When people say snowflake, they often mean snow crystal. A snow crystal is a single crystal of ice within which the water molecules are lined up in a hexagonal array. That's probably the image you think of when you are thinking of a snowflake. However, the term snowflake is actually a lot more general than that. It can refer to a snow crystal, but it can also refer to almost anything that falls from winter clouds. You may have heard that every snowflake is unique, but why is that? Well, every snow crystal starts when an extremely cold water droplet freezes onto a pollen or dust particle in the sky, forming a small hexagonal plate.. Branches sprout from the corners as it grows larger. As a snow crystal tumbles through the clouds, it experiences different temperatures and humidities, which affect the growth of the snowflake's branches in unique ways. No two snowflakes are the same because no two snowflakes have had the exact same journey through the atmosphere! Contrary to popular belief, most snowflakes are not perfectly symmetrical. The branches will look similar because they have all been through the same changes as they moved through the atmosphere, but irregular snowflakes are much more common than the near-perfect kind. Now that we know a little bit about snowflake science, here's an experiment you can try at home to make your own "snowflake". Borax Snowflake What you'll need:
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