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Skoki Mountain
Skoki Mountain is a mountain located in Banff National Park in Alberta, Canada. It is situated towards the east of the Skoki Valley, at the head of the Red Deer River, and is part of the Slate Range. At the base of the mountain lies Skoki Lodge, a historic ski lodge constructed in 1931, where several routes up to the peak originate. Skoki Mountain was named by James F. Porter in 1911 after the Indian word for marsh or swamp A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in .... References Two-thousanders of Alberta Mountains of Banff National Park {{AlbertaRockies-geo-stub ...
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Slate Range (Alberta)
The Slate Range is a mountain range of the Canadian Rockies, located in Banff National Park, Canada. The range is named after slate, the primary composition of the mountains in the area. The Lake Louise Ski Resort is on the southern slopes of this range. This range includes the following mountains and peaks: See also * Ranges of the Canadian Rockies References

{{Canadian Rockies, state=collapsed Ranges of the Canadian Rockies Mountain ranges of Alberta Mountains of Banff National Park ...
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Alberta
Alberta ( ) is one of the thirteen provinces and territories of Canada. It is part of Western Canada and is one of the three prairie provinces. Alberta is bordered by British Columbia to the west, Saskatchewan to the east, the Northwest Territories (NWT) to the north, and the U.S. state of Montana to the south. It is one of the only two landlocked provinces in Canada (Saskatchewan being the other). The eastern part of the province is occupied by the Great Plains, while the western part borders the Rocky Mountains. The province has a predominantly continental climate but experiences quick temperature changes due to air aridity. Seasonal temperature swings are less pronounced in western Alberta due to occasional Chinook winds. Alberta is the fourth largest province by area at , and the fourth most populous, being home to 4,262,635 people. Alberta's capital is Edmonton, while Calgary is its largest city. The two are Alberta's largest census metropolitan areas. More tha ...
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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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National Topographic System
The National Topographic System or NTS is the system used by Natural Resources Canada for providing general purpose topographic maps of the country. NTS maps are available in a variety of scales, the standard being 1:50,000 and 1:250,000 scales. The maps provide details on landforms and terrain, lakes and rivers, forested areas, administrative zones, populated areas, roads and railways, as well as other man-made features. These maps are currently used by all levels of government and industry for forest fire and flood control (as well as other environmental issues), depiction of crop areas, right-of-way, real estate planning, development of natural resources and highway planning. To add context, land area outside Canada is depicted on the 1:250,000 maps, but not on the 1:50,000 maps. History Topographic mapping in Canada was originally undertaken by many different agencies, with the Canadian Army’s Intelligence Branch forming a survey division to create a more standardized mappi ...
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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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Banff National Park
Banff National Park is Canada's oldest National Parks of Canada, national park, established in 1885 as Rocky Mountains Park. Located in Alberta's Rockies, Alberta's Rocky Mountains, west of Calgary, Banff encompasses of mountainous terrain, with many glaciers and ice fields, dense pinophyta, coniferous forest, and alpine landscapes. The Icefields Parkway extends from Lake Louise, Alberta, Lake Louise, connecting to Jasper National Park in the north. Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast. The main commercial centre of the park is the town of Banff, Alberta, Banff, in the Bow River valley. The Canadian Pacific Railway was instrumental in Banff's early years, building the Banff Springs Hotel and Chateau Lake Louise, and attracting tourists through extensive advertising. In the early 20th century, roads were built in Banff, at times by war internees from Wor ...
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Skoki Valley
Skoki Valley is a valley in Banff National Park in Alberta, Canada near the Town of Lake Louise. The valley is home to many lakes and passes such as Hidden Lake, Ptarmigan Lake and Deception Pass. The valley is popular among backcountry hikers, skiers and climbers because of its untouched snow and views. To accommodate skiers in the 1930s the Skoki Ski Lodge and Halfway Hut were built out of logs by local outfitters. The Red Deer Lakes which are the headwaters of the Red Deer River are located near the valley at the foot of Skoki Mountain Skoki Mountain is a mountain located in Banff National Park in Alberta, Canada. It is situated towards the east of the Skoki Valley, at the head of the Red Deer River, and is part of the Slate Range. At the base of the mountain lies Skoki Lodg .... References Banff National Park Valleys of Alberta {{AlbertaRockies-geo-stub ...
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Red Deer River
The Red Deer River is a river in Alberta and a small portion of Saskatchewan, Canada. It is a major tributary of the South Saskatchewan River and is part of the larger Saskatchewan-Nelson system that empties into Hudson Bay. Red Deer River has a total length of and a drainage area of . Its mean discharge is . The river got its name from the translation of ''Was-ka-soo seepee'' which means "elk river" in the Cree language. "Red deer" was an alternative name for elk, referring to a closely related Eurasian species. Communities located along the Red Deer River include Sundre, Red Deer, Drumheller, and Empress, The city of Brooks, as well as Dinosaur Provincial Park, are also located in the Red Deer River Basin. A glacial flood about 18,000 years ago eroded out a portion of this basin and apparently all or most of the scenic badlands bearing the dinosaur and other Cretaceous fossils. History Joseph Tyrrell discovered a huge coal seam here in 1883, besides large dinosa ...
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Skoki Ski Lodge
The Skoki Ski Lodge National Historic Site of Canada was built in 1930-31 in the Skoki Valley of Canada's Banff National Park. Built by local members of the Ski Club of the Canadian Rockies, the lodge was the first commercial building built specifically to serve skiers in Canada, and possibly in North America. Design and construction work was carried out by local outfitter and builder Earl Spencer with help from Spud White and Victor Kutschera. The lodge was progressively expanded through 1936 by outfitter, guide and log home builder Jim Boyce who was also managing the Lodge the time. It has remained unaltered since that time. The Lodge operates throughout the year. The Skoki Ski Lodge is from the nearest road. The lodge was conceived by Clifford Whyte and Cyril Paris. The first version of the lodge was a single story log building, by . A resting shelter, the Halfway Hut, was built the following year halfway between Skoki and the Lake Louise railway station. A kitchen and two ...
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Ski Lodge
A ski lodge or day lodge is a building located in a ski area that provides amenities such as food, beverages, seating area, restrooms, and locker rooms for skiers and snowboarders. Larger resorts have a day lodge at each base area and also at mid-mountain, summit, or remote locations within the ski area. Ski lodge can also refer to a resort area hotel such as Timberline Lodge in Oregon, or a ski club owned building with meeting space and overnight accommodations for members. Notable ski lodges Notable ski lodges include Skoki Ski Lodge in the Skoki Valley of Alberta, Canada's Banff National Park which was designated a National historic site of Canada in 1992, and the Lake Albina Ski Lodge which overlooks Lake Albina in Kosciuszko National Park in Australia. See also * Mountain hut * Chalet * Jagdschloss References {{reflist Buildings and structures by type Lodge Lodge is originally a term for a relatively small building, often associated with a larger one. Lodge or The ...
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Marsh
A marsh is a wetland that is dominated by herbaceous rather than woody plant species.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p Marshes can often be found at the edges of lakes and streams, where they form a transition between the aquatic and terrestrial ecosystems. They are often dominated by grasses, rushes or reeds. If woody plants are present they tend to be low-growing shrubs, and the marsh is sometimes called a carr. This form of vegetation is what differentiates marshes from other types of wetland such as swamps, which are dominated by trees, and mires, which are wetlands that have accumulated deposits of acidic peat. Marshes provide habitats for many kinds of invertebrates, fish, amphibians, waterfowl and aquatic mammals. This biological productivity means that marshes contain 0.1% of global sequestered terrestrial carbon. Moreover, they have an outsized influence on climate resi ...
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Swamp
A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations.Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammock (ecology), hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerates ...
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