Seismic Swarm S20170118.1: Analysis of Central Italy's January 2017 Activity
Central Italy lies within the Apennine mountain chain, a region shaped by ongoing extensional tectonics associated with the rollback of the Adriatic plate beneath the Eurasian plate. This geological setting produces frequent normal faulting along northwest-southeast trending structures, resulting in moderate to strong earthquakes at shallow to mid-crustal depths. The area has a well-documented history of seismic events, including the destructive 2009 L’Aquila earthquake and the 2016–2017 sequence that affected the Amatrice–Norcia region.
SeismoSight internal records classify swarm S20170118.1 as occurring in Central Italy. The sequence began at 09:31 on 18 January 2017 and concluded at 18:33 on 23 January 2017, spanning 129 hours and 1 minute. During this interval, 231 earthquakes were registered. Analysis of the first 100 events reveals a rapid onset of activity, with magnitudes ranging from 2.5 to 5.7 and focal depths predominantly between 7 and 15 km. Notable events included a magnitude 5.7 earthquake at 10:14 on 18 January at 7 km depth, followed closely by a magnitude 5.6 event at 10:25 at 10 km depth. A magnitude 5.2 shock occurred at 13:33 the same day at 7 km depth. The majority of events clustered between 10 and 14 km depth, consistent with the regional seismogenic layer.
The swarm exhibited typical swarm characteristics: an absence of a single dominant mainshock and a high rate of smaller events distributed over several days. Early activity featured multiple events above magnitude 4.0 within the first hours, followed by a gradual decline in both frequency and maximum magnitude. Depths remained stable, indicating consistent rupture within the same crustal volume.
Historical statistics maintained by SeismoSight document 16 swarms in Central Italy since 1 January 2000. These occurred in 2007 (1 swarm), 2009 (6 swarms), 2010 (4 swarms), 2011 (3 swarms), and 2016 (2 swarms). Such recurrence underscores the region’s persistent seismic productivity driven by active extension.
This swarm provides further evidence of the distributed deformation that characterizes the central Apennines. Continued monitoring remains essential for understanding strain accumulation along the major fault systems in the area.
References
- SeismoSight internal swarm classification database (S20170118.1 parameters and historical swarm counts).
- Istituto Nazionale di Geofisica e Vulcanologia (INGV) tectonic framework reports on the Apennines.