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Objective 5 October 2012 Describe the theory of continental drift.

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Presentation on theme: "Objective 5 October 2012 Describe the theory of continental drift."— Presentation transcript:

1 Objective 5 October 2012 Describe the theory of continental drift. Intro Did the Earth always look like this?

2 Continental Drift

3 Who? What? Where? When? Alfred Wegener Theory of Continental Drift
German scientist who developed the Theory of Continental Drift in 1912 The theory that states that the continents once formed a single landmass, broke up, and drifted to their present locations.

4 Restless Continents

5 Restless Continents Evidence of Continental Drift
Same fossils found on opposite continents Same rock types found on opposite continents Warm climate plant fossils on cold climate continents

6 Restless Continents Pangaea
All continents were once joined as a single, giant super- continent Greek for “all Earth” Existed 245 MYA

7 Restless Continents

8 Restless Continents Sea-Floor spreading
The process by which new oceanic lithosphere forms as magma rises toward the surface and solidifies Occurs at mid-ocean ridges (underwater mountain chains) CRT Question

9 Restless Continents Magnetic Reversals Proof of Sea-floor Spreading
Magnetic North and South poles switch positions Recorded when molten rock solidifies

10 Restless Continents Summary: Alfred Wegener developed continental drift hypothesis explaining that continents once formed Pangaea and then moved to their current positions. This occurs due to sea-floor spreading and that is proved by records of magnetic reversals solidified in new ocean rock.

11 Objective: 5 October 2012 Describe the theory of continental drift. Outro If Sea-Floor Spreading continues, what will the Earth look like in another 250 MY? Describe it or draw a picture!

12 Restless Continents When scientists proposed the Theory of Continental Drift, there were many skeptics. Which discovery confirmed that the continents move on plates? Deep-sea currents Earthquake formation Spreading of the sea floor Sedimentary rocks Interim 2


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