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The Rhine - a major fluvial record

Published online by Cambridge University Press:  01 April 2016

W.E. Westerhoff
W.E. Westerhoff*
Affiliation:
TNO Geological Survey of the Netherlands. PO Box 80.015, 3508 TA Utrecht, the Netherlands. Email: [email protected]
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Abstract

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This special issue contains the papers presented during the 2004 DEUQUA meeting. The papers provide an overview of recently carried out Quaternary geological studies on different aspects of the river Rhine system. The introductory paper follows the pathway of the Rhine downstream from its source in the Swiss Alps to the delta in the Netherlands. Along this route geological and geographical factors determine the regional subdivisions of the river: the Alps, the Upper Rhine Graben, the Rhenish Massif, and the Lower Rhine Embayment as part of the southern North Sea Basin. Each of these regions can be typified by a characteristic geological evolution.

New evidence from heavy-mineral analyses provides an improved lithostratigraphy and insight in the Quaternary evolution of the Rhine in the Upper Rhine Graben. The Plio-Pleistocene transition is determined by a palaeomagnetic study. The same paper emphasis on the impact of climate change on the composition of the magneto-mineralogy. Pollen analytical results show a complex interrelationship of a number of Middle Pleistocene interglacial periods in the northern part the Upper Rhine Graben. In the same area geomorphological analysis demonstrates a clear influence of tectonics on the preservation of fluvial terrace accumulations. A detailed pollen analytical study on the Late Glacial and Holocene development of the Rhine in the northern Upper Rhine Graben discusses the relation between vegetation cover and river behaviour. Finally, two papers from the Lower Rhine Embayment discuss a revised provenance based lithostratigraphy and its implications for understanding the fluvial history.

Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 87 , Issue 1 , March 2008 , pp. 3 - 5
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2008

References

Bos, J.A.A., Dambeck, R., Kalis, A.J., Schweizer, A., & Thiemeyer, H., 2008. alaeoenvironmenttal changes and vegetation history of the northern Upper Rhine Graben (southwestern Germany) since the Lateglacial. Netherlands Journal of Geosciences 87/1: 67–90.Google Scholar
Busschers, F.S., Weerts, H.J.T., Wallinga, J., Cleveringa, P., , Kasse, C, De Wolf, H. & Cohen, K.M., 2005. Sedimentary architecture and optical dating of Middle and late Pleistocene Rhine-Meuse deposits fluvial response to climate change, sea-level fluctuation and glaciation. Netherlands Journal of Geosciences 84/1: 25–41.Google Scholar
Gibbard, P.L. & Lautridou, J.P., 2003. The Quaternary history of the English Channel: an introduction. Journal of Quaternary Science 18: 195–199.Google Scholar
Gouw, M.J.P. & Erkens, G., 2007. Architecture of the Holocene Rhine-Meuse delta (the Netherlands) - A result of changing external controls. Netherlands Journal of Geosciences 86/1: 23–54.Google Scholar
Hagedom, E.M. & Boenigk, W., 2008. New evidences of the Pliocene and Quaternary sedimentary and fluvial history in the Upper Rhine Graben on basis of heavy mineral analyses. Netherlands Journal of Geosciences 87/1:21–32.Google Scholar
Hoek, W.Z. & Bohncke, S.J.P., 2002. Climatic and environmental events over the Last Termination, as recorded in the Netherlands: a review. Netherlands Journal of Geosciences 81: 123–137. Google Scholar
Kasse, C, Hoek, W.Z., Bohncke, S.J.P., Konert, M., Weijers, J.W.H., Van der Zee, R.M. & Cassee, M., 2005. Late Glacial fluvial response of the Niers- Rhine (western Germany) to climate and vegetation change. Journal of Quaternary Science 20(4): 377–394.Google Scholar
Kemna, H.A., 2008. A Revised Stratigraphy for the Pliocene and Lower Pleistocene Deposits of the Lower Rhine Embayment. Netherlands Journal of Geosciences 87/1: 91–105.Google Scholar
Knipping, M., 2008. Pollenanalytical investigations on deep borings in the northern Upper Rhine Graben. Netherlands Journal of Geosciences 87/1: 51–65.Google Scholar
Michon, I., Van Balen, R.T., Merle, O. & Pagnier, H., 2003. The Cenozoic evolution of the Roer Valley Rift System integrated at a European scale. Tectonophysics. 367: 101–126.Google Scholar
Preusser, F., 2008. Characterisation and evolution of the River Rhine system. Netherlands Journal of Geosciences 87/1: 7–19.CrossRefGoogle Scholar
Rolf, C, Hambach, U. & Weidenfeller, M., 2008. Rock and palaeomagnetic evidence for the Plio-Pleistocene palaeoclimatic change recorded in Upper Rhine Graben sediments (Bohrung Ludwigshafen-Parkinsel). Netherlands Journal of Geosciences 87/1: 41–50.CrossRefGoogle Scholar
Sissingh, W., 2006. Syn-kenematic palaeogeographic evolution of the West European Platform: correlation with Alpine plate collsion and foreland deformation. Netherlands Journal of Geosciences 85/2, 131–180.Google Scholar
Weidenfeller, M. & Kärcher, T., 2008. Tectonic influence on fluvial preservation: Aspects of the architecture of Middle and Late Pleistocene sediments in the northern Upper Rhine Graben, Germany. Netherlands Journal of Geosciences 87/1: 33–40.Google Scholar
Westerhoff, W.E., Kemna, H.A. & Boenigk, W., 2008. The confluence area of Rhine, Meuse, and Belgian rivers: Late Pliocene and Early Pleistocene fluvial history of the northern Lower Rhine Embayment. Netherlands Journal of Geosciences 87/1: 107–125.Google Scholar