The Salamander Glacier, Ice mass in Glacier National Park, Montana, United States.

The Salamander Glacier is an ice mass on the east side of the Continental Divide at approximately 7,200 feet (2,200 meters), situated on a rocky shelf. The frozen formation rests in an alpine basin surrounded by steep mountain terrain.

The ice mass was originally connected to Grinnell Glacier but separated before 1929 due to substantial retreat in the region. This separation was part of broader changes transforming Montana's high mountain landscape during the 20th century.

Scientists from the United States Geological Survey monitor the glacier to study climate patterns and document changes in Montana's alpine environment.

The best time to visit is between April and October when hiking trails are accessible. The Grinnell Glacier Trail is the main route for viewing the ice mass and departs from the Many Glacier area.

The glacier's name is descriptive: its outline on the rock shelf resembles a salamander. It sits on the east side of the arête on the Continental Divide, and though only about 0.10 mi (0.16 km) long, it is roughly 0.75 mi (1.21 km) wide.