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Ice-Wedge Polygons of Northern Alaska
1982Ice-wedge polygons, commonly 5–30 m in diameter, are strikingly developed over the Arctic Coastal Plain of northern Alaska. Troughs over ice wedges that outline the polygons are a few centimeters to several meters wide. Centers of polygons are flat, high centered, or low centered in a continuum in which relief generally is several decimeters to a meter.
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Ice-Wedge Cracks, Garry Island, Northwest Territories
Canadian Journal of Earth Sciences, 1974Observations made on winter ice-wedge cracks at Garry Island, N.W.T., for the 1967–73 period show that cracking tends to occur between mid-January and mid-March. On the average, nearly 40% of the ice wedges crack in any given year. The crack frequency varies inversely with snow depth.
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A fossil ice wedge at Perstorp, Skåne
Geologiska Föreningen i Stockholm Förhandlingar, 1977Abstract A fossil ice wedge is described. The wedge was about 0.5 m deep and almost as wide, even at the lower end. It cut through a bed of fine sand and coarse silt, which was overlain by sand and sandy gravel and underlain by sand and a sandy till.
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Ice wedge dynamics and local crushing
199312th International Conference on Port and Ocean Engineering Under Arctic Conditions, 17-20 August 1993, Hamburg ...
McKenna, R. F., Spencer, D.
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Antarctic Landfast Sea Ice: A Review of Its Physics, Biogeochemistry and Ecology
Reviews of Geophysics, 2023Alexander D Fraser +2 more
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Ice‐Nucleating Particles That Impact Clouds and Climate: Observational and Modeling Research Needs
Reviews of Geophysics, 2022Susannah Burrows +2 more
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