Seismic waves are created by the abrupt movement of elements within the Earth, such as fault slip during an earthquake.
Seismic waves can be caused by volcanic eruptions, explosions, landslides, avalanches, and even flowing rivers.
Types of Seismic waves:
Primary waves:
Primary waves (P-waves) are compressional waves that travel in a straight line.
P-waves are pressure waves that move quicker through the ground than other waves, arriving first to seismograph stations, thus the term "Primary."
These waves may move through any substance, including fluids, at roughly 1.7 times the speed of S-waves.
They assume the shape of sound waves in air and hence travel at the speed of sound.
Secondary waves:
Secondary waves (S-waves) are transversely oriented shear waves.
S-waves arrive at seismograph stations after the faster-moving P-waves and displace the ground perpendicular to the propagation direction.
The surface features of the wave might vary depending on its propagational direction; for example, in the case of horizontally polarised S waves, the ground moves alternately to one side and then the other.
Because fluids (liquids and gases) do not support shear forces, S-waves can only move through solids.
Surface waves:
A surface wave is a mechanical wave that propagates at the interface of two different mediums in physics.
Gravity waves on the surface of liquids, such as ocean waves, are a frequent example.
Gravity waves may also arise within liquids, for as at the interface of two fluids of differing densities.