Kjenndalsbreen, Glacier branch in Stryn Municipality, Norway
Kjenndalsbreen is a glacier branch that flows from the Jostedalsbreen system down into the Kjenndalen valley, creating prominent white ice formations. The ice descends from higher elevations and spreads across the valley floor in distinctive patterns and ridges.
The glacier advanced approximately 300 meters between 1980 and 1997 during a notable growth period. Since then, warming temperatures have caused significant ice retreat.
The glacier serves as a natural laboratory for scientists studying climate patterns and geological processes while attracting visitors from across Northern Europe.
A toll road from Loen leads to the glacier, and a short walk of about 15 minutes from the parking area reaches the viewing point. The access is straightforward, allowing visitors without specialized equipment to view the ice formations.
This is the lowest-elevation glacier branch of the Jostedalsbreen system, making it one of the most accessible ice formations in the region. The low altitude makes it a favored location for monitoring ice changes and understanding glacier dynamics.
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