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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.
In the 1980s the icefield covered an area of approximately 80 km 2 (30 sq mi). The glaciers popular with climbers [ 3 ] accessible in both summer and winter. Both ski trips in the winter and glacier hiking trips in the summer often combine a traverse of this icefield with a trip across the Waputik Icefield directly to the south.
Booming Ice Chasm is an ice cave, located in the Crowsnest Pass area [1] of the Rocky Mountains in Alberta, Canada. [2] [3]The entrance to Booming Ice Chasm was initially found by accident by members of the Alberta Speleological Society while attempting to reach a different cave in June, 2008.
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.
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;
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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The Saskatchewan Glacier is located in Banff National Park, Alberta, Canada, approximately 120 km (75 mi) northwest of the town of Banff, and can be accessed from the Icefields Parkway. Saskatchewan Glacier is the largest outflow glacier from the Columbia Icefield , which rests along the Continental Divide .
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