The tension between geothermal warmth carried by groundwater and winter chill carried in Arctic air masses forms a delicate balance in the icy bridges that span groundwater fed streams in the Hocking Hills of southeast Ohio and in moist rocky ravines throughout the Midwest.
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Fragile latticework of feathery ice bridging groundwater fed stream, Hocking Hills. |
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Delicate radiating ice crystals interlock for accidental strength, suspended above flowing water. |
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