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Dike Cirque
Dike Cirque () is a semi-circular glacial cirque wide in the Miller Range of Antarctica. It is carved into the Macdonald Bluffs at the southeast base of Kreiling Mesa. It was so named by the Ohio State University Geological Party, 1967–68, because the granite cliffs surrounding the cirque are cut by numerous black dikes.〔 == 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「Dike Cirque」の詳細全文を読む
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