Kawaii Halloween Decor Without Gore or Jump Scares
Create a gentle Halloween look with pastel colors, friendly ghosts, easy no-carve accents, and practical safety tips for your home.
The belief that no two snowflakes are exactly alike is just a myth . You will be surprised by the interesting facts about snow below.

Amazing facts about snow
Snow can also precipitate as graupel or hail. Not to be confused with hail, graupel (or snow pellets) are opaque ice particles that form in the atmosphere when ice crystals fall through frozen cloud droplets—that is, cloud particles that are colder than the freezing point of water but still in liquid form. The cloud droplets clump together to form a soft, lumpy mass. Hail, in contrast, consists of raindrops freezing into small, clear balls of ice as they fall from the sky.
America's snowiest major city has an impressive arsenal of plows, but in 1992, the city tried a new trick to control the whiteout. The City Council passed an ordinance that made any snowfall before Christmas Eve illegal. As it turned out, Mother Nature was the lawbreaker—it snowed just two days later.
In 1988, a scientist found two identical snow crystals. They came from a storm in Wisconsin.
According to some sources, the largest snowflakes ever observed fell during a blizzard in January 1887 at Montana's Fort Keogh. While eyewitnesses said the snowflakes were "larger than a milk pan." However, this claim has yet to be proven.
Snow, like the ice particles that make it up, is actually colorless. Snow is transparent, meaning that light does not pass through it easily (like clear glass), but instead reflects it. The light reflected off the surface of the snowflake is what gives it its white appearance.
But why white? The reason we see objects as colored is because some wavelengths of light are absorbed while others are reflected (remember, light is a spectrum of colors). Objects appear to be whatever color the light reflects. For example, the sky appears blue because blue wavelengths are reflected while other colors are absorbed. Because snow is made up of so many small surfaces, the light that hits it is scattered in many directions and will actually bounce from one surface to another as it is reflected. This means that no wavelength is absorbed or reflected with any consistency, so the white light is reflected back as white.
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