The Nevada Mineral Industry 2014

Total Page:16

File Type:pdf, Size:1020Kb

The Nevada Mineral Industry 2014 Nevada Bureau of Metals Mines and Geology Industrial Minerals Oil and Gas Special Publication MI-2014 Geothermal The Nevada Exploration Development Mineral Industry Mining 2014 Processing 1.0’ @ 80.056 opt Au Diluted grade: 25.215 opt Au over 3.2’ This report describes mineral, oil and gas, and geothermal activities and accomplishments in Nevada in 2014: production statistics, exploration and development including drilling for petroleum and geothermal resources, discoveries of orebodies, new mines opened, and expansion and other activities of existing mines. Statistics of known gold and silver deposits, and directories of mines and mills are included. Nevada System of Higher Education 2016 Board of Regents Daniel Klaich, Chancellor Andrea Anderson Sam Lieberman University of Nevada, Reno Cedric Crear Kevin C. Melcher Marc Johnson, President Mark W. Doubrava Kevin J. Page Jason Geddes Allison Stephens College of Science Trevor Hayes Rick Trachok, Chairman Jeffrey Thompson, Dean James Dean Leavitt Michael B. Wixom, Vice Chairman Mackay School of Earth Sciences and Engineering Russell Fields, Director Nevada Bureau of Mines and Geology James E. Faulds, Director/State Geologist Scientific Research Staff Research and Administrative Support Staff Economic Geology, Geologic Mapping, Cartography and Publication Support and Geologic Framework Jennifer Vlcan, Cartographic/GIS Manager James E. Faulds, Professor Jack Hursh, Cartographer/Publications Specialist Christopher D. Henry, Research Geologist Rachel Micander, Cartographer/GIS Specialist Nicholas H. Hinz, Research Geologist Katie Ryan, Cartographer/GIS Specialist Mike Ressel, Assistant Professor-Economic Geologist Irene Seelye, Cartographer/GIS Specialist Center for Research in Economic Geology Publication Sales and Information John Muntean, Director, Associate Professor Craig M. dePolo, Supervisor Great Basin Center for Geothermal Energy David Davis, Geologic Information Specialist Bridget Ayling, Director, Associate Professor Charlotte Stock, Sales Manager Bret Pecoraro, Development Technician Geologic Hazards and Engineering Geology Seth Dee, Geologic Mapping Specialist Administration Craig M. dePolo, Research Geologist Alex Nesbitt, Administrative Assistant Rich Koehler, Assistant Professor Linda Goar, Accounting Assistant Alan R. Ramelli, Research Geologist Nevada Geodetic Laboratory Geoffrey Blewitt, Research Professor William C. Hammond, Research Professor Corné W. Kreemer, Research Professor Cover Photo: Vonnie Vein Klondex Mines Ltd’s Fire Creek Mine Lander County Photographers: Eric Hobbs & Justin B. Milliard Nevada Bureau of Mines and Geology Special Publication MI-2014 The Nevada Mineral Industry 2014 Contents 3 Overview by John L. Muntean 13 Metals by David A. Davis and John L. Muntean 46 Major Precious-Metal Deposits by David A. Davis and John L. Muntean 100 Other Metallic Deposits by David A. Davis and John L. Muntean 110 Industrial Minerals by David A. Davis 125 Industrial Mineral Deposits by David A. Davis 131 Geothermal Energy by Lisa Shevenell 149 Oil and Gas by David A. Davis 160 Directory of Mining and Milling Operations by David A. Davis 2016 OVERVIEW by John L. Muntean This report highlights activities through 2014 in metals, Nevada was valued at $204.5 million. Construction industrial minerals, geothermal energy, and petroleum. The aggregate ranked fifth, with a value of $166 million. value of overall mineral and energy production in Nevada The section on Metals and the tables in Major in 2014 decreased 15.6% to just under $7.58 billion (table Precious-Metal Deposits and Other Metallic Deposits 1, fig. 1). The main cause, as was the case in 2013, was the provide details on exploration, new deposit discoveries, new decreasing price of gold from an all-time high average cost mine openings, mine closures, additions to reserves, and of $1,669/ounce in 2012, to $1,411/ounce in 2013, and to mine expansions. As has been the case for many years, gold $1,266/ounce in 2014. Gold production decreased for the continues to be the leading commodity produced in Nevada. second year in a row, declining 9.1% to 4.94 million ounces, Production of gold in 2014 came mainly from 14 major the first time it dropped below 5 million ounces since 1988 mining operations that each produced greater than 50,000 (fig. 2). Nevertheless, gold comprised 82.5% of the value of ounces. The Carlin trend in northeastern Nevada accounted Nevada’s mineral and energy production. Nevada led the for 35% of the total production, about the same as in 2013. nation in the production of gold and barite, and was the only There were nine mining operations not on the Carlin trend state that produced magnesite, lithium, and the specialty that each produced over 100,000 ounces of gold. clays, sepiolite and saponite. Other commodities mined and Nevada and the U.S. have produced a significant produced in Nevada in 2014, in order of value, included portion of the world’s gold. The U.S. Geological Survey copper, silver, geothermal energy, construction aggregate estimates that total world gold production, since the (sand, gravel, and crushed stone, including limestone and beginning of civilization, has been approximately 5.63 dolomite), diatomite, lime (produced from limestone and billion ounces. Although this seems like a large quantity, all dolomite), gypsum, petroleum, silica, and molybdenum. the gold ever mined would fit into a cube only ~21 m (68 ft) Additional mined materials with production values less than on a side. Interestingly, about 85% of that gold is still in use $10,000,000 in 2014 were clays, perlite, iron ore, dimension (in bullion, coins, jewelry, electronics, etc.), and most gold stone, salt, and semiprecious gemstones (opal). Locations of currently in use will be recycled. Total gold production in many of the sites mentioned in the text of this report are Nevada through 2014 was 213.4 million ounces. shown on NBMG Open-File Report 2014-01, Nevada Remarkably, 89% has been produced since the Carlin mine Active Mines and Energy Producers, which is available at began production in 1965; 86% has been produced during http://pubs.nbmg.unr.edu/Active-mines-and-energy-2014- the current boom from 1981 to the present; and 27% has p/of2014-01.htm. been produced in the last ten years. Cumulative U.S. Nevada dropped behind Arizona to second in the production, primarily since 1835, is approximately 581 United States, in terms of value of overall nonfuel million ounces or about 10.3% of total world gold (excluding oil, gas, coal, uranium, and geothermal) mineral production, and total Nevada production is 3.8% of production in 2014 (according to the U.S. Geological cumulative world production. The Carlin trend alone Survey, Mineral Commodity Summaries 2014, accounts for 1.5% of all the gold ever mined in the world. http://minerals.usgs.gov/minerals/pubs/mcs/2015/mcs2015 By the end of 2014, cumulative production from the Carlin .pdf). Arizona is the country’s major copper producer. trend was 84.2 million ounces, assuring its place as one of Minnesota, the leading iron ore producer in the U.S., was the most productive gold-mining districts in the world. third. Texas rose to fourth, mainly due to its booming Nevada continues to be in the midst of the biggest gold construction industry and demand for aggregate and boom in U.S. history, as the graph of historical U.S. gold cement. Utah was fifth, mainly because of its Bingham production illustrates (fig. 3). The recent surge in Canyon copper-gold mine near Salt Lake City. The production in the U.S. is largely the result of discoveries of contributions that mining makes to the economies of Carlin-type gold deposits and other deposits in which gold Nevada and the U.S. are significant in terms of jobs, occurs primarily in grains that are too small to be visible to commerce, taxes, improvements to the infrastructure, and the naked eye. These deposits are mostly in Nevada. The lowering of the U.S. trade deficit. U.S. production so far in the current boom, the period since Nevada's production of gold, valued at $6.26 billion, 1981, has been 261 million ounces. This is significantly accounted for 73% of the U.S. total and helped the U.S. greater than the total U.S. production during the era of the become the fourth leading gold producer in the world in California gold rush (1849 to 1859, with 29 million ounces, 2014. Nevada alone accounted for 5.4% of world although some estimates of unreported production may production of gold, which was approximately 92 million bring that figure up to 70 million ounces); the Comstock ounces in 2014. Only China, Australia, Russia, and Canada (Nevada) era from 1860 to 1875 (with 34 million ounces); produced more gold than the state of Nevada. Second to and the period from 1897 to 1920, when Goldfield gold in terms of Nevada's mineral value in 2014 was copper (Nevada), the Black Hills (South Dakota), Cripple Creek ($427 million), followed by silver ($209 million), which (Colorado), and byproduct gold production from copper was produced chiefly as a byproduct of gold production. mines in Arizona and Utah contributed to cumulative Electrical power from geothermal energy production in production of 95 million ounces. U.S. production in the last 3 TABLE 1. MINERAL, GEOTHERMAL POWER, AND PETROLEUM PRODUCTION IN NEVADA1 2013 (revised) 2014 Change from 2013 to 2014 Commodity Quantity Value Quantity Value Quantity Value (millions) (millions) Gold (thousand troy ounces) 5,436 $7,672.1 4,941 $6,256.7 -9.1% -18.4% Silver (thousand troy ounces)
Recommended publications
  • GEM FOCUS August 2020
    GEM FOCUS August 2020 GOLDSTONE, SUNSTONE, AVENTURESCENCE; A SPARKLING ENIGMA OF CENTURIES... emstones with unusual optical effects are know as sunstone feldspar today. Goldstone is cre - defined as phenomenal gems. Their unusual ated by mixing microscopic copper platelets into Geffect can designate a variety within a molten glass. The sheen and earthy color of this species and add value. i.e., star sapphire. Synthetic material was ideal for Italian mosaics and more counterparts or simulants are often seen, especially affordable jewelry, whereas much larger blocks when the natural counterpart is particularly valuable were used to create ornamental objects such as such as natural alexandrite and color change syn - snuff bottles, small bowls or carved figurines. A thetic sapphire. Aventurescence is a phenomenon common story to its origin purports that the Italian caused by light reflecting micro platelets in a gem glass producers discovered this particular effect by and is easily recognizable from the glittering sheen- accident, but when this was is not clear. Accounts like effect. While green mica crystals in quartz cre - of the first production date vary from one source to ates aventurine quartz, hematite and ilmenite crys - another and are stated as from 11th century to 13th tals create the same effect in sunstone feldspar. century. It is true that this rather attractive Murano glass with reddish brown speckles was a popular Out of all the phenomena seen in gems, aventures - and expensive glass production in Italy for many cence, especially the yellow-brown type, has been centuries but it is hard to believe that sunstone the subject of a long-standing discussion.
    [Show full text]
  • Mule Deer and Antelope Staff Specialist Peregrine Wolff, Wildlife Health Specialist
    STATE OF NEVADA Steve Sisolak, Governor DEPARTMENT OF WILDLIFE Tony Wasley, Director GAME DIVISION Brian F. Wakeling, Chief Mike Cox, Bighorn Sheep and Mountain Goat Staff Specialist Pat Jackson, Predator Management Staff Specialist Cody McKee, Elk Staff Biologist Cody Schroeder, Mule Deer and Antelope Staff Specialist Peregrine Wolff, Wildlife Health Specialist Western Region Southern Region Eastern Region Regional Supervisors Mike Scott Steve Kimble Tom Donham Big Game Biologists Chris Hampson Joe Bennett Travis Allen Carl Lackey Pat Cummings Clint Garrett Kyle Neill Cooper Munson Sarah Hale Ed Partee Kari Huebner Jason Salisbury Matt Jeffress Kody Menghini Tyler Nall Scott Roberts This publication will be made available in an alternative format upon request. Nevada Department of Wildlife receives funding through the Federal Aid in Wildlife Restoration. Federal Laws prohibit discrimination on the basis of race, color, national origin, age, sex, or disability. If you believe you’ve been discriminated against in any NDOW program, activity, or facility, please write to the following: Diversity Program Manager or Director U.S. Fish and Wildlife Service Nevada Department of Wildlife 4401 North Fairfax Drive, Mailstop: 7072-43 6980 Sierra Center Parkway, Suite 120 Arlington, VA 22203 Reno, Nevada 8911-2237 Individuals with hearing impairments may contact the Department via telecommunications device at our Headquarters at 775-688-1500 via a text telephone (TTY) telecommunications device by first calling the State of Nevada Relay Operator at 1-800-326-6868. NEVADA DEPARTMENT OF WILDLIFE 2018-2019 BIG GAME STATUS This program is supported by Federal financial assistance titled “Statewide Game Management” submitted to the U.S.
    [Show full text]
  • Got a Pocket Full of Sunstone? Maybe Think Twice
    Page 1 of 5 Got a pocket full of Sunstone? Maybe think twice Sunstone falls part of the Feldspar The larger and more abundant the mineral group. It is known for inclusions are, the more exhibiting what is called “Aventurescent” the stone will be “Aventurescence”. and the deeper the golden colour will appear. There are also transparent Sunstones from Oregon in the USA. They are often green and/or red in colour, with small copper inclusions (often in “streams”) creating a Aventurescence is a type of “Schiller” effect. iridescence (a play-of-colour) that is caused by the reflection of small, thin and platy inclusions - copper, goethite and/or hematite in the case of Sunstone - that are spread in a parallel orientation through the gem. This causes interference of light between the layers of platelets which creates the glittery sheen associated with Sunstone (see image on the above right). Kaylan Khourie, FGA All rights reserved. 08/09/2019 Page 2 of 5 Sunstone falls into three species Sunstone can fall into three species of the Feldspar group: Orthoclase, Oligoclase and Labradorite (this is also into where the Oregon material falls). Orthoclase falls under the “Alkali Feldspar” category whereas Oligoclase and Labradorite fall under the “Plagioclase Feldspar” category. Below is a table of each species of Sunstone and some of their properties: Specific Refractive Species Chemical Composition Birefringence Gravity Index Orthoclase KAlSi₃O₈ 2.58 1.518 - 1.526 0.005 -0.008 Solid solution between Oligoclase 2.65 1.539 - 1.547 0.007 - 0.010 NaAlSi₃O₈ and CaAlSi₂O₈ Solid solution between Labradorite 2.70 1.559 - 1.568 0.007 - 0.010 NaAlSi₃O₈ and CaAlSi₂O₈ ↳ Oregon Solid solution between 2.67 - 2.72 1.563 - 1.572 0.009 material NaAlSi₃O₈ and CaAlSi₂O₈ However, the gems being marketed as “Sunstone” are almost always pieces of man-made glass containing an abundance of tiny copper inclusions.
    [Show full text]
  • Lemhi County, Idaho
    DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR BUIJLETIN 528 GEOLOGY AND ORE DEPOSITS 1 OF LEMHI COUNTY, IDAHO BY JOSEPH B. UMPLEBY WASHINGTON GOVERNMENT PRINTING OFFICE 1913 CONTENTS. Page. Outline of report.......................................................... 11 Introduction.............................................................. 15 Scope of report......................................................... 15 Field work and acknowledgments...................................... 15 Early work............................................................ 16 Geography. .........> ....................................................... 17 Situation and access.........................--.-----------.-..--...-.. 17 Climate, vegetation, and animal life....................----.-----.....- 19 Mining................................................................ 20 General conditions.......... 1..................................... 20 History..............................-..............-..........:... 20 Production.................................,.........'.............. 21 Physiography.............................................................. 22 Existing topography.................................................... 22 Physiographic development............................................. 23 General features...............................................'.... 23 Erosion surface.................................................... 25 Correlation............. 1..........................................
    [Show full text]
  • COBALT GLASS AS a LAPIS LAZULI IMITATION by George Bosshart
    COBALT GLASS AS A LAPIS LAZULI IMITATION By George Bosshart A ~lecl<laceof round beads offered as "blue quartz from India" was analyzed by gemological and addition~~l advanced techniques. The violet-blue ornamental material, which resembled fine-q~ralitylapis lazuli, turned OLJ~LO be a nontransparent cobalt glass, unlil<e any glass observed before as a gem substit~zte.The characteristic color irregularities of lapis (whjtein blue) had been imjtated by white crystdlites of low- crjstobalite .ir~cludeclin the deep blue glass. The gemological world is accustomed to seeing gemstones from new localities, as well as new or improved synthetic crystals. With this in mind, it is not surprising that novel gem imitations are also encountered. One recent example is 'lopalitellla 400 500 600 700 convincing yet inexpensive plastic imitation of Wavelength A (nm) white opal manufactured in Japan. This article de- scribes another gem substitute that recently ap- Figure 1. Absorptio~ispectrum of a cobalt glass peared in the inarlzetplace. imitating lapis lazuli recorded ~hrougha chjp of Hearing of an "intense blue quartz from India1' approximately 2.44 inm thickness in the range of was intriguing enough to arouse the author's sus- 820 nm 10 300 nm, ot room temperature (Pye picion when a neclzlace of spherical opaque Ui7jcam SP8-100 Spectrophotometer). violet-blue 8-mm beads was submitted to the SSEF laboratory for identification. Because blue quartz in nature is normally gray-blue as a result of the refractive index of the tested material (1.508)does presence of Ti02(Deer et al.! 1975! p. 2071 or tour- not differ marlzedly from that of lapis (approxi- maline fibers (Stalder) 1967)! this particular iden- mately 1.50)/ its specific gravity of 2.453 is tification could be immediately rejected.
    [Show full text]
  • 2008 Washington Game Status and Trend Report
    S T A T E O F W A S H I N G T O N 20082008 GameGame StatusStatus andand TrendTrend ReRepportort AN OFFICIAL PUBLICATION OF THE STATE OF WASHINGTON 2008 GAME STATUS AND TREND REPORT July 1, 2007 – June 30, 2008 Washington Department of Fish and Wildlife 600 Capitol Way North Olympia, WA 98501-1091 STATE OF WASHINGTON Chris Gregoire Governor WASHINGTON DEPARTMENT OF FISH AND WILDLIFE Jeff P. Koenings, Ph.D. Director WILDLIFE PROGRAM Dave Brittell Assistant Director GAME DIVISION Dave Ware Game Division Manager This Program Receives Federal Aid in Wildlife Restoration, Project W-96-R, Statewide Wildlife Management. This report should be cited as: Washington Department of Fish and Wildlife. 2008. 2008 Game status and trend report. Wildlife Program, Washington Department of Fish and Wildlife, Olympia, Washington, USA. TABLE OF CONTENTS Deer .................................................................................................................................................. 1 Statewide Summary .................................................................................................................. 3 Region 1, PMUs 11, 13, GMUs 101-124 ................................................................................. 7 Region 1, PMUs 14, 15, GMUs 127-142 ............................................................................... 12 Region 2, PMUs 21, 22, GMUs 203-243 ............................................................................... 16 Region 2, PMUs 21, 23, 26 GMUs 243-269 .........................................................................
    [Show full text]
  • A Fundamental Study of Copper and Cyanide Recovery from Gold Tailings by Sulfidisation
    Western Australian School of Mines Department of Metallurgical and Minerals Engineering A Fundamental Study of Copper and Cyanide Recovery from Gold Tailings by Sulfidisation Andrew Murray Simons This thesis is presented for the Degree of Doctor of Philosophy of Curtin University June 2015 STATEMENT OF AUTHENTICITY To the best of my knowledge and belief this thesis contains no material previously published by any other person except where due acknowledgment has been made. This thesis contains no material which has been accepted for the award of any other degree or diploma in any university. Andrew Murray Simons i ABSTRACT Cyanide soluble copper in gold ores causes numerous problems for gold producers. This includes increased costs from high cyanide consumption and a requirement to destroy cyanide in the tailings before discharge into a tailings storage facility. Over recent years a cyanide recycling process known as SART (sulfidisation, acidification, recycle, and thickening) has gained attention as a method to remediate the increased costs and potential environmental impact caused by using cyanidation to process copper bearing gold ores. While sulfidisation processes, such as SART, have been demonstrated within the laboratory to be effective, there are several gold processing operations using sulfidisation which report high sulfide consumption compared to the expected reaction stoichiometry. Further to this problem, there is a lack of fundamental studies of sulfidisation of cyanide solutions resulting in a poor understanding of how various process variables impact the process. This thesis details work on sulfidisation of copper cyanide solutions to systematically determine the impact of process variables and impurities on the SART process.
    [Show full text]
  • Glossary of Jewellery Making and Beading Terms
    Glossary of Jewellery Making and Beading Terms A jewellery glossary of beading terms and jewellery making terminology combining clear images with easy to understand dictionary like definitions. This bead glossary also provides links to more in depth content and bead resources. It can be used as a beading A to Z reference guide to dip into as needed, or as a beading and jewellery glossary for beginners to help broaden beading and jewellery making knowledge. It is particularly effective when used alongside our Beading Guides, Histories, Theories and Tutorials, or in conjunction with our Gemstones & Minerals Glossary and Venetian Glass Making Glossary. A ABALONE These edible sea creatures are members of a large class of molluscs that have one piece shells with an iridescent interior. These shells have a low and open spiral structure, and are characterized by several open respiratory pores in a row near the shell’s outer edge. The thick inner layer of the shell is composed of a dichroic substance called nacre or mother-of-pearl, which in many species is highly iridescent, giving rise to a range of strong and changeable colors, making it ideal for jewellery and other decorative objects. Iridescent nacre varies in colour from silvery white, to pink, red and green- red, through to deep blues, greens, and purples. Read more in our Gemstones & Minerals Glossary. Above are examples of Paua and Red Abalone. ACCENT BEAD Similar in purpose to a Focal Bead, this is a bead that forms the focus for a piece of jewellery, but on this occasion rather then through its size, it is usually through contrast.
    [Show full text]
  • Davide Fuin Italy’S Brightest, Best, and Last
    Hot Glass Studio Profile Davide Fuin Italy’s Brightest, Best, and Last by Shawn Waggoner t is impossible to find another object that represents the centuries- Gherardo Ortalli, president of the Istituto; Gabriella Belli, director old history of Venetian glass better than the goblet. It would be of the Fondazione Musei Civici di Venezia; Georg J. Riedel, presi- Iequally challenging to find a gottieri, a master glassmaker who dent of Riedel Crystal; and Rosa Barovier, glass historian, selected specializes in the blowing of goblets, more respected and revered the award recipients and were in attendance. William Gudenrath, than Italy’s Davide Fuin. resident advisor for The Studio at the Corning Museum of Glass On September 15, 2015, at Palazzo Franchetti on the Grand Canal (CMOG), Corning, New York, was also present at the ceremony. in Venice, the Istituto Veneto di Scienze Lettere ed Arti honored “Fuin’s work was selected because he is the most visible, glass master Fuin for excelling in his ability to make blown work arguably the best, and some would say the last practitioner of the according to Murano tradition, highlighting especially the tech- tradition of goblet makers on Murano, who are said to date from niques of reticello and retortoli filigree, incalmo, and avventurina. the Renaissance. The goblet tradition in both Murano and Venice is in considerable peril,” says Gudenrath, who himself teaches advanced courses in Venetian techniques and ensures excellence in the CMOG studio facility and its programs. Born in 1962 on Murano, Fuin still lives and works on the island. Considered one of the most skilled masters of the last 30 years, he has collaborated with Italy’s famous glass houses including Venini, Toso, Pauly, Salviati, Elite, and De Majo, as well as with many international artists and designers.
    [Show full text]
  • Seeds of Light, Inc
    Seeds of Light, Inc. Product Descriptions If there are any blockages in the chakras, applying the correct stones, Condition of Sale color and/or light will enable the area to restore itself to its proper functioning. The 5th chakra is the center of expression and th Please see website for terms and conditions. communication. Some of the problems associated with the 5 chakra are . sore throat, inability to express personal truths, colds, and laryngitis, lack of inspiration. AWAKENED INSIGHT th PRODUCT DESCRIPTIONS 6 Chakra - Third Eye Planetary Influence: Mercury & Neptune Colors: Indigo Blue = Truth, Vision The Seven Light Centers Purple = Spirituality, Inspiration Stones: Sodalite – Opens 3rd Eye, Insight and Intuition Amethyst – Psychic, Overall healing stone, Divine Love Items: CA1-CA7 Amulets, CB1-CB7 Baby Wand Pendants 1 ¾’’, CE1- If there are any blockages in the chakras, applying the correct stones, CE7 Sterling Silver Earrings color and/or light will enable the area to restore itself to its proper functioning. Some of the problems associated with the 6th chakra are EARTH ENERGIES headaches, eye problems, nightmares, and lack of insight. st INSPIRATION 1 Chakra - The Root of the Kundalini th Planetary Influence: Pluto, Mars 7 Chakra - Crown Chakra Colors: Red = Courage, Passion Planetary Influence: Uranus Black = Protection from Negativity Colors: White = Divine light, Clairvoyance, Purity Stones: Black Obsidian – teaches us to deal with negativity Purple = Spirituality, Inspiration Garnet – stimulates passion and courage Stones : Amethyst – Psychic, overall healing stone, Divine love If there are any blockages in the chakras, applying the correct stones, Clear Quartz – dispels negativity color and/or light will enable the area to restore itself to its proper If there are any blockages in the chakras, applying the correct stones, st color and/or light will enable the area to restore itself to its proper functioning.
    [Show full text]
  • WASHINGTON GEOLOGY and Washington State Puget Sound Water Quality Author­ HYDROLOGY Ity, 1989, Puget Sound Water Quality Directory: Wash­ Korosec, M
    WASHINGTON GEOLOGIC NEWSLETTER Volume 18 Number 1 March 1990 Washington State Department of Natural Resources Division of Geology and Earth Resources Portland cement plant in Metaline Falls purchased by Lafarge Corp. in 1989, showing aerial tram that transports limestone from the quarry. IN THIS ISSUE Washington's Mineral Industry in 1989 ... ........... 3 Last Year's Coal Activity in Washington............. 24 Coastal Vertical Land Movement....................... 26 WASHINGTON Washington State Mineral GEOLOGIC Data Files, Division of Geology NEWSLETTER and Earth Resources By Raymond Lasmanis The Washington Geologic Newsletter Is published quarterly by the Division of Geology and Earth Resources, Department of Natural Re­ The key to the development of a successful min­ sources. The newsletter ls free upon request. The Division also publishes eral exploration program is the availability of back­ bulletins, Information circulars, reports of Investigations, geologic maps, ground information. Concepts evolve into a firm and open-file reports. A list of these publications will be sent upon request. proposal for management's consideration through a process of data synthesis. In that regard, the Division's files are invaluable to the explorationist. DEPARTMENT Brian J. Boyle To date, however, the value of this resource has not OF Commissioner of Public Lands been fully utilized by geologists served by the Divi­ NATURAL Art Stearns sion. It may be that the obscure citation (Reference RESOURCES Supervisor #158) in our out-of-print Bulletin 37, "Inventory of Washington Minerals; Part II, Metallic Minerals" has DMSIONOF Raymond Lasmanis discouraged use of the data files. Reference 158 GEOLOGY AND State Geologist reads "Washington Division of Mines and Geology EARTH RESOURCES J .
    [Show full text]
  • Magnetic Susceptibility Index for Gemstones ©2010 Kirk Feral Magnetic Responses Are Standardized to 1/2" X 1/2" N-52 Magnet Cylinders
    Magnetic Susceptibility Index for Gemstones ©2010 Kirk Feral Magnetic responses are standardized to 1/2" X 1/2" N-52 magnet cylinders. Colorless and extremely pale stones of any species tend to be Inert (Inert includes diamagnetic). Black opaque stones of many species are strongly magnetic and may Pick Up or Drag. Pick Up/Drag responses are weight-dependent. Larger Garnets may be too heavy to Pick Up. A few non-Garnet gems with strong magnetism may Pick Up when under 0 .5ct. Gemstone Response Range SI X 10 (-6) Range Cause of Color Amber (any color) Inert 0 (diamagnetic) Organic Andalusite Inert 0 (diamagnetic) Manganese Apatite (any color) Inert (Weak in rare cases) 0 (diamagnetic) Manganese, Rare-earth Astrophyllite Strong 1146-1328 Iron, Manganese Axinite Drags 603 SI Iron, Manganese Barite (pale brown) Inert 0 (diamagnetic) Unknown Beryl Aquamarine (pale to medium blue) Weak to Moderate 20-100 Iron Golden Beryl & Heliodor Weak 22-48 Iron Morganite Inert 0 (diamagnetic) Manganese Maxixe (blue Beryl) Inert 0 (diamagnetic) Color centers Bixbite (red Beryl) Weak 30 SI Manganese Emerald Weak 20-56 Chromium, Vanadium Synthetic Emerald Weak to Moderate 26-143 Chromium, Vanadium Calcite Most Calcite Colors Inert 0 (diamagnetic) Various Metals Pink Calcite Weak 22-26 Cobalt Chalcedony Most Agates & Jaspers Inert 0 (diamagnetic) Iron Red Jasper Weak to Picks Up 69-8836 Iron Mahogany Jasper Strong 217 SI Iron Bloodstone Weak to Strong 26-521 Iron Carnelian Inert 0 (diamagnetic) Iron Chrysoprase Weak to Strong 42-224 Nickel Fire Agate Picks Up
    [Show full text]