Opal

Opal
A blue-green section of opal encased inside a light brown rock
A rich seam of iridescent opal encased in matrix
General
CategoryMineraloid
Formula
(repeating unit)
Hydrated silica. SiO2·nH2O
IMA symbolOpl[1]
Crystal systemAmorphous[2]
Identification
ColorColorless, white, yellow, red, orange, green, brown, black, blue, pink
Crystal habitIrregular veins, in masses, in nodules
CleavageNone[2]
FractureConchoidal to uneven[2]
Mohs scale hardness5.5–6[2]
LusterSubvitreous to waxy[2]
StreakWhite
Diaphaneityopaque, translucent, transparent
Specific gravity2.15+0.08
−0.90
[2]
Density2.09 g/cm3
Polish lusterVitreous to resinous[2]
Optical propertiesSingle refractive, often anomalous double refractive due to strain[2]
Refractive index1.450+0.020
−0.080

Mexican opal may read as low as 1.37, but typically reads 1.42–1.43[2]
Birefringencenone[2]
PleochroismNone[2]
Ultraviolet fluorescenceblack or white body color: inert to white to moderate light blue, green, or yellow in long and short wave, may also phosphoresce, common opal: inert to strong green or yellowish green in long and short wave, may phosphoresce; fire opal: inert to moderate greenish brown in long and short wave, may phosphoresce[2]
Absorption spectragreen stones: 660 nm, 470 nm cutoff[2]
Diagnostic featuresdarkening upon heating
Solubilityhot salt water, bases, methanol, humic acid, hydrofluoric acid
References[3][4]
A map of the world displaying the countries where opal is most commonly found; Australia, Ethiopia, Brazil, Mexico and the United States of America are highlighted.
Main opal producing countries

Opal is a hydrated amorphous form of silica (SiO2·nH2O); its water content may range from 3% to 21% by weight, but is usually between 6% and 10%. Due to the amorphous (chemical)physical structure, it is classified as a mineraloid, unlike crystalline forms of silica, which are considered minerals. It is deposited at a relatively low temperature and may occur in the fissures of almost any kind of rock, being most commonly found with limonite, sandstone, rhyolite, marl, and basalt.

The name opal is believed to be derived from the Sanskrit word upala (उपल), which means 'jewel', and later the Greek derivative opállios (ὀπάλλιος).

There are two broad classes of opal: precious and common. Precious opal displays play-of-color (iridescence); common opal does not.[5] Play-of-color is defined as "a pseudo chromatic optical effect resulting in flashes of colored light from certain minerals, as they are turned in white light."[6] The internal structure of precious opal causes it to diffract light, resulting in play-of-color. Depending on the conditions in which it formed, opal may be transparent, translucent, or opaque, and the background color may be white, black, or nearly any color of the visual spectrum. Black opal is considered the rarest, while white, gray, and green opals are the most common.

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ a b c d e f g h i j k l m Gemological Institute of America, GIA Gem Reference Guide 1995, ISBN 0-87311-019-6
  3. ^ "Opal". Webmineral. Archived from the original on 18 October 2011. Retrieved 8 October 2011.
  4. ^ "Opal". Mindat.org. Archived from the original on 6 October 2011. Retrieved 8 October 2011.
  5. ^ "Opal Description". Gemological Institute of America. Retrieved 4 June 2018.
  6. ^ "Glossary: Play of Color". Mindat. Retrieved 4 June 2018.

Opal

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