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Cupaello Volcano

Updated: 16 mayo 2024 22:00 GMT -
Pyroclastic cone 650 m / 2133 ft
Italy, 42.43°N / 12.93°E
Current status: (probably) extinct (0 out of 5)

[smaller] [larger]
Typical eruption style: unspecified
Erupciones del volcán Cupaello: None during the past 10,000 years
Less than 2.58 million years ago (Pleistocene)

Latest nearby earthquakes

Fecha / HoraRevista / Prof.Distancia / Ubicación
16 may 22:20 (Rome)
1.3

13 km
29 km al noreste Italy: 1 km NE Cittareale (RI)
Más
16 may 21:05 (Rome)
1.4

12 km
29 km al noreste Italy: 1 km NE Cittareale (RI)
Más
miércoles, 15 mayo 2024 GMT (1 sismo)
15 may 17:05 (Rome)
1.1

15 km
20 km al noroeste de L'Aquila, L'Aquila, Los Abruzos, Italia
Más
domingo, 12 mayo 2024 GMT (1 sismo)
12 may 19:30 (Rome)
1.6

8.3 km
6.2 km al sureste Italy: 3 km W Castel Sant'Angelo (RI)
Más
jueves, 9 mayo 2024 GMT (1 sismo)
9 may 20:58 (Rome)
1.2

9.1 km
18 km al este de Terni, Terni, Umbría, Italia
Más
sábado, 4 mayo 2024 GMT (1 sismo)
4 may 10:04 (Rome)
1.5

8.8 km
16 km al noreste Italy: 3 km SW Borbona (RI)
Más

Background

Cupaello is responsible for a 750-m-long lava flow that covers layers of pyroclastic material, including ash, breccias, lapilli, and scoria. These products were channelized and accumulated downslope of the volcanic edifice (Stoppa and Cundari, 1995). These pyroclastics are carbonatitic in composition, and yielded an Ar/Ar age of 639 ka (Peccerillo, 2005). However, Stoppa and Cundari (1995) list a date of about 491 +/- 3 ka. Structures within the pyroclastic layers indicate that the tuff could still deform plastically when covered by the lava, suggesting that both the explosive and effusive phases were part of the same eruption (Stoppa and Cundari, 1995).
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Smithsonian / GVP volcano information

Latest satellite images

cupaello satellite image sat1cupaello satellite image sat2
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