DOCSLIB.ORG

Hyacinthaceae

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Hyacinthaceae 112 Bothalia 33,1 (2003) LAMIACEAE THE CORRECT NAME FOR SALVIA THERMARA Salvia thennara, published in Bothalia 29: 100, 101 ACKNOWLEDGEMENT (Van Jaarsveld 1999) was named with reference to the Goudini warm springs near Worcester, Western Cape. Mr I am indebted to Mr John Lavranos for bringing this John Lavranos, a well-known succulent plant botanist, error to my attention. who is Greek-speaking, brought to my attention that this name is not correct. The Latin word for hot springs, REFERENCE derived from Greek is thermae. In the genitive it is ther- manim = of the hot springs. VAN JAARSVELD, E.J. 1999. Salvia thennara, a new species from the Western Cape, South Africa. Bothalia 29: 100, 101. The conect name is therefore: Salvia thermarum Van Jaarsv. E.J. VAN JAARSVELD* TYPE.—Western Cape, 3319 (Worcester): Badsberg, * National Botanical Institute, Kirstenbosch, Private Bag XI, 7735 Goudini Spa, near Worcester on the Slanghoek trail, 15 Dec. Claremont. 1997, (-CB), Van Jaarsveld & Vorster 15533 (NBG holo.). MS. received: 2002-10-23. HYACINTHACEAE A NEW SPECIES OF ORNITHOGALUM FROM EASTERN CAPE. SOUTH AFRICA Ornithogalum perdurans A.PDold & S.A. Ham- 1 mm broad, white. Capsule ovoid-acute, 4. 5-5.0 x 3-4 mer, sp. nov., O. jimcifolio Jacq. affinis sed folio semi- mm, deeply 3-lobed, membranous, fragile, apices sepa- tereti pagina supera tenuiter canaliculata atroviridi et tota rating, becoming erect at dehiscence, pale brown, peri- pagina rugosa cum sulcis plus minusve parallelis trans- anth segments persistent, drying and withering irregular- versis undulatisque et subinde trichomatibus brevibus ly, equal to or just longer than capsule, pale brown with rigidis albidis omnino differt. dark brown midrib. Seed angular, up to 1.4 x 0.5 mm, rugose, black. Eigure 10. TYPE.—Eastern Cape, 3325 (Port Elizabeth): Komma- dagga Earm, Kommadagga, (-BB), 500 m, 6-9-1999, Bold Ornithogalum perdurans falls into subgenus Aspasia & Hammer 4441 (GRA, holo.). (Salisb.) Oberm. emend. U.Mull.-Doblies & D.Miilk- Doblies section Linaspasia U.Mull.-Doblies & D.Miilk- Plant xerophytic, dwarf. Bulb globose, epigeal, 20-30 Doblies series Juncifolia U.Mull.-Doblies & D.Miilk- mm diam.; outer tunics thin, wrinkled, pale brownish Doblies together with O. juncifolium but is distinguished grey, not neck-forming; inner tunics thin, clasping, per- from that species (Obermeyer 1978; Muller-Doblies & sistent, transparent with green venation, narrowing Muller-Doblies 1996) primarily on vegetative characters, abruptly to leaf base. Leaves 4-13, persistent, semi-terete, although some differences also occur in floral morpholo- linear, 40-60 x 1.0-1. 4 mm, erect, wiry, twisting 2-3 gy (Table 2). The long-lived leaves (persisting for over times, narrowly channelled adaxially, apices subacute, two years), are almost black in colour and are semi-terete dark green (almost black), entire surface rugose with ± in section with a narrow groove along the upper surface parallel, undulating, transverse grooves, with occasional and weak longitudinal ribs on the abaxial surface, occa- short, stiff, whitish trichomes 0.6 mm long throughout. sional, scattered white trichomes are found throughout. Raceme solitary, 20-40-flowered; peduncle 190-250 mm The entire leaf surface is rugose with ± parallel, undulat- long, up to 1.2 mm diam., stiffly erect, glabrous, dark ing, transverse grooves within which fine sand particles shiny green; bracts deltoid, 4.4 x 2.8 mm, auriculate, are held firmly (Eigure 11 A, B), giving the leaf a dry, clasping, attenuate, transparent with fawn-coloured keel; dusty appearance, not easily removed even with wash- lower pedicels longest, held at ± 45°, 7 mm long, up to 0.8 ing. This phenomenon in the suborder Liliiflorae has mm diam., green. Perianth segments spreading-reflexed; been suggested to be an adaptation against herbivory, inner elliptic, up to 6.4 x 2.8 mm; outer ovate, 7. 0-7.4 x high insolation and wind abrasion (Neinhuis et al. 1996). up to 3.2 mm, pale fawn-coloured with thin, green midrib The leaves do not sheath at the base and, being persis- (turning brown at senescence), apices incurved. Stamens tent, do not form a fibrous neck of old leaf bases. The patent; filaments lanceolate, broadest just above base, specific epithet perdurans refers to the perennial leaves. flattened, white, outer up to 4.5 x 0.8 mm, inner up to 4.5 A single inflorescence is produced. The perianth seg- X 1.2- 1.6 mm; anthers ovoid, up to 1.4 x 0.6 mm; ovary ments are 6.4—7.4 mm long. The deciduous leaves of ovoid, up to 3 X 2 mm, green; style up to 2.5 mm long, O. juncifolium are filiform to linear (involute or flat), terete, white; stigma 3-lobed, densely glandular-haired. conspicuously longitudinally ribbed abaxially with . Bothalia 33,1 (2003) 113 FIGURE 10. —Oniitliogaliim perdu- rcms, Dold & Hammer 4441 A. plant habit; B, inflores- cence in bud; C, inflores- cence at anthesis; D. peri- anth. Scale bars: 10 mm. strigose margins (Figure IIC) and are green in colour. Although Obermeyer (1978) includes 16 synonyms Sheathing at the base, the leaves form a membranous for the variable O. juncifoliwn, only one of which is res- neck that persists and often later becomes fibrous. One to urrected by Muller-Doblies & Mliller-Doblies (1996), three inflorescences are produced. The perianth seg- type material of all of these has been examined and the ments are 7-10 mm long. leaf characters of O. perdumns are distinctive. O. comp- TABLE 2. —Morphological differences between Ornithogaliim perdumns and O. juncifoliiim 0. perdumns O. jimcifolium Leaf long-lived deciduous almost black variably green semi-terete filiform to linear weakly longitudinally ribbed and rugose with undulating strongly longitudinally ribbed transverse grooves occasional short, stiff, whitish trichomes throughout margin strigose not membranous sheathing basally membranous sheathing fibrous neck absent fibrous neck present or absent Raceme 1 1-3 Perianth segments 6.4—7.4 mm long 7-10 mm long . 114 Bothalia 33,1 (2003) . FIGURE 1 1 —A, B, D, Omithogulum perdunins, Dold & Hammer 4441 A, leaf surface with sand particles removed showing undulating trans- verse grooves; B, leaf surface showing strongly adhering sand particles; D, seed. C, O. jimcifolium, leaf showing longitudinally ribbed sur- face with strigose margin, Dold 447. Scale bars; 100 pm. turn Baker and O. sardienii Van Jaarsv, have erect, wiry Table Farm is Grahamstown Silcrete that comprises sil- leaves resembling those of O. perdurans, however the crete remnants overlying kaolinized bedrock (Johnson & former is distinguished by its flattened lamina, without Le Roux 1994). The soil is consequently very shallow and adhering sand particles, and conspicuously thickened, ± nutrient poor. The rock types at Kommadagga Farm are cartilaginous margin. Furthermore, the lower pedicels made up of the Kommadagga subgroup of the Witteberg are 2-3 mm long, whereas the lower pedicels of O, per- group comprising shales, siltstones and subordinate sand- durems are up to 7 mm long, O. sardienii is easily disting- stones (Toerien & Hill 1989). uished by its unique mucronate leaf and tuberculate ovary, Oruithogalnm perdurans is known from two localities. Table Farm, 12 km west of Grahamstown (33°10'50"S 26°25'15"E), at an altitude of 550 m, with an average annual rainfall of 389 mm (R, White pers. comm,. Table Farm, Grahamstown 2002), and Kommadagga Farm, 60 km west of Grahamstown (33°09'30"S 25°53'00"E), at 500 m, with an average annual rainfall of 420 mm (J, Moolman pers, comm,, Kommadagga Earm) (Eigure 12), The vegetation type is classified as Eastern Mixed Nama- Karoo by Hoffman ( 1996), which was previously known as Fakse Karroid Broken Veld (Acocks 1988), Dominant species at these localities are Aristida congesta, Felicia muricata, Merxmuellera dislicha, Nenax inicrophylla, Pentzia glohosa and Tragus koelerioides. Succulent species include Corpuscularia lehnuinnii. Euphorbia meloformis, E. gorgonis, Senecio radicans and Tricliodia- dema hulhosum. d’he geological formation underlying Bothalia 33.1 (2003) 115 In his description of Ornithogalum unifolium (= O. O. perdurans dyeri) from Table Farm, Dyer (1930) noted that the EASTERN CAPE. 3326 (Grahamstown): Table Farm, 12 km we.st species is associated with many other miniature species — of Grahamstown, (-BC), 550 m, 14-07-2001, Dold4431 (GRA). of specialized growth form, viz., Eriospennum dregei, Schizobasis cf. macowanii and Bulhine mesembryanthe- moides—in reality an undescribed species (H. Baijnath ACKNOWLEDGEMENTS pers. comm.) referred to as Bulbine dime’ by Vander- plank (1998). Dyer’s (1930) observation is supported by Rhodes University Joint Research Council and the the recent discovery of Brachystelma luteum (Peckover Cactus and Succulent Society of America are thanked for 1992) and a dwarf variant of Orthopterum waltoniae financial support. Nancy Lawrence is thanked for the (Hammer 2001) from the same locality. It is suggested Latin diagnosis. The curators of BOL, G, NBG and PRE that this high succulent species diversity is found on the are thanked for loans of type material. ecotone between Succulent Thicket in the east and Nama- Karoo in the west and deserves further investigation. Dyer (1930) however, did not collect or record Ornitho- REFERENCES galum perdurans despite its close proximity to O. uni- ACOCKS, J.P.H. 1988. Veld Types of South Africa, edn 3. Memoirs of likely to its cryptic habit evident folium, most due and the Botanical Sun-ey of South Africa No. 57. rarity. The (2000) conservation status category lUCN DYER. R.A. 1930. New species of Ornithogalum and Albuca from is applied to this species. Vulnerable (VU D2) Albany Division. Records of the Albany Museum 4: 1 1 1-1 15. 1- HAMMER, S. 2001. Rustles of Spring. Mesemb Study Group Bulletin Other specimens examined 16.2:31,32. HOFFMAN, T. 1996. Eastern Mixed Nama Karoo. In A.B.
Load more

Recommended publications
  • Statistical Based Regional Flood Frequency Estimation Study For
    Statistical Based Regional Flood Frequency Estimation Study for South Africa Using Systematic, Historical and Palaeoflood Data Pilot Study – Catchment Management Area 15 by D van Bladeren, P K Zawada and D Mahlangu SRK Consulting & Council for Geoscience Report to the Water Research Commission on the project “Statistical Based Regional Flood Frequency Estimation Study for South Africa using Systematic, Historical and Palaeoflood Data” WRC Report No 1260/1/07 ISBN 078-1-77005-537-7 March 2007 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 EXECUTIVE SUMMARY INTRODUCTION During the past 10 years South Africa has experienced several devastating flood events that highlighted the need for more accurate and reasonable flood estimation. The most notable events were those of 1995/96 in KwaZulu-Natal and north eastern areas, the November 1996 floods in the Southern Cape Region, the floods of February to March 2000 in the Limpopo, Mpumalanga and Eastern Cape provinces and the recent floods in March 2003 in Montagu in the Western Cape. These events emphasized the need for a standard approach to estimate flood probabilities before developments are initiated or existing developments evaluated for flood hazards. The flood peak magnitudes and probabilities of occurrence or return period required for flood lines are often overlooked, ignored or dealt with in a casual way with devastating effects. The National Disaster and new Water Act and the rapid rate at which developments are being planned will require the near mass production of flood peak probabilities across the country that should be consistent, realistic and reliable.
    [Show full text]
  • The Stratigraphy and Structure of the Kommadagga Subgroup and Contiguous Rocks
    THE STRATIGRAPHY AND STRUCTURE OF THE KOMMADAGGA SUBGROUP AND CONTIGUOUS ROCKS by ROGER SWART B.Sc . (Hons) Thesis presented in fulfilment of the requirements for the degree of Master of Science in the Department of Geology, Rhodes University ,Grahamstown. January 1982 ABSTRACT The Lake Mentz and Kommadagga Subgroups were deposited i n a marine environment and are characterised by a heterogeneous sequence of sediments, which range in grain size from clays to grits . During the first phase of deposition the Kwee~ vlei Shale and Floriskraal Formations were deposited in a prograding shoreline environment, whereas the succeeding Waaipoort Shale Formation is interpreted as represnting a reworked shoreline. The final phase of deposition of the Cape Supergroup was a regressive one in which the Kommadagga Subgroup wa s fo rmed. The coa rs eni ng upward cycle of thi s subgroup represents a deltaic deposit. A significant time gap appears to exist before the deposition of the glacial-marine Dwyka Tillite Formation. Structurally, the area was subjected to deformation by buckle folding at about 250 Ma into a series of folds with southward dipping axial planes. Only one phase of deformation is recognised in the study area . A decrease in pore space, mineral overgrowths,formation of silica and calcite cements and development of aut~igenic minerals such as opal, stilpnomelane; analcite, prehnite, muscovite and various clay minerals are the characteristic diagenetic features of the sediments.The mineralogical evidence suggests that the maximum temperature
    [Show full text]
  • In the Eastern Cape, South Africa
    Bothalia 28,2: 141-149 (1998) A revision of Lachenalia (Hyacinthaceae) in the Eastern Cape, South Africa A.P. DOLD* and P.B. PHILLIPSON* Keywords: Eastern Cape, Hyacinthaceae, Luchenalui Jacq.f. ex Murray, South Africa, taxonomy ABSTRACT A taxonomic account of the genus Lacheiuiliii Jacq.f. ex Murray in the Eastern Cape, South Africa, is given. Eight species are recognised, and descriptions of these are amended and elaborated as necessary, three taxa have been reduced to synonymy and five species erroneously recorded within the province are excluded Three of the species are endemic to the province. An identification key is provided. INTRODUCTION & De Wet 1993 for references) and Duncan (1988, 1996, 1997), has resulted in the species from Western Cape The genus Lachenalia is confined to southern Africa becoming reasonably well known taxonomically. The and consists of a little over 100 species (Arnold & De same cannot be said for the Eastern Cape species. They Wet 1993). The majority of these species occur in the have mostly been unknown in cultivation, and they are winter rainfall region of the Western Cape in the sclero- generally represented only by few, rather old herbarium phyllous shrublands or ‘fynbos’ ol the Cape floristic specimens. region (sensu White 1983). The geographic range of a few species extends from this region into the western In the course of field work in the Eastern Cape it parts of the Eastern Cape and one even occurs as far became clear that Baker’s treatment was far from ade­ northeast as the Free State. The few remaining species quate.
    [Show full text]
  • DOWNLOAD the APP 94 95 Overview of Nelson Mandela Bay
    AuthenticAuthentic ExperiencesExperiences addo river safaris addo full day tours addo half day tours Test-drive our technology! Our revamped AutoPavilion features: • A kids’ experiential zone with driving simulators, colouring-in stations, ttoouurr,, ssaaffaarrii && aaddvveennttuurree ssppeecciiaalliissttss interactive displays and more • The newest addition to our much-loved Beetle family, Foxy Lady Disco Queen • The only Volkswagen XL1 hybrid concept car in South Africa • Visit the gift shop and take home your addo eco quad biking beach safari’s, sandboarding sledding and ferry rides piece of our Volkswagen brand Opening hours: Weekdays 08h30 - 16h00 and every first Saturday of the month 10h00 - 13h00. Closed all other weekends and public holidays. Open for all ages…Beetle fans especially welcome! fresh & salt water fishing river conservation & hiking birdwatching & photography www.crisscrossadventures.co.za CrisscrossAddo [email protected] +27 (0)83 330 0480 Crisscross Adventures - Addo CrissCross_Adventures 3 CONTENTS HALLO FROM NELSON MANDELA BAY 8 - 15 Warm Welcome 8 NMBT’s Visitor Information Centre’s 9 Tribute to Nelson Mandela 10 Important Information 12 – 14 Practical Safety Tips 15 HISTORICAL ATTRACTIONS 16 - 23 Port Elizabeth 16 - 20 Despatch 21 Uitenhage 22 - 23 WONDERFUL WILDLIFe and NATURE 24 - 33 Game Viewing 4, 24 - 29 Adventure Activities 2, 30 – 31, 37 The Great Outdoors 32 - 33 BEACHES, WATERSPORT and SPORTS 34 - 43 Beautiful Beaches 34 - 35 Wind & Watersport 36 – 39, 95 Dolphin Capital 40 Sports Scene
    [Show full text]
  • Blue Crane Route Local Municipality (Ec102)
    BLUE CRANE ROUTE LOCAL MUNICIPALITY (EC102) FINAL INTEGRATED DEVELOPMENT PLAN REVIEW 2020-2021 TABLED TO COUNCIL 3 JUNE 2020 Final Integrated Development Plan Review 2020-2021 Page 1 ABBREVIATIONS AND ACRONYMS AFS Annual Financial Statement AIDS Acquired Immune Deficiency Syndrome ASGISA Accelerated and Shared Growth Initiative for South Africa BCRM Blue Crane Route Municipality CDA Cacadu Development Agency CGTA Cooperative Governance and Traditional Affairs CPEX Capital Expenditure DEDEA Department of Economic Development and Environmental Affairs DFA Development Facilitation Act DLG&TA Department of Local Government and Traditional Affairs DOH Department of Health DOT Department of Transport DRPW Department of Roads and Public Works DSRAC Department of Sport, Recreation, Arts and Culture DWA Department of Water ECDC Eastern Cape Development Corporation ESKOM Electricity Supply Commission FMG Finance Municipal Grant GAMAP Generally Accepted Municipal Accounting Policies GDS Growth and Development Summit GGP Gross Geographic Product GRAP General Recognized Accounting Practise HIV Human Immunodeficiency Virus HR Human Resource ICT Information & Communication Technology IDC Industrial Development Corporation IDEA Individuals with Disabilities Education Act IDP Integrated Development Plan Final Integrated Development Plan Review 2020-2021 Page 2 ITP Integrated Transport Plan JIPSA Joint Initiative on Priority Skills Acquisition KPA Key Performance Areas KPI Key Performance Indicators LED Local Economic Development LLF Local Labour Forum
    [Show full text]
  • 3 Description of the Affected Environment
    3 DESCRIPTION OF THE AFFECTED ENVIRONMENT In terms of section 31 (2) of the EIA regulations (2010), an environmental impact assessment report must include:- (d) A description of the environment that may be affected by the activity and the manner in which the physical, biological, social, economic and cultural aspects of the environment may be affected by the proposed activity In line with the above-mentioned regulatory requirement this chapter provides a description of the natural and socio-economic environments that could potentially be impacted by the proposed Plan 8 Grahamstown Wind Energy Project. Previous studies have included detailed descriptions of the general characteristics of the area in terms of climate, topography, hydrology, geology and hydro- geology, and a synthesis of this information is provided in this chapter. Descriptions of the flora and fauna are based on on-site investigations and a survey of the relevant literature to determine what could legitimately be expected to be found in the study area. 3.1 The Bio-physical Environment 3.1.1 Climate Due to its the location at the confluence of the temperate and subtropical climatic regimes the Eastern Cape Province of South Africa has a complex climate. There are wide variations in temperature, rainfall and wind patterns, mainly as a result of movements of air masses, altitude, mountain orientation and the proximity of the Indian Ocean. The region in which the project area is situated is at the heart of three major transitional climatic regions: 1. From the south-western region there is a maritime influence of winter rainfall. In this region it changes to spring and autumn rainfall with south easterly winds bringing torrential rains which are very variable and inconsistent.
    [Show full text]
  • A Multivariate Analysis of Variation in Cineraria Lobata L'hér. and C
    Available online at www.sciencedirect.com South African Journal of Botany 73 (2007) 530–545 www.elsevier.com/locate/sajb A multivariate analysis of variation in Cineraria lobata L'Hér. and C. ngwenyensis Cron ⁎ G.V. Cron a, , K. Balkwill a, E.B. Knox b a School of Animal, Plant and Environmental Sciences, University of the Witwatersrand, Private Bag 3, Wits 2050, South Africa b Department of Biology, Indiana University, Bloomington, IN 47405, USA Received 16 August 2006; received in revised form 23 April 2007; accepted 25 April 2007 Abstract Cineraria lobata is a highly variable species centred in the Western and Eastern Cape Provinces, South Africa, with disjunct populations in Mpumalanga and Limpopo Provinces. Morphological variation was examined in order to delimit the species and to determine whether recognition at infraspecific levels was warranted. Plants from the Ngwenya Hills, Swaziland, similar to C. lobata in leaf shape and size, but with glabrous cypselae and a distinct type of trichome, are recognized as a distinct, but closely related species, C. ngwenyensis. Cluster Analysis and Principal Coordinates Analysis supported the recognition of four subspecies in C. lobata: from the Western Cape (ssp. lobata), Karoo (ssp. lasiocaulis), Soutpansberg (ssp. soutpansbergensis) and Eastern Cape (ssp. platyptera) regions. Five forms of C. lobata ssp. lobata from the Western Cape are also informally recognised. © 2007 SAAB. Published by Elsevier B.V. All rights reserved. Keywords: Cineraria; Cluster analysis; Compositae; Infraspecific variation; Principal Coordinates Analysis; Senecioneae 1. Introduction gascar. Cineraria is essentially an afromontane genus, with its centre of diversity in KwaZulu-Natal, followed closely by the Cineraria L.
    [Show full text]
  • Fronteer Wind Farm, Eastern Cape Province Basic Assessment Report March 2021
    Fronteer Wind Farm, Eastern Cape Province Basic Assessment Report March 2021 FRONTEER WIND FARM, EASTERN CAPE PROVINCE COMMENTS AND RESPONSES REPORT TABLE OF CONTENTS PAGE 1. COMMENTS RECEIVED DURING THE COMMENCEMENT OF THE BASIC ASSESSMENT PROCESS .............................................................................. 1 1.1. Organs of State .................................................................................................................................................................................................................................. 1 1.2. Key Stakeholders and Interested & Affected Parties .................................................................................................................................................................... 5 The Fronteer Wind Farm Basic Assessment (BA) Process was announced together with the Development of a Cluster of Renewable Energy Facilities located between Somerset East and Makhanda, Eastern Cape Province on Tuesday, 17 November 2020. The Background Information Document was distributed together with a notification letter which served to invite Interested and Affected Parties (I&APs) to register their interest in the project and to submit any comments / queries that they might have on any of the proposed developments or all. All written comments received during the BA process to date have been included in the table below and included in Appendix C7 of the Basic Assessment (BA) Report. The Basic Assessment (BA) Report is available for a 30-day review
    [Show full text]
  • Addo Elephant National Park – Geology
    Addo Elephant National Park – Geology Introduction Before we start, one must remember that we live on a dynamic planet, which is permanently changing and evolving. The earth has a radius of about 6 300km and is covered by a 40km thick crust. The surface crust is continuously being driven by convection currents in the underlying mantle. This causes the crustal plates (continents and oceans) to move relative to each other, a process called “continental drift”. Crustal plates can drift (float) from the warmer tropics to the colder pole regions, all the time changing the way in which a landscape evolves. The combination of earth processes and climatic conditions has a significant impact on the final landscape appearance. The oldest rocks – Peninsula formation quartzitic sandstone The easiest way to describe the geological evolution of the Park is to start with the oldest rocks and work our way towards the present. Our story begins when Africa was joined to a number of other continents to form a super continent called “Pangea”. We (South Africa) were stuck in the middle of this land mass and our landscape was, therefore, very different to what one sees today. The oldest rocks encountered in the Park occur as small islands in Algoa Bay. The Bird Island complex comprises Black Rock, Stag, Seal and Bird Islands and occurs about 10 km south of the Woody Cape cliffs. These rocky islands are made up of quartzitic sandstone of the Peninsula Formation, which forms part of the Table Mountain Group, which in turn forms part of the Cape Supergroup.
    [Show full text]
  • Eastern Cape No Fee Schools 2021
    EASTERN CAPE NO FEE SCHOOLS 2021 NATIONAL NAME OF SCHOOL SCHOOL PHASE ADDRESS OF SCHOOL EDUCATION DISTRICT QUINTILE LEARNER EMIS 2021 NUMBERS NUMBER 2021 200600003 AM ZANTSI SENIOR SECONDARY SCHOOL SECONDARY Manzimahle A/A,Cala,Cala,5455 CHRIS HANI EAST 1 583 200300003 AMABELE SENIOR SECONDARY SCHOOL SECONDARY Dyosini A/A,Ndabakazi,Ndabakazi,4962 AMATHOLE EAST 1 279 200300005 AMABHELENI JUNIOR SECONDARY SCHOOL PRIMARY Candu Aa,Dutywa,5000 AMATHOLE EAST 1 154 200400006 AMAMBALU JUNIOR SECONDARY SCHOOL COMBINED Xorana Administrative Area,Mqanduli,5080 O R TAMBO INLAND 1 88 200300717 AMAMBALU PRIMARY SCHOOL PRIMARY Qombolo A/A,Centane,4980 AMATHOLE EAST 1 148 200600196 AMOS MLUNGWANA PRIMARY SCHOOL PRIMARY Erf 5252,Extension 15,Cala,5455 CHRIS HANI EAST 1 338 200300006 ANTA JUNIOR PRIMARY SCHOOL PRIMARY Msintsana A/A,Teko 'C',Centane,4980 AMATHOLE EAST 1 250 200500004 ANTIOCH PRIMARY SCHOOL PRIMARY Nqalweni Aa,Mount Frere,5090 ALFRED NZO WEST 1 129 200500006 AZARIEL SENIOR SECONDARY SCHOOL SECONDARY AZARIEL LOCATION, P.O BOX 238, MATATIELE, 4730 ALFRED NZO WEST 1 520 200600021 B A MBAM JUNIOR PRIMARY SCHOOL PRIMARY Bankies Village,N/A,Lady Frere,5410 CHRIS HANI WEST 1 104 200600022 B B MDLEDLE JUNIOR SECONDARY SCHOOL COMBINED Askeaton A/A,Cala,5455 CHRIS HANI EAST 1 615 200300007 B SANDILE SENIOR PRIMARY SCHOOL PRIMARY Qombolo A/A,Nqileni Location,Kentani,4980 AMATHOLE EAST 1 188 200500007 BABANE SENIOR PRIMARY SCHOOL PRIMARY RAMZI A/A, PRIVATE BAG 505, FLAGSTAFF 4810, 4810 O R TAMBO COASTAL 1 276 200500008 BABHEKE SENIOR PRIMARY SCHOOL
    [Show full text]
  • 40549 20-1 Roadcarrierp
    Government Gazette Staatskoerant REPUBLIC OF SOUTH AFRICA REPUBLIEK VAN SUID AFRIKA Regulation Gazette No. 10177 Regulasiekoerant January Vol. 619 20 2017 No. 40549 Januarie PART 1 OF 2 ISSN 1682-5843 N.B. The Government Printing Works will 40549 not be held responsible for the quality of “Hard Copies” or “Electronic Files” submitted for publication purposes 9 771682 584003 AIDS HELPLINE: 0800-0123-22 Prevention is the cure 2 No. 40549 GOVERNMENT GAZETTE, 20 JANUARY 2017 14/1/1 Tel : (012) 748-6066 Fax : (012) 323-9574 E-mail : [email protected] 20 October 2016 Dear Value Customers The 27th of December 2016 has been declared as a public holiday by the State President Mr Jacob Zuma. For this reason, the closing date of all gazettes during that week will be a day before scheduled dates as published in the gazette or on the website. Sincerely, Maureen Toka Acting Assistant Director: Publications (Tel): 012 748-6066 This gazette is also available free online at www.gpwonline.co.za STAATSKOERANT, 20 JANUARIE 2017 No. 40549 3 IMPORTANT NOTICE: THE GOVERNMENT PRINTING WORKS WILL NOT BE HELD RESPONSIBLE FOR ANY ERRORS THAT MIGHT OCCUR DUE TO THE SUBMISSION OF INCOMPLETE / INCORRECT / ILLEGIBLE COPY. NO FUTURE QUERIES WILL BE HANDLED IN CONNECTION WITH THE ABOVE. Contents Page No. Transport, Department of Cross Border Road Transport Agency: Applications for Permits Menlyn .............................................................................................................................................................................4
    [Show full text]
  • Palaeontological Heritage of the Eastern Cape
    PALAEONTOLOGICAL HERITAGE OF THE EASTERN CAPE John Almond Natura Viva cc, CAPE TOWN Billy de Klerk Albany Museum, GRAHAMSTOWN Robert Gess Bernard Price Institute (Palaeontology), Wits University, JOHANNESBURG The Eastern Cape is the second largest province in South Africa, comprising some 14% of the area of the RSA. The population is about seven million. The province is renowned for its living biodiversity and it also boasts a rich fossil record stretching back some 560 million years. The majority of the provincial area is underlain by shallow marine, coastal and terrestrial sediments of Phanerozoic ( ie post- Precambrian) age that are known to contain fossils of some sort, or are potentially fossiliferous (See accompanying simplified geological map and stratigraphic chart, both produced by the Council for Geoscience, Pretoria). Among the palaeontological highlights of the Eastern Cape are: • diverse, high-latitude lacustrine to lagoonal biotas from the Late Devonian – Early Carboniferous Witteberg Group ( c. 360-345 Ma = million years ago). These include a variety of fish and vascular plants as well as rarer arthropods. • fish, reptiles and therapsids (“mammal-like reptiles”) from the Late Permian to Early Triassic Beaufort Group ( c. 266-250 Ma) • extraordinarily rich fossil floras from the Late Triassic Molteno Formation ( c. 220 Ma) • a range of Early Cretaceous dinosaurs and plant fossils from the Kirkwood Formation ( c. 135 Ma) • rich shelly marine faunas from the Early Cretaceous Sundays River Formation ( c. 135 Ma) • important coastal marine fossil biotas of the Algoa Group ranging from Eocene to Recent in age (50 to 0 Ma). Important fossil collections from the Eastern Cape are housed at several South African Institutions, such as: Iziko: South African Museum (Cape Town), Albany Museum (Grahamstown), Port Elizabeth Museum (Port Elizabeth), Bernard Price Institute for Palaeontology, Wits.
    [Show full text]