{"type":"Feature","properties":{"id":6417,"name":"Flysch Monte Cassio","description":"<p>Impressively parallel bedded basin-plain deposits mainly consisting of resedimented pelagic and hemipelagic biogenic oozes; subordinate, fine-grained sandstone forms darker and considerably thinner, more resistent units. These sediments, which are interpreted as a trench-fill, are thought to be a classic example of stacked megaturbidites triggered by seismic activity (seismoturbidites of Mutti et al., 1984). Thin-bedded sandstones and dark mudstones represent the background sedimentationof the basin plain.<br \/>\nMonte Cassio Flysch, late Cretaceous, northern Appennines<\/p>\n","modified":"2019-01-29T17:15:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/01\/2016-10-29-Flysch-Cassio_02-1024x686.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\/6417","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6417&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/flysch-monte-cassio\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.094345457668965,44.58982326981736]}}