Gulf of Mexico: Its Origin, Waters, and Marine LifeU.S. Government Printing Office, 1954 - 604 sider |
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Side viii
... Sea level . Availability of tidal data .. 104 108 110 110 112 113 113 114 115 117 Literature cited ......... . Physical oceanography of the Gulf of Mexico . By Dale F. Leipper - 118 119 Ocean currents____ Sea surface temperatures .. Sea ...
... Sea level . Availability of tidal data .. 104 108 110 110 112 113 113 114 115 117 Literature cited ......... . Physical oceanography of the Gulf of Mexico . By Dale F. Leipper - 118 119 Ocean currents____ Sea surface temperatures .. Sea ...
Side 45
... sea level to form barrier reefs , so that the lagoon has been filled to a shallow depth with sediment and organic growths ( 3.2 Sectors , fig . 14 ) . The drainage of northwestern Cuba is largely southward , so that only small streams ...
... sea level to form barrier reefs , so that the lagoon has been filled to a shallow depth with sediment and organic growths ( 3.2 Sectors , fig . 14 ) . The drainage of northwestern Cuba is largely southward , so that only small streams ...
Side 49
... sea level . The slope of the groundwater surface ( piezomet- ric ) toward the coast indicates a movement of underground water in that direction . Also , along much of the coast of Sector 2.1 there is an artesian groundwater head of ...
... sea level . The slope of the groundwater surface ( piezomet- ric ) toward the coast indicates a movement of underground water in that direction . Also , along much of the coast of Sector 2.1 there is an artesian groundwater head of ...
Side 51
... sea level . This Key range ends to the southwest in the Boot , Mara- thon , and Vaca group of Keys . Westward along the line of the Keys , there is a large emergence of the Miami oolite limestone stratum to the present intertidal zone ...
... sea level . This Key range ends to the southwest in the Boot , Mara- thon , and Vaca group of Keys . Westward along the line of the Keys , there is a large emergence of the Miami oolite limestone stratum to the present intertidal zone ...
Side 52
... sea level , as they , certainly in some cases , have been due to compaction or minor horizontal shoreline changes under essential still- stand of the sea . The history of the formation of the mangrove barrier ridge and lagoon may be ...
... sea level , as they , certainly in some cases , have been due to compaction or minor horizontal shoreline changes under essential still- stand of the sea . The history of the formation of the mangrove barrier ridge and lagoon may be ...
Vanlige uttrykk og setninger
Agassiz algae Allman Assn Atlantic average bacteria barrier island basin beach bottom Bull Campeche Campeche Bank Caribbean Carnegie Inst Cedar Keys charts coast of Florida continental shelf coral Cuba currents d'Orbigny delta deposits depth diatoms dinoflagellates distribution Dry Tortugas expedition fathoms fauna feet figure Fish Fisheries flora Florida Keys Foraminifera Galveston Geol geologic Gulf coast Gulf of Mexico Host hydrographic hydroids Jour Key West Laboratory lagoons limestone Linton Louisiana low waters mangrove Manter marine meters miles Mississippi River northern observations occur ocean Oceanographic offshore organic oyster parasites Peninsula Pensacola plankton plants range reefs region reported salinity sand sea level sea water Sector sediments semidaily shallow shore shoreline slope species sponges stations Straits of Florida surface swamp temperature Texas tidal tion trematodes tropical United States Coast Washington west coast wind Yucatán Channel Yucatán Peninsula zone Zool
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