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  1. Island arcs are long chains of active volcanoes with intense seismic activity found along convergent tectonic plate boundaries. Most island arcs originate on oceanic crust and have resulted from the descent of the lithosphere into the mantle along the subduction zone. They are the principal way by which continental growth is achieved.
    en.wikipedia.org/wiki/Island_arc
    One type of volcanic oceanic island is found in a volcanic island arc. These islands arise from volcanoes where the subduction of one plate under another is occurring. Examples are the Aleutian Islands, the Mariana Islands, and most of Tonga in the Pacific Ocean.
    en.wikipedia.org/wiki/Island
    intraoceanic arcs (primitive arcs) form when oceanic crust subducts beneath other oceanic crust on an adjacent plate, creating a volcanic island arc.
    en.wikipedia.org/wiki/Volcanic_arc
     
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    WEBJun 12, 2024 · If both plates are oceanic, as in the western Pacific Ocean, the volcanoes form a curved line of islands, known as an island arc, that is parallel to the trench, as in the case of the Mariana Islands and the …

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    WEBDec 7, 2017 · An island arc is a chain of volcanoes parallel to the boundary between two converging tectonic plates. Learn how subduction, plate tectonics and convergent boundaries create island arcs and see …

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