DOCSLIB.ORG

ITK Map 20190118 Digital

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
ITK Map 20190118 Digital 150°W 140°W 160°W 130°W 120°W 90°W 75°N 80°N 110°W 100°W 80°W 70°W 60°W 40°W 20°W 50°W 30°W 75°N 70°N 80°N ᖁᑦᑎᓂᖅᐹᖅ ᒥᑭᓂᖅᐹᒥᒃ ᑕᕆᐅᒥ ᓯᑯᖃᕐᓂᐅᔪᖕ (2012) ᒥᕐᖑᐃᖅᓯᕐᕕᒃ Quttiniqpaaq ᐅᑭᐅᒃᑯᐃᓐᓇᖅ ᓯᑯᕙᒃᑐᖅ Mikiniqpaamik tariumi sikuqarniujuq (2012) T Mirnguiqsirvik Ukiukkuinnaq sikuvaktuq Minimum extent of sea ice (2012) ᑦ A Seasonal sea ice Quttiniqpaaq ᓈ A National Park ᐅᑭᐅᖅᑕᖅᑑᑉ ᓄ N ᐃᓄᐃᑦ ᓄᓇᖓᑦ UKIUQTAQTUUP ᑦ U D N ᐃᒪᕕᖓ ᖡ N 20°W 160°W ᖦ IT A IMAVINGA ᓛ L L Inuit Nunangat ᑲ L N ARCTIC A E A E WWW.ITK.CA OCEAN L R A ᐅᒥᖕᒪᑦ ᓄᓈᑦ ᒥᕐᖑᐃᖅᓯᕐᕕᒃ K G Umingmat Nunaat Axel Heiberg Island Mirnguiqsirvik ᑲᓇᑕᒥ ᐃᓄᐃᑦ ᓄᓇᖓᑦ ᐃᓚᖃᖅᑐᖅ ᐊᖏᕈᑕᐅᓯᒪᔪᒃᑯᑦ ᑭᒡᓕᓕᐅᖅᓯᒪᔪᑦ ᐃᓄᕕᐊᓗᐃᑦ ᓄᓇᕗᑦ, ᓄᓇᕕᒃ, ᓄᓇᑦᓯᐊᕗᑦ ᐊᒻᒪᓗ ᐃᓄᕕᐊᓗᐃᑦ ᓄᓇᖓᑦ. ᓄᓇ, ᐃᒪᖅ ᐊᒻᒪᓗ ᓯᑯ ᐃᓚᒋᔭᐅᔪᑦ ᐃᓄᐃᑦ ᓄᓇᖓᓐᓂᑦ ᐊᖏᓂᖃᖅᖢᓂᓗ 35%− ¸ Ƥ¸ºë Ellesmere ᒋᔭᖓᓂᒃ ᓄᓇ ᑲᓇᑕᓕᒫᒥᑦ ᐊᒻᒪᓗ 50%−ᒋᔭᖓᓂᒃ ᓯᒡᔭᓂᒃ ᑲᓇᑕᓕᒫᒥᑦ. 65°N ᓄᓇᖓᑦ Island Inuit Nunangat Kanatami Inuit Nunangat ilaqaqtuq angirutausimajukkut kigliliuqsimajut Nunavut, Nunavik, Nunatsiavut ammalu Inuvialuit Nunangat. Nuna, imaq ammalu siku ilagijaujut Inuit Nunangannit 70°N Inuvialuit anginiqaq&unilu 35%−gijanganik nuna Kanatalimaamit ammalu 50%−gijanganik sigjanik Kanatalimaamit. 150°W ¥º Nunangat Inuit Nunangat is the Inuit homeland in Canada, encompassing the CANADA ᐅᐊᓕᓂᐅᑉ ᑕᕆᐅᖓ autonomous land claims regions of Nunavut, Nunavik, Nunatsiavut Ualiniup Tariunga ᐊᐅᓱᐃᑦᑐᖅ and the Inuvialuit Settlement Region. It is inclusive of land, water 30°W Ausuittuq and ice, and describes an area covering 35 percent of Canada’s Grise Fiord landmass and 50 percent of its coastline. U.S.A. Beaufort ᑲᓇᑕ Inuvialuit ᖃᐅᓱᐃᑦᑐᖅ ᒥᕐᖑᐃᖅᓯᕐᕕᒃ ᐊᒥᐊᕆᑲᐅᑉ ᓄᓇᕐᔪᐊᖓᑦ ᐃᓗᓪᓕᖅ CANADA Qausuittuq Mirnguiqsirvik U Americaup Nunarjuangat Ilulliq K ᐅ Sea Qausuittuq National Park IU ᑭ Melville Island A Q ᐅ G ᖅ ᕿᑭᖅᑕᕈᒃ Settlement T ᑕᓐᒫᖅᑕᕐᕕᒃᐸᒃ ᖓ IN A ᑕ ᔨ J Q ᖅ ᐊᐅᓚᕕᒃ ᔾ J A ᑳ R T ᑑ Qikiqtaruk A C U ᑉ Tanmaaqtarvik ᑕᕆᐅᒻ ᓂᕐᔪᑕᐃᑦ ᑕᓐᒫᖅᑕᕐᕕᒃᐸᒃ ᐅᑭᐅᒃᑯᐃᓐᓇᖅ ᓯᑯᕙᒃᑐᖅ ᑉ A T U ᑑ K I P ᑳ Herschel Island- ᑕᓪᓗᕈᑎᑦ C ᔾ Ukiukkuinnaq sikuvaktuq ᖅ P E K ᔨ ᒧᓇᕆᕕᒃᓴᖓᑦ Region ᑕ U L ᖓ C A ˆ Tarium Niryutait Aulavik Tallurutit ᖅ U C IR A Qikiqtaruk Tanmaaqtarvikpak ᐅ T J Territorial Park Seasonal sea ice IR C J Munariviksangat ᑭ Q C L I ᐅ A E N ᑕ ᖃᐅᓱᐃᑦᑐᖅ Devon Island T C G T ᓪᓗᕈ I arium Niryutait ᐊᖑᓂᐊᕐᕕᐊ ᓂᕿᕐᔪᐊᒻ ᑎᐅᑉ ᑐᐱᕐᕕᒃ ᒥᕐᖑᐃᓯᕐᕕᖓ Q T A ˆ Marine Protected Aulavik ᐃᒪᖓ Qausuittuq IU C Sachs Harbour National Park Ta ᓴᓐᓂᕈᑎᐅᑉ ᐃᒪᕕᒃ K R ᑕᓐᒫᖅᑕᕐᕕᒃᐸᒃᐃᕙᕕᒃ ᐃᒪᖓᑦ ᒧᓇᕆᕕᒃᓴᖓᑦ ᐃᑳᓱᒃ lluru Resolute Bay Tupirvik Mirnguiqsirvinga ᖓ U A Tanmaaqtarvikpak Ikaahuk tiup Ima ᐃᒪ Anguniarvia Niqiqyuam ᐃᑳᕆᐊᖅ nga (Resolute) Tupirvik Territorial Park ᕈᑎᐅᑉ ga Ivvavik Parry ᑕᓪᓗ Iman SANNIRUTIUP IMAVIK Area Imangat Munariviksangat Ikaariaq Channel tiup Banks Island ᕿᑭᖅᑕᓂ Talluru BAFFIN BAY NationalIvvavik Park ᐱᖑᖅᓵᕐᔪᐃᑦ ᑲᓇᑕᒥAnguniaqvia ᓇᓗᓇᐃᑦᑯᑕᐅᔪᑦ Niqiqyuam KALAALLIT NUNAAT ᕿᑎᕐᒥᐅᑦ ᑲᓛᖦᖡᑦ ᓄᓈᑦ PinguqsaaryuitMarine Kanatami Protected Area GREENLAND Nalunaitkutauyut Qikiqtani ᓯᕐᒥᓕᒃ ᒥᕐᖑᐃᖅᓯᕐᕕᒃ Pingo Canadian Landmark Kitikmeot ᑰᒐᓇᔪᒃ Sirmilik Mirnguiqsirvik Kuuganajuk ᐃᒃᐱᐊᕐᔪᒃ CANADA Ikpiarjuk Sirmilik National Park ᑲᓇᑕ ᐃᓅᕕᒃ ᑐᒃᑑᔭᖅᑑᖅ Somerset Island ᒥᑦᑎᒪᑕᓕᒃ Inuuvik Tuktuuyaqtuuq Arctic Bay Mittimatalik ᑭᑎᒐᕐᔪᐃᑦTuktoyaktuk ᑲᓇᑕᓕᒫᒥ ᓄᓇᒋᔭᐅᔪᑐᖃᕕᓂᖅ ᑭᙵᐃᓚᒃ Admiralty Inlet Pond Inlet ᐊᒃᖤᕐᕕᒃInuvik Kangiqsuk Kitigaryuit Kanatalimaami Nunagijaujutuqaviniq ᑲᖏᖅᓱᒃ Akłarvik M Kitigaryuit National Historic Site Kinngailak Aklavik ’ ᑕᒻᒫᕐᕕᒃ ᒥᕐᖑᐃᓯᕐᕕᖓ C Q ᖃ Prince of Wales Island l i n ᐅᓪᓗᖅᓴᑑᖅ a ᒡ Tammaarvik Mirnguiqsirvinga Ulukhaqtuuq t g ᒋ o g ᐅ Tammaarvik Territorial Park c 140°W Hᐋᐱ ᕚᓕ ᓄᓇᑦᓯᐊᕐᒥ ᒥᕐᖑᐃᖅᓯᕐᕕᒃ Ulukhaktok i ᐸᐅᓚᑑᖅ k u ᔭ ᑲᖏᖅᑐᒑᐱᒃ Happy Valley Nunatsiarmit Mirnguiqsirvik ᑮᓕᓂᖅ j ᖅ Paulatuuq C a Happy Valley Territorial Park Kiiliniq h q Paulatuk ᑐᒃᑐᑦ KangiqtugaapikClyde River ᓄᕐᕋᐃᑦ Victoria Island a ᑕᓐᒫᖅᑕᕐᕕᒃᐸᒃ n QIKIQTAALUUP IKINGA 40°W n T e 65°N Tanmaaqtarvikpakuktut Nurrait l ᕿᑭᖅᑖᓘᑉ ᐃᑭᖓ ᓄᓇᕗᑦ DAVIS STRAIT Tuktut Nogait ᑲᑦᔮᖅ Katjaaq National Park ᕿᑭᖅᑕᕐᔪᐊᖅ 60°N ᕿᑭᖅᑖᓗᒃ Qikiqtaaluk Arctic Red River Nunavut Qikiqtarjuaq ᐃᒡᓗᓕᒃ ᔫ Iglulik ᑳ Baffin Island ᐊᐅᔪᐃᑦᑐᖅ Y Igloolik U ᓐ ᐅᕙᔪᒃ ᒥᕐᖑᐃᓯᕐᕕᖓ ᑕᓗᕐᔪᐊᕐᒃ ᒥᕐᖑᐃᖅᓯᕐᕕᒃ K Uvajuk Mirnguiqsirvinga Talurjuaq Auyuittuq ᐃᖃᓗᒃᑑᑦᑎᐊᖅ Ovayok Territorial Park Taloyoak Mirnguiqsirvik O Iqaluktuuttiaq ᐃᑦᑐᐊᖅᑐᕐᕕᒃ Auyuittuq Mackenzie River ᓴᓂᕋᔭᒃ N ᖁᕐᓗᖅᑐᖅ Cambridge Bay Sanirajak National Park Kuukpakᑰᒃᐸᒃ Ittuaqturvik ᐱᓱᒃᑎᓄᑦ ᑐᙵᕕᒃ ᒥᕐᖑᐃᓯᕐᕕᖓ Qurluqtuq Hall Beach Kugluktuk ᐅᖅᓱᖅᑑᖅ Gulf of Pisuktinut Tunngavik Mirnguiqsirvinga Uqsuqtuuq Boothia Pisuktinut Tunngavik Territorial Park ᖁᕐᓗᖅ ᐅᑭᐅᖅᑕᖅᑐᒥ ᒥᕐᖑᐃᓯᕐᕕᖓ ᐅᒡᔪᓕᒃ Gjoa Haven ᑰᒑᕐᔪᒃ ᐊᒥᑦᑑᑉ ᕿᑭᖅᑕᑦ ᒥᕐᖑᐃᓯᕐᕕᖓ Qurluq/Bloody Falls Mirnguiqsirvinga Ugjulik ᐸᓐᓂᖅᑑᖅ Queen Maud Gulf Kuugaarjuk ᑕᕆᐅᖓ ᓇᑦᑎᓕᒃ Qikiqtat Mirnguiqsirvinga Kugluk/Bloody Falls Territorial Park Kugaaruk Panniqtuuq ᑦ ᐊᑯᓕᐅᑉ Amittuup Nattilik Pangnirtung Kekerten Territorial Park ᓄ ᓇ ᕗ ᐃᒪᖓ Nettilling Tariunga Lake ᖃᓄᑎᒋ ᓯᑯᖃᖅᑎᒋᓂᖓ ᑕᕆᐅᒥ (2012) Akuliup Imanga Qanutigi sikuqaqtigininga tariumi (2012) T Committee Maximum extent of sea ice (2012) N U N A VᑰᓐᓄᐊᖅU Bay Kuunnuaq ᓇᐹᖅᑐᓕᒃ Hayes River Napaaqtulik ᐊᒻᒫᕐᔪᐊᖅ Napaktulik Lake Ammaarjuaq N ᓄ ᓇᐅᔮᑦ Amadjuak ᓄᓇᕗᑦ/ᓄᓇᕕᐅᓪᓗ ᓄᓇᐃᑦ Lake O ᓇ Naujaat ᓯᑯᓰᓚᖅ R N ᑦᓯ ᓇᖕᒥᓂᖃᖃᑎᒌᖕᓂᖃᕐᕕᒋᔭᖏᑦ T U ᐊ Sikusiilaq ᐃᖃᓗᐃᑦ H ᖅ Nunavut/Nunaviullu nunait IQALUIT N ᕿᑎ ᐅᒃᑯᓯᒃᓴᓕᒃ Foxe Peninsula W A ᕐᒥᐅ nangminiqaqatigiingniqarvigijangit ᖃᐅᒻᒫᕐᕖᑦ ᐅᑭᐅᖅᑕᖅᑐᒥ ᒥᕐᖑᐃᓯᕐᕕᖓ T ᑭᕙ ᑦ ᒥᕐᖑᐃᖅᓯᕐᕕᒃ E S ᓪᓕ Qaummaarviit Ukiuqtaqtumi S I ᖅ Kitikmeo Ukkusiksalik Mirnguiqsirvik Nunavut/Nunavik ᓯᐅᕕᐊ ᒍᕆᓂᐅᓪ ᒥᕐᖑᐃᓯᕐᕕᖓ T A t ᒪᓪᓕᒃᔪᐊᖅ ᒥᕐᖑᐃᓯᕐᕕᖓ Mirnguiqsirvinga Q Kivalliq Ukkusiksalik jointly owned lands Sylvia Grinnell Mirnguiqsirvinga T Qaummaarviit E National Park Mallikjuaq Mirnguiqsirvinga Sylvia Grinnell Territorial Park ᐋᑦᓛᓐᑎᒃ ᐃᒪᖓ R ᐅᖓᓪᓕᖅᐹᖅ ᐊᑯᓪᓕᖅᐹᖅ Mallikjuaq Territorialᑭᙵᐃᑦ Park Territorial Park R ᓴᓪᓕᖅ Kinngait ᓄᓇᕕᐅᑉ ᐊᕕᒃᑐᖅᓯᒪᓂᖓᓂ I ᖃᒪᓂᖅ ᖃᒪᓂᖅ ᕿᑭᖅᑕᓂ ᑲᑕᓐᓂᓕᒃ ᒥᕐᖑᐃᖅᓯᕐᕕᒃ T Salliq ᑭᕙᓪᓕᖅ Cape Dorset ᑭᒻᒥᕈᑦ 60°N O Ungalliqpaaq Akulliqpaaq Katannilik Mirnguiqsirvik Kimmirut ᑕᕆᐅᖅ ATLANTIC OCEAN R qamaniq IE qamaniq ᐃᓅᔮᕐᕕᒃ ᒥᕐᖑᐃᓯᕐᕕᖓ Southampton Island Katannilik Territorial Park Nunaviup Aviktuqsimaningani Tariuq S ᐃᑭ ᖃᒪᓂ’ᑐᐊᖅ Inuujaarvik Mirnguiqsirvinga ᓴᓪᓕᖅ Ik ᕋᓴᕐ Nunavik Marine Region Aberdeen Lake Salliq ira ᔪᐊᖅ ᑲᖏᕐᔪᐊᖅ Qamani'tuaq Inuujaarvik Territorial Park ᑕᖃᐃᖅᓯᕐᕕᒃ ᒥᕐᖑᐃᓯᕐᕕᖓ sa 130°W Hu rj Qikiqtani d ua ᓛᐸᑐᐊᕆᑉ ᐃᒫᑉᐱᖓ Kangirjuaq Baker Lake ᖃᒪᓂ'ᑐᐊᖅ Coral Harbour son q LÂBRADORIP IMAPPINGA Kivalliq Thelon River Qamani’tuaq Taqaiqsirvik Mirnguiqsirvinga Stra ᑐᖓᐃᑦ ᖃᖅᑲᓱᐊᖏᓐᓂ Taqaiqsirvik Territorial Park it 50°W Baker Lake ᐃᒡᓗᓕᒑᕐᔪᒃ ᓯᓚᖅᑭᔭᑉᕕᖓ Igluligaarjuk ᑲᖏᕐᓱᔪᐊᖅ ᖁᐊᕐᑕᖅ Tungait KakKasuanginni Labrador Sea Chesterfield Inlet Kangiqsujuaq kanatami SilakKijapvinga ᑐᓕᒫᓗᒡᔪᐊᖅ ᓴᓪᓗᐃᑦ Quaqtaq ᐃᖃᓗᒑᕐᔫᑉ ᓄᓇᖓ Tulimaalugjuaq ᐃᕗᔨᕕᒃ Salluit ᕙ y Torngat Mountains 55°N ᒥᕐᖑᐃᖅᓯᕐᕕᒃ ᕐᑲᖏᖅᖠᓂᖅ Ivujivik ᖓ Ba National Park Dubawnt ᐅ a Lake Iqalugaarjuup Nunanga Mirnguiqsirvik Kangiq&iniq av Rankin Inlet ng Iqalugaarjuup Nunanga U ᑰᕈᕐᔪᐊᖅ Territorial Park ᐱᖑᐊᓗᐃᑦ Kuururjuaq ᑲᖏᕐᓱᒃ Pingualuit Kangiqsuk ᓄᓇᑦᓯᐊᕗᑦ ᑎᑭᕋᕐᔪᐊᖅ Kuururjuaq(Québec) Nat. Park ᐳ Tikirarjuaq Pingualiut(Québec) National Park ᕆ ᖃᒪᓂᖅ ᐅᖓᓪᓕᖅ Whale Cove ᐊᐅᐸᓗᒃ ᑎ Qamaniq Ungalliq ᐊᑯᓕᕕᒃ Aupaluk Nunatsiavut ᑲ Kamanik Lake ᓄᓇᕕᐅᑉ ᐊᕕᒃᑐᖅᓯᒪᓂᖓᓂ ᑕᕆᐅᖅ Akulivik ᑲᖕᒋᕐᓱᐊᓗᑦᔪᐊᖅ ᓚ ᔅ ᓴᕐᕙᖅᑑᖅ Kazan River Kangiqsualujjuaq Harvaqtuuq Nunaviup Aviktuqsimaningani Tariuq ᒻᐱ ᐳᕕᕐᓂᑐᖅ ᓄᓇᐃᖑᒃ ᐊ Nunavik Marine Region Puvirnituq Nunainguk B ᐊᕐᕕᐊᑦ ᑕᓯᐅᔭᖅ ᐅᓕᑦᑕᓂᐅᔭᓕᒃ Nain R Arviat Tasiujaq Ulittaniujalik ᑰᑦᔪᐊᖅ ᐊᑉᕕᑑᒃ I ᕿᑭᖅᑕᕆᐊᒃᑐᖅ Apvitok ᒪᖅᑰᕕᒃ T Qikiqtariaktuq Kuujjuaq Ulittaniujalik(Québec) Nat. Park C I Hopedale MaKovik ᑭᑭᐊᒃ O S Nueltin Lake Makkovik kikiak L H ᐅᑭᐅᒃᑯᐃᓐᓇᖅ ᓯᑯᕙᒃᑐᖅ ᓄᓇᕕᒃ Rigolet U Ukiukkuinnaq sikuvaktuq ᕿᐳᖅᑲᒃ M Seasonal sea ice KipukKak B Postville I Nunavik ᒦᓕ ᖃᖅᑲᓱᐊᖏᓐᓂ ᑲᓇᑕᒥ A ᐃᓄᒃᔪᐊᒃ ᓯᓚᖅᑭᔭᑉᕕᖓ ᐋ Inukjuak Meli KakKasuanginni kanatami ᓪ SilakKijapvinga 55°N A ᐴ ᑕᓯᐅᔭᕐᔪᐊᖅ Mealy Mountains National Park L ᑕ N ᓂᐅᕙᓐ B E TASIUJARJUAQ EW ᓛᓐ ᓛᐸᑐ R FOU ᐊ T A HUDSON BAY NDLAN ᑐᕐᓱᔪᕐᒃ D and LAB Tursujuq RA ᐅᒥᐅᔭᖅ DO ᑕ Umiujaq ᑲ ᓇ Tursujuq National R ᓇᓗᓇᐃᔭᐅᑎᖏᑦ/NALUNAIJAUTINGIT/LEGEND ᓄᓇᕗᑦ/ᓄᓇᕕᐅᓪᓗ ᓄᓇᐃᑦ ᓴᓂᑭᓗᐊᖅ Park (Québec) ᓴ ᓇᖕᒥᓂᖃᖃᑎᒌᖕᓂᖃᕐᕕᒋᔭᖏᑦ ᐃᓄᒋᐊᒃᑑᓂᖓ/Inugiaktuuninga ᔅᑳ Sanikiluaq ᓯᓚᕐᔪᐊᓕᒫᒥ ᑭᒡᓕᖃᕐᓂᕆᔭᐅᔪᑦ ᑦᑐ Nunavut/Nunaviullu nunait Population ᐊᓐ 50°N Silarjualimaami kigliqarnirijaujut S A nangminiqaqatigiingniqarvigijangit Nunavut 0–500 ᐃᒡᓗᓕᒑᕐᔪᒃ/Chesterfield Inlet International boundaries AS C KAT A N A D Nunavut/Nunavik 500–2,500 ᑲᖏᖅᖠᓂᖅ/ Rankin Inlet CHE jointly owned lands ᐊᕕᒃᑐᖅᓯᒪᓂᐅᔪᑦ/ᐳᕌᕕᓐᓯᐅᔪᑦ ᑭᒡᓕᒋᔭᖏᑦ WAN ᑰᑦᔪᐊᕌᐱᒃ 2,500–25,000 ᐃᓅᕕᒃ/Inuvik Aviktuqsimaniujut/Province-siujut Kigligijangit ᒫ Kuujjuaraapik Territorial/Provincial boundaries ᓂ ᑑ ᐸ ᒃ ᓄᓇᓕᐸᐅᔭᕆᔭᐅᔪᑦ ᐃᖃᓗᐃᑦ/IQALUIT ᐃ Nunalipaujagijaujut ᖃᖓᑕᓲᒃᑯᕝᕖᑦ ᑎᑭᑕᐅᒐᔪᑦᑐᑦ ᐸ Capitals M A ᑯ C Qangatasuukkuvviit Tikitaugajuttut N I T O B A B E Airports with regularly scheduled service U É ᓄᓇᐅᑉ ᖃᓄᐃᑦᑑᓂᖓ/Nunaup qanuittuuninga/Landcover Q ᓇᐹᖅᑐᖃᑦᓯᐊᖏᓐᓂᖅ/Napaaqtuqatsianginniq/Minimal vegetation ᖃᓄᑎᒋ ᓯᑯᖃᖅᑎᒋᓂᖓ ᑕᕆᐅᒥ (2012) ᓯ~ᓯᐱ ᐱᕈᖅᑐᖃᑦᓯᐊᖏᓐᓂᖅ−ᐃᕕᒃ/Piruqtuqatsianginniq−ivik/Low vegetation−grass ᔭᐃᒥᓯ ᐸᐃ Chisasibi Qanutigi sikuqaqtigininga tariumi (2012) Maximum extent of sea ice (2012) ᐱᕈᖅᑐᖃᑦᓯᐊᖏᓐᓂᖅ−ᐊᕚᓚᕿᐊᑦ/Piruqtuqatsianginniq−avaalaqiat/Low vegetation−shrub James Bay ᓇᐹᖅᑐᖃᕐᓂᖅ/Napaaqtuqarniq/Forest ᐃᕕᑑᖅ ᐊᒻᒪᓗ ᓇᐹᖅᑐᖃᑦᓯᐊᖏᓐᓂᖅ/Ivituuq ammalu napaaqtuqatsianginniq/Grassland and parkland ᑭᓚᒥᑕ 0 100 200 300 400 500 km ᐅ ᕆ ᐅ ᐃᓄᕕᐊᓗᐃᑦ ᑎᒥᖁᑎᖓ Inuvialuit Settlement Region Inuvialuit Regional Corporation www.irc.inuvialuit.com ᐋ ᓐ ᑎ ᓄᓇᕗᑦ ᑐᙵᕕᒃ Nunavut Nunavut Tunngavik Incorporated www.tunngavik.com ᐃᓕᑕᕆᓯᒪᓪᓗᒋᑦ/ILITARISIMALLUGIT/CREDITS 60°W ᐊᖏᑎᒋᓂᖓ/SCALE 1: 5,500,000 I O ᐱᕝᕕᐅᔪᑦ/Pivviujut/Sources: Base map: Natural Earth; Communities: Atlas of Canada, Natural ᒪᑭᕝᕕᒃ Nunavik Makivik Corporation www.makivik.org A R 70°W Resources Canada. Parks: Renewable Resources, Kativik Regional Government; Parks and Special ᑕᑯᒃᓴᐅᑎᑕᐅᓂᖓ: ᓛᒻᐳᕐᑦ ᓄᓇᕐᔪᐊᑉ ᑕᐅᑦᑐᖓᑎᒍᑦ ᑕᑯᒃᓴᐅᑎᑦᑎᓂᖓ; ᐊᑭᓕᕇᓕᖅᓯᒪᑎᑕᐅᓪᓗᑎᒃ 49°N ᐊᒻᒪᓗ 77°N ᓄᓇᑦᓯᐊᕗᑦ ᒐᕙᒪᖓᑦ Nunatsiavut Nunatsiavut Government www.nunatsiavut.com O N T Places, Dept. of Environment., Nunavut; Park Canada; Settlement Areas: Makivik Corp.; Nunavut Projection: Lambert Conformal Conic; principal parallels, 49°N and 77°N ᐃᓄᐃᑦ ᑕᐱᕇᑦ ᑲᓇᑕᒥ Inuit Nunangat Inuit Tapiriit Kanatami www.itk.ca © Inuit Tapiriit Kanatami 2018 Tunngavik Inc.; Inuvialuit Regional Corp.; Dept. of Land and Natural Resources, Nunatsiavut. : Steven Fick <www.fick.ca>, Signy Fridriksson ISBN 978-1-989179-22-2 ᓄᓇᖖᒍᐊᓕᐅᕈᓰᑦ/Nunangualiurusiit/Cartography 90°W 80°W 110°W 100°W.
Load more

Recommended publications
  • H a Guide to Sport Fishing in Nunavut
    h a guide to sport fishing in nunavut SPORT FISHING GUIDE / NUNAVUT TOURISM / NUNAVUTTOURISM.COM / 1.866.NUNAVUT 1 PLUMMER’S ARCTIC LODGES PLUMMER’S Fly into an untouched, unspoiled landscape for the adventure of a lifetime. Fish for record-size lake trout and pike in the treeless but colourful barrenlands. Try for arctic grayling in our cold clear waters. And, of course, set your sights on an arctic char on the Tree River, the Coppermine River, or dozens of other rivers across Nunavut that flow to the Arctic seas. Spend a full 24 hours angling for the species of your choice under the rays of the midnight sun. PLUMMER’S ARCTIC LODGES PLUMMER’S Pristine, teeming with trophy fish, rare wildlife and Read on to explore more about this remarkable place: nature at its rawest, Nunavut is a cut above any ordinary about the Inuit and their 1000-year history of fishing in sport fishing destination. Brave the stark but stunning one of the toughest climates in the world; about the wilderness of the region. Rise to the unique challenges experienced guides and outfitters ready to make your of Nunavut. And come back with jaw-dropping trophy- adventure run smoothly. Read on to discover your next sized catches, as well as memories and stories that great sport fishing experience! you’ll never tire of. Welcome To Sport Fishing Paradise. 2 SPORT FISHING GUIDE / NUNAVUT TOURISM / NUNAVUTTOURISM.COM / 1.866.NUNAVUT PLUMMER’S ARCTIC LODGES PRIZE OF THE ARCTIC Arctic Char The arctic char is on every sport fisher’s bucket list.
    [Show full text]
  • Modelling Population Mobility in Southern Baffin Island's Past
    MODELLING POPULATION MOBILITY IN SOUTHERN BAFFIN ISLAND’S PAST USING GIS AND LANDSCAPE ARCHAEOLOGY by Jeffrey Phillip Stup A Thesis submitted to the Faculty of Graduate Studies of The University of Manitoba in partial fulfillment of the requirements of the degree of MASTER OF ARTS Department of Anthropology University of Manitoba Winnipeg, Manitoba Copyright © 2015 by Jeffrey Phillip Stup Abstract Evidence of chert stone tools on southern Baffin Island of Canada dates back thousands of years, yet most of these materials are found far from coastal areas of use. In the central interior lakes region of Baffin Island, chert can be found but this area is extremely remote and hard to access. If past human populations moved inland from the coast to acquire chert toolstone and pursue seasonally specific subsistence-related activities, many archaeological sites should exist between these respective locales. Historically, it has been difficult to locate such intermediate sites given the expansive of the landscape and the logistical challenges of surveying it. In this study, free and open-source geospatial data were used in geographic information systems (GIS) to predict archaeological site formation and potential inland travel routes. The models created link the archaeologically dense coastal and inland regions. These were constructed with a landscape archaeology theoretical approach and validated by comparisons to Inuit ethnographic accounts of interior-bound pathways. A new archaeological-GIS method was created, using a flood allocation function on a ‘humanistic’ cost surface. This ‘mobility-shed’ method generates vast networks of areas most conducive to human movement, aids in solving problems about past human population movements for Baffin Island history, for an ongoing chert provenance study, and will lead to future research through ground-truthing and more in-depth geospatial studies.
    [Show full text]
  • Mining for Power: Uranium Mining in Baker Lake Nunavut
    Mining for Power: Uranium and the Community of Baker Lake, Nunavut Elaine Wang, University of Vermont (prepared for ENVS 295, Dr. Saleem H. Ali) December 2006 Three representations of the Kivalliq District, Nunavut Clockwise from upper left: project map released to the media by Titan Uranium; satellite image from Google Maps; caribou ranges mapped by Beverly-Qamanirjuaq Caribou Management Board “The Kiggavik Project near Baker Lake never went ahead. It is possible that, because of changing market conditions and the superior ore grades in neighboring Saskatchewan, 1989-90 had provided a window of opportunity for its development that was never to be repeated.” -Robert McPherson 2003, New Owners in the Own Land adapted from Cameco Corporation, 2006; not constant dollars Introduction In a plebiscite held on March 26, 1990, residents of the hamlet of Baker Lake (in what was then the District of Keewatin, Northwest Territories, now the District of Kivalliq, Nunavut, Canada), voted overwhelmingly against the development of a uranium mine by Urangesellschaft Canada Ltd. (UG) at a nearby site called Kiggavik, part of what prospectors know as the Thelon Basin. As a result, UG never explored its claims. In August of the same year, Bob Leonard, the president of the Keewatin Chamber of Commerce stated, “We are in an economic crisis. The economy in the Keewatin is in a mess. We are totally dependent on government spending and there’s no way that can continue.”1 The opening quote by Robert McPherson, a mining consultant in the Nunavut land claims negotiations, suggests that as recently as 2003, uranium mining near Baker Lake was, for many reasons, considered a non-option.
    [Show full text]
  • Taltheilei Houses, Lithics, and Mobility
    University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2012-09-06 Taltheilei houses, lithics, and mobility Pickering, Sean Joseph Pickering, S. J. (2012). Taltheilei houses, lithics, and mobility (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/27975 http://hdl.handle.net/11023/177 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Taltheilei Houses, Lithics, and Mobility by Sean J. Pickering A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS DEPARTMENT OF ARCHAEOLOGY CALGARY, ALBERTA SEPTEMBER, 2012 © Sean J. Pickering 2012 Abstract The precontact subsistence-settlement strategy of Taltheilei tradition groups has been interpreted by past researchers as representing a high residential mobility forager system characterized by ephemeral warm season use of the Barrenlands environment, while hunting barrenground caribou. However, the excavation of four semi-subterranean house pits at the Ikirahak site (JjKs-7), in the Southern Kivalliq District of Nunavut, has challenged these assumptions. An analysis of the domestic architecture, as well as the morphological and spatial attributes of the excavated lithic artifacts, has shown that some Taltheilei groups inhabited the Barrenlands environment during the cold season for extended periods of time likely subsisting on stored resources.
    [Show full text]
  • Bathurst Fact Sheet
    Qausuittuq National Park Update on the national park proposal on Bathurst Island November 2012 Parks Canada, the Qikiqtani Inuit Association (QIA) and the community of Resolute Bay are working together to create a new national park on Bathurst Island, Nunavut. The purpose of the park is to protect an area within the The park will be managed in co-operation with Inuit for Western High Arctic natural region of the national park the benefit, education and enjoyment of all Canadians. system, to conserve wildlife and habitat, especially areas It is expected that the park’s establishment will enhance important to Peary caribou, and enable visitors to learn and support local employment and business as well as about the area and its importance to Inuit. help strengthen the local and regional economies. Qausuittuq National Park and neighbouring Polar Bear Within the park, Inuit will continue to exercise their Pass National Wildlife Area will together ensure protec - right to subsistence harvesting. tion of most of the northern half of Bathurst Island as well as protection of a number of smaller nearby islands. Bringing you Canada’s natural and historic treasures Did you know? After a local contest, the name of the proposed national park was selected as Qausuittuq National Park. Qausuittuq means “place where the sun does - n't rise” in Inuktitut, in reference to the fact that the sun stays below the horizon for several months in the winter at this latitude. What’s happening? Parks Canada and Qikiqtani Inuit Association (QIA) are working towards completion and rati - fication of an Inuit Impact and Benefit Agree - ment (IIBA).
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • Geophysical and Geological Integration and Interpretation of the Northeast Thelon Basin, Nunavut
    GEOPHYSICAL INTERPRETATION OF THE NORTHEAST THELON BASIN GEOPHYSICAL AND GEOLOGICAL INTEGRATION AND INTERPRETATION OF THE NORTHEAST THELON BASIN, NUNAVUT By VICTORIA LYNN TSCHIRHART, B.Sc. A Thesis Submitted to the School of Graduate Studies in Partial Fulfillment of the Requirements for the Degree of Doctorate of Philosophy McMaster University © Copyright for Victoria Tschirhart, November 2013 i McMaster University DOCTORATE OF PHILOSPHY (2013) Hamilton, Ontario TITLE: Geophysical and geological integration and interpretation of the northeast Thelon Basin, Nunavut AUTHOR: Victoria Lynn Tschirhart, B.Sc. (McMaster University) SUPERVISOR: Dr. William A. Morris NUMBER OF PAGES: xii, 196 ii Abstract The northeast Thelon Basin, Nunavut, is a rapidly developing albeit poorly studied, frontier exploration domain for unconformity-associated uranium deposits. Critical criteria for unconformity –associated uranium deposit models are knowledge of the basement geology, fault history and depth to unconformity surface. This thesis sets forth to derive working geological and geophysical models for the northeast Thelon Basin through the implementation of integrated geophysical techniques. A physical rock property database is compiled defining average density and susceptibility values for key map units for integration into subsequent modelling iterations. Forward and inverse potential field modelling using these petrophysical with geological controls define the structure and geometry of the Shultz Lake intrusive complex and northeast Amer Belt, both of which are present below the Thelon sedimentary cover. Implementation of a new source edge detection technique estimates fault development and location within the basin. This provides a quantitative analysis of fault timing, identifying potentially reactivated faults which have an increased likelihood to serve as conduits to transport uranium-rich fluids and focus deposition.
    [Show full text]
  • Wolverine Ecology, Distribution, and Productivity in the Slave Geological Province
    WEST KITIKMEOT / SLAVE STUDY SOCIETY Re: Wolverine Ecology, Distribution and Productivity in a Tundra Environment Final Report STUDY DIRECTOR RELEASE FORM The above publication is the result of a project conducted under the West Kitikmeot / Slave Study. I have reviewed the report and advise that it has fulfilled the requirements of the approved proposal and can be subjected to independent expert review and be considered for release for public. March 14, 2001 Study Director Date INDEPENDENT EXPERT REVIEW FORM I have reviewed this publication for scientific content and scientific practices and find the report is acceptable given the specific purposes of this project and subject to the field conditions encountered. April 12, 2001 Reviewer Date INDEPENDENT EXPERT REVIEW FORM I have reviewed this publication for scientific content and scientific practices and find the report is acceptable given the specific purposes of this project and subject to the field conditions encountered. April 26, 2001 Reviewer Date BOARD RELEASE FORM The Study Board is satisfied that this final report has been reviewed for scientific content and approves it for release to the public. June 6, 2001 Chair Date West Kitikmeot/Slave Study Society Wolverine Ecology, Distribution, and Productivity in the Slave Geological Province Final Report to the West Kitikmeot / Slave Study Society Submitted by Robert Mulders Department of Resources, Wildlife and Economic Development Government of the Northwest Territories #600, 5102-50 Avenue, Yellowknife, NT, X1A 3S8 30 June, 2000 SUMMARY There are limited data available on the distribution, abundance, and ecology of wolverine (Gulo gulo) in the Northwest Territories and Nunavut. It’s believed that the current wolverine population on the central barrens is relatively healthy and serves as a refugia which supports the harvest of wolverines in adjacent areas.
    [Show full text]
  • ARCTIC CHANGE 2014 8-12 December - Shaw Centre - Ottawa, Canada
    ARCTIC CHANGE 2014 8-12 December - Shaw Centre - Ottawa, Canada Oral Presentation Abstracts Arctic Change 2014 Oral Presentation Abstracts ORAL PRESENTATION ABSTRACTS TEMPORAL TREND ASSESSMENT OF CIRCULATING conducted when possible. Results: Maternal levels of Hg and MERCURY AND PCB 153 CONCENTRATIONS AMONG PCB 153 significantly decreased between 1992 and 2013. NUNAVIMMIUT PREGNANT WOMEN (1992-2013) Overall, concentrations of Hg and PCB 153 among pregnant women decreased respectively by 57% and 77% over the last Adamou, Therese Yero (12) ([email protected]), M. Riva (12), E. Dewailly (12), S. Dery (3), G. Muckle (12), R. two decades. In 2013, concentrations of Hg and PCB 153 were Dallaire (12), EA. Laouan Sidi (1) and P. Ayotte (1,2,4) respectively 5.2 µg/L and 40.36 µg/kg plasma lipids (geometric means). Discussion: Our results suggest a significant decrease (1) Axe santé des populations et pratiques optimales en santé, of Hg and PCB 153 maternal levels from 1992 to 2013. Centre de Recherche du Centre Hospitalier Universitaire de Geometric mean concentrations of Hg and PCB 153 measured Québec, Québec,Québec, G1V 2M2 in 2013 were below Health Canada guidelines. The decline (2) Université Laval, Québec, Québec, G1V 0A6 observed could be related to measures implemented at regional, (3) Nunavik Regional Board of Health and Social Services, Kuujjuaq, Québec national and international levels to reduce environmental (4) Institut National de Santé Publique du Québec (INSPQ), pollution by mercury and PCB and/or a significant decrease Québec, G1V 5B3 of seafood consumption by pregnant women. These results have to be interpreted with caution.
    [Show full text]
  • Annual Report and Investigators' Summaries 1956
    CONFIDENT IAL FISHERIES RESEARCH BOARD OF CANADA ARCTIC UNIT Montreal, Que. Annual Report and Investigators' Summaries 195.6 H. D. Fisher, In Charge CONFIDENTIAL FISHERIES RESEARCH BOARD OF CANADA ARCTIC UNIT Montreal, Que. Annual Report and Investigators Summaries 19 56 H. D. Fisher, In Charge REPORT FOR 1956-57 OF THE ARCTIC UNIT, MONTREAL, QUE, by H. D. Fisher, Scientist in Charge The primary objectives of the Arctic Unit are to assess the marine resources of the arctic regions in the light of present utilization, and to carry out detailed biological studies on species of special importance either directly to the living economy or to the general productivity of the region. Marine mammal studies are extended south on the Atlantic side to include whaling and sealing problems in the Maritimes and Newfoundland area. Late in the year, re- sponsibilities for liaison with the Department of Fisheries regarding seal control on the east coast was transferred to the Unit from the St. Andrews Station. Liaison is maintained with the Department of Northern Affairs and National Resources regarding investi- gations touching on the role of marine resources in the human living economy. The dependence of many native groups on non- marine wildlife, as well as on marine animals, calls for occasional joint planning with that Department, which is responsible for such wildlife through the Canadian Wildlife Service. Liaison is maintained also with the Atlantic Oceanographic Group at St. Andrews, so that hydrographie work carried out by the Unit can fit as closely as possible into their arctic program. In addition, collection of biological material from arctic cruises of H.M.C.S.
    [Show full text]
  • Evaluation of Techniques for Flood Quantile Estimation in Canada
    Evaluation of Techniques for Flood Quantile Estimation in Canada by Shabnam Mostofi Zadeh A thesis presented to the University of Waterloo in fulfillment of the thesis requirement for the degree of Doctor of Philosophy in Civil Engineering Waterloo, Ontario, Canada, 2019 ©Shabnam Mostofi Zadeh 2019 Examining Committee Membership The following are the members who served on the Examining Committee for this thesis. The decision of the Examining Committee is by majority vote. External Examiner Veronica Webster Associate Professor Supervisor Donald H. Burn Professor Internal Member William K. Annable Associate Professor Internal Member Liping Fu Professor Internal-External Member Kumaraswamy Ponnambalam Professor ii Author’s Declaration This thesis consists of material all of which I authored or co-authored: see Statement of Contributions included in the thesis. This is a true copy of the thesis, including any required final revisions, as accepted by my examiners. I understand that my thesis may be made electronically available to the public. iii Statement of Contributions Chapter 2 was produced by Shabnam Mostofi Zadeh in collaboration with Donald Burn. Shabnam Mostofi Zadeh conceived of the presented idea, developed the models, carried out the experiments, and performed the computations under the supervision of Donald Burn. Donald Burn contributed to the interpretation of the results and provided input on the written manuscript. Chapter 3 was completed in collaboration with Martin Durocher, Postdoctoral Fellow of the Department of Civil and Environmental Engineering, University of Waterloo, Donald Burn of the Department of Civil and Environmental Engineering, University of Waterloo, and Fahim Ashkar, of University of Moncton. The original ideas in this work were jointly conceived by the group.
    [Show full text]