1 year seismological experiment at Strokkur in 2017/18 ...

• Main Authors: Eibl, E.P.S., Walter, T., Jousset, P., Dahm, T., Allahbakhshi, M., Müller, D., Hersir, G. P.
• Format: Dataset
• Language: English
• Published: GFZ Data Services 2020
• Subjects: EARTH SCIENCE > SOLID EARTH > TECTONICS > VOLCANIC ACTIVITY; EARTH SCIENCE > SOLID EARTH > TECTONICS > EARTHQUAKES; In Situ/Laboratory Instruments > Magnetic/Motion Sensors > Seismometers; In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS; In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS > SEISMOLOGICAL STATIONS; Monitoring system; Seismological stations; Passive seismic; Seismometers; Velocity; MiniSEED; GIPP; MESI; Geophysics; FOS: Earth and related environmental sciences; Volcano; Temporary[g]; Gylfi; Strokkur; Iceland
• Online Access: https://dx.doi.org/10.14470/2y7562610816; https://geofon.gfz-potsdam.de/doi/network/7L/2017

Strokkur_1yr is a one year seismological experiment realized at the most active geyser on Iceland by Eva Eibl (University of Potsdam) in collaboration with Thomas R. Walter, Phillippe Jousset, Torsten Dahm, Masoud Allahbakhshi, Daniel Müller from GFZ Potsdam and Gylfi P. Hersir from ISOR Iceland. The geyser is part of the Haukadalur geothermal area in south Iceland, which contains numerous geothermal anomalies, hot springs, and basins (Walter et al., 2018). Strokkur is a pool geyser and has a silica sinter edifice with a water basin on top, which is about 12 m in diameter with a central tube of more than 20 m depth. The aim of the seismic experiment is to monitor eruptions of Strokkur geyser from June 2017 to June 2018 using four broadband seismic stations (Nanometrics Trillium Compact Posthole 20 s). Sensors were buried 30–40 cm deep in the ground at distances of 38.8 m (G4, SE), 47.3 m (G3, SW), 42.5 m (G2, N), and 95.5 m (G1, NE) from Strokkur center. Data gaps represent 15–44 % of the records as during ...