“…The ongoing tectonic and volcanic unrest (since 2019) was marked by intense seismicity (Björnsson et al, 2020;Fischer et al, 2022;Hrubcová et al, 2021) and local surface deformation (Cubuk-Sabuncu et al, 2021;Ducrocq et al, 2024;Sigmundsson et al, 2022). As of June 2024, eight eruptions occurred (Bindeman et al, 2022;Eibl et al, 2023;Halldórsson et al, 2022;Sigmundsson et al, 2024; this study) with four of them occurring (i.e., 28 December 2023, and on 14 January, 8 February, and 16 March, 2024) along the 8.3 km-long Sundhnúkur cone row that last erupted at 2.4 ka, immediately north of the town of Grindavík (Jeness & Clifton 2009; Figure 1). The RVB is characterized by Pleistocene and Holocene extrusive volcanic rocks (e.g., J.…”