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BRSUG Number Mineral Name Hey Index Group Hey No
BRSUG Number Mineral name Hey Index Group Hey No. Chem. Country Locality Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-37 Copper Au) 1.1 4[Cu] U.K., 17 Basset Mines, nr. Redruth, Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-151 Copper Au) 1.1 4[Cu] U.K., 17 Phoenix mine, Cheese Wring, Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-280 Copper Au) 1.1 4[Cu] U.K., 17 County Bridge Quarry, Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and South Caradon Mine, 4 miles N of Liskeard, B-319 Copper Au) 1.1 4[Cu] U.K., 17 Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-394 Copper Au) 1.1 4[Cu] U.K., 17 ? Cornwall? Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-395 Copper Au) 1.1 4[Cu] U.K., 17 Cornwall Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-539 Copper Au) 1.1 4[Cu] North America, U.S.A Houghton, Michigan Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-540 Copper Au) 1.1 4[Cu] North America, U.S.A Keweenaw Peninsula, Michigan, Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, Ag and B-541 Copper Au) 1.1 4[Cu] North America, U.S.A Keweenaw Peninsula, Michigan, Elements and Alloys (including the arsenides, antimonides and bismuthides of Cu, -
Geochemistry, Mineralogy and Microbiology of Cobalt in Mining-Affected Environments
minerals Article Geochemistry, Mineralogy and Microbiology of Cobalt in Mining-Affected Environments Gabriel Ziwa 1,2,*, Rich Crane 1,2 and Karen A. Hudson-Edwards 1,2 1 Environment and Sustainability Institute, University of Exeter, Penryn TR10 9FE, UK; [email protected] (R.C.); [email protected] (K.A.H.-E.) 2 Camborne School of Mines, University of Exeter, Penryn TR10 9FE, UK * Correspondence: [email protected] Abstract: Cobalt is recognised by the European Commission as a “Critical Raw Material” due to its irreplaceable functionality in many types of modern technology, combined with its current high-risk status associated with its supply. Despite such importance, there remain major knowledge gaps with regard to the geochemistry, mineralogy, and microbiology of cobalt-bearing environments, particu- larly those associated with ore deposits and subsequent mining operations. In such environments, high concentrations of Co (up to 34,400 mg/L in mine water, 14,165 mg/kg in tailings, 21,134 mg/kg in soils, and 18,434 mg/kg in stream sediments) have been documented. Co is contained in ore and mine waste in a wide variety of primary (e.g., cobaltite, carrolite, and erythrite) and secondary (e.g., erythrite, heterogenite) minerals. When exposed to low pH conditions, a number of such minerals are 2+ known to undergo dissolution, typically forming Co (aq). At circumneutral pH, such aqueous Co can then become immobilised by co-precipitation and/or sorption onto Fe and Mn(oxyhydr)oxides. This paper brings together contemporary knowledge on such Co cycling across different mining environments. -
Summary Report
5-6 EDWARD VII. SESSIONAL PAPER No. 26 A. 1906 SUMMARY REPORT OF THE GEOLOGICAL SURVEY DEPARTMENT OF CANADA F OR THE CALENDA R YEAR 1905 P R INTED BY OR DER OF P ARLIAME NT OTTAWA PRINTED BYS. E. DAWSON, PRIN'fER TO THE KING'S MOST EXCELLENT MAJESTY 1906 (No. 26-1906.J . .... ...... • -, . .. : : : ... ·: .. : ... ~ .. ...... : ... : : ., ; : : : .·. : ·. : ..- ·.. :····"·... : : ) · ~ .··· ·,·/ "• ..... ·.· : .. · : : :·· ·... .. ."' II.. ·. · :; ,.· •••· : ... • • ••··. , ".•:'"·.·:· "'.: . .. • : ·. : ••:: · ,:. • • • : : : . ·=· .... ...... ·. : :· .. ..... .. "., .: .~: . .. .. ... ~ " .... ... : : .. : : .. : ; : .. ' ~ ..... ...... ·.. ···.. : ...·" ·:·: .. ·... • .. .- .. ... .. : ·.· ..: ....·. ··. .. :; ·.·.:·.... ..... : ·. ...· .. ::·.: ... ......... ·:·• . • 5-6 EDWARD VII. SESSIONAL PAPER No. 26 A. 1906 To His Excellency the Right Honourable Sir Albert Henry George, Earl Grey, ,Viscount Howick, Baron Grey of Howick, a Baronet, G. C. M. G., &:c., &:c., &:c., Governor General oj Canada. MAY IT PLEASE YOUR EXCELLENCY,- The undersigned has the honour to lay before Your Excellency, in compliance with 3 Vic., Chap. 2, Section 6, the Summary Report of the Operations of the Geological Survey Department for the calendar year ending December 31, 1905. Respectfully submitted. FRANK OLIVER, Ministe1· of the Interior . .. 5-6 EDWARD VII. SESSIONAL PAPER No. 26 A. 1906 rrABLE 0 F CONTENTS SUMMARY R EPOR'l' OJI 1'ffll ACTING D mECTOR :- Advantage of Geological Surveys .. ..... 1 Geological Society of America . .............. .... 2 International -
54 SKUTTERUDITE FROX{ COBALT. ONTARIOI on Some Specimens
54 THE AMENICAN M]NENALOGIST SKUTTERUDITE FROX{ COBALT. ONTARIOI T. I/. WALKER Uruiuersily oJ Torontn On somespecimens recently obtained from the Temiskaming mine, Cobalt, Ontario, small brilliant crystals resembling smal- tite were observed,imbedded in fragments of soft chloritic or micaceouscountry rock includedin the vein. As is well known, smaltite and chloanthite closelyresemble one another and are commonlyintergrown in the samecrystal. It was with a view to determiningthe relative purity of the supposedsmaltite that this examinationwas undertaken. The principal ore in the vein is smaltite,usually massive, but occasionallyforming rough crystalsup to b or 6 millimeters in diameter. The rest of the vein matter is either calcite or lrag- ments of country rock. The small crystals under investigation seemto representthe latest mineral to form;they are tirr white, and verSzlustrous. The specific gravity, determined on 0.62 gram of carefully selectedcrystals, is 6.29,which is closerto the value usually given for skutterudite (CoAss) than to that for smaltite (CoAsz). The crystals, which seldom exceed a millimeter in diameter, were measured on a Goldschmidt goniometer. The fol- lowing forms were obseryed on each crystal: a(IOO), o(111), d(110), and n(211). The relative development of the forms is shown in figure 1. Nothing observed suggests that the crystals are Frc.1. hemihedral-the faces of the last two formswere not alwayspresent in full, but the omissionsappeared to be quite irregular. These four forms have all been observed on both smaltite and skutterudite. An analysis made on the powdered mineral is shown in I. l Presented at the firrt annual meeting of the Mineralogical Society of America, December 28, 1920. -
Metals from Ores: an Introduction
CRIMSONpublishers http://www.crimsonpublishers.com Mini Review Aspects Min Miner Sci ISSN 2578-0255 Metals from Ores: An Introduction Fathi Habashi* Department of Mining, Laval University, Canada *Corresponding author: Fathi Habashi, Department of Mining, Metallurgical and Materials Engineering, Laval University, Quebec City, Canada Submission: October 09, 2017; Published: December 11, 2017 Introduction of metallic lustre. Of these about 300 are used industrially in the chemical industry, in building materials, in fertilizers, as fuels, etc., chemical composition, constant physical properties, and a A mineral is a naturally occurring substance having a definite characteristic crystalline form. Ores are a mixture of minerals: they are processed to yield an industrial mineral or treated chemically and are known as the industrial minerals Figure 3. to yield a single or several metals. Ores that are generally processed for only a single metal are those of iron, aluminium, chromium, tin, mercury, manganese, tungsten, and some ores of copper. Gold ores may yield only gold, but silver is a common associate. Nickel ores are always associated with cobalt, while lead and zinc always occur together in ores. All other ores are complex yielding a number of metals. before being treated by chemical methods to recover the metals. Ores undergo a beneficiation process by physical methods and grinding then separation of the individual mineral by physical Figure 2: Metals and metalloids obtained from ores. Beneficiation processes involve liberation of minerals by crushing methods (gravity, magnetic, etc.) or physicochemical methods pyrometallurgical, and electrochemical methods. Metals and (flotation) Figure 1. Chemical methods involve hydrometallurgical, metalloids obtained from ores are shown in Figure 2. -
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, -
Cassels and Riddell Town Ontario Ships and Is Located 5Km East of Temagami in the District of Nipissing
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). -
Bulletin 65, the Minerals of Franklin and Sterling Hill, New Jersey, 1962
THEMINERALSOF FRANKLINAND STERLINGHILL NEWJERSEY BULLETIN 65 NEW JERSEYGEOLOGICALSURVEY DEPARTMENTOF CONSERVATIONAND ECONOMICDEVELOPMENT NEW JERSEY GEOLOGICAL SURVEY BULLETIN 65 THE MINERALS OF FRANKLIN AND STERLING HILL, NEW JERSEY bY ALBERT S. WILKERSON Professor of Geology Rutgers, The State University of New Jersey STATE OF NEw JERSEY Department of Conservation and Economic Development H. MAT ADAMS, Commissioner Division of Resource Development KE_rr_ H. CR_V_LINCDirector, Bureau of Geology and Topography KEMBLEWIDX_, State Geologist TRENTON, NEW JERSEY --1962-- NEW JERSEY GEOLOGICAL SURVEY NEW JERSEY GEOLOGICAL SURVEY CONTENTS PAGE Introduction ......................................... 5 History of Area ................................... 7 General Geology ................................... 9 Origin of the Ore Deposits .......................... 10 The Rowe Collection ................................ 11 List of 42 Mineral Species and Varieties First Found at Franklin or Sterling Hill .......................... 13 Other Mineral Species and Varieties at Franklin or Sterling Hill ............................................ 14 Tabular Summary of Mineral Discoveries ................. 17 The Luminescent Minerals ............................ 22 Corrections to Franklln-Sterling Hill Mineral List of Dis- credited Species, Incorrect Names, Usages, Spelling and Identification .................................... 23 Description of Minerals: Bementite ......................................... 25 Cahnite .......................................... -
Primary Native-Silver Ores Near Wickenburg, Arizona, and Their Bearing on the Genesis of the Silver Ores of Cobalt, Ontario
PRIMARY NATIVE-SILVER ORES NEAR WICKENBURG, ARIZONA, AND THEIR BEARING ON THE GENESIS OF THE SILVER ORES OF COBALT, ONTARIO. By E. S. BASTIN. INTRODUCTION. The silver ores of the Monte Cristo mine, near Wickenburg, Ariz., are of peculiar interest to economic geologists because their prin cipal silver mineral native silver is primary, whereas most occur rences of native silver are unquestionably secondary the products of downward enrichment. Of interest also is the association of the native silver with nickel arsenides, in which respect the Wickenburg ores resemble the famous silver ores of Cobalt, Ontario, though they differ markedly from the Cobalt ores in another respect, for at Cobalt the native silver has commonly replaced calcite or arsenides or antimonides of nickel or cobalt, whereas at the Monte Cristo mine the native silver crystallized nearly or quite contemporaneously with the nickel arsenides, and there is no evidence that it has re placed any other minerals. The field work on which this report is based was done in 1913 in the course of a study of silver enrichment undertaken by the United States Geological Survey in many mining camps of the western United States. The work of preparing the results for publication has been delayed by the war and other causes. The Monte Cristo mine is about 12£ miles by wagon road north east of Wickenburg, half a mile southwest of Constellation post office, and 65- miles northwest of Phoenix. No topographic maps of the district are available. In 1913 the mine was owned by Mr. Ezra Thayer, of Phoenix, to whom the writer is indebted for many specimens of high-grade ore and for numerous data concerning the mine. -
Alt I5LNER&S
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Nickel Deposits of North America
Nickel Deposits of North America By H. R. CORNWALL GEOLOGICAL SURVEY BULLETIN 1223 Geology, resources, and reserves of nickel sulfide and nickeliferous laterite deposits in 7 Provinces of Canada and 15 States of the United States UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director l!'irst printing 1966 Second printing 1967 For sale by the Superintendent of Documents, U.S. Government Printint Office Washintton, D.C. 20402- Price 25 cents (paper cover) CONTENTS Page Abstract---------------------------------------------------------- 1 Introduction __________________________ --.- _____________________ ---- 1 Types of deposits __________________________________________ ---- 2 Sulfide deposits------------------------------------------- 3 Nickeliferous laterite deposits _______ ------------------------ 4 Nickel minerals _____________________________ -----___ ---------- 4 Native nickel-iron _____________________________________ ---- 6 Sulfides-------------------------------------------------- 7 PenUandue___________________________________________ 7 Bravoite and violarite ______________________________ ---- 7 Vaesite----------------------------------------------- 8 8 Heazlewoodite_~illerite---------------------------------------------- __ __ _ _ __ __ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ __ __ _ _ _____ 8 Linnaeite, polydymite, siegenite, and violarite_____________ 8 Other minerals ___ ------___________________________________ -
Practical Geology and Mineralogy for Prospectors
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”).