Sie befinden Sich nicht im Netzwerk der Universität Paderborn. Der Zugriff auf elektronische Ressourcen ist gegebenenfalls nur via VPN oder Shibboleth (DFN-AAI) möglich. mehr Informationen...
A younger glacial signature is superimposed on this old fluvial landscape, with selective erosion where the base of the ice sheet was at the pressure melting point and preservation of the old landscape where the base of the ice was cold. Resolution of this issue requires a detailed knowledge of the behaviour of the ice sheet during the last glacial maximum and the Holocene, as the globe transitioned from full-glacial to full-interglacial conditions.