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Chrysocolla

Phyllosilicate mineral


Phyllosilicate mineral

FieldValue
nameChrysocolla
categoryPhyllosilicate minerals
boxbgcolor#36cacb
imageChrysocolla-230109.jpg
captionChrysocolla specimen from Ray mine, in the Scott Mountain area of Mineral Creek District, Pinal County, Arizona, US
formula(*x*
IMAsymbolCcl
strunz9.ED.20
unit cella = 5.7 Å, b = 8.9 Å,
c = 6.7 Å; Z = 1
colorBlue, cyan (blue-green), green, dark blue to black, brown, rarely yellow
habitMassive, nodular, botryoidal
systemOrthorhombic
Unknown space group
cleavagenone
fractureIrregular/uneven, sub-conchoidal
tenacityBrittle to sectile
mohs2.5–3.5 (7 for chrysocolla chalcedony, high-silica content)
lusterVitreous to dull
refractivenα = 1.575–1.585 nβ = 1.597 nγ = 1.598–1.635
opticalpropBiaxial (−)
birefringenceδ = 0.023–0.050
streakWhite to a blue-green color
gravity1.9–2.4
diaphaneityTranslucent to opaque
references

c = 6.7 Å; Z = 1 Unknown space group

Chrysocolla ( ) is a hydrous copper phyllosilicate mineral and mineraloid with the formula (x

The structure of the mineral has been questioned, as a 2006 spectrographic study suggest material identified as chrysocolla may be a mixture of the copper hydroxide spertiniite and chalcedony.

Chrysocolla typically forms amorphously.

History

The name chrysocolla comes from the Ancient Greek () and (), meaning "gold" and "glue" respectively, in allusion to the name of the material used to solder gold. The word was first used by Theophrastus in 315 BC.

Geology

Chrysocolla has a cyan (blue-green) color and is a minor ore of copper, having a hardness of 2.5 to 7.0. It is of secondary origin and forms in the oxidation zones of copper ore bodies. Associated minerals are quartz, limonite, azurite, malachite, cuprite, and other secondary copper minerals. It is typically found as botryoidal or rounded masses and crusts, or vein fillings.

A 2006 study has produced evidence that chrysocolla may be a microscopic mixture of the copper hydroxide mineral spertiniite, amorphous silica and water.

Jewelry

Due to being somewhat more common than turquoise, its wide availability, and vivid, beautiful blue and blue-green colors, chrysocolla has been popular for use as a gemstone for carvings and ornamental use since antiquity. It is often used in silversmithing and goldsmithing in place of turquoise and is relatively easy to work and shape. Chrysocolla exhibits a wide range of Mohs hardness ranging from 2 through 7, which is dependent on the amount of silica incorporated into the stone when it is forming. Generally, dark navy blue chrysocolla is too soft to be used in jewelry, while cyan, green, and blue-green chrysocolla can have a hardness approaching 6, similar to turquoise. Chrysocolla chalcedony is a heavily silicified form of chrysocolla that forms in quartz deposits and can be very hard and approach a hardness of 7.

References

References

  1. Warr, L. N.. (2021). "IMA–CNMNC approved mineral symbols". [[Mineralogical Magazine]].
  2. "Chrysocolla".
  3. "Chrysocolla".
  4. {{Mindat
  5. Barthelmy, Dave. "Chrysocolla Mineral Data".
  6. Chen, Chermaine. (2021-09-02). "Chrysocolla Stone: Meaning, Uses & Other Facts about this Blue Green Crystal".
  7. {{cite EB1911. Leonard James. Spencer
  8. [http://www.slac.stanford.edu/cgi-wrap/getdoc/slac-pub-12232.pdf François Farges, Karim Benzerara, Gordon E. Brown, Jr.; ''Chrysocolla Redefined as Spertiniite''; SLAC-PUB-12232; 13th International Conference On X-Ray Absorption Fine Structure (XAFS13); July 9-14, 2006; Stanford, California]
  9. "Gem Silica: The blue, most valuable variety of chalcedony".
  10. "Chrysocolla: The gemstone chrysocolla information and pictures".
  11. "Chrysocolla Value, Price, and Jewelry Information - IGS".
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