Articles | Volume 11, issue 5
Research article
05 Oct 2023
Research article |  | 05 Oct 2023

Subaerial and subglacial seismic characteristics of the largest measured jökulhlaup from the eastern Skaftá cauldron, Iceland

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

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Cited articles

Allen, R.: Automatic phase pickers: Their present use and future prospects, B. Seismol. Soc. Am., 72, S225–S242,, 1982. a
Ankerst, M., Breunig, M. M., Kriegel, H.-P., and Sander, J.: OPTICS: Ordering points to identify the clustering structure, Sigmod. Rec., 28, 49–60,, 1999. a
Ármannsson, H.: The fluid geochemistry of Icelandic high temperature geothermal areas, Appl. Geochem., 66, 14–64,, 2016. a
Arnórsson, S. and Andrésdóttir, A.: Processes controlling the distribution of boron and chlorine in natural waters in Iceland, Geochim. Cosmochim. Ac., 59, 4125–4146,, 1995. a
Bartholomaus, T. C., Amundson, J. M., Walter, J. I., O'Neel, S., West, M. E., and Larsen, C. F.: Subglacial discharge at tidewater glaciers revealed by seismic tremor, Geophys. Res. Lett., 42, 6391–6398,, 2015. a, b, c, d, e, f, g, h
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.