International Council for the Exploration Ofthe Sea ICES C.M
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KU for Kommuneplanens Arealdel 2017 – 2029
KU for Kommuneplanens Arealdel 2017 – 2029 Konsekvensutredning for byggeområder til arealdelen Henningsvær vegen i november 2011 – Stormen Berit går på land i Vågan! (Foto: Vågan kommune) Svolvær 19 juni-17, revidert 11 des 2017 etter kommunestyrets vedtak i sak 102 og mekling 19 des- 17. Plankart og vurderinger er oppdatert 20 mars-18 i hht kommunestyrets vedtak i sak 102 og meklingsresultat avklart hos fylkesmannen 19 des-17. 1 1 - INNLEDNING Denne konsekvensutredning inngår som del av forslaget til arealplan med tilhørende bestemmelser, retningslinjer og ROS-analyse. Planens viktigste siktemål er å tilrettelegge for vekst og utvikling i hele kommunen. Dette er et perspektiv som gjennomsyrer kommunens planlegging. Dette har også fått som konsekvens at de viktigste vekstområder i kommunen – Svolvær og Kabelvåg – behandles i egne kommunedelplaner som må sees i sammenheng med denne arealplanen. Svolvær har sin kommunedelplan fra 2012, mens Kabelvåg skal revidere sin gamle plan fra 1995 så snart som mulig. I dette planforslaget er fokus innrettet mot kommunens 8 viktige småsteder som har sine egne skoler og servicetjenester som kan styrke den spredte bosetting og næringsstruktur som kommunen ønsker å videreføre. Kommunen satser tungt på å skape nye arbeidsplasser i skolekretsene for å opprettholde og øke befolkningsgrunnlaget der. Dette sterke fokus på vekst i kommunens ytre områder, kan bli oppfattet som konfliktfylt visavis nasjonale mål om en bærekraftig areal og transportpolitikk der sykkel og gange skal være den gjennomgående strategi for å bedre miljøet i Norge og alle lokalsamfunn. I et slikt perspektiv vil utviklingen i hele kommunen være avgjørende der aksen Svolvær – Kabelvåg vil representere den store vekstkraften. -
Cruise Report
CRUISE REPORT MARINE GEOLOGICAL CRUISE TO VESTFJORDEN AND EASTERN NORWEGIAN SEA R.V. Jan Mayen 29.05. -08.06. 2003 by Gaute Mikalsen Torbjørn Dalhgren DEPARTMENT OF GEOLOGY UNIVERSITY OF TROMSØ N-9037 TROMSØ, NORWAY Introduction The cruise was a joint cruse between four projects at The Department of Geology, University of Tromsø. For the last part of the cruise we were joined by one scientist and tow technicians from the Norwegian Collage of Fisheries, they embarked in Andenes. Their work spanned the last two days of the cruise And is not reported here. Objectives and Projects The main objective for this cruise was to retrieve sediment cores and seismics for the projects SPONCOM, NORDPAST-2, EUROSTRATAFORM and Dr. T. Dalhgrens project (Statoil). SPONCOM: “Sedimentary Processes and Palaeoenvironment on Northern Continental Margins” is a strategic university programme at Department of Geology, University of Tromsø founded by the Norwegian Research Council. The primary goal is to assess the changes in the physical environment of the seafloor and its overlying water and ice of West Spitsbergen and North Norwegian fjords and continental margin during the last glacial – interglacial cycle. On this cruise the aim was to retrieve material from North-Norwegian fjords and the continental margin elucidating the following sub goals: 1). The chronology and dynamics of the last glaciation – deglaciation. 2). Processes and fluxes of fjord, continental shelf and – slope sedimentation. 3). Rapid palaeoceanographic and palaeclimatic changes, particularly during the last deglaciation and the Holocene. NORPAST-2: “Past Climate of the Norwegian Region – 2” is a national project founded by the Norwegian Research Council. -
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). -
Connectivity Among Subpopulations of Norwegian Coastal Cod Impacts of Physical-Biological Factors During Egg Stages
Connectivity among subpopulations of Norwegian Coastal cod Impacts of physical-biological factors during egg stages Mari Skuggedal Myksvoll Dissertation for the degree of Philosophiae Doctor (PhD) Geophysical Institute, University of Bergen, Norway January 2012 Connectivity among subpopulations of Norwegian Coastal cod Impacts of physical-biological factors during egg stages Mari Skuggedal Myksvoll Institute of Bjerknes Center for Marine Research Climate Research Dissertation for the degree of Philosophiae Doctor (PhD) Geophysical Institute, University of Bergen, Norway January 2012 Outline This thesis consists of an introduction and four papers. The introduction provides a scientic background of the population structure of Atlantic cod stocks in Norwegian Waters and the research history of fjord dynamics (Section 1). Section 2 states the motivation for the study and the most important results from the papers. A discussion follows focusing on the implications of the present results (Section 3) and perspectives for future research are stated in Section 4. • Paper I: Retention of coastal cod eggs in a fjord caused by interactions between egg buoyancy and circulation pattern Myksvoll, M.S., Sundby, S., Ådlandsvik, B. and Vikebø, F. (2011) Marine and Coastal Fisheries, 3, 279-294. • Paper II: Importance of high resolution wind forcing on eddy activity and particle dispersion in a Norwegian fjord Myksvoll, M.S., Sandvik, A.D., Skarðhamar, J. and Sundby, S. (2012) Submitted to Estuarine, Coastal and Shelf Sciences • Paper III: Eects of river regulations on fjord dynamics and retention of coastal cod eggs Myksvoll, M.S., Sandvik, A.D., Asplin, L. and Sundby, S. (2012) Manuscript • Paper IV: Modeling dispersal of eggs and quantifying connectivity among Norwegian Coastal cod subpopulations Myksvoll, M.S., Jung, K.-M., Albretsen, J. -
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. -
Absorption Properties of High-Latitude Norwegian Coastal Water: the Impact of CDOM and Particulate Matter
Estuarine, Coastal and Shelf Science 178 (2016) 158e167 Contents lists available at ScienceDirect Estuarine, Coastal and Shelf Science journal homepage: www.elsevier.com/locate/ecss Absorption properties of high-latitude Norwegian coastal water: The impact of CDOM and particulate matter * Ciren Nima a, b, , Øyvind Frette a, Børge Hamre a, Svein Rune Erga c, Yi-Chun Chen a, Lu Zhao a, Kai Sørensen d, Marit Norli d, Knut Stamnes e, Jakob J. Stamnes a a Department of Physics and Technology, University of Bergen, Norway b Department of Physics, Tibet University, China c Department of Biology, University of Bergen, Norway d Norwegian Institute for Water Research, Norway e Stevens Institute of Technology, USA article info abstract Article history: We present data from measurements and analyses of the spectral absorption due to colored dissolved Received 22 October 2015 organic matter (CDOM), total suspended matter (TSM), phytoplankton, and non-algal particles (NAP) in Received in revised form high-latitude northern Norwegian coastal water based on samples taken in spring, summer, and autumn. 9 April 2016 The Chlorophyll-a (Chl-a) concentration was found to vary significantly with season, whereas regardless Accepted 12 May 2016 of season CDOM was found to be the dominant absorber for wavelengths shorter than 600 nm. The Available online 18 May 2016 À1 absorption spectral slope S350À500 for CDOM varied between 0.011 and 0.022 nm with mean value and À standard deviation given by (0.015 ± 0.002) nm 1. The absorption spectral slope was found to be strongly Keywords: fi High-latitude coastal water dependent on the wavelength interval used for tting. -
Fault-Controlled Asymmetric Landscapes and Low-Relief Surfaces on Vestvågøya, Lofoten, North Norway: Inherited Mesozoic Rift-Margin Structures?
NORWEGIAN JOURNAL OF GEOLOGY Vol 98 Nr. 4 https://dx.doi.org/10.17850/njg98-3-06 Fault-controlled asymmetric landscapes and low-relief surfaces on Vestvågøya, Lofoten, North Norway: inherited Mesozoic rift-margin structures? Steffen G. Bergh1, Kristian H. Liland2, Geoffrey D. Corner1, Tormod Henningsen2 & Petter A. Lundekvam1 1Department of Geosciences, University of Tromsø UiT-The Arctic University of Norway, 9037 Tromsø, Norway. 2Equinor ASA, Harstad, Norway E-mail corresponding author (Steffen G. Bergh): [email protected] The Lofoten Ridge is an integral basement horst of the hyperextended continental rift-margin off northern Norway. It is a key area for studying onshore–offshore rift-related faults, and for evaluating tectonic control on landscape development along the North Atlantic margin. This paper combines onshore geomorphological relief/aspect data and fault/fracture analysis with offshore bathymetric and seismic data, to demonstrate linkage of landscapes and Mesozoic rift-margin structures. At Leknes on Vestvågøya, an erosional remnant of a down-faulted Caledonian thrust nappe (Leknes Group) is preserved in a complex surface depression that extends across the entire Lofoten Ridge. This depression is bounded by opposing asymmetric mountains comprising fault-bounded steep scarps and gently dipping, partly incised low- relief surfaces. Similar features and boundary faults of Palaeozoic–Mesozoic age are present on the offshore margin surrounding the Lofoten Ridge. The offshore margin is underlain by a crystalline, Permo–Triassic to Early Jurassic, peneplained basement surface that was successively truncated by normal faults, down-dropped and variably rotated into asymmetric fault blocks and basins in the Mesozoic, and the basins were subsequently filled by Late Jurassic to Early Cretaceous sedimentary strata. -
Landskapsressursanalyse Pilotturløype Lototen
FORPROSJEKT - PILOTTURLØYPE LOFOTEN ROLVSFJORD-LAUVDALEN-HELLOSAN LANDSKAPSRESSURSANALYSE 1 Forprosjektet “Pilotturløype Lofoten - Rolvsfjord, Lauvdalen, Hellosan”, er gjennomført i perioden august 2014 - februar 2015. Forprosjektet er utført i samarbeid med de tre lokale gårdsbedriftene LofotHest, Aalan gård og Reinmo gård. Norsk landbruksrådgiving Lofoten v/Are Johansen og Lofoten friluftsråd v/Karianne Steen har vært viktige bidragsytere. Prosjektet er blitt til etter initiativ fra Fylkes mannen i Nordland, v/Hanne Sofie Trager. Layout: Kjersti Isdal Kart/foto: Kjersti Isdal (dersom ikke annet er nevnt) Trykk: Forretningstrykk AS, Bodø Lofoten friluftsråd, mars 2015 Kjersti Isdal prosjektleder Forsidebilde: Lauvdalen, sett fra fjellområdet mellom Rolvsfjord, Lauvdalen og Hellosan. Foto: Kjersti Isdal. 2 FORPROSJEKT - PILOTTURLØYPE LOFOTEN ROLVSFJORD-LAUVDALEN-HELLOSAN LANDSKAPSRESSURSANALYSE 3 Innhold Sammendrag 5 Innledning 6 Bakgrunn Organisering Mål Gjennomføring Deltakerklyngen Prosjektområdet Landskapsressursanalyse Landskapsanalyse 12 Landskapsregion Landskapstyper Verdiskapningsgrunnlag 18 Kartlegging av turtrasé Delområde 1: Rolvsfjorden Delområde 2: Hellosan Delområde 3: Lauvdalen Delområde 4: Linken Eiendomsstruktur Videre arbeid 37 Oppfølgingsprosjekt Skilting Tilrettelegging Rasteplasser Produktutvikling Utvidelse av turløype Tilskuddsordninger Litteratur og kilder 4 Tromsø Lofoten Bodø Trondheim Bergen Oslo Lokalisering av pilotturløypeprosjektet i Vestvågøy, Lofoten. Sammendrag Hovedmålet for denne landskapsressursanalysen