Wave climate exerts a significant influence on the development of Holocene sedimentary prograding wedges. This is demonstrated by
the fact that near-bed orbital velocities between 0.10 and 0.14 m/s (threshold for resuspension) occur in the vicinity of the infralittoral
prograding wedges (IPW) offlap-breaks during storm-weather conditions, but during medium wave energy conditions in the case of
prodeltaic wedges
