The Science of Snowflakes: Are Two Snowflakes the Same? Clouds are made up of water droplets, water vapour and suspended impurities such as tiny dust particles. If the temperature of the cloud then decreases the water molecules can begin to crystallise, arranging themselves around the dust particles in a hexagonal lattice structure known as Ice Ih (see figure 1). There are fourteen known forms of ice, but ice Ih, an abbreviation for "form 1 hexagonal", is stable between -100°C and 0°C and so it is the form seen in snowflakes. The hexagonally arranged water molecules stack in sheets with sides that are perfectly straight and angled at 120° to each other, called 'facets' (see figure 2). Figure 1 Red spheres represent oxygen atoms and white spheres represent hydrogen atoms. As the air is cooled, the closest neighbouring water molecules begin to arrange themselves into a lattice, gradually taking on the hexagonal geometry of '