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Volcanoes
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What is Magma? dr evil
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Magma Magma: Liquid rock under Earth’s surface
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Magma forms when… The temperature rises above the melting point of the rock The pressure is lower, which lowers the melting point of rock The addition of water lowers the melting point of the rock
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Volcano 101 video The video says that volcanoes are “both creators and destroys”. What does this mean? What are examples of this? volcanoes 101
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Volcanism Volcanism: the movement of magma onto Earth’s surface
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Volcanism Lava: magma on top of Earth’s surface
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In your packet: Explain the difference between magma and lava.
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Volcanism Volcano: an opening in earth’s surface through which magma and gases are expelled
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Major Volcanic Zones Most volcanoes form along convergent or divergent plate boundaries
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Volcanoes at Divergent Boundaries
Divergent boundaries: mid-ocean ridges The largest amount of lava rises at divergent boundaries Most are unnoticed by humans because it happens underwater
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Iceland Iceland: the only place on Earth where a divergent boundary is above sea level
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Convergent Boundaries
Volcanoes at Convergent boundaries: Volcanic mountain chains or volcanic island arcs Examples: Japan, Alaska Aleutian Islands, Mount Saint Helens The ring of fire is mostly made up of convergent boundaries
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Draw triangles on your map on page 1 to represent volcanoes on plate boundaries
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The Ring of Fire The Ring of fire: an area surrounding the Pacific Ocean where a large number of volcanoes and earthquakes occur.
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What about Hawaii?
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Hot Spots Hot spots: areas on Earth’s surface where magma is close to the surface Also called mantle plumes
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Hot Spots Hawaii and Yellowstone are examples of hot spots
Hawaii and Yellowstone are examples of hot spots The PLATE moves NOT the hot spot!!! Yellowstone
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Studying volcanoes Volcano Hazards:
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Types of Magma Mafic magma: rich in iron and magnesium and forms dark colored rock Example: Oceanic crust Produces: runny, quiet eruptions
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Types of Magma Felsic magma: rich in silicate materials and forms light colored rock Example: continental crust Produces: thick, explosive eruptions Magma with more dissolved gases is more explosive
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Types of Eruptions The flow of magma or lava depends on the viscosity of the magma Viscosity: how much a fluid resists flowing High Viscosity= lava that moves very slowly Low Viscosity= lava that moves quickly High Viscosity Low Viscosity
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Quiet Eruptions Quiet eruptions: mafic magma flows out slowly and has a high viscosity Examples: Hawaii
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More explosive because it has more dissolved gases in it
Explosive Eruptions Explosive Eruptions: Felsic magma that is thicker and has a low viscosity More explosive because it has more dissolved gases in it
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Types of Lava pahoe 2014 1. Pahoehoe lava: mafic lava that flows slowly and forms a wrinkled crust lava flows
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Lava Flows 2. Aa lava: mafic lava that flows faster and has a chunky texture Aa lava flow
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Lava Flows 3. Blocky Lava: cooled lava at surface breaks into large chunks
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Types of pyroclastic materials
4. Pyroclastic Material: Escaping gases send molten and solid rock into the air pyroclastic flow
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Types of Pyroclastic Material
Classified by particle size Ash: less than 2mm diameter
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Cont. Types of Pyroclastic Material
Volcanic bombs: molten rock larger than 64 mm in diameter Volcanic blocks: solid rock that can be larger than a house
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BOOM! Volcanic eruptions can be more powerful than atomic bombs!!
Marum Crater
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