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Note:This page contains AI-generated content for informational and entertainment purposes only. It may contain inaccuracies. Raw event data is from USGS and EMSC. All statistics, lists, and derived information are generated by this site. Full disclaimerFound an error?
Location:
Period:
3 Jan 2012 07:25:45 - 6 Jan 2012 10:35:14 (3 days 3 hours 9 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
69
15 swarms found nearby.
2004
S20040612.1(24.2km)
12 Jun
1 day 20 hours
35 earthquakes
2005
S20050626.1(27.0km)
26 Jun
4 days 0 hours
149 earthquakes
2011
14 Sep
1 day 10 hours
42 earthquakes
1 Oct
14 days 16 hours
382 earthquakes
19 Oct
4 days 5 hours
106 earthquakes
27 Oct
5 days 18 hours
177 earthquakes
7 Nov
2 days 7 hours
43 earthquakes
10 Nov
5 days 3 hours
128 earthquakes
29 Dec
3 days 3 hours
89 earthquakes
2012
9 Jan
6 days 16 hours
139 earthquakes
31 Jan
3 days 5 hours
62 earthquakes
2014
S20140728.1(27.5km)
28 Jul
8 days 21 hours
346 earthquakes
2015
S20150112.1(28.3km)
12 Jan
3 days 23 hours
157 earthquakes
2017
S20170627.1(15.6km)
27 Jun
4 days 8 hours
69 earthquakes
2018
S20180522.1(28.1km)
22 May
15 hours
26 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20120103.1 Near Calpine, California

Earthquake swarm S20120103.1 was recorded 5 km west of Calpine in Sierra County, California. The sequence began at 07:25 on 3 January 2012 and concluded at 10:35 on 6 January 2012, spanning 75 hours and 9 minutes. During this interval, 69 earthquakes were registered.

The swarm occurred in a region of the northern Sierra Nevada characterized by active faulting along the Sierra Nevada Fault system and associated extensional structures. This tectonic setting accommodates regional strain from Pacific-North American plate interactions, occasionally producing clustered seismicity rather than isolated mainshock-aftershock sequences. Depths of recorded events clustered between 29 km and 33 km, with isolated shallower occurrences near 8–13 km, consistent with activity within the mid-crustal brittle-ductile transition zone of the Sierra Nevada block.

Magnitudes remained low throughout, ranging from –0.6 to 1.7. The largest events reached 1.7 and occurred on 3 January between 22:25 and 23:34. Subsequent activity on 4 and 5 January included several events of magnitude 1.2–1.6, after which the sequence tapered. The absence of a dominant mainshock and the tight spatial-temporal clustering are typical of swarm behavior, often linked to transient fluid pressure changes or slow slip within fractured crust.

Historical records indicate nine swarms have occurred in the same area since 1 January 2000. Earlier episodes were documented in 2004 (one swarm) and 2005 (one swarm), followed by elevated activity in 2011 (seven swarms). This pattern suggests recurring localized stress release within a structurally favorable volume west of Calpine.

The January 2012 swarm adds to the documented record of non-stationary seismicity in the northern Sierra Nevada. Continued monitoring of such sequences provides insight into the interplay between deep crustal processes and surface fault systems in this portion of California.

References
SeismoSight internal swarm classification S20120103.1
USGS Earthquake Catalog (regional Sierra County events)