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.
The speed of P waves and S waves increases as they travel deeper into the Earth’s mantleA zone of hot rock in the interior of the earth located between the outer crust and the molten core. It has the properties of a solid, although it can also flow, very slowly..
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
S waves
Transverse
Slower moving than P waves
Travel through solids only
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.
A surface wave travels along the surface of the Earth. It is the slowest of the three types of seismic wave. Surface waves usually have larger amplitude than the other waves and cause the most damage.
A P wave is a longitudinal wave and travels the fastest. It can travel through solids and liquids.
An S wave is a transverse wave and travels slower than a P wave, thus arriving after the P wave. S waves can only travel through solids, and as a result do not travel through the liquid core of the Earth.