Chiusa of Ceraino

Chiusa of Ceraino it is the natural bottleneck that was formed during the glacial period

Chiusa of Ceraino it is located where the Val d’Adige ends at the height of Ceraino and the rocky wall that crosses the valley furrow thus forced the glacier to bend to the right and deposit morainic debris that today form the beautiful amphitheater of Rivoli. When the glaciers withdrew the water had to look for another way of venting, so began to erode the rock wall, coming over time to dig that very suggestive furrow that we can see today.