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Volcano Types and Formation
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Shield Volcano Typically occur at divergent boundaries and hot spots.
Molten rock pushes its way up to the surface as the plates spread. Oceanic crust passes over a hot spot in the mantle. Very large in scale. Erupt in gentle lava flows ( mainly basaltic lava)
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Formation over a hot spot.
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Haleakala, HI
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Mauna Loa, HI
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Cinder Cone Usually Small in scale.
Formed from cinders piling up on itself. Typically felsic lava.
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Pyroclastic Layers
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Pyroclasts Rock fragments from a volcanic eruption. Smallest = Ash
Medium = Cinder Largest = Bombs Which is the most deadly?
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Composite Volcanoes Contain granite lavas that are very viscous.
These lavas can trap gas and act as “plugs” in the vent of a volcano. Pressure builds up and can cause explosive eruptions. Formed from alternating layers of lava flows and pyroclastic eruptions. Mixture of felsic and basaltic lava. Continent-Oceanic convergent boundaries
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Dissected Stratovolcano
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Mt. Hood, Washington
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Mt. Egmont, New Zealand
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Calderas Formed from the largest and most explosive volcanic eruptions. Extremely large volumes of magma are removed from below the ground. The empty chamber then collapses.
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Crater Lake, Oregon
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Yellowstone National Park, WY
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