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What is Seismic Refraction Method Explained about?

This document discusses seismic refraction, which uses the refraction of seismic waves to characterize subsurface geology. It works by generating seismic waves at the surface using a hammer or dynamite, which are detected by geophones. The refraction and reflection of waves between geophones as they pass through different subsurface layers are recorded. Data processing involves analyzing travel time graphs to determine layer velocities and depths based on wave propagation speed changes at boundaries. While

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