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Download Geologic Setting Hot Spots (and Mid
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VOLCANIC PROCESSES SUMMARY TABLE Geologic Setting Hot Spots (and Mid-Ocean Ridges) Subduction Zones Cause of Melting Decompression Melting causes partial melting of mantle rock. Water Fluxing causes partial melting of mantle rock (produces mafic magma) Melting of continental crust by hot mafic magma. Magma/Lava Composition Mafic (basaltic). Consistent composition. Intermediate is most common, but sometimes felsic and occasionally mafic. The composition of the lava erupted is variable primarily because the amounts of assimilation and differentiation that occur to magma on its way to the surface vary (see the volcanic processes handout). Gas content of magma/lava Generally relatively low in dissolved gasses. Generally relatively high in dissolved gas. Viscosity of magma/lava Generally low viscosity and runny. Generally relatively high viscosity; often only capable of very slow flow. Style of Volcanism Lava flows, fountaining if there is enough dissolved gas. Often very explosive, but can produce lava flows as well. The combination of gas-rich very viscous magma/lava can cause catastrophically explosive eruptions. Types of Volcanoes Formed Shield volcanoes (not at mid-ocean ridges); cinder cones. Note that basaltic volcanism can occur at locations other than hot spots and mid-ocean ridges, and that shield volcanoes can form wherever there is a lot of basaltic volcanism. Composite or Stratovolcano. Example Volcanoes Mauna Loa, Newberry Volcano Cascade volcanoes in northwest U.S., including Mt. St. Helens, Mt. Rainier, and Mt. Hood; other famous examples include Mt. Pinatubo (Phillipines), Mt. Fuji (Japan), and Mt. Vesuvius (Italy).