservoir for at least four hydropower stations along the Nile River. Globally, the lake is the second largest freshwater after Lake Superior in North America and the largest lake in Africa. With a surface area of approximately 59,947 km2, Lake Victoria is Africa's largest lake by area, the world's largest tropical lake, and the world's second-largest fresh water lake by surface area after Lake Superior in North America.
In terms of volume, Lake Victoria is the world's ninth-largest continental lake, containing about 2,424 km3 of water. Lake Victoria occupies a shallow depression in Africa.
Lake Victoria receives 80 percent of its water from direct rainfall. Average evaporation on the lake is between 2.0 and 2.2 metres (6 ft 7 in and 7 ft 3 in) per year, almost double the precipitation of riparian areas. 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.
In the Kenya sector, the main influent rivers are the Sio, Nzoia, Yala, Nyando, Sondu Miriu, Mogusi, and Migori. The only outflow from Lake Victoria is the Nile River, which exits the lake near Jinja, Uganda.
In terms of contributed water, this makes Lake Victoria the principal source of the longest branch of the Nile. However, the most distal source of the Nile Basin, and therefore the ultimate source of the Nile, is more often considered to be one of the tributary rivers of the Kagera River (the exact tributary remains undetermined), and which originates in either Rwanda or Burundi.
The uppermost section of the Nile is generally known as the Victoria Nile until it reaches Lake Albert.
Lake Tanganyika
Lake Tanganyika, world’s longest lake, and the deepest lake in Africa, borders Tanzania, Burundi, Zambia and Democratic Republic of Congo, covers an estimated surface area of 32600 km2, a volume of 18980 km3 and a shoreline of 1828 km. Lake Tanganyika is also the largest lake among the Albertine Rift lakes.
Lake Tanganyika was formed about 9-12 million years ago in the western arm of the East African rift valley. It is located within Burundi (8%), Democratic Republic of the Congo (DRC) (45%), Tanzania (41%), and Zambia (6%). It has a basin area of 223,000 km2 and extends for 676 km in a north-south direction and averages 50 km in width.
It is the deepest lake in Africa with a maximum depth of 1,470 m and average depth of 580 m, the second deepest lake in the world, and the largest among the rift lakes with a surface area of 32,600 km2 and a shoreline of 1,828 km. The lake holds an estimated 18,980 km3 of water, which is as much as the five North American Great Lakes combined. Despite its large volume, the lake is sensitive to climatic conditions.
The climate of the basin is characterized by two seasons; a wet season between October and April, and a dry season between May and September. Rainfall is estimated at 29 km3/year and evaporation at 50 km3/year, therefore, any major drop in annual rainfall and consistent increase in temperature can affect the lake’s water level.
Lake Turkana
Lake Turkana, shared by Kenya and Ethiopia is the largest permanent desert lake. The lake, though alkaline and shallow whose depth varies between 30 m in some places with other places being as deep as 109 m.
Lake Malawi/ Niassa/ Nyasa
Lake Malawi/ Niassa/ Nyasa shared by Tanzania, Malawi and Mozambique, has an average depth of 264 m and a maximum depth of 700m making it the third deepest freshwater lake globally and the ninth largest freshwater lake on Earth.
Lake Kivu
Lake Kivu is shared between Democratic Republic of Congo DRC and Rwanda with a shoreline of 860 km, a volume of 500 km3 and a surface area of about 2370 km2 making it the second smallest African Great lakes and situated at the highest altitude. It is the third deepest among the African Great Lakes and the only lake with high amounts of Carbon (IV) oxide and methane among those lakes.
Lake Albert
Lake Albert is shared by Democratic Republic of Congo DRC and Uganda.
Lake Edward
Lake Edward is the smallest African Great Lake and is shared by Democratic Republic of Congo DRC and Uganda occupying a surface area of 2325 km2, a volume of 40 km3 and a shoreline of 290 km.
Economic and Social Impact
Fishing-primarily of tilapia species but also of Nile perch-provides the main livelihood for people in the region. With four Great Lakes on its borders, Uganda ranks as one of the world's largest producers of freshwater fish.
The economies of the Great Lakes region states have different structures and are at various stages of development. The population density of the Lake Tanganyika basin varies between 13-250 persons/km2.
The full drainage basin has a population of greater than 10 million people which is growing at a rate of 2.0-3.2 percent per year. This is putting much pressure on the resources and is worsened by the small economies of the countries that border the lake, which are among the poorest nations in the world with an average per capita GNP of US $110-320. The lake basin has the poorest and least developed regions of the four riparian countries with low literacy levels, especially in parts of Burundi and DRC where a large portion of the population live on less than US $1 per day. This makes adaptation to environmental stresses such as climate change a major problem.
Environmental Challenges and Conservation
Starting in the 1950s, many species have been introduced to Lake Victoria where they have become invasive and a prime reason for the extinction of many endemic haplochromine cichlids. Among the introductions are several tilapias: redbreast (Coptodon rendalli), redbelly (C. zillii), Nile (Oreochromis niloticus) and blue-spotted tilapias (O. leucostictus), as well as Nile perch (Lates niloticus) and silver cyprinid (Rastrineobola argentea).
The release of large amounts of untreated wastewater (sewage) and agricultural and industrial runoff directly into Lake Victoria over the past 30 years has greatly increased the nutrient levels of nitrogen and phosphorus in the lake "triggering massive growth of exotic water hyacinth, which colonised the lake in the late 1990s".
This invasive weed creates anoxic (total depletion of oxygen levels) conditions in the lake, inhibiting decomposing plant material, raising toxicity and disease levels to both fish and people. At the same time, the plant's mat or "web" creates a barrier for boats and ferries to maneuver, impedes access to the shoreline, interferes with hydroelectric power generation, and blocks the intake of water for industries.
| Lake | Countries | Surface Area (km2) | Max. Depth (m) |
|---|---|---|---|
| Victoria | Kenya, Tanzania, Uganda | 59,947 | 82 |
| Tanganyika | Tanzania, Burundi, Zambia, DRC | 32,600 | 1,470 |
| Malawi/Nyasa | Tanzania, Malawi, Mozambique | 29,600 | 706 |
| Turkana | Kenya, Ethiopia | 6,405 | 109 |
| Albert | DRC, Uganda | 5,600 | 51 |
| Kivu | DRC, Rwanda | 2,700 | 480 |
| Edward | DRC, Uganda | 2,325 | 112 |
More recently, measures have been used such as the introduction of natural insect predators, including two different water hyacinth weevils and large harvesting and chopping boats, which seem to be much more effective in eliminating the water hyacinth.
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