The relation between climate and river processes, landforms and deposits during the Quaternary

Author:

Vandenberghe J.

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference52 articles.

1. Le système des terrasses du Bassin de la Somme;Antoine;Quaternaire,1993

2. Numerical modelling of the response of alluvial rivers to Quaternary climate change;Bogaart;Global and Planetary Change,2000

3. Bogaart, P.W., Tucker, G.E., de Vries, J.J., Channel network morphology and sediment dynamics under alternating periglacial and temperate regimes: a numerical simulation study, submitted for publication.

4. Vegetation and climate during the Weichselian Early Glacial and Pleniglacial in the Niederlausitz, Eastern Germany—macrofossil and pollen evidence from Nochten;Bos;Journal of Quaternary Science,2001

5. Brown, A.G., 1995. Lateglacial-Holocene sedimentation in lowland temperate environments: floodplain metamorphosis and multiple channel systems. In: Frenzel, B., Vandenberghe, J., Kasse, C., Bohncke, S., Gläser, B. (Eds.), European river activity and climate change during the Lateglacial and early Holocene, ‘European Palaeoclimate and Man ‘9, Paläoklimaforschung 14, Gustar Fischer Verlag, Stuttgart, pp. 21–35.

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