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Concept
Lake Edward
Summary
Lake Edward (locally Rwitanzigye or Rweru) is one of the smaller African Great Lakes. It is located in the Albertine Rift, the western branch of the East African Rift, on the border between the Democratic Republic of the Congo (DRC) and Uganda, with its northern shore a few kilometres south of the equator.
Henry Morton Stanley first saw the lake in 1888, during the Emin Pasha Relief Expedition. The lake was named in honour of Albert Edward, Prince of Wales, son of then British monarch Queen Victoria, and later to become King Edward VII.
In 1973, Uganda and Zaire (DRC) renamed it Lake Idi Amin after Ugandan dictator Idi Amin. After his overthrow in 1979, it recovered its former name.
In 2014, the lake was the center of an oil dispute. SOCO international entered the premises of the Virunga National Park where the lake is situated to prospect for oil. However, villagers and workers who attempted to stop the oil company from entering the area were beaten up and even kidnapped and tortured. Plans to redraw the lines of Virunga's boundaries and exclude the lake were taken into consideration. However, since the Park is a world heritage site and the lake is part of it such plans naturally go against the World Heritage Convention.
Lake Edward lies at an elevation of , is long by wide at its maximum points, and covers a total surface area of , making it the 15th-largest on the continent. The lake is fed by the Nyamugasani River, the Ishasha River, the Rutshuru River, the Ntungwe River, and the Rwindi River. Lake George to the northeast empties into it via the Kazinga Channel. Lake Edward empties to the north via the Semliki River into Lake Albert.
The western escarpment of the Great Rift Valley towers up to above the western shore of the lake. The southern and eastern shores are flat lava plains. The Ruwenzori Mountains are north of the lake.
The region shows much evidence of volcanic activity over the last 5000 years. The Katwe-Kikorongo and Bunyaruguru Volcanic Fields, with extensive cones and craters, lie either side of the Kazinga Channel on the northwest shore of the lake.
Official source
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