On the Move: 2023 Observations on Real Time Graben Formation, Grindavík, Iceland

Gregory P. De Pascale*, Tomáš J. Fischer, William Michael Moreland, Halldór Geirsson, Pavla Hrubcová, Vincent Drouin, Danielle Forester, Méline Payet--Clerc, Diana Brum da Silveira, Josef Vlček, Benedikt G. Ófeigsson, Ármann Höskuldsson, Helga Kristín Torfadóttir, Iðunn Kara Valdimarsdóttir, Birta Dís Jónsdóttir Blöndal, Ingibjörg Jónsdóttir, Sigurjón Jónsson, Thor Thordarson

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

Grabens, or valleys formed during extensional tectonic events, are common but rarely observed during formation. In November 2023, inelastic surface deformation formed abruptly along Iceland's plate boundary in Grindavík. We documented graben formation in real-time through satellite mapping (InSAR), seismicity, GNSS data, repeated lidar surveys, and field mapping. Five normal faults and ∼12 fissures ruptured the surface delineating two grabens separated by a horst, a context not present in other contemporary case studies. The graben normal faults slipped rapidly (over hours) and maximum surface motions coincided with the occurrence of turbulent seismic swarms in both space and time. Although 3 eruptions took place ∼15 km northeast of Grindavík from 2021 to 2023, attributed to magma intrusions (i.e., dikes), none of these also formed grabens. Thus, the Grindavík grabens shows evidence for tectonic origins. Real-time monitoring of these phenomena provide insight into graben formation on Earth and potentially on other planets.

Original languageEnglish (US)
Article numbere2024GL110150
JournalGeophysical Research Letters
Volume51
Issue number14
DOIs
StatePublished - Jul 28 2024

Bibliographical note

Publisher Copyright:
© 2024. The Author(s).

Keywords

  • earthquakes
  • graben formation
  • Iceland
  • plate boundary
  • reykjanes peninsula
  • tectonics

ASJC Scopus subject areas

  • Geophysics
  • General Earth and Planetary Sciences

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