Canadian Arctic Cabled Ocean Observatory Study
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North America Other Continents
Arctic Ocean Europe North Asia America Atlantic Ocean Pacific Ocean Africa Pacific Ocean South Indian America Ocean Oceania Southern Ocean Antarctica LAND & WATER • The surface of the Earth is covered by approximately 71% water and 29% land. • It contains 7 continents and 5 oceans. Land Water EARTH’S HEMISPHERES • The planet Earth can be divided into four different sections or hemispheres. The Equator is an imaginary horizontal line (latitude) that divides the earth into the Northern and Southern hemispheres, while the Prime Meridian is the imaginary vertical line (longitude) that divides the earth into the Eastern and Western hemispheres. • North America, Earth’s 3rd largest continent, includes 23 countries. It contains Bermuda, Canada, Mexico, the United States of America, all Caribbean and Central America countries, as well as Greenland, which is the world’s largest island. North West East LOCATION South • The continent of North America is located in both the Northern and Western hemispheres. It is surrounded by the Arctic Ocean in the north, by the Atlantic Ocean in the east, and by the Pacific Ocean in the west. • It measures 24,256,000 sq. km and takes up a little more than 16% of the land on Earth. North America 16% Other Continents 84% • North America has an approximate population of almost 529 million people, which is about 8% of the World’s total population. 92% 8% North America Other Continents • The Atlantic Ocean is the second largest of Earth’s Oceans. It covers about 15% of the Earth’s total surface area and approximately 21% of its water surface area. -
Geography Notes.Pdf
THE GLOBE What is a globe? a small model of the Earth Parts of a globe: equator - the line on the globe halfway between the North Pole and the South Pole poles - the northern-most and southern-most points on the Earth 1. North Pole 2. South Pole hemispheres - half of the earth, divided by the equator (North & South) and the prime meridian (East and West) 1. Northern Hemisphere 2. Southern Hemisphere 3. Eastern Hemisphere 4. Western Hemisphere continents - the largest land areas on Earth 1. North America 2. South America 3. Europe 4. Asia 5. Africa 6. Australia 7. Antarctica oceans - the largest water areas on Earth 1. Atlantic Ocean 2. Pacific Ocean 3. Indian Ocean 4. Arctic Ocean 5. Antarctic Ocean WORLD MAP ** NOTE: Our textbooks call the “Southern Ocean” the “Antarctic Ocean” ** North America The three major countries of North America are: 1. Canada 2. United States 3. Mexico Where Do We Live? We live in the Western & Northern Hemispheres. We live on the continent of North America. The other 2 large countries on this continent are Canada and Mexico. The name of our country is the United States. There are 50 states in it, but when it first became a country, there were only 13 states. The name of our state is New York. Its capital city is Albany. GEOGRAPHY STUDY GUIDE You will need to know: VOCABULARY: equator globe hemisphere continent ocean compass WORLD MAP - be able to label 7 continents and 5 oceans 3 Large Countries of North America 1. United States 2. Canada 3. -
Statutory Report on Wildlife to the Nunavut Legislative Assembly Section 176 of the Wildlife Act
Statutory Report on Wildlife to the Nunavut Legislative Assembly Section 176 of the Wildlife Act 1.0 Review of Wildlife and Habitat Management Programs for Terrestrial Species in Nunavut…………………………………………………………….1 1.1 Wildlife Act and Wildlife Regulations………………………………………………..2 1.2 Qikiqtaaluk Region……………………………………………………………………2 1.2.1 Qikiqtaaluk Research Initiatives…………………………………………………….2 a. Peary caribou………………………………………………………………………….2 b. High Arctic muskox…………………………………………………………………...3 c. North Baffin caribou…………………………………………………………………..4 1.2.2 Qikiqtaaluk Management Initiatives………………………………………………...5 a. Peary Caribou Management Plan……………………………………………………...5 b. High Arctic Muskox…………………………………………………………………..5 c. South Baffin Management Plan……………………………………………………….6 1.3 Kitikmeot Region……………………………………………………………………...8 1.3.1 Kitikmeot Research Initiatives………………………………………………………9 a. Wolverine and Grizzly bear Hair Snagging………………………………………….. 9 b. Mainland Caribou Projects……………………………………………………………9 c. Boothia Caribou Project……………………………………………………………...10 d. Dolphin and Union Caribou Project……………………............................................10 e. Mainland and Boothia Peninsula Muskoxen………………………………………...11 f. Harvest and Ecological Research Operational System (HEROS)…………………...12 g. Vegetation Mapping……………………………………………………………….....12 1.3.2 Kitikmeot Management Initiatives…………………………………………………12 a. Grizzly Bear Management…………………………………………………………...12 b. Bluenose East Management Plan…………………………………………………….12 c. DU Caribou Management Plan………………………………………………………13 d. Muskox Status -
(Late Tertiary) As Seen from Prince Patrick Island, Arctic Canada’ JOHN G
ARCTIC WL. 43, NO. 4 (DECEMBER 1990) P. 393-403 Beaufort Formation (Late Tertiary) as Seen from Prince Patrick Island, Arctic Canada’ JOHN G. FYLES’ (Received 20 March 1990; accepted in revked form 14 June 1990) ABSTRACT. The Beaufort Formation, in its typearea on Prince Patrick Island, is a single lithostratigraphicunit, a few tens of metres thick, consisting of unlithified sandy deposits of braided rivers. Organicbeds in the sand have yielded more than 200 species of plants and insects and probably originated during the Pliocene, when the area supported coniferous forest. ThisBeaufort unit forms the thin eastern edge of a northwest-thickeningwedge of sand and gravel beneath the western part of the island. These largely unexposed beds,up to several hundred metres thick, include the Beaufort unit and perhaps other older or younger deposits.On the islands northeast and southwest of PrincePatrick Island (MeighenIsland to Banks Island),the name BeaufortFormation has been appliedto similar deposits of late Rrtiary age. Most recorded Beaufort beds on these islands are stratigraphically and paleontologically equivalentto the “type” Beaufort, but a few sites that have been called Beaufort (suchas Duck Hawk Bluffsand the lower unit at Ballast Brook,on Banks Island) differ stratigraphicallyand paleontologically from the “type” Beaufort. This paper recommends that these deposits (probably middle Miocene) and others like them be assigned new stratigraphic names and not be included in the Beaufort Formation as now defined. Informal names Mary Sachs gravel (Duck HawkBluffs) and Ballast Brookbeds are proposed as an initial step. Formal use of the name Beaufort Formation shouldrestricted be to the western Arctic Islands. -
A Historical and Legal Study of Sovereignty in the Canadian North : Terrestrial Sovereignty, 1870–1939
University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2014 A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939 Smith, Gordon W. University of Calgary Press "A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939", Gordon W. Smith; edited by P. Whitney Lackenbauer. University of Calgary Press, Calgary, Alberta, 2014 http://hdl.handle.net/1880/50251 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 A HISTORICAL AND LEGAL STUDY OF SOVEREIGNTY IN THE CANADIAN NORTH: TERRESTRIAL SOVEREIGNTY, 1870–1939 By Gordon W. Smith, Edited by P. Whitney Lackenbauer ISBN 978-1-55238-774-0 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 ucpress@ ucalgary.ca 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 specificwork without breaching the artist’s copyright. -
PALEOLIMNOLOGICAL SURVEY of COMBUSTION PARTICLES from LAKES and PONDS in the EASTERN ARCTIC, NUNAVUT, CANADA an Exploratory Clas
A PALEOLIMNOLOGICAL SURVEY OF COMBUSTION PARTICLES FROM LAKES AND PONDS IN THE EASTERN ARCTIC, NUNAVUT, CANADA An Exploratory Classification, Inventory and Interpretation at Selected Sites NANCY COLLEEN DOUBLEDAY A thesis submitted to the Department of Biology in conformity with the requirements for the degree of Doctor of Philosophy Queen's University Kingston, Ontario, Canada December 1999 Copyright@ Nancy C. Doubleday, 1999 National Library Bibliothèque nationale 1*1 of Canada du Canada Acquisitions and Acquisitions et Bibf iographic Services services bibliographiques 395 Wellington Street 395. rue Wellington Ottawa ON KIA ON4 Ottawa ON K1A ON4 Canada Canada Your lYe Vorre réfhœ Our file Notre refdretua The author has granted a non- L'auteur a accordé une licence non exclusive licence allowing the exclusive pemettant à la National Library of Canada to Bibliothèque nationale du Canada de reproduce, Ioan, distribute or sell reproduire, prêter, distribuer ou copies of this thesis in microform, vendre des copies de cette thèse sous paper or electronic formats. la forme de microfiche/nlm, de reproduction sur papier ou sur format électronique. The author retains ownership of the L'auteur conserve la propriété du copyright in this thesis. Neither the droit d'auteur qui protège cette thèse. thesis nor substantial extracts fiom it Ni la thèse ni des extraits substantiels may be printed or othemise de celle-ci ne doivent être imprimés reproduced without the author's ou autrement reproduits sans son pemission. autorisation. ABSTRACT Recently international attention has been directed to investigation of anthropogenic contaminants in various biotic and abiotic components of arctic ecosystems. Combustion of coai, biomass (charcoal), petroleum and waste play an important role in industrial emissions, and are associated with most hurnan activities. -
Annual Report: October 1, 2014 Assessing the Impact of Small, Canadian Arctic River Flows to the Freshwater Budget of the Canadian Archipelago Matthew B
Annual Report: October 1, 2014 Assessing the impact of small, Canadian Arctic River flows to the freshwater budget of the Canadian Archipelago Matthew B. Alkire, University of Washington Assessing the impact of small, Canadian Arctic river flows to the freshwater budget of the Canadian Archipelago (or SCARFs) is a scientific research project funded by the National Science Foundation (USA). The purpose of this project is to collect water samples from seven different rivers and their adjoining estuaries throughout the Canadian Arctic Archipelago (see Fig. 1) in order to determine whether or not their chemical signatures differ from larger North American rivers such as the Mackenzie and Yukon Rivers. Five of the rivers are located within Nunavut, Canada: the Coppermine River (near Kugluktuk), Ellice River (~140 km southeast of Cambridge Bay), Back River (~180 km southeast of Gjoa Haven), Cunningham River (~77 km southeast of Resolute Bay on Somerset Island), and Kangiqtugaapik River (near Clyde River, Baffin Island). Two of the rivers are located within the Northwest Territories, Canada: the Kujjuua River (located approximately 67 km northeast of Ulukhaktok on Victoria Island) and Thomsen River (specifically near the mouth of the river where it empties into Castel Bay, on Banks Island). Figure 1. Map of the Canadian Arctic Archipelago. The red stars indicate the mouths of the rivers sampled during this study: (1) Coppermine R., (2) Ellice R., (3) Back R., (4) Kuujuua R. (Victoria Island), (5) Thomsen R. (Banks Island), (6) Cunningham R. (Somerset Island), and (7) Clyde R. (Baffin Island). The Coppermine, Ellice, and Back Rivers are located on the mainland of Nunavut. -
Taima'na Uqamaqattangitlutit, the Polar Bears Can Hear
Taima’na Uqamaqattangitlutit, The Polar Bears Can Hear Consequences of words and actions in the Central Arctic • JERRY: [First in Inuktitut] My name is Jerry Arqviq and I am from Gjoa Haven, Nunavut. My father was a polar bear hunter. I am a polar bear hunter, and I now I am teaching my son. I started hunting when I was 6 years old and I caught my first polar bear when I was 14 years old. • DARREN: My name is Darren Keith and I am the Senior Researcher for the Kitikmeot Heritage Society which is based in Cambridge Bay. Jerry and I would like to thank some people who made it possible for us to be here in Paris: Canadian North Airlines who sponsored a portion of Jerry’s travel, World Wildlife Fund Canada, the organizing committee of the 15th Inuit Studies Conference, and a special thanks to Professor Beatrice Collignon. DARREN: The area we will be discussing is the Nattilik area of the Kitikmeot Region of Nunavut. For the Inuit of the central Arctic, who live in the communities of Gjoa Haven, Taloyoak and Kugaaruk, Nunavut polar bears have always been an essential part of an Inuit or Inuktitut way of life based on hunting animals. Our paper will discuss some aspects of the relationship between Inuit and polar bears, and the sensitivity of polar bears to the statements and actions of human beings. JERRY: [talks about his community and the continued importance of country food to the people including polar bears – explains picture of young people fishing at the weir at Iqalungmiut last year, as they do every year.] • DARREN: This paper draws mainly on interviews with Elders conducted during a project for the Gjoa Haven Hunters and Trappers Organization of Gjoa Haven Nunavut. -
Mycology in the Canadian Arctic
MYCOLOGY INTHE CANADIAN ARCTIC* D. B. 0. Savile Introduction and history TUDENTS of arctic fungi have traditionally relied largely on the practice S of gleaning inconspicuous saprophytes from the old stems and leaves of vascular plant specimens brought back by botanists or others. Except for a few conspicuous fleshy fungi, which were often unidentifiable because of inappropriate handling, most of these specimens have been collected unin- tentionally. This was the way in which Canadian arctic mycology started. First Rostrup (1906) scrutinized Simmons’s collections from Ellesmere Island made during the second voyage of the Fram. Later Lind (1910) published an account of fungi gleaned from the plantsof the GjZa expedition, collected at King Point on the Yukon coast and King William Island; and Dearness (1923) similarly treated the fungi taken on the Canadian Arctic Expedition at various points along the arctic coast. Lind (1934) added a numberof further Canadian records, arctic and sub- arctic, in his discussion of circumpolar microfungi. Linder (1947) made the next substantial contribution to our knowledgeof Canadian arctic fungi, but his treatment, although part of Polunin’s “Flora of the Canadian Eastern Arctic’’ was actually limited to those fungi collected by Polunin and did not bring together the available records. A conspicuous feature of almost all the early records from the Canadian Arctic is the extreme paucityof parasitic fungi. Dearness was impressed by the lack of such fungi and wrote “the smuts, like the rusts, seem to be rare in the Canadian arctic regions”. He recorded only one smut and three rusts from the collectioqsof the Canadian Arctic Expedition. -
Seventh Grade Social Studies, Eastern Hemisphere Course Essential Questions (From Phase I Report)
Davison Community Schools ADVISORY CURRICULUM COUNCIL Phase II, April 2012 Seventh Grade Social Studies, Eastern Hemisphere Course Essential Questions (from Phase I report): 1. How does the past link to the present and determine the future? 2. How does the United States fit into the global world and how is the United States impacted by other nations? 3. What is the relationship between people and the Earth? 4. How can information be used to make informed decisions about understanding the world around us? Phase II Curriculum Unit: Geography Essential Questions: Essential Understanding: How do we use maps and other geographic tools Physical features impact where and how people to acquire information about the world? live What methods of inquiry and analysis do we use Geography impacts population patterns to answer geographic questions? Latitude and elevations impact climate zones How do we use themes, connections and spatial Geographers use 5 themes of geography to patterns to describe and study the Earth? describe regions or places on earth How do we compare and describe natural regions? Human and physical characteristics are used to How do we use human characteristics to study study the earth places on the Earth? Map skills are necessary for understanding information for a variety of maps Recognize distortion in a variety of map scale/projections Economic indicators (GDP, Literacy rate …..) are used to evaluate a country Globalization has created a global interdependence among people There are different purposes of world organizations Curriculum Standards G1.1.1 Explain and use a variety of maps, globes, and web based geography technology to study the world, including global, interregional, regional, and local scales. -
Who Discovered the Northwest Passage? Janice Cavell1
ARCTIC VOL. 71, NO.3 (SEPTEMBER 2018) P.292 – 308 https://doi.org/10.14430/arctic4733 Who Discovered the Northwest Passage? Janice Cavell1 (Received 31 January 2018; accepted in revised form 1 May 2018) ABSTRACT. In 1855 a parliamentary committee concluded that Robert McClure deserved to be rewarded as the discoverer of a Northwest Passage. Since then, various writers have put forward rival claims on behalf of Sir John Franklin, John Rae, and Roald Amundsen. This article examines the process of 19th-century European exploration in the Arctic Archipelago, the definition of discovering a passage that prevailed at the time, and the arguments for and against the various contenders. It concludes that while no one explorer was “the” discoverer, McClure’s achievement deserves reconsideration. Key words: Northwest Passage; John Franklin; Robert McClure; John Rae; Roald Amundsen RÉSUMÉ. En 1855, un comité parlementaire a conclu que Robert McClure méritait de recevoir le titre de découvreur d’un passage du Nord-Ouest. Depuis lors, diverses personnes ont avancé des prétentions rivales à l’endroit de Sir John Franklin, de John Rae et de Roald Amundsen. Cet article se penche sur l’exploration européenne de l’archipel Arctique au XIXe siècle, sur la définition de la découverte d’un passage en vigueur à l’époque, de même que sur les arguments pour et contre les divers prétendants au titre. Nous concluons en affirmant que même si aucun des explorateurs n’a été « le » découvreur, les réalisations de Robert McClure méritent d’être considérées de nouveau. Mots clés : passage du Nord-Ouest; John Franklin; Robert McClure; John Rae; Roald Amundsen Traduit pour la revue Arctic par Nicole Giguère. -
Historical Developments in Utkuhiksalik Phonology; 5/16/04 Page 1 of 36
Carrie J. Dyck Department of Linguistics Memorial University of Newfoundland St. John’s NL A1B 3X9 Jean L. Briggs Department of Anthropology Memorial University of Newfoundland St. John’s NL A1B 3X9 Historical developments in Utkuhiksalik phonology; 5/16/04 page 1 of 36 1 Introduction* Utkuhiksalik has been analysed as a subdialect of Natsilik within the Western Canadian Inuktun (WCI) dialect continuum (Dorais, 1990:17; 41). 1 While Utkuhiksalik has much in com- mon with the other Natsilik subdialects, the Utkuhiksalingmiut and the Natsilingmiut were his- torically distinct groups (see §1.1). Today there are still lexical (see §1.2) and phonological dif- ferences between Utkuhiksalik and Natsilik. The goal of this paper is to highlight the main phonological differences by describing the Utkuhiksalik reflexes of Proto-Eskimoan (PE) *c, *y, and *D. 1.1 Overview of dialect relations2 The traditional territory of the Utkuhiksalingmiut (the people of the place where there is soapstone) lay between Chantrey Inlet and Franklin Lake. Utkuhiksalik speakers also lived in the * Research for this paper was supported by SSHRC grant #410-2000-0415, awarded to Jean Briggs. The authors would also like to acknowledge the invaluable assistance of the Utkuhiksalingmiut who presently live in Gjoa Haven, especially Briggs’s adoptive mother and aunts. Tape recordings of these consultants, collected by Briggs from the 1960’s to the present, constitute the data for this paper. Briggs is currently compiling a dictionary of Utkuhiksalik. 1 We use the term Natsilik, rather than Netsilik, to denote a dialect cluster that includes Natsilik, Utkuhik- salik, and Arviligjuaq.