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Plate Tectonics

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... the older the rocks were. The oldest rocks are about 4 million years old. The newer rocks were always in the center of the ridges Evidence Magnetic Stripes. – PowerPoint PPT presentation

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Title: Plate Tectonics


1
Plate Tectonics

2
Theory of Plate Tectonics
  • Meaning plate structure
  • Developed 1960s
  • Explains the movement of Earths plates, causes
    of volcanoes, earthquakes, ocean trenches,
    mountain formation, and other geological
    phenomena.

3
  • Plates move about 1-10 cm per year!!!
  • Seismic activity (volcanoes and earthquakes)
    occur as plate boundaries interact.

4
Plate Boundaries
  • There are 3 types of plate boundaries
  • Divergent
  • Convergent
  • Transform

5
Divergent movement of 2 plates away from
each other
6
Convergent colliding of 2 plates
7
Transform plates sliding horizontally past each
other.
8
Earths Major Plates
  • Eurasian Caribbean
  • Australian-Indian South American
  • Pacific African
  • Juan de Fuca Antarctic
  • North American

9
Earths Major Plates
10
Crust
  • Oceanic thin, under ocean crust is thin and not
    very dense, active
  • Continental thick, under land, constantly
    created and destroyed.

11
  • http//www2.wwnorton.com/college/geo/egeo/animatio
    ns/ch2.htm

12
Sea- floor Spreading
  • The longest chain of mountains in the world is
    the Mid-Ocean Ridge.
  • Scientists have mapped the ocean floor and
    mid-ocean ridge using S.O.N.A.R.
  • The mid-ocean ridge extends into all of Earths
    oceans.
  • The Island of Iceland is part of the ridge that
    rises above the surface in the Atlantic Ocean.
  • Down the middle of the ridge is an area called
    the rift valley It is almost twice as deep as
    the Grand Canyon

13
Harry Hess
  • Harry Hess examined maps of the mid-ocean ridge
    and proposed that the ocean floors move like
    conveyor belts, carrying the continents along
    with them.
  • This movement begins at the Mid- Ocean Ridge.
  • At the ridge, the molten material rises from the
    mantle and erupts (much like a volcano).
  • The oldest rock is farthest from the center of
    the ridge.
  • Harry Hess first proposed the idea of Sea-Floor
    Spreading.

14
Evidence for Sea-Floor Spreading
  • Molten Material. The submersible ALVIN was sent
    down to study the rift valley.

15
Evidence
  • Rock Sampling. The Glomar Challenger was a
    drilling ship the gathered samples from the ocean
    floor.
  • The scientists determined the age- of the rocks
    in the samples and found that the farther-away
    from the ridge, the older the rocks were.
  • The oldest rocks are about 4 million years old.
  • The newer rocks were always in the center of the
    ridges

16
Evidence
  • Magnetic Stripes. How does the pattern of
    matching stripes show evidence of sea-floor
    spreading?

17
How does the ocean floor keep getting wider
  • The ocean floor plunges into deep under water
    trenches.
  • A deep ocean trench forms where the oceanic crust
    collides with continental crust.
  • Subduction is the process by which the ocean
    floor sinks beneath a deep-ocean trench and back
    into the mantle.

18
FYI
  • Most ocean trenches are found in the Pacific
    Ocean.
  • The deepest part of the ocean is the Mariannas
    Deep. It is located in the Pacific Ocean
  • The Pacific Ocean is shrinking, but it is still
    the Largest ocean
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