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  2. Aswa Dislocation - Wikipedia

    en.wikipedia.org/wiki/Aswa_Dislocation

    The reactivated section of the Aswa lineament connects the eastern and western branches of the East African rift system. It seems also to truncate the Nyanza rift, which extends ENE from Lake Victoria. The section of the Aswa Dislocation between the two rifts forms part of the boundary between the Somali Plate and the African Plate.

  3. East African Revival - Wikipedia

    en.wikipedia.org/wiki/East_African_Revival

    The East African Revival (Luganda: Okulokoka) was a movement of renewal in the Christian Church in East Africa during the late 1920s and 1930s. It began on a hill called Gahini in then Belgian Ruanda-Urundi in 1929, and spread to the eastern mountains of Belgian Congo, Uganda Protectorate (British Uganda), Tanganyika Territory and Kenya Colony during the 1930s and 1940s.

  4. East African Railways and Harbours Corporation - Wikipedia

    en.wikipedia.org/wiki/East_African_Railways_and...

    The East African Railways and Harbours Corporation (EAR&H) is a defunct company that operated railways and harbours in East Africa from 1948 to 1977. It was formed in 1948 for the new East African High Commission by merging the Kenya and Uganda Railways and Harbours with the Tanganyika Railway of the Tanganyika Territory .

  5. Rukwa Rift Basin - Wikipedia

    en.wikipedia.org/wiki/Rukwa_Rift_Basin

    Rukwa Rift Basin. Coordinates: 8.16305°S 32.56492°E. The Rukwa Rift Basin, located in southwestern Tanzania, is an endorheic rift basin that contains Lake Rukwa. It forms part of the East African Rift system and has produced a number of Cretaceous and Oligocene fossils.

  6. Rwenzori Mountains - Wikipedia

    en.wikipedia.org/wiki/Rwenzori_Mountains

    The Ruwenzori, also spelled Rwenzori and Rwenjura, or Rwenzururu ( Swahili: Milima ya Ruwenzori) are a range of mountains in eastern equatorial Africa, located on the border between Uganda and the Democratic Republic of the Congo. The highest peak of the Ruwenzori reaches 5,109 metres (16,762 ft), and the range's upper regions are permanently ...

  7. Ol Doinyo Lengai - Wikipedia

    en.wikipedia.org/wiki/Ol_Doinyo_Lengai

    Ol Doinyo Lengai is part of the Gregory Rift, which is part of the active East African Rift. The East African Rift is a continental rift extending from eastern to southern Africa over a length of 4,000 kilometres (2,500 mi), where there is high heat flow through a thinner crust. In the Gregory Rift, spreading began about 1.2 million years ago ...

  8. Muglad Basin - Wikipedia

    en.wikipedia.org/wiki/Muglad_Basin

    Mesozoic rift basins including Muglad develop oblique to East African Rift. The Muglad Basin is a large rift basin in Northern Africa. The basin is situated within southern Sudan and South Sudan, and it covers an area of approximately 120,000 square kilometres (46,000 sq mi) across the two nations. It contains a number of hydrocarbon ...

  9. Scramble for Africa - Wikipedia

    en.wikipedia.org/wiki/Scramble_for_Africa

    The Scramble for Africa [a] was the invasion and colonisation of most of Africa by seven Western European powers during the era of "New Imperialism" (1833–1914). In 1870, 10% of the continent was formally under European control. By 1914, this figure had risen to almost 90%, with only Liberia and Ethiopia retaining their full sovereignty.