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・ Danube Army
・ Danube Banovina
・ Danube Bend
・ Danube bleak
・ Danube Bridge
・ Danube Canyon
・ Danube Commission (1948)
・ Danube company
・ Danube Cossack Host
・ Danube Cossacks
・ Danube crested newt
・ Danube Delta
・ Danube delta dwarf goby
・ Danube Delta horse
・ Danube Express
Danube fan
・ Danube Flotilla
・ Danube glaciation
・ Danube International School
・ Danube Legion
・ Danube Palace
・ Danube Planum
・ Danube Private University
・ Danube Promenade
・ Danube Province
・ Danube River Commission
・ Danube River Conference of 1948
・ Danube school
・ Danube Seven
・ Danube Sinkhole


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Danube fan : ウィキペディア英語版
Danube fan
The Danube fan is a relict sedimentary feature in the northwestern part of the bottom of the Black Sea. It crosses three of its four major physiographic provinces: basin slope, basin apron, and the Euxine abyssal plain) and splits the abyssal plain into two inequal parts.〔Chapter: "Bathymetry and Microtopography of Black Sea: Structure" of the 20th Memoir ''The Black Sea — Geology, Chemistry, and Biology'' of the American Association of Petroleum Geologists (1974)〕
The fan was deposited by the Danube (mostly), Dniester, Southern Bug, and Dnieper rivers. It extends from the shelf break zone an approximately 200m isobath〔"Environmental Degradation of the Black Sea: Challenges and Remedies", editors Șükrü T. Beșiktepe, Ümit Ünlüata, Alexandru S. Bologa, 1999, ISBN

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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