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Extrusion zone of the cardona diapir, located at the Catalan Potash sub-basin (Ebro Basin, NE Iberia). Halite, anhydrite and Sylvite interlayers are strongly folded as a result of the salt ductile flow during diapirism. Evaporite layers exhibiti thin intercalations of claystone and marlstone.<\/p>\n","modified":"2021-04-28T09:10:32","color":"","icon":"","noDetails":false,"noInteraction":false,"zindex":"","imageGallery":[{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2021\/04\/IMG_20200226_151305-1024x576.jpg","id":8326,"caption":""},{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2021\/04\/IMG_20200226_150939-1024x576.jpg","id":8324,"caption":""}],"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2021\/04\/IMG_20200226_151305-1024x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"reachability":{"by_bike":{"check":false,"description":""},"on_foot":{"check":false,"description":""},"by_car":{"check":false,"description":""},"by_public_transportation":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/8323","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=8323&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/cardona-diapir\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.6728553118319,41.902861911753]}}