Saskatchewan Glacier, Glacier in Alberta, Canada
Saskatchewan Glacier is a large ice mass that flows from the Columbia Icefield and stretches for about 6 kilometers across the Canadian Rockies. Its surface is marked by deep crevasses and flowing ice patterns that shift continuously throughout the year.
This glacier formed during the last ice age as part of a vast connected ice sheet covering much of the region. It has retreated steadily since the early 1900s, shrinking visibly each year as climate patterns have shifted.
Indigenous peoples of the Rocky Mountains have maintained connections to the Saskatchewan Glacier region through generations of traditional knowledge and practices.
Visit only with proper equipment and an experienced guide, as hidden crevasses and unstable ice make independent exploration dangerous. The best time to go is during warmer months when conditions are more stable and hazards are easier to spot.
Meltwater from this glacier feeds multiple river systems that flow in different directions toward distant oceans. This hidden role as a water source is surprising to many visitors who see it mainly as a scenic landmark.
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