A seasonal spring that flows during the winter, maintains a pocket of warm water that never ices over. This provides an area of open water that is available through the coldest of winters.
When all other water sources are covered by ice, birds swarm here to drink and bath.
The pond doesn’t stay at the full level for very long. As the water exits through the pond bottom, ice is left on the bank behind the receding pool.
The thin layer of ice is marked by bands created by the departing water. Adhesion holds the water against the lower side of the ice. A thin line of ice forms along the water margin, increasing the effectiveness of the bond between water and ice. Eventually, the water drops to a point where gravity defeats adhesion and the process begins again at a slightly lower level. Each time this occurs, another band is added to the ice.
The falling water level leaves ice collars on the willows and dogwoods. When the water falls low enough, rabbits often seek shelter beneath the ice roofs.
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