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The paleic surface or palaeic surface ((ノルウェー語:paleisk overflate), 〔) is an erosion surface of gentle slopes that exist in Southern Norway. It is considered a continuation to the Sub-Cambrian peneplain found further east. The peneplain surfaces of the paleic surface are apparently disrupted by vertical displacement along faults, following an NNE-SSW orientation.〔 The paleic surface has reached its elevated position in a process related to the opening Atlantic Ocean that begun 140 millions years ago. The concept of a paleic surface was first introduced by Hans Reusch in 1901. ==See also== *Muddus plains *South Småland peneplain *Strandflat 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「Paleic surface」の詳細全文を読む スポンサード リンク
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