White Wolf Fault

From Wikipedia, the free encyclopedia

The White Wolf Fault is a fault in southern California, located north of the intersection of the San Andreas Fault and the Garlock Fault, and north of the Tehachapi Mountains. It is classed as a reverse (vertical motion) fault with a left lateral (sinistral) component. The White Wolf Fault was the source of the July 21, 1952, Kern County earthquake (M=7.3), the second largest earthquake in California during the 20th century.

References

  • Steinbrugge, Karl V., and Moran, Donald F. (1954) An Engineering Study of the Southern California Earthquake of July 21, 1952, and its Aftershocks. Bulletin of the Seismological Society of America, Vol. 44, No. 2B, pp. 201-462.
  • Stein. R. S. (1981) Seismic and aseismic deformation associated with the 1952 Kern County, California Earthquake and relationship to the Quaternary history of the White Wolf Fault, Journal of Geophysical Research, Vol. 86, No. NB6, pp. 4913-4928.
  • Dreger D., Savage B. (1999) Aftershocks of the 1952 Kern County, California, earthquake sequence, Bulletin of the Seismological Society of America, Vol. 89, No. 4, pp. 1094-1108.
  • Bawden, G. W. (2001) Source parameters for the 1952 Kern County earthquake, California: A joint inversion of leveling and triangulation observations, Journal of Geophysical Research, Vol. 106, No. B1, pp. 771-785.

External links



This article is issued from Wikipedia. The text is available under the Creative Commons Attribution/Share Alike; additional terms may apply for the media files.