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Volcanoes
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They result from plate tectonics
Volcanoes They result from plate tectonics The movement of plates or plate shifting Vents- openings in the Earth’s crust; magma exits
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3 things they release Molten rock (magma) When it reaches the Earth’s surface it is called lava Ash Poisonous gases
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Shield Volcano Composite Volcano Cinder Cone Volcano
3 types of Volcanoes Shield Volcano Composite Volcano Cinder Cone Volcano Depends on the type of eruption
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Eruptions can happen several times
Shield Volcanoes Largest volcanoes Mild eruptions Eruptions can happen several times
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Shield Volcanoes magma
Rich in iron Very fluid Can flow a great distance Produce gently sloping mountains
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Where are they found? Hawaii Mauna Loa
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Shield Volcanoes
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Composite Volcanoes Made of alternating layers of: Ash Cinders Lava
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Composite Volcanoes More violent eruptions
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Composite Volcanoes Magma
Rich in Silicates Thicker lava Gases are trapped in magma
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Composite Volcanoes Because of gases This causes eruptions that alternated between flow and explosive activity Steeper slopes 1000’s of meter high
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Examples Mount St. Helen Mount Fuji
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Smallest & most abundant Violent eruptions Gases are trapped in magma
Cinder Cone Volcanoes Smallest & most abundant Violent eruptions Gases are trapped in magma Larger amounts of gases
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Hot ash and lava are thrown from the vent forming a cone.
Cinder Cone Volcanoes Hot ash and lava are thrown from the vent forming a cone.
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They are only active for a short period of time.
Cinder Cone They are only active for a short period of time.
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Cinder Cone
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They are called seamounts Similar to Shield volcanoes
Can occur under water They are called seamounts Similar to Shield volcanoes
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Converging Boundaries
Volcanoes occur at convergent Boundaries. Usually around the Pacific Ocean Ring of fire – 75% of all volcanoes are located on the Pacific Plate Boundary.
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Convergent As ocean plates subduct: Magma rises and forms volcanoes
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Divergent Boundaries Volcanoes can occur at divergent boundaries also.
When plates move apart: Magma rises and fills in gaps Magma creates a volcanic mountain
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Hot Spots Magma from deep inside the mantle rises to the surface
This happens in the middle of plates This is called a hot spot This can form Islands
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Chain of Islands Plates can move Hot Spots do not move
This is how chains of islands are formed Hawaiian Islands
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