Basalt pushed into the crust by subduction will likely become metamorphosed into a rock called eclogite due to the high pressure and temperature conditions experienced in the subduction zone.
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.
A continent to continent convergent boundary does not have a subduction zone.
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.
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.
Basalt pushed into the crust by subduction will likely become metamorphosed into a rock called eclogite due to the high pressure and temperature conditions experienced in the subduction zone.
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.
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.
C. subduction zone
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.