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. 2022 Sep 14;609(7927):529–534. doi: 10.1038/s41586-022-04981-x

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© The Author(s) 2022

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 1 — a, Geological setting of the RP and the ITSCs of Reykjanes, Svartsengi, Fagradalsfjall, Krýsuvík and Brennisteinsfjöll extending from west to east are shown in bold¹³. The inset map of Iceland shows the location of the RP. Scale bar, 5 km b, The Fagradalsfjall ITSC and the eruption sites. The extent of the lava field corresponds to 10 May 2021¹⁶. The eruptive vents are shown with red circles. Sampling localities are also shown with white diamonds. Scale bar, 1 km.

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