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Seismic waves – WJECP and S waves' paths through Earth

Earthquakes produce shockwaves called seismic waves. These waves can be detected using seismographs. Some seismic waves are surface waves, while others can travel through the Earth.

Part of Physics (Single Science)Electricity, energy and waves

P and S waves' paths through Earth

The speed of P waves and S waves increases as they travel deeper into the Earth’s .

They travel through the Earth in curved paths, but they change direction suddenly when they pass through the boundary between substances in different states.

The diagrams show what happens when P waves and S waves pass through the Earth.

P waves

  • Longitudinal
  • Fast moving
  • Travel through liquids and solids
Diagram showing the curved path of P waves through the Earth. They travel through the mantle, the liquid outer core and the solid inner core.
Figure caption,
P waves can pass through the Earth's core

S waves

  • Transverse
  • Slower moving than P waves
  • Travel through solids only
Diagram showing the curved path of S waves through the Earth. They travel through the mantle but cannot pass through the liquid outer core.
Figure caption,
S waves do not pass through the Earth's core

S waves cannot pass through the liquid outer core, but P waves can. The waves are refracted as they travel through the Earth due to a change in density of the medium. This causes the waves to travel in curved paths. When the waves cross the boundary between two different layers, there is a sudden change in direction due to refraction.

Question

Compare the properties of P waves, S waves and surface seismic waves.