The morphogenesis of tills below the culmination zones of the Weichselian inland ice has been studied in an upland area with a relief of 1500 m. The thickness of the tills varies considerably, depending principally on ...

A number of localities with sub-till sediments have recently been found in the Gudbrandsdal area. The sediments are mostly of glacio-lacustrine origin and of an assumed Middle Weichselian age. Only a few of the findings ...