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
✦ LIBER ✦
Morphological and sedimentological changes in the Senegal River estuary after the constuction of the Diama dam
✍ Scribed by J. Paul Barusseau; Mariline Bǎ; Cyr Descamps; E. Salif Diop; Bachir Diouf; Alioune Kane; Jean Luc Saos; A. Soumaré
- Book ID
- 108460251
- Publisher
- Elsevier Science
- Year
- 1998
- Tongue
- English
- Weight
- 951 KB
- Volume
- 26
- Category
- Article
- ISSN
- 1464-343X
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