DOCSLIB.ORG

Unis|Course Catalogue

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

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. The REQUIREMENTS | within the field of biology Biology, Arctic Geology, Arctic Geophysics and Arctic Tech- Master- or PhD level international setting and the small and intimate campus, nology. at a Norwegian institution of higher education, a Scandinavian makes UNIS a unique destination that provides students Department of Arctic Geophysics: institution of higher education or a NOKUT (The Norwegian hands-on experience in Arctic studies. The student evalu- 90 ECTS within the field of mathematics, physics or geo- UNIS’ geographical position provides unique advantages, Agency for Quality Assurance in Education) approved inter- ations show that students rate their UNIS experience as physics enabling students and faculty to use the High Arctic nature national institution of higher education. awesome. as laboratory, arena for observations and data collection. Department of Arctic Geology: Most courses include fieldwork and/or excursions. Applicants must also fulfill discipline/academic require- 60 ECTS within general natural science, of which 30 ECTS SCIENTIFIC STAFF ments and, where applicable, any additional course require- within the field of geology/geosciences HisTORY UNIS’ staff consist currently of about 20 professors and ments set by UNIS. associate professors, 23 adjunct professors and over UNIS was established in 1993 to provide university level Department of Arctic Technology: 140 guest lecturers who specialize in Arctic issues. UNIS Note on safety: UNIS has strict safety guidelines that must education in the Arctic, to carry out high quality research, 60 ECTS within the field of mathematics, physics, mechanics researchers collaborate with Norwegian and foreign be followed when students and staff are in the field. The and to contribute to the development of Svalbard as an or chemistry research institutions and are involved in a large number safety aspects of the fieldwork will be part of the admission international research platform. UNIS is a share-holding of joint research projects. As a result, there are excellent evaluation process. company, owned by the Norwegian Ministry of Education MASTER AND PHD LEVEL opportunities for UNIS students to get involved in a wide and Research. (300- AND 800-LEVEL COURSES) range of exciting research projects. BACHELOR LEVEL (200 LEVEL COURSES) The applicant must be enrolled in a relevant Master or PhD UNIS offers a quality based educational system recognized program at his/her home institution. by the Norwegian authorities. EDUCATION STRATEGY FUll tiME seMester stUDY (30 ECTS). • UNIS offers cutting edge research- and field based The applicant must be enrolled in a Bachelor program at his/ Note: You might also find relevant courses in other UNIS In 2011 UNIS signed a formal agreement with all the Norwegian education in Arctic science and provides students her home institution. departments than your program department. universities to further strengthen cooperation and to ensure state of the art research infrastructure. that UNIS courses complement the education provided by • UNIS offers an international educational setting UNIS arranges some interdisciplinary courses each term at the Norwegian mainland universities. DOinG PARTS OF A MASTER/PHD AT UNIS: that motivates excellence in academic achievements. Bachelor level. See the course table for more information. • UNIS shall be an active partner in the international A student who has been accepted as a Master or PhD networks of Arctic universities, promoting student ex- student at his/her home educational institution may carry change programs. out parts of his/her Master or PhD at UNIS. This requires a separate application and an academic contact person at UNIS. Guidelines are found at www.unis.no/studies under “Admission”. 6 UNIS | ARCTIC SIENCE FOR GLOBAL CHALLENGES 7 Longyearbyen is on top of literally on top of the world! the world HOW TO | Photo: Eva Therese Jenssen APPLY | 1 Register your preliminary application online at: AppLICATION DEADLinES www.unis.no. Autumn semester: April 15 Spring semester: October 15 2 An application form will then be sent to your registered e-mail. Note: Some Master/PhD courses may have extended deadlines. Complete your application by returning the applica- 3 tion form and required documentation to UNIS. ThE ADmissiON PROCEDURE 4 You have to attach official credentials when submit- UNIS will notify all applicants about the status of their ting the application form. Application forms that application (“accepted”, “on waiting list” or “declined”) do not contain the required documentation will not about 5-7 weeks after the application deadline. be considered in the admission process. Note: Students on waiting lists should be prepared to Only certified copies of original transcripts and accept an admission offer on short notice. 5 diplomas are accepted. Official translation to Norwegian or English is required. ACADEMIC MATTERS | ACADEMIC CALENDAR International students will be matriculated at the Univer- Autumn semester 2012: July – December sity of Tromsø if no other arrangements have been made. Spring semester 2013: January – June The registration process will take place after you have ar- rived at UNIS. CREDITS AND GRADES DEADLinE FOR SEMESTER REGisTRATION UNIS uses the European Credit Transfer System, ECTS for credits. One semester of full-time study is 30 ECTS and one Autumn semester: September 1 year is 60 ECTS. UNIS follows the ECTS standard grading Spring semester: February 1 system, with a descending scale from A (top mark) to E for pass and F for fail. Semester registration requires payment of the semester fee within the registration deadline. Currently the semester In order to pass a course at UNIS the student must pass all fee is NOK 420 (ca. 55 Euro). Students who fail to register assessments that are part of the course. within the deadline will not be registered for the exams. Mandatory assignments: Please note that most courses TRAnsCRIPTS AND CERTIFICATES include mandatory activities (fieldwork, lab work, etc.), that UNIS does not issue official grade transcripts as UNIS is a must be completed and approved in order for a student to university centre and not accredited to provide academic take the final exam. See course descriptions for details. degrees. A transcript can be issued upon request by the Norwegian university in which the student is registered at. REGisTRATION AND MATRICULATION aRCTIC Dette er en bildetekst som Students admitted to UNIS, who are enrolled at other Nor- TECHNOLOGY skal følge overskriften. Her UNIS COURSES AS PART OF YOUR skriver du en bildetekst. wegian universities, will remain registered at these univer- uniVERSITY EDUCATION STUDENTS... | Photo by: Ola Normann sities. These students must pay the semester fee and reg- We recommend all our students to get their UNIS courses ister for exams at their home university. This procedure can approved by their home institution in advance. be done from UNIS. 8 UNIS | ARCTIC SCIENCE FOR GLOBAL CHALLENGES 9 practical UNIS is located in the the Svalbard Svalbard Science Centre. Science Centre information | | Photo: Nils Petter Dale ACADEMIC EXPEnsES ACCOmmODATION There is no tuition fee, but currently a semester fee of NOK The student housing facilities in Longyearbyen is owned 420 (ca. 55 Euro). If you are on an overnight scientific cruise, and administered by the Student Welfare Organization in fieldwork or excursion you will have to pay a fee of NOK 200 Tromsø (SiTø). The student housing is located in Nybyen, per day for food. about 3 km from the UNIS campus. Please note that there is no public transportation system in Longyearbyen. FinANCinG
Recommended publications
  • Handbok07.Pdf

    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? ....
  • Climate in Svalbard 2100

    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.
  • Checklist of Lichenicolous Fungi and Lichenicolous Lichens of Svalbard, Including New Species, New Records and Revisions

    Checklist of Lichenicolous Fungi and Lichenicolous Lichens of Svalbard, Including New Species, New Records and Revisions

    Herzogia 26 (2), 2013: 323 –359 323 Checklist of lichenicolous fungi and lichenicolous lichens of Svalbard, including new species, new records and revisions Mikhail P. Zhurbenko* & Wolfgang von Brackel Abstract: Zhurbenko, M. P. & Brackel, W. v. 2013. Checklist of lichenicolous fungi and lichenicolous lichens of Svalbard, including new species, new records and revisions. – Herzogia 26: 323 –359. Hainesia bryonorae Zhurb. (on Bryonora castanea), Lichenochora caloplacae Zhurb. (on Caloplaca species), Sphaerellothecium epilecanora Zhurb. (on Lecanora epibryon), and Trimmatostroma cetrariae Brackel (on Cetraria is- landica) are described as new to science. Forty four species of lichenicolous fungi (Arthonia apotheciorum, A. aspicili- ae, A. epiphyscia, A. molendoi, A. pannariae, A. peltigerina, Cercidospora ochrolechiae, C. trypetheliza, C. verrucosar- ia, Dacampia engeliana, Dactylospora aeruginosa, D. frigida, Endococcus fusiger, E. sendtneri, Epibryon conductrix, Epilichen glauconigellus, Lichenochora coppinsii, L. weillii, Lichenopeltella peltigericola, L. santessonii, Lichenostigma chlaroterae, L. maureri, Llimoniella vinosa, Merismatium decolorans, M. heterophractum, Muellerella atricola, M. erratica, Pronectria erythrinella, Protothelenella croceae, Skyttella mulleri, Sphaerellothecium parmeliae, Sphaeropezia santessonii, S. thamnoliae, Stigmidium cladoniicola, S. collematis, S. frigidum, S. leucophlebiae, S. mycobilimbiae, S. pseudopeltideae, Taeniolella pertusariicola, Tremella cetrariicola, Xenonectriella lutescens, X. ornamentata,
  • P-092 Cornice Dynamics Above Nybyen in Svalbards High Arctic

    P-092 Cornice Dynamics Above Nybyen in Svalbards High Arctic

    2010 International Snow Science Workshop P-092 Cornice dynamics above Nybyen in Svalbards high arctic landscape Stephan C. Vogel1 Markus Eckerstorfer1 Hanne Christiansen1, 2 1. Arctic Geology Department, University Centre in Svalbard, Longyearbyen, Norway; 2. Department of Geosciences, University of Oslo, Oslo, Norway The development of cornices, their cracking and consequent failures largely controlled by meteorology along the Gruvefjellet plateau ridge was investigated in the two consecutive snow seasons of 2009 and 2010. These natural processes endanger life and infrastructure in Longyearbyen, Svalbard’s main settlement in the High Arctic. Two automatic time lapse cameras provided up to 6 daily pictures of the entire Gruvefjellet slope from the valley bottom and monitored the cornice development and tension cracking from the ridgeline. Further- more stakes on the plateau were used to record snow depth distribution and cornice growth. 45 field trips up the plateau were carried out to study the processes and to manually measure cornice crack opening rates. Meteorological data were recorded by an automatic weather station situated on the Gruvefjellet plateau source area. Both snow seasons indicated that cornices were built up by a low number of distinct storm events and that cornice scouring due to high wind speeds is rather limited. In 2009 the first cornice cracks were observed in mid April, while in 2010, probably due to persistent warm weather in combination with large amounts of rain, cornice cracks were already developing at the end of January. Cornice crack measurements showed a linear de- velopment, indicating the major influence of gravity. 177 cornice failures have been recorded, whereof 11 were “D3-R3” and “D3-R4” avalanches which nearly reached housing infrastructure.
  • The “Coolest” and Northernmost FAQ Welcome to UNIS We Hope You Will

    The “Coolest” and Northernmost FAQ Welcome to UNIS We Hope You Will

    The “coolest” and northernmost FAQ Everything you might or might not want to know about your stay at UNIS Made by the UNIS Student Council autumn 2016 Welcome to UNIS We hope you will have a great time here ͺ Before arrival Important: Remember to apply for housing, and sign your contract before arriving, ​ and check the dates. Your room will first be opened in the afternoon the day your contract starts, so if you arrive 3am you should make sure the contract starts the day before arrival. If your contract starts in the weekend your room will be opened at Friday afternoon (Samskipnaden opens your room and leaves the key inside, so you don’t need to worry about not being able to access your room) Rifles: If you want to borrow rifles (you need them when leaving town) during your ​ stay please read the rifle part http://www.unis.no/studies/student-life/new-students/ Q: What do I need to pack? http://www.unis.no/wp-content/uploads/2014/08/PACKING-LIST.pdf - When it comes to equipment and how warm clothing you need it is up to what you plan to do and how easily you freeze - You should bring or buy a pair of thin liner gloves to wear under thicker ​ ​ mittens. During field work you will find that it is very hard to write with the thick scooter mittens, and that is awfully cold to do anything bare handed in -20 degrees celsius - Liner gloves can be very nice to have during the safety course, you will do part of it outside.
  • Lichens and Vascular Plants in Duvefjorden Area on Nordaust- Landet, Svalbard

    Lichens and Vascular Plants in Duvefjorden Area on Nordaust- Landet, Svalbard

    CZECH POLAR REPORTS 9 (2): 182-199, 2019 Lichens and vascular plants in Duvefjorden area on Nordaust- landet, Svalbard Liudmila Konoreva1*, Mikhail Kozhin1,2, Sergey Chesnokov3, Soon Gyu Hong4 1Avrorin Polar-Alpine Botanical Garden-Institute of Kola Scientific Centre of RAS, 184250 Kirovsk, Murmansk Region, Russia 2Department of Geobotany, Faculty of Biology, Lomonosov Moscow State University, Leninskye Gory 1–12, GSP–1, 119234 Moscow, Russia 3Komarov Botanical Institute RAS, Professor Popov St. 2, 197376 St. Petersburg, Russia 4Division of Polar Life Sciences, Korea Polar Research Institute, 26, Songdomirae-ro, Yeonsu-gu, Incheon 21900, Republic of Korea Abstract Floristic check-lists were compiled for the first time for Duvefjorden Bay on Nordaust- landet, Svalbard, based on field work in July 2012 and on data from literature and herbaria. The check-lists include 172 species of lichens and 51 species of vascular plants. Several species rare in Svalbard and in the Arctic were discovered: Candelariella borealis was new to Svalbard. 51 lichen species were newly recorded on Nordaustlandet and 131 lichen species were observed in the Duvefjorden area for the first time. Among lichen species rare in Svalbard and in the Arctic the following can be mentioned: Caloplaca magni-filii, C. nivalis, Lecidea silacea, Phaeophyscia nigricans, Polyblastia gothica, Protothelenella sphinctrinoidella, Rinodina conradii, Stenia geophana, and Tetramelas pulverulentus. Two species of vascular plants, Saxifraga svalbardensis and S. hyperborea, were found new to the Duvefjorden area. The investigated flora is represented mostly by species widespread in Svalbard and in the Arctic. Although Duvefjorden area is situated in the northernmost part of Svalbard, its flora is characterized by relatively high diversity of vascular plants and lichens.
  • Polish Polar Research 4-16.Indd

    Polish Polar Research 4-16.Indd

    vol. 37, no. 4, pp. 493–509, 2016 doi: 10.1515/popore-2016-0026 Vegetation diversity and selected abiotic factors influencing the primary succession process on the foreland of Gåsbreen, Svalbard Paulina WIETRZYK1*, Michał WĘGRZYN1 and Maja LISOWSKA2 1 Prof. Z. Czeppe Department of Polar Research and Documentation, Institute of Botany, Jagiellonian University, Kopernika 27, 31-501 Kraków, Poland <[email protected]>, <[email protected]> 2 Centre for Polar Studies, University of Silesia, Będzińska 60, 41-200 Sosnowiec, Poland <[email protected]> * corresponding author Abstract: The rapidly changing Arctic provides excellent opportunities for investigat- ing primary succession on freshly deglaciated areas. Research on the Gåsbreen foreland (S Spitsbergen) traced the succession of particular groups of organisms and species, particularly lichens and bryophytes, and determined the effect of selected abiotic fac- tors on this succession. Fieldwork in 2008, employed a continuous linear transect of phytosociological relevés (1 m2) along the foreland. Data analysis allowed to distinguish five different succession stages and three types of colonisers. Canonical correspondence analysis and a permutation test showed that distance from the front of the glacier and fine grain material in the substrate mostly influenced the distribution and abundance of vegetation, and the steepness of the moraine hills affected the colonisation process, mainly in the older part of the marginal zone. Key words: Arctic, colonisation, glacier, lichens, bryophytes, vascular plants. Introduction Arctic regions offer perfect opportunities for studying primary succession processes on freshly deglaciated areas (Frenot et al. 1998; Jorgenson et al. 2015). Areas which are exposed from retreating glaciers are successively colonised by different groups of organisms such as cyanobacteria, lichens, bryophytes and vascular plants.
  • The Flora of Jan Mayen

    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.
  • Status of Echinococcus Multilocularis in Svalbard - Final Report to Svalbard Environmental Protection Fund NORWEGIAN VETERINARY INTSTITUTE

    Status of Echinococcus Multilocularis in Svalbard - Final Report to Svalbard Environmental Protection Fund NORWEGIAN VETERINARY INTSTITUTE

    Rapport 11- 2019 Status of Echinococcus multilocularis in Svalbard - Final Report to Svalbard Environmental protection Fund NORWEGIAN VETERINARY INTSTITUTE Status of Echinococcus multilocularis in Svalbard Preface This is the final report of the project “Status of Echinococcus multilocularis in Svalbard” 16/42. Funding for this project was allocated by the Svalbard Environmental Protection Foundation in the spring of 2016. The project was carried out by a team of researchers from the Norwegian Veterinary Institute and the Norwegian Polar Institute, who for the first time collaborated in this project. The Norwegian Veterinary Institute has contributed with expert knowledge on E. multilocularis, pathology, parasitological and molecular methods, and the Norwegian Polar Institute with specific expertise on Arctic foxes, sibling voles, E. multilocularis and environmental aspects. In addition, we have benefitted from working together with Fredrik Samuelsson, Svalbard guide with an MSc in Parasitology, whose local knowledge has greatly facilitated the sample collection. The results of our project were presented to locals at a seminar at the University Centre in Svalbard 19.11.2018. We gratefully acknowledge the Svalbard Environmental Protection Fund for supporting our project. We would also like to thank Paul Lutnæs/the Govenor of Svalbard, Rupert Krapp from the Norwegian Polar Institute and the Svalbard Vets for assisting in collecting samples for the project; Longyearbyens Hundeklubb, commercial dog sledging companies and private dog owners who kindly let us collect faecal samples from their dogs; arctic fox hunters who donated foxes for our study, and inhabitants in Longyearbyen who helped trapping sibling voles. In this project we have collaborated with Dr.
  • Fossil Hunt with Green Dog

    Fossil Hunt with Green Dog

    FOSSIL HUNT WITH GREEN DOG At the top of the Longyear Valley there are two SVERDRUPBYEN glaciers, the Lars and Longyear Glaciers. The To the west of Nybyen, just on the other side of Longyear Glacier has, over thousands of years, the river, is a place called Sverdrupbyen, named eroded the bedrock and moved rocks and gravel after Einar Sverdrup (1895 - 1942), the managing into a large moraine. It is in these types of rocks director of the mining company Store Norske we can find 40 - 60 million year old fossils of Spitsbergen Kulkompani. He was the leader of ancient flora and fauna. Operation Fritham in World War II, but died in the course of that operation, which attempted to SAFETY secure Svalbard for the Allies. Most buildings in Please do not walk too far away from your armed Sverdrupbyen, including those of Mine 1B, were guide, in case a polar bear shows up. When destroyed in a fire rehearsal in the 1980s before using a rock hammer, be careful to protect your they became protected under the cultural eyes from stone ragments. heritage preservation law. MINING All together, 9 mines in and around ON THE WAY TO Longyearbyen have been active. Today, the only THE FOSSIL LOCATION, active mine in the local area is Gruve 7. Store YOU WILL PASS Norskes main activity is at the mine in Svea. AND SEE GRUVE 1A, AMERIKANERGRUVA • The first mine in Longyearbyen. The Arctic NYBYEN Coal Company (ACC), led by the American Nybyen is a small settlement located on the John Munroe Longyear, established southern outskirts of Longyearbyen.
  • Walking Around Longyearbyen Updatedaug2014

    Walking Around Longyearbyen Updatedaug2014

    CHEESEMANS’ ECOLOGY SAFARIS 20800 Kittridge Road Saratoga, CA 95070-6322 USA (800)527-5330 (408)741-5330 [email protected] cheesemans.com Walking around Longyearbyen Updated August 2014 Longyearbyen, a Norwegian mining settlement, is the administrative center of Svalbard, and has an airport open throughout the year. The settlement of Longyearbyen is small (about 1 x 2 miles or 1.6 x 3.3 km), so we can reach anywhere on foot. There are bicycles for rent at Nybyen (Guesthouse 102), if you so desire. There is more than enough to do in and around town to fill a day. Please do not stray from the roads around town (the surrounding hills); Polar Bears can be found in the area! Aerial view from airplane on approach Map of Longyearbyen 1. Radisson Blue Polar Hotel 2. Sentrum (Center) • Shopping at Svalbardbutikken • Lompen senteret with many shops 3. Haugen (Spitsbergen Hotel) 4. Mine 2b 5. Nybyen (Guesthouse 102) 6. Sverdrupbyen (Huset, theater) 7. Svalbard Museum 8. Wharf, airport, Mine 3 Page 1 of 2 1. Radisson Blu Polar Hotel – The Radisson opened as a hotel on March 4, 1995 after hosting sponsors of the American winter Olympic national team in 1994. The hotel contains a restaurant, pub, conference room, and library. 2a. Svalbardbutikken – A supermarket and department store rolled into one. It stocks a variety of articles including groceries, clothing, shoes, electrical appliances, cosmetics, jewelry, gifts, souvenirs, wines and spirits. Svalbard is a duty and tax-free region, so alcohol can be purchased at low prices. In such a remote outpost of civilization, you may be surprised to find the most modern of computer games and DVDs here.
  • Svalbard's Risk of Russian Annexation

    Svalbard's Risk of Russian Annexation

    The Coldest War: Svalbard's Risk of Russian Annexation The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Vlasman, Savannah. 2019. The Coldest War: Svalbard's Risk of Russian Annexation. Master's thesis, Harvard Extension School. Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:42004069 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA The Coldest War: Svalbard’s Risk of Russian Annexation Savannah Vlasman A Thesis In the Field of International Relations for the Degree of Master of Liberal Arts in Extension Studies Harvard University 2018 Savannah Vlasman Copyright 2018 Abstract Svalbard is a remote Norwegian archipelago in the Arctic Ocean, home to the northernmost permanent human settlement. This paper investigates Russia’s imperialistic interest in Svalbard and examines the likelihood of Russia annexing Svalbard in the near future. The examination reveals Svalbard is particularly vulnerable at present due to melting sea ice, rising oil prices, and escalating tension between Russia and the West. Through analyzing the past and present of Svalbard, Russia’s interests in the territory, and the details of the Svalbard Treaty, it became evident that a Russian annexation is plausible if not probable. An assessment of Russia’s actions in annexing Crimea, as well as their legal justifications, reveals that these same arguments could be used in annexing Svalbard.