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When Volcanoes Erupt PG. 107
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Volcano a break/hole on the crust of Earth that emits lava, ash, and gases. (usually forms a mountain)
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What’s inside a volcano?
Crater The central funnel shaped vent at the top of a volcano Vent—an opening at the surface of the Earth through which volcanic material passes Magma Chamber—the body of molten rock that feeds a volcano Magma Chamber
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What are non- explosive eruptions?
Volcanoes that erupt only lava and gas The most common type of eruption
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What erupts from a volcano?
1. Lava-- 4 types Pahoehoe Low viscosity- flows quickly, smooth glassy surface A’a—high viscosity- flows slowly, brittle jagged surface
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Pillow lava—lava that erupts under water
Blocky lava—sharp edged chunks of stiff lava
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What are explosive eruptions?
Clouds of hot rock, ash and gas rapidly shoot out from the volcano Millions of tons blast out in a few seconds
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2. Pyroclastic material 4 types of material
Bombs—large blobs of magma that harden when they fly through the air Blocks—largest pieces of solid rock blown away from the volcano
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4. Volcanic ash– magma explodes into tiny glass like slivers
3. Lapilli—little stones of magma that harden before they hit the ground
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What are pyroclastic flows?
Enormous amounts of hot ash, dust and gas are ejected from a volcano Races downhill at more than 200 km / hr Temperatures can exceed 700 degrees C
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What are the effects of volcanic eruptions?
Climate can be changed as ash and gas spread throughout the atmosphere Eruptions can affect the whole Earth with lower temperatures
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Other effects… Pyroclastic materials (ash and rock)
can travel at high speeds and can be deadly Lava can be very destructive—it’s very hard to stop
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Mt. Vesuvius and Pompeii
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Mt. Vesuvius and Pompeii
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3 types What are other types of Volcanic Landforms?
1. Lava Lakes- large amounts of molten lava contained in a depression A
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2. Calderas A semicircular depression that forms when the magma chamber partly empties and causes the ground above to sink Many times larger than a crater
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3. Lava Plateaus A wide flat area caused by repeated nonexplosive eruptions of lava that spread over a large area
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