A volcanic island arc is a chain of islands formed by the subduction of one tectonic plate beneath another, leading to volcanic activity. These arcs are typically found along convergent plate boundaries, where an oceanic plate subducts beneath either another oceanic plate or a continental plate, resulting in the formation of a series of volcanoes that emerge above sea level as islands. The geological processes involved in creating volcanic island arcs also influence surrounding ocean basins and seafloor features.
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