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South Småland peneplain : ウィキペディア英語版 | South Småland peneplain
The South Småland peneplain ((スウェーデン語:Sydsmåländska peneplanet)) is a large flattish erosion surface, a peneplain, formed during the Tertiary, covering large swathes of southern Småland and nearby areas in Southern Sweden.〔 The South Småland peneplain is believed to never have been covered by sedimentary rocks. To the south and west (chiefly Halland and Blekinge) the peneplain transitions into Mesozoic aged non-peneplain surfaces.〔 The surface extends over an altitude range of 100 to 150 meters above sea level. The existence of this plain was first noted by Sten De Geer in 1913 who termed it ''Smålands urbergslätt''.〔 ==See also==
*Norrland terrain *Paleic surface *Sub-Cambrian peneplain
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「South Småland peneplain」の詳細全文を読む
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