What is Snow?


Snow is really nothing more than frozen water. They why doesn’t it look like ice? They are a large number of ice crystals in each snowflake, and the reflection of light from all the surfaces of the crystals makes it look white. Snow begins to be formed when water vapour in the atmosphere freezes.

Tiny crystals are formed that are clear and transparent. Since there are current in the air, these tiny crystals are carried up and down in the atmosphere. They fall and rise as different air currents move them along.

While this is happening, the crystals begin to gather around a nucleus, so that in time there may be a hundred or more gathered together. When this group of ice crystals is big enough, it floats down towards the ground.

We call this collection of ice crystals a "snowflakes". Some crystals are flat and some are like a column of needles. But regardless of the shape, snow crystals always have six sides or angles. The branches of any single snowflake are always identical, but the arrangement of the branches id different in every case.

Not two snowflakes are ever exactly alike. Did you know that snow is not always white? In many parts of the world red, green, blue, and even black snow has been! The reason for the different colors is that sometimes there are tiny fungi in the air, or dust is floating about, and this is collected by the snow as it falls.

Because snow contains so much air, it is a poor conductor of heat. That is why a "blanket" of snow can protect dormant vegetation in the ground and why igloos and snow huts can be made of blocks of snow and keep people inside quite warm.

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