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Arctic Archipelago Marine
The Arctic Archipelago Marine Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is a marine ecozone in the Canadian Arctic, encompassing Hudson Bay, James Bay, the internal waters and some shores of the islands in the Canadian Arctic Archipelago, and the shores of the territories, northern Ontario and western Quebec. Early exploration of these waters by Europeans were conducted to find a passage to the Orient, now referred to as the Northwest Passage. It is inextricably tied to the terrestrial ecozones of the Arctic Cordillera, Northern Arctic, Southern Arctic, Hudson Plains, Taiga Shield, Taiga Plains, and Taiga Cordillera, as well as the marine ecozones of the Arctic Basin Marine and Northwest Atlantic Marine. Climate It is characterised by frigid, windy winters with average temperatures below -30 degrees Celsius, and summer temperatures typically near 10 degrees. The thick ice which cover the ecozone in the winter connect the islands and continental l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beluga Whale
The beluga whale () (''Delphinapterus leucas'') is an Arctic and sub-Arctic cetacean. It is one of two members of the family Monodontidae, along with the narwhal, and the only member of the genus ''Delphinapterus''. It is also known as the white whale, as it is the only cetacean to regularly occur with this colour; the sea canary, due to its high-pitched calls; and the melonhead, though that more commonly refers to the melon-headed whale, which is an oceanic dolphin. The beluga is adapted to life in the Arctic, with anatomical and physiological characteristics that differentiate it from other cetaceans. Amongst these are its all-white colour and the absence of a dorsal fin, which allows it to swim under ice with ease. It possesses a distinctive protuberance at the front of its head which houses an animal echolocation, echolocation organ called the Melon (whale), melon, which in this species is large and deformable. The beluga's body size is between that of a dolphin and a true ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Provinces And Territories Of Canada
Within the geographical areas of Canada, the ten provinces and three territories are sub-national administrative divisions under the jurisdiction of the Canadian Constitution. In the 1867 Canadian Confederation, three provinces of British North America—New Brunswick, Nova Scotia, and the Province of Canada (which upon Confederation was divided into Ontario and Quebec)—united to form a federation, becoming a fully independent country over the next century. Over its history, Canada's international borders have changed several times as it has added territories and provinces, making it the world's second-largest country by area. The major difference between a Canadian province and a territory is that provinces receive their power and authority from the ''Constitution Act, 1867'' (formerly called the ''British North America Act, 1867''), whereas territorial governments are creatures of statute with powers delegated to them by the Parliament of Canada. The powers flowing from t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wind
Wind is the natural movement of air or other gases relative to a planet's surface. Winds occur on a range of scales, from thunderstorm flows lasting tens of minutes, to local breezes generated by heating of land surfaces and lasting a few hours, to global winds resulting from the difference in absorption of solar energy between the climate zones on Earth. The two main causes of large-scale atmospheric circulation are the differential heating between the equator and the poles, and the rotation of the planet (Coriolis effect). Within the tropics and subtropics, thermal low circulations over terrain and high plateaus can drive monsoon circulations. In coastal areas the sea breeze/land breeze cycle can define local winds; in areas that have variable terrain, mountain and valley breezes can prevail. Winds are commonly classified by their spatial scale, their speed and direction, the forces that cause them, the regions in which they occur, and their effect. Winds have various asp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northwest Atlantic Marine
The Northwest Atlantic Marine Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is a Canadian marine ecozone forming a transitional region between the cold northern waters of the Arctic Ocean and the more temperate waters in its southern extent. Geography Stretching in a narrow strip offshore from Ellesmere Island and Devon Island in Baffin Bay, it runs parallel to the coast of Bylot Island and Baffin Island until meeting it at the Cumberland Peninsula. It covers the waters of the Davis Strait and the Hudson Strait, Ungava Bay and portions of the Labrador Sea, including all coastal areas of Labrador and the northern coast of Newfoundland. It also includes the Gulf of Saint Lawrence to the mouth of the Saint Lawrence River. The cold, highly saline North Atlantic Deep Water forms in the Labrador Sea and flows at great depth along the western edge of the North Atlantic. Moreover, in this ecozone the cold Labrador Current meets the Gulf Stream at the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arctic Basin Marine
The Arctic Basin Marine Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is a Canadian marine ecozone encompassing the northwestern areas of waters on the Arctic continental shelf. It is bitterly cold and permanently covered in ice. Polar nights and the midnight sun may last months in this region, which has come to characterize the stereotype of the north. Its only land contact is with the northern coast of Ellesmere Island. Because of this, there are no inhabitants in this zone. All human activity here involves scientific excursions, petroleum exploration, rare hunting groups and extreme adventurers. Geography Ice floes that are kilometres long and several metres thick are common in this Arctic Ocean ecozone. Undersea, the dominant feature is the deep Canada Basin, extending from the Beaufort Sea to the North Pole to depths reaching 3,600 m. The Lomonosov Ridge represents its northern submarine extent. Climate The region is arid, receiving betw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taiga Cordillera
The Taiga Cordillera Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is a rugged, mountainous terrestrial ecozone of Canada spanning most of northern Yukon and significant portions of the border between the Yukon and the Northwest Territories. This ecozone is very sparsely populated, with only a few hundred inhabitants who rely on subsistence living and the tourism industry. Most of the area's population consists of members of the Vuntut Gwitchin First Nation in the community of Old Crow, located on the Porcupine River. Geography To the south is the Boreal Cordillera, to the east are the Taiga Plains, and its northern extent is defined by Yukon's coastline, at which it abuts the Southern Arctic ecozone. The northernmost area is an arctic tundra which is beyond the tree line, so is characterised by small plants and shrubs. These transition to alpine tundra and lowland taiga in a southeastern arc across the zone. To the northwest are rolling hills, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taiga Plains
The Taiga Plain Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is a Canadian terrestrial ecozone that covers most of the western Northwest Territories, extending to northwest Alberta, northeast British Columbia and slightly overlapping northeastern Yukon. It is the site of the Peace-Athabasca Delta, a globally significant wetland in Wood Buffalo National Park, and Nahanni National Park Reserve. Geography Its eastern boundary is located by Great Bear and Great Slave lakes in the Taiga Shield, site of the world's oldest known rock formations. To its south are the Boreal Plains, a vast forest of spruce and other timber with numerous wetland habitats. Portions of Wood Buffalo National Park and Whooping Crane Summer Range, the only nesting area for the critically endangered whooping crane, overlap onto the Taiga Plains from the Boreal Plains. To the west it abuts the foothills of the Boreal Cordillera in British Columbia and southern Yukon, and the Taig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taiga Shield
The Taiga Shield Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is an ecozone which stretches across Canada's subarctic region. Some regions exhibit exposed Precambrian bedrock of the Canadian Shield, the oldest of the world's geological formations. The world's oldest rocks, dating to four billion years, are found in the Canadian Shield north of Great Slave Lake. Geography The Taiga Shield ecozone covers almost all of the eastern area of the Northwest Territories, a tiny corner of northeastern Alberta, a narrow strip of all northern Saskatchewan and northwestern Manitoba, as well as all some parts of southern Nunavut. Here, it is interrupted by Hudson Bay, where it abuts with the marine ecozone of the Arctic Archipelago Marine, and resumes on the eastern shores of Hudson Bay on the coast of Quebec, where it continues in a consistently-wide strip towards the ocean, encompassing all but a small portion of Labrador. It is one of the largest ecozones in Cana ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hudson Plains
The Southern Hudson Bay taiga is a terrestrial ecoregion, as classified by the World Wildlife Fund, which extends along the southern coast of Hudson Bay and resides within the larger taiga biome. The region is nearly coterminous with the Hudson Plain, a Level I ecoregion of North America as designated by the Commission for Environmental Cooperation (CEC) in its ''North American Environmental Atlas''. Entirely located in Canada, the Southern Hudson Bay taiga covers an area of approximately and crosses the provinces of Manitoba, Ontario, and the western portion of Quebec. Various islands in James Bay which belong to Nunavut are also considered to be part of the ecoregion. It includes the largest continuous wetland in the world. It covers nearly a quarter of Ontario's landmass, and 3.6% of Canada's total area, Its historical prominence is due to the harshness endured by pioneer explorers who established fortifications for Hudson's Bay Company, and as a result of regional wars be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Arctic
The Southern Arctic Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is a Canadian terrestrial ecozone which spans the northern coast of mainland Northwest Territories, most of northern mainland Nunavut excepting the northeast peninsula, and a portion of northwestern Quebec. Its two constituent territories are interrupted by Hudson Bay. The ecozone can also be described as including the northernmost part of the Interior Plains of Western Canada and parts of the Canadian Shield located on both sides of northern Hudson Bay. It is sparsely populated, with less than 10,000 inhabitants in 17 major settlements, the largest of which is Rankin Inlet. About 80% of the population is Inuit. Geography Its southern boundary demarcates the tree line, and to the north it meets the Northern Arctic terrestrial ecozone and the Arctic Archipelago Marine ecozone. It was formed from glacial deposits left by retreating glaciers about 8,500 years ago, which amassed into morain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Arctic
The Northern Arctic Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is a Canadian terrestrial ecozone which includes most of the Canadian Arctic Archipelago, the Boothia and Melville Peninsulas of Nunavut, and the northwestern tip of Quebec. Its marine borders are with the Arctic Archipelago Marine Ecozone, and it is adjacent to the mainland Southern Arctic Ecozone. Sparsely populated, it is home to 15,000 inhabitants, approximately 80% of whom are Inuit. The largest settlement is Iqaluit. The cold winters are very dark, typically having no daylight for weeks or even months north of the Arctic Circle. Geography Palaeozoic and Mesozoic sedimentary rock forms the western portion of the ecozone, whereas Precambrian granite is the dominant feature in the east. Broad flat plains are common on the coastlines, and extend inland up to in some parts. In the east, plateaus and rocky hills merge into the foothills of the Arctic Cordillera. The west is charact ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arctic Cordillera
The Arctic Cordillera is a terrestrial ecozone in northern Canada characterized by a vast, deeply dissected chain of mountain ranges extending along the northeastern flank of the Canadian Arctic Archipelago from Ellesmere Island to the northeasternmost part of the Labrador Peninsula in northern Labrador and northern Quebec, Canada. It spans most of the eastern coast of Nunavut with high glaciated peaks rising through ice fields and some of Canada's largest ice caps, including the Penny Ice Cap on Baffin Island. It is bounded to the east by Baffin Bay, Davis Strait and the Labrador Sea while its northern portion is bounded by the Arctic Ocean. Overview The range is mostly located in Nunavut but extends southeast into the northernmost tip of Labrador and northeastern Quebec. The system is divided into a series of ranges, with mountains reaching heights of more than . The highest is Barbeau Peak on Ellesmere Island at , which is the highest point in eastern North America. The syst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
