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Alicudi Volcano

Updated: Apr 19, 2024 07:39 GMT -
Stratovolcano 675 m / 2215 ft
Eolian Islands, Italy, 38.55°N / 14.33°E
Current status: (probably) extinct (0 out of 5)

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Typical eruption style: unspecified
Alicudi volcano eruptions: None during the past 10,000 years
Less than 2.58 million years ago (Pleistocene)

Latest nearby earthquakes

TimeMag. / DepthDistance / Location
Apr 10, 11:50 am (Rome)
2.1

9.5 km
13 km (8.3 mi) to the W Italy: Tirreno Meridionale (MARE)
Info
Monday, April 8, 2024 GMT (2 quakes)
Apr 8, 01:40 pm (Rome)
1.5

7.7 km
16 km (10.2 mi) to the E Italy: Isole Eolie (Messina)
Info
Apr 8, 01:25 pm (Rome)
1.6

9.9 km
16 km (9.8 mi) to the E Italy: Isole Eolie (Messina)
Info

Background

Alicudi, in the Aeolian Island Arc, is a basaltic to andesitic stratovolcano containing a summit caldera, domes, and lava flows that formed over the course of three main stages in its eruptive history (Peccerillo, 2005). The first two stages involved basaltic to basaltic-andesitic lava flows and minor scoria and ash deposits, both followed by a summit collapse, the second of which formed the Dirittusu caldera (Peccerillo, 2005; Guest et al., 2003). Pyroclastic activity increased towards the end of the second stage (Guest et al., 2003). The third stage was dominated by andesite lava flows and the formation of domes within the summit crater and on the southeastern cone flank (Peccerillo, 2005). The youngest K-Ar date from Alicudi is 0.027-0.028 Ma, and the oldest, obtained from the lowest exposed rocks, is about 60-90 ka (Capaldi et al., 1985; Peccerillo, 2005; Guest et al., 2003).
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Smithsonian / GVP volcano information

Alicudi Volcano Photos

Latest satellite images

alicudi satellite image sat1alicudi satellite image sat2
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