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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:
18 Jul 2008 14:09:32 - 23 Jul 2008 01:18:17 (4 days 11 hours 8 minutes)
Volcanoes in 100km radius:
Earthquakes:
64
8 swarms found nearby.
2002
S20020727.1(13.7km)
26 Jul
1 day 13 hours
35 earthquakes
2009
S20090314.1(29.8km)
14 Mar
6 days 18 hours
105 earthquakes
S20090730.1(12.0km)
29 Jul
2 days 2 hours
46 earthquakes
S20090811.1(11.4km)
10 Aug
2 days 7 hours
47 earthquakes
24 Aug
1 day 21 hours
100 earthquakes
2014
12 Jan
3 days 18 hours
70 earthquakes
S20140215.1(12.7km)
14 Feb
1 day 14 hours
65 earthquakes
2019
S20190611.1(24.7km)
11 Jun
1 day 18 hours
29 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm Near Beatty, Nevada: July 2008 Analysis

The seismic swarm designated S20080719.1 occurred approximately 30 km north of Beatty, Nevada, in the Basin and Range Province. It began at 14:09 on 18 July 2008 and concluded at 01:18 on 23 July 2008, spanning 107 hours and 8 minutes. During this interval, 64 earthquakes were recorded, with magnitudes ranging from -0.1 to 2.6 and focal depths between 0 and 6 km. All events remained shallow, consistent with activity along local normal faults in an extensional tectonic regime.

This swarm exemplifies clustered seismicity without a dominant mainshock-aftershock sequence. Magnitudes stayed predominantly below 1.0, with only four events exceeding 1.5. The largest, magnitude 2.4 and 2.6, occurred within minutes of each other near midnight on 21 July at depths of 4 km. Such patterns align with fluid migration or stress triggering along pre-existing fractures common in the region.

Geologically, the area north of Beatty features Quaternary normal faults linked to the Walker Lane shear zone and the broader Pacific-North American plate boundary. The crust experiences ongoing extension at rates of several millimeters per year, producing frequent small-magnitude events. Proximity to the Nevada National Security Site and former Yucca Mountain repository studies has yielded extensive fault-mapping data, confirming active structures capable of hosting swarms.

Historical records indicate sparse swarm activity since 2000, with only one prior episode noted in 2002 within the monitored catalog. This low recurrence underscores the episodic nature of clustered events amid background seismicity rates typical of southern Nevada.

Monitoring networks operated by the USGS and regional partners provide continuous detection in this sparsely populated area, aiding hazard assessment for nearby infrastructure and communities. Depths confined to the upper crust suggest limited rupture potential for individual events, though cumulative swarm effects warrant continued observation.

References

USGS Earthquake Catalog (earthquake.usgs.gov)
Nevada Seismological Laboratory historical data
Basin and Range Province tectonic summaries from USGS Professional Papers