ROYAL HOLLOWAY, UNIVERSITY of LONDON the Obsidian Evidence
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Geberit's Building Technology and Acoustics Laboratory the Cave Art
Know- how Customer Magazine December 2017 20 years Geberit’s Building Technology and Acoustics Laboratory 15,000 years The cave art of Lascaux document553997946950109986.indd 1 13.12.2017 09:09:53 Know-how runs through everything we do. Publisher Geberit Southern Africa (Pty.) Ltd. 6 Meadowview Lane Meadowview Business Estate Longmeadow, Linbro Park ZA-Johannesburg Phone +27 11 444 50 70 Fax +27 11 656 34 55 [email protected] → www.geberit.co.za Number of copies Issued: quarterly. The reproduction of individual articles, in part or in full, is subject to approval from the editorial staff. Photos Ben Huggler (cover picture, page 16, back page) Sergio Grazia (pages 22–23) Michael Suter (pages 10–13) Tribecraft (pages 14–15, 17) On the cover Vibrometric sensors are positioned in order to analyse sound transmissions. 2 document8739697254805857473.indd 2 13.12.2017 09:09:46 Contents A company on the move Ten years Geberit Southern Africa 18 Long-lasting pleasure Products & solutions 14 News/Agenda 5 Building Technology and Acoustics Laboratory 6 Mapress Carbon Steel 10 Online bathroom planner 13 Reference object 22 Diese Schwitzwasser-Isolation wirkt sich überall vor- 26-28 dB (A) leise, nach DIN 52218. teilhaft aus, jedoch besonders in Gegenden mit kaltem GEBERIT* Wasser oder mit hoher Luftfeuchtigkeit, bei stark gebert + cie frequentierten Klosettanlagen sowie in innenliegenden Armaturen-und Apparatefabrik WC-Räumen. Zudem trägt sie dazu bei, daß der bekannt JJJj^j§^omT" am Zürichsee leise GEBERIT-Spülkasten noch leiser wurde, genau: Telex75625 Once upon a time <-:.: Diese Schwitzwasser-Isolation wirkt sich überall vor- 26-28 dB (A) leise, nach DIN 52218. -
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. -
A Íalvak Foglalkozási Szerkezetének Átalakulása Borsod-Abaúj-Zemplén Megyében
A íalvak foglalkozási szerkezetének átalakulása Borsod-Abaúj-Zemplén megyében BODNÁR LÁSZLÓ tanszékvezető docens Borsod-Abaúj-Zemplén megye falusi településhálózata a közelmúlt- ban lényegi változásokon ment keresztül. A végbement koncentráció kapcsán már több helyütt felmerültek azok a sokágú kapcsolatok, amelyek a hálózati nagyságrendi struktúrát és a funkcionális struktúrát fűzik szoros egységbe. A funkcionális fejlődést, egy-egy megye országos fejlődési áramkörbe való gyorsabb bekapcsolódását éppen az ott uralkodó hálózati struktúra lassítja vagy éppen meggátolja. Módosításuk, cLZclZ ct társadalom új térbeli igényeihez való „igazításuk" magas beruházási költségkihatásain jelentkezik. A múltbeli örökség mellett — amely a korábbiakból átöröklött eredmé- nyek összegzője, s egyben a fejlődési folyamatosság biztosítója — a hálózat funkcionális felépítettségc tölti ki tartalommal a településhálózat funkcioná- lis szerkezetét. Ezek, az egymással bonyolult kölcsönkapcsolati rendszerben álló funk- ciók, mint a társadalom alapvető „életjelenségei", mindegyikének sajátos térbeli rendje van, együttesük pedig a funkcionális hálózat térbeli rendszeré- nek meghatározója. A múltbeli rendhez képest új térbeli hálózati struktúra kialakítását, azaz az adott térségnek a maga meglévő igényeihez való formálását tükrözi a településhálózat szerkezete. A településhálózat funkcionális szerkezetének aránytalanságai — azaz a közeli és régmúltból öröklött egyenlőtlen gazdasági fejlettség — miatt, a ter- mészeti erőforrások adta területi pontenciáltól nem kellő -
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. -
Terminal Pleistocene Lithic Variability in the Western Negev (Israel): Is There Any Evidence for Contacts with the Nile Valley? Alice Leplongeon, A
Terminal Pleistocene lithic variability in the Western Negev (Israel): Is there any evidence for contacts with the Nile Valley? Alice Leplongeon, A. Nigel Goring-Morris To cite this version: Alice Leplongeon, A. Nigel Goring-Morris. Terminal Pleistocene lithic variability in the Western Negev (Israel): Is there any evidence for contacts with the Nile Valley?. Journal of lithic studies, University of Edinburgh, 2018, 5 (5 (1)), pp.xx - xx. 10.2218/jls.2614. hal-02268286 HAL Id: hal-02268286 https://hal.archives-ouvertes.fr/hal-02268286 Submitted on 20 Aug 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Terminal Pleistocene lithic variability in the Western Negev (Israel): Is there any evidence for contacts with the Nile Valley? Alice Leplongeon 1,2,3, A. Nigel Goring-Morris 3 1. UMR CNRS 7194, Human & Environment Department, Muséum national d’Histoire Naturelle - Université Via Domitia Perpignan - Sorbonne Universités, 1 rue René Panhard, 75013 Paris, France. Email: [email protected] 2. McDonald Institute for Archaeological Research, University of Cambridge, Downing Street, CB2 3ER Cambridge, U.K. 3. Institute of Archaeology, The Hebrew University of Jerusalem, Jerusalem 91905, Israel. -
Act Cciii of 2011 on the Elections of Members Of
Strasbourg, 15 March 2012 CDL-REF(2012)003 Opinion No. 662 / 2012 Engl. only EUROPEAN COMMISSION FOR DEMOCRACY THROUGH LAW (VENICE COMMISSION) ACT CCIII OF 2011 ON THE ELECTIONS OF MEMBERS OF PARLIAMENT OF HUNGARY This document will not be distributed at the meeting. Please bring this copy. www.venice.coe.int CDL-REF(2012)003 - 2 - The Parliament - relying on Hungary’s legislative traditions based on popular representation; - guaranteeing that in Hungary the source of public power shall be the people, which shall pri- marily exercise its power through its elected representatives in elections which shall ensure the free expression of the will of voters; - ensuring the right of voters to universal and equal suffrage as well as to direct and secret bal- lot; - considering that political parties shall contribute to creating and expressing the will of the peo- ple; - recognising that the nationalities living in Hungary shall be constituent parts of the State and shall have the right ensured by the Fundamental Law to take part in the work of Parliament; - guaranteeing furthermore that Hungarian citizens living beyond the borders of Hungary shall be a part of the political community; in order to enforce the Fundamental Law, pursuant to Article XXIII, Subsections (1), (4) and (6), and to Article 2, Subsections (1) and (2) of the Fundamental Law, hereby passes the following Act on the substantive rules for the elections of Hungary’s Members of Parliament: 1. Interpretive provisions Section 1 For the purposes of this Act: Residence: the residence defined by the Act on the Registration of the Personal Data and Resi- dence of Citizens; in the case of citizens without residence, their current addresses. -
Prehistoric Exploitation of Limnosilicites in Northern Hungary: Problems and Perspectives Zsolt Mester and Norbert Faragó
Archaeologia Polona, vol. 54: 2016, 1 – 5 PL ISSN 0066 - 5924 Editorial The first scientific investigations of the sources of flint in Poland were undertaken by archaeologist Stefan Krukowski and geologist Jan Samsonowicz in the early 20th century. Krukowski used archaeological materials to identify the macroscopic char- acteristics of ‘chocolate’ flints, described their differences, and showed the potential location of the deposits (Krukowski 1920: 189–195; Budziszewski 2008: 33). In the search for deposits of flint, their outcrops, and prehistoric mines, Krukowski was accompanied by young geologist Jan Samsonowicz. The result of their cooperation was the discovery in 1921 of in situ deposits and surface accumulations of limestones containing fragments of flint and, in 1922, the identification of a prehistoric mine at Krzemionki Opatowskie (Krukowski 1923; Samsonowicz 1923; Bąbel 2014). This long tradition of studying siliceous rocks has continued at the Institute of Archaeology and Ethnology, Polish Academy of Science. In 1965 Zygmunt Krzak published the first characterization of gray white-spotted (świeciechów) flint (Krzak 1965) and five years later he described Turonian flint from Ożarów (Krzak 1970). In 1971 Romuald Schild devised a classification of ‘chocolate’ flint from the north-east margin of the Holy Cross (Świątokrzyskie) Mountains (Schild 1971, 1976) and Bogdan Balcer investigated a flint mine in Świeciechów, Kraśnik district, and the use of gray white-spotted (świeciechów) flint during the Neolithic (Balcer 1975, 1976). In 1980 Jacek Lech discussed the geology of Jurassic-Cracow flint and showed its relevance to archaeology (Lech 1980). Since that time Polish archeologists have carried out many investigations on different types of flint (e.g., Budziszewski and Michniak 1983/1989; Pawlikowski 1989; Budziszewski and Michinak eds 1995; Schild and Sulgostowska eds 1997; Matraszek and Sałaciński eds 2002; Gutowski 2004; Borkowski et al., 2008; Migaszewski et al., 2006, Krajcarz et al., 2014). -
Late Pleistocene Age and Archaeological Context for the Hominin Calvaria from Gvjm-22 (Lukenya Hill, Kenya)
Late Pleistocene age and archaeological context for the hominin calvaria from GvJm-22 (Lukenya Hill, Kenya) Christian A. Tryona,1, Isabelle Crevecoeurb, J. Tyler Faithc, Ravid Ekshtaina, Joelle Nivensd, David Pattersone, Emma N. Mbuaf, and Fred Spoorg,h aDepartment of Anthropology, Harvard University, Cambridge, MA 02138; bUnité Mixte de Recherche 5199, de la Préhistoire à l’Actuel: Culture, Environnement, et Anthropologie, Centre National de la Recherche Scientifique, Université de Bordeaux, 33615 Talence, France; cArchaeology Program, School of Social Science, University of Queensland, Brisbane, QLD 4072, Australia; dDepartment of Anthropology, New York University, New York, NY 10003; eCenter for the Advanced Study of Hominid Paleobiology, Department of Anthropology, The George Washington University, Washington, DC 20052; fNational Museums of Kenya, Nairobi, Kenya 00100; gDepartment of Human Evolution, Max Planck Institute for Evolutionary Anthropology, D-04103, Leipzig, Germany; and hDepartment of Cell and Developmental Biology, University College London, WC1E 6BT London, United Kingdom Edited by Erik Trinkaus, Washington University, St. Louis, MO, and approved January 16, 2015 (received for review September 19, 2014) Kenya National Museums Lukenya Hill Hominid 1 (KNM-LH 1) is Hominid 1 (KNM-LH 1) partial calvaria from site GvJm-22 at a Homo sapiens partial calvaria from site GvJm-22 at Lukenya Hill, Lukenya Hill, Kenya, the only eastern African fossil hominin Kenya, associated with Later Stone Age (LSA) archaeological de- from a Last Glacial Maximum [LGM; 19–26.4 kya (19)] LSA posits. KNM-LH 1 is securely dated to the Late Pleistocene, and archaeological context. We construct a revised accelerator mass samples a time and region important for understanding the origins spectrometry (AMS) radiocarbon chronology built on 26 new of modern human diversity. -
ADDRESSING VIOLENCE, PROMOTING INTEGRATION FIELD ASSESSMENT of VIOLENT INCIDENTS AGAINST ROMA in HUNGARY: Key Developments, Fi
Office for Democratic Institutions and Human Rights ADDRESSING VIOLENCE, PROMOTING INTEGRATION FIELD ASSESSMENT OF VIOLENT INCIDENTS AGAINST ROMA IN HUNGARY: Key Developments, Findings and Recommendations June-July 2009 Warsaw 15 June 2010 TABLE OF CONTENTS 1. Introduction ................................................................................................................... 3 2. Summary of Key Developments, Underlying Context and Major Recommendations ........................................................................................................... 5 3. Violent Incidents against Roma ............................................................................... 11 4. Reactions to Violent Incidents and Anti-Roma Sentiments................................. 15 5. Challenges to Combating Hate Crimes in Hungary ............................................. 39 6. Underlying Factors and the Overall Context in Which Violent Incidents Have Occurred .......................................................................................................................... 44 7. Recommendations .................................................................................................... 49 APPENDICES................................................................................................................. 55 Appendix 1: Incidents and Violence against Roma in Hungary in 2008-2009 . 56 Appendix 2: List of Delegation Members................................................................ 65 Appendix 3: List of meetings -
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. -
Tennessee Archaeology 2(2) Fall 2006
TTEENNNNEESSSSEEEE AARRCCHHAAEEOOLLOOGGYY Volume 2 Fall 2006 Number 2 EDITORIAL COORDINATORS Michael C. Moore TTEENNNNEESSSSEEEE AARRCCHHAAEEOOLLOOGGYY Tennessee Division of Archaeology Kevin E. Smith Middle Tennessee State University VOLUME 2 Fall 2006 NUMBER 2 EDITORIAL ADVISORY COMMITTEE David Anderson 62 EDITORS CORNER University of T ennessee ARTICLES Patrick Cummins Alliance for Native American Indian Rights 63 The Archaeology of Linville Cave (40SL24), Boyce Driskell Sullivan County, Tennessee University of T ennessee JAY D. FRANKLIN AND S.D. DEAN Jay Franklin 83 Archaeological Investigations on Ropers East Tennessee State University Knob: A Fortified Civil War Site in Williamson County, Tennessee Patrick Garrow BENJAMIN C. NANCE Dandridge, Tennessee Zada Law 107 Deep Testing Methods in Alluvial Ashland City, Tennessee Environments: Coring vs. Trenching on the Nolichucky River Larry McKee SARAH C. SHERWOOD AND JAMES J. KOCIS TRC, Inc. Tanya Peres RESEARCH REPORTS Middle Tennessee State University 120 A Preliminary Analysis of Clovis through Sarah Sherwood Early Archaic Components at the Widemeier University of Tennessee Site (40DV9), Davidson County, Tennessee Samuel D. Smith JOHN BROSTER, MARK NORTON, BOBBY HULAN, Tennessee Division of Archaeology AND ELLIS DURHAM Guy Weaver Weaver and Associates LLC Tennessee Archaeology is published semi-annually in electronic print format by the Tennessee Council for Professional Archaeology. Correspondence about manuscripts for the journal should be addressed to Michael C. Moore, Tennessee Division of Archaeology, Cole Building #3, 1216 Foster Avenue, Nashville TN 37210. The Tennessee Council for Professional Archaeology disclaims responsibility for statements, whether fact or of opinion, made by contributors. On the Cover: Ceramics from Linville Cave, Courtesy, Jay Franklin and S.D. -
VARGA A.: a Magyarországi Bodrogköz Mollusca Faunája
Varga_Bodrogkoz_Mollusca.qxd 2009.01.12. 13:28 Page 27 FOLIA HISTORICO NATURALIA MUSEI MATRAENSIS 2008 32: 27–55 A magyarországi Bodrogköz Mollusca faunája VARGA ANDRÁS ABSTRACT: This study reports the occurrence of 84 species from the Bodrogköz region of northeastern Hungary. The 65 species known from literature data are now extended with 19 species, which represent new records from this area. Theodoxus transversalis is believed to be extinct, and the presence of Anisus calculi- formis is dubious. Remarkable finds are the discoveries of live populations of Valvata macrostoma and Gyraulus riparius. This territory is inhabited by nine protected species, namely: Anisus vorticulus, Bielzia coerulans, Borysthenia naticina, Helix lutescens, Helix pomatia, Monachoides vicinus, Perforatella bidentata, Pseudanodonta complanata, Unio crassus. The species list is extended with 36, apparently non-indigenous species that were found in the flotsam of the Tisza and Bodrog Rivers. Bevezetés A Bodrogköz magyarországi területének (TUBA & SZIRMAI 2007) puhatestûivel foglalkozó átfogó dolgozatot a hazai malakológiai irodalomban (VARGA, FÜKÖH & KROLOPP 2005) nem találunk. Szórványos adatok elõfordulnak a publikációkban, de a terület szisztematikus fel- tárása még váratott magára. Az 1960-70-es években megtörtént több hazai problematikus genus revíziója (Aegopinella, Carychium, Oxychilus, Vallonia, Vitrea, stb.), s ezzel párhuzamosan megindult a magyarországi Mollusca fauna rendszeres felmérése, a hazai gyûjteményekben fellelhetõ adatok UTM rendszerû adatbázisba