The Life Cycle of a Mineral Deposit: a Teacher's Guide for Hands-On
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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. -
The Sedimentology and Mineralogy of the River Uranium Deposit Near Phuthaditjhaba, Qwa-Qwa
PER-74 THE SEDIMENTOLOGY AND MINERALOGY OF THE RIVER URANIUM DEPOSIT NEAR PHUTHADITJHABA, QWA-QWA by J. P. le Roux NUCLEAR DEVELOPMENT CORPORATION OF SOUTH AFRICA (PTY) LTD NUCOR PRIVATE MO X2M PRETORIA 0001 m•v OCTOBER 1982 PER-74- THE SEDIMENTOLOGY AND MINERALOGY OF THE RIVER URANIUM DEPOSIT NEAR PHUTHADITJHABA, QWA-QWA b/ H.J. Brynard * J.P. le Roux * * Geology Department POSTAL ADDRESS: Private Bag X256 PRETORIA 0001 PELINDABA August 1982 ISBN 0-86960-747-2 CONTENTS SAMEVATTING ABSTRACT 1. INTRODUCTION 1 2. SEDIMENTOLOGY 1 2.1 Introduction 1 2.2 Depositional Environment 2 2.2.1 Palaeocurrents 2 2.2.2 Sedimentary structures and vertical profiles 5 2.2.3 Borehole analysis 15 2.3 Uranium Mineralisation 24 2.4 Conclusions and Recommendations 31 3. MINERALOGY 33 3.1 Introduction 33 3.2 Procedure 33 3.3 Terminology Relating to Carbon Content 34 3.4 Petrographic Description of the Sediments 34 3.5 Uranium Distribution 39 3.6 Minor and Trace Elements 42 3.7 Petrogenesis 43 3.8 Extraction Metallurgy 43 4. REFERENCES 44 PER-74-ii SAMEVATTING 'n Sedimentologiese en mineralogiese ondersoek is van die River-af setting uittigevoer wat deur Mynboukorporasie (Edms) Bpk in Qwa-Qwa, 15 km suaidwes van Phu triad it jnaba, ontdek is. Die ertsliggaam is in íluviale sand-steen van die boonste Elliot- formasie geleë. Palleostroomrigtings dui op 'n riviersisteem met 'n lae tot baie lae 3d.nuositeit en met "h vektor-gemiddelde aanvoer- rigting van 062°. 'n Studie van sedimentere strukture en korrelgroottes in kranssnitte is deuir to ontleding van boorgatlogs aangevul wat die sedimentêre afsettingsoragewing as h gevlegte stroom van die Donjek-tipe onthul. -
(WHO) Report on Microplastics in Drinking Water
Microplastics in drinking-water Microplastics in drinking-water ISBN 978-92-4-151619-8 © World Health Organization 2019 Some rights reserved. This work is available under the Creative Commons Attribution-NonCommercial-ShareAlike 3.0 IGO licence (CC BY-NC-SA 3.0 IGO; https://creativecommons.org/licenses/by-nc-sa/3.0/igo). Under the terms of this licence, you may copy, redistribute and adapt the work for non-commercial purposes, provided the work is appropriately cited, as indicated below. In any use of this work, there should be no suggestion that WHO endorses any specific organization, products or services. The use of the WHO logo is not permitted. If you adapt the work, then you must license your work under the same or equivalent Creative Commons licence. If you create a translation of this work, you should add the following disclaimer along with the suggested citation: “This translation was not created by the World Health Organization (WHO). WHO is not responsible for the content or accuracy of this translation. The original English edition shall be the binding and authentic edition”. Any mediation relating to disputes arising under the licence shall be conducted in accordance with the mediation rules of the World Intellectual Property Organization. Suggested citation. Microplastics in drinking-water. Geneva: World Health Organization; 2019. Licence: CC BY-NC-SA 3.0 IGO. Cataloguing-in-Publication (CIP) data. CIP data are available at http://apps.who.int/iris. Sales, rights and licensing. To purchase WHO publications, see http://apps.who.int/bookorders. To submit requests for commercial use and queries on rights and licensing, see http://www.who.int/about/licensing. -
Archaean Cratonization and Deformation in the Northern Superior Province, Canada: an Evaluation of Plate Tectonic Versus Vertical Tectonic Models Jean H
Precambrian Research 127 (2003) 61–87 Archaean cratonization and deformation in the northern Superior Province, Canada: an evaluation of plate tectonic versus vertical tectonic models Jean H. Bédard a,∗, Pierre Brouillette a, Louis Madore b, Alain Berclaz c a Geological Survey of Canada, Division Québec, 880, ch.Ste-Foy, Quebec City, Que., Canada G1S 2L2 b Géologie Québec, Ministère des ressources naturelles du Québec, 5700, 4e Avenue Ouest, Charlesbourg, Que., Canada G1H 6R1 c Géologie Québec, Ministère des ressources naturelles du Québec, 545 Crémazie Est, bureau 1110, Montreal, Que., Canada H2M 2V1 Accepted 10 April 2003 Abstract The Archaean Minto Block, northeastern Superior Province, is dominated by tonalite–trondhjemite, enderbite (pyroxene tonalite), granodiorite and granite, with subordinate mafic rocks and supracrustal belts. The plutons have been interpreted as the batholithic roots of Andean-type plate margins and intra-oceanic arcs. Existing horizontal-tectonic models propose that penetrative recrystallization and transposition of older fabrics during terrane assembly at ∼2.77 and ∼2.69 Ga produced a N-NW tectonic grain. In the Douglas Harbour domain (northeastern Minto Block), tonalite and trondhjemite dominate the Faribault–Thury complex (2.87–2.73 Ga), and enderbite constitutes 50–100 km-scale ovoid massifs (Troie and Qimussinguat complexes, 2.74–2.73 Ga). Magmatic muscovite and epidote in tonalite–trondhjemite have corroded edges against quartz + plagioclase, suggesting resorption during ascent of crystal-charged magma. Foliation maps and air photo interpretation show the common development of 2–10 km-scale ovoid structures throughout the Douglas Harbour domain. Outcrop and thin-section scale structures imply that many plutons experienced a phase of syn-magmatic deformation, typically followed by high temperature sub-magmatic overprints. -
Minerals in Your Home Activity Book Minerals in Your Home Activity Book
Minerals In Your Home Activity Book Minerals in Your Home Activity Book Written by Ann-Thérèse Brace, Sheila Stenzel, and Andreea Suceveanu Illustrated by Heather Brown Minerals in Your Home is produced by MineralsEd. © 2017 MineralsEd (Mineral Resources Education Program of BC) 900-808 West Hastings St., Vancouver, BC V6C 2X4 Canada Tel. (604) 682-5477 | Fax (604) 681-5305 | Website: www.MineralsEd.ca Introduction As you look around your home, it is important to think of the many things that you have and what are they made from. It’s simple - everything is made from Earth’s natural resources: rocks, soil, plants, animals, and water. They can be used in their natural state, or processed, refined and manufactured by people into other useable things. The resources that grow and can be replaced when they die or are harvested, like plants and animals, are called renewable resources. Those that cannot be regrown and replaced, like rocks, soil and water, are called non-renewable resources. All natural resources are valuable and we must use them conservatively. Mineral resources are natural Earth materials that must be mined from the ground. We use them every day, and they are non- renewable. Some are changed very little before they are used, like the rock granite for example, that is commonly used to make kitchen countertops or tombstones. Other mineral resources, like those that contain useful metals, must be processed to extract the metal ingredient. The metal is then manufactured into different parts of a product, like a toaster or a smartphone. Whether you are practicing violin in your room, eating a meal in the kitchen, watching TV in the living room or brushing your teeth in the bathroom, your daily activities use things that come from mineral resources. -
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. -
Sand-Gravel Marine Deposits and Grain-Size Properties
GRAVEL ISSN 1678-5975 Novembro - 2005 Nº 3 59-70 Porto Alegre Sand-Gravel Marine Deposits and Grain-Size Properties L. R. Martins1,2 & E. G. Barboza2 1 COMAR- South West Atlantic Coastal and Marine Geology Group; 2 Centro de Estudos de Geologia Costeira e Oceânica – CECO/IG/UFRGS. RESUMO A plataforma continental Atlântica do Rio Grande do Sul e Uruguai foi utilizada como laboratório natural para testar as relações entre propriedades de tamanho de grão e ambiente sedimentar. A evolução Pleistoceno/Holoceno da região foi intensamente estudada através de um mapeamento detalhado, e de estudos sedimentológicos e estratigráficos, oferecendo, dessa forma, uma excelente oportunidade para esse tipo de trabalho. Acumulações de areia e cascalho, vinculadas a níveis de estabilização identificados da transgressão Holocênica, localizados nas isóbatas de 110-120 e 20-30 metros, fornecem elementos confiáveis relacionados com a fonte, transporte e nível de energia de deposição e podem ser utilizados como linhas de evidencias na interpretação ambiental. ABSTRACT The Atlantic Rio Grande do Sul (Brazil) and Uruguay inner continental shelf was used as a natural laboratory to test the relationship between grain-size properties and sedimentary environment. The Pleistocene/Holocene evolution of the region was intensively studied through detailed mapping, sedimentological and stratigraphic research thus offering an excellent opportunity of developing this type of work. Sand and gravel deposits linked with identified stillstands of the Holocene transgression located at 110-120 and 20-30 meters isobath provided elements related to the source, transport and depositional energy level and can be used as a tool for environmental interpretation. Keywords: marine deposits, grain-size, sand-gravel, Holocene. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
The Study of Fossils: the “Glossary of Geology” Defines a Fossil As “Any
The Study of Fossils: The “Glossary of Geology” defines a fossil fossils were originally studied by Thomas Jefferson and Benjamin as “any remains, trace, or imprint of a plant or animal that has been Franklin. preserved in the Earth’s crust since some past geologic or prehis- Collecting in Kentucky: The laws governing fossil collecting in toric time.” The study of fossils is called paleontology and is closely Kentucky are the same as in most states: you need permission from associated with geology. Paleontologists use fossils to reconstruct the landowner before you can enter and collect. Native American what the Earth was like in the distant past, to show how life has artifacts are protected by the Kentucky Antiquities Law. Although changed through time, and to correlate rock strata from one area to the Kentucky Geological Survey (KGS) does not publish lists of another to aid in searching for fossil fuels (oil, natural gas, and coal) fossil collecting localities, clubs and organizations can help you get and minerals. started (try the Kentucky Paleontological Society in care of Dan Fossil-Bearing Rocks: Fossils are most commonly found in sedi- Phelps, 606-277-3148). You can find your own collection sites, using mentary rocks. Almost all of Kentucky’s rocks at the surface are geologic quadrangle maps (GQ’s). These maps are available at the sedimentary, so Kentucky is an excellent place to collect fossils. KGS and illustrate the age and types of rocks at the surface of the The types of fossils found across Kentucky vary with the age of the Earth in 7.5-minute areas (approximately 7 x 9 miles). -
Chapter 2 the Solid Materials of the Earth's Surface
CHAPTER 2 THE SOLID MATERIALS OF THE EARTH’S SURFACE 1. INTRODUCTION 1.1 To a great extent in this course, we will be dealing with processes that act on the solid materials at and near the Earth’s surface. This chapter might better be called “the ground beneath your feet”. This is the place to deal with the nature of the Earth’s surface materials, which in later sections of the chapter I will be calling regolith, sediment, and soil. 1.2 I purposely did not specify any previous knowledge of geology as a prerequisite for this course, so it is important, here in the first part of this chapter, for me to provide you with some background on Earth materials. 1.3 We will be dealing almost exclusively with the Earth’s continental surfaces. There are profound geological differences between the continents and the ocean basins, in terms of origin, age, history, and composition. Here I’ll present, very briefly, some basic things about geology. (For more depth on such matters you would need to take a course like “The Earth: What It Is, How It Works”, given in the Harvard Extension program in the fall semester of 2005– 2006 and likely to be offered again in the not-too-distant future.) 1.4 In a gross sense, the Earth is a layered body (Figure 2-1). To a first approximation, it consists of concentric shells: the core, the mantle, and the crust. Figure 2-1: Schematic cross section through the Earth. 73 The core: The core consists mostly of iron, alloyed with a small percentage of certain other chemical elements. -
Mineral Magnetism: Providing New Insights
Mineral Magnetism: Providing New Insights into Geoscience Processes ABOVE : Single-domain grain (50 nm) of magnetite from a magnetotactic 1 2 bacteria displaying a Richard J. Harrison and Joshua M. Feinberg dipole-like external magnetic field and a 1811-5209/09/0005-0209$2.50 DOI: 10.2113/gselements.5.4.209 uniformally magnetized interior agnetic minerals are ubiquitous in the natural environment, and glacial and interglacial cycles and they are also present in a wide range of biological organisms, from variations in the Asian monsoon stretching back 2 million years. More bacteria to human beings. The last ten years have seen a striking M recently, magnetic measurements improvement in our ability to detect and image the magnetization of minerals of marine sediments have been used in geological and biological samples. These minerals carry a wealth of information to determine paleooceanographic encoded in their magnetic properties. Mineral magnetism (together with circulation patterns by constraining the geographical extent of ice- the related disciplines of rock magnetism, paleomagnetism, environmental rafted detritus during the last glacial magnetism, and biomagnetism) decodes this information and applies it to maximum. Even the spread of an ever increasing range of geoscience problems, from the origin of magnetic anthropogenic pollutants can be anomalies on Mars to quantifying variations in Earth’s paleoclimate. traced throughout a city environ- ment by measuring the magnetic KEYWORDS : magnetism, magnetic minerals, magnetism theory, electron holography properties of leaves, which trap magnetic particles from passing MAgnETIC minERALS ARE EVERYWHERE! vehicles (Maher 2009 this issue). Look closely enough at any geological sample and you will In addition to the many geoscience applications, the find traces of magnetic minerals. -
GEOLOGY THEME STUDY Page 1
NATIONAL HISTORIC LANDMARKS Dr. Harry A. Butowsky GEOLOGY THEME STUDY Page 1 Geology National Historic Landmark Theme Study (Draft 1990) Introduction by Dr. Harry A. Butowsky Historian, History Division National Park Service, Washington, DC The Geology National Historic Landmark Theme Study represents the second phase of the National Park Service's thematic study of the history of American science. Phase one of this study, Astronomy and Astrophysics: A National Historic Landmark Theme Study was completed in l989. Subsequent phases of the science theme study will include the disciplines of biology, chemistry, mathematics, physics and other related sciences. The Science Theme Study is being completed by the National Historic Landmarks Survey of the National Park Service in compliance with the requirements of the Historic Sites Act of l935. The Historic Sites Act established "a national policy to preserve for public use historic sites, buildings and objects of national significance for the inspiration and benefit of the American people." Under the terms of the Act, the service is required to survey, study, protect, preserve, maintain, or operate nationally significant historic buildings, sites & objects. The National Historic Landmarks Survey of the National Park Service is charged with the responsibility of identifying America's nationally significant historic property. The survey meets this obligation through a comprehensive process involving thematic study of the facets of American History. In recent years, the survey has completed National Historic Landmark theme studies on topics as diverse as the American space program, World War II in the Pacific, the US Constitution, recreation in the United States and architecture in the National Parks.