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The confluence area of Rhine, Meuse, and Belgian rivers: Late Pliocene and Early Pleistocene fluvial history of the northern Lower Rhine Embayment

Part of: Fluvial sedimentary record of the Rhine/Meuse system

Published online by Cambridge University Press:  01 April 2016

W.E. Westerhoff ,
H.A. Kemna  and
W. Boenigk
W.E. Westerhoff*
Affiliation:
TNO Geological Survey of the Netherlands, PO Box 80015, 3508 TA Utrecht, the Netherlands
H.A. Kemna
Affiliation:
Geologisches Institut, Universitat zu Koln, Zülpicherstrasse 49a, Germany
W. Boenigk
Affiliation:
Geologisches Institut, Universitat zu Koln, Zülpicherstrasse 49a, Germany
*
*Corresponding author. Email:[email protected]

Abstract

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The fluvial history of the northern Lower Rhine Embayment shows interplay of three main river systems: Rhine, Meuse and smaller rivers draining the central and northern part of Belgium.

The Pliocene and Early Pleistocene (pre-)Rhine and Meuse river systems had their conjunction in the southern part of the Roer Valley Graben between Aachen and Jülich. Despite slight differences in the heavy-mineral assemblages the lithological composition of the Pliocene deposits of the three river systems shows close resemblance and therefore they cannot be mapped separately. However, due to a marked change of the petrographical composition the Upper Pliocene and Lower Pleistocene deposits of the Rhine are easily recognised and as a result Rhine and Meuse deposits can be mapped separately upstream of their confluence.

The Lower Pleistocene deposits of Rhine, Meuse and the Belgian rivers show a clear interrelationship. They are bounded by two regional well-mapable unconformities and are preserved in from west to east changing lithostratigraphical sequences. Revision of the lithostratigraphical schemes in Germany and the Netherlands and the better defined lithostratigraphical position of Meuse deposits in Germany now strongly constrain the correlation of the various fluvial deposits. As a result existing reconstructions of the fluvial deposition and tectonic history of the southern Roer Valley Graben can be evaluated and re-adjusted.

It is concluded that the main course of the Meuse was aligned through the so-called East Meuse valley during the larger part of the Early Pleistocene. Available pollen data do not conflict with this conclusion. At the same time the Rhine ceased to enter the southern part of the Roer Valley Graben. Instead, the Meuse accumulated here a series of deposits derived from the East-Meuse valley. Simultaneously, the Belgian rivers filled available accommodation space in the Roer Valley Graben of the southern Netherlands. The conclusions are based primarily on the revised lithostratigraphical framework. In general they simplify the picture of fluvial and tectonic behaviour of the area.

Keywords

Lower Rhine EmbaymentRhineMeusepalaeogeographylithostratigraphyheavy mineralssubsidence
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 87 , Issue 1 , March 2008 , pp. 107 - 125
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2008

References

Berendsen, H.J.A. & Stouthamer, E., 2002. Palaeogeographic evolution and avulsion history of the Holocene Rhine-Meuse delta, the Netherlands. Netherlands Journal of Geosciences 81: 97–112.CrossRefGoogle Scholar
Boenigk, W., 1970. Zur Kenntnis des Altquartärs bei Brüggen. Sonderveröffent- Uchungen Geologisches Institut Universität Köln 17: 1-141.Google Scholar
Boenigk, W., 1978a. Gliderung der altquartären Ablagerungen in der Nieder- rheinischen Bucht. Fortschritte Geologie Rheinland und Westfalen 28: 135–212.Google Scholar
Boenigk, W., 1978b. Die fluβgeschichtliche Entwicklung der Niederrheinischen Bucht im Jungtertiär and Altquartär. Eiszeitalter und Gegenwart 28: 1–9.Google Scholar
Boenigk, W., 2002. The Pleistocene drainage pattern in the Lower Rhine Basin. Netherlands Journal of Geosciences 81: 201–209.Google Scholar
Boenigk, W., Koãi, A. & Brunnacker, K., 1979. Magnetostratigraphie im Pliozän der Niederrheinischen Bucht. Neues Jahrbuch Geologie Paläontologie Monatshefte 1979(9): 513–528.Google Scholar
Boenigk, W. & Frechen, M., 2006. The Pliocene and Quaternary Fluvial Archives of the Rhine System. Quaternary Science Reviews 25: 550–574.Google Scholar
Breddin, H., 1955. Die Gliederung der altdiluvialen Hauptterrasse von Rhein und Maas in der Niederrheinische Bucht. Der Niederihein 3-4: 76–79. Google Scholar
Bridge, J.S., 2003. Rivers and Floodplains: forms, processes, and sedimentary record. Blackwell Science Ltd.: 491 pp.Google Scholar
Brueren, J.W.R., 1945. Het terrassenlandschap van Zuid-Limburg. Mededelingen Geologische Stichting, C-VI-1: 1–93.Google Scholar
Bruins, H.J., 1981. Paleomagnetische datering van de Maasterrassen en Vroeg- Pleistocene Lössafzettingen in Zuid-Limburg. Internal report Wageningen University Researchcentre (WUR).Google Scholar
Busschers, F.S., 2007. Unravelling the Rhine; Response of a fluvial system to climate change, sea-level oscillation and glaciation. PhD. dissertation Vrije Universiteit Amsterdam. TNO-Geological Survey of the Netherlands, Utrecht. Geology of the Netherlands 1: 1–183 Google Scholar
De Ploey, J., 1961. Morfologie en Kwartair-stratigrafie van de Antwerpse Noorderkempen. Acta geographica Lovaniensi, 1: 130 pp.Google Scholar
Doppert, J.W.C., Ruegg, G.H.J., van Staalduinen, C.J., Zagwijn, W.H. & Zandstra, J.G., 1975. Formaties van het Kwartair en Boven Tertiair in Nederland. In: Zagwijn, W.H., Van Staalduinen, C.J. (eds): Toelichtingen bij de geologische overzichtskaarten van Nederland, Rijks Geologische Dienst Haarlem: 11–56.Google Scholar
Felder, W.M. & Bosch, P.B., 1989. Geologisch kaart van Zuid-Limburg en omgeving, 1 : 50 000. Afzettingen van de Maas. Rijks Geologische Dienst, Haarlem. Google Scholar
Fliegel, G., & Stoller, J., , 1910. Jungtertiäre und altdiluviale pflanzenfiihrende Ablagerungen im Niederrheingebiet. Jahrbuch PreufSische Geologische Landes-Anstalt 31(1): 227–257.Google Scholar
Geluk, M.C., Duin, E.J.T., Dusar, M., Rijkers, R.H.B., Van den Berg, M.W., Van Rooijen, P., 1994. Stratigraphy and tectonics of the Roer Valley Graben. Geologie en Mijnbouw 73: 129–141.Google Scholar
Gliese, J. & Hager, H., 1978. On browncoal resources in the Lower Rhine Embayment (West Germany). Geologie en Mijnbouw 57: 517–525.Google Scholar
Hagedorn, E.-M., 2004. Sedimentpetrographie und Lithofazies der jungtertiären und quartären Sedimente im Oberrheingebiet. Inaugural-Dissertation, Geologisches Institut der Universität zu Köln: 248 pp. http://kups.ub.uni-koeln.de/volltexte/2004/1253/ Google Scholar
Hagedorn, E-M. & Boenigk, W., 2008. The Pliocene and Quaternary sedimentary and fluvial history in the Upper Rhine Graben based on heavy mineral analyses. Netherlands Journal of Geosciences 87/1: 21–32.CrossRefGoogle Scholar
Houtgast, R.F. & Van Balen, R.T., 2000. Neotectonics of the Roer Valley Rift System, the Netherlands. Global and Planetary Change 27: 131–146.CrossRefGoogle Scholar
Juvigné, E. & Renard, F., 1992. Les terrasses de la Meuse de Liége a Maastricht. Annales de la Société Géologique de Belgique T. 115 (fasicicule 1): 167–186.Google Scholar
Kasse, C, 1988. Early Pleistocene tidal and fluvial environments in the southern Netherlands and northern Belgium, Dissertatie Vrije Universiteit Amsterdam: 190 pp.Google Scholar
Kasse, C, 1990. Lithostratigraphy and provenance of the Early-Pleistocene deposits in the southern Netherlands and northern Belgium. Geologie en Mijnbouw, 69-4: 327–340.Google Scholar
Kasse, C. & Bohncke, S., 2001. Early Pleistocene fluvial and estuarine records of climate change in the southern Netherlands and northern Belgium. In: Maddy, D., Macklin, M.G. & Woodward, J.C. (eds): River basin sediment systems. Archives of environmental change. Balkema (Rotterdam): 171–193.Google Scholar
Kemna, H.A., 2005. Pliocene and Lower Pleistocene stratigraphy in the Lower Rhine Embayment, Germany. Kolner Forum 14: 1–121.Google Scholar
Kemna, H., 2007. Pliocene and Lower Pleistocene fluvial history of the Lower Rhine Embayment, Germany: Examples of the tectonic forcing of River courses. Quaternary International, doi.10.1016/j.quaint.2007.08.038.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
Kemna, H.A. & Westerhoff, W.E., 2007. Remarks on the palynology-based chronostratigraphical subdivision of Pliocene terrestrial deposits in NW- Europe. Quaternary International, 164-165 (2007): 185–196.CrossRefGoogle Scholar
Klostermann, J., 1983. Die Geologie der Venloer Scholle (Niederrhein). Geologisches Jahrbuch A 66: 3–115.Google Scholar
Kurtz, E., 1913. Die Verbreitung der diluvialen Hauptterrassenschotter von Rhein and Maas in der Niederrheinischen Bucht. Verhandlungen der Natur- historische Vereins, Jahrgang 70: 87–108.Google Scholar
Kuyl, O.S., 1980. Toelichtingen bij de geologisch kaart van Nederland, 1 : 50 000, Blad Heerlen, 62W-62O. Rijks Geologische Dienst, Haarlem. 1–206.Google Scholar
Macar, P., 1976. Les mouvements épéirogeéniques decelables en Belque. L'aide de la Géomorphologie. In: Pissart, A. (ed.): Geomorphologie de la Belgique, Université de Liége, 1976: 29–49.Google Scholar
Miall, A.D., 1996. The Geology of Fluvial Deposits. Sedimentary Facies, Basin Analysis, and Petroleum Geology. Springer (Berlin): 582 pp. 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
Michon, L. & Van Balen, R.T., 2005. Characterization and quantification of active faulting in the Roer valley rift system based on high precision digital elevation models. Quaternary Science Reviews 24: 455–472 Google Scholar
Pissart, A., 1974. la Meuse en France et Belgique. In: Macar, P. (ed): L'évolution Quaternaire des bassins fluviaux de la Mer du Nord meridionale. Soc. geol. de Belgique, Liege: 105–131.Google Scholar
Schnütgen, A., 1974. Die Hauptterrassenfolge am linken Niederrhein aufgrund der Schotterpetrographie. Forschungsberichte des Landes Nordrhein-Westfalen, Nr. 2399: 1–149.Google Scholar
Tavemier, R. & De Moor, C, 1974. L'évolution du basin de l'Escaut. In: Macar, p. (ed.): [.'evolution Quaternaire des basins fluviaux de la Mer du Nord méridionale. Soc. Géol. de Belgique (Liége): 159–231.Google Scholar
Tesch, P., 1908. Der Niederländische Boden und die Ablagerungen des Rheines und der Maas aus der jüngeren Tertiär-und der älteren Deluvialzeit. Mededelingen van de Rijksdienst der Opsporing van Delfstoffen No. 1: 1–74.Google Scholar
Tesch, P., 1941. De schiervlakte van Eifel en Ardennen voor de opheffing tot Bergland. Tijdschrift Nederlandsch Aardrijkskundig Genootschap, 2e serie, deel LVIII: 63–71.Google Scholar
Urban, B., 1978a. Vegetationsgeschichtliche Untersuchungen zur Gliedrung des Altquartärs der Niederrheinischen Bucht. Sonderveröff. Geol. Inst. Univ. Köln. 34: 1–65.Google Scholar
Urban, B., 1978b. The interglacial of Frechen I/Rheinland - a section of the Tiglian A type. Geologie en Mijnbouw 57: 401–406.Google Scholar
Van Balen, R.T., Houtgast, R.F. & Cloetingh, S.A.P.L., 2005. Neotectonics of the Netherlands: a review. Quaternary Science Reviews 24: 439–454.Google Scholar
Van den Berg, M.W., 1989. Toelichting op kaartblad 59-62, Geomorfologische kaart van Nederland, 1 : 50 000 - DL0 Staringscentrum, Wageningen/Rijks Geologische Dienst Haarlem: 1–32.Google Scholar
Van den Berg, M.W., 1994. Neotectonics of the Roer Valley rift system. Style and rate of cmstal deformation inferred from syn-tectonic sedimentation. Geologie en Mijnbouw 73: 143–156.Google Scholar
Van den Berg, M.W. & Van Hoof, T., 2001. The Maas terrace sequence at Maastricht, SE Netherlands: evidence for 200 m of late Neogene and Quaternary surface uplift. In: Maddy, D., Macklin, M.G. & Woodward, J.C. (eds): River Basin Sediment Systems: Archives of Environmental Change, Balkema (Rotterdam): 45–86,Google Scholar
Van der Vlerk, I.M. & Florschiitz, F., 1953. The palaeontological base of the subdivision of the Pleistocene in the Netherlands. Verhandelingen Koninklijke Nederlandse Akademie Wetenschappen Afdeeling Natuurkunde le Reeks 20: 1–58.Google Scholar
Van Straaten, L.M.J.U., 1956. Structural features of the ‘Papzand’ Formation at Tegelen (Netherlands). Geologie en Mijnbouw 18: 121–135 Google Scholar
Vandenberghe, J. & De Smedt, P., 1979. Palaeomorphology in the eastern Scheldt basin (Central Belgium)-The Dijle-Demer-Grote Nete confluence area. Catena 6: 73–105.Google Scholar
Vandenberghe, N., Laga, P., Louwye, S., Vanhoorne, R., Marquet, R., De Meuter, F., Wouters, K., & Hageman, H.W., 2005. Stratigraphic interpretation of the Neogene marine - continental record in the Maaseik well (49W0220) in the Roer Valley Graben, NE Belgium. Memoirs of the Geological Survey of Belgium 52: 1–39.Google Scholar
Weerts, H.J.T., 1996. Complex Confining Layers. Nederlandse Geografische Studien, 213: 1–189.Google Scholar
Weerts, H., Cleveringa, P., Ebbing, J.H.J., De Lang, F.D. & Westerhoff, W.E., 2003. De Uthostratigrafische indeling van Nederland. Formaties uit het Tertiair en Kwartair. Rapport NITG-TN0 03-051-A (Internal report TNO Geological Survey of the Netherlands).Google Scholar
Westerhoff, W.E., 2004. Upper Pliocene and Lower Pleistocene Rhine-Meuse deposits in the Tegelen-Reuver type area. With contributions by H.A. Kemna. DEUQUA meeting 2004 Nijmegen Excursion guide: 79–130.Google Scholar
Westerhoff, W.E., Wong, Th.E. & Geluk, M.C., 2003. De opbouw van de ondergrond. In: De Mulder, E.F.J., Geluk, M.C., Ritsema, I., Westerhoff, W.E. & Wong, Th.E. (eds): De ondergrond van Nederland. Nederlands Instituut voor Toegepaste Geowetenschappen TNO. Geologie van Nederland 7: 247–352.Google Scholar
Westerhoff, W.E., Menkovic, A & De Lang, F.D., in prep. A revised lithostratigraphy of Upper Pliocene and Lower Pleistocene deposits derived from the Rhine- Meuse-Schelde catchments in the Netherlands (NJG - Lithostratigraphy of the Netherlands).Google Scholar
Wunstorf, W. & Fliegel, C, 1910. Die Geologie des Niederrheinischen Tieflandes. Abhandlungen der Königlich Preuβschen Geologischen Landesanstalt. Neue Folge, Heft 67: 1–172.Google Scholar
Zagwijn, W.H., 1960. Aspects of the Pliocene and Early Pleistocene vegetation in the Netherlands. Mededelingen Geologische Stichting C-III-1(5): 1–78.Google Scholar
Zagwijn, W.H., 1963. Pollen-analytic investigations in the Tiglian of the Netherlands. Mededelingen Geologische Stichting. Nieuwe Serie 16: 49–71.Google Scholar
Zagwijn, W.H., 1974. Pollenanalytisch onderzoek van een humeuze kleilaag in de groeve bij Siisterseel en een opmerking n.a.v. rapport 369. Intern rapport Paleobotanie 719. Rijks Geologische Dienst (presently at the files of TNO).Google Scholar
Zagwijn, W.H., 1985. An outline of the Quaternary stratigraphy of the Netherlands. Geologie en Mijnbouw 64: 17–24.Google Scholar
Zagwijn, W.H., 1989. The Netherlands during the Tertiary and Quaternary: a case history of Coastal Lowlands evolution. Geologie en Mijnbouw 68: 107–121.Google Scholar
Zagwijn, W.H., 1992. The beginning of the ice age in Europe and its major subdivisions. Quaternary Science Reviews, 11: 583–591.Google Scholar
Zagwijn, W.H., 1998. Borders and boundaries: a century of stratigraphical research in the Tegelen-Reuver area of Limburg (the Netherlands). Mededelingen Nederlands Instituut Toegepaste Geowetenschappen TNO 60: 19–34.Google Scholar
Zagwijn, W.H. & De Jong, J., 1963. Pollenanalytisch materiaal uit een groeve te Platte Bosschen. Intern Rapport Paleobotanie 369. Rijks Geologische Dienst (presently at the files of TNO).Google Scholar
Zagwijn, W.H. & De Jong, J., 1984. Die Interglaziale von Bavel und Leerdam und Ihre Stratigraphische Stellung im Niederländischen Früh-Pleistozän. Mededelingen Rijks Geologische Dienst 37-3: 155–169.Google Scholar
Ziegler, P.A., 1994. Cenozoic rift system of western and central Europe: an overview. Geologie en Mijnbouw 73: 99–127.Google Scholar
Zonneveld, J.I.S., 1949. Zand-Petrologische onderzoekingen in de tenassen van Zuid-Limburg. Mededelingen Geologische Stichting, Nieuwe Serie No. 3: 103–123.Google Scholar
Zonneveld, J.I.S., 1955. De Kwartaire rivierterrassen van Zuid-Limburg. Tijdschrift Koninklijk Nederlands Aardrijkskundig Genootschap: 72.Google Scholar
Zonneveld, J.I.S., 1957. River terraces and the Quaternary chronology in the Netherlands. Geologie en Mijnbouw N.S. 19: 277–285.Google Scholar