Banff National Park

© RicardMN Photography

© RicardMN Photography

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© RicardMN Photography

© RicardMN Photography

Canvas, framed, acrylic and metal prints / Art prints / Greeting cards / Phone cases / Throw pillows

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Banff National Park is Canada’s oldest national park, established in 1885 in the Rocky Mountains.

The park, located 110–180 kilometres (68–112 mi) west of Calgary in the province of Alberta, encompasses 6,641 square kilometres (2,564 sq mi) of mountainous terrain, with numerous 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.

Over the past few million years, glaciers have at times covered most of the park, but today are found only on the mountain slopes though they include the Columbia Icefield, the largest uninterrupted glacial mass in the Rockies. Erosion from water and ice have carved the mountains into their current shapes.

Johnston Creek is a tributary of the Bow River in Canada’s Rocky Mountains. The creek is located in Banff National Park.

Johnston Creek originates north of Castle Mountain in a glacial valley southwest of Badger Pass and south of Pulsatilla Pass, at an elevation of 2,500 meters (8,200 ft). The creek flows southeast between Helena Ridge and the Sawback Range, and then south through a gorge known as Johnston Canyon. The stream empties into the Bow River, south of Castle Mountain, between Banff and Lake Louise, at an elevation of 1,440 meters (4,720 ft).

As Johnston Creek approaches the Bow River, it flows through a large canyon formed by erosion over thousands of years. The creek has cut through the limestone rock to form sheer canyon walls, as well as waterfalls, tunnels, and pools.

A popular hiking trail follows the canyon and leads to a meadow within the Johnston Valley above the canyon. The first part of the trail consists of a constructed walkway with safety rails and bridges, while the last part of the trail is natural and more rugged. Within the meadow are the Ink Pots, which are six blue-green spring-fed pools.

Ice climbing is a popular activity on the frozen waterfalls in winter. (Description from Wikipedia).

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Hong Hing Mural Detail

© RicardMN Photography

© RicardMN Photography

Detail of the Hong Hing Waterfront Store mural, Chemainus, Vancouver Island, BC, Canada. It was painted by Paul Marcano.

The Hong Hing text panel says: “Hong Hing was actually the name of his store, his real name being Fong Yen Lew. After a half-century career as a shopkeeper, second-hand dealer, bootlegger, gambling house, and general busboy he returned to China, presumably to die. Instead, he married a woman forty years his junior, who presented him with an heir before old Hong joined his ancestors.”

Chemainus is a community on the east coast of Vancouver Island, British Columbia, Canada.

Founded as a logging town in 1858, the town is now famous for its 39 outdoor murals. This outdoor gallery has given birth to many businesses, including a theatre, antiques dealers, and eateries. The tourist industry stemming from the murals helped rejuvenate the town after its large sawmill closed in the early 1980s and was replaced by a smaller but far more efficient mill.

The name “Chemainus” comes from the native shaman and prophet “Tsa-meeun-is” (Broken Chest). Legend says that the man survived a massive wound in his chest to become a powerful chief. His people took his name to identify their community, the Stz’uminus First Nation, formerly the Chemainus Indian Band.

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Moraine Lake, Alberta, Canada

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© RicardMN Photography

Moraine Lake is a glacially-fed lake in Banff National Park, 14 kilometres (8.7 mi) outside the Village of Lake Louise, Alberta, Canada. It is situated in the Valley of the Ten Peaks, at an elevation of approximately 6,183 feet (1,885 m). The lake has a surface area of .5 square kilometres (0.19 sq mi).
The lake, being glacially fed, does not reach its crest until mid to late June. When it is full, it reflects a distinct shade of blue. The color is due to the refraction of light off the rock flour deposited in the lake on a continual basis.

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Canadian Rockies

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B&W photographs of Canadian Rockies by RicardMN Photography. (See in 480p)
Music: Dream On – Aerosmith
The Canadian Rockies comprise the Canadian segment of the North American Rocky Mountains range. They are the eastern part of the Canadian Cordillera, extending from the Interior Plains of Alberta to the Rocky Mountain Trench of British Columbia. The southern end borders Idaho and Montana of the USA. The northern end is at the Liard River in northern British Columbia.

The Canadian Rockies have numerous high peaks and ranges, such as Mount Robson (3,954 m (12,972 ft)) and Mount Columbia (3,747 m (12,293 ft)). The Canadian Rockies are composed of shale and limestone. Much of the range is protected by parks and a World Heritage Site.

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