Difference between revisions of "Orthorhombic system"
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| − | + | The '''orthorhombic''' [[crystal system]] has three unequal [[axis|axes]], all at [[right angle]]s to one another. | |
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| + | [[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). | ||
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| + | ==Sources== | ||
| + | *Chesterman, Charles W. ''The Audubon Society Field Guide to North American Rocks and Minerals'', Alfred A. Knopf: New York (1987), ''pp. 33-34'' | ||
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| + | [[Category:Crystallography]] | ||
Latest revision as of 02:11, May 2, 2011
The orthorhombic crystal system has three unequal axes, all at right angles to one another.
Crystals are generally short, stubby, with a diamond-shaped or rectangular cross section; characteristic forms are four-sided prisms, pyramids, and pinacoids (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