Figure 1 - uploaded by Robert Groenewege
Content may be subject to copyright.
1. Drainage basin of the river Rhine, and topographic setting of the Lower Rhine (from Erkens, 2009).

1. Drainage basin of the river Rhine, and topographic setting of the Lower Rhine (from Erkens, 2009).

Source publication
Thesis
Full-text available
When rivers keep meandering long enough, their channel belts widen to a certain width due to lateral channel migration processes. A meandering river tends to shift and sharpen its bends as the outcome of channel migration, and at some point cut them off. This leaves a cutoff meander element (usually a point bar complex with an oxbow lake) with a ce...

Contexts in source publication

Context 1
... this study has shown how the Sadler effect is predominantly responsible for meander-belt scale preservation ( §6.2.1; Fig. 6.5; Fig. 6.6; Fig. 6.11). As a result, more young deposits and fewer old deposits will be visible at the end of meander simulations (and in geological-geomorphological maps of a meandering system in autogenic equilibrium). This is true both in the vertical sense and in its horizontal, planform expression. This study further implies that stratigraphic hiatuses ...
Context 2
... end %% Time series (Fig. 5.1 scat=scatplot (varX,varY,'circles',[], [],[],4,6); smoothed = smooth(varX,varY,0.1,'rloess'); [varX_sort,sortind]=sort(varX); hold on; plot(varX_sort,smoothed(sortind),'-k','LineWidth',2); ylabel({'reworking frequency','(nr of timesteps)'}); xlabel('lateral position in meander belt'); xticks(linspace (-1,1,11)); legend('off'); box on; set(gca,'YAxisLocation','right'); text(0.005,0.95,'(d)',' Color','k','Units','normalized','FontSize',14,'FontWeight', 'bold'); cb = colorbar(" FontSize",14); cb.Layout.Tile = 'west'; cb.Label.String = 'data density'; cb.TickLabels = {'Low','High'}; cb.Ticks = [0. ...