OCEANOGRAPHIC CRUISE SUMMARY GEOPHYSICAL INVESTIGATIONS IN THE NORTHERN LABRADOR SEA.

A cooperative Naval Oceanographic Office, University of Wisconsin, and U.S. Coast Guard geological, geophysical survey was conducted in the northern Labrador Sea during August and September 1967. Bathymetry, magnetics, seismic reflection, and seismic refraction observations were obtained. The geomor...

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Main Author: Johnson, G. Leonard
Other Authors: NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS
Format: Text
Language:English
Published: 1968
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0835675
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0835675
id ftdtic:AD0835675
record_format openpolar
spelling ftdtic:AD0835675 2023-05-15T16:00:13+02:00 OCEANOGRAPHIC CRUISE SUMMARY GEOPHYSICAL INVESTIGATIONS IN THE NORTHERN LABRADOR SEA. Johnson, G. Leonard NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS 1968-05 text/html http://www.dtic.mil/docs/citations/AD0835675 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0835675 en eng http://www.dtic.mil/docs/citations/AD0835675 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography (*MARINE GEOPHYSICS NEWFOUNDLAND(PROVINCE)) BATHYTHERMOGRAPH DATA OCEANOGRAPHIC SHIPS SEISMOLOGY OCEAN BOTTOM REFLECTION OCEAN BOTTOM TOPOGRAPHY MAGNETIC FIELDS REFRACTION OCEAN CURRENTS HYDROGRAPHIC SURVEYING ROCK SEDIMENTATION GREENLAND Text 1968 ftdtic 2016-02-19T05:33:57Z A cooperative Naval Oceanographic Office, University of Wisconsin, and U.S. Coast Guard geological, geophysical survey was conducted in the northern Labrador Sea during August and September 1967. Bathymetry, magnetics, seismic reflection, and seismic refraction observations were obtained. The geomorphology of the sea floor was delineated and was found to be more complex than previously thought. North-south striking sea floor canyons and a trench at the base of the Greenland continental slope were investigated. These features possibly are the result of large scale sea floor sculpting by bottom currents. Investigations revealed that the western portion of Davis Strait is swept clear of sediments and consists of outcropping basement rock. (Author) Text Davis Strait Greenland Labrador Sea Newfoundland Defense Technical Information Center: DTIC Technical Reports database Greenland Newfoundland
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
(*MARINE GEOPHYSICS
NEWFOUNDLAND(PROVINCE))
BATHYTHERMOGRAPH DATA
OCEANOGRAPHIC SHIPS
SEISMOLOGY
OCEAN BOTTOM
REFLECTION
OCEAN BOTTOM TOPOGRAPHY
MAGNETIC FIELDS
REFRACTION
OCEAN CURRENTS
HYDROGRAPHIC SURVEYING
ROCK
SEDIMENTATION
GREENLAND
spellingShingle Physical and Dynamic Oceanography
(*MARINE GEOPHYSICS
NEWFOUNDLAND(PROVINCE))
BATHYTHERMOGRAPH DATA
OCEANOGRAPHIC SHIPS
SEISMOLOGY
OCEAN BOTTOM
REFLECTION
OCEAN BOTTOM TOPOGRAPHY
MAGNETIC FIELDS
REFRACTION
OCEAN CURRENTS
HYDROGRAPHIC SURVEYING
ROCK
SEDIMENTATION
GREENLAND
Johnson, G. Leonard
OCEANOGRAPHIC CRUISE SUMMARY GEOPHYSICAL INVESTIGATIONS IN THE NORTHERN LABRADOR SEA.
topic_facet Physical and Dynamic Oceanography
(*MARINE GEOPHYSICS
NEWFOUNDLAND(PROVINCE))
BATHYTHERMOGRAPH DATA
OCEANOGRAPHIC SHIPS
SEISMOLOGY
OCEAN BOTTOM
REFLECTION
OCEAN BOTTOM TOPOGRAPHY
MAGNETIC FIELDS
REFRACTION
OCEAN CURRENTS
HYDROGRAPHIC SURVEYING
ROCK
SEDIMENTATION
GREENLAND
description A cooperative Naval Oceanographic Office, University of Wisconsin, and U.S. Coast Guard geological, geophysical survey was conducted in the northern Labrador Sea during August and September 1967. Bathymetry, magnetics, seismic reflection, and seismic refraction observations were obtained. The geomorphology of the sea floor was delineated and was found to be more complex than previously thought. North-south striking sea floor canyons and a trench at the base of the Greenland continental slope were investigated. These features possibly are the result of large scale sea floor sculpting by bottom currents. Investigations revealed that the western portion of Davis Strait is swept clear of sediments and consists of outcropping basement rock. (Author)
author2 NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS
format Text
author Johnson, G. Leonard
author_facet Johnson, G. Leonard
author_sort Johnson, G. Leonard
title OCEANOGRAPHIC CRUISE SUMMARY GEOPHYSICAL INVESTIGATIONS IN THE NORTHERN LABRADOR SEA.
title_short OCEANOGRAPHIC CRUISE SUMMARY GEOPHYSICAL INVESTIGATIONS IN THE NORTHERN LABRADOR SEA.
title_full OCEANOGRAPHIC CRUISE SUMMARY GEOPHYSICAL INVESTIGATIONS IN THE NORTHERN LABRADOR SEA.
title_fullStr OCEANOGRAPHIC CRUISE SUMMARY GEOPHYSICAL INVESTIGATIONS IN THE NORTHERN LABRADOR SEA.
title_full_unstemmed OCEANOGRAPHIC CRUISE SUMMARY GEOPHYSICAL INVESTIGATIONS IN THE NORTHERN LABRADOR SEA.
title_sort oceanographic cruise summary geophysical investigations in the northern labrador sea.
publishDate 1968
url http://www.dtic.mil/docs/citations/AD0835675
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0835675
geographic Greenland
Newfoundland
geographic_facet Greenland
Newfoundland
genre Davis Strait
Greenland
Labrador Sea
Newfoundland
genre_facet Davis Strait
Greenland
Labrador Sea
Newfoundland
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0835675
op_rights APPROVED FOR PUBLIC RELEASE
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