Grotta delle Palombe

Grotta delle Palombe is a cave system situated beneath the Monti Rossi, containing layered chambers at different elevations. Its interior is characterized by vertical shafts that create a intricate network of passages and spaces.

The cave formed during Mount Etna's eruption in 1669, which also created the Monti Rossi formation. A documented exploration followed in 1823 when Mario Gemmellaro and John Marshall reached its lower sections.

The cave takes its name from the pigeons that once nested within its chambers, reflecting how local wildlife shaped the site's identity. Today visitors can see how volcanic forces have carved out the landscape that surrounds them.

Accessing this cave requires specialized speleological equipment and technical climbing skills due to its vertical shafts. Visitors should understand that only trained and properly equipped groups can safely explore this formation.

The cave houses scientific instruments including seismographs that monitor Etna's ongoing volcanic activity. This transforms the space into an active research site where real-time data about volcanic processes is being collected.