Fyrliste for Svalbard
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
Meddelelser139.Pdf
MEDDELELSER NR. 139 Soviet Geological Research in Svalbard 1962-1992 Extended abstracts of unpublished reports Edited by: A.A. Krasil'scikov Polar Marine Geological Research Expedition NORSK POLARINSTITUTT OSLO 1996 Sponsored by: Russian-Norwegian Joint Venture "SEVOTEAM", St.Petersburg lAse Secretariat, Oslo ©Norsk Polarinstitutt, Oslo 1996 Compilation: AAKrasil'sCikov, M.Ju.Miloslavskij, AV.Pavlov, T.M.Pcelina, D.V.Semevskij, AN.Sirotkin, AM.Teben'kov and E.p.Skatov: Poljamaja morskaja geologorazvedocnaja ekspedicija, Lomonosov - St-Peterburg (Polar Marine Geological Research Expedition, Lomonosov - St.Petersburg) 189510, g. Lomonosov, ul. Pobedy, 24, RUSSIA Figures drawn by: N.G.Krasnova and L.S.Semenova Translated from Russian by: R.V.Fursenko Editor of English text: L.E.Craig Layout: W.K.Dallmann Printed February 1996 Cover photo: AM. Teben'kov: Field camp in Møllerfjorden, northwestem Spitsbergen, summer 1991. ISBN 82-7666-102-5 2 CONTENTS INTRODUCTORY REMARKS by W.K.DALLMANN 6 PREFACE by A.A.KRASIL'SCIKOV 7 1. MAIN FEATURES OF THE GEOLOGY OF SVALBARD 8 KRASIL'SCIKOV ET 1986: Explanatory notes to a series of geological maps of Spitsbergen 8 AL. 2. THE FOLDED BASEMENT 16 KRASIL'SCIKOV& LOPA 1963: Preliminary results ofthe study ofCaledonian granitoids and Hecla TIN Hoek gneis ses in northernSvalbard 16 KRASIL'SCIKOV& ABAKUMOV 1964: Preliminary results ofthe study of the sedimentary-metamorphic Hecla Hoek Complex and Paleozoic granitoids in centralSpitsbergen and northern Nordaustlandet 17 ABAKUMOV 1965: Metamorphic rocks of the Lower -
Palaeogene Deposits and the Platform Structure of Svalbard
NORSK POLARINSTITUTT SKRIFTER NR. 159 v JU. JA. LIVSIC Palaeogene deposits and the platform structure of Svalbard NORSK POLARINSTITUTT OSLO 1974 DET KONGEUGE DEPARTEMENT FOR INDUSTRI OG IlANDVERK NORSK POLARINSTITUTT Rolfstangveien 12, Snareya, 1330 Oslo Lufthavn, Norway SALG AV B0KER SALE OF BOOKS Bekene selges gjennom bokhandlere, eller The books are sold through bookshops, or bestilles direkte fra : may be ordered directly from: UNlVERSITETSFORLAGET Postboks 307 16 Pall Mall P.O.Box 142 Blindem, Oslo 3 London SW 1 Boston, Mass. 02113 Norway England USA Publikasjonsliste, som ogsa omfatter land List of publications, including maps and og sjekart, kan sendes pa anmodning. charts, wiZ be sent on request. NORSK POLARINSTITUTT SKRIFTER NR.159 JU. JA. LIVSIC Palaeogene deposits and the platform structure of Svalbard NORSK POLARINSTITUTT OSLO 1974 Manuscript received March 1971 Published April 1974 Contents Abstract ........................ 5 The eastern marginal fault zone 25 The Sassendalen monocline ...... 25 AHHOTaU;HH (Russian abstract) 5 The east Svalbard horst-like uplift 25 The Olgastretet trough .. .. .. .. 26 Introduction 7 The Kong Karls Land uplift .... 26 Stratigraphy ..................... 10 The main stages of formation of the A. Interpretation of sections ac- platform structure of the archipelago 26 cording to areas ............ 11 The Central Basin ........... 11 The Forlandsundet area ..... 13 The importance of Palaeogene depo- The Kongsfjorden area ....... 14 sits for oil and gas prospecting in The Renardodden area ...... 14 Svalbard .. .. .. .. .. .. .. 30 B. Correlation of sections ....... 15 Bituminosity and reservoir rock C. Svalbard Palaeogene deposits properties in Palaeogene deposits 30 as part of the Palaeogene depo- Hydrogeological criteria testifying sits of the Polar Basin ...... 15 to gas and oil content of the rocks 34 Tectonic criteria of oil and gas con- Mineral composition and conditions of tent . -
Spitsbergen Nordaustlandet Polhavet Barentshavet
5°0'0"E 10°0'0"E 15°0'0"E 20°0'0"E 25°0'0"E 30°0'0"E 35°0'0"E 81°0'0"N Polhavet Prins Oscars Land Orvin Land Vesle Tavleøya Gustav V Land Nordaustlandet Karl XII-øya Phippsøya Sjuøyane Gustav Adolf Land 80°0'0"N Martensøya Parryøya Kvitøyjøkulen Waldenøya Foynøya Nordkappsundet Kvitøya Repøyane Castrénøyane 434 433 ZorgdragerfjordenDuvefjorden Snøtoppen Nordenskiöldbukta Scoresbyøya Wrighttoppen Brennevinsfjorden 432 Laponiahalvøya Damflya Lågøya Storøya Kvitøyrenna Storøysundet Botniahalvøya Sabinebukta Orvin Land 437 Rijpfjorden Prins Lady Franklinfjorden Maudbreen Oscars Franklinsundet Worsleybreen Sverdrupisen 80°0'0"N Land Andrée Land Rijpbreen Albert I Land Norskebanken Ny-Friesland Storsteinhalvøya Olav V Land Franklinbreane James I Land Oscar II Land 401 Hinlopenrenna Haakon VII Land Gustav V Moffen Celsiusberget Murchisonfjorden Land Rijpdalen Søre Russøya Vestfonna Harald V Land Mosselhalvøya Austfonna Sorgfjorden 436 Heclahuken Gotiahalvøya Nordaustlandet Harald V Land Fuglesongen Oxfordhalvøya Breibogen Bragebreen Etonbreen IdunfjelletWahlenbergfjorden 435 Amsterdamøya Reinsdyrflya 427 Raudfjorden Balberget Hartogbukta Danskøya Vasahalvøya Smeerenburgfjorden Valhallfonna 79°0'0"N Ben Nevis 428 Woodfjorden Reuschhalvøya Palanderbukta Gustav Adolf Liefdefjorden Magdalenefjorden Åsgardfonna Albert I Glitnefonna Roosfjella Wijdefjorden Land 430 431 Hoelhalvøya Scaniahalvøya Land Bockfjorden Lomfjorden Hinlopenstretet Vibehøgdene Lomfjordhalvøya Svartstupa Monacobreen 429 Seidfjellet Svartknausflya Bråsvellbreen 402 Lomfjella Vibebukta -
Twenty of the Most Thermophilous Vascular Plant Species in Svalbard and Their Conservation State
Twenty of the most thermophilous vascular plant species in Svalbard and their conservation state Torstein Engelskjøn, Leidulf Lund & Inger Greve Alsos An aim for conservation in Norway is preserving the Svalbard archi- pelago as one of the least disturbed areas in the Arctic. Information on local distribution, population sizes and ecology is summarized for 20 thermophilous vascular plant species. The need for conservation of north- ern, marginal populations in Svalbard is reviewed, using World Conser- vation Union categories and criteria at a regional scale. Thirteen species reach their northernmost distribution in Svalbard, the remaining seven in the western Arctic. Nine species have 1 - 8 populations in Svalbard and are assigned to Red List categories endangered or critically endangered: Campanula rotundifolia, Euphrasia frigida, Juncus castaneus, Kobresia simpliciuscula, Rubus chamaemorus, Alchemilla glomerulans, Ranuncu- lus wilanderi, Salix lanata and Vaccinium uliginosum, the last four spe- cies needing immediate protective measures. Five species are classifi ed as vulnerable: Betula nana, Carex marina ssp. pseudolagopina, Luzula wahlenbergii, Ranunculus arcticus and Ranunculus pallasii. Six species are considered at lower risk: Calamagrostis stricta, Empetrum nigrum ssp. hermaphroditum, Hippuris vulgaris (only occurring on Bjørnøya), Juncus triglumis, Ranunculus lapponicus and Rhodiola rosea. The warmer Inner Arctic Fjord Zone of Spitsbergen supports most of the 20 target species and is of particular importance for conservation. Endan- gered or vulnerable species were found in a variety of edaphic conditions; thus, several kinds of habitats need protection. T. Engelskjøn, I. G. Alsos, Tromsø Museum, University of Tromsø, NO-9037 Tromsø, Norway, torstein@ tmu.uit.no; L. Lund, Phytotron, University of Tromsø, NO-9037 Tromsø, Norway. -
Nasjonsrelaterte Stedsnavn På Svalbard Hvilke Nasjoner Har Satt Flest Spor Etter Seg? NOR-3920
Nasjonsrelaterte stedsnavn på Svalbard Hvilke nasjoner har satt flest spor etter seg? NOR-3920 Oddvar M. Ulvang Mastergradsoppgave i nordisk språkvitenskap Fakultet for humaniora, samfunnsvitenskap og lærerutdanning Institutt for språkvitenskap Universitetet i Tromsø Høsten 2012 Forord I mitt tidligere liv tilbragte jeg to år som radiotelegrafist (1964-66) og ett år som stasjonssjef (1975-76) ved Isfjord Radio1 på Kapp Linné. Dette er nok bakgrunnen for at jeg valgte å skrive en masteroppgave om stedsnavn på Svalbard. Seks delemner har utgjort halve mastergradsstudiet, og noen av disse førte meg tilbake til arktiske strøk. En semesteroppgave omhandlet Norske skipsnavn2, der noen av navna var av polarskuter. En annen omhandlet Språkmøte på Svalbard3, en sosiolingvistisk studie fra Longyearbyen. Den førte meg tilbake til øygruppen, om ikke fysisk så i hvert fall mentalt. Det samme har denne masteroppgaven gjort. Jeg har også vært student ved Universitetet i Tromsø tidligere. Jeg tok min cand. philol.-grad ved Institutt for historie høsten 2000 med hovedfagsoppgaven Telekommunikasjoner på Spitsbergen 1911-1935. Jeg vil takke veilederen min, professor Gulbrand Alhaug for den flotte oppfølgingen gjennom hele prosessen med denne masteroppgaven om stedsnavn på Svalbard. Han var også min foreleser og veileder da jeg tok mellomfagstillegget i nordisk språk med oppgaven Frå Amarius til Pardis. Manns- og kvinnenavn i Alstahaug og Stamnes 1850-1900.4 Jeg takker også alle andre som på en eller annen måte har hjulpet meg i denne prosessen. Dette gjelder bl.a. Norsk Polarinstitutt, som velvillig lot meg bruke deres database med stedsnavn på Svalbard, men ikke minst vil jeg takke min kjære Anne-Marie for hennes tålmodighet gjennom hele prosessen. -
Nazewnictwo Geograficzne Ś Wiata
NAZEWNICTWO GEOGRAFICZNE NAZEWNICTWO GEOGRAFICZNE Ś WIATA Zeszyt 12 Ś WIATA 12. Europa – Cz WIATA 12. Europa Europa Część II ęść II IISBNSBN 9978-83-254-0825-178-83-254-0825-1 GŁÓWWNYNY UURZRZĄD GGEODEZJIEODEZJI I KKARTOGRAFIIARTOGRAFII OOkladka.inddkladka.indd 226767 66/10/10/10/10 110:13:170:13:17 PPMM KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju NAZEWNICTWO GEOGRAFICZNE ŚWIATA Zeszyt 12 Europa Część II GŁÓWNY URZĄD GEODEZJI I KARTOGRAFII Warszawa 2010 EEuropa2.indburopa2.indb 1 66/10/10/10/10 9:49:219:49:21 PPMM KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju Waldemar Rudnicki (przewodniczący), Andrzej Markowski (zastępca przewodniczącego), Maciej Zych (zastępca przewodniczącego), Katarzyna Przyszewska (sekretarz); członkowie: Stanisław Alexandrowicz, Andrzej Czerny, Janusz Danecki, Janusz Gołaski, Romuald Huszcza, Sabina Kacieszczenko, Dariusz Kalisiewicz, Artur Karp, Zbigniew Obidowski , Jerzy Ostrowski, Jarosław Pietrow, Jerzy Pietruszka, Andrzej Pisowicz, Bogumiła Więcław, Ewa Wolnicz-Pawłowska, Bogusław R. Zagórski Opracowanie Elżbieta Chudorlińska (Belgia, Holandia, Irlandia, Szwajcaria, Szwecja, Wielka Brytania), Andrzej Czerny (Austria, Niemcy), Jarosław Pietrow (Dania, Finlandia, Islandia, Norwegia, Szwecja), Agnieszka Pietrzak (Hiszpania, Malta, Portugalia, Włochy), Maksymilian Skotnicki (Francja), Maciej Zych (Andora, Francja, Gibraltar, Guernsey, Holandia, Jan Mayen, Jersey, Liechtenstein, Luksemburg, -
Ground-Penetrating Radar Studies in Svalbard Aimed to the Calculation of the Ice Volume of Its Glaciers
ISSN 0211-6820 Cuadernos de Investigación Geográfica 2016 Nº 42 (2) pp. 399-414 EISSN 1697-9540 DOI: 10.18172/cig.2929 © Universidad de La Rioja GROUND-PENETRATING RADAR STUDIES IN SVALBARD AIMED TO THE CALCULATION OF THE ICE VOLUME OF ITS GLACIERS F. J. NAVARRO1*, J. LAPAZARAN1, A. MARTÍN-ESPAÑOL2,1, J. OTERO1 1Departamento de Matemática Aplicada a las Tecnologías de la Información y las Comunicaciones, Universidad Politécnica de Madrid, Spain. 2School of Geographical Sciences, Bristol University, United Kingdom. ABSTRACT. During the period 1999-2014, the Group of Numerical Simulation in Sciences and Engineering of Universidad Politécnica de Madrid carried out many ground-penetrating radar campaigns in Svalbard, aimed to the study of glacier ice-thickness and the physical properties of glacier ice. The regions covered were Nordenskiöld Land, Wedel Jarlsberg Land, Sabine Land and Nordaustlandet. We here present a review of these works, focused on the aspects related to the estimate of the volume of individual glaciers and its extrapolation to the entire set of Svalbard glaciers, for which the authors estimate a total volume of 6700±835 km3, or 17±2 mm in sea-level equivalent. Estudios de georradar en Svalbard orientados al cálculo del volumen de hielo de sus glaciares RESUMEN. Durante el periodo 1999-2014, el grupo de Simulación Numérica en Ciencias e Ingeniería de la Universidad Politécnica de Madrid llevó a cabo numerosas campañas de georradar en Svalbard orientadas al estudio del espesor y las propiedades físicas del hielo de sus glaciares. Las regiones cubiertas abar- caron Nordenskiöld Land, Wedel Jarlsberg Land, Sabine Land y Nordaustlandet. -
SVALBARD-BATHYMETRY.Pdf
0Ê 30Ê 10Ê 20Ê m SVALBARD Nansen Basin TOPOGRAPHY AND BATHYMETRY 0 Compilation made by ZBIGNIEW PERSKI Geological Visualization Laboratory at Chair of Fundamental Geology -20 Faculty of Earth Sciences UNIVERSITY OF SILESIA Bedzinska 60, 41-200 Sosnowiec POLAND -50 [email protected] -100 DATA SOURCES BATHYMETRY: Ermak Plateau Litke Trough -150 International Bathymetric Chart of the Arctic Ocean (IBCAO). The goal of this initiative is to develop a digital data base that contains all available bathymetric data north of 64 degrees -200 North, for use by mapmakers, researchers, and others whose work requires a detailed and acurate knowledge of the depth and the shape of the Arctic seabed. Initiated in 1997, this undertaking has so far engaged the volunteer efforts of investigators who are affiliated with -250 eleven institutions in eight countries: Canada, Denmark, Germany, Iceland, Norway, Russia, Quest Channel Quest B Sweden, and the USA. The activity has also been endorsed and/or supported financially by Lena Trough -300 the Intergovernmental Oceanographic Commission (IOC), the International Arctic Science 80Ê Kvitùyra Committee (IASC), the International Hydrographic Organization (IHO), the US Office of Naval 80Ê A Research (ONR), and the US National Geophysical Data Center (NGDC). Baie Nordenskiold -400 T http://www.ngdc.noaa.gov/mgg/bathymetry/arctic/arctic.html Hinlopenrenna H AWI Bathymetric Charts of the Fram Strait (AWI BCFS). Based on data from R/V Polarstern multibeam sonar surveys between 1984 and 1997 we produced a high resolution bathymetry Spitsbergen Trough* -500 Y of the central Fram Strait. The area insonified covers approx. 36,500 km2 between 78oN - 80 o o o Norske Bank N and 0 E - 7.5 E. -
Regulations Relating to Tourism, Field Operations and Other Travel in Svalbard
Regulations relating to tourism, field operations and other travel in Svalbard Section 1 – Purpose The purpose of these Regulations is to regulate tourism, field operations and other travel in Svalbard within the framework of Norwegian Svalbard policy, particularly in order to: a) provide for the safety of tourists and other travellers b) ensure that field operations and travel programmes do not impair the virtually untouched environment of Svalbard with regard to continuous areas of wilderness, landscape, flora, fauna, and cultural heritage c) ensure that field operations and travel programmes take into consideration the general public's experience of Svalbard's wilderness and culture d) ensure compliance with other laws and regulations. Section 2 – Scope The Regulations apply to Svalbard's land territory and sea territory to the limit of the territorial waters. The Ministry of Justice and Public Security may determine that the Regulations shall not apply to particular delimited areas of Svalbard. The Ministry may also issue other special rules for specific geographical areas. Section 3 – Definitions The following definitions apply in these Regulations: a) Tour operator: anyone who, in return for payment, organises travels with accompanying services, or who transports persons within Svalbard for tourist purposes. Payments made to meet actual expenses without any profit being calculated are also regarded as such payment. b) Research and educational institutions: institutes and institutions that are engaged in research and educational programmes, including schools, colleges and universities. c) Management Area 10: Nordenskiöld Land, Sabine Land, Bünsow Land and Dickson Land, bounded to the north and east by Kapp Nathorst, Sophus Liefjellet, Terrierfjellet, Hallberget, Elfenbeinbreen, and Kjellstrømdalen. -
The Geology of Svalbard to Svalbard Colleagues
The Geology of Svalbard To Svalbard Colleagues Geological Society Memoirs Series Editor A. J. FLEET View of Ny-.&lesund settlement seen from the west with three mountain peaks, Tre Kroner, in the distance. The peaks are capped by Carboniferous strata unconformably resting on Early Devonian rocks. They are 30 km distant from the buildings, being foreshortened by the telephoto lens. The glacier from which they emerge as nunataks extends about 15 km nearer. The remaining 15 km just visible is the eastern, inner part of Kongsfjorden. To the right in the foreground is a raised, insulated and heated utiliduct supplying water from a small lake. Photo M. J. Hambrey, CSE 1962 (SP.941e). View WSW from the old road quay at Ny Alesund, with Scheteligf]ellet in the centre right formed mainly of Carboniferous and Permian strata. Typical low cloud is creeping half way up the mountain from the right. The middle foreshortened low tundra with snow is characteristic raised beach or strandflat topography. The cliffs in the foreground usually about 5-10 m high form the coastline of the shallow bay, Thiisbukta, where in somewhat deeper water motorboats have a sheltered anchorage. The ice in the foreground is 'bay ice', which forms each winter and melts in the early summer. After a hard winter (probably in June) this bay ice is grounded in shallow water at low tide. In a few days it would disintegrate and drift away with tide. Photo M. J. Hambrey (SP631). The Geology of Svalbard By W. BRIAN HARLAND (University of Cambridge, UK) Assisted by LESTER M. -
Michael Frank William Holland
NORSK POLARINSTITUTT SKRIFTER NR. 122 MICHAEL FRANK WILLIAM HOLLAND THE GEOLOGY OF CERTAIN PARTS OF EASTERN SPITSBERGEN NORS K POLAR I N STITUTT OSLO 1961 DET KONGELIGE DEPARTEMENT FOR INDUSTRI OG HANDVERK NO RSK POLARI NSTITUTT Observatoriegt. 1, Oslo, Norway Short account of the publications of Norsk Polarinstitutt. The two series published by Norsk Polarinstitutt,SKRIFTERand MEDDELELSER, were taken over from the former institution, Norges Svalbard- og Ishavs-unders0kel ser (NSIU), which was incorporated in Norsk Polarinstitutt, when this was founded in 1948. A third series, Norsk Polarinstitutt -ARBOK, will be published with one volum per year. The first volume will soon appear. SKRIFTER includes scientific papers, published in English, French or German. MEDDELELSER comprises shorter papers, often being reprints from other journals. They are generally in a more popular scale and are mostly published in Norwegian. SKRIFTER has in the past been published under various titles: Nos. 1-11. Resultater av De norske statsunderst0ttede Spitsbergen-ekspe disjoner. No. 12. Skrifter om Svalbard og Nordishavet. Nos. 13-81. Skrifter om Svalbard og Ishavet. 82-89. Norges Svalbard- og Ishavs-unders0kelser. Skrifter. 90- . Norsk Polarinstitutt. Skrifter. Further Norsk Polarinstitutt also publishes a special series: NORWEGIAN BRITISH-SWEDISH ANTARCTIC EXPEDITION, 1949-52. SCIENTIFIC RESULTS. This series will consist of 6 vols. By now 20 papers are published, and the series will probably be completed within 1963. Topographical and hydrographical surveying also plays an important part of the work done by Norsk Polarinstitutt. A list of the published maps and charts is found on the back page of SKRIFTER. A complete list of publications (including maps and charts) is enclosed in S KRI FTER No. -
RESEARCH in SVALBARD 2004 a Yearly Information Bulletin Based on Contributions from Scientists Working in Svalbard
RESEARCH IN SVALBARD 2004 A yearly information bulletin based on contributions from scientists working in Svalbard Svalbard Science Forum Longyearbyen 2004 © The Research Council of Norway Title: Research in Svalbard 2004 Editor: Kjell Tore Hansen, Svalbard Science Forum, Longyearbyen Are Bjørdal, Norwegian Polar Institute, Tromsø ISBN: 82-12-01972-1 Order additional copies from: Svalbard Science Forum P.O.Box 506 N-9171 Longyearbyen Norway Tlf: (+47)79022616 Fax: (+47)79022604 E-mail: [email protected] You will be able to view and print the bulletin from: http://www.npolar.no/ris 2 Table of contents Introduction 6 SomeStatistics 7 ProjectReportsforBiology 11 "Digestibility of ice algae and phytoplankton: The potential impacts of changing food supply to the arctic benthos" (Marine Ecology) 11 "On Thin Ice? Climatic Influence on Energy Flow and Trophic Structure in Arctic Marine Ecosystems" (Marine Ecology) 13 Environmental effects of offshore oil activities: Experimental tests of petroleum-associated components on benthos at community, individual, and cellular levels (EXPAC) (Marine Ecology) 15 Description of parameters of the population dynamics of polar bivalve communities, first year: growth and reproductive cycle of the dominant Greenland cockles (Serripes groenlandicus) (Benthology) 17 Food in the Arctic pelagic system, its role in the diet of filter feeders, and fertilisation by exu- dates: an experiment in situ (Benthology) 19 Succession of benthic communities in polar environments: Benthic resilience in polar environments: a comparison