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Earth Part 2 G. Yannakoulias
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Earth’s Layers
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Image of Earth’s Crust
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Earth’s Crust Thin layer of solid rock surrounding Earth
Thickness of crust varies depending whether oceanic or continental crust Thinner under the oceans—called oceanic crust (10 km) Thicker under the continents—continental crust (40 km) Continental crust—mostly granite rock Oceanic crust—mostly basalt rock
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Image of Earth’s Mantle—Upper and Lower Mantle Exist
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Upper Mantle Thickness: 660 km Temperatures: 500-1000 degrees Celsium
Top part of this layer is solid Top part of solid mantle and crust together make up the lithosphere (Gk. lithos = rock) Lower part of upper mantle is “gooey” like taffy and is responsible for movement of surface plates through convection currents
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Lower Mantle Thickness: 2200 km
Temperatures: degrees celsius Mostly solid in texture Made of dense solid rock
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Outer Core
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Outer Core Composition
Liquid layer 2270 km in thickness Made of mostly iron and nickel Responsible for creating the magnetic field of the Earth Temperatures: degrees Celsius
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Inner Core Thickness: 1200 km Temperature: 5000-6000 degrees Celsius
Solid in Composition Solid due to high pressures
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