United States Naval Oceanographic Office Marine Geophysical Survey Program 1965-1967, North Atlantic Ocean, Norwegian Sea, and Mediterranean Sea Area 3, Volume 5, Geology and Geophysics.
Area 3 contains extensive abyssal-plain development on the ocean-basin floor seaward of the continental margins. The depth of the abyssal plains increases from 2550 fm on the Biscay abyssal plain at 48 degrees N to 2825 fm on the Iberia abyssal plain at 40 degrees N. The two plains are joined by The...
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ftdtic:AD0845252 2023-05-15T17:35:35+02:00 United States Naval Oceanographic Office Marine Geophysical Survey Program 1965-1967, North Atlantic Ocean, Norwegian Sea, and Mediterranean Sea Area 3, Volume 5, Geology and Geophysics. TEXAS INSTRUMENTS INC DALLAS SCIENCE SERVICES DIV 1968-10-29 text/html http://www.dtic.mil/docs/citations/AD0845252 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0845252 en eng http://www.dtic.mil/docs/citations/AD0845252 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Geology Geochemistry and Mineralogy *MARINE GEOPHYSICS *GEOLOGICAL SURVEYS OCEAN BOTTOM TOPOGRAPHY OCEAN BOTTOM SAMPLING SEDIMENTATION BATHYTHERMOGRAPH DATA ATLANTIC OCEAN NORWEGIAN SEA MEDITERRANEAN SEA MAPS ABYSSAL HILLS ABYSSAL PLAINS SEAMOUNTS Text 1968 ftdtic 2016-02-19T05:45:23Z Area 3 contains extensive abyssal-plain development on the ocean-basin floor seaward of the continental margins. The depth of the abyssal plains increases from 2550 fm on the Biscay abyssal plain at 48 degrees N to 2825 fm on the Iberia abyssal plain at 40 degrees N. The two plains are joined by Theta gap, a deep-sea channel system. Sediment thickness exceeds 1 km of predominantly terrigenous products. An area of abyssal hills extends west from the Iberia abyssal plain to the flank of the Mid-Atlantic ridge. The flank provinces of the Mid-Atlantic ridge are generally well-developed distinct features, mantled by 200 to 400 m of sediment except on the crestal provinces where sediment accumulation is much reduced. A seamount group oriented NW-SE effectively divides the lower step into two separate segments with contrasting topography and slope. King's trough, a NW-SE-trending trough and ridge complex, disrupts the middle step and part of the upper step in the central portion of the area. A portion of the Azores plateau is situated in the southwest corner of Area 3; a NW-SE-oriented positive feature, it lies normal to and disrupts the Mid-Atlantic ridge between 38 degrees N and 41 degrees N. The sediments on the Mid-Atlantic ridge are primarily fine-grained pelagics. That portion of the ridge below 2500 fm contains increased accumulations of red clay. (Author) Text North Atlantic Norwegian Sea Defense Technical Information Center: DTIC Technical Reports database Mid-Atlantic Ridge Norwegian Sea |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography Geology Geochemistry and Mineralogy *MARINE GEOPHYSICS *GEOLOGICAL SURVEYS OCEAN BOTTOM TOPOGRAPHY OCEAN BOTTOM SAMPLING SEDIMENTATION BATHYTHERMOGRAPH DATA ATLANTIC OCEAN NORWEGIAN SEA MEDITERRANEAN SEA MAPS ABYSSAL HILLS ABYSSAL PLAINS SEAMOUNTS |
spellingShingle |
Physical and Dynamic Oceanography Geology Geochemistry and Mineralogy *MARINE GEOPHYSICS *GEOLOGICAL SURVEYS OCEAN BOTTOM TOPOGRAPHY OCEAN BOTTOM SAMPLING SEDIMENTATION BATHYTHERMOGRAPH DATA ATLANTIC OCEAN NORWEGIAN SEA MEDITERRANEAN SEA MAPS ABYSSAL HILLS ABYSSAL PLAINS SEAMOUNTS United States Naval Oceanographic Office Marine Geophysical Survey Program 1965-1967, North Atlantic Ocean, Norwegian Sea, and Mediterranean Sea Area 3, Volume 5, Geology and Geophysics. |
topic_facet |
Physical and Dynamic Oceanography Geology Geochemistry and Mineralogy *MARINE GEOPHYSICS *GEOLOGICAL SURVEYS OCEAN BOTTOM TOPOGRAPHY OCEAN BOTTOM SAMPLING SEDIMENTATION BATHYTHERMOGRAPH DATA ATLANTIC OCEAN NORWEGIAN SEA MEDITERRANEAN SEA MAPS ABYSSAL HILLS ABYSSAL PLAINS SEAMOUNTS |
description |
Area 3 contains extensive abyssal-plain development on the ocean-basin floor seaward of the continental margins. The depth of the abyssal plains increases from 2550 fm on the Biscay abyssal plain at 48 degrees N to 2825 fm on the Iberia abyssal plain at 40 degrees N. The two plains are joined by Theta gap, a deep-sea channel system. Sediment thickness exceeds 1 km of predominantly terrigenous products. An area of abyssal hills extends west from the Iberia abyssal plain to the flank of the Mid-Atlantic ridge. The flank provinces of the Mid-Atlantic ridge are generally well-developed distinct features, mantled by 200 to 400 m of sediment except on the crestal provinces where sediment accumulation is much reduced. A seamount group oriented NW-SE effectively divides the lower step into two separate segments with contrasting topography and slope. King's trough, a NW-SE-trending trough and ridge complex, disrupts the middle step and part of the upper step in the central portion of the area. A portion of the Azores plateau is situated in the southwest corner of Area 3; a NW-SE-oriented positive feature, it lies normal to and disrupts the Mid-Atlantic ridge between 38 degrees N and 41 degrees N. The sediments on the Mid-Atlantic ridge are primarily fine-grained pelagics. That portion of the ridge below 2500 fm contains increased accumulations of red clay. (Author) |
author2 |
TEXAS INSTRUMENTS INC DALLAS SCIENCE SERVICES DIV |
format |
Text |
title |
United States Naval Oceanographic Office Marine Geophysical Survey Program 1965-1967, North Atlantic Ocean, Norwegian Sea, and Mediterranean Sea Area 3, Volume 5, Geology and Geophysics. |
title_short |
United States Naval Oceanographic Office Marine Geophysical Survey Program 1965-1967, North Atlantic Ocean, Norwegian Sea, and Mediterranean Sea Area 3, Volume 5, Geology and Geophysics. |
title_full |
United States Naval Oceanographic Office Marine Geophysical Survey Program 1965-1967, North Atlantic Ocean, Norwegian Sea, and Mediterranean Sea Area 3, Volume 5, Geology and Geophysics. |
title_fullStr |
United States Naval Oceanographic Office Marine Geophysical Survey Program 1965-1967, North Atlantic Ocean, Norwegian Sea, and Mediterranean Sea Area 3, Volume 5, Geology and Geophysics. |
title_full_unstemmed |
United States Naval Oceanographic Office Marine Geophysical Survey Program 1965-1967, North Atlantic Ocean, Norwegian Sea, and Mediterranean Sea Area 3, Volume 5, Geology and Geophysics. |
title_sort |
united states naval oceanographic office marine geophysical survey program 1965-1967, north atlantic ocean, norwegian sea, and mediterranean sea area 3, volume 5, geology and geophysics. |
publishDate |
1968 |
url |
http://www.dtic.mil/docs/citations/AD0845252 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0845252 |
geographic |
Mid-Atlantic Ridge Norwegian Sea |
geographic_facet |
Mid-Atlantic Ridge Norwegian Sea |
genre |
North Atlantic Norwegian Sea |
genre_facet |
North Atlantic Norwegian Sea |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0845252 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766134797732675584 |