Peyto Glacier is located in the
Canadian Rockies in
Banff National Park,
Alberta,
Canada, approximately 90 km (56 miles) northwest of the town of
Banff, and can be accessed from the
Icefields Parkway. Peyto Glacier is an outflow glacier from the
Wapta Icefield, which rests along the
Continental divide. The glacier snout is subject to high melt rates from season to season and there is marked surface lowering on several parts of the glacier. Glacial
silt, which is carried from the glacier by streams, ensures a turquoise appearance to
Peyto Lake, a popular tourist destination. As is true for the vast majority of glaciers worldwide, Peyto Glacier has been retreating rapidly, especially since the last half of the 20th century, and has reportedly lost 70% of its mass since it was first researched (Demuth and Keller, 2006). In 1987, an automatic weather station was constructed near the glacier that monitors temperature changes, radiation, and precipitation
Peyto Glacier provides the most direct access to
Peyto Hut, a base of both summer and winter mountaineering.
See also
References
- Demuth, M.N. and R. Keller, 2006. An assessment of the mass balance of Peyto Glacier (1966–1995) and its relation to recent and past century climatic variability. In – , M.N. Demuth, D.S. Munro and G.J. Young Eds. National Hydrology Research Institute Science Report 8: 83-132.
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