Gemmologythe Journal of Volume 35 / No
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Raman Investigations to Identify Corallium Rubrum in Iron Age Jewelry and Ornaments
minerals Article Raman Investigations to Identify Corallium rubrum in Iron Age Jewelry and Ornaments Sebastian Fürst 1,†, Katharina Müller 2,†, Liliana Gianni 2,†, Céline Paris 3,†, Ludovic Bellot-Gurlet 3,†, Christopher F.E. Pare 1,† and Ina Reiche 2,4,†,* 1 Vor- und Frühgeschichtliche Archäologie, Institut für Altertumswissenschaften, Johannes Gutenberg-Universität Mainz, Schillerstraße 11, Mainz 55116, Germany; [email protected] (S.F.); [email protected] (C.F.E.P.) 2 Sorbonne Universités, UPMC Université Paris 06, CNRS, UMR 8220, Laboratoire d‘archéologie moléculaire et structurale (LAMS), 4 Place Jussieu, 75005 Paris, France; [email protected] (K.M.); [email protected] (L.G.) 3 Sorbonne Universités, UPMC Université Paris 06, CNRS, UMR 8233, De la molécule au nano-objets: réactivité, interactions et spectroscopies (MONARIS), 4 Place Jussieu, 75005 Paris, France; [email protected] (C.P.); [email protected] (L.B.-G.) 4 Rathgen-Forschungslabor, Staatliche Museen zu Berlin-Preußischer Kulturbesitz, Schloßstraße 1 a, Berlin 14059, Germany * Correspondence: [email protected] or [email protected]; Tel.: +49-30-2664-27101 † These authors contributed equally to this work. Academic Editor: Steve Weiner Received: 31 December 2015; Accepted: 1 June 2016; Published: 15 June 2016 Abstract: During the Central European Iron Age, more specifically between 600 and 100 BC, red precious corals (Corallium rubrum) became very popular in many regions, often associated with the so-called (early) Celts. Red corals are ideally suited to investigate several key questions of Iron Age research, like trade patterns or social and economic structures. While it is fairly easy to distinguish modern C. -
Pearls and Organic Gemstones
Pearls and Organic Gemstones INTRODUCTION Pearls were probably the first discovered gems of significance. Because they need no cutting or treatment to enhance their beauty and are rare natural occurrences, they have most likely always been highly esteemed. Organic gemstones are anything created by living processes. We have looked at amber in the past, but bone, teeth (such as ivory), and shells all have some value and are used today as gemstones. Pearls in General A pearl is grown by a mollusk (a bivalve such as a clam, oyster, or mussel or snail [single shell = valve]) in response to an irritant. Bivalves (two shelled mollusks) that secrete pearls live in both fresh‐ and saltwater. The irritant in most cases is a parasite (though it could be a grain of sand or other object). The parasite, a worm or other creature, is walled off by a secretion of calcium carbonate and protein. The calcium carbonate is the same as the inorganic material that makes stalactites in caves, and the protein is called conchiolin. The combination of these two substances (calcium carbonate and protein) makes the pearl's nacre (Nacre is also called mother of pearl). The nacre is a lustrous deposit around the irritant and forms concentric layers (overlapping circles). Many concentric layers of nacre build up over a period of a few years creating a pearl. The internal pattern is much like that seen in a jawbreaker. The layers create a sheen or luster that has iridescence and is described as both pearly luster and if colors of the rainbow are present, the pearl's orient. -
Download Course Outline for This Program
Program Outline 434- Jewellery and Metalwork NUNAVUT INUIT LANGUAGES AND CULTURES Jewelry and Metalwork (and all fine arts) PROGRAM REPORT 434 Jewellery and Metalwork Start Term: No Specified End Date End Term: No Specified End Date Program Status: Approved Action Type: N/A Change Type: N/A Discontinued: No Latest Version: Yes Printed: 03/30/2015 1 Program Outline 434- Jewellery and Metalwork Program Details 434 - Jewellery and Metalwork Start Term: No Specified End Date End Term: No Specified End Date Program Details Code 434 Title Jewellery and Metalwork Start Term No Specified End Date End Term No Specified End Date Total Credits Institution Nunavut Faculty Inuit Languages and Cultures Department Jewelry and Metalwork (and all fine arts) General Information Eligible for RPL No Description The Program in Jewellery and Metalwork will enable students to develop their knowledge and skills of jewellery and metalwork production in a professional studio atmosphere. To this end the program stresses high standards of craftship and creativity, all the time encouraging and exposing students to a wide range of materials, techniques and concepts. This program is designed to allow the individual student to specialize in an area of study of particular interest. There is an emphasis on creative thinking and problem-solving throughout the program.The first year of the program provides an environment for the students to acquire the necessary skills that will enable them to translate their ideas into two and three dimensional jewellery and metalwork. This first year includes courses in: Drawing and Design, Inuit Art and Jewellery History, Lapidary and also Business and Communications. -
Naming Polyatomic Ions and Acids Oxyanions
Oxyanions Naming Polyatomic Ions and Oxyanions Acids Oxyanions- negative ions containing Oxyanions may contain the prefix oxygen. “hypo-”, less than, or “per-”, more than. These have the suffix “-ate” or “-ite” For example - “-ate” means it has more oxygen atoms ClO4 Perchlorate bonded, “-ite” has less - ClO3 Chlorate For example - ClO2 Chlorite 2- SO4 sulfate ClO- Hypochlorite 2- SO3 sulfite Acids Naming acids Naming Acids Certain compounds produce H+ ions in Does it contain oxygen? water, these are called acids. If it does not, it gets the prefix “hydro-” and If it does contain an oxyanion, then the suffix “-ic acid” replace the ending. You can recognize them because the neutral compound starts with “H”. HCl If the ending was “–ate”, add “-ic acid” Hydrochloric acid If the ending was “–ite”, add “-ous acid” For example HCl, H2SO4, and HNO3. HF Don’t confuse a polyatomic ion with a H2SO4 Sulfuric Acid Hydrofluoric acid neutral compound. H2SO3 Sulfurous Acid HCN HCO - is hydrogen carbonate, not an acid. 3 Hydrocyanic acid Examples Examples Nomenclature (naming) of Covalent compounds HNO3 HNO3 Nitric Acid HI HI Hydroiodic acid H3AsO4 H3AsO4 Arsenic Acid HClO2 HClO2 Chlorous Acid 1 Determining the type of bond Covalent bonding is very Covalent bonding is very First, determine if you have an ionic different from ionic naming compound or a covalent compound. similar to ionic naming A metal and a nonmetal will form an You always name the one that is least Ionic names ignored the subscript ionic bond. electronegative first (furthest from because there was only one possible Compounds with Polyatomic ions form fluorine) ratio of elements. -
Geology and Selected Minerals of the Diamond Hill Quartz Mine Antreville, South Carolina by Mike Streeter, GMS Member Copyright March 2004
Tips and Trips Page 11 The Georgia Mineral Society May 2004 Geology and Selected Minerals of the Diamond Hill Quartz Mine Antreville, South Carolina by Mike Streeter, GMS Member Copyright March 2004 Chrissy and I have spent a great deal of time at the Diamond Diamond Hill is nothing short of remarkable when you consider Hill Quartz Mine near Antreville, South Carolina over the past that the actual collecting areas occupy a total of less than 3 several months. Chester Karwoski, who purchased the acres and that each variety requires its own unique set of property in 2003, brought in some heavy earth-moving conditions to form. The three most sought after varieties of equipment last fall and has opened up some new collecting quartz at the mine are skeletal, smoky and amethyst. opportunities. On our most recent trip to the mine on February 28, 2004, members of the Rome Georgia Gem and Mineral Skeletal quartz (also known Society and the Southern Appalachian Mineral Society joined as elestial quartz) exhibits a us. Since it is no secret that that I am a geologist by trade, I layered or ribbed pattern. am often asked geological and mineralogical questions about Its appearance gave rise to collecting locales. While digging at Diamond Hill, I was asked the term "skeletal" as the to explain how the rocks and crystals formed. Now there's a crystals resemble what $64,000 question for you! I answered the question as best I someone with a good could at the time. Since then, I have researched the literature imagination would expect to obtain a more detailed explanation that I would like to share the skeleton of a quartz with you. -
Preliminary Investigation of Purple Garnet from a New Deposit in Mozambique
GIT GEMSTONE UPDATE Preliminary Investigation of Purple Garnet from a New Deposit in Mozambique By GIT-Gem testing laboratory 11 May 2016 Introduction In March 2016, a group of Thai gem dealer led by Mr. Pichit Nilprapaporn paid a visit to the GIT and informed us about a new garnet deposit in Mozambique, that was discovered near the western border with Zimbabwe. They also displayed a large parcel of rough and a few cut stones claimed to be the material found in this new deposit (Figure 1). According to the stone’s owner, these garnet specimens were unearthed from an unconsolidated sediment layer, just a few meters below ground surface. This brief report is our preliminary investigation on the interesting vivid purple garnet from the new deposit in Mozambique. Figure 1: Mr. Pichit Nilprapaporn (center), the stone’s owner, showing a large parcel of purple gar- net roughs claimed to be from a new deposit in Mozambique to the GIT director (left). The Gem and Jewelry Institute of Thailand (Public Organization) 140, 140/1-3, 140/5 ITF-Tower Building. 1st - 4th and 6th Floor,Silom Road, Suriyawong, Bangrak, Bangkok 10500 Thailand Tel: +66 2634 4999 Fax: +66 2634 4970; Web: http://www.git.or.th; E-mail: [email protected] 11 May, 2016 Preliminary Investigation of Purple Garnet from a New Deposit in Mozambique 2 Samples and Testing Procedure The stone’s owners donated some specimens (one 6.10 ct oval-facetted stone and 13 rough samples weighing from 3.83 to 9.43 cts) to the GIT Gem Testing Laboratory for studying. -
Shear Zone Initiation in the Marcy Anorthosite Massif, Adirondacks, New York, USA James Hodge University of Maine, [email protected]
The University of Maine DigitalCommons@UMaine Electronic Theses and Dissertations Fogler Library Summer 8-23-2019 Fractures, Fluids, and Metamorphism: Shear Zone Initiation in the Marcy Anorthosite Massif, Adirondacks, New York, USA James Hodge University of Maine, [email protected] Follow this and additional works at: https://digitalcommons.library.umaine.edu/etd Part of the Geochemistry Commons, Geology Commons, and the Tectonics and Structure Commons Recommended Citation Hodge, James, "Fractures, Fluids, and Metamorphism: Shear Zone Initiation in the Marcy Anorthosite Massif, Adirondacks, New York, USA" (2019). Electronic Theses and Dissertations. 3050. https://digitalcommons.library.umaine.edu/etd/3050 This Open-Access Thesis is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Electronic Theses and Dissertations by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. FRACTURES, FLUIDS, AND METAMORPHISM: SHEAR ZONE INITIATION IN THE MARCY ANORTHOSITE MASSIF, ADIRONDACKS, NEW YORK, USA By James Hodge B.S. College of Saint Rose, 2017 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science (in Earth and Climate Sciences) The Graduate School The University of Maine August 2019 Advisory Committee: Scott Johnson, Professor and Director School of Earth and Climate Sciences, Advisor Chris Gerbi, Professor School of Earth and Climate Sciences, Advisor Alicia Cruz-Uribe, Professor School of Earth and Climate Sciences Martin Yates, Professor School of Earth and Climate Sciences FRACTURES, FLUIDS, AND METAMORPHISM: SHEAR ZONE INITIATION IN THE MARCY ANORTHOSITE MASSIF, ADIRONDACKS, NEW YORK, USA By James Hodge Thesis Advisors: Dr. -
The Good Germans the Hemmerles, Munich’S First Family of Jewelry, Design Baubles That Are Truly One of a Kind
Clockwise from left: Chris- tian and Stefan Hemmerle at home; Hemmerle’s 18k white gold, black iron and aquamarine ring, 18k red gold, moonstone, amethyst and sapphire brooch, and 18k white gold, red patinated copper, spinel and amethyst earrings, prices available upon request, at Hemmerle, 011.800.2422.6000. ccessories ∂lash ccessories a W The Good Germans The Hemmerles, Munich’s first family of jewelry, design baubles that are truly one of a kind. Photographs by S t e f a n K o r t e t’s not every client request that 230 pieces of haute joaillerie each year in its inspires a designer to branch off into a 12-artisan Munich workshop, is renowned direction he never before imagined— for its austere architectural settings ren- I and subsequently to develop an entirely dered in unorthodox materials including new style in doing so. But that’s exactly how copper, stainless steel, brass, aluminum and the German jewelry house Hemmerle came rare woods, and for its use of exquisitely to enjoy its current status as one of today’s cut colored gemstones. The heaviness of most inventive and sought-after jewelers. a masculine charcoal-hued iron band, for It all began in 1995, when a prominent instance, only enhances the sharp angles of Munich art collector commissioned Ste- an emerald-cut 40-carat electric blue aqua- fan Hemmerle, a third-generation jeweler, marine ring, while the warm hues of orange to create a birthday present for his wife, a and red patinated copper perfectly com- woman who detested flashy gems. -
Acetate C2H3O2 Or CH3COO Or CH3CO2 Ammonium NH4
Name:_____________________ Memorization For AP Chem Polyatmic Ions AP Chemistry Polyatomic Ion list - - - Acetate C2H3O2 or CH 3COO or CH 3CO 2 + Ammonium NH 4 - Ammonium Carbonate NH 4CO 3 Cyanide CN - 2- Carbonate CO 3 2- Dichromate Cr 2O7 - Dihydrogen phosphate H2PO 4 - Hydrogen carbonate HCO 3 - Hydrogen sulfate HSO 4 - Hydronium H3O Hydroxide OH - 2- Monohydrogen Phosphate HPO 4 - Nitrate NO 3 - Nitrite NO 2 2- Oxalate C2O4 - Permanganate MnO 4 3- Phosphate PO 4 2- Sulfate SO 4 2- Sulfite SO 3 Hypochlorite ClO - - Chlorite ClO 2 - Chlorate ClO 3 - Perchlorate ClO 4 2- Chromate CrO 4 2- Silicate SiO 3 Thiocyanate SCN - 2- Thiosulfate S2O3 - Bromate BrO 3 2- Selenate SeO 4 - Bisulfite HSO 3 Name:_____________________ Memorization For AP Chem Rules for Naming an Acid When the name of the anion ends in –ide, the acid name begins with the prefix hydro-, the stem of the anion has the suffix –ic and it is followed by the word acid. -ide becomes hydro _____ic Acid Cl- is the Chloride ion so HCl = hydrochloric acid When the anion name ends in –ite, the acid name is the stem of the anion with the suffix –ous, followed by the word acid. -ite becomes ______ous Acid - ClO 2 is the Chlorite ion so HClO 2 = Chlorous acid. When the anion name ends in –ate, the acid name is the stem of the anion with the suffix –ic, followed by the word acid. -ate becomes ______ic Acid - ClO 3 is the Chlorate ion so HClO 3 = Chloric acid. Rules for Naming Ionic Compounds 1. -
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 .................................... -
CHARON KRANSEN ARTS 817 WEST END AVENUE NEW YORK NY 10025 USA PHONE: 212 627 5073 FAX: 212 663 9026 EMAIL: [email protected]
CHARON KRANSEN ARTS 817 WEST END AVENUE NEW YORK NY 10025 USA PHONE: 212 627 5073 FAX: 212 663 9026 EMAIL: [email protected] www.charonkransenarts.com AUGUST. 2020 A JEWELER’S GUIDE TO APPRENTICESHIPS: HOW TO CREATE EFFECTIVE PROGRAMS suitable for shop owners, students as well as instructors, the 208 page volume provides detailed, proven approaches for finding , training and retaining valuable employees. it features insights into all aspects of setting up an apprenticeship program, from preparing a shop and choosing the best candidates to training the apprentice in a variety of common shop procedures. an mjsa publication. $ 29.50 ABSOLUTE BEAUTY – 2007catalog of the silver competition in legnica poland, with international participants. the gallery has specialized for 30 years in promoting contemporary jewelry. 118 pages. full color. in english. $ 30.00 ADDENDA 2 1999- catalog of the international art symposium in norway in 1999 in which invited international jewelers worked with jewelry as an art object related to the body. in english. 58 pages. full color. $ 20.00 ADORN – NEW JEWELLERY - this showcase of new jewelry offers a global view of exciting work from nearly 200 cutting-edge jewelry designers. it highlights the diverse forms that contemporary jewelry takes, from simple rings to elaborate body jewelry that blurs the boundaries between art and adornment. 460 color illustrations. 272 pages. in english. $ 35.00 ADORNED – TRADITIONAL JEWELRY AND BODY DECORATION FROM AUSTRALIA AND THE PACIFIC adorned draws on the internationally recognised ethnographic collection of the macleay museum at the university of sidney and the collections of individual members of the oceanic art society of australia.