The Geography, Demography and Idstory of the Chukotka Autonomous District
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Title Post-Soviet Period Changes in Resource Utilization and Their
Post-Soviet Period Changes in Resource Utilization Title and Their Impact on Population Dynamics: Chukotka Autonomous Okrug Author(s) Litvinenko, Tamara Vitalyevna; Kumo, Kazuhiro Citation Issue Date 2017-08 Type Technical Report Text Version publisher URL http://hdl.handle.net/10086/28761 Right Hitotsubashi University Repository Center for Economic Institutions Working Paper Series No. 2017-3 “Post-Soviet Period Changes in Resource Utilization and Their Impact on Population Dynamics: Chukotka Autonomous Okrug” Tamara Vitalyevna Litvinenko and Kazuhiro Kumo August 2017 Center for Economic Institutions Working Paper Series Institute of Economic Research Hitotsubashi University 2-1 Naka, Kunitachi, Tokyo, 186-8603 JAPAN http://cei.ier.hit-u.ac.jp/English/index.html Tel:+81-42-580-8405/Fax:+81-42-580-8333 Post-Soviet Period Changes in Resource Utilization and Their Impact on Population Dynamics: Chukotka Autonomous Okrug Tamara Vitalyevna Litvinenko Institute of Geography, Russian Academy of Sciences Kazuhiro Kumo Institute of Economic Research, Hitotsubashi University, Japan Abstract This study examines changes that have occurred in the resource utilization sector and the impact of these changes on population dynamics in the Chukotka Autonomous Okrug during the post-Soviet period. This paper sheds light on the sorts of population-dynamics-related differences that have emerged in the region and how these differences relate to the use of natural resources and the ethnic composition of the population. Through this study, it was shown that changes have tended to be small in local areas where indigenous peoples who have engaged in traditional natural resource use for a large proportion of the population, while changes have been relatively large in areas where the proportion of non-indigenous people is high and the mining industry has developed. -
Russia and the Eurasian Republics THIS REGION Spans the Continents of Europe and Asia
390-391 U5 CH14 UO TWIP-860976 3/15/04 5:21 AM Page 390 Unit Workers on the statue Russians in front of Motherland Calls, St. Basil’s Cathedral, Volgograd Moscow 224 390-391 U5 CH14 UO TWIP-860976 3/15/04 5:22 AM Page 391 RussiaRussia andand the the EurasianEurasian f you had to describe Russia RepublicsRepublics Iin one word, that word would be BIG! Russia is the largest country in the world in area. Its almost 6.6 million square miles (17 million sq. km) are spread across two continents—Europe and Asia. As you can imagine, such a large country faces equally large challenges. In 1991 Russia emerged from the Soviet Union as an independent country. Since then it has been struggling to unite its many ethnic groups, set up a demo- cratic government, and build a stable economy. ▼ Siberian tiger in a forest NGS ONLINE in eastern Russia www.nationalgeographic.com/education 225 392-401 U5 CH14 RA TWIP-860976 3/15/04 5:28 AM Page 392 REGIONAL ATLAS Focus on: Russia and the Eurasian Republics THIS REGION spans the continents of Europe and Asia. It includes Russia—the world’s largest country—and the neigh- boring independent republics of Armenia, Georgia, Azerbaijan, Kazakhstan, Uzbekistan, Turkmenistan, Kyrgyzstan, and Tajikistan. Russia and the Eurasian republics cover about 8 million square miles (20.7 million sq. km). This is greater than the size of Canada, the United States, and Mexico combined. The Caspian Sea is actually a salt lake that lies at the base of the Caucasus Mountains in The Land Russia’s southwest. -
Summary Audit Report 2017
SUMMARY AUDIT REPORT for the August 2016 International Cyanide Management Code Recertification Audit Prepared for: Chukotka Mining and Geological Company Kinross Gold Corporation/ Kupol Project Submitted to: International Cyanide Management Institute 1400 I Street, NW, Suite 550 Washington, DC 20005, USA FINAL 26 April 2017 Ramboll Environ 605 1st Avenue, Suite 300 Seattle, Washington 98104 www.ramboll.com SUMMARY AUDIT REPORT Name of Mine: Kupol Mine Name of Mine Owner: Kinross Gold Corporation Name of Mine Operator: CJSC Chukotka Mining and Geological Company Name of Responsible Manager: Dave Neuburger, General Manager Address: CJSC Chukotka Mining and Geological Company Legal Address: Rultyegina Street, 2B Anadyr, Chukotka Autonomous Region Russia, 689000 Postal Address: 23 Parkovaya Street Magadan, Russia, 685000 Telephone: +7 (4132) 22-15-04 Fax: +7 (4132) 64-37-37 E-mail: [email protected] Location details and description of operation: The Kupol Mine is located in a remote north-central area of the Chukotka Autonomous Okrug (AO), Russian Federation. Majority ownership of the mine was acquired by Kinross Gold Corporation (Kinross) in 2008, and has been 100% owned since 2011. The mine is operated by a wholly-owned subsidiary, CJSC Chukotka Mining and Geological Company (CMGC). The Kupol deposit is presently mined using underground methods. Another underground operation has been developed at Dvoinoye, a site 100 km due north of Kupol. No separate milling or leaching operations are presently undertaken at Dvoinoye, and ore from this operation is being processed in the Kupol mill. In 2015, combined gold production from both mines was 758 563 ounces. The Kupol and Dvoinoye mine locations are shown in Figure 1. -
Conditional Probabilities for the Beaufort Sea Planning Area
OCS Report BOEM 2020-003 Oil Spill Risk Analysis: Conditional Probabilities for the Beaufort Sea Planning Area US Department of the Interior Bureau of Ocean Energy Management Headquarters This page intentionally left blank. OCS Report BOEM 2020-003 Oil Spill Risk Analysis: Conditional Probabilities for the Beaufort Sea Planning Area January 2020 Authors: Zhen Li Caryn Smith In-House Document by U.S. Department of the Interior Bureau of Ocean Energy Management Division of Environmental Sciences Sterling, VA US Department of the Interior Bureau of Ocean Energy Management Headquarters This page intentionally left blank. REPORT AVAILABILITY To download a PDF file of this report, go to the U.S. Department of the Interior, Bureau of Ocean Energy Management Oil Spill Risk Analysis web page (https://www.boem.gov/environment/environmental- assessment/oil-spill-risk-analysis-reports). CITATION Li Z, Smith C. 2020. Oil Spill Risk Analysis: Conditional Probabilities for the Beaufort Sea Planning Area. Sterling (VA): U.S. Department of the Interior, Bureau of Ocean Energy Management. OCS Report BOEM 2020-003. 130 p. ABOUT THE COVER This graphic depicts the study area in the Beaufort and Chukchi Seas and boundary segments used in the oil spill risk analysis model for the the Beaufort Sea Planning Area. Table of Contents Table of Contents ........................................................................................................................................... i List of Figures ............................................................................................................................................... -
Contemporary State of Glaciers in Chukotka and Kolyma Highlands ISSN 2080-7686
Bulletin of Geography. Physical Geography Series, No. 19 (2020): 5–18 http://dx.doi.org/10.2478/bgeo-2020-0006 Contemporary state of glaciers in Chukotka and Kolyma highlands ISSN 2080-7686 Maria Ananicheva* 1,a, Yury Kononov 1,b, Egor Belozerov2 1 Russian Academy of Science, Institute of Geography, Moscow, Russia 2 Lomonosov State University, Faculty of Geography, Moscow, Russia * Correspondence: Russian Academy of Science, Institute of Geography, Moscow, Russia. E-mail: [email protected] a https://orcid.org/0000-0002-6377-1852, b https://orcid.org/0000-0002-3117-5554 Abstract. The purpose of this work is to assess the main parameters of the Chukotka and Kolyma glaciers (small forms of glaciation, SFG): their size and volume, and changes therein over time. The point as to whether these SFG can be considered glaciers or are in transition into, for example, rock glaciers is also presented. SFG areas were defined from the early 1980s (data from the catalogue of the glaciers compiled by R.V. Sedov) to 2005, and up to 2017: these data were retrieved from sat- Key words: ellite images. The maximum of the SGF reduction occurred in the Chantalsky Range, Iskaten Range, Chukotka Peninsula, and in the northern part of Chukotka Peninsula. The smallest retreat by this time relates to the gla- Kolyma Highlands, ciers of the southern part of the peninsula. Glacier volumes are determined by the formula of S.A. satellite image, Nikitin for corrie glaciers, based on in-situ volume measurements, and by our own method: the av- climate change, erage glacier thickness is calculated from isogypsum patterns, constructed using DEMs of individu- glacier reduction, al glaciers based on images taken from a drone during field work, and using ArcticDEM for others. -
Federal Research Division Country Profile: Tajikistan, January 2007
Library of Congress – Federal Research Division Country Profile: Tajikistan, January 2007 COUNTRY PROFILE: TAJIKISTAN January 2007 COUNTRY Formal Name: Republic of Tajikistan (Jumhurii Tojikiston). Short Form: Tajikistan. Term for Citizen(s): Tajikistani(s). Capital: Dushanbe. Other Major Cities: Istravshan, Khujand, Kulob, and Qurghonteppa. Independence: The official date of independence is September 9, 1991, the date on which Tajikistan withdrew from the Soviet Union. Public Holidays: New Year’s Day (January 1), International Women’s Day (March 8), Navruz (Persian New Year, March 20, 21, or 22), International Labor Day (May 1), Victory Day (May 9), Independence Day (September 9), Constitution Day (November 6), and National Reconciliation Day (November 9). Flag: The flag features three horizontal stripes: a wide middle white stripe with narrower red (top) and green stripes. Centered in the white stripe is a golden crown topped by seven gold, five-pointed stars. The red is taken from the flag of the Soviet Union; the green represents agriculture and the white, cotton. The crown and stars represent the Click to Enlarge Image country’s sovereignty and the friendship of nationalities. HISTORICAL BACKGROUND Early History: Iranian peoples such as the Soghdians and the Bactrians are the ethnic forbears of the modern Tajiks. They have inhabited parts of Central Asia for at least 2,500 years, assimilating with Turkic and Mongol groups. Between the sixth and fourth centuries B.C., present-day Tajikistan was part of the Persian Achaemenian Empire, which was conquered by Alexander the Great in the fourth century B.C. After that conquest, Tajikistan was part of the Greco-Bactrian Kingdom, a successor state to Alexander’s empire. -
Helicobacter Pylori's Historical Journey Through Siberia and the Americas
Helicobacter pylori’s historical journey through Siberia and the Americas Yoshan Moodleya,1,2, Andrea Brunellib,1, Silvia Ghirottoc,1, Andrey Klyubind, Ayas S. Maadye, William Tynef, Zilia Y. Muñoz-Ramirezg, Zhemin Zhouf, Andrea Manicah, Bodo Linzi, and Mark Achtmanf aDepartment of Zoology, University of Venda, Thohoyandou 0950, Republic of South Africa; bDepartment of Life Sciences and Biotechnology, University of Ferrara, 44121 Ferrara, Italy; cDepartment of Mathematics and Computer Science, University of Ferrara, 44121 Ferrara, Italy; dDepartment of Molecular Biology and Genetics, Research Institute for Physical-Chemical Medicine, 119435 Moscow, Russia; eDepartment of Diagnostic and Operative Endoscopy, Pirogov National Medical and Surgical Center, 105203 Moscow, Russia; fWarwick Medical School, University of Warwick, Coventry CV4 7AL, United Kingdom; gLaboratorio de Bioinformática y Biotecnología Genómica, Escuela Nacional de Ciencias Biológicas, Unidad Profesional Lázaro Cárdenas, Instituto Politécnico Nacional, 11340 Mexico City, Mexico; hDepartment of Zoology, University of Cambridge, Cambridge CB2 3EJ, United Kingdom; and iDepartment of Biology, Division of Microbiology, Friedrich Alexander University Erlangen-Nuremberg, 91058 Erlangen, Germany Edited by Daniel Falush, University of Bath, Bath, United Kingdom, and accepted by Editorial Board Member W. F. Doolittle April 30, 2021 (received for review July 22, 2020) The gastric bacterium Helicobacter pylori shares a coevolutionary speakers). However, H. pylori’s presence, diversity, and structure history with humans that predates the out-of-Africa diaspora, and in northern Eurasia are still unknown. This vast region, hereafter the geographical specificities of H. pylori populations reflect mul- Siberia, extends from the Ural Mountains in the west to the tiple well-known human migrations. We extensively sampled H. -
Sources and Pathways 4.1
Chapter 4 Persistant toxic substances (PTS) sources and pathways 4.1. Introduction Chapter 4 4.1. Introduction 4.2. Assessment of distant sources: In general, the human environment is a combination Longrange atmospheric transport of the physical, chemical, biological, social and cultur- Due to the nature of atmospheric circulation, emission al factors that affect human health. It should be recog- sources located within the Northern Hemisphere, par- nized that exposure of humans to PTS can, to certain ticularly those in Europe and Asia, play a dominant extent, be dependant on each of these factors. The pre- role in the contamination of the Arctic. Given the spa- cise role differs depending on the contaminant con- tial distribution of PTS emission sources, and their cerned, however, with respect to human intake, the potential for ‘global’ transport, evaluation of long- chain consisting of ‘source – pathway – biological avail- range atmospheric transport of PTS to the Arctic ability’ applies to all contaminants. Leaving aside the region necessarily involves modeling on the hemi- biological aspect of the problem, this chapter focuses spheric/global scale using a multi-compartment on PTS sources, and their physical transport pathways. approach. To meet these requirements, appropriate modeling tools have been developed. Contaminant sources can be provisionally separated into three categories: Extensive efforts were made in the collection and • Distant sources: Located far from receptor sites in preparation of input data for modeling. This included the Arctic. Contaminants can reach receptor areas the required meteorological and geophysical informa- via air currents, riverine flow, and ocean currents. tion, and data on the physical and chemical properties During their transport, contaminants are affected by of both the selected substances and of their emissions. -
Poland's Voivodeships and Poviats and the Geographies Of
Prace Komisji Geografii Przemysłu Polskiego Towarzystwa Geograficznego Studies of the Industrial Geography Commission of the Polish Geographical Society 30 (2) · 2016 UniversityStanley of Kentucky,D. Brunn Lexington, USA CracowMarcin University Semczuk of Economics, Poland PedagogicalRafał Koszek, UniversityPoland’s Karolinaof VoivodeshipsCracow, Poland Gołuszka, and Poviats Gabriela and the Bołoz Geographies of Knowledge: Addressing Uneven Human Resources Abstract: - - In a postindustrial economic world, information economies are key components in local, region al and national development. These are service economies, built on the production, consumption and dis semination of information, including education, health care, outsourcing, tourism, sustainability and related- perlinkshuman welfare are electronic services. knowledge We explore data the that geography/knowledge can be mapped to highlight intersections the areas in Poland’sof most and voivodeships least informa and- poviats by using the volumes of information or hyperlinks about selected information economies. Google hy tion about certain subject categories. While some mapping results are expected, such as Warsaw and Krakow, being prominent, in other regions there are unexpected gaps within eastern, northern and southern Poland,- including some places near major metropolitan centers. There is a significant difference between the cities with poviat rights, which stand out in the number of information on items comparing to the poviats that sur round them. The majority of poviats in Mazowieckie voivodeship are surprisingly recognized as core areas onKeywords: the map of knowledge, nevertheless they are considered undeveloped from the economic point of view. Received: Google hyperlinks; human welfare; knowledge economies; knowledge gaps Accepted: 13 January 2016 Suggested 6citation: June 2016 Prace Komisji Geografii przemy- słuBrunn, Polskiego S.D., Semczuk, Towarzystwa M., Koszek, Geograficznego R., Gołuszka, [Studies K., Bołoz of the G. -
Sverdrup-Among-The-Tundra-People
AMONG THE TUNDRA PEOPLE by HARALD U. SVERDRUP TRANSLATED BY MOLLY SVERDRUP 1939 Copyright @ 1978 by Regents of the University of California. All rights reserved. No part of this book may be reproduced or utilized in any form or by any means, elec- tronic or mechanical, including photocopying, recording, or by any information storage and retrieval system, without permission in writing from the regents. Distributed by : Scripps Institution of Oceanography A-007 University of California, San Diego La Jolla, California 92093 Library of Congress # 78-60483 ISBN # 0-89626-004-6 ACKNOWLEDGMENTS We are indebted to Molly Sverdrup (Mrs. Leif J.) for this translation of Hos Tundra-Folket published by Gyldendal Norsk Forlag, Oslo, 1938. We are also indebted to the late Helen Raitt for recovering the manuscript from the archives of the Scripps Institution of Oceanography. The Norwegian Polar Institute loaned negatives from Sverdrup's travels among the Chukchi, for figures 1 through 4. Sverdrup's map of his route in the Chukchi country in 19 19/20 was copied from Hos Tundra-Folket. The map of the Chukchi National Okrug was prepared by Fred Crowe, based on the American Geographic Society's Map of the Arctic Region (1975). The map of Siberia was copied from Terence Armstrong's Russian Settlement in the North (1 965) with permission of the Cambridge University Press. Sam Hinton drew the picture of a reindeer on the cover. Martin W. Johnson identified individuals in some of the photographs. Marston C Sargent Elizabeth N. Shor Kittie C C Kuhns Editors The following individuals, most of whom were closely associated with Sverdrup, out of respect for him and wishing to assure preservation of this unusual account, met part of the cost of publication. -
Spanning the Bering Strait
National Park service shared beringian heritage Program U.s. Department of the interior Spanning the Bering Strait 20 years of collaborative research s U b s i s t e N c e h UN t e r i N c h UK o t K a , r U s s i a i N t r o DU c t i o N cean Arctic O N O R T H E L A Chu a e S T kchi Se n R A LASKA a SIBERIA er U C h v u B R i k R S otk S a e i a P v I A en r e m in i n USA r y s M l u l g o a a S K S ew la c ard Peninsu r k t e e r Riv n a n z uko i i Y e t R i v e r ering Sea la B u s n i CANADA n e P la u a ns k ni t Pe a ka N h las c A lf of Alaska m u a G K W E 0 250 500 Pacific Ocean miles S USA The Shared Beringian Heritage Program has been fortunate enough to have had a sustained source of funds to support 3 community based projects and research since its creation in 1991. Presidents George H.W. Bush and Mikhail Gorbachev expanded their cooperation in the field of environmental protection and the study of global change to create the Shared Beringian Heritage Program. -
Paleozoic Rocks of Northern Chukotka Peninsula, Russian Far East: Implications for the Tectonicsof the Arctic Region
TECTONICS, VOL. 18, NO. 6, PAGES 977-1003 DECEMBER 1999 Paleozoic rocks of northern Chukotka Peninsula, Russian Far East: Implications for the tectonicsof the Arctic region BorisA. Natal'in,1 Jeffrey M. Amato,2 Jaime Toro, 3,4 and James E. Wright5 Abstract. Paleozoicrocks exposedacross the northernflank of Alaskablock the essentialelement involved in the openingof the the mid-Cretaceousto Late CretaceousKoolen metamorphic Canada basin. domemake up two structurallysuperimposed tectonic units: (1) weaklydeformed Ordovician to Lower Devonianshallow marine 1. Introduction carbonatesof the Chegitununit which formed on a stableshelf and (2) strongly deformed and metamorphosedDevonian to Interestin stratigraphicand tectoniccorrelations between the Lower Carboniferousphyllites, limestones, and an&site tuffs of RussianFar East and Alaska recentlyhas beenrevived as the re- the Tanatapunit. Trace elementgeochemistry, Nd isotopicdata, sult of collaborationbetween North Americanand Russiangeol- and texturalevidence suggest that the Tanataptuffs are differen- ogists.This paperpresents the resultsof one suchstudy from the tiatedcalc-alkaline volcanic rocks possibly derived from a mag- ChegitunRiver valley, Russia,where field work was carriedout matic arc. We interpretthe associatedsedimentary facies as in- to establishthe stratigraphic,structural, and metamorphicrela- dicativeof depositionin a basinal setting,probably a back arc tionshipsin the northernpart of the ChukotkaPeninsula (Figure basin. Orthogneissesin the core of the Koolen dome yielded a