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The '''orthorhombic''' [[crystal system]] has three unequal [[axis|axes]], all at [[right angle]]s to one another.

[[Crystal]]s are generally short, stubby, with a [[diamond]]-shaped or [[rectangle|rectangular]] cross section; characteristic forms are four-sided [[prism]]s, [[pyramid]]s, and [[pinacoid]]s (open forms made up of two [[parallel]] faces).

==Sources==
*Chesterman, Charles W. ''The Audubon Society Field Guide to North American Rocks and Minerals'', Alfred A. Knopf: New York (1987), ''pp. 33-34''

[[Category:Crystallography]]
nsTeam1RO, nsTeam1RW, nsTeam1_talkRO, nsTeam1_talkRW
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