Stone polygons commonly form in silty alluvium associated with river floodplains and delta plain in periglacial regions.

Name: Stone polygons commonly form in silty alluvium associated with river floodplains and delta plain in periglacial regions.
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Stone polygons typically form in periglacial regions with frost action, often in fine-grained soils like silts and clays, but they are not commonly associated with river floodplains and delta plains.

Stone Polygons Commonly Form in Silty Alluvium Associated with River