Fig. 5From: Reconstruction of sediment-transport pathways on a modern microtidal coast by a new grain-size trend analysis methoda A photograph of a braided channel formed by the fluvial flooding event in July 2011. The braided channel cuts the spit and flows into the tidal sand flat. b Dunes in the braided channel. The left side of the photo is seaward. c The appearance of the active layer observed at point 3 soon after the fluvial flooding (August 1, 2011)Back to article page