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Watermelon Peak
Watermelon Peak is a summit located in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Deluc Peak, to the east. __NOTOC__ History Watermelon Peak was named in 1966 by William L. Putnam, member of the first ascent party, which carried a four-kilogram watermelon to the summit, and consumed it there. The July 1966 first ascent party included David Michael, W.V.G. Matthews, William L. Putnam, M. Stearns, and L.R. Wallace. However, the name is not officially recognized by the Geographical Names Board of Canada.The peak is not listed in the Canadian Geographical Names Database. Geology Like other mountains in Banff Park, Watermelon 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, Watermelon Peak is located in a subarctic cli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canadian Rockies
The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico. Canada officially defines the Rocky Mountains system as the mountain chains east of the Rocky Mountain Trench extending from the Liard River valley in northern British Columbia to the Albuquerque Basin in New Mexico, not including the Mackenzie, Richardson and British Mountains/Brooks Range in Yukon and Alaska (which are all included as the "Arctic Rockies" in the United States' definition of the Rocky Mountains system). The Canadian Rockies, bein ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Observation Peak (Alberta)
Observation Peak is a mountain summit located in Banff National Park, Alberta, Canada. The mountain can be seen from the Icefields Parkway near the Bow Summit. The peak was named in 1898 by Charles L. Noyes, a Boston clergyman, who upon climbing to the top found it to have the best viewpoint he had ever reached. The mountain can be scrambled using the western slopes and after reaching the top of the false summit, a 20-minute plod to the northwest leads to the true summit about higher. 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 classification, Observation Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque Peak (Alberta)
Cirque Peak is a mountain, peak located directly west of Dolomite Pass in the Bow River, Bow River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. The mountain forms a cirque, hence the name. Scrambling Route The scrambling route (rated easy) begins just beyond Helen Lake which can be reached by following the Helen Lake/Dolomite Pass trail 6 km from the trail head beside the Icefields Parkway. From the lake, follow the trail into Dolomite Pass and then choose a line up the peak. Geology Like other mountains in Banff Park, Cirque 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, Cirque Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite Peak
__NOTOC__ Dolomite Peak is a mountain summit located in the Bow River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Cirque Peak, to the northwest. Dolomite Peak can be seen from the Icefields Parkway with its distinctive crags and colorful towers that are a mixture of dolomite and limestone. Dolomite is rare in the Rockies and is stronger than limestone. History Dolomite Peak was named in 1897 by Charles E. Fay, Norman Collie, and Charles Thompson for its resemblance to the Dolomites of the Italian Alps. The mountain's name became official in 1924 by the Geographical Names Board of Canada. The first ascent of Dolomite Peak was made in 1930 by J. Monroe Thorington, with Peter Kaufmann (as guide). Geology Like other mountains in Banff Park, Dolomite 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Rocky Mountains
The geology of the Rocky Mountains is that of a discontinuous series of mountain ranges with distinct geological origins. Collectively these make up the Rocky Mountains, a mountain system that stretches from Northern British Columbia through central New Mexico and which is part of the great mountain system known as the North American Cordillera. The rocky cores of the mountain ranges are, in most places, formed of pieces of continental crust that are over one billion years old. In the south, an older mountain range was formed 300 million years ago, then eroded away. The rocks of that older range were reformed into the Rocky Mountains. The Rocky Mountains took shape during an intense period of plate tectonic activity that resulted in much of the rugged landscape of the western North America. The Laramide orogeny, about 80–55 million years ago, was the last of the three episodes and was responsible for raising the Rocky Mountains. Subsequent erosion by glaciers has created the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Alberta
Alberta is one of the thirteen provinces and territories of Canada. Located in Western Canada, the province has an area of and is bounded to the south by the United States state of Montana along 49° north for ; to the east at 110° west by the province of Saskatchewan for ; and at 60° north the Northwest Territories for . The southern half of the province borders British Columbia along the Continental Divide of the Americas on the peaks of the Rocky Mountains, while the northern half borders British Columbia along the 120th meridian west. Along with Saskatchewan it is one of only two landlocked provinces or territories. Terrain Alberta's landscape is marked by the impact of the Wisconsin Glaciation, about 75,000 to 11,000 years ago, when the entire future province was covered in ice. As the ice sheet receded, the landscape was changed, and large amounts of glacial till were left behind. The southern portion consists chiefly of plains that are almost entirely treeless. As ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In The Canadian Rockies
A list of highest peaks in the Canadian Rockies is shown below: References ;Notes {{reflist, group=notes *• Canadian Rockies The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part ... Mountains, Rockies Mountains, Rockies ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saskatchewan River
The Saskatchewan River (Cree: ''kisiskāciwani-sīpiy'', "swift flowing river") is a major river in Canada. It stretches about from where it is formed by the joining together of the North Saskatchewan and South Saskatchewan Rivers to Lake Winnipeg. It flows roughly eastward across Saskatchewan and Manitoba to empty into Lake Winnipeg. Through its tributaries the North Saskatchewan and South Saskatchewan, its watershed encompasses much of the prairie regions of Canada, stretching westward to the Rocky Mountains in Alberta and north-western Montana in the United States. Including its tributaries, it reaches to its farthest headwaters on the Bow River, a tributary of the South Saskatchewan in Alberta. Description It is formed in central Saskatchewan, approximately east of Prince Albert, by the confluence of its two major branches, the North Saskatchewan and the South Saskatchewan, at the Saskatchewan River Forks. Both source rivers originate from glaciers in the Alberta Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Siffleur River
The Siffleur River is a short river rising in the Canadian Rockies in western Alberta. The Siffleur River is an early tributary of the North Saskatchewan River. The river begins between Devon Mountain and Clearwater Mountain, at Clearwater Pass. The Siffleur is then joined by Dolomite Creek (flowing from Isabella Lake), and the Escarpment River. After plummeting over Siffleur Falls, the Siffleur River joins the North Saskatchewan River before Lake Abraham Abraham Lake, also known as Lake Abraham, is an artificial lake and Alberta's largest reservoir. It is located in the " Kootenay Plains area of the Canadian Rockies' front range", on the North Saskatchewan River in western Alberta, Canada. Descr ....Mussio Ventures. ''Southwestern Alberta Backroad Mapbook.'' Burnaby: Backroad Mapbooks (2004) Like the Siffleur Wilderness Area and Siffleur Mountain, the river's name was chosen by James Hector in 1858 for the shrill whistles of the marmot which inhabit the area ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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