Long Valley Caldera Seismic Activity
Seimic Network
Earthquakes occurring in the Long Valley area are recorded
by a network of 18 seismic stations within the caldera and an additional
20 stations within a distance of 50 km beyond the caldera boundary. These
stations comprise parts of both the Northern California Seismic Network (NCSN)
operated by the U.S. Geological Survey in Menlo Park, California (stations
names ending in M), and the Nevada seismic network operated by the University
of Nevada, Reno (station names ending in R). The signals from the combined
stations are shared by both networks. The signals telemetered to USGS headquarters
in Menlo Park are processed along with data from the rest of the Northern
California Seismic Network and archived on a mass storage device at the
University of California, Berkeley - USGS data center (http://quake.geo.berkeley.edu)
Historical seismicity
A period of ongoing geologic unrest
in the Long Valley area began in 1978, when a magnitude 5.4
earthquake struck 6 miles southeast of the caldera. This tremblor
ended two decades of low quake activity in eastern
California. The area has since experienced numerous swarms
of earthquakes, especially in the southern part of the caldera
and the adjacent Sierra Nevada (Bailey and Hill, 1990).
Most earthquakes occuring near Long Valley caldera have the broad band
signature typical of tectonic or volcano-tectonics earthquakes with impulsive,
high frequency P and S waves. With the Mammoth Mountain earthquake swarm
in mid 1989, the seismic network begin to detect events with features typical
of long-period volcanic earthquakes. These events may indicate the movement
of magmatic fluids (Pitt and Hill, 1994).
A limited number of anomalous seismic events characterized by non-douple
couple moment tensors and significant volumetric components have been observed
during the 1997 episode of caldera deformation. These anomalous events may
have been triggered by fault normal stress reduction due to high-pressure
fluid injection or pressurization of fluid saturated faults due to magmatic
heating (Dreger et al., 2000).
An update map of the caldera
seismic activity is available on the Long Valley Observatory
web page (http://lvo.wr.usgs.gov)
References
Bailey, R.A., and Hill, D.P., 1990. Magmatic unrest at
Long Valley Caldera, California, 1980-1990: Geoscience Canada, v. 17, no.
3, p. 175-179.
Dreger, D. S., H. Tkalcic, and M. Johnston, 2000. Dilational
processes accompanying earthquakes in the Long Valley Caldera, Science,
288, 122-125.
Pitt, A.M. and Hill, D.P., 1994. Long-period earthquakes
in the Long VAlley caldera region, eastern California, Geophys. Res. Lett.,
21, 1679-1682.
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