Topaz

Last updated

Topaz
Topaze, quartz fume 1.jpg
Topaz crystal on white matrix
General
Category Nesosilicate minerals
Formula
(repeating unit)		Al2SiO4(F,OH)2
IMA symbol Tpz [1]
Strunz classification 9.AF.35
Crystal system Orthorhombic
Crystal class Dipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
Space group Pbnm
Unit cell a = 4.65  Å, b = 8.8 Å,
c = 8.4 Å; Z = 4
Identification
ColorColorless (if there are no impurities), white, blue, brown, orange, gray, yellow, yellowish brown, green, pink, reddish pink or even red
Crystal habit Prismatic crystal
Twinning Rarely on [111] [2]
Cleavage [001] Perfect
Fracture Subconchoidal to uneven
Mohs scale hardness8 (defining mineral)
Luster Vitreous
Streak White
Diaphaneity Transparent
Specific gravity 3.49–3.57
Optical propertiesBiaxial (+)
Refractive index nα = 1.606–1.629
nβ = 1.609–1.631
nγ = 1.616–1.638
Birefringence δ = 0.010
Pleochroism Weak in thick sections X = yellow; Y = yellow, violet, reddish; Z = violet, bluish, yellow, pink
Ultraviolet fluorescence Short UV=golden yellow; Long UV=cream
References [3] [4] [5] [6]

Topaz is a silicate mineral made of aluminum and fluorine with the chemical formula Al 2 Si O 4(F, OH)2. 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. [7] Topaz is often treated with heat or radiation to make it a deep blue, reddish-orange, pale green, pink, or purple. [8]

Contents

Topaz is a nesosilicate mineral, and more specifically, an aluminosilicate mineral. [9] 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. [10]

It occurs in many places in the world. Some of the most popular places where topaz is sourced are Brazil and Russia. [7] Topaz is often mined in open pit or alluvial settings. [11]

Etymology

The word "topaz" is usually believed to be derived (via Old French: Topace and Latin: Topazius) from the Greek Τοπάζιος (Topázios) or Τοπάζιον (Topázion), [12] from Τοπαζος. This is the ancient name of St. John's Island in the Red Sea which was difficult to find and from which a yellow stone (now believed to be chrysolite: yellowish olivine) was mined in ancient times. The name topaz was first applied to the mineral now known by that name in 1737. [13] Ancient Sri Lanka (Tamraparni) exported topazes to Greece and ancient Egypt, which led to the etymologically related names of the island by Alexander Polyhistor (Topazius) and the early Egyptians (Topapwene) – "land of the Topaz". [14] [15] Pliny said that Topazos is a legendary island in the Red Sea and the mineral "topaz" was first mined there. Alternatively, the word topaz may be related to the Sanskrit word तपस् "tapas", meaning "heat" or "fire". [12]

History

Nicols, the author of one of the first systematic treatises on minerals and gemstones, dedicated two chapters to the topic in 1652. [16] In the Middle Ages, the name topaz was used to refer to any yellow gemstone, but in modern times it denotes only the silicate described above.

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 topazi[os], which referred to a yellow stone that was not topaz, but probably chrysolite (chrysoberyl or peridot), topaz is likely not meant here. [17]

An English superstition also held that topaz cured lunacy. [18] The ancient Romans believed that topaz provided protection from danger while traveling. [19] During the Middle Ages, it was believed that attaching the topaz to the left arm protected the owner from any curse and warded off the evil eye. It was also believed that wearing topaz increased body heat, which would enable people to relieve a cold or fever. [20] In Europe during the Middle Ages, topaz was believed to enhance mental powers. [21] In India, people believed topaz granted beauty, intelligence, and longevity when worn over the heart. [22]

Gemstone

Topaz is a gemstone. In cut and polished form, it is used to make jewelry or other adornments. Lower quality topaz is commonly used as an abrasive material due to its hardness and it is used to produce refractory materials for high temperature environments. [7] Topaz can be used as a flux in steel production. [23] Using topaz as a refectory material does have some health and environmental concerns due to the production of fluorine as a byproduct of calcining topaz.

Topaz is a part of the second rank of gemstones, or semiprecious stones, accompanying aquamarine, morganite, and tourmaline. [7] 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. [24] Blue topaz is the state gemstone of the US state of Texas. [25] The 4th wedding anniversary gem is blue topaz and the 23rd is imperial topaz. [22]

Synthetic topaz can be produced using a method that includes the thermal hydrolysis of SiO2 and AlF3. [26] When these compounds are heated to temperatures of 750° to 850 °C topaz is formed. Another method uses a combination of amorphous Al2O3, Na2SiF6, and water which is heated to a temperature of 500 °C, put under a pressure of 4000 bars, and left for 9 days. [26]

To care for a topaz gemstone, it is best to avoid ultrasonic cleaners or steam as this could produce small fractures within the crystal. [22] 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. [27] If the seller cannot produce information about the locality and mine that the topaz was collected from, it is likely that it was collected unethically.

Mineralogy

Topaz's crystal structure using polyhedrons showcasing the aluminum octahedron (grey), silica tetrahedron (blue), oxygen (red), and fluorine (green). Topaz.GIF
Topaz's crystal structure using polyhedrons showcasing the aluminum octahedron (grey), silica tetrahedron (blue), oxygen (red), and fluorine (green).

Topaz is an accessory mineral to felsic igneous, sedimentary, and hydrothermally altered rocks. [28]

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. [28] 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. [29]

On occasion, cavities can be found within topaz and they are filled with a liquid called brewsterlinite. [26] Brewsterlinite was discovered by David Brewster upon heating a sample of topaz. [30] 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. [26]

Topaz's crystal habit takes many forms. It can display a range of slender and long crystals to bulky and short. [29] 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. [31] This cleavage is diagnostic for this mineral. The 2V optical angle in topaz can range from 48° to 69.5°. [29] Low fluorine content yields a smaller angle and high fluorine content yields a larger angle.

Characteristics

Blue topaz crystal Topaz-k-182a.jpg
Blue topaz crystal

Topaz in its natural state is colorless, often with a greyish cast. It also occurs as a golden brown to yellow color which makes it sometimes confused with citrine, a less valuable gemstone. [32] The specific gravity of all shades of topaz, however, means that it is considerably heavier than citrine (about 25% per volume) and this difference in weight can be used to distinguish two stones of equal volume. Also, if the volume of a given stone can be determined, its weight if it were topaz can be established and then checked with a sensitive scale. Likewise, glass stones are also much lighter than equally sized topaz.

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. [33]

Large topaz gemstone and small irradiated topaz fragment on display at the Smithsonian Museum of Natural History. Topaz with irradiated fragment - Smithsonian Museum of Natural History - 2012-05-17.jpg
Large topaz gemstone and small irradiated topaz fragment on display at the Smithsonian Museum of Natural History.

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. [34] [35] 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. [35] Mystic topaz is a colorless topaz that has been artificially coated via a vapor deposition process giving it a rainbow effect on its surface. [36]

Sherry-colored topaz from Utah, USA Topaz-k312b.jpg
Sherry-colored topaz from Utah, USA

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 atomic bonding of the stone's molecules 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. [37]

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. [38] 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). [39]

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. [39]

Localities and occurrence

Main topaz producing countries Topaze gisements.jpg
Main topaz producing countries

Topaz is commonly associated with silicic igneous rocks of the granite and rhyolite type. It typically crystallizes in granitic pegmatites [7] or in vapor cavities in rhyolite lava flows including those at Topaz Mountain in western Utah and Chivinar in South America. It can be found with fluorite and cassiterite in various areas including the Ural and Ilmensky mountains of Russia, Afghanistan, Sri Lanka, the Czech Republic, Germany, Norway, Pakistan, Italy, Sweden, Japan, Brazil, Mexico; Flinders Island, Australia; Nigeria and the United States. Topaz was found around the time of the 1700s in a pegmatite formation within the central Urals Mountains in Russia. [7]

Topaz varieties found in Pakistan. Topaz from Pakistan.jpg
Topaz varieties found in Pakistan.

Brazil is one of the largest producers of topaz, [40] some clear topaz crystals from Brazilian pegmatites can reach boulder size and weigh hundreds of pounds. The Topaz of Aurangzeb, observed by Jean Baptiste Tavernier weighed 157.75 carats (31.550 g). [41] The American Golden Topaz, a more recent gem, weighed 22,892.5 carats (4,578.50 g). Large, vivid blue topaz specimens from the St. Anns mine in Zimbabwe were found in the late 1980s. [42] Colorless and light-blue varieties of topaz are found in Precambrian granite in Mason County, Texas [43] within the Llano Uplift. There is no commercial mining of topaz in that area. [44] It is possible to synthesize topaz. [45]

Mining

Large-scale topaz mining typically uses open pit and underground mining to extract the gem. [46] The waste material is discarded using large machines to transport it away while the valuable ore is washed and sorted to recover the topaz gems. In smaller-scale mines, dry sieving is used in alluvial environments by shoveling the material into sieves to separate the gems from unwanted dust and debris. [46] The topaz can then be selected by hand from the remaining material. Mined topaz is then sent to be processed for use in jewelry by polishing the gem and treating it to achieve the desired color. [46]

Mining for topaz can cause some environmental concerns mostly associated with larger-scale operations. [11] 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. [47] These loose sediments can be washed away to other areas, cutting off water features, destroying farmland, and creating a threat of landslides. The pollution produced by mining can impact the environment around it and damage its health. [47] Deforestation undergone to create the mine, along with the machinery used during the mining process, adds greenhouse gasses 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. [11] Tailings leftover from the mining process can leach contaminants into nearby water systems and can contaminate the drinking water of local communities. [47]

Some ways humans can be impacted by gem mining is through danger in mines and inadequate compensation. [47] 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. [47]

See also

Related Research Articles

<span class="mw-page-title-main">Amblygonite</span>

Amblygonite is a fluorophosphate mineral, (Li,Na)AlPO4(F,OH), composed of lithium, sodium, aluminium, phosphate, fluoride and hydroxide. The mineral occurs in pegmatite deposits and is easily mistaken for albite and other feldspars. Its density, cleavage and flame test for lithium are diagnostic. Amblygonite forms a series with montebrasite, the low fluorine endmember. Geologic occurrence is in granite pegmatites, high-temperature tin veins, and greisens. Amblygonite occurs with spodumene, apatite, lepidolite, tourmaline, and other lithium-bearing minerals in pegmatite veins. It contains about 10% lithium, and has been utilized as a source of lithium. The chief commercial sources have historically been the deposits of California and France.

<span class="mw-page-title-main">Beryl</span> Gemstone: beryllium aluminium silicate

Beryl ( BERR-əl) is a mineral composed of beryllium aluminium silicate with the chemical formula Be3Al2Si6O18. Well-known varieties of beryl include emerald and aquamarine. Naturally occurring hexagonal crystals of beryl can be up to several meters in size, but terminated crystals are relatively rare. Pure beryl is colorless, but it is frequently tinted by impurities; possible colors are green, blue, yellow, pink, and red (the rarest). It is an ore source of beryllium.

<span class="mw-page-title-main">Gemstone</span> Piece of mineral crystal used to make jewelry

A gemstone is a piece of mineral crystal which, when cut or polished, is used to make jewelry or other adornments. Certain rocks and occasionally organic materials that are not minerals may also be used for jewelry and are therefore often considered to be gemstones as well. Most gemstones are hard, but some softer minerals such as brazilianite may be used in jewelry because of their color or luster or other physical properties that have aesthetic value. However, generally speaking, soft minerals are not typically used as gemstones by virtue of their brittleness and lack of durability.

<span class="mw-page-title-main">Quartz</span> Mineral made of silicon and oxygen

Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon–oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is, therefore, classified structurally as a framework silicate mineral and compositionally as an oxide mineral. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar.

<span class="mw-page-title-main">Tourmaline</span> Cyclosilicate mineral group

Tourmaline is a crystalline silicate mineral group in which boron is compounded with elements such as aluminium, iron, magnesium, sodium, lithium, or potassium. This gemstone comes in a wide variety of colors.

<span class="mw-page-title-main">Fluorite</span> Mineral form of calcium fluoride

Fluorite (also called fluorspar) is the mineral form of calcium fluoride, CaF2. It belongs to the halide minerals. It crystallizes in isometric cubic habit, although octahedral and more complex isometric forms are not uncommon.

<span class="mw-page-title-main">Chrysoberyl</span> Mineral or gemstone of beryllium aluminate

The mineral or gemstone chrysoberyl is an aluminate of beryllium with the formula BeAl2O4. The name chrysoberyl is derived from the Greek words χρυσός chrysos and βήρυλλος beryllos, meaning "a gold-white spar". Despite the similarity of their names, chrysoberyl and beryl are two completely different gemstones, although they both contain beryllium. Chrysoberyl is the third-hardest frequently encountered natural gemstone and lies at 8.5 on the Mohs scale of mineral hardness, between corundum (9) and topaz (8).

<span class="mw-page-title-main">Zircon</span> Zirconium silicate mineral

Zircon is a mineral belonging to the group of nesosilicates and is a source of the metal zirconium. Its chemical name is zirconium(IV) silicate, and its corresponding chemical formula is ZrSiO4. An empirical formula showing some of the range of substitution in zircon is (Zr1–y, REEy)(SiO4)1–x(OH)4x–y. Zircon precipitates from silicate melts and has relatively high concentrations of high field strength incompatible elements. For example, hafnium is almost always present in quantities ranging from 1 to 4%. The crystal structure of zircon is tetragonal crystal system. The natural color of zircon varies between colorless, yellow-golden, red, brown, blue, and green.

<span class="mw-page-title-main">Cubic zirconia</span> The cubic crystalline form of zirconium dioxide

Cubic zirconia (abbreviated CZ) is the cubic crystalline form of zirconium dioxide (ZrO2). The synthesized material is hard and usually colorless, but may be made in a variety of different colors. It should not be confused with zircon, which is a zirconium silicate (ZrSiO4). It is sometimes erroneously called cubic zirconium.

<span class="mw-page-title-main">Pleochroism</span> Optical phenomenon

Pleochroism is an optical phenomenon in which a substance has different colors when observed at different angles, especially with polarized light.

<span class="mw-page-title-main">Spodumene</span> Pyroxene, inosilicate mineral rich in lithium

Spodumene is a pyroxene mineral consisting of lithium aluminium inosilicate, LiAl(SiO3)2, and is a commercially important source of lithium. It occurs as colorless to yellowish, purplish, or lilac kunzite (see below), yellowish-green or emerald-green hiddenite, prismatic crystals, often of great size. Single crystals of 14.3 m (47 ft) in size are reported from the Black Hills of South Dakota, United States.

<span class="mw-page-title-main">Rhodochrosite</span> Mineral of manganese carbonate

Rhodochrosite is a manganese carbonate mineral with chemical composition MnCO3. In its pure form (rare), it is typically a rose-red colour, but it can also be shades of pink to pale brown. It streaks white, and its Mohs hardness varies between 3.5 and 4.5. Its specific gravity is between 3.45 and 3.6. The crystal system of rhodochrosite is trigonal, with a structure and cleavage in the carbonate rhombohedral system. The carbonate ions (CO2−
3) are arranged in a triangular planar configuration, and the manganese ions (Mn2+) are surrounded by six oxygen ions in an octahedral arrangement. The MnO6 octahedra and CO3 triangles are linked together to form a three-dimensional structure. Crystal twinning is often present. It can be confused with the manganese silicate rhodonite, but is distinctly softer. Rhodochrosite is formed by the oxidation of manganese ore, and is found in South Africa, China, and the Americas. It is one of the national symbols of Argentina and the state of Colorado.

<span class="mw-page-title-main">Euclase</span>

Euclase is a beryllium aluminium hydroxide silicate mineral (BeAlSiO4(OH)). It crystallizes in the monoclinic crystal system and is typically massive to fibrous as well as in slender prismatic crystals. It is related to beryl (Be3Al2Si6O18) and other beryllium minerals. It is a product of the decomposition of beryl in pegmatites.

<span class="mw-page-title-main">Brazilianite</span> Yellow-green phosphate mineral

Brazilianite, whose name derives from its country of origin, Brazil, is a typically yellow-green phosphate mineral, most commonly found in phosphate-rich pegmatites.

<span class="mw-page-title-main">Phenakite</span>

Phenakite or phenacite is a fairly rare nesosilicate mineral consisting of beryllium orthosilicate, Be2SiO4. Occasionally used as a gemstone, phenakite occurs as isolated crystals, which are rhombohedral with parallel-faced hemihedrism, and are either lenticular or prismatic in habit: the lenticular habit is determined by the development of faces of several obtuse rhombohedra and the absence of prism faces. There is no cleavage, and the fracture is conchoidal. The Mohs hardness is high, being 7.5–8; the specific gravity is 2.96. The crystals are sometimes perfectly colorless and transparent, but more often they are greyish or yellowish and only translucent; occasionally they are pale rose-red. In general appearance the mineral is not unlike quartz, for which indeed it has been mistaken. Its name comes from Ancient Greek: φέναξ, romanized: phénax, meaning "deceiver" due to its close visual similarity to quartz, named by Nils Gustaf Nordenskiöld in 1833.

<span class="mw-page-title-main">Diamond simulant</span> Diamond-like object which is not a diamond

A diamond simulant, diamond imitation or imitation diamond is an object or material with gemological characteristics similar to those of a diamond. Simulants are distinct from synthetic diamonds, which are actual diamonds exhibiting the same material properties as natural diamonds. Enhanced diamonds are also excluded from this definition. A diamond simulant may be artificial, natural, or in some cases a combination thereof. While their material properties depart markedly from those of diamond, simulants have certain desired characteristics—such as dispersion and hardness—which lend themselves to imitation. Trained gemologists with appropriate equipment are able to distinguish natural and synthetic diamonds from all diamond simulants, primarily by visual inspection.

<span class="mw-page-title-main">Danburite</span> Tectosilicate mineral

Danburite is a calcium boron silicate mineral with a chemical formula of CaB2(SiO4)2.

<span class="mw-page-title-main">Jeremejevite</span> Aluminium borate mineral with variable fluoride and hydroxide ions

Jeremejevite is an aluminium borate mineral with variable fluoride and hydroxide ions. Its chemical formula is Al6B5O15(F,OH)3. It is considered as one of the rarest, thus one of the most expensive stones. For nearly a century, it was considered as one of the rarest gemstones in the world.

<span class="mw-page-title-main">Chiolite</span> Dipyramidal mineral

Chiolite is a tetragonal-ditetragonal dipyramidal mineral, composed of sodium, fluorine, and aluminium. The name originates from the combination of the Greek words for snow (χιώυ) and stone (λίθος). It is an allusion to its similarity and appearance to cryolite. Chiolite is an IMA approved mineral that has been grandfathered, meaning the name chiolite is believed to refer to a valid species to this day. Synonyms of chiolite are arksudite, arksutite, chodneffite, chodnewite and nipholith. It was first discovered in the Ilmen mountains, Russia, in 1846. Chiolite has been a valid species from the same year of its discovery.

<span class="mw-page-title-main">Aquamarine (gem)</span> Variety of beryl

Aquamarine is a pale-blue to light-green variety of the beryl family, with its name relating to water and sea. The color of aquamarine can be changed by heat, with a goal to enhance its physical appearance. It is the birth stone of March.

References

  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. ↑ Nesse, William D. (2000). Introduction to mineralogy. New York: Oxford University Press. p. 313. ISBN   9780195106916.
  3. ↑ Hurlbut, Cornelius S.; Klein, Cornelis (1985). Manual of Mineralogy (20 ed.). Wiley. ISBN   0-471-80580-7.
  4. ↑ Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C., eds. (1995). "Topaz" (PDF). Handbook of Mineralogy. Vol. II (Silica, Silicates). Chantilly, VA, US: Mineralogical Society of America. ISBN   978-0-9622097-1-0 . Retrieved December 5, 2011.
  5. ↑ Topaz. Mindat.org. Retrieved on 2011-10-29.
  6. ↑ Topaz. Webmineral.com. Retrieved on 2011-10-29.
  7. 1 2 3 4 5 6 Menzies, Michael A. (2023-12-08). "Connoisseur's Choice: Topaz from Granite Pegmatites: Limoeiro Mine, Virgem da Lapa, Araçuaí Pegmatite District, Minas Gerais, Brazil". Rocks & Minerals. 99 (1): 36–55. doi:10.1080/00357529.2023.2253100. ISSN   0035-7529. S2CID   266145193.
  8. ↑ "Topaz Value, Price, and Jewelry Information". International Gem Society. Retrieved 2021-11-16.
  9. ↑ Tennakoon, Sumudu; Peng, Ye; Mookherjee, Mainak; Speziale, Sergio; Manthilake, Geeth; Besara, Tiglet; Andreu, Luis; Rivera, Fernando (2018-01-22). "Single crystal elasticity of natural topaz at high-temperatures". Scientific Reports. 8 (1): 1372. Bibcode:2018NatSR...8.1372T. doi:10.1038/s41598-017-17856-3. ISSN   2045-2322. PMC   5778148 . PMID   29358663.
  10. ↑ Handbook of mineralogy. 2,2: Silica, Silicates: Pt. 2. Tucson, Ariz: Mineral Data Publ. 1995. ISBN   978-0-9622097-1-0.
  11. 1 2 3 "Topaz Mining: Balancing Resource Extraction and Sustainability". www.brilliyond.com. Retrieved 2024-03-20.
  12. 1 2 Harper, Douglas. "topaz". Online Etymology Dictionary .
  13. ↑ Hurlbut & Klein 1985.
  14. ↑ Suckling, Horatio John (1876). Ceylon: A General Description of the Island, Historical, Physical, Statistical. Containing the Most Recent Information. Chapman & Hall. p.  10 . Retrieved 28 June 2019. topaz taprobane.
  15. ↑ "Astrological Magazine". Astrological Magazine. 56 (1–6): 75. 1967. Retrieved 28 June 2019.
  16. ↑ A Lapidary or History of Gemstones, University of Cambridge, 1652.
  17. ↑ Farrington, Oliver (1903) Gems and Gem Minerals. Chicago. p. 119.
  18. ↑ 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.
  19. ↑ Webster, R. (2012). The encyclopedia of superstitions. Llewellyn Worldwide. p. 256. ISBN   9780738725611.
  20. ↑ Webster 2012, p. 260.
  21. ↑ Simmons, Robert (2005). The book of stones : who they are & what they teach. East Montpelier, VT: Heaven and Earth Pub. p. 403. ISBN   978-0962191039.
  22. 1 2 3 "November Birthstone". Gemological Institute of America. Retrieved 2024-02-18.
  23. ↑ "Topaz" (PDF). resourcesregulator.nsw.gov. NSW Department of Primary Industries. Retrieved March 20, 2024.
  24. ↑ "Utah State gem – Topaz". Pioneer.utah.gov. 16 June 2010. Archived from the original on 14 November 2012. Retrieved 29 October 2011.
  25. ↑ "Texas state gem – Blue Topaz. State gemstone cut – Lone Star cut". state.tx.us. Archived from the original on 2009-03-12.
  26. 1 2 3 4 Deer, W. A.; Howie, Robert A.; Zussman, Jack (1989). An introduction to the rock-forming minerals (16. impr ed.). London: Longman [u.a.] ISBN   978-0-582-44210-8.
  27. ↑ Breakfast, Gem. "The Most Comprehensive Guide to Buying Ethical Gemstones". Gem Breakfast. Retrieved 2024-04-10.
  28. 1 2 Nesse, William D. (2017). Introduction to mineralogy (3rd ed.). New York Oxford: Oxford University Press. ISBN   978-0-19-061835-3.
  29. 1 2 3 Wise, Michael A. (1995–2002). "Topaz: A Mineralogical Review". Rocks & Minerals. 70 (1): 16–25. doi:10.1080/00357529.1995.9926593. ISSN   0035-7529.
  30. ↑ "Topaz"  . Encyclopædia Britannica . Vol. XXIII (9th ed.). 1888. p. 446.
  31. ↑ Ribbe, P. H.; Gibbs, G. V. (1971). The crystal structure of topaz and its relation to physical properties. The American mineralogist. Vol. 56. Washington, DC: Mineralogical Society of America. pp. 24–30. ISSN   0003-004X.
  32. ↑ Hurrell, Karen; Johnson, Mary L. (15 December 2016). Gemstones: A Complete Color Reference for Precious and Semiprecious Stones of the World. Book Sales. p. 169. ISBN   978-0-7858-3498-4.
  33. ↑ Gübelin, Edward; Graziani, Giorgio; Kazmi, A. H. (1986-10-01). "Pink Topaz from Pakistan". Gems & Gemology. 22 (3): 140–151. doi:10.5741/GEMS.22.3.140. ISSN   0016-626X.
  34. ↑ "Imperial topaz". nhm.org. Natural History Museum of Los Angeles County. Archived from the original on 13 May 2009.
  35. 1 2 "Gemstones & Gemology – Topaz". academic.emporia.edu. Emporia State University.
  36. ↑ "Mystic topaz, consumer information". Farlang.com. 30 October 2008. Retrieved 29 October 2011.
  37. ↑ Newman, Renee (7 January 2015). Gem & Jewelry Pocket Guide: A traveler's guide to buying diamonds, colored gems, pearls, gold and platinum jewelry. BookBaby. p. 104. ISBN   978-0-929975-49-8.
  38. ↑ Dake, H. (16 April 2013). The Art of Gem Cutting – including cabochons, faceting, Sspheres, tumbling, and special techniques. Read Books Limited. p. 105. ISBN   978-1-4474-8480-6.
  39. 1 2 B. Anderson (2011). Gem Testing. Read Books.
  40. ↑ "Topaz Guide". Ayana Jewellery. Archived from the original on November 24, 2016. Retrieved November 23, 2016.
  41. ↑ Famous and Notheworthy Topazes Rao Bahadur, A Handbook of Precious Stones, Geological Survey of India
  42. ↑ "Topaz (Blue)". Cape Minerals. Archived from the original on 8 February 2017. Retrieved 7 February 2017.
  43. ↑ Handbook of Texas Online – Mineral Resources and Mining. Tshaonline.org. Retrieved on 2011-10-29.
  44. ↑ Mason, Texas Chamber of Commerce Web site
  45. ↑ Rosenberg, Philip E. (1972). "Compositional variations in synthetic topaz" (PDF). American Mineralogist. 57: 169–187.
  46. 1 2 3 Australia, Geoscience (2020-02-07). "Topaz". Geoscience Australia. Retrieved 2024-03-20.
  47. 1 2 3 4 5 "7 Negative Environmental Impacts Of The Gem Mining Industry". BIRON® Gems. Retrieved 2024-04-10.
This page is based on this Wikipedia article
Text is available under the CC BY-SA 4.0 license; additional terms may apply.
Images, videos and audio are available under their respective licenses.