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Tunnel Mountain, also known as Sleeping Buffalo (Siksiká: Iinii Istako; Nakoda: Eyarhey Tatanga Woweyahgey Wakân), is a mountain located in the Bow River Valley of Banff National Park in Alberta, Canada at the junction of the Spray River with the Bow and overlooking the Hot Springs on Sulphur Mountain.
Banff National Park is Canada's first national park, established in 1885 as Rocky Mountains Park.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) [3] of mountainous terrain, with many glaciers and ice fields, dense coniferous forest, and alpine landscapes.
Mount Rundle is a mountain in Canada's Banff National Park overlooking the towns of Banff and Canmore, Alberta.The Cree name was Waskahigan Watchi or house mountain. [Notes 1] [1] [failed verification] In 1858 John Palliser renamed [1] the mountain after Reverend Robert Rundle, a Methodist invited by the Hudson's Bay Company to do missionary work in western Canada in the 1840s.
S. Saddle Mountain (Alberta) Saint Nicholas Peak (Canada) Mount Sarbach; Mount Saskatchewan (Alberta) Sawback Range; Scarab Peak (Canada) Mount Shark; Silverhorn Mountain
The Cave and Basin National Historic Site of Canada is located in the town of Banff, Alberta, within the Canadian Rocky Mountains, at the site of natural thermal mineral springs around which Canada's first national park, Banff National Park, was established.
National parks of Canada are vast natural spaces located throughout the country that are protected by Parks Canada, a government agency.Parks Canada manages the National Parks and Reserves in order to protect and preserve the Canadian wildlife and habitat that fall within the ecosystems of the park, keep them safe, educate visitors, and ensure public enjoyment in ways that do not compromise ...
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The Tunnel Mountain Formation is present in the front ranges of the Canadian Rockies of western Alberta, and reaches a maximum thickness of about 200 metres (600 ft). It unconformably overlies the Etherington Formation or the Todhunter Formation of the Mississippian Rundle Group, and is conformably overlain by the Late Pennsylvanian Kananaskis Formation.
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