1986 Chalfant Valley earthquake
|Date||21 July 1986|
|Origin time||14:42 UTC|
|Magnitude||6.4 ML |
|Depth||10.8 km (6.7 mi) |
|Countries or regions||California
|Total damage||$2.7 million USD |
|Max. intensity||VI (Strong) |
|Peak acceleration||.46g |
|Foreshocks||5.7 ML July 20 at 14:29 |
|Aftershocks||5.8 ML July 31 at 7:22 |
|Casualties||2 injured |
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 several moderate events, and was the last in a series of three earthquakes that affected southern California and the northern Owens Valley in July 1986.
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. 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.
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 ruturing events in 1915, 1932, and 1954 delineate the Eastern California-Central Nevada seismic zone. 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.
The mainshock occurred at 14:43 UTC and registered 6.4 local magnitude as measured by the UC Berkeley Seismological Lab. Due to the dense array of seismometers in the area, the focal mechanisms of the three largest events were especially well-constrained, and were primarily strike-slip with a minor amount of normal slip.
Foreshock activity began eighteen days prior to the main event, with most of the events remaining below 3.5 local magnitude, but peaked with a 5.7 event that occurred one day before the July 21 mainshock.
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. 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.
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.
- Smith & Priestley 2000, p. 816
- 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
- Smith & Priestley 2000, p. 824
- 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
- Pinter, N. (1995), "Faulting on the Volcanic Tableland, Owens Valley, California", The Journal of Geology (University of Chicago Press) 103 (1): 73–75
- Cockerham & Corbett 1987, p. 285
- 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
- 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.
- George Ramos; Kenneth Reich (July 23, 1986). "More Big Temblors Could Rock Sierra in Next Few Days". Los Angeles Times.
- Smith & Priestley 2000, pp. 815–818
- 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): 280–289
- 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): 813–831
- Historic Earthquakes — United States Geological Survey
- Processed strong-motion data from the Chalfant Valley earthquakes of July 1986 — California Strong Motion Instrumentation Program
- Eastern California Shear Zone Puzzles Seismologists — Science Daily