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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

11.9 Why are earthquakes destructive?

Images to show how damage is greatest when liquefaction occurs during shaking.

The underlying material greatly affects susceptibility of an area to ground shaking damage.

Saturated sediments undergo liquefaction (becoming fluidic) during the shaking event.

Fig 11.38

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