Cloudcroft Peaks

Cloudcroft Peaks is a summit in the Lewis Range within Glacier National Park, rising to approximately 2,700 meters. The slopes reveal layered sedimentary rock formations, while higher elevations open into alpine meadows with low-growing plants and flowering cushions.

The mountain formed through the Lewis Overthrust event approximately 170 million years ago, when ancient rock layers were pushed from below over younger formations. This massive crustal movement shaped the entire Lewis Range and created the geological foundation of the landscape visible today.

The region held deep importance for Indigenous peoples as a hunting and gathering area long before the park existed. Visitors walking through these mountains can sense how the landscape shaped the lives and traditions of those who came here.

Conditions here change rapidly, and hikers should prepare for extreme temperature swings, particularly in winter when it drops below freezing. Good footwear, layered warm clothing, and plenty of water are necessary no matter the season.

From the summit, views extend to two neighboring peaks that stand like sentinels of the region, clearly visible on clear days in full detail. This vista reveals the connected structure of the Lewis Range and how the summits relate to one another across the landscape.