Peyto Glacier

Peyto Glacier is a large ice mass in the Canadian Rocky Mountains that stretches along the Continental Divide as part of the Wapta Icefield. The ice sits at high elevation and feeds streams that flow down into the valley below.

The glacier was first documented scientifically in 1896 when Walter D. Wilcox photographed it during an expedition. This early record shows how the ice has changed its appearance over the decades that followed.

Scientists from around the world come here to study how climate change affects glaciers and ice movement. This research work has made the site important for understanding how glaciers behave and change.

The glacier can be reached from the Icefields Parkway via a marked trail that has parking and information panels. It is wise to bring proper hiking gear and be ready for the cold, open mountain conditions at high altitude.

The glacier feeds Peyto Lake with mineral-rich meltwater that gives the lake a bright turquoise color. This striking hue is especially visible during the warmer months when snowmelt is at its peak.

Location: Alberta

GPS coordinates: 51.67810,-116.54700

Latest update: December 10, 2025 16:25