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A subduction volcano forms at a convergent plate boundary, where one tectonic plate slides beneath another into the Earth's mantle. This process, known as subduction, often occurs when an oceanic plate is forced under a continental plate or a younger oceanic plate. As the denser plate descends, it carries water and carbon dioxide into the mantle, which can lower the melting point of the surrounding rock, generating magma. This magma rises to the surface, erupting to form volcanoes, typically explosive stratovolcanoes. These volcanoes are a significant feature of the Ring of Fire, a zone of intense seismic and volcanic activity encircling the Pacific Ocean.12

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