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The percent of silicon di oxide in magma |
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Slow moving, high SiO2, more difficult for gas to escape, more explosive |
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Low SiO2, more fluid, easy for gas to escape, less explosive |
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Eruption column formed from Height From what type of volcanoes |
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Plinian eruption Up to 45 KM Subduction zone volcanoes |
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Section of the oceanic crust exposed above sea level by tectonic forces |
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Two types of basalt flows |
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Flow where lava cools to form smooth, ropy texture |
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Lava cools to form rough, blocky texture |
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Texture of basalt when eruption is under water. Forms top layer of ocean crust |
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Hot rock fragments and gasses, dry flow |
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Pyroclastic Flow occur in |
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Source of prosylactic flow |
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Collapse of eruption column |
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Rapidly flowing mixture of pyroclasts and water, originate from the melting of ice, rainfall or the breakout of a lake |
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Viscous lava solidifies in the caldera (or crater) of a composite volcano. |
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Tall Eruption Column, go into stratosphere |
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Large volume of basaltic lava erupting on surface |
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Alternating layers of pyroclasts and lava flows. (Subduction zone volcanoes- Ring of Fire), Explosive Eruptions |
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Major gasses emitted from volcanoes and percentage |
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Water vapor 50 percent CO2 Sulfer dioxide |
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3 tectonic settings w/ volcanic activity Most common lava types erupting at each |
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Divergent plate boundaries (both types) Subduction zones (sheild and composite) Hot spots: source mantle plumes |
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Most active volcano on Hawaii and in the world |
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Mt. St. Helens and Mt. Rainer location and what is hazard |
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Cascade arc Lahars will be serious hazards |
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Indonesia's most active volcano in erupted in October 2010 |
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Part of indonesian volcanic arc, largest eruption in history Global cooling and year without summer, blocked sun |
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