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The Ice Plug, the 'end' of the cave, was discovered by Mike Boon during a controversial solo trip in the winter of 1970. Soon thereafter cavers helped produce The Longest Cave, a National Film Board production, during which some side passages were explored. The first woman to the Ice Plug at the end of Castleguard Cave was Jane Mulkewich.
Canyon Creek Ice Cave, also known as Bragg Creek Ice Cave or Moose Mountain Ice Cave, is a small ice cave in limestone located in Kananaskis Country near the community of Bragg Creek, Alberta, Canada. Known to natives through prehistory, its 'discovery' is attributed to Stan Fullerton in 1905.
An ice cave is any type of natural cave (most commonly lava tubes or limestone caves) that contains significant amounts of perennial (year-round) ice. At least a portion of the cave must have a temperature below 0 °C (32 °F) all year round, and water must have traveled into the cave’s cold zone.
Booming Ice Chasm is located on the Southern end of the Continental Divide of the Canadian Rockies, in Alberta. [2] [3] It is approximately 150 kilometre south-southwest of Calgary, Alberta and is situated near the summit of Mount Sentry [9] at an elevation of 2200 metres on the south-side ridge. [10]
Alberta: 1,891 220 2,791 Located near Cadomin. Closed in 2010 due to an outbreak of white nose syndrome. Canyon Creek Ice Cave Alberta: 1,769 +89.4 727.12 Located near the town of Bragg Creek. Impassable beyond the first 150m since 1980, due to ice buildup. [3] Castleguard Cave Alberta: 2,016 [3] 384 20,357 Located in Banff National Park. It is ...
The Columbia Icefield is the largest ice field in North America's Rocky Mountains. [1] Located within the Canadian Rocky Mountains astride the Continental Divide along the border of British Columbia and Alberta, Canada, the ice field lies partly in the northwestern tip of Banff National Park and partly in the southern end of Jasper National Park.
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Pages in category "Ice fields of Alberta" The following 4 pages are in this category, out of 4 total. This list may not reflect recent changes. C. Chaba Icefield;
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