Articles | Volume 21, issue 7
https://doi.org/10.5194/nhess-21-2197-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-21-2197-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A harmonised instrumental earthquake catalogue for Iceland and the northern Mid-Atlantic Ridge
Faculty of Industrial Engineering, Mechanical Engineering and Computer Science, University of Iceland, Hjarðarhagi 2, Reykjavík, Iceland
Bjarni Bessason
Faculty of Civil and Environmental Engineering, University of Iceland, Hjarðarhagi 2, Reykjavík, Iceland
Ásdís Helgadóttir
Faculty of Industrial Engineering, Mechanical Engineering and Computer Science, University of Iceland, Hjarðarhagi 2, Reykjavík, Iceland
Páll Einarsson
Science Institute, University of Iceland, Sturlugata 7, Reykjavík, Iceland
Gunnar B. Guðmundsson
Icelandic Meteorological Office, Bústaðavegur 7–9, Reykjavík, Iceland
Bryndís Brandsdóttir
Science Institute, University of Iceland, Sturlugata 7, Reykjavík, Iceland
Kristín S. Vogfjörd
Icelandic Meteorological Office, Bústaðavegur 7–9, Reykjavík, Iceland
Kristín Jónsdóttir
Icelandic Meteorological Office, Bústaðavegur 7–9, Reykjavík, Iceland
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Eva P. S. Eibl, Kristin S. Vogfjörd, Benedikt G. Ófeigsson, Matthew J. Roberts, Christopher J. Bean, Morgan T. Jones, Bergur H. Bergsson, Sebastian Heimann, and Thoralf Dietrich
Earth Surf. Dynam., 11, 933–959, https://doi.org/10.5194/esurf-11-933-2023, https://doi.org/10.5194/esurf-11-933-2023, 2023
Short summary
Short summary
Floods draining beneath an ice cap are hazardous events that generate six different short- or long-lasting types of seismic signals. We use these signals to see the collapse of the ice once the water has left the lake, the propagation of the flood front to the terminus, hydrothermal explosions and boiling in the bedrock beneath the drained lake, and increased water flow at rapids in the glacial river. We can thus track the flood and assess the associated hazards better in future flooding events.
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Short summary
Local information on epicentres and Mw magnitudes from international catalogues have been combined to compile a catalogue of earthquakes in and near Iceland in the years 1900–2019. The magnitudes are either moment-tensor modelled or proxy values obtained with regression on Ms or exceptionally on mb. The catalogue also covers the northern Mid-Atlantic Ridge with less accurate locations but similarly harmonised magnitudes.
Local information on epicentres and Mw magnitudes from international catalogues have been...
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