Topaz is a silicate mineral made of aluminium and fluorine with the chemical formula aluminiumsiliconoxygen(fluorine, hydroxide). It is used as a gemstone in jewelry and other adornments. Common topaz in its natural state is colorless, though trace element impurities can make it pale blue or golden-brown to yellow-orange. Topaz is often treated with heat or radiation to make it a deep blue, reddish-orange, pale green, pink, or purple.
Topaz is a nesosilicate mineral, and more specifically, an aluminosilicate mineral. It is one of the hardest naturally occurring minerals and has a relatively low index of refraction. It has the orthorhombic crystal system and a dipyramidial crystal class.
It occurs in many places in the world. Two of the most popular places that topaz is sourced are Brazil and Russia. Topaz is often mined in open-pit or alluvial settings.
Many English translations of the Bible, including the King James Version, mention topaz. However, because these translations as topaz all derive from the Septuagint translation topazios, which referred to a yellow stone that was not topaz, but probably chrysolite (chrysoberyl or peridot), topaz is likely not meant here.Farrington, Oliver (1903) Gems and Gem Minerals. Chicago. p. 119.
An English superstition also held that topaz cured lunatic.Pettigrew, Thomas Joseph (1844) On Superstitions Connected with the History and Practice of Medicine and Surgery. Philadelphia E. Barrington and G.D. Haswell. p. 70. The ancient Romans believed that topaz provided protection from danger while traveling.
Topaz is a part of the second rank of gemstones, or semiprecious stones, accompanying aquamarine, morganite, and tourmaline. The first rank of gemstones, or precious stones, includes ruby, sapphire, diamond, and emerald.
Orange topaz, also known as precious topaz, is the birthstone for the month of November, the symbol of friendship, and the state gemstone of the U.S. state of Utah. Blue topaz is the state gemstone of the US state of Texas. The 4th wedding anniversary gem is blue topaz and the 23rd is imperial topaz.
Synthetic topaz can be produced using a method that includes the thermal hydrolysis of SiO2 and AlF3.
To care for a topaz gemstone, it is best to avoid ultrasonic cleaners or steam as this could produce small fractures within the crystal. Warm water with soap is the best way to wash it.
To choose an ethically sourced topaz gemstone, it is recommended to search for a stone that the seller knows the origin of.
The crystal structure of topaz alternates between sheets of (F, OH)2O and O along (010) with Al3+ occupying the octahedral sites and Si4+ in the tetrahedral sites. Fluorine can be substituted by hydroxide in topaz by up to 30 mol.% in nature and hydroxide-dominating topaz can be made in laboratories but has not been found in nature.
On occasion, cavities can be found within topaz and they are filled with a liquid called brewsterlinite. Brewsterlinite was discovered by David Brewster upon heating a sample of topaz. After heating, the topaz lost mass, and through examination Brewster concluded Topaz was formed in a wet environment creating these liquid-filled cavities. This liquid is a hydrocarbon with a refractive index of 1·13.
Topaz's crystal habit takes many forms. It can display a range of slender and long crystals to bulky and short. There can also be variation in the terminations displaying blunt, pyramidal, chisel, or wedge-shaped terminations. The perfect cleavage {001} in topaz breaks no Si-O bonds within its structure and only breaks Al-O and Al-F bonds. This cleavage is diagnostic for this mineral. The 2V optical angle in topaz can range from 48° to 69.5°. Low fluorine content yields a smaller angle and high fluorine content yields a larger angle.
A variety of impurities and treatments may make topaz wine red, pale gray, reddish-orange, pale green, or pink (rare), and opaque to translucent/transparent. The pink and red varieties come from chromium replacing aluminium in its crystalline structure. Imperial topaz is yellow, pink (rare, if natural), or pink-orange. Brazilian imperial topaz can often have a bright yellow to deep golden brown hue, sometimes even violet. Many brown or pale topazes are treated to make them bright yellow, gold, pink, or violet colored. Some imperial topaz stones can fade from exposure to sunlight for an extended period of time. Naturally occurring blue topaz is quite rare. Typically, colorless, gray, or pale yellow and blue material is heat treated and irradiated to produce a more desired darker blue. Mystic topaz is a colorless topaz that has been artificially coated via a vapor deposition process giving it a rainbow effect on its surface.
Although very hard, topaz must be treated with greater care than some other minerals of similar hardness (such as corundum) because of a weakness of chemical bonding of the stone's ionic components along one or another axial plane (whereas diamonds, for example, are composed of carbon atoms bonded to each other with equal strength along all of its planes). This gives topaz a tendency to break along such a cleavage plane if struck with sufficient force.
Topaz has a relatively low index of refraction for a gemstone, and so stones with large facets or tables do not sparkle as readily as stones cut from minerals with higher refractive indices, though quality colorless topaz sparkles and shows more "life" than similarly cut quartz. When given a typical "brilliant" cut, topaz may either show a sparkling table facet surrounded by dead-looking crown facets or a ring of sparkling crown facets with a dull well-like table. It also takes an exceptionally fine polish, and can sometimes be distinguished from citrine by its slippery feel alone (quartz cannot be polished to this level of smoothness).
Another method of distinguishing topaz from quartz is by placing the unset stone in a solution of bromoform or methylene iodide. Quartz will invariably float in these solutions, whereas topaz will sink.
Mining for topaz can cause some environmental concerns mostly associated with larger-scale operations. The introduction of a large open pit mine into an environment leads to modification of the land around it to make it accessible to workers. After use of such mines is over, they are often refilled with loose sediments left over from the mining process. These loose sediments can be washed away to other areas, cutting off water features, destroying farmland, and creating a threat of Landslide. The pollution produced by mining can impact the environment around it and damage its health. Deforestation undergone to create the mine, along with the machinery used during the mining process, adds Greenhouse gas to the atmosphere. Deforestation also removes habitats and biodiversity from a large area of natural space. These disruptions to the ecosystem can be challenging to wildlife and local populations. Water, also a large component of mining operations, is drawn away from neighboring communities to create a lack of water. Tailings leftover from the mining process can leach contaminants into nearby water systems and can contaminate the drinking water of local communities.
Some ways humans can be impacted by gem mining is through danger in mines and inadequate compensation. Accidents such as collapsing mines and machinery malfunctioning can put human life in danger. Those working in the mines can also be exposed to harmful chemicals and heavy metals that can impact their health. For income, there can be an unequal dispersal of the funds made from gem mining between land owners, laborers, and the operators of the mine. In illegal mining operations, there can be more money given to miners, however, these operations have fewer regulations and more dangerous environments.
Localities and occurrence
Mining
See also
External links
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