A Reaction Study of Sulfur Vapor with Silver and Silver–Indium Solid Solution As a Tarnishing Test Method
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Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
Not for Publication United States Court of Appeals
NOT FOR PUBLICATION FILED DEC 20 2018 UNITED STATES COURT OF APPEALS MOLLY C. DWYER, CLERK FOR THE NINTH CIRCUIT U.S. COURT OF APPEALS CYNTHIA CARDARELLI PAINTER, No. 17-55901 individually and on behalf of other members of the general public similarly situated, D.C. No. 2:17-cv-02235-SVW-AJW Plaintiff-Appellant, v. MEMORANDUM* BLUE DIAMOND GROWERS, a California corporation and DOES, 1-100, inclusive, Defendants-Appellees. Appeal from the United States District Court for the Central District of California Stephen V. Wilson, District Judge, Presiding Argued and Submitted December 3, 2018 Pasadena, California Before: D.W. NELSON and WARDLAW, Circuit Judges, and PRATT,** District Judge. * This disposition is not appropriate for publication and is not precedent except as provided by Ninth Circuit Rule 36-3. ** The Honorable Robert W. Pratt, United States District Judge for the Southern District of Iowa, sitting by designation. Cynthia Painter appeals the district court’s order dismissing her complaint with prejudice on grounds of preemption and failure to state a claim pursuant to Federal Rule of Civil Procedure 12(b)(6). On behalf of a putative class, Painter claims that Blue Diamond Growers (“Blue Diamond”) mislabeled its almond beverages as “almond milk” when they should be labeled “imitation milk” because they substitute for and resemble dairy milk but are nutritionally inferior to it. See 21 C.F.R. § 101.3(e)(1). We have jurisdiction under 28 U.S.C. § 1291 and review the district court’s dismissal de novo. Durnford v. MusclePharm Corp., 907 F.3d 595, 601 (9th Cir. -
Black Diamond Pegmatite Custer County, South Dakota
Diamond-drilling Exploration of the Beecher No. 3- Black Diamond Pegmatite Custer County, South Dakota GEOLOGICAL SURVEY BULLETIN 1162-E Diamond-drilling Exploration of the Beecher No. 3- Black Diamond Pegmatite Custer County, South Dakota By J. A. REDDEN CONTRIBUTIONS TO ECONOMIC GEOLOGY GEOLOGICAL SURVEY BULLETIN 1162-E UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract___________._______________________.__ El Introduction.___________________________________ ________ 1 Description of pegmatite units_____________________ _____.-__ 2 Structural geology_________________________________________________ 9 Economic appraisal of the exploration____________________________ 10 References. ___ __________________________ 11 ILLUSTRATION Page PLATE 1. Outline map and sections, Beecher No. 3-Black Diamond peg- matite______________________________________ In pocket TABLE Page TABLE 1. Diamond-drill logs, Black Diamond pegmatite.____________ E3 m CONTRIBUTIONS TO ECONOMIC GEOLOGY DIAMOND-DRILLING EXPLORATION OF THE BEECHER NO. 3-BLACK DIAMOND PEGMATITE, CUSTER COUNTY, SOUTH DAKOTA By J. A. REDDEN ABSTRACT Diamond-drilling at the Beecher No. 3-Black Diamond pegmatite, Ouster County, S. Dak., has provided information that modifies and supplements findings reported previously (Redden, 1959). Two zones not exposed at the surface were found during the drilling: a quartz-albite-perthite-muscovite-pegmatite zone and a quartz-albite-perthite-spodumene pegmatite zone. Previous concepts of the structure near the surface require no significant change, but the new data make possible a greatly improved interpretation of the structure at depth. The most notable change is the recognition of a narrow constriction in the pegmatite at a depth of 60 to 100 feet. -
United States Patent (19) 11 Patent Number: 4,640,713 Harris 45 Date of Patent: Feb
United States Patent (19) 11 Patent Number: 4,640,713 Harris 45 Date of Patent: Feb. 3, 1987 (54) TARNESHREMOVER/METAL POLISH 3,458,300 7/1969 Duvall et al. ........................... 106/3 FORMULATION COMPRISING A METAL 3,502,503 3/1970 Bartlo et al. ............................ 134/2 IODIDE, ANACID, AND WATER 3,518,098 6/1970 Ford et al. .............................. O6/3 3,582,366 6/1971 Brieger et al. 75 Inventor: Robert B. Harris, Racine County, 3,687,855 8/1972 Halpern..... Wis. 3,879,216 4/1975 Austin ..................................... 134/4 3,914, 161 10/1975 Yonezawa et al. a 73 Assignee: S. C. Johnson & Son, Inc., Racine, 3,997,460 12A1976 Sirine ............. Wis. 4,097,590 6/1978 Weisz ..... 4,116,699 9/1978 Rooney...... ...10673 21 Appl. No.: 672,966 4,207,310 6/1980 Langford ... ... 252A106 22) Filed: Nov. 19, 1984 4,444,756 4/984 Schlissier ........................... 252/106 51 Int. Cl. .......................... C09G 1/04; C09G 1/06 Primary Examiner-Theodore Morris (52) U.S. C. ........................................... 106/3; 106/10 57 ABSTRACT 58) Field of Search ............................. 106/3; 252/106 A tarnish remover/metal polish formulation comprising 56 References Cited water, an acid, and metal iodide, such as potassium U.S. PATENT DOCUMENTS iodide, is described. The components of the formulation chemically react with the tarnish or stain on a metal 840,167 1/1907 Springborn et al. .................... 106/6 1,280,939 0/1918 Allen ................ ... 06/3 surface, removing the tarnish or stain while leaving the 1,737,222 11/1929 Dewey, Jr. ... 106/9 metal unaffected. -
Copper Alloys
THE COPPER ADVANTAGE A Guide to Working With Copper and Copper Alloys www.antimicrobialcopper.com CONTENTS I. Introduction ............................. 3 PREFACE Conductivity .....................................4 Strength ..........................................4 The information in this guide includes an overview of the well- Formability ......................................4 known physical, mechanical and chemical properties of copper, Joining ...........................................4 as well as more recent scientific findings that show copper has Corrosion ........................................4 an intrinsic antimicrobial property. Working and finishing Copper is Antimicrobial ....................... 4 techniques, alloy families, coloration and other attributes are addressed, illustrating that copper and its alloys are so Color ..............................................5 adaptable that they can be used in a multitude of applications Copper Alloy Families .......................... 5 in almost every industry, from door handles to electrical circuitry to heat exchangers. II. Physical Properties ..................... 8 Copper’s malleability, machinability and conductivity have Properties ....................................... 8 made it a longtime favorite metal of manufacturers and Electrical & Thermal Conductivity ........... 8 engineers, but it is its antimicrobial property that will extend that popularity into the future. This guide describes that property and illustrates how it can benefit everything from III. Mechanical -
In Montana's Gravel Bars; Diamond Once Found in Pioneer Gulch
' w .- CHOTBAU ÀCANTHA in Montana’s Gravel Bars; Diamond Once Found in Pioneer Gulch By IDWAIO B. REYNOLDS 1T is doubtful If even Ripley weald consider diamond mining in Mon- New $225,000 Residence Hall At State University Completed bat- such a venture is not Montana Dwarf Looks Back . entirely improbable. Mining in the ITreasure mate always baa been connected with tbe various mrtsH ■ On Life of Colorful Events principally gold, silver, copper, sine and lead. It is on these metals that With not more than three years left birthday he grew to his full height oí Butte has gained its reputation of be to live, Don Ward of Missoula, Mon 47 inches. As a trapeze performer his ing situated on "the richest hill on tana’s only native-son dwarf, is out toweight was 75 pounds. He now weighs earth,” and that Anaconda was created "make the most” of his remaining days,123 pounds. as the site of the world’s largest copper looking back on a colorful past packed Butte Favorite City smelter with Great Falls as the site with a multitude of interesting ex In recent years Ward has worked as of one of the world's greatest copper periences such as the average personan entertainer in various Montana refineries. is never privileged to enjoy. cities and appeared at several celebra However, despite all the fame gained Now 64, the 47-inch-tall man who tions. Butte is among his favorite cities. by these three cities in the mining was Mrs. Tom Thumb’s original coach “I’ve been three years in Europe and world for metals, Montana is also famed man in Europe, who traveled the circus 19 times in every state and every as a mining state in which precious routes for 19 years and who is the onlyprovince of Canada, but I’ve never met gems are found in commercially im little man ever to work on a trapeze,a better class of people, more con portant quantities. -
Diamond Craters Oregon's Geologic
Text by Ellen M. Benedict, 1985 Features at stops correspond to points on a clock ago, a huge mass of hot gases, volcanic ashes, bits face. Imagine that you are standing in the middle of a of pumice and other pyroclastics (fire-broken rock) Travel And Hiking Hints clock face. Twelve o’clock is the road in front of you violently erupted. The blast – greater than the May and 6 o’clock the road behind. If you always align the 18, 1980, eruption of Mt. St. Helens – deposited a Diamond Craters is located in the high desert country clock face with the road, you should be able to locate layer of pyroclastics 30 to 130 feet thick over an area about 55 miles southeast of Burns, Oregon. It’s an the features. almost 7,000 square miles! isolated place and some precautions should be taken . when traveling in the area. Start Tour. Mileage begins halfway Pyroclastics are between milepost 40 and 41 on State normal behavior Diamond Craters has no tourist facilities. The nearest Highway 205 at the junction to Diamond. for magmas place where gasoline is sold is at Frenchglen. Turn left. (subsurface That’s the opinion held by scores of molten rocks) Keep your scientists and educators who have visited Diamond, Oregon, a small ranching community, was of rhyolitic (a vehicle on named in 1874 for Mace McCoy’s Diamond brand. volcanic material and studied the area. It has the “best and hard-packed The nearby craters soon became known as Diamond related to granite) most diverse basaltic volcanic features in the road surfaces Craters. -
The Care and Preservation of Historical Silver by CLARA DECK, CONSERVATOR REVISIONS by LOUISE BECK, CONSERVATOR
The Care and Preservation of Historical Silver BY CLARA DECK, CONSERVATOR REVISIONS BY LOUISE BECK, CONSERVATOR Introduction Historical silver can be maintained for years of use and enjoyment provided that some basic care and attention is given to their preservation. The conservation staff at The Henry Ford have compiled the information in this fact sheet to help individuals care for their objects and collections. The first step in the care of all collections is to understand and minimize or eliminate conditions that can cause damage. The second step is to follow basic guidelines for care, handling and cleaning. Most people know that silver is a white, lustrous metal. Pure or “fine” silver is called “Sterling” if it is made up of no less than 925 parts silver to 75 parts alloy. Sterling will thus often have ‘.925’ stamped somewhere on it, as an identifier. Silver objects, especially coins and jewelry, contain copper as an alloying metal for added hardness. The copper may corrode to form dark brown or green deposits on the surface of the metal. Silver is usually easy to differentiate from lead or pewter, which are generally dark gray and not very shiny. Silver is often plated (deposited) onto other metallic alloys, almost always with an intermediate layer of copper in between. The earliest plating process, “Sheffield Plate” was developed in England in 1742. By the mid-19th century, the process was largely replaced by electroplating (which used less silver). The base metal in plated artifacts may consist of any of the following metals or alloys: copper, brass, “German silver” or “nickel silver” (50% copper, 30% nickel, 20% zinc), “Brittania metal” (97% tin, 7% antimony, 2% copper), or a “base” silver containing a high percentage of copper. -
JD: Jewelry Design
JD: Jewelry Design JD 101 — Introduction to Jewelry JD 115 — Metal Forming Techniques: Fabrication Chasing and Repousse 2 credits; 1 lecture and 2 lab hours 1.5 credits; 3 lab hours Basic processes used in the design and Introduces students to jewelry-forming creation of jewelry. Students fabricate their techniques by making their own dapping own designs in the studio. and chasing tools by means of forging, JD 102 — Enameling Techniques for annealing, and tempering. Using these Precious Metals/Fine Jewelry/Objects tools, objects are created by repousse and D'Art other methods. 2 credits; 1 lecture and 2 lab hours Prerequisite(s): all first-semester Jewelry Vitreous enameling on precious metals. Design courses or approval of chairperson Studies include an emphasis on the "Co-requisite(s): JD 116, JD 122, JD metallurgical properties of gold, silver, and 134, JD 171, and JD 173 or approval of platinum and their chemical compatibility chairperson. with enamels. Surface treatments, ancient JD 117 — Enameling for Contemporary and modern, that intensify the jewel- Jewelry like qualities of vitreous enamel on 2 credits; 1 lecture and 2 lab hours precious metal will be explored. along with Vitreous enamel has been used for construction techniques that help students centuries as a means of adding color transform glass into beautiful, functional and richness to precious objects and jewelry and objects of art. jewelry. This course examines historical Prerequisite(s): JD 101. and contemporary uses of enamel, and JD 103 — Jewelry and Accessories explores the various methods of its Fabrication (Interdisciplinary) application, including cloisonne, limoges 2 credits; 1 lecture and 2 lab hours and champleve, the use of silver and gold This is an interdisciplinary course cross- foils, oxidation, surface finishing and setting listed with LD 103. -
Kimberley Process Clean Diamond Trade Act Fact Sheet
Kimberley Process Clean Diamond Trade Act The Kimberley Process Certification Scheme Export Requirements regulates the international rough diamond trade. The . Exports of rough diamonds from the United scheme is an internationally recognized certification States must be accompanied by a Kimberley system that establishes requirements to designate certificate, obtained from a U.S. Kimberley shipments of rough diamonds as conflict-free and prevent Process licensee and validated by the U.S. them from entering legitimate trade. Census Bureau. The Clean Diamond Trade Act was implemented on . Rough diamonds may only be exported to countries that participate in the Kimberley Process. July 29, 2003. The act requires that rough diamonds www.federalregister.gov imported or exported from the United States be controlled through the Kimberley Process. Exports of rough diamonds must be sealed in a tamper-resistant container. Packaging must have Importing requirements an indicator or barrier that can reasonably provide visible evidence that tampering had . Imports of rough diamonds must be accompanied occurred. by an original Kimberley Process certificate. U.S. Census Bureau requires that export information in filed through the automated export . Rough diamonds may be imported or exported system. Submitting export information through only to countries that participate in the Kimberley this system must be done in advance and Process. www.federalregister.gov confirmed by the return of an internal transaction Sheet number. Regardless of quantity or value, shipments must be entered on a formal entry. Importers may . Returning this number to the filer will validate the retain a customs broker at the relevant port of Kimberley certificate to export rough diamonds entry to assist with filing. -
Gemstones by Donald W
GEMSTONES By Donald W. olson Domestic survey data and tables were prepared by Nicholas A. Muniz, statistical assistant, and the world production table was prepared by Glenn J. Wallace, international data coordinator. In this report, the terms “gem” and “gemstone” mean any gemstones and on the cutting and polishing of large diamond mineral or organic material (such as amber, pearl, petrified wood, stones. Industry employment is estimated to range from 1,000 to and shell) used for personal adornment, display, or object of art ,500 workers (U.S. International Trade Commission, 1997, p. 1). because it possesses beauty, durability, and rarity. Of more than Most natural gemstone producers in the United states 4,000 mineral species, only about 100 possess all these attributes and are small businesses that are widely dispersed and operate are considered to be gemstones. Silicates other than quartz are the independently. the small producers probably have an average largest group of gemstones; oxides and quartz are the second largest of less than three employees, including those who only work (table 1). Gemstones are subdivided into diamond and colored part time. the number of gemstone mines operating from gemstones, which in this report designates all natural nondiamond year to year fluctuates because the uncertainty associated with gems. In addition, laboratory-created gemstones, cultured pearls, the discovery and marketing of gem-quality minerals makes and gemstone simulants are discussed but are treated separately it difficult to obtain financing for developing and sustaining from natural gemstones (table 2). Trade data in this report are economically viable deposits (U.S. -
Garnets from the Camafuca-Camazambo Kimberlite (Angola)
Anais da Academia Brasileira de Ciências (2006) 78(2): 309-315 (Annals of the Brazilian Academy of Sciences) ISSN 0001-3765 www.scielo.br/aabc Garnets from the Camafuca-Camazambo kimberlite (Angola) EUGÉNIO A. CORREIA and FERNANDO A.T.P. LAIGINHAS Departamento de Geologia, Faculdade de Ciências da Universidade do Porto Praça de Gomes Teixeira, 4050 Porto, Portugal Manuscript received on November 17, 2004; accepted for publication on June 13, 2005; presented by ALCIDES N. SIAL ABSTRACT This work presents a geochemical study of a set of garnets, selected by their colors, from the Camafuca- Camazambo kimberlite, located on northeast Angola. Mantle-derived garnets were classified according to the scheme proposed by Grütter et al. (2004) and belong to the G1, G4, G9 and G10 groups. Both sub-calcic (G10) and Ca-saturated (G9) garnets, typical, respectively, of harzburgites and lherzolites, were identified. The solubility limit of knorringite molecule in G10D garnets suggests they have crystallized at a minimum pressure of about 40 to 45 kbar (4– 4.5 GPa). The occurrence of diamond stability field garnets (G10D) is a clear indicator of the potential of this kimberlite for diamond. The chemistry of the garnets suggests that the source for the kimberlite was a lherzolite that has suffered a partial melting that formed basaltic magma, leaving a harzburgite as a residue. Key words: kimberlite, diamond, garnet, lherzolite, harzburgite. INTRODUCTION GEOCHEMICAL STUDY OF GARNETS The Camafuca-Camazambo kimberlite belongs to The geochemical study of mantle-derived garnets a kimberlite province comprising over a dozen of occurring in kimberlites progressed remarkably in primary occurrences of diamond, located along- recent years, as their chemistry is not only a possible side the homonymous brook which is a tributary of indicator of the presence of diamonds in their host the Chicapa river, in the proximity of the Calonda rock but also their abundance is a likely indicator of village, northeast Angola (Fig.