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Sedimentary structures formed in sand by surface tension on melting hailstones.

January 1, 1984

When a hailstone melts, wet but unsaturated sand within the crater is attracted to the hailstone surface by surface tension. Shrinkage of the melting hailstone then produces one or more rings of sand within the impact crater.-from Authors

Publication Year 1984
Title Sedimentary structures formed in sand by surface tension on melting hailstones.
Authors D. M. Rubin, R. E. Hunter
Publication Type Article
Publication Subtype Journal Article
Series Title Journal of Sedimentary Petrology
Index ID 70013502
Record Source USGS Publications Warehouse