Abstract
The reconstruction of the tectonic behaviour of a Central European upland region seems to be fairly easy, provided there are valleys traversing the area concerned. The development of these valleys in Central Europe was determined to a great extent by the Pleistocene periglacial climate. The variable morphological intensity of this climate led to the alternation of periods with prevailing erosion, and of periods with prevailing accumulation. The terraced valley slopes, which document the course of former valley floors, are the result of these alternations. By the correlation of terrace remnants, which belong to the same age, a longitudinal profile of a former valley floor can be constructed, which then allows statements on subsequent tectonic movements.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Bibus, E., 1983. Distribution and dimension of young tectonics in the Neuwied Basin and the Ldtoer Middle Rhine. This vol.
Brunnacker, K. and Boenigk, W., 1983. The Rhine valley between the Neuwied Basin and the Lower Rhenish Embayment. This vol.
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1983 Springer-Verlag Berlin Heidelberg
About this paper
Cite this paper
Semmel, A. (1983). Plateau Uplift During Pleistocene Time - Preface. In: Fuchs, K., von Gehlen, K., Mälzer, H., Murawski, H., Semmel, A. (eds) Plateau Uplift. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-69219-2_4
Download citation
DOI: https://doi.org/10.1007/978-3-642-69219-2_4
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-69221-5
Online ISBN: 978-3-642-69219-2
eBook Packages: Springer Book Archive