Chukotsky Autonomous Okrug Russian E a S 737,000 Sq
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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. -
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. -
The Pacific Gateway to the Arctic: Recent Change in the Bering Strait - Observations, Drivings and Implications
1 The Pacific Gateway to the Arctic: Recent change in the Bering Strait - observations, drivings and implications Rebecca Woodgate, Cecilia Peralta-Ferriz University of Washington, Seattle, USA Recent Change in the Bering Strait New Climatology and Bering Strait products The long-sought “Pacific-ARCTIC” pressure head forcing NASA The Bering Strait, … on a good day Alaska Russia ~ 85 km wide, ~ 50 m deep LOCALLY: - divided into 2 channels by - is an integrator of the the Diomede Islands properties of the Bering Sea - split by the US-Russian - dominates the water border properties of the Chukchi Sea - ice covered ~ Jan - April 8th July 2010 Ocean Color oceancolor.gsfc.nasa.gov (from Bill Crawford) ... influences Important for ~ half of the Russia 80N Marine Life Arctic Ocean Most nutrient-rich watersBarents entering Sea the Arctic (Walsh et al, 1989) Heat to melt ice Fram In spring, trigger western Arctic StraitGreenland melt onset Sea Bering Impacts Global climate stability Year-round subsurface heatStrait Doubling of flow affects Gulf source in ~ half of Arctic Greenland Alaska Stream, overturning circulation (Paquette & Bourke, 1981; Ahlnäs & Garrison,1984; (Wadley & Bigg, 2002; Huang & Schmidt, 1993; Woodgate et al, 2010; 2012) CanadianDeBoer & Nof , 2004; Hu & Meehl, 2005) Archipelago Important for Arctic Stratification Significant part of Arctic In winter, Pacific waters (fresher than Freshwater Budget Atlantic waters) form a cold ~ 1/3rd of Arctic Freshwater (halocline) layer, which insulates the Large (largest?) ice from the warm Atlantic water interannual variability beneath (Wijffels et al, 1992; Aagaard & Carmack, 1989; (Shimada et al, 2001, Steele et al, 2004) Woodgate & Aagaard, 2005) Figure from Woodgate, 2013, Nature Education 4 Overview of Bering Strait measurements MODIS SST 26th Aug 2004 Early 1990s, 2004-2006 == 1+ moorings also in Russian waters. -
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. -
Pamphlet to Accompany Scientific Investigations Map 3131
Bedrock Geologic Map of the Seward Peninsula, Alaska, and Accompanying Conodont Data By Alison B. Till, Julie A. Dumoulin, Melanie B. Werdon, and Heather A. Bleick Pamphlet to accompany Scientific Investigations Map 3131 View of Salmon Lake and the eastern Kigluaik Mountains, central Seward Peninsula 2011 U.S. Department of the Interior U.S. Geological Survey Contents Introduction ....................................................................................................................................................1 Sources of data ....................................................................................................................................1 Components of the map and accompanying materials .................................................................1 Geologic Summary ........................................................................................................................................1 Major geologic components ..............................................................................................................1 York terrane ..................................................................................................................................2 Grantley Harbor Fault Zone and contact between the York terrane and the Nome Complex ..........................................................................................................................3 Nome Complex ............................................................................................................................3 -
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. -
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. -
Inuit People
Inuit People Most of these objects were made in the 19th century by the Inuit, whose name means ‘the people’. The Athabascans called their Inuit neighbours ‘Eskimo’ meaning ‘eaters of raw flesh’. The Inuit way of life was adapted to their harsh territory which stretched 6000 miles across the Arctic from the Bering Sea to Greenland. Carving 80 Chisel handle made from bone with a carved face and animal figures. Possibly from south Alaska, made before 1880. 81 Carrying strap made of hide with a carved stone toggle, made in the 19th century. 82 Smoking pipe made of ivory and decorated with whaling scenes. Made by the western Inuit in the late 19th century. 83 Ivory toggle carved in the form of a seal. Probably made by the western Inuit before 1854. 84 Ivory toggle carved in the form of a bear. Probably made by the western Inuit before 1854. Hunting 85 Snow goggles made of wood. Used in the snow like sun glasses to protect the eyes. Made by the central Inuit before 1831. 86 Bolas made of ivory balls and gut strips, from Cape Lisburn, Bering Strait, made before 1848. Thrown when hunting to entangle a bird or other quarry. 87 Harpoon head, probably for a seal harpoon. Made by the western Inuit in the 19th century. 88 Seal decoy made of wood with claws. It was Used to scratch the ice. The sound attracted seals to breathing holes. Probably made by the western Inuit in the late 19th century. 89 Bone scoop used for clearing seal breathing holes in the ice, made in the 19th century. -
The Importance of Protection 57 60 1
Arctic Ocean B e a u Utqiagvik f o r t Wrangel 4 (Point Barrow) S e a Island 62 49 52 3 61 1 2 Pacific Walrus Haulout 21. Dezhnev Bay 42. Tyulen’e Ozero Bay 58 The Importance of Protection 57 60 1. Cape Blossom 22. Anastasia Bay 43. Srednyaya Bay 56 59 23. Bogoslava Island 44. Somneniye Chukchi Sea 2. Somnitelnaya Spit 55 24. Cape Tiomney 45. Olutorskaya Spit The Walrus Islands State Game Sanctuary (WISGS) was established 51 3. Davidova Spit 54 25. Cape Sery-Anana 46. Lekalo Spit in 1960 to protect Pacific walrus haulout sites on seven small craggy 4. Gavai 39 53 5. Kolyuchyn Island 26. Verkhoturova Island 47. Cape Vankarem 47 27. Cape Golenishcheva 48. Cape Onmyn islands in northern Bristol Bay: Round Island, Summit Island, Crooked 48 6. Belyaka Spit 7. Strait of Neskenpil’gyn Lagoon 28. Cape Semionova 49. Ayon Island Island, High Island, Black Rock, and The Twins. Chukotka, Russia 5 7 30 50 29. Little Diomede Island 50. Cape Serdtse-Kamen’ t S o u 8. Unlisted 6 i e n u d a e b 30. Kotzebue Sound 51. Ryrkaipii r z t 9. Cape Inkigur 9 t 10 o The sanctuary includes the surrounding waters that support a diverse S K 31. King Island 52. Cape Shelagsky 10. Cape Dezhnev 16 12 11 group of marine mammals, seabirds, and other marine wildlife. 15 32. Gambell 53. Cape Lisburne g 29 11. Big Diomede Island 17 n Alaska, USA i 31 A b a r 33. Savoonga 54. -
A Region with Special Needs the Russian Far East in Moscow’S Policy
65 A REGION WITH SPECIAL NEEDS THE RUSSIAN FAR EAST IN MOSCOW’s pOLICY Szymon Kardaś, additional research by: Ewa Fischer NUMBER 65 WARSAW JUNE 2017 A REGION WITH SPECIAL NEEDS THE RUSSIAN FAR EAST IN MOSCOW’S POLICY Szymon Kardaś, additional research by: Ewa Fischer © Copyright by Ośrodek Studiów Wschodnich im. Marka Karpia / Centre for Eastern Studies CONTENT EDITOR Adam Eberhardt, Marek Menkiszak EDITOR Katarzyna Kazimierska CO-OPERATION Halina Kowalczyk, Anna Łabuszewska TRANSLATION Ilona Duchnowicz CO-OPERATION Timothy Harrell GRAPHIC DESIGN PARA-BUCH PHOTOgrAPH ON COVER Mikhail Varentsov, Shutterstock.com DTP GroupMedia MAPS Wojciech Mańkowski PUBLISHER Ośrodek Studiów Wschodnich im. Marka Karpia Centre for Eastern Studies ul. Koszykowa 6a, Warsaw, Poland Phone + 48 /22/ 525 80 00 Fax: + 48 /22/ 525 80 40 osw.waw.pl ISBN 978-83-65827-06-7 Contents THESES /5 INTRODUctiON /7 I. THE SPEciAL CHARActERISticS OF THE RUSSIAN FAR EAST AND THE EVOLUtiON OF THE CONCEPT FOR itS DEVELOPMENT /8 1. General characteristics of the Russian Far East /8 2. The Russian Far East: foreign trade /12 3. The evolution of the Russian Far East development concept /15 3.1. The Soviet period /15 3.2. The 1990s /16 3.3. The rule of Vladimir Putin /16 3.4. The Territories of Advanced Development /20 II. ENERGY AND TRANSPORT: ‘THE FLYWHEELS’ OF THE FAR EAST’S DEVELOPMENT /26 1. The energy sector /26 1.1. The resource potential /26 1.2. The infrastructure /30 2. Transport /33 2.1. Railroad transport /33 2.2. Maritime transport /34 2.3. Road transport /35 2.4.