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Earthquakes
 
Global Seismicity
Continental Drift Animation based on paleomaps from  University of Texas Arlington
Plate tectonics:  predicting the future
Plate tectonics in the future: 50 my Australia will straddle the equator E. Africa will form new continent Antarctica will swing off the south pole Mediterranean will close off Atlantic Ocean will grow Pacific Ocean will shrink
Global Seismicity
Rocks are stressed too… Rock stress:  from tectonic forces, gravity, and weight of rocks above Types of stress Tension (stretching) Compression (shortening) Shear (twisting or tearing)
Strain = how rocks respond to stress 2 types folding (bending) faulting (breaking) depends on rock composition, pressure, and rock characteristics (brittle vs. ductile)
Types of folds Anticline  simple upfold layers slope down from axis younger on outside Syncline simple downfold layers slope up from axis younger on inside younger older younger older
Types of folds syncline anticline overturned anticline
Types of Faults Tension Compression Shear Stretching Shortening Twisting
Faulting = rocks on either side of a fracture are displaced relative to each other Earthquake:  caused by sudden release of energy along a fault
Anatomy of a fault Fault scarp  = steep cliffs that make up the edge of a displaced block
3 Types of Faults Normal tension Reverse compression Strike-slip (transcurrent) shearing lateral displacement
3 Types of Faults
3 Types of Faults Divergent Plate Boundaries
3 Types of Faults Convergent Plate Boundaries
3 Types of Faults Transform Plate Boundaries
Earthquakes = vibration in the Earth produced by shockwaves from sudden movements along faults Seismic = pertaining to earthquakes
Focus vs epicenter Focus  = center of fault motion Epicenter  = surface directly above focus
Seismometer
Seismogram
Richter Scale Scale is  exponential For every increase of 1 in the Richter scale,  the  wave amplitude   increases x10 Exponential decay Exponential growth y = y 0 e -kx y = e kx
a = 10 M Where  M is Richter magnitude, and  a is wave amplitude M = log 10 (a) Which is the same as Richter Scale Scale is  exponential For every increase of 1 in the Richter scale,  the  wave amplitude   increases x10
But  wave amplitude   is not the same as  energy released .  (see pg 408 in Strahler) E = 10 (4.8+1.5M)  = 10 4.8  ·10 1.5M Where  M is Richter magnitude, and  E is energy released So for every increase of 1 in the Richter magnitude,  energy increases   x 32 Richter Scale
How much energy is released? For example, the earthquake that caused the Indian Ocean tsunamis on Boxing Day 2004 (12/26/04) measured 9 on the Richter scale   How much energy was released by this quake? E = 10 (4.8 + 1.5M)
The Boxing Day Quake How much energy was released by this quake? E = 10 (4.8 + 1.5M) = 10 (4.8 + 1.5(9)) = 10 (4.8 + 13.5) = 10 (18.3) =  1.99 x 10 18 J For comparison, the average U.S. electric power consumption rate is 3 x 10 12 J/sec

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Lecture11 earthquakes

  • 2.  
  • 4. Continental Drift Animation based on paleomaps from University of Texas Arlington
  • 5. Plate tectonics: predicting the future
  • 6. Plate tectonics in the future: 50 my Australia will straddle the equator E. Africa will form new continent Antarctica will swing off the south pole Mediterranean will close off Atlantic Ocean will grow Pacific Ocean will shrink
  • 8. Rocks are stressed too… Rock stress: from tectonic forces, gravity, and weight of rocks above Types of stress Tension (stretching) Compression (shortening) Shear (twisting or tearing)
  • 9. Strain = how rocks respond to stress 2 types folding (bending) faulting (breaking) depends on rock composition, pressure, and rock characteristics (brittle vs. ductile)
  • 10. Types of folds Anticline simple upfold layers slope down from axis younger on outside Syncline simple downfold layers slope up from axis younger on inside younger older younger older
  • 11. Types of folds syncline anticline overturned anticline
  • 12. Types of Faults Tension Compression Shear Stretching Shortening Twisting
  • 13. Faulting = rocks on either side of a fracture are displaced relative to each other Earthquake: caused by sudden release of energy along a fault
  • 14. Anatomy of a fault Fault scarp = steep cliffs that make up the edge of a displaced block
  • 15. 3 Types of Faults Normal tension Reverse compression Strike-slip (transcurrent) shearing lateral displacement
  • 16. 3 Types of Faults
  • 17. 3 Types of Faults Divergent Plate Boundaries
  • 18. 3 Types of Faults Convergent Plate Boundaries
  • 19. 3 Types of Faults Transform Plate Boundaries
  • 20. Earthquakes = vibration in the Earth produced by shockwaves from sudden movements along faults Seismic = pertaining to earthquakes
  • 21. Focus vs epicenter Focus = center of fault motion Epicenter = surface directly above focus
  • 24. Richter Scale Scale is exponential For every increase of 1 in the Richter scale, the wave amplitude increases x10 Exponential decay Exponential growth y = y 0 e -kx y = e kx
  • 25. a = 10 M Where M is Richter magnitude, and a is wave amplitude M = log 10 (a) Which is the same as Richter Scale Scale is exponential For every increase of 1 in the Richter scale, the wave amplitude increases x10
  • 26. But wave amplitude is not the same as energy released . (see pg 408 in Strahler) E = 10 (4.8+1.5M) = 10 4.8 ·10 1.5M Where M is Richter magnitude, and E is energy released So for every increase of 1 in the Richter magnitude, energy increases x 32 Richter Scale
  • 27. How much energy is released? For example, the earthquake that caused the Indian Ocean tsunamis on Boxing Day 2004 (12/26/04) measured 9 on the Richter scale How much energy was released by this quake? E = 10 (4.8 + 1.5M)
  • 28. The Boxing Day Quake How much energy was released by this quake? E = 10 (4.8 + 1.5M) = 10 (4.8 + 1.5(9)) = 10 (4.8 + 13.5) = 10 (18.3) = 1.99 x 10 18 J For comparison, the average U.S. electric power consumption rate is 3 x 10 12 J/sec