Jump to content
 







Main menu
   


Navigation  



Main page
Contents
Current events
Random article
About Wikipedia
Contact us
Donate
 




Contribute  



Help
Learn to edit
Community portal
Recent changes
Upload file
 








Search  

































Create account

Log in
 









Create account
 Log in
 




Pages for logged out editors learn more  



Contributions
Talk
 



















Contents

   



(Top)
 


1 See also  





2 References  





3 External links  














Balcones Fault






Français
Italiano
Norsk bokmål
Svenska
 

Edit links
 









Article
Talk
 

















Read
Edit
View history
 








Tools
   


Actions  



Read
Edit
View history
 




General  



What links here
Related changes
Upload file
Special pages
Permanent link
Page information
Cite this page
Get shortened URL
Download QR code
Wikidata item
 




Print/export  



Download as PDF
Printable version
 
















Appearance
   

 






From Wikipedia, the free encyclopedia
 


Escarpment formed by the Balcones Fault at Mount Bonnell
Balcones Fault Trend and affected counties
Geologic map of the Balcones, and the Mexia-Talco-Luling Fault Trends, where black lines are faults, the blue shaded area is the Claiborne Group, yellow is the Jackson Group, and tan is the Wilcox Group

The Balcones[pronunciation?] FaultorBalcones Fault Zone is an area of largely normal faulting[1] in the U.S. stateofTexas that runs roughly from the southwest part of the state near Del Rio to the north-central region near Dallas[2] along Interstate 35. The Balcones Fault zone is made up of many smaller features, including normal faults, grabens, and horsts.[3] One of the obvious features is the Mount Bonnell Fault.[4]

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 worn away in Texas, the roots of these ancient mountains still exist, buried beneath thousands of feet of sediment. These buried Ouachita Mountains[5] 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 has remained inactive for nearly 15 million years, with the last activity being during the Neogene period. 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. The Balcones Fault 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 for species distributions, e.g., the California fan palm (Washingtonia filifera) is the only species of palm tree native to the continental United States west of the Balcones Fault.[9]

See also[edit]

References[edit]

  1. ^ "Major Faults of the Edwards Aquifer". Edwards Aquifer. Archived from the original on 13 April 2010. Retrieved 11 May 2010. Edwards Aquifer
  • ^ Laubach, Stephen E. (1997). "Tectonic Map of Texas" (PDF). Bureau of Economic Geology, The University of Texas at Austin. Retrieved 30 July 2015.
  • ^ 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. Archived from the original on 2008-11-07. 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 (ed.). First Annual Report of the Geological Survey of Texas, 1889. Austin: State Printing Office. p. 134. Archived from the original on 2010-06-21. Retrieved 2008-10-27.
  • ^ "Ouachita Mountains". J.S. Aber. Archived from the original on 2010-07-28. Retrieved 11 May 2010. J.S. Aber
  • ^ "Peak Acceleration (%g) with 10% Probability of Exceedance in 50 Years". USGS. October 2002. Archived from the original (GIF) on 2007-06-27.
  • ^ Balcones Escarpment from the Handbook of Texas Online. Retrieved 30 July 2015. 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. Archived from the original on 2009-09-30. Retrieved 2009-07-13.
  • External links[edit]


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Balcones_Fault&oldid=1225055118"

    Categories: 
    Escarpments of the United States
    Geology of Texas
    Landforms of Texas
    Seismic faults of the United States
    Hidden categories: 
    Articles with short description
    Short description matches Wikidata
    Articles needing pronunciation
     



    This page was last edited on 22 May 2024, at 02:27 (UTC).

    Text is available under the Creative Commons Attribution-ShareAlike License 4.0; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a non-profit organization.



    Privacy policy

    About Wikipedia

    Disclaimers

    Contact Wikipedia

    Code of Conduct

    Developers

    Statistics

    Cookie statement

    Mobile view



    Wikimedia Foundation
    Powered by MediaWiki