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Inside Earth: Chapter 1- Plate Tectonics Section 3: Drifting Continents

Inside Earth: Chapter 1- Plate Tectonics

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Inside Earth: Chapter 1- Plate Tectonics. Section 3: Drifting Continents. Guide For Reading. What is continental drift? Why was Alfred Wegener’s theory rejected?. The Theory of Continental Drift. Pangaea. - PowerPoint PPT Presentation

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Page 1: Inside Earth: Chapter 1- Plate Tectonics

Inside Earth: Chapter 1- Plate Tectonics

Section 3: Drifting Continents

Page 2: Inside Earth: Chapter 1- Plate Tectonics

Guide For Reading

• What is continental drift?

• Why was Alfred Wegener’s theory rejected?

Page 3: Inside Earth: Chapter 1- Plate Tectonics

The Theory of Continental Drift

Page 4: Inside Earth: Chapter 1- Plate Tectonics

Pangaea• The name of the single landmass

that broke apart 200 million years ago and gave the rise to today’s continents

Page 5: Inside Earth: Chapter 1- Plate Tectonics

Continental Drift• A hypothesis that the continents

slowly move across Earth’s surface

Page 6: Inside Earth: Chapter 1- Plate Tectonics

Guide For Reading: What is Wegener’s theory of continental drift? • Continental drift is the hypothesis

that all the continents had once been joined together in a single landmass

• The continents have slowly moved apart over Earth’s surface

Page 7: Inside Earth: Chapter 1- Plate Tectonics

Evidence From Landforms

Page 8: Inside Earth: Chapter 1- Plate Tectonics

Evidence From Landforms• A mountain range in South Africa

lines up identical with mountain ranges in Argentina (South America)

• Brazilian coal fields match up identical with coal fields in South Africa

Page 9: Inside Earth: Chapter 1- Plate Tectonics

Figure 11: Observing: Which coastlines seem to match up like jig-saw puzzle?

• The continents of Africa and South America best match up like jigsaw-puzzle pieces

Page 10: Inside Earth: Chapter 1- Plate Tectonics

Figure 12: Inferring: According to Wegener’s theory, what does the presence of similar mountain ranges in Africa and South America indicate?

• The presence of similar mountain ranges indicates that Africa and South America were once joined.

Page 11: Inside Earth: Chapter 1- Plate Tectonics

Evidence From Fossils

Page 12: Inside Earth: Chapter 1- Plate Tectonics

Fossil• Fossil: A trace of an organism that

has been preserved in rock

Page 13: Inside Earth: Chapter 1- Plate Tectonics

How did Wegener use evidence based on fossils to support his theory that the continents had moved?

• Glossopteris fossils have been found in rocks in Africa, South America, Australia, India, and Antarctica unexpectedly

• Seeds could not have travel that far over the oceans to reach other continents

Page 14: Inside Earth: Chapter 1- Plate Tectonics

Evidence From Climate

Page 15: Inside Earth: Chapter 1- Plate Tectonics

What two examples of climate change did Wegener use to support his theory of continental drift? • The Island of Spitsbergen (Artic

Ocean) has evidence of tropical plants

• Deep scratches in rocks were found in South Africa

• These scratches support evidence of glaciers

Page 16: Inside Earth: Chapter 1- Plate Tectonics

Checkpoint: What were the three types of evidence Wegner used to support his theory of continental drift?

• Landforms

• Fossils

• Climate

Page 17: Inside Earth: Chapter 1- Plate Tectonics

Scientists Reject Wegener’s Theory

Page 18: Inside Earth: Chapter 1- Plate Tectonics

Guide For Reading: Why was Alfred Wegener’s theory rejected?

• Wegener could not provide a satisfactory explanation for the force that pushes or pulls the continents

• He could not identify the cause of continental drift

• Geologists needed more evidence of how the continents and mountains were formed