Updated Independent Technical Report for the Maniitsoq Nickel-Copper-Cobalt-PGM Project, Greenland Page I
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
[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 -
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: -
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. -
A Pilot Project to Undertake Genetic Stock of Origin
International Atlantic Salmon Research Board SAG(14)5 Identification of Genetic Stock of Origin of European Atlantic Salmon Captured at West Greenland for the Years 2002-2012 Not to be cited without prior reference to the authors 6 May 2014 SAG(14)5 Identification of Genetic Stock of Origin of European Atlantic salmon Captured at West Greenland for the Years 2002-2012. This draft final report was prepared in fulfilment of a contract to undertake genetic stock identification of Atlantic salmon captured at West Greenland for the period 2002-2012. The project sponsors were the Agri-Food and Biosciences Institute for Northern Ireland (AFBINI), the International Atlantic Salmon Research Board (IASRB) of the North Atlantic Salmon Conservation Organisation (NASCO) and the Atlantic Salmon Trust (AST). Contributors to the report were Philip McGinnity (UCC), Paulo Prödohl (QUB), Caroline Bradley (QUB), Tim Sheehan (NOAA), Barb Lubinski (USGS), Tim King (USGS) and Tom Cross (UCC). Background Previous physical tagging (Reddin et al. 2012) and genetic stock identification studies (Gauthier-Ouellet et al 2009; Sheehan et al. 2010) of Atlantic salmon at continental scale suggest that fish from North America and Europe, and European fish from the Northern and Southern Multi-Sea-Winter (MSW) population complexes, contribute to the Atlantic salmon catch off West Greenland. However, little is known of the proportions of fish originating from different European regions and individual rivers within these regions. European Atlantic salmon caught at West Greenland appear to be predominantly, non- maturing one-sea-winter fish. These are fish that mature after two or more winters at sea, and are commonly known as 1SW non-maturing or multi-sea-winter (MSW) maturing fish. -
Greenland Last Ice Area
kn Greenland Last Ice Area Potentials for hydrocarbon and mineral resources activities Mette Frost, WWF-DK Copenhagen, September 2014 Report Greenland Last Ice Area. Potentials for hydrocarbon and mineral resources activities. The report is written by Mette Frost, WWF Verdensnaturfonden. Published by WWF Verdensnaturfonden, Svanevej 12, 2400 København NV. Denmark. Phone +45 3536 3635 – E-mail: [email protected] WWF Global Arctic Programme, 275 Slater Street, Ottawa, Ontario, K1P 5L4. Canada. Phone: +1 613 232 2535 Project The report has been developed under the Last Ice Area project, a joint project between WWF Canada, WWF Denmark and WWF Global Arctic Programme. Other WWF reports on Greenland – Last Ice Area Greenland Last Ice Area. Scoping study: socioeconomic and socio-cultural use of the Greenland LIA. By Pelle Tejsner, consultant and PhD. and Mette Frost, WWF-DK. November 2012. Seals in Greenland – an important component of culture and economy. By Eva Garde, WWF-DK. November 2013. Front page photo: Yellow house in Kullorsuaq, Qaasuitsup Kommunia, Greenland. July 2012. Mette Frost, WWF Verdensnaturfonden. The report can be downloaded from www.wwf.dk [1] CONTENTS Last Ice Area Introduction 4 Last Ice Area / Sikuusarfiit Nunngutaat 5 Last Ice Area/ Den Sidste Is 6 Summary 7 Eqikkaaneq 12 Sammenfatning 18 1. Introduction – scenarios for resources development within the Greenland LIA 23 1.1 Last Ice Area 23 1.2 Geology of the Greenland LIA 25 1.3 Climate change 30 2. Mining in a historical setting 32 2.1 Experiences with mining in Greenland 32 2.2 Resources development to the benefit of society 48 3. -
The Necessity of Close Collaboration 1 2 the Necessity of Close Collaboration the Necessity of Close Collaboration
The Necessity of Close Collaboration 1 2 The Necessity of Close Collaboration The Necessity of Close Collaboration 2017 National Spatial Planning Report 2017 autumn assembly Ministry of Finances and Taxes November 2017 The Necessity of Close Collaboration 3 The Necessity of Close Collaboration 2017 National Spatial Planning Report Ministry of Finances and Taxes Government of Greenland November 2017 Photos: Jason King, page 5 Bent Petersen, page 6, 113 Leiff Josefsen, page 12, 30, 74, 89 Bent Petersen, page 11, 16, 44 Helle Nørregaard, page 19, 34, 48 ,54, 110 Klaus Georg Hansen, page 24, 67, 76 Translation from Danish to English: Tuluttut Translations Paul Cohen [email protected] Layout: allu design Monika Brune www.allu.gl Printing: Nuuk Offset, Nuuk 4 The Necessity of Close Collaboration Contents Foreword . .7 Chapter 1 1.0 Aspects of Economic and Physical Planning . .9 1.1 Construction – Distribution of Public Construction Funds . .10 1.2 Labor Market – Localization of Public Jobs . .25 1.3 Demographics – Examining Migration Patterns and Causes . 35 Chapter 2 2.0 Tools to Secure a Balanced Development . .55 2.1 Community Profiles – Enhancing Comparability . .56 2.2 Sector Planning – Enhancing Coordination, Prioritization and Cooperation . 77 Chapter 3 3.0 Basic Tools to Secure Transparency . .89 3.1 Geodata – for Structure . .90 3.2 Baseline Data – for Systematization . .96 3.3 NunaGIS – for an Overview . .101 Chapter 4 4.0 Summary . 109 Appendixes . 111 The Necessity of Close Collaboration 5 6 The Necessity of Close Collaboration Foreword A well-functioning public adminis- by the Government of Greenland. trative system is a prerequisite for a Hence, the reports serve to enhance modern democratic society. -
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. -
Draft Copy 30/5 2005
Thematic maps and data of North and North East Greenland: geology, mineral occurrences and hydrocarbons Draft copy 30/5 2005 G E U S 2 1. Abstract 5 2. Introduction 6 2.1 Geographical area...................................................................................................6 2.2 Limitations ...............................................................................................................6 3. Digital topographic data 8 3.1 Introduction .............................................................................................................8 3.2 History .....................................................................................................................8 3.3 Coverage, origin and description of topographic data .............................................9 3.4 Place names .........................................................................................................12 4. Digital geological maps 14 4.1 Data sources .........................................................................................................14 4.2 Map at target scale of 1:250 000...........................................................................14 4.3 Synoptic maps.......................................................................................................16 4.4 Source maps .........................................................................................................16 4.5 Datasheet presentation .........................................................................................19 -
The East Greenland Rifted Volcanic Margin
GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 24 • 2011 The East Greenland rifted volcanic margin C. Kent Brooks GEOLOGICAL SURVEY OF DENMARK AND GREENLAND DANISH MINISTRY OF CLIMATE, ENERGY AND BUILDING 1 Geological Survey of Denmark and Greenland Bulletin 24 Keywords East Greenland, North Atlantic, rifted volcanic margin, large igneous province, LIP, Palaeogene, basalt, syenite, nephelinite, carbona- tite, uplift. Cover Sundown over the nunataks in the Main Basalts (Skrænterne Fm) to the south of Scoresby Sund. Camped on the glacier, the 1965 Ox- ford University East Greenland Expedition travelled and collected from this area on foot, manhauling equipment on the sledge to the left. The expedition results were published in Fawcett et al. (1973). Frontispiece: facing page Mountains of horizontally layered basalt flows rising to about 2000 m on the south side of Scoresby Sund. Typical trap topography as found throughout most of the Kangerlussuaq–Scoresby Sund inland area. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Department of Geoscience, Aarhus University; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Department of Geography and Geology, University of Copenhagen Scientific editor of this volume: Adam A. Garde Editorial secretaries: Jane Holst and Esben W. Glendal Referees: Dennis K. Bird (USA) and Christian Tegner (DK) Illustrations: Eva Melskens with contributions from Adam A. Garde Digital photographic work: Benny Schark Graphic production: Kristian A. Rasmussen Printers: Rosendahls · Schultz Grafisk A/S, Albertslund, Denmark Manuscript received: 1 March 2011 Final version approved: 20 September 2011 Printed: 22 December 2011 ISSN 1604-8156 ISBN 978-87-7871-322-3 Citation of the name of this series It is recommended that the name of this series is cited in full, viz. -
Status of the Black-Legged Kittiwake (Rissa Tridactyla) Breeding
Status of the black-legged kittiwake (Rissa tridactyla) breeding population in Greenland, 2008por_169 391..403 Aili Lage Labansen,1 Flemming Merkel,2 David Boertmann2 & Jens Nyeland3 1 Greenland Institute of Natural Resources, PO Box 570, DK-3900 Nuuk, Greenland 2 National Environmental Research Institute, Department of Arctic Environment, Aarhus University, Frederiksborgvej 399, DK-4000 Roskilde, Denmark 3 Naturama, Dronningmaen 30, DK-5700 Svendborg, Denmark Keywords Abstract Black-legged kittiwake; Greenland; population status; Rissa tridactyla. Based on the intensified survey efforts (since 2003) of Greenlandic breeding colonies of black-legged kittiwake (Rissa tridactyla), the total Greenland breed- Correspondence ing population was estimated at roughly 110 000 breeding pairs, constituting Aili Lage Labansen, Greenland Institute of about 4% of the total North Atlantic breeding population. This population Natural Resources, PO Box 570, DK-3900 estimate of black-legged kittiwake is the most reliable and updated estimate Nuuk, Greenland. E-mail: [email protected] hitherto reported for Greenland. The results confirm considerable population doi:10.1111/j.1751-8369.2010.00169.x declines in many areas of West Greenland. The breeding population of black- legged kittiwakes in the Qaanaaq area appears healthy, whereas the rest of the west coast has experienced declines, especially the north-western region (in the area from Upernavik to Kangaatsiaq). Exactly when these reductions have occurred is uncertain because of the limited survey effort in the past, but some colonies declined as far back as the mid-1900s, whereas declines of other colonies have occurred since the 1970–80s. East Greenland data from the past are few, but recent aerial surveys confirm that the abundance of breeding kittiwakes on this inaccessible coast is low. -
Not to Be Cited Without Prior Reference to the Author(S)
NOT TO BE CITED WITHOUT PRIOR REFERENCE TO THE AUTHOR(S) Northwest Atlantic Fisheries Organization Serial No. N7091 NAFO SCR Doc. 20/043 SCIENTIFIC COUNCIL MEETING – JUNE 2020 An assessment of the stocks of Greenland halibut in the South West Greenland fjords division 1BC, 1D and 1EF all located in NAFO subarea 1, using the Depletion Corrected Average Catch model. by Rasmus Nygaard Greenland Institute of Natural Resources, P.O. Box 570, 3900 Nuuk, Greenland Summary The Greenland halibut fishery in the fjords in West Greenland started with the introduction of longlines about 110 years ago. The fishery is most pronounced in the Disko Bay, the Uummannaq fjord and the fjords near Upernavik, but the fishery in the other fjord areas further south in West Greenland has just as long a history with catch statistics going back to the 1960’s in all areas and even back to 1910 in the fjords around Qaqortoq in south Greenland (1F). In this study, the depletion corrected average catch (DCAC) model is used to approximate a sustainable level of catch, for the fjord stocks of Greenland halibut in NAFO subarea 1 subdivision 1BC, 1D and 1EF inshore. The harvest control rules suggested in the ICES DLS Guidance Report 2012 and supplementary knowledge can be used to advise a stepwise adjustment of the catch to the DCAC approximated sustainable level of catch in the coming years. The approximated sustainable level catch calculated through catch data from 1960 to present is 300 t in the combined area 1B and one 1C (the fjords around Sisimiut and Maniitsoq), 398 t in 1D (the fjords near Nuuk) and 222 t in the combined 1E and 1F area (fjords between Paamiut, Qaqortoq, narsaq and Nanortalik).