At 4:57 a.m. local time on June 28, 1992, a magnitude 7.3 earthquake awoke much of Southern California. Though it turned out it was not the so-called "Big One" as many people would think, it was still a very strong earthquake. The shaking lasted for two to three minutes. Although this earthquake was much more powerful than the 1994 Northridge earthquake, the damage and loss of life were minimized by its location in the sparsely-populated Mojave Desert. The earthquake was a right-lateral strike-slip event, and involved the rupture of several different faults over a length of. The names of those that were involved are the Johnson Valley, Kickapoo, Homestead Valley, Homestead/Emerson, Emerson Valley and Camp Rock faults. The surface rupture extended for, with a maximum horizontal displacement of and a maximum vertical displacement of.
Damage
Damage to the area directly surrounding the epicenter was severe. Roads were buckled, buildings and chimneys collapsed. There were also large surface fissures. To the west in the Los Angeles Basin damage was much less severe. The majority of damage in the Los Angeles area involved items which had fallen off shelves. Unlike the 1994 Northridge earthquake nineteen and a half months later, no freeway bridges collapsed because of the epicenter's remote location. Electricity was cut to thousands of residents, but was generally restored within two to three hours. There was also some damage to homes from water displaced from swimming pools. Loss of life in this earthquake was minimal. Two people died as a result of heart attacks, and a 3-year-old boy from Massachusetts, who was visiting Yucca Valley with his parents, died when bricks from a chimney collapsed into a living room where he was sleeping. More than 400 people sustained injuries as a result of the earthquake.
Related events
The quake was preceded by the 6.1 magnitude Joshua Tree earthquake at 4:51 on April 23, 1992, which was south of the future Landers epicenter. The 6.5 magnitude Big Bear earthquake, which hit about three hours after the Landers mainshock, was originally considered an aftershock. However, the United States Geological Survey determined that this was a separate, but related, earthquake. These two earthquakes are considered a regional earthquake sequence, rather than a main shock and aftershock. The 5.7 magnitude Little Skull Mountain earthquake the following day, June 29, 1992, at 10:14 UTC near Yucca Mountain, Nevada, is also considered part of the regional sequence and may have been triggered by surface wave energy produced by the Landers earthquake. Foreshock activity, in the form of a significant increase in micro-earthquakes, was observed at Little Skull Mountain following the Landers earthquake, and the activity continued until the main LSM earthquake.
Theories
The Landers earthquake and the other large quakes associated with it in the Mojave region have been attributed to two possible long-term trends. One of these is that the San Andreas Fault may be in the process of being replaced as the plate boundary by a new trend across the Mojave and east of the Sierra Nevada Mountains. The other is that these quakes were a manifestation of the propagation of rifting coming up from the Gulf of California. Research is ongoing.
