Technical Report KMF/RS/2018/C 1.7 31ST MARCH 2018
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Tectonic and Climatic Control on Evolution of Rift Lakes in the Central Kenya Rift, East Africa
Quaternary Science Reviews 28 (2009) 2804–2816 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Tectonic and climatic control on evolution of rift lakes in the Central Kenya Rift, East Africa A.G.N. Bergner a,*, M.R. Strecker a, M.H. Trauth a, A. Deino b, F. Gasse c, P. Blisniuk d,M.Du¨ hnforth e a Institut fu¨r Geowissenschaften, Universita¨t Potsdam, K.-Liebknecht-Sr. 24-25, 14476 Potsdam, Germany b Berkeley Geochronology Center, Berkeley, USA c Centre Europe´en de Recherche et d’Enseignement de Ge´osciences de l’Environement (CEREGE), Aix en Provence, France d School of Earth Sciences, Stanford University, Stanford, USA e Institute of Arctic and Alpine Research, University of Colorado, Boulder, USA article info abstract Article history: The long-term histories of the neighboring Nakuru–Elmenteita and Naivasha lake basins in the Central Received 29 June 2007 Kenya Rift illustrate the relative importance of tectonic versus climatic effects on rift-lake evolution and Received in revised form the formation of disparate sedimentary environments. Although modern climate conditions in the 26 June 2009 Central Kenya Rift are very similar for these basins, hydrology and hydrochemistry of present-day lakes Accepted 9 July 2009 Nakuru, Elmenteita and Naivasha contrast dramatically due to tectonically controlled differences in basin geometries, catchment size, and fluvial processes. In this study, we use eighteen 14Cand40Ar/39Ar dated fluvio-lacustrine sedimentary sections to unravel the spatiotemporal evolution of the lake basins in response to tectonic and climatic influences. We reconstruct paleoclimatic and ecological trends recor- ded in these basins based on fossil diatom assemblages and geologic field mapping. -
Hydrologic Analysis of Malewa Watershed
HYDROLOGIC ANALYSIS OF MALEWA WATERSHED AS A BASIS FOR IMPLEMENTING PAYMENT FOR ENVIRONMENTAL SERVICES (PES) PHILIP LUKE OGWENO MASTER OF SCIENCE (Soil and Water Engineering) JOMOKENYATTA UNIVERSITY OF AGRICULTURE AND TECHNOLOGY 2009 Hydrologic Analysis of Malewa Watershed as a basis for Implementing Payment for Environmental Services (PES) Ogweno Luke Philip A thesis submitted in partial fulfilment for the Degree of Masters of Science in Soil and Water Engineering in the Jomo Kenyatta University of Agriculture and Technology. 2009 ii DECLARATION This thesis is my original work and has not been presented for a degree in any other University Signature ………………….. Date…………...... Ogweno Luke Philip This thesis has been submitted for examination with our approval university supervisors 1. Signature …………… Date…….……… Dr J. M. Gathenya JKUAT, KENYA 2. Signature…………….. Date………………… Dr. P.G. Home JKUAT, KENYA i DEDICATION This work is dedicated to my late father John Alfred Ondulo Aduda for his inspiration and mentorship. The discipline towards work that you instilled in me will live and I will propagate your legacy for the rest of my life, rest in peace. It is also dedicated to all who are struggling to conserve and preserve the environment for the future progeny, to my family members and Cecilia Anyango. ii ACKNOWLEDGEMENT The success of this project owes much to the constant and helpful supervision given by Dr. J.M. Gathenya and Dr. P.G. Home, senior lecturers at the Department of Biomechanical and Environmental Engineering, Jomo Kenyatta University. Their guidance in getting research materials/project and encouragement throughout the course contributed constructively towards the success of this project. -
Orpower 4 Inc Environmental Impact Assessment Olkaria Iii Geothermal
0 ORPOWER 4 INC Public Disclosure Authorized ENVIRONMENTAL IMPACT ASSESSMENT OLKARIA III GEOTHERMAL POWER PLANT Public Disclosure Authorized Public Disclosure Authorized Prepared by Prof. Mwakio P. Tole and Colleagues School of Environmental Studies Moi University Public Disclosure Authorized P. O. Box 3900 Eldoret, KENYA August, 2000 1 TABLE OF CONTENTS Content Page Number 0.0 Executive Summary 5 1.0 Introduction 25 2.0 Policy, Legal and Administrative Framework 26 3.0 Description of the Proposed Project 28 4.0 Baseline Data 39 5.0 Significant Environmental Impacts 83 6.0 Assessment of Alternatives 100 6.0 Mitigation Measures 105 7.0 Conclusions and Recommendations 114 8.0 Bibliography 115 9.0 Appendices 122 2 LIST OF TABLES Table No. Title Page No. Table 1 Noise levels at selected areas around Olkaria West 47 Table 2 Effects of CO2 on Human Health 50 Table 3 Effects of H2S on Human Health 52 Table 4 H2S concentration Frequencies around the Olkaria I field 55 Table 5 Mean Concentrations of Brine in Olkaria Field 60 Table 6 Permissible levels of some heavy metals in drinking water 60 Table 7 Biological impacts of selected metals on human health 61 Table 8. Radiation Exposure Sources in Britain 63 Table 9 Chemical composition of Lake Naivasha waters 65 Table 10 Mammal Census at the Hell’s Gate National Park 72 Table 11 Traffic on Olkaria West–KWS road 84 Table 12 Expected releases of Non-condensable gases into the atmosphere 88 Table 13 Concentrations of H2S in wells at Olkaria III 90 3 LIST OF FIGURES Figure No. -
Wildlife Safari in Kenya September 1-15, 2023
Wildlife Safari in Kenya September 1-15, 2023 (Pre-Trip Extension #1: Victoria Falls/Botswana Aug 22-31) (Pre-Trip Extension #2: Cape Town Adventure Aug 18-22) 15 Nights – 2 Full Weeks on Safari During the Migration Season! Accommodations in some of the Premier Tent Camps & Lodges Kenya has to offer! Samburu and Mara Reserves + Lake Elementeita Daily Game Drives and Other Activities Animals, Animals, Animals, as well as Local Culture and Color Transportation provided in your own, dedicated, 4-person Toyota Land Cruiser driven by some of the best guides in Kenya! Visit to the world-famous Daphne Sheldrick Elephant Orphanage Plus a visit to Hope Streams Academy, an inspiring success story for one of Nairobi’s largest slums DAY -2 - WED AUG 30 OPTIONAL: Those traveling from the West Coast may wish to spend the night near JFK. For those interested in doing this, I will make reservations for the group. DAY -1 - THUR AUG 31 Board your flight from the States (if not doing Vic Falls/Botswana pre-trip) and begin your journey to Nairobi. DAY 1 - FRI SEP 1 NAIROBI Today we arrive in Nairobi, are met by our host representative and transferred to our hotel. We will meet this evening for a Welcome Reception. Accommodation: Karen Blixen Coffee Garden and Cottages DAY 2 NAIROBI After breakfast we head out for a day of activities in and around Nairobi. The morning will be spent visiting the Karen Blixen Museum followed by a moving visit to Hope Streams Academy. We will then visit Utamaduni, the famous arts and crafts emporium before heading back to Karen Blixen Cottages for lunch. -
Analysis and Mapping of Water-Related Conflicts in the Catchment of Lake Naivasha (Kenya)
Competition over water resources: analysis and mapping of water-related conflicts in the catchment of Lake Naivasha (Kenya) Carolina Boix Fayos February 2002 Competition over water resources: analysis and mapping of water-related conflicts in the catchment of Lake Naivasha (Kenya) By Carolina Boix Fayos Supervisors: Dr. M.McCall (Social Sciences) Drs. J. Verplanke (Social Sciences) Drs. R. Becht (Water Resources) Thesis submitted to the International Institute for Geoinformation Science and Earth Observation in partial fulfilment of the requirements for the degree of Master of Science in Water Resources and Environmental Management Degree Assessment Board Chairman: Prof. Dr. A.M.J. Meijerink (Water Resources) External examiner: Prof. A. van der Veen (University of Twente) Members: Dr. M.K. McCall (Social Sciences) Drs. J.J. Verplanke (Social Sciences) Drs. R. Becht (Water Resources) INTERNATIONAL INSTITUTE FOR GEOINFORMATION SCIENCE AND EARTH OBSERVATION ENSCHEDE, THE NETHERLANDS Disclaimer This document describes work undertaken as part of a programme of study at the International Institute for Geoinformation Science and Earth Observation. All views and opinions expressed therein remain the sole responsibility of the author, and do not necessarily represent those of the institute. A mi abuelo Paco (Francisco Fayos Artés) que me enseñó a apreciar la tierra y sus gentes y a disfrutar con la Geografía y la Historia ACKNOWLEDGEMENT The experience of ITC has been very special. I am very grateful to the Fundación Alfonso Martín Escudero (Madrid, Spain) who paid the ITC fees and supported me economically during the whole period. I am also very grateful to my supervisors Dr. Mike McCall, Drs. -
Kenyan Stone Age: the Louis Leakey Collection
World Archaeology at the Pitt Rivers Museum: A Characterization edited by Dan Hicks and Alice Stevenson, Archaeopress 2013, pages 35-21 3 Kenyan Stone Age: the Louis Leakey Collection Ceri Shipton Access 3.1 Introduction Louis Seymour Bazett Leakey is considered to be the founding father of palaeoanthropology, and his donation of some 6,747 artefacts from several Kenyan sites to the Pitt Rivers Museum (PRM) make his one of the largest collections in the Museum. Leakey was passionate aboutopen human evolution and Africa, and was able to prove that the deep roots of human ancestry lay in his native east Africa. At Olduvai Gorge, Tanzania he excavated an extraordinary sequence of Pleistocene human evolution, discovering several hominin species and naming the earliest known human culture: the Oldowan. At Olorgesailie, Kenya, he excavated an Acheulean site that is still influential in our understanding of Lower Pleistocene human behaviour. On Rusinga Island in Lake Victoria, Kenya he found the Miocene ape ancestor Proconsul. He obtained funding to establish three of the most influential primatologists in their field, dubbed Leakey’s ‘ape women’; Jane Goodall, Dian Fossey and Birute Galdikas, who pioneered the study of chimpanzee, gorilla and orangutan behaviour respectively. His second wife Mary Leakey, whom he first hired as an artefact illustrator, went on to be a great researcher in her own right, surpassing Louis’ work with her own excavations at Olduvai Gorge. Mary and Louis’ son Richard followed his parents’ career path initially, discovering many of the most important hominin fossils including KNM WT 15000 (the Nariokotome boy, a near complete Homo ergaster skeleton), KNM WT 17000 (the type specimen for Paranthropus aethiopicus), and KNM ER 1470 (the type specimen for Homo rudolfensis with an extremely well preserved Archaeopressendocranium). -
Geology Natvasha Area
Report No. 55 GOVERNMENT OF KENYA* MINISTRY OF COMMERCE AND INDUSTRY GEOLOGICAL SURVEY OF KENYA GEOLOGY OF THE NATVASHA AREA EXPLANATION OF DEGREE SHEET 43 S.W. (with coloured geological map) by A. O. THOMPSON M.Sc. and R. G. DODSON M.Sc. Geologists Fifteen Shillings - 1963 Scanned from original by ISRIC - World Soil Information, as ICSU World Data Centre for Soils. The purpose is to make a safe depository for endangered documents and to make the accrued information available for consultation, following Fair Use Guidelines. Every effort is taken to respect Copyright of the materials within the archives where the identification of the Copyright holder is clear and, where feasible, to contact the originators. For questions please contact soil.isric(a>wur.nl indicating the item reference number concerned. ISRIC LIBRARY ü£. 6Va^ [ GEOLOGY Wageningen, The Netherlands | OF THE EXPLANATION OF DEGREE SHEET 43 S.W. (with coloured geological map) by A. O. THOMPSON M.Sc. and R. G. DODSON M.Sc. Geologists FOREWORD Previous to the undertaking of modern geological surveys the Naivasha area, in the south-central part of Kenya Rift Valley, was probably the best known part of the Colony from the geological point of view. This resulted partly from ease of access, as from the earliest days the area was crossed by commonly used routes of com munication, and partly from the presence of lakes, which in Pleistocene times were much larger and made the country an ideal habitat for Prehistoric Man and animals that have left their traces behind them in the beds that were then deposited. -
Simon Mang'erere Onywere
Onywere Summer School 2005 Morphological Structure and the Anthropogenic Dynamics in the Lake Naivasha Drainage Basin and its Implications to Water Flows Simon Mang’erere Onywere Department of Environmental Planning and Management, Kenyatta University P.O. Box 43844 Nairobi 00100, Kenya E-mail: [email protected] Abstract Throughout its length, the Kenyan Rift Valley is characterized by Quaternary volcanoes. At Lake Naivasha drainage basin, the Eburru (2830m) and Olkaria (2434m) volcanic complexes and Kipipiri (3349m), Il Kinangop (3906m) and Longonot (2777m) volcanoes mark the terrain. Remote sensing data and field survey were used to make morphostructural maps and to determine the structural control and the land use impacts on the drainage systems in the basin. Lake Naivasha is located at the southern part of the highest part of Kenya’s Rift Valley floor in a trough marked to the south and north by Quaternary normal faults and extensional fractures striking in a N18°W direction. The structure of the rift floor influences the axial geometry and the surface process. Simiyu and Keller (2001) interpret the rift floor structure as due to thickening related to the pre-rift crustal type and modification by magmatic processes. The rift marginal escarpments of Sattima and Mau form the main watershed areas. From the marginal escarpments the Rift Valley is formed by a series of down-stepped fault scraps. These influence the nature of the soils and the rainfall regime. The drainage is also influenced by the fault trends. At the Malewa fault line for example the drainage is south-easterly influenced by the trend of the Malewa fault line (Thompson and Dodson, 1963). -
Hydrodynamics of Topographically Closed Lakes in the Ethio-Kenyan Rift: the Case of Lakes Awassa and Naivasha," Journal of Spatial Hydrology: Vol
Journal of Spatial Hydrology Volume 7 Number 1 Article 4 2007 Hydrodynamics of topographically closed lakes in the Ethio- Kenyan Rift: The case of lakes Awassa and Naivasha Follow this and additional works at: https://scholarsarchive.byu.edu/josh BYU ScholarsArchive Citation (2007) "Hydrodynamics of topographically closed lakes in the Ethio-Kenyan Rift: The case of lakes Awassa and Naivasha," Journal of Spatial Hydrology: Vol. 7 : No. 1 , Article 4. Available at: https://scholarsarchive.byu.edu/josh/vol7/iss1/4 This Article is brought to you for free and open access by the Journals at BYU ScholarsArchive. It has been accepted for inclusion in Journal of Spatial Hydrology by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Journal of Spatial Hydrology Vol.7, No.1, Spring 2007 Hydrodynamics of topographically closed lakes in the Ethio-Kenyan Rift: The case of lakes Awassa and Naivasha Tenalem Ayenew1*, Robert Becht2, Arno van Lieshout2, Yemane Gebreegziabher3, Dagnachew Legesse1, Japheth Onyando4 Abstract The hydrodynamics and the long-term water balance of two topographically closed crater lakes is presented in a comparative manner using a spread-sheet hydrological model. The main objective of the work is to study the role of groundwater and the effect of water abstraction from lakes Awassa and Naivasha. The rationale of selection of the two lakes separated by thousands of kilometers is the striking similarity of their hydrogeological and geomorphological setting and future intended water uses for large-scale abstraction from the lakes and feeder rivers. The net groundwater outflow from Lake Awassa and the effect of water abstraction from Lake Naivasha under different scenarios were calculated based upon the average monthly hydrometeorological data of rainfall, evaporation and river inflows. -
(Algae and Chironomids) from Kenyan Saline Lakes (Bogoria and Nakuru): Evaluation and Verification of Two Compartment Toxicokinetic Models
BIOACCUMULATION OF TRACE METALS IN BIOTA (ALGAE AND CHIRONOMIDS) FROM KENYAN SALINE LAKES (BOGORIA AND NAKURU): EVALUATION AND VERIFICATION OF TWO COMPARTMENT TOXICOKINETIC MODELS. Von der Fakultät für Mathematik und Naturwissenschaften der Carl von Ossietzky Universität Oldenburg zur Erlangung des Grades und Titels eines Doktors der Naturwissenschaften (Dr. rer. nat.) angenommene Dissertation Von Frau Muohi, Ann Wairimu Geboren am 20th 10 1975 in Thika. ii Gutachterin/Gutachter: Dr. Gerd-Peter Zauke Zweitgutachterin/-gutachter: Prof. Dr. Hans-J Brumsack Tag der Disputation: 11/12/2007 iii BIOACCUMULATION OF TRACE METALS IN BIOTA (ALGAE AND CHIRONOMIDS) FROM KENYAN SALINE LAKES (BOGORIA AND NAKURU): EVALUATION AND VERIFICATION OF TWO COMPARTMENT TOXICOKINETIC MODELS. By ANN WAIRIMU MUOHI B.Ed. hons. Kenyatta University, Kenya. M.Sc. University of Nairobi, Kenya. Supervisors First: Dr. Gerd-Peter Zauke…………………………………… Second: Prof. Dr. Hans-J. Brumsack….....……………….……… Local: Prof. Kenneth M. Mavuti …….………………………… A THESIS SUBMITTED TO THE FACULTY OF MATHEMATICS AND NATURAL SCIENCES, AT THE CARL VON OSSIETZKY UNIVERSITÄT, OLDENBURG, GERMANY, IN FULFILMENT OF THE DEGREE OF DOCTOR OF rer.nat. (NATURAL SCIENCES) ii Acknowledgments This study was first developed with the initiative and under the supervision of the late Prof. Dr. Ekkehard Vareschi. Much tribute is thus paid, in his memory and that of his wife Angelika, who together encountered an accident during a scientific field trip in Momella National Park, Arusha, Tanzania. I am very grateful to The Deutscher Akademischer Austausch Dienst (DAAD) for the full sponsorship of this study. I express my gratitude to The Carl von Ossietzky Universität, Oldenburg (UoO), for granting me the academic registration towards the fulfilment of this study. -
Seeking a Sustainable Future for Lake Naivasha Table of Contents
Prepared by EGASY PStrategy & DevelopmentS REPORT 2011 Shared risk and opportunity in water resources: SEEKING A SUSTAINABLE FUTURE FOR LAKE NAIVASHA TABLE OF CONTENTS Executive Summary 1 1 Introduction 2 2 Physical description 4 3 Economic activity and land use in the Naivasha basin 5 3.1 Population distribution 7 3.2 Export vegetable farming 8 3.3 Vegetable farming for domestic consumption 9 3.4 Cut-flower farming 10 3.5 Geothermal electricity generation 12 3.6 Construction and manufacturing activity 12 3.7 Tourism and residential estates 12 3.8 Trade, services and government 13 3.9 Economic activity in relation to Kenya’s economy 13 4 Hydrology, Water Use and Ecosystem Functioning 15 4.1 Lake and catchment hydrology 16 4.2 Water losses 16 4.3 Water quality conditions and ecosystem functioning 18 5 Water Footprint and the Economic Use of Water 19 6 Institutional Arrangements 21 6.1 Legal, Policy and Institutional Framework in Kenya 21 6.2 Institutional Arrangements and Partnerships in Lake Naivasha 23 6.3 Institutional Opportunities and Challenges 25 7 Understanding Shared Risk for the Naivasha Basin 26 7.1 Bio-physical risk 27 7.2 Socio-political risk 28 7.3 Regulatory risk 29 7.4 Reputational risk 29 7.5 Investment risk 30 7.6 Economic-financial risk 31 8 Possibilities for responding to these risks 32 8.1 Governance 32 8.2 Partnerships 33 8.3 Responsible action and water stewardship 33 Table of Contents WWF Report | Lake Naivasha and Shared Risk and Opportunity EXECUTIVE SUMMARY Lake Naivasha is a freshwater lake in the Kenyan Rift Valley. -
Mainstreaming Ecosystem Services and Biodiversity Into Agricultural Production and Management in East Africa Technical Guidance Document
MAINSTREAMING ECOSYSTEM SERVICES AND BIODIVERSITY INTO AGRICULTURAL PRODUCTION AND MANAGEMENT IN EAST AFRICA TECHNICAL GUIDANCE DOCUMENT BIODIVERSITY & ECOSYSTEM SERVICES IN AGRICULTURAL PRODUCTION SYSTEMS BIODIVERSITY & ECOSYSTEM SERVICES IN AGRICULTURAL PRODUCTION SYSTEMS MAINSTREAMING ECOSYSTEM SERVICES AND BIODIVERSITY INTO AGRICULTURAL PRODUCTION AND MANAGEMENT IN EAST AFRICA Practical issues for consideration in National Biodiversity Strategies and Action Plans to minimize the use of agrochemicals TECHNICAL GUIDANCE DOCUMENT FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS and SECRETARIAT OF THE CONVENTION ON BIOLOGICAL DIVERSITY ROME, 2016 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO), or of CBD concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO, or CBD in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of AOF , or CBD. ISBN 978-92-5-109215-6 (FAO) © FAO, 2016 FAO encourages the use, reproduction and dissemination of material in this information product. Except where otherwise indicated, material may be copied, downloaded and printed for private study, research and teaching purposes, or for use in non-commercial products or services, provided that appropriate acknowledgement of FAO as the source and copyright holder is given and that FAO’s endorsement of users’ views, products or services is not implied in any way.