Athabasca Glacier flowing from the Columbia Icefield in Jasper National Park, surrounded by snow-covered mountains and rocky foreground terrain

    Athabasca Glacier descending from the Columbia Icefield, framed by rugged alpine slopes and glacial meltwater in Jasper National Park, Canada

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    Columbia Icefield

    Glacier

    The Columbia Icefield is one of the largest non-polar icefields in North America, straddling the Continental Divide in the Canadian Rockies. Multiple outlet glaciers are visible from the Icefields Parkway. The composition resolves through the vast ice surface set against mountain ridgelines.

    52.21900, -117.22700

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    Gallery

    Athabasca Glacier flowing between snow-covered peaks within the Columbia Icefield in Jasper National Park, Alberta, Canada.

    The Athabasca Glacier descends from the Columbia Icefield into a broad alpine va…

    Visitors walking on the Columbia Icefield Skywalk overlooking glacier valleys in Jasper National Park, Alberta, Canada

    A glass-floored Skywalk extends over the Sunwapta Valley with views toward the C…

    Athabasca Glacier flowing between snow-covered peaks in Jasper National Park, Alberta, Canada

    The broad icy surface of Athabasca Glacier stretches down from the Columbia Icef…

    Melting glacier edge flowing into turquoise meltwater lake at the Columbia Icefield in Jasper National Park, Alberta, Canada

    Meltwater pools form along the retreating ice at the Columbia Icefield, revealin…

    Athabasca Glacier flowing from the Columbia Icefield in Jasper National Park, surrounded by snow-covered mountains and rocky foreground terrain

    Athabasca Glacier descending from the Columbia Icefield, framed by rugged alpine…

    Quick Facts

    Access

    Roadside / Step-out

    5–15 min

    Elevation Gain

    20 m

    Best Light

    Golden Hour
    Overcast

    Diffused light preserves detail across the ice surface while low sun defines surrounding mountain structure and glacier contours.

    Why This Light

    Softens Contrast
    Low-Angle Relief

    Season

    Seasonally Distinct

    The icefield remains present year-round, with seasonal snow cover altering surface texture and contrast between ice and surrounding rock.

    Crowds

    Often Busy

    Restrictions

    Fee Common

    Roadside access via Icefields Parkway with designated viewpoints and visitor centre; guided glacier access requires permits or tours.

    Photography Notes

    Photographs are typically made from roadside viewpoints and designated viewing areas where the glacier surface and surrounding peaks form layered compositions. Small shifts in position change how ice textures align with the mountain backdrop and affect depth across the scene.
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