Title: Plate Tectonics
1Plate Tectonics
- Prepared by Betsy Conklin for
- Dr. Isiorho
2Plate 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
3The 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
4Skepticism 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
5Sea-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
6Plates 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
7Divergent Plate Boundaries
- divergent plate boundary a boundary between
plates that are moving apart
8Transform 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
9Convergent 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
10Convergent 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
11Convergent Plate Boundaries (cont.)
- continent-continent convergence when two
continents approach each other an collide
12What 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)
13Mantle 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.
14Pictures
- 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.