{"ID":5390,"name":"Oraefajokull","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":"374010","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":"64","longitude":"-16.65","images":[{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_009D_02597_080910.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_009D_02597_080910.jpg","width":501,"height":669,"mime":"image\/jpeg","size":159543,"filename":"oraefajokull_009D_02597_080910.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_111D_02490_152021.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_111D_02490_152021.jpg","width":501,"height":669,"mime":"image\/jpeg","size":168268,"filename":"oraefajokull_111D_02490_152021.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_118A_02507_211817.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_118A_02507_211817.jpg","width":501,"height":669,"mime":"image\/jpeg","size":146257,"filename":"oraefajokull_118A_02507_211817.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_111D_02489_111313.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_111D_02489_111313.jpg","width":501,"height":669,"mime":"image\/jpeg","size":146191,"filename":"oraefajokull_111D_02489_111313.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_147A_02488_131211.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_147A_02488_131211.jpg","width":501,"height":669,"mime":"image\/jpeg","size":158188,"filename":"oraefajokull_147A_02488_131211.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_009D_02504_202119.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_009D_02504_202119.jpg","width":501,"height":668,"mime":"image\/jpeg","size":169237,"filename":"oraefajokull_009D_02504_202119.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_147A_02466_191712.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_147A_02466_191712.jpg","width":501,"height":669,"mime":"image\/jpeg","size":169351,"filename":"oraefajokull_147A_02466_191712.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_045A_02538_121210.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_045A_02538_121210.jpg","width":501,"height":667,"mime":"image\/jpeg","size":141765,"filename":"oraefajokull_045A_02538_121210.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_045A_02494_171816.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/oraefajokull\/oraefajokull_045A_02494_171816.jpg","width":501,"height":669,"mime":"image\/jpeg","size":167601,"filename":"oraefajokull_045A_02494_171816.jpg"}],"uri":"https:\/\/comet.nerc.ac.uk\/volcanoes\/oraefajokull\/","api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/volcano\/5390","measurement_methods":"InSAR, GPS - continuous, GPS - campaign, Levelling, Strainmeter, Tiltmeter, EDM","inferred_causes":[],"references":["Smithsonian Institution Global Volcanism Program
\nhttp:\/\/www.volcano.si.edu\/volcano.cfm?vn=374010","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 14:12:57","last_modified":"2015-09-21 14:12:57"}