We report here on a laboratory-scale experiment which reproduces a rich
variety of natural patterns with few control parameters. In particular, we
focus on intriguing rhomboid structures often found on sandy shores and flats.
We show that the standard views based on water surface waves come short to
explain the phenomenon and we evidence a new mechanism based on a mud avalanche
instability.Comment: 4 pages, 4 figures, to appear as Phys. Rev. E rapid com