The Picking Table Volume 45, No. 1 – Spring 2004
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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 -
Charlesite, a New Mineral of the Ettringite Group, from Franklin, New Jersey
American Mineralogist, Volume 68, pages 1033-1037,1983 Charlesite, a new mineral of the ettringite group, from Franklin, New Jersey PBre J. DuxN Department of Mineral Sciences SmithsonianInstitution, Washington,D. C. 20560 DoNero R. Peecon Department of GeologicalSciences University of Michigan, Ann Arbor, Michigan 48109 PBrnn B. LBavBNs Departmentof Geology Universityof Delaware, Newark, Delaware l97ll eNo JonN L. Beuu Franklin Mineral Museum Franklin. New Jersey 07416 Abstract Charlesite,ideally C4(AI,Si)z(SO4)2(B(OH)4)(OH,O)r2.26H2Ois a member of the ettrin- gite group from Franklin, New Jersey, and is the Al analogueof sturmanite. Chemical analysisyielded CaO27.3, Al2O3 5.1, SiO2 3.1, SO3 12.8,B2o33.2, H2O 48.6, sum : 100.1 percent.-Charlesiteis hexagonal,probable spacegroup P3lc, with a = ll.16(l), c = 21.21(2)4. The strongest lines in the X-ray powder difraction pattern (d, IlIo, hkl) are: 9.70,100, 100;5.58, 80, 110;3.855,80, ll4;2.749,70,304;2.538,70,126;2.193,70,2261 404. Charlesite occurs as simple hexagonal crystals tabular on {0001} and has a perfect {10T0}cleavage. The densityis 1.77glcm3 (obs.) and 1.79glcms (calc.). Optically, charlesite is uniaxial( -) with a : | .492(3)and e : 1.475(3).It occurswith clinohedrite,ganophyllite, xonotlite, prehnite, roeblingite and other minerals in severalparageneses at Franklin, New Jersey. Charlesite is named in honor of the late Professor Charles Palache. Introduction were approved, prior to publication, by the Commission Minerals and Mineral Names. I. M. A. The An ettringite-like mineral was first described from on New specimenwas divided into three portions. -
List of New Mineral Names: with an Index of Authors
415 A (fifth) list of new mineral names: with an index of authors. 1 By L. J. S~v.scs~, M.A., F.G.S. Assistant in the ~Iineral Department of the,Brltish Museum. [Communicated June 7, 1910.] Aglaurito. R. Handmann, 1907. Zeita. Min. Geol. Stuttgart, col. i, p. 78. Orthoc]ase-felspar with a fine blue reflection forming a constituent of quartz-porphyry (Aglauritporphyr) from Teplitz, Bohemia. Named from ~,Xavpo~ ---- ~Xa&, bright. Alaito. K. A. ~Yenadkevi~, 1909. BuU. Acad. Sci. Saint-P6tersbourg, ser. 6, col. iii, p. 185 (A~am~s). Hydrate~l vanadic oxide, V205. H~O, forming blood=red, mossy growths with silky lustre. Founi] with turanite (q. v.) in thct neighbourhood of the Alai Mountains, Russian Central Asia. Alamosite. C. Palaehe and H. E. Merwin, 1909. Amer. Journ. Sci., ser. 4, col. xxvii, p. 899; Zeits. Kryst. Min., col. xlvi, p. 518. Lead recta-silicate, PbSiOs, occurring as snow-white, radially fibrous masses. Crystals are monoclinic, though apparently not isom0rphous with wol]astonite. From Alamos, Sonora, Mexico. Prepared artificially by S. Hilpert and P. Weiller, Ber. Deutsch. Chem. Ges., 1909, col. xlii, p. 2969. Aloisiite. L. Colomba, 1908. Rend. B. Accad. Lincei, Roma, set. 5, col. xvii, sere. 2, p. 233. A hydrated sub-silicate of calcium, ferrous iron, magnesium, sodium, and hydrogen, (R pp, R',), SiO,, occurring in an amorphous condition, intimately mixed with oalcinm carbonate, in a palagonite-tuff at Fort Portal, Uganda. Named in honour of H.R.H. Prince Luigi Amedeo of Savoy, Duke of Abruzzi. Aloisius or Aloysius is a Latin form of Luigi or I~ewis. -
Clinohedrite Caznsio4 ² H2O C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Monoclinic
Clinohedrite CaZnSiO4 ² H2O c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: m: Crystals typically prismatic or tabular, to 4 mm; may be wedge-shaped re°ecting the domatic class in which the species crystallizes. Physical Properties: Cleavage: Perfect on 010 . Hardness = 5.5 D(meas.) = 3.28{3.335 D(calc.) = [3.32] Strongly pyroelectric. f g Optical Properties: Transparent to translucent. Color: Amethystine, colorless to white. Luster: Brilliant, glassy; pearly on 010 . f g Optical Class: Biaxial ({). Orientation: Z = b; Y c = 28±. ® = 1.662 ¯ = 1.667 ° = 1.669 2V(meas.) = Large. ^ Cell Data: Space Group: Cc: a = 5.090{5.131 b = 15.829{15.928 c = 5.386{5.422 ¯ = 103:39± 103:43± Z = 4 ¡ X-ray Powder Pattern: Franklin, New Jersey, USA. (ICDD 17-214). 2.76 (100), 3.23 (70), 2.50 (60), 7.81 (50), 3.97 (50), 2.36 (50), 2.47 (40) Chemistry: (1) (2) (3) SiO2 27.22 26.73 27.87 (Fe; Al)2O3 0.28 0.37 MnO 0.50 1.11 ZnO 37.44 37.13 37.76 MgO 0.07 CaO 26.25 26.25 26.01 + H2O 8.56 8.09 8.36 Total 100.32 99.68 100.00 (1) Franklin, New Jersey, USA; average of two analyses. (2) Do. (3) CaZnSiO4 ² H2O: Occurrence: In a metamorphosed stratiform zinc orebody (Franklin, New Jersey, USA). Association: Hancockite, nasonite, glaucochroite, roeblingite, calcite, willemite, axinite, larsenite, hodgkinsonite, franklinite (Franklin, New Jersey, USA); stringhamite, kinoite, apophyllite (Christmas mine, Arizona, USA). Distribution: From Franklin, Sussex Co., New Jersey; in the Christmas mine, Gila Co., Arizona, USA. -
General Index
CAL – CAL GENERAL INDEX CACOXENITE United States Prospect quarry (rhombs to 3 cm) 25:189– Not verified from pegmatites; most id as strunzite Arizona 190p 4:119, 4:121 Campbell shaft, Bisbee 24:428n Unanderra quarry 19:393c Australia California Willy Wally Gully (spherulitic) 19:401 Queensland Golden Rule mine, Tuolumne County 18:63 Queensland Mt. Isa mine 19:479 Stanislaus mine, Calaveras County 13:396h Mt. Isa mine (some scepter) 19:479 South Australia Colorado South Australia Moonta mines 19:(412) Cresson mine, Teller County (1 cm crystals; Beltana mine: smithsonite after 22:454p; Brazil some poss. melonite after) 16:234–236d,c white rhombs to 1 cm 22:452 Minas Gerais Cripple Creek, Teller County 13:395–396p,d, Wallaroo mines 19:413 Conselheiro Pena (id as acicular beraunite) 13:399 Tasmania 24:385n San Juan Mountains 10:358n Renison mine 19:384 Ireland Oregon Victoria Ft. Lismeenagh, Shenagolden, County Limer- Last Chance mine, Baker County 13:398n Flinders area 19:456 ick 20:396 Wisconsin Hunter River valley, north of Sydney (“glen- Spain Rib Mountain, Marathon County (5 mm laths donite,” poss. after ikaite) 19:368p,h Horcajo mines, Ciudad Real (rosettes; crystals in quartz) 12:95 Jindevick quarry, Warregul (oriented on cal- to 1 cm) 25:22p, 25:25 CALCIO-ANCYLITE-(Ce), -(Nd) cite) 19:199, 19:200p Kennon Head, Phillip Island 19:456 Sweden Canada Phelans Bluff, Phillip Island 19:456 Leveäniemi iron mine, Norrbotten 20:345p, Québec 20:346, 22:(48) Phillip Island 19:456 Mt. St-Hilaire (calcio-ancylite-(Ce)) 21:295– Austria United States -
The Picking Table Volume 9, No. 1
JOURNAL OF THE FRANKLIN-OGDENSBURG MINERALOGIGAL SOCIETY VOLUME 9 FEBRUARY 1968 NUMBER 1 The contents of The Picking Table are licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. CLUB PROGRAM - SPRING 1968 All meetings will be held at the Hardyston School, intersection of Routes #23 and #517, Franklin, 5f. J. Pre meeting activities start at 1:00 P. A. Speaker will be announced at 2:30 P. M. Saturday Field Trip, 10 A.M. to 1:00 P.M. to March 16th Geology Department, Lafayette College, Easton, Pa. Details later. Saturday , Proposed Field Trip to Fossil Location. April 6th Saturday, Field Trip, 9:00 A.,,, to iioon, April 20th Buckwheat Dump, Franklin, N.J. Meeting 2:30 P.M. Speaker, Alexander Klinshaw on "The Minerals of New Jersey" Sunday, Proposed Field Trip, 5th. Limecrest wuarry, uparta, K. J. Saturday , Proposed Field Trip, 9:00 n..^. to Noon. May 18th Open Cut, Sterling Hill r'iine, Ogdensburg, N.J. Meeting, 2:30 P.M. Speaker, Dr. Clifford Frondel, Saturday, Identification Workshop. June 8th ^aturday, Field Trip, 9:00 A.M. to i<oon June 22nd Farber Quarry, Franklin, &.J. Swap Session (interclub) Saturday, Field Trip, 12 noon to 3'-30 P.k. July 13th Bethlehem Steel Co., Cornwall, Pa. Recommended ^a turday/Sunday Fourth annual Mineral Show sponsored by May llth/12th the Matawan Mineralogical Society, Inc. Matawan Kerional High School, Atlantic ..venue, Matawan, N.J. June 27th/29th eastern Federation Mineral Show Curtis Hickson Convention Center, Tampa, Florida. * * * * THE PICKING TABLr. is issued twice a year; a February issue to reach members about March 1st with news and the Club Spring program; an August issue to reach members about September 1st with news and the Fall program. -
The Lead Silicates from Franklin, New Jersey: Occurrence and Composition
MINERALOGICAL MAGAZINE, DECEMBER 1985, VOL. 49, PP. 7217 The lead silicates from Franklin, New Jersey: occurrence and composition PETE J. DUNN Department of Mineral Sciences, Smithsonian Institution, Washington, DC 20560, USA ABSTRACT. The lead silicate minerals from Franklin, History and occurrence New Jersey, occurred in two separate assemblages. One of these is characterized by esperite associated with hardy- Inasmuch as the Franklin Mine was mined-out stonite and occasionallarsenite. The second assemblage and flooded in 1954, examination of the geologic can be considered as two parts: one consists of margaro- relations of the occurrences of the lead silicates was sanite, barysilite, nasonite, and ganomalite; the other not possible. Recourse was made to mine maps and contains roeblingite and hancockite, together with a interviews with former employees ofthe New Jersey number of highly hydrated phases. Chemical analyses Zinc Company who had examined these occur- indicate that these species conform to their theoretical rences, most notably John L. Baum, retired resident compositions. There are no simple lead siJicates at geologist for the Franklin Mine. Franklin; al1 are compound silicates of Pb with Mn, Zn, and Ca. KEYWORDS: lead silicates, barysilite, esperite, ganomal- Table l. The lead silicate minerals found at ite, hancockite, larsenite, margarosanite, nasonite, roe- Franltlin, New Jersey blingite, Franklin, New Jersey, USA. BARYSILITE PbSMn(Si207)3 ATthe end of the 19th century a remarkable suite of ESPERITE ca3PbZn4(Si04)4 uncommon minerals was found on the Parker GANOMALITE Pb9CaSMnSi9ÜJ3 dump, near the Parker shaft of the Franklin Mine, (OH) in Franklin, Sussex County, New Jersey. This suite HANCOCKITE PbCa(A1,Fe3+)3(Si04)3 inc\uded a number of unknown minerals which LARSENITE PbZnSi04 were subsequently described as new species. -
Franklin, Fluorescent Mineral Capital of the World
FRANKLIN, FLUORESCENT MINERAL CAPITAL OF THE WORLD © Spex Industries, Inc. 1981 by R.W. )ones, Jr. 3520 N. Rose Circle Dr., Scottsdale, AZ 85251 Tell people that Franklin, New Jersey is lots. In the hustle and bustle of their daily The deposit has yielded close to 300 noted throughout the world for its myriad lives, people tend to forget New Jersey's different minerals, a number vastly fluorescent minerals and your reward is natural endowments: the rich farmlands greater than from any other known source likely to be a blank stare. Tell them that of the south, t he rolling forest and grazing in the world. More amazing, nearly 60 of Franklin, along with neighboring Ogdens lands of the northwest, the manicured these minerals exhibit luminescence, in burg, is the home of a truly unique metal lawns and rich green golf courses of its the form of almost instantaneous fluores deposit and boredom sets in for sure. But suburbs, and the unique zinc-manganese- cence or as days long persistent take them for a walk on a dark night iron deposits of Franklin and Sterling Hill phosphorescence. across the waste rock dumps atop this ore Maybe for two or three weeks of t he deposit and they begin to act strangely. su mmer people forego the turmoil and The luminescence of many Frankl in Like children in a candy shop, they're cavort on ocean beaches or bask in the species explains the strange behavior intrigued, captivated by the multi-hued glory of a sun-dappled lake. But to accept noted among miners and mineral colors of these chameleon rocks. -
Redetermination of the Crystal Structure of Clinohedrite, Caznsi04
Zeitschrift fiir Kristallographie, Bd. 144, S. 377-392 (1976) Redetermination of the crystal structure of clinohedrite, CaZnSi04 . H20 By CL. C. VENETOPOULOSand P. J. RENTZEPERIS Applied Physics Laboratory, Aristotle University of Thessaloniki, Thessaloniki, Greece (Received 6 April 1976) Auszug . Die Kristallstruktur des Klinoedrits, CaZnSi04. H20, von Franklin, New Jersey, wurde mit Hilfe dreidimensionaler Diffraktometer-Daten (Philips PW 1100) neu bestimmt. Sie ist von derjenigen von NIKITIN and BELOV (1963) wesentlich verschieden. Die Gitterkonstanten, ermittelt nach der Methode der kleinsten Quadrate mit direkt auf dem Diffraktometer gemessenen I:J-Werten, sind: a = 5,090, b = 15,829, e = 5,386 A, fJ = 103,260; Z = 4, Raumgruppe Ce. Atomparameter und anisotrope Temperaturfaktoren wurden nach der Methode der kleinsten Quadrate bis zu R = 0,041 verfeinert. Die Struktur enthiilt isolierte Si04-Tetraeder, nicht Si207-Gruppen. Das Si04-Tetraeder ist fast regelmiiBig mit < Si-O > = 1,620 A und < 0-0> = 2,645 A. Die Zn-Atome sind von vier O-Atomen in den Ecken eines verzerrten Tetraeders umgeben; < Zn-O > = 1,959 A und < 0-0> = 3,181 A. Jedes Ca.Atom ist von vier O.Atomen und zwei H20.Molek-iilen umgeben, welche ein stark verzerrtes Oktaeder bilden; < Ca-O > = 2,372 A und < 0-0 > = 3,306 A. Jedes Zn04- Tetraeder hat gemeinsame Ecken mit vier benachbarten Si04-Te- traedern, zwei anderen Zn04-Tetraedern und zwei CaOa-Oktaedern, wobei zwei- dimensionale (ZnSi04);;2n-Netze, parallel (010), zustande kommen. Das CaOa-Ok- taeder hat gemeinsame Ecken mit vier Si 0 4- und zwei Zn 0 4-Tetraedern. AuBerdem hat es zwei Kanten mit benachbarten Oktaedern gemeinsam. -
A Specific Gravity Index for Minerats
A SPECIFICGRAVITY INDEX FOR MINERATS c. A. MURSKyI ern R. M. THOMPSON, Un'fuersityof Bri.ti,sh Col,umb,in,Voncouver, Canad,a This work was undertaken in order to provide a practical, and as far as possible,a complete list of specific gravities of minerals. An accurate speciflc cravity determination can usually be made quickly and this information when combined with other physical properties commonly leads to rapid mineral identification. Early complete but now outdated specific gravity lists are those of Miers given in his mineralogy textbook (1902),and Spencer(M,i,n. Mag.,2!, pp. 382-865,I}ZZ). A more recent list by Hurlbut (Dana's Manuatr of M,i,neral,ogy,LgE2) is incomplete and others are limited to rock forming minerals,Trdger (Tabel,l,enntr-optischen Best'i,mmungd,er geste,i,nsb.ildend,en M,ineral,e, 1952) and Morey (Encycto- ped,iaof Cherni,cal,Technol,ogy, Vol. 12, 19b4). In his mineral identification tables, smith (rd,entifi,cati,onand. qual,itatioe cherai,cal,anal,ys'i,s of mineral,s,second edition, New york, 19bB) groups minerals on the basis of specificgravity but in each of the twelve groups the minerals are listed in order of decreasinghardness. The present work should not be regarded as an index of all known minerals as the specificgravities of many minerals are unknown or known only approximately and are omitted from the current list. The list, in order of increasing specific gravity, includes all minerals without regard to other physical properties or to chemical composition. The designation I or II after the name indicates that the mineral falls in the classesof minerals describedin Dana Systemof M'ineralogyEdition 7, volume I (Native elements, sulphides, oxides, etc.) or II (Halides, carbonates, etc.) (L944 and 1951). -
Esperite Pbca3zn4(Sio4)4 C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Monoclinic
Esperite PbCa3Zn4(SiO4)4 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: Granular aggregates, massive, to 9 cm. Physical Properties: Cleavage: Distinct on 010 and 100 ; poor on 101 . Fracture: Conchoidal. Hardness = 5{5.5 D(mefas.) g= 4.28f{4.42g D(calc.)f= 4.g25 Brilliant yellow °uorescence under SW UV; kelly green cathodoluminescence. Optical Properties: Opaque, transparent in small grains. Color: White, darkening on exposure to light. Luster: Dull to slightly greasy. Optical Class: Biaxial ({). ® = 1.760{1.762 ¯ = 1.769{1.770 ° = 1.769{1.774 2V(meas.) = 5±{40± Cell Data: Space Group: P 21=n: a = 17.628(4) b = 8.270(3) c = 30.52(2) ¯ = 90± Z = 12 X-ray Powder Pattern: Franklin, New Jersey, USA. 3.017 (100), 2.534 (75), 7.62 (45), 1.944 (45), 2.367 (40), 2.884 (33), 3.363 (23) Chemistry: (1) (2) SiO2 24.10 25.3 FeO 0.48 MnO 0.57 0.6 ZnO 30.61 32.3 PbO 27.63 26.8 MgO 0.23 0.4 CaO 16.36 16.4 H2O¡ 0.12 Total 100.10 101.8 (1) Franklin, New Jersey, USA; corresponding to Pb1:23(Ca2:89Mn0:08Mg0:06)§=3:03Zn3:73 Si3:98O16: (2) Do.; by electron microprobe, average of 10 analyses, corresponding to Pb1:15 (Ca2:80Mg0:09Mn0:08)§=2:97Zn3:80Si4:04O16: Occurrence: In a metamorphosed stratiform zinc orebody. Association: Willemite, zincite, hardystonite, glaucochroite, andradite, franklinite, clinohedrite, leucophoenicite, larsenite, copper. Distribution: From Franklin, Sussex Co., New Jersey, USA. -
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.