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Knight Inlet
Knight Inlet (Kwakʼwala: ''Tsawatti'') is one of the principal inlets of the British Columbia Coast, and the largest of the major inlets in the southern part of the Coast. It is fifth in sequence of the great saltwater inlets north from the 49th parallel near Vancouver, but it is the first whose outflow points away from the Strait of Georgia, opening into Queen Charlotte Strait at the Kwakwakaʼwakw community of Memkumlis (often known by the name of the group who were based there, the Mamalilikala) on Village Island. Geography The inlet's opening lies east of Malcolm Island and the fishing town of Port McNeill on Vancouver Island, and just north of the opening of the upper end of Johnstone Strait, which separates Vancouver Island from the archipelago between it and the mainland. Knight Inlet is one of the longest on the BC Coast at about in length; it is about in average width. Its great volume of water causes a major current and severe turbulence at its mouth during tidal c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Waddington Regional District
The Regional District of Mount Waddington (RDMW) is a regional district in British Columbia. It takes in the lower Central Coast region centred on the Queen Charlotte Strait coast of northern Vancouver Island and the adjoining parts of mainland British Columbia. It has a total land area of 20,288.4 km² (7,833.4 sq mi) and a 2016 census population of 11,035 persons, most of which is in towns on Vancouver Island and adjoining islands. The administrative centre is in the town of Port McNeill. Other municipalities include the district municipality of Port Hardy, the village of Port Alice, and the village of Alert Bay. Demographics As a census division in the 2021 Census of Population conducted by Statistics Canada, the Regional District of Mount Waddington had a population of living in of its total private dwellings, a change of from its 2016 population of . With a land area of , it had a population density of in 2021. Municipalities *Alert Bay *Port Alice *Port Hardy * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port McNeill
Port McNeill is a town in the North Island region of Vancouver Island, British Columbia, Canada with a population of 2,356 (2021). Located on Vancouver Island's north-east shore on Queen Charlotte Strait, it was originally a base camp for loggers. Port McNeill became a settlement in 1936. The town was named after Captain William Henry McNeill of the Hudson's Bay Company. Demographics In the 2021 Census of Population conducted by Statistics Canada, Port McNeill had a population of 2,356 living in 1,019 of its 1,111 total private dwellings, a change of from its 2016 population of 2,337. With a land area of , it had a population density of in 2021. Religion According to the 2021 census, religious groups in Port McNeill included: *Irreligion (1,545 persons or 65.9%) *Christianity (730 persons or 31.1%) *Buddhism (10 persons or 0.4%) Tourism and location Along with housing the headquarters of the Regional District of Mount Waddington, Port McNeill acts as a central hub for ... [...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] |
William Robert Broughton
William Robert Broughton (22 March 176214 March 1821) was a British naval officer in the late 18th century. As a lieutenant in the Royal Navy, he commanded HMS ''Chatham'' as part of the Vancouver Expedition, a voyage of exploration through the Pacific Ocean led by Captain George Vancouver in the early 1790s. Personal life William Robert Broughton was born on 22 March 1762.J. K. Laughton, 'Broughton, William Robert, naval officer, (1762–1821)', rev. Roger Morriss, ''Oxford Dictionary of National Biography'', Oxford University Press, 2004; online edn, May 200retrieved 29 December 2015/ref> His father, Charles Broughton, was a Hamburg merchant and his mother, Anne Elizabeth, was the daughter of Baron William de Hertoghe. Broughton married his cousin, Jemima, on 26 November 1802. They had four children. On 12 March 1821, while in Florence, Broughton suffered an angina attack and died two days later. He was buried in the English burial ground in Leghorn. Early career Broughton' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silverthrone Caldera
The Silverthrone Caldera is a potentially active caldera complex in southwestern British Columbia, Canada, located over northwest of the city of Vancouver and about west of Mount Waddington in the Pacific Ranges of the Coast Mountains. The caldera is one of the largest of the few calderas in western Canada, measuring about long (north-south) and wide (east-west). Mount Silverthrone, an eroded lava dome on the caldera's northern flank that is high, may be the highest volcano in Canada. The main glaciers in the Silverthrone area are the Pashleth, Kingcome, Trudel, Klinaklini and Silverthrone glaciers. Most of the caldera lies in the Ha-Iltzuk Icefield, which is the largest icefield in the southern half of the Coast Mountains; it is one of the five icefields in southwestern British Columbia that thinned between the mid-1980s and 1999 due to global warming. Nearly half of the icefield is drained by the Klinaklini Glacier, which feeds the Klinaklini River. The Silverthrone ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coast Mountains
The Coast Mountains (french: La chaîne Côtière) are a major mountain range in the Pacific Coast Ranges of western North America, extending from southwestern Yukon through the Alaska Panhandle and virtually all of the Coast of British Columbia south to the Fraser River. The mountain range's name derives from its proximity to the sea coast, and it is often referred to as the Coast Range. The range includes volcanic and non-volcanic mountains and the extensive ice fields of the Pacific and Boundary Ranges, and the northern end of the volcanic system known as the Cascade Volcanoes. The Coast Mountains are part of a larger mountain system called the Pacific Coast Ranges or the Pacific Mountain System, which includes the Cascade Range, the Insular Mountains, the Olympic Mountains, the Oregon Coast Range, the California Coast Ranges, the Saint Elias Mountains and the Chugach Mountains. The Coast Mountains are also part of the American Cordilleraa Spanish term for an extensive chain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Cap
In glaciology, an ice cap is a mass of ice that covers less than of land area (usually covering a highland area). Larger ice masses covering more than are termed ice sheets. Description Ice caps are not constrained by topographical features (i.e., they will lie over the top of mountains). By contrast, ice masses of similar size that ''are'' constrained by topographical features are known as ice fields. The ''dome'' of an ice cap is usually centred on the highest point of a massif. Ice flows away from this high point (the ice divide) towards the ice cap's periphery. Ice caps have significant effects on the geomorphology of the area that they occupy. Plastic moulding, gouging and other glacial erosional features become present upon the glacier's retreat. Many lakes, such as the Great Lakes in North America, as well as numerous valleys have been formed by glacial action over hundreds of thousands of years. On Earth, there are about of total ice mass. The average temperature ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ha-Iltzuk Icefield
The Ha-Iltzuk Icefield is an icefield in the central Pacific Ranges of the Coast Mountains in British Columbia, Canada. It is the largest icefield in the Coast Mountains south of the Alaska Panhandle, with an area of . It is located on the west side of the Klinaklini River and the Waddington Range. The highest summit in the icefield is Mount Silverthrone, which is a mountain on the northeast edge of a circular, wide, deeply dissected caldera complex called the Silverthrone Caldera. The southern half of the icefield is named the Silverthrone Glacier and flows west, joining the Klinaklini Glacier just above that glacier's terminus, where its outflow is short but very large, and joins the Klinaklini River within a few kilometres. The Klinaklini Glacier constitutes the northern half of the icefield, and off its northwest edge a glacial tongue produces the head of the Machmell River. The name Ha-Iltzuk Icefield does not appear in government gazettes. The term is almost certainly a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Klinaklini Glacier
The Klinaklini Glacier is a glacier west of the Klinaklini River and head of Knight Inlet the Coast Land District of British Columbia, Canada Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by tot ... (51° 28′ 0″ N, 125° 47′ 0″ W). It flows generally southward from Mt. Silverthrone. The glacier is one of the largest glaciers in western North America. The Hakai Institute has installed a weather station and camera above Klinaklini Glacier that will provide data in near real time to scientists and operational users. References Glaciers of the Pacific Ranges Central Coast of British Columbia {{canada-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chilcotin Country
The Chilcotin () region of British Columbia is usually known simply as "the Chilcotin", and also in speech commonly as "the Chilcotin Country" or simply Chilcotin. It is a plateau and mountain region in British Columbia on the inland lee of the Coast Mountains on the west side of the Fraser River. Chilcotin is also the name of the river draining that region. In the language of the Chilcotin people their name and the name of the river means "people of the red ochre river" (its tributary the Chilko River means "red ochre river") The Chilcotin district is often viewed as an extension of the Cariboo region, east of that river, although it has a distinct identity from the Cariboo District. It is, nonetheless, part of the Cariboo Regional District which is a municipal-level body governing some aspects of infrastructure and land-used planning. The vast majority of the population are First Nations people, members of the Tsilhqot'in and Dakelh peoples, while others are settlers and ran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Klinaklini River
The Klinaklini River ( Kwak'wala name T̓linat̓łina also spelled ƛ̓inaƛ̓ina) is one of the major rivers of the Pacific Ranges section of the Coast Mountains in the Canadian province of British Columbia. It originates in the Pantheon Range and empties into the head of Knight Inlet. A different spelling of ''Klinaklini'' is Kleena Kleene, which is the name of a recreational community on the river just below its exit from the Pantheon Range onto the Chilcotin Plateau. In the area of Kleena Kleene the Klinaklini, Homathko and Chilanko River basins share the same stretch of plateau. The names Kleena Kleene and Klinaklini derive from the Kwak'wala word for eulachon grease, which is made from the eulachon, a small oily fish that ascend coastal rivers. There is a First Nation village of the Tanakteuk subdivision of the Kwakwaka'wakw peoples at the mouth of the river, Tsawatti. Located on the Indian Reserve of the same name, it is the primary eulachon fishing and preservati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Interior Plateau
The Interior Plateau comprises a large region of the Interior of British Columbia, and lies between the Cariboo and Monashee Mountains on the east, and the Hazelton Mountains, Coast Mountains and Cascade Range on the west.''Landforms of British Columbia'', S. Holland, Government of British Columbia'' The continuation of the plateau into the United States is known there as the Columbia Plateau. Physiographically, the Interior Plateau is a section of the larger Northern Plateaus province, which in turn is part of the Intermontane Plateaus physiographic division. (The Interior Plateau is ''not'' part of the Interior Mountains, a huge area that constitutes most of the northern two thirds of the Canadian province of British Columbia between the Coast Mountains, Rocky Mountains and the various small ranges on the inland lea of the Coast Mountains between the Bulkley Ranges and the Bella Coola River). Subdivisions It has several subdivisions, these being: * The Fraser Plateau ** The Chi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
