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Line 1: {{Short description|Part of the Southern Ocean along the Antarctic Peninsula}} [[File:Antarctic-seas-en. The '''Bellingshausen Sea''' is an area along the west side of the [[Antarctic Peninsula]], west of [[Alexander Island]], east of [[Cape Flying Fish]] on [[Thurston Island]], and south of [[Peter I Island]] (there the southern ''Vostokkysten'').<ref>[http://data.aad.gov.au/aadc/gaz/display_name.cfm?gaz_id=107742 Australian Antarctic Data Centre, Antarctic Gazetteer: Bellingshausen Sea]</ref> In the south are, from west to east, [[Eights Coast]], [[Bryan Coast]] and [[English Coast]] (west part) of [[West Antarctica]]. To the west of Cape Flying Fish joins [[Amundsen Sea]].▼ [[File:Bellingshausen_Sea_shaded_and_IHO_proposal.svg|thumb|upright=1.5|Bellingshausen Sea, [[International Hydrographic Organization|IHO]] definition (proposed)]] ▲The '''Bellingshausen Sea''' is an area along the west side of the [[Antarctic Peninsula]] between 57°18'W and 102°20'W, west of [[Alexander Island]], east of [[Cape Flying Fish]] on [[Thurston Island]], and south of [[Peter I Island]] (there the southern ''Vostokkysten'').<ref>[http://data.aad.gov.au/aadc/gaz/display_name.cfm?gaz_id=107742 Australian Antarctic Data Centre, Antarctic Gazetteer: Bellingshausen Sea]</ref> Bellingshausen Sea has an area of {{convert|487,000|km2|abbr=on}} and reaches a maximum depth of {{convert| The Antarctic Slope Current (ASC) is thought to originate in the Bellingshausen Sea as the result of a density front at the shelf break, rather than being wind-driven.<ref>{{Cite journal |last1=Thompson |first1=Andrew F. |last2=Speer |first2=Kevin G. |last3=Schulze Chretien |first3=Lena M. |date=2020-08-28 |title=Genesis of the Antarctic Slope Current in West Antarctica |url=https://authors.library.caltech.edu/records/a4mft-xj680/files/2020GL087802.pdf?download=1 |journal=Geophysical Research Letters |language=en |volume=47 |issue=16 |doi=10.1029/2020GL087802 |bibcode=2020GeoRL..4787802T |issn=0094-8276}}</ref> It takes its name from [[Admiral Thaddeus Bellingshausen]], who explored in the area in 1821.▼ ▲It takes its name from [[ In the late [[Pliocene Epoch]], about 2.15 million years ago, the [[Eltanin asteroid]] impacted here. This is the only known impact in a [[deep ocean|deep-ocean basin]] in the world.<ref>{{cite journal |last=Gersonde |first=Rainer |author2=F. T. Kyte |author3=T. Frederichs |author4=U. Bleil |author5=H.-W. Schenke |author6=G. Kuhn |year=2005 |title=The late Pliocene impact of the Eltanin asteroid into the Southern Ocean – Documentation and environmental consequences |journal=Geophysical Research Abstracts |volume=7 |id=1607-7962/gra/EGU05-A-02449 |url=http://www.cosis.net/abstracts/EGU05/02449/EGU05-J-02449.pdf |accessdate=2008-06-22}}</ref>▼ ▲In the late [[Pliocene Epoch]], about 2.15 million years ago, the [[Eltanin asteroid]] (about 1-4 km in diameter) impacted ==References== Line 13 ⟶ 17: ==External links== * [https://web.archive.org/web/20061011091638/http://www.visibleearth.nasa.gov/view_rec.php?id=3939 NASA Bellinghausen Sea satellite photo]▼
▲* [http://visibleearth.nasa.gov/view_rec.php?id=3939 NASA Bellinghausen Sea satellite photo] * [http://www.antarctica.ac.uk/data/absl/ Bellinghausen Sea climatological low pressure system]
{{List of seas}} {{Authority control}}▼ {{coord|71|S|85|W|scale:10000000_source:GNIS|display=title}} ▲{{Authority control}} [[Category:Seas of the Southern Ocean]] [[Category:Antarctic region]] |