Chaney Glacier

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 maintains detailed photographic records of Chaney Glacier, contributing to scientific understanding of climate effects on alpine environments.

Reaching the glacier is challenging because the terrain is steep and heavily exposed. Visitors need professional guidance and specialized equipment to approach the site safely.

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.