A prominent, high-elevation accumulation of perennial ice and snow situated on the northernmost peak within the Big Sky, Montana region. Such features are often formed by consistent snowfall and cold temperatures, allowing snow to persist through warmer months, contributing to the local hydrology and landscape.
These snow formations play a vital role in maintaining streamflow during summer months, impacting local ecosystems and water resources. Historically, these areas have served as landmarks for navigation and, increasingly, are studied for their climate change implications. Their presence also influences the types of vegetation and wildlife that can thrive in the surrounding area.