. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. Possible deep current dtrecliun during Fiexuosa nterval of warm climate 1460 m AI64-44 AI73-4 1007. Left IO0%Right Left Worm Cold W Right C > Coiling of Globorotalia truncatulinoldes AI64-44 AI73-4 Fine Fraction: < JAjj. 0% I007o 0% 100%. Fig. 5. The Muir Seamount cores. in the region of the Muir seamount during the last ice age must have been from southwest to northeast. However, within the fiexuosa zone of core A173-4 the coarse fraction reaches 90%, a value which can only be explained by current scour winnowing. T
. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. Possible deep current dtrecliun during Fiexuosa nterval of warm climate 1460 m AI64-44 AI73-4 1007. Left IO0%Right Left Worm Cold W Right C > Coiling of Globorotalia truncatulinoldes AI64-44 AI73-4 Fine Fraction: < JAjj. 0% I007o 0% 100%. Fig. 5. The Muir Seamount cores. in the region of the Muir seamount during the last ice age must have been from southwest to northeast. However, within the fiexuosa zone of core A173-4 the coarse fraction reaches 90%, a value which can only be explained by current scour winnowing. Thus, the direction of deep circulation must have been quite different during the time of relatively warm climate represented by the fiexuosa zone. To account for current scour at this station, A172-4, it is necessary to suppose that the direction of deep circulation was parallel to the long axis of the seamount. The fact that the percentage of coarse fraction in the fiexuosa zone of core A164-44 is normal for the depth of water suggests that the direction. 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
