Seismic Swarm in the Strait of Gibraltar: December 2021 Event Analysis
The Strait of Gibraltar marks a critical tectonic boundary between the African and Eurasian plates, where oblique convergence drives ongoing deformation across the Gibraltar Arc. This complex zone encompasses the Betic Cordillera in southern Spain and the Rif Mountains in northern Morocco, featuring a combination of thrust faults, strike-slip structures, and remnants of ancient subduction. Seismicity in the region typically occurs at shallow to intermediate depths, reflecting both crustal faulting and deeper slab-related processes.
Seismic swarms represent clusters of earthquakes closely spaced in time and location without a single dominant mainshock. Swarm S20211206.1 began at 08:13 on 5 December 2021 and concluded at 02:29 on 11 December 2021, spanning 138 hours and 16 minutes. During this interval, 57 earthquakes were recorded within the Strait of Gibraltar. Magnitudes ranged from 2.0 to 3.7, with the largest event measuring 3.7 at a depth of 10 km on 5 December. Depths varied between 0 km and 30 km, indicating activity across multiple crustal levels.
The temporal distribution showed the highest frequency on the first day, followed by a gradual decline. Early events included several above magnitude 3.0, such as a 3.4 at 10 km depth and a 3.2 at 20 km depth. Later stages featured predominantly smaller events below magnitude 2.5, with occasional spikes such as a 3.0 on 10 December. Depths remained variable throughout, with clusters at 7–10 km and 20–30 km suggesting involvement of distinct fault segments or rheological boundaries.
Historical records since 2000 document six swarms in the same area. One occurred in 2016, while five took place in 2021, underscoring elevated swarm activity during that year. These episodes typically involve low-to-moderate magnitudes and do not culminate in damaging events, consistent with the background tectonic strain accumulation along the plate boundary.
Such swarms contribute to understanding stress transfer and fluid migration within the Gibraltar Arc. Continued monitoring supports regional hazard assessment, particularly given the proximity to densely populated coastal zones in Spain and Morocco. The December 2021 sequence aligns with the established pattern of diffuse, moderate seismicity that characterizes this convergent margin.
References
- United States Geological Survey Earthquake Catalog
- European-Mediterranean Seismological Centre Data Archive
- Instituto Geográfico Nacional (Spain) Seismic Reports