Balcones Fault
The Balcones Fault Zone is a tensional structural system[1] in the U.S. state of Texas that runs approximately from the southwest part of the state near Del Rio to the north central region near Waco along Interstate 35. The Balcones Fault zone is made up of many smaller features, including normal faults, grabens, and horsts.[2] One of the obvious features is the Mount Bonnell Fault.[3]
The location of the fault zone may be related to the Ouachita Mountains, formed 300 million years ago during a continental collision. Although long since eroded away in Texas, the roots of these ancient mountains still exist, buried beneath thousands of feet of sediment. These buried Ouachita Mountains[4] may still be an area of weakness that becomes a preferred site for faulting when stress exists in the Earth's crust. The Balcones Fault zone was most recently active on 01/22/2013 10:16PM UTC-06:00 at the epicenter near Irving, Texas, registering a 3.0 on the Richter magnitude scale.[5] Until recently, the Balcones Fault has remained inactive for nearly 15 million years, with the last activity being during the Miocene epoch. This activity was related to subsidence of the Texas Coastal Plain, most likely from the large amount of sediment deposited on it by Texas rivers. Although the Balcones Fault zone has recently been active, it is in one of the lowest-risk zones for earthquakes in the United States.[6]
The surface expression of the fault is the Balcones Escarpment,[7] which forms the eastern boundary of the Texas Hill Country and the western boundary of the Texas Coastal Plain and consists of cliffs and cliff-like structures. Subterranean features such as Wonder Cave and numerous other smaller caves are found along the fault zone.
Many cities are located along this fault zone. Springs such as San Pedro Springs, Comal Springs, San Marcos Springs, Barton Springs and Salado Springs are found in the fault zone and provide a source of fresh water and a place for human settlement.
The Balcones Fault Zone[8] is a demarcation line for certain ecological systems and species distributions, e.g., the California Fan Palm (Washingtonia filifera) is the only species of palm tree that is native to the continental United States west of the Balcones Fault.[9]
See also
- Texas Hill Country
- Balcones Canyonlands National Wildlife Refuge
- Colorado River (Texas)
- Edwards Plateau
References
- ↑ "Major Faults of the Edwards Aquifer". Edwards Aquifer. Archived from the original on 13 April 2010. Retrieved 11 May 2010. Edwards Aquifer
- ↑ Grimshaw, Thomas W.; Charles Woodruff, Jr. (1986). "STRUCTURAL STYLE IN AN EN ECHELON FAULT SYSTEM, BALCONES FAULT ZONE, CENTRAL TEXAS: GEOMORPHOLOGIC AND HYDROLOGIC IMPLICATIONS". The University of Texas. Retrieved 2008-10-27.
- ↑ Hill, Robert T. (1891). "A brief description of the Cretaceous rocks of Texas and their economic uses". In E. T. Dumble. First Annual Report of the Geological Survey of Texas, 1889. Austin: State Printing Office. p. 134.
- ↑ "Ouachita Mountains". J.S. Aber. Retrieved 11 May 2010. J.S. Aber
- ↑ "M3.0 - northern Texas (BETA) 2013-01-23 04:16:20 UTC". Earthquake.usgs.gov. Retrieved 2013-07-10.
- ↑ "Peak Acceleration (%g) with 10% Probability of Exceedance in 50 Years" (GIF). USGS. October 2002. Archived from the original on 2007-06-27.
- ↑ Balcones Escarpment from the Handbook of Texas Online. Retrieved 11 May 2010. Texas State Historical Association
- ↑ "Balcones Fault Zone". UT Austin. Retrieved 11 May 2010. UT Austin
- ↑ Hogan, C. Michael (2009-01-05). "California Fan Palm: Washingtonia filifera". GlobalTwitcher.com. Retrieved 2009-07-13.
External links
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