Franklin-Sterling 2017 Gem and Mineral Show

Total Page:16

File Type:pdf, Size:1020Kb

Franklin-Sterling 2017 Gem and Mineral Show Franklin-Sterling 2017 GEM & MINERAL SHOW SATURDAY, SEPTEMBER 23rd • 9-5 SUNDAY, SEPTEMBER 24th • 10-4 Littell Community Center FRANKLIN, NEW JERSEY The Fluorescent Mineral Capital of the World Miners Day and Volunteer Appreciation Day, Franklin Mineral Museum, May 7, 2017 Local miners and their families have been honored by the Franklin Mineral Museum for many years. Held on the first Sunday of May, Miners Day also honors museum volunteers. Attendance is by invitation, and the festivities include a buffet lunch, a concert by the famous Franklin Band, and awards to science students in local schools. Mineral collectors and citizens of New Jersey, thank these miners when you see them! They worked to mine our state's zinc and iron ores while recovering the mineral heritage displayed in museums here in Franklin and Sterling Hill, and at many other museums in our country and around the world. These miners worked at the Sterling Mine at Sterling Hill in Ogdensburg, N.J., with the exception of Bob Allen, a veteran of the Scrub Oaks Mine in Mine Hill, N.J. Left to right: Rich Gunderman, Bob Allen, Dick Bostwick (in front), Dom Lorenzo, Tom Laner, Steve Delmar, Mike Hallowich, Paul Rizzo, Andy Gancarcik, Al Restrepo, Chris Auer, Ed Keith, Lenny Talmadge (in back), Bernie Kozykowski, Harvey Barlow (in back), Doug Francisco, and Bill Rude. Sterling Hill miners who were present but missing from both photos are John Antal, Al Grazevich, Mike Gunderman, Ted Hanson, Fred Kirk, Steve Sanford, Henry Wisniewski, and John Yanish. Also present for Miners Day but missing from the photos is Ron Mishkin, who worked at Franklin in the sum- mers of 1952 and 1953, and later in iron mines near Dover. Photo by Tema Hecht. MINERAL SPECIES FOUND AT FRANKLIN-STERLING HILL, NJ Revised by the Mineral List Committee, August 2017 ([email protected] ) Bementite - F (TL), 0 Cuprostibite - F Acanthite - F,O Berthierite - 0 Cuspidine - F Actinolite - F,O Bianchite - 0 Cyanotrichite - 0 Adamite - F,O Bimessite - 0 Adelite - F,O Bomite - F,O Datolite - F Aegirine - F,O Bostwickite - F (TL) Descloizite - 0 Aegirine-augite - F Brandtite - 0 Devilline - 0 Akrochordite - 0 Breithauptite - F Digenite - 0 Albite - F,O Brochantite - F,0 Diopside - F,0 Allactite - F,O Brookite - F Djurleite - F,0 Allanite-(Ce) - F Brucite - F,0 Dolomite - F,0 Alleghanyite - F,0 Bultfonteinite - F Domeykite - F Almandine - F Bustamite - F (TL), 0 Dravite - F,0 Analcime - F Duftite - 0 Anandite - 0 Cahnite - F (TL) Dundasite - 0 Anatase - F Calcite - F,0 Dypingite - F,0 Andradite - F,0 Canavesite - 0 Anglesite - F,O Carrollite- F Edenite - F,0 Anhydrite - F,O Caryopilite - F,0 Epidote - F,0 Annabergite - F Celestine - F,0 Epsomite - 0 Annite - 0 Celsian - F Erythrite - F,0 Anorthite - F,0 Cerussite - F,0 Esperite - F (TL) Anorthoclase - F Chabazite-Ca - F,0 Euchroite - 0 Antigorite - F Chalcocite - F,0 Eveite - 0 Antlerite - F Chalcophanite- F,0 (TL) Aragonite - F,O Chalcopyrite - F,0 Fayalite - F,0 Arakiite - F Chamosite - F Feitknechtite - F (TL) Arsenic - 0 Charlesite - F (TL) Ferrimolybdite - 0 Arseniosiderite - 0 Chloritoid - F Ferro-actinolite - F Arsenolite - 0 Chlorophoenicite-F (TL) Ferrohomblende - 0 Arsenopyrite - F,O Chondrodite - F Flinkite - F Atacamite - F Chrysocolla - F,0 Fluckite - 0 Augite - F,O Chrysotile - F,0 Fluoborite - F,0 Aurichalcite - F,O Cianciulliite - F (TL) Fluorapatite - F,0 Aurorite - 0 Clinochlore - F,0 Fluorapophyllite-(K) - F,0 Austinite - F,O Clinoclase - 0 Fluorapophyllite-(Na) - F Axinite-(Fe) - F Clinohedrite - F (TL) Fluorite - F,0 Axinite-(Mn) - F (TL), 0 Clinohumite - 0 Fluorophlogopite - F,0 Azurite - F,O Clinozoisite - 0 Fluor-uvite - F (TL), 0 Clintonite - F Forsterite - 0 Bakerite - F Conichalcite - 0 Fraipontite - 0 Bannisterite - F (TL) Connellite - 0 Franklinfurnaceite-(TL) Bariopharmacosiderite - 0 Copper - F,0 Franklinite - F (TL), 0 Barite (IMA = baryte) - F,O Corundum - F,0 Franklinphilite - F (TL) Barylite - F Covellite - 0 Friedelite - F,0 Barysilite - F Cryptomelane - 0 Bassanite - 0 Cummingtonite - 0 Gageite - F (TL) Baumhauerite - 0 Cuprite - F,0 Gahnite - F,0 Galena — F,O Johannsenite — F (TL) Mimetite — F,0 Ganomalite — F Johnbaumite — F (TL), 0 Minehillite — F (TL) Ganophyllite — F Junitoite — F Molybdenite — F,O Genthelvite — F,O Monazite-(Ce) — F Gersdorffite — F Kaolinite — 0 Monohydrocalcite — 0 Gerstmannite — 0 (TL) Kentrolite — F Mooreite — 0 (TL) Glaucochroite — F (TL) Kittatinnyite — F (TL) Muscovite — F,0 Glaucodot — F Kolicite — F,O (TL) Goethite — F,O Kiittigite — 0 Nasonite — F (TL) Gold — 0 Kraisslite — 0 (TL) Natrolite — 0 Goldmanite — 0 Kutnohorite — F,O Nelenite — F (TL) Graeserite — 0 Neotocite — F,O Graphite — F,O Larsenite — F (TL) Newberyite — 0 Greenockite — F,O Laumontite — 0 Niahite — 0 Grossular — F,O Lavendulan — 0 Nickeline — F Groutite — F Lawsonbauerite — 0 (TL) Nontronite — 0 Grunerite — F Lead — F Norbergite — F,O Guerinite — 0 Legrandite — 0 Gypsum — F,O Lennilenapeite — F (TL) Ogdensburgite — 0 (TL) Leucophoenicite — F (TL) Ojuelaite — 0 Haidingerite — 0 Linarite — 0 Opal — F,0 Halotrichite — 0 Liroconite — 0 Orthoclase — F Hancockite—F(TL) Lizardite — F Orthoserpierite — 0 Hardystonite — F (TL) Lollingite — F,O Otavite — 0 Hastingsite — F,O Loseyite — F (TL) Hauckite — 0 (TL), F Parabrandtite — 0 (TL) Hausmannite — F Magnesiochlorophoenicite Paragonite — 0 Hawleyite — F,O F (TL) Pararammelsbergite — F Hedenbergite — F Magnesio-hornblende — F,0 Pararealgar — 0 Hedyphane — F Magnesio-riebeckite — F Parasymplesite — 0 Hellandite-(Y) — F Magnetite — F,O Pargasite — F Hematite — F,O Magnussonite — 0 Pectolite — F Hemimorphite — F,O Malachite — F,O Pennantite — F Hendricksite — F (To, 0 Manganberzeliite — F Petedunnite — F (TL) Hercynite — F,O Manganhumite — F Pharmacolite — 0 Hetaerolite — 0 (TL), F Manganite — F Pharmacosiderite — 0 Heulandite-Na — 0 Manganocummingtonite — F,O Phlogopite — 0 Hexahydrite — 0 Manganohornesite — 0 Picropharmacolite — 0 Hodgkinsonite —F(TL), 0 Manganosite — F Piemontite — 0 Holdenite — F (To, 0 Manjiroite — 0 Pimelite — F Hilbnerite — F Marcasite — F Powellite — F,O Humite — F,0 Margarite — F,O Prehnite — F Hydrohetaerolite — 0 (TL) Margarosanite — F (TL) Pumpellyite-(Mg) — F Hydrotalcite — F,0 Marialite — F Pyrite — F,O Hydroxyapophyllite-(K)—F Marsturite — F (TL) Pyroaurite — 0 Hydrozincite — F,0 Mcallisterite — 0 Pyrobelonite — F Mcgovernite — 0 (TL) Pyrochroite—F,0 Ilmenite — F Meionite — F,O Pyromorphite — 0 Meta-ankoleite — 0 Pyrophanite — 0 Jacobsite — F Metalodevite — 0 Pyrosmalite-(Mn) — 0 (TL) Jarosewichite — F (TL) Metazeunerite — 0 Pyroxferroite — F Jarosite — F Microcline — F,O Pyroxmangite — F,O Jerrygibbsite — F (TL) Miguelromeroite— 0 (TL) Pyrrhotite — F,O Quartz — F,O Spinel — F,0 Wollastonite — F,O Starkeyite — 0 Woodruffite — 0 (TL) Rammelsbergite — F Sterlinghillite — 0 (TL) Wulfenite — 0 Realgar — 0 Stibnite — 0 Wurtzite — 0 Reinerite - 0 Stilbite — 0 Retzian-(La) — 0 (TL) Stilpnomelane — F Xonotlite- F Retzian-(Nd) — 0 (TL) Strontianite — F Rhodochrosite — F,O Sulfur (IMA = sulphur) — 0 Yeatmanite — F (n), 0 Rhodonite — F,O Sussexite — F (TL), 0 Yukonite — 0 Ribbeite — F Synadelphite — 0 Richterite — F Synchysite-(Ce) — F Zincite — F (TL), 0 Roeblingite — F (TL) Szaibelyite — 0 Zinkenite — 0 Romeite I— F Zircon — F,0 Rosasite — F,O Talc — F,0 Znucalite — 0 Rouaite — 0 (TL) Tennantite — F,0 Roweite — F (TL) Tenorite — F Rutile — F,O Tephroite — 0 (TL), F Tetrahedrite — 0 Safflorite — F Thomsonite-Ca — F,O Samfowlerite — F (TL) Thorite — F Sarkinite — F,O Thortveitite — 0 Sauconite — 0 Thorutite — F Schallerite — F (TL) Tilasite — 0 Scheelite — F,0 Titanite — F,O Schorl — 0 Todorokite — F,O Sclarite — F (TL) Torreyite — 0 (TL) Scorodite — 0 Tremolite — F,O Seligmannite — 0 Turneaureite — F (TL) Sepiolite — F Uraninite — F,O Serpierite - 0 Uranophane — 0 Siderite — F,0 Uranospinite — 0 Sillimannite — 0 Silver — F,0 Vesuvianite — F,O Skutterudite — F Smithsonite — F,O Wallkilldellite — 0 (TL) Sonolite — 0 Wawayandaite — F (TL) Spangolite — 0 Wendwilsonite (TL) - 0 Spessartine — F,O Willemite — F,O Sphalerite — F,O In this list F = Franklin, 0 = Ogdensburg, (TL) = type locality, bold type = mineral unique to the Franklin-Ogdensburg area. Total Mineral Species Identified = 367 Total Unique Minerals = 19 (bold) https://www.facebook.com/Franklin-Mineral-Museum-145164278912640/timeline/ Driveway out of parking lot C Ramp outside — Entrance to building 7 8 9 /1 DaYlight Exhibits Entranceway 12 11 10 13 14 15 16 6 22 23 24 17 18 5 21 20 19 rs „ nidien 4 3 2 1 Garage Door Main Entranceway Driveway into parking area Drawing not to scale. Littell Community Center 'ooth # Dealer's Name 5ooth # Dealer's Name I Alan's Quality Minerals 14 AYS International 7- Stonetrust I5 The Mineral Cabinet 3 Fowlers Wire Wrapping Ifo Eccentricities 4 Michael Weinstein/Artifacts 11 Exotic Minerals 5 RAJ Minerals INC IS Sagicorp LLC 10 Land of Crystals Vi Amazon Imports 1 Jessie's Gems 2-0 Gary's Gem Garden 8 Michigan Rocks & Minerals 2I Gem Art Studio g Life In Art Minerals 7-2 Earth Art Gallery 10 China & South Seas, Inc. 23 Crystal Passion II Argentum Sales 24 Crystal Dawn Gems I2 Just Keep A Rockin 25 Casio Minerals Franklin – Sterling Show Fluorescent Exhibits Richard Bostwick - Exhibit Coordinator 1. Franklin Mineral Museum, Red With Desire, Green With Envy 2. Steven & Daniel Kuitems, Franklin Delights 3. Denis DeAngelis, Shortwave Sunshine 4. Alex Kerstanski, Vein Rocks 5. Mark Dahlman and Chris Luzier, Picture This 6. Len and Lenny Lee, Fabulous Fluorescents From Franklin Daylight Exhibits Steven Misiur—Exhibit Coordinator 1. Franklin Mineral Museum, Minerals of the Franklin Marble 2. Mark Mayfield, Found in The Field Since 2015 3. Steven Kuitems, Franklin Classics 4. Ken Reynolds, Classic Hemimorphite from Sterling Hill *Special Thanks to the Hardyston & Hamburg Boy Scouts Troop 187 for sponsoring the food!!! Want to display in the exhibits or be a dealer next year please email: [email protected] Fluorescent Minerals of Franklin and Sterling Hill, N.J. A 2017 CHECK-LIST BASED ON OBSERVATIONS OF CONFIRMED SPECIMENS By Richard Bostwick, with the assistance of Earl Verbeek, Mark Boyer, Paul Shizume, Steven Kuitems, Richard Keller, Paul Can and others.
Recommended publications
  • Mineral Processing
    Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
    [Show full text]
  • Single Crystal Raman Spectroscopy of Selected Arsenite, Antimonite and Hydroxyantimonate Minerals
    SINGLE CRYSTAL RAMAN SPECTROSCOPY OF SELECTED ARSENITE, ANTIMONITE AND HYDROXYANTIMONATE MINERALS Silmarilly Bahfenne B.App.Sci (Chem.) Chemistry Discipline This thesis is submitted as part of the assessment requirements of Master of Applied Science Degree at QUT February 2011 KEYWORDS Raman, infrared, IR, spectroscopy, synthesis, synthetic, natural, X-ray diffraction, XRD, scanning electron microscopy, SEM, arsenite, antimonate, hydroxyantimonate, hydrated antimonate, minerals, crystal, point group, factor group, symmetry, leiteite, schafarzikite, apuanite, trippkeite, paulmooreite, finnemanite. i ii ABSTRACT This thesis concentrates on the characterisation of selected arsenite, antimonite, and hydroxyantimonate minerals based on their vibrational spectra. A number of natural arsenite and antimonite minerals were studied by single crystal Raman spectroscopy in order to determine the contribution of bridging and terminal oxygen atoms to the vibrational spectra. A series of natural hydrated antimonate minerals was also compared and contrasted using single crystal Raman spectroscopy to determine the contribution of the isolated antimonate ion. The single crystal data allows each band in the spectrum to be assigned to a symmetry species. The contribution of bridging and terminal oxygen atoms in the case of the arsenite and antimonite minerals was determined by factor group analysis, the results of which are correlated with the observed symmetry species. In certain cases, synthetic analogues of a mineral and/or synthetic compounds isostructural or related to the mineral of interest were also prepared. These synthetic compounds are studied by non-oriented Raman spectroscopy to further aid band assignments of the minerals of interest. Other characterisation techniques include IR spectroscopy, SEM and XRD. From the single crystal data, it was found that good separation between different symmetry species is observed for the minerals studied.
    [Show full text]
  • Shin-Skinner January 2018 Edition
    Page 1 The Shin-Skinner News Vol 57, No 1; January 2018 Che-Hanna Rock & Mineral Club, Inc. P.O. Box 142, Sayre PA 18840-0142 PURPOSE: The club was organized in 1962 in Sayre, PA OFFICERS to assemble for the purpose of studying and collecting rock, President: Bob McGuire [email protected] mineral, fossil, and shell specimens, and to develop skills in Vice-Pres: Ted Rieth [email protected] the lapidary arts. We are members of the Eastern Acting Secretary: JoAnn McGuire [email protected] Federation of Mineralogical & Lapidary Societies (EFMLS) Treasurer & member chair: Trish Benish and the American Federation of Mineralogical Societies [email protected] (AFMS). Immed. Past Pres. Inga Wells [email protected] DUES are payable to the treasurer BY January 1st of each year. After that date membership will be terminated. Make BOARD meetings are held at 6PM on odd-numbered checks payable to Che-Hanna Rock & Mineral Club, Inc. as months unless special meetings are called by the follows: $12.00 for Family; $8.00 for Subscribing Patron; president. $8.00 for Individual and Junior members (under age 17) not BOARD MEMBERS: covered by a family membership. Bruce Benish, Jeff Benish, Mary Walter MEETINGS are held at the Sayre High School (on Lockhart APPOINTED Street) at 7:00 PM in the cafeteria, the 2nd Wednesday Programs: Ted Rieth [email protected] each month, except JUNE, JULY, AUGUST, and Publicity: Hazel Remaley 570-888-7544 DECEMBER. Those meetings and events (and any [email protected] changes) will be announced in this newsletter, with location Editor: David Dick and schedule, as well as on our website [email protected] chehannarocks.com.
    [Show full text]
  • Open-File Report 96-513-A. Significant Metalliferous And
    PUBANN.DOC-September 17,1996 Open-File Report 96-513-A. Significant metalliferous and selected non-metalliferous lode deposits and placer districts for the Russian Far East, Alaska, and the Canadian Cordillera, by Warren J. Nokleberg, Thomas K. Bundtzen, Kenneth M. Dawson, Roman A. Eremin, Nikolai A. Goryachev, Richard D. Koch, Vladimir V. Ratkin, Ilya S. Rozenblum, Vladimir I. Shpikerman, and Yuri F. Frolov, Mary E. Gorodinsky, Vladimir D. Melnikov, Nikolai V. Ognyanov, Eugene D. Petrachenko, Rimma I.Petrachenko, Anany I. Pozdeev, Katherina V. Ross, Douglas H. Woodv Donald Grybeck, Alexander I. Khanchuck, Lidiya I. Kovbas, Ivan Ya. Nekrasov, and Anatoloy A. Sidorov, 1996, 385 p. This report is a written tabular compilation of the significant metalliferous and selected non-metalliferous lode deposits and placer districts of the Russian Far East, Alaska, and the Canadian Cordillera. The report provides detailed summaries of the important features of the significant lode deposits and placer districts along with a summary of mineral deposit models, and a bibliography of cited references. Data are provided for 1,079 significant lode deposits and 158 significant placer districts of the region. This version of the report is issued on standard paper (Open-File Report 96-513-A). A subsequent digital version will be issued on CD-ROM (Open-File Report 96-513-B). The digital version will contain the introduction, description of mineral deposit models, and bibliography of cited references in ASCII (TXT) and RTF (Rich-Text Format) formats, and the mineral-deposit and placer district tables in dBase 3/4, FileMaker Pro 2.0, and tab-delineated text (TXT) formats.
    [Show full text]
  • Formulae of Selected Arsenic Minerals Are Listed in Chapter 2, APPENDIX 1 (P
    INDEX Arsenic minerals (in which As is essential to the crystal structure) Formulae of selected arsenic minerals are listed in Chapter 2, APPENDIX 1 (p. 174-183). abernathyite 145 274, 280-282, 295, 297, 301, adamite 23, 31, 39, 44, 115, 116, 118, 240, 304, 317, 350, 355-357, 359, 243, 311, 474, 476, 594, 610-615, 361, 366, 436, 473-475, 477, 620, 624, 627 483, 486, 490-492, 494-497, adelite 23, 111, 112, 476, 477, 519 537, 539, 542, 544, 546, 549, aerugite 130 554, 559, 561-564, 567, 571, agardite 75, 111, 624 574-578, 581, 624 akrochordite 23, 88, 95, 96 arsenovanmeersscheite 145 alarsite 26, 84, 85, 90 arsentsumebite 95, 610-613, 624 algodonite 23 arsenuranospathite 145 alacranite 28, 29 arsenuranylite 145 allactite 23, 24, 104, 124 arthurite 120, 121, 144, 474, 476 alumopharmacosiderite 39, 43, 75, 109 asbecasite 24, 133, 139 andyrobertsite 100, 101, 624 asselbornite 145 angelellite 26, 33, 36, 118, 312, 348, 364 atelestite 128 annabergite 23, 26, 48, 51, 57, 69, attikaite 75, 144 73-76, 96, 274, 476, 627 auriacusite 118 arakiite 143, 144 austinite 23, 112, 244, 474, 476, 594, ardennite 25 612, 613, 620, 624, 627 arhbarite 107 barahonaite-(Al) 75, 144, 146 armangite 23, 131, 138, 141, 142 barahonaite-(Fe) 146 arsenbrackebuschite 95, 624 barian tomichite 140 arsendescloizite 112, 476, 624 bariopharmacosiderite 23, 33, 34, 109 arsenic, native or elemental 3, 4, 218, baumhauerite 23 248, 266, 272, 274, bayldonite 65, 67, 74, 75, 97, 244, 476, 357, 475, 476, 612 594, 602, 603, 610-613, arseniopleite 23, 122 617-619, 621, 624, 627 arseniosiderite
    [Show full text]
  • View of Previous Workers’ Attempts at Dating and Thus Constraining the Timing of Ore Formation in The
    Geochronology, Isotope Geochemistry, and Molybdenum Distribution in the Central African Copperbelt: Examples from Chibuluma West, Kamoa, and Kipushi by Samuel Bowman A thesis submitted in partial fulfilment of the requirements for the degree of Master of Science Department of Earth and Atmospheric Sciences University of Alberta © Samuel Bowman, 2018 ii Abstract The Chibuluma West, Kamoa, and Kipushi stratiform deposits of the Central African Copperbelt have been evaluated using a series of geochemical techniques to better constrain the timing and origin of these deposits, with relevance to the origin of the Copperbelt as a whole. Petrographic, isotopic (Os, Pb, and O), and Mo distribution analyses have determined four mineralization events, occurring before, during, and after the Lufilian orogeny. A possible preenrichment event occurred throughout deposition of the Sturtian glaciation. The glacier scoured and carried U-rich lithic clats from the basement before depositing the Grand Conglomerate (host rock of Kamoa deposit). Radiogenic lead is likely the cause of apparent diagenetic model lead ages for other deposits throughout the Central African Copperbelt. The second mineralization event occurred during the Lufilian orogeny. The Chibuluma West and Kamoa deposits experienced the majority of ore mineralization ~550 to 540 Ma and ~510 to 480 Ma respectively. The Kamoa deposit is unfolded and unmetamorphosed, allowing the true age of the stratiform mineralization to be placed in the late stage of the Lufilian orogeny. The ores of these deposits were likely sourced from the crust. The third mineralization event occurred after the Lufilian orogeny. The ores of the Kipushi deposit mineralized <430 Ma. A new geothermometric approach, using oxygen diffusion in syn-ore dolomite has been successfully shown to estimate fluid temperatures.
    [Show full text]
  • Leiteiteo Znasronz a Novel Type of Tetrahedral Layer Structure With
    American Mineralogist, Volume 72, pages 629-632, 1987 Leiteiteo ZnAsrOnzA novel type of tetrahedral layer structure with arsenitechainst SusRAraGnosr Mineral PhysicsGroup, Department of Geological Sciences,University of Washington, Seattle,Washington 98195, U.S.A. P. K. SnN Gupra Department of Geology, Memphis State University, Memphis, Tennessee38152, U.S.A. E. O. ScHr,nlrpnn Department of Chemistry, University of Missouri, Columbia, Missouri 6521I, U.S.A. Ansrucr Leiteite, ZnAsrOo,from Tsumeb,Namibia, is monoclinic, a: 4.542(l), b: 5.022(l), c : 17.597(l A, B : 90.81(3F,space group P2r/c, Z: 2. The crystalstructure has been determined by direct methods and refined by the method of least squaresto an R factor of 0.048 based on 731 independent reflections measured on an automatic single-crystal X-ray diffractometer. The crystal structure consistsof open Zn tetahedral sheetsflanked by single arsenite chains on either side. The composite layers are cross-linked through weak (2.8-3.3 A1 es-O bonds. kiteite representsa new structure type. The averagetet- rahedral Zn-O distanceis 1.99 A, and the averageAs-O distancesand O-AFO anglesin the two distinct trigonal pyramidal arsenite groups are 1.79 A, 95.5" for As(l) and 1.78 A, 95.8"for As(2). INrnooucrroN ExpnmlrBNur- The rare zinc arsenite mineral leiteite, ZnAsrOo, was The chemical composition of leiteite from Tsumeb is discovered by Luis Teixeira kite from the oxidation zone (ZnonrFeoor)AsrOo(Cesbron et al., 1977). For the purposes of in Tsumeb, Namibia. It occurs in associationwith ten- crystal-structuredetermination, we have assumedthe ideal com- nantite, chalcocite,smithsonite, and schneiderhiihnite.Its position ZnAsrOo.
    [Show full text]
  • NVMC Apr 2020 Newsletter.Pdf
    The Mineral Newsletter Meeting (unless canceled): April 27 Time: 7:45 p.m. Long Branch Nature Center, 625 S. Carlin Springs Rd., Arlington, VA Volume 61, No. 4 April 2020 Explore our website! April meeting might be canceled! Our meeting room is closed for now—details on page 6 In this issue … Mineral of the month: Orpiment ............. p. 2 April program details ................................ p. 6 President’s collected thoughts ................. p. 6 Combing Calvert Cliffs .............................. p. 7 Quartz ....................................................... p. 8 The newsletter that wasn’t ...................... p. 10 Virginia state fossil .................................... p. 11 Orpiment Bench tip: Cutting a bolt ........................... p. 11 Georgeite and reinerite ............................ p. 12 Twin Creeks Mine, Nevada Source: Wikipedia; photo: Robert Lavinsky. Field trip opportunities ............................. p. 14 EFMLS: Safety matters ............................. p. 14 Note! AFMS: Code of Ethics ............................... p. 15 Coronavirus transmission remains a high risk. Before EFMLS: Wildacres in the fall ..................... p. 15 attending any event, including the April NVMC meet- ing, make sure it is actually being held! Upcoming events ................................... p. 17 Mineral of the Month Orpiment by Sue Marcus Happy Easter! Our April Mineral of the Month is orpiment, a lovely, toxic mineral that can crumble to powder. It is an arse- Northern Virginia Mineral Club nic sulfide (As2S3). Its name, orpiment, is an allusion to its color and an early use, Auripigmentum—Latin members, for gold (auri) pigment (pigmentum). Read on, for not The Long Branch Nature Center where our club all orpiment turns to dust. meets is temporarily closed, as are most restaurants. Igneous Origins Plans for our speaker on April 27, Linda Benedict, are Fumeroles and volcanically heated orifices like hot on hold.
    [Show full text]
  • Reinerite, Zng(Asoa)2T Br Trs€Rite with a Novel Type of Zn-Tehahedral
    American Mineralogist, Volume 62, pages ll29-1134, 1977 Reinerite, Zng(AsOa)2tBr trs€rite with a noveltype of Zn-tehahedral doublechainr SusRere GHose, Pe.ul BovING,WIlr-Illr A. LlCHe.psLLEAND CHr'Nc WeN Department of Geological Sciences, Uniuersity of Washington Seattle, Washington98 I 95 Abstract Reinerite,Znr(AsOs)z from Tsumeb,S. W. Africa, is orthorhombic, with cell dimensionsa = 6.092(2),b : 14.407(2),c : 7.811(l)A, space group Pbam and Z : 4. The crystal structure has been determinedby the symbolic addition method and differenceFourier synthesisand refined by the method of least squaresto an R factor of 0.051 based on 1289 reflections, measuredon an automatic single-crystaldiffractometer. The standarddeviation in Zn-O and As-O bond lengthsis 0.003 and 0.0044 and in O-Zn-O and O-As-O angles0.02". The structureof reineritecontains a new type of Zn-tetrahedraldouble chain, [ZnoOro]-, with two-tetrahedralrepeat and four-memberedrings; thesedouble chains are cross-linked into a three-dimensional framework through corner-sharing of a new type of edge-sharingZn- tetrahedraldimers and two types of trigonal pyramidal arsenitegroups. The averageZn-O bond distanceswithin the two independentZn-O tetrahedraare 1.958and 1.964A.Both the arsenitegroups have the point symmetry m, wilh averageAs-O bond distances1.776 and l.77lA and averaseO-As-O bond aneles98.4 and 96.8'. lntroduction : 2n and hol, h : 2r present. Of the two possible spacegroups, Pbam and Pba2, the first proved to be In the course of our investigation of the stereo- correct on the basisof an l(z)-test of the measured cheniistryof copper and zinc (Ghose and Wan, 1974; X-ray diffraction intensities.
    [Show full text]
  • Handheld Raman Library
    Compact Rugged Spectrometers - A Universe of Spectroscopy Systems Handheld Raman Library StellarRAM – Mineral Raman Library StellarNet Inc., Tampa FL, USA StellarNet proudly announces a mineral database for StellarRAM handheld Raman systems. The database includes over 200 minerals. This database and library can only be used with our StellarRAM handheld Raman system. It is included with the purchase of the instrument. If the mineral you are trying to measure is not listed you can always add additional library items to the database.
    [Show full text]
  • 62Nd Annual Franklin-Sterling Gem and Mineral Show – 2018
    Franklin-Sterling 2018 GEM & MINERAL SHOW SATURDAY, SEPTEMBER 29th • 9-5 SUNDAY, SEPTEMBER 30th • 10-4 Littell Community Center FRANKLIN, NEW JERSEY The Fluorescent Mineral Capital of the World Miners Day and Volunteer Appreciation Day, Franklin Mineral Museum, May 6, 2018 Local miners and their families have been honored by the Franklin Mineral Museum for many years. Held on the first Sunday of May, Miners Day also honors museum volunteers. Attendance is by invitation, and the festivities include a buffet lunch, a concert by the famous Franklin Band, and awards to science students in local schools. Mineral collectors and citizens of New Jersey, thank these miners when you see them! They worked to mine our state's zinc and iron ores while recovering the mineral heritage displayed in museums here in Franklin and Sterling Hill, and at many other museums in our country and around the world. Miners and other New Jersey Zinc Company employees attending this year's Miners Day: John Anderson, Al Grazevich, Bob Allen, Fred Kirk, Stephen Dekmar, Josef Man6k, John Antal, Bill Rude, Paul Rizzo, Bernard Kozykow- ski, Tom Laner, Steve Sanford, Edward Hamilton, Ted Hanson, Doug Francis- co, Richard Bostwick, Christopher Allen. Photo by Kristofor Giordano. Web: www.franklinmineralmuseum.com • Email: [email protected] MINERAL SPECIES FOUND AT FRANKLIN-STERLING HILL, NJ Revised by the Mineral List Committee, August 2017 ([email protected] ) Bornite - F,O Diopside - F,0 Acanthite - F,O Bostwickite - F (TL) Djurleite - F,0 Actinolite -
    [Show full text]
  • New Mineral Names*
    American Mineralogist, Volume 93, pages 1686–1691, 2008 New Mineral Names* PAULA C. PIILONEN ,1,† GLENN POIRIER,1 AND KIMBERLY T. TAI T 2 1Mineral Sciences Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada 2Department of Natural History, Royal Ontario Museum, 100 Queen’s Park, Toronto, Ontario M5S 2C6, Canada CALVER T I T E * Single-crystal X-ray studies of a grain removed from a pol- J.L. Jambor, A.C. Roberts, L.A. Groat, C.J. Stanley, A.J. Criddle, ished section indicate the mineral is cubic, with a = 5.337(1) with allowable space groups of Fm3m, F432, and F43m. A and M.N. Feinglos (2007) Calvertite, Cu5Ge0.5S4 , a new mineral species from Tsumeb, Namibia. Can. Mineral., 45, re-analysis a year later of the same single crystal produced no 1519–1523. reflections, but the original powder sample showed no change after 11 years. Calvertite was discovered during the examination of another The authors suggest that the small unit cell and the un- new mineral (gallobeaudanite) from the Tsumeb mine. The un- stable character of calvertite indicate that it is a metastable, oxidized portions of the sample in which calvertite was found highly disordered mineral whose ordered equivalent would consist mainly of calvertite and reinerite with minor tennantite be Cu10GeS8 with a = 2 × 5.337 Å. It is named for Lauriston and gallite inclusions. Calvertite occurs in a granular texture (Larry) Derwent Calvert (1924–1993) of the National Research formed by a network of chalcocite veins. The calvertite grains Council, Ottawa, Canada.
    [Show full text]