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The Earth’s Interior. Most of what we know is from geophysics.

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Presentation on theme: "The Earth’s Interior. Most of what we know is from geophysics."— Presentation transcript:

1 The Earth’s Interior

2 Most of what we know is from geophysics

3 Evidence from Seismic Waves Seismic Reflection Seismic Refraction

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7 Earth’s Internal Structure The Core P-wave Shadow Zone S-wave Shadow Zones Liquid Outer Core Solid Inner Core

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9 S-Wave Shadow Zone

10 Earth’s Internal Structure The Earth’s Crust Continental crust- sial Less dense and thicker than oceanic crust Oceanic crust- sima Mohorovicic discontinuity

11 P-Wave Velocities & Boundaries Moho

12 Earth’s Internal Structure The Mantle Ultramafic Rock Lithosphere Crust & uppermost mantle Asthenosphere Low velocity zone Lower mantle

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14 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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