Sermilik Glacier

Sermilik Glacier flows through the southern Byam Martin Mountains within Sirmilik National Park, creating a sprawling ice field marked by crevasses and ice formations. The frozen mass covers a substantial area and connects adjacent mountain regions.

This glacier developed over thousands of years through continuous snow accumulation and compression in the Arctic mountains. Its current form reflects the long-term climate patterns of the high north.

The Inuit population has maintained deep connections with this glacial territory, incorporating its presence into their traditional hunting and navigation practices.

Access requires a permit from Sirmilik National Park and proper equipment for extreme cold and rough terrain. Visitors should consult with park rangers about safe routes and current conditions.

The glacier sits at such a high latitude that the sun remains above the horizon throughout summer and disappears entirely for months in winter. These extreme lighting conditions dramatically shape how visitors perceive the landscape.