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Location:
Period:
2 Jan 2002 07:56:11 - 5 Jan 2002 13:50:15 (3 days 5 hours 54 minutes)
Volcanoes in 100km radius:
Earthquakes:
53
49 swarms found nearby.
2001
31 Oct
10 days 17 hours
471 earthquakes
2002
S20021024.3(10.6km)
23 Oct
2 days 17 hours
38 earthquakes
2003
S20031113.1(10.5km)
12 Nov
1 day 17 hours
31 earthquakes
2005
S20050612.1(12.5km)
12 Jun
26 days 19 hours
904 earthquakes
19 Aug
3 days 23 hours
96 earthquakes
2009
S20090818.1(20.4km)
17 Aug
1 day 21 hours
39 earthquakes
2010
8 Feb
3 days 22 hours
44 earthquakes
5 Apr
5 days 18 hours
62 earthquakes
12 Jun
9 days 5 hours
239 earthquakes
7 Jul
35 days 19 hours
1709 earthquakes
2 Dec
10 days 0 hours
68 earthquakes
2011
18 Mar
1 day 23 hours
34 earthquakes
S20110416.1(12.8km)
15 Apr
7 days 6 hours
90 earthquakes
S20110727.1(10.6km)
26 Jul
4 days 1 hours
42 earthquakes
2012
20 May
4 days 2 hours
45 earthquakes
21 Jun
3 days 19 hours
39 earthquakes
29 Jun
2 days 0 hours
31 earthquakes
2013
10 Mar
72 days 2 hours
2118 earthquakes
S20130920.1(13.5km)
19 Sep
1 day 10 hours
31 earthquakes
21 Sep
8 days 10 hours
91 earthquakes
30 Dec
8 days 18 hours
91 earthquakes
2014
7 Aug
1 day 13 hours
28 earthquakes
2015
31 Mar
38 days 7 hours
543 earthquakes
S20150531.1(21.6km)
31 May
2 days 9 hours
45 earthquakes
2016
9 Jun
33 days 4 hours
1773 earthquakes
19 Jul
6 days 5 hours
68 earthquakes
25 Oct
5 days 21 hours
73 earthquakes
S20161230.1(10.4km)
29 Dec
4 days 7 hours
48 earthquakes
2017
9 Nov
2 days 20 hours
44 earthquakes
2018
S20180203.1(27.0km)
2 Feb
28 days 21 hours
426 earthquakes
S20180305.1(25.0km)
4 Mar
19 days 17 hours
203 earthquakes
13 Mar
1 day 13 hours
26 earthquakes
S20180630.1(29.0km)
29 Jun
41 days 14 hours
582 earthquakes
S20180811.1(28.3km)
11 Aug
209 days 15 hours
6032 earthquakes
2019
S20190426.1(28.5km)
25 Apr
1 day 22 hours
37 earthquakes
2020
4 Apr
40 days 3 hours
2928 earthquakes
2 Jun
2 days 12 hours
63 earthquakes
25 Sep
2 days 2 hours
44 earthquakes
2022
13 Jan
4 days 5 hours
157 earthquakes
18 May
1 day 8 hours
29 earthquakes
S20220714.1(13.2km)
13 Jul
1 day 12 hours
26 earthquakes
S20220825.1(16.9km)
25 Aug
1 day 3 hours
27 earthquakes
22 Sep
1 day 18 hours
31 earthquakes
29 Sep
4 days 5 hours
69 earthquakes
31 Dec
2 days 20 hours
86 earthquakes
2023
S20230324.1(25.2km)
23 Mar
2 days 2 hours
50 earthquakes
2024
20 Jun
3 days 0 hours
41 earthquakes
2025
S20250516.1(26.9km)
16 May
4 days 7 hours
45 earthquakes
16 Nov
3 days 16 hours
56 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Activity: The January 2002 Earthquake Swarm Near Borrego Springs, California

The region 15 km NNW of Borrego Springs, California, lies within the tectonically active San Jacinto Fault Zone, part of the broader San Andreas Fault system. This area experiences frequent seismicity due to right-lateral strike-slip motion along the boundary between the Pacific and North American plates. The local geology features sedimentary basins, crystalline basement rocks, and alluvial deposits shaped by ongoing faulting and erosion in the Anza-Borrego Desert.

Earthquake swarms are common in this zone, often linked to fluid migration or stress transfer along fault segments. Historical records indicate low overall swarm frequency, with only one documented swarm since January 2000—the event of 2001. The S20020102.1 swarm began at 07:56 on 2 January 2002 and concluded at 13:50 on 5 January 2002, lasting 77 hours and 54 minutes. It produced 53 earthquakes, with hypocentral depths predominantly between 7 km and 13 km.

The sequence initiated with a magnitude 0.9 event at 10 km depth. The largest shock, magnitude 4.2 at 11 km depth, occurred at 12:11 on 2 January, followed by an aftershock sequence of smaller events mostly below magnitude 2.0. Depths remained stable around 10–13 km for the majority of events, with occasional shallower occurrences near 6–9 km later in the swarm. Magnitudes clustered tightly between 0.7 and 1.9 after the initial peak, showing a typical swarm decay pattern without a clear mainshock-aftershock cascade.

This activity reflects the region's persistent background seismicity, where swarms serve as indicators of fault-zone dynamics rather than precursors to larger quakes. Updated monitoring since 2002 has confirmed continued low-level activity along the same fault segments, consistent with long-term strain accumulation rates of several millimeters per year.

References
SeismoSight internal classification for swarm S20020102.1
USGS Earthquake Hazards Program regional reports on San Jacinto Fault Zone seismicity