There are 3 broad types of seismic waves, Surface waves, S-waves and P-waves. Love waves (a type of surface wave) and S-waves are transverse waves and P-waves are compressional.
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.
P-waves and S-waves. P waves are known as Primary waves as they have a high velocity and so are recorded at seismometer stations before Secondary or S-waves. P waves may also be known as pressure waves as they are in fact compression or longitudinal waves. S-waves may also be known as shear waves as they are transverse waves.
The Love and Rayleigh waves (collectively known as surface waves) are the slowest moving but most damaging of the seismic waves.
Seismic waves
True
light waves are transversal, seismic waves are longitudinal.
The three types of seismic waves are:P waves, S waves, and Surface waves
sound waves, seismic wavessound waves
Primary or P waves
Primary or P waves
Primary seismic waves are longitudinal waves. Longitudinal waves can travel through solids, liquids and gasses (although seismic waves are of to low a frequency to normally be heard). Secondary seismic waves are transverse waves and only travel through solids.
The Answer is primary waves.
There are 3 broad types of seismic waves, Surface waves, S-waves and P-waves. Love waves (a type of surface wave) and S-waves are transverse waves and P-waves are compressional.
Longitudinal Waves
Seismic waves: longitudinal compression waves.
Seismic waves: longitudinal compression waves.