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CONTINENTAL DRIFT. Alfred L. Wegener  Geologist and meteorologist Alfred Wegener noticed similar rocks & fossil remains were found on continents which.

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Presentation on theme: "CONTINENTAL DRIFT. Alfred L. Wegener  Geologist and meteorologist Alfred Wegener noticed similar rocks & fossil remains were found on continents which."— Presentation transcript:

1 CONTINENTAL DRIFT

2 Alfred L. Wegener  Geologist and meteorologist Alfred Wegener noticed similar rocks & fossil remains were found on continents which seemed to fit together  He hypothesized there was once a super continent he named Pangaea  In 1912 Wegener published the first version & died defending his theory  Geologist and meteorologist Alfred Wegener noticed similar rocks & fossil remains were found on continents which seemed to fit together  He hypothesized there was once a super continent he named Pangaea  In 1912 Wegener published the first version & died defending his theory

3 Support for Continental Drift  Wegener was not the first one to notice the fit of the continents.  1500s: Cartographer Abraham Ortelius depicted Africa and South America connected.  Wegener was, however, the first to include other evidence to support his hypothesis.  Wegener was not the first one to notice the fit of the continents.  1500s: Cartographer Abraham Ortelius depicted Africa and South America connected.  Wegener was, however, the first to include other evidence to support his hypothesis.

4 Support for Continental Drift 1. SHAPE OF THE CONTINENTS Continents fit together like puzzle pieces 1. SHAPE OF THE CONTINENTS Continents fit together like puzzle pieces

5 Mesosaurus was incapable of swimming across a large ocean. 2. FOSSIL EVIDENCE SAME FOSSILS: DIFFERENT CONTINENTS Support for Continental Drift

6 3. ROCK EVIDENCE – Mountain ranges Support for Continental Drift  SAME ROCK: DIFFERENT RANGE Existing mountain ranges separated by vast oceans contain rocks of identical mineral content.  A prime example are the Appalachian Mountains in the eastern U.S and the Caledonian Mountains in the British Isles.  SAME ROCK: DIFFERENT RANGE Existing mountain ranges separated by vast oceans contain rocks of identical mineral content.  A prime example are the Appalachian Mountains in the eastern U.S and the Caledonian Mountains in the British Isles.

7 SAME SCARS: DIFFERENT CONTINENTS Support for Continental Drift 4. GLACIAL SCARS

8 5. LOCATION OF COAL DEPOSITS Coal deposits have been found in temperate and polar regions; however, coal is only formed in tropical climates. Support for Continental Drift

9 PANGAEA the large landmass that included all of Earth’s present day continents http://www.youtube.com/watch?v=uGcDed4xVD4

10 CONTINENTAL DRIFT IN DOUBT Why didn’t people accept continental drift?  People couldn’t imagine that the Earth could have looked so different millions of years ago  People didn’t know of a force great enough to move the continents  People couldn’t understand how the continents could move through a solid seafloor Why didn’t people accept continental drift?  People couldn’t imagine that the Earth could have looked so different millions of years ago  People didn’t know of a force great enough to move the continents  People couldn’t understand how the continents could move through a solid seafloor

11 Misconceptions of the Seafloor 1.Flat 2.Unchanging 3.Older than continental crust 1.Flat 2.Unchanging 3.Older than continental crust  Not until technological advancements from WWII were these misconceptions shown to be false

12 Mapping the Ocean Floor  Advancements in sonar allowed scientists to make topographic maps of the ocean floor.  What they found were massive underwater mountain chains complemented by deep canyons.

13 Radiometric Dating  Analysis of ocean rocks showed that the ocean floor is younger near the ridges and older by the deep-sea trenches.

14 Magnetic Reversal  Our magnetic field changes depending on the direction of convection currents in the liquid outer core.  A magnetometer is able to detect the polarity of the rock.  Our magnetic field changes depending on the direction of convection currents in the liquid outer core.  A magnetometer is able to detect the polarity of the rock.

15 Seafloor Spreading  These advancements led to the Seafloor Spreading theory – explains how new ocean floor is created at ocean ridges and destroyed at deep-sea trenches.

16 But, I’m pretty sure this is how it really happened…  http://www.youtube.com/watch?v= TzzGPfVx32M http://www.youtube.com/watch?v= TzzGPfVx32M  http://www.youtube.com/watch?v= TzzGPfVx32M http://www.youtube.com/watch?v= TzzGPfVx32M


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