Written Exam SH-201 the History of Svalbard the University Centre in Svalbard, Monday 6 February 2012
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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? .... -
Petroleum, Coal and Research Drilling Onshore Svalbard: a Historical Perspective
NORWEGIAN JOURNAL OF GEOLOGY Vol 99 Nr. 3 https://dx.doi.org/10.17850/njg99-3-1 Petroleum, coal and research drilling onshore Svalbard: a historical perspective Kim Senger1,2, Peter Brugmans3, Sten-Andreas Grundvåg2,4, Malte Jochmann1,5, Arvid Nøttvedt6, Snorre Olaussen1, Asbjørn Skotte7 & Aleksandra Smyrak-Sikora1,8 1Department of Arctic Geology, University Centre in Svalbard, P.O. Box 156, 9171 Longyearbyen, Norway. 2Research Centre for Arctic Petroleum Exploration (ARCEx), University of Tromsø – the Arctic University of Norway, P.O. Box 6050 Langnes, 9037 Tromsø, Norway. 3The Norwegian Directorate of Mining with the Commissioner of Mines at Svalbard, P.O. Box 520, 9171 Longyearbyen, Norway. 4Department of Geosciences, University of Tromsø – the Arctic University of Norway, P.O. Box 6050 Langnes, 9037 Tromsø, Norway. 5Store Norske Spitsbergen Kulkompani AS, P.O. Box 613, 9171 Longyearbyen, Norway. 6NORCE Norwegian Research Centre AS, Fantoftvegen 38, 5072 Bergen, Norway. 7Skotte & Co. AS, Hatlevegen 1, 6240 Ørskog, Norway. 8Department of Earth Science, University of Bergen, P.O. Box 7803, 5020 Bergen, Norway. E-mail corresponding author (Kim Senger): [email protected] The beginning of the Norwegian oil industry is often attributed to the first exploration drilling in the North Sea in 1966, the first discovery in 1967 and the discovery of the supergiant Ekofisk field in 1969. However, petroleum exploration already started onshore Svalbard in 1960 with three mapping groups from Caltex and exploration efforts by the Dutch company Bataaffse (Shell) and the Norwegian private company Norsk Polar Navigasjon AS (NPN). NPN was the first company to spud a well at Kvadehuken near Ny-Ålesund in 1961. -
Climate in Svalbard 2100
M-1242 | 2018 Climate in Svalbard 2100 – a knowledge base for climate adaptation NCCS report no. 1/2019 Photo: Ketil Isaksen, MET Norway Editors I.Hanssen-Bauer, E.J.Førland, H.Hisdal, S.Mayer, A.B.Sandø, A.Sorteberg CLIMATE IN SVALBARD 2100 CLIMATE IN SVALBARD 2100 Commissioned by Title: Date Climate in Svalbard 2100 January 2019 – a knowledge base for climate adaptation ISSN nr. Rapport nr. 2387-3027 1/2019 Authors Classification Editors: I.Hanssen-Bauer1,12, E.J.Førland1,12, H.Hisdal2,12, Free S.Mayer3,12,13, A.B.Sandø5,13, A.Sorteberg4,13 Clients Authors: M.Adakudlu3,13, J.Andresen2, J.Bakke4,13, S.Beldring2,12, R.Benestad1, W. Bilt4,13, J.Bogen2, C.Borstad6, Norwegian Environment Agency (Miljødirektoratet) K.Breili9, Ø.Breivik1,4, K.Y.Børsheim5,13, H.H.Christiansen6, A.Dobler1, R.Engeset2, R.Frauenfelder7, S.Gerland10, H.M.Gjelten1, J.Gundersen2, K.Isaksen1,12, C.Jaedicke7, H.Kierulf9, J.Kohler10, H.Li2,12, J.Lutz1,12, K.Melvold2,12, Client’s reference 1,12 4,6 2,12 5,8,13 A.Mezghani , F.Nilsen , I.B.Nilsen , J.E.Ø.Nilsen , http://www.miljodirektoratet.no/M1242 O. Pavlova10, O.Ravndal9, B.Risebrobakken3,13, T.Saloranta2, S.Sandven6,8,13, T.V.Schuler6,11, M.J.R.Simpson9, M.Skogen5,13, L.H.Smedsrud4,6,13, M.Sund2, D. Vikhamar-Schuler1,2,12, S.Westermann11, W.K.Wong2,12 Affiliations: See Acknowledgements! Abstract The Norwegian Centre for Climate Services (NCCS) is collaboration between the Norwegian Meteorological In- This report was commissioned by the Norwegian Environment Agency in order to provide basic information for use stitute, the Norwegian Water Resources and Energy Directorate, Norwegian Research Centre and the Bjerknes in climate change adaptation in Svalbard. -
Terrestrial Inputs Govern Spatial Distribution of Polychlorinated Biphenyls (Pcbs) and Hexachlorobenzene (HCB) in an Arctic Fjord System (Isfjorden, Svalbard)*
Environmental Pollution 281 (2021) 116963 Contents lists available at ScienceDirect Environmental Pollution journal homepage: www.elsevier.com/locate/envpol Terrestrial inputs govern spatial distribution of polychlorinated biphenyls (PCBs) and hexachlorobenzene (HCB) in an Arctic fjord system (Isfjorden, Svalbard)* * Sverre Johansen a, b, c, Amanda Poste a, Ian Allan c, Anita Evenset d, e, Pernilla Carlsson a, a Norwegian Institute for Water Research, Tromsø, Norway b Norwegian University of Life Sciences, Ås, Norway c Norwegian Institute for Water Research, Oslo, Norway d Akvaplan-niva, Tromsø, Norway e UiT, The Arctic University of Norway, Tromsø, Norway article info abstract Article history: Considerable amounts of previously deposited persistent organic pollutants (POPs) are stored in the Received 20 July 2020 Arctic cryosphere. Transport of freshwater and terrestrial material to the Arctic Ocean is increasing due to Received in revised form ongoing climate change and the impact this has on POPs in marine receiving systems is unknown This 11 March 2021 study has investigated how secondary sources of POPs from land influence the occurrence and fate of Accepted 13 March 2021 POPs in an Arctic coastal marine system. Available online 17 March 2021 Passive sampling of water and sampling of riverine suspended particulate matter (SPM) and marine sediments for analysis of polychlorinated biphenyls (PCBs) and hexachlorobenzene (HCB) was carried out Keywords: Particle transport in rivers and their receiving fjords in Isfjorden system in Svalbard. Riverine SPM had low contaminant < S e Terrestrial runoff concentrations ( level of detection-28 pg/g dw PCB14,16 100 pg/g dw HCB) compared to outer marine Environmental contaminants sediments 630-880 pg/g dw SPCB14,530e770 pg/g dw HCB). -
Seasonal Dynamics of the Marine CO System in Adventfjorden, a West
RESEARCH ARTICLE Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord Ylva Ericson1,2, Melissa Chierici1,3, Eva Falck1,2, Agneta Fransson4, Elizabeth Jones3 & Svein Kristiansen5 1Department of Arctic Geophysics, University Centre in Svalbard, Longyearbyen, Norway; 2Geophysical Institute, University of Bergen, Bergen, Norway; 3Institute of Marine Research, Fram Centre, Tromsø, Norway; 4Norwegian Polar Institute, Fram Centre, Tromsø, Norway; 5Department of Arctic and Marine Biology, UiT—The Arctic University of Norway, Tromsø, Norway Abstract Keywords Marine carbonate system; aragonite; Time series of the marine CO2 system and related parameters at the IsA Sta- net community production; Arctic fjord tion, by Adventfjorden, Svalbard, were investigated between March 2015 biogeochemistry; Svalbard and November 2017. The physical and biogeochemical processes that govern changes in total alkalinity (TA), total dissolved inorganic carbon (DIC) and the Correspondence Ylva Ericson, Department of Arctic saturation state of the calcium carbonate mineral aragonite (ΩAr) were assessed on a monthly timescale. The major driver for TA and DIC was changes in salin- Geophysics, University Centre in Svalbard, ity, caused by river runoff, mixing and advection. This accounted for 77 and PO Box 156, NO-9171 Longyearbyen, Norway. E-mail: [email protected] 45%, respectively, of the overall variability. It contributed minimally to the variability in ΩAr (5%); instead, biological activity was responsible for 60% of Abbreviations the monthly variations. For DIC, the biological activity was also important, con- ArW: Arctic water; AW: Atlantic water; tributing 44%. The monthly effect of air–sea CO2 fluxes accounted for 11 and CC: coastal current; CTD: conductivity– temperature–depth instrument; DIC: 15% of the total changes in DIC and ΩAr, respectively. -
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.. -
Youth Guide to Biodiversity
SPECIES ECOSYSTEMS HABITATS SOILS CLOUDS LAKES RIVERS MOUNTAINS HUMANS INSECTS MAMMALS OCEANS BIRDS FISHES WORMS PLANTS FLOWERS BEES ACTIONS HABITS ORGANIZATIONS SPECIES ECOSYSTEMS HABITATS SOILS CLOUDS LAKES RIVERS MOUNTAINS HUMANS INSECTS MAMMALS OCEANS BIRDS FISHES WORMS PLANTS FLOWERS BEES ACTIONS HABITS ORGANIZATIONS SPECIES ECOSYSTEMS HABITATS SOILS CLOUDS LAKES RIVERS MOUNTAINS HUMANS INSECTS YOUTH AND UNITED NATIONS GLOBAL ALLIANCE LEARNING AND ACTION SERIES MAMMALS OCEANS BIRDS FISHES WORMS PLANTS FLOWERS BEES ACTIONS HABITS ORGANIZATIONS SPECIES ECOSYSTEMS HABITATS SOILS CLOUDS LAKES RIVERS YOUTH AND UNITED NATIONS GLOBAL ALLIANCE LEARNING AND ACTION SERIES SUPPORTED BY MOUNTAINS HUMANS INSECTS MAMMALS OCEANS BIRDS FISHES WORMS PLANTS FLOWERS BEES ACTIONS HABITS ORGANIZATIONS SPECIES ECOSYSTEMS HABITATS TAKE ACTION FOR BIODIVERSITY! THE TO SOILS CLOUDS LAKES RIVERS MOUNTAINS HUMANS INSECTS MAMMALS OCEANS BIRDS FISHES WORMS PLANTS FLOWERS BEES ACTIONS HABITS ORGANIZATIONS SPECIES ECOSYSTEMS HABITATS SOILS CLOUDS LAKES RIVERS MOUNTAINS HUMANS INSECTS MAMMALS OCEANS BIRDS FISHES WORMS PLANTS FLOWERS BEES YOUTHGUIDE BIODIVERSITY ACTIONS HABITSWE ORGANIZATIONS ARE SPECIES ECOSYSTEMS MANY HABITATS SOILS CLOUDS LAKES RIVERS MOUNTAINS HUMANS INSECTS MAMMALS OCEANS BIRDS FISHES WORMS PLANTS FLOWERS BEES ACTIONS HABITS ORGANIZATIONS SPECIES ECOSYSTEMS HABITATS SOILS CLOUDS LAKES RIVERS MOUNTAINS HUMANS INSECTS MAMMALS OCEANS BIRDS FISHES WORMS PLANTS FLOWERS BEES ACTIONS HABITS ORGANIZATIONSwww. SPECIES ECOSYSTEMS HABITATS SOILS CLOUDS -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Appendix: Economic Geology: Exploration for Coal, Oil and Minerals
Downloaded from http://mem.lyellcollection.org/ by guest on October 1, 2021 PART 4 Appendix: Economic geology: exploration for coal, oil and Glossary of stratigraphic names, 463 minerals, 449 References, 477 Index of place names, 455 General Index, 515 Alkahornet, a distinctive landmark on the northwest, entrance to Isfjorden, is formed of early Varanger carbonates. The view is from Trygghamna ('Safe Harbour') with CSE motorboats Salterella and Collenia by the shore, with good anchorage and easy access inland. Photo M. J. Hambrey, CSE (SP. 1561). Routine journeys to the fjords of north Spitsbergen and Nordaustlandet pass by the rocky coastline of northwest Spitsbergen. Here is a view of Smeerenburgbreen from Smeerenburgfjordenwhich affords some shelter being protected by outer islands. On one of these was Smeerenburg, the principal base for early whaling, hence the Dutch name for 'blubber town'. Photo N. I. Cox, CSE 1989. Downloaded from http://mem.lyellcollection.org/ by guest on October 1, 2021 The CSE motorboat Salterella in Liefdefjorden looking north towards Erikbreen with largely Devonian rocks in the background unconformably on metamorphic Proterozoic to the left. Photo P. W. Web, CSE 1989. Access to cliffs and a glacier route (up Hannabreen) often necessitates crossing blocky talus (here Devonian in foreground) and then possibly a pleasanter route up the moraine on to hard glacier ice. Moraine generally affords a useful introduction to the rocks to be traversed along the glacial margin. The dots in the sky are geese training their young to fly in V formation for their migration back to the UK at the end of the summer. -
AMNH Digital Library
"^^ Ji\!*"^ ^i r ^ THE GREATEST RISK IS NOT TAKING ONE. for years? What does it take to break through a foundation of thinking that's been accepted all A bold stroke. But, it doesn't mean turning things on their heads without understanding the possible consequences, it takes a complete understanding of what lies on the other side. No one is in a better position to help guide clients than AiG. With operations in 130 countries and jurisdictions throughout the world, we have an unmatched knowledge of local conditions and regulations to help manage risks. So, when you're ready to take on a risky venture, contact AIG. We'll help knock down the barriers that may be holding you back. WORLD LEADERS IN INSURANCE AND FINANCIAL SERVICES AIG Insurance and services provided by members of American International Group. Inc.. 70 Pine Street, Department A, New York. New York 10270. With Bristol-Myers Squibb research, , a tiny pair of chromosomes could make a huge difference to this pair of Armstrongs. W" 4^ ^>i, '•^l ^ii^S^BKmKEt ^^W«» mmm^m^^' ";'*•" mmmmam m;s!J5i-i'iw^.^ "''^''. Three-time Tour de France winner ^i''^v% • Lance Armstrong, with his son Luke. gj^^2 ^'^^^^^^^^'^^-i'^^^S!^iSK jgmLiJmL Five years ago, cyclist Lance Armstrong was diagnosed with testicular cancer. It had already spread to his abdomen, lungs and brain. But with aggressive treatments, including three Bristol-Myers Squibb medicines. Lance conquered his cancer. He has gone on to win the Tour de France three times, and even to have a wonderful son— Luke. -
Volume 2. Animals
AC20 Doc. 8.5 Annex (English only/Seulement en anglais/Únicamente en inglés) REVIEW OF SIGNIFICANT TRADE ANALYSIS OF TRADE TRENDS WITH NOTES ON THE CONSERVATION STATUS OF SELECTED SPECIES Volume 2. Animals Prepared for the CITES Animals Committee, CITES Secretariat by the United Nations Environment Programme World Conservation Monitoring Centre JANUARY 2004 AC20 Doc. 8.5 – p. 3 Prepared and produced by: UNEP World Conservation Monitoring Centre, Cambridge, UK UNEP WORLD CONSERVATION MONITORING CENTRE (UNEP-WCMC) www.unep-wcmc.org The UNEP World Conservation Monitoring Centre is the biodiversity assessment and policy implementation arm of the United Nations Environment Programme, the world’s foremost intergovernmental environmental organisation. UNEP-WCMC aims to help decision-makers recognise the value of biodiversity to people everywhere, and to apply this knowledge to all that they do. The Centre’s challenge is to transform complex data into policy-relevant information, to build tools and systems for analysis and integration, and to support the needs of nations and the international community as they engage in joint programmes of action. UNEP-WCMC provides objective, scientifically rigorous products and services that include ecosystem assessments, support for implementation of environmental agreements, regional and global biodiversity information, research on threats and impacts, and development of future scenarios for the living world. Prepared for: The CITES Secretariat, Geneva A contribution to UNEP - The United Nations Environment Programme Printed by: UNEP World Conservation Monitoring Centre 219 Huntingdon Road, Cambridge CB3 0DL, UK © Copyright: UNEP World Conservation Monitoring Centre/CITES Secretariat The contents of this report do not necessarily reflect the views or policies of UNEP or contributory organisations.