Preservation and Transformation of Certain Aspects of the Traditional
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Second Report Submitted by the Russian Federation Pursuant to The
ACFC/SR/II(2005)003 SECOND REPORT SUBMITTED BY THE RUSSIAN FEDERATION PURSUANT TO ARTICLE 25, PARAGRAPH 2 OF THE FRAMEWORK CONVENTION FOR THE PROTECTION OF NATIONAL MINORITIES (Received on 26 April 2005) MINISTRY OF REGIONAL DEVELOPMENT OF THE RUSSIAN FEDERATION REPORT OF THE RUSSIAN FEDERATION ON THE IMPLEMENTATION OF PROVISIONS OF THE FRAMEWORK CONVENTION FOR THE PROTECTION OF NATIONAL MINORITIES Report of the Russian Federation on the progress of the second cycle of monitoring in accordance with Article 25 of the Framework Convention for the Protection of National Minorities MOSCOW, 2005 2 Table of contents PREAMBLE ..............................................................................................................................4 1. Introduction........................................................................................................................4 2. The legislation of the Russian Federation for the protection of national minorities rights5 3. Major lines of implementation of the law of the Russian Federation and the Framework Convention for the Protection of National Minorities .............................................................15 3.1. National territorial subdivisions...................................................................................15 3.2 Public associations – national cultural autonomies and national public organizations17 3.3 National minorities in the system of federal government............................................18 3.4 Development of Ethnic Communities’ National -
Siberia, the Wandering Northern Terrane, and Its Changing Geography Through the Palaeozoic ⁎ L
Earth-Science Reviews 82 (2007) 29–74 www.elsevier.com/locate/earscirev Siberia, the wandering northern terrane, and its changing geography through the Palaeozoic ⁎ L. Robin M. Cocks a, , Trond H. Torsvik b,c,d a Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK b Center for Geodynamics, Geological Survey of Norway, Leiv Eirikssons vei 39, Trondheim, N-7401, Norway c Institute for Petroleum Technology and Applied Geophysics, Norwegian University of Science and Technology, N-7491 NTNU, Norway d School of Geosciences, Private Bag 3, University of the Witwatersrand, WITS, 2050, South Africa Received 27 March 2006; accepted 5 February 2007 Available online 15 February 2007 Abstract The old terrane of Siberia occupied a very substantial area in the centre of today's political Siberia and also adjacent areas of Mongolia, eastern Kazakhstan, and northwestern China. Siberia's location within the Early Neoproterozoic Rodinia Superterrane is contentious (since few if any reliable palaeomagnetic data exist between about 1.0 Ga and 540 Ma), but Siberia probably became independent during the breakup of Rodinia soon after 800 Ma and continued to be so until very near the end of the Palaeozoic, when it became an integral part of the Pangea Supercontinent. The boundaries of the cratonic core of the Siberian Terrane (including the Patom area) are briefly described, together with summaries of some of the geologically complex surrounding areas, and it is concluded that all of the Palaeozoic underlying the West Siberian -
Ukrainians in Russia: a Bibliographic and Statistical Guide
Research Report No. 55 Ukrainians in Russia: A Bibliographic and Statistical Guide Compiled by Serge Cipko Canadian Institute of Ukrainian Studies Press University of Alberta Edmonton 1994 Canadian Institute of Ukrainian Studies Press Occasional Research Reports The Institute publishes research reports periodically. Copies may be ordered from the Canadian Institute of Ukrainian Studies Press, 352 Athabasca Hall, University of Alberta, Edmonton, Alberta, Canada T6G 2E8. The name of the publication series and the substantive material in each issue (unless otherwise noted) are copyrighted by the Canadian Institute of Ukrainian Studies Press. PRINTED IN CANADA Occasional Research Reports Ukrainians in Russia: A Bibliographic and Statistical Guide Compiled by Serge Cipko Research Report No. 55 Canadian Institute of Ukrainian Studies Press University of Alberta Edmonton 1994 Digitized by the Internet Archive in 2016 https://archive.org/details/ukrainiansinruss55cipk Table of Contents Introduction 1 A Select Bibliography 3 Newspaper Articles 9 Ukrainian Periodicals and Journals Published in Russia 15 Periodicals Published Abroad by Ukrainians from Russia 18 Biographies of Ukrainians in Russia 21 Biographies of Ukrainians from Russia Resettled Abroad 31 Statistical Compendium of Ukrainians in Russia 33 Addresses of Ukrainian Organizations in Russia 39 Periodicals and Journals Consulted 42 INTRODUCTION Ukrainians who live in countries bordering on Ukraine constitute perhaps the second largest ethnic minority in Europe after the Russians. Despite their significant numbers, however, these Ukrainians remain largely unknown to the international community, receiving none of the attention that has been accorded, for example, to Russian minorities in the successor states to the former Soviet Union. According to the last Soviet census of 1989, approximately 4.3 million Ukrainians live in the Russian Federation; unofficial estimates of the size of this group run considerably higher. -
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Arctic and North. 2018. No. 33 55 UDC [332.1+338.1](985)(045) DOI: 10.17238/issn2221-2698.2018.33.66 The prospects of the Northern and Arctic territories and their development within the Yenisei Siberia megaproject © Nikolay G. SHISHATSKY, Cand. Sci. (Econ.) E-mail: [email protected] Institute of Economy and Industrial Engineering of the Siberian Department of the Russian Academy of Sci- ences, Kransnoyarsk, Russia Abstract. The article considers the main prerequisites and the directions of development of Northern and Arctic areas of the Krasnoyarsk Krai based on creation of reliable local transport and power infrastructure and formation of hi-tech and competitive territorial clusters. We examine both the current (new large min- ing and processing works in the Norilsk industrial region; development of Ust-Eniseysky group of oil and gas fields; gasification of the Krasnoyarsk agglomeration with the resources of bradenhead gas of Evenkia; ren- ovation of housing and public utilities of the Norilsk agglomeration; development of the Arctic and north- ern tourism and others), and earlier considered, but rejected, projects (construction of a large hydroelectric power station on the Nizhnyaya Tunguska river; development of the Porozhinsky manganese field; place- ment of the metallurgical enterprises using the Norilsk ores near Lower Angara region; construction of the meridional Yenisei railroad and others) and their impact on the development of the region. It is shown that in new conditions it is expedient to return to consideration of these projects with the use of modern tech- nologies and organizational approaches. It means, above all, formation of the local integrated regional pro- duction systems and networks providing interaction and cooperation of the fuel and raw, processing and innovative sectors. -
West Siberian Plain As a Late Glacial Desert
Quaternary International 237 (2011) 45e53 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint West Siberian Plain as a late glacial desert A.A. Velichko a,*, S.N. Timireva a, K.V. Kremenetski b, G.M. MacDonald b, L.C. Smith b a Institute of Geography, Russian Academy of Sciences, Staromonetny, 29, Moscow 109027, Russia b University of California, Los Angeles, CA 90095-1524, USA article info abstract Article history: The paper presents results of morphoscopic studies of quartz grains recovered from sands underlying Available online 18 January 2011 surficial peat over the West Siberian Plain. The field materials were collected in the course of the RussianeAmerican expedition in 1999e2001. The data obtained proved the existence of a vast area in West Siberia similar to cold deserts in appearance at the late glacial time (and probably even as early as the Last Glacial Maximum e 18e20 ka BP). The desert was confined to the arctic and temperate belts, the southernmost part of the plain being an area of loess accumulation. Ó 2011 Elsevier Ltd and INQUA. All rights reserved. 1. Introduction northern and central regions; sands are found not only in fluvial (terrace) sequences, but also on higher levels including the main At the present stage of the geosphere evolution, West Siberia is divide, the ridge of Siberian Uvals. As the sands occur at the base of the largest area of wetlands (including bogs, marshes and peatlands peats, it was of particular interest to study more fully their genetic in the Northern Hemisphere, just as Amazonia is in the Southern properties, to reconstruct environments at the time immediately Hemisphere). -
Siberia╎s First Nations
TITLE: SIBERIA'S FIRST NATIONS AUTHOR: GAIL A. FONDAHL, University of Northern British Columbia THE NATIONAL COUNCIL FOR SOVIET AND EAST EUROPEAN RESEARCH TITLE VIII PROGRAM 1755 Massachusetts Avenue, N.W. Washington, D.C. 20036 PROJECT INFORMATION:1 CONTRACTOR: Dartmouth College PRINCIPAL INVESTIGATOR: Gail A. Fondahl COUNCIL CONTRACT NUMBER: 808-28 DATE: March 29, 1995 COPYRIGHT INFORMATION Individual researchers retain the copyright on work products derived from research funded by Council Contract. The Council and the U.S. Government have the right to duplicate written reports and other materials submitted under Council Contract and to distribute such copies within the Council and U.S. Government for their own use, and to draw upon such reports and materials for their own studies; but the Council and U.S. Government do not have the right to distribute, or make such reports and materials available, outside the Council or U.S. Government without the written consent of the authors, except as may be required under the provisions of the Freedom of Information Act 5 U.S.C. 552, or other applicable law. 1 The work leading to this report was supported in part by contract funds provided by the National Council for Soviet and East European Research, made available by the U. S. Department of State under Title VIII (the Soviet-Eastern European Research and Training Act of 1983, as amended). The analysis and interpretations contained in the report are those of the author(s). CONTENTS Executive Summary i Siberia's First Nations 1 The Peoples of the -
Chronology of Stalin's Life
Chronology of Stalin's Life ('Old Style' to February 1918) 1879 9 Dec Born in Gori. 1888 Sept Enters clerical elementary school in Gori. 1894 Sept Enters theological seminary in Tbilisi. 1899 May Expelled from seminary. 1900 Apr Addresses worker demonstration near Tbilisi. 1902 Apr Arrested in Batumi following worker demonstration of which he was an organizer. 1903 July-Aug Appearance of Lenin's Bolshevik faction at the Second Congress of the Russian Social-Democratic Workers' Party (Stalin not present). 1904 Jan Escapes from place of exile in Siberia and returns to underground revolutionary work in Transcaucasia. 1905 Revolution, reaching peak in Oct-Dec. threatens the survival of the tsarist government. Stalin marries Ekaterina Svanidze. Dec Attends Bolshevik conference. also attended by Lenin, in Tammerfors, Finland. 1906 Apr Attends 'Unity' congress of party in Stockholm. 1907 Mar Birth of first child, Yakov. Apr Publishes first substantial piece of writing, 'Anarchism or Socialism?' Apr-May Attends party congress in London. Jun Moves operations to Baku. Oct Death of his wife, Ekaterina. 1908 Mar Arrested in Baku. 317 318 Chronology of Stalin's Life 1909 June Escapes from place of exile, Solvychegodsk, returns to underground in Baku. 1910 Mar Arrested and jailed. Oct Returned to exile in Solvychegodsk. 1911 June Police permit his legal residence in Vologda. Sept Illegally goes to St Petersburg but is arrested and returned to Vologda. 1912 Jan Bolshevik conference in Prague at which Lenin attempts to establish his control of party; Stalin not present but soon after is co-opted to new Central Committee. Apr Illegally moves to St Petersburg, but is arrested there. -
Defining Territories and Empires: from Mongol Ulus to Russian Siberia1200-1800 Stephen Kotkin
Defining Territories and Empires: from Mongol Ulus to Russian Siberia1200-1800 Stephen Kotkin (Princeton University) Copyright (c) 1996 by the Slavic Research Center All rights reserved. The Russian empire's eventual displacement of the thirteenth-century Mongol ulus in Eurasia seems self-evident. The overthrow of the foreign yoke, defeat of various khanates, and conquest of Siberia constitute core aspects of the narratives on the formation of Russia's identity and political institutions. To those who disavow the Mongol influence, the Byzantine tradition serves as a counterweight. But the geopolitical turnabout is not a matter of dispute. Where Chingis Khan and his many descendants once held sway, the Riurikids (succeeded by the Romanovs) moved in. *1 Rather than the shortlived but ramified Mongol hegemony, which was mostly limited to the middle and southern parts of Eurasia, longterm overviews of the lands that became known as Siberia, or of its various subregions, typically begin with a chapter on "pre-history," which extends from the paleolithic to the moment of Russian arrival in the late sixteenth, early seventeenth centuries. *2 The goal is usually to enable the reader to understand what "human material" the Russians found and what "progress" was then achieved. Inherent in the narratives -- however sympathetic they may or may not be to the native peoples -- are assumptions about the historical advance deriving from the Russian arrival and socio-economic transformation. In short, the narratives are involved in legitimating Russia's conquest without any notion of alternatives. Of course, history can also be used to show that what seems natural did not exist forever but came into being; to reveal that there were other modes of existence, which were either pushed aside or folded into what then came to seem irreversible. -
Flux of Nutrients from Russian Rivers to the Arctic Ocean: Can We Establish a Baseline Against Which to Judge Future Changes? R
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by UNH Scholars' Repository University of New Hampshire University of New Hampshire Scholars' Repository Faculty Publications 8-1-2000 Flux of nutrients from Russian rivers to the Arctic Ocean: Can we establish a baseline against which to judge future changes? R. M. Holmes B. J. Peterson V. V. Gordeev A. V. Zhulidov M. Meybeck Université de Paris See next page for additional authors Follow this and additional works at: https://scholars.unh.edu/faculty_pubs Recommended Citation Holmes, R.M., B.J. Peterson, V.V. Gordeev, A.V. Zhulidov, M. Meybeck, R.B. Lammers, and C.J. Vorosmarty (2000) Flux of nutrients from Russian rivers to the Arctic Ocean: Can we establish a baseline against which to judge future changes? Water Resources Research, 36:2309-2320. This Article is brought to you for free and open access by University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Faculty Publications by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. Authors R. M. Holmes, B. J. Peterson, V. V. Gordeev, A. V. Zhulidov, M. Meybeck, Richard B. Lammers, and Charles J. Vorosmarty This article is available at University of New Hampshire Scholars' Repository: https://scholars.unh.edu/faculty_pubs/150 WATER RESOURCES RESEARCH, VOL. 36, NO. 8, PAGES 2309-2320, AUGUST 2000 Flux of nutrients from Russian rivers to the Arctic Ocean: Can we establish a baseline against which to judge future changes? R. -
Last Ned Publikasjon
NGU Report 2007.056 New insights into the West Siberian Basin from the satellite mission GRACE Geological Survey of Norway NO-7491 Trondheim, Norway Tel.: 47 73 90 40 11 REPORT Telefax 47 73 92 16 20 Report no.: 2007.056 ISSN 0800-3416 Grading: Confidential to 31.12.2009 Title: New insights into the West Siberian Basin from the satellite mission GRACE Authors: Client: Carla Braitenberg & Jörg Ebbing Statoil ASA County: Commune: Map-sheet name (M=1:250.000) Number of pages: 64 Price (NOK): Map enclosures: Fieldwork carried out: Date of report: Project no.: Person responsible: 31.08.2007 3133.00 Summary: The West Siberian Basin covers an area of ~3.2 x106 km2 and is among the most extended basins in the world. Recent investigations have revealed that the basin contains an extensive layer of flood basalts of late Permian-Triassic age, which have been set into relation to the basalts of the Siberian traps. In the northern parts of the basin, the basalts overly older sediments that reach locally over 15 km in thickness. Our work aims at reducing the observed gravity field to the basement level, estimating the contribution of the sediments and of the basalt layer to the gravity field. Published seismic sections with well-calibration are used for constraining the sediment isopachs and for estimating the density-depth functions. We also make use of published models on crustal thickness and basement depth and the gravity field derived from the integration of the satellite mission GRACE with terrestrial gravity measurements. The resulting 3D-density model is used for inferring density anomalies in the lower crust and upper mantle and allows calculating the total load acting on the crust and estimating the isostatic state of the region. -
Number and Distribution of Gyrfalcons on the West Siberian Plain. Pages 267–272 in R
NUMBER AND DISTRIBUTION OF GYRFALCONS ON THE WEST SIBERIAN PLAIN IRINA POKROVSKAYA AND GRIGORY TERTITSKI Institute of Geography, Russian Academy of Sciences, 29 Staromonetny per., Moscow, 119017, Russia. E-mail: [email protected] ABSTRACT.—Using our own observations and published records, we discuss the breeding range, number, and distribution of Gyrfalcons (Falco rusticolus) on the West Siberian plain. We show that the currently accepted assessment of Gyrfalcon numbers appears to be underestimated. The southern limit of the species’ breeding range should be defined south of forest-tundra. With the predicted northward expansion of forest due to climate change, West Siberian and neighboring Gyrfalcons of subspecies F. r. intermedius appear preadapted to such habitat and may be favored by its expansion. These considerations call for increased efforts to survey the region for the pres- ence of nesting Gyrfalcons. Received 22 March 2011, accepted 23 May 2011. POKROVSKAYA, I., AND G. TERTITSKI. 2011. Number and distribution of Gyrfalcons on the West Siberian Plain. Pages 267–272 in R. T. Watson, T. J. Cade, M. Fuller, G. Hunt, and E. Potapov (Eds.). Gyrfalcons and Ptarmigan in a Changing World, Volume II. The Peregrine Fund, Boise, Idaho, USA. http://dx.doi.org/ 10.4080/gpcw.2011.0305 Key words: Gyrfalcon, West Siberian Plain, breeding range, forest-tundra, taiga. FOR EFFECTIVE INTERNATIONAL MANAGEMENT Plain. Approximately 25–50 breeding pairs OF GYRFALCONS (FALCO RUSTICOLUS), an accu- nest there in forest-tundra habitat in a study rate estimate of the abundance and distribution area of 28,000 km2 (Figure 1, site 1). This is of the species in Russia is important because the highest reported density of Gyrfalcons in Russia contains the largest part of the species’ the world at about 12.2 pairs per 1,000 km2 world range. -
Indigenous Peoples in the Russian Federation
INDIGENOUS PEOPLES IN THE RUSSIAN FEDERATION INDIGENOUS PEOPLES IN THE RUSSIAN FEDERATION Johannes Rohr Report 18 IWGIA – 2014 INDIGENOUS PEOPLES IN THE RUSSIAN FEDERATION Copyright: IWGIA Author: Johannes Rohr Editor: Diana Vinding and Kathrin Wessendorf Proofreading: Elaine Bolton Cover design and layout: Jorge Monrás Cover photo: Sakhalin: Indigenous ceremony opposite to oil facilities. Photographer: Wolfgang Blümel Prepress and print: Electronic copy only Hurridocs Cip data Title: IWGIA Report 18: Indigenous Peoples in the Russian Federation Author: Johannes Rohr Editor: Diana Vinding and Kathrin Wessendorf Number of pages: 69 ISBN: 978-87-92786-49-4 Language: English Index: 1. Indigenous peoples – 2. Human rights Geographical area: Russian Federation Date of publication: 2014 INTERNATIONAL WORK GROUP FOR INDIGENOUS AFFAIRS Classensgade 11 E, DK 2100 - Copenhagen, Denmark Tel: (45) 35 27 05 00 - Fax: (45) 35 27 05 07 E-mail: [email protected] - Web: www.iwgia.org This report has been prepared and published with the financial support of the Foreign Ministry of Denmark through its Neighbourhood programme. CONTENTS Introduction................................................................................................................................................................. 8 1 The indigenous peoples of the north ................................................................................................................... 9 1.1 Matters of definition .........................................................................................................................................