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Kern Canyon Fault

The Kern Canyon Fault is a geological fault which runs the length of Kern Canyon in the southern Sierra Nevada mountains in California.

The fault was once considered inactive, but recent studies show the contrary.[1][2]

The fault is a break in the southern section of the Sierra Nevada-Great Valley Block, manifesting differences in the stresses in this region over a period of over 100 million years. The fault was formerly right lateral-moving (horizontal sliding), but has changed to a normal (vertical lifting) mode of motion over the past several thousands of years.[2]

See also

References

  1. ^ Nadin, E. S.; Saleeby, J. B. (2005). "Recent Motion on the Kern Canyon Fault, Southern Sierra Nevada, California". American Geophysical Union, Fall Meeting 51: 1369.  
  2. ^ a b Nadin, Elisabeth S.; Saleeby, Jason B. (September 2010). "Quaternary Reactivation of the Kern Canyon Fault System, Southern Sierra Nevada, California". GSA Bulletin 122 (9–10): 1671–1685.  


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