Late-glacial sedimentological and morpho
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Margriet Huisink
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Article
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1997
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John Wiley and Sons
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English
⚖ 602 KB
The late Pleniglacial and Late-glacial Maas valley, south of Nijmegen, contains four terraces. Three river systems are described based on the morphology of channel scars on these terrace surfaces and by sediment characteristics. The River Maas reacted to climatic warming at the start of the Weichsel