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												  Cultural Heritage Resources ReportNTI IIBA for Phase I Draft: Conservation Cultural Heritage Areas Resources Report Cultural Heritage Area: Akpait and and Interpretative Qaqulluit National Wildlife Materials Study Areas 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Archaeologist Note on Place Names: The current official names of places are used here except in direct quotations from historical documents. Throughout the document “Qikiqtarjuaq” refers to the settlement established in the 1950s and previously known as Broughton Island. Except when used in a direct quotation, the term “Broughton Island” in the report refers to the geographic feature (the island) on which the community of Qikiqtarjuaq is located. Names of places that do not have official names will appear as they are found in
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												  Polar Bear Hunting: Three Areas \Vere Most Important for Hunting Was Less Mtensive South of Shaftesbury Inlet, Where Polar Bear1Ire8, 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.
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												  Territorial Sea Geographical Coordinates (Area 7) Décret Sur Les Coordonnées Géographiques Pour La Order Mer Territoriale (Région 7)CANADA CONSOLIDATION CODIFICATION Territorial Sea Geographical Décret sur les coordonnées Coordinates (Area 7) Order géographiques pour la mer territoriale (région 7) SOR/85-872 DORS/85-872 Current to September 11, 2021 À jour au 11 septembre 2021 Published by the Minister of Justice at the following address: Publié par le ministre de la Justice à l’adresse suivante : http://laws-lois.justice.gc.ca http://lois-laws.justice.gc.ca OFFICIAL STATUS CARACTÈRE OFFICIEL OF CONSOLIDATIONS DES CODIFICATIONS Subsections 31(1) and (3) of the Legislation Revision and Les paragraphes 31(1) et (3) de la Loi sur la révision et la Consolidation Act, in force on June 1, 2009, provide as codification des textes législatifs, en vigueur le 1er juin follows: 2009, prévoient ce qui suit : Published consolidation is evidence Codifications comme élément de preuve 31 (1) Every copy of a consolidated statute or consolidated 31 (1) Tout exemplaire d'une loi codifiée ou d'un règlement regulation published by the Minister under this Act in either codifié, publié par le ministre en vertu de la présente loi sur print or electronic form is evidence of that statute or regula- support papier ou sur support électronique, fait foi de cette tion and of its contents and every copy purporting to be pub- loi ou de ce règlement et de son contenu. Tout exemplaire lished by the Minister is deemed to be so published, unless donné comme publié par le ministre est réputé avoir été ainsi the contrary is shown. publié, sauf preuve contraire. ... [...] Inconsistencies in regulations
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												  Glaciers of CanadaGlaciers of North America— GLACIERS OF CANADA GLACIERS OF THE ARCTIC ISLANDS GLACIERS OF BAFFIN ISLAND By JOHN T. ANDREWS With sections on BARNES ICE CAP: GEOMORPHOLOGY AND THERMODYNAMICS By GERALD HOLDSWORTH LATE 20TH CENTURY CHANGE AT THE BARNES ICE CAP MARGIN By JOHN D. JACOBS SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The glaciers on Baffin Island are primarily ice caps or ice fields and associated valley outlet glaciers and include numerous small glaciers as well. The two largest ice caps, the Barnes Ice Cap (5,935 km2) and the Penny Ice Cap (5,960 km2) are thought to be the last remnants of the Laurentide Ice Sheet. Approximately 8 percent of Baffin Island is covered by glaciers (36,839 km2). Nearby Bylot Island is heavily glacierized; it has 4,859 km2 of its area covered by glaciers, about 45 percent of the island. The Barnes Ice Cap has been slowly shrinking; the recession could accelerate if significant regional warming were to take place CONTENTS Page Abstract ---------------------------------------------------------------------------- J165 Introduction----------------------------------------------------------------------- 165 FIGURE 1. Sketch map of Baffin Island and adjacent regions ------------- 166 TABLE 1. Selected climatic data for climatic regions on Baffin Island and environs ------------------------------------------------- 167 Distribution of Glaciers --------------------------------------------------------
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												  Distribution and Migration of the Bowhead Whale, Balaena Mysticetus, in the Eastern North American ArcticARCTIC VOL. 36, NO. 1 (MARCH lW)P. 5-64 Distribution and Migration of the Bowhead Whale, Baluenu mysticetus, in the Eastern North American Arctic RANDALL REEVES,’ EDWARD MITCHELL,’ ARTHUR MANSFIELD,’ and MICHELE MCLAUGHLIN’.~ ABSTRACT. Largecatches of bowhead whales, Bulaena mysficerus, were made in the Eastern Arctic of NorthAmerica, principally in Davis Strait, Baffin Bay, the Lancaster Sound region, Hudson Bay, and southern Foxe Basin, between 1719 and 1915. Initial stock sizes have been estimated as 1 I OOO in 1825 for the “Davis Strait stock” and 680 in 1859 for the “Hudson Bay stock.” The separate identity of these two putative stocks needs confirmation through direct evidence. Three sets of data were used to evaluate historic and present-day trends in the distribution of bowheads in the Eastern Arctic andto test hypotheses concerning the nature, timing, and routes of their migration. Published records from commercial whale fisheries prior to 1915, unpublished and some publishedrecords from the post-commercial whaling period 1915-1974, and reportedsightings made mainly by environmental assessment per- sonnel between 1975 and 1979, were tabulated and plotted on charts. Comments made by whalers and nineteenthcentury naturalists concerning bowhead distribution and movements were summarized and critically evaluated. The major whalinggrounds were: (1) the west coast of Greenland betweenca. 60”Nand 73”N, the spring and early summer “east side” grounds of the British whalers;(2) the spring “south-west fishing” grounds, including the northeast coast of Labrador, the mouth of Hudson Strait, southeast Baftin Island, and the pack ice edge extending east from Resolution Island; (3) the summer “west water” grounds, including Pond Inlet, the Lan- caster Sound region, and Prince Regent Inlet; (4) the autumn “rock-nosing” grounds along the entire east coast of Baffin Island; (5) Cumbedand Sound, a spring and fall ground; and (6)northwest Hudson Bay/southwest Foxe Basin.
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												  Polaris: the Chief Scientist's Recollections of the American North Pole Expedition, 1871-73University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2016-11 Polaris: The Chief Scientist's Recollections of the American North Pole Expedition, 1871-73 Bessels, Emil; Barr, William (Editor and translator) University of Calgary Press http://hdl.handle.net/1880/51750 book http://creativecommons.org/licenses/by-nc-nd/4.0/ Attribution Non-Commercial No Derivatives 4.0 International Downloaded from PRISM: https://prism.ucalgary.ca POLARIS: The Chief Scientist’s Recollections of the American North Pole Expedition, 1871–73 by Emil Bessels Translated and edited by William Barr ISBN 978-1-55238-876-1 THIS BOOK IS AN OPEN ACCESS E-BOOK. It is an electronic version of a book that can be purchased in physical form through any bookseller or on-line retailer, or from our distributors. Please support this open access publication by requesting that your university purchase a print copy of this book, or by purchasing a copy yourself. If you have any questions, please contact us at [email protected] Cover Art: The artwork on the cover of this book is not open access and falls under traditional copyright provisions; it cannot be reproduced in any way without written permission of the artists and their agents. The cover can be displayed as a complete cover image for the purposes of publicizing this work, but the artwork cannot be extracted from the context of the cover of this specific work without breaching the artist’s copyright. COPYRIGHT NOTICE: This open-access work is published under a Creative Commons licence.
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												  EBSA) in the Eastern Arctic Biogeographic RegionCanadian Science Advisory Secretariat (CSAS) Research Document 2017/080 Central and Arctic Region Information in support of the evaluation of Ecologically and Biologically Significant Areas (EBSA) in the Eastern Arctic Biogeographic Region O. Schimnowski, J.E. Paulic, and K.A. Martin Fisheries and Oceans Canada Freshwater Institute 501 University Crescent Winnipeg, MB R3T 2N6 January 2018 Foreword This series documents the scientific basis for the evaluation of aquatic resources and ecosystems in Canada. As such, it addresses the issues of the day in the time frames required and the documents it contains are not intended as definitive statements on the subjects addressed but rather as progress reports on ongoing investigations. Research documents are produced in the official language in which they are provided to the Secretariat. Published by: Fisheries and Oceans Canada Canadian Science Advisory Secretariat 200 Kent Street Ottawa ON K1A 0E6 http://www.dfo-mpo.gc.ca/csas-sccs/ [email protected] © Her Majesty the Queen in Right of Canada, 2018 ISSN 1919-5044 Correct citation for this publication: Schimnowski, O., Paulic, J.E., and Martin, K.A. 2018. Information in support of the evaluation of Ecologically and Biologically Significant Areas (EBSA) in the Eastern Arctic Biogeographic Region. DFO Can. Sci. Advis. Sec. Res. Doc. 2017/080. v + 109 p. TABLE OF CONTENTS ABSTRACT ............................................................................................................................... IV RÉSUMÉ ..................................................................................................................................
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												  Clyde River InterviewsAlooloo Kautuq -Clyde River Where and when were you born? Alooloo Kautuq, born at Naqsaalukuluk, near the mouth of Sam Ford Fiord in January 11, 1949. Can you describe the areas you used to frequent during the different seasons and what you did there? When you were a child? When you were youth? When you were a young adult? Now? I spent my childhood until I became a teenager at Naqsaalukuluk. Just before I became a young man, my father died then we moved to Home Bay. Later on, my mother remarried. We lived at Home Bay for awhile, then we moved to Isabella Bay in 1967 and lived at Aulattivik Island. In 1969 we moved closer to Clyde River then in 1970, we move to Clyde River. Although we lived at Ailaqtalik and other places near Clyde River area. Because the health of my parents we had move to Clyde River. We went caribou hunting in fall using Clyde River community boat, the snow did not come for longest time that fall. It usually happen so that when the weather warms up the conditions would change. Do you think the weather has changed since you were a child? How has it changed? When did you first notice changing in the weather? Did your parent mention any changes in the weather at any time in their lifetime before you were born and started remembering? Yes my parents use to talk about the weather changing in fall and winter. How are changes in weather and surrounding land affecting your activities? What changes have you had to make as a result of these changes? The climate has changed so that I don't spend more time as I would like too do these days to work outside the house.
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												  The Maximum Extent of the Laurentide Ice Sheet Along the East Coast of North America During the Last GlaciationThe Maximum Extent of the Laurentide Ice Sheet along the East Coast of North America during the Last Glaciation JACK D. IVES ABSTRACT. During the lasthundred years, two widely opposing viewsof the maximum extent of the Laurentide Ice Sheet have prevailed at diierent times. Between 1860 and 1940, it was assumed that ice extent along the eastern seaboard was limited and that ice-free areas persisted during the Maximum of the Last Glaciation. After 1940, this interpretation was replaced by one contending that all high coastalmountains were inundated. This view,proposed by the late R.F. Flint, was widely accepted as fact until the last few years. This paper reviews the opposing interpretations and analyses the frequently equivocal field evidence and the developments of thought responsible for them. On the basis of field work carried out over the last twenty years, it is suggested that the earlier viewpoint was the more accurate. A map is presented of the author's conclusions regarding maximum ice limits. R~SUMÉ.L'étendue maximale de la couche glaciaire des Laurentides le long de la côte orientale de l'dmtrique du Nord durant la derni2re période glaciaire. Au cours des cent dernières années, deux opinions nettement opposées ont prévalu, selon les éuoques, quant l'étendue maxima de la couche glaciaire des Laurentides. De 1860 à 1940, il fut admis que l'étendue des glaces le long du littoral oriental était limitée etque des régions dépourvues de glaces persistaient aucours du Maximum de la Dernière Période Glaciaire. Après 1940, cette interprétation fut remplacée par une autre, différente, qui soutenait que toutes les hautes montagnes côtikres étaient recouvertes de glaces.
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												  Postglacial Isostatic Movement in Northeastern Devon Island: a ReappraisalPostglacial Isostatic Movement in Northeastern Devon Island: A Reappraisal WILLIAM BARR1 ABSTRACT. Amended emergence and uplift curves are presented for the Truelove Inlet area. The new curves are based mainly on radiocarbondates from whalebone, driftwood and basal peat. The marine limit lies at 76 m.a.s.l., and dates to approxi- mately 9,450 B.P., which is also considered to be the date of deglaciation; total postglacial uplift is 107 m. The rate of uplift during the first thousand years fol- lowing deglaciation reached 4.05 m. per century, which is markedly less rapid than was previously reported. The rate of uplift decreased steadily thereafter and, at present, appears tobe matched by eustatic sea level rise. What had appeared to be fossil evidence of restrained rebound at the onset of uplift, was probably due to accidental mixing during collection of interstadial shells with postglacial shells. The total amount of postglacial uplift, and the rates of uplift,have probably beensomewhat suppressed by the close proximity of the Devon Island Ice Cap. €U?!SUM& Réévaluation du mouvement isostatique postglaciaire dans le nord-est de Vile Devon. L'auteur présente des courbes corrigées d'émergence et de relèvement pour la région de Truelove Inlet. Ces nouvelles courbes sont surtout basées sur des radiodatations d'os de baleines, de bois flotté etde tourbe profonde. La limite marine se trouve à 76 m au dessus du niveau de la mer et remonte approximative- ment à 9450 A.P., ce qui est aussi considéré comme la date de la déglaciation; l'émergence postglaciaire totale est de 107 m.
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												  ARC 402 Instructions NautiquesPêches et Océans Fisheries and Oceans Canada Canada Corrigé jusgu’à l’Édition mensuelle n° 08/2021 ARC 402 PREMIÈRE ÉDITION Arctique de l’East Instructions nautiques Légende des pictogrammes Mouillage C12 C11 Quai C10 C8 C9 Port de plaisance C7 C5 Courant C4 Avertissement C6 C3 Feu Point d’appel par radio C2 Station de sauvetage C1 Pilotage Ministère des Pêches et des Océans Renseignements généraux 1-613-993-0999 Garde Cotiere canadienne Recherche et sauvetage Centre conjoint de coordination de sauvetage Trenton (Grands Lacs et Arctique) 1-800-267-7270 1-613-965-3870 (Appels par téléphone satellite, locaux ou à l’extérieur de la région) Photographie en couverture Navy Board Inlet (vue vers l’Est) Tim Janzen, SHC F A S C I C U L E A R C 4 0 2 Corrigé jusqu’à l’Édition mensuelle n° 08/2021 Instructions nautiques Arctique de l’Est Première édition 2014 Pêches et Océans Canada Les usagers de cette publication sont priés de signaler les dangers nouvellement repérés, les changements des aides à la navigation, l’existence de nouveaux hauts-fonds ou chenaux, les erreurs d’impression ou autres renseignements utiles à la correction des cartes marines et des publications hydrographiques touchant les eaux canadiennes au : Directeur général Service hydrographique du Canada Pêches et Océans Canada Ottawa (Ontario) Canada K1A 0E6 Le Service hydrographique du Canada (SHC) produit et distribue des cartes marines, des Instructions nautiques, des Tables des marées et courants du Canada et des Atlas de courants des voies navigables du Canada. On peut se procurer ces publications auprès des dépositaires autorisés du Service hydrographique du Canada.
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												  Abernethy Lowland 195 Abitibi Lowlands 518 Abitibi Upland 215INDEX Abernethy Lowland 195 Aikins Moraine 160 Abitibi lowlands 518 Alaska 24,40,119,120 Abitibi Upland 215 Alaskan Coastal Plain 129 Acadian Bay Lobe 410,416 Albany River 236 Acton, D.F 669-671,673,675 Alberta Plateau 140 Adam Till 233,236 Albertan Till 43,63,154 Adelaide Peninsula 194,208 Aleutian Trench 26 Adirondack Mountains 322,373 Alexis River 263 Advance Algoma Great Lakes 249 Battle Mountain advance 74 Algonquin Arch 326 Canmore advance 66,68 Algonquin Highlands 373 Crowfoot advance 74 Allan Park kame delta 343 Drystone Creek advance 66 Alle/Ile * see amino acid 235,286 Eisenhower Junction advance 66 Allegheny Basin 326 Labuma advance 152,164 Allerod Interval 368 Late Portage Mountain advance 54,66 Alliston embayment 344 Marquette ice advance 161,162,236,242,349 Amadjuak Lake 184,277 Obed advance 66 America Plate 25 Two Rivers advance 349 Amery Till 228,231 Waconichi ice advance 272 Amherst Silt 412 Waterton I advance 154 Amino acid racemization 5 Waterton II advance 64 Amino acid stratigraphy -definition 235,286,544,545 Waterton IV-Hidden Creek advance 65,66 Amund Ringnes Island 449 Agassiz Ice Cap 454,462,469,470,471,472 Amundsen Glaciation 121 Age Amundsen Gulf 102,127,128,132 10 ka to 8.4 ka 208,240,295,556 Anahim Belt 25,49 11 ka 207,295 Anderson Plain 131 11 ka to 10 ka 208,240,299 Anderson River 102,128,132 8.4 ka 209,297 Anderson, T.W 483-486,498-500,507-508,520-528 Cape Ball 488,491 Andrews, J.T 178-189,235,276-301,543-562 Early Pleistocene 119,152 Ange-Gardien Till 371 Early Wisconsinan 57,61,66,68,125-128,131,155,325,337