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Cape Bexley
Cape Bexley is a headland in the northern Canadian territory of Nunavut. It is located on the mainland, on the south shore of Dolphin and Union Strait, and bounded on the south by Souths Bay. It was named after Nicholas Vansittart, 1st Baron Bexley. It is the ancestral home of the Akuliakattagmiut, a Copper Inuit subgroup. Haneragmiut Haneragmiut were a geographically defined Copper Inuit subgroup in the Canadian territory of Nunavut. They were the most westerly band of those that hunted in southern Victoria Island. They were generally located on the north shore of Dolphin and U ... camped here, too, and Nagyuktogmiut were visitors. References Bexley Former populated places in the Kitikmeot Region {{KitikmeotNU-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headland
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Canada
Northern Canada, colloquially the North or the Territories, is the vast northernmost region of Canada variously defined by geography and politics. Politically, the term refers to the three Provinces_and_territories_of_Canada#Territories, territories of Canada: Yukon, Northwest Territories and Nunavut. This area covers about 48 per cent of Canada's total land area, but has less than 1 per cent of demographics of Canada, Canada's population. The terms "northern Canada" or "the North" may be used in contrast with ''the far north'', which may refer to the Canadian Arctic, the portion of Canada that lies north of the Arctic Circle, east of Alaska and west of Greenland. However, in many other uses the two areas are treated as a single unit. __TOC__ Definitions Subdivisions As a social rather than political region, the Canadian North is often subdivided into two distinct regions based on climate, the ''near north'' and the ''far north''. The different climates of these two regions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nunavut
Nunavut ( , ; iu, ᓄᓇᕗᑦ , ; ) is the largest and northernmost Provinces and territories of Canada#Territories, territory of Canada. It was separated officially from the Northwest Territories on April 1, 1999, via the ''Nunavut Act'' and the ''Nunavut Land Claims Agreement, Nunavut Land Claims Agreement Act'', which provided this territory to the Inuit for independent government. The boundaries had been drawn in 1993. The creation of Nunavut resulted in the territorial evolution of Canada, first major change to Canada's political map in half a century since the province of Newfoundland and Labrador, Newfoundland was admitted in 1949. Nunavut comprises a major portion of Northern Canada and most of the Arctic Archipelago. Its vast territory makes it the list of the largest country subdivisions by area, fifth-largest country subdivision in the world, as well as North America's second-largest (after Greenland). The capital Iqaluit (formerly Frobisher Bay), on Baffin Islan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolphin And Union Strait
Dolphin and Union Strait lies in both the Northwest Territories (Inuvik Region) and Nunavut (Kitikmeot Region), Canada, between the mainland and Victoria Island. It is part of the Northwest Passage. It links Amundsen Gulf, lying to the northwest, with Coronation Gulf, lying to the southeast. The southeastern end of the strait is marked by Austin Bay. It gets its name from the two boats used by the Scottish naval surgeon and explorer John Richardson, who was the first known European to explore it in 1826. The Inuit who use this area have been variously known as the Copper Inuit, the Copper Eskimos, or the "People at the end of the world," because few other Indigenous groups had continuously used the area before. This is partly why the first Europeans who ventured into this area, were amazed by the "blond" Inuit they had encountered. There are several islands within the strait, including the Liston and Sutton Islands, historically home to the Noahonirmiut band of Copper Inuit. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nicholas Vansittart, 1st Baron Bexley
Nicholas Vansittart, 1st Baron Bexley, (29 April 1766 – 8 February 1851) was an English politician, and one of the longest-serving Chancellors of the Exchequer in British history. Background and education The fifth son of Henry Vansittart (died 1770), the Governor of Bengal, Vansittart was born in Bloomsbury, Middlesex, and raised in Bray, Berkshire. Educated at Christ Church, Oxford, he took his degree in 1787, and was called to the bar at Lincoln's Inn. From the early 1770s he was living with his mother at 60 Crooms Hill, Greenwich. Political career Vansittart began his public career by writing pamphlets in defence of the administration of William Pitt, especially on its financial side, and in May 1796 became Member of Parliament for Hastings, retaining his seat until July 1802, when he was returned for Old Sarum. In February 1801 he was sent on a diplomatic errand to Copenhagen, and shortly after his return was appointed joint Secretary to the Treasury, a position ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Akuliakattagmiut
Akuliakattagmiut were a geographically defined Copper Inuit subgroup in the Canadian territory of Nunavut. They were located near Cape Bexley on the south shore, mainland side of Dolphin and Union Strait, and in the vicinity of the Melville Hills' Akuliakattak Lake, the source of the Rae River. Culture Akuliakattagmiut wore more seal than other Copper Inuit. They did not wear belts at the hips, rather their pants come to the waist. According to Vilhjalmur Stefansson, the Akuliakattagmiut showed fear of guns, while other Inuit did not. All of their tools were sharp: iron snow knives, ulus; steel whittling knives, crooked knives, needles; copper ice picks; and metal scrappers. Some Akuliakattagmiut songs were of Uallirnergmiut origin. Their trade partners included the Haneragmiut Haneragmiut were a geographically defined Copper Inuit subgroup in the Canadian territory of Nunavut. They were the most westerly band of those that hunted in southern Victoria Island. They were gen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Copper Inuit
Copper Inuit, also known as Kitlinermiut and Inuinnait, are a Canadian Inuit group who live north of the tree line, in what is now the Kitikmeot Region of Nunavut and in the Inuvialuit Settlement Region in the Inuvik Region of the Northwest Territories. Most of them historically lived in the area around Coronation Gulf, on Victoria Island, and southern Banks Island. Their western boundary was Wise Point, near Dolphin and Union Strait. Their northwest territory was the southeast coast of Banks Island. Their southern boundary was the eastern shore of Great Bear Lake, Contwoyto Lake and Lake Beechey on the Back River. To the east, the Copper Inuit and the Netsilingmiut were separated by Perry River in Queen Maud Gulf. While Copper Inuit travelled throughout Victoria Island, to the west, they concentrated south of Walker Bay, while to the east, they were concentrated south of Denmark Bay. As the people have no collective name for themselves, they have adopted the English term "C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haneragmiut
Haneragmiut were a geographically defined Copper Inuit subgroup in the Canadian territory of Nunavut. They were the most westerly band of those that hunted in southern Victoria Island. They were generally located on the north shore of Dolphin and Union Strait, north of Cape Bexley, and south of Prince Albert Sound, on Victoria Island. Though they migrated seasonally both north and south for hunting, fishing, and trade, they were unaware that Victoria Island was an island. Ethnology Arctic explorer Vilhjalmur Stefansson discovered the Hanergmiut on May 17, 1910. At the time, the Haneragmiut numbered approximately 40 people. Seasonally, a few Haneragmiut hunted and traded to the south on the mainland with another Cape Bexley subgroup, the Akuliakattagmiut, while other Haneragmiut migrated as far north as Tahiryuak Lake to hunt caribou with the Kanianermiut. The Ekalluktogmiut were situated to the east of the Haneragmiut. After his return to Seattle and New York City in 1912, Stefa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of Kitikmeot Region
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a Cape (geography), cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking Wave, waves, Rocky shore, rocky shores, intense erosion, and steep sea cliffs, sea cliff. Headlands and Bay, bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as Sand, sands and Clay, clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
