How do these delicate frosty flakes form, and are they truly unique?
Snowflakes form around tiny particles of dust or pollen floating through the atmosphere; as a particle passes through clouds of water molecules, they stick to its surface to form a droplet. At freezing temperatures high in the atmosphere, this droplet begins to freeze and form crystal faces. These crystals begin the formation of the snowflake’s shape. The reason for their symmetrical shape is due to the structure of the water molecules. Hydrogen and oxygen atoms bond together at a 104.5-degree angle, creating a V-shaped structure with two hydrogen atoms attached to one oxygen atom in the middle. As water molecules bond to one another, six of these ‘V’ structures form a hexagonal shape. This process continues and the crystals begin to fall as more water molecules join the frozen particle party – as many as 1 billion billion (1018) water molecules can be present in the average flake! The surrounding temperature of a falling snowflake will increase as it nears the ground. This limits the amount of freeze and the number of water molecules that can join onto it, creating spiking symmetrical structures, although with many variations. As the old saying goes, no two snowflakes are ever the same. During its descent several factors affect the eventual shape and size of a snowflake. Humidity, wind, temperature and even the variant of hydrogen atoms present – all these factors have an effect on flake formation. Unless each individual water molecule and forming crystals are exposed to the exact same conditions they will not form in the exact same way, which explains the countless varieties of snowflake.
Stellar snowflakes form when water molecules collect at the outermost points of the snowflake, creating branches