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PLATE TECTONICS Why the Earth is Like It Is. What Did The Earth Look Like In The Past?

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Presentation on theme: "PLATE TECTONICS Why the Earth is Like It Is. What Did The Earth Look Like In The Past?"— Presentation transcript:

1 PLATE TECTONICS Why the Earth is Like It Is

2 What Did The Earth Look Like In The Past?

3 Why Do Plates Move? Plates are “pushed” and “pulled” over the surface of the Earth due to unbalanced forces. REMEMBER CONVECTION? Convection currents reach the surface, plates are pushed apart. As the plates move away from each other, part of them are pulled into the Earth’s mantle.

4 Names of Plates

5 Plate Move In Different Ways

6 Plates Move Away From Each Other This is called Divergence – these are constructive boundaries since they produce new land as magma rises to the surface to fill in the space. Click to view animation – minimize PPT screen to see webpage

7 Rift Valley forms if the land is above water Sea Floor Spreading forms ridges as the sea floor spreads apart and lava rises Resulting landforms from Divergence – Moving Apart Click to view interactive map

8 Plates Move Toward Each Other This is called Convergence – these are destructive boundaries since they deform the plates. Collision or Subduction occurs as the more dense plate slide under the less dense plate. Continent/Continent Ocean/Continent Ocean/Ocean Click to view animationClick to view animation minimize PPT screen to see webpage

9 Resulting landforms from Convergence – Moving Together Trenches Mountains Structural Mountains Volcanoes Click to view interactive map

10 Plates slide paste each other When plates are sliding past each other in opposite directions it is a Transform Boundary. Transform boundaries occur in a few places to accommodate lateral, or side to side motion, in which plates slide past one another. Click to view animation Click to view animation minimize PPT screen to see webpage

11 When two plates are sliding past each other in opposite directions it creates a fault line. The result of two huge plates of land moving opposite one another is that massive amounts of energy build up. Occasionally this energy is released suddenly in the form of an earthquake. Resulting landforms from Transform Boundaries – sliding past each other Click to view interactive map

12 TAKS Type Items and Answer Analysis

13 As two continental plates move toward each other, what landforms would you expect to see? A. Volcanoes B. Cliffs C. Mesas D. Structural Mountains

14 As two continental plates move toward each other, what landforms would you expect to see? A. Volcanoes Incorrect These form at edges of plates or over hot spots.

15 As two continental plates move toward each other, what landforms would you expect to see? B. Cliffs Incorrect These are erosional landforms or minor uplift areas.

16 As two continental plates move toward each other, what landforms would you expect to see? C. Mesas Incorrect These are erosional landforms in a desert.

17 As two continental plates move toward each other, what landforms would you expect to see? D. Structural Mountains – correct - Two continental masses will push into each other and “crumple” the edges to form mountains.

18 Where would you find the newest land on Earth? A. In areas of continental convergence B. In areas where two ocean plates come together C. In areas where plates are moving apart D. In areas where two plates are sliding past each other

19 Where would you find the newest land on Earth? A. In areas of continental convergence Incorrect Structural mountains would form here from existing land.

20 Where would you find the newest land on Earth? B. In areas where two ocean plates come together Incorrect You would find trenches and subduction in this area.

21 Where would you find the newest land on Earth? D. In areas where two plates are sliding past each other Incorrect You would find land movement, but not new land being formed.

22 Where would you find the newest land on Earth? C. In areas where plates are moving apart Correct When plates move apart, it is due to magma reaching the surface. When magma cools, new land is formed.


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