Magma that is created by ocean-continent convergence forms either island arcs or belts of igneous activity on the edges of continents.

Name: Magma that is created by ocean-continent convergence forms either island arcs or belts of igneous activity on the edges of continents.
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This statement is true. Magma generated by oceanic plates being subducted under continental plates can form island arcs or belts of igneous activity at the edges of continents. This process is known as subduction zone volcanism.

Magma That Is Created by Ocean-Continent Convergence Forms Either Island