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Plate Tectonics

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continental drift: the idea that continents move freely over the earth's surface, ... The Early Case for Continental Drift ... Continental breakup caused by a ... – PowerPoint PPT presentation

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Title: Plate Tectonics


1
Plate Tectonics
  • Prepared by Betsy Conklin for
  • Dr. Isiorho

2
Plate Tectonics
  • plate tectonics the idea that the earths
    surface is divided into a few large, thick plates
    that move slowly and change in size
  • continental drift the idea that continents move
    freely over the earths surface, changing their
    positions relative to one another
  • sea-floor spreading a hypothesis that the sea
    floor forms at the crest of the mid-oceanic
    ridge, then moves horizontally away from the
    ridge crest toward an oceanic trench

3
The Early Case for Continental Drift
  • continents can be made to fit together like
    pieces of a picture puzzle
  • Alfred Wegener purposed that the continents were
    originally one giant supercontinent which he
    called Pangaea. Pangaea then split into two parts
    - Laurasia which is now North America and
    Eurasia, and Gondwanaland which is now the
    southern-hemisphere continents and India
  • polar wandering an apparent movement of the
    earths poles
  • the distribution of fossils on various continents

4
Skepticism about Continental Drift
  • fossil plants could have been spread from one
    continent to another by winds or ocean current
  • polar wandering might have been caused by moving
    poles rather than by moving continents

5
Sea-Floor Spreading
  • subduction the sliding of the sea floor beneath
    a continent or island arc
  • convection a circulation pattern driven by the
    rising of hot material and\or the sinking of cold
    material

6
Plates and Plate Motion
  • plate a large, mobile slab of rock that is part
    of the earths surface
  • lithosphere the relatively rigid outer shell of
    the earth of which the plates are a part
  • asthenosphere a zone of low seismic-wave
    velocity that behaves plastically because of
    increased temperature and pressure
  • transform fault the portion of a fracture zone
    between two offset portions of a ridge crest

7
Divergent Plate Boundaries
  • divergent plate boundary a boundary between
    plates that are moving apart

8
Transform Plate Boundaries
  • transform plate boundary a boundary between
    plates that are moving horizontally past one
    another

Transform boundaries between two ridges
Transform boundaries between a ridge and a
trench
Transform boundaries between two trenches
9
Convergent Plate Boundaries
  • convergent plate boundary a boundary between
    plates that are moving toward each other
  • ocean-ocean convergence when two plates capped
    by sea floor converge and one plate subducts
    under the other
  • island arc a curved line of volcanoes that form
    a string of islands parallel to the oceanic trench

10
Convergent Plate Boundaries (cont.)
  • ocean-continent convergence when a plate
    captured by oceanic crust is subducted under the
    continental lithosphere and an accretionary wedge
    and forearc basin form an active continental
    margin between the trench and the continent
  • magmatic arc a broad term used both for island
    arcs at sea and for belts of igneous activity on
    the edges of continents

11
Convergent Plate Boundaries (cont.)
  • continent-continent convergence when two
    continents approach each other an collide

12
What causes Plate Tectonics
  • mid-oceanic ridge crests are hot and elevated,
    while trenches are cold and deep
  • ridge crests have tensional cracks
  • the leading edges of some plates are subducting
    sea floor, while the leading edges of other
    plates are continents (which cannot subduct)

13
Mantle Plumes and Hot Spots
  • mantle plumes narrow columns of hot mantle rock
    that rise through the mantle, much like smoke
    rising from a chimney

Continental breakup caused by a mantle plume. (A)
A dome forms over a mantle plume rising beneath
a continent. (B) Three radial rifts develop due
to outward radial flow from the top of the
mantle plume. (C) Continent separates into two
pieces along two of the three rifts, with new
ocean floor forming between the diverging
continents. The third rift becomes an inactive
failed rift (or aulacogen) filled with
continent sediment.
14
Pictures
  • All pictures used in this power point
    presentation were taken from the following
  • Carlson, Diane H., David McGeary and Charles C.
    Plummer. Physical Geology Updated Eighth
    Edition. New York City, McGraw-Hill Higher
    Education, 2001.
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