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For seismic waves through the bulk material the longitudinal or compressional waves are called P waves (for primary waves) whereas the transverse waves are callled S waves (secondary waves). Since any material, solid or liquid (fluid) is subject to compression, the P waves can travel through any kind of material.
Surface waves are the slowest seismic waves and are the final waves to hit an area after an earthquake. First, P-waves move through compression through the deep layers of the Earth. P-waves are also carried by air and water, causing them to make a sound when they hit the Earth's surface. They result in minimal damage.