Location:
Period:
13 Nov 2017 19:31:29 - 22 Nov 2017 21:22:22 (9d 1h 50m)
Volcanoes in 100km radius:
None
Earthquakes:
181
25 swarms found nearby.
2000
S20000928.1(13.3km)
27 Sep
5 days 8 hours
79 earthquakes
2001
S20010703.1(10.0km)
2 Jul
11 days 2 hours
150 earthquakes
28 Dec
9 days 8 hours
171 earthquakes
2003
S20030523.1(16.5km)
22 May
3 days 3 hours
44 earthquakes
2004
S20041124.1(24.1km)
23 Nov
5 days 10 hours
80 earthquakes
2005
S20050725.1(13.0km)
24 Jul
4 days 19 hours
120 earthquakes
2006
S20060308.1(15.2km)
8 Mar
2 days 10 hours
39 earthquakes
31 Mar
4 days 6 hours
62 earthquakes
S20060909.1(26.4km)
8 Sep
1 day 23 hours
63 earthquakes
2007
S20071128.1(21.9km)
28 Nov
9 days 20 hours
183 earthquakes
S20071211.1(15.2km)
10 Dec
6 days 14 hours
91 earthquakes
2008
21 Dec
3 days 10 hours
60 earthquakes
2009
S20090120.1(10.1km)
19 Jan
3 days 5 hours
68 earthquakes
2011
S20110112.1(27.5km)
12 Jan
4 days 12 hours
66 earthquakes
26 Aug
9 days 11 hours
162 earthquakes
S20111220.1(12.9km)
19 Dec
3 days 3 hours
59 earthquakes
2012
S20120406.1(14.3km)
5 Apr
5 days 8 hours
55 earthquakes
2014
S20140108.1(17.6km)
8 Jan
2 days 0 hours
34 earthquakes
2018
S20180124.7(23.4km)
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
S20220905.1(13.7km)
4 Sep
1 day 12 hours
27 earthquakes
2025
22 Feb
1 day 4 hours
26 earthquakes
2026
S20260812.1(10.4km)
11 Aug
1 day 3 hours
29 earthquakes
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Seismic Swarm S20171113.1: Analysis of Activity Near Tres Pinos, California

Seismic swarm S20171113.1 occurred in central California, centered 17 km south-southeast of Tres Pinos in San Benito County. The sequence began at 19:31 UTC on 13 November 2017 and concluded at 21:22 UTC on 22 November 2017, spanning 217 hours and 50 minutes. During this period, 181 earthquakes were recorded.

The swarm region lies within the California Coast Ranges, a tectonically active zone shaped by the interaction between the Pacific and North American plates along the San Andreas Fault system. Tres Pinos sits near the Calaveras Fault, a major right-lateral strike-slip branch of the San Andreas. This setting produces frequent small-to-moderate earthquakes due to distributed shear and fault creep. Depths of events in the swarm clustered between 3 and 6 km, consistent with shallow crustal faulting typical of the area.

Historical records indicate 18 prior swarms in the same locale since 2000. These occurred in 2000 (1 swarm), 2001 (2), 2003 (1), 2004 (1), 2005 (1), 2006 (3), 2007 (2), 2008 (1), 2009 (1), 2011 (3), 2012 (1), and 2014 (1). Such episodic clusters reflect the region's persistent low-level seismicity driven by regional plate motion.

Examination of the first 100 events reveals a classic swarm pattern without a single dominant mainshock. The initial event reached magnitude 4.5 at 6 km depth. Subsequent activity included multiple events above magnitude 2.0, with notable peaks at magnitudes 3.7, 3.1, 2.8 (three instances), and 2.7. Depths remained shallow, predominantly 4–6 km. Magnitudes generally ranged from 0.6 to 2.8 after the opening shock, showing a gradual decline in both frequency and size over the first two days. The sequence exhibited typical swarm characteristics: numerous events of similar magnitude occurring in rapid succession without clear foreshock-mainshock-aftershock progression.

This activity aligns with known behavior along creeping sections of the Calaveras Fault, where aseismic slip and small earthquakes accommodate strain. No damage or injuries were reported from the swarm.

References

USGS Earthquake Catalog (events 2000–2017)
California Geological Survey, Regional Fault Maps
USGS San Andreas Fault System Overview (updated 2023)