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Rock under stress breaks at the focus, releasing energy and vibrations called seismic waves, which travel away from the focus, through Earth's interior, and across the surface. The three types of seismic waves are: Primary waves: The first to arrive at seismographs Secondary waves: The second to arrive at seismographs Surface waves: The last and most severe to arrive at seismographs
P-waves are the first seismic waves to arrive at a seismograph station.
A surface wave is the last seismic wave to arrive after an earthquake.
P-waves
# Types of Waves that Travel Through the Earth's Surface * P waves arrive first and vibrate energy back and forth * S waves arrive second and shake side to side and up and down * Surface waves arrive last when an earthquake has occurred, they last the longest, are the most violent from the surface
No
p waves s waves surface waves so no
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
P waves are the fastest seismic waves and would arrive first.
Primary waves are seismic waves and the arrive first after an earthquake occurs.
P Wave
P waves
Rock under stress breaks at the focus, releasing energy and vibrations called seismic waves, which travel away from the focus, through Earth's interior, and across the surface. The three types of seismic waves are: Primary waves: The first to arrive at seismographs Secondary waves: The second to arrive at seismographs Surface waves: The last and most severe to arrive at seismographs
P Wave
P-waves
P Wave
P-waves are the first seismic waves to arrive at a seismograph station.