|Chemical formula||lead sulfide (PbS)|
|Color||Lead gray, silvery|
|Crystal habit||Cubes and octahedra, tabular and sometimes skeletal crystals|
|Crystal system||Isometric hexoctahedral|
|Fracture||Flat (when cubic) to even|
|Mohs Scale hardness||2.5 - 2.75|
|Specific gravity||7.4 - 7.6|
Galena is the natural mineral form of lead sulfide. It is one of the most abundant and widely distributed sulfide minerals. It is the most important lead ore mineral. It is also an important source of silver, which is often found in the mineral. It was once used as the semiconductor (or "crystal") in crystal radio sets.
Lead ore deposits
Galena deposits often contain significant amounts (up to one percent) of silver as included silver sulfide mineral phases or as limited solid solution within the galena structure. In addition, zinc, cadmium, antimony, arsenic and bismuth also occur in variable amounts in lead ores. Selenium substitutes for sulfur in the structure constituting a solid solution series. The lead telluride mineral altaite has the same crystal structure as galena. Within the weathering or oxidation zone, galena changes to anglesite (lead sulfate) or cerussite (lead carbonate).
Galena deposits are found in France, Romania, Austria, Belgium, Italy, Spain, Scotland, England, Australia, and Mexico. Noted deposits include those at Freiberg, Saxony; Cornwall, Derbyshire, and Cumberland, England; the Sullivan mine of British Columbia; and Broken Hill, Australia. Galena also occurs at Mount Hermon in Northern Israel. In the United States it occurs most notably in the Mississippi Valley type deposits of the Lead Belt in southeastern Missouri, and in similar environments in Illinois, Iowa and Wisconsin. Galena also was a major mineral of the zinc-lead mines of the tri-state district around Joplin in southwestern Missouri and the adjoining areas of Kansas and Oklahoma. Galena is also an important ore mineral in the silver mining regions of Colorado, Idaho, Utah and Montana. Of the latter, the Coeur d'Alene district of northern Idaho was most prominent.
Galena is the official state mineral of the states of Missouri and Wisconsin.
Galena has practically the same crystal structure as halite (sodium chloride, NaCl). It crystallizes in the cubic crystal system, often showing octahedral forms. In addition, it is a semiconductor with a small bandgap of 0.4 electron volts (eV).
Galena is now the principal ore of lead. Also, given the large quantities of the mineral that are processed, argentiferous (silver-containing) galenas have long been the most important ore of silver. In addition, in the early days of wireless, it was used as the semiconductor (or "crystal") in crystal radio sets. Combined with a safety pin or similar sharp wire known as a "cat's whisker," the galena crystal became part of a point-contact diode used to detect radio signals.
- Metropolitan Museum of Art. The Art of Medicine in Ancient Egypt. (New York: The Museum, 2005), p. 10. ISBN 1588391701
ReferencesISBN links support NWE through referral fees
- Farndon, John. 2006. The Practical Encyclopedia of Rocks & Minerals: How to Find, Identify, Collect and Maintain the World's best Specimens, with over 1000 Photographs and Artworks. London: Lorenz Books. ISBN 0754815412
- Klein, Cornelis, and Barbara Dutrow. 2007. Manual of Mineral Science, 23rd edition. New York: John Wiley. ISBN 9780471721574
- Pellant, Chris. 2002. Rocks and Minerals. Smithsonian Handbooks. New York: Dorling Kindersley. ISBN 0789491060
- Shaffer, Paul R., Herbert S. Zim, and Raymond Perlman. 2001. Rocks, Gems and Minerals, Revised edition. New York: St. Martin's Press. ISBN 1582381321
- Mindat.org. 2007. Galena. Mindat.org. Retrieved April 10, 2007.
- Mineral Gallery. 2006. The Mineral Galena. Amethyst Galleries. Retrieved April 10, 2007.
- Mineral Gallery. 2006. The Galena Group of Minerals. Amethyst Galleries. Retrieved April 10, 2007.
All links retrieved May 18, 2017.
New World Encyclopedia writers and editors rewrote and completed the Wikipedia article in accordance with New World Encyclopedia standards. This article abides by terms of the Creative Commons CC-by-sa 3.0 License (CC-by-sa), which may be used and disseminated with proper attribution. Credit is due under the terms of this license that can reference both the New World Encyclopedia contributors and the selfless volunteer contributors of the Wikimedia Foundation. To cite this article click here for a list of acceptable citing formats.The history of earlier contributions by wikipedians is accessible to researchers here:
The history of this article since it was imported to New World Encyclopedia:
Note: Some restrictions may apply to use of individual images which are separately licensed.