Abstract
We use the Rhine-Meuse fluvial deposits to evaluate our findings from the
modelling study. Using paleogeographic maps representing the delta evolution over
the Holocene, we calculated time series of bifurcation frequency, avulsion frequency,
and the number of co-existing active channel belts on the floodplain (Stouthamer and
Berendsen, 2001; Stouthamer and Berendsen, 2007). These time
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