Convergent boundaries can form between two oceanic plates, between one oceanic plate and one continental plate, or between two continental plates.
Convergent (destructive) margins.
A subduction zone can be a result of a convergent plate boundary, but the terms are not synonymous. If the two convergent plates are continental, neither of them will subduct.
A continent to continent convergent boundary does not have a subduction zone.
In plate tectonics, when two tectonic plates move toward each other, it results in the formation of what is called a convergent plate boundary. The two plates are said to converge. One plate may be more dense than the other, and with the two plates pushing against each other, the plate that is more dense will "slide under" the other plate. The plate sliding under is said to subduct the other plate, and this creates what is called a subduction zone. Not all convergent plate boundaries have subduction zones, but all subduction zones are formed at convergent plate boundaries.
The subducted plate descends into the mantle at subduction zone
Mount St. Helens was formed along a subduction zone, where the Juan de Fuca Plate plate dives under (subducts) the North American plate.
A subduction zone is where one plate is being subducted ( pulled down) under another plate, No it is not a plate boundary but it is were it happens. hope this helps
Convergent Boundaries
Convergent Boundaries
It is called a subduction zone.
Yes. They occur at convergent plate boundaries (especially oceanic-continental and occasionally at oceanic-oceanic convergent boundaries).
A subduction zone can be a result of a convergent plate boundary, but the terms are not synonymous. If the two convergent plates are continental, neither of them will subduct.
A continent to continent convergent boundary does not have a subduction zone.
It is the subduction zone between the Cocos and North American plates.
In plate tectonics, when two tectonic plates move toward each other, it results in the formation of what is called a convergent plate boundary. The two plates are said to converge. One plate may be more dense than the other, and with the two plates pushing against each other, the plate that is more dense will "slide under" the other plate. The plate sliding under is said to subduct the other plate, and this creates what is called a subduction zone. Not all convergent plate boundaries have subduction zones, but all subduction zones are formed at convergent plate boundaries.
The subducted plate descends into the mantle at subduction zone
The subducted plate descends into the mantle at subduction zone
Volcanic islands typically form near subduction zone, but they can also form at hot spots, which are not associated with plate boundaries.