Location:
Period:
5 Apr 2012 21:47:39 - 11 Apr 2012 06:01:37 (5d 8h 13m)
Volcanoes in 100km radius:
None
Earthquakes:
55
23 swarms found nearby.
2000
27 Sep
5 days 8 hours
79 earthquakes
2001
S20010703.1(23.2km)
2 Jul
11 days 2 hours
150 earthquakes
S20011228.1(11.3km)
28 Dec
9 days 8 hours
171 earthquakes
2003
22 May
3 days 3 hours
44 earthquakes
2004
S20041124.1(10.7km)
23 Nov
5 days 10 hours
80 earthquakes
2005
24 Jul
4 days 19 hours
120 earthquakes
2006
8 Mar
2 days 10 hours
39 earthquakes
31 Mar
4 days 6 hours
62 earthquakes
2007
28 Nov
9 days 20 hours
183 earthquakes
10 Dec
6 days 14 hours
91 earthquakes
2008
S20081221.1(13.9km)
21 Dec
3 days 10 hours
60 earthquakes
2009
S20090120.1(23.4km)
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
2014
8 Jan
2 days 0 hours
34 earthquakes
2017
S20171113.1(14.3km)
13 Nov
9 days 1 hours
181 earthquakes
2018
23 Jan
1 day 22 hours
29 earthquakes
S20181102.1(18.2km)
1 Nov
3 days 21 hours
53 earthquakes
2019
S20191016.1(10.5km)
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(21.1km)
22 Feb
1 day 4 hours
26 earthquakes
2026
11 Aug
1 day 3 hours
29 earthquakes
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Seismic Swarm S20120406.1 Near Greenfield, California

Seismic swarm S20120406.1 occurred approximately 24 km northeast of Greenfield in Monterey County, California. The sequence began at 21:47 UTC on 5 April 2012 and concluded at 06:01 UTC on 11 April 2012, spanning 128 hours and 13 minutes. During this interval, 55 earthquakes were recorded, with magnitudes ranging from 0.5 to 3.6 and focal depths between 2 km and 10 km. The largest event, magnitude 3.6, occurred at 02:55 UTC on 6 April at a depth of 5 km. Subsequent notable events included several magnitude 2.0–2.5 shocks clustered between 6 and 8 April, primarily at depths of 4–5 km. The majority of activity remained below magnitude 2.0, consistent with typical swarm characteristics where energy release occurs through numerous small events rather than a dominant mainshock followed by aftershocks. The swarm region lies within the central California Coast Ranges, part of the broader San Andreas Fault system. This tectonically active zone accommodates right-lateral strike-slip motion between the Pacific and North American plates at a rate of approximately 35–38 mm per year. Local faulting includes strands of the San Andreas Fault itself and subsidiary structures such as the Calaveras and Sargent faults to the north. Crustal deformation in the area is influenced by both regional plate motion and local restraining bends that can promote distributed seismicity. Earthquake swarms in central California often reflect transient stress changes, possibly driven by aseismic slip or fluid migration along fault zones. Depths recorded during this swarm (mostly 3–7 km) align with the brittle-ductile transition zone in this portion of the San Andreas system, where small-magnitude events are common. No surface rupture or significant damage was associated with the sequence. Historical records indicate recurrent swarm activity in the region. Since 1 January 2000, 14 swarms have been documented near Greenfield, occurring in the years 2000 (1), 2001 (2), 2003 (1), 2004 (1), 2005 (1), 2006 (2), 2007 (2), 2008 (1), 2009 (1), and 2011 (2). This pattern suggests episodic strain release along the same fault network.

References

USGS Earthquake Hazards Program – San Andreas Fault System overview
California Geological Survey – Regional fault and seismicity maps
USGS Earthquake Catalog (general tectonic framework)