Smithsonite
Smithsonite was named in 1832 in honor of English chemist and mineralogist, James Smithson, who first identified the mineral in 1802.
It usually occurs as earthy botryoidal masses. Grape-like clusters have pearly luster and are often slightly banded. Well-formed crystals are rare.
Bonamite is a trade name for cabochon-cut massive pieces of Smithsonite.
General Information |
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Other Names/Trade Names: | |
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Chemical Formula | Michael O’Donoghue, Gems, Sixth Edition (2006) More from other references |
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Physical Properties of Smithsonite |
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Mohs Hardness | 5 to 5.5Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Specific Gravity | 4.00 to 4.65Walter Schumann, Gemstones of the world (2001) More from other references |
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Tenacity | BrittleWalter Schumann, Gemstones of the world (2001) |
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Cleavage Quality | PerfectArthur Thomas, Gemstones (2009) More from other references |
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Fracture | UnevenWalter Schumann, Gemstones of the world (2001) More from other references |
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Optical Properties of Smithsonite |
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Refractive Index | 1.620 to 1.850Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Optical Character | Uniaxial/-Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Birefringence | 0.228Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Pleochroism | AbsentWalter Schumann, Gemstones of the world (2001) More from other references |
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Dispersion | 0.014 to 0.031Walter Schumann, Gemstones of the world (2001) More from other references |
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Colour |
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Colour (General) | White, yellowish, brown, green, gray, pink, bluish, orange-yellowUlrich Henn and Claudio C. Milisenda, Gemmological Tables (2004) More from other references |
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Causes of Colour | Blue-green, Cu2+. Pink, Co2+W. William Hanneman, Pragmatic Spectroscopy For Gemologists (2011) |
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Transparency | Translucent,OpaqueHerve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Lustre | Vitreous,PearlyArthur Thomas, Gemstones (2009) |
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Fluorescence & other light emissions |
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Fluorescence (General) | Blue-white, pink, brownWalter Schumann, Gemstones of the world (2001) |
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Crystallography of Smithsonite |
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Crystal System | TrigonalHerve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Habit | Botryoidal, rhombohedralArthur Thomas, Gemstones (2009) More from other references |
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Geological Environment |
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Where found: | Smithsonite occurs as a secondary mineral in the oxidized zone of zinc-bearing deposits.Michael O’Donoghue, Gems, Sixth Edition (2006) |
Further Information |
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Mineral information: | Smithsonite information at mindat.org |
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Significant Gem Localities |
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| Namibia | |
| Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 205, 251, 919. | | USA | |
- Magdalena Mining District
| Gems, Sixth Edition, Michael O’Donoghue, 2006, p. 452 |
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