Pyroclastic deposits at the base of dacitic dome (grey in color). Photo ID 640<\/p>\n
Photograph: Alessandro Da Mommio<\/p>\n
Reference: The transition from subduction arc to slab tearing: Evidence from Capraia Island, northern Tyrrhenian Sea. Massimo Gasparona, Gideon Rosenbauma, Jan Wijbransb, Piero Manetti<\/p>\n","modified":"2018-06-30T11:11:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Capraia-1-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2059","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2059&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/capraia-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.837454855442047,43.05253796358115]}}