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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. -
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. -
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. -
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). -
NORWEGIAN MIDNIGHT SUN Across the Arctic Circle and Onto the North Cape
Lofoten Island Village NORWEGIAN MIDNIGHT SUN Across the Arctic Circle and onto the North Cape “Bucket list” destinations for most serious motorcycle globe- European large cities trotters include places such as Ushuaia, Prudhoe Bay, and • Spectacular southern Norway with its stave churches, some “the big one” - the northernmost point in the world to which of the oldest wooden buildings on the planet it’s possible to ride a motorcycle - Norway’s North Cape. • Ferry ride on the “world’s most beautiful fjord” - Geiranger is “tour to the top of the world” takes riders nearly 400 Fjord miles north of the Arctic Circle. Our major destination, Norway’s North Cape, is 50 miles further north of the Arctic • Trollstigen, Norway’s most spectacular pass road Circle than Prudhoe Bay, Alaska - the northernmost point • A rest day in Alesund, art nouveau city on the West Coast in North America accessible by motorcycle. is Adventure • e spectacular Lofoten Islands, where mountains rise directly will take you through the pristine beauty of Northern Norway out of the ocean with stunning and bizarre landscapes on endless roads through uninhabited wilderness. We will ride along the • Crossing the Arctic Circle Norwegian fjord–dotted coastline, cross the Lofoten Islands • An optional whale safari from Andenes and ride the never ending plains of Lappland up to the border of Russia. With 24 hours of daylight, you won’t miss a thing. • e North Cape, the northern tip of Europe is tour is about challenging and experiencing mother e last riding day is long, so you may wish to extend your stay nature and riding the roads that lead you to where Europe in Tromsø to enjoy additional sightseeing. -
THE NORTHERN NORWAY REGIONAL HEALTH AUTHORITY (Helse Nord RHF)
THE NORTHERN NORWAY REGIONAL HEALTH AUTHORITY (Helse Nord RHF) Northern Norway Regional Health Authority (Helse Nord RHF) is responsible for the public hospitals in northern Norway. The hospitals are organised in five trusts: • Finnmark Hospital Trust • University Hospital of Northern Norway Trust • Nordland Hospital Trust • Helgeland Hospital Trust • Hospital Pharmacy of North Norway Trust The trusts have their own management boards and are independent legal entities. Sector Healthcare Locations The four hospital Trusts are located in all of North Norway and Svalbard. Size Enterprise Data 5000 users since its launch in early 2011, will scale to approx. 12,500 users by the end of 2014. Company Website www.helse-nord.no For Reference Trond Kristiansen, E-Learning advisor. Nordland Hospital Trust Email - [email protected] Tel. +47 470 12 344 Øystein Lorentzen, Manager for IT Nordland Hospital Trust Email - [email protected] Tel. +47 900 40 566 THE NORTHERN NORWAY REGIONAL HEALTH AUTHORITY (Helse Nord RHF) Case Study Copyright © 2013 Docebo S.p.A. All rights reserved. Docebo is either a registered trademark or trademark of Docebo S.p.A. Other marks are the properties of their respective owners. To contact Docebo, please visit: www.docebo.com Company Customer Challenge The Northern Norway Regional Hospitals are often large and very Health Authority (Helse Nord RHF) complex organizations and is responsible for the public Docebo’s functionality fulfills many hospitals in northern Norway. of our needs right out of the box. The Regional Health Authority was Only basic customization with little established on the 1st January or no development is needed to "THROUGH COOPERATION 2002 when the central government implement the Docebo solution. -
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. -
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. -
Ultimate Norway Aurora Trip Itinerary
norway.nordicvisitor.com ULTIMATE NORWAY AURORA TRIP ITINERARY DAY 1 DAY 1: WELCOME TO OSLO When you arrive at Oslo‘s Gardermoen Airport, make your way into Oslo‘s city centre. Many travellers opt to take the express train to Oslo Central Station, but we can arrange a private transfer for you (at additional cost). For those arriving early, we recommend exploring Oslo by foot, spending the afternoon at sights including the Royal Palace, Akershus fortress, Oslo City Hall, Oslo Opera House, and the Aker Brygge area. Other notable attractions include the beautiful Vigeland Sculpture Park, the Viking Ship Museum and Karl Johans street. Spend the night in Oslo. Attractions: Aker Brygge, Oslo, Oslo City Hall, Oslo Opera House, The Royal Palace (Oslo) DAY 2 DAY 2: NORWAY IN A NUTSHELL IN WINTER - THE FLÅM RAILWAY Get an early start and head to Oslo Central Station, where you’ll begin the Norway in a Nutshell® railway journey towards Bergen, with an overnight stop in Flåm. This train ride takes you over Norway’s “mountainous rooftops”, through charming villages like Gol and Geilo. In Myrdal, you’ll switch trains to the famous Flåm Railway (Flåmsbana) for an incredible ride to the beautiful village of Flåm, which is especially lovely in winter. Enjoy a relaxing day in Flåm, where you can follow one of the many hiking trails in the mountains around the village, or participate in an optional activity such as a winter fjord safari. Spend the night in Flåm. We recommend booking our luggage transfer for the travel between Oslo and Bergen. -
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. -
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.