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Snow Cover Dynamics in Andean Watersheds of Chile (32.0-39.5°S) During the Years 2000 - 2013
Hydrol. Earth Syst. Sci. Discuss., doi:10.5194/hess-2016-357, 2016 Manuscript under review for journal Hydrol. Earth Syst. Sci. Published: 20 September 2016 c Author(s) 2016. CC-BY 3.0 License. Snow cover dynamics in Andean watersheds of Chile (32.0-39.5°S) during the years 2000 - 2013 Alejandra Stehr1,2,3 and Mauricio Aguayo1,2 1Centre for Environmental Sciences EULA-CHILE, University of Concepción, Concepción, Chile 5 2Faculty of Environmental Sciences, University of Concepción, Concepción, Chile 3CRHIAM, University of Concepción, Concepción, Chile Correspondence to: A. Stehr ([email protected]) Abstract. Andean watersheds present important snowfall accumulation mainly during the winter which is later melted during spring and part of the summer. The effect of snowmelt on the water balance can be critical to sustain agriculture activities, 10 hydropower generation, urban water supply and wildlife. In Chile 25% of the territory between the Valparaiso and Araucanía Regions comprise areas where snow precipitation occurs. As in many other difficult-to-access regions of the world, in the Chilean Andes there is a lack of hydrological data like discharge, snow courses, snow depths, which complicate the analysis of important hydrological processes (e.g. water availability). Remote sensing provides a promising opportunity to enhance the assessment and monitoring of the spatial and temporal variability of snow characteristics, like Snow Cover Area (SCA) and 15 Snow Cover Dynamic (SCD). In the above mentioned context the objectives of this study are to evaluate the suitability of MOD10A2 to estimate SCA and to assess SCD at five watersheds (Aconcagua, Rapel, Maule, Biobío and Toltén) located in the Chilean Andes, between latitude 32.0ºS and 39.5ºS. -
Mozambique Zambia South Africa Zimbabwe Tanzania
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11010329.Pdf
THE RISE, CONSOLIDATION AND DISINTEGRATION OF DLAMINI POWER IN SWAZILAND BETWEEN 1820 AND 1889. A study in the relationship of foreign affairs to internal political development. Philip Lewis Bonner. ProQuest Number: 11010329 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 11010329 Published by ProQuest LLC(2018). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States C ode Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106- 1346 ABSTRACT The Swazi kingdom grew out of the pressures associated with competition for trade and for the rich resources of Shiselweni. While centred on this area it acquired some of its characteristic features - notably a regimental system, and the dominance of a Dlamini aristocracy. Around 1815 the Swazi came under pressure from the South, and were forced to colonise the land lying north of the Lusutfu. Here they remained for some years a nation under arms, as they plundered local peoples, and were themselves swept about by the currents of the Mfecane. In time a more settled administration emerged, as the aristocracy spread out from the royal centres at Ezulwini, and this process accelerated under Mswati as he subdued recalcitrant chiefdoms, and restructured the regiments. -
1 Geography 243 Geography of Africa
Geography 243 Geography of Africa: Local Resources and Livelihoods in a Global Context 1 First Year Seminar Fall Semester, 2018 Class Time and Location : 1:20-2:50, Tuesdays & Thursdays, Rm 105, Carnegie Hall Instructor : Bill Moseley Office : Rm 104d, Carnegie Hall Office Hours : 1:30-2:30pm MW, 3-4pm on Thurs, or by appointment Phone : 651-696-6126. Email : [email protected] Writing Assistant: Rosie Chittick ([email protected] ). Office hrs: 6:30-8pm MW, Dupre, Geography Dept Office Lounge, Carnegie 104 Course Description and Objectives From the positive images in the film Black Panther , to the derogatory remarks of President Trump, the African continent often figures prominently in our collective imagination. This class goes beyond the superficial media interpretations of the world’s second largest region to complicate and ground our understanding of this fascinating continent. Africa South of the Sahara has long been depicted in the media as a place of crisis – a region of the world often known for civil strife, disease, corruption, hunger and environmental destruction. This perception is not entirely unfounded, after all, Ebola in west and central Africa, the kidnapping of school girls in northern Nigeria, or civil war and hunger in Somalia are known problems. Yet Africa is a place of extraordinarily diverse, vibrant, and dynamic cultures. Many Africans also expertly manage their natural resources, are brilliant agriculturalists and have traditions of democratic governance at the local level. As such, the African story is extremely diverse and varied. The thoughtful student must work hard to go beyond the superficial media interpretations of the vast African continent and appreciate its many realities without succumbing to a romanticized view. -
Models and Methods of Tectonic Geomorphology and the Reconstruction of Hominin Landscapes
This is a repository copy of Landscapes of human evolution : models and methods of tectonic geomorphology and the reconstruction of hominin landscapes. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/11178/ Version: Accepted Version Article: Bailey, G.N. orcid.org/0000-0003-2656-830X, Reynolds, Sally and King, G.C.P. (2011) Landscapes of human evolution : models and methods of tectonic geomorphology and the reconstruction of hominin landscapes. Journal of Human Evolution. pp. 257-80. ISSN 0047-2484 https://doi.org/10.1016/j.jhevol.2010.01.004 Reuse Items deposited in White Rose Research Online are protected by copyright, with all rights reserved unless indicated otherwise. They may be downloaded and/or printed for private study, or other acts as permitted by national copyright laws. The publisher or other rights holders may allow further reproduction and re-use of the full text version. This is indicated by the licence information on the White Rose Research Online record for the item. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ This is an author-created pdf. Cite as: In press, J Hum Evol (2010), doi:10.1016/j.jhevol.2010.01.004 Landscapes of human evolution: models and methods of tectonic geomorphology and the reconstruction of hominin landscapes Geoffrey N. Bailey 1 Sally C. Reynolds 2, 3 Geoffrey C. -
Risk Factors Associated with Sexual Violence Towards Girls in Swaziland
Research Risk factors associated with sexual violence towards girls in Swaziland Matthew J Breiding,a Avid Reza,b Jama Gulaid,c Curtis Blanton,b James A Mercy,a Linda L Dahlberg,a Nonhlanhla Dlaminid & Sapna Bamrahe Objective To explore risk factors for sexual violence in childhood in a nationally representative sample of females aged 13 to 24 years in Swaziland. Methods During a household survey respondents were asked to report any experiences of sexual violence before the age of 18 years. The association between childhood sexual violence and several potential demographic and social risk factors was explored through bivariate and multivariate logistic regression. Findings Participants totalled 1244. Compared with respondents who had been close to their biological mothers as children, those who had not been close to her had higher odds of having experienced sexual violence (crude odds ratio, COR: 1.89; 95% CI: 1.14–3.14), as did those who had had no relationship with her at all (COR: 1.93; 95% CI: 1.34–2.80). In addition, greater odds of childhood sexual violence were noted among respondents who were not attending school at the time of the survey (COR: 2.26; 95% CI: 1.70–3.01); who were emotionally abused as children (COR: 2.04; 95% CI: 1.50–2.79); and who knew of another child who had been sexually assaulted (COR: 1.77; 95% CI: 1.31–2.40) or was having sex with a teacher (COR: 2.07; 95% CI: 1.59–2.69). Childhood sexual violence was positively associated with the number of people the respondent had lived with at any one time (COR: 1.03; 95% CI: 1.01–1.06). -
Fire and Its Effects on Vegetation in the Okavango Delta.Pdf
MICHAEL HEINL Fire and its effects on vegetation in the Okavango Delta, Botswana Feuer und sein Einfluss auf die Vegetation im Okavango Delta, Botswana supported by Fire and its effects on vegetation in the Okavango Delta, Botswana Feuer und sein Einfluss auf die Vegetation im Okavango Delta, Botswana Diplomarbeit am Lehrstuhl für Vegetationsökologie Technische Universität München Freising-Weihenstephan Prof. Dr. Jörg Pfadenhauer - 25. August 2001 - Autor: Michael Heinl ([email protected]) Betreuer: Dr. Jan Sliva ([email protected]) Prof. Jörg Pfadenhauer Dr. E. Veenendaal supported by PREFACE II Fire and its effects on vegetation in the Okavango Delta, BoBotttswanaswana Preface The present MSc-Thesis (Diplomarbeit) describes the results of a one-year project about the effects of fire on vegetation, with special focus on the Okavango Delta region, Botswana. The study is based on a new initiated research co-operation between Harry Oppenheimer Okavango Research Centre (HOORC) in Maun, Botswana, part of University of Botswana and the Chair of Vegetation Ecology of the Technische Universität München (TUM), Germany funded by Stifterverband für die Deutsche Wissenschaft within their programme “Forschung für Naturräume“ for young scientists. Under the topic “Elements in Conflict - Anthropogenic fires in the RAMSAR-wetland Okavango-Delta (Botswana)”, prerequisites were set for future co- operative research projects between HOORC and TUM during August 2000 to August 2001. Besides the theoretical introduction to the ecology of the study area ‘Okavango Delta’, this period was primarily used to gain first practical experience on the vegetation and the fire ecology of the Okavango Delta during the stays in Botswana in October 2000 and March/April/Mai 2001. -
O C E a N O C E a N C T I C P a C I F I C O C E a N a T L a N T I C O C E a N P a C I F I C N O R T H a T L a N T I C a T L
Nagurskoye Thule (Qanaq) Longyearbyen AR CTIC OCE AN Thule Air Base LAPTEV GR EENLA ND SEA EAST Resolute KARA BAFFIN BAY Dikson SIBERIAN BARENTS SEA SEA SEA Barrow SEA BEAUFORT Tiksi Prudhoe Bay Vardo Vadso Tromso Kirbey Mys Shmidta Tuktoyaktuk Narvik Murmansk Norilsk Ivalo Verkhoyansk Bodo Vorkuta Srednekolymsk Kiruna NORWEGIAN Urengoy Salekhard SEA Alaska Oulu ICELA Anadyr Fairbanks ND Arkhangelsk Pechora Cape Dorset Godthab Tura Kitchan Umea Severodvinsk Reykjavik Trondheim SW EDEN Vaasa Kuopio Yellowknife Alesund Lieksa FINLAND Plesetsk Torshavn R U S S Yakutsk BERING Anchorage Surgut I A NORWAY Podkamennaya Tungusk Whitehorse HUDSON Nurssarssuaq Bergen Turku Khanty-Mansiysk Apuka Helsinki Olekminsk Oslo Leningrad Magadan Yurya Churchill Tallin Stockholm Okhotsk SEA Juneau Kirkwall ESTONIA Perm Labrador Sea Goteborg Yedrovo Kostroma Kirov Verkhnaya Salda Aldan BAY UNITED KINGDOM Aluksne Yaroslavl Nizhniy Tagil Aberdeen Alborg Riga Ivanovo SEA Kalinin Izhevsk Sverdlovsk Itatka Yoshkar Ola Tyumen NORTH LATVIA Teykovo Gladkaya Edinburgh DENMARK Shadrinsk Tomsk Copenhagen Moscow Gorky Kazan OF BALTIC SEA Cheboksary Krasnoyarsk Bratsk Glasgow LITHUANIA Uzhur SEA Esbjerg Malmo Kaunas Smolensk Kaliningrad Kurgan Novosibirsk Kemerovo Belfast Vilnius Chelyabinsk OKHOTSK Kolobrzeg RUSSIA Ulyanovsk Omsk Douglas Tula Ufa C AN Leeds Minsk Kozelsk Ryazan AD A Gdansk Novokuznetsk Manchester Hamburg Tolyatti Magnitogorsk Magdagachi Dublin Groningen Penza Barnaul Shefeld Bremen POLAND Edmonton Liverpool BELARU S Goose Bay NORTH Norwich Assen Berlin -
Resume of Chief Examiners' Report for the General
RESUME OF CHIEF EXAMINERS’ REPORT FOR THE GENERAL SUBJECTS SECTION 1. STANDARD OF PAPERS All the Chief Examiners reported that the standard of the papers compared favourably with that of previous years. 2. PERFORMANCE OF CANDIDATES The Chief Examiners expressed varied opinions about candidates’ performance. An improved performance was reported by the Chief Examiners of History, Economics, Geography 1B, Christian Religious Studies, Islamic Studies, Government and Social Studies. However the Chief Examiner for Geography 2 reported a slight decline in the performance of candidates. 3. A SUMMARY OF CANDIDATES’ STRENGTHS The Chief Examiners noted the following commendable features in the candidates’ scripts. (1) Orderly Presentation of material and good expression The subjects for which candidates were commended for orderly presentation of material and clarity of expression include Christian Religious Studies, Economics, History, Islamic Studies , Government and Social Studies . (2) Relevant examples and illustrations An appreciable number of candidates in Geography 1, Social Studies, History and Government were commended by the Chief Examiners for buttressing their points with relevant examples. (3) Compliance with the rubrics Candidates of History, Christian Religious Studies, Government , Geography 1 and 2 were reported to have adhered to the rubrics of the paper very strictly. (4) Legible Handwriting The Chief Examiners for Christian Religious Studies, Economics , History, Islamic Studies, Government and Social Studies commended candidates for good handwriting. 4. A SUMMARY OF CANDIDATES’WEAKNESSES The Chief examiners reported the following as weaknesses of most of the candidates: (1) Inability to draw diagrams properly The Chief Examiner for Geography 1B reported that the candidates failed to draw well-labelled diagrams and could not interpret graph and other statistical data. -
Palaeoecology of Africa*
Intimations on Quaternary palaeoecology of Africa* E.M. van Zinderen+Bakker Palynological Research Unit of the C.S.I.R. and the University of the Orange Free State at Bloemfontein 1. THE BIOGEOGRAPHIC PATTERN OF AFRICA of with of is little The biogeography Africa, as compared that Europe known and it is only in recent years that more detailed studies have been made of cer- of tain areas. Taxonomists working on groups lower plants and animals and even on flowering plants will still find many rich new areas for collecting in Africa, while the results of these taxonomic studies are the basis of any biogeo- graphic investigation. The study of the factors responsible for the present-day pattern of distribution of plants and animals has been initiated in Africa only The which directed towards fairly recently. present intimations, are mostly botanical problems, are therefore general in nature and are often hypothetical. They are only intended to indicate possible historical approaches to the study of biogeography of Africa. The flora and fauna of Africa, the continent for which some of the most an- cient radiometric dates have been assessed, must in consequence be old in origin. The priscotropical flora of the forests, savannas, mountains and deserts of Africa has been isolated from the other continents since mesozoic times and has wealth of in the flora. Botanical developed a great species especially Cape Gondwana affinities are apparent in this southern flora, while boreal influences of found in the mountainfloras from the Sa- a comparatively younger age are hara and Ethiopia in the north right down the length of the continent to the Africa. -
About the Geography of Africa
CK_4_TH_HG_P087_242.QXD 10/6/05 9:02 AM Page 146 IV. Early and Medieval African Kingdoms Teaching Idea Create an overhead of Instructional What Teachers Need to Know Master 21, The African Continent, and A. Geography of Africa use it to orient students to the physical Background features discussed in this section. Have them use the distance scale to Africa is the second-largest continent. Its shores are the Mediterranean compute distances, for example, the Sea on the north, the Atlantic Ocean to the west, the Red Sea and Indian Ocean length and width of the Sahara. to the east, and the Indian Ocean to the south. The area south of the Sahara is Students might be interested to learn often called sub-Saharan Africa and is the focus of Section C, “Medieval that the entire continental United Kingdoms of the Sudan,” (see pp. 149–152). States could fit inside the Sahara. Mediterranean Sea and Red Sea The Red Sea separates Africa from the Arabian Peninsula. Except for the small piece of land north of the Red Sea, Africa does not touch any other land- Name Date mass. Beginning in 1859, a French company dug the Suez Canal through this nar- The African Continent row strip of Egypt between the Mediterranean and the Red Seas. The new route, Study the map. Use it to answer the questions below. completed in 1869, cut 4,000 miles off the trip from western Europe to India. Atlantic and Indian Oceans The Atlantic Ocean borders the African continent on the west. The first explorations by Europeans trying to find a sea route to Asia were along the Atlantic coast of Africa. -
Cartography and the Conception, Conquest and Control of Eastern Africa, 1844-1914
Delineating Dominion: Cartography and the Conception, Conquest and Control of Eastern Africa, 1844-1914 DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Robert H. Clemm Graduate Program in History The Ohio State University 2012 Dissertation Committee: John F. Guilmartin, Advisor Alan Beyerchen Ousman Kobo Copyright by Robert H Clemm 2012 Abstract This dissertation documents the ways in which cartography was used during the Scramble for Africa to conceptualize, conquer and administer newly-won European colonies. By comparing the actions of two colonial powers, Germany and Britain, this study exposes how cartography was a constant in the colonial process. Using a three-tiered model of “gazes” (Discoverer, Despot, and Developer) maps are analyzed to show both the different purposes they were used for as well as the common appropriative power of the map. In doing so this study traces how cartography facilitated the colonial process of empire building from the beginnings of exploration to the administration of the colonies of German and British East Africa. During the period of exploration maps served to make the territory of Africa, previously unknown, legible to European audiences. Under the gaze of the Despot the map was used to legitimize the conquest of territory and add a permanence to the European colonies. Lastly, maps aided the capitalist development of the colonies as they were harnessed to make the land, and people, “useful.” Of special highlight is the ways in which maps were used in a similar manner by both private and state entities, suggesting a common understanding of the power of the map.