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The Art of Survey of the Earth from Finnmark Expeditions in Finnmark for «Struve's Geodetic Arc» 1845-1850
Gerd Johanne Valen 2016 The Art of Survey of the Earth from Finnmark Expeditions in Finnmark for «Struve's geodetic arc» 1845-1850. Written by Gerd Johanne Valen 2016. Struve's geodetic arc was added to Unesco’s list of the world’s natural and cultural heritage in 2005. The geodetic arc was measured from 1816 to 1852. It was the first accurate measurement of a long geodetic arc which made it possible to calculate the earth's size and shape. It was also the longest and northernmost geodetic arc in the 1800s. The co-operation between prominent surveyors, geodesists and monarchs characterized the story of this world heritage. Less well known is an account of the surveyors' seasonal fieldwork in West Finnmark from 1845 to 1850. What were the major challenges? How did they use the landscape of West Finnmark to measure a chain of triangles and a series of measurements from Hammerfest to the Black Sea? This article will mainly look closer to the story we can read from the fieldworks logbooks. The World Heritage Struve's geodetic arc was named after Fredrik Georg Wilhelm Struve (17931864), who was a professor of mathematics and astronomy in today`s Tartu in Estonia. He was responsible for the triangulation in Livland, which was a part of Russia. In 1820 Struve put forward a suggestion to the authorities to carry out a chain of survey triangulation in the Baltic region. He argued that this work would have great scientific value and would also be important for mapping the country. The military surveyor Carl Tenner was engaged in surveying work in Lithuania. -
Studies on the Latest Precambrian and Eocambrian Rocks in Norway
NORGES GEOLOGISKE UNDERSØKELSE NR. 251 Studies on the latest Precambrian and Eocambrian Rocks in Norway No. 3. Latest Precambrian and Eocambrian Stratigraphy of Norway By K. Bjørlykke, J. O. Englund and L. A. Kirkhusmo No. 4. The Eocambrian "Reusch moraine" at Bigganjargga and the Geology around Varangerfjord; Northern Norway By Knut Bjørlykke No. 5. Microfossils from late Precambrian sediments around lake Mjøsa, Southern Norway By Svein Manum No. 6. Fossils from pebbles in the Biskopåsen Formation in Southern Norway By Nils Spjeldnæs No. 7. Eocambrian rocks on the north-west border of the Trondheim basin Ly J. Springer Peacey No. 8. Stratigraphy and structure of Eocambrian and younger deposits in a part of the Gudbrandsdal valley district, South Norway By Trygve Strand OSLO 1967 UNIVERSITETSFORLAGET STATENS TEKNQLQBISaE INSTITUTT BIBLIOTEKET Contents Illest krecamlirian and Locainiirian Ztracizrapn^ of Norway by K. Lj^rlxkke, J. O. Englund and L. A. Kirkhusmo 5 The Eocambrian «Reusch moraine» at Bigganjargga and the Geology around Va rangerfjord; Northern Norway by Knut Bjørlykke 18 Microfossils from late Precambrian sediments around lake Mjøsa, Southern Norway fZ by Svein Manum 45 se I 1055i1z from pebbleB in the Biskopåsen Formation in Southern Norway by Nils Spjeldnæs 53 3 o Eocambrian rocks on the north-west border of the Trondheim basin by J. Springer Peacey 83 g » m Stratigraphy and structure of Eocambrian and younger deposits in a part of the Gudbrandsdal valley district, South Norway by Trygve Strand 93 co STUDIES ON THE LATEST PRECAMBRIAN AND EOCAMBRIAN ROCKS IN NORWAY No. 3. LATEST PRECAMBRIAN AND EOCAMBRIAN Biil^iittie^rnr OF NORWAY By K. -
Our. Knowledge of the Geology of the Alta District of West Finnmark Owes Much to the Work of Holtedahl (1918, 1960) and Føyn (1964)
Correlation of Autochthonous Stratigraphical Sequences in the Alta-Repparfjord Region, West Finnmark DAVID ROBERTS & EIGILL FARETH Roberts, D. & Fareth, E.: Correlation of autochthonous stratigraphical se quences in the Alta-Repparfjord region, west Finnmark. Norsk Geologisk Tidsskrift, Vol. 54, pp. 123-129. Oslo 1974. An outline of the geology of the area between Alta and the Komagfjord tectonic window is presented. Lithologies (including a tillite) constituting an autochthonous sequence are described from an area on the north-east side of Altafjord, and from their similarity to those of formations occurring in adjacent areas a revised regional stratigraphical correlation is proposed. An occurrence of biogenic structures appears to provide confirmatory evidence for an earlier suggested correlation with Late Precambrian sequences be tween west and east Finnmark. D. Roberts & E. Fareth, Norges Geologiske Undersøkelse, Postboks 3006, 7001 Trondheim, Norway. Regional setting; previous correlations Our. knowledge of the geology of the Alta district of west Finnmark owes much to the work of Holtedahl (1918, 1960) and Føyn (1964). The oldest rocks, the Raipas Group or Series (Reitan 1963a) of Precambrian (Karelian) age, are represented by a sequence of greenschist facies metasediments, metavolcanics and intrusives. Lying unconformably upon the Raipas is a quartzite formation, a thin tillite, and a mixed shale and sandstone succession. Holtedahl (1918) re ferred to these autochthonous post-Raipas rocks as the 'Bossekopavdelingen', but Føyn (1964) later demonstrated the presence of an angular uncon formity beneath the tillite and adopted this break as the border between what he termed the Bossekop Group and the overlying sediments, the Borras Group. These were later referred to as sub-groups (Føyn 1967, Pl. -
Komsa Dokumentasjonsvedlegg
DOKUMENTASJONSVEDLEGG § 19 FREDNING, KOMSA, ALTA, FINNMARK Reidun Laura Andreassen 1 1. Kvartærgeologi i Indre Altafjord Etter siste istid, for ca 10 000 år siden lå isfronten innerst i fjordene i Finnmark. Vekten av isen presset landet ned, men da avsmeltningen begynte og breens vekt minket, hevet landet seg igjen. Den enorme mengden smeltevann førte imidlertid til at havet steg, og i enkelte perioder var landhevningen og havstigningen like stor. Trykket av isen var imidlertid størst lengst inn mot bresenteret, i det indre av den Skandinaviske halvøya, og avtok gradvis ut mot kysten hvor breen var tynnest. Derfor hevet landet seg mer i de indre fjordstrøk enn ute ved kysten. Den marine grense i det indre av Altafjorden ligger på ca. 75m over dagens havnivå hvor havet stod for ca 10 000 år siden. Havet stod i flere perioder og vasket innover land, noe som førte til dannelsen av markerte strandterrasser som viser hvor havet en gang har stått. Oppover hele Altadalen ser vi merker etter havnivåene til enhver tid. Det er en generell arkeologisk oppfatning at bosetningen er knyttet til stranden, og at en derfor kan relatere boplasser til kronologi ut fra hvor høyt over havet de ligger. Kartene nedfor viser hvordan landskapet i indre Altafjord har endret seg gjennom tid i forhold til endring av havnivået. Som en ser av kartene var Komsa ei øy som gradvis ble landfast fra isens avsmeltning for ca. 10 000 år siden og helt fram til for ca 5-6000 år siden. 9 000 år siden 5500 år siden dagens havnivå 70 m.o.h 25 m.o.h Figur 1 Kartframstilling av havnivå fra forskjellige perioder. -
Lacewings (Neuroptera) and Alderflies (Megaloptera) from Finnmark, Northern Norway
© Norwegian Journal of Entomology. 5 December 2012 Lacewings (Neuroptera) and Alderflies (Megaloptera) from Finnmark, northern Norway LITA GREVE & TROND ANDERSEN Greve, L. & Andersen, T. 2012. Lacewings (Neuroptera) and Alderflies (Megaloptera) from Finnmark, northern Norway. Norwegian Journal of Entomology 59, 122–132. Records of 22 species of Neuroptera and four species of Megaloptera from Finnmark, northern Norway are presented based partly on material collected in 2010, partly on material housed in the entomological collections at the Natural History museums in Norway. Of these, 13 species have previously not been recorded from Finnmark, i.e.: Coniopteryx tineiformis Curtis, 1834; Hemerobius atrifrons McLachlan, 1868; H. fenestratus Tjeder, 1932; H. humulinus Linnaeus, 1758; H. marginatus Stephens, 1836; H. nitidulus Fabricius, 1777; H. pini Stephens, 1836; Micromus angulatus (Stephens, 1836); Sympherobius fuscescens (Wallengren, 1863); Wesmaelius concinnus (Stephens, 1836); W. mortoni (McLachlan, 1899); W. quadrifasciatus (Reuter, 1894) and Chrysoperla carnea (Stephens, 1836). The total number of Neuroptera known to occur in Finnmark is now 23 of which four belong in the family Coniopterygidae, 17 in Hemerobidae, and one in each of the families Chrysopidae and Sisyridae. All four species of Megaloptera reported in this paper belong to the genus Sialis Latreille, 1802, the sole genus of the order occurring in Norway. One of these, Sialis sibirica McLachlan, 1872, is recorded as Data Deficient (DD) in the 2010 Norwegian Red List for Species. In addition to the four species reported here a fifth species,Sialis lutaria (Linnaeus, 1758) is known to occur in Finnmark. Key words: Neuroptera, Megaloptera, distribution, Finnmark, Norway. Lita Greve & Trond Andersen, Department of Natural History, University Museum of Bergen, University of Bergen, P.O. -
Årsmelding 2015 Foto: Siv J
Årsmelding 2015 Foto: Siv J. Suhr Foto: www.altajff.no Miljøavdelingen Tlf. 78 45 50 00 Postboks 1403, 9506 Alta http://www.alta.kommune.no/ Miljøavdelingen – en viktig adresse i natur- og miljøforvaltningen. • Faglige råd om naturbruk • Fiskekultivering og tilrettelegging • Friluftsliv • Nærgående elg i tettstedet og skadet vilt m.m. • Motorferdsel i utmark • Forurensning En god forvaltning er avhengig av innspill fra dere som er friluftsfolk, jegere og fiskere. Har dere spørsmål eller klare meninger om utmarksforvaltningen i Alta kommune, ta kontakt med oss. FOTO: LARS H. KREMPIG H. LARS FOTO: Jon Håvar Haukland, avd.leder Amund Heitmann Suhr, naturforvalter Miljøavdelingen Innkalling til årsmøte Tlf. 78 45 50 00 Sted: Klubbhuset til Alta jeger- og fiskerforening på Kvenvikmoen Postboks 1403, 9506 Alta http://www.alta.kommune.no/ Tid: Torsdag 25. februar 2016 kl. 18.00 Miljøavdelingen – en viktig adresse i SAKSLISTE: 3 1. Konstituering av møtet natur- og miljøforvaltningen. - Godkjenning av innkalling - Godkjenning av dagsorden • Faglige råd om naturbruk - Godkjenning av forretningsorden Har du • Fiskekultivering og tilrettelegging - Valg av ordstyrer • Friluftsliv - Valg av protokollfører husket å fornye • Nærgående elg i tettstedet og skadet vilt - Valg av tellekorps medlemskapet m.m. - Valg av to medlemmer til å underskrive protokoll ditt? • Motorferdsel i utmark 2. Årsmelding fra siste kalenderår • Forurensning 3. Revidert regnskap siste kalenderår 4. Innkomne saker med styrets forslag til vedtak En god forvaltning er avhengig av innspill fra 5. Forslag om vedtektsendringer: husutvalget dere som er friluftsfolk, jegere og fiskere. 6. Styrets forslag til arbeidsprogram 7. Styrets forslag til budsjett Har dere spørsmål eller klare meninger 8. Foreningens kontingentandel for 2017 om utmarksforvaltningen i Alta kommune, 9. -
Atlas of Airports
COMPOSMENT TYPOLOGY CONFIGURATION AIRFIELDS NORWAY Norwegian airports with more than 100 000 passengers This airport research combines selected airports that with a certain annual passengers in Norway. The methodology of juxtaposition, the analysis of Terminals, Runway, Airport cities patterns as well as configuration, spatial, morphology, forms, which serve as a base-data for airport design. TYPOLOGY OF AIRPORTS - NORWAY SELECTED AIRPORT ANALYSIS & STUDY con- tent Oslo 3 Bergen 5 Stavanger 7 Trondheim 9 Tromsø 11 Sandefjord 13 Bodø 15 Kristiansand 17 Ålesund 19 Haugesund 21 Narvik and Harstad (Evenes Airport) 23 Alta 25 VMolde 27 Kristiansund 29 Kirkenes 31 Bardufoss 33 Hammerfest 35 Longyearbyen, Svalbard 37 Florø 39 Stokmarknes 41 Mo i Rana 43 Runway 45 Configuration 47 Airport cities 49 Terminals 51 OSL 60°12’10’’N 011°05’02’’E Airport type Public Operator Oslo Lufthavn AS Serves Oslo, Norway Location Gardermoen, Ullensaker, Akershus Runways 3,600/2,950 Passengers 25,788,610 International 14,567,406 Domestic 11,221,204 Aircraft movements 237,618 Cargo (tonnes) 130,301 3 OSL RUNWAY TERMINAL AIRPORT CITY STRUCTURE 1 AIRPORT CITY PATTERN TRANSFER AIRPORT CITY PATTERN The first airports to serve Oslo was Kjeller Airport that opened in 1912 and Gressholmen Airport that served seaplanes after its opening in 1926. The airport location was first used by the Norwegian Army from 1940, with the first military airport facilities being built during the 1940s. An expansion with a new terminal building and a third pier is scheduled to open in 2017.Oslo Airport is the largest and busiest of three major international airports located around Oslo. -
Read the Report
REPORT NO 1804 | Svein Bråthen, Karoline L. Hoff, Lage Lyche and Hilde J. Svendsen ECONOMIC IMPACT ASSESSMENT OF THE NEW ICAO STANDARD FOR CONTAMINATED RUNWAYS A case study of four Norwegian airports 2 TITLE Economic impact a ssessment of the new ICAO standard for contaminated runways. A case study of four Norwegian airports. AUTHORS Svein Bråthen, Karoline L. Hoff, Lage Lyche, Hilde J. Svendsen PROJECT LEADER Svein Bråthen REPORT NO . 1804 PAGES 39 PROJECT NO. 2743 PROJEC T TITLE RWY Friction COMMISSIONED BY Avinor AS PUBLISHER Møreforsking Molde AS PLACE FOR PUBLISHING Molde YEAR 2018 ISSN 0806 -0789 ISBN (PRINTED ) 978 -82 -7830 -293 -4 ISBN (ELECTRONIC) 978-82-7830-294-1 DISTRIBUTION Molde University College , The Library, PO box 2110, N-6402 Molde, Norway Phone 71 21 41 61, e-mail: [email protected] www.moreforsk.no SHORT SUMMARY This is a summary of a case study of four Norwegian airports that are likely to be exposed to the impacts of ICAO State letter AN 4/1.2.26-16/19 regulations of minimum friction on contaminated runways, in terms of reduced regularity. The report assesses the economic effects for passengers and operators, in terms of additional costs. The new ICAO standard is suggested to maintain the existing high level of safety within aviation. This study does not discuss any economic benefits from imposing the new standard. The study assesses five scenarios: Scenario P1 and P2 assess an increase in airfares of 20 % and 50% respectively and the use of smaller aircraft to maintain regularity on today’s level. -
On the Traces of the Ice Ages in Nordland, Troms, and the South Western Part of Finnmark in Northern Norway
Ms. re c. May 18, l 938. ON THE TRACES OF THE ICE AGES IN NORDLAND, TROMS, AND THE SOUTH WESTERN PART OF FINNMARK IN NORTHERN NORWAY BY OLE T. GRØNLIE 18 TEKSTF!G. AND 5 PL. Introdu c ti on. In later years several authors have devoted a more or less close study to the quaternary geology of Northern Norway. In the first place are here to be mentioned TANNER 1930 (20) and NORDHAGEN 1933 and 1935 (14 and 15). The present author has also for many years been interested in quaternary geological problems and has in the course of time collected a varied material concerning these matters in that part of our country. On account of duties as a functionary I have had too little time for working out the material collected or the working has been so much retarded that something may have been forgotten and more or less lost when it was to be used. As it is the quaternary conditions of Northern Norway have at present got such an actuality that I find it appropriate to present a part of the material which I have been able to work out, and to take a preliminary view of the said problems. CONTENTS Page I. The Great lee Age . 2 Il. The Last lee Age . Il l. Stages of the ice border during the metting period . Il 2. The maximal thickness of the last in land ice . .... .... ......... .. 20 3. The evidences of fossils and living plants of a last ice age ........... 25 Ill. The Late Glacial Shore Lines . -
Alta Og Talvik Menighetsblad 02/2019
NR. 2 – 2019 En relevant kirke AV ROLF EDMUND LUND I skyggen av kommune- og fylkestings- valget forsøker kirka etter beste evne å skape blest om sitt eget skjøre demokrati for menighetsråd og bispedømmeråd. Om det ikke er en død hest som piskes hvert fjerde år, så er det i hvert fall en øvelse Rolf Edmund Lund, ansvarlig for spesielt interesserte. redaktør i Mediehuset Altaposten Det vil si; det er faktisk over 12.000 kandidater som synliggjør forskjellene mellom som stiller til valg rundt omkring i landet, med de ulike listene. Det er nok ufred i det de beste intensjoner om å påvirke sentrale ordinære valget, så det er ingen som spørsmål i kirkelivet, lokalt og nasjonalt. savner verbale sverdslag, men det er mer 110 menighetsråd og 11 bispedømmeråd et spørsmål om å betone hva de forskjellige skal settes sammen i løpet av høsten, alternativene innebærer. Det koker litt ned men mistanken er at personvalget teller til den pedagogiske utfordringen det er å langt mer enn sakskompleksene. Kanskje fange oppmerksomhet i en oppjaget tid, spesielt i menighetsrådene der det finnes der spesielt informasjonssamfunnet er nære relasjoner og kandidatene gjerne er overveldende. Frikoblet fra staten gjelder kjentfolk. Med sine verdier og kvaliteter. det kanskje å definere denne veien selv. Noen kaller det for det hemmelige valget, Det kan tenkes at vi i media ikke er flinke men jeg tror det er mer treffsikkert å bruke nok til å sette fokus på kirkevalget, rent det usynlige valget, all den tid kirka selv bortsett fra de mest kontroversielle sakene, ønsker og etterstreber både involvering, som eksempelvis spørsmålet om likekjønnet engasjement og oppslutning. -
The Art of Survey of the Earth from Finnmark Expeditions in Finnmark for «Struve's Geodetic Arc» 1845-1850
Gerd Johanne Valen 2016 The Art of Survey of the Earth from Finnmark Expeditions in Finnmark for «Struve's geodetic arc» 1845-1850. Written by Gerd Johanne Valen 2016. Struve's geodetic arc was added to Unesco’s list of the world’s natural and cultural heritage in 2005. The geodetic arc was measured from 1816 to 1852. It was the first accurate measurement of a long geodetic arc which made it possible to calculate the earth's size and shape. It was also the longest and northernmost geodetic arc in the 1800s. The co-operation between prominent surveyors, geodesists and monarchs characterized the story of this world heritage. Less well known is an account of the surveyors' seasonal fieldwork in West Finnmark from 1845 to 1850. What were the major challenges? How did they use the landscape of West Finnmark to measure a chain of triangles and a series of measurements from Hammerfest to the Black Sea? This article will mainly look closer to the story we can read from the fieldworks logbooks. The World Heritage Struve's geodetic arc was named after Fredrik Georg Wilhelm Struve (17931864), who was a professor of mathematics and astronomy in today`s Tartu in Estonia. He was responsible for the triangulation in Livland, which was a part of Russia. In 1820 Struve put forward a suggestion to the authorities to carry out a chain of survey triangulation in the Baltic region. He argued that this work would have great scientific value and would also be important for mapping the country. The military surveyor Carl Tenner was engaged in surveying work in Lithuania. -
Arctic Scandinavia Travel Routes
© Lonely Planet Publications 297 Arctic North Scandinavia Pole Travel Routes CONTENTS Getting Around 298 Itinerary 2: Northwest Itinerary 1: The Finland 326 Scandinavian North 299 Rovaniemi 327 Mo i Rana 301 Kittilä 327 Arctic Circle (Polarsirkelen) 302 Levi & Sirkka 327 Bodø 302 Kilpisjärvi 328 Lofoten 303 Essential Facts 328 Vesterålen 307 Dangers & Annoyances 328 Narvik 307 Further Reading 328 Riksgränsen 309 Money 328 Kiruna 309 Telephone 328 Gällivare 311 Time 329 Jokkmokk 312 Tourist Information 329 Luleå 312 Visas 329 Haparanda & Tornio 313 ARCTIC SCANDINAVIA ARCTIC SCANDINAVIA Rovaniemi 314 Napapiiri (The Arctic Circle) 316 ROUTES TRAVEL Sodankylä 316 Urho Kekkonen National Park 317 Inari 317 Karigasniemi 318 Karasjok 319 Nordkapp 319 Hammerfest 321 Alta 321 Tromsø 323 HIGHLIGHTS Making it to Svalbard (p324), one of the Svalbard most impressive destinations on earth Enjoying a cocktail at the ultra-cool Ice Hotel near Kiruna (p309) Hiking in Pallas-Ounastunturi National Park (p327) or the Kilpisjärvi region (p328) Looking out over the turquoise seas and fabulous scenery of the Lofoten islands Hurtigruten (p303) Route Kilpisjärvi Sitting back and admiring the fantastic Pallas-Ounastunturi coastal scenery from the legendary Lofoten National Park Hurtigruten steamer (p298) Islands Kiruna 298 ITINERARY 1: THE SCANDINAVIAN NORTH 299 The starkly beautiful wilderness of the Scandinavian Arctic makes it a perfect place for the road trip of a lifetime. It’s one of Europe’s last great wilderness areas and a land of invigorating TO THE NORTH POLE extremes, but at the same time it’s much more accessible than other Arctic regions. A good Getting to the North Pole from Scandinavia is probably the simplest route around, and a host of companies offer trips and tours.