The East African Rift was formed as a result of tectonic processes where the African tectonic plate is splitting into two smaller plates: the Somali Plate and the Nubian Plate. This rifting process began around 25 million years ago and is characterized by volcanic activity and the creation of fault lines as the Earth's crust stretches and thins. Over time, this has led to the formation of a series of valleys, lakes, and volcanic mountains, marking a significant geological feature in East Africa. The ongoing rifting continues to shape the landscape and has implications for seismic activity in the region.
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