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Introduction to Plate Tectonics Alfred Wegener & Continental Drift

Introduction to Plate Tectonics Alfred Wegener & Continental Drift

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Page 1: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

Introduction to Plate Tectonics

Alfred Wegener

&

Continental Drift

Page 2: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

QOD

• How has Earth’s Surface changed over time?

• What processes change Earth’s Surface?

Page 3: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

Early Thoughts on the Motion of Continents

• 1596 -- Abraham Ortelius a Dutch map-maker in Thesaurus Geographicus.– the Americas were "torn away from Europe

and Africa . . . by earthquakes and floods" – "The vestiges of the rupture reveal

themselves, if someone brings forward a map of the world and considers carefully the coasts of the three [continents].“

Page 4: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

1858-- Antonio Snider-Pellegrini

• Geographer• Maps show his version of how the American and African continents

may once have fit together, then later separated. • Left: The formerly joined continents before their separation. • Right: The continents after the separation. • (Reproductions of the original maps courtesy of University of

California, Berkeley.)

Page 5: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

Continental Drift

• 1912 – the full-blown scientific theory of Continental Drift – Alfred Lothar Wegener -- a

32-year-old German meteorologist

• Studied evidence from all the Earth Sciences

• Proposed the supercontinent Pangaea

– Supporter: Alexander Du Toit, Professor of Geology at Johannesburg University

• Named Laurasia and Gondwanaland

Page 6: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

Activity

You are going to map Wegner’s Evidence

1.Fit of the continents

2.Fossils

3.Climate

4.Rock types and mountain ranges

Answer the questions at the end of the activity for homework tonight.

Page 7: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

QOD

• Describe the orientation of continents 250 million years ago.

• How has the orientation changed?

Page 8: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

•Pangaea -- a supercontinent began to split up 200 million years ago.

•Pangaea first broke into two large continental landmasses

1) Laurasia in the northern hemisphere

2) Gondwanaland in the southern hemisphere.

•Laurasia and Gondwanaland continued to break apart into the various smaller continents that exist today.

Page 9: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

Wegener's Evidence

• fit of the South American and African continents• unusual geologic structures on both continents• plant and animal fossils found on the matching

coastlines of South America and Africa. – it was physically impossible for most of these

organisms to have swum or have been transported across the vast oceans.

– the presence of identical fossil species along the coastal parts of Africa and South America was the most compelling evidence that the two continents were once joined.

Page 10: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

A Explanation for many Observations

• The break-up of Pangaea also explained – the evidence of dramatic climate changes on

some continents. – fossils of tropical plants in coal deposits in

Antarctica– distinctive fossil ferns (Glossopteris)

discovered in now-polar regions– glacial deposits in present-day arid Africa,

such as the Vaal River valley of South Africa.

Page 11: Introduction to Plate Tectonics Alfred Wegener & Continental Drift
Page 12: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

Convincing Others

• The scientific community firmly believed the continents and oceans to be permanent features on the Earth's surface.

• Wegener’s proposal was not well received

Page 13: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

The Fatal Weakness

– There was no explanation for the kind of forces that would be strong enough to move such large masses of solid rock over such great distances.

– Wegener -- continents plowed through the ocean floor

– Harold Jeffreys, a noted English geophysicist, disagreed:

• it was physically impossible for a large mass of solid rock to plow through the ocean floor without breaking up.

Page 14: Introduction to Plate Tectonics Alfred Wegener & Continental Drift

Wegener’s Death

• He devoted the rest of his life to find additional evidence to defend his theory.

• He froze to death in 1930 during an expedition crossing the Greenland ice cap

• After his death, new evidence from ocean floor exploration and other studies rekindled interest in Wegener's theory, ultimately leading to the development of the theory of plate tectonics.