EGU25-17683, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-17683
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
Impact of Cooling Rate on Rheology and Emplacement Dynamics of Basaltic Lava Flows: Insights from the 2023-2024 Sundhnúksgígar Eruption (Iceland)
1,2,4,1,1- 1Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy (fabrizio.difiore@ingv.it)
- 2Dipartimento di Scienze, Università degli Studi Roma Tre, Roma, Italy
- 3Institute of Science, Technology and Sustainability for Ceramics (ISSMC) of the National Research Council (CNR), Faenza, Italy
- 4Nordic Volcanological Centre, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
- 5Dipartimento di Scienze della Terra, Sapienza-Università di Roma, Roma, Italy
- 6Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany
How to cite: Di Fiore, F., Vona, A., Di Genova, D., Caracciolo, A., Pontesilli, A., Calabro', L., Giuliani, G., Mollo, S., Bondar, D., Nazzari, M., Romano, C., and Scarlato, P.: Impact of Cooling Rate on Rheology and Emplacement Dynamics of Basaltic Lava Flows: Insights from the 2023-2024 Sundhnúksgígar Eruption (Iceland), EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-17683, https://doi.org/10.5194/egusphere-egu25-17683, 2025.