Antidunes are observed in a small-scale beach gorge that is made by a creek flow debouched from the sea bluff, the Sanriku Coast, northeast Japan. The occurrence of such bedforms may not be unusual but have probably been overlooked to date. Antidunes reported here are three-dimensional (3-D) bedforms and show rather different hydraulic conditions from those produced as two-dimensional (2-D) antidunes that commonly occur in laboratory flume experiments. Geometries of antidunes in ancient rocks may give us some clues to deduce paleohydraulic conditions, such as the paleo-flow velocity. However, we have to be cautious and need to know what type of antidunes is predominant in individual outcrops.
Despite a little volume of the creek discharge, homogeneous, well-sorted and medium- to fine-grained beach sands on the Sanriku Coast together with the rapid flow of the creek provide the best opportunity to produce the bedforms of upper-flow-regime.
View full abstract