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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. -
(Smes) in Gilgil Town of Nakuru County, Kenya
IOSR Journal Of Humanities And Social Science (IOSR-JHSS) Volume 20, Issue 8, Ver. IV (Aug 2015), PP 109-115 e-ISSN: 2279-0837, p-ISSN: 2279-0845. www.iosrjournals.org Socio-Economic Determinants of Performance of Small and Medium Enterprises (SMEs) in Gilgil Town of Nakuru County, Kenya Kamau John Gathii1, and Mathew Mwangi Ngura2, Abstract: This study sought to establish the socio-economic determiners of performance of SMEs in Gilgil town of Nakuru County, Kenya. It adopted a survey research design involving SMEs in Gilgil town. Questionnaires were used as research instruments to gather information on variables of interest. The target population of the study included the 400 SMEs in Gilgil town registered with the County Council of Nakuru in the year 2012 and thereafter a sample size of 196 (49%) SMEs owners were systematically selected as respondents for the study. Data collected was coded and analyzed with the aid of Statistical Package for Social Sciences (SPSS) computer programme. Quantitative data was analyzed using descriptive statistics such as percentages and frequencies while the qualitative data derived from open-ended questions was analyzed according to themes based on the study objectives and research questions and there after inferences and conclusions were drawn. The study revealed that very few SMEs owners had obtained management training; most of them had only obtained secondary education; SMEs lacked access to financial resources and very few had integrated technology in their business operation. These shortcomings have adversely affected the performance of the SMEs in Gilgil town going by the low profits that they are making. -
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! -
Case Study Report For
Case Study One Indigenous Peoples’ Rights in the Kenya Lake System in the Great Rift Valley 1 By DR. KANYINKE SENA Indigenous Peoples’ Rights in the Kenya Lake System in the Great Rift Valley 1 CASE STUDY ONE Indigenous Peoples’ Rights in the Kenya World Heritage (IIPFWH), as a standing global Lake System in the Great Rift Valley body aimed at representing indigenous peo- ples voices in the World Heritage Committee processes.5 The Committee referred to the establishment of the IIPFWH, “As an impor- tant reflection platform on the involvement of Indigenous Peoples in the identification, conservation and management of World Heritage properties, with a particular focus on the nomination process.” 6 Pursuant to the mandate of the Forum, this report aims at analyzing Indigenous Peoples’ involvement in the Kenya Lakes System in the Great Rift Valley World Heritage Site. The report is as result of extensive literature re- view and interviews with communities in and around the lakes that comprise the Kenya K. Sena: Lake Bogoria Lakes System. The Kenya Lake System in the Great Rift Val- ley is a World Heritage site in Kenya which comprises three inter-linked, relatively shal- low, alkaline lakes and their surrounding territories. The lakes system includes Lakes Elementeita, Nakuru and Bogoria in the Rift Valley. The lakes cover a total area of 32,034 and was inscribed as a world heritage site in 2011. The inscription was based on the lakes system outstanding universal values and criterion (vii), (ix) and (x) as provided for, under paragraph 77 of the Operational Guidelines for the Implementation of the World Heritage Convention. -
View (State Party of Kenya, 2020)
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org Kenya Lake System in the Great Rift Valley - 2020 Conservation Outlook Assessment Kenya Lake System in the Great Rift Valley 2020 Conservation Outlook Assessment SITE INFORMATION Country: Kenya Inscribed in: 2011 Criteria: (vii) (ix) (x) The Kenya Lake System in the Great Rift Valley , a natural property of outstanding beauty, comprises three inter-linked relatively shallow lakes (Lake Bogoria, Lake Nakuru and Lake Elementaita) in the Rift Valley Province of Kenya and covers a total area of 32,034 hectares. The property is home to 13 globally threatened bird species and some of the highest bird diversities in the world. It is the single most important foraging site for the lesser flamingo anywhere, and a major nesting and breeding ground for great white pelicans. The property features sizeable mammal populations, including black rhino, Rothschild's giraffe, greater kudu, lion, cheetah and wild dogs and is valuable for the study of ecological processes of major importance. © UNESCO SUMMARY 2020 Conservation Outlook Finalised on 01 Dec 2020 SIGNIFICANT CONCERN The three lakes which make up the Kenya Lake System World Heritage site are subject to pronounced and unpredictable fluctuations in rainfall, water levels and alkalinity – factors which determine the movements of flamingoes and other birds between these lakes, and others beyond. Waterbird counts over the past 20 years suggest that bird populations are stable, but their distribution has changed, with uncertainties over the future of the lakes as the catchment areas come under progressively more intensive land use, with the loss of wetlands through livestock grazing, with increasingly large volumes of water abstracted upstream for agriculture, whilst floods are becoming more severe, with the associated sediments carried into and accumulating within the lakes. -
Omenda Geothermal Heat Sources in East Africa Rift System 2016
Heat Sources for Geothermal Systems in East African Rift System Peter Omenda Classification by Temperature Volcano hosted Geothermal Systems • Typical model for volcano hosted geothermal system Volcano hosted Geothermal Systems-Menengai • Associated with main rift volcanoes Menengai Geothermal field • Temperatures of > 400oC measured • Shallow magma bodies ~2.3km Geophysical Model across Menengai • Seismics show high velocity under volcano • Common feature of all volcanoes in EARS rift axis MEQ Studies T o B MN15 a Marigat MN13 r in g Coffee o Farm MN12 Bahati ru Majani Mingi ru hu ya 9985000 N To MN14 • Studies revealed that 9980000 Kabarak s s s MN09 Bahati g g g brittle ductile transition MN10 n n n i i i CALDERA Settlement h h h t t t r r r o o o MN11 N N N MN07 To d d d i i i E r r r l MN08 do G G G re zone under Menengai is 9975000 t MN06 Residential Area MN04 at 6km depth T o Nairobi 9970000 NAKURU MN05 MN03URBAN AREA Lake Rongai Nakuru Lake Nakuru Farms National Park MN02 MN01 165000 170000 175000 180000 Grid Eastings (m) NorthWest Ol Rongai Men. Caldera SouthEast 0 -2 ) ) m m K K ( ( h h t t -4 p p e e D D -6 -8 165000 167500 170000 172500 175000 177500 180000 Distance (M) Menengai Stratigraphy • Stratigraphy dominated by trachytes and pyroclastics • Magma body at ~2.3km • Syenitic cap present • Tmax 400oC Menengai stratigraphic Model Tuff layers Trachyte Syenite Magma Menengai Model 200 isotherm 250 isotherm 350 isotherm Magma Olkaria Volcanic Complex • The heat source at Olkaria is associated with – discrete magma chambers that underlie the volcanic centres Main Ethiopian Rift Recent volcano tectonic activity is mainly within the axis. -
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). -
Classic Kenya Safari Saint Louis Zoo Travel’S Most Popular Adventure Is Back in 2011 with Some Exciting Changes and Additions
Classic Kenya Safari Saint Louis Zoo Travel’s most popular adventure is back in 2011 with some exciting changes and additions. Join us for an unforgettable adventure into the ITINERARY heart of Africa. You can expect to see more than 35 types of mammals, enjoy the comfort of world- Classic Kenya Safari renowned lodges and luxury tented camps, and June 5 - 17, 2011 $4,190 per person, double occupancy, experience the beauty of East Africa’s plains. land only. $4,890 per person single occupancy, land only. This trip is a great first-time Lake Nakuru where you can expect to African wildlife safari with visits to see thousands of flamingos and other Airfare is estimated at $2,100. outstanding national parks and water birds, the white rhino, and the reserves. There’s no place on Earth Rothschild’s giraffe. Then spend three > Sunday, June 5 like East Africa for unrivalled wildlife days in the beautiful Masai Mara St. Louis-London viewing, including the chance to see Game Reserve where you should > Monday, June 6 elephants, hippos, cheetahs, giraffes, see lions, elephants, black rhinos London-Nairobi, Kenya rhinos, zebras, lions and much, much and hippos, plus many fine birds. > Tuesday, June 7 more. We visit a number of very special Nairobi to Sweetwaters Private Reserve places during this two-week adventure. We hope that you will join us on this once-in-a-lifetime trip! > Wednesday, June 8 We’ll drive to Sweetwaters Tented Sweetwaters to Samburu National Reserve Camp to see a variety of wildlife Trip Activity Level: This is a very easy including northern species like the trip. -
HIGH FLUORIDE WATER in the GILGIL AREA of NAKURU COUNTY, KENYA Enos W Wambu,A GK Muthakiab Nairobi, Kenya
37 Research report High F water in Nakuru County, Kenya 37 Fluoride 44(1)37–41 Wambu, Muthakia January-March 2011 HIGH FLUORIDE WATER IN THE GILGIL AREA OF NAKURU COUNTY, KENYA Enos W Wambu,a GK Muthakiab Nairobi, Kenya SUMMARY: Fluoride (F) levels were determined in 37 randomly sampled water sources in the Gilgil-Elementaita area and part of the Nakuru municipality in Nakuru County, Kenya using a F ion selective electrode. Lake water had F levels close to 200 ppm. Of the other sources, the highest mean F levels were in piped water (7.69 ppm) and borehole water (6.57 ppm). The level of water F appeared to increase with proximity of the source to the lakes in the region. There was also an apparent increase in the level of F in piped water compared to the original borehole water, which is ascribed to extensive evaporation during treatment and storage of piped water. With one exception, the river water had the lowest mean F concentrations (<0.1 ppm). These results indicate that most of the rivers in this region are relatively low in F and therefore are the safest sources of water for domestic and industrial use. Keywords: Borehole water; Fluoride in water; Gilgil area; Kenya water sources; Lake Elementaita; Nakuru County, Kenya. INTRODUCTION Endemic fluorosis in Kenya has been a public health problem for many years,1 and now there is a heightened public health concern about the fate of fluoride (F) in soil and groundwater sources, particularly in areas associated with the Great Rift Valley and the Central Highlands.2 In addition, rapid population growth3 and changes in rainfall patterns in many parts of Kenya have exacerbated the problem of water scarcity, forcing communities to turn to poor quality water sources for their needs.4 Primary sources of water for rural populations in Kenya are rivers, streams, springs, and wells in well-watered areas and boreholes in arid and semi-arid regions. -
The Estimation of Lake Naivasha Area Changes Using of Hydro-Geospatial Technologies
http://dx.doi.org/10.4314/rj.v1i1S.3D The Estimation of Lake Naivasha Area Changes Using of Hydro-Geospatial Technologies A. Ruhakana Soil and Water Management Research Program Rwanda Agriculture Board, Huye, Rwanda [email protected] Abstract: Remote Sensing (RS) and Geographical Information System (GIS) were proved as new technology to intervene in monitoring, managing and protecting environmental resources among others lake and water reservoir are mostly anxious resources. The objective of the study was to estimate the surface area change of the lake Naivasha using RS, GIS techniques and hydrological modeling for the lake water balance. Landat images Thematic Mapper/Enhanced Thematic Mapper Plus (TM/ETM+) taken respectively in the same month of January 1986; 1995; 2003 and 2010 were the input data used to assess the different changes of the lake area on one hand. on other hand the spread sheet data set helped to build the hydrological model to estimate the long term lake Level fluctuation, the rainfall versus evaporation as in flow and out flow from the lake. The lake volume showed the dynamic of ground water to simulate the long-term fluctuation of the lake level. The lake area changes from the model were calculated from the spread sheet input data from 1986 to 2003 while the lake area changes from the Landsat images were calculated from 1986 to 2010. The comparative results from the area lake changes both from Landsat images and hydrological model confirmed the correlation results, 45.72 Km2 or 32.03 % in 2010 for the Landsat while the hydrological model estimated to 12km2 or 8% area reduction in 2003. -
Nature [October 12, 1929
574 NATURE [OCTOBER 12, 1929 The alkali reserve of Lake N aivasha, expressed in Letters to the Editor. normality, was 0·004 (cf. Cambridge tap water 0·0042 N.), but instead of calcium, as in English hard waters, [The Editor does not hold himself responsible for the base was sodium derived from the surrounding opinions expressed by his correspondents. Neither alkaline lavas. This may have had a specific effect, can he undertake to return, nor to correspond with as in increasing concentrations the alkalinity appeared the writers of, rejected manuscripts intended for this to effect a marked reduction in quantity of both fauna or any other part of NATURE. No notice is taken and flora. The other lakes illustrated this, since their of anonymous communications.] alkalinity increased in the order: L. Baringo (0·01 N.), Crater Lake (0·11 N.), L. Elmenteita (0·22 N.), and L. Biology of Lakes in Kenya. Nakuru (0·27 N.). This increase raised the hydrogen WESENBURG-LUND, Thienemann, and others have ion concentration from pH 9·0 to about pH ll·2. for years been emphasising the need for more detailed Lake Baringo contained Crustacea, Rotifera, insect studies of tropical fresh waters. Having recently larvre, and fish, and also Microcystis sp., but no higher plants were seen. The three others, ' soda ' lakes, contained chiefly Roti fera and insect larvre, Lake Nakuru having apparently only one species of Brachionus. They were further characterised by the presence of a very abundant blue - green alga, Spirulina sp., in the plankton and an entire absence of shore vegetation, which was replaced by foul, barren mud, largely admixed with flamingo excreta.