Table 3.5 List of Land Cover in the Vicinity of National Assessment Sample Sites Selected, Grouped Per WMA No
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An Assessment of Fish and Fisheries in Impoundments in the Upper Orange-Senqu River Basin and Lower Vaal River Basin
AN ASSESSMENT OF FISH AND FISHERIES IN IMPOUNDMENTS IN THE UPPER ORANGE-SENQU RIVER BASIN AND LOWER VAAL RIVER BASIN Submitted in fulfillment of the requirements in respect of the Doctoral Degree DOCTOR OF PHILOSOPHY in the Department of Zoology and Entomology in the Faculty of Natural and Agricultural Sciences at the University of the Free State by LEON MARTIN BARKHUIZEN 1 July 2015 Promoters: Prof. O.L.F. Weyl and Prof. J.G. van As Table of contents Abstract ........................................................................................................................................ vi Acknowledgements .............................................................................................................................. ix List of tables ....................................................................................................................................... xii List of figures ....................................................................................................................................... xv List of some acronyms used in text .................................................................................................. xviii Chapter 1 General introduction and thesis outline ...................................................................... 1 Chapter 2 General Literature Review ........................................................................................... 7 2.1 Introduction ............................................................................................................................ -
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 .................... -
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. -
Thusong — Bringing Hope to Small Towns
THUSONG — BRINGING HOPE TO SMALL TOWNS Small towns such as Burgersdorp, Oviston, Steynsburg and Venterstad subsist off the beaten track. The local Community Wwork Programme is creating work opportunities and stimulating entrepreneurship in an area where unemployment if rife – and even boosting the coffers of the local municipality. There is a stark beauty to the Free State and northern Within many homesteads trenches have been Eastern Cape. It’s a part of South Africa that has ploughed, ready to be sown with vegetables and grain. inspired thousands of paintings – a vast rural The local primary school has been completely landscape with potholed roads rolling down re-painted and re-furbished, and feels like a pleasant escarpments into countless plateaus, punctuated by environment where learners can be proud to study. windmills, mountain ranges and the occassional Before the advent of CWP, the members here would farmhouse either fish for subsistence or “do nothing”. Settlements are few and far between. Neighbours can The knock-on effects of the CWP programme in the be many kilometers away. Small forgotten towns such Thusong site is clearly evident. Gideon Mapete, Unit as Burgersdorp, Oviston, Steynsburg and and Manager of Steynsburg municipality and CWP Venterstad subsist quietly out of sight. This was once municipal contact, can undoubtedly see the positives. burgeoning farm country, full of grazing livestock. Not only has there been a small dent made into the From a distance the townships and towns are distinct unemployment rates, but also a small increase in the income of local government. As CWP members and clear. Iron sheets of RDP housing reflect the harsh sun on one side of the road, while a are receiving regular income, more are paying for neighbouring hamlet rests in the shade of large trees municipal services, therefore growing coffers and on the other. -
Request for Proposals: Establishing Environment Clubs and Science Clubs in Britstown, Hanover, Burgersdorp, Steynsburg and Venterstad
DREUNBERG LOCAL COMMUNITY TRUST, JOE GQABI BROAD TRUST, LINDE LOCAL COMMUNITY TRUST, PIXLEY KA SEME BROAD BASED TRUST REQUEST FOR PROPOSALS: ESTABLISHING ENVIRONMENT CLUBS AND SCIENCE CLUBS IN BRITSTOWN, HANOVER, BURGERSDORP, STEYNSBURG AND VENTERSTAD BACKGROUND AND CONTEXT: Scatec Solar develops, builds, operates and owns solar power plants that generate cost-effective, clean and reliable electricity. Scatec Solar works along three principle areas for all employees to focus on; delivering competitive renewable energy, contributing to local value creation and being a trusted business partner. Scatec Solar is committed to value creation and economic development in the communities close to the solar plants. Scatec Solar has identified the need for enterprise development in the above-mentioned towns. It has also identified the small market, coupled with low overall skill levels, as a major inhibitor to the growth of the economy in the towns mentioned. This is a vicious cycle that Scatec Solar aims to address through the integration of a broad-based economic development strategy spanning a 20-year period. One of the tenets of the strategy is a focus on youth development and sustainable enterprise development through the sciences and amongst the youth population. It is against this backdrop that Scatec Solar is seeking to appoint a service provider that can manage the formulation of Environment and Science Clubs. It is expected that this will be a 12-24-month contract. THE STRATEGY: Outlined below is the core strategy that Scatec Solar is following -
PUBLIC NOTICE No: 03/2020
PUBLIC NOTICE No: 03/2020 PUBLIC NOTICE: MID-YEAR BUDGET ISAZISO KULUNTU: INGXELO AND PERFORMANCE ASSESSMENT YOHLAHLO LWABIWO MALI REPORT FOR THE 2019/20 NENKCITHO KUNYAKA MALI KA FINANCIAL YEAR 2019/20 Notice is hereby given in terms of Oku kukwazisa ukuba ngokomhlathi Section 5 4 (1) of the Local Government wama 54 (1) ngokomthetho wolawulo Municipal Budget and Reporting lwezimali nen gxelo yomgaqo wonyaka ka Regulations, 2008 that the Honourable 2008 ku Rhulumente wasemakhaya, Executive Mayor of the Joe Gqabi District uSodolophu womasipala wesithili iJoe Municipality, Councillor Z.I. Dumzela, has Gqabi, uZI Dumzela, uthe thaca tabled in the Municipal Council the Mid- kwibhunga likamasipala ingxelo year Budget and Performance yesiqingatha sonyaka kuhlahlo lwabiwo Assess ment Report of the Joe Gqabi mali nenkcitho yalo masipala, kwakunye District Municipality and the Joe Gqabi nequmrhu lophuhliso eli bizwa JoGEDA Economic Development Agency kumnyaka ka 2019/20 (JoGEDA) for the 2019/20 financial year. Imiqulu engalengxelo iyafumaneka Copies of the documents are available kwiofisi zikamasipala wesithili eF79, Cnr for scrutiny during office hours at the Joe Cole and Graham Street, Barkly East Gqabi District Municipal offices, o ffice 9786. nakwezinye iofisi zalomasipala F79, Cnr Cole and Graham Street, Barkly ezikwezidolophu zilandelayo: Aliwal East, 9786. District satelite offices: North, Burgersdorp, Venterstad, Aliwal North, Burgersdorp, Venterstad, Steynsburg, Sterkspruit, Maclear, Ugie Steynsburg, Sterkspruit, Maclear, Ugie nase Mt Fletcher, kwiofisi zikamasipala and Mt Fletcher, Local Municipalities (Elundini, Senqu, Walter Sisulu , (Elundini, Senqu, Walter Sisulu, kumathala ogcino ncwadi Libraries as well a s on the District kwakwezidolophu zingentla nakwi website: www.jgdm.gov.za . For any website yethu ethi: www.jgdm.gov.za . -
Towards Improving the Assessment and Implementation of the Reserve
Towards improving the assessment and implementation of the Reserve: Real-time assessment and implementation of the Ecological Reserve Final report WRC project K8/881/2 March 2011 Sharon Pollard1 Stephen Mallory2 Edward Riddell3 Tendai Sawunyama2 1 Association for Water & Rural Development (AWARD) 2 Water for Africa (IWR Water Resources) 3 University of KwaZulu-Natal Water Research Commission Executive Summary When the Olifants River in north-east South Africa ceased flowing in 2005, widespread calls were made for an integrated focus on all of the easterly-flowing rivers of the lowveld of South Africa. These are the Luvuvhu, Letaba, Olifants, Sabie-Sand, Crocodile and Komati Rivers in Water Management Areas 2,4 and 5. Most of these rivers appeared to be deteriorating in terms of water quantity and quality despite the 1998 National Water Act (NWA). As most of the rivers flow through Kruger National Park (KNP) and all of them form part of international systems the implications of their degradation were profound and of international significance (Pollard and du Toit 2010). The aims of this study were to assess the state of compliance with the Ecological Reserve (ER) – as a benchmark for sustainability - in these rivers and some of their tributaries. It also explored the problems associated with an assessment of compliance. In short these include the lack of planning and integration of ER determination methods with operations and the difficulties associated with real-time predictions of ER requirements. These factors severely constrain planning, monitoring and the management action to mitigate non-compliance. In South Africa, the ER is defined as a function of the natural flow which, because the natural flow in a system is not known at any point in time, is creating problems with real-time implementation. -
Review of Existing Infrastructure in the Orange River Catchment
Study Name: Orange River Integrated Water Resources Management Plan Report Title: Review of Existing Infrastructure in the Orange River Catchment Submitted By: WRP Consulting Engineers, Jeffares and Green, Sechaba Consulting, WCE Pty Ltd, Water Surveys Botswana (Pty) Ltd Authors: A Jeleni, H Mare Date of Issue: November 2007 Distribution: Botswana: DWA: 2 copies (Katai, Setloboko) Lesotho: Commissioner of Water: 2 copies (Ramosoeu, Nthathakane) Namibia: MAWRD: 2 copies (Amakali) South Africa: DWAF: 2 copies (Pyke, van Niekerk) GTZ: 2 copies (Vogel, Mpho) Reports: Review of Existing Infrastructure in the Orange River Catchment Review of Surface Hydrology in the Orange River Catchment Flood Management Evaluation of the Orange River Review of Groundwater Resources in the Orange River Catchment Environmental Considerations Pertaining to the Orange River Summary of Water Requirements from the Orange River Water Quality in the Orange River Demographic and Economic Activity in the four Orange Basin States Current Analytical Methods and Technical Capacity of the four Orange Basin States Institutional Structures in the four Orange Basin States Legislation and Legal Issues Surrounding the Orange River Catchment Summary Report TABLE OF CONTENTS 1 INTRODUCTION ..................................................................................................................... 6 1.1 General ......................................................................................................................... 6 1.2 Objective of the study ................................................................................................ -
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. -
HYDROGEOLOGY of GROUNDWATER REGION 7 POLOKWANE/PIETERSBURG PLATEAU JR Vegter
HYDROGEOLOGY OF GROUNDWATER REGION 7 POLOKWANE/PIETERSBURG PLATEAU Prepared for the Water Research Commission by JR Vegter Hydrogeological Consultant WRC Report No. TT 209/03 October 2003 Obtainable from: Water Research Commission Private Bag X03 GEZINA 0031 Pretoria The publication of this report emanates from a project entitled: Hydrogeology of groundwater region 7 Pietersburg Plateau (WRC Consultancy No. K8/466) DISCLAIMER This report has been reviewed by the Water Research Commission (WRC) and approved for publication. Approval does not signify that the contents necessarily reflect the views and policies of the WRC, nor does mention of trade names or commercial products constitute endorsement or recommendation for use. ISBN No. 1-77005-027-2 ISBN Set No. 1-86845-645-5 Printed in the Republic of South Africa EXECUTIVE SUMMARY The more important findings of this study are summarised below under “Statistical analyses”, “Role of geophysical methods” and “Hydrogeological control of drilling operations” General Groundwater Region 7, a rectangular area of about 12 000 km2, is located in the Limpopo Province. Its eastern boundary is the watershed between the Sand River and its tributaries and the eastward draining Letaba and Pafuri Rivers. Its northern boundary is formed by Formations of the Soutpansberg Group that built the mountain range of that name. The western boundary consists from north to south firstly of Waterberg Group sedimentary rocks, followed by mafic Bushveld rocks and lastly by strata of the Wolkberg Group including the Black Reef Formation. These strata build the Highlands Mountains and the east- northeasterly trending Strydpoort Mountains that form the southern boundary. -
Biodiversity Plan V1.0 Free State Province Technical Report (FSDETEA/BPFS/2016 1.0)
Biodiversity Plan v1.0 Free State Province Technical Report (FSDETEA/BPFS/2016_1.0) DRAFT 1 JUNE 2016 Map: Collins, N.B. 2015. Free State Province Biodiversity Plan: CBA map. Report Title: Free State Province Biodiversity Plan: Technical Report v1.0 Free State Department of Economic, Small Business Development, Tourism and Environmental Affairs. Internal Report. Date: $20 June 2016 ______________________________ Version: 1.0 Authors & contact details: Nacelle Collins Free State Department of Economic Development, Tourism and Environmental Affairs [email protected] 051 4004775 082 4499012 Physical address: 34 Bojonala Buidling Markgraaf street Bloemfontein 9300 Postal address: Private Bag X20801 Bloemfontein 9300 Citation: Report: Collins, N.B. 2016. Free State Province Biodiversity Plan: Technical Report v1.0. Free State Department of Economic, Small Business Development, Tourism and Environmental Affairs. Internal Report. 1. Summary $what is a biodiversity plan This report contains the technical information that details the rationale and methods followed to produce the first terrestrial biodiversity plan for the Free State Province. Because of low confidence in the aquatic data that were available at the time of developing the plan, the aquatic component is not included herein and will be released as a separate report. The biodiversity plan was developed with cognisance of the requirements for the determination of bioregions and the preparation and publication of bioregional plans (DEAT, 2009). To this extent the two main products of this process are: • A map indicating the different terrestrial categories (Protected, Critical Biodiversity Areas, Ecological Support Areas, Other and Degraded) • Land-use guidelines for the above mentioned categories This plan represents the first attempt at collating all terrestrial biodiversity and ecological data into a single system from which it can be interrogated and assessed. -
A Comparative Study of the Origins of Cyanobacteria at Musina Water Treatment Plant Using Dna Fingerprints
A COMPARATIVE STUDY OF THE ORIGINS OF CYANOBACTERIA AT MUSINA WATER TREATMENT PLANT USING DNA FINGERPRINTS Murendeni Magonono (11573449) Supervisor: Prof JR Gumbo Co-supervisor: Prof PJ Oberholster A Dissertation submitted to the Department of Ecology & Resources Management, University of Venda, for the fulfilment of the requirements for the degree of Master of Earth Sciences in Hydrology & Water Resources August 2017 i DECLARATION ii DEDICATION I would like to dedicate my thesis to my parents Mr A.N Ma gonono and Mrs A.S Magonono who supported me throughout my studies. This thesis is also dedicated to all other people who helped in the success of this project. iii ACKNOWLEDGEMENTS I would like to thank Prof Gumbo for the continuous support and influence he showed during this Master’s program. It will never be enough by words to show how much I appreciate his efforts; he was involved in sponsorship attraction, progress and supply of knowledge to the author without giving up. I would also like to thank everyone for the laboratory assistan ce as well as Prof Shonai and Prof Gitari for allowing me the access to their laborat ies. I would also take this moment to thank Dr Gachara, Mr Glen Mr B Ogola and Mr S Makumere for their energy and time used in analyzing my results, and the influence they gave to me without giving up. I would like to also give a thank you to Mr E Matamba who spent his time reanalyzing my results and reading my thesis, his influence is very much appreciated.