Seismic Swarm S20170926.1 Near Anza, California
The seismic swarm designated S20170926.1 occurred 5 km west-southwest of Anza in Riverside County, California. It began at 04:08 UTC on 25 September 2017 and concluded at 01:15 UTC on 28 January 2018, spanning 2,997 hours and 7 minutes. During this interval, 2,217 earthquakes were recorded.
Analysis of the first 100 events reveals predominantly low-magnitude activity. Magnitudes ranged from -0.1 to 2.1, with the majority below 1.0 and only a few exceeding 1.5. Depths varied between 2 km and 17 km, clustering most frequently between 4 km and 6 km. Early events on 25 September included several at depths of 4–6 km with magnitudes of 0.4–2.1, while subsequent days showed continued shallow activity interspersed with occasional deeper occurrences up to 17 km. This pattern is consistent with fluid-driven swarm behavior rather than a single mainshock-aftershock sequence.
The Anza region lies within the Peninsular Ranges province of southern California, part of the broader San Andreas Fault system. The area is influenced by the northwest-trending San Jacinto Fault Zone, which accommodates a significant portion of the Pacific-North America plate boundary slip. Right-lateral strike-slip motion along these faults generates frequent seismicity. The local geology features crystalline basement rocks of the Peninsular Ranges Batholith overlain by sedimentary units, with faulting concentrated along narrow zones that can produce earthquake swarms through aseismic slip and fluid migration.
Historical records indicate 26 swarms in the region since 1 January 2000. These occurred in the following years with the listed event counts: 2002 (1), 2003 (1), 2005 (2), 2009 (1), 2010 (2), 2011 (3), 2012 (1), 2013 (1), 2014 (3), 2015 (2), 2016 (4), and 2017 (5). Such recurrent swarms highlight the persistent seismic hazard in this portion of the fault system.
SeismoSight internal classification.
Data source: SeismoSight swarm catalog S20170926.1.