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- The glacial ice starts flowing downwards, slowly abrading and plucking the bedrock. The accumulation of snow that is compacting and recrystallizing is called firn. The flow then accelerates across the steep rock where the deep crevasses or gaping fractures mark the icefall. The lower part of the glacier denotes ablation.eartheclipse.com/science/geography/alpine-glaciers.html
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Alpine Glaciers: Formation, Types, Location and Facts
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