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Sigsbee Escarpment : ウィキペディア英語版 | Sigsbee Escarpment
The Sigsbee Escarpment is a major bathymetric feature of the Gulf of Mexico, extending for about . It separates the lower continental slope of the northern gulf from the abyssal plain of the Sigsbee Deep and has up to of relief across it. It has formed as a result of salt tectonics, due to the effects of loading of a thick layer of Jurassic halite (Louann Salt) by Upper Jurassic to Cenozoic sedimentary rocks. ==References==
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「Sigsbee Escarpment」の詳細全文を読む
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