ARCTIC RIFT COPPER Part of World’S Newest Metallogenic Province: Kiffaanngissuseq

Total Page:16

File Type:pdf, Size:1020Kb

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. The large scale of the mineral system, widespread copper anomalism, combined with dual mineralising events are analogous to Earth’s great copper systems. The Company considers that Kiffaanngissuseq has the potential to be a world-class mineral province. A coincident magnetic-gravity-conductivty and high-grade geochemical copper anomaly occurs within the project. The anomalism is located at an oxidation boundary and is proposed to be the expression of a hydrothermal outlet. This site of focussed fluid flow forms the basis of a high-priority, near- term target, known as the ‘Minik Singularity’. Authors: Dr Jonathan Bell (lead author), Greenfields Executive Director (Technical) PhD Mineral Economics, MSc Mineral Economics, BSc Applied Geology, Member of the Australian Institute of Geoscientists 1 (MAIG, #3116), Graduate of the Australian Institute of Company Directors 2 (GAICD), Associate of the Resources and Energy Law Association, Affiliate of the Stockbrokers Association of Australia (AfSAFAA), RG146 Accredited3. Joel Burkin (contributor), Greenfields Geologist BSc (Hons) Geology, Graduate of the Australian Institute of Geoscientists (GAIG, #7724), Fellow of the Geological Society of London (FGS, #0001040164). Lindsay Dick (contributor), Greenfields Executive Director (Corporate) BSc Chemistry, LLB (Dist), Young Professional of the Resources and Energy Law Association. Reviewers: Mathew Longworth (internal review), Greenfields Chairperson BSc Geology, Member of the Australasian Institute of Mining and Metallurgy (MAusIMM , #110783). Dr Mark Hutchison (external, paid review), Consultant Director of Trigon Geoservices Ltd PhD Geology, BSc (Hons) Geology, Member & Registered Professional Geologist of the Australian Institute of Geoscientists (MAIG RPGeo, #10080). Consent & Disclaimer: Greenfields prepared this Report and gives its consent to use this document for Public Reporting purposes. This Report meets the minimum requirements of the VALMIN Code (2015), which is the industry standard designed to fit with the Australian regulatory frameworks. All beliefs expressed in this Report by the Company are expressed in good faith and are believed to have a reasonable basis on the knowledge available to The Company. However, to the extent permitted by law the Company and the authors of this Report disclaim any liability for any expenses, losses, damages or costs incurred from any reliance on the content of this Report. The Company advises that this Report may contain forward-looking statements which may be subject to significant uncertainties outside of The Company’s control. Actual future events may vary from these forward-looking statements and you are cautioned not to place undue reliance on any forward-looking statement. © Greenfields Exploration Ltd, ABN 50 619 328 442, 17/11/2020 Contact details & registered address Online Level 14, 197 St Georges Terrace gexpl.com Perth WA 6000 linkedin.com/company/Greenfields-exploration-ltd/ P: 08 6270 6318 facebook.com/gexpl/ E: [email protected] Twitter: GreenfieldsExpl Document information: Reporting standards JORC Code 2012, VALMIN Code 2015 Report date: 18 November 2020 Effective date 17 November 2020 Status: Draft for client review 1 https://www.aig.org.au/ 2 http://aicd.companydirectors.com.au/ 3 http://asic.gov.au/regulatory-resources/find-a-document/regulatory-guides/rg-146-licensing-training-of-financial- product-advisers/ gexpl.com Greenfields Exploration Ltd | November 2020 CONTENTS Contents ______________________________________________________________________________ 4 1 Summary _______________________________________________________________________ 10 2 Introduction _____________________________________________________________________ 12 2.1 Scope of Work 12 2.2 Effective Date 12 2.3 Reporting Standards 12 2.4 Reliance on Other Experts 12 2.5 Information Sources 13 2.6 Site Visit 13 2.7 Report costs and Relationships 13 2.8 Qualifications and Experience 13 3 Project Description and Location _____________________________________________________ 14 3.1 Location and Tenure 14 3.2 Accessibility, Climate, Local Resources, Infrastructure and Physiography 20 3.3 Mining Industry 25 4 History _________________________________________________________________________ 28 5 Geological Setting ________________________________________________________________ 29 5.1 Regional Geology 29 5.2 Local Geology 47 6 Exploration ______________________________________________________________________ 65 6.1 Prospecting 65 6.2 Geochemistry 65 6.3 Geophysics 67 6.4 Singularity 68 6.5 Drilling 70 6.6 Prospectivity and Endowment Study 70 7 Mineralisation ____________________________________________________________________ 71 7.1 Known Prospects 73 7.2 Deposit Type 79 7.3 Mineral System 85 8 Data Integrity ___________________________________________________________________ 103 8.1 Sample Preparation, Analyses and Security 103 8.2 Data Verification 103 9 Mineral Resource Estimates _______________________________________________________ 103 10 Modifying Factors________________________________________________________________ 103 10.1 Environmental Studies Permitting, and Social/Community Impact 103 10.2 Project Infrastructure 105 10.3 Mining Methods 106 10.4 Mineral Processing and Metallurgical Testing 107 10.5 Recovery Methods 107 iv 4 Contents ARCTIC RIFT COPPER | Greenfields Exploration Limited 10.6 Capital and Operating Costs 108 10.7 Market Studies and Contracts 108 10.8 Economic Evaluations 110 11 Ore Reserve Estimates ___________________________________________________________ 110 12 Other Relevant Data and Information ________________________________________________ 110 13 Interpretations and Conclusions_____________________________________________________ 111 13.1 New insights 111 13.2 Significance 112 13.3 Knowledge Gaps 113 14 Recommendations _______________________________________________________________ 114 15 References ____________________________________________________________________ 117 16 Consent and Compliance Statement: Dr Bell ___________________________________________ 143 17 Appendix 1: JORC Table 1 ________________________________________________________ 144 18 Appendix 2: License Details ________________________________________________________ 148 19 Appendix 3: Supporting figures _____________________________________________________ 149 Tables Table 1: Licence details and estimated holding costs 14 Table 2: Geochronological dating summary 64 Table 3: North Greenland mineral system hierarchy 86 Table 4: Empirical evidence of a mineral system 87 Table 5: Mineral system certainty estimates c. 1,250 Ma 101 Table 6: Mineral system certainty estimates c. 385 Ma 102 Table 7: Proposed budget 116 Table 8: ARC licence co-ordinates 148 Figures Figure 1: Historical results 11 Figure 2: ARC’s location 14 Figure 3: Greenland’s bureaucratic structure 16 Figure 4: Licence map 19 Figure 5: Daylight statistics for Station Nord 20 Figure 6: Weather statistics for Station Nord 21 Figure 7: Physiography of Neergaard Dal/Elv 21 Figure 8: Buildings in Jørgen Brønlund Fjord 22 Figure 9: Arctic sea ice extent 23 Figure 10: Satellite image of J.C. Christensen Land 24 Figure 11: Miners at the historical Blyklippen lead-zinc mine in eastern Greenland 26 Figure 12: Photo from the portal of the Black Angel in western Greenland 26 Figure 13: Adjacent projects and deposits 26 Figure 14: Airplanes used to explore North Greenland 1933-1938 28 Figure 15: Geology of Greenland 30 Figure 16: Timeline of geological events in North Greenland 31 Contents 5 Greenfields Exploration Ltd | November 2020 Figure 17: Reconstruction of Columbia at c. 1,600 Ma 32 Figure 18 Neoproterozoic-aged sedimentary basins of the Laurentian margin 32 Figure 19: Arctic plates and volcanic
Recommended publications
  • Book Review ''Harald Moltke – Painter of the Aurora'
    CMYK RGB Book Review Hist. Geo Space Sci., 3, 127–129, 2012 History of www.hist-geo-space-sci.net/3/127/2012/ Geo- and Space doi:10.5194/hgss-3-127-2012 © Author(s) 2012. CC Attribution 3.0 License. Access Open Sciences Advances in Science & Research Open Access Proceedings Book Review Drinking Water Drinking Water “Harald Moltke – Painter of the Aurora” Engineering and Science Engineering and Science Open Access Access Open Discussions S. Silverman Discussions Correspondence to: S. Silverman ([email protected]) Earth System Earth System Science Science Peter Stauning: Harald Moltke – Painter of the Aurora, Den- “[e]ven in those days [about 1815] Helmuth had the tal- mark, www.forlagetepsilon.dk, 216 pp., ISBN-13: 978-87- ent of sketching with a firm hand characteristic pictures of Open Access Open Open Access Open Data Data 993384-3-6, EUR 40.00, 2011, Published in collaboration such objects as interested him. How he developed this tal- with the Danish Meteorological Institute. ent later on is seen by the many illustrations in ink or pencil Discussions Harald Moltke – Painter of the Aurora, by Peter Stauning, of the descriptions which his letters contain.” (Hegermann- is a well-designed, oversize, glossy paper book focusing on Lindencrone, 1893). An example of one of his sketches is re- the paintings of aurora done during two expeditions, one produced in Thies (photos between pp.Social 192–193). Helmuth Social to Iceland and one to Finland, in 1899 and 1900. The first von Moltke, from a collateral branch of the family, in the Open Access Open Geography Open Access Open Geography two chapters provide background on early Danish studies of early nineteenth century was trained in the Danish military the aurora, and those of the Danish Meteorological Institute academy, commissioned as a lieutenant, and then advised by which led to the two expeditions for the study of the aurora.
    [Show full text]
  • Arktisk Kommando for Både Forskere Og Transportør
    UNCLASSIFIED Possibilities for logistic support from Joint Arctic Command 2020 DTU Logistikworkshop 2019 Bettina Ovgaard Science Liaison Officer JOINT ARCTIC COMMAND UNCLASSIFIED UNCLASSIFIED AGENDA Area of Operation and tasks Assets How to apply for support Support to Science 2019 Evaluation of science support 2019 Support from Navy ships 2020 Station Nord boarder control – how to UNCLASSIFIED 2. december 2019 UNCLASSIFIED AREA OF RESPONSIBILITY UNCLASSIFIED TASKS Military: • Military defence of Greenland and Faroe Islands • Surveillance and maintenance of territorial sovereignty Coast guard: • Anti-pollution and oil spill recovery • Fishery Protection Search and Rescue: • Joint Rescue Coordination Centre (JRCC Greenland) Additional: • Hydrographical surveys of Greenland • Support to local communities • Police support UNCLASSIFIED 2. december 2019 UNCLASSIFIED ASSETS UNCLASSIFIED 2. december 2019 UNCLASSIFIED REQUEST FOR SUPPORT UNCLASSIFIED 2. december 2019 UNCLASSIFIED INTRUSIVE AND NON-INTRUSIVE PROJECTS Intrusive support is defined as binding the ship in time and space. Request for support from the Royal Danish Navy for an intrusive project (with or with out finance) is through DANISH CENTER FOR MARITIME RESEARCH. Non-intrusive support is defined as assistance done en route while patrolling and with great flexibility of time. Application for support from the Royal Danish Navy for a non-intrusive project is through ISAAFFIK.ORG. UNCLASSIFIED 2. december 2019 UNCLASSIFIED RULES OF ENGAGEMENT • Support in remote areas without commercial infrastructure. • Cost free for the Danish Defense. • Cancellation of support can happen with little notice due to operational tasks and weather. • All support is executed given that permits and other documents are obtained and in order. UNCLASSIFIED 2. december 2019 UNCLASSIFIED DEADLINE FOR APPLICATION Apply through DCH (intrusive) with or without funding Deadline: 1 April for the year to come.
    [Show full text]
  • Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting
    Polarforschung 74 (1-3), 21 – 39, 2004 (erschienen 2006) Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting by H. Ruth Jackson1, Tim Hannon1, Sönke Neben2, Karsten Piepjohn2 and Tom Brent3 Abstract: Three major tectonic boundaries are predicted to be present beneath durch eine folgende kompressive Phase reaktiviert wurde. Als Arbeitshypo- the waters of this segment of Nares Strait: (1) the orogenic front of the Paleo- these fassen wir die oberflächennahen Teile dieses Systems als Stirn der Plat- zoic Ellesmerian Foldbelt between thrust sheets on Ellesmere Island and flat- tengrenze zwischen Nordamerika und Grönland auf. lying foreland rocks on Greenland, (2) the supposed sinistral strike-slip plate boundary of Paleocene age between the Ellemere Island section of the North America plate and the Greenland plate, and (3) the orogenic front of the Eocene to Oligocene Eurekan Foldbelt that must lie between thrust tectonics INTRODUCTION on Ellesmere Island and undeformed rocks of Greenland. To understand this complicated situation and to look for direct evidence of the plate boundary, The Late Cretaceous and Tertiary deformation on Ellesmere new seismic reflection profiles were collected and, together with industry data in the south, interpreted. The profiles are clustered in three areas controlled by Island (Fig. 1) called the Eurekan Orogeny has been attributed the distribution of the sea ice. Bathymetry is used to extrapolate seismic to the counter clockwise rotation of Greenland (e.g., OKULITCH features with a topographic expression between the regions. Based on high- & TRETTIN 1991). However reconciling the geology on oppo- resolution boomer and deeper penetration airgun profiles five seismic units are mapped.
    [Show full text]
  • (Late Tertiary) As Seen from Prince Patrick Island, Arctic Canada’ JOHN G
    ARCTIC WL. 43, NO. 4 (DECEMBER 1990) P. 393-403 Beaufort Formation (Late Tertiary) as Seen from Prince Patrick Island, Arctic Canada’ JOHN G. FYLES’ (Received 20 March 1990; accepted in revked form 14 June 1990) ABSTRACT. The Beaufort Formation, in its typearea on Prince Patrick Island, is a single lithostratigraphicunit, a few tens of metres thick, consisting of unlithified sandy deposits of braided rivers. Organicbeds in the sand have yielded more than 200 species of plants and insects and probably originated during the Pliocene, when the area supported coniferous forest. ThisBeaufort unit forms the thin eastern edge of a northwest-thickeningwedge of sand and gravel beneath the western part of the island. These largely unexposed beds,up to several hundred metres thick, include the Beaufort unit and perhaps other older or younger deposits.On the islands northeast and southwest of PrincePatrick Island (MeighenIsland to Banks Island),the name BeaufortFormation has been appliedto similar deposits of late Rrtiary age. Most recorded Beaufort beds on these islands are stratigraphically and paleontologically equivalentto the “type” Beaufort, but a few sites that have been called Beaufort (suchas Duck Hawk Bluffsand the lower unit at Ballast Brook,on Banks Island) differ stratigraphicallyand paleontologically from the “type” Beaufort. This paper recommends that these deposits (probably middle Miocene) and others like them be assigned new stratigraphic names and not be included in the Beaufort Formation as now defined. Informal names Mary Sachs gravel (Duck HawkBluffs) and Ballast Brookbeds are proposed as an initial step. Formal use of the name Beaufort Formation shouldrestricted be to the western Arctic Islands.
    [Show full text]
  • Possibilities for Logistic Support from Joint Arctic Command 2021 ​DTU Logistikworkshop 2020
    UNCLASSIFIED Possibilities for logistic support from Joint Arctic Command 2021 ​DTU Logistikworkshop 2020 ​Bettina Ovgaard ​Science Liaison Officer JOINT ARCTIC COMMAND UNCLASSIFIED UNCLASSIFIED AREA OF RESPONSIBILITY 3 December2020 UNCLASSIFIED JACO TASKS Military: • Military defence of Greenland and Faroe Islands • Surveillance and maintenance of territorial sovereignty Coast guard: • Anti-pollution and oil spill recovery • Fishery Protection Search and Rescue: • Joint Rescue Coordination Centre (JRCC Greenland) Additional: • Hydrographical surveys of Greenland • Support to local communities • Police support UNCLASSIFIED 3 December2020 UNCLASSIFIED ASSETS UNCLASSIFIED 3 December2020 UNCLASSIFIED REQUEST FOR SUPPORT UNCLASSIFIED 3 December2020 UNCLASSIFIED INTRUSIVE AND NON-INTRUSIVE PROJECTS Intrusive support is defined as binding the ship in time and space. Request for support from the Royal Danish Navy for an intrusive project (with or with out finance) is through DANISH CENTER FOR MARITIME RESEARCH. Non-intrusive support is defined as assistance done en route while patrolling and with flexibility of time. Application for support from the Royal Danish Navy for a non-intrusive project is through ISAAFFIK.ORG. UNCLASSIFIED 3 December2020 UNCLASSIFIED RULES OF ENGAGEMENT • Support in remote areas without commercial infrastructure. • Cost free for the Danish Defense. • Cancellation of support can happen with little notice due to operational tasks and weather. • All support is executed given that permits and other documents are obtained and in order inclusive approval of entry from the Greenlandic Covid-19 Secretariat. UNCLASSIFIED 3 December2020 UNCLASSIFIED DEADLINE FOR APPLICATION Apply through DCH (intrusive) with or without funding Deadline: 1 April for the year to come. Apply through Isaaffik.org (non-intrusive) First priority Deadline: 15 January 2021 for 2021 Feedback: At the latest ultimo February 2021.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • The Committee for Greenlandic Mineral Resources to the Benefit of Society
    to the benefit of greenland The Committee for Greenlandic Mineral Resources to the Benefit of Society Ilisimatusarfik, University of Greenland · P.O.Box 1061 · Manutooq 1 · DK-3905 Nuussuaq · +299 36 23 00 · [email protected] University of Copenhagen · Nørregade 10 · DK-1165 Copenhagen K · +45 35 32 26 26 · [email protected] table of contents foreword .................................................................................................................................................................4 structure .................................................................................................................................................................5 introduction .........................................................................................................................................................6 exploitation of greenlandic natural resources for the benefit of society ................8 Scenarios for Greenland’s future ............................................................................................................................ 16 Scenario 1: Status quo ........................................................................................................................................... 16 Scenario 2: Greenland becomes a natural resource exporter ................................................................................... 17 Scenario 3: Resource value is optimised through a wealth fund .............................................................................. 20 Scenario 4:
    [Show full text]
  • Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait
    Polarforschung 74 (1-3), 129 – 160, 2004 (erschienen 2006) In Search of the Wegener Fault: Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait by J. Christopher Harrison1 Abstract: A total of 28 geological-geophysical markers are identified that lich der Bache Peninsula und Linksseitenverschiebungen am Judge-Daly- relate to the question of strike slip motions along and bordering Nares Strait. Störungssystem (70 km) und schließlich die S-, später SW-gerichtete Eight of the twelve markers, located within the Phanerozoic orogen of Kompression des Sverdrup-Beckens (100 + 35 km). Die spätere Deformation Kennedy Channel – Robeson Channel region, permit between 65 and 75 km wird auf die Rotation (entgegen dem Uhrzeigersinn) und ausweichende West- of sinistral offset on the Judge Daly Fault System (JDFS). In contrast, eight of drift eines semi-rigiden nördlichen Ellesmere-Blocks während der Kollision nine markers located in Kane Basin, Smith Sound and northern Baffin Bay mit der Grönlandplatte zurückgeführt. indicate no lateral displacement at all. Especially convincing is evidence, presented by DAMASKE & OAKEY (2006), that at least one basic dyke of Neoproterozoic age extends across Smith Sound from Inglefield Land to inshore eastern Ellesmere Island without any recognizable strike slip offset. INTRODUCTION These results confirm that no major sinistral fault exists in southern Nares Strait. It is apparent to both earth scientists and the general public To account for the absence of a Wegener Fault in most parts of Nares Strait, that the shape of both coastlines and continental margins of the present paper would locate the late Paleocene-Eocene Greenland plate boundary on an interconnected system of faults that are 1) traced through western Greenland and eastern Arctic Canada provide for a Jones Sound in the south, 2) lie between the Eurekan Orogen and the Precam- satisfactory restoration of the opposing lands.
    [Show full text]
  • 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.
    [Show full text]
  • Faroe Islands and Greenland 2008
    N O R D I C M E D I A T R E N D S 10 Media and Communication Statistics Faroe Islands and Greenland 2008 Compiled by Ragnar Karlsson NORDICOM UNIVERSITY OF GOTHENBURG 2008 NORDICOM’s activities are based on broad and extensive network of contacts and collaboration with members of the research community, media companies, politicians, regulators, teachers, librarians, and so forth, around the world. The activities at Nordicom are characterized by three main working areas. Media and Communication Research Findings in the Nordic Countries Nordicom publishes a Nordic journal, Nordicom Information, and an English language journal, Nordicom Review (refereed), as well as anthologies and other reports in both Nordic and English langu- ages. Different research databases concerning, among other things, scientific literature and ongoing research are updated continuously and are available on the Internet. Nordicom has the character of a hub of Nordic cooperation in media research. Making Nordic research in the field of mass communication and media studies known to colleagues and others outside the region, and weaving and supporting networks of collaboration between the Nordic research communities and colleagues abroad are two prime facets of the Nordicom work. The documentation services are based on work performed in national documentation centres at- tached to the universities in Aarhus, Denmark; Tampere, Finland; Reykjavik, Iceland; Bergen, Norway; and Göteborg, Sweden. Trends and Developments in the Media Sectors in the Nordic Countries Nordicom compiles and collates media statistics for the whole of the Nordic region. The statistics, to- gether with qualified analyses, are published in the series, Nordic Media Trends, and on the homepage.
    [Show full text]
  • 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.
    [Show full text]