{"ID":3298,"name":"Morne Diablotins","location":[{"name":"West Indies","url":"https:\/\/comet.nerc.ac.uk\/location\/west-indies\/","slug":"west-indies","id":44,"api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/location\/44"}],"volcano_number":"360090","country":"Dominica","geodetic_measurements":"Yes","deformation_observation":"No","duration_of_observation":"2006-2008","characteristics_of_deformation":"
No deformation was detected at Morne Diablotins\u00a0during a 2006-2008 ALOS\u00a0survey of Latin America (Fournier et al., 2010).
\n <\/p>\n","latitude":"15.503","longitude":"-61.397","images":[{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/morne_diablotins\/morne-diablotins_054D_07351_051104.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/morne_diablotins\/morne-diablotins_054D_07351_051104.jpg","width":750,"height":1110,"mime":"image\/jpeg","size":160194,"filename":"morne-diablotins_054D_07351_051104.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/morne_diablotins\/morne-diablotins_164A_07620_000518.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/morne_diablotins\/morne-diablotins_164A_07620_000518.jpg","width":501,"height":660,"mime":"image\/jpeg","size":89356,"filename":"morne-diablotins_164A_07620_000518.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/morne_diablotins\/morne-diablotins_054D_07353_071304.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/morne_diablotins\/morne-diablotins_054D_07353_071304.jpg","width":501,"height":669,"mime":"image\/jpeg","size":96493,"filename":"morne-diablotins_054D_07353_071304.jpg"}],"uri":"https:\/\/comet.nerc.ac.uk\/volcanoes\/morne-diablotins\/","api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/volcano\/3298","measurement_methods":"InSAR","inferred_causes":[],"references":["Fournier, T. J., M. E. Pritchard, and S. N. Riddick (2010), Duration, magnitude, and frequency of subaerial volcano deformation events: New results from Latin America using InSAR and a global synthesis, Geochem. Geophys. Geosyst., 11, Q01003, doi:10.1029\/2009GC002558."],"date_added":"2015-11-10 12:49:19","last_modified":"2015-11-10 12:49:19"}