This high-altitude accumulation of ice and compacted snow is situated on the northern face of a prominent peak within the Big Sky Resort area. Formed by consistent snowfall and cold temperatures, it persists throughout much of the year, sometimes lingering into the summer months. Its location subjects it to specific weather patterns and influences the surrounding microclimate.
The presence of this feature is significant for several reasons. It acts as a crucial water reservoir, slowly releasing meltwater that feeds local streams and supports vegetation. Furthermore, its existence contributes to the unique character of the landscape, attracting adventurous skiers and snowboarders seeking challenging terrain and breathtaking views. Historically, these types of snowfields have played a role in shaping the region’s ecology and recreational opportunities.
