Lago di Andalo

Lake Andalo is a periodic karst lake whose changing water level can transform the basin into a meadow. At the foot of Piz Galin, it expresses a relationship between the mountain landscape and water moving beneath the surface.

Why it matters

The lake is not a permanent sheet of water with a fixed shoreline. Snowmelt and underground drainage give the same basin markedly different appearances, making seasonal change central to its character.

What to notice

Spring meltwater fills the depression through natural openings. During summer, water filters into the subsoil and the exposed bed can become flowered ground. The contrast between open water and meadow sits within the broader setting of the Brenta mountains and Paganella.

Context and history

Karst processes connect the visible basin with a less visible underground water system. The changing lake has also become part of Andalo's everyday landscape, where the water's presence or retreat continually reshapes the relationship between shore, vegetation and surrounding open ground.