{"ID":5388,"name":"Tjornes Fracture Zone","location":[{"name":"Iceland and Arctic Ocean","url":"https:\/\/comet.nerc.ac.uk\/location\/iceland-and-arctic-ocean\/","slug":"iceland-and-arctic-ocean","id":52,"api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/location\/52"}],"volcano_number":"373100","country":"Iceland","geodetic_measurements":"Yes","deformation_observation":"No","duration_of_observation":"Continuous","characteristics_of_deformation":"
The Icelandic Meteorological Office (IMO)<\/a><\/span>\u00a0leads long-term monitoring of geohazards in Iceland and is responsible for maintaining instrument networks for this purpose. FutureVolc detail a\u00a0description of in-situ monitoring networks in Iceland and available results<\/a>.\u00a0In-situ instrumentation to monitor geological hazards in Iceland includes seismic, GPS, strain, hydrological, radar, infrasound networks, and scanning DOAS spectrometers. With InSAR, the volcanoes in Iceland are not covered by a single systematic study but 85% of them have been included in separate studies of volcanic, seismic, cryospheric or geothermal processes (Biggs et al., 2014).<\/span><\/span><\/p>\n","latitude":"66.3","longitude":"-17.1","images":[],"uri":"https:\/\/comet.nerc.ac.uk\/volcanoes\/tjornes-fracture-zone\/","api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/volcano\/5388","measurement_methods":"GPS - continuous, GPS - campaign, Levelling, Strainmeter, Tiltmeter, EDM","inferred_causes":[],"references":["Smithsonian Institution Global Volcanism Program
\nhttp:\/\/www.volcano.si.edu\/volcano.cfm?vn=373100","The Icelandic Meteorological Office (IMO)","Sturkell, E., Einarsson, P., Sigmundsson, F., Geirsson, H., Olafsson, H., Pedersen, R., ... & Stef\u00e1nsson, R. (2006). Volcano geodesy and magma dynamics in Iceland. Journal of Volcanology and Geothermal Research, 150(1), 14-34."],"date_added":"2015-09-21 14:10:37","last_modified":"2015-09-21 14:10:37"}