1. How Convection Works!
Magma expands when heated making volume larger making magma less dense therefore it will __________ to the top of more dense magma
When the magma reaches the surface it cools and contracts becoming _________ _____________ and it will sink.
The process keeps continuing in a circle or cyclic cycle.

2. Sinking
Rising

3. Example 2: Plates Pulling Apart and Pushing Together

4. You don’t have to memorize
Circle and Label where the convection currents are moving plates together and pulling them apart.

5. Tell your neighbor….
WHAT HAPPENS TO THE CRUST WHEN THE PLATES ARE MOVING AROUND???? What things do we see at these places?

6. Part III. Convergent Plate Boundaries

7. Earthquake Map

8. I. Plate Tectonics
A. Plate Tectonics Theory states that the lithosphere is broken up into 8 major plates that move relative to one another.

9. I. Plate Tectonics
B. Much of Earth’s mountain building, earthquakes, and volcanoes occur at boundaries between plates.

11. II. Plate Boundaries (Borderlines between plates)
A. Convergent Plate Boundaries
1. Occur when 2 plates converge, or move towards one another.

12. Checkpoint!   Convergent
Use your hands to demonstrate the motion at a convergent plate boundary
Convergent
 

13. III. Convergent Plate Boundaries
A. Continental-Continental Boundary
1. When 2 continents collide, they bunch up together, because they have approximately the same density. In other words, mountains form.

14. Animation

15. 2. The best example of this occurs where the Indian- Australian Plate is colliding with the Eurasian Plate. This collision formed the Himalayas.
Mt. Everest

17. Checkpoint
Using your arms as plates, be ready to show what happens when two continental plates collide.
Go!

18. III. Convergent Plate Boundaries
B. Oceanic-Continental Boundary
1. When a continental plate and oceanic plate converge, the oceanic plate sinks below because it is more dense.

19. Checkpoint!
Recall how it gets hotter as you go deeper into the Earth’s interior…
Visualize what will happen to an oceanic plate as it sinks further and further below continental crust…
Discuss what will happen to that oceanic plate.

21. Animation

22. III. Convergent Plate Boundaries
2. This is called a Subduction Zone.
When the more dense oceanic plate goes under (subducts) the less dense continental crust.

23. IV. Environmental Characteristics of a Subduction Zone
A. EARTHQUAKES occur when plates grind against one another.

25. IV. Environmental Characteristics of a Subduction Zone
B. VOLCANOES form when magma rises back through the crust.

27. IV. Environmental Characteristics of a Subduction Zone
C. Trenches or large canyons form in the ocean.

28. Lets find some convergent plate boundaries using the ESRT pg. 5

29. Assessment
Question #1
What are the plates at a convergent boundary doing?
Moving Apart
Moving Together
Sliding Past Each Other
Staying Still

30. Assessment
Question #2
Which plate will float atop the other at a Continental-Oceanic Crust Convergent Boundary?
Continental Crust
Oceanic Crust
Asthenosphere
Lithosphere

31. Part IV: Divergent Plates Boundaries

32. Diverging Plate Boundaries
-When 2 or More plates separate or pull-apart
-Magma rises between plates and makes new rock (Igneous Intrusion)
-Shallow Earthquakes occur at this boundary
Features at Divergent Boundaries include
-Mid-Ocean Ridges
-Rift Zones

33. *As the magma rises and the plates separate new igneous rock is made

34. Feature #1: Mid-Ocean Ridge
When Oceanic Crust is being pulled-apart or separated
Features
-Longest volcanoes in the world, from the rising magma through cracks in lithosphere
-Shallow Earthquakes occurring, from movement of lithosphere
-Youngest rock in the ocean, because new rocks are made from solidification of magma

35. Cross-Section of a Mid-Ocean Ridge

36. Mid-Ocean Ridges and Seafloor Spreading
Seafloor Spreading creates mid-ocean ridges
They are underwater mountain ranges and can stretch for of Kilometers

37. Animation of Seafloor Spreading

38. Feature #2: Rifting
When Continental Crust is being pulled apart or separated
If new crust is created at divergent boundaries, is the Earth getting larger?

39. *Both Rifting and Seafloor Spreading occurs in the same sequence

40. EVENTUALLY THE RED SEA MAY BECOME THE RED OCEAN

41. Lets find some divergent plate boundaries using the ESRT pg. 5

42. Checkpoint
What is the major difference between seafloor spreading and rifting?
Answer: seafloor spreading occurs when oceanic crust separates, rifting is when continental crust separates

43. Part V: Transform Plate Boundaries and Hot Spots

44. Transform Plate Boundary: is when two plates slide past each other.
Properties: 1. Shallow Earthquakes
2. Mostly occur at mid-ocean ridges

45. Basic California Geography
San
Andreas
Fault
San Francisco
San
Joaquin
Valley
Basic
California
Geography
Death Valley
Mojave Desert
Los Angeles
Imperial
Valley

48. Transform faults occur frequently at mid-ocean ridges

49. Lets find some transform plate boundaries using the ESRT pg. 5

50. Hot Spots
Definition:
Volcanic activity that doesn’t occur at a plate boundary
Facts
Usually forms volcanic islands
Hawaii is a Hot Spot
There is a list of hot spots on the tectonic plates page 5 of the ESRT

51. Hot Spot

52. Hot Spot: Cont. - Consider that Hawaii is a Hot Spot!
-Hot Spots remains stationary as the plates move over them
- Consider that Hawaii is a Hot Spot!

53. Explain its positioning.

55. Lets find some Hot Spots using the ESRT pg. 5

56. Earthquake Patterns
Question: Where do most Earthquakes occur?