Why Puddles Always Freeze From the Edges First (Not the Center)
Sunday, March 1, 2026
| March 01, 2026 | |||||
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A Predictable Winter Morning PatternWalk past a puddle on a cold morning and you'll notice ice has formed around the edges while the center remains liquid. Sometimes just a thin ring borders the puddle; other times ice extends partway across. This edge-first freezing appears so consistently it seems inevitable, yet both edges and center are exposed to the same cold air. What gives edges an advantage? Shallow Water Freezes Faster Ground Temperature Is Crucial Why the Pattern Reinforces:
Puddles offer accessible ways to observe freezing physics in real time. Discover why temperature cycling creates visible layers, how moving water disrupts ice formation, and why this same principle makes shoreline ice thicker and stronger than ice farther out on ponds and lakes. | |||||
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posted by Myrna Sophia at 3:34 PM
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