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NUNAVUT a 100 , 101 H Ackett R Iver , Wishbone Xstrata Zinc Canada R Ye C Lve Coal T Rto Nickel-Copper-PGE 102, 103 H Igh Lake , Izo K Lake M M G Resources Inc
150°W 140°W 130°W 120°W 110°W 100°W 90°W 80°W 70°W 60°W 50°W 40°W 30°W PROJECTS BY REGION Note: Bold project number and name signifies major or advancing project. AR CT KITIKMEOT REGION 8 I 0 C LEGEND ° O N umber P ro ject Operato r N O C C E Commodity Groupings ÉA AN B A SE M ET A LS Mineral Exploration, Mining and Geoscience N Base Metals Iron NUNAVUT A 100 , 101 H ackett R iver , Wishbone Xstrata Zinc Canada R Ye C lve Coal T rto Nickel-Copper-PGE 102, 103 H igh Lake , Izo k Lake M M G Resources Inc. I n B P Q ay q N Diamond Active Projects 2012 U paa Rare Earth Elements 104 Hood M M G Resources Inc. E inir utt Gold Uranium 0 50 100 200 300 S Q D IA M ON D S t D i a Active Mine Inactive Mine 160 Hammer Stornoway Diamond Corporation N H r Kilometres T t A S L E 161 Jericho M ine Shear Diamonds Ltd. S B s Bold project number and name signifies major I e Projection: Canada Lambert Conformal Conic, NAD 83 A r D or advancing project. GOLD IS a N H L ay N A 220, 221 B ack R iver (Geo rge Lake - 220, Go o se Lake - 221) Sabina Gold & Silver Corp. T dhild B É Au N L Areas with Surface and/or Subsurface Restrictions E - a PRODUCED BY: B n N ) Committee Bay (Anuri-Raven - 222, Four Hills-Cop - 223, Inuk - E s E E A e ER t K CPMA Caribou Protection Measures Apply 222 - 226 North Country Gold Corp. -
Stream Sediment and Stream Water OG SU Alberta Geological Survey (MITE) ICAL 95K 85J 95J 85K of 95I4674 85L
Natural Resources Ressources naturelles Canada Canada CurrentCurrent and and Upcoming Upcoming NGR NGR Program Program Activities Activities in in British British Columbia, Columbia, NationalNational Geochemical Geochemical Reconnaissance Reconnaissance NorthwestNorthwest Territories, Territories, Yukon Yukon Territory Territory and and Alberta, Alberta, 2005-06 2005-06 ProgrProgrammeamme National National de de la la Reconnaissance Reconnaissance Géochimique Géochimique ActivitésActivités En-cours En-cours et et Futures Futures du du Programme Programme NRG NRG en en Colombie Colombie Britannique, Britannique, P.W.B.P.W.B. Friske, Friske,S.J.A.S.J.A. Day, Day, M.W. M.W. McCurdy McCurdy and and R.J. R.J. McNeil McNeil auau Territoires Territoires de du Nord-Ouest, Nord-Ouest, au au Territoire Territoire du du Yukon Yukon et et en en Alberta, Alberta, 2005-06 2005-06 GeologicalGeological Survey Survey of of Canada Canada 601601 Booth Booth St, St, Ottawa, Ottawa, ON ON 11 Area: Edéhzhie (Horn Plateau), NT 55 Area: Old Crow, YT H COLU Survey was conducted in conjunction with Survey was conducted in conjunction with and funded by IS M EUB IT B and funded by NTGO, INAC and NRCAN. NORTHWEST TERRITORIES R I the Yukon Geological Survey and NRCAN. Data will form A 124° 122° 120° 118° 116° B Alberta Energy and Utilities Board Data will form the basis of a mineral potential GEOSCIENCE 95N 85O the basis of a mineral potential evaluation as part of a 95O 85N evaluation as part of a larger required 95P 85M larger required Resource Assessment. OFFICE .Wrigley RESEARCH ANALYSIS INFORMATION Resource Assessment. .Wha Ti G 63° YUKON 63° Metals in the Environment (MITE) E Y AGS ESS Program: O E ESS Program: Metals in the Environment V .Rae-Edzo L R GSEOLOGICAL URVEY Survey Type: Stream Sediment and Stream Water OG SU Alberta Geological Survey (MITE) ICAL 95K 85J 95J 85K OF 95I4674 85L Survey Type: Stream Sediment, stream M Year of Collection: 2004 and 2005 A C K ENZI E R 2 62° I V water, bulk stream sediment (HMCs and KIMs). -
Arviat, ᐊᕐᕕᐊᑦ, “Place of the Bowhead Whale”
Arviat, ᐊᕐᕕᐊᑦ, “Place of the bowhead whale” Kugaaruk, ᑰᒑᕐᔪ, “Little stream” Introduction Kugaaruk is located on the southwest shore of the Simpson Peninsula, on the east side of Pelly Bay in the Kitikmeot region. In 2016 the population was 933. The wildlife economy plays an important role in Kugaaruk, with many residents supporting themselves by hunting, fishing, trapping, and gathering. Community members also participate in wage-based economic activities1. Important coastal resources in the Kugaaruk region include bowhead whales, narwhals, seals, polar bears, and Arctic char, with residents sometimes travelling long distances to reach hunting and fishing grounds2. The community’s hunting and fishing area includes Pelly Bay, Boothia Peninsula, Committee Bay, Rae Strait, and The Gulf of Boothia2. Current there are no national or territorial parks located near Kugaaruk, however, several fishing and hunting camps exist nearby. Community Restoration Priorities 1. The restoration of key fishing rivers and monitoring of water quality and fish health in local waterbodies, as water levels are too low, and rivers are drying up - remediation action and new infrastructure will be required; and 2. Observed changes in water quality and fish health in some areas have been noted for awhile. A community-led water quality and fish health monitoring programs should be put in place. Community Map and Workshop Highlights The CRN research team visited the community in March 2019. Literature Review Kugaaruk is characterized by coastal mountains and well-vegetated lowlands with several lakes, rivers, and ponds throughout the region, which provide important habitat for a variety of plants and animals2. Land-fast lead systems are areas of separated land-fast ice and pack ice and can be found throughout this region2. -
At Nanoq's Home, Searching the King of the Arctic
AT NANOQ'S HOME, SEARCHING THE KING OF THE ARCTIC 1.000 Km route in Baffin island in a sled conditioned for travellers hauled by a snowmobile to watch polar bears with an Inuit experts on tracking Arctic wildlife 1000 Km route in a sled conditioned for travellers hauled by snowmobile through the frozen ice sea of the big Baffin Island, located in the Canadian High Arctic, nearly 3,000 km north of the great cities in Canada. Guided by Inuits with lot of experience in polar bear tracking, we will cross the frozen sea on the east coast of Baffin, in search of the world's largest carnivore. This area is considered one of the world's Capital of Polar Bear or "Nanoq" as Inuits call this amazing animal. Our trip starts in the small Inuit town of Kanngiqtugaapik, located on the East coast of Baffin. Our goal is to observe, photograph and film the Polar Bear in freedom. Therefore we are going into his territory, where this enormous plantigrade is without question “the King ”. Observing this great mammal in its natural habitat is a real privilege reserved only for those who venture into the endless white landscapes. Accompanied by Inuits expert in tracking of Arctic fauna, we will advance on the icy ice pack of Isabella and Home Bay, where pressure ridges, ice plains, snowdrifts and floating ice floes follow each other. This favorite hunting place for polar bears. In this area there is also a good chance of watching seals lying on the ice near their breathing holes. -
Radiocarbon Dates Iv \V
I RADIO(;AIn ', A oi.. 7, 1965, l'. 24-461 GEOLOGICAL SURVEY OF CANADA RADIOCARBON DATES IV \V. DYCK, J. C. FYLES, and W. BLAKE, JR.* Geological Survey of Canada, Ottawa, Canada 1NTR )I)U TION Most of the determinations reported here were obtained with the 2 L counter described in our first date list ( CSC I ) . All age calculations are based oh a C1 t half-life of 5568 + 30 yr and 0.95 of the activity of the NBS oxalic- acid standard, and the ages are quoted in years before 1950. The age errors include : counting errors of sample, background, and standard, the error in the half-life of C14, and an error term to account for the average variation of :± 1.5/ in the C'4 concentration during the past 1100 yr. `Greater than' ages are based on the 4 rr criterion I GSC I I l . After extensive testing and modification a 5 L counter was brought into routine operation in April, 1961.Its more important counting characteristics are given in Table 1. The background increases somewhat with an increase in pressure, but the C14 and meson plateaus improve. The apparent non-linearity in the counting rate of the standard is probably due to the arbitrary choice of the operating point on the plateau. The counter was constructed from a 51,4 in. 0.1)., in, wall copper tube having an overall length of 20 in. Approx. 30 mils were removed from the inner surface of the tube, by machining on a lathe, to provide a contamination- fre surface. -
Gjoa Haven © Nunavut Tourism
NUNAVUT COASTAL RESOURCE INVENTORY ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut Ministère de l’Environnement Gjoa Haven © Nunavut Tourism ᐊᕙᑎᓕᕆᔨᒃᑯᑦ Department of Environment Avatiliqiyikkut NUNAVUT COASTAL RESOURCE INVENTORY • Gjoa Haven INVENTORY RESOURCE COASTAL NUNAVUT Ministère de l’Environnement Nunavut Coastal Resource Inventory – Gjoa Haven 2011 Department of Environment Fisheries and Sealing Division Box 1000 Station 1310 Iqaluit, Nunavut, X0A 0H0 GJOA HAVEN Inventory deliverables include: EXECUTIVE SUMMARY • A final report summarizing all of the activities This report is derived from the Hamlet of Gjoa Haven undertaken as part of this project; and represents one component of the Nunavut Coastal Resource Inventory (NCRI). “Coastal inventory”, as used • Provision of the coastal resource inventory in a GIS here, refers to the collection of information on coastal database; resources and activities gained from community interviews, research, reports, maps, and other resources. This data is • Large-format resource inventory maps for the Hamlet presented in a series of maps. of Gjoa Haven, Nunavut; and Coastal resource inventories have been conducted in • Key recommendations on both the use of this study as many jurisdictions throughout Canada, notably along the well as future initiatives. Atlantic and Pacific coasts. These inventories have been used as a means of gathering reliable information on During the course of this project, Gjoa Haven was visited on coastal resources to facilitate their strategic assessment, two occasions: -
Polar Bear Hunting: Three Areas \Vere Most Important for Hunting Was Less Mtensive South of Shaftesbury Inlet, Where Polar Bear
1Ire8, whenever seen, most often when people • SlImmary: In compan on with othcr Kcc\\attn settlements. ibou or trappmg. the people of Chesterfield use a rclati\"cl) small arca of land. ÏlItt11iDl Hunting. 80th ringed and bearded seals Chesterfield is a small c1osc-knit seulement. and evcryone year rooud. In sommer people hunt along shares the land and game of the area. There is usually JnIet toParther Hope Point including Barbour suffieient supply of game nearby without their having to e coast from Whale Cove to Karmarvik Harbour, travel very far. Many people are also wage carners and are omiles mland. For mueh of the year people hunt Iimited to day and weekend hunting trips, exeept for holiday' 'h . d 1 oe èdge, which is usually three or four miles out ln t e spnng an summer. ement; however, the distance varies along The area most important to the people of Chesterfield is !'the pnncipal seal hunting season is spring, w en the mouth of the inlet. north along the coast from Cape the ice. At this time, too, young seals are hunted Silumiut to Daly Bay: and ülland to nearby caribou hunting lairs. The area from Baker Foreland to Bern and fishmg areas. ThiS rcglOn 15 nch ln gamc. and il COI1 and along Chesterfield Inlet to Big Island is weil stitutes the traditional hunting ground for 1110st of the :Cape Silumiut area is extremely popular for week Chesterfield people. Il does not overlap with land cOJnmonly trips, and people often hunt atthe floe edge near used by any other seUlement, although people from Rankin t. -
Canada Topographical
University of Waikato Library: Map Collection Canada: topographical maps 1: 250,000 The Map Collection of the University of Waikato Library contains a comprehensive collection of maps from around the world with detailed coverage of New Zealand and the Pacific : Editions are first unless stated. These maps are held in storage on Level 1 Please ask a librarian if you would like to use one: Coverage of Canadian Provinces Province Covered by sectors On pages Alberta 72-74 and 82-84 pp. 14, 16 British Columbia 82-83, 92-94, 102-104 and 114 pp. 16-20 Manitoba 52-54 and 62-64 pp. 10, 12 New Brunswick 21 and 22 p. 3 Newfoundland and Labrador 01-02, 11, 13-14 and 23-25) pp. 1-4 Northwest Territories 65-66, 75-79, 85-89, 95-99 and 105-107) pp. 12-21 Nova Scotia 11 and 20-210) pp. 2-3 Nunavut 15-16, 25-27, 29, 35-39, 45-49, 55-59, 65-69, 76-79, pp. 3-7, 9-13, 86-87, 120, 340 and 560 15, 21 Ontario 30-32, 40-44 and 52-54 pp. 5, 6, 8-10 Prince Edward Island 11 and 21 p. 2 Quebec 11-14, 21-25 and 31-35 pp. 2-7 Saskatchewan 62-63 and 72-74 pp. 12, 14 Yukon 95,105-106 and 115-117 pp. 18, 20-21 The sector numbers begin in the southeast of Canada: They proceed west and north. 001 Newfoundland 001K Trepassey 3rd ed. 1989 001L St: Lawrence 4th ed. 1989 001M Belleoram 3rd ed. -
Seasonal Summary
Canadian Ice Service Seasonal Summary for the Canadian Arctic Summer 2009 Produced by the Canadian Ice Service November 06th, 2009 Seasonal Summary - Canadian Arctic Waters - Summer 2009 -1- Canadian Ice Service Table of Contents Hudson and Foxe .......................................................................................................... 4 June 2009.................................................................................................................... 4 July 2009 ..................................................................................................................... 5 August 2009 ................................................................................................................ 5 September 2009 .......................................................................................................... 6 Eastern and High Arctic.............................................................................................. 12 June 2009.................................................................................................................. 12 July 2009 ................................................................................................................... 13 August 2009 .............................................................................................................. 13 September 2009 ........................................................................................................ 14 Western and Central Arctic ....................................................................................... -
And Oceans, Iqaluit, Wunayl!L! I I I
Arctic Biological Consultants for Canada Department gfFisheries ' and Oceans, Iqaluit, WuNaYl!l! I I I I INUIT KNOWLEDGE OF BELUGAS AND NARWHALS I IN THE CANADIAN EASTERN ARCTIC I I l by I I D.8. Stewart I Arctic Biological Consultants Box 68, St. Norbert Postal Station 95 Turnbull Drive I Winnipeg, Manitoba CANADA R3V 1L5 I stewart4@m b.sym patico.ca I I 2001 I I I ii PREFACE This report was prepared under contract for the Canadian Department of Fisheries and Oceans. Scientific Authorities for this contract were Karen Ditz of the Department of Fisheries and Oceans, Iqaluit, NT, Canada, XOA OHO and Pierre Richard , Department of Fisheries and Oceans, 501 University Crescent, Winnipeg, Manitoba, R3T 2N6. Correct citation for this report is: Stewart, D. B. 2001 . Inuit knowledge of belugas and narwhals in the Canadian eastern Arctic. Prepared by Arctic Biological Consultants, Winnipeg, MB for Canada Department of Fisheries and Oceans, Iqaluit, Nunavut. iv+ 32 p. I iii I TABLE OF CONTENTS ABSTRACT/RESUME . iv 5 Areas where hunters have observed INTRODUCTION . 1 belugas during auja (summer) . 20 METHODS ...... ... .. .. .. ... .... 1 I Sampling method . .. .. .. .. 6 Areas where hunters have observed Questionnaire versus workshop approach belugas during ukiaksak (early fall) . 21 Knowledge versus opinion . 2 I Area coverage . 2 7 Areas where hunters have observed Seasonal observations . 2 belugas during ukia (late fall) . 22 INUIT KNOWLEDGE OF BELUGAS . 3 I Seasonal distribution and movements . 3 8 Areas where belugas have been Changes in seasonal distribution found entrapped by ice . 23 and behaviour . 6 I Reproduction . 7 9 Areas where hunters have observed Food and feeding . -
'Round Lord Mayor Bay with James Clark Ross: the Original Diary Of
ARCTIC VOL. 43, NO. 1 (MARCH 1990) P. 66-79 ’Round Lord MayorBay with James Clark Ross: The Original Diaryof 1830 REAR ADMIRAL JAMES ROSS’and JAMES M. SAVELLE2 (Received 30 June 1988; accepted in revisedform 17 July 1989) ABSTRACT. During John Ross’s arctic expedition of 1829-33 in search of a northwest passage, approximately 1000 km of new coastlinewas mapped. Included in these new coastlineswas Lord MayorBay on eastern Boothia Peninsula, which was surveyed by Ross’s nephew and second-in-command, James Clark Ross, in1830. The results of the Lord MayorBay survey effectively ended any chance of there being a northwest passage south andeast of Somerset Island or west of northern Foxe Basinand northwest Hudson Bay. Despite the obvious importance of James Clark Ross’s survey, it was not included in John Ross’s published narrative of the expedition. The original diary hasrecently been located and is reproduced here, together with accompanying sketches and observations and a discussion of the circumstances of the survey. Key words: James Clark Ross, Lord Mayor Bay,1829-33, unpublished diary,arctic exploration RESUME.Aucoursdel’ex~itiondeJohnRossdansl’ArctiqueBlarecherchedupassageduNord~estdel829il833,futdress~elacarte&environ 1000 km de nouveau littoral. Sur ce nouveau littoral se trouvaitla baie Lord Mayorsur la partie orientale de la peninsule de Boothia, dont le relev6 fut effectue en 1830 par James Clark Ross, neveu de Ross et commandant en second. Les resultats desreleves de la baie Lord Mayormirent fin une fois pour toutes B la possibilite de trouver unpassage vers le Nord-Ouest au sud et i l’est de l’ile Somerset ou B l’ouest de la partie septentrionale du bassin de Foxe et du nord-ouest de la baie &Hudson. -
The Hudson Bay Lithospheric Experiment (Huble): Insights Into Precambrian Plate Tectonics and the Development of Mantle Keels
Downloaded from http://sp.lyellcollection.org/ by guest on September 25, 2021 The Hudson Bay Lithospheric Experiment (HuBLE): insights into Precambrian plate tectonics and the development of mantle keels I. D. BASTOW1*, D. W. EATON2, J.-M. KENDALL3, G. HELFFRICH3, D. B. SNYDER4, D. A. THOMPSON5, J. WOOKEY3, F. A. DARBYSHIRE6 & A. E. PAWLAK2 1Department of Earth Science and Engineering, Imperial College London, London SW7 2AZ, UK 2Department of Geoscience, University of Calgary, Alberta, Canada T2N 1N4 3Department of Earth Sciences, University of Bristol, Bristol BS8 1RJ, UK 4Geological Survey of Canada, Natural Resources Canada, Ottawa, Ontario, Canada K1A 0E9 5School of Earth and the Environment, University of Leeds, Leeds LS2 9JT, UK 6Centre de Recherche GEOTOP, Universite´ du Que´bec a´ Montre´al, Montre´al, Que´bec, Canada H3C 3P8 *Corresponding author (e-mail: [email protected]) Abstract: Hudson Bay Lithospheric Experiment (HuBLE) was designed to understand the pro- cesses that formed Laurentia and the Hudson Bay basin within it. Receiver function analysis shows that Archaean terranes display structurally simple, uniform thickness, felsic crust. Beneath the Palaeoproterozoic Trans-Hudson Orogen (THO), thicker, more complex crust is inter- preted as evidence for a secular evolution in crustal formation from non-plate-tectonic in the Palaeoarchaean to fully developed plate tectonics by the Palaeoproterozoic. Corroborating this hypothesis, anisotropy studies reveal 1.8 Ga plate-scale THO-age fabrics. Seismic tomography shows that the Proterozoic mantle has lower wavespeeds than surrounding Archaean blocks; the Laurentian keel thus formed partly in post-Archaean times. A mantle transition zone study indi- cates ‘normal’ temperatures beneath the Laurentian keel, so any cold mantle down-welling associ- ated with the regional free-air gravity anomaly is probably confined to the upper mantle.