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Narvik (Lofoten) Explore Lofoten with your motorhome rental from Narvik Rent a campervan or a motorhome in Narvik (Lofoten) with CampingCar-Online/Ramble Campervans, specialists in motorhome rentals since 2001. We have carefully selected the best range of vehicles for you to choose from. Narvik (Lofoten) is an excellent starting point to explore northern Norway and the Lofoten Archipelago. Our specialists will guide you step by step through the motorhome rental process from Narvik (Lofoten). Narvik is situated in northern Norway on Ofotfjord close to Harstad/Narvik Airport (EVE) . The gateway to the Lofoten Islands, pick up your campervan or motorhome and explore the stunning scenery as you hop island to island through tiny fishing villages using bridges and ferries. The Lofoten Islands will enchant you. From Narvik you are surrounded by incredible outdoors, which give the opportunity to enjoy an almost limitless selection of outdoor activities. The arctic wilderness awaits you, from trail running, to climbing, to mountain biking, downhill skiing, hiking, alpine cross country skiing; you are spoiled for choice. Take a train ride across the whole of Norway to Kiruna in Sweden. The train ride only takes one hour and offers unparalleled views of the wild landscape, fjords and mountains. CampingCar-Online/Ramble Campervans can offer you the best value for money when renting your RV, motorhome or campervan from Narvik (Lofoten). We can also help you choose the best motorhome or campervan for your needs to explore Norway and the great outdoors departing from Narvik (Lofoten). © CampingCar-Online – 10 rue de Civry, 75016 Paris – FR : +33 (0) 1 40 71 10 20 / BE : 0 800 77 163 / CH : 0 800 56 33 79 - RCS Paris 434 838 140 Powered by TCPDF (www.tcpdf.org).

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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.
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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.
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NARVIK – Norwegian Eldorado for Wreck-Divers Wrecks of Narvik
NARVIK – Norwegian Eldorado for wreck-divers Wrecks of Narvik Text by Erling Skjold (history and diving) and Frank Bang (diving) Underwater photography by Frank Bang Ship photography by Erling Skjolds, NSA collection Translation by Michael Symes Dieter von Roeder The port of Narvik in north Norway was established around the export of iron-ore from Sweden. This was due to the very good harbour and its ice-free con- ditions. At the outbreak of World War II, Narvik was a strategically important harbour, and during the first few days of the war a very intense battle was fought out here between German, Norwegian and British naval forces. During this fighting several ships were sunk, both warships and civil merchant ships. Narvik harbour was transformed into a great ship ceme- tery, with wrecks sticking up out of the water every- where. Several of the ships were later salvaged, but many wrecks still remained. With its high density of wrecks, Narvik is an eldorado for wreck divers. A diver explores the wreck of the German destroyer Hermann Künne in Trollvika 61 X-RAY MAG : 5 : 2005 EDITORIAL FEATURES TRAVEL NEWS EQUIPMENT BOOKS SCIENCE & ECOLOGY EDUCATION PROFILES PORTFOLIO CLASSIFIED features Narvik Wrecks www.navalhistory.net Narvik harbour Maps outline battles in Narvik and around Norway during World War II Narvik harbour The importance of Narvik as a strate- Attack on April 9th the Eidsvold in just a few seconds. The that it was British gic harbour increased immediately at The German attack was a great surprise German ships could thereafter sail into forces that were the outbreak of World War II.
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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).
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Geochemical Investigations of Northern Norwegian Fjord Sediments – Sources and Spatial Variability of Marine and Terrigenous Components
Faculty of Science and Technology Department of Geology Geochemical investigations of northern Norwegian fjord sediments – Sources and spatial variability of marine and terrigenous components — Lea Philine Canzler Master thesis in Marine Geology and Geophysics (GEO-3900) May 2016 Abstract Fjords represent unique coastal marine environments with high sedimentation rates. They can be used for intensive investigations focusing on geochemical, mineralogical, biological, and sedimentological processes. In this study I investigate 42 surface sediment samples from the outer and inner parts of the Vestfjord, Ofotfjord, Tysfjord and tributary fjord arms in northern Norway. Samples were analysed for their bulk elemental composition, grain size distribution, and total carbon and nitrogen contents (Ctot, Ntot). Furthermore, total organic and inorganic carbon and nitrogen concentrations (Corg, Cinorg, Norg and Ninorg) as well as the carbon and nitrogen isotopes (δ13C, δ15N) were analysed. The measurements were performed to identify geochemical proxies for the contribution of terrestrial organic matter (TOM) versus marine organic matter (MOM) into the fjords. The results indicate a sedimentary environment characterized by an overall dominant contribution of MOM compared to the relatively small input of terrestrial derived material. The extremely high supply of MOM is presented by 13 Corg/Norg ratios ranging between 6 and 10, stable carbon isotope values (δ Corg) between -24‰ 15 and -21‰, and stable organic nitrogen (δ Norg) signatures that vary between 4.7‰ and 6.9‰. The terrigenous material content is in general extraordinary low, and TOM increases from the outer part of the Vestfjord towards the innermost fjord parts of the Ofotfjord and Tysfjord. A 13 15 correlation between δ Corg and δ Norg and the Corg/Norg ratios indicates high influences of marine derived OM.
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Cruice North 2013 Magasin.Indd
CRUISE NORTH 2013 EDITION TIME TO TURNAROUND IN THE NORTH? RUSSIA NEXT WINTER CRUISING NORTHERN SEA ROUTE TO JAPAN cnns.no It’s all about people, comfort and experiences in good All over Northern company. Norway Out travelling? Let us give you an unforgettable experience in our majestic landscape. www.boreal.no BODØ – HARSTAD/NARVIK – ANDØYA – BARDUFOSS – TROMSØ – ALTA – LAKSELV – KIRKENES – SVALBARD avinor.no/northernlights 2 CRUICE NORTH 2013 Contents Editorial 5 Turnarounds in Arctic Europe 6 Brønnøysund: A World Heritage Experience 13 Bodø: First port of call north of the Arctic Circle 14 Lofoten: Struck by Nature 15 Vesterålen: New port, new Adventures 16 Harstad: A cultural Destination 17 Narvik: Where two Borders meet 18 Tromsø: The Gateway to the Arctic 19 Alta: Winter Capital 20 Hammerfest: New Energy 21 North Cape: More than a Plateau 22 Vardø: Real Arctic 23 Kirkenes: Where East meets West 24 Longyearbyen: Northernmost Cruise Destination 25 Winter Cruise – The next thing to do 27 Who’s cruising the Northern Sailing Route first? 30 Explorer cruises in the North-East 31 Facts about CNNS 34 Editor: Erik Joachimsen (Cruise Northern Norway & Svalbard), [email protected] Layout: Idemasjon AS, Tromsø, Norway English translation and proof reading: Gavin Tanguay Oversetting og språkvasking, Tromsø, Norway Print run: 5.000 Printing: Lundblad Media, Tromsø, Norway Paper quality: G-Print 90x64 – 90 gr / MultiArt Gloss 46 x 64 130 gr Ecolabel: The Swan Copyright: Cruise Northern Norway & Svalbard SA (cnns.no) Meet Cruise Northern Norway & Svalbard at Cruise Shipping in Miami, March 11 – 14, 2013, at Booth # 892.
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International Council for the Exploration Ofthe Sea ICES C.M
.International Council for the ICES C.M. 1996/H:33 Exploration ofthe Sea Pelagic Fish Committee ACOUSTIC ABUNDANCE ESTIMATION OF THE STOCK OF NORWEGIAN SPRING SPAWNING HERRING, WINTER 1995-1996 by Kenneth G. Foote, Marek Ostrowski, IngolfR.0ttingen, Arill Engäs, Kaare A. Hansen, Kjellrun Hiis Hauge, Roar Skeide, Aril Slotte and 0yvind Torgersen Institute ofMarine Research P.O. Box 1870, N-5024 Bergen, Norway . ABSTRACT Standard echo integration methodology has been applied to the stock of Norwegian spring spawning herring (Clupea harengus) wintering in the Ofotfjord-Tysfjord-Vestfjord system during late autumn 1995 and early winter 1996. The primary instruments of acoustic data collection and processing were the SIMRAD EK500/38-kHz echo sounder and the Bergen Echo Integrator. Biological sampling was effected by means of a so-called MultiSampIer pelagic trawl in addition to standard pelagic trawls. Compensation was made during postprocessing for the effect ofacoustic extinction. The major complication ofthe survey and . challenge ofthe analysis has been stratification. This is discussed in the context of(1) mixing cif immature and mature year classes, each with its own behavioural characteristics apropos of diurnal vertical migration and outwards spawning migration, (2) degree of achieved survey coverage, depending on fjord geometry, navigational hazards, available time, and fish distribution, and (3) ongoing spawning migration. Because ofvarious uncertainties, aseries of abundance estimates is presented. These are accompanied by fitted variogram models and geostatistical variance estimates. .-------- ~---------- - --------- I • " .,.'i .I :I INTRODUCTION The spawning stock of Norwegian spring spawnmg herring (Clupea harengus) has been wintering in the fjords of northern Nonvay since autumn 1987.The stock has been concentrated, apparently exclusively, in the Ofotfjord-Tysfjord-Vestfjord system (Fig.
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Winter / Spring 2021
WINTER / SPRING 2021 Photo: Kjell G. Karlsen Photo: Rune Dahl SUMMER/AUTUMN 2021 CONTENT Narvik 68.44° N, 17.43° E WINTER | SPRING Piste Map 6-7 Cable Car Winter | Spring 8-9 Skiing | Snowboarding 10-11 Freeriding | Ski Touring 12-13 Ski School 14-15 16-17 Snowshoeing | Racing 18-19 Lights at the Lodge 20-21 Aurora at Narvikhytta SUMMER | AUTUMN Cable Car Summer | Autumn 24-25 Mountain Biking 26-27 Hiking 28-29 Tromsø YEAR-ROUND FUN Rope Park, Mountain Bike Flow Trail, Children Fun Park 30-31 Bardufoss ACCOMMODATION 32-33 ABOUT US 36 Our Cable Car 37 Harstad/Evenes Train to/from Stockholm The Guardians Mountain Restaurant 38 Ski Center 39 Kiruna The Train Factor 40 Narvik 2020/27 41 INFORMATION Prices 42-44 Contact & Where to Find Us 44-45 How to reach Narvik: Greenest : Night train from Stockholm (18 hours) Closest airport: Harstad/Narvik Evenes - 58 km (ca. 50 min) Other airports: Bardufoss - 103 km (ca. 1.5 hrs) Kiruna (SWE) - 187 km (ca. 2.5 hrs) Tromsø - 235 km (ca. 3.5 hrs) Car access: Via E6, Norway's main N-S road Via E10 from Lofoten or Sweden 2 3 Winter | Spring 4 5 Photo: Rune Dahl 6 7 Photo: Rune Dahl Narvikfjellet.no Photo: Kjetil Janson Cable Car Winter | Spring Photo: Kjetil Janson Photo: Josu Media Photo: Jonas Parkstam Season: December - May Our cable car is still unique in Northern Scandinavia. Nowhere (All year round on request) else you can reach such amazing scenery of mountains and fjords so fast and comfortably - our ten-seater gondola takes Activity Type: Your adventure you in just 6 minutes to 659 m above the Ofotfjord.
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The Influence of Fishing Activity on Killer Whale Feeding Behaviour
The influence of fishing activity on killer whale feeding behaviour Ylva Ericson Degree project in Biology 20 p, 2005 Biological Education Centre, Uppsala University Supervisors: Bo Tallmark, Department of Zooecology, Uppsala University Tiu Similä, WWF Killer whale project, Straumsjøen, Norway Summary The main wintering area of the North Atlantic herring is in the three fjords Tysfjord, Ofotfjord and Vestfjord in Northern Norway. The estimated amounts of herring overwintering in the fjords were 6 million tonnes in 2003 and 7 million tonnes in 2004. The stock stays in these fjords from mid-October to January. The herring is every year accompanied by around 1500 killer whales, specialised on the herring as their main prey species. The killer whales have evolved a fascinating feeding technique, called “carousel feeding”. During this procedure they circle around a school of herring to get it tight and bring it to the surface; the surface then acts as a barrier which prevents the herring from escaping. When the school is tight enough the whales slap their tail flukes through it, to stun or kill the fish. After that they eat the motionless fish one by one. Since the beginning of the 1990s, the herring fishery in the fjords has increased a lot, and it is still expanding each year as the herring biomass increases. When a purse-seiner or a pair trawler hauls in its net, or when two pair trawlers pull their nets between them to catch a school of herring, loud sounds are formed which draws killer whales to the place. The whales know that tired and lethargic fish escape in the processes, and these fish are easy to catch for them.
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Guns Blazing! Newsletter of the Naval Wargames Society No
All Guns Blazing! Newsletter of the Naval Wargames Society No. 194 –June 2010 EDITORIAL Gentlemen, You may find this difficult to believe, but this All Guns Blazing is my twelfth! Where the time has gone I can‘t even bring myself to fathom. It must be that adage about time passing quicker the older you get. Now there‘s a cheery thought! While I‘m wearing my editor‘s hat, I‘d like to apologise if this AGB seems a trifle rushed. For most of May I‘ve been working morning, noon and night, which has also included a two hundred-mile round trip commute to London on most days. Time, as you will appreciate, has been somewhat scarce! And while I‘m on the subject, this month is going to be hellish busy too, so if July‘s issue is a mite delayed, please bare with me—it‘s on its way! Actually, I‘ll be starting work at the Festival Theatre in Chichester for two-and-a-half months, which, as I‘m sure many of you are aware, is only a stone‘s throw from Portsmouth! If there are any members in that neck of the woods, especially if you‘re actually going to see ‗42nd Street‘ at the theatre, drop me an e-line and perhaps we could share a rum ration or two. While whizzing up and down the M40 can be wearing to both man and motor, it does have the benefit of throwing me in the path of all the delicious bookshops on, and just off, the Charing Cross Road.
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Northern Norway
Norway | Northern Norway Northern Norway Reine, The Lofoten Northern Norway’s weather No matter the time of year there is much to Tromso/ experience and discover in the land above the beaten landscape of high Arctic Circle. It is the region that keeps on giving Andenes mountain peaks, protected and will leave you wanting to explore further. inlets, farmland and idyllic Ringstad Sortland Stokmarknes Hadsel fishing villages can only be VESTVÅGØY Svolv described as a masterpiece North Cape Leknes nninsv Stamsund Narvik almost untouched by time. Alta Reine Kirkenes Tromsø Senja S Hadsel Svolv Leknes nninsv 1 2 3 Stamsund 4 Reine Wildlife Illuminating Arctic lights Unique hotels The Lofoten archipelago Look up and you might see a Even at the height of winter, at the Northern Norway is home to the The Lofoten is a nature lover’s Golden Eagle, White Tailed Eagle, time of the polar nights, Northern Sorrisniva Igloo Hotel and the paradise. A land of jagged mountain Gannets, Puffin or Kittiwakes. Take a Norway is alight with a magical Kirkenes Snow Hotel. A night here is peaks, sheltered bays, a coastline boat trip to see sperm, humpback, glow - twinkling stars, moonlight an experience that will remain with dotted with picture-postcard minke, orca and pilot whales, Not to and the Aurora Borealis. you for a lifetime. wooden houses and large areas of mention moose and reindeer. virgin territory with beaches, fjords and sea bird colonies. Note: Not all our accommodation is suitable for guests with reduced mobility. Please contact us to answer any questions you may have regarding our properties and to discuss their suitability for those with health conditions or impairments.
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Winter / Spring 2021
WINTER / SPRING 2021 Photo: Kjell G. Karlsen Photo: Rune Dahl SUMMER/AUTUMN 2021 CONTENT Narvik 68.44° N, 17.43° E WINTER | SPRING Piste Map 6-7 Cable Car Winter | Spring 8-9 Skiing | Snowboarding 10-11 Freeriding | Ski Touring 12-13 Ski School 14-15 Snowshoeing | Racing 16-17 Lights at the Lodge 18-19 Aurora at Narvikhytta 20-21 SUMMER | AUTUMN Cable Car Summer | Autumn 24-25 Mountain Biking 26-27 Hiking 28-29 Tromsø YEAR-ROUND FUN Rope Park, Mountain Bike Flow Trail, Children Fun Park 30-31 Bardufoss ACCOMMODATION 32-33 ABOUT US Our Cable Car 36 37 Harstad/Evenes Train to/from Stockholm The Guardians Mountain Restaurant 38 Ski Center 39 Kiruna The Train Factor 40 Narvik 2020/27 41 INFORMATION Prices 42-44 Contact & Where to Find Us 44-45 How to reach Narvik: Greenest : Night train from Stockholm (18 hours) Closest airport: Harstad/Narvik Evenes - 58 km (ca. 50 min) Other airports: Bardufoss - 103 km (ca. 1.5 hrs) Kiruna (SWE) - 187 km (ca. 2.5 hrs) Tromsø - 235 km (ca. 3.5 hrs) Car access: Via E6, Norway's main N-S road Via E10 from Lofoten or Sweden 2 3 Winter | Spring 4 5 Photo: Rune Dahl 6 7 Photo: Rune Dahl Narvikfjellet.no Photo: Kjetil Janson Cable Car Winter | Spring Photo: Kjetil Janson Photo: Josu Media Photo: Jonas Parkstam Season: December - May Our cable car is still unique in Northern Scandinavia. Nowhere (All year round on request) else you can reach such amazing scenery of mountains and fjords so fast and comfortably - our ten-seater gondola takes Activity Type: Your adventure you in just 6 minutes to 659 m above the Ofotfjord.
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