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Mount St. Helens, 1980 eruption
VOLCANISM Mount St. Helens, 1980 eruption
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Where are volcanoes located?
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Volcanoes are located over divergent plate boundaries (mid-oceanic ridges)
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Laki fissure, Iceland
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Volcanoes are located over convergent plate boundaries (subduction zones)
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Mount Rainier, Tacoma, Washington
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Volcanoes are located over Hot spots
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What are the products of volcanism?
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Welded tuff (ash & flow deposits)
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Vesicular Basalt
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Pyroclastic eruption at Arenal Volcano, Costa Rica
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Volcanic Bombs
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Pyroclastic flow at Mount Unzen
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Volcanic Breccia
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WHY DO DIFFERENT VOLCANOES HAVE DIFFERENT SHAPES?
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Gentle-slopes (Shield Volcano)
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Non-explosive eruptions Basaltic flows Low-viscosity Lava
Gentle-slopes (Shield Volcano) Non-explosive eruptions Basaltic flows Low-viscosity Lava Low SiO2 content Mafic composition
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steep-slopes (Cinder-cone Volcano)
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steep-slopes (Cinder-cone Volcano)
Pyroclastic material High SiO2 content More Felsic composition
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steep-slopes (Composite Volcano)
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steep-slopes (Composite Volcano)
Alternating layers of Basaltic flows and pyroclastic material Mafic-felsic composition
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Volcanic domes
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Lava accumulates over the vent
Volcanic domes Felsic lava Very high viscosity Lava accumulates over the vent
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Evolution of Crater Lake Caldera
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Mount St. Helens (Before eruption)
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Mount St. Helens (During eruption)
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Mount St. Helens (After eruption)
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Mount St. Helens (Before eruption)
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Hot Spots and Plate movement
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Volcanic Hazards
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Pyroclastic Flows are the most dangerous
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