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granular snow formed by alternate thawing and freezing
Snow condition usually occurring in spring and consisting of small, rounded "kernels" or balls.
unconsolidated granular snow that has gone through a short freeze-and-thaw process. This type of snow is prevalent throughout the High Sierra in April and May.
Snow consisting of large ice particles formed by continued freeze-thaw-refreeze cycles
more info Large-grained, rounded crystals formed from repeated melting and freezing of the snow.
snow that has partly melted and refrozen and acts like ball-bearings
Thawed snow which has refrozen.
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