National Water Resource Strategy First Edition, September 2004 ______
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THE CASE of NDUMO GAME RESERVE, SOUTH AFRICA By
FINDING THE COMMUNITY IN COMMUNITY-BASE NATURAL RESOURCE MANAGEMENT: THE CASE OF NDUMO GAME RESERVE, SOUTH AFRICA by Talia Meer Submitted in partial fulfilment of the requirements for the degree of Master of Arts at Dalhousie University Halifax, Nova Scotia August 2010 © Copyright by Talia Meer, 2010 DALHOUSIE UNIVERSITY DEPARTMENT OF INTERNATIONAL DEVELOPMENT STUDIES The undersigned hereby certify that they have read and recommend to the Faculty of Graduate Studies for acceptance a thesis entitled “FINDING THE COMMUNITY IN COMMUNITY-BASE NATURAL RESOURCE MANAGEMENT: THE CASE OF NDUMO GAME RESERVE, SOUTH AFRICA” by Talia Meer in partial fulfilment of the requirements for the degree of Master of Arts. Dated: 18 August 2010 Supervisor: _________________________________ Readers: _________________________________ _________________________________ Departmental Representative: _________________________________ ii DALHOUSIE UNIVERSITY DATE: 18 August 2010 AUTHOR: Talia Meer TITLE: FINDING THE COMMUNITY IN COMMUNITY-BASE NATURAL RESOURCE MANAGEMENT: THE CASE OF NDUMO GAME RESERVE, SOUTH AFRICA DEPARTMENT OR SCHOOL: Department of International Development Studies DEGREE: MA CONVOCATION: October YEAR: 2010 Permission is herewith granted to Dalhousie University to circulate and to have copied for non-commercial purposes, at its discretion, the above title upon the request of individuals or institutions. _______________________________ Signature of Author The author reserves other publication rights, and neither the thesis nor extensive extracts from it may be printed or otherwise reproduced without the author’s written permission. The author attests that permission has been obtained for the use of any copyrighted material appearing in the thesis (other than the brief excerpts requiring only proper acknowledgement in scholarly writing), and that all such use is clearly acknowledged. -
The Geology of the Olifants River Area, Transvaal
REPUBLIC OF SOUTH AFRICA REPUBLIEK VANSUID-AFRIKA· DEPARTMENT OF MINES DEPARTEMENT VAN MYNWESE GEOLOGICAL SURVEY GEOLOGIESE OPNAME THE GEOLOGY OF THE OLIFANTS RIVER AREA, TRANSVAAL AN EXPLANATION OF SHEETS 2429B (CHUNIESPOORT) AND 2430A (WOLKBERG) by J. S. I. Sehwellnus, D.Se., L. N. J. Engelbrecht, B.Sc., F. J. Coertze, B.Sc. (Hons.), H. D. Russell, B.Sc., S. J. Malherbe, B.Sc. (Hons.), D. P. van Rooyen, B.Sc., and R. Cooke, B.Sc. Met 'n opsomming in Afrikaans onder die opskrif: DIE GEOLOGIE VAN DIE GEBIED OLIFANTSRIVIER, TRANSVAAL COPYRIGHT RESERVED/KOPIEREG VOORBEHOU (1962) Printed by and obtainable (rom Gedruk deur en verkrygbaar the Government Printer, B(ls~ van die Staatsdrukker, Bosman man Street, Pretoria. straat, Pretoria. Geological map in colour on a Geologiese kaart in kleur op 'n scale of I: 125,000 obtainable skaal van I: 125.000 apart ver separately at the price of 60c. krygbaar teen die prys van 60c. & .r.::-~ h'd'~, '!!~l p,'-' r\ f: ~ . ~) t,~ i"'-, i CONTENTS PAGE ABSTRACT ........................ ' ••• no ..........' ........" ... • • • • • • • • •• 1 I. INTRODUCTION........ •.••••••••.••••••••.....••...•.•..••••..• 3 II. PHYSIOGRAPHY................................................ 4 A. ToPOGRAPHY..... • • . • • . • . • • . • • • . • • . • . • • • • • . • • • • • . • • • • • • ... 4 B. DRAINAGE.................................................... 6 C. CLIMATE ..........•.••••.•••••.••....................... ,.... 7 D. VEGETATION .••••.•••••.•.........•..... , ..............•... , . 7 III. GEOLOGICAL FORMATIONS .................... -
11010329.Pdf
THE RISE, CONSOLIDATION AND DISINTEGRATION OF DLAMINI POWER IN SWAZILAND BETWEEN 1820 AND 1889. A study in the relationship of foreign affairs to internal political development. Philip Lewis Bonner. ProQuest Number: 11010329 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 11010329 Published by ProQuest LLC(2018). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States C ode Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106- 1346 ABSTRACT The Swazi kingdom grew out of the pressures associated with competition for trade and for the rich resources of Shiselweni. While centred on this area it acquired some of its characteristic features - notably a regimental system, and the dominance of a Dlamini aristocracy. Around 1815 the Swazi came under pressure from the South, and were forced to colonise the land lying north of the Lusutfu. Here they remained for some years a nation under arms, as they plundered local peoples, and were themselves swept about by the currents of the Mfecane. In time a more settled administration emerged, as the aristocracy spread out from the royal centres at Ezulwini, and this process accelerated under Mswati as he subdued recalcitrant chiefdoms, and restructured the regiments. -
Integrated Management Plan: 2009-2013
Ndumo Game Reserve KwaZulu-Natal South Africa Integrated Management Plan: 2009-2013 Reviewed and edited by EKZNW Management Planning Co-ordination Unit Based on the original Integrated Management Plan (2007 - 2012) Compiled by Terratest (Pty) Ltd and MCDS Cover design by Di Martin Design Studio, Ezemvelo KZN Wildlife Citation Ndumo Game Reserve: Integrated Management Plan: 2009–2013, Version 1.0. (2009). Ezemvelo KZN Wildlife, Pietermaritzburg, 106 pp. and 7 maps (4 x A4, 3 x A3). _________________________________________________________________________________________________________ I Ndumo Game Reserve - Integrated Management Plan: 2009 to 2013 (Version 1.0) _________________________________________________________________________________________________________ I Ndumo Game Reserve - Integrated Management Plan: 2009 to 2013 (Version 1.0) TABLE OF CONTENTS AUTHORISATION.........................................................................................................................................II TABLE OF CONTENTS................................................................................................................................III LIST OF FIGURES.......................................................................................................................................VI LIST OF MAPS.............................................................................................................................................VI LIST OF TABLES.........................................................................................................................................VI -
Zululand District Municipality Integrated
ZULULAND DISTRICT MUNICIPALITY INTEGRATED DEVELOPMENT PLAN: 2020/2021 REVIEW Integrated Development Planning is an approach to planning that involves the entire municipality and its citizens in finding the best solutions to achieve good long- term development. OFFICE OF THE MUNICIPAL MANAGER [Email address] TABLE OF CONTENTS Page No. 1 INTRODUCTION .............................................................................................................................................. 1 1.1 Purpose .................................................................................................................................................................. 1 1.2 Introduction to the Zululand District Municipality ................................................................................................. 1 1.3 Objectives of the ZDM IDP...................................................................................................................................... 3 1.4 Scope of the Zululand District Municipality IDP ..................................................................................................... 4 1.5 Approach ................................................................................................................................................................ 5 1.6 Public Participation ................................................................................................................................................. 6 2 PLANNING AND DEVELOPMENT LEGISLATION AND POLICY ......................................................................... -
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 Vegetation Ecology of the Lower Mkuze River Floodplain, Northern
The vegetation ecology ofthe lower Mkuze River floodplain, northern KwaZulu-Natal: A landscape ecology perspective. Submitted in fulfillment ofthe requirements for the degree ofMaster ofScience in the School ofLife and Environmental Sciences, University ofNatal-Durban. 2001 Marian J. Neal PREFACE The work described was carried out between January 1999 and December 2001, in the School of Life and Environmental Sciences (previously the Department of Geographical and Environmental Sciences) at the University of Natal-Durban, under the supervision of Prof. W.N. Ellery. The study represents original work by the author and has not been submitted in any other form to another university. Where use was made of the work of others, it has been duly acknowledged in the text. 11 ACKNOWLEDGEMENTS This study fonns part of an ongoing research programme conducted in the Greater Mkuze Wetland System, northern KwaZulu-Natal and was made possible through the funding from Wildlife & Environment Society of southern Africa, the University ofNatal Masters special fund and the National Research Foundation. I would like to acknowledge the following people without whom this thesis would not have been possible: • Prof. Fred Ellery, for the enthusiasm he has for wetlands, for the discussions, time and encouragement and for instilling in me a work ethic I will carry with me throughout my career. • Dr Annika Dahlberg, for advice, support and assistance, especially in the field. • Prof. Gerry Garland, for the assistance and advice during the soil analysis phase. • Ezemvelo KwaZulu-Natal Wildlife, for granting pennission to access the study area and for the use of the Manzibomvu camp. Special mention must go to Drikus Gissing for his hospitality and logistical support. -
The Lower Umkhomazi Bulk Water Supply Scheme – Sediment Impact Opinion
NM Environmental December 2017 Report for: NM Environmental PO Box 63, Caversham Glen, Pinetown, 3616, SOUTH AFRICA Report by: ASP Technology (Pty) Ltd PO Box 12793, Die Boord, 7613, Stellenbosch, SOUTH AFRICA Table of Contents 1. Introduction ................................................................................................................................... 1 2. Hydrodynamic Modelling of the Non-Cohesive Sediment Loads .............................................. 2 3. Total Sediment Loads in the uMkhomazi River .......................................................................... 3 4. Comparison of Sediment Loads for Current and Future Scenarios ........................................... 4 5. The Release of Sediment Back Into the uMkhomazi River ......................................................... 6 6. Consideration of the South KwaZulu-Natal Coastal Sediment Erosion..................................... 8 6.1 Interpretation of Previous Studies on the KZN Coastal Sediment Erosion ............................. 8 6.2 uMkhomazi River Sand Yield Reductions in Context of the Coastal Sediment Erosion .......... 9 6.3 Shoreline Variability and Long-Term Stability ....................................................................... 11 6.3.1 INTERPRETATION OF AERIAL PHOTOGRAPHY .............................................................. 11 6.3.2 INTERPRETATION OF COASTAL TOPOGRAPHIC SURVEYS ............................................. 16 7. Conclusions and Recommendations ......................................................................................... -
Mozambique National Report Phase 1: Integrated Problem Analysis
Global Environment Facility GEF MSP Sub-Saharan Africa Project (GF/6010-0016): “Development and Protection of the Coastal and Marine Environment in Sub-Saharan Africa” MOZAMBIQUE NATIONAL REPORT PHASE 1: INTEGRATED PROBLEM ANALYSIS António Mubango Hoguane (National Coordinator), Helana Motta, Simeão Lopes and Zélia Menete March 2002 Disclaimer: The content of this document represents the position of the authors and does not necessarily reflect the views or official policies of the Government of Mozambique, ACOPS, IOC/UNESCO or UNEP. The components of the GEF MSP Sub-Saharan Africa Project (GF/6010-0016) "Development and Protection of the Coastal and Marine Environment in Sub-Saharan Africa" have been supported, in cash and kind, by GEF, UNEP, IOC-UNESCO, the GPA Coordination Office and ACOPS. Support has also been received from the Governments of Canada, The Netherlands, Norway, United Kingdom and the USA, as well as the Governments of Côte d'Ivoire, the Gambia, Ghana, Kenya, Mauritius, Mozambique, Nigeria, Senegal, Seychelles, South Africa and Tanzania. Table of Contents Page Eexecutive Summary................................................................................................................................ i Mozambique Country Profile................................................................................................................ vii Chapter 1 1. Background............................................................................................................................1 1.1 The National Report...............................................................................................................1 -
Kwazulu-Natal Situational Overview
KWAZULU-NATAL SITUATIONAL OVERVIEW April 2016 Page 1 of 443 TABLE OF CONTENTS LIST OF ABBREVIATIONS ...................................................................................................................... 24 INTRODUCTION ............................................................................................................................ 29 OVERVIEW OF KZN FROM A NATIONAL PERSPECTIVE .............................................................. 31 THE NATIONAL PLANNING COMMISSION AND NATIONAL GROWTH PATH ......................................... 31 THE NINE POINT GROWTH PLAN ..................................................................................................... 35 THE STATUS OF WOMEN AND GIRLS ................................................................................................ 37 YOUTH DEVELOPMENT.................................................................................................................... 40 RURAL DEVELOPMENT .................................................................................................................... 40 THE PHYSICAL AND ENVIRONMENTAL LANDSCAPE.................................................................. 41 TOPOGRAPHY................................................................................................................................ 41 Elevation .......................................................................................................................... 41 Slope ................................................................................................................................ -
Geological Inventory of the Maremani Nature Reserve
Geological Inventory Of The Maremani Nature Reserve Professor Jay Barton Department of Geology, Rand Afrikaans University (RAU) P.O. Box 524, Auckland Park 2006, South Africa Telephone: 27-11-489-2304 FAX: 27-11-489-2309 E-mail: [email protected] Introduction The Maremani Nature Reserve is presently being established and this document is intended as a summary of aspects of the geology within the boundaries of the Reserve. I have taken the liberty also to express my opinions with regard to possible roles that the Reserve might fulfill with regard to promoting geological awareness, education and research. The geology of the area covered by the Reserve was mapped in 1976 by Gunther Brandl and W. O. Willoughby of the Geological Survey of South Africa (presently the Council For Geo- science) at a scale of 1:50 000 for compilation at a scale of 1:250 000 (Brandl, 1981). The western portion to 30o 15’ east was previously mapped at a scale of 1:10 000 for compilation at scales of 1:50 000 and 1:125 000 by P. G. Söhnge (1946; Söhnge et al., 1948). Also locally within the western portion of the Reserve, maps at the scale of 1:5 000 were compiled by Messina Transvaal Development Corporation on farms and prospects investigated by the staff of the Messina Copper Mine. These maps are presently archived with me at RAU. Peter Horrocks wrote a PhD thesis on the geology of part of the western portion of what is now the Reserve (Horrocks, 1981). Charles Guerin in the late 1970’s worked on an unfin- ished MSc thesis on the calc-silicate rocks exposed in an area south of that studied by Peter Horrocks, some of which occur within the Reserve. -
Coping with Floods – the Experience of Mozambique1
1st WARFSA/WaterNet Symposium: Sustainable Use of Water Resources, Maputo, 1-2 November 2000 COPING WITH FLOODS – THE EXPERIENCE OF MOZAMBIQUE1 Álvaro CARMO VAZ Professor, Faculty of Engineering, Eduardo Mondlane University Director, CONSULTEC – Consultores Associados Lda. e-mail: [email protected] ABSTRACT A summary review is made of the major floods that have occurred in Mozambique since the Independence in 1975, describing the most important negative impacts and consequences. Various types of measures for flood mitigation are analysed, considering how they have been used in past floods and their potential for coping with floods in the future. These measures are grouped into structural (dams, levees, flooding areas, river training) and non-structural measures (flood zoning, flood management, flood warning systems, emergency plans, raising awareness, insurance). The paper briefly refers the need for adequate and comprehensive reports on past floods and some related research areas. 1 THE FLOOD PRONE RIVERS OF MOZAMBIQUE More than 50% of the Mozambican territory is part of international river basins – from South to North, the Maputo, Umbeluzi, Incomati, Limpopo, Save, Buzi, Pungoé, Zambezi and Rovuma, see figures 1 and 2. All these rivers have their flood plains inside Mozambique, with the exception of the Rovuma river that forms the border between this country and Tanzania. The largest basins are the Zambezi (1,200,000 Km2) and the Limpopo (412,000 Km2) and the smallest one is the Umbeluzi (5,600 Km2) with the others ranging from about 30,000 to 150,000 Km2. The climatic conditions of Mozambique indicate that the country is subject to various types of events that can originate floods: cyclones and tropical depressions from the Indian Ocean and cold fronts from the south.