Stock Definition of Belugas and Narwhals in Nunavut
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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. -
EXPERIENCES 2021 Table of Contents
NUNAVUT EXPERIENCES 2021 Table of Contents Arts & Culture Alianait Arts Festival Qaggiavuut! Toonik Tyme Festival Uasau Soap Nunavut Development Corporation Nunatta Sunakkutaangit Museum Malikkaat Carvings Nunavut Aqsarniit Hotel And Conference Centre Adventure Arctic Bay Adventures Adventure Canada Arctic Kingdom Bathurst Inlet Lodge Black Feather Eagle-Eye Tours The Great Canadian Travel Group Igloo Tourism & Outfitting Hakongak Outfitting Inukpak Outfitting North Winds Expeditions Parks Canada Arctic Wilderness Guiding and Outfitting Tikippugut Kool Runnings Quark Expeditions Nunavut Brewing Company Kivalliq Wildlife Adventures Inc. Illu B&B Eyos Expeditions Baffin Safari About Nunavut Airlines Canadian North Calm Air Travel Agents Far Horizons Anderson Vacations Top of the World Travel p uit O erat In ed Iᓇᓄᕗᑦ *denotes an n u q u ju Inuit operated nn tau ut Aula company About Nunavut Nunavut “Our Land” 2021 marks the 22nd anniversary of Nunavut becoming Canada’s newest territory. The word “Nunavut” means “Our Land” in Inuktut, the language of the Inuit, who represent 85 per cent of Nunavut’s resident’s. The creation of Nunavut as Canada’s third territory had its origins in a desire by Inuit got more say in their future. The first formal presentation of the idea – The Nunavut Proposal – was made to Ottawa in 1976. More than two decades later, in February 1999, Nunavut’s first 19 Members of the Legislative Assembly (MLAs) were elected to a five year term. Shortly after, those MLAs chose one of their own, lawyer Paul Okalik, to be the first Premier. The resulting government is a public one; all may vote - Inuit and non-Inuit, but the outcomes reflect Inuit values. -
Wolf-Sightings on the Canadian Arctic Islands FRANK L
ARCTIC VOL. 48, NO.4 (DECEMBER 1995) P. 313–323 Wolf-Sightings on the Canadian Arctic Islands FRANK L. MILLER1 and FRANCES D. REINTJES1 (Received 6 April 1994; accepted in revised form 13 March 1995) ABSTRACT. A wolf-sighting questionnaire was sent to 201 arctic field researchers from many disciplines to solicit information on observations of wolves (Canis lupus spp.) made by field parties on Canadian Arctic Islands. Useable responses were obtained for 24 of the 25 years between 1967 and 1991. Respondents reported 373 observations, involving 1203 wolf-sightings. Of these, 688 wolves in 234 observations were judged to be different individuals; the remaining 515 wolf-sightings in 139 observations were believed to be repeated observations of 167 of those 688 wolves. The reported wolf-sightings were obtained from 1953 field-weeks spent on 18 of 36 Arctic Islands reported on: no wolves were seen on the other 18 islands during an additional 186 field-weeks. Airborne observers made 24% of all wolf-sightings, 266 wolves in 48 packs and 28 single wolves. Respondents reported seeing 572 different wolves in 118 separate packs and 116 single wolves. Pack sizes averaged 4.8 ± 0.28 SE and ranged from 2 to 15 wolves. Sixty-three wolf pups were seen in 16 packs, with a mean of 3.9 ± 2.24 SD and a range of 1–10 pups per pack. Most (81%) of the different wolves were seen on the Queen Elizabeth Islands. Respondents annually averaged 10.9 observations of wolves ·100 field-weeks-1 and saw on average 32.2 wolves·100 field-weeks-1· yr -1 between 1967 and 1991. -
Transits of the Northwest Passage to End of the 2020 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2020 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 7 April 2021 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. <[email protected]> The earliest traverse of the Northwest Passage was completed in 1853 starting in the Pacific Ocean to reach the Atlantic Oceam, but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 319 complete maritime transits of the Northwest Passage have been made to the end of the 2020 navigation season, before winter began and the passage froze. These transits proceed to or from the Atlantic Ocean (Labrador Sea) in or out of the eastern approaches to the Canadian Arctic archipelago (Lancaster Sound or Foxe Basin) then the western approaches (McClure Strait or Amundsen Gulf), across the Beaufort Sea and Chukchi Sea of the Arctic Ocean, through the Bering Strait, from or to the Bering Sea of the Pacific Ocean. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the central or northern coast of west Greenland. The routes and directions are indicated. Details of submarine transits are not included because only two have been reported (1960 USS Sea Dragon, Capt. George Peabody Steele, westbound on route 1 and 1962 USS Skate, Capt. Joseph Lawrence Skoog, eastbound on route 1). Seven routes have been used for transits of the Northwest Passage with some minor variations (for example through Pond Inlet and Navy Board Inlet) and two composite courses in summers when ice was minimal (marked ‘cp’). -
Thermodynamic and Dynamic Ice Thickness Contributions in the Canadian Arctic Archipelago in NEMO-LIM2 Numerical Simulations
The Cryosphere, 12, 1233–1247, 2018 https://doi.org/10.5194/tc-12-1233-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Thermodynamic and dynamic ice thickness contributions in the Canadian Arctic Archipelago in NEMO-LIM2 numerical simulations Xianmin Hu1,a, Jingfan Sun1,b, Ting On Chan1,c, and Paul G. Myers1 1Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, T6G 2E3, Canada anow at: Bedford Institute of Oceanography, Fisheries and Oceans Canada, Dartmouth, Nova Scotia, Canada bnow at: School of Electrical and Computer Engineering, Georgia Institute of Technology, Atlanta, GA, USA cnow at: Skytech Solutions Ltd., Canada Correspondence: Xianmin Hu ([email protected]) Received: 6 September 2017 – Discussion started: 10 October 2017 Revised: 16 March 2018 – Accepted: 19 March 2018 – Published: 10 April 2018 Abstract. Sea ice thickness evolution within the Canadian is found in the northern CAA and Baffin Bay while a de- Arctic Archipelago (CAA) is of great interest to science, as cline (r2 ≈ 0:6, p < 0:01) is simulated in Parry Channel re- well as local communities and their economy. In this study, gion. The two main contributors (thermodynamic growth and based on the NEMO numerical framework including the lateral transport) have high interannual variabilities which LIM2 sea ice module, simulations at both 1=4 and 1=12◦ hor- largely balance each other, so that maximum ice volume can izontal resolution were conducted from 2002 to 2016. The vary interannually by ±12 % in the northern CAA, ±15 % in model captures well the general spatial distribution of ice Parry Channel, and ±9 % in Baffin Bay. -
Canada's Sovereignty Over the Northwest Passage
Michigan Journal of International Law Volume 10 Issue 2 1989 Canada's Sovereignty Over the Northwest Passage Donat Pharand University of Ottawa Follow this and additional works at: https://repository.law.umich.edu/mjil Part of the International Law Commons, and the Law of the Sea Commons Recommended Citation Donat Pharand, Canada's Sovereignty Over the Northwest Passage, 10 MICH. J. INT'L L. 653 (1989). Available at: https://repository.law.umich.edu/mjil/vol10/iss2/10 This Article is brought to you for free and open access by the Michigan Journal of International Law at University of Michigan Law School Scholarship Repository. It has been accepted for inclusion in Michigan Journal of International Law by an authorized editor of University of Michigan Law School Scholarship Repository. For more information, please contact [email protected]. CANADA'S SOVEREIGNTY OVER THE NORTHWEST PASSAGE Donat Pharand* In 1968, when this writer published "Innocent Passage in the Arc- tic,"' Canada had yet to assert its sovereignty over the Northwest Pas- sage. It has since done so by establishing, in 1985, straight baselines around the whole of its Arctic Archipelago. In August of that year, the U. S. Coast Guard vessel PolarSea made a transit of the North- west Passage on its voyage from Thule, Greenland, to the Chukchi Sea (see Route 1 on Figure 1). Having been notified of the impending transit, Canada informed the United States that it considered all the waters of the Canadian Arctic Archipelago as historic internal waters and that a request for authorization to transit the Northwest Passage would be necessary. -
In Arctic and Subarctic Seas, and the Modifying Ejfects of Hydrographic Differences in the Environment'
The Journal of Marine Research is an online peer-reviewed journal that publishes original research on a broad array of topics in physical, biological, and chemical oceanography. In publication since 1937, it is one of the oldest journals in American marine science and occupies a unique niche within the ocean sciences, with a rich tradition and distinguished history as part of the Sears Foundation for Marine Research at Yale University. Past and current issues are available at journalofmarineresearch.org. Yale University provides access to these materials for educational and research purposes only. Copyright or other proprietary rights to content contained in this document may be held by individuals or entities other than, or in addition to, Yale University. You are solely responsible for determining the ownership of the copyright, and for obtaining permission for your intended use. Yale University makes no warranty that your distribution, reproduction, or other use of these materials will not infringe the rights of third parties. This work is licensed under the Creative Commons Attribution- NonCommercial-ShareAlike 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/4.0/ or send a letter to Creative Commons, PO Box 1866, Mountain View, CA 94042, USA. Journal of Marine Research, Sears Foundation for Marine Research, Yale University PO Box 208118, New Haven, CT 06520-8118 USA (203) 432-3154 fax (203) 432-5872 [email protected] www.journalofmarineresearch.org The Life Cycle of Sagitta elegans in Arctic and Subarctic Seas, and the Modifying Ejfects of Hydrographic Differences in the Environment' M. -
ENGLISH 261 Summer18
ENGLISH 261 ARCTIC ENCOUNTERS 4-6:10, Gaige Hall 303 (days vary) Dr. Russell A. Potter http://eng261.blogspot.com There are few places left on earth where simply going there seems extraordinary – but a trip north of the Arctic Circle still seems to signify the experience of something astonishing. This course takes up the history of human exploration and interaction in the Arctic, from the early days of the nineteenth century to the present, with a focus on contact between European and American explorers and the Eskimo, or Inuit as they are more properly known today. We read first-hand accounts and view dramatic films and documentaries that recount these histories, both from the Western and the Inuit side of the story. Each week, we’ll have new readings both in our books and online, and a response to one of that week’s blog posts is due. There will also be a final paper of 4-6 pages on a topic of the student’s choosing related to our course subjects. This summer, we’ll also have an unusual opportunity: I’ll be teaching the second half of the course from on board a ship in the Arctic! As I have in past summers, I’ll be aboard the research vessel Akademik Ioffe as part of a team of experts working with passengers on a series of expedition cruises. I’ll be in the Canadian Maritimes, Newfoundland and Labrador, and eventually in Nunavut heading up the coast of Baffin Island. I’ll be posting text, and some pictures (the limited bandwidth of the ship’s e-mail means that these will mostly be rather small ones) and posting/commenting on our class blog. -
NTI IIBA for Conservation Areas Cultural Heritage and Interpretative
NTI IIBA for Phase I: Cultural Heritage Resources Conservation Areas Report Cultural Heritage Area: Dewey Soper and Interpretative Migratory Bird Sanctuary Materials Study Prepared for Nunavut Tunngavik Inc. 1 May 2011 This report is part of a set of studies and a database produced for Nunavut Tunngavik Inc. as part of the project: NTI IIBA for Conservation Areas, Cultural Resources Inventory and Interpretative Materials Study Inquiries concerning this project and the report should be addressed to: David Kunuk Director of Implementation Nunavut Tunngavik Inc. 3rd Floor, Igluvut Bldg. P.O. Box 638 Iqaluit, Nunavut X0A 0H0 E: [email protected] T: (867) 975‐4900 Project Manager, Consulting Team: Julie Harris Contentworks Inc. 137 Second Avenue, Suite 1 Ottawa, ON K1S 2H4 Tel: (613) 730‐4059 Email: [email protected] Report Authors: Philip Goldring, Consultant: Historian and Heritage/Place Names Specialist Julie Harris, Contentworks Inc.: Heritage Specialist and Historian Nicole Brandon, Consultant: Archaeologist Note on Place Names: The current official names of places are used here except in direct quotations from historical documents. Names of places that do not have official names will appear as they are found in the source documents. Contents Maps and Photographs ................................................................................................................... 2 Information Tables .......................................................................................................................... 2 Section -
Canadian Arctic Tide Measurement Techniques and Results
International Hydrographie Review, Monaco, LXIII (2), July 1986 CANADIAN ARCTIC TIDE MEASUREMENT TECHNIQUES AND RESULTS by B.J. TAIT, S.T. GRANT, D. St.-JACQUES and F. STEPHENSON (*) ABSTRACT About 10 years ago the Canadian Hydrographic Service recognized the need for a planned approach to completing tide and current surveys of the Canadian Arctic Archipelago in order to meet the requirements of marine shipping and construction industries as well as the needs of environmental studies related to resource development. Therefore, a program of tidal surveys was begun which has resulted in a data base of tidal records covering most of the Archipelago. In this paper the problems faced by tidal surveyors and others working in the harsh Arctic environment are described and the variety of equipment and techniques developed for short, medium and long-term deployments are reported. The tidal characteris tics throughout the Archipelago, determined primarily from these surveys, are briefly summarized. It was also recognized that there would be a need for real time tidal data by engineers, surveyors and mariners. Since the existing permanent tide gauges in the Arctic do not have this capability, a project was started in the early 1980’s to develop and construct a new permanent gauging system. The first of these gauges was constructed during the summer of 1985 and is described. INTRODUCTION The Canadian Arctic Archipelago shown in Figure 1 is a large group of islands north of the mainland of Canada bounded on the west by the Beaufort Sea, on the north by the Arctic Ocean and on the east by Davis Strait, Baffin Bay and Greenland and split through the middle by Parry Channel which constitutes most of the famous North West Passage. -
The Quest for the Northwest Passage, by James P. Delgado
REVIEWS • 323 learn the identity of what they have been reading up to that BRAY, E.F. de. 1992. A Frenchman in search of Franklin: De point. The document identified as HBCA E.37/3, which Bray’s Arctic journal, 1852–1854. Edited by William Barr. Barr, following Anderson, refers to as a full journal Toronto and Buffalo: University of Toronto Press. (p. 166, n.1), turns out to be what I would call Anderson’s PELLY, D. 1981. Expedition: An Arctic journey through history on field notes, written daily during the expedition. In con- George Back’s River. Toronto: Betelgeuse. trast, the document that Barr has referred to in footnotes as the “fair copy of Anderson’s journal” (HBCA B.200/a/ I.S. MacLaren 31), although based on those field notes, was written after Canadian Studies Program the expedition: it shows signs of revision and narrative Department of Political Science polish. Barr’s use of the term journal to refer to both University of Alberta documents is misleading, as it blurs that important distinc- Edmonton, Alberta, Canada tion. Furthermore, justification for subordinating Stewart’s T6G 2H4 journal (Provincial Archives of Alberta 74.1/137) to Anderson’s is rendered only implicitly: Stewart’s is “gen- erally less detailed than” Anderson’s (p. 166–167). One is ACROSS THE TOP OF THE WORLD: THE QUEST FOR left to infer that the editing accords with the chain of THE NORTHWEST PASSAGE. By JAMES P. DELGADO. command, Stewart being Anderson’s junior. None of these Vancouver and Toronto: Douglas & McIntyre, 1999. -
Quaternary Geology of Bluegoose Prairie, Baffin Island, Nunavut
QUATERNARY GEOLOGY OF BLUEGOOSE PRAIRIE, BAFFIN ISLAND, NUNAVUT by Kayla J. Vickers B.Sc., University of Alberta, 2004 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE In the Department of Earth Sciences © Kayla J. Vickers 2011 SIMON FRASER UNIVERSITY Spring 2011 All rights reserved. However, in accordance with the Copyright Act of Canada, this work may be reproduced, without authorization, under the conditions for Fair Dealing. Therefore, limited reproduction of this work for the purposes of private study, research, criticism, review and news reporting is likely to be in accordance with the law, particularly if cited appropriately. APPROVAL Name: Kayla Vickers Degree: Master ofScience Title of Thesis: Quaternary Geology of Bluegoose Prairie, Baffin Island, Nunavut Examining Committee: Chair: Dr. Gwenn Flowers Associate Professor, Department ofEarth Sciences Dr. Brent Ward Senior Supervisor Associate Professor, Department ofEarth Sciences "By video teleconference from Halifax. Nova Scotia" Mr. Daniel Utting Supervisor Geologist, Nova Scotia Department ofNatural Resources Dr. Olav Lian Supervisor Adjunct, Department ofEarth Sciences Dr. Rod Smith External Examiner Geological Survey ofCanada th Date Defended/Approved: April 13 • 2011 II Declaration of Partial Copyright Licence The author, whose copyright is declared on the title page of this work, has granted to Simon Fraser University the right to lend this thesis, project or extended essay to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users.