Minerals and Mineral Products in Our Bedroom Bed Hematite

Total Page：16

File Type：pdf, Size：1020Kb

Minerals and Mineral Products in Our Bedroom Bed Hematite

Minerals and Mineral Products in our Bedroom Make-Up Kit Muscovite Bed Talc Hematite: hinges, handles, Mica mattress springs Hematite: for color Chromite: chrome plating Bismuth Radio Barite Copper: wiring Plastic Pail Quartz: clock Mica Gold: connections Cassiterite: solder Toilet Bowl / Tub Closet Feldspar: porcelain Chromite: chrome plating Pyrolusite: coloring Hematite: hinges, handles (steel) Chromite: plumbing fixtures Quartz : mirror on door Copper: tubing Desk Toothpaste Hematite: hinges, handles (steel) Apatite: teeth Chromite: chrome plating Fluorite: toothpaste Mirror Rutile: to color false Hematite: handle, frame teeth yellow Chromite: plating Gold: fillings Gold: plating Cinnabar: fillings Quartz: mirror Towels Table Lamp Sphalerite: dyes Brass (an alloy of copper and Chromite: dyes zinc): base Quartz: bulb Water Pipe/Faucet/Shower bulb Wolframite: lamp filament Brass Copper: wiring Iron Nickel Minerals and Mineral Products in our Bedroom Chrome: stainless steel Bathroom Cleaner Department of Environment and Natural Resources Borax: abrasive, cleaner, and antiseptic MINES AND GEOSCIENCES BUREAU Deodorant Spray Can Cassiterite Chromite Copper Carpet Quartz Sphalerite: dyes Telephone Chromite: dyes Drinking Glasses Copper: wiring Sulfur: foam padding Quartz Chromite: plating Gold: red color Clock Silver: electronics Pentlandite: spring Graphite: batteries Refrigerator Quartz: glass, time keeper Hematite Television Chromite: stainless steel Chromite: plating Computer Galena Wolframite: monitor Wolframite: monitor Copper Copper: wiring Copper: wiring Cinnabar: thermometer Quartz: electronics Quartz: electronics Pentlandite Silver Silver Salt & Pepper Shakers Vacuum Cleaner Easy Chair Halite: salt Copper: wiring Sphalerite: dyes Chromite Chromite: dyes Chromite: plating Sulfur: foam rubber Silver: electronics Stove Hematite: steel Hematite Pottery Pentlandite: stainless steel Chromite: stainless steel and resistance in Kaolinite electrical heating Pyrolusite: coloring Minerals and Mineral Products in our Kitchen equipment Galena: glaze Galena Table Lamp Blender Copper Brass (an alloy of copper and Hematite Cinnabar: thermometer zinc): base Chromite Pentlandite Quartz: bulb Galena Toaster Copper Wolframite: lamp filament Hematite Copper: wiring Quartz Chromite: stainless steel and resistance in Can Opener electrical heating equipment A publication of the Hematite Galena MINES AND GEOSCIENCES BUREAU Chromite Copper MGB Compound, North Avenue 1100 Diliman Galena Cinnabar: thermometer Quezon City, Philippines Telephone No. (6 32) 9209120/ Fax No. (6 32) 9201635 Copper Pentlandite Email: [email protected] / Website: http://www.mgb.gov.ph Dishwasher Trash Can Hematite Hematite Chromite Chromite Galena .

Copy Link

Recommended publications

Podiform Chromite Deposits—Database and Grade and Tonnage Models
Podiform Chromite Deposits—Database and Grade and Tonnage Models Scientific Investigations Report 2012–5157 U.S. Department of the Interior U.S. Geological Survey COVER View of the abandoned Chrome Concentrating Company mill, opened in 1917, near the No. 5 chromite mine in Del Puerto Canyon, Stanislaus County, California (USGS photograph by Dan Mosier, 1972). Insets show (upper right) specimen of massive chromite ore from the Pillikin mine, El Dorado County, California, and (lower left) specimen showing disseminated layers of chromite in dunite from the No. 5 mine, Stanislaus County, California (USGS photographs by Dan Mosier, 2012). Podiform Chromite Deposits—Database and Grade and Tonnage Models By Dan L. Mosier, Donald A. Singer, Barry C. Moring, and John P. Galloway Scientific Investigations Report 2012-5157 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 This report and any updates to it are available online at: http://pubs.usgs.gov/sir/2012/5157/ For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Mosier, D.L., Singer, D.A., Moring, B.C., and Galloway, J.P., 2012, Podiform chromite deposits—database and grade and tonnage models: U.S.
[Show full text]
Download PDF About Minerals Sorted by Mineral Name
MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky.
[Show full text]
Overview of Tungsten Indicator Minerals Scheelite and Wolframite with Examples from the Sisson W-Mo Deposit, Canada
Overview of tungsten indicator minerals scheelite and wolframite with examples from the Sisson W-Mo deposit, Canada M. Beth McClenaghan1, M.A. Parkhill2, A.A. Seaman3, A.G. Pronk3, M. McCurdy1 & D.J. Kontak4 1Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada K1A 0E8 (e-mail: [email protected]) 2New Brunswick Department of Energy and Mines, Geological Surveys Branch, P.O. Box 50, Bathurst, New Brunswick, Canada E2A 3Z1 3New Brunswick Department of Energy and Mines, Geological Surveys Branch, P.O. Box 6000, Fredericton, New Brunswick, Canada E3B 5H1 4Department of Earth Sciences, Laurentian University, Sudbury, Ontario, Canada P3E 2C6 These short course notes provide an overview of published lit- Table 1. List of regional surveys and case studies conducted around erature on the use of scheelite and wolframite as indicator min- the world in which scheelite and/or wolframite in surficial sediments erals for W, Mo, and Au exploration. The use of scheelite and have been used as indicator minerals. wolframite in stream sediments is well documented for mineral Mineral Media Location Source of Information exploration but less so for using glacial sediments (Table 1). scheelite stream sediments Pakistan Asrarullah (1982) wolframite stream sediments Burma ESCAP Scretariat (1982) The Geological Survey of Canada has recently conducted a scheelite, wolframite stream sediments USA Theobald & Thompson (1960) glacial till and stream sediment indicator mineral case study scheelite stream sediments, soil Thailand Silakul (1986) around the Sisson W-Mo deposit in eastern Canada. scheelite stream sediments Greenland Hallenstein et al. (1981) Preliminary indicator mineral results from this ongoing study scheelite stream sediments Spain Fernández-Turiel et al.
[Show full text]
Accretion of Water in Carbonaceous Chondrites: Current Evidence and Implications for the Delivery of Water to Early Earth
ACCRETION OF WATER IN CARBONACEOUS CHONDRITES: CURRENT EVIDENCE AND IMPLICATIONS FOR THE DELIVERY OF WATER TO EARLY EARTH Josep M. Trigo-Rodríguez1,2, Albert Rimola3, Safoura Tanbakouei1,3, Victoria Cabedo Soto1,3, and Martin Lee4 1 Institute of Space Sciences (CSIC), Campus UAB, Facultat de Ciències, Torre C5-parell-2ª, 08193 Bellaterra, Barcelona, Catalonia, Spain. E-mail: [email protected] 2 Institut d’Estudis Espacials de Catalunya (IEEC), Edif.. Nexus, c/Gran Capità, 2-4, 08034 Barcelona, Catalonia, Spain 3 Departament de Química, Universitat Autònoma de Barcelona, 08193 Bellaterra, Catalonia, Spain. E-mail: [email protected] 4 School of Geographical and Earth Sciences, University of Glasgow, Gregory Building, Lilybank Gardens, Glasgow G12 8QQ, UK. Manuscript Pages: 37 Tables: 2 Figures: 10 Keywords: comet; asteroid; meteoroid; meteorite; minor bodies; primitive; tensile strength Accepted in Space Science Reviews (SPAC-D-18-00036R3, Vol. Ices in the Solar System) DOI: 10.1007/s11214-019-0583-0 Abstract: Protoplanetary disks are dust-rich structures around young stars. The crystalline and amorphous materials contained within these disks are variably thermally processed and accreted to make bodies of a wide range of sizes and compositions, depending on the heliocentric distance of formation. The chondritic meteorites are fragments of relatively small and undifferentiated bodies, and the minerals that they contain carry chemical signatures providing information about the early environment available for planetesimal formation. A current hot topic of debate is the delivery of volatiles to terrestrial planets, understanding that they were built from planetesimals formed under far more reducing conditions than the primordial carbonaceous chondritic bodies.
[Show full text]
The H/F Ratio As an Indicator of Contrasted Wolframite Deposition Mechanisms
Ore Geology Reviews 104 (2019) 266–272 Contents lists available at ScienceDirect Ore Geology Reviews journal homepage: www.elsevier.com/locate/oregeorev Short communication The H/F ratio as an indicator of contrasted wolframite deposition T mechanisms ⁎ Julie Anne-Sophie Michaud , Michel Pichavant Université d'Orléans/CNRS/ISTO/BRGM, UMR 7327, 1A rue de la Férollerie, 45100 Orléans, France ARTICLE INFO ABSTRACT Keywords: Understanding wolframite deposition mechanisms is a key to develop reliable exploration guides for W. In quartz Wolframite veins from the Variscan belt of Europe and elsewhere, wolframites have a wide range of compositions, from Hübnerite hübnerite- (MnWO4) to ferberite-rich (FeWO4). Deposition style, source of Mn and Fe, distance from the heat/ W deposition fluid source and temperature have been proposed to govern the wolframite H/F (hübnerite/ferberite ratio) Magmatic control defined as 100 at. Mn/(Fe + Mn). The Argemela mineralized district, located near the world-class Panasqueira W ore deposit W mine in Portugal, exposes a quartz-wolframite vein system in close spatial and genetic association with a rare- Veins metal granite. Wolframite is absent as a magmatic phase, but W-rich whole-rock chemical data suggest that the granite magma is the source of W. Wolframite occurs as large homogeneous hübnerites (H/F = 64–75%) co- existing with montebrasite, K-feldspar and cassiterite in the latest generation of intragranitic veins corre- sponding to magmatic fluids exsolved from the granite. Locally, early hübnerites evolve to late more Fe-rich compositions (H/F = 45–55%). In a country rock vein, an early generation of Fe-rich hübnerites (H/ F = 50–63%) is followed by late ferberites (H/F = 6–23%).
[Show full text]
Petrology of Ore Deposits
Petrology of Ore Deposits An Introduction to Economic Geology Introductory Definitions Ore: a metalliferous mineral, or aggregate mixed with gangue that can me mined for a profit Gangue: associated minerals in ore deposit that have little or no value. Protore: initial non-economic concentration of metalliferous minerals that may be economic if altered by weathering (Supergene enrichment) or hydrothermal alteration Economic Considerations Grade: the concentration of a metal in an ore body is usually expressed as a weight % or ppm. The process of determining the grade is termed “assaying” Cut-off grade: after all economic and political considerations are weighed this is the lowest permissible grade that will mined. This may change over time. Example Economic Trends Economy of Scale As ore deposits are mined the high-grade zones are developed first leaving low-grade ores for the future with hopefully better technology Since mining proceeds to progressively lower grades the scale of mining increases because the amount of tonnage processed increases to remove the same amount of metal Outputs of 40,000 metric tons per day are not uncommon Near-surface open pit mines are inherently cheaper than underground mines Other factors important to mining costs include transportation, labor, power, equipment and taxation costs Classification of Ore bodies Proved ore: ore body is so thoroughly studied and understood that we can be certain of its geometry, average grade, tonnage yield, etc. Probable ore: ore body is somewhat delineated by surface mapping and some drilling. The geologists is reasonably sure of geometry and average grade. Possible Ore: outside exploration zones the geologist may speculate that the body extends some distance outside the probable zone but this is not supported by direct mapping or drilling.
[Show full text]
MACKINAWITE from SOUTH AFRICA W. C J. Van RDNSBU*.O, Geological Surtey Oj Soulh Africa, Preloria, Soulh A.[Ri Co, L. Lrbnunsbyc
TI.IE AMERICAN MINERALOGIST, VOL 52, JULY AUGUST, 1967 MACKINAWITE FROM SOUTH AFRICA W. C J. vAN RDNSBU*.o,Geological Surtey oJ Soulh Africa, Preloria,Soulh A.[rico, AND L. LrBnuNsByc, Deparlment of Geology,Llnit:ersity of Pretoria, Pre!oria,Soul h Africa. ABSTRAcT Mackinawite has been identified in mafic and ultramafic rocks of the Bushveld igneous complex and Insizwa and also in the carbonatite and pegmatoid of Loolekop, Phalaborrva complex in South Africa. The mineral occurs predominantly as somewhat irregular to oriented intergrowths in pentlandite in all these occurrences and less commonly as regular oriented lamellae in chalcopyrite and rarely in cubanite. The textural evidence suggests that mackinawite may represent an exsolution product of pentlandite, chalcopyrite and cubanite. INrnonucrroN The iron sulphide, mackinawite was recently named in a paper by Evans, et al, (1964). Natural occurrencesof this mineral f rom Finland were describedby- Kouvo et al (1963)and from the Muskox intrusion in Canada by Chamberlain and Delabio (1965). During the presentinvestigation mackinawite was distinguishedfrom valleriite in the carbonatite and pegmatoid of Loolekop, Phalaborwa complex, in the Bushveld igneous complex, and from Insizwa, Cape Province.The mode of occurrenceof the mackinawite in the carbonatite difiers somewhatfrom that in the mafic rocks of Insizwa and the Bush- veld complex. MrNnn.q.rocv The physicaland optical propertiesof mackinawitefrom the Bushveid complex,Insizwa and Loolekop are very similar and are in closeagree- ment with the propertiesgiven for the same mineral from the Muskox intrusion by Chamberlain and Delabio (1965). The mineral takes a fairly good polish,particularly after buffing with a chromic oxide slurry.
[Show full text]
Download the Scanned
Tne AMBRrcAx M rNBRALocrsr JOURNAL OF THE MINERALOGICAL SOCIETY OF AMERICA Vol.20 NOVEMBER, 1935 No. 11 THE PEGMATITE MINERALS FROM NEAR AMELIA, VIRGINIA* Jnwrr.r. J. Gless, U. S. Geological'Suraey, Washington, D. C. CoNrnxrs 1' rntroduction 741 2. Rutherfordmine 743 3' Morefield mine ' ' 744 4. Minerals 745 Albite, bertrandite, beryl, biotite, calcite, cassiterite, cerussite, chalcopy- rite, fluorite, galena, manganotantalite, microcline, microlite, monazite, muscovite, phenacite, pyrite, pyrolusite, qtsartz, spessartite, topaz, tourmaline, triplite, zinnwaldite, zircon. 5. Rarer elements identified by spectrographic analyses 764 6. Luminescence of minerals 766 7. Selected bibliography 768 1. INTnooucrroN The first commercial mica mines near Amelia Court House, Virginia, were opened in the early seventies, and the remarkable size and quality of the mica early awakened a keen economic in- terest in the pegmatite dikes of the region, but the richnessof the locality in rare and beautiful mineral specimenshas promoted a scientific interest which has persisted for sixty years. Thirty-six mineral species have been reported from the Rutherford mine alone,and the variety and perfection of many of thesehave led to their inclusion in most of the museums of the world. The concen- tration of unusual minerals in an easily accessible deposit at- tracted various scientific investigators and mineral collectors to this locality for successivegenerations. Such intensive investiga- tion of a locality might suggest that little remains to be learned about its minerals, but the recent opening of a new mine near Amelia and the reopening of the Rutherford mine have given new * Published by permission of the Director, U. S. Geological Survey. 742 THE AMERICAN MINERALOGIST opportunities for study.
[Show full text]
Mineral Processing
Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
[Show full text]
Structure and Mineralization of Precambrian Rocks in the Galena-Roub Aix District, Black Hills, South Dakota
Structure and Mineralization of Precambrian Rocks in the \ Galena-Roubaix District, Black Hills, South Dakota ( By R. W. BAYLEY » CONTRIBUTIONS TO ECONOMIC GEOLOGY V ' GEOLOGICAL SURVEY BULLETIN 1312-E UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 55 cents (paper cover) CONTENTS Page Abstract_ ____-_-_----_-----__--_-----_--_--.. El Introduction _________________________________ 1 Field methods_______-_____-_____-_____-__--_ 2 General geology.___-__--__-_--__-_--___._-_--_. 3 Stratigraphy. ___________________---__--__-__-.. 4 Metabasalt and chert.______-__-__-_____-_. 4 Graphitic schist and cherty ferruginous schist. 5 Metagraywacke, schist, and slate_ ___________ 6 Structure. ___________.-______-_-__-_-_-_-___-. 6 Distribution of gold. 7 Diamond drilling. __ 9 Magnetic survey. __ 10 Summary________ 14 References. -. ______ 15 ILLUSTEATIONS Page PLATE 1. Geologic map of the Galena-Roubaix district, Lawrence County, Black Hills, South Dakota.________________ In pocket FIGURE 1. Generalized geologic map of the northern Black Hills____-___ E2 2. Magnetic survey in the vicinity of U.S. Geological Survey diamond-drill hole 1__________________________________ 13 TABLE Page TABLIS 1. Results of core-sample analyses, U.S. Geological Survey diamond-drill hole 1, Galena-Roubaix district.____________ Ell ra CONTRIBUTIONS TO ECONOMIC GEOLOGY STRUCTURE AND MINERALIZATION OF PRECAMBRIAN ROCKS IN THE GALENA-ROUB AIX DISTRICT, BLACK HILLS, SOUTH DAKOTA ByK.W.BAYLEY ABSTRACT The Galena-Roubaix district is underlain chiefly by tightly folded and mod erately metamorphosed sedimentary and volcanic rocks of Precambrian age.
[Show full text]
40 Common Minerals and Their Uses
40 Common Minerals and Their Uses Aluminum Beryllium The most abundant metal element in Earth’s Used in the nuclear industry and to crust. Aluminum originates as an oxide called make light, very strong alloys used in the alumina. Bauxite ore is the main source aircraft industry. Beryllium salts are used of aluminum and must be imported from in fluorescent lamps, in X-ray tubes and as Jamaica, Guinea, Brazil, Guyana, etc. Used a deoxidizer in bronze metallurgy. Beryl is in transportation (automobiles), packaging, the gem stones emerald and aquamarine. It building/construction, electrical, machinery is used in computers, telecommunication and other uses. The U.S. was 100 percent products, aerospace and defense import reliant for its aluminum in 2012. applications, appliances and automotive and consumer electronics. Also used in medical Antimony equipment. The U.S. was 10 percent import A native element; antimony metal is reliant in 2012. extracted from stibnite ore and other minerals. Used as a hardening alloy for Chromite lead, especially storage batteries and cable The U.S. consumes about 6 percent of world sheaths; also used in bearing metal, type chromite ore production in various forms metal, solder, collapsible tubes and foil, sheet of imported materials, such as chromite ore, and pipes and semiconductor technology. chromite chemicals, chromium ferroalloys, Antimony is used as a flame retardant, in chromium metal and stainless steel. Used fireworks, and in antimony salts are used in as an alloy and in stainless and heat resisting the rubber, chemical and textile industries, steel products. Used in chemical and as well as medicine and glassmaking.
[Show full text]
Chrome/Refractory Uses, While the Rest with Ratio Below 1.8 Are Used for Production of Chemical [1]
Magnetic and Electrical Separation, Vol.8, pp. 175-183 (C) 1997 OPA (Overseas Publishers, Association) Reprints available directly from the publisher Amsterdam B.V. Published in The Netherlands under Photocopying permitted by license only. license by Gordon and Breach Science Publishers Printed in India IMPROVING GRADE OF INDIAN CHROMITE ORES BY HIGH-GRADIENT MAGNETIC SEPARATION R. BHIMA RAO, B. DAS AND S.R.S. SASTRI Regional Research Laboratory, Council for Scientific and Industrial Research, Bhubaneswar 751 013, India (Received July 3, 1996, in final form August 12, 1996) Abstract Investigations were carried out to improve the chromium-to-iron ratio of two off-grade chromite samples from Orissa, India, having different physical natures. The results of these investigations indicated that the chromium-to-iron ratio could be improved from 1.85 to 3.0 with around 10% to 30% recoveries by high-intensity magnetic separation of the washed ores. A common flowsheet is suggested for processing of these two ores. INTRODUCTION The major portion of the Indian chromite ore reserves are located in Sukinda-Naushai belt of Orissa, and belong to the lateritic iron group ores group. Approximately 40% of these reserves are suitable for metallurgical use, 33% for refractory making and 27% for chemical industries [1]. The purpose for which a given ore can be used depends on the chromium-to-iron ratio besides the CrO content. Ores having chromium-to-iron ratio above 2.8 are considered suitable for metallurgical purposes and those with the ratio between 2.8 and 1.8 for charge chrome/refractory uses, while the rest with ratio below 1.8 are used for production of chemical [1].
[Show full text]