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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 Winchester-King's Somborne Syncline ： ウィキペディア英語版 Winchester-King's Somborne Syncline The Winchester-King's Somborne Syncline is one of a series of parallel east-west trending folds in the Cretaceous chalk of Hampshire. It lies at the western end of the South Downs, immediately to the north of the Winchester-East Meon Anticline and east of Salisbury Plain. ==Structure== The fold axis runs for around from north of East Tytherley in the west, between Winchester and Kings Worthy, towards Four Marks in the east. To the north-east of Winchester the fold axis is followed by the valley of the River Itchen, which turns abruptly south to cut across the structure and the Winchester-East Meon Anticline to the south. Parallel folds to the north include the Stockbridge Anticline and the Micheldever Syncline. To the south-west across the River Test is the similar Alderbury-Mottisfont Syncline. As with other nearby folds, the structure is controlled by movement of fault blocks within the Jurassic strata below. 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「Winchester-King's Somborne Syncline」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.