Articles | Volume 15, issue 1
https://doi.org/10.3285/eg.15.1.02
© Author(s) 1964. This work is distributed under the Creative Commons Attribution 3.0 License.
01 Nov 1964
Eine begrabene Solifluktionsdecke und ihr Einfluß auf die heutige Vegetation: Beobachtungen auf einer Bliesterterrasse (Saarland)
Abstract. 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.
