Caldera 3390 m / 11,122 ft California, 37.7°N / -118.87°W Lista de erupción: 111,000-57,000 years ago (formation of Mammoth Mountain)
Long Term Trends
Seismic trend: Earthquake activity at Long Valley caldera has remained low since mid-1999, averaging just five to ten earthquake per day with magnitudes less than M2 and occasional events M3.
Deformation trend: Renewed uplift of the resurgent dome that began in early 2002 ended in early 2003 largely offsetting the 2 cm of subsidence that accumulated from early 1999 through the end of 2001. The resurgent dome has since shown minor fluctuations in uplift and subsidence but remains roughly 80 cm higher than in the late 1970's.
CO2 trend: The diffuse carbon dioxide gas flux in the Horseshoe Lake tree-kill area has shown little change from the relatively high levels of 50 to 150 tons per day sustained for the past several years.
(Source: Long Valley Observatory Recent Status Report (USGS)
2002 seismic swarm
The M7.9 earthquake at the Denali Fault earthquake of 3 November 2002 was followed and perhaps triggered 60 small tremors in Long Valley.
1996 earthquake swarm
One of the most intense earthquake swarms at the Long Valley caldera occurred in March and April 1996. About 25 earthquakes were recorded at magnitude 3 or higher.
1992 Landers earthquake triggers seismic swarm
On 28 June 1992, a magnitude 7.3 earthquake struck the Mojave Desert 400 km south of Long Valley caldera. 30 seconds after the S wave of the earthquake had passed, an earthquake swarm was triggered beneath the south-moat of Long Valley. This was the first documented case, where a remote earthquake triggered seismic activity in another area.
1990 gas emission - trees dying
During the early 1990's, large amounts of CO2 seeping through the soil caused trees to die off at several places on Mammoth Mountain on the southwest edge of Long Valley Caldera. Such emissions of volcanic gas, originating from the magma chamber, often precede volcanic eruptions. But vice versa, only about 1 in 6 such episodes at calderas is followed by an eruption.
1989 long-lasting seismic swarm
Between May-Dec 1989 a long swarm of small earthquakes occurred under the SE rim of the caldera, probably caused by the intrusion of magma at 3 km depth. It was accompanied by minor deformation (approximately 1 cm of uplift) and included only four M~3 earthquakes, but thousands of smaller earthquakes.
[ocultar] In early May 1989, an 8-month-long swarm of small earthquakes began under Mammoth Mountain on the southwest rim of the caldera and persisted to the end of that year. This swarm appears to have been associated with a dikelike (tabular shape with a vertical orientation) intrusion of magma to depths as shallow as 3 km beneath Mammoth Mountain. Although the swarm was not particularly energetic, it was prolonged. It was accompanied by minor deformation (approximately 1 cm of uplift) and included only four M~3 earthquakes in addition to thousands of smaller earthquakes and frequent spasmodic bursts, the latter of which were likely associated with very-long-period (VLP) earthquakes. This swarm marked the onset of (1) a continuing series of deep, long-period (LP) volcanic earthquakes centered at depths of 10 to 25 km (6 to 15 miles) beneath the southwest flank of Mammoth Mountain and the Devils Postpile, and (2) the diffuse emission of cold, magmatic CO2 in the soil in several areas around the flanks of Mammoth Mountain. Both the deep LP earthquakes and CO2 emissions have continued into 2001, and both appear to be related to the presence of basaltic magma at mid-crustal depths (10 to 25 km or 6 to 15 miles) beneath the southwest flank of Mammoth Mountain and Devils Postpile.
In January 1982, a new group of fumaroles was discovered in the vicinity of Casa Diablo Hot Springs, about 2.5 km E of the earthquake epicenters, and existing fumaroles in the area had become more vigorous.
Source: GVP monthly reports
1980 seismic swarm
Following the M5.8 Wheeler Crest earthquake on 4 October 1978, a series of M3-4 earthquake swarms occurred intermittently within the south moat of Long Valley caldera and beneath the south flank of Mammoth Mountain.
The most intense of these swarms began on 25 May 1980 and included four strong magnitude 6 shocks, three of which struck on the same day.
The first was located just west of Convict Lake near the south margin of the caldera, the second beneath the south moat, the third within the Sierra Nevada block about 5 km south of the caldera. The fourth on 27 May 1980 M6 earthquake was 10 km south of the caldera.
Immediately following these shocks, scientists from the U.S. Geological Survey (USGS) began a reexamination of the Long Valley area and detected other evidence of unrest—a dome-like uplift in the caldera. Their measurements showed that the center of the caldera had risen almost a foot since the summer of 1979, after decades of stability. This continuing swelling, which by early 2000 totaled nearly 2.5 feet and affects more than 100 square miles, is caused by new magma rising beneath the caldera.
Living With a Restless Caldera—Long Valley, California (USGS)
In September 1941, a cluster of four M>5 earthquakes and one M6 event occurred along the Sierra Nevada escarpment ca. 10 km southeast of the Long Valley caldera.
Source: Wallace, T. C., W. U. Savage, and J. S. Barker (1984). The 1941 earthquake sequence near Long Valley
caldera, California (abstract), EOS, Trans. Am. Geophys. Union 45, 1117
19th century activity
In 1872, the magnitude 7.6 Owens Valley earthquake was felt throughout most of California, and a number of moderate (magnitude 5 to 6) earthquakes have shaken the Long Valley area during this century.
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