The 1981 Westmorland earthquake occurred at 05:09 Pacific Daylight Time (12:09 UTC) on April 26. The moderate strike-slip shock took place in the Imperial Valley of Southern California, just north of the Mexico–United States border. No injuries or deaths occurred, but damage was estimated at $1–3 million. With a Mercalli intensity of VII (Very strong), this was one of fifteen intensity VII or greater shocks in the Imperial Valley that were observed in the 20th century up until April 1981. The region experiences large stand-alone events and earthquake swarms due to its position in an area of complex conditions where faulting transitions from strike-slip movement to the north and divergence to the south.
  | |
| UTC time | 1981-04-26 12:09:31 |
|---|---|
| ISC event | 628772 |
| USGS-ANSS | ComCat |
| Local date | April 26, 1981 |
| Local time | 5:09 a.m. PDT |
| Magnitude | 5.9 Mw(ISC) |
| Depth | 10 km (6.2 mi)[1] |
| Epicenter | 33°01′N 115°41′W / 33.02°N 115.68°W[1] |
| Type | Strike-slip[2] |
| Areas affected | Imperial Valley Southern California United States |
| Total damage | US$1–3 million[3] |
| Max. intensity | MMI VII (Very strong)[3] |
Preface
editThe Imperial Valley of Southern California is very active seismically and has been subject to numerous destructive earthquakes since communities began to form in this desert area in the late 19th and early 20th centuries. Records of events prior to this period do not exist due to a lack of settlers in the area. Fifteen shocks of intensity VII or higher were recorded prior to April 1981 and beginning with the intensity VIII shock of April 18, 1906, which was a triggered event following the 1906 San Francisco earthquake.[4][5]
Tectonic setting
editThe Gulf of California Rift Zone underlies the Gulf of California from the mouth of the Colorado River in Baja California and stretching to the southeast. It contains numerous right-lateral transform faults and rift zones that make up the Pacific–North American plate boundary. The southern portion has matured into seafloor spreading, and at the northern end of the province is the Salton Trough, which is considered to be an onshore spreading center. The rift zone is covered by thick layers of sediment from the Colorado River drainage basin.[6]
The region experiences large stand-alone events and earthquake swarms due to its position in an area of complex faulting where it transitions from the strike-slip movement of the San Andreas Fault system to that of the divergent Gulf of California Rift Zone, which is an area of active seafloor spreading.
Earthquake
editThe Global Centroid Moment Tensor Database shows a NNW strike on a nearly vertical fault, with a rake angle that is within 45 degrees of being pure strike-slip.[2]
Intensity
editCalipatria and Westmorland both experienced intensity VII shaking (Very strong), which was the maximum observed intensity for the event. At these locations, roads and house foundations were cracked, interior and exterior walls experienced partial collapse, chimneys fell, windows were broken, and underground water pipes burst. The shock was felt over an area of 73,500 km2, and the communities of Encino and Cedar Glen in California, and Bouse in Arizona were at the outermost extremity of the felt area in the United States.[7]
See also
edit
References
edit- ^ a b ISC (2015), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 4.0, International Seismological Centre
- ^ a b PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey, September 4, 2009, archived from the original on 2020-03-13
- ^ a b Stover, C.W.; Coffman, J.L. (1993). Seismicity of the United States, 1568–1989 (Revised). U.S. Geological Survey professional paper 1527. United States Government Printing Office. pp. 96, 168.
- ^ Barnhard, Thenhaus & Algermissen 1982, pp. 1, 1A, 1B
- ^ Meltzner, A. J.; Wald, D. J. (2003), "Aftershocks and Triggered Events of the Great 1906 California Earthquake", Bulletin of the Seismological Society of America, 93 (5): 2, 160, 2, 164, 2, 166, 2, 169, 2, 170, Bibcode:2003BuSSA..93.2160M, doi:10.1785/0120020033, S2CID 128704816
- ^ Han, Liang; Hole, John A.; Stock, Joann M.; Fuis, Gary S.; Kell, Annie; Driscoll, Neal W.; Kent, Graham M.; Harding, Alistair J.; Rymer, Michael J.; González-Fernández, Antonio; Lázaro-Mancilla, Octavio (2016), "Continental rupture and the creation of new crust in the Salton Trough rift, Southern California and northern Mexico: Results from the Salton Seismic Imaging Project", Journal of Geophysical Research: Solid Earth, 121 (10): 7471, 7472, Bibcode:2016JGRB..121.7469H, doi:10.1002/2016JB013139
- ^ Stover, C.W. (1984), "United States earthquakes, 1981", Open-File Report, pp. 21–26, doi:10.3133/ofr84981
Sources
- Barnhard, L.M.; Thenhaus, P.C.; Algermissen, S.T. (1982), "Distribution of intensity for the Westmorland, California, earthquake of April 26, 1981", Open-File Report, Open-File Report 82-485, United States Geological Survey, doi:10.3133/ofr82485
Further reading
edit- Dorsey, Rebecca J. (2010). "Sedimentation and crustal recycling along an active oblique-rift margin: Salton Trough and northern Gulf of California" (PDF). Geology. 38 (5). Geological Society of America: 443–446. Bibcode:2010Geo....38..443D. doi:10.1130/g30698.1. ISSN 1943-2682.
- Lohman, R. B., and McGuire, J. J. (2007), Earthquake swarms driven by aseismic creep in the Salton Trough, California, J. Geophys. Res., 112, B04405, doi:10.1029/2006JB004596.
- Maley, R.P.; Etheredge, E.C. (1981), "Strong-motion data from the Westmorland, California, earthquake of April 26, 1981", Open-File Report, doi:10.3133/ofr811149