Multiple Scales of Diamond Mining in Akwatia, Ghana: Addressing Environmental and Human Development Impact
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A Review of the Birimian Supergroup- and Tarkwaian Group-Hosted Gold Deposits of Ghana
177 A review of the Birimian Supergroup- and Tarkwaian Group-hosted gold deposits of Ghana Albertus J. B. Smith1,2*, George Henry1,2 and Susan Frost-Killian3 1 DST-NRF Centre of Excellence for Integrated Mineral and Energy Resource Analysis, Department of Geology, University of Johannesburg, Auckland Park, 2006, South Africa. *Corresponding author e-mail address: [email protected] 2 Palaeoproterozoic Mineralisation Research Group, Department of Geology, University of Johannesburg, Auckland Park, 2006, South Africa 3 The MSA Group, 20B Rothesay Avenue, Craighall Park, 2196, South Africa DOI: 10.18814/epiiugs/2016/v39i2/95775 Ghana is the largest producer of gold in West Africa, veins. The vein- and sulphide-hosted gold is strongly a region with over 2,500 years of history with regards to associated with deformational fabrics formed by the gold production and trade. Modern exploration for and Eburnean extensional and compressional events, mining of gold in Ghana dates from 1874 with the respectively, suggesting that disseminated sulphide establishment of the British Gold Coast Colony, which mineralisation predates quartz vein-hosted was followed in 1957 by the independence of Ghana and mineralisation. The fluid from which the gold precipitated increased gold production since the early 1980s through is believed to have been of metamorphic origin and Ghana’s Economic Recovery Plan. At the time of writing, carbon dioxide (CO2) dominated, with lesser water (H2O) gold production (108.2 tonnes or 3.48 million ounces and nitrogen (N2) and minor methane (CH4). Gold [Moz] in 2014) accounted for approximately one-third precipitation was probably caused by decrease in of Ghana’s export revenues, with 36% of gold production pressure, temperature and CO2-H2O immiscibility, at coming from small-scale mining. -
LOCATIONS for 2020 SSNIT MOBILE SERVICE the Annual SSNIT Mobile Service Comes Off Frommonday, 26Th October to Friday, 30Th October, 2020
SOCIAL SECURITY AND NATIONAL INSURANCE TRUST (SSNIT) LOCATIONS FOR 2020 SSNIT MOBILE SERVICE The annual SSNIT Mobile Service comes off fromMonday, 26th October to Friday, 30th October, 2020. Major activities to be undertaken at the SSNIT Mobile Service locations include: • Statement issuance • Benefits Processing Initiation andbenefit status verification • Resolution of Compliance Concerns • Contribution collection • Biometric Registration • SSNIT cards activation and distribution • Student Loan Payment Issues • Employer Registration • Submission and validation of contribution report • General enquiries about the business and operations of SSNIT During this period, SSNIT will bring its services closer to you at the following vantage locations: AREA BRANCH LOCATION AREA BRANCH LOCATION 1. Forecourt of St. John Ambulance Service Accra Central (Ghana Ambulance Service) near the Ministry Akim Oda 1. Opposite Kenop pharmacy, Liberty of Agriculture on the Accra High Street. Adabraka 1. Forecourt of old Globe Cinema 1. Frontage of the Volta Regional Education Office HO Accra 1. St. Michael’s Garrison Catholic Church, Block - Ministries Airport South 37 Military Hospital 1. Forecourt of the old Hohoe Municipal Assembly 1. Korle-Bu Teaching Hospital, in front of the Hohoe Korle-Bu Hall (behind the taxi rank) Administration block 1. St. Dominic’s Hospital, Akwatia from 26th to Pension House 1. Frontage of the Oxford Street Mall (Shoprite) 28th Oct., 2020 Achimota 1. Premises of Mecham House, Papaye, Lapaz Kade 2. Ghana Oil Palm Development Corporation, Agona Swedru 1. Shell Fuel Station, Texaco Okumaning from 29th to 30th October, 2020 1. Jinlet Pharmacy, opposite Fanmilk Ltd, North Koforidua AIA Industrial Area 1. The Premises of Regional Co-ordinating Council K o k o m l e m l e 1. -
The Geology of the Gold Deposits of Prestea Gold Belt of Ghana*
The Geology of the Gold Deposits of Prestea Gold Belt of Ghana* K. Dzigbodi-Adjimah and D. Nana Asamoah Dzigbodi-Adjimah, K. and Nana Asamoah, D., (2009), “The Geology of the Gold Deposits of Prestea Gold Belt of Ghana”, Ghana Mining Journal, Vol. 11, pp. 7 - 18. Abstract This paper presents the geology of the gold deposits along the Prestea gold belt of Ghana to assist exploration work for new orebodies along the belt. Prestea district is the third largest gold producer in West Africa after Obuasi and Tarkwa districts (over 250 metric tonnes Au during the last century). The gold deposits are structurally controlled and occur in a deep-seated fault or fissure zone that is regarded as the ore channel. This structure, which lies at the contact between metavolcanic and metasedimentary rocks in Birimian rocks, is more open (and contains more quartz lodes) at the southern end around Prestea than at Bogoso to the north. The gold deposits consist of the Quartz Vein Type, (QVT) and the Dis- seminated Sulphide Type (DST). The QVT orebodies, which generally carry higher Au grades, lie within a graphitic gouge in the fissure zones whilst the DST is found mostly in sheared or crushed rocks near the fissure zones. Deposits were grouped into three in terms of geographic location and state of development; The deposits south of Prestea are the least developed but have been extensively explored by Takoradi Gold Company. Those at Prestea have been worked exclusively as underground mines on QVT orebodies by Prestea Goldfields Limited and its forerunners; Ariston and Ghana Main Reef companies until 1998 whilst the deposits north of Prestea, which were first worked as surface mines (on DST orebodies) by Marlu Mines up to 1952, were revived by Billiton Bogoso Gold in 1990. -
The Economics of the Atewa Forest Range, Ghana
THE ECONOMICS OF THE ATEWA FOREST RANGE, GHANA Living water from the mountain Protecting Atewa water resources THE ECONOMICS OF THE ATEWA FOREST RANGE, GHANA Living water from the mountain Protecting Atewa water resources DISCLAIMER This report was commissioned by IUCN NL and A Rocha Ghana as part of the ‘Living Water from the mountain - Protecting Atewa water resources’ project. The study received support of the Forestry Commission, the Water Resource Commission and the NGO Coalition Against Mining Atewa (CONAMA) and financial assistance of the Dutch Ministry of Foreign Affairs as part of the Ghana – Netherlands WASH program. The findings, interpretations and conclusions expressed here are those of the authors and do not necessarily reflect the views of the Dutch Ministry of Foreign Affairs, IUCN NL, A Rocha Ghana, the Forestry Commission, the Water Resource Commission or the NGO Coalition Against Mining Atewa (CONAMA). Any errors are purely the responsibility of the authors. Not all economic values presented in this study are captured by market mechanisms or translated to financial streams; the values of ecosystem services calculated in this study should therefore not be interpreted as financial values. Economic values represent wellbeing of stakeholders and do not represent the financial return of an investment case. The study should not be used as the basis for investments or related actions and activities without obtaining specific professional advice. This publication may be reproduced in whole or in part and in any form for educational -
Geochemistry of an Ultramafic-Rodingite Rock Association in the Paleoproterozoic Dixcove Greenstone Belt, Southwestern Ghana
Journal of African Earth Sciences 45 (2006) 333–346 www.elsevier.com/locate/jafrearsci Geochemistry of an ultramafic-rodingite rock association in the Paleoproterozoic Dixcove greenstone belt, southwestern Ghana Kodjopa Attoh a,*, Matthew J. Evans a,1, M.E. Bickford b a Department of Earth and Atmospheric Sciences, Cornell University, Snee Hall, Ithaca, NY 14853, USA b Department of Earth Sciences, Syracuse University, Syracuse, NY 13244, USA Received 11 January 2005; received in revised form 20 February 2006; accepted 2 March 2006 Available online 18 May 2006 Abstract Rodingite occurs in ultramafic rocks within the Paleoproterozoic (Birimian) Dixcove greenstone belt in southwestern Ghana. U–Pb analyses of zircons from granitoids intrusive into the greenstone belt constrain the age of the rodingite-ultramafic association to be older than 2159 Ma. The ultramafic complex consists of variably serpentinized dunite and harzburgite overlain by gabbroic rocks, which together show petrographic and geochemical characteristics consistent with their formation by fractional crystallization involving olivine and plagioclase cumulates. Major and trace element concentrations and patterns in the ultramafic–mafic cumulate rocks and associated plagiogranite are similar to rocks in ophiolitic suites. The rodingites, which occur as irregular pods and lenses, and as veins and blocks in the serpentinized zones, are characterized by high Al2O3 and CaO contents, which together with petrographic evidence indicate their formation from plagioclase-rich protoliths. The peridotites are highly depleted in REE and display flat, chondrite-normalized REE pat- terns with variable, but mostly small, positive Eu anomalies whereas the rodingites, which are also highly depleted, with overall REE contents from 0.04 to 1.2 times chondrite values, display distinct large positive Eu anomalies. -
The Composite Budget of the Denkyembour District Assembly For
REPUBLIC OF GHANA THE COMPOSITE BUDGET OF THE DENKYEMBOUR DISTRICT ASSEMBLY FOR THE 2016 FISCAL YEAR DENKYEMBOUR DISTRICT ASSEMBLY, AKWATIA Page 1 Table of Contents 1.1 Name Of District .......................................................................................................................... 4 L2 Establishing The District ............................................................................................................. 4 1.3 The Assembly Structure ............................................................................................................. 4 1.4 Population .................................................................................................................................... 4 1.5 The District Economy ................................................................................................................. 4 1.6 Agriculture ................................................................................................................................... 5 1.7 Roads ............................................................................................................................................ 5 1.8 Education ..................................................................................................................................... 5 1.9 Health ........................................................................................................................................... 5 1.10 Environment ............................................................................................................................. -
Sa˜O Luıs Craton and Gurupi Belt (Brazil)
Sa˜o Luı´s Craton and Gurupi Belt (Brazil): possible links with the West African Craton and surrounding Pan-African belts E. L. KLEIN1,2 & C. A. V. MOURA3 1CPRM (Companhia de Pesquisa de Recursos Minerais)/Geological Survey of Brazil, Av. Dr. Freitas, 3645, Bele´m-PA, CEP 66095-110, Brazil (e-mail: [email protected]) 2Researcher at CNPq (Conselho Nacional de Desenvolvimento Cientı´fico e Tecnolo´gico) 3Laborato´rio de Geologia Isoto´pica/Para´-Iso, Universidade Federal do Para´, Centro de Geocieˆncias, CP 1611, Bele´m-PA, Brazil, CEP 66075-900 Abstract: The Sa˜o Luı´s Craton and the Palaeoproterozoic basement rocks of the Neoproterozoic Gurupi Belt in northern Brazil are part of an orogen having an early accretionary phase at 2240– 2150 Ma and a late collisional phase at 2080 + 20 Ma. Geological, geochronological and isotopic evidence, along with palaeogeographic reconstructions, strongly suggest that these Brazilian terrains were contiguous with the West African Craton in Palaeoproterozoic times, and that this landmass apparently survived subsequent continental break-up until its incorporation in Rodinia. The Gurupi Belt is an orogen developed in the southern margin of the West African–Sa˜o Luı´s Craton at c. 750–550 Ma, after the break up of Rodinia. Factors such as present-day and possible past geographical positions, the timing of a few well-characterized events, the structural polarity and internal structure of the belt, in addition to other indirect evidence, all favour correlation between the Gurupi Belt and other Brasiliano/Pan-African belts, especially the Me´dio Coreau´ domain of the Borborema Province and the Trans-Saharan Belt of Africa, despite the lack of proven physical links between them. -
A Contextual Review of the Ghanaian Small-Scale Mining Industry
Mining, Minerals and Sustainable Development September 2001 No. 76 A Contextual Review of the Ghanaian Small-scale Mining Industry Gavin Hilson Imperial College Centre for Environmental Technology, London, UK This report was commissioned by the MMSD project of IIED. It remains the Copyright © 2002 IIED and WBCSD. All rights reserved sole responsibility of the author(s) and does not necessarily reflect the views of Mining, Minerals and the MMSD project, Assurance Group or Sponsors Group, or those of IIED or Sustainable Development is WBCSD. The Report has been edited by an MMSD editor. a project of the International Institute for Environment and Development (IIED). The project was made possible by the support of the World Business Council for Sustainable Development (WBCSD). IIED is a company limited by guarantee and incorporated in England. Reg. No. 2188452. VAT Reg. No. GB 440 4948 50. Registered Charity No. 800066 Gavin Hilson Environmental Policy and Management Group (EPMG) Imperial College Centre for Environmental Technology Royal School of Mines Prince Consort Road London SW7 2BP [email protected] Introduction 3 An Overview of Small-scale Mining in Ghana 3 Historical Perspective 3 Geological Setting 4 Socio-economic Impact of Small-scale Mining in Ghana 5 Employment 5 Production from Small-scale Mining and Revenues Accrued 7 The Precious Minerals Marketing Corporation (PMMC) 8 Organization of Small-scale Mining Operations in Ghana 9 Support Schemes for Small-scale Mining in Ghana 12 Environmental Impact of Small-Scale Mining in Ghana 15 Land Use Disputes Between Large- and Small-scale Miners 18 Regulatory Framework for Small-scale Mining in Ghana 21 Contact Information 24 Background Reading 25 Grey Literature, Reports and Unpublished Studies 25 Journal Articles, Books and Book Chapters 26 Literature Cited 27 2 A Contextual Review of the Ghanaian Small-scale Mining Industry Introduction The aim of this report is to provide a detailed overview of the Ghanaian small-scale mining industry. -
Paper 5 Ppoint Presentation
COMMUNITIES AND SMALL SCALE MINING (CASM) 3 RD AGM AND LEARNING EVENT-ELMINA, GHANA SEPTEMBER 8th-10 th 2003 PRESENTATION BY PRECIOUS MINERALS MARKETING COMPANY LTD TOPIC: THE IMPORTANCE OF MARKETING IN SMALL SCALE MINING REGULARIZATION PROCESS IN GHANA FORMAT OF PRESENTATION • DEFINITION • NATURE • CHARACTERISTICS • HISTORICAL PERSPECTIVE - GOLD - DIAMOND • EARLY DISPOSAL BY WINNERS - DIAMOND - GOLD • ROLE OF PMMC • MARKETING OF SMALL SCALE MINERS’ WINNINGS - INTRODUCTION - DIAMOND - GOLD • CONCLUSION 1 • DEFINITION Small scale mining • Is also called artisanal mining • It involves alluvial mining operations (alluvial gold) from uncertain reserves . • It is a process where peasant miners pan for gold along the banks and the beds of rivers and streams • May involve mining deep down to gold bearing rocks (lode gold) and diamondiferous gravels. NATURE Small scale mining is: • Driven by the get rich quick mentality of transient youth. • Family- oriented analogous to subsistence farming • Largely poverty driven activity • Generally labour intensive • Widespread and prevalent in many of the world’s poorest countries in Africa and South America. CHARACTERISTICS Small scale mining is characterized by • The absence or low degree of mechanization, explosives and chemicals. • Low safety standards • Poorly trained personnel • High production waste due to low recovery • Inadequate capital • High exposure to risk and health hazards • Some illegality due to refusal to acquire mining rights and excessive trespassing • Very little consideration for environmental issues 2 HISTORICAL PERSPECTIVE GOLD • Ghana formerly Gold Coast had been associated with gold several years before arrival of Europeans. • Gold used as ornaments by Chiefs and the wealthy for barter and as a treasure in ancient kingdoms and pre-colonial Arab trading. -
Structural Constraints of the Birimian Lithium Pegmatites of Bougouni (Southern Mali, Leo-Man Shield)
EGU21-6752 https://doi.org/10.5194/egusphere-egu21-6752 EGU General Assembly 2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Structural constraints of the Birimian lithium pegmatites of Bougouni (Southern Mali, Leo-Man shield) Séko Sanogo, Cyril Durand, Michel Dubois, and Ousmane Wane Université de Lille, Villeneuve d'asq, France ([email protected]) The Bougouni region is located in the southern Mali, 170 km south-east of Bamako. It is part of the northern edge of the Leo-Man [UdMO1] shield (southern part of the West-African Craton). It is known for its swarm of pegmatites, most investigated as a lithium resource (spodumene pegmatites) and its gold potential. It is made up of metavolcanosedimentary rocks and plutonic complexes of the Birimian (Paleoproterozoic). The objectives of this study are: 1) to make a review of the main regional structural features, 2) to define the structural control of the pegmatite emplacement. To reach these aims a structural analysis was carried out using the information collected during our field campaigns (2018 and 2019) and data from previous works. Metavolcanosedimentary rocks had undergone a low grade metamorphism degree. Schistosities in these rocks (n=156 measurements) are distributed along 2 main directions which indicate two deformation phases. The first one, D1, oriented NNW-SSE to N-S. It is ductile, responsible for low grade regional metamorphism (Baratoux et al., 2011) and crustal thickening of the volcano- sedimentary rocks (Wane et al., 2018). It is linked to a compression event oriented E-W to ESE- WNW (Baratoux et al., 2011; Wane et al., 2018). -
Mapping the Expansion of Galamsey Gold Mines in the Cocoa Growing Area of Ghana Using Optical Remote Sensing
Mapping the expansion of galamsey gold mines in the cocoa growing area of Ghana using optical Remote Sensing B. Snapira, D.M. Simmsa, T.W. Wainea,∗ aCranfield University, Cranfield, Bedfordshire, MK43 0AL, UK Abstract Artisanal gold mining (galamsey) and cocoa farming are essential sources of income for local populations in Ghana. Unfortunately the former poses serious threats to the environment and human health, and conflicts with cocoa farm- ing and other livelihoods. Timely and spatially referenced information on the extent of galamsey is needed to understand and limit the negative impacts of mining. To address this, we use multi-date UK-DMC2 satellite images to map the extent and expansion of galamsey from 2011 to 2015. We map the total area of galamsey in 2013 over the cocoa growing area, using k-means clustering on a cloud-free 2013 image with strong spectral contrast between galamsey and the surrounding vegetation. We also process a pair of hazy images from 2011 and 2015 with Multivariate Alteration Detection to map the 2011{2015 galamsey expansion in a subset, labelled the change area. We use a set of visually inter- preted random sample points to compute bias-corrected area estimates. We also delineate an indicative impact zone of pollution proportional to the density of galamsey, assuming a maximum radius of 10 km. In the cocoa growing area of Ghana, the estimated total area of galamsey in 2013 is 27,839 ha with an impact zone of 551,496 ha. In the change area, galamsey has more than tripled between 2011 and 2015, resulting in 603 ha of direct encroachment into protected forest reserves. -
Ghana: Floods
Disaster relief emergency fund (DREF) Ghana: Floods DREF operation n° MDRGH004 GLIDE n° FL-2011-000106-GHA 19 August, 2011 The International Federation of Red Cross and Red Crescent (IFRC) Disaster Relief Emergency Fund (DREF) is a source of un-earmarked money created by the Federation in 1985 to ensure that immediate financial support is available for Red Cross and Red Crescent emergency response. The DREF is a vital part of the International Federation’s disaster response system and increases the ability of National Societies to respond to disasters. CHF 91,510 has been allocated from the IFRC’s Disaster Relief Emergency Fund (DREF) to support the Ghana Red Cross Society in delivering immediate assistance to some 2,500 beneficiaries Un-earmarked funds to repay DREF are encouraged. Summary: A 10-hour torrential rainfall in Ghana on 20 July, 2011 and the overflow of the Birim River in the Eastern Region have caused heavy flooding in some parts of the country. One Hundred and Thirty communities in 15 districts of the Eastern and Volta Regions were the most affected with 1,875 houses damaged. Nine lives were lost to the floods. Some 872 acres of farmlands have been submerged with crops washed away while some bridges have also Many of the affected persons were trapped with their houses been damaged by the floods, thereby making submerged while vehicular movement was disrupted by flood water/photo GRCS movement of people and goods difficult. Over 45,000 persons have been displaced in 4 regions of Ghana, namely Eastern, Volta, Ashanti and Central –with the Eastern and Volta being the most affected (36,517 persons).