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The influence of floodplain morphology and river works on spatial patterns of overbank deposition \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Thonon, I. \ Middelkoop, H. \ Perk, M. van der \ 2007
Floodplain topography and related patterns of overbank flow constitute a major control on the amounts and patterns of sediment deposition on floodplains. We studied the differences in sediment deposition at two scales along two river branches of the ...
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Towards a process-based model to predict dune erosion along the Dutch Wadden coast \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Ruessink, B.G. \ Boers, M. \ Geer, P.F.C. van \ 2012
An equilibrium dune-erosion model is used every six years to assess the capability of the most seaward dune row on the Dutch Wadden islands to withstand a storm with a 1 in 10,000 probability for a given year. The present-day model is the culmination ...
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The Roman Limes in the Netherlands: how a delta landscape determined the location of the military structures \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Dinter, M. van \ 2013
From the 40s A.D. onwards a dense military system was established in the Lower Rhine delta in the Netherlands. Long since, it is questioned why this system was established in a wetland area and even turned into the northwest frontier of the Roman Emp ...
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Opposite hysteresis of sand and gravel transport upstream and downstream of a bifurcation during a flood in the River Rhine, the Netherlands \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Kleinhans, M.G. \ Wilbers, A.W.E. \ Brinke, W.B.M. ten \ 2007
Prediction of the sediment transport rate and division thereof at bifurcations is of utmost importance for understanding the evolution of the bifurcates for short-term management purposes and for long-term fluvial plain development. However, measured ...
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New groundwater-level rise data from the Rhine-Meuse delta – implications for the reconstruction of Holocene relative mean sea-level rise and differential land-level movements \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Berendsen, H.J.A. \ Makaske, A. \ Plassche, O. van de \ 2007
We present new local groundwater-level rise data from two Late Glacial aeolian dunes, located near Barendrecht and Oud-Alblas in the western Rhine-Meuse delta. These data are based on AMS radiocarbon dating of terrestrial macrofossils, collected from ...
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Holocene water level development in The Netherlands' river area : implications for sea-level reconstruction \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Dijk, G.J. van \ Berendsen, H.J.A. \ Roeleveld, W. \ 1991
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Heavy-metal pollution of the river Rhine and Meuse floodplains in the Netherlands \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Middelkoop, H. \ 2000
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From river valley to estuary: the evolution of the Rhine mouth in the early to middle Holocene (western Netherlands, Rhine-Meuse delta) \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Hijma, M.P. \ Cohen, K.M. \ Hoffmann, G. \ Spek, A.J.F. van der \ Stouthamer, E. \ 2009
The aim of this paper is to reconstruct the evolution of the early to middle Holocene Rhine-Meuse river mouths in the western Netherlands and to understand the observed spatial and temporal changes in facies. This is achieved by constructing three de ...
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Drift sands, lakes, and soils : the multiphase Holocene history of the Laarder Wasmeren area near Hilversum, the Netherlands \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Sevink, J. \ Koster, E.A. \ Geel, B. van \ Wallinga, J. \ 2013
Around 3,000 BC groundwater in the area reached a maximum altitude of about 230 cm +NAP, resulting in local open water in the area. This rise is probably linked to the development of the Dutch coastal area, where at that time peat accumulated and dra ...
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Climate-proofing the flood protection of the Netherlands \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Vellinga, P. \ Marinova, N. \ Loon-Steensma, J.M. van \ 2009
Global sea level is rising at an increased rate since the late 19th century as a result of rising global mean temperatures. This rise is geographically non-uniform, with substantial spatial differences, and in the latest decade faster than expected. ...
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Climate-driven fluvial development and valley abandonment at the last glacial-intergalcial transition (Oude IJssel-Rhine, Germany) \ Geologie en mijnbouw : orgaan voor officieele mededelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien [Artikel]
Janssens, M.M. \ Kasse, C. \ Bohne, S.J.P. \ 2012
This study aims to reconstruct the fluvial development and forcings that culminated at the time of the Lateglacial to Holocene transition. The final abandonment of the Oude IJssel-Rhine and Niers-Rhine courses can be attributed to deep incision of th ...
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