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An Analysis of the Afar-Somali Conflict in Ethiopia and Djibouti
Regional Dynamics of Inter-ethnic Conflicts in the Horn of Africa: An Analysis of the Afar-Somali Conflict in Ethiopia and Djibouti DISSERTATION ZUR ERLANGUNG DER GRADES DES DOKTORS DER PHILOSOPHIE DER UNIVERSTÄT HAMBURG VORGELEGT VON YASIN MOHAMMED YASIN from Assab, Ethiopia HAMBURG 2010 ii Regional Dynamics of Inter-ethnic Conflicts in the Horn of Africa: An Analysis of the Afar-Somali Conflict in Ethiopia and Djibouti by Yasin Mohammed Yasin Submitted in partial fulfilment of the requirements for the degree PHILOSOPHIAE DOCTOR (POLITICAL SCIENCE) in the FACULITY OF BUSINESS, ECONOMICS AND SOCIAL SCIENCES at the UNIVERSITY OF HAMBURG Supervisors Prof. Dr. Cord Jakobeit Prof. Dr. Rainer Tetzlaff HAMBURG 15 December 2010 iii Acknowledgments First and foremost, I would like to thank my doctoral fathers Prof. Dr. Cord Jakobeit and Prof. Dr. Rainer Tetzlaff for their critical comments and kindly encouragement that made it possible for me to complete this PhD project. Particularly, Prof. Jakobeit’s invaluable assistance whenever I needed and his academic follow-up enabled me to carry out the work successfully. I therefore ask Prof. Dr. Cord Jakobeit to accept my sincere thanks. I am also grateful to Prof. Dr. Klaus Mummenhoff and the association, Verein zur Förderung äthiopischer Schüler und Studenten e. V., Osnabruck , for the enthusiastic morale and financial support offered to me in my stay in Hamburg as well as during routine travels between Addis and Hamburg. I also owe much to Dr. Wolbert Smidt for his friendly and academic guidance throughout the research and writing of this dissertation. Special thanks are reserved to the Department of Social Sciences at the University of Hamburg and the German Institute for Global and Area Studies (GIGA) that provided me comfortable environment during my research work in Hamburg. -
Proposal for Inclusion of the African Wild Ass (Eritrea)
CMS CONVENTION ON Distribution: General MIGRATORY UNEP/CMS/COP12/Doc.25.1.7(a) 9 June 2017 SPECIES Original: English 12th MEETING OF THE CONFERENCE OF THE PARTIES Manila, Philippines, 23 - 28 October 2017 Agenda Item 25.1 PROPOSAL FOR THE INCLUSION OF THE AFRICAN WILD ASS (Equus africanus) ON APPENDIX I AND II OF THE CONVENTION Summary: The Government of Eritrea has submitted the attached proposal* for the inclusion of the African Wild Ass (Equus africanus) on Appendix I and II of CMS. A proposal for the inclusion of the same taxon on Appendix I of CMS has been submitted independently by the Government of Ethiopia. The proposal is reproduced in document UNEP/CMS/COP12/Doc.25.1.7(b). *The geographical designations employed in this document do not imply the expression of any opinion whatsoever on the part of the CMS Secretariat (or the United Nations Environment Programme) concerning the legal status of any country, territory, or area, or concerning the delimitation of its frontiers or boundaries. The responsibility for the contents of the document rests exclusively with its author. UNEP/CMS/COP12/Doc.25.1.7(a) PROPOSAL FOR THE INCLUSION OF THE AFRICAN WILD ASS (Equus africanus) ON APPENDIX I AND II OF THE CONVENTION A. PROPOSAL Inclusion of all subspecies of African wild ass Equus africanus to Appendix I and Appendix II of the Convention on the Conservation of Migratory Species of Wild Animals: B. PROPONENT: ERITREA C. SUPPORTING STATEMENT 1. Taxonomy This proposal does not follow the current nomenclatural reference for terrestrial mammals adopted by CMS, i.e. -
Alluvial Fans in the Death Valley Region California and Nevada
Alluvial Fans in the Death Valley Region California and Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 Alluvial Fans in the Death Valley Region California and Nevada By CHARLES S. DENNY GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 A survey and interpretation of some aspects of desert geomorphology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publications as follows: Denny, Charles Storrow, 1911- Alluvial fans in the Death Valley region, California and Nevada. Washington, U.S. Govt. Print. Off., 1964. iv, 61 p. illus., maps (5 fold. col. in pocket) diagrs., profiles, tables. 30 cm. (U.S. Geological Survey. Professional Paper 466) Bibliography: p. 59. 1. Physical geography California Death Valley region. 2. Physi cal geography Nevada Death Valley region. 3. Sedimentation and deposition. 4. Alluvium. I. Title. II. Title: Death Valley region. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C., 20402 CONTENTS Page Page Abstract.. _ ________________ 1 Shadow Mountain fan Continued Introduction. ______________ 2 Origin of the Shadow Mountain fan. 21 Method of study________ 2 Fan east of Alkali Flat- ___-__---.__-_- 25 Definitions and symbols. 6 Fans surrounding hills near Devils Hole_ 25 Geography _________________ 6 Bat Mountain fan___-____-___--___-__ 25 Shadow Mountain fan..______ 7 Fans east of Greenwater Range___ ______ 30 Geology.______________ 9 Fans in Greenwater Valley..-----_____. 32 Death Valley fans.__________--___-__- 32 Geomorpholo gy ______ 9 Characteristics of fans.._______-___-__- 38 Modern washes____. -
West Africa Part III: Central Africa Part IV: East Africa & Southern Africa Name: Date
Part I: North Africa Part II: West Africa Part III: Central Africa Part IV: East Africa & Southern Africa Name: Date: AFRI CA Overview RICA lies at the heart of the earth's land Then, during the nineteenth century, masses. It sits astride the equator, with European traders began setting up trading sta . almost half the continent to the north tions along the coast of West Africa. The of the equator, and half to the south. It con traders, and their governments, soon saw great tains some of the world's greatest deserts, as opportunity for profit in Africa. Eventually, well as some of the world's greatest rivers. It many European countries took control of the has snow-capped mountains, and parched, arid land and divided it into colonies. plains. The first humans came from Africa. By the middle of the twentieth century, peo And in the millennia since those fust humans ple all across Africa had demanded indepen walked the plains of Africa, many different cul dence from colonial rule. By the end of the tures have arisen there. century, government had passed firmly into Physically, Africa is one enormous plateau. It African hands. However, the newly independ has no continental-scale mountain chains, no ent nations must still deal with the legacy of peninsulas, no deep fjords. Most of the conti colonialism. The boundaries the European nent is more than 1000 feet (300m) above sea powers created often cut across ethnic and cul level; over half is above 2500 feet (800 m). tural groups. Many African nations today are Africa's early history reflects the wide stretch still struggling to reconcile the different cul of the continent. -
RABBINIC KNOWLEDGE of BLACK AFRICA (Sifre Deut. 320)
1 [The following essay was published in the Jewish Studies Quarterly 5 (1998) 318-28. The essay appears here substantially as published but with some additions indicated in this color .]. RABBINIC KNOWLEDGE OF BLACK AFRICA (Sifre Deut. 320) David M. Goldenberg While the biblical corpus contains references to the people and practices of black Africa (e.g. Isa 18:1-2), little such information is found in the rabbinic corpus. To a degree this may be due to the different genre of literature represented by the rabbinic texts. Nevertheless, it seems unlikely that black Africa and its peoples would be entirely unknown to the Palestinian Rabbis of the early centuries. An indication of such knowledge is, I believe, found imbedded in a midrashic text of the third century. Deut 32:21 describes the punishment God has decided to inflict on Israel for her disloyalty to him: “I will incense them with a no-folk ( be-lo < >am ); I will vex them with a nation of fools ( be-goy nabal ).” A tannaitic commentary to the verse states: ואני אקניאם בלא עם : אל תהי קורא בלא עם אלא בלוי עם אלו הבאים מתוך האומות ומלכיות ומוציאים אותם מתוך בתיהם דבר אחר אלו הבאים מברבריא וממרטניא ומהלכים ערומים בשוק “And I will incense them with a be-lo < >am .” Do not read bl < >m, but blwy >m, this refers to those who come from among the nations and kingdoms and expel them [the Jews] from their homes. Another interpretation: This refers to those who come from barbaria and mr ãny <, who go about naked in the market place. -
Maloti-Drakensberg Park, Lesotho & South Africa
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Maloti-Drakensberg Park - 2020 Conservation Outlook Assessment Maloti-Drakensberg Park 2020 Conservation Outlook Assessment SITE INFORMATION Country: Lesotho, South Africa Inscribed in: 2000 Criteria: (i) (iii) (vii) (x) The Maloti-Drakensberg Park is a transboundary site composed of the uKhahlamba Drakensberg National Park in South Africa and the Sehlathebe National Park in Lesotho. The site has exceptional natural beauty in its soaring basaltic buttresses, incisive dramatic cutbacks, and golden sandstone ramparts as well as visually spectacular sculptured arches, caves, cliffs, pillars and rock pools. The site's diversity of habitats protects a high level of endemic and globally important plants. The site harbors endangered species such as the Cape vulture (Gyps coprotheres) and the bearded vulture (Gypaetus barbatus). Lesotho’s Sehlabathebe National Park also harbors the Maloti minnow (Pseudobarbus quathlambae), a critically endangered fish species only found in this park. This spectacular natural site contains many caves and rock-shelters with the largest and most concentrated group of paintings in Africa south of the Sahara. They represent the spiritual life of the San people, who lived in this area over a period of 4,000 years. © UNESCO SUMMARY 2020 Conservation Outlook Finalised on 01 Dec 2020 SIGNIFICANT CONCERN The conservation outlook for Maloti-Drakensberg Park is of significant concern. The EKZNW management staff are highly dedicated and experienced and there is also significant appreciation for the values of the Maloti Drakensberg by communities living nearby as evidenced, for example, by the vehemently strong opposition to the possibility of oil and gas exploration in the area. -
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. -
Bromine Geochemistry of Salar De Uyuni and Deeper Salt Crusts
... .............. * .. ........, ., ;: ... ... ........ .. ........, ., '_.~' . ...: .. ,... ' :, .. , ._... , .-. ,; ..,. _I. ................. .. ; . ... ............ ~ .. .- ............'. ............ .... , . :.. , *.,:.:-' ' .., '. -. - .. 'c..;..,. CHEMICAL /./da 3-4 GEOLOGY lSCL1lDlNri L ISOTOPE GEOSCIEiYCE ELSEVIER Chemical Geology 167 (2000) 373-392 www.elsevier.com/locate/chemgeo Bromine geochemistry of salar de Uyuni and deeper salt crusts, Central Altiplano, Bolivia I FranGois/Risacher a, Bertrand Fritz i E IRD-Centre de Géochiiliie de Ia Siriface, Fralice CNRS 1 rite Blessig, 67084 Strasboiirg Cedex, France Received 15 August 1999; accepted 13 December 1999 Abstract The salar of Uyuni, in the central Bolivian Altiplano, is probably the largest salt pan in the world (10000 km'). A 121 m deep well drilled in the central salar disclosed a complex evaporitic sequence of 12 salt crusts separated by 11 mud layers. In the lower half of the profile, thick halite beds alternate with thin mud layers. The mud layers thicken upwards and show clear lacustrine features. The thickness of the salt beds decreases markedly from the base upward. The bromine content of the halite ranges from 1.3 to 10.4 mg/kg. The halite does not originate from the evaporation of the dilute inflow waters of the Altiplano, which would lead to Br content of tens of mg/kg. The presence of halite of very low Br content (2 mg/kg) in a gypsum diapir strongly suggests that most of the halite deposited at Uyuni originated from the leaching of ancient salt formations associated with the numerous gypsum diapirs of the Altiplano. The deep and thick halite beds were probably deposited in a playa lake, as suggested by their very low and fairly constant Br content (1.6-2.3 mg/kg) and by the abundance of detrital minerals. -
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. -
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. -
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).