Emeralds and Green Beryls of Upper Egypt
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The Red Emerald
The Red Emerald Black Album Words by Seth William Rozendaal Photos by David Rozendaal This work is for the enjoyment of gemstone aficionados around the world and throughout time, and dedicated to the divine muse who inspires everything. This book celebrates the Red Emerald’s public debut at the 2017 Tucson Gem and Mineral Show. Graphics taken from the Mineralogical Record Volume 47 Number 1: Colombian Emeralds where noted. The two photos of the Heart matrix specimen on the top of the page in Section VI were taken by Wayne Schrimp. Seth Rozendaal is responsible for the landscape photo in Section II, the beveled heart in Section VI and Office Suite Graphics. The Suite Treasure necklace photo in Section XIII was taken at the Brent Isenberger Studio. Cover and all other interior photos in this album were taken by David Rozendaal. Without his tireless dedication, this publication would not have been possible. For additional information, please contact: Seth William Rozendaal (515) 868-7207 [email protected] Index I - Red Beryl IS Red Emerald II - Formation III - Matrix Specimens IV - Wafers V - Prisms VI - Twins VII - Clusters VIII - Bixbyite Combinations IX - Topaz Combinations X - Hourglass Patterning XI - The Scarlet Spectrum XII - Facet-Grade Red Emerald XIII - The Red Emerald Suite Treasure I ~ Red Beryl IS Red Emerald The human infatuation with Emeralds runs so deep, and our desire for them traces so far back… It's one of the only gemstones found in rank-signifying Neolithic headdresses. Yeah, you heard me: Caveman Crowns. Aja Raden - Author, Historian and Scientist Diamonds may be forever, but only Emeralds are eternal; our appreciation of Emeralds stretches from the beginning of human civilization to the very end. -
Intergrown Emerald Specimen from Chivor Tity Was Confirmed by Raman Spectroscopy
Editor Nathan Renfro Contributing Editors Elise A. Skalwold and John I. Koivula Intergrown Emerald Specimen from Chivor tity was confirmed by Raman spectroscopy. The inclusion exhibited a well-formed hexagonal prismatic shape with Colombia’s Chivor emerald mines are located in the east- pyramid-like termination (figure 2). Although intergrowth ern zone of the Eastern Cordillera range of the Andes emerald crystals have been described and documented in Mountains. Chivor translates to “green and rich land” in the literature several times (G. Grundmann and G. Giu- Chibcha, the language of the indigenous people who were liani, “Emeralds of the world,” in G. Giuliani et al., Eds., already mining emerald more than 500 years ago, before Emeralds of the World, extraLapis English, No. 2, 2002, pp. the arrival of the Spanish conquistadors (D. Fortaleché et al., “The Colombian emerald industry: Winds of change,” Fall 2017 G&G, pp. 332–358). Chivor emeralds exhibit a bright green color with a tint of blue; they have relatively Figure 1. An emerald crystal inclusion measuring high clarity and fewer inclusions than emeralds found in ~2.67 × 2.71 × 5.43 mm is found inside this large Colombia’s western belt. emerald specimen (18.35 × 10.69 × 9.79 mm) from Colombia’s Chivor mine. Photo by John Jairo Zamora. The authors recently examined a rough emerald crystal specimen (figure 1), measuring 18.35 × 10.69 × 9.79 mm, reportedly from Chivor. This crystal weighed 3.22 g (16.10 ct) and had a prismatic hexagonal crystal shape. Standard gemological examination confirmed the gemstone to be emerald, and ultraviolet/visible/near-infrared (UV-Vis-NIR) spectroscopy showed a classic Colombian emerald absorp- tion spectrum. -
Fall 1996 Gems & Gemology Gem News
GEM Editors Mary L. Johnson and John I. Koivula Contributing Editors Dino DeGhionno, Robert C. Kammerling, Shane F, McClure, GIA GTL, Santa Monica, California Henry A. Hanni, SSEF, Basel, Switzerland Karl Schmetzer, Petershausen, Germany DIAMONDS plus other types, whereas type Da near-colorless natural Chatham synthetic "white" diamonds at JCK show. diamonds are relatively rare. Three years ago, Tom Chatham of Chatham Created Energy-dispersive X-ray fluorescence (EDXRF] spec- Gems, San Francisco, California, announced that he troscopy disclosed both iron (Fe)and germanium (Gel in would be marketing "white" synthetic diamonds from all four crystals. GIA Research had not previously detect- Russia for jewelry use. Although it took longer than he ed germanium in any diamond, natural or synthetic. originally anticipated, Mr. Chatham offered for sale a They suspect that Ge is being added to the growth envi- number of near-colorless synthetic diamond crystals at ronment of these crystals to prevent nitrogen from incor- the June 1996 JCK show in Las Vegas, Nevada. porating into the crystal structure of the synthetic dia- Mr. Chatham offered GLA Research a brief opportu- monds, as the nitrogen would color them yellow. nity to examine about 100 of these synthetic diamond Although all of these properties indicated that these crystals (which ranged from about 10 points to almost a samples were synthetics, conclusive proof was provided carat) before the show. Most were of small size and had most readily by the metallic inclusions, which were eye- too many inclusions for faceting. Research Associate visible in all four samples, and were easily identified with Sam Muhlmeister and Research Gemologist Shane Elen magnification. -
Garnet, Industrial 2016
2016 Minerals Yearbook GARNET, INDUSTRIAL [ADVANCE RELEASE] U.S. Department of the Interior September 2018 U.S. Geological Survey Garnet, Industrial By Robert M. Callaghan and Kenneth C. Curry Domestic survey data and table were prepared by Chanda C. Williams, statistical assistant. In 2016, U.S. production of crude garnet concentrate for combination with one or two other minerals, have reserves that industrial use was estimated to be 56,400 metric tons (t) valued can be mined at a low cost, and have the ability to react rapidly at about $12.8 million, a slight increase in tonnage and virtually to changes in market demand. The value of industrial garnet is unchanged in value from 55,200 t valued at $12.7 million in 2015. influenced by the size and grade of reserves, the type and quality U.S. production of refined garnet in 2016 was estimated to be of garnet mined, the proximity of deposits to infrastructure and 49,400 t valued at $24.4 million, a slight increase in tonnage and consumers, and the milling costs. The majority of industrial- a slight decrease in value from 48,700 t valued at $24.8 million grade garnet mined in the United States consists of almandine in 2015. U.S. exports of industrial garnet were 13,400 t, a 9% (iron-aluminum silicate) and pyrope (magnesium-aluminum decrease compared with those in 2015. Imports of garnet were silicate), although some andradite (calcium-iron silicate) also is estimated to be 150,000 t in 2016, a 38% decrease compared with mined domestically. -
Women's Position and Attitudes Towards Female Genital Mutilation in Egypt
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Springer - Publisher Connector Van Rossem et al. BMC Public Health (2015) 15:874 DOI 10.1186/s12889-015-2203-6 RESEARCH ARTICLE Open Access Women's position and attitudes towards female genital mutilation in Egypt: A secondary analysis of the Egypt demographic and health surveys, 1995-2014 Ronan Van Rossem1*, Dominique Meekers2 and Anastasia J. Gage2 Abstract Background: Female genital mutilation (FGM) is still widespread in Egyptian society. It is strongly entrenched in local tradition and culture and has a strong link to the position of women. To eradicate the practice a major attitudinal change is a required for which an improvement in the social position of women is a prerequisite. This study examines the relationship between Egyptian women’s social positions and their attitudes towards FGM, and investigates whether the spread of anti-FGM attitudes is related to the observed improvements in the position of women over time. Methods: Changes in attitudes towards FGM are tracked using data from the Egypt Demographic and Health Surveys from 1995 to 2014. Multilevel logistic regressions are used to estimate 1) the effects of indicators of a woman’ssocial position on her attitude towards FGM, and 2) whether these effects change over time. Results: Literate, better educated and employed women are more likely to oppose FGM. Initially growing opposition to FGM was related to the expansion of women’s education, but lately opposition to FGM also seems to have spread to other segments of Egyptian society. -
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 .................................... -
INCLUSIONS in AQUAMARINE from AMBATOFOTSIKELY, MADAGASCAR Fabrice Danet, Marie Schoor, Jean-Claude Boulliard, Daniel R
NEW Danet G&G Fall 2012_Layout 1 9/27/12 11:31 AM Page 205 RAPID COMMUNICATIONS INCLUSIONS IN AQUAMARINE FROM AMBATOFOTSIKELY, MADAGASCAR Fabrice Danet, Marie Schoor, Jean-Claude Boulliard, Daniel R. Neuville, Olivier Beyssac, and Vincent Bourgoin grams of translucent to transparent beryl were pro- duced, as well as several tonnes of opaque material In January 2012, aquamarine crystals containing for industrial use. While only a very small percentage interesting inclusions were extracted from the Am- was suitable for faceting, several hundred aqua- batofotsikely area northwest of Antsirabe, Mada- marines in the 1–35 ct range have been cut. In April gascar. These specimens displayed various types 2012, one of the authors (FD) traveled to the locality of eye-visible and microscopic inclusions, and and obtained representative samples. some had an unusual form. Raman microspec- troscopy identified reddish brown plate lets as Location and Geologic Setting. The workings are lo- hematite, while ilmenite was found as black cated less than 1 km north of Ambatofotsikely (a village platelets, black needles, and distinctive dark gray now locally known as Ambatofotsy Carole), 22 km dendrites. Similar inclusions are known in beryl north-northwest of Ankazomiriotra, and 74 km north- from Brazil, India, Mozambique, and Sri Lanka. west of Antsirabe. The deposit is centered at coordinates 19°27.662¢S, 46°27.450¢E, at an elevation of 1,010 m. The site is accessed by a paved road (RN 34) from ining activity near the central Malagasy village Antsirabe to a point 16 km west of Ankazomiriotra. of Ambatofotsikely was first documented nearly From there, a trail extends 15 km to Ambatofotsikely. -
The Journal of Gemmology Editor: Dr R.R
he Journa TGemmolog Volume 25 No. 8 October 1997 The Gemmological Association and Gem Testing Laboratory of Great Britain Gemmological Association and Gem Testing Laboratory of Great Britain 27 Greville Street, London Eel N SSU Tel: 0171 404 1134 Fax: 0171 404 8843 e-mail: [email protected] Website: www.gagtl.ac.uklgagtl President: Professor R.A. Howie Vice-Presidents: LM. Bruton, Af'. ram, D.C. Kent, R.K. Mitchell Honorary Fellows: R.A. Howie, R.T. Liddicoat Inr, K. Nassau Honorary Life Members: D.). Callaghan, LA. lobbins, H. Tillander Council of Management: C.R. Cavey, T.]. Davidson, N.W. Decks, R.R. Harding, I. Thomson, V.P. Watson Members' Council: Aj. Allnutt, P. Dwyer-Hickey, R. fuller, l. Greatwood. B. jackson, J. Kessler, j. Monnickendam, L. Music, l.B. Nelson, P.G. Read, R. Shepherd, C.H. VVinter Branch Chairmen: Midlands - C.M. Green, North West - I. Knight, Scottish - B. jackson Examiners: A.j. Allnutt, M.Sc., Ph.D., leA, S.M. Anderson, B.Se. (Hons), I-CA, L. Bartlett, 13.Se, .'vI.phil., I-G/\' DCi\, E.M. Bruton, FGA, DC/\, c.~. Cavey, FGA, S. Coelho, B.Se, I-G,\' DGt\, Prof. A.T. Collins, B.Sc, Ph.D, A.G. Good, FGA, f1GA, Cj.E. Halt B.Sc. (Hons), FGr\, G.M. Howe, FG,'\, oo-, G.H. jones, B.Se, PhD., FCA, M. Newton, B.Se, D.PhiL, H.L. Plumb, B.Sc., ICA, DCA, R.D. Ross, B.5e, I-GA, DGA, P..A.. Sadler, 13.5c., IGA, DCA, E. Stern, I'GA, DC/\, Prof. I. -
Gem-Quality Chrysoprase from Haneti-Itiso Area, Central Tanzania
GEM-QUALITY CHRYSOPRASE FROM HANETI-ITISO AREA, CENTRAL TANZANIA KARI A. KINNUNEN and ELIAS J. MALISA KINNUNEN, KARI A. and MALISA ELIAS J., 1990: Gem-quality Chrysoprase from Haneti-Itiso area, Central Tanzania. Bull. Geol. Soc. Finland 62, Part 2, 157—166. Gem-quality, apple-green, Ni-bearing chalcedonic quartz occurs as near-surface veins in silicified serpentinite in the Haneti-Itiso area, Central Tanzania. AAS de- terminations revealed a high Ni content, 0.55 wt.%, and low Co and Cr contents of 120 and 1 ppm respectively. NAA determination revealed near chondritic REE contents. X-ray diffraction determinations showed that the Chrysoprase consists main- ly of alpha quartz with some opal-CT. The gemmological properties are: refractive indices from 1.548 to 1.553 (±0.002), mean specific gravity 2.56, hardness about 7 on Moh's scale, inert to ultraviolet radiation, green through Chelsea filter, and absorption in the deep red and violet part of the optical absorption spectrum. The results confirm the identity of the material as Chrysoprase. Microscopically the Tanzanian Chrysoprase consists of spherules which are high- ly disordered, concentric, and composed of bipyramidal quartz, chalcedony, quart- zine, and opal-A. They were classified into four main types according to the shell arrangement. The diameter of the spherules ranged from 40 um to 77 um. Fluid inclusion types in the bipyramidal quartz were monophasic, low-temperature type. The spherules, silica types and REE contents suggest that this Chrysoprase was deposited by evaporation of surface waters connected with the silicification of the serpentinites. Genetically analogous formations, common in Africa, include M-fabric type, weathering profile silcretes. -
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 _____________________________________ -
Knowledge Hunt: Hall of Ancient Egypt
Hall of Ancient Egypt Third Floor Vocabulary (8 th Grade): Agricultural, ancient, ancestry, branches of government, capitol, civilization, coffin, dilapidated, drought, erode, flood plain, heritage, hieroglyphic, mummification, mummy, ruins, sarcophagus, script, society, temples, pyramids, Pharaoh Egypt: Gift of the Nile Which continent is Egypt located? What river runs through Egypt? After reading the text panel above, examine the map to answer the questions below. Notice the river running through Egypt and explain why the Nile River is the backbone of Egypt. What geographical formation could protect the Egyptians from foreign enemies? Extend your Knowledge! Keeping in mind what you know about the Nile River, why do you think Upper Egypt is south of Lower Egypt? Timeline of Egyptian History Look at the timeline above to answer the following questions. What famous Queen ruled Egypt during the Ptolemaic Egyptian time period (332 – 30 BC)? What culture surfaced in North America during Ptolemaic Egypt? Name two things that occurred in other parts of the world during the New Kingdom. 1. 2. According to the timeline, in what year was the Rosetta Stone created? Which time period came 1st, 2nd, and 3rd? New Kingdom, Old Kingdom, and Middle Kingdom. 1st: ______________________________ 2nd: ______________________________ 3rd: ______________________________ Map: Egypt Color and label the map with the 12 places listed below and include a compass rose. Use the text panels throughout this Knowledge Hunt to help you locate the areas listed. Lower Egypt -
Winter 2009 Gems & Gemology
G EMS & G VOLUME XLV WINTER 2009 EMOLOGY W INTER 2009 P AGES 235–312 Ruby-Sapphire Review V Nanocut Plasma-Etched Diamonds OLUME Chrysoprase from Tanzania 45 N Demantoid from Italy O. 4 THE QUARTERLY JOURNAL OF THE GEMOLOGICAL INSTITUTE OF AMERICA EXPERTISE THAT SPREADS CONFIDENCE. Because Public Education AROUND THE WORLD AND AROUND THE CLOCK. Happens at the Counter. ISRAEL 5:00 PM GIA launches Retailer Support Kit and website Cutter checks parameters online with GIA Facetware® Cut Estimator. NEW YORK 10:00 AM GIA Master Color Comparison Diamonds confirm color quality of a fancy yellow. CARLSBAD 7:00 AM MUMBAI 7:30 PM Laboratory technicians calibrate Staff gemologist submits new findings on measurement devices before coated diamonds to GIA global database. the day’s production begins. HONG KONG 10:00 PM Wholesaler views grading results and requests additional services online at My Laboratory. JOHANNESBURG 5:00 PM Diamond graders inscribe a diamond and issue a GIA Diamond Dossier® A $97.00 value, shipping and handling extra. All across the planet, GIA labs and gemological reports are creating a common language for accurate, unbiased gemstone GIA’s Retailer Support Kit has been developed to help evaluation. From convenient locations in major gem centers, to frontline detection of emerging treatments and synthetics, to online services that include ordering, tracking, and report previews — GIA is pioneering the technology, tools and talent sales associates educate the public about diamonds, that not only ensure expert service, but also advance the public trust in gems and jewelry worldwide. the 4Cs, and thoroughly explain a GIA grading report.