Now that the snow is here for the season, let's look a little more closely at what causes some to rejoice and other to hide until spring arrives.
- They have 6 sides
- They begin as ice crystals from water vapor in the atmosphere. The ice crystals begin as hexagonal shapes (6-sided). As they fall toward earth, they may collect more water, creating the familiar branching patterns
- When it is particularly cold, well below the 32 degree freezing mark, snowflakes may stay as crystals. If the temperature is close to 32 degrees, there is a higher possibility of more water vapor in the air, creating traditional branched snowflakes. So, temperature plays a part in the formation of snowflakes, along with humidity, wind, and other atmospheric conditions.
I find it fascinating that there are roughly 6 distinct types of snowflakes:
- Plates
- Columns
- Stars
- Dendrites
- Prisms
- Needles
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Prism - very basic form, 6 sided |
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A columnar flake with hollowed ends |
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A great figure in snowflake history is Wilson Bentley, also known as "Snowflake" Bentley. A gentleman from Vermont, farming during the season and experimenting with snowflake photography in the off-season, Mr. Bentley spent much of his life figuring out the mysteries of snowflakes. His first photograph of a snowflake occurred on January 15, 1885, seen below:
What is fascinating is not that the snowflake was photographed, but that it was done after many years of trial and error in the late 1800s, and to such quality. For more information about Snowflake Bentley and the museum curating his work, please visit www.snowflakebentley.com.
Whether snow is a boon or a bane to you, one can always appreciate the intricacies of nature, specifically snowflakes. Here's to 2013 and all it brings!
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