Earthquakes produce "seismic" waves. These can be split into two main types: Body Waves and Surface Waves. Body waves consist of P-waves (compression or longitudinal waves) and S-waves (shear or transverse waves). P-waves can go through solid, liquid, and gas forms but S waves can only travel through solids. The P waves reach seismic stations quicker than S waves as they travel at a greater speed. Surface waves travel more slowly than Body waves and there are two main types: The Rayleigh and Love wave.
The waves produced by earthquakes are called seismic waves.
earthquakes
Waves produced by earthquakes are called seismic waves. These waves can be further categorized into primary (P-waves), secondary (S-waves), and surface waves.
Seismic waves are produced by earthquakes
seismic waves
They're called Seismic waves
Seismic waves is the usual description.
A seismometer or seismograph will measure the amplitude and frequency of seismic waves which are produced by earthquakes.
Seismic waves such as those produced by earthquakes.
Seismic waves are the forms of energy produced by an earthquake.
Seismic Waves
Seismic waves are produced by earthquakes and travel through the Earth. These waves can be divided into two main types: body waves (P-waves and S-waves) that travel through the interior of the Earth, and surface waves that travel along the Earth's surface.