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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 Pendant bar ： ウィキペディア英語版 Pendant bar A pendant bar is a fluvial geomorphology term that is usually applied to large landforms created by large scale flooding events. Pendant bars are thin, sharp-crested deposits, and are typically made up of coarser sediment from the bed load. This type of bar is found on the downstream side of a weathering-resistant protrusion such as a large outcrop of bedrock, and is separated from the protrusion by a depression. ==Formation== Pendant bars form as high-velocity floodwater moves around a protrusion. The water scours out a depression behind the protusion and deposits the sediment a short distance downstream in a bar-shaped formation. A similar process forms a sand splay, which is much like a shoal but is formed on floodplains or terraces in lower-intensity flooding episodes.〔 Other fluvial features that are formed by bed load sediments are the point bar, longitudinal bar, and expansion bar.〔(【引用サイトリンク】title=The Lake Bonneville Flood )〕 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「Pendant bar」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.