South America is a notable one, where the Pacific Plate subducts below the Andes, uplifting the land, and creating the long volcanic chain.
This is known as a subduction zone.
A subduction zone and a collision zone are the same place, a collision just happens earlier, when the crusts of the two plates are interacting. Later, when the crust of one plate is being forced under the crust of another plate into the mantle, it becomes a subduction zone.
A subduction zone
Most notable is the so-called 'Ring of Fire', an area encircling the Pacific Ocean where oceanic crustal plates are subducting under continental plates and less dense oceanic plates.
A subduction zone is an area on Earth where two tectonic plates move towards one another and subduction occurs. Subduction is the process that takes place at convergent boundaries by which one tectonic plate moves under another tectonic plate, sinking into the Earth's crust, as the plates converge
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.
anything can happen at a subduction zone
This is known as a subduction zone.
A subduction zone and a collision zone are the same place, a collision just happens earlier, when the crusts of the two plates are interacting. Later, when the crust of one plate is being forced under the crust of another plate into the mantle, it becomes a subduction zone.
A subduction zone
Subduction is part of the geological process of plate tectonics. A subduction zone is a place where the oceanic plate is sinking back in to the mantle (usually at the edge of a continental plate.
Subduction zone
A continent to continent convergent boundary does not have a subduction zone.
A subduction zone is a place that occurs between two tectonic plates. It is the site where these tectonic plates have collided.
This is called a subduction zone.
The subduction zone.
Most notable is the so-called 'Ring of Fire', an area encircling the Pacific Ocean where oceanic crustal plates are subducting under continental plates and less dense oceanic plates.