{"ID":5064,"name":"Apagado","location":[{"name":"South America","url":"https:\/\/comet.nerc.ac.uk\/location\/south-america\/","slug":"south-america","id":53,"api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/location\/53"}],"volcano_number":"358024","country":"Chile","geodetic_measurements":"Yes","deformation_observation":"No","duration_of_observation":"1993-1999 (ERS), 2006-2010 (ALOS)","characteristics_of_deformation":"
No deformation was detected at Apagado volcano during ERS and ALOS surveys of the Southern Andes (Pritchard and Simons, 2004; Fournier et al., 2010; Pritchard et al., 2013).<\/p>\n","latitude":"-41.88","longitude":"-72.58","images":[],"uri":"https:\/\/comet.nerc.ac.uk\/volcanoes\/apagado-2\/","api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/volcano\/5064","measurement_methods":"InSAR","inferred_causes":[],"references":["Pritchard, M. E., and M. Simons (2004), An InSAR-based survey of volcanic deformation in the southern Andes, Geophys. Res. Lett., 31, L15610, doi:10.1029\/2004GL020545.
\n","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.
\n"],"date_added":"2018-03-01 15:25:41","last_modified":"2018-03-01 15:25:41"}