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How Uniform Was the Old Norse Religion?
II. Old Norse Myth and Society HOW UNIFORM WAS THE OLD NORSE RELIGION? Stefan Brink ne often gets the impression from handbooks on Old Norse culture and religion that the pagan religion that was supposed to have been in Oexistence all over pre-Christian Scandinavia and Iceland was rather homogeneous. Due to the lack of written sources, it becomes difficult to say whether the ‘religion’ — or rather mythology, eschatology, and cult practice, which medieval sources refer to as forn siðr (‘ancient custom’) — changed over time. For obvious reasons, it is very difficult to identify a ‘pure’ Old Norse religion, uncorroded by Christianity since Scandinavia did not exist in a cultural vacuum.1 What we read in the handbooks is based almost entirely on Snorri Sturluson’s representation and interpretation in his Edda of the pre-Christian religion of Iceland, together with the ambiguous mythical and eschatological world we find represented in the Poetic Edda and in the filtered form Saxo Grammaticus presents in his Gesta Danorum. This stance is more or less presented without reflection in early scholarship, but the bias of the foundation is more readily acknowledged in more recent works.2 In the textual sources we find a considerable pantheon of gods and goddesses — Þórr, Óðinn, Freyr, Baldr, Loki, Njo3rðr, Týr, Heimdallr, Ullr, Bragi, Freyja, Frigg, Gefjon, Iðunn, et cetera — and euhemerized stories of how the gods acted and were characterized as individuals and as a collective. Since the sources are Old Icelandic (Saxo’s work appears to have been built on the same sources) one might assume that this religious world was purely Old 1 See the discussion in Gro Steinsland, Norrøn religion: Myter, riter, samfunn (Oslo: Pax, 2005). -
Using Optimization and Simulation to Evaluate Differentiated Stroke Treatment
Using optimization and simulation to evaluate differentiated stroke treatment Andreas Bergstrøm Aarnseth Erlend Moen Hov Industrial Economics and Technology Management Submission date: June 2018 Supervisor: Henrik Andersson, IØT Norwegian University of Science and Technology Department of Industrial Economics and Technology Management Preface This thesis concludes our Master of Science in Industrial Economics and Technology Manage- ment at the Norwegian University of Science and Technology. The objective of this thesis is to implement a model that enables differentiated treatment paths for stroke patients based on their diagnosis. At the same time, the general demand for emergency resources must be cov- ered. By supplementing existing models and methods, optimization will be used to determine optimal allocation of the available emergency units. A comprehensive simulation program is also developed for this thesis. This is used to evaluate the performance of the different opti- mization solutions. The work on this Master’s Thesis in Managerial Economics and Operations Research (TIØ4905) was carried out in the Spring 2018. We would like to thank the personnel at the Ambulance Service at St. Olav Hospital for providing us with necessary data and valuable inputs. We also would like to thank our supervisor, Professor Henrik Andersson, at the Department of Industrial Economics and Technology Management, for constructive discussions and his in- valuable guidance. Trondheim, 2018-06-10 Andreas Bergstrøm Aarnseth Erlend Moen Hov i Sammendrag En av samfunnets viktigste oppgaver er å tilby et velfungerende helsevesen til sine innbyggere. En stor del av helsevesenet omhandler akuttmedisinske tjenester, et samlebegrep som innbe- fatter blant annet AMK-sentraler, ambulanser og luftambulanser. -
Hr-2001-00004B 365/1999
Judgment of 21 June 2001 serial number 4B/2001: 1. Jon Inge Sirum (et al. a total of 200 parties) (Advocate Ola Brekken) versus 1. Essand Reindeer Pasturing District and 2. Riast/Hylling Reindeer Pasturing District (Advocate Erik Keiserud). Justice Matningsdal: This case concerns a dispute as to whether Essand and Riast/Hylling Reindeer Pasturing Districts have common of pasture for their reindeer in privately owned unenclosed areas within the district boundaries in the Municipal Authority Area of Selbu in the county of Sør-Trøndelag. The areas in dispute The two districts were established by Royal Decree on 10 July 1894 under section 6 of what was called the Joint Lapp Act – the Act of 2 June 1883 concerning the Lapps in the United Kingdoms of Norway and Sweden. The districts have been retained unchanged under subsequent reindeer husbandry legislation. Riast and Hylling were originally separate districts, but for the last fifty or sixty years they have been considered and administered as one district. Essand covers an area of approximately 2,300 km2. In the east the boundary of the district follows the national border with Sweden. The southern boundary starts at the national border at Skardsfjellet [Mount Skard], and goes westwards from there to Lake Stugu in Tydal, where it follows the Rivers Tya and Nea to Lake Selbu, then follows the latter and the Rivers Tømra and Kleivåa over into the county of Nord-Trøndelag to the River Stjørdal, and thereafter follows the latter up through Hegra and Meråker back to the national border. Riast/Hylling covers an area of approximately 1,900 km2 and lies south of Essand. -
Norway Maps.Pdf
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Tectonic Features of an Area N.E. of Hegra, Nord-Trøndelag, and Their Regional Significance — Preliminary Notes by David Roberts
Tectonic Features of an Area N.E. of Hegra, Nord-Trøndelag, and their regional Significance — Preliminary Notes By David Roberts Abstract Following brief notes on the low-grade metasediments occurring in an area near Hegra, 50 km east of Trondheim, the types of structures associated with three episodes of deformation of main Caledonian (Silurian) age are described. An outline of the suggested major stmctural picture is then presented. In this the principal structure is seen as a WNW-directed fold-nappe developed from the inverted western limb of the central Stjørdalen Anticline. A major eastlward closing recumbent syncline underlies this nappe-like structure. These initial structures were then deformed by at least twofur ther folding episodes. In conclusion, comparisons are noted between the ultimate fold pattern, the suggested evolution of these folds and H. Ramberg's experimentally produced orogenic structures. Introduction A survey of this particular area, situated north of the valley of Stjørdalen, east from Trondheim, was begun during the 1965 field-season and progressed during parts of the summers of 1966 and 1967 in conjunction with a mapping programme led by Statsgeolog Fr. Chr. Wolff further east in this same seg ment of the Central Norwegian Caledonides. Further geological mapping is contemplated, the aim being to eventually complete the 1 : 100,000 sheet 'Stjørdal' (rectangle 47 C). In view of the time factor involved in the comple tion of this work, and the renewed interest being devoted to the geological problems of the Trondheim region (Peacey 1964, Oftedahl 1964, Wolff 1964 and 1967, Torske 1965, Siedlecka 1967, Ramberg 1967), some notes on the tectonics of the Hegra area would seem appropriate at this stage. -
Huseiernes Bankundersøkelse 2020
Huseiernes bankundersøkelse 2020 Hvordan er konkurransebildet i det norske bankmarkedet, og hvem kan få lån hvor? Huseiernes Boligfakta Nr 2-2020 Versjon 1, 30.november 2020 Kontaktperson: Kristin Gyldenskog Banker som har kommentarer eller endringer til oversikten kan ta kontakt på [email protected] Forsidefoto: Samuel Han (fra Unsplash) 2 Innledning Den aller største bokostnaden for nordmenn er rentekostnaden. Huseierne er opptatt av at norske boligeiere skal ha så lave rente- og bokostnader som mulig. Derfor er det viktig med størst mulig konkurranse i bankmarkedet. På landsbasis er rentekostnadene i 2019 for en gjennomsnittsbolig på 120 kvadratmeter 47.280 kroner, mens totale bokostnader er på 116.392 kroner. Det betyr at rentekostnadene utgjorde 41 prosent av boligeiernes samlede bokostnader. Dette viser Huseiernes bokostnadsindeks for 2020. For å få ned rentekostnadene er det viktig at konkurransen i bankmarkedet er størst mulig, men det norske bankmarkedet er uoversiktlig for forbrukerne. Det tradisjonelle mønsteret med landsdekkende, regionale og lokale banker brytes nå opp med digital tilgang til banktjenester. Samtidig er det fortsatt flere banker som bare gir lån i sine lokalområder. Derfor er det svært vanskelig for bankkunder i ulike kommuner å finne ut hvilke banker de faktisk kan bli kunde og få lån i. Huseierne har derfor gått gjennom alle norske banker som tilbyr boliglån til forbrukere, for å kartlegge hvilke banker som gir lån i hvilke kommuner. Målet er å vise konkurransebildet for forbrukerne i de ulike delene av landet, og fortelle forbrukerne i ulike kommuner hvilke banker de faktisk kan få lån i. Undersøkelsen er foretatt i oktober og november 2020. -
Administrative and Statistical Areas English Version – SOSI Standard 4.0
Administrative and statistical areas English version – SOSI standard 4.0 Administrative and statistical areas Norwegian Mapping Authority [email protected] Norwegian Mapping Authority June 2009 Page 1 of 191 Administrative and statistical areas English version – SOSI standard 4.0 1 Applications schema ......................................................................................................................7 1.1 Administrative units subclassification ....................................................................................7 1.1 Description ...................................................................................................................... 14 1.1.1 CityDistrict ................................................................................................................ 14 1.1.2 CityDistrictBoundary ................................................................................................ 14 1.1.3 SubArea ................................................................................................................... 14 1.1.4 BasicDistrictUnit ....................................................................................................... 15 1.1.5 SchoolDistrict ........................................................................................................... 16 1.1.6 <<DataType>> SchoolDistrictId ............................................................................... 17 1.1.7 SchoolDistrictBoundary ........................................................................................... -
Skredhendelser I Trøndelag Og På Nord-Møre Mars/April 2012
Skredhendelser i Trøndelag og på Nord-Møre mars/april 2012 NVEs håndtering av hendelsene og geografisk fordeling av skredene 68 2013 RAPPORT Skredhendelser i Trøndelag og på Nord‐Møre mars‐april 2012 NVEs håndtering av hendelsene og geografisk fordeling av skredene Norges vassdrags‐ og energidirektorat 2013 Rapport nr. 68 – 2013 Skredhendelser i Trøndelag og på Nord‐Møre mars‐april 2012 NVEs håndtering av hendelsene og geografisk fordeling av skredene Utgitt av: Norges vassdrags‐ og energidirektorat Forfattere: Terje H. Bargel og Yngvild Solberg Kvalvik Trykk: NVEs hustrykkeri Opplag: 50 Forsidefoto: Grunn utglidning i leire i avskoget boligfelt (”hageutglidning”). Gammellina, Selsbakk, Trondheim. Foto: Terje H. Bargel ISSN: 1501-2832 ISBN: 978‐82‐410‐0938‐9 Sammendrag: Langvarig høy temperatur, intens nedbør og snøsmelting i Trøndelag og de nordøstlige deler av Møre og Romsdal i mars 2012 forårsaket mange jordskred. Særlig områdene omkring sørøstlige del av Trondheimsfjorden ble rammet. Emneord: Grunne leirskred, jordskred, erosjon, nedbør, snøsmelting, tele, Møre og Romsdal, Trøndelagsfylkene. Norges vassdrags‐ og energidirektorat Postboks 5091 Majorstua 0301 OSLO Telefon: 09575 Telefaks: 22 95 90 00 Internett: www.nve.no Mai 2013 2 INNHOLD Forord.............................................................................................................................. 4 Sammendrag................................................................................................................... 5 1 Skredhendelser i Trøndelag og Nord‐Møre -
Studies in the Trondheim Region, Central Norwegian Caledonides II
NORGES GEOLOGISKE UNDERSØKELSE Studies in the Trondheim Region, Central Norwegian Caledonides II Published by FR. CHR. WOLFF et al. UNIVERSITETSFORLAGET TRONDHEIM 1967 WATHS TERHLKISXE IflSTrøT? BIBLIOTEKET CONTENTS I. GEOLOGY OF THE MERÅKER AREA. Fr, Chr. Wolff: Introduction 5 Aim of study 5 Location of the area investigated 5 Planning and organization of the work 5 Geological setting 7 Previous investigations 7 Acknowledgements 8 /. Chaloupsky and F. Fediuk: Geology of the western and north eastern part of the Meråker area 9 Abstract 9 Introduction 9 Lithological descriptions 10 Notes on stratigraphy. tectonics and metamorphism 17 Sammendrag 21 A. Siedlecka: Geology of the eastern part of the Meråker area 22 Abstract 22 Introduction 22 Acknowledgements 23 Rock characteristics 23 Metagraywacke-slate association 23 Structural and textural features 24 Petrology 30 Metaconglomerates 38 Black-grey metasiltstone-slate association 39 Gabbro-diorite intrusions 41 Development of sediments 43 Stratigraphy 46 Remarks concerning the structural geology 49 Metamorphism 53 Conclusions 52 Sammendrag 53 References 55 Table 58 A. Siedlecka and S. Siedlecki: Geology of the northernmost part of the Meråker area 59 Abstract 59 Introduction 59 Acknowledgements 60 Stratigraphy and lithology 60 Fundsjø Group 60 Sulåmo Group 60 Kjølhaugene Group 62 Slågån Group 62 Remarks concerning the structural geology 63 Sammendrag 63 D. Roberts: Structural observations from the Kopperå - Riksgrense area and discussion of the tectonics of Stjørdalen and the N.E. Trondheim region . 64 Abstract 64 A. The Kopperå - Riksgrense area 65 Introduction 65 The early minor folds and related struetures 66 The Teveldal syncline 73 The later folds 76 Joints 80 Thrusting 82 Mineralogical notes 85 Summary and structural relationships 87 B. -
Homogenization of Norwegian Monthly Precipitation Series for the Period 1961-2018
No. 4/2021 ISSN 2387-4201 METreport Climate Homogenization of Norwegian monthly precipitation series for the period 1961-2018 Elinah Khasandi Kuya, Herdis Motrøen Gjelten, Ole Einar Tveito METreport Title Date Homogenization of Norwegian monthly 2021-04-30 precipitation series for the period 1961-2018 Section Report no. Division for Climate Services No. 4/2021 Author(s) Classification Elinah Khasandi Kuya, Herdis Motrøen Gjelten, ● Free ○ Restricted Ole Einar Tveito Abstract Climatol homogenization method was applied to detect inhomogeneities in Norwegian precipitation series, during the period 1961-2018. 370 series (including 44 from Sweden and one from Finland) of monthly precipitation sums, from the ClimNorm precipitation dataset were used in the analysis. The homogeneity analysis produced a 58-year long homogenous dataset for 325 monthly precipitation sum with regional temporal variability and spatial coherence that is better than that of non-homogenized series. The dataset is more reliable in explaining the large-scale climate variations and was used to calculate the new climate normals in Norway. Keywords Homogenization, climate normals, precipitation Disciplinary signature Responsible signature 2 Abstract Climate normals play an important role in weather and climate studies and therefore require high-quality dataset that is both consistent and homogenous. The Norwegian observation network has changed considerably during the last 20-30 years, introducing non-climatic changes such as automation and relocation. Homogenization was therefore necessary and work has been done to establish a homogeneous precipitation reference dataset for the purpose of calculating the new climatological standard normals for the period 1991-2020. The homogenization tool Climatol was applied to detect inhomogeneities in the Norwegian precipitation series for the period 1961-2018. -
Inflation Report 2/2004 Norges Bank’S Inflation Report
Reports from the Central Bank of Norway No 3/2004 11 Inflation report 2 with monetary policy assessments 04 J u l y Inflation report 2/2004 Norges Bank’s Inflation Report Norges Bank’s Inflation Report is published three times a year, in February/March, June/July and October/November.Sections 1-4 of the report contain an analysis of developments in inflation, output and demand 3 years ahead. As from Inflation Report 2/04, the Executive Board’s monetary policy strategy and interest rate setting will be published in Section 5 of the Inflation Report. 2 The Inflation Report is published three times a year, and together with Financial Stability, is part of Norges Bank’s series of reports. The report is also available on Norges Bank’s website: http://www.norges-bank.no. The series of reports is included in the subscription for Economic Bulletin. To subscribe please write to: Norges Bank Subscription Service PO Box 1179 Sentrum N-0107 Oslo Norway Telephone: +47 22 31 63 83 Fax: + 47 22 41 31 05 E-mail: [email protected] Editor: Svein Gjedrem (Section 5 presents the Executive Board's assessments) Design: Grid Strategisk Design AS Setting and printing: Reclamo grafisk senter AS The text is set in 111⁄2 point Times ISSN 0807-8521 Inflation report 2/2004 Monetary policy in Norway Objective The Government has defined an inflation target for monetary policy in Norway. Norges Bank’s operational conduct of monetary policy shall be oriented towards low and stable inflation. The operational target of monetary policy shall be annual consumer price inflation of approximately 2.5 per cent over time. -
Stortingsvalget 1927
NORGES OFFISIELLE STATISTIKK. VIII. 69 STORTINGSVALGET 1927. (Élections en 1927 pour le «Storting».) UTGITT AV STORTINGETS KONTOR. OSLO. I KOMMISJON HOS H. ASCHEHOUG & CO. 1928. OSLO - O. FREDR. ARNESENS BOK- OG AKCIDENSTRYKKERI - 1928. Forord. Nærværende statistikk er utarbeidet efter samme system som de efter valgene i 1921 og 1924 utkomne. Første del, som inneholder de almindelig^ statistiske Oplysninger (tab. 1—4, s. 1—30), er utarbeidet av fullmektig i Stortinget P. A. "W e s s e 1 - B e r g på grunnlag av de fra valg- styrenes formenn innsendte skjematiske opgaver. Disse har som før i stor utstrekning måttet sammenholdes med og suppleres ved hjelp av de til Stortingets kontor innsendte valgdokumenter. Annen del inneholder den politiske fordeling av stemmene. Fordelingen er skjedd på grunnlag av de på hvert enkelt parti falne listestemmer under sammenhold med de øvrige valgdokumenter og innsendte opgaver. Utregningen, som omfatter s. 31—112, er foretatt av sekretær ved Stortingets kontor K. Bjørn stad. — De siste sider (tab. 5—6, s. 113—126) er utarbeidet av arkivar i Stortinget V. H af f ner. Oslo i juli 1928. P. Å. Wessel-Berg. Karl Bjørnstad. Valgdistrikter, valgsogn m. v. Siden 7de oktober 1924 til og med 7de oktober 1927 er foretatt følgende herreds- delinger og endringer av herreds- og bynavn m. v. 1. Tolga herred er fra Iste juli 1926 delt i Tolga og Os herreder. 2. Alversund herred er fra 15de oktober 1924 delt i Alversund og Mæland herreder. 3. Røros herred er fra Iste juli 1926 delt i Røros, Røros landsogn, Glaamos og Brækken herreder, 4.