TY - JOUR
T1 - On the Move
T2 - 2023 Observations on Real Time Graben Formation, Grindavík, Iceland
AU - De Pascale, Gregory P.
AU - Fischer, Tomáš J.
AU - Moreland, William Michael
AU - Geirsson, Halldór
AU - Hrubcová, Pavla
AU - Drouin, Vincent
AU - Forester, Danielle
AU - Payet--Clerc, Méline
AU - da Silveira, Diana Brum
AU - Vlček, Josef
AU - Ófeigsson, Benedikt G.
AU - Höskuldsson, Ármann
AU - Torfadóttir, Helga Kristín
AU - Valdimarsdóttir, Iðunn Kara
AU - Blöndal, Birta Dís Jónsdóttir
AU - Jónsdóttir, Ingibjörg
AU - Jónsson, Sigurjón
AU - Thordarson, Thor
N1 - Publisher Copyright:
© 2024. The Author(s).
PY - 2024/7/28
Y1 - 2024/7/28
N2 - 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.
AB - 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.
KW - earthquakes
KW - graben formation
KW - Iceland
KW - plate boundary
KW - reykjanes peninsula
KW - tectonics
UR - http://www.scopus.com/inward/record.url?scp=85198554514&partnerID=8YFLogxK
U2 - 10.1029/2024GL110150
DO - 10.1029/2024GL110150
M3 - Article
AN - SCOPUS:85198554514
SN - 0094-8276
VL - 51
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 14
M1 - e2024GL110150
ER -