Abstract
The Fagradalsfjall eruption commenced on 19 March 2021 on a ~180-m-long eruptive fissure, following a 23-day dike intrusion. New eruptive fissures opened northeast of the initial eruption site on 5, 6–7, 10, and 13 April 2021. The northernmost eruption occurred on 5 April, approximately 1 km northeast of the initial fissure, with the other fissure openings between this and the initial eruptive vents. Still images from web cameras and time-lapse cameras are available for five of the fissure openings. These data show that the eruptions were preceded by steam emitted from cracks in the exact locations where the eruptions started. The time between the first steam observations and the visual appearance of glowing lava ranged between 15 s and 1.5 min during night observations and from 9 to 23 min during daytime observations. The difference in observation time is likely explained by the different lighting conditions. The eruptive vents are located where the north-easterly oriented dike intersected pre-existing north-south-oriented fractures, inferred to be strike-slip faults. These fractures could be identified on a high-resolution ICEYE interferogram as well as on pre-existing aerial photographs and digital elevation models. This interferogram spanned the first day of the eruption (19–20 March 2021). It not only displays deformation related to the pre-eruptive dike intrusion but also shows lineations in locations where eruptive vent openings occurred later in April 2021. These findings demonstrate how Interferometric Synthetic Aperture Radar Analysis (InSAR) can be used to forecast likely locations of subsequent eruptive vent openings, which is of great importance for hazard assessment and defining exclusion zones during fissure eruptions.
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Acknowledgements
We would like to express our gratitude to the Icelandic Coast Guard which assisted us and other scientists to get to areas which were difficult to access on land. We would also like to thank the Iceland Aviation Service and the Garðaflug Corp. as well as the pilots Ú. Henningsson, G. Halldórsdóttir, K. Kárason, G. Árnason, and J. Sverrisson for their assistance during the eruption. B. Abera, A. Bergþórsdóttir, and A. Blischke assisted us during field work. F. Sigmundsson provided an image of the eruption. We would also like to thank the Morgunblaðið newspaper and the Icelandic National Broadcasting Service (Ríkisútvarpið) for the data from their webcameras. The ArcticDEMs were provided by the Polar Geospatial Center under NSF-OPP awards 1043681, 1559691, and 1542736. We thank the editor and the two anonymous reviewers of this paper for their constructive comments. Á.R. Hjartardóttir was partly funded by the Icelandic Research Fund (grant number: 196226-052).
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Low intensity basalt eruptions: the 2021 Geldingadalir and 2022 Meradalir eruptions of the Fagradalsfjall Fires, SW Iceland.
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Hjartardóttir, Á.R., Dürig, T., Parks, M. et al. Pre-existing fractures and eruptive vent openings during the 2021 Fagradalsfjall eruption, Iceland. Bull Volcanol 85, 56 (2023). https://doi.org/10.1007/s00445-023-01670-z
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DOI: https://doi.org/10.1007/s00445-023-01670-z