Solefluxion stripes on the summit of Mount Svorikhti, produced by the alternate freezing and thawing of stony mud. At this altitude (2320 m) periglacial activity still goes on. Trowel is parallel to the stripes. July 1989.
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posted on 2024-01-04, 15:39 authored by Sphakia SurveySolefluxion stripes on the summit of Mount Svorikhti, produced by the alternate freezing and thawing of stony mud. At this altitude (2320 m) periglacial activity still goes on. Trowel is parallel to the stripes. July 1989.
