Traleika Glacier

Traleika Glacier is a large expanse of ice in Denali that flows from surrounding peaks and splits into two major branches before joining forces. As the streams merge, they eventually connect with the Muldrow Glacier system, creating a unified flow of ice moving downslope.

Bradford Washburn named this glacier in 1945 after a Susitna term meaning 'great one' or 'high one'. This naming was part of Washburn's systematic mapping work across Alaska's mountain ranges during that period.

The name comes from the Dena'ina word Dghelaay Ka'a, showing how indigenous peoples shaped the way this place is called and understood. Visitors walking through this landscape connect with that long cultural presence.

Exploring this glacier requires mountaineering experience and specialized gear, as it is remote and challenging terrain. Plan your visit during warmer months when conditions are more favorable, but always arrange professional guidance for safety.

The western fork drops dramatically through the Traleika Icefall, where ice breaks into jagged blocks and deep crevasses as it descends steeply. This turbulent, craggy section creates a striking visual spectacle for those able to reach it.