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Bow Hut
The Bow Hut is an alpine hut located at an elevation of on the eastern edge of the Wapta Icefield in Banff National Park. It is the largest, best equipped, and most accessible of the four alpine huts on the Wapta Icefield, and serves as the base for a wide variety of ski tours and mountaineering ascents to half a dozen peaks on the Wapta. It is the easiest and safest starting point for the Wapta traverse; and Balfour Hut, the next hut on the traverse, can easily be reached from it in a day. It can also serve as an intermediate stop in a longer traverse which starts at the less easily accessible Peyto Hut. The hut is maintained by the Alpine Club of Canada. The hut sleeps 30 and is equipped with propane powered lamps and stovetop, and a wood stove for heating. There are two indoor drum toilets. History The original Bow Hut was built in 1968 by a group led by Peter Fuhrmann, who later became president of the Alpine Club of Canada from 1984 to 1988, and was funded by Peter and ...
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Wapta Icefield
The Wapta Icefield is located on the Continental Divide in the Waputik Mountains of the Canadian Rockies, in the provinces of British Columbia and Alberta. The icefield is shared by Banff and Yoho National Parks and numerous outlet glaciers extend from the icefield, including the Vulture, Bow and Peyto Glaciers. Runoff from the icefields and outlet glaciers supply water to both the Kicking Horse and Bow Rivers, as well as numerous streams and lakes. The icefield is one of the most studied in the Canadian Rockies and all evidence supports the conclusion that the icefield is shrinking in area, especially near the lowest altitudes of its outlet glaciers, including Peyto Glacier, in which the glacier has become both shorter in length and thinner in thickness. In the 1980s the icefield covered an area of approximately . The icefield is easily accessible by mountaineers in both the summer and winter. Both ski trips in the winter and glacier hiking trips in the summer often combine a ...
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Bow Lake (Alberta)
Bow Lake is a small lake in western Alberta, Canada. It is located on the Bow River, in the Canadian Rockies, at an altitude of 1920 m. The lake lies south of the Bow Summit, east of the Waputik Range (views including Wapta Icefield, Bow Glacier, Bow Peak, Mount Thompson (Alberta), Mount Thompson, Crowfoot Glacier and Crowfoot Mountain) and west of the Dolomite Pass, Dolomite Peak and Cirque Peak. Bow Lake is one of the lakes that line the Icefields Parkway in Banff National Park and Jasper National Park, other such lakes being Hector Lake, Lake Louise, Alberta, Lake Louise, Peyto Lake, ''Mistaya Lake'', ''Waterfowl Lakes'', ''Chephren Lake'' and ''Sunwapta Lake''. Historical Simpson's Num-Ti-Jah Lodge is located on the shores of Bow Lake at the foot of Mount Jimmy Simpson.Tim Whyte Bow Lake is the closest lake to the headwaters of Bow River, and has a total area of 3.21 km2. Water in the lake is meltwater of the Bow Glacier and its turquoise colouring is due to Till, glaci ...
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1968 Establishments In Alberta
The year was highlighted by protests and other unrests that occurred worldwide. Events January–February * January 5 – "Prague Spring": Alexander Dubček is chosen as leader of the Communist Party of Czechoslovakia. * January 10 – John Gorton is sworn in as 19th Prime Minister of Australia, taking over from John McEwen after being elected leader of the Liberal Party the previous day, following the disappearance of Harold Holt. Gorton becomes the only Senator to become Prime Minister, though he immediately transfers to the House of Representatives through the 1968 Higgins by-election in Holt's vacant seat. * January 15 – The 1968 Belice earthquake in Sicily kills 380 and injures around 1,000. * January 21 ** Vietnam War: Battle of Khe Sanh – One of the most publicized and controversial battles of the war begins, ending on April 8. ** 1968 Thule Air Base B-52 crash: A U.S. B-52 Stratofortress crashes in Greenland, discharging 4 nuclear bombs. * January 23 ...
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Mountain Huts In Canada
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 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 isolated summits, but most occur in mountain ranges. Mountains are formed through 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 slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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Peter And Catharine Whyte Hut
The Peter and Catharine Whyte Hut, also known as the Peyto Hut, is an alpine hut located on the northern tip of the Wapta Icefield in Banff National Park. It is nicknamed the Peyto hut due to its proximity on the Peyto Glacier. The hut is maintained by the Alpine Club of Canada. The hut sleeps 18 in the summer and 16 in the winter. It is equipped with propane powered lamps and stovetop. There is a single outdoor drum toilet at this facility. Hut access requires approximately 6 to 8 hours of travel {{cite web , url=http://www.alpineclubofcanada.ca/facility/info/PeytoHut.pdf , title=Archived copy , accessdate=2011-08-04 , url-status=dead , archiveurl=https://web.archive.org/web/20110928130634/http://www.alpineclubofcanada.ca/facility/info/PeytoHut.pdf , archivedate=2011-09-28 Petyo Hut Information including at least an hour of glacier travel to get to from Peyto Lake, or 6 to 8 hours of glacier travel from the Bow Hut. Nearby * Peyto Lake * Peyto Glacier * Wapta Icefield ...
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Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Proven ...
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Saint Nicholas Peak (Canada)
Saint Nicholas Peak is a mountain summit in the Rocky Mountains of Canada. It is located on the Continental Divide, on the Alberta-British Columbia border, in both Banff National Park and Yoho National Park. It lies at the eastern edge of the Wapta Icefield, and is part of the Waputik Mountains which are a sub-range of the Canadian Rockies. Name It was named in 1916 by Arthur O. Wheeler; a particular gendarme on the mountain is said to resemble Santa Claus. Geology The peak 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 classification, it is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below -20 C with wind chill factors below -30 C. Gallery Mountain in the Canada Rockies.jpg, Saint Nicholas Peak Saint Nicholas Peak and Bow ...
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Icefields Parkway
Highway 93 is a north–south highway in Alberta, Canada. It is also known as the Banff-Windermere Parkway south of the Trans-Canada Highway ( Highway 1) and the Icefields Parkway north of the Trans-Canada Highway. It travels through Banff National Park and Jasper National Park and is maintained by Parks Canada for its entire length. It runs from the British Columbia border at Vermilion Pass in the south, where it becomes British Columbia Highway 93, to its terminus at the junction with the Yellowhead Highway ( Highway 16) at Jasper. The route takes its number from U.S. Route 93, which runs uninterrupted south to central Arizona, and was initially designated as '93' in 1959. Route description Banff-Windermere Highway The southern portion of the route is part of the Banff-Windermere Highway, a highway that travels from British Columbia Highway 95 at Radium Hot Springs, through Kootenay National Park and Vermilion Pass across the Continental Divide, ...
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Lake Louise, Alberta
Lake Louise is a hamlet within Banff National Park in Alberta, Canada. Named after Princess Louise, Duchess of Argyll, it lies in Alberta's Rockies on the Bow River, northeast of the lake that shares its name. Initially settled in 1884 as an outpost for the Canadian Pacific Railway, Lake Louise sits at an elevation of , making it Canada's highest community. The nearby lake, framed by mountains, is one of the most famous mountain vistas in the world; the famous Chateau Lake Louise also overlooks the lake. History Prior to the arrival of Europeans, Indigenous peoples lived in the foothills and forests of the Rocky Mountains - including what is today Lake Louise, where they hunted bison and other big game animals. In the Stoney language of the Nakoda people the area is called , meaning "lake of the little fishes". During the 1870s, the construction of the Canadian Pacific Railway (CPR) started. The railway was planned to run through Bow Valley. A Nakoda guide took CPR workman ...
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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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Headwater
The headwaters of a river or stream is the farthest place in that river or stream from its estuary or downstream confluence with another river, as measured along the course of the river. It is also known as a river's source. Definition The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly known as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri—lower Mississippi length figure in lists of lengths of rivers around the world. Most rivers have numerous tributaries and change names often; it is customary to regard the longest t ...
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