{"ID":4981,"name":"Tolhuaca","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":"357093","country":"Chile","geodetic_measurements":"Yes","deformation_observation":"No","duration_of_observation":"2006-2008","characteristics_of_deformation":"
No deformation was detected at Tolhuaca during a regional ALOS InSAR survey of Southern Andean Volcanoes (Fournier et al., 2010).<\/p>\n","latitude":"-38.31","longitude":"-71.645","images":[{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/tolhuaca\/tolhuaca_091A_12777_131313.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/tolhuaca\/tolhuaca_091A_12777_131313.jpg","width":501,"height":669,"mime":"image\/jpeg","size":191482,"filename":"tolhuaca_091A_12777_131313.jpg"},{"path":"\/nas\/content\/live\/cometnerc\/wp-content\/uploads\/figures_sentinel\/tolhuaca\/tolhuaca_083D_12832_131313.jpg","url":"https:\/\/comet.nerc.ac.uk\/wp-content\/uploads\/figures_sentinel\/tolhuaca\/tolhuaca_083D_12832_131313.jpg","width":501,"height":669,"mime":"image\/jpeg","size":186378,"filename":"tolhuaca_083D_12832_131313.jpg"}],"uri":"https:\/\/comet.nerc.ac.uk\/volcanoes\/tolhuaca\/","api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/volcano\/4981","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.
\n"],"date_added":"2018-03-01 13:43:07","last_modified":"2018-03-01 13:43:07"}