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The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch 3,000 mi (4,800 km) in straight-line distance from the northernmost part of western Canada, to New Mexico in the southwestern United States. Depending on differing definitions between Canada and the United States, its northern terminus is located either in northern British Columbia's Terminal Range south of the Liard River and east of the Trench, or in the northeastern foothills of the Brooks Range/British Mountains that face the Beaufort Sea coasts between the Canning River and the Firth River across the Alaska-Yukon border. Its southernmost point is near the Albuquerque area adjacent to the Rio Grande Basin and north of the Sandia–Manzano Mountain Range. Being the easternmost portion of the North American Cordillera, the Rockies are distinct from the tectonically younger Cascade Range and Sierra Nevada, which both lie farther to its west.
Banff National Park is Canada's oldest national park, established in 1885. Located in Alberta's Rocky Mountains, 110–180 kilometres (68–112 mi) west of Calgary, Banff encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with many glaciers and ice fields, dense coniferous forest, and alpine landscapes. The Icefields Parkway extends from 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, in the Bow River valley.
Glacier National Park is an American national park located in northwestern Montana, on the Canada–United States border, adjacent to the Canadian provinces of Alberta and British Columbia. The park encompasses more than 1 million acres (4,000 km2) and includes parts of two mountain ranges, more than 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem," a region of protected land encompassing 16,000 square miles (41,000 km2).
Waterton Lakes National Park is a national park located in the southwest corner of Alberta, Canada. It borders Glacier National Park in Montana, United States. Waterton was the fourth Canadian national park, formed in 1895 and named after Waterton Lake, in turn after the Victorian naturalist and conservationist Charles Waterton. Its range is between the Rocky Mountains and prairies. This park contains 505 km2 (195 sq mi) of rugged mountains and wilderness.
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Mount Revelstoke National Park is located adjacent to the city of Revelstoke, British Columbia, Canada. The park is relatively small for a national park, covering 260 km2 (100 sq mi). It is located in the Selkirk Mountains and was founded in 1914. Approximately 600,000 visitors enter Mount Revelstoke and nearby Glacier National Park each year.
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National Park Service rustic – sometimes colloquially called Parkitecture – is a style of architecture that developed in the early and middle 20th century in the United States National Park Service (NPS) through its efforts to create buildings that harmonized with the natural environment. Since its founding in 1916, the NPS sought to design and build visitor facilities without visually interrupting the natural or historic surroundings. The early results were characterized by intensive use of hand labor and a rejection of the regularity and symmetry of the industrial world, reflecting connections with the Arts and Crafts movement and American Picturesque architecture. Architects, landscape architects and engineers combined native wood and stone with convincingly native styles to create visually appealing structures that seemed to fit naturally within the majestic landscapes. Examples of the style can be found in numerous types of National Park structures, including entrance gateways, hotels and lodges, park roads and bridges, visitor centers, trail shelters, informational kiosks, and even mundane maintenance and support facilities. Many of these buildings are listed on the National Register of Historic Places.
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Ainsworth Hot Springs, previously named Ainsworth, is a historic village on Kootenay Lake in British Columbia, Canada and has a population of 20. Founded on May 31, 1883, it is the oldest surviving community on Kootenay Lake. Ainsworth Hot Springs is located on Highway 31, 11 miles (18 km) north of Balfour and 12 miles (19 km) south of Kaslo, British Columbia. Today, Ainsworth Hot Springs and the Cody Caves are a popular destination for tourists and spelunkers.
The Twin Falls Tea House National Historic Site of Canada, located in Yoho National Park, British Columbia as a resting place for hikers and trail riders in the park. The rustic structure is located near Twin Falls in the Little Yoho Valley. The first phase of construction took place about 1908. A separate two-story cabin was built adjoining the original cabin about 1923, and the two structures were linked between 1925 and 1928. Proposed for demolition in 1969, the Tea House was designated a National Historic Site of Canada in 1992, and was extensively renovated in 2005.
The Illecillewaet Glacier is a glacier in British Columbia, Canada. It is located inside Glacier National Park in the Selkirk Mountains, a sub-range of the Columbia Mountains. After the construction of the Canadian Pacific Railway (CPR) near the glacier’s terminus, and the building of a hotel nearby, the glacier became a prominent tourist destination in the Canadian west. Easily accessible by road and railway, it is one of the most-studied glaciers in North America. Its retreat over the last one hundred years has been extensively documented.
References
- 1 2 Morris, Michael. "Nakimu Caves". National Park Feature Articles. Columbia Mountains Institute of Applied Ecology. Retrieved 27 April 2013.
- ↑ Rollins, Jon (2004). Caves of the Canadian Rockies & the Columbian Mountains. Nanoose Bay, BC: Heritage House. pp. 288–289. ISBN 9780921102946.
- ↑ Horne, Greg (September 2005). "Cave Management Guidelines for western mountain national parks of Canada" (PDF).
- ↑ Goodchild, MF; Ford, DC (January 1971). "Analysis of Scallop Patterns by Simulation Under Controlled Conditions". Journal of Geology. 79 (1): 52–62. doi:10.1086/627586. S2CID 129432271.