BeschreibungOricola-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 were K-Ar dated at about 530 ka (Peccerillo, 2005).
Smithsonian / GVP volcano information
Siehe auch: Sentinel hub | Landsat 8 | NASA FIRMS