Genesis of the cliff-face near Bergen op Zoom in the southwest of the Netherlands
Abstract
A cliff-face stretching north-south in the southwest part of the Netherlands, (from Halsteren to near the Belgium border) separates Holocene marine sediments from tidal and aeolian Pleistocene deposits. There is a difference of opinion regarding the age of the formation of this cliff-face. The main objective of this study was to verify the origin of this feature. To this end auger drilling and pollen analysis on peat was carried out. The cliff-face proved to have been formed by marine erosion during the Eemian.
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