Composite and shield volcanoes are key in forming large volcanic mountains through specific characteristics and eruption styles.
Composite volcanoes commonly develop to form large volcanic mountains. They are steep-sided, symmetrical cones built of multiple layers of viscous lava and ash. Examples include Mt. Fuji in Japan and Mt. Ranier in Washington.
Shield volcanoes are huge, gently sloping volcanoes characterized by broad, low-angle flanks. Basaltic magma and effusive eruption styles contribute to their formation.
Volcanic mountains are constructional mountains formed when volcanoes emit lava and solid particles, building up to create hills or mountains.
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