BAHAMAS
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Larry J. DOYLE ; Orrin H. Pilkey | TULSA : SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS | 1979Continental slopes are the edges of continental blocks, the zones of change from continental crust to oceanic crust. They are critical links in the chain of sedimentary processes that eventually carry sediment to the true ocean basin floor. Spur[...]
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Norman D. NEWELL ; John IMBRIE ; Edward G. Et Al PURDY | NEW YORK : AMERICAN MUSEUM OF NATURAL HISTORY $c BULLETIN OF THE AMERICAN MUSEUM OF NATURAL HISTORY | 1959GENERAL PHYSICAL CONDITIONS ON THE GREAT BAHAMA BANK Location and climate Topography Salinity of the bank waters Measurements of pH Organic matter and Eh TIME OF ORIGIN OF BOTTOM COMMUNITIES AND SEDIMENTS BOTTOM FACIES AND COMMUNITIES, GENERAL C[...]
