
The most striking feature of the lake is the intricate ice block pattern the develop on the lake surface during winter. The ice pattern is caused by repeated cycles of freezing, fracturing, and refreezing of the ice due to variations in temperature and wind-induced ice motion. Usually, when lakes freeze over, they tend to develop a thick crust of uniform ice, which only breaks apart when the warmer season comes. But, in order for that to happen, environmental conditions must remain steady for at least a short while, allowing the ice to establish itself. When this does not happen, only superficial layers of water freeze over, while the others do not. Slight variations in ambient temperatures can then break some of the ice apart, rearranging it into new patterns. When temperatures drop by a few degrees, the ice solidifies again.



Source: Amusing Planet
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