Lodowczyk Mięguszowiecki

Lodowczyk Mięguszowiecki is a snowpack formation in the mountains of Brzegi, situated between 1973 and 2035 meters in elevation on the slopes below Mięguszowiecka Pass. The ice surface spans about 107 meters wide and 81 meters long, sloping at about 35 degrees across the mountainside.

The snowpack was first documented in 1924 through an expedition led by Stanisław Krystyn Zaremba, who recorded detailed observations of its characteristics. Since then, it has served as a reference point for tracking changes in alpine ice formations.

Scientists and researchers regularly visit this location to study the behavior of alpine glaciers and document the effects of environmental changes.

Visitors should come prepared with sturdy equipment, as steep terrain and ice require special safety measures. The best time to explore is in late spring or early summer, when conditions are more stable.

Beneath the snowpack lies a meltwater tunnel, and a crevasse between the ice and rock walls descends about 32 meters into the earth. These hidden features reveal how active and dynamic alpine ice formations truly are.