Shock waves can be classified into
two broad categories.Waves that send particles oscillating back and forth in the same
direction as the waves are traveling are called primary.
Primary waves, sometimes called compressional waves, travel through the
earth beneath the crust. Secondary waves cause vibrations which move perpendicular to the
wave. These waves travel on the surface of the earth and move much slower than primary
waves. Thus, when an earthquake occurs, seismic centers throughout the world record
primary waves before the secondary waves arrive.