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Theory of Plate Tectonics. How do we know the plates exist?  Earthquake and Volcano Zones  Ocean floor features (Trenches and Mid-Oceanic ridges)

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Presentation on theme: "Theory of Plate Tectonics. How do we know the plates exist?  Earthquake and Volcano Zones  Ocean floor features (Trenches and Mid-Oceanic ridges)"— Presentation transcript:

1 Theory of Plate Tectonics

2 How do we know the plates exist?  Earthquake and Volcano Zones  Ocean floor features (Trenches and Mid-Oceanic ridges)

3 Plate Boundary Features Plate Boundary Features

4 Lithospheric Plates  7 major Plates (continental crust, oceanic crust) The Earth is made up of a dozen or so major plates and several minor plates. Tectonic plates are constantly on the move. The fastest plate races along at 15 centimeters (6 inches) per year while the slowest plates crawl at less than 2.5 centimeters (1 inch) per year.

5 Lithospheric Plate Cross Section

6 How do we know the plates move?  Evidence Supporting Continental Drift  Movement of the Pacific Plate (Hawaiian island chain formed over a hotspot)

7 How do the Plates Move?

8 Explain this diagram:

9 Sea Floor Spreading mid-ocean ridges rift valley lithospheric plate asthenosphere magma newer less dense crustolder more dense crust

10 Sea Floor Spreading  A rift valley is volcanically active forming new oceanic crust on each side of the valley creating Mid-Ocean Ridges.  The new crust pushes the older crust away from the mid-ocean ridge, moving the ocean floor & the continents  Ex: Mid-Atlantic Ridge

11 Evidence of Sea Floor Spreading  Rock samples are younger closer to a mid-ocean ridge

12

13 What Destroys Crust? Subduction Zones  Occurs when oceanic crust collides with oceanic or continental crust  The older, more dense, oceanic crust plunges back into the mantle at a deep ocean trench.  Forms deep ocean trenches & volcanic mountains or island arcs.

14 Trenches of the World

15 Oceanic - Continental Subduction Oceanic - Oceanic Subduction Plate Collisions Continental– Continental (No Subduction)

16 Convergent Margins: India-Asia Collision II Convergent Margins: India-Asia Collision II

17 Three Plate Boundaries  Divergent –plates move apart; sea floor spreading  Convergent –Plates collide together; subduction  Transform (strike-slip) –Plates slide past each other; San Andreas fault

18 Transform Boundary: San Andreas Fault

19 Motion at Plate Boundaries Motion at Plate Boundaries

20 Plate Boundaries

21 What Causes the Plates to Move?  Convection Currents in mantle  Ridge Push  Slab Pull

22 Lava Lamp Convection Lava Lamp Convection

23 and Tectonics Convection and Tectonics


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