Spitsbergen - Realm of the Polar Bear
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Arctic Expedition12° 16° 20° 24° 28° 32° Spitsbergen U Svalbard Archipelago 80° 80°
distinguished travel for more than 35 years Voyage UNDER THE Midnight Sun Arctic Expedition12° 16° 20° 24° 28° 32° Spitsbergen u Svalbard Archipelago 80° 80° 80° Raudfjorden Nordaustlandet Woodfjorden Smeerenburg Monaco Glacier The Arctic’s 79° 79° 79° Kongsfjorden Svalbard King’s Glacier Archipelago Ny-Ålesund Spitsbergen Longyearbyen Canada 78° 78° 78° i Greenland tic C rcle rc Sea Camp Millar A U.S. North Pole Russia Bellsund Calypsobyen Svalbard Archipelago Norway Copenhagen Burgerbukta 77° 77° 77° Cruise Itinerary Denmark Air Routing Samarin Glacier Hornsund Barents Sea June 20 to 30, 2022 4° 8° Spitsbergen12° u Samarin16° Glacier20° u Calypsobyen24° 76° 28° 32° 36° 76° Voyage across the Arctic Circle on this unique 11-day Monaco Glacier u Smeerenburg u Ny-Ålesund itinerary featuring a seven-night cruise round trip Copenhagen 1 Depart the U.S. or Canada aboard the Five-Star Le Boréal. Visit during the most 2 Arrive in Copenhagen, Denmark enchanting season, when the region is bathed in the magical 3 Copenhagen/Fly to Longyearbyen, Spitsbergen, light of the Midnight Sun. Cruise the shores of secluded Norway’s Svalbard Archipelago/Embark Le Boréal 4 Hornsund for Burgerbukta/Samarin Glacier Spitsbergen—the jewel of Norway’s rarely visited Svalbard 5 Bellsund for Calypsobyen/Camp Millar archipelago enjoy expert-led Zodiac excursions through 6 Cruising the Arctic Ice Pack sandstone mountain ranges, verdant tundra and awe-inspiring 7 MåkeØyane/Woodfjorden/Monaco Glacier ice formations. See glaciers calve in luminous blues and search 8 Raudfjorden for Smeerenburg for Arctic wildlife, including the “King of the Arctic,” the 9 Ny-Ålesund/Kongsfjorden for King’s Glacier polar bear, whales, walruses and Svalbard reindeer. -
Handbok07.Pdf
- . - - - . -. � ..;/, AGE MILL.YEAR$ ;YE basalt �- OUATERNARY votcanoes CENOZOIC \....t TERTIARY ·· basalt/// 65 CRETACEOUS -� 145 MESOZOIC JURASSIC " 210 � TRIAS SIC 245 " PERMIAN 290 CARBONIFEROUS /I/ Å 360 \....t DEVONIAN � PALEOZOIC � 410 SILURIAN 440 /I/ ranite � ORDOVICIAN T 510 z CAM BRIAN � w :::;: 570 w UPPER (J) PROTEROZOIC � c( " 1000 Ill /// PRECAMBRIAN MIDDLE AND LOWER PROTEROZOIC I /// 2500 ARCHEAN /(/folding \....tfaulting x metamorphism '- subduction POLARHÅNDBOK NO. 7 AUDUN HJELLE GEOLOGY.OF SVALBARD OSLO 1993 Photographs contributed by the following: Dallmann, Winfried: Figs. 12, 21, 24, 25, 31, 33, 35, 48 Heintz, Natascha: Figs. 15, 59 Hisdal, Vidar: Figs. 40, 42, 47, 49 Hjelle, Audun: Figs. 3, 10, 11, 18 , 23, 28, 29, 30, 32, 36, 43, 45, 46, 50, 51, 52, 53, 54, 60, 61, 62, 63, 64, 65, 66, 67, 68, 69, 71, 72, 75 Larsen, Geir B.: Fig. 70 Lytskjold, Bjørn: Fig. 38 Nøttvedt, Arvid: Fig. 34 Paleontologisk Museum, Oslo: Figs. 5, 9 Salvigsen, Otto: Figs. 13, 59 Skogen, Erik: Fig. 39 Store Norske Spitsbergen Kulkompani (SNSK): Fig. 26 © Norsk Polarinstitutt, Middelthuns gate 29, 0301 Oslo English translation: Richard Binns Editor of text and illustrations: Annemor Brekke Graphic design: Vidar Grimshei Omslagsfoto: Erik Skogen Graphic production: Grimshei Grafiske, Lørenskog ISBN 82-7666-057-6 Printed September 1993 CONTENTS PREFACE ............................................6 The Kongsfjorden area ....... ..........97 Smeerenburgfjorden - Magdalene- INTRODUCTION ..... .. .... ....... ........ ....6 fjorden - Liefdefjorden................ 109 Woodfjorden - Bockfjorden........ 116 THE GEOLOGICAL EXPLORATION OF SVALBARD .... ........... ....... .......... ..9 NORTHEASTERN SPITSBERGEN AND NORDAUSTLANDET ........... 123 SVALBARD, PART OF THE Ny Friesland and Olav V Land .. .123 NORTHERN POLAR REGION ...... ... 11 Nordaustlandet and the neigh- bouring islands........................... 126 WHA T TOOK PLACE IN SVALBARD - WHEN? .... -
Arctic Environments
Characteristics of an arctic environment and the physical geography of Svalbard - ‘geography explained’ fact sheet The Arctic environment is little studied at Key Stage Three yet it is an excellent basis for an all-encompassing study of place or as a case study to illustrate key concepts within a specific theme. Svalbard, an archipelago lying in the Arctic Ocean north of mainland Europe, about midway between Norway and the North Pole, is a place with an awesome landscape and unique geography that includes issues and themes of global, regional and local importance. A study of Svalbard could allow pupils to broaden and deepen their knowledge and understanding of different aspects of the seven geographical concepts that underpin the revised Geography Key Stage Three Programme of Study. Many pupils will have a mental image of an Arctic landscape, some may have heard of Svalbard. A useful starting point for study is to explore these perceptions using visual prompts and big questions – where is the Arctic/Svalbard? What is it like? What is happening there? Why is it like this? How will it change? Svalbard exemplifies the distinctive physical and human characteristics of the Arctic and yet is also unique amongst Arctic environments. Perceptions and characteristics of the Arctic may be represented in many ways, including art and literature and the pupil’s own geographical imagination of the place. Maps and photographs are vital in helping pupils develop spatial understanding of locations, places and processes and the scale at which they occur. Source: commons.wikimedia.org/wiki/Image:W_W_Svalbard... 1 Longyearbyen, Svalbard’s capital Source:http://www.photos- The landscape of Western Svalbard voyages.com/spitzberg/images/spitzberg06_large.jpg Source: www.hi.is/~oi/svalbard_photos.htm Where is Svalbard? Orthographic map projection centred on Svalbard and showing location relative to UK and EuropeSource: www.answers.com/topic/orthographic- projection.. -
Arctic Saga: Exploring Spitsbergen Via the Faroes and Jan Mayen Three
SPITSBERGEN, THE FAROES & JAN MAYEN SPITSBERGEN, GREENLAND & ICELAND Exploring the Fair Isle coastline; an encounter with Svalbard Reindeer; capturing the scenery. A Zodiac cruise with a view. Arctic Ocean GREENLAND SVALBARD Longyearbyen Bellsund Longyearbyen Hornsund Greenland Sea Arctic Saga: Barents GREENLAND Sea Three Arctic Islands: SVALBARD Jan Mayen FROM Exploring Spitsbergen via OSLO Norwegian Sea Spitsbergen, Greenland and Iceland SOUTHBOUND the Faroes and Jan Mayen Scoresby Atlantic Ocean A Sund RCT TO IC C OSLO Departing from Aberdeen, Scotland, the Arctic Saga voyage visits four remote IRCL Named one of the 50 Tours of a Lifetime by National Geographic Traveler, E Milne Ittoqqortoormiit Arctic islands. Sail through the North Atlantic to Fair Isle, famous for its bird Faroe Islands NORWAY this voyage offers the best of the eastern Arctic in one voyage. You start in Land observatory, followed by two days exploring the Viking and Norse sites on Shetland Spitsbergen, Norway, then sail south to Greenland to explore the world’s Denmark Islands Strait the Faroe Islands. Then it’s onto the world’s northernmost volcanic island, Atlantic Ocean Oslo largest fjord system and end in Iceland. There’s something for everyone: CLE Orkney C CIR ARCTI Jan Mayen. The last two days of your 14-day voyage are spent exploring Islands Fair Isle polar bears, walrus, muskoxen, local culture, ancient Thule settlements, Aberdeen Spitsbergen, always on the lookout for polar bears. hikes along the glacial moraine and tundra, and more. Reykjavik ICELAND Nature is the tour guide: Sea, ice, and weather conditions will determine your trip itinerary. Embrace the unexpected. -
Oceanography and Biology; of Arctic Seas
Rapp. P.-v. Réun. Cons. int. Explor. Mer, 188: 23-35. 1989 Climatic fluctuations in the Barents Sea Lars Midttun Midttun, Lars. 1989. Climatic fluctuations in the Barents Sea. Rapp. P.-v. Réun. Cons. int. Explor. Mer, 188: 23—35. The circulation system of the Barents Sea is described. Warm water flows into the sea from the west and is gradually transformed into Arctic water, which then flows out of the sea, partly as surface currents, partly as dense bottom water. The climatic conditions of the Barents Sea are determined both by the variations in the inflow and by processes taking place in the sea itself. The great variations in temperature and salinity observed along standard sections crossing the inflowing water masses are examined, and possible explanations are discussed. Lars Midttun: Institute of Marine Research, P.O. Box 1870 - Nordnes, N-5024 Bergen, Norway. Introduction The main purpose of this paper is to present and discuss been the most intensively studied area, and several stan the rather marked climatic variations observed in the dard sections have been established in order to investi Barents Sea. However it may be worth while first to gate variations in the inflowing water masses. Measure give a short description of the circulation system as ments in the Kola section were started as early as 1900 known from the literature. by Dr N. Knipowich and have been regularly continued Based on early observations, Knipowich (1905) gave since 1920. Bochkov (1976) studied temperature var a description of the water masses of the Barents Sea, iations in relation to solar activity. -
Hacquebord, Louwrens; Veluwenkamp, Jan Willem
University of Groningen Het topje van de ijsberg Boschman, Nienke; Hacquebord, Louwrens; Veluwenkamp, Jan Willem IMPORTANT NOTE: You are advised to consult the publisher's version (publisher's PDF) if you wish to cite from it. Please check the document version below. Document Version Publisher's PDF, also known as Version of record Publication date: 2005 Link to publication in University of Groningen/UMCG research database Citation for published version (APA): Boschman, N., Hacquebord, L., & Veluwenkamp, J. W. (editors) (2005). Het topje van de ijsberg: 35 jaar Arctisch centrum (1970-2005). (Volume 2 redactie) Barkhuis Publishing. Copyright Other than for strictly personal use, it is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license (like Creative Commons). The publication may also be distributed here under the terms of Article 25fa of the Dutch Copyright Act, indicated by the “Taverne” license. More information can be found on the University of Groningen website: https://www.rug.nl/library/open-access/self-archiving-pure/taverne- amendment. Take-down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Downloaded from the University of Groningen/UMCG research database (Pure): http://www.rug.nl/research/portal. For technical reasons the number of authors shown on this cover page is limited to 10 maximum. Download date: 04-10-2021 Twenty five years of multi-disciplinary research into the17th century whaling settlements in Spitsbergen L. -
MARITIME ACTIVITY in the HIGH NORTH – CURRENT and ESTIMATED LEVEL up to 2025 MARPART Project Report 1
MARITIME ACTIVITY IN THE HIGH NORTH – CURRENT AND ESTIMATED LEVEL UP TO 2025 MARPART Project Report 1 Authors: Odd Jarl Borch, Natalia Andreassen, Nataly Marchenko, Valur Ingimundarson, Halla Gunnarsdóttir, Iurii Iudin, Sergey Petrov, Uffe Jacobsen and Birita í Dali List of authors Odd Jarl Borch Project Leader, Nord University, Norway Natalia Andreassen Nord University, Norway Nataly Marchenko The University Centre in Svalbard, Norway Valur Ingimundarson University of Iceland Halla Gunnarsdóttir University of Iceland Iurii Iudin Murmansk State Technical University, Russia Sergey Petrov Murmansk State Technical University, Russia Uffe Jakobsen University of Copenhagen, Denmark Birita í Dali University of Greenland 1 Partners MARPART Work Package 1 “Maritime Activity and Risk” 2 THE MARPART RESEARCH CONSORTIUM The management, organization and governance of cross-border collaboration within maritime safety and security operations in the High North The key purpose of this research consortium is to assess the risk of the increased maritime activity in the High North and the challenges this increase may represent for the preparedness institutions in this region. We focus on cross-institutional and cross-country partnerships between preparedness institutions and companies. We elaborate on the operational crisis management of joint emergency operations including several parts of the preparedness system and resources from several countries. The project goals are: • To increase understanding of the future demands for preparedness systems in the High North including both search and rescue, oil spill recovery, fire fighting and salvage, as well as capacities fighting terror or other forms of destructive action. • To study partnerships and coordination challenges related to cross-border, multi-task emergency cooperation • To contribute with organizational tools for crisis management Project characteristics: Financial support: -Norwegian Ministry of Foreign Affairs, -the Nordland county Administration -University partners. -
Development and Achievements of Dutch Northern and Arctic Cartography
ARCTIC’ VOL. 37, NO. 4 (DECEMBER 1984) P. 493.514 Development and Achievements of Dutch Northern and Arctic Cartography. in the Sixteenth and Seventeenth :Centuries GUNTER. SCHILDER* ther north, as far as the Shetlands the Faroes, in line with INTRODUCTION and the expansion of the Dutch .fishing and trading areas. The During the sixteenth and .seventeenth. centuries, the Dutch Thresmr contains a number of coastal viewsfrom the voyage made. a vital contribution to. the mapphg of the northern and around the North Capeas far as ‘‘Wardhuys”. Although there arctic regions, and their caPtographic work piayed a decisive is no mapofthis region, there is.a map of the coasts of Karelia part in expanding. the ,geographical .knowledgeof that time. and Russia to the east of the White Sea asfar as the Pechora, Amsterdam became the centre.of international map production accompanied by a text with instructionsfor navigation as far as and the map trade. Its Cartographers and publishers acquired Vaygach and Novaya Zemlya (Waghenaer, 1592:fo101-105). their knowledge partly from the results of expeditions fitted A coastal view.of the latter is also given.s The fact that Wag- out by theirfellow countrymen and, partlyfrom foreign henaer had access to original sources is shown by the inclusion voyages of discovery. This paper will describe the growing- in the Thresoor of the only known accountof Olivier Brunel’s Dutch..awarenessof .the northern and arctic regions. stage by voyage to-NovayaZemlya in 1584 (Waghenaer, ‘1592:P104).6 stage and region by region, with the aid of Dutch. maps. Anotherimportant document is WillemBiuentsz’s map of northern Scandinavia, which extends as faras the entrance to THE PROGRESS OF DUTCH KNOWLEDGE IN THE NORTH .the White Sea, and shows.al1 the reefs and shallows(Fig. -
Ms Spitsbergen Voyage Handbook 2019–2020
voyage handbook MS SPITSBERGEN VOYAGE HANDBOOK 2019–2020 1 Dear Adventurer 2 Norway 4 Dear adventurer, Iceland 6 Congratulations on book- This handbook includes in- Svalbard 8 ing an extraordinary cruise formation on your chosen aboard MS Spitsbergen. destination, as well as other destinations this ship visits Faroe Islands 12 Norwegian explorer Roald during the 2019-2020 sailing Amundsen’s success as an ex- season. We hope you will find Orkney Islands 14 plorer is often explained by his this information inspiring. thorough preparations before Shetland Islands 16 departure. He once said “vic- We promise you an amazing Contents tory awaits him who has every- adventure! thing in order.” Being true to Franz Josef Land 18 Amund sen’s heritage of good Welcome aboard for the ad- planning, we encourage you to venture of a lifetime! Important Information 20 read this handbook. Frequently Asked Questions 21 It will provide you with good Your Hurtigruten Team advice, historical context, practical information, and in- Life on Board MS Spitsbergen 22 spiring information that will Practical Information make your voyage even more 28 enjoyable. Before and After Your Voyage Pack Like an Explorer 30 Our Team on Board 32 Landing by Small Boats 34 Important Phone Numbers 35 Maritime Expressions 35 MS Spitsbergen Deck Plan 36 2 COVER FRONT PHOTO: © ANDREA KLAUSSNER / HURTIGRUTEN 3 COVER BACK PHOTO: © DOMINIC BARRINGTON / HURTIGRUTEN © KARSTEN BIDSTRUP / HURTIGRUTEN / KARSTEN © BIDSTRUP came to prominence during the NATURE AND WILDLIFE Norway is a Viking era (800–1050 B.C.), Deep fjords, islets, and the high with strong trade relations and mountains of the Scandes, unique country colonies in Greenland, Ire- which belong to the Caledonien land, England, Scotland, and mountain range, characterize that continous- Normandy. -
Genomic Platforms and Molecular Physiology of Insect Stress Tolerance
Genomic Platforms and Molecular Physiology of Insect Stress Tolerance DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Justin Peyton MS Graduate Program in Evolution, Ecology and Organismal Biology The Ohio State University 2015 Dissertation Committee: Professor David L. Denlinger Advisor Professor Zakee L. Sabree Professor Amanda A. Simcox Professor Joseph B. Williams Copyright by Justin Tyler Peyton 2015 Abstract As ectotherms with high surface area to volume ratio, insects are particularly susceptible to desiccation and low temperature stress. In this dissertation, I examine the molecular underpinnings of two facets of these stresses: rapid cold hardening and cryoprotective dehydration. Rapid cold hardening (RCH) is an insect’s ability to prepare for cold stress when that stress is preceded by an intermediate temperature for minutes to hours. In order to gain a better understanding of cold shock, recovery from cold shock, and RCH in Sarcophaga bullata I examine the transcriptome with microarray and the metabolome with gas chromatography coupled with mass spectrometry (GCMS) in response to these treatments. I found that RCH has very little effect on the transcriptome, but results in a shift from aerobic metabolism to glycolysis/gluconeogenesis during RCH and preserved metabolic homeostasis during recovery. In cryoprotective dehydration (CD), a moisture gradient is established between external ice and the moisture in the body of an insect. As temperatures decline, the external ice crystals grow, drawing in more moisture which dehydrates the insect causing its melting point to track the ambient temperature. To gain a better understanding of CD and dehydration in Belgica antarctica I explore the transcriptome with RNA sequencing ii and the metabolome with GCMS. -
Protected Areas in Svalbard – Securing Internationally Valuable Cultural and Natural Heritage Contents Preface
Protected areas in Svalbard – securing internationally valuable cultural and natural heritage Contents Preface ........................................................................ 1 – Moffen Nature Reserve ......................................... 13 From no-man’s-land to a treaty and the Svalbard – Nordaust-Svalbard Nature Reserve ...................... 14 Environmental Protection Act .................................. 4 – Søraust-Svalbard Nature Reserve ......................... 16 The history of nature and cultural heritage – Forlandet National Park .........................................18 protection in Svalbard ................................................ 5 – Indre Wijdefjorden National Park ......................... 20 The purpose of the protected areas .......................... 6 – Nordenskiöld Land National Park ........................ 22 Protection values ........................................................ 7 – Nordre Isfjorden National Park ............................ 24 Nature protection areas in Svalbard ........................10 – Nordvest-Spitsbergen National Park ................... 26 – Bird sanctuaries ..................................................... 11 – Sassen-Bünsow Land National Park .................... 28 – Bjørnøya Nature Reserve ...................................... 12 – Sør-Spitsbergen National Park ..............................30 – Ossian Sars Nature Reserve ................................. 12 Svalbard in a global context ..................................... 32 – Hopen Nature Reserve -
Svalbard 2015–2016 Meld
Norwegian Ministry of Justice and Public Security Published by: Norwegian Ministry of Justice and Public Security Public institutions may order additional copies from: Norwegian Government Security and Service Organisation E-mail: [email protected] Internet: www.publikasjoner.dep.no KET T Meld. St. 32 (2015–2016) Report to the Storting (white paper) Telephone: + 47 222 40 000 ER RY M K Ø K J E L R I I Photo: Longyearbyen, Tommy Dahl Markussen M 0 Print: 07 PrintMedia AS 7 9 7 P 3 R 0 I 1 08/2017 – Impression 1000 N 4 TM 0 EDIA – 2 Svalbard 2015–2016 Meld. St. 32 (2015–2016) Report to the Storting (white paper) 1 Svalbard Meld. St. 32 (2015–2016) Report to the Storting (white paper) Svalbard Translation from Norwegian. For information only. Table of Contents 1 Summary ........................................ 5 6Longyearbyen .............................. 39 1.1 A predictable Svalbard policy ........ 5 6.1 Introduction .................................... 39 1.2 Contents of each chapter ............... 6 6.2 Areas for further development ..... 40 1.3 Full overview of measures ............. 8 6.2.1 Tourism: Longyearbyen and surrounding areas .......................... 41 2Background .................................. 11 6.2.2 Relocation of public-sector jobs .... 43 2.1 Introduction .................................... 11 6.2.3 Port development ........................... 44 2.2 Main policy objectives for Svalbard 11 6.2.4 Svalbard Science Centre ............... 45 2.3 Svalbard in general ........................ 12 6.2.5 Land development in Longyearbyen ................................ 46 3 Framework under international 6.2.6 Energy supply ................................ 46 law .................................................... 17 6.2.7 Water supply .................................. 47 3.1 Norwegian sovereignty .................. 17 6.3 Provision of services .....................