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Steep-sided volcanoes found along convergent boundaries are typically stratovolcanoes, also known as composite volcanoes. These volcanoes form where an oceanic plate subducts beneath a continental plate, leading to explosive eruptions due to the buildup of magma. Examples include Mount St. Helens in the United States and Mount Fuji in Japan. Their steep profiles result from alternating layers of lava flow, ash, and volcanic rock.

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