The Cross and the River:Ethiopia, Egypt, and the Nile
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Humanitarian Situation Report No. 19 Q3 2020 Highlights
Sudan Humanitarian Situation Report No. 19 Q3 2020 UNICEF and partners assess damage to communities in southern Khartoum. Sudan was significantly affected by heavy flooding this summer, destroying many homes and displacing families. @RESPECTMEDIA PlPl Reporting Period: July-September 2020 Highlights Situation in Numbers • Flash floods in several states and heavy rains in upriver countries caused the White and Blue Nile rivers to overflow, damaging households and in- 5.39 million frastructure. Almost 850,000 people have been directly affected and children in need of could be multiplied ten-fold as water and mosquito borne diseases devel- humanitarian assistance op as flood waters recede. 9.3 million • All educational institutions have remained closed since March due to people in need COVID-19 and term realignments and are now due to open again on the 22 November. 1 million • Peace talks between the Government of Sudan and the Sudan Revolu- internally displaced children tionary Front concluded following an agreement in Juba signed on 3 Oc- tober. This has consolidated humanitarian access to the majority of the 1.8 million Jebel Mara region at the heart of Darfur. internally displaced people 379,355 South Sudanese child refugees 729,530 South Sudanese refugees (Sudan HNO 2020) UNICEF Appeal 2020 US $147.1 million Funding Status (in US$) Funds Fundi received, ng $60M gap, $70M Carry- forward, $17M *This table shows % progress towards key targets as well as % funding available for each sector. Funding available includes funds received in the current year and carry-over from the previous year. 1 Funding Overview and Partnerships UNICEF’s 2020 Humanitarian Action for Children (HAC) appeal for Sudan requires US$147.11 million to address the new and protracted needs of the afflicted population. -
Sudan's Spreading Conflict (II): War in Blue Nile
Sudan’s Spreading Conflict (II): War in Blue Nile Africa Report N°204 | 18 June 2013 International Crisis Group Headquarters Avenue Louise 149 1050 Brussels, Belgium Tel: +32 2 502 90 38 Fax: +32 2 502 50 38 [email protected] Table of Contents Executive Summary ................................................................................................................... i Recommendations..................................................................................................................... iii I. Introduction ..................................................................................................................... 1 II. A Sudan in Miniature ....................................................................................................... 3 A. Old-Timers Versus Newcomers ................................................................................. 3 B. A History of Land Grabbing and Exploitation .......................................................... 5 C. Twenty Years of War in Blue Nile (1985-2005) ........................................................ 7 III. Failure of the Comprehensive Peace Agreement ............................................................. 9 A. The Only State with an Opposition Governor (2007-2011) ...................................... 9 B. The 2010 Disputed Elections ..................................................................................... 9 C. Failed Popular Consultations ................................................................................... -
Anatomy of the Nile Following the Twists and Turns of the World's Longest River
VideoMedia Spotlight Anatomy of the Nile Following the twists and turns of the world's longest river For the complete video with media resources, visit: http://education.nationalgeographic.org/media/anatomy-nile/ Funder The Nile River has provided fertile land, transportation, food, and freshwater to Egypt for more than 5,000 years. Today, 95% of Egypt’s population continues to live along its banks. Where does the Nile begin? Where does it end? Watch this video, from Nat Geo WILD’s “Destination Wild” series, to find out. For an even deeper look at the Nile, use our vocabulary list and explore our “geo-tour” of the Nile to understand the geography of the river and answer the questions in the Questions tab. Questions Where is the source, or headwaters, of the Nile River? The streams of Rwanda’s Nyungwe Forest are probably the most remote sources of the Nile. The snow-capped peaks of the Rwenzori Mountains are another one of the remote sources of the Nile. The Rwenzori Mountains, sometimes nicknamed the “Mountains of the Moon,” straddle the border between the Democratic Republic of the Congo and Uganda. Many geographers also consider Lake Victoria, the largest lake in Africa, to be a source of the Nile. The most significant outflow from Lake Victoria, winding northward through Uganda, is called the “Victoria Nile.” Can you find a waterfall on the Nile River? As it twists more than 6,500 kilometers (4,200 miles) through Africa, the Nile has dozens of small and large waterfalls. The most significant waterfall on the Nile is probably Murchison Falls, Uganda. -
The Blue Nile the BLUE NILE
The Blue Nile THE BLUE NILE Bahar Dar Renaissance Tissitat ROUTE PLAN Addis Ababa - Addis Ababa - Bahar Dar - Tana Lake - Tissitat - Renaissance Dam THE BLUE NILE For most of us, the Nile has no colour. And it is Egyptian. That’s because many of us pay more attention to history than to geography, and in the stories of history, we tend to listen only to the voice of the victors. Once upon a time there was Egypt, the daughter of all the possible gods, including the sun no less. An Egypt self-proclaimed "Gift of the Nile". Without the summer floods, no fertile silt was deposited on the banks and thus there was no Egypt. The affair was understood: the Nile and Egypt were intrinsically linked, and all the more closely since the Pharaohs had, by weaving this Union, created the most poetic of mythologies, illustrated by the most beautiful of bestiaries: jackal, falcon, cat ... And add to that a grandiose civilisation of the dead. How could one fight against it? It would be like separating the Parthenon from the Acropolis. And when the great powers, Ottoman or British, dominated Cairo and the delta, meaning downstream of the river, what other choice did the countries upstream have but to give up the water to their all-powerful neighbour, even if this water came from their land ? THE BLUE NILE a Spaniard who discovered two natural springs sixty kilometres south-southwest of Lake Tana at the foot of Mount Gish on 21 April 1618. From there flows a river which little by little swells and reaches the lake. -
The Nile: Evolution, Quaternary River Environments and Material Fluxes
13 The Nile: Evolution, Quaternary River Environments and Material Fluxes Jamie C. Woodward1, Mark G. Macklin2, Michael D. Krom3 and Martin A.J. Williams4 1School of Environment and Development, The University of Manchester, Manchester M13 9PL, UK 2Institute of Geography and Earth Sciences, University of Wales, Aberystwyth, Aberystwyth SY23 3DB, UK 3School of Earth Sciences, University of Leeds, Leeds LS2 9JT, UK 4Geographical and Environmental Studies, University of Adelaide, Adelaide, South Australia 5005, Australia 13.1 INTRODUCTION et al., 1980; Williams et al., 2000; Woodward et al., 2001; Krom et al., 2002) as well as during previous interglacial The Nile Basin contains the longest river channel system and interstadial periods (Williams et al., 2003). The true in the world (>6500 km) that drains about one tenth of the desert Nile begins in central Sudan at Khartoum (15° African continent. The evolution of the modern drainage 37′ N 32° 33′ E) on the Gezira Plain where the Blue Nile network and its fl uvial geomorphology refl ect both long- and the White Nile converge (Figure 13.1). These two term tectonic and volcanic processes and associated systems, and the tributary of the Atbara to the north, are changes in erosion and sedimentation, in addition to sea all large rivers in their own right with distinctive fl uvial level changes (Said, 1981) and major shifts in climate and landscapes and process regimes. The Nile has a total vegetation during the Quaternary Period (Williams and catchment area of around 3 million km2 (Figure 13.1 and Faure, 1980). More recently, human impacts in the form Table 13.1). -
The Nile Dam Dispute: Issues for Congress
INSIGHTi The Nile Dam Dispute: Issues for Congress July 27, 2020 Overview A long-running dispute between Ethiopia, Egypt, and Sudan over the waters of the Nile flared in 2020, as Ethiopia moves toward completion of Africa’s largest hydroelectric power project, the Grand Ethiopian Renaissance Dam (GERD). The domestic stakes are high for both Ethiopian Prime Minister Abiy Ahmed, who seeks to guide Ethiopia through a fragile political transition, and Egypt’s President Abdel Fattah al Sisi, who seeks to preserve Egypt’s share of the Nile amidst population growth, pollution, and rising sea levels. Efforts to resolve the conflict, including by the United States, have yet to result in a final agreement. Alongside the potential for the dispute to escalate, failure to reach an accord could set a negative precedent for transboundary water cooperation at a time of growing global concern over climate change, demographic growth, and resource scarcity. Background For Ethiopia, where almost 70% the rural population lacks access to electricity, the GERD would significantly expand domestic power capacity and allow the country to sell excess electricity to its neighbors. When construction began on the $4 billion project in 2011, then-Prime Minister Meles Zenawi pledged that Ethiopia would finance the project itself, funding it through government bonds, donations, taxes, and a portion of civil servants’ salaries. He envisioned the 6,000-megawatt GERD as powering Ethiopia’s development and helping to lift its population out of poverty. The project has been a source of national pride for Ethiopians, and a rallying point amidst recent domestic troubles. -
Egypt and the Hydro-Politics of the Blue Nile River Daniel Kendie
Egypt and the Hydro-Politics of the Blue Nile River Daniel Kendie Northeast African Studies, Volume 6, Number 1-2, 1999 (New Series), pp. 141-169 (Article) Published by Michigan State University Press DOI: https://doi.org/10.1353/nas.2002.0002 For additional information about this article https://muse.jhu.edu/article/23689 [ This content has been declared free to read by the pubisher during the COVID-19 pandemic. ] Egypt and the Hydro-Politics of the Blue Nile River Daniel Kendie Henderson State University As early as the 4th century B.C., Herodotus observed that Egypt was a gift of the Ni l e . That observation is no less true today than in the distant past, because not only the prosperity of Egypt, but also its very existence depends on the annual flood of the Nile. Of its two sources, the Blue Nile flows from Lake Tana in Ethiopia, while the White Nile flows from Lake Victoria in Uganda. Some 86 pe r cent of the water that Egypt consumes annually originates from the Blue Nile Ri ve r , while the remainder comes from the White Nile. Since concern with the fr ee flow of the Nile has always been a national security issue for Egypt, as far as the Blue Nile goes it has been held that Egypt must be in a position either to dominate Ethiopia, or to neutralize whatever unfriendly regime might emerge th e r e. As the late President Sadat stated: “ Any action that would endanger the waters of the Blue Nile will be faced with a firm reaction on the part of Egypt, even if that action should lead to war. -
Water Atlas of the TEKEZE-ATBARA-SETIT SUB-BASIN
Water Atlas of THE TEKEZE-ATBARA-SETIT SUB-BASIN Draft Draft Eastern Nile Technical Regional Office (ENTRO) , 2006 page - Table of Content Introduction 1 Quick Overview of the Eastern Nile Basin 3 General 1.1. Location of Baro-Akobo-Sobat Basin 1.. Administrative Units 1.. Demography 1.4. Economy 1.5. Historical and Cultural Places Land Surface Feature 4 2.1. Topography 2.. Slope and Terrain 2. Relief 2.3. Land and River Profiles Climate 5 3.1. Rainfall 3.. Air Temperature 3.. Evaporation 3.4. Humidity Land 6 4.1. Land use /Land Cover 4.. Soil 4.. Geology 4.4. Vegetation Hydrology 7 5.1. River network and Catchments 5.. Sub-Basin Runoff volumes and Water resource 5.. River System Schematics andDraft Indicative Water Balance 5.4. Sediment Infrastructure and Utilities 8 6.1. Dams and reservoirs 6.. Irrigations and Agriculture 6.. Hydropower and Electric 6.4. Communication and Transport Environmental 9 7.1. Land Degradation 7.. Water quality Problems 7. Parks , wetlands and Protected areas 7.4 Water related Disease Eastern Nile Technical Regional Office (ENTRO) , 2006 page - Draft Eastern Nile Technical Regional Office (ENTRO) , 2006 page - 4 Introduction The Eastern Nile Technical Regional Office (ENTRO) is an organization meant to realize ENSAP (Eastern Nile Subsidiary Action Program) in the Eastern Nile Basin countries, namely Egypt, Ethiopia and Sudan. ENSAP seeks to realize the NBI Shared vision for the EN region aimed at reducing poverty, foster economic growth and the reversal of environmental degradation. Currently, under ENSAP, planning is underway for the multipurpose development of the region. To sup- port its multipurpose development objectives, ENTRO proposes to synthesize information at sub basin level categorized in three themes namely, Water Resources, Environment and Socioeconomy. -
From the Yellow Nile to the Blue Nile. the Quest for Water and the Diffusion of Northern East Sudanic Languages from the Fourth to the First Millenia BCE"
This lecture was delivered in ECAS 2009 (3rd European Conference on African Studies, Panel 142: African waters - water in Africa, barriers, paths, and resources: their impact on language, literature and history of people) in Leipzig, 4 to 7 June 2009. "From the Yellow Nile to the Blue Nile. The quest for water and the diffusion of Northern East Sudanic languages from the fourth to the first millenia BCE". Dr. Claude Rilly (CNRS-LLACAN, Paris) The quest for water and hence, for food supply, is a key issue in the appearance and diffusion of languages in the Sahelian regions of Africa. Climate changes, as occurred from the end of Neolithic period down to the second millenium BCE, played a major role in the redistribution of populations along the Nile river and its tributaries and can explain the appearance of a recently defined linguistic family, namely Northern East Sudanic (NES). This paper must be considered as a synthesis of several recent publications I wrote on this subject, so that I shall have to refer the reader, more often than not, to these earlier studies. Detailed demonstration of all these points would require much more time than is allotted to me. The Northern East Sudanic language group In his seminal study published in 1963, J. H. Greenberg divided the languages of Africa into four major phyla or superfamilies, namely Afroasiatic, Niger-Congo, Khoisan and Nilo-Saharan. If the three first phyla were more or less obvious, Nilo-Saharan was not so easily constituted, requiring from Greenberg a long work to merge twelve different families into one phylum. -
Digital Reconstruction of the Archaeological Landscape in the Concession Area of the Scandinavian Joint Expedition to Sudanese Nubia (1961–1964)
Digital Reconstruction of the Archaeological Landscape in the Concession Area of the Scandinavian Joint Expedition to Sudanese Nubia (1961–1964) Lake Nasser, Lower Nubia: photography by the author Degree project in Egyptology/Examensarbete i Egyptologi Carolin Johansson February 2014 Department of Archaeology and Ancient History, Uppsala University Examinator: Dr. Sami Uljas Supervisors: Prof. Irmgard Hein & Dr. Daniel Löwenborg Author: Carolin Johansson, 2014 Svensk titel: Digital rekonstruktion av det arkeologiska landskapet i koncessionsområdet tillhörande den Samnordiska Expeditionen till Sudanska Nubien (1960–1964) English title: Digital Reconstruction of the Archaeological Landscape in the Concession Area of the Scandinavian Joint Expedition to Sudanese Nubia (1961–1964) A Magister thesis in Egyptology, Uppsala University Keywords: Nubia, Geographical Information System (GIS), Scandinavian Joint Expedition to Sudanese Nubia (SJE), digitalisation, digital elevation model. Carolin Johansson, Department of Archaeology and Ancient History, Uppsala University, Box 626 SE-75126 Uppsala, Sweden. Abstract The Scandinavian Joint Expedition to Sudanese Nubia (SJE) was one of the substantial contributions of crucial salvage archaeology within the International Nubian Campaign which was pursued in conjunction with the building of the High Dam at Aswan in the early 1960’s. A large quantity of archaeological data was collected by the SJE in a continuous area of northernmost Sudan and published during the subsequent decades. The present study aimed at transferring the geographical aspects of that data into a digital format thus enabling spatial enquires on the archaeological information to be performed in a computerised manner within a geographical information system (GIS). The landscape of the concession area, which is now completely submerged by the water masses of Lake Nasser, was digitally reconstructed in order to approximate the physical environment which the human societies of ancient Nubia inhabited. -
In Muslim Sudan
Downloaded from Nile Basin Research Programme www.nile.uib.no through Bergen Open Research Archive http://bora.uib.no Trade and Wadis System(s) in Muslim Sudan Intisar Soghayroun Elzein Soghayroun FOUNTAIN PUBLISHERS Kampala Fountain Publishers P. O. Box 488 Kampala - Uganda E-mail: [email protected] [email protected] Website: www.fountainpublishers.co.ug © Intisar Soghayroun Elzein Soghayroun 2010 First published 2010 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 electronic, mechanical, photocopying, recording or otherwise without the prior written permission of the publisher. ISBN: 978-9970-25-005-9 Dedication This book is dedicated to my father: Soghayroun Elzein Soghayroun, with a tremendous debt of gratitude. iii Contents Dedication..................................................................................................... iiv List.of .Maps..................................................................................................vi List.of .plates..................................................................................................vii Preface.......................................................................................................... viii Acknowledgement.........................................................................................xiii 1 The Land, its People and History ...................................... 1 The Physiographic Features of the Country ......................................1 -
Prediction of Hydrometeorological Extremes in the Sudanese Nile Region: a Need for International Co-Operation
Hydrology for the Water Management of Large Riva- Basins (Proceedings of the Vienna Symposium, August 1991). IAHS Publ. no. 201,1991. PREDICTION OF HYDROMETEOROLOGICAL EXTREMES IN THE SUDANESE NILE REGION: A NEED FOR INTERNATIONAL CO-OPERATION K. ANBAH Water Resources Research and Documentation Centre, Italian University for Foreigners, Villa La Colombella, 06080 Colombella (PG), Italy. F. SICCARDI Institute of Hydraulics, University of Genoa, Via Montallegro 1, 16145 Genoa, Italy ABSTRACT Analysis of the 1988 floods in Sudan have shown, that a lead time of at least one month is required for mitigation interventions. The present 5 days lead time for prediction of Nile floods in Khartoum are not adequate for an efficient advance warning.The rainfall over Sudan exhibits frequent positive and negative anomalies. Two approaches are suggested in the present work. The first involves further analysis on the possible spatial coherence and teleconnections of rainfall anomalies over Africa to enhance the lead time based on prediction of extreme events in other regions. The second requires an integrated real time flood forecasting and an effective weather monitoring system covering the countries sharing the Nile Basin. These demand technical cooperation between the countries within the basin. INTRODUCTION Flood Hazards Prediction For the purposes of flood prediction, the Nile basin can be divided into four main environments, namely the Equatorial Lakes, the Ethiopian, the Sudanese and the Egyptian ambient. The Equatorial Lakes and the Aswan reservoir effect long- term regulation on the flows of the White Nile and the Main Nile respectively. The Ethiopian riverine ambient with steep and confined channel does not present serious problems of inundation.