A Crystallographic Analysis of the Tavernier Blue Diamond
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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. -
Blue Diamond Prices Are on the Rise
This copy is for your personal, non-commercial use only. To order presentation-ready copies for distribution to your colleagues, clients or customers visit http://www.djreprints.com. https://www.barrons.com/articles/blue-diamond-prices-are-on-the-rise-1518037930 Blue Diamond Prices Are on the Rise By Ariel R. Shapiro Feb. 7, 2018 4:12 p.m. ET The fancy color diamond market is on the upswing, according to a report, with blue diamonds seeing the largest gains. Blue diamonds saw a 5.9% increase in value in the fourth quarter of 2017 in a year-over-year comparison, according to data published on Feb. 1 by the Fancy Color Research Foundation (FCRF). Pink and yellow diamond prices decreased slightly in the same period, at 0.8% and 1.8%, respectively. The market overall was up 0.1%. A fancy vivid blue diamond ring (est. $14-18 million) goes on view at Sotheby's on Oct. 13, 2017 in London. ILLUSTRATION: GETTY IMAGES FOR SOTHEBY'S In November 2017, Christie’s sold a 8.67-carat fancy intense blue diamond ring in Geneva, Switzerland for $13.2 million. The reason for this disparity has less to do with demand, than it does with the rarity of the stone, says FCRF Chairman Eden Rachminov. Demand for yellow and pink diamonds is actually higher, but the amount of blue diamonds being mined is decreasing. “Almost nothing is coming out of the ground,” he says. Pink diamonds have seen the highest gains in the last 13 years with an overall appreciation of 361.9%, according to FCRF’s index, which is compiled through survey data provided by manufacturers and brokers. -
Microstructural, Mechanical, Corrosion and Cytotoxicity Characterization of Porous Ti-Si Alloys with Pore-Forming Agent
materials Article Microstructural, Mechanical, Corrosion and Cytotoxicity Characterization of Porous Ti-Si Alloys with Pore-Forming Agent Andrea Školáková 1,*, Jana Körberová 1 , Jaroslav Málek 2 , Dana Rohanová 3, Eva Jablonská 4, Jan Pinc 1, Pavel Salvetr 1 , Eva Gregorová 3 and Pavel Novák 1 1 Department of Metals and Corrosion Engineering, University of Chemistry and Technology Prague, Technická 5, 166 28 Prague 6, Czech Republic; [email protected] (J.K.); [email protected] (J.P.); [email protected] (P.S.); [email protected] (P.N.) 2 UJP Praha a.s., Nad Kamínkou 1345, 156 10 Prague 16, Czech Republic; [email protected] 3 Department of Glass and Ceramics, University of Chemistry and Technology Prague, Technická 5, 166 28 Prague 6, Czech Republic; [email protected] (D.R.); [email protected] (E.G.) 4 Department of Biochemistry and Microbiology, University of Chemistry and Technology Prague, Technická 5, 166 28 Prague 6, Czech Republic; [email protected] * Correspondence: [email protected]; Tel.: +420-220-444-055 Received: 12 November 2020; Accepted: 7 December 2020; Published: 9 December 2020 Abstract: Titanium and its alloys belong to the group of materials used in implantology due to their biocompatibility, outstanding corrosion resistance and good mechanical properties. However, the value of Young’s modulus is too high in comparison with the human bone, which could result in the failure of implants. This problem can be overcome by creating pores in the materials, which, moreover, improves the osseointegration. Therefore, TiSi2 and TiSi2 with 20 wt.% of the pore-forming agent (PA) were prepared by reactive sintering and compared with pure titanium and titanium with the addition of various PA content in this study. -
Experimental and Computational Study of Fracturing in an Anisotropic Brittle Solid
Mechanics of Materials 28Ž. 1998 247±262 Experimental and computational study of fracturing in an anisotropic brittle solid Abbas Azhdari 1, Sia Nemat-Nasser ) Center of Excellence for AdÕanced Materials, Department of Applied Mechanics and Engineering Sciences, UniÕersity of California-San Diego, La Jolla, CA 92093-0416, USA Received 21 November 1996; revised 26 August 1997 Abstract For isotropic materials, stress- and energy-based fracture criteria lead to fairly similar results. Theoretical studies show that the crack-path predictions made by these criteria are not identical in the presence of strong material anisotropy. Therefore, experiments are performed to ascertain which criterion may apply to anisotropic materials. Notched specimens made from sapphire, a microscopically homogeneous and brittle solid, are used for the experiments. An attempt is made to locate the notch on different crystallographic planes and thus to examine the fracture path along different cleavage planes. The experimental observations are compared with the numerical results of the maximum tensile stress and the maximum energy-release rate criteria. It is observed that most of the notched specimens are fractured where the tensile stress is maximum, whereas the energy criterion fails to predict the fracture path of most of the specimens. For the tensile-stress Žn. s p s r g s fracture criterion, a dimensionless parameter, A ''2 R0 nn a Enn, is introduced, where nnand E nn, respectively, are the tensile stress and Young's modulus in the direction normal to the cleavage plane specified by the angle a Žthe fracture surface energy of this plane is ga . and R0 is a characteristic length, e.g. -
Queer Utopia in Steven Universe Mandy Elizabeth Moore University of Florida, [email protected]
Research on Diversity in Youth Literature Volume 2 | Issue 1 Article 5 June 2019 Future Visions: Queer Utopia in Steven Universe Mandy Elizabeth Moore University of Florida, [email protected] Follow this and additional works at: http://sophia.stkate.edu/rdyl Recommended Citation Moore, Mandy Elizabeth (2019) "Future Visions: Queer Utopia in Steven Universe," Research on Diversity in Youth Literature: Vol. 2 : Iss. 1 , Article 5. Available at: http://sophia.stkate.edu/rdyl/vol2/iss1/5 This Article is brought to you for free and open access by SOPHIA. It has been accepted for inclusion in Research on Diversity in Youth Literature by an authorized editor of SOPHIA. For more information, please contact [email protected]. Moore: Future Visions: Queer Utopia in Steven Universe Since it premiered on Cartoon Network in 2013, Steven Universe has garnered both praise and criticism for its portrayal of queer characters and its flexible approach to gender. Created by Rebecca Sugar, a bisexual and nonbinary artist, the show tells the story of Steven, a half-human, half-alien teenager raised by a trio of alien parental figures called the Crystal Gems. Steven’s adventures range from helping his friends at the local donut shop to defending Earth from the colonizing forces of the Gem Homeworld. Across its five seasons, this series has celebrated many queer firsts for animated children’s content. In 2018, Steven Universe aired one of the first cartoon same-sex wedding scenes (“Reunited”), and in 2019, it became the first animated show to win a Gay and Lesbian Alliance Against Defamation (GLAAD) award, taking home the prize for Outstanding Kids and Family Programming. -
Activity 21: Cleavage and Fracture Maine Geological Survey
Activity 21: Cleavage and Fracture Maine Geological Survey Objectives: Students will recognize the difference between cleavage and fracture; they will become familiar with planes of cleavage, and will use a mineral's "habit of breaking" as an aid to identifying common minerals. Time: This activity is intended to take one-half (1/2) period to discuss cleavage planes and types and one (1) class period to do the activity. Background: Cleavage is the property of a mineral that allows it to break smoothly along specific internal planes (called cleavage planes) when the mineral is struck sharply with a hammer. Fracture is the property of a mineral breaking in a more or less random pattern with no smooth planar surfaces. Since nearly all minerals have an orderly atomic structure, individual mineral grains have internal axes of length, width, and depth, related to the consistent arrangement of the atoms. These axes are reflected in the crystalline pattern in which the mineral grows and are present in the mineral regardless of whether or not the sample shows external crystal faces. The axes' arrangement, size, and the angles at which these axes intersect, all help determine, along with the strength of the molecular bonding in the given mineral, the degree of cleavage the mineral will exhibit. Many minerals, when struck sharply with a hammer, will break smoothly along one or more of these planes. The degree of smoothness of the broken surface and the number of planes along which the mineral breaks are used to describe the cleavage. The possibilities include the following. Number of Planes Degree of Smoothness One Two Three Perfect Good Poor Thus a mineral's cleavage may be described as perfect three plane cleavage, in which case the mineral breaks with almost mirror-like surfaces along the three dimensional axes; the mineral calcite exhibits such cleavage. -
Correlation of the Mohs's Scale of Hardness with the Vickers' S Hardness Numbers
718 Correlation of the Mohs's scale of hardness with the Vickers' s hardness numbers. By E. WILFRED TAYLOR, C.B.E., F.R.M.S., F. Inst. P. Messrs. Cooke, Troughton & Simms, Ltd., York. [Read June 23, 1949.] INERALOGISTS have long been accustomed to describe hard- M ness with the aid of a scale devised by Friedrich Mohs, who lived from 1773 to 1839. The test is qualitative, each mineral in the scale being capable of scratching those that precede it, but the ten minerals have held their ground as a useful representative series with which it is now interesting to compare another method of estimating hard- ness. In the metallurgical world hardness is now usually expressed by means of the Vickers's hardness numbers or their equivalent, and the figures are derived from the size of the impression made by a diamond indenter in the form of a four-sided pyramid with the opposite faces worked to an included angle of 136 ~ More recently micro-hardness testers have been devised to enable minute impressions to be formed under light loads on small individual crystals of a metallic alloy, 1 and it occurred to the author to obtain hardness figures for the various types of optical glass by means of a scratch test with such an instrument. The intention was to draw a lightly loaded diamond across a polished glass surface and to measure the width of the resulting furrow. This method proved to be promising, but as an experiment a static indenter was also used, and it was dis- covered that glass was sufficiently plastic to take good impressions, so long as the load did not exceed 50 grams or thereabouts. -
Geology and Beryl Deposits of the Peerless Pegmatite Pennington County South Dakota
Geology and Beryl Deposits of the Peerless Pegmatite Pennington County South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-A This report concerns work done partly on behalj of the U. S. Atomic Energy Commission and is published with the permission of the , » Commission Geology and Beryl Deposits of the Peerless Pegmatite Pennington County South Dakota By DOUGLAS M. SHERllDAN, HAL G. STEPHENS, MORTIMER H. STAATZ and JAMES J. NORTON PEGMATITES AND OTHER PRECAMBRIAN ROCKS IN THE SOUTHERN BLACK HILLS GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-A This report concerns work done partly on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.50 (paper cover) CONTENTS Page Page Abstract.__________________________________________ 1 Geology Continued Introduction _______________________________________ 1 Peerless pegmatite Continued Location_____________________________________ 1 Chemical composition......____________ 17 History and production________________________ 2 Origin________ ____________________ _. 18 Past and present investigations.__________________ 3 Mineral deposits_____________________________ 21 Acknowledgments__________________________ 4 Mica__ _________ _________________________ 21 Mine workings _____________________________________ -
Mineral Identification Chart – LECTURE
Mineral Identification Chart – LECTURE NONMETALLIC MINERALS (listed in decreasing hardness) Review mineral formula to connect to family! H=Hardness; SG = specific gravity Mineral H SG Streak Color (and/or luster) Form Cleavage/Fracture Distinctive properties Garnet 7 3.5- White Red, black, or brown; can Dodecahedrons (12- No cleavage. Dodecahedron form, X3Y2(SiO4)3 where X and Y are 4.3 be yellow, green, pink. sided polygons) Brittle. Conchoidal red, glassy, conchoidal combinations of Ca, Mg, Fe, Al Glassy. Translucent. fracture. fracture, H=7. Olivine (Mg,Fe)2SiO4 7 3.3- White Pale or dark olive green Short prisms Conchoidal Green, conchoidal 3.4 to yellow or brown. (usually too small to fracture. fracture, glassy, H=7. Glassy. Transparent. see). Brittle. Usually granular. Quartz SiO2 7 2.7 White Colorless, white, or gray; Massive; or Conchoidal Glassy, conchoidal can occur in all colors. hexagonal prisms fracture. fracture, H=7. Hex. Glassy and/or greasy. that end in a point. prism with point end. Plagioclase Feldspar family: 6 2.6- White Colorless, white, gray, or Tabular crystals or 2 good cleavage Twinning. 2 cleavages Anorthite and Labradorite 2.8 black; can have iridescent thin needles planes at nearly at 90°. CaAl2Si2O8 to Oligoclase and play of color from within. right angles. Albite NaAlSi3O8 Translucent to opaque. Potassium Feldspar family: 6 2.5- White Pink. Or white, orange, Tabular crystals 2 good cleavage Subparallel exsolution Orthoclase and Microcline 2.6 brown, gray, green. planes at nearly lamellae. 2 cleavages KAlSi3O8 Translucent to opaque. right angles. at 90°. Pink color. Pyroxene family: Augite 5.5- 3.2- White, Green to black; opaque. -
Gemstones by Donald W
GEMSTONES By Donald W. olson Domestic survey data and tables were prepared by Nicholas A. Muniz, statistical assistant, and the world production table was prepared by Glenn J. Wallace, international data coordinator. In this report, the terms “gem” and “gemstone” mean any gemstones and on the cutting and polishing of large diamond mineral or organic material (such as amber, pearl, petrified wood, stones. Industry employment is estimated to range from 1,000 to and shell) used for personal adornment, display, or object of art ,500 workers (U.S. International Trade Commission, 1997, p. 1). because it possesses beauty, durability, and rarity. Of more than Most natural gemstone producers in the United states 4,000 mineral species, only about 100 possess all these attributes and are small businesses that are widely dispersed and operate are considered to be gemstones. Silicates other than quartz are the independently. the small producers probably have an average largest group of gemstones; oxides and quartz are the second largest of less than three employees, including those who only work (table 1). Gemstones are subdivided into diamond and colored part time. the number of gemstone mines operating from gemstones, which in this report designates all natural nondiamond year to year fluctuates because the uncertainty associated with gems. In addition, laboratory-created gemstones, cultured pearls, the discovery and marketing of gem-quality minerals makes and gemstone simulants are discussed but are treated separately it difficult to obtain financing for developing and sustaining from natural gemstones (table 2). Trade data in this report are economically viable deposits (U.S. -
Methods Used to Identifying Minerals
METHODS USED TO IDENTIFYING MINERALS More than 4,000 minerals are known to man, and they are identified by their physical and chemical properties. The physical properties of minerals are determined by the atomic structure and crystal chemistry of the minerals. The most common physical properties are crystal form, color, hardness, cleavage, and specific gravity. CRYSTALS One of the best ways to identify a mineral is by examining its crystal form (external shape). A crystal is defined as a homogenous solid possessing a three-dimensional internal order defined by the lattice structure. Crystals developed under favorable conditions often exhibit characteristic geometric forms (which are outward expressions of the internal arrangements of atoms), crystal class, and cleavage. Large, well- developed crystals are not common because of unfavorable growth conditions, but small crystals recognizable with a hand lens or microscope are common. Minerals that show no external crystal form but possess an internal crystalline structure are said to be massive. A few minerals, such as limonite and opal, have no orderly arrangement of atoms and are said to be amorphous. Crystals are divided into six major classes based on their geometric form: isometric, tetragonal, hexagonal, orthorhombic, monoclinic, and triclinic. The hexagonal system also has a rhombohedral subdivision, which applies mainly to carbonates. CLEAVAGE AND FRACTURE After minerals are formed, they have a tendency to split or break along definite planes of weakness. This property is called cleavage. These planes of weakness are closely related to the internal structure of the mineral, and are usually, but not always, parallel to crystal faces or possible crystal faces. -
Almonds on Parade! Meet Your New Board Director Protein Powder
NEWS, VIEWS, AND INDUSTRY INSIGHT JANUARY– FEBRUARY 2020 Almonds Protein Powder Meet Your New on Parade! Launch Board Director Contents JAN–FEB 2020 8 FIELD TEAM 10 NEWS IN A NUTSHELL 16 CULTIVATING SUSTAINABILITY 20 CORNERING THE MARKET 24 ADVOCACY REPORT 28 GROWING THE GOODNESS 30 IN YOUR ORCHARD 50 CLASSIFIED ADS Features 6 President’s Corner 20 Blue Diamond Unveils New Almond President and CEO Mark Jansen shares what we Protein Powder have to look forward to in this new year and new Blue Diamond’s first new major product of 2020 decade, including the celebration of the co-op’s showcases the latest innovation offering consumers protein 110th anniversary. powder made with 100 percent pure almond protein. 14 Almonds on Parade 28 Meet Your New District 8 Board Director For the second year in a row, Blue Diamond brought its As a fifth generation farmer and third generation almond almond growing history to the life in the Rose Parade, grower, being part of the Blue Diamond family has been held New Year’s Day in Pasadena, California. memorable for Matthew Efird and his family. ON THE COVER: Blue Diamond growers represented the co-op and Almond Breeze brand at the Rose Parade in Pasadena, California. JANUARY–FEBRUARY 2020 3 BOARD OF DIRECTORS Dan Cummings, Chairman of the Board | Chico Dale Van Groningen, Vice Chairman | Ripon John Monroe | Arbuckle Kevin Fondse | Ripon Stephen Van Duyn | Modesto Charles Crivelli III | Turlock Dan Mendenhall | Winton Matthew Efird | Fresno Kent Stenderup | Arvin Joe Huston | Monterey OFFICERS Mark Jansen, President and CEO Dean LaVallee, Chief Financial Officer ALMOND FACTS STAFF Samantha DeMelo, Managing Editor Mel Machado, Contributing Photographer Gray Allen, Advertising Sales 916.783.4334 & 916.765.3234 Blue Diamond, the world’s largest processor and marketer of almonds, exports to over 100 countries.