Cornice Mountain (Cambria Icefield)
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Cornice Mountain (Cambria Icefield)
Cornice Mountain, , is a mountain in the Cambria Icefield of the Boundary Ranges of the northern Coast Mountains in British Columbia, Canada. The peak is on the north flank of the Cambria Icefield, south of Strohn Creek and between Meziadin Lake Meziadin Lake Provincial Park is a provincial park in 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 ... and the Bear River Pass, northeast of the town of Stewart. See also * Cornice Mountain (Stikine Icecap) * Cornice Ridge References {{coord, 56, 04, 25, N, 129, 36, 16, W, display=title, source:BCNames Boundary Ranges Stewart Country Two-thousanders of British Columbia ...
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Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Cambria Icefield
The Cambria Icefield is an icefield in the Boundary Ranges of the Coast Mountains in northwestern British Columbia, Canada, located southeast of Stewart. Climate Based on the Köppen climate classification, the Cambria Icefield is located in a subarctic climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the icefield experiences high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Gallery File:Cambria Icefield.jpg, Cambria Icefield File:Bromley Peak.jpg, Bromley Peak and Cambria Icefield File:Mount Camber.jpg, Mount Camber and Cambria Icefield File:Mt. McLeod.jpg, Mount McLeod and Cambria Icefield File:Mount Magee.jpg, Mt. Magee (left) and gl ...
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Boundary Ranges
The Boundary Ranges, also known in the singular and as the Alaska Boundary Range, are the largest and most northerly subrange of the Coast Mountains. They begin at the Nass River, near the southern end of the Alaska Panhandle in the Canadian province of British Columbia and run to the Kelsall River, near the Chilkoot Pass, beyond which are the Alsek Ranges of the Saint Elias Mountains, and northwards into the Yukon Territory flanking the west side of the Yukon River drainage as far as Champagne Pass, north of which being the Yukon Ranges. To their east are the Skeena Mountains and Stikine Plateau of the Interior Mountains complex that lies northwest of the Interior Plateau; the immediately adjoining subregion of the Stikine Plateau is the Tahltan Highland. To their northeast is the Tagish Highland, which is a subregion of the Yukon Plateau. Both highlands are considered in some descriptions as included in the Coast Mountains. The Alexander Archipelago lies offshore and is ...
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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 ...
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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 ...
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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 total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ...
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Strohn Creek
Strohn is an ''Ortsgemeinde'' – a municipality belonging to a '' Verbandsgemeinde'', a kind of collective municipality – in the Vulkaneifel district in Rhineland-Palatinate, Germany. It belongs to the ''Verbandsgemeinde'' of Daun, whose seat is in the like-named town. Geography Location The municipality lies in the Vulkaneifel, a part of the Eifel known for its volcanic history, geographical and geological features, and even ongoing activity today, including gases that sometimes well up from the earth. Strohn lies south of Gillenfeld and the Pulvermaar, a local volcanic crater lake, on the river Alf’s left bank. Constituent communities The following hamlets and homesteads belong to Strohn: Altheck, Buchholz, Dornheck, Herrenbüsch, Sprink, Tannenhof and Trautzberg. Vulcanism The surrounding area is characterized by the Eifel’s vulcanism. Particularly worthy of mention is the Strohner Märchen, a small maar that has almost dried up (''Märchen'' her ...
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Meziadin Lake
Meziadin Lake Provincial Park is a provincial park in 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 .... It sits east of Stewart, British Columbia. ReferencesBC Parks webpage* Provincial parks of British Columbia Nass Country Lakes of British Columbia 1987 establishments in British Columbia Protected areas established in 1987 {{BritishColumbia-park-stub ...
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Bear River Pass
Bears are carnivoran mammals of the family Ursidae. They are classified as caniforms, or doglike carnivorans. Although only eight species of bears are extant, they are widespread, appearing in a wide variety of habitats throughout the Northern Hemisphere and partially in the Southern Hemisphere. Bears are found on the continents of North America, South America, Europe, and Asia. Common characteristics of modern bears include large bodies with stocky legs, long snouts, small rounded ears, shaggy hair, plantigrade paws with five nonretractile claws, and short tails. While the polar bear is mostly carnivorous, and the giant panda feeds almost entirely on bamboo, the remaining six species are omnivorous with varied diets. With the exception of courting individuals and mothers with their young, bears are typically solitary animals. They may be diurnal or nocturnal and have an excellent sense of smell. Despite their heavy build and awkward gait, they are adept runners, climb ...
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Stewart, British Columbia
Stewart is a district municipality at the head of the Portland Canal in northwestern British Columbia, Canada, near the Alaskan panhandle. In 2011, its population was about 494. History The Nisga'a, who live around the Nass River, called the head of Portland Canal , meaning "safe house" or "strong house", probably because it served them as a retreat from the harassment of the Haida and Tlingit from the outer coast. They travelled in the area seasonally to pick berries and hunt birds. It and the rest of the Portland Canal had previously been the domain of the Tsetsaut people, also called the Skam-a-Kounst Indians, or in Nisga'a, an Athapaskan people who became decimated by war and disease and were driven out of the Stewart area by either Haida or Nisga'a in 1856–57. The Portland Canal was first explored and named in July 1793 by Captain George Vancouver in honour of William Cavendish-Bentinck, 3rd Duke of Portland (1738–1808), Home Secretary from 1794 to 1801. Vancouver me ...
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Cornice Mountain (Stikine Icecap)
Cornice Mountain, 1503 m (4931 feet), is a mountain in the Stikine Icecap area of the Boundary Ranges in northwestern British Columbia, Canada. It is located southwest of the confluence of the Flood and Stikine Rivers. See also *Cornice Mountain (Cambria Icefield) Cornice Mountain, , is a mountain in the Cambria Icefield of the Boundary Ranges of the northern Coast Mountains in British Columbia, Canada. The peak is on the north flank of the Cambria Icefield, south of Strohn Creek and between Meziadin La ... * Cornice Ridge References {{coord, 57, 08, 12, N, 131, 57, 03, W, display=title Boundary Ranges Stikine Country ...
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Cornice Ridge
In architecture, a cornice (from the Italian ''cornice'' meaning "ledge") is generally any horizontal decorative Moulding (decorative), moulding that crowns a building or furniture element—for example, the cornice over a door or window, around the top edge of a pedestal, or along the top of an interior wall. A simple cornice may be formed just with a crown, as in crown moulding atop an interior wall or above kitchen cabinets or a bookcase. A projecting cornice on a building has the function of throwing rainwater free of its walls. In residential building practice, this function is handled by projecting gable ends, roof eaves and rain gutter, gutters. However, house eaves may also be called "cornices" if they are finished with decorative moulding. In this sense, while most cornices are also eaves (overhanging the sides of the building), not all eaves are usually considered cornices. Eaves are primarily functional and not necessarily decorative, while cornices have a decorati ...
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