In the Kullen region in northwestern Scania, the author has examined the lithologic composition of the fine gravel fraction in different till beds, with the aim of elucidating the direction and chronology of the corresponding ice streams. The determining factor has been to find, in one and the same section, direction-indicating additional material in a till in relation to the immediate older till. Complete till cuttings have been prerequisite for this. Two examples are given of the applicability of the method in the Kullen region, where there are very few conventional indicator boulders. The examples are illustrated by diagrams which show the changes in the lithologic composition of the different stratigraphic levels in each section. The method and results of the author differ in essential respects from those of earlier investigators in this region.