{"ID":5189,"name":"San Mart\u00edn","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":"341110","country":"Mexico","geodetic_measurements":"Yes","deformation_observation":"No","duration_of_observation":"2007-2010","characteristics_of_deformation":"
No deformation was observed at San Mart\u00edn, part of the Tuxtla volcanic field, in a regional ALOS survey of Mexican volcanoes (Chaussard et al., 2013<\/em>).<\/p>\n","latitude":"18.57","longitude":"-95.2","images":[{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_107A_07124_101204.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_107A_07124_101204.jpg","width":501,"height":669,"mime":"image\/jpeg","size":148397,"filename":"san-martin_107A_07124_101204.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_172D_07281_171518.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_172D_07281_171518.jpg","width":501,"height":660,"mime":"image\/jpeg","size":146111,"filename":"san-martin_172D_07281_171518.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_070D_07100_041013.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_070D_07100_041013.jpg","width":501,"height":668,"mime":"image\/jpeg","size":148773,"filename":"san-martin_070D_07100_041013.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_172D_07248_131213.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_172D_07248_131213.jpg","width":501,"height":669,"mime":"image\/jpeg","size":150017,"filename":"san-martin_172D_07248_131213.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_107A_07051_231204.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/san_martin\/san-martin_107A_07051_231204.jpg","width":501,"height":660,"mime":"image\/jpeg","size":146552,"filename":"san-martin_107A_07051_231204.jpg"}],"uri":"https:\/\/comet.nerc.ac.uk\/volcanoes\/san-martin\/","api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/volcano\/5189","measurement_methods":"InSAR","inferred_causes":[],"references":["Chaussard, E., F. Amelung, and Y. Aoki (2013), Characterization of open and closed volcanic systems in Indonesia and Mexico using InSAR time series, J. Geophys. Res. Solid Earth, 118, 3957\u20133969, doi:10.1002\/jgrb.50288."],"date_added":"2015-03-09 11:37:06","last_modified":"2015-03-09 11:37:06"}