IAVCEI National Report Russia 2007-2010
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Confirmed Soc Reports List 2015-2016
Confirmed State of Conservation Reports for natural and mixed World Heritage sites 2015 - 2016 Nr Region Country Site Natural or Additional information mixed site 1 LAC Argentina Iguazu National Park Natural 2 APA Australia Tasmanian Wilderness Mixed 3 EURNA Belarus / Poland Bialowieza Forest Natural 4 LAC Belize Belize Barrier Reef Reserve System Natural World Heritage in Danger 5 AFR Botswana Okavango Delta Natural 6 LAC Brazil Iguaçu National Park Natural 7 LAC Brazil Cerrado Protected Areas: Chapada dos Veadeiros and Natural Emas National Parks 8 EURNA Bulgaria Pirin National Park Natural 9 AFR Cameroon Dja Faunal Reserve Natural 10 EURNA Canada Gros Morne National Park Natural 11 AFR Central African Republic Manovo-Gounda St Floris National Park Natural World Heritage in Danger 12 LAC Costa Rica / Panama Talamanca Range-La Amistad Reserves / La Amistad Natural National Park 13 AFR Côte d'Ivoire Comoé National Park Natural World Heritage in Danger 14 AFR Côte d'Ivoire / Guinea Mount Nimba Strict Nature Reserve Natural World Heritage in Danger 15 AFR Democratic Republic of the Congo Garamba National Park Natural World Heritage in Danger 16 AFR Democratic Republic of the Congo Kahuzi-Biega National Park Natural World Heritage in Danger 17 AFR Democratic Republic of the Congo Okapi Wildlife Reserve Natural World Heritage in Danger 18 AFR Democratic Republic of the Congo Salonga National Park Natural World Heritage in Danger 19 AFR Democratic Republic of the Congo Virunga National Park Natural World Heritage in Danger 20 AFR Democratic -
Alaska Interagency Operating Plan for Volcanic Ash Episodes
Alaska Interagency Operating Plan for Volcanic Ash Episodes MAY 1, 2008 Cover: A plume of volcanic gas and water vapor rises above the summit crater and growing lava dome at Augustine Volcano in southern Cook Inlet. A mantle of light brown ash discolors the snow on the upper flanks. View is towards the southwest. Photograph taken by C. Read, U.S. Geological Survey, January 24, 2006. Alaska Volcano Observatory database image from http://www.avo.alaska.edu/image.php?id=7051. Alaska Interagency Operating Plan for Volcanic Ash Episodes May 1, 2008 Table of Contents 1.0 Introduction ............................................................................................................... 3 1.1 Integrated Response to Volcanic Ash ....................................................................... 3 1.2 Data Collection and Processing ................................................................................ 4 1.3 Information Management and Coordination .............................................................. 4 1.4 Distribution and Dissemination.................................................................................. 5 2.0 Responsibilities of the Participating Agencies ........................................................... 5 2.1 ALASKA DIVISION OF HOMELAND SECURITY AND EMERGENCY MANAGEMENT (DHS&EM) .............................................................................. 5 2.2 ALASKA VOLCANO OBSERVATORY (AVO)........................................................... 6 2.2.1 Organization..................................................................................................... -
Pskov from Wikipedia, the Free Encyclopedia Coordinates: 57°49′N 28°20′E
Create account Log in Article Talk Read Edit View history Pskov From Wikipedia, the free encyclopedia Coordinates: 57°49′N 28°20′E Pskov (Russian: Псков; IPA: [pskof] ( listen), ancient Russian spelling "Плѣсковъ", Pleskov) is Navigation Pskov (English) a city and the administrative center of Pskov Oblast, Russia, located about 20 kilometers Псков (Russian) Main page (12 mi) east from the Estonian border, on the Velikaya River. Population: 203,279 (2010 [1] Contents Census);[3] 202,780 (2002 Census);[5] 203,789 (1989 Census).[6] - City - Featured content Current events Contents Random article 1 History Donate to Wikipedia 1.1 Early history 1.2 Pskov Republic 1.3 Modern history Interaction 2 Administrative and municipal status Help 3 Landmarks and sights About Wikipedia 4 Climate Community portal 5 Economy Recent changes 6 Notable people Krom (or Kremlin) in Pskov Contact Wikipedia 7 International relations 7.1 Twin towns and sister cities Toolbox 8 References 8.1 Notes What links here 8.2 Sources Related changes 9 External links Upload file Special pages History [edit] Location of Pskov Oblast in Russia Permanent link Page information Data item Early history [edit] Cite this page The name of the city, originally spelled "Pleskov", may be loosely translated as "[the town] of purling waters". Its earliest mention comes in 903, which records that Igor of Kiev married a [citation needed] Print/export local lady, St. Olga. Pskovians sometimes take this year as the city's foundation date, and in 2003 a great jubilee took place to celebrate Pskov's 1,100th anniversary. Create a book Pskov The first prince of Pskov was Vladimir the Great's younger son Sudislav. -
Volcanic Arc of Kamchatka: a Province with High-␦18O Magma Sources and Large-Scale 18O/16O Depletion of the Upper Crust
Geochimica et Cosmochimica Acta, Vol. 68, No. 4, pp. 841–865, 2004 Copyright © 2004 Elsevier Ltd Pergamon Printed in the USA. All rights reserved 0016-7037/04 $30.00 ϩ .00 doi:10.1016/j.gca.2003.07.009 Volcanic arc of Kamchatka: a province with high-␦18O magma sources and large-scale 18O/16O depletion of the upper crust 1, 2 3 1 ILYA N. BINDEMAN, *VERA V. PONOMAREVA, JOHN C. BAILEY, and JOHN W. VALLEY 1Department of Geology and Geophysics, University of Wisconsin, Madison, WI, USA 2Institute of Volcanic Geology and Geochemistry, Petropavlovsk-Kamchatsky, Russia 3Geologisk Institut, University of Copenhagen, Copenhagen, Denmark (Received March 20, 2003; accepted in revised form July 16, 2003) Abstract—We present the results of a regional study of oxygen and Sr-Nd-Pb isotopes of Pleistocene to Recent arc volcanism in the Kamchatka Peninsula and the Kuriles, with emphasis on the largest caldera- forming centers. The ␦18O values of phenocrysts, in combination with numerical crystallization modeling (MELTS) and experimental fractionation factors, are used to derive best estimates of primary values for ␦18O(magma). Magmatic ␦18O values span 3.5‰ and are correlated with whole-rock Sr-Nd-Pb isotopes and major elements. Our data show that Kamchatka is a region of isotopic diversity with high-␦18O basaltic magmas (sampling mantle to lower crustal high-␦18O sources), and low-␦18O silicic volcanism (sampling low-␦18O upper crust). Among one hundred Holocene and Late Pleistocene eruptive units from 23 volcanic centers, one half represents low-␦18O magmas (ϩ4 to 5‰). Most low-␦ 18O magmas are voluminous silicic ignimbrites related to large Ͼ10 km3 caldera-forming eruptions and subsequent intracaldera lavas and domes: Holocene multi-caldera Ksudach volcano, Karymsky and Kurile Lake-Iliinsky calderas, and Late Pleistocene Maly Semyachik, Akademy Nauk, and Uzon calderas. -
From Sacred Cow to Cash Cow Muller, Martin
From sacred cow to cash cow Muller, Martin License: Creative Commons: Attribution-NoDerivs (CC BY-ND) Document Version Publisher's PDF, also known as Version of record Citation for published version (Harvard): Müller, M 2014, 'From sacred cow to cash cow: the shifting political ecologies of protected areas in Russia', Zeitschrift für Wirtschaftsgeographie, vol. 58, no. 2-3, pp. 127-143. Link to publication on Research at Birmingham portal General rights Unless a licence is specified above, all rights (including copyright and moral rights) in this document are retained by the authors and/or the copyright holders. The express permission of the copyright holder must be obtained for any use of this material other than for purposes permitted by law. •Users may freely distribute the URL that is used to identify this publication. •Users may download and/or print one copy of the publication from the University of Birmingham research portal for the purpose of private study or non-commercial research. •User may use extracts from the document in line with the concept of ‘fair dealing’ under the Copyright, Designs and Patents Act 1988 (?) •Users may not further distribute the material nor use it for the purposes of commercial gain. Where a licence is displayed above, please note the terms and conditions of the licence govern your use of this document. When citing, please reference the published version. Take down policy While the University of Birmingham exercises care and attention in making items available there are rare occasions when an item has been uploaded in error or has been deemed to be commercially or otherwise sensitive. -
Weathering of Volcanic Ash in the Cryogenic Zone of Kamchatka, Eastern Russia
Clay Minerals, (2014) 49, 195–212 OPEN ACCESS Weathering of volcanic ash in the cryogenic zone of Kamchatka, eastern Russia 1, 2 E. KUZNETSOVA * AND R. MOTENKO 1 SINTEF Building and Infrastructure, Trondheim, NO-7465, Norway, and 2 Lomonosov Moscow State University, Moscow, 119991, Russia (Received 8 August 2012; revised 28 August 2013; Editor: Harry Shaw) ABSTRACT: The nature of the alteration of basaltic, andesitic and rhyolitic glass of Holocene and Pleistocene age and their physical and chemical environments have been investigated in the ash layers within the cryogenic soils associated with the volcanoes in the central depression of Kamchatka. One of the main factors controlling the alteration of the volcanic glass is their initial chemistry with those of andesitic (SiO2 =53À65 wt.%) and basaltic (SiO2 < 53 wt.%) compositions being characterized by the presence of allophane, whereas volcanic glass of rhyolitic composition (SiO2>65 wt.%) are characterized by opal. Variations in the age of eruption of individual ashes, the amount and nature of the soil water, the depth of the active annual freeze-thawing layer, the thermal conductivity of the weathering soils, do not play a controlling role in the type of weathering products of the ashes but may affect their rates of alteration. KEYWORDS: volcanic ash, allophane, opal, unfrozen water, thermal conductivity, permafrost, Kamchatka. The highly active volcanic area of Kamchatka in local and remote eruptions and from the secondary eastern Russia is part of the circum-Pacific belt of re-deposition of ash (Bazanova et al., 2005). andesitic volcanism. It is situated north of the 49th Considerable research has been carried out on the parallel of latitude and is characterized by a weathering of volcanic glass. -
Peace in Palestine Via the World Heritage Convention
. Michael K. Madison II. Peace in Palestine ..........through World Heritage Promoting Peace via Global Conventions - 1 - Peace in Palestine via the World Heritage Convention Promoting Peace via Global Conventions The Global Problem "Throughout history, religious differences have divided men and women from their neighbors and have served as justification for some of humankind's bloodiest conflicts. In the modern world, it has become clear that people of all religions must bridge these differences and work together, to ensure our survival and realize the vision of peace that all faiths share." -- H.R.H. Prince El-Hassan bin Talal, Jordan Moderator, WCRP Governing Board Tolerance, Economic Growth and Fear Global peace and harmony is not possible without religious tolerance. Unfortunately, there is no instant microwavable solution. We can’t just add water and/or milk to the current situation and hope that the world will ameliorate itself overnight. No. The world needs help. The problem is not the outliers; it is larger groups of people that need to change. Outliers will always be present. The world needs religious-minded policymakers to take giant steps that lead to peace, but in a mutually beneficial way. Indeed, peace for peace’s sake is not always enough incentive to all parties involved. Therefore, if the conflict cannot be resolved by tolerance, then let it be resolved by greed as we find a way to help the countries involved to achieve a better economic position. If the conflict cannot be resolved by boosting the corresponding economies, then let it be resolved by fear as we convince the nations involved that one false move means it will be - 2 - their country against the rest of the world and not just their “enemy of the day”. -
2005 Volcanic Activity in Alaska, Kamchatka, and the Kurile Islands: Summary of Events and Response of the Alaska Volcano Observatory
The Alaska Volcano Observatory is a cooperative program of the U.S. Geological Survey, University of Alaska Fairbanks Geophysical Institute, and the Alaska Division of Geological and Geophysical Surveys . The Alaska Volcano Observtory is funded by the U.S. Geological Survey Volcano Hazards Program and the State of Alaska. 2005 Volcanic Activity in Alaska, Kamchatka, and the Kurile Islands: Summary of Events and Response of the Alaska Volcano Observatory Scientific Investigations Report 2007–5269 U.S. Department of the Interior U.S. Geological Survey Cover: Southeast flank of Augustine Volcano showing summit steaming, superheated fumarole jet, and ash dusting on snow. View is toward the northwest with Iniskin Bay in the distance. Photograph taken by Chris Waythomas, AVO/USGS, December 20, 2005. 2005 Volcanic Activity in Alaska, Kamchatka, and the Kurile Islands: Summary of Events and Response of the Alaska Volcano Observatory By R.G. McGimsey, C.A. Neal, J.P. Dixon, U.S. Geological Survey, and Sergey Ushakov, Institute of Volcanology and Seismology The Alaska Volcano Observatory is a cooperative program of the U.S. Geological Survey, University of Alaska Fairbanks Geophysical Institute, and the Alaska Division of Geological and Geophuysical Surveys. The Alaska Volcano Observatory is funded by the U.S. Geological Survey Volcano Hazards Program and the State of Alaska. Scientific Investigations Report 2007–5269 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. -
Учреждение Российской Академии Наук Геологический Институт РАН Geological Institute of the Russian Academy of Sciences
Учреждение Российской Академии наук Геологический институт РАН Geological Institute of the Russian Academy of Sciences Университет Тохоку, Япония Tohoku University, Japan Университет Хиросимы, Япония Hiroshima University, Japan Тезисы совместного российско-японского рабочего совещания «Офиолиты и связанные с ними комплексы: значение для геодинамических интерпретаций» 15-16 июня 2010 г. Abstracts of the Russian – Japanese workshop symposium "Ophiolites and related complexes: significance for geodynamic interpretations" June 15-16, 2010 Совещание проводится в рамках совместного российско-японского проекта (№ 09-05-92103) Российского фонда фундаментальных исследований (РФФИ) и Японского Общества Продвижения науки (JSPS) The workshop is held within the scope of the joint Russian-Japanese project (No 09-05-92103) of the Russian Foundation for Basic Research and Japanese Society for Promotion of Science Москва-2010 Moscow -2010 PROGRAM - ПРОГРАММА Day 1: June 15, 2010 10-00 – 10-30 Ishiwatari A.*, Machi S.**, Hayasaka Y.***, Ledneva G.V.****, Sokolov S.D.****, Palandzhyan S.A.****, Bazylev B.A.***** Paleozoic ophiolitic complexes in Northeast Russia: Evidence for opening of the Paleo-Pacific ocean? (*Tohoku University, Japan; **Kanazawa University, Japan; ***Hiroshima University, Japan; ****Geological Institute RAS, Moscow Russia; *****Vernadsky Institute RAS, Moscow, Russia) 10-30 – 11-00 Palandzhyan S.A. On principles of defining ophiolites (Geological Institute RAS, Moscow, Russia) 11-00 – 11-30 Silantyev S. Oceanic Core Complex as a key -
The Active Volcanoes of Kamchatka and Paramushir Island, North Kurils in 2007 O
ISSN 0742-0463, Journal of Volcanology and Seismology, 2009, Vol. 3, No. 1, pp. 1–17. © Pleiades Publishing, Ltd., 2009. Original Russian Text © O.A. Girina, S.V. Ushakov, N.A. Malik, A.G. Manevich, D.V. Mel’nikov, A.A. Nuzhdaev, Yu.V. Demyanchuk, L.V. Kotenko, 2009, published in Vul- kanologiya i Seismologiya, 2009, No. 1, pp. 3–20. The Active Volcanoes of Kamchatka and Paramushir Island, North Kurils in 2007 O. A. Girina, S. V. Ushakov, N. A. Malik, A. G. Manevich, D. V. Mel’nikov, A. A. Nuzhdaev, Yu. V. Demyanchuk, and L. V. Kotenko Institute of Volcanology and Seismology of the Far East Division of the Russian Academy of Sciences, 9 Piipa Boulevard, Petropavlovsk-Kamchatskii, 683006 Russia Received March 6, 2008 Abstract—Eight strong eruptions of four Kamchatka volcanoes (Bezymyannyi, Klyuchevskoi, Shiveluch, and Karymskii) and Chikurachki Volcano on Paramushir Island, North Kurils took place in 2007. In addition, an explosive event occurred on Mutnovskii Volcano and increased fumarole activity was recorded on Avacha and Gorelyi volcanoes in Kamchatka and Ebeko Volcano on Paramushir Island, North Kurils. Thanks to close coop- eration with colleagues involved in the Kamchatkan Volcanic Eruption Response Team (KVERT) project from the Elizovo Airport Meteorological Center and volcanic ash advisory centers in Tokyo, Anchorage, and Wash- ington (Tokyo VAAC, Anchorage VAAC, and Washington VAAC), all necessary precautions were taken for flight safety near Kamchatka. DOI: 10.1134/S0742046309010011 INTRODUCTION two months in 2005–2006 the volcano remained rela- tively quiet, up to December 4, 2006. The extrusive– The comprehensive monitoring of active volcanoes explosive eruption of Molodoi (Young) Shiveluch Vol- in Kamchatka and North Kurils is carried out under the cano commenced on that date, with a strong ash ejec- KVERT project [2, 4, 5] in close cooperation with col- tion, and continued during all of 2007. -
Priority Pass Lounge Directory
Content correct as of 24 September 2021 Priority Pass™ Lounge Directory This PDF Lounge Directory details all the lounges in the Priority Pass program – more than 1200 in total, covering over 400 airports around the world. Priority Pass is the world's leading independent lounge program, making membership a must for any frequent traveler. As a Priority Pass member, wherever you travel, you can be sure that you'll experience outstanding standards of comfort and service – a world away from chaotic airport terminals. Do some business. Catch up with calls. Send a few emails. Browse through a favorite magazine. Enjoy refreshments of your choice. Or simply indulge yourself by doing nothing at all. You can use the Priority Pass lounges as detailed in this directory, regardless of your choice of airline, class of ticket or membership in any frequent flyer club. Just be sure to take your Priority Pass membership card with you wherever you travel in order to gain access to participating lounges. Enjoy your visit! For the most up-to-date lounge information and full Priority Pass Conditions of Use, visit our website at prioritypass.com © Priority Pass Ltd 2021. Opening times and availability of facilities may be subject to change. Admittance to the lounges is conditional upon presentation of a valid Priority Pass card only. Page 2 of 473 Content correct as of 24 September 2021 Facility Symbols Air Conditioning Conference Facilities Digital Membership Card Digital Membership Card Unavailable Disabled Access Fax Flight Information Monitor Internet/Dataport Newspapers/Magazines Refreshments (Alcoholic) Refreshments (Soft Drinks) Shower Facilities Telephone Television Wi-fi © Priority Pass Ltd 2021. -
EVENT PASSPORT of the REGION KAMCHATKA Portrait of the Region: a Few Facts
Kamchatka and salmon caviar are virtually inseparable. This gourmet product has long become the brand of the region, along with volcanoes and geysers. The Geyser Valley on Kamchatka is one of the largest in the whole world. It was recognized by nationwide vote as one of the seven wonders of Russia. EVENT PASSPORT OF THE REGION KAMCHATKA Portrait of the Region: A Few Facts Kamchatka is the most remote region from the central part of the country, the area with pristine nature and a very small population. This is the land of volcanoes, geysers and bears. The natural volcano landscape in Kamchatka was included in the UNESCO World Heritage List. FISHING SHOP KAMCHATKA EXHIBITION OF RUSSIA AND INVESTMENT CENTER The fishing industry is the main ● Area: exhibition and congress halls: Largest events link in the economic structure of 600 and 400 m2. at the venue: Kamchatka Krai. In addition to fishing, processing fish, studying fish and fish ● Number of venues: 2 exhibition farming sectors, the local economy and congress halls, a conference ● Kamchatka Forum of Entrepre- includes a number of auxiliary and hall: 80 sq. m, seating 70 people, neurs (November 26–28, 2018). service sectors, as well as institutions 2 meeting rooms. of manufacturing and social ● Total capacity of two halls and ● Architectural exposition, exhibition infrastructure. The most important meeting rooms: up to 500 people. “Your Home 2018.” of those are ship repair, construction, transport, storage and transshipment ● Distance to the city’s historic ● Kamchatka Business Strategy and of fish products. downtown area: 11 km. Management Cup. LEADING ECONOMY SECTORS Fishing Minerals and Energy Tourism Agriculture and fish other natural farming Resources PLANNING BRIGHTEST WEATHER IN A VISIT IMPRESSIONS PETROPAVLOVSK- Visit the unique Kronotsky Nature KAMCHATSKY Accessibility Reserve—the caldera of Uzon Volcano and one of seven wonders of Russia, Elizovo Airport is the main arrival the Valley of Geysers.