|
Seymour Inlet
Seymour Inlet is one of the lesser travelled of the principal inlets of the British Columbia Coast. Unlike larger inlets such as Knight or Bute, it is not flanked by mountains but by relatively low, but still rugged, coastal hill-country and forms a maze of complex, narrow waterways and tidal pools and lagoons. It is located within a corresponding maze of peninsulas on the mainland on the northwest side of the Queen Charlotte Strait region. Its main arm is in length from the mouth of the Seymour River to the mouth of its north arm, Belize Inlet, which is about in length and has its own side inlets, narrow waterways named Wentworth Sound and Alison Sound. In between Belize Inlet and Seymour Inlet is Nugent Sound, named for the first United States Consul in Victoria; Seymour Inlet itself is named for Frederick Seymour, Governor of the Crown Colony of British Columbia from 1864 to 1869. Seymour Inlet has its own side-inlets, the largest being a south arm named Frederick Sound ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east and the Yukon and Northwest Territories to the north. With an estimated population of 5.3million as of 2022, it is Canada's third-most populous province. The capital of British Columbia is Victoria and its largest city is Vancouver. Vancouver is the third-largest metropolitan area in Canada; the 2021 census recorded 2.6million people in Metro Vancouver. The first known human inhabitants of the area settled in British Columbia at least 10,000 years ago. Such groups include the Coast Salish, Tsilhqotʼin, and Haida peoples, among many others. One of the earliest British settlements in the area was Fort Victoria, established ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Victoria, British Columbia
Victoria is the capital city of the Canadian province of British Columbia, on the southern tip of Vancouver Island off Canada's Pacific coast. The city has a population of 91,867, and the Greater Victoria area has a population of 397,237. The city of Victoria is the 7th most densely populated city in Canada with . Victoria is the southernmost major city in Western Canada and is about southwest from British Columbia's largest city of Vancouver on the mainland. The city is about from Seattle by airplane, seaplane, ferry, or the Victoria Clipper passenger-only ferry, and from Port Angeles, Washington, by ferry across the Strait of Juan de Fuca. Named for Queen Victoria, the city is one of the oldest in the Pacific Northwest, with British settlement beginning in 1843. The city has retained a large number of its historic buildings, in particular its two most famous landmarks, the Parliament Buildings (finished in 1897 and home of the Legislative Assembly of British Columbia ... [...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] |
List Of Fjords In Canada
Fjords in Canada are long, narrow inlets characterized by steep sides, created in a valley carved by glacial activity. A fjord can have two or more basins separated by sills. The bowls can have a depth of and the dividing sills can raise up to a few metres below the water surface. Mountainous glaciated areas in Canada are along the British Columbia Coast: from the Alaskan border along the Portland Canal to Indian Arm. Kingcome Inlet is a typical west coast fjord. In Newfoundland and Labrador, Saglek Fiord, Nachvak Fiord, and Hebron Fiord, are in Labrador. While Western Brook Pond, Trout River Big Pond, and Bonne Bay in Gros Morne National Park are located along the coastline of the island of Newfoundland. Quebec's Saguenay River valley contains a fjord. The Saguenay Fjord is long and deep. The Arctic Archipelago features fjords such as those around Ellesmere and Baffin Island, including Alexandra Fiord, Ellesmere Island, and Kangiqtualuk Uqquqti, Baffin Island. Whe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tidal Race
Tidal race or tidal rapid is a natural occurrence whereby a fast-moving tide passes through a constriction, resulting in the formation of waves, eddies and hazardous currents. The constriction can be a passage where the sides narrow, for example the Gulf of Corryvreckan and the Saltstraumen maelstrom, or an underwater obstruction (a reef or rising seabed), such as is found at the Portland Race in the United Kingdom. In extreme cases, such as Skookumchuck Narrows in British Columbia, through which tides can travel at more than 17 knots, very large whirlpools develop, which can be extremely hazardous to navigation. Notable tidal races * Cape Reinga in New Zealand * Skookumchuck Narrows in British Columbia, Canada * The Bitches in Wales, United Kingdom * |
Bramham Island
Bramham Island is an island in the Queen Charlotte Strait region of the British Columbia Coast, Central Coast of British Columbia, Canada, on the north side of the entrance to that strait. It lies in the entrance to the maze of waterways inland to the northeast, focused on Seymour Inlet, which includes Belize Inlet and Allison Harbour and Nugent Sound, though it is flanked only by Slingsby Channel on its north, and Schooner Channel (formerly Schooner Passage) on its east. To its west are the open waters at the convergence of Queen Charlotte Sound (Canada), Queen Charlotte Sound and Queen Charlotte Strait. About 23 km2 in size, it is mostly low-lying hills and has a number of freshwater lakes. Bramham Island was also the name of a former post office at , though there has been no settlement there since 1923. Name origin The island was named c. 1866 by Captain Pender of the Royal Navy after Bramham Park, the Yorkshire home of George Lane-Fox (MP), George Lane-Fox, in association ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schooner Channel
Schooner Channel, formerly Schooner Passage, is a strait on the east side of Bramham Island in the Central Coast region of British Columbia, Canada. Nearby, Allison Harbour Allison Harbour, also formerly known as False Bay and False Schooner Passage, is a natural harbour on the Central Coast of British Columbia, Canada, extending north from Queen Charlotte Strait to the southeast of Bramham Island. It is the site of ... was formerly known as False Schooner Passage. Links * * * Central Coast of British Columbia Channels of British Columbia {{BritishColumbiaCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slingsby Channel
Slingsby Channel is a strait on the north side of Bramham Island in the Queen Charlotte Strait region of the British Columbia Coast, Central Coast of British Columbia. It is one of only two entrances to Seymour Inlet and the associated maze of waterways inland, which lie to the northeast of Bramham. The other entrance is Schooner Channel, formerly Schooner Passage, on the east side of that island. The Fox Islands (British Columbia), Fox Islands, which lie in its entrance, Bramham Island and the channel itself, plus Slingsby Rock and Slingsby Point, are named in association with Bramham Park, the Yorkshire home of George Lane-Fox (MP), George Lane-Fox. Through the Slingsby Channel flows the world's strongest current, the Nakwakto Rapids, that has been measured at speeds up to 18.4 miles per hour. The current is so fast at times, that people have tied a rope to Turret Rock, which is located right in the middle of the rapids, and then water-skied. References Central Coas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frederick Sound (Canada)
Frederick Sound is a sound in the Central Coast of British Columbia, Canada. It is the largest branch of Seymour Inlet and along with that inlet was named in honour of Frederick Seymour, second governor of the Colony of British Columbia. Frederick Sound has two inlets, one named Salmon Arm and the other unnamed. The complex maze of hidden waterways forming Seymour Inlet is in the region of Queen Charlotte Strait. Frederick Sound should not be confused with Frederick Arm, which extends north from Cordero Channel between Loughborough and Bute Inlet , image = Bute Inlet.jpg , image_size = 260px , alt = , caption = , image_bathymetry = , alt_bathymetry = , caption_bathymetry = , location = Strathcona RD, British Col ...s. References * Central Coast of British Columbia Sounds of British Columbia {{BritishColumbiaCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colony Of British Columbia (1866–1871)
The Colony of British Columbia was a British Crown Colony that resulted from the amalgamation of the two former colonies, the Colony of Vancouver Island and the mainland Colony of British Columbia. The two former colonies were united in 1866, and the united colony existed until its incorporation into the Canadian Confederation in 1871. Background The Colony of Vancouver Island had been created in 1849 to bolster British claims to the whole island and the adjacent Gulf Islands, and to provide a North Pacific home port for the Royal Navy at Esquimalt. By the mid-1850s, the Island Colony's non-indigenous population was around 800 people; a mix of mostly British, French-Canadian, Hawaiians, but with handfuls of Iroquoians, Métis and Cree in the employ of the fur company, and a few Belgian and French Oblate priests (thousands of First Nations died due to the smallpox epidemic, which had occurred in the 16th century). Three years earlier, the Treaty of Washington had establishe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_VICTORIA_FROM_JAMES'_BAY_LOOKING_UP_GOVERNMENT_STREET.jpg "Click for more on -> Victoria, British Columbia")
.jpg "Click for more on -> Fjords Of British Columbia")
