Crustal Structure Between the Knipovich Ridge and the Van Mijenfjorden (Svalbard)
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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. -
Tertiary Fold-And-Thrust Belt of Spitsbergen Svalbard
Winfried K. Dallmann • Arild Andersen • Steffen G. Bergh • Harmond D. Maher Jr. • Yoshihide Ohta Tertiary fold-and-thrust belt of Spitsbergen Svalbard ' ~dl... ,, !!~"\\ MEDDELELSER NR.128 9,.~,f OSLO 1993 k ·pOlARll'l'>'\ MEDDELELSER NR. 128 WINFRIED K. DALLMANN, ARILD ANDRESEN, STEFFEN G. BERGH, HARMON D. MAHER Jr. & YOSHIHIDE OHTA Tertiary f old-and-thrust belt of Spitsbergen Svalbard COMPILATION MAP, SUMMARY AND BIBLIOGRAPHY NORSK POLARINSTITUTT OSLO 1993 Andresen, Arild: Univ. Oslo, Institutt for geologi, Pb. 1047 Blindern, N-0316 Oslo Bergh, Steffen G.: Univ. Tromsø, Institutt for biologi og geologi, N-9037 Tromsø Dallmann, Winfried K.: Norsk Polarinstitutt, Pb. 5072 Majorstua, N-0301 Oslo Maher, Harmon D., Jr.: Univ. Nebraska, Dept. of Geography and Geology, Omaha, USA-Nebraska 68182-0199 Ohta, Yoshihide: Norsk Polarinstitutt, Pb. 5072 Majorstua, N-0301 Oslo ISBN 82-7666-065-7 Printed December 1993 Cover photo by W. K. Dallmann: Folded Triassic sandstones and shales within the interior part of the Tertiary fold-and-thrust belt at Curie Sklodowskafjellet, Wedel Jarlsberg Land, Svalbard. CONTENTS: Introduction 5 Map data and explanatory remarks 6 Sources, compilation and accuracy of the geological base map 7 Explanation of map elements 7 Stratigraphy 7 Structure 8 Outline of the Tertiary fold-and-thrust belt of Spitsbergen 10 Tectonic setting 10 Dimensions and directions 11 Structural subdivision and characteristics 13 Interior part of foldbelt 13 Western Basement High 15 Forlandsundet Graben 16 Central Tertiary Basin 16 Billefjorden Fault Zone 17 Lomfjorden Fault Zone 17 Structural descriptions (including explanation of cross sections) 17 Sørkapp-Hornsund area 17 Interior Wedel Jarlsberg Land/Torell Land - Bellsund 19 Western and Central Nordenskiold Land 21 Oscar li Land 22 Brøggerhalvøya 24 Billefjorden - Eastern Nordenskiold Land 24 Agardhbukta - Negribreen 25 Bibliography 29 Maps and map descriptions 29 Proceedings of symposia etc. -
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. -
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. -
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. -
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 . -
Van Mijenfjorden -Van Keulenfjorden Area New Investigations and Status of Knowledge
RAPPORTSERIE 121 NORSK POLARINSTITUTT Christian Lydersen, Bjørn A. Krafft, Magnus Andersen and Kit M. Kovacs Marine mammals in the Bellsund - Van Mijenfjorden -Van Keulenfjorden area New investigations and status of knowledge 1 RAPPORTSERIE NR. 121, NOVEMBER 2002, NORSK POLARINSTITUTT, POLARMILJØSENTERET, 9296 TROMSØ, www.npolar.no Rapportserie 121 Christian Lydersen, Bjørn A. Krafft, Magnus Andersen and Kit M. Kovacs Marine mammals in the Bellsund – Van Mijenfjorden –Van Keulenfjorden area New investigations and status of knowledge Norsk Polarinstitutt er Norges sentrale statsinstitusjon for kartlegging, miljøovervåking og forvaltningsrettet forskning i Arktis og Antarktis. Insti- tuttet er faglig og strategisk rådgiver i miljøvernsaker i disse områdene og forvaltningsmyndighet i norsk del av Antarktis. The Norwegian Polar Institute is Norway’s main institution for research, monitoring and topographic mapping in the Norwegian polar regions. The institute also advises Norwegian authorities on matters concerning polar environmental management. Norsk Polarinstitutt 2002 2 3 Adresser: Christian Lydersen Norsk Polarinstitutt N-9296 Tromsø Norsk Polarinstitutt, Polarmiljøsenteret, N-9296 Tromsø www.npolar.no Forsidefoto: Kit & Christian, Norsk Polarinstitutt and Hans Wolkers, Norsk Polarinstitutt Teknisk redaktør: Ann Kristin Balto Grafisk design: Jan Roald Design omslag: Audun Igesund Trykket: November 2002, Grafisk Nord, Finnsnes ISBN: 82-7666-193-9 ISSN: 0803-0421 2 3 Contents 1. Preface page 4 2. Map of study area page 5 3. Norwegian summary page 6 4. English summary page 7 5. Ringed seals page 8 6. Bearded seals page 16 7. Harbour seals page 19 8. Polar bears page 22 9. White whales page 25 10. Other marine mammals page 30 11. Recommendations for future investigations page 33 12. -
Svalbardstatistikk 2005 Svalbard Statistics 2005
D 330 Norges offisielle statistikk Official Statistics of Norway Svalbardstatistikk 2005 Svalbard Statistics 2005 Statistisk sentralbyrå • Statistics Norway Oslo-Kongsvinger Internasjonale oversikter Oslo Telefon / Telephone +47 21 09 00 00 Telefaks / Telefax +47 21 09 49 73 Besøksadresse / Visiting address Kongens gt. 6 Postadresse / Postal address Pb. 8131 Dep N-0033 Oslo Kongsvinger Telefon / Telephone +47 62 88 50 00 Telefaks / Telefax +47 62 88 50 30 Besøksadresse / Visiting address Otervn. 23 Postadresse / Postal address N-2225 Kongsvinger Internett / Internet http://www.ssb.no/ E-post / E-mail [email protected] © Statistisk sentralbyrå, august 2005 © Statistics Norway, August 2005 Ved bruk av materiale fra denne publikasjonen, vennligst oppgi Statistisk sentralbyrå som kilde. When using material from this publication, please give Statistics Norway as your source. Standardtegn i tabeller / Symbol Explanation of Symbols Tall kan ikke forekomme / . Category not applicable Oppgave mangler / . Data not available ISBN 82-537- 6809-5 Trykt versjon / Printed version Oppgave mangler foreløpig / . ISBN 82-537- 6810-9 Elektronisk versjon / Electronic version Data not yet available Tall kan ikke offentliggjøres / Not for publication : Omslagsdesign / Null / Nil - Cover design: Enzo Finger Design Omslagsillustrasjon / Mindre enn 0,5 av den brukte enheten / 0 Less than 0.5 of unit employed Cover illustration: Siri Boquist Omslagsfoto / Mindre enn 0,05 av den brukte enheten / 0.0 Less than 0.05 of unit employed Cover photo: Torfinn Kjærnet Piktogrammer / Foreløpig tall / Provisional or preliminary figure * Pictograms: Trond Bredesen Brudd i den loddrette serien / _ Break in the homogeneity of a vertical series Trykk / Print: PDC Tangen Brudd i den vannrette serien / Break in the homogeneity of a horizontal series 2 Forord Svalbardstatistikk 2005 inneholder en sammenstilling av tilgjengelig statistikk om Svalbard som Statistisk sentralbyrå har samlet inn. -
St.Meld. Nr. 9 (1999)
St.meld. nr. 9 (1999) Svalbard Tilråding fra Justis- og politidepartementet av 29. oktober 1999, godkjent i statsråd samme dag. Forklaring på forkortinger LL Longyearbyen lokalstyre SND Statens nærings- og distriktsutviklingsfond SNU Svalbard Næringsutvikling AS SSD Svalbard Samfunnsdrift AS SSS Svalbard ServiceSenter AS Store Norske Store Norske Spitsbergen Kulkompani AS St.meld. nr. 39 Stortingsmelding nr. 39 (1974–75) Vedrørende Sval- bard St.meld. nr. 40 Stortingsmelding nr. 40 (1985–86) Svalbard St.meld. nr. 50 Stortingsmelding nr. 50 (1990–91) Næringstiltak for Svalbard St.meld. nr. 42 Stortingsmelding nr. 42 (1992–93) Norsk polarfors- kning St.meld. nr. 22 Stortingsmelding nr. 22 (1994–95) Om miljøvern på Svalbard UNIS Universitetsstudiene på Svalbard Kapittel 1 St.meld. nr. 9 3 Svalbard 1 Bakgrunn Ved behandlingen av St.meld. nr. 22 (1994–95) Miljøvern på Svalbard ba Stor- tinget regjeringen om å foreta en helhetlig vurdering av svalbardsamfunnet der miljø, kulldrift og annen næringsvirksomhet, utenrikspolitiske og andre relevante forhold ble sett i sammenheng. I tillegg ble regjeringen i Dokument nr. 8:85 (1994–1995) bedt om å legge opp til en styringsmodell for Longyear- byen som gir befolkningen muligheter til demokratisk innflytelse i lokalsam- funnet i den helhetlige gjennomgangen av svalbardsamfunnet Stortinget har bedt om. I forbindelse med utarbeidelsen av stortingsmeldingen om Svalbard har det vært nedsatt en interdepartemental styringsgruppe bestående av repre- sentanter fra Finansdepartementet, Justisdepartementet, Kirke, utdannings- og forskningsdepartementet, Kommunal- og regionaldepartementet, Miljø- verndepartementet, Nærings- og handelsdepartementet og Utenriksdeparte- mentet. Som ledd i arbeidet med meldingen har det også vært nedsatt to arbeids- grupper, som har utredet spørsmålet om lokaldemokrati nærmere. -
Review Article: Permafrost Trapped Natural Gas in Svalbard, Norway
https://doi.org/10.5194/tc-2021-226 Preprint. Discussion started: 9 August 2021 c Author(s) 2021. CC BY 4.0 License. 1 Review Article: Permafrost Trapped Natural Gas in 2 Svalbard, Norway 3 Authors: Thomas Birchall*1, 2, Malte Jochmann1, 3, Peter Betlem1, 2, Kim Senger1, Andrew 4 Hodson1, Snorre Olaussen1 5 1Department of Arctic Geology, The University Centre in Svalbard, P.O. Box 156, N-9171 Longyearbyen, 6 Svalbard, Norway 7 2Department of Geosciences, University of Oslo, P.O. Box 1047, Blindern, 0316 Oslo, Norway 8 3Store Norske Spitsbergen Kulkompani AS, Vei 610 2, 9170 Longyearbyen, Svalbard. Norway 9 *Correspondence to: Thomas Birchall ([email protected]) 10 11 Abstract. Permafrost has become an increasingly important subject in the High Arctic archipelago of Svalbard. 12 However, whilst the uppermost permafrost intervals have been well studied, the processes at its base and the 13 impacts of the underlying geology have been largely overlooked. More than a century of coal, hydrocarbon and 14 scientific drilling through the permafrost interval shows that accumulations of natural gas trapped at the base 15 permafrost is common. They exist throughout Svalbard in several stratigraphic intervals and show both 16 thermogenic and biogenic origins. These accumulations combined with the relatively young permafrost age 17 indicate gas migration, driven by isostatic rebound, is presently ongoing throughout Svalbard. The accumulation 18 sizes are uncertain, but one case demonstrably produced several million cubic metres of gas over eight years. Gas 19 encountered in two boreholes on the island of Hopen appears to be situated in the gas hydrate stability zone and 20 thusly extremely voluminous.