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Measuring Up
Annual review 2016 The value we bring to media Measuring MESSAGE FROM THE CHAIR There are many positive testimonials to the work of the foundation over the years from the thousands of alumni who have benefited from our training. The most heartening compliment, repeated often, is that a Thomson Foundation course has been “a life-changing experience.” In an age, however, when funders want a more quantifiable impact, it is gratifying to have detailed external evidence of our achievements. Such is the case in Sudan (pages 10-13) where, over a four-year period, we helped to improve the quality of reporting of 700 journalists from print, radio and TV. An independent evaluation, led by a respected media development expert during 2016, showed that 98 per cent of participants felt the training had given them tangible benefits, including helping their career development. The evaluation also proved that a long-running training programme had helped to address systemic problems in a difficult regime, such as giving journalists the skills to minimise self-censorship and achieve international Measuring standards of reporting. Measuring the effectiveness of media development and journalism training courses has long been a contentious our impact issue. Sudan shows it is easier to do over the long term. As our digital training platform develops (pages 38-40), it will also be possible to measure the impact of a training in 2016 course in the short term. Our interactive programmes have been designed, and technology platform chosen, specifically so that real-time performance data for each user can be made easily available and progress measured. -
Back Matter (PDF)
Index Page numbers in italic refer to tables, and those in bold to figures. accretionary orogens, defined 23 Namaqua-Natal Orogen 435-8 Africa, East SW Angola and NW Botswana 442 Congo-Sat Francisco Craton 4, 5, 35, 45-6, 49, 64 Umkondo Igneous Province 438-9 palaeomagnetic poles at 1100-700 Ma 37 Pan-African orogenic belts (650-450 Ma) 442-50 East African(-Antarctic) Orogen Damara-Lufilian Arc-Zambezi Belt 3, 435, accretion and deformation, Arabian-Nubian Shield 442-50 (ANS) 327-61 Katangan basaltic rocks 443,446 continuation of East Antarctic Orogen 263 Mwembeshi Shear Zone 442 E/W Gondwana suture 263-5 Neoproterozoic basin evolution and seafloor evolution 357-8 spreading 445-6 extensional collapse in DML 271-87 orogenesis 446-51 deformations 283-5 Ubendian and Kibaran Belts 445 Heimefront Shear Zone, DML 208,251, 252-3, within-plate magmatism and basin initiation 443-5 284, 415,417 Zambezi Belt 27,415 structural section, Neoproterozoic deformation, Zambezi Orogen 3, 5 Madagascar 365-72 Zambezi-Damara Belt 65, 67, 442-50 see also Arabian-Nubian Shield (ANS); Zimbabwe Belt, ophiolites 27 Mozambique Belt Zimbabwe Craton 427,433 Mozambique Belt evolution 60-1,291, 401-25 Zimbabwe-Kapvaal-Grunehogna Craton 42, 208, 250, carbonates 405.6 272-3 Dronning Mand Land 62-3 see also Pan-African eclogites and ophiolites 406-7 Africa, West 40-1 isotopic data Amazonia-Rio de la Plata megacraton 2-3, 40-1 crystallization and metamorphic ages 407-11 Birimian Orogen 24 Sm-Nd (T DM) 411-14 A1-Jifn Basin see Najd Fault System lithologies 402-7 Albany-Fraser-Wilkes -
Pan-African Orogeny 1
Encyclopedia 0f Geology (2004), vol. 1, Elsevier, Amsterdam AFRICA/Pan-African Orogeny 1 Contents Pan-African Orogeny North African Phanerozoic Rift Valley Within the Pan-African domains, two broad types of Pan-African Orogeny orogenic or mobile belts can be distinguished. One type consists predominantly of Neoproterozoic supracrustal and magmatic assemblages, many of juvenile (mantle- A Kröner, Universität Mainz, Mainz, Germany R J Stern, University of Texas-Dallas, Richardson derived) origin, with structural and metamorphic his- TX, USA tories that are similar to those in Phanerozoic collision and accretion belts. These belts expose upper to middle O 2005, Elsevier Ltd. All Rights Reserved. crustal levels and contain diagnostic features such as ophiolites, subduction- or collision-related granitoids, lntroduction island-arc or passive continental margin assemblages as well as exotic terranes that permit reconstruction of The term 'Pan-African' was coined by WQ Kennedy in their evolution in Phanerozoic-style plate tectonic scen- 1964 on the basis of an assessment of available Rb-Sr arios. Such belts include the Arabian-Nubian shield of and K-Ar ages in Africa. The Pan-African was inter- Arabia and north-east Africa (Figure 2), the Damara- preted as a tectono-thermal event, some 500 Ma ago, Kaoko-Gariep Belt and Lufilian Arc of south-central during which a number of mobile belts formed, sur- and south-western Africa, the West Congo Belt of rounding older cratons. The concept was then extended Angola and Congo Republic, the Trans-Sahara Belt of to the Gondwana continents (Figure 1) although West Africa, and the Rokelide and Mauretanian belts regional names were proposed such as Brasiliano along the western Part of the West African Craton for South America, Adelaidean for Australia, and (Figure 1). -
Militia Politics
INTRODUCTION Humboldt – Universität zu Berlin Dissertation MILITIA POLITICS THE FORMATION AND ORGANISATION OF IRREGULAR ARMED FORCES IN SUDAN (1985-2001) AND LEBANON (1975-1991) Zur Erlangung des akademischen Grades doctor philosophiae (Dr. phil) Philosophische Fakultät III der Humbold – Universität zu Berlin (M.A. B.A.) Jago Salmon; 9 Juli 1978; Canberra, Australia Dekan: Prof. Dr. Gert-Joachim Glaeßner Gutachter: 1. Dr. Klaus Schlichte 2. Prof. Joel Migdal Tag der mündlichen Prüfung: 18.07.2006 INTRODUCTION You have to know that there are two kinds of captain praised. One is those who have done great things with an army ordered by its own natural discipline, as were the greater part of Roman citizens and others who have guided armies. These have had no other trouble than to keep them good and see to guiding them securely. The other is those who not only have had to overcome the enemy, but, before they arrive at that, have been necessitated to make their army good and well ordered. These without doubt merit much more praise… Niccolò Machiavelli, The Art of War (2003, 161) INTRODUCTION Abstract This thesis provides an analysis of the organizational politics of state supporting armed groups, and demonstrates how group cohesion and institutionalization impact on the patterns of violence witnessed within civil wars. Using an historical comparative method, strategies of leadership control are examined in the processes of organizational evolution of the Popular Defence Forces, an Islamist Nationalist militia, and the allied Lebanese Forces, a Christian Nationalist militia. The first group was a centrally coordinated network of irregular forces which fielded ill-disciplined and semi-autonomous military units, and was responsible for severe war crimes. -
A Review of the Neoproterozoic to Cambrian Tectonic Evolution
Accepted Manuscript Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution H. Fritz, M. Abdelsalam, K.A. Ali, B. Bingen, A.S. Collins, A.R. Fowler, W. Ghebreab, C.A. Hauzenberger, P.R. Johnson, T.M. Kusky, P. Macey, S. Muhongo, R.J. Stern, G. Viola PII: S1464-343X(13)00104-0 DOI: http://dx.doi.org/10.1016/j.jafrearsci.2013.06.004 Reference: AES 1867 To appear in: African Earth Sciences Received Date: 8 May 2012 Revised Date: 16 June 2013 Accepted Date: 21 June 2013 Please cite this article as: Fritz, H., Abdelsalam, M., Ali, K.A., Bingen, B., Collins, A.S., Fowler, A.R., Ghebreab, W., Hauzenberger, C.A., Johnson, P.R., Kusky, T.M., Macey, P., Muhongo, S., Stern, R.J., Viola, G., Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution, African Earth Sciences (2013), doi: http://dx.doi.org/10.1016/j.jafrearsci.2013.06.004 This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. 1 Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian 2 tectonic evolution 3 H. -
113–729 State, Foreign Operations, and Related Programs Appropriations for Fiscal Year 2015
S. HRG. 113–729 STATE, FOREIGN OPERATIONS, AND RELATED PROGRAMS APPROPRIATIONS FOR FISCAL YEAR 2015 HEARINGS BEFORE A SUBCOMMITTEE OF THE COMMITTEE ON APPROPRIATIONS UNITED STATES SENATE ONE HUNDRED THIRTEENTH CONGRESS SECOND SESSION ON H.R. 5013/S. 2499 AN ACT MAKING APPROPRIATIONS FOR THE DEPARTMENT OF STATE, FOREIGN OPERATIONS, AND RELATED PROGRAMS FOR THE FISCAL YEAR ENDING SEPTEMBER 30, 2015, AND FOR OTHER PURPOSES Department of State United States Agency for International Development Printed for the use of the Committee on Appropriations ( Available via the World Wide Web: http://www.gpo.gov/fdsys/browse/ committee.action?chamber=senate&committee=appropriations U.S. GOVERNMENT PUBLISHING OFFICE 87–254 PDF WASHINGTON : 2015 For sale by the Superintendent of Documents, U.S. Government Publishing Office Internet: bookstore.gpo.gov Phone: toll free (866) 512–1800; DC area (202) 512–1800 Fax: (202) 512–2104 Mail: Stop IDCC, Washington, DC 20402–0001 COMMITTEE ON APPROPRIATIONS BARBARA A. MIKULSKI, Maryland, Chairwoman PATRICK J. LEAHY, Vermont RICHARD C. SHELBY, Alabama, Vice TOM HARKIN, Iowa Chairman PATTY MURRAY, Washington THAD COCHRAN, Mississippi DIANNE FEINSTEIN, California MITCH McCONNELL, Kentucky RICHARD J. DURBIN, Illinois LAMAR ALEXANDER, Tennessee TIM JOHNSON, South Dakota SUSAN M. COLLINS, Maine MARY L. LANDRIEU, Louisiana LISA MURKOWSKI, Alaska JACK REED, Rhode Island LINDSEY GRAHAM, South Carolina MARK L. PRYOR, Arkansas MARK KIRK, Illinois JON TESTER, Montana DANIEL COATS, Indiana TOM UDALL, New Mexico ROY BLUNT, Missouri JEANNE SHAHEEN, New Hampshire JERRY MORAN, Kansas JEFF MERKLEY, Oregon JOHN HOEVEN, North Dakota MARK BEGICH, Alaska MIKE JOHANNS, Nebraska CHRISTOPHER A. COONS, Delaware JOHN BOOZMAN, Arkansas CHARLES E. -
A Detrital Record of the Nile River and Its Catchment
Downloaded from http://jgs.lyellcollection.org/ by guest on September 26, 2021 Research article Journal of the Geological Society Published online December 7, 2016 https://doi.org/10.1144/jgs2016-075 | Vol. 174 | 2017 | pp. 301–317 A detrital record of the Nile River and its catchment Laura Fielding1, Yani Najman1*, Ian Millar2, Peter Butterworth3, Sergio Ando4, Marta Padoan4, Dan Barfod5 & Ben Kneller6 1 Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK 2 NIGL, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK 3 BP Egypt, 14 Road 252, Al Maadi, Cairo, Egypt 4 DISAT, University of Milano-Bicocca, Piazza della Scienza, 4 20126 Milano, Italy 5 SUERC, Rankine Ave, Scottish Enterprise Technology Park, East Kilbride, G75 0QF, UK 6 University of Aberdeen, Aberdeen AB24 3FX, UK *Correspondence: [email protected] Abstract: This research uses analyses from Nile catchment rivers, wadis, dunes and bedrocks to constrain the geological history of NE Africa and document influences on the composition of sediment reaching the Nile delta. Our data show evolution of the North African crust, highlighting phases in the development of the Arabian–Nubian Shield and amalgamation of Gondwana in Neoproterozoic times. The Saharan Metacraton and Congo Craton in Uganda have a common history of crustal growth, with new crust formation at 3.0 – 3.5 Ga, and crustal melting at c. 2.7 Ga. The Hammamat Formation of the Arabian– Nubian Shield is locally derived and has a maximum depositional age of 635 Ma. By contrast, Phanerozoic sedimentary rocks are derived from more distant sources. The fine-grained (mud) bulk signature of the modern Nile is dominated by input from the Ethiopian Highlands, transported by the Blue Nile and Atbara rivers. -
Getting by on the Margins: Sudanese and Somali Refugees a Case Report of Refugees in Towns Cairo, Egypt
Getting by on the Margins: Sudanese and Somali Refugees A Case Report of Refugees in Towns Cairo, Egypt Paul Miranda Cairo, Egypt / A Case Report of Refugees in Towns 1 JUNE 2018 Contents About the RIT Project 3 Location 4 Introduction 5 About the Author and How He Wrote the Report 5 Background on Forced Migration to Egypt 6 Legal Framework Governing Refugees in Egypt 8 Background on Forced Migration in Greater Cairo 9 Mapping Cairo’s Refugees 10 Sudanese and Somali Neighborhoods: Hay el Ashr and Araba wa Nus 12 Governance 12 Demographics 13 Spatial Distribution of Populations in Hay el Ashr and Araba wa Nus 13 Refugees’ Experiences 15 Livelihoods 15 Children’s Education 16 Medical services 17 Urban Impact on the Economy and Housing 17 The local economy: Sudanese and Somali businesses 18 Housing 18 Governance 20 African Refugees’ Experiences 21 Racism 21 Social Networks and Political Mobilization 23 Gangs 23 Future Outlooks on Integration 24 Conclusion 25 References 26 Cairo, Egypt / A Case Report of Refugees in Towns 2 About the RIT Project The Refugees in Towns (RIT) project promotes understanding of the migrant/refugee experience in urban settings. Our goal is to understand and promote refugee integration by drawing on the knowledge and perspective of refugees and locals to develop deeper understanding of the towns in which they live. The project was conceived and is led by Karen Jacobsen. It is based at the Feinstein International Center at Tufts University and funded by the Henry J. Leir Foundation. Our goals are twofold Our first long-term goal is to build a theory of integration form the ground up by compiling a global database of case studies and reports to help us analyze and understand the process of immigrant/refugee integration. -
Nuba Mountains So That Nothing Can Exist There.’13 Zens by Sudan’S Arab Elite, the Nuba’S Was Brutal
expanding herds.9 Although repre- Yousif Kuwa Mekke, they demanded out of their homes were forcibly relo- senting a ‘bewildering complexity’ of ‘the right to be Nuba’ and an end to cated to ‘peace camps’ in government- tribes,10 with different cultures, inter- marginalization in all its forms. As controlled areas. Nuba women were ests, and grievances, most Nuba are ‘Africans’ within the political bounda- systematically raped and children for- sedentary farmers and share an expe- ries of Arab-dominated northern Sudan, cibly Islamized.12 The head of security rience of oppression. The subjugation they fervently supported SPLA Chair- in South Kordofan, who later sought extends from the slaving raids of the man John Garang’s vision of a ‘New political asylum in Switzerland, said 19th century to the jihad declared against Sudan’, in which all Sudanese would the orders given to government troops them during the civil war by the gov- have equal rights and duties, irrespec- were ‘to kill anything that is alive . ernment of President Omar al-Bashir. tive of ethnicity. to destroy everything, to burn the area Long regarded as second-class citi- The civil war in the Nuba Mountains so that nothing can exist there.’13 zens by Sudan’s Arab elite, the Nuba’s was brutal. The government of Sadiq For 13 years, Nuba in SPLM/A- indigenous cultures and religions were al-Mahdi (1986–89) armed the Baggara controlled areas went without humani- suppressed, and local languages banned. to fight their Nuba neighbours, politi- tarian aid: the government sealed off Many reacted to political, economic, cizing age-old resource tensions. -
A Detrital Record of the Nile River and Its Catchment
Research article Journal of the Geological Society Published online December 7, 2016 https://doi.org/10.1144/jgs2016-075 | Vol. 174 | 2017 | pp. 301–317 A detrital record of the Nile River and its catchment Laura Fielding1, Yani Najman1*, Ian Millar2, Peter Butterworth3, Sergio Ando4, Marta Padoan4, Dan Barfod5 & Ben Kneller6 1 Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK 2 NIGL, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK 3 BP Egypt, 14 Road 252, Al Maadi, Cairo, Egypt 4 DISAT, University of Milano-Bicocca, Piazza della Scienza, 4 20126 Milano, Italy 5 SUERC, Rankine Ave, Scottish Enterprise Technology Park, East Kilbride, G75 0QF, UK 6 University of Aberdeen, Aberdeen AB24 3FX, UK *Correspondence: [email protected] Abstract: This research uses analyses from Nile catchment rivers, wadis, dunes and bedrocks to constrain the geological history of NE Africa and document influences on the composition of sediment reaching the Nile delta. Our data show evolution of the North African crust, highlighting phases in the development of the Arabian–Nubian Shield and amalgamation of Gondwana in Neoproterozoic times. The Saharan Metacraton and Congo Craton in Uganda have a common history of crustal growth, with new crust formation at 3.0 – 3.5 Ga, and crustal melting at c. 2.7 Ga. The Hammamat Formation of the Arabian– Nubian Shield is locally derived and has a maximum depositional age of 635 Ma. By contrast, Phanerozoic sedimentary rocks are derived from more distant sources. The fine-grained (mud) bulk signature of the modern Nile is dominated by input from the Ethiopian Highlands, transported by the Blue Nile and Atbara rivers. -
Local and Regional Dimensions of Chad–Sudan Rapprochement
25 Renouncing the Rebels: Local and Regional Dimensions of Chad–Sudan Rapprochement By Jérôme Tubiana Copyright Published in Switzerland by the Small Arms Survey © Small Arms Survey, Graduate Institute of International and Development Studies, Geneva 2011 First published in March 2011 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, without prior permission in writing of the Small Arms Survey, or as expressly permitted by law, or under terms agreed with the appropriate reprographics rights organi- zation. Enquiries concerning reproduction outside the scope of the above should be sent to the Publications Manager, Small Arms Survey, at the address below. Small Arms Survey Graduate Institute of International and Development Studies 47 Avenue Blanc, 1202 Geneva, Switzerland Edited by Diana Rodriguez and Emile LeBrun Copy-edited by Alex Potter ([email protected]) Proofread by John Linnegar ([email protected]) Typeset in Optima and Palatino by Richard Jones ([email protected]) Printed by nbmedia in Geneva, Switzerland ISBN 978-2-940415-48-9 2 Small Arms Survey HSBA Working Paper 25 Tubiana Denouncing the Rebels 3 Contents List of abbreviations and acronyms .................................................................................................................................... 5 Executive summary ..................................................................................................................................................................................... -
Class G Tables of Geographic Cutter Numbers: Maps -- by Region Or Country -- Eastern Hemisphere -- Africa
G8202 AFRICA. REGIONS, NATURAL FEATURES, ETC. G8202 .C5 Chad, Lake .N5 Nile River .N9 Nyasa, Lake .R8 Ruzizi River .S2 Sahara .S9 Sudan [Region] .T3 Tanganyika, Lake .T5 Tibesti Mountains .Z3 Zambezi River 2717 G8222 NORTH AFRICA. REGIONS, NATURAL FEATURES, G8222 ETC. .A8 Atlas Mountains 2718 G8232 MOROCCO. REGIONS, NATURAL FEATURES, ETC. G8232 .A5 Anti-Atlas Mountains .B3 Beni Amir .B4 Beni Mhammed .C5 Chaouia region .C6 Coasts .D7 Dra region .F48 Fezouata .G4 Gharb Plain .H5 High Atlas Mountains .I3 Ifni .K4 Kert Wadi .K82 Ktaoua .M5 Middle Atlas Mountains .M6 Mogador Bay .R5 Rif Mountains .S2 Sais Plain .S38 Sebou River .S4 Sehoul Forest .S59 Sidi Yahia az Za region .T2 Tafilalt .T27 Tangier, Bay of .T3 Tangier Peninsula .T47 Ternata .T6 Toubkal Mountain 2719 G8233 MOROCCO. PROVINCES G8233 .A2 Agadir .A3 Al-Homina .A4 Al-Jadida .B3 Beni-Mellal .F4 Fès .K6 Khouribga .K8 Ksar-es-Souk .M2 Marrakech .M4 Meknès .N2 Nador .O8 Ouarzazate .O9 Oujda .R2 Rabat .S2 Safi .S5 Settat .T2 Tangier Including the International Zone .T25 Tarfaya .T4 Taza .T5 Tetuan 2720 G8234 MOROCCO. CITIES AND TOWNS, ETC. G8234 .A2 Agadir .A3 Alcazarquivir .A5 Amizmiz .A7 Arzila .A75 Asilah .A8 Azemmour .A9 Azrou .B2 Ben Ahmet .B35 Ben Slimane .B37 Beni Mellal .B4 Berkane .B52 Berrechid .B6 Boujad .C3 Casablanca .C4 Ceuta .C5 Checkaouene [Tétouan] .D4 Demnate .E7 Erfond .E8 Essaouira .F3 Fedhala .F4 Fès .F5 Figurg .G8 Guercif .H3 Hajeb [Meknès] .H6 Hoceima .I3 Ifrane [Meknès] .J3 Jadida .K3 Kasba-Tadla .K37 Kelaa des Srarhna .K4 Kenitra .K43 Khenitra .K5 Khmissat .K6 Khouribga .L3 Larache .M2 Marrakech .M3 Mazagan .M38 Medina .M4 Meknès .M5 Melilla .M55 Midar .M7 Mogador .M75 Mohammedia .N3 Nador [Nador] .O7 Oued Zem .O9 Oujda .P4 Petitjean .P6 Port-Lyantey 2721 G8234 MOROCCO.