5.9A) and width/thickness ratio is low (Gouw and Berendsen, 2007), which explains the low CDP for the pre-3000 cal yr BP succession. ... These channels were able to migrate laterally at a higher rate, because of the larger discharge and higher stream power. ... In conclusion, the geometry of the channel belts in the downstream part of the Rhine-Meuse delta varied over time parallel to changing channelanbsp;...
|Title||:||Alluvial architecture of the Holocene Rhine-Meuse delta (the Netherlands) and the Lower Mississippi Valley (U.S.A.)|