Canada and the American Curriculum
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The Thermal State of Permafrost in Canada – Results from the International Polar Year
The Thermal State of Permafrost in Canada – Results from the International Polar Year Sharon L. Smith 1, Antoni G. Lewkowicz 2, Christopher R. Burn 3, Michel Allard 4 & Jennifer Throop 2 1Geological Survey of Canada, Natural Resources Canada, Ottawa, Ontario, Canada 2Department of Geography, University of Ottawa, Ottawa, Ontario, Canada 3Department of Geography and Environmental Studies, Carleton University, Ottawa, Ontario, Canada 4Centre d’études nordiques, Université Laval, Ste-Foy, Québec, Canada ABSTRACT A snapshot of permafrost thermal state in northern Canada during the International Polar Year was developed with ground temperature measurements from about 170 boreholes. The measurements span a wide range of ecoclimate and geological conditions and are at various elevations. Ground temperatures within the discontinuous permafrost zone are generally above -2°C and range to as low as -15°C in the continuous zone. Permafrost temperatures have generally increased across northern Canada for the past several decades, with greater warming rates occurring north of tree line. Consequently the spatial diversity of permafrost thermal conditions is decreasing over time. RÉSUMÉ Un instantané de l’état thermique du pergélisol dans le nord du Canada au cours de l’Année polaire internationale a été élaboré en utilisant les mesures des températures au sol obtenues d’environ 170 puits. Les mesures couvraient une vaste gamme de conditions écoclimatiques et géologiques et diverses élévations. Les températures au sol au sein de la zone discontinue de pergélisol étaient généralement supérieures à -2°C et descendaient jusqu’à -15°C dans la zone continue. Les températures du pergélisol ont généralement augmenté dans tout le nord du Canada au cours des dernières décennies, les taux de réchauffement les plus marqués étant survenus au nord de la ligne des arbres. -
I. 1. the Influence of Permafrost on Northern Development
I. 1. THE INFLUENCE OF PERMAFROST ON NORTHERN DEVELOPMENT INTRODUCTION The expansion of settlement from man's early home in the fertile, friendly and protected river valleys of the Middle East has been marked by conquest of one natural obstacle after another. Broad seas, hot, dry deserts, mountain ranges and dense forests each in their turn arrested his progress until new techniques were devised and perfected, and became common knowledge. His invasion of the tropical rainforests was delayed by diseases, and his ventures into the far north - what Stefansson has termed "The .Northward Course of Empire" (1) - were handicapped by severe cold and snow, and by the heavy ice which impeded and damaged his ships. In his long and frequently frustrated efforts to make a home in even the remotest parts of the earth, man has encountered, and eventually learned to deal with, an enormous variety of natural hazards. Perennially frozen ground in the polar regions is one of his most recent natural obstacles. It has become of major importance only in the past few decades, although its existence has long been known. Alexander Mackenzie mentioned it and Jules Verne wrote a novel (2) based in part on it, while the quick-frozen mammoths of Siberia have been a cause of wonder for generations. How was it that such a widespread phenomenon, covering about one-half of Canada and almost as great a proportion of the Soviet Union, should nevertheless have attracted so little attention that until a few years ago it even lacked a commonly accepted English name and is only now being honoured in Canada by a national symposium ? The world population map demonstrates that man has as yet barely reached in any numbers the southern limit of that one-fifth of the land surface underlain by permafrost. -
1 of 10 Course Syllabus Geography of Canada
Course Syllabus Geography of Canada - GEOG 2570 A01 Department of Environment and Geography Clayton H. Riddell Faculty of Environment, Earth, and Resources Instructor: Dr. Janna Wilson 216 Sinnott Building 204.480.1817 [email protected] (preferred means of contact) Office Hours: Monday: 1:00-2:30 PM Or by appointment; Wednesday: 1:00 – 2:00 PM please email Subject to change Lecture Room: 201 St. John’s College Lecture Slot: M/W/F: 10:30 - 11:20 AM Course Dates: Sept. 8 – Dec. 9, 2016 Final Exam Period: December 12-22, 2016 Final Voluntary Nov. 18, 2016 (50% of the course grade will be available by this date) Withdrawal Date: For more information: http://umanitoba.ca/student/records/leave_return/695.html Required Course Materials Bone, R.M. (2014). The Regional Geography of Canada (6th ed.). Oxford University Press. ISBN: 978-0-19-900242-9 Cost: $109.95 Student study guide on the textbook website: http://www.oupcanada.com/higher_education/companion/geography/9780199002429/stude nt_resources.html Note: If you are using a different textbook than the 6th edition of Bone, the assigned readings may not correspond. The instructor offers no guarentee that the content in other textbooks/or editions will be the same as the 6th edition of Bone. Consequently, you may or may not be able to answer “textbook” exam questions. You may use any book you want, but it is at your own risk. GEOG 2570 J. Wilson/F2016 1 of 10 Course Description: (Formerly 053.257) A regional study of Canada in which the major regions of Canada are studied with respect to geographical patterns of their physical environment, settlement, culture, economic activity, and land use. -
The Territorial North
The Territorial 11 North Learning Objectives To describe the physical and historical geography of the Territorial North as a basis for understanding the region’s social and econom- ic position in Canada To describe the dual character of the Territorial North (in terms of resource frontier and homeland) To describe the Territorial North’s position as a resource frontier in the core/periphery model To outline the key role Canada’s north plays in geopolitics by discussing Arctic sovereignty To outline the key role played by megaprojects in the region’s development Chapter Overview The Territorial North is Canada’s largest region and the only one to be categorized as a resource frontier in the core/periphery model. Key themes of this chapter include: 1. Remoteness of the Territorial North. 2. Resources within the Territorial North. 3. Recognition of this region as a homeland for Indigenous peoples The Territorial North within Canada and the World The Territorial North comprises 39 per cent of Canada’s area, 0.3 per cent of its GDP, and 0.3 per cent of its population. As a result of its geographic remoteness and dependence on resources, mega- projects in this region have significant implications not only for economic development but also for social conditions and the environment. Physical Geography of the Territorial North The Territorial North extends across four physiographic regions and two climate zones. Bone points out that the physical geography of the Territorial North is influenced more by its cold environment than by physical topography (p. 367). It is largely because of the cold environment that northern ecosystems are frequently described as “fragile” or “delicate,” and require prolonged periods of time to recover from human activity. -
Human Geography of Canada: Developing a Vast Wilderness
Chapter 7 Guided Notes _________________________________________________________________________________________ NAME Human Geography of Canada: Developing a Vast Wilderness Three major groups in Canada—the native peoples, the French, and the English—have melded into a diverse and economically strong nation. Section 1: History and Government of Canada French and British settlement greatly influenced Canada’s political development. Canada’s size and climate affected economic growth and population distribution. The First Settlers and Colonial Rivalry Early Peoples After Ice Age, migrants cross Arctic land bridge from Asia o ancestors of Arctic Inuit (Eskimos); North American Indians to south Vikings found Vinland (Newfoundland) about A.D. 1000; later abandon Colonization by France and Britain French explorers claim much of Canada in 1500–1600s as “New France”; British settlers colonize the Atlantic Coast Steps Toward Unity Establishing the Dominion of Canada In 1791 Britain creates two political units called provinces o Upper Canada (later, Ontario): English-speaking, Protestant; Lower Canada (Quebec): French-speaking, Roman Catholic Rupert’s Land a northern area owned by fur-trading company Immigrants arrive, cities develop: Quebec City, Montreal, Toronto o railways, canals are built as explorers seek better fur-trading areas Continental Expansion and Development From the Atlantic to the Pacific In 1885 a transcontinental railroad goes from Montreal to Vancouver o European immigrants arrive and Yukon gold brings fortune hunters; -
The Rise and Decline of Hybrid (Metis) Societies on the Frontier of Western Canada and Southern Africa
THE RISE AND DECLINE OF HYBRID (METIS) SOCIETIES ON THE FRONTIER OF WESTERN CANADA AND SOUTHERN AFRICA ALVIN KIENETZ, P.O. Box 402, The Pas, Manitoba, Canada, R9A 1K5. ABSTRACT/RESUME A comparison of the development of the Metis in Canada and similar peoples in Southern Africa reveals some remarkable similarities between the two groups. The existence of these parallels suggests that a more extensive comparative study of peoples of mixed race throughout the world would be of value. Une comparaison de l'évolution des Métis au Canada et de celle de certains peuples similaires dans le Sud africain révèle des ressemblances frappantes entre les deux groupes. Ce parallèle suggère qu'une étude comparative plus complete des peuples de race mixte dans le monde entier présenterait une valeur incontestable. THE CANADIANJOURNAL OF NATIVE STUDIES Ill, 1(1983): 3.21 4 ALVIN KIENETZ The comparative study of the "frontier" as a historical-geographical phe- nomenon appears to have, or have had, two main traditions: the first of these, the purpose of which is ultimately practical (i.e. applied geography) is found in the largely pre-World I pioneer settlement studies of Bowman and others (1937). The other tradition involves attempts to apply the "frontier thesis" of Frederick Jackson Turner to other historical settlement frontiers(c.f.Wyman and Kroeber, 1957). What both of these traditions have in common is that they focus almost entirely on the advancing, colonizing culture; the retreating, native groups that are being colonized, or - better - colonialized, 1 are hardly even mentioned. 2 Only relatively recently have scholars begun to give due recognition to the roles and contributions of native or aboriginal societies on the frontier. -
An Introduction to Inuit and Chukchi Experiences in the Bering Strait, Beaufort Sea, and Baffin Bay
water Article Crossroads of Continents and Modern Boundaries: An Introduction to Inuit and Chukchi Experiences in the Bering Strait, Beaufort Sea, and Baffin Bay Henry P. Huntington 1,* , Richard Binder Sr. 2, Robert Comeau 3, Lene Kielsen Holm 4, Vera Metcalf 5, Toku Oshima 6, Carla SimsKayotuk 7 and Eduard Zdor 8 1 Ocean Conservancy, Eagle River, AK 99577, USA 2 Inuvik, NT X0E 0T0, Canada; [email protected] 3 Iqaluit, NU X0A 0H0, Canada; [email protected] 4 Greenland Institute of Natural Resources, Nuuk 3900, Greenland; [email protected] 5 Eskimo Walrus Commission, Nome, AK 99762, USA; [email protected] 6 Qaanaaq 3971, Greenland; [email protected] 7 North Slope Borough Department of Wildlife Management, Kaktovik, AK 99747, USA; [email protected] 8 Department of Anthropology, University of Alaska Fairbanks, Fairbanks, AK 99775, USA; [email protected] * Correspondence: [email protected] Received: 21 May 2020; Accepted: 20 June 2020; Published: 24 June 2020 Abstract: The homeland of Inuit extends from Asia and the Bering Sea to Greenland and the Atlantic Ocean. Inuit and their Chukchi neighbors have always been highly mobile, but the imposition of three international borders in the region constrained travel, trade, hunting, and resource stewardship among neighboring groups. Colonization, assimilation, and enforcement of national laws further separated those even from the same family. In recent decades, Inuit and Chukchi have re-established many ties across those boundaries, making it easier to travel and trade with one another and to create new institutions of environmental management. To introduce Indigenous perspectives into the discussion of transboundary maritime water connections in the Arctic, this paper presents personal descriptions of what those connections mean to people who live and work along and across each of the national frontiers within the region: Russia–U.S., U.S.–Canada, and Canada–Greenland. -
Canada: Physical Background
Canada: Physical Background Why look at Canada’s Physical Geography? • It helps shape the human geography of Canada – And its regions Reading • Take a look at any traditional textbook in the geography of Canada – There is usually a chapter on physical geography – Chapter 2 from Bob Bone’s book is copied and on reserve in GRC S403 Ross Canada • Is built on continental crust • Therefore contains very ancient rocks • Has a long and very complex geological history • Is most geologically active around its edges • We live here in one of its quieter middle bits – Life in the slow lane Geologic Provinces • Shield (continental crust) • Sedimentary platforms • Fold mountain belts • Arctic coastal plain Geologic Time Scale Period Millions of Regions formed Years Ago Quaternary 2-0 Great Lakes Cenozoic 100-0 Cordillera, Inuitian Mesozoic 250-100 Interior plains Paleozoic 600-250 Appalachian uplands, Arctic lands Precambrian 3500-600 Shield Canadian Shield • Ancient (3500 million years +) • Crystalline base of continent • Formed at great depth & pressure – faulted, folded, flowed – metamorphic rocks: gneiss – from 5+ phases of mountain building • Poor agricultural soils Shield Rocks • Formed in an era of rather small continents – 1/10th the size of present-day continents or less • North American shield: – Formed out of 7 ‘provinces’ – Each with separate belts/terranes Shield Rocks • The zones of mountain building (orogens) were smaller too • Plate tectonics operated – But in many ways differently than today Nain Province Ungava, Quebec Churchill province -
Changes in Snow, Ice and Permafrost Across Canada
CHAPTER 5 Changes in Snow, Ice, and Permafrost Across Canada CANADA’S CHANGING CLIMATE REPORT CANADA’S CHANGING CLIMATE REPORT 195 Authors Chris Derksen, Environment and Climate Change Canada David Burgess, Natural Resources Canada Claude Duguay, University of Waterloo Stephen Howell, Environment and Climate Change Canada Lawrence Mudryk, Environment and Climate Change Canada Sharon Smith, Natural Resources Canada Chad Thackeray, University of California at Los Angeles Megan Kirchmeier-Young, Environment and Climate Change Canada Acknowledgements Recommended citation: Derksen, C., Burgess, D., Duguay, C., Howell, S., Mudryk, L., Smith, S., Thackeray, C. and Kirchmeier-Young, M. (2019): Changes in snow, ice, and permafrost across Canada; Chapter 5 in Can- ada’s Changing Climate Report, (ed.) E. Bush and D.S. Lemmen; Govern- ment of Canada, Ottawa, Ontario, p.194–260. CANADA’S CHANGING CLIMATE REPORT 196 Chapter Table Of Contents DEFINITIONS CHAPTER KEY MESSAGES (BY SECTION) SUMMARY 5.1: Introduction 5.2: Snow cover 5.2.1: Observed changes in snow cover 5.2.2: Projected changes in snow cover 5.3: Sea ice 5.3.1: Observed changes in sea ice Box 5.1: The influence of human-induced climate change on extreme low Arctic sea ice extent in 2012 5.3.2: Projected changes in sea ice FAQ 5.1: Where will the last sea ice area be in the Arctic? 5.4: Glaciers and ice caps 5.4.1: Observed changes in glaciers and ice caps 5.4.2: Projected changes in glaciers and ice caps 5.5: Lake and river ice 5.5.1: Observed changes in lake and river ice 5.5.2: Projected changes in lake and river ice 5.6: Permafrost 5.6.1: Observed changes in permafrost 5.6.2: Projected changes in permafrost 5.7: Discussion This chapter presents evidence that snow, ice, and permafrost are changing across Canada because of increasing temperatures and changes in precipitation. -
For Budding Fit::Ld
652 Christmas Books Nature Vol. 276 7 December 1978 latest velsion of the world picture book ments, crystals, gemstones, economic Armchair geology that grandma bought us for our eleventh minerals and the building of a mineral birthdays. There is little one can fault collection. This book too is but a variant THE mere statistics of wilderness areas Banyard on, lest it be lack of inspiration; of its numerous predecessors over the are impressive enough. The Earth's but it is at times like this that one comes years; but within its stated limitations surface contains something like 18 x 10'; to appreciate Anthony Smith's sense of it is far more authoritative and better km 2 of desert, about half of which is personal quest and involvement. produced than most. accounted for by Australia and the Involvement of another kind is inherent Aggregates of minerals (tllat is, rocks) Sahara. And to this 12 % of the total in Alan Woolley's JIIustrated Ellcyclo are generally less colourful than some land surface must be added II % under paedia of the Mil/era! Killgdolll, (Hamlyn: of the pure minerals and thus less popular permanent ice cover, 9 % covered with Feltham, UK, £5 .95) for mineralogy as collectors' items. The most colourful mountain, a further 9 ~ ( ; of cold and in its simplest form, the collection of specimens in Rucks (J( the World, (Per waterlogged tundra, and 29 ~/~ of other minerals, is the most popular of geology's gamon : Oxford, £ 15), which is not a wise uncultivable continent comprising branches, at least as far as the amateur book but a neatly-mounted set of 36 of semi-arid regions, bare rock, frost-prone is concerned. -
Maintaining Arctic Cooperation with Russia Planning for Regional Change in the Far North
Maintaining Arctic Cooperation with Russia Planning for Regional Change in the Far North Stephanie Pezard, Abbie Tingstad, Kristin Van Abel, Scott Stephenson C O R P O R A T I O N For more information on this publication, visit www.rand.org/t/RR1731 Library of Congress Cataloging-in-Publication Data is available for this publication. ISBN: 978-0-8330-9745-3 Published by the RAND Corporation, Santa Monica, Calif. © Copyright 2017 RAND Corporation R® is a registered trademark. Cover: NASA/Operation Ice Bridge. Limited Print and Electronic Distribution Rights This document and trademark(s) contained herein are protected by law. This representation of RAND intellectual property is provided for noncommercial use only. Unauthorized posting of this publication online is prohibited. Permission is given to duplicate this document for personal use only, as long as it is unaltered and complete. Permission is required from RAND to reproduce, or reuse in another form, any of its research documents for commercial use. For information on reprint and linking permissions, please visit www.rand.org/pubs/permissions. The RAND Corporation is a research organization that develops solutions to public policy challenges to help make communities throughout the world safer and more secure, healthier and more prosperous. RAND is nonprofit, nonpartisan, and committed to the public interest. RAND’s publications do not necessarily reflect the opinions of its research clients and sponsors. Support RAND Make a tax-deductible charitable contribution at www.rand.org/giving/contribute www.rand.org Preface Despite a period of generally heightened tensions between Russia and the West, cooperation on Arctic affairs—particularly through the Arctic Council—has remained largely intact, with the exception of direct mil- itary-to-military cooperation in the region. -
Northern Connections
NORTHERN CONNECTIONS A Multi-Modal Transportation Blueprint for the North FEBRUARY 2008 Government of Yukon Photos and maps courtesy of: ALCAN RaiLink Inc. Government of British Columbia Government of Northwest Territories Government of Nunavut Government of Yukon Designed and printed in Canada’s North Copyright February 2008 ISBN: 1-55362-342-8 MESSAGE FROM MINISTERS It is our pleasure to present Northern Connections: A Multi-Modal Transportation Blueprint for the North, a pan-territorial perspective on the transportation needs of Northern Canada. This paper discusses a vision for the development of northern transportation infrastructure in the context of a current massive infrastructure decit. Research has proven that modern transportation infrastructure brings immense benets. The northern transportation system of the future must support economic development, connect northern communities to each other and to the south, and provide for enhanced sovereignty and security in Canada’s north. This document complements a comprehensive national transportation strategy – Looking to the Future: A Plan for Investing in Canada’s Transportation System – released under the auspices of the Council of the Federation in December 2005. The three territories support the details contained in Looking to the Future that call for a secure, long-term funding framework for transportation infrastructure that will benet all Canadians. Equally important, northern territories stress that this national strategy – and any subsequent funding mechanisms that follow – must account for unique northern needs and priorities, which would be largely overlooked using nation-wide criteria only. This paper is also consistent with A Northern Vision: A Stronger North and a Better Canada, the May 2007 release of a pan-territorial vision for the north.