Since the water have an unusual salty consistency, its have a lower freezing point, thus, made its not to freeze as it passes across the glacier.
These are water from the subglacial lake seeps that goes through some fissure in the glacier.
The salty water also moved down the Taylor Glacier into Lake Bonney
However, as the water have an unusual salty consistency, its have a lower freezing point that made its not to freeze as it passes across the glacier.
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