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  1. 1. Earthquakes
  2. 2. Global Earthquake Locations
  3. 3. Earthquakes• Shaking of earth due to movement of rocks along a fault.• Rocks under stress accumulate strain energy over time.• When stress exceeds strength of rocks, rock breaks.• Strain energy is released as seismic waves. The longer that energy is stored up and is maintained without release, the more likely that a strong earthquake will occur.Types of seismic waves1. Body waves -- travel through interior2. Surface waves -- travel on surface of earth 
  4. 4. Surface or "Love" (“L”) WavesCause vertical & horizontal shakingTravel exclusively along surface of earthSpecific Body WavesPrimary or "P" Waves: Primary waves Highest velocity. Causes compression and expansion in direction of wave travel.Secondary or "S" Waves: Secondary or shear waves Slower than P waves but faster than surface waves. Causes shearing of rock perpendicular to direction of wave propagation. Cannot travel through liquids
  5. 5. Primary or “P”WaveSecondary or“S” Wave
  6. 6. Seismographs
  7. 7. Seismogram Printout
  8. 8. Determining the location of an earthquakeFirst, distance to earthquake is determined.1. Seismographs record seismic waves 2. From seismograph record called the seismogram, measure time delay between P & S wave arrival 3. Use travel time curve to determine distance to earthquake as function of P-S time delay  
  9. 9. Determining the location of an earthquake Now we know distance waves traveled, but we dont know the direction fromwhich they came.We must repeat the activity for each of at least three (3) stations totriangulate a point (epicenter of quake). Plot a circle around seismograph location; radius of circle is the distance to thequake.Quake occurred somewhere along that circle.Do the same thing for at least 3 seismograph stations; circles intersect at epicenter. Thus, point is triangulated and epicenter is located. 
  10. 10. Focus and Epicenter of Earthquake
  11. 11. Time-Travel Curve
  12. 12. Triangulationof 3 stationsto locateearthquakeepicenter
  13. 13. Determining the magnitude of an earthquakeMagnitude -- measure of energy released during earthquake.There are several different ways to measure magnitude.Most common magnitude measure is Richter Magnitude, named for the renowned seismologist, Charles Richter. Richter Magnitude• Measure amplitude of largest S wave on seismograph record.• Take into account distance between seismograph & epicenter. Richter Scale• Logarithmic numerical (NOT a physical) scale• Increasing one whole unit on Richter Scale represents 10 times greater magnitude.• Going up one whole unit on Richter Scale represents about a 30 times greater release of energy.Intensity• Intensity refers to the amount of damage done in an earthquake• Mercalli Scale is used to express damage
  14. 14. Hazards associated with Quakes• Shaking: Frequency of shaking differs for different seismic waves. High frequency body waves shake low buildings more. Low frequency surface waves shake high buildings more. Intensity of shaking also depends on type of subsurface material. Unconsolidated materials amplify shaking more than rocks do. Fine-grained, sensitive materials can lose strength when shaken. They lose strength by liquefaction. Buildings respond differently to shaking depending on construction styles, materials Wood -- more flexible, holds up well Earthen materials -- very vulnerable to shaking.
  15. 15. Hazards associated with Quakes• Ground displacement: Ground surface may shift during an earthquake (esp. if focus is shallow). Vertical displacements of surface produce fault scarps.• Tsunamis (NOT tidal waves) Tsunamis are huge waves generated by earthquakes undersea or below coastal areas. If earthquake displaces sea surface, wave is generated that can grow as it moves over sea surface.• Fires Usually occurs from shifting of subsurface utilities (gas lines)
  16. 16. Tsunami Movement
  17. 17. Tsunami Movement: ~600 mph in deep water ~250 mph in medium depth water ~35 mph in shallow water
  18. 18. Earthquake Prediction (?)How can scientists predict an earthquake?Currently, that is not possible.Future technology will monitor subsurface seismic waves and periodic shifting indicative of future slippage.Tracking organic movement is also a source of future study.
  19. 19. Earthquake Hazard Potential MapParkfield, CA“Earthquake Capital of the World”
  20. 20. World’s Largest Earthquake: 1964 Anchorage, Alaska Registered 8.6 on Richter Scale