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An earthquake generates three kinds of waves: surface waves (L-waves), which are the slowest and weakest,...
An earthquake generates three kinds of waves: surface waves (L-waves), which are the slowest and weakest, shear (S) waves, which are transverse waves and earn- most of the energy, and pressure (P) waves, which are longitudinal waves and are the fastest. People do not generally feel the P waves, but animals seem to be sensitive to them. Take the density of the material through which these waves travel to be 2.0 times 10^3 kg/m^3, the Young's modulus to be 9.8 times 10^10 N/m^2,...