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An ice crystal becomes a snowflake through a process called crystallization, where water vapor in the atmosphere condenses and freezes around a small particle, such as dust or pollen. As the crystal falls through varying temperatures and humidity levels, additional water vapor freezes onto it, causing the crystal to grow and develop intricate patterns. The unique shape of each snowflake is influenced by these environmental conditions, resulting in the diverse and beautiful forms we see. Ultimately, snowflakes are essentially complex, symmetrical ice crystals that have formed as they descend through the atmosphere.

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1mo ago

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