THE BOTTOM RELIEF OF THE BERING SEA
The Bering Sea is a deep-water sea with a maximum depth of 4420 m in Kamchatskiy Proliv and somewhat lesser depths (4151 and 4096 m, as far as is known) in the deep trough of the sea. The Bering Sea is much deeper than the shallow seas along the continental shelf. This is the deepest sea in the Far...
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ftdtic:AD0602196 2023-05-15T15:42:50+02:00 THE BOTTOM RELIEF OF THE BERING SEA Udintsev,G. B. Boichenko,I. B. Kanaev,V. F. AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS 1963-09 text/html http://www.dtic.mil/docs/citations/AD0602196 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0602196 en eng http://www.dtic.mil/docs/citations/AD0602196 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS BERING SEA OCEAN BOTTOM TOPOGRAPHY MARINE GEOLOGY HYDROGRAPHIC SURVEYING OCEANOGRAPHIC DATA MAPS SCIENTIFIC ORGANIZATIONS OCEANOGRAPHY USSR Text 1963 ftdtic 2016-02-21T16:36:18Z The Bering Sea is a deep-water sea with a maximum depth of 4420 m in Kamchatskiy Proliv and somewhat lesser depths (4151 and 4096 m, as far as is known) in the deep trough of the sea. The Bering Sea is much deeper than the shallow seas along the continental shelf. This is the deepest sea in the Far East; its maximum depth is 751 m greater than the corresponding depth of the Sea of Japan (3669 m) and 1046 m greater than that of the Sea of Okhotsk (3370m). In the region north of Kamchatskiy Proliv, the bottom rises in the form of a sill, whose depth does not exceed 3589 m. The main feature of the Bering Sea is its division into two distinct parts: a vast shallow water area with depths less than 200 m and a deep basin with depths greater than 3000 m. Rel'ef Dna Beringova Morya, trans. of Akademiya Nauk SSSR. Institut Okeanologii. Trudy, 1959, v. 29, p. 17-64. Text Bering Sea Defense Technical Information Center: DTIC Technical Reports database Bering Sea Kamchatskiy ENVELOPE(163.053,163.053,56.022,56.022) Kamchatskiy Proliv ENVELOPE(164.500,164.500,56.000,56.000) Okhotsk |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
BERING SEA OCEAN BOTTOM TOPOGRAPHY MARINE GEOLOGY HYDROGRAPHIC SURVEYING OCEANOGRAPHIC DATA MAPS SCIENTIFIC ORGANIZATIONS OCEANOGRAPHY USSR |
spellingShingle |
BERING SEA OCEAN BOTTOM TOPOGRAPHY MARINE GEOLOGY HYDROGRAPHIC SURVEYING OCEANOGRAPHIC DATA MAPS SCIENTIFIC ORGANIZATIONS OCEANOGRAPHY USSR Udintsev,G. B. Boichenko,I. B. Kanaev,V. F. THE BOTTOM RELIEF OF THE BERING SEA |
topic_facet |
BERING SEA OCEAN BOTTOM TOPOGRAPHY MARINE GEOLOGY HYDROGRAPHIC SURVEYING OCEANOGRAPHIC DATA MAPS SCIENTIFIC ORGANIZATIONS OCEANOGRAPHY USSR |
description |
The Bering Sea is a deep-water sea with a maximum depth of 4420 m in Kamchatskiy Proliv and somewhat lesser depths (4151 and 4096 m, as far as is known) in the deep trough of the sea. The Bering Sea is much deeper than the shallow seas along the continental shelf. This is the deepest sea in the Far East; its maximum depth is 751 m greater than the corresponding depth of the Sea of Japan (3669 m) and 1046 m greater than that of the Sea of Okhotsk (3370m). In the region north of Kamchatskiy Proliv, the bottom rises in the form of a sill, whose depth does not exceed 3589 m. The main feature of the Bering Sea is its division into two distinct parts: a vast shallow water area with depths less than 200 m and a deep basin with depths greater than 3000 m. Rel'ef Dna Beringova Morya, trans. of Akademiya Nauk SSSR. Institut Okeanologii. Trudy, 1959, v. 29, p. 17-64. |
author2 |
AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS |
format |
Text |
author |
Udintsev,G. B. Boichenko,I. B. Kanaev,V. F. |
author_facet |
Udintsev,G. B. Boichenko,I. B. Kanaev,V. F. |
author_sort |
Udintsev,G. B. |
title |
THE BOTTOM RELIEF OF THE BERING SEA |
title_short |
THE BOTTOM RELIEF OF THE BERING SEA |
title_full |
THE BOTTOM RELIEF OF THE BERING SEA |
title_fullStr |
THE BOTTOM RELIEF OF THE BERING SEA |
title_full_unstemmed |
THE BOTTOM RELIEF OF THE BERING SEA |
title_sort |
bottom relief of the bering sea |
publishDate |
1963 |
url |
http://www.dtic.mil/docs/citations/AD0602196 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0602196 |
long_lat |
ENVELOPE(163.053,163.053,56.022,56.022) ENVELOPE(164.500,164.500,56.000,56.000) |
geographic |
Bering Sea Kamchatskiy Kamchatskiy Proliv Okhotsk |
geographic_facet |
Bering Sea Kamchatskiy Kamchatskiy Proliv Okhotsk |
genre |
Bering Sea |
genre_facet |
Bering Sea |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0602196 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766376797475176448 |