33831: Uncommon and Rare Minerals
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Bereichs- Fahrplan
Ausgabe 2016 Alles was ich will! Bereichs- fahrplan Alle Informationen rund um AST, Bus und Bahn inklusive Fahrplanauszüge gültig von 13.12.2015 bis 10.12.2016 (Die Fahrpläne der alten Ausgabe sind ab dem Fahrplanwechsel Mitte Dezember 2015 nicht mehr gültig.) Mit freundlicher Unterstützung von: Linienverzeichnis Bahnlinie R42 (Bestwig/Brilon Stadt) – Brilon Wald – Willingen – Korbach – Frankenberg – Marburg/L. ..................................... S. 4 Kostenlose Fahrt mit SauerlandCard zwischen Brilon und Willingen Bf. Kostenlose Fahrt mit MeineCardPlus im Bereich Willingen – Frankenberg. (Willingen – Ernsthausen = NVV-Tarif, ansonsten DB-Tarif) Buslinie 382 Willingen – Brilon Wald – Brilon ............................................ S. 14 Kostenlose Fahrt mit SauerlandCard auf gesamter Strecke. (Willingen – Brilon = Ruhr-Lippe-Tarif) Buslinie 486 Brilon – Gudenhagen – Willingen .......................................... S. 16 Kostenlose Fahrt mit SauerlandCard auf gesamter Strecke. Liebe Gäste, liebe Willinger, (Willingen – Brilon = Ruhr-Lippe-Tarif) die Zahl der Fahrtstrecken, Haltestellen und Verkehrsmittel ist Buslinie 506 sowohl im Verkehrsgebiet des Nordhessischen VerkehrsVerbundes Willingen – Schwalefeld – Rattlar – Diemelsee – (NVV) als auch im Bereich des Landkreises Waldeck-Frankenberg Bad Arolsen – Marsberg ....................................................... S. 18 und des angrenzenden Hochsauerlandkreises so umfangreich, Kostenlose Fahrt mit SauerlandCard und MeineCardPlus auf gesamter Strecke. dass ein dickes Buch zu -
Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Bestwig & Meschede 2021
Bestwig & Meschede 2021 www.hennesee-sauerland.de HerzlichHerzlich willkommen willkommen Herzlich willkommen im Sauerland, herzlich willkommen in ferienregion_hennesee der Ferienregion „Rund um den Hennesee“. Der wunderschö- Touristinfo.Bestwig. ne Hennesee in der Mitte und rundherum ein attraktives Meschede Mittelgebirge bis 750 m ü.NN - so präsentieren sich Ihnen Meschede und Bestwig - sehr zentral im Sauerland gelegen. Zahlreiche Wander- und Radwege durchziehen die waldreiche Landschaft. Gepflegte Dörfer mit hochwertigen Hotels und Gasthöfen laden zur Einkehr ein. Meschede, die Kreis- und Hochschulstadt, steht für geschäftiges Leben in intakter Landschaft. Der Hennesee-Boulevard verbindet die Stadt mit dem Hennesee. Bestwig ist stolz auf einige bedeutende Freizeitziele im Sauerland: der Freizeitpark Fort Fun Aben- teuerland, das Erlebnisbergwerk Schieferbau Nuttlar, das Sauerländer Besucherbergwerk Ramsbeck. Wir freuen uns auf Ihren Besuch! Ihre Tourist-Informationen „Rund um den Hennesee“ und alle Gastgeber. 2 Anreise Nur eine Stunde Fahrzeit vom Ruhrgebiet entfernt liegt unser Feriengebiet um Bestwig und Meschede - mit direktem Anschluss an die Autobahn 46. Tourist-Informationen „Rund um den Hennesee“ Tourist-Info Bestwig Bundesstraße 139 59909 Bestwig Sauerland Tel. 02904-712810 Tourist-Info Meschede Le-Puy-Straße 6-8 59872 Meschede Tel. 0291-9022443 Öffnungszeiten Unser Team ist für Sie zu folgenden Zeiten erreichbar: 1. Mai - 30. September: Mo-Fr 9-13 Uhr und 14-18 Uhr, Sa 10-13 Uhr 1. Oktober - 30. April: Mo-Fr 9-13 Uhr und 14-17 Uhr, Sa 10-13 Uhr E-Mail: [email protected] www.hennesee-sauerland.de Lörmecketurm Inhalt S. 4-9 Das Sauerland erleben - Wandern, Radfahren, Ausflugsziele, Sparangebote u.v.m. S. 10-13 Pauschalangebote S. -
Trainini Model Railroad Magazine
October 2020 Volume 16 • Issue 183 International Edition Free, electronic magazine for railroad enthusiasts in the scale 1:220 and Prototype www.trainini.eu Published monthly Trainini no guarantee German Magazine for Z G auge ISSN 2512-8035 Along the Ruhr and the Diemel Railway Lines along Wine Mountainsides A German Oddity Trainini ® International Edition German Magazine for Z Gauge Introduction Dear Readers, If I were to find a headline for this issue that could summarise (almost) all the articles, it would probably have to read as follows: “Travels through German lands”. That sounds almost a bit poetic, which is not even undesirable: Our articles from the design section invite you to dream or help you to make others dream. Holger Späing Editor-in-chief With his Rhosel layout Jürgen Wagner has created a new work in which the landscape is clearly in the foreground. His work was based on the most beautiful impressions he took from the wine-growing regions along the Rhein and Mosel (Rhine and Moselle). At home he modelled them. We like the result so much that we do not want to withhold it from our readers! We are happy and proud at the same time to be the first magazine to report on it. Thus, we are today, after a short break in the last issue, also continuing our annual main topic. We also had to realize that the occurrence of infections has queered our pitch. As a result, we have not been able to take pictures of some of the originally planned layouts to this day, and many topics have shifted and are now threatening to conglomerate towards the end of the year. -
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 -
Nuttlar Viaduct Unites Regions at a Height of 115 Metres
Sborník 21. Betonářské dny (2014) Sekce ST2A: Vyzvané přednášky NUTTLAR VIADUCT UNITES REGIONS AT A HEIGHT OF 115 METRES Gero Marzahn Hans Grassl Gerhard Dieter Guido Bogdan Buddenkotte Schummer Abstract The Nuttlar motorway viaduct is currently under construction in North Rhine Westphalia, the most populated area in Germany with 18 million inhabitants. Because of its exposed position, it sets extreme technical demands on the engineers in terms of the design and implementation of the construction work. With a total length of 660 metres, it spans the deep valley of the Schlebornbach at a height of 115 metres (pier height 110 metres). It is part of the new 5.6 km section of the A46 between Bestwig/Velmede and Nuttlar. Supported on six piers, the structure creates a well-proportioned geometry with seven spans and ensures that impact on the landscape is minimised. Designed as a composite- steel bridge, the steel superstructure was inserted over a maximum single span of 115 metres without the aid of auxiliary supports or pylons using an incremental launching method, something completely new for Germany. The slab for the bridge deck has been poured section-by-section since April. The viaduct is designed for a cross-section of RQ 26 with a usable width of 28.60 metres between the rails. Klíčová slova: motorway viaduct, incremental launching method, composite-steel bridge 1 Introduction/basic parameters of the project The Ruhr region is one of the largest urban centres in Europe, so that infrastructural measures such as the expansion of traffic connections play a vital role here. -
Download the Scanned
MTNERALOGTCALSOCIETY (LONDON) A meeting of the Society was held on Thursday, January 11th, 1951,in the apartments of the Geological Society of London, Burlington House, Piccadilly, W. 1 (by kind permis- sion). Exnrsrrs (1) Crystals of analcime and baryte from the trachyte of Traprain Law, East Lothian: by Dr. S. I. Tomkeiefi. (2) The use of a Laspeyres ocular lens in preference to the Berek compensator: by Dr. A. F. Hallimond. (3) Sections and colour photographs of (a) artificial corundum, (b) kyanite-staurolite intergrowth, (c) garnet: by Dr. Francis Jones. Papnns The following papers were read: (1) 'RnrcrmNlecn' AND 'BREZTNA'Leltrr,rln rN METEoRrrrc IRoNS. By Dr. L. J. Spencer Reichenbach lamellae, seen as bands on etched sections, were originally described as enclosed plates of troilite parallel to cube pianes in the kamacite-taenite structure, and Brczina lamellae as schreibersite parallel to the rhombic-dodecahedron. These minerals, and also cohenite, have since been observed in both of these and in other orientations. It has sometimes been assumed that bands at right angles indicate orientation on cube planes, but they may also be due to other orientations. On a section parallel to an octahedral plane it is possible only with lamellae parailel to the rhombic dodecahedron' (2) SnorrunNraRy INSLUSTSNSrN tnn IIvpnnsTHENE-GABBRo, ARDNAItrUR6HAN,ARGYLL- SIIIRE. By Mr. M. K. Wells The hypersthene-gabbro contains an abundance of granular basic hornfels inclusions which have all been interpreted in the past as recrystallized basic igneous rocks. Some of these inclusions, particularly banded ones, are now believed to be sedimentary rocks which have sufiered considerable metasomatism. -
38Th RMS Program Notes
E.fu\wsoil 'og PROGRAM Thursday Evening, April 14, 2011 PM 4:00-6:00 Cocktails and Snacks – Hospitality Suite 400 (4th Floor) 6:00-7:45 Dinner – Baxter’s 8:00-9:15 THE GUALTERONI COLLECTION: A TIME CAPSULE FROM A CENTURY AGO – Dr. Renato Pagano In 1950, the honorary curator of the Museum of Natural History in Genoa first introduced Dr. Renato Pagano to mineral collecting as a Boy Scout. He has never looked back. He holds a doctorate in electrical engineering and had a distinguished career as an Italian industrialist. His passion for minerals has produced a collection of more than 13,000 specimens, with both systematic and aesthetic subcollections. His wife Adriana shares his passion for minerals and is his partner in collecting and curating. An excellent profile of Renato, Adriana, and their many collections appeared earlier this year in Mineralogical Record (42:41-52). Tonight Dr. Pagano will talk about an historic mineral collection assembled between 1861 and 1908 and recently acquired intact by the Museum of Natural History of Milan. We most warmly welcome Dr. Renato Pagano back to the speakers’ podium. 9:15 Cocktails and snacks in the Hospitality Suite on the 4th floor will be available throughout the rest of the evening. Dealers’ rooms will be open at this time. All of the dealers are located on the 4th floor. Friday Morning, April 15, 2011 AM 9:00 Announcements 9:15-10:15 CRACKING THE CODE OF PHLOGOPITE DEPOSITS IN QUÉBEC (PARKER MINE), MADAGASCAR (AMPANDANDRAVA) AND RUSSIA (KOVDOR) – Dr. Robert F. Martin Robert François Martin is an emeritus professor of geology at McGill University in Montreal. -
Liroconite Cu2al(Aso4)(OH)4 • 4H2O C 2001-2005 Mineral Data Publishing, Version 1
Liroconite Cu2Al(AsO4)(OH)4 • 4H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Typically as crystals with a flattened octahedral or lenticular aspect, dominated by {110} and {011} and striated parallel to their intersections, also {001}, {010}, {100}, to 3.6 cm, alone and in sub-parallel groups. May be granular, massive. Physical Properties: Cleavage: On {110}, {011}, indistinct. Fracture: Uneven to conchoidal. Hardness = 2–2.5 D(meas.) = 2.94–3.01 D(calc.) = [3.03] Optical Properties: Transparent to translucent. Color: Sky-blue, bluish green, verdigris-green, emerald-green; pale blue to pale bluish green in transmitted light. Streak: Pale blue to pale green. Luster: Vitreous to resinous. Optical Class: Biaxial (–). Orientation: Y = b; Z ∧ a =25◦. Dispersion: r< v,moderate. α = 1.612(3) β = 1.652(3) γ = 1.675(3) 2V(meas.) = n.d. 2V(calc.) = 72(5)◦ Cell Data: Space Group: I2/a. a = 12.664(2) b = 7.563(2) c = 9.914(3) β =91.32(2)◦ Z=4 X-ray Powder Pattern: Cornwall, England. 6.46 (10), 3.01 (10), 5.95 (9), 2.69 (6), 3.92 (5), 2.79 (5), 2.21 (5) Chemistry: (1) (2) P2O5 3.73 As2O5 23.05 26.54 Al2O3 10.85 11.77 Fe2O3 0.98 CuO 36.38 36.73 H2O 25.01 24.96 Total 100.00 100.00 • (1) Cornwall, England. (2) Cu2Al(AsO4)(OH)4 4H2O. Occurrence: A rare secondary mineral in the oxidized zone of some copper deposits. Association: Olivenite, chalcophyllite, clinoclase, cornwallite, strashimirite, malachite, cuprite, “limonite”. -
Utahite, a New Mineral and Associated Copper Tellurates from the Centennial Eureka Mine, Tintic District, Juab County, Utah
UTAHITE, A NEW MINERAL AND ASSOCIATED COPPER TELLURATES FROM THE CENTENNIAL EUREKA MINE, TINTIC DISTRICT, JUAB COUNTY, UTAH Andrew C. Roberts and John A. R. Stirling Geological Survey of Canada 601 Booth Street Ottawa, Ontario, Canada K IA OE8 Alan J. Criddle Martin C. Jensen Elizabeth A. Moffatt Department of Mineralogy 121-2855 Idlewild Drive Canadian Conservation Institute The Natural History Museum Reno, Nevada 89509 1030 Innes Road Cromwell Road Ottawa, Ontario, Canada K IA OM5 London, England SW7 5BD Wendell E. Wilson Mineralogical Record 4631 Paseo Tubutama Tucson, Arizona 85750 ABSTRACT Utahite, idealized as CusZn;(Te6+04JiOH)8·7Hp, is triclinic, fracture. Utahite is vitreous, brittle and nonfluorescent; hardness space-group choices P 1 or P 1, with refined unit-cell parameters (Mohs) 4-5; calculated density 5.33 gtcm' (for empirical formula), from powder data: a = 8.794(4), b = 9996(2), c = 5.660(2);\, a = 5.34 glcm' (for idealized formula). In polished section, utahite is 104.10(2)°, f3 = 90.07(5)°, y= 96.34(3YO, V = 479.4(3) ;\3, a:b:c = slightly bireflectant and nonpleochroic. 1n reflected plane-polar- 0.8798:1 :0.5662, Z = 1. The strongest five reflections in the X-ray ized light in air it is very pale brown, with ubiquitous pale emerald- powder pattern are (dA(f)(hkl)]: 9.638(100)(010); 8.736(50)(100); green internal reflections. The anisotropy is unknown because it is 4.841(100)(020); 2.747(60)(002); 2.600(45)(301, 311). The min- masked by the internal reflections. Averaged electron-microprobe eral is an extremely rare constituent on the dumps of the Centen- analyses yielded CuO = 25.76, ZnO = 15.81, Te03 = 45.47, H20 nial Eureka mine, Tintic district, Juab County, Utah, where it (by difference) {12.96], total = {100.00] weight %, corresponding occurs both as isolated 0.6-mm clusters of tightly bound aggre- to CU49;Zn29lTe6+04)39l0H)79s' 7.1H20, based on 0 = 31. -
NEW MINERALS It Is Proposed Hereafter to Indicate In.A General Way the Classification of All New Minerals Recoided in This Department
JOURNAL MINERALOGICAL SOCIETY OF AMENICA 63 Dr. Kunz then spoke of the various city localities and the minerals found therein. He stated that the East Side, from 37 to 110 St., probably afforded the most specimens. The various tunnels and their minerals were spoken of. Capt. Miller called attention to the fine collection of Brooklyn Drift Minerals and Rocks in the collection of the Long Island Historical Society. Ife abo mentioned the occurrence of monazite and xenotime crystals, on the Speedway,Harlem River. Dr. Kunz emphasizedthe irnportance of complete records being kept of all finds. Tnou,q,s L Mrr,r,nn, SecretaryPro, Tem. NEW MINERALS It is proposed hereafter to indicate in.a general way the classification of all new minerals recoided in this department. Subdivision will be first into "families," of which nine may be recognized,as listed in the January number (Am. Min.6 (1), 12,1921). Eachfamilywillbe separatedinto "subfamilies " based on special features of composition. This arrangement is tentative and open to modification, and criticism of it will be welcome, [Eo.] FAMILY 2. SULFIDES, ETC. SosreMrr,v 3. Doust,u suLFrDEs oF METALSAND sEMr-METAr,s. I'LTRABASITE V. Rosrcxf and J. Srnnse-Btinu. Ultrabasit, ein neues Mineral aus Freiberg in Sachsen. (Ultrabasite, a new mineral from Freiberg, Saxony). Rozpr.Eeslcd Ako,il. Prag,25, No. 45, 1916;Z. Krgst. Min., 55,43H39, 1920, Neun: From its extremely basic chemical composition. Pnrsrcar, Pnopnnrrus Color black, somewhat grayish; luster metallic; streak black; cleavage none; fracture scaly, with somewhat greasy luster on the surface. H. : 5; sp. gr. -
New Mineral Names*
American Mineralogist, Volume 75, pages 240-246, 1990 NEW MINERAL NAMES* JOHN L. JAMBOR CANMET, 555 Booth Street, Ottawa, Ontario KIA OGI, Canada EDWARD S. GREW Department of Geological Sciences, University of Maine, Orono, Maine 04469, U.S.A. Baiyuneboite-(Ce) the formula for cordylite-(Ce) requires revision such that Pigqiu Fu, Xlanze Su (1987) Baiyuneboite-A new min- cordylite-(Ce) and baiyuneboite-(Ce) may be identical. The eral. Acta Mineralogica Sinica, 7, 289-297 (in Chinese, Chairman therefore withdrew the approval and asked that English abstract). the authors withhold publication of their description of Pingqiu Fu, Youhua Kong, Guohong Gong, Meicheng baiyuneboite-(Ce) until the matter could be resolved. The Shao, Jinzi Qian (1987) The crystal structure of bai- request, unfortunately, was ignored. J.L.J. yuneboite-(Ce). Acta Mineralogica Sinica, 7, 298-304 (in Chinese, English abstract). Diaoyudaoite* Electron-microprobe analyses of ten grains, whose va- lidity was checked by single-crystal X-ray methods prior Shunxi Shen, Lirong Chen, Anchun Li, Tailu Dong, Qiu- to analysis, gave an average ofNa20 4.73, CaO 1.04, BaO huo Huang, Wenqiang Xu (1986) Diaoyudaoite-A new 20.38, Ce20, 24.21, La20, 10.92, Pr20, 0.62, Nd20, 10.04, mineral. Acta Mineralogica Sinica, 6, 224-227 (in Gd20, 0.13, F 2.50, C02 (by gas chromatography) 24.64, Chinese, English abstract). o == F 1.05, sum 98.16 wt%, corresponding to Nal.OS- The average of 13 electron-microprobe analyses gave (BaO.94CaO.I,)n07( Ce I.OSLao.4sN do.42Pr 0.0'Gdo.OI)"1.99F 0.9'C,.97- Na20 4.54, AI20, 93.00, Cr20, 1.95, MgO 0.10, CaO 0.10, 012.07'ideally NaBaCe2F(CO')4' The mineral occurs as yel- SiOz 0.23, K20 0.12, sum 100.04 wt%, corresponding to low, irregular grains 0.3 to 3 mm in size, frequently as (N ao.87Ko.ozMgo.02CaO.01)ro.92(AllO.84CrO.lsSio.02)"'1.01 0,7, ide- thin hexagonal tablets.