02342oam 2200469zu 450 991087658730332120210807004703.01-118-67019-1(CKB)3450000000004143(SSID)ssj0001034051(PQKBManifestationID)11684497(PQKBTitleCode)TC0001034051(PQKBWorkID)11006603(PQKB)11179741(NjHacI)993450000000004143(PPN)189506652(EXLCZ)99345000000000414320160829d2013 uy engur|||||||||||txtccrQuaternary 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[Place of publication not identified]American Geophysical Union20131 online resource (iii, 38 pages)Bibliographic Level Mode of Issuance: Monograph0-87590-576-5 Includes bibliographical references.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.Sediments (Geology)FloridaBarrier islandsFloridaGulf CoastSediments (Geology)Barrier islands551.304Davis Richard A103204Hine Albert CPQKBBOOK9910876587303321Quaternary 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 19892267807UNINA