Mantle or Core but I think its the mantle
mantle
the waves caused by an earthquake are called seismic waves
focus
The Love and Rayleigh waves (collectively known as surface waves) are the slowest moving but most damaging of the seismic waves.
the seismic waves work when the erosion happened in the middle of the ocean and then they burn so they explode!!
mantle
The epicenter does not recive seismic waves.
The first waves to arrive at a seismograph station are primary waves, or P waves.
P-waves are the first to arrive at a seismic station. There are two major types of waves: Body waves and surface waves. P-waves and S-waves come under Body waves while Love and Rayleigh waves come under surface waves. Body waves are much faster than the Surface waves. Waves are detected in the following order: P, S, Love and Rayleigh
it take 45or350 p-waves to get to the seismic station
the energy of an earthquake, called seismic waves,originates from a point called the ? epicenter
The difference in arrival times of P and S waves.
P-waves are the first seismic waves to arrive at a seismograph station.
There are three types of seismic waves released by an earthquake. Primary waves (P waves) are longitudinal or compressional waves and travel through the Earth's interior. They are first to arrive at a seismic station (velocity 5-8 km/s). Secondary waves (S waves) are a transverse or shear wave and move at a lower speed than that of primary waves (velocity 3-5 km/s). They arrive second at the seismic station. Finally, there are surface waves which as the name suggests travel along the Earth's surface, there are two main types (the Love wave and Rayleigh wave) and these are the slowest types of seismic waves (velocity 2.5 - 4.5 km/s) and hence arrive last at the seismic station.
Seismic waves are any waves that travel through the Earth. As such all earthquake waves are seismic waves, however not all seismic waves are caused by earthquakes.
P-waves which are a compression or pressure wave are the fastest seismic waves. As they are the fastest they will reach the seismic station before any of the other seismic waves and be recorded first. Seismologists can use the difference between the arrival times of different seismic waves to calculate the distance and ultimately the location of the earthquakes epicentre. For information on this, please see the related question.
(not seismic, seismic wave)Seismic waves are waves of energy that travel through the earth.