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Although some scientists have
found fault with the saying, most researchers agree that no
two snowflakes are alike.
Here's how
it works: A snowflake starts out as a simple hexagonal prism. As each flake
falls, it bumps into a unique range of shape-changing conditions.
In the 1970s, researchers at the Science University of Tokyo
discovered that humidity, temperature, and air pressure determine the shape of
a snowflake.
“Although no two crystals end up exactly alike, the six arms
of a single crystal all travel together, so they all grow in synchrony, giving
each falling crystal a unique and intricate structure with a recognizable
symmetry,” said Kenneth Libbrecht, a physicist at the California Institute of
Technology.
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