Location:
Period:
31 Mar 2006 21:48:14 - 5 Apr 2006 04:00:01 (4d 6h 11m)
Volcanoes in 100km radius:
None
Earthquakes:
62
24 swarms found nearby.
2000
27 Sep
5 days 8 hours
79 earthquakes
2001
S20010703.1(13.3km)
2 Jul
11 days 2 hours
150 earthquakes
28 Dec
9 days 8 hours
171 earthquakes
2003
S20030523.1(12.0km)
22 May
3 days 3 hours
44 earthquakes
2004
S20041124.1(20.3km)
23 Nov
5 days 10 hours
80 earthquakes
2005
24 Jul
4 days 19 hours
120 earthquakes
2006
S20060308.1(11.1km)
8 Mar
2 days 10 hours
39 earthquakes
S20060909.1(28.9km)
8 Sep
1 day 23 hours
63 earthquakes
2007
S20071128.1(17.8km)
28 Nov
9 days 20 hours
183 earthquakes
S20071211.1(11.0km)
10 Dec
6 days 14 hours
91 earthquakes
2008
21 Dec
3 days 10 hours
60 earthquakes
2009
S20090120.1(13.6km)
19 Jan
3 days 5 hours
68 earthquakes
2011
26 Aug
9 days 11 hours
162 earthquakes
19 Dec
3 days 3 hours
59 earthquakes
2012
5 Apr
5 days 8 hours
55 earthquakes
2014
S20140108.1(12.9km)
8 Jan
2 days 0 hours
34 earthquakes
2017
13 Nov
9 days 1 hours
181 earthquakes
2018
S20180124.7(19.6km)
23 Jan
1 day 22 hours
29 earthquakes
1 Nov
3 days 21 hours
53 earthquakes
2019
15 Oct
4 days 18 hours
67 earthquakes
2021
2 Jan
4 days 9 hours
53 earthquakes
2022
4 Sep
1 day 12 hours
27 earthquakes
2025
S20250222.3(11.3km)
22 Feb
1 day 4 hours
26 earthquakes
2026
11 Aug
1 day 3 hours
29 earthquakes
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Seismic Swarm S20060401.1: Analysis of Activity Near Soledad, California

Seismic swarm S20060401.1 occurred 23 km east-northeast of Soledad in Monterey County, California. The sequence began at 21:48 on 31 March 2006 and concluded at 04:00 on 5 April 2006, spanning 102 hours and 11 minutes. During this period, 62 earthquakes were recorded, with magnitudes ranging from 0.8 to 4.3 and focal depths predominantly between 0 and 5 km.

The swarm exhibited typical characteristics of clustered microseismicity, featuring a mainshock of magnitude 4.3 on 1 April at 12:25:59 UTC at 1 km depth, followed by numerous aftershocks of lower magnitude. Activity showed temporal clustering, with peak rates on 1 April and a gradual decline thereafter. Depths remained shallow throughout, consistent with brittle failure in the upper crust.

The Soledad region lies within the central Coast Ranges of California, adjacent to the San Andreas Fault system. This transform boundary accommodates right-lateral strike-slip motion between the Pacific and North American plates at rates of approximately 35–40 mm per year. Local geology includes the Gabilan Range to the east and the Salinas Valley, underlain by Mesozoic basement rocks and Cenozoic sedimentary sequences. Nearby faults, including strands of the San Andreas and subsidiary structures such as the Calaveras Fault, contribute to distributed seismicity.

Earthquake swarms in this tectonic setting often arise from fluid migration or aseismic slip triggering brittle failure along fault networks. Historical records indicate recurrent swarm activity in the area since 2000, with seven documented episodes: one each in 2000, 2003, 2004, 2005, and 2006, plus two in 2001. These events underscore the persistent seismic hazard associated with the broader fault system.

The 2006 swarm produced no reported damage or felt intensities beyond light shaking, reflecting the modest magnitudes involved. Such sequences provide valuable data for refining models of fault interaction and stress transfer in transform margins.

References

USGS Earthquake Catalog
California Geological Survey Fault Activity Map
SeismoSight internal swarm classification records