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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)』 ■ウィキペディアで「Danube fan」の詳細全文を読む
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