Intimate Spirits of Places
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Inuit Nunangat – Relocation Route
IInnuuiitt NNuunnaannggaatt ARCTIC OCEAN Grise Fiord RReellooccaattiioonn RRoouuttee ! Beaufort Sea Resolute Bay ! Parry Channel Baffin Bay Sachs Harbour ! Pond Inlet Tuktoyaktuk ! ! ! INUVIALUIT Arctic Bay Aklavik Clyde River ! Inuvik ! ! Inuit Com m unity ! ! Ulukhaktok (Holman Island) ! ! Paulatuk ! Davis Strait Inuit Regions Y U KON Qikiqtarjuaq ! Igloolik Inuvialuit Taloyoak ! Cambridge Bay ! Hall Beach ! ! N unavut Kugluktuk Pangnirtung ! Gjoa Haven ! ! !Kugaaruk (Pelly Bay) Umingmaktok N unatsiavut ! Great Bear Lake Bathurst Inlet ! Repulse Bay N unavik ! Iqaluit ! N ORTHW EST TERRITORIES NUNAVUT Cape Dorset ! !Kimmirut Coral Harbour Baker Lake ! ! Labrador Sea Kangiqsujuaq ! ! Chesterfield Inlet ! Ivujivik ! ! Salluit Quaqtaq Rankin Inlet ! Kangirsuk Great Slave Lake ! Whale Cove ! Akulivik ! NUNATSIAVUT ! Aupaluk! Kangiqsualujjuaq BRITISH Puvirnituq Nain ! ! ! Hopedale COLU MBIA Arviat ! Tasiujaq ! Kuujjuaq ! ! Makkovik ALBERTA ! Postville ! Inukjuak Rigolet • Distanc e b etween Inukjuak and Grise Fiord : 1,250 km (b y p lane) ! NUNAVIK • Distanc e b etween Grise Fiord and Resolute Bay : 250 km (b y p lane) Hudson Bay • Distanc e b etween Ottawa and Atlanta : 1,300 km (p ar avion) ! Churchill • Tim e Fram e Umiujaq ! N EW FOU N DLAN D AN D LABRADOR - The reloc atees' sea voyage b egan in late July 1953 in Inukjuak where Sanikiluaq ! they b oard ed the C.D. Howe. ) 7 - In late August the C.D. Howe arrived at Pond Inlet and p ic ked up the 3 Kuujjuarapik 8 0 MAN ITOBA ! 8 Q U EBEC 1 ad d itional Inuit fam ilies from Pond Inlet. 0 6 9 # - One group arrived at Grise Fiord in late August 1953 while the sec ond s c o d group arrived at Resolute Bay on C Chisasibi G ( Sep tem b er 7, 1953, as they had to c hange ship s from the C.D. -
THAW SETTLEMENT of DEGRADING PERMAFROST: a GEOHAZARD AFFECTING the PERFORMANCE of MAN-MADE INFRASTRUCTURES at UMIUJAQ in NUNAVIK (QUÉBEC) Richard Fortier, Ing., Ph.D
THAW SETTLEMENT OF DEGRADING PERMAFROST: A GEOHAZARD AFFECTING THE PERFORMANCE OF MAN-MADE INFRASTRUCTURES AT UMIUJAQ IN NUNAVIK (QUÉBEC) Richard Fortier, ing., Ph.D. Centre d’études nordiques, Université Laval, Québec, QC, Canada, G1V 0A6, [email protected] Maxime Bolduc, ing. jr. INSPEC-SOL, Montréal, QC, Canada, H4S 1C7 RÉSUMÉ La dégradation du pergélisol dans les régions nordiques peut provoquer des risques naturels comme la subsidence au dégel qui affecte la performance des infrastructures civiles. Par exemple, le long d’un segment de 300 m de longueur de la route d’accès à l’aéroport d’Umiujaq au Nunavik (Québec), trois zones de subsidence au dégel ont été étudiées durant l’été 2006; soit 15 ans après la construction de la route. La subsidence atteint par endroit jusqu’à 0,63 m pour un volume total de près de 530 m3. Des levés de géoradar et un profilage de résistivité électrique ont été réalisés afin de caractériser la stratigraphie du sous-sol et les conditions du pergélisol. Le dégel de sédiments marins gélifs sur une épaisseur d’au moins 4 m sous les zones de subsidence a provoqué un tassement et une diminution de l’indice des vides d’environ 15%. Le tassement au dégel est non seulement provoquée par la tendance au réchauffement climatique récemment observée au Nunavik mais aussi par l’accumulation de la neige le long de la route. Le couvert nival isole ainsi la surface du sol et prévient tout regel du sous-sol en hiver. Alors que la route est toujours carrossable, la seule mitigation économiquement viable au dégel du pergélisol est de laisser libre cours au tassement au dégel et de recharger le remblai lorsque cela est nécessaire jusqu’à sa stabilisation. -
Abstracts Annual Scientific Meeting ᐊᕐᕌᒍᑕᒫᕐᓯᐅᑎᒥᒃ ᑲᑎᒪᓂᕐᒃ
Abstracts Annual Scientific Meeting ᐊᕐᕌᒍᑕᒫᕐᓯᐅᑎᒥᒃ ᑲᑎᒪᓂᕐᒃ 2016 Réunion scientifique annuelle 5-9/12/2016, Winnipeg, MB ASM2016 Conference Program Oral Presentation and Poster Abstracts ABSTRACTS FROBISHER BAY: A NATURAL LABORATORY complete habitat characterization. This recent sampling FOR THE STUDY OF ENVIRONMENTAL effort recorded heterogeneous substrates composed of CHANGE IN CANADIAN ARCTIC MARINE various proportions of boulder, cobbles, gravel, sand HABITATS. and mud forming a thin veneer over bedrock at water depths less than 200 metres. Grab samples confirm Aitken, Alec (1), B. Misiuk (2), E. Herder (2), E. the relative abundance of mollusks, ophiuroids and Edinger (2), R. Deering (2), T. Bell (2), D. Mate(3), C. tubiculous polychaetes as constituents of the infauna Campbell (4), L. Ham (5) and V.. Barrie (6) in the inner bay. Drop video images captured a diverse (1) University of Saskatchewan (Saskatoon, Canada); epifauna not previously described from the FRBC (2) Department of Geography, Memorial University of research. A variety of bryozoans, crinoid echinoderms, Newfoundland (St. John’s, NL, Canada); sponges and tunicates recorded in the images remain (3) Polar Knowledge Canada (Ottawa, Ontario, to be identified. Habitat characterization will allow us Canada); to quantify ecological change in benthic invertebrate (4) Marine Resources Geoscience, Geological Survey of species composition within the habitat types represented Canada (Dartmouth, NS, Canada); at selected sampling stations through time. Such long- (5) Canada-Nunavut Geoscience Office, Natural term studies are crucial for distinguishing directional Resources Canada (Iqaluit, NU, Canada); change in ecosystems. Marine Geological Hazards (6) Marine Geoscience, Geological Survey of Canada and Seabed Disturbance: Extensive multibeam (Sidney, BC, Canada) echosounding surveys have recorded more than 250 submarine slope failures in inner Frobisher Bay. -
Protecting the Nastapoka River – a Multicultural Approach to Sustainability
Geophysical Research Abstracts Vol. 21, EGU2019-3379, 2019 EGU General Assembly 2019 © Author(s) 2019. CC Attribution 4.0 license. Protecting the Nastapoka River – A Multicultural Approach to Sustainability Arielle Frenette and Najat Bhiry Centre for Northern Studies (CEN), Dép. de géorgaphie, Université Laval, Canada This presentation aims to describe and analyze a case study concerning the creation of a 27,000 km2 national park near the village of Umiujaq, Nunavik (Northern Québec). The aim of the park is to protect the Nastapoka River and the majority of its watershed from mining and hydroelectric development projects. With a 30 m high waterfall near its mouth, the Nastapoka River is of great importance to the region as it is part of the ancestral Inuit land as well as a habitat for the world’s only population of freshwater seals. It is located on Inuit and Cree territory, whose people hunt and fish in the area. The river was first targeted by Hydro-Québec (a provincial hydroelectricity company) for a mega-complex project called Grande-Baleine, but that was set aside by the government of Québec in 1994. In 2008, an important development project named Plan Nord was announced by the government of Québec. Plan Nord was implemented in 2011 to provide access to natural resources in Northern Québec. It aims to protect 50% of northern natural land – an objective that was largely denounced as a form of “compensation” so that Plan Nord could be held up as an “exemplary project of sustainable development”. National park projects were already underway in Nunavik. -
Transportation Department Activity Report
TRANSPORTATION department ACTIVITY REPORT MARCH 2020 TO MAY 2021 The Transportation department is responsible for the safe and secure management of 14 certified airports, 14 Marine Ports, the Usijit para-transport and public transit services, and the Off Highway Vehicle awareness program in Nunavik. Human Resources Hiring: Noah Jaaka, Coordinator, Operations and Maintenance, Kangiqsujuaq Malek Kalthoum, Coordinator, Infrastructure and Projects, Kuujjuaq Lissa Deveaux, Administrative Technician, Kuujjuaq Jose Pauyungie, Observer/Communicator Trainee, Akulivik Uttuqi Carrier, Observer/Communicator, Quaqtaq Robbie Ningiuruvik, Rotational Observer/Communicator, Nunavik Qirniulau Rockfort, Maintainer, Kuujjuaq Peter Annanack, Seasonal Maintainer, Kangiqsualujjuaq Elijah Etok, Seasonal Maintainer, Aupaluk Uqittuk Iyaituk, Seasonal Maintainer, Ivujivik Noah Qurnak, Seasonal Maintainer, Salluit Michel Boivin, Rotational Electrician, Nunavik William Taylor, Airport Response Specialist, Puvirnituq Training: Workplace Hazardous Material Information System (WHMIS) training tour started in March. Maintainers and Observer/Communicators from Inukjuak, Puvirnituq, Salluit, Kangiqsujuaq, Quaqtaq, Tasiujaq, and Kuujjuaq have been trained so far, as well as rotational mechanics and electricians. Every airport employee will be trained before the end of the summer. Heavy equipment training in winter conditions was given to Maintainers at Umiujaq and Akulivik airports in March. Airfield Movement Surface Condition Reporting (AMSCR) training -
Recovery Strategy for the Harbour Seal, Lacs Des Loups Marins Subspecies (Phoca Vitulina Mellonae)
Species at Risk Act 1 Recovery Strategy Series Recovery strategy for the Harbour Seal, Lacs des Loups Marins subspecies (Phoca vitulina mellonae) Harbour Seal, Lacs des Loups Marins subspecies Photo: F. Martin 2018 Recommended citation: DFO. 2018. Recovery Strategy for the Harbour Seal, Lacs des Loups Marins subspecies (Phoca vitulina mellonae). Species at Risk Act Recovery Strategy Series. Fisheries and Oceans Canada, Ottawa. v + 28 pp. For copies of the recovery strategy, or for additional information on species at risk, including COSEWIC Status Reports, residence descriptions, action plans, and other related recovery documents, please visit the SAR Public Registry1. Cover illustration: François Martin, Nunavik Research Center, Makivik Également disponible en français sous le titre «Programme de rétablissement du phoque commun, sous-espèce des lacs des Loups Marins (Phoca vitulina mellonae)» © Her Majesty the Queen in Right of Canada, represented by the Minister of Fisheries and Oceans, 2018. All rights reserved. ISBN 978-0-660-09219-5 Catalogue no. En3-4/259-2017E-PDF Content (excluding the illustrations) may be used without permission, with appropriate credit to the source. 1 http://www.registrelep.gc.ca/ Recovery strategy for the Lacs des Loups Marins Harbour Seal 2018 PREFACE The federal, provincial, and territorial government signatories under the Accord for the Protection of Species at Risk (1996) agreed to establish complementary legislation and programs that provide for effective protection of species at risk throughout Canada. Under the Species at Risk Act (S.C. 2002, c.29) (SARA), the competent federal ministers are responsible for the preparation of recovery strategies for listed extirpated, endangered, and threatened species and are required to report on progress five years after the publication of the final document on the SAR Public Registry. -
Stream Turbidity Within Degrading Permafrost Terrain in the Tasiapik Valley, Umiujaq Region, Nunavik
Geophysical Research Abstracts Vol. 21, EGU2019-2753, 2019 EGU General Assembly 2019 © Author(s) 2018. CC Attribution 4.0 license. Stream Turbidity within Degrading Permafrost Terrain in the Tasiapik Valley, Umiujaq Region, Nunavik Frederic Manseau (1,2), Najat Bhiry (1,2), John Molson (2,3), Danielle Cloutier (2,4) (1) Department of Geography, Laval University, Québec, Canada, (2) Centre for Northern Studies (CEN), Laval University, Québec, Canada, (3) Department of Geology and Geological Engineering, Laval University, Québec, Canada, (4) Faculty of Forestry, Geography and Geomatics, Laval University, Québec, Canada Permafrost degradation caused by rising temperatures has had a significant impact on northern ecosystems. For example, it contributes to greenhouse gas emissions, increased recurrence of landslides, and changes in water resources. Sediment migration to the soil surface has also been observed during soil settlement caused by thawing permafrost. Soil settlement increases the flow of water, which is enriched in organic matter and mineral sediments, toward streams and lakes, resulting in increased suspended sediment load and increased river turbidity. Furthermore, during flood episodes in spring and high rainfall in autumn, the loose sediment is supported and transported toward the river by surface runoff. This increase in turbidity can have negative effects on the trophic chain, especially on fish as a result of the abrasion of their gills. Variations in river turbidity have been examined in several studies (Lawler et al., 2006; Hamilton and Luff- man, 2009). However, in the context of current and future climate change, there is limited knowledge about the effects of variations in river turbidity associated with permafrost degradation. -
Nord-Du-Québec Plan Régional De Conservation Des Milieux Humides 10 Et De Leurs Terres Hautes Adjacentes
RÉGION Nord-du-Québec Plan régional de conservation des milieux humides 10 et de leurs terres hautes adjacentes LES MILIEUX HUMIDES UNE SOURCE DE VIE PLAN DE CONSERVATION Portrait des milieux humides et de leurs terres hautes adjacentes de la région administrative du Nord-du-Québec 2009 Analyse et rédaction : Pierre Dulude, biologiste, CIC Jason Beaulieu, spécialiste en géomatique, CIC Géomatique et cartes : Sylvie Picard, technicienne en géomatique, CIC Karine Boisvert, technicienne en géomatique, CIC Comité externe de lecture : Luc Bélanger, biologiste, EC/SCF Jean Huot, biologiste, Université Laval Marcel Laperle, biologiste Michel Lepage, biologiste Monique Poulin, prof. adj., dép. phytologie, FSAA, U. L. Guy Pustelnik, directeur, EPTB-ÉPIDOR (France) Révision linguistique : Marie Blais, CIC Préparé par Canards Illimités Canada, en partenariat avec le ministère des Ressources naturelles et de la Faune (MRNF) du Québec, le ministère du Développement durable, de l’Environnement et des Parcs (MDDEP) du Québec, le ministère des Affaires municipales et des Régions (MAMR) du Québec, Environnement Canada (SCF/EC), et Pêches et Océans Canada (MPO). Canards Illimités Canada 2009 ISBN 978-2-923725-13-0 Dépôt légal – Bibliothèque nationale du Québec, 2009 Dépôt légal – Bibliothèque nationale du Canada, 2009 Citation recommandée CANARDS ILLIMITÉS CANADA. 2009. Plan de conservation des milieux humides et de leurs terres hautes adjacentes de la région administrative du Nord-du-Québec [en ligne], [http://www.canardsquebec.ca], 101 p. Plan de conservation -
Les Changements Climatiques Au Nunavik Et Au Nord Du Québec: L’Accès Au Territoire Et Aux Ressources
1 Les changements climatiques au Nunavik et au Nord du Québec: L’accès au territoire et aux ressources Rapport Final Présenté aux Initiatives des écosystèmes nordiques Environnement Canada Soumis par : Martin Tremblay et Christopher Furgal Service des Ressources renouvelables - Administration régionale Kativik et Indigenous Environmental Studies Program - Trent University Kuujjuaq 31 mars 2008 2 Service des Ressources renouvelables Administration régionale Kativik C.P. 9 Kuujjuaq (Québec) J0M 1C0 Téléphone : (819) 964-2961 Fax : (819) 964-0694 Photos de la page couverture : 1) Motoneigiste à Puvirnituq, 2) Village nordique de Kangiqsujuaq, 3) Chasseur à Umiujaq et 4) Glaces mobiles au Détroit d’Hudson. © Service des Ressources renouvelables, Administration régionale Kativik, 2008. Les changements climatiques au Nunavik et au Nord du Québec : L’accès au territoire et aux ressources Initiatives des écosystèmes nordiques – Environnement Canada Rapport final, Mars 2008 3 Table des matières Table des matières................................................................................................................3 Liste des figures ...................................................................................................................5 Liste des tableaux.................................................................................................................6 1. Renseignements généraux sur le projet (1.) *...................................................................7 1.1 Nom du projet (1.1) * ................................................................................................... -
THE Nunavik INUIT
THE NUNAVIK INUIT POPULATION AND TERRITORY THE DEVELOPMENT OF NUNAVIK SINCE 1975 AND MAJOR CURRENT ISSUES • In Québec, the Inuit reside in Nunavik, a semi-arctic and arctic region th located north of the 55 parallel. • In 1975, the Inuit, the Cree, Québec and the federal government concluded the James Bay and Northern Québec Agreement (JBNQA). - Over the last three centuries, contacts between Europe and Nunavik were largely maintained by Anglican missionaries, fur traders and the - For a quarter of a century after this, JBNQA shaped the political, Hudson Bay Company. economic, social, legal and institutional world of Northern Québec. - The Inuit were a nomadic people. They adopted a settled lifestyle at • For the Inuit, economic development, preservation of their culture and the beginning of the Fifties. language, improvement of public health and education, elimination of social problems (violence, alcohol and drugs, etc.) and the establishment 2 • An immense territory of approximately 500,000 km of a justice administration appropriate to the community represent the (one-third of Québec), Nunavik has a population of about 11,000, major long-term issues. of whom 10,000 are Inuit. • The first schools were established during the Fifties. Since the end of the - The population of Nunavik is young: 60% is under the age of 25, i.e. Seventies, the educational system has come under Québec’s jurisdiction twice the proportion in Southern Québec. and was placed under the purview of the Kativik School Board. - They live in 14 villages of between 150 to 1,800 residents. These - Inuit language and culture are taught throughout the elementary and villages are located along Hudson Bay and Ungava Bay. -
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20+ NEWEST LANDSCAPE LENSES X GUIDE TO LAKE TAHOE NEW LOOK! SCENIC WILDLIFE TRAVEL SPORTS outdoorphotographer.com LANDSCAPE ISSUE Robert Glenn Ketchum ALASKA’S STUNNING SOUTHWEST Justin Black LANDSCAPE ABSTRACTIONS Stan Moniz ADVENTURE IN OREGON + TECHNIQUE Make a Wildlife Panorama March 2017 Exceptional Images Deserve an Exceptional Presentation Images by: Neil Simmons Oachs, Stephen Max Seigal, MetalPrint Clusters & Splits Available in 21 Arrangements & Sizes Display Your Images in Their Element Choose our Wood Prints to lend a warm, natural feel to your images, MetalPrints infused on aluminum for a vibrant, luminescent look or Acrylic Prints for a vivid, high-impact display. All options provide exceptional durability and image stability, for a gallery-worthy presentation that will last a lifetime. Available in a wide range of sizes, perfect for anything from small displays to large installations. Learn more at bayphoto.com/wall-displays 25% Get 25% off your fi rst order with Bay Photo Lab! For instructions on how to redeem this special off er, create a free OFF account at bayphoto.com. Your First Order NEW! Easy Web Ordering! o rd om Stunning Prints er.bayphoto.c on Natural Wood, High Defi nition Metal, or Vivid Acrylic Quality. Service. Innovation. We’re here for you! CONTENTS VOL. 33 NO. 2 | MARCH 2017 FEATURES 28 ALASKAN LEGACY How Robert Glenn Ketchum became a leading advocate for the preservation of Southwest Alaska’s ecosystems and economies By Wes Pitts / Photography By Robert Glenn Ketchum 36 OREGON ODYSSEY An adventure photographer’s -
Processus Gravitaires Dans La Vallée Tasiapik (Nunavik) : Témoins Géomorphologiques De La Dynamique De Versant Récente Et Passée
Processus gravitaires dans la vallée Tasiapik (Nunavik) : témoins géomorphologiques de la dynamique de versant récente et passée Mémoire Samuel Veilleux Maîtrise en sciences géographiques - avec mémoire Maître en sciences géographiques (M. Sc. géogr.) Québec, Canada © Samuel Veilleux, 2019 ii Résumé Ce projet de recherche, mené près d’Umiujaq (Nunavik), a été réalisé afin de documenter les processus gravitaires dominants qui se manifestent sur les versants escarpés de la vallée Tasiapik. Des relevés topographiques, granulométriques, morphométriques, pétrographiques et de végétation ont permis de caractériser 18 talus d’éboulis situés sur les versants sud-ouest et nord-est. Les résultats obtenus ont permis d’établir que l’éboulisation importante sur les versants de la vallée est un phénomène à la fois ancien, engendré par des processus paraglaciaires, et récent, résultat de processus périglaciaires toujours actifs aujourd’hui. Cela se traduit notamment par différents stades de développement des talus d’éboulis subactuels, illustrés par certains dépôts de versant frais et d’autres très anciens, mais aussi avec des topographies de pente très variables. Sur une échelle de temps plus courte, entre août 2017 et juillet 2018, les avalanches se sont avérées être un processus majeur, tel qu’observé sur les 14 000 photographies obtenues grâce à trois caméras à déclenchement automatique installées à l’été 2017. Ces avalanches, souvent déclenchées par des chutes de corniches à neige, ont été particulièrement fréquentes au printemps 2018, résultant de conditions météorologiques propices telles qu’une hausse rapide des températures journalières et des épisodes de pluie abondante. Des dépôts d’avalanches sales témoignent d’une grande capacité érosive, et incidemment de leur grand apport en débris vers les talus d’éboulis.