The East African Rift (EAR) or East African Rift System (EARS) is an active continental rift zone in East Africa. The EAR began developing around the onset of the Miocene, 22–25 million years ago. [1] It was formerly considered to be part of a larger …

The East African Rift System (EARS) is one of the geologic wonders of the world, a place where the earth's tectonic forces are presently trying to create new plates by splitting apart old ones.

East African Rift System, one of the most extensive rifts on Earth’s surface, extending from Jordan in southwestern Asia southward through eastern Africa to Mozambique. The system is some 4,000 miles (6,400 km) long and averages 30–40 miles (48–64 km) wide.

The East African Rift Valley (EAR) is a developing divergent plate boundary in East Africa. Here the eastern portion of Africa, the Somalian plate, is pulling away from the rest of the continent, that comprises the Nubian plate.

2023年9月9日 · The East African Rift (EAR) is an extensive, intra-continental lowland region that is being slowly split by tectonic activity. As the name posits, it can be traced across the Eastern portion of the African continent, running in a generally North-South direction but with many meandering deviations.

2019年12月1日 · The East African Rift (EAR) is an extensive continental rift located in East Africa. The rift has been developing for the past 20 to 25 million years, beginning in the Miocene epoch, and was previously considered to be part of the much larger Great Rift Valley.

The east African rift valley was formed by the movement of tectonic plates in the Earth’s crust. The African plate and the Somali plate are moving away from each other, creating a rift zone between them. As the plates move apart, magma rises to the surface, creating volcanic activity.