Annual Report 2016-2017 ENG 25-09-2018
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Tipi Instructions
Tipi Instructions Hello and thanks for buying one of our Tipi Tents. Here are the instructions for the best way to put it up, take it down and how to store when not in use. We’ve provided a step-by-step picture guide for you to follow along with the written instructions. At the bottom of these instructions we’ve added some advice and tips on how to get years of good service out of your tent by looking after it properly. Enjoy! And don’t hesitate to contact us if you have any questions, good ideas or better ways of doing it. Once you’ve erected your tent, we would love to see your Boutique Camping pictures, so please send them to us at [email protected]. They may even feature on our blog or Facebook page! Putting up a Tipi Tent Some general advice • We advise having 2 people to erect the tent, as it will of course simplify the process. By all means, you can put it up on your own, but of course the more the merrier, easier and quicker! • Find a flat piece of land, with ample space to comfortably put up your tent remembering to include room for the guy ropes • To prevent damaging the groundsheet, remove all sharp objects from the area. Things like stones and roots etc • Be careful when creating tension with the guy ropes, always try to keep the tension even, and never over do it. Be firm but gentle. • Before you peg out the tent, make sure all zips are closed, and check again when you adjust the guy ropes • Peg out the guy ropes in line with the tent seams How to Put Up Your Tipi A1)Open all bags and lay out all parts. -
Winter Camping and Backpacking Tips
Winter Camping and Backpacking Tips Camping or backpacking in the snow appeals to anyone who enjoys the beauty and peacefulness of a pristine winter wonderland. There are no bugs or crowds, and who doesn't enjoy playing in the snow? With a little preparation, you also might be surprised at how comfortable it can be. Here's a look at how to get started. Pre-trip Planning Winter outings offer different challenges than summer camping. You must be prepared for more severe weather and shorter daylight hours by having extra gear and additional skills. Before you leave home, have a plan. Don't go alone. Share your adventure with a few friends who have expertise in different winter skills (snow shelters, route finding, snow travel, etc.). Study maps and research the area. How long will it take to get there and set up camp? If something goes wrong, what emergency services (i.e., medical, search & rescue) are closest? Talk to people who have been there and can give you pointers. Check the weather forecast. Are conditions favorable? The NOAA-NWS Web site offers detailed backcountry forecasts. Check the local road and trail conditions. Recognize and avoid avalanche areas. Check the local avalanche forecast and don't go if avalanche danger is high. Keep in mind that avalanche forecasts may be general and not accurate for specific areas. If you are on or near any slope greater than 20°, your group should have formal avalanche training. Leave a trip plan. Let others know where you'll be, when you'll be there, when you'll return, vehicle information and names and contact number for participants in your group. -
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. -
The Sámi People and Their Culture the Sámi Or Saami Were Also Called Lapps Or Laplanders by the English
The Sámi people and their culture The Sámi or Saami were also called Lapps or Laplanders by the English. Sámi people consider the English terms derogatory. The Sámi are recognized as the only indigenous people of Europe. They have lived in Norway, Sweden, Finland and Russia. Their origins are Finno‐Ugric, a Hungarian and Yugra (Urals) past, inhabiting the Sápmi region. Today, the region encompasses large parts of Norway and Sweden, northern parts of Finland, and the Murmansk Oblast (Kola Peninsula) of Russia. The Sámi people have their own language, culture and customs that differ from others around them. This has caused the Sámi social problems and culture clashes. As we learned from our Sámi culture presentation and a quote from ‐religiousstudiesproject.com the following: “The history between the Sámi and the Norwegian government has left a stain on the Sámi for generations: The Norwegianization policy undertaken by the Norwegian government from the 1850s up until the Second World War resulted in the apparent loss of Sami language and assimilation of the coastal Sami as an ethnically‐distinct people into the northern Norwegian population. Together with the rise of an ethno‐political movement since the 1970s, however, Sami culture has seen a revitalization of language, cultural activities, and ethnic identity (Brattland 2010:31).” Note: Suggested readings, ‐laits.utexas.edu, a 19‐part series by the University of Texas entitled “Sámi Culture.” The other reading is‐ unsr.vtaulicorpuz.org. It is a report by the United Nations on the rights of indigenous people such as the Sámi. Reindeer are the Sámi key element to how they live. -
Nunavik Comparative Price Index
Nunavik Comparative Price Index Gérard Duhaime Pierre Fréchette Jean-François Langlais Tanya Lynn Strong Collection RECHERCHE EN LIGNE La Chaire de recherche du Canada sur la condition autochtone comparée est affiliée au Centre interuniversitaire d’études et de recherches autochtones (CIÉRA) et à la Faculté des sciences sociales de l'Université Laval. Le présent document a été publié initialement dans la collection Recherche du Groupe d’études inuit et circumpolaires. Adresse postale: Chaire de recherche du Canada sur la condition autochtone comparée Centre interuniversitaire d’études et de recherches autochtones Pavillon Charles-De Koninck Université Laval Québec, QC Canada G1K 7P4 Téléphone: (418) 656-7596 Télécopieur: (418) 656-3023 [email protected] © Gérard Duhaime, Pierre Fréchette, Jean-François Langlais, Tanya Lynn Strong ISBN : 2-921438-44-5 Dépôt légal: Bibliothèque nationale du Québec, 2è trimestre 2000 Bibliothèque nationale du Canada, 2è trimestre 2000 La Chaire de recherche du Canada sur la condition autochtone comparée est affiliée au Centre inte- runiversitaire d’études et de recherches autochtones (CIÉRA) et à la Faculté des sciences sociales de l'Université Laval. Le présent document a été publié initialement dans la collection Recherche du Groupe d’études inuit et circumpolaires. Adresse postale: Chaire de recherche du Canada sur la condition autochtone comparée Centre interuniversitaire d’études et de recherches autochtones Pavillon Charles-De Koninck Université Laval Québec, QC Canada G1K 7P4 Téléphone: (418) 656-7596 Télécopieur: (418) 656-3023 [email protected] Photographie de la couverture: Nick Bernard © Gérard Duhaime, Pierre Fréchette, Jean-François Langlais, Tanya Lynn Strong ISBN : 2-921438-44-5 Dépôt légal: Bibliothèque nationale du Québec, 2è trimestre 2000 Bibliothèque nationale du Canada, 2è trimestre 2000 TABLE OF CONTENTS TABLE OF CONTENTS............................................................................................................................ -
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. -
Parc Des Pingualuit
PAP_etat.qxd 9/7/01 8:53 AM Page 3 Status Report Parc des Pingualuit Société de la faune et des parcs du Québec Acknowledgements I am grateful to everyone who contributed to this report in any way. I would especially like to thank the following people: Parc des Pingualuit Working Group Vicky Gordon Willie Adams Michael Barrett Michel Damphousse Charlie Ulaku Community of Kangiqsujuaq Ulaayu Pilurtuut Arngak Charlie Arngak Betsy Etidloe Papikatuk Sakiagak Société de la faune et des parcs du Québec Marthe Laflamme Serge Alain Jean Boisclair Stéphane Cossette Jean Gagnon Gilles Harvey André Lafrenière Louis Lefebvre André Rancourt Jacques Talbot Denis Vandal Raymonde Pomerleau Project Coordinator, Parc des Pingualuit Acknowledgements I Table of contents List of maps, tables, and figures V List of maps V List of tables V List of figures VI Introduction VII Regional Context 1 Northern Québec 1 Demography 1 Territorial access and transportation 5 Local administration 6 Economic activity 8 Tourism development 9 Northern Village of Kangiqsujuaq 10 Population and services 10 Economic activity 10 Access 10 Land regime 15 Study Area 17 Climatic conditions 17 Temperature 18 Frost–free season 18 Precipitation 18 Day length 33 Ice formation and break-up on lakes and rivers 33 Biophysical resources 33 Relief and slopes 33 Geology 34 Origin of the crater 41 Geomorphology 42 The Pleistocence 42 The Holocene 51 Deposits 59 Hydrography 63 Vegetation 68 Fauna 75 Special features 89 Table of contents III Archaeological and historical resources 89 Archaeology -
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. -
Inuit Knowledge and Use of Wood Resources on the West Coast Of
Document generated on 10/02/2021 5:05 a.m. Études/Inuit/Studies Inuit knowledge and use of wood resources on the west coast of Nunavik, Canada Savoir inuit et utilisation des ressources en bois sur la côte ouest du Nunavik, Canada Stéphanie Steelandt, Najat Bhiry, Dominique Marguerie, Caroline Desbiens, Minnie Napartuk and Pierre M. Desrosiers Volume 37, Number 1, 2013 Article abstract Driftwood and shrubs are the primary wood resources available in most areas URI: https://id.erudit.org/iderudit/1025259ar of coastal Nunavik. Today, they are mainly used as fuel for campfires, but DOI: https://doi.org/10.7202/1025259ar historically they were very important for the ancestors of present-day Inuit. This article documents Inuit traditional knowledge about the origin, See table of contents availability, gathering, and exploitation of wood resources in this region located in the Low Arctic and the Subarctic. Interviews were conducted with 27 Inuit between 60 and 89 years of age in the villages of Ivujivik, Akulivik, Publisher(s) Inukjuak, and Umiujaq on the east coast of Hudson Bay. Our data reveal, among other things, that Inuktitut names for pieces of driftwood were based Association Inuksiutiit Katimajiit Inc. on shape, aspect, colour, and texture. This traditional knowledge was very Centre interuniversitaire d’études et de recherches autochtones (CIÉRA) accurate and highly diverse in the southern villages because of their significant exposure to driftwood. Wood from shrubs (i.e. willows, birches, and alders) ISSN was mainly harvested in the fall and used to make fires, mattresses, sleeping mats (alliat), and other objects. According to the participants, driftwood 0701-1008 (print) originates in southern Hudson Bay and James Bay and is washed up on the 1708-5268 (digital) beaches in late summer and the fall. -
Tent Inspection
Tent Guide Information referenced from the 2015 Frederick County Fire Prevention Code A Tent is defined as a structure, enclosure or shelter, with or without sidewalls or drops, constructed of fabric or pliable material supported by any manner except by air or the contents that it protects. All Tents: • A permit issued by the Frederick County Fire Marshal’s office shall be required for tents over 900 square feet not being used for recreational camping purposes. (Frederick County fire Prevention Code section 107.2 Permit Required.) • A detailed site and floor plan for tents with occupant load of 50 or more shall be required with each application for approval. The tent floor plan shall indicate details of means of egress, seating capacity, arrangement of seating and location and types of heating and electrical equipment. (Frederick County fire Prevention Code section 3103.6 Construction documents.) • An unobstructed fire break passageway or fire road not less than 12 feet wide and free from guy ropes or other obstructions shall be maintained on all sides of all tents unless otherwise approved by the fire code official. (Frederick County fire Prevention Code section 3103.8.6 Fire break.) • A certificate from an approved laboratory stating that the materials used in tent meet the flame- retardant criteria needed to pass NFPA Test Method 1 or Test Method 2. (Frederick County fire Prevention Code section 3104.2 Flame propagation performance treatment.) • Approved “No Smoking” signs shall be conspicuously posted. (Frederick County fire Prevention Code section 3104.6 Smoking.) • At least one 5lb. multipurpose 2A 10BC portable fire extinguisher shall be hung and tagged within 75 ft of travel distance. -
Building a Tipi
Building a Tipi Overview: This lesson uses photographs, objects, and a small tipi to introduce students to the tipi as one type of housing used long ago by Indians living on the Kansas plains. Sentence strips and corresponding pictures reinforce ten facts about the tipi. This lesson is designed to be taught in two parts. Recommendation: It is recommended that the lesson “Indians in Kansas Today” be taught first and that the tipi lesson be taught in conjunction with those on the grass house and earth lodge. Objectives: Content The student identifies facts about the tipi. The student identifies that natural resources were used to make tools and tipis. The student identifies where tipis were used in Kansas. Skills The student matches pictures to expository text. The student reads expository text to gain knowledge. The student reads to practice fluency. Essential Questions: Who lived in tipis in Kansas? Why did Indians choose to make their house out of bison hide and wood? Trunk Materials Needed: “Setting Up a Tipi” sequence cards Miniature tipi o Tipi cover (fabric) o Tipi footprint marked for pole placement (fabric) o 4 Lacing Pins o Tipi Instruction Sheet Kansas floor map (fabric) Tipi scale model 10 pink tipi sentence strips and corresponding picture clue cardss Pocket chart Reproduction Objects Pole sample Scraper (stone attached to elk antler) Tanned hide without fur Sinew Awl Flesher Images #13-20 #13 – Dry Kansas Environment Indian Homes in Kansas - A Traveling Resource Trunk Kansas State Historical Society ©2006 40 #14 – Tipi Village #15 – Bison #16 – Travois #17 – Setting Up a Tipi #18 – Scraping a Bison Hide #19 – Three Tipis #20 –Girls with a Toy Tipi Materials You Need to Supply: 11 poles for tipi (These should be 36” long and approximately 5/16” in diameter. -
Northern News and AINA News
INFONORTH • 221 NORTHERN NEWS Grant-in-Aid Program Recipients for 2007 The Grant-in-Aid committee received 25 applications Mitiarjuk Attasie Nappaaluk, 1931–2007 this year, and sufficient funds were available for grants to Mitiarjuk Nappaaluk, Nunavik educator and author, ten individuals. The committee congratulates the success- died in Kangiqsujuaq, Quebec, on 30 April 2007. Dedi- ful applicants, whose names and research topics are listed cated to preserving Inuit culture, Mitiarjuk Nappaaluk below. Gregory Goldsmith, University of Alaska Fairbanks, authored over 20 books during her lifetime, including is studying the genetic characterization of interrelatedness Sanaaq, the first novel written in syllabics. Among her and clonality in expanding populations of arctic willow many accomplishments, Mitiarjuk also compiled an (Salix spp.) shrubs. Jennifer Rohrs-Richey, University of Inuttitut encyclopedia of Inuit traditional knowledge, trans- Alaska Fairbanks, is investigating the combination of lated the Catholic prayer book into Inuttitut, and helped to drought stress and the canker pathogen Valsa melanodiscus develop curriculum materials for the Kativik School Board. as agents in the mortality of alders in Alaska. Linda In 1999, Mitiarjuk Nappaaluk received the National Abo- Gormezano, American Museum of Natural History, will riginal Achievement Award in the Heritage and Spiritual- be estimating the abundance, spatial distribution, and ity category, and in 2004 she was appointed to the Order of genetic structure of polar bears using passively collected Canada. hair and feces. Shelly Rayback, University of Vermont, will use dendroclimatological and stable-isotope tech- niques to reconstruct the recent past climate of an alpine Northwest Territories/Nunavut Bird Checklist Survey site at White Pass, Yukon, Canada.