1992 Landers earthquake

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1992 Landers earthquake
Landers quake bowling alley.jpg
Damage to the Yucca Lanes Bowling Center from the 1992 quake
USGS ShakeMap - 1992 Landers earthquake.jpg
USGS ShakeMap made for the event
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Palm Springs
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Los Angeles
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UTC  time1992-06-28 11:57:35
ISC  event 289086
USGS-ANSS ComCat
Local dateJune 28, 1992
Local time4:57:35 am PDT
Duration2−3 minutes
Magnitude7.3 Mw
Depth0.68 mi (1.09 km)
Epicenter 34°13′01″N116°25′59″W / 34.217°N 116.433°W / 34.217; -116.433 [1]
Type Strike-slip
Areas affected Southern California
United States
Total damage$92 million [2]
Max. intensity MMI IX (Violent) [3]
Foreshocks6.1 Mw April 23 at 4:51 [4]
Casualties3 killed
400+ injured

The 1992 Landers earthquake occurred on Sunday, June 28 with an epicenter near the town of Landers, California, in San Bernardino County. [5] The shock had a moment magnitude of 7.3 and a maximum Mercalli intensity of IX (Violent). [6]

Contents

Earthquake

At 4:57 a.m. local time (11:57 UTC) 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 75 to 85 km (47 to 53 mi). [5] [7] The names of those that were involved are the Johnson Valley, Kickapoo (also known as Landers), Homestead Valley, Homestead/Emerson, Emerson Valley and Camp Rock faults. [5] [7]

The surface rupture extended for 70 km (43 mi), with a maximum horizontal displacement of 5.5 m (18 ft) and a maximum vertical displacement of 1.8 m (5.9 ft). [8]

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 the damage in the Los Angeles area involved items that 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. [9] More than 400 people sustained injuries as a result of the earthquake. [2]

Recording of the June 28 earthquakes on a seismograph at Griffith Observatory The Double Earthquakes of June 28, 1992.jpg
Recording of the June 28 earthquakes on a seismograph at Griffith Observatory

The quake was preceded by the 6.1 magnitude Joshua Tree earthquake at 4:51 on April 23, 1992 (UTC), which was south of the future Landers epicenter. [10] [11] 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. [12]

The magnitude 5.7 Little Skull Mountain (LSM) 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. [13]

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 (between the North American plate and the Pacific plate) 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. [14]

The earthquake is featured in the television documentary series produced by GRB Entertainment, aired on The Learning Channel and other television channels around the world, about natural disasters titled Earth's Fury (also known internationally as Anatomy of Disaster) in an episode entitled "Earthquake!" [15]

See also

Related Research Articles

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The 2019 Ridgecrest earthquakes of July 4 and 5 occurred north and northeast of the town of Ridgecrest, California located in Kern County and west of Searles Valley. They included three initial main shocks of Mw magnitudes 6.4, 5.4, and 7.1, and many perceptible aftershocks, mainly within the area of the Naval Air Weapons Station China Lake. Eleven months later, a Mw  5.5 aftershock took place to the east of Ridgecrest. The first main shock occurred on Thursday, July 4 at 10:33 a.m. PDT, approximately 18 km (11.2 mi) ENE of Ridgecrest, and 13 km (8.1 mi) WSW of Trona, on a previously unnoticed NE-SW trending fault where it intersects the NW-SE trending Little Lake Fault Zone. This quake was preceded by several smaller earthquakes, and was followed by more than 1,400 detected aftershocks. The M 5.4 and M 7.1 quakes struck on Friday, July 5 at 4:08 a.m. and 8:19 p.m. PDT approximately 10 km (6 miles) to the northwest. The latter, now considered the mainshock, was the most powerful earthquake to occur in the state in 20 years. Subsequent aftershocks extended approximately 50 km (~30 miles) along the Little Lake Fault Zone.

The 1933 Sumatra earthquake or Liwa earthquake occurred in West Lampung Regency, Lampung Province, Indonesia on June 25. The earthquake had an estimated surface-wave magnitude (Ms ) of 7.7 occurring at a shallow depth of 20 km. It had an epicenter onshore, devastating the city of Liwa. At least 788 people were reported killed, although the death toll may have been in the thousands. Aftershocks followed, including one which was strong enough to cause additional fatalities. The mainshock also triggered a nearby volcanic eruption two weeks later, killing some people.

The 1992 Joshua Tree earthquake occurred at 9:50:25 p.m. PDT on April 22 in Southern California. The magnitude 6.2 earthquake struck under the Little San Bernardino Mountains, near the town of Joshua Tree, California. Though no deaths were reported, the earthquake caused 32 injuries. A maximum Mercalli intensity of VII was observed in Joshua Tree and caused light to moderate damage. The event preceded the Landers and Big Bear earthquakes by two months but is now recognized as the beginning of a series of major earthquakes that culminated in two events on June 28, 1992.

References

  1. "Landers Earthquake". Southern California Earthquake Data Center. Archived from the original on March 5, 2014. Retrieved August 15, 2014.
  2. 1 2 "M7.3 – Southern California". United States Geological Survey.
  3. "M 7.3 – Landers, California Earthquake".
  4. Hauksson, E.; Jones, L. M.; Hutton, K.; Eberhart-Phillips, D. (1993). "The 1992 Landers Earthquake Sequence: Seismological observations" (PDF). Journal of Geophysical Research. 98 (B11): 19835–19858. Bibcode:1993JGR....9819835H. doi:10.1029/93jb02384.
  5. 1 2 3 "Landers Earthquake". Southern California Earthquake Data Center. Archived from the original on October 25, 2007. Retrieved November 4, 2007.
  6. "M 7.3 – Landers, California Earthquake".
  7. 1 2 Sébastien Leprince; François Ayoub; Yann Klinger; Jean-Philippe Avouac (July 2007). "Co-Registration of Optically Sensed Images and Correlation (COSI-Corr): An operational methodology for ground deformation measurements". 2007 IEEE International Geoscience and Remote Sensing Symposium (PDF). IEEE International. pp. 1943–1946. doi:10.1109/IGARSS.2007.4423207. ISBN   978-1-4244-1211-2. S2CID   10413144.
  8. National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information. "Significant Earthquake Information". doi:10.7289/V5TD9V7K . Retrieved March 21, 2024.
  9. Gebe Martinez (June 30, 1992). "The Landers and Big Bear Quakes : Death of Toddler Touches Many in Close-Knit Town". Los Angeles Times. Archived from the original on May 2, 2011. Retrieved December 10, 2021.
  10. "The 1992 Landers Earthquake Sequence: Seismological Observations". Archived from the original on September 29, 2012. Retrieved November 5, 2010.
  11. Boyer, Edward J.; Reich, Kenneth (April 23, 1992). "6.1 Quake Felt in Wide Area of Southland". Los Angeles Times . Retrieved April 12, 2020.
  12. "El Salvador". Earthquake Report. USGS Earthquake Hazards Program. Archived from the original on August 11, 2014. Retrieved October 10, 2008.
  13. Smith, K. D. (2001). "The 1992 Little Skull Mountain Earthquake Sequence, Southern Nevada Test Site" (PDF). Bulletin of the Seismological Society of America. 91 (6): 1595–1606. Bibcode:2001BuSSA..91.1595S. doi:10.1785/0120000089.
  14. LaMacchia, Diane (July 17, 1992). "Yucca Valley earthquake surprised experts". Lawrence Berkeley National Laboratory . Archived from the original on October 12, 2007. Retrieved November 4, 2007.
  15. "Earthquake!". Anatomy of Disaster. Season 1. Episode 3. 1997. The Learning Channel. Archived from the original on December 14, 2021. Retrieved October 6, 2020 via YouTube.

Further reading