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Plate Tectonics

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Title: Plate Tectonics


1
Plate Tectonics
  • Chapter 8
  • BHS Earth Science

2
Hollywoods Version
3
Continental Drift
  • Wegeners continental drift hypothesis stated
    that the continents had once been joined to form
    a single supercontinent.
  • Wegener proposed that the supercontinent,
    Pangaea, began to break apart 200 million years
    ago and form the present landmasses.

4
Continental Drift Evidence
  • Jig-Saw Fit
  • Continents fit together like Puzzle pieces
  • Fossil Evidence
  • fossils of same age and species were found in
    connecting bands on different continents
  • Rock Types and Structure
  • Similar bands of rocks types and mountain belts
    connect
  • Ancient Climates
  • PANGAEA!

5
Connecting Mountain Ranges
6
Top 100 Greatest Discovery
7
Rejecting the Hypothesis
  • Most scientists rejected Wegeners ground
    breaking hypothesis because he could not provide
    an explanating of how the plates moved
  • A NEW THEORY EMERGES!

8
Seafloor Spreading
  • In Wegeners theory, continents plowed through
    the sea like bull-dozers.
  • Not the case. Continents are actually connected
    to plates, which move
  • Continents actually move with lithospheric plates
    that are pushed by Mid-Ocean ridges

9
Harry Hess
  • Discovered Mid-Ocean Ridges
  • Spreading centers for tectonic plates
  • Noticed magnetic stripes on the ocean floor which
    proved that new crust was being created at these
    ocean ridges
  • Provided the mechanism for how the plates moved.

10
Top 100 Greatest Discovery
11
Topographic Map of the World
12
Plate Tectonics
  • The theory explaining how the movements of
    earths TECTONIC PLATES or moving plates
    create the geologic events like earthquakes,
    volcanoes and tsunamis.
  • Lithospheric Plates- giant puzzle pieces
    connecting on the surface of earth.
  • These sit on top of mantle so they can move around

13
Plate Boundaries
  • Three types
  • Divergent Boundary
  • Convergent Boundary
  • Transform Boundary

14
Divergent Boundary
  • Plate moving apart
  • Examples
  • Mid Atlantic Ocean Ridge
  • East Pacific Rise
  • Plates are being pushed apart as they are pushed
    apart, magma rises from the mantle and fills the
    void.
  • Mechanism for plate movement

15
Ocean Ridges
  • Oceanic ridges are continuous elevated zones on
    the floor of all major ocean basins. The rifts at
    the crest of ridges represent divergent plate
    boundaries.

16
Rift Valleys
  • Tears in the earth
  • Also caused by Divergent Boundaries

17
Convergent Boundaries
  • Two plates crashing together
  • Collliding
  • Three types
  • Continental to Continental
  • Ocean to Ocean
  • Ocean to Continental

18
Continent to Continent collision
  • When two continents collide, you will get
    mountain ranges
  • Example Himalayans (India crashing into Asia)

19
India and Asia
20
Ocean to Ocean Convergance
  • Two oceanic slab converge together. One is pulled
    under the other
  • Often forms volcanoes on seafloor
  • Volcanic Island Arcs
  • Aleutian Islands
  • Alaska

21
Ocean to Ocean Convergent
  • Aleutian Island, Alaska, US

22
Ocean to Continental Convergance
  • ALSO KNOWN AS SUBDUCTION ZONE
  • Oceanic plate is forced down into the mantle
    beneath a second continental plate
  • Creates volcanoes and deep ocean trenches
  • Examples Andes and Marianna Trench
  • Marianna Trench is deepest place in the WORLD!
    35,000 feet deep!!!!!

23
Subduction Zone
24
Subduction Zne
25
Subduction Zone process
  • Denser ocean slab pulled underneith continent
  • As it is pulled under, the oceanic crust begins
    to melt.
  • When crust begins to melt, magma rises
  • Magma rises to surface and creates volcanoes

26
Transform Boundaries
  • Plates grind past each other without destroying
    or creating new lithosphere
  • Like cars passing each other on a highway
  • Creates tremendous earthquakes
  • Example San Andreas Fault

27
Transform Boundaries
28
How do Plates Move?
  • The crust lies on top of the mantle.
  • It is believed that convection currents cause
    movement in the asthenosphere. Heat rises from
    interior.
  • Areas where the asthenosphere is raising causes
    plates to move apart (diverge) and areas where
    the asthenosphere is sinking causes plates to
    move together (converge).

29
Why do plates move?
  • Clear answer is yet unknown
  • There are theories for Ridge Push, Trench
    Suction, and just plain old Gravity

30
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