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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 Geology of Rutland ： ウィキペディア英語版 Geology of Rutland The geology of Rutland in eastern England largely consists of sedimentary rocks of Jurassic age which dip gently eastwards. == Jurassic == The oldest rocks that occur at the surface in the county of Rutland are the mudstones and limestones of the early Jurassic Lias Group. These are overlain to the east by a middle Jurassic sequence involving limestones, sandstones and mudstones of the Inferior Oolite Group and the succeeding Great Oolite Group with numerous outliers of the former occurring around Rutland Water and the country to its south. The lower part of the Great Oolite Group in the part of the Jurassic outcrop between Oxfordshire and Lincolnshire was once known as the 'Upper Estuarine Series' but is now formally referred to as the Rutland Formation. It comprises a series of seven or more depositional cycles resulting in a repeated suite of clays, limestones and clastics, some of which are marine in origin.〔Brenchley et al p348〕 A small outlier of the Oxford Clay Formation is found near Duddington, the main extent of this younger rock unit lying to the east of the county.〔British Geological Survey 1:625,000 scale geological map ''Bedrock Geology UK South'' 5th Edn. NERC 2007〕 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「Geology of Rutland」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.