Seismology
Linear elasticity is a property of materials that describes their ability to deform under stress and return to their original shape once the stress is removed, following Hooke's Law. This behavior is crucial in understanding how seismic waves, particularly surface waves, propagate through the Earth's crust, as it impacts their velocity and dispersion characteristics. The linear relationship between stress and strain in elastic materials allows for predictable behavior when subjected to various forces.
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