Overview of Norway's Follow-Up of the Report On
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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. -
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). -
Statnett Semi-Annual Report 2016
Half year report 2016 1. half year report 2016 1 Statnett - 1. half year report 2016 Table of contents 05 Director’s report 15 Statement of comprehensive income 16 Balance sheet 17 Statement of changes in equity 18 Cash flow statement 19 Selected notes 2 Statnett - 1. half year report 2016 In short Statnett is the transmission system operator in the Norwegian power system, and is responsible for socio-economically efficient operations and development of the central transmission grid for power. Statnett’s social mission is to ensure a reliable supply of electricity, contribute to value creation in society and pave the way for better environmental solutions. The power situation in Norway has been good during the first six months of 2016. A good hydrological balance at the beginning of the period meant that reservoir water levels at the end of the first six months were above the median. The operating situation has been satisfactory during the period. Statnett’s suppliers had two fatal accidents in connection with work on Statnett’s projects. This is not acceptable for Statnett, and the organisation have been marked by the development of an action plan in the second quarter. The Statnett Group’s underlying profit after tax amounted to NOK 696 million in the first six months of 2016 (NOK 823 million in the corresponding period in 2015). The reduction in underlying profit is mainly due to lower pension costs first half of 2015 as a result of a non-recurring effect caused by the transition from defined benefit to a defined contribution pension scheme, somewhat offset by higher permitted revenue in 2016, primarily as a result of an increased asset base in the Group. -
Framtidig Ledelse Ved Ofoten Tingrett Og Trondenes Tingrett
Saksframlegg – styret i DA Saksbehandler: Jon Bottheim Arkiv: Arkivsaksnr.: 19/1183 - 1 Framtidig ledelse ved Ofoten tingrett og Trondenes tingrett Vedlegg: Vedlegg 1 - Uttalelse fra sorenskriver i Ofoten tingrett Vedlegg 2 - Uttalelse fra advokatene i Narvik Vedlegg 3 - Uttalelse fra kommuneadvokaten i Narvik Vedlegg 4 - Uttalelse fra sorenskriver i Trondenes tingrett Direktørens sakssammendrag: Domstoladministrasjonen (DA) har gjort en vurdering av om det skal etableres felles ledelse mellom Ofoten tingrett og Trondenes tingrett som følge av at sorenskriveren ved Ofoten tingrett har søkt om avskjed og fratrer sitt embete fra 1. desember 2019. Etter en helhetsvurdering, foreslår direktøren at det etableres fast felles ledelse for Ofoten tingrett og Trondenes tingrett. Referanse til tidligere styresaker Sak 15/011 – Felles dommerstillinger (styremøte 23.02.2015) Sak 15/028 – Felles dommerstillinger – felles ledelse (styremøte 20.04.2015) Sak 15/049 – Domstolloven § 33c – felles dommerstillinger – felles ledelse (styremøte 28.09.2015) Sak 15/069 – Budsjett og budsjettiltak 2016 (styremøte 09.11.2015) Sak 16/037 – Orientering, eventuell felles ledelse i Brønnøy tingrett (styremøte 11.04.2016) Sak 16/091 – Felles ledelse av domstoler (styremøte 12.12.2016) Sak 17/005 – Felles ledelse, omgjøring til permanent felles ledelse for tingrettene på Helgeland og i Gudbrandsdal (styremøte 13.02.2017) Sak 17/032 – Felles ledelse for Lofoten tingrett og Salten tingrett (styremøte 12. – 13.06.2017) Sak 17/038 – Felles ledelse, omgjøring til fast felles ledelse for enkelte jordskifteretter (styremøte 12. – 13.06.2017) Sak 17/050 – Felles ledelse for Lofoten tingrett og Salten tingrett (styremøte 29.06.2017) Sak 18/014 – Styreleder orienterer – felles dommerembeter (styremøte 26.02.2018) Sak 18/057 – Framtidig ledelse ved Halden tingrett (styremøte 11. -
Individ Kjønn Kommune Kommentarer Fjellområde 2002 2003 2004 2005 2006 2007 2008 2009 2010 Ind1086 Hann Hattfjelldal Olfjellet, D020383
Individ Kjønn Kommune Kommentarer Fjellområde 2002 2003 2004 2005 2006 2007 2008 2009 2010 Ind1086 Hann Hattfjelldal Olfjellet, D020383. Voksen hann.Helgeland Merket som indre valp i Sør-Norge i 2003. X Ind568 Hann Lierne, Fauske, Saltdal,Almdalen (06), Furuhaugen, StorforsdalenBalvatn vest X X Ind1051 Tispe Rana Kjerringfjellet (07), Dourra (05) Rana øst X X Ind1100 Tispe Gällevare, Fauske Stora Sjøfallet (-06), Sorjus/SvarthammarenBalvatn nord X X X Ind1105 Tispe Hattfjelldal Moskefjellet (Vågvassfjell) Helgeland indre X Ind1115 Hann Narvik, Kiruna Gautelis, Torneträsk Ofoten indre - Sverige X X X Ind2001 Tispe Sørfold, Hamarøy, TysfjordLinàjaure, Rounasvagge, HellemobotnNord-Salten indre X X X Ind2002 Tispe Saltdal Balvatnet vest (08), Argalad (07) Balvatn X X Ind2003 Hann Tysfjord Amasjaure, Rounasvagge Nord-Salten indre X Ind2004 Tispe Sørfold Trolig yngletispa i Løyta - 08 Nord-Salten indre X X Ind2005 Tispe Saltdal Dypendal Saltfjellet øst X Ind2006† Hann Fauske, Jokkmokk, Sørfold509 km2. 8 år gammel. Grytvikmoen,Nord-Salten Løyta, Sorjus indre -(Sverige) Sverige X X † Ind2007 Hann Fauske, Saltdal Navnlausdalen, Sulis øst Balvatn X X X X Ind2008† Hann Meløy, Gildeskål Oterstranda (-07), SundsfjordfjelletSaltfjellet (4 prøver vest 21.01.08) X † Ind2009 Tispe Meløy Lysvatnet, Stor-Glomvatnet, Saltfjellet vest X X Ind2010 Hann Meløy Stor-Glomvatnet Saltfjellet vest X Ind2011† Hann Saltdal Storengskardet og Argaladdalen Balvatni -07. Skutt i Solvågtindsområdet 19. januar 2008 X † Ind2012 Hann Beiarn, Rana, Meløy Vegdalen, Burfjellet, -
Norway 4Th Periodical Report
Strasbourg, 1 July 2008 MIN-LANG/PR (2008) 6 EUROPEAN CHARTER FOR REGIONAL OR MINORITY LANGUAGES Fourth periodical report presented to the Secretary General of the Council of Europe in accordance with Article 15 of the Charter NORWAY Error! Unknown document Error! Unknown Error! Unknown document property name. document property name. property name. 2006/2972 KU/KU2 ckn 18 June 2008 European Charter for Regional or Minority Language Fourth periodical report Norway June 2008 Contents Preliminary section 1. Introductory remarks 2. Constitutional and administrative structure 3. Economy 4. Demography 5. The Sámi language 6. The Kven language 7. Romanes 8. Romany 2 Part I 1. Implementation provisions 2. Bodies or organisations working for the protection and development of regional or minority language 3. Preparation of the fourth report 4. Measures to disseminate information about the rights and duties deriving from the implementation of the Charter in Norwegian legislation 5. Measures to implement the recommendations of the Committee of Ministers Part II 1. Article 7 Objects and principles 2. Article 7 paragraph 1 sub-paragraphs f, g, h 3. Article 7 paragraph 3 4. Article 7 paragraph 4 Part III 1. Article 8 Educations 2. Article 9 Judicial authorities 3. Article 9 paragraph 3 Translation 4. Article 10 Administrative authorities and public service 5. Article 10 paragraph 5 6. Article 11 Media o Article 11 paragraph 1 sub-paragraph a o Article 11 paragraph 1 sub-paragraph b o Article 11 paragraph 1 sub-paragraph c o Article 11 paragraph 1 sub-paragraph e o Article 11 paragraph 1 sub-paragraph f o Article 11 paragraph 1 sub-paragraph g o Article 11 paragraph 2 7. -
BEVARINGSPLAN for PRIVATARKIV I Nordland Fylke
BEVARINGSPLAN FOR PRIVATARKIV i Nordland Fylke Foto fra arkivet etter Bodø Formannskap, Arkiv i Nordland Innholdsfortegnelse INNLEDNING ......................................................................................................... 4 Prosjektbeskrivelse ................................................................................... 5 Metode ............................................................................................................... 6 Bevarings- og innsamlingspolitikk ................................................... 6 Oppsett av bevaringsplanen ................................................................ 7 KAPITTEL 1: Bestandsanalyse av privatarkiv fra Nordland fylke ..... 8 Institusjonene .............................................................................................. 8 Arkiv i Nordland (AiN) ............................................................................... 8 Helgeland museum ..................................................................................... 8 Nordlandsmuseet ........................................................................................ 8 Museum Nord................................................................................................ 9 Norsk Luftfartsmuseum ............................................................................ 9 Statsarkivet i Tromsø ................................................................................ 9 Statsarkivet i Trondheim ......................................................................... -
Kunnskap for Et Bærekraftig Nordland Et Utdrag Av Kunnskapsgrunnlaget for Den Regionale Planstrategien 1 4 Arealbruk Og Arealressurser (Km²), 2011 Og 2020
Kunnskap for et bærekraftig Nordland Et utdrag av kunnskapsgrunnlaget for den regionale planstrategien 1 4 Arealbruk og arealressurser (km²), 2011 og 2020. Brutto driftsutgifter til samferdsel per innbygger (kr). 2011 2020 15 000 Boligbebyggelse 74,65 74,38 Finnmark fylkeskommune Finnmárkku fylkagielda Fritidsbebyggelse 26,74 30,36 Kunnskap for et 12 000 Troms fylkeskommune Romsa fylkagielda Bebygd område for landbruk og fiske 29,67 28,45 Næring, offentlig og privat tjenesteyting 33,54 31,84 Nordland fylkeskommune 9 000 bærekraftig Nordland Undervisning og barnehage 3,41 3,03 Møre og Romsdal fylkeskommune Helse- og sosialinstitusjoner 1,40 1,40 6 000 Kultur og religiøse aktiviteter 2,02 1,89 Sogn og Fjordane fylkeskommuneKunnskapsgrunnlaget som er utarbeidet for den regionale planstrategien Transport, telekom. og teknisk infrastruktur 164,17 168,04 3 000 2020-2024 skal bidra til å skape et felles fundament for fylkets utfordringer Beredskapstjenester og Forsvaret 3,03 1,75 Grønne områder, idretts- og sportsområder 10,18 13,30 og muligheter. 0 Uklassifisert bebyggelse og anlegg 9,92 14,44 2015 2017 2019 Jordbruksareal 727,20 753,41 Sogn og Fjordane fylkeskommune Møre og Romsdal fylkeskommune ette dokumentet er en kortutgave av kunnskaps- Et viktig element i regional utvikling er å avdekke og vide- Skog 10789,84 10813,98 Nordland fylkeskommune Troms fylkeskommune Romsa fylkagielda grunnlaget, og fører videre inndelingen etter FNs reutvikle områder som gjerne er stedsavhengig og som gir Åpen fastmark 17035,00 16762,47 Finnmark fylkeskommune Finnmárkku fylkagielda bærekraftsmål. Utviklingstrender i fylket knyttes opp regionale fortrinn. EU og OECD anbefaler den strategiske Våtmark 1392,56 1439,80 Dmot fylkeskommunens rolle som samfunnsutvikler. -
MESTO DEJINY Narvik, a Swedish Norwegian Border Town
MESTO a DEJINY Narvik, a Swedish Norwegian Border Town Steinar Aas vol. 8, 2019, 1, pp. 54-79 DOI: https://doi.org/10.33542/MAD2019-1-03 This article gives an insight into the industrialization and colonization processes of northern Scandinavia. Urbanization due to industrialization is a vital part of the perspective, and brings us into an industrial mega system in Swedish Lapland in the late nineteenth century based on iron ore export. It was to be connected to the industrial centre of Europe, especially the Ruhrgebiet of Germany, and paved the way for a new kind of urban development in peripheral Europe – the industrial network town. The history and foundation of the Norwegian harbour town Narvik is vital for gaining insight into this mega system. By studying Narvik we can envisage particularities of, and similarities and diff erences between Norway and Sweden when it comes to their urban economic foundations, urban development/planning regimes, and the relations between the municipalities, the modern nation states and the dominating companies. Even the development of a uniquely Scandinavian identity connected with the labour movement and the development of a post-war social democrat order visibly results from the new industries. Thus the common Swedish-Norwegian fi gure of the rallar – something like navvy or construction worker – has a signifi cant place in this study, and the use of the fi gure in addition to later processes of memory creation, both within the Norwegian and Swedish labour movements, is addressed. Keywords: Urban History. Modernization. Industrialization. Norwegian History. Swedish History. Technology. Urban Planning. Memory Studies. -
SARSIA Spring Spawning Herring When Entering the Cold Front in the Norwegian Sea
MIGRATION BEHAVIOUR OF NORWEGIAN SPRING SPAWNING HERRING WHEN ENTERING THE COLD FRONT IN THE NORWEGIAN SEA OLE ARVE MISUND, WEBJØRN MELLE & ANDERS FERNÖ MISUND, OLE A RVE, WEBJØRN MELLE & ANDERS FERNÖ 1997 08 15. Migration behaviour of Norwegian SARSIA spring spawning herring when entering the cold front in the Norwegian Sea. – Sarsia 82:107- 112. Bergen. ISSN 0036-4827. The distribution of Norwegian spring spawning herring when migrating to the feeding areas in the Norwegian Sea in spring was mapped by acoustic surveys in April 1995 and 1996. The schooling behaviour of the herring was recorded by a high-resolution sonar, and the swimming speed and swimming direction were quantified by tracking individual schools for up to one hour. In early April the herring migrated in the Norwegian Sea from the continental shelf off Norway, between 66° and 68°N, and westward to 2°W. When reaching the cold-water front, at about 0°, the herring turned southward along the front. During daytime the herring migrated in large schools at 300-400 m depth; at night they rose to surface and either dispersed or maintained schooling. Ole Arve Misund & Webjørn Melle, Institute of Marine Research, P.O. Box 1870 Nordnes, N- 5024 Bergen, Norway – Anders Fernö, University of Bergen, Department of Fisheries and Marine Biology, Bergen High-Technology Center, N-5020 Bergen, Norway KEYWORDS: Herring; migration; behaviour; schools; Norwegian Sea. INTRODUCTION schools and bottom layers in daytime, and scattered in extended layers at night (DEVOLD 1963). In early sum- The large-scale migration behaviour of the herring, mer the herring were found in dense schools near the Clupea harengus, in the Norwegian Sea during its sum- surface or in mid-water at depths up to 300 m mer feeding migrations, autumn aggregation migrations, (JAKOBSSON 1963; ØSTVEDT 1965). -
Rettsbok for Ofoten Jordskifterett
Rettsbok for Ofoten jordskifterett Den 31. mai 2002 ble jordskifterett holdt på Posthusloftet i Ballangen. Jordskiftedommer Per A. Normann er enedommer. I henhold til jordskiftelovens § 9, 2. ledd settes jordskifteretten uten meddommere. Sak nr. 7/1999 – Grunnvatnet naturreservat. Rekvirent: 1. Fylkesmannen i Nordland, miljøvernavdelingen, Moloveien 10, 8002 Bodø. Motparter: 2. Eier av gnr. 41/1, Ingeborg Sofie Bruksås, 8540 BALLANGEN 3. Eier av gnr. 41/2, 41/3, 42/2Hans Anton Arntsen, 8540 BALLANGEN 5. Eier av gnr. 42/5, Henry Kjell Arntsen, ukjent 6. Eier av gnr. 46/1, 46/17, Karl Johan Birger Johansen, Djupås, 8540 BALLANGEN 7. Eier av gnr. 46/2, 46/9, Atle Per Johan Larsen, Dypås, 8540 BALLANGEN 8. Eier av gnr. 46/3, 46/30, Ole Jørgen Iversen, Lomv 54, 8516 NARVIK 9. Eier av gnr. 46/3, 46/30, Laila Lill Weber, Paal Bergs V 44, 1348 RYKKINN 10.Eier av gnr. 46/3, 46/30, Karl Johan Iversen, Beverv 10, 8515 NARVIK 11.Eier av gnr. 46/3, 46/30, Margith Iversen, Olav Magnussons Veg 3, 7046 Trondheim 12.Eier av gnr. 46/3, 46/30, Inger Hjørdis Rag Sjåfjell, Ekornv 33, 8515 NARVIK 13.Eier av gnr. 46/4, 46/11, Jacob Martin Pettersen, 8540 BALLANGEN 14.Eier av gnr. 46/5, Tor Emil Pedersen, Lysakervegen 6, 9014 TROMSØ 15.Eier av gnr. 46/6, 46/12, Arild Oluf Johan Olsen, 8540 BALLANGEN 16.Eier av gnr. 46/7, 50/2, Oddveig Alise Ramstad, 8540 BALLANGEN 17.Eier av gnr. 46/7, 50/2, Kolbjørn Astor Ramstad, Langrennsv 16, 8515 NARVIK 18.Eier av gnr.