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East African Rift
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The East African Rift or East African Rift System is an active continental rift zone in East Africa. The EAR began developing around the onset of the Miocene, 22–25 million years ago. It is considered
An artificial rendering of the Albertine Rift, which forms the western branch of the East African Rift. Visible features include (from background to f
An artificial rendering of the Albertine Rift, which forms the western branch of the East African Rift. Visible features include (from background to foreground): Lake Albert, the Rwenzori Mountains, Lake Edward, the volcanic Virunga Mountains, Lake Kivu, and the northern part of Lake Tanganyika
Albertine Rift
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The Albertine Rift is the western branch of the East African Rift, covering parts of Uganda, the Democratic Republic of the Congo, Rwanda, Burundi and Tanzania. It extends from the northern end of Lak
Mount Stanley in the Rwenzori range. With an elevation of 5,109 m (16,763 ft), it is the tallest mountain in the Albertine Rift and the third tallest
Mount Stanley in the Rwenzori range. With an elevation of 5,109 m (16,763 ft), it is the tallest mountain in the Albertine Rift and the third tallest in Africa.