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Fjords Of 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. When a ...
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Bonne Bay
Bonne Bay is a bay in Newfoundland and Labrador, Newfoundland, Canada. It is located on the western coast of Newfoundland and separates the Great Northern Peninsula from the rest of the island. It is a part of Gros Morne National Park. It is separated into two sections: Inner Bonne Bay and Outer Bonne Bay. Inner Bonne Bay consists of two arms, one which is south which has wooded coves and beach landings. Outer Bonne Bay consists of the entrance to the fjord of Bonne Bay. Bonne Bay was carved out approximately 10,000 years ago by two large glaciers in each one of the arms. The glaciers then came together in the middle part of the Bay and continued to push on out to the ocean. Mafic rock underlies the western shores of Bonne Bay, and clastic sedimentary rock is found on the eastern side. Soils on mafic rock belong to the Serpentine Cove Association, while sedimentary rock supports the Cox's Cove Association. Recreation Recreation in Bonne Bay consists of: Gros Morne National Pa ...
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Douglas Channel
Douglas Channel is one of the principal inlets of the British Columbia Coast. Its official length from the head of Kitimat Arm, where the aluminum smelter town of Kitimat to Wright Sound, on the Inside Passage ferry route, is . The actual length of the fjord's waterway includes waters between there and the open waters of the Hecate Strait outside the coastal archipelago, comprising another for in total. Geography The Kitimat River flows into the Kitimat Arm portion of Douglas Channel. The channel is named in honour of Sir James Douglas, the first governor of the Colony of British Columbia. A major side-inlet, the Gardner Canal, is in length, and is accessed from the Kitimat Arm of Douglas Channel via Devastation Channel (), which is on the east side of Hawkesbury Island. South of Hawkesbury is Varney Passage (), which has a sidechannel, Ursula Passage (). Total waterway length of the fjord dominated by Douglas Channel is therefore, not counting smaller side-inlets, , longer tha ...
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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 ...
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Tsunami
A tsunami ( ; from ja, 津波, lit=harbour wave, ) is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions (including detonations, landslides, glacier calvings, meteorite impacts and other disturbances) above or below water all have the potential to generate a tsunami. Unlike normal ocean waves, which are generated by wind, or tides, which are in turn generated by the gravitational pull of the Moon and the Sun, a tsunami is generated by the displacement of water from a large event. Tsunami waves do not resemble normal undersea currents or sea waves because their wavelength is far longer. Rather than appearing as a breaking wave, a tsunami may instead initially resemble a rapidly rising tide. For this reason, it is often referred to as a tidal wave, although this usage is not favoured by the scientific community because it might give ...
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Kangiqtualuk Uqquqti
Kangiqtualuk Uqquqti (Inuktitut syllabics: ''ᑲᖏᖅᑐᐊᓗᒃ ᐅᖅᑯᖅᑎ'') formerly Sam Ford Fiord is an isolated, elongated Arctic fjord on Baffin Island's northeastern coast in the Qikiqtaaluk Region of Nunavut, Canada. The Inuit settlement of Pond Inlet is to the northwest and Clyde River is to the east. This fjord is reputed for the harsh beauty of its landscapes with rocky cliffs rising steeply from the shore. It is also a popular place with climbers. History Kangiqtualuk Uqquqti had been one of the traditional hunting areas of the Inuit. It was renamed in memory of Inuk linguist Sam Ford, who died in a helicopter crash but it has since reverted to its original name. Geography Kangiqtualuk Uqquqti stretches roughly from north northeast to south southwest for about . Its mouth, located between the Remote Peninsula and Erik Point, is over wide, the width of the fjord narrowing gradually to an average of about inland. Kangiqtualuk Agguqti is a tributary fjord ...
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Alexandra Fiord
Alexandra Fiord is a natural inlet on the Johan Peninsula of Ellesmere Island in the Qikiqtaaluk Region of Nunavut, Canada. To the east, it opens into Buchanan Bay. History Alexandra Fiord has a long and variable history, from the Paleo and Thule cultures that inhabited the fiord from 2500 BCE - 1500 CE, to the scientists that seasonally visit the fiord now. From 1953 to 1963, the Royal Canadian Mounted Police The Royal Canadian Mounted Police (RCMP; french: Gendarmerie royale du Canada; french: GRC, label=none), commonly known in English as the Mounties (and colloquially in French as ) is the federal police, federal and national police service of ... had a station at Alexandra Fjord () which, at the time, was the northernmost police station in the world. It was then used as a seasonally scientific research base from 1987 to 1992. About Ellesmere Island. ''The Canadian Encyclopedia''. Retrieved April 26, 2015. It is currently used as a seasonal scientific research base. ...
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Baffin Island
Baffin Island (formerly Baffin Land), in the Canadian territory of Nunavut, is the largest island in Canada and the fifth-largest island in the world. Its area is , slightly larger than Spain; its population was 13,039 as of the 2021 Canadian census; and it is located at . It also contains the city of Iqaluit, the capital of Nunavut. Name The Inuktitut name for the island is , which means "very big island" ( "island" + "very big") and in Inuktitut syllabics is written as . This name is used for the administrative region the island is part of ( Qikiqtaaluk Region), as well as in multiple places in Nunavut and the Northwest Territories, such as some smaller islands: Qikiqtaaluk in Baffin Bay and Qikiqtaaluk in Foxe Basin. Norse explorers referred to it as ("stone land"). In 1576, English seaman Martin Frobisher made landfall on the island, naming it "Queen Elizabeth's Foreland" and Frobisher Bay is named after him. The island is named after English explorer William Baff ...
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Ellesmere Island
Ellesmere Island ( iu, script=Latn, Umingmak Nuna, lit=land of muskoxen; french: île d'Ellesmere) is Canada's northernmost and List of Canadian islands by area, third largest island, and the List of islands by area, tenth largest in the world. It comprises an area of , slightly smaller than Great Britain, and the total length of the island is . Lying within the Arctic Archipelago, Ellesmere Island is considered part of the Queen Elizabeth Islands. Cape Columbia at 83°06′ is the northernmost point of land in Canada and one of the northernmost points of land on the planet (the northernmost point of land on Earth is the nearby Kaffeklubben Island of Greenland). The Arctic Cordillera mountain system covers much of Ellesmere Island, making it the most mountainous in the Arctic Archipelago. More than one-fifth of the island is protected as Quttinirpaaq National Park. In 2021, the population of Ellesmere Island was recorded at 144. There are three settlements: Alert, Nunavut, Aler ...
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Arctic Archipelago
The Arctic Archipelago, also known as the Canadian Arctic Archipelago, is an archipelago lying to the north of the Canadian continental mainland, excluding Greenland (an autonomous territory of Denmark). Situated in the northern extremity of North America and covering about , this group of 36,563 islands, surrounded by the Arctic Ocean, comprises much of Northern Canada, predominately Nunavut and the Northwest Territories. The archipelago is showing some effects of climate change, with some computer estimates determining that melting there will contribute to the rise in sea levels by 2100. History Around 2500 BCE, the first humans, the Paleo-Eskimos, arrived in the archipelago from the Canadian mainland. Between 1000–1500 CE, they were replaced by the Thule people, who are the ancestors of today's Inuit. British claims on the islands, the British Arctic Territories, were based on the explorations in the 1570s by Martin Frobisher. Canadian sovereignty was originally (187 ...
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Saguenay Fjord
Saguenay Fjord National Park (french: parc national du Fjord-du-Saguenay) is a provincial park located in Quebec, Canada. In the regions of Saguenay–Lac-Saint-Jean, Charlevoix, Côte-Nord, and Bas-Saint-Laurent, the park is situated along the eastern end of the Saguenay River and adjoins the Saguenay–St. Lawrence Marine Park for over 100 km (60 mi.). The park, originally named Saguenay National Park, was renamed on April 20, 2011.Le parc national du Saguenay devient le parc national du Fjord-du-Saguenay
Ministère du Développement durable, de l’Environnement et des Parcs. Retrieved 11 May 2012.


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Saguenay River
__NOTOC__ The Saguenay River () is a major river of Quebec, Canada. It drains Lac Saint-Jean in the Laurentian Highlands, leaving at Alma and running east; the city of Saguenay is located on the river. It drains into the Saint Lawrence River. Tadoussac, founded as a French colonial trading post in 1600, is located on the northeast bank at this site. The river has a very high flow-rate and is bordered by steep cliffs associated with the Saguenay Graben. Tide waters flow in its fjord upriver as far as Chicoutimi (about 100 kilometres). Many Beluga whales breed in the cold waters at its mouth, making Tadoussac a popular site for whale watching and sea kayaking; Greenland sharks also frequent the depths of the river. The area of the confluence of the Saguenay and Saint Lawrence is protected by the Saguenay–St. Lawrence Marine Park, one of Canada's national parks. History The Saguenay River was used as an important trade route into the interior for the First Nations people of ...
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