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

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Book 2018or the first time a wealth of information currently scattered among many national and regional journals. It will benefit earth scientists, environmental scientists, tourism geographers and conservationists alike..

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Morphogenic Setting and Diversity of Processes and Landforms: The Geomorphological Regions of Belgitries are presented. The dominant controls exerted on morphogenic processes by lithology and elevation (i.e., tectonic background) lead to distinguish northern Belgium, corresponding to the low-elevation Cenozoic Belgian basin where sedimentation generally prevails over erosion, and the Ardennian Pa

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The Climate of Belgium and Luxembourg,Mean annual air temperatures are around 10 ℃ and vary spatially mainly as a function of elevation. Annual temperature amplitudes are in the 13–17 °C range. Annual rainfall depths vary from ~700 mm in western Belgium to 1300–1400 mm in the wettest areas of NE and SW Ardenne. Belgium and Luxembourg ar

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Landscapes and Landforms of the Luxembourg Sandstone, Grand-Duchy of Luxembourg,up to 100-metres-thick unit in which rivers of all sizes have incised steep cliffs separating extended plateaus. The Luxembourg Sandstone landscapes display typical geomorphological features at various scales, mainly shaped by gravitational and fluvial processes that varied in intensity with climati

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,Erosion Surfaces in the Ardenne–Oesling and Their Associated Kaolinic Weathering Mantle,ery long persistence and high resistance to erosion of landscape elements created as far back in time as the Lower Cretaceous in a region of predominantly continental regime and constant low to moderate elevation since the Permian. We first present recent results regarding the antiquity of kaolinic

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,A Unique Boulder-Bed Reach of the Amblève River, Ardenne, at Fonds de Quarreux: Modes of Boulder Trian quartzites and surrounded by steep wooded hillslopes, a 3-km-long gorge is cluttered with hundreds of huge quartzite boulders up to several metres in size. These boulders originate from the locally outcropping Cambrian Venne Formation and reached the riverbed through periglacial slope processes.

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The Periglacial Ramparted Depressions of the Hautes Fagnes Plateau: Traces of Late Weichselian Lithnes area, NE Ardenne, have been recognized since the 1950s to represent relics of periglacial mounds. We examine first the regional distribution of these periglacial ramparted depressions (PRDs), whose location seems controlled mainly by elevation and lithologic factors. Geomorphological characteris

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The Karstic System of Han-sur-Lesse,orthern margin of the Lower Devonian Ardenne, it comprises all caves and underground flow paths related to the epigenetic Lesse River across the Givetian limestone anticline of Boine. The Han-sur-Lesse caves result from a two-stage karstogenesis. First, ghost-rock karstification, the residual alteri