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Some examples of rift volcanoes include those found along the East African Rift Valley, such as Mount Kilimanjaro and Mount Kenya. These volcanoes are formed along the divergent boundary where tectonic plates are moving away from each other, allowing magma to rise to the surface and create volcanic activity.
Volcanoes are found along the Rift Valley due to the movement of tectonic plates beneath the Earth's surface. As the plates shift and pull apart, magma rises up to the surface, resulting in volcanic activity along the rift. The East African Rift Valley is a classic example of this geologic process, with a chain of volcanoes forming along its length.
Explosive volcanoes are most common at subduction zones.
The continental rift along which parts of the African continent are beginning to slowly separate
Rift Volcanoes.
The Basin and Range Province is an example of a rift zone.