What happens is that most winters, the smaller creeks freeze to the bottom, but if their source water is an underground spring, it will continue to flow and force water to the surface through cracks in the ice, creating continuous layers of water and ice. Sometimes it can build up to 8 to ten ft thick (that's about 3 meters to the French). Where a trail crosses a creek, it can create an ice dam that will back up the overflow water, so that it spreads laterally up and down the trail, freezing into a sloping, slippery mess.
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