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Don t miss the big stories. Like us on Facebook. On a clear mid-winter day several years ago, my student Sarah Wakefield and I pulled on snowshoes, donned backpacks, and headed up through Smugglerâs Notch. Our destination was Big Spring, which rises from Mount Mansfieldâs bedrock before flowing east for 100 yards and entering a culvert under Vermont Route 108. When it emerges from the culvert, the spring water joins a stream fed by surface runoff and snowmelt. Illustration by Adelaide Murphy Tyrol Groundwater-fed springs can flow year-round, regardless of plunging temperatures that layer thick ice on surface water streams. Spring water maintains a constant temperature, due to its long-term contact far below the surface with bedrock, and the deep sands and gravels of subterranean aquifers that are protected from the vagaries of the weather. Springs take on the average annual air temperature of their locality, and Big Spring ....
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