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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.
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.
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.
The mountain was named in 1898 by J. Norman Collie because its permanently snow and ice-capped massif resembles a dome. [1] The mountain is one of two hydrological apexes of North America; it is a major triple divide between three great drainage basins.
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.
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Bow Glacier is located in Banff National Park, Alberta, Canada, approximately 37 km (23 mi) northwest of Lake Louise. It can be viewed from the Icefields Parkway. Bow Glacier is an outflow glacier from the Wapta Icefield, which rests along the Continental Divide. Runoff from the glacier supplies water to Bow Lake and the Bow River.
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