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Abstract
Till fabric in a dislocated till from a coastal cliff in western Sjælland, Denmark, is decribed. Based on analyses of different parts of a recumbent syncline, possible causes for the formation of the dislocations and the internal till fabric are discussed. It is concluded that the present till fabric is developed from an earlier fabric, which was reorientated subglacially due to inhomogeneous shear in connection with the transgression of a later glacier.