1. Plate Tectonics

2. What is Plate Tectonics? The Earth’s crust and upper mantle are broken into sections called plates. Plates move around on top of the mantle like rafts.

3. The Crust This is where we live! The Earth’s crust is made of: Continental Crust - thick (10-70km) - buoyant (less dense than oceanic crust) - mostly old Oceanic Crust - thin (~7 km) - dense (sinks under continental crust) - young

4. World Plates

5. What are tectonic plates made of? Plates are made of rigid lithosphere. The lithosphere is made up of the crust and the upper part of the mantle.

6. What lies beneath the tectonic plates? Below the lithosphere (which makes up the tectonic plates) is the asthenosphere.

7. Plate Movement “Plates” of lithosphere are moved around by the underlying mantle convection currents. –Also, gravity pulls harder on the more dense oceanic plates.

8. Questions... What causes plates to move? How is a convection current formed?

9. Questions... What is the theory of plate tectonics? What is the lithosphere? What is the asthenosphere? What is the connection between the two? What are the two types of plates?

10. Plate Boundaries

11. Divergent Convergent Transform Three types of plate boundary

12. Seafloor Spreading –As plates move apart new material is erupted to fill the gap Divergent Boundaries

13. Age of Oceanic Crust Courtesy of www.ngdc.noaa.gov

14. Iceland has a divergent plate boundary running through its middle Iceland: An example of continental rifting

15. Two plate that are colliding   There are three styles of convergent plate boundaries –Continent-continent collision –Continent-oceanic crust collision –Ocean-ocean collision Convergent Boundaries

16. Forms mountains, e.g. European Alps, Himalayas 1. Continent-Continent Collision

17. Himalayas

18. Called SUBDUCTION 2. Continent-Oceanic Collision

19. Oceanic lithosphere subducts underneath the continental lithosphere Oceanic lithosphere heats and dehydrates as it subsides The melt rises forming volcanism E.g. The Andes Subduction

20. When two oceanic plates collide, one runs over the other causing it to sink into the mantle forming a subduction zone. The subducting plate is bent downward to form a very deep depression in the ocean floor called a deep-sea trench. The deepest parts of the ocean are found along trenches. –The Mariana Trench is 11 km deep! 3. Ocean-Ocean Collision

22. Where plates slide past each other Transform Boundaries Above: View of the San Andreas transform fault

25. Questions... What are the three types of boundaries? What direction do plates go for each? Which boundary has a subduction zone…what occurs at a subduction zone?

26. Side Effects Earthquakes and volcanoes transfer energy from Earth’s interior to the surface. Earthquakes – mechanical energy Volcanoes – thermal and mechanical energy