Norway's Arctic Policy Creating Value, Managing Resources, Confronting Climate Change and Fostering Knowledge
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The Nickel Mineralizationof the Rana Mafic Intrusion, Nordland, Norway
• THE NICKEL MINERALIZATIONOF THE RANA MAFIC INTRUSION, NORDLAND, NORWAY. Rognvald Boyd and Carl 0. Mathiesen Norges geologiskeundersøkelse,Postboks 3006, 7001 Trondheim, Norway. NORGES GEOLOGISKE UNDERSØKELSE ABSTRACT The Råna synorogenicCaledonide intrusion in north Norway contains pentlandite+pyrrhotite+chalcopyrite+pyritedisseminationsgrading up tO 0.8% sulfide nickel in peridotite in the northwesternpart of the body. Peridotite and pyroxenite occur as bands and lenses within a peripheral zone mainly of norite, around a core mainly of quartz-norite.Crystal settling appears to have been an important process at Råna but over much of the intrusion primary structureshave been severely disturbed by the later Caledonian fold phases which also involved local overthrusting: these movements resulted in iniolding and thrustingof units of semipel- itic and calesilicate gneiss and black schist into the intrusion.The body has the form of an inverted, possibly truncated cone with its axiS plunging northwestwardsat a moderate angle. The peridotites show no obvioUs systematicvariation of sulfide or silicate mineralogy across strike. Locally, ass&iated with certain deformation zones, disseminationpasses into ma3sive mobilized sulfide ti with up to 5% nickel. The proximity of sulfide-bearingblack schists to mineralized rocks, the occurrence of graphite djsseminated in peridotite and other factors, suggest assimilationof sulfur from the Country rocks. Sulfur isotope studies do not, however, offer confirmationof the hypo- thesis that an external source ot sulfur nas had more than very local significanceat Råna. 1 NORGES GEOLOGISKE UNDERSØKELSE • INTRODUCTION The Råna mafic intrusion lies at approximately68°30'N, in steep mountainous terrain 20 km soutnwest of the iron-ore port of Narvik in north Norway (Fig.1).The present paper will give a brief description of the general geology of the complex, with a more detailed consider- ation of the sulfide-bearingareas - especially the main one at Bruvann (Fig.2) - and of the cenetic implicationsinvolved. -
NGU Rapport 2009.076 Kvernsteinsbrudd Og Kornkverner I Ofoten Og Sør-Troms
NGU Rapport 2009.076 Kvernsteinsbrudd og kornkverner i Ofoten og Sør-Troms 27 175,- INNHOLD: FORORD INNLEDNING KVERNER I OFOTEN OG SØR-TROMS RÅSTOFF FOR KVERNSTEIN SOMMERVIKA I EVENES KOMMUNE SVELLSHAMNA I SKÅNLAND KOMMUNE FRAMKOMMET INFORMASJON OM ANDRE UTTAKSSTEDER Sørreisa Nordreisa Karlsøy Målselv Harstad Seljeli i Vefsn INFO OM KORNMØLLER I FORBINDELSE MED UNDERSØKELSEN KONKLUSJON LITTERATUR FIGURER 1. Lokalisering av brudd i Sommervika 2. Oversiktbilde over bruddet i Sommervika 3. Sporene etter uttak i Sommervika, a - e 4. Lokalisering av brudd i Svellshamna 5. Oversiktsbilde over bruddet i Svellshamna 6. Sporene etter uttak i Svellshamna, a - e FORORD Nordland var for noen få år siden det fylket som hadde flest ansatte innenfor mineralindustri. Det har vært drevet uttak av bygningstein, mineraler og metaller som er brukt lokalt eller sendt ut av fylket. Selv om dette ikke er tilfelle i dag er mineralindustrien fremdeles viktig for fylket. Nordland har en variert geologi med mange typer bergarter og vil også i framtida kunne bli et viktig fylke for bygningstein. Fylkeskommunen har gjort en stor innsats, kanskje den største av alle landets fylker, på å øke den geologiske informasjonen for Nordland gjennom et geologisk fylkesprogram fra 1992-1999. NGU har gjort en stor egeninnsats men også trukket inn finansiering fra prosjekter som Nordland Mineral (NM) samt EU-prosjektene PNASTINA (Promotion of NAtural Stone deposits In the Northern Areas) og i dag NIBA (Natural stone deposits In Botnia Atlantica). Det er fremdeles kompetanse i fylket på drift av bygningstein selv om denne også er i ferd med å utarmes. Denne korte statusrapporten tar for seg kvernsteinuttakene i Ofoten og Sør-Troms som er dukket opp i forbindelse med arbeider i regi av NGU, NM og NIBA uten at det verken er gjort grundige litteraturstudier eller arbeider for å få en total oversikt. -
The Centrality of Small Islands in Arctic Norway from the Viking Age to Recent Historic Period
The Journal of Island and Coastal Archaeology ISSN: 1556-4894 (Print) 1556-1828 (Online) Journal homepage: http://www.tandfonline.com/loi/uica20 The Centrality of Small Islands in Arctic Norway From the Viking Age to Recent Historic Period Stephen Wickler To cite this article: Stephen Wickler (2016) The Centrality of Small Islands in Arctic Norway From the Viking Age to Recent Historic Period, The Journal of Island and Coastal Archaeology, 11:2, 171-194, DOI: 10.1080/15564894.2015.1134728 To link to this article: http://dx.doi.org/10.1080/15564894.2015.1134728 Published online: 26 Jan 2016. Submit your article to this journal Article views: 99 View related articles View Crossmark data Citing articles: 1 View citing articles Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=uica20 Download by: [UiT Norges arktiske universitet] Date: 04 November 2016, At: 07:25 The Journal of Island and Coastal Archaeology, 11:171–194, 2016 Copyright © 2016 Taylor & Francis Group, LLC ISSN: 1556-4894 print / 1556-1828 online DOI: 10.1080/15564894.2015.1134728 The Centrality of Small Islands in Arctic Norway From the Viking Age to Recent Historic Period Stephen Wickler Department of Cultural Sciences, Tromsø University Museum, University of Tromsø, Tromsø, Norway ABSTRACT The definition of island marginality in northern Norway was radically altered by the advent of motorized fishing vessels in the early twenti- eth century. Prior to this development, small offshore islands were of central importance for marine related activity due to their proximity to fishing grounds. This article presents four settlements on small and “marginal” islands in Arctic Norway from 68◦19’ to 71◦05’Nlatitude as cases that illustrate the centrality of such locations in a maritime context since the Viking Age (AD 800–1050). -
Illustration De L'effet Frontière
Kirkenes, bout du monde norvégien ou place commerciale transfrontalière ? Illustration de l’effet frontière 1 Frédéric Lasserre 1 Professeur au département de géographie de l’Université Laval, et directeur du Conseil québécois d’Études géopolitiques. [email protected] ARTICLE Résumé : La frontière terrestre entre Russie Introduction Une commune minière, et Norvège, longtemps très patrouillée et terminus du territoire La petite bourgade de Kirkenes, dans contrôlée lors de la Guerre froide, est norvégien aujourd’hui beaucoup plus ouverte. Le l’Arctique norvégien, compte environ nombre de passages annuels a connu une 3 500 habitants et fait partie de la Fondée en 1906 à partir d’un mo- nette augmentation au cours de la dernière municipalité de Sør-Varanger (Fig. 1). deste hameau de pêcheurs (Viken et décennie, les résidents des zones frontalières Elle se situe à 7 km de la frontière al 2008), la petite ville de Kirkenes a alimentant une activité de tourisme com- russe, sur le segment de 195,7 km de comme vocation économique son mercial bénéfique pour la communauté. frontière terrestre entre Russie et port qui dessert la mine de fer de Cette activité économique prend une Sydvaranger située à 8,5 km à importance croissante dans l’économie Norvège depuis que l’URSS a annexé locale alors même que l’activité minière le corridor de Petsamo aux dépens de l’intérieur des terres, et que relie une périclite. Kirkenes constitue un bon exemple la Finlande en 1944. voie ferrée construite pour l’occa- de l’effet frontière, dans lequel la frontière sion. La mine, l’usine de première ne constitue pas un frein, mais une interface Frontière terrestre longtemps très transformation et le port desservant moteur d’une activité économique. -
Felles Plattform for Fusjon
Felles plattform for fusjon (Grunnlagsdokument for sammenslåing) En fusjon mellom Universitetet i Nordland og Høgskolen i Nesna skal skape en sterk nasjonal aktør innenfor høyere utdanning og forskning som er godt egnet til å løse samfunnsoppdraget i hele Nordland. Det fusjonerte universitetet skal sikre bærekraft i et fremtidsperspektiv både for virksomheten på Helgeland og for universitetet som helhet. Versjon 2 Fra styringsgruppen for fusjon 1 Innledning Dette dokumentet presenterer en strategi for utvikling av et fusjonert universitet. Dokumentet er et omforent grunnlag for en fusjon mellom Universitetet i Nordland (UiN) og Høgskolen i Nesna (HiNe). Fusjonen vil være en omfattende prosess som vil berøre begge institusjoner i stor grad. Dette dokumentet har særlig fokus på organisering av aktivitetene på Helgeland. Dokumentet er ment å fungere som beslutningsgrunnlag for institusjonenes styrebehandling og beslutning vedrørende fusjon i institusjonenes styremøter i Juni 2015. Dette innebærer både standpunkt til fusjon, ny organisasjon, og hvordan en eventuell fusjon skal skje. Dokumentet skal gi retning for videre arbeid for implementering av fusjonen. Det legges til grunn at fusjonen skal være operativ fra 1.1.16, og det er i dokumentet fokusert på de avklaringene som må være på plass for at styrene skal kunne fatte sine vedtak, og for å få en styringsdyktig institusjon fra og med denne dato. Dokumentet er inndelt i to hoveddeler. Del 1 presenterer premissene for fusjon mellom Universitetet i Nordland og Høgskolen i Nesna. I denne delen er det derfor fokusert på å bringe klarhet i følgende: - Overordnede målsettinger/visjon for det fusjonerte universitetets virksomhet på Helgeland. - Fullmakter som skal ligge på Helgeland - Styringsstruktur for virksomheten på Helgeland Del 2 sier noe om bakgrunnen for fusjonsprosessen og hvilke politiske- og regionale hensyn og forutsetninger den endelige løsningen må ta hensyn til. -
Alpen Skal Erstatte Arhol
10 Saltenposten Lørdag 19. juli 2008 Alpen skal erstatte Arhol Stormen Narve sørget i januar 2006 for at kutteren «Arholmen» tilhørende Salten Veteranbåtlag falt ned av slippvogna på Rognan og totalhavarerte. Nå er tiden kommet for utskifting. KNUT F. O LSEN 97 17 89 71 SALTDAL:«Arholmen» på 43 fot var stasjonert i Saltdal, tjente Veteran- båtlaget i cirka 10 år og var på mange lofotturer. Båten ble bygd på Rognan og endte dermed et langt og strabasiøst liv der,og ring- en var sluttet. Men nå har Veteranbåtlaget fått en henvendelse og sjanse til å er- statte tapet av «Arholmen» som de ikke vil la gå fra seg. Sjelden motorskøyte – Det er nåværende eier, pensjo- nert skipstømmermann og båtbyg- ger Arne Pedersen (85) fra Forra i Ofoten som har tatt kontakt med oss, fordi han vil at hans sjeldne motorskøyte M/S «Alpen» (37 fot) som er bygd i Saltdal i 1914 skal komme tilbake til utgangspunktet. Båten er en videreføring av lister- båt, som er båter som først ble bygd på Lista i Vest-Agder. «Alpen» ble bygd på Brenne av far til Harald Pedersen som igjen starta båtbyggerlinja på Røkland. Mangler 50.000 Arne makter ikke med båten leng- re. Han har brukt seks år og 6.000 arbeidstimer på å restaurere, for- SJELDEN MOTORSKØYTE.Andreas Hals fra Veteranbåtlaget viser bilder av M/S «Alpen» og eier Arne Pedersen (85) fra Forra i Ofoten som vil at båten som er bygd i teller Andreas Hals i Veteranbåtla- Saltdal skal tilbake dit. FOTO:KNUT F. O LSEN get i Saltdal og føyer til at Arne Pe- – Vi er opptatt av at ei Saltdals- handa er 100.000 kroner. -
The Lillevik Dyke Complex, Narvik: Geochemistry and Tectonic Implications of a Probable Ophiolite Fragment in the Caledonides of the Ofoten Region, North Norway
The Lillevik dyke complex, Narvik: geochemistry and tectonic implications of a probable ophiolite fragment in the Caledonides of the Ofoten region, North Norway ROGNVALD BOYD Boyd, R.: The Lillevik dyke complex, Narvik: geochemistry and tectonic implications of a probable ophiolite fragment in the Caledonides of the Ofoten region, North Norway. Norsk Geologisk Tidsskrift, Vol. 63, pp. 39-54. Oslo 1983, ISSN 0029-196X. The Lillevik dyke complex occurs in an allochthonous unit and shows field relationships indicative of a transition from the mafic cumulate to the sheeted dyke zone in a segment of an ophiolite. Major and trace element chemistry confirm the MORB character of most of the diabases. Certain diabase, gabbro and trondhjemite dykes have REE patterns suggesting a later stage of ocean-island volcanism. The Lillevik complex and equivalent bodies along strike on the eastern limb of the Ofoten synform are a probable source for the mafic facies of the overlying Elvenes Conglomerate. Analogies with other areas suggest that the Lillevik complex was obducted during the Finnmarkian orogeny. R. Boyd, Norges geologiske undersøkelse, Postboks 3006, N-7001 Trondheim, Norway. The topic of this paper is a tectonically bounded gen Groups is marked by a conglomerate hori lens, consisting of gabbro cut by diabase and zon, the Elvenes Conglomerate, which consists gabbroic dykes and by leucocratic veins, which is mainly of matrix-supported cobbles of meta exposed on a shore section within the town of trondhjemite, quartzite and dolomitic marble in Narvik in North Norway. The section Iies in the a matrix of calcareous mica schist (Foslie 1941, upperrnost part of the Narvik Group of Gustav Gustavson 1966); this unit is currently being son (1966, 1972) (Fig. -
K Yanite-Grade Metamorphism in the Evenes and Bogen Groups, Ofoten
Kyanite-grade metamorphism in the Evenes and Bogen Groups, Ofoten, North Norway MARK G. STELTENPOHL & JOHN M. BARTLEY Steltenpohl, M. G. & Bartley, J. M. : Kyanite-grade metamorphism in the Evenes and Bogen Groups, Ofoten, North Norway. Norsk Geologisk Tidsskrift, Vol. 64, pp. 21-26. Oslo 1984. ISSN 0029-196X. Directly north of Ofotfjorden in northern Norway, pelitic schists within the Evenes and Bogen Groups contain the mineral assemblage garnet + biotite ± kyanite ± staurolite + white mica + quartz ± plagio clase. This assemblage implies metamorphic P-T minima of- 540"C and - 4. 8 kb. The rocks are thus at a higher grade than suggested by previous reports, which placed them in the greenschist facies. This indicates that several metamorphic allochthons in Ofoten, including rocks of the Narvik, Evenes, Bogen, and Niingen Groups, are all at kyanite grade, supporting recent interpretations which on structural grounds concluded that the metamorphic peak outlasted stacking of these allochthons. A proposed correlation of the Evenes Group with the Middle Ordovician-Lower Silurian Balsfjord Supergroup implies that this stacking and associated kyanite-grade metamorphism are post-early Silurian and are related to the Scandian phase of the Caledonian orogeny. M. G. Steltenpohl & J. M. Bartley, Department of Geology, University of North Carolina, Chapel Hill, North Carolina 27514, USA. Our mapping, structural analysis, and petro ultramafic rocks of the Narvik Group, which are graphic studies in Ofoten have concentrated on presently at kyanite grade (Foslie 1941, 1949, the structural and metamorphic development of Gustavson 1966, 1972, Hodges 1982a, Tull et al. the Caledonian nappe stack. Figure l shows a in press). -
Joint Barents Transport Plan Proposals for Development of Transport Corridors for Further Studies
Joint Barents Transport Plan Proposals for development of transport corridors for further studies September 2013 Front page photos: Kjetil Iversen, Rune N. Larsen and Sindre Skrede/NRK Table of Contents Table Summary 7 1 Introduction 12 1.1 Background 12 1.2 Objectives and members of the Expert Group 13 1.3 Mandate and tasks 14 1.4 Scope 14 1.5 Methodology 2 Transport objectives 15 2.1 National objectives 15 2.2 Expert Group’s objective 16 3 Key studies, work and projects of strategic importance 17 3.1 Multilateral agreements and forums for cooperation 17 3.2 Multilateral projects 18 3.4 National plans and studies 21 4 Barents Region – demography, climate and main industries 23 4.1 Area and population 23 4.2 Climate and environment 24 4.3 Overview of resources and key industries 25 4.4 Ores and minerals 25 4.5 Metal industry 27 4.6 Seafood industry 28 4.7 Forest industry 30 4.8 Petroleum industry 32 4.9 Tourism industry 35 4.10 Overall transport flows 37 4.11 Transport hubs 38 5 Main border-crossing corridors in the Barents Region 40 5.1 Corridor: “The Bothnian Corridor”: Oulu – Haparanda/Tornio - Umeå 44 5.2 Corridor: Luleå – Narvik 49 5.3 Corridor: Vorkuta – Syktyvkar – Kotlas – Arkhangelsk - Vartius – Oulu 54 5.4 Corridor: “The Northern Maritime Corridor”: Arkhangelsk – Murmansk – The European Cont. 57 5.5 Corridor: “The Motorway of the Baltic Sea”: Luleå/Kemi/Oulu – The European Continent 65 5.6 Corridor: Petrozavodsk – Murmansk – Kirkenes 68 5.7 Corridor: Kemi – Salla – Kandalaksha 72 5.8 Corridor: Kemi – Rovaniemi – Kirkenes 76 -
Action Plan Pasvik-Inari Trilateral Park 2019-2028
Action plan Pasvik-Inari Trilateral Park 2019-2028 2019 Action plan Pasvik-Inari Trilateral Park 2019-2028 Date: 31.1.2019 Authors: Kalske, T., Tervo, R., Kollstrøm, R., Polikarpova, N. and Trusova, M. Cover photo: Young generation of birders and environmentalists looking into the future (Pasvik Zapovednik, О. Кrotova) The Trilateral Advisory Board: FIN Metsähallitus, Parks & Wildlife Finland Centre for Economic Development, Transport and the Environments in Lapland (Lapland ELY-centre) Inari Municipality NOR Office of the Finnmark County Governor Øvre Pasvik National Park Board Sør-Varanger Municipality RUS Pasvik Zapovednik Pechenga District Municipality Nikel Local Municipality Ministry of Natural Resource and Ecology of the Murmansk region Ministry of Economic Development of the Murmansk region, Tourism division Observers: WWF Barents Office Russia, NIBIO Svanhovd Norway Contacts: FINLAND NORWAY Metsähallitus, Parks & Wildlife Finland Troms and Finnmark County Governor Ivalo Customer Service Tel. +47 789 50 300 Tel. +358 205 64 7701 [email protected] [email protected] Northern Lapland Nature Centre Siida RUSSIA Tel. +358 205 64 7740 Pasvik State Nature Reserve [email protected] (Pasvik Zapovednik) Tel./fax: +7 815 54 5 07 00 [email protected] (Nikel) [email protected] (Rajakoski) 2 Action Plan Pasvik-Inari Trilateral Park 2019-2028 3 Preface In this 10-year Action Plan for the Pasvik-Inari Trilateral Park, we present the background of the long-lasting nature protection and management cooperation, our mutual vision and mission, as well as the concrete development ideas of the cooperation for the next decade. The plan is considered as an advisory plan focusing on common long-term guidance and cooperation. -
Green Building in the Arctic Region: State-Of-The-Art and Future Research Opportunities
sustainability Review Green Building in the Arctic Region: State-of-the-Art and Future Research Opportunities Lucrezia Ravasio *, Svein-Erik Sveen and Raymond Riise Department of Building, Energy and Material Technology, UiT—The Arctic University of Norway, 8515 Narvik, Norway; [email protected] (S.-E.S.); [email protected] (R.R.) * Correspondence: [email protected]; Tel.: +47-93959483 Received: 15 October 2020; Accepted: 8 November 2020; Published: 10 November 2020 Abstract: The concept of Green Building refers to environmentally friendly constructions with the target of minimizing the impact on the natural environment through sustainable and efficient use of resources over their life cycle. Since modern buildings are large contributors to global energy consumption and greenhouse gas emissions, policies and international strategies intended to reduce the carbon footprint of conventional buildings are highlighting the role of this recently introduced building concept. This study provides a systematic literature review of existing research related to Green Buildings in the Arctic. Despite numerous studies and projects developed during the last decades, a study describing the current research status for this region is still missing. The review first examines the role that national and international policies developed by the arctic countries have on the development process of Green Buildings. Second, it provides an overview of the most commonly used and promoted Green Building rating systems used by the same countries in the region. The analysis highlights benefits and critical issues of Green Buildings located in the Arctic in comparison with conventional buildings, focusing on environmental, economic, and social dimensions. Finally, future research opportunities are presented and discussed. -
Ms Spitsbergen Voyage Handbook 2019–2020
voyage handbook MS SPITSBERGEN VOYAGE HANDBOOK 2019–2020 1 Dear Adventurer 2 Norway 4 Dear adventurer, Iceland 6 Congratulations on book- This handbook includes in- Svalbard 8 ing an extraordinary cruise formation on your chosen aboard MS Spitsbergen. destination, as well as other destinations this ship visits Faroe Islands 12 Norwegian explorer Roald during the 2019-2020 sailing Amundsen’s success as an ex- season. We hope you will find Orkney Islands 14 plorer is often explained by his this information inspiring. thorough preparations before Shetland Islands 16 departure. He once said “vic- We promise you an amazing Contents tory awaits him who has every- adventure! thing in order.” Being true to Franz Josef Land 18 Amund sen’s heritage of good Welcome aboard for the ad- planning, we encourage you to venture of a lifetime! Important Information 20 read this handbook. Frequently Asked Questions 21 It will provide you with good Your Hurtigruten Team advice, historical context, practical information, and in- Life on Board MS Spitsbergen 22 spiring information that will Practical Information make your voyage even more 28 enjoyable. Before and After Your Voyage Pack Like an Explorer 30 Our Team on Board 32 Landing by Small Boats 34 Important Phone Numbers 35 Maritime Expressions 35 MS Spitsbergen Deck Plan 36 2 COVER FRONT PHOTO: © ANDREA KLAUSSNER / HURTIGRUTEN 3 COVER BACK PHOTO: © DOMINIC BARRINGTON / HURTIGRUTEN © KARSTEN BIDSTRUP / HURTIGRUTEN / KARSTEN © BIDSTRUP came to prominence during the NATURE AND WILDLIFE Norway is a Viking era (800–1050 B.C.), Deep fjords, islets, and the high with strong trade relations and mountains of the Scandes, unique country colonies in Greenland, Ire- which belong to the Caledonien land, England, Scotland, and mountain range, characterize that continous- Normandy.