Falling Ice Glacier

Falling Ice Glacier sits on the southeastern cliffs of Mount Moran, displaying white and gray patterns against the dark stone face. The glacier is clearly visible from multiple viewpoints across the park, making it an easy landmark to spot when looking at the peaks.

This glacier formed during the Little Ice Age, a period of cooler temperatures that affected mountain regions globally. Since the mid-1800s, it has been shrinking steadily, reflecting changes in regional climate patterns over time.

The glacier shapes how people experience the Teton landscape, serving as a visible reminder of the mountains' natural power and evolution. Its presence anchors the connection between the peaks and the valley below in visitors' minds.

The best views come from the turnouts and overlooks positioned along the main park roads, especially those facing Mount Moran. Clear weather brings out the glacier's colors and details most clearly, so aim for sunny or partly cloudy days when visibility is high.

Meltwater from the glacier feeds directly into Leigh Lake below, creating a hidden water connection between the high peaks and the valley floor. Many visitors walk past this flow without realizing how this glacial system quietly sustains the entire ecosystem of the surrounding area.

Location: Wyoming

GPS coordinates: 43.83333,-110.77028

Latest update: December 14, 2025 18:00