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VOLCANOES!
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Factors Affecting Eruptions
Magma temperature Hotter flows easier… Magma viscosity – determined by temp and composition. High silica = high viscosity (thickness) High viscosity = violent eruptions… Dissolved gases More gasses means more violent eruptions…
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Volcanic Materials- Lava
3 TYPES OF LAVA FLOWS Aa- rough and jagged 2) Pahoehoe - wrinkly and ropey texture 3) Pillow - forms underwater at boundaries
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Aa Pahoehoe Pillow
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Volcanic Materials- Gases
Water Vapor, Carbon Dioxide, Nitrogen, Sulfur Dioxide, and Chlorine Kilauea Volcano, Hawai`i From emitted 1,000-2,000 metric tons of SO2 every day!
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Volcanic Materials Pyroclastic Materials = Ejected fragments
Ash – fine material Cinders and lapilli = medium/pebble sized Bombs and blocks (big stuff) block = hard, bombs = lava
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Ash Bombs & Blocks Cinders
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Volcanic Terms Crater – steep walled depression at top
Caldera – large depression in a volcano due to collapse of volcano
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Volcanic Terms Conduit – pipe connecting magma chamber to the surface Vent – top of the conduit
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Volcanic Terms Lava plateau – raised flat area of lava
Volcanic neck – remnant of eroded volcano
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Columbia Lava Plateau- covers parts of Washington, Oregon, and Idaho
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Composite Cinder Cone Shield
Types of Volcanoes Composite Cinder Cone Shield
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Shield Volcanoes broad base with gently sloping sides
Huge in size, mild eruptions, mostly flows, ex: Hawaii Mauna Kea, Hawaii
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Cinder Cone Narrow base and steep sides
-Small, violent for size, pyroclastic eruptions, ex: Mt. Paricutin, Sunset crater in AZ
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Composite Cone Medium base and moderately sloped size (volcano looking) Medium size, violent eruptions, andesitic lava, combination of flows and pyroclastic eruptions, ex: Mt. St. Helens
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Mt. St. Helens Before & After
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Igneous Activity Plutons (intrusive igneous bodies)
Classified by shape, size, and relationship to surrounding rock layers Sill – horizontal and between rock layers Dike – vertical and cut across rock layers Laccolith – dome/mushroom shaped plutons Batholith – more than 100 km2 of exposed rock Stock – less than 100 km2 of exposed rock
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Volcano Dangers Pyroclastic flows – hot gases, glowing ash, and larger rock fragments Very hot (like cook your butt hot) Can attain 200 km/hr Lahars – mudflow formed from volcanic ash and water (melted snow or rain) Eruptions – you’re there one minute and gone the next…can you say vaporized
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Origin of Magma Read pages 291 – 292 The role of heat
The role of pressure The role of water
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Volcano Locations Convergent plates Divergent plates
Subducting plate melts and magma rises Japan and Mt St Helens Divergent plates Plate diverge and magma rises through the rift Mid-ocean ridge Iceland East African Rift Intraplate (hot spots) Mantle plume rises towards the surface Hawaii and Yellowstone
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