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Evidences of Plate
Movements
Week 8 - Science 10
Objectives
- Describe the possible causes of the plate movement
(S10ES –Iaj-36.5)
- Enumerate the lines of evidence that support plate
movement. (S10ES –Ia-j-36.6)
Kumusta kayo?
Complete This!
It was in 1912 when a German meteorologist named
Alfred Wegener proposed the Continental Drift Theory. In
this theory, he proposed the existence of a single landmass
which he called Pangaea (which means “all land”).
Take note also that the Pangaea is surrounded by an
ocean called Panthalassa. Wegener emphasized that this
landmass broke apart as continents “drift” away from each
other.
Evidences of
Continental Drift Theory
The Jigsaw Fit of the Continents
 Continents are once joined
 Impossible to have a perfect “fit” due to
erosion
 1960s - Edward Bullard come up with a
map that continents fit together by
means of continental shelf
 Other landmasses that were noticed to
fit together are India and Antarctica with
Australia; and Eurasia with North
America.
Continental
Shelf
Continental Shelf
edge of the
continent
beneath the
ocean
Fossil
Evidence
Fossils are
remains of
prehistoric
organisms
preserved in
petrified form,
cast or mold in a
rock
Geologic Fit
Rocks in South America
and Africa are continuous
with one another.
Ages of the rocks in these
continents are similar
Geologic Features
 Fragments of Old Mountains
align perfectly if continents
are positioned together.
 Mountain ranges that line up
along coastlines terminate
and then reappears again on
another landmass.
 Example: Appalachian
Mountains
Paleoclimatic Evidence
 Ancient Climate
 Coal in Antarctica
 Coalfields of the eastern United
States and Europe.
 Layers of similarly aged tillites -
deposits of rock debris from
glaciers.
Look back!
What are the evidences of
Continental Drift Theory
based on the Pictures?
Thank you!

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Evidences of Plate Movements.pptx

  • 2. Objectives - Describe the possible causes of the plate movement (S10ES –Iaj-36.5) - Enumerate the lines of evidence that support plate movement. (S10ES –Ia-j-36.6)
  • 4. Complete This! It was in 1912 when a German meteorologist named Alfred Wegener proposed the Continental Drift Theory. In this theory, he proposed the existence of a single landmass which he called Pangaea (which means “all land”). Take note also that the Pangaea is surrounded by an ocean called Panthalassa. Wegener emphasized that this landmass broke apart as continents “drift” away from each other.
  • 6. The Jigsaw Fit of the Continents  Continents are once joined  Impossible to have a perfect “fit” due to erosion  1960s - Edward Bullard come up with a map that continents fit together by means of continental shelf  Other landmasses that were noticed to fit together are India and Antarctica with Australia; and Eurasia with North America.
  • 7. Continental Shelf Continental Shelf edge of the continent beneath the ocean
  • 9. Geologic Fit Rocks in South America and Africa are continuous with one another. Ages of the rocks in these continents are similar
  • 10. Geologic Features  Fragments of Old Mountains align perfectly if continents are positioned together.  Mountain ranges that line up along coastlines terminate and then reappears again on another landmass.  Example: Appalachian Mountains
  • 11. Paleoclimatic Evidence  Ancient Climate  Coal in Antarctica  Coalfields of the eastern United States and Europe.  Layers of similarly aged tillites - deposits of rock debris from glaciers.
  • 12. Look back! What are the evidences of Continental Drift Theory based on the Pictures?

Editor's Notes

  1. Continental Shelf edge of the continent Beneath the ocean (extension of Continents) – From shore to shelf break to ocean floor. This is called continental