大象传媒

Seismic waves - Higher

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 .

Cross-section showing structure of the Earth: the inner core, outer core, mantle and crust.

Properties of seismic waves

There are two types of seismic wave:

  • P waves, which are
  • S waves, which are

P waves and S waves have different properties. The table summarises these properties:

P wavesS waves
Type of waveLongitudinalTransverse
Relative speedFasterSlower
Can travel throughSolids and liquidsSolids only
Type of wave
P wavesLongitudinal
S wavesTransverse
Relative speed
P wavesFaster
S wavesSlower
Can travel through
P wavesSolids and liquids
S wavesSolids 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 . Their paths are usually curved 鈥 this is due to the fact that the waves are 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 must be liquid.

S waves travelling through the Earth.

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.

P waves travelling through the Earth.
Figure caption,
P waves are refracted as they travel through the Earth