EGQSJ E&G Quaternary Science Journal EGQSJ E&G Quaternary Sci. J. 2199-9090 Geozon Science Media Göttingen, Germany 10.3285/eg.15.1.02 Eine begrabene Solifluktionsdecke und ihr Einfluß auf die heutige Vegetation: Beobachtungen auf einer Bliesterterrasse (Saarland) Hard Gerhard 01 11 1964 15 1 40 43 Copyright: © 1964 Gerhard Hard 1964 This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit https://creativecommons.org/licenses/by/3.0/ This article is available from https://egqsj.copernicus.org/articles/15/40/1964/egqsj-15-40-1964.html The full text article is available as a PDF file from https://egqsj.copernicus.org/articles/15/40/1964/egqsj-15-40-1964.pdf

In the lower Blies valley the author discovered a periglacial mudflow consisting of white marl and fragments of limestone, surmounted by 25-30 cm river-sand belonging to a Riß-terrace. The surface of these deposits was covered by fossil ice-wedges. The changes in the phyto-sociological structure of the vegetation cover permitted to fix the exact extension of the periglacial mudflow.