Available Weekly Reports
| Pantelleria |

There are no activity reports for Pantelleria.
Summary of eruption dates and Volcanic Explosivity Indices (VEI).
| Start Date | Stop Date | Eruption Certainty | VEI | Evidence | Activity Area or Unit |
|---|---|---|---|---|---|
| [ 1891 Dec ] | [ Unknown ] | Uncertain | South of Pantelleria | ||
| 1891 Oct 17 | 1891 Oct 25 | Confirmed | 1 | Historical | Foerstner (4 km NNW of Pantelleria) |
| [ 1831 ] | [ Unknown ] | Uncertain | Off the northern coast | ||
| 1080 BCE ± 300 years | Unknown | Confirmed | Radiocarbon (uncorrected) | Hingeline vent system | |
| 4430 BCE ± 200 years | Unknown | Confirmed | Radiocarbon (corrected) | Cuddia Randazzo | |
| 4550 BCE ± 300 years | Unknown | Confirmed | Magnetism | Serra della Fastuca | |
| 5610 BCE ± 100 years | Unknown | Confirmed | Radiocarbon (uncorrected) | Punta Tracino | |
| 6130 BCE ± 75 years | Unknown | Confirmed | Radiocarbon (uncorrected) | Cuddia Patite ? | |
| 7050 BCE (?) | Unknown | Confirmed | Potassium-Argon | Cuddia di Mida, Valenza |
The island of Pantelleria is constructed above a drowned continental rift in the Strait of Sicily and has been the locus of intensive volcano-tectonic activity. Two large Pleistocene calderas dominate the island, which contains numerous post-caldera lava domes and cinder cones and is the type locality for peralkaline rhyolitic rocks, pantellerites. The 15-km-long island is the emergent summit of a largely submarine edifice. The 6-km-wide Cinque Denti caldera, the youngest of the two calderas, formed about 45,000 years ago and contains the two post-caldera shield volcanoes of Monte Grande and Monte Gibele. Holocene eruptions have constructed pumice cones, lava domes, and short, blocky lava flows. Many Holocene vents are located on three sides of the uplifted Montagna Grande block on the SE side of the island. A submarine eruption in 1891 from a vent off the NW coast is the only confirmed historical activity.