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The South German Scarplands〔Dickinson (1964), pp 564-584.〕 is a geological and geomorphological natural region or landscape in Switzerland and the south German states of Bavaria and Baden-Württemberg. The landscape is characterised by escarpments. It is variously referred to in the German literature as the: * ''Südwestdeutsche Schichtstufenland'' (Southwest German Scarplands) * ''Südwestdeutsche Schichtstufenlandschaft'' (Southwest German Scarp Landscape) * ''Schwäbisch-Fränkische(s) Schichtstufenland'' (Swabian-Franconian Scarpland(scape)) * ''Süddeutsche(s) Schichtstufenland(schaft)'' (South German Scarpland(scape)) == Location and short description == The South German Scarplands run (from north(-northeast) to south(-southwest)) more or less between the southern Rhön, the Spessart, the Odenwald and the Black Forest in the west, the Franconian Jura in the east, the Swabian Jura to the southeast and the northeastern foothills of the Jura to the south. The wooded west and northwest-facing scarps drop sharply towards the Rhine Rift Valley and the Rhine-Main Plain, whilst the dip slopes fall comparatively gradually towards the (north-)east into the depressions beyond which lie the Thuringian Forest, Thuringian Highland, Franconian Forest, Fichtelgebirge, Upper Palatine Forest and Bavarian Forest. Similarly the Swabian and Franconian Jura descend quite gently towards the south(east) to the Danube valley, whilst the Swabian Jura, for example, drop very steeply to the north(-northwest) from the so-called Albtrauf - the top of the main scarp.〔Dickinson (1964), p 567.〕 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 German Scarplands」の詳細全文を読む スポンサード リンク
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