6.3.7

Uses of Sound Waves: Earthquakes

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Earthquakes

Seismic waves are waves which travel through the Earth. Earthquakes produce two types of seismic waves:

P-waves (primary)

P-waves (primary)

  • These are longitudinal, seismic waves.
  • P-waves travel at different speeds through solids and liquids.
S-waves (secondary)

S-waves (secondary)

  • These are transverse, seismic waves.
  • S-waves cannot travel through liquids (only through solids).
Uses of seismic waves

Uses of seismic waves

  • Seismic waves cannot travel through all parts of the earth because the earth is made up of different materials.
  • Scientists have used this principle to work out the different materials that the earth is made up of.
  • By detecting seismic waves from Earthquakes, scientists have worked out that the Earth has a solid core surrounded by a liquid outer core.
    • A mantle of changing density surrounds the Earth’s core. This mantle causes the refraction of the seismic waves.
Jump to other topics
1

Energy

2

Electricity

3

Particle Model of Matter

4

Atoms & Radiation

5

Forces

5.1

Basics of Motion

5.2

Forces

5.3

Effects of Forces

5.4

Pressure

6

Waves

6.1

Wave Basics

6.2

Waves at a Boundary

6.3

Sound Waves

6.4

Electromagnetic Waves

6.5

Lenses

6.6

Heat & Radiation

7

Magnetism

8

Astrophysics

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