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Published byAshley Stephens Modified over 8 years ago
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The Earth’s Interior
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Most of what we know is from geophysics
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Evidence from Seismic Waves Seismic Reflection Seismic Refraction
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Earth’s Internal Structure The Core P-wave Shadow Zone S-wave Shadow Zones Liquid Outer Core Solid Inner Core
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S-Wave Shadow Zone
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Earth’s Internal Structure The Earth’s Crust Continental crust- sial Less dense and thicker than oceanic crust Oceanic crust- sima Mohorovicic discontinuity
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P-Wave Velocities & Boundaries Moho
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Earth’s Internal Structure The Mantle Ultramafic Rock Lithosphere Crust & uppermost mantle Asthenosphere Low velocity zone Lower mantle
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Earth’s Internal Structure Composition of the Core Made of metal The Core-Mantle Boundary Convection in both core and mantle
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