1986 Chalfant Valley earthquake

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1986 Chalfant Valley earthquake
1986 Chalfant Valley earthquake is located in California
Oceanside
Oceanside
Palm Springs
Palm Springs
Bishop
Bishop
1986 Chalfant Valley earthquake
Date 21 July 1986 (1986-07-21)
Origin time 14:42 UTC
Magnitude 6.4 ML [1]
Depth 10.8 km (6.7 mi) [1]
Epicenter 37°32′N 118°27′W / 37.53°N 118.45°W / 37.53; -118.45Coordinates: 37°32′N 118°27′W / 37.53°N 118.45°W / 37.53; -118.45 [2]
Type Strike-slip
Areas affected California
United States
Total damage $2.7 million USD [2]
Max. intensity VI (Strong) [2]
Peak acceleration .46g [1]
Foreshocks 5.7 ML July 20 at 14:29 [1]
Aftershocks 5.8 ML July 31 at 7:22 [1]
Casualties 2 injured [2]

The 1986 Chalfant Valley earthquake struck southern Mono County near Bishop and Chalfant, California at 7:42 a.m. Pacific Daylight Time on July 21. With a Richter magnitude of 6.4 and a maximum perceived intensity of VI (Strong) on the Mercalli intensity scale, the shock injured two people and caused property damage estimated at $2.7 million in the affected areas. The earthquake had a significant foreshock and aftershock sequence that included a few moderate events, and was the last in a series of three earthquakes that affected southern California and the northern Owens Valley in July 1986.

Preface[edit]

July 1986 was an unusually active month for moderate to strong earthquakes in California, with three events occurring in less than two weeks, each with mild to moderate effects. The first of these shocks came on July 8 with a M6.0 event on the Banning fault near Palm Springs and the second event occurred off the coast of Oceanside as a M5.8 shock on July 13. While the earthquake off the southern California coast occurred in an area thought to be capable of generating a tsunami, the earthquake near Palm Springs occurred on a portion of the southern San Andreas Fault system that has been designated a seismic gap, and is a likely location for a very large earthquake. The same seismic gap theory had also been presented for the White Mountains area near Chalfant.[3]

Tectonic setting[edit]

The Owens Valley region

The Owens Valley, located at the western boundary of the Basin and Range Province, is confined by the Sierra Nevada mountain range to the west and the White-Inyo Mountains to the east. The valley was brought about by active tectonics over the last 2–4 million years, and was the scene of a very large earthquake in 1872 that generated surface rupture from Lone Pine in the south to as far north as Big Pine, a distance of approximately 100 kilometers (62 mi). Other large, surface rupturing events in 1915, 1932, and 1954 delineate the Eastern California-Central Nevada seismic zone.[4]

As no large earthquake has occurred between the southern extent of the 1932 Cedar Mountain earthquake's rupture and the northern extent of the 1872 Lone Pine earthquake's rupture in the south (a distance of 130 km (81 mi)), the zone has been labeled the White Mountain seismic gap. The 1934 M6.3 Excelsior Mountains earthquake and the 1986 Chalfant Valley event were several smaller earthquakes that have occurred within the gap, and both generated limited surface faulting and some surface cracking in the Volcanic Tableland, which was created .7 mya from a major volcanic eruption that also formed the Long Valley Caldera northwest of Bishop. An estimated 500 cubic kilometers of material (tephra) produced in the event covers the northern Owens Valley as a rocky landform. The surface of the layered plateau is known as Bishop Tuff and features fumarole mounds and hundreds of north-south oriented fault scarps, many of which are visible on topographic maps, via aerial photography, and satellite imagery.[4]

Earthquake[edit]

USGS ShakeMap for the Chalfant Valley mainshock

The mainshock occurred at 14:42 UTC on July 21 and caused the most damage in the sequence of events. The shock measured 6.4 (local magnitude) as measured by the Berkeley Seismological Laboratory and originated at a depth of approximately 11 kilometers (6.8 mi). The focal mechanisms of the three largest events (the mainshock, along with the significant July 20 foreshock, and the largest aftershock) were primarily strike-slip with a minor amount of normal slip and were especially well-constrained due to the dense array of seismometers in the area that were operated by the University of Nevada, Reno (UNR) and the United States Geological Survey (USGS). The primary foreshock's preferred fault-plane solution indicated left-lateral slip on a fault striking N25°E, but neither the mainshock nor the largest aftershock conformed with their right-lateral slip striking N25°W and N15°W respectively.[5]

Foreshocks[edit]

Data from the UNR and USGS networks was transmitted in real time to Reno and Menlo Park and digitized for later investigation. The foreshock activity was found to have begun eighteen days prior to the main event on July 3, with the onset of a 3.5 event (local magnitude). Activity increased on July 18 with several double events then reduced again in the hours prior to the primary foreshock on July 20. All forty events that were recorded by the UNR and USGS networks before that event were within 2 km (1.2 mi) its epicenter, and another 132 events that were considered its aftershocks were documented in the remaining 24 hours leading up to the mainshock.[6]

Damage[edit]

In Bishop, windows were shattered and ceiling tiles fell in several buildings, and a portion of the brick facade at the First Sierra bank building fell onto the sidewalk. A Burger King restaurant had part of its ceiling come down. Northwest of Bishop, a portion of U.S. Route 395 was blocked temporarily by a landslide. Campers were briefly trapped at the Pleasant Valley Reservoir when a 150 ft (46 m) section of an access road was destroyed as a result of land movement. Both injuries that were reported occurred to the north in Chalfant Valley (minor cuts and injuries from falling objects) where 53 mobile homes were knocked off their foundations and two homes were destroyed. Nearly all the buildings in that small town were affected, with water and sewer lines broken there as well.[7]

Aftershocks
Mag Date (UTC) MMI
5.6 ML July 21 at 14:51 V
5.4 ML July 21 at 22:07 Felt
5.8 ML July 31 at 7:22 VI
Stover & Coffman 1993, pp. 97, 98
Cockerham & Corbett 1987, pp. 285, 286

Many of the mobile homes were able to be remounted on their foundations, but 18–20 of the homes were unable to be repaired. The overall damage from the event was compared with the other events in southern California. While the Oceanside shock caused $200,000 in damage, the Palm Springs event caused an estimated $8 million in damage.[8]

Strong motion[edit]

Further information: Strong ground motion

The foreshock, mainshock, and the two largest aftershocks were recorded by strong motion stations that were operated by the California Strong Motion Instrumentation Program (CSMIP) and the United States Geological Survey. A total of 36 seismograms were captured from 11 stations, including a two story steel frame building, the Long Valley Dam, and several free field stations. The Chalfant strong motion station recorded the largest horizontal accelerations for the foreshock, mainshock, and the July 21 M.5.6 aftershock of .28g, .46g, and .17g. The instruments at the building on North Main street in Bishop recorded all four shocks and indicated .25g at ground level and .4g on the roof, both during the mainshock. The station at the earthen Long Valley Dam had produced many quality recordings since being put into operation in 1979 and saw mainshock accelerations of .09g on bedrock, and .24g on an upper abutment.[9]

References[edit]

  1. ^ a b c d e Smith, K. D.; Priestley, K. F. (2000), Faulting in the 1986 Chalfant, California, Sequence: Local tectonics and earthquake source parameters, Bulletin of the Seismological Society of America (Seismological Society of America) 90 (4): 816, 824, doi:10.1785/0119990129 
  2. ^ a b c d 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. 97, 107 
  3. ^ Pacheco, J.; Nabelek, J. (1988), Source mechanisms of three moderate California earthquakes of July 1986, Bulletin of the Seismological Society of America (Seismological Society of America) 78 (6): 1907–1909 
  4. ^ a b Pinter, N. (1995), Faulting on the Volcanic Tableland, Owens Valley, California, The Journal of Geology (University of Chicago Press) 103 (1): 73–76, doi:10.1086/629723 
  5. ^ Cockerham, R. S.; Corbett, E. J. (1987), The July 1986 Chalfant Valley, California, earthquake sequence: Preliminary results, Bulletin of the Seismological Society of America (Seismological Society of America) 77 (1): 280–285 
  6. ^ Smith, K. D.; Priestley, K. F. (1988), The foreshock sequence of the 1986 Chalfant, California, earthquake, Bulletin of the Seismological Society of America (Seismological Society of America) 78 (1): 173, 177 
  7. ^ George Ramos; Kenneth Reich (July 22, 1986). "6.1 Quake Jars Eastern Sierra : State's 4th Temblor in Two Weeks Damages Homes, Traps Campers". Los Angeles Times. 
  8. ^ George Ramos; Kenneth Reich (July 23, 1986). "More Big Temblors Could Rock Sierra in Next Few Days". Los Angeles Times. 
  9. ^ Sherburne, R. W.; Parke, D. L.; Huang, M. J.; Shakal, A. F. (1988), CSMIP strong-motion records from the Chalfant Valley, California earthquakes, Report OSMS 86-06, California Strong Motion Instrumentation Program, California Division of Mines and Geology, pp. 1–3 

External links[edit]