
Michelle Parks1, Freysteinn Sigmundsson2, Sara Barsotti1, Halldór Geirsson2, Kristín S. Vogfjörð1, Benedikt Ófeigsson1, Páll Einarsson2
1 Icelandic Meteorological Office, Reykjavik, Iceland.
2 Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, Reykjavik, Iceland.
Overview and background
Volcano-tectonic reactivation of the Reykjanes Peninsula commenced in December 2019, and accounts for, so far, four dike intrusions and three eruptions in the Fagradalsfjall area, and an additional four dike intrusions and three eruptions in the Svartsengi volcanic system, in the area at and near the Sundhnúkur crater row, extending into Grindavík (see Figure 1).
When the unrest started in 2019, a series of earthquakes were detected in the Fagradalsfjall region at depths between 3-7 km. The timing of the reactivation of volcanic activity on the Reykjanes Peninsula was not unexpected, considering knowledge about the previous eruptive period, with the average interval between eruptive activity being about 800-1000 years. The preceding period of eruptive activity, Reykjaneseldar, lasted from 950 to1240. The first clear sign of new magma migration beneath the peninsula was detected on 21 January 2020 – with a strong increase in seismicity and crustal deformation marking the first uplift period in the Svartsengi area, indicative of pressure increase in the crust and interpreted as magma accumulation. The first diking and eruptive activity in the ongoing activity period was, however, in the Fagradalsfjall area. From February 2021 until August 2023, 4 dike intrusions and 3 eruptions occurred there (Figure 1). Seismicity and geodetic data has been crucial for evaluating the nature of the hazards in the areas influenced.
At Fagradalsfjall, the first dike intrusion (the largest to date in this area) took place from 24 February until 19 March 2021, when an eruption began. Ground deformation and seismicity were studied and reported by Sigmundsson et al. (2022). The inferred initial magma inflow rate into the dike was 30-35 m3/s which reduced to <10 m3/s prior to the eruption onset. Our measurements and analyses have shown a strong correlation between inferred inflow rate to the dike immediately before eruption onset and the initial lava extrusion rate, which is very important for determining the risk related to lava flows.
At Svartsengi, the initial period of uplift in January 2020, was followed by 4 additional uplift periods (two of which occurred in 2020 between March – April and May – July, one in May-June 2022 and an additional period from 27 October to 10 November 2023). Magma accumulation in the last period caused sufficient pressure increase to trigger a major dike intrusion on 10 November 2023 under the Sundhnúkur crater row and the town of Grindavík (Figure 2; Sigmundsson et al., 2024).