1.3 Drifting Continents. I. The Theory of Continental Drift A. Alfred Wegener, German scientist...

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1.3 Drifting Continents

Transcript of 1.3 Drifting Continents. I. The Theory of Continental Drift A. Alfred Wegener, German scientist...

Page 1: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

1.3 Drifting Continents1.3 Drifting Continents

Page 2: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

I. The Theory of Continental DriftI. The Theory of Continental Drift A. Alfred Wegener, German scientist

formed a hypothesis on Earth’s continents.

B. Wegener’s hypothesis was that all the continents had once been joined together in a single landmass and have since drifted apart

A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.

B. Wegener’s hypothesis was that all the continents had once been joined together in a single landmass and have since drifted apart

Page 3: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

C. Pangaea = all lands. D. Continental drift - the continents

slowly move over Earth’s surface E. Evidence From Landforms

Mountain ranges in South Africa lined up with a range in South America.

C. Pangaea = all lands. D. Continental drift - the continents

slowly move over Earth’s surface E. Evidence From Landforms

Mountain ranges in South Africa lined up with a range in South America.

Page 4: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

F. Evidence from Fossils -

Fossils are any trace of an ancient organism that has been preserved in rock.

Mesosaurus and Lystrosaurus fossils have been found in Africa and South America.

F. Evidence from Fossils -

Fossils are any trace of an ancient organism that has been preserved in rock.

Mesosaurus and Lystrosaurus fossils have been found in Africa and South America.

Page 5: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

MESOSAURUSMESOSAURUS

Page 6: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

LYSTROSAURUS

LYSTROSAURUS

Page 7: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

GlossopterisGlossopteris

Page 8: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

G. Evidence from Climate:

Glaciers were found in South America, Africa, India, Australia, Antarctica

G. Evidence from Climate:

Glaciers were found in South America, Africa, India, Australia, Antarctica

Page 9: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

How does the location of the continent affect it’s climate?

How does the location of the continent affect it’s climate?

As a continent moves closer to the equator it becomes warmer.

As a continent moves closer to the poles it becomes colder.

As a continent moves closer to the equator it becomes warmer.

As a continent moves closer to the poles it becomes colder.

Page 10: 1.3 Drifting Continents. I. The Theory of Continental Drift  A. Alfred Wegener, German scientist formed a hypothesis on Earth’s continents.  B. Wegener’s.

II. Scientists Reject Wegener’s TheoryII. Scientists Reject Wegener’s Theory Wegener thought that mountains

formed when drifting continents collided, causing their edges to crumple and fold.

Mountains usually occur in narrow bands along the edges of continents, as you would expect if the collision of continents forms mountains.

Wegener thought that mountains formed when drifting continents collided, causing their edges to crumple and fold.

Mountains usually occur in narrow bands along the edges of continents, as you would expect if the collision of continents forms mountains.