. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. Fig. 6. 43° 31..5'X, 12° 3fi'W. Depth 5200 m. Head of Biscay-Iberia inlerplain channel. (Photo by N.I.O.) Semi-consolidated sedimentary rocks exposed on the cliffs of an eroded channel cut into the Biscay abyssal plain by turbidity currents. These may represent the degree of lithification of abyssal-plain sediments buried some 100 m deep.. Fig. 7. 11°51'N, 164° 55'E. Depth 1730 m. Sylvania Tablemount near Bikini. Area of picture 1^ by U m. (U.S. Navy Electronics Laboratory photo by C. J. Shipek.) Manganese-encrusted volcan
![. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. Fig. 6. 43° 31..5'X, 12° 3fi'W. Depth 5200 m. Head of Biscay-Iberia inlerplain channel. (Photo by N.I.O.) Semi-consolidated sedimentary rocks exposed on the cliffs of an eroded channel cut into the Biscay abyssal plain by turbidity currents. These may represent the degree of lithification of abyssal-plain sediments buried some 100 m deep.. Fig. 7. 11°51'N, 164° 55'E. Depth 1730 m. Sylvania Tablemount near Bikini. Area of picture 1^ by U m. (U.S. Navy Electronics Laboratory photo by C. J. Shipek.) Manganese-encrusted volcan Stock Photo](https://c8.alamy.com/comp/RE8JF3/the-earth-beneath-the-sea-history-ocean-bottom-marine-geophysics-fig-6-43-315x-12-3fiw-depth-5200-m-head-of-biscay-iberia-inlerplain-channel-photo-by-nio-semi-consolidated-sedimentary-rocks-exposed-on-the-cliffs-of-an-eroded-channel-cut-into-the-biscay-abyssal-plain-by-turbidity-currents-these-may-represent-the-degree-of-lithification-of-abyssal-plain-sediments-buried-some-100-m-deep-fig-7-1151n-164-55e-depth-1730-m-sylvania-tablemount-near-bikini-area-of-picture-1-by-u-m-us-navy-electronics-laboratory-photo-by-c-j-shipek-manganese-encrusted-volcan-RE8JF3.jpg)
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. The Earth beneath the sea : History. Ocean bottom; Marine geophysics. Fig. 6. 43° 31..5'X, 12° 3fi'W. Depth 5200 m. Head of Biscay-Iberia inlerplain channel. (Photo by N.I.O.) Semi-consolidated sedimentary rocks exposed on the cliffs of an eroded channel cut into the Biscay abyssal plain by turbidity currents. These may represent the degree of lithification of abyssal-plain sediments buried some 100 m deep.. Fig. 7. 11°51'N, 164° 55'E. Depth 1730 m. Sylvania Tablemount near Bikini. Area of picture 1^ by U m. (U.S. Navy Electronics Laboratory photo by C. J. Shipek.) Manganese-encrusted volcanic boulders and rippled Globi(/eriita ooze. Similar boulders were dredged near by, showing these rocks to be olivine-basalt boulders coated by a thick crust of manganese.. 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 work.. Hill, M. N. (Maurice Neville), 1919-. New York : Interscience Pub.