Orion Set to Fast-Track Exploration and Evaluation of the Okiep Copper District After Securing Major Database
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6 the Environments Associated with the Proposed Alternative Sites
6 THE ENVIRONMENTS ASSOCIATED WITH THE PROPOSED ALTERNATIVE SITES The purpose of this section is to describe the environments associated with the proposed alternative sites. The information contained herein was extracted from the relevant specialist studies. Please refer to Section 3.5 for a list of all the relevant specialists and their fields of expertise and to Appendix E for the original specialist reports. 6.1 Brazil Site 6.1.1 Physical (a) Location The Brazil site is situated in the Kleinzee / Nolloth region of the Northern Cape, within the jurisdiction of the Nama-Khoi Municipality ( Figure 16). The site has the following co-ordinates: 29°48’51.40’’S and 17°4’42.21’’E. The Brazil site is situated approximately 500 km north of Cape Town and 100 km west-southwest of Springbok. Kleinzee is located 15 km north, Koiingnaas is 90 km south and Kamieskroon is located 90 km southeast of the Brazil site. Figure 16: Location of the proposed Brazil site in relation to the surrounding areas (Bulman, 2007) Nuclear 1 EIA: Final Scoping Report Eskom Holdings Limited 6-1 Issue 1.0 / July 2008 (b) Topography The topography in the Brazil region is largely flat, with only a gentle slope down to the coast. The coast is composed of both sandy and rocky shores. The topography is characterised by a small fore-dune complex immediately adjacent to the coast with the highest elevation of approximately nine mamsl. Further inland the general elevation depresses to about five mamsl in the middle of the study area and then gradually rises towards the east. -
Explore the Northern Cape Province
Cultural Guiding - Explore The Northern Cape Province When Schalk van Niekerk traded all his possessions for an 83.5 carat stone owned by the Griqua Shepard, Zwartboy, Sir Richard Southey, Colonial Secretary of the Cape, declared with some justification: “This is the rock on which the future of South Africa will be built.” For us, The Star of South Africa, as the gem became known, shines not in the East, but in the Northern Cape. (Tourism Blueprint, 2006) 2 – WildlifeCampus Cultural Guiding Course – Northern Cape Module # 1 - Province Overview Component # 1 - Northern Cape Province Overview Module # 2 - Cultural Overview Component # 1 - Northern Cape Cultural Overview Module # 3 - Historical Overview Component # 1 - Northern Cape Historical Overview Module # 4 - Wildlife and Nature Conservation Overview Component # 1 - Northern Cape Wildlife and Nature Conservation Overview Module # 5 - Namaqualand Component # 1 - Namaqualand Component # 2 - The Hantam Karoo Component # 3 - Towns along the N14 Component # 4 - Richtersveld Component # 5 - The West Coast Module # 5 - Karoo Region Component # 1 - Introduction to the Karoo and N12 towns Component # 2 - Towns along the N1, N9 and N10 Component # 3 - Other Karoo towns Module # 6 - Diamond Region Component # 1 - Kimberley Component # 2 - Battlefields and towns along the N12 Module # 7 - The Green Kalahari Component # 1 – The Green Kalahari Module # 8 - The Kalahari Component # 1 - Kuruman and towns along the N14 South and R31 Northern Cape Province Overview This course material is the copyrighted intellectual property of WildlifeCampus. It may not be copied, distributed or reproduced in any format whatsoever without the express written permission of WildlifeCampus. 3 – WildlifeCampus Cultural Guiding Course – Northern Cape Module 1 - Component 1 Northern Cape Province Overview Introduction Diamonds certainly put the Northern Cape on the map, but it has far more to offer than these shiny stones. -
Nc Travelguide 2016 1 7.68 MB
Experience Northern CapeSouth Africa NORTHERN CAPE TOURISM AUTHORITY Tel: +27 (0) 53 832 2657 · Fax +27 (0) 53 831 2937 Email:[email protected] www.experiencenortherncape.com 2016 Edition www.experiencenortherncape.com 1 Experience the Northern Cape Majestically covering more Mining for holiday than 360 000 square kilometres accommodation from the world-renowned Kalahari Desert in the ideas? North to the arid plains of the Karoo in the South, the Northern Cape Province of South Africa offers Explore Kimberley’s visitors an unforgettable holiday experience. self-catering accommodation Characterised by its open spaces, friendly people, options at two of our rich history and unique cultural diversity, finest conservation reserves, Rooipoort and this land of the extreme promises an unparalleled Dronfield. tourism destination of extreme nature, real culture and extreme adventure. Call 053 839 4455 to book. The province is easily accessible and served by the Kimberley and Upington airports with daily flights from Johannesburg and Cape Town. ROOIPOORT DRONFIELD Charter options from Windhoek, Activities Activities Victoria Falls and an internal • Game viewing • Game viewing aerial network make the exploration • Bird watching • Bird watching • Bushmen petroglyphs • Vulture hide of all five regions possible. • National Heritage Site • Swimming pool • Self-drive is allowed Accommodation The province is divided into five Rooipoort has a variety of self- Accommodation regions and boasts a total catering accommodation to offer. • 6 fully-equipped • “The Shooting Box” self-catering chalets of six national parks, including sleeps 12 people sharing • Consists of 3 family units two Transfrontier parks crossing • Box Cottage and 3 open plan units sleeps 4 people sharing into world-famous safari • Luxury Tented Camp destinations such as Namibia accommodation andThis Botswanais the world of asOrange well River as Cellars. -
1. the Historic Copper Mine Route
4. The Pilgrimage Route On this route tourists can visit several churches and missionary stations in the Namakwa area that were established by the Rhenish Mission Society, 1. The Historic Copper Mine Route the London Mission Society, the Church of England, the Roman Catholic Church, the Methodist Church, the Jewish Society and many other church This is a self-drive tour through the region’s historic copper mining towns. The copper mining history dates back to 1685 when Simon van der organisations. These church organisations established both churches and schools in the area and contributed greatly to education and religion in the 7. The Museum Route Stel’s search for gold led him to discover copper at Carolusberg. Commercial copper mining commenced in 1852 and drew to a close in 2004. area. The pastors in charge of these churches also assisted in the negotiations for land and other rights for the local communities. The museums exhibit the historical and cultural lifestyles of the people of the area. The detailed exhibits and information keep tourists occupied for hours. The Okiep Copper Company (OCC), or “Jan Komponie” as the locals referred to it, was once a well-known industry leader in the copper mining We trust that you will be inspired by the relics and remains of the past decades which strived to preserve and develop religion in our communities. sector. This route will take you on a journey through Carolusberg, Springbok, Concordia, Okiep, Alexander Bay, Hondeklip Bay and Nababeep. Town Tourist Attractions We trust that your copper mining town experience will be one to remember. -
WEST COAST RESOURCES STEPS IT up Almost Two Years Have
WEST COAST RESOURCES STEPS IT UP Almost two years have passed since West Coast Resources acquired mining rights in the Namaqualand region of the Northern Cape and the Company has indeed made the most of that time. With mining operations underway and the staff complement steadily increasing, an exciting time lies ahead. Mining operations Construction of the Michells Bay production plant was completed towards the end of 2015. The 50 tons/hour DMS plant was commissioned in November, followed by the washing and screening plant in December. Mining operations also started in December in the Langklip area and as at 31 March 2016, initial production for the mine totalled 24 930 carats. Mining activities for the remainder of the year will focus on the Langklip area and sections of the Koingnaas area. Job creation As at the end of May 2016, the Company had created 166 permanent jobs and 24 part-time employees were employed as a result of the Company’s operations. West Coast Resources plans to create approximately 686 jobs, directly and indirectly, by 2020. 91% of all West Coast Resources employees comprise local residents originating from the nearby communities of, amongst others, Kommagas, Kleinzee, Nababeep, Concordia, Okiep, Koingnaas, Buffelsrivier, Hondeklip Bay and Soebatsfontein. 26% of the employees are 25 years old or younger, and 13% are women. The first phase of the Company’s trainee programme resulted in the permanent appointment of 20 young local matriculants, with no work experience, as trainees. These employees receive continuous on-the-job training, coaching and mentoring. In addition, they have attended work readiness training, legal compliance training and Code 10 driver’s licence training. -
Annual Report 2008/09
ANNUAL REPORT 2008/09 In terms of section 46 of the Municipal Systems Act and Section 121 of the Municipal Finance Management Act TABLE OF CONTENTS CHAPTER 1 - INTRODUCTION AND OVERVIEW ___________________________________________________________________________ 3 1.1 MAYOR’S FOREWORD .................................................................................................................................................................................................................. 4 1.2 OVERVIEW OF NAMA KHOI MUNICIPALITY ......................................................................................................................................................................... 5 1.3 EXECUTIVE SUMMARY ................................................................................................................................................................................................................... 6 CHAPTER 2 - PERFORMANCE HIGHLIGHTS ______________________________________________________________________________ 16 2.1 OFFICE OF THE MUNICIPAL MANAGER ................................................................................................................................................................................16 2.2 DEPARTMENT COMMUNITY SERVICES .................................................................................................................................................................................49 2.3 DEPARTMENT FINANCIAL SERVICES .....................................................................................................................................................................................72 -
The O'okiep Copper District, Namaqualand, South Africa: a Review of the Geology with Emphasis on the Petrogenesis of the Cupriferous Koperberg Suite
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/257331111 The O'okiep Copper District, Namaqualand, South Africa: A review of the geology with emphasis on the petrogenesis of the cupriferous Koperberg Suite Article in Mineralium Deposita · December 2012 DOI: 10.1007/s00126-012-0403-x CITATIONS READS 17 533 2 authors, including: Erika Barton Nelson Mandela University 35 PUBLICATIONS 798 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Regional geololgy View project All content following this page was uploaded by Erika Barton on 24 August 2020. The user has requested enhancement of the downloaded file. Miner Deposita DOI 10.1007/s00126-012-0403-x ARTICLE The O’okiep Copper District, Namaqualand, South Africa: a review of the geology with emphasis on the petrogenesis of the cupriferous Koperberg Suite Tom N. Clifford & Erika S. Barton Received: 26 April 2011 /Accepted: 18 January 2012 # Springer-Verlag 2012 Abstract The O’okiep Copper District is the oldest formal ore) that, in a number of ore-bodies, has been inverted mining area in South Africa. Between 1852 and 2002, the under upper amphibolite facies conditions to bornite+Ti- 2,500-km2 area yielded two million tons of copper from 32 free magnetite (Carolusberg-type ore). Meteoric fluids mines ranging in ore tonnages from 140,000 to 37 million resulted in supergene Cu enrichment in Koperberg bodies tons. This paper summarizes the calendar of events from the to ~500 m below the pre-Nama peneplane, and lower formation of the first primitive crust 1,700–2,000 Ma ago to greenschist facies metamorphism 500–570 Ma ago is early Cambrian times ~500 Ma ago, with particular empha- reflected by inter alia Hoits-type ore bearing second- sis on the Namaquan (Grenville) Orogeny, notably: the generation bornite+chalcopyrite(±covellite±chalcocite). -
THE ECONOMIC GEOLOGY of the OKIEP COPPER DEPOSITS, NAMAQUALAND, SOUTH AFRICA. This Dissertation Was Prepared in Accordance With
v THE ECONOMIC GEOLOGY OF THE OKIEP COPPER DEPOS ITS, NAMAQUALAND, SOUTH AFRICA . D. L. GADD-CLAXTON ~issertation submitted in partial fulfilment of the requirements for the degree of Master of Science (Mineral Exploration) at Rhodes University, Graha~stown. JANUARY 1981. This dissertation was prepared in accordance with specifications laid down by the University and was completed within a period of ten weeks full-time study. ABSTRACT The Okiep Copper District situated in the north-western Cape Pro- 2 vince, covers some 3 000 km and is the oldest mining area in the Re- public of South Africa. The Q'okiep Copper Company Limited commenced production in 1940 with a proven ore reserve of 9 million tons at 2,45 % cu. Production since 1940 and present ore reserves total some 93 million tonnes at 1,08 % Cu. The rocks comprising the Okiep Copper District are of Proterozoic age and have been subdivided into a meta-volcanosedimentary succession, intruded by various sub-horizontally emplaced granitoid intrusions. The various intrusions occurred at different stages relative to the main structural and metamorphic events. The copper deposits are confined to basic rocks which are the youngest major group of intrusives in the Dis trict. They occur as swarms of generally easterly-trending, steep north dipping, irregular dyke-like bodies consisting of diorite, anorthosite and norite. The dominant silicate constituents are andesite ranging to labradorite, hypersthene, biotite and phlogopite. Copper sulphides are preferentially associated with the more basic varieties. The copper sulphides are mainly chalcopyrite, bornite and subsidiary chalcocite. The copper content of the basic rocks is erratic ranging over small dis tances from a mere trace to several percent. -
Assessment and Eva Ecosystem Service Succulent Karoo
Assessment and Evaluation of Ecosystem Services in the Succulent Karoo Biome Prepared by the South African National Biodiversity Institute, with the support of the Critical Ecosystem Partnership Programme, for the Succulent Karoo Ecosystem Programme June 2009 ASSESSMENT AND EVALUATION OF ECOSYSTEM SERVICES IN THE SUCCULENT KAROO BIOME Report prepared for the Succulent Karoo Ecosystem Programme (SKEP) Coordination Unit Prepared by: the Council for Scientific and Industrial Research (CSIR). Authors: David Le Maitre, Patrick O’Farrell, Sue Milton, Doreen Atkinson, Willem De Lange, Benis Egoh, Belinda Reyers, Christine Colvin, Ashton Maherry and James Blignaut (2009) Assessment and evaluation of ecosystem services in the Succulent Karoo biome Executive summary What are ecosystem services? Within our landscapes there are innumerable interactions between species, their environment, and one another, going on at any one time. Some of these interactions are especially useful to people, supporting life and livelihoods in a variety of ways. These include the provision of oxygen to breathe and clean water to drink, fertile soils for our crops, the pollination of fruit and vegetables that we eat and even the provision of aesthetic beauty. The benefits we get from our ecosystems we collectively call ecosystem services. How we use and manage our landscapes influences the quality and the quantity of the ecosystem services that they in turn provide to us. Focus on the Succulent Karoo The focus of this study was on assessing the benefits of ecosystem services provided by the Succulent Karoo biome to the inhabitants of the region and elsewhere. The Succulent Karoo, situated in western South Africa, is a semi-arid area that has been globally recognised as extremely conservation worthy given the exceptional diversity of plants, reptiles, insects, birds and mammals – which make it the most diverse arid area in the world. -
The Geology of the Area South of Vioolsdrif, Cape Province
'•"•"••••••"ii.lii.u.......... PEL 257 THE GEOLOGY OF THE AREA SOUTH OF VIOOLSDRIF, CAPE PROVINCE by J.H.W. WARD ATOMIC ENERGY BOARD Pelindaba PRETORIA Republic of South Africa October 1977 3 ill lilllli •Hin!!ffl!J vlHiiR PEL-257 - 1 ATOMIC ENERGY BOARD THE GEOLOGY OF THE AREA SOUTH OF VIOOLSDRIF, CAPE PROVINCE by J.H.W. WARD* *BURSAR ADDRESS. Chamber of Mines Precambrian Research Unit Pelindaba Department of Geology October 1977 University of Cape Town ISBN 0 S6960 670 0 PEL 257 - 2 CONTENTS Page ACKNOWLEDGEMENT 3 SAMEVATHNG 3 ABSTRACT 3 1. INTRODUCTION 4 1.1 Physiographic introduction 4 1.2 Geological examination 4 1.2.1 Reports 4 1.2.2 Maps 5 2. NAMAQUALAND MET AMORPHIC COMPLEX 5 2.1 Quartzite 5 2.2 Amphibolite 5 2.3 Cordierite anthophyllite rock 6 2.4 Biotite gneiss and migmatite 6 2.5 Cordierite-sillimanite schists and migmatite 7 2.6 Biotite-cordierite-garnet-staurolite-andalusite-sillimanite rock 7 2.7 Calc-silicate rocks 8 2.8 Leptite 8 2.9 Hornblende gneiss 8 3. ORANGE RIVER GROUP 9 3.1 Haib Subgroup 9 3.1.1 Nous Formation 9 3.1.2 Tsams Formation 10 4. MAFIC INTRUSIVES 11 5. VIOOLSDRIF PLUTONIC COMPLEX 12 5.1 Introduction 12 5.2 Granodiorite 12 5.3 Porphyritic adamellite 14 5.4 Aplogranite 14 6. APLOGRANITIC GNEISS 15 6.1 Aplogranitic gneiss 15 6.2 Pink granitic gneiss 15 7. PEGMATITES 15 8. DYKES 17 8.1 Mafic dykes 17 8.2 Felsic dykes 17 9. THERMOTECTONIC HISTORY 17 9.1 Introduction 17 9.2 Tectonic Provinces in Namaqualand 18 9.3 Structure 19 9.3.1 Introduction 19 9.3.2 Primary tectonic fabric 19 9.3.3 Secondary tectonic fabric 23 9.3.4 Metamorphism 24 9.3.5 Conclusions 29 10. -
Hydrothermal Alteration at the Haib Porphyry Copper Deposit, Namibia: Stable Isotope and Fluid Inclusion Patterns
Communs geol. Surv. Namibia, 8 (1992/93), 23-35 Hydrothermal alteration at the Haib porphyry copper deposit, Namibia: Stable isotope and fluid inclusion patterns J.M. Barr and D.L. Reid Department of Geochemistry, University of Cape Town, Rondebosch 7700, Cape Town, RSA Porphyry-type copper mineralisation is developed in a quartz-feldspar porphyry pluton of the 1900-1730 Ma Vioolsdrif Intrusive Suite, which crops out near the lower Orange River in southern Namibia. Petrographic evidence for hydrothermal alteration is widespread, but most intense in a zone near the central part of the elongate porphyry body. Both the porphyry and metavolcanic country rocks are affected. Potassic alteration that often characterises Phanerozoic porphyry-type copper mineralisation is difficult to distinguish in the Haib deposit because of the high-K nature of the calc-alkaline host rocks. Stable isotope patterns indicate deple- tion in 18O (represented by low δ18O whole rock and mineral values) and deuterium (low δD values) during hydrothermal alteration, which suggests the introduction and circulation of heated meteoric fluids. Preliminary studies have identified two types of fluid, an early high-salinity high-temperature fluid trapped in primary inclusions, and a late-stage low-temperature low-salinity fluid trapped as secondary inclusions in healed fractures. Introduction several university-based research programs to run con- currently with exploration (Blignault, 1977; Reid, 1977; Copper in the Haib River area of southern Namibia Minnitt, 1979). These research results confirmed earlier (Fig. 1) was probably worked, like the richer Okiep de- assessments that the Haib deposit represented a well- posits further south in Namaqualand, in pre-European preserved Precambrian example of an important class times (Smalberger, 1975). -
Northern Cape Proposed Main Seat / Sub District
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