© in This Web Service Cambridge University

Total Page:16

File Type:pdf, Size:1020Kb

© in This Web Service Cambridge University Cambridge University Press 978-1-107-05579-7 - Quaternary Environmental Change in Southern Africa: Physical and Human Dimensions Edited by Jasper Knight and Stefan W. Grab Index More information Index /Xam Bushmen, 392 Bokoni, 401–402 Bond’s springbok, 297, 299 Acheulean, 106, 349, 357, 362 Boomplaas Cave, 392 Aeolian sand, 146 Border Cave, 77, 107, 379, 385 Aeolianite, 92, 209, 227 Bovids, 380 African Humid Period, 275 Braamhoek, 197, 311, 333–334 African Superswell, 32, 88 Breede River, 95 African Surfaces, 10, 26, 33, 35–36, 414 Bushveld Complex, 22 Afromontane forest, 313 Agropastoralism, 407 C3/C4 grasslands, 95, 273, 335, 337 Agulhas Bank, 91, 94, 203, 225 Calcrete, 102, 111, 225, 242 Agulhas Current, 205 Canteen Kopje, 355, 359, 362 Albany thicket, 94 Cape Fold Belt, 12, 89, 124 Alexandria dunefield, 206, 211 Cape Supergroup, 24, 124 Algoa Bay, 25, 206 Carbonate cementation, 211 Alluvial fans, 38 Carbonate rocks, 251 Anabranching rivers, 173 Catenas, 238 Anthropocene, 339, 416, 424 Cave of Hearths, 362 Anthropological turn, 399 Cave systems, 251, 420 Ardipithecus, 49, 51 Cederberg, 275, 313 Aridity, 9 Cenotes, 252 Australopithecus,49–50, 52, 58, 74 Cenozoic, 1, 8, 30, 39 Australopithecus sediba, 106 Charaman Industry, 363 Avulsion, 175, 177 Charcoal, 307, 314 Awash Valley, 68 Chemical weathering, 235 Cirques, 124 Barberton Supergroup, 20 Clarens Formation, 124 Barrier dunes, 92, 213 Climate aridity, 155 Bauxite, 245 Climate change, 412 Beachrock, 207, 211, 227 Climate feedbacks, 31 Benguela Current, 204–205, 337 Climate modelling, 129 Benguela Upwelling Zone, 333–334 Climate reconstruction, 317 Biogeographic patterns, 289 Coastal dunes, 204 Biomes, 270, 279, 286, 308 Coastal plain, 89, 93, 96, 203, 225 Black wildebeest, 285, 292 Coccoliths, 333, 338 Blesbok, 291 Cognitive complexity, 379 Blockstreams, 130 Cold Air Cave, 109, 258, 262 Blombos Cave, 211, 376, 379 Colluvial sediments, 104, 137, 141, 144 Blood Reef, 208 Congo basin, 39 Blue wildebeest, 295 Continental shelf, 91 432 © in this web service Cambridge University Press www.cambridge.org Cambridge University Press 978-1-107-05579-7 - Quaternary Environmental Change in Southern Africa: Physical and Human Dimensions Edited by Jasper Knight and Stefan W. Grab Index More information Index 433 Cornelia, 360 Fluvial climate records, 172 Cornelian mammalian assemblage, 285, 289 Fluvial systems, 174 Cornelia-Uitzoek, 295 Foraminifera, 330, 333, 337 Cosmogenic dating, 5, 35, 100, 415 Forcing–response, 413 Cradle of Humankind, 77, 350 Fynbos, 94, 273, 286, 311, 313 Cretaceous, 26 Crevice Cave, 258 Gariep belt, 31 Cultural landscapes, 419 Geoarchaeology, 420, 422 Geochronology, 99 Dansgaard-Oeschger cycles, 4, 95 Geological history, 5 Dante Cave, 263 Geomorphic models, 141 Davisian theory, 10 Geomorphological sensitivity, 182, 415 Dendroclimatology, 406 Glacial moraines, 125 Denudation rates, 140 Glacial–interglacial cycles, 96 Diatoms, 228, 329–331, 336–337 Glacioisostasy, 90 Diepkloof Cave, 107, 313 Gladysvale, 258, 292, 358 Dongas, 180 Gold reefs, 21 Drakensberg Group, 25 Golden Gate, 145 Drakensberg Range, 103, 124, 129 Goldsmith’s, 358 Duinefontein, 106, 361 Gondwana, 23–24, 26 Dune cordons, 205 Gondwana breakup, 90 Dune dynamics, 156 Great Escarpment, 2, 35, 122, 138 Durban Bay, 227 Great Zimbabwe, 110, 401 Durban Bluff, 208, 210 Gullying, 144, 147 Duricrusts, 242 Dwyka Group, 25, 122 Heinrich events, 4 Dynamic equilibrium, 192 Herders, 393, 400 Hex River Mountains, 131 Early Stone Age, 349 Highveld, 285 Eccentricity, 295 Historical archaeology, 421 Ecological functioning, 198 Holocene Altithermal, 312 Ecological resources, 389 Holocene climate change, 180, 196, 258, 275, 311, Ecosystem dynamics, 269 399 El Niño, 416 Holocene sea-level change, 224, 230 Elands Bay Cave, 388 Hominidae, 68 Elandsfontein, 69, 77, 286, 361 Hominin dispersal, 55 Electron spin resonance dating, 101 Hominin evolution, 47, 421 Environmental change, 174 Homo,59 Environmental determinism, 398, 405, Homo cranium, 74 413 Homo dentition, 74 Environmental resources, 413 Homo erectus, 68, 71 Epeirogenesis, 140 Homo ergaster, 358, 363 Epeirogenic uplift, 33 Homo habilis, 69, 71, 73, 357 Equilibrium profile, 191 Homo sapiens,78 Erfkroon, 177 Howiesons Poort, 107, 313, 376–378, 380 Estuaries, 219 Human behaviour, 418 Estuary evolution models, 229 Human evolution, 69, 96 Etosha pan, 38, 154 Human impacts, 279 Eustasy, 220 Hunter-gatherers, 393–394, 399 hxaro, 392, 400, 402 Faunal analysis, 397 Fauresmith Industry, 362 Ichnofossils, 211 Ferricrete, 242–243 Incised valleys, 222, 227 Fire, 279, 360, 379 Intertidal zone, 207 Flood frequency, 180 Intertropical Convergence Zone, 236 Floodplains, 189 IPCC, 4 Florisbad, 197, 295, 373 Iron Age, 108, 312, 418 Florisian, 285, 289 iSimangaliso World Heritage Site, 191 © in this web service Cambridge University Press www.cambridge.org Cambridge University Press 978-1-107-05579-7 - Quaternary Environmental Change in Southern Africa: Physical and Human Dimensions Edited by Jasper Knight and Stefan W. Grab Index More information 434 Index K2-Mapungubwe state, 401 Malapa, 75 Kaapvaal Craton, 18, 20, 31 Mammal faunas, 285 Kalahari, 176, 400 Mantle swells, 32–33 Kalahari Desert, 154, 162 Mapungubwe, 112, 400, 405 Karoo Supergroup, 25, 122 Maputo Bay, 228 Karst environments, 250 Marathodi, 401 Kathu Pan, 362 Marine basins, 39 Khoe-San, 375 Marine Isotope Stages, 338 Klasies River, 107, 373–374, 377 Marine resources, 96 Klip River, 177, 192 Maropeng, 358 Kosi Bay, 225, 228 Masotcheni Formation, 141, 146 Kosi Bay Formation, 212 Mass movement, 137 Kraals, 109 Maunder Minimum, 264 Kromdraai, 355 Medieval Warm Period, 177, 275, 404 Kruger National Park, 5, 103 Melikane, 400 KwaZulu-Natal, 405 Meltwater pulses, 227 Mfabeni, 273, 312 Lagoons, 219 mfecane, 403, 405 Lake Groenvlei, 229 Microfossils, 324, 338, 340 Lake Ngami, 337 Micromorphology, 420 Lake Sibaya, 223, 228, 312 Middle Stone Age, 77, 143, 314, 363, 371, 423 Lake St Lucia, 191, 221, 228 Miocene, 308 Lake Tritrivakely, 334 Modder River, 176 Land Mammal Ages, 288 Monsoon, 4 Land surface denudation, 103, 414 Mossel Bay, 210 Land surface instability, 414 Mount Enterprise, 126 Landscape disturbance, 417 Mozambique Channel, 312 Landscape evolution, 11, 30, 102, 138, 415 Landscape geomorphology, 414 Nahoon Point, 105, 211–212 Landscape resources, 423 n-alkanes, 1 Langebaan Lagoon, 221, 229, 361 Namib Desert, 103, 105, 154, 156 Langebaanweg, 55 Natal Bight, 91 Large Igneous Provinces (LIPs), 32 Neogene, 8, 47 Large low shear velocity provinces (LLSVPs), 32 Neoproterozoic, 23 Last Glacial Maximum, 125, 128, 161, 225, 273, 336 Nguni, 401 Later Stone Age, 78, 385 Non-material landscape resources, 418 Laterite, 37 Non-materiality, 423 Leqooa Valley, 126 Lesotho Highlands, 128 Oakleigh Farm, 404 Levallois, 376 Obliquity, 95 Likoaeng, 399 Ochre, 379 Limpopo, 423 Okavango Delta, 38, 176, 191, 336 Linear dunes, 156 Oldowan, 349 Lithic technology, 355 Olduvai, 71 Little Ice Age, 147, 264, 405 Olifants River, 181 Littlefoot, 106 Open-air sites, 350, 360 Livestock domestication, 392 Orange River, 25, 39, 203 Longshore drift, 206 Orrorin,50 Lowstand deltas, 225 Ostracods, 332 Luminescence dating, 100, 104, 157 Oxygen isotopes, 2 Lunettes, 160 Pakhuis Pass, 316 Macassa Bay, 228 Pakhuis Tillites, 125 Macrofossils, 306 Palaeoanthropocene, 416 Madagascar, 252 Palaeo-anthropology, 2, 412 Mahwaqa, 307, 311, 316 Palaeobotanical record, 314 Makapansgat, 47, 253, 405 Palaeo-cliff-line, 209 Makgadikgadi pan, 38, 155, 162, 336 Palaeoenvironmental change, 122, 132, 193 © in this web service Cambridge University Press www.cambridge.org Cambridge University Press 978-1-107-05579-7 - Quaternary Environmental Change in Southern Africa: Physical and Human Dimensions Edited by Jasper Knight and Stefan W. Grab Index More information Index 435 Palaeoenvironmental proxies, 325 Sand ramps, 165 Palaeoenvironmental reconstruction, 306, 339–340 Sandy beaches, 206 Palaeolandscapes, 95 Saprolite, 237 Palaeosols, 145, 177, 235 Schroda, 404 Palimpsest, 415 Sea-level change, 209, 220, 222 Pans, 198 Sea-level lowstands, 212, 222 Paranthropus, 68, 75 Sea-level transgression, 225 Paranthropus robustus, 357 Sediment accumulation rates, 194 Pedogenesis, 235–236 Sediment yield, 36 Peneplain, 10 Sehonhong shelter, 399 Penhill, 361 Sesquioxides, 237 Perched estuaries, 207 Shashe-Limpopo Confluence Area, 401, 403 Periglacial landforms, 121, 130 Shongweni, 404 Phanerozoic, 24 Sibudu Cave, 110, 314, 380–381, Phytoliths, 325, 329–330, 337 417, 420 Pinnacle Point, 95, 211, 372, 380 Silcrete, 242–243, 379 Pleistocene climate, 295, 310 Silver Leaves, 400 Pliocene, 26, 291 Skeleton Coast, 155 Podocarpus, 310, 312 Slope instability, 140 Pollen, 306, 329 Slopewash, 245 Pondoland, 205, 210 Snow accumulation, 129 Pongola Supergroup, 21 Soil classification, 238 Port Durnford Formation, 212, 225 Soil piping, 147 Precambrian, 18 Spatial modelling, 419 Principal Component Analysis, 196 Speleothems, 102, 250 Sterkfontein, 47, 69, 106, 251, 253, 350 Quaternary, 1, 4, 132, 413, 424 Still Bay, 108, 313, 375 Quaternary deposits, 211 Stone tool technology, 381 Quaternary ecosystems, 94 Summer rainfall zone, 270, 273, 398, 403 Quaternary environmental change, 1, 4, 270 Sundays River, 104, 175 Quaternary glaciation, 121 Sustainable development, 4 Quaternary sea-level change, 90, 212, 224 Swartkrans, 10, 69, 77, 350, 355 Radiocarbon dating, 101, 110–111, 128, 144, 312 Table Mountain Group, 205, 270 Radiolaria, 332 Taphonomy, 307 Rain-fed agriculture, 401 Tectonic uplift, 8 Rain-making, 419 Thúfur,
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Corrosion Map of South Africa's Macro Atmosphere
    Corrosion map of South Africa’s macro atmosphere AUTHORS: Darelle T. Janse van Rensburg1,2 The first atmospheric corrosion map of South Africa, produced by Callaghan in 1991, has become outdated, Lesley A. Cornish1 because it primarily focuses on the corrosivity of coastal environments, with little differentiation given Josias van der Merwe1 concerning South Africa’s inland locations. To address this problem, a study was undertaken to develop AFFILIATIONS: a new corrosion map of the country, with the emphasis placed on providing greater detail concerning 1School of Chemical and Metallurgical South Africa’s inland regions. Here we present this new corrosion map of South Africa’s macro atmosphere, Engineering and DST-NRF Centre of Excellence in Strong Materials, based on 12-month corrosion rates of mild steel at more than 100 sites throughout the country. Assimilations University of the Witwatersrand, and statistical analyses of the data (published, unpublished and new) show that the variability in the corrosion Johannesburg, South Africa rate of mild steel decreases significantly moving inland. Accordingly, the average first-year corrosion rate of 2Orytech (Pty) Ltd, Roodepoort, South Africa mild steel at the inland sites (at all corrosion monitoring spots located more than 30 km away from the ocean) measured 21±12 µm/a [95% CI: 18–23 µm/a]. The minimum inland figure was about 1.3 µm/a (recorded CORRESPONDENCE TO: at Droërivier in the Central Karoo) and the maxima were approximately 51 µm/a and 50 µm/a in the industrial Darelle Janse van Rensburg hearts of Germiston (Gauteng) and Sasolburg (Free State), respectively.
    [Show full text]
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Geophysical Modelling of the Molopo Farms Complex in Southern Botswana
    CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive GEOPHYSICAL MODELLING OF THE MOLOPO FARMS COMPLEX IN SOUTHERN BOTSWANA: IMPLICATIONS FOR ITS EMPLACEMENT WITHIN THE ~2 GA LARGE IGNEOUS PROVINCES OF SOUTHERN AND CENTRAL AFRICA A.S.D. WALKER British Geological Survey, Keyworth, Nottingham, United Kingdom, NG12 5GG e-mail: [email protected] R.M. KEY British Geological Survey, West Mains Road, Edinburgh, United Kingdom, EH9 3LA e-mail: [email protected] G. POULIQUEN Geosoft Europe Limited, Wallingford, United Kingdom, OX10 0AD e-mail: [email protected] G. GUNN British Geological Survey, Keyworth, Nottingham, United Kingdom, NG12 5GG e-mail: [email protected] J. SHARROCK Gondwana Ventures (Pty) Limited, P.O. Box 20241, Francistown, Botswana e-mail: [email protected] I. McGEORGE MSA Geoservices, P.O. Box 2258, Gaborone, Botswana email: [email protected] M. KOKETSO Department of Geological Survey, Private Bag 14, Lobatse, Botswana e-mail: [email protected] J. FARR Wellfield Consulting Services (Pty) Limited, P.O. Box 1502, Gaborone, Botswana e-mail: [email protected] ABSTRACT The Molopo Farms Complex is an extremely poorly exposed, major, ultramafic-mafic layered intrusion straddling the southern border of Botswana with South Africa. It lies within the south-western part of the ~2.0 Ga large igneous province of southern and central Africa that includes the better known Bushveld Complex. Integrated interpretation of regional gravity data and new high-resolution airborne magnetic data have constrained the geometry of the Molopo Farms Complex in southern Botswana as a strongly faulted, polyphase intrusion compartmentalised by regional ductile shear zones.
    [Show full text]
  • Wasps and Bees in Southern Africa
    SANBI Biodiversity Series 24 Wasps and bees in southern Africa by Sarah K. Gess and Friedrich W. Gess Department of Entomology, Albany Museum and Rhodes University, Grahamstown Pretoria 2014 SANBI Biodiversity Series The South African National Biodiversity Institute (SANBI) was established on 1 Sep- tember 2004 through the signing into force of the National Environmental Manage- ment: Biodiversity Act (NEMBA) No. 10 of 2004 by President Thabo Mbeki. The Act expands the mandate of the former National Botanical Institute to include respon- sibilities relating to the full diversity of South Africa’s fauna and flora, and builds on the internationally respected programmes in conservation, research, education and visitor services developed by the National Botanical Institute and its predecessors over the past century. The vision of SANBI: Biodiversity richness for all South Africans. SANBI’s mission is to champion the exploration, conservation, sustainable use, appreciation and enjoyment of South Africa’s exceptionally rich biodiversity for all people. SANBI Biodiversity Series publishes occasional reports on projects, technologies, workshops, symposia and other activities initiated by, or executed in partnership with SANBI. Technical editing: Alicia Grobler Design & layout: Sandra Turck Cover design: Sandra Turck How to cite this publication: GESS, S.K. & GESS, F.W. 2014. Wasps and bees in southern Africa. SANBI Biodi- versity Series 24. South African National Biodiversity Institute, Pretoria. ISBN: 978-1-919976-73-0 Manuscript submitted 2011 Copyright © 2014 by South African National Biodiversity Institute (SANBI) All rights reserved. No part of this book may be reproduced in any form without written per- mission of the copyright owners. The views and opinions expressed do not necessarily reflect those of SANBI.
    [Show full text]
  • The Climate of Botswana
    WildlifeCampus – Discovering Wilderness 1 Module # 3 – Component # 1 Discover the Ecology – South Africa Introduction South Africa caught the imagination of the world with Nelson Mandela’s release from prison in 1991, followed by the peaceful, first democratic elections in 1994. South Africa is an enigma in that it is neither First World nor Third World. It is neither exclusively remote ”old” Africa, nor is it exclusively African nor European. What South Africa has are blends and elements of the “Africa of old”, today’s Africa and the New World. In parts of the country, visitors can escape to wild and remote parks, and experience exceptional game viewing and true wilderness. Then, just an hours flight away, are modern cities and hotels that easily compete with the best in the World. South Africa is culturally diverse, with eleven different official languages, which enrich every traveller’s experience. It has an entire and unique Floral Kingdom in and around one of the World’s most beautiful cities – Cape Town. There are more naturally occurring, different species of flowers just around Cape Town than there are in the whole of North America or the whole of Europe. Table Mountain alone has more flowering plants than the United Kingdom. Everywhere you go the scenery is different. There are lush temperate and coastal forests, open savanna and many diverse and fascinating World Heritage Sites. South Africa also has deserts and arid areas, including the World’s first Transfrontier National Park, The Kgalagadi Transfrontier National Park straddling the borders of South Africa and Botswana. The travel slogan , “a world in one country”, is fitting.
    [Show full text]
  • New Ages from Boomplaas Cave, South Africa, Provide Increased Resolution on Late/Terminal Pleistocene Human Behavioural Variabil
    AZANIA: ARCHAEOLOGICAL RESEARCH IN AFRICA, 2018 https://doi.org/10.1080/0067270X.2018.1436740 New ages from Boomplaas Cave, South Africa, provide increased resolution on late/terminal Pleistocene human behavioural variability Justin Pargetera, Emma Loftusb, Alex Mackayc, Peter Mitchelld and Brian Stewarte aAnthropology Department, Stony Brook University, Stony Brook, NY 11790, United States of America and Centre for Anthropological Research & Department of Anthropology and Development Studies University of Johannesburg, PO Box 524, Auckland Park, 2006, South Africa; bResearch Laboratory for Archaeology and the History of Art, South Parks Road, Oxford, OX1 3QY, United Kingdom and Department of Archaeology, University of Cape Town, Rondebosch, 7700, South Africa; cCentre for Archaeological Science, School of Earth and Environmental Sciences, University of Wollongong, Wollongong, NSW 2522, Australia and Department of Archaeology, University of Cape Town, Rondebosch, 7700, South Africa; dSchool of Archaeology, University of Oxford/St Hugh’s College, Oxford, OX2 6LE, United Kingdom and School of Geography, Archaeology and Environmental Studies, University of the Witwatersrand, PO Wits 2050, South Africa; eMuseum of Anthropological Archaeology and Department of Anthropology, University of Michigan, 1109 Geddes Ave., Ann Arbor, MI 48109-1079, United States of America and Rock Art Research Institute, University of the Witwatersrand, PO Wits 2050, South Africa. ABSTRACT ARTICLE HISTORY Boomplaas Cave, South Africa, contains a rich archaeological
    [Show full text]
  • The Sahara Desert Hydroclimate and Expanse: Natural Variability And
    The Sahara Desert Hydroclimate and Expanse: Natural Variability and Climate Change Sumant Nigam and Natalie P Thomas, Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD, United States © 2019 Elsevier Inc. All rights reserved. Introduction 1 Datasets and Analysis Method 2 Observational Datasets 2 Desert Expansion 2 Statistical Significance 3 Seasonal Climatology 3 Centennial Trends in Surface Air Temperature and Precipitation 3 Change in Sahara Desert Expanse Over 20th Century 5 Sahara’s Advance 7 Sahara’s Expanse 9 Sahara’s Expanse: Variation and Potential Mechanisms 9 Concluding Remarks 10 References 12 Abstract The Sahara Desert is the largest warm desert on the planet, with an area comparable to that of contiguous United States. It is a key element of the African climate system. 20th-Century trends in seasonal temperature and precipitation over the African continent are analyzed from observational data to characterize the seasonal footprints of hydroclimate change. Given the prominence of agricultural economies on the continent, a seasonal perspective was considered more pertinent than the annual-average typically used in desert characterization as the latter can mask off-setting but agriculturally-sensitive seasonal hydroclimate trends. Seasonal surface air temperature (SAT) trends show that heat stress has increased in several regions, including Sudan and Northern Africa where largest SAT trends occur in the warm season—in stark contrast with the seasonal structure of climate change over northern continents where the warming is most pronounced in winter. Precipitation trends are varied but notable declining trends are found in the countries along the Gulf of Guinea, especially in the source region of Niger river in West Africa, and in the Congo river basin.
    [Show full text]