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Plate Tectonics Drifting Continents. Pangaea  The Earth once had a single landmass that broke up into large pieces, which have since drifted apart. This.

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Presentation on theme: "Plate Tectonics Drifting Continents. Pangaea  The Earth once had a single landmass that broke up into large pieces, which have since drifted apart. This."— Presentation transcript:

1 Plate Tectonics Drifting Continents

2 Pangaea  The Earth once had a single landmass that broke up into large pieces, which have since drifted apart. This giant landmass in the past was called Pangaea (pan=all, gaea=land or earth)  The Earth once had a single landmass that broke up into large pieces, which have since drifted apart. This giant landmass in the past was called Pangaea (pan=all, gaea=land or earth)

3 Pangaea

4

5 Alfred Wegener  Alfred Wegener was a German scientist who was able to explain a scientific case to support the Pangaea theory.  He called this theory the Theory of Continental Drift.  Alfred Wegener was a German scientist who was able to explain a scientific case to support the Pangaea theory.  He called this theory the Theory of Continental Drift.

6 Alfred Wegener (1880-1930)

7 Evidence  Evidence to support this theory comes from fossils, the preserved remains of ancient organisms.

8 Evidence  Similar fossils, such as Glossopteris, an ancient plant, have been found in Africa, Australia, India, and Antarctica.  The seeds of this plant could not have traveled the great distance between continents.  Similar fossils, such as Glossopteris, an ancient plant, have been found in Africa, Australia, India, and Antarctica.  The seeds of this plant could not have traveled the great distance between continents.

9 Evidence  This suggests that these places were once closer together.

10 Evidence  Another form of evidence comes from rocks.  Rock formations in Africa line up with matching ones from South America.  Another form of evidence comes from rocks.  Rock formations in Africa line up with matching ones from South America.


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