Hallstätter Glacier

The Hallstätter Glacier is an ice mass situated at about 2,600 meters elevation on the Dachstein massif, extending across several kilometers of alpine terrain. The glacier is surrounded by steep rock walls and scree slopes that shape this part of the mountain landscape.

The glacier formed during the last ice age approximately 12,000 years ago and shaped surrounding valleys through continuous erosion over millennia. Its extent and size have visibly changed over recent decades, recording shifts in mountain climate.

Scientists and researchers frequently visit the glacier to study climate patterns and document changes in ice formation within the UNESCO World Heritage region.

Marked hiking trails lead from Hallstatt and Obertraun toward the glacier area, with mountain huts providing rest stops along the routes. Visitors should bring weatherproof clothing and sturdy footwear, as conditions at this elevation change quickly.

The meltwater has carved distinctive rock formations, including a large cauldron about 5 meters wide and spiral water channels in the underlying limestone. These erosion patterns formed over long periods and demonstrate the powerful effect of flowing water on rock layers.

Location: Hallstatt

Location: Obertraun

Elevation above the sea: 2,587 m

GPS coordinates: 47.47960,13.61130

Latest update: December 10, 2025 20:01