A Tiny Particle High in Earth’s Atmosphere


A snowflake begins when a tiny dust or pollen particle comes into contact with water vapor high in Earth’s atmosphere. The water vapor coats the tiny particle and freezes into a tiny crystal of ice. This tiny crystal will be the “seed” from which a snowflake will grow.

Hexagonal “Mineral” Crystals

The molecules of water that form each tiny ice crystal naturally arrange themselves into a hexagonal (six-sided) structure. The result will be a snowflake with six sides or six arms. Ice crystals are “minerals” because they are naturally occurring solids with a definite chemical composition and an ordered internal structure.

snowflakes - unique shape
Snowflakes have unique shapes: Photographs of many snowflakes showing how each has a hexagonal crystalline structure but a unique geometry. The shapes of the flakes are determined by the atmospheric conditions experienced as it fell through the sky. Conditions of temperature and humidity can change as the flake falls and cause variations in crystal growth.

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