The Great Rift Valley or East African Rift is a continuous geographical trench, about 6,440 kilometres (3,700 mi) in length, that runs from northern Syria in Southwest Asia to central Mozambique in East Africa. The rift is bordered by a series of mountains and active volcanoes. Basically, the western part of Africa is rifting away from the eastern part. This causes all the geological activity at the Valley. Far in the future, a sea will run between these two parts of Africa. The Arabian peninsula is already almost separated. The whole process is part of plate tectonics. In eastern Africa, the valley divides into two, the Western Rift Valley and the Eastern Rift Valley.
There are about 20 UNESCO World Heritage Sites which owe their formation to the geography and geology of the Great Rift Valley.