The formation of a snowflake begins when a water droplet freezes onto a dust particle in the frigid upper atmosphere. As the crystal grows, it takes on a hexagonal shape due to the arrangement of water molecules in an ice lattice. However, what truly sets snowflakes apart is their astonishing diversity. No two snowflakes are exactly alike, and this is due to the variable conditions they encounter during their descent to Earth. Factors like temperature, humidity, and the path they take through the atmosphere influence their growth, resulting in an array of intricate patterns.

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