Composite volcanoes, also known as stratovolcanoes, are characterized by their steep, conical shapes and are formed from multiple layers of lava flow, volcanic ash, and other volcanic materials. Their formation involves several key processes:
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Subduction Zones: Most composite volcanoes are located at convergent plate boundaries, where one tectonic plate is forced beneath another in a process called subduction. This can lead to the melting of the subducted plate and the generation of magma.
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Magma Generation: As the subducted plate descends into the mantle, it heats up and releases fluids that lower the melting point of the surrounding rocks. This process creates magma, which is less dense than the surrounding rock and thus rises towards the surface.
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Eruption Style: Composite volcanoes typically produce explosive eruptions due to the high viscosity of their magma, which is often andesitic in composition. The viscosity prevents gas from escaping easily, leading to pressure buildup before explosive release. These eruptions can eject ash, pumice, and volcanic rocks into the atmosphere.
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Layering of Materials: After an explosive eruption, the volcano may go through periods of less explosive activity where it emits more fluid lava flows. This combination of explosive and effusive eruptions contributes to the layering characteristic of composite volcanoes:
- Layers of Ash and Tephra: Explosive eruptions deposit fine ash and larger volcanic rocks, creating layers of tephra around the volcano.
- Lava Flows: The subsequent effusive eruptions produce lava flows that can travel significant distances, adding to the structure of the volcano.
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Continuous Growth: Over time, the repeated cycles of explosive and effusive activity lead to the accumulation of materials, resulting in the characteristic steep-sided profile of composite volcanoes. This growth can occur over thousands to millions of years, resulting in a significant mountain structure.
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Volcanic Activity: Composite volcanoes are often associated with a variety of volcanic features, including lava domes, craters, and volcanic ash deposits. They are also susceptible to hazards such as pyroclastic flows, lahars, and ashfall, which can pose risks to nearby populations.
Some well-known examples of composite volcanoes include Mount St. Helens, Mount Fuji, and Mount Vesuvius.