BackgroundVulcano was constructed during six volcanic stages during the past 136,000 years. Two overlapping calderas, the 2.5-km-wide Caldera del Piano on the SE and the 4-km-wide Caldera della Fossa on the NW, were formed at about 100,000 and 24,000-15,000 years ago, respectively, and volcanism has migrated to the north over time.
La Fossa cone, active throughout the Holocene and the location of most of the historical eruptions of Vulcano, occupies the 3-km-wide Caldera della Fossa at the NW end of the elongated, 3 x 7 km island. The Vulcanello lava platform forms a low, roughly circular peninsula on the northern tip of Vulcano that was formed as an island beginning in 183 BC and was connected to Vulcano in about 1550 AD. Vulcanello is capped by three pyroclastic cones and was active intermittently until the 16th century. The latest eruption from Vulcano consisted of explosive activity from the Fossa cone from 1898 to 1900. Source: Smithsonian GVP
On the crater rim of La Fossa volcano, Vulcano Island (Photo: Tom Pfeiffer)
Our group on Vulcano Island (Photo: Tom Pfeiffer)
The sun is out again - on our hotel on Vulcano (Photo: Tom Pfeiffer)
Night on the beach of Porto di Ponente (Vulcano) (Photo: Tom Pfeiffer)
Vulcano volcano tours:Volcanoes of Italy - the Grand Tour (15-days study & walking tour from Vesuvius to Etna)From Stromboli to Etna (9-day walking & study tour to Stromboli, Lipari, Vulcano and Etna with our expert volcanologist)
See also: Sentinel hub | Landsat 8 | NASA FIRMS