Seismology
Site response refers to the way local soil and geological conditions amplify or attenuate seismic waves during an earthquake, significantly affecting ground motion at a specific location. This phenomenon is crucial for understanding how different areas experience varying levels of shaking and potential damage during seismic events. The characteristics of the underlying materials, such as their type, thickness, and layering, play a key role in determining the site response, which is often incorporated into ground motion prediction equations to assess earthquake hazards more accurately.
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