DOCSLIB.ORG

Wildlife Safari in Kenya September 1-15, 2023

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
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. After a little rest up (time permitting), we will go to Daphne Sheldrake Elephant Orphanage for the 5pm stable/bedtime visit with the baby elephants. You will need to sponsor an elephant ($50) to participate (this must be booked far in advance, so only those who have signed up and sponsored their elephant in time will be able to participate). Dinner will be on your own at the Cottage restaurant. Accommodation: Karen Blixen Coffee Garden and Cottages (B, L) DAY 3 NAIROBI to SAMBURU After breakfast, we begin our exciting Safari adventure in Kenya, driving to Samburu National Reserve, and checking into Larsen’s Camp in time for lunch. The Lodge is situated inside the reserve which offers the opportunity to see an abundance of wildlife and bird life which has much to do with the “River of Brown Water” (Uaso Nyiro in the Samburu language), fed by rains in the far-off Aberdare ranges. Acacia trees, doum palms and mswaki (the toothbrush tree) provide balanced habitat for the vast variety of game. This afternoon we embark on our first exciting game drive in Kenya. DAYS 4-5 SAMBURU In our two full days in Samburu National Reserve we will have two GAME DRIVES each day, with an opportunity to see the famous big five and other wildlife, some found only here; like the long necked Gerenuk, Antelope, Somali Ostrich, Grevy’s Zebra, Majestic Beisa Oryx and the Reticulated Giraffe, perhaps we will be lucky and get a glimpse of Africa’s famous wild dogs. We will also visit the nearby Samburu Village if we were not able to do it on our first day. The Camp offers modern luxury tents with a private view over the river banks rich with wildlife. Each evening of our 3-night stay here, we will gather to entertain each other with stories of what we have seen and experienced during our game drives that day. Accommodation: Larsen’s Camp (3 nights) (B,L,D) DAY 6 SAMBURU to SWEETWATERS To break up the long drive from Samburu to Elementeita we will do a one-night stopover at Sweetwaters Serena tented camp in Ol Pejeta Conservancy. Time permitting we will stop on the way at Mount Kenya Safari Club to visit the animal orphanage (a.k.a. the best adult petting zoo ever!), where As You Like It (Safaris) Inc. is a sponsoring member. After our visit we continue on to Sweetwaters, arriving for lunch before an afternoon game drive. One night will not be enough, and we will wish we could stay longer, but we must continue tomorrow on our journey south toward the Mara. Accommodation: Sweetwaters Serena (1 night) (B,L,D) DAY 7 SWEETWATERS to LAKE ELEMENTEITA SOYSAMBU CONSERVANCY Today we drive across and down into the Great Rift Valley. Along the way we will see how the people live, their farms, their markets, their daily existence. By mid day we reach Lake Elementeita and our lodge for the next two nights. Hopefully we will find the famous pink flamingos that wade in the shallow shores together with multitudes of pelicans and a wide variety of other birds. Leopard can be found in the Conservancy, as well as buffalo and other game. Uniquely situated on the shoreline of sapphire-blue Lake Elmenteita where hundreds of thousands of birds congregate, the small and exclusive Lake Elmenteita Serena Camp in Kenya opened in July 2011. This area of breathtaking beauty, also home to many rare species of animals, is less than two hours’ drive from Nairobi and just a short distance to the famous Flamingo filled Lake Nakuru. Evocatively styled to echo the area’s rich history, our safari camp blends aristocratic elegance with modern luxury and will offer cuisine and service of fittingly high standards. DAY 8 ELEMENTEITA Another relaxed day in Elmenteita, driving in the Conservancy game viewing, swimming in the inviting pool, walking in their beautiful gardens, and bird watching will be phenomenal. Perhaps you will want to pamper yourself with an optional massage in the camp’s lovely spa, in between the twice daily game drives, of course. Often overlooked by people rushing from Lake Naivasha to Lake Nakuru, the area around Lake Elmenteita and up into the lower foothills of the Aberdare range offers some off-the-beaten-track destinations such as Kariandusi prehistoric site and other activities, including first-rate wildlife viewing, which take advantage of the pretty, lightly wooded hills and lush valley of the Malewa River. In addition, several top-end lodges provide an intimate alternative to their more touristy cousins around lakes Nakuru and Naivasha. Accommodation: Elementeita Serena Camp (2 nights) (B,L,D) DAY 9 ELEMENTEITA to MAASAI MARA Early this morning we continue our Kenya odyssey, as we journey to the Mara Triangle. After a rough ride on a tough road, we will check in for lunch, and be shown to our rooms in the Mara Serena Safari Lodge. After a rest, and maybe a swim, we will have our cup of ‘afternoon tea’ (or coffee) and, if we feel like it, head out for an afternoon game drive. Our lodge has one of the most spectacular views imaginable across the vast plains, forests and rivers that make up the Maasai Mara – one of the world’s richest wildlife sanctuaries. Seasoned safari travelers, travel writers, documentary makers and researchers often admit that the Maasai Mara is one of their favorite places. So why is that? Perhaps it is because of the 'big skies', the open savannahs, the romance of films like Out of Africa and certainly because of the annual wildebeest migration, the density of game, the variety of bird life and the chance of a hot air balloon ride. Also because of the tall red-robed Maasai people whose lifestyle is completely at odds with western practices, and from whom one learns to question certain western values. A combination of all these things plus something to do with the spirit of the place - which is hard to put into words - is what attracts people to the Mara over and over. DAY 10 MAASAI MARA After Breakfast, or perhaps an optional sunrise Hot Air Balloon Ride, we are off with our guides to explore what’s out there, up close and personal. The excitement is in the search, the adventure is awesome, the thrill is in finding – perhaps a cheetah on a kill, or a gazelle giving birth, lion cubs frolicking, zebra grazing, or a topi standing atop a mound like a centurion on guard. The ultimate goal of course, will be to witness a crossing. We wait in hope of seeing crossing herds while finding limitless chances for game spotting and spectacular photography. Accommodation: Mara Serena Lodge (2 nights) (B,L,D) DAY 11 MARA SERENA to LITTLE MARA BUSH CAMP After breakfast we game drive our way over to the Little Mara Bush Camp. This will be your truly “Out of Africa,” eco-friendly experience, and you will lap up and love the luxury and service, quite apart from the fact that you will be right in the midst of one of the best game viewing areas in Kenya. The Little Mara Bush Camp boasts one of the best and most spectacular locations in the famous Maasai Mara Game Reserve. On the banks of the seasonal Olare Orok River, it overlooks a large hippo pool with a population of over 40 hippos at any given time. With only 12 luxury tents on wooden platforms, Little Mara Bush Camp offers the desired exclusivity for guests who are looking for maximum privacy. Join us in the Bar/Lounge where an array of classic cocktails and sundowners await you. You will find a charging station for your camera batteries and laptops in the Photo Lounge. All Guest Tents are designed with great attention to detail. Mahogany furniture and luxurious soft furnishings give it the desired comfort of a luxury Camp with a "bush feeling".
Load more

Recommended publications
  • 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.
    [Show full text]
  • Conserving Wildlife in African Landscapes Kenya’S Ewaso Ecosystem
    Smithsonian Institution Scholarly Press smithsonian contributions to zoology • number 632 Smithsonian Institution Scholarly Press AConserving Chronology Wildlife of Middlein African Missouri Landscapes Plains Kenya’sVillage Ewaso SitesEcosystem Edited by NicholasBy Craig J. M. Georgiadis Johnson with contributions by Stanley A. Ahler, Herbert Haas, and Georges Bonani SERIES PUBLICATIONS OF THE SMITHSONIAN INSTITUTION Emphasis upon publication as a means of “diffusing knowledge” was expressed by the first Secretary of the Smithsonian. In his formal plan for the Institution, Joseph Henry outlined a program that included the following statement: “It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge.” This theme of basic research has been adhered to through the years by thousands of titles issued in series publications under the Smithsonian imprint, com- mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Contributions to Anthropology Smithsonian Contributions to Botany Smithsonian Contributions to History and Technology Smithsonian Contributions to the Marine Sciences Smithsonian Contributions to Museum Conservation Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology In these series, the Institution publishes small papers and full-scale monographs that report on the research and collections of its various museums and bureaus. The Smithsonian Contributions Series are distributed via mailing lists to libraries, universities, and similar institu- tions throughout the world. Manuscripts submitted for series publication are received by the Smithsonian Institution Scholarly Press from authors with direct affilia- tion with the various Smithsonian museums or bureaus and are subject to peer review and review for compliance with manuscript preparation guidelines.
    [Show full text]
  • 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.
    [Show full text]
  • Journal of the East Africa Natural History Society and National Museum
    JOURNAL OF THE EAST AFRICA NATURAL HISTORY SOCIETY AND NATIONAL MUSEUM 15 October, 1978 Vol. 31 No. 167 A CHECKLIST OF mE SNAKES OF KENYA Stephen Spawls 35 WQodland Rise, Muswell Hill, London NIO, England ABSTRACT Loveridge (1957) lists 161 species and subspecies of snake from East Mrica. Eighty-nine of these belonging to some 41 genera were recorded from Kenya. The new list contains some 106 forms of 46 genera. - Three full species have been deleted from Loveridge's original checklist. Typhlops b. blanfordii has been synonymised with Typhlops I. lineolatus, Typhlops kaimosae has been synonymised with Typhlops angolensis (Roux-Esteve 1974) and Co/uber citeroii has been synonymised with Meizodon semiornatus (Lanza 1963). Of the 20 forms added to the list, 12 are forms collected for the first time in Kenya but occurring outside its political boundaries and one, Atheris desaixi is a new species, the holotype and paratypes being collected within Kenya. There has also been a large number of changes amongst the 89 original species as a result of revisionary systematic studies. This accounts for the other additions to the list. INTRODUCTION The most recent checklist dealing with the snakes of Kenya is Loveridge (1957). Since that date there has been a significant number of developments in the Kenyan herpetological field. This paper intends to update the nomenclature in the part of the checklist that concerns the snakes of Kenya and to extend the list to include all the species now known to occur within the political boundaries of Kenya. It also provides the range of each species within Kenya with specific locality records .
    [Show full text]
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • Geothermal Exploration in 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. APPLICATION OF MICRO-SEISMIC METHODS TO GEOTHERMAL EXPLORATION: EXAMPLES FROM THE KENYA RIFT Silas M. Simiyu Kenya Electricity Generating Company Ltd. (KenGen) P.O. Box 785, Naivasha KENYA [email protected] ABSTRACT Results from volcano-seismic studies of many geothermal fields show that they are possible resource-mapping tools for geothermal exploration and reservoir monitoring. They have been able to map the size and depth of possible shallow geothermal heat sources by analyzing data for seismic gaps, S-wave attenuation, reflected arrivals and converted waves. Analysis of shear wave split data for fracture density show high permeability areas that are potential targets for drilling high-producer wells. Variation of Vp/Vs ratios is related to reservoir fluid phases where low values are related to a decrease in P-wave velocity in the area with low pore pressure, high heat flow, fracturing and steam/gas saturation in the reservoir. High velocity ratios were found in the relatively liquid-saturated high-pressure fields that these ratios are useful tools for monitoring reservoirs under exploitation. The volcano-seismic approach can be useful as a stand alone tool for analyzing geothermal resource both at the exploration and exploitation stage that is cost effective in the long term 1. INTRODUCTION The main objective of any scientific investigation for a geothermal resource is to locate a potentially attractive reservoir which can be economically exploited for electric power generation and other uses.
    [Show full text]
  • 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.
    [Show full text]
  • Technical Report KMF/RS/2018/C 1.7 31ST MARCH 2018
    KENYA MARINE AND FISHERIES RESEARCH INSTITUTE FRESH WATER SYSTEMS ASSESSMENT OF THE FISHERIES STATUS IN RIVER MALEWA TO GUIDE MANAGEMENT OF THE FISHERY Technical Report KMF/RS/2018/C 1.7 31ST MARCH 2018 i DOCUMENT CERTIFICATION Certification by KMFRI Assistant Director Freshwater Systems I hereby certify that this report has been done under my supervision and submitted to the Director. Name: Christopher Aura Mulanda (PhD) Signature: 8th Feb., 2018 Certification by Director KMFRI I hereby acknowledge receipt of this Report Name: Prof. James M. Njiru (PhD) Signature: Date: 18th June 2018 ii Produced by: Kenya Marine and Fisheries Research Institute P. O. Box 81651-80100 Mombasa Kenya Tel: +254 (041)475151/4 Website: www.kmfri.co.ke Email: [email protected] Suggested citation formats: Nzioka, A., Morara, G., Boera, P.,Waithaka, E., Mutie, A., Obegi, B., and Loki, P (2017). Assessment of the fisheries status in River Malewa to guide management of the fishery. Technical report KMF/RS/2018/C1.7. Kenya Marine and Fisheries Research Institute. 28pp iii Acknowledgements We wish to thank the Government of Kenya for funding this activity through the Director KMFRI and Deputy Director Fresh Water systems for facilitating. Many thanks to KMFRI Naivasha technical team for assisting with logistics and sampling, and to the entire KMFRI Naivasha staff for their support. iv Abstract This study presents the first documentation of the status of the River Malewa fishery, a major river draining into Lake Naivasha and, to relate the status of the current commercial fishery to information on potential yields so as to identify whether or not there is a scope for better management and utilization of the resource (River Malewa fishery).Six sampling sites were selected from the upper catchment area of the Malewa river system to the lower catchment as it drains into Lake Naivasha.An integrated assessment of water quality to all sites, including the collection of fish communities, physical habitat and chemical information to assess river Malewa conditions was conducted.
    [Show full text]
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • (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.
    [Show full text]