NARVIK – Norwegian Eldorado for Wreck-Divers Wrecks of Narvik
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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. -
LOFOTEKSPRESSEN SOMMERRUTE/SUMMER ROUTE 2019 Bård Løken/Nordnorge.Com Bård REINE Jørn Allan Pedersen/Visitnorway.Com Allan Jørn
LOFOTEKSPRESSEN SOMMERRUTE/SUMMER ROUTE 2019 Bård Løken/nordnorge.com Bård REINE Jørn Allan Pedersen/visitnorway.com Allan Jørn Lofotekspressen lets you discover the Lofoten Islands Lofotekspressen lar deg oppleve fantastiske Lofoten Lofotekspressen lets you discover the Lofoten Islands slik du selv ønsker. I sommer har vi hyppigere avganger your way. With more frequent routes, you can see the og går hele tre ganger daglig mellom Narvik og Å. extraordinary surroundings whenever and wherever Prøv vår reiseplanlegger på 177nordland.no, you want to. Check out our new travel planner on hvor du enkelt kan planlegge hvor du vil dra 177nordland.no, where you can easily plan where you og hvordan du kommer deg dit. Med vårt nye want to go and how to get there. With Travel Pass reisepass, Travel Pass Nordland, kan du ta buss Nordland you can hop on and off all of our buses and og hurtigbåt så mye du ønsker i sju dager. express boats as much as you like for seven days. We have gathered the best tips, 177 NORDLAND destinations and personal favourites App for route information from Lofoten on our website. 177nordland.no/lofotekspressen 2 3 I sommerhalvåret går rute 300 fra Å til Narvik tre VERDENS VAKRESTE ganger om dagen. Len deg tilbake og nyt en av de mest spektakulære bussturene du noen gang kommer til å ta. RUTEBUSSTUR Mellom Å og Narvik er naturen så slående at du skulle ønske reisen varte lenger. Lokalbefolkningen trekker fram Auster- og Vesterstraumen som spesielt naturskjønne motiver. Husk å ha kameraet klart! Fra Narvik kan du ta Ofotbanen til Nord-Sverige eller fly fra Harstad/Narvik Lufthavn til dine valgte lokasjoner. -
The >494 Ma Lillevik Ophiolite Fragment (Gratangseidet Igneous
University of Plymouth PEARL https://pearl.plymouth.ac.uk Faculty of Science and Engineering School of Geography, Earth and Environmental Sciences 2021-01-05 The >494 Ma Lillevik ophiolite fragment (Gratangseidet Igneous Complex) near Narvik, Scandinavian Caledonides Slagstad, T http://hdl.handle.net/10026.1/17056 10.17850/njg100-4-5 Norwegian Journal of Geology Geological Society of Norway All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. NORWEGIAN JOURNAL OF GEOLOGY https://dx.doi.org/10.1785/njg100-4-5 The >494 Ma Lillevik ophiolite fragment (Gratangseidet Igneous Complex) near Narvik, Scandinavian Caledonides Trond Slagstad¹, Mark Anderson², Kerstin Saalmann¹ & Graham Hagen-Peter¹ 1Geological Survey of Norway, 7491 Trondheim, Norway. ²School of Geography, Earth and Environmental Sciences, Plymouth University, Plymouth, UK. E-mail corresponding author (Trond Slagstad): [email protected] Keywords: One of several irregular, plagioclase-phyric felsic veins in the Lillevik ophiolite fragment (Gratangseidet • Lillevik ophiolite fragment Igneous Complex) in Narvik, northern Norway, yielded a U–Pb zircon age of 494 ± 5 Ma. The veins cut • Caledonides deformed, compositionally layered, light REE-depleted gabbros that arguably constituted part of the • Ophiolite now-dismembered ophiolite stratigraphy. The felsic veins were themselves deformed, probably during • Cambrian Silurian Scandian deformation, but the cross-cutting relationships suggest that they post-date initial deformation of the ophiolitic rocks. -
January Cover.Indd
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Neotectonics in Norway
Neotectonics in Norway N TNU Trondheim NGU Report 2000.002 Neotectonics in Norway Final Report Geological Survey of Norway N-7491 Trondheim, Norway Tel.: 47 73 90 40 11 Telefax 47 73 92 16 20 REPORT Report no.: 2000.002 ISSN 0800-3416 Grading: Confidential to 01.07.2001 Title: Neotectonics in Norway, Final Report Authors: Clients: Odleiv Olesen, John Dehls, Hilmar Bungum, Fridtjof BP-Amoco, Norsk Hydro, Phillips Petroleum, Riis, Erik Hicks, Conrad Lindholm, Lars Harald Statkraft, NFR, NGU, NORSAR, NPD and Blikra, Willy Fjeldskaar, Lars Olsen, Oddvar Longva, SK Jan Inge Faleide, Lars Bockmann, Leif Rise, David Roberts, Alvar Braathen and Harald Brekke. County: Number of pages: 135 Price (NOK): Finnmark, Troms, Nordland, Møre & Romsdal, Sogn Map enclosures: 1 & Fjordane, Hordaland and Rogaland Fieldwork carried out: Date of report: Project no.: Person responsible: 31.01.2000 2757.00 Summary: Geodynamic modelling of the present crustal uplift indicates that the uplift of western Norway and northern Norway is partly due to other mechanisms that the glacioisostatic rebound. We have also deduced a new model based on the ‘seismic pumping’ mechanism to explain the observed correlation between land uplift and groundwater yield in Norway. Rock avalanches and landslides represent the most hazardous effects of earthquakes in Norway with its mountainous terrain, deep fjords and relatively large areas with unstable quick-clay. New seismic mini-arrays in the Ranafjord area and the northern North Sea have sharply defined zones of increased seismicity. A total of 350 earthquakes have been detected in the outer Ranafjord area during the project period (2½ years), with magnitudes up to 2.8. -
The Heroic Destroyer and "Lucky" Ship O.R.P. "Blyskawica"
Transactions on the Built Environment vol 65, © 2003 WIT Press, www.witpress.com, ISSN 1743-3509 The heroic destroyer and "lucky" ship O.R.P. "Blyskawica" A. Komorowski & A. Wojcik Naval University of Gdynia, Poland Abstract The destroyer O.R.P. "Blyskawica" is a precious national relic, the only remaining ship that was built before World War I1 (WW2). On the 5oth Anniversary of its service under the Polish flag, it was honoured with the highest military decoration - the Gold Cross of the Virtuti Militari Medal. It has been the only such case in the whole history of the Polish Navy. Its our national hero, war-veteran and very "lucky" warship. "Blyskawica" took part in almost every important operation in Europe throughout WW2. It sailed and covered the Baltic Sea, North Sea, all the area around Great Britain, the Atlantic Ocean and Mediterranean Sea. During the war "Blyskawica" covered a distance of 148 thousand miles, guarded 83 convoys, carried out 108 operational patrols, participated in sinking two warships, damaged three submarines and certainly shot down four war-planes and quite probably three more. It was seriously damaged three times as a result of operational action. The crew casualties aggregated to a total of only 5 killed and 48 wounded petty officers and seamen, so it was a very "lucky" ship during WW2. In July 1947 the ship came back to Gdynia in Poland and started training activities. Having undergone rearmament and had a general overhaul, it became an anti-aircraft defence ship. In 1976 it replaced O.R.P. "Burza" as a Museum-Ship. -
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. -
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). -
5Th – 14Th MARCH 2020
5th – 14th MARCH 2020 Photo: Jan-Arne Pettersen Jan-Arne Photo: Finally the time has come for Narvik and races in Narvik are the most important races in Narvikfjellet to be filled with alpinists, their careers so far. We know that some of the managers, drivers, service personnel, parents, competitors will become world stars in a few and others from all over the world. years time. The last big international races in Narvik were However, everyone is equally important to us, in 1992 and 1996, when we held the World and our goal is for everyone to remember this Cup women’s race. We have great ambitions championship in Narvik as a great experience. for future events, and the goal is to be able to apply for the World Championships in We hope that everyone has a wonderful alpine skiing in 2027. In order to achieve this and memorable stay in Narvik, and that the dream, we have to deliver at all levels for all conditions are the runs on the mountain - from children’s the same for all races to now, the FIS Alpine Junior World Ski competitors. Championships 2020. We have worked long and hard to provide the best runs, the best food, the best ceremonies, With sporting and the best logistics for each and every one greetings of you during the championships. Many of the competitors here are attempting to become Erik D. Plener World Cup skiers, and, for most of them, these CEO, Narvik Alpin AS On behalf of Narvik and Northern Norway beautiful fjords and lakes has immense value I welcome you all to the FIS Alpine Junior for us. -
1997 FF13.Pdf
"'\ "',-' ,,- .' ' ... ' ( >J .•; International Council for the ICES C.M. 1997/FF:13 Exploration'of the Sea Fisheries Technology Theme Session ABUNDANCE ESTIMATION OF NORWEGIAN SPRING SPAWNING HERRING WINTERING IN THE VESTFJORD SYSTEM, DECEMBER 1996 by 2 4 Kenneth G. FooteI, Marek Ostrowski , Ingolf R~ttingen3 and Aril Slotte • Institute ofMarine Research P. O. Box 1870 N-5024 Bergen, Norway ABSTRACT The spawning stock ofNorwegian spawning herring has been surveyed when wintering in the Vestfjord, Tysfjord, and Ofotfjord, in northern Norway in December 1996. Tbe basic method is that of echo integration, with compensation for acoustic extinction. Physical capture has been effected by means of the MultisampIer pelagic trawl, which allows remote opening and • closing of each of three codends at arbitrary depths. This has shown essentially thorough mixing of the dominant year classes except in the two fjord arms, where the sampIes contained a larger proportion of older fish (1983 year class). Geostatistics has been employed to describe the spatial structure and to provide an estimate of variance. Data quality control procedures have been performed and are described. 1 e-mail: [email protected] teU: +47 55 23 84 65 fax; +47 55 23 85 32 2 e-mail: [email protected] telf: +47 55 23 6848 fax: +4755 23 83 32 3 e-mail: [email protected]· telf: +47 55238404 fax: +47 55 23 86 87 4 e-mail: [email protected] telf; +4755 23 84 22 fax: +4755 23 86 87 - .. _------------ INTRODUCTION The spawning stock ofNorwegian spring spawning'heinri~'~~'been wintering in the _fjords of northern Norway since 1987. -
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. -
01 CERL VII Prelims 31/8/07 6:15 PM Page I
01 CERL VII prelims 31/8/07 6:15 PM Page i imprints and owners 01 CERL VII prelims 31/8/07 6:15 PM Page ii 01 CERL VII prelims 31/8/07 6:15 PM Page iii cerl papers . vii Imprints and owners: Recording the cultural geography of Europe Papers presented on 10 November 2006 at the CERL Seminar hosted by the National Széchényi Library, Budapest edited by David J. Shaw London 2007 Consortium of European Research Libraries 01 CERL VII prelims 31/8/07 6:15 PM Page iv Published in 2007 by The Consortium of European Research Libraries The Finsbury Business Centre, 40 Bowling Green Lane, Clerkenwell, London ec1r 0ne Telephone 020 7415 7134 Fax 020 7970 5643 www.cerl.org Copyright © 2007 the contributors isbn 0–9541535–6–1 Designed by James Mosley, Justin Howes and Derek Brown, and typeset by Derek Brown in Matthew Carter’s Galliard CC Produced by Oblong Creative Ltd, Wetherby, West Yorkshire 01 CERL VII prelims 31/8/07 6:15 PM Page v Contents 2 Ádám Hegyi and Róbert Zawiasa: Character encoding in the Mokka-r 1 István Monok: The Union Catalogue of Rare Book Collections in the Carpathian Basin: about the expert system on book history in Hungary 7 Marianne Rozsondai and Béla Rozsondai: Cataloguing rare books in the Library of the Hungarian Academy of Sciences: problems of incunabula and copy-specific data 15 Tony Curwen and Gunilla Jonsson: Provenance and the Itinerary of the Book: recording provenance data in on-line catalogues 31 Alexander Jahnke: Accessing the record of European printed heritage: the CERL Thesaurus as an international repository of names from the hand-press era 49 Kristian Jensen: Old books in new libraries: democratisation of access or a digital divide 67 2 List of contributors 83 v 01 CERL VII prelims 31/8/07 6:15 PM Page vi 02 CERL VII art 01 31/8/07 6:16 PM Page 1 Characer encoding in the Mokka-r ádám hegyi and róbert zawiasa A Magyar Országos Közös Katalógus – Régi Nyomtatványok (MOKKA-R) során többször találkozunk a karakterkódolás problémájával.