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Danmarks Geologiske Undersøgelse II. Række
The investigations of the glacial sequence in the Randers area include mapping of the surface layers, study of bore profiles and detailed examination of outcrops, concentrating on the determination of transport directions in the deposits.The following stratigraphic succession has been established:Highest: NE tillTebbestrup Formation (melt water deposits)SE tillHaldum Formation (melt water deposits)Lowest: NE tillThe two uppermost units can with certainty be referred to Weichselian. Argumentsdoi:10.34194/raekke2.v111.6902 fatcat:evvgaabh5jggrnkiybbr3ildqe