DICTIONARY of GEMS and GEMOLOGY V: ;8Y the SAME PUBLISHERS
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THn ArrERrcAN M rlrERA LocIST JOURNAL OF THE MINERALOGICAL SOCIETY OF AMERICA Vol. 50 ]ANUARY-FEBRUARY. 1965 Nos. 1 and 2 STUDIES OF THE TORBERNITE MINERALS (III): ROLE OF THE INTERLAYER OXONIUM, POTASSIUM, AND AMMONIUM IONS, AND WATER MOLECULES1 Mercorlt Ross Ar.rnH. T. EvaNs, Jn., LI. S. GeologicalSuraey, Wash,i,ngton,D. C. Alstnact Structural and chemical evidence is given to show that solid-solution series probably exist in the torbernite mineral group between the foliowing pairs of end members: K(UOzAsOa)'3I{:O (abernathyite) and H3O(UOrAsOD.3HzO (troegerite),K(UOrPO' '3HzO (meta-ankoleite) and HaO(UOzPO4).3HrO, NH+(UOzAsOd.3HzO and lroegerite, and NHr(UOzPOt '3HrO (uramphite) and H:O(UO:PO ) '3HrO. These seriesare erpressed by the formula A,_u(ttro)u(uorxo4).3H,o r,vhereA:K+ or NHa+, and X:As or P. Other possiblesolid-solution seriesare also given. The structures of K(UOzAsOa).3HzO (abernathyite), NHr(UOzAsOr)'3HzO, K(HrO)(UO:AsOa)z'6HrO, and Cu(UOrPOr)r'SHzO (meta-torbernite) are related to other torbernite minerals and possible structural similarities are suggested. The role of the interlayer cations and water moleculesin the torbernite minerals is related to other mineral groups including the zeolites, the feldspars and micas, the clay minerals, the jarosites and alunites, and the clathrate compounds. It is predicted that the distribution of the cations H3O+, K+, and NHr+ over the ll'ater molecules sites observed in the abernathyite-like compounds may be a common feature of the interlayer structure of the hydrous layer sili- cates and of the intercage structure of the zeolites and clathrate compounds The specia- nature of the oxonium ion in hvdrous structures is discussed. -
The Wittelsbach-Graff and Hope Diamonds: Not Cut from the Same Rough
THE WITTELSBACH-GRAFF AND HOPE DIAMONDS: NOT CUT FROM THE SAME ROUGH Eloïse Gaillou, Wuyi Wang, Jeffrey E. Post, John M. King, James E. Butler, Alan T. Collins, and Thomas M. Moses Two historic blue diamonds, the Hope and the Wittelsbach-Graff, appeared together for the first time at the Smithsonian Institution in 2010. Both diamonds were apparently purchased in India in the 17th century and later belonged to European royalty. In addition to the parallels in their histo- ries, their comparable color and bright, long-lasting orange-red phosphorescence have led to speculation that these two diamonds might have come from the same piece of rough. Although the diamonds are similar spectroscopically, their dislocation patterns observed with the DiamondView differ in scale and texture, and they do not show the same internal strain features. The results indicate that the two diamonds did not originate from the same crystal, though they likely experienced similar geologic histories. he earliest records of the famous Hope and Adornment (Toison d’Or de la Parure de Couleur) in Wittelsbach-Graff diamonds (figure 1) show 1749, but was stolen in 1792 during the French T them in the possession of prominent Revolution. Twenty years later, a 45.52 ct blue dia- European royal families in the mid-17th century. mond appeared for sale in London and eventually They were undoubtedly mined in India, the world’s became part of the collection of Henry Philip Hope. only commercial source of diamonds at that time. Recent computer modeling studies have established The original ancestor of the Hope diamond was that the Hope diamond was cut from the French an approximately 115 ct stone (the Tavernier Blue) Blue, presumably to disguise its identity after the that Jean-Baptiste Tavernier sold to Louis XIV of theft (Attaway, 2005; Farges et al., 2009; Sucher et France in 1668. -
Renowned for His Iconic Designs and Breathtaking Gem Collections, Harry Winston Was a Man Who Knew the True Value of a Diamond
A BRILLIANT LEGACY Renowned for his iconic designs and breathtaking gem collections, Harry Winston was a man who knew the true value of a diamond. BY ALLISON HATA 54 A diamond is anything but just another stone. Highly coveted, precious and exceedingly rare, diamonds can take on different meanings: a symbol of status, a statement of love or a sign of purity. “Diamonds are a physical connection to [the earth] other than our feet on the ground,” says Russell Shor, a senior industry analyst for the Gemologist Institute of America. “When the earth was young and there was volcanic mass seething inside—this is how diamonds were formed. Diamonds connect us to that.” One man understood this intrinsic connection and dedicated his life to bringing the world closer to the precious gem through his jewelry designs and generous gifts to national institu- tions. Known as the “king of dia- monds,” the late Harry Winston was the first American jeweler to own and cut some of the most iconic stones in history, in addi- tion to setting a new standard for jewelry that showcases a gem’s natural beauty. Born more than a century ago, the young Winston—the son of a small jewelry shop owner—demonstrated a natural instinct for examining diamonds and precious gems. In subsequent years, he cultivated this talent to become one of the most prominent diamond merchants and designers of his time. His legacy lives on through the house of Harry Winston, which pairs his classic vision with a contemporary sensi- bility to create modern pieces that still grace the red carpet today. -
RMSH August 2012 Newsletter.Pdf
VOLUME 47, NO. 8 A UGUST 2012 CHALCEDONY MEETING BY D EAN S AKABE Wednesday This month’s topic is the most worked I call a stone Chalcedony, when it is sort of upon stone in any lapidary operation, translucent and homogeneous in color. August 22 Chalcedony . Chalcedony in a cryptocrys- Such as the Malawi Blue Chalcedony. 6:15-8:00 pm talline form of silica, composed of very Makiki District fine intergrowths of Quartz and Moganite. These are both silica minerals, which differ Park in the respect that quartz has a trigonal Administration crystal structure, while moganite is mono- Building clinic. Chalcedony's standard chemical structure is SiO 2 (Silicon Dioxide). Chalcedony has a waxy luster and is usu- NEXT MONTH ally semitransparent or translucent. It can Wednesday assume a wide range of colors, with the Blue Lace Agate most common seen as white to gray, blue, September 26 or brown ranging from pale to nearly Flourite black. Agates are stones which usually have col- ored layers. These are colored layers of The name "chalcedony" comes from the differently colored layers of Chalcedony. LAPIDARY calcedonius Latin , from a translation from Such as the Blue Lace Agate or Holly Blue Every Thursday khalkedon. the Greek word Unfortu- Agate. 6:30-8:30pm natelly, a connection to the town of Chal- cedon, in Asia Minor could not be found, Forms of Chalcedony are found in all 50 Second-floor Arts but one can always be hopeful. state, occurring in many colors and color and Crafts Bldg combinations. Some of the better known To make things alittle confusing is that ones are: Makiki District Chalcedony and Agate are terms used al- Park most interchangeably, as both are forms of quartz and are both Silicon Dioxide. -
List of New Mineral Names: with an Index of Authors
415 A (fifth) list of new mineral names: with an index of authors. 1 By L. J. S~v.scs~, M.A., F.G.S. Assistant in the ~Iineral Department of the,Brltish Museum. [Communicated June 7, 1910.] Aglaurito. R. Handmann, 1907. Zeita. Min. Geol. Stuttgart, col. i, p. 78. Orthoc]ase-felspar with a fine blue reflection forming a constituent of quartz-porphyry (Aglauritporphyr) from Teplitz, Bohemia. Named from ~,Xavpo~ ---- ~Xa&, bright. Alaito. K. A. ~Yenadkevi~, 1909. BuU. Acad. Sci. Saint-P6tersbourg, ser. 6, col. iii, p. 185 (A~am~s). Hydrate~l vanadic oxide, V205. H~O, forming blood=red, mossy growths with silky lustre. Founi] with turanite (q. v.) in thct neighbourhood of the Alai Mountains, Russian Central Asia. Alamosite. C. Palaehe and H. E. Merwin, 1909. Amer. Journ. Sci., ser. 4, col. xxvii, p. 899; Zeits. Kryst. Min., col. xlvi, p. 518. Lead recta-silicate, PbSiOs, occurring as snow-white, radially fibrous masses. Crystals are monoclinic, though apparently not isom0rphous with wol]astonite. From Alamos, Sonora, Mexico. Prepared artificially by S. Hilpert and P. Weiller, Ber. Deutsch. Chem. Ges., 1909, col. xlii, p. 2969. Aloisiite. L. Colomba, 1908. Rend. B. Accad. Lincei, Roma, set. 5, col. xvii, sere. 2, p. 233. A hydrated sub-silicate of calcium, ferrous iron, magnesium, sodium, and hydrogen, (R pp, R',), SiO,, occurring in an amorphous condition, intimately mixed with oalcinm carbonate, in a palagonite-tuff at Fort Portal, Uganda. Named in honour of H.R.H. Prince Luigi Amedeo of Savoy, Duke of Abruzzi. Aloisius or Aloysius is a Latin form of Luigi or I~ewis. -
Symposium on Agate and Cryptocrystalline Quartz
Symposium on Agate and Cryptocrystalline Quartz September 10 – 13, 2005 Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter; Colorado School of Mines Geology Museum; and U.S. Geological Survey 2 Cover Photos {top left} Fortification agate, Hinsdale County, Colorado, collection of the Geology Museum, Colorado School of Mines. Coloration of alternating concentric bands is due to infiltration of Fe with groundwater into the porous chalcedony layers, leaving the impermeable chalcedony bands uncolored (white): ground water was introduced via the symmetric fractures, evidenced by darker brown hues along the orthogonal lines. Specimen about 4 inches across; photo Dan Kile. {lower left} Photomicrograph showing, in crossed-polarized light, a rhyolite thunder egg shell (lower left) a fibrous phase of silica, opal-CTLS (appearing as a layer of tan fibers bordering the rhyolite cavity wall), and spherulitic and radiating fibrous forms of chalcedony. Field of view approximately 4.8 mm high; photo Dan Kile. {center right} Photomicrograph of the same field of view, but with a 1 λ (first-order red) waveplate inserted to illustrate the length-fast nature of the chalcedony (yellow-orange) and the length-slow character of the opal CTLS (blue). Field of view about 4.8 mm high; photo Dan Kile. Copyright of articles and photographs is retained by authors and Friends of Mineralogy, Colorado Chapter; reproduction by electronic or other means without permission is prohibited 3 Symposium on Agate and Cryptocrystalline Quartz Program and Abstracts September 10 – 13, 2005 Editors Daniel Kile Thomas Michalski Peter Modreski Held at Green Center, Colorado School of Mines Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter Colorado School of Mines Geology Museum U.S. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
Blue Sapphire Engagement Ring, RG-2817U Dramatic Color And
Blue Sapphire Engagement Ring, RG-2817u Dramatic color and unusual elegance come together in this vintage style blue sapphire engagement ring. The 18k white gold band of this engagement ring is set along the shoulders and shank with a collection of seventy-four round brilliant cut diamonds that total 0.52 carats. Eight of these diamonds, four on each side, are arranged in a floral design. The diamond flowers flank a bewitching blue sapphire at the center. This is a vintage style (new) blue sapphire engagement ring. Options None Item # rg2817u Metal 18k white gold Weight in grams 4.6 Special characteristics A matching band is available and may be purchased separately. Please see item RG-2817wb. Condition New Diamond cut or shape round brilliant Diamond carat weight 0.52 Diamond mm measurements 1.4-0.9 Diamond color G-H Diamond clarity VS1 Diamond # of stones 74 Gemstone name Natural Corundum (sapphire) Gemstone cut or shape round faceted mixed cut Gemstone carat weight 1.05 Gemstone type Type II Gemstone clarity VS Gemstone hue very very slightly greenish blue Gemstone tone 4-Medium Light Gemstone saturation 4-Moderately Strong Gemstone # of stones 1 Top of ring length (N-S) 6.75 mm [0.26 in] Width of shank at shoulders 4.85 mm [0.19 in] Width of shank at base 2.25 mm [0.09 in] Ring height above finger 6.9 mm [0.27 in] Other ring info For new rings like this one, the gram weight, diamond and gemstone carat weights, color, and clarity, as well as other jewelry details, may vary from the specifications shown on this page, but are similar in quality. -
Tigers Eye Free
FREE TIGERS EYE PDF Karen Robards | 400 pages | 11 May 2010 | HarperCollins Publishers Inc | 9780380755554 | English | New York, United States Tigers Eye Stone Meaning & Uses: Aids Harmonious Balanced Action Tiger's eye also called tiger eye is a Tigers Eye gemstone that is usually a metamorphic rock with a golden to red-brown colour and a silky lustre. As members of the quartz group, tiger's eye and the related blue-coloured mineral hawk's eye gain their silky, lustrous appearance from the parallel intergrowth of quartz crystals and altered amphibole fibres that have mostly turned into limonite. Tiger iron is an altered rock composed chiefly of tiger's eye, red jasper and black hematite. The undulating, contrasting bands of colour and lustre make for an attractive motif and it is Tigers Eye used for Tigers Eye and ornamentation. Tiger iron is a popular ornamental material Tigers Eye in a variety of applications, from beads to knife hilts. Tiger iron is mined primarily in South Africa and Western Australia. Tiger's eye is composed chiefly of silicon dioxide SiO 2 and is coloured mainly by Tigers Eye oxide. The specific gravity ranges from 2. Serpentine deposits in which are occasionally found chatoyant bands of chrysotile fibres have been found in the US states of Arizona and California. These have been cut and sold as "Arizona tiger-eye" and "California tiger's eye" gemstones. In some parts of the world, the stone is believed to ward off the evil eye. Gems are usually given a cabochon cut to best display their chatoyance. -
Pleasant Memories of Foreign Travel
THE LIBRARY OF THE UNIVERSITY OF CALIFORNIA LOS ANGELES r < Oh O D Q < S3 Pleasant Memories OF Foreign Travel By S. M. BURNHAM AUTIIOK OF "Tub ITiSTonY and Uses of Limestones and Marbles," "PuECious Stones in Nature, Art and Literature," "The Struggles of the Nations." IFllustrateD BOSTON: BRADLEE WHIDDEN 1896 COPYEIGHT, 1896, BY S. M. BUKNHAM. INTRODUCTION. The rapid transit across the ocean at the present time has doubtless greatly increased the number of travellers to foreign lands. Some tourists make an annual trip of only a few- weeks. There may be advantages in such a plan, especially for those who find it difficult to be absent from home and business for a prolonged visit, while, on the other hand, time and a careful study of the interesting objects and places to be seen, in order to derive the greatest pleasure and benefit, especially in visiting the celebrated art collections, is essential. Most of the large cities of Europe attained their full growth ages ago, hence they appear to-day much the same as in past centuries, with the exception of having expanded their limits by absorbing adjacent territory. Towns and cities in America are often the growth of a few years, but it is not so in the Old World, where time was needed for their development. There antiquity is venerated ; here it is frequently regarded with indifference. Mistakes and faults are common to both hemi- spheres ; but frequent communication between the two will in time correct many of these errors, and bring the nations into a more familiar acquaintance with one another. -
Evaluation of Brilliance, Fire, and Scintillation in Round Brilliant
Optical Engineering 46͑9͒, 093604 ͑September 2007͒ Evaluation of brilliance, fire, and scintillation in round brilliant gemstones Jose Sasian, FELLOW SPIE Abstract. We discuss several illumination effects in gemstones and University of Arizona present maps to evaluate them. The matrices and tilt views of these College of Optical Sciences maps permit one to find the stones that perform best in terms of illumi- 1630 East University Boulevard nation properties. By using the concepts of the main cutter’s line, and the Tucson, Arizona 85721 anti-cutter’s line, the problem of finding the best stones is reduced by E-mail: [email protected] one dimension in the cutter’s space. For the first time it is clearly shown why the Tolkowsky cut, and other cuts adjacent to it along the main cutter’s line, is one of the best round brilliant cuts. The maps we intro- Jason Quick duce are a valuable educational tool, provide a basis for gemstone grad- Jacob Sheffield ing, and are useful in the jewelry industry to assess gemstone American Gem Society Laboratories performance. © 2007 Society of Photo-Optical Instrumentation Engineers. 8917 West Sahara Avenue ͓DOI: 10.1117/1.2769018͔ Las Vegas, Nevada 89117 Subject terms: gemstone evaluation; gemstone grading; gemstone brilliance; gemstone fire; gemstone scintillation; gemstone cuts; round brilliant; gemstones; diamond cuts; diamonds. James Caudill American Gem Society Advanced Instruments Paper 060668R received Aug. 28, 2006; revised manuscript received Feb. 16, 8881 West Sahara Avenue 2007; accepted for publication Apr. 10, 2007; published online Oct. 1, 2007. Las Vegas, Nevada 89117 Peter Yantzer American Gem Society Laboratories 8917 West Sahara Avenue Las Vegas, Nevada 89117 1 Introduction are refracted out of the stone. -
Epr Investigation of Carbonaceous Natural
Canodian Mineralogist Yol. 27, pp. 219-224(1989) EPRINVESTIGATION OF CARBONACEOUSNATURAL OUARTZ SINGLE CRYSTALS PILLUTLA S. RAO, JOHN A. WEIL AND JOHN A.S. WILIAMS Departmentof Chemistry,University of Saskatchewan,Saskatoon, Saskatchewan S7N 0W0 ABSTRACT Nos donn€esne rdvblent aucune 6vidence de centresi liai- sonscarbone-oryglne daus lesquels le C pourrait substi- As part of an investigation of whether carbon can sub- tuer au Si. stitute for silicon in ming1sfu, electron paramagnetic resonancestudies were carried out on natural crystals of Clraduit par la Rddaction) a4;laftz from carbonaceous surroutrding.s, i.e., a cat- bonized log found in Utah, For these, as obtained, the Mots<lds:carbone, charbon, lacunes, r6sonance 6lectro- room-teNnperatureresufts at 9.6 GHz indicate f.hepresence nique paramagn€tique,quartz, dioxydede silicium. of the well-known oxygen vacancy (Er ') silicon center and an isotropic broad line with g-factor 2.@28(l) attributed to coal-like macro-regions in the crystals. No signals from INTRoDUCTIoN tAlo4lo or other 4lrrmins6 hole centers usually found in o-quartz were observable,even at low lemperaturs (35 XC We undertook the current investigation pasly in and after X-irradiation. Thus the dark color is not that of the hope of finding a paramagnetic center involving smoky quartz, but is due to macroscopic coal-like impuri- carbon occurring substitutionally for silicon in srys- ties. A weak Mn2+ spectrum could be observedat 2A C,Hz talline quartz. Certainly the question of whether car- but not at9.6 GHaIn concurrent masuremetrts of Her- bon ever enters silicate structures substitutionally is (New kimer "diamonds" York state), doubly terminated of considerable interest.