Über Aufbau und Altersgliederung des Holozäns der Lüneburger Elbmarsch

Jobst-Henrich Benzler
At the beginning of the Holocene the glaciofluvial sands of the Elbe glacial stream valley were traversed by channels of melting waters, through which the old arms of the river Elbe were flowing. The winds accumulated these sands to dunes, on the top of which podzols were formed. During the whole of the Holocene the river Elbe deposited loamy-sandy sediments on the higher zone near the banks, but clayey sediments in the lower zone of...