Abstract

The Brorfelde hills in northwestern Sjælland are built up of thick fluvioglacial deposits covered by basal till. A stress analysis of syn‐ and postdepositional normal faults in these sediments indicates that the faults are a result of buried dead ice. The hills can be classified as autochthonous ice‐sustained kame or crevasse deposits which have been transgressed by a later ice advance

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