Difference between revisions of "Galena" - New World Encyclopedia
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{{Infobox mineral | {{Infobox mineral | ||
| name = Galena | | name = Galena | ||
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− | '''Galena''' is the natural mineral form of [[lead sulfide]]. It is one of the most abundant and widely distributed sulfide minerals. | + | '''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 set|crystal radio sets]]. |
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− | It is the most important [[lead]] [[ore]] mineral. | ||
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==Lead ore deposits== | ==Lead ore deposits== | ||
+ | Galena is often associated with the minerals [[sphalerite]], [[calcite]], and [[fluorite]]. | ||
− | + | 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 | + | 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. | |
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− | Galena is the | ||
== Characteristics == | == Characteristics == | ||
− | It crystallizes in the [[Cubic (crystal system)|cubic]] crystal system often showing [[octahedral]] forms. | + | Galena has practically the same crystal structure as halite (sodium chloride, NaCl). It crystallizes in the [[Cubic (crystal system)|cubic]] crystal system, often showing [[octahedral]] forms. In addition, it is a semiconductor with a small bandgap of 0.4 electron volts (eV). |
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==Uses== | ==Uses== | ||
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− | One of the earliest uses of galena was as [[kohl]], which in [[ | + | One of the earliest uses of galena was as [[kohl]], which in [[ancient Egypt]] was applied around the eyes to reduce the glare of the desert sun and to repel flies, a potential source of disease.<ref>Metropolitan Museum of Art. ''The Art of Medicine in Ancient Egypt.'' (New York: The Museum, 2005), p. 10. ISBN 1588391701</ref> |
− | Galena is | + | 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 set|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. |
==See also== | ==See also== | ||
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==References== | ==References== | ||
− | + | * Farndon, John. ''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, 2006. ISBN 0754815412 | |
− | * Farndon, John | + | * Klein, Cornelis, and Barbara Dutrow. ''Manual of Mineral Science'', 23rd ed. New York: John Wiley, 2007. ISBN 978-0471721574 |
− | + | * Pellant, Chris. ''Rocks and Minerals''. Smithsonian Handbooks. New York: Dorling Kindersley, 2002. ISBN 0789491060 | |
− | * Klein, Cornelis, and Barbara Dutrow | + | * Shaffer, Paul R., Herbert S. Zim, and Raymond Perlman. ''Rocks, Gems and Minerals'', Revised edition. New York: St. Martin's Press, 2001. ISBN 1582381321 |
− | + | * Mindat.org. 2007. [http://www.mindat.org/min-1641.html Galena.] ''Mindat.org''. Retrieved October 22, 2022. | |
− | * Pellant, Chris | ||
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− | * Shaffer, Paul R., Herbert S. Zim, and Raymond Perlman | ||
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− | * Mindat.org. 2007. [http://www.mindat.org/min-1641.html Galena.] ''Mindat.org''. Retrieved | ||
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==External links== | ==External links== | ||
+ | All links retrieved April 17, 2024. | ||
− | * [http://webmineral.com/data/Galena.shtml Galena Mineral Data.] | + | * [http://webmineral.com/data/Galena.shtml Galena Mineral Data.] |
− | + | * [http://rruff.geo.arizona.edu/doclib/hom/galena.pdf Galena.] | |
− | + | * [http://www.atsdr.cdc.gov/toxfaqs/tf.asp?id=93&tid=22 ToxFAQs™ for Lead.] | |
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− | * [http://rruff.geo.arizona.edu/doclib/hom/galena.pdf Galena.] | ||
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− | * [http://www.atsdr.cdc.gov/ | ||
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[[Category:Physical sciences]] | [[Category:Physical sciences]] |
Latest revision as of 03:50, 18 April 2024
Galena | |
---|---|
General | |
Category | Sulfides |
Chemical formula | lead sulfide (PbS) |
Identification | |
Color | Lead gray, silvery |
Crystal habit | Cubes and octahedra, tabular and sometimes skeletal crystals |
Crystal system | Isometric hexoctahedral |
Cleavage | Cubic |
Fracture | Flat (when cubic) to even |
Mohs Scale hardness | 2.5 - 2.75 |
Luster | Metallic |
Refractive index | Opaque |
Pleochroism | None |
Streak | Lead gray |
Specific gravity | 7.4 - 7.6 |
Fusibility | 2 |
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 is often associated with the minerals sphalerite, calcite, and fluorite.
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.
Characteristics
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).
Uses
One of the earliest uses of galena was as kohl, which in ancient Egypt was applied around the eyes to reduce the glare of the desert sun and to repel flies, a potential source of disease.[1]
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.
See also
Notes
- ↑ 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. 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, 2006. ISBN 0754815412
- Klein, Cornelis, and Barbara Dutrow. Manual of Mineral Science, 23rd ed. New York: John Wiley, 2007. ISBN 978-0471721574
- Pellant, Chris. Rocks and Minerals. Smithsonian Handbooks. New York: Dorling Kindersley, 2002. ISBN 0789491060
- Shaffer, Paul R., Herbert S. Zim, and Raymond Perlman. Rocks, Gems and Minerals, Revised edition. New York: St. Martin's Press, 2001. ISBN 1582381321
- Mindat.org. 2007. Galena. Mindat.org. Retrieved October 22, 2022.
External links
All links retrieved April 17, 2024.
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