Hillslopes in Arctic regions with frozen soils can host a suite of geometric patterns, from circles and stripes to polygonal patterned ground. They can also have solifluction patterns, or markings left behind when partially thawed permafrost slips and flows down a slope. Solifluction patterns look like pairings of flat, terraced soil—like a big staircase—and rounded lobes of soil at the terrace’s base.
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