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EARTH SCIENCE Mrs. Baker cjcb2015
VOLCANOES EARTH SCIENCE Mrs. Baker cjcb2015
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Volcanoes An opening in the Earth’s crust that erupts gases, ash, and lava (pyroclastic material). There are more than 600 active volcanoes on Earth! Mt. Kilauea in Hawaii is the most active volcano!
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Vocabulary
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Parts of a Volcano A Magma Reservoir B Flank C Conduit D Crater
E Solidified Lava F Dike G Ash H Vent I Sill INTERACTIVE WEBSITES (GO TO “LAUNCH”): (images) (LOTS of information)
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Viscosity The ability of a substance to resist flowing.
Materials that flow quickly have a low viscosity. Examples: water, basaltic magma Materials that flow slowly have a high viscosity. Examples: syrup, Rhyolitic magma
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Types of Magma Temperature, pressure, and amount of water affect the formation of magma.
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Explosiveness of a Volcano
The explosiveness of a volcano depends on the viscosity of the magma within it. High in silica, low in water vapor = High viscosity. The magma will clog the main vent, build up pressure and result in an explosion.
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Life of a Volcano Extinct- has not erupted in recorded history
Dormant- has erupted in recorded history, not currently erupting Active- is currently erupting
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Batholith: Large igneous rock mass underneath mountains
Dike: Magma that cuts across preexisting rock Laccolith: small pool of magma that collects just under Earth’s surface Pluton: Intrusive igneous rocks formed by converging plates Sill: Pool of solidified magma in between rock layers Stock: Small batholith
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Caldera: large crater formed from volcano collapse during or after it
erupts Crater: depression at volcano’s Summit Hot Spot: Hot area of a tectonic plate not along plate boundary Tephra: Rock fragments thrown into the air during a volcanic eruption Vent: Opening in Earth’s crust where lava erupts and flows outward Pyroclastic Flow: Fast-moving cloud of ash, gas, and volcanic material after an eruption
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Types of Volcanoes Cinder Cone Composite Shield
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Composite Volcanoes Pyroclastic material Solidified Lava Composed of alternating bands of pyroclastic material (volcanic fragments) and lava. Explosive eruptions Andesitic magma (high silica) Example: Mt St Helens and Mt. Rainier in the Cascade Range Mt St Helens
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Mt. Rainier
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Shield Volcanoes Wide volcanoes, gentle slope
Composed of layers of solidified magma Calm lava eruptions Basaltic Magma (low silica) Example: Hawaiian Islands Solidified lava
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Cinder Cone Composed of pyroclastic material (Tephra- volcanic fragments) Small and steep Explosive eruptions (high silica) Example: Paricutin in Mexico Pyroclastic Materials
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-due to the subduction of the Pacific Plate.
Volcanoes The majority of Earth’s surface volcanoes are found along the Pacific Plate Boundary- Ring of Fire. -due to the subduction of the Pacific Plate.
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Volcano Formation at Convergent Boundaries
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Volcano Formation at Convergent Boundaries
Mt St. Helens Mt. Pinatubo Aleutian Islands
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Volcanoes also form along the mid-ocean ridges
-due to upwelling of magma - long fissures in places
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Volcano Formation at Divergent Boundaries
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Volcano Formation at Divergent Boundaries
Iceland Volcanic Activity Black Smoker, Mid-Atlantic Ridge Pillow Basalts, South Pacific
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Volcano Formation NOT at Plate Boundaries: Hot Spot Volcanoes
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The Islands of Hawaii These islands formed over a period of 5 million years. The islands are slowly moving to the northwest with a active hot spot currently under the island of Hawaii. Plate Movement Hot Spot
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The Yellowstone Caldera is the volcanic caldera located in Yellowstone National Park in the United States, sometimes referred to as the Yellowstone Supervolcano
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Volcanic Hazards Lava Flows Pyroclastic Flows Lahars Earthquakes
Tsunamis Toxic Gases Volcanic Bombs Ash Falls More…
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