GEOG 100--Lecture 12--Plate Tectonics

1,415 views
1,313 views

Published on

Published in: Education
0 Comments
2 Likes
Statistics
Notes
  • Be the first to comment

No Downloads
Views
Total views
1,415
On SlideShare
0
From Embeds
0
Number of Embeds
254
Actions
Shares
0
Downloads
0
Comments
0
Likes
2
Embeds 0
No embeds

No notes for slide
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • \n
  • GEOG 100--Lecture 12--Plate Tectonics

    1. 1. Plate Tectonics Chapter 9
    2. 2. Rigid Earth Theory
    3. 3. Rigid Earth Theory• It was once believed that Earth’s crust was hard and brittle and could not bend
    4. 4. Rigid Earth Theory• It was once believed that Earth’s crust was hard and brittle and could not bend
    5. 5. Rigid Earth Theory• It was once believed that Earth’s crust was hard and brittle and could not bend• Plasticity
    6. 6. Rigid Earth Theory• It was once believed that Earth’s crust was hard and brittle and could not bend• Plasticity – We now know that Earth’s crust can bend (like a tough plastic) before breaking
    7. 7. Isostacy• “The maintenance of hydrostatic equilibrium in the crust” – hydrostatics—branch of physics related to the pressure and equilibrium of liquids (hydro) • statics—bodies not active; at rest; in equilibrium; as opposed to dynamics
    8. 8. Isostacy
    9. 9. Isostacy• Addition or removal of crustal material causes a sinking or rebounding of crust
    10. 10. Isostacy• Addition or removal of crustal material causes a sinking or rebounding of crust – Add or remove continental mass and the crust will sink or rise to accommodate the added/removed weight
    11. 11. Isostacy• Addition or removal of crustal material causes a sinking or rebounding of crust – Add or remove continental mass and the crust will sink or rise to accommodate the added/removed weight • a glacier growing or remelting, crust eroding off the surface, sediment deposits, water bodies on land, esp. those created by dams
    12. 12. Alfred Wegener andHis Continental Drift Theory
    13. 13. Alfred Wegener and His Continental Drift Theory• German meteorologist, 1920s “The present continents were originally connected as one enormous landmass that has broken up and drifted apart over the last few 100 million years. The drifting continues….”
    14. 14. Alfred Wegener and His Continental Drift Theory• German meteorologist, 1920s “The present continents were originally connected as one enormous landmass that has broken up and drifted apart over the last few 100 million years. The drifting continues….”• Pangaea (Gk. “whole land”)
    15. 15. Alfred Wegener and His Continental Drift Theory• German meteorologist, 1920s “The present continents were originally connected as one enormous landmass that has broken up and drifted apart over the last few 100 million years. The drifting continues….”• Pangaea (Gk. “whole land”)
    16. 16. Wegener’s Lines of Evidence
    17. 17. Wegener’s Lines of Evidence• Similar geology (rocks and rock structures)…
    18. 18. Wegener’s Lines of Evidence• Similar geology (rocks and rock structures)…• …petrology (rock chemistry),
    19. 19. Wegener’s Lines of Evidence• Similar geology (rocks and rock structures)…• …petrology (rock chemistry),• …paleontology (fossilized plants and animals),
    20. 20. Wegener’s Lines of Evidence• Similar geology (rocks and rock structures)…• …petrology (rock chemistry),• …paleontology (fossilized plants and animals),• …matching glacial features (U-shaped valleys, glacial deposits, etc.) on continents separated by oceans
    21. 21. Wegener’s Lines of Evidence• Similar geology (rocks and rock structures)…• …petrology (rock chemistry),• …paleontology (fossilized plants and animals),• …matching glacial features (U-shaped valleys, glacial deposits, etc.) on continents separated by oceans• …continent shapes that seem to fit together,
    22. 22. Wegener’s Lines of Evidence• Similar geology (rocks and rock structures)…• …petrology (rock chemistry),• …paleontology (fossilized plants and animals),• …matching glacial features (U-shaped valleys, glacial deposits, etc.) on continents separated by oceans• …continent shapes that seem to fit together,• …patterns in the locations of volcanoes
    23. 23. Wegener’s Lines of Evidence• Similar geology (rocks and rock structures)…• …petrology (rock chemistry),• …paleontology (fossilized plants and animals),• …matching glacial features (U-shaped valleys, glacial deposits, etc.) on continents separated by oceans• …continent shapes that seem to fit together,• …patterns in the locations of volcanoes
    24. 24. Wegener’s Lines of Evidence• Similar geology (rocks and rock structures)…• …petrology (rock chemistry),• …paleontology (fossilized plants and animals),• …matching glacial features (U-shaped valleys, glacial deposits, etc.) on continents separated by oceans• …continent shapes that seem to fit together,• …patterns in the locations of volcanoesEx.: S. America/Africa, Madagascar/India, Australia/Antarctica
    25. 25. …but no one bought it.
    26. 26. …but no one bought it. Thecrust is too rigid!
    27. 27. …but no one bought it. The So why don’t wecrust is see the crust too ripping apart rigid! right now?
    28. 28. …but no one bought it. The So why don’t wecrust is see the crust too ripping apart rigid! right now? What do you mean, “Thecontinents are floating???”
    29. 29. …but no one bought it. The So why don’t wecrust is see the crust too ripping apart rigid! right now? And hey, what’s the What do you power source driving mean, “The these movements of allcontinents are the land masses, floating???” anyway???
    30. 30. …but no one bought it. The So why don’t wecrust is see the crust too ripping apart rigid! right now? And hey, what’s the What do you power source driving mean, “The these movements of allcontinents are the land masses, floating???” anyway??? What a knucklehead.
    31. 31. Then along came OceanographerHarry Hess in the 1960s…
    32. 32. Then along came OceanographerHarry Hess in the 1960s…
    33. 33. The evidence continued to mount…
    34. 34. The evidence continued to mount…• Military seafloor mapping: Seafloor geology— structure, chemistry, and age
    35. 35. The evidence continued to mount…• Military seafloor mapping: Seafloor geology— structure, chemistry, and age – Oceanic crust: only 100 m.y.o
    36. 36. The evidence continued to mount…• Military seafloor mapping: Seafloor geology— structure, chemistry, and age – Oceanic crust: only 100 m.y.o – Continental crust: 4.1 b.y.o.
    37. 37. The evidence continued to mount…• Military seafloor mapping: Seafloor geology— structure, chemistry, and age – Oceanic crust: only 100 m.y.o – Continental crust: 4.1 b.y.o.• Core sampling
    38. 38. The evidence continued to mount…• Military seafloor mapping: Seafloor geology— structure, chemistry, and age – Oceanic crust: only 100 m.y.o – Continental crust: 4.1 b.y.o.• Core sampling• Seafloor sediment
    39. 39. The evidence continued to mount…• Military seafloor mapping: Seafloor geology— structure, chemistry, and age – Oceanic crust: only 100 m.y.o – Continental crust: 4.1 b.y.o.• Core sampling• Seafloor sediment• Rigid Earth folks retired—paradigm shift to plasticity
    40. 40. The evidence continued to mount…• Military seafloor mapping: Seafloor geology— structure, chemistry, and age – Oceanic crust: only 100 m.y.o – Continental crust: 4.1 b.y.o.• Core sampling• Seafloor sediment• Rigid Earth folks retired—paradigm shift to plasticity• Convection currents as mechanism/power source
    41. 41. The evidence continued to mount…• Military seafloor mapping: Seafloor geology— structure, chemistry, and age – Oceanic crust: only 100 m.y.o – Continental crust: 4.1 b.y.o.• Core sampling• Seafloor sediment• Rigid Earth folks retired—paradigm shift to plasticity• Convection currents as mechanism/power source• Geologists, geophysicists, seismologists, oceanographers, physicists, and paleontologists all agree the theory fits the evidence gathered within their respective fields
    42. 42. The Theory of Plate TectonicsTectonic (crustal) plates• Pulling apart (spreading/diverging)• Slamming together and sinking (subducting/converging)• Sliding laterally (sideways)
    43. 43. Divergent Plate Boundaries• Spreading centers – Crust pulling apart, magma rising to the surface
    44. 44. Convergent Plate Boundaries
    45. 45. Convergent Plate Boundaries• Subduction zones
    46. 46. Convergent Plate Boundaries• Subduction zones – Crust being forced together
    47. 47. Convergent Plate Boundaries• Subduction zones – Crust being forced together – Lightest material rises (mountain-building) while the heaviest stuff sinks (pushed back into the mantle)
    48. 48. Convergent Plate Boundaries• Subduction zones – Crust being forced together – Lightest material rises (mountain-building) while the heaviest stuff sinks (pushed back into the mantle) – Remelting (mostly from friction) creates volcanoes
    49. 49. Convergent Plate Boundaries• Subduction zones – Crust being forced together – Lightest material rises (mountain-building) while the heaviest stuff sinks (pushed back into the mantle) – Remelting (mostly from friction) creates volcanoes – Intense, deep-focus earthquakes
    50. 50. Three Types of Subduction Zones
    51. 51. Three Types of Subduction Zones1. Continental crust meets oceanic crust
    52. 52. Three Types of Subduction Zones1. Continental crust meets oceanic crust – Oceanic crust sinks
    53. 53. Three Types of Subduction Zones1. Continental crust meets oceanic crust – Oceanic crust sinks – Big trench offshore
    54. 54. Three Types of Subduction Zones1. Continental crust meets oceanic crust – Oceanic crust sinks – Big trench offshore – Volcanoes on the continental margin
    55. 55. Three Types of Subduction Zones1. Continental crust meets oceanic crust – Oceanic crust sinks – Big trench offshore – Volcanoes on the continental margin – Big earthquakes (potential for tsunamis)
    56. 56. Continental-Oceanic Subduction
    57. 57. Three Types of Subduction Zones
    58. 58. Three Types of Subduction Zones2. Oceanic crust meets oceanic crust
    59. 59. Three Types of Subduction Zones2. Oceanic crust meets oceanic crust – The older and colder crust will probably sink
    60. 60. Three Types of Subduction Zones2. Oceanic crust meets oceanic crust – The older and colder crust will probably sink – Big earthquakes and volcanic islands (called “island arcs”)
    61. 61. Three Types of Subduction Zones2. Oceanic crust meets oceanic crust – The older and colder crust will probably sink – Big earthquakes and volcanic islands (called “island arcs”) – Deep ocean trench
    62. 62. Three Types of Subduction Zones2. Oceanic crust meets oceanic crust – The older and colder crust will probably sink – Big earthquakes and volcanic islands (called “island arcs”) – Deep ocean trench – Potential for tsunamis
    63. 63. Oceanic-Oceanic Subduction
    64. 64. Three Types of Subduction Zones
    65. 65. Three Types of Subduction Zones3. Continental crust meets continental crust
    66. 66. Three Types of Subduction Zones3. Continental crust meets continental crust – Too light to subduct
    67. 67. Three Types of Subduction Zones3. Continental crust meets continental crust – Too light to subduct – Mountain-building
    68. 68. Three Types of Subduction Zones3. Continental crust meets continental crust – Too light to subduct – Mountain-building – Big earthquakes
    69. 69. Three Types of Subduction Zones3. Continental crust meets continental crust – Too light to subduct – Mountain-building – Big earthquakes – Little if any volcanism (mostly intrusive)
    70. 70. Continental-Continental Subduction
    71. 71. Transform Fault Boundaries
    72. 72. Transform Fault Boundaries• Tectonic plates slide past one another
    73. 73. Transform Fault Boundaries• Tectonic plates slide past one another – Earthquakes are less intense than subduction
    74. 74. Transform Fault Boundaries• Tectonic plates slide past one another – Earthquakes are less intense than subduction – No volcanoes
    75. 75. Transform Fault Boundaries• Tectonic plates slide past one another – Earthquakes are less intense than subduction – No volcanoes – Little or no mountain-building
    76. 76. “Hot spots”
    77. 77. “Hot spots”• Also called magma plumes
    78. 78. “Hot spots”• Also called magma plumes• Generally occur some distance from any other type of plate boundary
    79. 79. “Hot spots”• Also called magma plumes• Generally occur some distance from any other type of plate boundary• Unrelated to convergent, divergent, or transform boundaries
    80. 80. “Hot spots”• Also called magma plumes• Generally occur some distance from any other type of plate boundary• Unrelated to convergent, divergent, or transform boundaries• Anomalous (odd) “balloons” of rising magma
    81. 81. “Hot spots”• Also called magma plumes• Generally occur some distance from any other type of plate boundary• Unrelated to convergent, divergent, or transform boundaries• Anomalous (odd) “balloons” of rising magma – Hot spot stays in one position as the moving, island-covered crustal plate rides away from it
    82. 82. Accreted Terranes• A moving continent may pick up new land material as lighter (felsic) material scrapes off of a subducting plate
    83. 83. Accreted Terranes• A moving continent may pick up new land material as lighter (felsic) material scrapes off of a subducting plate
    84. 84. Craton• These terranes were added to the original material first formed from magma that rose out of Earth’s earliest crust – Craton--the name given to these ancient proto- continents cratons 29
    85. 85. Continental Shields• More magma material was added to the cratons, forming continents. – Continental shields: Where the earliest continental material still exists intact and is exposed at the surface. 30
    86. 86. 31
    87. 87. Topography• Right from the very beginning, the crust was affected by stresses and strains that caused crustal deformations• Over time, the crust has continued to be folded, faulted, broken, eroded and further built upon, creating the topography, the ups and downs of land relief, that we see today 32

    ×