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Chapter 9 Section 1 VOLCANIC ERUPTIONS
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A vent or fissure in the Earth’s surface through which magma and gases are expelled VOLCANO
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Nonexplosive Most common Produce relatively calm flows of lave Can be huge amounts Explosive Much rarer Effects can be incredibly destructive Ash from explosions can circle in upper atmosphere for years causing climate changes ERUPTIONS
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Vents- and opening at the surface of the Earth through which volcanic material passes Magma chamber- the body of molten rock that feeds a volcano Lava- liquid magma flows from a volcano’s vents FEATURES OF A VOLCANO
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“Aa”- pours out quickly forms brittle crust with jagged pieces “ Pahoehoe”- flows slowly “ way from a candle” glassy surface, rounded wrinkles “Pillow” – underwater, rounded lumps shaped like pillows “Blocky” – Cool and stiff does not travel far from vent, oozes, forms jumbled heaps of sharp-edged chunks 4 TYPES OF LAVA
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If water content is high explosive eruptions are likely If rich with silica explosive eruptions are likely Magma that contains less silica has a more fluid, runnier consistency- gases can escape more easily explosions less likely to occur HOW MAGMA EFFECTS ERUPTIONS
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Pyroclastic Material Volcanic blocks- largest pieces of pyroclastic material, solid rock Volcanic bombs- are large blobs of magma that harden in the air Lapilli- “little stones” pebblelike bits if magma that harden before they hit the ground Volcanic ash- forms when the gases in stiff magma expand rapidly and the walls of the gas bubbles explode into tiny, glasslike slivers- makes up most of pyroclastic material
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