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Earth’s Crust in Motion. Stress in the Crust Earthquake is the shaking and trembling that results from the movement of rock beneath Earth’s surface.

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Presentation on theme: "Earth’s Crust in Motion. Stress in the Crust Earthquake is the shaking and trembling that results from the movement of rock beneath Earth’s surface."— Presentation transcript:

1 Earth’s Crust in Motion

2 Stress in the Crust Earthquake is the shaking and trembling that results from the movement of rock beneath Earth’s surface.

3 Types of Stress 1.Shearing 2.Tension 3.Compression

4 Types of Stress

5 Faults 1.Strike-Slip Fault 2.Normal Fault 3.Reverse Fault

6 Strike-Slip Fault Stress that causes Strike-Slip Faults: Shearing

7 Strike-Slip Fault Example The San Andreas Fault in California.

8 Normal Fault Stress that causes Normal Fault is: Tension

9 Normal Fault Example The Sandia Mountains in New Mexico were created by a Normal Fault.

10 Reverse Fault Stress that causes a reverse fault: Compression

11 Reverse Fault Example Mt Gould in Glacier National Park

12 Friction Along Faults Little Friction- quicker movement, less force to overcome friction. More Friction- stress must build up to move one plate past another. When stress is released more powerful earthquake can result.

13 Mountain Building Mountains Formed by Faulting. Fault Block Mountains- Teton Range Wyoming (2 normal faults)

14 Mountains by Folding Folds are bends in rock that form when compression shortens and thickens part of Earth’s crust

15 Folded Mountains Example: Himalayas and Alps

16 Anticlines and Synclines

17 Examples of Anticlines and Synclines Anticline-Black Hills South Dakota Syncline-Illinois Basin

18 South Dakota

19 Plateau Example- Colorado Plateau including Four Corners (Arizona, Utah Colorado, New Mexico)

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