Briksdal Glacier
Sogn og Fjordane
Briksdal Glacier, locally known as Briksdalsbreen, is one of the most accessible and well-known arms of the Jostedalsbreen glacier, located in Stryn Municipality within Vestland county, Norway. Situated inside Jostedalsbreen National Park, the glacier lies in the Briksdalen valley at the end of Oldedalen valley, terminating in the glacial lake Briksdalsbrevatnet at 346 meters above sea level. The glacier's size fluctuates with temperature and precipitation, having experienced periods of advance and retreat throughout the 20th and 21st centuries. Notably, it expanded during the late 20th century even as other European glaciers receded, attracting international scientific interest. Since 2000, the glacier has mostly been retreating, with its front moving onto dry land by 2007, a position similar to that in the 1960s. Briksdal Glacier is celebrated for its dramatic landscape, accessible hiking routes, and the spectacular view of ice meeting water, making it a popular natural attraction in Norway.
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Tip: The best time to visit Briksdal Glacier is during summer months when hiking trails are accessible and the weather is milder. Visitors are advised to wear sturdy footwear and dress in layers due to variable mountain weather. Purchasing tickets or booking guided tours in advance can help avoid crowds. Be aware that the glacier's front position changes over time, so check current conditions before visiting. Discounts may be available for groups, seniors, or children. Guided tours provide safety and educational insights into glacial dynamics.
Interesting facts
- •Briksdal Glacier is one of the most accessible arms of the Jostedalsbreen glacier, the largest glacier in continental Europe.
- •The glacier's front has fluctuated significantly over the past century, with periods of both advance and retreat.
- •In the 1990s, Briksdal Glacier was growing while most European glaciers were shrinking, attracting international scientific interest.
- •The glacier terminates in a glacial lake, Briksdalsbrevatnet, at 346 meters above sea level.
- •Recent studies suggest the glacier's size may be the smallest since the 13th century.
History
Briksdal Glacier has been monitored since 1900, showing small advances in the early 20th century, notably in 1910 and 1929.
Between 1934 and 1951, it receded significantly, exposing the glacial lake.
From 1967 to 1997, the glacier advanced again, covering the lake entirely.
After 2000, it retreated rapidly, with the glacier front moving behind the lake by 2007.
Measurements in 2010 indicated a brief advance, but climatic conditions suggest further retreat is likely.
The glacier's size in recent decades may be the smallest since the 13th century, reflecting long-term climatic trends.
Place Guide
Briksdalsbrevatnet Lake
A small glacial lake at the terminus of Briksdal Glacier, offering stunning views of the ice meeting water and a popular spot for photography and rest during hikes.
Briksdalen Valley
The valley in which Briksdal Glacier is located, providing accessible hiking trails and natural scenery showcasing typical Norwegian fjord landscape.