MadSci Network: Earth Sciences |
Hi Travis, Let's first look at what a fault is. A fault results when the earth's crust suddenly yields under unequal stress. The crust gets displaced along the plane of breakage, also called the fault plane. This displacement can be vertical or horizontal, or a combination of both. Faults are often of great extent along the earth's surface (several kilometers), and they show up quite clearly (for example, the San Andreas Fault). Over time, even small faulting movements can add up considerably so that some faults have displacements of thousands of meters. If you get a situation where a block of crust gets elevated between two normal faults, you get what is called a Horst. Horsts make blocklike plateaus that have flat tops and steep straight sides. In regions where faulting takes place on a grand scale, this produces mountain masses called fault block mountains. An example of a fault block mountain is the Basin and Range of Nevada. It consists of a system of ranges which formed during the Tertiary as a consequence of the stretching of the continental crust. The Sierra Nevada mountains are a gigantic tilted normal fault-block structure where the crust was being extended or pulled apart, and Horsts and Grabens (the opposite of a Horst - a block has sunk between two faults) formed with the uplifted Horsts becoming the mountain ranges. These mountains are separated from the intervening valley floors by normal faults of great displacement. Here are some web links on the issue: The "Geology on the Web"-Site has a geological dictionary: http://www .geotech.org/survey/geotech/dictiona.html#sectF This high school website has a good section of faults and faulting: http://www.blackgold.ab.ca/science/science_8_pages/unit_4/8scu4t4l1.ht ml There is a good graphic here at Volcano World that illustrates how a fault-block is uplifted: http://volcano.und.nodak.edu/vwdocs/vwlessons/lessons/Ch1CMA/Answer _Key_Rev iew_1.html The Department of Geosciences at Penn State talks about types of Mountain Belts: http://www.ge osc.psu.edu/~engelder/geosc20/lect30.html And last but not least, this is a good introductory textbook, if you want to know more about Physical Geography and Geology: Strahler, A. N., Strahler, A. H., 1989: Elements of Physical Geography. 4th Edition. **************** Katja Bach, B.Sc. (Geography), Ph.D. (Remote Sensing) RADARSAT International Richmond, British Columbia, Canada kbach@rsi.ca www.rsi.ca *****************
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