Distribution and Abundance P Caribou
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Western Elements in the Early Thule Culture of the Eastern High Arctic PETER SCHLEDERMANN' and KAREN Mccullough'
ARCTIC VOL. 33, NO. 4 (DECEMBER l-), P. 833-841 Western Elements in the Early Thule Culture of the Eastern High Arctic PETER SCHLEDERMANN' and KAREN McCULLOUGH' ABSTRACT. Excavations of Thule culture wintersites in the Bache Peninsula regionon the east coastof Ellesmere Island have yielded a numberof finds which indicate a strong relationship to cultural developments in the Bering Sea region. Specific elements under discussion include dwelling styles, clay pottery, needle cases, a brow band and harpoon heads. Evidence is presented suggesting an initial arrivalof the Thule cultureInuit in the eastern Arctic around 1050 A.D. INTRODUCTION Much has been writtenabout the origins and expansionof the Thule culture into the Canadian Arctic. That this event took place as a result of population move- ment and migration from the west is never seriously contested. However, the timing and causes of this movement are subjects of continuing debate. During the past three summers, excavations have taken placeon several Thule culture winter sites in the Bache Peninsula region onthe east coast of Ellesmere Island (Fig. 1). The winter settlements, containing approximately 150 house ruins distributed over 12 sites, span a 500 to 600 year occupation period which ended about 1700 A.D. The retreat of the Thule culture Inuit fromthis region to the more viable Thuledistrict in northwest Greenland probably marksthe final abandonment of the Canadian High Arctic as a semi-permanent settlement area. Research into the early Thule culture occupation in the study area has been one of several primary objectives, particularly in relation to the temporal and spatial &hities of the NQgdlit and Ruin Island phases initially described by Holtved (1944; 1954). -
New Constraints on the Age, Geochemistry
New constraints on the age, geochemistry, and environmental impact of High Arctic Large Igneous Province magmatism: Tracing the extension of the Alpha Ridge onto Ellesmere Island, Canada T.V. Naber1,2, S.E. Grasby1,2, J.P. Cuthbertson2, N. Rayner3, and C. Tegner4,† 1 Geological Survey of Canada–Calgary, Natural Resources Canada, Calgary, Canada 2 Department of Geoscience, University of Calgary, Calgary, Canada 3 Geological Survey of Canada–Northern, Natural Resources Canada, Ottawa, Canada 4 Centre of Earth System Petrology, Department of Geoscience, Aarhus University, Aarhus, Denmark ABSTRACT Island, Nunavut, Canada. In contrast, a new Province (HALIP), is one of the least studied U-Pb age for an alkaline syenite at Audhild of all LIPs due to its remote geographic lo- The High Arctic Large Igneous Province Bay is significantly younger at 79.5 ± 0.5 Ma, cation, and with many exposures underlying (HALIP) represents extensive Cretaceous and correlative to alkaline basalts and rhyo- perennial arctic sea ice. Nevertheless, HALIP magmatism throughout the circum-Arctic lites from other locations of northern Elles- eruptions have been commonly invoked as a borderlands and within the Arctic Ocean mere Island (Audhild Bay, Philips Inlet, and potential driver of major Cretaceous Ocean (e.g., the Alpha-Mendeleev Ridge). Recent Yelverton Bay West; 83–73 Ma). We propose anoxic events (OAEs). Refining the age, geo- aeromagnetic data shows anomalies that ex- these volcanic occurrences be referred to col- chemistry, and nature of these volcanic rocks tend from the Alpha Ridge onto the northern lectively as the Audhild Bay alkaline suite becomes critical then to elucidate how they coast of Ellesmere Island, Nunavut, Canada. -
Geostrategy and Canadian Defence: from C.P. Stacey to a Twenty-First Century Arctic Threat Assessment
Journal of Military and Strategic VOLUME 20, ISSUE 1 Studies Geostrategy and Canadian Defence: From C.P. Stacey to a Twenty-First Century Arctic Threat Assessment Ryan Dean and P. Whitney Lackenbauer1 “If some countries have too much history, we have too much geography.” -- Prime Minister William Lyon Mackenzie King, 1936 Geostrategy is the study of the importance of geography to strategy and military operations. Strategist Bernard Loo explains that “it is the influence of geography on tactical and operational elements of the strategic calculus that underpins, albeit subliminally, strategic calculations about the feasibility of the use of military force because the geographical conditions will influence policy-makers’ and strategic 1 An early version of some sections of this article appeared as “Geostrategical Approaches,” a research report for Defence Research and Development Canada (DRDC) project on the Assessment of Threats Against Canada submitted in 2015. We are grateful to the coordinators of that project, as well as to reviewers who provided feedback that has strengthened this article. Final research and writing was completed pursuant to a Department of National Defence MINDS Collaborative Network grant supporting the North American and Arctic Defence and Security Network (NAADSN). ©Centre of Military and Strategic Studies, 2019 ISSN : 1488-559X JOURNAL OF MILITARY AND STRATEGIC STUDIES planners’ perceptions of strategic vulnerabilities or opportunities.”2 By extension, the geographical size and location of a country are key determinants -
A Hans Krüger Arctic Expedition Cache on Axel Heiberg Island, Nunavut ROBERT W
ARCTIC VOL. 60, NO. 1 (MARCH 2007) P. 1–6 A Hans Krüger Arctic Expedition Cache on Axel Heiberg Island, Nunavut ROBERT W. PARK1 and DOUGLAS R. STENTON2 (Received 13 June 2006; accepted in revised form 31 July 2006) ABSTRACT. In 1999 a team of geologists discovered an archaeological site near Cape Southwest, Axel Heiberg Island. On the basis of its location and the analysis of two artifacts removed from the site, the discoverers concluded that it was a hastily abandoned campsite created by Hans Krüger’s German Arctic Expedition, which was believed to have disappeared between Meighen and Amund Ringnes islands in 1930. If the attribution to Krüger were correct, the existence of this site would demonstrate that the expedition got farther on its return journey to Bache Peninsula than previously believed. An archaeological investigation of the site by the Government of Nunavut in 2004 confirmed its tentative attribution to the German Arctic Expedition but suggested that it is not a campsite, but the remains of a deliberately and carefully constructed cache. The finds suggest that one of the three members of the expedition may have perished before reaching Axel Heiberg Island, and that the survivors, in order to lighten their sledge, transported valued but heavy items (including Krüger’s geological specimens) to this prominent and well-known location to cache them, intending to return and recover them at some later date. Key words: German Arctic Expedition, Hans Krüger, archaeology, geology, Axel Heiberg Island, Nunavut RÉSUMÉ. En 1999, une équipe de géologues a découvert un lieu d’importance archéologique près du cap Southwest, sur l’île Axel Heiberg. -
Hot Rocks from Cold Places: a Field, Geochemical and Geochronological Study from the High Arctic Large Igneous P Rovince (HALIP) at Axel Heiberg Island, Nunavut
! !"#$%"&'($)*"+$,"-.$/-0&1(2$3$451-.6$71"&81+5&0-$09.$ 71"&8*"9"-":5&0-$;#<.=$)*"+$#81$!5:8$3*&$>0*:1$ ?:91"<($/*"@59&1$A!3>?/B$0#$3C1-$!15D1*:$?(-09.6$ E<90@<#$ $ $ by Cole Girard Kingsbury A thesis submitted to the Faculty of Graduate and Postdoctoral Affairs in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Earth Sciences Ottawa – Carleton Geoscience Centre and Carleton University Ottawa, Ontario © 2016 Cole Girard Kingsbury ! ! !"#$%&'$() ) ) ) ) ) ) ) ) ) ) The geology of the Arctic is greatly influenced by a period of widespread Cretaceous magmatic activity, the High Arctic Large Igneous Province (HALIP). Two major tholeiitic magmatic pulses characterize HALIP: an initial 120 -130 Ma pulse that affected Arctic Canada and formally adjacent regions of Svalbard (Norway) and Franz Josef Land (Russia). In Canada, this pulse fed lava flows of the Isachsen Formation. A second 90-100 Ma pulse that apparently only affected the Canadian side of the Arctic, fed flood basalts of the Strand Fiord Formation. The goal of this thesis is to improve understanding of Arctic magmatism of the enigmatic HALIP through field, remote sensing, geochemical and geochronology investigations of mafic intrusive rocks collected in the South Fiord area of Axel Heiberg Island, Nunavut, and comparison with mafic lavas of the Isachsen and Strand Fiord Formations collected from other localities on the Island. Ground-based and remote sensing observations of the South Fiord area reveal a complex network of mafic sills and mainly SSE-trending dykes. Two new U-Pb baddeleyite ages of 95.18 ± 0.35 Ma and 95.56 ± 0.24 Ma from South Fiord intrusions along with geochemical similarity confirm these intrusions (including the SSE-trending dykes) are feeders for the Strand Fiord Formation lavas. -
Volume 12, 1959
THE ARCT IC CIRCLE THE COMMITTEE 1959 Officers President: Dr. D.C. Rose Vice -Presidents Mr. L.A.C.O. Hunt Secretary: Mr. D. Snowden Treasurer: Mr. J .E. Cleland Publications Secretary: Miss Mary Murphy Editor: Mrs .G.W. Rowley Members Mr. Harvey Blandford Mr. Welland Phipps Mr. J. Cantley Mr. A. Stevenson Mr. F..A. Cate Mr. Fraser Symington L/Cdr. J.P. Croal, R.C.N. Mr. J .5. Tener Miss Moira Dunbar Dr. R. Thorsteinsson W IC K. R. Greenaway, R.C.A.F. Dr. J.S. Willis Mr. T .H. Manning Mr. J. Wyatt Mr. Elijah Menarik CONTENTS VOLUME XlI, 1959 NO.1 Meetings of the Arctic Circle 1 Officers and Committee Members for 1959 Z Research in the Lake Hazen region of northern Ellesmere Island in the International Geophysical Year Z Anthropological work in the Eastern Arctic, 1958 13 Geomorphological studies on Southampton Island, 1958 15 Bird Sanctuaries in Southampton Island 17 Subscriptions for 1959 18 Change of Address 18 Editorial Note 18 NO. Z U.S. Navy airship flight to Ice Island T3 19 Firth River archaeological activities. 1956 and 1958 Z6 A light floatplane operation in the far northern islands, 1958 Z9 Change of Address 31 Editorial Note 31 NO.3 Meetings of the Arctic Circle 3Z The Polar Continental Shelf Project, 1959 3Z Jacobsen-McGill Arctic Research Expedition to Axel Heiberg Island 38 Biological work on Prince of Wales Island in the summer of 1958 40 Geographical Branch Survey in southern Melville Peninsula, 1959 43 Pilot of Arctic Canada 48 Subsc riptions for 1960 50 Change of Address 51 • Editorial Note 51 I NO.4 Meetings of the Arctic Circle 52 Officers and Committee Members for 1960 52 Some factors regarding northern oil and gas 53 Nauyopee. -
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. -
Geographical Report of the Crocker Land Expedition, 1913-1917
5.083 (701) Article VL-GEOGRAPHICAL REPORT OF THE CROCKER LAND EXPEDITION, 1913-1917. BY DONALD B. MACMILLAN CONTENTS PAGE INTRODUCTION......................................................... 379 SLEDGE TRIP ON NORTH POLAR SEA, SPRING, 1914 .......................... 384 ASTRONOMICAL OBSERVATIONS-ON NORTH POLAR SEA, 1914 ................ 401 ETAH TO POLAR SEA AND RETURN-MARCH AVERAGES .............. ........ 404 WINTER AND SPRING WORK, 1915-1916 ............. ......................... 404 SPRING WORK OF 1917 .................................... ............ 418 GENERAL SUMMARY ....................................................... 434 INTRODUCTJON The following report embraces the geographical work accomplished by the Crocker Land Expedition during -four years (Summer, 19.13, to Summer, 1917) spent at Etah, NortJaGreenland. Mr. Ekblaw, who was placed in charge of the 1916 expeditin, will present a separate report. The results of the expedition, naturally, depended upon the loca tion of its headquarters. The enforced selection of Etah, North Green- land, seriously handicapped the work of the expedition from start to finish, while the. expenses of the party were more than doubled. The. first accident, the grounding of the Diana upon the coast of Labrador, was a regrettable adventure. The consequent delay, due to unloading, chartering, and reloading, resulted in such a late arrival at Etah that our plans were disarranged. It curtailed in many ways the eageimess of the men to reach their objective point at the head of Flagler Bay, te proposed site of the winter quarters. The leader and his party being but passengers upon a chartered ship was another handicap, since the captain emphatically declared that he would not steam across Smith Sound. There was but one decision to be made, namely: to land upon the North Greenland shore within striking distance of Cape Sabine. -
Thermal Physics, Daniel V
PHY293F1 - Particles Part Lecturer: Prof. Kaley Walker Office: MP712; 416 978 8218 E-mail: [email protected] • Replies to e-mail within 2 business days (i.e. excluding weekends) but will not answer detailed questions by e-mail Office hours: Fridays 14:00 – 15:00 Course website for Particles Part: • http://www.physics.utoronto.ca/~phy293h1f/293_particles.html • Class announcements given on the website Lectures: 3 hours/week in MP203 • Mon. 15:00-17:00, Tues. 15:00-17:00 and Fri. 15:00-17:00 My research (1) • I am the Deputy Mission Scientist for the Atmospheric Chemistry Experiment (ACE) satellite • Launched in August 2003 for a two-year mission and still going strong… • We measure over 30 different species in the ACE satellite Earth’s atmosphere each day to study the changing composition relating to – Ozone depletion –Air quality –Climate change My research (2) • Studying the Arctic atmosphere from the Canadian high Arctic - PEARL in Eureka, Nunavut • A team of researchers will be going up there to see what happens when sunlight returns to the high Arctic (Feb.- Apr.) • On Ellesmere Island, 1100 km from the North Pole • PEARL is the most northern civilian research laboratory in the world • Nearest community is 420 km south at Grise Fiord PEARL, Eureka, Nunavut, 80 °N Textbook and Resources An Introduction to Thermal Physics, Daniel V. Schroeder (Addison Wesley Longman, 2000) • Available at UoT bookstore etc., should be some used ones Additional references available on short-term loan from the Physics and Gerstein libraries -
ESTIMATING PEARY CARIBOU (Rangifer Tarandus Pearyi) and MUSKOX (Ovibos Moschatus) NUMBERS, COMPOSITION and DISTRIBUTIONS on the HIGH ARCTIC ISLANDS of NUNAVUT
ESTIMATING PEARY CARIBOU (Rangifer tarandus pearyi) AND MUSKOX (Ovibos moschatus) NUMBERS, COMPOSITION AND DISTRIBUTIONS ON THE HIGH ARCTIC ISLANDS OF NUNAVUT Mitch Campbell1 1Regional Wildlife Biologist, Department of Environment, Government of Nunavut, P.O. Box 120, Arviat, NU X0C 0E0 2006 Status Report, No. 19 Campbell, M. 2006. Estimating Peary caribou (Rangifer tarandus pearyi) and muskox (Ovibos moschatus) numbers, composition and distributions on Ellesmere Island, Nunavut. Government of Nunavut, Department of Environment, Status report: 19, Iqaluit, 12 pp. SUMMARY REPORT TO NUNAVUT CO-MANAGERS Prepared By: Mitch W. Campbell Regional Biologist Department of Environment Wildlife Research Division P.O. 120 Arviat, Nu X0C 0E0 Ph: (867)857-2828 Fax: (867)857-2986 E-mail: [email protected] June 15th, 2006 Title: Estimating Peary Caribou (Rangifer tarandus pearyi) and Muskox (Ovibos moschatus) Numbers, Composition and Distributions on Ellesmere Island, Nunavut. Summary: The scientific study of Peary caribou and Muskox on Nunavut’s high arctic islands has been ongoing since May 2000. The data collected thus far on West Devon Island, Bathurst Island and Ellesmere Island are being analyzed and archived. The resulting file report will include a history of scientific study of Peary Caribou, the methods used during these studies, the population estimates of all surveys up to and including the 2006 Ellesmere survey, an analysis of satellite collar movement data, a resource selection analysis examining Peary caribou habitat, a summary of IQ collected by GN Biologists and a in-depth section pulling all aspects of the report into comprehensive management recommendations for the future study and continued co-management of Peary Caribou in Nunavut. -
Diet of Arctic Wolves on Banks and Northwest Victoria Islands, 1992-2001
Diet of Arctic Wolves on Banks and Northwest Victoria Islands, 1992-2001 Nicholas C. Larter Department of Environment and Natural Resources Government of the Northwest Territories 2013 Manuscript Report No. 230 The contents of this paper are the sole responsibility of the author. i ii ABSTRACT As part of a larger study, wolf stomachs were collected from entire wolf carcasses collected by local harvesters from Sachs Harbour (71°59’N 125°15’W) on Banks Island from 1992-2001, and from Ulukhaktok, formerly Holman (70°45’N 117°42’W) on Northwest Victoria Island from 1998-2001. Wolf scats were collected opportunistically during field research trips conducted on Banks Island from 1993-2001 and on Northwest Victoria Island from 1998-1999. A total of 129 stomachs and 38 scats from Banks Island, and 30 stomachs and two scats from Northwest Victoria Island were analyzed macro and microscopically for hair, feather, and bone fragments of prey items. Prey items were identified as closely as possible to species. Seventeen stomachs were empty. Remains of muskoxen (Ovibos moschatus) predominated being found in 90% of 115 and 88% of 27 stomachs from Banks Island and Northwest Victoria Island, respectively, and 87% of 38 and 100% of two scats from Banks Island and Northwest Victoria Island, respectively. Peary caribou (Rangifer tarandus pearyi), collared lemming (Dicrostonyx torquatus), Arctic hare (Lepus arcticus), Arctic fox (Alopex lagopus), snow goose (Chen caerulescens), ptarmigan (Lagopus spp.), and plant material were also found in stomachs and scats; however, only Peary caribou and collared lemming occurred in ≥5% of either stomachs or scats. -
Queen Elizabeth Islands: Problems Associated with Water Balance Research
Northern Research Basins Water Balance (Proceedings of a workshop held at Victoria, Canada, March 2004). IAHS Publ. 290, 2004 Queen Elizabeth Islands: problems associated with water balance research KATHY L. YOUNG1 & MING-KO WOO2 1 Geography Department, York University, 4700 Keele Street, Toronto, Ontario, M3JIP3, Canada klyoung(S>.vorku.ca 2 School of Geography and Geology, McMaster University, Hamilton, Ontario, L8S 4K1, Canada Abstract The Queen Elizabeth Islands in Arctic Canada are in an extremely remote region with long, cold winters, and 2- to 3-month summers, with 24-h daylight. Snow is a major part of annual precipitation, but there are few Arctic weather stations and precipitation data accuracy is hampered by gauge undercatch. Large spatial variations in snowmelt and evaporation make it difficult to extend point calculations over a basin. Currently no official hydrometric station exists in the Islands and the short-term available records are afflicted by stream gauging problems during peak flows. Annual water balances are often not closed, as not all the components are measured or calculated; this applies to early studies and to all glacierized catchments. Given the sensitivity of polar regions to climatic change and the likely importance of freshwater input to the Arctic Ocean, performing proper water balances for the basins in the Arctic Archipelago is a challenge. Key words Canadian Arctic; evaporation; permafrost; precipitation; Queen Elizabeth Islands; runoff; storage; water balance INTRODUCTION In the early 1970s, interest in Arctic hydrological research was largely stimulated by the planning of megaprojects in the Canadian Arctic Islands, such as the opening of mines and the designing of gas pipelines.