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This paper deals wi th erosional forms, especially those caused by running water , in the central South Swedish Highlands. The southern area is well peneplained and resembles a lake plateau wi th gently inclining facet towards the S, SW and SE. Nor thwards and towards the centre the relief locally increases as the landscape rises. The southern area is characterized by small erosion channels originat ing f rom the last glaciation, but in the central and nor thern areas there are also large canyons in the bedrock.

Erosion channels and canyons in the central South Swedish Highlands – a short survey