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Location:
Period:
4 Apr 2010 14:02:48 - 23 May 2010 11:30:38 (48 days 21 hours 27 minutes)
Volcanoes in 100km radius:
Earthquakes:
7938
21 swarms found nearby.
2000
VS20001102.1(12.8km)
2 Nov
2 days 22 hours
63 earthquakes
2002
S20020222.1(14.1km)
22 Feb
6 days 19 hours
453 earthquakes
S20020303.1(18.2km)
2 Mar
4 days 12 hours
88 earthquakes
2005
VS20050510.1(17.8km)
9 May
9 days 8 hours
196 earthquakes
2006
S20060528.1(24.0km)
27 May
1 day 14 hours
27 earthquakes
2008
VS20080209.1(18.0km)
9 Feb
19 days 1 hours
830 earthquakes
S20080626.1(16.3km)
25 Jun
21 hours
27 earthquakes
VS20081120.1(13.7km)
20 Nov
2 days 0 hours
35 earthquakes
2009
S20090920.1(21.1km)
19 Sep
2 days 5 hours
46 earthquakes
S20091230.1(27.2km)
30 Dec
2 days 18 hours
112 earthquakes
2010
PS20100405.1(26.2km)
4 Apr
1 hours
5 earthquakes
S20100405.2(22.7km)
4 Apr
20 days 15 hours
840 earthquakes
4 Apr
7 days 6 hours
271 earthquakes
5 Apr
5 days 23 hours
131 earthquakes
7 Apr
27 days 1 hours
638 earthquakes
S20100620.1(10.7km)
19 Jun
13 days 17 hours
161 earthquakes
S20100701.1(22.7km)
30 Jun
2 days 2 hours
35 earthquakes
S20101211.1(29.9km)
11 Dec
2 days 18 hours
50 earthquakes
2024
S20240512.1(24.4km)
12 May
2 days 10 hours
93 earthquakes
S20240605.1(29.7km)
5 Jun
13 hours
25 earthquakes
S20241009.2(26.7km)
8 Oct
22 hours
25 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Analysis of the 2010 Earthquake Swarm Near Progreso, Baja California

The earthquake swarm designated S20100405.1 occurred approximately 20 km west-northwest of Progreso in Baja California, Mexico. It began at 14:02 on 4 April 2010 and concluded at 11:30 on 23 May 2010. During this period of 1173 hours and 27 minutes, a total of 7938 earthquakes were recorded.

This region lies within the Mexicali Valley, part of the active transform boundary between the Pacific and North American plates. The area is influenced by the Imperial and Cerro Prieto fault systems, which accommodate right-lateral strike-slip motion. Shallow crustal seismicity is common here, often manifesting as swarms driven by tectonic loading and fluid migration along fault zones. Depths typically remain under 15 km, consistent with the brittle upper crust in this extensional-transform setting.

The initial 100 events of the swarm exhibited magnitudes between 0.5 and 4.6, with the majority falling in the 2.5–3.9 range. Depths varied from 0 to 14 km, predominantly clustered between 1 and 6 km. Activity commenced with a magnitude 1.9 event at 5 km depth, followed rapidly by several events exceeding magnitude 3.5 within the first hours. The strongest event in this subset reached magnitude 4.6 at 4 km depth on 5 April at 01:52. Temporal clustering was pronounced, with multiple events occurring within minutes during peak phases on 4 and 5 April.

Historical records indicate that ten swarms have occurred in the region since 1 January 2000. These include one swarm each in 2000, 2005, and 2006; two in 2002 and 2009; and three in 2008. Such recurrent swarms underscore the area's propensity for episodic seismic sequences rather than isolated mainshock-aftershock patterns.

The 2010 swarm aligns with the established tectonic framework of the Salton Trough–Gulf of California system, where distributed deformation produces frequent low-to-moderate magnitude events. No single large mainshock dominated the sequence, reinforcing its classification as a classic swarm.

References

USGS Earthquake Catalog (earthquake.usgs.gov)
Servicio Sismológico Nacional, Mexico (www.ssn.unam.mx)
Southern California Earthquake Data Center (scedc.caltech.edu)