Glaciar Universidad

Glaciar Universidad is a large ice mass in the Andes mountains of the O'Higgins Region that stretches across multiple kilometers. The glacier consists of two separate basins that flow together and merge into a unified ice tongue at lower elevations.

The glacier formed over long periods through natural mountain-building processes and remains part of the Andean range. Throughout the last century, the ice mass has shifted significantly, revealing how sensitive these formations are to environmental change.

The glacier attracts researchers and students interested in climate science and mountain environments. This presence brings scientific activity to the remote peaks and helps local communities understand changes happening in their landscape.

Visitors should prepare for high altitude conditions and bring warm clothing and sturdy hiking footwear. Local guides help people navigate the remote mountain terrain and arrange visits to the ice field.

The ice field divides into two separate basins that converge at a specific elevation and form a visible tongue. This two-part structure reveals how ice flows from different sources and merges into a single mass as it descends.

Location: O'Higgins Region

Elevation above the sea: 4,478 m

GPS coordinates: -34.68722,-70.33899

Latest update: December 13, 2025 17:06