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Earthquakes - Structure of the Earth - P Waves and S Waves.
The two
types of wave which travel through the planet
from an earthquake
are called P waves and S
waves.
S waves are transverse,
P waves are longitudinal.
P waves travel faster
than S waves.
In the picture below, P
waves are shown in blue and S
waves in red.
The earthquake has occurred on the left
side of the planet,
the waves are moving from left
to right.

The transverse S waves
cannot travel through the liquid
outer core.
They can travel through the mantle
because the mantle behaves more like a solid
than a liquid.
The S waves curve as
they move through the mantle
due to refraction as the density
of the mantle changes.
The longitudinal P waves
can travel through the whole planet.
They also curve with the changing
density of both the mantle and the core
(except the wave passing through the centre,
which travels in a straight line, normal
to the boundary).
The P waves change direction
suddenly
at the boundary between the different
layers of the Earth.
This is due to refraction caused by the different
densities of the layers.
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Copyright © 2007 Dr. Colin France. All Rights Reserved.