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A large rift is forming in the Afar region of Ethiopia, where the Nubian, Somali and Arabian tectonic plates meet and slowly pull apart. A 35-mile crack opened suddenly in 2005, showing that the area is actively rifting. Over millions of years, continued spreading could create a new ocean basin, similar to how the Atlantic once formed.
Scientists think a deep mantle plume beneath East Africa may be helping drive the separation, but the exact cause is still debated. The plates move at different speeds โ the Arabian Plate at roughly a few millimetres to about an inch per year, and the African plates even more slowly. If the rift keeps widening and the land eventually drops below sea level, seawater will fill the basin and form a new ocean.
This process is real but extremely slow, taking millions of years.