Challenges in Water Management in the Lake Naivasha Basin
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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. -
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. -
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. -
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. -
Geothermal Potential of the Kenya Rift
Presented at Short Course III on Exploration for Geothermal Resources, organized by UNU-GTP and KenGen, at Lake Naivasha, Kenya, October 24 - November 17, 2008. GEOTHERMAL TRAINING PROGRAMME Kenya Electricity Generating Co., Ltd. STATUS OF GEOTHERMAL EXPLORATION IN KENYA AND FUTURE PLANS FOR ITS DEVELOPMENT Peter A. Omenda Kenya Electricity Generating Company Ltd. (KenGen) P.O. Box 785, Naivasha KENYA [email protected] ABSTRACT The high temperature geothermal prospects in Kenya are located within and are associated with the development of the Kenya Rift. Kenya Rift is a continental scale volcano-tectonic feature that stretches from northern to southern Africa. Development of the Rift started during the Oligocene (30million years ago) and activity has continued to recent times. The last 2 million years saw the development of large shield volcanoes within the axis of the rift. These centres are the most important geothermal prospects within the rift. Association between rifting and most of the occurrences of geothermal energy is mainly due to shallow magma chambers underneath the young volcanoes within the rift axis. KenGen in collaboration with the Ministry of Energy of the Government of Kenya has undertaken detailed surface studies of most of the prospects in the central sector of the rift which comprises Suswa, Longonot, Olkaria, Eburru, Menengai, Lakes Bogoria and Baringo, Korosi and Paka volcanic fields. Electric power is currently being generated at Olkaria with 130MWe installed while exploration drilling has been undertaken at Eburru and a 2.5MWe pilot plant is planned for development by KenGen and commissioning by 2009. Common methods that have been used by KenGen during exploration expeditions include geology (lithology, geochronology, structures); geophysics (seismic, gravity, magnetic, and resistivity); geochemistry (fluid and thermometry), heat flow and environmental baseline assessments. -
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. -
NOTES on the HYDROLOGY of LAKE NAIVASHA.• The
NOTES ON THE HYDROLOGY OF LAKE NAIV ASHA .• By H. L. SIKES, C.B.E., B.A., B.E., M.INST.C.E., F.G.S. The hydrological features of Lake Naivashaare not only of scientific interest but are also of some economic importance. A record of tpe fluctuations of lake level has been maintained with four short breaks since tpe end of 19oB, readings being taken weekly. A b.athy• metrical survey was carried out in 1927 with sufficient precision to enable the volume of water and the area of the lake to be c~culated approximately as the level varies. Evaporation meter readings were started in 1917, but, in the case of those prior to 1920, the method adopted is not regarded as sufficiently reliable to be of value; the records are incomplete for the years 1927 and 1928, but complete records exist for 14 years. The number of rain gauges in the drainage area of the lake, 1,203 square miles, is still regrettably small. Only six pave been established and of these the longest record is·from 1904·' However, a number of gauges outside the drainage area, under climatic conditions which appear to correspond fairly well with one or other pIlrt of the drainage area, provide useful data for co-ordination and check. With the help of these a reasonably accurate knowledge of the rainfall on the drainage or catchment area and on Lake Naivasha itself is thougpt to have been achieved, though, in the case of a region where much of the rainfall is of the instability type, precision is im• possible of attainment. -
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). -
HYDROCHEMISTRY of OLKARIA and EBURRU Geotilermal Fields, KENYAN RIFT VALLEY
Repon 2, 1991 HYDROCHEMISTRY OF OLKARIA AND EBURRU GEOTIlERMAL FIElDS, KENYAN RIFT VALLEY Musa Kipchirchir Arusei, UNU Geothermal Training Programme, Orkustofnun - National Energy Authority, Grensasvegur 9, 108 Reykjavik, ICElAND. Permanent address: Olkaria Geothermal Project, P.O. Box 785, Naivasha, KENYA 3 ABSTRACf The chemical composition of waters from cold and warm borehoies, springs, Lake Naivasha, River Morendati and geothermal waters from the Olkaria and Eburru fields is presented. The study of the chemistry of the waters has been used to suggest movement and processes affecting the groundwater in the Rift Valley. The study has shown that Lake Naivasha, which is the only fresh water lake in the Kenyan Rift Valley, recharges most of the nearby boreholes. The chemical characteristics of the geothermal waters in Olkaria and Eburru geothermal fields are similar. Eburru and Olkaria geothermal reservoirs get some of their recharge from the rift groundwater. The waters from some boreholes to the north of Eburru and Elementeita spring are outflows from Eburru geothermal field and there seems to be no other geothermal resource in the Elementeita area. The escarpment warm spring waters are shallow escarpment waters that have been heated by shallow hot rock, probably below the location of the springs. They may not be related to the geothennal systems at Olkaria and Eburru. Monitoring of water levels around the lake is recommended to determine the possible effect of geothermal exploitation at Olkaria on Lake Naivasha. Further work to estimate the outflow of water from the lake and inflow into it is also recommended. 4 TABLE OF CONTENTS Page ABSTRACT ......................................... -
The Ecological State of Lake Naivasha, Kenya, 2005: Turning 25 Years Research Into an Effective Ramsar Monitoring Programme
The ecological state of Lake Naivasha, Kenya, 2005: Turning 25 years research into an effective Ramsar monitoring programme Item Type Proceedings Paper Authors Mavuti, K.M.; Harper, David Citation Odada, Eric & Olago, Daniel O. (Ed.) Proceedings of the 11th World Lakes Conference: vol. 2. p. 30-34. Download date 28/09/2021 04:05:11 Link to Item http://hdl.handle.net/1834/2127 The ecological state of Lake Naivasha, Kenya, 2005: Turning 25 years research into an effective Ramsar monitoring programme K.M.Mavuti1 & D. M. Harper2 1 Department of Zoology, University of Nairobi, Kenya 2 Department of Biology University of Leicester, England Introduction (LNROA), was formed and had the legal right to resolve disputes between adjacent landowners over Lake Naivasha (0. 45ºS, 36. 26ºE), altitude 1890, their use of this riparian lake bed (Enniskillen, 2002). lies in the Eastern Rift Valley and currently covers approximately 100 km2. It is the second-largest In the early 1980s, successful experiments in freshwater lake in Kenya (after the Kenya portion of production of cut flowers led to the growth of a Victoria). It is one of a series of 23 major lakes in the horticultural industry dependent upon irrigation Eastern Rift Valley – eight in central Ethiopia, eight water. Since the first flower farms started there has in Kenya and seven in Tanzania – spanning been a fairly constant increase of the area latitudes from approximately 7º N to 5º S. The cultivated, more rapidly in the last five years, to overall climate of the Eastern Rift Valley is semi-arid. occupy now about 4,000 ha (Becht, unpublished). -
Lake Naivasha
Community The Shop Login/Register Shopping Cart Footprint Latin America Asia Africa & Middle East Australasia Europe North America Activity DPoubpaOiut MapEgs y&p tGuidesIsrael Jordan Kenya Lebanon Morocco More... Africa & Middle East » Kenya » Rift Valley » Naivasha and around » Lake Quick Search GO Kenya Naivasha About Kenya Planning Lake Naivasha Products in this Region Essentials Nairobi Rift Valley No related products Naivasha and around Contents Nairobi to Naivasha 1 Introduction Naivasha Lake Naivasha 2 Ins and outs PDF Downloads Hell's Gate National Park 3 Background Kigio Wildlife Conservancy 4 Sights Mount Longonot National No PDFs currently available Park Nakuru and around Further north Lake Naivasha is one of the few fresh-water lakes in the Rift Valley. It Masai Mara National Reserve is 170 sq km in size, at about 1890 m above sea level and is a lovely Digital Products Western Kenya place to come for a weekend if you are staying in Nairobi as it is only Central Highlands a 1½-hour drive away. Strong afternoon winds cause the lake to get Southern Kenya suddenly very rough and the local Masai called the lake Nai'posha Available NOW! Lamu Archipelago meaning 'rough water', which the British later miss-spelled as Read more... Northern Kenya Naivasha. Much of the lake is surrounded by forests of the yellow- The coast barked acacia tree, full of birds and black and white colobus Traveller's tales monkeys. Acacia were once called 'yellow fever trees' after explorers who camped under them caught malaria. The lake has no apparent Shop in Kenya outlet, but it is believed to drain underground, and is quite picturesque with floating islands of papyrus.