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Glacier foreland : ウィキペディア英語版 | Glacier foreland
The region between the current leading edge of the glacier and the moraines of latest maximum is called glacier foreland or glacier forefield. In the Alps this maximum was in 1850 and since then the region has become ice free due to deglaciation. Because of this relative recent development of vegetation and morphodynamic the glacier foreland differs considerably from the surrounding landscape. ==See also==
*List of alluvial sites in Switzerland
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「Glacier foreland」の詳細全文を読む
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