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Paha (landform) : ウィキペディア英語版 | Paha (landform)
Paha are landforms composed of prominent hills that are oriented from northwest to southeast and typically have large loess deposits. They developed during the period of mass erosion that developed the Iowan surface, and are considered erosional remnants and are often at interstream divides. Paha generally rise above the surrounding landscape more than .〔(Paha Ridge Landform Features of Iowa ), Iowa Geological Survey, 2006. Accessed 2008-08-12.〕 The word ''paha'' means hill in Dakota Sioux.〔''Landforms of Iowa'' by Jean C. Prior, University of Iowa Press, Iowa City, 1991〕 A well known Paha is the hill on which the town of Mount Vernon, Iowa developed. == Origin ==
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「Paha (landform)」の詳細全文を読む
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