XIV. Plate Tectonics

A. History
  1. Continental Drift
    1. Wegener (1915)
    2. Pangaea (fig. 15.2)
    3. evidence (fig. 15.3, 15.4, 15.6, 15.7)
  2. Sea Floor spreading
    1. seafloor data from WWII
    2. mid-ocean ridge volcanoes
  3. Plate Tectonics
    1. added data from Pacific Ocean
    2. 3 types of plate boundaries (fig. 15.9)
B. Divergent Boundaries (fig. 15.10)
plates move away from each other 

  1. oceanic spreading centers
    1. create new oceanic crust
    2. surface expression - mid-ocean ridges
    3. volcanism: (fig. 16.13)
      • basalt volcanoes,
      • lava flows,
      • mafic dikes
    4. earthquakes:
      • shallow to intermediate earthquakes;
      • small to medium magnitude
      • modern examples: mid-Atlantic ridge, Iceland
  2. continental rifts (fig. 15.11)
    1. break-up continent, earliest stages of ocean formation (fig. 16.15)
    2. surface expression: rift valley and volcanoes
    3. volcanoes:
      • basalt volcanoes,
      • lava flows
    4. earthquakes:
      • shallow to intermediate earthquakes;
      • small to medium magnitude 
    5. modern example: Rio Grande Rift, East African Rift
C. Convergent Boundaries

plates move toward each other

  1. subduction zones -  requires involvement of at least one ocean plate (fig. 15.14, 15.15)
    1. destroy ocean crust
    2. surface expression:
      • trench,
      • island arc or volcanic arc 
    3. volcanoes:
      • explosive composite volcanoes
    4. earthquakes:
      • Benioff zone;
      • small to huge earthquakes,
      • shallow to very deep (700 km)
    5. modern examples: Japan, Philippines, Aleutians, Andes, S. Mexico, Mt. St. Helens
  2. continental collisions:  (fig. 15.14, 15.15)
    1. suture continents together, also folding, faulting and metamorphism
    2. surface expression: forms huge mountains
    3. volcanoes: none
    4. earthquakes: variable in depth and size
    5. modern example: Himalayas
D. Transform (fig. 15.16)
 plates slide side-by-side

  1. neither create nor destroy crust
  2. surface expression: fault which is often hard to identify, subtle landscape variations
  3. volcanoes: none
  4. earthquakes: variable in depth and magnitude
  5. modern example: San Andreas Fault
E. Driving Mechanisms
  1. convection  (fig. 15.27)
  2. slab-pull, ridge-push (fig. 15.26)
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