NONE!!!!
P-Waves. See the related links.
Seismic waves, such as compressional (P-waves) and shear (S-waves), can deform rocks by alternately compressing and stretching them as they pass through the Earth's crust during an earthquake. This can lead to the fracturing and displacement of rock layers.
The first waves to hit are primary waves. Primary waves are seismic waves that compress and stretch the ground. P waves, or primary waves, can wreck buildings and can move straightforward through solids and liquids.
P waves
P waves
Source earthquake waves are seismic waves produced directly from the earthquake's source, such as the initial rupture of rocks along a fault. These waves include P-waves and S-waves that travel through the Earth and are used to locate and study earthquakes. Source earthquake waves provide valuable information about the earthquake's characteristics and help in assessing its impact.
S waves
A Pwave is the first wave to arrive during an earthquake, P waves compress and then expand. They can damage buildings.
Seismic Waves
The fastest waves that compress and expand the ground like an accordion are primary waves (P-waves). These seismic waves are the first to arrive after an earthquake and travel through solids, liquids, and gases. They cause particles in the ground to move in the same direction as the wave itself, resulting in the compressional and expansion effects.
water
Longitudinal waves.