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Ptarmigan Lake (Alberta)
Ptarmigan Lake is an alpine lake at the foot of Ptarmigan Peak. Several backcountry campgrounds are situated near the lake, as well as the 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 spe ... just over Deception Pass. The main access to the lake is a trail near the Lake Louise Mountain Resort. The lake drains into the Bow River via the Skoki Valley. References Lakes of Alberta Banff National Park {{AlbertaRockies-geo-stub ...
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Ptarmigan Peak (Alberta)
Ptarmigan Peak is a mountain, peak located beside Pika Peak in Banff National Park, Alberta, Canada. The mountain was named in 1909 by J.W.A. Hickson after he found several rock ptarmigan, ptarmigan in the meadows below the peak. Hickson also made the first ascent guided by Edward Feuz jr. The Lake Louise Mountain Resort is developed on the southern slopes of the Merlin Ridge, which includes Mount Richardson (Alberta), Mount Richardson, Ptarmigan Peak, Pika Peak. A backcountry campground is located at the foot of the mountain, near Hidden Lake (Alberta), Hidden Lake. Routes The scrambling route is via southern slopes starting from Hidden Lake (Alberta), Hidden Lake. Geology Like other mountains in Banff Park, the mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate Based on the Köppen climate classif ...
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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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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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Alpine Lake
Alpine lakes are classified as lakes at high altitudes in mountainous zones, usually near or above the tree line, with extended periods of ice cover. These lakes are commonly formed from glacial activity (either current or in the past) but can also be formed from geological processes such as volcanic activity or landslides. Many alpine lakes that are fed from glacial melt have the characteristic bright turquoise or green color as a result of glacial flour, suspended minerals derived from a glacier scouring the bedrock. When active glaciers are not supplying water to the lake, such as a majority of alpine lakes of the Rocky Mountains in the U.S., the lakes may still be bright blue due to the lack of algae growth resulting from cold temperatures, lack of nutrient run-off from surrounding land, and lack of sediment input. The coloration and mountain locations of alpine lakes attract lots of recreational activity. Alpine lakes are some of the most abundant types of lakes on Earth. In ...
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Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ...
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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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Fossil Mountain Seen From Ptarmigan Lake
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the a ...
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Alpine Lake
Alpine lakes are classified as lakes at high altitudes in mountainous zones, usually near or above the tree line, with extended periods of ice cover. These lakes are commonly formed from glacial activity (either current or in the past) but can also be formed from geological processes such as volcanic activity or landslides. Many alpine lakes that are fed from glacial melt have the characteristic bright turquoise or green color as a result of glacial flour, suspended minerals derived from a glacier scouring the bedrock. When active glaciers are not supplying water to the lake, such as a majority of alpine lakes of the Rocky Mountains in the U.S., the lakes may still be bright blue due to the lack of algae growth resulting from cold temperatures, lack of nutrient run-off from surrounding land, and lack of sediment input. The coloration and mountain locations of alpine lakes attract lots of recreational activity. Alpine lakes are some of the most abundant types of lakes on Earth. In ...
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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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Lake Louise Mountain Resort
The Lake Louise Ski Resort & Summer Gondola is a ski resort in western Canada, located in Banff National Park near the village of Lake Louise, Alberta. Located west of Banff, Lake Louise is one of three major ski resorts within Banff National Park. The resort is situated on the southern slopes of the Slate Range, between the heights of Mount Richardson, Ptarmigan Peak, Pika Peak and Redoubt Mountain, all around above sea level. The base of the slopes is defined by Pipestone River, a tributary of the Bow River, immediately north of the intersections between Highway 1A (Bow Valley Trail), Highway 1 (Trans-Canada Highway), and Highway 93 (Icefields Parkway). History Lake Louise has been a home to skiing since the 1920s, as the gateway to the Skoki Ski Lodge. The first lift was constructed in 1954, and a poma was added in 1960. Until autumn 2008, the ski resort was owned and operated by the Resorts of the Canadian Rockies (RCR) company. In 2008, Charlie Locke, a former ...
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Bow River
The Bow River is a river in Alberta, Canada. It begins within the Canadian Rocky Mountains and winds through the Alberta foothills onto the prairies, where it meets the Oldman River, the two then forming the South Saskatchewan River. These waters ultimately flow through the Nelson River into Hudson Bay. The Bow River runs through the city of Calgary, taking in the Elbow River at the historic site of Fort Calgary near downtown. The Bow River pathway, developed along the river's banks, is considered a part of Calgary's self-image. First Nations made varied use of the river for sustenance before settlers of European origin arrived, such as using its valleys in the buffalo hunt. The name ''Bow ''refers to the reeds that grew along its banks and were used by the First Nations to make bows; the Blackfoot language name for the river is , meaning "river where bow reeds grow". The river is an important source of water for irrigation and drinking water. Between the years 1910 and 1 ...
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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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