Chaney Glacier, Alpine glacier in Glacier National Park, Montana, US.

Chaney Glacier is an alpine glacier located southeast of Mount Kipp in Glacier National Park's eastern section. It sits on the eastern side of the Continental Divide and remains a key site for monitoring high-altitude ice formations.

The glacier was first documented in 1911 and has changed significantly since its initial recording. Between 1966 and 2005 it lost roughly one-third of its surface area, showing how climate shifts have affected high mountain landscapes.

The U.S. Geological Survey's Glacier Monitoring Research program studies Chaney Glacier using remote sensing equipment and repeat photography, taking images from identical locations periodically to track changes in mass balance.

Chaney Glacier sits in a cirque southeast of Mount Kipp, on the east side of the Continental Divide in Glacier National Park. It is monitored by the U.S. Geological Survey with remote sensing equipment and repeat photography, with images taken periodically from identical locations. Approach is over steep, exposed terrain; the sources give no trail or access details.

The glacier's terminus is shaped by talus piles formed from broken rock and ice. These rocky mounds reveal how the ice continuously shifts and transforms the landscape beneath it.