domingo, 21 de julho de 2013

Lapis lazuli

Lapis lazuli


Lapis lazuli
Lapis lazuli block.jpg
A polished specimen of lapis lazuli.
General
Category Rock
Formula
(repeating unit)
mixture of minerals
Identification
Color Blue, mottled with white calcite and brassy pyrite
Crystal habit Compact, massive
Crystal system None, as lapis is a rock. Lazurite, the main constituent, frequently occurs as dodecahedra
Cleavage None
Fracture Uneven-Conchoidal
Mohs scale hardness 5–5.5
Luster dull
Streak light blue
Specific gravity 2.7–2.9
Refractive index 1.5
Other characteristics The variations in composition cause a wide variation in the above values.
Lapis lazuli specimen (rough), Afghanistan
Lapis lazuli (/ˈlæpɪs ˈlæzjʉl/ or /ˈlæzjʉli/ LAP-iss LAZ-zew-ly/lee,[1]) (sometimes abbreviated to lapis) is a relatively rare semi-precious stone that has been prized since antiquity for its intense blue color.
Lapis lazuli was being mined in the Badakhshan province of Afghanistan as early as the 3rd millennium BC,[2] and there are sources that are found as far east as in the region around Lake Baikal in Siberia[citation needed]. Trade in the stone is ancient enough for lapis jewelry to have been found at Predynastic Egyptian and ancient Sumerian sites, and as lapis beads at neolithic burials in Mehrgarh, the Caucasus, and even as far from Afghanistan as Mauritania.[3]

Contents

Description

Lapis lazuli is a rock, largely formed from the mineral lazurite.[4]
The main component of lapis lazuli is lazurite (25% to 40%), a feldspathoid silicate mineral with the formula (Na,Ca)8(AlSiO4)6(S,SO4,Cl)1-2.[5] Most lapis lazuli also contains calcite (white), sodalite (blue), and pyrite (metallic yellow). Other possible constituents: augite; diopside; enstatite; mica; hauynite; hornblende, and nosean. Some lapis lazuli contains trace amounts of the sulfur-rich löllingite variety geyerite.
Lapis lazuli usually occurs in crystalline marble as a result of contact metamorphism.

Etymology

Lapis is the Latin word for "stone" and lazuli is the genitive form of the Medieval Latin lazulum, which is taken from the Arabic لازورد lāzaward, itself from the Persian لاژورد lāžaward, the name of a place where lapis lazuli was mined.[6][7] Taken as a whole, lapis lazuli means "stone of Lāzhward".
The name of the place came to be associated with the stone mined there and, eventually, with its color. The French azur, the Italian azzurro, the Polish lazur, Romanian azur and azuriu, and the Portuguese and Spanish azul, Hungarian azúr are cognates.

Sources

Lapis lazuli is found in limestone in the Kokcha River valley of Badakhshan province in northeastern Afghanistan, where the Sar-e-Sang mine deposits have been worked for more than 6,000 years.[8] Afghanistan was the source of lapis for the ancient Egyptian and Mesopotamian civilizations, as well as the later Greeks and Romans. During the height of the Indus valley civilization about 2000 BC, the Harappan colony now known as Shortugai was established near the lapis mines.[3]
In addition to the Afghan deposits, lapis has been extracted for many years in the Andes (near Ovalle, Chile), the Lake Baikal region of Russia[citation needed]; Siberia; Angola; Argentina; Burma; Pakistan; Canada; India; and in the USA in California and Colorado.

Alternatives

Lapis lazuli is commercially "synthesized" (actually simulated) by the Gilson process, using artificial ultramarine and hydrous zinc phosphates.[9] It may be substituted by spinel or sodalite, or by dyed jasper or howlite.[10]

Uses

Lapis takes an excellent polish and can be made into jewelry, carvings, boxes, mosaics, ornaments, and vases. It was also ground and processed to make the pigment ultramarine for tempera paint and, more rarely, oil paint. Its usage as a pigment in oil paint ended in the early 19th century when a chemically identical synthetic variety, often called French ultramarine, became available.

Historical usage

In ancient Egypt, lapis lazuli was a favorite stone for amulets and ornaments such as scarabs; it was also used in ancient Mesopotamia by the Sumerians, Akkadians, Assyrians, and Babylonians for seals and jewelry. In the Epic of Gilgamesh; the oldest known story in human history, lapis lazuli is referenced several times. Lapis jewelry has been found at excavations of the Predynastic Egyptian site Naqada (3300–3100 BC), and powdered lapis was used as eyeshadow by Cleopatra.[3] In ancient Mesopotamia, lapis artifacts can be found in great abundance, with many notable examples having been excavated at the 25th-century BC Statue of Ebih-Il, discovered in ancient Mari in Syria, uses lapis lazuli inlays that were imported from as far east as Afghanistan.[11]
In ancient times, lapis lazuli was known as sapphire,[12] which is the name that is used today for the blue corundum variety sapphire. It has also been used in the Taj Mahal in India.

Color

The intense blue color is due to the presence of the S3- radical anion in the crystal.[13] An electronic excitation of one electron from the highest doubly filled molecular orbital (No. 24) into the lowest singly occupied orbital (No. 25)[14] results in a very intense absorption line at λmax ~617 nm.

Gallery

See also

Notes

  1. ^ The New Penguin English Dictionary, 2000
  2. ^ Moorey, Peter Roger (1999). Ancient Mesopotamian Materials and Industries: the Archaeological Evidence. Eisenbrauns. pp. 86–87. ISBN 978-1-57506-042-2.
  3. ^ a b c Bowersox & Chamberlin 1995
  4. ^ Mindat entry relating to lapis lazuli
  5. ^ Mindat – Lazurite
  6. ^ Senning, Alexander (2007). "lapis lazuli (lazurite)". Elsevier's Dictionary of Chemoetymology. Amsterdam: Elsevier. p. 224. ISBN 978-0-444-52239-9.
  7. ^ Weekley, Ernest (1967). "azure". An Etymological Dictionary of Modern English. New York: Dover Publications. p. 97.
  8. ^ Oldershaw 2003
  9. ^ Read, Peter (2005). Gemmology, Elsevier, p. 185. ISBN 0-7506-6449-5
  10. ^ Lapis lazuli, Gemstone Buzz.
  11. ^ Claire, Iselin. "Ebih-Il, the Superintendent of Mari". Musée du Louvre. Retrieved 10 October 2012.
  12. ^ Schumann, Walter (2006) [2002]. "Sapphire". Gemstones of the World. trans. Annette Englander & Daniel Shea (newly revised & expanded 3rd ed.). New York: Sterling. p. 102. "In antiquity and as late as the Middle Ages, the name sapphire was understood to mean what is today described as lapis lazuli."
  13. ^ E. Boros, M. J. Earle, M. A. Gilea, A. Metlen, A.-V. Mudring, F. Rieger, A. J. Robertson, K. R. Seddon, A. A. Tomaszowska, L. Trusov and J. S. Vyle, "On the dissolution of non-metallic solid elements (sulfur, selenium, tellurium and phosphorus) in ionic liquids," Chem. Comm., 2010, 46, 716–718. doi:10.1039/b910469k
  14. ^ H. S. Rzepa, "Lapis lazuli: the Colour of Ultramarine." Accessed: 2011-03-06. (Archived by WebCite® at http://www.webcitation.org/5wyiNxh3B)

References

  • Bowersox, Gary W.; Chamberlin, Bonita E. (1995). Gemstones of Afghanistan. Tucson, AZ: Geoscience Press..
  • Oldershaw, Cally (2003). "Lapis Lazuli". Firefly Guide to Gems. Toronto: Firefly Books..

Spodumene

Spodumene


"Kunzite" redirects here. For the Sailor Moon character, see Shitennou.
Spodumene
Spodumene-usa59abg.jpg
Walnut Hill Pegmatite Prospect, Huntington, Hampshire County, Massachusetts, USA (Size: 14.2 x 9.2 x 3.0 cm)
General
Category Silicate mineral, pyroxene
Formula
(repeating unit)
lithium aluminium silicate, LiAl(SiO3)2
Crystal symmetry Monoclinic 2/m
Unit cell a = 9.46 Å, b = 8.39 Å, c = 5.22 Å; β = 110.17°; Z = 4
Identification
Color Highly variable: white, colorless, gray, pink, lilac, violet, yellow and green, may be bicolored; emerald green - hiddenite; lilac - kunzite
Crystal habit prismatic, generally flattened and elongated, striated parallel to {100}, commonly massive
Crystal system Monoclinic; 2/m
Twinning Common on {100}
Cleavage Perfect prismatic, two directions {110} ∧ {110} at 87°
Fracture Uneven to subconchoidal
Tenacity Brittle
Mohs scale hardness 6.5–7
Luster Vitreous, pearly on cleavage
Streak white
Specific gravity 3.03–3.23
Optical properties Biaxial (+)
Refractive index nα = 1.648–1.661 nβ = 1.655–1.670 nγ = 1.662–1.679
Birefringence δ = 0.014–0.018
Pleochroism Strong in kunzite: α-purple, γ-colorless; hiddenite: α-green, γ-colorless
2V angle 54° to 69°
Fusibility 3.5
Solubility insoluble
Other characteristics Tenebrescence, chatoyancy, kunzite often fluorescent under UV[citation needed]
References [1][2][3][4]
Spodumene is a pyroxene mineral consisting of lithium aluminium inosilicate, LiAl(SiO3)2, and is a 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.[5]
The normal low-temperature form α-spodumene is in the monoclinic system whereas the high-temperature β-spodumene crystallizes in the tetragonal system. The normal α-spodumene converts to β-spodumene at temperatures above 900 °C.[4] Crystals are typically heavily striated parallel to the principal axis. Crystal faces are often etched and pitted with triangular markings.

Contents

Discovery and occurrence

Spodumene was first described in 1800 for an occurrence in the type locality in Utö, Södermanland, Sweden. The name is derived from the Greek spodumenos (σποδυμενος), meaning "burnt to ashes," owing to the opaque, ash-grey appearance of material refined for use in industry.[1]
Spodumene occurs in lithium-rich granite pegmatites and aplites. Associated minerals include: quartz, albite, petalite, eucryptite, lepidolite and beryl.[2]
Transparent material has long been used as a gemstone with varieties kunzite and hiddenite noted for their strong pleochroism. Source localities include Afghanistan, Australia, Brazil, Madagascar, Pakistan, Québec in Canada and North Carolina, California in the USA.

Economic importance

Spodumene is an important source of lithium for use in ceramics, mobile phone and automotive batteries, medicine and as a fluxing agent. Lithium is extracted from spodumene by fusing in acid.
World production of lithium via spodumene is around 80,000 metric tonnes per annum, primarily from the Greenbushes pegmatite of Western Australia, and some Chinese and Chilean sources. The Talison mine in Greenbushes, Western Australia has an estimated reserve of 13 million tonnes.[6]
Some think that spodumene will become a less important source of lithium due to the emergence of alkaline brine lake sources in Chile, China and Argentina, which produce lithium chloride directly. Lithium chloride is converted to lithium carbonate and lithium hydroxide by reaction with sodium carbonate and calcium hydroxide respectively.
But, pegmatite-based projects benefit from being quicker to move into production than brines, which can take 18 months to 3 years, depending on evaporation rates. With pegmatites, once a mill is built, the production of lithium carbonate is only a matter of days.
Another key advantage that spodumene has over its more popular brine rivals, is the purity of the lithium carbonate it can produce. While all product used by the battery industry have to grade at least 99.5% lithium carbonate, the make up of that final 0.5% is important. If it contains higher amounts of iron, magnesium or other deleterious materials it is less attractive to end users.

Gemstone varieties

Hiddenite

Hiddenite is a pale emerald green gem variety first reported from Alexander County, North Carolina, U. S. A.
This emerald green variety of spodumene is colored by chromium, just like emeralds. Not all green spodumene is colored with chromium, which tend to have a lighter color, and therefore are not true hiddenite.

Kunzite

Kunzite is a pink to lilac colored gemstone, a variety of spodumene with the color coming from minor to trace amounts of manganese. Some (but not all) kunzite used for gemstones has been heated to enhance its color. It is also frequently irradiated to enhance the color. Many kunzites fade when exposed to sunlight.
Kunzite was discovered in 1902, and was named after George Frederick Kunz, Tiffany & Co's chief jeweler at the time, and a noted mineralogist. It has been found in Brazil, USA, Canada, CIS, Mexico, Sweden, Western Australia, Afghanistan and Pakistan.
One notable example of kunzite used in jewellery is in the Russian Palmette tiara and necklace worn by the Duchess of Gloucester.[7]

See also

Notes

  1. ^ a b Spodumene, Mindat.org
  2. ^ a b Anthony, John W., Bideaux, Richard A., Bladh, Kenneth W., and Nichols, Monte C. (1990). Handbook of Mineralogy. Mineral Data Publishing, Tucson, Arizona
  3. ^ Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., ISBN 0-471-80580-7
  4. ^ a b Deer, Howie and Zussman, Rock Forming Minerals, v. 2 Chain Silicates, Wiley, 1963 pp. 92-98
  5. ^ Robert Louis Bonewitz, 2005, Rock and Gem, London, Dorling Kindersley
  6. ^ "Spodumene". Bunbury Port Authority. February 26, 2008. Retrieved 2008-11-27.
  7. ^ State Visit from India: HRH The Duchess of Gloucester, madhattery.com

References

  • Kunz, George Frederick (1892). Gems and Precious Stones of North America. New York: The Scientific Publishing Company.
  • Palache, C., Davidson, S. C., and Goranson, E. A. (1930). "The Hiddenite deposit in Alexander County, N. Carolina". American Mineralogist Vol. 15 No. 8 p. 280
  • Webster, R. (2000). Gems: Their Sources, Descriptions and Identification (5th ed.), pp. 186–190. Great Britain: Butterworth-Heinemann.
  • The key players in Quebec lithium, “Daily News”, The Northern Miner. August 11, 2010.

Pedras de ametista são atrativos para turistas em cidade no Norte do RS

  Pedras de ametista são atrativos para turistas em cidade no Norte do RS Ametista do Sul se intitula a "capital mundial da pedra ametista". Mineração é a principal atividade econômica da cidade e atrai visitantes.
Pedra ametista - Ametista do Sul - Nossa Terra RS (Foto: Prefeitura de Ametista do Sul/Divulgação)
Do G1 RS
Com pouco mais de 7 mil habitantes, o município de Ametista do Sul leva no nome o seu principal atrativo. A cidade situada no Norte do Rio Grande do Sul , vizinha a Frederico Westphalen, se intitula “capital mundial da pedra ametista” em razão da abundância do mineral nas regiões do Médio e Alto Uruguai.
A mineração é a principal atividade econômica da cidade. Atualmente, há mais de 100 minas licenciadas para a exploração de ametistas e ágatas no município. A beleza das pedras em estado bruto ou beneficiadas para a comercialização também têm atraído um número cada vez maior de turistas para a região.
Galeria subterrânia mina Ametista do Sul RS Nossa Terra
“Temos dados na Secretaria de Turismo que mostram que cerca de 50 mil pessoas passaram por Ametista do Sul em 2012”, diz ao G1 o secretário de turismo do município, Claudimir Capra. A contribuição para a economia da cidade é valiosa, garante Capra. Visitantes acabam levando lembranças consigo. "Para divulgar Ametista, começamos a nos inserir em grandes feiras no estado, como a Expobento e Fenadoce. Sempre mostramos as nossas atrações", complementa.
Algumas minas da cidade são abertas aos turistas, que podem conhecer a atividade do garimpo e como as pedras são extraídas do interior das galerias subterrâneas. O principal passeio é oferecido pelo Ametista Parque Museu. A visita começa com um tour pelo local, onde estão expostas mais de 1,5 mil pedras procedentes de várias partes do mundo.
Segundo os administradores, o museu abriga a pedra ametista "mais valiosa do mundo" encontrada até hoje, com 2,5 toneladas de peso. Outra “joia” do local é um meteorito raro de aproximadamente 140 quilos, que, conforme pesquisadores, teria explodido dentro de uma estrela ou planeta.
Igreja Ametista do Sul RS Nossa Terra
A visita prossegue com um passeio no interior das minas subterrâneas. Ali, o visitante pode presenciar explosões preparadas pelos garimpeiros para encontrar as pedras. Em outra mina desativada, o visitante percorre um trecho de cerca de 200 metros onde estão expostas pedras belíssimas e geodos incrustados na rocha, além dos equipamentos usados pelos garimpeiros. Um guia explica tudo aos turistas.
O passeio termina com a visita a um espaço onde estão concentradas várias lojas que vendem pedras precisosas, joias e artesanatos. A diversidade dos produtos feitos com ametistas e outras pedras é grande, assim como os preços, que vão desde R$ 1 por uma simples lembrança até milhares de reais pagos por peças mais elaboradas e raras.
Por toda a cidade, a presença da pedra é marcante. Além de inúmeros lojas, há hotéis temáticos e até mesmo templos religiosos decorados com ela. Inaugurada em 2008, a Igreja São Gabriel foi revestida com 40 toneladas de pedras ametista em suas paredes. A Pia Batistmal da igreja também foi esculpida em um geodo de cerca de 500 quilos.
Pirâmide esotéria Ametista do Sul RS Nossa Terra
Uma pirâmide de vidro e com o interior revestido de ametistas também foi erguida na praça central da cidade. O local costuma atrair visitantes interessados em apreciar a beleza da estrutura ou os que acreditam nos aspectos esotéricos e espirituais da energia transmitida pelos cristais.
De dois em dois anos, Ametista do Sul também sedia uma feira de pedras, a Expopedras, com exposição de vários tipos de minerais, feira da indústria, comércio, serviços e shows, entre outras atrações. A nona edição do evento está marcada para 20 a 23 de março de 2014.
Mas se engana quem pensa que as pedras são as únicas belezas de Ametista do Sul. As paisagens bucólicas dos vinhedos da região e as belezas naturais dos arredores do Rio da Várzea ou a cascata do Rio do Mel são algumas das mais bonitas paisagens da região, apesar de ainda serem pouco conhecidas até mesmo pelos gaúchos.
Cascata do Rio do Mel Ametista do Sul RS Nossa Terra

Topaz

Topaz


Topaz
TopazUSGOV.jpg
A group of topaz crystals on matrix
General
Category Silicate mineral
Formula
(repeating unit)
Al2SiO4(F,OH)2
Strunz classification 9.AF.35
Crystal symmetry Orthorhombic dipyramidal
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
Color Colorless (if no impurities), blue, brown, orange, gray, yellow, green, pink and reddish pink
Crystal habit Prismatic crystals with faces striated parallel to long dimension; also columnar, compact, massive
Crystal system Orthorhombic
Cleavage [001] Perfect
Fracture Subconchoidal to uneven
Mohs scale hardness 8 (defining mineral)
Luster Vitreous
Streak White
Diaphaneity Transparent
Specific gravity 3.49–3.57
Optical properties Biaxial (+)
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
Other characteristics Fluorescent, short UV=golden yellow, long UV=cream
References [1][2][3][4]
Topaz is a silicate mineral of aluminium and fluorine with the chemical formula Al2SiO4(F,OH)2. Topaz crystallizes in the orthorhombic system, and its crystals are mostly prismatic terminated by pyramidal and other faces.

Contents

Color and varieties

Facet Cut Topaz Gemstones in various colors
Pure topaz is colorless and transparent but is usually tinted by impurities; typical topaz is wine, yellow, pale gray, reddish-orange, or blue brown. It can also be made white, pale green, blue, gold, pink (rare), reddish-yellow or opaque to transparent/translucent.
Orange topaz, also known as precious topaz, is the traditional November birthstone, the symbol of friendship, and the state gemstone of the US state of Utah.[5]
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 on exposure to sunlight for an extended period of time.[6][7]
Yellow topaz in stepped kite-shaped cut
Blue topaz is the state gemstone of the US state of Texas.[8] 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.[7]
Mystic topaz is colorless topaz which has been artificially coated giving it the desired rainbow effect.[9]

Localities and occurrence

Topaz Mountain, Utah
Topaz is commonly associated with silicic igneous rocks of the granite and rhyolite type. It typically crystallizes in granitic pegmatites or in vapor cavities in rhyolite lava flows like those at Topaz Mountain in western Utah. It can be found with fluorite and cassiterite in various areas including the Ural and Ilmen mountains of Russia, in Afghanistan, Sri Lanka, Czech Republic, Germany, Norway, Pakistan, Italy, Sweden, Japan, Brazil, Mexico; Flinders Island, Australia; Nigeria and the United States.
Some clear topaz crystals from Brazilian pegmatites can reach boulder size and weigh hundreds of pounds. Crystals of this size may be seen in museum collections. The Topaz of Aurangzeb, observed by Jean Baptiste Tavernier measured 157.75 carats.[10] The American Golden Topaz, a more recent gem, measured a massive 22,892.5 carats.
Colorless and light-blue varieties of topaz are found in Precambrian granite in Mason County, Texas[11] within the Llano Uplift. There is no commercial mining of topaz in that area.[12]

Etymology and historical and mythical usage

Etymology

Colorless topaz, Minas Gerais, Brazil
The name "topaz" is derived (via Old French: Topace and Latin: Topazus) from the Greek Τοπάζιος (Τοpáziοs) or Τοπάζιον (Τοpáziοn),[13] 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; topaz itself (rather than topazios) was not really known about before the classical era. Pliny said that Topazos is a legendary island in the Red Sea and the mineral "topaz" was first mined there.
The word topaz is related to the Sanskrit word तपस्"tapas" meaning "heat" or "fire",[13] and also to the Hebrew word for "orange" (the fruit): tapooz (תפוז), both of which predate the Greek word.

History

Nicols, the author of one of the first systematic treatises on minerals and gemstones, dedicated two chapters to the topic in 1652.[14] 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.

Biblical background, etymology, and analysis

Many modern English translations of the Bible, including the King James Version mention topaz in Exodus 28:17 in reference to a stone in the Hoshen: "And thou shalt set in it settings of stones, even four rows of stones: the first row shall be a sardius, a topaz, and a carbuncle (garnet): this shall be the first row."
However, because these translations as topaz all derive from the Septuagint translation topazi[os], which as mentioned above referred to a yellow stone that was not topaz, but probably chrysolite (chrysoberyl or peridot), it should be borne in mind that topaz is likely not meant here.[15] The masoretic text (the Hebrew on which most modern Protestant Bible translations of the Old Testament are based) has pitdah as the gem the stone is made from; some scholars think it is related to an Assyrian word meaning "flashed".[citation needed] More likely, pitdah is derived from Sanskrit words (पीत pit = yellow, दह् dah = burn), meaning "yellow burn" or, metaphorically, "fiery".

References

  1. ^ Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., ISBN 0-471-80580-7
  2. ^ Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W. and Nichols, Monte C., ed. (1995). "Topaz" (PDF). Handbook of Mineralogy. II (Silica, Silicates). Chantilly, VA, US: Mineralogical Society of America. ISBN 0-9622097-1-6. Retrieved December 5, 2011.
  3. ^ Topaz. Mindat.org. Retrieved on 2011-10-29.
  4. ^ Topaz. Webmineral.com. Retrieved on 2011-10-29.
  5. ^ Utah State Gem – Topaz. Pioneer.utah.gov (2010-06-16). Retrieved on 2011-10-29.
  6. ^ Imperial Topaz, Natural History Museum of Los Angeles County
  7. ^ a b Gemstones & Gemology – Topaz, Emporia State University
  8. ^ State Gem – Texas Blue Topaz. State Gemstone Cut – Lone Star Cut. state.tx.us
  9. ^ Mystic Topaz, Consumer Information. Farlang.com (2008-10-30). Retrieved on 2011-10-29.
  10. ^ Famous and Notheworthy Topazes Rao Bahadur, A Handbook of Precious Stones, Geological Survey of India
  11. ^ Handbook of Texas Online – Mineral Resources and Mining. Tshaonline.org. Retrieved on 2011-10-29.
  12. ^ Mason, Texas Chamber of Commerce Web site
  13. ^ a b Harper, Douglas. "topaz". Online Etymology Dictionary.
  14. ^ A Lapidary or History of Gemstones, University of Cambridge, 1652.
  15. ^ See for extensive discussion Oliver Farrington, Gems and Gem Minerals, Chicago, 1903, p. 119. Farrington was curator of Natural History Museum in Chicago.