A chain of linked basins running about 6,000 kilometres from Lebanon to Mozambique
The Jordan valley and the Dead Sea form its northern end; the Red Sea and Gulf of Aden branch off it
Geography · Physical geography
East Africa and the Levant — Mozambique to Lebanon
A chain of linked rift basins running some 6,000 kilometres from Lebanon to Mozambique, named by the Scottish geologist John Walter Gregory in the 1890s. Its African section is where the continental crust is splitting in two along the East African Rift, throwing up Kilimanjaro and the soda lakes and preserving, in its volcanic ash layers, the best early-hominin fossil record anywhere on Earth.
A chain of linked basins running about 6,000 kilometres from Lebanon to Mozambique
The Jordan valley and the Dead Sea form its northern end; the Red Sea and Gulf of Aden branch off it
Named in the 1890s by the Scottish geologist John Walter Gregory
Its Kenyan section is still sometimes called the Gregory Rift
Its African arm is a continental rift where the crust is splitting into two plates
The Nubian and Somali plates are separating by a few millimetres a year
The Leakeys' excavations in a Tanzanian gorge on its floor transformed the study of human origins
Olduvai Gorge, where Mary Leakey found Zinjanthropus in 1959
'Lucy' was found in its Ethiopian section in 1974 (1974)
The Australopithecus afarensis skeleton from Hadar, in the Afar Triangle
Its eastern arm holds caustic soda lakes where millions of lesser flamingos feed
Lakes Natron, Nakuru and Bogoria; Natron's water can reach pH 10 and 60 °C
Its western arm holds Africa's deepest lake and the world's second deepest
Lake Tanganyika, 1,470 m deep, in the Albertine Rift