Runoff from the Athabasca Glacier in Jasper National Park, Alberta, Canada
The Athabasca Glacier is one of the six principal 'toes' of the Columbia Icefield, located in the Canadian Rockies. The glacier currently recedes at a rate of 20-30 metres per year and has receded more than 1.5 km in the past 125 years and lost over half of its volume. The glacier moves down from the icefield at a rate of several centimetres per day. Due to its close proximity to the Icefields Parkway, between the Alberta towns of Banff and Jasper, and rather easy accessibility, it is the most visited glacier in North America.
- Jasper-Runoff from the Athabasca Glacier-001.tif
- ©Ken Kaminesky
- Image Size
- 5616x3744 / 60.2MB
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