Geographical Investigations in the Management of the Svalbard Environment
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- . - - - . -. � ..;/, 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. -
South Spitsbergen S/V Noorderlicht
South Spitsbergen 28 September – 05 October 2008 on board S/V Noorderlicht The Noorderlicht was originally built in 1910, in Flensburg. For most of her life she served as a light vessel on the Baltic. Then, in 1991 the present owners purchased the ship and re-rigged and re-fitted her thoroughly, according to the rules of ‘Register Holland’. Noorderlicht is 46 metres long and 6.5 metres breadth, a well-balanced, two- masted schooner rig that is able to sail all seas. With: Captain: Gert Ritzema (Netherlands) First mate: Dickie Koolwijk (Netherlands) Second mate: Elisabeth Ritzema (Netherlands) Chef: Anna Kors (Niederlande) Expedition leader: Rolf Stange (Germany) And 19 brave polar explorers from Germany, The Netherlands, Spain, Switzerland and The United Kingdom 28. September 2008 – Longyearbyen Position at 1700: 78°14’N /15°37’E. Calm, 6°C he first bit of arctic soil that we set our feet on was the the runway of the little airport near Longyearbyen and there we met by our fearless leader, Rolf Stange from Germany, who Twas easily identified thanks to a Noorderlicht life ring. Soon we were on a bus on the way to the high arctic metropolis of Longyearbyen, where we still had some hours time to explore the settlement with its various excitements such as museum, supermarket and cafes and restaurants. Around 1700, we boarded the Noorderlicht which was alongside in the harbour of Longyearbyen. We moved into our cabins, stored our luggage away and then met the friendly crew for the first time. Captain Gert and Rolf welcomed us once again, introduced the ship and her crew, gave us some information about life on board and about some important safety issues. -
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. -
Tundra Times 2017
Indigenous Lens: Greenland | Polar Bear Basics | Separating Fact from Fiction Tundra Times The Annual Newsmagazine of Polar Bears International FALL 2017 Tracking Polar Bear Dens in Svalbard photo © Daniel J. Cox/NaturalExposures.com THE COMPASS POINTS NORTH Inside ast February, I joined a Polar Bears International research 3 team on an expedition to study polar bear den sites in Svalbard. Along Lwith partners from the Norwegian Polar Institute and San Diego Zoo Global, we skied to the remote snow dens of polar bear moms and cubs, 4 transporting our gear by traditional sleds called qamutiiks. Visiting the region that has served as photo © Simon Gee a polar bear nursery for hundreds, if not thousands, of years, was an exhilarating experience—but also disconcerting. Normally, the fjords surrounding the island are frozen at that time of year, providing hungry polar bear moms with quick access to their seal-hunting 6 grounds when they emerge with their cubs in spring. Without a platform of ice, the families seemed likely to face a rough spring instead of a time of plenty. Helping the public understand the polar bear’s dependence on sea ice—and the need to take action on climate change—is a core focus 8 of our work at Polar Bears International, whether we’re conducting field research or taking part in conservation outreach. In this year’s Tundra Times, scientist Andrew Derocher takes us through the basics of what it means to be a polar bear, with sea ice playing a central role. The theme appears again as scientists Nicholas 10 Pilfold and Kristen Laidre transport us to Canada, Svalbard, and Greenland. -
The Late Weichselian Glacial Maximum in Western Svalb Ar D
The Late Weichselian glacial maximum in western Svalbar d JAN MANGERUD, MAGNE BOLSTAD, ANNE ELGERSMA, DAG HELLIKSEN, JON Y. LANDVIK, ANNE KATRINE LYCKE, IDA LBNNE, Om0 SALVIGSEN, TOM SANDAHL AND HANS PETTER SEJRUP Mangerud, J., Bolstad, M., Elgersma, A., Helliksen, D., Landvik, J. Y., Lycke, A. K., L~nne,I.. Salvigsen, O., Sandahl, T. & Sejrup, H. P. 1987: The Late Weichselian glacial maximum in western Svalbard. Polar Research 5 n.s., 275-278. Jan Mangerud, Magne Bolstad, Anne Elgersma, Dog Helliksen, Jon Y. Landoik, Anne Katrine Lycke, Ida Lpnne, Tom Sandahl and Hans Pener Sejrup, Department of Geology, Sect. B, Uniuersiry of Bergen, Allkgaten 41, N-5007 Bergen, Norway; Otto Saluigsen, Norsk Polarimtitutt, P.O. Box 158, N-1330 Oslo lufthaun, Norway. The glacial history of Svalbard and the Barents Sea during the Linnkdalen is the westernmost valley on the south shore of Late Weichselian has been much debated during the last few Isfjorden (Fig. 1). All mapped glacial striae and till fabrics years; reviews are presented by Andersen (1981), Boulton et al. indicate an ice movement towards the north, i.e. down valley. (1982), ElverhBi & Solheim (1983) and Vorren & Kristoffersen We assume that they exclude the possibility of an ice stream (1986). In our opinion (Mangerud et al. 1984) it is now demon- coming out of Isfjorden at the time of their formation. Strati- strated that a relatively large ice-sheet complex existed over graphic sequences along the river Linntelva cover much of most of Svalbard and large parts (if not all) of the Barents Sea. the Weichselian; all pebble counts, till fabric analyses and One of the main arguments for a large ice sheet is the pattern sedimentary structures measured in these sediments record a of uplift, including the 9,800 B.P. -
The Flora of Jan Mayen
NORSK POLARINSTITUTT SKRIFTER NR. 130 JOHANNES LID THE FLORA OF JAN MAYEN IlJustrated by DAGNY TANDE LID or1(f t ett} NORSK POLARINSTITUTT OSLO 1964 DET KONGELIGE DEPARTEMENT FOR INDUSTRI OG HÅNDVERK NORSK POLARINSTITUTT Observatoriegt. l, Oslo, Norway Short account of the publications of Norsk Polarinstitutt The two series, Norsk Polarinstitutt - SKRIFTER and Norsk Polarinstitutt - MEDDELELSER, were taken over from the institution Norges Svalbard- og Ishavs undersøkelser (NSIU), which was incorporated in Norsk Polarinstitutt when this was founded in 1948. A third series, Norsk Polarinstitutt - ÅRBOK, is published with one volum(� per year. SKRIFTER includes scientific papers, published in English, French or German. MEDDELELSER comprises shortcr papers, often being reprillts from other publi cations. They generally have a more popular form and are mostly published in Norwegian. SKRIFTER has previously been published under various tides: Nos. 1-11. Resultater av De norske statsunderstuttede Spitsbergen-ekspe. ditioner. No 12. Skrifter om Svalbard og Nordishavet. Nos. 13-81. Skrifter om Svalbard og Ishavet. 82-89. Norges Svalbard- og Ishavs-undersøkelser. Skrifter. 90- • Norsk Polarinstitutt Skrifter. In addition a special series is published: NORWEGIAN-BRITISH-SWEDISH ANTARCTIC EXPEDITION, 1949-52. SCIENTIFIC RESULTS. This series will comprise six volumes, four of which are now completed. Hydrographic and topographic surveys make an important part of the work carried out by Norsk Polarinstitutt. A list of the published charts and maps is printed on p. 3 and 4 of this cover. A complete list of publications, charts and maps is obtainable on request. ÅRBØKER Årbok 1960. 1962. Kr.lS.00. Årbok 1961. 1962. Kr. 24.00. -
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. -
View Travel Planning Guide
YOUR O.A.T. ADVENTURE TRAVEL PLANNING GUIDE® New! Arctic Expedition: Untamed Norway & Svalbard 2021 Small Groups: 20-25 travelers—guaranteed! (average of 22) Overseas Adventure Travel ® The Leader in Personalized Small Group Adventures on the Road Less Traveled 1 Dear Traveler, At last, the world is opening up again for curious travel lovers like you and me. And the O.A.T. New! Arctic Expedition: Untamed Norway & Svalbard itinerary you’ve expressed interest in will be a wonderful way to resume the discoveries that bring us so much joy. You might soon be enjoying standout moments like these: Throughout your cruise, you’ll gain in-depth insights into the mysteries of the Arctic alongside an experienced Expedition Team who will share their expertise with you. They’ll provide vital information about your voyage, lead insightful discussions about the Arctic, and join you on every Zodiac excursion. You’ll also meet with two local experts at the Bellona Foundation—an independent non-profit organization working to identify and implement sustainable environmental solutions—to discuss whether the country is acting heroically, or hypocritically, when it comes to the issue of climate change. Although the country boasts some of the most progressive environmentally-friendly practices around the globe, Norway dredges up more oil per capita than most other countries in the world. Some experts say the country is making a grave misstep on the fight to protect the climate, while others believe there are many benefits to Norway’s oil production. We’ll get a firsthand account from both sides of this controversy with a representative of the Bellona Foundation and a local offshore oil worker. -
Unis|Course Catalogue
1 COURSE UNIS| CATALOGUE the university centre in svalbard 2012-2013 2 UNIS | ARCTIC SCIENCE FOR GLOBAL CHALLENGES UNIS | ARCTIC SCIENCE FOR GLOBAL CHALLENGES 3 INTRODUCTION | 4 map over svalbard ADMISSION REQUIREMENTS | 5 HOW TO APPLY | 7 moffen | ACADEMIC MATTERS | 7 nordaustlandet | ÅsgÅrdfonna | PRACTICAL INFORMATION | 8 newtontoppen | ny-Ålesund | safety | 8 pyramiden | prins Karls | THE UNIS CAMPUS | forland | 8 barentsØya | UNIVERSITY OF THE ARCTIC | longyearbyen | 9 barentsburg | COURSES AT UNIS | isfJord radio | 10 sveagruva | ARCTIC BIOLOGY (AB) | 13 EDGEØYA | storfJorden | ARCTIC GEOLOGY (AG) | 29 hornsund | ARCTIC GEOPHYSICS (AGF) | 67 ARCTIC TECHNOLOGY (AT) SVALBARD | | 85 GENERAL COURSES | 105 4 UNIS | ARCTIC SCIENCE FOR GLOBAL CHALLENGES UNIS | ARCTIC SCIENCE FOR GLOBAL CHALLENGES 5 Semester studies are UNIS OFFERS BACHELOR-, MASTER AND PhD courses available at Bachelor LEVEL COURSES in: level (two courses AT unis | providing a total of ARCTIC BIOLOGY (AB) 30 ECTS). At Master ARCTIC GEOLOGY (AG) and PhD level UNIS offers 3-15 ECTS courses lasting from ARCTIC GEOphYsiCS (AGF) a few weeks to a full semester. In the 2012-2013 academic year, UNIS will be offering altogether 83 courses. An over- ARCTIC TEChnOLOGY (AT) INTRODUCTION view is found in the course table (pages 10-11). The University Centre in Svalbard (UNIS) is the world’s STUDENTS Admission to courses AcaDEMic reQUireMents: northernmost higher education institution, located in at UNIS requires that About 400 students from all over the world attend courses ADMISSION Department of Arctic Biology: Longyearbyen at 78º N. UNIS offers high quality research the applicant is en- annually at UNIS. About half of the students come from 60 ECTS within general natural science, of which 30 ECTS based courses at Bachelor-, Master-, and PhD level in Arctic rolled at Bachelor-, abroad and English is the official language at UNIS. -
Arctic Cruise Svalbard Circumnavigation July 11-23, 2022
ARCTIC CRUISE SVALBARD CIRCUMNAVIGATION JULY 11-23, 2022 ARCTIC CRUISE - 2022 Pollina Tours’ much awaited cruise to the Arctic is now scheduled for July 11-23, 2022. Please mark your calendar and book your space now as booking will only be accepted only on first come first served basis. The goal of this ARCTIC voyage is to circumnavigate Svalbard, a bucket list item for many! During the adventure we will enjoy the immense beauty of Svalbard on this high Arctic voyage among whales, walruses, polar bears and millions of sea birds. We approach the polar bear´s favorite summer residence, as we cruise to 80 degrees north, getting as close as possible to the pack ice north of Svalbard. How far north we reach, and the exact route will depend on the ice conditions, while the many amazing locations along the coasts of Svalbard’s islands are kept navigable by the warm Gulf Stream. Onboard Ocean Atlantic you will experience areas of Svalbard not easily accessible otherwise. But we are not only cruising in the far north, we will also visit some extraordinary locations in the eastern part of Svalbard with Edgeøya and in the south part of Spitsbergen like Bellsund and Hornsund. 1 ARCTIC CRUISE SVALBARD CIRCUMNAVIGATION JULY 11-23, 2022 During the short summer, wildlife such as reindeer is busy amassing energy for the icy polar winter. The cliffs shimmer with life as every surface is populated with countless birds. On several shores, the huge walruses enjoy the short Arctic summer as well as many whales and seals foraging along the edge of the pack ice and the coasts. -
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 .