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Wegener
1880-1930




                   earthobservatory.nasa.gov

            Alfred Wegener first proposed the
            theory of continental drift.
 Continental drift was Wegener’s theory
  that all continents had once been joined
  together in a single landmass and have
  drifted apart since.
 Wegener named this supercontinent
  Pangaea.
 Wegener’s theory was rejected by
  scientists because he could not explain
  what force pushes or pulls continents.
                            Continental drift video clip
Fit of Continents
Across the Atlantic

Mountain ranges in
South America line
 up exactly with
 those in Africa!
http://evolution.berkeley.edu/evolibrary/images/history/fossils3.gif




Notice how fossils lined up across continents!
Amazing Facts: Did you know...

...that India was once in the Southern Hemisphere
connected to Antarctica?
...that North America was once surrounded by warm,
tropical seas?
...that Africa was once covered by glaciers, which were
kilometers in thickness?
...that the Sahara desert was once a tropical rain forest?
An example of the proof for changing climate:


                                              At one time,
                                              the area that
                                              is New
                                              Mexico (and
                                              the rest of
                                              the USA was
                                              below the
                                              equator!



As North America has drifted to different latitudes,
changing climates were experienced. This shows the
changes in the state of New Mexico.
He could not find the force that was
 causing the continents to drift.
 Because of this, he could not convince
 anyone that continents could move.
 He died in Greenland on an expedition.
 At the time of his death, no one believed
 his hypothesis!
Technology developed during the 1940’s
changed all that!
Discovery of Sea-Floor Spreading




 Sea floor spreading video clip
Sea-Floor
Spreading
              m.y.
              means
              million
              years ago



            Notice this
            compass. It
            is important
            for the next
            slide
http://platetectonics.pwnet.org/img/blocks.gif




As the sea floor spreads, the lava cools according to the
magnetic poles at the time. The rocks on the ocean
floor have proved that the earth’s magnetic field
sometimes reverses. The inner core flips and so the
north pole moves to the southern hemisphere! The
earth itself does not flip.
What causes sea floor spreading?
     Convection currents!
Click here for a hyperlink to an animation of convection

         Be sure to click the play button!
Animation of sea floor spreading




Can you explain this diagram!?
The place where two plates move
apart or diverge is called a divergent
boundary.
This is a model of sea floor spreading at a divergent
boundary called a mid ocean ridge.
: www.ocean.udel.edu


Did you know that the Earth’s longest mountain range is
underwater and is called the mid-ocean ridge?

 The Mid-Ocean Ridge system, shown above snaking its way
 between the continents, is more than 56,000 kilometers (35,000 mi)
 long. It circles the earth like the stitching on a baseball!
Continental crust diverging from continental
A convergent boundary is where two plates
come together, or converge. The result of the
plates hitting together is called a collision.
A transform boundary is a place where
two plates slip past each other, moving in
opposite directions.
San Andreas Fault in California
en ta l
                           on tin
                            oc
                    ru st t
             t al c           Continen
                                       ta     l c ru s t to
      n en                                                    o c e a n ic
   nti
Co

                Oceanic crust to oceanic
Continental crust to continental crust
collision              Before collision




      India-Asia (Himalayas)                         After collision
                               from: http://www.geo.lsa.umich.edu/~crlb/COURSES/270
Because one plate gets pushed under
  another, it is called subduction. This
  is where volcanoes form!
                                      Oceanic crust
Oceanic crust colliding
                                      colliding with
with continental crust
                                      oceanic crust




                          all from: http://www.geo.lsa.umich.edu/~crlb/COURSES/270
The process by
which the ocean
floor sinks
beneath a deep-
ocean trench
and back into
the mantle is
called
Here is an great link for seeing where each type of
  boundary is located.
  Click here for a great hyperlink! Make sure you
  click on each type of boundary in the key!




Plate tectonics video clip
Worldwide Earthquake patterns help us
know where the edges of plates are located
The Earth’s Plates
Here you see
the two slides
together.
What do you
see?
http://www.livescience.com/images/pangea_animation_03.gif

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Continental drift presentation

  • 1.
  • 2. Wegener 1880-1930 earthobservatory.nasa.gov Alfred Wegener first proposed the theory of continental drift.
  • 3.  Continental drift was Wegener’s theory that all continents had once been joined together in a single landmass and have drifted apart since.  Wegener named this supercontinent Pangaea.  Wegener’s theory was rejected by scientists because he could not explain what force pushes or pulls continents. Continental drift video clip
  • 4.
  • 5. Fit of Continents Across the Atlantic Mountain ranges in South America line up exactly with those in Africa!
  • 7. Amazing Facts: Did you know... ...that India was once in the Southern Hemisphere connected to Antarctica? ...that North America was once surrounded by warm, tropical seas? ...that Africa was once covered by glaciers, which were kilometers in thickness? ...that the Sahara desert was once a tropical rain forest?
  • 8. An example of the proof for changing climate: At one time, the area that is New Mexico (and the rest of the USA was below the equator! As North America has drifted to different latitudes, changing climates were experienced. This shows the changes in the state of New Mexico.
  • 9. He could not find the force that was causing the continents to drift. Because of this, he could not convince anyone that continents could move. He died in Greenland on an expedition. At the time of his death, no one believed his hypothesis! Technology developed during the 1940’s changed all that!
  • 10. Discovery of Sea-Floor Spreading Sea floor spreading video clip
  • 11. Sea-Floor Spreading m.y. means million years ago Notice this compass. It is important for the next slide
  • 12.
  • 13. http://platetectonics.pwnet.org/img/blocks.gif As the sea floor spreads, the lava cools according to the magnetic poles at the time. The rocks on the ocean floor have proved that the earth’s magnetic field sometimes reverses. The inner core flips and so the north pole moves to the southern hemisphere! The earth itself does not flip.
  • 14. What causes sea floor spreading? Convection currents!
  • 15. Click here for a hyperlink to an animation of convection Be sure to click the play button!
  • 16. Animation of sea floor spreading Can you explain this diagram!?
  • 17. The place where two plates move apart or diverge is called a divergent boundary.
  • 18. This is a model of sea floor spreading at a divergent boundary called a mid ocean ridge.
  • 19. : www.ocean.udel.edu Did you know that the Earth’s longest mountain range is underwater and is called the mid-ocean ridge? The Mid-Ocean Ridge system, shown above snaking its way between the continents, is more than 56,000 kilometers (35,000 mi) long. It circles the earth like the stitching on a baseball!
  • 20. Continental crust diverging from continental
  • 21. A convergent boundary is where two plates come together, or converge. The result of the plates hitting together is called a collision.
  • 22. A transform boundary is a place where two plates slip past each other, moving in opposite directions.
  • 23. San Andreas Fault in California
  • 24. en ta l on tin oc ru st t t al c Continen ta l c ru s t to n en o c e a n ic nti Co Oceanic crust to oceanic
  • 25. Continental crust to continental crust collision Before collision India-Asia (Himalayas) After collision from: http://www.geo.lsa.umich.edu/~crlb/COURSES/270
  • 26.
  • 27.
  • 28.
  • 29. Because one plate gets pushed under another, it is called subduction. This is where volcanoes form! Oceanic crust Oceanic crust colliding colliding with with continental crust oceanic crust all from: http://www.geo.lsa.umich.edu/~crlb/COURSES/270
  • 30.
  • 31.
  • 32. The process by which the ocean floor sinks beneath a deep- ocean trench and back into the mantle is called
  • 33. Here is an great link for seeing where each type of boundary is located. Click here for a great hyperlink! Make sure you click on each type of boundary in the key! Plate tectonics video clip
  • 34. Worldwide Earthquake patterns help us know where the edges of plates are located
  • 36. Here you see the two slides together. What do you see?