When an earthquake occurs the stress released is redistributed to the surrounding rocks causing a number of aftershocks which depends on the magnitude of the triggering event (Helmstetter, 2003). The rate of occurrence is governed by the Omori law (Omori, 1894)where n is the number of aftershock, t is the time elapsed from the mainshock occurrence and k, c, and p are experimentally estimated parameters. k depends exponentially on the mainshock magnitude (Helmstetter, 2003), c makes the Omori law normalizable, whereas p controls the velocity of aftershocks rate decay.The Omori law is one of the principal components for the Epidemic Type Aftershock Sequences (ETAS) model (Ogata, 1985(Ogata, , 1998 which views the earthquake occurrence as the superposition of a constant rate of occurrence, μ, and the aftershocks occurrence rate. Aftershocks occur following a cascade process: a parent earthquake can generate some offspring who can, in turn, generate their own offspring. This is a very general characteristic of aftershocks occurrence.Differently from mainshock-aftershock sequences, earthquake swarms are defined as earthquakes clustered in space and time without a triggering mainshock (Hainzl et al., 2012). Swarm activity has been associated to stress changes induced by aseismic processes such as pore pressure changes (Miller et al., 2004) or fluid intrusion (Toda et al., 2002) or seismic ones as observed at the Corinth Gulf (Mesimeri et al., 2016). Mogi (1963) first suggested that swarms occur in regions characterized by high heterogeneity in terms of material properties and stress concentration. Swarms are recorded in volcanic, geothermal or tectonic environments (Hainzl & Fischer, 2002;Tramelli et al., 2021;White & McCausland, 2015) and their triggering mechanism is interpreted as due to processes of injection and/or movement of fluids (Chouet, 1996;Glazner & McNutt, 2021;Hainzl, 2003;Tramelli et al., 2021). Volcanic swarms are usually the main reported seismic precursor for volcanic eruptions especially for volcanoes that have been silent for decades or more (White & McCausland, 2015).