{"type":"Feature","properties":{"id":1695,"name":"Sardic Angular Unconformity","description":"<p>Cambrian-Early Ordovician shale (Cabitza Shists) are separated from overlying Upper Ordovician-lower Carfoniferous<br \/>\nsedimentary cycle by sharp angular unconformity (Sardic phase) and overlain by trasgressive polygenic<br \/>\nmetaconglomerate, the Puddinga Auct.<br \/>\nPhotoID422<\/p>\n<p>Photograph: F.Milazzo<\/p>\n<p>Reference: Luigi CARMIGNANI, Giacomo OGGIANO, Sebastiano BARCA, Paolo CONTI, Antonio ELTRUDIS, Antonio FUNEDDA, Sandro PASCI e Ilio SALVADORI GEOLOGY OF SARDINIA (Explanatory notes of the Geologic map of Sardinia at 1:200,000 scale) Martini, I.P., Tongiorgi, M., Oggiano, G. and Cocozza, T. 1991. Ordovician alluvial fan to marine shelf transition in SW Sardinia, Western Mediterranean Sea: tectonically (Sardic phase) influenced clastic sedimentation. Sedimentary Geology, 72: 97-115.<\/p>\n","color":"#85aa27","icon":"wm-icon-mine-15","noDetails":false,"noInteraction":false,"image":"http:\/\/outcropedia.be.webmapp.it\/wp-content\/uploads\/2018\/06\/Sardic-Angular-Unconformity-768x576.jpg","taxonomy":{"webmapp_category":[229,232,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"source":"http:\/\/outcropedia.be.webmapp.it\/wp-json\/wp\/v2\/poi\/1695","web":"http:\/\/outcropedia.be.webmapp.it\/poi\/sardic-angular-unconformity\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":"","related":{"poi":{"neighbors":[],"related":[]}}},"geometry":{"type":"Point","coordinates":[8.440471887588501,39.30623512847013]}}