Spring 2002 Gems & Gemology
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The New IMA List of Gem Materials – a Work in Progress – Updated: July 2018
The New IMA List of Gem Materials – A Work in Progress – Updated: July 2018 In the following pages of this document a comprehensive list of gem materials is presented. The list is distributed (for terms and conditions see below) via the web site of the Commission on Gem Materials of the International Mineralogical Association. The list will be updated on a regular basis. Mineral names and formulae are from the IMA List of Minerals: http://nrmima.nrm.se//IMA_Master_List_%282016-07%29.pdf. Where there is a discrepancy the IMA List of Minerals will take precedence. Explanation of column headings: IMA status: A = approved (it applies to minerals approved after the establishment of the IMA in 1958); G = grandfathered (it applies to minerals discovered before the birth of IMA, and generally considered as valid species); Rd = redefined (it applies to existing minerals which were redefined during the IMA era); Rn = renamed (it applies to existing minerals which were renamed during the IMA era); Q = questionable (it applies to poorly characterized minerals, whose validity could be doubtful). Gem material name: minerals are normal text; non-minerals are bold; rocks are all caps; organics and glasses are italicized. Caveat (IMPORTANT): inevitably there will be mistakes in a list of this type. We will be grateful to all those who will point out errors of any kind, including typos. Please email your corrections to [email protected]. Acknowledgments: The following persons, listed in alphabetic order, gave their contribution to the building and the update of the IMA List of Minerals: Vladimir Bermanec, Emmanuel Fritsch, Lee A. -
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 .................................... -
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. -
Optical Properties of Common Rock-Forming Minerals
AppendixA __________ Optical Properties of Common Rock-Forming Minerals 325 Optical Properties of Common Rock-Forming Minerals J. B. Lyons, S. A. Morse, and R. E. Stoiber Distinguishing Characteristics Chemical XI. System and Indices Birefringence "Characteristically parallel, but Mineral Composition Best Cleavage Sign,2V and Relief and Color see Fig. 13-3. A. High Positive Relief Zircon ZrSiO. Tet. (+) 111=1.940 High biref. Small euhedral grains show (.055) parallel" extinction; may cause pleochroic haloes if enclosed in other minerals Sphene CaTiSiOs Mon. (110) (+) 30-50 13=1.895 High biref. Wedge-shaped grains; may (Titanite) to 1.935 (0.108-.135) show (110) cleavage or (100) Often or (221) parting; ZI\c=51 0; brownish in very high relief; r>v extreme. color CtJI\) 0) Gamet AsB2(SiO.la where Iso. High Grandite often Very pale pink commonest A = R2+ and B = RS + 1.7-1.9 weakly color; inclusions common. birefracting. Indices vary widely with composition. Crystals often euhedraL Uvarovite green, very rare. Staurolite H2FeAI.Si2O'2 Orth. (010) (+) 2V = 87 13=1.750 Low biref. Pleochroic colorless to golden (approximately) (.012) yellow; one good cleavage; twins cruciform or oblique; metamorphic. Olivine Series Mg2SiO. Orth. (+) 2V=85 13=1.651 High biref. Colorless (Fo) to yellow or pale to to (.035) brown (Fa); high relief. Fe2SiO. Orth. (-) 2V=47 13=1.865 High biref. Shagreen (mottled) surface; (.051) often cracked and altered to %II - serpentine. Poor (010) and (100) cleavages. Extinction par- ~ ~ alleL" l~4~ Tourmaline Na(Mg,Fe,Mn,Li,Alk Hex. (-) 111=1.636 Mod. biref. -
Sadanagaite and Magnesio.Sadanagaite, New Silica-Poor Members of Calcic Amphibole from Japan
American Mineralogist, Volume 69, pages 465471, 19E4 Sadanagaiteand magnesio.sadanagaite,new silica-poor membersof calcic amphibole from Japan Hrppnxo Sntrraezerr Geological Institute, Faculty of Science University of Tolcyo, Hongo, Tolcyo l13, Japan Mrcnrerr Buuxor Department of Mineralogy, The University Museum University of Tolcyo, Hongo, Tolcyo 113, Japan nxo Tonnu Ozewe Mineralogical Institute, Faculty of Science University of Tolcyo, Hongo, Tolcyo ll3, Japan Abstract Sadanagaite,(K,Na)CazGe2*,Mg,Al,Fe3*,Ti)r[(Si,AlhO22(OH)2] where Fe2* = Mg, Al = Fe3* and Si < 5.5, and its Mg-rich analogue,magnesio-sadanagaite Fe2+ < Mg, are extremely SiO2-poor new amphiboles, which require the compositional extension of the edenite-pargasiteseries, and amending of the classification and nomenclature of amphi- boles (Leake, 1978). Theseare monoclinic,C2, Cm or Cllm; a = 9.922(10),b : 1E.03(2),c : 5.352(9)4,B: 105.30(10f,Z = 2 for sadanagaitewith Si - 5.0, and a : 9.964(2),D : 18.008(3),c : 5.354(2)4,B = 105.55(2)",2= 2 for magnesio-sadanagaitewith Si:5.0. The strongest lines in the X-ray powder pattern for magnesio-sadanagaiteare: 8.48(80)(ll0), 3.39(40Xl3l), 3.28(100X240),3.15(70)(3r0), 2.951(50X22r),2.823(30)(330), 2.766(45)(33r), 2.707(60Xl5l),2.594(35X061),2.162(55)(261),1.654(30X461), thesebeing similar to thoseof X-ray powder patterns of SiO2-poorcalcic amphiboles, especially kaersutite. Both specieshave very similar physical properties, and are dark brown to black with a vitreousluster. Streak very light brown. -
Quartz: a Bull's Eye on Optical Activity
Quartz: a Bull’s Eye on Optical Activity Elise A. Skalwold The Mineralogical Society of America William A. Bassett Title: Quartz: a Bull’s Eye on Optical Activity Authors: Elise Ann Skalwold & William Akers Bassett Edition: First edition Publisher: Mineralogical Society of America, Chantilly, Virginia, USA Copyright: © 2015 by the authors, artists, and photographers. Reproduced with permission. All Rights Reserved. ISBN: 978-0-939950-00-3 Photographer & Designer: Elise A. Skalwold Front cover: Natural quartz crystal 60 x 65 x 40 mm; Hot Springs, Arkansas; ex. Dr. R.W.M. Woodside collection. Back cover: Lab-grown quartz cluster, 140 mm x 90 mm (hydrothermally grown by Mila and Vladimir A. Klipov, R&D XTALS, Inc.). Below: Natural quartz crystals and basal sections. On-going collaboration with Cornell’s Professor Emeritus William A. Bassett is truly priceless to me for this and other projects in the wings, as well as for those over the past eight years of work and research together. Bill shares my enthusi- asm for exploring the fascinating aspects of the classical science of mineralogy, and as my co-author he sets the highest bar for accuracy. All students should be so lucky to have such a mentor. Elise A. Skalwold, 2015 Ithaca, New York Mineralogical Society of America Quartz: a Bull’s Eye on Optical Activity Elise A. Skalwold [email protected] William A. Bassett [email protected] Both Authors: Department of Earth & Atmospheric Sciences Snee Hall, Cornell University Ithaca, NY 14853 All photographs: Elise A. Skalwold Figure 1. The “bull’s eye” uniaxial optic figure characteristic of quartz is indicative of its optical activity. -
General Information- Michigan's Gem Stones
CONTENTS: INDUSTRIES MAP —————— FACING I GENERAL INFORMATION- —————— I MICHIGAN'S GEM STONES- —————— 4 ASSAYS AND TESTS———— ————— I I ARTICLES, PERIODICALS, BOOKS- —————12 SOCIETIES—————————————————— ———— 23 MUSEUMS—————————————————— ———— 26 GEOLOGIC TIME SCALE ———— 30 GEOLOGIC MAP —————— ————— 3 I NMICHIGAN DEPARTMENT OF CONSERVATION ^GEOLOGICAL SURVEY DIVISION FREE DISTRIBUTION ONLY PREFACE TO THIRD EDITION The first edition, published in April, 1958 was needed in responding to queries following a mineral show on the Depart- ment T-V program "Michigan Conservation11. The second edition, July, 1959) was characterized by the addition of the section on gem stones* An abstracted version of the second edition titled "Pebbles to Pendants" was published in the July, 1958 issue of "Michigan Conservation". The present 'third edition is another major revision. Among the new materials added are: l) bedrock geologic map, 2) mineral industries map, 3) rock column and time scale, 4) mineral and fossil sketches, and 5) locality sketch maps* These, along with the cover, were prepared by Jim Campbell of our staff. The book list has been expanded and several titles were added to the articles list. Suggestions received from Arthur Johnstone, of the Michigan Mineralogical Society, were particularly helpful. Information regarding mineral and lapidary businesses may be found in the appropriate advertising media as well as from many of the clubs. Robert W. Kelley, Geologist Geological Survey Division Michigan Dept. Conservation March, I960 Lansing MICHIGAN'S MIN ERAL EXTRACTING INDUSTRIES D NON-METALLIC B BRINE H SALT 0 CLAY 0 SHALE 9 DOLOMITE H LIMESTONE 13 SAND& GRAVELCPRINCIPAL AREA) H GLASS SAND 0 GYPSUM B SANDSTONE D MARLCPRINCIPAL AREA) B PEAT • MISCELLANEOUS STONE A METALLIC L COPPER A IRON O FUELS <D GAS • OIL MAJOR FIELDS € OIL & GAS INDIANA O H I O GENERAL INFORMATION INTRODUCTION Interest in collecting minerals and gem stones and in doing lapidary work certainly is on the increase today. -
Occurrences of Grandidierite, Serendibite and Tourmaline Near Ihosy, Southern Madagascar
SHORT COMMUNICATIONS 131 tine, lavendulan, schoepite, vandendriesscheite, Collins, J. H. (1881) Catalogue of the Minerals in the kahlerite and metakahlerite are confirmed for the Museum of the Royal Institution of Cornwall, 2, 32. first time from the British Isles. Foshag, W. F. (1924)Am. Mineral. 9, 30-1. Goldsmith (1877) Proc. Acad. Nat. Sci. Philadelphia, Acknowledgements. For X-ray diffraction work, the 192. authors are grateful to the late Dr R. J. Davis of the Guillemin, C. (1956) Bull. Soc. franc. Min. Crist. 79, British Museum (Natural History), to Dr T. M. Seward, 7-95. then of the Geology Department, University of Man- Harrison, R. K., Tresham, A. E., Young, B. R. and chester, to Dr D. Rushton, then of the Manchester Lawson, R. I. (1975) Bull. Geol. Survey Great Britain, Museum, and to the staff of the Royal Scottish Museum. 52, 1-26. We thank Ian Brough of the Metallurgy Department, Macpherson, H. G. and Livingstone, A. (1982) Gloss- University of Manchester and U.M.I.S.T. for scanning ary of Scottish Mineral Species 1981. Scottish Journal electron microscope analysis. For their help in field work of Geology. we thank Dr George Ryback, Dr T. M. Seward and Miller, J. M. and Taylor, K. (1966) Bull. Geol. Survey Mr T. G. P. Ziemba. Great Britain, 25, 1-8. Weisbach, A. (1871)Neues Jahrb. Min. 869-70. -- (1877) Ibid., 1. References [Manuscript received 25 January 1989; Breithaupt, J. F. A. (1837)J. prakt. Chem. 10,505. revised 18 April 1989] Clark, A. M., Couper, A. G., Embrey, P. G. -
Khmaralite, a New Beryllium-Bearing Mineral Related to Sapphirine: a Superstructure Resulting from Partial Ordering of Be, Al, and Si on Tetrahedral Sites
American Mineralogist, Volume 84, pages 1650–1660, 1999 Khmaralite, a new beryllium-bearing mineral related to sapphirine: A superstructure resulting from partial ordering of Be, Al, and Si on tetrahedral sites JACQUES BARBIER,1,* EDWARD S. GREW,2 PAULUS B. MOORE,3 AND SHU-CHUN SU4 1Department of Chemistry, McMaster University, Hamilton, Ontario, L8S 4M1 Canada 2Department of Geological Sciences, University of Maine 5790 Bryand Center Orono, Maine 04469, U.S.A. 3P.O. Box 703, Warwick, New York,10990, U.S.A. 4Hercules Research Center, 500 Hercules Road, Wilmington, Delaware 19808, U.S.A. ABSTRACT 3+ 2+ Khmaralite, Ca0.04Mg5.46Fe 0.12Fe 1.87Al14.26Be1.43B0.02Si4.80O40, is a new mineral closely related to sapphirine from Khmara Bay, Enderby Land, Antarctica. It occurs in a pegmatite metamorphosed at T ≥ 820 °C, P ≥ 10 kbar. The minerals surinamite, musgravite, and sillimanite associated with khmaralite at Casey Bay saturate it in BeO, and thus its BeO content could be close to the maximum possible. Optically, khmaralite is biaxial (–); at λ = 589 nm, α = 1.725(2), β = 1.740(2), γ = 1.741(2), 2Vmeas = 34.4 (1.8)°, v > r strong, and β b. The weak superstructure reported using electron diffraction has been confirmed by single-crystal X-ray diffraction. The superstructure corresponds to a doubling of the a axis in monoclinic sapphirine-2M (P21/c setting) with the following unit-cell parameters: a = 3 19.800(1), b = 14.371(1), c = 11.254(1) Å, β = 125.53(1)°, Z = 4, Dcalc = 3.61 g/cm . -
Gemology with Kelly Sitek Ologies Podcast October 10, 2017
Gemology with Kelly Sitek Ologies Podcast October 10, 2017 Heeey, okay just a quick note up top, that this episode gets a little, like, woo-doo-to-doo, like a little mystical. We don’t not talk about the power of crystals in this. I wanted to know, as a gemologist, what this Ologist’s belief was in the mystical nature of rocks, if she believed in it. So, I hear her out, I also discuss the neuroscience of the placebo effect and how our thoughts can change our behaviors. It’s based in neuroscience. Try not to @ me about it ‘cause, like, I get it. Okay? Cool Episode 4 of Ologies, comin’ in hawt. First off, thanks to everyone who’s been listening and leaving reviews on iTunes, and rating, and subscribing. The more you do that, the higher this gets on the charts and the more people see it. And the more people share dumb science jokes, I guess, the better. I don't know. Also thank you to everyone who’s supporting on Patreon. I see you and I love you. And For everyone who had a hankering for merch and who’s been to OlogiesMerch.com. Cool shirt, or mug, or tote. Okay. Gems. This episode about gems is truly outrageous. Well, it’s pretty good. We don’t talk about crotches very much, but it's a pretty good episode. Let’s start with the etymology of gemology, it comes from ‘ology,’ the study of, and ‘gems,’ meaning gems. But ‘gems’ comes from an old dusty Latin word for.. -
Weight of Production of Emeralds, Rubies, Sapphires, and Tanzanite from 1995 Through 2005
Weight of Production of Emeralds, Rubies, Sapphires, and Tanzanite from 1995 Through 2005 By Thomas R. Yager, W. David Menzie, and Donald W. Olson Open-File Report 2008–1013 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Yager, T.R., Menzie, W.D., and Olson, D. W., 2008, Weight of production of emeralds, rubies, sapphires, and tanzanite from 1995 through 2005: U.S. Geological Survey Open-File Report 2008-1013, 9 p., available only online, http://pubs.usgs.gov/of/2008/1013. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. ii Contents Introduction ...................................................................................................................................1 Emeralds.......................................................................................................................................2 -
1 Optical Properties of Gem Substances
Optical Properties of Gem Substances Educational objective: This exercise, unit 7 in the above syllabus, will introduce students to skills and equipment that will continue to be used throughout the following modules. You should attempt to master these skills and the use of the equipment. The student should become familiar with the equipment, its application to solving gem problems, its proper use, and the precautions necessary to ensure both the safety of the student and the equipment. This lab may take up to two full meetings. Depending on equipment availability and time one or two setups for each experiment may be present. For each lab experiment, the student group will consist of 2 students. Groups are requested to make a 5 to 10 minute presentation using the digital Elmo overhead projector or a series of digital images (as in previous labs). There are some guiding questions for each exercise, but your overall grade is based on your presentation and discussion ensuing from it, plus observations of your behavior and preparedness in the lab. Images for your presentation are available in a “lab library” of images that you can pick and choose from as you see fit. The order in which the experiments will be presented does not have to correspond with the order they are presented here. 1. Refraction and the critical angle. Objectives. To observe the change in light’s path as it moves from one substance to another, record the angle of incidence and refraction, see total internal reflection, attempt to measure the critical angle, and learn about refractive index.