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lecture11

Table of Contents

  1. Deformation of Rocks
  2. Why study rock deformation?
  3. Why study rock deformation?
  4. Why study rock deformation?
  5. Why study rock deformation?
  6. Why study rock deformation?
  7. Why study rock deformation?
  8. Why study rock deformation?
  9. Why study rock deformation?
  10. Why study rock deformation?
  11. Why study rock deformation?
  12. Why study rock deformation?
  13. Why study rock deformation?
  14. Why study rock deformation?
  15. Why study rock deformation?
  16. 11.1 What do deformed rocks look like?
  17. 11.1 What do deformed rocks look like?
  18. 11.1 What do deformed rocks look like?
  19. 11.1 What do deformed rocks look like?
  20. 11.1 What do deformed rocks look like?
  21. 11.1 What do deformed rocks look like?
  22. 11.1 What do deformed rocks look like?
  23. 11.1 What do deformed rocks look like?
  24. 11.1 What do deformed rocks look like?
  25. 11.1 What do deformed rocks look like?
  26. 11.1 What do deformed rocks look like?
  27. 11.1 What do deformed rocks look like?
  28. 11.1 What do deformed rocks look like?
  29. 11.1 What do deformed rocks look like?
  30. 11.1 What do deformed rocks look like?
  31. 11.1 What do deformed rocks look like?
  32. 11.1 What do deformed rocks look like?
  33. 11.1 What do deformed rocks look like?
  34. 11.2 How are resources related to geologic structures?
  35. 11.2 How are resources related to geologic structures?
  36. 11.2 How are resources related to geologic structures?
  37. 11.2 How are resources related to geologic structures?
  38. 11.3 Why do rocks deform?
  39. 11.3 Why do rocks deform?
  40. 11.3 Why do rocks deform?
  41. 11.3 Why do rocks deform?
  42. 11.3 Why do rocks deform?
  43. 11.4 How do we know ... why some rocks break and others flow?
  44. 11.4 How do we know ... why some rocks break and others flow?
  45. 11.4 How do we know ... why some rocks break and others flow?
  46. 11.4 How do we know ... why some rocks break and others flow?
  47. 11.4 How do we know ... why some rocks break and others flow?
  48. 11.4 How do we know ... why some rocks break and others flow?
  49. 11.4 How do we know ... why some rocks break and others flow?
  50. 11.5 How do geologic structures relate to stress, strain, and strength?
  51. 11.5 How do geologic structures relate to stress, strain, and strength?
  52. 11.5 How do geologic structures relate to stress, strain, and strength?
  53. 11.5 How do geologic structures relate to stress, strain, and strength?
  54. 11.5 How do geologic structures relate to stress, strain, and strength?
  55. 11.5 How do geologic structures relate to stress, strain, and strength?
  56. 11.5 How do geologic structures relate to stress, strain, and strength?
  57. 11.5 How do geologic structures relate to stress, strain, and strength?
  58. 11.5 How do geologic structures relate to stress, strain, and strength?
  59. 11.6 How does strength vary in the lithosphere?
  60. 11.6 How does strength vary in the lithosphere?
  61. 11.6 How does strength vary in the lithosphere?
  62. 11.7 How do earthquakes relate to rock deformation?
  63. 11.7 How do earthquakes relate to rock deformation?
  64. 11.7 How do earthquakes relate to rock deformation?
  65. 11.7 How do earthquakes relate to rock deformation?
  66. Elastic Rebound
  67. 11.7 How do earthquakes relate to rock deformation?
  68. 11.7 How do earthquakes relate to rock deformation?
  69. 11.7 How do earthquakes relate to rock deformation?
  70. 11.8 How are earthquakes measured?
  71. 11.8 How are earthquakes measured?
  72. 11.8 How are earthquakes measured?
  73. 11.8 How are earthquakes measured?
  74. 11.8 How are earthquakes measured?
  75. 11.8 How are earthquakes measured?
  76. 11.8 How are earthquakes measured?
  77. 11.8 How are earthquakes measured?
  78. 11.8 How are earthquakes measured?
  79. 11.9 Why are earthquakes destructive?
  80. 11.9 Why are earthquakes destructive?
  81. 11.9 Why are earthquakes destructive?
  82. 11.9 Why are earthquakes destructive?
  83. 11.9 Why are earthquakes destructive?
  84. 11.9 Why are earthquakes destructive?
  85. 11.9 Why are earthquakes destructive?
  86. 11.9 Why are earthquakes destructive?
  87. 11.9 Why are earthquakes destructive?
  88. 11.9 Why are earthquakes destructive?
  89. 11.9 Why are earthquakes destructive?

Text and Images from Slide

Image shows 1 meter offseet of highway pavement in southern California during the movement on a strike-slip fault in 1992

3 meter high scrap in central Idaho occured during movement on a normal dip-slip fault in 1983.

Fig 11.28

11.7 How do earthquakes relate to rock deformation?

Motion along faults: Note the displacement in the highway (left) of a right-lateral strike-slip fault (the farther block moved to the right relative to the closer one), and the fault scarp (right) on the footwall of a normal dip-slip fault.

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