Mineral Pigments of Interest in Asian Painting
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New Mineral Names
-------- American Mineralogist, Volume 81, pages 1282-1286, 1996 NEW MINERAL NAMES. JOHN L. JAMBOR,l VLADIMIR A. KOVALENKER,2 JACEK PuZIEWICZ,3 ANDANDREW C. ROBERTS4 lDepartment of Earth Sciences, University of Waterloo, Waterloo, Ontario N2L 3Gl, Canada 21GREM RAN, Russian Academy of Sciences, Moscow 10917, Staromonetnii 35, Russia 'Institute of Geological Sciences, University of Wroc1aw, Cybulskiego 30, 50-205 Wroc1aw, Poland 4Geological Survey of Canada, 601 Booth Street, Ottawa KIA OE8, Canada Clinoatacamite* mineral from the Clear Creek claim, San Benito Coun- ty, California: Description and crystal structure. Pow- J.L. Jambor, J.E. Dutrizac, AC. Roberts, J.D. Grice, J.T. Szymanski (1996) Clinoatacamite, a new polymorph of der Diffraction, 11(1), 45-50. Cu2(OH)3C1,and its relationship to paratacamite and The mineral occurs sparingly with calomel, native mer- "anarakite." Can. Mineral., 34, 61-72. cury, cinnabar, montroydite, and quartz in a single spec- J.D. Grice, J.T. Szymanski, J.L. Jambor (1996) The crys- imen of float near a prospect pit at the former Clear Creek tal structure of clinoatacamite, a new polymorph of mercury mine in the new Idria district of California. The Cu2(OH)3Cl. Can. Mineral., 34, 73-78. specimen contains subhedral to anhedral crystals, typi- Electron microprobe analysis gave CuO 74.7 (73.4- cally bladed to platy, maximum size 0.3 x 0.3 mm, stri- 76.0), C1l6.5 (15.7-17.2), H20 (calc.) 13.5, sum 104.7, ated [001], black to dark brown-black color, dark red- less 0 == Cl 3.7, total 101.0 wt%, corresponding to brown to black streak, opaque to translucent on thin CU1.9603.o3H3.l1Clo.97, ideally Cu2(OH)3C1. -
Bromide from Terlingua, Texas
Canadian Mineralogist Vol. 19, pp. 393-396 (1981) COMANCHEITE,A NEW MEBGURYOXVCHLORIDE - BROMIDE FROMTERLINGUA, TEXAS A.C. ROBERTS eNn H.G. ANSELL Geologicalsurvey of Canada,60l Booth street, ottawa, ontario KlA 088 P.J. DUNN Depdrtmentol Mineral Sciences,Sntithsonian Instittttion, Washington, D.C. 20560, US'A' ABSTRACT en lumibre ultraviolette.Extinction paralldle.allon- gementpositif. Les indicesde r6fraction se situent '1..79. Comancheite is a new mercurv oxychloride- entre 1.78 et Densit6 mesur6e7.7G). cal- bromide mineral from the Mariposa mine. Terlingua cul6e 8.0. A la microsonde6lectronique' on trouve district, Texas. Associated minerals are calcite, la formule Hg,r(Clr.o,Brs.on)t".nrOo.n".d'oi la for- goethite, hematite and quartz. Comancheite occurs mule id6alisdeHgrs(Cl,Br)nOo. La comanch€iteest as anhedral crystalline massesand as stellate groups orthorhombique.groupe spatialPnnm ou Pnn2. a of acicilar crystals, elongate parallel to c. a\reraging 18.4t(l), b 21.64(l),c 6.677(21A', z = 4' Les 80 um lons and 3 to 4 um wide. Masses are red seot raies les plus intensesdu clich6 de poudre (d with an orange-yellow streak and have a resinous (A), / sur 6chellede l0) sont: 5.68(7).5.42(6), lustre; crystals are orange-red to vellow. vitreous 2.878(8). 2.71I(il, 2.669(10). 2.4s7(5\ et and nanslucent to transparent. Comancheite is 1.415(5). brittle with fair cleavase parallel to {001} and (Traduit Par la R6daction) not {ll0}, has a Mohs hardness of 2 and does de lieht. Opticallv. coman- Mots-clds: comanch6ite,oxychlorure-bromure fluoiesce in ultraviolet mine Mari- exhibits parallel extinction and is length- mercure. -
Rediscovery of the Elements — a Historical Sketch of the Discoveries
REDISCOVERY OF THE ELEMENTS — A HISTORICAL SKETCH OF THE DISCOVERIES TABLE OF CONTENTS incantations. The ancient Greeks were the first to Introduction ........................1 address the question of what these principles 1. The Ancients .....................3 might be. Water was the obvious basic 2. The Alchemists ...................9 essence, and Aristotle expanded the Greek 3. The Miners ......................14 philosophy to encompass a obscure mixture of 4. Lavoisier and Phlogiston ...........23 four elements — fire, earth, water, and air — 5. Halogens from Salts ...............30 as being responsible for the makeup of all 6. Humphry Davy and the Voltaic Pile ..35 materials of the earth. As late as 1777, scien- 7. Using Davy's Metals ..............41 tific texts embraced these four elements, even 8. Platinum and the Noble Metals ......46 though a over-whelming body of evidence 9. The Periodic Table ................52 pointed out many contradictions. It was taking 10. The Bunsen Burner Shows its Colors 57 thousands of years for mankind to evolve his 11. The Rare Earths .................61 thinking from Principles — which were 12. The Inert Gases .................68 ethereal notions describing the perceptions of 13. The Radioactive Elements .........73 this material world — to Elements — real, 14. Moseley and Atomic Numbers .....81 concrete basic stuff of this universe. 15. The Artificial Elements ...........85 The alchemists, who devoted untold Epilogue ..........................94 grueling hours to transmute metals into gold, Figs. 1-3. Mendeleev's Periodic Tables 95-97 believed that in addition to the four Aristo- Fig. 4. Brauner's 1902 Periodic Table ...98 telian elements, two principles gave rise to all Fig. 5. Periodic Table, 1925 ...........99 natural substances: mercury and sulfur. -
Mercury--Quicksilver
scueu« No. 12 Mineral Technology Series No 6 University of Arizona Bulletin Mercury---Quicksilver By P. E. JOSEPH SECOND ISSUE NOVEMBER, 1916. Entered as second class matter November 2:1, 191~, at the postoftice at Tucson, Arizona. under the Act ot August 24, 1912. Issued weekb". September to Ya)·. PUBLISHED BY THE University of Arizona Bureau of Mines CHARLES F. WILLIS, Director TUCSON, ARIZONA 1916-17 BIBLIOGRAPHY Bancroft, Howland. Notes on the occurrence of cinnabar in central western Arizona. U. S. G. S. Bull. 430, pp. 151-153, 1910. Becker, G. F. Geology of- the quicksilver deposits of the Pacific slope, with atlas. Mon. 13, p. 486, 1888. Only the atlas in stock. Quicksilver Ore Deposits; Mineral Resources U. S. for 1892, pp. 139-168, 1893. Christy, S. B. Quicksilver reduction at New Almaden, Cal. Min- eral Resources U. S. for 1883-1884, pp. 603-636, 1885. Hillebrand, W. F., and Schaller, W. T. Mercury miner-als from Terlingua, Tex. U. S. G. S. Bull. 405, pp. 174, 1909. McCaskey, H. D. Quicksilver in 1912; Mineral Resources U. S. for 1912, Pt. 1, pp. 931-948, 1913. Quicksilver in 1913-Production and Resources; Mineral Resources U. S. for 1913, Pt. 1, pp. 197-212, 1914. Melville, W. H., and Lindgren, Waldemar. Contributions to the mineralogy of the Pacific coast. U. S. G. S. Bull. 61, 30 pp., 1890. Parker, E. W. Quicksilver; Twenty-first Ann. Rept. U. S. G. S., Pt. 6, pp. 273-283, 1901. University of Arizona Bulletin BULLETIN No. 12 SECOND ISSUE, NOVEMBER, 1916 MERCURY-QUICKSILVER By P. -
Mottramite Pbcu(VO4)(OH) C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Orthorhombic
Mottramite PbCu(VO4)(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 2/m 2/m 2/m. As crystals, equant or dipyramidal {111}, prismatic [001] or [100], with {101}, {201}, many others, to 3 mm, in drusy crusts, botryoidal, usually granular to compact, massive. Physical Properties: Fracture: Small conchoidal to uneven. Tenacity: Brittle. Hardness = 3–3.5 D(meas.) = ∼5.9 D(calc.) = 6.187 Optical Properties: Transparent to nearly opaque. Color: Grass-green, olive-green, yellow- green, siskin-green, blackish brown, nearly black. Streak: Yellowish green. Luster: Greasy. Optical Class: Biaxial (–), rarely biaxial (+). Pleochroism: Weak to strong; X = Y = canary-yellow to greenish yellow; Z = brownish yellow. Orientation: X = c; Y = b; Z = a. Dispersion: r> v,strong; rarely r< v.α= 2.17(2) β = 2.26(2) γ = 2.32(2) 2V(meas.) = ∼73◦ Cell Data: Space Group: P nma. a = 7.667–7.730 b = 6.034–6.067 c = 9.278–9.332 Z=4 X-ray Powder Pattern: Mottram St. Andrew, England; close to descloizite. 3.24 (vvs), 5.07 (vs), 2.87 (vs), 2.68 (vs), 2.66 (vs), 2.59 (vs), 1.648 (vs) Chemistry: (1) (2) (1) (2) CrO3 0.50 ZnO 0.31 10.08 P2O5 0.24 PbO 55.64 55.30 As2O5 1.33 H2O 3.57 2.23 V2O5 21.21 22.53 insol. 0.17 CuO 17.05 9.86 Total 100.02 100.00 (1) Bisbee, Arizona, USA; average of three analyses. (2) Pb(Cu, Zn)(VO4)(OH) with Zn:Cu = 1:1. -
Crystals of an Insoluble Carbonate of Copper Grown Under a Soda Solution L
Journal of the Arkansas Academy of Science Volume 1 Article 22 1941 Crystals of an Insoluble Carbonate of Copper Grown under a Soda Solution L. B. Roberts University of Arkansas at Monticello Edwin Roberts University of Arkansas at Monticello Follow this and additional works at: http://scholarworks.uark.edu/jaas Part of the Organic Chemistry Commons Recommended Citation Roberts, L. B. and Roberts, Edwin (1941) "Crystals of an Insoluble Carbonate of Copper Grown under a Soda Solution," Journal of the Arkansas Academy of Science: Vol. 1 , Article 22. Available at: http://scholarworks.uark.edu/jaas/vol1/iss1/22 This article is available for use under the Creative Commons license: Attribution-NoDerivatives 4.0 International (CC BY-ND 4.0). Users are able to read, download, copy, print, distribute, search, link to the full texts of these articles, or use them for any other lawful purpose, without asking prior permission from the publisher or the author. This Article is brought to you for free and open access by ScholarWorks@UARK. It has been accepted for inclusion in Journal of the Arkansas Academy of Science by an authorized editor of ScholarWorks@UARK. For more information, please contact [email protected], [email protected]. Journal of the Arkansas Academy of Science, Vol. 1 [1941], Art. 22 CRYSTALS OF AN INSOLUBLE CARBONATE OF COPPER GROWN UNDER A SODA SOLUTION1 L. B. Roberts and Edwin Roberts, Arkansas Agricultural and Mechanical College, Monticello When an old fire extinguisher of the soda-acid type was opened and emptied preparatory to recharging, several grams of blue crystals were found in the bottom of the container. -
Formation of Chrysocolla and Secondary Copper Phosphates in the Highly Weathered Supergene Zones of Some Australian Deposits
Records of the Australian Museum (2001) Vol. 53: 49–56. ISSN 0067-1975 Formation of Chrysocolla and Secondary Copper Phosphates in the Highly Weathered Supergene Zones of Some Australian Deposits MARTIN J. CRANE, JAMES L. SHARPE AND PETER A. WILLIAMS School of Science, University of Western Sydney, Locked Bag 1797, Penrith South DC NSW 1797, Australia [email protected] (corresponding author) ABSTRACT. Intense weathering of copper orebodies in New South Wales and Queensland, Australia has produced an unusual suite of secondary copper minerals comprising chrysocolla, azurite, malachite and the phosphates libethenite and pseudomalachite. The phosphates persist in outcrop and show a marked zoning with libethenite confined to near-surface areas. Abundant chrysocolla is also found in these environments, but never replaces the two secondary phosphates or azurite. This leads to unusual assemblages of secondary copper minerals, that can, however, be explained by equilibrium models. Data from the literature are used to develop a comprehensive geochemical model that describes for the first time the origin and geochemical setting of this style of economically important mineralization. CRANE, MARTIN J., JAMES L. SHARPE & PETER A. WILLIAMS, 2001. Formation of chrysocolla and secondary copper phosphates in the highly weathered supergene zones of some Australian deposits. Records of the Australian Museum 53(1): 49–56. Recent exploitation of oxide copper resources in Australia these deposits are characterized by an abundance of the has enabled us to examine supergene mineral distributions secondary copper phosphates libethenite and pseudo- in several orebodies that have been subjected to intense malachite associated with smaller amounts of cornetite and weathering. -
Reduction Spheroids from the Upper Carboniferous Hopewell Group, Dorchester Cape, New Brunswick: Notes on Geochemistry, Mineralogy and Genesis
Atlantic Geology 159 Reduction spheroids from the Upper Carboniferous Hopewell Group, Dorchester Cape, New Brunswick: notes on geochemistry, mineralogy and genesis Allan W. Lines 1, John Parnell^, and David J. Mossman^ * 1 Department of Physics, Engineering and Geoscience, Mount Allison University, Sackville, New Brunswick EOA 3C0, Canada 2 School of Geosciences, The Queen’s University of Belfast, Belfast, BT71NM, United Kingdom Date Received September 29, 1995 Date Accepted December 18, 1995 The bajada-playa sequence of terrestrial Upper Carboniferous redbeds of the Hopewell Group at Dorchester Cape, New Brunswick, hosts innumerable reduction spheroids in fine- to coarse-grained clastic sedimentary rocks, paleosols and caliche beds. The spheroids are grey-green, typically 2 to 3 cm in diameter, and may contain a dark, mineralized central core and less commonly one or more mineralized rings, concentric about the core. They de crease progressively in average diameter from 2.75 cm at the base to 0.85 cm at the top of an overall upward- fining 250 m thick measured stratigraphic section. Conditions controlling the genesis of the spheroids were established shortly after sedimentation. Develop ment was subtly controlled by groundwater flow patterns and by various sedimentary structures. The enclosing redbeds provide an adequate source for the metals contained in the mineralized spheroids. Low-temperature chlo ride complexes originating from evaporative fluids concentrated during redbed formation are believed to have been responsible for transport of the metals to reduction sites. Precipitation probably occurred as a result of a change in redox potential governed by electrical self-potentials of various detrital and early diagenetic grains, particularly pyrite and/or Fe-Ti oxides. -
Geology and Mineralogy of the Ape.X Washington County, Utah
Geology and Mineralogy of the Ape.x Germanium-Gallium Mine, Washington County, Utah Geology and Mineralogy of the Apex Germanium-Gallium Mine, Washington County, Utah By LAWRENCE R. BERNSTEIN U.S. GEOLOGICAL SURVEY BULLETIN 1577 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1986 For sale by the Distribution Branch, Text Products Section U.S. Geological Survey 604 South Pickett St. Alexandria, VA 22304 Library of Congress Cataloging-in-Publication Data Bernstein, Lawrence R. Geology and mineralogy of the Apex Germanium Gallium mine, Washington County, Utah (U.S. Geological Survey Bulletin 1577) Bibliography: p. 9 Supt. of Docs. no.: I 19.3:1577 1. Mines and mineral resources-Utah-Washington County. 2. Mineralogy-Utah-Washington County. 3. Geology-Utah-Wasington County. I. Title. II. Series: United States. Geological Survey. Bulletin 1577. QE75.B9 no. 1577 557.3 s 85-600355 [TN24. U8] [553' .09792'48] CONTENTS Abstract 1 Introduction 1 Germanium and gallium 1 Apex Mine 1 Acknowledgments 3 Methods 3 Geologic setting 3 Regional geology 3 Local geology 3 Ore geology 4 Mineralogy 5 Primary ore 5 Supergene ore 5 Discussion and conclusions 7 Primary ore deposition 7. Supergene alteration 8 Implications 8 References 8 FIGURES 1. Map showing location of Apex Mine and generalized geology of surrounding region 2 2. Photograph showing main adit of Apex Mine and gently dipping beds of the Callville Limestone 3 3. Geologic map showing locations of Apex and Paymaster mines and Apex fault zone 4 4. Scanning electron photomicrograph showing plumbian jarosite crystals from the 1,601-m level, Apex Mine 6 TABLES 1. -
Duftite Pbcu(Aso4)(OH) C 2001-2005 Mineral Data Publishing, Version 1 Crystal Data: Orthorhombic
Duftite PbCu(AsO4)(OH) c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Orthorhombic. Point Group: 222. Crystals may be pseudo-octahedral, or elongated along [001], commonly curved and rough, to 5 mm; usually in crusts and aggregates. Physical Properties: Fracture: Conchoidal. Hardness = 4.5 D(meas.) = 6.40 D(calc.) = 6.602 Optical Properties: Subtranslucent. Color: Bright olive-green to gray-green; pale apple-green in transmitted light, generally zoned due to compositional variations. Streak: Pale green to white. Luster: Dull to vitreous on fractures. Optical Class: Biaxial (–). Dispersion: r> v,perceptible. α = 2.03–2.04 β = 2.06–2.08 γ = 2.08–2.10 2V(meas.) = Large. Cell Data: Space Group: P 212121 (synthetic). a = 7.768(1) b = 9.211(1) c = 5.999(1) Z=4 X-ray Powder Pattern: Tsumeb, Namibia. 3.26 (10), 2.85 (8), 2.65 (8), 2.57 (6), 4.21 (5), 2.28 (5), 1.87 (5) Chemistry: (1) (2) (3) (1) (2) (3) SiO2 0.44 CaO 0.75 0.9 + As2O5 26.01 26.1 26.93 H2O 2.65 − (Fe, Al)2O3 0.6 H2O 0.08 CuO 19.32 18.6 18.65 H2O 2.3 2.11 ZnO 0.46 0.7 Total 99.81 99.8 100.00 PbO 50.10 50.6 52.31 (1–2) Tsumeb, Namibia. (3) PbCu(AsO4)(OH). Mineral Group: Adelite group. Occurrence: An uncommon mineral in the oxidized zone of some hydrothermal base-metal deposits. Association: Olivenite, mottramite, azurite, malachite, wulfenite, calcite (Tsumeb, Namibia); bayldonite, beudantite, mimetite, cerussite (Cap Garonne mine, France). -
Minerals Found in Michigan Listed by County
Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee, -
New Mineral Names*
American Mineralogist, Volume 68, pages 1248-1252,1983 NEW MINERAL NAMES* Perr J. DUNN, MrcHeE'r-FLerscHen, Gr,oncB Y. CHno, Lours J. Cesnr, AND JosEpHA. MexoanrNo Biivoetite* Lcpersonnite* bright yellow and is transparent and translucent. No fluores- Unnamed CeNi-Mg uranyl silicate cence was observed under short- or long-wave UV. The mea- sureddensity is 3.97g/cmr. It is opticallybiaxial negative,2V = M. Deliensand P. Piret (1982)Bijvoetite et lepersonnite,carbon- 73" calc.,a = 1.638, : 1.666,y : 1.682;pleochroic with X pale ates hydratds d'uranyle et des terres rares de Shinkolobwe, B yellow, bright yellow and Z bnght yellow; orientation, only Zaire. Can. Mineral.. 20.231J38. I=cisgiven. = Bijvoetite The mineral is orthorhombic, Pnnm or Pnn2 with a 16.23(3), b = 38.7aQ),c : rr.73Q)4, Z : 2, (V : 7375(50)43,J.A.M.). Blivoetite and lepersonniteoccur with hydrated uranium ox- The density calculated from the unit cell parameters and the ides near primary uraninite in the lower part of the oxidation empirical formula is 4.01 g/cm3. Strongest lines in the X-ray zone at Shinkolobwe, Zaire. Bijvoetite is rare and is known only powder diffraction pattern (for CuKa) are: 8.15(100X200), from a single specimen. Associated minerals are: lepersonnite, 4.06(I 5X400),3.65(70X1 33), 3.2I (50X0.I 2.0) and 2.86(40)(283). sklodowskite, curite, uranophane, becquerelite, rutherfordine, An electronmicroprobe analysis gave: SiO22.79, UOj76.14, studtite and a CeMg-Ni uranyl silicate structurally related to Gd2O32.W,Dy2O3 1.07, Y2O3 0.41, Tb2O3 0.(D, CaO 0.45,CO2 uranophane.