Symphony of Horizon
Oricola-Carsoli, about 40 km SW of L'Aquila, is part of the Intra-Appenine Magmatic Province. Its mongenetic pyroclastic cones are composed of altered breccias, tuff, and surge and fall deposits. They are possibly hydrovolcanic in origin. These deposits
| Elevation | |
| Volcano Type | Pyroclastic cone(s) |
| Geologic Epoch | Pleistocene |
| Country | Italy |
| Region | Mediterranean and Western Asia |
| Subregion | Italy |
| Tectonic Setting | |
| Dominant Rock |
