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Emerald Fracture Zone : ウィキペディア英語版 | Emerald Fracture Zone
Emerald Fracture Zone () is an undersea fracture zone running the distance from the southwest corner of the Campbell Plateau to the northern tip of Iselin Bank. The name was proposed by Dr. Steven C. Cande of the Scripps Institution of Oceanography for the vessel ''Emerald'', which traversed this region in 1821, and was approved by the Advisory Committee for Undersea Features in June 1997.〔 == 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「Emerald Fracture Zone」の詳細全文を読む
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