The Fishing Capital of Norway Municipality Facts

Total Page:16

File Type:pdf, Size:1020Kb

The Fishing Capital of Norway Municipality Facts Municipality of Båtsfjord The Fishing Capital of Norway Municipality facts • Located in Eastern Finnmark on the north side of the Varanger Peninsula • The municipality covers 1433 square kilometres • Borders the Municipalities of Berlevåg, Vardø, Vadsø and Tana • The name Båtsfjord probably comes from the word «botn», which means «innermost part of a fjord’» • The Båtsfjorden is 13 kilometers long • All housing in the municipality is concentrated in the municipal centre of Båtsfjord • Population of 2201 • Hurtigruten calls here twice daily • Båtsfjord Airport is Norway’s newest airport • It has 4 daily departures Municipality of Båtsfjord Båtsfjord harbour Health care and social care for all Båtsfjord is one of Norway’s largest fishing villages in terms of All residents of Båtsfjord receive the medical and other care they quantities brought ashore. Guaranteed ice-free harbour with 1850 require. We prioritise measures that prevent, reduce or delay the metres of wharf front with electricity, water and waste disposal. The need for institutional care. The health centre combines all sector harbour also offers 7 floating piers of various sizes. There is also a services for the municipality. rescue boat stationed in Båtsfjord. Services offered: A growing village • Community nursing care and home care We are a growing municipality! At the end of September 2013, • Serviced apartments for the elderly Båtsfjord had a population of 2201. This is an increase of 7% over • Nursing home and infirmary the last three years. • The Fjellheimen dementia care home • Intellectual disability homes Well developed educational facilities The municipality aims to offer user adapted and modern educational Other health and social services: facilities by focusing efforts on its two schools. • Telegrafen - Psyciatric day care centre • Coordinated Care Service which consists of Pedagogical • In 2013, Klausjorda and Nordskogen kindergartens had close to Psychological Services, Public Health Centre for children and 90 places for children ages 0-6 years young people, and Child Welfare Services • In 2013, Nordskogen school, with grades 1 to 4, and Båtsfjord • Båtsfjord Service AS is an ASVL company that offers permanent school, with grades 5 to 10, had a total of 263 students adapted work to the occupationally disabled and work in • Båtsfjord Municipal School of Culture and Creative Arts is sheltered workshops housed in the Skansen community centre and offers instrument • Melkarn Boligstiftelse has flats and houses reserved for people and music classes, as well as art education. The School of with mental disabilities and those with physical disabilities Culture and Creative Arts also offers conducting services to Båtsfjord’s three choirs. In 2013, the school had more than 90 students • There is also an upper secondary school (high school) in Båtsfjord Båtsfjord, the fishing capital of Norway FisHiNg ANd THe FisHiNg iNdusTry Are THe priMAry sOurCe OF income iN BåTsFjOrd, ClOsely FOllOWed By lArge regiONAl compANies ANd OrgANisatiONs iN THe serviCe sector AFFiliated WiTH THe FisHeries ANd FisHiNg iNdusTry. THe total NuMBer OF BåTsFjOrd boats regisTered iN THe vessel regisTer iN 2013 was 54, consisTiNg OF both lArge ANd sMAll vessels. Active innovator Wide range and comprehensive services Numerous exciting and innovative new businesses have been The service sector in Båtsfjord is large and varied. It includes: Ship established in the municipality. Various projects have resulted in electronics, fishing equipment shops, maritime mechanical work- permanent jobs and growth in the community in recent years. The shop, laboratory services, bunkering facilities, bank, car repair shop, municipal department of commerce and industry actively contributes petrol stations, numerous speciality shops (clothing, tools, construc- to facilitating the establishment of new companies and is a driving tion materials, health food, handicrafts, sports equipment and force for increasing competence in the business community.The electronics), kiosks, supermarkets, restaurants, snack bars, a hotel Municipality of Båtsfjord makes resources available and provides and overnight accommodations. loans from its business development and fishing fund on a regular basis. Community work The Båtsfjord Handelstands Fiskerigruppe is an active association Cornerstone companies established in 1946 for the business community and fishing industry. Our two largest cornerstone companies are Norway Seafoods AS, It works to promote the interests of the members of the business Båtsfjord division, and AS Båtsfjordbruket, with a total of approxi- community, while at the same time ensuring that Båtsfjord is, and mately 200 employees. Both are important contributors to the will continue to be, a complete society that meets all the needs of its local community. They produce around 150 000 individual meals residents and the business community. The association has been an every day. invaluable support for the Municipality of Båtsfjord, as well as for sports and culture in the municipality. Several of the companies in the construction, factory and electrical sector are among the largest in the region. The five largest As a result, Båtsfjord has a very high GDP per capita. companies in Båtsfjord achieved a turnover of around NOK 100 millions in 2012. Wild, unique and beautiful BÅTSFJORD HAS UNIQUE NATURE AND A WIDE RANGE OF SIGHTS TO SEE. THE MUNICIPALITY IS LOCATED ON THE BEAUTIFUL VARANGER PENINSULA AND BORDERS DIRECTLY ON THE SOMETIMES WILD BARENTS SEA. HERE YOU CAN EXPERIENCE LOVELY SUMMER NIGHTS WITH THE MIDNIGHT SUN AND WINTERS FILLED WITH NORTHERN LIGHTS AND A VAST SNOwY LANDSCAPE. Magnificent nature wide range of species. Here you will find such rare arctic species as The municipality is surrounded by a landscape preservation area and the Svalbard poppy, Fringed Sandworts and the Svalbard snowy several nature reserves, as well as the Varanger Peninsula National cinquefoil. Large areas of the valley are nature reserves. There are Park, witch is 1804 and with an arctic high mountain landscape and numerous good hunting grounds in Syltefjord Valley, with the untouched, magnificent nature with unique flora and fauna. possibility to hunt both small game and moose. The Stauran bird cliff at the far end of Syltefjorden, stretching Makkaur 3 km and with cliffs over 220 metres high, is one of the largest bird Roadless Makkaur is located at the far end of Båtsfjorden. In the cliffs in Norway. Stauran is world famous for its diversity of past, it was one of the largest towns in the municipality and has kittiwakes, northern gannets, razorbills, white-breasted guillemots, been mentioned in documents dating back to the 1500s. Witch arctic guillemots, puffins and, of course, sea eagles. A colony of trials also took place here. The distinctive Makkaur Lighthouse, with around 250 grey seals also lives here. features of industrial architecture, was built in 1928 and was automated in 2005. Båtsfjord The area surrounding Båtsfjord has numerous marked hiking trails Hamningberg and excursion destinations, including two illuminated trails. Ski trails With its numerous pre-war buildings and structures dating back to are also groomed during the winter. Nordskogen and Båtsfjord Valley the 1700s, Hamningberg is unique in Finnmark, as large areas of the are used for recreation and other activities all year round. region were burnt to the ground during World War II. Today, it is very popular with locals and cabin owners all year round. Syltefjordelva During the summer, it is teeming with crowds from both Norway and This river is 30 kilometres long and one of the best salmon rivers in the rest of the world. The road to Hamningberg is a unique attraction Finnmark. and a designated National Tourist Road. During the peak year of 2012, close to 5.5 tons of salmon were fished from this river, the largest weighing 24 kilos. Varanger Peninsula National Park This national park was established in 2006 and is 1804 square Syltefjord Valley kilometres in size. It was established to protect the unspoilt nature of One of the world’s northernmost birch forests, which covers the the area and is virtually free of human intervention. This is the most bottom of the lower part of the Syltefjord Valley. Of botanical arctic part of continental Norway, with its distinctive landforms and interest is the tall perennial vegetation in the birch forest and, of deposits from the last ice age. Here you will find flora and fauna with course, the calcareous grounds in many of the narrow and south eastern and arctic characteristics. The national park is a central area facing side valleys on the north side of the main valley and home to a for the arctic fox and unique Sami cultural sites. lots of organised activities BåTsFjOrd HAs A Wide rANge OF OrgANisatiONs devoted to CulTure, spOrTs, HeAlTH, reCreatiON ANd NuMerOus resideNTs’ AssOCiatiONs. There are numerous and varied leisure activities, including football, shooting, horseback riding, music and singing. If there is a desire to further develop an existing organisation or start a new activity, the Båtsfjord Volunteer Office can provide the necessary assistance. excellent facilities Almost all types of recreational facilities can be found in Båtsfjord. This includes 100 and 300 metre shooting ranges, an indoor riding arena, motocross track, illuminated ski trails, biathlon facilities, good swimming facilities, a new artificial grass pitch and a multi-purpose sports centre. Båtsfjord sports Club This is the largest club in Båtsfjord and is an umbrella organisation for badminton, football, cycling, swimming, wrestling and skiing/ biathlon. The club has around 500 members. events in Båtsfjord • The Midnight Ski Race for Women is held the first weekend of May each year and has been organised for more than 20 years, having about 600-700 participants in the best years • The Båtsfjordmessa is organised during the first half of June and attracts exhibitors with much to offer from far and wide • «Båtsfjord i Fest» is held the last week in July and offers numerous cultural experiences. The festival is a meeting place for the people of Båtsfjord and is a lively event.
Recommended publications
  • Bird Report for the Varanger Peninsula 7-13 March 2013
    Bird report for the Varanger Peninsula, Norway, 7-13 March 2013 Authors: Gitte Kruse Allan Kruse Aoi Bringsøe Henrik Bringsøe – DOF Køge (Danish Ornithological Society, Køge regional group) Photos: Henrik Bringsøe Introduction We had three main reasons for going to the Varanger Peninsula in the far north-east of Norway in March 2013. We wished to see the: King Eider Steller’s Eider Northern lights (or aurora borealis) The two ducks and several other species will winter at Varanger which is always ice-free because of the warm water moves of the Gulf Stream. The ice-free conditions attract ducks from Siberia and other north-eastern areas to spend the winter there. For our journey we chose a period of the very early phase of the new moon (7%). The moon was only visible at daytime which meant that the nights were as dark as possible. As it was close to the equinox, the days were not too short (sunrise at 5:50, sunset at 16:35). Other bird groups were also given high priority, i.e. gulls, eagles and tits. Had we made our journey in April it would not have been possible to see King Eider although there would be less snow in April and it would be easier to get around. Gitte and Allan were responsible for the overall travel plans as they had visited Varanger in June 2010 and gained valuable experience. They booked accommodation at Mr. Øyvind Artnzen in Vadsø in September 2012 and bought flight tickets to Kirkenes. For their homeward journey they chose the coastal service Hurtigruten from Kirkenes to Tromsø and then a flight to Copenhagen.
    [Show full text]
  • The Concept of Cryo-Conditioning in Landscape Evolution
    Quaternary Research 75 (2011) 378–384 Contents lists available at ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres The concept of cryo-conditioning in landscape evolution Ivar Berthling a,⁎, Bernd Etzelmüller b a Department of Geography, Norwegian University of Science and Technology, Norway b Department of Geosciences, University of Oslo, Norway article info abstract Article history: Recent accounts suggest that periglacial processes are unimportant for large-scale landscape evolution and Received 15 December 2010 that true large-scale periglacial landscapes are rare or non-existent. The lack of a large-scale topographical Available online 17 January 2011 fingerprint due to periglacial processes may be considered of little relevance, as linear process–landscape development relationships rarely can be substantiated. Instead, periglacial landscapes may be classified in Keywords: terms of specific landform associations. We propose “cryo-conditioning”,defined as the interaction of cryotic Periglacial surface and subsurface thermal regimes and geomorphic processes, as an overarching concept linking landform Periglacial geomorphology Landscape and landscape evolution in cold regions. By focusing on the controls on processes, this concept circumvents Landscape evolution scaling problems in interpreting long-term landscape evolution derived from short-term processes. It also Cryo-conditioning contributes to an unambiguous conceptualization of periglacial geomorphology. We propose that the Scale development of several key elements in the Norwegian geomorphic landscape can be explained in terms of Cryo-geomorphology cryo-conditioning. © 2010 University of Washington. Published by Elsevier Inc. All rights reserved. Introduction individual landforms that make up the landscape are or must be of the same scale as the landscape itself.
    [Show full text]
  • The Expert Mechanism on the Rights of Indigenous Peoples (EMRIP)
    The Expert Mechanism on the Rights of Indigenous Peoples (EMRIP) Your ref Our ref Date 18/2098-13 27 February 2019 The Expert Mechanism on the Rights of Indigenous Peoples (EMRIP) – Norway's contribution to the report focusing on recognition, reparation and reconciliation With reference to the letter of 20th November 2018 from the Office of the United Nations High Commissioner for Human Rights where we were invited to contribute to the report of the Expert Mechanism on recognition, reparation and reconciliation initiatives in the last 10 years. Development of the Norwegian Sami policy For centuries, the goal of Norwegian Sami policy was to assimilate the Sami into the Norwegian population. For instance Sami language was banned in schools. In 1997 the King, on behalf of the Norwegian Government, gave an official apology to the Sami people for the unjust treatment and assimilation policies. The Sami policy in Norway today is based on the recognition that the state of Norway was established on the territory of two peoples – the Norwegians and the Sami – and that both these peoples have the same right to develop their culture and language. Legislation and programmes have been established to strengthen Sami languages, culture, industries and society. As examples we will highlight the establishment of the Sámediggi (the Sami parliament in Norway) in 1989, the Procedures for Consultations between the State Authorities and Sámediggi of 11 May 2005 and the Sami Act. More information about these policies can be found in Norway's reports on the implementation of the ILO Convention No. 169 and relevant UN Conventions.
    [Show full text]
  • Diagenesis and Weathering of Quartzite at the Palaeic Surface on the Varanger Peninsula, Northern Norway
    NORWEGIAN JOURNAL OF GEOLOGY Diagenesis and weathering of quartzite at the Paleic surface 239 Diagenesis and weathering of quartzite at the palaeic surface on the Varanger Peninsula, northern Norway Jakob Fjellanger & Johan Petter Nystuen Fjellanger, J. & Nystuen, J. P. Weathering of quartzite at the palaeic surface on the Varanger Peninsula, northern Norway. Norwegian Journal of Geology, Vol. 87, pp. 133-145.Trondheim 2007. ISSN 029-196X. Weathered zones in quartzitic bedrock on the Hak alancˇearru Mountain on the Varanger Peninsula, northern Norway, have been examined, as has the timing of their development. The weathered zones are mainly associated with fractures formed by tectonic shear. SEM, microprobe and thin section studies reveal features belonging to the diagenesis and weathering history of the rock. Flakes of phyllosilicate minerals were originally depo- sited together with the quartz sand and became attached as coatings to the surface of individual quartz grains as well as forming an intergranular fill. Some of the detrital clay minerals turned into kaolinite during an early stage of the burial diagenesis. Kaolinite was later partly transformed to dickite. Quartz dissolution with concomitant quartz cementation and illite formation took place during later burial diagenesis. The kaolinite occurs in intergranular voids where it was partly transformed to pyrophyllite at a peak temperature of about 300 ˚C. As the overlying rocks were eroded the previously formed tectonic joints and small faults enhanced the circulation of ground water. This facilitated chemical weathering along joints and nearby grain contacts where slight dissolution of quartz significantly weakened inter-granular bonds. The resulting increase in permeability facilita- ted recent disintegration of the quartzite by mechanical processes.
    [Show full text]
  • VARANGER – ARCTIC NORWAY Thursday 26Th May to Thursday 2Nd June 2016
    VARANGER – ARCTIC NORWAY Thursday 26th May to Thursday 2nd June 2016 TOUR OVERVIEW The Varanger peninsula offers some of the best bird watching in the world, and to couple this with stunning landscapes and seascapes within the Arctic Circle, a visit to this iconic destination becomes irresistible to both birders and nature lovers. By late May the spring thaw is in full swing and bird activity is at its height. Migrant waders and waterfowl moving further into the arctic congregate in large flocks competing for food with locally breeding Temminck’s Stint and Red-necked Phalarope. The sheltered bays host sea duck and divers a plenty, whilst offshore large seabird colonies can be approached by boat giving access to the much sought after Brunnich’s Guillemot. Nearby the open tundra is home to Long-tailed Skuas, Rough-legged Buzzards, Snow and Lapland Buntings plus the exquisite Red- throated Pipit. As if this was not enough, Varanger is an incredibly scenic place to visit with an appeal amplified by it being the last true wilderness in Europe. Furthermore avian rarities such as White-billed Diver and both King and Steller’s Eider can linger well into June bringing further interest. The area is home to Reindeer and Elk who eak a living from the bleak but beautiful tundra landscape. Wild flowers include a number of orchids, and some will be in bloom bringing a blessing of colour to the stark fell and rock slopes. PHOTOGRAPHIC OPPORTUNITIES: The Varanger peninsula is home to abundant wildlife, in particular birds, and many of the species approach closely.
    [Show full text]
  • Birding Abroad Limited Northern Norway – Early
    BIRDING ABROAD LIMITED NORTHERN NORWAY – EARLY SPRING IN THE ARCTIC CIRCLE 12 - 18 MARCH 2020 TOUR OVERVIEW: The Varanger Peninsula in northern Norway offers some of the finest and most accessible Arctic bird watching in the world. Situated within the Arctic Circle, it is a land adorned with stunning landscapes and seascapes; an iconic destination irresistible to globe-trotting bird watchers and nature lovers alike. By March, with the spring equinox approaching, days will have lengthened significantly, and the early spring sunlight casts a dazzling aura over the tundra, fiords and forests. Bird activity will already be in full swing. Sheltered bays are largely ice-free due to the influence of the Gulf Stream, and these host sea duck a plenty, including colourful and resplendent Steller’s and King Eiders. Offshore, large seabird colonies can be approached by boat, giving access to the much sought after Brunnich’s Guillemot. Nearby the open Arctic tundra is still frozen but resident Willow Grouse and Rock Ptarmigan tough it out on the stark fells, ideally adapted to this challenging environment. The area is also home to Reindeer and Elk, both eking a living from their bleak but beautiful surroundings and with luck some sea mammals might additionally be seen. Just south of the Arctic tundra, the Pasvik valley is a patchwork of ancient woodland, bogs and lakes, which forms the most north-western corner of the great Siberian taiga forest. Amongst many great birds, this is home to the stunning Northern Hawk-owl. Here too several keenly sought-after northern species can be found, including Siberian Jay, Siberian Tit and Pine Grosbeak, which often show very confidingly at feeders provided by local residents.
    [Show full text]
  • Varanger Berlevåg
    VARANGER BERLEVÅG BIRDING DESTINATION KONGSFJORD Varanger is the worlds easiest accessible arctic birding destination. In Varanger you Syltefjord- HAMNINGBERG have the northern taiga, tundra and arctic coastline in one destination. Within a 7 stauran days drive you can experience the pine grosbeaks in the taiga, and se a wide variety 8 BÅTSFJORD SANDFJORDEN of species on the tundra of the Varanger peninsula. At the coastal bird cliffs the SYLTEFJORDEN arctic species Brünnichs Guillemot is accompanied by a hundred thousand seabirds. PERSFJORDEN HORNØYA The summer is a hectic season with 24 hour daylight and birds in beautiful breeding VARDØ plumage. In winter and early spring arctic seaducks concentrate in huge rafts, and 6 at night the Aurora borealis completes the experience. At the northern edge of Barvikmyra Europe, further east then Istansbul, the Gulf stream keeps the Varanger fjord ice free. It is the only fjord in Norway facing the east, and the shallow waters provide feeding grounds for great numbers of birds. GEDJNE KIBERG KRAMVIK 9 HØYHOLMEN VARANGER 700 NORTH 300 EAST 100% BIRDING KOMAGVÆR AUSTER- TANA SKALLELV Eider raft Hurtigruten / Coastal Express 5 VESTRE VADSØ EKKERØY JAKOBSELV MESKELV NESSEBY 4 VARANGERBOTN 1 2 3 VADSØYA TANA BRU VARANGERFJORDEN KARLEBOTN BUGØYNES Puffin fight club Varangerbotn: Tidal landscape & deciduous forest, Sylefjordstauran: Bird cliff, Gannets, White- 1 waders, ducks, Arctic Warbler, Siberian Tit. 7 tailed Eagles, Kittiwakes. Nesseby: Tidal landscape, waders, ducks, sea- Båtsfjord, Kongsfjord, Berlevåg: King Eider, 2 watching (petrels, etc on easterly winds). 8 Steller´s Eider (seaduck photo hide Feb-Apr), seawatching, White- Vestre Jakobselv: Siberian Tit, Arcitc Redpoll, tailed Eagles, Dotterel at Gednje.
    [Show full text]
  • Integrated Planning of National Parks and Adjacent Areas – Possibilities and Limits in Cooperation for Nature-Based Tourism and Place Making
    6th Symposium Conference Volume for Research in Protected Areas pages 633 - 635 2 to 3 November 2017, Salzburg Integrated planning of national parks and adjacent areas – possibilities and limits in cooperation for nature-based tourism and place making Knut Bjørn Stokke & Morten Clemetsen Abstract In Norway, there have traditionally been a segregated approach to management of national parks, focusing on protecting nature from human activities. However, in recent years, we have seen tendencies toward a more integrative approach, focusing on integration of nature based tourism, place making and nature conservation. The aim for this paper is to highlight some preliminary results, based on an ongoing research from the Varanger Peninsula National Park and its adjacent areas in the far north of the Norwegian mainland. Key words National park management, local planning, network arrangements, nature-based tourism, place making Introduction Nature conservation are taking new directions in several countries, where protected areas are increasingly being viewed in a wider regional context (MOSE 2007; HAMMER et al. 2012), i.e. as a tool for tourism development and place-making. HAMMER et al. (2016:19) emphasis that the majority of European parks today ‘are no longer nature reserves but have the character of living or working landscapes’. To a certain extent, the Norwegian nature protection policy has also been undergoing similar changes in recent years (HAUKELAND et al. 2013). In Norway, the management responsibility for a number of national parks and other large protected areas has since 2010 been delegated from the County Governor (the state representative in the Norwegian counties) to inter-municipal boards.
    [Show full text]
  • Late Precambrian Sedimentary Rocks, E. Finnmark, and the Trollf!'Ord-Komagelv Fault 533
    Late Precambrian sedimentary rocks, E. Finnmark, and the Trollf!'ord-Komagelv Fault 533 1972b. The stratigraphy and sedimentology of the Smog, A. 1972. Kongsfjord Formation---a late Pre- Lakesfjord Group, Finnmark. Norg. geol. Unders. 278, cambrian flysch sequence from the Varanger Peninsula, 13-40. Finnmark. Norg. geol. Unders. 2"/8, 41-80. Imvm.t., B. K. & ROBERTS, D. 1977. A re-investigation of 1973. The late Precambrian IDst-Finnmark the geology of north-west Varanger Peninsula, East Supergroup--a new lithostratigraphic unit of high rank. Finnmark, north Norway. Norg. geol. Unders. 334, 83- Norg. geol. Unders. 2,119, 55-60. 90. 1975. Late Precambrian stratigraphy and structure of PRICE, N. J. 1968. A dynamic mechanism for the develop- the north-eastern margin of the Fennoscandian Shield ment of second order faults and related structures. Proc. (East Finnmark-Timan Region). Norg. geol. Unders. of Conf. on Research in Tectonics (Kink bands and brittle 316, 313-48. deformation) Ottawa 1968. Geol. Surv. Can. 68-52, & SIEDLECra, S. 1967. Some new aspects of the geology 49-72. of Varanger Peninsula (northern Norway). Norg. geol. PR~GLE, R. 1972. Rb-Sr age determinations on shales as- Unders. 2,47, 288-306. sociated with the Varanger Ice Age. Geol. Mag. 109, & 1971. Late Precambrian sedimentary rocks of 465-72. the Tanafjord-Varangerfjord region of Varanger Penin- RAMSAY, D. M. 1973. Possible existence of a stillborn margi- sula, northern Norway. Norg. geol. Unders. 269, 246-94. nal ocean in the Caledonian orogenic belt of northwest & 1972. Lithostratigraphic correlation and Norway. Nature, Phys. Sci. 245, 107-9.
    [Show full text]
  • New Aspects of Deglaciation in Southern Norway
    New aspects of deglaciation in southern Norway Climate variability derived from surface exposure ages of Late Quaternary and Holocene landforms Dissertation zur Erlangung des Doktorgrades Dr. rer. nat. der Mathematisch-Naturwissenschaftlichen Fakultät der Rheinischen Friedrich-Wilhelms-Universität Bonn Bonn, September 2019 Vorgelegt von Philipp Marr aus Kronach Angefertigt mit Genehmigung der Mathematisch-Naturwissenschaftlichen Fakultät der Rheinischen Friedrich-Wilhelms-Universität Bonn 1. Gutachter: Prof. Dr. Jörg Löffler Geographisches Institut, Rheinische Friedrich-Wilhelms-Universität Bonn 2. Gutachter: Prof. Dr. Lothar Schrott Geographisches Institut, Rheinische Friedrich-Wilhelms-Universität Bonn Tag der mündlichen Prüfung: 29. Januar 2020 Erscheinungsjahr: 2020 New aspects of deglaciation in southern Norway Abstract Abstract The investigation of periglacial and related landforms in South Norway is of high interest for exploring timings of deglaciation and to assess their geomorphological connectivity to palaeoclimatic changes during the Late Quaternary and the Holocene. The ice margins of the Scandinavian Ice Sheet during the Last Glacial Maximum (LGM) are fairly well known, the palaeo-ice thickness, however, which can only be esti- mated by modelling, remains unclear over large parts of Norway owing to rare field based evidences. Due to the significant influence of the former horizontal and vertical ice-sheet extent on sea-level rise, atmos- pheric and oceanic circulation patterns, erosive properties of glaciers and ice sheets, englacial thermal boundaries and deglaciation dynamics, it is crucial to better understand the topographic features of the LGM ice sheet. Despite recent advances, there is a lack of terrestrial evidences from numerical data in South Norway. In this thesis two high-mountain regions and their surroundings in west (Dalsnibba, 1476 m a.s.l.) and east (Blåhø, 1617 m a.s.l.) South Norway were used to reconstruct palaeoclimatic conditions and degla- ciation patterns.
    [Show full text]
  • The Bedrock Geology of Varanger Peninsula, Finnmark, North Norway: Norges Geologiske Undersøkelse an Excursion Guide
    THE BEDROCK GEOLOGY OF VARANGER PENINSULA, FINNMARK, NORTH NORWAY: NORGES GEOLOGISKE UNDERSØKELSE AN EXCURSION GUIDE Anna Siedlecka & David Roberts Special Publication 5 The NGU Special Publications series comprises consecutively numbered volumes containing papers and proceedings from national and international symposia or meetings dealing with Norwegian and international geology, geophysics and geochemistry; excursion guides from such symposia or from international collaborative projects; and in some cases collections of thematic articles. The language of the Special Publications series is English. Editor: Forsker dr. philos. David Roberts © 1992 Norges geologiske undersøkelse Published by Norges geologiske undersøkelse (Geological Survey of Norway) PO Box 3006 - Lade 7002 Trondheim Norway All rights reserved ISSN: 0801-5961 ISBN: 82-7385-085-4 Printed by: Bjærum as Cover illustration: View towards the north from Ruossabak'ti on the eastern side of the Tana river.ln the forground, from the left: Gamasfjellet Formation, Smalfjord Formation (tillite - the thick, pale brown unit) and Nyborg Formation. In the middle-ground to the right, Raudberget Mt. (Gamasfjellet Formation) and to the left the delta of the Tana river. In the background from the left to right: rocks of the Tanafjorden Group with Stangenestind, 725 m a.s.L, the highest point on the Varanger Peninsula; below, along the shore, the Vagge Section - the type section of the Tanafjorden Group. Photo: Anna Siedlecka. The bedrock geology of Varanger Peninsula, Finnmark, North Norway: an excursion guide NORGES GEOLOGISKE UNDERSØKELSE SPECIAL PUBLICATION NO. 5 The bedrock geology of Varanger Peninsula, Finnmark, North Norway: an excursion guide ANNA SIEDLECKA & DAVID ROBERTS H Nasjonalbiblioteket Depotbiblioteket Anna Siedlecka & David Roberts, Norges geologiske undersøkelse, Post Box 3006 - Lade, 7002 Trondheim, Norway.
    [Show full text]
  • The Expeditio Litteraria Ad Polum Arcticum
    Chapter 5 He Came, He Saw, He Conquered?: The Expeditio litteraria ad Polum Arcticum In these northern regions, so rarely visited and so little explored, everything is of interest, and Father Hell studied everything. jérôme de lalande1 ∵ To commission a high-quality, internationally respected astronomical observa- tion and thus restore Denmark’s dwindling fame as a “nation of astronomy” was no doubt the chief ambition of Hell’s sponsors. In the very first letter from Foreign Minister Bernstorff to his Viennese envoy, the only explicit aim of the expedition is observation of the transit of Venus from Vardø.2 Although the expedition’s timeframe expanded significantly, with the departure from Vien- na finally set more than a year ahead of the astronomical event, there is no evi- dence in the ensuing diplomatic correspondence between Vienna and Copen- hagen to suggest that Denmark–Norway was preparing to support a wholescale encyclopedic expedition entailing years of exploration and voluminous publi- cations.3 Such plans, however, soon took form in Hell’s mind. Besides bending to God’s will, Hell must have been all too aware that to the Republic of Letters the region in question was still virtually a terra incognita. It was exotic and “liminal,” with the aurora borealis, polar night, and midnight sun, along with extreme weather and natural dangers such as the maelstrom of Moskenes, and above all the indigenous Sámi (Saami, Sami) population—known in those days as “Lapps”—forming intriguing objects of study with a broad popular ap- peal.4 The Lapland voyages of Linnaeus and Maupertuis in the 1730s had 1 Jérôme de Lalande, Bibliographie astronomique avec l’histoire de l’astronomie depuis 1781 jusqu’à 1802 (Paris: Imprimerie de la République, 1803), 721.
    [Show full text]