On the History of Archaeological Studies in the Russian Arctic
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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. -
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. -
Nornickel and the Kola Peninsula
THE BELLONA FOUNDATION Nornickel and the Kola Peninsula Photo: Thomas Nilsen ENVIRONMENTAL RESPONSIBILITY IN THE YEAR OF ECOLOGY JANUARY 2018 The Bellona Foundation is an international environmental NGO based in Norway. Founded in 1986 as a direct action protest group, Bellona has become a recognized technology and solution- oriented organizations with offices in Oslo, Brussels, Kiev, St. Petersburg and Murmansk. Altogether, some 60 engineers, ecologists, nuclear physicists, economists, lawyers, political scientists and journalists work at Bellona. Environmental change is an enormous challenge. It can only be solved if politicians and legislators develop clear policy frameworks and regulations for industry and consumers. Industry plays a role by developing and commercializing environmentally sound technology. Bellona strives to be a bridge builder between industry and policy makers, working closely with the former to help them respond to environmental challenges in their field, and proposing policy measures that promote new technologies with the least impact on the environment. Authors: Oskar Njaa © Bellona 201 8 Design: Bellona Disclaimer: Bellona endeavors to ensure that the information disclosed in this report is correct and free from copyrights, but does not warrant or assume any legal liability or responsibility for the accuracy, completeness, interpretation or usefulness of the information which may result from the use of this report. Contact: [email protected] Web page: www.bellona.org 1 Table of Contents 1 Introduction: ...................................................................................................................... -
Living in Two Places : Permanent Transiency In
living in two places: permanent transiency in the magadan region Elena Khlinovskaya Rockhill Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge CB2 1ER, UK; [email protected] abstract Some individuals in the Kolyma region of Northeast Russia describe their way of life as “permanently temporary.” This mode of living involves constant movements and the work of imagination while liv- ing between two places, the “island” of Kolyma and the materik, or mainland. In the Soviet era people maintained connections to the materik through visits, correspondence and telephone conversations. Today, living in the Kolyma means living in some distant future, constantly keeping the materik in mind, without fully inhabiting the Kolyma. People’s lives embody various mythologies that have been at work throughout Soviet Kolyma history. Some of these models are being transformed, while oth- ers persist. Underlying the opportunities afforded by high mobility, both government practices and individual plans reveal an ideal of permanency and rootedness. KEYWORDS: Siberia, gulag, Soviet Union, industrialism, migration, mobility, post-Soviet The Magadan oblast’1 has enjoyed only modest attention the mid-seventeenth century, the history of its prishloye in arctic anthropology. Located in northeast Russia, it be- naseleniye3 started in the 1920s when the Kolyma region longs to the Far Eastern Federal Okrug along with eight became known for gold mining and Stalinist forced-labor other regions, okrugs and krais. Among these, Magadan camps. oblast' is somewhat peculiar. First, although this territory These regional peculiarities—a small indigenous pop- has been inhabited by various Native groups for centu- ulation and a distinct industrial Soviet history—partly ries, compared to neighboring Chukotka and the Sakha account for the dearth of anthropological research con- Republic (Yakutia), the Magadan oblast' does not have a ducted in Magadan. -
Circumpolar Wild Reindeer and Caribou Herds DRAFT for REVIEW
CircumpolarCircumpolar WildWild ReindeerReindeer andand CaribouCaribou HerdsHerds DRAFTDRAFT FORFOR REVIEWREVIEW 140°W 160°W 180° 160°E Urup ALEUTIAN ISLANDS NORTH PACIFIC OCEAN KURIL ISANDS Paramushir ALEUTIAN ISLANDS Petropavlovsk Kamchatskiy Commander Islands Bering Sea Kronotskiy Gulf r ive Gulf of Kamchatka a R k 50°N at ch NORTH PACIFIC OCEAN m Ka 40°N Sea of Okhotsk Bristol Bay KAMCHATKA PENINSULA Karaginskiy Gulf Okha ALASKA PENINSULA Tatar Strait Kodiak Gulf of Sakhalin Bethel Iliamna Lake Shelikhova Gulf P’yagina Pen. Koni Pen. Riv Homer ina er iver zh Magadan Cook Inlet R n m Pe Taygonos Pen. wi Coos Bay ok sk u Kenai K Kotlit S . F Gulf of Anadyr' Okhotsk-Kolyma Upland Kenai Peninsula o Western Arctic Wi r Uda Bay llam Anchorage k iver Eugenee Ku r’ R tt Tillamook Gulf of Alaska sk dy e S o Nome A na R Prince William Sound kw Salem2iv Queen Charlotte Islands u im s e Astoria Palmeri R Norton Sound ive r t iv R r STANOVOY RANGE n e a r a Valdez m Portland2 R y r Aberdeen2 Port HardyQueen Charlotte Sound i l e Dixon Entrance v o v Vancouver1 e CHUKCHI PENINSULA K i r R y r Centralia Bering Strait O u e Sitka l t v Olympia Seward Peninsula o h i ALASKA RANGE y R k R Courtenay ive u ia KetchikanAlexander Archipelago r K b TacomaStrait of Juan de Fuca Nanaimo m r Bol’sho u e y l A Wrangell v n o Puget Sound Strait of Georgia i United States of America yu C SeattleEverett R y r er Kotzebue Sound Ri e Juneau p ve iv BellinghamVancouver2 S op r R Yakima t C Kotzebue n ik r o COAST MOUNTAINS in e l COLUMBIA PLAT. -
K. Fujita1, E. E. Dretzka2 and A. Grantz3 This Report Is Preliminary and Has Not Been Reviewed for Conformity with U. S. Geologi
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY BIBLIOGRAPHY OF NORTHEAST SIBERIAN GEOLOGY AND GEOPHYSICS (SECOND EDITION) K. Fujita1, E. E. Dretzka2 and A. Grantz3 OPEN FILE REPORT 82-616 This report is preliminary and has not been reviewed for conformity with U. S. Geological Survey editorial standards. Menlo Park, California July 1982 1. Department of Geology, Michigan State University, East Lansing MI 48824 2. Department of Geological Sciences, Northwestern University, Evanston IL 60201; now at: Department of Computer Sciences, Stanford University, Stanford CA 94305. 3. U. S. Geological Survey, Menlo Park, CA 94025 INTRODUCTION This bibliography is a compendium of literature available in English, either in its original form or in translation, on the geology and geophysics of northeast Siberia and adjacent seas and shelves. It is an expanded version of Fujita and Dretzka (1978-) and has been updated to include publications released through early 1982. The area! coverage extends from the edge of the Siberian platform (just east of the Lena River) on the east to the U. S. - Russia Convention Line of 1867 on the west. The East Siberian and Chukchi Seas are included as the northern limit while the Sea if Okhotsk and Kamchatka represent the southern limits. Sakhalin has been excluded and some, but not all, references to the Kuril Islands have been included. A sketch map of the area is shown in figure 1. It is hoped that this listing is nearly exhaustive for works on this area with some exceptions. Neither the Paleontological Journal nor Petroleum Geology have been indexed in this edition and, in addition, articles on Recent seismicity and volcanic activity in the Kuril-Kamchatka arc have been omitted. -
Kola Oleneostrovskiy Grave Field: a Unique Burial Site in the European Arctic
Kola Oleneostrovskiy Grave Field: A Unique Burial Site in the European Arctic Anton I. Murashkin, Evgeniy M. Kolpakov, Vladimir Ya. Shumkin, Valeriy I. Khartanovich & Vyacheslav G. Moiseyev Anton I. Murashkin, Department of Archaeology, St Petersburg State University, Mendeleyevskaya liniya 5, RU-199034 St Petersburg, Russia: [email protected], [email protected] Evgeniy M. Kolpakov, Department of Palaeolithic, Institute for the History of Material Culture, Russian Academy of Sciences, Dvortsovaya nab. 18, RU-191186 St Petersburg, Russia: [email protected] Vladimir ya. Shumkin, Department of Palaeolithic, Institute for the History of Material Culture, Russian Academy of Sciences, Dvortsovaya nab. 18, RU-191186 St Petersburg, Russia: [email protected] Valeriy I. Khartanovich, Department of Anthropology, Peter the Great Museum of Anthropology and Ethnography (Kunstkamera), Russian Academy of Sciences, Universitetskaya nab. 3, RU-199034 St Petersburg, Russia: [email protected] Vyacheslav G. Moiseyev, Department of Anthropology, Peter the Great Museum of Anthropology and Ethnography (Kunstkamera), Russian Academy of Sciences, Universitetskaya nab. 3, RU-199034 St Petersburg, Russia: [email protected] Abstract The Kola Oleneostrovskiy grave field (KOG) is the main source of information for the physical and cultural anthropology of the Early Metal Period population of the Kola Peninsula and the whole northern Fennoscandia.1 Excavations were conducted here in 1925, 1928, 1947–1948, and 2001–2004 by A. Shmidt, N. Gurina, and V. Shumkin. Altogether 32 burials containing the remains of 43 individuals were investigated. During the excavations, also remains of wooden grave constructions were found. The site is exceptionally rich in burial goods, including numerous bone, antler, stone, ceramic, and bronze items. -
Inventory and Distribution of Rock Glaciers in Northeastern Yakutia
land Article Inventory and Distribution of Rock Glaciers in Northeastern Yakutia Vasylii Lytkin Melnikov Permafrost Institute, Siberian Branch of the Russian Academy of Sciences, Yakutsk 677010, Russia; [email protected] Received: 2 September 2020; Accepted: 8 October 2020; Published: 10 October 2020 Abstract: Rock glaciers are common forms of relief of the periglacial belt of many mountain structures in the world. They are potential sources of water in arid and semi-arid regions, and therefore their analysis is important in assessing water reserves. Mountain structures in the north-east of Yakutia have optimal conditions for the formation of rock glaciers, but they have not yet been studied in this regard. In this article, for the first time, we present a detailed list of rock glaciers in this region. Based on geoinformation mapping using remote sensing data and field studies within the Chersky, Verkhoyansk, Momsky and Suntar-Khayata ranges, 4503 rock glaciers with a total area of 224.6 km2 were discovered. They are located within absolute altitudes, from 503 to 2496 m. Their average minimum altitude was at 1456 m above sea level, and the maximum at 1527 m. Most of these formations are located on the sides of the trough valleys, and form extended sloping types of rock glaciers. An assessment of the exposure of the slopes where the rock glaciers are located showed that most of the rock glaciers are facing north and south. Keywords: rock glacier; permafrost; inventory; northeastern Yakutia; remote sensing 1. Introduction The geography of distribution of rock glaciers is quite extensive. They are found in many mountainous regions of Europe, North and South America and Asia, including some circumpolar regions [1–18]. -
LATE PLEISTOCENE and EARLY HOLOCENE WINTER AIR TEMPERATURES in KOTELNY ISLAND: RECONSTRUCTIONS USING STABLE ISOTOPES of ICE WEDGES Yu.K
Kriosfera Zemli, 2019, vol. XXIII, No. 2, pp. 12–24 http://www.izdatgeo.ru DOI: 10.21782/EC2541-9994-2019-2(12-24) LATE PLEISTOCENE AND EARLY HOLOCENE WINTER AIR TEMPERATURES IN KOTELNY ISLAND: RECONSTRUCTIONS USING STABLE ISOTOPES OF ICE WEDGES Yu.K. Vasil’chuk1,2, V.M. Makeev3, A.A. Maslakov1, N.A. Budantseva1, A.C. Vasil’chuk1 1 Lomonosov Moscow State University, Faculty of Geography and Faculty of Geology, 1, Leninskie Gory, Moscow, 119991, Russia 2 Tyumen State University, 6, Volodarskogo str., Tyumen, 625003, Russia; [email protected] 3Russian State Hydrometeorological University, 98, Malookhtinsky prosp., St. Petersburg, 109017, Russia Late Pleistocene and Holocene winter air temperatures in Kotelny Island, northeastern Russian Arctic, have been reconstructed using oxygen isotope compositions of ice wedges and correlated with evidence of Late Pleistocene and Holocene climate variations inferred from pollen data. The δ18О values range exceeds 6 ‰ in Late Pleistocene ice wedges but is only 1.5 ‰ in the Holocene ones (–30.6 ‰ to –24.0 ‰ against –23.1 ‰ to –21.6 ‰, respectively). The Late Pleistocene mean January air temperatures in Kotelny Island were 10–12 °С lower than the respective present temperature. On the other hand, mean winter temperatures in cold substages during the Karga interstadial were colder than those during the Sartan glacial event. The Late Pleistocene– Holocene climate history included several warm intervals when air temperatures were high enough to maintain the existence of low canopy tree patches in Kotelny Island. Mean January air temperatures in the early Holocene were only 1.0–1.5 °С lower than now. -
Grey Seals on the Murman Coast, Russia: Status and Present Knowledge
Grey seals on the Murman coast, Russia: status and present knowledge Sergej V. Ziryanov and Vasily L. Mishin Polar research Institute of Marine Fisheries and Oceanography (PINRO), 183763 Murmansk, Russia ABSTRACT Grey seals (Halichoerus grypus) are distributed along the entire northern Murman coast in Russia. Breeding sites are located mainly on the Ainov and Seven islands, which belong to the Kandalaksha Nature Reserve. The annual pup production was estimated to be around 800 pups in the early 1990s, and the pup mortality has been observed to be relatively high. The population was estimated to be approxi- mately 3,500 individuals in 1994. Grey seals migrate in small numbers into the White Sea during sum- mer. The grey seal is protected and registered in the Red Books of Russia, Murmansk region and Fen- noscandia. The main results of grey seals investigations from 1986 to 2000 are briefly reviewed. There are no recent studies on abundance, seasonal distribution, growth, moulting and feeding of the species. Ziryanov, S.V. and Mishin, V.L. 2007. Grey seals on the Murman coast, Russia: status and present knowledge. NAMMCO Sci. Publ. 6:13-22. INTRODUCTION The grey seal (Halichoerus grypus) occurs works did not permit adequate assessment of in coastal waters of northern Murman (Fig. the status of breeding colonies. Aspects of bi- 1). Local hunting for grey seals has been per- ology such as breeding season, moulting and formed on the Murman coast for many years. behaviour were not covered (Kondakov 1997). N. A. Smirnov did his biological identifica- tion of the species in the area of Murman just Investigations of the local fauna, including grey at the beginning of the 20th century (Smirnov seals, were attempted starting in 1938, when a 1903). -
The Mesozoic–Cenozoic Tectonic Evolution of the New Siberian Islands, NE Russia
Geol. Mag. 152 (3), 2015, pp. 480–491. c Cambridge University Press 2014 480 doi:10.1017/S0016756814000326 The Mesozoic–Cenozoic tectonic evolution of the New Siberian Islands, NE Russia ∗ CHRISTIAN BRANDES †, KARSTEN PIEPJOHN‡, DIETER FRANKE‡, NIKOLAY SOBOLEV§ & CHRISTOPH GAEDICKE‡ ∗ Institut für Geologie, Leibniz Universität Hannover, Callinstraße, 30167 Hannover, Germany ‡Bundesanstalt für Geowissenschaften und Rohstoffe (BGR), Stilleweg 2, 30655 Hannover, Germany §A.P. Karpinsky Russian Geological Research Institute (VSEGEI), Sredny av. 74, 199106 Saint-Petersburg, Russia (Received 27 December 2013; accepted 4 June 2014; first published online 25 September 2014) Abstract – On the New Siberian Islands the rocks of the east Russian Arctic shelf are exposed and allow an assessment of the structural evolution of the region. Tectonic fabrics provide evidence of three palaeo-shortening directions (NE–SW, WNW–ESE and NNW–SSE to NNE–SSW) and one set of palaeo-extension directions revealed a NE–SW to NNE–SSW direction. The contractional deformation is most likely the expression of the Cretaceous formation of the South Anyui fold–thrust belt. The NE–SW shortening is the most prominent tectonic phase in the study area. The WNW–ESE and NNW–SSE to NNE–SSW-oriented palaeo-shortening directions are also most likely related to fold belt formation; the latter might also have resulted from a bend in the suture zone. The younger Cenozoic NE–SW to NNE–SSW extensional direction is interpreted as a consequence of rifting in the Laptev Sea. Keywords: New Siberian Islands, De Long Islands, South Anyui suture zone, fold–thrust belt. 1. Introduction slip data. Such datasets deliver important information for understanding the regional geodynamic evolution In the last decades, several plate tectonic models have of the study area. -
Songs of the Kolyma Tundra
‘Songs of the Kolyma Tundra’ – Co-Production and Perpetuation of Knowledge Concerning Ecology and Weather in the Indigenous Communities of Nizhnikolyma, Republic of Sakha (Yakutia), Russian Federation Tero Mustonen (1), Viatcheslav Shadrin (2), Kaisu Mustonen (1), Vladimir Vasiliev (3) together with the community representatives from Kolumskaya, Cherski, Andrejuskino, Podhovsk and the nomadic communities of Nutendli and Turvaurgin in the Niznikolyma region, Republic of Sakha-Yakutia, Russian Federation (1) Snowchange Cooperative / University of Joensuu (2) Institute of the Indigenous Peoples of the North (3) Northern Forum Academy Contact Information: Tero Mustonen, Snowchange Cooperative Havukkavaarantie 29 FIN 8125 Lehtoi Finland Email: [email protected] www.snowchange.org Abstract This article highlights community-based observations of climate and weather related changes in Indigenous communities of Niznikolyma or Lower Kolyma Region, Republic of Sakha (Yakutia), Russian Federation along with local efforts to preserve traditional knowledge through a nomadic school, in part as an adaptive mechanism. The observations have been collected using a method of co-production of knowledge, which allows the local Indigenous peoples to participate in a meaningful way in research that involves and affects them. In the past four years, the Snowchange Cooperative based in Finland, in cooperation with the Institute of the Indigenous Peoples of the North and Northern Forum Academy based in Yakutsk, has conducted field research in the region to document and assess observations of rapid changes to weather, ecosystems, and human societies of North-East Siberia. Thawing of the continuous permafrost, disappearance of fishing lakes, and increased flooding and erosion are some of the observed changes impacting the region and its inhabitants.