Briksdalsbreen

Briksdalsbreen is a glacier arm in Stryn Municipality that extends across steep mountain slopes and ends in a turquoise lake. The lake sits at about 346 meters above sea level at the valley's end.

The glacier formed at the end of the Ice Age as massive ice sheets retreated across Scandinavia. Between 1967 and 1997 it advanced by 465 meters and completely covered the lake, which set it apart among European glaciers at that time.

The glacier draws visitors who want to observe how natural forces shape ice and mountain landscapes. People come here to witness seasonal changes and weather patterns directly affecting the ice surface.

The path to the glacier starts from the parking area in Olden and follows a marked trail through the valley. Visitors should wear sturdy footwear and be prepared for changing weather, especially on windy days.

The glacier is part of Jostedalsbreen, Europe's largest continental ice mass, and responds differently to climate shifts than neighboring formations. This distinct behavior makes it a valuable spot for scientists studying how glaciers move and change.

Location: Stryn Municipality

Part of: Jostedal Glacier

GPS coordinates: 61.66583,6.89000

Latest update: January 8, 2026 17:30