Uses of waves and electromagnetic radiation - OCR GatewaySeismic waves - Higher
All objects emit and absorb electromagnetic radiation, which is essential for life on Earth. Waves can be used to probe inside the Earth to examine its internal structure.
seismic wavesShock waves travelling through the Earth, usually caused by an earthquake. are produced by earthquakes in the Earth鈥檚 crust. They can cause damage to structures on the Earth鈥檚 surface, as well as tsunamiA large destructive wave caused by earthquakes, volcanic activity or landslides under water..
Properties of seismic waves
There are two types of seismic wave:
P waves, which are longitudinal waveA wave that moves in the same direction as the way in which the particles are moving.
S waves, which are transverse waveA wave that moves in a direction at right angles to the way in which the particles are vibrating.
P waves and S waves have different properties. The table summarises these properties:
P waves
S waves
Type of wave
Longitudinal
Transverse
Relative speed
Faster
Slower
Can travel through
Solids and liquids
Solids only
Type of wave
P waves
Longitudinal
S waves
Transverse
Relative speed
P waves
Faster
S waves
Slower
Can travel through
P waves
Solids and liquids
S waves
Solids only
Investigating the Earth's structure using seismic waves
The study of seismic waves provides evidence for the internal structure of the Earth, which cannot be observed directly.
Seismic waves from large earthquakes are detected around the world using seismometerA machine that detects seismic waves caused by earthquakes.. Their paths are usually curved 鈥 this is due to the fact that the waves are refractionProcess by which a wave changes speed and sometimes direction upon entering a denser or less dense medium, eg a light ray changes direction when refracted by a lens. as they meet the gradually changing density of the layers within the Earth.
S waves are not detected on the opposite side of the Earth 鈥 this suggests that the mantle has solid properties, but the outer coreThe Earth's outer core is a fluid layer that sits above the solid inner core. must be liquid.
P waves are detected on the opposite side of the Earth. Refractions between
layers cause two shadow zones, where no P waves are detected 鈥 the size and positions of these shadow zones indicate there is a solid inner core.