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South Bentinck Arm
South Bentinck Arm is a long side-inlet of Dean Channel in the Central Coast region of British Columbia, Canada. At the north end of the arm it meets the North Bentinck Arm and then the Dean Channel before flowing into the Burke Channel. Rivers The arm is fed by the Taleomey River, which flows from the Taleomey Glacier just north of the Monarch Icefield. The Taleomy Indian Reserve No. 3 lies on the west side of the rivers mouth next to the Taleomey Narrows. Just to the north is the Noeick River and the locality of South Bentinck on the east shore of the inlet. Name origin South and North Bentinck Arms were named by George Vancouver, as "Bentinck Arms", in 1793, after the House of Portland; the Duke of Portland Duke is a male title either of a monarch ruling over a duchy, or of a member of royalty, or nobility. As rulers, dukes are ranked below emperors, kings, grand princes, grand dukes, and sovereign princes. As royalty or nobility, they are ranke ... at the time was W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dean Channel
Dean Channel is the upper end of one of the longest inlets of the British Columbia Coast, from its head at the mouth of the Kimsquit River. The Dean River, one of the main rivers of the Coast Mountains, enters Dean Channel about below the head of the inlet, at the community of Kimsquit. History Dean Channel was named by Captain Vancouver in 1793 after Rev. James King, Dean of Raphoe, Ireland. The channel was surveyed by Captain Richards in 1861 of HMS ''Hecate''. It is located within the Central Coast region. Branches Ending at the mouth of Cousins Inlet, which is the harbour for the abandoned town of Ocean Falls, the fjord's name changes to Fisher Channel down the west side of King Island. Below Fisher Channel's length the fjord merges with Burke Channel, which is a arm of the Dean/Fisher Channel on the east side of King Island, the name of the fjord changes to Fitz Hugh Sound, which is considerably wider than the upper part of the fjord at about in width and is itse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Noeick River
The Noeick River is a river in the Central Coast region of British Columbia, Canada, flowing west out of the northernmost Pacific Ranges to enter saltwater on the east side of South Bentinck Arm, immediately to the north of the mouth of the Taleomey River at Taleomey Narrows. The locality of South Bentinck is located at the river's mouth. There was a Nuxalk village, ''Nuiku'', on a raised mound south of the mouth of the Noieck River. Another village, ''Kadis'', was on the east side of South Bentinck Arm about ¼-mile north of the mouth of the Noieck. The river originates at the Noeick Glacier, which is to the northwest of Mount Jacobsen. See also *List of rivers of British Columbia The following is a partial list of rivers of British Columbia, organized by watershed. Some large creeks are included either because of size or historical importance (See Alphabetical List of British Columbia rivers ). Also included are lakes tha ... References Rivers of the Central Coa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
History Of British Columbia
The history of British Columbia covers the period from the arrival of Paleo-Indians thousands of years ago to the present day. Prior to European colonization, the lands encompassing present-day British Columbia were inhabited for millennia by a number of First Nations. Several European expeditions to the region were undertaken in the late 18th and early 19th centuries. After the Oregon boundary dispute between the UK and US government was resolved in 1846, the colonies of Vancouver Island and colony of British Columbia were established; the former in 1849 and the latter in 1858. The two colonies were merged to form a single colony in 1866, which later joined the Canadian Confederation on 20 July 1871. An influential historian of British Columbia, Margaret Ormsby, presented a structural model of the province's history in ''British Columbia: A History'' (1958); that has been adopted by numerous historians and teachers. Chad Reimer says, "in many aspects, it still has not been ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fjords Of British Columbia
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords whe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
William Cavendish-Bentinck, 3rd Duke Of Portland
William Henry Cavendish Cavendish-Bentinck, 3rd Duke of Portland, (14 April 173830 October 1809) was a British Whig and then a Tory politician during the late Georgian era. He served as Chancellor of the University of Oxford (1792–1809) and twice as Prime Minister of Great Britain (1783) and then of the United Kingdom (1807–1809). The gap of 26 years between his two terms as Prime Minister is the longest of any British Prime Minister. He was also the fourth great-grandfather of King Charles III through his great-granddaughter Cecilia Bowes-Lyon, Countess of Strathmore and Kinghorne. Portland was known before 1762 by the courtesy title Marquess of Titchfield. He held a title for every degree of British nobility: duke, marquess, earl, viscount, and baron. He was the leader of the Portland Whigs faction, which broke with the Whig leadership of Charles James Fox and joined with William Pitt the Younger in the wake of the French Revolution. Early life and education Lord Tit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Earl Of Portland
Earl of Portland is a title that has been created twice in the Peerage of England, firstly in 1633 and secondly in 1689. What proved to be a long co-held title, Duke of Portland, was created in 1716 and became extinct in 1990 upon the death of the ninth Duke, at which point the earldom passed to the most senior agnatic (solely male-line) cousin, namely one of the 6th degree. First creation (1633) The title of Earl of Portland was first created for the politician Richard Weston, 1st Baron Weston, in 1633. He was Chancellor of the Exchequer from 1621 to 1628 and Lord High Treasurer from 1628 to 1635. He had already been created Baron Weston of Nayland in the County of Suffolk in 1628; this title was also in the Peerage of England. He was succeeded by his son, the second Earl. He served as Joint Lord Lieutenant of Hampshire. His son, the third Earl, was killed at the Battle of Lowestoft in 1665. He was unmarried and was succeeded by his uncle, the fourth Earl. He was childless and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
George Vancouver
Captain George Vancouver (22 June 1757 – 10 May 1798) was a British Royal Navy officer best known for his 1791–1795 expedition, which explored and charted North America's northwestern Pacific Coast regions, including the coasts of what are now the Canadian province of British Columbia as well as the US states of Alaska, Washington and Oregon. He also explored the Hawaiian Islands and the southwest coast of Australia. Vancouver Island, the city of Vancouver in British Columbia, Vancouver, Washington in the United States, Mount Vancouver on the Canadian–US border between Yukon and Alaska, and New Zealand's fourth-highest mountain, also Mount Vancouver, are all named after him. Early life George Vancouver was born in the seaport town of King's Lynn (Norfolk, England) on 22 June 1757 - the sixth and youngest child of John Jasper Vancouver, a Dutch-born deputy collector of customs, and Bridget Berners. He came from an old respected family. The surname Vancouver comes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Bentinck
South Bentinck is a locality on South Bentinck Arm in the Central Coast region of British Columbia, Canada, located on the north side of the mouth of the Noeick River on the east shore of that inlet. See also *List of communities in British Columbia Communities in the province of British Columbia, Canada can include incorporated municipalities, Indian reserves, unincorporated communities or localities. Unincorporated communities can be further classified as recreational or urban. Indian ... References Central Coast of British Columbia Unincorporated settlements in British Columbia {{BritishColumbiaCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia Coast
, settlement_type = Region of British Columbia , image_skyline = , nickname = "The Coast" , subdivision_type = Country , subdivision_name = Canada , subdivision_type1 = Province , subdivision_name1 = British Columbia , parts_type = Principal cities , p1 = Vancouver , p2 = Surrey , p3 = Burnaby , p4 = Richmond , p5 = Abbotsford , p6 = Coquitlam , p7 = Delta , p8 = Nanaimo , p9 = Victoria , p10 = Chilliwack , p11 = Maple Ridge , p12 = New Westminster , p13 = Port Coquitlam , p14 = North Vancouver , area_blank1_title = 15 Districts , area_blank1_km2 = 244,778 , area_footnotes = , elevation_max_m = 4019 , elevation_min_m = 0 , elevation_max_footnotes = Mt. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monarch Icefield
The Monarch Icefield is the northernmost of a series of large continental icecaps studding the heights of the Pacific Ranges of the Coast Mountains in southern British Columbia. Located southeast of the town of Bella Coola and west of the headwaters of the Atnarko River, a tributary of the Bella Coola River The Bella Coola River is a major river on the Pacific slope of the Coast Mountains in southern British Columbia. The town of Bella Coola is at its mouth on North Bentinck Arm. Bella Coola Indian Reserve No. 1 the location of the main community ..., it lies to the north of the Ha-Iltzuk Icefield, which is the largest icefield of the group and home to the Silverthrone volcano. The Monarch Icefield is very remote and is rarely visited by mountaineering parties. References BCGNIS listing "Monarch Icefield" Central Coast of British Columbia Glaciers of the Pacific Ranges Ice fields of British Columbia {{BritishColumbiaCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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