Wilderness in the Circumpolar North: Searching for Compatibility In
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Kujalleq Nutaaq ERHVERVSUDVIKLINGS FORSLAG for Kommune Kujalleq
Kujalleq Nutaaq ERHVERVSUDVIKLINGS FORSLAG for Kommune Kujalleq Version 1.0 - 2020 Innovation South Greenland A/S, Torvevej 34, Postboks 313, 3920 Qaqortoq, Greenland Oqarasuaat +299 537777, e-mail: [email protected] Forord Innovation South Greenland arbejder målrettet for at få udviklingen i gang i hele Sydgrønland. Dette dokument afspejler anbefalingerne til Kommunalbestyrelsen. 1. Ser man på infrastrukturen er det gennem en årrække blevet svært at rejse rundt i Kommunen. 2. Det er en udfordring at få vareforsyninger, dyrt og svært at sende varer fra sydgrønland og svært at holde møder osv. Af disse og flere andre årsager er udviklingen gået nærmest i stå. 3. Resultatet har været at der er sket en gradvis en fraflytning. Desuden har personer med højere kompetencer fået gode jobs andre steder. Det er ganske enkelt blevet svært at skabe et livsgrundlag på et personligt plan, for familier og for erhvervslivet. Derfor har man etableret Innovation South Greenland A/S for at skabe vækst, udvikling og rådgivning af iværksættere. En konkret opgave som er blevet givet Innovation South Greenland A/S er at finde en løsning for Narsarsuaq i et nyt scenarie. Det vigtige er imidlertid at se på hele Sydgrønland som en sammenhængende region. Den første forudsætning er at skabe håb og troværdighed. Dernæst at man får en tidssvarende infrastruktur på plads. Ydermere skal der opdyrkes en iværksætterkultur som understøttes af igangsætning af konkrete projekter. Sidst og ikke mindst skal der tiltrækkes investeringer udefra og indgås bilaterale aftaler som kan styrke regionen. Erhvervsudviklingen skal baseres på et tæt samarbejde med Erhvervslivet, Kommunen, Selvstyret og Uddannelsesinstitutionerne i kommunen. -
The Origin, Development, and History of the Norwegian Seventh-Day Adventist Church from the 1840S to 1889" (2010)
Andrews University Digital Commons @ Andrews University Dissertations Graduate Research 2010 The Origin, Development, and History of the Norwegian Seventh- day Adventist Church from the 1840s to 1889 Bjorgvin Martin Hjelvik Snorrason Andrews University Follow this and additional works at: https://digitalcommons.andrews.edu/dissertations Part of the Christian Denominations and Sects Commons, Christianity Commons, and the History of Christianity Commons Recommended Citation Snorrason, Bjorgvin Martin Hjelvik, "The Origin, Development, and History of the Norwegian Seventh-day Adventist Church from the 1840s to 1889" (2010). Dissertations. 144. https://digitalcommons.andrews.edu/dissertations/144 This Dissertation is brought to you for free and open access by the Graduate Research at Digital Commons @ Andrews University. It has been accepted for inclusion in Dissertations by an authorized administrator of Digital Commons @ Andrews University. For more information, please contact [email protected]. Thank you for your interest in the Andrews University Digital Library of Dissertations and Theses. Please honor the copyright of this document by not duplicating or distributing additional copies in any form without the author’s express written permission. Thanks for your cooperation. ABSTRACT THE ORIGIN, DEVELOPMENT, AND HISTORY OF THE NORWEGIAN SEVENTH-DAY ADVENTIST CHURCH FROM THE 1840s TO 1887 by Bjorgvin Martin Hjelvik Snorrason Adviser: Jerry Moon ABSTRACT OF GRADUATE STUDENT RESEARCH Dissertation Andrews University Seventh-day Adventist Theological Seminary Title: THE ORIGIN, DEVELOPMENT, AND HISTORY OF THE NORWEGIAN SEVENTH-DAY ADVENTIST CHURCH FROM THE 1840s TO 1887 Name of researcher: Bjorgvin Martin Hjelvik Snorrason Name and degree of faculty adviser: Jerry Moon, Ph.D. Date completed: July 2010 This dissertation reconstructs chronologically the history of the Seventh-day Adventist Church in Norway from the Haugian Pietist revival in the early 1800s to the establishment of the first Seventh-day Adventist Conference in Norway in 1887. -
North America Name North America
Not at same scale Hawaii (U.S.) Name North America Name North America Greenland North America ARCTIC Sea Bering Bering Strait OCEAN Canada is on the continent Helpful Sea of North America. Hint Greenland Alaska Beaufort (Denmark) One U.S. state, Sea Two countries, the United States and Mexico, (U.S.) Baffin share the continent with Canada. North Hawaii, is not Bay part of North Gulf of America also includes Greenland, the countries Alaska America. %Nuuk of Central America, and many islands. Labrador Use the map to answer these questions about North America. Sea Hudson Canada Bay 1. In which direction is Mexico from the United States? R 2. Name three countries O C Mississippi Ottawa% K River that share a border with Mexico. Y M O U N T ATLANTIC A I 3. What country shares a border N Washington, D.C.% S OCEAN on the south with Canada? United States PACIFIC Rio of America Grande Bermuda (U.K.) 4. What U.S. state is on the northwest OCEAN part of North America? Bahamas Gulf of Mexico Cuba Dominican North America Mexico Republic 5. What oceans border the east Haiti Puerto Rico (U.S.) % National capital Mexico City Jamaica and west coasts of North America? % Mountain Belize Border Honduras 6. What ocean is north of this continent? Caribbean Sea Guatemala Nicaragua El Salvador N N 7. What is the capital of Canada? NW NE Costa Rica Area of detail WE WE Panama SOUTH AMERICA 8. What river forms part of the border Miles SW SE 0 200 400 600 S S between the U.S. -
Pdf Dokument
Udskriftsdato: 2. oktober 2021 BEK nr 517 af 23/05/2018 (Historisk) Bekendtgørelse om ændring af den fortegnelse over valgkredse, der indeholdes i lov om folketingsvalg i Grønland Ministerium: Social og Indenrigsministeriet Journalnummer: Økonomi og Indenrigsmin., j.nr. 20175132 Senere ændringer til forskriften LBK nr 916 af 28/06/2018 Bekendtgørelse om ændring af den fortegnelse over valgkredse, der indeholdes i lov om folketingsvalg i Grønland I medfør af § 8, stk. 1, i lov om folketingsvalg i Grønland, jf. lovbekendtgørelse nr. 255 af 28. april 1999, fastsættes: § 1. Fortegnelsen over valgkredse i Grønland affattes som angivet i bilag 1 til denne bekendtgørelse. § 2. Bekendtgørelsen træder i kraft den 1. juni 2018. Stk. 2. Bekendtgørelse nr. 476 af 17. maj 2011 om ændring af den fortegnelse over valgkredse, der indeholdes i lov om folketingsvalg i Grønland, ophæves. Økonomi- og Indenrigsministeriet, den 23. maj 2018 Simon Emil Ammitzbøll-Bille / Christine Boeskov BEK nr 517 af 23/05/2018 1 Bilag 1 Ilanngussaq Fortegnelse over valgkredse i hver kommune Kommuneni tamani qinersivinnut nalunaarsuut Kommune Valgkredse i Valgstedet eller Valgkredsens område hver kommune afstemningsdistrikt (Tilknyttede bosteder) (Valgdistrikt) (Afstemningssted) Kommune Nanortalik 1 Nanortalik Nanortalik Kujalleq 2 Aappilattoq (Kuj) Aappilattoq (Kuj) Ikerasassuaq 3 Narsaq Kujalleq Narsaq Kujalleq 4 Tasiusaq (Kuj) Tasiusaq (Kuj) Nuugaarsuk Saputit Saputit Tasia 5 Ammassivik Ammassivik Qallimiut Qorlortorsuaq 6 Alluitsup Paa Alluitsup Paa Alluitsoq Qaqortoq -
Imperializing Norden
Neumann, Iver B. Imperializing Norden Article (Accepted version) (Refereed) Original citation: Neumann, Iver B. (2014) Imperializing Norden. Cooperation and Conflict, 49 (1). pp. 119-129. ISSN 0010-8367 DOI: 10.1177/0010836714520745 © 2014 by Nordic International Studies Association, SAGE Publications This version available at: http://eprints.lse.ac.uk/56565/ Available in LSE Research Online: April 2016 LSE has developed LSE Research Online so that users may access research output of the School. Copyright © and Moral Rights for the papers on this site are retained by the individual authors and/or other copyright owners. Users may download and/or print one copy of any article(s) in LSE Research Online to facilitate their private study or for non-commercial research. You may not engage in further distribution of the material or use it for any profit-making activities or any commercial gain. You may freely distribute the URL (http://eprints.lse.ac.uk) of the LSE Research Online website. This document is the author’s final accepted version of the journal article. There may be differences between this version and the published version. You are advised to consult the publisher’s version if you wish to cite from it. Imperializing Norden.1 Cooperation and Conflict 49 (1): 119-129 (2014) Epilogue for a special issue on Post-Imperial Sovereignty Games in Norden Iver B. Neumann, [email protected] Abstract The two pre-Napoleonic Nordic polities are best understood as empires. Drawing on recent analytical and historical scholarship on empires, I argue that 17th and 18th-century Denmark, on which the piece concentrates, was very much akin to other European empires that existed at the time. -
Geological Survey of Denmark and Greenland Bulletin 11, 87-99
Zircon geochronology from the Kangaatsiaq– Qasigiannguit region, the northern part of the 1.9–1.8 Ga Nagssugtoqidian orogen, West Greenland Kristine Thrane and James N. Connelly The Kangaatsiaq–Qasigiannguit region in the northern part of the Palaeoproterozoic Nagssugto- qidian orogen of West Greenland consists of poly-deformed orthogneisses and minor occurrences of interleaved, discontinuous supracrustal belts. Laser ablation ICP-MS 207Pb/206Pb analyses of detrital zircons from four metasedimentary rocks (supplemented by ion probe analysis of one sample) and igneous zircons from six granitoid rocks cutting metasedimentary units indicate that the supracrustal rocks in the Kangaatsiaq–Qasigiannguit (Christianshåb) region are predominantly Archaean in age. Four occurrences of metasedimentary rocks are clearly Archaean, two have equivocal ages, and only one metasedimentary unit, from within the Naternaq (Lersletten) supracrustal belt, is demonstrably Palaeoproterozoic and readily defines a large fold complex of this age at Naternaq. The 2.9–2.8 Ga ages of detrital Archaean grains are compatible with derivation from the local basement orthogneisses within the Nagssugtoqidian orogen. The detrital age patterns are similar to those of metasediments within the central Nagssugtoqidian orogen but distinct from age patterns in metasediments of the Rinkian belt to the north, where there is an additional component of pre-2.9 Ga zircons. Synkine- matic intrusive granitoid rocks constrain the ages of some Archaean deformation at 2748 ± 19 Ma and some -
[BA] COUNTRY [BA] SECTION [Ba] Greenland
[ba] Validity date from [BA] COUNTRY [ba] Greenland 26/08/2013 00081 [BA] SECTION [ba] Date of publication 13/08/2013 [ba] List in force [ba] Approval [ba] Name [ba] City [ba] Regions [ba] Activities [ba] Remark [ba] Date of request number 153 Qaqqatisiaq (Royal Greenland Seagfood A/S) Nuuk Vestgronland [ba] FV 219 Markus (Qajaq Trawl A/S) Nuuk Vestgronland [ba] FV 390 Polar Princess (Polar Seafood Greenland A/S) Qeqertarsuaq Vestgronland [ba] FV 401 Polar Qaasiut (Polar Seafood Greenland A/S) Nuuk Vestgronland [ba] FV 425 Sisimiut (Royal Greenland Seafood A/S) Nuuk Vestgronland [ba] FV 4406 Nataarnaq (Ice Trawl A/S) Nuuk Vestgronland [ba] FV 4432 Qeqertaq Fish ApS Ilulissat Vestgronland [ba] PP 4469 Akamalik (Royal Greenland Seafood A/S) Nuuk Vestgronland [ba] FV 4502 Regina C (Niisa Trawl ApS) Nuuk Vestgronland [ba] FV 4574 Uummannaq Seafood A/S Uummannaq Vestgronland [ba] PP 4615 Polar Raajat A/S Nuuk Vestgronland [ba] CS 4659 Greenland Properties A/S Maniitsoq Vestgronland [ba] PP 4660 Arctic Green Food A/S Aasiaat Vestgronland [ba] PP 4681 Sisimiut Fish ApS Sisimiut Vestgronland [ba] PP 4691 Ice Fjord Fish ApS Nuuk Vestgronland [ba] PP 1 / 5 [ba] List in force [ba] Approval [ba] Name [ba] City [ba] Regions [ba] Activities [ba] Remark [ba] Date of request number 4766 Upernavik Seafood A/S Upernavik Vestgronland [ba] PP 4768 Royal Greenland Seafood A/S Qeqertarsuaq Vestgronland [ba] PP 4804 ONC-Polar A/S Alluitsup Paa Vestgronland [ba] PP 481 Upernavik Seafood A/S Upernavik Vestgronland [ba] PP 4844 Polar Nanoq (Sigguk A/S) Nuuk Vestgronland -
Greenland Explorer
GREENLAND EXPLORER Valleys and Fjords EXPEDITION IN BRIEF The Trip Overview Meet locals along the west coast of Greenland and experience traditional Inuit settlements Visit the Ilulissat Icefjord, a UNESCO World Heritage Site The west coast of Greenland is Europe’s final frontier, and sailing along it is Explore historic places from Norse the best way to sample its captivating history, enthralling wildlife and distinct and Viking eras culture. Explore places from the Norse and Viking eras, experience the Spot arctic wildlife, such as whales, birds and seals Ilulissat Icefjord—a UNESCO World Heritage Site— and visit two Greenland Cruise in a Zodiac to get up close to communities, encountering an ancient culture surviving in a modern world. glaciers, fjords, icebergs and more For trip inquiries, speak to our Polar Travel Advisers at 1. 844.205.0837 | Visit QuarkExpeditions.com for more details or get a free quote here. and geography of Greenland, your next Itinerary stop. Join expedition staff on deck and on the bridge as they look out for whales and seabirds, get to know your fellow Ban Bay GREENLAND DAY 1 | ARRIVE IN guests or simply take in the natural REYKJAVIK, ICELAND ARCTIC beauty that surrounds you. CIRCLE Arrive in the Icelandic capital in the Eqip Sermia Ilulissat morning and make your way to your DAY 4 | EAST GREENLAND Sisimiut Kangerlussuaq Experience a true arctic ghost town Itilleq included hotel. You will have the day Scoresby Sund to explore the city on your own. In when we visit the abandoned settlement Nuuk of Skjoldungen, where inhabitants the evening, join us at your hotel for a Skjoldungen Denmark Strait welcome briefing. -
Ilulissat Icefjord
World Heritage Scanned Nomination File Name: 1149.pdf UNESCO Region: EUROPE AND NORTH AMERICA __________________________________________________________________________________________________ SITE NAME: Ilulissat Icefjord DATE OF INSCRIPTION: 7th July 2004 STATE PARTY: DENMARK CRITERIA: N (i) (iii) DECISION OF THE WORLD HERITAGE COMMITTEE: Excerpt from the Report of the 28th Session of the World Heritage Committee Criterion (i): The Ilulissat Icefjord is an outstanding example of a stage in the Earth’s history: the last ice age of the Quaternary Period. The ice-stream is one of the fastest (19m per day) and most active in the world. Its annual calving of over 35 cu. km of ice accounts for 10% of the production of all Greenland calf ice, more than any other glacier outside Antarctica. The glacier has been the object of scientific attention for 250 years and, along with its relative ease of accessibility, has significantly added to the understanding of ice-cap glaciology, climate change and related geomorphic processes. Criterion (iii): The combination of a huge ice sheet and a fast moving glacial ice-stream calving into a fjord covered by icebergs is a phenomenon only seen in Greenland and Antarctica. Ilulissat offers both scientists and visitors easy access for close view of the calving glacier front as it cascades down from the ice sheet and into the ice-choked fjord. The wild and highly scenic combination of rock, ice and sea, along with the dramatic sounds produced by the moving ice, combine to present a memorable natural spectacle. BRIEF DESCRIPTIONS Located on the west coast of Greenland, 250-km north of the Arctic Circle, Greenland’s Ilulissat Icefjord (40,240-ha) is the sea mouth of Sermeq Kujalleq, one of the few glaciers through which the Greenland ice cap reaches the sea. -
Road Construction in Greenland – the Greenlandic Case
THIS PROJECT IS BEING PART-FINANCED BY THE EUROPEAN UNION EUROPEAN REGIONAL DEVELOPMENT FUND ROAD CONSTRUCTION IN GREENLAND – THE GREENLANDIC CASE October 2007 Arne Villumsen Anders Stuhr Jørgensen Abdel Barten Janne Fritt-Rasmussen Laust Løgstrup Niels Brock Niels Hoedeman Ragnhildur Gunnarsdóttir Sara Borre Thomas Ingeman-Nielsen ROAD CONSTRUCTION IN GREENLAND – THE GREENLANDIC CASE October 2007 Arne Villumsen Anders Stuhr Jørgensen Abdel Barten Janne Fritt-Rasmussen Laust Løgstrup Niels Brock Niels Hoedeman Ragnhildur Gunnarsdóttir Sara Borre Thomas Ingeman-Nielsen Translation: J. Richard Wilson CONTENTS 1. GEOLOGY, NatURE AND CLIMate OF GREENLAND ........................... 4 1.1. GEOLOGY. 4 1.2. CLIMate . .5 1.3. Weather AND CLIMate IN AND AROUND GREENLAND . .5 1.4. Precipitation . .5 1.5. Weather- AND CLIMate REGIONS IN GREENLAND . .6 1.6. PERMAFROST. .9 1.7. Vegetation. .10 2. Relevant INFORMation FOR ROAD-BUILDING PROJECTS IN GREENLAND ........................................................................................... 11 3. EXISTING ROADS IN towns AND VILLAGES IN GREENLAND ......... 17 3.1. EXAMination OF EXISTING ROADS IN towns AND VILLAGES IN GREENLAND. 19 3.1.1. ROADS IN SISIMIUT town. .19 3.1.2. SISIMIUT Airport . 19 3.1.3. THE ROAD FROM KANGERLUSSSUAQ to THE INLAND ICE. 20 3.1.4. KANGERLUSSUAQ Airport. 21 3.2. STUDIES OF ROADS ELSEWHERE IN GREENLAND. .22 3.2.1. SOUTH GREENLAND . 23 3.2.2. ILLORSUIT. .27 4. THE SISIMIUT-KANGERLUSSUAQ ROAD ............................................ 32 4.1. GEOLOGICAL AND GEOGRAPHICAL overview. .32 4.2. SUitable Materials FOR ROAD CONSTRUCTION AND PERMAFROST. .35 4.3. GEOLOGICAL MODEL FOR THE AREA. 39 4.4. SUMMARY. .55 4.5. ENVIRONMental AND conservation ASPECTS. .55 4.6. ROUTE PROPOSAL – GENERAL ASPECTS. -
The Greenlander of Today 5
Top-Sukkertoppen, a west Greenland settlement, is located on rocky terrain. It is the centre of a valuablesealing and cod-salting industry. Bottom-Godthaab, capital of Greenland, was founded by the Danish missionary Hans Egede in 1721. This view shows the older part of the town including the hospital to the left. .. THE GREENLANDER OFTODAY* By Eske Brun. The Greenland Administration, Copenhagen, Denmark. SHOULD like to begin by saying something about the first and most I serious error generally made about Greenland, and the one which is, I think, the most difficult to eradicate: It is popularly believed that it is cold in Greenland, so cold that wherever and whenever you are there you are frozen stiff, and that there is nothing there but ice and snow. This idea of Greenland as an enormous lump of ice is largely due to the ice-cap. Five-sixths of Greenland’s two million square kilometers are covered by this ice-cap. There is so much ice there that, if it melted, the oceans and seasall over theworld would rise eight meters. The existence of the ice-cap is not due to any excessive cold in Greenland, but mainly to the considerable height of the country, the average height of the surface of the ice-cap being about 2000 meters, and to the heavy snowfall. Paradoxical as it may seem ,the ice-cap is thicker in southern Greenland than in northern Greenland, because the snowfall is heavier in the south. The largest continuous tracts of land not covered with ice are to be found in Peg-yland on the northern coast of the country. -
Natural Resources in the Nanortalik District
National Environmental Research Institute Ministry of the Environment Natural resources in the Nanortalik district An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project NERI Technical Report No. 384 National Environmental Research Institute Ministry of the Environment Natural resources in the Nanortalik district An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project NERI Technical Report No. 384 2001 Christain M. Glahder Department of Arctic Environment Data sheet Title: Natural resources in the Nanortalik district Subtitle: An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project. Arktisk Miljø – Arctic Environment. Author: Christian M. Glahder Department: Department of Arctic Environment Serial title and no.: NERI Technical Report No. 384 Publisher: Ministry of Environment National Environmental Research Institute URL: http://www.dmu.dk Date of publication: December 2001 Referee: Peter Aastrup Greenlandic summary: Hans Kristian Olsen Photos & Figures: Christian M. Glahder Please cite as: Glahder, C. M. 2001. Natural resources in the Nanortalik district. An interview study on fishing, hunting and tourism in the area around the Nalunaq gold project. Na- tional Environmental Research Institute, Technical Report No. 384: 81 pp. Reproduction is permitted, provided the source is explicitly acknowledged. Abstract: The interview study was performed in the Nanortalik municipality, South Green- land, during March-April 2001. It is a part of an environmental baseline study done in relation to the Nalunaq gold project. 23 fishermen, hunters and others gave infor- mation on 11 fish species, Snow crap, Deep-sea prawn, five seal species, Polar bear, Minke whale and two bird species; moreover on gathering of mussels, seaweed etc., sheep farms, tourist localities and areas for recreation.