Scenic Norway - Majestic & Vibrant
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UNESCO Fjord Bus Tour
2017 UNESCO Fjord Bus tour Sognefjord - Geirangerfjord Sogndal-Loen-Stryn-Geiranger Geiranger-Stryn-Loen-Sogndal 1 Geirangerfjord UNESCO Fjord Bus tour Geiranger Flydalsjuvet One-way Adult NOK Child NOK Sogndal–Geiranger 600,- 300,- Sogndal/Geiranger-Loen/Stryn 400,- 200,- Loen/Stryn-Sogndal/Geiranger 400,- 200,- Geiranger-Sogndal 600,- 300,- Stryn Loen Nordfjord Round trip Adult NOK Child NOK Sogndal–Geiranger, return 1200,- 600,- Sogndal–Loen/Stryn, return 800,- 400,- Loen/Stryn–Sogndal/Geiranger, return 800,- 400,- Geiranger-Loen/Stryn, return 800,- 400,- Geiranger-Sogndal, return 1 200,- 600,- Sogndal DAILY Geiranger DAILY 19.6-13.8 19.6-13.8 Bus from Sogndal 08:00 Bus from Geiranger 15:30 Arrival Loen 09:50 Arrival Stryn 17:05 Departure Loen 10:00 Departure Stryn 17:10 Arrival Stryn 10:10 Arrival Loen 17:20 Departure Stryn 10:15 Departure Loen 17:25 Arrival Geiranger 12:00 Arrival Sogndal 19:30 Fjærlandsfjord Sogndal Sognefjord 2 3 Welcome to the UNESCO Fjord Bus tour Welcome on board and enjoy the world famous fjords and Norway’s natural marvels. The tour will take you between 4 amazing fjords, Geirangerfjord- Stops along the route Nordfjord-Fjærlandsfjord-Sognefjord. You will see towering peaks, roaring waterfalls, charming villages Sogndal bus terminal and idyllic farmland. The Sogndal bus terminal is located in the centre of the small village. The bus station is a 3 minutes walk from the walk from Quality Hotel Sogndal. Loen bus stop The bus stop is located close to Hotel Alexandra and Loen Services during the journey Active Base Camp This brochure is your guide during your journey. -
Loen Hotell Alexandra En Vestlandsperle Loen Ligger Som Et Vakkert Smykke Mellom Fjellene Og Nordfjorden
Loen Hotell Alexandra En vestlandsperle Loen ligger som et vakkert smykke mellom fjellene og Nordfjorden. Over oss stiger velkjente tinder som Skåla, med sitt velkjente tårn på toppen. Innover i Loen har vi det smaragdgrønne Lovatnet som strekker seg vakkert innover i dalen. De vakre naturinntrykkene speiler seg mot oss fra alle kanter, der fjellene står stolt opp mot himmelen over. Hotellet vårt, Loen Alexandra, er noe av det beste Norge har å by på. Den renommerte restau- ranten serverer mat i ypperste klasse, bygd på deilige, ferske, lokale matvarer. Med sitt fokus på utsøkt kvalitet og gastronomi i verdensklasse, er dette stedet for deg som elsker et bedre måltid. Kanskje vil du også prøve et glass fra restaurantens velfylte vinkjeller? I spaavdelingen kan vi nyte eksklusive behandlinger som får deg til å fylles av glede i både kropp og sjel. Badeanlegget på hotellet innbyr også til en liten svømmetur, eller en avslappende stund i et av de mange badene Loen Alexandra har å tilby sine gjester. La tankene flyve mens det for- friskende og varme vannet omslutter deg. Fra vår fortreffelige base på Loen Alexandra, tar vi utflukter til de mange spennende områdene rundt. Vår reise tar oss til den fabelaktige Briksdalsbreen, innerst i Olden. på en vakker båttur over det krystallklare Lovatnet, og ikke minst til vidunderlige Unesco verdensarvstedet Geiran- ger. Inkludert i prisen: • Buss Oslo - Loen t/r • Buss Bergen - Loen t/ • 5 netter på Hotell Alexandra (superiorrom med fjellutsikt) • 5 x frokost • 5 x middag • Utflukt til Briksdalsbreen • Trollbiler ved Briksdalsbreen • Utflukt til Geirangerfjorden • Vandretur i Loen • Båttur på Lovatnet • Norsk reiseleder Tillegg pr. -
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. -
WEST NORWEGIAN FJORDS UNESCO World Heritage
GEOLOGICAL GUIDES 3 - 2014 RESEARCH WEST NORWEGIAN FJORDS UNESCO World Heritage. Guide to geological excursion from Nærøyfjord to Geirangerfjord By: Inge Aarseth, Atle Nesje and Ola Fredin 2 ‐ West Norwegian Fjords GEOLOGIAL SOCIETY OF NORWAY—GEOLOGICAL GUIDE S 2014‐3 © Geological Society of Norway (NGF) , 2014 ISBN: 978‐82‐92‐39491‐5 NGF Geological guides Editorial committee: Tom Heldal, NGU Ole Lutro, NGU Hans Arne Nakrem, NHM Atle Nesje, UiB Editor: Ann Mari Husås, NGF Front cover illustrations: Atle Nesje View of the outer part of the Nærøyfjord from Bakkanosi mountain (1398m asl.) just above the village Bakka. The picture shows the contrast between the preglacial mountain plateau and the deep intersected fjord. Levels geological guides: The geological guides from NGF, is divided in three leves. Level 1—Schools and the public Level 2—Students Level 3—Research and professional geologists This is a level 3 guide. Published by: Norsk Geologisk Forening c/o Norges Geologiske Undersøkelse N‐7491 Trondheim, Norway E‐mail: [email protected] www.geologi.no GEOLOGICALSOCIETY OF NORWAY —GEOLOGICAL GUIDES 2014‐3 West Norwegian Fjords‐ 3 WEST NORWEGIAN FJORDS: UNESCO World Heritage GUIDE TO GEOLOGICAL EXCURSION FROM NÆRØYFJORD TO GEIRANGERFJORD By Inge Aarseth, University of Bergen Atle Nesje, University of Bergen and Bjerkenes Research Centre, Bergen Ola Fredin, Geological Survey of Norway, Trondheim Abstract Acknowledgements Brian Robins has corrected parts of the text and Eva In addition to magnificent scenery, fjords may display a Bjørseth has assisted in making the final version of the wide variety of geological subjects such as bedrock geol‐ figures . We also thank several colleagues for inputs from ogy, geomorphology, glacial geology, glaciology and sedi‐ their special fields: Haakon Fossen, Jan Mangerud, Eiliv mentology. -
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. -
IFLA Annual Report 2004-2005
IFLA Section on Library and Research Services for Parliaments ANNUAL REPORT September 2004 – September 2005 ACKNOWLEDGMENTS The work for the Section has been made possible thanks to the active contribution, keen participation and commitment of the Section Officers: Dr. June Verrier, Secretary of the Section and Gro Sandgrind, our Information Coordinator. Unfortunately, during the year 2005, Dr. Verrier resigned her position. The Conferences have been a success primarily thanks to organizers of specific meetings, rapporteurs, presentators, and the commitment of colleagues, friends and participants, and the commitment of the Norwegian Parliamentary Library. We are particularly thankful for receiving the third comer up Newsletter of the Year Award, with the invaluable work of June Verrier and her assistant, Ms. Katrina Arte, seconded by the Chair. Our special thanks and recognition to the Norwegian Storting for the generous hosting, the extraordinarly well organized Preconference, with special mention of the contents and participants, as well as the production efforts to get things going seamlessly and without a glitch. With our gratitude, and congratulations. M.D. SCOPE STATEMENT In accordance with the mission and objectives of IFLA, the Section on Library and Research Services for Parliaments recognises the central role that information must play in the effective functioning of a democratic legislature. In representing parliamentary libraries, the Section encompasses parliamentary and legislative libraries that provide information and documentation services to Parliamentarians and also those that include a research and analysis service. These services are provided to national legislatures in unitary states and to both national and regional legislatures in countries with a federal system of government. -
Knut Døscher Master.Pdf (1.728Mb)
Knut Kristian Langva Døscher German Reprisals in Norway During the Second World War Master’s thesis in Historie Supervisor: Jonas Scherner Trondheim, May 2017 Norwegian University of Science and Technology Preface and acknowledgements The process for finding the topic I wanted to write about for my master's thesis was a long one. It began with narrowing down my wide field of interests to the Norwegian resistance movement. This was done through several discussions with professors at the historical institute of NTNU. Via further discussions with Frode Færøy, associate professor at The Norwegian Home Front Museum, I got it narrowed down to reprisals, and the cases and questions this thesis tackles. First, I would like to thank my supervisor, Jonas Scherner, for his guidance throughout the process of writing my thesis. I wish also to thank Frode Færøy, Ivar Kraglund and the other helpful people at the Norwegian Home Front Museum for their help in seeking out previous research and sources, and providing opportunity to discuss my findings. I would like to thank my mother, Gunvor, for her good help in reading through the thesis, helping me spot repetitions, and providing a helpful discussion partner. Thanks go also to my girlfriend, Sigrid, for being supportive during the entire process, and especially towards the end. I would also like to thank her for her help with form and syntax. I would like to thank Joachim Rønneberg, for helping me establish the source of some of the information regarding the aftermath of the heavy water raid. I also thank Berit Nøkleby for her help with making sense of some contradictory claims by various sources. -
Morphological Signatures of Mass Wasting and Delta Processes in A
Morphological signatures of mass wasting and delta processes in a fjord-lake system : insights from Lovatnet, western Norway Louise Hansen, Nicolas Waldmann, Joep Storms, Raymond S. Eilertsen, Daniel Ariztegui, Emmanuel Chapron, Atle Nesje To cite this version: Louise Hansen, Nicolas Waldmann, Joep Storms, Raymond S. Eilertsen, Daniel Ariztegui, et al.. Morphological signatures of mass wasting and delta processes in a fjord-lake system : insights from Lovatnet, western Norway. Norwegian Journal of Geology, Norwegian Geological Society (Norsk Ge- ologisk Forening, NGF), 2016, 96 (3), pp.9-30. hal-01326339 HAL Id: hal-01326339 https://hal.archives-ouvertes.fr/hal-01326339 Submitted on 3 Jun 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. NORWEGIAN JOURNAL OF GEOLOGY Vol 96 Nr. 3 (2016) http://dx.doi.org/10.17850/njg96-3-02 Morphological signatures of mass wasting and delta processes in a fjord-lake system: insights from Lovatnet, western Norway Louise Hansen1, Nicolas Waldmann2, Joep E.A. Storms3, Raymond S. Eilertsen1, Daniel Ariztegui4, Emmanuel Chapron5 & Atle Nesje5,6 1Geological Survey of Norway, Leiv Erikssons vei 39, N–7491 Trondheim, Norway. 2The Dr. Moses Strauss Department of Marine Geosciences, Charney School of Marine Sciences, University of Haifa, Mount Carmel, 31905 Haifa, Israel. -
The Race for Norwegian Heavy Ater, 1940-1945 Table of Contents
IFS Info 4/1995 Olav Njolstad Ole Kristian Grimnes Joachim RBnneberg Bertrand Goldschmidt The Race for Norwegian Heavy ater, 1940-1945 Table of Contents Olav Nj0lstad : Introduction .............................................................................................. :........ 5 Ole Kristian Grimnes : The Allied heavy water operations at Rjukan .................................................. 7 Joachim R0nneberg : Operation "Gunnerside": Reminiscences of a heavy water saboteur ............ 13 Bertrand Goldschmidt : The supplies of Norwegian heavy water to France and the early development of atomic energy ......................................................... 17 Introduction By Olav Njl!llstad The sabotage action against Norsk Hydro's heavy that the Norwegian-Allied heavy water operations water factory at Vemork, Rjukan, in February 1943 "may be considered the first attempt to secure the was undoubtedly one of the most astonishing and non-proliferation of nuclear weapons by military heroic Norwegian-Allied operations in Norway action", and he discusses what kind oflegacy they during the Second World War. Its blend of high represent in that respect. politics, scientific adventure, military drama and In the second paper, Joachim RIilnneberg, who individual courage has intrigued people for more at the age of22 led the sabotage action in February than fifty years. Numerous accounts of the event 1943, shares with us his memories of that dramatic have been made, including two commercial films, event. In addition to the many fascinating details and in Norsk Industriarbeidermuseum (the Norwe about how the sabotage was planned and executed, gian Industrial Workers Museum) at Rjukan there the reader will find some very valuable reflections is now a permanent exhibition of related sabotage on why that particular operation became such a memorabilia. On each anniversary hundreds of huge success. -
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. -
Lithostratigraphy and U-Pb Geochronology of the Telemark Supracrustals in the Bandak-Sauland Area, Te Le Mark, South Norway
NORWEGIAN JOURNAL OF GEOLOGY Lithostratigraphy and geochronologyof the Telemark supracrustals 119 U-Pb lithostratigraphy and geochronology of the Telemark supracrustals in the Bandak-Sauland area, Telemark, South Norway Kauko Laajoki, Fernando Corfu & Tom Andersen Laajoki, K., Corfu, F. &Andersen, T.: Lithostratigraphy and U-Pb geochronology of the Telemark supracrustals in the Bandak-Sauland area, Te le mark, South Norway. Norsk Geologisk Tidsskrift,Vol. 82, pp. 119-138. Trondheim 2002, ISSN 029-196X. The Mesoproterowic Te lemark supracrustals in southern Norway have been subdivided into four groups: (l) the ca. 1500 Ma volcanic Rjukan group overlain by (2) the quartzite-dominatedSeljord group, itself overlain by (3) the ca. 1160 Ma volcanic-sedimentary Bandak group in the west and by (4) the undated Heddal group in the east. New mapping and U-Pb work provide considerable refinement to this stratigraphy. The Ljosdals vatnet porphyry near the base of the Bandak gro up has an age of 1155 ± 3 Ma age, but it overlies that part of the Seljord gro up, which was folded and eroded before deposition of the Bandak gro up. The Brunkeberg porphyry, which has previously been correlated to the Rjukan gro up, yields an identical age of 1155 ± 2 Ma. It is unconformably overlain by a quartzite, which has also been included into the Seljord group. This group must, therefore, consist of two separate successions separated by a period of folding, here referred to as the Vindeggengro up (older) and the Lifiellgro up (younger). The former represents a thick, fluvial,shallow sea sandstone - intertidal heterolithic sequence, whereas the latter is composed of a relati vely thin and mature beach-shoreline sandstone sequence.