Organisasjon Tiltak Beløp Kommune
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The Permo-Carboniferous Oslo Rift Through Six Stages and 65 Million Years
52 by Bjørn T. Larsen1, Snorre Olaussen2, Bjørn Sundvoll3, and Michel Heeremans4 The Permo-Carboniferous Oslo Rift through six stages and 65 million years 1 Det Norske Oljeselskp ASA, Norway. E-mail: [email protected] 2 Eni Norge AS. E-mail: [email protected] 3 NHM, UiO. E-mail: [email protected] 4 Inst. for Geofag, UiO. E-mail: [email protected] The Oslo Rift is the northernmost part of the Rotliegen- des basin system in Europe. The rift was formed by lithospheric stretching north of the Tornquist fault sys- tem and is related tectonically and in time to the last phase of the Variscan orogeny. The main graben form- ing period in the Oslo Region began in Late Carbonif- erous, culminating some 20–30 Ma later with extensive volcanism and rifting, and later with uplift and emplacement of major batholiths. It ended with a final termination of intrusions in the Early Triassic, some 65 Ma after the tectonic and magmatic onset. We divide the geological development of the rift into six stages. Sediments, even with marine incursions occur exclusively during the forerunner to rifting. The mag- matic products in the Oslo Rift vary in composition and are unevenly distributed through the six stages along the length of the structure. Introduction The Oslo Palaeorift (Figure 1) contributed to the onset of a pro- longed period of extensional faulting and volcanism in NW Europe, which lasted throughout the Late Palaeozoic and the Mesozoic eras. Widespread rifting and magmatism developed north of the foreland of the Variscan Orogen during the latest Carboniferous and contin- ued in some of the areas, like the Oslo Rift, all through the Permian period. -
What's Inside
TAKE ONE! June 2014 Paving the path to heritage WHAT’S INSIDE President’s message . 2 SHA memorials, membership form . 10-11 Picture this: Midsummer Night . 3 Quiz on Scandinavia . 12 Heritage House: New path, new ramp . 4-5 Scandinavian Society reports . 13-15 SHA holds annual banquet . 6-7 Tracing Scandinavian roots . 16 Sutton Hoo: England’s Scandinavian connection . 8-9 Page 2 • June 2014 • SCANDINAVIAN HERITAGE NEWS President’s MESSAGE Scandinavian Heritage News Vol. 27, Issue 67 • June 2014 Join us for Midsummer Night Published quarterly by The Scandinavian Heritage Assn . by Gail Peterson, president man. Thanks to 1020 South Broadway Scandinavian Heritage Association them, also. So far 701/852-9161 • P.O. Box 862 we have had sev - Minot, ND 58702 big thank you to Liz Gjellstad and eral tours for e-mail: [email protected] ADoris Slaaten for co-chairing the school students. Website: scandinavianheritage.org annual banquet again. Others on the Newsletter Committee committee were Lois Matson, Ade - Midsummer Gail Peterson laide Johnson, Marion Anderson and Night just ahead Lois Matson, Chair Eva Goodman. (See pages 6 and 7.) Our next big event will be the Mid - Al Larson, Carroll Erickson The entertainment for the evening summer Night celebration the evening Jo Ann Winistorfer, Editor consisted of cello performances by Dr. of Friday, June 20, 2014. It is open to 701/487-3312 Erik Anderson (MSU Professor of the public. All of the Nordic country [email protected] Music) and Abbie Naze (student at flags will be flying all over the park. Al Larson, Publisher – 701/852-5552 MSU). -
THE LION FLAG Norway's First National Flag Jan Henrik Munksgaard
THE LION FLAG Norway’s First National Flag Jan Henrik Munksgaard On 27 February 1814, the Norwegian Regent Christian Frederik made a proclamation concerning the Norwegian flag, stating: The Norwegian flag shall henceforth be red, with a white cross dividing the flag into quarters. The national coat of arms, the Norwegian lion with the yellow halberd, shall be placed in the upper hoist corner. All naval and merchant vessels shall fly this flag. This was Norway’s first national flag. What was the background for this proclamation? Why should Norway have a new flag in 1814, and what are the reasons for the design and colours of this flag? The Dannebrog Was the Flag of Denmark-Norway For several hundred years, Denmark-Norway had been in a legislative union. Denmark was the leading party in this union, and Copenhagen was the administrative centre of the double monarchy. The Dannebrog had been the common flag of the whole realm since the beginning of the 16th century. The red flag with a white cross was known all over Europe, and in every shipping town the citizens were familiar with this symbol of Denmark-Norway. Two variants of The Dannebrog existed: a swallow-tailed flag, which was the king’s flag or state flag flown on government vessels and buildings, and a rectangular flag for private use on ordinary merchant ships or on private flagpoles. In addition, a number of special flags based on the Dannebrog existed. The flag was as frequently used and just as popular in Norway as in Denmark. The Napoleonic Wars Result in Political Changes in Scandinavia At the beginning of 1813, few Norwegians could imagine dissolution of the union with Denmark. -
Delprosjekt Eidsvoll
Norges vassdrags- og energidirektorat Telefon: 22 95 95 95 Middelthunsgate 29 Telefaks: 22 95 90 00 Postboks 5091 Majorstua Internett: www.nve.no 0301 Oslo Flomsonekart Delprosjekt Eidsvoll Ahmed Reza Naserzadeh Julio Pereira 2 2007 FLOMSONEKART Flomsonekart nr 2/2007 Delprosjekt Eidsvoll Utgitt av: Norges vassdrags- og energidirektorat Forfattere: Ahmed Reza Naserzadeh Julio Pereira Trykk: NVEs hustrykkeri Opplag: 100 Forsidefoto: Sundet, vårflommen 10.06.1995 ©FOTONOR ISSN: 1504-5161 Emneord: Flomsone, flom, flomanalyse, flomareal, flomberegning, vannlinjeberegning, Vorma, Mjøsa, Eidsvoll kommune Norges vassdrags- og energidirektorat Middelthuns gate 29 Postboks 5091 Majorstua 0301 OSLO Telefon: 22 95 95 95 Telefaks: 22 95 90 00 Internett: www.nve.no Januar 2007 Sammendrag Rapporten inneholder detaljer rundt flomsonekartlegging av Vorma, fra Steinerud til Minnesund, en strekning på totalt ca 11 km. Området ligger i Eidsvoll kommune i Akershus. Grunnlaget for flomsonekartene er flomfrekvensanalyse og vannlinjeberegninger. Digitale flomsoner for 10-, 100-, 200-, og 500-årsflom dekker hele den kartlagte strekningen. I tillegg er det gitt vannstander for 20-, og 50-årsflom. Det er produsert flomsonekart for et område ved Minnesund og ved Sundet. Flomsonekart for 200-årsflommen samt flomdybdekart for 200-årsflommen ved Sundet er vedlagt rapporten. For at de beregnede flommene skal være mest mulig representative for fremtiden, er det valgt å betrakte perioden etter 1961, dvs. perioden etter de viktigste reguleringene fant sted. Det er derfor ikke tatt hensyn til flommer før 1961. Det er vårflommene som er de største både i Mjøsa og i Vorma. De fleste opptrer fra slutten av mai til midten av juli. Flom i Vorma innebærer en langsom vannstandsstigning på grunn av Mjøsa. -
Edu Immigration ACCEPTED.Pdf (882.2Kb)
ARTICLE Does education affect immigration attitudes? Evidence from an education reform / Henning Finseraas, Øyvind Søraas Skorge, Marte Strøm VERSION: POST PRINT/GREEN OPEN ACCESS This document is the author’s post print (final accepted version). The document is archived in the institutional archive of Institute for Social Research. The final publication is available in: Electoral Studies 2018, / DOI: 10.1016/j.electstud.2018.06.009 does education affect immigration attitudes? Evidence from an education reform∗ Henning Finseraas,y Øyvind Skorge,z and Marte Strømx Accepted for publication in Electoral Studies July 2, 2018 Abstract Empirical research consistently finds that people with high education have more liberal immigration attitudes. To what extent this relationship reflects a causal effect of education is, however, largely unknown. We rely on the staggered introduction of a major Norwegian education reform to get exogenous variation in respondents’ level of education. The reform lifted the bottom of the education distribution by increasing the compulsory years of education by two years. We find no significant differences in immigration attitudes between those who were educated in the old and the new education system. Our results suggest that if education has a causal effect on immigration attitudes, it is likely to operate on other education margins. ∗We would like to thank seminar participants at the Institute for Social Research, Frisch Center for Economic Research, and University of Bergen for comments on a previous draft of the paper. Funding from the Research Council of Norway is acknowledged (grant no. 270687). yInstitute for Social Research, Oslo, P.O. Box 3233 Elisenberg, 0208 Oslo, Norway. -
Agenda 2030 in Asker
Agenda 2030 in Asker Voluntary local review 2021 Content Opening Statement by mayor Lene Conradi ....................................4 Highlights........................................................................................5 Introduction ....................................................................................6 Methodology and process for implementing the SDGs ...................8 Incorporation of the Sustainable Development Goals in local and regional frameworks ........................................................8 Institutional mechanisms for sustainable governance ....................... 11 Practical examples ........................................................................20 Sustainability pilots .........................................................................20 FutureBuilt, a collaboration for sustainable buildings and arenas .......20 Model projects in Asker ...................................................................20 Citizenship – evolving as a co-creation municipality ..........................24 Democratic innovation.....................................................................24 Arenas for co-creation and community work ....................................24 Policy and enabling environment ..................................................26 Engagement with the national government on SDG implementation ...26 Cooperation across municipalities and regions ................................26 Creating ownership of the Sustainable Development Goals and the VLR .......................................................................... -
Forskrift Om Skolerute for Viken Skoleåret 2021-2022
Forskrift om skolerute for Viken skoleåret 2021-2022 Forskrift gitt med hjemmel i opplæringslovens §3-2. Vedtatt av fylkestinget i Viken fylkeskommune dato 21.oktober 2020 Skoleruta for skoleåret 2021-2022 for skoler i Hurdal, Eidsvoll, Nes, Aurskog-Høland, Marker, Aremark, Halden, Hvaler, Sarpsborg, Rakkestad, Fredrikstad, Råde, Moss, Våler, Skiptvedt, Indre Østfold, Vestby, Ås, Frogn, Nesodden, Nordre Follo, Enebakk, Lørenskog, Rælingen, Lillestrøm, Nittedal, Gjerdrum, Ullensaker, Nannestad, Asker og Bærum Skoledager elever Ferier, fridager, kommentarer August 10 Første skoledag: uke 33, onsdag 18.08 September 22 Oktober 16 Høstferie: uke 40: f.o.m. mandag 04.10 t.o.m. fredag 08.10 November 21 Onsdag 17.11 Fri for elever, felles plandag for lærere Desember 15 Juleferie f.o.m. onsdag 22.12 Januar 21 Juleferie t.o.m. søndag 02.01 Februar 15 Vinterferie uke 8: f.o.m. mandag 21.02 t.o.m. fredag 25.02 Mars 23 April 15 Påskeferie f.o.m lørdag 09.04 t.o.m. mandag 18.04 Mai 20 Fri/helgedag: 17.05, 26.05 Juni 12 Fri 06.06 Siste skoledag: fredag 17.06 Sum 190 Offentlige fridager: Søndag 01.05 Tirsdag 17.05 Torsdag 26.05 Kr. Himmelfartsdag Mandag 06.06 2. pinsedag Oslo, 25.06.2020 Skoleruta for skoleåret 2021-2022 for skoler i Hemsedal, Gol, Ål, Nes i Hallingdal, Hol, Nore og Uvdal, Modum, Flå, Ringerike, Hole, Krødsherad, Sigdal, Rollag, Flesberg, Øvre Eiker, Kongsberg, Drammen, Lier, Jevnaker og Lunner Skoledager elever Ferier, fridager, kommentarer August 10 Første skoledag: uke 33, onsdag 18.08 September 22 Oktober 16 Høstferie: uke 40: f.o.m. -
Rangering K.Gr. 13 Totalt
Rangering K.gr. 13 Totalt Grunnskole Pleie og omsorg Barnevern Barnehage Hamar 4 Fjell 30 Moss 11 Moss 92 Asker 6 Grimstad 34 Tønsberg 17 Halden 97 Oppegård 13 Bodø 45 Kongsberg 19 Gjøvik 104 Lier 22 Røyken 67 Nedre Eiker 26 Lillehammer 105 Sola 29 Gjøvik 97 Nittedal 27 Ringsaker 123 Lillehammer 37 Kristiansund 107 Skedsmo 49 Tønsberg 129 Kongsberg 38 Horten 109 Sandefjord 67 Steinkjer 145 Ski 41 Kongsberg 113 Lørenskog 70 Stjørdal 146 Moss 55 Karmøy 114 Lier 75 Porsgrunn 150 Nittedal 55 Hamar 123 Oppegård 86 Kristiansund 170 Tønsberg 56 Steinkjer 137 Karmøy 101 Kongsberg 172 Elverum 59 Skedsmo 168 Røyken 104 Bodø 173 Bodø 69 Haugesund 186 Ski 112 Horten 178 Skedsmo 72 Moss 188 Porsgrunn 115 Nedre Eiker 183 Lørenskog 74 Lier 191 Horten 122 Hamar 185 Molde 88 Sola 223 Sola 129 Asker 189 Kristiansund 97 Ullensaker 230 Harstad 136 Haugesund 206 Steinkjer 98 Sarpsborg 232 Haugesund 151 Arendal 207 Ringsaker 100 Arendal 234 Asker 154 Sarpsborg 232 Røyken 108 Askøy 237 Arendal 155 Sandefjord 234 Ålesund 116 Gj.sn. k.gr. 13 238 Hamar 168 Harstad 237 Askøy 121 Lørenskog 254 Ringerike 169 Gj.sn. k.gr. 13 240 Horten 122 Oppegård 261 Gj.sn. k.gr. 13 174 Lier 247 Grimstad 125 Halden 268 Lillehammer 174 Rana 250 Porsgrunn 133 Elverum 274 Ullensaker 177 Skien 251 Gj.sn. k.gr. 13 139 Nedre Eiker 276 Molde 182 Elverum 254 Skien 151 Ringerike 283 Askøy 213 Askøy 256 Haugesund 165 Ålesund 288 Bodø 217 Sola 273 Arendal 176 Ski 298 Ringsaker 225 Grimstad 278 Nedre Eiker 179 Harstad 309 Skien 239 Molde 306 Gjøvik 210 Skien 311 Eidsvoll 252 Ski 307 Ringerike -
Camilla Brautaset 26 Petra Hyncicova 27 Ane Johnsen 28 Jesse Knori 29-30 Anne Siri Lervik 31 Lucy Newman 32-33 Christina Rolandsen 34
Women’s Nordic Camilla Brautaset 26 Petra Hyncicova 27 Ane Johnsen 28 Jesse Knori 29-30 Anne Siri Lervik 31 Lucy Newman 32-33 Christina Rolandsen 34 25 2017 colorado buffaloes Camilla Brautaset A A A 5-5 Senior Women’s Nordic Oslo, Norway (Oslo Handelsgym/Heming Ski Club) 3 Letters; 2014 as a freshman, 2015 as a sophomore, 2016 as a junior Career at Colorado— 2016 (Junior)— An experienced veteran, she enters her senior campaign with 30 races under her belt - the most by any Buffalo on the women’s Nordic team entering the 2017 season. SEASON BY SEASON RESULTS She finished all 10 races through the RMISA Championships and had seven top 20 finishes. 2014 CL FS She placed ninth in the classic race at the RMISA Championships for her top finish of the season in her very last meet. Her top freestyle result was 12th place in the freestyle at New 2M0e1x5ic o(.S Sohpeh womaso ar me)e— mber of the National Collegiate All-Academic Ski Team for maintaining above a 3.5 grade point average and participating at the RMISA Championships/NCAA West Regional. Utah Invitational ̶̶ Montana State Invitational 8 11 She competed and finished 10 events, with four top 20 and two top Colorado Invitational 23 11 2150 1ap4p (eFarreasnhcmesa. Ant) —the New Mexico Invitational, she placed tenth in the 10k classic. She placed eleventh in the 10k classic at the Utah Invitational. She was a member of CU’s 4.0 Club and is N20ew15 Mexico Invitational C45L FS a part of the National All Academic Ski Team. -
Supplementary File for the Paper COVID-19 Among Bartenders And
Supplementary file for the paper COVID-19 among bartenders and waiters before and after pub lockdown By Methi et al., 2021 Supplementary Table A: Overview of local restrictions p. 2-3 Supplementary Figure A: Estimated rates of confirmed COVID-19 for bartenders p. 4 Supplementary Figure B: Estimated rates of confirmed COVID-19 for waiters p. 4 1 Supplementary Table A: Overview of local restrictions by municipality, type of restriction (1 = no local restrictions; 2 = partial ban; 3 = full ban) and week of implementation. Municipalities with no ban (1) was randomly assigned a hypothetical week of implementation (in parentheses) to allow us to use them as a comparison group. Municipality Restriction type Week Aremark 1 (46) Asker 3 46 Aurskog-Høland 2 46 Bergen 2 45 Bærum 3 46 Drammen 3 46 Eidsvoll 1 (46) Enebakk 3 46 Flesberg 1 (46) Flå 1 (49) Fredrikstad 2 49 Frogn 2 46 Gjerdrum 1 (46) Gol 1 (46) Halden 1 (46) Hemsedal 1 (52) Hol 2 52 Hole 1 (46) Hurdal 1 (46) Hvaler 2 49 Indre Østfold 1 (46) Jevnaker1 2 46 Kongsberg 3 52 Kristiansand 1 (46) Krødsherad 1 (46) Lier 2 46 Lillestrøm 3 46 Lunner 2 46 Lørenskog 3 46 Marker 1 (45) Modum 2 46 Moss 3 49 Nannestad 1 (49) Nes 1 (46) Nesbyen 1 (49) Nesodden 1 (52) Nittedal 2 46 Nordre Follo2 3 46 Nore og Uvdal 1 (49) 2 Oslo 3 46 Rakkestad 1 (46) Ringerike 3 52 Rollag 1 (52) Rælingen 3 46 Råde 1 (46) Sarpsborg 2 49 Sigdal3 2 46 Skiptvet 1 (51) Stavanger 1 (46) Trondheim 2 52 Ullensaker 1 (52) Vestby 1 (46) Våler 1 (46) Øvre Eiker 2 51 Ål 1 (46) Ås 2 46 Note: The random assignment was conducted so that the share of municipalities with ban ( 2 and 3) within each implementation weeks was similar to the share of municipalities without ban (1) within the same (actual) implementation weeks. -
Upcoming Projects Infrastructure Construction Division About Bane NOR Bane NOR Is a State-Owned Company Respon- Sible for the National Railway Infrastructure
1 Upcoming projects Infrastructure Construction Division About Bane NOR Bane NOR is a state-owned company respon- sible for the national railway infrastructure. Our mission is to ensure accessible railway infra- structure and efficient and user-friendly ser- vices, including the development of hubs and goods terminals. The company’s main responsible are: • Planning, development, administration, operation and maintenance of the national railway network • Traffic management • Administration and development of railway property Bane NOR has approximately 4,500 employees and the head office is based in Oslo, Norway. All plans and figures in this folder are preliminary and may be subject for change. 3 Never has more money been invested in Norwegian railway infrastructure. The InterCity rollout as described in this folder consists of several projects. These investments create great value for all travelers. In the coming years, departures will be more frequent, with reduced travel time within the InterCity operating area. We are living in an exciting and changing infrastructure environment, with a high activity level. Over the next three years Bane NOR plans to introduce contracts relating to a large number of mega projects to the market. Investment will continue until the InterCity rollout is completed as planned in 2034. Additionally, Bane NOR plans together with The Norwegian Public Roads Administration, to build a safer and faster rail and road system between Arna and Stanghelle on the Bergen Line (western part of Norway). We rely on close -
The Nature of Ordovician Limestone-Marl Alternations in the Oslo-Asker District
.re./sereprs OPEN The nature of Ordovician limestone-marl alternations in the Oslo-Asker District (Norway): reee: 1 e 01 epe: 0 eer 01 witnesses of primary glacio-eustasy se: 07 r 016 or diagenetic rhythms? Chloé E. A. Amberg1, Tim Collart2, Wout Salenbien2,3, Lisa M. Egger4,5, Axel Munnecke4, Arne T. Nielsen6, Claude Monnet1, Øyvind Hammer7 & Thijs R. A. Vandenbroucke1,2 Ordovician limestone-marl alternations in the Oslo-Asker District have been interpreted as signaling glacio-eustatic lowstands, which would support a prolonged “Early Palaeozoic Icehouse”. However, these rhythmites could alternatively refect diferential diagenesis, without sedimentary trigger. Here, we test both hypotheses through one Darriwilian and three Katian sections. Our methodology consists of a bed-by-bed analysis of palynological (chitinozoan) and geochemical (XRF) data, to evaluate whether the limestone/marl couplets refect an original cyclic signal. The results reveal similar palynomorph assemblages in limestones and marls. Exceptions, which could be interpreted as refecting palaeoclimatological fuctuations, exist at the species level: Ancyrochitina bornholmensis seems to be more abundant in the marl samples from the lower Frognerkilen Formation on Nakkholmen Island. However, these rare cases where chitinozoans difer between limestone/marl facies are deemed insufcient for the identifcation of original cyclicity. The geochemical data show a near-perfect correlation between insoluble elements in the limestone and the marls, which indicates a similar composition of the potential precursor sediment, also in the Frognerkilen Formation. This is consistent with the palynological data. Although an original cyclic pattern could still be recorded by other, uninvestigated parameters, our palaeontological and geochemical data combined do not support the presence of such a signal.