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Abstract
The till in the central part of the province of Skåne, southern Sweden, was investigated with reference to the content of indicators from local bedrock sources. Samples were taken 0.5–1.0 m below the ground surface and the size fraction 4–6 mm was analyzed. The indicator trains demonstrate that the last ice-movement which prevailed in the whole area investigated was from the ENE. Later, in the eastern part of the area, an ice-movement from the NE occurred.