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The Dynamic Earth and Plate Tectonics. Early Ideas on a moving Earth Alfred Wegener proposed idea: “Continental Drift” – Stated that all continents used.

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Presentation on theme: "The Dynamic Earth and Plate Tectonics. Early Ideas on a moving Earth Alfred Wegener proposed idea: “Continental Drift” – Stated that all continents used."— Presentation transcript:

1 the Dynamic Earth and Plate Tectonics

2 Early Ideas on a moving Earth Alfred Wegener proposed idea: “Continental Drift” – Stated that all continents used to be joined in Pangaea (meaning “all land”) that broke up into smaller continents, “drifted” to current locations

3 What patterns do we see in continent shapes?

4 Continental Drift - Wegener’s hypothesis of continent movement after Pangaea broke apart Early evidence #1:Coastlines on early maps seem to fit like puzzle pieces

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8 Why are there fossils of cynognathus on both Africa and South America and no where else?

9 “Continental Drift”, Early evidence #2 Fossils of the same organism were on opposite land masses (puzzle pieces), known to have been joined at one time

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12 Why do rocks from Rhode Island and Scotland match?

13 “Continental Drift”, early evidence #3 Mountains and rocks continued on opposite puzzle pieces

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15 Why did southern India used to have glaciers?

16 “Continental Drift”, early evidence #4 Misplaced glacial remnants and tropical swamps can be explained if continents were once joined

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18 Newer evidence Proof of seafloor spreading at the Mid- Atlantic Ridge (1947) – Rock at the ridge was dated much younger than continental rock – Paleomagnetism also apparent As magma solidifies, iron crystals align with Earth’s magnetic field like a compass. Geologists have known that this happens periodically throughout history, as magnetic poles flip flop.

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20 Modern Theory of Plate Tectonics Earth is made up of 9 primary plates and several microplates made up of continental and oceanic crust. – Upper lithosphere is crusty and moves about on plasticy asthenosphere. – Asthenosphere moves most likely due to convection in the mantle due to heat from core and radioactivity from mantle Where plates meet is called a plate boundary – Types: Convergent, divergent, transform

21 PLATE BOUNDARIES 1. Convergent Boundary Ocean – Continent Ocean – Ocean Continent – Continent Continent – Continent convergence Ocean – Continent Convergence

22 2. Divergent Boundary 3. Transform Boundary

23 Where in the World do we find those boundaries?


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