The term 'guje' is a local Piedmontese dialect word referring to the deep, rounded potholes or 'giant's kettles' formed by hydraulic action in riverbeds.
The Chiusella River, which feeds these pools, originates in the Gran Paradiso National Park area.
The rock formations here were sculpted over millennia by glacial meltwater and the high-velocity transport of stones during flood events.
The site remains a focal point for local geological studies regarding the erosion patterns of the Ivrea amphitheater's surrounding valleys.
The Guje di Garavot are a series of natural potholes and rock basins carved into the granite bed of the Chiusella River. Located within the Val di Chy near Ivrea, the site is known for its distinctively smooth, eroded rock formations and emerald-colored pools. The river flow creates a natural aquatic path through a wooded gorge. The site is accessible via a trail that leads down from the higher road levels into the riverbed area. The geology is defined by the crystalline rocks typical of the lower Aosta Valley and Canavese region. These basins are part of a wider network of fluvial erosion features in the area.
From the rocky vantage points overlooking the largest central pool during low-flow conditions.
Wear sturdy, closed-toe water shoes or hiking sandals with good grip for navigating slippery, wet rock surfaces.
Carry all waste back out with you, as there are no trash collection facilities on-site.
Visit during the shoulder seasons to avoid peak summer crowds and high water levels.
Do not attempt to hike the riverbed during or immediately after heavy rainfall due to the risk of sudden water level rises.
Best accessed between late spring and early autumn; trails may be inaccessible or hazardous during winter snow or heavy rains.
Avoid jumping into the pools if you are not an experienced swimmer; the water is cold and currents can be unpredictable.
