Geoscience Atlas of Svalbard

Total Page:16

File Type:pdf, Size:1020Kb

Geoscience Atlas of Svalbard Report Series No. 148 Rapportserie nr. 148 Winfried K. Dallmann (Editor) Geoscience Atlas of Svalbard Norsk Polarinstitutt er Norges hovedinstitusjon for kartlegging, miljoovervaking og forvaltningsrettet forskning i Arktis og Antarktis Instituttet er faglig og srrategisk radgiver i miljovernsaker i disse omradene og nar forvaltningsmyndighet i norsk del av Antarktis. Instituttet er et direktorat under Klima- og miljodepartementet. The Norwegian Polar Institute is Norway's central governmental institution for management-related research, mapping and environmental monitoring in the Arctic and the Antarctic. The Institute advises Norwegian authorities on matters concerningpolar environmental management and is the official environmental management body for Norway's Antarctic territorial claims. The institute is a Directorate within the Ministry of Climate and Environment. Contents Authors. Initials and acronyms for photo and author references 2 Preface and introduction 3 Contents 4 CHAPTER 1: HISTORY OF GEOSCIENTIFIC EXPLORATION l-l Early discovery 1-2 19th century pioneers 10 1-3 Early 20th century 12 1-4 Post-war era (1945-1978) 14 1-5 Exploration since 1979 16 CHAPTER 2: PHYSICAL GEOGRAPHY 19 2-1: Physical geography of the Arctic 20 2-2: Bathymetry of Svalbard's environs 24 2-3: Physical geography of Svalbard 28 CHAPTER 3: OCEAN AND SEA ICE 31 3-1: Ocean currents and distribution of water masses 32 3-2: Sea ice 36 CHAPTER 4: GLACIERS 43 4-1: Glaciers in Svalbard 44 4-2: Glacier mass balance 48 4-3: Glacier change and surge 50 CHAPTER 5: QUATERNARY GEOLOGY AND GEOMORPHOLOGY 53 5-1: Landscapes 54 5-2: Arctic landforms 58 5-3: Changing landscapes 62 5-4: Permafrost 66 5-5: Karst and thermokarst 68 5-6: Superficial deposits 72 5-7: Glacial geology 74 5-8: Fjord bathymetry and geology 78 CHAPTER 6: HISTORICAL GEOLOGY 89 6-1 Geological timescale 90 6-2 Pre-Caledonian era 94 6-3 Caledonian period 98 6-4 Devonian 102 6-5 Carboniferous 106 6-6 Permian 110 6-7 Triassic 114 6-8 Jurassic 118 6-9 Cretaceous 122 6-10: Palaeogene 126 6-11: Neogene and Quaternary 130 CHAPTER 7: BEDROCK GEOLOGY 133 7-1: Geology of Svalbard's environs 134 7-2: Stratigraphy of Svalbard 136 7-3: Rock types of Svalbard 138 7-4: Geological map of Svalbard 142 7-5: Cross sections 170 CHAPTER 8: TECTONICS AND TECTONOTHERMAL EVENTS 175 8-1: Tectonic terranes of the Arctic 176 8-2: Tectonic provinces of Svalbard 180 8-3: Long-lived fault zones 182 8-4: Basement provinces of northern Svalbard 186 8-5: Basement of southwestern Svalbard 190 8-6: West Spitsbergen Fold Belt 194 8-7: Devonian basins 198 8-8: Carboniferous basins 202 8-9: Palaeogene basins 206 8-10: Metamorphism and igneous activity 210 8-11: Neogene-Quaternary volcanism and thermal springs 214 8-12: Glossary of tectonic and structural geological terms 220 CHAPTER 9: GEOPHYSICS 225 9-1: Seismicity 226 9-2: Gravimetry 230 9-3: Geomagnetism 234 9-4: Magnetic declination 238 CHAPTER 10: GEOCHEMISTRY OF SUPERFICIAL DEPOSITS 241 Main and trace element distribution 242 CHAPTER 11: GEORESOURCES 249 11-1: History of resource exploitation 250 11-2: Mineral deposits 254 11-3: Coal 255 11-4: Hydrocarbons 257 CHAPTER 12: MANAGEMENT AND INFRASTRUCTURE 259 12-1: Management 260 12-2: Infrastructure 262 Bibliography 267 Index 281 .
Recommended publications
  • Or Later, but Before 1650] 687X868mm. Copper Engraving On
    60 Willem Janszoon BLAEU (1571-1638). Pascaarte van alle de Zécuften van EUROPA. Nieulycx befchreven door Willem Ianfs. Blaw. Men vintfe te coop tot Amsterdam, Op't Water inde vergulde Sonnewÿser. [Amsterdam, 1621 or later, but before 1650] 687x868mm. Copper engraving on parchment, coloured by a contemporary hand. Cropped, as usual, on the neat line, to the right cut about 5mm into the printed area. The imprint is on places somewhat weaker and /or ink has been faded out. One small hole (1,7x1,4cm.) in lower part, inland of Russia. As often, the parchment is wavy, with light water staining, usual staining and surface dust. First state of two. The title and imprint appear in a cartouche, crowned by the printer's mark of Willem Jansz Blaeu [INDEFESSVS AGENDO], at the center of the lower border. Scale cartouches appear in four corners of the chart, and richly decorated coats of arms have been engraved in the interior. The chart is oriented to the west. It shows the seacoasts of Europe from Novaya Zemlya and the Gulf of Sydra in the east, and the Azores and the west coast of Greenland in the west. In the north the chart extends to the northern coast of Spitsbergen, and in the south to the Canary Islands. The eastern part of the Mediterranean id included in the North African interior. The chart is printed on parchment and coloured by a contemporary hand. The colours red and green and blue still present, other colours faded. An intriguing line in green colour, 34 cm long and about 3mm bold is running offshore the Norwegian coast all the way south of Greenland, and closely following Tara Polar Arctic Circle ! Blaeu's chart greatly influenced other Amsterdam publisher's.
    [Show full text]
  • Ortelius's Typus Orbis Terrarum (1570)
    Ortelius’s Typus Orbis Terrarum (1570) by Giorgio Mangani (Ancona, Italy) Paper presented at the 18th International Conference for the History of Cartography (Athens, 11-16th July 1999), in the "Theory Session", with Lucia Nuti (University of Pisa), Peter van der Krogt (University of Uthercht), Kess Zandvliet (Rijksmuseum, Amsterdam), presided by Dennis Reinhartz (University of Texas at Arlington). I tried to examine this map according to my recent studies dedicated to Abraham Ortelius,1 trying to verify the deep meaning that it could have in his work of geographer and intellectual, committed in a rather wide religious and political programme. Ortelius was considered, in the scientific and intellectual background of the XVIth century Low Countries, as a model of great morals in fact, he was one of the most famous personalities of Northern Europe; he was a scholar, a collector, a mystic, a publisher, a maps and books dealer and he was endowed with a particular charisma, which seems to have influenced the work of one of the best artist of the time, Pieter Bruegel the Elder. Dealing with the deep meaning of Ortelius’ atlas, I tried some other time to prove that the Theatrum, beyond its function of geographical documentation and succesfull publishing product, aimed at a political and theological project which Ortelius shared with the background of the Familist clandestine sect of Antwerp (the Family of Love). In short, the fundamentals of the familist thought focused on three main points: a) an accentuated sensibility towards a mysticism close to the so called devotio moderna, that is to say an inner spirituality searching for a direct relation with God.
    [Show full text]
  • Snake in the Clouds: a New Nearby Dwarf Galaxy in the Magellanic Bridge ∗ Sergey E
    MNRAS 000, 1{21 (2018) Preprint 19 April 2018 Compiled using MNRAS LATEX style file v3.0 Snake in the Clouds: A new nearby dwarf galaxy in the Magellanic bridge ∗ Sergey E. Koposov,1;2 Matthew G. Walker,1 Vasily Belokurov,2;3 Andrew R. Casey,4;5 Alex Geringer-Sameth,y6 Dougal Mackey,7 Gary Da Costa,7 Denis Erkal8, Prashin Jethwa9, Mario Mateo,10, Edward W. Olszewski11 and John I. Bailey III12 1McWilliams Center for Cosmology, Carnegie Mellon University, 5000 Forbes Ave, 15213, USA 2Institute of Astronomy, University of Cambridge, Madingley road, CB3 0HA, UK 3Center for Computational Astrophysics, Flatiron Institute, 162 5th Avenue, New York, NY 10010, USA 4School of Physics and Astronomy, Monash University, Clayton 3800, Victoria, Australia 5Faculty of Information Technology, Monash University, Clayton 3800, Victoria, Australia 6Astrophysics Group, Physics Department, Imperial College London, Prince Consort Rd, London SW7 2AZ, UK 7Research School of Astronomy and Astrophysics, Australian National University, Canberra, ACT 2611, Australia 8Department of Physics, University of Surrey, Guildford, GU2 7XH, UK 9European Southern Observatory, Karl-Schwarzschild-Str. 2, 85748 Garching, Germany 10Department of Astronomy, University of Michigan, 311 West Hall, 1085 S University Avenue, Ann Arbor, MI 48109, USA 11Steward Observatory, The University of Arizona, 933 N. Cherry Avenue., Tucson, AZ 85721, USA 12Leiden Observatory, Leiden University, Niels Bohrweg 2, 2333 CA Leiden, The Netherlands Accepted XXX. Received YYY; in original form ZZZ ABSTRACT We report the discovery of a nearby dwarf galaxy in the constellation of Hydrus, between the Large and the Small Magellanic Clouds. Hydrus 1 is a mildy elliptical ultra-faint system with luminosity MV 4:7 and size 50 pc, located 28 kpc from the Sun and 24 kpc from the LMC.
    [Show full text]
  • Map Projections
    Map Projections Chapter 4 Map Projections What is map projection? Why are map projections drawn? What are the different types of projections? Which projection is most suitably used for which area? In this chapter, we will seek the answers of such essential questions. MAP PROJECTION Map projection is the method of transferring the graticule of latitude and longitude on a plane surface. It can also be defined as the transformation of spherical network of parallels and meridians on a plane surface. As you know that, the earth on which we live in is not flat. It is geoid in shape like a sphere. A globe is the best model of the earth. Due to this property of the globe, the shape and sizes of the continents and oceans are accurately shown on it. It also shows the directions and distances very accurately. The globe is divided into various segments by the lines of latitude and longitude. The horizontal lines represent the parallels of latitude and the vertical lines represent the meridians of the longitude. The network of parallels and meridians is called graticule. This network facilitates drawing of maps. Drawing of the graticule on a flat surface is called projection. But a globe has many limitations. It is expensive. It can neither be carried everywhere easily nor can a minor detail be shown on it. Besides, on the globe the meridians are semi-circles and the parallels 35 are circles. When they are transferred on a plane surface, they become intersecting straight lines or curved lines. 2021-22 Practical Work in Geography NEED FOR MAP PROJECTION The need for a map projection mainly arises to have a detailed study of a 36 region, which is not possible to do from a globe.
    [Show full text]
  • Cartographer's Experience of Time in the Mercator-Hondius Atlas (1606
    JANNE TUNTURI Cartographer’s experience of time in the Mercator-Hondius Atlas (1606, 1613) his article analyses the articulations of tempor­ The Mercator-Hondius Atlas is the work of two ality in the Mercator­Hondius Atlas. Firstly, cartographers who belonged to different generations; Tthe atlas reflects the sense of the past as the Gerardus Mercator (1512–94) was fifty years older cartog raphers had to assess the information included than Jodocus Hondius (1563–1612). Moreover, the in ancient texts in relation to modern testimonies. Sec­ scale of the atlases differed considerably, as Mercator’s ondly, Hondius had to take into account the worldview edition mapped only European countries (with not- provided by the explorers in the fifteenth and sixteenth able omissions such as Spain), while Hondius’ edi- centuries. Hence the experience of time articulated tion was universal. Mercator drew maps for his atlas in the Mercator­Hondius Atlas reflected not only the in the 1560s and the 1570s. The unfinished Atlas sive cartog raphers’ ideas of the Dutch cartographic industry cosmo graphicae meditationes de fabrica mundi et fab- but also directed the making of the atlas. ricati figura was published posthumously in 1595. In 1606 Hondius utilised the copperplates on Mercator’s maps he had bought together with Cornelis Claesz. The Mercator-Hondius Atlas, published by and added maps, some of his own, to compile an atlas Jodocus Hondius in 1606, summarises the early-sev- that would be convenient and met current standards. enteenth-century Dutch golden age of map-making, (Van der Krogt 1995: 115–16) famous for the skilled cartographers and the atlases During the publication of Mercator’s and Hondius’ it produced.
    [Show full text]
  • The European Towns in Braun & Hogenberg's Town Atlas, 1572-1617
    Belgeo Revue belge de géographie 3-4 | 2008 Formatting Europe – Mapping a Continent Mapping the towns of Europe: The European towns in Braun & Hogenberg’s Town Atlas, 1572-1617 Cartographie des villes d’Europe: Les villes européennes dans l’Atlas des Villes de Braun et Hogenberg, 1572-1617 Peter van der Krogt Electronic version URL: http://journals.openedition.org/belgeo/11877 DOI: 10.4000/belgeo.11877 ISSN: 2294-9135 Publisher: National Committee of Geography of Belgium, Société Royale Belge de Géographie Printed version Date of publication: 31 December 2008 Number of pages: 371-398 ISSN: 1377-2368 Electronic reference Peter van der Krogt, “Mapping the towns of Europe: The European towns in Braun & Hogenberg’s Town Atlas, 1572-1617”, Belgeo [Online], 3-4 | 2008, Online since 22 May 2013, connection on 05 February 2021. URL: http://journals.openedition.org/belgeo/11877 ; DOI: https://doi.org/10.4000/ belgeo.11877 This text was automatically generated on 5 February 2021. Belgeo est mis à disposition selon les termes de la licence Creative Commons Attribution 4.0 International. Mapping the towns of Europe: The European towns in Braun & Hogenberg’s Town A... 1 Mapping the towns of Europe: The European towns in Braun & Hogenberg’s Town Atlas, 1572-1617 Cartographie des villes d’Europe: Les villes européennes dans l’Atlas des Villes de Braun et Hogenberg, 1572-1617 Peter van der Krogt This article is based upon the research for Koeman’s Atlantes Neerlandici, vol. IV: The Town Atlases, in preparation, scheduled for publication late 2009. Introduction “The Civitates is one of the great books of the World, (...) a wonderful compendium of knowledge of life in Europe in the sixteenth century, (...) it gives a visual printed record of mediaeval Europe, and is one of the most valuable sources remaining to the student and historian of these periods” (R.V.Tooley)1.
    [Show full text]
  • The Part Borne by the Dutch in the Discovery of Australia 1606-1765
    THE PART BORNE BY THE DUTCH IN THE DISCOVERY OF AUSTRALIA 1606-1765. BY J. E. HEERES, LL. D. PROFESSOR AT THE DUTCH COLONIAL INSTITUTE DELFT PUBLISHED BY THE ROYAL DUTCH GEOGRAPHICAL SOCIETY IN COMMEMORATION OF THE XXVth ANNIVERSARY OF ITS FOUNDATION (No. 19. Little map of the world from the Journal of the Nassau fleet, 1626) LONDON LUZAC & CO, 46 GREAT RUSSELL STREET W. C. 1899 (ebook produced by Colin Choat) CONTENTS. Page Images in English Page Images in Dutch List of books, discussed or referred to in the work List of Maps and Figures Introduction DOCUMENTS: I. Dutch notions respecting the Southland in 1595 II. Notices of the south-coast of New Guinea in 1602 III. Voyage of the ship Duifken under command of Willem Jansz(oon) and Jan Lodewijkszoon Rosingeyn to New Guinea.--Discovery of the east-coast of the present Gulf of Carpentaria (1605-1606) IV. Fresh expedition to New Guinea by the ship Duifken (1607) V. Voyage of the ships Eendracht and Hoorn, commanded by Jacques Le Maire and Willem Corneliszoon Schouten through the Pacific Ocean and along the north-coast of New Guinea (1616) VI. Project for the further discovery of the Southland--Nova Guinea (1616) VII. Voyage of de Eendracht under command of Dirk Hartogs(zoon). Discovery of the West-coast of Australia in 1616: Dirk Hartogs-island and -road, Land of the Eendracht or Eendrachtsland (1616) VIII. Voyage of the ship Zeewolf, from the Netherlands to India, under the command of supercargo Pieter Dirkszoon and skipper Haevik Claeszoon van Hillegom.--Further discovery of the West-coast of Australia (1618) IX.
    [Show full text]
  • Understanding Map Projections
    Understanding Map Projections GIS by ESRI ™ Copyright © 19942000 Environmental Systems Research Institute, Inc All rights reserved Printed in the United States of America The information contained in this document is the exclusive property of Environmental Systems Research Institute, Inc This work is protected under United States copyright law and other international copyright treaties and conventions No part of this work may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying and recording, or by any information storage or retrieval system, except as expressly permitted in writing by Environmental Systems Research Institute, Inc All requests should be sent to Attention: Contracts Manager, Environmental Systems Research Institute, Inc , 380 New York Street, Redlands, CA 92373-8100, USA The information contained in this document is subject to change without notice US GOVERNMENT RESTRICTED/LIMITED RIGHTS Any software, documentation, and/or data delivered hereunder is subject to the terms of the License Agreement In no event shall the U S Government acquire greater than RESTRICTED/LIMITED RIGHTS At a minimum, use, duplication, or disclosure by the U S Government is subject to restrictions as set forth in FAR §52 227-14 Alternates I, II, and III (JUN 1987); FAR §52 227-19 (JUN 1987) and/or FAR §12 211/12 212 (Commercial Technical Data/Computer Software); and DFARS §252 227-7015 (NOV 1995) (Technical Data) and/or DFARS §227 7202 (Computer Software), as applicable Contractor/Manufacturer
    [Show full text]
  • Europe: Glaciers of Svalbard, Norway
    Glaciers of Europe- GLACIERS OF SVALBARD, NORWAY By OLAV LIESTØL SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386-E-5 Svalbard, Norway, an archipelago in the North Atlantic Ocean, has more than 2,100 glaciers that cover 36,591 square kilometers, or 59 percent of the total area of the islands; images have been used to monitor fluctuations in the equilibrium line and glacier termini and to revise maps CONTENTS Page Abstract.............................................................................. E127 Introduction......................................................................... 127 FIGURE 1. Index map showing the location of Svalbard, the islands that make up the archipelago, the areas covered by glaciers, and the glaciers mentioned in the text .................... 128 TABLE 1. Area encompassed by glaciers on each of the islands in the Svalbard archipelago ........................................ 129 Previous glacier investigations ................................................ 127 FIGURE 2. Index to photogrammetric satellite image and map coverage of glaciers of Svalbard and location of mass-balance measurements made by Norwegian and Soviet glaciologists ................................................. 130 3. Color terrestrial photograph of the grounded front of the Kongsvegen glacier at the head of Kongsfjorden, Spitsbergen, in August 1974 ............................... 131 4. Radio-echosounding cross section (A-A') through
    [Show full text]
  • GERARDUS MERCATOR RUPELMUNDANUS Cartographer & Renaissance Man Carlos Van Caiiwenherghe Former Head of Hydrographic Service, Belgium
    page 16 bU''0 GERARDUS MERCATOR RUPELMUNDANUS Cartographer & Renaissance Man Carlos van Caiiwenherghe Former Head of Hydrographic Service, Belgium Introduction An insight into the life of Geradus Mercator (1512-1594) can be found via several basic sources Firstly, there is his biography published in 1595 by his friend, Walter Ghim, Mayor of Duisburg in Germany This introduced his celebrated Atlas ctmtaining 107 maps (Mercator, 1595) published after Mercator's death by his son, Rumold Secondly, there is his surviving correspondence and there are also accounts of his life by other contemporaries such as the cartographer Abraham Ortelius (1527-1598) and the Flemish historian, Antonius Sanderus (1586-1664) Additionally, much historical information was provided by Mercator himself, mainly in the form of prefaces to his works or as notes on his many maps while the archives of the University of Louvain also provide additional details on this very talented and versatile Renaissance man Mainly revered as a cartographer. Mercator was nonetheless noted for many other abilities He was, for instance, an accomplished mathematician, philosopher, metaphysic, theologian, historian, geographer, land surveyor, engraver, instrument maker, calligrapher, astronomer and cosmographer But it was not until the 19th century that his true importance was rediscovered Childhood and education In Antwerp, Mercator first met the such as copper and wood At the same Gerardus Mercator (or Gerard de Oenier Flemish astronomer and cartographer, time he pursued studies in mathematics
    [Show full text]
  • Mass Balance of Austre Grønfjordbreen, Svalbard, 2006–2020, Estimated by Glaciological, Geodetic and Modeling Aproaches
    geosciences Article Mass Balance of Austre Grønfjordbreen, Svalbard, 2006–2020, Estimated by Glaciological, Geodetic and Modeling Aproaches Nelly Elagina 1,*, Stanislav Kutuzov 1 , Ekaterina Rets 2, Andrei Smirnov 1, Robert Chernov 1, Ivan Lavrentiev 1 and Bulat Mavlyudov 1 1 Institute of Geography, Russian Academy of Science, Moscow 119017, Russia; [email protected] (S.K.); [email protected] (A.S.); [email protected] (R.C.); [email protected] (I.L.); [email protected] (B.M.) 2 Institute of Water Problems, Russian Academy of Science, Moscow 119333, Russia; [email protected] * Correspondence: [email protected] Abstract: Glacier mass balance measurements, reconstructions and modeling are the precondition for assessing glacier sensitivity to regional climatic fluctuations. This paper presents new glaciological and geodetic mass balance data of Austre Grønfjordbreen located in the western part of Nordenskiöld Land in Central Spitsbergen. The average annual mass balance from 2014 to 2019 was −1.59 m w.e. The geodetic mass balance from 2008 to 2017 was −1.34 m w.e. The mass balance was also reconstructed by the temperature-index model from 2006 to 2020 and by spatially-distributed energy- − balance models for 2011–2015 and 2019. We found a cumulative mass balance of 21.62 m w.e. over 2006–2020. The calculated mass-balance sensitivity to temperature was −1.04 m w.e. ◦C−1, which Citation: Elagina, N.; Kutuzov, S.; corresponds to the highest glacier mass balance sensitivity among Svalbard glaciers. Sensitivity to Rets, E.; Smirnov, A.; Chernov, R.; precipitation change was 0.10 m w.e. for a 10% increase in precipitation throughout the balance year.
    [Show full text]
  • GERARDUS MERCATOR (March 5, 1512 – December 2, 1594) by HEINZ KLAUS STRICK, Germany
    GERARDUS MERCATOR (March 5, 1512 – December 2, 1594) by HEINZ KLAUS STRICK, Germany The Belgian stamp of 1962 shows GERARDUS MERCATOR. In his hands he holds a globe with the outlines of America and East Asia. MERCATOR is considered the most important cosmographer of the 16th century (that is: "world describer"; from the Greek kosmos and graphein). His work became the basis for the development of the science of geography and cartography. In order to become independent of Arab, Ottoman and Venetian intermediaries, Portuguese navigators had begun to seek new routes to India. Under HENRY THE NAVIGATOR the coast of West Africa had been explored, and BARTOLOMEU DIAS was the first to sail round the southern tip of Africa in 1487. After the Reconquista, the Spanish also appeared on the scene and on their behalf, the Genoese CHRISTOPHER COLUMBUS sailed west in 1492 to find a new sea route to India. On the basis of CLAUDIUS PTOLEMY's Geographia this was based on the assumption that Europe's east-west distance from Asia was too small. Around 150 AD, PTOLEMY had introduced the system of terrestrial longitude and latitude, which is still used today, and had recorded the coordinates of numerous places on the known globe in a catalogue. Since then, it was assumed that only about half of the earth was "known" (Europe, Asia and Africa). Thus the globe of the Nuremberg cloth merchant MARTIN BEHAIM from 1492 shows only the "known" part of the earth, the back of the globe is not inscribed (stamp on the left). The world map by MARTIN WALDSEEMÜLLER from 1507, however, already contained the newly discovered continent.
    [Show full text]