LEADER 02353oam 2200469zu 450 001 996217175903316 005 20210807004703.0 010 $a1-118-67019-1 035 $a(CKB)3450000000004143 035 $a(SSID)ssj0001034051 035 $a(PQKBManifestationID)11684497 035 $a(PQKBTitleCode)TC0001034051 035 $a(PQKBWorkID)11006603 035 $a(PQKB)11179741 035 $a(NjHacI)993450000000004143 035 $a(PPN)189506652 035 $a(EXLCZ)993450000000004143 100 $a20160829d2013 uy 101 0 $aeng 135 $aur||||||||||| 181 $ctxt 182 $cc 183 $acr 200 10$aQuaternary 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 210 31$a[Place of publication not identified]$cAmerican Geophysical Union$d2013 215 $a1 online resource (iii, 38 pages) 300 $aBibliographic Level Mode of Issuance: Monograph 311 $a0-87590-576-5 320 $aIncludes bibliographical references. 330 $aPublished 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. 606 $aSediments (Geology)$zFlorida 606 $aBarrier islands$zFlorida$zGulf Coast 615 0$aSediments (Geology) 615 0$aBarrier islands 676 $a551.304 700 $aDavis$b Richard A$0103204 702 $aHine$b Albert C 801 0$bPQKB 906 $aBOOK 912 $a996217175903316 996 $aQuaternary 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$92267807 997 $aUNISA