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East West

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East West
East West
East West
East West
East West
East West
East West
East West
East West
East West
East West
East West
East West
East West
East West
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Reykjavik 220, Iceland

The East African Rift is an active continental rift zone in East Africa. The EAR began developing around the onset of the Miocene, 22–25 million years ago. In the past, it was considered to be part of a larger Great Rift Valley that extended north to Asia Minor. The rift is a narrow zone that is a developing divergent tectonic plate boundary, where the African Plate is in the process of splitting into two tectonic plates, called the Somali Plate and the Nubian Plate, at a rate of 6–7 mm annually. As extension continues, lithospheric rupture will occur within 10 million years, the Somali plate will break off, and a new ocean basin will form.
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