Area of ocean in which wind blows (fetch), wind velocity, and wind duration control the size of ocean waves.
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Love and Rayleigh waves which are collectively known as surface waves cause the most damage during earthquakes.
They would likely have much less of an impact than real ocean waves do. As it is, the only compressional waves that can move through water are sound waves, as water is, of the most part, incompressible, as are most liquids and solids.
Rock under stress breaks at the focus, releasing energy and vibrations called seismic waves, which travel away from the focus, through Earth's interior, and across the surface. The three types of seismic waves are: Primary waves: The first to arrive at seismographs Secondary waves: The second to arrive at seismographs Surface waves: The last and most severe to arrive at seismographs
S waves
no a volcano