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Plate Tectonics part III

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Continental drift early 1900's. Sea-floor spreading early 1960's ... for moving the continents, which the continental drift theory did not satisfy. ... – PowerPoint PPT presentation

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Title: Plate Tectonics part III


1
Plate Tectonics (part III)
2
Plate Tectonics
  • A modern version of an old idea
  • Product of the merging of two earlier ideas
  • Continental drift early 1900s
  • Sea-floor spreading early 1960s
  • Was widely accepted even in other scientific
    fields (i.e. Physics, Biology)

3
  • The problem of ploughing of continental crust
    into oceanic crusting was solved.
  • In plate tectonics, both continental crust and
    oceanic crust can move together.

4
  • There was a mechanism for moving the continents,
    which the continental drift theory did not
    satisfy.

5
  • Most importantly, magnetism, a field of study in
    Physics, was the convincing proof for the plate
    tectonics theory.

6
  • Plate Tectonics provided a mechanism to explain
    the distribution of present-day organisms
  • Modern organisms with similar ancestries had to
    evolve in isolation during the last few tens of
    millions of years
  • Australian marsupials (e.g. Kangaroos) and South
    American marsupial opposums.

7
  • Explains the strange behavior of animals

8
  • Wide acceptance by the scientific community
  • Alfred Wegener was vindicated

9
A triumph of the human mind and spirit !!!
10
Plate Boundaries
Insert picture of plates
11
Plate Boundaries
  • A. Divergent
  • B. Convergent
  • C. Transform-
  • Fault

12
A. Divergent plate
13
B. Convergent plate
  • Oceanic-Continental convergence

14
B. Convergent plate
  • 2. Oceanic-Oceanic convergence

15
B. Convergent plate
  • 3. Continental-Continental convergence

16
C. Transform-Fault
17
Transform-Fault
18
Testing the model
  • Earthquakes along plate boundaries
  • Evidence from ocean drilling
  • Hot spots
  • Direct measurements from Global Positioning
    Systems

19
  • Earthquakes occur in plate margins

20
Shallow, intermediate and deep focus earthquakes
define subduction zones (Benioff Zone)
21
(No Transcript)
22
The pile of sediments get thicker farther away
from the oceanic ridge
23
Hot Spots a concentration of heat in the mantle
capable of producing
magma which, in turn, extrudes onto the Earths
surface
24
Global Positioning Systems (GPS) measured
movement is 1-10 cm per year
Insert picture of GPS
25
The Driving Mechanism?!
Convection cells that move the lithosphere in a
conveyor-like fashion
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