Ice as a Mineral
A Stefanie Hubbard Production
for GO336 Mineralogy
Created in conjunction with Old
Mother Hubbard Creations
![]() up to 100 feet tall, slips into a crevasse at the toe of a glacier. Image taken from: http://www.airbornescientific.com/Glaciers.htm. |

There are numerous uses for ice, for our: drinks, coolers, injuries, and sculptures. Ice plays a big part in recreation: ice skating, hockey, skiing, snow boarding, sledding, and ice fishing. Before refrigeration, ice was used to keep food from spoiling, and in some countries it is still used for this purpose. Ice may be used for medical purposes, such as to lower a patient's body temperature for surgery without anesthetic. Ice crystals can be easily seen in a freezer, on frozen food, in the ice cube tray, or on the freezer walls as moisture accumulates forming ice crystals. In nature ice crystals form over bodies of water when the water cools below the freezing point. Ice crystals come from the sky as snow, freezing rain, sleet, hail, and frost (Roberts, 295).
Large amounts of ice are found in glaciers formed from compacted and recrystallized snow. There are also semi-permanent areas of snow and permafrost at higher latitudes (Frye, 639). Although ice may not commonly be thought of as a mineral it meets the criteria of the definition for a mineral. It is solid below 0 ºC, homogeneous, naturally occurring, crystalline structure, has definite chemical compostition of H2O, and is formed by inorganic processes (Hurlbut pg 1).

![]() | These images are taken from the Jericho Historical Society, http://www.snowflakebentley.com, taken by William Bentley. Notice the hexgonal symmetry of the snow crystals. No two snowflakes are alike. |

This page was created on 9 December, 1999. Send me e-mail to:
hubbards@esuvm.emporia.edu
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