Continental drift and the theory of plate tectonics

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16 Terms

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Who created the first modern atlas?

Abraham Ortelius

<p>Abraham Ortelius</p>
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Which meteorologist proposed the theory of continental drift?

Alfred Wegener

<p>Alfred Wegener</p>
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In what year was the theory of continental drift proposed?

1912

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What evidence is there to support the theory of continental drift?

  • the theory of plate tectonics

  • Mesosaurus fossils

  • geological columns

  • plant fossils

  • animal fossils

  • complimentary continent shapes

<ul><li><p>the theory of plate tectonics</p></li><li><p>Mesosaurus fossils</p></li><li><p>geological columns</p></li><li><p>plant fossils</p></li><li><p>animal fossils</p></li><li><p>complimentary continent shapes</p></li></ul><p></p>
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plate tectonics

the process whereby heated rock is moved within the Earth in vast convection currents, which drag along the underside of the Earth’s plates, forcing them to slowly drift across the planet

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What is the thickness of conintental crust?

30-70km

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What is the age of continental crust?

over 1,500 million years old

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What is the density of continental crust?

2.6g/cm3

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What is the composition of continental crust?

mainly granite

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What is the thickness of oceanic crust?

6-10km

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What is the age of oceanic crust?

less than 200 million years old

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What is the density of oceanic crust?

3.0g/cm3

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What is the composition of oceanic crust?

mainly basalt

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convection currents

  1. Heat from the core (hot spots) warms the mantle, causing it to rise up

  2. This movement within the mantle moves the plates above it

  3. The mantle nearer the surface cools and creates new crust

  4. The mantle moves back down towards the core

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ridge push

  1. At a constructive plate boundary, plates are pulling apart

  2. Magma rises to the surface and forms new crust

  3. This heats the surrounding rocks, which expand and rise above the surface, creating a slope

  4. New crust cools and becomes denser, sliding downslope away from the late margin

  5. This puts pressure on the plates, causing them to pull apart

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slab pull

  1. At destructive plate margins, denser crust is forced under less dense crust

  2. The sinking of the plate edge pulls the rest of the plate towards the boundary