1. (Types of Plate Boundaries)
Tuesday November 2, 2010
(Types of Plate Boundaries)

2. The Launch Pad Tuesday, 11/2/10 the fit of South America and Africa
In 1915, Alfred Wegener first proposed the continental drift hypothesis, which states that a supercontinent called Pangaea began breaking apart about 200 million years ago. He said that the continents “drifted” to their present positions.
List 5 pieces of evidence cited by Wegener that supported his hypothesis.
the fit of South America and Africa
fossils match across the seas
rock types and structures match across the seas
similar mountain ranges on different continents
similar ancient climates evidence matches on present-day continents

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5. Plate Boundaries Plate boundaries occur where two crustal plates meet.
There are three types of plate boundaries:
Divergent plate boundaries (constructive margins) occur where two plates move apart.
Convergent plate boundaries (destructive margins) occur where two plates collide.
Transform fault boundaries occur where plates slide past one another

6. Divergent Plate Boundaries
Divergent plate boundaries (constructive margins) occur where two plates move apart.
The mantle material up-wells to create new seafloor.
Oceanic ridges develop along well-developed boundaries.
Along ridges, seafloor spreading creates new seafloor.

7. Divergent boundaries are located along oceanic ridges.
Figure 7.11

8. Distribution of the Oceanic Ridge System

9. Figure 7.10 (left)

10. The East African rift is a divergent boundary on land
Continental rifts form at spreading centers within a continent.
Figure 7.13

11. Figure 7.13 (top right)

12. Continental
rifting

13. Convergent Plate Boundaries
Convergent plate boundaries (destructive margins) occur when plates collide, an ocean trench forms, and lithosphere is subducted into the mantle.

14. Convergent Plate Boundaries
Oceanic - continental convergence occurs when a denser oceanic slab sinks into the asthenosphere.
Pockets of magma develop and rise and a continental volcanic arc forms.

15. An Oceanic - Continental Convergent Plate Boundary
Figure 7.15 A

16. Convergent Plate Boundaries
Examples of oceanic – continental convergence include:
the Andes Mountains of South America.

17. Convergent Plate Boundaries
Examples of oceanic – continental convergence include:
the Cascade Mountains of Washington and Oregon.

18. Convergent Plate Boundaries
Examples of oceanic – continental convergence include:
the Sierra Nevada Mountains of California.

19. Convergent Plate Boundaries
Oceanic - oceanic convergence occurs when two oceanic slabs converge and one descends beneath the other.
This often forms volcanoes on the ocean floor.
A volcanic island arc forms as volcanoes emerge from the sea.

20. Convergent Plate Boundaries
Examples of oceanic – oceanic convergence include:
the Aleutian Islands.

21. Convergent Plate Boundaries
Examples of oceanic – oceanic convergence include:
the Mariana Islands.

22. Convergent Plate Boundaries
Examples of oceanic – oceanic convergence include:
the Tonga Islands.

23. Convergent Plate Boundaries
Continental - Continental Convergence
When two continental plates converge, they collide.
One continental plate subducts under the other.
This can produce buckling of the upper plate and new mountain ranges form, such as the Himalayas

24. The Collision of India and Asia Produced the Himalayas

25. Transform Plate Boundaries
Transform plates slide past one another.
No new crust is created or destroyed.
Transform faults are created.
Most transform faults join two segments of a mid-ocean ridge.
These faults and ridges aid the movement of oceanic crustal material.

26. California’s Fault Issue

27. GEODe Earth Science
Plate Tectonics
Slides (P5)