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oceanic island

geology
Also known as: volcanic island

Quick Summary

Oceanic islands are landmasses that rise from the seafloor without any underlying continental rock, typically formed by volcanic activity. These islands are often found along the axes of oceanic ridges, where tectonic plates move apart and magma wells up from the mantle, creating new ocean floor.12

Some oceanic islands emerge above sea level, forming volcanic islands. Examples include Iceland, the Azores, and islands in the Hawaiian chain, which are thought to form over "hot spots" in the Earth's mantle. Another type of volcanic island formation occurs in island arcs, which are curved chains of islands associated with volcanic and seismic activity, often found where tectonic plates converge. These arcs can consist of explosive volcanoes or nonvolcanic islands, and are frequently accompanied by deep-sea trenches.123

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