Earth's Internal Structure: Seismic Waves (2.2.3) Flashcards
1
Q
Energy and Seismic Waves
A
- Measure energy in joules (1 J = 1 Nm).
- Seismic waves emanate out all directions from earthquake focus.
- Surface waves: analogous to water waves, travel along Earth’s surface.
- Body waves: travel through interior (faster than surface waves).
- P-wave (pressure wave)
- S-wave (shear wave)
- Rayleigh wave
- Love wave
2
Q
How is magnitude of earthquakes measured?
A
- Use Moment Magnitude Scale (not Richter Scale).
- Based on energy released (area of rupture x slip x rock rigidity).
3
Q
How often do large earthquakes occur?
A
- Only 7 large earthquakes (>8.8 magnitude) have occurred since 1900.
- 3 of them occurred past 15 years.
4
Q
How are historical earthquake sizes estimated?
A
- Moment Magnitude Scale and Richter Scale can’t be applied to any pre-WWII.
- Modified Mercalli Scale used (qualitative scale based on effects of earthquake from I to XII).
5
Q
What are the travel and arrival times of seismic waves?
A
- Body waves travel shorter distances than surface waves.
- Body waves faster than surface waves.
- P-, S-waves arrive first, followed by Love, Rayleigh waves.
- Difference in arrival times of P- and S-waves = locate epicentre of earthquake.