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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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sir George Back
Admiral Sir George Back (6 November 1796 – 23 June 1878) was a British Royal Navy officer, explorer of the Canadian Arctic, naturalist and artist. He was born in Stockport. Career As a boy, he went to sea as a volunteer in the frigate in 1808 and took part in the destruction of batteries on the Spanish coast. In the following year, he was involved in combat in the Bay of Biscay, until he was captured by the French. Back remained a prisoner at Verdun until the peace of early 1814; during this time he studied French and mathematics and practised his skills as an artist, which he later put to use in recording his travels through the Canadian Arctic. Following his release, Back served on and as a midshipman before volunteering to serve under John Franklin in his first expedition to the Arctic in 1818. Back also served under Franklin in his two overland expeditions to survey the northern coast of North America, first on the Coppermine expedition—when Back was responsibl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haningayogmiut
The Haningayogmiut were a Copper Inuit subgroup located on the Back River (''Haningayok''). According to Arctic explorer Vilhjalmur Stefansson Vilhjalmur Stefansson (November 3, 1879 – August 26, 1962) was an Arctic explorer and ethnologist. He was born in Manitoba, Canada. Early life Stefansson, born William Stephenson, was born at Arnes, Manitoba, Canada, in 1879. His parents had ..., the Haningayogmiut were a small tribe. The Kaernermiut were also located on the Back River and may have been the same subgroup. References Copper Inuit {{NorthwestTerritories-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tree Line
The tree line is the edge of the habitat at which trees are capable of growing. It is found at high elevations and high latitudes. Beyond the tree line, trees cannot tolerate the environmental conditions (usually cold temperatures, extreme snowpack, or associated lack of available moisture). The tree line is sometimes distinguished from a lower timberline, which is the line below which trees form a forest with a closed Canopy (biology), canopy. At the tree line, tree growth is often sparse, stunted, and deformed by wind and cold. This is sometimes known as ''krummholz'' (German for "crooked wood"). The tree line often appears well-defined, but it can be a more gradual transition. Trees grow shorter and often at lower densities as they approach the tree line, above which they are unable to grow at all. Given a certain latitude, the tree line is approximately 300 to 1000 meters below the permanent snow line and roughly parallel to it. Causes Due to their vertical structure, tree ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rapids
Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Rapids are hydrological features between a ''run'' (a smoothly flowing part of a stream) and a ''cascade''. Rapids are characterized by the river becoming shallower with some rocks exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white color, forming what is called "whitewater". Rapids occur where the bed material is highly resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length. Rapids cause water aeration of the stream or river, resulting in better water quality. Rapids are categorized in classes, generally running from I to VI. A Class 5 rapid may be categorized as Class 5.1-5.9. While Class I rapids are eas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canoeing
Canoeing is an activity which involves paddling a canoe with a single-bladed paddle. Common meanings of the term are limited to when the canoeing is the central purpose of the activity. Broader meanings include when it is combined with other activities such as canoe camping, or where canoeing is merely a transportation method used to accomplish other activities. Most present-day canoeing is done as or as a part of a sport or recreational activity. In some parts of Europe canoeing refers to both canoeing and kayaking, with a canoe being called an ''open canoe''. A few of the recreational forms of canoeing are canoe camping and canoe racing. Other forms include a wide range of canoeing on lakes, rivers, oceans, ponds and streams. History of organized recreational canoeing Canoeing is an ancient mode of transportation. Modern recreational canoeing was established in the late 19th century. In 1924, canoeing associations from Austria, Germany, Denmark and Sweden founded the ''I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kazan River
The Kazan River (Inuktitut ''Harvaqtuuq'', Inuktitut syllabics ᓴᕐᕙᖅᑑᖅ; meaning "strong rapids", "the big drift" or "place of much fast flowing water"), is a Canadian Heritage River located in Nunavut, Canada. The Dene name for the river was Kasba-tue meaning "white partridge river." The name was apparently changed to Kazan in the late 19th century due to the influence of Order of Mary Immaculate missionaries. The river headwaters are in northern Saskatchewan"Nunavut: Heritage Rivers" ''The Atlas of Canada'' at Kasba Lake, and it flows north for about 1000 km (621 mi) before emptying into Baker Lake (), on the opposite side of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dubawnt Lake
Dubawnt Lake is a lake in the Kivalliq Region, Nunavut, Canada. It is in size and has several islands. It is about north of the Four Corners, about west of Hudson Bay and about south of the Arctic Circle. To the northwest is the Thelon Wildlife Sanctuary. Its main inlet and outlet is the north-flowing Dubawnt River which joins the Thelon River at Beverly Lake. The Thelon flows east to Hudson Bay at Chesterfield Inlet. It is on the line of contact between the Sayisi Dene band of Eastern Caribou-Eater Chipewyan people and the Harvaqtuurmiut and Ihalmiut bands of Caribou Inuit. The first recorded European to reach the lake was Samuel Hearne in 1770, but it remained largely unknown to outsiders until it was explored by Joseph Tyrrell in 1893. There are no permanent settlements but there are fly-in fish camps where large lake trout can be caught during the two month ice-free season. Dubawnt River The Dubawnt River is long and begins in the Northwest Territories from a tributary o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hood River (Nunavut)
The Hood River of Nunavut, Canada, is a long river draining into the Arctic Ocean from its headwaters in the interior of Canada's tundra at Napaktulik Lake, close to the Northwest Territories border. The river ends at Arctic Sound near the community of Bathurst Inlet. The river is above the Arctic Circle and tree line. Lake trout are plentiful and can be almost a metre long. The upper lakes of the Hood can be frozen until July, and on the banks of the river, grizzlies, wolves, wolverines, and muskox are plentiful. In the short Arctic summer, canoeists braving the mighty river can see the migration of the barren-ground caribou through the area. Muskox and wolves are also common sights. There are numerous rapids, waterfalls and glaciers along the river. Wilberforce Gorge is a steep, high gorge that runs for at almost deep. Kattimannap Qurlua, at the head of the gorge, is the highest waterfall north of the Arctic Circle falling in two drops. During Sir John Franklin's first ov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coppermine River
The Coppermine River is a river in the North Slave and Kitikmeot regions of the Northwest Territories and Nunavut in Canada. It is long. It rises in Lac de Gras, a small lake near Great Slave Lake, and flows generally north to Coronation Gulf, an arm of the Arctic Ocean. The river freezes in winter but may still flow under the ice. The community of Kugluktuk (formerly Coppermine) is located at the river's mouth. The river was named for the copper ores which are located along the river, by Samuel Hearne in 1771. Hearne found only one lump of copper and commercial mining was not considered viable. Bloody Falls, part of the Kugluk/Bloody Falls Territorial Park, is located from Kugluktuk, and was home to the Kogluktogmiut a sub-group of the Copper Inuit. It is the site of the Bloody Falls Massacre, when Matonabbee, Samuel Hearne's guide, and his fellow Chipewyan warriors ambushed and massacred the local Inuit. Gallery See also *List of longest rivers of Canada Among the lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hayes River (Nunavut)
The Hayes River is a river in the Kitikmeot and Kivalliq Regions of Nunavut, Canada. It is in the Arctic Ocean drainage basin and is a tributary of the Back River. Course The river begins at an unnamed lake in Kivalliq Region, and reaches its mouth at the Back River in Kitikmeot Region, just south of that river's mouth at Cockburn Bay on Chantrey Inlet Chantrey Inlet (''Tariunnuaq'') is a bay on the Arctic coast of Canada. It marks the southeast "corner" where the generally east–west coast turns sharply north. To the west is the Adelaide Peninsula and to the east is mainland. King William Is ... on the Arctic Ocean. References * * Rivers of Kitikmeot Region Rivers of Kivalliq Region {{Nunavut-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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