The Politics of the Nile Basin
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Outcomes of the EU Horizon 2020 DAFNE PROJECT the Omo
POLICY BRIEF October 2020 Outcomes of the EU Horizon 2020 DAFNE PROJECT The Omo-Turkana River Basin Progress towards cooperative frameworks KEY POLICY MESSAGES The OTB has reached a stage of pivotal importance for future development; the time to establish a cooperative framework on water governance is now. Transparency and accountability must be improved in order to facilitate the sharing of data and information, increasing trust and reducing the perception of risk. Benefit-sharing which extends beyond energy could enhance regional integration and improve sustainable development within the basin . THE OMO-TURKANA RIVER BASIN potential for hydropower and irrigation schemes that are, if scientifically and equitably managed, crucial to lift millions within and outside the basin out of extreme poverty; this has led to transboundary cooperation in recent years. This policy brief is derived from research conducted under the €5.5M four-year EU Horizon 2020 and Swiss funded ‘DAFNE’ project which concerns the promotion of integrated and adaptive water resources management, explicitly addressing the WEF Nexus and aiming to promote a sustainable economy in regions where new infrastructure and expanding The Omo-Turkana River Basin (OTB) – for the agriculture has to be balanced with social, purposes of the DAFNE Project – comprises of economic and environmental needs. The project two main water bodies: the Omo River in takes a multi- and interdisciplinary approach to Ethiopia and Lake Turkana which it drains into. the formation of a decision analytical While the Omo River lies entirely within Ethiopian territory, Lake Turkana is shared by framework (DAF) for participatory and both Kenya and Ethiopia, with the majority of integrated planning, to allow the evaluation of Lake Turkana residing within Kenya. -
Environmental Conflicts: the Case of the Nile River Basin
Environmental Conflicts: The case of the Nile River Basin BY MAHLAKENG KHOSI MAHLAKENG 2007117787 Submitted in fulfilment of the requirements of the Master’s Degree in the Department of Political Science Faculty of Humanities at the University of the Free State. BLOEMFONTEIN JULY 2015 SUPERVISOR: MR. PA SCHOEMAN CO-SUPERVISOR: PROF. H SOLOMON i TABLE OF CONTENTS ACKNOWLEDGEMENTS ........................................................................................... V DECLARATIONS ........................................................................................................ V ABSTRACT AND KEY WORDS.…...……………………………………………………VII Key Words………………………………………………………………………………….VII Abstract…………………………………………………………………………………….VIII LIST OF ABBREVIATIONS ........................................................................................ IX CHAPTER 1: INTRODUCTION ................................................................................... 1 1.1 Orientation and background ........................................................................... 1 1.2 Problem statement and research question ..................................................... 5 1.3 Aims and objectives of the study .................................................................... 8 1.4 Research methodology .................................................................................. 8 1.5 Literature review ........................................................................................... 10 1.6 Outline of the study ..................................................................................... -
Lake Turkana and the Lower Omo the Arid and Semi-Arid Lands Account for 50% of Kenya’S Livestock Production (Snyder, 2006)
Lake Turkana & the Lower Omo: Hydrological Impacts of Major Dam & Irrigation Development REPORT African Studies Centre Sean Avery (BSc., PhD., C.Eng., C. Env.) © Antonella865 | Dreamstime © Antonella865 Consultant’s email: [email protected] Web: www.watres.com LAKE TURKANA & THE LOWER OMO: HYDROLOGICAL IMPACTS OF MAJOR DAM & IRRIGATION DEVELOPMENTS CONTENTS – VOLUME I REPORT Chapter Description Page EXECUTIVE(SUMMARY ..................................................................................................................................1! 1! INTRODUCTION .................................................................................................................................... 12! 1.1! THE(CONTEXT ........................................................................................................................................ 12! 1.2! THE(ASSIGNMENT .................................................................................................................................. 14! 1.3! METHODOLOGY...................................................................................................................................... 15! 2! DEVELOPMENT(PLANNING(IN(THE(OMO(BASIN ......................................................................... 18! 2.1! INTRODUCTION(AND(SUMMARY(OVERVIEW(OF(FINDINGS................................................................... 18! 2.2! OMO?GIBE(BASIN(MASTER(PLAN(STUDY,(DECEMBER(1996..............................................................19! 2.2.1! OMO'GIBE!BASIN!MASTER!PLAN!'!TERMS!OF!REFERENCE...........................................................................19! -
Lake Turkana National Parks - 2017 Conservation Outlook Assessment (Archived)
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Lake Turkana National Parks - 2017 Conservation Outlook Assessment (archived) IUCN Conservation Outlook Assessment 2017 (archived) Finalised on 26 October 2017 Please note: this is an archived Conservation Outlook Assessment for Lake Turkana National Parks. To access the most up-to-date Conservation Outlook Assessment for this site, please visit https://www.worldheritageoutlook.iucn.org. Lake Turkana National Parks عقوملا تامولعم Country: Kenya Inscribed in: 1997 Criteria: (viii) (x) The most saline of Africa's large lakes, Turkana is an outstanding laboratory for the study of plant and animal communities. The three National Parks serve as a stopover for migrant waterfowl and are major breeding grounds for the Nile crocodile, hippopotamus and a variety of venomous snakes. The Koobi Fora deposits, rich in mammalian, molluscan and other fossil remains, have contributed more to the understanding of paleo-environments than any other site on the continent. © UNESCO صخلملا 2017 Conservation Outlook Critical Lake Turkana’s unique qualities as a large lake in a desert environment are under threat as the demands for water for development escalate and the financial capital to build major dams becomes available. Historically, the lake’s level has been subject to natural fluctuations in response to the vicissitudes of climate, with the inflow of water broadly matching the amount lost through evaporation (as the lake basin has no outflow). The lake’s major source of water, Ethiopia’s Omo River is being developed with a series of major hydropower dams and irrigated agricultural schemes, in particular sugar and other crop plantations. -
Turkana, Kenya): Implications for Local and Regional Stresses
Research Paper GEOSPHERE Early syn-rift igneous dike patterns, northern Kenya Rift (Turkana, Kenya): Implications for local and regional stresses, GEOSPHERE, v. 16, no. 3 tectonics, and magma-structure interactions https://doi.org/10.1130/GES02107.1 C.K. Morley PTT Exploration and Production, Enco, Soi 11, Vibhavadi-Rangsit Road, 10400, Thailand 25 figures; 2 tables; 1 set of supplemental files CORRESPONDENCE: [email protected] ABSTRACT basins elsewhere in the eastern branch of the East African Rift, which is an active rift, several studies African Rift. (Muirhead et al., 2015; Robertson et al., 2015; Wadge CITATION: Morley, C.K., 2020, Early syn-rift igneous dike patterns, northern Kenya Rift (Turkana, Kenya): Four areas (Loriu, Lojamei, Muranachok-Muru- et al., 2016) have explored interactions between Implications for local and regional stresses, tectonics, angapoi, Kamutile Hills) of well-developed structure and magmatism in the upper crust by and magma-structure interactions: Geosphere, v. 16, Miocene-age dikes in the northern Kenya Rift (Tur- ■ INTRODUCTION investigating stress orientations inferred from no. 3, p. 890–918, https://doi.org /10.1130/GES02107.1. kana, Kenya) have been identified from fieldwork cone lineaments and caldera ellipticity (dikes were Science Editor: David E. Fastovsky and satellite images; in total, >3500 dikes were The geometries of shallow igneous intrusive sys- insufficiently well exposed). Muirhead et al. (2015) Associate Editor: Eric H. Christiansen mapped. Three areas display NNW-SSE– to N-S– tems -
The Water Resources of the Nile Basin
Chapter 2 The Water Resources of the Nile Basin 500 Soroti (1914–2003) 400 300 200 100 Average monthly rainfall 0 JFMAMJ JASOND 25 KEY MESSAGES • The Nile Basin is characterized by high climatic • The headwater regions of the Nile are subject diversity and variability, a low percentage of rainfall to widespread soil erosion. Sediment yields are reaching the main river, and an uneven distribution particularly high in the Eastern Nile sub-basin, of its water resources. Potential evaporation rates which contributes 97 per cent of the total sediment in the Nile region are high, making the basin load. Most sediment is captured in reservoirs in The particularly vulnerable to drought. Sudan and Egypt, which leads to a rapid loss of • White Nile flows only contribute up to 15 per cent reservoir storage capacity. of the annual Nile discharge, but are fairly stable • The finite Nile flows are now fully utilized for throughout the year. The Eastern Nile region agricultural, domestic, industrial, and environmental supplies up to 90 per cent of annual Nile flows, but purposes, while water demand continues to rise its contribution is highly seasonal. steadily due to population growth and economic • Extensive regional aquifer systems holding development. substantial quantities of groundwater underlie the • Irrigated agriculture in Egypt and The Sudan Nile region. Some of the aquifers hold fossil water, represents the single most important consumer but others are recharged from precipitation over of the waters of the Nile, but the upper riparians the basin, or from irrigation areas and the baseflow are planning investments that will use the river’s of the Nile. -
Provenance of Sandstones in Ethiopia During
1 Provenance of sandstones in Ethiopia during Late 2 Ordovician and Carboniferous–Permian Gondwana 3 glaciations: petrography and geochemistry of the Enticho 4 Sandstone and the Edaga Arbi Glacials 5 6 Anna Lewina,*, Guido Meinholdb,c, Matthias Hinderera, Enkurie L. Dawitd, 7 Robert Busserte 8 9 aInstitut für Angewandte Geowissenschaften, Fachgebiet Angewandte 10 Sedimentologie, Technische Universität Darmstadt, Schnittspahnstraße 9, 11 64287 Darmstadt, Germany 12 bAbteilung Sedimentologie / Umweltgeologie, Geowissenschaftliches 13 Zentrum Göttingen, Universität Göttingen, Goldschmidtstraße 3, 37077 14 Göttingen, Germany 15 cSchool of Geography, Geology and the Environment, Keele University, 16 Keele, Staffordshire, ST5 5BG, UK 17 dDepartment of Geology, University of Gondar, P.O. Box 196, Gondar, 18 Ethiopia 19 eInstitut für Angewandte Geowissenschaften, Fachgebiet 20 Explorationsgeologie, Technische Universität Berlin, Ackerstraße 76, 13355 21 Berlin, Germany 22 23 *corresponding author. Tel. +49 6151 1620634 24 E-mail address: [email protected] (A. Lewin). 25 26 27 Abstract 28 29 We compare Ethiopian glaciogenic sandstone of the Late Ordovician 30 and Carboniferous–Permian Gondwana glaciations petrographically 31 and geochemically to provide insight into provenance, transport, and 32 weathering characteristics. Although several studies deal with the 33 glacial deposits in northern Africa and Arabia, the distribution of ice 34 sheets and continent-wide glacier dynamics during the two 35 glaciations remain unclear. Provenance data on Ethiopian Palaeozoic 36 sedimentary rocks are scarce. The sandstones of the Late Ordovician 37 glaciation are highly mature with an average quartz content of 95% 1 38 and an average chemical index of alteration of 85, pointing to intense 39 weathering and reworking prior to deposition. -
The Politics of the Nile Basin
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Wits Institutional Repository on DSPACE THE POLITICS OF THE NILE BASIN ELIAS ASHEBIR Supervisor:- Larry Benjamin A Dissertation Submitted to the Department of International Relations, at the University of the WitWatersRand, in Partial Fulfillment of the Requirements for Obtaining the Degree of Master of Arts in Hydropotitics Studies Johannesburg 2009 DECLARATION I hereby declare that this dissertation is my own unaided and has not been submitted to any other University for any other degree. Elias Ashebir May 2009 2 TABLE OF CONTENTS Acknowledgment.............................. VI Abstract ................................... VII Introduction................................ VIII Chapter I A Brief Survey of the Nile Basin 1. General overview 1-3 2. Exploration of the Nile 3. Geographical & Hydrological Feature of the Nile Basin 3-4 3.1 The Blue Nile 4 3.2 The White Nile 4-9 Chapter II The Nile Riparian Countries & Future Challenges 1. Subsystems of the Nile Basin 10 1.1 The White Nile Subsystem 11 1.2 The Abbay (Blue Nile) Subsystem 11-12 1.3 The Tekeze (Atbara) Subsystem 12 1.4 The Baro-Akobo (Sobat) Subsystem 12-13 2. General Descriptions of the Nile Riparian Countries 2.1 Upper Riparian Countries of the Nile Basin a) Ethiopia 14-24 b) Eritrea 24-26 c) Kenya 27-32 2.2 The Equatorial upper riparian countries a) Tanzania 32-37 b) Uganda 37-41 c) Democratic Republic of Congo 42-46 3 d) Rwanda 47-50 e) Burundi 50-53 2.3 The Lower riparian countries a) Egypt 53-57 b) Sudan 57-62 Chapter III Legal aspects of the use of the Nile waters 1. -
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. -
Case Study: Friends of Lake Turkana
Case Study: Friends of Lake Turkana Read the passage below. Ikal Angelei, 2012 winner of the prestigious Goldman Environmental Prize, works in the remote Lake Turkana region of Kenya and Ethiopia. Friends of Lake Turkana, a nonprofit organization she founded in 2007, works to stop construction of Ethiopia’s Gilgel Gibe III Dam on the Omo River. The Omo is the major tributary to Lake Turkana, and a dam upstream would drastically impact the lake environment. Changes to the lake’s chemistry and shoreline would devastate the ecology of the region, as well as the local economies that have developed around it, such as fishing, agriculture, and pastoralism. Angelei remembers being shocked on learning of the dam’s likely impact. “At first, I thought, it can’t be real,” she told the New York Times. “I couldn’t imagine the area without the lake.” Geography Located in northern Kenya, the Lake Turkana Basin is a 70,000-square-kilometer (27,027-square- mile) region that is home to Lake Turkana, the most saline lake in East Africa and the largest desert lake in the world. The area includes three national parks: Sibiloi National Park, South Island National Park, and Central Island National Park. Lake Turkana, nicknamed the “Jade Sea” due to its striking color, is a major stopover for migrating waterfowl. The surrounding area is a major breeding ground for Nile crocodiles, hippopotamuses, and a range of venomous snakes. The basin surrounding Lake Turkana is arid and receives little rainfall outside the “long rain” season of March, April, and May. -
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. -
New Thinking, New Technology, New Hydrocarbons
PES GB New Thinking, New Technology, 16th New Hydrocarbons AFR CAN JOIN US AT THE BUSINESS DESIGN CENTRE, LONDON ON 31 AUGUST - 1 SEPTEMBER 2017 This annual event, alternating between London and Houston, has established itself as the premier event for technical discussions and networking on exploration and geosciences in Africa. The 2015 London conference was the largest event to date with 624 delegates in attendance including operators, consultants, governments and academia. There were 34 technical papers presented in a high quality oral programme, 30 poster presentations, complemented by a bustling show floor with 61 exhibitors. Early Bird Registration closing soon at pesgb.org.uk Member Early Bird £330 / Standard from 1 July £420 Non Member Early Bird £390 / Standard from 1 July £480 There will be a limited number of discounted places for those who have been made unemployed. Please contact [email protected] to apply EVENING LECTURE: AFRICA SPECIAL Tuesday 29 August 2017, The Geological Society of London “Gondwana re-assembled: Challenges for making the new map and insights for exploration” With Colin Reeves, Earthworks FREE but registration required at www.pesgb.org.uk- open to PESGB members and African E&P Conference delegates PESGB June 2017 21 THURSDAY 31 AUGUST 2017 08.30 REGISTRATION & COFFEE 09.20 WELCOME & INTRODUCTION SESSION 1: NEW INSIGHTS INTO YOUNG RIFTS ORAL Session Chairs: Jerry Jarvis 09.30 KEYNOTE: Contrasting fault and rift basin evolution in the East Africa Rift: Role of magmatism and magmatic volatile release James