{"ID":1643,"name":"Chiquimula Volcanic Field","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":"342200","country":"Guatemala","geodetic_measurements":"Yes","deformation_observation":"No","duration_of_observation":"2007-2010","characteristics_of_deformation":"
No deformation was detected at the Chiquimula\u00a0Volcanic Field (detection threshold 2\u00a0cm\/yr) during an ALOS survey of Central American volcanoes (<\/span>Ebmeier et al., 2013<\/em>).<\/span><\/p>\n","latitude":"14.83","longitude":"-89.55","images":[{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_063A_07484_040804.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_063A_07484_040804.jpg","width":750,"height":1110,"mime":"image\/jpeg","size":311608,"filename":"chiquimula-volcanic-field_063A_07484_040804.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_128D_07552_151615.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_128D_07552_151615.jpg","width":501,"height":669,"mime":"image\/jpeg","size":188809,"filename":"chiquimula-volcanic-field_128D_07552_151615.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_063A_07458_041304.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_063A_07458_041304.jpg","width":501,"height":669,"mime":"image\/jpeg","size":188868,"filename":"chiquimula-volcanic-field_063A_07458_041304.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_128D_07531_131313.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_128D_07531_131313.jpg","width":501,"height":669,"mime":"image\/jpeg","size":188958,"filename":"chiquimula-volcanic-field_128D_07531_131313.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_063A_07559_161820.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/chiquimula_volcanic_field\/chiquimula-volcanic-field_063A_07559_161820.jpg","width":501,"height":669,"mime":"image\/jpeg","size":188621,"filename":"chiquimula-volcanic-field_063A_07559_161820.jpg"}],"uri":"https:\/\/comet.nerc.ac.uk\/volcanoes\/chiquimula-volcanic-field\/","api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/volcano\/1643","measurement_methods":"InSAR","inferred_causes":[],"references":["Ebmeier, S. K., J. Biggs, T. A. Mather, and F. Amelung (2013), On the lack of InSAR observations of magmatic deformation at Central American volcanoes, J. Geophys. Res. Solid Earth, 118, 2571\u20132585, doi:10.1002\/jgrb.50195."],"date_added":"2015-07-14 15:16:25","last_modified":"2015-07-14 15:16:25"}