Tectonic Plates moving away from each other.
if a rift zone stops speeding, the volcano will become extinct:)
The Basin and Range Province is an example of a rift zone.
The rift valley was formed when the continents divided it split open a large area in Africa and formed The Great Rift Valley.
Rift zones are formed when tectonic plates move apart, creating a fracture in the Earth's crust. This movement can result in volcanic activity and the release of magma, leading to the formation of new crust. Over time, the rift zone widens as the tectonic plates continue to pull apart, eventually forming a new oceanic ridge.
A rift valley is a trough-like zone along the peak of a mid-ocean ridge. It is formed as tectonic plates move apart, allowing magma to rise up and create new oceanic crust. The rift valley is typically deeper than the surrounding seafloor and can be several kilometers wide.
the rifts didn't developin exactly the same places where Pangaea was first sutured together. for example, the rift that formed the Atlantic ocean was located to the east of the present Appalachian mountains.
Ol Doinyo Lengai is not associated with a subduction zone. It is associated with the East African Rift, which is a continental rift.
The thin crust of a rift zone causes melting in the upper mantle, resulting in volcanic activity.
The deepest canyon on Venus is called Devana Chasma. It is classified as a rift zone formed by tectonic processes.
What you call a pull apart rift zone is what is called a divergent boundary. Most divergent zones are located under water and are a zone where new oceanic crust is born. One location where a divergent zone can be seen on land can be found in Iceland.
the answer is a rift zone
A pull-apart rift zone is associated with a transform plate boundary where two plates slide past each other horizontally. This type of boundary can lead to the formation of a linear valley or depression as the plates move in opposite directions. An example of a pull-apart rift zone is the East African Rift.