"Unlike a pond, the depth of the Great Lakes prevent it from being a completely frozen sheet of ice, but instead the ice atop the lakes can actually move with the wind, according to Austin. Due to the ability of the ice to move around, the thickness of the ice across the lakes vary and therefore researchers do not know how thick the ice is in all portions of the lake."
A positive aspect of this ice coverage is that it will replenish the lake levels come spring and summer.
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