W. E. Lawrence Minter; Origin of mud polygons that are concave downward. Journal of Sedimentary Research ; 40 (2): 755–756. doi: https://doi.org/10.1306/74D7203B-2B21-11D7-8648000102C1865D
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Deposition during stream bank flooding, drainage more rapid than evaporation causing downward curling
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