But the main ones are:
– Primary (“P”) waves which are longitudinal (they compress and expand along the direction of the wave) and travel fastest
– Secondary (“S”) waves which are transverse (they shake up and down along the direction of the wave) and are a bit slower.
Geologists can find out about the structure of the Earth from how the waves arrive at different locations, a bit like a medical ultrasound but for the whole planet.
There are 3 main types of waves. In longitudinal waves, particles oscillate parallel to the direction of travel of the wave (like sound). In transverse waves, particles oscillate perpendicular to the direction of travel of the wave (like light). In surface waves, particles oscillate in a circular motion (like ocean waves).
Earthquakes can produce all three of these types of waves
Comments