San Felipe Fault Zone
The San Felipe Fault Zone (also known as the Agua Caliente or Murrieta Hot Springs fault zone) is an active Quaternary fault zone made up of continuous right-lateral fault strands]. The fault zone strikes WNW and consists of a central Easterly fault with adjacent strands extending out from the San Felipe anticline.[3] The fault zone is part of the Earthquake Valley, within the Pacific Border Ranges and Basin and Range physiographic provinces.[3] In total the faults run 170 kilometers long.[2]
The main San Felipe fault extends from the Geography
Origin
The San Felipe fault zone is estimated to have originated 1.1-1.3 Ma.[1][3] During its rise to the surface, the San Felipe fault created the San Felipe-Borrego basin and the San Felipe anticline.[4]
Movement
About half of the San Andreas fault system's movement has been from the San Felipe fault zone.
References
- ^ a b c Janecke, S. U., Dorsey, R. J., Forand, D., Steely, A. N., Kirby, S. M., Lutz, A. T., ... & Rittenour, T. M. (2011). High geologic slip rates since early Pleistocene initiation of the San Jacinto and San Felipe fault zones in the San Andreas fault system: Southern California, USA.
- ^ a b Bryant, William A. (2017). "Quaternary Fault and Fold Database of the United States". earthquake.usgs.gov. Retrieved 2021-12-18.
- ^ a b c d e f Alexander N. Steely, Susanne U. Janecke, Rebecca J. Dorsey, Gary J. Axen; Early Pleistocene initiation of the San Felipe fault zone, SW Salton Trough, during reorganization of the San Andreas fault system. GSA Bulletin 2009;; 121 (5-6): 663–687. doi: https://doi.org/10.1130/B26239.1
- ^ a b c Kirby, S. M., Janecke, S. U., Dorsey, R. J., Housen, B. A., Langenheim, V. E., McDougall, K. A., & Steely, A. N. (2007). Pleistocene Brawley and Ocotillo formations: Evidence for initial strike-slip deformation along the San Felipe and San Jacinto fault zones, southern California. The Journal of Geology, 115(1), 43-62.