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Inside the Earth Study Guide
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Solid because of the intense pressure pushing in on the INNER MOST layer. HOT! HOT! HOT! Inner core
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The Mantle Thickest layer
Molten magma layer allows convection currents that create plate movement Hotter than the crust, cooler than the core The Mantle
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Crust Least dense and lowest temperatures
Temperature is same as the air above it Crust
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Layer Composition State Crust Rock Solid Mantle Semi-solid Outer Core Metal (iron and nickel) Liquid Inner Core Temperature and Pressure INCREASE as you go deeper into the Earth!!!!! Layers of the Earth
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Tectonic Plates U.S. is part of the North American plate
Plates folding (converging) create mountains Plates moving apart create volcanoes Tectonic Plates
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Hot Spots Weak spots in the Earth’s crust
Because of sea-floor spreading, hot spots move, causing new land to form above them. Hot Spots
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Supercontinent composed of all of today’s continents put together into one large mass
Pangaea
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Focus is BENEATH the Earth’s surface where the Earthquake begins
Epicenter is ABOVE Earth’s surface, directly above the focus Seismic Waves
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Tsunami Created from an earthquake on an ocean floor
Creates large waves in the crust and in the water Tsunami
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Boundaries
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Most explosive = High silica content and low viscosity (thin consistency)
Slow flowing magma = Low silica content and high viscosity (thick consistency) Volcanoes go BOOM!
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Mid Ocean Ridges occur at Divergent Oceanic Plate Boundaries
Trenches occur at Convergent Oceanic Plate Boundaries Sea floor spreading
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Rift Valley
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Hot Springs
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The crater formed when the top of a volcanic mountain collapses
Calderas
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Island Arc
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Were on Earth for a short amount of time, but covered a large area
Index Fossils
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