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Volcanic mountains, from gentle shield volcanoes to towering stratovolcanoes and underwater submarine peaks, showcase Earth's dynamic geological processes and fiery origins
Characterized by broad, gentle slopes, these volcanoes form from low-viscosity lava that can travel great distances. Notable examples include Mauna Loa
These volcanoes have steep, conical profiles and are built from alternating layers of lava flows, volcanic ash, and other volcanic debris. Examples include Mount Fuji in Japan
Formed from pyroclastic fragments, these small, steep-sided volcanoes result from relatively short-lived explosive eruptions. Paricutin in Mexico is a well-known example
Created by slow eruptions of viscous lava, these domes form rounded, steep-sided mounds. The lava is too thick to flow far, so it piles up near the vent
Large volcanic craters, often formed by collapse of a volcano after a massive eruption. These craters can fill with water to form lakes. The Yellowstone Caldera is a famous example
These structures are composed of multiple volcanic centers, such as cones and domes, often in various stages of activity. They result from changes in eruption locations over time
Located on the ocean floor, these volcanoes can create new islands if they erupt enough material above sea level. They primarily produce pillow lava formations