Seismic waves consist of
The P Waves. Then the S Waves.
Love waves are the most strongest type of Earthquakes.
Primary and secondary waves.
P-waves(primary waves) travel faster than S-waves(secondary waves)
A surface wave is the last seismic wave to arrive after an earthquake.
The P Waves. Then the S Waves.
seismic waves and pressure waves it depends on intensity of the earthquake
S waves arrive second after an earthquake.
P waves - compress and expand the ground like a accordion S waves - vibrate from side to side as well as up and down Surface waves - make the ground roll like ocean waves The Earthquake is produced by each of the three types of seismic waves.
Seismic waves.
Love waves are the most strongest type of Earthquakes.
The surface waves (of which their are two types, Rayleigh and Love waves) cause the most damage during an earthquake.
Seismic waves can be used to determine the location of an earthquake focus. These waves are triggered by tectonic plates.
Primary and secondary waves.
Primary waves
Rayleigh waves are a type of Surface wave. Surface waves occur when Secondary waves and Primary waves reach the Surface of the Earth's crust during an earthquake. Surface waves cause the most damage.
A P wave is a type of seismic wave that is caused by an earthquake. P waves are the first seismic waves felt during an earthquake. When the P wave moves, rock particles move back and forth along the direction of the P wave.