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Location:
Period:
1 Jul 2012 03:25:20 - 4 Jul 2012 05:47:11 (3 days 2 hours 21 minutes)
Volcanoes in 100km radius:
Earthquakes:
77
M 7.0+:
22 swarms found nearby.
2000
S20000502.1(24.6km)
1 May
4 days 19 hours
60 earthquakes
VS20001102.1(25.8km)
2 Nov
2 days 22 hours
63 earthquakes
2001
S20011209.1(26.7km)
8 Dec
3 days 15 hours
57 earthquakes
2002
S20020222.1(18.6km)
22 Feb
6 days 19 hours
453 earthquakes
S20020303.1(14.1km)
2 Mar
4 days 12 hours
88 earthquakes
2006
S20060528.1(22.8km)
27 May
1 day 14 hours
27 earthquakes
2008
VS20080209.1(26.9km)
9 Feb
19 days 1 hours
830 earthquakes
S20080626.1(16.1km)
25 Jun
21 hours
27 earthquakes
VS20081120.1(26.6km)
20 Nov
2 days 0 hours
35 earthquakes
2009
S20090920.1(21.0km)
19 Sep
2 days 5 hours
46 earthquakes
2010
4 Apr
1 hours
5 earthquakes
S20100405.4(22.6km)
4 Apr
7 days 6 hours
271 earthquakes
S20100410.1(25.1km)
9 Apr
1 day 9 hours
29 earthquakes
S20100501.1(13.3km)
1 May
4 days 3 hours
63 earthquakes
S20100508.1(29.3km)
7 May
6 days 19 hours
95 earthquakes
S20100517.1(21.8km)
16 May
23 days 11 hours
365 earthquakes
S20100620.1(21.0km)
19 Jun
13 days 17 hours
161 earthquakes
24 Jul
9 days 17 hours
117 earthquakes
15 Aug
5 days 9 hours
45 earthquakes
11 Dec
2 days 18 hours
50 earthquakes
2024
S20240512.1(27.4km)
12 May
2 days 10 hours
93 earthquakes
S20240605.1(29.4km)
5 Jun
13 hours
25 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20120701.1: Analysis of Activity Near Alberto Oviedo Mota, Baja California

Seismic swarm S20120701.1 occurred 11 km west of Alberto Oviedo Mota in Baja California, Mexico. The sequence began at 03:25 on 1 July 2012 and concluded at 05:47 on 4 July 2012. Over 74 hours and 21 minutes, 77 earthquakes were recorded, with magnitudes ranging from 1.5 to 4.6 and depths predominantly between 0 and 19 km.

This swarm exemplifies typical clustered seismicity in the region, where multiple events occur without a dominant mainshock. The largest events reached magnitude 4.6 at shallow depths of 2–9 km, consistent with shallow crustal faulting. Activity peaked in the first 24 hours, with 43 events on 1 July, followed by a steady decline. Smaller events clustered at depths around 9 km, suggesting a concentrated source volume along a fault segment.

The location lies within the Mexicali Valley, part of the Pacific–North American plate boundary. Here, right-lateral strike-slip motion occurs along the Cerro Prieto and Imperial faults, which form the northern extension of the Gulf of California rift system. The area experiences frequent low-to-moderate seismicity due to transtensional tectonics and geothermal activity associated with the Cerro Prieto volcanic field.

Historical data indicate 20 swarms in the region since 2000, with notable concentrations in 2000 (two events), 2008 (three), and especially 2010 (ten). The 2010 Sierra El Mayor–Cucapah earthquake (M 7.2) occurred only 12 km from the 2012 swarm center on 4 April 2010, highlighting the persistent seismic hazard along these faults. Post-2010 activity likely reflects ongoing stress adjustment within the fault network.

Such swarms provide insight into fluid migration and aseismic slip processes common in geothermal and rift settings. Depths under 10 km for most events align with brittle failure in the upper crust, while occasional deeper shocks (up to 19 km) indicate limited extension into the transition zone.

References

USGS Earthquake Catalog
Servicio Sismológico Nacional (Mexico)
SeismoSight internal swarm classification S20120701.1