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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 ..................................................................................... -
Geology, Geochronology, and Rift Basin Development in the Central Sector of the Main Ethiopia Rift
Geology, geochronology, and rift basin development in the central sector of the Main Ethiopia Rift GIDAY WOLDEGABRIEL* ) n „ „, JAMES L ARONSON J DePartment °J Geological Sciences, Case Western Reserve University, Cleveland, Ohio 44106 ROBERT C. WALTER Institute of Human Origins, 2453 Ridge Road, Berkeley, California 94709 ABSTRACT 37°30'-40°. A satellite thematic mapper image of this classic rift region (Fig. 1) shows all but the southwestern part of the study area. The MER is Based on stratigraphic relationships and K/Ar dating of volcanic divided geographically into three sectors: northern, central, and southern rocks from both of the escarpments, flanking plateaus, and from the (inset map, Fig. 2), and most of the central sector of the rift proper is in this rift floor of the central sector of the Main Ethiopian Rift, six major image. The MER divides the 1,000-km-wide uplifted Ethiopian volcanic volcanic episodes are recognized in the rift's development over a time province asymmetrically into the northwest and southeast plateaus (inset span from the late Oligocene to the Quaternary. Using the K/Ar data, map, Fig. 2). Volcanic sequences that cover an area several hundred correlation of volcanic units from the six periods of activity through- kilometers across are more voluminous and widespread on the northwest out the study area forms the basis for establishing six time- plateau than on the opposite side. Contrary to previous suggestions that stratigraphic chronozones for the central sector that are related to volcanism migrated from the northwest plateau toward the Ethiopian Rifts volcanism in the Ethiopian Cenozoic volcanic province. -
Geological Evolution of the Red Sea: Historical Background, Review and Synthesis
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/277310102 Geological Evolution of the Red Sea: Historical Background, Review and Synthesis Chapter · January 2015 DOI: 10.1007/978-3-662-45201-1_3 CITATIONS READS 6 911 1 author: William Bosworth Apache Egypt Companies 70 PUBLICATIONS 2,954 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Near and Middle East and Eastern Africa: Tectonics, geodynamics, satellite gravimetry, magnetic (airborne and satellite), paleomagnetic reconstructions, thermics, seismics, seismology, 3D gravity- magnetic field modeling, GPS, different transformations and filtering, advanced integrated examination. View project Neotectonics of the Red Sea rift system View project All content following this page was uploaded by William Bosworth on 28 May 2015. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Geological Evolution of the Red Sea: Historical Background, Review, and Synthesis William Bosworth Abstract The Red Sea is part of an extensive rift system that includes from south to north the oceanic Sheba Ridge, the Gulf of Aden, the Afar region, the Red Sea, the Gulf of Aqaba, the Gulf of Suez, and the Cairo basalt province. Historical interest in this area has stemmed from many causes with diverse objectives, but it is best known as a potential model for how continental lithosphere first ruptures and then evolves to oceanic spreading, a key segment of the Wilson cycle and plate tectonics. -
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 Cretaceous Geology of the East Texas Basin Ronald D
Thesis Abstracts thinking is more important than elaborate FRANK CARNEY, PH.D. PROFESSOR OF GEOLOGY BAYLOR UNIVERSITY 1929-1934 Objectives of Geological Training at Baylor The training of a geologist in a university covers but a few years; his education continues throughout his active life. The purposes of train ing geologists at Baylor University are to provide a sound basis of understanding and to foster a truly geological point of view, both of which are essential for continued professional growth. The staff considers geology to be unique among sciences since it is primarily a field science. All geologic research in cluding that done in laboratories must be firmly supported by field observations. The student is encouraged to develop an inquiring ob jective attitude and to examine critically all geological concepts and principles. The development of a mature and professional attitude toward geology and geological research is a principal concern of the department. Cover: Trinity Group isopach map illustrating depositional trends of Trinity rocks. (From French) THE BAYLOR PRINTING SERVICE WACO, TEXAS BAYLOR GEOLOGICAL STUDIES BULLETIN NO. 52 THESIS ABSTRACTS These abstracts are taken from theses written in partial fulfillment of degree requirements at Baylor University. The original, unpublished versions of the theses, complete with appendices and bibliographies, can be found in the Ferdinand Roemer Library, Department of Geology, Baylor University, Waco, Texas. BAYLOR UNIVERSITY Department of Geology Waco, Texas Fall Baylor Geological Studies EDITORIAL STAFF Janet L. Burton, Editor O. T. Hayward, Ph.D., Advisor, Cartographic Editor Stephen I. Dworkin, Ph.D. general and urban geology and what have you geochemistry, diagenesis, and sedimentary petrology Joe C. -
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. -
Hewn Churches and Its Surroundings, Tigray Region, Northern Ethiopia
Research Article http://dx.doi.org/10.4314/mejs.v9i2.4 Geological and Geomechanical Properties of Abraha-Atsibha and Wukro rock- hewn churches and its surroundings, Tigray Region, Northern Ethiopia Asmelash Abay*, Gebreslassie Mebrahtu and Bheemalingeswara Konka School of Earth Sciences, Mekelle University, P.O.Box:231, Mekelle, Ethiopia (*[email protected]). ABSTRACT Globally well-known ancient rock-hewn churches are present in Ethiopia in general and particularly in the central and eastern parts of Tigray regional state. They are important sites of heritage and tourism. Most of them are facing destabilization problem in different degree due to natural and anthropogenic factors. Among the affected, two churches hewn into sandstone located near Abreha-Atsibaha and Wukro (Kirkos/Cherkos church) in Tigray region were chosen for detailed study in terms of geological and engineering geological condition of the rocks in to which they are hewn. Both of them are affected by weathering and seepage. Both are carved into Mesozoic Adigrat sandstone that occupy higher elevations in topography, red in color and with iron and silica-rich alternating bands. Petrographic data suggest that the rock is dominated by quartz followed by feldspars; opaque and heavy minerals; pore spaces and carbonate/iron/silica cement. The rock is characterized by low to medium unconfined compressive strength. The alternating bands with varying mineralogical composition differ in mechanical properties and are responding differently to weathering and erosion. This is resulting in the development of minor spalling, pitting etc in the pillars, walls and roofs of the churches. Keeping the geological condition in view remedial measures are to be planned to minimize deterioration with time. -
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. -
Geology and Petroleum Resources of Central and East-Central Africa by James A. Peterson* Open-File Report 85-589 This Report Is
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geology and petroleum resources of central and east-central Africa By James A. Peterson* Open-File Report 85-589 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature Missoula, Montana 1985 CONTENTS Page Abs tract 1 Introduction 2 Sources of Information 2 Geography 2 Acknowledgment s 2 Regional geology 5 Structure 5 Horn of Africa 5 Plateau and rift belt 11 Red Sea and Gulf of Aden Basins 13 Central Africa interior basins 13 Upper Nile Basin (Sudan trough) 13 Chad, Doba-Doseo (Chari), and lullemmeden (Niger) Basins 13 Benue trough 15 Stratigraphy 15 Precambrian 19 Paleozoic 19 Mesozoic 21 East-central Africa 21 Jurassic 21 Cretaceous 22 Tertiary 22 Central Africa interior basins 26 Benue trough 27 Petroleum geology 27 Somali basin 28 Res ervo i r s 2 9 Source rocks 29 Seals 29 Traps 2 9 Estimated resources 30 Plateau and rift belt 30 Red Sea Basin (western half) 30 Reservoirs 30 Source rocks 34 Seals 34 Traps 34 Estimated resources 34 Central Africa interior basins 34 Reservoirs, source rocks, seals 36 Traps 36 Estimated resources 36 Benue trough 40 Res er voi r s 4 0 Source rocks 40 Seals 40 Traps 40 Estimated resources 40 CONTENTS (continued) Page Resource assessment 42 Procedures 42 As s es smen t 4 3 Comments 43 Selected references 45 ILLUSTRATIONS Figure 1. Index map of north and central Africa 3 2. Generalized structural map of central and east Africa 4 3. -
Chapter2: Geological Review
Chapter2: Geological Review Chapter 2 Geological Review 2.1. Introduction: In Sudan, five NW-SE trending continental rifts are known. They define together an extensional province, which has a wide of 1000 km and a length of at least 800 km parallel to the strike direction (Figure 2.1) (Fairhead, 1988). From North to South, these rifts are referred to as: The Atbara rift. The Blue Nile Rift (Khartoum and Khartoum South). The White Nile Rift (Melut or Bara and Kosti). The Muglad-Abu Gabra Rift (the Muglad-Abu Gabra and Bahr el Arab rifts are collectively referred to as the Southern Sudan rift). The Muglad is the best known and is the largest of the Sudan rift basins. The Bagarra Basin. Figure(2.1): shows the tectonic model of the West and Central African Rift System (Fairhead,1988). 6 Chapter2: Geological Review In the northwest, the Sudan rift basins terminate along the transcurrent fault zone in continental scale, the Central African Shear Zone (Figure 2.1). The Central African Shear Zone is envisioned to link the Sudan rift basins with the Lower and Upper Cretaceous rift basins in Chad and Niger (Fairhead,1988). The south-eastern terminations of the Sudan rifts are more complex (Schull 1988). 2.2. Muglad Basin: The Muglad basin is rift basin of Meso-cenozoic, which caused by the shear zone of middle-Africa and developed on the firm basement of Precambrian(Vail, 1978; Whiteman, 1971). There are three superimposed rift formations of different periods in Muglad area since Early Cretaceous(Fairhead, 1988). The first one is Abu Gabra Fm - Bentiu Fm of Lower Cretaceous, the second one is the Darfour group of Upper Cretaceous–Paleocene of Paleogene, and the third is Eocene of paleogene– Neogene. -
U.S. Geological Survey Open-File Report 82-788 This Report Is Preliminary and Has Not Been Reviewed for Conformity with U.S
SO-2 HUT1D STATES OF THE HCTOLIO* GEOLOGICAL SURVEY PROJECT REPORT Somalia Investigation (IR)SO-2 A PRELIMINARY EVALUATION OF THE NON-FUEL MINERAL POTENTIAL OF SOMALIA By William Rucker Greenwood U.S. Geological Survey U.S. Geological Survey Open-File Report 82-788 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratlgraphic nomenclature. (Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS.) TOR? CONTENTS Page Abstract................................................................. 1 Introduction............................................................. 2 Summary of Geology....................................................... 3 PreCambrian......................................................... 3 Bur Region..................................................... 3 Northern Mountains............................................. 4 Gneissic complex.......................................... 4 Inda Ad Series............................................ 5 Mafic igneous rocks....................................... 5 Granite................................................... 5 Structure................................................. 5 Metamorphism.............................................. 6 Phanerozoic......................................................... 6 Jurassic rocks................................................. 6 Borama-Zeila area......................................... 6 Bihendula area...........................................