Whale Cove, Nunavut
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Whale Cove, Nunavut
Whale Cove (ᑎᑭᕋᕐᔪᐊᖅ in Inuktitut syllabics) (''Tikiraqjuaq'', meaning "long point"), is a hamlet located south southwest of Rankin Inlet, northeast of Arviat, in Kivalliq Region, Nunavut, Canada, on the western shore of Hudson Bay. The community is named for the many beluga whales which congregate off the coast. Many of the inhabitants hunt these whales every fall and use their by-products for their oil and food. Whale Cove, initially settled by three distinct Inuit groups (one inland and two coastal), is a relatively traditional community: 99% Inuit, who still wear fur, hunt, fish, eat raw meat and fish. Several bowhead whales may appear in the area as well. Whale Cove is on the polar bear migration route. Local Inuit regularly travel by snowmobile in the winter or by boat in summer months between the hamlet of Rankin Inlet and Whale Cove, a distance of . The terrain is Arctic tundra, this consists mostly of rocks, mosses and lichens. History Inuit in the Whale ...
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Provinces And Territories Of Canada
Within the geographical areas of Canada, the ten provinces and three territories are sub-national administrative divisions under the jurisdiction of the Canadian Constitution. In the 1867 Canadian Confederation, three provinces of British North America—New Brunswick, Nova Scotia, and the Province of Canada (which upon Confederation was divided into Ontario and Quebec)—united to form a federation, becoming a fully independent country over the next century. Over its history, Canada's international borders have changed several times as it has added territories and provinces, making it the world's second-largest country by area. The major difference between a Canadian province and a territory is that provinces receive their power and authority from the ''Constitution Act, 1867'' (formerly called the ''British North America Act, 1867''), whereas territorial governments are creatures of statute with powers delegated to them by the Parliament of Canada. The powers flowing from t ...
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Beluga Whale
The beluga whale () (''Delphinapterus leucas'') is an Arctic and sub-Arctic cetacean. It is one of two members of the family Monodontidae, along with the narwhal, and the only member of the genus ''Delphinapterus''. It is also known as the white whale, as it is the only cetacean to regularly occur with this colour; the sea canary, due to its high-pitched calls; and the melonhead, though that more commonly refers to the melon-headed whale, which is an oceanic dolphin. The beluga is adapted to life in the Arctic, with anatomical and physiological characteristics that differentiate it from other cetaceans. Amongst these are its all-white colour and the absence of a dorsal fin, which allows it to swim under ice with ease. It possesses a distinctive protuberance at the front of its head which houses an animal echolocation, echolocation organ called the Melon (whale), melon, which in this species is large and deformable. The beluga's body size is between that of a dolphin and a true ...
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Ihalmiut
The Ahiarmiut ᐃᓴᓪᒥᐅᑦ or Ihalmiut ("People from Beyond") or ("the Out-of-the-Way Dwellers") are a group of inland Inuit who lived along the banks of the Kazan River, Ennadai Lake, and Little Dubawnt Lake (renamed ''Kamilikuak''), as well as north of Thlewiaza River ("Big River"), in northern Canada's Keewatin Region of the Northwest Territories, now the Kivalliq Region ("Barren Lands") of present-day Nunavut. Through three decades of research by David Serkoak, an Ahiarmiut elder, who was a child when his family was repeatedly relocated from Ennadai Lake by the federal government under then-prime ministers, Louis St. Laurent and John Diefenbaker, the story of the Ahiarmiut and their search for justice has been shared. For ten years, starting in 1949, as part of a northern policy regarding Inuit communities, the Ahiarmiut were relocated to Nueltin Lake, then Henik Lake, and Whale Cove, among other places. In 2018, the Ahiarmiut and the Canadian government came to a ...
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Caribou Inuit
Caribou Inuit ( iu, Kivallirmiut/ᑭᕙᓪᓕᕐᒥᐅᑦ), barren-ground caribou hunters, are Inuit who live west of Hudson Bay in Kivalliq Region, Nunavut, between 61° and 65° N and 90° and 102° W in Northern Canada. They were originally named "Caribou Eskimo" by the Danish Fifth Thule Expedition of 19211924 led by Knud Rasmussen. Caribou Inuit are the southernmost subgroup of the Central Inuit. Groups ;Ahialmiut Ahialmiut relied on caribou year-round. They spent summers on the Qamanirjuaq calving grounds at Qamanirjuaq Lake ("huge lake adjoining a river at both ends") and spent winters following the herd to the north. ;Akilinirmiut Akilinirmiut were located in the Thelon River area by the Akiliniq Hills (''A-ki'', meaning "the other side") to the north of Beverly Lake and also visible above Aberdeen Lake. Some lived northwest of Baker Lake (''Qamani'tuuaq''), along with Qairnirmiut and Hauniqturmiut. Many relocated to Aberdeen Lake because of starvation or education o ...
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Baker Lake, Nunavut
Baker Lake (Inuktitut syllabics: ᖃᒪᓂᑦᑐᐊᖅ 'big lake joined by a river at both ends', Inuktitut: ''Qamani'tuaq'' 'where the river widens') is a hamlet in the Kivalliq Region, in Nunavut on mainland Canada. Located inland from Hudson Bay, it is near the nation's geographical centre, and is notable for being Nunavut's sole inland community. The hamlet is located at the mouth of the Thelon River on the shore of Baker Lake. The community was given its English name in 1761 from Captain William Christopher who named it after Sir William Baker, the 11th Governor of the Hudson's Bay Company. History In 1916, the Hudson's Bay Company established a trading post at Baker Lake, followed by Anglican missionaries in 1927. The Royal Canadian Mounted Police had been in the area for fifteen years before establishing a post at Baker Lake in 1930. In 1946 the population was 32, of which 25 were Inuit. A small hospital was built in 1957, followed by a regional school the next year. ...
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Garry Lake
Garry Lake (variant: Garry Lakes; Inuktitut: , meaning "sideways", or "crooked") is a lake in sub-Arctic Kivalliq Region, Nunavut, Canada. As a portion of the Back River waterway, Garry Lake originates directly east of Lake Pelly and drains to the east by the Back River. A set of rapids separate Buliard Lake (directly to the north) from Garry Lake. Two other sets of rapids separate Garry Lake's three sections (Upper Garry Lake, Garry Lake, Lower Garry Lake) which are also differentiated by elevation. Garry Lakes are isolated from nearby communities. Geography Garry Lakes are a part of the Churchill craton—Rae craton geological province. It is a low relief area including sedge/grass meadows along lake shores, and substrates of glacial silts, sands, and gravels. Fauna As moulting Canada geese arrive in late summer, the Canadian Wildlife Service designated the area as a Key Migratory Bird Terrestrial Habitat site. Ethnography ''Hanningajuq'' is the Inuktitut word for both Gar ...
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Back River (Nunavut)
The Back River, formerly Back's River ( Dogrib: ''Thlewechodyeth'', Inuktitut: ''Haningayok'', or Great Fish River), is the 20th longest Canadian river and is located in the Northwest Territories and Nunavut. It rises at an unnamed lake in the North Slave Region of the Northwest Territories and flows more than mostly through the Kivalliq Region, Nunavut, to its mouth at the Arctic Ocean in the Kitikmeot Region of Nunavut. Course The river begins at the outflow of an unnamed lake at an elevation of and flows west into Sussex Lake, then north to Muskox Lake, at the border between the Northwest Territories and the Kivalliq Region, Nunavut, where it takes in the left tributary Icy River. It flows over the Muskox Rapids, takes in the left tributary Contwoyto River, and heads east through the Heywood Range. The Back River heads over the Malley Rapids, takes in the left tributary Siorak River and enters the long lake-expansion Lake Beechey in a southeast direction. It heads east ...
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Ennadai Lake
Ennadai Lake is a lake in the Kivalliq Region, Nunavut, Canada. It is long, and wide. It is drained to the north by the Kazan River. A section of the Kazan River from the outlet of Ennadai Lake to Baker Lake, was designated as a part of the Canadian Heritage Rivers System in 1990. Geography The lake is within the Hearne Domain. Climate Ennadai Lake is of the few weather stations in Nunavut to report a subarctic climate (Köppen ''Dfc'') as opposed to a tundra climate (Köppen ET). Two months — July and August — have monthly means above ; July averages ; while the coldest month, January, has a mean monthly temperature of . The average annual precipitation is . Flora At Ennadai Lake's Kazan River outflow, the forest includes sparse black spruce and tamarack that grow approximately high, stunted because of harsh winds and dry summers. Fauna Ennadai Lake is part of the "annual migration route of the almost 500,000 strong Qamanirjuaq barren-ground caribo ...
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Churchill, Manitoba
Churchill is a town in northern Manitoba, Canada, on the west shore of Hudson Bay, roughly from the Manitoba–Nunavut border. It is most famous for the many polar bears that move toward the shore from inland in the autumn, leading to the nickname "Polar Bear Capital of the World" that has benefited its burgeoning tourism industry. Geography Churchill is located on Hudson Bay, at the mouth of the Churchill River on the 58th parallel north, far above most Canadian populated areas. Churchill is far from any other towns or cities, with Thompson, approximately to the south, being the closest larger settlement. Manitoba's provincial capital, Winnipeg, is approximately south of Churchill. While not part of the city, Eskimo Point and Eskimo Island are located across river with the former site of the Prince of Wales Fort. History A variety of nomadic Arctic peoples lived and hunted in this region. The Thule people arrived around the year 1000 from the west, the ancestors of the presen ...
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Hudson's Bay Company
The Hudson's Bay Company (HBC; french: Compagnie de la Baie d'Hudson) is a Canadian retail business group. A fur trading business for much of its existence, HBC now owns and operates retail stores in Canada. The company's namesake business division is Hudson's Bay, commonly referred to as The Bay ( in French). After incorporation by English royal charter in 1670, the company functioned as the ''de facto'' government in parts of North America for nearly 200 years until the HBC sold the land it owned (the entire Hudson Bay drainage basin, known as Rupert's Land) to Canada in 1869 as part of the Deed of Surrender, authorized by the Rupert's Land Act 1868. At its peak, the company controlled the fur trade throughout much of the English- and later British-controlled North America. By the mid-19th century, the company evolved into a mercantile business selling a wide variety of products from furs to fine homeware in a small number of sales shops (as opposed to trading posts) acros ...
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Whale Cove, Nunavut2
Whales are a widely distributed and diverse group of fully aquatic placental marine mammals. As an informal and colloquial grouping, they correspond to large members of the infraorder Cetacea, i.e. all cetaceans apart from dolphins and porpoises. Dolphins and porpoises may be considered whales from a formal, cladistic perspective. Whales, dolphins and porpoises belong to the order Cetartiodactyla, which consists of even-toed ungulates. Their closest non-cetacean living relatives are the hippopotamuses, from which they and other cetaceans diverged about 54 million years ago. The two parvorders of whales, baleen whales (Mysticeti) and toothed whales (Odontoceti), are thought to have had their last common ancestor around 34 million years ago. Mysticetes include four extant (living) families: Balaenopteridae (the rorquals), Balaenidae (right whales), Cetotheriidae (the pygmy right whale), and Eschrichtiidae (the grey whale). Odontocetes include the Monodontidae (belugas and n ...
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Tundra
In physical geography, tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. The term ''tundra'' comes through Russian (') from the Kildin Sámi word (') meaning "uplands", "treeless mountain tract". There are three regions and associated types of tundra: Arctic tundra, alpine tundra, and Antarctic tundra. Tundra vegetation is composed of dwarf shrubs, sedges, grasses, mosses, and lichens. Scattered trees grow in some tundra regions. The ecotone (or ecological boundary region) between the tundra and the forest is known as the tree line or timberline. The tundra soil is rich in nitrogen and phosphorus. The soil also contains large amounts of biomass and decomposed biomass that has been stored as methane and carbon dioxide in the permafrost, making the tundra soil a carbon sink. As global warming heats the ecosystem and causes soil thawing, the permafrost carbon cycle accelerates and releases much of these soil-contained g ...
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