Basic Fault Types |
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| As discussed in class, a fault is a break in the rock layers along which the rock moves. There are 4 basic types of faults found on the Earth. | |
The Normal Fault The normal fault is not necessarily normal in the sense that it is common....because.... it is not the most common of faults. However what is normal about them is that their movement tends to follow the gravitational pull on the fault blocks involved. |
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The Reverse Fault |
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Thrust Fault |
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Strike-Slip Fault (Transverse) Probably the most well known and well studied fault of this type is known as the San Andreas fault of California. This fault is on the boundry between the Pacific and North American Plates. Actually anything crossing this fault zone is either slowly torn apart, or offset. These faults can be very long, the San Andreas is nearly 600 miles long |
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Other types of Deformation on the Earth's Crust |
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Rocks under STRESS. |
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| Compression is the type of stress that occurs when rock is squeezed. Compression occurs when tectonic plates collide (move towards each other). This can cause some spectacular consequences! The Sinai Massif is an example of stress occuring on rock layers. | |
| Tension | |
| Shear | |
Questions: 1.) Why would id be a bad idea to build your house near any fault?
2.) Explain the following terms: Compression stress, deformation, and tension stress.
3.) Which type of fault occurs when the rock layers are pulled or streatched?
4.) Explain the difference between a Thrust fault and a reverse fault.
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| Graphics for this page from: Dr. M. Mustoe, Area Coordinator for Geography at the University of Texas of the Permian Basin Odessa, Texas |
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