Vegetational Change and Land Degradation in the Lake Baringo
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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. -
ICMB-VIII Abstract Book
Program and Abstracts for the 8 th International Conference on Marine Bioinvasions (20-22 August 2013, Vancouver, Canada) Cover photography & design: Kimberley Seaward, NIWA Layout: Kimberley Seaward & Graeme Inglis, NIWA 8th International Conference on Marine Bioinvasions Vancouver 2013 8th International Conference on Marine Bioinvasions Dear Conference Participant On behalf of the Scientific Steering Committee (SSC) and our sponsors, we would like to welcome you to Vancouver for the 8th International Conference on Marine Bioinvasions. Vancouver is a culturally diverse metropolitan city serving as the western gateway to Canada. We hope you will spend some time to explore all this city has to offer. We are grateful for all of the efforts of the SSC and the local organizing committee as well as for the generous support of our sponsors: the Biodiversity Research Centre at the University of British Columbia for hosting the event; the Canadian Aquatic Invasive Species Network (CAISN), for providing additional funding by sponsoring one of the plenary presentations; The North Pacific Marine Science Organization (PICES), for providing travel awards to early career scientists; and the National Oceanographic and Atmospheric Administration (NOAA), for donating additional funds. Above all else, we are grateful for your participation and willingness to discuss your ideas, latest research results, and vision. Among the papers, posters, and plenary presentations that comprise the conference, we hope you will find many opportunities for discussion and -
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. -
Biogeochemistry of Kenyan Rift Valley Lake Sediments
Geophysical Research Abstracts Vol. 15, EGU2013-9512, 2013 EGU General Assembly 2013 © Author(s) 2013. CC Attribution 3.0 License. Biogeochemistry of Kenyan Rift Valley Lake Sediments Sina Grewe (1) and Jens Kallmeyer (2) (1) University of Potsdam, Institute of Earth and Environmental Sciences, Geomicrobiology Group, Potsdam, Germany ([email protected]), (2) German Research Centre for Geosciences, Section 4.5 Geomicrobiology, Potsdam, Germany ([email protected]) The numerous lakes in the Kenyan Rift Valley show strong hydrochemical differences due to their varying geologic settings. There are freshwater lakes with a low alkalinity like Lake Naivasha on the one hand and very salt-rich lakes with high pH values like Lake Logipi on the other. It is known that the underlying lake sediments are influenced by the lake chemistry and by the microorganisms in the sediment. The aim of this work is to provide a biogeochemical characterization of the lake sediments and to use these data to identify the mechanisms that control lake chemistry and to reconstruct the biogeochemical evolution of each lake. The examined rift lakes were Lakes Logipi and Eight in the Suguta Valley, Lakes Baringo and Bogoria south of the valley, as well as Lakes Naivasha, Oloiden, and Sonachi on the Kenyan Dome. The porewater was analysed for different ions and hydrogen sulphide. Additionally, alkalinity and salinity of the lake water were determined as well as the cell numbers in the sediment, using fluorescent microscopy. The results of the porewater analysis show that the overall chemistry differs considerably between the lakes. In some lakes, concentrations of fluoride, chloride, sulphate, and/or hydrogen sulphide show strong concentration gradients with depth, whereas in other lakes the concentrations show only minor variations. -
RIFT VALLEY LAKES-LEVEL RISE and FLOOD CHALLENGES Lakes Nakuru, Bogoria, Baringo Onywere, Et Al Kenyatta University [email protected] [email protected]
Understanding the Environment, Promoting Health in Lake Baringo and Bogoria Drainage Basin RIFT VALLEY LAKES-LEVEL RISE AND FLOOD CHALLENGES Lakes Nakuru, Bogoria, Baringo Onywere, et al Kenyatta University [email protected] [email protected] Onywere et al (2013) - KU NACOSTI - Project participants • Prof. Simon M Onywere – Kenyatta University and Team Leader (geospatial mapping and environmental health analysis) • Prof. Chris Shisanya – Kenyatta University (Biodiversity assessment, irrigation agriculture and water quality) • Prof. Joy Obando – Kenyatta University (Community livelihood systems and health) • Dr. Daniel Masiga – ICIPE (Bacteriological analysis) • Mr . Zephania Irura – Division of Diseases Surveillance and Response (DDSR), Ministry of Public Health and Sanitation – (health implications of consumption of contaminated waters) • Dr. Nicholas Mariita – Kengen (geophysical survey and mapping of shallow aquifers) • Mr. Huron Maragia - Mines and Geology (Chemical analysis, geochemistry and geohazards • Mr. Antony Oduya Ndubi - FAO Somalia, SWALIM Project (Image Data analysis) Onywere et al (2013) - KU Unprecedented lakes level rise in the Rift Valley • Are we prepared for the consequences? • Recent events in the rift valley in Kenya and at least since the long rains of 2011 have seen a consistent and increased recharge into all the Rift Valley lakes • This has lead to the lake levels rising to unprecedented levels since 1963 when the event was last observed. • Historical records also indicate a flooded lake environment in -
Wetlands of Kenya
The IUCN Wetlands Programme Wetlands of Kenya Proceedings of a Seminar on Wetlands of Kenya "11 S.A. Crafter , S.G. Njuguna and G.W. Howard Wetlands of Kenya This one TAQ7-31T - 5APQ IUCN- The World Conservation Union Founded in 1948 , IUCN— The World Conservation Union brings together States , government agencies and a diverse range of non - governmental organizations in a unique world partnership : some 650 members in all , spread across 120 countries . As a union , IUCN exists to serve its members — to represent their views on the world stage and to provide them with the concepts , strategies and technical support they need to achieve their goals . Through its six Commissions , IUCN draws together over 5000 expert volunteers in project teams and action groups . A central secretariat coordinates the IUCN Programme and leads initiatives on the conservation and sustainable use of the world's biological diversity and the management of habitats and natural resources , as well as providing a range of services . The Union has helped many countries to prepare National Conservation Strategies , and demonstrates the application of its knowledge through the field projects it supervises . Operations are increasingly decentralized and are carried forward by an expanding network of regional and country offices , located principally in developing countries . IUCN — The World Conservation Union - seeks above all to work with its members to achieve development that is sustainable and that provides a lasting improvement in the quality of life for people all over the world . IUCN Wetlands Programme The IUCN Wetlands Programme coordinates and reinforces activities of the Union concerned with the management of wetland ecosystems . -
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. -
The Effects of Catchment Land Cover Change on Sedimentation in Back Lake, Merimbula, NSW.”
University of Wollongong Research Online Faculty of Science, Medicine & Health - Honours Theses University of Wollongong Thesis Collections 2013 “The Effects of Catchment Land Cover Change on Sedimentation in Back Lake, Merimbula, NSW.” Alison Borrell University of Wollongong Follow this and additional works at: https://ro.uow.edu.au/thsci University of Wollongong Copyright Warning You may print or download ONE copy of this document for the purpose of your own research or study. The University does not authorise you to copy, communicate or otherwise make available electronically to any other person any copyright material contained on this site. You are reminded of the following: This work is copyright. Apart from any use permitted under the Copyright Act 1968, no part of this work may be reproduced by any process, nor may any other exclusive right be exercised, without the permission of the author. Copyright owners are entitled to take legal action against persons who infringe their copyright. A reproduction of material that is protected by copyright may be a copyright infringement. A court may impose penalties and award damages in relation to offences and infringements relating to copyright material. Higher penalties may apply, and higher damages may be awarded, for offences and infringements involving the conversion of material into digital or electronic form. Unless otherwise indicated, the views expressed in this thesis are those of the author and do not necessarily represent the views of the University of Wollongong. Recommended Citation Borrell, Alison, “The Effects of Catchment Land Cover Change on Sedimentation in Back Lake, Merimbula, NSW.”, Bachelor of Environmental Science (Honours), School of Earth & Environmental Science, University of Wollongong, 2013. -
Kenya Nairobi-Samburu Mount Kenya-Lake Nakuru- Lake Naivasha-Masai Mara 8 Days | African Charm
Kenya Nairobi-Samburu mount Kenya-Lake Nakuru- Lake Naivasha-masai mara 8 Days | African Charm DAY 1 Destination: Arrival at Jomo Kenyatta International Airport; Transfer to Nairobi Accommodations: Ololo Safari Lodge Activities: Optional Game Drive Arrival at Jomo Kenyatta International Airport. After clearing customs, you will be met by your expert naturalist guide and transferred to the lovely Ololo Safari Lodge, an elegant, thatched-roof African manor situated right on the edge of the African wilderness, overlooking Nairobi National Park. Just outside of Nairobi’s central business district is Nairobi National Park, Kenya’s first national park established in 1946. This park is iconic for its wide open grass plains and scattered acacia bush with the city of Nairobi’s skyscrapers in the backdrop. Despite its small size and proximity to human civilization, this park plays host to a wide variety of wildlife including lions, leopards, cheetahs, hyenas, buffaloes, giraffes and diverse birdlife with over 400 species recorded. As well, it is home to one of Kenya’s most successful rhino sanctuaries, and you are likely to see the endangered black rhino here. After settling in, you will meet with your guide to briefly go over your safari itinerary. Enjoy a lovely lunch, featuring Ololo’s garden grown produce and eggs. You then have the option of going on a late afternoon game drive into Nairobi National Park or staying at the lodge, perhaps taking a dip in the pool, walking around the beautiful gardens, reading a book by the fire, or enjoying a drink on the terrace overlooking the park. -
Kenyas Geothermal Prospects Outside Olkaria
Mwangi, M.: Geothermal in Kenya and Africa Reports 2005 Number 4, 41-50 GEOTHERMAL TRAINING PROGRAMME LECTURE 4 KENYA’S GEOTHERMAL PROSPECTS OUTSIDE OLKARIA: STATUS OF EXPLORATION AND DEVELOPMENT Godwin M. Mwawongo Kenya Electricity Generating Company Ltd, Olkaria Geothermal Project P.O. Box 785, Naivasha 20117 KENYA [email protected] ABSTRACT Implementation of the geothermal resource assessment program (GRA) has resulted in exploration studies being done in five other prospects in the Kenyan rift between 2004 and 2005. The same studies in all the geothermal prospects north of Lake Baringo will be complete by 2010. So far Menengai is ranked first followed by Longonot and Suswa. For prospects with no central volcano, L Baringo is ranked last after L Bogoria and Arus. Over 6,838 MWt is lost naturally from the already explored geothermal prospects in the rift. Areas of heat leakages in the rift are controlled by NW-SE trending faults. At Olkaria, over 84,800 GWH have been generated from geothermal resulting to a saving of over 4,900 million US$ in foreign exchange. 1. INTRODUCTION Kenya is located in the eastern part of Africa with 14 geothermal prospects identified in the Kenya rift starting from Barrier in the north to L Magadi in the south with an estimated potential of over 2000 MWe (Omenda et al., 2000). Studies done in the rift in mid 1960 identified Olkaria as the most economical prospect to develop (KPC, 1994). Exploration and field development was then done leading to the establishment of sectors which form the Great Olkaria Geothermal area (GOGA) currently with an installed capacity of 130 MWe. -
Kenya Nairobi-Amboseli-Samburu Mount Kenya-Lake Nakuru- Lake Naivasha-Masai Mara 13 Days | African Charm & Close to Nature
Kenya Nairobi-amboseli-Samburu mount Kenya-Lake Nakuru- Lake Naivasha-masai mara 13 Days | African Charm & Close to Nature DAY 1 Destination: Arrival at Jomo Kenyatta International Airport; Transfer to Nairobi Accommodations: Ololo Safari Lodge Activities: Optional Game Drive Arrival at Jomo Kenyatta International Airport. After clearing customs, you will be met by your expert naturalist guide and transferred to the lovely Ololo Safari Lodge, an elegant, thatched-roof African manor situated right on the edge of the African wilderness, overlooking Nairobi National Park. Just outside of Nairobi’s central business district is Nairobi National Park, Kenya’s first national park established in 1946. This park is iconic for its wide open grass plains and scattered acacia bush with the city of Nairobi’s skyscrapers in the backdrop. Despite its small size and proximity to human civilization, this park plays host to a wide variety of wildlife including lions, leopards, cheetahs, hyenas, buffaloes, giraffes and diverse birdlife with over 400 species recorded. As well, it is home to one of Kenya’s most successful rhino sanctuaries, and you are likely to see the endangered black rhino here. After settling in, you will meet with your guide to briefly go over your safari itinerary. Enjoy a lovely lunch, featuring Ololo’s garden grown produce and eggs. You then have the option of going on a late afternoon game drive into Nairobi National Park or staying at the lodge, perhaps taking a dip in the pool, walking around the beautiful gardens, reading a book by the fire, or enjoying a drink on the terrace overlooking the park.