8.2 volcanic eruptions where the rock cycle begins
TRANSCRIPT
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8.2 VOLCANIC ERUPTIONS
Where the rock cycle begins
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Learning Targets
1. Compare the types of volcanic eruptions
2. Describe a method for predicting volcanic eruptions
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Volcanic Eruption
1. Magma collects in magma chamber2. Hot magma expands creates
pressure3.Vent: crack in the earth’s surface4. Magma moving through vent =
eruption
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How do volcanoes erupt?
1. Types of eruptions:a)Explosiveb) Non-explosive; effusive
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Explosive Eruptions
1. Can be 1000 times more powerful than atomic bomb
2. Pressure builds as gases in magma expand
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Explosive Eruptions
1. Explosion shoots ash and gas high in the air
2. Heavy debris falls; light debris may float around for years
3. Why is ash and gas in the air important?
a) Blocks sunlight, produces poisonous gas, mixes with water to form acid, global climate change
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Explosive Eruptions
1. Some magma crystallizes in the air
2. Called pyroclastic material: ash, lapilli, bomb
3. Can come down miles from the volcano
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Non-explosive eruptions
1. Another name for non-explosive eruptions
a)Effusive eruptions
2. Different mix of minerals in magma
3.No gas build up4. Less dangerous but lava flows
are consistent and unstoppable
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Magma Formation
1. What causes magma to forma) High heat
i. Hot Spots; effusive
b) Decreased pressurei. Divergent boundaries; effusive
c) Increased water contenti. Subduction zones; explosive
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Lava - Viscosity
1. Viscosity: Resistance to flowa) Honey, ketchup, water
2. High viscositya) High silica contentb)Explosive eruptions pressure
3. Low viscositya) Low silica contentb)Effusive eruptions no
pressure
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Lava formations
1.Explosive lava Pyroclastic material
a) Pyroclast – lava solidifies in the atmosphere
b)Pyroclastic flow – fast moving current of superheated gas and rock
i. Can move hundreds of miles per hour
2.Effusive lavaa) A’a: jagged, gravelly textureb) Pahoehoe: smooth, even lava flowc) Pillow lava: cools underwater forms rounded
lobes
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Predicting Eruptions
1.History of eruptiona)Active, dormant, extinct
2.Earthquakesa)Pressure of magma causes
earthquakes
3.Slope deformationa) Plastic deformation due to pressure
4.Gas emissionsa) Gas escapes before magma
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5. Remote Monitoring