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Earthquake Faults Occur Throughout Nevada - Nbmg Unr
Get Earthquake Faults Occur Throughout Nevada - Nbmg Unr
Port is an update of the database used in Nevada for estimating losses from possible earthquakes and floods with HAZUS, the Federal Emergency Management Agency s computer model. It is available for HAZUS users as an online document at www.nbmg.unr.edu. The Nevada Bureau of Mines and Geology (NBMG) is a research and public service unit of the University of Nevada, Reno and is the State geological survey. Established.
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Approx FAQ
Two types of faults are common in Southern Nevada: normal and strike slip. Along normal faults rocks above the fault move down relative to those below the fault. Along strike-slip faults the rocks across the fault move horizontally past each other.
These include the Honey Lake, Warm Springs Valley, Pyramid Lake, and Olinghouse fault zones. The first three of these are part of a regional feature referred to as the Walker Lane.
Earthquakes in Western Nevada are caused by the extension that is pulling Nevada apart and wrenching created as the Sierra Nevada is pulled to the north because it is caught up in the Pacific-North America plate motion. The extension creates normal faults such as the Genoa fault, which bounds Carson Valley, the Mt.
The San Andreas Fault, while not in Nevada, is the other major fault in the Western U.S. It's a continuous line that stretches from east of San Diego up past San Francisco and accounts for a majority of the seismic motion felt on the West Coast.
The most earthquakes are in the western half of Nevada, where tectonic rates are highest. Based on this figure and many other studies, scientists conclude that a major earthquake can strike anywhere in Nevada and the chance of experiencing one or more earthquakes in western Nevada is high.
Shear forces replace compression as the North American plate begins riding over with the Pacific plate. On the other side of the Sierra Nevada Range, the Basin and Range Province is pulled apart as the force of compression increases.
There are four types of faulting -- normal, reverse, strike-slip, and oblique. A normal fault is one in which the rocks above the fault plane, or hanging wall, move down relative to the rocks below the fault plane, or footwall. A reverse fault is one in which the hanging wall moves up relative to the footwall.
The Las Vegas Valley fault system represents Quaternary faults within the Las Vegas metropolitan area (Figure 1). The fault system includes the north- to northeast-trending 11-km long Eglington intrabasin fault and the 18-km long basin bounding Frenchman Mountain fault.
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