{"ID":4434,"name":"Cerro Prieto","location":[{"name":"Mexico and Central America","url":"https:\/\/comet.nerc.ac.uk\/location\/mexico-and-central-america\/","slug":"mexico-and-central-america","id":41,"api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/location\/41"}],"volcano_number":"341000","country":"Mexico","geodetic_measurements":"Yes","deformation_observation":"Yes","duration_of_observation":"1994-2006 (levelling), 1993-1997 (ERS InSAR), 2003-2006 (Envisat InSAR)","characteristics_of_deformation":"
Between 1993 and 1997, ERS InSAR data showed that the Cerro Prieto Geothermal Field was subsiding at up to 6 cm year-1\u00a0<\/sup>(Carnec and Fabriol 1999).
\nSarychikhina et al (2011) used a combination of levelling surveys and InSAR and observed a maximum subsidence rate of 9 cm year-1\u00a0<\/sup>between 1994 and 1997 (levelling), 12\u00a0cm year-1<\/sup> between 1997 and 2006 (levelling), and 18 cm year-1\u00a0<\/sup>between 2004 and 2005 (InSAR).<\/p>\n","latitude":"32.418","longitude":"115.305","images":[{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/cerro_prieto\/cerro-prieto_166A_05685_131313.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/cerro_prieto\/cerro-prieto_166A_05685_131313.jpg","width":501,"height":660,"mime":"image\/jpeg","size":171363,"filename":"cerro-prieto_166A_05685_131313.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/cerro_prieto\/cerro-prieto_173D_05770_131311.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/cerro_prieto\/cerro-prieto_173D_05770_131311.jpg","width":501,"height":666,"mime":"image\/jpeg","size":154938,"filename":"cerro-prieto_173D_05770_131311.jpg"}],"uri":"https:\/\/comet.nerc.ac.uk\/volcanoes\/cerro-prieto\/","api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/volcano\/4434","measurement_methods":"InSAR, Levelling","inferred_causes":"Hydrothermal","references":["Carnec C, Fabriol H, 1999. Monitoring and modeling land subsidence at the Cerro Prieto geothermal field, Baja California, Mexico, using SAR interferometry. Geophysical Research Letters, 26: 1211-1214.","Sarychikhina, O. E. Glowacka, R. Mellors and F. Su\u00e1rez Vidal, 2011. Land subsidence in the Cerro Prieto Geothermal Field, Baja California, Mexico, from 1994 to 2005: An integrated analysis of DInSAR, leveling and geological data. J. Volcanol. Geotherm. Res., 204 (2011) 76-90."],"date_added":"2018-02-27 11:53:48","last_modified":"2018-02-27 11:53:48"}