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Volcanic Activity Chapter 18
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Magma Formation Forms deep beneath the Earth’s surface
Temperature must be high enough to melt rocks What factors, other than temperature, affect the formation of magma? Magma Formation
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Factors Affecting Magma Formation
Rocks in Earth’s lower crust and upper mantle do not melt to form magma, even though temperatures are high enough. Pressure Increases with depth As pressure increases, melting point increases Factors Affecting Magma Formation
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Factors Affecting Magma Formation
2. Water: Water lowers the melting point of rocks Factors Affecting Magma Formation
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Classifying Magma Magma is classified based on the composition
Composition of magma impacts magma’s viscosity Types of Magma: Basaltic Andesitic Rhyolitic Classifying Magma
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Types of Magma Basaltic Magma Forms in upper mantle Low viscosity
Small amounts of dissolved gas and silica Quiet eruptions Types of Magma
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Types of Magma 2. Andesitic Magma Found in subduction zones
~60% Silica Intermediate viscosity Source material Ocean crust Ocean Sediments Types of Magma
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Types of Magma 3. Rhyolitic Magma
Forms from mixing of molten material with silica and water-rich continental crust High Viscosity Large volume of trapped gas Explosive volcanoes Types of Magma
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Viscosity Higher temperatures = lower viscosity
More silica = higher viscosity Viscosity
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Plutons Form when magma cools beneath the Earth’s surface
Intrusive igneous rock bodies Can be exposed at Earth’s surface Classified by: Size Shape Relationship to surrounding rock Plutons
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Types of Plutons Batholiths Stocks Irregular shape
Largest Common in mountain chains Mainly composed of granite Gabbro and diorite also California Stocks Irregular shape Smaller than batholiths Types of Plutons
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Batholiths in Real Life
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Types of Plutons 3. Laccoliths Rounded side and flat side
Mushroom shaped Up to 16 km wide Utah, South Dakota, Montana How did this laccolith become exposed at Earth’s surface? Types of Plutons
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Types of Plutons 4. Sills 5. Dikes Intrudes parallel layers of rocks
Few cm to hundreds of meters Svalbard 5. Dikes Cuts across preexisting rocks Arizona Types of Plutons
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Sills and Dikes in Real Life
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Label
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Anatomy of a Volcano Vent: hole where lava comes out
Crater: depression around vent Less than 1 km Calderas: larger depressions Crater Lake Anatomy of a Volcano
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Types of Volcanoes Shield Volcanoes: Broad, gently sloping sides
Circular base Largest type Layered basaltic lava Hawaiian Islands Types of Volcanoes
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Types of Volcanoes 2. Cinder-Cone Volcanoes:
Material ejected piles up around vent Steep sides Usually small <500m high More water and silica than shield Hawaii Types of Volcanoes
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Types of Volcanoes 3. Composite Volcanoes
Layered volcanic fragments with lava Magma has large amounts of silica, water, and gases Mount St. Helens Types of Volcanoes
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Tephra: rock fragments thrown in the air during a volcanic eruptions
Classified by size Ranges from ash to the size of a car or house Volcanic blocks: angular fragments Volcanic bombs: rounded tephra Volcanic Material
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Clouds of gas, ash, and other tephra moving at incredible speeds
Nearly 200 km/hr Can contain poisonous gases Temperatures can exceed 700°C Pyroclastic Flows
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Where Do Volcanoes Occur?
Convergent Volcanism Magma is forced upwards through the plate and forms volcanoes Pacific Ring of Fire – Does the affect our country? Where Do Volcanoes Occur?
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Where Do Volcanoes Occur?
Divergent Volcanism Magma is forced upward into fractures and faults Rift volcanism occurs along ocean ridges This is how new seafloor is formed Iceland Divergent volcanism above water Where Do Volcanoes Occur?
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Where Do Volcanoes Occur?
Hot Spots Regions of the mantle where high temperature material moves to the surface Moves vertically, not laterally Hawaiian Islands Oldest island = Kauai Where Do Volcanoes Occur?
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