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Titlebook: Landscapes and Landforms of Belgium and Luxembourg; Alain Demoulin Book 2018 Springer International Publishing AG 2018 Coastal Geomorpholo

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The Campine Plateau,epositing debris from southern origin, the Campine Plateau became a positive relief as the combined result of uplift, the protective role of the sedimentary cover, and presumably also base level fluctuations. The escarpments bordering the Campine Plateau are tectonic or erosional in origin, showi
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Morphotectonics and Past Large Earthquakes in Eastern Belgium,tigations identified such landforms in Belgium, which is located in the most seismically active region of stable Europe northwest of the Alps. Here, we present two active fault zones among the best documented in continental Europe, and whose geomorphology is related to earthquake activity in eastern
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,Gullies and Closed Depressions in the Loess Belt: Scars of Human–Environment Interactions,sts may help unraveling human–environment interactions in (pre)historical times. The Meerdaal Forest in central Belgium, being continuously a forest for at least eight centuries and most probably already from the fifth century AD onwards, offers a unique opportunity to study such geomorphic features
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The Flemish Valley: Response of the Scheldt Drainage System to Climatic and Glacio-Eustatic Oscilla of the Belgian part of the Scheldt basin, in which the Flemish Valley is essentially a buried incised-valley system that once drained the Scheldt area. The Scheldt is typically a lowland river flowing across a subdued hilly topography in its middle course and on the flat plain chiefly made of its o
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