Geology and Geophysics Program Summary for FY90. SEAMARC II investigation of the Northern Norwegian-Greenland Sea: Program 1990 and Expansion
The high-latitude northern Norwegian-Greenland Sea and the adjacent part of the Arctic Ocean north of Spitsbergen comprise an unequaled natural laboratory for the study of several important processes involving the generation and/or modification of sea-floor topography, subbottom structure, and mater...
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ftdtic:ADA266622 2023-05-15T15:05:14+02:00 Geology and Geophysics Program Summary for FY90. SEAMARC II investigation of the Northern Norwegian-Greenland Sea: Program 1990 and Expansion Shor, Alexander N. Crane, Kathleen de Moustier, Christian HAWAII INST OF GEOPHYSICS HONOLULU 1991-03 text/html http://www.dtic.mil/docs/citations/ADA266622 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA266622 en eng http://www.dtic.mil/docs/citations/ADA266622 Approved for public release; distribution is unlimited. DTIC AND NTIS Physical and Dynamic Oceanography Geology Geochemistry and Mineralogy *GEOLOGY *GEOPHYSICS GREENLAND SEA MATERIAL PROPERTIES Text 1991 ftdtic 2016-02-22T06:48:08Z The high-latitude northern Norwegian-Greenland Sea and the adjacent part of the Arctic Ocean north of Spitsbergen comprise an unequaled natural laboratory for the study of several important processes involving the generation and/or modification of sea-floor topography, subbottom structure, and material properties. These processes, active now or in the geologically recent past, include (1) tectonism (faulting), volcanism, magma intrusion into rift valley seafloor sediments; (2) erosion and redeposition of sediment by bottom currents; (3) slumping and other downslope processes on glaciated margins; (4) sedimentation from sea ice/icebergs/ice sheets, at water depths less than 100- 500 m, (5) erosion and redeposition by icebergs and grounded ice shelves/sheets. SeaMARC II is the ideal tool for investigating the results of these processes, e.g. the present bathymetric and back-scatter characteristics of the seafloor. The investigation area is probably unique in terms of diversity of processes which can be examined in a relatively small region. Text Arctic Arctic Ocean Greenland Greenland Sea Ice Shelves Iceberg* Sea ice Spitsbergen Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Greenland |
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Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography Geology Geochemistry and Mineralogy *GEOLOGY *GEOPHYSICS GREENLAND SEA MATERIAL PROPERTIES |
spellingShingle |
Physical and Dynamic Oceanography Geology Geochemistry and Mineralogy *GEOLOGY *GEOPHYSICS GREENLAND SEA MATERIAL PROPERTIES Shor, Alexander N. Crane, Kathleen de Moustier, Christian Geology and Geophysics Program Summary for FY90. SEAMARC II investigation of the Northern Norwegian-Greenland Sea: Program 1990 and Expansion |
topic_facet |
Physical and Dynamic Oceanography Geology Geochemistry and Mineralogy *GEOLOGY *GEOPHYSICS GREENLAND SEA MATERIAL PROPERTIES |
description |
The high-latitude northern Norwegian-Greenland Sea and the adjacent part of the Arctic Ocean north of Spitsbergen comprise an unequaled natural laboratory for the study of several important processes involving the generation and/or modification of sea-floor topography, subbottom structure, and material properties. These processes, active now or in the geologically recent past, include (1) tectonism (faulting), volcanism, magma intrusion into rift valley seafloor sediments; (2) erosion and redeposition of sediment by bottom currents; (3) slumping and other downslope processes on glaciated margins; (4) sedimentation from sea ice/icebergs/ice sheets, at water depths less than 100- 500 m, (5) erosion and redeposition by icebergs and grounded ice shelves/sheets. SeaMARC II is the ideal tool for investigating the results of these processes, e.g. the present bathymetric and back-scatter characteristics of the seafloor. The investigation area is probably unique in terms of diversity of processes which can be examined in a relatively small region. |
author2 |
HAWAII INST OF GEOPHYSICS HONOLULU |
format |
Text |
author |
Shor, Alexander N. Crane, Kathleen de Moustier, Christian |
author_facet |
Shor, Alexander N. Crane, Kathleen de Moustier, Christian |
author_sort |
Shor, Alexander N. |
title |
Geology and Geophysics Program Summary for FY90. SEAMARC II investigation of the Northern Norwegian-Greenland Sea: Program 1990 and Expansion |
title_short |
Geology and Geophysics Program Summary for FY90. SEAMARC II investigation of the Northern Norwegian-Greenland Sea: Program 1990 and Expansion |
title_full |
Geology and Geophysics Program Summary for FY90. SEAMARC II investigation of the Northern Norwegian-Greenland Sea: Program 1990 and Expansion |
title_fullStr |
Geology and Geophysics Program Summary for FY90. SEAMARC II investigation of the Northern Norwegian-Greenland Sea: Program 1990 and Expansion |
title_full_unstemmed |
Geology and Geophysics Program Summary for FY90. SEAMARC II investigation of the Northern Norwegian-Greenland Sea: Program 1990 and Expansion |
title_sort |
geology and geophysics program summary for fy90. seamarc ii investigation of the northern norwegian-greenland sea: program 1990 and expansion |
publishDate |
1991 |
url |
http://www.dtic.mil/docs/citations/ADA266622 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA266622 |
geographic |
Arctic Arctic Ocean Greenland |
geographic_facet |
Arctic Arctic Ocean Greenland |
genre |
Arctic Arctic Ocean Greenland Greenland Sea Ice Shelves Iceberg* Sea ice Spitsbergen |
genre_facet |
Arctic Arctic Ocean Greenland Greenland Sea Ice Shelves Iceberg* Sea ice Spitsbergen |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA266622 |
op_rights |
Approved for public release; distribution is unlimited. |
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1766336967221444608 |