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Τι (ποιος) είναι lussatite - ορισμός
![The crystal structure of crystalline α-[[cristobalite]]. Locally, the structures of some opals, opal-C, are similar to this.](https://commons.wikimedia.org/wiki/Special:FilePath/Alphacrist.png?width=200 "The crystal structure of crystalline α-[[cristobalite]]. Locally, the structures of some opals, opal-C, are similar to this.")
![Boulder opal, Carisbrooke Station near [[Winton, Queensland]]](https://commons.wikimedia.org/wiki/Special:FilePath/Boulder Opal.jpg?width=200 "Boulder opal, Carisbrooke Station near [[Winton, Queensland]]")
![This multicolored rough opal from [[Coober Pedy]], [[South Australia]], displays nearly every color of the [[visible spectrum]].](https://commons.wikimedia.org/wiki/Special:FilePath/Coober Pedy Opal 2.jpg?width=200 "This multicolored rough opal from [[Coober Pedy]], [[South Australia]], displays nearly every color of the [[visible spectrum]].")
![silica]] molecules arranged in regular, closely packed planes (idealized diagram).](https://commons.wikimedia.org/wiki/Special:FilePath/Opal molecular structure2.jpg?width=200 "silica]] molecules arranged in regular, closely packed planes (idealized diagram).")
![Precious opal replacing [[ichthyosaur]] backbone, as a display specimen in [[South Australian Museum]]](https://commons.wikimedia.org/wiki/Special:FilePath/Opalised Ichthyosaur backbone.jpg?width=200 "Precious opal replacing [[ichthyosaur]] backbone, as a display specimen in [[South Australian Museum]]")
Βικιπαίδεια
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 its amorphous property, 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), which means 'to see a change in color'.
There are two broad classes of opal: precious and common. Precious opal displays play-of-color (iridescence); common opal does not. 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." 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.
