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17-09-2008
Glacial ice often appears blue when it has become very dense. Years of compression
gradually make the ice denser over time, forcing out the tiny air pockets between
crystals. When glacier ice becomes extremely dense, the ice absorbs all other colours
in the spectrum and reflects primarily blue, which is what we see. When glacier ice is
white, that usually means that there are many tiny air bubbles still in the ice.
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