Radicofani Volcano
Updated: 19 abr. 2024 15:41 GMT -
Volcanic remnant unknown
Italy, 42.87°N / 11.77°E
Current status: (probably) extinct (0 out of 5)
Italy, 42.87°N / 11.77°E
Current status: (probably) extinct (0 out of 5)
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Erupciones del volcán Radicofani: None during the past 10,000 years
Less than 2.58 million years ago (Pleistocene)
Latest nearby earthquakes
Fecha / Hora | Revista / Prof. | Distancia / Ubicación | |||
18 abr 23:50 (Rome) | 1.3 10.4 km | 1.4 km al oeste | 6.8 km al este de Abbadia San Salvatore, Siena, Toscana, Italia | Más | |
18 abr 23:28 (Rome) | 1.4 8.5 km | 2.7 km al noroeste | 5.9 km al este de Abbadia San Salvatore, Siena, Toscana, Italia | Más | |
18 abr 20:17 (Rome) | 2.5 5 km | 1.8 km al noroeste | Italy: 2 km SW Radicofani (SI) | Más |
Background
Radicofani, a part of the Tuscan Magmatic Province located within the Sierra-Radicofani Graben, is a relatively small monogenetic volcano now represented by a volcanic neck (Peccerillo, 2005; Conticello et al., 2011). Although the original edifice was a cinder cone, it is highly dissected, leaving only lava flow remnants and scoria deposits east of Monte Amiata (Peccerillo, 2005; Conticello et al., 2011). Columnar jointing is present in the middle and lower portions of the neck and large lava blocks and bombs are scattered about within several kilometers (Conticello et al., 2011). The lavas are generally basaltic-andesitic to shoshonitic in composition (Conticello et al., 2011). The lavas of the upper and lower parts of the neck have been dated to about 1.3 Ma and 1.08-1.22 Ma ago, respectively (Conticello et al., 2011; Peccerillo, 2005).---
Smithsonian / GVP volcano information