The Northernmost Ruins of the Globe: Eigil Knuth's Archaeological
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Geology of Greenland Bulletin 185, 67-93
Sedimentary basins concealed by Acknowledgements volcanic rocks The map sheet was compiled by J.C. Escher (onshore) In two areas, one off East Greenland between latitudes and T.C.R. Pulvertaft (offshore), with final compilation 72° and 75°N and the other between 68° and 73°N off and legend design by J.C. Escher (see also map sheet West Greenland, there are extensive Tertiary volcanic legend). In addition to the authors’ contributions to the rocks which are known in places to overlie thick sedi- text (see Preface), drafts for parts of various sections mentary successions. It is difficult on the basis of exist- were provided by: L. Melchior Larsen (Gardar in South ing seismic data to learn much about these underlying Greenland, Tertiary volcanism of East and West Green- sediments, but extrapolation from neighbouring onshore land); G. Dam (Cretaceous–Tertiary sediments of cen- areas suggests that oil source rocks are present. tral West Greenland); M. Larsen (Cretaceous–Tertiary Seismic data acquired west of Disko in 1995 have sediments in southern East Greenland); J.C. Escher (map revealed an extensive direct hydrocarbon indicator in of dykes); S. Funder (Quaternary geology); N. Reeh the form of a ‘bright spot’ with a strong AVO (Amplitute (glaciology); B. Thomassen (mineral deposits); F.G. Versus Offset) anomaly, which occurs in the sediments Christiansen (petroleum potential). Valuable comments above the basalts in this area. If hydrocarbons are indeed and suggestions from other colleagues at the Survey are present here, they could either have been generated gratefully acknowledged. below the basalts and have migrated through the frac- Finally, the bulletin benefitted from thorough reviews tured lavas into their present position (Skaarup & by John Korstgård and Hans P. -
Geology of Greenland Survey Bulletin 173, 1997, 1-37
G E O L O G Y O F G R E E N L A N D S U R V E Y B U L L E T I N 1 7 3 · 1 9 9 7 Cambrian shelf stratigraphy of North Greenland Jon R. Ineson and John S. Peel GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF ENVIRONMENT AND ENERGY Geology of Greenland Survey Bulletin 173 Keywords Franklinian Basin, North Greenland, shelf setting, Cambrian, lithostratigraphy, platform carbonates, outer shelf carbonates and siliciclastics Cover Lower – Middle Cambrian strata near the head of Nordenskiöld Fjord, north of Jungersen Gletscher, Freuchen Land. Reddish sandstones and succeeding, scree-covered mudstones of the Buen Formation (at glacier level) are conformably overlain by proximal slope-outer shelf carbonates and siliciclastics of the Brønlund Fjord Group. This area has proved critical in the correlation from Cambrian platform interior and platform margin strata to the equivalent slope and outer shelf carbonates and siliciclastics. Exposed Brønlund Fjord Group section is c. 300 m thick. Photo: Jakob Lautrup Jon R. Ineson, Geological Survey of Denmark and Greenland, Thoravej 8, DK-2400 Copenhagen NV, Denmark John S. Peel, Department of Historical Geology & Palaeontology, Institute of Earth Sciences, Uppsala University, Norbyvägen 22, S-752 36 Uppsala, Sweden Chief editor of this series: Peter R. Dawes Scientific editor: W. Stuart Watt Editorial secretary: Esben W. Glendal Critical readers: Tim de Freitas (Canada) and Loren E. Babcock (USA) Drawing work: Bente Thomas and others Photographic work: Jakob Lautrup Reproduction and graphic production: Knud Graphic Consult, Odense Manuscript submitted: 5th May, 1995 Final version approved: 9th August, 1996 Printed: 29th April, 1997 ISBN 87-7871-013-8 ISSN 1397-1905 Citation of the name of this series: It is recommended that the name of this series is cited in full, viz. -
ARCTIC RIFT COPPER Part of World’S Newest Metallogenic Province: Kiffaanngissuseq
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/346029727 ARCTIC RIFT COPPER Part of world’s newest metallogenic province: Kiffaanngissuseq Technical Report · November 2020 DOI: 10.13140/RG.2.2.18610.84161 CITATIONS 0 2 authors, including: Jonathan Bell Curtin University 17 PUBLICATIONS 13 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Greenland View project Mineral asset valuation and pricing View project All content following this page was uploaded by Jonathan Bell on 20 November 2020. The user has requested enhancement of the downloaded file. ARCTIC RIFT COPPER Part of world’s newest metallogenic province: Kiffaanngissuseq Technical Assessment Report Greenfields Exploration Ltd November 2020 This report presents a holistic view of north eastern Greenland’s geology. The empirical evidence of mineralisation and geological record are tied in with mineral system components from global through to prospect scales. The source rocks, geodynamic triggers, pathways, and deposition sites are all identified within a preserved terrane. This work defines the Kiffaanngissuseq metallogenic province, a previously undescribed mineral system. For the first time, we identify a c. 1,250 Ma orogenic event in the basement as the geodynamic trigger related to the basalt- hosted native copper within the Arctic Rift Copper project. A c. 385 Ma fluid migration is identified as the trigger for a second copper-sulphide mineralising event expressed within the project, that also emplaced a distal zinc deposit within Kiffaanngissuseq. This multi-episodal mineral system is supported by a regional geochemical and hydrodynamic framework that is not articulated elsewhere. -
Årsrapport 2012 Museet
ÅRSRAPPORT 2012 MUSEET Nunatta Katersugaasivia Allagaateqarfialu Grønlands Nationalmuseum og Arkiv P.O. Box 145, DK-3900 Nuuk www.natmus.g Årsrapport 2012 for Grønlands Nationalmuseum FORORD I 2012 fik vi søsat et forprojekt til et af vore større indsatsområder inden for forskning, nemlig et tværvidenskabeligt projekt som vi kalder Alle Tiders Mennesker – den globale klimaændring og kulturminderne i Grønland. Projektets formål er at undersøge klima- ændringernes indvirkning på bevaringen af fortidsminder i Grønland. Et pilotprojekt blev afviklet i Nuuk-området i første omgang i samarbejde med forskere fra flere forsknings- institutioner i Danmark. Det er et spændende tiltag som fortsætter i 2013 i fuld vigør. Den første halvdel af året har arbejdspladsen stået i trommedansens tegn. Museet fortsatte indsatsområderne inden for den immaterielle kulturarv med at slå et slag for trommedansen, da det er et område som har museets særlige bevågenhed. Således har vi i samarbejde med udøvende trommedansere arrangeret mange workshops i flere byer, hvor vi aktiverede en del unge mennesker med at få dem til at bygge egne tromme og lærte dem i udøvelse i trommedans og -sang. Det blev et vældig succesfuldt projekt som man lagde mærke til i offentligheden og som allevegne blev positivt modtaget. På formidlingssiden har året også været præget af forberedelse til opsætning af en ny permanent udstilling om de ældste tider og kulturer. Således åbnede vi udstillingen Inutoqqat - Ancient People og som fortæller om de tidligste kulturer fra omkring 2500 f.Kr. og op til år 1200 e.Kr. Årsrapporten vil give et lille indblik i, hvad vi foretager os på museet. -
No. Name of Locality Delimitation Description of Site Disturbing Acti- Visitors Vities 1 Offrey Ø – Hall’S the Coast from Approx
Regulation of Regulation of No. Name of locality Delimitation Description of site disturbing acti- visitors vities 1 Offrey Ø – Hall’s The coast from approx. 81°15’N to The area has very important Paleoinuit Admission only Only 20 visitors grave, Hall Land the South including Offrey Ø and sites at Solbakken as well as a memorial with NKA at a time a few to the North including Hall’s grave (Hall’s grave) for an American approved guide times in a year at 81°38’N expedition 2 Frigg Fjord, The area between the two rivers on Adam C. Knuth Site is the largest Admission only Only 20 visitors Johannes V Jensen each side of Adam C. Knuth Site Independence I site at Johannes V. Jensen with NKA at a time a few Land and 1,3 km into land Land. Nearby is a small Greenlandic approved guide times in a year Dorset Site and two whale sculls 3 Kølnæs – Kap Eiler The coast from Kølnæs to Kap By Kølnæs are some settlements from the Admission only Only 20 visitors Rasmussen, Peary Eiler Rasmussen by 82°35’45”N Thule Culture, where the world’s oldest with NKA at a time a few Land 83°32’40”N and 1 km from the umiaq from the 1460’ies was found. approved guide times in a year coast except from the part to the Barely 2 km from the coast a small very North where a narrow strip Paleoinuit site is situated on a beach cuts into the land terrace. -
Catalogue of Place Names in Northern East Greenland
Catalogue of place names in northern East Greenland In this section all officially approved, and many Greenlandic names are spelt according to the unapproved, names are listed, together with explana- modern Greenland orthography (spelling reform tions where known. Approved names are listed in 1973), with cross-references from the old-style normal type or bold type, whereas unapproved spelling still to be found on many published maps. names are always given in italics. Names of ships are Prospectors place names used only in confidential given in small CAPITALS. Individual name entries are company reports are not found in this volume. In listed in Danish alphabetical order, such that names general, only selected unapproved names introduced beginning with the Danish letters Æ, Ø and Å come by scientific or climbing expeditions are included. after Z. This means that Danish names beginning Incomplete documentation of climbing activities with Å or Aa (e.g. Aage Bertelsen Gletscher, Aage de by expeditions claiming ‘first ascents’ on Milne Land Lemos Dal, Åkerblom Ø, Ålborg Fjord etc) are found and in nunatak regions such as Dronning Louise towards the end of this catalogue. Å replaced aa in Land, has led to a decision to exclude them. Many Danish spelling for most purposes in 1948, but aa is recent expeditions to Dronning Louise Land, and commonly retained in personal names, and is option- other nunatak areas, have gained access to their al in some Danish town names (e.g. Ålborg or Aalborg region of interest using Twin Otter aircraft, such that are both correct). However, Greenlandic names be - the remaining ‘climb’ to the summits of some peaks ginning with aa following the spelling reform dating may be as little as a few hundred metres; this raises from 1973 (a long vowel sound rather than short) are the question of what constitutes an ‘ascent’? treated as two consecutive ‘a’s. -
Descriptive Text to the 1995 Geological Map of Greenland, 1:2 500 000
GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 18 2009 Greenland from Archaean to Quaternary Descriptive text to the 1995 Geological map of Greenland, 1:2 500 000. 2nd edition Niels Henriksen, A.K. Higgins, Feiko Kalsbeek and T. Christopher R. Pulvertaft GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE AND ENERGY Geological Survey of Denmark and Greenland Bulletin 18 Keywords Archaean, Caledonides, Cenozoic, economic geology, geological map, Greenland, ice sheet, Mesozoic, offshore, orogenic belts, Palaeozoic, petroleum, Phanerozoic, Proterozoic, sedimentary basins. Cover illustration The cover design depicts mountains of the East Greenland Caledonian fold belt. The view, west of Mestersvig (located on map, page 4), is north over Bersærkerbræ and the northern part of the Stauning Alper to Kong Oscar Fjord with Traill Ø in the right backgro- und. The mountains up to 1800 m high are of the Neoproterozoic Eleonore Bay Supergroup. To the right: first author Niels Henriksen, for many years head of geological mapping at GGU/GEUS, and participant in field work in Greenland for more than 45 years. Frontispiece: facing page Major Caledonian syncline involving reactivated Archaean basement gneisses containing amphibolite bands. Overlying rusty coloured Mesoproterozoic metasediments (Krummedal supracrustal sequence) just visible in tight core of the fold. The intensity of deformation in the syncline clearly increases towards the core, where the basement gneisses become more strongly foliated. Some of the amphibolite bands were derived from cross-cutting basic intrusions, which are still discernable in the less severely deformed parts of the Archaean basement (Fig. 17, p. 31). The height of the section is c. 2000 m. -
Crossing North Peary Land in Summer 1953
CROSSING NORTHPEARY LAND IN SUMMER 1953 E. J. Friinkl* oRmPeary Land, the most northerly part of Greenland, is a large penin- sula bounded on the east and north by the Arctic Ocean, and on the Nsouth by Frederick E. HydeFjord andits western prolongation, a deep valleyleading toHarder Fjord. It is crossed from east to west bya mountainrange, 60 to 70 km.wide, which contains alpine peaks 6,300 feet high. The valleys aremainly occupied by glaciers, butthere arelarge ice-free areas on the north coast and the shores of Frederick E. Hyde Fjord. Since 1900, when Peary journeyed along the north coast of Peary Land anddiscovered Kap Morris Jesup, the area has been visited by several explorersand scientists. J. P. Kochreached the east coast of northPeary Land in 1907, and in 1909 MacMillan and Borup visited Kap Morris Jesup. In 1921 Lauge Koch led the Danish Jubilee expedition round the north coast, makingscientific observations from which a geological map of Peary Land was drawn.Since then Danish expeditions to' east andnorth Greenland have beenfrequent, and a program of mappingand geological surveying has been carried out.This was continued by the Danish East Greenland expedition 1953, under the leadership of Lauge Koch, which was composed ofgeologists workingin east Greenlandfrom the base on Ella (3, 73"N., who included J. Haller, studying the Caledonian metamorphics at the edge of the ice cap; E. Wenk and P. Bearth, mapping plutonic centres in Scoresby Land; H. Butler, continuing his studies of theDevonian, and M. Sommer working inLyells Land. In addition two groups of geologists worked in north Greenland from the base at Centrums@, 80"N. -
Arkæologisk/Kulturhistorisk Bidrag Til ”Zone-Inddeling Af Nationalparken”
Nunatta Katersugaasivia Allagaateqarfialu Greenland National Museum and Archives P.O. Boks 145; 3900 – Nuuk; Grønland/Greenland. Tlf.: +(299) 322611; Fax: (+299) 322622 e-mail: [email protected] ; home page: www.natmus.gl 29. december 2009 Arkæologisk/kulturhistorisk bidrag til ”Zone-inddeling af Nationalparken” Revideret Version, dec 2009. NKA = Nunatta Katersugaasivia Allagaateqarfialu / Grønlands Nationalmuseum og Arkiv. Hermed fremsendes oversigt over de områder, som Grønlands Nationalmuseum og Arkiv anser for særligt beskyttelsesværdige. Arkæologiske lokaliteter i Nord- og Nordøstgrønland Særkendet ved Nationalparken er, at lovgivningen både beskytter hele den synlige forhistorie og de kultur- og naturlandskaber, som er skabt gennem årtusinder. I takt med forbedrede transport- og sikkerhedsteknologier vil interessen for at besøge fjerne, eksotiske områder stige. Det betyder, at der må tages særlige forhold i brug for at beskytte dette unikke, arktiske kulturlandskab. Kulturminder I betragtning af Grønlands størrelse er der kun få kulturminder; den begrænsede mængde er et produkt af en kort historie (4.400 år), de nomadiske livsformer og få personer i hver kulturperiode. I de eskimoiske kulturer er der generelt fokus på de samme ressourcer: sæl, hval, rensdyr, moskusokse og fugle og visse lokalitetstyper som polynia-områder, der ofte rummer særlige bopladser, som skal sikres, fordi de har stort forskningspotentiale, stort formidlingspotentiale og lign. Mange forskellige parametre medgår derfor ved udskillelsen af særligt sårbare områder I Nationalparken stiger mængden af fortidsminder fra Nord til Syd. Det store skift sker omkring 77°N (nordlige Germania Land). Nord for denne bredde-grad er de fleste kulturminder stærkt eksponerede, fordi der næsten ingen jordpålejring har været gennem 4.400 år - udover flyvesand. -
Palaeoeskimo Dwellings in Greenland: a Survey Les Habitations Paléoesquimaudes Du Groenland: Une Synthèse Claus Andreasen
Document généré le 29 sept. 2021 01:04 Études/Inuit/Studies Palaeoeskimo dwellings in Greenland: A survey Les habitations paléoesquimaudes du Groenland: une synthèse Claus Andreasen Architecture paléoesquimaude Résumé de l'article Palaeoeskimo Architecture Au Groenland, les habitations paléoesquimaudes sont principalement Volume 27, numéro 1-2, 2003 concentrées au nord et au nord-est de l'île. On en retrouve quelques-unes au sud-est, à l'ouest (de Nuuk à la baie de Disko) et au nord-ouest (Inglefield Land URI : https://id.erudit.org/iderudit/010805ar et Washington Land). Durant l'ensemble de la période du Paléoesquimau, on DOI : https://doi.org/10.7202/010805ar remarque la présence d'aménagements axiaux dans les habitations. Au Paléoesquimau ancien (Saqqaquien et Indépendancien I), le foyer, en forme de boîte, se situe à l'intérieur de deux rangées parallèles faites de dalles ou de Aller au sommaire du numéro blocs. Les pierres pour la cuisson et/ou l'ébullition sont courantes durant le Saqqaquien puis se rarifient au Dorsétien. Au cours du Saqqaquien récent, on observe un changement dans le style des habitations avec l'intégration de Éditeur(s) plateformes de couchage, tel qu'illustré dans la région de Disko Bay. Durant l'Indépendancien II, les bordures externes de l'aménagement axial s'étendent Association Inuksiutiit Katimajiit Inc. souvent vers le devant de l'habitation et peuvent avoir des “ailes” à une ou aux deux extrémités. Le Dorsétien ancien n'est recensé qu'au nord-ouest du ISSN Groenland où on a répertorié, dans la région d'Inglefield Land, au moins 0701-1008 (imprimé) quatre types d'habitations dont certaines plus substantielles comportaient un 1708-5268 (numérique) aménagement axial bien défini. -
Lichens from Peary Land, North Greenland
Folia Cryptog. Estonica, Fasc. 50: 3–11 (2013) http://dx.doi.org/10.12697/fce.2013.50.02 Lichens from Peary Land, North Greenland Eric Steen Hansen Natural History Museum of Denmark, University of Copenhagen, Herbarium, Botanical Garden, Øster Farimagsgade 2 C, DK-1123 Copenhagen K, Denmark. E-mail: [email protected] Abstract: A total of 81 taxa of lichens are reported from Peary Land and adjacent areas in North Greenland. Six taxa are new to Peary Land. INTRODUCTION The exploration of the lichen flora of the norther- Johnsen, E. Knuth, K. Ellitsgaard Rasmussen most arctic land area in the world, Peary Land, and J. Troelsen. Holmen spent four summers does not date far back in time. The Swedish and one winter in Peary Land. I wish to dedicate botanist, Thorild Wulff collected 64 lichen taxa the present paper to my former teacher in gla- in this region in June 1917 during ”The Second ciology, Børge Fristrup, and my former teacher Thule Expedition”. He died from exhaustion du- in bryology and arctic botany, Kjeld Holmen. ring the sledge-journey, but his collections were Apart from an incomplete list of lichens without saved (Lynge, 1923). ”The Danish Peary Land precise indication of localities (Dietz & Andersen, Expedition 1947–50” was the next expedition to 1984), this important lichen material from the visit the region. An extensive material of lichens middle of the 19th century has remained un- were collected by B. Fristrup, K. Holmen, P. published until now. The vascular plants and Fig. 1. Location of the two investigation areas in North Greenland. -
En Queerteoretisk Læsning Af Kønsopfattelser I Grønland I Et Historisk Perspektiv
EN QUEERTEORETISK LÆSNING AF KØNSOPFATTELSER I GRØNLAND I ET HISTORISK PERSPEKTIV Navn: Malu Aima Rohmann Fleischer Opgavetype: Speciale ECTS-Point: 30 Institution: Ilisimatusarfik- Grønlands Universitet Afdeling: Kultur- og Samfundshistorie Vejleder: Ebbe Volquardsen Afleverings dato: 28. januar 2020 Antal sider: 90, uden forside, litteraturliste og bilag Antal tegn: 218.726 (uden mellemrum) Foto: Eigil Knuth (Knuth 2003 [1943]:151,189) Abstract The main purpose with this thesis is to examine how inuit in Greenland have perceived various gender identities, throughout time. I have chosen to examine this starting with the identity categories tikkaliaq and nuliakaaliaq, which means people who are raised to be a as the “opposite gender” In present day, there are multiple contradicting theories about gender perception of precolonial inuit in Greenland. The majority of those that work with gender perception of inuit agree that the majority of the European missionaries and Arctic explorers, whom have described a binary gender perception, both within precolonial as well as colonial inuit, have not had a focus on the inuits own perception of gender, and the importance of gender in the inuit society. The main argument is often that the binary gender perception there is present today that effects inuit in Greenland, is a result of colonization. Some of the most dominating theories that are used in present day regarding gender in precolonial inuit, is the thesis that inuit has had a third gender, and the thesis of genderlesness. It is the idea that the social structure of precolonial inuit in reality was not based on gender. In both theses, identity categories like tikkaliaq and nuliakaaliaq are used as an argument for that gender either has had a significant importance to the inuits precolonial social structure, or that gender has not played a significant role.