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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. -
United States Department of the Interior U.S. Geological Survey
UNITED STATES DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY RESOURCE ASSESSMENT OF THE BUREAU OF LAND MANAGEMENT'S WINNEMUCCA DISTRICT AND SURPRISE RESOURCE AREA, NORTHWEST NEVADA AND NORTHEAST CALIFORNIA An Interim Project Status Report by Jeff L. Doebrich \ George V. Albino 2, Charles E. Barker 3, Wendell A. Duffield 4, Victor C. Dunn s, Willam F. Hanna 6, Joseph P. McFarlan 7, Dawn J. McGuire 8, Michael S. Miller 9, Stephen G. Peters \ Donald Plouff 10, Gary L. Raines \ Don L. Sawatzky1, and Gregory T. Spanski " United States Geological Survey Open-File Report 94-712 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North America Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1994 'USGS, MS 176, Reno Field Office, Mackay School of Mines, University of Nevada, Reno, NV 89557-0047 2U.S. Geological Survey, Unit 62101, APO AE 09811-2101 3USGS, MS 971, Box 25046, Denver Federal Center, Denver, CO 80225-0046 4USGS, Bldg. 3, 2255 North Gemini Dr., Flagstaff, AZ 86001-1698 5Bureau of Land Management, 705 E. 4th St., Winnemucca, NV 89445 6USGS, National Center, MS 927, 12201 Sunrise Valley Dr., Reston, VA 22092-0001 7Bureau of Land Management, P.O. Box 460, Cedarville, CA 96104 8USGS, MS 973, Box 25046, Denver Federal Center, Denver, CO 80225-0046 'Western Field Operations Center, U.S. Bureau of Mines, E. 360 Third Ave., Spokane, WA 99202 10USGS, MS 989, Bldg. -
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. -
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. -
Bulletin 65, the Minerals of Franklin and Sterling Hill, New Jersey, 1962
THEMINERALSOF FRANKLINAND STERLINGHILL NEWJERSEY BULLETIN 65 NEW JERSEYGEOLOGICALSURVEY DEPARTMENTOF CONSERVATIONAND ECONOMICDEVELOPMENT NEW JERSEY GEOLOGICAL SURVEY BULLETIN 65 THE MINERALS OF FRANKLIN AND STERLING HILL, NEW JERSEY bY ALBERT S. WILKERSON Professor of Geology Rutgers, The State University of New Jersey STATE OF NEw JERSEY Department of Conservation and Economic Development H. MAT ADAMS, Commissioner Division of Resource Development KE_rr_ H. CR_V_LINCDirector, Bureau of Geology and Topography KEMBLEWIDX_, State Geologist TRENTON, NEW JERSEY --1962-- NEW JERSEY GEOLOGICAL SURVEY NEW JERSEY GEOLOGICAL SURVEY CONTENTS PAGE Introduction ......................................... 5 History of Area ................................... 7 General Geology ................................... 9 Origin of the Ore Deposits .......................... 10 The Rowe Collection ................................ 11 List of 42 Mineral Species and Varieties First Found at Franklin or Sterling Hill .......................... 13 Other Mineral Species and Varieties at Franklin or Sterling Hill ............................................ 14 Tabular Summary of Mineral Discoveries ................. 17 The Luminescent Minerals ............................ 22 Corrections to Franklln-Sterling Hill Mineral List of Dis- credited Species, Incorrect Names, Usages, Spelling and Identification .................................... 23 Description of Minerals: Bementite ......................................... 25 Cahnite .......................................... -
Larsenite Pbznsio4 C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Orthorhombic
Larsenite PbZnSiO4 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Orthorhombic. Point Group: mm2: Crystals slender prismatic, striated elongation; rarely tabular, °attened on 010 , equant, to 3 mm. k f g Physical Properties: Cleavage: 120 , distinct. Tenacity: Brittle. Hardness = 3 D(meas.) = 5.90 D(calc.) = 6.141 fPiezogelectric. Optical Properties: Transparent. Color: White, colorless. Luster: Adamantine, pearly on platy surfaces. Optical Class: Biaxial ({). Orientation: X = a; Y = c; Z = b. Dispersion: r > v; easily perceptible. Absorption: Strong. ® = 1.92(1) ¯ = 1.95(1) ° = 1.96(1) 2V(meas.) = 80± Cell Data: Space Group: P na21: a = 8.244 b = 18.963 c = 5.06 Z = 8 X-ray Powder Pattern: Synthetic. 3.19 (100), 2.854 (90), 4.88 (80), 3.04 (80), 4.19 (60), 4.11 (50), 4.03 (50) Chemistry: (1) (2) (3) SiO2 16.87 17.2 16.48 FeO 0.10 MnO 0.14 ZnO 22.74 24.0 22.32 PbO 56.66 59.1 61.20 MgO 0.20 CaO 2.42 0.1 H2O 0.76 Total 99.89 100.4 100.00 (1) Franklin, New Jersey, USA; average of two analyses. (2) Do.; by electron microprobe. (3) PbZnSiO4: Occurrence: A very rare secondary mineral in veins cutting and replacing coarse, massive willemite-franklinite ore in a metamorphosed stratiform zinc deposit (Franklin, New Jersey, USA). Association: Willemite, clinohedrite, esperite, hardystonite, hodgkinsonite, andradite, calcite, smithsonite, zincite, franklinite, roeblingite (Franklin, New Jersey, USA); queitite, alamosite (Tsumeb, Namibia). Distribution: From Franklin, Sussex Co., New Jersey, USA. At Tsumeb, Namibia. In the Puttapa zinc mine, near Beltana, South Australia. -
THE PICKING TABLE Journal of the Franklin-Ogdensburg Mineralogical Society
THE PICKING TABLE Journal of the Franklin-Ogdensburg Mineralogical Society Vol. 55, No. 2 – Fall 2014 $10.00 U.S. IN THIS ISSUE • Blue leD Fluorescent Minerals • lavenDulan ADDeD to species list the Franklin-ogDensBurg Mineralogical society, inc. OFFICERS AND STAFF PRESIDENT, 2013-2014 TRUSTEES JAMES VAN FLEET Richard C. Bostwick (2013-2014) 222 Market Street Mark Boyer (2013-2014) Mifflinburg, PA 17844 George Elling (2014-2015) C: 570-412-2978 Richard J. Keller, Jr. (2013-2014) [email protected] Bernard T. Kozykowski, RA (2013-2014) Steven M. Kuitems, DMD (2013-2014) VICE PRESIDENT Chester S. Lemanski, Jr. (2014-2015) MARK DAHLMAN Lee Lowell (2014-2015) 11906 Scovell Terrace Earl R. Verbeek, PhD (2014-2015) Germantown, MD 20874 C: 301-428-0455 LIAISON WITH THE EASTERN [email protected] FEDERATION OF MINERALOGICAL AND LAPIDARY SOCIETIES (EFMLS) SECOND VICE PRESIDENT Delegate Richard C. Bostwick HAROLD (PAT) HINTZ Alternate Tema J. Hecht 6 Helene Drive Randolph, NJ 07869 COMMITTEE CHAIRPERSONS C: 862-219-0229 Field Trip [email protected] Coordinator Richard J. Keller, Jr. Nominating Richard J. Keller, Jr. SECRETARY Program Mark Dahlman TEMA J. HECHT Swap & Sell Chester S. Lemanski, Jr. 600 West 111th Street, Apt. 11B New York, NY 10025 H: 212-749-5817 C: 917-903-4687 [email protected] TREASURER DENISE KROTH 240 Union Avenue Wood-Ridge, NJ 07075 H: 201-933-3029 [email protected] Coarse-grained pink leucophoenicite and green willemite in a vein 0.8 inch (2.2 cm) thick cutting granular franklinite-willemite- leucophoenicite ore. The front surface is polished. The specimen, no. 5024 in the collection of the Franklin Mineral Museum, measures 5.5 × 2.8 × 0.8 inches (14 × 7 × 2 cm) and was donated to the museum by Henry Althoen. -
Sursassite from New Brunswick1
SURSASSITEFROM NEW BRUNSWICK1 E. Wu. HEINRICH The [Jn'fuersityof M'ich'igan,Ann Arbor, M'ichigan Ansrnecr Sursassite, previously known only from Oberhalbstein, Graubtinden, Switzerland, o".ri" i" veiniets cutting Middle Siiurian Fe-Mn ores about five miles west of Wood- .to"ii, N"* Brunswick. fhe composition based on a new analysis is Mne Al4 (Si,ADrrogo .6HzO. Associated minerals are barite, calcite, and quartz, and the. veins appear to trulr" U""" formed near the end of a period of low-grade metamorphism, by solutions operating under the intensity environment of the greenschistfacies' INrnoouctrow During the summer of 1958, while investigating manganese deposits in eastern Maine and adjacent New Brunswick, the writer found a copper-coloured fibrous mineral which he did not recognize. Subsequently it was identified as sursassite, a mineral that previously had been found at only one locality. The cost of the chemical analysis and thin sections was defrayed by Michigan Memorial Phoenix Project No. 150. The writer also is indebted to E. B. Gross for laboratory assistance and to Dr. E. H. Nickel for directing his attention to several references. History t.r igro Miiller published tsro papers (1916o, b) describing the miner- alogy of a manganese deposit at Oberhalbstein, Graubiinden, Switzerland. t" tir" first article Miiller identifies psilomelane, polianite, zoisite, pied- montite, rhodochrosite, rhodonite and a copper-coloured mineral resemb- ling a mica about which he says (1916a, p. 224): "Auzerdem fand sich ein kupferfarbenes, an Glimmer errinnerndes Mineral das ebenfalls in enger Verbindung mit dem Manganerz auftritt und auf Grund einer Analyse als ein wasserhaltiges Mn-silikat zubezeichen ist." The analysis was presented in Miiller's second paper (1916b), but the mineral was not given a name. -
Fluorescent Rocks & Minerals
Fluorescent Rocks & Minerals Auckland Teacher's Day Dec 4th 2020 Martyn P. Coles 2 Definitions and Background • LUMINESCENCE defined as: "Light, or a glow, emitted by a luminescent (cool) object or surface" (Oxford English Dictionary) • an energy source promotes an electron of an atom from its "ground" (lowest-energy) state into an "excited" (higher-energy) state • the electron gives back the energy in the form of light so it can fall back to its "ground" state Excited State ENERGY e e LIGHT Ground Ground State State 3 Types of Luminescence CHEMILUMINESCENCE : luminescence where the energy is supplied by chemical reactions For example - Glow-sticks • typically the reaction of hydrogen peroxide with a solution of phenyl oxylate ester and a dye molecule (http://www.neonhusky.com) Ph O O O H2O2 O C Dye 2 Ph OH + 2 CO2 + Dye* O C O O O LIGHT Ph Dye 5 Types of Luminescence BIOLUMINESCENCE : luminescence where the chemical reactions occur in living things (a type of Chemiluminescence) For example – Glow Worm (Lampyris Noctiluca) • chemical responsible : LUCIFERIN CO H N N 2 HO S S (http://www.wildinbritain.co.uk) • enzyme (LUCIFERASE) catalyses Luciferin Oxyluciferin oxidation of luciferin to give + O2 inactive oxyluciferin and light LIGHT 5b New Zealand’s own Arachnocampa Luminosa Waitomo Glowworm Caves (can also be seen in Zealandia / Karori…) 6 Fluorescence FLUORESCENCE : luminescence where the energy is supplied by electro- magnetic radiation "The coloured luminosity produced in some transparent bodies by the direct action of light, esp. of the violet and ultra-violet rays; the property, in certain substances, of rendering the ultra-violet rays visible, so as to produce this phenomenon" (Oxford English Dictionary) UV-Light Eu3+ vis Eu3+ UV 7 Electromagnetic Spectrum Wavelength (l) u Radio l = c Microwave E = h u E = h c Infrared l Visible • l inverse relationship with frequency, u Ultraviolet i.e. -
Glossary of Obsolete Mineral Names
Ca acetate = synthetic (CH3COO)2Ca·H2O, AM 77, 450 (1992). Ca-aegerine = Ca-rich aegerine, CM 39, 930 (2001). Ca-agardite = zálesíite, LAP 24(7/8), 36 (1999). Ca-Al clinopyroxene = synthetic CaAl[(AlSi)O6], AM 68, 542 (1983). Ca(Al,Fe)garnet = Fe-rich grossular, Deer et al. 1B, 117 (1986). Ca-Al-montmorillonite = Ca-Al-exchanged Na-rich montmorillonite, CCM 34, 535 (1986). Ca-Al-pyroxene = synthetic CaAl[(AlSi)O6], EJM 9, 198 (1997). Ca-Al tschermak's molecule = synthetic pyroxene CaAl[(AlSi)O6], AM 65, 302 (1980). Ca-amphibole (Hietanen) = hornblende, AM 59, 22 (1974). Ca-amphibole (Okamura et al.) = magnesiohornblende + tremolite + edenite, MM 70, 21 (2006). Ca-anorthite = high pressure Ca[(Si2Al2)O8], EJM 22, 103 (2010). Ca-apatite = fluorapatite, AM 89, 1323 (2004). Ca-attapulgite = Ca-saturated palygorskite, CCM 27, 285 (1979). Ca-augite = diopside, MM 42, 53 (1978). Ca-autunite = autunite, AM 14, 269 (1929). cabalt-chrysotile = synthetic serpentine Co3[Si2O5](OH)4, Embrey & Fuller 76 (1980). Ca-Ba-mimetite = Ca-Ba-As-rich pyromorphite, Kostov & Breskovska 189 (1989). Ca-barysilite = synthetic CaPb8[Si2O7]3, AM 52, 1083 (1967). cabasita subfamily = chabazite, Dana 6th, 1109 (1892). cabazita subfamily = chabazite, Zirlin 41 (1981). Ca-beidellite = Ca-rich beidellite, AM 64, 1091 (1979). cabello de Venus = acicular rutile + grey Al+H±Li-rich quartz, Novitzky 148 (1951). Ca-bentonite = Ca-rich montmorillonite, ClayM 32, 33 (1997). Ca2+-bentonite = Ca-rich montmorillonite, CCM 38, 250 (1990). cabesa de Moro = elbaite, de Fourestier 55 (1999). Ca-betafite = pyrochlore, AM 68, 266 (1983), CM 48, 692 (2010). Ca-birnessite (Chukhrov et al.) = Ca-rich birnessite, CCM 28, 346 (1980).