Limpopo Fossil Heritage
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Limpopo Municipal Profiles
NCOP PROFILE OF MUNICIPALITIES There are three forms of financial misconduct that usually lead to public institutions receiving audit outcomes that are not satisfactory and these are unauthorised expenditure, fruitless and wasteful expenditure and irregular expenditure. Unauthorised expenditure is expenditure that was incurred without having been budgeted for; Irregular expenditure is expenditure that was incurred in violation of the requirements of legislation, such as the MFMA; and Fruitless and wasteful expenditure is expenditure that was incurred in a manner which could have been avoided had reasonable care been taken. Municipality Financial 2014/15 2015/16 2016/17 2017/18 2018/19 misconduct Modimolle- R59 888 880 R39 763 962 R19 521 858 R59 200 393 R141 408 216 Mookgophong Unauthorised R42 363 554 R20 708 225 R2 293 576 R76 343 632 R22 250 957 Irregular Fruitless & R5 129 187 R13 903 344 R28 010 002 R19 912 005 R47 533 002 Wasteful R1 099 604 Consultants Mogalakwena R47 929 088 R121 023 373 R286 527 038 R1 117 369 419 R2 845 387 113 Unauthorised R175 512 018 R487 490 102 R556 837 632 R373 685 032 R551 211 993 Irregular Fruitless & R385 320 R339 562 R597 327 R2 606 694 R11 305 709 Wasteful R54 089 284 Consultants Thabazimbi R30 815 935 R87 995 356 R32 018 831 R19 448 745 0 Unauthorised R13 231 860 R4 677 951 R1 601 978 R2 736 496 R39 495 921 Irregular Fruitless & R18 293 692 R25 414 892 R34 923 251 R10 412 593 R8 479 630 Wasteful R3 568 798 Consultants 1 WATERBERG DISTRICT THABAZIMBI LOCAL MUNICIPALITY Project Name Project Project Budget Project Project end Source Local employment Location start date date of Purpose of project Youth Adult People funding Male Female Male Female with disability 1. -
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. -
Timeline of Natural History
Timeline of natural history This timeline of natural history summarizes significant geological and Life timeline Ice Ages biological events from the formation of the 0 — Primates Quater nary Flowers ←Earliest apes Earth to the arrival of modern humans. P Birds h Mammals – Plants Dinosaurs Times are listed in millions of years, or Karo o a n ← Andean Tetrapoda megaanni (Ma). -50 0 — e Arthropods Molluscs r ←Cambrian explosion o ← Cryoge nian Ediacara biota – z ←Earliest animals o ←Earliest plants i Multicellular -1000 — c Contents life ←Sexual reproduction Dating of the Geologic record – P r The earliest Solar System -1500 — o t Precambrian Supereon – e r Eukaryotes Hadean Eon o -2000 — z o Archean Eon i Huron ian – c Eoarchean Era ←Oxygen crisis Paleoarchean Era -2500 — ←Atmospheric oxygen Mesoarchean Era – Photosynthesis Neoarchean Era Pong ola Proterozoic Eon -3000 — A r Paleoproterozoic Era c – h Siderian Period e a Rhyacian Period -3500 — n ←Earliest oxygen Orosirian Period Single-celled – life Statherian Period -4000 — ←Earliest life Mesoproterozoic Era H Calymmian Period a water – d e Ectasian Period a ←Earliest water Stenian Period -4500 — n ←Earth (−4540) (million years ago) Clickable Neoproterozoic Era ( Tonian Period Cryogenian Period Ediacaran Period Phanerozoic Eon Paleozoic Era Cambrian Period Ordovician Period Silurian Period Devonian Period Carboniferous Period Permian Period Mesozoic Era Triassic Period Jurassic Period Cretaceous Period Cenozoic Era Paleogene Period Neogene Period Quaternary Period Etymology of period names References See also External links Dating of the Geologic record The Geologic record is the strata (layers) of rock in the planet's crust and the science of geology is much concerned with the age and origin of all rocks to determine the history and formation of Earth and to understand the forces that have acted upon it. -
1 CHAPTER 1 GENERAL INTRODUCTION 1.1 Introduction
1 CHAPTER 1 GENERAL INTRODUCTION 1.1 Introduction People and things are given names for identification purposes. A name is a title given to a person or a thing. A name is defined by Sebashe (2003:12) as a word or words by which a person, animal, place or a thing is spoken of or referred to. In other words, a name distinguishes a particular thing from others. Names have political, social, economic and religious significance. As far as this study is concerned, the emphasis would be on the political significance of a name. The Black South Africans suffered a significant harm during the apartheid regime. The Europeans dominated in everything which resulted in Blacks losing their identity, culture, values, heritage an tradition. The European domination interfered with the naming patterns of the indigenous people of South Africa. Names of places were virtually Eurocentric. This is evident in town names, for example, Johannesburg, Pretoria, Pietersburg and Potgietersrus. Tables turned when a democratic government was elected in 1994. The affected people started to realize the negative impact of apartheid on numerous things, places names inclusive. The new government started to implement political changes. Some place names are changed to strike a balance between races, new places are named according to what the people want. Place naming starts to shift a distance away from Eurocentric to African names. Towns, streets, sporting facilities, names of settlements, businesses and 2 educational institutions are the most places affected by name changes and new naming patterns. 1.2 Background to the problem The problem of place naming in Africa in general and South Africa in particular started during the colonial period when many European countries scrambled for Africa in the 17th century. -
South Africa's Coalfields — a 2014 Perspective
International Journal of Coal Geology 132 (2014) 170–254 Contents lists available at ScienceDirect International Journal of Coal Geology journal homepage: www.elsevier.com/locate/ijcoalgeo South Africa's coalfields — A 2014 perspective P. John Hancox a,⁎,AnnetteE.Götzb,c a University of the Witwatersrand, School of Geosciences and Evolutionary Studies Institute, Private Bag 3, 2050 Wits, South Africa b University of Pretoria, Department of Geology, Private Bag X20, Hatfield, 0028 Pretoria, South Africa c Kazan Federal University, 18 Kremlyovskaya St., Kazan 420008, Republic of Tatarstan, Russian Federation article info abstract Article history: For well over a century and a half coal has played a vital role in South Africa's economy and currently bituminous Received 7 April 2014 coal is the primary energy source for domestic electricity generation, as well as being the feedstock for the Received in revised form 22 June 2014 production of a substantial percentage of the country's liquid fuels. It furthermore provides a considerable source Accepted 22 June 2014 of foreign revenue from exports. Available online 28 June 2014 Based on geographic considerations, and variations in the sedimentation, origin, formation, distribution and quality of the coals, 19 coalfields are generally recognised in South Africa. This paper provides an updated review Keywords: Gondwana coal of their exploration and exploitation histories, general geology, coal seam nomenclature and coal qualities. With- Permian in the various coalfields autocyclic variability is the norm rather than the exception, whereas allocyclic variability Triassic is much less so, and allows for the correlation of genetically related sequences. During the mid-Jurassic break up Coalfield of Gondwana most of the coal-bearing successions were intruded by dolerite. -
Subsurface Facies Analysis of the Devonian Berea Sandstone in Southeastern Ohio
SUBSURFACE FACIES ANALYSIS OF THE DEVONIAN BEREA SANDSTONE IN SOUTHEASTERN OHIO William T. Garnes A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2014 Committee: James Evans, Advisor Jeffrey Snyder Charles Onasch ii ABSTRACT James Evans, Advisor The Devonian Berea Sandstone is an internally complex, heterogeneous unit that appears prominently both in outcrop and subsurface in Ohio. While the unit is clearly deltaic in outcrops in northeastern Ohio, its depositional setting is more problematic in southeastern Ohio where it is only found in the subsurface. The goal of this project was to search for evidence of a barrier island/inlet channel depositional environment for the Berea Sandstone to assess whether the Berea Sandstone was deposited under conditions in southeastern Ohio unique from northeastern Ohio. This project involved looking at cores from 5 wells: 3426 (Athens Co.), 3425 (Meigs Co.), 3253 (Athens Co.), 3252 (Athens Co.), and 3251 (Athens Co.) In cores, the Berea Sandstone ranges from 2 to 10 m (8-32 ft) thick, with an average thickness of 6.3 m (20.7 ft). Core descriptions involved hand specimens, thin section descriptions, and core photography. In addition to these 5 wells, the gamma ray logs from 13 wells were used to interpret the architecture and lithologies of the Berea Sandstone in Athens Co. and Meigs Co. as well as surrounding Vinton, Washington, and Morgan counties. Analysis from this study shows evidence of deltaic lobe progradation, abandonment, and re-working. Evidence of interdistributary bays with shallow sub-tidal environments, as well as large sand bodies, is also present. -
Meandering in the Main Karoo Basin, Eastern Cape, South Africa FIELD TRIP LEADERS: Emese Bordy & Goonie Marsh
POST 10 Meandering in the main Karoo Basin, Eastern Cape, South Africa FIELD TRIP LEADERS: Emese Bordy & Goonie Marsh This comprehensive five day trip will take us through, via an unique route in the shortest travel time and distance, a geo-traverse through over 400 million years of South African geological history. The main focus of the field trip is the sedimentary fill of the southern main Karoo Basin, including the nature of some of the major Karoo intrusive and volcanic complexes of the Eastern Cape. Field Trip Leaders: Emese Bordy and Goonie Marsh Start: Port Elizabeth End: Port Elizabeth Dates: 3-8 September 2016 ITINERARY SUGGESTION OF FLIGHT BOOKING FROM CAPE TOWN TO PORT ELIZABETH: SOUTH AFRICAN AIRWAYS FLIGHT 1803 DEPARTING CAPE TOWN AT 07h00, ARRIVING PORT ELIZABETH AT 08h15 Day 1 3 September 2016, Saturday Arrival at Port Elizabeth Airport and transfer to Grahamstown Overnight at the Graham Hotel in Grahamstown BB via Addo Elephant Park Day 2 4 September 2016, Sunday Stop 1 : Overview of 400 million years of South African geological history though the rocks and landscape of Grahamstown, Eastern Cape. Topics covered: Cape and Karoo systems, formation of the main Karoo Basin and Cape Fold Belt, Gondwana breakup, Cenozoic sea level changes. Location : 1820 Settlers' Monument Features to be seen : Relationship of the geology and geomorphology Cape Fold Belt - large-scale geological and geomorphological features: Witteberg quartzite ridges with some mudstone lenses to the south (cut by the N2 national road) & to the north (called Botha’s Ridge) running across the horizon. City bowl overlying the E-W running contact between soft Witteberg mudstones to the south and Dwyka tillites to the north Flat peneplain underlain by hard silcretes (with Joza/ King’s Flat township on it), visible along the northeastern horizon. -
Limpopo Province Elim Hospital
Limpopo Province Elim Hospital - Complex Central/Provincial tertiary Hospital/s: Elim District Hospitals: Community Health Centre Primary Health Care: Regional Hospitals: None Siloam Hospital Bungeni Health Centre Watervall Clinic Lebowakgomo Hospital – Complex Central/Provincial tertiary Community Health Centre: Hospital/s: Lebowakgomo District Hospitals: None Primary Health Care Mokopane Regional Hospital Zebediela hospital Lebowakgomo zone B clinic Thabamoopo Pschiatry hospital Regional Hospital: None Mokopane Hospital – Complex Central/Provincial tertiary Hospital/s: None District Hospitals: Community Health Centre Primary Health Care Regional Hospitals Voortrekker Hopsital Thabaleshoba CHC Mokopane Zone 1 Mokopane Regional Hospital Mokopane Zone 2 Manyoga Clinic Letaba Hospital – Complex Central/Provincial tertiary Primary Health Care: None Hospital/s: None District Hospitals: Community Health Centre Regional Hospitals Kgapane Hospital Nkowankowa CHC Letaba Regional Hospital Van Velden Hospital Pietersburg/Mankweng-Seshego Hospital – Complex Central/Provincial tertiary Hospital/s District Hospitals: Community Healtcare Centre Primary Health Care Pietersburg Hospital/ Mankweng hospital Seshego Hospital Buite Clinic Seshego Clinic Regional Hospitals: None Evelyn Lekganyane Clinic Specialized Hospitals: Thabamoopo Pschiatry Mankweng Clinic Rethabile Clinic St Rita's – Complex Central/Provincial tertiary Community Healthcare Primary Health Care: None Hospital/s: None District Hospitals: Centre Regional Hospitals Jane Furse Hospital Phokoane -
The Sauropodomorph Biostratigraphy of the Elliot Formation of Southern Africa: Tracking the Evolution of Sauropodomorpha Across the Triassic–Jurassic Boundary
Editors' choice The sauropodomorph biostratigraphy of the Elliot Formation of southern Africa: Tracking the evolution of Sauropodomorpha across the Triassic–Jurassic boundary BLAIR W. MCPHEE, EMESE M. BORDY, LARA SCISCIO, and JONAH N. CHOINIERE McPhee, B.W., Bordy, E.M., Sciscio, L., and Choiniere, J.N. 2017. The sauropodomorph biostratigraphy of the Elliot Formation of southern Africa: Tracking the evolution of Sauropodomorpha across the Triassic–Jurassic boundary. Acta Palaeontologica Polonica 62 (3): 441–465. The latest Triassic is notable for coinciding with the dramatic decline of many previously dominant groups, followed by the rapid radiation of Dinosauria in the Early Jurassic. Among the most common terrestrial vertebrates from this time, sauropodomorph dinosaurs provide an important insight into the changing dynamics of the biota across the Triassic–Jurassic boundary. The Elliot Formation of South Africa and Lesotho preserves the richest assemblage of sauropodomorphs known from this age, and is a key index assemblage for biostratigraphic correlations with other simi- larly-aged global terrestrial deposits. Past assessments of Elliot Formation biostratigraphy were hampered by an overly simplistic biozonation scheme which divided it into a lower “Euskelosaurus” Range Zone and an upper Massospondylus Range Zone. Here we revise the zonation of the Elliot Formation by: (i) synthesizing the last three decades’ worth of fossil discoveries, taxonomic revision, and lithostratigraphic investigation; and (ii) systematically reappraising the strati- graphic provenance of important fossil locations. We then use our revised stratigraphic information in conjunction with phylogenetic character data to assess morphological disparity between Late Triassic and Early Jurassic sauropodomorph taxa. Our results demonstrate that the Early Jurassic upper Elliot Formation is considerably more taxonomically and morphologically diverse than previously thought. -
Eskom Holdings SOC Limited
Eskom Holdings SOC Limited Environmen tal Impact Assessment for the Proposed 1x40 0kV Tabor-Bokmakirie (Nzhelele) and 4 X 250MVA 400kV/132kV Nzhelele Mai n Transmission Station, Limpopo Province SOCIO-ECONOMIC IMPACT REPORT DEA EIA Reference Number: 14/12/16/3/3/2/317 NEAS Ref Number: DEA/EIA/0001132/2012 LDEDET Ref Number: 12/1/9/E-V178 Date: February 2013 Report Version: Draft 1 Lidwala Consulting Engineers (SA) (Pty) Ltd Randburg Office: Pretoria Office: 11th Church Avenue, Ruiterhof, Randburg, 2194, 1121 Hertzog Street, Office F005, Waverley, Pretoria, 0186, PO Box 4221, Northcliff, 2115. PO Box 32497, Waverley, Pretoria, 0135, Tel: 0861 543 9252 Tel/faxs: 0861 543 9252 Polokwane Office : Nelspruit Office: 128 Marshall Street, Amy Park no. 5, Polokwane 39 Emkhe Street, Nelpruit, 1200 PO Box 3558, Polokwane, 0700 PO Box 2930, Nelspruit, 1200 Tel: 0861 543 9252 Tel: 0861 543 9252 TABLE OF CONTENTS 1. Introduction 5 1.1. Methodology 5 2. Social impacts expected during all project stages: 5 3. Description of the socio-economic setting – demographic information regarding the area in which the proposed line will be constructed: 6 3.1 Demographic profiles 7 3.2 Economic activities, Tourism and farming: 9 3.2.2 Tourism 9 3.2.3 Farming in the MLM 10 3.3 Employment rates and livelihoods 12 3.4 Access to services 12 3.4.1 Electricity 12 3.4.2. Access to water and sanitation facilities 13 3.4.3 Waste management 14 3.4.4 Transport 14 3.4.5 Educational facilities and libraries 14 3.4.6 Health facilities 15 3.4.7 Telecommunication and Postal Services 15 3.5 Conclusions from the social and economic environment within which the new power line is planned 16 4. -
The Role of Fossils in Interpreting the Development of the Karoo Basin
Palaeon!. afr., 33,41-54 (1997) THE ROLE OF FOSSILS IN INTERPRETING THE DEVELOPMENT OF THE KAROO BASIN by P. J. Hancox· & B. S. Rubidge2 IGeology Department, University of the Witwatersrand, Private Bag 3, Wits 2050, South Africa 2Bernard Price Institute for Palaeontological Research, University of the Witwatersrand, Private Bag 3, Wits 2050, South Africa ABSTRACT The Permo-Carboniferous to Jurassic aged rocks oft1:J.e main Karoo Basin ofSouth Africa are world renowned for the wealth of synapsid reptile and early dinosaur fossils, which have allowed a ten-fold biostratigraphic subdivision ofthe Karoo Supergroup to be erected. The role offossils in interpreting the development of the Karoo Basin is not, however, restricted to biostratigraphic studies. Recent integrated sedimentological and palaeontological studies have helped in more precisely defming a number of problematical formational contacts within the Karoo Supergroup, as well as enhancing palaeoenvironmental reconstructions, and basin development models. KEYWORDS: Karoo Basin, Biostratigraphy, Palaeoenvironment, Basin Development. INTRODUCTION Invertebrate remains are important as indicators of The main Karoo Basin of South Africa preserves a facies genesis, including water temperature and salinity, retro-arc foreland basin fill (Cole 1992) deposited in as age indicators, and for their biostratigraphic potential. front of the actively rising Cape Fold Belt (CFB) in Fossil fish are relatively rare in the Karoo Supergroup, southwestern Gondwana. It is the deepest and but where present are useful indicators of gross stratigraphically most complete of several depositories palaeoenvironments (e.g. Keyser 1966) and also have of Permo-Carboniferous to Jurassic age in southern biostratigraphic potential (Jubb 1973; Bender et al. Africa and reflects changing depositional environments 1991). -
Red Data List Special Edition
Newsletter of the Southern African Botanical Diversity Network Volume 6 No. 3 ISSN 1027-4286 November 2001 Invasive Alien Plants Part 2 Southern Mozambique Expedition Living Plant Collections: Lowveld, Mozambique, Namibia REDSABONET NewsDATA Vol. 6 No. 3 November LIST 2001 SPECIAL EDITION153 c o n t e n t s Red Data List Features Special 157 Profile: Ezekeil Kwembeya ON OUR COVER: 158 Profile: Anthony Mapaura Ferraria schaeferi, a vulnerable 162 Red Data Lists in Southern Namibian near-endemic. 159 Tribute to Paseka Mafa (Photo: G. Owen-Smith) Africa: Past, Present, and Future 190 Proceedings of the GTI Cover Stories 169 Plant Red Data Books and Africa Regional Workshop the National Botanical 195 Herbarium Managers’ 162 Red Data List Special Institute Course 192 Invasive Alien Plants in 170 Mozambique RDL 199 11th SSC Workshop Southern Africa 209 Further Notes on South 196 Announcing the Southern 173 Gauteng Red Data Plant Africa’s Brachystegia Mozambique Expedition Policy spiciformis 202 Living Plant Collections: 175 Swaziland Flora Protection 212 African Botanic Gardens Mozambique Bill Congress for 2002 204 Living Plant Collections: 176 Lesotho’s State of 214 Index Herbariorum Update Namibia Environment Report 206 Living Plant Collections: 178 Marine Fishes: Are IUCN Lowveld, South Africa Red List Criteria Adequate? Book Reviews 179 Evaluating Data Deficient Taxa Against IUCN 223 Flowering Plants of the Criterion B Kalahari Dunes 180 Charcoal Production in 224 Water Plants of Namibia Malawi 225 Trees and Shrubs of the 183 Threatened