Earthquake
- Minor earth tremors by wave of vibration within the earth crust.
- Major earthquake by movement along faults.
- Produce gigantic tidal wave called tsunami.
- Major Earthquake: Great Lisbon Earthquake (1755) & Tokyo & Yokohama (1923), San Francisco (1906), Kansu in china (1920)
- Regions of greatest seismicity are Circum-Pacific areas, with the epicentres and the most frequent occurrences along the ‘Pacific Ring of Fire’.
- 70 % of earthquakes occur in the Circum-Pacific belt. Another 20% of earth quakes take place in the Mediterranean-Himalayan belt.
Earthquake waves
- Suddern release of energy (Tremos/vibtations). The energy travel in the form of waves (Sesmic waves).
- Focus – Point where earthquake first orginated/develop (Hypocenter)
- Epicenter – Point on the surface of earth, where earthquake is first felt.
P Waves | S waves | L Waves/ R Waves |
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Reason for shadow zone
- S waves – 105° - 105° - Because it asssed only solid.
- P Waves – 105 - 145° - It passed all layers, but different density of layer reflect the wave pass.
Types of Earthquakes
- Tectonic earthquakes - Sliding of rocks along a fault plane.
- Volcanic earthquake - Special class of tectonic earthquake.
- collapse earthquakes - Areas of intense mining activity.
- explosion earthquakes - Explosion of chemical or nuclear devices.
- Reservoir induced earthquakes. – Area of large reservoirs.
Measuring Earthquakes
- Magnitude scale - Energy released – Richter scale (Range: 0-10).
- Intensity scale – Damage caused – Mercalli (Range: 1-12).
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