2. Looking at the world map, what do you notice about the shape of the continents? Jot down your ideas on your paper…

3. The thing is…the world didn’t always look like this! It used to look like this:

4. How is this possible?!?!?

5.  The continents have shifted their position over geologic time Continental Drift Theory

6.  At one time all land masses were connected into one piece called Pangaea

7. oPangaea began to split apart 200 million years ago oDiagram North America LaurasiaGreenland Eurasia Pangaea Africa West G.S.America Gondwanaland Antarctica East G.Australia India

9. oThe continents are like packages on the seafloor conveyor belt Continents

11. oHigh probability that the continents fit together Evidence

12. oMinerals, fossils, and mountains on now different continents match if the continents were together Evidence

13. oGlaciation patterns indicate a common ice cap at the South Pole Evidence

14. oPaleomagnetism oPaleomagnetism (magnetism of old rocks) indicate a common pole if the continents were all connected Evidence

16. Seafloor Spreading Theory : Ocean floors are moving like broad conveyor belts

17. New ocean floor crust is being created at the mid-ocean ridges

18. Convection currents within the mantle  The up-welling leg of the current creates a divergent boundary which produces mid-ocean ridges What causes this?

19.  The down-welling leg of the current creates one type of convergent boundary that results in trenches and a subduction zone

20. oMid-ocean ridges are warmer than surrounding ocean floors oActive volcanoes on ridges, earthquakes on ridges oMid-ocean ridge rocks are younger than surrounding ocean floor rocks oMid-ocean ridge volcanoes are younger than volcanoes further away What evidence do we have to support this idea?

21. oOcean floor sediments are thin on the ridges and get thicker as the distance from the ridges increase oPolar reversal magnetism proves that the ocean floor is moving away from the ridges What evidence do we have to support this idea?

22. 2-3  Atlantic Ocean – 2-3 cm/year 15-18  South Pacific Ocean – 15-18 cm/year Speed of Spreading

23.  The lithosphere is divided into a number of large and small plates and the plates are floating on the mantle Plate Tectonics Theory

24. crust mantle Lithosphere = the Earth’s crust plus the upper portion of the mantle layer

27. Boundaries between Tectonic Plates

28. Get Out the Following Things: Plate Tectonic Notes Plate Tectonic Directed Reading MAKE SURE YOU HAVE YOUR TEXTBOOK!!!

29. Plate Boundaries Divergent boundary: oPlates are moving away from each other oMid-ocean ridges are created and new ocean floor plates are created

30. Plate Boundaries Divergent boundary:

31. Leif the Lucky Bridge Bridge between continents in Reykjanes peninsula, southwest Iceland across the Alfagja rift valley, the boundary of the Eurasian and North American continental tectonic plates.

32.  Convergent Boundary  Convergent Boundary: plates are moving toward each other and are colliding (3 types)

33. Create subduction zones, trenches Create near coast volcanoes When Ocean Plates Collide with Continental Plates

34. When ocean plates collide with other ocean plates Island arcs are created (a pattern of volcanic islands created from a subduction zone that is located off the coast)

35. MountainrangesMountain ranges are created (example: Himalayan Mountains) When a continental plate collides with another continental plate

36. Himalayan Mountains Mountain Formation Video Clip

37. Transform Boundary  Plates are neither moving toward nor away from each other, they are moving past one another.

38. Transform Boundary  The plates may move in opposite directions or in the same directions but at different rates and frequent earthquakes are created (example: San Andreas Fault)

39. San Andreas Fault

40. oNo oPlates are destroyed as fast as they are created (2 ways) oPlates may be subducted and melted or may push be pushed upward to form mountains So is the Earth getting bigger?

41. Plate Tectonic Review