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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. -
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. -
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]. -
The Population History of Northeastern Siberia Since the Pleistocene Martin Sikora1,43*, Vladimir V
ARTICLE https://doi.org/10.1038/s41586-019-1279-z The population history of northeastern Siberia since the Pleistocene Martin Sikora1,43*, Vladimir V. Pitulko2,43*, Vitor C. Sousa3,4,5,43, Morten E. Allentoft1,43, Lasse Vinner1, Simon Rasmussen6,41, Ashot Margaryan1, Peter de Barros Damgaard1, Constanza de la Fuente1,42, Gabriel Renaud1, Melinda A. Yang7, Qiaomei Fu7, Isabelle Dupanloup8, Konstantinos Giampoudakis9, David Nogués-Bravo9, Carsten Rahbek9, Guus Kroonen10,11, Michaël Peyrot11, Hugh McColl1, Sergey V. Vasilyev12, Elizaveta Veselovskaya12,13, Margarita Gerasimova12, Elena Y. Pavlova2,14, Vyacheslav G. Chasnyk15, Pavel A. Nikolskiy2,16, Andrei V. Gromov17, Valeriy I. Khartanovich17, Vyacheslav Moiseyev17, Pavel S. Grebenyuk18,19, Alexander Yu. Fedorchenko20, Alexander I. Lebedintsev18, Sergey B. Slobodin18, Boris A. Malyarchuk21, Rui Martiniano22, Morten Meldgaard1,23, Laura Arppe24, Jukka U. Palo25,26, Tarja Sundell27,28, Kristiina Mannermaa27, Mikko Putkonen25, Verner Alexandersen29, Charlotte Primeau29, Nurbol Baimukhanov30, Ripan S. Malhi31,32, Karl-Göran Sjögren33, Kristian Kristiansen33, Anna Wessman27,34, Antti Sajantila25, Marta Mirazon Lahr1,35, Richard Durbin22,36, Rasmus Nielsen1,37, David J. Meltzer1,38, Laurent Excoffier4,5* & Eske Willerslev1,36,39,40* Northeastern Siberia has been inhabited by humans for more than 40,000 years but its deep population history remains poorly understood. Here we investigate the late Pleistocene population history of northeastern Siberia through analyses of 34 newly recovered ancient -
Wiiw Balkan Observatory Working Paper 106: the Spatial Structure Of
The wiiw Balkan Observatory December Working Papers|106| 2012 Valentina Lapo The spatial structure of the Russian economy and the multipolar world The wiiw Balkan Observatory www.balkan-observatory.net About Shortly after the end of the Kosovo war, the last of the Yugoslav dissolution wars, the Balkan Reconstruction Observatory was set up jointly by the Hellenic Observatory, the Centre for the Study of Global Governance, both institutes at the London School of Economics (LSE), and the Vienna Institute for International Economic Studies (wiiw). A brainstorming meeting on Reconstruction and Regional Co-operation in the Balkans was held in Vouliagmeni on 8-10 July 1999, covering the issues of security, democratisation, economic reconstruction and the role of civil society. It was attended by academics and policy makers from all the countries in the region, from a number of EU countries, from the European Commission, the USA and Russia. Based on ideas and discussions generated at this meeting, a policy paper on Balkan Reconstruction and European Integration was the product of a collaborative effort by the two LSE institutes and the wiiw. The paper was presented at a follow-up meeting on Reconstruction and Integration in Southeast Europe in Vienna on 12-13 November 1999, which focused on the economic aspects of the process of reconstruction in the Balkans. It is this policy paper that became the very first Working Paper of the wiiw Balkan Observatory Working Papers series. The Working Papers are published online at www.balkan- observatory.net, the internet portal of the wiiw Balkan Observatory. It is a portal for research and communication in relation to economic developments in Southeast Europe maintained by the wiiw since 1999. -
Modernism and Reindeer in the Bering Straits
More Things on Heaven and Earth: Modernism and Reindeer in the Bering Straits By Bathsheba Demuth Summer 2012 Bathsheba Demuth is a PhD candidate in the Department of History at the University of California, Berkeley The Scene On a modern map, the shoulders of Eurasia and North America nearly touch at the Bering Strait, a 52-mile barrier between Old World and New. During the rolling period of ice ages known as the Pleistocene, the Pacific Ocean pulled back leaving the Chukchi Peninsula connected to Alaska’s Seward Peninsula by a wide, grassy plain. Two million years ago, the animal we call the reindeer emerged along this continental juncture.1 As glaciers spread, reindeer followed them southward; by 20,000 years ago, Rangifer tarandus had moved deep into Western Europe, forming the base of Neolithic hunters’ diets and appearing, antlers lowered in the fall rutting charge, on the walls of Lascaux.2 Reindeer, like our human ancestors who appeared a million and a half years after them, are products of the ice age. They are gangly, long-nosed, and knob-kneed, with a ruff of white fur around their deep chests, swooping antlers and nervous ears, and have the capacity to not just survive but thrive in million-strong herds despite the Arctic dark and cold. Like any animal living in the far north, reindeer – or caribou, as they are known in North America – must solve the problem of energy. With the sun gone for months of the year, the photosynthetic transfer of heat into palatable calories is minimal; plants are small, tough, often no more than the rock-like scrum of lichens. -
Crustal Architecture of the East Siberian Arctic Shelf and Adjacent Arctic Ocean Constrained by Seismic Data and Gravity Modeling Results
This is a repository copy of Crustal architecture of the East Siberian Arctic Shelf and adjacent Arctic Ocean constrained by seismic data and gravity modeling results. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/129730/ Version: Accepted Version Article: Drachev, SS, Mazur, S, Campbell, S et al. (2 more authors) (2018) Crustal architecture of the East Siberian Arctic Shelf and adjacent Arctic Ocean constrained by seismic data and gravity modeling results. Journal of Geodynamics, 119. pp. 123-148. ISSN 0264-3707 https://doi.org/10.1016/j.jog.2018.03.005 Crown Copyright © 2018 Published by Elsevier Ltd. This is an author produced version of a paper published in Journal of Geodynamics. Uploaded in accordance with the publisher's self-archiving policy. This manuscript version is made available under the Creative Commons CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/. Reuse This article is distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) licence. This licence only allows you to download this work and share it with others as long as you credit the authors, but you can’t change the article in any way or use it commercially. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. -
The Russian-U.S. Borderland: Opportunities and Barriers, Desires and Fears
The Russian-U.S. Borderland: Opportunities and Barriers, Desires and Fears Serghei Golunov∗ Abstract The paper focuses on the Russia-U.S. cross-border area that lies in the Bering Sea region. Employing the concept of geographical proximity, I argue that the U.S.-Russian proximity works in a limited number of cases and for relatively few kinds of actors, such as companies supplying Chukotka with American goods, border guards conducting rescue operations, organizers of environmental projects and cruise tours, and aboriginal communities. The impressive territorial proximity between Asia and North America induces ambitious and sometimes widely advertised official and public desires of conquering the spatial divide, promoted by extreme travellers and planners of transcontinental tunnel or bridge projects. At the same time, cooperation is seriously hindered by limited economic potential of the Russian North-East, weakness of transportation networks, harsh climate, and pervasive alarmist sentiments on the Russian side of the border. Introduction Russian and U.S. territories are situated close to each other in the areas of the Bering Sea: the shortest distance between the closest islands across the border is less than four kilometers. However, the nearby territories are sparsely populated and have limited resources that make intensive cooperation between them problematic while larger cities are situated at a much larger distance across the border. The area where Russian and U.S. territories are close to each other can be conceptualized as a geographical proximity that is a multidimensional, relational, and highly subjective phenomenon. In what respects and for whom does the Russia-U.S. proximity matter? To what extent does it matter for cross-border cooperation? What kinds of desires does such proximity induce? Are there some pervasive alarmist sentiments linked with proximity and, if there are, what ways do they influence cross-border interaction? To respond to these questions, the following issues are addressed. -
VI. Republic of Sakha (Yakutia) Overview of the Region Josh
Saving Russia's Far Eastern Taiga : Deforestation, Protected Areas, and Forests 'Hotspots' VI. Republic of Sakha (Yakutia) Overview of the Region Josh Newell Location The Republic of Yakutia (Sakha), situated in northeastern Siberia, stretches to the Henrietta Islands (77 N) in the far north and is washed by the Arctic Ocean (Laptev and Eastern Siberian Seas). These waters, the coldest and iciest of all seas in the northern hemisphere, are covered by ice for 9 to 10 months of the year. The Stanovoy Ridge (55 D. 30 D. N) borders Yakutia in the south, the upper reaches of the Olenyok River form the western border, and Chukotka forms the eastern border (165 E). Size Almost one-fifth of the territory of the Russian Federation (3,103,200 sq. km.) and greater than the combined areas of France, Austria, Germany, Italy, Sweden, England, Greece, and Finland. Climate Winter is prolonged and severe, with average January temperatures about -40C. Summer is short but warm; the average in July is 13C and temperatures have reached 39C in Yakutsk. In the northeast, the town of Verekhoyansk reaches -70C (-83F) and is considered the coldest inhabited place on Earth. There is little precipitation - from 150-200 mm. in Central Yakutia to 500-700 mm. in the mountains of eastern and southern Yakutia. Geography and Ecology Forty percent of Yakutia lies within the Arctic Circle and all of it is covered by eternally frozen ground- permafrost - which greatly influences the region's ecology and limits forests to the southern region. Yakutia can be divided into three great vegetation belts. -
Revising the Archaeological Record of the Upper Pleistocene Arctic Siberia: Human Dispersal and Adaptations in MIS 3 and 2
Quaternary Science Reviews 165 (2017) 127e148 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Revising the archaeological record of the Upper Pleistocene Arctic Siberia: Human dispersal and adaptations in MIS 3 and 2 * Vladimir Pitulko a, , Elena Pavlova b, Pavel Nikolskiy c a Institute for the Material Culture History, Russian Academy of Sciences, 18 Dvortsovaya nab., St Petersburg, 191186, Russia b Arctic & Antarctic Research Institute, 38 Bering St., St Petersburg, 199397, Russia c Geological Institute, Russian Academy of Sciences, 7 Pyzhevsky per., 119017 Moscow, Russia article info abstract Article history: As the main external driver, environmental changes largely predetermine human population distribu- Received 21 June 2016 tion, especially in the Arctic, where environmental conditions were often too extreme for human sur- Received in revised form vival. Not that long ago the only evidence of human presence here was the Berelekh site in the lower 20 March 2017 reaches of the Indighirka River. This landmark dates to 13,000e12,000 years ago but it was widely Accepted 1 April 2017 accepted as documentation of the earliest stage of human dispersal in the Arctic. New research discussed here, shows that humans began colonizing the Siberian Arctic at least by the end of the early stage of MIS 3 at around 45,000 years ago. For now, this earliest known stage of human occupation in the arctic Keywords: Upper Paleolithic regions is documented by the evidence of human hunting. The archaeological record of continued human fi Arctic occupation is fragmentary; nevertheless, evidence exists for each signi cant phase including the Last Taimyr Glacial Maximum (LGM).