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La pénéplanation des chaînes de montagnes est généralement considérée comme résultant de l'action de l'érosion à long terme, qui lisse le relief et diminue leur altitude jusqu'à tendre vers le niveau marin. Nous proposons un nouveau modèle, dans lequel la sédimentation de piedmont traduit une montée du niveau de base de la chaîne, entraînant son aplanissement en altitude. Ce modèle est illustré à...
Set the date range to filter the displayed results. You can set a starting date, ending date or both. You can enter the dates manually or choose them from the calendar.