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Ch. 17 Sec. 1 Drifting Continents.

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Presentation on theme: "Ch. 17 Sec. 1 Drifting Continents."— Presentation transcript:

1 Ch. 17 Sec. 1 Drifting Continents

2 Early Observers Mapmakers were the first people to consider the idea of moving landmasses in late 1500’s Abraham Ortelius noticed a fit of continents Believed that continents were separated by earthquakes and floods

3 Continental Drift Theory
Proposed by Alfred Wegener Theory proposes that all the continents were once joined together as a single landmass Pangaea, Greek word meaning “all Earth” Broke apart about 200 million years ago Continents look like puzzle pieces

4 Theory Evidence Rock Formations
At separation, large land masses would have broken apart Mountain ranges Noticed that Appalachian Mts. & rocks in Greenland were similar

5 Theory Evidence Fossils
Similar fossils from plants and animals found on different continents 1) Land dwelling animals could not have swam a great distance Kannemeyrid and Labyrinthodont 2) Mesosaurus, which is a fresh water reptile, could not have survived the salt water swim 3) Glossopteris, a fern in tropical weather, is found on lower continents proving that they were once closer together

6 Fossils

7 Theory Evidence Climatic Evidence Coal deposits found on Antarctica
Coal form from dead swap plants from wet and spongy areas Glacial deposits in Africa, India, and Australia

8 Rejected Hypothesis Two Flaws First Second
Scientists did not believe that there couldn’t be enough force to move a continent Second Continents could not push through the ocean floor Crustal rock way to brittle


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