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Volcanic Eruptions
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Mafic Lava Dark colored Rich in magnesium and iron
Formed from oceanic crust Cools rapidly
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Felsic Lava Light colored Rich in silica Formed from continental crust
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Eruptions Composition of lava determines the force of the eruption
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Oceanic Eruptions Erupt on the ocean floor and oceanic islands
Mafic lava Very hot Very thin (watery) Flows easily
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Continental Eruptions
Erupt on the land Felsic lava Cooler Thicker Contains large amounts of gases Carbon dioxide and water vapor Explosive
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Mafic Lava Pyroclastic material (tephra)-rock fragments ejected from volcanoes Volcanic ash- less than 2 mm Volcanic dust- less than .25 mm Both can travel around the Earth in the atmosphere
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Volcanic Cones Piles of volcanic material around the vent
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Volcanic cones Shield cones Cover wide areas Broad at the base
Gentle slope Quiet eruptions Example Hawaiian Islands
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Shield cones
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Volcanic cones Cinder cones Explosive eruptions Very steep slopes
Rarely more than a few hundred meters high
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Cinder cones
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Volcanic cones Composite cones Develop into high volcanic mountains
Alternating types of eruptions Examples: Mount Fuji, Mount Hood, Mount St. Helens
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Composite cones
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Crater Funnel shaped pit at the top of a volcanic vent
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Caldera Large basin shaped depression caused by an explosive eruption
Magma chamber below a vent, causing the volcanic cone to collapse
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Predicting Volcanoes Earthquakes
Temperature changes in rock around vent Bulging of the surface of the volcano Change in gases given off
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