. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. Phi scole 3^4 4 5 6 Microns 125// 62 31 16 9 102034 5 6 78 2 1 250// 125 62 31 16 8 4 Fig. 5. A mechanical analysis of cores 180-1 and 180-2. Note the well defined particle grading in both cores. Also note the sharply contrasting particle size distribution in the abyssal clay facies at 150 cm in core 180-1. (After Heezen, Ericson and Ewing, 1954.). Fig. 6. Generalized bathymetric map of the western Mediterranean Sea, showing the area in which submarine cables were broken on the Balearic Abyssal Plain, following the 1954 Or
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. Phi scole 3^4 4 5 6 Microns 125// 62 31 16 9 102034 5 6 78 2 1 250// 125 62 31 16 8 4 Fig. 5. A mechanical analysis of cores 180-1 and 180-2. Note the well defined particle grading in both cores. Also note the sharply contrasting particle size distribution in the abyssal clay facies at 150 cm in core 180-1. (After Heezen, Ericson and Ewing, 1954.). Fig. 6. Generalized bathymetric map of the western Mediterranean Sea, showing the area in which submarine cables were broken on the Balearic Abyssal Plain, following the 1954 Orleansville earthquake. Depths in fathoms. (After Heezen and Ewing, 1955.). 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
