Earth's Interior Structure: A Seismic and Geochemical Perspective
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The Seismic Method
An indirect method of study that looks at the variations in the propagation speed of seismic waves as they travel through different materials inside the geosphere.
What are Seismic Waves?
Vibrations generated inside the Earth at the point where an earthquake takes place. They propagate in all directions, and the more rigid the material they pass through, the more quickly they travel. There are three types:
- P waves: Cause the material to vibrate, alternating between compression and dilation. These waves propagate through solids and liquids.
- S waves: Cause the material to oscillate perpendicular to the direction of propagation. They are slower and cannot travel through liquids.
- Surface waves: Generated when P and S waves reach the