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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 Caves of the Tullybrack and Belmore hills ： ウィキペディア英語版 Caves of the Tullybrack and Belmore hills The Caves of the Tullybrack and Belmore hills can be found in south-west County Fermanagh, Northern Ireland. The region is also described as the West Fermanagh Scarplands by environmental agencies and shares many similar karst features with the nearby Marble Arch Caves Global Geopark. The caves are situated under the hills of Tullybrack () – which incorporates Glenkeel () and Knockmore () – and Belmore () and feature three major cave systems: Reyfad–Glenkeel, Noon's Hole–Arch Cave and Boho Caves. They have been described as nationally significant by the Northern Ireland Environment Agency.〔(【引用サイトリンク】publisher=Northern Ireland Environment Agency )〕 The caves and related features are formed predominantly in the Dartry Limestone Formation – a sequence of rocks assigned to the Asbian sub-stage of the Visean stage of the Carboniferous period. Within this Formation, the Knockmore Limestone Member is also an important cave forming rock sequence. Cave development has occurred within the Quaternary period and certain features are ascribed to the Holocene epoch of the last 10,000 years. With the exception of Arch Cave, all of the caves and related karstic features listed below have been designated as provisional Areas of Special Scientific Interest (provisional ASSIs or PASSI's) – a conservation designation in Northern Ireland equivalent to SSSI's in other parts of the United Kingdom. == Belmore Mountain == 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「Caves of the Tullybrack and Belmore hills」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.