Chrysoprase
Chrysoprase is an attractive apple-green form of
Chalcedony that is coloured by nickel. One of the most prized forms of
Chalcedony.
Colour can fade in sunlight and when heated, colours may recover under moist storage.
Used as cabochons, for necklaces, and for ornamental objects. In earlier centuries, it was used as a luxurious decorative stone for interior decorations.
| General Information |
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| A variety or type of: | Chalcedony, which is a variety of Quartz |
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| Chemical Formula | Walter Schumann, Gemstones of the world (2001) |
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| Chrysoprase Treatments |
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| Dyed green (chromium) - chelsea: pinkish to reddish. Might be dyed with nickel-rich solution: standard tests limited - Blue Chart Gem Identification, Herve Nicolas Lazzarelli, 2010, p 7 |
| Physical Properties of Chrysoprase |
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| Mohs Hardness | 6.5 to 7Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) |
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| Specific Gravity | 2.58 to 2.64Walter 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 | NoneWalter Schumann, Gemstones of the world (2001) |
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| Optical Properties of Chrysoprase |
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| Refractive Index | 1.530 to 1.543Herve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) |
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| Optical Character | Uniaxial/+Ulrich Henn and Claudio C. Milisenda, Gemmological Tables (2004) |
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| Birefringence | up to to 0.004Walter Schumann, Gemstones of the world (2001) |
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| Pleochroism | AbsentWalter Schumann, Gemstones of the world (2001) |
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| Dispersion | NoneWalter Schumann, Gemstones of the world (2001) |
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| Colour |
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| Colour (General) | GreenUlrich Henn and Claudio C. Milisenda, Gemmological Tables (2004) More from other references |
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| Colour (Chelsea Filter) | GreenishHerve Nicolas Lazzarelli, Blue Chart Gem Identification (2010) |
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| Causes of Colour | Green colour is caused by microscopic inclusions of silicates with Ni-bearing layers (willemseite, népouite, etc).Gemdat.org, Management Team (2012) More from other references |
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| Transparency | Translucent,OpaqueUlrich Henn and Claudio C. Milisenda, Gemmological Tables (2004) More from other references |
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| Fluorescence & other light emissions |
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| Fluorescence (General) | NoneWalter Schumann, Gemstones of the world (2001) |
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| Crystallography of Chrysoprase |
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| Crystal System | TrigonalUlrich Henn and Claudio C. Milisenda, Gemmological Tables (2004) |
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| Habit | Microcrystalline aggregatesWalter Schumann, Gemstones of the world (2001) |
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| Geological Environment |
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| Where found: | It occurs in quartz veins in nickel-bearing rocks or in veins in laterites overlying Ni-bearing serpentinites
(Queensland) and associated with jadeite in veins in serpentinized gabbro and ultramafic inclusions (Lower Silesia.)Michael O’Donoghue, Gems, Sixth Edition (2006) |
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| Spectrographic Data |
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Calculated Spectra:
Click spectra for more information |  Chrysoprase - Locality: Unknown |
| Further Information |
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| Mineral information: | Chrysoprase information at mindat.org |
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| Significant Gem Localities |
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| Myanmar | | |
| Ted Themelis (2008) Gems & mines of Mogok | |
| Ted Themelis (2008) Gems & mines of Mogok | | Poland | |
- Lower Silesian Voivodeship
- ZÄ…bkowice ÅšlÄ…skie County
| Gemstones of the world, Walter Schumann (2001) | | USA | | |
| Tucker, W. Burling (1919), El Dorado, Lassen, Modoc, Tehama, and Tulare Counties: California Mining Bureau. Report 15: 911; MacFall (1951), Gem Hunter's Guide, 1st ed.; Goodwin, Joseph Grant (1958), Mines and mineral resources of Tulare County, California: California Journal of Mines and Geology (Report 54): 54(3): 344; Murdoch, Joseph & Robert W. Webb (1966), Minerals of California, Centennial Volume (1866-1966): California Division Mines & Geology Bulletin 189: 318; Pemberton, H. Earl (1983), Minerals of California; Van Nostrand Reinholt Press: 350, 424. |
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