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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 Cantonnier Lode ： ウィキペディア英語版 Cantonnier Lode The Cantonnier lode formed in the Piégut-Pluviers Granodiorite, part of the basement rocks of the northwestern French Massif Central. Its importance is highlighted by very rare mineral parageneses. == Geography == The lode lies about 2 kilometers east of the town of Nontron, the northern ''subpréfecture'' of the Dordogne. It can be reached via a small left side stream of the Bandiat River; the stream starts at the hamlet of ''Brégout'', flows to the Northwest past the lode and merges just upstream from ''Moulin de Bord'' with the Bandiat. Higher up on its left hillslope passes the D 707 from Nontron to Saint-Pardoux-la-Rivière. The lode is known to be at least 70 meters long ending at an elevation of 185 meters near the left bank of the stream. 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「Cantonnier Lode」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.