. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. SECT. 3] SHALLOW-WATER CARBONATE SEDIMENTS 78°30' 78°00' 579 TT-ao'. 24°30' Z^'OO' - 26«00' 25°30' 25°0O Za'BO' 24°00' zsoso'- TS-OO' re'so' 78°00' 77°30' Fig. 14. Non-skeletal grains > ^ mm in percentage of total sediment. (Data supplied by Edward Purdy.) also mapped the percentage distribution of non-skeletal grains in the sediments of the Gulf of Batabano off the south coast of Cuba. Their results show the edge of what is probably a large area of non-skeletal sands (Fig. 8). Both of these areas, Great Bahama Bank and
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. SECT. 3] SHALLOW-WATER CARBONATE SEDIMENTS 78°30' 78°00' 579 TT-ao'. 24°30' Z^'OO' - 26«00' 25°30' 25°0O Za'BO' 24°00' zsoso'- TS-OO' re'so' 78°00' 77°30' Fig. 14. Non-skeletal grains > ^ mm in percentage of total sediment. (Data supplied by Edward Purdy.) also mapped the percentage distribution of non-skeletal grains in the sediments of the Gulf of Batabano off the south coast of Cuba. Their results show the edge of what is probably a large area of non-skeletal sands (Fig. 8). Both of these areas, Great Bahama Bank and the southeastern part of the 20—s. Ill. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Hill, M. N. (Maurice Neville), 1919-. New York : Interscience Pub.
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Keywords: ., bookcentury1900, bookcollectionbiodivers, booksubjectoceanbottom
