A geographical subduction zone is a fault line where two plates move towards each other. The more dense plate gets pushed under the other; this is called subduction.
Moun Cleveland formed as a result of a subduction zone, but is not a subduction zone in and of itself. A subduction zone is a feature that forms volcanoes, not a kind of volcano.
subduction zone
A continent to continent convergent boundary does not have a subduction zone.
subduction zone
no
Earthquakes and volcanic eruptions do not usually happen away from a subduction zone. Subduction zones are known for their intense seismic activity and volcanic activity due to the movement of tectonic plates.
C. subduction zone
Spreading center earthquakes are always shallow, subduction zone earthquakes can be very deep.Spreading center earthquakes are typically of lower magnitude than subduction zone earthquakes.
A subduction zone is a tectonic boundary where one tectonic plate is being forced beneath another. So, in a subduction zone, the process of subduction is taking place, rather than being created or destroyed.
It is called a subduction zone.
A subduction zone is a region where oceanic plates sink down into the asthenosphere beneath another plate, such as at convergent plate boundaries. This process can lead to the formation of deep oceanic trenches, volcanic arcs, and earthquakes.
The subducted plate descends into the mantle at subduction zone