Recent microseismicity observed at Hekla volcano and first velocity inversion results
- 1Dublin Institute for Advanced Studies, Geophysics, Dublin, Ireland (martin@dias.ie)
- 2Icelandic Meteorological Office, Bustadavegi 7-9, 108 Reykjavik, Iceland
- 3British Geological Survey, The Lyell Centre, Research Avenue South, Edinburgh, EH14 4AP, Scotland
Hekla is one of the most active and dangerous volcanoes in Iceland presenting a high hazard to air travel and a growing tourist population. Until now the pre-eruption warning time at Hekla is only around one hour. In 2018 we installed the real-time seismic network HERSK directly on Hekla's edifice. If microseismicity on Hekla increases prior to the next eruption the network could possibly provide a means to improve early warning. In addition it is hoped that HERSK will better our understanding of the processes driving the evolution of pre-eruptive seismicity. The configuration and tuning of a dedicated real-time detection and location system requires the determination of a suitable velocity model and station corrections. We present a catalogue of recently detected local events that we use to invert for a 1-D velocity model. We observe significant variations in station corrections and conclude that it is important to account for these in the real-time detection and location system which we are developing based on the SeisComp3 software.
How to cite: Möllhoff, M., Rezaeifar, M., Bean, C. J., Vogfjörd, K. S., Bergsson, B. H., and Buxel, H.: Recent microseismicity observed at Hekla volcano and first velocity inversion results, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18954, https://doi.org/10.5194/egusphere-egu2020-18954, 2020.