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Sabie 109Tt Presentation August 2014
INDEX 1. INTRODUCTION 11. VALUABLE SUPPORTING INFORMATION 2. THE SABIE 109TT 12. TOURIST ACTIVITY AND INVESTMENT 3. THE ISLE OF MAN TT 13. TOURIST ACTIVITY 2017 AND ONWARDS 4. MOTIVATION FOR THE SABIE 109TT 14. IN TIME TO FOLLOW 5. THE COMPANY 15. EXPOSURE FOR THE PROVINCE AND REGION 6. THE ROAD TO THE SABIE 109TT 16. COMMUNITY DEVELOPMENT 7. ADVANTAGES 17. THE SABIE 109TT LEGACY 8. EVENTS 18. GOVERNMENT 9. CRUCIAL FACTORS ASSISTANCE REQUIRED 19. THE VISION 10. PROJECTED 22TT INCOME 20. LINKS TO THE ISLE OF MAN TT VIDEOS 1. INTRODUCTION In the past worthwhile “signature events” brought fame and fortune to countries, provinces and cities all over the world. Modern times with its competition on all fronts and increasing entertainment options make it very difficult to find a place in the sun for any new activity, and it is not easy to create such events without simply copying another event. Our aim was to find an event that would stand out and live up to the challenge of becoming a Signature event for Mpumalanga. This presentation tells you more. 2. THE SABIE 109TT This will be an event based on international proven results that will, combined with local vision and drive, create a Signature event for Mpumalanga. Chances are that it will become one of the best and most exciting South African Sporting events, ever! This event will be based on a world-renowned motorcycle race, held annually for more than a century on the Isle of Man. 3. THE ISLE OF MAN TT The Isle of Man TT is a race for motorcycles that has been running since 1907. -
U–Pb Zircon (SHRIMP) Ages for the Lebombo Rhyolites, South Africa
Journal of the Geological Society, London, Vol. 161, 2004, pp. 547–550. Printed in Great Britain. 2000) and the ages corroborate and further strengthen the SPECIAL chronology of the Lebombo stratigraphy. The rapid eruption of the Karoo succession is thought to have been responsible for trigger- U–Pb zircon (SHRIMP) ing the early Toarcian extinction event (Hesselbo et al. 2000). Geological setting. The Karoo Supergroup succession along the ages for the Lebombo Lebombo monocline is highlighted in Figure 1. The oldest phase of Karoo volcanism is marked by the Mashikiri nephelinites, rhyolites, South Africa: which unconformably overlie Jurassic Clarens Formation sand- stones (Fig. 2). The nephelinites have been dated at 182.1 Æ refining the duration of 1.6 Ma (40Ar/39Ar plateau age; Duncan et al. 1997) and form a lava succession up to 170 m thick (Bristow 1984). These rocks Karoo volcanism are confined to the northern part of the Lebombo rift and are absent along the central and southern sections. The nephelinites T. R. RILEY1,I.L.MILLAR2, are conformably overlain by picrites and picritic basalts of the 3 1 Letaba Formation, although in the southern Lebombo the picrites M. K. WATKEYS ,M.L.CURTIS, directly overlie the Clarens Formation. The picrites overlap in 1 3 P. T. LEAT , M. B. KLAUSEN & age (182.7 Æ 0.8 Ma; Duncan et al. 1997) with the Mashikiri C. M. FANNING4 nephelinites and are believed to form a succession up to 4 km in thickness. 1British Antarctic Survey, High Cross, Madingley Road, The Letaba Formation picrites are in turn overlain by a major Cambridge, CB3 0ET, UK (e-mail: [email protected]) succession (4–5 km thick) of low-MgO basalts, termed the Sabie 2British Antarctic Survey c/o NERC Isotope Geosciences River Basalt Formation (Cleverly & Bristow 1979). -
Casterbridge-Fact-Sheet.Pdf
TOP 25 HOTELS IN SOUTH AFRICA WHITE RIVER I MPUMALANGA www.casterbridgehollow.co.za AUGUST 2019 Pilgrim’sGRASKOP Rest R535 Graskop HAZYVIEW R536 Hazyview Kruger National Park MOZAMBIQUE LIMPOPO PROVINCE KRUGER BOTSWANA Skukuza NATIONAL CASTERBRIDGE SABIE PARK HOLLOW R40 Johannesburg Sabie R538 NAMIBIA NORTH WEST PROVINCE GAUTENG MPUMALANGA Pretoriuskop SWAZILAND R37 R537 FREE STATE KWAZULU- NATAL White River LESOTHO KRUGER NORTHERN CAPE WHITE RIVER Casterbridge Lifestyle Centre Durban NATIONAL PLASTON PARK EASTERN CAPE R37 KMIA Kruger Mpumalanga R40 International Airport WESTERN CAPE Cape Town N4 NELSPRUIT N4 R40 WHITE RIVER I MPUMALANGA Casterbridge, once a spreading Mango plantation in White River, has been transformed into one of the most original and enchanting country estates in South Africa. Just 20 km from Nelspruit, a mere 40 km from Hazyview and Sabie; White River has become home to a host of creative talents; artists, designers, fine craftsmen, ceramicists, cooks and restaurateurs. Casterbridge Hollow is a concept that has evolved with great charm with colours reminiscent of romantic hillside villages in Provence and Tuscany. LOCATION • Casterbridge Hollow Boutique Hotel is situated outside White River. • It is the ideal destination from which to access the reserves of the Lowveld and the attractions of Mpumalanga. ACCOMMODATION 30 ROOMS • 24 Standard, 2 Honeymoon and 4 Family • Air-conditioning and heating • Ceiling fans • Balconies overlook the courtyard and swimming pool • Satellite television • Tea / coffee making facilities -
Insights from the Kruger National Park, South Africa
Morphodynamic response of a dryland river to an extreme flood Morphodynamics of bedrock-influenced dryland rivers during extreme floods: Insights from the Kruger National Park, South Africa David Milan1,†, George Heritage2, Stephen Tooth3, and Neil Entwistle4 1School of Environmental Sciences, University of Hull, Cottingham Road, Hull, HU6 7RX, UK 2AECOM, Exchange Court, 1 Dale Street, Liverpool, L2 2ET, UK 3 Department of Geography and Earth Sciences, Aberystwyth University, Llandinam Building, Penglais Campus, Aberystwyth, SY23 3DB, UK 4School of Environment and Life Sciences, Peel Building, University of Salford, Salford, M5 4WT, UK ABSTRACT some subreaches, remnant islands and vege- the world’s population (United Nations, 2016). tation that survived the 2000 floods were re- Drylands are characterized by net annual mois- High-magnitude flood events are among moved during the smaller 2012 floods owing ture deficits resulting from low annual precipita- the world’s most widespread and signifi- to their wider exposure to flow. These find- tion and high potential evaporation, and typically cant natural hazards and play a key role in ings were synthesized to refine and extend a by strong climatic variability. Although precipi- shaping river channel–floodplain morphol- conceptual model of bedrock-influenced dry- tation regimes vary widely, many drylands are ogy and riparian ecology. Development of land river response that incorporates flood subject to extended dry periods and occasional conceptual and quantitative models for the sequencing, channel type, and sediment sup- intense rainfall events. Consequently, dryland response of bedrock-influenced dryland ply influences. In particular, with some cli- rivers are commonly defined by long periods rivers to such floods is of growing scientific mate change projections indicating the po- with very low or no flow, interspersed with in- and practical importance, but in many in- tential for future increases in the frequency frequent, short-lived, larger flows. -
The Geology and Geochemistry of the Sterkspruit Intrusion, Barberton Mountain Land, Mpumalanga Province
THE GEOLOGY AND GEOCHEMISTRY OF THE STERKSPRUIT INTRUSION, BARBERTON MOUNTAIN LAND, MPUMALANGA PROVINCE Gavin Patrick Conway A dissertation submitted to the Faculty of Science, University of the Witwatersrand, Johannesburg, in fulfilment of the requirements for the degree of Master of Science. Johannesburg, 1997 11 DECLARATION I declare that this dissertation is my own, unaided work. It is being submitted for the Degree of Master of Science in the University of the Witwatersrand, Johannesburg. It has not been submitted before for any degree or examination in any other University. __I_It __ ·daYOf A~V\.-~t 19 't1-- 111 ABSTRACT The Sterkspruit Intrusion, in the south-western portion of the Barberton greenstone belt, is a sill-like body containing rocks of gabbroic to dioritic composition. It is hosted by a sequence of komatiitic basalts and komatiites of the Lower Onverwacht Group. The intrusion is considered unique in this area in that it lacks ultramafic components and has no affinities with the surrounding mafic- to- ultramafic lavas. The gabbroic suite also contains an unusual abundance of quartz, and the chill margin shows an evolved quartz-normative, tholeiitic parental magma. Based on petrographic and geochemical evidence, the intrusion can be subdivided into four gabbroic zones and a quartz diorite, which is an end product of a differentiating magma. The chill margin records an MgO content of 4.8%, an Mg# of 42, an Si02 value of 52.5% and a normative plagioclase composition of An 44. The sill-like nature of the body, indicated by geochemical trends, and the steep sub-vertical layering, point to a body that has been tilted along with the surrounding lavas. -
Our Glorious AFS Itinerary Jun 17 Air Is
Our Glorious AFS Itinerary Jun 17 Air is so easy round-trip to Jo’burg (JNB)! Full details to come on this in AFS Trip Tips with info about flights, overnight options, packing, etc. We urge you to fly in a day early to arrive Jun 18. Full details to come on all air options, overnight options and packing in AFS trips tips. Day 1: Fri, Jun 19 Chisomo Safari Camp, Kruger Private Reserves Our land tour officially begins! We gather early morning at JNB Airport and fly an hour to Kruger. We arrive in time for lunch and a short rest before heading out on your first afternoon game drive. South Africa This vast country is undoubtedly one of the most culturally and geographically diverse places on earth. Fondly known by locals as the 'Rainbow Nation', South Africa has 11 official languages and its multicultural inhabitants are influenced by a fascinating mix of cultures. Discover the gourmet restaurants, impressive art scene, vibrant nightlife and beautiful beaches of Cape Town; enjoy a local braai (barbecue) in the Soweto Township; browse the bustling Indian markets in Durban; or sample some of the world’s finest wines at the myriad wine estates dotting the Cape Winelands. Some historical attractions to explore include the Zululand battlefields of KwaZulu-Natal, the Apartheid Museum in Johannesburg and Robben Island, just off the coast of Cape Town. Above all else, its remarkably untamed wilderness with its astonishing range of wildlife roaming freely across massive unfenced game reserves such as the world-famous Kruger National Park. With all of this variety on offer, it is little wonder that South Africa has fast become Africa’s most popular tourist destination. -
Vaccination Sites: Ehlanzeni District Office 09
66 AndersonEnq: Mr Street IL Mtungwa, Nelspruit, 1200, Mpumalanga Province Private Bag X11278, Nelspruit, 1200, Mpumalanga Province Tel l: +27 (13) 755 5100, Fax: +27 (13) 752 7498 VACCINATION SITES: EHLANZENI DISTRICT OFFICE Litiko Letemphilo 09Departement – 14 AUGUST van Gesondheid 2021 UmNyango WezeMaphilo DATES SUB-DISTRICT SITES: NUMBER OF TARGET TEAM LEADER Pfizer VACCINATORS Nkomazi Phiva 6 240 MR NB Khoza Mdladla 6 240 MS MN Mpangane Dludluma 6 240 MS V Mkhatshwa Ngwenyeni 6 240 MS N Shongwe Bushbuckridge AFM Church (Majembeni) 4 160 Sydwell Mathebula Maromeng Nazarene 12 480 Audrey Mashego Church Hlangalezwe P School 5 200 Victress Mbokodo (Soweto Oakley) Swavana Dropping Centre 4 160 Sostina Maluleke 09/08/2021 Skukuza Community Hall 4 160 Martha Cibe Sesete P School(Whit City) 5 200 Beauty Chauke Thaba Chweu Lydenburg Civic Center 4 160 Gloria Manale Graskop Town Hall 4 160 Xolani Mnisi Sabie Municipal Hall 4 160 Sthembile Mnisi Simile Chamber 4 160 Sthembile Mnisi Sizabantu 4 160 Conrade Mashego VACCINATION SITES: EHLANZENI DISTRICT 09 – 14 AUGUST 2021 Leroro Community Hall 4 160 Mmathabo Mashego Nkomazi Magogeni 7 280 MS MN Mpangane Marloth Park 7 280 MR NB Khoza Komatipoort 7 280 MS N Shongwe City of Mbombela Fairview mine 04 200 ST Nkosi “South” Sikhulile old age home 02 100 L Nkosi centre Nelshoogte 04 150 B Nkosi City of Mbombela Mvangatini 05 200 Tholiwe Hade “North” Nkohlakalo hall Sifunindlela Mvangatini 06 240 NP Mazibane Nkohlakalo hall Sifunindlela 10/08/2021 Buyelani 05 200 C.N. Makutu Luphisi Whiteriver Hall 04 160 J.M. Maseko Hills view Hall 06 240 N.P. -
Nelspruit Phalaborwa Skukuza
ZIMBBABWE PHALABORWA Letaba Rest Camp Phalaborwa Gate LIMPOPO R71 TO TZANEEN Hans Merensky Golf KRUGER NATIONAL PARK BOTSWANA Polokwane er r ts Riv ive SELATI lifan i R r O m Phalaborwa e alu R526 lar Riv h PALABORWA N e Pondoro Game Lodge i AIRPORT r r e ve Pretoria Garonga Safari s i R40 a R Mafikeng Skukuza Camp l UMBAMBAT ti Johannesburg K va MPUMALANGA ba NAMIBIA NORTH WEST MAKALALI BALULE im Klerksdorp GAUTENG KLASERIE Motswari T MICA Nelspruit Makalali Simbavati Tshukudu Africa on Foot R530 Kings Camp nThambo Tree Camp Singita Lebombo EASTGATE Gomo Gomo Tanda Tula & Singita Sweni Upington FREE STATE Timbavati Kimberley KWA ZULU AIRPORT Umlani Hluhluwe Hoedspruit Gate Bloemfontein NATAL LIMPOPO Kambaku &Beyond Ngala Safari Lodge THORNYBUSH Pietermaritzburg R527 31 Thornybush Game Lodge Main Camp 31 32 Chapungu Luxury Tented Camp NORTHEN CAPE LESOTHO d 33 Shumbalala Game Lodge Durban KAPAMA1.37 Exeter32 River LodgeTIMBAVATI 34 34 Serondella Lodge Roa 35 Royal Malewane KAPAMA 39 38 33 Hamiltons, Hoyo-Hoyo 37 Camp Jabulani & Imbali Lodges 36 Jackalberry Lodge R531 41 sey THORNYBUSH 38 Kapama Main Lodge Hoedspruit n Satara Rest Camp r Ngala Tented Camp Umtata 39 Kapama River Lodge Endangered 40 e Orpen Gate 40 Kapama Karula Species Centre u 36 35 G 41 Moholoholo Honeyguide Khoka Moya & Mantobeni Camps EASTERN CAPE RehabilitationKl aserie R531 Centre Tintswalo Safari Lodge & Manor House WESTERN CAPE East London Acorn Hoek Cape Town D406 SABI SANDS Port Elizabeth MANYELETI Mossel Bay 17 Arathusa Safari Lodge BLYDE RIVER CANYON 18 Djuma Vuyatela Lodge Gowrie Gate 19 Cheetah Plains Lodge NATURE RESERVE 42 20 Simbambili Game Lodge 21 Nkorho Bush Lodge 20 18 22 Chitwa Chitwa Game Lodge Kruger National Park SABI SANDS 42 Elephant Plains 1 &Beyond Exeter River Lodge 17 2 &Beyond Exeter Dulini Lodge 22 21 3 &Beyond Exeter Kirkman’s Kamp Where nearly 2 million hectares of unrivalled diversity of life forms fuses with historical and archaeological sites - 4 Ulusaba Safari Lodge 19 7 1 this is real Africa. -
Phase 1 AIA / HIA Sabie Hydro Project, Hazyview
SPECIALIST REPORT PHASE 1 ARCHAEOLOGICAL / HERITAGE IMPACT ASSESSMENT FOR PROPOSED SABIE HYDRO POWER (PTY Ltd) PROJECT, ON PORTION 17 OF THE FARM TEVREDE 178 JT, HAZYVIEW, MPUMALANGA PROVINCE REPORT COMPILED FOR RHENGU ENVIRONMENTAL SERVICES MR. RALF KALWA P.O. Box 1046, MALELANE, 1320 Cell: 0824147088 / Fax: 0866858003 / e-mail: [email protected] SEPTEMBER 2016 ADANSONIA HERITAGE CONSULTANTS ASSOCIATION OF SOUTHERN AFRICAN PROFESSIONAL ARCHAEOLOGISTS C. VAN WYK ROWE E-MAIL: [email protected] Tel: 0828719553 / Fax: 0867151639 P.O. BOX 75, PILGRIM'S REST, 1290 1 EXECUTIVE SUMMARY A Phase 1 Heritage Impact Assessment (HIA) regarding archaeological and other cultural heritage resources was conducted on the footprint for the proposed Sabie Hydro Power project next to the Sabie River near Hazyview. The study area is located on portion 17 of the farm TEVREDE 178JT, Hazyview. The farm is situated on topographical maps, 1:50 000, 2530 BB (SABIE) & 2531 AA (KIEPERSOL), which is in the Mpumalanga Province. The study area is situated on 2530 BB SABIE. This area falls under the jurisdiction of the Ehlanzeni District Municipality, and Thaba Chweu Local Municipality. The National Heritage Resources Act, no 25 (1999)(NHRA), protects all heritage resources, which are classified as national estate. The NHRA stipulates that any person who intends to undertake a development, is subjected to the provisions of the Act. The applicants (private landowner with some shareholders) in co-operation with Rhengu Environmental Services are requesting the establishment of a hydro facility on the Sabie River near Hazyview. There was a hydro facility on the farm approximately 40 years ago and the new one will follow more or less the same route and alignment. -
Seasonal Metal Speciation in the Sabie River Catchment, Mpumalanga, South Africa
18th JOHANNESBURG Int'l Conference on Science, Engineering, Technology & Waste Management (SETWM-20) Nov. 16-17, 2020 Johannesburg (SA) Seasonal Metal Speciation in the Sabie River Catchment, Mpumalanga, South Africa 1,2R. Lusunzi, 1E. Fosso-Kankeu, 1F. Waanders of water. Abstract - The present study investigated the hydrochemical Various anthropogenic sources which include mining, characteristic changes of the Sabie River catchment. Water sampling agricultural activities and industrial wastewater contribute to was done in November and December (wet season, 2019) and July pollution of surface water [1], [2]. Various factors that influence (Dry season, 2020). Physicochemical parameters and metal speciation were analyzed to assess their impact on water quality and fitness for the mobility of the likely or definite contaminants from human consumption. The hydrochemical characteristics of Sabie anthropogenic activities such as mining and mineral processing catchment showed variation of quality with seasons when compared activities had been described [3] and [4]. These factors include with drinking water guidelines. Seepage from Nestor tailings storage occurrence, abundance, reactivity and hydrology. The term facility (TSF) was also collected during wet season. In both season, species had been defined as different forms of a particular aqueous metal speciation was done using the PHREEQC geochemical 2+ 2- element or its compounds [5]. For this study, the term speciation modelling code. Higher concentrations of Ca and SO4 were found in mine water while the dominant anion and cation were Mg2+ and Cl- had been used to indicate the distribution of species in samples in surface water samples. Additionally, the seasonal variation in the from the Sabie catchment. -
River Flow and Quality
Setting the Thresholds of Potential Concern for River Flow and Quality Rationale All of the seven major rivers which flow in an easterly direction through the Kruger National Park (KNP) originate in the higher lying areas west of the KNP where they are highly utilised (Du Toit, Rogers and Biggs 2003). The KNP lies in a relatively arid (490 mm KNP average rainfall) area and thus the rivers are a crucially important component for the conservation of biodiversity in the KNP (Du Toit, Rogers and Biggs 2003). Population growth in the eastern Lowveld of South Africa during the past three decades has brought with it numerous environmental challenges. These include, but are not limited to, extensive planting of exotic plantations, overgrazing, erosion, over-utilisation and pollution of rivers, as well as clearing of indigenous forests from large areas in the upper catchments outside the borders of the KNP. The degradation of each river varies in character, intensity and causes with a substantial impact on downstream users. The successful management of these rivers poses one of the most serious challenges to the KNP. However, over the past 10 years South Africa has revolutionised its water legislation (National Water Act, Act number 36 of 1998). This Act substantially elevated the status of the environmental needs, through defining the ecological reserve as a priority water requirement. In other words this entails water of sufficient flow and quality to maintain the integrity of the ecological system, including the water therein, for human use. With the current levels of abstraction in the upper catchments, the KNP quite simply does not receive the water quantity and quality required to maintain the in-stream biota. -
Mpumalanga Biodiversity Conservation Plan Handbook
cove 3/5/07 0:59 age 3 MPUMALANGA BIODIVERSITY CONSERVATION PLAN HANDBOOK Tony A. Ferrar and Mervyn C. Lötter S C ON CC O D 3/ /07 8: 3 age MPUMALANGA BIODIVERSITY CONSERVATION PLAN HANDBOOK AUTHORS Tony A. Ferrar1 and Mervyn C. Lötter2 CONTRIBUTIONS BY Brian Morris3 Karen Vickers4 Mathieu Rouget4 Mandy Driver4 Charles Ngobeni2 Johan Engelbrecht2 Anton Linström2 Sandy Ferrar1 This handbook forms part of the three products produced during the compilation of the Mpumalanga Biodiversity Conservation Plan (MBCP). CITATION: Ferrar, A.A. & Lötter, M.C. 2007. Mpumalanga Biodiversity Conservation Plan Handbook. Mpumalanga Tourism & Parks Agency, Nelspruit. OTHER MBCP PRODUCTS INCLUDE: Lötter, M.C. & Ferrar, A.A. 2006. Mpumalanga Biodiversity Conservation Plan Map. Mpumalanga Tourism & Parks Agency, Nelspruit. Lötter. M.C. 2006. Mpumalanga Biodiversity Conservation Plan CD-Rom. Mpumalanga Tourism & Parks Board, Nelspruit. Affiliations: 1 Private, 2 MTPA, 3 DALA, 4 SANBI, i S C ON CC O D 3/7/07 0: 5 age ISBN: 978-0-620-38085-0 This handbook is published by the Mpumalanga Provincial Government, in Nelspruit, 2007. It may be freely copied, reproduced quoted and disseminated in any form, especially for educational and scientific purposes, provided the source is properly cited in each and all instances. The Mpumalanga Tourism and Parks Agency welcomes comment and feedback on the Handbook, in particular the identification of errors and omissions. Provision of new information that should be incorporated into any revised edition of the Biodiversity Plan or this handbook would be particularly appreciated. For this or any other correspondence please contact: MPUMALANGA TOURISM AND PARKS AGENCY SCIENTIFIC SERVICES TEL: 013 759 5300 Mpumalanga Tourism and Parks Agency S C ON CC O D 3/ /07 8: 3 age TABLE OF CONTENTS TABLE OF CONTENTS Acknowledgements iv Foreword v Acronyms vi Executive Summary vii 1.