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An island arc forms.
continental crust
New oceanic lithosphere forms as a result of continental drift.
Just as new oceanic crust forms at mid-ocean ridges, old oceanic crust is destroyed at subduction zones.
Basalt is found by comparing oceanic plates beneath the ocean floor.
a subduction zone
C. subduction zone
An island arc forms.
continental crust
An island arc forms when two tectonic plates converge and one oceanic plate is forced beneath the other in a process known as subduction. The subducted plate melts, creating magma that rises to the surface and forms a volcanic arc of islands. This process is typically associated with ocean-ocean plate boundaries.
At some convergent boundaries, an oceanic plate collides with acontinental plate. Oceanic crust tends to be denser and thinner thancontinentalcrust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thicker continental crust. This forms what is called a subduction zone.
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.
New oceanic lithosphere forms as a result of continental drift.
Just as new oceanic crust forms at mid-ocean ridges, old oceanic crust is destroyed at subduction zones.
Basalt is found by comparing oceanic plates beneath the ocean floor.
basalt forms in oceanic crust granite forms in continental
mid ocean ridge