DOCSLIB.ORG

Sibiloi National Park

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Sibiloi National Park CAMPING Public campsites: Turkana Campsite (latrines only-no water) and Koobi Fora Campsite (latrines only- no water) Sunset Strip Camp: this popular campsite at Loiyangalani offers a communal dining area, water, showers and lavatories. Contact: Tel (Nairobi) +254 (O)20 891348· Email: [email protected] WHAT TO TAKE WITH YOU: Allsupplies: especially fuel (the last fuel stations are in Marsabit or Maralal), food and water. Also useful are: camping equipment, breakdown equipment and medical kit as well as a camera, binoculars, hat, sunglasses and guidebooks PLEASE RESPECTTHE WILDLIFE CODE Respect the privacy of the wildlife, this is their habitat. Beware of the animals, they are wild and can be unpredictable. Don't crowd the animals or make sudden noises or movements. Don't feed the animals, it upsets their diet and leads to human dependence. Keep quiet, noise disturbs the wildlife and may antagonize your fellow visitors. Stay in your vehicle at all times, except at designated picnic or walking areas. Keep below the maximum speed limit (40kph/25mph). Never drive off-road, this severely damages the habitat. When viewing wildlife keep to a minimum distance of 20 meters and pull to the side of the road so as to allow others to pass. KENYA WILDLIFE SERVICE PARKS AND RESERVES Leave no litter and never leave fires unattended or discard burning objects. • ABERDARE NATIONAL PARK. AMBOSEU NATIONAL PARK. ARABUKO SOKOKE NATIONAL RESERVE. Respect the cultural heritage of Kenya, never take pictures of the local people or their • CENTRAL" SOUTHERN ISLAND NATIONAL PARK. CHYULU HILLS NATIONAL PARK • habitat without asking their permission, respect the cultural traditions of Kenya and • HELLS CATE NATIONAL PARK. KAKAMECA FOREST NATIONAL RESERVE. KISITE MpUNCUTI MARINE PARK. always dress with decorum. • KISUMU IMPALA SANCTUARY. KIUNCA NATIONAL MARINE RESERVE. KORA NATIONAL PARK. Stay over or leave before dusk, visitors must vacate the Park between 7.00pm - • LAKE NAKURU NATIONAL PARK. MAUNDI MARINE NATIONAL PARK. • MARSAIIT NATIONAL PARK" RESERVE. MERU NATIONAL PARK. MOMBASA MARINE NATIONAL PARK. 6.00am unless they are camping overnight. Night game driving is not allowed. • MOMIASA MARINE RESERVE. MOUNT ELCON NATIONAL PARK • • MT. KENYA NATIONAL PARK. MT. lONCONOT NATIONAL PARK. MWEA NATIONAL RESERVE. HOW TO GETTH ERE • NAIROBI NATIONAL PARK. NAIROBI SAFARI WALK" ORPHANACE. NDERE ISLAND NATIONAL PARK. Roads: • OL DONYO SABUK NATIONAL PARK. RUMA NATIONAL PARK. SAIWA SWAMP NATIONAL PARK. The lake is a three day drive from Nairobi via Marsabit and North Horr, or Maralal and south • SHIMBA HILLS NATIONAL RESERVE. SIBILOI NATIONAL PARK. TANA RIVER PRIMATE RESERVE • Horr. Alternatively travel by road from Nairobi to Kalokol on the lake's western shores, via • TSAVO EAST NATIONAL PARK. TSAVO WEST NATIONAL PARK. WATAMU MARINE NATIONAL RESERVE. Kitale and Lodwar. From Kalokol boat hire services are available across the lake to AIIiaBay. Airstrips: access to Lake Turkana is usually by air and there are two all-weather airstrips. KtNYA WlLOlln Open: stIMCE n Daily 6.00am - 6.00pm. Note: No entry is allowed on foot, and visitors will not be allowed Marketing & Business Development into the Park after 6.15pm. P.O.Box40241 - 00100 Nairobi Kenya. Current entry dlarges: Tel: +254 (020) 6000800, 6002345 Fax: +254 (020) 6007024 Current entry charges: Obtainable via KWSHQ:Tel: +254(20}6000800, 602345 ISDN:+254 (020) 3992000 Fax: 6007024 • Email: [email protected] Telkom Wireless: '·$afarl Card' reqiJlrtdl +254 (020) 2379407/8/9, 2379410/1/3/4/5/6 At present the park does not operate on the safari card system. Entry is by cash only (KShs orUS S). Mobile Numbers: Th Warden: +254 (0) 726610508/9,735 663 421, 736 663 400 P.O.Box 219, LowdarJel: +254 (054) 21223 Email: [email protected] The Koobi Fora Museum, Allia Bay Although all KoobiFora's human fossils are now housed Nairobi's National Museum, you can still view the fossils a 3 million year old giant tortoise, an ancient species of crocodile and a 1.5 million year old behemoth on site. Note: please do not remove any fossils remains from the sites as they may compromise the future research The tempestuous 'Jade Sea" The largest permanent desert lake in the world, lake Turkana isan isolated chloro-carbon -carbonate alkine giant covering 6,400 sq Km.lts mercurial blue-green colour has earned it the title 'The Jade Sea: Crocodile Kingdom Survivors of an epoch long before mankind, lake Turkana's estimated 12,000 crocodiles have not changed in 130 million years. Despite their monstrous size and formidable appearance they are generally inoffensive creatures living in perfect harmony with their environment and feeding on the lake's prolificfish. Petrified forests The largest areas of petrified wood lying around Sibiloi are the remains of a once-great cedar forest, which covered the lake's shores 7 million years ago. "CRADLEOF MANKIND, GARDENOF EDEN" Prolific birdlife Shimmering like a mirage in the harshly beautiful desert landscape of northern Kenya Sibiloi'savain highlights include: Somali ostrich, Koriand Heuglin's bustard, northern lie the blue-green waters of lake Turkana. On its shores lies one of the world's greatest WHERE TO STAY carmine and Somali bee-eater, chestnut-bellied sand grouse and fox kestrel. The Park is Lodges and Tented Camps treasures, the 3 million year old KoobiFora palaeontological site. First discovered by Dr also famous for the European migrants that sweep across its skies between March-May. Oasis lodge: located towards the southern end of the lake, there are 15 luxury bungalows Richard leaky and his team in 1972, Sibiloi is now universally recognized as the 'Cradle (with private bath and electricity), two spring-fed swimming pools, car and boat hire. of Mankind' and the most likely biblical Garden of Eden. WHEN TO GO Contact: Tel;(Nairobi) +254 (20) 503267 • Email:[email protected] The park isaccessible all year round. The Shimba hills are a dissected plateau that ascends steeply from the coastal plains, 30 lobolo Tented Camp: located on the western shore of the lake this hosted camp offers 6 km south west of Mombasa and just south of Kwaletown. The surrounding escarpment luxury tents and full board. rises from around 120m to 300m across the bulk of the plateau and as high as 450m at Contact: Bush Homes EA.Tel(Nairobi) +254 (0) 20 350703, 571661. Marere and Pengo hills. Allhills have views points, which offer splendid views of the Email: [email protected]· Website: www.bush-honies.co.ke hilly and forested countryside and far as the Indian Ocean and Chale Island to the East and the Tsavoplains and Taita hills to the West. Self-catering Accommodation AIIiaBayGuesthouse: this well equipped KWS-managed lakeshore guesthouse offers 3 WHAT TO SEE double bedrooms (mosquito nets and mattresses provided - take your own bedding, linen 'Sku1l1470~Homo habilis and towels). Solar generated electricity is provided. There is a furnished indoor sitting and Known as the 'Cradle of Mankind'Sibiloi National Park was created to protect the sites of dining area, one bathroom and an indoor kitchen (including a gas stove, cooking utensils, the many remarkable hominid fossils finds revealed by its searing winds. The park cutlery, crockery and glasses).Contact: KWSHQ,Nairobi. yielded its most striking treasure in 1972 when a 2 million year old fossilized skull was discovered by eminent paleontologist DrRichard leaky and his team. The almost National Museums of Kenya, Koobi fora complete skull (labeled '1470' by the National Museum of Kenya) confirmed the Thissite has simple chalets with a communal dining area, Water, showers and lavatories. existence of a sophisticated evolutionary hominid named Homo habilis, the direct There isalso a campsite. ancestor of Homo sapiens. Evidence of Homo erectus was also unearthed along with Contact: NMK.Tel:(Nairobi) +254 (0) 20 891348.· Email: [email protected] some 160 additional finds relating to the early hominids..
Load more

Recommended publications
  • Outcomes of the EU Horizon 2020 DAFNE PROJECT the Omo
    POLICY BRIEF October 2020 Outcomes of the EU Horizon 2020 DAFNE PROJECT The Omo-Turkana River Basin Progress towards cooperative frameworks KEY POLICY MESSAGES The OTB has reached a stage of pivotal importance for future development; the time to establish a cooperative framework on water governance is now. Transparency and accountability must be improved in order to facilitate the sharing of data and information, increasing trust and reducing the perception of risk. Benefit-sharing which extends beyond energy could enhance regional integration and improve sustainable development within the basin . THE OMO-TURKANA RIVER BASIN potential for hydropower and irrigation schemes that are, if scientifically and equitably managed, crucial to lift millions within and outside the basin out of extreme poverty; this has led to transboundary cooperation in recent years. This policy brief is derived from research conducted under the €5.5M four-year EU Horizon 2020 and Swiss funded ‘DAFNE’ project which concerns the promotion of integrated and adaptive water resources management, explicitly addressing the WEF Nexus and aiming to promote a sustainable economy in regions where new infrastructure and expanding The Omo-Turkana River Basin (OTB) – for the agriculture has to be balanced with social, purposes of the DAFNE Project – comprises of economic and environmental needs. The project two main water bodies: the Omo River in takes a multi- and interdisciplinary approach to Ethiopia and Lake Turkana which it drains into. the formation of a decision analytical While the Omo River lies entirely within Ethiopian territory, Lake Turkana is shared by framework (DAF) for participatory and both Kenya and Ethiopia, with the majority of integrated planning, to allow the evaluation of Lake Turkana residing within Kenya.
    [Show full text]
  • 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!
    [Show full text]
  • Phytolith Analysed to Compare Changes in Vegetation Structure of Koobi Fora and Olorgesailie Basins Through the Mid- Pleistocene-Holocene Periods
    Phytolith analysed to Compare Changes in Vegetation Structure of Koobi Fora and Olorgesailie Basins through the Mid- Pleistocene-Holocene Periods. By KINYANJUI, Rahab N. Student number: 712138 Submitted on 28th February, 2017 Submitted the revised version on 22nd February, 2018 Declaration A thesis submitted to the Faculty of Science in fulfilment of the requirements for PhD degree. At School of Geosciences, Evolutionary Studies Institute (ESI) University of Witwatersrand, Johannesburg South Africa. I declare that this is my own unaided work and has not been submitted elsewhere for degree purposes KINYANJUI, Rahab N. Student No. 712138 ii Abstract Phytolith analyses to compare changes in vegetation structure of Koobi Fora and Olorgesailie Basins through Mid-Pleistocene-Holocene Periods. By Rahab N Kinyanjui (Student No: 712138) Doctor of Philosophy in Palaeontology University of Witwatersrand, South Africa School of Geological Sciences, Evolutionary Science Institute (GEOS/ESI) Supervisor: Prof Marion Bamford. The Koobi Fora and Olorgesailie Basins are renowned Hominin sites in the Rift Valley of northern and central Kenya, respectively with fluvial, lacustrine and tuffaceous sediments spanning the Pleistocene and Holocene. Much research has been done on the fossil fauna, hominins and flora with the aim of trying to understand when and how the hominins evolved, and how the environment impacted on their behaviour, land-use and distribution over time. One of the most important factors in trying to understand the hominin-environment relationship is firstly to reconstruct the environment. Important environmental factors are the climate, rate or degree of climate change, vegetation structure and resources, floral and faunal resources. Vegetation structure/composition is a key component of the environments and, it has been hypothesized the openness and/or closeness of vegetation structure played a key role in shaping the evolutionary history not only of man but also other mammals.
    [Show full text]
  • Lake Turkana National Parks - 2017 Conservation Outlook Assessment (Archived)
    IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Lake Turkana National Parks - 2017 Conservation Outlook Assessment (archived) IUCN Conservation Outlook Assessment 2017 (archived) Finalised on 26 October 2017 Please note: this is an archived Conservation Outlook Assessment for Lake Turkana National Parks. To access the most up-to-date Conservation Outlook Assessment for this site, please visit https://www.worldheritageoutlook.iucn.org. Lake Turkana National Parks عقوملا تامولعم Country: Kenya Inscribed in: 1997 Criteria: (viii) (x) The most saline of Africa's large lakes, Turkana is an outstanding laboratory for the study of plant and animal communities. The three National Parks serve as a stopover for migrant waterfowl and are major breeding grounds for the Nile crocodile, hippopotamus and a variety of venomous snakes. The Koobi Fora deposits, rich in mammalian, molluscan and other fossil remains, have contributed more to the understanding of paleo-environments than any other site on the continent. © UNESCO صخلملا 2017 Conservation Outlook Critical Lake Turkana’s unique qualities as a large lake in a desert environment are under threat as the demands for water for development escalate and the financial capital to build major dams becomes available. Historically, the lake’s level has been subject to natural fluctuations in response to the vicissitudes of climate, with the inflow of water broadly matching the amount lost through evaporation (as the lake basin has no outflow). The lake’s major source of water, Ethiopia’s Omo River is being developed with a series of major hydropower dams and irrigated agricultural schemes, in particular sugar and other crop plantations.
    [Show full text]
  • 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.
    [Show full text]
  • Later Stone Age Toolstone Acquisition in the Central Rift Valley of Kenya
    Journal of Archaeological Science: Reports 18 (2018) 475–486 Contents lists available at ScienceDirect Journal of Archaeological Science: Reports journal homepage: www.elsevier.com/locate/jasrep Later Stone Age toolstone acquisition in the Central Rift Valley of Kenya: T Portable XRF of Eburran obsidian artifacts from Leakey's excavations at Gamble's Cave II ⁎ ⁎⁎ Ellery Frahma,b, , Christian A. Tryonb, a Yale Initiative for the Study of Ancient Pyrotechnology, Council on Archaeological Studies, Department of Anthropology, Yale University, New Haven, CT, United States b Department of Anthropology, Harvard University, Peabody Museum of Archaeology and Ethnology, Cambridge, MA, United States ARTICLE INFO ABSTRACT Keywords: The complexities of Later Stone Age environmental and behavioral variability in East Africa remain poorly Obsidian sourcing defined, and toolstone sourcing is essential to understand the scale of the social and natural landscapes en- Raw material transfer countered by earlier human populations. The Naivasha-Nakuru Basin in Kenya's Rift Valley is a region that is not Naivasha-Nakuru Basin only highly sensitive to climatic changes but also one of the world's most obsidian-rich landscapes. We used African Humid Period portable X-ray fluorescence (pXRF) analyses of obsidian artifacts and geological specimens to understand pat- Hunter-gatherer mobility terns of toolstone acquisition and consumption reflected in the early/middle Holocene strata (Phases 3–4 of the Human-environment interactions Eburran industry) at Gamble's Cave II. Our analyses represent the first geochemical source identifications of obsidian artifacts from the Eburran industry and indicate the persistent selection over time for high-quality obsidian from Mt. Eburru, ~20 km distant, despite changes in site occupation intensity that apparently correlate with changes in the local environment.
    [Show full text]
  • On the Conservation of the Cultural Heritage in the Kenyan Coast
    THE IMPACT OF TOURISM ON THE CONSERVATION OF THE CULTURAL HERITAGE IN THE KENYAN COAST BY PHILEMON OCHIENG’ NYAMANGA - * • > University ol NAIROBI Library "X0546368 2 A THESIS SUBMITTED TO THE INSTITUTE OF ANTHROPOLOGY, GENDER AND AFRICAN STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS IN ANTHROPOLOGY OF THE UNIVERSITY OF NAIROBI NOVEMBER 2008 DECLARATION This thesis is my original work. It has not been presented for a Degree in any other University. ;o§ Philemon Ochieng’ Nyamanga This thesis has been submitted with my approval as a university supervisor D ate..... J . l U ■ — • C*- imiyu Wandibba DEDICATION This work is dedicated to all heritage lovers and caregivers in memory of my late parents, whose inspiration, care and love motivated my earnest quest for knowledge and committed service to society. It is also dedicated to my beloved daughter. Leticia Anvango TABLE OF CONTENTS List of Tables----------------------------------------------------------------------------------------------------------------- v List of Figures----------------------------------------------------------------------------------------------------------------v List of P la tes---------------------------------------------------------------------------------------------------------------- vi Abbreviations/Acronvms----------------------------------------------------------------------------------------------- vii Acknowledgements-------------------------------------------------------------------------------------------------------viii
    [Show full text]
  • 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.
    [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]
  • The Characteristics and Chronology of the Earliest Acheulean at Konso, Ethiopia
    The characteristics and chronology of the earliest Acheulean at Konso, Ethiopia Yonas Beyenea,b, Shigehiro Katohc, Giday WoldeGabrield, William K. Harte, Kozo Utof, Masafumi Sudog, Megumi Kondoh, Masayuki Hyodoi, Paul R. Rennej,k, Gen Suwal,1, and Berhane Asfawm,1 aAssociation for Research and Conservation of Culture (A.R.C.C.), Awassa, Ethiopia; bFrench Center for Ethiopian Studies, Addis Ababa, Ethiopia; cDivision of Natural History, Hyogo Museum of Nature and Human Activities, Yayoigaoka 6, Sanda 669-1546, Japan; dEES-6/D462, Los Alamos National Laboratory, Los Alamos, NM 87545; eDepartment of Geology and Environmental Earth Science, Miami University, Oxford, OH 45056; fNational Institute of Advanced Industrial Science and Technology, 1-1-1 Umezono, Tsukuba 305-8567, Japan; gInstitute of Earth and Environmental Science, University of Potsdam, 14476 Golm, Germany; hLaboratory of Physical Anthropology, Ochanomizu University, Otsuka, Bunkyo-ku, Tokyo 112-8610, Japan; iResearch Center for Inland Seas, Kobe University, Kobe 657-8501, Japan; jBerkeley Geochronology Center, Berkeley, CA 94709; kDepartment of Earth and Planetary Science, University of California, Berkeley, CA 94720; lUniversity Museum, University of Tokyo, Hongo, Bunkyo-ku, Tokyo 113-0033, Japan; and mRift Valley Research Service, Addis Ababa, Ethiopia This contribution is part of the special series of Inaugural Articles by members of the National Academy of Sciences elected in 2008. Contributed by Berhane Asfaw, December 8, 2012 (sent for review November 30, 2012) The Acheulean technological tradition, characterized by a large carcass processing (13, 14), usually interpreted as a part of an (>10 cm) flake-based component, represents a significant techno- advanced subsistence strategy coincident with or postdating the logical advance over the Oldowan.
    [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]
  • 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.
    [Show full text]