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Abstract
The pronounced ice marginal deposit on the west coast of Sweden called the Gothenburg moraine, is discussed. This terminal moraine has been surveyed from the eastern part of Gothenburg in the north to the area south of the river Viskan in the south. About 17 kilometres in the northern part of the county of Halland is surveyed for a map in the scale of 1:20.000. The general features of the terminal moraine and its relation to topographical conditions, its stratification and age are discussed.