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翻訳と辞書　辞書検索 [ 開発暫定版 ] スポンサード リンク Stavelot Massif ： ウィキペディア英語版 Stavelot Massif The Stavelot Massif is a geological massif in the Belgian Ardennes (geologically a part of the Rhenish Massif). Most of the massif crops out in Belgium, but a small part lies across the border with Germany. The massif consists of early Paleozoic (late Cambrian and Ordovician in age) metamorphic rocks, mostly quartzites and phyllites. In other parts of the Ardennes they form a basement which is covered by only slightly metamorphosed late Paleozoic limestones and sandstones, that only saw a low degree of metamorphism. On the other hand, the early Paleozoic rocks were deformed and metamorphosed to a higher degree during the Caledonian orogeny (about ). Both the Caledonian basement and the low grade cover rocks were deformed again during the Hercynian orogeny (about ). This phase of deformation created a large northeast-southwest oriented anticline that runs across the Belgian part of the Rhenish Massif (the Ardennes anticline). In the core of this anticline a number of massifs of early Paleozoic rocks crop out. The Stavelot Massif is one the larger, other Caledonian massifs are the Rocroi Massif, the Serpont Massif and the Givonne Massif. The higher competence of the Caledonian basement rocks made them more resistant to erosion. The massif therefore forms a plateau in the topography. This plateau is called the High Fens and encompasses the highest summits of Belgium. 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「Stavelot Massif」の詳細全文を読む スポンサード リンク 翻訳と辞書 : 翻訳のためのインターネットリソース Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.