Corrosion Map of South Africa's Macro Atmosphere
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THE DIAZ EXPRESS (Pty) Ltd All Aboard the Diaz Express, a Fun Rail Experience in the Garden Route Region of South Africa
THE DIAZ EXPRESS (Pty) Ltd All aboard the Diaz Express, a fun rail experience in the Garden Route region of South Africa. Sit back and experience the lovely views over the Indian ocean, the river estuaries, the bridges, the tunnel, as the railway line meanders high above the seaside resorts and past the indigenous plant life of the Cape Floral Kingdom. The Diaz Express consists of three restored Wickham railcars, circa 1960, that operates on the existing Transnet Freight Rail infrastructure between George, the capital of the Southern Cape, and the seaside resort of Mossel Bay. With our variety of excursions we combine unsurpassed scenery, history, visits to quaint crafts shops and art galleries with gastronomic experiences par excellence!!! CONTACT US +27 (0) 82 450 7778 [email protected] www.diazexpress.co.za Reg No. 2014 / 241946 / 07 GEORGE AIRPORT SKIMMELKRANS STATION MAALGATE GREAT BRAK RIVER GLENTANA THE AMAZING RAILWAY LINE SEEPLAAS BETWEEN GEORGE AND MOSSEL BAY HARTENBOS MAP LEGEND Mossel Bay – Hartenbos shuttle Hartenbos – Glentana Lunch Excursion Hartenbos – Seeplaas Breakfast Excursion Great Brak – Maalgate Scenic Excursion PLEASE NOTE We also have a whole day excursion from Mossel Bay to to Maalgate, combining all of the above. MOSSEL BAY HARBOUR THE SEEPLAAS BREAKFAST RUN Right through the year (except the Dec school holiday) we depart from the Hartenbos station in Port Natal Ave (next to the restaurant “Dolf se Stasie”) at 09:00. Our destination is the boutique coffeeshop/art gallery Seeplaas where we enjoy a hearty breakfast at Seeplaas with stunning scenery and the artwork of Kenny Maloney. -
Lesotho Fourth National Report on Implementation of Convention on Biological Diversity
Lesotho Fourth National Report On Implementation of Convention on Biological Diversity December 2009 LIST OF ABBREVIATIONS AND ACRONYMS ADB African Development Bank CBD Convention on Biological Diversity CCF Community Conservation Forum CITES Convention on International Trade in Endangered Species CMBSL Conserving Mountain Biodiversity in Southern Lesotho COP Conference of Parties CPA Cattle Post Areas DANCED Danish Cooperation for Environment and Development DDT Di-nitro Di-phenyl Trichloroethane EA Environmental Assessment EIA Environmental Impact Assessment EMP Environmental Management Plan ERMA Environmental Resources Management Area EMPR Environmental Management for Poverty Reduction EPAP Environmental Policy and Action Plan EU Environmental Unit (s) GA Grazing Associations GCM Global Circulation Model GEF Global Environment Facility GMO Genetically Modified Organism (s) HIV/AIDS Human Immuno Virus/Acquired Immuno-Deficiency Syndrome HNRRIEP Highlands Natural Resources and Rural Income Enhancement Project IGP Income Generation Project (s) IUCN International Union for Conservation of Nature and Natural Resources LHDA Lesotho Highlands Development Authority LMO Living Modified Organism (s) Masl Meters above sea level MDTP Maloti-Drakensberg Transfrontier Conservation and Development Project MEAs Multi-lateral Environmental Agreements MOU Memorandum Of Understanding MRA Managed Resource Area NAP National Action Plan NBF National Biosafety Framework NBSAP National Biodiversity Strategy and Action Plan NEAP National Environmental Action -
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. -
Upper Mantle P and S Wave Velocity Structure of the Kalahari Craton And
RESEARCH LETTER Upper Mantle P and S Wave Velocity Structure of the 10.1029/2019GL084053 Kalahari Craton and Surrounding Proterozoic Key Points: • Thick cratonic lithosphere extends Terranes, Southern Africa beneath the Rehoboth Province and Kameron Ortiz1, Andrew Nyblade1,5 , Mark van der Meijde2, Hanneke Paulssen3 , parts of the northern Okwa Terrane 4 4 5 2,6 and Magondi Belt Motsamai Kwadiba , Onkgopotse Ntibinyane , Raymond Durrheim , Islam Fadel , • The northern edge of the greater and Kyle Homman1 Kalahari Craton lithosphere lies along the northern boundary of the 1Department of Geosciences, Pennsylvania State University, University Park, PA, USA, 2Faculty for Geo‐information Rehoboth Province and Magondi Science and Earth Observation (ITC), University of Twente, Enschede, Netherlands, 3Department of Earth Sciences, Belt 4 • Cratonic mantle lithosphere Faculty of Geosciences, Utrecht University, Utrecht, Netherlands, Botswana Geoscience Institute, Lobatse, Botswana, 5 6 beneath the Okwa Terrane and School of Geosciences, The University of the Witwatersrand, Johannesburg, South Africa, Geology Department, Faculty Magondi Belt may have been of Science, Helwan University, Ain Helwan, Egypt chemically altered by Proterozoic magmatic events Abstract New broadband seismic data from Botswana and South Africa have been combined with Supporting Information: existing data from the region to develop improved P and S wave velocity models for investigating the • Supporting Information S1 upper mantle structure of southern Africa. Higher craton‐like velocities are imaged beneath the Rehoboth Province and parts of the northern Okwa Terrane and the Magondi Belt, indicating that the Correspondence to: northern edge of the greater Kalahari Craton lithosphere lies along the northern boundary of these A. Nyblade, terranes. -
Pinnacle Point Cave 13B (Western Cape Province, South Africa) in Context: the Cape Floral Kingdom, Shellfish, and Modern Human Originsq
Journal of Human Evolution 59 (2010) 425e443 Contents lists available at ScienceDirect Journal of Human Evolution journal homepage: www.elsevier.com/locate/jhevol Pinnacle Point Cave 13B (Western Cape Province, South Africa) in context: The Cape Floral kingdom, shellfish, and modern human originsq Curtis W. Marean Institute of Human Origins, School of Human Evolution and Social Change, P.O. Box 872402, Arizona State University, Tempe, AZ 85287-2402, USA article info abstract Article history: Genetic and anatomical evidence suggests that Homo sapiens arose in Africa between 200 and 100 ka, Received 15 December 2009 and recent evidence suggests that complex cognition may have appeared between w164 and 75 ka. This Accepted 19 March 2010 evidence directs our focus to Marine Isotope Stage (MIS) 6, when from 195e123 ka the world was in a fluctuating but predominantly glacial stage, when much of Africa was cooler and drier, and when dated Keywords: archaeological sites are rare. Previously we have shown that humans had expanded their diet to include Middle Stone Age marine resources by w164 ka (Æ12 ka) at Pinnacle Point Cave 13B (PP13B) on the south coast of South Mossel Bay Africa, perhaps as a response to these harsh environmental conditions. The associated material culture Origins of modern humans documents an early use and modification of pigment, likely for symbolic behavior, as well as the production of bladelet stone tool technology, and there is now intriguing evidence for heat treatment of lithics. PP13B also includes a later sequence of MIS 5 occupations that document an adaptation that increasingly focuses on coastal resources. -
Dear Museum Friends Issue 6 of 201 Most Important
June 2011 Phone 044-620-3338 Fax 044-620-3176 Email: [email protected] www.greatbrakriver.co.za www.ourheritage.org.za Editor Rene’ de Kock Dear Museum Friends Issue 6 of 201 Most Important May is always a busy month at the museum. Our AGM took place on the 11th and Heritage Mossel much of the past committee was reelected for the April 2011-March 2012 year. Bay is holding its A. Chairperson Rene’ de Kock nd B. Heritage Nisde McRobert AGM on the 22 C. Secretary Hope de Kock June 2011 at 6.30 D. Treasurer Rodney McRobert pm. E. Additional Committee Members Coralie van Heerden, Kitty Munch, and Jan Nieuwoudt The Museum is The two members elected from the above to represent the museum on the Board of open Monday, Control are Nisde McRobert and Jan Nieuwoudt. We would like to welcome Jan Tuesday, Thursday Nieuwoudt who has a good deal of knowledge on Great Brak’s history. and Friday between 9 am and In addition was the bi-annual Arts and Crafts week organised by Hope de Kock 4 pm and on with the assistance of many of her craft class members. The standard this year Wednesdays from has been simply amazing and the work done by the class was outstanding with 9.00 to 12.30 pm. many new crafts being worked and on display. In-between these craft displays were a large collected Hopes next fund works by Vivian raising “Hands Holtzhouzen of Laotian On” crafts hand woven silks never workshop will be before seen. -
A Brief Botanical Survey Into Kumbira Forest, an Isolated Patch of Guineo-Congolian Biome
A peer-reviewed open-access journal PhytoKeys 65: 1–14 (2016)A brief botanical survey into Kumbira forest, an isolated patch... 1 doi: 10.3897/phytokeys.65.8679 CHECKLIST http://phytokeys.pensoft.net Launched to accelerate biodiversity research A brief botanical survey into Kumbira forest, an isolated patch of Guineo-Congolian biome Francisco M. P. Gonçalves1,2, David J. Goyder3 1 Herbarium of Lubango, ISCED-Huíla, Sarmento Rodrigues, S/N Lubango, Angola 2 University of Ham- burg, Biocentre Klein Flottbek, Ohnhorststr.18, 22609 Hamburg, Germany 3 Herbarium, Royal Botanic Gardens, Kew, Richmond, Surrey,TW9 3AB, UK Corresponding author: Francisco Maiato Pedro Gonçalves ([email protected]) Academic editor: D. Stevenson | Received 31 March 2016 | Accepted 31 May 2016 | Published 15 June 2016 Citation: Gonçalves FMP, Goyder DJ (2016) A brief botanical survey into Kumbira forest, an isolated patch of Guineo- Congolian biome. PhytoKeys 65: 1–14. doi: 10.3897/phytokeys.65.8679 Abstract Kumbira forest is a discrete patch of moist forest of Guineo-Congolian biome in Western Angola central scarp and runs through Cuanza Norte and Cuanza Sul province. The project aimed to document the floristic diversity of the Angolan escarpment, a combination of general walk-over survey, plant specimen collection and sight observation was used to aid the characterization of the vegetation. Over 100 plant specimens in flower or fruit were collected within four identified vegetation types. The list of species in- cludes two new records of Guineo-Congolian species in Angola, one new record for the country and one potential new species. Keywords Kumbira forest, Guineo-Congolian, floristic diversity Introduction Angola lies almost wholly within the southern zone of tropical grassland, bounded by tropical rain forest of the Congo in the north and by the Kalahari Desert in the south (Shaw 1947). -
Sonar Surveys for Bat Species Richness and Activity in the Southern Kalahari Desert, Kgalagadi Transfrontier Park, South Africa
diversity Article Sonar Surveys for Bat Species Richness and Activity in the Southern Kalahari Desert, Kgalagadi Transfrontier Park, South Africa Rick A. Adams 1,* and Gary Kwiecinski 2 1 School of Biological Sciences, University of Northern Colorado, Greeley, CO 80639, USA 2 Department of Biology, University of Scranton, Scranton, PA 18510, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-970-351-2057 Received: 27 March 2018; Accepted: 10 September 2018; Published: 18 September 2018 Abstract: Kgalagadi Transfrontier Park is located in northwestern South Africa and extends northeastward into Botswana. The park lies largely within the southern Kalahari Desert ecosystem where the Auob and Nassob rivers reach their confluence. Although these rivers run only about once every 100 years, or shortly after large thunderstorms, underground flows and seeps provide consistent surface water for the parks sparse vegetation and diverse wildlife. No formal studies on bats have previously occurred at Kgalagadi. We used SM2 + BAT ultrasonic detectors to survey 10 sites along the Auob and Nassob rivers from 5–16 April 2016. The units recorded 3960 call sequences that were analyzed using Kaleidoscope software for South African bats as well as visual determinations based on call structure attributes (low frequency, characteristic frequency, call duration, and bandwidth). We identified 12 species from four families: Rhinolophidae: Rhinolophus fumigatus. Molossidae: Chaerephon pumilus, and Sauromys petrophilus, Tadarida aegyptiaca; Miniopteridae: Miniopteris schreibersi (natalensis), Vespertilionidae: Laephotis botswanae, Myotis tricolor, Neoromicia capensis, N. nana, Pipistrellus hesperidus, Scotophilus dinganii, and S. viridus. The most abundant species during the survey period was N. capensis. We also used paired-site design to test for greater bat activity at water sources compared to dry sites, with dry sites being significantly more active. -
Physical Map Unit
AfricaAnnabelle ate apples in the purple poppies. © 2015Physical Thomas Teaching Tools Map Annabelle ate apples in the purple poppies. © 2015 Thomas TeachingUnit Tools Thanks for Your Purchase! I hope you and your students enjoy this product. If you have any questions, you may contact me at [email protected]. © 2015 Thomas Teaching Tools © 2015 Thomas Teaching Tools Terms of Use This teaching resource includes one single-teacher classroom license. Photocopying this copyrighted product is permissible only for one teacher for single classroom use and for teaching purposes only. Duplication of this resource, in whole or in part, for other individuals, teachers, schools, institutions, or for commercial use is strictly forbidden without written permission from the author. This product may not be distributed, posted, stored, displayed, or shared electronically, digitally, or otherwise, without written permission of the author, MandyAnnabelle Thomas. ate Copying apples any in thepart purple of this poppies. product and placing it on the internet in any form (even a personal/classroom website) is strictly forbidden© 2015 Thomas and is a Teaching violation Toolsof the Digital Millennium Copyright Act (DMCA). You may purchase additional licenses at a reduced price on the “My Purchases”Annabelle page of TpTate ifapples you wish in the to purpleshare withpoppies. your fellow teachers, department, or school. If you have any questions, you may contact me© 2015 at [email protected] Thomas Teaching Tools . Thanks for downloading this product! I hope you and your students enjoy this resource. Feedback is greatly appreciated. Please fee free to contact me if you have any questions. My TpT Store: https://www.teacherspayteachers.com/Store/Tho mas-Teaching-Tools © 2015 Thomas Teaching Tools © 2015 Thomas Teaching Tools Teaching Notes Planning Suggestions This map unit is a great addition to any study of Africa. -
A Review of the Impacts and Opportunities for African Urban Dragonflies
insects Review A Review of the Impacts and Opportunities for African Urban Dragonflies Charl Deacon * and Michael J. Samways Department of Conservation Ecology and Entomology, Stellenbosch University, Matieland, Stellenbosch 7600, South Africa; [email protected] * Correspondence: [email protected] Simple Summary: The expansion of urban areas in combination with climate change places great pressure on species found in freshwater habitats. Dragonflies are iconic freshwater organisms due to their large body sizes and striking coloration. They have been widely used to indicate the impacts of natural and human-mediated activities on freshwater communities, while also indicating the mitigation measures required to ensure their conservation. Here, we review the major threats to dragonflies in southern Africa, specifically those in urban areas. We also provide information on effective mitigation measures to protect dragonflies and other aquatic insects in urban spaces. Using three densely populated areas as case studies, we highlight some of the greatest challenges for dragonflies in South Africa. More importantly, we give a summary of current mitigation measures which have maintained dragonflies in urban spaces. In addition to these mitigation measures, public involvement and raising awareness contribute greatly to the common cause of protecting dragonflies around us. Abstract: Urban settlements range from small villages in rural areas to large metropoles with densely Citation: Deacon, C.; Samways, M.J. packed infrastructures. Urbanization presents many challenges to the maintenance of freshwater A Review of the Impacts and quality and conservation of freshwater biota, especially in Africa. There are many opportunities Opportunities for African Urban as well, particularly by fostering contributions from citizen scientists. -
Effects of Atmospheric CO2 Variability of the Past 800 Kyr on the Biomes of Southeast Africa
Clim. Past, 15, 1083–1097, 2019 https://doi.org/10.5194/cp-15-1083-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Effects of atmospheric CO2 variability of the past 800 kyr on the biomes of southeast Africa Lydie M. Dupont1, Thibaut Caley2, and Isla S. Castañeda3 1MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany 2EPOC, UMR 5805, CNRS, University of Bordeaux, Pessac, France 3University of Massachusetts Amherst, Department of Geosciences, Amherst, MA, USA Correspondence: Lydie M. Dupont ([email protected]) Received: 6 February 2019 – Discussion started: 20 February 2019 Revised: 10 May 2019 – Accepted: 23 May 2019 – Published: 19 June 2019 Abstract. Very little is known about the impact of atmo- 1 Introduction spheric carbon dioxide pressure (pCO2) on the shaping of biomes. The development of pCO2 throughout the Brun- Understanding the role of atmospheric carbon dioxide pres- hes Chron may be considered a natural experiment to eluci- sure (pCO2) is paramount for the interpretation of the of date relationships between vegetation and pCO2. While the the palaeovegetation record. The effects of low pCO2 on glacial periods show low to very low values (∼ 220 to ∼ glacial vegetation have been discussed in a number of stud- 190 ppmv, respectively), the pCO2 levels of the interglacial ies (Ehleringer et al., 1997; Jolly and Haxeltine, 1997; Cowl- periods vary from intermediate to relatively high (∼ 250 to ing and Sykes, 1999; Prentice and Harrison, 2009; Prentice more than 270 ppmv, respectively). To study the influence of et al., 2017) predicting that glacial increases in C4 vegeta- pCO2 on the Pleistocene development of SE African vege- tion favoured by low atmospheric CO2 would have opened tation, we used the pollen record of a marine core (MD96- the landscape and lowered the tree line. -
Threatened Ecosystems in South Africa: Descriptions and Maps
Threatened Ecosystems in South Africa: Descriptions and Maps DRAFT May 2009 South African National Biodiversity Institute Department of Environmental Affairs and Tourism Contents List of tables .............................................................................................................................. vii List of figures............................................................................................................................. vii 1 Introduction .......................................................................................................................... 8 2 Criteria for identifying threatened ecosystems............................................................... 10 3 Summary of listed ecosystems ........................................................................................ 12 4 Descriptions and individual maps of threatened ecosystems ...................................... 14 4.1 Explanation of descriptions ........................................................................................................ 14 4.2 Listed threatened ecosystems ................................................................................................... 16 4.2.1 Critically Endangered (CR) ................................................................................................................ 16 1. Atlantis Sand Fynbos (FFd 4) .......................................................................................................................... 16 2. Blesbokspruit Highveld Grassland