The Fortress Trail at Oscarsborg Fortress
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Frisk Oslofjord: RESYME Etter Seminar 14/11-2018 Statens Park Tønsberg
Frisk Oslofjord: RESYME etter seminar 14/11-2018 Statens Park Tønsberg Oslofjordens tilstand er svekket og fjorden er nærmest fiskedød. FRISK OSLOFJORD skal samle og formidle kunnskap om det undersjøiske landskapet og livet under de blå flater i Færder og Ytre Hvaler nasjonalparker og etablerer et grunnlag for kunnskapsbasert forvaltning. Kystforvaltning skal ikke lenger gjøres i blinde, og befolkningen, spesielt barn og unge som er framtidens beslutningstakere, skal opplyses for å styrke et bredt eierskap til fjorden og de tiltak som må gjennomføres. FRISK OSLOFJORD skal ta i bruk ny teknologi som kan revolusjonere framtidig kartlegging og overvåking i havet. Prosjektet ble presentert i Auditoriet Statens Park Tønsberg den 11 nov. 2018 for nærmere 60 fremmøtte med representanter fra: Besøkssenter Færder nasjonalpark, Besøkssenter Ytre Hvaler nasjonalpark, Fiskeridirektoratet, Fylkesmannen i Vestfold, Fylkesmannen i Østfold, Færder kommune, Kystverket, Nasjonalparkstyrene, Miljødirektoratet / Statens naturoppsyn, Oslofjordens Friluftsråd, RFF Oslofjordfondet, Skjærgårdstjenesten Færder, Små fiskeren, Sparebankstiftelsen DNB, Statens naturoppsyn, Vannområde Horten-Larvik/Aulivassdraget, Vestfold fylkeskommune, Vestfold fylkeskommune Utdanningsavdelingen, Østfold fylkeskommune, Opplæringsavdelingen, samt deltakere fra de 6 partnere som har gått sammen for å gjennomføre prosjektet FRISK OSLOFJORD: Havforskningsinstituttet, Inspiria, Kartverket sjødivisjonen, Kongsberg Maritime, NGU og NIVA. Færder og Ytre Hvaler nasjonalparker er prosjekteier -
1 Introduction
Notes 1 Introduction 1. Donald Macintyre, Narvik (London: Evans, 1959), p. 15. 2. See Olav Riste, The Neutral Ally: Norway’s Relations with Belligerent Powers in the First World War (London: Allen and Unwin, 1965). 3. Reflections of the C-in-C Navy on the Outbreak of War, 3 September 1939, The Fuehrer Conferences on Naval Affairs, 1939–45 (Annapolis: Naval Institute Press, 1990), pp. 37–38. 4. Report of the C-in-C Navy to the Fuehrer, 10 October 1939, in ibid. p. 47. 5. Report of the C-in-C Navy to the Fuehrer, 8 December 1939, Minutes of a Conference with Herr Hauglin and Herr Quisling on 11 December 1939 and Report of the C-in-C Navy, 12 December 1939 in ibid. pp. 63–67. 6. MGFA, Nichols Bohemia, n 172/14, H. W. Schmidt to Admiral Bohemia, 31 January 1955 cited by Francois Kersaudy, Norway, 1940 (London: Arrow, 1990), p. 42. 7. See Andrew Lambert, ‘Seapower 1939–40: Churchill and the Strategic Origins of the Battle of the Atlantic, Journal of Strategic Studies, vol. 17, no. 1 (1994), pp. 86–108. 8. For the importance of Swedish iron ore see Thomas Munch-Petersen, The Strategy of Phoney War (Stockholm: Militärhistoriska Förlaget, 1981). 9. Churchill, The Second World War, I, p. 463. 10. See Richard Wiggan, Hunt the Altmark (London: Hale, 1982). 11. TMI, Tome XV, Déposition de l’amiral Raeder, 17 May 1946 cited by Kersaudy, p. 44. 12. Kersaudy, p. 81. 13. Johannes Andenæs, Olav Riste and Magne Skodvin, Norway and the Second World War (Oslo: Aschehoug, 1966), p. -
The Historian-Filmmaker's Dilemma: Historical Documentaries in Sweden in the Era of Häger and Villius
ACTA UNIVERSITATIS UPSALIENSIS Studia Historica Upsaliensia 210 Utgivna av Historiska institutionen vid Uppsala universitet genom Torkel Jansson, Jan Lindegren och Maria Ågren 1 2 David Ludvigsson The Historian-Filmmaker’s Dilemma Historical Documentaries in Sweden in the Era of Häger and Villius 3 Dissertation in History for the Degree of Doctor of Philosophy presented at Uppsala University in 2003 ABSTRACT Ludvigsson, David, 2003: The Historian-Filmmaker’s Dilemma. Historical Documentaries in Sweden in the Era of Häger and Villius. Written in English. Acta Universitatis Upsalien- sis. Studia Historica Upsaliensia 210. (411 pages). Uppsala 2003. ISSN 0081-6531. ISBN 91-554-5782-7. This dissertation investigates how history is used in historical documentary films, and ar- gues that the maker of such films constantly negotiates between cognitive, moral, and aes- thetic demands. In support of this contention a number of historical documentaries by Swedish historian-filmmakers Olle Häger and Hans Villius are discussed. Other historical documentaries supply additional examples. The analyses take into account both the produc- tion process and the representations themselves. The history culture and the social field of history production together form the conceptual framework for the study, and one of the aims is to analyse the role of professional historians in public life. The analyses show that different considerations compete and work together in the case of all documentaries, and figure at all stages of pre-production, production, and post-produc- tion. But different considerations have particular inuence at different stages in the produc- tion process and thus they are more or less important depending on where in the process the producer puts his emphasis on them. -
Late-Pleistocene Foraminifera from the Oslofj Ord Area, Southeast Norway
NORSK GEOLOGISK TIDSSKRIFT 33 LATE-PLEISTOCENE FORAMINIFERA FROM THE OSLOFJ ORD AREA, SOUTHEAST NORWAY BY RoLF W. FEYLI�G-HANSSEN (University of Oslo) CONTENTS P age Abstract 109 Introduction .................... ... ....... 109 The Yoldia-clay ...................... ..... 113 The Arca-clay ................... ............ 119 Transitional sediments . ......... .......... 120 The lsocardia-clay ....... ..................... 121 The Foraminifera ..... ........... .. .. 125 Index of foraminiferal species . .. .. .. .. 144 References .. .. .. .. .. .. .. .. .. .. .. .. 146 Plates I-Il . ... ..................... ..... 151 Abst rac t : The present paper is a preliminary report on a quanti tative study of the foraminiferal contents of Late- and Post-Glacial clay samples from the Oslofjord area. It appears that sedimen�s of Late-Glacial and Post-Glacial age are sharply defined by a few dominent species in their foraminiferal faunas. A subdivision can be based partly on the dominance of some species and partly on the presence of certain a::cessory species. In this way, most samples from the area could be rapidly pla::ed in the old strati graphic scheme based on megafossils. Introduction. For the Oslofjord area BRøGGER (1900-19 01) established a stratigraphy of the sediments dep)sited at the r etreating front of the ice of the latest glaciation on the basis of their content of fossil 12 -Geo!. 33 110 ROLF W. FEYLI:-.IG-HAXSSEN pelecypods. He thus divided the clay sediments into the following main horizons: Yoldia-clay, Arca-clay, Mytilus- and Cyprina-clay, (of Late-Glacialage) Cardium-clay, Ostrea-clay, Isocardia-clay, (of Post Glacial age), and Mya-clay which is of recent origin. The Yoldia-clay is a high-arctic sediment. Its index fossil is Portlandia arctica (GRAY) ( = Yoldia arctica GRAY) which at present lives only in arctic waters, e.g. -
Introduction to the Studies of Pollution in the Oslofjord
Helgol~inder wiss. Meeresunters. 17, 455-461 (1968) Introduction to the studies of pollution in the Oslofjord JOHAN T. RUUD Institute of Marine Biology, University of Oslo, Oslo, Norway KURZFASSUNG: Einfiihrung in die Untersuchungen fiber die Verunreinigung im Oslo- fjord. Der Oslofjord erstreckt sich etwa 100 km in n/Srdlicher Richtung yore Skagerrak bis nach Oslo. Bei Dr~bak, etwa auf dem zweiten Drittel des Weges nach Oslo, gibt es eine Reihe yon Hindernissen, die einem ungehinderten Austausch der Wassermassen im Fjord entgegenstehen. Der wichtigste Durchlaf~ ist nur etwa 300 m breit und hat eine Wassertiefe ~iber der Schwelle yon 19 m. Hinter Drobak besteht der Fjord aus zwei Becken, dem Westfjord und dem Bunne- fjord, die Tiefen yon 164 m beziehungsweise von 160 m aufweisen. Der Fjord hinter Drobak hat eine Fl~che yon 191 km~; die Wassermenge betr~igt nach Berechnungen 9,4 Milliarden m ~. Der j~hrliche Zufluf~ an Siit~wasser, das durch Abw~.sser yon ca. 700 000 Menschen und einer bedeutenden Industrie verunreinigt wird, betr~igt etwa 800 Millionen m 3. Studien fiber die Fauna wurden im 18. Jahrhundert von O. F. MiSLLER und im 19. Jahrhundert von M. und G. O. SARS vorgenommen. Ausgedehntere Untersuchungen wurden um 1900 yon J. Hjollx und H. H. GRAN begonnen. Seit Anfang der dreit~iger Jahre sind diese Untersuchungen yon den biologischen Instituten der Universit~it Oslo weitergefiihrt worden. 1953 wurde die Situation hinsichtlich der Verunreinigung des Fjords alarmierend. Die Beh/Srden der Stadt Oslo wurden davon unterrichtet, dal~ umfassendere Untersuchungen notwendig seien, um die Folgen, die dadurch entstehen, daf~ der Fjord als Auffangbecken f~ir die Abw~isser der Stadt dient, zu erforschen. -
How Can Cooperation Between Neighbouring Ports Within the Oslofjord Area Become Reality?
HØGSKOLEN I VESTFOLD How can cooperation between neighbouring ports within the Oslofjord area become reality? A study of two neighbouring ports and the opportunities of future collaboration for mutual benefits Øivind Berg November 2013 In partial fulfilment of the degree Master in Maritime Management, Department of Maritime Technology and Innovation, Vestfold University College, Horten, Norway Acknowledgement This thesis would not have arisen without the kind contribution from Finn Flogstad, Port Director, Port of Grenland, Jan Fredrik Jonas, Port Director, Port of Larvik, Jan Einar Skarding, Marketing and Logistics Manager, Port of Grenland, Per Kvaale Caspersen, Project Manager at Vestfold Municipal County, and Olav Risholt, Project Manager Telemark Municipal County. I must also thank advisors and colleagues at Vestfold University College; Halvor Schøyen, PhD, Kjell Ivar Øvergård Dr. Professor, Jørn Kragh Project Manager and Tine Viveka Westerberg for valuable information and good advice. And, not at least: the one at home Halldis, who has not seen me for a good while. Contents Introduction ................................................................................................................................ 1 Background ............................................................................................................................. 1 Research question ................................................................................................................... 2 Relation to other work in the area ......................................................................................... -
Metreport Oceanography a High-Resolution, Curvilinear ROMS Model for the Oslofjord Fjordos Technical Report No
No. 4/2016 ISSN 2387-4201 METreport Oceanography A high-resolution, curvilinear ROMS model for the Oslofjord FjordOs technical report No. 2 Lars Petter Røed1,2, Nils Melsom Kristensen1, Karina Bakkeløkken Hjelmervik3 and André Staalstrøm4 1Norwegian Meteorological Institute, 2Department of Geosciences, University of Oslo, 3University College of Southeast Norway, 4Norwegian Institute of Water Research aa METreport Title Date A high-resolution, curvilinear ROMS model for the Oslofjord. Fjor- June 7, 2016 dOs technical report No. 2 Section Report no. Ocean and Ice 4/2016 Author(s) Classification Lars Petter Røed, Nils Melsom Kristensen, Karina Bakkeløkken ③Free ❥Restricted Hjelmervik, André Staalstrøm Client(s) Client’s reference Oslofjordfondet Abstract Provided is documentation of a new Oslofjord model, FjordOs CL, utilizing the curvilinear option of the Regional Ocean Modeling System - ROMS. The development is part of the project FjordOs. FjordOs CL has a spatial grid size varying from about 50 meters in the Drøbak sound to about 300 meters at its southern open boundary bordering on the Sk- agerrak. It features 42 terrain-following levels in the vertical. In addition to being forced by atmospheric, river and tidal input it is also forced by oceanic input at the open boundary. The atmospheric input is extracted from MET Norway’s operational NWP model (AROME- MetCoOp), while oceanic input is extracted from MET Norway’s operational, ocean forecast- ing model NorKyst800. The river input consists of observational based estimated discharges from 37 rivers along the perimeter of the fjord. The tidal input is based on the TPXO Atlantic database modified by observations and consists of nine tidal constituents as input. -
Travel Guide
TRAVEL GUIDE Traces of the COLD WAR PERIOD The Countries around THE BALTIC SEA Johannes Bach Rasmussen 1 Traces of the Cold War Period: Military Installations and Towns, Prisons, Partisan Bunkers Travel Guide. Traces of the Cold War Period The Countries around the Baltic Sea TemaNord 2010:574 © Nordic Council of Ministers, Copenhagen 2010 ISBN 978-92-893-2121-1 Print: Arco Grafisk A/S, Skive Layout: Eva Ahnoff, Morten Kjærgaard Maps and drawings: Arne Erik Larsen Copies: 1500 Printed on environmentally friendly paper. This publication can be ordered on www.norden.org/order. Other Nordic publications are available at www.norden.org/ publications Printed in Denmark T R 8 Y 1 K 6 S 1- AG NR. 54 The book is produced in cooperation between Øhavsmuseet and The Baltic Initiative and Network. Øhavsmuseet (The Archipelago Museum) Department Langelands Museum Jens Winthers Vej 12, 5900 Rudkøbing, Denmark. Phone: +45 63 51 63 00 E-mail: [email protected] The Baltic Initiative and Network Att. Johannes Bach Rasmussen Møllegade 20, 2200 Copenhagen N, Denmark. Phone: +45 35 36 05 59. Mobile: +45 30 25 05 59 E-mail: [email protected] Top: The Museum of the Barricades of 1991, Riga, Latvia. From the Days of the Barricades in 1991 when people in the newly independent country tried to defend key institutions from attack from Soviet military and security forces. Middle: The Anna Akhmatova Museum, St. Petersburg, Russia. Handwritten bark book with Akhmatova’s lyrics. Made by a GULAG prisoner, wife of an executed “enemy of the people”. Bottom: The Museum of Genocide Victims, Vilnius, Lithuania. -
Heavy Cruisers of the Admiral Hipper Class Free
FREE HEAVY CRUISERS OF THE ADMIRAL HIPPER CLASS PDF Gerhard Koop,Klaus-Peter Schmolke | 208 pages | 06 Jun 2014 | Pen & Sword Books Ltd | 9781848321953 | English | Barnsley, United Kingdom Heavy Cruisers of the Admiral Hipper and the Prinz Eugen class Admiral Hipperthe first of five ships of her class, was the lead ship of the Admiral Hipper class of heavy cruisers which served with Nazi Germany 's Kriegsmarine during World War II. The ship was named after Admiral Franz von Hippercommander of the German battlecruiser squadron during the Battle of Jutland in and later commander-in-chief of the German High Seas Fleet. She was armed with a main battery of eight Admiral Hipper saw a significant amount of action during the war, notably present during the Battle of the Atlantic. In Decembershe broke out into the Atlantic Ocean to operate against Allied merchant shipping, though this operation ended without significant success. In FebruaryAdmiral Hipper sortied again, sinking several merchant vessels before eventually returning to Germany via the Denmark Strait. As a result, Admiral Hipper was returned to Germany and decommissioned for repairs. The ship was never restored to operational status, however, and Heavy Cruisers of the Admiral Hipper Class 3 MayRoyal Air Force bombers severely damaged her while she was in Kiel. Her crew scuttled the ship at her mooringsand in Julyshe was raised and towed to Heikendorfer Bay. She was ultimately broken up for scrap in — and her bell is currently on display at the Laboe Naval Memorial. The Admiral Hipper class of heavy cruisers was ordered in the context of German naval rearmament after the Nazi Party came to power in and repudiated the disarmament clauses of the Treaty of Versailles. -
Contribution to the Geology of the So.Uthern Part Of
CONTRIBUTION TO THE GEOLOGY OF THE SO. UTHER N PART OF THE OSLOFJORD THE RHOMB-PORPHYRY CONGLOMERATE WITH REMARKS ON YOUNGER TECTONICS WITH 12 TEXT·FIGURES, 5 PLATES AND l MAP BY LEIF STØRME R Introduction. In his classical work: "O ber die Bildungsgeschichte des Kristiania fjords" ( = Oslofjord), Brøgger (1886) was a ble to demonstrate and explain in their main features, the peculiar geologic structures which led to the formation of the Oslofjord and influenced the topo graphy also of the adjacent parts of the Oslo Region. The origin of the fjord is chiefly due to considerable subsidences along mainly N-S fault-lines probably of Permian age. The greatest fault runs along the east side of the fjord and borders the Oslo Region with its Paleozoic sediments and igneous rocks, from the Precambrian area to the east. The present paper deals primarily with the so-called rhomb porphyry conglomerate which forms one of the youngest sedimentary series of the Oslo Region and which occurs on a num ber of islands situated along the east side of the fjord. The term rhomb-porphyry conglomerate was introduced by Brøgger (1900) to signi fy a thick series chiefly of breccias and conglomerates consisting almost ex clusively of fragments of various types of Permian rhomb-porphyry Javas. The sediments exhibit several peculiar characteristics which are described and tentatively interpreted in the present paper. The consolidated sediments have in post-Permian time been subject to considerable tectonic disturbances. A study of the structures has led the author to the conception of a connection with the late Mesozoic and Tertiary orogenetic movements of northern Europe. -
Edvard MUNCH
THE OFFICIAL GUIDE FOR OSLO AND SURROUNDING REGION OSLO GUIDE2013 WELCOME TO OSLO The experience starts with us at the Tourist Information Offices No one knows Oslo better than us! We know what’s happening and where, and we are committed to make your stay eventful and fun! We have all the brochures and maps you need to find your way around Oslo. We also offer the Oslo Pass, hotel reservations, city bike hire, tickets for public transport or sightseeing trips, train tickets (including Norway in a nutshell®), currency exchange, gift items and more. www.visitoslo.com Here you will find all the latest information about Oslo, as well as useful tips on how to make your stay in Oslo the best possible. Book your hotel accommodation and tickets for sightseeing, etc., in advance. Contact us at: To Holmenkollen Email: [email protected] Ski Jump & Museum Phone: +47 815 30 555 www.visitoslo.com SLOTTSPARKEN Youngstorget AKERSELVA Kristian IV’s gate Royal www.facebook.com/visitoslo Nydalsveien Palace www.twitter.com/visitoslo Storgata Fredriks gate Stortorvet Oslo S National Karl Johans gate Theatre Stortingsgata Train The Tourist Information Office Station Oslo Tollbugata near Oslo CityTo Vigeland Hall (Rådhuset) City Hall Oslo Park Rådhusgata Opera Fr. Nansens plass 5, House Munkedamsveien Entr. from Roald Amundsens gate Akershus Castle & For opening hours see: www.visitoslo.com Fortress Facebook.com/OsloTouristInformation BJØRVIKA 0 250 M 0 250 YARDS CONTENTS FACTS AND HISTORY 08 ACTIVITIES: WINTER 10 ACTIVITIES: CHILDREN 14 ACTIVITIES: SUMMER 14 SIGHTSEEING 18 MUSEUMS & ATTRACTIONS 22 FESTIVALS - CONCERTS - PERFORMING ARTS 38 GAY OSLO 43 SHOPPING 44 RESTAURANTS AND NIGHTLIFE 48 ACCOMMODATION 60 CONFERENCE INFORMATION 65 THE OSLO REGION 68 USEFUL INFORMATION 70 CRUISE 76 PUBLISHER: VisitOSLO as, Grev Wedels pl. -
Quatemary Sediments and Bedrock Geology in the Outer Oslofjord and Northemmost Skagerrak
Quatemary sediments and bedrock geology in the outer Oslofjord and northemmost Skagerrak ANDERS SOLHEIM & GISLE GRØNLIE Solheim, A. & Grønlie, G.: Quaternary sediments and bedrock geology in the outer Oslofjord and northernmost Skagerrak. Norsk Geologisk Tidsskrift, Vol. 63, pp. 55-72. ISSN 0029-196X. Shallow seismic (sparker), magnetic and bathymetric profiling were carried out on two cruises in the outer Oslofjord in 1979 and 1980. The survey area is characterized by deep silled basins defined by the main structural trends of the surrounding land area. The Quaternary scdiments, largcly restricted to these major basins. can be dividcd into three main units of supposed pre-Weichselian to Holocene age. Most of the sediments were probably deposited during relatively short time intervals in the Late Weichselian under ice-proximal conditions, and in the early Holocene. Magnetic total field and scismic data wcrc uscd to map the submarine outlines of the Permo Carboniferous Vestfold lavas, the Perm i an sedimentary rocks and the Larvik i te body. The presencc of other intrusives in the eastern and southern part of the survey area is discussed. A. Solheim & G. Grønlie, Institutt for geologi, Postboks 1047, Blindern, Oslo 3, Norway. Present address of A. So/heim: Norsk Polarinstitutt, Rolfstangvn. 12, N-1330, Oslo Lufthavn. Present address of G. Grønlie: Det Norske Oljeselskap, Postboks 9556, Egertorget, N-Os/o l. The survey area is situated in the southern part 3. to map the submarine bedrock geology and of the Permo-Carboniferous Oslo Graben, a structural pattern. downfaulted block of Paleozoic rocks, about 50 In this paper we present data and results ob km wide and more than 200 km long in a north tained during both cruises.