The Quaternary of the Lower Rhine Bay - deposits of the last ice age on the Lower Rhine

The special publication gives the readership the opportunity to get an overview of the strata sequences of the Quaternary of the Lower Rhine Bay and their chronostratigraphic subdivision in a short time. A powerful and relatively complete stratum sequence of the Quaternary period could be deposited, because the Lower Rhine Bay is a young tectonic subsidence area. The descriptions of the sedimentary units are primarily based on the recordings of gravel and clay pits as well as drilling. [1992. 200 p., 30 fig., 8 tab., 1 color. Kt. 1:200,000; ISBN 978-3-86029-925-8 (out of print)]