Volcanic arcs and oceanic trenches commonly form at subduction zones.
Subduction Zone.
About 150km from a subduction zone.
They are less dense that is why there is no subduction zone
In a subduction zone the crust is forced inot the mantle where it is eventually melted and destroyed
No it is really 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.
a subduction zone forms
mountain or volcanoe
C. subduction zone
The Andes mountain range in South America is an example of a mountain range that forms near a subduction zone. The subduction of the Nazca Plate beneath the South American Plate has contributed to the uplift and formation of the Andes.
The Andes mountain range forms near a subduction zone where the Nazca Plate is subducting beneath the South American Plate. This subduction process has resulted in the uplift of the Andes mountains over millions of years.
When two plates move together (at least one must be oceanic crust), one will sink beneath the other. The result is that a subduction zone forms between the two plates at the location where they meet.
A subduction zone forms when one oceanic plate is forced beneath another plate. This process can lead to the formation of volcanic arcs, deep ocean trenches, and seismic activity.
Convergent Boundaries
subduction zone
Usually either a mountain range, or a subduction zone.
A continent to continent convergent boundary does not have a subduction zone.