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Note:This page contains AI-generated content for informational and entertainment purposes only. It may contain inaccuracies. Raw event data is from USGS and EMSC. All statistics, lists, and derived information are generated by this site. Full disclaimerFound an error?
Location:
Period:
6 Jun 2000 19:27:31 - 8 Jun 2000 21:30:42 (2 days 2 hours 3 minutes)
Volcanoes in 100km radius:
Earthquakes:
60
8 swarms found nearby.
2000
4 Mar
17 hours
71 earthquakes
9 May
21 hours
65 earthquakes
21 Jun
2 days 3 hours
130 earthquakes
31 Jul
1 day 1 hours
31 earthquakes
17 Aug
1 day 8 hours
45 earthquakes
2013
S20130213.1(26.2km)
12 Feb
11 days 5 hours
345 earthquakes
2020
S20200726.1(28.9km)
25 Jul
11 days 0 hours
125 earthquakes
2021
S20210117.2(28.6km)
17 Jan
1 day 7 hours
25 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20000607.2: Analysis of Activity East of Benton, California

Seismic swarm S20000607.2 was recorded 22 km east of Benton, California, in Mono County. The sequence began at 19:27 on 6 June 2000 and concluded at 21:30 on 8 June 2000, encompassing 60 earthquakes over 50 hours and 3 minutes. This event represents the first of two swarms documented in the region since 1 January 2000. Magnitudes during the swarm ranged from -0.8 to 3.2, with the majority of events below 2.0. Depths clustered between 5 km and 12 km, indicating shallow crustal activity typical of the area. The largest event, magnitude 3.2, occurred at 18:20 on 7 June at 6 km depth. Subsequent notable shocks included multiple magnitude 2.1 events on 7 and 8 June. The swarm exhibited a rapid onset followed by a gradual decline in frequency, consistent with fluid-driven or stress-release processes in extensional settings. The location lies within the western Basin and Range Province, where active normal faulting accommodates regional extension. Nearby structures include the White Mountains fault zone and proximity to the Long Valley Caldera volcanic complex, both known for episodic seismicity. Historical records show that such swarms often occur without producing surface rupture or larger mainshock-aftershock sequences. This swarm provides insight into the distributed, low-magnitude nature of seismicity east of Benton. Most events remained under magnitude 1.5, with only a handful exceeding 2.0, underscoring the swarm's diffuse character rather than a single dominant rupture.

References

USGS Earthquake Catalog (earthquake.usgs.gov)
California Geological Survey Regional Fault Maps
Nevada Seismological Laboratory Regional Seismicity Reports