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The formation of snow occurs through a process called crystallization, which begins when water vapor in the atmosphere cools and condenses into tiny ice crystals. These crystals grow by absorbing additional water vapor, and as they collide and stick together, they form snowflakes. The structure of the snowflakes is influenced by temperature and humidity conditions, resulting in the unique and intricate patterns we observe. When enough of these snowflakes accumulate, they fall to the ground as snow.

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