1987 Superstition Hills earthquakes

The Elmore Ranch earthquake occurred at 5:53 pm measuring M_w  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]

The Superstition Hills earthquake measured M_w  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]

A USGS ShakeMap for the November 24 main shock.

Strong motion data was first compiled by the U.S. 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]

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]

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 stoking 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]

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]