A Biomonitoring Survey of the Olifants River Catchment Falling Within Limpopo Province
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Bezhoek Heritage Report
Francois P Coetzee Heritage Survey of the farm Bezuidenhoutshoek 274JS Cultural Heritage Survey of the Farm Bezuidenhoutshoek 274JS, Magisterial District of Middelburg, Mpumalanga For Bezuidenhoutshoek Farm (Pty) Ltd P O Box 1152 Gallo Manor 2052 By Francois P Coetzee Department of Anthropology & Archaeology University of South Africa PO Box 392 Pretoria 0003 Tel: (012) 429 6297 Fax: (012) 429 6091 [email protected] August 2009 Francois P Coetzee Heritage Survey of the farm Bezuidenhoutshoek 274JS Contents Executive Summary 1. Introduction 2. Terms of Reference 3. Nature of the Proposed Activity or Development 4. Definitions and Approach 5. Methodology 5.1 Maps and Other Sources 5.2 Fieldwork 5.3 Visibility and Constraints 6. Description of Study Area 7. Archaeological Sequence 8. Archaeological Context 8.1 Stone Age 8.2 Iron Age Sequence 8.3 Ethno-historical Context 9. Description of Sites 10. Summary of Sites 11. Rock Art Sites 12. Director-General: Survey Maps 13. Conclusions and Recommendations Bibliography Francois P Coetzee Heritage Survey of the farm Bezuidenhoutshoek 274JS Executive Summary This report focuses on the results from a cultural heritage investigation on the farm Bezuidenhoutshoek 274JS. The area is characterised by mountainous areas (featuring the Olifants River) as well as open grassland. The area has a rich cultural heritage with Ndebele people living in the area since AD1650 and white farmers settling in the late 19th Century. Iron Age settlements Five Late Iron Age stone-walled settlements were recorded during the survey. These are preliminarily associated with Ndzundza-Ndebele occupation (AD 1650 – AD 1830). Some of these sites are extensive and have substantial archaeological deposits. -
Meso-Archaean and Palaeo-Proterozoic Sedimentary Sequence Stratigraphy of the Kaapvaal Craton
Marine and Petroleum Geology 33 (2012) 92e116 Contents lists available at SciVerse ScienceDirect Marine and Petroleum Geology journal homepage: www.elsevier.com/locate/marpetgeo Meso-Archaean and Palaeo-Proterozoic sedimentary sequence stratigraphy of the Kaapvaal Craton Adam J. Bumby a,*, Patrick G. Eriksson a, Octavian Catuneanu b, David R. Nelson c, Martin J. Rigby a,1 a Department of Geology, University of Pretoria, Pretoria 0002, South Africa b Department of Earth and Atmospheric Sciences, University of Alberta, Canada c SIMS Laboratory, School of Natural Sciences, University of Western Sydney, Hawkesbury Campus, Richmond, NSW 2753, Australia article info abstract Article history: The Kaapvaal Craton hosts a number of Precambrian sedimentary successions which were deposited Received 31 August 2010 between 3105 Ma (Dominion Group) and 1700 Ma (Waterberg Group) Although younger Precambrian Received in revised form sedimentary sequences outcrop within southern Africa, they are restricted either to the margins of the 27 September 2011 Kaapvaal Craton, or are underlain by orogenic belts off the edge of the craton. The basins considered in Accepted 30 September 2011 this work are those which host the Witwatersrand and Pongola, Ventersdorp, Transvaal and Waterberg Available online 8 October 2011 strata. Many of these basins can be considered to have formed as a response to reactivation along lineaments, which had initially formed by accretion processes during the amalgamation of the craton Keywords: Kaapvaal during the Mid-Archaean. Faulting along these lineaments controlled sedimentation either directly by Witwatersrand controlling the basin margins, or indirectly by controlling the sediment source areas. Other basins are Ventersdorp likely to be more controlled by thermal affects associated with mantle plumes. -
Water Affairs in the Lower Blyde River the Role of DWAF in Local Water Management
Water Affairs in the Lower Blyde River The role of DWAF in local water management IWMI Working Paper B.W. Raven, April 2004, Wageningen Acknowledgments The author likes to thank specifically Barbara van Koppen (IWMI) and Jeroen Warner (Wageningen University) for their help and contribution to this case study. The author further thanks: Willy Enright (DWAF Western Cape), Edward Lahiff (Western Cape University), Cees Leeuwis (Wageningen University), Derek Weston and Francois van der Merwe (DWAF Pretoria), Gert Bezuidenhout Johan Du Preez (Lower Blyde River WUA) Francis Mohlala (Mametja / Sekororo communities), Marie Tinka Uys (Environmental issues Blyde River), Gerhard Backeberg (WRC Pretoria), Anthony Turton (AWIRU Pretoria), Herve Levite, Nicholas Faysse, Tebogo Seshoka and other colleagues of IWMI Pretoria. 1 Content 1 Introduction 1.1 Case Study: The Lower Blyde River 1.2 The Case Study in perspective: South Africa and The Netherlands 1.3 Case Study Objectives 2 General Background 2.1 Multi Stakeholder Participation 2.2 Former SA irrigation policy 2.3 The new SA water policy: NWA 1998 2.4 Building CMAs and WUAs 3 The Lower Blyde River 3.1 The Blyde River Catchment 3.2 Stakeholders 3.2.1 Irrigation Farmers 3.2.2 Mametja / Sekororo Communities 3.2.3 Upstream Stakeholders 3.2.4 Downstream Stakeholders 3.2.5 Governments involved 4 Water Management in the Lower Blyde River 4.1 The Lower Blyde WUA 4.2 The Lower Blyde Irrigation Pipeline 4.3 The 800ha Black Emerging Farmers Project 4.4 Domestic Water Supply Mametja / Sekororo communities 5 Conclusions Bibliography Annex: list of interviews 2 1 Introduction “The new South Africa is the world in microcosm, in its population mix, its wealth gap and above all in the impact which the new forces of globalisation are having on it. -
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 .................... -
Potential Impacts to Be Considered by the Oryx Gems Prospecting Rights Application
Potential impacts to be considered by the Oryx Gems prospecting rights application Biodiversity, Ecosystems & Natural Resources The farm portions overlap with several Critical Biodiversity Areas (CBA) and Ecological Support Areas (ESA) under the Mpumalanga Biodiversity Sector Plan (MBSP, 2014) and the National Freshwater Ecosystem Priority Areas (NFEPA, 2011) o Multiple Irreplaceable and Optimal terrestrial CBAs and ESAs o Multiple CBA and ESA rivers, wetlands and catchments (including the Blyde & Lisbon Rivers as listed CBA rivers) o Several downstream aquatic CBAs and ESAs under the Limpopo Conservation Plan (2013) will also be affected The farm portions overlap with three NEMBA listed Threatened Ecosystems: o Northern Escarpment Dolomite Grassland (Vulnerable) o Blyde Quartzite Grasslands (Endangered) o Malmali Karstlands (Endangered) The Unique community, ‘Graskop grassland’, registered under Mpumalanga Nature Conservation Act (1998) is located on the farm portions Birdlife Important Bird and Biodiversity Areas (IBA): area overlaps with the globally listed Blyde River Canyon IBA Threatened or rare species, or species of conservation concern potentially occurring on the farm portions: o Bird species: Blue swallow, Bald Ibis, Striped Flufftail, Stanley’s Bustard (Neotis denhami), Blackwinged Plover (Vanellus melanopterus), Buffstreaked Chat (Oenanthe bifaciata) o Mammal species: Oribi, Rough-haired Golden Mole, Meester’s Golden Mole, Short-eared Trident Bat, Natal Long-fingered Bat o Reptile species: Bradypodion transvaalense, Lamprophis -
Sequence Stratigraphic Development of the Neoarchean Transvaal Carbonate Platform, Kaapvaal Craton, South Africa Dawn Y
DAWN Y. SUMNER AND NICOLAS J. BEUKES 11 Sequence Stratigraphic Development of the Neoarchean Transvaal carbonate platform, Kaapvaal Craton, South Africa Dawn Y. Sumner Department of Geology, University of California 1 Shields Ave, Davis, CA 95616 USA e-mail: [email protected] Nicolas J. Beukes Department of Geology, University of Johannesburg P.O. Box 524, Auckland Park, 2000 South Africa e-mail: [email protected] © 2006 March Geological Society of South Africa ABSTRACT The ~2.67 to ~2.46 Ga lower Transvaal Supergroup, South Africa, consists of a mixed siliciclastic-carbonate ramp that grades upward into an extensive carbonate platform, overlain by deep subtidal banded iron-formation. It is composed of 14 third-order sequences that develop from a mixed siliciclastic-carbonate ramp to a steepened margin followed by a rimmed margin that separated lagoonal environments from the open ocean. Drowning of the platform coincided with deposition of banded iron-formation across the Kaapvaal Craton. The geometry and stacking of these sequences are consistent with more recent patterns of carbonate accumulation, demonstrating that Neoarchean carbonate accumulation responded to subsidence, sea level change, and carbonate production similarly to Proterozoic and Phanerozoic platforms. The similarity of carbonate platform geometry through time, even with significant changes in dominant biota, demonstrates that rimmed margins are localized primarily by physiochemical conditions rather than growth dynamics of specific organisms. Stratigraphic patterns during deposition of the Schmidtsdrift and Campbellrand-Malmani subgroups are most consistent with variable thinning of the Kaapvaal Craton during extrusion of the ~2.7 Ga Ventersdorp lavas. Although depositional patterns are consistent with rifting of the western margin of the Kaapvaal Craton during this time, a rift-to-drift transition is not required to explain subsidence. -
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. -
INVESTOR FACT SHEET 4. Blyde River Hydro Power Project
INVESTOR FACT SHEET 4. Blyde River Hydro Power Project A. PROJECT SECTOR: Renewable Energy I. INTRODUCTION The Blyde River (Happy River) or Motlatse River, is a river in Mpumalanga Province South Africa. It flows north through the steep-sided valleys and ravines of the Mpumalanga Drakensberg (Dragon Mountains), before it enters the Lowveld Escapement – one of Africa’s prime wildlife and game reserves destinations. The Blyde River Hydro Power Project is a small Hydo-Electric Project involving the re-engineering and re-establishment of an existing hydro-electric power plant. II. LOCATION South Africa – Mpumalanga Province – Thaba Chweu Municipality III. PROJECT DESCRIPTION This renewable energy project is situated in the environmentally sensitive Blyde River Canyon Nature Reserve of Mpumalanga Province. This area attracts over one million tourists a year to the natural wonder of the surrounding Bourke’s Luck Potholes, Gods Window, the Blyde River Canyon and the world famous Kruger National Park. Mpumalanga Province is an attractive Green Energy investment destination in support of the tourism infrastructure and local communities. The existing but non-operational Belvedere Hydro-Electric Power Plant was commissioned in 1911 to supply power to the historic gold mining town of Pilgrim’s Rest. This 2,000 Kw power station was at its time the largest hydro-electric power station in the Southern Hemisphere and Pilgrim’s Rest was electrified before the City of London. The Blyde River Hydro Power Project entails the design, engineering and commissioning of a new hydro-power station to generate renewable green energy to be supplied the surrounding tourism attractions and adjacent communities. -
Article ISSN 1179-3163 (Online Edition)
Phytotaxa 408 (1): 069–076 ISSN 1179-3155 (print edition) https://www.mapress.com/j/pt/ PHYTOTAXA Copyright © 2019 Magnolia Press Article ISSN 1179-3163 (online edition) https://doi.org/10.11646/phytotaxa.408.1.5 Gymnosporia sekhukhuniensis (Celastraceae), a new species from South Africa MARIE JORDAAN1,2 & ABRAHAM E. VAN WYK1,2* 1National Herbarium, South African National Biodiversity Institute, Private Bag X101, Pretoria, 0001 South Africa. 2H.G.W.J. Schweickerdt Herbarium, Department of Plant and Soil Sciences, University of Pretoria, Pretoria, 0002 South Africa. *Author for correspondence. E-mail: [email protected] Abstract Gymnosporia sekhukhuniensis, a new species from north-eastern South Africa, is described, illustrated, mapped, and compared with closely related species. It belongs to Gymnosporia sect. Buxifoliae, more specifically Group 1, the members of which are characterized by the capsules being (2)3(4)-valved, rugose or verrucose, and the seeds partially covered by the aril. The new species has a restricted distribution range and is near-endemic to the Sekhukhuneland Centre of Endemism. This biogeographical region rich in restricted-range plants is more or less congruent with surface outcrops of mafic and ultramafic igneous rocks belonging to the Rustenburg Layered Suite of the eastern Bushveld Complex. The range of the new species shows marginal intrusion into the far northern part of the nearby Wolkberg Centre of Endemism, where it is associated with dolomites of the Malmani Subgroup. Gymnosporia sekhukhuniensis is a suffrutex mainly associated with rocky outcrops in open savannah. Diagnostic characters include its dwarf habit (up to 1.6 m tall), capsules that are relatively small (5–8 mm long), woody, scaly-rugose, with hard pointed apices, and leaves that are very laxly arranged on the stems, with some often present on the thorns. -
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. -
A New Species of Disa (Orchidaceae) from Mpumalanga, South Africa ⁎ D
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Elsevier - Publisher Connector South African Journal of Botany 72 (2006) 551–554 www.elsevier.com/locate/sajb A new species of Disa (Orchidaceae) from Mpumalanga, South Africa ⁎ D. McMurtry a, , T.J. Edwards b, B. Bytebier c a Whyte Thorne, P O Box 218, Carino 1204, South Africa b School of Biological and Conservation Sciences, University of KwaZulu–Natal Pietermaritzburg, Private Bag X01, Scottsville 3209, South Africa c Biochemistry Department, Stellenbosch University, Private Bag X1, Stellenbosch 7602, South Africa Received 10 November 2005; accepted 8 March 2006 Abstract A new species, Disa vigilans D. McMurtry and T.J. Edwards, is described from the Mpumalanga Escarpment. The species is a member of the Disa Section Stenocarpa Lindl. Its alliances are discussed in terms of its morphology and its phylogenetic placement is elucidated using molecular data. D. vigilans has previously been considered as an anomalous form of Disa montana Sond. but is more closely allied to Disa amoena H.P. Linder. © 2006 SAAB. Published by Elsevier B.V. All rights reserved. Keywords: Disa; Draensberg endemic; New species; Orchidaceae; Section Stenocarpae; South Africa; Mpumalanga province 1. Introduction with 3 main veins, margins thickened and translucent. Inflorescence lax, cylindrical, 40–75 mm long; bracts light green suffused pinkish Disa is the largest genus of Orchidaceae in southern Africa (162 with darker green veins, linear-lanceolate, acuminate, 11–29×2– spp.) and has been the focus of considerable taxonomic investigation 3 mm, scarious at anthesis. Flowers white suffused with carmine- (Linder, 1981a,b, 1986; Linder and Kurzweil, 1994). -
Klaserie Eco School Pitlochry 14 KU.Pdf
Phase 1 Archaeological and Heritage Impact Assessment on a Portion of the farm Pitlochry 14 KU in respect of the proposed construction of a School, Klaserie, Mpumalanga Province. Compiled by: For Henwood Environmental Services Surveyor: Mr JP Celliers 4 February, 2019 Table of Contents Introduction .................................................................................................................................. 3 1.1. Terms of reference ............................................................................................................. 3 1.1.1 Project overview ........................................................................................................... 3 1.1.2. Constraints and limitations ........................................................................................... 3 1.2. Legislative Framework ....................................................................................................... 3 1.2.1. Heritage in Protected areas .......................................................................................... 5 1.3. Approach and statutory requirements ................................................................................. 6 2. Description of surveyed area .................................................................................................... 6 3. Methodology ............................................................................................................................. 7 3.1. Archaeological and Archival background studies ..............................................................