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The Geosphere
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Essential Question How does the structure of the earth affect the composition and distribution of resources?
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All are connected with each other
Earth System Geosphere Atmosphere Hydrosphere Biosphere All are connected with each other
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Geosphere The rock and soil that make up the solid part of the earth
Diameter of the earth at the equator: 12, 756km (7,926 mi.) Diameter of the earth at the poles: 12, 715km (7,901 mi.)
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Compositional Layers Determined by chemistry
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Compositional Layers Crust Thin outer layer 5-70km thick
Thicker but less dense under continents Thinner but denser under oceans
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Compositional Layers Mantle 2,900km 2/3 mass of earth Iron
Convection currents
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Compositional Layers Core 3,400km thick Densest layer Iron and Nickel
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Physical Layers Determined by physical properties
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Physical Layers Lithosphere 15-300km thick Crust and upper mantle
Rigid Tectonic plates
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Physical Layers Asthenosphere 250km thick Solid and plastic
Fluid (moves slowly)
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Physical Layers Mesosphere 2,550km thick Lower part of mantle
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Physical Layers Outer Core Inner Core 2,200km thick
Liquid nickel and iron Inner Core 1,228km thick Solid Nickel and iron
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Plate Tectonics Alfred Wegener – 1912
Continents were once single land mass Drifted apart Considered a crackpot The lithosphere is broken into different plates Plates move on top of plastic asthenosphere
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Pangea
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Laurasia and Gondwana 200Mya
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Convergant Boundaries
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Convergant Boundaries
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Divergent Boundaries
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Divergent Boundaries
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Transform Boundaries
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Ring of Fire
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