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Location:
Period:
8 Oct 2024 18:54:30 - 9 Oct 2024 17:05:10 (22 hours 10 minutes)
Volcanoes in 100km radius:
Earthquakes:
25
22 swarms found nearby.
2000
VS20001102.1(19.2km)
2 Nov
2 days 22 hours
63 earthquakes
2002
S20020104.2(23.9km)
4 Jan
5 days 21 hours
156 earthquakes
S20020222.1(27.0km)
22 Feb
6 days 19 hours
453 earthquakes
2005
S20050201.1(25.8km)
31 Jan
1 day 5 hours
32 earthquakes
VS20050510.1(11.2km)
9 May
9 days 8 hours
196 earthquakes
2006
S20060528.1(21.0km)
27 May
1 day 14 hours
27 earthquakes
2008
VS20080209.1(16.1km)
9 Feb
19 days 1 hours
830 earthquakes
S20080603.1(25.2km)
2 Jun
4 days 11 hours
54 earthquakes
S20080626.1(29.0km)
25 Jun
21 hours
27 earthquakes
VS20081120.1(17.9km)
20 Nov
2 days 0 hours
35 earthquakes
2009
S20090920.1(22.0km)
19 Sep
2 days 5 hours
46 earthquakes
30 Dec
2 days 18 hours
112 earthquakes
2010
S20100405.1(26.7km)
4 Apr
48 days 21 hours
7938 earthquakes
PS20100405.1(38.3km)
4 Apr
1 hours
5 earthquakes
S20100405.4(27.3km)
4 Apr
7 days 6 hours
271 earthquakes
S20100405.8(28.5km)
5 Apr
5 days 23 hours
131 earthquakes
S20100408.1(26.0km)
7 Apr
27 days 1 hours
638 earthquakes
2016
S20161127.1(23.7km)
26 Nov
2 days 0 hours
50 earthquakes
2024
S20240212.1(28.5km)
12 Feb
3 days 2 hours
363 earthquakes
S20240512.1(16.7km)
12 May
2 days 10 hours
93 earthquakes
S20240605.1(18.4km)
5 Jun
13 hours
25 earthquakes
2025
S20250101.1(26.4km)
1 Jan
2 hours
28 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20241009.2 Near Puebla, Baja California

A seismic swarm designated S20241009.2 was recorded 7 km east-southeast of Puebla, Baja California, Mexico. The sequence began at 18:54 on 8 October 2024 and concluded at 17:05 on 9 October 2024, spanning 22 hours and 10 minutes. During this period, 25 earthquakes were registered, with magnitudes ranging from 1.2 to 3.2 and focal depths between 16 km and 25 km.

The events clustered tightly in both time and space, characteristic of swarm behavior rather than a mainshock-aftershock sequence. The largest event reached magnitude 3.2 at 06:05 on 9 October, followed closely by a magnitude 3.0 shock later that morning. Most events occurred at mid-crustal depths around 18–24 km, consistent with regional faulting patterns.

This swarm represents the third documented swarm in the area during 2024. Historical records since 2000 show 21 swarms in total, with notable activity in 2008 (four swarms) and 2010 (five swarms). Earlier episodes occurred in 2000, 2002, 2005, 2006, 2009, and 2016. Such recurrent swarms indicate persistent tectonic strain release along local structures.

The Puebla region lies within the Mexicali Valley, part of the Salton Trough tectonic province. This area forms the southern extension of the San Andreas fault system at the boundary between the Pacific and North American plates. Right-lateral strike-slip motion along northwest-trending faults, combined with minor extension, produces frequent small-magnitude seismicity. Geothermal activity and fluid migration in the subsurface further facilitate swarm-type sequences by reducing fault friction.

Seismic monitoring in northern Baja California has improved significantly since the early 2000s, allowing better documentation of low-magnitude events. The current swarm aligns with long-term patterns of distributed microseismicity observed across the Imperial and Cerro Prieto fault zones.

References
SeismoSight internal classification for swarm parameters and historical statistics.
USGS Earthquake Hazards Program for regional tectonic framework of the Salton Trough.
Servicio Sismológico Nacional (Mexico) for historical seismicity context in Baja California.