Sodalite
Sodalite is named after its sodium content, it may be classed as a feldspathoid. Only blue stones are used in jewelry, sometimes they have violet tint. Sodalite may also be grey, yellow, green, or pink and is often mottled with white veins or patches.
It was first discovered in 1811 in Greenland, but became important as an ornamental stone in 1891 when vast deposits of fine material were discovered in Ontario, Canada.
General Information |
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Varieties/Types: | Hackmanite - Pink to grey-white to white variety of Sodalite. |
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Chemical Formula | Michael O’Donoghue, Gems, Sixth Edition (2006) More from other references |
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Sodalite Treatments |
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Sodalite is reported to lose its color on heating and regain it on irradiation (Przibram and Caffyn, 1956), indicating the probable presence of a color center - Nassau (1984) |
Physical Properties of Sodalite |
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Mohs Hardness | 5 to 6Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Specific Gravity | 2.15 to 2.40Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Tenacity | BrittleAnthony et al, Handbook of mineralogy (2001) |
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Cleavage Quality | IndistinctWalter Schumann, Gemstones of the world (2001) More from other references |
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Fracture | UnevenArthur Thomas, Gemstones (2009) More from other references |
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Optical Properties of Sodalite |
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Refractive Index | 1.478 to 1.488Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Optical Character | IsotropicUlrich Henn and Claudio C. Milisenda, Gemmological Tables (2004) More from other references |
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Birefringence | NoneWalter Schumann, Gemstones of the world (2001) |
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Pleochroism | AbsentWalter Schumann, Gemstones of the world (2001) |
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Dispersion | 0.018Walter Schumann, Gemstones of the world (2001) More from other references |
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Colour |
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Colour (General) | Blue, blue-violetUlrich Henn and Claudio C. Milisenda, Gemmological Tables (2004) More from other references |
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Causes of Colour | Blue, interstitial oxygen ion O- near Al or Si. Pink, (hackmanite), unstable electron substituting for Cl- in a tetrahedron of Na+ ionsW. William Hanneman, Pragmatic Spectroscopy For Gemologists (2011) |
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Transparency | Transparent,Translucent,OpaqueUlrich Henn and Claudio C. Milisenda, Gemmological Tables (2004) More from other references |
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Lustre | Vitreous,GreasyArthur Thomas, Gemstones (2009) |
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Fluorescence & other light emissions |
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Fluorescence (General) | Strong; orangeWalter Schumann, Gemstones of the world (2001) More from other references |
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Crystallography of Sodalite |
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Crystal System | IsometricHerve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Habit | Polycrystalline aggregate, commonly with white veinsUlrich Henn and Claudio C. Milisenda, Gemmological Tables (2004) More from other references |
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Geological Environment |
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Where found: | Formed in nepheline syenites, phonolites, and related rock types. In metasomatized calcareous rocks, and in cavities in ejected volcanic blocks.Anthony et al, Handbook of mineralogy (2001) |
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Inclusions in Sodalite |
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White calcite patches and veins. No pyrite inclusions unlike lapis. Translucent sodalite: small black inclusions common - Blue Chart Gem Identification, Herve Nicolas Lazzarelli, 2010, p 9 |
Further Information |
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Mineral information: | Sodalite information at mindat.org |
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Significant Gem Localities |
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| Bolivia | |
| | | Greenland | |
| Gems, Sixth Edition, Michael O’Donoghue, 2006, p. 453 | | Myanmar | |
| [var: Hackmanite] |
| Ted Themelis (2008) Gems & mines of Mogok |
| [var: Hackmanite] Ted Themelis (2008) Gems & mines of Mogok |
- Dattaw-taung (Dattaw hill)
| [var: Hackmanite] Ted Themelis (2008) Gems & mines of Mogok |
| [var: Hackmanite] Ted Themelis (2008) Gems & mines of Mogok |
| [var: Hackmanite] Ted Themelis (2008) Gems & mines of Mogok |
| [var: Hackmanite] |
- Pein-Pyit (Painpyit; Pyan Pyit)
| [var: Hackmanite] Ted Themelis (2008) Gems & mines of Mogok |
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