Moiry Glacier, Alpine glacier in Pennine Alps, Valais, Switzerland.
Moiry Glacier is a large ice mass in the Pennine Alps that descends from high peaks toward the valleys below. The ice field displays layers of white snow and exposed blue ice, with rocky ridges breaking through the frozen surface.
This glacier was considerably larger during colder periods in the past, carving the surrounding valleys through its slow movement. Its size has changed significantly over recent decades as climate conditions have shifted.
Local mountain guides share their knowledge of Alpine glaciology with visitors through educational tours that examine the glacier's geological patterns.
Visit during summer and early fall when the trails are most accessible and weather conditions are more stable. Wear sturdy hiking boots and bring protective clothing, as mountain weather can change quickly and temperatures drop with altitude.
The meltwater from this ice mass feeds directly into Lac de Moiry, which supplies a hydroelectric system that powers the region. This connection between the glacier's natural processes and local energy production is a striking example of how mountains sustain modern infrastructure.
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