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Science 14 December 1973: Vol. 182. no. 4117, pp. 1127 - 1129 DOI: 10.1126/science.182.4117.1127
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Articles
Point Mugu, California, Earthquake of 21 February 1973 and Its Aftershocks
W. L. Ellsworth 1,
R. H. Campbell 1,
D. P. Hill 1,
R. A. Page 1,
R. W. Alewine III 2,
T. C. Hanks 2,
T. H. Heaton 2,
J. A. Hileman 2,
H. Kanamori 2,
B. Minster 2, and
J. H. Whitcomb 2
1 National Center for Earthquake Research, U.S. Geological Survey, Menlo Park, California 94025
2 Seismological Laboratory, California Institute of Technology, Pasadena 91109
Seismological investigations show that the Point Mugu earthquake involved north-south crustal shortening deep within the complex fault zone that marks the southern front of the Transverse Ranges province. This earthquake sequence results from the same stress system responsible for the deformation in this province in the Pliocene through Holocene and draws attention to the significant earthquake hazard that the southern frontal fault system poses to the Los Angeles metropolitan area.
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