Seismic Waves Flashcards
What are seismic waves?
Seismic waves are produced by earthquakes and volcanic eruptions.
What have scientists used to determine the internal structure of the Earth?
Scientists have used the properties of seismic waves.
What are seismic waves?
Waves produced by an earthquake or volcanic eruption that travel through the Earth
Seismic waves can be detected by instruments called seismometers.
What instruments detect seismic waves?
Seismometers
These instruments measure the seismic waves generated by earthquakes or volcanic eruptions.
What can scientists learn from seismic waves?
The inner structure of the Earth
By measuring the time it takes for seismic waves to reach different points and identifying locations they don’t reach.
What do scientists measure to study seismic waves?
- The time it takes for the seismic waves to reach different points on the surface
- Which places the seismic waves don’t reach
This information helps infer the Earth’s internal structure.
What happens if seismic waves do not reach a location?
They must have been reflected or refracted by a boundary between different types of material
This indicates a change in material properties within the Earth.
What are the two types of seismic waves?
- P waves
- S waves
These waves have different characteristics and behaviors as they travel through the Earth.
What are P waves?
Longitudinal waves that travel at different speeds through solids and liquids
P waves are the fastest seismic waves.
What are S waves?
Transverse waves that cannot travel through liquids
S waves are slower than P waves and only travel through solid materials.