Snow is precipitation in the form of crystalline water ice, consisting of a multitude of snowflakes. Since it is composed of small rough particles it is a granular material. It has an open and therefore soft structure, unless packed by external pressure. Snow is commonly formed when water vapor undergoes deposition high in the atmosphere at a temperature of less than 0°C (32°F), and then falls to the ground.

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Published Sunday, January 13, 2008 by Jim Meldrum | E-mail this post

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  • Heres some of the highlights of our trip to Peru. Its taken me a while to post these!





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