Mount Gould (9,557 ft (2,913 m)) is a peak on the Continental Divide in Glacier National Park, Montana, United States.

It starts from the Highline Trail, which skirts the west side of the peak, and involves some rock scrambling but no technical climbing.

Climbing the sheer East Face of Mount Gould is theoretically possible; however the brittle, loose nature of the rock in Glacier National Park makes the ascent highly technical, unpleasant, and dangerous.

Like the mountains in Glacier National Park, Mount Gould is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

[8] The bulk of the peak is composed of limestone of the Siyeh Formation, and the conspicuous dark band on the east face is a diorite sill.