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South Africa – Cape Restaurants
Recommended Restaurants – Johannesburg and Pretoria JOHANNESBURG AFRICAN CUISINE ITALIAN/MEDITERRANEAN Moyo - Melrose Arch 2 Medeo Restaurant at The Palazzo 13 Moyo - Zoo Lake 2 La Cucina Di Ciro 14 Pronto 14 ASIAN Café del Sol Botanico 15 Kong Roast 3 The Lotus Teppanyaki & Sushi Bar 3 STEAKHOUSE Wombles Steakhouse Restaurant 15 BISTRO Turn 'n' Tender Illovo 16 Eatery JHB 4 Coobs 4 CONTEMPORARY Cube Tasting Kitchen 5 PRETORIA Winehouse - Ten Bompas 5 CONTEMPORARY Level Four Restaurant 6 Blu Saffron 16 March Restaurant 6 De Kloof Restaurant 17 Roots at Forum Homini - Prosopa Waterkloof Muldersdrift 7 17 FINE DINING FINE DINING Luke Dale Roberts X (Saxon Hotel) 7 Kream 18 DW Eleven-13 8 Restaurant Mosaic at The Orient 18 Signature Restaurant 8 Pigalle - Michelangelo Towers 9 Pigalle - Melrose Arch 9 oneNINEone 10 AtholPlace Restaurant 10 The Residence 11 FRENCH Emoyeni 11 Le Souffle 12 INDIAN Ghazal 12 Vikrams 13 1 **To make early reservations, please contact your AAC consultant, the hotel concierge or the restaurant directly.** JOHANNESBURG AFRICAN CUISINE MOYO (Melrose Arch) Shop 5, The High St / Tel: +27 11 684 1477 http://www.moyo.co.za/moyo-melrose-arch/ From the food and décor to the music and live entertainment, moyo is strongly African in theme. The focus of the rich and varied menu is pan-African, incorporating tandoori cookery from northern Africa, Cape Malay influences and other dishes representing South Africa. In the heart of Johannesburg, the 350-seater, multi-level modern restaurant – clad in copper with pressed pebble walls - embodies Africa’s finest music and urban cuisine offerings. -
Maloti-Drakensberg Park, Lesotho & South Africa
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Maloti-Drakensberg Park - 2020 Conservation Outlook Assessment Maloti-Drakensberg Park 2020 Conservation Outlook Assessment SITE INFORMATION Country: Lesotho, South Africa Inscribed in: 2000 Criteria: (i) (iii) (vii) (x) The Maloti-Drakensberg Park is a transboundary site composed of the uKhahlamba Drakensberg National Park in South Africa and the Sehlathebe National Park in Lesotho. The site has exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts as well as visually spectacular sculptured arches, caves, cliffs, pillars and rock pools. The site's diversity of habitats protects a high level of endemic and globally important plants. The site harbors endangered species such as the Cape vulture (Gyps coprotheres) and the bearded vulture (Gypaetus barbatus). Lesotho’s Sehlabathebe National Park also harbors the Maloti minnow (Pseudobarbus quathlambae), a critically endangered fish species only found in this park. This spectacular natural site contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. They represent the spiritual life of the San people, who lived in this area over a period of 4,000 years. © UNESCO SUMMARY 2020 Conservation Outlook Finalised on 01 Dec 2020 SIGNIFICANT CONCERN The conservation outlook for Maloti-Drakensberg Park is of significant concern. The EKZNW management staff are highly dedicated and experienced and there is also significant appreciation for the values of the Maloti Drakensberg by communities living nearby as evidenced, for example, by the vehemently strong opposition to the possibility of oil and gas exploration in the area. -
NASCA Human and Social Sciences
HUMAN AND SOCIAL SCIENCES Department Higher Education and Training 123 Francis Baard Street Private Bag X174 Pretoria, 0001 South Africa Tel: +27 12 312 5911 103 Plein Street, ParliamentCape Town OfficeTowers Private Bag X9192 Cape Town, 8000 Tel: +27 021 469 5175 Fax: +27 021 461 4761 Website: www.dhet.gov.za Design and Layout by: Mzelers Media. www.mzelers.com ISBN: 978-1-77018-792-4 HUMAN AND SOCIAL SCIENCES CONTENTS PAGE Introduction 3 Exit-Level Outcomes 3 Approaches to Teaching and Learning 3 Assumptions About Prior Knowledge and Skills 3 Part 1 - Geography 4 What is Geography? 4 Assessment Objectives 4 Specific Aims of Geography 4 Weighting of Levels of Cognitive Demand 5 Content Outline 6 General Geographic Techniques 6 Theme 1 - Physical Geography 11 Theme 2 - Human Geography 15 Part 2 - History 19 What is History? 19 Assessment Objectives 19 Specific Aims of History 19 Weighting of Levels of Cognitive Demand 20 Scheme of Assessment 20 Content Outline 21 Theme 1 - Cold War 22 Theme 2 - Independent Africa 1960s-1970s 23 Theme 3 - Civil Resistance in South Africa 1970s-1980s 23 Theme 4 - Coming of Democracy to South Africa 24 Recommended Study Hours for Human and Social Sciences 25 Glossary of Terms Used in Human and Social Sciences 25 Bibliography 26 HUMAN AND SOCIAL SCIENCES Introduction Human and Social Sciences aims to introduce students to a world beyond their everyday realities. It includes programmes that provide for the study of people, places, environments, culture, time continuity, change, individual identity, individual groups and institutions, power, authority, governance and civic ideals and practices. -
Predicting Wetland Occurrence in the Arid to Semi— Arid 1 Interior of the Western Cape, South Africa, for Improved 2 Mapping and Management
Predicting Wetland Occurrence in the Arid to Semi— Arid 1 Interior of the Western Cape, South Africa, for Improved 2 Mapping and Management Donovan Charles Kotze ( [email protected] ) University of KwaZulu-Natal https://orcid.org/0000-0001-9048-1773 Nick Rivers-Moore University of KwaZulu-Natal Michael Grenfell University of the Western Cape Nancy Job South African National Biodiversity Institute Research Article Keywords: drylands, hydrogeomorphic type, logistic regression, probability, vulnerability Posted Date: August 17th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-716396/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License 1 Predicting wetland occurrence in the arid to semi—arid 2 interior of the Western Cape, South Africa, for improved 3 mapping and management 4 5 D. C. Kotze1*, N.A. Rivers-Moore1,2, N. Job3 and M. Grenfell4 6 1Centre for Water Resources Research, University of KwaZulu-Natal, Private Bag X01, 7 Scottsville, 3209, South Africa 8 2Freshwater Research Centre, Cape Town, South Africa 9 3Kirstenbosch Research Centre, South African National Biodiversity Institute, Private Bag X7, 10 Newlands, Cape Town, 7945, South Africa 11 4Institute for Water Studies, Department of Earth Science, University of the Western Cape, 12 Private Bag X17, Bellville, 7535, South Africa 13 *Corresponding author: [email protected] 14 15 Abstract 16 As for drylands globally, there has been limited effort to map and characterize such wetlands in 17 the Western Cape interior of South Africa. Thus, the study assessed how wetland occurrence and 18 type in the arid to semi-arid interior of the Western Cape relate to key biophysical drivers, and, 19 through predictive modelling, to contribute towards improved accuracy of the wetland map layer. -
Lesotho Fourth National Report on Implementation of Convention on Biological Diversity
Lesotho Fourth National Report On Implementation of Convention on Biological Diversity December 2009 LIST OF ABBREVIATIONS AND ACRONYMS ADB African Development Bank CBD Convention on Biological Diversity CCF Community Conservation Forum CITES Convention on International Trade in Endangered Species CMBSL Conserving Mountain Biodiversity in Southern Lesotho COP Conference of Parties CPA Cattle Post Areas DANCED Danish Cooperation for Environment and Development DDT Di-nitro Di-phenyl Trichloroethane EA Environmental Assessment EIA Environmental Impact Assessment EMP Environmental Management Plan ERMA Environmental Resources Management Area EMPR Environmental Management for Poverty Reduction EPAP Environmental Policy and Action Plan EU Environmental Unit (s) GA Grazing Associations GCM Global Circulation Model GEF Global Environment Facility GMO Genetically Modified Organism (s) HIV/AIDS Human Immuno Virus/Acquired Immuno-Deficiency Syndrome HNRRIEP Highlands Natural Resources and Rural Income Enhancement Project IGP Income Generation Project (s) IUCN International Union for Conservation of Nature and Natural Resources LHDA Lesotho Highlands Development Authority LMO Living Modified Organism (s) Masl Meters above sea level MDTP Maloti-Drakensberg Transfrontier Conservation and Development Project MEAs Multi-lateral Environmental Agreements MOU Memorandum Of Understanding MRA Managed Resource Area NAP National Action Plan NBF National Biosafety Framework NBSAP National Biodiversity Strategy and Action Plan NEAP National Environmental Action -
Overview of Experiences in the Limpopo River Basin
intersectorai Management of River Basins Overview of Experiences in the Limpopo River Basin Thomas Schild Team Leader, German Agency for Technical Co-operation (GTZ), Windhoek, Namibia Abstract The paper presents a summary of the findings of a German mission to four countries of Southern Africa, in which many people at different levels were asked to give their views about water issues in two trans-national river basins, the Limpopo and the Orange-Senqu. The principal common factors in people's responses are identified. Various sources and types of inequity are described. In conclusion, it is found that external assistance could be especially useful in areas of information and communication, and in organisational development for river-basin management. 1. Context A mission by a project appraisal team of the German Agency for Technical Co operation (GTZ) was carried out in September 2000, for the support of regional water management in the SADC (Southern African Development Community) region. The team talked to stakeholders of the Limpopo and the Orange-Senqu river basins. The mission had the following major tasks; Map the scene; Capture the expectations and issues of concern of the stakeholders with regard to the establishment of river basin commissions; Identify possible areas for technical co-operation; Make preparations for the planning workshop. 2. Procedures Between 14 and 29 September 2000, the group visited Zimbabwe, Mozambique, Botswana and South Africa and held discussions with relevant government institutions, parastatals and donor organisations involved in water resources management of the Limpopo and, where applicable, of the Orange/Senqu. Other resource persons, such as representatives of water users' organisations, researchers, non-governmental organisations (NGOs) and consultants were met. -
Early History of South Africa
THE EARLY HISTORY OF SOUTH AFRICA EVOLUTION OF AFRICAN SOCIETIES . .3 SOUTH AFRICA: THE EARLY INHABITANTS . .5 THE KHOISAN . .6 The San (Bushmen) . .6 The Khoikhoi (Hottentots) . .8 BLACK SETTLEMENT . .9 THE NGUNI . .9 The Xhosa . .10 The Zulu . .11 The Ndebele . .12 The Swazi . .13 THE SOTHO . .13 The Western Sotho . .14 The Southern Sotho . .14 The Northern Sotho (Bapedi) . .14 THE VENDA . .15 THE MASHANGANA-TSONGA . .15 THE MFECANE/DIFAQANE (Total war) Dingiswayo . .16 Shaka . .16 Dingane . .18 Mzilikazi . .19 Soshangane . .20 Mmantatise . .21 Sikonyela . .21 Moshweshwe . .22 Consequences of the Mfecane/Difaqane . .23 Page 1 EUROPEAN INTERESTS The Portuguese . .24 The British . .24 The Dutch . .25 The French . .25 THE SLAVES . .22 THE TREKBOERS (MIGRATING FARMERS) . .27 EUROPEAN OCCUPATIONS OF THE CAPE British Occupation (1795 - 1803) . .29 Batavian rule 1803 - 1806 . .29 Second British Occupation: 1806 . .31 British Governors . .32 Slagtersnek Rebellion . .32 The British Settlers 1820 . .32 THE GREAT TREK Causes of the Great Trek . .34 Different Trek groups . .35 Trichardt and Van Rensburg . .35 Andries Hendrik Potgieter . .35 Gerrit Maritz . .36 Piet Retief . .36 Piet Uys . .36 Voortrekkers in Zululand and Natal . .37 Voortrekker settlement in the Transvaal . .38 Voortrekker settlement in the Orange Free State . .39 THE DISCOVERY OF DIAMONDS AND GOLD . .41 Page 2 EVOLUTION OF AFRICAN SOCIETIES Humankind had its earliest origins in Africa The introduction of iron changed the African and the story of life in South Africa has continent irrevocably and was a large step proven to be a micro-study of life on the forwards in the development of the people. -
The Poetic Utilization of Dialectal Varieties of the Afrikaans Language for Strategic Purposes in the Southern African Context
Bernard J. Odendaal The Poetic Utilization of Dialectal Varieties of the Afrikaans Language for Strategic Purposes in the Southern African Context Abstract: Afrikaans is a southern African language named after the continent on which it has evolved from seventeenth-century Dutch in a complex contact situa- tion between European settlers, their imported slaves, and indigenous peoples. It was standardized in the late nineteenth and early twentieth centuries for literary purposes, among others. The poetic utilization of dialectal or colloquial varieties of Afrikaans, however, has been an important trend in its literary history, espe- cially since the advent of the so-called Movement of the 1960s. The relevant vari- eties include geolects like Karoo Afrikaans, but also sociolects like “Loslitafri- kaans” (informal Afrikaans, characterized by being mixed with English), Cape Afrikaans, and Griqua Afrikaans. As a stylistic device, the use of dialectal Afri- kaans has served both literary-strategic purposes (literary renewal) and socio-po- litical aims (as actuality literature or socio-politically engaged poetry). As a whole, it transpires that the pressing socio-political and broader cultural condi- tions that have dictated past developments, or are driving present ones, in South and southern Africa (resistance to nineteenth-century efforts at anglicizing south- ern Africa, the advent and decline of Apartheid, the increasingly hegemonic posi- tion of English in the post-Apartheid dispensation) loom large behind the relative importance of this trend in Afrikaans poetry. Keywords: actuality, Afrikaans geolects and sociolects, socio-political and cultur- al conditions, socio-political engagement, strategic poetic utilization, stylistic re- newal 1 Introductory notes on the origins of the Afrikaans language and literature Afrikaans is a southern African language, named after the continent on which it originated. -
Upper Mantle P and S Wave Velocity Structure of the Kalahari Craton And
RESEARCH LETTER Upper Mantle P and S Wave Velocity Structure of the 10.1029/2019GL084053 Kalahari Craton and Surrounding Proterozoic Key Points: • Thick cratonic lithosphere extends Terranes, Southern Africa beneath the Rehoboth Province and Kameron Ortiz1, Andrew Nyblade1,5 , Mark van der Meijde2, Hanneke Paulssen3 , parts of the northern Okwa Terrane 4 4 5 2,6 and Magondi Belt Motsamai Kwadiba , Onkgopotse Ntibinyane , Raymond Durrheim , Islam Fadel , • The northern edge of the greater and Kyle Homman1 Kalahari Craton lithosphere lies along the northern boundary of the 1Department of Geosciences, Pennsylvania State University, University Park, PA, USA, 2Faculty for Geo‐information Rehoboth Province and Magondi Science and Earth Observation (ITC), University of Twente, Enschede, Netherlands, 3Department of Earth Sciences, Belt 4 • Cratonic mantle lithosphere Faculty of Geosciences, Utrecht University, Utrecht, Netherlands, Botswana Geoscience Institute, Lobatse, Botswana, 5 6 beneath the Okwa Terrane and School of Geosciences, The University of the Witwatersrand, Johannesburg, South Africa, Geology Department, Faculty Magondi Belt may have been of Science, Helwan University, Ain Helwan, Egypt chemically altered by Proterozoic magmatic events Abstract New broadband seismic data from Botswana and South Africa have been combined with Supporting Information: existing data from the region to develop improved P and S wave velocity models for investigating the • Supporting Information S1 upper mantle structure of southern Africa. Higher craton‐like velocities are imaged beneath the Rehoboth Province and parts of the northern Okwa Terrane and the Magondi Belt, indicating that the Correspondence to: northern edge of the greater Kalahari Craton lithosphere lies along the northern boundary of these A. Nyblade, terranes. -
Pinnacle Point Cave 13B (Western Cape Province, South Africa) in Context: the Cape Floral Kingdom, Shellfish, and Modern Human Originsq
Journal of Human Evolution 59 (2010) 425e443 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol Pinnacle Point Cave 13B (Western Cape Province, South Africa) in context: The Cape Floral kingdom, shellfish, and modern human originsq Curtis W. Marean Institute of Human Origins, School of Human Evolution and Social Change, P.O. Box 872402, Arizona State University, Tempe, AZ 85287-2402, USA article info abstract Article history: Genetic and anatomical evidence suggests that Homo sapiens arose in Africa between 200 and 100 ka, Received 15 December 2009 and recent evidence suggests that complex cognition may have appeared between w164 and 75 ka. This Accepted 19 March 2010 evidence directs our focus to Marine Isotope Stage (MIS) 6, when from 195e123 ka the world was in a fluctuating but predominantly glacial stage, when much of Africa was cooler and drier, and when dated Keywords: archaeological sites are rare. Previously we have shown that humans had expanded their diet to include Middle Stone Age marine resources by w164 ka (Æ12 ka) at Pinnacle Point Cave 13B (PP13B) on the south coast of South Mossel Bay Africa, perhaps as a response to these harsh environmental conditions. The associated material culture Origins of modern humans documents an early use and modification of pigment, likely for symbolic behavior, as well as the production of bladelet stone tool technology, and there is now intriguing evidence for heat treatment of lithics. PP13B also includes a later sequence of MIS 5 occupations that document an adaptation that increasingly focuses on coastal resources. -
Corrosion Map of South Africa's Macro Atmosphere
Corrosion map of South Africa’s macro atmosphere AUTHORS: Darelle T. Janse van Rensburg1,2 The first atmospheric corrosion map of South Africa, produced by Callaghan in 1991, has become outdated, Lesley A. Cornish1 because it primarily focuses on the corrosivity of coastal environments, with little differentiation given Josias van der Merwe1 concerning South Africa’s inland locations. To address this problem, a study was undertaken to develop AFFILIATIONS: a new corrosion map of the country, with the emphasis placed on providing greater detail concerning 1School of Chemical and Metallurgical South Africa’s inland regions. Here we present this new corrosion map of South Africa’s macro atmosphere, Engineering and DST-NRF Centre of Excellence in Strong Materials, based on 12-month corrosion rates of mild steel at more than 100 sites throughout the country. Assimilations University of the Witwatersrand, and statistical analyses of the data (published, unpublished and new) show that the variability in the corrosion Johannesburg, South Africa rate of mild steel decreases significantly moving inland. Accordingly, the average first-year corrosion rate of 2Orytech (Pty) Ltd, Roodepoort, South Africa mild steel at the inland sites (at all corrosion monitoring spots located more than 30 km away from the ocean) measured 21±12 µm/a [95% CI: 18–23 µm/a]. The minimum inland figure was about 1.3 µm/a (recorded CORRESPONDENCE TO: at Droërivier in the Central Karoo) and the maxima were approximately 51 µm/a and 50 µm/a in the industrial Darelle Janse van Rensburg hearts of Germiston (Gauteng) and Sasolburg (Free State), respectively. -
Case Study of Mazowe Catchment, Zimbabwe
Water quality and sediment transport issues in surface water Proc. IAHS, 377, 57–66, 2018 https://doi.org/10.5194/piahs-377-57-2018 Open Access © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Sedimentation and Its Impacts/Effects on River System and Reservoir Water Quality: case Study of Mazowe Catchment, Zimbabwe Colleta Tundu1, Michael James Tumbare2, and Jean-Marie Kileshye Onema3 1Zimbabwe National Water Authority, P.O. Box Cy617 Causeway, Harare, Zimbabwe 2Department of Civil Engineering, University of Zimbabwe, P.O. Box MP167, Mt Pleasant, Harare, Zimbabwe 3WaterNet Secretariat, P.O. Box MP600, Mount Pleasant, Harare, Zimbabwe Correspondence: Colleta Tundu ([email protected]) Received: 7 June 2017 – Accepted: 10 October 2017 – Published: 16 April 2018 Abstract. Sediment delivery into water sources and bodies results in the reduction of water quantity and quality, increasing costs of water purification whilst reducing the available water for various other uses. The paper gives an analysis of sedimentation in one of Zimbabwe’s seven rivers, the Mazowe Catchment, and its impact on water quality. The Revised Universal Soil Loss Equation (RUSLE) model was used to compute soil lost from the catchment as a result of soil erosion. The model was used in conjunction with GIS remotely sensed data and limited ground observations. The estimated annual soil loss in the catchment indicates soil loss ranging from 0 to 65 t ha yr−1. Bathymetric survey at Chimhanda Dam showed that the capacity of the dam had reduced by 39 % as a result of sedimentation and the annual sediment deposition into Chimhanda Dam was estimated to be 330 t with a specific yield of 226 t km−2 yr−1.