{"ID":4395,"name":"Santo Tomas","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":"342800","country":"Guatemala","geodetic_measurements":"Yes","deformation_observation":"No","duration_of_observation":"2007-2010","characteristics_of_deformation":"
No deformation\u00a0was observed\u00a0at Santo Tomas,\u00a0due to low coherence in an ALOS survey of Central American volcanoes (Ebmeier et al., 2013<\/em>).<\/p>\n","latitude":"14.71","longitude":"-91.479","images":[],"uri":"https:\/\/comet.nerc.ac.uk\/volcanoes\/santo-tomas-2\/","api_endpoint":"https:\/\/comet.nerc.ac.uk\/wp-json\/volcanodb\/v1\/volcano\/4395","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":"2018-02-27 10:52:05","last_modified":"2018-02-27 10:52:05"}