Location:
Period:
24 Jul 2005 12:43:18 - 29 Jul 2005 08:27:51 (4d 19h 44m)
Volcanoes in 100km radius:
None
Earthquakes:
120
23 swarms found nearby.
2000
27 Sep
5 days 8 hours
79 earthquakes
2001
S20010703.1(22.1km)
2 Jul
11 days 2 hours
150 earthquakes
S20011228.1(10.3km)
28 Dec
9 days 8 hours
171 earthquakes
2003
22 May
3 days 3 hours
44 earthquakes
2004
S20041124.1(11.5km)
23 Nov
5 days 10 hours
80 earthquakes
2006
8 Mar
2 days 10 hours
39 earthquakes
31 Mar
4 days 6 hours
62 earthquakes
2007
28 Nov
9 days 20 hours
183 earthquakes
10 Dec
6 days 14 hours
91 earthquakes
2008
S20081221.1(12.9km)
21 Dec
3 days 10 hours
60 earthquakes
2009
S20090120.1(22.4km)
19 Jan
3 days 5 hours
68 earthquakes
2011
26 Aug
9 days 11 hours
162 earthquakes
19 Dec
3 days 3 hours
59 earthquakes
2012
5 Apr
5 days 8 hours
55 earthquakes
2014
8 Jan
2 days 0 hours
34 earthquakes
2017
S20171113.1(13.0km)
13 Nov
9 days 1 hours
181 earthquakes
2018
S20180124.7(10.8km)
23 Jan
1 day 22 hours
29 earthquakes
S20181102.1(17.1km)
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
4 Sep
1 day 12 hours
27 earthquakes
2025
S20250222.3(20.1km)
22 Feb
1 day 4 hours
26 earthquakes
2026
11 Aug
1 day 3 hours
29 earthquakes
AI-generated article - for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20050725.1: Analysis of Activity Near Soledad, California

Seismic swarm S20050725.1 was recorded in central California, centered 22 km northeast of Soledad. The sequence initiated at 12:43 on 24 July 2005 and concluded at 08:27 on 29 July 2005, spanning 115 hours and 44 minutes. During this interval, 120 earthquakes were registered.

The events clustered at shallow depths, predominantly between 2 km and 4 km, with one outlier reaching 11 km. Magnitudes remained modest, ranging from 0.0 to a peak of 3.4. The largest event occurred at 09:42 on 25 July 2005 at 3 km depth. Subsequent analysis of the first 100 events reveals a rapid onset with multiple magnitude-2+ shocks within the initial 24 hours, followed by a gradual decline in both frequency and size. Depths stayed consistent in the upper crust, consistent with typical swarm behavior in strike-slip regimes.

This swarm fits within the broader tectonic framework of the California Coast Ranges. The region lies near the boundary between the Pacific and North American plates, where right-lateral strike-slip motion along the San Andreas Fault system accommodates most regional strain. Subsidiary structures, including segments of the Calaveras and Sargent faults, contribute to distributed seismicity east of the main trace. Soledad itself occupies the Salinas Valley, underlain by Cenozoic sedimentary rocks overlying Mesozoic basement, with active faulting influencing local groundwater and surface deformation patterns.

Historical records maintained by SeismoSight indicate five prior swarms in the same locale since 1 January 2000. These occurred in 2000 (1 swarm), 2001 (2 swarms), 2003 (1 swarm), and 2004 (1 swarm). Such recurrent, low-magnitude clustering is characteristic of the area and does not necessarily precede larger mainshock events.

The 2005 sequence exhibited classic swarm traits: no single dominant event, tightly grouped hypocenters, and a high proportion of events below magnitude 2.0. Most activity concentrated within the first 48 hours, after which rates decayed steadily until termination.

References

USGS Earthquake Catalog
California Geological Survey Fault Database
SeismoSight Internal Swarm Classification Records