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Published byEsmond Chandler Modified over 8 years ago
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volcanism:any activity that includes the movement of magma toward the surface of the Earth volcano: place where magma reaches the surface
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magma: liquid, molten rock underground lava: magma that reaches the surface lost gas, gained rock
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MID-OCEAN RIDGE: occurs where plates are moving apart lava flows out smoothly and fluidly from cracks
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SUBDUCTION ZONE: occurs at subduction boundaries usually explosive and erupted material is mostly lava
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HOT SPOTS: areas of volcanic activity in the middle of a lithospheric plates
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Hawaiian Islands are an example
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two types of lava: felsic: much silica (Rhyolitic), light-colored, slow moving (viscous), continental crust
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mafic: low silica (basaltic), dark-colored, fast moving (least viscous), oceanic crust
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Pahoehoe (puh- HOEEE-hoeee): thin mafic lava. –usually hardens with wrinkled surface –means “ropey” in Hawaiian Pahoehoe Lava
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Aa (AH-ah): sharp block shapes of hardened mafic lava. –caused by rapid cooling on surface of lava –breaks into jagged chunks Aa Lava
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PahoehoeLava
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Pahoehoe
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Aa
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Pillow lava from Hawaii
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many magmas contain dissolved gases that are given off water vapor, carbon dioxide (CO 2 ), sulfur (S) magmas with more gases have more explosive eruptions
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tephra:solid fragments ejected from a volcano ash (<2mm) bombs lapilli (<64mm) blocks Sometimes called pyroclastic material
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lapilli
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bombs
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blocks
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Vent: opening from which lava flows Crater: funnel-shaped pit or depression at top of volcano Caldera:craters whose walls have collapsed
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composed of quiet lava flows form gently sloping, dome- shaped mountain basaltic (mafic) magma
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largest = Mauna Loa in Hawaii
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Made mostly of tephra and other rock particles Formed from explosive eruptions Not very high, narrow base, steep sides Rhyolitic (felsic) magma
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built up of alternating layers of rock & lava explosive eruptions at first with tephra, then quiet with lava forms large, cone-shaped mountains made of rhyolitic & basaltic magma
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Mount Fuji
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