Late Weichselian and Holocene marine transgressions in northern Jutland, Denmark.

Abstract

New information regarding the history of the Limfjord is presented, based on two investigation wells at the Agger isthmus, showing a transgression of the SW part of the Limfjord during the Boreal and Early Atlantic followed by a continuous marine sedimentation up to within the Iron Age, 2110 BP. -from Author