1987 Superstition Hills earthquakes
1987 Superstition Hills earthquakes is located in California
Ridgecrest
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1987 Superstition Hills earthquakes
UTC time1987-11-24 01:54:14
 1987-11-24 13:15:56
ISC event453653
 453722
USGS-ANSSComCat
 ComCat
Local dateNovember 23 1987
 November 24 1987
Local time5:53 p.m.
 5:16 a.m.
Magnitude6.0 Mw
 6.5 Mw
Depth2.3 km
 7.5 km
Epicenter33°05′24″N 115°47′31″W / 33.090°N 115.792°W / 33.090; -115.792
TypeStrike-slip
Areas affectedCalifornia and Mexico
Total damage$3 million
Max. intensityVI (Strong)

VII (Very strong)
Casualties2 dead, 90+ injured

The 1987 Superstition Hills and Elmore Ranch earthquakes were a pair of earthquakes measuring Mw  6.0 and 6.5 that rattled the Imperial Valley of California. The earthquakes caused damage in Southern California and Mexico, but was limited due to their location in a sparsely populated area. It was felt as far as Las Vegas and Phoenix. More than 90 were injured, and two people were killed in Mexico.

Geology

The Imperial Valley is a seismically active area in California. It is in this area where the San Andreas Fault and San Jacinto Fault Zone (SJFZ) terminate in the south. This region is a transition zone between the continental transform boundary to oceanic rifting in the Gulf of California. South of the San Andreas Fault and between the Imperial Fault is the Brawley Seismic Zone—the northernmost ridge feature in the Gulf of California ridge–transform boundary. Faults in the Brawley Seismic Zone typically trend northeast, perpendicular to the plate boundary faults. Labeled "cross-faults", these are oriented perpendicular to the direction of rifting and have been inferred to be normal faults. However, recent seismic activity show that these faults produce left-lateral strike-slip motion.[1]

The SJFZ is a 244 km (152 mi)-long right-lateral structure that runs parallel to the San Andreas Fault.[2] The SJFZ is southern California's most seismically active fault zone. It was responsible for the large surface-rupturing Borrego Mountain earthquake in 1968. It is a highly segmented fault zone consisting of seven individually named segments.[3] One of these segments is the Superstition Hills Fault, a vertically-dipping, 38 km (24 mi)-long section.[4] In 1951, a magnitude 5.6 earthquake caused it to generate a small surface rupture. It also produced triggered slip following the 1968 Borrego Mountain and 1979 Imperial Valley earthquakes.[5]

Earthquakes

Elmore Ranch earthquake

The Elmore Ranch earthquake occurred at 5:53 pm measuring Mw  6.0 at a depth of 2.3 km (1.4 mi).[6] The epicenter was located in a sparsely populated area 22.5 km (14.0 mi) southwest of Westmorland.[7] The location of its aftershocks strongly implied rupture occurred along a northeast striking fault zone. The aftershock zone also implied that the mainshock ruptured in a bilateral nature; northeast towards the Brawley Seismic Zone and southwest, where it traverse the Superstition Hills Fault. The fault zone responsible for this earthquake was unidentified prior to 1987, but it was later named Elmore Ranch Fault Zone (ERFZ). The fault ruptured for 20–25 km (12–16 mi) but surface ruptures was only observed for half that length. It was associated with left-lateral slip and had a maximum offset of nearly 20 cm (7.9 in). Between 2.8 cm (1.1 in) and 4.8 cm (1.9 in) of slip was measured on the Lone Tree, Kane Springs, and Eastern Kane Springs faults (part of the ERFZ). The main Elmore Ranch Fault strand had a measured displacement of 13 cm (5.1 in).[1]

Superstition Hills earthquake

The Superstition Hills earthquake measured Mw  6.5 at 7.5 km (4.7 mi) depth.[8] It occurred nearly 12 hours after the Elmore Ranch earthquake.[5] The epicenter was located at the northwestern termination of the Superstition Hills Fault, where it intersects the ERFZ. An aftershock zone roughly parallel to the Superstition Hills Fault formed, although it was several kilometers southwest of the main rupture trace.[1] Surface rupture was observed along the Superstition Hills Fault with a maximum offset of 80 cm (31 in).[9] The surface rupture extended southeastward from the epicenter for 27 km (17 mi). No surface rupture was detected along the fault after the Elmore Ranch earthquake.[5] The Superstition Hills Fault continued to produce slip even a year after the mainshock. A vertical displacement of 25 cm (9.8 in) was recorded at the southern end of the rupture.[10]

Ground motion

A USGS ShakeMap for the November 24 main shock.

Strong motion data was first compiled by the United States Coast and Geodetic Survey in 1932 with the installation of an accelerograph at El Centro. Up till 1987, nearly 700 strong motion data (accelerograms) have been gathered from earthquakes in the Imperial Valley. The 1987 earthquakes produced 65 accelerograms from 40 stations across the valley. Horizontal peak ground accelerations (pga) during the Elmore Ranch earthquake exceeded 0.1 g at six stations. The nearest station at Superstition Mountain was 13 km (8.1 mi) away; it measured a pga of 0.13 g. The highest pga was 0.22 g at Calipatria, 26 km (16 mi) away.[11]

During the Superstition Hills earthquake, 25 stations recorded a maximum horizontal pga exceeding 0.1 g within 60 km (37 mi) of the epicenter. These stations recorded a pga nearing or were greater than 0.3 g. The Superstition Mountain station recorded a pga that was the largest and longest ever observed in its 55-year history of data records. A pga of 0.9 g and 0.7 g in both horizontal direction and 0.6 g in vertical direction was recorded.[11]

Triggered slip

Surface ruptures were observed on the central section of the Coyote Creek Fault, another segment of the SJFZ. The Coyote Creek Fault was associated with the 1968 earthquake. This section of the fault produced considerable afterslip and vertical displacements after the 1968 earthquake. It is located roughly to the north of the 1987 earthquakes. In response to the 1987 earthquakes, new surface ruptures measuring 3 km (1.9 mi) with right-lateral slip of 1.5 cm (0.59 in) occurred. Minor vertical displacements were also recorded. Creepmeters also indicated that several millimeters of slip occurred on the San Andreas Fault, but was insufficient to create a surface rupture. Triggered slip was also measured on the Imperial Fault.[12]

Impact

Damage from the Elmore Ranch earthquake in Calipatria, El Centro, Heber and Westmorland corresponded to VI on the Modified Mercalli intensity scale (MMI).[13] The Superstition Hills earthquake had a maximum MMI of VI–VII at El Centro and Westmorland. Intensity VI was felt at Brawley, Calexico, Calipatria, Heber, Holtville, Imperial and Seeley. It was widely felt across southern California. Shaking was also felt in Las Vegas, Nevada and Tempe, Arizona. In Mexico, the earthquake was felt in Tijuana and Ensenada.[14][15] Although both earthquakes were larger than the Whittier Narrows earthquake of October 1987, damage was moderate due to their location in the sparsely populated valley.[16]

United States

Telephone services were affected because the earthquake had destroyed some lines. Minor damage was reported in Calipatria, El Centro, Heber and Westmorland.[17] At the epicentral area, damage was limited to fallen chimneys, broken underground pipes, broken windows, and large displacements in roads. A bridge across the New River required repairs on both sides due to liquefaction. At the Desert Test Range Control Center in Westmorland, equipment fell through a window and water tanks tilted. Operations at the facility ceased for several days.[14][13]

About 40 mobile homes were wrenched from their stands. The Southern California Irrigation District estimated $600,000 to $750,000 of damage to canal facilities.[14] The initial earthquake resulted in minor buckling of the canal concrete reinforce while the second shock collapsed many of the concrete.[14] In Calexico, the wall of a furniture store collapsed on automobiles, and in El Centro, another brick wall fell onto a car. Many homes and businesses lost power following the earthquake. Fifty people were injured in Imperial County. California 86 between Westmorland and El Centro was damaged and closed off. California 98 was closed at Ocotillo at the junction with Interstate 8 after a road buckled.

A runway at the Naval Air Facility El Centro was closed but no damage was found after inspection. At the San Onofre Nuclear Plant, there was an "unusual event" declaration but the facility was unaffected.[17] An entry station between Mexicali and Calexico was closed for damage inspection.[18]

In October the same year, Los Angeles was affected by the Whittier Narrows earthquake. The Los Angeles Fire Department received calls from residents asking if there had been an earthquake.[17] Many people were frightened but the city did not experience major damage. In Orange County, people started stocking up on survival appliances including water purification tablets and water bottles for their earthquake preparedness kits. The California Department of Transportation began inspecting freeways for damage.[18] San Diego city councils were having a conference on the 12th floor when the first earthquake struck.[17] The San Diego Fire Department reported minor cracks at five of their stations.[18]

Mexico

In Mexicali—two people—a woman and her child died after being struck by an oncoming vehicle as they were fleeing a factory.[18] At least 35 buildings were damaged including several hospitals; hundreds of people were evacuated from buildings.[18] Structural damage and fires were reported in some buildings. Forty-four people were injured in Baja California Sur; the injuries included broken bones, sprains, cuts and some heart attacks.[16]

See also

References

  1. 1 2 3 Hudnut, K.W.; Seeber, L.; Rockwell, T.K.; Goodmacher, J.; Klinger, R.; Lindvall, S.; McElwain, R. (1989). "Surface ruptures on cross-faults in the 24 November 1987 Superstition Hills, California, earthquake sequence". Bulletin of the Seismological Society of America. 79 (2): 282–296. doi:10.1785/BSSA0790020282 (inactive 1 August 2023).{{cite journal}}: CS1 maint: DOI inactive as of August 2023 (link)
  2. ↑ Singer, Eugene (1998), Geology of California's Imperial Valley: A Monograph by Eugene Singer, archived from the original on 24 March 2011, retrieved 13 December 2020
  3. ↑ Dorsey, Rebecca J. (2002). "Stratigraphic record of Pleistocene initiation and slip on the Coyote Creek fault, lower Coyote Creek, southern California". Contributions to Crustal Evolution of the Southwestern United States. Vol. 365. pp. 251–269. doi:10.1130/0-8137-2365-5.251. ISBN 9780813723655. {{cite book}}: |journal= ignored (help)
  4. ↑ Treiman, J.A.; Lundberg, M.; compilers (1999). "Fault number 125f, San Jacinto fault, Superstition Hills section, in Quaternary fault and fold database of the United States". United States Geological Survey. Retrieved 25 August 2022.
  5. 1 2 3 Magistrale, Harold; Jones, Lucile; Kanamori, Hiroo (April 1989). "The Superstition Hills, California, earthquakes of 24 November 1987". Bulletin of the Seismological Society of America. 79 (2): 239–251. Bibcode:1989BuSSA..79..239M. doi:10.1785/BSSA0790020239. ISSN 0037-1106.
  6. ↑ International Seismological Centre, On-line Bulletin, Thatcham, United Kingdom [Event 453653 ].
  7. ↑ "Earthquakes Strike Imperial Valley in "Superstition Hills Sequence"". California Geology. 41. 1988.
  8. ↑ International Seismological Centre, On-line Bulletin, Thatcham, United Kingdom [Event 453722 ].
  9. ↑ Hudnut, K.W.; Seeber, L.; Pacheco, J. (1989). "Cross-fault triggering in the November 1987 Superstition Hills Earthquake Sequence, southern California". Geophysical Research Letters. 16 (2): 199–202. Bibcode:1989GeoRL..16..199H. doi:10.1029/GL016i002p00199.
  10. ↑ Sharp, R. V.; Budding, K. E.; Boatwright, J.; Ader, M. J.; Bonilla, M. G.; Clark, M. M.; Fumal, T. E.; Harms, K. K.; Lienkaemper, J. J.; Morton, D. M.; O'Neill, B. J.; Ostergren, C. L.; Ponti, D. J.; Rymer, M. J.; Saxton, J. L.; Sims, J. D. (1989). "Surface faulting along the Superstition Hills fault zone and nearby faults associated with the earthquakes of 24 November 1987". Bulletin of the Seismological Society of America. 79 (2): 252–281. Bibcode:1989BuSSA..79..252S. doi:10.1785/BSSA0790020252.
  11. 1 2 Porcella, R.L.; Etheredge, E.; Maley, R.; Switzer, J. (1987), Strong-motion data from the Superstition Hills earthquakes of 0154 and 1315 [GMT], November 24, 1987 (PDF), Open-File Report 87-672, United States Geological Survey, pp. 2–6
  12. ↑ Hudnut, K. W.; Clark, M. M. (1989). "New slip along parts of the 1968 Coyote Creek fault rupture, California". Bulletin of the Seismological Society of America. 79 (2): 451–465. doi:10.1785/BSSA0790020451 (inactive 1 August 2023).{{cite journal}}: CS1 maint: DOI inactive as of August 2023 (link)
  13. 1 2 ANSS. "M 6.2 - 17km WNW of Westmorland, CA". Comprehensive Catalog. U.S. Geological Survey.
  14. 1 2 3 4 Stover, Carl W.; Coffman, Jerry L. (1993). Seismicity of the United States, 1568-1989 (Revised) (1527 ed.). United States Government Printing Office, Washington: U.S. Geological Survey Professional Paper. doi:10.3133/pp1527.
  15. ↑ ANSS. "M 6.6 - 22km W of Westmorland, CA". Comprehensive Catalog. U.S. Geological Survey.
  16. 1 2 Armstrong, Scott (25 November 1987). "California gets more reminders of quake potential. Experts say temblors that hit the lower Imperial Valley and Mexicali, Mexico don't mean more are likely to follow soon". The Christian Science Monitor. Retrieved 26 August 2022.
  17. 1 2 3 4 Feldman, Paul; Reza, H.G. (24 November 1987). "Imperial Valley Rocked by 6.2 Quake; Damage Minor". Los Angeles Times. Retrieved November 21, 2020.
  18. 1 2 3 4 5 Kenneth Reich, H. G. Reza (25 November 1987). "6.3 Quake Injures 94 Along Mexican Border: Imperial Valley Temblor, 2nd in 12 Hours, Damages Buildings in Mexicali, El Centro". Los Angeles Times.
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