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EarthSci 4 - Earthquake
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EarthSci 4 - Earthquake


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  • 1. Focus, Epicenter, and Fault
  • 2. Elastic Rebound Hypothesis
  • 3. Elastic Rebound Hypothesis
  • 4. Seismograph
  • 5. Seismogram
  • 6. Seismic Waves Paths Through the Earth
  • 7. Measuring EarthquakesP Waves - Are push-pull waves that push (compress) and pull (expand) in the direction that the waves travel - Travel through solids, liquids, and gases - Have the greatest velocity of all earthquake waves
  • 8. Measuring EarthquakesS Waves - Seismic waves that travel along Earth’s outer layer - Shake particles at right angles to the direction that they travel - Travel only through solids - Slower velocity than P waves
  • 9. Earth’s Interior Showing P and S Wave Paths
  • 10. Measuring EarthquakesLocating an Earthquake Earthquake Distance • The epicenter is located using the difference in the arrival times between P and S wave recordings, which are related to distance. Earthquake Direction • Travel-time graphs from three or more seismographs can be used to find the exact location of an earthquake epicenter. Earthquake Zones • About 95 percent of the major earthquakes occur in a few narrow zones.
  • 11. Locating an Earthquake
  • 12. Pusan Seismic Station S-P Interval = seconds
  • 13. Tokyo Seismic Station S-P Interval = seconds
  • 14. Akita Seismic Station S-P Interval = seconds
  • 15. Station S-P Interval Epicentral DistancePusan 60 seconds KMTokyo 50 seconds KMAkita 70 seconds KM
  • 16. RECORDING S-P EPICENTER STATION INTERVAL DISTANCE PUSAN 56 sec 549 km TOKYO 44 sec 434 km AIKITA 71 sec 697 km
  • 17. Location You Found Actual Location
  • 18. Measuring Earthquakes Richter Scale • Based on the amplitude of the largest seismic wave • Each unit of Richter magnitude equates to roughly a 32-fold energy increase • Does not estimate adequately the size of very large earthquakes
  • 19. Measuring Earthquakes Modified Mercalli • scales measures how people feel and react to the shaking of an earthquake. • It is a relative scale, because people experience different amounts of shaking in different places. • It is based on a series of key responses such as people awakening, the movement of furniture, and damage to structures.
  • 20. Earthquake Magnitudes
  • 21. Destruction from Earthquakes Seismic Vibrations  Liquefaction • Saturated material turns fluid • Underground objects may float to surface
  • 22. Tsunami
  • 23. Tsunami Cause of Tsunamis • A tsunami triggered by an earthquake occurs where a slab of the ocean floor is displaced vertically along a fault. • A tsunami also can occur when the vibration of a quake sets an underwater landslide into motion. • Tsunami is the Japanese word for “seismic sea wave.”
  • 24. Destruction from Earthquakes  Landslides • With many earthquakes, the greatest damage to structures is from landslides and ground subsidence, or the sinking of the ground triggered by vibrations.  Fire • In the San Francisco earthquake of 1906, most of the destruction was caused by fires that started when gas and electrical lines were cut.
  • 25. Predicting Earthquakes Short-Range Predictions • So far, methods for short-range predictions of earthquakes have not been successful. Long-Range Forecasts • Scientists don’t yet understand enough about how and where earthquakes will occur to make accurate long-term predictions. • A seismic gap is an area along a fault where there has not been any earthquake activity for a long period of time.