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Published byPosy Norman Modified over 9 years ago
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VOLCANISM 80% of the earths crust is composed of volcanic rocks Volcanism: the process by which magma from the interior of the earth rises through the crust, emerges onto the surface as lava, and cools into volcanic rock
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Anatomy of a volcano
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Types of lava (based on silica content) felsic, andesitic, mafic Types of Volcanic Deposits Basaltic: Flood Basalts Different Layers of Basalt
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Types of Volcanic Deposits (cont) Basaltic:Pahoehoe, Aa, Pillow lava Rhyolitic Andesitic
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Textures glassy, vesicular (related to cooling rates and gas content)
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Explosive vs. Gentle Eruptions
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Pyroclastic Deposits Air fall or tephra Ejecta: ash, tuffs and breccias, bombs Explosive vs. Gentle Eruptions
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Pyroclastic Flows Surge – directed blast of hot material nuée ardante (glowing cloud) Mudflow lahar
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Landforms and Eruptive Styles 1.Shield Volcanoes i.gentle eruptions consisting of basaltic lavas ii.low silica and low viscosity iii.fissure eruptions and flood basalts iv.example: Mauna Loa
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Volcanic Domes i.explosive eruptions consisting of felsic volcanism ii.high silica and high viscosity iii.ash flows iv.example: Mount St. Helens (1980)
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Cinder-Cones Volcanoes i.pyroclastic eruptions
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Composite Volcanoes (stratovolcano) i.alternating lava and pyroclastic eruptions
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Craters i. central depression at the summit of most volcanoes Calderas (collapsed craters)
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Other Volcanic Features 1.diatremes 2.fumaroles, hot springs, geysers
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Plate Tectonics and Volcanism
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Plate Tectonics and Volcanism (cont) 1.Spreading zone volcanism: basalts 2.Convergence zone volcanism: Ring of Fire i.OC-OC convergence: basalts and occasional andesites ii.OC-CC convergence: ash and rhyolite 3.Interplate volcanism 4.Hot Spot Activity
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Benefits of Volcanism atmosphere, oceans, land masses, soil, geothermal uses
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