Celestine
Celestine is named after Latin "caelestis" - of the sky, alluding to the sky-blue colour commonly exhibited by its crystals.
Celestine is usually colourless or pale blue, but orange (Ontario, Canada), brown, yellow and greenish material has been reported.
It occurs as tabular and prismatic crystals, and also in compact massive and fibrous forms or as numerous crystals lining geodes. The geode has crystals as 18 inches wide (46 cm) across, estimated weight up to 300 pounds (135 kg) each.
Perfect cleavage and brittleness make Celestine difficult to facet. Cut stones rarely exceed 10 carats.
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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Celestine Treatments |
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Celestite, SrSO4, also called celestine, as well as the closely related ,materials anhydrite, CaSO4, also called vulpinite (Webster, p. 298), and barite, BaSO4, are soft sulfates which occur at times with attractive violet or blue colors. Heating to as little as 200°C causes these colors to fade, as also sometimes happens on exposure to light. Irradiation restores or produces the blue or violet color, sometimes in a banded form; the color may be stable to light or may fade, depending on the nature of the material (Przibram and Caffyn, 1956; Pough, 1957). In celestite there are several color centers involved, including SO-3, SO-2 and O-, all stabilized by a potassium impurity (Bernstein, 1979) – Nassau (1984) |
Physical Properties of Celestine |
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Mohs Hardness | 3 to 3.5Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Specific Gravity | 3.90 to 4.00Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Tenacity | BrittleHerve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) |
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Cleavage Quality | PerfectArthur Thomas, Gemstones (2009) |
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Fracture | UnevenArthur Thomas, Gemstones (2009) |
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Heat Sensitivity | Sensitive to heatHerve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) |
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Optical Properties of Celestine |
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Refractive Index | 1.619 to 1.635Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Optical Character | Biaxial/+Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Birefringence | 0.004 to 0.012Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Pleochroism | Weakly trichroicArthur Thomas, Gemstones (2009) |
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Dispersion | NilArthur Thomas, Gemstones (2009) |
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Colour |
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Colour (General) | Bluish-white, colourless, seldom reddish, greenWalter Schumann, Gemstones of the world (2001) More from other references |
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Transparency | TransparentMichael O’Donoghue, Gems, Sixth Edition (2006) More from other references |
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Lustre | VitreousWalter Schumann, Gemstones of the world (2001) More from other references |
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Fluorescence & other light emissions |
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Fluorescence (General) | Inert to weak fluorescence of body color (possible phosphorescence)Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Crystallography of Celestine |
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Crystal System | OrthorhombicHerve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) More from other references |
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Habit | TabularMichael O’Donoghue, Gems, Sixth Edition (2006) More from other references |
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Geological Environment |
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Where found: | The origin of celestine is chiefly sedimentary. It occurs as cavity or
fissure fillings, particularly in limestones and in hydrothermal veins.Michael O’Donoghue, Gems, Sixth Edition (2006) |
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Inclusions in Celestine |
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Liquid inclusions, partially healed fractures - Blue Chart Gem Identification, Herve Nicolas Lazzarelli, 2010, p 5 |
Further Information |
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Mineral information: | Celestine information at mindat.org |
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Significant Gem Localities |
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| Namibia | |
| Gems, Sixth Edition, Michael O’Donoghue, 2006, p. 396 |
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