The First Tourist Cruise in the Soviet Arctic WILLIAM BARR’
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Arctic Marine Transport Workshop 28-30 September 2004
Arctic Marine Transport Workshop 28-30 September 2004 Institute of the North • U.S. Arctic Research Commission • International Arctic Science Committee Arctic Ocean Marine Routes This map is a general portrayal of the major Arctic marine routes shown from the perspective of Bering Strait looking northward. The official Northern Sea Route encompasses all routes across the Russian Arctic coastal seas from Kara Gate (at the southern tip of Novaya Zemlya) to Bering Strait. The Northwest Passage is the name given to the marine routes between the Atlantic and Pacific oceans along the northern coast of North America that span the straits and sounds of the Canadian Arctic Archipelago. Three historic polar voyages in the Central Arctic Ocean are indicated: the first surface shop voyage to the North Pole by the Soviet nuclear icebreaker Arktika in August 1977; the tourist voyage of the Soviet nuclear icebreaker Sovetsky Soyuz across the Arctic Ocean in August 1991; and, the historic scientific (Arctic) transect by the polar icebreakers Polar Sea (U.S.) and Louis S. St-Laurent (Canada) during July and August 1994. Shown is the ice edge for 16 September 2004 (near the minimum extent of Arctic sea ice for 2004) as determined by satellite passive microwave sensors. Noted are ice-free coastal seas along the entire Russian Arctic and a large, ice-free area that extends 300 nautical miles north of the Alaskan coast. The ice edge is also shown to have retreated to a position north of Svalbard. The front cover shows the summer minimum extent of Arctic sea ice on 16 September 2002. -
Plumulitid Machaeridian Remains from the Silurian (Telychian) of Severnaya Zemlya, Arctic Russia
NORWEGIAN JOURNAL OF GEOLOGY Plumulitid mochoeridion remains from the Silurion, Arctic Russio 53 Plumulitid machaeridian remains from the Silurian (Telychian) of Severnaya Zemlya, Arctic Russia Anette E.S. Hogstrom, Olga K. Bogolepova & Alexander P. Gubanov Hogstrom, A.E.S., Bogolepova, O.K. and Gubanov, A.P.: Plumulitid machaeridian remains from the Silurian (Telychian) of Sevemaya Zemlya, Arc tic Russia. Norsk Geologisk Tidsskrift, Vol. 82, pp. 53-55. Trondheim 2002, ISSN 029-196X. The machaeridian genus Plumulites is reported for the first time from the Severnaya ZemlyaArchipelago of Arctic Russia, where it occurs in limes tone concretions within the Sredninskaya Formation. Graptolites fromthe same concretions indicate the late crispus- griestoniensisBiozones of the mid Telychian (Uandovery). Similarities to plumulitid sclerites from the Upper Ordovician of the Tairnyr Peninsula promotes further interest in machaeridian faunas fromthis region. A.E.S. Hogstromi, O.K. Bogolepova and A.P. Gubanov, Historical Geology & Palaeontology, Dept. of Earth Sciences, Uppsala University, Norbyviigen 22, SE-752 36, Uppsala, Sweden. I Temporaryaddress: Dept. of Earth Sciences, Wills Memorial Building, Queen's Road, Bristol BSB l RJ, UK. lntroduction Stratigraphy and locality The global record of Silurian machaeridians is limited, Machaeridians discussed herein originate from the but includes rare articulated specimens, and more com Lower Silurian Sredninskaya Formation (Matukhin et monly isolated sclerites that have been found in Britain al. 1999). To avoid nomenclatural questions, it should (de Koninck 1857; Woodward 1865; Withers 1926 and be noted that these rocks were previously referred to as Adrain et al. 1991), the Baltic Region (Aurivillius 1892; the Golomaynnaya Formation (Menner et al. -
Region Building and Identity Formation in the Baltic Sea Region
IJIS Volume 3 REGION BUILDING AND IDENTITY FORMATION IN THE BALTIC SEA REGION ∗ Imke Schäfer Abstract This paper examines the concept of “new region building” in the Baltic Sea region with emphasis on the construction of a collective “Baltic” identity. Possible implications of these processes on Russia as a non-EU member state are discussed. Region building around the Baltic Sea is conceptualised within the framework of social constructivism, and a connection between region building and identity formation is established. Furthermore, an attempt is made to shed light on the way in which a “Baltic identity” is promoted in the region. By means of a short discourse analysis, certain characteristics of the Baltic Sea region are discovered that are promoted as the basis for a regional identity by various regional actors. The impact of these characteristics on relations between Russia, the EU and the other Baltic Sea states are examined and conclusions are drawn in relation to the region building processes in the Baltic Sea area. INTRODUCTION Cooperation in the Baltic Sea region (BSR) has prospered since the independence of the Baltic States in the beginning of the 1990s. Several programmes and initiatives have been established, such as the Northern Dimension initiative (ND), the Council of Baltic Sea States (CBSS) or the Baltic Sea States Subregional Cooperation (BSSSC). The EU actively supports cooperation in this region. In 1997, at the Luxembourg European Council, Finland’s Northern Dimension initiative (ND) was recognized as part of the -
AQUILA BOOKS Specializing in Books and Ephemera Related to All Aspects of the Polar Regions
AQUILA BOOKS Specializing in Books and Ephemera Related to all Aspects of the Polar Regions Winter 2012 Presentation copy to Lord Northcliffe of The Limited Edition CATALOGUE 112 88 ‘The Heart of the Antarctic’ 12 26 44 49 42 43 Items on Front Cover 3 4 13 9 17 9 54 6 12 74 84 XX 72 70 21 24 8 7 7 25 29 48 48 48 37 63 59 76 49 50 81 7945 64 74 58 82 41 54 77 43 80 96 84 90 100 2 6 98 81 82 59 103 85 89 104 58 AQUILA BOOKS Box 75035, Cambrian Postal Outlet Calgary, AB T2K 6J8 Canada Cameron Treleaven, Proprietor A.B.A.C. / I.L.A.B., P.B.F.A., N.A.A.B., F.R.G.S. Hours: 10:30 – 5:30 MDT Monday-Saturday Dear Customers; Welcome to our first catalogue of 2012, the first catalogue in the last two years! We are hopefully on schedule to produce three catalogues this year with the next one mid May before the London Fairs and the last just before Christmas. We are building our e-mail list and hopefully we will be e-mailing the catalogues as well as by regular mail starting in 2013. If you wish to receive the catalogues by e-mail please make sure we have your correct e-mail address. Best regards, Cameron Phone: (403) 282-5832 Fax: (403) 289-0814 Email: [email protected] All Prices net in US Dollars. Accepted payment methods: by Credit Card (Visa or Master Card) and also by Cheque or Money Order, payable on a North American bank. -
Russia and Siberia: the Beginning of the Penetration of Russian People Into Siberia, the Campaign of Ataman Yermak and It’S Consequences
The Aoyama Journal of International Politics, Economics and Communication, No. 106, May 2021 CCCCCCCCC Article CCCCCCCCC Russia and Siberia: The Beginning of the Penetration of Russian People into Siberia, the Campaign of Ataman Yermak and it’s Consequences Aleksandr A. Brodnikov* Petr E. Podalko** The penetration of the Russian people into Siberia probably began more than a thousand years ago. Old Russian chronicles mention that already in the 11th century, the northwestern part of Siberia, then known as Yugra1), was a “volost”2) of the Novgorod Land3). The Novgorod ush- * Associate Professor, Novosibirsk State University ** Professor, Aoyama Gakuin University 1) Initially, Yugra was the name of the territory between the mouth of the river Pechora and the Ural Mountains, where the Finno-Ugric tribes historically lived. Gradually, with the advancement of the Russian people to the East, this territorial name spread across the north of Western Siberia to the river Taz. Since 2003, Yugra has been part of the offi cial name of the Khanty-Mansiysk Autonomous Okrug: Khanty-Mansiysk Autonomous Okrug—Yugra. 2) Volost—from the Old Russian “power, country, district”—means here the territo- rial-administrative unit of the aboriginal population with the most authoritative leader, the chief, from whom a certain amount of furs was collected. 3) Novgorod Land (literally “New City”) refers to a land, also known as “Gospodin (Lord) Veliky (Great) Novgorod”, or “Novgorod Republic”, with its administrative center in Veliky Novgorod, which had from the 10th century a tendency towards autonomy from Kiev, the capital of Ancient Kievan Rus. From the end of the 11th century, Novgorod de-facto became an independent city-state that subdued the entire north of Eastern Europe. -
Drydocks World Dubai
G<CK75G=B;H<9@5H9GH89J9@CDA9BHG=BA5F=B9A5=BH9B5B79<5F8K5F9 GC:HK5F95B8H97<BC@C;=9G SEPTEMBER 2012 Exclusive interview: Drydocks World Dubai Gas turbines Extend maintenance intervals without affecting performance How to maintain climate specialist vessels during operation Australian Navy A new service regime to keep the fleet afloat Offshore wind farms Overcoming logistic challenges C ICEBREAKERS Climate specialist vessels Break the ice It’s not just the harsh weather that makes it difficult to protect and maintain climate specialist vessels Neil Jones, Marine Maintenance Technology International aintaining icebreaking and ice strengthened vessels does, as you might expect, have its Mchallenges. For a start, the nature of the way they operate subjects them to a huge amount of vibration, not to mention the impact of constantly operating in harsh weather. But conversely, as Albert Hagander, technical manager of the Swedish Maritime Administration’s Shipping Management Department, points out, there is actually a weather-related advantage in that the vessels are not usually in service during the summer. “You really can’t do much when they’re in service simply because of the weather conditions, often with ice on deck,” he points out. “In the summer, it’s often a better situation than with a conventional vessel, as you have the time to work on them while they’re alongside the dock or even in dry dock.” The Administration operates four big icebreakers plus a slightly smaller one for Lake Vänern that supplements the capability during the early or late season. That the icebreakers are vital can be seen from the fact that 95% of Swedish export/import trade is seaborne. -
Inventory Acc.12696 William Laird Mckinlay
Acc.12696 December 2006 Inventory Acc.12696 William Laird McKinlay National Library of Scotland Manuscripts Division George IV Bridge Edinburgh EH1 1EW Tel: 0131-466 2812 Fax: 0131-466 2811 E-mail: [email protected] © Trustees of the National Library of Scotland Correspondence and papers of William Laird McKinlay, Glasgow. Background William McKinlay (1888-1983) was for most of his working life a teacher and headmaster in the west of Scotland; however the bulk of the papers in this collection relate to the Canadian National Arctic Expedition, 1913-18, and the part played in it by him and the expedition leader, Vilhjalmur Stefansson. McKinlay’s account of his experiences, especially those of being shipwrecked and marooned on Wrangel Island, off the coast of Siberia, were published by him in Karluk (London, 1976). For a rather more detailed list of nos.1-27, and nos.43-67 (listed as nos.28-52), see NRA(S) survey no.2546. Further items relating to McKinlay were presented in 2006: see Acc.12713. Other items, including a manuscript account of the expedition and the later activities of Stefansson – much broader in scope than Karluk – have been deposited in the National Archives of Canada, in Ottawa. A small quantity of additional documents relating to these matters can be found in NRA(S) survey no.2222, papers in the possession of Dr P D Anderson. Extent: 1.56 metres Deposited in 1983 by Mrs A.A. Baillie-Scott, the daughter of William McKinlay, and placed as Dep.357; presented by the executor of Mrs Baillie-Scott’s estate, November 2006. -
Accelerated Glacier Mass Loss in the Russian Arctic (2010-2017) Christian Sommer1, Thorsten Seehaus1, Andrey Glazovsky2, Matthias H
https://doi.org/10.5194/tc-2020-358 Preprint. Discussion started: 28 December 2020 c Author(s) 2020. CC BY 4.0 License. Brief communication: Accelerated glacier mass loss in the Russian Arctic (2010-2017) Christian Sommer1, Thorsten Seehaus1, Andrey Glazovsky2, Matthias H. Braun1 1Institut für Geographie, Friedrich-Alexander-Universität Erlangen-Nürnberg, Erlangen, 91058, Germany 5 2Institute of Geography RAS, Moscow, 119017, Russia Correspondence to: Christian Sommer ([email protected]) Abstract. Glaciers in the Russian High Arctic have been subject to extensive warming due to global climate change, yet their contribution to sea level rise has been relatively small over the past decades. Here we show surface elevation change measure- ments and geodetic mass balances of 93% of all glacierized areas of Novaya Zemlya, Severnaya Zemlya and Franz Josef Land 10 using interferometric synthetic aperture radar measurements taken between 2010 and 2017. We calculate an overall mass loss rate of -23±5 Gt a-1, corresponding to a sea level rise contribution of 0.06±0.01 mm a-1. Compared to measurements prior to 2010, mass loss of glaciers on the Russian archipelagos has doubled in recent years. 1 Introduction The Arctic has undergone large environmental changes due to increases in temperature and humidity (Box et al., 2019) and an 15 increase in glacier mass loss has been observed in many polar regions (Morris et al., 2020). The Russian Arctic, including the archipelagos Novaya Zemlya, Severnaya Zemlya and Franz Josef Land, is one of these regions. Despite a glacierized area of ~52,000 km², in-situ observations of glacier mass change are sparse. -
It's a Dog's Life in Antarctica
REVIEWS • 321 IT’S A DOG’S LIFE IN ANTARCTICA: EXPLORING Peter arrived at Scott Base as a fresh 24-year-old recruit, THE TRANSANTARCTIC MOUNTAINS BY DOG after three months of vigorous training in New Zealand. I SLEDGE 1960 – 1962 – AND BEYOND. By PETER arrived at neighbouring McMurdo as a scientific assistant OTWAY. Tauranga, New Zealand: Self Published, Kale on almost the same day in mid-October 1960 and met Peter Print (www.kaleprint.co.nz), 2015. ISBN 978-0-473334- soon after, while skiing in the evenings on the Antarc- 642. 276 p., maps, b&w and colour illus., end dedication tic’s only ski lift – assisted ski slope, at Scott Base. In late note. Softbound. NZ$100.00, including postage charges. November Peter departed to the field with one of two par- ties working between the Byrd and the Nimrod, two huge The era of heroic and arduous dog sledging in Antarctica outlet glaciers feeding into the Ross Ice Shelf. Peter was is over. Dogs are no longer allowed to be on the continent, the assistant surveyor in the north party, while Wally was but this excellently illustrated book describes in detail three the surveyor for the south party. The appropriately named survey and geological journeys undertaken by Peter shortly “Starshot Glacier” separated the two. Peter’s survey efforts before the ban on dogs was imposed. I have never seen a used “shots” to the stars, in 24-hour polar daylight, to polar book that is so focused on our canine friends, but it determine exact geographic positions, which was a unique also shows the scenery of the Transantarctic Mountains viv- method and more exacting than using the sun as a target. -
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Silurian and Devonian strata on the Severnaya Zemlya and Sedov archipelagos (Russia) Peep MÄNNIK Institute of Geology, Tallinn Technical University, Estonia Ave 7, 10143 Tallinn (Estonia) [email protected] Vladimir V. MENNER Institute of Geology and Exploitation of Combustible Fuels (IGIRGI), Fersman Str. 50, 117312 Moscow (Russia) [email protected] [email protected] Rostislav G. MATUKHIN Siberian Research Institute of Geology, Geophysics and Mineral Resources (SNIIGiMS), Krasnyj Ave 67, 630104 Novosibirsk (Russia) [email protected] Visvaldis KURŠS Institute of Geology, University of Latvia, Raina Ave 19, LV-1050 Rīga (Latvia) [email protected] Männik P., Menner V. V., Matukhin R. G. & Kuršs V. 2002. — Silurian and Devonian strata 406 on the Severnaya Zemlya and Sedov archipelagos (Russia). Geodiversitas 24 (1) : 99-122. ABSTRACT Silurian and Devonian strata are widely distributed on the islands of the Severnaya Zemlya and Sedov archipelagos. The Silurian is represented by fossiliferous shallow-water carbonates underlain by variegated sandstones and siltstones of Ordovician age. The Devonian consists mainly of various red sandstones, siltstones and argillites, with carbonates only in some inter- KEY WORDS vals. The best sections available for study are located in the river valleys, and Silurian, in the cliffs along the coastline of islands. Type sections of most of the strati- Devonian, Sedov Archipelago, graphical units identified are located on the Matusevich River, October Severnaya Zemlya Archipelago, Revolution Island. As the Quaternary cover is poorly developed on Russia, lithostratigraphy, Severnaya Zemlya, the Palaeozoic strata can be easily traced also outside the biostratigraphy. sections. GEODIVERSITAS • 2002 • 24 (1) © Publications Scientifiques du Muséum national d’Histoire naturelle, Paris. -
Summary of the Arctic Archipelagos and Islands Off Eurasia
SUMMARY OF THE ARCTIC ARCHIPELAGOS AND ISLANDS OFF EURASIA R. K. Headland revised 18 May 2017 SPRI, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. These Arctic lands include a diverse range of archipelagos and separate islands. The positions given are approximately the middle point for smaller islands and their limits for larger ones and groups. Names are given in the forms recommended by the Union Géographique International with, where the name has varied through double transliteration, the original form, and, in other cases, an English translation. Sightings, landings, and winterings are the first recorded; there may have been previous ones for some islands. Islands only a short distance off the continental mainland are not included. In easterly order the islands are: JAN MAYEN 70·83°-71·17°N, 8°-9°W One isolated active volcanic island (latest eruption 1985); in the Greenland Sea. Area 373 km². Highest elevation: 2277 m (Beerenberg, volcano). 33% glacierized. Discovered 1614 by a Netherlands whaling voyage (Jan Jacobz. May aboard de goude Cath). First wintering 1633-34 (by whalers, all perished); meteorological station, established 1921, open. Norwegian territory; annexed in 1929. SPITSBERGEN ARKIPELAGO (Acute Peaks) 76·50°-80·80°N, 10°-34°E Four main islands and about 150 lesser ones; in the Barents Sea, of sedimentary origin with igneous overlay. Area: 62 842 km². Highest elevation: 1713 m (Newtontoppen). 60% glacierized. Possibly sighted 1194; discovered 1596 by a Dutch whaling voyage (Jacob Heemskerck aboard Hazewind). First wintering 1630-31 (by whalers); permanent settlement (coal mine) established 1906, currently 3 remain open, 1 other settlement occupied and 4 meteorological stations open. -
ARCTIC FLOATING UNIVERSITY PROGRAM 8–28 July 2017
ARCTIC FLOATING UNIVERSITY PROGRAM 8–28 July 2017 Saturday 8th 12.00 Departure of RV «Professor Molchanov» from Arkhanglesk Introductory meeting of the expedition participants, safety traing 14.00 – 15.00 Lunch Evacuation training from the vessel 18.00 – 19.00 Dinner Presentation of the expedition route Announcements on tomorrow schedule Introduction of the expedition members Sunday 9th 8.00-9.00 Breakfast Lecture: Introduction to physical oceanography (Vesman Anna, Arctic and Antarctic Research Institute ) Lecture: Weather and climate. Factors of climate formation (Urazgildeeva Aleksandra, Arctic and Antarctic Research Institute) 12.00-13.00 Lunch Lecture: XVIth century : "Reaching China,’Discovering' of Northern Russia" (Hösli Eric, Federal Polytechnic School of Lausanne) Lecture: Formation of landscapes in polar regions of the Earth - geographical zonality, factors and processes (Goryachkin Sergey, Institute of Geography, Russian Academy of Sciences ) Group work 18.00 -19.00 Dinner Lecture: Regional Geology of the Barents-Kara continental margin of Eurasia (Dmitry Metelkin, Novosibirsk State University) Announcements on tomorrow schedule Monday 10th 8.00-9.00 Breakfast Lecture: The Arctic Ocean (Vesman Anna, Arctic and Antarctic Research Institute ) Lecture: Features of climate formation in the Arctic (Urazgildeeva Aleksandra, Arctic and Antarctic Research Institute) 12.00-13.00 Lunch Lecture: XVIIIth and XIXth century : "Is There a Passage between Asia and America?” (Hösli Eric, Federal Polytechnic School of Lausanne) Lecture: Geoecological characteristics of European Arctic archipelagos and coasts and global change challenges (Goryachkin Sergey, Institute of Geography, Russian Academy of Sciences ) Group work 18.00 -19.00 Dinner Lecture: The Intrigue of Mesozoic Magmatism on the Franz Josef Land Archipelago: a Hot Spot or a Failed Rift? (Mikhaltsov Nikolay, Novosibirsk State University) Announcements on tomorrow schedule Tuesday 11th 8.00-9.00 Breakfast Lecture: The features of hydrological regime of the Barents Sea.