Narvik Cruise Port Narvik – Norway in Miniature
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Nord-Norgebanen Innspillkonferansene 2 Nordlandsbanen Ved Polarsirkelen Tre Innspillkonferanser Ble Avholdt I 2018
Nord-Norgebanen Innspillkonferansene 2 Nordlandsbanen ved Polarsirkelen Tre innspillkonferanser ble avholdt i 2018 • 8. juni i Tromsø • 11. september i Narvik • 2. oktober i Fauske 3 Forberedte innlegg i Tromsø • Troms fylkeskommune • Nordland fylkeskommune • Sametinget • Forsvaret • Naturvernforbundet • Tromsø kommunes jernbaneutvalg • Tromskomiteen for jernbane • NITO 4 Forberedte innlegg i Narvik • Sør-Troms regionråd • Ofoten regionråd • Narvik havn • Tromskomiteen for jernbane • NITO • Pole Position Logistics • Aksjonsgruppa for Nord- Norgebanen 5 U Utsikt fra Ofotbanen Forberedte innlegg på Fauske • Nord-Norsk reiseliv • Statens vegvesen • NHO Nordland • Gruppearbeid med innspill • Samt innspill direkte til prosjektgruppa utenom konferansene 6 Fauske stasjon Innspillene kan sorteres på følgende tema • Trafikksikkerhet, forsynings- sikkerhet og effektive transport- korridorer • Klima og miljø • Traséer • Sjømat og økende transportbehov • Regionforstørring og ringvirkninger • Sammenheng med andre baner • Samfunnsøkonomi 7 Trafikksikkerhet, forsyningssikkerhet og effektive transportkorridorer • Stadig flere vogntog på veg, følger for trafikksikkerhet og vegslitasje • Ventet videre økning i tungtrafikk vil gi store utfordringer på veg • Næringslivet i deler Nord-Norge avhengig av svensk bane og veg • Nord-Norgebanen vil bedre forsyningssikkerheten nasjonalt • Nord-Norgebanen bidrar til redusert sårbarhet Innspill Opplasting i Mosjøen 8 Miljø og klima • Krav til etisk og bærekraftig transport av mat vil komme i framtida (0-utslipp) • -
NINA Rapport Om Reindrift
1537 Reguleringsplan for Harstad/Narvik lufthavn og Evenes flystasjon Konsekvensutredning for reindrift Tømmervik, H., Henaug, C., Danielsen, I. & Langeland, K. NINAs publikasjoner NINA Rapport Dette er NINAs ordinære rapportering til oppdragsgiver etter gjennomført forsknings-, overvåkings- eller utredningsarbeid. I tillegg vil serien favne mye av instituttets øvrige rapportering, for eksempel fra seminarer og konferanser, resultater av eget forsknings- og utredningsarbeid og litteraturstudier. NINA Rapport kan også utgis på annet språk når det er hensiktsmessig.. NINA Temahefte Som navnet angir behandler temaheftene spesielle emner. Heftene utarbeides etter behov og serien favner svært vidt; fra systematiske bestemmelsesnøkler til informasjon om viktige problemstillinger i samfunnet. NINA Temahefte gis vanligvis en populærvitenskapelig form med mer vekt på illustrasjoner enn NINA Rapport. NINA Fakta Faktaarkene har som mål å gjøre NINAs forskningsresultater raskt og enkelt tilgjengelig for et større publikum. Faktaarkene gir en kort framstilling av noen av våre viktigste forskningstema. Annen publisering I tillegg til rapporteringen i NINAs egne serier publiserer instituttets ansatte en stor del av sine vitenskapelige resultater i internasjonale journaler, populærfaglige bøker og tidsskrifter. Reguleringsplan for Harstad/Narvik lufthavn og Evenes flystasjon Konsekvensutredning for reindrift Hans Tømmervik Cathrine Henaug Inge Danielsen Knut Langeland Norsk institutt for naturforskning NINA Rapport 1537 Tømmervik, H. Henaug, C., Danielsen, -
Stable Isotope Records for the Last 10 000 Years from Okshola Cave (Fauske, Northern Norway) and Regional Comparisons
Clim. Past, 5, 667–682, 2009 www.clim-past.net/5/667/2009/ Climate © Author(s) 2009. This work is distributed under of the Past the Creative Commons Attribution 3.0 License. Stable isotope records for the last 10 000 years from Okshola cave (Fauske, northern Norway) and regional comparisons H. Linge1,2, S.-E. Lauritzen1,5, C. Andersson2,1, J. K. Hansen1, R. Ø. Skoglund1, and H. S. Sundqvist3,4 1Department of Earth Science, University of Bergen, Allegaten´ 41, 5007 Bergen, Norway 2Bjerknes Centre for Climate Research, Allegaten´ 55, 5007 Bergen, Norway 3Department of Physical Geography and Quaternary Geology, Stockholm University, 10691 Stockholm, Sweden 4Bert Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden 5Department of Plant and Environmental Sciences, Norwegian University of Life Sciences, 1432 As,˚ Norway Received: 8 June 2009 – Published in Clim. Past Discuss.: 1 July 2009 Revised: 14 October 2009 – Accepted: 23 October 2009 – Published: 3 November 2009 18 Abstract. The sensitivity of terrestrial environments to past development for the last millennium. Although the δ Oc changes in heat transport is expected to be manifested in records show similar patterns and amplitudes of change, Holocene climate proxy records on millennial to seasonal the main challenges for utilising high-latitude stalagmites as timescales. Stalagmite formation in the Okshola cave near palaeoclimate archives are i) the accuracy of the age mod- Fauske (northern Norway) began at about 10.4 ka, soon after els, ii) the ambiguity of the proxy signals, and iii) calibration the valley was deglaciated. Past monitoring of the cave and with monitoring data. -
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. -
Kiruna Ice Guide
Ice climbing in Lapland A guide by Rick1 McGregor Copyright: Rick McGregor and the photographers, 2014. First edition: 2005 Revised edition: 2014. Acknowledgements: Thanks to the photographers for the use of their photos, and to Peter Engström, Dick Johansson, Børge Soleng, Henrik Lindgren, Rafael Jensen, Peter Sundvall and many others for information about the climbs. Cover photo: Henrik Lindgren climbing on Kaisepakte (photo: Rick McGregor) 2 Ice climbing in Lapland A guide to ice climbs in the Kiruna area, Northern Scandinavia by Rick McGregor The Rock Falcon Press Kiruna, Sweden Revised Edition, March 2014 3 Contents Introduction................................................................................................................................ 5 Kiruna......................................................................................................................................... 6 West of Kiruna........................................................................................................................... 6 Torneträsk........................................................................................................................... 6 Kaisepakte/Gaisebakti........................................................................................................ 7 Hidden Valley/Gömda dalen.............................................................................................. 9 Lillpakte........................................................................................................................... -
Revision of the EU's Arctic Strategy
Sent by e-mail Breivikbotn, November 9th 2020 Input – Revision of the EU’s Arctic strategy Additional input from a total of 40 municipalities in North Norway, to the public consultation regarding the revision of the EU’s Arctic strategy. The municipalities are represented by 5 inter- municipal counsils; Vest-Finnmark Rådet (7 municipalities in Troms and Finnmark County), Vesterålen regionråd (6 municipalities in Nordland County), Salten Regionråd (10 municipalities in Nordland County), Indre Helgeland Regionråd (5 municipalities in Nordland County) and Helgelandsrådet (12 municipalities in Nordland County); 1. In your view, what have been the EU’s main achievements and failures under each of the three priorities in the 2016 Joint Communication? Vest-Finnmark Rådet, Vesterålen regionråd, Salten Regionråd, Indre Helgeland Regionråd and Helgelandsrådet embraces the EU’s engagement in promoting sustainable development in the Arctic. This priority marks a positive shift in how the Arctic is perceived as a strategically important territory, with green growth potential for the region and Europe. The EU’s top priority should be to assist the region in overcoming the Arctic paradox. That is, changing a demographic trend that is inversely correlated with economic growth. A stable demographic development is a necessary precondition for development and security in the Arctic regions. The most important means of meeting regional challenges in the Nordic/European part of the Arctic is by making use of the large natural resources in the region to stimulate economic growth and create new attractive jobs including utilizing the research institutions in the Arctic. The EU’s Arctic engagement shows great achievement, as exemplified by the processes leading to the report on Arctic investment needs in 2017, and the EU Arctic Forum in 2019. -
Norwegian Journal of Entomology
Norwegian Journal of Entomology Volume 47 No. 1 • 2000 Published by the Norwegian Entomological Society Oslo and Stavanger NORWEGIAN JOURNAL OF ENTOMOLOGY A continuation of Fauna Norvegica Serie B (1979-1998), Norwegian Journal ofEntomology (1975 1978) and Norsk Entomologisk TIdsskrift (1921-1974). Published by The Norwegian Entomological Society (Norsk entomologisk forening). Norwegian Journal of Entomology publishes original papers and reviews on taxonomy, faunistics, zoogeography, general and applied ecology of insects and related terrestrial arthropods. Short com munications, e.g. less than two printed pages, are also considered. Manuscripts should be sent to the editor. Editor Lauritz S~mme, Department of Biology, University of Oslo, P.O.Box 1050 Blindem, N-03l6 Oslo, Norway. E-mail: [email protected]. Editorial secretary Lars Ove Hansen, Zoological Museum, University of Oslo, Sarsgate 1, N-0562 Oslo. E-mail: [email protected]. Editorial board Ame C. Nilssen, Troms~ John O. Solem, Trondheim Uta Greve Jensen, Bergen Knut Rognes, Stavanger Ame Fjellberg, Tj~me The goal of The Norwegian Entomological Society is to encourage the study of entomology in Norway and to provide a meeting place for those who are interested in the field. Annual membership fees are NOK 200 Guniors NOK 100) for members with addresses in Norway, and NOK 220 (Juniors NOK 110) for members abroad. Inquiries about membership should be sent to the secretary: Jan A. Stenl~kk, P.O.Box 386, N-4oo2 Stavanger. Norway. E-mail: [email protected]. Norsk entomologisk forening (NEF) ser som sin oppgave afremme det entomologiske studium i Norge, og danne et bindeledd mellom de interesserte. -
Ski Touring in the Narvik Region
SKI TOURING IN THE NARVIK REGION TOP 5 © Mattias Fredriksson © Mattias Narvik is a town of 14 000 people situated in Nordland county in northern Norway, close to the Lofoten islands. It is also a region that serves as an excellent base for alpine ski touring and off-piste skiing. Here, you are surrounded by fjords, islands, deep valleys, pristine lakes, waterfalls, glaciers and mountain plateaus. But, first and foremost, wild and rugged mountains in seemingly endless terrain. Imagine standing on one of those Arctic peaks admiring the view just before you cruise down on your skis to the fjord side. WHY SKI TOURING IN THE NARVIK REGION? • A great variety in mountain landscapes, from the fjords in coastal Norway to the high mountain plateaus in Swedish Lapland. • Close to 100 high quality ski touring peaks within a one- hour drive from Narvik city centre. • Large climate variations within short distances, which improves the chances of finding good snow and weather. • A ski touring season that stretches from the polar night with its northern lights, to the late spring with never- ending days under the midnight sun. • Ascents and descents up to 1700 metres in vertical distance. • Some of the best chute skiing in the world, including 1200-metre descents straight down to the fjord. • Possibilities to do train accessed ski touring. • A comprehensive system of huts that can be used for hut-to-hut ski touring or as base camps. • 5 alpine skiing resorts within a one-hour car drive or train ride • The most recognised heli-skiing enterprise in Scandinavia, offering access to over 200 summits. -
Year-End Report 2019: Strong Earnings in an Uncertain Market
PRESS RELEASE Attachments: Date: 1 (3) 11/02/2020 Contact: Bo Krogvig, Senior Vice President Communications and Climate, LKAB Telephone: +46 (0)8 429 3445 Email: [email protected] Year-end report 2019: Strong earnings in an uncertain market Stable production and favourable market conditions enabled LKAB to increase its operating profit both for the quarter and for the full year, this despite lower delivery volumes. The market remains uncertain, however. Sales for full-year 2019 increased to MSEK 31,260 (25,892) and operating profit strengthened to MSEK 11,788 (6,869), an increase of 72 percent. The improved earnings are mainly due to higher iron ore prices and a stronger dollar exchange rate. Lower sales had an adverse effect. Operating cash flow for the full year increased to MSEK 6,981 (3,386). The improvement is mainly due to the increase in profits and to lower levels of capital expenditure. Higher expenditure on urban transformation had a negative impact. Profit for the year amounted to MSEK 10,173 (5,274) and the Board is proposing to the Annual General Meeting an ordinary dividend amounting to MSEK 6,104 (3,164). For the fourth quarter sales increased to MSEK 6,947 (6,911) and operating profit increased to MSEK 2,047 (1,900). The improved earnings are mainly a result of a stronger dollar exchange rate and lower costs for urban transformation provisions. Lower prices for highly upgraded iron ore products and lower delivery volumes during the quarter had an adverse effect. “I am pleased that we are delivering strong earnings despite an uncertain market and despite making significant investments in both the ongoing urban transformation and our projects for the future. -
PORT of NARVIK Arctic-Hub
PORT OF NARVIK Arctic-Hub Narvik is a part of the CORE EU TEN-T rail, port and road Network 1 Arctic-Hub The geographic location of Narvik as a hub/transit port is strategically excellent in order to move goods to and from the region (north/south and east/west) as well as within the region itself. The port of Narvik is incorporated in EU’s TEN-T CORE NETWORK. On-dock rail connects with the international railway network through Sweden for transport south and to the European continent, as well as through Finland for markets in Russia and China. Narvik is the largest port in the Barents Region and an important maritime town in terms of tonnage. Important for the region Sea/port Narvik’s location, in relation to the railway, road, sea and airport, Ice-free, deep sea port which connects all other modes of makes the Port of Narvik a natural logistics intersection. transport and the main fairway for shipping. Rail Airport: The port of Narvik operates as a hub for goods transported by Harstad/Narvik Airport, Evenes is the largest airport in North- rail (Ofotbanen) to this region. There are 19 cargo trains, in ern Norway and is one of only two wide body airports north each direction (north/south), moving weekly between Oslo and of Trondheim. Current driving time 1 hour, however when the Narvik. Transportation time 27 hours with the possibility of Hålogaland Bridge opens in 2017, driving time will be reduced making connections to Stavanger and Bergen. to 40 minutes. The heavy haul railway between Kiruna and Narvik transports There are several daily direct flights from Evenes to Oslo, 20 mt of iron ore per year (2015). -
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).