Convergent Boundaries
Convergent Boundaries
Subduction occurs when an oceanic plate slides under a continental plate. When the oceanic plate does this, it descends into the mantle, and the place where the subduction begins forms a deep-ocean trench.
It is called subduction and only occurs in oceanic to oceanic or oceanic to continental plate collisions.
a subduction zone
It's called destructive plate margin/boundary, or convergent plate margin though this term applies to all plate margins where two plates are moving towards each other (such as continental + continental or oceanic + oceanic).
subduction boundary!!!
a convergent boundary. The oceanic plate is then subducted under the continental plate because it is denser. This subduction creates earthquakes and volcanoes
A subduction zone at a convergent plate boundary. Undersea trenches are formed where the oceanic plate subducts, and volcanism and earthquakes may result from the partial melting and downward movement of the subducting crust.
C. subduction zone
Oceanic crust sinking under a plate with continental crust
An oceanic plate can descend beneath another oceanic plate - Japan, Indonesia, and the Aleutian Islands are examples of this type of subduction. Alternately, an oceanic plate can descend beneath a continental plate - South America, Central America, and the Cascade Volcanoes are an example of this type of subduction.
In a subduction zone an oceanic plate slides under a continental plate or another oceanic plate. The subduction plate introduces water into the mantle, lowering melting temperatures and generating magma. This causes volcanoes, usually stratovolcanoes, to form on the overriding plate. If the overriding plate is continental a mountain range may develop.