Quttinirpaaq National Park
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Late Wisconsinan Glaciation of Southern Eureka Sound: Evidence for Extensive Innuitian Ice in the Canadian High Arctic During Th
Quaternary Science Reviews 19 (2000) 1319}1341 Late Wisconsinan glaciation of southern Eureka Sound: evidence for extensive Innuitian ice in the Canadian High Arctic during the Last Glacial Maximum Colm OD Cofaigh! *, John England!, Marek Zreda" !Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada T6G 2E3 "Department of Hydrology and Water Resources, University of Arizona, Tucson, Arizona 85721, USA Abstract Southern Eureka Sound was originally proposed as the centre of an Innuitian Ice Sheet in the Canadian High Arctic at the Last Glacial Maximum (LGM) based largely on the pattern of Holocene emergence. This paper focuses on the glacial geological evidence for such an ice sheet in the region. Granite dispersal trains and ice-moulded bedrock record regional, westward #ow of warm-based ice into Eureka Sound from SE Ellesmere Island. Regional ice was coalescent with local ice domes on inter-"ord peninsulas. Marine limit in the form of raised deltas, beaches and washing limits formed during deglaciation of the regional ice. Throughout southern Eureka Sound, marine limit dates )9.2 ka BP, indicating that ice commenced retreat during the early Holocene. Ice-divides were located along the highlands of central Ellesmere and Axel Heiberg islands, from which ice inundated Eureka Sound, #owing north and south along the channel. Regional radiocarbon dates on marine limit show that deglaciation occurred in two steps. Initial break-up and radial retreat of ice from Eureka Sound to the inner "ords was rapid and preceded stabilisation along adjacent coastlines and at "ord heads. Two-step deglaciation is also re#ected in di!erences in glacial geomorphology between the inner and outer parts of many "ords. -
Read the National Inuit Strategy on Research
National Inuit Strategy on Research www.itk.ca About Inuit Tapiriit Kanatami Inuit Tapiriit Kanatami (ITK) is the national representational organization for the 65,000 Inuit in Canada, the majority of whom live in Inuit Nunangat, specifically, the Inuvialuit Settlement Region (Northwest Territories), Nunavut, Nunavik (Northern Québec), and Nunatsiavut (Northern Labrador). Collectively, these four regions make up Inuit Nunangat, our homeland in Canada. It includes 53 communities and encompasses roughly 35 percent of Canada’s landmass and 50 percent of its coastline. Consistent with its founding purpose, ITK represents the rights and interests of Inuit at the national level through a democratic governance structure that represents all Inuit regions. The comprehensive land claim agreements that have been settled in Inuit Nunangat form a core component of our organization’s mandate. These land claims have the status of protected treaties under section 35 of the Constitution Act, 1982, and we remain committed to fully implementing them in partnership with the Crown. ITK advocates for policies, programs, and services to address the social, cultural, political, and environmental issues facing our people. ITK is governed by a Board of Directors composed of the following members: Chair and CEO, Inuvialuit Regional Corporation • President, Makivik Corporation • President, Nunavut Tunngavik Incorporated • President, Nunatsiavut Government • In addition to voting members, the following non-voting Permanent Participant Representatives also sit on the -
Visitor Information Package to Arrive Prepared, to Identify Backcountry Challenges and to Plan an Enriching Arctic Experience, Please Read This Package Thoroughly
Visitor Information Package To arrive prepared, to identify backcountry challenges and to plan an enriching Arctic experience, please read this package thoroughly. 2019 For more information To reach park staff between September and early May, please contact Parks Canada in Iqaluit or visit our website. During the summer field season (approximately mid-May to mid-August), the Resolute office will assist you in connecting with field staff. Iqaluit office Hours of operation Resolute Bay office Phone: 867-975-4673 Year round Phone: 867-252-3000 Fax: 867-975-4674 Monday to Friday [email protected] 8:30 a.m. - 12 noon and 1 p.m. - 5 p.m. [email protected] Related websites Additional Resources: www.pc.gc.ca/quttinirpaaq Mirnguiqsirviit – Nunavut Territorial Parks: www.nunavutparks.com Nunavut Tourism: www.nunavuttourism.com Transport Canada: www.tc.gc.ca Weather Conditions: Resolute Bay: www.weatheroffice.gc.ca/city/pages/nu-27_metric_e.html Grise Fiord: www.weatheroffice.gc.ca/city/pages/nu-12_metric_e.html All photos copyright Parks Canada unless otherwise stated. 2019 Table of contents Welcome 2 Important information 3 - 4 Pre-trip, post-Trip, permits 3 Registration & de-registration 4 Planning your trip 5 Ukkusiksalik National Park map 5 Topographical maps 5 How to get here 6 - 7 Air access to Nunavut 6 Emergency medical travel 6 Travelling with dangerous goods 7 Community information 8 Local outfitters, visitor Information 8 Accommodations 8 Activities 9 - 11 Hiking and travelling to the North -
INTO the ARCTIC: Tour Companion Booklet
INTO THE ARCTIC Cory Trépanier’s Impassioned Vision of Canada’s Far North Over 50 Paintings • 3 Films • 1 Remarkable Experience Produced by David J. Wagner L.L.C. Companion Booklet to the Into The Arctic Prospectus 4 Cory Trépanier’s INTO THE ARCTIC A traveling museum exhibition of Canadian Arctic oil paintings by Cory Trépanier Produced by David J. Wagner L.L.C. Member of the American Alliance of Museums and International Council of Museums 414.221.6878 [email protected] davidjwagnerllc.com Exhibition artwork, video journals, photographs, and more at: www.intothearctic.ca 2 TABLE OF CONTENTS Introduction...............................................................................................................5 Glacierside at Embassy of Canada in Washington D.C. ................6 Glacierside: One of Four Pillars of the Collection.............................7 Great Glacier: Centrepiece of the Exhibition .....................................9 Testimonials..............................................................................................................11 Artist Bio................................................................................................................... 12 Artist Statement.....................................................................................................13 On Painting the Arctic.......................................................................................14 Painting With Arctic Peoples.........................................................................15 Artist -
Quttinirpaaq National Park Management Plan 2009
Quttinirpaaq National Park of Canada Management Plan Cover Photograph: Gull Glacier, Tanquary Fiord, © Parks Canada National Library of Canada cataloguing in publication data: Parks Canada. Nunavut Field Unit. Quttinirpaaq National Park of Canada: Management Plan / Parks Canada. Issued also in French under title: Parc national du Canada Quttinirpaaq, plan directeur. Issued also in Inuktitut under title: ᖁᑦᑎᓂᕐᐹᖅ ᑲᓇᑕᐅᑉ ᒥᕐᖑᐃᖅᓯᕐᕕᖓ ᒥᕐᖑᐃᖅᓯᕐᕕᓕᕆᓂᕐᒧᑦ ᐸᕐᓇᐅᑎ 1. Quttinirpaaq 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. FC3364.R53P37 2006 333.7809719'52 C2006-980239-4 © Her Majesty the Queen in the Right of Canada, represented by the Chief Executive Officer of Parks Canada, 2009. Paper: ISBN: 0-662-44205-9 Catalogue No.: R63-341/2006E PDF: ISBN 0-662-44206-7 Catalogue No.: R63-341/2006E-PDF Cette publication est aussi disponible en français. wktg5 wcomZoxaymuJ6 wktgotbsix3g6 . Quttinirpaaq NATIONAL PARK OF CANADA Management Plan OCTOBER 2009 Minister’s Foreword Canada’s national historic sites, national parks and national marine conservation areas offer Canadians from coast-to-coast-to-coast unique opportunities to experience and understand our wonderful country. They are places of learning, recreation and inspiration where Canadians can connect with our past and appreciate the natural, cultural and social forces that shaped Canada. From our smallest national park to our most visited national historic site to our largest national marine conservation area, each of these places offers Canadians and visitors several experiential opportunities to enjoy Canada’s historic and natural heritage. These places of beauty, wonder and learning are valued by Canadians - they are part of our past, our present and our future. -
Nunavut Photo Essay
ARCTIC VOL. 52, NO. 1 (MARCH 1999) P. 106– 112 InfoNorth Nunavut Photo Essay To celebrate the creation of Nunavut on 1 April 1999, we’ve gathered together a collection of photographs of Canada’s newest territory from friends, staff, and research associates of the Arctic Institute. In future issues of InfoNorth, we will present selections of photographs from Canada’s other territories. Many thanks to our contributors: J. Crump, M. Goodjohn, G. Holdsworth, J. Kobalenko, R. MacDonald, T. Nail, D.G. Reid, P. Schledermann, and D. Stenton. A special thank you to Frances Abele for her efforts on our behalf. The Nunavut Planning Commission Transition Team at Wager Bay Wilderness Lodge, July 1996. From left to right (top): Ron Tologanak, Louis Pilakapsi, Peter Suwaksiork, Loseeosee Aipellee, Bob Lyall, David Kunuk; (bottom): Bob Aknavigak, Sandra Fogliani, Akalayok Qavavau, Jobie Nutaraq. (J. Crump) Arctic tern. Mountain avens (Dryas integrifolia). Polar bear. (P. Schledermann) (P. Schledermann) (P. Schledermann) 106 INFONORTH • 107 Peary’s huts at Fort Conger, Ellesmere Island. (P. Schledermann) Iceberg in Alexandra Fiord, Ellesmere Island. (P. Schledermann) Ausuittuq (Grise Fiord), Ellesmere Island. (J. Kobalenko) Tanquary Fiord, Ellesmere Island. (J. Kobalenko) Ice cap on northern Ellesmere Island. (J. Kobalenko) Muskoxen on Truelove Lowland, August 1998. Arctic poppy (Papaver radicatum). Red-throated loon on the nest, Devon Island. (G. Holdsworth) (P. Schledermann) (T. Nail) 108 • INFONORTH The airport at Salliq (Coral Harbour), Southampton Island. (M. Goodjohn) Kangiqsliniq (Rankin Inlet). (M. Goodjohn) Cambridge Point, Coburg Island, June 1979. (D.G. Reid) Drying char at Omingmaktok (Bay Chimo). (J. Crump) Kugluktuk (Coppermine). (J. Crump) Elders from Ikaluktutiak (Cambridge Bay). -
Paper 63-30 Mesozoic and Tertiary Stratigraphy
PAPER 63-30 MESOZOIC AND TERTIARY STRATIGRAPHY, WESTERN ELLESMERE ISLAND AND AXEL HEIBERG ISLAND, DISTRICT OF FRANKLIN (Preliminary Account) E. T. Tozer Price 35 cents 1963 GEOLOGICAL SURVEY OF CANADA PAPER 63-30 MESOZOIC AND TERTIARY STRATIGRAPHY, WESTERN ELLESMERE ISLAND AND AXEL HEIBERG ISLAND, DISTRICT OF FRANKLIN (PRELIMINARY ACCOUNT) By E. T. Tozer DEPARTMENT OF MINBS AND TECHNICAL SURVEYS CANADA CONTENTS Page Introduction .........•.. , ...•.•........•.... , . • . • . • 1 Triassic .•..•...••.......•..•...•...•....• ,............... 2 Bjorne Formation ••........•.. , •... , .. , ...•...• , ,·. • 2 Blind Fiord Formation . • • . • . • • . • . • . • . • . • 3 Schei Point Formation ..••....•.••..•.• , . • . • • . • 4 B1aa Mountain Formation ...•..••...•..•• , •.. , • . • • . 6 Raanes Peninsula •.. , . • . • . • . • • • . • • . • • . 7 Fosheim Peninsula .•..••.•..•••.. , . • . • • . • 9 Northern Ellesmere Island..................... 9 Eastern'Axel Heiberg Island . • • . • • . • • • 13 Southwestern Axel Heiberg Island............... 13 Northwestern Axel Heiberg Island . • • . • • . • • . • 14 Northeastern Axel Heiberg Island . • • . • • . • . 14 Heiberg Formation • . • • • . • . • • . • . • • . • . • . • . • 15 Jurassic and Lower Cretaceous • • . • . • . • . • • . • . • . • . • • . 15 Borden Island Formation . • . • • . • . • • . • . 16 Savik Formation •... , . • . • • . • . • . • • . • • . • • • . 17 Southwestern Axel Heiberg Island............... 19 Northwestern ~xel Heiberg Island • . • . • . • . • . 21 Fay Islands,................................. -
Quttinirpaaq National Park of Canada State of the Park Assessment (2018)
Quttinirpaaq National Park of Canada State of the Park Assessment (2018) Prepared by: Jenna Boon, Field Unit Superintendent, Nunavut Field Unit Approved: ________________________________________ ______________________ Trevor Swerdfager Date Senior Vice-President, Operations Overview of Indicators- Quttinirpaaq National Park Satisfaction Buildings Learning Dams Enjoyment Fortifications Visits Highways Supportive Other Knowledge-based Roads Respectful Vehicular Bridges Indicator Ratings Good Accessible N/R Airfields Fair Partnerships Forest Poor N/R Not Rated Support Tundra N/A Not Applicable Promotion Shrublands Objects Wetlands Landscape Features Grasslands Freshwater Buildings and Glaciers Coastal/Marine Engineering Works Archaeological Sites Ecological Integrity Indicators Indicators Measures Overview This is the first Ecological Integrity (EI) assessment for Quttinirpaaq National Park. Following Agency direction for EI monitoring in northern parks, the EI monitoring program reports on two indicators: Tundra and Freshwater. The Tundra Plant Phenology (2017) overall condition and trend assessment for Ecological Integrity is ‘good’ and considered ‘stable’. Plant Community N/R Plant phenology is rated as “good” and “stable”. The program for the ground temperature, thaw tube and plant community measures is new and “not Plant Productivity (2013) rated”, as there is insufficient data for analysis available, although a baseline can be determined. The water flow program has a longer dataset, but a Active Layer – baseline cannot be determined yet as data was not collected during the same CALM Grid (2017) ↓ time-frames. These issues are being addressed. Inuit Knowledge measures have not yet been developed for the park. -- Ground N/R Temperature ↓ The overall trend for the Tundra Indicator is determined to be ‘stable’. The Circumpolar Active Layer Monitoring grid condition is rated as ‘good’, but with -- Thaw tube N/R a declining trend. -
Polar Continental Shelf Program Science Report 2016: Logistical Support for Leading-Edge Scientific Research in Canada and Its Arctic
PROGRAMME DU PLATEAU CONTINENTAL POLAIRE RAPPORT SCIENTIFIQUE 2016 POLAIRE RAPPORT CONTINENTAL PROGRAMME DU PLATEAU au Canada et dans l’Arctique dans et Canada au Soutien logistique à la recherche scientifique de pointe pointe de scientifique recherche la à logistique Soutien 2016 SCIENTIFIQUE RAPPORT Programme du plateau continental polaire continental plateau du Programme T 2016 Polar Continental Shelf Program SCIENCE REPOR SCIENCE REPORT 2016 Logistical support for leading-edge scientific research in Canada and its Arctic POLAR CONTINENTAL SHELF PROGRAM POLAR CONTINENTAL Polar Continental Shelf Program SCIENCE REPORT 2016 Logistical support for leading-edge scientific research in Canada and its Arctic Polar Continental Shelf Program Science Report 2016: Logistical support for leading-edge scientific research in Canada and its Arctic Contact information Polar Continental Shelf Program Natural Resources Canada 2464 Sheffield Road Ottawa ON K1B 4E5 Canada Tel.: 613-998-8145 Email: [email protected] Website: pcsp.nrcan.gc.ca Cover photograph: A meteorological, snow and permafrost data station in the Qarlikturvik valley, Bylot Island, Nunavut. The data from this station will be used to quantify the impact of willow growth on the permafrost thermal regime. Section header image: Preparing for departure on the Agassiz Ice Cap, Northern Ellesmere Island, after a successful ice core drilling mission. Photographers and map designers (alphabetically) Sean Arruda, Queen’s University: page 28 Max Friesen, University of Toronto: page -
Glaciers of North America— GLACIERS of CANADA
Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE ARCTIC ISLANDS GLACIERS OF THE HIGH ARCTIC ISLANDS By ROY M. KOERNER 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 Canadian High Arctic ice caps, both dynamic and stagnant, respond only very slowly to changes in climate. Ice cores contain records of environmental change during the past 100 thousand years, temperatures ranging from –20º C to +2.5º C. The last 150 years have been the warmest in the past 1,000 years, but only slight changes in area and volume (mass-balance) of ice caps are evident CONTENTS Page Abstract ---------------------------------------------------------------------------- J111 History of Glacier Research --------------------------------------------------- 111 FIGURE 1. Index map of the Canadian High Arctic islands ---------------- 112 The Ice Caps and Glaciers ----------------------------------------------------- 113 Dynamic Ice Caps and Outlet Glaciers -------------------------------- 113 FIGURE 2. Landsat 3 MSS image showing the western part of Devon Ice Cap on 10 August 1979 --------------------------------------- 114 3. Vertical aerial photograph taken in 1959 of Sverdrup Glacier on the northwest side of Devon Ice Cap --------------------- 115 4. Landsat 1 MSS false-color composite image of southwestern Ellesmere Island and part of northwestern Devon Island on 22 August 1974 ----------------------------------------------- 116 Topography ------------------------------------------------------------- 113 FIGURE 5. Landsat 1 MSS false-color composite image mosaic of the Prince of Wales Icefield and part of the Manson Icefield, central and southeastern Ellesmere Island on 20 and 22 August 1974 -------------------------------------------------- 117 6. Ice-thickness profiles measured by radio-echosounding in April-May 1976 ----------------------------------------------- 118 7. -
Arctic Plants Produce Vastly Different Numbers of Flowers in Three Contrasting Years at Lake Hazen, Quttinirpaaq National Park, Ellesmere Island, Nunavut, Canada
Arctic Plants Produce Vastly Different Numbers of Flowers in Three Contrasting Years at Lake Hazen, Quttinirpaaq National Park, Ellesmere Island, Nunavut, Canada ZOE A. P ANCHEN Department of Biology, Carleton University, 1125 Colonel By Drive, Ottawa ON K1S 5B6 Canada; email: Zoe.Panchen@ Carleton.ca Panchen, Zoe A. 2016. Arctic plants produce vastly different numbers of flowers in three contrasting years at Lake Hazen, Quttinirpaaq National Park, Ellesmere Island, Nunavut, Canada. Canadian Field-Naturalist 130(1): 56–63. To maximise reproductive success in the short Arctic growing season, plants pre-form flower buds the year prior to flower - ing. Flower bud production depends on warm ambient temperatures. Thus, although currently Arctic plants have low rates of sexual reproductive success, the warming climate may increase reproductive success. Following the long, warm growing season in 2012, plants at Lake Hazen, Ellesmere Island, produced many flowers in the short, cold growing season of 2013. Conversely, few flowers were produced in 2014, a long, warm growing season, but many flowers were produced in 2015, another long, warm growing season. Potentially higher rates of reproductive success in a warming climate could be compro - mised if consecutive years do not have long, warm growing seasons. Key Words: Arnica angustifolia ; Narrow-leaved Arnica; Cassiope tetragona ; Arctic White Heather; Pedicularis capitata ; Capitate Lousewort; climate change; flowering; flower abundance; reproductive success Introduction Saxifrage; Aupilattunnguat [Aiken et al. 2007]; Saxifra - To maximise sexual reproductive success in the short gaceae) at Tanquary Fiord, Quttinirpaaq National Park, Arctic growing season and to minimise time spent Ellesmere Island, Nunavut, is influenced by August and developing flower buds at the beginning of the grow - October mean minimum temperature, respectively, in ing season, many Arctic plants pre-form their flower the year preceding flowering (Panchen and Gorelick buds in the year or years prior to flowering (Sørensen 2015). -
Regional Congruence of Vegetation and Summer Climate Patterns in the Queen Elizabeth Islands, Northwest Territories, Canada SYLVIA A
ARCTIC VOL. 42, NO. 1 (MARCH 1989) P. 3-23 Regional Congruence of Vegetation and Summer Climate Patterns in the Queen Elizabeth Islands, Northwest Territories, Canada SYLVIA A. EDLUND’ and BEA TAYLOR ALT’ (Received 30 June 1986; accepted in revised form 21 June 1988) ABSTRACT. In the Queen Elizabeth Islands, regional distributions of vegetation and many summer climate patterns show similar, distinctive S-shaped patterns, a response to the interaction between regional topography and persistent northwesterly flow from the central Arctic Ocean. The cool and cloudy central polar pack ice climate bulges almost unimpeded into the low-lying islands of the northwest and north-central sector. This region has the least vascular plant diversity and is dominated almost entirely by herbaceous species. The mountainsof Axel Heiberg and Ellesmere islands create a barrier that effectively shelters an intermontane region from both thecentral Arctic Ocean climate and travelling cyclonic systems.In this large intermontane zone regional minimums of cloud cover and maximums of temperatures and melt season duration are found. This area contains the most dense and diverse vascular plant assemblages. Woody species and sedges dominate, and many species with more southerly limits occur as disjuncts. The plateaus and highlands in the southern islands modify the central Arctic Ocean climate sufficiently to produce an intermediate climate. Woody species and sedges also dominate this area; however, the density and diversity are less than that of the intermontane area. Several phytogeographic limits occur in the Queen Elizabeth Islands, including the northern limits of woody plants and sedges, and the northern limits of the dominanceof woody plants and sedges.