Experiences 2020
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Module 10: the Cold
i2P • AP Module 10 • The Cold War The Cold War Module 10 - Akshayuk Pass Expedition Resolute Bay, 1953 – shortly after the Inuit from Inukjuaq and Pond Inlet were relocated. “The experiment we are making this year is to transfer a few families from Port Harrison and Pond Inlet to Resolute Bay on Cornwallis Is- land and Craig Harbor and Cape Herschel, on Ellesmere Island. The primary object is to find out how Eskimos from overpopulated southern areas can adapt themselves to conditions in the high Arctic where there is at present no Eskimo population.” - Acting Deputy Minister, Department of Resources and Development, Government of Canada, August 1953. i2P • Akshayuk Pass Education Resource 1 i2P • AP Module 10 • The Cold War TERRA INCOGNITA As the i2P expedition team treks through the Akshayuk Pass, the question should be asked, “Whose land are we on?” The answer, however, is not as straightforward as one might imagine. When you look at a standard world map, all the land on the globe is allotted one color or another, and each colored area of land has a name assigned to it – which indicates the country that governs that land. There are no tracts of land on the map that are not col- ored and do not belong to an assigned country. This was not always so. In fact for some people the thought that land could be owned was completely foreign. As we learned in module 4, human beings spread around the world from an original base in Africa. As they migrated and settled, they earned their livelihood from the land, either by hunting, fishing and gathering food, or by growing livestock and crops. -
Draft – 2016 3.1.2 Territorial Parks Awaiting Full Establishment (Maps 70-84) - PA
Draft – 2016 3.1.2 Territorial Parks Awaiting Full Establishment (Maps 70-84) - PA .................................................................. 51 Chapter 1: Introduction...................................... 7 3.1.3 Proposed National Parks .................................... 51 1.1 How to Use This Document ...............................7 3.1.4 Proposed Territorial Parks (Maps 70-84) - PA...... 51 3.2 Proposed Lancaster Sound National Marine 1.2 Purpose ............................................................7 Conservation Areas (Map 85) - PA .........................52 1.3 How Land Use Decisions Were Made .................7 3.3 Conservation Areas .........................................52 1.4 Options for Land Use Policy ...............................7 3.3.1 Thelon Wildlife Sanctuary (Map 86) - PA............. 52 1.4.1 Option 1- Protected Area (PA).............................. 8 3.3.2 Migratory Bird Sanctuaries (Maps 87-99) - PA .... 53 1.4.2 Option 2 - Special Management Area (SMA)......... 8 3.3.3 National Wildlife Areas (Maps 95-99) - PA .......... 57 1.4.3 Option 3 - Mixed Use (MU) .................................. 8 3.4 Historic Sites (Maps 100-114) - PA ...................60 1.4.4 Option 4 – Information on Valued Components (VCs) ............................................................................ 8 3.5 Heritage Rivers (Maps 115-119) – PA, VEC, & VSEC ....................................................................61 1.5 Considered Information ....................................8 3.5.1 Recommendation -
Akshayuk Pass, Ski Expedition
Akshayuk Pass, Ski Expedition Program Descriptive: Akshayuk Pass, Auyuittuq National Park Majestic towers, carved in bedrock by glaciers, shooting straight for the sun: such scenery is what Auyuittuq National Park has to offer. It is, without a doubt, one of the most awe-inspiring places on Earth. Set in the middle of the Penny Ice Cap, bisected from North to South by the Akshayuk pass, an immense valley opens inland. An expedition surrounded by austere looking, barren plateaus, that will take you to two of the park’s most spectacular lookouts, Thor Peak and Mount Asgard. On your way, you will have an opportunity to see impressive rock formations dating back to the last ice age, ice caps, moraines, boulder fields, and much more. During this ski expedition, your will tread over terrain ranging from arid gravel to frozen river, with sharp peaks and a huge glacier in the backdrop. So many images that will remain with you forever. Following a 3-hour snowmobile ride from Qikiqtarjuaq we arrive at the park’s northern entrance, and then follow 11 days of cross-country skiing and 100 km of breathtaking scenery, to be crossed on skis, boots and crampons over the more difficult sections (especially the river’s ice cascades). Along the way, you will have an opportunity to see impressive rock formations dating back to the last ice age, moraines, boulder fields, with spectacular views of Mount Thor and Mount Asgard. Throughout the expedition, you will be mesmerized by the presence of glaciers, landscapes and mountains each more impressive than the last. -
Origin, Burial and Preservation of Late Pleistocene-Age Glacier Ice in Arctic
Origin, burial and preservation of late Pleistocene-age glacier ice in Arctic permafrost (Bylot Island, NU, Canada) Stephanie Coulombe1 2 3, Daniel Fortier 2 3 5, Denis Lacelle4, Mikhail Kanevskiy5, Yuri Shur5 6 1Polar Knowledge Canada, Cambridge Bay, X0B 0C0, Canada 5 2Department of Geography, Université de Montréal, Montréal, H2V 2B8, Canada 3Centre for Northern Studies, Université Laval, Quebec City, G1V 0A6, Canada 4Department of Geography, Environment and Geomatics, University of Ottawa, Ottawa, K1N 6N5, Canada 5Institute of Northern Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5910, USA 6Department of Civil and Environmental Engineering, University of Alaska Fairbanks, Fairbanks, 99775-5960, USA 10 Correspondence to: Stephanie Coulombe ([email protected]) Over the past decades, observations of buried glacier ice exposed in coastal bluffs and headwalls of retrogressive thaw slumps of the Arctic indicate that considerable amounts of late Pleistocene glacier ice survived the deglaciation and are still preserved in permafrost. In exposures, relict glacier ice and intrasedimental ice often coexist and look alike but their genesis is strikingly different. This paper aims to present a detailed description and infer the origin of a massive ice body preserved in the permafrost 15 of Bylot Island (Nunavut). The massive ice exposure and core samples were described according to the cryostratigraphic approach, combining the analysis of permafrost cryofacies and cryostructures, ice crystallography, stable O-H isotopes and cation contents. The ice was clear to whitish in appearance with large crystals (cm) and small gas inclusions (mm) at crystal intersections, similar to observations of englacial ice facies commonly found on contemporary glaciers and ice sheets. -
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. -
Auyuittuq, Hiking Expedition
Auyuittuq, Hiking Expedition Program Descriptive & Day-by-day: Auyuittuq National Park Majestic towers, carved in bedrock by glaciers, shooting straight for the sun: such scenery is what Auyuittuq National Park has to offer. It is, without a doubt, one of the most awe-inspiring places on Earth. Set in the middle of the Penny Ice Cap, bisected from North to South by the Akshayuk pass, an immense valley opens inland. After a two-day hike surrounded by severe-looking, barren plateaus, we will set up base camp. From there, you will go on a day hike to one of the most spectacular lookouts of the park, Mount Thor. On your way, you will have an opportunity to see impressive rock formations dating back to the last ice age, moraines, boulder fields, and much more. During this five-day hike, you will tread over terrain ranging from arid gravel to humid, fertile tundra, with sharp peaks and a huge glacier in the backdrop. Memories like these are unlikely to fade away. The hiking trip To hike Auyuittuq Park you will need to be able to walk with a 16 to 20 kg (35-45 lb) back pack for a distance of 8 to 18 km (5 to 12 mi) per day (4 to 8 hours a day). Trail is not technical and do not present an altitude challenge, be ready to have, at moment to cross glacier river (water high to your knees). Days will be spent in the great outdoor while nights will be spent in tent. You should be prepared to live outside for the entire trip and have minimal camping experience Kekerten Island and Pangnirtung After leaving Auyuittuq Park, an Inuit guide will take you on a boat ride to the remarkable Kekerten Island. -
Dorset Site Variation on the Southeast Coast of Baffin Island
ARCTIC VOL. 33, NO. 3 (SEPTEMBER 1980). P. 505-516 Dorset Site Variation onthe Southeast Coast of Baffin Island MOREAU S. MAXWELL’ ABSTRACT. The wide variation in Dorset residence structures may indicate seasonal site differences greater than a simple summer/ winter dichotomy. This is further suggested by a comparison of selected stone tool frequencies from Dorset sites near Lake Harbour, N.W.T. Here manufacturing activities appear to differ from springto summer to winter. The evidence also suggests that in this region Late Dorset winter settlements were located on the fast sea ice. RÉSUMÉ. La grande variation de structure dans les residences d’age Dorset, peut indiquer les différences de site saisonier plus importantes que celles du passage de l’hiverà l’été. Cela est de loin suggbré par une comparaison dans la frequénce d’outils en pierre sélectionés, provenant de sites d’age Dorset aux alentours de Lake Harbour - N.W.T. Là, les activites artisanales apparaissent changer du printemps à l’été puisàl’hiver. Dans cette region, il parait evident que les colonies hivernales d’age Dorset terminal se placaient sur la glace de mer immobilisée. Traduit par Alain de Vendegies, Aquitaine Company of Canada Ltd. INTRODUCTION Through the past 52 years of Dorset studies less attention has been paid to settlement systems than to inter-site comparisons of artifact complexes. This is partly due to the general nature of Dorset artifacts. They differ distinctively from those of other Arctic cultural periods and within specific categories theyto tend be stylistically similarover a broadarea. Artifact styles appear to conform nearly simultaneously at specific points in time. -
Importance of Auyuittuq National Park
Auyuittuq NATIONAL PARK OF CANADA Draft Management Plan January 2009 i Cover Photograph(s): (To be Added in Final Version of this Management Plan) National Library of Canada cataloguing in publication data: Parks Canada. Nunavut Field Unit. Auyuittuq National Park of Canada: Management Plan / Parks Canada. Issued also in French under title: Parc national du Canada Auyuittuq, plan directeur. Issued also in Inuktitut under title: ᐊᐅᔪᐃᑦᑐᖅ ᒥᕐᖑᐃᓯᕐᕕᓕᕆᔨᒃᑯᑦ ᑲᓇᑕᒥ ᐊᐅᓚᓯᓂᕐᒧᑦ ᐊᑐᖅᑕᐅᔪᒃᓴᖅ 1. Auyuittuq National Park (Nunavut)‐‐Management. 2. National parks and reserves‐‐Canada‐‐Management. 3. National parks and reserves‐‐Nunavut‐‐ Management. I. Parks Canada. Western and Northern Service Centre II. Title. FC XXXXXX 200X XXX.XXXXXXXXX C200X‐XXXXXX‐X © Her Majesty the Queen in the Right of Canada, represented by the Chief Executive Officer of Parks Canada, 200X. Paper: ISBN: XXXXXXXX Catalogue No.: XXXXXXXXX PDF: ISBN XXXXXXXXXXX Catalogue No.: XXXXXXXXXXXX Cette publication est aussi disponible en français. wktg5 wcomZoxaymuJ6 wktgotbsix3g6. i Minister’s Foreword (to be included when the Management Plan has been approved) QIA President’s Foreword (to be included when the Management Plan has been approved) NWMB Letter (to be included when the Management Plan has been approved) Recommendation Statement (to be included when the Management Plan has been approved) i Acknowledgements The preparation of this plan involved many people. The input of this diverse group of individuals has resulted in a plan that will guide the management of the park for many years. -
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: -
National Park System: a Screening Level Assessment
Environment Canada Parks Canada Environnement Canada Parcs Canada Edited by: Daniel Scott Adaptation & Impacts Research Group, Environment Canada and Roger Suffling School of Planning, University of Waterloo May 2000 Climate change and Canada’s national park system: A screening level assessment Le Changement climatique et le réseau des parcs nationaux du Canada : une évaluation préliminaire This report was prepared for Parks Canada, Department of Canadian Heritage by the Adaptation & Impacts Research Group, Environment Canada and the Faculty of Environmental Studies, University of Waterloo. The views expressed in the report are those of the study team and do not necessarily represent the opinions of Parks Canada or Environment Canada. Catalogue No.: En56-155/2000E ISBN: 0-662-28976-5 This publication is available in PDF format through the Adaptation and Impacts Research Group, Environment Canada web site < www1.tor.ec.gc.ca/airg > and available in Canada from the following Environment Canada office: Inquiry Centre 351 St. Joseph Boulevard Hull, Quebec K1A 0H3 Telephone: (819) 997-2800 or 1-800-668-6767 Fax: (819) 953-2225 Email: [email protected] i Climate change and Canada’s national park system: A screening level assessment Le Changement climatique et le réseau des parcs nationaux du Canada : une évaluation préliminaire Project Leads and Editors: Dr. Daniel Scott1 and Dr. Roger Suffling2 1 Adaptation and Impacts Research Group, Environment Canada c/o the Faculty of Environmental Studies, University of Waterloo Waterloo, Ontario N2L 3G1 519-888-4567 ext. 5497 [email protected] 2 School of Planning Faculty of Environmental Studies, University of Waterloo Waterloo, Ontario N2L 3G1 Research Team: Derek Armitage - Ph.D. -
Cultural Heritage Resources Report
NTI 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 -
Glacier Monitoring and Assessment, Penny Ice Cap, Nunavut (Auyuittuq National Park)
Project title: Glacier monitoring and assessment, Penny Ice Cap, Nunavut (Auyuittuq National Park) Summary: Higher than normal summer temperatures over the past few decades have resulted in increased melt of glaciers and ice caps in the Canadian Arctic, particularly since 2005. In order to better understand past and future changes of glaciers in the southern Canadian Arctic, the Geological Survey of Canada, Parks Canada and University of Ottawa have been studying Penny Ice Cap on southern Baffin Island since 2007. It is the largest ice mass in the southern Canadian Arctic, covering ~6400 km2. Every year a research team flies to the ice cap from Pangnirtung to take measurements of how much ice is melting versus how much snow is accumulating. The Higher thanteam also measures changes in ice volume, how fast the ice moves, what the ice cap looks like many meters below the surface and the temperature. Ice cores from Penny Ice Cap show that the rate of melt we see today has not been observed for over 3,000 years. Meltwater from the ice cap along with increased rain has contributed to severe flooding events in Akshayuk Pass, a hiking and travel route adjacent to the ice cap and close to Pangnirtung. Understanding how the ice cap will respond to changes in climate in the future will help provide more realistic prediction of future flooding events in the area. Studying Penny Ice Cap also helps answer a question many scientists around the globe are asking. How much will glaciers melt over the next century and how will this contribute to global sea level rise? We know that glaciers in the Canadian Arctic are now the largest contributor of water to global sea level rise outside of Greenland and Antarctica and that these glaciers will continue to lose ice over the next century from models, but much more work is required to improve estimates of ice loss, and therefore sea level rise, over the next century.