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[null,"1.","Record Nr.",null,"UNISA996217175903316"]
[null,null,"Autore",null,"Davis Richard A"]
[null,null,"Titolo",null,"Quaternary Geology and Sedimentology of the Barrier Island and Marshy Coast, West-Central Florida, U. S. A.: Mullet Key, Pinellas County to Crystal River, Florida, July 20 - 23 1989"]
[null,null,"Pubbl/distr/stampa",null,"[Place of publication not identified], : American Geophysical Union, 2013"]
[null,null,"ISBN",null,"1-118-67019-1"]
[null,null,"Descrizione fisica",null,"1 online resource (iii, 38 pages)"]
[null,null,"Disciplina",null,"551.304"]
[null,null,"Soggetti",null,"Sediments (Geology) - Florida"]
[{"$nulls":4},"Barrier islands - Florida - Gulf Coast"]
[null,null,"Lingua di pubblicazione",null,"Inglese"]
[null,null,"Formato",null,"Materiale a stampa"]
[null,null,null,"Livello bibliografico","Monografia"]
[null,null,null,"Note generali","Bibliographic Level Mode of Issuance: Monograph"]
[null,null,null,"Nota di bibliografia","Includes bibliographical references."]
[null,null,null,"Sommario/riassunto","Published by the American Geophysical Union as part of the Field Trip Guidebooks Series, Volume 375.The reach of coast covered by this excursion represents a broad range in coastal morphology and environmental conditions. It extends from Egmont Channel, the entrance to Tampa Bay, on the south, to Crystal River on the north, a total distance of nearly 150 km. This portion of the west-peninsular Florida coast is divided into a barrier island section on the south and a marsh-dominated coast on the north (fig. 1). Orientation of the coast ranges from northwest to north-northeast although locally, the irregular, non-barrier coast may have almost any orientation."]