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Plate Tectonics

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Chapter 9 Earth s Interior Structure Breakup of Pangaea Evidence of Continental Drift Continental Puzzle Fossil Geological Climate Glacier Evidence Theory of Plate ... – PowerPoint PPT presentation

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Title: Plate Tectonics


1
Chapter 9
2
Earths Interior Structure
3
  • Continental Drift hypothesis
  • Alfred Wegener
  • Supercontinent Pangaea began to break apart 200
    million years ago
  • Continents drifted to where they are today

4
Breakup of Pangaea
5
"Pangea Ultima" is hypothesized to form 250
million years in the Future
6
Continental Drift
7
Evidence of Continental Drift
  • Continental Puzzle
  • Fossil
  • Geological
  • Climate

8
Continental Puzzle
Figure 1 A Curious Fit This map shows the best
fit of South America and Africa at a depth of
about 900 meters. The areas where continents
overlap appear in brown. Inferring Why are there
areas of overlap?
9
Fossil
10
Identical fossil remains of Mesosaurus, a small,
extinct land reptile that lived 270 million years
ago, has been found in both eastern South America
and western Africa. These reptiles could not
have swum across the Atlantic Ocean.
11
Geological
Matching Mountain Ranges
12
Geological
13
Climate
Ancient Glaciers grooves (shown by arrows) in
present day structures)
14
Gondwana Reconstruction of Southern hemisphere
super continent. Notice how ring of glaciers
match the patterns of a polar ice
15
Glacier Evidence
16
  • Theory of Plate Tectonics
  • Earths crust consists of a number of rigid, but
    moving pieces called plates
  • -plates are not defined by continental boundaries

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18
Lithosphere
  • The outer shell of the Earth
  • Made of crust and upper mantle
  • Rigid but broken into plates that move with
    respect to one another

19
Types of Earths Crust
  • Oceanic Crust
  • Made up of material on the ocean floor
  • Continental Crust
  • Made up of continental landmasses

20
Asthenosphere
  • Layer within mantle that lithospheric plates rest
    on
  • Molten

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  • Convection Currents
  • movement of heat through the asthenosphere
  • -causes plates to move

23
Where convection currents are rising
  • New material moves to Earths surface
  • Pushes older material aside
  • Lithospheric plates move apart

24
Where cooler, denser currents are sinking
  • Lithospheric plates are pulled together!

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Plate Boundaries
  • Place where one plate is moving relative to
    another plate

27
Kinds of Plate Boundaries
28
Divergent boundaries
  • lithospheric plates are moving apart
  • Form mid-ocean ridges which have deep valleys
    along entire length called rift valleys
  • Seafloor spreading As plates move apart, molten
    rock rises and fills space between plates cools
    and hardens as new ocean floor

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continental rift when a divergent boundary
occurs in a continental landmass creates rift
valley
Continental rift near Krafla, Iceland
32
East African Rift Valley
33
Transform Fault Boundaries
  • Lithospheric plates are sliding past one another
  • Transform fault break or crack in the Earths
    crust along which movements have occurred

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Example San Andreas Fault
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Convergent Boundaries
  • Lithospheric plates come together
  • There are 3 types.

38
Oceanic-Continental Convergence
  • oceanic plate and continental plate collide
    SUBDUCTION!
  • Ocean plate slides under continental plate
    WHY!?!
  • Forms deep-ocean trenches and continental
    volcanic arcs

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Continental - Continental Convergence
  • Two continental plates collide
  • Become crumpled and uplifted
  • Form mountain ranges

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45
Collision of India and Asia
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OCEANIC-OCEANIC Convergence
  • One plate is subducted, forms trench
  • Subducted plate melts
  • Molten rock rises to surface along trench
  • Forms island chain called an ISLAND ARC
    (VOLCANOES)

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Evidence of Plate Tectonics
  • Paleomagnetism
  • Seafloor Spreading
  • Earthquake Patterns
  • Ocean Drilling
  • Hot Spots

50
? Paleomagnetism rocks formed millions of years
ago show the location of the magnetic poles at
the time of their formation.
  • Normal polaritywhen rocks show the same
    magnetism as the present magnetism field
  • Reverse polaritywhen rocks show the opposite
    magnetism as the present magnetism field

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Paleomagnetism Preserved in Lava Flows
53
Polarity of the Ocean Crust
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Ocean Drilling
  • Confirm seafloor spreading
  • Compare age of sediment to distance from
    mid-ocean ridge

57
Hot Spots
  • Rising plume of mantle pushed towards surface
  • Melts and creates a volcanic area
  • NOT along plate boundary
  • Ex. Hawaiian Islands

58
Lets go to this website and review!
CLICK HEREgtgtgt
http//www.pbs.org/wgbh/aso/tryit/tectonics/
Click on Plate Tectonics Activity (with a yellow
arrow) when you get there!
59
Here it is all in one big picture
Can you pick out the types of Plate Boundaries?
60
Were you right?
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