Gold in South Africa by P.R
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Acid Mine Drainage and Human Rights
Acid Mine Drainage and Human Rights The South African Human Rights commission acknowledges MARIETTE LIEFFERINK and EUGENE VILJOEN for providing the photographs that appear in this booklet. Mariette is the CEO of the Federation for a Sustainable Environment and was a member of the SAHRC Section 05 Committee on Human Rights and Acid Mine Drainage. Eugene is one of the Commission’s valuable stakeholders who has worked on mining issues in the West Rand, Mogale City, for several years. 2 TABLE OF CONTENTS 1. What is Acid Mine Drainage? ---------------------------------------------------------4 2. How does Acid Mine Drainage impact on human rights? ---------------------6 2.1 Who is affected by the development of mines? --------------------------7 Consultation -----------------------------------------------------------------------8 Human rights and Business ----------------------------------------------------9 3. How is Acid Mine Drainage treated? --------------------------------------------- 10 Active Treatment Technology ------------------------------------------------ 11 Passive Treatment Technology ---------------------------------------------- 12 Recovery of useful minerals from AMD ----------------------------------- 13 4. What are mines doing about Acid Mine Drainage? --------------------------- 13 Industry Responses ------------------------------------------------------------- 14 5. What is the South African Government doing about Acid Mine Drainage in Gauteng? -------------------------------------------------- 15 5.1 Delayed Government -
South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
Acid Mine Drainage and Its Governance in the Gauteng City-Region 2015
R E P Acid Mine Drainage A P L A N and its Governance O I S A C in the Gauteng City-Region C 10O Researched and written for the GCRO by Kerry Bobbins May 2015 ISBN Number: 978-0-620-65778-5 R E P Acid Mine Drainage A P L A N and its Governance O I S A C in the Gauteng City-Region C O Researched and written for the GCRO by Kerry Bobbins May 2015 List of Acronyms AECOM AECOMSM AMD Acid Mine Drainage BKS BKS Group (Pty) Ltd CB Central Basin CBD Central Business District CBEC Central Basin Environmental Corporation CGS Council for Geo-science CME Compliance and Monitoring Enforcement CRG Central Rand Gold CSIR Council for Scientific and Industrial Research DBSA Development Bank of South Africa DEA Department of Environmental Affairs DMR Department of Mineral Resources DNT Department of National Treasury DWA Department of Water Affairs DWAF Department of Water Affairs and Forestry DWE Digby Wells Environmental DWS Department of Water and Sanitation EB Eastern Basin EBEC Eastern Basin Environmental Corporation ECL Environmental Critical Level EIA Environmental Impact Assessment ERPM/ERM East Rand Proprietary Mines FSE Federation for a Sustainable Environment GCIS Government Communication and Information System GCR Gauteng City-Region GCRO Gauteng City-Region Observatory GDACE Gauteng Department of Agriculture, Environment and Conservation GDARD Gauteng Department of Agriculture and Rural Development HDS High Density Sludge I&AP Interested and affected party IDC Industrial Development Corporation IMC Inter-Ministerial Committee LHWP Lesotho -
Alternative Model for the Derivation of Gold in the Witwatersrand Supergroup
J. geol. Soc. London, Vol. 141, 1984, pp. 263-272, 3 figs., 3 tables. Printed in Northern Ireland. Alternative model for the derivation of gold in the Witwatersrand Supergroup Thomas 0. Reimer SUMMARY: Present models of the derivation of the gold in the Witwatersrand conglomerates of South Africa as detrital grains directly from primary deposits in a source area consisting mainly of Archaean schist belts meets with a volume problem. Witwatersrand deposits have yielded about 923 kg/km2 Au compared to about 65 kg/km* Au in the richest known schist belts. Differences in the extent of mining activities cannot account for these differences in yield. Gold fineness, grain size, and morphology of the gold particles are also difficult to reconcile with a purely detrital derivation. Data on the mobility of gold in the hydrosphere and in the weatheringcycle are used to erect a model which predicts that mostof the gold in the Witwatersrand conglomerates was derived from a source area in trace amounts in a ‘dissolved’ form and precipitated at or close to the edge of the depositional basin, possibly under organic influences. Subsequent sedimentary reworking and metamorphiddiagenetic remobilization led to the formation of the complex association of minerals observed now in the conglomerates. Since the dawn of civilization an estimatedtotal of data irreconcilable with the ‘mechanical’ model of about 65 000 tons of gold has been produced. Of this derivation of the Witwatersrand gold. Atthe same about 55% has beenderived fromthe auriferous time an alternative model for the processes which led conglomerates of the early Proterozoic Witwatersrand tothe spectacularconcentration of gold in these Supergroup (2.3-2.7 Ga.). -
Merafong City Local Municipality Local Integrated Transport Plan (LITP)
Merafong City Local Municipality Local Integrated Transport Plan (LITP) October 2018 SUMMARY SHEET Report Type Transportation Planning Title Report Framework: Merafong City Local Municipality – Local Integrated Transport Plan Location Merafong City Local Municipality Client West Rand District Municipality Reference Number ITS 3893 Project Team Dr Pieter Pretorius Florence Asiimwe Henri Vorster Charmaine Dladla Cobus Lotz Contact Details Tel: 012 349 1664 Date October 2018 Report Status Second Draft INNOVATIVE TRANSPORT SOLUTIONS (PTY) LTD Page i TABLE OF CONTENTS 1. INTRODUCTION .......................................................................................................................... 3 1.1. Background ................................................................................................................................. 3 1.2. Legislation requirements ............................................................................................................ 3 1.3. Format of the LITP ...................................................................................................................... 4 2. TRANSPORT STATUS QUO .......................................................................................................... 5 2.1. Commuter Rail Facilities ............................................................................................................. 5 1.1. Mini-Bus Taxi Facilities .............................................................................................................. -
Appendix E 1: I&Ap Database
Scoping Report for the Proposed West Wits Mining Project August 2018 APPENDIX E 1: I&AP DATABASE E WEST WITS MLI (PTY) LTD WEST WITS MLI RIGHT APPLICAITON INTERESTED AND AFFECTED PARTY DATABASE TABLE 1: WARD COUNCILLORS, MUNICIPAL STRUCTURES, RESIDENTS AND RELATED FORUMS OR ASSOCIATIONS ........................................................................... 2 TABLE 2: MEETING ATTENDANCE REGISTERS................................................................................................................................................................................ 13 TABLE 3: COMMERCIAL AND INDUSTRIAL BUSINESSES, PARASTATALS, COMMUNITY STRUCTURES, NON-GOVERNMENT ORGANISATIONS ASSOCIATIONS .............. 84 TABLE 4: REGULATORY AUTHORITIES .......................................................................................................................................................................................... 91 1 TABLE 1: WARD COUNCILLORS, MUNICIPAL STRUCTURES, RESIDENTS AND RELATED FORUMS OR ASSOCIATIONS Name and Surname Interest in Project Postal Address Contact numbers E-mail Elivis Matji Business 0792536704 [email protected]; AC Swart Hamberg Resident and 2 Bree Street 0832503492 [email protected]; Representative in Communities Hamberg Against Mining Roodepoort 1724 Alton Snyders Davidsonville Resident 0748743658 [email protected]; Fabian Minaar Resident 0781024421 Elizabeth Stapelberg Resident 29 Geoffrey Street 0820716437 [email protected]; Creswell Park [email protected]; Roodepoort -
Palaeontological Heritage of the Free State
SAHRA PALAEOTECHNICAL REPORT PALAEONTOLOGICAL HERITAGE OF THE FREE STATE Brandwag Rock Golden Gate Highlands National Park. Photograpgh: Gideon Groenewald Dr Gideon Groenewald Cell: (082) 339-9202 David Groenewald Cell: (083) 469-4696 Logistical Support: Sue Groenewald Cell: (082) 339 9202 PO Box 360, Clarens, 9707 ([email protected]) (Copyright: March 2014) GENERAL INTRODUCTION The core purpose of this SAHRA palaeotechnical report (PTR) is to briefly but comprehensively document the palaeontological heritage resources in South Africa in an accessible and useful format. Following the request by SAHRA, the report is presented in the form of two sections. The first section outlines the general geological history of South Africa and the second section provides a more detailed, geological history of the Free State, Gauteng, North West, Limpopo and Mpumalanga Provinces with specific reference to the palaeontological sensitivity of geological formations and their importance to the development of life through 3600 million years of time in Earth history. The first section summarises the geological history of South Africa and gives a very brief description of the six major events that shaped the Earth over time. The known and predicted fossil heritage within all the major fossiliferous stratigraphic units (formations, groups etc) that crop out in South Africa are presented on a map that relates directly to the composite geological map of South Africa where mapping was done on a 1:250 000 scale. The palaeontological sensitivity of geological units was allocated sensitivity ratings on a five point scale: very high sensitivity, high sensitivity, moderate sensitivity, low sensitivity and very low sensitivity (Table 1). -
Mine Water Management in the Witwatersrand Gold Fields with Special Emphasis on Acid Mine Drainage
MINE WATER MANAGEMENT IN THE WITWATERSRAND GOLD FIELDS WITH SPECIAL EMPHASIS ON ACID MINE DRAINAGE REPORT TO THE INTER-MINISTERIAL COMMITTEE ON ACID MINE DRAINAGE DECEMBER 2010 REPORT TO THE INTER-MINISTERIAL COMMITTEE ON ACID MINE DRAINAGE MINE WATER MANAGEMENT IN THE WITWATERSRAND GOLD FIELDS WITH SPECIAL EMPHASIS ON ACID MINE DRAINAGE Prepared by the Expert Team of the Inter-Ministerial Committee under the Coordination of the Council for Geoscience Team of Experts drawn from: The Council for Geoscience Department of Water Affairs Department of Mineral Resources Council for Scientific and Industrial Research Mintek Water Research Commission and Advisors: Prof. TS McCarthy – University of the Witwatersrand Prof G Steyl – University of the Free State Prof. J Maree – Tshwane University of Technology Prof. B Zhao – University of Fort Hare December 2010 TEAM OF EXPERTS — RESEARCHERS Chairperson Dr T Ramontja Chief Executive Officer – Council for Geoscience Compilers and contributing authors: Dr H Coetzee Specialist Scientist: Environmental Geoscience – Council for Geoscience Mr PJ Hobbs Senior Research Hydrogeologist – Council for Scientific and Industrial Research Dr JE Burgess Research Manager – Water Research Commission Prof. A Thomas Unit Manager: Central Regions – Council for Geoscience Mr M Keet Acting Director: Gauteng Regional Office – Department of Water Affairs Contributing authors: Dr B Yibas Geochemist/Geologist – Council for Geoscience Ms D van Tonder Geologist – Council for Geoscience Mr F Netili Hydrogeologist – Council for -
Management of Water Levels in the Flooded Mines of the Witwatersrand, South Africa
Proceedings IMWA 2016, Freiberg/Germany | Drebenstedt, Carsten, Paul, Michael (eds.) | Mining Meets Water – Conflicts and Solutions Management of water levels in the flooded mines of the Witwatersrand, South Africa Henk Coetzee1,2 1Council for Geoscience, 280 Pretoria Street, Silverton, Pretoria, South Africa, 2Department of Geosciences/Africa Earth Observatory Network, Nelson Mandela Metropolitan University, Summerstrand Campus, Port Elizabeth, South Africa [email protected] Abstract Following the cessation of underground mining in the three original mining complexes in South Africa’s Witwatersrand Gold Field, mines started to flood with no control measures in place. In 2002, acidic water began to discharge from the West Rand Gold Field’s underground workings, negatively impacting on the downstream environment, with impacts identified in both surface and underground water. In the years following this, underground operations ceased in the Central Rand and East Rand Gold Fields and the underground workings were allowed to flood. Three approaches have been identified for the management of the flooded underground workings: Flooding and management of the discharge at surface. Maintaining the water level at a pre-determined safe level, locally referred to as an “environmental critical level” by pumping. Controlling the water level in the underground workings by means of a discharge tunnel. Currently, pump and treat programmes are at various stages of development and implementation in the three original gold fields. Planning for these has been severely hampered by a lack of reliable historical data on volumes pumped. The absence of supporting data also led to the selection of conservative environmental critical levels, which will be extremely costly to maintain. -
South Africa's Coalfields – a 2014 Perspective
South Africa's coalfields – a 2014 perspective 1Hancox, P. John and 2,3Götz, Annette E. 1University of the Witwatersrand, School of Geosciences, Private Bag 3, 2050 Wits, South Africa; [email protected] 2University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa; [email protected] 3Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation Highlights • South Africa’s Coalfields are presented. • The role of Gondwanan coals as palaeoclimate archives is stated. • Future research fields include palynology, sequence stratigraphy, basin fill. Abstract For well over a century and a half coal has played a vital role in South Africa’s economy and currently bituminous coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the production of a substantial percentage of the country’s liquid fuels. It furthermore provides a considerable source of foreign revenue from exports. Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review of their exploration and exploitation histories, general geology, and coal seam nomenclature and coal qualities. Within the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up of Gondwana most of the coals bearing successions were intruded by dolerite. These intrusions are important as they may cause devolatilisation and burning of the coal, create structural disturbances and related seam correlation problems, and difficulties in mining operations. -
A Case Study from the Witwatersrand Gold Basin, South Africa
South African Journal of Geomatics, Vol. 4, No. 2, June 2015 Mineralogy and heavy metal content of secondary mineral salts: A case study from the Witwatersrand Gold Basin, South Africa. Mafuza Maya 1,3, Malcom Sutton1, Hlanganani Tutu2, Isabel Weiersbye 1, 1School of Animal, Plant and Environmental Sciences; University of Witwatersrand 2Molecular Sciences Institute, School of Chemistry, University of the Witwatersrand 3Council for Geoscience Corresponding author: Email: [email protected] DOI: http://dx.doi.org/10.4314/sajg.v4i2.8 Abstract Secondary minerals associated with acid mine drainage play an important role in metal cycling and may pose a geochemical hazard. The occurrence of secondary minerals indicates prevailing and past geochemical conditions. Detecting and characterising secondary minerals is necessary to the planning of remediation programmes. This paper investigates the mineralogical and heavy metal contents of mineral salts associated with acid mine drainage in the East Rand area of the Witwatersrand Basin. Powdered X-ray diffraction was used to identify and quantify mineralogical phases and a scanning electron microscope was used to determine the morphology of the identified minerals. Major cations and anions were determined using Inductively Coupled Plasma Mass Spectrometry (ICP-MS) and Ion Chromatography (IC). Geochemical modelling was used to predict the saturation of the minerals. Efflorescent crusts contained high levels of trace metals. Enrichment of trace metals, electrical conductivity and sulphate were highest in white salts. A high metal content was associated with low pH values in mineral salts. The salts were dominated by quartz and clay minerals of the smectite group. Tamarugite, apjohnite and jarosite were the predominant sulphate minerals in the salts. -
Appendix the Economic Commodities
Appendix The Economic Commodities This section provides a commodity cross-reference to ARSENIC the geological descriptions of the main text. The page (209-210) numbers given after most section headings (main entries are enumerated in italic type) are intended to direct the World 1979 production of arsenic trioxide 32 824 t. reader to the pages in which the geological descriptions Share of production: USSR 23%, France 22%, Sweden are found. The brief entries also give some idea of the 21%, Mexico 18%, Namibia 8%. These figures exclude world's annual production, and the five major countries the USA, whose production figures are withheld. Arse that share in this. Commodity production figures are nic compounds are used in herbicides and plant desic based on those of the Bureau of Mines (1980a,b) and cants, wood preservatives, mineral flotation agents, United Nations (1979). Other important references are glassware and pharmaceuticals. Arsenic is produced Brobst and Pratt (1973) and LeFond (1975). always as a by-product of some metal, and the principal There is no unified quantity of measure. Commodities ore minerals are arsenopyrite FeAsS, lOllingite FeAs2, may be traditionally quoted in metric tonnes (denoted smaltite CoAs2, niccolite NiAs, tennantite by t) ( = 2205 pounds), long tons ( = 2240 pounds) and (Cu,Fe)sAs2S7, enargite Cu3AsS4, proustite Ag3AsS3 short tons (2000 pounds). Precious metals are usually and relagar AsS (Gualtieri, 1973). quoted in troy ounces ( = 31.103 grams), diamonds in carats ( = 0.2 gram) and mercury in flasks ( = 76 pounds). The standard unit used throughout this book is the ASBESTOS metric tonne (tonne), which is equal to 1000 000 grams (1 Mg).